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  <channel>
    <title>Registry of Open Data on AWS</title>
    <link>https://registry.opendata.aws</link>
    <description>Recent datasets listed on the Registry of Open Data on AWS</description>
    <language>en-us</language>
    <managingEditor>opendata@amazon.com</managingEditor>
    <lastBuildDate>Tue, 09 Jun 2026 01:33:16 GMT</lastBuildDate>
    <item>
      <title>The Human Sleep Project</title>
      <link>https://registry.opendata.aws/bdsp-hsp</link>
      <guid>https://registry.opendata.aws/bdsp-hsp</guid>
      <description>The Human Sleep Project (HSP) sleep physiology dataset is a growing collection of clinical polysomnography (PSG) recordings. Beginning with PSG recordings from from ~15K patients evaluated at the Massachusetts General Hospital, the HSP will grow over the coming years to include data from &amp;gt;200K patients, as well as people evaluated outside of the clinical setting. This data is being used to develop CAISR (Complete AI Sleep Report), a collection of deep neural networks,  rule-based algorithms, and signal processing approaches designed to provide better-than-human detection of conventional PSG scoring metrics, including sleep stages, arousals, apnea and hypopnea events and their subtypes, and periodic limb movements. Beyond conventional scoring, the HSP dataset is intended to support research seeking to identify &amp;quot;hidden&amp;quot; information within the brain&amp;#39;s activity during sleep that can be used to directly measure brain health. These brain health indicators include measures of risk for common neurologic diseases, including cerebrovascular disease, and Alzheimer&amp;#39;s disease and related neurodegenerative diseases of aging; and indicators of response to therapies, including lifestyle interventions (e.g. diet, meditation, exercise) and pharmacologic interventions. These data are shared via the BDSP (Brain Data Science Platform, a resource developed by an international coalition of investigators that aggregates and harmonizes a wide range of large-scale human clinical neuroscience data to support research aimed at improving diagnosis, treatment, and prevention of neurologic disease, and promotion of brain health. The summary data provided here are released for the benefit of the wider scientific community without restriction on use.</description>
    </item>
    <item>
      <title>Common Crawl</title>
      <link>https://registry.opendata.aws/commoncrawl</link>
      <guid>https://registry.opendata.aws/commoncrawl</guid>
      <description>A corpus of web crawl data composed of over 300 billion web pages.</description>
    </item>
    <item>
      <title>The Cancer Genome Atlas</title>
      <link>https://registry.opendata.aws/tcga</link>
      <guid>https://registry.opendata.aws/tcga</guid>
      <description>The Cancer Genome Atlas (TCGA), a collaboration between the National Cancer Institute (NCI) and National Human Genome Research Institute (NHGRI), aims to generate comprehensive, multi-dimensional maps of the key genomic changes in major types and subtypes of cancer. TCGA has analyzed matched tumor and normal tissues from 11,000 patients, allowing for the comprehensive characterization of 33 cancer types and subtypes, including 10 rare cancers.
The dataset contains open Clinical Supplement, Biospecimen Supplement, RNA-Seq Gene Expression Quantification, miRNA-Seq Isoform Expression Quantification, miRNA Expression Quantification, Genotyping Array Copy Number Segment, Genotyping Array Masked Copy Number Segment, Genotyping Array Gene Level Copy Number Scores, and WXS Masked Somatic Mutation data from Genomic Data Commons (GDC).
This dataset also contains controlled Whole Exome Sequencing (WXS), RNA-Seq, miRNA-Seq, ATAC-Seq Aligned Reads, WXS Annotated Somatic Mutation, WXS Raw Somatic Mutation, and WXS Aggregated Somatic Mutation data from GDC.
TCGA is made available on AWS via the &lt;a href&#x3D;&quot;https://aws.amazon.com/blogs/publicsector/aws-and-national-institutes-of-health-collaborate-to-accelerate-discoveries-with-strides-initiative/&quot;&gt;NIH STRIDES Initiative&lt;/a&gt;.</description>
    </item>
    <item>
      <title>CCRS MODIS albedo over Canada | Albédo MODIS du CCT couvrant le Canada</title>
      <link>https://registry.opendata.aws/ccrsmodisalbedo</link>
      <guid>https://registry.opendata.aws/ccrsmodisalbedo</guid>
      <description>Times series of 10-day spectral and broadband albedo products derived at 250-m spatial resolution over Canadian territory and neighboring areas produced at the Canada Centre for Remote Sensing (CCRS) since February 2000 using MODIS L1B C6.1 swath imagery as input. The imagery for all spectral bands was downscaled and re-projected into the Lambert Conformal Conic (LCC) projection at 250-m spatial resolution.  The area size is 5,700 km x 4,800 km (22,800 pixel x 19,200 lines).
Séries temporelles de produits d’albédo spectral et à large bande générés à des intervalles de 10 jours avec une résolution spatiale de 250 m, couvrant le territoire canadien et les régions voisines. Ces produits sont élaborés par le Centre canadien de télédétection (CCT) depuis février 2000 à partir des images MODIS L1B C6.1. Les images de toutes les bandes spectrales ont été rééchantillonnées et reprojetées en projection conforme de Lambert (LCC) à une résolution spatiale de 250 m. La zone couverte est d’environ 5 700 km par 4 800 km (22 800 pixels par 19 200 lignes).</description>
    </item>
    <item>
      <title>Foldingathome COVID-19 Datasets</title>
      <link>https://registry.opendata.aws/foldingathome-covid19</link>
      <guid>https://registry.opendata.aws/foldingathome-covid19</guid>
      <description>&lt;a href&#x3D;&quot;http://foldingathome.org&quot;&gt;Folding@home&lt;/a&gt; is a massively distributed computing project that uses biomolecular simulations to investigate the &lt;a href&#x3D;&quot;https://foldingathome.org/diseases/&quot;&gt;molecular origins of disease&lt;/a&gt; and accelerate the discovery of new therapies. Run by the &lt;a href&#x3D;&quot;https://foldingathome.org/about/the-foldinghome-consortium/&quot;&gt;Folding@home Consortium&lt;/a&gt;, a worldwide network of research laboratories focusing on a variety of different diseases, Folding@home seeks to address problems in human health on a scale that is infeasible by another other means, sharing the results of these large-scale studies with the research community through &lt;a href&#x3D;&quot;https://foldingathome.org/papers-results/&quot;&gt;peer-reviewed publications&lt;/a&gt; and publicly shared datasets. During the &lt;a href&#x3D;&quot;https://en.wikipedia.org/wiki/Coronavirus_disease_2019&quot;&gt;COVID-19 epidemic&lt;/a&gt;, Folding@home focused its resources on understanding the vulnerabilities in &lt;a href&#x3D;&quot;https://en.wikipedia.org/wiki/Severe_acute_respiratory_syndrome_coronavirus_2&quot;&gt;SARS-CoV-2&lt;/a&gt;, the virus that causes COVID-19 disease, and working closely with a number of experimental collaborators to accelerate progress toward effective therapies for treating COVID-19 and ending the pandemic. In the process, it created the world&amp;#39;s first &lt;a href&#x3D;&quot;https://doi.org/10.1101/2020.06.27.175430&quot;&gt;exascale distributed computing resource&lt;/a&gt;, enabling it to generate valuable scientific datasets of unprecedented size. More information about Folding@home&amp;#39;s COVID-19 research activities at the &lt;a href&#x3D;&quot;https://foldingathome.org/diseases/infectious-diseases/covid-19/&quot;&gt;Folding@home COVID-19 page&lt;/a&gt;. In addition to working directly with experimental collaborators and rapidly sharing new research findings through preprint servers, Folding@home has joined other researchers in committing to &lt;a href&#x3D;&quot;https://doi.org/10.1021/acs.jcim.0c00319&quot;&gt;rapidly share all COVID-19 research data&lt;/a&gt;, and has joined forces with &lt;a href&#x3D;&quot;https://aws.amazon.com/&quot;&gt;AWS&lt;/a&gt; and the &lt;a href&#x3D;&quot;http://molssi.org&quot;&gt;Molecular Sciences Software Institute (MolSSI)&lt;/a&gt; to share datasets of unprecedented side through the &lt;a href&#x3D;&quot;https://registry.opendata.aws/&quot;&gt;AWS Open Data Registry&lt;/a&gt;, indexing these massive datasets via the &lt;a href&#x3D;&quot;https://covid.molssi.org/&quot;&gt;MolSSI COVID-19 Molecular Structure and Therapeutics Hub&lt;/a&gt;. The complete index of all Folding@home datasets can be found &lt;a href&#x3D;&quot;https://covid.molssi.org//org-contributions/#folding--home&quot;&gt;here&lt;/a&gt;. This repository contains several major datasets from this effort and comprises the single largest collection of molecular simulation data ever released.</description>
    </item>
    <item>
      <title>Sentinel-2</title>
      <link>https://registry.opendata.aws/sentinel-2</link>
      <guid>https://registry.opendata.aws/sentinel-2</guid>
      <description>The &lt;a href&#x3D;&quot;https://sentinel.esa.int/web/sentinel/missions/sentinel-2&quot;&gt;Sentinel-2 mission&lt;/a&gt; is
a land monitoring constellation of two satellites that provide high resolution
optical imagery and provide continuity for the current SPOT and Landsat missions.
The mission provides a global coverage of the Earth&amp;#39;s land surface every 5 days,
making the data of great use in on-going studies. L1C data are available from
June 2015 globally. L2A data are available from November 2016 over Europe
region and globally since January 2017.</description>
    </item>
    <item>
      <title>Therapeutically Applicable Research to Generate Effective Treatments (TARGET)</title>
      <link>https://registry.opendata.aws/target</link>
      <guid>https://registry.opendata.aws/target</guid>
      <description>Therapeutically Applicable Research to Generate Effective Treatments (TARGET) is the collaborative effort of a large, diverse consortium of extramural and NCI investigators. The goal of the effort is to accelerate molecular discoveries that drive the initiation and progression of hard-to-treat childhood cancers and facilitate rapid translation of those findings into the clinic.
TARGET projects provide comprehensive molecular characterization to determine the genetic changes that drive the initiation and progression of childhood cancers.The dataset contains open Clinical Supplement, Biospecimen Supplement, RNA-Seq Gene Expression Quantification, miRNA-Seq Isoform Expression Quantification, miRNA-Seq miRNA Expression Quantification data from Genomic Data Commons (GDC), and open data from GDC Legacy Archive.</description>
    </item>
    <item>
      <title>USGS Landsat</title>
      <link>https://registry.opendata.aws/usgs-landsat</link>
      <guid>https://registry.opendata.aws/usgs-landsat</guid>
      <description>This joint NASA/USGS program provides the longest continuous space-based record of 
Earth’s land in existence. Every day, Landsat satellites provide essential information 
to help land managers and policy makers make wise decisions about our resources and our environment.
Data is provided for Landsats 1, 2, 3, 4, 5, 7, 8, and 9 (excludes Landsat 6).As of June 28, 2023 (&lt;a href&#x3D;&quot;https://www.usgs.gov/landsat-missions/news/changes-coming-landsats-simple-notification-service-amazon-web-service&quot;&gt;announcement&lt;/a&gt;),
the previous single SNS topic &lt;code&gt;arn:aws:sns:us-west-2:673253540267:public-c2-notify&lt;/code&gt; was replaced with
three new SNS topics for different types of scenes.</description>
    </item>
    <item>
      <title>Allen Cell Imaging Collections</title>
      <link>https://registry.opendata.aws/allen-cell-imaging-collections</link>
      <guid>https://registry.opendata.aws/allen-cell-imaging-collections</guid>
      <description>This bucket contains multiple datasets (as Quilt packages) created by the Allen Institute for Cell Science. The types of data included in this bucket are listed below:&lt;ol&gt;
&lt;li&gt;Field of view or cropped images of cells&lt;/li&gt;
&lt;li&gt;Segmentations of structures in the images (e.g., boundaries of cells, DNA, other intracellular structures, etc.)&lt;/li&gt;
&lt;li&gt;Processed versions of the above images and segmentations&lt;/li&gt;
&lt;li&gt;Machine learning predictions and labels of the data listed above&lt;/li&gt;
&lt;li&gt;Models trained on the previously listed data&lt;/li&gt;
&lt;li&gt;Additional supporting non-image data related to the above listed data types (e.g., gene expression data, whole genome sequencing data, features derived from the images or model predictions, metadata)&lt;/li&gt;
&lt;li&gt;Simulation, analysis, and visualization data of in silico cell structures, cells, and cell populations&lt;/li&gt;
&lt;/ol&gt;
External funding:The generation of some datasets was supported by the National Human Genome Research Institute of the National Institutes under Award Number UM1HG011593. The content is solely the responsibility of the authors and does not necessarily represent the official views of the National Institutes of Health.</description>
    </item>
    <item>
      <title>Sudachi Language Resources</title>
      <link>https://registry.opendata.aws/sudachi</link>
      <guid>https://registry.opendata.aws/sudachi</guid>
      <description>Japanese dictionaries and pre-trained models (word embeddings and language models) for natural language processing.
&lt;a href&#x3D;&quot;https://github.com/WorksApplications/SudachiDict&quot;&gt;SudachiDict&lt;/a&gt; is the dictionary for a Japanese tokenizer (morphological analyzer) &lt;a href&#x3D;&quot;https://github.com/WorksApplications/Sudachi&quot;&gt;Sudachi&lt;/a&gt;.
&lt;a href&#x3D;&quot;https://github.com/WorksApplications/chiVe&quot;&gt;chiVe&lt;/a&gt; is Japanese pretrained word embeddings (word vectors), trained using the ultra-large-scale web corpus NWJC by National Institute for Japanese Language and Linguistics, analyzed by Sudachi.
&lt;a href&#x3D;&quot;https://github.com/WorksApplications/SudachiTra&quot;&gt;chiTra&lt;/a&gt; is a library for using large-scale pre-trained language models with the Japanese tokenizer SudachiPy.</description>
    </item>
    <item>
      <title>CELLxGENE Discover Census</title>
      <link>https://registry.opendata.aws/biohub-cellxgene-census</link>
      <guid>https://registry.opendata.aws/biohub-cellxgene-census</guid>
      <description>CELLxGENE Discover (&lt;a href&#x3D;&quot;https://cellxgene.cziscience.com/&quot;&gt;cellxgene.cziscience.com&lt;/a&gt;) is a free-to-use platform for the exploration, analysis, and retrieval of single-cell data. CELLxGENE Discover hosts the largest aggregation of standardized single-cell data from the major human and mouse tissues, with modalities that include gene expression, chromatin accessibility, DNA methylation, and spatial transcriptomics.
This year, CELLxGENE Discover has made available all of its human and mouse RNA single-cell data through Census (&lt;a href&#x3D;&quot;https://chanzuckerberg.github.io/cellxgene-census/&quot;&gt;https://chanzuckerberg.github.io/cellxgene-census/&lt;/a&gt;) – a free-to-use service with an API and data that allows for querying its single-cell data corpus directly from Python or R. 
The API uses a new technology, TileDB-SOMA, that allows for efficient and low-latency querying. The data are fully standardized and hosted publicly for free access, and they are composed by a count matrix of tens of millions of cells (observations) by &amp;gt;60 k genes (features) accompanied by standard cell metadata variables (e.g. cell type, tissue, sequencing technology, donor id, etc)  and gene metadata that includes GENCODE-based IDs and gene names. While these data are built from hundreds of datasets, the APIs enable convenient cell- and gene-based filtering to obtain any slice of interest in a matter of seconds. All data can be quickly transformed to NumPy, Pandas, Anndata, Seurat, or R base objects. We created data loaders for the data to be directly used by PyTorch for modeling at scale.
In addition, all the source dataset files in H5AD format are also available for retrieval. </description>
    </item>
    <item>
      <title>Gabriella Miller Kids First Pediatric Research Program (Kids First)</title>
      <link>https://registry.opendata.aws/kids-first</link>
      <guid>https://registry.opendata.aws/kids-first</guid>
      <description>The NIH Common Fund&amp;#39;s Gabriella Miller Kids First Pediatric Research Program’s (“Kids First”) vision is to “alleviate suffering from childhood cancer and structural birth defects by fostering collaborative research to uncover the etiology of these diseases and by supporting data sharing within the pediatric research community.” The program continues to generate and share whole genome sequence data from thousands of children affected by these conditions, ranging from rare pediatric cancers, such as osteosarcoma, to more prevalent diagnoses, such as congenital heart defects. In 2018, Kids First launched the Gabriella Miller Kids First Data Resource Center, charged with building a large-scale data platform supporting clinical and genetic data from these patients and their families in order to accelerate discovery and ultimately clinical impact. Researchers can search, access, aggregate, and analyze these data through the Kids First Data Resource Portal. Additionally, by using cloud-based individual workspaces in CAVATICA, a data analysis and sharing computation platform, researchers can cross-analyze Kids First data with data from other efforts, such as NCI’s TARGET program and consortia-based datasets like the Children’s Brain Tumor Tissue Consortium (CBTTC).
Kids First is made available on AWS via the &lt;a href&#x3D;&quot;https://aws.amazon.com/blogs/publicsector/aws-and-national-institutes-of-health-collaborate-to-accelerate-discoveries-with-strides-initiative/&quot;&gt;NIH STRIDES Initiative&lt;/a&gt;.</description>
    </item>
    <item>
      <title>NOAA Geostationary Operational Environmental Satellites (GOES) 16, 17, 18 &amp; 19</title>
      <link>https://registry.opendata.aws/noaa-goes</link>
      <guid>https://registry.opendata.aws/noaa-goes</guid>
      <description>&lt;br/&gt;
&lt;br/&gt; 
NEW GOES-19 Data!! On April 4, 2025 at 1500 UTC, the GOES-19 satellite will be declared the Operational GOES-East satellite. All products and services, including NODD, for GOES-East will transition to GOES-19 data at that time. GOES-19 will operate out of the GOES-East location of 75.2°W starting on April 1, 2025 and through the operational transition. Until the transition time and during the final stretch of Post Launch Product Testing (PLPT), GOES-19 products are considered non-operational regardless of their validation maturity level. Shortly following the transition of GOES-19 to GOES-East, all data distribution from GOES-16 will be turned off. GOES-16 will drift to the storage location at 104.7°W. GOES-19 data should begin flowing again on April 4th once this maneuver is complete. 
&lt;br/&gt;
&lt;br/&gt;
NEW GOES 16 Reprocess Data!! The reprocessed GOES-16 ABI L1b data mitigates systematic data issues (including data gaps and image artifacts) seen in the Operational products, and improves the stability of both the radiometric and geometric calibration over the course of the entire mission life. These data were produced by recomputing the L1b radiance products from input raw L0 data using improved calibration algorithms and look-up tables, derived from data analysis of the NIST-traceable, on-board sources. In addition, the reprocessed data products contain enhancements to the L1b file format, including limb pixels and pixel timestamps, while maintaining compatibility with the operational products. The datasets currently available span the operational life of GOES-16 ABI, from early 2018 through the end of 2024. The Reprocessed L1b dataset shows improvement over the Operational L1b products but may still contain data gaps or discrepancies. Please provide feedback to Dan Lindsey (dan.lindsey@noaa.gov) and Gary Lin (guoqing.lin-1@nasa.gov). More information can be found in the [GOES-R ABI Reprocess User Guide](https://github.com/NOAA-Big-Data-Program/nodd-data-docs/blob/main/GOES/GOES-R_ABI_Reprocessed_L1b_User_Guide-v1.1.pdf).
&lt;br/&gt;
&lt;br/&gt;  
NOTICE: As of January 10th 2023, GOES-18 assumed the GOES-West position and all data files are deemed both operational and provisional, so no ‘preliminary, non-operational’ caveat is needed. GOES-17 is now offline, shifted approximately 105 degree West, where it will be in on-orbit storage. GOES-17 data will no longer flow into the GOES-17 bucket. Operational GOES-West products can be found in the GOES-18 bucket. 
&lt;br/&gt;
&lt;br/&gt; 
GOES satellites (GOES-16, GOES-17, GOES-18 &amp; GOES-19) provide continuous weather imagery and
monitoring of meteorological and space environment data across North America.
GOES satellites provide the kind of continuous monitoring necessary for
intensive data analysis. They hover continuously over one position on the surface.
The satellites orbit high enough to allow for a full-disc view of the Earth. Because
they stay above a fixed spot on the surface, they provide a constant vigil for the
atmospheric &quot;triggers&quot; for severe weather conditions such as tornadoes, flash floods,
hailstorms, and hurricanes. When these conditions develop, the GOES satellites are able
to monitor storm development and track their movements. SUVI products available in both NetCDF and FITS. 
</description>
    </item>
    <item>
      <title>Sentinel-2 Cloud-Optimized GeoTIFFs</title>
      <link>https://registry.opendata.aws/sentinel-2-l2a-cogs</link>
      <guid>https://registry.opendata.aws/sentinel-2-l2a-cogs</guid>
      <description>The &lt;a href&#x3D;&quot;https://sentinel.esa.int/web/sentinel/missions/sentinel-2&quot;&gt;Sentinel-2 mission&lt;/a&gt; is
a land monitoring constellation of two satellites that provide high resolution
optical imagery and provide continuity for the current SPOT and Landsat missions.
The mission provides a global coverage of the Earth&amp;#39;s land surface every 5 days,
making the data of great use in ongoing studies.
This dataset is the same as the &lt;a href&#x3D;&quot;https://registry.opendata.aws/sentinel-2/&quot;&gt;Sentinel-2&lt;/a&gt;
dataset, except the JP2K files were converted into Cloud-Optimized GeoTIFFs (COGs).
Additionally, SpatioTemporal Asset Catalog metadata has were in a JSON file
alongside the data, and a STAC API called &lt;a href&#x3D;&quot;https://earth-search.aws.element84.com/v1&quot;&gt;Earth-search&lt;/a&gt;
is freely available to search the archive. This dataset contains all of the scenes in the
original Sentinel-2 Public Dataset and will grow as that does.
L2A data are available from April 2017 over wider Europe region and globally since December 2018.</description>
    </item>
    <item>
      <title>Terrain Tiles</title>
      <link>https://registry.opendata.aws/terrain-tiles</link>
      <guid>https://registry.opendata.aws/terrain-tiles</guid>
      <description>A global dataset providing bare-earth terrain heights, tiled for easy usage and provided on S3.</description>
    </item>
    <item>
      <title>NASA Prediction of Worldwide Energy Resources (POWER)</title>
      <link>https://registry.opendata.aws/nasa-power</link>
      <guid>https://registry.opendata.aws/nasa-power</guid>
      <description>NASA&amp;#39;s goal in Earth science is to observe, understand, and model the Earth system to discover how it is changing, to better predict change, and to understand the consequences for life on Earth. The Applied Sciences Program, within the Earth Science Division of the NASA Science Mission Directorate, serves individuals and organizations around the globe by expanding and accelerating societal and economic benefits derived from Earth science, information, and technology research and development.&lt;br/&gt;&lt;br/&gt;
The &lt;a href&#x3D;&quot;https://power.larc.nasa.gov/&quot;&gt;Prediction Of Worldwide Energy Resources (POWER)&lt;/a&gt; Project, funded through the Applied Sciences Program at NASA Langley Research Center, gathers NASA Earth observation data and parameters related to the fields of surface solar irradiance and meteorology to serve the public in several free, easy-to-access and easy-to-use methods. POWER helps communities become resilient amid observed climate variability by improving data accessibility, aiding research in energy development, building energy efficiency, and supporting agriculture projects.&lt;br/&gt;&lt;br/&gt;
The POWER project contains over 380 satellite-derived meteorology and solar energy Analysis Ready Data (ARD) at four temporal levels: hourly, daily, monthly, and climatology. The POWER data archive provides data at the native resolution of the source products. The data is updated nightly to maintain near real time availability (2-3 days for meteorological parameters and 5-7 days for solar). The POWER services catalog consists of a series of RESTful Application Programming Interfaces, geospatial enabled image services, and web mapping Data Access Viewer. These three service offerings support data discovery, access, and distribution to the project’s user base as ARD and as direct application inputs to decision support tools.&lt;br/&gt;&lt;br/&gt;
The latest data version update includes hourly-based source ARD, in addition to enhanced daily, monthly, annual, and climatology data. The daily time series for meteorology is available from 1981, while solar-based parameters start in 1984. The hourly source data are from Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) and Global Modeling and Assimilation Office (GMAO), spanning from 1984 for meteorology and from 2001 for solar-based parameters. The hourly data equips users with the ARD needed to model building system energy performance, providing information directly amenable to decision support tools introducing the industry standard EnergyPlus Weather file format.&lt;br/&gt;&lt;br/&gt;</description>
    </item>
    <item>
      <title>NEXRAD on AWS</title>
      <link>https://registry.opendata.aws/noaa-nexrad</link>
      <guid>https://registry.opendata.aws/noaa-nexrad</guid>
      <description>Real-time and archival data from the Next Generation Weather Radar (NEXRAD) network.
&lt;br&gt;&lt;h4&gt;Update&lt;/h4&gt;
The NEXRAD Level II archive data is moving to a new bucket: &lt;code&gt;unidata-nexrad-level2&lt;/code&gt; 
and SNS topic: &lt;code&gt;arn:aws:sns:us-east-1:684042711724:NewNEXRADLevel2Archive&lt;/code&gt;. The old
bucket and SNS topic are now deprecated and will no longer be available starting September 1, 2025.
&lt;br&gt;&lt;br&gt;
</description>
    </item>
    <item>
      <title>1000 Genomes Phase 3 Reanalysis with DRAGEN 3.5, 3.7, 4.0, 4.2, and 4.4</title>
      <link>https://registry.opendata.aws/ilmn-dragen-1kgp</link>
      <guid>https://registry.opendata.aws/ilmn-dragen-1kgp</guid>
      <description>&lt;b&gt; Overview &lt;/b&gt;&lt;p&gt;This dataset contains alignment files and small variant (includes single nucleotide variants (SNV) and indels), copy number variant (CNV), short tandem repeat (i.e., repeat expansion; STR), structural variant (SV) and other variant call files from the &lt;a href&#x3D;&quot;https://www.internationalgenome.org/&quot;&gt;1000 Genomes Project (1KGP) Phase 3 dataset&lt;/a&gt; (3,202 individuals, 602 trios) using Illumina DRAGEN v3.5.7b, v3.7.6, v4.0.3, v4.2.7, and v4.4.7 software.
All DRAGEN analyses were performed in the cloud using the &lt;a href&#x3D;&quot;https://www.illumina.com/products/by-type/informatics-products/connected-analytics.html&quot;&gt;Illumina Connected Analytics&lt;/a&gt; bioinformatics platform powered by Amazon Web Services (see &lt;a href&#x3D;&quot;https://www.illumina.com/science/genomics-research/articles/data-solution-empowering-population-genomics-research.html&quot;&gt;&amp;#39;Data solution empowering population genomics&amp;#39;&lt;/a&gt; for more information).
The v3.7.6, v4.2.7, and v4.4.7 datasets include results from trio small variant, &lt;em&gt;de novo&lt;/em&gt; structural variant, and &lt;em&gt;de novo&lt;/em&gt; copy number variant calls on 602 trio families comprised of members from the 1KGP Phase 3 dataset.
Trio repeat expansion calling was included in the v3.7.6 dataset only.
Joint cohort analysis was also performed on the entire 1KGP sample dataset for the v3.7.6, v4.0.3, v4.2.7, and v4.4.7 re-analyses using &lt;a href&#x3D;&quot;https://www.illumina.com/products/by-type/informatics-products/dragen-secondary-analysis/iterative-GVCF-genotyper.html&quot;&gt;DRAGEN Iterative gVCF Genotyper&lt;/a&gt; v3.8.3, v4.2.0, v4.2.7, v4.4.7, respectively (see &lt;a href&#x3D;&quot;https://www.illumina.com/science/genomics-research/articles/gVCF-Genotyper.html&quot;&gt;&amp;#39;Genotyping variants at population scale using DRAGEN gVCF Genotyper&amp;#39;&lt;/a&gt; and &lt;a href&#x3D;&quot;https://help.dragen.illumina.com/product-guide/dragen-v4.4/dragen-dna-pipeline/iterative-gvcf-genotyper&quot;&gt;&amp;#39;Population Genotyping&amp;#39;&lt;/a&gt;).&lt;b&gt; DRAGEN Versions &lt;/b&gt;&lt;p&gt;&lt;h5 id&#x3D;&quot;v37&quot;&gt;v3.7&lt;/h5&gt;
&lt;a href&#x3D;&quot;https://support.illumina.com/content/dam/illumina-support/documents/documentation/software_documentation/dragen-bio-it/Illumina-DRAGEN-Bio-IT-Platform-User-Guide-1000000141465-00.pdf&quot;&gt;User Guide&lt;/a&gt; | &lt;a href&#x3D;&quot;https://www.illumina.com/content/dam/illumina-support/documents/downloads/software/dragen/release-notes/Illumina-DRAGEN-Bio-IT-Platform-3.7-Release-Notes-1000000142362-v00.pdf&quot;&gt;Release Notes&lt;/a&gt;Improvements and new features in the v3.7.6 individual samples analyses include &lt;em&gt;CYP2D6&lt;/em&gt; variant calling (see &amp;#39;&lt;a href&#x3D;&quot;https://www.illumina.com/science/genomics-research/articles/CYP21A2.html&quot;&gt;Overcoming high homology to detect variation in CYP21A2 with whole-genome sequencing in DRAGEN&lt;/a&gt;&amp;#39;) and joint detection and use of graph-based hg19 and hg38 reference hash tables (see &lt;a href&#x3D;&quot;https://www.illumina.com/science/genomics-research/dragen-wins-precisionfda-challenge-showcase-accuracy-gains.html&quot;&gt;&amp;#39;DRAGEN Wins at PrecisionFDA Truth Challenge V2 Showcase Accuracy Gains from Alt-aware Mapping and Graph Reference Genomes&amp;#39;&lt;/a&gt; and &lt;a href&#x3D;&quot;https://www.illumina.com/science/genomics-research/articles/dragen-demystifying-reference-genomes.html&quot;&gt;&amp;#39;Demystifying the versions of GRCh38/hg38 reference genomes, how they are used in DRAGEN and their impact on accuracy&amp;#39;&lt;/a&gt; for details).&lt;h5 id&#x3D;&quot;v40&quot;&gt;v4.0&lt;/h5&gt;
&lt;a href&#x3D;&quot;https://support-docs.illumina.com/SW/DRAGEN_v40/Content/SW/FrontPages/DRAGEN.htm&quot;&gt;User Guide&lt;/a&gt; | &lt;a href&#x3D;&quot;https://support.illumina.com/content/dam/illumina-support/documents/downloads/software/dragen/release-notes/200024449_01_DRAGEN-4.0-Customer-Release-Notes.pdf&quot;&gt;Release Notes&lt;/a&gt;The DRAGEN v4.0.3 dataset features improved small variant calling accuracy due to utilization of a newly integrated &lt;a href&#x3D;&quot;https://support-docs.illumina.com/SW/dragen_v42/Content/SW/DRAGEN/ml_for_vc.htm?Highlight&#x3D;dragen-ml&quot;&gt;machine learning functionality&lt;/a&gt; with an updated graph based reference for difficult to map regions (see &lt;a href&#x3D;&quot;https://www.illumina.com/science/genomics-research/articles/dragen-shines-again-precisionfda-truth-challenge-v2.html&quot;&gt;&amp;#39;DRAGEN Sets New Standard for Data Accuracy in PrecisionFDA Benchmark Data. Optimizing Variant Calling Performance with Illumina Machine Learning and DRAGEN Graph&amp;#39;&lt;/a&gt;); accuracy and runtime improvements in the SV caller; new targeted callers including &lt;em&gt;CYP2B6&lt;/em&gt;, &lt;em&gt;GBA&lt;/em&gt;, &lt;em&gt;SMN&lt;/em&gt; and a Star Allele PGx caller; and an expanded catalog for use with Expansion Hunter STR caller.&lt;h5 id&#x3D;&quot;v42&quot;&gt;v4.2&lt;/h5&gt;
&lt;a href&#x3D;&quot;https://support-docs.illumina.com/SW/dragen_v42/Content/SW/FrontPages/DRAGEN.htm&quot;&gt;User Guide&lt;/a&gt; | &lt;a href&#x3D;&quot;https://support.illumina.com/content/dam/illumina-support/documents/downloads/software/dragen/release-notes/200040845_02_DRAGEN-4.2-Customer-Release-Notes.pdf&quot;&gt;Release Notes&lt;/a&gt;DRAGEN v4.2.7 offers significant accuracy improvements in small variant, CNV, and SV calling, includes new targeted callers (&lt;em&gt;HBA&lt;/em&gt;, &lt;em&gt;LPA&lt;/em&gt;, &lt;em&gt;RH&lt;/em&gt;, &lt;em&gt;CYP21A2&lt;/em&gt;, &lt;em&gt;SMN&lt;/em&gt; silent carrier variant), and supports Star Allele calling for five additional pharmacogenes (&lt;em&gt;BCHE&lt;/em&gt;, &lt;em&gt;ABCG2&lt;/em&gt;, &lt;em&gt;NAT2&lt;/em&gt;, &lt;em&gt;F5&lt;/em&gt;, and &lt;em&gt;UGT2B17&lt;/em&gt;).
These are further improved by upgraded machine learning models.
See &lt;a href&#x3D;&quot;https://developer.illumina.com/news-updates/dragen-4-2-enhanced-machine-learning-new-targeted-callers-and-more&quot;&gt;DRAGEN 4.2: Enhanced machine learning, new targeted callers, and more&lt;/a&gt; for further details on these and other enchancements.&lt;h5 id&#x3D;&quot;v44&quot;&gt;v4.4&lt;/h5&gt;
&lt;a href&#x3D;&quot;https://help.dragen.illumina.com/product-guide/dragen-v4.4&quot;&gt;User Guide&lt;/a&gt; | &lt;a href&#x3D;&quot;https://www.illumina.com/content/dam/illumina-support/documents/downloads/software/dragen/release-notes/200068065_00_DRAGEN-4_4_4-Customer-Release-Notes.pdf&quot;&gt;Release Notes&lt;/a&gt;DRAGEN v4.4.7 boosts the speed and accuracy of all callers via the official release of an optimized pangenome graph reference (&amp;#39;&lt;a href&#x3D;&quot;https://www.illumina.com/science/genomics-research/articles/second-gen-multigenome-mapping.html&quot;&gt;The quest for accuracy gains in the dark regions of the genomes: Presenting the DRAGEN multigenome mapper and pangenome reference updates in version 4.3&lt;/a&gt;&amp;#39;).
Namely, SV calling accuracy is substantially increased via the implementation of a multigenome mapper capable of exploiting the power of a pangenome reference.
Runtime is further reduced by supporting AWS F2 EC2 instances (&lt;a href&#x3D;&quot;https://aws.amazon.com/blogs/hpc/enabling-rapid-genomic-and-multiomic-data-analysis-with-illumina-dragen-v4-4-on-amazon-ec2-f2-instances/&quot;&gt;Enabling Rapid Genomic and Multiomic Data Analysis with Illumina DRAGEN™ v4.4 on Amazon EC2 F2 Instances&lt;/a&gt;)&lt;b&gt; Annotation &lt;/b&gt;&lt;p&gt;Starting with the v4.0.3 reanalysis, annotation using the Illumina Connected Annotations (also known as Illumina Annotation Engine or Nirvana) was included as part of the analysis (see &lt;a href&#x3D;&quot;https://help.dragen.illumina.com/product-guide/dragen-v4.4/nirvana&quot;&gt;Illumina Connected Annotations documentation&lt;/a&gt; for more information).
For the v4.0.3, v4.2.7, and v4.4.7 datasets, annotation was performed on the merged small variant VCF generated by the DRAGEN Iterative gVCF Genotyper for the entire 1KGP cohort.
For v4.2.7 and v4.4.7, annotation was also performed on the merged CNV, SV, and STR VCFs for the entire cohort.</description>
    </item>
    <item>
      <title>Cell Painting Gallery</title>
      <link>https://registry.opendata.aws/cellpainting-gallery</link>
      <guid>https://registry.opendata.aws/cellpainting-gallery</guid>
      <description>The Cell Painting Gallery is a collection of image datasets created using the &lt;a href&#x3D;&quot;https://pubmed.ncbi.nlm.nih.gov/27560178/&quot;&gt;Cell Painting&lt;/a&gt; assay. 
The images of cells are captured by microscopy imaging, and reveal the response of various labeled cell components to whatever treatments are tested, which can include genetic perturbations, chemicals or drugs, or different cell types. 
The datasets can be used for diverse applications in basic biology and pharmaceutical research, such as identifying disease-associated phenotypes, understanding disease mechanisms, and predicting a drug’s activity, toxicity, or mechanism of action (&lt;a href&#x3D;&quot;https://carpenter-singh-lab.broadinstitute.org/files/anne/files/141_Chandrasekaran_NatRevDrugDiscov_2020.pdf&quot;&gt;Chandrasekaran et al 2020&lt;/a&gt;). 
This collection is maintained by the &lt;a href&#x3D;&quot;https://carpenter-singh-lab.broadinstitute.org/&quot;&gt;Carpenter–Singh lab&lt;/a&gt; and the &lt;a href&#x3D;&quot;https://cimini-lab.broadinstitute.org/&quot;&gt;Cimini lab&lt;/a&gt; at the &lt;a href&#x3D;&quot;https://www.broadinstitute.org/&quot;&gt;Broad Institute&lt;/a&gt;.
A human-friendly listing of datasets, instructions for accessing them, and other documentation is at the &lt;a href&#x3D;&quot;https://github.com/broadinstitute/cellpainting-gallery&quot;&gt;corresponding GitHub page&lt;/a&gt; about the Gallery.</description>
    </item>
    <item>
      <title>Inter-mission Time Series of Land Ice Velocity and Elevation (ITS_LIVE)</title>
      <link>https://registry.opendata.aws/its-live-data</link>
      <guid>https://registry.opendata.aws/its-live-data</guid>
      <description>The Inter-mission Time Series of Land Ice Velocity and Elevation (ITS_LIVE) project has a singular mission: to accelerate ice sheet and glacier research by producing globally comprehensive, high resolution, low latency, temporally dense, multi-sensor records of land ice and ice shelf change while minimizing barriers between the data and the user.
ITS_LIVE data currently consists of NetCDF Level 2 scene-pair ice flow products posted to a standard 120 m grid derived from Landsat 4/5/7/8/9, Sentinel-2 optical scenes, and Sentinel-1 SAR scenes. We have processed all land-ice intersecting image pairs separated by ≤546 days for optical and ≤12 for SAR sensors, for all missions from each mission start to the end of 2022.
The ITS_LIVE project will continue processing new optical and radar scene pairs as they come in, and will soon increase production to include SAR image pairs separated by more than 12 days. We also expect to extend processing to include ASTER, RADARSAT, and NISAR imagery. Further, all scene pair data are combined into a set of Zarr datacubes that are cloud-optimized for time-series analysis, with a suite of user tools available to query the data effectively.
The ITS_LIVE project is also producing a suite of Level 3 products, including quarterly and annual ice-sheet and regional velocity mosaics as Cloud-Optimized GeoTIFFs, standardized records of elevation change rates for Greenland and Antarctica, and ice shelf and tidewater glacier front positions.
For more information about the ITS_LIVE project, please see &lt;a href&#x3D;&quot;https://its-live.jpl.nasa.gov/&quot;&gt;https://its-live.jpl.nasa.gov/&lt;/a&gt;.</description>
    </item>
    <item>
      <title>MERRA-2 tavg1_2d_slv_Nx: 2d,1-Hourly,Time-Averaged,Single-Level,Assimilation,Single-Level Diagnostics 0.625 x 0.5 degree</title>
      <link>https://registry.opendata.aws/nasa-m2t1nxslv</link>
      <guid>https://registry.opendata.aws/nasa-m2t1nxslv</guid>
      <description>M2T1NXSLV (or  tavg1_2d_slv_Nx) is an hourly time-averaged 2-dimensional data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2).  This collection consists of meteorology diagnostics at popularly used vertical levels, such as air temperature at 2-meter (or at 10-meter, 850hPa, 500 hPa, 250hPa), wind components at 50-meter (or at 2-meter, 10-meter, 850 hPa, 500hPa, 250 hPa), sea level pressure, surface pressure, and total precipitable water vapor (or ice water, liquid water).  The data field is time-stamped with the central time of an hour starting from 00:30 UTC, e.g.: 00:30, 01:30, … , 23:30 UTC.MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4.  The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing:  Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page.  Note that a reprocessed data filename is different from the original file.MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#100;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#100;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list.Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;,  “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page.  If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#108;&amp;#x2d;&amp;#104;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#108;&amp;#x2d;&amp;#104;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#118;&lt;/a&gt;).
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>ESA WorldCover</title>
      <link>https://registry.opendata.aws/esa-worldcover-vito</link>
      <guid>https://registry.opendata.aws/esa-worldcover-vito</guid>
      <description>The European Space Agency (ESA) WorldCover product provides global land cover maps for 2020 &amp;amp; 2021 at 10 m resolution based on Copernicus Sentinel-1 and Sentinel-2 data. The WorldCover product comes with 11 land cover classes and has been generated in the framework of the ESA WorldCover project, part of the 5th Earth Observation Envelope Programme (EOEP-5) of the European Space Agency. A first version of the product (v100), containing the 2020 map was released in October 2021. The 2021 map was released in October 2022 using an improved algorithm (v200). The WorldCover 2020 and 2021 maps were generated with different algorithm versions and therefore changes between the maps should be treated with caution as these contain both real land cover changes as well as changes due to the used algorithms.</description>
    </item>
    <item>
      <title>Genome Aggregation Database (gnomAD)</title>
      <link>https://registry.opendata.aws/broad-gnomad</link>
      <guid>https://registry.opendata.aws/broad-gnomad</guid>
      <description>The Genome Aggregation Database (gnomAD) is a resource developed by an international coalition of investigators that aggregates and harmonizes both exome and genome data from a wide range of large-scale human sequencing projects. The summary data provided here are released for the benefit of the wider scientific community without restriction on use.
The v4.1 data set (GRCh38) spans 730,947 exome sequences and 76,215 whole-genome sequences from unrelated individuals, of &lt;a href&#x3D;&quot;https://gnomad.broadinstitute.org/stats#diversity&quot;&gt;diverse ancestries&lt;/a&gt;, sequenced sequenced as part of various disease-specific and population genetic studies.
The gnomAD Principal Investigators and team can be found &lt;a href&#x3D;&quot;https://gnomad.broadinstitute.org/team&quot;&gt;here&lt;/a&gt;, and the groups that have contributed data to the current release are listed &lt;a href&#x3D;&quot;https://gnomad.broadinstitute.org/about&quot;&gt;here&lt;/a&gt;.
Sign up for the gnomAD mailing list &lt;a href&#x3D;&quot;http://broad.io/gnomad_list&quot;&gt;here&lt;/a&gt;.</description>
    </item>
    <item>
      <title>GeoNet Aotearoa New Zealand Data</title>
      <link>https://registry.opendata.aws/geonet</link>
      <guid>https://registry.opendata.aws/geonet</guid>
      <description>GeoNet provides geological hazard information for Aotearoa New Zealand. This dataset contains data and products recorded by the GeoNet sensor network. &lt;br /&gt; &lt;br /&gt; GNSS (Global Navigation Satellite System) data include raw data in proprietary and Receiver Independent Exchange Format (RINEX) and local tie-in survey conducted during equipment changes, more details can be found on &lt;a href&#x3D;&quot;https://www.geonet.org.nz/data/types/geodetic&quot;&gt;the GeoNet geodetic page&lt;/a&gt; website. &lt;br /&gt; Coastal gauge data include relative measurement of sea level measured by tsunami monitoring gauges. Raw and quality control data are provided in CREX format (Character Form for the Representtion and eXchange of metereological data), more details can be found on &lt;a href&#x3D;&quot;https://www.geonet.org.nz/data/types/tidal_gauges&quot;&gt;the GeoNet coastal tsunami monitoring gauges page&lt;/a&gt;. &lt;br /&gt; Camera images data include webcam images from the GeoNet Volcano monitoring network and Built Environment Instrumentation Programme, more details can be found on &lt;a href&#x3D;&quot;https://www.geonet.org.nz/data/types/camera&quot;&gt;the GeoNet camera page&lt;/a&gt;. &lt;br /&gt; Waveform data include raw data from weak and strong motion instruments of the GeoNet seismic networks, more details can be found on &lt;a href&#x3D;&quot;https://www.geonet.org.nz/data/types/seismic_waveforms&quot;&gt;the GeoNet seismic waveform page&lt;/a&gt;. &lt;br /&gt; Seismic data products include strong motion derived data, more details can be found on &lt;a href&#x3D;&quot;https://strongmotion.geonet.org.nz&quot;&gt;the GeoNet Strong Motion products page&lt;/a&gt;. &lt;br /&gt; Time Series data products include derived time series data from a subgroup of the GeoNet sensor network. Data are in compressed comma separated format (csv.gz), more details can be found on &lt;a href&#x3D;&quot;https://tilde.geonet.org.nz/ui/data-exploration&quot;&gt;the GeoNet tilde website page&lt;/a&gt;. &lt;br /&gt; &lt;br /&gt;</description>
    </item>
    <item>
      <title>MERRA-2 inst3_3d_aer_Nv: 3d,3-Hourly,Instantaneous,Model-Level,Assimilation,Aerosol Mixing Ratio 0.625 x 0.5 degree</title>
      <link>https://registry.opendata.aws/nasa-m2i3nvaer</link>
      <guid>https://registry.opendata.aws/nasa-m2i3nvaer</guid>
      <description>M2I3NVAER (or  inst3_3d_aer_Nv) is an instantaneous 3-dimensional 3-hourly data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2).  This collection consists of assimilations of aerosol mixing ratio parameters at 72 model layers, such as dust, sulphur dioxide, sea salt, black carbon, and organic carbon.  The data field is available every three hour starting from 00:00 UTC, e.g.: 00:00, 03:00, … , 21:00 UTC. Section 4.2 of the MERRA-2 File Specification document provides pressure values nominal for a 1000 hPa surface pressure and refers to the top edge of the layer. The lev&#x3D;1 is for the top layer, and lev&#x3D;72 is for the bottom (or surface) model layer. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4.  The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing:  Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page.  Note that a reprocessed data filename is different from the original file.MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#111;&amp;#118;&quot;&gt;&amp;#103;&amp;#115;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#111;&amp;#118;&lt;/a&gt;) to be added to the list.Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;,  “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page.  If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#x76;&lt;/a&gt;).
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>MERRA-2 inst3_3d_asm_Np: 3d,3-Hourly,Instantaneous,Pressure-Level,Assimilation,Assimilated Meteorological Fields</title>
      <link>https://registry.opendata.aws/nasa-m2i3npasm</link>
      <guid>https://registry.opendata.aws/nasa-m2i3npasm</guid>
      <description>M2I3NPASM (or  inst3_3d_asm_Np) is an instantaneous 3-dimensional 3-hourly data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2).  This collection consists of assimilations of meteorological parameters at 42 pressure levels, such as  temperature, wind components, vertical pressure velocity, water vapor, ozone mass mixing ratio, and layer height. The data field is available every three hours starting from 00:00 UTC, e.g.:  00:00, 03:00, … , 21:00 UTC. The information on the pressure levels can be found in the section 4.2 of the MERRA-2 File Specification document.  MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4.  The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing:  Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page.  Note that a reprocessed data filename is different from the original file.MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#100;&amp;#105;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#100;&amp;#105;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;) to be added to the list.Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;,  “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page.  If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#x64;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#x64;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#x76;&lt;/a&gt;).
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>MERRA-2 inst3_3d_asm_Nv: 3d,3-Hourly,Instantaneous,Model-Level,Assimilation,Assimilated Meteorological Fields 0.625 x 0.5 degree</title>
      <link>https://registry.opendata.aws/nasa-m2i3nvasm</link>
      <guid>https://registry.opendata.aws/nasa-m2i3nvasm</guid>
      <description>M2I3NVASM (or  inst3_3d_asm_Nv) is an instantaneous 3-dimensional 3-hourly data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2).  This collection consists of assimilations of meteorological parameters at 72 model layers, such as temperature, wind components, vertical pressure velocity, water vapor, and layer height.  The data field is available every three hour starting from 00:00 UTC, e.g.:  00:00, 03:00, … , 21:00 UTC. Section 4.2 of the MERRA-2 File Specification document provides pressure values nominal for a 1000 hPa surface pressure and refers to the top edge of the layer. The lev&#x3D;1 is for the top layer, and lev&#x3D;72 is for the bottom (or surface) model layer. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4.  The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing:  Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page.  Note that a reprocessed data filename is different from the original file.MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#99;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#45;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#64;&amp;#109;&amp;#x61;&amp;#x69;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#99;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#45;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#64;&amp;#109;&amp;#x61;&amp;#x69;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list.Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;,  “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page.  If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#108;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#108;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;).
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>NOAA Joint Polar Satellite System (JPSS)</title>
      <link>https://registry.opendata.aws/noaa-jpss</link>
      <guid>https://registry.opendata.aws/noaa-jpss</guid>
      <description>&lt;em&gt;Near Real Time JPSS data is now flowing! See bucket information on the right side of this page to access products!&lt;/em&gt; &lt;br /&gt; Satellites in the JPSS constellation gather global measurements of atmospheric, terrestrial and oceanic conditions, including sea and land surface temperatures, vegetation, clouds, rainfall, snow and ice cover, fire locations and smoke plumes, atmospheric temperature, water vapor and ozone. JPSS delivers key observations for the Nation&amp;#39;s essential products and services, including forecasting severe weather like hurricanes, tornadoes and blizzards days in advance, and assessing environmental hazards such as droughts, forest fires, poor air quality and harmful coastal waters. Further, JPSS will provide continuity of critical, global observations of Earth’s atmosphere, oceans and land through 2038.</description>
    </item>
    <item>
      <title>SpaceNet</title>
      <link>https://registry.opendata.aws/spacenet</link>
      <guid>https://registry.opendata.aws/spacenet</guid>
      <description>SpaceNet, launched in August 2016 as an open innovation project offering a repository of freely available
imagery with co-registered map features. Before SpaceNet, computer vision researchers had minimal options
to obtain free, precision-labeled, and high-resolution satellite imagery. Today, SpaceNet hosts datasets
developed by its own team, along with data sets from projects like IARPA’s Functional Map of the World (fMoW).</description>
    </item>
    <item>
      <title>The Singapore Nanopore Expression Data Set</title>
      <link>https://registry.opendata.aws/sgnex</link>
      <guid>https://registry.opendata.aws/sgnex</guid>
      <description>The Singapore Nanopore Expression (SG-NEx) project is an international collaboration to generate reference transcriptomes and a comprehensive benchmark data set for long read Nanopore RNA-Seq. Transcriptome profiling is done using PCR-cDNA sequencing (PCR-cDNA), amplification-free cDNA sequencing (direct cDNA), direct sequencing of native RNA (direct RNA), and short read RNA-Seq. The SG-NEx core data includes 5 of the most commonly used cell lines and it is extended with additional cell lines and samples that cover a broad range of human tissues. All core samples are sequenced with at least 3 high quality replicates. For a subset of samples spike-in RNAs are used and matched m6A profiling data is available.</description>
    </item>
    <item>
      <title>2021 Amazon Last Mile Routing Research Challenge Dataset</title>
      <link>https://registry.opendata.aws/amazon-last-mile-challenges</link>
      <guid>https://registry.opendata.aws/amazon-last-mile-challenges</guid>
      <description>The 2021 Amazon Last Mile Routing Research Challenge was an innovative research initiative led by Amazon.com and supported by the Massachusetts Institute of Technology’s Center for Transportation and Logistics. Over a period of 4 months, participants were challenged to develop innovative machine learning-based methods to enhance classic optimization-based approaches to solve the travelling salesperson problem, by learning from historical routes executed by Amazon delivery drivers. The primary goal of the Amazon Last Mile Routing Research Challenge was to foster innovative applied research in route planning, building on recent advances in predictive modeling, and using a real-world problem and data. The dataset released for the research challenge includes route-, stop-, and package-level features for 9,184 historical routes performed by Amazon drivers in 2018 in five metropolitan areas in the United States. This real-world dataset excludes any personally identifiable information (all route and package identifiers have been randomly regenerated and related location data have been obfuscated to ensure anonymity). Although multiple synthetic benchmark datasets are available in the literature, the dataset of the 2021 Amazon Last Mile Routing Research Challenge is the first large and publicly available dataset to include instances based on real-world operational routing data. The dataset is fully described and formally introduced in the following Transportation Science article: &lt;a href&#x3D;&quot;https://pubsonline.informs.org/doi/10.1287/trsc.2022.1173&quot;&gt;https://pubsonline.informs.org/doi/10.1287/trsc.2022.1173&lt;/a&gt;</description>
    </item>
    <item>
      <title>Distributed Archives for Neurophysiology Data Integration (DANDI)</title>
      <link>https://registry.opendata.aws/dandiarchive</link>
      <guid>https://registry.opendata.aws/dandiarchive</guid>
      <description>DANDI is a public archive of neurophysiology datasets, including raw and processed data,
and associated software containers. Datasets are shared according to Creative Commons
CC0 or CC-BY licenses. This US BRAIN Initiative supported archive provides a broad range
of cellular neurophysiology data including intracellular and extracellular electrophysiology,
optophysiology, calcium imaging, fiber photometry, behavioral time-series, and images from
immunostaining experiments, from over 20 species.Data is organized using community standards:
&lt;a href&#x3D;&quot;https://www.nwb.org/nwb-neurophysiology/&quot;&gt;NWB - Neurodata Without Borders&lt;/a&gt;,
&lt;a href&#x3D;&quot;https://bids.neuroimaging.io/&quot;&gt;BIDS - Brain Imaging Data Structure&lt;/a&gt;,
&lt;a href&#x3D;&quot;https://ngff.openmicroscopy.org/&quot;&gt;NGFF - Next Generation File Format&lt;/a&gt; for Zarr-based imaging data, and
&lt;a href&#x3D;&quot;http://nidm.nidash.org/&quot;&gt;NIDM - Neuro Imaging Data Model&lt;/a&gt;.The S3 bucket is organized as follows:&lt;ul&gt;
&lt;li&gt;&lt;strong&gt;dandisets/&lt;/strong&gt; - Metadata and manifests for each Dandiset version; manifests reference keys
under blobs/ or zarrs/ for actual data. See &lt;a href&#x3D;&quot;https://github.com/dandi/schema/&quot;&gt;DANDI schema&lt;/a&gt;
for manifest format specifications.&lt;/li&gt;
&lt;li&gt;&lt;strong&gt;blobs/&lt;/strong&gt; - Deduplicated binary data (NWB files) indexed by content hash.&lt;/li&gt;
&lt;li&gt;&lt;strong&gt;zarrs/&lt;/strong&gt; - Zarr arrays for large imaging datasets.&lt;/li&gt;
&lt;/ul&gt;
Development of DANDI is supported by the National Institute of Mental Health.</description>
    </item>
    <item>
      <title>Digital Earth Africa Global Mangrove Watch</title>
      <link>https://registry.opendata.aws/deafrica-mangrove</link>
      <guid>https://registry.opendata.aws/deafrica-mangrove</guid>
      <description>The Global Mangrove Watch (GMW) dataset is a result of the collaboration between Aberystwyth University (U.K.), solo Earth Observation (soloEO; Japan), Wetlands International the World Conservation Monitoring Centre (UNEP-WCMC) and the Japan Aerospace Exploration Agency (JAXA). The primary objective of producing this dataset is to provide countries lacking a national mangrove monitoring system with first cut mangrove extent and change maps, to help safeguard against further mangrove forest loss and degradation.
The Global Mangrove Watch dataset (version 2) consists of a global baseline map of mangroves for 2010 and changes from this baseline for six epochs i.e. 1996, 2007, 2008, 2009, 2015 and 2016. Annual maps are planned from 2018 and onwards. The dataset can be used to identify mangrove ecosystems and monitor changes in mangrove extent. This is important in applications such as quantifying ‘blue carbon’, mitigating risks from natural disasters, and prioritising restoration activities. For more information on the Global Watch Mangrove product see the Global Mangrove Watch website.</description>
    </item>
    <item>
      <title>Digital Earth Africa Landsat Collection 2 Level 2</title>
      <link>https://registry.opendata.aws/deafrica-landsat</link>
      <guid>https://registry.opendata.aws/deafrica-landsat</guid>
      <description>Digital Earth Africa (DE Africa) provides free and open access to a copy of Landsat Collection 2 Level-2 products over Africa. These products are produced and provided by the United States Geological Survey (USGS).
The Landsat series of Earth Observation satellites, jointly led by USGS and NASA, have been continuously acquiring images of the Earth’s land surface since 1972. DE Africa provides data from Landsat 5, 7 and 8 satellites, including historical observations dating back to late 1980s and regularly updated new acquisitions.
New Level-2 Landsat 7 and Landsat 8 data are available after 15 to 27 days from acquisition. See Landsat Collection 2 Generation Timeline for details.
USGS Landsat Collection 2 was released early 2021 and offers improved processing, geometric accuracy, and radiometric calibration compared to previous Collection 1 products. The Level-2 products are endorsed by the Committee on Earth Observation Satellites (CEOS) to be Analysis Ready Data for Land (CARD4L)-compliant. This internationally recognized certification ensures these products have been processed to a minimum set of requirements and organized into a form that allows immediate analysis with a minimum of additional user effort and interoperability both through time and with other datasets.</description>
    </item>
    <item>
      <title>Fly Brain Anatomy: FlyLight Gen1 and Split-GAL4 Imagery</title>
      <link>https://registry.opendata.aws/janelia-flylight</link>
      <guid>https://registry.opendata.aws/janelia-flylight</guid>
      <description>This data set, made available by Janelia&amp;#39;s FlyLight project, consists of fluorescence images 
of Drosophila melanogaster driver lines, aligned to standard templates, and stored in formats 
suitable for rapid searching in the cloud. Additional data will be added as it is published. </description>
    </item>
    <item>
      <title>RADIANT Public Data</title>
      <link>https://registry.opendata.aws/radiant</link>
      <guid>https://registry.opendata.aws/radiant</guid>
      <description>The Real-time Analysis and Discovery in Integrated And Networked Technologies (RADIANT) initiative seeks to develop an extensible, federated framework for rapid exchange of  multimodal clinical and research data on behalf of accelerated discovery and patient impact. Coordination and implementation of initial RADIANT deployments will leverage a network of  more than 35 partnered health care systems and participating patient families within the  Children’s Brain Tumor Network (CBTN) and the Pediatric Neuro-Oncology Consortium (PNOC).  This data set is composed of public multi-modal data provisioned by RADIANT. The initial bolus of data is from CBTN and consists of clinical data extracted/abstracted from  electronic medical records, omic data such as genomics, transcriptomics and proteomics and radiology and pathology imaging data. Data are collected or generated as part of consent-based,  IRB-approved observational or interventional studies with the goal of making it available globally to researchers across a broad number of disciplines. </description>
    </item>
    <item>
      <title>Digital Earth Africa - Copernicus Global Land Service - Lake Water Quality</title>
      <link>https://registry.opendata.aws/deafrica-clgm-lwq</link>
      <guid>https://registry.opendata.aws/deafrica-clgm-lwq</guid>
      <description>The Copernicus Global Land Service – Lake Water Quality products offer a comprehensive, satellite-derived monitoring system for assessing key water quality indicators in major large lakes, typically those greater than 50 hectares. These datasets are generated using optical satellite sensors, primarily Sentinel-2 MSI and Sentinel-3 OLCI, with earlier archives derived from Envisat MERIS. Spanning multiple spatial resolutions (100 m and 300 m) and temporal scales (10-day composites), they support both near-real-time and retrospective assessments of inland water quality.Key parameters include surface reflectance, turbidity, total suspended matter (TSM), chlorophyll-a concentration, trophic state index, and floating cyanobacteria risk—all essential for monitoring eutrophication, ecological health, and harmful algal blooms (HABs). The datasets cover the period from 2002 to the present, providing long-term continuity for environmental monitoring and scientific research, with focused coverage in Europe and Africa.All products are delivered using standardized geospatial grids (EPSG:4326) and include quality flags, detailed metadata, and validation against in situ observations to ensure reliability. Continuous improvements across product versions—such as enhanced atmospheric correction and updated retrieval algorithms—have significantly improved accuracy and usability. In addition, comprehensive user manuals, technical documentation, and support materials are available, making the data highly accessible to researchers, policymakers, and environmental managers.Digital Earth Africa (DE Africa) hosts these datasets for the African region, providing free and open access to both the data and associated tools.</description>
    </item>
    <item>
      <title>Digital Earth Africa CHIRPS Rainfall</title>
      <link>https://registry.opendata.aws/deafrica-chirps</link>
      <guid>https://registry.opendata.aws/deafrica-chirps</guid>
      <description>Digital Earth Africa (DE Africa) provides free and open access to a copy of the Climate Hazards Group InfraRed Precipitation with Station data (CHIRPS) monthly and daily products over Africa. The CHIRPS rainfall maps are produced and provided by the Climate Hazards Center in collaboration with the US Geological Survey, and use both rain gauge and satellite observations.
The CHIRPS-2.0 Africa Monthly dataset is regularly indexed to DE Africa from the CHIRPS monthly data. The CHIRPS-2.0 Africa Daily dataset is likewise indexed from the CHIRPS daily data. Both products have been converted to cloud-opitmized GeoTIFFs, and can be accessed through DE Africa’s Open Data Cube. This means the full archive of CHIRPS daily and monthly rainfall can be easily used for inspection or analysis across DE Africa platforms, including the user-interactive DE Africa Map.
For more information on the dataset, see the &lt;a href&#x3D;&quot;https://www.chc.ucsb.edu/data/chirps&quot;&gt;CHIRPS website&lt;/a&gt;.</description>
    </item>
    <item>
      <title>Digital Earth Africa Coastlines</title>
      <link>https://registry.opendata.aws/deafrica-coastlines</link>
      <guid>https://registry.opendata.aws/deafrica-coastlines</guid>
      <description>Africa&amp;#39;s long and dynamic coastline is subject to a wide range of pressures, including extreme weather and climate, sea level rise and human development. Understanding how the coastline responds to these pressures is crucial to managing this region, from social, environmental and economic perspectives.
The Digital Earth Africa Coastlines (provisional) is a continental dataset that includes annual shorelines and rates of coastal change along the entire African coastline from 2000 to the present.
The product combines satellite data from the Digital Earth Africa program with tidal modelling to map the typical location of the coastline at mean sea level for each year. The product enables trends of coastal erosion and growth to be examined annually at both a local and continental scale, and for patterns of coastal change to be mapped historically and updated regularly as data continues to be acquired. This allows current rates of coastal change to be compared with that observed in previous years or decades.
The ability to map shoreline positions for each year provides valuable insights into whether changes to the coastline are the result of particular events or actions, or a process of more gradual change over time. This information can enable scientists, managers and policy makers to assess impacts from the range of drivers impacting the coastlines and potentially assist planning and forecasting for future scenarios.</description>
    </item>
    <item>
      <title>Digital Earth Africa GeoMAD</title>
      <link>https://registry.opendata.aws/deafrica-geomad</link>
      <guid>https://registry.opendata.aws/deafrica-geomad</guid>
      <description>GeoMAD is the Digital Earth Africa (DE Africa) surface reflectance geomedian and triple Median Absolute Deviation data service. It is a cloud-free composite of satellite data compiled over specific timeframes.
The geomedian component combines measurements collected over the specified timeframe to produce one representative, multispectral measurement for every pixel unit of the African continent. The end result is a comprehensive dataset that can be used to generate true-colour images for visual inspection of anthropogenic or natural landmarks. The full spectral dataset can be used to develop more complex algorithms.
For each pixel, invalid data is discarded, and remaining observations are mathematically summarised using the geomedian statistic. Flyover coverage provided by collecting data over a period of time also helps scope intermittently cloudy areas.
Variations between the geomedian and the individual measurements are captured by the three Median Absolute Deviation (MAD) layers. These are higher-order statistical measurements calculating variation relative to the geomedian. The MAD layers can be used on their own or together with geomedian to gain insights about the land surface, and understand change over time.
Calculating GeoMAD over different timeframes and sensors provides a range of insights to the environment. An annual timeframe allows better correction for cloud cover and reduces artifacts for comparison over multiple years. A semiannual timeframe, for example six-month blocks, better captures seasonal variation within one year, but can also be used to compare equivalent periods from different years. Likewise, Landsat sensors allows full utility of the surface reflectance archive dating back to 1984, while more recent Sentinel-2 data provides higher-frequency flyovers and better resolution.
The Digital Earth Africa GeoMAD service currently provides annual and six-month semiannual datasets, with separate services for Landsat and Sentinel-2 sensors.</description>
    </item>
    <item>
      <title>Digital Earth Africa Sentinel-2 Level-2A Surface Reflectance Collection 1</title>
      <link>https://registry.opendata.aws/deafrica-sentinel-2-c1</link>
      <guid>https://registry.opendata.aws/deafrica-sentinel-2-c1</guid>
      <description>The Sentinel-2 mission is part of the European Union Copernicus programme for Earth observations. Sentinel-2 consists of twin satellites, Sentinel-2A (launched 23 June 2015) and Sentinel-2B (launched 7 March 2017). The two satellites have the same orbit, but 180° apart for optimal coverage and data delivery. Their combined data is used in the Digital Earth Africa Sentinel-2 product.
Together, they cover all Earth’s land surfaces, large islands, inland and coastal waters every 3-5 days.
Sentinel-2 data is tiered by level of pre-processing. Level-0, Level-1A and Level-1B data contain raw data from the satellites, with little to no pre-processing. Level-1C data is surface reflectance measured at the top of the atmosphere. This is processed using the Sen2Cor algorithm to give Level-2A, the bottom-of-atmosphere reflectance (Obregón et al, 2019). Level-2A data is the most ideal for research activities as it allows further analysis without applying additional atmospheric corrections.
Digital Earth Africa Sentinel-2 Level-2A Surface Reflectance Collection 1 is the Sentinel-2 product processed for enhanced calibration and consistent time series between Sentinel-2A and Sentinel-2B. Digital Earth Africa does not host any lower-level Sentinel-2 data.Note that this data is a subset of the Sentinel-2 COGs dataset.</description>
    </item>
    <item>
      <title>Digital Earth Africa Water Observations from Space</title>
      <link>https://registry.opendata.aws/deafrica-wofs</link>
      <guid>https://registry.opendata.aws/deafrica-wofs</guid>
      <description>Water Observations from Space (WOfS) is a service that draws on satellite imagery to provide historical surface water observations of the whole African continent. WOfS allows users to understand the location and movement of inland and coastal water present in the African landscape. It shows where water is usually present; where it is seldom observed; and where inundation of the surface has been observed by satellite.
They are generated using the WOfS classification algorithm on Landsat satellite data. There are several WOfS products available for the African continent including scene-level data and annual or all time summaries.</description>
    </item>
    <item>
      <title>International Neuroimaging Data-Sharing Initiative (INDI)</title>
      <link>https://registry.opendata.aws/fcp-indi</link>
      <guid>https://registry.opendata.aws/fcp-indi</guid>
      <description>This bucket contains multiple neuroimaging datasets that are part of the International Neuroimaging Data-Sharing Initiative. Raw human and non-human primate neuroimaging data include 1) Structural MRI; 2) Functional MRI; 3) Diffusion Tensor Imaging; 4) Electroencephalogram (EEG)
In addition to the raw data, preprocessed data is also included for some datasets.
A complete list of the available datasets can be seen in the documentation lonk provided below. </description>
    </item>
    <item>
      <title>Low Altitude Disaster Imagery (LADI) Dataset</title>
      <link>https://registry.opendata.aws/ladi</link>
      <guid>https://registry.opendata.aws/ladi</guid>
      <description>The Low Altitude Disaster Imagery (LADI) Dataset consists of human and machine annotated airborne images collected by the Civil Air Patrol in support of various disaster responses from 2015-2023. Two key distinctions are the low altitude, oblique perspective of the imagery and disaster-related features, which are rarely featured in computer vision benchmarks and datasets.</description>
    </item>
    <item>
      <title>Maxar Open Data Program</title>
      <link>https://registry.opendata.aws/maxar-open-data</link>
      <guid>https://registry.opendata.aws/maxar-open-data</guid>
      <description>Pre and post event high-resolution satellite imagery in support of emergency planning, risk assessment, 
monitoring of staging areas and emergency response, damage assessment, and recovery. These images are generated
using the &lt;a href&#x3D;&quot;https://ard.maxar.com/docs&quot;&gt;Maxar ARD&lt;/a&gt; pipeline, tiled on an organized grid in analysis-ready
cloud-optimized formats.</description>
    </item>
    <item>
      <title>NOAA Operational Forecast System (OFS)</title>
      <link>https://registry.opendata.aws/noaa-ofs</link>
      <guid>https://registry.opendata.aws/noaa-ofs</guid>
      <description>ANNOUNCEMENTS: [NOS OFS Version Updates and Implementation of Upgraded Oceanographic Forecast Modeling Systems for Lakes Superior and Ontario; Effective October 25, 2022}(&lt;a href&#x3D;&quot;https://www.weather.gov/media/notification/pdf2/scn22-91_nos_loofs_lsofs_v3.pdf&quot;&gt;https://www.weather.gov/media/notification/pdf2/scn22-91_nos_loofs_lsofs_v3.pdf&lt;/a&gt;)
&lt;br/&gt;
&lt;br/&gt;
For decades, mariners in the United States have depended on NOAA&amp;#39;s Tide Tables for the best estimate of expected water levels. These tables provide accurate predictions of the astronomical tide (i.e., the change in water level due to the gravitational effects of the moon and sun and the rotation of the Earth); however, they cannot predict water-level changes due to wind, atmospheric pressure, and river flow, which are often significant.
&lt;br/&gt;
&lt;br/&gt;
The National Ocean Service (NOS) has the mission and mandate to provide guidance and information to support navigation and coastal needs. To support this mission, NOS has been developing and implementing hydrodynamic model-based &lt;a href&#x3D;&quot;https://tidesandcurrents.noaa.gov/forecast_info.html&quot;&gt;Operational Forecast Systems&lt;/a&gt;. 
&lt;br/&gt;
&lt;br/&gt;
This forecast guidance provides oceanographic information that helps mariners safely navigate their local waters. This national network of hydrodynamic models provides users with operational nowcast and forecast guidance (out to 48 – 120 hours) on parameters such as water levels, water temperature, salinity, and currents. These forecast systems are implemented in critical ports, harbors, estuaries, Great Lakes and coastal waters of the United States, and form a national backbone of real-time data, tidal predictions, data management and operational modeling.
&lt;br/&gt;
&lt;br/&gt;
Nowcasts and forecasts are scientific predictions about the present and future states of water levels (and possibly currents and other relevant oceanographic variables, such as salinity and temperature) in a coastal area. These predictions rely on either observed data or forecasts from a numerical model. A nowcast incorporates recent (and often near real-time) observed meteorological, oceanographic, and/or river flow rate data. A nowcast covers the period from the recent past (e.g., the past few days) to the present, and it can make predictions for locations where observational data are not available. A forecast incorporates meteorological, oceanographic, and/or river flow rate forecasts and makes predictions for times where observational data will not be available. A forecast is usually initiated by the results of a nowcast.
&lt;br/&gt;
&lt;br/&gt;
OFS generally runs four times per day (every 6 hours) on NOAA&amp;#39;s Weather and Climate Operational Supercomputing Systems (WCOSS) in a standard Coastal Ocean Modeling Framework (COMF) developed by the &lt;a href&#x3D;&quot;https://tidesandcurrents.noaa.gov/&quot;&gt;Center for Operational Oceanographic Products and Services (CO-OPS)&lt;/a&gt;. COMF is a set of standards and tools for developing and maintaining NOS’s hydrodynamic model–based operational forecast systems. The goal of COMF is to provide a standard and comprehensive software infrastructure to enhance ease of use, performance, portability, and interoperability of NOS’s operational forecast systems.
&lt;br/&gt;
&lt;br/&gt;</description>
    </item>
    <item>
      <title>Open Targets</title>
      <link>https://registry.opendata.aws/opentargets</link>
      <guid>https://registry.opendata.aws/opentargets</guid>
      <description>The Open Targets Platform is a comprehensive data integration tool that supports systematic identification and prioritisation of potential therapeutic drug targets. By integrating publicly available datasets including data generated by the Open Targets experimental and informatics research programmes, the Platform provides data and services to assist in the task of therapeutic hypothesis building.</description>
    </item>
    <item>
      <title>The Cancer Dependency Map (DepMap) Cancer Cell Line Encyclopedia (CCLE) Dataset</title>
      <link>https://registry.opendata.aws/depmap-omics-ccle</link>
      <guid>https://registry.opendata.aws/depmap-omics-ccle</guid>
      <description>This dataset consists of whole genome sequencing (WGS), whole exome sequencing (WES), and RNA sequencing files generated from ~1000 cancer cell lines described in Ghandi et al., 2019.</description>
    </item>
    <item>
      <title>Alliance of Genome Resources</title>
      <link>https://registry.opendata.aws/alliance-genome-resources</link>
      <guid>https://registry.opendata.aws/alliance-genome-resources</guid>
      <description>The Alliance of Genome Resources is a consortium that integrates genomic, genetic, and molecular data from leading model organism databases including Drosophila melanogaster, Caenorhabditis elegans, Danio rerio (zebrafish), Mus musculus (mouse), Rattus norvegicus (rat), Saccharomyces cerevisiae (yeast), Xenopus laevis and Xenopus tropicalis (frogs), and human reference data. The Alliance provides comprehensive datasets including gene annotations, disease associations, expression data (bulk and single-cell RNA-Seq), protein and genetic interactions, orthology relationships, variants and alleles, and complete genome sequences with annotations. Data is organized into Alliance-wide integrated datasets and organism-specific collections, supporting comparative genomics, disease modeling, and functional genomics research.</description>
    </item>
    <item>
      <title>CBERS on AWS</title>
      <link>https://registry.opendata.aws/cbers</link>
      <guid>https://registry.opendata.aws/cbers</guid>
      <description>Imagery acquired
by the China-Brazil Earth Resources Satellite (CBERS), 4 and 4A.
The
image files are recorded and processed by Instituto Nacional de Pesquisas
Espaciais (INPE) and are converted to Cloud Optimized Geotiff
format in order to optimize its use for cloud based applications.
Contains all CBERS-4 MUX, AWFI, PAN5M and
PAN10M scenes acquired since
the start of the satellite mission and is daily updated with
new scenes.
CBERS-4A MUX Level 4 (Orthorectified) scenes are being
ingested starting from 04-13-2021. CBERS-4A WFI Level 4 (Orthorectified)
scenes are being ingested starting from 10-12-2022.
CBERS-4A WPM Level 4 (Orthorectified) scenes are being ingested starting from 03-27-2022.</description>
    </item>
    <item>
      <title>Digital Earth Africa Sentinel-1 Radiometrically Terrain Corrected</title>
      <link>https://registry.opendata.aws/deafrica-sentinel-1</link>
      <guid>https://registry.opendata.aws/deafrica-sentinel-1</guid>
      <description>DE Africa’s Sentinel-1 backscatter product is developed to be compliant with the CEOS Analysis Ready Data for Land (CARD4L) specifications.
The Sentinel-1 mission, composed of a constellation of two C-band Synthetic Aperture Radar (SAR) satellites, are operated by European Space Agency (ESA) as part of the Copernicus Programme. The mission currently collects data every 12 days over Africa at a spatial resolution of approximately 20 m.
Radar backscatter measures the amount of microwave radiation reflected back to the sensor from the ground surface. This measurement is sensitive to surface roughness, moisture content and viewing geometry. DE Africa provides Sentinel-1 backscatter as Radiometrically Terrain Corrected (RTC) gamma-0 (γ0) where variation due to changing observation geometries has been mitigated.
The dual polarisation backcastter time series can be used in applications for forests, agriculture, wetlands and land cover classification. SAR’s ability to ‘see through’ clouds makes it critical for mapping and monitoring land cover changes in the wet tropics.</description>
    </item>
    <item>
      <title>Digital Earth Africa Sentinel-2 Level-2A</title>
      <link>https://registry.opendata.aws/deafrica-sentinel-2</link>
      <guid>https://registry.opendata.aws/deafrica-sentinel-2</guid>
      <description>The Sentinel-2 mission is part of the European Union Copernicus programme for Earth observations. Sentinel-2 consists of twin satellites, Sentinel-2A (launched 23 June 2015) and Sentinel-2B (launched 7 March 2017). The two satellites have the same orbit, but 180° apart for optimal coverage and data delivery. Their combined data is used in the Digital Earth Africa Sentinel-2 product.
Together, they cover all Earth’s land surfaces, large islands, inland and coastal waters every 3-5 days.
Sentinel-2 data is tiered by level of pre-processing. Level-0, Level-1A and Level-1B data contain raw data from the satellites, with little to no pre-processing. Level-1C data is surface reflectance measured at the top of the atmosphere. This is processed using the Sen2Cor algorithm to give Level-2A, the bottom-of-atmosphere reflectance (Obregón et al, 2019). Level-2A data is the most ideal for research activities as it allows further analysis without applying additional atmospheric corrections.
The Digital Earth Africa Sentinel-2 dataset contains Level-2A data of the African continent. Digital Earth Africa does not host any lower-level Sentinel-2 data.
Note that this data is a subset of the Sentinel-2 COGs dataset.</description>
    </item>
    <item>
      <title>Garvan Institute Long Read Sequencing Benchmark Data</title>
      <link>https://registry.opendata.aws/gtgseq</link>
      <guid>https://registry.opendata.aws/gtgseq</guid>
      <description>The dataset contains reference samples that will be useful for benchmarking and comparing bioinformatics tools for genome analysis. Examples include: NA12878 (HG001) and NA24385 (HG002) sequenced on an Oxford Nanopore Technologies (ONT) PromethION using the latest R10.4.1 flowcells; and, UHR RNA (direct-RNA) on an ONT PromethION using the latest RNA004 flowcells. Raw signal data output by the sequencer is provided for these datasets in BLOW5 format, and can be rebasecalled when basecalling software updates bring accuracy and feature improvements over the years. Raw signal data is not only for rebasecalling, but also can be used for emerging bioinformatics tools that directly analyse raw signal data. We also provide the basecalled data alongside the raw signal data.</description>
    </item>
    <item>
      <title>IBL Neuropixels Brainwide Map on AWS</title>
      <link>https://registry.opendata.aws/ibl-brain-wide-map</link>
      <guid>https://registry.opendata.aws/ibl-brain-wide-map</guid>
      <description>Electrophysiological recordings of mouse brain activity acquired during a decision making task.</description>
    </item>
    <item>
      <title>Multi-Scale Ultra High Resolution (MUR) Sea Surface Temperature (SST)</title>
      <link>https://registry.opendata.aws/mur</link>
      <guid>https://registry.opendata.aws/mur</guid>
      <description>A global, gap-free, gridded, daily 1 km Sea Surface Temperature (SST) dataset created by merging multiple Level-2 satellite SST datasets. Those input datasets include the NASA Advanced Microwave Scanning Radiometer-EOS (AMSR-E), the JAXA Advanced Microwave Scanning Radiometer 2 (AMSR-2) on GCOM-W1, the Moderate Resolution Imaging Spectroradiometers (MODIS) on the NASA Aqua and Terra platforms, the US Navy microwave WindSat radiometer, the Advanced Very High Resolution Radiometer (AVHRR) on several NOAA satellites, and in situ SST observations from the NOAA iQuam project. Data are available from 2002 to present in Zarr format. The original source of the MUR data is the NASA JPL Physical Oceanography DAAC.</description>
    </item>
    <item>
      <title>NHGRI AnVIL Project</title>
      <link>https://registry.opendata.aws/anvilproject</link>
      <guid>https://registry.opendata.aws/anvilproject</guid>
      <description>The NHGRI Analysis, Visualization, and Informatics Lab-space (AnVIL) Project (&lt;a href&#x3D;&quot;https://anvilproject.org/&quot;&gt;https://anvilproject.org/&lt;/a&gt;) is the National Human Genome Research Institute&amp;#39;s cloud-based platform for genomic data sharing and analysis. AnVIL hosts widely used human genome reference datasets generated through NHGRI-funded research. AnVIL on Open Data on AWS provides public access to open-access datasets available through AnVIL. The project is a collaborative effort involving NHGRI, the Broad Institute, Johns Hopkins University, the University of California Santa Cruz, Vanderbilt University Medical Center, Brigham and Women&amp;#39;s Hospital, the Carnegie Institution for Science, the City University of New York, the Fred Hutchinson Cancer Research Center, Harvard University, Oregon Health &amp;amp; Science University, Massachusetts General Hospital, Moffitt Cancer Center, Penn State University, and Washington University.</description>
    </item>
    <item>
      <title>New Zealand Imagery</title>
      <link>https://registry.opendata.aws/nz-imagery</link>
      <guid>https://registry.opendata.aws/nz-imagery</guid>
      <description>The New Zealand Imagery dataset consists of New Zealand&amp;#39;s publicly owned aerial and satellite imagery, which is freely available to use under an open licence. The dataset ranges from the latest high-resolution aerial imagery down to 5cm in some urban areas to lower resolution satellite imagery that provides full coverage of mainland New Zealand, Chathams and other offshore islands. It also includes historical imagery that has been scanned from film, orthorectified (removing distortions) and georeferenced (correctly positioned) to create a unique and crucial record of changes to the New Zealand landscape. &lt;br/&gt;
All of the imagery files are &lt;a href&#x3D;&quot;https://www.cogeo.org/&quot;&gt;Cloud Optimised GeoTIFFs&lt;/a&gt; using lossless WEBP compression for the main image and lossy WEBP compression for the overviews. These image files are accompanied by &lt;a href&#x3D;&quot;https://stacspec.org/&quot;&gt;STAC metadata&lt;/a&gt;. The imagery is organised by region and survey.</description>
    </item>
    <item>
      <title>RADARSAT-1</title>
      <link>https://registry.opendata.aws/radarsat-1</link>
      <guid>https://registry.opendata.aws/radarsat-1</guid>
      <description>Developed and operated by the Canadian Space Agency, it is Canada&amp;#39;s first commercial Earth observation satellite 
&lt;br/&gt; &lt;br/&gt;
Développé et exploité par l&amp;#39;Agence spatiale canadienne, il s&amp;#39;agit du premier satellite commercial d&amp;#39;observation de la Terre au Canada.</description>
    </item>
    <item>
      <title>Catalina Sky Survey (CSS) subset data on AWS</title>
      <link>https://registry.opendata.aws/sbn-css</link>
      <guid>https://registry.opendata.aws/sbn-css</guid>
      <description>Raw data that discovers Near Earth Objects (NEOs) which potentially could impact Earth</description>
    </item>
    <item>
      <title>Department of Energy&#x27;s Open Energy Data Initiative (OEDI)</title>
      <link>https://registry.opendata.aws/oedi-data-lake</link>
      <guid>https://registry.opendata.aws/oedi-data-lake</guid>
      <description>Data released under the Department of Energy&amp;#39;s (DOE) Open Energy Data Initiative
(OEDI). The Open Energy Data Initiative aims to improve and automate
access of high-value energy data sets across the U.S. Department of Energy’s
programs, offices, and national laboratories. OEDI aims to make data
actionable and discoverable by researchers and industry to accelerate
analysis and advance innovation.</description>
    </item>
    <item>
      <title>Digital Earth Africa ALOS PALSAR, ALOS-2 PALSAR-2 and JERS-1</title>
      <link>https://registry.opendata.aws/deafrica-alos-jers</link>
      <guid>https://registry.opendata.aws/deafrica-alos-jers</guid>
      <description>The ALOS/PALSAR annual mosaic is a global 25 m resolution dataset that combines data from many images captured by JAXA’s PALSAR and PALSAR-2 sensors on ALOS-1 and ALOS-2 satellites respectively. This product contains radar measurement in L-band and in HH and HV polarizations. It has a spatial resolution of 25 m and is available annually for 2007 to 2010 (ALOS/PALSAR) and 2015 to 2020 (ALOS-2/PALSAR-2).
The JERS annual mosaic is generated from images acquired by the SAR sensor on the Japanese Earth Resources Satellite-1 (JERS-1) satellite. This product contains radar measurement in L-band and HH polarization. It has a spatial resolution of 25 m and is available for 1996.
This mosaic data is part of a global dataset provided by the Japan Aerospace Exploration Agency (JAXA) Earth Observation Research Center.</description>
    </item>
    <item>
      <title>Digital Earth Africa Cropland Extent Map (2019)</title>
      <link>https://registry.opendata.aws/deafrica-crop-extent</link>
      <guid>https://registry.opendata.aws/deafrica-crop-extent</guid>
      <description>Digital Earth Africa&amp;#39;s cropland extent map (2019) shows the estimated location of croplands in Africa for the period January to December 2019. Cropland is defined as: &amp;quot;a piece of land of minimum 0.01 ha (a single 10m x 10m pixel) that is sowed/planted and harvest-able at least once within the 12 months after the sowing/planting date.&amp;quot; This definition will exclude non-planted grazing lands and perennial crops which can be difficult for satellite imagery to differentiate from natural vegetation. 
This provisional cropland extent map has a resolution of 10m, and was built using Copernicus Sentinel-2 satellite images from 2019. The cropland extent map was produced using extensive training data from regions across Africa, coupled with a Random Forest machine learning model. The continental service contains maps built separately for eight Agro-Ecological Zones (AEZs). For a detailed exploration of the methods used to produce the cropland extent map, read the Jupyter Notebooks in DE Africa’s crop-mask GitHub repository.</description>
    </item>
    <item>
      <title>Digital Earth Africa Fractional Cover</title>
      <link>https://registry.opendata.aws/deafrica-fractional-cover</link>
      <guid>https://registry.opendata.aws/deafrica-fractional-cover</guid>
      <description>Fractional cover (FC) describes the landscape in terms of coverage by green vegetation, non-green vegetation (including deciduous trees during autumn, dry grass, etc.) and bare soil. It provides insight into how areas of dry vegetation and/or bare soil and green vegetation are changing over time. The product is derived from Landsat satellite data, using an algorithm developed by the &lt;a href&#x3D;&quot;https://www.jrsrp.org.au/&quot;&gt;Joint Remote Sensing Research Program&lt;/a&gt;. 
Digital Earth Africa&amp;#39;s FC service has two components. Fractional Cover is estimated from each Landsat scene, providing measurements from individual days. Fractional Cover Annual Summary (Percentiles) provides 10th, 50th, and 90th percentiles estimated independently for the green vegetation, non-green vegetation, and bare soil fractions observed in each calendar year (1st of January - 31st December).
While the scene based Fractional Cover can be used to study dynamic processes, the annual summaries make it easier to analyse year to year changes. The percentiles provide robust estimates of the low, median and high proportion values observed for each cover type in a year, which can be used to characterise the land cover.</description>
    </item>
    <item>
      <title>Digital Earth Africa Monthly Normalised Difference Vegetation Index (NDVI) Anomaly</title>
      <link>https://registry.opendata.aws/deafrica-ndvi_anomaly</link>
      <guid>https://registry.opendata.aws/deafrica-ndvi_anomaly</guid>
      <description>Digital Earth Africa’s Monthly NDVI Anomaly service provides estimate of vegetation condition, for each caldendar month, against the long-term baseline condition measured for the month from 1984 to 2020 in the NDVI Climatology.  A standardised anomaly is calculated by subtracting the long-term mean from an observation of interest and then dividing the result by the long-term standard deviation. Positive NDVI anomaly values indicate vegetation is greener than average conditions, and are usually due to increased rainfall in a region. Negative values indicate additional plant stress relative to the long-term average. The NDVI anomaly service is therefore effective for understanding the extent, intensity and impact of a drought.Abrupt and significant negative anomalies may also be caused by fire disturbance.</description>
    </item>
    <item>
      <title>KyFromAbove on AWS</title>
      <link>https://registry.opendata.aws/kyfromabove</link>
      <guid>https://registry.opendata.aws/kyfromabove</guid>
      <description>The KyFromAbove initiative is focused on building and maintaining a current basemap for Kentucky that can meet the needs of its users at the state, federal, local, and regional level. A common basemap, including current color leaf-off aerial photography and elevation data (LiDAR), reduces the cost of developing GIS applications, promotes data sharing, and add efficiencies to many business processes. All basemap data acquired through this effort is made available in the public domain. KyFromAbove acquires aerial imagery and LiDAR during leaf-off conditions in the Commonwealth. The imagery typically ranges from 6-inches to 3-inches in resolution and is available from the kyfromabove Amazon S3 bucket in a Cloud Optimized GeoTiff format. LiDAR data acquired by the program is USGS Quality Level 2 (QL2). Digital Elevation Models (DEMs) at a 2-foot resolution, point cloud data in an LAS format, spot elevations in a geopackage format, and contours in a geopackage format are also available from the kyfromabove Amazon S3 bucket. KyFromAbove LiDAR and imagery data resources are managed in a Kentucky-specific 5000x5000 foot grid (FIPS:1600) (EPSG:3089). More details about the program can be found at (&lt;a href&#x3D;&quot;https://kyfromabove.ky.gov/&quot;&gt;https://kyfromabove.ky.gov/&lt;/a&gt;).</description>
    </item>
    <item>
      <title>Louisiana Watershed Initiative (LWI) Model Data</title>
      <link>https://registry.opendata.aws/lwi-model-data</link>
      <guid>https://registry.opendata.aws/lwi-model-data</guid>
      <description>Geographic (land cover, land elevation, etc.), meteorologic (pluvial, wind, etc.),  hydrologic (fluvial, tidal, etc.), hydrodynamic (water surface elevations, flow velocities), and built environment (structures, levees, floodgates, culverts) data used as inputs to and  outputs from numerical modeling software for the prediction of flood risk in stochastic and probabilistic frameworks. This data was collected from open sources, such as from the  National Oceanographic and Atmospheric Administration (NOAA) or the  United States Geological Survey (USGS). The format of these data is modified to suit the needs of the modeling program and software, and then used to predict flooding in Louisiana across a range of scenarios. The modeling software used to predict flooding which utilizes and creates this data is freely available from the  United States Army Corps of Engineers Hydrologic Engineering Center’s Hydrologic Modeling System (HEC-HMS) and River Analysis System (HEC-RAS). All data is made public by the State of Louisiana for the benefit of its citizens. This flood prediction data can be used by federal, state, and local decision makers as well as private citizens to assess the flood risk they face and make sound science-based decisions for response and adaptation.</description>
    </item>
    <item>
      <title>NREL Wind Integration National Dataset</title>
      <link>https://registry.opendata.aws/nrel-pds-wtk</link>
      <guid>https://registry.opendata.aws/nrel-pds-wtk</guid>
      <description>Released to the public as part of the Department of Energy&amp;#39;s Open Energy Data Initiative,
the &lt;a href&#x3D;&quot;https://www.nrel.gov/grid/wind-toolkit.html&quot;&gt;Wind Integration National Dataset (WIND)&lt;/a&gt;
is an update and expansion of the Eastern Wind Integration Data Set and
Western Wind Integration Data Set. It supports the next generation of wind
integration studies.</description>
    </item>
    <item>
      <title>Open NeuroData</title>
      <link>https://registry.opendata.aws/open-neurodata</link>
      <guid>https://registry.opendata.aws/open-neurodata</guid>
      <description>This bucket contains multiple neuroimaging datasets (as Neuroglancer Precomputed Volumes) across multiple modalities and scales, ranging from nanoscale (electron microscopy), to microscale (cleared lightsheet microscopy and array tomography), and mesoscale (structural and functional magnetic resonance imaging). Additionally, many of the datasets include segmentations and meshes.</description>
    </item>
    <item>
      <title>PubSeq - Public Sequence Resource</title>
      <link>https://registry.opendata.aws/pubseq</link>
      <guid>https://registry.opendata.aws/pubseq</guid>
      <description>COVID-19 PubSeq is a free and open online bioinformatics public sequence resource with on-the-fly analysis of sequenced SARS-CoV-2 samples that allows for a quick turnaround in identification of new virus strains. PubSeq allows anyone to upload sequence material in the form of FASTA or FASTQ files with accompanying metadata through the web interface or REST API.</description>
    </item>
    <item>
      <title>Southern California Earthquake Data</title>
      <link>https://registry.opendata.aws/southern-california-earthquakes</link>
      <guid>https://registry.opendata.aws/southern-california-earthquakes</guid>
      <description>This dataset contains ground motion velocity and acceleration seismic waveforms recorded by the Southern California Seismic Network (SCSN) and archived at the Southern California Earthquake Data Center (SCEDC). A Distributed Acousting Sensing (DAS) dataset is included.</description>
    </item>
    <item>
      <title>Steinegger Lab Datasets</title>
      <link>https://registry.opendata.aws/steineggerlab</link>
      <guid>https://registry.opendata.aws/steineggerlab</guid>
      <description>The Steinegger Lab Dataset comprises biological databases and resources critical for protein sequence and structure analysis, developed to support ColabFold, MMseqs2, and Foldseek/Foldcomp—three high-performance computational tools widely used in bioinformatics.The MMseqs2 dataset serves as the backbone for our fast structure prediction tool, ColabFold, and includes UniRef30, BFD, and the ColabFold environmental databases.
These datasets are specifically designed for the rapid generation of multiple sequence alignments (MSAs), which are essential for high-accuracy structure prediction.
Beyond MSA generation, these resources allow for fast taxonomy annotations and functional annotation, supporting a wide range of bioinformatics applications.The Foldseek dataset includes preprocessed databases such as the AlphaFold Database (AFDB), PDB, SwissProt, and CATH, specifically designed for protein structure similarity searches.
These datasets encompass the majority of both experimental and predicted structural resources, supporting analyses for monomers and multimers alike.</description>
    </item>
    <item>
      <title>USGS 3DEP LiDAR Point Clouds</title>
      <link>https://registry.opendata.aws/usgs-lidar</link>
      <guid>https://registry.opendata.aws/usgs-lidar</guid>
      <description>The goal of the &lt;a href&#x3D;&quot;https://www.usgs.gov/core-science-systems/ngp/3dep&quot;&gt;USGS 3D Elevation Program &lt;/a&gt; (3DEP) is to collect elevation data in the form of light detection and ranging (LiDAR) data over the conterminous United States, Hawaii, and the U.S. territories, with data acquired over an 8-year period. This dataset provides two realizations of the 3DEP point cloud data. The first resource is a public access organization provided in &lt;a href&#x3D;&quot;https://entwine.io/entwine-point-tile.html&quot;&gt;Entwine Point Tiles&lt;/a&gt; format, which a lossless, full-density, streamable octree based on &lt;a href&#x3D;&quot;https://laszip.org&quot;&gt;LASzip&lt;/a&gt; (LAZ) encoding. The second resource is a &lt;a href&#x3D;&quot;https://docs.aws.amazon.com/AmazonS3/latest/dev/RequesterPaysBuckets.html&quot;&gt;Requester Pays&lt;/a&gt; of the original, Raw LAZ (Compressed LAS) 1.4 3DEP format, and more complete in coverage, as sources with incomplete or missing CRS, will not have an ETP tile generated.  Resource names in both buckets correspond to the USGS project names.</description>
    </item>
    <item>
      <title>World Bank - Light Every Night</title>
      <link>https://registry.opendata.aws/wb-light-every-night</link>
      <guid>https://registry.opendata.aws/wb-light-every-night</guid>
      <description>Light Every Night - World Bank Nighttime Light Data – provides open access to all nightly imagery and data from the Visible Infrared Imaging Radiometer Suite Day-Night Band (VIIRS DNB) from 2012-2020 and the Defense Meteorological Satellite Program Operational Linescan System (DMSP-OLS) from 1992-2013. The underlying data are sourced from the NOAA National Centers for Environmental Information (NCEI) archive. Additional processing by the University of Michigan enables access in Cloud Optimized GeoTIFF format (COG) and search using the Spatial Temporal Asset Catalog (STAC) standard. The data is published and openly available under the terms of the World Bank’s open data license.</description>
    </item>
    <item>
      <title>nuScenes</title>
      <link>https://registry.opendata.aws/motional-nuscenes</link>
      <guid>https://registry.opendata.aws/motional-nuscenes</guid>
      <description>Public large-scale dataset for autonomous driving. It enables researchers to study challenging urban driving situations using the full sensor suite of a real self-driving car.</description>
    </item>
    <item>
      <title>ArcticDEM</title>
      <link>https://registry.opendata.aws/pgc-arcticdem</link>
      <guid>https://registry.opendata.aws/pgc-arcticdem</guid>
      <description>ArcticDEM - 2m GSD Digital Elevation Models (DEMs) and mosaics from 2007 to the present. The ArcticDEM project seeks to fill the need for high-resolution time-series elevation data in the Arctic. The time-dependent nature of the strip DEM files allows users to perform change detection analysis and to compare observations of topography data acquired in different seasons or years. The mosaic DEM tiles are assembled from multiple strip DEMs with the intention of providing a more consistent and comprehensive product over large areas. ArcticDEM data is constructed from in-track and cross-track high-resolution (~0.5 meter) imagery acquired by the Maxar constellation of optical imaging satellites.</description>
    </item>
    <item>
      <title>Boreas Autonomous Driving Dataset</title>
      <link>https://registry.opendata.aws/boreas</link>
      <guid>https://registry.opendata.aws/boreas</guid>
      <description>This autonomous driving dataset includes data from a 128-beam Velodyne Alpha-Prime lidar, a 5MP Blackfly camera, a 360-degree Navtech radar, and post-processed Applanix POS LV GNSS data. This dataset was collect in various weather conditions (sun, rain, snow) over the course of a year. The intended purpose of this dataset is to enable benchmarking of long-term all-weather odometry and metric localization across various sensor types. In the future, we hope to also support an object detection benchmark.</description>
    </item>
    <item>
      <title>CHAMMI-75</title>
      <link>https://registry.opendata.aws/chammi</link>
      <guid>https://registry.opendata.aws/chammi</guid>
      <description>Quantifying cell morphology using images and machine learning models has proven to be a powerful tool to study the response of cells to treatments. 
However, the models used to quantify cellular morphology are typically trained with a single microscopy imaging type and under controlled experimental conditions. 
This results in specialized models that cannot be reused across biological studies because the technical specifications do not match (e.g., different number of channels), 
or because the target experimental conditions are out of distribution. We have created CHAMMI-75, a large-scale dataset containing 2.8 million multi-channel, 
high-resolution images curated from 75 diverse, publicly available biological studies. This dataset is useful to investigate and develop channel-adaptive models, 
which could process microscopy images of varying technical specifications and regardless of the number of channels. By breaking the limitations of existing models, 
CHAMMI-75 is an invaluable resource for creating the next generation of foundation models for image-based biological research.  </description>
    </item>
    <item>
      <title>CMIP6 GCMs downscaled using WRF</title>
      <link>https://registry.opendata.aws/wrf-cmip6</link>
      <guid>https://registry.opendata.aws/wrf-cmip6</guid>
      <description>High-resolution historical and future climate simulations from 1980-2100</description>
    </item>
    <item>
      <title>Cancer Cell Line Encyclopedia (CCLE)</title>
      <link>https://registry.opendata.aws/ccle</link>
      <guid>https://registry.opendata.aws/ccle</guid>
      <description>The Cancer Cell Line Encyclopedia (CCLE) project is an effort to conduct a detailed genetic
characterization of a large panel of human cancer cell lines. The CCLE provides public access to
genomic data, visualization and analysis for over 1100 cancer cell lines. This dataset contains
RNA-Seq Aligned Reads, WXS Aligned Reads, and WGS Aligned Reads data.</description>
    </item>
    <item>
      <title>Co-Produced Climate Data to Support California&#x27;s Resilience Investments</title>
      <link>https://registry.opendata.aws/caladapt-coproduced-climate-data</link>
      <guid>https://registry.opendata.aws/caladapt-coproduced-climate-data</guid>
      <description>Downscaled future and historical climate projections for California and her environs in support of California&amp;#39;s Fifth Climate Assessment</description>
    </item>
    <item>
      <title>DOE&#x27;s Water Power Technology Office&#x27;s (WPTO) US Wave dataset</title>
      <link>https://registry.opendata.aws/wpto-pds-us-wave</link>
      <guid>https://registry.opendata.aws/wpto-pds-us-wave</guid>
      <description>Released to the public as part of the Department of Energy&amp;#39;s Open Energy Data Initiative,
this is the highest resolution publicly available long-term wave hindcast
dataset that – when complete – will cover the entire U.S. Exclusive Economic
Zone (EEZ).</description>
    </item>
    <item>
      <title>Digital Earth Africa Normalised Difference Vegetation Index (NDVI) Climatology</title>
      <link>https://registry.opendata.aws/deafrica-ndvi_climatology_ls</link>
      <guid>https://registry.opendata.aws/deafrica-ndvi_climatology_ls</guid>
      <description>Digital Earth Africa’s NDVI climatology product represents the long-term average baseline condition of vegetation for every Landsat pixel over the African continent. Both mean and standard deviation NDVI climatologies are available for each calender month.Some key features of the product are:&lt;ul&gt;
&lt;li&gt;NDVI climatologies were developed using harmonized Landsat 5,7,and 8 satellite imagery.&lt;/li&gt;
&lt;li&gt;Mean and standard deviation NDVI climatologies are produced for each calender month, using a temporal baseline period from 1984-2020 (inclusive)&lt;/li&gt;
&lt;li&gt;Datasets have a spatial resolution of 30 metres&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>Logan Unitigs and Contigs of the Sequence Read Archive (SRA) on AWS</title>
      <link>https://registry.opendata.aws/pasteur-logan</link>
      <guid>https://registry.opendata.aws/pasteur-logan</guid>
      <description>This repository is a re-analysis of the NCBI Sequence Read Archive (SRA), December 2023 freeze, to make it more accessible. The SRA is an open access database of biological sequences, containing raw data from high-throughput DNA and RNA sequencing platforms. It is the largest database of public DNA sequences worldwide, containing a wealth of genomic diversity across all living organisms. This repository contains Logan, a set of compressed FASTA files for all individual SRA accessions, in the form of unitigs and contigs. Borrowing methods from the realm of genome assembly, unitigs preserve nearly all the information present in the original sample, whereas contigs get rid of variations to increase sequence lengths. Altogether, Logan recapitulates the information present in the SRA while making it an order of magnitude more accessible due to 20-100x smaller size and higher quality genomic content.</description>
    </item>
    <item>
      <title>NIH Roadmap Epigenomics</title>
      <link>https://registry.opendata.aws/roadmapepigenomics</link>
      <guid>https://registry.opendata.aws/roadmapepigenomics</guid>
      <description>The NIH Roadmap Epigenomics Mapping Consortium was launched with the goal of producing a public resource of human epigenomic data to catalyze basic biology and disease-oriented research. The project has generated high-quality, genome-wide maps of several key histone modifications, chromatin accessibility, DNA methylation and mRNA expression across 100s of human cell types and tissues. To see what data is available, please check the directory listing: &lt;a href&#x3D;&quot;https://roadmapepigenomics.s3.us-west-2.amazonaws.com/index.html&quot;&gt;https://roadmapepigenomics.s3.us-west-2.amazonaws.com/index.html&lt;/a&gt;.</description>
    </item>
    <item>
      <title>NOAA Water-Column Sonar Data Archive</title>
      <link>https://registry.opendata.aws/ncei-wcsd-archive</link>
      <guid>https://registry.opendata.aws/ncei-wcsd-archive</guid>
      <description>Water-column sonar data archived at the NOAA National Centers for Environmental Information.</description>
    </item>
    <item>
      <title>New Zealand Elevation</title>
      <link>https://registry.opendata.aws/nz-elevation</link>
      <guid>https://registry.opendata.aws/nz-elevation</guid>
      <description>The New Zealand Elevation dataset consists of New Zealand&amp;#39;s publicly owned digital elevation models and digital surface models, which are freely available to use under an open licence. The dataset contains 1m resolution grids derived from LiDAR data. Point clouds are not included in the initial release.All of the elevation files are &lt;a href&#x3D;&quot;https://www.cogeo.org/&quot;&gt;Cloud Optimised GeoTIFFs&lt;/a&gt; using LERC compression for the main grid and LERC compression with lower max_z_error for the overviews. These elevation files are accompanied by &lt;a href&#x3D;&quot;https://stacspec.org/&quot;&gt;STAC metadata&lt;/a&gt;. The elevation data is organised by region and survey.</description>
    </item>
    <item>
      <title>Northern California Earthquake Data</title>
      <link>https://registry.opendata.aws/northern-california-earthquakes</link>
      <guid>https://registry.opendata.aws/northern-california-earthquakes</guid>
      <description>This dataset contains various types of digital data relating
to earthquakes in central and northern California. 
Time series data come from broadband, short period, and strong motion
seismic sensors, GPS, and other geophysical sensors.</description>
    </item>
    <item>
      <title>Open CEDA by Watershed</title>
      <link>https://registry.opendata.aws/open-ceda</link>
      <guid>https://registry.opendata.aws/open-ceda</guid>
      <description>CEDA is a multi-regional Environmentally-Extended Input-Output (EEIO) model developed to support a wide range of environmental systems analyses—including corporate carbon accounting and sustainable spend analysis. CEDA provides unparalleled global coverage and granularity, representing 95% of the world&amp;#39;s GDP across 148 countries and 400 sectors, enabling robust and geographically comprehensive Scope 3 greenhouse gas (GHG) measurement. 
Open CEDA is the publicly avaialable version of CEDA, now easy to download and available for free for all use cases. For more information please visit our website at openceda.org.
This data registry entry contains CEDA 2025 and CEDA 2024 in two separate files. CEDA 2025, the latest version of CEDA, uses 2023 as its base year, ensuring that emissions factors and economic data reflect the most recent global economic landscape available. To maintain accuracy and relevance, CEDA is updated annually with the latest data releases.
At its core, CEDA connects economic exchanges to GHG emissions by quantifying the life-cycle emissions of products and services. This is achieved through the integration of input-output tables, which represent the full supply-chain network of the global economy, with GHG emissions data. As a result, CEDA provides users with a powerful tool to assess the environmental impacts embedded in corporate value chains.</description>
    </item>
    <item>
      <title>Radiant MLHub</title>
      <link>https://registry.opendata.aws/radiant-mlhub</link>
      <guid>https://registry.opendata.aws/radiant-mlhub</guid>
      <description>Radiant MLHub is an open library for geospatial training data that hosts datasets generated by &lt;a href&#x3D;&quot;https://www.radiant.earth/&quot;&gt;Radiant Earth Foundation&lt;/a&gt;&amp;#39;s team as well as other training data catalogs contributed by Radiant Earth’s partners. Radiant MLHub is open to anyone to access, store, register and/or share their training datasets for high-quality Earth observations. All of the training datasets are stored using a &lt;a href&#x3D;&quot;https://stacspec.org/&quot;&gt;SpatioTemporal Asset Catalog (STAC)&lt;/a&gt; compliant catalog and exposed through a common API. Training datasets include pairs of imagery and labels for different types of machine learning problems including image classification, object detection, and semantic segmentation. Labels are generated from ground reference data and/or image annotation.</description>
    </item>
    <item>
      <title>Reference Elevation Model of Antarctica (REMA)</title>
      <link>https://registry.opendata.aws/pgc-rema</link>
      <guid>https://registry.opendata.aws/pgc-rema</guid>
      <description>The Reference Elevation Model of Antarctica - 2m GSD Digital Elevation Models (DEMs) and mosaics from 2009 to the present. The REMA project seeks to fill the need for high-resolution time-series elevation data in the Antarctic. The time-dependent nature of the strip DEM files allows users to perform change detection analysis and to compare observations of topography data acquired in different seasons or years. The mosaic DEM tiles are assembled from multiple strip DEMs with the intention of providing a more consistent and comprehensive product over large areas. REMA data is constructed from in-track and cross-track high-resolution (~0.5 meter) imagery acquired by the Maxar constellation of optical imaging satellites.</description>
    </item>
    <item>
      <title>Toxicant Exposures and Responses by Genomic and Epigenomic Regulators of Transcription (TaRGET)</title>
      <link>https://registry.opendata.aws/targetepigenomics</link>
      <guid>https://registry.opendata.aws/targetepigenomics</guid>
      <description>The TaRGET (Toxicant Exposures and Responses by Genomic and Epigenomic Regulators of Transcription) Program is a research consortium funded by the National Institute of Environmental Health Sciences (NIEHS). The goal of the collaboration is to address the role of environmental exposures in disease pathogenesis as a function of epigenome perturbation, including understanding the environmental control of epigenetic mechanisms and assessing the utility of surrogate tissue analysis in mouse models of disease-relevant environmental exposures.</description>
    </item>
    <item>
      <title>U.S. Environmental Protection Agency (EPA) Center for Computational Toxicology and Exposure High Throughput Transcriptomics Data</title>
      <link>https://registry.opendata.aws/epa-ccte-httr</link>
      <guid>https://registry.opendata.aws/epa-ccte-httr</guid>
      <description>High-throughput transcriptomics (HTTr) data generated by US EPA Office of Research and Development, Center for Computational Toxicology and Exposure (CCTE), Biomolecular and Computational Toxicology Division.  All data is generated using TempO-Seq targeted RNA-seq technology from in vitro cell culture systems.</description>
    </item>
    <item>
      <title>ASTER L1T Cloud-Optimized GeoTIFFs</title>
      <link>https://registry.opendata.aws/aster-l1t</link>
      <guid>https://registry.opendata.aws/aster-l1t</guid>
      <description>The Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) Level 1
Precision Terrain Corrected Registered At-Sensor Radiance (AST_L1T) data contains
calibrated at-sensor radiance, which corresponds with the ASTER Level 1B (AST_L1B),
that has been geometrically corrected, and rotated to a north-up UTM projection.
The AST_L1T is created from a single resampling of the corresponding ASTER L1A (AST_L1A) product.The precision terrain correction process incorporates GLS2000 digital elevation data with
derived ground control points (GCPs) to achieve topographic accuracy for all daytime scenes
where correlation statistics reach a minimum threshold. Alternate levels of correction are
possible (systematic terrain, systematic, or precision) for scenes acquired at night or that
otherwise represent a reduced quality ground image (e.g., cloud cover).Each AST_L1T granule is converted into three different COG files based on the sensor and spatial resolution,
VNIR at 15m, SWIR at 30m and TIR at 90m. The metadata required to transform the digital numbers (DN) to 
radiance and reflectance values are also incorporated as metadata in the TIFF files.
The filenaming convention and the organization of bands are described
&lt;a href&#x3D;&quot;https://github.com/awslabs/open-data-docs/tree/main/docs/aster-l1t&quot;&gt;here&lt;/a&gt;.</description>
    </item>
    <item>
      <title>BossDB Open Neuroimagery Datasets</title>
      <link>https://registry.opendata.aws/bossdb</link>
      <guid>https://registry.opendata.aws/bossdb</guid>
      <description>This data ecosystem, Brain Observatory Storage Service &amp;amp; Database (BossDB), contains several neuro-imaging datasets across multiple modalities and scales, ranging from nanoscale (electron microscopy), to microscale (cleared lightsheet microscopy and array tomography), and mesoscale (structural and functional magnetic resonance imaging). Additionally, many of the datasets include dense segmentation and meshes.</description>
    </item>
    <item>
      <title>CIViC (Clinical Interpretation of Variants in Cancer)</title>
      <link>https://registry.opendata.aws/civic</link>
      <guid>https://registry.opendata.aws/civic</guid>
      <description>Precision medicine refers to the use of prevention and treatment strategies that are tailored to the unique features of each individual and their disease. In the context of cancer this might involve the identification of specific mutations shown to predict response to a targeted therapy. The biomedical literature describing these associations is large and growing rapidly. Currently these interpretations exist largely in private or encumbered databases resulting in extensive repetition of effort. Realizing precision medicine will require this information to be centralized, debated and interpreted for application in the clinic. CIViC is an open access, open source, community-driven web resource for Clinical Interpretation of Variants in Cancer. Our goal is to enable precision medicine by providing an educational forum for dissemination of knowledge and active discussion of the clinical significance of cancer genome alterations.</description>
    </item>
    <item>
      <title>Clinical Proteomic Tumor Analysis Consortium 2 (CPTAC-2)</title>
      <link>https://registry.opendata.aws/cptac-2</link>
      <guid>https://registry.opendata.aws/cptac-2</guid>
      <description>The Clinical Proteomic Tumor Analysis Consortium (CPTAC) is a national effort to accelerate the
understanding of the molecular basis of cancer through the application of large-scale proteome and
genome analysis, or proteogenomics. CPTAC-2 is the Phase II of the CPTAC Initiative (2011-2016).
Datasets contain open RNA-Seq Gene Expression Quantification, miRNA-Seq Isoform Expression
Quantification, and miRNA Expression Quantification data.</description>
    </item>
    <item>
      <title>Coupled Model Intercomparison Project 6</title>
      <link>https://registry.opendata.aws/cmip6</link>
      <guid>https://registry.opendata.aws/cmip6</guid>
      <description>The sixth phase of global coupled ocean-atmosphere general circulation model ensemble. 
&lt;br /&gt;&lt;br /&gt;</description>
    </item>
    <item>
      <title>Earth Observation Data Cubes for Brazil</title>
      <link>https://registry.opendata.aws/brazil-data-cubes</link>
      <guid>https://registry.opendata.aws/brazil-data-cubes</guid>
      <description>Earth observation (EO) data cubes produced from analysis-ready data (ARD) of CBERS-4, Sentinel-2 A/B and Landsat-8 satellite images for Brazil. The datacubes are regular in time and use a hierarchical tiling system. Further details are described in &lt;a href&#x3D;&quot;https://www.mdpi.com/2072-4292/12/24/4033&quot;&gt;Ferreira et al. (2020)&lt;/a&gt;.</description>
    </item>
    <item>
      <title>GEOS-Chem Input Data</title>
      <link>https://registry.opendata.aws/geoschem-input-data</link>
      <guid>https://registry.opendata.aws/geoschem-input-data</guid>
      <description>Input data for the GEOS-Chem Chemical Transport Model, includes NASA/GMAO MERRA-2 and GEOS-FP &lt;a href&#x3D;&quot;https://geos-chem.readthedocs.io/en/latest/gcclassic-user-guide/input-overview.html#met&quot;&gt;meteorological products&lt;/a&gt;, &lt;a href&#x3D;&quot;https://geos-chem.readthedocs.io/en/latest/gcclassic-user-guide/input-overview.html#chemistry-input-data&quot;&gt;chemistry input data&lt;/a&gt;, &lt;a href&#x3D;&quot;https://geos-chem.readthedocs.io/en/latest/gcclassic-user-guide/input-overview.html#emis-inputs&quot;&gt;emissions input data&lt;/a&gt;, and other smaller datasets such as model &lt;a href&#x3D;&quot;https://geos-chem.readthedocs.io/en/latest/gcclassic-user-guide/input-overview.html#initial-conditions-input-data%3E&quot;&gt;initial conditions&lt;/a&gt;.</description>
    </item>
    <item>
      <title>GEOS-Chem Nested Input Data</title>
      <link>https://registry.opendata.aws/geoschem-nested-input-data</link>
      <guid>https://registry.opendata.aws/geoschem-nested-input-data</guid>
      <description>Input data for nested-grid simulations using the GEOS-Chem Chemical Transport Model. This includes the NASA/GMAO MERRA-2 and GEOS-FP &lt;a href&#x3D;&quot;https://geos-chem.readthedocs.io/en/latest/gcclassic-user-guide/input-overview.html#met&quot;&gt;meteorological products&lt;/a&gt;, the &lt;a href&#x3D;&quot;https://geos-chem.readthedocs.io/en/latest/gcclassic-user-guide/input-overview.html#emis-inputs&quot;&gt;HEMCO emission inventories&lt;/a&gt;, and other small data such as &lt;a href&#x3D;&quot;https://geos-chem.readthedocs.io/en/latest/gcclassic-user-guide/restart-files.html&quot;&gt;model initial conditions&lt;/a&gt;.</description>
    </item>
    <item>
      <title>Global Database of Events, Language and Tone (GDELT)</title>
      <link>https://registry.opendata.aws/gdelt</link>
      <guid>https://registry.opendata.aws/gdelt</guid>
      <description>This project monitors the world&amp;#39;s broadcast, print,
and web news from nearly every corner of every country in
over 100 languages and identifies the people, locations,
organizations, counts, themes, sources, emotions,
quotes, images and events driving our global society every
second of every day.</description>
    </item>
    <item>
      <title>IBL Neuropixels Reproducible Ephys Data on AWS</title>
      <link>https://registry.opendata.aws/ibl-reproducible-ephys</link>
      <guid>https://registry.opendata.aws/ibl-reproducible-ephys</guid>
      <description>Electrophysiological recordings acquired using Neuropixels probes in different mice and labs, targeting the same brain locations (including posterior parietal cortex, hippocampus, and thalamus).</description>
    </item>
    <item>
      <title>ICGC on AWS</title>
      <link>https://registry.opendata.aws/icgc</link>
      <guid>https://registry.opendata.aws/icgc</guid>
      <description>The International Cancer Genome Consortium (ICGC) coordinates projects with the common aim of accelerating research into the causes and control of cancer. The PanCancer Analysis of Whole Genomes (PCAWG) study is an international collaboration to identify common patterns of mutation in whole genomes from ICGC. More than 2,400 consistently analyzed genomes corresponding to over 1,100 unique ICGC donors are now freely available on Amazon S3 to credentialed researchers subject to ICGC data sharing policies.</description>
    </item>
    <item>
      <title>Materials Project Data</title>
      <link>https://registry.opendata.aws/materials-project</link>
      <guid>https://registry.opendata.aws/materials-project</guid>
      <description>Materials Project is an open database of computed materials properties aiming to accelerate materials science research. The resources in this OpenData dataset contain the raw, parsed, and build data products.</description>
    </item>
    <item>
      <title>NOAA National Water Model CONUS Retrospective Dataset</title>
      <link>https://registry.opendata.aws/nwm-archive</link>
      <guid>https://registry.opendata.aws/nwm-archive</guid>
      <description>The NOAA National Water Model Retrospective dataset contains input and output from multi-decade CONUS retrospective simulations. These simulations used meteorological input fields from meteorological retrospective datasets. The output frequency and fields available in this historical NWM dataset differ from those contained in the real-time operational NWM forecast model. Additionally, note that no streamflow or other data assimilation is performed within any of the NWM retrospective simulations
&lt;br/&gt;
&lt;br/&gt;
One application of this dataset is to provide historical context to current near real-time streamflow, soil moisture and snowpack conditions. The retrospective data can be used to infer flow frequencies and perform temporal analyses with hourly streamflow output and 3-hourly land surface output. This dataset can also be used in the development of end user applications which require a long baseline of data for system training or verification purposes. &lt;br /&gt;
&lt;br/&gt;
&lt;br/&gt;
Details for Each Version of the NWM Retrospective Output
&lt;br/&gt;
&lt;br/&gt;
&lt;strong&gt;CONUS Domain&lt;/strong&gt; - CONUS retrospective output is provided by all four versions of the NWM
&lt;br/&gt;&lt;ol&gt;
&lt;li&gt;Version 3.0 - A 44-year (February 1979 through January 2023) retrospective simulation using version 3.0 of the National Water Model.&lt;/li&gt;
&lt;li&gt;Version 2.1 - A 42-year (February 1979 through December 2020) retrospective simulation using version 2.1 of the National Water Model.&lt;/li&gt;
&lt;li&gt;Version 2.0 - A 26-year (January 1993 through December 2018) retrospective simulation using version 2.0 of the National Water Model.&lt;/li&gt;
&lt;li&gt;Version 1.2 - A 25-year (January 1993 through December 2017) retrospective simulation using version 1.2 of the National Water Model.&lt;br/&gt;
&lt;br/&gt;&lt;/li&gt;
&lt;/ol&gt;
&lt;strong&gt;oCOUNS Domains&lt;/strong&gt; - Only v3.0 of the NWM Retrospective data set provides coverage of the NWM Alaska, Hawaii and Puerto Rico / US Virgin Island domains.
&lt;br/&gt;
&lt;br/&gt;
&lt;strong&gt;CONUS Meteorological Forcing&lt;/strong&gt;&lt;ol&gt;
&lt;li&gt;Versions 3.0 and 2.1:  NWM Retrospective simulations used forcing from the Office of Water Prediction Analysis of Record for Calibration (AORC) dataset.  NWM v2.1 used AORC v1.0 for 1979-2006 and AORC v1.1 for 2007-2020, while NWM v3.0 used AORC v1.1 for the full v3.0  (1979-2023 period)&lt;/li&gt;
&lt;/ol&gt;
&lt;strong&gt;Important Warning&lt;/strong&gt; - While the metadata tag in the NWM v3.0 forcing files label the files as “v2.1”, the files are in fact v3.0 forcing files.
2) Versions 2.0 and 1.2 -  NWM Retrospective simulation uses forcing from the North American Land Data Assimilation System (NLDAS) dataset
&lt;br/&gt;
&lt;strong&gt;oCONUS Meteorological Forcing&lt;/strong&gt;&lt;ol&gt;
&lt;li&gt;Version 3.0 -  AORC Alaska forcing was used to drive the NWM Alaska simulation, while North American Regional Reanalysis (NARR) data along with precipitation from the Alaska Pacific River Forecast Center (APRFC) was used to drive the Hawaii retrospective simulation.  Similarly, the Puerto Rico / US Virgin Island retrospective simulation was driven by NARR data along with precipitation from the Southeast River Forecast Center.&lt;br/&gt;
&lt;br/&gt;&lt;/li&gt;
&lt;/ol&gt;
&lt;strong&gt;Formats&lt;/strong&gt; - NWM Retrospective data is available in two formats, NetCDF and Zarr.  The NetCDF files contain the full set of NWM output data, while the Zarr files contain a subset of NWM output fields that vary with model version.
&lt;br/&gt;
&lt;br/&gt;&lt;ol&gt;
&lt;li&gt;NWM V3.0:  All model output and forcing input fields are available in the NetCDF format.  All model output fields along with the precipitation forcing field are available in the Zarr format.&lt;/li&gt;
&lt;li&gt;NWM V2.1:  All model output and forcing input fields are available in the NetCDF format.  Many of the model output fields along with the precipitation forcing field are available in the Zarr format&lt;/li&gt;
&lt;li&gt;NWM V2.0:  All model output fields are available in NetCDF format.  Model channel output including streamflow and related fields are available in Zarr format.&lt;/li&gt;
&lt;li&gt;NWM V1.2:  All model output fields are available in NetCDF format.&lt;br/&gt;
&lt;br/&gt;
A table listing the data available within each NetCDF and Zarr file is located in the &#x27;[documentation page](https://github.com/NOAA-Big-Data-Program/bdp-data-docs/blob/main/nwm/README.md)&#x27;.  This data includes meteorological NWM forcing inputs along with NWM hydrologic and land surface outputs, and varies by version number.&lt;/li&gt;
&lt;/ol&gt;
</description>
    </item>
    <item>
      <title>OpenAQ</title>
      <link>https://registry.opendata.aws/openaq</link>
      <guid>https://registry.opendata.aws/openaq</guid>
      <description>Global, aggregated physical air quality data from public data sources provided by government, research-grade and other sources. These awesome groups do the hard work of measuring these data and publicly sharing them, and our community makes them more universally-accessible to both humans and machines.</description>
    </item>
    <item>
      <title>OpenAerialMap on AWS</title>
      <link>https://registry.opendata.aws/openaerialmap</link>
      <guid>https://registry.opendata.aws/openaerialmap</guid>
      <description>OpenAerialMap is a collection of high-resolution openly licensed satellite and aerial imagery.</description>
    </item>
    <item>
      <title>Scottish Public Sector LiDAR Dataset</title>
      <link>https://registry.opendata.aws/scottish-lidar</link>
      <guid>https://registry.opendata.aws/scottish-lidar</guid>
      <description>This dataset is Lidar data that has been collected by the Scottish public sector and made available under the Open Government Licence. The data are available as point cloud (LAS format or in LAZ compressed format), along with the derived Digital Terrain Model (DTM) and Digital Surface Model (DSM) products as Cloud optimized GeoTIFFs (COG) or standard GeoTIFF. The dataset contains multiple subsets of data which were each commissioned and flown in response to different organisational requirements. The details of each can be found at &lt;a href&#x3D;&quot;https://remotesensingdata.gov.scot/data#/list&quot;&gt;https://remotesensingdata.gov.scot/data#/list&lt;/a&gt;</description>
    </item>
    <item>
      <title>SnpEff &amp; SnpSift Genomic Variant Annotation Databases</title>
      <link>https://registry.opendata.aws/snpeff</link>
      <guid>https://registry.opendata.aws/snpeff</guid>
      <description>SnpEff is a variant annotation and effect prediction tool that annotates and predicts the effects of genetic variants on genes and proteins (such as amino acid changes). It supports over 38,000 genomes and provides comprehensive genomic databases for variant annotation. The databases include reference genomes, gene annotations, protein sequences, and regulatory elements from trusted sources like ENSEMBL, RefSeq, and UCSC. SnpSift complements SnpEff by providing tools to annotate genomic variants using databases, filter large genomic datasets, and manipulate annotated variants. Together, these tools provide a complete solution for genomic variant analysis, supporting research in human genetics, cancer genomics, pharmacogenomics, and model organism studies.</description>
    </item>
    <item>
      <title>nuPlan</title>
      <link>https://registry.opendata.aws/motional-nuplan</link>
      <guid>https://registry.opendata.aws/motional-nuplan</guid>
      <description>nuPlan is the world&amp;#39;s first large-scale planning benchmark for autonomous driving.</description>
    </item>
    <item>
      <title>10m Annual Land Use Land Cover (9-class)</title>
      <link>https://registry.opendata.aws/io-lulc</link>
      <guid>https://registry.opendata.aws/io-lulc</guid>
      <description>This dataset, produced by Impact Observatory, Microsoft, and Esri, displays a global map of land use and land cover (LULC)
derived from ESA Sentinel-2 imagery at 10 meter resolution for the years 2017 - 2023. Each map is a composite of LULC predictions for 9 classes throughout the year
in order to generate a representative snapshot of each year. This dataset was generated by Impact Observatory, which used billions of human-labeled pixels 
(curated by the National Geographic Society) to train a deep learning model for land classification. 
Each global map was produced by applying this model to the Sentinel-2 annual scene collections
from the Mircosoft Planetary Computer. Each of the maps has an assessed average accuracy of over 75%. These maps have been improved from Impact Observatory’s previous release and provide
a relative reduction in the amount of anomalous change between classes,
particularly between “Bare” and any of the vegetative classes
“Trees,” “Crops,” “Flooded Vegetation,” and “Rangeland”.
This updated time series of annual global maps is also re-aligned to match the ESA UTM tiling grid for Sentinel-2 imagery. Data can be accessed directly from the Registry of Open Data on AWS, from the &lt;a href&#x3D;&quot;https://api.impactobservatory.com/stac-aws/collections/io-10m-annual-lulc/items&quot;&gt;STAC 1.0.0 endpoint&lt;/a&gt;, or from the &lt;a href&#x3D;&quot;https://www.impactobservatory.com/maps-for-good/&quot;&gt;IO Store&lt;/a&gt; for a specific Area of Interest (AOI).   </description>
    </item>
    <item>
      <title>AIRS/Aqua L1C Infrared (IR) resampled and corrected radiances V6.7 (AIRICRAD) at GES DISC</title>
      <link>https://registry.opendata.aws/nasa-airicrad</link>
      <guid>https://registry.opendata.aws/nasa-airicrad</guid>
      <description>The Atmospheric Infrared Sounder (AIRS) is a grating spectrometer (R &#x3D; 1200) aboard the second Earth Observing System (EOS) polar-orbiting platform, EOS Aqua. In combination with the Advanced Microwave Sounding Unit (AMSU) and the Humidity Sounder for Brazil (HSB), AIRS constitutes an innovative atmospheric sounding group of visible, infrared, and microwave sensors. The AIRS Infrared (IR) level 1C data set contains AIRS infrared calibrated and geolocated radiances in W/m2/micron/ster. This data set is generated from AIRS level 1B data. The spectral coverage of L1C data is from 3.74 to 15.4 mm. The nominal spectral resolution lambda / delta lambda &#x3D; 1200. The spectrum is sampled twice per spectral resolution element in a total of 2645 spectral channels. A day of AIRS data is divided into 240 granules (scenes) each of 6-minute duration. For the AIRS IR measurements, an individual granule contains 135 pixels across-track and 90 along-track pixels; there are total of 135 x 90 &#x3D; 12,150 pixels per granule. AIRS employs a 49.5 degree crosstrack scanning with a 1.1 degree instantaneous field of view (IFOV) to provide twice daily coverage of essentially the entire globe in a 1:30 PM sun synchronous orbit with the 13.5 x 13.5 km2 spatial resolution at nadir. The L1C swath products are derived from the L1B swath products. The primary purpose of the level 1C is to generate the spectra of radiances without spectral gaps caused by the instrument design and bad spectral points. The AIRS L1C data can be used for comparative (with other IR measurements) studies and for weather-climate research.This is the latest version of this collection. The DOIs assigned to previous versions, which are no longer available, now direct
to this page. For this collection the switchover occurred on June 1, 2020.
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>Argoverse</title>
      <link>https://registry.opendata.aws/argoverse</link>
      <guid>https://registry.opendata.aws/argoverse</guid>
      <description>Home of the Argoverse datasets.Public datasets supported by detailed maps to test, experiment, and teach self-driving vehicles how to understand the world around them.This bucket includes the following datasets:&lt;ol&gt;
&lt;li&gt;Argoverse 1 (AV1)&lt;/li&gt;
&lt;/ol&gt;
&lt;ul&gt;
&lt;li&gt;Motion Forecasting&lt;/li&gt;
&lt;li&gt;Tracking&lt;/li&gt;
&lt;/ul&gt;
&lt;ol start&#x3D;&quot;2&quot;&gt;
&lt;li&gt;Argoverse 2 (AV2)&lt;/li&gt;
&lt;/ol&gt;
&lt;ul&gt;
&lt;li&gt;Motion Forecasting&lt;/li&gt;
&lt;li&gt;Lidar&lt;/li&gt;
&lt;li&gt;Sensor&lt;/li&gt;
&lt;/ul&gt;
&lt;ol start&#x3D;&quot;3&quot;&gt;
&lt;li&gt;Trust, but Verify (TbV)&lt;/li&gt;
&lt;/ol&gt;
&lt;ul&gt;
&lt;li&gt;Map Change Detection&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>Capella Space Synthetic Aperture Radar (SAR) Open Dataset</title>
      <link>https://registry.opendata.aws/capella_opendata</link>
      <guid>https://registry.opendata.aws/capella_opendata</guid>
      <description>Open Synthetic Aperture Radar (SAR) data from Capella Space. Capella Space is an information services company
  that provides on-demand, industry-leading, high-resolution synthetic aperture radar (SAR) Earth observation
  imagery. Through a constellation of small satellites, Capella provides easy access to frequent, timely, and
  flexible information affecting dozens of industries worldwide. Capella&amp;#39;s high-resolution SAR satellites are
  matched with unparalleled infrastructure to deliver reliable global insights that sharpen our understanding
  of the changing world – improving decisions about commerce, conservation, and security on Earth. Learn more
  at &lt;a href&#x3D;&quot;http://www.capellaspace.com&quot;&gt;www.capellaspace.com&lt;/a&gt;.</description>
    </item>
    <item>
      <title>Clinical Proteomic Tumor Analysis Consortium 3 (CPTAC-3)</title>
      <link>https://registry.opendata.aws/cptac-3</link>
      <guid>https://registry.opendata.aws/cptac-3</guid>
      <description>The Clinical Proteomic Tumor Analysis Consortium (CPTAC) is a national effort to accelerate the
understanding of the molecular basis of cancer through the application of large-scale proteome and
genome analysis, or proteogenomics. CPTAC-3 is the Phase III of the CPTAC Initiative. The dataset
contains open RNA-Seq Gene Expression Quantification data.</description>
    </item>
    <item>
      <title>CryoET Data Portal</title>
      <link>https://registry.opendata.aws/cryoet-data-portal</link>
      <guid>https://registry.opendata.aws/cryoet-data-portal</guid>
      <description>Cryo-electron tomography (cryoET) is a powerful technique for visualizing 3D structures of cellular macromolecules at near atomic resolution in their native environment. Observing the inner workings of cells in context enables better understanding about the function of healthy cells and the changes associated with disease. However, the analysis of cryoET data remains a significant bottleneck, particularly the annotation of macromolecules within a set of tomograms, which often requires a laborious and time-consuming process of manual labelling that can take months to complete. Given the current success of machine learning (ML) methods for image analysis, it seems likely that ML will have a significant impact on resolving this bottleneck. The scientific community has expressed the need to encourage further ML algorithm development by providing large training sets of annotated cryoET data in standardized formats. In response to this, we (Biohub) have established the CryoET Data Portal (&lt;a href&#x3D;&quot;https://cryoetdataportal.czscience.com/&quot;&gt;https://cryoetdataportal.czscience.com/&lt;/a&gt;) to provide biologists and developers open access to high-quality, standardized, annotated data that can be readily used to retrain or develop new annotation models and algorithms.</description>
    </item>
    <item>
      <title>DCR Office of Resilience Planning – Public File Repository</title>
      <link>https://registry.opendata.aws/vadcr-crmp-aws</link>
      <guid>https://registry.opendata.aws/vadcr-crmp-aws</guid>
      <description>The Virginia Department of Conservation and Recreation’s Office of Resilience Planning maintains this public file repository to provide access to flood resilience open data products. The repository is designed to house public data produced for the Virginia Coastal Resilience Master Plan (CRMP), Virginia Flood Protection Master Plan (VFPMP), and other purposes. At present, the repository hosts only data products produced for the CRMP Phase II (2025) and Phase I (2021). 
&lt;br/&gt;</description>
    </item>
    <item>
      <title>DE Africa Waterbodies Monitoring Service</title>
      <link>https://registry.opendata.aws/deafrica-waterbodies</link>
      <guid>https://registry.opendata.aws/deafrica-waterbodies</guid>
      <description>The Digital Earth Africa continental Waterbodies Monitoring Service identifies more than 700,000 water bodies from over three decades of satellite observations. This service maps persistent and seasonal water bodies and the change in their water surface area over time. Mapped water bodies may include, but are not limited to, lakes, ponds, man-made reservoirs, wetlands, and segments of some river systems.On a local, regional, and continental scale, this service helps improve our understanding of surface water dynamics and water availability and can be used for monitoring water bodies such as wetlands, lakes and dams in remote and/or inaccessible locations.</description>
    </item>
    <item>
      <title>ESM Atlas — Protein Features and Structures</title>
      <link>https://registry.opendata.aws/biohub-esm-atlas</link>
      <guid>https://registry.opendata.aws/biohub-esm-atlas</guid>
      <description>The ESM Atlas is a large-scale public dataset of computational outputs generated by ESMC and ESMFold2, derived from a deduplicated set of over 6.8 billion publicly available protein sequences spanning all domains of life — including viral proteins and previously unannotated sequences representing metagenomic dark matter sampled from a wide range of biomes. The dataset includes two primary components. A sparse autoencoder (SAE) features for ~6.8 billion proteins, capturing interpretable biological representations from the ESMC 6B model, and predicted three-dimensional protein structures for ~1.1 billion proteins generated using ESMFold2. Proteins are organized into 7.7 million clusters based on SAE feature similarity, enabling functional grouping across the protein universe. The dataset is accessible via AWS CLI. A companion data explorer is available at &lt;a href&#x3D;&quot;https://biohub.ai/esmc/atlas&quot;&gt;https://biohub.ai/esmc/atlas&lt;/a&gt;.</description>
    </item>
    <item>
      <title>EarthDEM</title>
      <link>https://registry.opendata.aws/pgc-earthdem</link>
      <guid>https://registry.opendata.aws/pgc-earthdem</guid>
      <description>EarthDEM - 2m GSD Digital Elevation Models (DEMs) and mosaics from 2002 to the present. The EarthDEM project seeks to fill the need for high-resolution time-series elevation data in non-polar regions. The time-dependent nature of the strip DEM files allows users to perform change detection analysis and to compare observations of topography data acquired in different seasons or years. The mosaic DEM tiles are assembled from multiple strip DEMs with the intention of providing a more consistent and comprehensive product over large areas. EarthDEM data is constructed from in-track and cross-track high-resolution (~0.5 meter) imagery acquired by the Maxar constellation of optical imaging satellites. Only a portion of the worldwide EarthDEM dataset is available publicly. Federally-funded researchers may access the entire dataset via NASA CSDA&amp;#39;s Smallsat Data Explorer (see Data at Work section).</description>
    </item>
    <item>
      <title>GeoJSON Files for Geo-TIDE</title>
      <link>https://registry.opendata.aws/geo_tide_geojsons</link>
      <guid>https://registry.opendata.aws/geo_tide_geojsons</guid>
      <description>GeoJSON files for the MIT Climate &amp;amp; Sustainability Consortium&amp;#39;s Geospatial Trucking Industry Decarbonization Explorer</description>
    </item>
    <item>
      <title>HYCOM-OceanTrack Integrated HYCOM Eulerian Fields and Lagrangian Trajectories Dataset</title>
      <link>https://registry.opendata.aws/hycom-global-drifters</link>
      <guid>https://registry.opendata.aws/hycom-global-drifters</guid>
      <description>A combined dataset of simulated ocean sea surface height, near-surface velocities, and particle trajectories from a global 1/25th degree HYbrid Coordinate Ocean Model (HYCOM) 1-year run.</description>
    </item>
    <item>
      <title>HYbrid Coordinate Ocean Model Global Ocean Forecast System Reanalysis</title>
      <link>https://registry.opendata.aws/hycom-gofs-3pt1-reanalysis</link>
      <guid>https://registry.opendata.aws/hycom-gofs-3pt1-reanalysis</guid>
      <description>Global Ocean Forecasting System (GOFS) 3.1 output on the GLBv0.08 grid. The resolution is 0.08° resolution between 40°S and 40°N, 0.04° poleward of these latitudes. The temportal frequenct is 3 hourly. This data was created by the Naval Research Laboratory: Ocean Dynamics and Prediction Branch.</description>
    </item>
    <item>
      <title>IBL Behavioral Data on AWS</title>
      <link>https://registry.opendata.aws/ibl-behaviour</link>
      <guid>https://registry.opendata.aws/ibl-behaviour</guid>
      <description>Behavioral data of mice performing a decision-making task, associated with 2020 publication of the IBL.</description>
    </item>
    <item>
      <title>NOAA Rapid Refresh Forecast System (RRFS) [Prototype]</title>
      <link>https://registry.opendata.aws/noaa-rrfs</link>
      <guid>https://registry.opendata.aws/noaa-rrfs</guid>
      <description>The Rapid Refresh Forecast System (RRFS) is the National Oceanic and Atmospheric Administration’s (NOAA) next generation convection-allowing, rapidly-updated ensemble prediction system, currently scheduled for operational implementation in 2026. The operational configuration will feature a 3 km grid covering North America and include deterministic forecasts every hour out to 18 hours, with deterministic and ensemble forecasts to 60 hours four times per day at 00, 06, 12, and 18 UTC.The RRFS will provide guidance to support forecast interests including, but not limited to, aviation, severe convective weather, renewable energy, heavy precipitation, and winter weather on timescales where rapidly-updated guidance is particularly useful.&lt;br/&gt;&lt;br/&gt;The RRFS is underpinned by the &lt;a href&#x3D;&quot;https://ufscommunity.org/&quot;&gt;Unified Forecast System (UFS)&lt;/a&gt;, a community-based Earth modeling initiative, and benefits from collaborative development efforts across NOAA, academia, and research institutions.&lt;br/&gt;&lt;br/&gt;This bucket provides access to a real time, pre-implementation RRFS prototype.  It also hosts some final retrospective parallel output used in the evaluation of RRFSv1&lt;br/&gt;&lt;br/&gt;&lt;hr/&gt;

The real-time RRFS output is not under 24x7 monitoring and is not operational. Output may be delayed or missing. Outputs will change. When significant changes to output take place, this description will be updated.&lt;br/&gt;&lt;br/&gt;We currently provide hourly deterministic forecasts at 3 km grid spacing out to 84 hours at 00, 06, 12, and 18 UTC, and out to 18 hours for other cycles. Output is organized by cycle date and cycle hour.We are now dividing what is provided in this bucket into a fuller set of products (intended primarily for model developers of RRFSv2 using this data to initialize their forecasts), and a more limited set of products that will approximate what we&amp;#39;ll be able to provide operationally over NOMADS.  The fuller set of data is under the rrfs_a/ subdirectory:For example, &lt;code&gt;rrfs_a/rrfs.20260114/12&lt;/code&gt; contains the deterministic forecast initialized at 12 UTC on 14 January 2026. Users will find two primary types of output in GRIB2 format. The first is:&lt;br/&gt;&lt;br/&gt;
&lt;code&gt;rrfs.t12z.natlev.3km.f018.na.grib2&lt;/code&gt; &lt;br/&gt;&lt;br/&gt;Meaning that this is the RRFS initialized at 12 UTC, covers the full North America domain, and is the native level post-processed gridded data at hour 18.  This output is on a rotated latitude-longitude grid at 3 km grid spacing.&lt;br/&gt;&lt;br/&gt;A second output file in grib2 format is:&lt;br/&gt;&lt;br/&gt;&lt;code&gt;rrfs.t12z.prslev.3km.f018.conus.grib2&lt;/code&gt; &lt;br/&gt;&lt;br/&gt;The “prslev” descriptor indicates that this post-processed gridded data is output on pressure levels. The “conus” descriptor indicates that it covers the contiguous United StatesFor users interested in other domains, output is provided on the full 3-km North American grid and also for subset over Alaska, Hawaii, and Puerto Rico. The files are identified as follows: &lt;br/&gt;&lt;br/&gt;North America: &lt;code&gt;rrfs.t00z.prslev.3km.f002.na.grib2&lt;/code&gt;
Alaska: &lt;code&gt;rrfs.t00z.prslev.3km.f002.ak.grib2&lt;/code&gt;
Hawaii: &lt;code&gt;rrfs.t00z.prslev.2p5km.f002.hi.grib2&lt;/code&gt;
Puerto Rico: &lt;code&gt;rrfs.t00z.prslev.2p5km.f002.pr.grib2&lt;/code&gt;&lt;br/&gt;&lt;br/&gt;We also provide prototype RRFSv1 ensemble output and products. Output is available for 00, 06, 12, and 18 UTC cycles, and is organized by cycle date and cycle hour. For example, &lt;code&gt;rrfs_a/rrfsens.20260115/00/m001&lt;/code&gt; contains the forecast from member 1, and &lt;code&gt;rrfs_a/refs.20260115/00/enspost_timelag&lt;/code&gt; contains the combined ensemble products.The set of files that will be available operationally over NOMADS (and which most users should use rather than the rrfs_a/ products) is under the rrfs_public/ subdirectory:Most naming conventions listed above for rrfs_a apply here as well.  However, it will not include full North America domain output, and only provides hourly output to 60 h (with 3 h resolution beyond that).  Also, only the 00/03/06/09/12/15/18/21 UTC cycles are provided.  Individual ensemble forecast members are not included, but the combined ensemble products are.  However, the combined ensemble products are under rrfs_public/refs.20260304/12/ensprod/ types of directories, which will better match the operational directory structure name.  Final retrospective parallel output is under the retro_output_final/ directory, with spring (May 2024), summer (July 2023), and winter (~Jan 8 to Feb 8, 2024) output available.</description>
    </item>
    <item>
      <title>NYU Langone &amp; FAIR FastMRI Dataset</title>
      <link>https://registry.opendata.aws/nyu-fastmri</link>
      <guid>https://registry.opendata.aws/nyu-fastmri</guid>
      <description>This dataset contains deidentified raw k-space data and DICOM image files of over 1,500 knees and 6,970 brains.</description>
    </item>
    <item>
      <title>New York City Taxi and Limousine Commission (TLC) Trip Record Data</title>
      <link>https://registry.opendata.aws/nyc-tlc-trip-records-pds</link>
      <guid>https://registry.opendata.aws/nyc-tlc-trip-records-pds</guid>
      <description>Data of trips taken by taxis and for-hire vehicles in New York City. Note: access to this dataset is free, however direct S3 access does require an AWS account. Anonymous downloads are accessible from the dataset&amp;#39;s documentation webpage listed below.</description>
    </item>
    <item>
      <title>OME-Zarr Open SciVis Datasets</title>
      <link>https://registry.opendata.aws/ome-zarr-open-scivis</link>
      <guid>https://registry.opendata.aws/ome-zarr-open-scivis</guid>
      <description>This project provides the Open SciVis Datasets in a chunked, highly-compressed, multi-scale format, encodes metadata in JSON according to the OME-Zarr specification, and hosts the datasets on AWS S3 through the AWS Open Data Program, aiming to serve as a web-based resource for the scientific visualization community to enhance reproducibility and facilitate testing and development of OME-Zarr tools.</description>
    </item>
    <item>
      <title>Open Bioinformatics Reference Data for Galaxy</title>
      <link>https://registry.opendata.aws/open-bio-ref-data</link>
      <guid>https://registry.opendata.aws/open-bio-ref-data</guid>
      <description>This dataset provides genomic reference data and software packages for use with &lt;a href&#x3D;&quot;https://galaxyproject.org/&quot;&gt;Galaxy&lt;/a&gt; and &lt;a href&#x3D;&quot;https://bioconductor.org/&quot;&gt;Bioconductor&lt;/a&gt; applications. The reference data is available for hundreds of reference genomes and has been formatted for use with a variety of tools. The available configuration files make this data easily incorporable with a local Galaxy server without additional data preparation. Additionally, Bioconductor&amp;#39;s AnnotationHub and ExperimentHub data are provided for use via R packages through which the data can be downloaded and installed into any R environment.</description>
    </item>
    <item>
      <title>OpenEEW</title>
      <link>https://registry.opendata.aws/grillo-openeew</link>
      <guid>https://registry.opendata.aws/grillo-openeew</guid>
      <description>Grillo has developed an IoT-based earthquake early-warning system,
with sensors currently deployed in Mexico, Chile, Puerto Rico and Costa Rica,
and is now opening its entire archive of unprocessed accelerometer
data to the world to encourage the development of new algorithms
capable of rapidly detecting and characterizing earthquakes in
real time.</description>
    </item>
    <item>
      <title>Pacific Ocean Sound Recordings</title>
      <link>https://registry.opendata.aws/pacific-sound</link>
      <guid>https://registry.opendata.aws/pacific-sound</guid>
      <description>This project offers passive acoustic data (sound recordings) from a deep-ocean environment off central California.  Recording began in July 2015, has been nearly continuous, and is ongoing.  These resources are intended for applications
in ocean soundscape research, education, and the arts.</description>
    </item>
    <item>
      <title>Planette C3S Seasonal Forecast Data</title>
      <link>https://registry.opendata.aws/planette_c3s_seasonal_forecast_data</link>
      <guid>https://registry.opendata.aws/planette_c3s_seasonal_forecast_data</guid>
      <description>The C3S seasonal forecast dataset provides global, daily, probabilistic forecasts of the Earth system, 
enabling users to assess the likelihood of future climate states. These forecasts are particularly 
valuable for studying slowly evolving climate patterns such as El Niño, La Niña, and the North Atlantic 
Oscillation (NAO), which can be predicted with greater skill than the chaotic atmosphere. This dataset 
is derived from the Copernicus Climate Change Service (C3S) archive and includes SEAS5 hindcasts 
(1981-2016) and forecasts (2017-present) at 1°x1° global resolution. More models from the C3S archive will
be updated as they are processed into cloud native format. The planette C3S archive stores this data in 
cloud native format for easy access and analysis. </description>
    </item>
    <item>
      <title>Planette ERA5 Archive</title>
      <link>https://registry.opendata.aws/planette_era5_reanalysis</link>
      <guid>https://registry.opendata.aws/planette_era5_reanalysis</guid>
      <description>The ERA5 archive provides a comprehensive record of global weather and climate from 1940 to present, 
with multiple temporal aggregations for flexible analysis. This dataset is derived from 
the ECMWF/Copernicus ERA5 reanalysis and includes daily means, 7-day rolling means, 
and monthly/seasonal aggregations at 0.25°×0.25° global resolution. The Planette ERA5 archive stores 
this data in cloud-native format (Zarr with icechunk) for efficient access and analysis.The dataset includes essential atmospheric variables at both surface and pressure levels, enabling a 
wide range of climate analyses, from daily weather patterns to long-term climate trends. Daily means 
are computed by averaging hourly ERA5 data, while longer temporal aggregations are derived from these 
daily means.</description>
    </item>
    <item>
      <title>PoroTomo</title>
      <link>https://registry.opendata.aws/nrel-pds-porotomo</link>
      <guid>https://registry.opendata.aws/nrel-pds-porotomo</guid>
      <description>Released to the public as part of the Department of Energy&amp;#39;s Open Energy Data
Initiative, these data represent vertical and horizontal distributed acoustic
sensing (DAS) data collected as part of the Poroelastic Tomography (PoroTomo)
project funded in part by the Office of Energy Efficiency and Renewable
Energy (EERE), U.S. Department of Energy.</description>
    </item>
    <item>
      <title>Public Utility Data Liberation Project</title>
      <link>https://registry.opendata.aws/catalyst-cooperative-pudl</link>
      <guid>https://registry.opendata.aws/catalyst-cooperative-pudl</guid>
      <description>The Public Utility Data Liberation Project (PUDL) provides analysis-ready U.S. energy
system data in bulk for programmatic use. Sources include the U.S. Energy
Information Administration (EIA), the Environmental Protection Agency (EPA), the
Federal Energy Regulatory Commission (FERC), the Pipeline and Hazardous Materials
Safety Administration (PHMSA), the Securities and Exchange Commission (SEC).  The
primary focus is on the electricity sector, with additional data on the natural gas
system and energy company financial reporting.</description>
    </item>
    <item>
      <title>RCM CEOS Analysis Ready Data | Données prêtes à l&#x27;analyse du CEOS pour le MCR</title>
      <link>https://registry.opendata.aws/rcm-ceos-ard</link>
      <guid>https://registry.opendata.aws/rcm-ceos-ard</guid>
      <description>The &lt;a href&#x3D;&quot;https://www.asc-csa.gc.ca/eng/satellites/radarsat/&quot;&gt;RADARSAT Constellation Mission (RCM)&lt;/a&gt; is Canada&amp;#39;s third generation of Earth observation satellites. Launched on June 12, 2019, the three identical satellites work together to bring solutions to key challenges for Canadians. As part of ongoing &lt;a href&#x3D;&quot;https://open.canada.ca/en/about-open-government&quot;&gt;Open Government&lt;/a&gt; efforts, NRCan produces a CEOS analysis ready data (ARD) of Canada landmass using a 30M Compact-Polarization standard coverage, every 12 days. RCM CEOS-ARD (POL) is the first ever polarimetric dataset &lt;a href&#x3D;&quot;https://ceos.org/ard/index.html#datasets&quot;&gt;approved by the CEOS committee&lt;/a&gt;. Previously, users were stuck ordering, downloading and processing RCM images (level 1) on their own, often with expensive software. This new dataset aims to remove these burdens with a new STAC catalog for discovery and direct download links.
&lt;br/&gt; &lt;br/&gt;
La mission de la Constellation RADARSAT (MCR) est la troisième génération de satellites d&amp;#39;observation de la Terre du Canada. Lancés le 12 juin 2019, les trois satellites identiques travaillent ensemble pour apporter des solutions aux principaux défis des Canadiens. Dans le cadre des efforts continus pour un gouvernement ouvert, RNCan produit des données prêtes à l&amp;#39;analyse CEOS (ARD) de la masse terrestre du Canada en utilisant une couverture standard de 30 m en polarisation compacte, tous les 12 jours. Les CEOS-ARD (POL) du MCR constituent le premier ensemble de données polarimétriques jamais &lt;a href&#x3D;&quot;https://ceos.org/ard/index.html#datasets&quot;&gt;approuvé par le comité CEOS&lt;/a&gt;. Auparavant, les utilisateurs étaient obligés de commander, de télécharger et de traiter eux-mêmes les images RCM (niveau 1), souvent à l&amp;#39;aide de logiciels coûteux. Ce nouvel ensemble de données vise à supprimer ces fardeaux avec un nouveau catalogue STAC à découvrir et à télécharger directement depuis S3.</description>
    </item>
    <item>
      <title>RarePlanes</title>
      <link>https://registry.opendata.aws/rareplanes</link>
      <guid>https://registry.opendata.aws/rareplanes</guid>
      <description>RarePlanes is a unique open-source machine learning dataset from CosmiQ Works and AI.Reverie that incorporates both real and synthetically generated satellite imagery. The RarePlanes dataset specifically focuses on the value of AI.Reverie synthetic data to aid computer vision algorithms in their ability to automatically detect aircraft and their attributes in satellite imagery. Although other synthetic/real combination datasets exist, RarePlanes is the largest openly-available very high resolution dataset built to test the value of synthetic data from an overhead perspective. The real portion of the dataset consists of 253 Maxar WorldView-3 satellite scenes spanning 112 locations and 2,142 km^2 with 14,700 hand-annotated aircraft. The accompanying synthetic dataset is generated via AI.Reverie’s novel simulation platform and features 50,000 synthetic satellite images with ~630,000 aircraft annotations.</description>
    </item>
    <item>
      <title>Sentinel-1 Monthly Mosaic</title>
      <link>https://registry.opendata.aws/deafrica-sentinel-1-mosaic</link>
      <guid>https://registry.opendata.aws/deafrica-sentinel-1-mosaic</guid>
      <description>Synthetic Aperture Radar (SAR) sensor have the advantage of operating at wavelengths not impeded by cloud cover and can acquire data over a site during the day or night. The Sentinel-1 mission, part of the Copernicus joint initiative by the European Commission (EC) and the European Space Agency (ESA), provides reliable and repeated wide-area monitoring using its SAR instrument.Sentinel-1 Monthly Mosaics are analysis-ready product of individual Sentinel-1 acquisitions. Sentinel-1 monthly mosaics are generated from Radiometric Terrain Corrected (RTC) backscatter data, with variations from changing observation geometries mitigated. RTC images acquired within a calendar month are combined using a multitemporal compositing algorithm. This algorithm calculates a weighted average of valid pixels, assigning higher weights to pixels with higher local resolution (e.g., slopes facing away from the sensor). This local resolution weighting approach minimizes noise and improves spatial homogeneity in the composites. Sinergise (Planet Labs) processed and indexed the product on the DE Africa platform</description>
    </item>
    <item>
      <title>Serratus: Ultra-deep Search for Novel Viruses - Versioned Data Release</title>
      <link>https://registry.opendata.aws/serratus-lovelywater</link>
      <guid>https://registry.opendata.aws/serratus-lovelywater</guid>
      <description>Serratus is a collaborative open science project for ultra-rapid discovery of known and unknown coronaviruses in response to the COVID-19 pandemic through re-analysis of publicly available genomic data. Our resulting vertebrate viral alignment data is explorable via the &lt;a href&#x3D;&quot;https://serratus.io/explorer&quot;&gt;Serratus Explorer&lt;/a&gt; and directly accessible on Amazon S3.</description>
    </item>
    <item>
      <title>Solar Dynamics Observatory (SDO) Machine Learning Dataset</title>
      <link>https://registry.opendata.aws/sdoml-fdl</link>
      <guid>https://registry.opendata.aws/sdoml-fdl</guid>
      <description>The v1 dataset includes AIA/HMI observations 2010-2018 and v2 includes AIA/HMI observations 2010-2020 in all 10 wavebands (94A, 131A, 171A, 193A, 211A, 304A, 335A, 1600A, 1700A, 4500A), with 512x512 resolution and 6 minutes cadence; HMI vector magnetic field observations in Bx, By, and Bz components, with 512x512 resolution and 12 minutes cadence; The EVE observations in 39 wavelengths from 2010-05-01 to 2014-05-26, with 10 seconds cadence.</description>
    </item>
    <item>
      <title>The MIT Supercloud Dataset</title>
      <link>https://registry.opendata.aws/dcc</link>
      <guid>https://registry.opendata.aws/dcc</guid>
      <description>Collection of parsed datacenter logs and time series data of hardware utilization from the MIT Supercloud system.</description>
    </item>
    <item>
      <title>Wildfire Projections to Support Climate Resilience</title>
      <link>https://registry.opendata.aws/caladapt-wildfire-dataset</link>
      <guid>https://registry.opendata.aws/caladapt-wildfire-dataset</guid>
      <description>Wildfire projections for California and her environs in support of California&amp;#39;s Fifth  Climate Assessment supported with historical weather observations and renewable energy  capacity profiles for grid operations.</description>
    </item>
    <item>
      <title>2010 Census Production Settings Demographic and Housing Characteristics (DHC) Demonstration Noisy Measurement File</title>
      <link>https://registry.opendata.aws/census-2010-dhc-nmf</link>
      <guid>https://registry.opendata.aws/census-2010-dhc-nmf</guid>
      <description>The 2010 Census Production Settings Demographic and Housing Characteristics (DHC) Demonstration Noisy Measurement File (2023-06-30) is an intermediate output of the 2020 Census Disclosure Avoidance System (DAS) TopDown Algorithm (TDA) (as described in Abowd, J. et al [2022] &lt;a href&#x3D;&quot;https://doi.org/10.1162/99608f92.529e3cb9&quot;&gt;https://doi.org/10.1162/99608f92.529e3cb9&lt;/a&gt; , and implemented in &lt;a href&#x3D;&quot;https://github.com/uscensusbureau/DAS_2020_Redistricting_Production_Code&quot;&gt;https://github.com/uscensusbureau/DAS_2020_Redistricting_Production_Code&lt;/a&gt;). The NMF was produced using the official “production settings,” the final set of algorithmic parameters and privacy-loss budget allocations, that were used to produce the 2020 Census Redistricting Data (P.L. 94-171) Summary File and the 2020 Census Demographic and Housing Characteristics File.  The NMF consists of the full set of privacy-protected statistical queries (counts of individuals or housing units with particular combinations of characteristics) of confidential 2010 Census data relating to the 2010 Demonstration Data Products Suite – Redistricting (P.L. 94-171) and Demographic and Housing Characteristics File – Production Settings (2023-04-03). These statistical queries, called “noisy measurements” were produced under the zero-Concentrated Differential Privacy framework (Bun, M. and Steinke, T [2016] &lt;a href&#x3D;&quot;https://arxiv.org/abs/1605.02065&quot;&gt;https://arxiv.org/abs/1605.02065&lt;/a&gt;; see also Dwork C. and Roth, A. [2014] &lt;a href&#x3D;&quot;https://www.cis.upenn.edu/~aaroth/Papers/privacybook.pdf&quot;&gt;https://www.cis.upenn.edu/~aaroth/Papers/privacybook.pdf&lt;/a&gt;) implemented via the discrete Gaussian mechanism (Cannone C., et al., [2023] &lt;a href&#x3D;&quot;https://arxiv.org/abs/2004.00010&quot;&gt;https://arxiv.org/abs/2004.00010&lt;/a&gt;), which added positive or negative integer-valued noise to each of the resulting counts. The noisy measurements are an intermediate stage of the TDA prior to the post-processing the TDA then performs to ensure internal and hierarchical consistency within the resulting tables. The Census Bureau has released these 2010 Census demonstration data to enable data users to evaluate the expected impact of disclosure avoidance variability on 2020 Census data. The 2010 Census Production Settings Demographic and Housing Characteristics (DHC) Demonstration Noisy Measurement File (2023-04-03) has been cleared for public dissemination by the Census Bureau Disclosure Review Board (CBDRB-FY22-DSEP-004). &lt;br/&gt; &lt;br/&gt; The 2010 Census Production Settings Demographic and Housing Characteristics Demonstration Noisy Measurement File includes zero-Concentrated Differentially Private (zCDP) (Bun, M. and Steinke, T [2016]) noisy measurements, implemented via the discrete Gaussian mechanism. These are estimated counts of individuals and housing units included in the 2010 Census Edited File (CEF), which includes confidential data initially collected in the 2010 Census of Population and Housing. The noisy measurements included in this file were subsequently post-processed by the TopDown Algorithm (TDA) to produce the 2010 Census Production Settings Privacy-Protected Microdata File - Redistricting (P.L. 94-171) and Demographic and Housing Characteristics File (2023-04-03) (&lt;a href&#x3D;&quot;https://www2.census.gov/programs-surveys/decennial/2020/program-management/data-product-planning/2010-demonstration-data-products/04-Demonstration_Data_Products_Suite/2023-04-03/&quot;&gt;https://www2.census.gov/programs-surveys/decennial/2020/program-management/data-product-planning/2010-demonstration-data-products/04-Demonstration_Data_Products_Suite/2023-04-03/&lt;/a&gt;). As these 2010 Census demonstration data are intended to support study of the design and expected impacts of the 2020 Disclosure Avoidance System, the 2010 CEF records were pre-processed before application of the zCDP framework. This pre-processing converted the 2010 CEF records into the input-file format, response codes, and tabulation categories used for the 2020 Census, which differ in substantive ways from the format, response codes, and tabulation categories originally used for the 2010 Census. &lt;br/&gt; &lt;br/&gt; The NMF provides estimates of counts of persons in the CEF by various characteristics and combinations of characteristics including their reported race and ethnicity, whether they were of voting age, whether they resided in a housing unit or one of 7 group quarters types, and their census block of residence after the addition of discrete Gaussian noise (with the scale parameter determined by the privacy-loss budget allocation for that particular query under zCDP). Noisy measurements of the counts of occupied and vacant housing units by census block are also included. Lastly, data on constraints—information into which no noise was infused by the Disclosure Avoidance System (DAS) and used by the TDA to post-process the noisy measurements into the 2010 Census Production Settings Privacy-Protected Microdata File - Redistricting (P.L. 94-171) and Demographic and Housing Characteristics File (2023-04-03) —are provided.</description>
    </item>
    <item>
      <title>2020 Census Demographic and Housing Characteristics (DHC) Noisy Measurement File</title>
      <link>https://registry.opendata.aws/census-2020-dhc-nmf</link>
      <guid>https://registry.opendata.aws/census-2020-dhc-nmf</guid>
      <description>The 2020 Census Demographic and Housing Characteristics Noisy Measurement File is an intermediate output of the 2020 Census Disclosure Avoidance System (DAS) TopDown Algorithm (TDA) (as described in Abowd, J. et al [2022], and implemented in &lt;a href&#x3D;&quot;https://github.com/uscensusbureau/DAS_2020_DHC_Production_Code/blob/main/das_decennial/programs/engine/primitives.py&quot;&gt;primitives.py&lt;/a&gt;). The 2020 Census Demographic and Housing Characteristics Noisy Measurement File includes zero-Concentrated Differentially Private (zCDP) (Bun, M. and Steinke, T [2016]) noisy measurements, implemented via the discrete Gaussian mechanism (Cannone C., et al., [2023] ), which added positive or negative integer-valued noise to each of the resulting counts. These are estimated counts of individuals and housing units included in the 2020 Census Edited File (CEF), which includes confidential data collected in the 2020 Census of Population and Housing.
&lt;br/&gt;
&lt;br/&gt;
The noisy measurements included in this file were subsequently post-processed by the TopDown Algorithm (TDA) to produce the Census Demographic and Housing Characteristics Summary File. In addition to the noisy measurements, constraints based on invariant calculations --- counts computed without noise --- are also included (with the exception of the state-level total populations, which can be sourced separately from data.census.gov).
&lt;br/&gt;
&lt;br/&gt;
The Noisy Measurement File was produced using the official “production settings,” the final set of algorithmic parameters and privacy-loss budget allocations that were used to produce the 2020 Census Redistricting Data (P.L. 94-171) Summary File and the 2020 Census Demographic and Housing Characteristics File.
&lt;br/&gt;
&lt;br/&gt;
The noisy measurements are produced in an early stage of the TDA. Afterward, these noisy measurements are post-processed to ensure internal and hierarchical consistency within the resulting tables. The Census Bureau has released these noisy measurements to enable data users to evaluate the impact of disclosure avoidance variability on 2020 Census data. The 2020 Census Demographic and Housing Characteristics (DHC) Noisy Measurement File has been cleared for public dissemination by the Census Bureau Disclosure Review Board (CBDRB-FY22-DSEP-004).
&lt;br/&gt;
&lt;br/&gt;</description>
    </item>
    <item>
      <title>3000 Rice Genomes Project</title>
      <link>https://registry.opendata.aws/3kricegenome</link>
      <guid>https://registry.opendata.aws/3kricegenome</guid>
      <description>The 3000 Rice Genome Project is an international effort to sequence the genomes of 3,024 rice varieties from 89 countries.</description>
    </item>
    <item>
      <title>AWS Public Blockchain Data</title>
      <link>https://registry.opendata.aws/aws-public-blockchain</link>
      <guid>https://registry.opendata.aws/aws-public-blockchain</guid>
      <description>&lt;p&gt;The AWS Public Blockchain Data initiative provides free access to blockchain datasets through collaboration with data providers. The data is optimized for analytics by being transformed into compressed Parquet files, partitioned by date for efficient querying.&lt;/p&gt;
&lt;h4&gt;Datasets&lt;/h4&gt; &lt;b&gt;Blockchain dataset - Maintained by - Path:&lt;/b&gt;&lt;br&gt; - Bitcoin                 - AWS     - &lt;code&gt;s3://aws-public-blockchain/v1.0/btc/&lt;/code&gt;&lt;br&gt; - Ethereum                - AWS     - &lt;code&gt;s3://aws-public-blockchain/v1.0/eth/&lt;/code&gt;&lt;br&gt; - Aptos                   - SonarX  - &lt;code&gt;s3://aws-public-blockchain/v1.1/sonarx/aptos/&lt;/code&gt;&lt;br&gt; - Arbitrum                - SonarX  - &lt;code&gt;s3://aws-public-blockchain/v1.1/sonarx/arbitrum/&lt;/code&gt;&lt;br&gt; - Base                    - SonarX  - &lt;code&gt;s3://aws-public-blockchain/v1.1/sonarx/base/&lt;/code&gt;&lt;br&gt; - BNB Chain               - BNB Chain - &lt;code&gt;s3://aws-public-blockchain/v1.1/bnb/&lt;/code&gt;&lt;br&gt; - Cronos                  - Cronos - &lt;code&gt;s3://aws-public-blockchain/v1.1/cronos/&lt;/code&gt;&lt;br&gt; - Provenance              - SonarX  - &lt;code&gt;s3://aws-public-blockchain/v1.1/sonarx/provenance/&lt;/code&gt;&lt;br&gt; - Stellar(&lt;a href&#x3D;&quot;https://developers.stellar.org/docs/learn/fundamentals/data-format/xdr&quot; rel&#x3D;&quot;noopener noreferrer&quot;&gt;XDR files&lt;/a&gt;) - Stellar - &lt;code&gt;s3://aws-public-blockchain/v1.1/stellar/&lt;/code&gt;&lt;br&gt; - The Open Network (TON)  - TON - &lt;code&gt;s3://aws-public-blockchain/v1.1/ton/&lt;/code&gt;&lt;br&gt; - XRP Ledger              - SonarX  - &lt;code&gt;s3://aws-public-blockchain/v1.1/sonarx/xrp/&lt;/code&gt;&lt;br&gt; &lt;/br&gt; 
&lt;h4&gt;Become a Data Provider&lt;/h4&gt; &lt;p&gt;We welcome additional blockchain data providers to join this initiative. If you&#x27;re interested in contributing datasets to the AWS Public Blockchain Data program, please contact our team at &lt;a href&#x3D;&quot;mailto:aws-public-blockchain@amazon.com&quot;&gt;aws-public-blockchain@amazon.com&lt;/a&gt;.&lt;/p&gt;
</description>
    </item>
    <item>
      <title>Amazonia EO satellite on AWS</title>
      <link>https://registry.opendata.aws/amazonia</link>
      <guid>https://registry.opendata.aws/amazonia</guid>
      <description>Imagery acquired
by Amazonia-1 satellite.
The
image files are recorded and processed by Instituto Nacional de Pesquisas
Espaciais (INPE) and are converted to Cloud Optimized Geotiff
format in order to optimize its use for cloud based applications.
WFI Level 4 (Orthorectified) scenes are being
ingested daily starting from 08-29-2022, the complete
Level 4 archive will be ingested by the end of October 2022.</description>
    </item>
    <item>
      <title>Argo marine floats data and metadata from Global Data Assembly Centre (Argo GDAC)</title>
      <link>https://registry.opendata.aws/argo-gdac-marinedata</link>
      <guid>https://registry.opendata.aws/argo-gdac-marinedata</guid>
      <description>Argo is an international program to observe the interior of the ocean with a fleet of profiling floats drifting in the deep ocean currents (&lt;a href&#x3D;&quot;https://argo.ucsd.edu&quot;&gt;https://argo.ucsd.edu&lt;/a&gt;). Argo GDAC is a dataset of 5 billion in situ ocean observations from 18.000 profiling floats (4.000 active) which started 20 years ago. Argo GDAC dataset is a collection of 18.000 NetCDF files.   It is a major asset for ocean and climate science, a contributor to IOCCP reports.</description>
    </item>
    <item>
      <title>Automated Segmentation of Intracellular Substructures in Electron Microscopy (ASEM) on AWS</title>
      <link>https://registry.opendata.aws/asem-project</link>
      <guid>https://registry.opendata.aws/asem-project</guid>
      <description>The Automated Segmentation of intracellular substructures in Electron Microscopy (ASEM) project provides deep learning models trained to segment structures in 3D images of cells acquired by Focused Ion Beam Scanning Electron Microscopy (FIB-SEM). Each model is trained to detect a single type of structure (mitochondria, endoplasmic reticulum, golgi apparatus, nuclear pores, clathrin-coated pits) in cells prepared via chemically-fixation (CF) or high-pressure freezing and freeze substitution (HPFS). You can use our open source pipeline to load a model and predict a class of sub-cellular structures in naive FIB-SEM cells images. If required, a fine-tuning procedure allows a model to be trained on a small amount of additional ground truth annotations to improve a prediction on a naive dataset. Together with the trained models, we also provide the training, validation and test datasets.</description>
    </item>
    <item>
      <title>CAM6 Data Assimilation Research Testbed (DART) Reanalysis: Cloud-Optimized Dataset</title>
      <link>https://registry.opendata.aws/ncar-dart-cam6</link>
      <guid>https://registry.opendata.aws/ncar-dart-cam6</guid>
      <description>This is a cloud-hosted subset of the CAM6+DART (Community Atmosphere Model version 6 Data Assimilation Research Testbed) Reanalysis dataset. These data products are designed to facilitate a broad variety of research using the NCAR CESM 2.1 (National Center for Atmospheric Research&amp;#39;s Community Earth System Model version 2.1), including model evaluation, ensemble hindcasting, data assimilation experiments, and sensitivity studies. They come from an 80 member ensemble reanalysis of the global troposphere and stratosphere using DART and CAM6. The data products represent states of the atmosphere consistent with observations from 2011 through 2019 at 1 degree horizontal resolution and weekly frequency. Each ensemble member is an equally likely description of the atmosphere, and is also consistent with dynamics and physics of CAM6. The dataset also contains corresponding land surface values at 6-hourly frequency.  This dataset is a reformatting, with no change to numerical values, of data from the &amp;quot;CAM6 Data Assimilation Research Testbed (DART) Reanalysis&amp;quot;, &lt;a href&#x3D;&quot;https://doi.org/10.5065/JG1E-8525&quot;&gt;DOI:10.5065/JG1E-8525&lt;/a&gt;.</description>
    </item>
    <item>
      <title>CAncer MEtastases in LYmph nOdes challeNge (CAMELYON) Dataset</title>
      <link>https://registry.opendata.aws/camelyon</link>
      <guid>https://registry.opendata.aws/camelyon</guid>
      <description>&amp;quot;This dataset contains the all data for the &lt;a href&#x3D;&quot;https://camelyon17.grand-challenge.org&quot;&gt;CAncer MEtastases in LYmph nOdes challeNge or CAMELYON&lt;/a&gt;. CAMELYON was the first challenge using whole-slide images in computational pathology and aimed to help pathologists identify breast cancer metastases in sentinel lymph nodes. Lymph node metastases are extremely important to find, as they indicate that the cancer is no longer localized and systemic treatment might be warranted. Searching for these metastases in H&amp;amp;E-stained tissue is difficult and time-consuming and AI algorithms can play a role in helping make this faster and more accurate.</description>
    </item>
    <item>
      <title>CESM-HR</title>
      <link>https://registry.opendata.aws/cesm-hr</link>
      <guid>https://registry.opendata.aws/cesm-hr</guid>
      <description>This dataset provides several global fields describing the state of atmosphere, ocean, land and ice from a high-resolution (0.1o for the ocean/ice models 0.25o for the land/atmosphere models) numerical earth system model, the Community Earth System Model (CESM, &lt;a href&#x3D;&quot;https://www.cesm.ucar.edu/&quot;&gt;https://www.cesm.ucar.edu/&lt;/a&gt;). Texas A&amp;amp;M University (TAMU) and National Center for Atmospheric Research together with international partners collaboratively carried out a large set of high-resolution climate simulations, including a 500-year long preindustrial control simulation (PI-CTRL) described here. The CESM uses dynamic equations with a climatological (observations, long-term averaged) initial state of the earth system and the preindustrial greenhouse gas forcing (kept constant at the 1850 conditions) for making this PI-CTRL. Compared to standard low-resolution (1o) CMIP-class simulations, this high-resolution simulation dataset enables researchers to explore the contribution from processes at a wide range of spatial scales, from mesoscales to global scales, in shaping various observed climate phenomena with better accuracy.</description>
    </item>
    <item>
      <title>CMAS Data Warehouse</title>
      <link>https://registry.opendata.aws/cmas-data-warehouse</link>
      <guid>https://registry.opendata.aws/cmas-data-warehouse</guid>
      <description>CMAS Data Warehouse on AWS collects and disseminates meteorology, emissions and air quality model input and output for Community Multiscale Air Quality (CMAQ) Model Applications. This dataset is available as part of the AWS Open Data Program, therefore egress fees are not charged to either the host or the person downloading the data.  This S3 bucket is maintained as a public service by the University of North Carolina&amp;#39;s CMAS Center, the US EPA’s Office of Research and Development, and the US EPA’s Office of Air and Radiation.  Metadata and DOIs for datasets included in the CMAS Data Warehouse are available from the CMAS Dataverse site: &lt;a href&#x3D;&quot;https://dataverse.unc.edu/dataverse/cmascenter&quot;&gt;https://dataverse.unc.edu/dataverse/cmascenter&lt;/a&gt; </description>
    </item>
    <item>
      <title>Caenorabditis Diversity Natural Resource</title>
      <link>https://registry.opendata.aws/caendr</link>
      <guid>https://registry.opendata.aws/caendr</guid>
      <description>The Caenorhabditis Natural Diversity Resource (CaeNDR) is a data repository and analysis hub of wild strains of selfing Caenhorabditis species C. elegans, C. briggsae, and C. tropicalis from around the world to facilitate discovery of genetic variation across all three species through genome-wide association mappings to correlate genotype with phenotype and identify genetic variation underlying quantitative traits.</description>
    </item>
    <item>
      <title>CoMMpass from the Multiple Myeloma Research Foundation</title>
      <link>https://registry.opendata.aws/mmrf-commpass</link>
      <guid>https://registry.opendata.aws/mmrf-commpass</guid>
      <description>The Relating Clinical Outcomes in Multiple Myeloma to Personal Assessment of Genetic Profile study is the Multiple Myeloma Research Foundation (MMRF)’s landmark personalized medicine initiative.  CoMMpass is a
longitudinal observation study of around 1000 newly diagnosed myeloma patients receiving various
standard approved treatments. The MMRF’s vision is to track the treatment and results for each
CoMMpass patient so that someday the information can be used to guide decisions for newly
diagnosed patients. CoMMpass checked on patients every 6 months for 8 years, collecting tissue
samples, genetic, information, quality of life and various disease and clinical outcomes. The
study has produced one of the largest genomic and clinical datasets of a single disease.</description>
    </item>
    <item>
      <title>Community Earth System Model Large Ensemble (CESM LENS)</title>
      <link>https://registry.opendata.aws/ncar-cesm-lens</link>
      <guid>https://registry.opendata.aws/ncar-cesm-lens</guid>
      <description>The Community Earth System Model (CESM) Large Ensemble Numerical Simulation (LENS) dataset includes a 40-member ensemble of climate simulations for the period 1920-2100 using historical data (1920-2005) or assuming the RCP8.5 greenhouse gas concentration scenario (2006-2100), as well as longer control runs based on pre-industrial conditions. The data comprise both surface (2D) and volumetric (3D) variables in the atmosphere, ocean, land, and ice domains. The total data volume of the original dataset is ~500TB, which has traditionally been stored as ~150,000 individual CF/NetCDF files on disk or magnetic tape made available through the NCAR Climate Data Gateway for download or via web services.   NCAR has copied a subset (currently ~70 TB) of CESM LENS data to Amazon S3 as part of the AWS Public Datasets Program. To optimize for large-scale analytics we have represented the data as ~275 Zarr stores format accessible through the Python Xarray library. Each Zarr store contains a single physical variable for a given model run type and temporal frequency (monthly, daily, 6-hourly).</description>
    </item>
    <item>
      <title>Daylight Map Distribution of OpenStreetMap</title>
      <link>https://registry.opendata.aws/daylight-osm</link>
      <guid>https://registry.opendata.aws/daylight-osm</guid>
      <description>Daylight is a complete distribution of global, open map data that’s freely available with support from community and professional mapmakers. Meta combines the work of global contributors to projects like OpenStreetMap with quality and consistency checks from Daylight mapping partners to create a free, stable, and easy-to-use street-scale global map. &lt;br/&gt;&lt;br/&gt;
The Daylight Map Distribution contains a validated subset of the OpenStreetMap database. In addition to the standard OpenStreetMap PBF format, Daylight is available in two parquet formats that are optimized for AWS Athena including geometries (Points, LineStrings, Polygons, or MultiPolygons). First, &lt;strong&gt;Daylight OSM Features&lt;/strong&gt; contains the nearly 1B renderable OSM features. Second, &lt;strong&gt;Daylight OSM Elements&lt;/strong&gt; contains all of OSM, including all 7B nodes without attributes, and relations that do not contain geometries, such as turn restrictions. &lt;br/&gt;&lt;br/&gt; 
Daylight Earth Table is a new data schema that classifies OpenStreetMap-style tags into a 3-level ontology (theme, class, subclass) and is the result of running the earth table classification over the latest release (v1.18) of the Daylight Map Distribution. The Daylight Earth Table is available as parquet files on Amazon S3. </description>
    </item>
    <item>
      <title>EEGDash on AWS</title>
      <link>https://registry.opendata.aws/eegdash</link>
      <guid>https://registry.opendata.aws/eegdash</guid>
      <description>The EEG-DaSh (EEG Data Sharing) data archive is a large-scale data-sharing resource for magnetoencephalography and electroencephalography (MEEG) data hosted at the Swartz Center for Computational Neuroscience (SCCN), UC San Diego. It provides curated, BIDS-formatted datasets for neuroscience research, machine learning, and deep learning applications. The archive spans three S3 buckets: (1) the EEGDash bucket for data served through the EEGDash platform, (2) the NEMAR archive containing datasets contributed through the NEMAR (Neuroelectromagnetic Data Archive and Tools Resource) platform, which serves as the upstream data source for EEGDash, and (3) a competition-specific collection of datasets adapted and preprocessed for machine learning benchmarks and competitions.</description>
    </item>
    <item>
      <title>ESA WorldCover Sentinel-1 and Sentinel-2 10m Annual Composites</title>
      <link>https://registry.opendata.aws/esa-worldcover-vito-composites</link>
      <guid>https://registry.opendata.aws/esa-worldcover-vito-composites</guid>
      <description>The WorldCover 10m Annual Composites were produced, as part of the European Space Agency (ESA) WorldCover project, from the yearly Copernicus Sentinel-1 and Sentinel-2 archives for both years 2020 and 2021. These global mosaics consists of four products composites. A Sentinel-2 RGBNIR yearly median composite for bands B02, B03, B04, B08. A Sentinel-2 SWIR yearly median composite for bands B11 and B12. A Sentinel-2 NDVI yearly percentiles composite (NDVI 90th, NDVI 50th NDVI 10th percentiles). A Sentinel-1 GAMMA0 yearly median composite for bands VV, VH and VH/VV (power scaled). Each product is delivered as a series of Cloud-Optimized GeoTIFFs (COGs) in WSG84 projection in a grid of 1 by 1 degrees and at 0.3 arc seconds resolution (approx. 10m), except for the SWIR composite which is delivered at 0.6 arc seconds (approx. 20m). The Sentinel-2 composites were produced from the L2A archive. The GAMMA0 composite was produced by pre-processing the Sentinel-1 GRD products using &lt;a href&#x3D;&quot;https://www.gamma-rs.ch/&quot;&gt;GAMMA software&lt;/a&gt;.</description>
    </item>
    <item>
      <title>End-Use Load Profiles for the U.S. Building Stock</title>
      <link>https://registry.opendata.aws/nrel-pds-building-stock</link>
      <guid>https://registry.opendata.aws/nrel-pds-building-stock</guid>
      <description>The U.S. Department of Energy (DOE) funded a three-year project, End-Use Load Profiles for the U.S. Building Stock, that culminated in this publicly
available dataset of calibrated and validated 15-minute resolution load profiles for all major residential and commercial building types and end uses,
across all climate regions in the United States. These EULPs were created by calibrating the ResStock and ComStock physics-based building stock models
using many different measured datasets, as described &lt;a href&#x3D;&quot;https://www.nrel.gov/docs/fy22osti/80889.pdf&quot;&gt;here&lt;/a&gt;.
This dataset includes load profiles for both the baseline building stock and the building stock with various energy efficiency, electrification,
and demand flexibility upgrades applied.</description>
    </item>
    <item>
      <title>GPM IMERG Early Precipitation L3 Half Hourly 0.1 degree x 0.1 degree V07 (GPM_3IMERGHHE) at GES DISC</title>
      <link>https://registry.opendata.aws/nasa-gpm3imerghhe</link>
      <guid>https://registry.opendata.aws/nasa-gpm3imerghhe</guid>
      <description>Version 07B is the current version of the IMERG data sets. Older versions will no longer be available and have been superseded by Version 07.The Integrated Multi-satellitE Retrievals for GPM (IMERG) is the unified U.S. algorithm that provides the multi-satellite precipitation product for the U.S. GPM team.The precipitation estimates from the various precipitation-relevant satellite passive microwave (PMW) sensors comprising the GPM constellation are computed using the 2021 version of the Goddard Profiling Algorithm (GPROF2021), then gridded, intercalibrated to the GPM Combined Ku Radar-Radiometer Algorithm (CORRA) product, and merged into half-hourly 0.1°x0.1° (roughly 10x10 km) fields. Note that CORRA is adjusted to the monthly Global Precipitation Climatology Project (GPCP) Satellite-Gauge (SG) product over high-latitude ocean to correct known biases.The half-hourly intercalibrated merged PMW estimates are then input to both a Morphing-Kalman Filter (KF) Lagrangian time interpolation scheme based on work by the Climate Prediction Center (CPC) and the Precipitation Estimation from Remotely Sensed Information using Artificial Neural Networks (PERSIANN) Dynamic Infrared–Rain Rate (PDIR) re-calibration scheme. In parallel, CPC assembles the zenith-angle-corrected, intercalibrated merged geo-IR fields and forwards them to PPS for input to the PERSIANN-CCS algorithm (supported by an asynchronous re-calibration cycle) which are then input to the KF morphing (quasi-Lagrangian time interpolation) scheme.The KF morphing (supported by an asynchronous KF weights updating cycle) uses the PMW and IR estimates to create half-hourly estimates. Motion vectors for the morphing are computed by maximizing the pattern correlation of successive hours within each of the precipitation (PRECTOT), total precipitable liquid water (TQL), and vertically integrated vapor (TQV) data fields provided by the Modern-Era Retrospective Analysis for Research and Applications, Version 2 (MERRA-2) and Goddard Earth Observing System model Version 5 (GEOS-5) Forward Processing (FP) for the post-real-time (Final) Run and the near-real-time (Early and Late) Runs, respectively. The vectors from PRECTOT are chosen if available, else from TQL, if available, else from TQV. The KF uses the morphed data as the “forecast” and the IR estimates as the “observations”, with weighting that depends on the time interval(s) away from the microwave overpass time. The IR becomes important after about ±90 minutes away from the overpass time. Variable averaging in the KF is accounted for in a routine (Scheme for Histogram Adjustment with Ranked Precipitation Estimates in the Neighborhood, or SHARPEN) that compares the local histogram of KF morphed precipitation to the local histogram of forward- and backward-morphed microwave data and the IR.The IMERG system is run twice in near-real time:&amp;quot;Early&amp;quot; multi-satellite product ~4 hr after observation time using only forward morphing and
&amp;quot;Late&amp;quot; multi-satellite product ~14 hr after observation time, using both forward and backward morphing
and once after the monthly gauge analysis is received:&amp;quot;Final&amp;quot;, satellite-gauge product ~4 months after the observation month, using both forward and backward morphing and including monthly gauge analyses.In V07, the near-real-time Early and Late half-hourly estimates have a monthly climatological concluding calibration based on averaging the concluding calibrations computed in the Final, while in the post-real-time Final Run the multi-satellite half-hourly estimates are adjusted so that they sum to the Final Run monthly satellite-gauge combination. In all cases the output contains multiple fields that provide information on the input data, selected intermediate fields, and estimation quality. In general, the complete calibrated precipitation, precipitation, is the data field of choice for most users.Precipitation phase is a diagnostic variable computed using analyses of surface temperature, humidity, and pressure. 
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>GPM IMERG Final Precipitation L3 1 month 0.1 degree x 0.1 degree V07 (GPM_3IMERGM) at GES DISC</title>
      <link>https://registry.opendata.aws/nasa-gpm3imergm</link>
      <guid>https://registry.opendata.aws/nasa-gpm3imergm</guid>
      <description>Version 07B is the current version of the IMERG data sets. Older versions will no longer be available and have been superseded by Version 07.The Integrated Multi-satellitE Retrievals for GPM (IMERG) is the unified U.S. algorithm that provides the multi-satellite precipitation product for the U.S. GPM team.The precipitation estimates from the various precipitation-relevant satellite passive microwave (PMW) sensors comprising the GPM constellation are computed using the 2021 version of the Goddard Profiling Algorithm (GPROF2021), then gridded, intercalibrated to the GPM Combined Ku Radar-Radiometer Algorithm (CORRA) product, and merged into half-hourly 0.1°x0.1° (roughly 10x10 km) fields. Note that CORRA is adjusted to the monthly Global Precipitation Climatology Project (GPCP) Satellite-Gauge (SG) product over high-latitude ocean to correct known biases.The half-hourly intercalibrated merged PMW estimates are then input to both a Morphing-Kalman Filter (KF) Lagrangian time interpolation scheme based on work by the Climate Prediction Center (CPC) and the Precipitation Estimation from Remotely Sensed Information using Artificial Neural Networks (PERSIANN) Dynamic Infrared–Rain Rate (PDIR) re-calibration scheme. In parallel, CPC assembles the zenith-angle-corrected, intercalibrated merged geo-IR fields and forwards them to PPS for input to the PERSIANN-CCS algorithm (supported by an asynchronous re-calibration cycle) which are then input to the KF morphing (quasi-Lagrangian time interpolation) scheme.The KF morphing (supported by an asynchronous KF weights updating cycle) uses the PMW and IR estimates to create half-hourly estimates. Motion vectors for the morphing are computed by maximizing the pattern correlation of successive hours within each of the precipitation (PRECTOT), total precipitable liquid water (TQL), and vertically integrated vapor (TQV) data fields provided by the Modern-Era Retrospective Analysis for Research and Applications, Version 2 (MERRA-2) and Goddard Earth Observing System model Version 5 (GEOS-5) Forward Processing (FP) for the post-real-time (Final) Run and the near-real-time (Early and Late) Runs, respectively. The vectors from PRECTOT are chosen if available, else from TQL, if available, else from TQV. The KF uses the morphed data as the “forecast” and the IR estimates as the “observations”, with weighting that depends on the time interval(s) away from the microwave overpass time. The IR becomes important after about ±90 minutes away from the overpass time. Variable averaging in the KF is accounted for in a routine (Scheme for Histogram Adjustment with Ranked Precipitation Estimates in the Neighborhood, or SHARPEN) that compares the local histogram of KF morphed precipitation to the local histogram of forward- and backward-morphed microwave data and the IR.The IMERG system is run twice in near-real time:&amp;quot;Early&amp;quot; multi-satellite product ~4 hr after observation time using only forward morphing and
&amp;quot;Late&amp;quot; multi-satellite product ~14 hr after observation time, using both forward and backward morphing
and once after the monthly gauge analysis is received:&amp;quot;Final&amp;quot;, satellite-gauge product ~4 months after the observation month, using both forward and backward morphing and including monthly gauge analyses.In V07, the near-real-time Early and Late half-hourly estimates have a monthly climatological concluding calibration based on averaging the concluding calibrations computed in the Final, while in the post-real-time Final Run the multi-satellite half-hourly estimates are adjusted so that they sum to the Final Run monthly satellite-gauge combination. In all cases the output contains multiple fields that provide information on the input data, selected intermediate fields, and estimation quality. In general, the complete calibrated precipitation, precipitation, is the data field of choice for most users.Briefly describing the Final Run, the input precipitation estimates computed from the various satellite passive microwave sensors are intercalibrated to the CORRA product (because it is presumed to be the best snapshot TRMM/GPM estimate after adjustment to the monthly GPCP SG), then &amp;quot;forward/backward morphed&amp;quot; and combined with microwave precipitation-calibrated geo-IR fields, and adjusted with seasonal GPCP SG surface precipitation data to provide half-hourly and monthly precipitation estimates on a 0.1°x0.1° (roughly 10x10 km) grid over the globe. Precipitation phase is a diagnostic variable computed using analyses of surface temperature, humidity, and pressure. The current period of record is June 2000 to the present (delayed by about 4 months).
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>GPM IMERG Final Precipitation L3 Half Hourly 0.1 degree x 0.1 degree V07 (GPM_3IMERGHH) at GES DISC</title>
      <link>https://registry.opendata.aws/nasa-gpm3imerghh</link>
      <guid>https://registry.opendata.aws/nasa-gpm3imerghh</guid>
      <description>Version 07B is the current version of the IMERG data sets. Older versions will no longer be available and have been superseded by Version 07.The Integrated Multi-satellitE Retrievals for GPM (IMERG) is the unified U.S. algorithm that provides the multi-satellite precipitation product for the U.S. GPM team.The precipitation estimates from the various precipitation-relevant satellite passive microwave (PMW) sensors comprising the GPM constellation are computed using the 2021 version of the Goddard Profiling Algorithm (GPROF2021), then gridded, intercalibrated to the GPM Combined Ku Radar-Radiometer Algorithm (CORRA) product, and merged into half-hourly 0.1°x0.1° (roughly 10x10 km) fields. Note that CORRA is adjusted to the monthly Global Precipitation Climatology Project (GPCP) Satellite-Gauge (SG) product over high-latitude ocean to correct known biases.The half-hourly intercalibrated merged PMW estimates are then input to both a Morphing-Kalman Filter (KF) Lagrangian time interpolation scheme based on work by the Climate Prediction Center (CPC) and the Precipitation Estimation from Remotely Sensed Information using Artificial Neural Networks (PERSIANN) Dynamic Infrared–Rain Rate (PDIR) re-calibration scheme. In parallel, CPC assembles the zenith-angle-corrected, intercalibrated merged geo-IR fields and forwards them to PPS for input to the PERSIANN-CCS algorithm (supported by an asynchronous re-calibration cycle) which are then input to the KF morphing (quasi-Lagrangian time interpolation) scheme.The KF morphing (supported by an asynchronous KF weights updating cycle) uses the PMW and IR estimates to create half-hourly estimates. Motion vectors for the morphing are computed by maximizing the pattern correlation of successive hours within each of the precipitation (PRECTOT), total precipitable liquid water (TQL), and vertically integrated vapor (TQV) data fields provided by the Modern-Era Retrospective Analysis for Research and Applications, Version 2 (MERRA-2) and Goddard Earth Observing System model Version 5 (GEOS-5) Forward Processing (FP) for the post-real-time (Final) Run and the near-real-time (Early and Late) Runs, respectively. The vectors from PRECTOT are chosen if available, else from TQL, if available, else from TQV. The KF uses the morphed data as the “forecast” and the IR estimates as the “observations”, with weighting that depends on the time interval(s) away from the microwave overpass time. The IR becomes important after about ±90 minutes away from the overpass time. Variable averaging in the KF is accounted for in a routine (Scheme for Histogram Adjustment with Ranked Precipitation Estimates in the Neighborhood, or SHARPEN) that compares the local histogram of KF morphed precipitation to the local histogram of forward- and backward-morphed microwave data and the IR.The IMERG system is run twice in near-real time:&amp;quot;Early&amp;quot; multi-satellite product ~4 hr after observation time using only forward morphing and
&amp;quot;Late&amp;quot; multi-satellite product ~14 hr after observation time, using both forward and backward morphing
and once after the monthly gauge analysis is received:&amp;quot;Final&amp;quot;, satellite-gauge product ~4 months after the observation month, using both forward and backward morphing and including monthly gauge analyses.In V07, the near-real-time Early and Late half-hourly estimates have a monthly climatological concluding calibration based on averaging the concluding calibrations computed in the Final, while in the post-real-time Final Run the multi-satellite half-hourly estimates are adjusted so that they sum to the Final Run monthly satellite-gauge combination. In all cases the output contains multiple fields that provide information on the input data, selected intermediate fields, and estimation quality. In general, the complete calibrated precipitation, precipitation, is the data field of choice for most users.Briefly describing the Final Run, the input precipitation estimates computed from the various satellite passive microwave sensors are intercalibrated to the CORRA product (because it is presumed to be the best snapshot TRMM/GPM estimate after adjustment to the monthly GPCP SG), then &amp;quot;forward/backward morphed&amp;quot; and combined with microwave precipitation-calibrated geo-IR fields, and adjusted with seasonal GPCP SG surface precipitation data to provide half-hourly and monthly precipitation estimates on a 0.1°x0.1° (roughly 10x10 km) grid over the globe. Precipitation phase is a diagnostic variable computed using analyses of surface temperature, humidity, and pressure. The current period of record is June 2000 to the present (delayed by about 4 months).
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>GPM IMERG Late Precipitation L3 Half Hourly 0.1 degree x 0.1 degree V07 (GPM_3IMERGHHL) at GES DISC</title>
      <link>https://registry.opendata.aws/nasa-gpm3imerghhl</link>
      <guid>https://registry.opendata.aws/nasa-gpm3imerghhl</guid>
      <description>Version 07B is the current version of the IMERG data sets. Older versions
will no longer be available and have been superseded by Version 07.\n\nThe Integrated
Multi-satellitE Retrievals for GPM (IMERG) is the unified U.S. algorithm that provides
the multi-satellite precipitation product for the U.S. GPM team.\n\nThe precipitation
estimates from the various precipitation-relevant satellite passive microwave (PMW)
sensors comprising the GPM constellation are computed using the 2021 version of
the Goddard Profiling Algorithm (GPROF2021), then gridded, intercalibrated to the
GPM Combined Ku Radar-Radiometer Algorithm (CORRA) product, and merged into half-hourly
0.1°x0.1° (roughly 10x10 km) fields. Note that CORRA is adjusted to the monthly
Global Precipitation Climatology Project (GPCP) Satellite-Gauge (SG) product over
high-latitude ocean to correct known biases.\n\nThe half-hourly intercalibrated
merged PMW estimates are then input to both a Morphing-Kalman Filter (KF) Lagrangian
time interpolation scheme based on work by the Climate Prediction Center (CPC) and
the Precipitation Estimation from Remotely Sensed Information using Artificial Neural
Networks (PERSIANN) Dynamic Infrared–Rain Rate (PDIR) re-calibration scheme. In
parallel, CPC assembles the zenith-angle-corrected, intercalibrated merged geo-IR
fields and forwards them to PPS for input to the PERSIANN-CCS algorithm (supported
by an asynchronous re-calibration cycle) which are then input to the KF morphing
(quasi-Lagrangian time interpolation) scheme.\n\nThe KF morphing (supported by an
asynchronous KF weights updating cycle) uses the PMW and IR estimates to create
half-hourly estimates. Motion vectors for the morphing are computed by maximizing
the pattern correlation of successive hours within each of the precipitation (PRECTOT),
total precipitable liquid water (TQL), and vertically integrated vapor (TQV) data
fields provided by the Modern-Era Retrospective Analysis for Research and Applications,
Version 2 (MERRA-2) and Goddard Earth Observing System model Version 5 (GEOS-5)
Forward Processing (FP) for the post-real-time (Final) Run and the near-real-time
(Early and Late) Runs, respectively. The vectors from PRECTOT are chosen if available,
else from TQL, if available, else from TQV. The KF uses the morphed data as the
“forecast” and the IR estimates as the “observations”, with weighting that depends
on the time interval(s) away from the microwave overpass time. The IR becomes important
after about ±90 minutes away from the overpass time. Variable averaging in the KF
is accounted for in a routine (Scheme for Histogram Adjustment with Ranked Precipitation
Estimates in the Neighborhood, or SHARPEN) that compares the local histogram of
KF morphed precipitation to the local histogram of forward- and backward-morphed
microwave data and the IR.\n\nThe IMERG system is run twice in near-real time:\n\n&amp;quot;Early&amp;quot;
multi-satellite product ~4 hr after observation time using only forward morphing
and\n&amp;quot;Late&amp;quot; multi-satellite product ~14 hr after observation time, using both
forward and backward morphing\nand once after the monthly gauge analysis is received:\n\n&amp;quot;Final&amp;quot;,
satellite-gauge product ~4 months after the observation month, using both forward
and backward morphing and including monthly gauge analyses.\n\nIn V07, the near-real-time
Early and Late half-hourly estimates have a monthly climatological concluding calibration
based on averaging the concluding calibrations computed in the Final, while in the
post-real-time Final Run the multi-satellite half-hourly estimates are adjusted
so that they sum to the Final Run monthly satellite-gauge combination. In all cases
the output contains multiple fields that provide information on the input data,
selected intermediate fields, and estimation quality. In general, the complete calibrated
precipitation, precipitation, is the data field of choice for most users.\n\nPrecipitation
phase is a diagnostic variable computed using analyses of surface temperature, humidity,
and pressure. \n\n\n\nRead our doc on how to get AWS Credentials to retrieve this
data: &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>Global 30m Height Above Nearest Drainage (HAND)</title>
      <link>https://registry.opendata.aws/glo-30-hand</link>
      <guid>https://registry.opendata.aws/glo-30-hand</guid>
      <description>Height Above Nearest Drainage (HAND) is a terrain model that normalizes topography to the relative heights along the drainage network and is used to describe the relative soil gravitational potentials or the local drainage potentials. Each pixel value represents the vertical distance to the nearest drainage. The HAND data provides near-worldwide land coverage at 30 meters and was produced from the 2021 release of the Copernicus GLO-30 Public DEM as distributed in the &lt;a href&#x3D;&quot;https://registry.opendata.aws/copernicus-dem/&quot;&gt;Registry of Open Data on AWS&lt;/a&gt;.</description>
    </item>
    <item>
      <title>Global Seasonal Sentinel-1 Interferometric Coherence and Backscatter Data Set</title>
      <link>https://registry.opendata.aws/ebd-sentinel-1-global-coherence-backscatter</link>
      <guid>https://registry.opendata.aws/ebd-sentinel-1-global-coherence-backscatter</guid>
      <description>This data set is the first-of-its-kind spatial representation of multi-seasonal, global SAR repeat-pass interferometric coherence and backscatter signatures. Global coverage comprises all land masses and ice sheets from 82 degrees northern to 79 degrees southern latitude. The data set is derived from high-resolution multi-temporal repeat-pass interferometric processing of about 205,000 Sentinel-1 Single-Look-Complex data acquired in Interferometric Wide-Swath mode (Sentinel-1 IW mode) from 1-Dec-2019 to 30-Nov-2020. The data set was developed by &lt;a href&#x3D;&quot;https://earthbigdata.com&quot;&gt;Earth Big Data LLC&lt;/a&gt; and &lt;a href&#x3D;&quot;https://www.gamma-rs.ch&quot;&gt;Gamma Remote Sensing AG&lt;/a&gt;, under contract for &lt;a href&#x3D;&quot;https://jpl.nasa.gov&quot;&gt;NASA&amp;#39;s Jet Propulsion Laboratory&lt;/a&gt;. The data set covers four sets of seasonal (DJF/MAM/JJA/SON) metrics: 1) Median 6-, 12-, 18-, 24-, 36-, and 48-day repeat coherence estimates for C-band VV and HH polarized data, 2) Mean backscatter (gamma naught) for VV, VH, HH, and HV polarizations, 3) Seasonal coherence decay model parameters rho, tau, and rmse, 4) Local incidence and layover/shadow regions for all relative orbits (175 orbits). Note that in the data set filenames the seasons were referred to as northern hemisphere winter (DJF), spring (MAM), summer (JJA), and fall (SON). The data set is available in two main components: 1) 1x1 degree tiles. Each tile contains GeoTiffs at 3 arcsec pixel spacing of all metrics available in the tile. (s3://sentinel-1-global-coherence-earthbigdata/data/tiles/), 2) Global mosaicked tiles as cloud optimized GeoTIFFs (COG) at 0.01 degree pixel spacing (s3://sentinel-1-global-coherence-earthbigdata/data/mosaics/) for each of the computed metrics.</description>
    </item>
    <item>
      <title>High resolution, annual cropland and landcover maps for selected African countries</title>
      <link>https://registry.opendata.aws/mapping-africa</link>
      <guid>https://registry.opendata.aws/mapping-africa</guid>
      <description>High resolution, annual cropland and landcover maps for selected African countries developed by &lt;a href&#x3D;&quot;https://clarku.edu&quot;&gt;Clark University&lt;/a&gt;&amp;#39;s &lt;a href&#x3D;&quot;https://agroimpacts.info/&quot;&gt;Agricultural Impacts Research Group&lt;/a&gt; using various machine learning approaches applied to Planet imagery, including field boundary and cultivated frequency maps, as well as multi-class land cover.</description>
    </item>
    <item>
      <title>IBL Neuropixels Brainwide Map on AWS</title>
      <link>https://registry.opendata.aws/ibl-autism</link>
      <guid>https://registry.opendata.aws/ibl-autism</guid>
      <description>Electrophysiological recordings of mouse brain activity acquired during a decision making task in multiple autism mice models.</description>
    </item>
    <item>
      <title>JMA Himawari-8/9</title>
      <link>https://registry.opendata.aws/noaa-himawari</link>
      <guid>https://registry.opendata.aws/noaa-himawari</guid>
      <description>Himawari-9, stationed at 140.7E, owned and operated by the Japan Meteorological Agency (JMA), is a geostationary meteorological satellite, with Himawari-8 as on-orbit back-up, that provides constant and uniform coverage of east Asia, and the west and central Pacific regions from around 35,800 km above the equator with an orbit corresponding to the period of the earth’s rotation. This allows JMA weather offices to perform uninterrupted observation of environmental phenomena such as typhoons, volcanoes, and general weather systems. Archive data back to July 2015 is available for Full Disk (AHI-L1b-FLDK) products in the bucket. For questions regarding Himawari-9 imagery specifications, visit the JMA site at &lt;a href&#x3D;&quot;https://www.data.jma.go.jp/mscweb/en/himawari89/space_segment/spsg_ahi.html&quot;&gt;https://www.data.jma.go.jp/mscweb/en/himawari89/space_segment/spsg_ahi.html&lt;/a&gt;.  For examples of Full Disk Himawari-9 imagery coverage, visit the NOAA Himawari-9 data page at &lt;a href&#x3D;&quot;https://www.ospo.noaa.gov/Products/imagery/himawari.html&quot;&gt;https://www.ospo.noaa.gov/Products/imagery/himawari.html&lt;/a&gt;.</description>
    </item>
    <item>
      <title>MONKEY</title>
      <link>https://registry.opendata.aws/monkey</link>
      <guid>https://registry.opendata.aws/monkey</guid>
      <description>This dataset contains the training data for the &lt;a href&#x3D;&quot;https://monkey.grand-challenge.org/&quot;&gt;Machine learning for Optimal detection of iNflammatory cells in the KidnEY or MONKEY&lt;/a&gt; challenge. The MONKEY challenge focuses on the automated detection and classification of inflammatory cells, specifically monocytes and lymphocytes, in kidney transplant biopsies using Periodic acid-Schiff (PAS) stained whole-slide images (WSI). It contains 80 WSI, collected from 4 different pathology institutes, with annotated regions of interest. For each WSI up to 3 different PAS scans and one IHC slide scan are available. This dataset and challenge support the development of AI models that can aid in the diagnostic process, reduce pathologists’ workload, and improve patient outcomes in renal transplantation.</description>
    </item>
    <item>
      <title>Meta-Organized Stimuli And fMRI Imaging data for Computational modeling (MOSAIC)</title>
      <link>https://registry.opendata.aws/mosaic</link>
      <guid>https://registry.opendata.aws/mosaic</guid>
      <description>This extensible dataset, MOSAIC, aggregates individual functional magnetic resonance imaging (fMRI) datasets by leveraging a shared preprocessing pipeline and stimulus curation procedure. This dataset aggregation procedure achieves the scale necessary for neural network training and the diversity needed for generalizable results.</description>
    </item>
    <item>
      <title>NASA / USGS Lunar Orbiter Laser Altimeter Cloud Optimized Point Cloud</title>
      <link>https://registry.opendata.aws/nasa-usgs-lunar-orbiter-laser-altimeter</link>
      <guid>https://registry.opendata.aws/nasa-usgs-lunar-orbiter-laser-altimeter</guid>
      <description>The lunar orbiter laser altimeter (LOLA) has collected and released almost 7 billion individual laser altimeter returns from the lunar surface. This dataset includes individual altimetry returns scraped from the Planetary Data System (PDS) LOLA Reduced Data Record (RDR) Query Tool, V2.0. Data are organized in 15˚ x 15˚ (longitude/latitude) sections, compressed and encoded into the Cloud Optimized Point Cloud (COPC) file format, and collected into a Spatio-Temporal Asset Catalog (STAC) collection for query and analysis. The data are in latitude, longitude, and radius (X, Y, Z) format with the proper IAU 2015 30100 well-known text projection string. These data are in the -180 to 180, center longitude 0 domain. Users of this data set are encouraged to use the Point Data Abstract Library (PDAL) STAC driver to query at the collection level or the COPC driver to query individual COPC tiles within the dataset. Queries of these data using bounding boxes, buffered points, or other geometries should use the -180 to 180 longitude domain (converting from 0-360, clone 180 as needed).</description>
    </item>
    <item>
      <title>NASA Earth Exchange (NEX) Data Collection</title>
      <link>https://registry.opendata.aws/nasanex</link>
      <guid>https://registry.opendata.aws/nasanex</guid>
      <description>A collection of downscaled climate change projections, derived from the
General Circulation Model (GCM) runs conducted under the Coupled Model
Intercomparison Project Phase 5 (CMIP5) [Taylor et al. 2012] and across
the four greenhouse gas emissions scenarios known as Representative
Concentration Pathways (RCPs) [Meinshausen et al. 2011]. The NASA Earth
Exchange group maintains the NEX-DCP30 (CMIP5), NEX-GDDP (CMIP5), and
LOCA (CMIP5).NOTE: The S3 Bucket location for this dataset changed on 5/6/2026</description>
    </item>
    <item>
      <title>NIH NCBI Sequence Read Archive (SRA) on AWS</title>
      <link>https://registry.opendata.aws/ncbi-sra</link>
      <guid>https://registry.opendata.aws/ncbi-sra</guid>
      <description>The Sequence Read Archive (SRA), produced by the &lt;a href&#x3D;&quot;https://www.ncbi.nlm.nih.gov/&quot;&gt;National Center for Biotechnology Information (NCBI)&lt;/a&gt; at the &lt;a href&#x3D;&quot;http://nlm.nih.gov/&quot;&gt;National Library of Medicine (NLM)&lt;/a&gt; at the &lt;a href&#x3D;&quot;http://www.nih.gov/&quot;&gt;National Institutes of Health (NIH)&lt;/a&gt;, stores raw DNA sequencing data and alignment information from high-throughput sequencing platforms. The SRA provides open access to these biological sequence data to support the research community&amp;#39;s efforts to enhance reproducibility and make new discoveries by comparing data sets. Buckets in this registry contain public SRA data in the original (user submitted) format from select high value and newly-released studies as well as all public-access SRA formatted ETL+BQS data. Also included is all SRA metadata that can be leveraged for attribute-based data discovery.</description>
    </item>
    <item>
      <title>NOAA National Air Quality Forecast Capability (NAQFC) Regional Model Guidance</title>
      <link>https://registry.opendata.aws/noaa-nws-naqfc-pds</link>
      <guid>https://registry.opendata.aws/noaa-nws-naqfc-pds</guid>
      <description>The National Air Quality Forecasting Capability (NAQFC) dataset contains model-generated air quality (AQ) forecast guidance from three different prediction systems. The first system is a coupled weather and atmospheric chemistry numerical forecast model, known as the Air Quality Model (AQM). It is used to produce forecast guidance for ozone (O3) and particulate matter that is less than or equal to 2.5 micrometers in diameter (PM2.5). Prior to May 14, 2024, AQM predictions were derived using the EPA’s Community Multiscale Air Quality (CMAQ) model, driven by meteorological fields from NCEP’s operational weather forecast models, specifically the North American Mesoscale Model (NAM; prior to 20 July 2021) and the Global Forecast System (GFS; beginning 20 July 2021). Since May 14, 2024, AQM guidance has been produced by a unique application within the community-based Unified Forecast System (UFS). The core model components in this application are derived directly from the fully online-coupled UFS-based weather and CMAQ-based chemistry models. In addition, it incorporates information related to chemical and particle source emissions as it integrates forward in time, including anthropogenic chemical emissions provided by the EPA, fire emissions from NOAA/NESDIS, and airborne particles generated by human activities and those predicted to be generated by wind-driven erosion and biosphere at ground level. The NCEP NAQFC AQM output fields in this archive include model raw and bias-corrected predictions dating back to 1 January 2020, all generated by the contemporaneous operational AQM, beginning with AQMv5 in 2020, transitioning to AQMv6 on 20 July 2021, and to AQMv7 on 14 May 2024. The length of each forecast was 48 hours prior to the implementation of AQMv6, and has been 72 hours ever since. The history of AQM upgrades is documented &lt;a href&#x3D;&quot;https://www.emc.ncep.noaa.gov/mmb/aq/AQChangelog.html&quot;&gt;here&lt;/a&gt;
&lt;br/&gt;
&lt;br/&gt;
The second prediction is known as the Hybrid Single-Particle Lagrangian Integrated Trajectory model (HYSPLIT). It is a widely used atmospheric transport and dispersion model containing an internal dust-generation module. It provides forecast guidance for atmospheric dust concentration and, prior to 28 June 2022, it also provided the NAQFC forecast guidance for smoke. Starting on that date, the third prediction system, a regional numerical weather prediction (NWP) model known as the Rapid Refresh (RAP) model, subsumed HYSPLIT for operational smoke guidance, simulating the emission, transport, and deposition of smoke particles that originate from biomass burning (fires) and anthropogenic sources.
&lt;br/&gt;
&lt;br/&gt;
The output from each of these modeling systems is generated over three separate domains, one covering CONUS, another over Alaska, and the other over Hawaii. Currently, for this archive, the O3, PM2.5, and smoke output is available over all three domains, while dust products are available only over the CONUS domain. The predicted concentrations of all species in the lowest model layer (i.e., the layer in contact with the surface) are available, as are vertically integrated values of smoke and dust. The data is gridded horizontally within each domain, with a grid spacing of approximately 5 km over CONUS, 6 km over Alaska, and 2.5 km over Hawaii. O3 concentrations are provided in parts per billion (PPB), while the concentrations of all other species are quantified in units of micrograms per cubic meter (ug/m3), except for the column-integrated smoke values which are expressed in units of milligrams per square meter (mg/m2).
&lt;br/&gt;
&lt;br/&gt;
Temporally, O3 and PM2.5 are available as maximum and/or averaged values over various time periods, selected in part for consistency with the EPA’s National Ambient Air Quality Standards. Specifically, O3 is available in both 1-hour and 8-hour (backward calculated) averages, as well as preceding 1-hour and 8-hour maximum values. Similarly, PM2.5 is available in 1-hour and 24-hour average values and 24-hour maximum values. In addition, all O3 and PM2.5 fields are available with bias-corrected magnitudes, based on derived historical model biases relative to observations.
&lt;br/&gt;
&lt;br/&gt;
The AQM produces hourly forecast guidance for O3 and PM2.5 up to 72 hours twice per day. Smoke guidance is available up to 51 hours from once-per-day RAP forecasts, while dust guidance from HYSPLIT is available up to 48 hours.</description>
    </item>
    <item>
      <title>New Zealand Coastal Elevation</title>
      <link>https://registry.opendata.aws/nz-coastal</link>
      <guid>https://registry.opendata.aws/nz-coastal</guid>
      <description>The New Zealand Coastal Elevation dataset consists of New Zealand&amp;#39;s publicly owned coastal digital elevation models, which are freely available to use under an open licence. The data consists of bare earth (DEM) data that traverses the coastal zone, including the seabed down to approximately 25m in depth. Data is provided as nationally consistent 1m resolution tiles derived from LiDAR surveys.All of the coastal elevation files are &lt;a href&#x3D;&quot;https://www.cogeo.org/&quot;&gt;Cloud Optimised GeoTIFFs&lt;/a&gt; using LERC compression for the main grid and LERC compression with lower max_z_error for the overviews. These elevation files are accompanied by &lt;a href&#x3D;&quot;https://stacspec.org/&quot;&gt;STAC metadata&lt;/a&gt;. The coastal elevation data is organised by region and survey.</description>
    </item>
    <item>
      <title>Normalized Difference Urban Index (NDUI)</title>
      <link>https://registry.opendata.aws/ndui</link>
      <guid>https://registry.opendata.aws/ndui</guid>
      <description>NDUI is combined with cloud shadow-free Landsat Normalized Difference Vegetation Index (NDVI) composite and DMSP/OLS Night Time Light (NTL) to characterize global urban areas at a 30 m resolution,and it can greatly enhance urban areas, which can then be easily distinguished from bare lands including fallows and deserts. With the capability to delineate urban boundaries and, at the same time, to present sufficient spatial details within urban areas, the  NDUI has the potential for urbanization studies at regional and global scales.</description>
    </item>
    <item>
      <title>OPERA Dynamic Surface Water Extent from Harmonized Landsat Sentinel-2 product (Version 1)</title>
      <link>https://registry.opendata.aws/nasa-operal3dswx-hlsv1</link>
      <guid>https://registry.opendata.aws/nasa-operal3dswx-hlsv1</guid>
      <description>This dataset contains Level-3 Dynamic OPERA surface water extent product version 1.  The data are validated surface water extent observations beginning April 2023. Known issues and caveats on usage are described under Documentation. The input dataset for generating each product is the Harmonized Landsat-8 and Sentinel-2A/B/C (HLS) product version 2.0. HLS products provide surface reflectance (SR) data from the Operational Land Imager (OLI) aboard the Landsat 8 satellite and the MultiSpectral Instrument (MSI) aboard the Sentinel-2A/B/C satellite. The surface water extent products are distributed over projected map coordinates using the Universal Transverse Mercator (UTM) projection. Each UTM tile covers an area of 109.8 km × 109.8 km. This area is divided into 3,660 rows and 3,660 columns at 30-m pixel spacing. Each product is distributed as a set of 10 GeoTIFF (Geographic Tagged Image File Format) files including water classification, associated confidence, land cover classification, terrain shadow layer, cloud/cloud-shadow classification, Digital elevation model (DEM), and Diagnostic layer.
&lt;br&gt;&lt;br&gt;
The digital elevation model (DEM) provided as a layer of the DSWx-HLS product (band 10) was generated using the Copernicus DEM 30-m and Copernicus DEM 90-m models provided by the European Space Agency. The Copernicus DEM 30-m and Copernicus DEM 90-m were produced using Copernicus WorldDEM-30 © DLR e.V. 2010-2014 and © Airbus Defence and Space GmbH 2014-2018 provided under COPERNICUS by the European Union and ESA; all rights reserved. The organizations in charge of the OPERA project, the Copernicus programme, and Airbus Defence and Space GmbH by law or by delegation do not assume any legal responsibility or liability, whether express or implied, arising from the use of this DEM.
&lt;br&gt;&lt;br&gt;
The OPERA DSWx-HLS product contains modified Copernicus Sentinel data (2023-2025).
&lt;br&gt;&lt;br&gt;
To access the calibration/validation database for OPERA Dynamic Surface Water Extent Products, please contact &lt;a href&#x3D;&quot;mailto:&amp;#112;&amp;#111;&amp;#100;&amp;#x61;&amp;#97;&amp;#x63;&amp;#64;&amp;#x70;&amp;#111;&amp;#100;&amp;#97;&amp;#x61;&amp;#x63;&amp;#46;&amp;#106;&amp;#112;&amp;#108;&amp;#46;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#112;&amp;#111;&amp;#100;&amp;#x61;&amp;#97;&amp;#x63;&amp;#64;&amp;#x70;&amp;#111;&amp;#100;&amp;#97;&amp;#x61;&amp;#x63;&amp;#46;&amp;#106;&amp;#112;&amp;#108;&amp;#46;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#x76;&lt;/a&gt; 
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://archive.podaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;https://archive.podaac.earthdata.nasa.gov/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>Open-Meteo Weather API Database</title>
      <link>https://registry.opendata.aws/open-meteo</link>
      <guid>https://registry.opendata.aws/open-meteo</guid>
      <description>Open-Meteo integrates weather models from reputable national weather services, offering a swift and efficient weather API. Real-time weather forecasts are unified into a time-series database that provides historical and future weather data for any location worldwide.Through Open-Meteo on AWS Open Data, you can download the Open-Meteo weather database and analysis weather data locally. Docker images are provided to download data and to expose an HTTP API endpoint. Using Open-Meteo SDKs, you can seamlessly integrate weather data into your Python, Typescript, Swift, Kotlin, or Java applications.The entire source code is open-source, and contributions are welcome!To get started, familiarize yourself with the &lt;a href&#x3D;&quot;https://github.com/open-meteo/open-data&quot;&gt;available weather models&lt;/a&gt; and explore tutorials on downloading 80 years of &lt;a href&#x3D;&quot;https://github.com/open-meteo/open-data/tree/main/tutorial_download_era5&quot;&gt;historical weather data from ERA5&lt;/a&gt; or set up your own &lt;a href&#x3D;&quot;https://github.com/open-meteo/open-data/tree/main/tutorial_weather_api&quot;&gt;real-time weather API&lt;/a&gt; with high-resolution models.If you have any questions, feel free to reach out on &lt;a href&#x3D;&quot;https://github.com/open-meteo/open-meteo/discussions&quot;&gt;GitHub discussions&lt;/a&gt;.</description>
    </item>
    <item>
      <title>OpenStreetMap on AWS</title>
      <link>https://registry.opendata.aws/osm</link>
      <guid>https://registry.opendata.aws/osm</guid>
      <description>OSM is a free, editable map of the world, created and maintained by volunteers. Regular OSM data archives are made available in Amazon S3 in both standard formats (OSM PBF, XML) and cloud-native formats optimized for analytics workloads.</description>
    </item>
    <item>
      <title>Overture Maps Foundation Open Map Data</title>
      <link>https://registry.opendata.aws/overture</link>
      <guid>https://registry.opendata.aws/overture</guid>
      <description>Overture is a collaboratively built, global, open map data project for developers who build map services or use geospatial data. Overture Open Map Data contains data that are standardized under the themes of Admins, Base, Buildings, Places, and Transportation. Overture also includes a Global Entity Reference System (GERS) which encodes map data to a shared universal reference. Beginning with the Overture 2023-11-14-alpha.0 release, the data is available as cloud-native GeoParquet files. </description>
    </item>
    <item>
      <title>Ozone Monitoring Instrument (OMI) / Aura NO2 Tropospheric Column Density</title>
      <link>https://registry.opendata.aws/omi-no2-nasa</link>
      <guid>https://registry.opendata.aws/omi-no2-nasa</guid>
      <description>NO2 tropospheric column density, screened for CloudFraction &amp;lt; 30% global daily
 composite at 0.25 degree resolution for the temporal range of 2004 to May
2020. Original archive data in HDF5 has been processed into a &lt;a href&#x3D;&quot;https://www.cogeo.org/&quot;&gt;Cloud-Optimized
GeoTiff (COG)&lt;/a&gt; format. Quality Assurance - This data
has been validated by the NASA Science Team at Goddard Space Flight Center.Cautionary Note: &lt;a href&#x3D;&quot;https://airquality.gsfc.nasa.gov/caution-interpretation&quot;&gt;https://airquality.gsfc.nasa.gov/caution-interpretation&lt;/a&gt;.</description>
    </item>
    <item>
      <title>Prefeitura Municipal de São Paulo (PMSP) LiDAR Point Cloud</title>
      <link>https://registry.opendata.aws/pmsp-lidar</link>
      <guid>https://registry.opendata.aws/pmsp-lidar</guid>
      <description>The objective of the Mapa 3D Digital da Cidade (M3DC) of the São Paulo City Hall is to publish LiDAR point cloud data. The initial data was acquired in 2017 by aerial surveying and future data will be added. This publicly accessible dataset is provided in the &lt;a href&#x3D;&quot;https://entwine.io/entwine-point-tile.html&quot;&gt;Entwine Point Tiles&lt;/a&gt; format as a lossless octree, full density, based on &lt;a href&#x3D;&quot;https://laszip.org&quot;&gt;LASzip&lt;/a&gt; (LAZ) encoding.</description>
    </item>
    <item>
      <title>Protein Data Bank 3D Structural Biology Data</title>
      <link>https://registry.opendata.aws/pdb-3d-structural-biology-data</link>
      <guid>https://registry.opendata.aws/pdb-3d-structural-biology-data</guid>
      <description>The &amp;quot;Protein Data Bank (PDB) archive&amp;quot; was established in 1971 as the first open-access digital data archive in biology. It is a collection of three-dimensional (3D) atomic-level structures of biological macromolecules (i.e., proteins, DNA, and RNA) and their complexes with one another and various small-molecule ligands (e.g., US FDA approved drugs, enzyme co-factors). For each PDB entry (unique identifier: 1abc or PDB_0000001abc) multiple data files contain information about the 3D atomic coordinates, sequences of biological macromolecules, information about any small molecules/ligands present in the entry, details about the structure-determination experiment, authors and publication information, experimental data, and the wwPDB validation report. Additional content stored in the archive includes documentation, summary reports, and software (among others).
The PDB is a jointly-managed core archive of the Worldwide Protein Data Bank partnership [RCSB Protein Data Bank (RCSB PDB, rcsb.org); Protein Data Bank in Europe (PDBe, pdbe.org); Protein Data Bank Japan (PDBj, pdbj.org); Electron Microscopy Data Bank (EMDB, emdb-empiar.org); and Biological Magnetic Resonance Bank (BMRB, bmrb.io)].
RCSB PDB serves as the wwPDB-designated Archive Keeper for the Protein Data Bank.
Additional wwPDB Core Archives are as follows:
Electron Microscopy Data Bank (wwPDB-designated Archive Keeper: EMDB)
Biological Magnetic Resonance Bank (wwPDB-designated Archive Keeper: BMRB)</description>
    </item>
    <item>
      <title>RACECAR Dataset</title>
      <link>https://registry.opendata.aws/racecar-dataset</link>
      <guid>https://registry.opendata.aws/racecar-dataset</guid>
      <description>The RACECAR dataset is the first open dataset for full-scale and high-speed autonomous racing. Multi-modal sensor data has been collected from fully autonomous Indy race cars operating at speeds of up to 170 mph (273 kph). Six teams who raced in the Indy Autonomous Challenge during 2021-22 have contributed to this dataset. The dataset spans 11 interesting racing scenarios across two race tracks which include solo laps, multi-agent laps, overtaking situations, high-accelerations, banked tracks, obstacle avoidance, pit entry and exit at different speeds. The data is organized and released in both ROS2 and nuScenes format. We have also developed the ROS2-to-nuScenes conversion library to achieve this. The RACECAR data is unique because of the high-speed environment of autonomous racing and is suitable to explore issues regarding localization, object detection and tracking (LiDAR, Radar, and Camera), and mapping that arise at the limits of operation of the autonomous vehicle.</description>
    </item>
    <item>
      <title>SPARC: Datasets bridging the body and the brain</title>
      <link>https://registry.opendata.aws/sparc</link>
      <guid>https://registry.opendata.aws/sparc</guid>
      <description>The SPARC Datasets comprise a collection of scientific data that is focused
on bridging the body and the brain. The datasets focus on neural connectivity,
organ innervation and detailed anatomical mapping of the peripheral nervous system.
SPARC datasets distinguish themselves from other data resources through its multi-modal
approach to scientific data and integrates molecular, imaging, timeseries and other
datatypes associated with the interaction between the peripheral nervous system and 
organs. SPARC data provides a unique integrated effort to develop next generation mapping
of anatomical and functional connectivity of the nervous system.</description>
    </item>
    <item>
      <title>SPARTAN Data</title>
      <link>https://registry.opendata.aws/spartan-cloud</link>
      <guid>https://registry.opendata.aws/spartan-cloud</guid>
      <description>SPARTAN (Surface PARTiculate mAtter Network) measures and provides surface ambient particulate matter (PM2.5 and PM10) concentration and the chemical composition around the world, with the purpose of connecting ground-based PM2.5 and satellite remote sensing.</description>
    </item>
    <item>
      <title>Sanborn Maps Data Package</title>
      <link>https://registry.opendata.aws/loc-sanborn-maps</link>
      <guid>https://registry.opendata.aws/loc-sanborn-maps</guid>
      <description>The dataset contains metadata records for 50,600 maps from the &lt;a href&#x3D;&quot;https://www.loc.gov/collections/sanborn-maps/&quot;&gt;Sanborn Fire Insurance Maps collection&lt;/a&gt; and their corresponding 440,048 JPEG images. The Sanborn collection at Library of Congress includes over fifty thousand editions of fire insurance maps comprising almost seven hundred thousand individual sheets. The Library of Congress holdings represent the largest extant collection of maps produced by the Sanborn Map Company.</description>
    </item>
    <item>
      <title>Sea Around Us Global Fisheries Catch Data</title>
      <link>https://registry.opendata.aws/sau-global-fisheries-catch-data</link>
      <guid>https://registry.opendata.aws/sau-global-fisheries-catch-data</guid>
      <description>The project presents Sea Around Us Global Fisheries Catch Data aggregated at EEZ level. The data are computed from reconstructed catches from various official fisheries statistics, scientific, technical and policy reports about the fisheries, and includes estimation of discards, unreported and illegal catch data from all maritime countries and major territories of the world.This project was the result of a work between Sea Around Us and the CIC programme, a collaborative programme between the University of British Columbia (UBC) and AWS.</description>
    </item>
    <item>
      <title>Sofar Spotter Archive</title>
      <link>https://registry.opendata.aws/sofar-spotter-archive</link>
      <guid>https://registry.opendata.aws/sofar-spotter-archive</guid>
      <description>This dataset includes archival hourly data from the [Sofar Spotter buoy global network] (&lt;a href&#x3D;&quot;https://weather.sofarocean.com/&quot;&gt;https://weather.sofarocean.com/&lt;/a&gt;) from 2019 to March 2022. &lt;br /&gt;</description>
    </item>
    <item>
      <title>SondeHub Radiosonde Telemetry</title>
      <link>https://registry.opendata.aws/sondehub-telemetry</link>
      <guid>https://registry.opendata.aws/sondehub-telemetry</guid>
      <description>SondeHub Radiosonde telemetry contains global radiosonde (weather balloon) data captured by SondeHub from our participating radiosonde_auto_rx receiving stations. radiosonde_auto_rx is a open source project aimed at receiving and decoding telemetry from airborne radiosondes using software-defined-radio techniques, enabling study of the telemetry and sometimes recovery of the radiosonde itself.
Currently 313 receiver stations are providing data for an average of 384 radiosondes a day.  The data within this repository contains received telemetry frames, including radiosonde type, gps position, and for some radiosondes atmospheric sensor data (temperature, humidity, pressure). As the downlinked telemetry does not always contain calibration information, any atmospheric sensor data should be considered to be uncalibrated. Note that radiosonde_auto_rx does not have sensor data support for all radiosonde types.</description>
    </item>
    <item>
      <title>The Human Connectome Project</title>
      <link>https://registry.opendata.aws/hcp-openaccess</link>
      <guid>https://registry.opendata.aws/hcp-openaccess</guid>
      <description>The Human Connectome Project (HCP Young Adult, HCP-YA) is mapping the healthy human connectome by collecting and freely distributing neuroimaging and behavioral data on 1,200 normal young adults, aged 22-35.</description>
    </item>
    <item>
      <title>Vermont Open Geospatial on AWS</title>
      <link>https://registry.opendata.aws/vt-opendata</link>
      <guid>https://registry.opendata.aws/vt-opendata</guid>
      <description>The State of Vermont has partnered with Amazon&amp;#39;s Open Data Initative to make a wide range of geospatial data available in the public domain. Vermont acquires aerial imagery and LiDAR during leaf-off conditions. The imagery typically ranges from 30-centimeter to 15-centimeter in resolution and is available from Vermont&amp;#39;s Amazon S3 bucket in a Cloud Optimized GeoTiff (COG) format. LiDAR data has been acquired and is available as USGS Quality Level-1 (QL1) and Level-2 (QL2) compliant datasets in COG format. Geospatial datasets derived from imagery and/or lidar are also available as COGs, including high resolution landcover.</description>
    </item>
    <item>
      <title>A region-wide, multi-year set of crop field boundary labels for Africa</title>
      <link>https://registry.opendata.aws/africa-field-boundary-labels</link>
      <guid>https://registry.opendata.aws/africa-field-boundary-labels</guid>
      <description>Crop field boundaries digitized in Planet imagery collected across Africa between 2017 and 2023, developed by &lt;a href&#x3D;&quot;https://farmerline.co/&quot;&gt;Farmerline&lt;/a&gt;, &lt;a href&#x3D;&quot;https://spatialcollective.com/&quot;&gt;Spatial Collective&lt;/a&gt;,  and the &lt;a href&#x3D;&quot;https://agroimpacts.info/&quot;&gt;Agricultural Impacts Research Group&lt;/a&gt; at &lt;a href&#x3D;&quot;https://www.clarku.edu/&quot;&gt;Clark University&lt;/a&gt;, with support from the &lt;a href&#x3D;&quot;https://lacunafund.org/&quot;&gt;Lacuna Fund&lt;/a&gt; (&lt;a href&#x3D;&quot;https://arxiv.org/abs/2412.18483&quot;&gt;Estes et al, 2024&lt;/a&gt;; &lt;a href&#x3D;&quot;https://zenodo.org/records/11060871&quot;&gt;Wussah et al. (2023)&lt;/a&gt;). This dataset has been  further supplemented by additional labels collected primarily for  for 2018 over a subset of countries, which provide an example of their application in training and validating a CNN-based cropland mapping model  &lt;a href&#x3D;&quot;https://www.mdpi.com/2072-4292/17/3/474&quot;&gt;(Khallaghi et al. 2025)&lt;/a&gt;.</description>
    </item>
    <item>
      <title>APEX-CONNECTS</title>
      <link>https://registry.opendata.aws/apex</link>
      <guid>https://registry.opendata.aws/apex</guid>
      <description>The BRAIN Initiative Connectivity Across Scales (CONNECTS) program is working to create detailed maps of brain  wiring across different species and scales, using advanced imaging technologies.  APEX supports this effort by serving as a central hub that brings together and coordinates data and tools  from research focused on brain connectivity in humans and animals. Together, these efforts aim to improve our  understanding of how the brain is structured and functions.</description>
    </item>
    <item>
      <title>ASKAP Radio Telescope</title>
      <link>https://registry.opendata.aws/askap</link>
      <guid>https://registry.opendata.aws/askap</guid>
      <description>ASKAP is the CSIRO’s newest radio telescope. It is situated at the Inyarrimanha Ilgari Bundara, the CSIRO Murchison Radio-astronomy Observatory on Wajarri Yamaji Country in the Murchison region of Western Australia, about 800 km north of Perth. ASKAP consists of 36 12m dishes, spread-out as far as 6km apart. It uses a new technology called Phased Array Feeds (PAFs), which allows it to see more of the sky at once. This novel technology allows ASKAP to achieve extremely high survey speed, making it one of the best instruments in the world for mapping the sky at radio wavelengths. Initial dataset available - The Rapid ASKAP Continuum Survey (RACS)RACS is the first large-area survey completed with ASKAP. This survey is revolutionary as the entire sky was observed in a matter of weeks, doing what previously took telescopes years to do. RACS initially covered the whole sky at 890 MHz (RACS-Low), and has since expanded to ASKAP’s other bands (1.4 and 1.7 GHz). RACS also covers the sky in multiple epochs, with a second epoch of RACS-Low and RACS-Mid obtained and processed.  RACS provides astronomers with a unique opportunity to study the radio sky and radio populations, in particular supermassive blackholes (active galactic nuclei) and their role in galaxy evolution. The multi-epoch approach also allows a study of the transient sky and testing and verification of calibration methods. The large area allows for cosmological studies, such as a search for anisotropy in the galaxy population, or cosmic dipole. </description>
    </item>
    <item>
      <title>BUSCO Datasets</title>
      <link>https://registry.opendata.aws/busco-data</link>
      <guid>https://registry.opendata.aws/busco-data</guid>
      <description>Lineage datasets for use with BUSCO software package. Each dataset contains HMM profiles for clade specific, universal, single-copy marker genes. Datasets are available across archaea, bacteria, eukaryota and virus domains. The repository also includes necessary data files for phylogenetic placement of an input assembly.</description>
    </item>
    <item>
      <title>Basic Local Alignment Sequences Tool (BLAST) Databases</title>
      <link>https://registry.opendata.aws/ncbi-blast-databases</link>
      <guid>https://registry.opendata.aws/ncbi-blast-databases</guid>
      <description>A centralized repository of pre-formatted BLAST databases created by the National Center for Biotechnology Information (NCBI).</description>
    </item>
    <item>
      <title>Chalmers Cloud Ice Climatology</title>
      <link>https://registry.opendata.aws/ccic</link>
      <guid>https://registry.opendata.aws/ccic</guid>
      <description>The Chalmers Cloud Ice Climatology (CCIC) is a novel, deep-learning-based climate record of ice-particle concentrations in the atmosphere. CCIC results are available at high spatial and temporal resolution (0.07° / 3 h from 1983, 0.036° / 30 min from 2000) and thus ideally suited for evaluating high-resolution weather and climate models or studying individual weather systems.</description>
    </item>
    <item>
      <title>Community Earth System Model v2 Large Ensemble (CESM2 LENS)</title>
      <link>https://registry.opendata.aws/ncar-cesm2-lens</link>
      <guid>https://registry.opendata.aws/ncar-cesm2-lens</guid>
      <description>The US National Center for Atmospheric Research partnered with the IBS Center for Climate Physics in South Korea to generate the CESM2 Large Ensemble which consists of 100 ensemble members at 1 degree spatial resolution covering the period 1850-2100 under CMIP6 historical and SSP370 future radiative forcing scenarios. Data sets from this ensemble were made downloadable via the Climate Data Gateway on June 14th, 2021.
NCAR has copied a subset (currently ~500 TB) of CESM2 LENS data to Amazon S3 as part of the AWS Public Datasets Program. To optimize for large-scale analytics we have represented the data as ~275 Zarr stores format accessible through the Python Xarray library. Each Zarr store contains a single physical variable for a given model run type and temporal frequency (monthly, daily).</description>
    </item>
    <item>
      <title>Community coral reef image classification training data</title>
      <link>https://registry.opendata.aws/coralreef-image-classification-training</link>
      <guid>https://registry.opendata.aws/coralreef-image-classification-training</guid>
      <description>Community-sourced repository of coral reef image classification training data, including continually updated confirmed annotations from &lt;a href&#x3D;&quot;https://datamermaid.org/&quot;&gt;MERMAID&lt;/a&gt;</description>
    </item>
    <item>
      <title>Data to Science Catalog</title>
      <link>https://registry.opendata.aws/data-to-science</link>
      <guid>https://registry.opendata.aws/data-to-science</guid>
      <description>A user-generated geospatial data collection maintained by the Data to Science  platform. Contributions vary by project, but typically include cloud-optimized  datasets such as Cloud-Optimized GeoTIFFs (COGs) and Cloud-Optimized Point  Clouds (COPCs), designed for efficient streaming, visualization, and analysis  in modern geospatial applications.</description>
    </item>
    <item>
      <title>Demand-Side Grid (dsgrid) Toolkit</title>
      <link>https://registry.opendata.aws/nrel-pds-dsgrid</link>
      <guid>https://registry.opendata.aws/nrel-pds-dsgrid</guid>
      <description>Projects that use the dsgrid toolkit assemble bottom-up descriptions of electricity 
demand and related data that are highly resolved geographically, temporally, and sectorally. 
Typically modelers describe multiple scenarios of future energy use at hourly resolution, 
suitable for inclusion in long-term power system planning models, i.e., capacity expansion and 
production cost models. </description>
    </item>
    <item>
      <title>ECMWF real-time forecasts</title>
      <link>https://registry.opendata.aws/ecmwf-forecasts</link>
      <guid>https://registry.opendata.aws/ecmwf-forecasts</guid>
      <description>These products are a subset of the ECMWF real-time forecast data and are made available to the public free of charge. They are based on the medium-range (high-resolution and ensembles) forecast models.
Note: The ECMWF Open Data Portal provides a rolling archive (most recent forecast runs), while the AWS replica bucket is updated as new data are published and may retain older data conventions/versions over time.</description>
    </item>
    <item>
      <title>Earth Radio Occultation</title>
      <link>https://registry.opendata.aws/gnss-ro-opendata</link>
      <guid>https://registry.opendata.aws/gnss-ro-opendata</guid>
      <description>This is an updating archive of radio occultation (RO) data using the transmitters of the Global Navigation Satellite Systems (GNSS) as generated and processed by the COSMIC DAAC (ucar), the Jet Propulsion Laboratory (jpl) of the California Institute of Technology, and the Radio Occultation Meteorology Satellite Application Facility (romsaf). The contributions for ucar and romsaf are currently active. &lt;p&gt; This dataset is funded by the NASA Earth Science Data Systems and the Advancing Collaborative Connections for Earth System Science (ACCESS) 2019 program.</description>
    </item>
    <item>
      <title>Encyclopedia of DNA Elements (ENCODE)</title>
      <link>https://registry.opendata.aws/encode-project</link>
      <guid>https://registry.opendata.aws/encode-project</guid>
      <description>The Encyclopedia of DNA Elements (ENCODE) Consortium is an international collaboration of
research groups funded by the National Human Genome Research Institute (NHGRI). The goal
of ENCODE is to build a comprehensive parts list of functional elements in the human genome,
including elements that act at the protein and RNA levels, and regulatory elements that
control cells and circumstances in which a gene is active. ENCODE investigators employ a
variety of assays and methods to identify functional elements. The discovery and annotation
of gene elements is accomplished primarily by sequencing a diverse range of RNA sources,
comparative genomics, integrative bioinformatic methods, and human curation. Regulatory
elements are typically investigated through DNA hypersensitivity assays, assays of
DNA methylation, and immunoprecipitation (IP) of proteins that interact with DNA and RNA,
i.e., modified histones, transcription factors, chromatin regulators, and
RNA-binding proteins, followed by sequencing.</description>
    </item>
    <item>
      <title>Epigenomes of the Human Pangenome Reference Consortium (HPRC) Release 2</title>
      <link>https://registry.opendata.aws/hprc-epigenome</link>
      <guid>https://registry.opendata.aws/hprc-epigenome</guid>
      <description>The Human Pangenome Reference Consortium (HPRC) Release 2 represents a landmark achievement in genomics, providing high-quality phased genome assemblies from over 200 individuals with comprehensive functional genomics data. The HPRC Epigenome Browser provides researchers a way to explore all epigenomics data generated by release 2. The HPRC Epigenome Browser (HPRCEB) is a modern, interactive web portal that democratizes access to HPRC Release 2 epigenomics data through an intuitive interface supporting genome selection, data visualization, and bulk download capabilities. The portal integrates genome assemblies, DNA methylation profiles, gene expression data, and chromatin accessibility measurements across diverse populations, enabling researchers to efficiently identify and retrieve datasets matching their specific research needs.</description>
    </item>
    <item>
      <title>Epilepsy.Science</title>
      <link>https://registry.opendata.aws/epilepsy-science</link>
      <guid>https://registry.opendata.aws/epilepsy-science</guid>
      <description>Epilepsy.Science comprise a set of datasets focused on Epilepsy Research that
span both Clinical Data and Pre-clinical data. Datasets are contributed by the 
Epilepsy Research community and published using a standardized structure and 
metadata. Clinical datasets include de-identified subject information, EEG, and
clinical imaging.</description>
    </item>
    <item>
      <title>FoMo - A Multi-Season Dataset for Robot Navigation in Forêt Montmorency</title>
      <link>https://registry.opendata.aws/fomo-norlab</link>
      <guid>https://registry.opendata.aws/fomo-norlab</guid>
      <description>The FoMo dataset is a multi-season collection recorded in a boreal forest environment, featuring deep snow, off-road terrain, steep slopes, and highly variable weather. It provides synchronized multi-modal sensor data—including two lidars (RoboSense and Leishen), an FMCW radar (Navtech), stereo and monocular cameras, dual IMUs, wheel odometry, power data, calibration sequences, and precise ground-truth trajectories via GNSS-PPK fusion.
Designed to support research on robust robot autonomy under adverse conditions, FoMo includes repeated traversals of six trajectories of varying complexity for long-term SLAM and odometry evaluation, as well as rich metadata such as one-minute weather station measurements.
The dataset is intended to challenge state-of-the-art SLAM, localization, traversability analysis, and multi-season robotics research.</description>
    </item>
    <item>
      <title>GEOGLOWS Hydrological Model Version 2</title>
      <link>https://registry.opendata.aws/geoglows-v2</link>
      <guid>https://registry.opendata.aws/geoglows-v2</guid>
      <description>GEOGLOWS is the Group on Earth Observation&amp;#39;s Global Water Sustainability Program. It coordinates efforts from public 
and private entities to make application ready river data more accessible and sustainably available to underdeveloped 
regions. The GEOGLOWS Hydrological Model provides a retrospective and daily forecast of global river discharge at 7 
million river sub-basins. The stream network is a hydrologically conditioned subset of the TDX-Hydro streams and 
basins data produced by the United State&amp;#39;s National Geospatial Intelligence Agency. The daily forecast provides 3 
hourly average discharge in a 51 member ensemble and 15 day lead time derived from the ECMWF Integrated Forecast 
System (IFS). The retrospective simulation is derived from ERA5 climate reanalysis data and provides daily average 
streamflow beginning on 1 January 1940. New forecasts are uploaded daily and the retrospective simulation is updated 
weekly on Sundays to keep the lag time between 5 and 12 days.&lt;br&gt;&lt;br&gt;
The geoglows-v2 bucket contains: (1) model configuration files used to generate the simulations, (2) the GIS streams 
datasets used by the model, (3) the GIS streams datasets optimized for visualizations used by Esri&amp;#39;s Living Atlas 
layer, (4) several supporting table of metadata including country names, river names, hydrological properties used for
modeling.&lt;br&gt;&lt;br&gt;
The geoglows-v2-forecasts bucket contains: (1) daily 15 forecasts in zarr format optimized for time series queries of 
all ensemble members in the prediction, (2) CSV formatted summary files optimized for producing time series animated 
web maps for the entire global streams dataset.&lt;br&gt;&lt;br&gt;
The geoglows-v2-retrospective bucket contains: (1) the model retrospective outputs in (1a) zarr format optimized for 
time series queries of up to a few hundred rivers on demand as well as (1b) in netCDF format best for bulk downloading 
the dataset, (2) estimated return period flows for all 7 million million rivers (2a) in zarr format optimized for 
reading subsets of the dataset as well as (2b) in netCDF format best for bulk downloading. (3) The initialization files 
produced at the end of each incremental simulation useful for restarting the model from a specific date.</description>
    </item>
    <item>
      <title>GPM IMERG Early Precipitation L3 1 day 0.1 degree x 0.1 degree V07 (GPM_3IMERGDE) at GES DISC</title>
      <link>https://registry.opendata.aws/nasa-gpm3imergde</link>
      <guid>https://registry.opendata.aws/nasa-gpm3imergde</guid>
      <description>Version 07 is the current version of the data set. Older versions will no longer be available and have been superseded by Version 07.The Integrated Multi-satellitE Retrievals for GPM (IMERG) IMERG is a NASA product estimating global surface precipitation rates at a high resolution of 0.1° every half-hour beginning 2000.  It is part of the joint NASA-JAXA Global Precipitation Measurement (GPM) mission, using the GPM Core Observatory satellite as the standard to combine precipitation observations from an international constellation of satellites using advanced techniques.  IMERG can be used for global-scale applications as well as over regions with sparse or no reliable surface observations.  The fine spatial and temporal resolution of IMERG data allows them to be accumulated to the scale of the application for increased skill.  IMERG has three Runs with varying latencies in response to a range of application needs: rapid-response applications (Early Run, 4-h latency), same/next-day applications (Late Run, 14-h latency), and post-real-time research (Final Run, 3.5-month latency).  While IMERG strives for consistency and accuracy, satellite estimates of precipitation are expected to have lower skill over frozen surfaces, complex terrain, and coastal zones.  As well, the changing GPM satellite constellation over time may introduce artifacts that affect studies focusing on multi-year changes.This dataset is the GPM Level 3 IMERG  &lt;em&gt;Early&lt;/em&gt; Daily  10 x 10 km (GPM_3IMERGDE) derived from the half-hourly GPM_3IMERGHHE. The derived result represents an early (expedited) estimate of the daily mean precipitation rate in mm/day. The dataset is produced by first computing the mean precipitation rate in (mm/hour) in every grid cell, and then multiplying the result by 24.  This minimizes the possible dry bias in versions before &amp;quot;07&amp;quot;, in the simple daily totals  for cells where less than 48 half-hourly observations are valid for the day. The latter under-sampling is very rare in the combined microwave-infrared (and rain gauge in the final) dataset, variable &amp;quot;precipitation&amp;quot;,  and appears in higher latitudes. Thus, in most cases users of global &amp;quot;precipitation&amp;quot; data will not notice any difference. This correction, however, is noticeable in the high-quality microwave retrieval, variable &amp;quot;MWprecipitation&amp;quot;, where the occurrence of less than 48 valid half-hourly samples per day is very common. The counts of the valid half-hourly samples per day have always been provided as a separate variable, and users of daily data were advised to pay close attention to that variable and use it to calculate the correct precipitation daily rates. Starting with version &amp;quot;07&amp;quot;, this is done in production to minimize possible misinterpretations of the data. The counts are still provided in the data, but they are only given to gauge the significance of the daily rates, and reconstruct the simple totals if someone wishes to do so. The latency of the derived Early daily product is a couple of minutes after the last granule of GPM_3IMERGHHE for the UTC data day is received at GES DISC. Since the target latency of GPM_3IMERGHHE is 4 hours, the daily should appear about 4 hours after the closure of the UTC day. For information on the original data (GPM_3IMERGHHE), please see the Documentation (Related URL). The daily mean rate (mm/day) is derived by first computing the mean precipitation rate (mm/hour) in a grid cell for the data day, and then multiplying the result by 24.  Thus, for every grid cell we have                Pdaily_mean     &#x3D; SUM{Pi * 1[Pi valid]} / Pdaily_cnt  * 24, i&#x3D;[1,Nf]Where:
Pdaily_cnt &#x3D; SUM{1[Pi valid]}Pi              - half-hourly input, in (mm/hr)
Nf              - Number of half-hourly files per day, Nf&#x3D;48
1[.]            - Indicator function; 1 when Pi is valid, 0 otherwise
Pdaily_cnt      - Number of valid retrievals in a grid cell per day.Grid cells for which Pdaily_cnt&#x3D;0, are set to fill value in the Daily files.
Note that Pi&#x3D;0 is a valid value.Pdaily_cnt are provided in the data files as variables &amp;quot;precipitation_cnt&amp;quot; and &amp;quot;MWprecipitation_cnt&amp;quot;, for correspondingly the microwave-IR-gauge and microwave-only retrievals. They are only given to gauge the significance of the daily rates, and reconstruct the simple totals if someone wishes to do so. There are various ways the daily error could be estimated from the source half-hourly random error (variable &amp;quot;randomError&amp;quot;). The daily error provided in the data files is calculated in a fashion similar to the daily mean precipitation rate. First, the mean of the squared half-hourly &amp;quot;randomError&amp;quot;  for the day is computed, and the resulting (mm^2/hr) is converted to (mm^2/day). Finally, square root is taken to get the result in (mm/day):Perr_daily &#x3D; { SUM{ (Perr_i)^2 * 1[Perr_i valid] ) } / Ncnt_err  * 24}^0.5, i&#x3D;[1,Nf]
Ncnt_err   &#x3D; SUM( 1[Perr_i valid] )where:
Perr_i        - half-hourly input, &amp;quot;randomError&amp;quot;, (mm/hr)
Perr_daily    - Magnitude of the daily error, (mm/day)
Ncnt_err        - Number of valid half-hour error estimatesAgain, the sum of squared &amp;quot;randomError&amp;quot; can be reconstructed, and other estimates can be derived using the available counts in the Daily files.Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>GPM IMERG Final Precipitation L3 1 day 0.1 degree x 0.1 degree V07 (GPM_3IMERGDF) at GES DISC</title>
      <link>https://registry.opendata.aws/nasa-gpm3imergdf</link>
      <guid>https://registry.opendata.aws/nasa-gpm3imergdf</guid>
      <description>Version 07 is the current version of the data set. Older versions will no longer be available and have been superseded by Version 07.The Integrated Multi-satellitE Retrievals for GPM (IMERG) IMERG is a NASA product estimating global surface precipitation rates at a high resolution of 0.1° every half-hour beginning 2000.  It is part of the joint NASA-JAXA Global Precipitation Measurement (GPM) mission, using the GPM Core Observatory satellite as the standard to combine precipitation observations from an international constellation of satellites using advanced techniques.  IMERG can be used for global-scale applications as well as over regions with sparse or no reliable surface observations.  The fine spatial and temporal resolution of IMERG data allows them to be accumulated to the scale of the application for increased skill.  IMERG has three Runs with varying latencies in response to a range of application needs: rapid-response applications (Early Run, 4-h latency), same/next-day applications (Late Run, 14-h latency), and post-real-time research (Final Run, 3.5-month latency).  While IMERG strives for consistency and accuracy, satellite estimates of precipitation are expected to have lower skill over frozen surfaces, complex terrain, and coastal zones.  As well, the changing GPM satellite constellation over time may introduce artifacts that affect studies focusing on multi-year changes.This dataset is the GPM Level 3 IMERG  &lt;em&gt;Final&lt;/em&gt; Daily  10 x 10 km (GPM_3IMERGDF) derived from the half-hourly GPM_3IMERGHH.  The derived result represents the Final estimate of the daily mean precipitation rate in mm/day. The dataset is produced by first computing the mean precipitation rate in (mm/hour) in every grid cell, and then multiplying the result by 24.  This minimizes the possible dry bias in versions before &amp;quot;07&amp;quot;, in the simple daily totals  for cells where less than 48 half-hourly observations are valid for the day. The latter under-sampling is very rare in the combined microwave-infrared and rain gauge  dataset, variable &amp;quot;precipitation&amp;quot;,  and appears in higher latitudes. Thus, in most cases users of global &amp;quot;precipitation&amp;quot; data will not notice any difference. This correction, however, is noticeable in the high-quality microwave retrieval, variable &amp;quot;MWprecipitation&amp;quot;, where the occurrence of less than 48 valid half-hourly samples per day is very common. The counts of the valid half-hourly samples per day have always been provided as a separate variable, and users of daily data were advised to pay close attention to that variable and use it to calculate the correct precipitation daily rates. Starting with version &amp;quot;07&amp;quot;, this is done in production to minimize possible misinterpretations of the data. The counts are still provided in the data, but they are only given to gauge the significance of the daily rates, and reconstruct the simple totals if someone wishes to do so. The latency of the derived &lt;em&gt;Final&lt;/em&gt; Daily product depends on the delivery of the IMERG &lt;em&gt;Final&lt;/em&gt; Half-Hourly product GPM_IMERGHH. Since the latter are delivered in a batch, once per month for the entire month, with up to 4 months latency, so will be the latency for the Final Daily, plus about 24 hours. Thus, e.g. the Dailies for January  can be expected to appear no earlier than April 2. The daily mean rate (mm/day) is derived by first computing the mean precipitation rate (mm/hour) in a grid cell for the data day, and then multiplying the result by 24.  Thus, for every grid cell we have                Pdaily_mean     &#x3D; SUM{Pi * 1[Pi valid]} / Pdaily_cnt  * 24, i&#x3D;[1,Nf]Where:
Pdaily_cnt &#x3D; SUM{1[Pi valid]}Pi              - half-hourly input, in (mm/hr)
Nf              - Number of half-hourly files per day, Nf&#x3D;48
1[.]            - Indicator function; 1 when Pi is valid, 0 otherwise
Pdaily_cnt      - Number of valid retrievals in a grid cell per day.Grid cells for which Pdaily_cnt&#x3D;0, are set to fill value in the Daily files.
Note that Pi&#x3D;0 is a valid value.Pdaily_cnt are provided in the data files as variables &amp;quot;precipitation_cnt&amp;quot; and &amp;quot;MWprecipitation_cnt&amp;quot;, for correspondingly the microwave-IR-gauge and microwave-only retrievals. They are only given to gauge the significance of the daily rates, and reconstruct the simple totals if someone wishes to do so. There are various ways the daily error could be estimated from the source half-hourly random error (variable &amp;quot;randomError&amp;quot;). The daily error provided in the data files is calculated in a fashion similar to the daily mean precipitation rate. First, the mean of the squared half-hourly &amp;quot;randomError&amp;quot;  for the day is computed, and the resulting (mm^2/hr) is converted to (mm^2/day). Finally, square root is taken to get the result in (mm/day):Perr_daily &#x3D; { SUM{ (Perr_i)^2 * 1[Perr_i valid] ) } / Ncnt_err  * 24}^0.5, i&#x3D;[1,Nf]
Ncnt_err   &#x3D; SUM( 1[Perr_i valid] )where:
Perr_i        - half-hourly input, &amp;quot;randomError&amp;quot;, (mm/hr)
Perr_daily    - Magnitude of the daily error, (mm/day)
Ncnt_err        - Number of valid half-hour error estimatesAgain, the sum of squared &amp;quot;randomError&amp;quot; can be reconstructed, and other estimates can be derived using the available counts in the Daily files.Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>GPM IMERG Late Precipitation L3 1 day 0.1 degree x 0.1 degree V07 (GPM_3IMERGDL) at GES DISC</title>
      <link>https://registry.opendata.aws/nasa-gpm3imergdl</link>
      <guid>https://registry.opendata.aws/nasa-gpm3imergdl</guid>
      <description>Version 07 is the current version of the data set. Older versions will no longer be available and have been superseded by Version 07.The Integrated Multi-satellitE Retrievals for GPM (IMERG) IMERG is a NASA product estimating global surface precipitation rates at a high resolution of 0.1° every half-hour beginning 2000.  It is part of the joint NASA-JAXA Global Precipitation Measurement (GPM) mission, using the GPM Core Observatory satellite as the standard to combine precipitation observations from an international constellation of satellites using advanced techniques.  IMERG can be used for global-scale applications as well as over regions with sparse or no reliable surface observations.  The fine spatial and temporal resolution of IMERG data allows them to be accumulated to the scale of the application for increased skill.  IMERG has three Runs with varying latencies in response to a range of application needs: rapid-response applications (Early Run, 4-h latency), same/next-day applications (Late Run, 14-h latency), and post-real-time research (Final Run, 3.5-month latency).  While IMERG strives for consistency and accuracy, satellite estimates of precipitation are expected to have lower skill over frozen surfaces, complex terrain, and coastal zones.  As well, the changing GPM satellite constellation over time may introduce artifacts that affect studies focusing on multi-year changes.This dataset is the GPM Level 3 IMERG  Late Daily  10 x 10 km (GPM_3IMERGDL) derived from the half-hourly GPM_3IMERGHHL. The derived result represents a Late expedited estimate of the daily mean precipitation rate in mm/day. The dataset is produced by first computing the mean precipitation rate in (mm/hour) in every grid cell, and then multiplying the result by 24.  This minimizes the possible dry bias in versions before &amp;quot;07&amp;quot;, in the simple daily totals  for cells where less than 48 half-hourly observations are valid for the day. The latter under-sampling is very rare in the combined microwave-infrared (and rain gauge in the final) dataset, variable &amp;quot;precipitation&amp;quot;,  and appears in higher latitudes. Thus, in most cases users of global &amp;quot;precipitation&amp;quot; data will not notice any difference. This correction, however, is noticeable in the high-quality microwave retrieval, variable &amp;quot;MWprecipitation&amp;quot;, where the occurrence of less than 48 valid half-hourly samples per day is very common. The counts of the valid half-hourly samples per day have always been provided as a separate variable, and users of daily data were advised to pay close attention to that variable and use it to calculate the correct precipitation daily rates. Starting with version &amp;quot;07&amp;quot;, this is done in production to minimize possible misinterpretations of the data. The counts are still provided in the data, but they are only given to gauge the significance of the daily rates, and reconstruct the simple totals if someone wishes to do so. The latency of the derived Late daily product is a couple of minutes after the last granule of GPM_3IMERGHHL for the UTC data day is received at GES DISC. Since the target latency of GPM_3IMERGHHL is 14 hours, the daily should appear no earlier than 14 hours after the closure of the UTC day. For information on the original data (GPM_3IMERGHHL), please see the Documentation (Related URL).  The daily mean rate (mm/day) is derived by first computing the mean precipitation rate (mm/hour) in a grid cell for the data day, and then multiplying the result by 24.  Thus, for every grid cell we have                Pdaily_mean     &#x3D; SUM{Pi * 1[Pi valid]} / Pdaily_cnt  * 24, i&#x3D;[1,Nf]Where:
Pdaily_cnt &#x3D; SUM{1[Pi valid]}Pi              - half-hourly input, in (mm/hr)
Nf              - Number of half-hourly files per day, Nf&#x3D;48
1[.]            - Indicator function; 1 when Pi is valid, 0 otherwise
Pdaily_cnt      - Number of valid retrievals in a grid cell per day.Grid cells for which Pdaily_cnt&#x3D;0, are set to fill value in the Daily files.
Note that Pi&#x3D;0 is a valid value.Pdaily_cnt are provided in the data files as variables &amp;quot;precipitation_cnt&amp;quot; and &amp;quot;MWprecipitation_cnt&amp;quot;, for correspondingly the microwave-IR-gauge and microwave-only retrievals. They are only given to gauge the significance of the daily rates, and reconstruct the simple totals if someone wishes to do so. There are various ways the daily error could be estimated from the source half-hourly random error (variable &amp;quot;randomError&amp;quot;). The daily error provided in the data files is calculated in a fashion similar to the daily mean precipitation rate. First, the mean of the squared half-hourly &amp;quot;randomError&amp;quot;  for the day is computed, and the resulting (mm^2/hr) is converted to (mm^2/day). Finally, square root is taken to get the result in (mm/day):Perr_daily &#x3D; { SUM{ (Perr_i)^2 * 1[Perr_i valid] ) } / Ncnt_err  * 24}^0.5, i&#x3D;[1,Nf]
Ncnt_err   &#x3D; SUM( 1[Perr_i valid] )where:
Perr_i        - half-hourly input, &amp;quot;randomError&amp;quot;, (mm/hr)
Perr_daily    - Magnitude of the daily error, (mm/day)
Ncnt_err        - Number of valid half-hour error estimatesAgain, the sum of squared &amp;quot;randomError&amp;quot; can be reconstructed, and other estimates can be derived using the available counts in the Daily files.Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>Genome in a Bottle on AWS</title>
      <link>https://registry.opendata.aws/giab</link>
      <guid>https://registry.opendata.aws/giab</guid>
      <description>Several reference genomes to enable translation of whole human genome sequencing to clinical practice. On 11/12/2020 these data were updated to reflect the most &lt;a href&#x3D;&quot;https://www.nist.gov/programs-projects/genome-bottle&quot;&gt;up to date GIAB release&lt;/a&gt;.</description>
    </item>
    <item>
      <title>High Resolution Canopy Height Maps by WRI and Meta</title>
      <link>https://registry.opendata.aws/dataforgood-fb-forests</link>
      <guid>https://registry.opendata.aws/dataforgood-fb-forests</guid>
      <description>Global and regional Canopy Height Maps (CHM). Created using machine learning models on high-resolution worldwide Maxar satellite imagery. </description>
    </item>
    <item>
      <title>IDEAM - Colombian Radar Network</title>
      <link>https://registry.opendata.aws/ideam-radares</link>
      <guid>https://registry.opendata.aws/ideam-radares</guid>
      <description>Historical and one-day delay data from the IDEAM radar network.</description>
    </item>
    <item>
      <title>International Skin Imaging Collaboration (ISIC) Archive</title>
      <link>https://registry.opendata.aws/isic-archive</link>
      <guid>https://registry.opendata.aws/isic-archive</guid>
      <description>A public-access archive of skin lesion images, supporting teaching, research, and the development and evaluation of diagnostic algorithms.</description>
    </item>
    <item>
      <title>JAXA / USGS / NASA Kaguya/SELENE Terrain Camera Digital Terrain Models</title>
      <link>https://registry.opendata.aws/jaxa-usgs-nasa-kaguya-tc-dtms</link>
      <guid>https://registry.opendata.aws/jaxa-usgs-nasa-kaguya-tc-dtms</guid>
      <description>The Japan Aerospace EXploration Agency (JAXA) SELenological and ENgineering Explorer (SELENE) mission’s Kaguya spacecraft was launched on September 14, 2007 and science operations around the Moon started October 20, 2007. The primary mission in a circular polar orbit 100-km above the surface lasted from October 20, 2007 until October 31, 2008. An extended mission was then conducted in lower orbits (averaging 50km above the surface) from November 1, 2008 until the SELENE mission ended with Kaguya impacting the Moon on June 10, 2009. These data are digital terrain models derived using the NASA Ames Stereo Pipeline (ASP) and the Kaguya stereoscopic data. Digital terrain models (DTMs) in this data set were bundle adjusted and aligned to Lunar Orbiter Laser Altimeter (LOLA) shot data. The sensor model intrinsics used for these data have been re-estimated to reduce inter-DTM horizontal and vertical errors. Data are controlled to LOLA using the ASP pc_align program. Data co-register at orthoimage resolution (11-37 meters per pixel). At image resolution horizontal offsets are measurable. Horizontal precision is measures to be better than 30 meters per pixel on average. Vertical errors are mean centered to zero. An assessment of overlapping DTMs showed vertical precision on the order of 4 meters. Spacecraft jitter and unmodelled lense distortion at the observation edges is believed to be the major contributor to the vertical errors. To create these analysis ready data, we have taken the ASP genreated data, map projected the data to a stereopair centered orthographic projection and converted to a Cloud Optimized GeoTiff (COG) for online streaming. These data use a priori spacecraft ephemerides (for the nominal mission) and improved, but not controlled spacecraft ephemerides for the extended mission. These data co-register with other LOLA controlled data to the aforementioned horizontal and vertical accuracies.</description>
    </item>
    <item>
      <title>JAXA / USGS / NASA Kaguya/SELENE Terrain Camera Observations</title>
      <link>https://registry.opendata.aws/jaxa-usgs-nasa-kaguya-tc</link>
      <guid>https://registry.opendata.aws/jaxa-usgs-nasa-kaguya-tc</guid>
      <description>The Japan Aerospace EXploration Agency (JAXA) SELenological and ENgineering Explorer (SELENE) mission’s Kaguya spacecraft was launched on September 14, 2007 and science operations around the Moon started October 20, 2007. The primary mission in a circular polar orbit 100-km above the surface lasted from October 20, 2007 until October 31, 2008. An extended mission was then conducted in lower orbits (averaging 50km above the surface) from November 1, 2008 until the SELENE mission ended with Kaguya impacting the Moon on June 10, 2009. These data were collected in monoscopic observing mode. To create these analysis ready data, we have taken the JAXA Data ARchives and Transmission System (DARTS) archived data, map projected the data to equirectangular or polar stereographic (pole centered) based on the center latitude of the observation, and converted to a Cloud Optimized GeoTiff (COG) for online streaming. These data use a priori spacecraft ephemerides (for the nominal mission) and improved, but not controlled spacecraft ephemerides for the extended mission. Therefore, these uncontrolled data are not guaranteed to co-register with other data sets.</description>
    </item>
    <item>
      <title>Met Office Blended Probabilistic Forecast – Global gridded percentiles</title>
      <link>https://registry.opendata.aws/met-office-bpf-global-gridded-percentiles</link>
      <guid>https://registry.opendata.aws/met-office-bpf-global-gridded-percentiles</guid>
      <description>This product provides percentile weather forecasts. The grid resolution is approximately 20km and covers the whole globe. It is produced by the Met Office IMPROVER Blended Probabilistic Forecast system. It is available in NetCDF format. 
&lt;br&gt;&lt;br&gt;Blended Probabilistic Forecast data is derived from the Met Office&amp;#39;s operational NWP (Numerical Weather Prediction) ensembles and nowcasts. To give more reliable predictions, these are then blended and calibrated using the IMPROVER pipeline, and verified using spread–skill and reliability checks. 
&lt;br&gt;&lt;br&gt;This is 1 of 8 Blended Probabilistic Forecast products published by the Met Office on the Registry of Open Data on AWS. Data is available for the Global and UK domains, as gridded and spot (site-specific), and represented as percentiles and probabilities. 
&lt;br&gt;&lt;br&gt;This info is correct as of April 2026, but some things (like the number of sites, parameters and timesteps) may change in future. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;How percentiles work&lt;/b&gt;
&lt;br&gt;
Ensemble forecasts show a range of possible weather outcomes. However, some users may find it more useful to see ensemble forecasts presented as percentiles, particularly when they want to see where each member of an ensemble sits within the full range of possible outcomes. 
&lt;br&gt;&lt;br&gt;Percentiles are generated from an ensemble forecast by first sorting all the members of that ensemble, for example from the coldest temperature to the warmest. To then identify a particular percentile forecast (e.g. the 10th percentile), we find the temperature at which 10% of the ensemble members predict colder conditions. As only 10% of the ensemble members are predicting a lower temperature than the 10th percentile forecast, this indicates that it is giving a relatively low forecast of temperature. Similarly, 90% of ensemble members would predict a lower temperature than the 90th percentile forecast, indicating that it is giving a relatively high forecast of temperature.&lt;br&gt;&lt;br&gt;&lt;br&gt;&lt;b&gt;Precipitation percentiles should be used cautiously&lt;/b&gt;
&lt;br&gt;
Precipitation percentiles are potentially useful for experts. But we don&amp;#39;t recommend that most people use them, as they are hard to interpret. 
&lt;br&gt;&lt;br&gt;Precipitation is spatially noisy (i.e. it can vary a lot over small distances), especially when it is showery. This means that the individual ensemble forecasts that the percentiles are generated from are likely to have their heaviest precipitation positioned in different places. As a result, a high percentile (e.g. 95th) will pick up the high values from all those different locations and make it appear that heavy rain could occur over a wider area than is physically plausible. In other words, the spatial extent of the precipitation when using a high percentile is not physically realistic. High percentiles can be very useful for finding out what the values at the higher end may be, but not how they are spatially organised. 
&lt;br&gt;&lt;br&gt;Likewise, the spatial extent of the precipitation will be greatly reduced for the lower percentiles. If there are differences between the ensemble forecasts about where it will rain or not, it is possible that a low percentile precipitation field may show zero precipitation everywhere. Again, that is potentially misleading because it suggests it might be dry everywhere, which is not what the individual forecasts are necessarily saying. It is better to view different percentile maps together (5th, 50th, 95th) to get a more informative impression. 
&lt;br&gt;&lt;br&gt;Even the 50th percentile can be misleading as, by definition, it will never include the highest predicted values. Nor is there any guarantee that the peaks in the 50th percentile grid will align with the peaks in the 95th percentile grid. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;About the grid&lt;/b&gt;
&lt;br&gt;
The grid resolution for Best Probabilistic Forecast Global gridded probabilities is approximately 20km and covers the whole globe. 
&lt;br&gt;&lt;br&gt;Numerical weather prediction (NWP) models generate forecasts for each grid point within a geographical area of interest. Each of these gridded forecasts corresponds to a particular diagnostic (e.g. precipitation rate) at a particular time. IMPROVER then takes an ensemble of these gridded forecasts and applies post-processing techniques to enhance them and represent them probabilistically. The resulting grid of values represents probabilities of exceeding or falling below a particular threshold.&lt;br&gt;&lt;br&gt;&lt;br&gt;&lt;table&gt;
&lt;tr&gt;&lt;th&gt;Aspect&lt;/th&gt;&lt;th&gt;Values&lt;/th&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Projection&lt;/td&gt;&lt;td&gt;Equirectangular Latitude-Longitude&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Standard parallel&lt;/td&gt;&lt;td&gt;48.16° N&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Reference datum&lt;/td&gt;&lt;td&gt;earth_radius &#x3D; 6371229.0 m&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Nominal resolution&lt;/td&gt;&lt;td&gt;20 km or N640&lt;/td&gt;&lt;/tr&gt; 
&lt;tr&gt;&lt;td&gt;North-South spacing&lt;/td&gt;&lt;td&gt;0.1875° (20.85 km)&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;East-West spacing&lt;/td&gt;&lt;td&gt;0.28125° (~20.86 km - UK, 31.27 km - equator)&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;North-West corner&lt;/td&gt;&lt;td&gt;89.90625°N, 179.859375°W&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;South-West corner&lt;/td&gt;&lt;td&gt;89.90625°S, 179.859375°W&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;South-East corner&lt;/td&gt;&lt;td&gt;89.90625°S, 179.859375°E&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;North-East corner&lt;/td&gt;&lt;td&gt;89.90625°N, 179.859375°E&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;East-West points&lt;/td&gt;&lt;td&gt;1280&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;North-South points&lt;/td&gt;&lt;td&gt;960&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Grid type&lt;/td&gt;&lt;td&gt;Arakawa A&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;
&lt;br&gt;&lt;br&gt;

&lt;b&gt;Parameters and timesteps&lt;/b&gt;
&lt;br&gt;
There are 38 weather parameters available including:  &lt;ul&gt;
&lt;li&gt;Cloud  &lt;/li&gt;
&lt;li&gt;Temperature&lt;/li&gt;
&lt;li&gt;Pressure&lt;/li&gt;
&lt;li&gt;Humidity&lt;/li&gt;
&lt;li&gt;Visibility  &lt;/li&gt;
&lt;li&gt;Precipitation rate and accumulations (see note above about care required with use)&lt;/li&gt;
&lt;li&gt;UV&lt;/li&gt;
&lt;li&gt;Wind
&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
For most parameters, the following timesteps are available: &lt;ul&gt;
&lt;li&gt;Every hour from 0 to 120 hours &lt;/li&gt;
&lt;li&gt;Every 3 hours from 123 to 192 hours
&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
However, timesteps vary significantly for some parameters. Check the &lt;a href&#x3D;&quot;https://www.metoffice.gov.uk/binaries/content/assets/metofficegovuk/csv/data/blended-probabilistic-forecast-parameter-catalogue.xlsx&quot;&gt;parameter documentation&lt;/a&gt; for more details. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;Latency&lt;/b&gt;
&lt;br&gt;
Data is made available shortly after the blend time. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;Archive length&lt;/b&gt;
&lt;br&gt;
Data is available for the past 30 days. 
&lt;br&gt;
&lt;br&gt; &lt;b&gt;Business needs&lt;/b&gt;
&lt;br&gt;
This product supports risk-based decision-making by providing uncertainty ranges rather than single deterministic values. Typical uses include:&lt;ul&gt;
&lt;li&gt;assessing uncertainty for operational planning&lt;/li&gt;
&lt;li&gt;evaluating weather-related risk thresholds&lt;/li&gt;
&lt;li&gt;deriving deterministic products (e.g. 50th percentile) from probabilistic outputs 
&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
Gridded forecasts show how a diagnostic varies spatially across a domain at a given time. By using a time series of gridded fields, you can determine how a weather diagnostic is expected to evolve across a geographic area. 
&lt;br&gt;&lt;br&gt;If you need a forecast for a specific location, a spot forecast may suit your needs better than gridded data. Spot Blended Probabilistic Forecasts are also available as percentiles and probabilities for both the UK and Global domains.</description>
    </item>
    <item>
      <title>Met Office Blended Probabilistic Forecast – Global gridded probabilities</title>
      <link>https://registry.opendata.aws/met-office-bpf-global-gridded-probabilities</link>
      <guid>https://registry.opendata.aws/met-office-bpf-global-gridded-probabilities</guid>
      <description>This product provides gridded probabilistic weather forecasts. The grid resolution is approximately 20km and covers the whole globe. It is produced by the Met Office IMPROVER Blended Probabilistic Forecast system. It is available in NetCDF format.
&lt;br&gt;&lt;br&gt;
Blended Probabilistic Forecast data is derived from the Met Office&amp;#39;s operational NWP (Numerical Weather Prediction) ensembles and nowcasts. To give more reliable predictions, these are then blended and calibrated using the IMPROVER pipeline, and verified using spread–skill and reliability checks. 
&lt;br&gt;&lt;br&gt;
This is 1 of 8 Blended Probabilistic Forecast products published by the Met Office on the Registry of Open Data on AWS. Data is available for the Global and UK domains, as gridded and spot (site-specific), and represented as percentiles and probabilities. 
&lt;br&gt;&lt;br&gt;
This info is correct as of April 2026, but some things (like the number of sites, parameters and timesteps) may change in future. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;How probabilities work&lt;/b&gt;
&lt;br&gt;
Ensemble forecasts show a range of possible weather outcomes. However, some users may find it more useful to see ensemble forecasts presented as probabilities, particularly when they&amp;#39;re interested in specific thresholds.
&lt;br&gt;&lt;br&gt;
Probabilities are generated from an ensemble forecast by counting how many members of that ensemble exceed a particular threshold value. For example, if the threshold for screen temperature is 5°C, and 9 out of 18 ensemble members show a screen temperature above 5°C, there is a 50% chance of temperatures exceeding 5°C.
&lt;br&gt;&lt;br&gt;&lt;b&gt;About the grid&lt;/b&gt; 
&lt;br&gt;
The grid resolution for Blended Probabilistic Forecast Global gridded probabilities is approximately 20km and covers the whole globe. 
&lt;br&gt;&lt;br&gt;
Numerical weather prediction (NWP) models generate forecasts for each grid point within a geographical area of interest. Each of these gridded forecasts corresponds to a particular diagnostic (e.g. precipitation rate) at a particular time. IMPROVER then takes an ensemble of these gridded forecasts and applies post-processing techniques to enhance them and represent them probabilistically. The resulting grid of values represents probabilities of exceeding or falling below a particular threshold. 
&lt;br&gt;&lt;br&gt;&lt;table&gt;
&lt;tr&gt;&lt;th&gt;Aspect&lt;/th&gt;&lt;th&gt;Values&lt;/th&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Projection&lt;/td&gt;&lt;td&gt;Equirectangular Latitude-Longitude&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Standard parallel&lt;/td&gt;&lt;td&gt;48.16° N&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Reference datum&lt;/td&gt;&lt;td&gt;earth_radius &#x3D; 6371229.0 m&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Nominal resolution&lt;/td&gt;&lt;td&gt;20 km or N640&lt;/td&gt;&lt;/tr&gt; 
&lt;tr&gt;&lt;td&gt;North-South spacing&lt;/td&gt;&lt;td&gt;0.1875° (20.85 km)&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;East-West spacing&lt;/td&gt;&lt;td&gt;0.28125° (~20.86 km - UK, 31.27 km - equator)&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;North-West corner&lt;/td&gt;&lt;td&gt;89.90625°N, 179.859375°W&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;South-West corner&lt;/td&gt;&lt;td&gt;89.90625°S, 179.859375°W&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;South-East corner&lt;/td&gt;&lt;td&gt;89.90625°S, 179.859375°E&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;North-East corner&lt;/td&gt;&lt;td&gt;89.90625°N, 179.859375°E&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;East-West points&lt;/td&gt;&lt;td&gt;1280&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;North-South points&lt;/td&gt;&lt;td&gt;960&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Grid type&lt;/td&gt;&lt;td&gt;Arakawa A&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;
&lt;br&gt;&lt;br&gt;

&lt;b&gt;Parameters and timesteps&lt;/b&gt; 
&lt;br&gt;
There are 31 weather parameters available including:  &lt;ul&gt;
&lt;li&gt;Cloud  &lt;/li&gt;
&lt;li&gt;Lightning  &lt;/li&gt;
&lt;li&gt;Humidity  &lt;/li&gt;
&lt;li&gt;Visibility  &lt;/li&gt;
&lt;li&gt;Precipitation rate and accumulations  &lt;/li&gt;
&lt;li&gt;UV  &lt;/li&gt;
&lt;li&gt;Wind
&lt;br&gt;&lt;br&gt;
For most parameters, the following timesteps are available:&lt;/li&gt;
&lt;li&gt;Every hour from 0 to 120 hours &lt;/li&gt;
&lt;li&gt;Every 3 hours from 123 to 192 hours 
&lt;br&gt;&lt;br&gt;
However, timesteps vary significantly for some parameters. Check the &lt;a href&#x3D;&quot;https://www.metoffice.gov.uk/binaries/content/assets/metofficegovuk/csv/data/blended-probabilistic-forecast-parameter-catalogue.xlsx&quot;&gt;parameter documentation&lt;/a&gt; for more details. 
&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
&lt;b&gt;Latency&lt;/b&gt;
&lt;br&gt;
Data is made available shortly after the blend time. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;Archive length&lt;/b&gt;
&lt;br&gt;
Data is available for the past 30 days. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;Business needs&lt;/b&gt;
&lt;br&gt;
This product supports risk-based decision-making by providing uncertainty ranges rather than single deterministic values. Typical uses include: &lt;ul&gt;
&lt;li&gt;assessing uncertainty for operational planning  &lt;/li&gt;
&lt;li&gt;evaluating weather-related risk thresholds  &lt;/li&gt;
&lt;li&gt;deriving deterministic products (e.g. 50th percentile) from probabilistic outputs
&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
Gridded forecasts show how a diagnostic varies spatially across a domain at a given time. By using a time series of gridded fields, you can determine how a weather diagnostic is expected to evolve across a geographic area. 
&lt;br&gt;&lt;br&gt;If you need a forecast for a specific location, a spot forecast may suit your needs better than gridded data. Spot Blended Probabilistic Forecasts are also available as percentiles and probabilities for both the UK and Global domains. </description>
    </item>
    <item>
      <title>Met Office Blended Probabilistic Forecast – Global spot percentiles</title>
      <link>https://registry.opendata.aws/met-office-bpf-global-spot-percentiles</link>
      <guid>https://registry.opendata.aws/met-office-bpf-global-spot-percentiles</guid>
      <description>This product provides percentile weather forecasts for 5,956 sites (or spots) across the globe. It is produced by the Met Office IMPROVER Blended Probabilistic Forecast system. It is available in NetCDF format.
&lt;br&gt;&lt;br&gt;Blended Probabilistic Forecast data is derived from the Met Office&amp;#39;s operational NWP (Numerical Weather Prediction) ensembles and nowcasts. To give more reliable predictions, these are then blended and calibrated using the IMPROVER pipeline, and verified using spread–skill and reliability checks. 
&lt;br&gt;&lt;br&gt;This is 1 of 8 Blended Probabilistic Forecast products published by the Met Office on the Registry of Open Data on AWS. Data is available for the Global and UK domains, as gridded and spot (site-specific), and represented as percentiles and probabilities. 
&lt;br&gt;&lt;br&gt;This info is correct as of April 2026, but some things (like the number of sites, parameters and timesteps) may change in future.
&lt;br&gt;&lt;br&gt;&lt;b&gt;How percentiles work&lt;/b&gt;
&lt;br&gt;Ensemble forecasts show a range of possible weather outcomes. However, some users may find it more useful to see ensemble forecasts presented as percentiles, particularly when they want to see where each member of an ensemble sits within the full range of possible outcomes. 
&lt;br&gt;&lt;br&gt;
Percentiles are generated from an ensemble forecast by first sorting all the members of that ensemble, for example from the coldest temperature to the warmest. To then identify a particular percentile forecast (e.g. the 10th percentile), we find the temperature at which 10% of the ensemble members predict colder conditions. As only 10% of the ensemble members are predicting a lower temperature than the 10th percentile forecast, this indicates that it is giving a relatively low forecast of temperature. Similarly, 90% of ensemble members would predict a lower temperature than the 90th percentile forecast, indicating that it is giving a relatively high forecast of temperature. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;Precipitation percentiles should be used cautiously&lt;/b&gt; 
&lt;br&gt;
Precipitation percentiles are potentially useful for experts. But we don&amp;#39;t recommend that most people use them, as they are hard to interpret. 
&lt;br&gt;&lt;br&gt;Precipitation is spatially noisy (i.e. it can vary a lot over small distances), especially when it is showery. This means that the individual ensemble forecasts that the percentiles are generated from are likely to have their heaviest precipitation positioned in different places. As a result, a high percentile (e.g. 95th) will pick up the high values from all those different locations and make it appear that heavy rain could occur over a wider area than is physically plausible. In other words, the spatial extent of the precipitation when using a high percentile is not physically realistic. High percentiles can be very useful for finding out what the values at the higher end may be, but not how they are spatially organised. 
&lt;br&gt;&lt;br&gt;Likewise, the spatial extent of the precipitation will be greatly reduced for the lower percentiles. If there are differences between the ensemble forecasts about where it will rain or not, it is possible that a low percentile precipitation field may show zero precipitation everywhere. Again, that is potentially misleading because it suggests it might be dry everywhere, which is not what the individual forecasts are necessarily saying. It is better to view different percentile maps together (5th, 50th, 95th) to get a more informative impression. 
&lt;br&gt;&lt;br&gt;Even the 50th percentile can be misleading as, by definition, it will never include the highest predicted values. Nor is there any guarantee that the peaks in the 50th percentile grid will align with the peaks in the 95th percentile grid. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;How spot data works&lt;/b&gt; 
&lt;br&gt;
Spot data is derived by extracting site‑specific forecasts from post‑processed gridded forecasts. 
&lt;br&gt;&lt;br&gt;IMPROVER operates on two domains: &lt;ul&gt;
&lt;li&gt;the UK domain, which primarily covers the region around the United Kingdom, Ireland and parts of Western Europe &lt;/li&gt;
&lt;li&gt;the Global domain, which covers the whole world&lt;/li&gt;
&lt;/ul&gt;
Within each domain, IMPROVER post-processes most forecasts on a grid, though the resolution of this grid differs between the two domains. Site-specific forecasts are drawn from these grids at the end of the post-processing chains. Sites within the UK domain draw forecasts from the high-resolution UK domain grid, as this should provide the best possible forecast, whereas sites outside of this domain draw from the lower resolution Global grid. The two domains are represented in two separate datasets. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;Global domain sites&lt;/b&gt;
&lt;br&gt;There are 5,956 sites in the Global domain. (The Global domain excludes the British Isles and parts of Western Europe. For sites in the UK, Ireland and the parts of Western Europe not included in the Global domain, please see the UK Spot Percentiles dataset.) 
&lt;br&gt;&lt;br&gt;Site-specific forecasts in the Global domain are calculated from the MOGREPS-G model alone. However this model is time-lagged to provide additional forecast spread and reduce inter-cycle variation. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;Parameters and timesteps&lt;/b&gt;
&lt;br&gt;
There are 68 weather parameters available including:  &lt;ul&gt;
&lt;li&gt;Cloud&lt;/li&gt;
&lt;li&gt;Temperature&lt;/li&gt;
&lt;li&gt;Pressure&lt;/li&gt;
&lt;li&gt;Humidity&lt;/li&gt;
&lt;li&gt;Visibility&lt;/li&gt;
&lt;li&gt;Precipitation rate and accumulations (see note above about care required with use)&lt;/li&gt;
&lt;li&gt;UV&lt;/li&gt;
&lt;li&gt;Wind
&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
For most parameters, the following timesteps are available: &lt;ul&gt;
&lt;li&gt;Every hour from 0 to 120 hours &lt;/li&gt;
&lt;li&gt;Every 3 hours from 123 to 192 hours 
&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
However, timesteps vary significantly for some parameters. Check the &lt;a href&#x3D;&quot;https://www.metoffice.gov.uk/binaries/content/assets/metofficegovuk/csv/data/blended-probabilistic-forecast-parameter-catalogue.xlsx&quot;&gt;parameter documentation&lt;/a&gt; for more details. 
&lt;br&gt;&lt;br&gt;This dataset also contains deterministic “weather symbol” parameters. These are designed to complement the percentiles information in cases where the user wants to extract a single “deterministic” forecast. The 50th percentile works well for some parameters, but others are better represented by the weather symbol. Check the &lt;a href&#x3D;&quot;https://www.metoffice.gov.uk/binaries/content/assets/metofficegovuk/csv/data/blended-probabilistic-forecast-parameter-catalogue.xlsx&quot;&gt;parameter documentation&lt;/a&gt; for guidance on where this applies. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;Latency&lt;/b&gt;
&lt;br&gt;
Data is made available shortly after the blend time. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;Archive length&lt;/b&gt;
&lt;br&gt;
Data is available for the past 30 days. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;Business needs&lt;/b&gt;
&lt;br&gt;
This product supports risk-based decision-making by providing uncertainty ranges rather than single deterministic values. Typical uses include: &lt;ul&gt;
&lt;li&gt;assessing uncertainty for operational planning&lt;/li&gt;
&lt;li&gt;evaluating weather-related risk thresholds&lt;/li&gt;
&lt;li&gt;deriving deterministic products (e.g. 50th percentile) from probabilistic outputs
&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
Spot forecasts provide information about weather diagnostics at single sites. By using a time series of these forecasts, you can determine how a weather diagnostic is expected to evolve at a particular location. This is ideal for users if you are not moving spatially and are instead interested in how conditions are evolving at your location. This is the kind of time-series information you see in the Met Office app when you look at a forecast for your home address.&lt;br&gt;&lt;br&gt;&lt;br&gt;Gridded forecasts show how a diagnostic varies spatially across a domain at a given time. By using a time series of gridded fields, you can determine how a weather diagnostic is expected to evolve across a geographic area. So you may find them more useful if you need to consider moving spatially. This kind of product is very familiar from television broadcast weather forecasts. Gridded Blended Probabilistic Forecasts are also available as percentiles and probabilities for both the UK and Global domains.  </description>
    </item>
    <item>
      <title>Met Office Blended Probabilistic Forecast – Global spot probabilities</title>
      <link>https://registry.opendata.aws/met-office-bpf-global-spot-probabilities</link>
      <guid>https://registry.opendata.aws/met-office-bpf-global-spot-probabilities</guid>
      <description>This product provides probabilistic weather forecasts for 5,956 sites (or spots) across the globe. It is produced by the Met Office IMPROVER Blended Probabilistic Forecast system. It is available in NetCDF format. 
&lt;br&gt;&lt;br&gt;Blended Probabilistic Forecast data is derived from the Met Office&amp;#39;s operational NWP (Numerical Weather Prediction) ensembles and nowcasts. To give more reliable predictions, these are then blended and calibrated using the IMPROVER pipeline, and verified using spread–skill and reliability checks. 
&lt;br&gt;&lt;br&gt;This is 1 of 8 Blended Probabilistic Forecast products published by the Met Office on the Registry of Open Data on AWS. Data is available for the Global and UK domains, as gridded and spot (site-specific), and represented as percentiles and probabilities. 
&lt;br&gt;&lt;br&gt;This info is correct as of April 2026, but some things (like the number of sites, parameters and timesteps) may change in future. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;How probabilities work&lt;/b&gt;
&lt;br&gt;Ensemble forecasts show a range of possible weather outcomes. However, some users may find it more useful to see ensemble forecasts presented as probabilities, particularly when they&amp;#39;re interested in specific thresholds. 
&lt;br&gt;&lt;br&gt;Probabilities are generated from an ensemble forecast by counting how many members of that ensemble exceed a particular threshold value. For example, if the threshold for screen temperature is 5°C, and 9 out of 18 ensemble members show a screen temperature above 5°C, there is a 50% chance of temperatures exceeding 5°C. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;How spot data works&lt;/b&gt;
&lt;br&gt;
Spot data is derived by extracting site‑specific forecasts from post‑processed gridded forecasts. 
&lt;br&gt;&lt;br&gt;IMPROVER operates on two domains: &lt;ul&gt;
&lt;li&gt;the UK domain, which primarily covers the region around the United Kingdom, Ireland and parts of Western Europe&lt;/li&gt;
&lt;li&gt;the Global domain, which covers the whole world
&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
Within each domain, IMPROVER post-processes most forecasts on a grid, though the resolution of this grid differs between the two domains. Site-specific forecasts are drawn from these grids at the end of the post-processing chains. Sites within the UK domain draw forecasts from the high-resolution UK domain grid, as this should provide the best possible forecast, whereas sites outside of this domain draw from the lower resolution Global grid. The two domains are represented in two separate datasets. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;Global domain sites&lt;/b&gt;
&lt;br&gt;
There are 5,956 sites in the Global domain. (The Global domain excludes the British Isles and parts of Western Europe. For sites in the UK, Ireland and the parts of Western Europe not included in the Global domain, please see the UK Spot Percentiles dataset.) 
&lt;br&gt;&lt;br&gt;Site-specific forecasts in the Global domain are calculated from the MOGREPS-G model alone. However this model is time-lagged to provide additional forecast spread and reduce inter-cycle variation. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;Parameters and timesteps&lt;/b&gt;
&lt;br&gt;
There are 33 weather parameters available including:&lt;ul&gt;
&lt;li&gt;Cloud&lt;/li&gt;
&lt;li&gt;Lightning&lt;/li&gt;
&lt;li&gt;Pressure&lt;/li&gt;
&lt;li&gt;Humidity&lt;/li&gt;
&lt;li&gt;Visibility&lt;/li&gt;
&lt;li&gt;Precipitation rate and accumulations&lt;/li&gt;
&lt;li&gt;UV&lt;/li&gt;
&lt;li&gt;Wind
&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
For most parameters, the following timesteps are available:&lt;ul&gt;
&lt;li&gt;Every hour from 0 to 120 hours&lt;/li&gt;
&lt;li&gt;Every 3 hours from 123 to 192 hours
&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
However, timesteps vary significantly for some parameters. Check the &lt;a href&#x3D;&quot;https://www.metoffice.gov.uk/binaries/content/assets/metofficegovuk/csv/data/blended-probabilistic-forecast-parameter-catalogue.xlsx&quot;&gt;parameter documentation&lt;/a&gt; for more details. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;Latency&lt;/b&gt;
&lt;br&gt;
Data is made available shortly after the model blend time. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;Archive length&lt;/b&gt;
&lt;br&gt;
Data is available for the past 30 days. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;Business needs&lt;/b&gt;
&lt;br&gt;
This product supports risk-based decision-making by providing uncertainty ranges rather than single deterministic values. Typical uses include: &lt;ul&gt;
&lt;li&gt;assessing uncertainty for operational planning&lt;/li&gt;
&lt;li&gt;evaluating weather-related risk thresholds&lt;/li&gt;
&lt;li&gt;deriving deterministic products (e.g. 50th percentile) from probabilistic outputs 
&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
Spot forecasts provide information about weather diagnostics at single sites. By using a time series of these forecasts, you can determine how a weather diagnostic is expected to evolve at a particular location. This is ideal for users if you are not moving spatially and are instead interested in how conditions are evolving at your location. This is the kind of time-series information you see in the Met Office app when you look at a forecast for your home address.&lt;br&gt;&lt;br&gt;&lt;br&gt;Gridded forecasts show how a diagnostic varies spatially across a domain at a given time. By using a time series of gridded fields, you can determine how a weather diagnostic is expected to evolve across a geographic area. So you may find them more useful if you need to consider moving spatially. This kind of product is very familiar from television broadcast weather forecasts. Gridded Blended Probabilistic Forecasts are also available as percentiles and probabilities for both the UK and Global domains.</description>
    </item>
    <item>
      <title>Met Office Blended Probabilistic Forecast – UK Spot Percentiles</title>
      <link>https://registry.opendata.aws/met-office-bpf-uk-spot-percentiles</link>
      <guid>https://registry.opendata.aws/met-office-bpf-uk-spot-percentiles</guid>
      <description>This product provides percentile weather forecasts for 7,213 sites (or spots) across the United Kingdom, Ireland and parts of Western Europe. It is produced by the Met Office IMPROVER Blended Probabilistic Forecast system. It is available in NetCDF format. 
&lt;br&gt;&lt;br&gt;Blended Probabilistic Forecast data is derived from the Met Office&amp;#39;s operational NWP (Numerical Weather Prediction) ensembles and nowcasts. To give more reliable predictions, these are then blended and calibrated using the IMPROVER pipeline, and verified using spread–skill and reliability checks. 
&lt;br&gt;&lt;br&gt;This is 1 of 8 Blended Probabilistic Forecast products published by the Met Office on the Registry of Open Data on AWS. Data is available for the Global and UK domains, as gridded and spot (site-specific), and represented as percentiles and probabilities. 
&lt;br&gt;&lt;br&gt;This info is correct as of April 2026, but some things (like the number of sites, parameters and timesteps) may change in future. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;How percentiles work&lt;/b&gt;
&lt;br&gt;
Ensemble forecasts show a range of possible weather outcomes. However, some users may find it more useful to see ensemble forecasts presented as percentiles, particularly when they want to see where each member of an ensemble sits within the full range of possible outcomes. 
&lt;br&gt;&lt;br&gt;Percentiles are generated from an ensemble forecast by first sorting all the members of that ensemble, for example from the coldest temperature to the warmest. To then identify a particular percentile forecast (e.g. the 10th percentile), we find the temperature at which 10% of the ensemble members predict colder conditions. As only 10% of the ensemble members are predicting a lower temperature than the 10th percentile forecast, this indicates that it is giving a relatively low forecast of temperature. Similarly, 90% of ensemble members would predict a lower temperature than the 90th percentile forecast, indicating that it is giving a relatively high forecast of temperature. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;Precipitation percentiles should be used cautiously&lt;/b&gt;
&lt;br&gt;
Precipitation percentiles are potentially useful for experts. But we don&amp;#39;t recommend that most people use them, as they are hard to interpret. 
&lt;br&gt;&lt;br&gt;Precipitation is spatially noisy (i.e. it can vary a lot over small distances), especially when it is showery. This means that the individual ensemble forecasts that the percentiles are generated from are likely to have their heaviest precipitation positioned in different places. As a result, a high percentile (e.g. 95th) will pick up the high values from all those different locations and make it appear that heavy rain could occur over a wider area than is physically plausible. In other words, the spatial extent of the precipitation when using a high percentile is not physically realistic. High percentiles can be very useful for finding out what the values at the higher end may be, but not how they are spatially organised. 
&lt;br&gt;&lt;br&gt;Likewise, the spatial extent of the precipitation will be greatly reduced for the lower percentiles. If there are differences between the ensemble forecasts about where it will rain or not, it is possible that a low percentile precipitation field may show zero precipitation everywhere. Again, that is potentially misleading because it suggests it might be dry everywhere, which is not what the individual forecasts are necessarily saying. It is better to view different percentile maps together (5th, 50th, 95th) to get a more informative impression. 
&lt;br&gt;&lt;br&gt;Even the 50th percentile can be misleading as, by definition, it will never include the highest predicted values. Nor is there any guarantee that the peaks in the 50th percentile grid will align with the peaks in the 95th percentile grid. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;How spot data works&lt;/b&gt;
&lt;br&gt;
Spot data is derived by extracting site‑specific forecasts from post‑processed gridded forecasts. 
&lt;br&gt;&lt;br&gt;IMPROVER operates on two domains: &lt;ul&gt;
&lt;li&gt;the UK domain, which primarily covers the region around the United Kingdom, Ireland and parts of Western Europe &lt;/li&gt;
&lt;li&gt;the Global domain, which covers the whole world 
&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
Within each domain, IMPROVER post-processes most forecasts on a grid, though the resolution of this grid differs between the two domains. Site-specific forecasts are drawn from these grids at the end of the post-processing chains.&lt;br&gt;&lt;br&gt;&lt;br&gt;&lt;b&gt;UK domain sites&lt;/b&gt;
&lt;br&gt;
There are 7,213 forecast sites in the UK domain. IMPROVER calculates forecasts for these sites from UK domain gridded forecasts. These gridded forecasts are generated from a lead-time-dependent blend of up to 4 forecasting models: an extrapolation nowcast (MONOW), UKV, MOGREPS-UK, and MOGREPS-G. The blend can also involve multiple cycles of a model at different lead times. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;Parameters and timesteps&lt;/b&gt;
&lt;br&gt;
There are 61 weather parameters available including:  &lt;ul&gt;
&lt;li&gt;Cloud&lt;/li&gt;
&lt;li&gt;Temperature&lt;/li&gt;
&lt;li&gt;Pressure&lt;/li&gt;
&lt;li&gt;Humidity&lt;/li&gt;
&lt;li&gt;Visibility&lt;/li&gt;
&lt;li&gt;Precipitation rate and accumulations&lt;/li&gt;
&lt;li&gt;UV&lt;/li&gt;
&lt;li&gt;Wind&lt;br&gt;&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
For most parameters, the following timesteps are available: &lt;ul&gt;
&lt;li&gt;Every hour from 0 to 120 hours &lt;/li&gt;
&lt;li&gt;Every 3 hours from 123 to 186 hours 
&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
However, timesteps vary significantly for some parameters. Check the &lt;a href&#x3D;&quot;https://www.metoffice.gov.uk/binaries/content/assets/metofficegovuk/csv/data/blended-probabilistic-forecast-parameter-catalogue.xlsx&quot;&gt;parameter documentation&lt;/a&gt; for more details. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;Latency&lt;/b&gt;
&lt;br&gt;
Data is made available shortly after the model blend time. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;Archive length&lt;/b&gt;
&lt;br&gt;
Data is available for the past 30 days. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;Business needs&lt;/b&gt;&lt;br&gt;&lt;br&gt;
This product supports risk-based decision-making by providing uncertainty ranges rather than single deterministic values. Typical uses include: &lt;ul&gt;
&lt;li&gt;assessing uncertainty for operational planning&lt;/li&gt;
&lt;li&gt;evaluating weather-related risk thresholds&lt;/li&gt;
&lt;li&gt;deriving deterministic products (e.g. 50th percentile) from probabilistic outputs 
&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
Spot forecasts provide information about weather diagnostics at single sites. By using a time series of these forecasts, you can determine how a weather diagnostic is expected to evolve at a particular location. This is ideal for users if you are not moving spatially and are instead interested in how conditions are evolving at your location. This is the kind of time-series information you see in the Met Office app when you look at a forecast for your home address.
&lt;br&gt;&lt;br&gt;Gridded forecasts show how a diagnostic varies spatially across a domain at a given time. By using a time series of gridded fields, you can determine how a weather diagnostic is expected to evolve across a geographic area. So you may find them more useful if you need to consider moving spatially. This kind of product is very familiar from television broadcast weather forecasts. Gridded Blended Probabilistic Forecasts are also available as percentiles and probabilities for both the UK and Global domains. </description>
    </item>
    <item>
      <title>Met Office Blended Probabilistic Forecast – UK Spot Probabilities</title>
      <link>https://registry.opendata.aws/met-office-bpf-uk-spot-probabilities</link>
      <guid>https://registry.opendata.aws/met-office-bpf-uk-spot-probabilities</guid>
      <description>This product provides probabilistic weather forecasts for 7,213 sites (or spots) across the United Kingdom, Ireland and parts of Western Europe. It is produced by the Met Office IMPROVER Blended Probabilistic Forecast system. It is available in NetCDF format.
&lt;br&gt;&lt;br&gt;Blended Probabilistic Forecast data is derived from the Met Office&amp;#39;s operational NWP (Numerical Weather Prediction) ensembles and nowcasts. To give more reliable predictions, these are then blended and calibrated using the IMPROVER pipeline, and verified using spread–skill and reliability checks. 
&lt;br&gt;&lt;br&gt;This is 1 of 8 Blended Probabilistic Forecast products published by the Met Office on the Registry of Open Data on AWS. Data is available for the Global and UK domains, as gridded and spot (site-specific), and represented as percentiles and probabilities. 
&lt;br&gt;&lt;br&gt;This info is correct as of April 2026, but some things (like the number of sites, parameters and timesteps) may change in future. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;How probabilities work&lt;/b&gt;
&lt;br&gt;
Ensemble forecasts show a range of possible weather outcomes. However, some users may find it more useful to see ensemble forecasts presented as probabilities, particularly when they&amp;#39;re interested in specific thresholds. 
&lt;br&gt;&lt;br&gt;Probabilities are generated from an ensemble forecast by counting how many members of that ensemble exceed a particular threshold value. For example, if the threshold for screen temperature is 5°C, and 9 out of 18 ensemble members show a screen temperature above 5°C, there is a 50% chance of temperatures exceeding 5°C. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;How spot data works&lt;/b&gt;
&lt;br&gt;
Spot data is derived by extracting site‑specific forecasts from post‑processed gridded forecasts. 
&lt;br&gt;&lt;br&gt;IMPROVER operates on two domains: &lt;ul&gt;
&lt;li&gt;the UK domain, which primarily covers the region around the United Kingdom, Ireland and parts of Western Europe &lt;/li&gt;
&lt;li&gt;the Global domain, which covers the whole world 
&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
Within each domain, IMPROVER post-processes most forecasts on a grid, though the resolution of this grid differs between the two domains. Site-specific forecasts are drawn from these grids at the end of the post-processing chains.&lt;br&gt;&lt;br&gt;&lt;br&gt;&lt;b&gt;UK domain sites&lt;/b&gt;
&lt;br&gt;
There are 7,213 forecast sites in the UK domain. IMPROVER calculates forecasts for these sites from UK domain gridded forecasts. These gridded forecasts are generated from a lead-time-dependent blend of up to 4 forecasting models: an extrapolation nowcast (MONOW), UKV, MOGREPS-UK, and MOGREPS-G. The blend can also involve multiple cycles of a model at different lead times. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;Parameters and timesteps&lt;/b&gt;
&lt;br&gt;
There are 61 weather parameters available including:  &lt;ul&gt;
&lt;li&gt;Cloud&lt;/li&gt;
&lt;li&gt;Temperature&lt;/li&gt;
&lt;li&gt;Pressure&lt;/li&gt;
&lt;li&gt;Humidity&lt;/li&gt;
&lt;li&gt;Visibility&lt;/li&gt;
&lt;li&gt;Precipitation rate and accumulations&lt;/li&gt;
&lt;li&gt;UV&lt;/li&gt;
&lt;li&gt;Wind&lt;br&gt;&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
For most parameters, the following timesteps are available: &lt;ul&gt;
&lt;li&gt;Every hour from 0 to 120 hours &lt;/li&gt;
&lt;li&gt;Every 3 hours from 123 to 186 hours 
&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
However, timesteps vary significantly for some parameters. Check the &lt;a href&#x3D;&quot;https://www.metoffice.gov.uk/binaries/content/assets/metofficegovuk/csv/data/blended-probabilistic-forecast-parameter-catalogue.xlsx&quot;&gt;parameter documentation&lt;/a&gt; for more details. 
&lt;br&gt;&lt;br&gt;This dataset also contains deterministic “weather symbol” parameters. These are designed to complement the percentiles information in cases where the user wants to extract a single “deterministic” forecast. The 50th percentile works well for some parameters, but others are better represented by the weather symbol. Check the &lt;a href&#x3D;&quot;https://www.metoffice.gov.uk/binaries/content/assets/metofficegovuk/csv/data/blended-probabilistic-forecast-parameter-catalogue.xlsx&quot;&gt;parameter documentation&lt;/a&gt; for guidance on where this applies. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;Latency&lt;/b&gt;
&lt;br&gt;
Data is made available shortly after the model blend time. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;Archive length&lt;/b&gt;
&lt;br&gt;
Data is available for the past 30 days. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;Business needs&lt;/b&gt;&lt;br&gt;&lt;br&gt;
This product supports risk-based decision-making by providing uncertainty ranges rather than single deterministic values. Typical uses include: &lt;ul&gt;
&lt;li&gt;assessing uncertainty for operational planning&lt;/li&gt;
&lt;li&gt;evaluating weather-related risk thresholds&lt;/li&gt;
&lt;li&gt;deriving deterministic products (e.g. 50th percentile) from probabilistic outputs 
&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
Spot forecasts provide information about weather diagnostics at single sites. By using a time series of these forecasts, you can determine how a weather diagnostic is expected to evolve at a particular location. This is ideal for users if you are not moving spatially and are instead interested in how conditions are evolving at your location. This is the kind of time-series information you see in the Met Office app when you look at a forecast for your home address.
&lt;br&gt;&lt;br&gt;Gridded forecasts show how a diagnostic varies spatially across a domain at a given time. By using a time series of gridded fields, you can determine how a weather diagnostic is expected to evolve across a geographic area. So you may find them more useful if you need to consider moving spatially. This kind of product is very familiar from television broadcast weather forecasts. Gridded Blended Probabilistic Forecasts are also available as percentiles and probabilities for both the UK and Global domains. </description>
    </item>
    <item>
      <title>Met Office Blended Probabilistic Forecast – UK gridded percentiles</title>
      <link>https://registry.opendata.aws/met-office-bpf-uk-gridded-percentiles</link>
      <guid>https://registry.opendata.aws/met-office-bpf-uk-gridded-percentiles</guid>
      <description>This product provides gridded percentile weather forecasts. The grid resolution is approximately 2km and covers the UK and parts of Western Europe. It is produced by the Met Office IMPROVER Blended Probabilistic Forecast system. It is available in NetCDF format. 
&lt;br&gt;&lt;br&gt;Blended Probabilistic Forecast data is derived from the Met Office&amp;#39;s operational NWP (Numerical Weather Prediction) ensembles and nowcasts. To give more reliable predictions, these are then blended and calibrated using the IMPROVER pipeline, and verified using spread–skill and reliability checks. 
&lt;br&gt;&lt;br&gt;This is 1 of 8 Blended Probabilistic Forecast products published by the Met Office on the Registry of Open Data on AWS. Data is available for the Global and UK domains, as gridded and spot (site-specific), and represented as percentiles and probabilities. 
&lt;br&gt;&lt;br&gt;This info is correct as of April 2026, but some things (like the number of sites, parameters and timesteps) may change in future. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;How percentiles work&lt;/b&gt; 
&lt;br&gt;
Ensemble forecasts show a range of possible weather outcomes. However, some users may find it more useful to see ensemble forecasts presented as percentiles, particularly when they want to see where each member of an ensemble sits within the full range of possible outcomes. 
&lt;br&gt;&lt;br&gt;Percentiles are generated from an ensemble forecast by first sorting all the members of that ensemble, for example from the coldest temperature to the warmest. To then identify a particular percentile forecast (e.g. the 10th percentile), we find the temperature at which 10% of the ensemble members predict colder conditions. As only 10% of the ensemble members are predicting a lower temperature than the 10th percentile forecast, this indicates that it is giving a relatively low forecast of temperature. Similarly, 90% of ensemble members would predict a lower temperature than the 90th percentile forecast, indicating that it is giving a relatively high forecast of temperature.&lt;br&gt;&lt;br&gt;&lt;br&gt;&lt;b&gt;Precipitation percentiles should be used cautiously&lt;/b&gt;
&lt;br&gt;
Precipitation percentiles are potentially useful for experts. But we don&amp;#39;t recommend that most people use them, as they are hard to interpret. 
&lt;br&gt;&lt;br&gt;Precipitation is spatially noisy (i.e. it can vary a lot over small distances), especially when it is showery. This means that the individual ensemble forecasts that the percentiles are generated from are likely to have their heaviest precipitation positioned in different places. As a result, a high percentile (e.g. 95th) will pick up the high values from all those different locations and make it appear that heavy rain could occur over a wider area than is physically plausible. In other words, the spatial extent of the precipitation when using a high percentile is not physically realistic. High percentiles can be very useful for finding out what the values at the higher end may be, but not how they are spatially organised. 
&lt;br&gt;&lt;br&gt;Likewise, the spatial extent of the precipitation will be greatly reduced for the lower percentiles. If there are differences between the ensemble forecasts about where it will rain or not, it is possible that a low percentile precipitation field may show zero precipitation everywhere. Again, that is potentially misleading because it suggests it might be dry everywhere, which is not what the individual forecasts are necessarily saying. It is better to view different percentile maps together (5th, 50th, 95th) to get a more informative impression. 
&lt;br&gt;&lt;br&gt;Even the 50th percentile can be misleading as, by definition, it will never include the highest predicted values. Nor is there any guarantee that the peaks in the 50th percentile grid will align with the peaks in the 95th percentile grid.&lt;br&gt;&lt;br&gt;&lt;br&gt;&lt;b&gt;About the grid&lt;/b&gt;
&lt;br&gt;
The grid resolution is approximately 2km and covers the UK and parts of Western Europe. 
&lt;br&gt;&lt;br&gt;Numerical weather prediction (NWP) models generate forecasts for each grid point within a geographical area of interest. Each of these gridded forecasts corresponds to a particular diagnostic (e.g. precipitation rate) at a particular time. IMPROVER then takes an ensemble of these gridded forecasts and applies post-processing techniques to enhance them and represent them probabilistically. The resulting grid of values represents probabilities of exceeding or falling below a particular threshold. 
&lt;br&gt;&lt;br&gt;&lt;table&gt;
&lt;tr&gt;&lt;th&gt;Aspect&lt;/th&gt;&lt;th&gt;Values&lt;/th&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Projection&lt;/td&gt;&lt;td&gt;Lambert Azimuthal Equal Area&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Longitude of Prime Meridian&lt;/td&gt;&lt;td&gt;0.0° W&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Reference datum&lt;/td&gt;&lt;td&gt;ETRS89 - uses the GRS80 as a reference ellipsoid.&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Nominal resolution&lt;/td&gt;&lt;td&gt;2 km&lt;/td&gt;&lt;/tr&gt; 
&lt;tr&gt;&lt;td&gt;Extreme West&lt;/td&gt;&lt;td&gt;-1158 km&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Extreme East&lt;/td&gt;&lt;td&gt;924 km&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Extreme North&lt;/td&gt;&lt;td&gt;902 km&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Extreme South&lt;/td&gt;&lt;td&gt;-1036 km&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Northwest Corner (Long, Lat)&lt;/td&gt;&lt;td&gt;-24.5099247, 61.31885886&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Northeast Corner (Long, Lat)&lt;/td&gt;&lt;td&gt;15.27976922, 61.9206868&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Southwest Corner (Long, Lat)&lt;/td&gt;&lt;td&gt;-17.11712928, 44.51715281&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Southeast Corner (Long, Lat)&lt;/td&gt;&lt;td&gt;9.21255933, 44.899873&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Semi Major Axis&lt;/td&gt;&lt;td&gt;6378.137 km&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Semi MinorAxis&lt;/td&gt;&lt;td&gt;6356.75231414036 km&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Longitude of Projection Origin&lt;/td&gt;&lt;td&gt;2.5° W&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Latitude of Projection Origin&lt;/td&gt;&lt;td&gt;54.9° N&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;False Eastings&lt;/td&gt;&lt;td&gt;0.0 km&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;False Northings&lt;/td&gt;&lt;td&gt;0.0 km&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;East-West points&lt;/td&gt;&lt;td&gt;1042&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;North-South points&lt;/td&gt;&lt;td&gt;970&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Grid type&lt;/td&gt;&lt;td&gt;Arakawa A&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;
&lt;br&gt;&lt;br&gt;

&lt;b&gt;Parameters and timesteps&lt;/b&gt;
&lt;br&gt;
There are 44 weather parameters available including:&lt;ul&gt;
&lt;li&gt;Cloud&lt;/li&gt;
&lt;li&gt;Temperature&lt;/li&gt;
&lt;li&gt;Pressure&lt;/li&gt;
&lt;li&gt;Humidity&lt;/li&gt;
&lt;li&gt;Visibility&lt;/li&gt;
&lt;li&gt;Precipitation rate and accumulations (see note above about care required with use)&lt;/li&gt;
&lt;li&gt;UV&lt;/li&gt;
&lt;li&gt;Wind&lt;br&gt;&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
For most parameters, the following timesteps are available:&lt;ul&gt;
&lt;li&gt;Every hour from 0 to 120 hours&lt;/li&gt;
&lt;li&gt;Every 3 hours from 123 to 186 hours 
&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
However, timesteps vary significantly for some parameters. Check the &lt;a href&#x3D;&quot;https://www.metoffice.gov.uk/binaries/content/assets/metofficegovuk/csv/data/blended-probabilistic-forecast-parameter-catalogue.xlsx&quot;&gt;parameter documentation&lt;/a&gt; for more details. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;Latency&lt;/b&gt; 
&lt;br&gt;
Data is made available shortly after the model blend time. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;Archive length&lt;/b&gt;
&lt;br&gt;
Data is available for the past 30 days. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;Business needs&lt;/b&gt;
&lt;br&gt;
This product supports risk-based decision-making by providing uncertainty ranges rather than single deterministic values. Typical uses include: &lt;ul&gt;
&lt;li&gt;assessing uncertainty for operational planning&lt;/li&gt;
&lt;li&gt;evaluating weather-related risk thresholds&lt;/li&gt;
&lt;li&gt;deriving deterministic products (e.g. 50th percentile) from probabilistic outputs 
&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
Gridded forecasts show how a diagnostic varies spatially across a domain at a given time. By using a time series of gridded fields, you can determine how a weather diagnostic is expected to evolve across a geographic area. 
&lt;br&gt;&lt;br&gt;If you need a forecast for a specific location, a spot forecast may suit your needs better than gridded data. Spot Blended Probabilistic Forecasts are also available as percentiles and probabilities for both the UK and Global domains.</description>
    </item>
    <item>
      <title>Met Office Blended Probabilistic Forecast – UK gridded probabilities</title>
      <link>https://registry.opendata.aws/met-office-bpf-uk-gridded-probabilities</link>
      <guid>https://registry.opendata.aws/met-office-bpf-uk-gridded-probabilities</guid>
      <description>This product provides gridded probabilistic weather forecasts. The grid resolution is approximately 2km and covers the UK and parts of Western Europe. It is produced by the Met Office IMPROVER Blended Probabilistic Forecast system. It is available in NetCDF format.
&lt;br&gt;&lt;br&gt;Blended Probabilistic Forecast data is derived from the Met Office&amp;#39;s operational NWP (Numerical Weather Prediction) ensembles and nowcasts. To give more reliable predictions, these are then blended and calibrated using the IMPROVER pipeline, and verified using spread–skill and reliability checks.
&lt;br&gt;&lt;br&gt;This is 1 of 8 Blended Probabilistic Forecast products published by the Met Office on the Registry of Open Data on AWS. Data is available for the Global and UK domains, as gridded and spot (site-specific), and represented as percentiles and probabilities. 
&lt;br&gt;&lt;br&gt;This info is correct as of April 2026, but some things (like the number of sites, parameters and timesteps) may change in future. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;How probabilities work&lt;/b&gt; 
&lt;br&gt;
Ensemble forecasts show a range of possible weather outcomes. However, some users may find it more useful to see ensemble forecasts presented as probabilities, particularly when they&amp;#39;re interested in specific thresholds.
&lt;br&gt;&lt;br&gt;Probabilities are generated from an ensemble forecast by counting how many members of that ensemble exceed a particular threshold value. For example, if the threshold for screen temperature is 5°C, and 9 out of 18 ensemble members show a screen temperature above 5°C, there is a 50% chance of temperatures exceeding 5°C.
&lt;br&gt;&lt;br&gt;&lt;b&gt;About the grid&lt;/b&gt;
&lt;br&gt;
The grid resolution is approximately 2km and covers the UK and parts of Western Europe. 
&lt;br&gt;&lt;br&gt;Numerical weather prediction (NWP) models generate forecasts for each grid point within a geographical area of interest. Each of these gridded forecasts corresponds to a particular diagnostic (e.g. precipitation rate) at a particular time. IMPROVER then takes an ensemble of these gridded forecasts and applies post-processing techniques to enhance them and represent them probabilistically. The resulting grid of values represents probabilities of exceeding or falling below a particular threshold. 
&lt;br&gt;&lt;br&gt;&lt;table&gt;
&lt;tr&gt;&lt;th&gt;Aspect&lt;/th&gt;&lt;th&gt;Values&lt;/th&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Projection&lt;/td&gt;&lt;td&gt;Lambert Azimuthal Equal Area&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Longitude of Prime Meridian&lt;/td&gt;&lt;td&gt;0.0° W&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Reference datum&lt;/td&gt;&lt;td&gt;ETRS89 - uses the GRS80 as a reference ellipsoid.&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Nominal resolution&lt;/td&gt;&lt;td&gt;2 km&lt;/td&gt;&lt;/tr&gt; 
&lt;tr&gt;&lt;td&gt;Extreme West&lt;/td&gt;&lt;td&gt;-1158 km&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Extreme East&lt;/td&gt;&lt;td&gt;924 km&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Extreme North&lt;/td&gt;&lt;td&gt;902 km&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Extreme South&lt;/td&gt;&lt;td&gt;-1036 km&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Northwest Corner (Long, Lat)&lt;/td&gt;&lt;td&gt;-24.5099247, 61.31885886&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Northeast Corner (Long, Lat)&lt;/td&gt;&lt;td&gt;15.27976922, 61.9206868&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Southwest Corner (Long, Lat)&lt;/td&gt;&lt;td&gt;-17.11712928, 44.51715281&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Southeast Corner (Long, Lat)&lt;/td&gt;&lt;td&gt;9.21255933, 44.899873&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Semi Major Axis&lt;/td&gt;&lt;td&gt;6378.137 km&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Semi MinorAxis&lt;/td&gt;&lt;td&gt;6356.75231414036 km&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Longitude of Projection Origin&lt;/td&gt;&lt;td&gt;2.5° W&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Latitude of Projection Origin&lt;/td&gt;&lt;td&gt;54.9° N&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;False Eastings&lt;/td&gt;&lt;td&gt;0.0 km&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;False Northings&lt;/td&gt;&lt;td&gt;0.0 km&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;East-West points&lt;/td&gt;&lt;td&gt;1042&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;North-South points&lt;/td&gt;&lt;td&gt;970&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td&gt;Grid type&lt;/td&gt;&lt;td&gt;Arakawa A&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;
&lt;br&gt;&lt;br&gt;

&lt;b&gt;Parameters and timesteps&lt;/b&gt;
&lt;br&gt;
There are 44 weather parameters available including:&lt;ul&gt;
&lt;li&gt;Cloud&lt;/li&gt;
&lt;li&gt;Temperature&lt;/li&gt;
&lt;li&gt;Pressure&lt;/li&gt;
&lt;li&gt;Humidity&lt;/li&gt;
&lt;li&gt;Visibility&lt;/li&gt;
&lt;li&gt;Precipitation rate and accumulations&lt;/li&gt;
&lt;li&gt;Wind&lt;br&gt;&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
For most parameters, the following timesteps are available:&lt;ul&gt;
&lt;li&gt;Every hour from 0 to 120 hours&lt;/li&gt;
&lt;li&gt;Every 3 hours from 123 to 186 hours 
&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
However, timesteps vary significantly for some parameters. Check the &lt;a href&#x3D;&quot;https://www.metoffice.gov.uk/binaries/content/assets/metofficegovuk/csv/data/blended-probabilistic-forecast-parameter-catalogue.xlsx&quot;&gt;parameter documentation&lt;/a&gt; for more details. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;Latency&lt;/b&gt; 
&lt;br&gt;
Data is made available shortly after the model blend time. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;Archive length&lt;/b&gt;
&lt;br&gt;
Data is available for the past 30 days. 
&lt;br&gt;&lt;br&gt;&lt;b&gt;Business needs&lt;/b&gt;
&lt;br&gt;
This product supports risk-based decision-making by providing uncertainty ranges rather than single deterministic values. Typical uses include: &lt;ul&gt;
&lt;li&gt;assessing uncertainty for operational planning&lt;/li&gt;
&lt;li&gt;evaluating weather-related risk thresholds&lt;/li&gt;
&lt;li&gt;deriving deterministic products (e.g. 50th percentile) from probabilistic outputs 
&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
Gridded forecasts show how a diagnostic varies spatially across a domain at a given time. By using a time series of gridded fields, you can determine how a weather diagnostic is expected to evolve across a geographic area. 
&lt;br&gt;&lt;br&gt;If you need a forecast for a specific location, a spot forecast may suit your needs better than gridded data. Spot Blended Probabilistic Forecasts are also available as percentiles and probabilities for both the UK and Global domains.</description>
    </item>
    <item>
      <title>Met Office Global Ensemble Prediction System (MOGREPS-G) on a 30-day rolling archive</title>
      <link>https://registry.opendata.aws/met-office-global-ensemble</link>
      <guid>https://registry.opendata.aws/met-office-global-ensemble</guid>
      <description>THIS DATASET IS CHANGING&lt;br&gt;&lt;br&gt;Files uploaded from late January 2026 onward will contain changes including:&lt;ul&gt;
&lt;li&gt;precision changes&lt;/li&gt;
&lt;li&gt;new parameters&lt;/li&gt;
&lt;li&gt;changes to existing parameters e.g. adding vertical levels and timesteps&lt;/li&gt;
&lt;li&gt;the height_asl_on_pressure_levels parameter will be replaced by geopotential_height_on_pressure_levels&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
Please check your systems are prepared for these changes.&lt;br&gt;&lt;br&gt;A numerical weather prediction model that produces forecasts for the whole globe up to a week ahead. The projection used is the Equirectangular Latitude-Longitude and the grid resolution is 20km. The data is available as NetCDF files. It&amp;#39;s offered on a free, unsupported basis, so we don’t recommend using it for any critical business purposes.&lt;br&gt;&lt;br&gt;Met Office Global Ensemble Prediction System (MOGREPS-G) is a global configuration of the Unified Model, which is the Met Office&amp;#39;s flagship Numerical Weather Prediction model.&lt;br&gt;&lt;br&gt;The archive contains 30 days of data. The data is typically available approximately 10-11 hours after the model run time.&lt;br&gt;&lt;br&gt;The following timesteps are available:&lt;ul&gt;
&lt;li&gt;Every hour from 0 to 54 hours or from 0 to 132 hours (depending on the parameter)&lt;/li&gt;
&lt;li&gt;Every 3 hours between 57 to 198 hours or from 135 to 198 hours (depending on the parameter) for data prior to late January 2026. Data produced after this run out to 246 hours.&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>Met Office Global and Regional Ensemble Prediction System - UK (MOGREPS-UK) on a 30-day rolling archive</title>
      <link>https://registry.opendata.aws/met-office-uk-ensemble</link>
      <guid>https://registry.opendata.aws/met-office-uk-ensemble</guid>
      <description>THIS DATASET IS CHANGING&lt;br&gt;&lt;br&gt;Files uploaded from late January 2026 onward will contain changes including:&lt;ul&gt;
&lt;li&gt;precision changes&lt;/li&gt;
&lt;li&gt;new parameters&lt;/li&gt;
&lt;li&gt;changes to existing parameters e.g. adding vertical levels and timesteps&lt;/li&gt;
&lt;li&gt;the height_asl_on_pressure_levels parameter will be replaced by geopotential_height_on_pressure_levels&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
Please check your systems are prepared for these changes.&lt;br&gt;&lt;br&gt;A numerical weather prediction model that produces forecasts for the UK for the next 5 days. Parameters including temperature, pressure, wind, humidity, etc. are forecast at grid points separated by about 2.2 km, and the model has multiple vertical levels. The data is available as NetCDF files. It&amp;#39;s offered on a free, unsupported basis, so we don’t recommend using it for any critical business purposes.&lt;br&gt;&lt;br&gt;Met Office Global and Regional Ensemble Prediction System - UK (MOGREPS-UK) is a UK configuration of the Unified Model, which is the Met Office&amp;#39;s flagship Numerical Weather Prediction model.&lt;br&gt;&lt;br&gt;The archive contains 30 days of data. The data is typically available approximately 10-11 hours after the model run time.&lt;br&gt;&lt;br&gt;For most parameters, timesteps are provided every hour from 0 to 126 hours</description>
    </item>
    <item>
      <title>Molecular Profiling to Predict Response to Treatment (phs001965)</title>
      <link>https://registry.opendata.aws/mp2prt</link>
      <guid>https://registry.opendata.aws/mp2prt</guid>
      <description>The Molecular Profiling to Predict Response to Treatment (MP2PRT) program is part of the NCI&amp;#39;s Cancer Moonshot Initiative. The aim of this program is the retrospective characterization and analysis of biospecimens collected from completed NCI-sponsored trials of the National Clinical Trials Network and the NCI Community Oncology Research Program. This study, titled &amp;quot;Identification of Genetic Changes Associated with Relapse and/or Adaptive Resistance in Patients Registered as Favorable Histology Wilms Tumor on AREN03B2&amp;quot;, performs genomic characterization (WGS 30X, Total RNAseq, miRNAseq) on a discovery set of 70 trio cases (normal tissue, tumor tissue at time of diagnosis, tumor tissue at time of relapse) from patients who relapsed with Favorable Histology Wilms Tumor. Prioritized findings from the discovery set will be validated using Targeted Sequencing in an independent validation set of 47 relapse samples. The MP2PRT study is made available on AWS via the NIH STRIDES Initiative (&lt;a href&#x3D;&quot;https://aws.amazon.com/blogs/publicsector/aws-and-national-institutes-of-health-collaborate-to-accelerate-discoveries-with-strides-initiative/&quot;&gt;https://aws.amazon.com/blogs/publicsector/aws-and-national-institutes-of-health-collaborate-to-accelerate-discoveries-with-strides-initiative/&lt;/a&gt;).</description>
    </item>
    <item>
      <title>Mouse Brain Anatomy: MouseLight Imagery</title>
      <link>https://registry.opendata.aws/janelia-mouselight</link>
      <guid>https://registry.opendata.aws/janelia-mouselight</guid>
      <description>This data set, made available by Janelia&amp;#39;s MouseLight project, consists of 
images and neuron annotations of the Mus musculus brain, stored in formats suitable
for viewing and annotation using the HortaCloud cloud-based annotation system.</description>
    </item>
    <item>
      <title>NA-CORDEX - North American component of the Coordinated Regional Downscaling Experiment</title>
      <link>https://registry.opendata.aws/ncar-na-cordex</link>
      <guid>https://registry.opendata.aws/ncar-na-cordex</guid>
      <description>The NA-CORDEX dataset contains regional climate change scenario data and guidance for North America, for use in impacts, decision-making, and climate science. The NA-CORDEX data archive contains output from regional climate models (RCMs) run over a domain covering most of North America using boundary conditions from global climate model (GCM) simulations in the CMIP5 archive. These simulations run from 1950–2100 with a spatial resolution of 0.22°/25km or 0.44°/50km.  This AWS S3 version of the data includes selected variables converted to Zarr format from the original NetCDF. Only daily data are currently available; all daily data were mapped to the Gregorian calendar. Sub-daily data may be added later. Both raw and bias-corrected data are available. Further details about this version of the dataset are available at the documentation link below.</description>
    </item>
    <item>
      <title>NAIP on AWS</title>
      <link>https://registry.opendata.aws/naip</link>
      <guid>https://registry.opendata.aws/naip</guid>
      <description>The National Agriculture Imagery Program (NAIP) acquires aerial imagery during the agricultural growing seasons in the continental U.S. This &amp;quot;leaf-on&amp;quot; imagery andtypically ranges from 30 centimeters to 100 centimeters in resolution and is available from the naip-analytic Amazon S3 bucket as 4-band (RGB + NIR) imagery in MRF format, on naip-source Amazon S3 bucket as 4-band (RGB + NIR) in uncompressed Raw GeoTiff format and naip-visualization as 3-band (RGB) Cloud Optimized GeoTiff format. More details on &lt;a href&#x3D;&quot;https://naip-usdaonline.hub.arcgis.com/&quot;&gt;NAIP&lt;/a&gt;</description>
    </item>
    <item>
      <title>NASA / USGS Controlled Europa DTMs</title>
      <link>https://registry.opendata.aws/nasa-usgs-europa-dtms</link>
      <guid>https://registry.opendata.aws/nasa-usgs-europa-dtms</guid>
      <description>Knowledge of a planetary surface’s topography is necessary to understand its geology and enable landed mission operations. The Solid State Imager (SSI) on board NASA’s Galileo spacecraft acquired more than 700 images of Jupiter’s moon Europa. Although moderate- and high-resolution coverage is extremely limited, repeat coverage of a small number of sites enables the creation of digital terrain models (DTMs) via stereophotogrammetry. Here we provide stereo-derived DTMs of five sites on Europa. The sites are the bright band Agenor Linea, the crater Cilix, the crater Pwyll, pits and chaos adjacent to Rhadamanthys Linea, and ridged plains near Yelland Linea. We generated the DTMs using BAE’s SOCET SET® software and each was manually edited to correct identifiable errors from the automated stereo matching process. Additionally, we used the recently updated image pointing information provided by the U.S. Geological Survey (Bland, et al., 2021), which ties the DTMs to an existing horizontal datum and enables the DTMs to easily be used in coordination with that globally controlled image set. The DTMs are of the highest quality achievable with Galileo data and are therefore suitable for most scientific analysis. However, there are inherent uncertainties in the DTMs including horizontal resolutions that are typically 1–2 km (~10x the image pixel scale) and expected vertical precision (the root mean square (RMS) uncertainty in a point elevation) of 10s–100s of m. The DTMs and their uncertainties are discussed in detail in the documentation.</description>
    </item>
    <item>
      <title>NASA / USGS Controlled THEMIS Mosaics</title>
      <link>https://registry.opendata.aws/nasa-usgs-themis-mosaics</link>
      <guid>https://registry.opendata.aws/nasa-usgs-themis-mosaics</guid>
      <description>These data are infrared image mosaics, tiled to the Mars quadrangle, generated using Thermal Emission Imaging System (THEMIS) images from the 2001 Mars Odyssey orbiter mission. The mosaic is generated at the full resolution of the THEMIS infrared dataset, which is approximately 100 meters/pixel. The mosaic was absolutely photogrammetrically controlled to an improved Viking MDIM network that was develop by the USGS Astrogeology processing group using the Integrated Software for Imagers and Spectrometers. Image-to-image alignment precision is subpixel (i.e., &amp;lt;100m). These 8-bit, qualitative data are released as losslessly compressed Cloud Optimized GeoTiffs (COGs). Data are released using simple cylindrical (planetocentric positive East, center longitude 0, -180 to 180 longitude domain).</description>
    </item>
    <item>
      <title>NASA / USGS Europa Controlled Observation Mosaics</title>
      <link>https://registry.opendata.aws/nasa-usgs-europa-mosaics</link>
      <guid>https://registry.opendata.aws/nasa-usgs-europa-mosaics</guid>
      <description>The Solid State Imager (SSI) on NASA&amp;#39;s Galileo spacecraft acquired more than 500 images of Jupiter&amp;#39;s moon, Europa. These images vary from relatively low-resolution hemispherical imaging, to high-resolution targeted images that cover a small portion of the surface. Here we provide a set of 92 image mosaics generated from minimally processed, projected Galileo images with photogrammetrically improved locations on Europa&amp;#39;s surface.&lt;br/&gt;&lt;br/&gt;
These images provide users with nearly the entire Galileo Europa imaging dataset at its native resolution and with improved relative image locations. The Solid State Imager on NASA&amp;#39;s Galileo spacecraft provided the only moderate- to high-resolution images of Jupiter&amp;#39;s moon, Europa. Unfortunately, uncertainty in the position and pointing of the spacecraft, as well as the position and orientation of Europa, when the images were acquired resulted in significant errors in image locations on the surface. The result of these errors is that images acquired during different Galileo orbits, or even at different times during the same orbit, are significantly misaligned (errors of up to 100 km on the surface). &lt;br/&gt;&lt;br/&gt;
The dataset provides a set of individual images that can be used for scientific analysis and mission planning activities.</description>
    </item>
    <item>
      <title>NASA / USGS Europa Controlled Observations</title>
      <link>https://registry.opendata.aws/nasa-usgs-europa-observations</link>
      <guid>https://registry.opendata.aws/nasa-usgs-europa-observations</guid>
      <description>The Solid State Imager (SSI) on NASA&amp;#39;s Galileo spacecraft acquired more than 500 images of Jupiter&amp;#39;s moon, Europa. These images vary from relatively low-resolution hemispherical imaging, to high-resolution targeted images that cover a small portion of the surface. Here we provide a set of 481 minimally processed, projected Galileo images with photogrammetrically improved locations on Europa&amp;#39;s surface. These individual images were subsequently used as input into a set of 92 observation mosaics. &lt;br/&gt;&lt;br/&gt;
These images provide users with nearly the entire Galileo Europa imaging dataset at its native resolution and with improved relative image locations. The Solid State Imager on NASA&amp;#39;s Galileo spacecraft provided the only moderate- to high-resolution images of Jupiter&amp;#39;s moon, Europa. Unfortunately, uncertainty in the position and pointing of the spacecraft, as well as the position and orientation of Europa, when the images were acquired resulted in significant errors in image locations on the surface. The result of these errors is that images acquired during different Galileo orbits, or even at different times during the same orbit, are significantly misaligned (errors of up to 100 km on the surface). &lt;br/&gt;&lt;br/&gt;
The dataset provides a set of individual images that can be used for scientific analysis and mission planning activities.</description>
    </item>
    <item>
      <title>NASA / USGS Mars Reconnaissance Orbiter (MRO) Context Camera (CTX) Targeted DTMs</title>
      <link>https://registry.opendata.aws/nasa-usgs-controlled-mro-ctx-dtms</link>
      <guid>https://registry.opendata.aws/nasa-usgs-controlled-mro-ctx-dtms</guid>
      <description>As of March, 2023 the Mars Reconnaissance Orbiter (MRO) High Resolution Science Experiment (HiRISE) sensor has collected more than 5000 targeted stereopairs. During HiRISE acquisition, the Context Camera (CTX) also collects lower resolution, higher spatial extent context images. These CTX acquisitions are also targeted stereopairs. This data set contains targeted CTX DTMs and orthoimages, created using the NASA Ames Stereopipeline. These data have been created using relatively controlled CTX images that have been globally bundle adjusted using the USGS Integrated System for Imagers and Spectrometers (ISIS) jigsaw application. Relative control at global scale reduces common issues such as spacecraft jitter in the resulting DTMs. DTMs were aligned as part of 26 different groupings to the ultimate MOLA product using an iterative pc_align approach. Therefore, all DTMs and orthoimages are absolutely controlled to MOLA, a proxy product for the Mars geodetic coordinate reference frame.</description>
    </item>
    <item>
      <title>NASA / USGS Released HiRISE Digital Terrain Models</title>
      <link>https://registry.opendata.aws/nasa-usgs-mars-hirise-dtms</link>
      <guid>https://registry.opendata.aws/nasa-usgs-mars-hirise-dtms</guid>
      <description>These data are digital terrain models (DTMs) created by multiple different institutions and released to the Planetary Data System (PDS) by the University of Arizona. The data are processed from the Planetary Data System (PDS) stored JP2 files, map projected, and converted to Cloud Optimized GeoTiffs (COGs) for efficient remote data access. These data are controlled to the Mars Orbiter Laser Altimeter (MOLA). Therefore, they are a proxy for the geodetic coordinate reference frame. These data are not guaranteed to co-register with an uncontrolled products (e.g., the uncontrolled High Resolution Science Imaging Experiment (HiRISE) Reduced Data Record (RDR) data). Data are released using simple cylindrical (planetocentric positive East, center longitude 0, -180 - 180 longitude domain) or a pole centered polar stereographic projection. Data are projected to the appropriate IAU Well-known Text v2 (WKT2) represented projection.</description>
    </item>
    <item>
      <title>NASA / USGS Uncontrolled HiRISE RDRs</title>
      <link>https://registry.opendata.aws/nasa-usgs-mars-hirise</link>
      <guid>https://registry.opendata.aws/nasa-usgs-mars-hirise</guid>
      <description>These data are red and color Reduced Data Record (RDR) observations collected and originally processed by the High Resolution Imaging Science Experiment (HiRISE) team. The mdata are processed from the Planetary Data System (PDS) stored RDRs, map projected, and converted to Cloud Optimized GeoTiffs (COGs) for efficient remote data access. These data are not photogrammetrically controlled and use a priori NAIF SPICE pointing. Therefore, these data will not co-register with controlled data products. Data are released using simple cylindrical (planetocentric positive East, center longitude 0, -180 - 180 longitude domain) or a pole centered polar stereographic projection. Data are projected to the appropriate IAU Well-known Text v2 (WKT2) represented projection.</description>
    </item>
    <item>
      <title>NOAA Global Forecast System (GFS)</title>
      <link>https://registry.opendata.aws/noaa-gfs-bdp-pds</link>
      <guid>https://registry.opendata.aws/noaa-gfs-bdp-pds</guid>
      <description>NOTE - Upgrade NCEP Global Forecast System to v16.3.0 - Effective November 29, 2022 See notification &lt;a href&#x3D;&quot;https://www.weather.gov/media/notification/pdf2/scn22-104_gfs.v16.3.0.pdf&quot;&gt;HERE&lt;/a&gt;
&lt;br/&gt;
&lt;br/&gt;
The Global Forecast System (GFS) is a weather forecast model produced
by the National Centers for Environmental Prediction (NCEP). Dozens of
atmospheric and land-soil variables are available through this dataset,
from temperatures, winds, and precipitation to soil moisture and
atmospheric ozone concentration. The entire globe is covered by the GFS
at a base horizontal resolution of 18 miles (28 kilometers) between grid
points, which is used by the operational forecasters who predict weather
out to 16 days in the future. Horizontal resolution drops to 44 miles
(70 kilometers) between grid point for forecasts between one week and two
weeks.
&lt;br/&gt;
&lt;br/&gt;
The NOAA Global Forecast Systems (GFS) Warm Start Initial Conditions are 
produced by the National Centers for Environmental Prediction Center (NCEP) 
to run operational deterministic medium-range numerical weather predictions.&lt;br&gt;The GFS is built with the GFDL Finite-Volume Cubed-Sphere Dynamical Core (FV3) 
and the Grid-Point Statistical Interpolation (GSI) data assimilation system.&lt;br&gt;Please visit the links below in the Documentation section to find more details 
about the model and the data assimilation systems.   The current operational 
GFS is run at 64 layers in the vertical extending from the surface to the upper
stratosphere and on six cubic-sphere tiles at  the C768 or 13-km horizontal
resolution.  A new version of the GFS that has 127 layers extending to the
mesopause will be implemented for operation on February 3, 2021.   These initial
conditions are made available four times per day for running forecasts at the
00Z, 06Z, 12Z and 18Z cycles, respectively.   For each cycle, the dataset
contains the first guess of the atmosphere states found in the directory
./gdas.yyyymmdd/hh-6/RESTART, which are  6-hour GDAS forecast from the last
cycle,  and atmospheric analysis increments and surface analysis for the current
cycle  found in the directory ./gfs.yyyymmdd/hh, which are produced by the data
assimilation systems. </description>
    </item>
    <item>
      <title>NOAA Global Historical Climatology Network Daily (GHCN-D)</title>
      <link>https://registry.opendata.aws/noaa-ghcn</link>
      <guid>https://registry.opendata.aws/noaa-ghcn</guid>
      <description>&lt;br /&gt; UPDATE TO GHCN PREFIXES - The NODD team is working on improving performance and access to the GHCNd data and will be implementing an updated prefix structure. For more information on the prefix changes, please see the &amp;quot;&lt;a href&#x3D;&quot;https://github.com/NOAA-Big-Data-Program/bdp-data-docs/tree/main/GHCN-D&quot;&gt;READ ME on the NODD Github&lt;/a&gt;&amp;quot;. If you have questions, comments, or feedback, please reach out to &lt;a href&#x3D;&quot;mailto:&amp;#110;&amp;#111;&amp;#100;&amp;#x64;&amp;#x40;&amp;#110;&amp;#111;&amp;#x61;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#110;&amp;#111;&amp;#100;&amp;#x64;&amp;#x40;&amp;#110;&amp;#111;&amp;#x61;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt; with GHCN in the subject line. &lt;br /&gt; &lt;br &gt;
Global Historical Climatology Network - Daily is a dataset from NOAA that contains daily observations over global land areas. It contains station-based measurements from land-based stations worldwide, about two thirds of which are for precipitation measurement only. Other meteorological elements include, but are not limited to, daily maximum and minimum temperature, temperature at the time of observation, snowfall and snow depth. It is a composite of climate records from numerous sources that were merged together and subjected to a common suite of quality assurance reviews.  Some data are more than 175 years old. The data is in CSV format. Each file corresponds to a year from 1763 to present and is named as such.</description>
    </item>
    <item>
      <title>NOAA High-Resolution Rapid Refresh (HRRR) Model</title>
      <link>https://registry.opendata.aws/noaa-hrrr-pds</link>
      <guid>https://registry.opendata.aws/noaa-hrrr-pds</guid>
      <description>The HRRR is a NOAA real-time 3-km resolution, hourly updated, cloud-resolving, convection-allowing atmospheric model, initialized by 3km grids with 3km radar assimilation. Radar data is assimilated in the HRRR every 15 min over a 1-h period adding further detail to that provided by the hourly data assimilation from the 13km radar-enhanced Rapid Refresh. &lt;br /&gt; &lt;br /&gt; The HRRR ZARR formatted data was originally generated by the University of Utah under a grant provided by NOAA. They are are continuing to publish ZARR versions of HRRR data. For information about data in the s3://hrrrzarr/ please contact &lt;a href&#x3D;&quot;mailto:&amp;#97;&amp;#x74;&amp;#x6d;&amp;#x6f;&amp;#x73;&amp;#45;&amp;#x6d;&amp;#101;&amp;#x73;&amp;#x6f;&amp;#119;&amp;#101;&amp;#115;&amp;#116;&amp;#x40;&amp;#x6c;&amp;#x69;&amp;#x73;&amp;#x74;&amp;#x73;&amp;#x2e;&amp;#117;&amp;#x74;&amp;#97;&amp;#x68;&amp;#46;&amp;#101;&amp;#x64;&amp;#x75;&quot;&gt;&amp;#97;&amp;#x74;&amp;#x6d;&amp;#x6f;&amp;#x73;&amp;#45;&amp;#x6d;&amp;#101;&amp;#x73;&amp;#x6f;&amp;#119;&amp;#101;&amp;#115;&amp;#116;&amp;#x40;&amp;#x6c;&amp;#x69;&amp;#x73;&amp;#x74;&amp;#x73;&amp;#x2e;&amp;#117;&amp;#x74;&amp;#97;&amp;#x68;&amp;#46;&amp;#101;&amp;#x64;&amp;#x75;&lt;/a&gt;. </description>
    </item>
    <item>
      <title>NOAA&#x27;s Coastal Ocean Reanalysis (CORA) Dataset: 1979-2022</title>
      <link>https://registry.opendata.aws/noaa-nos-cora</link>
      <guid>https://registry.opendata.aws/noaa-nos-cora</guid>
      <description>NOAA&amp;#39;s &lt;a href&#x3D;&quot;https://tidesandcurrents.noaa.gov/cora.html&quot;&gt;Coastal Ocean Reanalysis (CORA)&lt;/a&gt; for the Gulf, East Coast/Atlantic, and Caribbean (GEC) is produced using verified hourly water levels from the National Ocean Service’s &lt;a href&#x3D;&quot;https://tidesandcurrents.noaa.gov/&quot;&gt;Center of Operational Oceanographic Products &amp;amp; Services&lt;/a&gt; (CO-OPS).  &lt;a href&#x3D;&quot;https://www.erdc.usace.army.mil/Media/Fact-Sheets/Fact-Sheet-Article-View/Article/476698/advanced-circulation-model/&quot;&gt;ADvanced CIRCulation Model (ADCIRC)&lt;/a&gt; and &lt;a href&#x3D;&quot;https://www.tudelft.nl/en/ceg/about-faculty/departments/hydraulic-engineering/sections/environmental-fluid-mechanics/research/swan&quot;&gt;Simulating WAves Nearshore (SWAN)&lt;/a&gt; models are coupled to model coastal water levels and nearshore waves. Hourly water level observations are used for data assimilation and validation to improve the accuracy of modeled water levels and wave datasets.
&lt;br&gt;&lt;br&gt;
&lt;b&gt;Additional Details:&lt;/b&gt;&lt;br&gt;
Metadata associated with model domain and time span:&lt;ul&gt;
&lt;li&gt;Timeseries - 1979 to 2022&lt;/li&gt;
&lt;li&gt;Size - Approx. 44.6 TB&lt;/li&gt;
&lt;li&gt;Domain - Lat 5.8 to 45.8 ; Long -98.0 to -53.8  &lt;/li&gt;
&lt;li&gt;Nodes - &lt;a href&#x3D;&quot;https://www.fisheries.noaa.gov/inport/item/75048&quot;&gt;CORA Metadata Library&lt;/a&gt; &lt;/li&gt;
&lt;li&gt;Grid cells - &lt;a href&#x3D;&quot;https://www.fisheries.noaa.gov/inport/item/75048&quot;&gt;CORA Metadata Library&lt;/a&gt;&lt;/li&gt;
&lt;li&gt;Spatial Resolution:&lt;ul&gt;
&lt;li&gt;Centroids: 300-400 meters &lt;/li&gt;
&lt;li&gt;Gridded: 500 meters&lt;/li&gt;
&lt;li&gt;Projection: 1983 Contiguous USA Albers projection (EPSG:5070)
&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
&lt;/li&gt;
&lt;/ul&gt;
&lt;b&gt;NOTICE: Upcoming AWS S3 Directory Restructuring:&lt;/b&gt;&lt;br&gt;
Water level and wave datasets resulting from the computation, assimilation, validation, and optimization reanalysis datasets. All products are available in NetCDF (.nc) format:&lt;ul&gt;
&lt;li&gt;Effective Date: May - September, 2026&lt;/li&gt;
&lt;li&gt;Changes: CORA datasets are being restructured within NOAA’s &lt;a href&#x3D;&quot;https://noaa-nos-cora-pds.s3.amazonaws.com/index.html&quot;&gt;S3 Directory Catalogs&lt;/a&gt; to support the addition of new domains, derived data, and product application. Before this point, datasets were stored by version to support prototyping. As production and application evolve, this change supports a more stable long-term infrastructure. &lt;/li&gt;
&lt;li&gt;CORA Datasets will be rearranged by &lt;ul&gt;
&lt;li&gt;Domain: CORA-GEC, CORA-Pac, etc. &lt;/li&gt;
&lt;li&gt;Format:  Native grid, centroid, and 500m grid, etc. &lt;/li&gt;
&lt;li&gt;Origin: Direct model output or a datasets derived from model outputs (E.g. Shoreline datasets, derived daily and monthly maximums, high tide flood predictions, etc.)&lt;/li&gt;
&lt;/ul&gt;
&lt;/li&gt;
&lt;li&gt;Impacts: The CORA_V1.1_intake.yml file will be updated for new file paths for use with GitHub Repository Notebooks, and/or hard-coded data paths should be updated to reflect new structure.
&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
&lt;b&gt;Datasets:&lt;/b&gt;&lt;br&gt;
Water level and wave datasets resulting from the computation, assimilation, validation, and optimization reanalysis datasets. All products are available in NetCDF (.nc) format:&lt;ul&gt;
&lt;li&gt;fort.63.nc - Water level elevation&lt;/li&gt;
&lt;li&gt;fort.73.nc - Atmospheric pressure at sea level&lt;/li&gt;
&lt;li&gt;fort.74.nc - Wind Velocity - 10 m elevation&lt;/li&gt;
&lt;li&gt;maxele.63.nc - Maximum water elevation&lt;/li&gt;
&lt;li&gt;swan_DIR.63.nc - Spectral mean wave direction&lt;/li&gt;
&lt;li&gt;swan_TMM10.63.nc - Spectral mean wave period&lt;/li&gt;
&lt;li&gt;swan_TPS.63.nc - Spectral  peak wave period&lt;/li&gt;
&lt;li&gt;swan_HS.63.nc - Spectral zeroth moment wave height&lt;/li&gt;
&lt;li&gt;swan_HS_max.63.nc - Maximum spectral zeroth moment wave height
&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
&lt;b&gt;Derived Products:&lt;/b&gt;&lt;br&gt;
Datasets resulting from the computation, modeling, or other processing using existing/collected data. All products are available in NetCDF (.nc) format:&lt;ul&gt;
&lt;li&gt;CORA-V1.1-fort.63: Hourly water levels &lt;/li&gt;
&lt;li&gt;CORA-V1.1-swan_DIR.63: Hourly mean wave direction &lt;/li&gt;
&lt;li&gt;CORA-V1.1-swan_TPS.63: Hourly peak wave periods &lt;/li&gt;
&lt;li&gt;CORA-V1.1-swan_HS.63: Hourly significant wave heights &lt;/li&gt;
&lt;li&gt;CORA-V1.1-Grid: Hourly water levels interpolated from model nodes to uniform 500-meter resolution grid 
&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>NREL National Solar Radiation Database</title>
      <link>https://registry.opendata.aws/nrel-pds-nsrdb</link>
      <guid>https://registry.opendata.aws/nrel-pds-nsrdb</guid>
      <description>Released to the public as part of the Department of Energy&amp;#39;s Open Energy Data Initiative,
the &lt;a href&#x3D;&quot;https://nsrdb.nrel.gov/&quot;&gt;National Solar Radiation Database (NSRDB)&lt;/a&gt; is
a serially complete collection of hourly and half-hourly values of the three
most common measurements of solar radiation – global horizontal, direct
normal, and diffuse horizontal irradiance — and meteorological data. These
data have been collected at a sufficient number of locations and temporal and
spatial scales to accurately represent regional solar radiation climates.</description>
    </item>
    <item>
      <title>OPERA Radiometric Terrain Corrected SAR Backscatter from Sentinel-1 validated product (Version 1)</title>
      <link>https://registry.opendata.aws/nasa-operal2rtc-s1v1</link>
      <guid>https://registry.opendata.aws/nasa-operal2rtc-s1v1</guid>
      <description>The Observational Products for End-Users from Remote Sensing Analysis (OPERA) Radiometric Terrain Corrected (RTC) SAR Backscatter from Sentinel-1 (S1) validated product consists of radar backscatter normalized with respect to the topography. The product maps signals related to the physical properties of ground scattering objects, such as surface roughness and soil moisture and/or vegetation. The OPERA RTC-S1 product is derived from Copernicus Sentinel-1 Interferometric Wide (IW) Single Look Complex (SLC) data with a near global scope and temporal sampling coincident with the availability of S1 SLC data. Each OPERA RTC-S1 product corresponds to a single S1 burst projected onto a pre-defined UTM/Polar stereographic map projection system map grid with a 30-meter spacing. The Copernicus global 30 m (GLO-30) Digital Elevation Model (DEM) is the reference DEM used to correct for the impacts of topography and to geocode the product.  The OPERA RTC-S1 product is normalized to the backscatter coefficient gamma-naught, ɣ0,  obtained from the original radar brightness beta-naught, β0,  through radiometric terrain correction.  The RTC-S1 product is distributed as cloud optimized GeoTIFFs with one GeoTIFF file per processed polarization. The RTC-S1 product metadata is provided in the Hierarchical Data Format version 5 (HDF5) format. The OPERA RTC-S1 product contains modified Copernicus Sentinel data (2016-2025).Due to the S1 mission’s narrow orbital tube, radar-geometry layers such as incidence angle, local incidence angle, number of looks, and RTC Area Normalization Factor (ANF) vary slightly over time for each position on the ground, and therefore are considered static. These static layers are provided separately from the OPERA RTC-S1 product, as they are produced only once or a limited number of times, to account for changes in the DEM, in the S1 orbit, or in the static-layers generation algorithm. The static layers are available in the associated OPERA Radiometric Terrain Corrected SAR Backscatter from Sentinel-1 Static Layers validated product (Version 1) dataset.
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://cumulus.asf.alaska.edu/s3credentialsREADME&quot;&gt;https://cumulus.asf.alaska.edu/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>OpenAlex dataset</title>
      <link>https://registry.opendata.aws/openalex</link>
      <guid>https://registry.opendata.aws/openalex</guid>
      <description>An open, comprehensive index of scolarly papers, citations, authors, institutions, and journals.</description>
    </item>
    <item>
      <title>OpenCell on AWS</title>
      <link>https://registry.opendata.aws/czb-opencell</link>
      <guid>https://registry.opendata.aws/czb-opencell</guid>
      <description>The OpenCell project is a proteome-scale effort to measure the localization and interactions of human proteins using high-throughput genome engineering to endogenously tag thousands of proteins in the human proteome. This dataset consists of the raw confocal fluorescence microscopy images for all tagged cell lines in the OpenCell library.These images can be interpreted both individually, to determine the localization of particular proteins of interest,  and in aggregate, by training machine learning models to classify or quantify subcellular localization patterns.</description>
    </item>
    <item>
      <title>OpenFold3 Training Data</title>
      <link>https://registry.opendata.aws/openfold3</link>
      <guid>https://registry.opendata.aws/openfold3</guid>
      <description>This dataset contains MSAs and predicted structures used to train  OpenFold3 preview, an open-source, all-atom ligand, RNA and protein structure prediction software. This includes - &lt;ul&gt;
&lt;li&gt;PDB - 245k structures and alignments from the RCSB Protein Data Bank - &lt;a href&#x3D;&quot;https://www.rcsb.org/&quot;&gt;https://www.rcsb.org/&lt;/a&gt;&lt;/li&gt;
&lt;li&gt;Long monomer distillation set - ~13 million long (sequence length &amp;gt;&#x3D; 200 amino acids) monomers from the MGNIFY database - &lt;a href&#x3D;&quot;https://www.ebi.ac.uk/metagenomics/&quot;&gt;https://www.ebi.ac.uk/metagenomics/&lt;/a&gt;.&lt;/li&gt;
&lt;li&gt;Short monomer distillation set - 400k short (sequence length &amp;lt; 200 amino acid) monomers from the MGNIFY database - &lt;a href&#x3D;&quot;https://www.ebi.ac.uk/metagenomics/&quot;&gt;https://www.ebi.ac.uk/metagenomics/&lt;/a&gt;.&lt;/li&gt;
&lt;li&gt;Disordered set - AF2-predicted structures for unresolved segments missing from the PDB&lt;/li&gt;
&lt;li&gt;RNA - OF3p2-predicted RNA monomer structures generated from a clustered version of RFAM (current version)
For the distillation sets MSAs were generated using the AF3 protocol, and were used to predict structures with AlphaFold2, more details can be found in our whitepaper - &lt;a href&#x3D;&quot;https://portal.openfold.omsf.io/reports/of3p2_technical_report.pdf&quot;&gt;https://portal.openfold.omsf.io/reports/of3p2_technical_report.pdf&lt;/a&gt;
For a full description and an interactive data explorer, please visit &lt;a href&#x3D;&quot;https://portal.openfold.omsf.io/datasets&quot;&gt;https://portal.openfold.omsf.io/datasets&lt;/a&gt;&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>Refgenie reference genome assets</title>
      <link>https://registry.opendata.aws/refgenie</link>
      <guid>https://registry.opendata.aws/refgenie</guid>
      <description>Pre-built refgenie reference genome data assets used for aligning and analyzing DNA sequence data.</description>
    </item>
    <item>
      <title>SILO climate data on AWS</title>
      <link>https://registry.opendata.aws/silo</link>
      <guid>https://registry.opendata.aws/silo</guid>
      <description>&lt;a href&#x3D;&quot;https://www.longpaddock.qld.gov.au/silo&quot;&gt;SILO&lt;/a&gt; is a database of Australian &lt;a href&#x3D;&quot;https://www.longpaddock.qld.gov.au/silo/about/climate-variables&quot;&gt;climate data&lt;/a&gt; from 1889 to the present. It provides continuous, daily time-step &lt;a href&#x3D;&quot;https://www.longpaddock.qld.gov.au/silo/about/data-products&quot;&gt;data products&lt;/a&gt; in ready-to-use &lt;a href&#x3D;&quot;https://www.longpaddock.qld.gov.au/silo/about/file-formats-and-samples&quot;&gt;formats&lt;/a&gt; for research and operational applications.
SILO&amp;#39;s gridded datasets (in NetCDF and GeoTiff formats) are hosted on AWS Public Data. Point data (at both station and grid cell locations) are available from the &lt;a href&#x3D;&quot;https://www.longpaddock.qld.gov.au/silo/&quot;&gt;SILO website&lt;/a&gt;. Incremental update files for mirroring point datasets at station locations are also available on AWS Public Data.</description>
    </item>
    <item>
      <title>Sea Surface Temperature Daily Analysis: European Space Agency Climate Change Initiative product version 2.1</title>
      <link>https://registry.opendata.aws/surftemp-sst</link>
      <guid>https://registry.opendata.aws/surftemp-sst</guid>
      <description>Global daily-mean sea surface temperatures, presented on a 0.05° latitude-longitude grid, with gaps between available daily observations filled by statistical means, spanning late 1981 to recent time.  Suitable for large-scale oceanographic meteorological and climatological applications, such as evaluating or constraining environmental models or case-studies of marine heat wave events. Includes temperature uncertainty information and auxiliary information about land-sea fraction and sea-ice coverage. For reference and citation see: &lt;a href&#x3D;&quot;http://www.nature.com/articles/s41597-019-0236-x&quot;&gt;www.nature.com/articles/s41597-019-0236-x&lt;/a&gt;.</description>
    </item>
    <item>
      <title>Sentinel-2 L2A 120m Mosaic</title>
      <link>https://registry.opendata.aws/sentinel-s2-l2a-mosaic-120</link>
      <guid>https://registry.opendata.aws/sentinel-s2-l2a-mosaic-120</guid>
      <description>Sentinel-2 L2A 120m mosaic is a derived product, which contains best pixel values for 10-daily periods, modelled by removing the cloudy pixels and then performing interpolation among remaining values. As there are some parts of the world, which have lengthy cloudy periods, clouds might be remaining in some parts. The actual modelling script is available &lt;a href&#x3D;&quot;https://sentinel-hub.github.io/custom-scripts/sentinel-2/interpolated_time_series/&quot;&gt;here&lt;/a&gt;.</description>
    </item>
    <item>
      <title>Sentinel-3</title>
      <link>https://registry.opendata.aws/sentinel-3</link>
      <guid>https://registry.opendata.aws/sentinel-3</guid>
      <description>This data set consists of observations from the Sentinel-3 satellite of the European Commission’s Copernicus Earth Observation Programme. Sentinel-3 is a polar orbiting satellite that completes 14 orbits of the Earth a day. It carries the Ocean and Land Colour Instrument (OLCI) for medium resolution marine and terrestrial optical measurements, the Sea and Land Surface Temperature Radiometer (SLSTR), the SAR Radar Altimeter (SRAL), the MicroWave Radiometer (MWR) and the Precise Orbit Determination (POD) instruments. The satellite was launched in 2016 and entered routine operational phase in 2017. Data is available from July 2017 onwards.</description>
    </item>
    <item>
      <title>Sentinel-5P Level 2</title>
      <link>https://registry.opendata.aws/sentinel5p</link>
      <guid>https://registry.opendata.aws/sentinel5p</guid>
      <description>This data set consists of observations from the Sentinel-5 Precursor (Sentinel-5P) satellite of the European Commission’s Copernicus Earth Observation Programme. Sentinel-5P is a polar orbiting satellite that completes 14 orbits of the Earth a day. It carries the TROPOspheric Monitoring Instrument (TROPOMI) which is a spectrometer that senses ultraviolet (UV), visible (VIS), near (NIR) and short wave infrared (SWIR) to monitor ozone, methane, formaldehyde, aerosol, carbon monoxide, nitrogen dioxide and sulphur dioxide in the atmosphere. The satellite was launched in October 2017 and entered routine operational phase in March 2019. Data is available from July 2018 onwards.</description>
    </item>
    <item>
      <title>SiPeCaM (Sitios Permanentes de la Calibración y Monitoreo de la Biodiversidad)</title>
      <link>https://registry.opendata.aws/sipecam</link>
      <guid>https://registry.opendata.aws/sipecam</guid>
      <description>The SiPeCaM goal is to create a data source that allows to evaluate changes in the biodiversity state, considering key aspect of how does the ecosystem behaves.</description>
    </item>
    <item>
      <title>Speedtest by Ookla Global Fixed and Mobile Network Performance Maps</title>
      <link>https://registry.opendata.aws/speedtest-global-performance</link>
      <guid>https://registry.opendata.aws/speedtest-global-performance</guid>
      <description>Global fixed broadband and mobile (cellular) network performance, allocated to zoom level 16 web mercator tiles (approximately 610.8 meters by 610.8 meters at the equator). Data is provided in both Shapefile format as well as Apache Parquet with geometries represented in Well Known Text (WKT) projected in EPSG:4326. Download speed, upload speed, and latency are collected via the Speedtest by Ookla applications for Android and iOS and averaged for each tile. Measurements are filtered to results containing GPS-quality location accuracy.</description>
    </item>
    <item>
      <title>Storm EVent ImageRy (SEVIR)</title>
      <link>https://registry.opendata.aws/sevir</link>
      <guid>https://registry.opendata.aws/sevir</guid>
      <description>Collection of spatially and temporally aligned GOES-16 ABI satellite imagery, NEXRAD radar mosaics, and GOES-16 GLM lightning detections.</description>
    </item>
    <item>
      <title>Synthea synthetic patient generator data in OMOP Common Data Model</title>
      <link>https://registry.opendata.aws/synthea-omop</link>
      <guid>https://registry.opendata.aws/synthea-omop</guid>
      <description>The Synthea generated data is provided here as a 1,000 person (1k), 100,000 person (100k), and 2,800,000 persom (2.8m) data sets in the &lt;a href&#x3D;&quot;https://www.ohdsi.org/data-standardization/&quot;&gt;OMOP Common Data Model&lt;/a&gt; format.  SyntheaTM is a synthetic patient generator that models the medical history of synthetic patients. Our mission is to output high-quality synthetic, realistic but not real, patient data and associated health records covering every aspect of healthcare. The resulting data is free from cost, privacy, and security restrictions. It can be used without restriction for a variety of secondary uses in academia, research, industry, and government (although a citation would be appreciated).
You can read our first academic paper here: &lt;a href&#x3D;&quot;https://doi.org/10.1093/jamia/ocx079&quot;&gt;https://doi.org/10.1093/jamia/ocx079&lt;/a&gt;</description>
    </item>
    <item>
      <title>The Impact of Variation on Function Consortium (IGVF)</title>
      <link>https://registry.opendata.aws/igvf-consortium</link>
      <guid>https://registry.opendata.aws/igvf-consortium</guid>
      <description>The IGVF (Impact of Genomic Variation on Function) Consortium aims to understand how genomic variation affects genome function, 
which in turn impacts phenotype. The NHGRI is funding this collaborative program that brings together teams of investigators who 
will use state-of-the-art experimental and computational approaches to model, predict, characterize and map genome function, how 
genome function shapes phenotype, and how these processes are affected by genomic variation. These joint efforts will produce a 
catalog of the impact of genomic variants on genome function and phenotypes.&lt;br&gt;The Data Corpus consists of single-cell Genomics experiments (both single modal, and multimodal, typically snRNA-seq and snATAC-seq), 
Characterization experiments using Massively Parallel Reporter Assays (MPRAs) and CRISPR-screens along with a variety of protein mutatation 
assays, and Predictive Models.
There are a huge variety of files in IGVF that are stored in the AWS OpenData Set so we recommend using the &lt;a href&#x3D;&quot;&quot;&gt;metadata file&lt;/a&gt; or browsing the &lt;a href&#x3D;&quot;https://data.igvf.org&quot;&gt;IGVF Data Portal&lt;/a&gt;</description>
    </item>
    <item>
      <title>UK Biobank Linkage Disequilibrium Matrices</title>
      <link>https://registry.opendata.aws/ukbb-ld</link>
      <guid>https://registry.opendata.aws/ukbb-ld</guid>
      <description>Linkage disequilibrium (LD) matrices of UK Biobank participants of a British ancestry, based on imputed genotypes.</description>
    </item>
    <item>
      <title>UK Biobank Pan-Ancestry Summary Statistics</title>
      <link>https://registry.opendata.aws/broad-pan-ukb</link>
      <guid>https://registry.opendata.aws/broad-pan-ukb</guid>
      <description>A multi-ancestry analysis of 7,221 phenotypes using a generalized mixed model association testing framework, spanning 16,119 genome-wide association studies. We provide standard meta-analysis across all populations and with a leave-one-population-out approach for each trait. The data are provided in tsv format (per phenotype) and Hail MatrixTable (all phenotypes and variants). Metadata is provided in phenotype and variant manifests.</description>
    </item>
    <item>
      <title>Version 2 High Resolution Canopy Height Maps by WRI and Meta</title>
      <link>https://registry.opendata.aws/dataforgood-fb-forestsv2</link>
      <guid>https://registry.opendata.aws/dataforgood-fb-forestsv2</guid>
      <description>Version 2 Global and regional Canopy Height Maps (CHMv2). Created using machine learning models on high-resolution worldwide Vantor satellite imagery. </description>
    </item>
    <item>
      <title>Yale-CMU-Berkeley (YCB) Object and Model Set</title>
      <link>https://registry.opendata.aws/ycb-benchmarks</link>
      <guid>https://registry.opendata.aws/ycb-benchmarks</guid>
      <description>This project primarily aims to facilitate performance benchmarking in robotics research. The dataset provides mesh models, RGB, RGB-D and point cloud images of over 80 objects. The physical objects are also available via the &lt;a href&#x3D;&quot;http://www.ycbbenchmarks.com/&quot;&gt;YCB benchmarking project&lt;/a&gt;. The data are collected by two state of the art systems: UC Berkley&amp;#39;s scanning rig and the Google scanner. The UC Berkley&amp;#39;s scanning rig data provide meshes generated with Poisson reconstruction, meshes generated with volumetric range image integration, textured versions of both meshes, Kinbody files for using the meshes with OpenRAVE, 600 High-resolution RGB images, 600 RGB-D images, and 600 point cloud images for each object. The Google scanner data provides 3 meshes with different resolutions (16k, 64k, and 512k polygons), textured versions of each mesh, Kinbody files for using the meshes with OpenRAVE.</description>
    </item>
    <item>
      <title>Zwicky Transient Facility (ZTF)</title>
      <link>https://registry.opendata.aws/ztf</link>
      <guid>https://registry.opendata.aws/ztf</guid>
      <description>The Zwicky Transient Facility (ZTF) is a time-domain astronomy survey that uses the Palomar 48 inch Schmidt telescope and a custom-built wide-field camera to image the night sky in three photometric filters (g, r, and i). It is a fully-automated survey aimed at a systematic exploration of optical transient phenomena. It completes a scan of the observable northern sky approximately every three nights.</description>
    </item>
    <item>
      <title>iSDAsoil</title>
      <link>https://registry.opendata.aws/isdasoil</link>
      <guid>https://registry.opendata.aws/isdasoil</guid>
      <description>iSDAsoil is a resource containing soil property predictions for the entire African continent, generated using machine learning. Maps for over 20 different soil properties have been created at 2 different depths (0-20 and 20-50cm).  Soil property predictions were made using machine learning coupled with remote sensing data and a training set of over 100,000 analyzed soil samples. Included in this dataset are images of predicted soil properties, model error and satellite covariates used in the mapping process.</description>
    </item>
    <item>
      <title>real-changesets</title>
      <link>https://registry.opendata.aws/real-changesets</link>
      <guid>https://registry.opendata.aws/real-changesets</guid>
      <description>The real-changesets is an augmented representation of OpenStreetMap changesets in JSON format. It contains the current and the previous version of each feature in a changeset.
It&amp;#39;s primary used by OSMCha, the main OpenStreetMap validation tool, to have a visualization of the changeset and provide to the user the understanding of what was changed on the map.
The real-changesets are created by combining the changeset metadata and the augmented diff generated by overpass.</description>
    </item>
    <item>
      <title>1000 Genomes</title>
      <link>https://registry.opendata.aws/1000-genomes</link>
      <guid>https://registry.opendata.aws/1000-genomes</guid>
      <description>The 1000 Genomes Project is an international collaboration which has established the most detailed catalogue of human genetic variation, including SNPs, structural variants, and their haplotype context. The final phase of the project sequenced more than 2500 individuals from 26 different populations around the world and produced an integrated set of phased haplotypes with more than 80 million variants for these individuals.</description>
    </item>
    <item>
      <title>AG-LOAM Dataset</title>
      <link>https://registry.opendata.aws/ag-loam</link>
      <guid>https://registry.opendata.aws/ag-loam</guid>
      <description>AG-LOAM dataset has been released to facilitate the evaluation of LiDAR-based odometry algorithms in agricultural environments.&lt;ol&gt;
&lt;li&gt;It was collected by a wheeled mobile robot at the Agricultural Experimental Station of the University of California, Riverside, during Winter 2022 and Winter 2023.&lt;/li&gt;
&lt;li&gt;It provides LiDAR point cloud data captured using a Velodyne VLP-16 sensor, along with ground-truth trajectories obtained from an RTK-GPS system.&lt;/li&gt;
&lt;li&gt;It consists of 18 sequences collected over three phases, covering diverse planting environments, terrain conditions, path patterns, and robot motion profiles.&lt;/li&gt;
&lt;li&gt;It spans a total operation time of 3 hours, covers a total distance of 7.5 km, and constitutes 150 GB of data.&lt;/li&gt;
&lt;/ol&gt;
</description>
    </item>
    <item>
      <title>AI3 Protein-Ligand Binding Affinity Dataset</title>
      <link>https://registry.opendata.aws/ai3</link>
      <guid>https://registry.opendata.aws/ai3</guid>
      <description>The rapid advancement of computing technologies, particularly artificial intelligence (AI), has revolutionized various domains, including drug discovery. Curated datasets are crucial for developing reliable, generalizable, and accurate models for practical applications. Generating experimental data on a large scale is an expensive and arduous process. In domains such as medical diagnostics where real-life data is hard to obtain, synthetic data has been shown to be extremely valuable. We, teams from IIIT Hyderabad, Intel, AWS, and Insilico Medicine, have performed physics-based calculations (molecular dynamics simulations) on about 20,000 protein-ligand complexes. The dataset comprises molecular dynamics snapshots, binding affinities calculated using the MM-PBSA method, and individual energy components, including electrostatic and van der Waals interactions. DatasetFileFormats essentially incorporate i. 3D coordinates of the protein-ligand complexes (pdb) in tar.gz files, and ii. CSV files containing the energy data. DatasetUsages are on i. ML scoring function for predicting binding affinities of given protein-ligand complexes, ii. Classification models for predicting correct binding poses of ligands, iii. identification of cryptic binding pockets, and iv. optimization of binding features by exploiting the individual components of the energy (experimental data has only the total binding affinity). Further, the novelty of the dataset highlights the fact that existing AI/ML training datasets lack dynamic data and are inherently biased. Further, binding affinity data existing in the literature are obtained from different experimental protocols. Therefore, this dataset has been uniquely created (from the same computational protocols) followed by free energy calculations with molecular dynamics (MD) simulations. The dynamic data-enriched protein-ligand coordinates can be used to effectively train convolutional neural network-based regression models for more accurate binding affinity prediction.</description>
    </item>
    <item>
      <title>ASF SAR Data Products for Disaster Events</title>
      <link>https://registry.opendata.aws/asf-event-data</link>
      <guid>https://registry.opendata.aws/asf-event-data</guid>
      <description>synthetic Aperture Radar (SAR) data is a powerful tool for monitoring and assessing disaster events and can provide valuable insights for researchers, scientists, and emergency response teams. 
The Alaska Satellite Facility (ASF) curates this collection of (primarily) SAR and SAR-derived satellite data products from a variety of data sources for disaster events.</description>
    </item>
    <item>
      <title>AdaptiveFlow Ligand Libraries</title>
      <link>https://registry.opendata.aws/vf-libraries</link>
      <guid>https://registry.opendata.aws/vf-libraries</guid>
      <description>AdaptiveFlow Versions of Ligand Libraries in Ready-To-Dock Format</description>
    </item>
    <item>
      <title>Allen Ivy Glioblastoma Atlas</title>
      <link>https://registry.opendata.aws/allen-ivy-glioblastoma-atlas</link>
      <guid>https://registry.opendata.aws/allen-ivy-glioblastoma-atlas</guid>
      <description>This dataset consists of images of glioblastoma human brain tumor tissue sections that have been probed for expression of particular genes believed to play a role in development of the cancer.  Each tissue section is adjacent to another section that was stained with a reagent useful for identifying histological features of the tumor.  Each of these types of images has been completely annotated for tumor features by a machine learning process trained by expert medical doctors.</description>
    </item>
    <item>
      <title>Allen Mouse Brain Atlas</title>
      <link>https://registry.opendata.aws/allen-mouse-brain-atlas</link>
      <guid>https://registry.opendata.aws/allen-mouse-brain-atlas</guid>
      <description>The Allen Mouse Brain Atlas is a genome-scale collection of cellular resolution gene expression profiles using in situ hybridization (ISH). Highly methodical data production methods and comprehensive anatomical coverage via dense, uniformly spaced sampling facilitate data consistency and comparability across &amp;gt;20,000 genes. The use of an inbred mouse strain with minimal animal-to-animal variance allows one to treat the brain essentially as a complex but highly reproducible three-dimensional tissue array. The entire Allen Mouse Brain Atlas dataset and associated tools are available through an unrestricted web-based viewing application (&lt;a href&#x3D;&quot;http://mouse.brain-map.org&quot;&gt;http://mouse.brain-map.org&lt;/a&gt;). The collection of &amp;gt; 650,000 images have been made available in this Open Data bucket to enable efficient access and analysis of the this dataset.</description>
    </item>
    <item>
      <title>Beat Acute Myeloid Leukemia (AML) 1.0</title>
      <link>https://registry.opendata.aws/beataml</link>
      <guid>https://registry.opendata.aws/beataml</guid>
      <description>Beat AML 1.0 is a collaborative research program involving 11 academic medical centers who worked
collectively to better understand  drugs and drug combinations that should be prioritized for
further development within clinical and/or molecular subsets of acute myeloid leukemia (AML)
patients. Beat AML 1.0 provides the largest-to-date dataset on primary acute myeloid leukemia
samples offering genomic, clinical, and drug response.This dataset contains open Clinical Supplement and RNA-Seq Gene Expression Quantification data.This dataset also contains controlled Whole Exome Sequencing (WXS) and RNA-Seq Aligned Reads, WXS Annotated Somatic Mutation,
WXS Raw Somatic Mutation, and RNA-Seq Splice Junction Quantification  </description>
    </item>
    <item>
      <title>Blended TROPOMI+GOSAT Satellite Data Product for Atmospheric Methane</title>
      <link>https://registry.opendata.aws/blended-tropomi-gosat-methane</link>
      <guid>https://registry.opendata.aws/blended-tropomi-gosat-methane</guid>
      <description>A dataset of satellite retrievals of atmospheric methane that extends from 30 April 2018 to present.</description>
    </item>
    <item>
      <title>BraiDyn-BC: Cued lever-pull task dataset</title>
      <link>https://registry.opendata.aws/braidyn-bc_cued-lever-pull</link>
      <guid>https://registry.opendata.aws/braidyn-bc_cued-lever-pull</guid>
      <description>The BraiDyn-BC (Brain Dynamics underlying emergence of Behavioral Change) Database offers an extensive, multimodal dataset that links
wide-field calcium imaging of the mouse neocortex to comprehensive behavioral measurements during a behavioral task.
As one of the contents in this database, we newly provide a dataset that includes 15 sessions spanning two weeks of motor skill learning, 
in which 25 mice were trained to pull a lever to obtain water rewards.
Simultaneous high-speed videography captures body, facial, and eye movements, and environmental parameters are monitored.
The dataset also features resting-state cortical activity and sensory-evoked responses, enhancing its utility for both learning-related and
sensory-driven neural dynamics studies.
Data are formatted in accordance with the Neurodata Without Borders (NWB) standard, ensuring compatibility with existing analysis tools and
adherence to the FAIR principles.
This resource enables in-depth investigations into the neural mechanisms underlying behavior and learning.
The platform encourages collaborative research, supporting the exploration of rapid within-session learning effects, long-term behavioral adaptations, and neural circuit dynamics.</description>
    </item>
    <item>
      <title>COBRA</title>
      <link>https://registry.opendata.aws/cobra</link>
      <guid>https://registry.opendata.aws/cobra</guid>
      <description>This page describes the COBRA (Classification Of Basal cell carcinoma, Risky skin cancers and Abnormalities) skin pathology dataset, which comprises over 7000 histopathology whole-slide-images related to the diagnosis of basal cell carcinoma skin cancer, the most commonly diagnosed cancer. The dataset includes biopsies and excisions and is divided into four groups. The first group contains about 2,500 BCC biopsies with subtype labels, while the second group includes 2,500 non-BCC biopsies with different types of skin dysplasia. The third group has 1,000 labelled risky cancer biopsies, including rare and dangerous types like melanoma, squamous cell carcinoma, and Merkel cell carcinoma. Finally, the fourth group contains 1,000 BCC excisions with or without free tumor margins, with 300 fully annotated. The dataset will be released over 2023 in stages, starting with the BCC and non-BCC biopsies, followed by BCC excisions, and finally the risky cancer biopsies.</description>
    </item>
    <item>
      <title>COVID-19 Harmonized Data</title>
      <link>https://registry.opendata.aws/talend-covid19</link>
      <guid>https://registry.opendata.aws/talend-covid19</guid>
      <description>A harmonized collection of the core data pertaining to COVID-19 reported cases by geography, in a format prepared for analysis</description>
    </item>
    <item>
      <title>CanElevation - LiDAR Point Clouds</title>
      <link>https://registry.opendata.aws/canelevation-pointcloud</link>
      <guid>https://registry.opendata.aws/canelevation-pointcloud</guid>
      <description>The &lt;a href&#x3D;&quot;https://open.canada.ca/data/en/dataset/7069387e-9986-4297-9f55-0288e9676947&quot;&gt;LiDAR Point Clouds&lt;/a&gt; is a product that is part of the CanElevation Series created to support the &lt;a href&#x3D;&quot;https://natural-resources.canada.ca/maps-tools-publications/satellite-elevation-air-photos/national-elevation-data-strategy&quot;&gt;National Elevation Data Strategy&lt;/a&gt; implemented by NRCan.
This product contains point clouds from various airborne LiDAR acquisition projects conducted in Canada. These airborne LiDAR acquisition projects may have been conducted by NRCan or by various partners. The LiDAR point cloud data is licensed under an &lt;a href&#x3D;&quot;https://open.canada.ca/en/open-government-licence-canada&quot;&gt;open government license&lt;/a&gt; and has been incorporated into the National Elevation Data Strategy.
Point cloud files are distributed by LiDAR acquisition project without integration between projects.
The point cloud files are distributed using the compressed .LAZ / &lt;a href&#x3D;&quot;https://copc.io/&quot;&gt;Cloud Optimized Point Cloud (COPC)&lt;/a&gt; format. The COPC open format is an octree reorganization of the data inside a .LAZ 1.4 file. It allows efficient use and visualization rendering via HTTP calls (e.g. via the web), while offering the capabilities specific to the compressed .LAZ format which is already well established in the industry. Point cloud files are therefore both downloadable for local use and viewable via URL links from a cloud computing environment.
The reference system used for all point clouds in the product is NAD83(CSRS), epoch 2010. The projection used is the UTM projection with the corresponding zone. Elevations are orthometric and expressed in reference to the Canadian Geodetic Vertical Datum of 2013 (CGVD2013).
&lt;br/&gt; &lt;br/&gt;
Le produit &lt;a href&#x3D;&quot;https://ouvert.canada.ca/data/fr/dataset/7069387e-9986-4297-9f55-0288e9676947&quot;&gt;Nuages de points lidar&lt;/a&gt; fait partie de la Série CanÉlévation créée pour appuyer la &lt;a href&#x3D;&quot;https://ressources-naturelles.canada.ca/carte-outils-publications/imagerie-satellitaire-donnees-elevation-photos-aeriennes/strategie-nationale-donnees-elevation&quot;&gt;Stratégie nationale de données d’élévation&lt;/a&gt; mise en oeuvre par Ressources naturelles Canada (RNCan).
Ce produit contient les nuages de points obtenus lors de divers projets d’acquisition par lidar aéroporté réalisés au Canada. Ces projets d’acquisition par lidar aéroporté peuvent avoir été réalisés par RNCan ou par divers partenaires. Les données de nuages de points lidar ont une licence de type &lt;a href&#x3D;&quot;https://ouvert.canada.ca/fr/licence-du-gouvernement-ouvert-canada&quot;&gt;gouvernement ouvert&lt;/a&gt; et ont été intégrés à la Stratégie nationale de données d’élévation.
Les fichiers de nuages de points sont distribués par projet d&amp;#39;acquisition et sans intégration entre les projets.
Les fichiers de nuages de points sont distribués en format compressé .LAZ / &lt;a href&#x3D;&quot;https://copc.io/&quot;&gt;Cloud Optimized Point Cloud (COPC)&lt;/a&gt;. Le format ouvert COPC est une réorganisation en octree des données à l’intérieur même d’un fichier .LAZ 1.4. Il permet une utilisation et un rendu de visualisation efficace via des appels HTTP (ex : via le web), tout en offrant les capacités propres au format .LAZ compressé qui est déjà bien établi dans l’industrie. Les fichiers de nuages de points sont donc autant téléchargeables pour une utilisation locale que visualisables via des liens URL provenant d’un environnement infonuagique.
Le système de référence utilisé pour tous les nuages de points du produit est le NAD83(SCRS), époque 2010. La projection utilisée est la projection UTM avec le fuseau correspondant. Les élévations sont orthométriques et exprimées par rapport au Système canadien de référence altimétrique de 2013 (CGVD2013).</description>
    </item>
    <item>
      <title>Canopy Tree Height Map for the Amazon Forest (mean height composite 2020-2024) by CTrees.org</title>
      <link>https://registry.opendata.aws/ctrees-amazon-canopy-height</link>
      <guid>https://registry.opendata.aws/ctrees-amazon-canopy-height</guid>
      <description>Mean canopy Tree Height for the Amazon Forest on the period 2020-2024 at 4.78 m of spatial resolution. Created using a deep learning model on high-resolution Planet imagery from the Norway&amp;#39;s International Climate and Forest Initiative (NICFI) Satellite Data Program. From the original research paper &lt;a href&#x3D;&quot;https://doi.org/10.48550/arXiv.2501.10600&quot;&gt;https://doi.org/10.48550/arXiv.2501.10600&lt;/a&gt;</description>
    </item>
    <item>
      <title>Cell Organelle Segmentation in Electron Microscopy (COSEM) on AWS</title>
      <link>https://registry.opendata.aws/janelia-cosem</link>
      <guid>https://registry.opendata.aws/janelia-cosem</guid>
      <description>High resolution images of subcellular structures.</description>
    </item>
    <item>
      <title>CitrusFarm Dataset</title>
      <link>https://registry.opendata.aws/citrus-farm</link>
      <guid>https://registry.opendata.aws/citrus-farm</guid>
      <description>CitrusFarm is a multimodal agricultural robotics dataset that provides both multispectral images and navigational sensor data for localization, mapping and crop monitoring tasks. &lt;ol&gt;
&lt;li&gt;It was collected by a wheeled mobile robot in the Agricultural Experimental Station at the University of California Riverside in the summer of 2023. &lt;/li&gt;
&lt;li&gt;It offers a total of nine sensing modalities, including stereo RGB, depth, monochrome, near-infrared and thermal images, as well as wheel odometry, LiDAR, IMU and GPS-RTK data. &lt;/li&gt;
&lt;li&gt;It comprises seven sequences collected from three citrus tree fields, featuring various tree species at different growth stages, distinctive planting patterns, as well as varying daylight conditions. &lt;/li&gt;
&lt;li&gt;It spans a total operation time of 1.7 hours, covers a total distance of 7.5 km, and constitutes 1.3 TB of data.&lt;/li&gt;
&lt;/ol&gt;
</description>
    </item>
    <item>
      <title>Clinical Trial Sequencing Project - Diffuse Large B-Cell Lymphoma</title>
      <link>https://registry.opendata.aws/ctsp-dlbcl</link>
      <guid>https://registry.opendata.aws/ctsp-dlbcl</guid>
      <description>The goal of the project is to identify recurrent genetic alterations (mutations, deletions,
amplifications, rearrangements) and/or gene expression signatures. National Cancer Institute (NCI)
utilized whole genome sequencing and/or whole exome sequencing in conjunction with transcriptome
sequencing. The samples were processed and submitted for genomic characterization using pipelines
and procedures established within The Cancer Genome Analysis (TCGA) project.</description>
    </item>
    <item>
      <title>DeepDrug Protein Embeddings Bank (DPEB)</title>
      <link>https://registry.opendata.aws/deepdrug-dpeb</link>
      <guid>https://registry.opendata.aws/deepdrug-dpeb</guid>
      <description>DPEB is a multimodal database of human protein embeddings integrating four biologically complementary representations—AlphaFold2, BioEmbeddings, ESM-2, and ProtVec—designed for enhanced protein-protein interaction prediction and functional classification.</description>
    </item>
    <item>
      <title>Department of Energy’s Geothermal Data Repository (GDR) Data Lake</title>
      <link>https://registry.opendata.aws/gdr-data-lake</link>
      <guid>https://registry.opendata.aws/gdr-data-lake</guid>
      <description>Data released from projects funded by the Department of Energy&amp;#39;s Geothermal 
Technologies Office (DOE GTO) that are too large or complex to be conveniently 
accessed by traditional means. The GDR data lake aims to improve and automate 
access of high-value geothermal data sets, making data actionable and discoverable 
by researchers and industry to accelerate analysis and advance innovation. 
This data lake is a sister-data lake to the Department of Energy’s Open Energy Data 
Initiative (OEDI) Data Lake.</description>
    </item>
    <item>
      <title>EURO-CORDEX - European component of the Coordinated Regional Downscaling Experiment</title>
      <link>https://registry.opendata.aws/euro-cordex</link>
      <guid>https://registry.opendata.aws/euro-cordex</guid>
      <description>The EURO-CORDEX dataset contains regional climate model data for Europe, for use in impacts, decision-making, and climate science. 
Currently, the bucket contains monthly datasets of 2m air temperature downscaled from CMIP5 global model datasets using different
regional climate models.</description>
    </item>
    <item>
      <title>Exceptional Responders Initiative</title>
      <link>https://registry.opendata.aws/exceptional-responders</link>
      <guid>https://registry.opendata.aws/exceptional-responders</guid>
      <description>The Exceptional Responders Initiative is a pilot study to investigate the underlying molecular factors driving exceptional treatment responses of cancer patients to drug therapies. Study researchers will examine molecular profiles of tumors from patients either enrolled in a clinical trial for an investigational drug(s) and who achieved an exceptional response relative to other trial participants, or who achieved an exceptional response to a non-investigational chemotherapy. An exceptional response is defined as achievement of either a complete response or a partial response for at least 6 months duration in a trial or treatment where the overall response rate is &amp;lt; 10%. The hope is to discover underlying molecular features that can be further investigated and may eventually predict benefit from a given drug or class of drugs for a particular patient.
This pilot project will successfully characterize approximately 100 cases of tumor tissue and, when available, case-matched germline DNA. All samples will undergo whole exome sequencing, and cases with sufficient nucleic acids will undergo additional analyses (e.g. whole genome sequencing, mRNA-sequencing, mi RNA sequencing, promoter methylation analysis, SNP etc). Each case will be annotated with demographic and clinical information, along with follow-up information minimally sufficient to correlate molecular profiles with response. Both retrospective and prospective collections will be considered. The project will also accept sequencing data and clinical data from patients who have had sequencing performed outside of this project. All data will be de-identified and placed in a controlled access database so other investigators may use them for additional insights.
Clinically annotated tissue specimens meeting the criteria will be provided by groups participating in the Exceptional Cases Initiative to a Biospecimen Core Resource (BCR), which will perform quality control on the tissues, and will use a standard operating procedure to isolate nucleic acids. The nucleic acids will be shipped to a sequencing center to perform whole exome sequencing and analysis. These findings will be made available to the broader cancer research community in a controlled access database.</description>
    </item>
    <item>
      <title>Finnish Meteorological Institute Weather Radar Data</title>
      <link>https://registry.opendata.aws/fmi-radar</link>
      <guid>https://registry.opendata.aws/fmi-radar</guid>
      <description>The up-to-date weather radar from the FMI radar network is available as Open Data. The data contain both single radar data along with composites over Finland in GeoTIFF and HDF5-formats. Available composite parameters consist of radar reflectivity (DBZ), rainfall intensity (RR), and precipitation accumulation of 1, 12, and 24 hours. Single radar parameters consist of radar reflectivity (DBZ), radial velocity (VRAD), rain classification (HCLASS), and Cloud top height (ETOP 20). Raw volume data from singe radars are also provided in HDF5 format with ODIM 2.3 conventions. Radar data becomes available as soon as it&amp;#39;s received from the radar and pre-processed into deliverable formats. Typically the most recent radar data was collected less than 5 minutes ago.</description>
    </item>
    <item>
      <title>Foundation Medicine Adult Cancer Clinical Dataset (FM-AD)</title>
      <link>https://registry.opendata.aws/fm-ad</link>
      <guid>https://registry.opendata.aws/fm-ad</guid>
      <description>The Foundation Medicine Adult Cancer Clinical Dataset (FM-AD) is a study conducted by Foundation
Medicine Inc (FMI). Genomic profiling data for approximately 18,000 adult patients with a diverse
array of cancers was generated using FoundationeOne, FMI&amp;#39;s commercially available, comprehensive
genomic profiling assay. This dataset contains open Clinical and Biospecimen data.</description>
    </item>
    <item>
      <title>GHRSST Level 4 MUR Global Foundation Sea Surface Temperature Analysis (v4.1)</title>
      <link>https://registry.opendata.aws/nasa-mur-jpl-l4-glob-v41</link>
      <guid>https://registry.opendata.aws/nasa-mur-jpl-l4-glob-v41</guid>
      <description>A Group for High Resolution Sea Surface Temperature (GHRSST) Level 4 sea surface temperature analysis produced as a retrospective dataset (four day latency) and near-real-time dataset (one day latency) at the JPL Physical Oceanography DAAC using wavelets as basis functions in an optimal interpolation approach on a global 0.01 degree grid. The version 4 Multiscale Ultrahigh Resolution (MUR) L4 analysis is based upon nighttime GHRSST L2P skin and subskin SST observations from several instruments including the NASA Advanced Microwave Scanning Radiometer-EOS (AMSR-E), the JAXA Advanced Microwave Scanning Radiometer 2 on GCOM-W1, the Moderate Resolution Imaging Spectroradiometers (MODIS) on the NASA Aqua and Terra platforms, the US Navy microwave WindSat radiometer, the Advanced Very High Resolution Radiometer (AVHRR) on several NOAA satellites, and in situ SST observations from the NOAA iQuam project. The ice concentration data are from the archives at the EUMETSAT Ocean and Sea Ice Satellite Application Facility (OSI SAF) High Latitude Processing Center and are also used for an improved SST parameterization for the high-latitudes.  The dataset also contains additional variables for some granules including a SST anomaly derived from a MUR climatology and the temporal distance to the nearest IR measurement for each pixel.This dataset is funded by the NASA MEaSUREs program ( &lt;a href&#x3D;&quot;http://earthdata.nasa.gov/our-community/community-data-system-programs/measures-projects&quot;&gt;http://earthdata.nasa.gov/our-community/community-data-system-programs/measures-projects&lt;/a&gt; ), and created by a team led by Dr. Toshio M. Chin from JPL. It adheres to the GHRSST Data Processing Specification (GDS) version 2 format specifications. Use the file global metadata &amp;quot;history:&amp;quot; attribute to determine if a granule is near-realtime or retrospective.
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://archive.podaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;https://archive.podaac.earthdata.nasa.gov/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>Global Cache of Japan</title>
      <link>https://registry.opendata.aws/wis2-global-cache-jma</link>
      <guid>https://registry.opendata.aws/wis2-global-cache-jma</guid>
      <description>Global real-time Earth system data deemed by the World Meteorological Organisation (WMO) as essential for provision of services for the protection of life and property and for the well-being of all nations. Data is sourced from all WMO Member countries / territories and retained for 24-hours. JMA operate this Global Cache service curating and publishing the dataset on behalf of WMO.</description>
    </item>
    <item>
      <title>Golden Retriever Lifetime Study: Whole genome genotyping of Golden Retrievers on Axiom HD Arrays</title>
      <link>https://registry.opendata.aws/maf-genome</link>
      <guid>https://registry.opendata.aws/maf-genome</guid>
      <description>Morris Animal Foundation’s Golden Retriever Lifetime Study is a longitudinal, prospective study following 3044 golden retrievers. The Study’s purpose is to identify the nutritional, environmental, lifestyle and genetic risk factors for cancer and other diseases. The Golden Oldie’s study enrolled an additional cohort of golden retrievers that had reached the age of 12 years or older and had not yet been diagnosed with a malignant cancer. This population can be used as a control group for conditions with high mortality in younger age. This dataset contains the data for ~1.1 million genetic markers from 3224 unique individual dogs processed using Axiom Canine Genotyping Array Sets A and B. Of the 3244 individual samples, 3024 were from the Golden Retriever Lifetime Study cohort and 200 from the Golden Oldies cohort. </description>
    </item>
    <item>
      <title>Human and Mammalian Brain Atlas</title>
      <link>https://registry.opendata.aws/allen-hmba-releases</link>
      <guid>https://registry.opendata.aws/allen-hmba-releases</guid>
      <description>Human and Mammalian Brain Atlas (HMBA) is a major atlas of the BRAIN Initiative Cell Atlas Network (BICAN) that proposes to establish a comprehensive, highly granular cell atlas in complete adult human, macaque, and marmoset brains that links brain structure, function and cellular architecture. Release artifacts have been made available in this OpenData bucket to enable utilization along with their paper publications by the neuroscience community.</description>
    </item>
    <item>
      <title>I-CARE:International Cardiac Arrest REsearch consortium Electroencephalography Database</title>
      <link>https://registry.opendata.aws/bdsp-icare</link>
      <guid>https://registry.opendata.aws/bdsp-icare</guid>
      <description>The International Cardiac Arrest REsearch consortium (I-CARE) Database includes baseline clinical information and continuous electroencephalography (EEG) recordings from 1,020 comatose patients with a diagnosis of cardiac arrest who were admitted to an intensive care unit from seven academic hospitals in the U.S. and Europe. Patients were monitored with 18 bipolar EEG channels over hours to days for the diagnosis of seizures and for neurological prognostication. Long-term neurological function was determined using the Cerebral Performance Category scale.</description>
    </item>
    <item>
      <title>Imaging MIT Licensed data and models</title>
      <link>https://registry.opendata.aws/biohub-imaging-mit</link>
      <guid>https://registry.opendata.aws/biohub-imaging-mit</guid>
      <description>This dataset contains a diverse range of imaging biological data and models. The data is sourced and curated by a team of experts at Biohub and is made available as part of these datasets only when it is not publicly accessible or requires transformations to support model training.</description>
    </item>
    <item>
      <title>Indiana Statewide Digital Aerial Imagery Catalog</title>
      <link>https://registry.opendata.aws/in-imagery</link>
      <guid>https://registry.opendata.aws/in-imagery</guid>
      <description>The State of Indiana Geographic Information Office and IOT Office of Technology manage a series of digital orthophotography dating back to 2005.  Every year&amp;#39;s worth of imagery is available as Cloud Optimized GeoTIFF (COG) files, original GeoTIFF, and other compressed deliverables such as ECW and MrSID.  Additionally, each imagery year is organized into a tile grid scheme covering the entire geography of Indiana.  All years of imagery are tiled from a 5,000 ft grid or sub tiles depending upon the resolution of the imagery.  The naming of the tiles reflects the lower left coordinate from the image.</description>
    </item>
    <item>
      <title>Indiana Statewide Elevation Catalog</title>
      <link>https://registry.opendata.aws/in-elevation</link>
      <guid>https://registry.opendata.aws/in-elevation</guid>
      <description>The State of Indiana Geographic Information Office and IOT Office of Technology manage a series of digital LiDAR LAS files stored in AWS, dating back to the 2011-2013 collection and including the NRCS-funded 2016-2020 collection. These LiDAR datasets are available as uncompressed LAS files, for cloud storage and access. Each year&amp;#39;s data is organized into a tile grid scheme covering the entire geography of Indiana, ensuring easy access and efficient processing. The tiles&amp;#39; naming reflects each tile&amp;#39;s lower left coordinate, facilitating accurate data management and retrieval. The AWS storage solution ensures that these extensive datasets are readily accessible for analysis and application across various projects.</description>
    </item>
    <item>
      <title>Japanese Tokenizer Dictionaries</title>
      <link>https://registry.opendata.aws/cotonoha-dic</link>
      <guid>https://registry.opendata.aws/cotonoha-dic</guid>
      <description>Japanese Tokenizer Dictionaries for use with MeCab.</description>
    </item>
    <item>
      <title>Kraken2 NCBI RefSeq Complete V205 database on AWS</title>
      <link>https://registry.opendata.aws/kraken2-ncbi-refseq-complete-v205</link>
      <guid>https://registry.opendata.aws/kraken2-ncbi-refseq-complete-v205</guid>
      <description>Database for use with Kraken2 (taxonomic annotation of metagenomic sequencing reads) including all NCBI RefSeq genomes available in release V205</description>
    </item>
    <item>
      <title>MIMIC-III (‘Medical Information Mart for Intensive Care’)</title>
      <link>https://registry.opendata.aws/mimiciii</link>
      <guid>https://registry.opendata.aws/mimiciii</guid>
      <description>MIMIC-III (‘Medical Information Mart for Intensive Care’) is a large, 
single-center database comprising information relating to patients 
admitted to critical care units at a large tertiary care hospital. 
Data includes vital signs, medications, laboratory measurements, 
observations and notes charted by care providers, fluid balance, 
procedure codes, diagnostic codes, imaging reports, hospital length 
of stay, survival data, and more. The database supports applications 
including academic and industrial research, quality improvement initiatives, 
and higher education coursework. The MIMIC-III dataset is freely-available. 
Researchers seeking to use the database must formally request access. For details, see 
&lt;a href&#x3D;&quot;https://mimic.physionet.org/gettingstarted/access/&quot;&gt;the getting started page&lt;/a&gt;.  Once you 
have a PhysioNet account, you must enable access to the MIMIC-III dataset from your 
AWS account.  To do this, please &lt;a href&#x3D;&quot;https://physionet.org/settings/cloud/&quot;&gt;input your AWS account number&lt;/a&gt;, and 
&lt;a href&#x3D;&quot;https://physionet.org/projects/mimiciii/1.4/request_access/2&quot;&gt;request access to the MIMIC-III Clinical Database on AWS&lt;/a&gt;.</description>
    </item>
    <item>
      <title>Medical Segmentation Decathlon</title>
      <link>https://registry.opendata.aws/msd</link>
      <guid>https://registry.opendata.aws/msd</guid>
      <description>With recent advances in machine learning, semantic segmentation algorithms are becoming increasingly general purpose and translatable to unseen tasks. Many key algorithmic advances in the field of medical imaging are commonly validated on a small number of tasks, limiting our understanding of the generalisability of the proposed contributions. A model which works out-of-the-box on many tasks, in the spirit of AutoML, would have a tremendous impact on healthcare. The field of medical imaging is also missing a fully open source and comprehensive benchmark for general purpose algorithmic validation and testing covering a large span of challenges, such as: small data, unbalanced labels, large-ranging object scales, multi-class labels, and multimodal imaging, etc. This challenge and dataset aims to provide such resource through the open sourcing of large medical imaging datasets on several highly different tasks, and by standardising the analysis and validation process.</description>
    </item>
    <item>
      <title>Met Office Global Deterministic 10km on a 2-year rolling archive</title>
      <link>https://registry.opendata.aws/met-office-global-deterministic</link>
      <guid>https://registry.opendata.aws/met-office-global-deterministic</guid>
      <description>THIS DATASET IS CHANGING&lt;br&gt;&lt;br&gt;Files uploaded from late January 2026 onward will contain changes including:&lt;ul&gt;
&lt;li&gt;precision changes&lt;/li&gt;
&lt;li&gt;new parameters&lt;/li&gt;
&lt;li&gt;changes to existing parameters e.g. adding vertical levels and timesteps&lt;/li&gt;
&lt;li&gt;the height_asl_on_pressure_levels parameter will be replaced by geopotential_height_on_pressure_levels&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
Please check your systems are prepared for these changes.&lt;br&gt;&lt;br&gt;A numerical weather prediction forecast for the whole globe, with a resolution of approximately 0.09 degrees i.e. 10km (2,560 x 1,920 grid points). The data is available as NetCDF files. It&amp;#39;s offered on a free, unsupported basis, so we don&amp;#39;t recommend using it for any critical business purposes.&lt;br&gt;&lt;br&gt;The global deterministic model is a global configuration of the Unified Model, which is the Met Office’s flagship Numerical Weather Prediction model. The model’s initial state is kept close to the real atmosphere using hybrid 4D-Var data assimilation.&lt;br&gt;&lt;br&gt;The archive contains data from the past two years. The data is typically available approximately 3 to 6 hours after the model run time.&lt;br&gt;&lt;br&gt;The following timesteps are available for most parameters:&lt;ul&gt;
&lt;li&gt;every hour from 0 to 54 hours&lt;/li&gt;
&lt;li&gt;every 3 hours from 57 to 144 hours&lt;/li&gt;
&lt;li&gt;every 6 hours from 150 to 168 hours&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>Met Office Global Ocean model on a 2-year rolling archive</title>
      <link>https://registry.opendata.aws/met-office-global-ocean</link>
      <guid>https://registry.opendata.aws/met-office-global-ocean</guid>
      <description>The Global Ocean component of the Met Office Global Coupled Atmosphere-Land-Ocean-Ice system which has been running in operations since May 2022. The system provides a global physical analysis and coupled forecast products providing 3D daily mean fields of temperature and salinity, zonal and meridional velocities; 2D daily mean fields of sea surface height, bottom temperature, mixed layer depth, sea ice fraction, sea ice thickness and sea ice zonal and meridional velocities; and instantaneous hourly fields for sea surface height, sea surface temperature and surface currents. The Met Office Global Coupled Atmosphere-Land-Ocean-Ice system is comprised of both deterministic and ensemble forecasting systems both of which are coupled to an interactive ocean. Ocean and ice analysis and forecast products are currently generated from the deterministic system once a day with forecast with lead time out to 7 days, interpolated onto a regular latitude-longitude grid products by our Global Marine Post Processing (MaPP-GL) system.</description>
    </item>
    <item>
      <title>Met Office Global Wave model on a 2-year rolling archive</title>
      <link>https://registry.opendata.aws/met-office-global-wave</link>
      <guid>https://registry.opendata.aws/met-office-global-wave</guid>
      <description>The Met Office runs global wave forecast models to support marine safety and operational decision making. Met Office configurations are developed to be run using the community wave model WAVEWATCH IIITM. The global wave configuration is designed to generate accurate forecasts for open waters of the world’s oceans and larger seas. The Met Office wave models are forced using wind data from the Met Office Global Atmospheric Hi-Res Model. The global wave model is run to provide a five day outlook for wave characteristics defining height, period and direction of waves within a given sea-state. The model uses a refined grid system in order to better represent fetch in constrained sea areas and blocking effects of islands and headlands. Please note this is a public beta and therefore a non-operational service.</description>
    </item>
    <item>
      <title>Met Office NWS Ocean model on a 2-year rolling archive</title>
      <link>https://registry.opendata.aws/met-office-nws-ocean</link>
      <guid>https://registry.opendata.aws/met-office-nws-ocean</guid>
      <description>The Northwest European continental shelf physical ocean model predicts temperature, salinity and circulation for waters surrounding the UK. 
Ocean physics analysis provides a 6-day forecast for the North-West European Atlantic shelf at 1.5km resolution:&lt;br/&gt;&lt;ul&gt;
&lt;li&gt;33 depth levels&lt;br/&gt;&lt;/li&gt;
&lt;li&gt;Currents&lt;br/&gt;&lt;/li&gt;
&lt;li&gt;Salinity&lt;br/&gt;&lt;/li&gt;
&lt;li&gt;Temperature&lt;br/&gt;&lt;/li&gt;
&lt;li&gt;Mixing Layer Thickness&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>Met Office NWS Wave model on a 2-year rolling archive</title>
      <link>https://registry.opendata.aws/met-office-nws-wave</link>
      <guid>https://registry.opendata.aws/met-office-nws-wave</guid>
      <description>Northwest European continental shelf regional wave model predicting sea-state and various sea and swell wave characteristics for waters surrounding the UK.The Met Office runs global and regional wave forecast models to support marine safety and operational decision making.
Met Office configurations are developed to be run using the community wave model WAVEWATCH IIITM.
The global wave configuration is designed to generate accurate forecasts for open waters of the world&amp;#39;s oceans and larger seas,
whilst regional configurations are run in order to improve accuracy closer to the coast.
The Met Office wave models are forced using wind data from the Met Office Global Atmospheric Hi-Res Model and, where
appropriate in regional configurations, currents from the Met Office shelf seas model.Met Office NWS Wave (UK wave) Model 6 day forecast to provide an outlook for wave characteristics defining height, period and direction of waves within a given sea-state.
The model uses a refined grid system in order to better represent fetch in constrained sea areas and blocking effects of
islands and headlands. Data are released at the model&amp;#39;s base resolution of 0.030303 degrees longitude by 0.0135135 degrees latitude
approximating to a 1.5km grid with a daily update cycle    at 00, 06, 12, 18z</description>
    </item>
    <item>
      <title>Met Office UK Deterministic (UKV)2km on a 2-year rolling archive</title>
      <link>https://registry.opendata.aws/met-office-uk-deterministic</link>
      <guid>https://registry.opendata.aws/met-office-uk-deterministic</guid>
      <description>THIS DATASET IS CHANGING&lt;br&gt;&lt;br&gt;Files uploaded from late January 2026 onward will contain changes including:&lt;ul&gt;
&lt;li&gt;precision changes&lt;/li&gt;
&lt;li&gt;new parameters&lt;/li&gt;
&lt;li&gt;changes to existing parameters e.g. adding vertical levels and timesteps&lt;/li&gt;
&lt;li&gt;the height_asl_on_pressure_levels parameter will be replaced by geopotential_height_on_pressure_levels&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
Please check your systems are prepared for these changes.&lt;br&gt;&lt;br&gt;A high-resolution gridded weather forecast for the UK, with a resolution of 0.018 degrees, projected on to a 2km horizontal grid. The data is available as NetCDF files. It&amp;#39;s offered on a free, unsupported basis, so we don’t recommend using it for any critical business purposes.&lt;br&gt;&lt;br&gt;Based on the Met Office UKV model, which is a deterministic, numerical weather prediction model for the UK and Ireland. It is a UK configuration of the Unified Model, which is the Met Office’s flagship Numerical Weather Prediction model.&lt;br&gt;&lt;br&gt;The archive contains data from the past two years. The data is typically available approximately 3 to 6 hours after the model run time.&lt;br&gt;&lt;br&gt;The following timesteps are available:&lt;ul&gt;
&lt;li&gt;every hour from 0 to 54 hours (for most parameters)&lt;/li&gt;
&lt;li&gt;every 3 hours from 57 to 120 hours&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;/ul&gt;
For some parameters, data is available for multiple vertical height or pressure levels through the atmosphere.</description>
    </item>
    <item>
      <title>Multiview Extended Video with Activities (MEVA)</title>
      <link>https://registry.opendata.aws/mevadata</link>
      <guid>https://registry.opendata.aws/mevadata</guid>
      <description>The Multiview Extended Video with Activities (MEVA) dataset consists
video data of human activity, both scripted and unscripted,
collected with roughly 100 actors over several weeks.  The data was
collected with 29 cameras with overlapping and non-overlapping
fields of view. The current release consists of about 328 hours
(516GB, 4259 clips) of video data, as well as 4.6 hours (26GB) of
UAV data. Other data includes GPS tracks of actors, camera models,
and a site map. We have also released annotations for roughly 184 hours of
data. Further updates are planned.</description>
    </item>
    <item>
      <title>NASA Earth Exchange Global Daily Downscaled Projections (NEX-GDDP-CMIP6)</title>
      <link>https://registry.opendata.aws/nex-gddp-cmip6</link>
      <guid>https://registry.opendata.aws/nex-gddp-cmip6</guid>
      <description>The NEX-GDDP-CMIP6 dataset is comprised of global downscaled climate
scenarios derived from the General Circulation Model (GCM) runs
conducted under the Coupled Model Intercomparison Project Phase 6
(CMIP6) and across two of the four &amp;quot;Tier 1&amp;quot; greenhouse gas emissions
scenarios known as Shared Socioeconomic Pathways (SSPs). The CMIP6
GCM runs were developed in support of the Sixth Assessment Report
of the Intergovernmental Panel on Climate Change (IPCC AR6). This
dataset includes downscaled projections from ScenarioMIP model
runs for which daily scenarios were produced and distributed
through the Earth System Grid Federation. The purpose of this dataset
is to provide a set of global, high resolution, bias-corrected
climate change projections that can be used to evaluate climate
change impacts on processes that are sensitive to finer-scale climate
gradients and the effects of local topography on climate conditions.</description>
    </item>
    <item>
      <title>NASA High Energy Astrophysics Mission Data</title>
      <link>https://registry.opendata.aws/nasa-heasarc</link>
      <guid>https://registry.opendata.aws/nasa-heasarc</guid>
      <description>NASA data for high energy astrophysics (generally x-ray and gamma-ray domains) is made available here by the High Energy Astrophysics Science Archive Research Center. The HEASARC hosts the full data archives of over 30 different missions spanning 50 years. The data archive for each mission will contain a range of data types from spacecraft housekeeping and raw photon event list data up to high level science-ready products such as images, light curves (time series), and energy spectra.
&lt;br/&gt;&lt;br/&gt;
This is a relatively modest total data volume but contains significant complexity and heterogeneity among the different missions. Data provided here are stored in the Flexible Image Transport System (&lt;a href&#x3D;&quot;https://heasarc.gsfc.nasa.gov/docs/heasarc/fits.html&quot;&gt;FITS&lt;/a&gt;) format common in astronomy. Higher level products are further defined to be consistent between missions following &lt;a href&#x3D;&quot;https://heasarc.gsfc.nasa.gov/docs/heasarc/ofwg/ofwg_recomm.html&quot;&gt;data model standards&lt;/a&gt; agreed by the community and maintained by the HEASARC. Analysis of these data may require software also provided by HEASARC, the &lt;a href&#x3D;&quot;https://heasarc.gsfc.nasa.gov/docs/software/lheasoft/&quot;&gt;HEASoft package&lt;/a&gt;, consisting of tools generic to all FITS data, generic to all HEASARC-compliant data, and/or specific to individual missions as appropriate. Some missions provide standard science-ready data products, while others provide low-level data types and software to generate science-ready products from them. See the links for each mission for more information on how to use the data.
&lt;br/&gt;&lt;br/&gt;
The &lt;a href&#x3D;&quot;https://heasarc.gsfc.nasa.gov/&quot;&gt;HEASARC Website&lt;/a&gt; also has archive browsing tools where you can query for observations corresponding to temporal and spatial constraints among others. These tools will ultimately point to files located on the archive by giving a URL beginning with the path &lt;a href&#x3D;&quot;https://heasarc.gsfc.nasa.gov/FTP/&quot;&gt;https://heasarc.gsfc.nasa.gov/FTP/&lt;/a&gt;. The data that are provided in the ODR follow the same structure, so when our tools give an https access URL, a user can simply swap in s3://nasa-heasarc/ for the first part of that URL and get a cloud URI. Note also that some selections have been made to what has been copied to the ODR, while the HEASARC archive itself remains the definitive and legacy source for the complete datasets.
&lt;br/&gt;&lt;br/&gt;
The HEASARC also provides user support, both generic and mission-specific, through a set of email helpdesks available through the website&amp;#39;s &lt;a href&#x3D;&quot;https://heasarc.gsfc.nasa.gov/cgi-bin/Feedback&quot;&gt;Feedback page&lt;/a&gt;.</description>
    </item>
    <item>
      <title>NASA Legacy Archive for Microwave Background Data Analysis (LAMBDA)</title>
      <link>https://registry.opendata.aws/nasa-lambda</link>
      <guid>https://registry.opendata.aws/nasa-lambda</guid>
      <description>NASA data for cosmic microwave background (CMB) analysis is made available here by the Legacy Archive for Microwave Background Data Analysis (LAMBDA), which is a part of NASA&amp;#39;s High Energy Astrophysics Science Archive Research Center (HEASARC). LAMBDA hosts the data archives of over 30 different CMB missions spanning 30+ years. The data archive for each mission may contain a range of data types from low-level time-ordered data to high level science-ready products such as sky maps and angular power spectra. Also provided in consistent formats are a variety of full sky maps in complementary wavebands that are useful for CMB analysis, such as maps of radio synchrotron or infrared dust emission.
&lt;br/&gt;&lt;br/&gt;
Data provided here are normally stored in the generic Flexible Image Transport System (&lt;a href&#x3D;&quot;https://heasarc.gsfc.nasa.gov/docs/heasarc/fits.html&quot;&gt;FITS&lt;/a&gt;) format common in astronomy. Sky maps are generally provided in the Hierarchical Equal-Area isoLatitude Pixelization (&lt;a href&#x3D;&quot;https://healpix.sourceforge.io/&quot;&gt;HEALPix&lt;/a&gt;) scheme, though the older COsmic Background Explorer (COBE) data is stored in COBE Quadrilateralizated Spherical Cube pixelization (&lt;a href&#x3D;&quot;https://lambda.gsfc.nasa.gov/product/cobe/skymap_info_new.html&quot;&gt;CSC&lt;/a&gt;). See the links for each mission for more information on the data and how to use it. LAMBDA also provides user support, both generic and mission-specific, through a helpdesk available through the website&amp;#39;s &lt;a href&#x3D;&quot;https://lambda.gsfc.nasa.gov/contact/contact.html&quot;&gt;Feedback page&lt;/a&gt;.&amp;quot;</description>
    </item>
    <item>
      <title>NASA SOHO/LASCO2 comet challenge on AWS</title>
      <link>https://registry.opendata.aws/nasa-soho-comet-challenge-on-aws</link>
      <guid>https://registry.opendata.aws/nasa-soho-comet-challenge-on-aws</guid>
      <description>The SOHO/LASCO data set (prepared for the challenge hosted in Topcoder) provided here comes from the instrument’s C2 telescope and comprises approximately 36,000 images spread across 2,950 comet observations. The human eye is a very sensitive tool and it is the only tool currently used to reliably detect new comets in SOHO data - particularly comets that are very faint and embedded in the instrument background noise. Bright comets can be easily detected in the LASCO data by relatively simple automated algorithms, but the majority of comets observed by the instrument are extremely faint, noise-level observations. Comets in SOHO/LASCO data are dynamic and morphologically diverse objects, and thus computationally highly complex to detect and track.</description>
    </item>
    <item>
      <title>NASA Space Biology Open Science Data Repository (OSDR)</title>
      <link>https://registry.opendata.aws/nasa-osdr</link>
      <guid>https://registry.opendata.aws/nasa-osdr</guid>
      <description>NASA’s Space Biology Open Science Data Repository (OSDR) introduces a one-stop site where users can explore and contribute a variety of NASA open science biological data. This site consolidates data from the Ames Life Sciences Data Archive (ALSDA) and GeneLab and includes information about the broader NASA Open Science and Open Data initiatives, all at one centralized location. Our mission is to maximize the utilization of the valuable biological research resources and enable new discoveries.&lt;br/&gt;&lt;br/&gt;
OSDR introduces access to data generated from spaceflight and space relevant experiments that explore the biological response of terrestrial biology through the AWS Open Data Registry page. The ALSDA is the official repository of non-human science data spanning a broad range of biological levels involving data from tissues, organs, whole organisms, physiology, and behavior. GeneLab is an open science repository hosting multiple types of ‘omics including transcriptomics, metagenomics, epigenomics, proteomics, and metabolomics data. Studies comprise of data from model organisms including microbes, plants, fruit flies, rodents, as well as human cell culture, ground study, and commercial astronaut data. In addition, the data repository includes metadata searches across several external omics database.&lt;br/&gt;&lt;br/&gt;</description>
    </item>
    <item>
      <title>NEXRAD ARCO - Analysis-Ready Cloud-Optimized Weather Radar</title>
      <link>https://registry.opendata.aws/nexrad-arco</link>
      <guid>https://registry.opendata.aws/nexrad-arco</guid>
      <description>NEXRAD Level II weather radar data converted to FAIR-compliant, analysis-ready cloud-optimized (ARCO) format using Zarr v3 and Icechunk V2. Hierarchically organized by Volume Coverage Pattern (VCP) and sweep, enabling instant time-series access to polarimetric variables (DBZH, ZDR, RHOHV, PHIDP, VELOCITY) without downloading individual files. Currently includes KLOT (Chicago, IL) with continuous updates.</description>
    </item>
    <item>
      <title>NIFS Large Helical Device (LHD) Experiment</title>
      <link>https://registry.opendata.aws/nifs-lhd</link>
      <guid>https://registry.opendata.aws/nifs-lhd</guid>
      <description>The Large Helical Device (LHD), owned and operated by the National Institute for Fusion Science (NIFS), is one of the world&amp;#39;s largest plasma confinement device which employs a heliotron magnetic configuration generated by the superconducting coils. The objectives are to conduct academic research on the confinement of steady-state, high-temperature, high-density plasmas, core plasma physics, and fusion reactor engineering, which are necessary to develop future fusion reactors. All the archived data of the LHD plasma diagnostics are available since the beginning of the LHD experiment, started on 31st of March, 1998.</description>
    </item>
    <item>
      <title>NOAA - hourly position, current, and sea surface temperature from drifters</title>
      <link>https://registry.opendata.aws/noaa-oar-hourly-gdp</link>
      <guid>https://registry.opendata.aws/noaa-oar-hourly-gdp</guid>
      <description>This dataset includes &lt;em&gt;hourly&lt;/em&gt; sea surface temperature and current data collected by satellite-tracked surface drifting buoys (&amp;quot;drifters&amp;quot;) of the &lt;a href&#x3D;&quot;https://www.aoml.noaa.gov/phod/gdp&quot;&gt;NOAA Global Drifter Program&lt;/a&gt;. The &lt;a href&#x3D;&quot;https://www.aoml.noaa.gov/phod/gdp/data.php&quot;&gt;Drifter Data Assembly Center (DAC) at NOAA’s Atlantic Oceanographic and Meteorological Laboratory (AOML)&lt;/a&gt; has applied quality control procedures and processing to edit these observational data and obtain estimates at regular hourly intervals. The data include positions (latitude and longitude), sea surface temperatures (total, diurnal, and non-diurnal components) and velocities (eastward, northward) with accompanying uncertainty estimates. Metadata include identification numbers, experiment number, start location and time, end location and time, drogue loss date, death code, manufacturer, and drifter type. &lt;br /&gt; &lt;br /&gt; Please note that data from the Global Drifter Program are also available at &lt;a href&#x3D;&quot;https://doi.org/10.25921/7ntx-z961&quot;&gt;6-hourly intervals&lt;/a&gt; but derived via alternative methods. The 6-hourly dataset goes back further in time (1979) and may be more appropriate for studies of long-term, low frequency patterns of the oceanic circulation. Yet, the 6-hourly dataset does not resolve fully high-frequency processes such as tides and inertial oscillations as well as sea surface temperature diurnal variability. &lt;br /&gt; &lt;br /&gt; [CITING NOAA - hourly position, current, and sea surface temperature from drifters data. Citation for this dataset should include the following information below.] &lt;br /&gt; Elipot, Shane; Sykulski, Adam; Lumpkin, Rick; Centurioni, Luca; Pazos, Mayra (2022). Hourly location, current velocity, and temperature collected from Global Drifter Program drifters world-wide. [indicate subset used]. NOAA National Centers for Environmental Information. Dataset. &lt;a href&#x3D;&quot;https://doi.org/10.25921/x46c-3620&quot;&gt;https://doi.org/10.25921/x46c-3620&lt;/a&gt;.</description>
    </item>
    <item>
      <title>NOAA Emergency Response Imagery</title>
      <link>https://registry.opendata.aws/noaa-eri</link>
      <guid>https://registry.opendata.aws/noaa-eri</guid>
      <description>In order to support NOAA&amp;#39;s homeland security and emergency response requirements, the National Geodetic Survey Remote Sensing Division (NGS/RSD) has the capability to acquire and rapidly disseminate a variety of spatially-referenced datasets to federal, state, and local government agencies, as well as the general public. Remote sensing technologies used for these projects have included lidar, high-resolution digital cameras, a film-based RC-30 aerial camera system, and hyperspectral imagers. Examples of rapid response initiatives include acquiring high resolution images with the Emerge/Applanix Digital Sensor System (DSS).</description>
    </item>
    <item>
      <title>NOAA GFS - dynamical.org Icechunk Zarr</title>
      <link>https://registry.opendata.aws/dynamical-noaa-gfs</link>
      <guid>https://registry.opendata.aws/dynamical-noaa-gfs</guid>
      <description>&lt;p&gt;The Global Forecast System (GFS) is a National Oceanic and Atmospheric Administration (NOAA) National Centers for Environmental Prediction (NCEP) weather forecast model that generates data for dozens of atmospheric and land-soil variables, including temperatures, winds, precipitation, soil moisture, and atmospheric ozone concentration. The system couples four separate models (atmosphere, ocean model, land/soil model, and sea ice) that work together to depict weather conditions.&lt;/p&gt;
&lt;p&gt;These datasets have been translated to cloud-optimized Icechunk Zarr format by &lt;a href&#x3D;&quot;https://dynamical.org&quot;&gt;dynamical.org&lt;/a&gt;.&lt;/p&gt;
&lt;ul&gt;
  &lt;li&gt;&lt;a href&#x3D;&quot;https://dynamical.org/catalog/noaa-gfs-analysis/&quot;&gt;NOAA GFS analysis&lt;/a&gt; - Weather analysis from the Global Forecast System (GFS) operated by NOAA NWS NCEP.&lt;/li&gt;
  &lt;li&gt;&lt;a href&#x3D;&quot;https://dynamical.org/catalog/noaa-gfs-forecast/&quot;&gt;NOAA GFS forecast&lt;/a&gt; - Weather forecasts from the Global Forecast System (GFS) operated by NOAA NWS NCEP.&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>NOAA Global Ensemble Forecast System (GEFS) Re-forecast</title>
      <link>https://registry.opendata.aws/noaa-gefs-reforecast</link>
      <guid>https://registry.opendata.aws/noaa-gefs-reforecast</guid>
      <description>NOAA has generated a multi-decadal reanalysis and reforecast data set to accompany the next-generation version of its ensemble prediction system, the Global Ensemble Forecast System, version 12 (GEFSv12). Accompanying the real-time forecasts are “reforecasts” of the weather, that is, retrospective forecasts spanning the period 2000-2019. These reforecasts are not as numerous as the real-time data; they were generated only once per day, from 00 UTC initial conditions, and only 5 members were provided, with the following exception. Once weekly, an 11-member reforecast was generated, and these extend in lead time to +35 days. </description>
    </item>
    <item>
      <title>NOAA IOOS MARACOOS Regional Ocean Modeling System (ROMS) &quot;Doppio&quot; Data Assimilative Reanalysis</title>
      <link>https://registry.opendata.aws/noaa-ioos-roms-doppio</link>
      <guid>https://registry.opendata.aws/noaa-ioos-roms-doppio</guid>
      <description>This dataset, identified as Doppio Analysis Version 3 Release 3 (DopAnV3R3-ini2007) initialized January 2007, comprises outputs from a Regional Ocean Modeling System (ROMS) data assimilative reanalysis of ocean circulation in the Mid-Atlantic Bight and Gulf of Maine for 2007-2024.
&lt;br&gt;&lt;br&gt;
A multi-year reanalysis (2007-2024) of circulation in the coastal ocean and adjacent deep sea of the northeast U.S. continental shelf has been computed using the Regional Ocean Modeling System (ROMS) with four-dimensional variational (4D-Var) data assimilation (DA) of observations from satellites, land-based ocean surface current measuring radar, and all available in situ observations from the MARACOOS (maracoos.org) and NERACOOS (neracoos.org) regional associations of the U.S. Integrated Ocean Observing System (IOOS). The reanalysis downscales open boundary information from the Copernicus Marine Service global analysis. The dynamic model is forced by regional meteorological analyses, observed daily river discharges, and harmonic tides that augment the open boundary conditions. The analysis covers the period 2-Jan-2007 to 31-Dec-2024 on a 7-km horizontal grid with 40 vertical terrain-following s-coordinate levels. Ocean state variables computed are sea level, velocity, temperature, and salinity. Air-sea fluxes of heat and momentum are included.
&lt;br&gt;&lt;br&gt;
The ROMS 4D-Var DA configuration and its performance in comparison to observations (both assimilated and independent) are described by Wilkin et al. (2022). The underlying ROMS ocean circulation model configuration is described by López et al (2020). Wilkin et al. (2022) also compare this analysis to Copernicus and the U.S. Navy Global Ocean Forecast System (GOFS) HYCOM model.
&lt;br&gt;&lt;br&gt;
All ROMS model outputs here are in netCDF format and the data and metadata follow CF-1.4 conventions for the description of coordinates and variables. The reanalysis results are provided on the model’s native 3-D grid in terrain-following coordinates aggregated into three collections with individual files containing 3 days of model output.
&lt;br&gt;&lt;br&gt;&lt;ul&gt;
&lt;li&gt;His: 1-hourly snapshots of the ocean state “history” (sea level and 3-D velocity, temperature and salinity) for 02-Jan-2007 01:00 through 31-Dec-2024 00:00&lt;/li&gt;
&lt;li&gt;Flx: 1-hourly snapshots of surface air-sea flux forcing (wind stress and net heat flux) from the posterior reanalysis for 02-Jan-2007 01:00 through 31-Dec-2024 00:00&lt;/li&gt;
&lt;li&gt;Avg: Daily averages for 02-Jan-2007 12:00 through 30-Dec-2024 12:00
&lt;br&gt;&lt;br&gt;
In addition to access here in the Registry of Open Data in AWS, Rutgers University operates a THREDDS (Thematic Real-time Environmental Distributed Data Services) web service at &lt;a href&#x3D;&quot;https://tds.marine.rutgers.edu/thredds/roms/doppio/catalog.html&quot;&gt;https://tds.marine.rutgers.edu/thredds/roms/doppio/catalog.html&lt;/a&gt; that supports geospatial and temporal sub-setting. Access protocols supported are OPeNDAP, WMS and netCDF subsetting. That collection includes: 
&lt;br&gt;&lt;br&gt;&lt;/li&gt;
&lt;li&gt;monthly averages for 17-Jan-2007 through 15-Dec-2021&lt;/li&gt;
&lt;li&gt;yearly averages for 2007 through 2021&lt;/li&gt;
&lt;li&gt;monthly ensemble averages
&lt;br&gt;&lt;br&gt;
The observations that were assimilated, after quality control and the formation of super-observations as described by Wilkin et al. (2022), can be accessed via an ERDDAP service at &lt;a href&#x3D;&quot;https://tds.marine.rutgers.edu/erddap/tabledap/DOPPIO_REANALYSIS_Ver3_OBS.graph&quot;&gt;https://tds.marine.rutgers.edu/erddap/tabledap/DOPPIO_REANALYSIS_Ver3_OBS.graph&lt;/a&gt;. The dataset includes observation type and provenance fields (documented in the ERDDAP metadata) that allow sub-selection by data types (temperate, salinity, velocity, etc.) or observing platform (e.g., Jason altimeter satellite, AVHRR SST, IOOS gliders, etc.). The ERDDAP catalog includes outputs of the DA system in observation space; namely, prior and posterior model errors, and the Copernicus and GOFS values interpolated to the observation position. An observation scale field flags data that were rejected by 4D-Var QC.&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>NOAA Multi-Radar/Multi-Sensor System (MRMS)</title>
      <link>https://registry.opendata.aws/noaa-mrms-pds</link>
      <guid>https://registry.opendata.aws/noaa-mrms-pds</guid>
      <description>The MRMS system was developed to produce severe weather, transportation, and precipitation products for improved decision-making capability to improve hazardous weather forecasts and warnings, along with hydrology, aviation, and numerical weather prediction.
&lt;br/&gt;
&lt;br/&gt;
MRMS is a system with fully-automated algorithms that quickly and intelligently integrate data streams from multiple radars, surface and upper air observations, lightning detection systems, satellite observations, and forecast models. Numerous two-dimensional multiple-sensor products offer assistance for hail, wind, tornado, quantitative precipitation estimations, convection, icing, and turbulence diagnosis.
&lt;br/&gt;
&lt;br/&gt;
MRMS is being used to develop and test new Federal Aviation Administration (FAA) NextGen products in addition to advancing techniques in quality control, icing detection, and turbulence in collaboration with the National Center for Atmospheric Research, the University Corporation for Atmospheric Research, and Lincoln Laboratories.
&lt;br/&gt;
&lt;br/&gt;
MRMS was deployed operationally in 2014 at the National Center for Environmental Prediction (NCEP). All of the 100+ products it produces are available via NCEP to all of the WFOs, RFCs, CWSUs and NCEP service centers. In addition, the MRMS product suite is publicly available to any other entity who wishes to access and use the data. Other federal agencies that use MRMS include FEMA, DOD, FAA, and USDA.
&lt;br/&gt;
&lt;br/&gt;&lt;br&gt;MRMS is the proposed operational version of the WDSS-II and NMQ research systems.
&lt;br/&gt;
&lt;br/&gt; 
The MRMS system was jointly developed in cooperation with the Cooperative Institute for Severe and High-Impact Weather Research and Operations (CIWRO) (formerly CIMMS), and the University of Oklahoma retains the right to commercially license the software. Several leading weather information companies have previously licensed the MRMS system from the University of Oklahoma for commercial use, although the software is available for government at no cost.
&lt;br/&gt;</description>
    </item>
    <item>
      <title>NOAA North American Multi-Model Ensemble (NMME)</title>
      <link>https://registry.opendata.aws/noaa-nmme</link>
      <guid>https://registry.opendata.aws/noaa-nmme</guid>
      <description>The North American Multi-Model Ensemble (NMME) is an experimental multi-model seasonal forecasting system consisting of coupled models from US modeling centers including NOAA/NCEP, NOAA/GFDL, NCAR, NASA, and Canada&amp;#39;s ECCC.
&lt;br&gt;&lt;br&gt;
The need for the development of NMME operational predictive capability was recommended in US National Academies report &amp;quot;Assessment of Intraseasonal to Interannual Climate Prediction and Predictability&amp;quot;.  Indeed, the national effort is required to meet the specific tailored regional prediction and decision support needs of a large community. The multi-model ensemble approach has proven extremely effective at quantifying prediction uncertainty due to uncertainty in model formulation, and has proven to produce better prediction quality (on average) than any single model ensemble. This multi-model approach is the basis for several international collaborative prediction research efforts, including an operational European system. There are numerous examples of how this multi-model ensemble approach yields superior forecasts compared to any single model.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NapierOne Mixed File Dataset</title>
      <link>https://registry.opendata.aws/napierone</link>
      <guid>https://registry.opendata.aws/napierone</guid>
      <description>NapierOne is a modern cybersecurity mixed file data set, primarily aimed at, but not limited to, ransomware detection and forensic analysis. The dataset contains over 500,000 distinct files, representing 44 distinct popular file types. It was designed to address the known deficiency in research reproducibility and improve consistency by facilitating research replication and repeatability. The data set was inspired by the Govdocs1 data set and it is intended that ‘NapierOne’ be used as a complement to this original data set. An investigation was performed with the goal of determining the common files types currently in use. No specific research was found that explicitly provided this information, so an alternative consensus approach was employed. This involved combining the findings from multiple sources of file type usage into an overall ranked list. After which 5,000 real-world example files were gathered, and a specific data subset was created, for each of the common file types identified. In some circumstances, multiple data subsets were created for a specific file type, each subset representing a specific characteristic for that file type. For example, there are multiple data subsets for the ZIP file type with each subset containing examples of a specific compression method. Ransomware execution tends to produce files that have high entropy, so examples of file types that naturally have this attribute are also present. The resulting entire data set comprises of more than 90 separate data subsets divided between 44 distinct file types, resulting in over 500,000 unique files in total. Currently, the data set contains examples of the following file types APK, BIN, BMP, CSS, CSV, DOC, DOCX, DWG, ELF, EPS,EPUB, EXE, GIF, GZIP, HTML, ICS, JS, JPG, JSON, MKV, MP3, MP4, ODS, OXPS, PDF, PNG, PPT, PPTX, PS1, RAR, SVG, TAR, TIF, TXT, WEBP, XLS, XLSX, XML, ZIP, ZLIB, 7Zip</description>
    </item>
    <item>
      <title>National Cancer Institute Imaging Data Commons (IDC) Collections</title>
      <link>https://registry.opendata.aws/nci-imaging-data-commons</link>
      <guid>https://registry.opendata.aws/nci-imaging-data-commons</guid>
      <description>&lt;a href&#x3D;&quot;https://imaging.datacommons.cancer.gov&quot;&gt;Imaging Data Commons (IDC)&lt;/a&gt;  is a repository within the 
&lt;a href&#x3D;&quot;https://datacommons.cancer.gov&quot;&gt;Cancer Research Data Commons (CRDC)&lt;/a&gt; that manages imaging data 
and enables its integration with the other components of CRDC. IDC hosts a growing number of imaging collections that are contributed 
by either funded US National Cancer Institute (NCI)  data collection 
activities, or by the individual researchers.Image data hosted by IDC is stored in DICOM  format. </description>
    </item>
    <item>
      <title>National Climate Database (NCDB)</title>
      <link>https://registry.opendata.aws/nrel-pds-ncdb</link>
      <guid>https://registry.opendata.aws/nrel-pds-ncdb</guid>
      <description>The National Climate Database (NCDB) seeks to be the definitive source of climate 
data for energy applications. The goal of the NCDB is to provide unbiased high 
temporal and spatial resolution climate data needed for renewable energy modeling. 
The NCDB seeks to maintain the inherent relationship between the various parameters 
that are needed to model solar, wind, hydrology and load and provide data for multiple 
important climate scenarios.  </description>
    </item>
    <item>
      <title>National Herbarium of NSW</title>
      <link>https://registry.opendata.aws/nsw-herbarium</link>
      <guid>https://registry.opendata.aws/nsw-herbarium</guid>
      <description>The National Herbarium of New South Wales is one of the most significant scientific, cultural and historical botanical resources in the Southern hemisphere. The 1.43 million preserved plant specimens have been captured as high-resolution images and the biodiversity metadata associated with each of the images captured in digital form. Botanical specimens date from year 1770 to today, and form voucher collections that document the distribution and diversity of the world&amp;#39;s flora through time, particularly that of NSW, Austalia and the Pacific.The data is used in biodiversity assessment, systematic botanical research, ecosystem conservation and policy development. The data is used by scientists, students and the public.</description>
    </item>
    <item>
      <title>ONT Methylation Benchmarking Datasets</title>
      <link>https://registry.opendata.aws/ont_basemod_data</link>
      <guid>https://registry.opendata.aws/ont_basemod_data</guid>
      <description>ONT Methylation Benchmarking Datasets are generated to benchmark existing methylation-calling tools on the Oxford Nanopore sequencing platform using their recent R10.4.1 flowcell chemistry. It spans a diverse range of species, including bacteria (E. coli, H. pylori J99, H. pylori 26695, A. variabilis, T. denticola), plants (Rice, Arabidopsis), and mammals (mouse, human).In addition, the dataset includes EMSeq data for E. coli, plant, and mouse samples, which can serve as ground truth for methylation studies. It also provides unmethylated whole-genome amplified (WGA) DNA for H. pylori 26695 and a dam- dcm- double mutant (DM) of E. coli that lacks canonical 5mC and 6mA methylation. These variants, together with their wild-type counterparts, offer value for both training and benchmarking DNA methylation calling models.</description>
    </item>
    <item>
      <title>OPERA Land Surface Disturbance Annual from Harmonized Landsat Sentinel-2 product (Version 1)</title>
      <link>https://registry.opendata.aws/nasa-operal3dist-ann-hlsv1</link>
      <guid>https://registry.opendata.aws/nasa-operal3dist-ann-hlsv1</guid>
      <description>The Observational Products for End-Users from Remote Sensing Analysis (&lt;a href&#x3D;&quot;https://www.jpl.nasa.gov/go/opera&quot;&gt;OPERA&lt;/a&gt;) Land Surface Disturbance Annual from Harmonized Landsat Sentinel-2 (HLS) product Version 1 summarizes the &lt;a href&#x3D;&quot;https://doi.org/10.5067/SNWG/OPERA_L3_DIST-ALERT-HLS_V1.001&quot;&gt;DIST-ALERT&lt;/a&gt; data product into an annual vegetation disturbance data product. Vegetation disturbance is mapped when there is an indicated decrease in vegetation cover within an HLS Version 2 pixel. The product also provides auxiliary generic disturbance information as determined from the variations of the reflectance through the DIST-ALERT scenes to provide information about more general disturbance trends. The DIST-ANN product tracks changes at the annual scale, aggregating changes identified in the DIST-ALERT product. Only confirmed disturbances from the associated year are reported together with the date of initial disturbance. As confirmed disturbances are determined using subsequent cloud-free observations to determine if the loss detections persist, the required number of HLS scenes depends on visibility of the target. Due to this dependency, summarizing the DIST-ALERT in the DIST-ANN product will have some latency contingent on the algorithmic calibration and is detailed in the Algorithm Theoretical Basis Document (ATBD).The OPERA_L3_DIST-ANN-HLS (or DIST-ANN) data product is provided in Cloud Optimized GeoTIFF (COG) format, and each layer is distributed as a separate COG. There are 21 layers contained within the DIST-ANN product: vegetation disturbance status, historical vegetation cover indicator, maximum vegetation cover indicator, maximum vegetation anomaly value, vegetation disturbance confidence layer, date of initial vegetation disturbance, number of detected vegetation loss anomalies, vegetation disturbance duration, date of last observation assessed for vegetation disturbance, and several generic disturbance layers. Each product layer is gridded to the same resolution and tiling system as HLS V2: 30 meter (m) and Military Grid Reference System (MGRS). See the Product Specification Document (PSD) for a more detailed description of the individual layers provided in the DIST-ANN product. The OPERA_L3_DIST-ANN-HLS product contains modified Copernicus Sentinel data (2020-2025).Known Issues&lt;ul&gt;
&lt;li&gt;Additional usage constraints are provided under Section 5 of the Algorithm Theoretical Basis Document (ATBD).
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&lt;/a&gt;&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>OPERA Radiometric Terrain Corrected SAR Backscatter from Sentinel-1 Static Layers validated product (Version 1)</title>
      <link>https://registry.opendata.aws/nasa-operal2rtc-s1-staticv1</link>
      <guid>https://registry.opendata.aws/nasa-operal2rtc-s1-staticv1</guid>
      <description>The Observational Products for End-Users from Remote Sensing Analysis (OPERA) Radiometric Terrain Corrected (RTC) SAR Backscatter from Sentinel-1 (S1) Static Layers (RTC-S1-STATIC) validated product contains static radar geometry layers associated with the OPERA Radiometric Terrain Corrected (RTC) SAR Backscatter from Sentinel-1 (S1) (RTC-S1) validated product.  Due to the S1 mission’s narrow orbital tube, radar-geometry layers such as incidence angle, local incidence angle, number of looks, and RTC Area Normalization Factor (ANF) vary slightly over time for each position on the ground, and therefore are considered static. These static layers are provided separately from the OPERA RTC-S1 product, as they are produced only once or a limited number of times, to account for changes in the DEM, in the S1 orbit, or in the static-layers generation algorithm.  Static layers are provided as single-band cloud-optimized GeoTIFF (COG) files, with map grid matching RTC-S1 products with the same burst ID.  The standard OPERA RTC-S1 product is derived from the original Copernicus Sentinel-1 (S1) interferometric wide (IW) single-look complex (SLC) data, provided by the European Space Agency, with a temporal sampling coincident with the availability of Sentinel-1A and Sentinel-1B SLC data. The OPERA RTC-S1-STATIC and RTC-S1 products are provided at a near global scope (land masses excluding Antarctica).  The RTC-S1 products are available in the associated OPERA Radiometric Terrain Corrected SAR Backscatter from Sentinel-1 validated product (Version 1) dataset.
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://cumulus.asf.alaska.edu/s3credentialsREADME&quot;&gt;https://cumulus.asf.alaska.edu/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>Open City Model (OCM)</title>
      <link>https://registry.opendata.aws/opencitymodel</link>
      <guid>https://registry.opendata.aws/opencitymodel</guid>
      <description>Open City Model is an initiative to provide cityGML data for all the buildings in the United States.
By using other open datasets in conjunction with our own code and algorithms it is our goal to provide 3D geometries for every US building.</description>
    </item>
    <item>
      <title>Open Human Genome Library</title>
      <link>https://registry.opendata.aws/openhgl</link>
      <guid>https://registry.opendata.aws/openhgl</guid>
      <description>The Open Human Genome Library (OpenHGL) is a collection of high-quality &lt;em&gt;de novo&lt;/em&gt; human assemblies that are publicly available in genomic databases (e.g. NCBI and CNCB) or from individual research papers. It provides consistent naming and uniform formats across datasets, supporting efficient subsequence retrieval and approximate string search.</description>
    </item>
    <item>
      <title>Open VLF: Scientific Open Data Initiative for CRAAM&#x27;s SAVNET and AWESOME VLF Data.</title>
      <link>https://registry.opendata.aws/craam-open-vlf</link>
      <guid>https://registry.opendata.aws/craam-open-vlf</guid>
      <description>This platform is maintained by &lt;a href&#x3D;&quot;https://www.mackenzie.br/centro-de-radio-astronomia-e-astrofisica-mackenzie&quot;&gt;CRAAM&lt;/a&gt; (Mackenzie Radio Astronomy and Astrophysics Center), a research center operated by &lt;a href&#x3D;&quot;https://www.mackenzie.br/&quot;&gt;UPM&lt;/a&gt; (Mackenzie Presbyterian University) and &lt;a href&#x3D;&quot;https://www.gov.br/inpe&quot;&gt;INPE&lt;/a&gt; (National Institute for Space Research), to provide public and free access for researchers, students, and the interested public to VLF (Very Low Frequency) data from CRAAM&amp;#39;s antenna systems. Amazon AWS supports all data stored through the &lt;a href&#x3D;&quot;https://aws.amazon.com/pt/opendata/&quot;&gt;AWS Open Data Program&lt;/a&gt;.
Very Low Frequency (VLF) signals can be used for navigation services, communication with submarines, and are a powerful tool to study the low-altitude Earth&amp;#39;s ionosphere, atmospheric and geophysics phenomena, space weather, magnetic field, and solar flares. Here, we provide historical and updated VLF data from two of CRAAM’s antenna systems, the SAVNET and AWESOME systems.
The SAVNET consists of a network of 11 VLF receiving/tracking stations located in Latin America and Antarctica. Five stations are in Brazil, three in Peru, one in Argentina, one in Mexico, and one in the Brazilian Antarctic Research Station Comandante Ferraz. The CRAAM AWESOME systems include two antennas in Brazil and Antarctica. Data since 2002 from both systems are available, with occasional gaps during periods when data collection is interrupted.
Data provided here is stored in different formats (.mat for AWESOME antenna system and .fits for SAVNET system). For documentation and details, please visit the project website &lt;a href&#x3D;&quot;https://open-vlf.web.app&quot;&gt;Open VLF&lt;/a&gt;.</description>
    </item>
    <item>
      <title>OpenProteinSet</title>
      <link>https://registry.opendata.aws/openfold</link>
      <guid>https://registry.opendata.aws/openfold</guid>
      <description>Multiple sequence alignments (MSAs) for 140,000 unique &lt;a href&#x3D;&quot;https://www.rcsb.org/&quot;&gt;Protein Data Bank&lt;/a&gt; (PDB) chains and 16,000,000 &lt;a href&#x3D;&quot;https://uniclust.mmseqs.com/&quot;&gt;UniClust30&lt;/a&gt; clusters. Template hits are also provided for the PDB chains and 270,000 UniClust30 clusters chosen for maximal diversity and MSA depth. MSAs were generated with HHBlits (-n3) and JackHMMER against MGnify, BFD, UniRef90, and UniClust30 while templates were identified from PDB70 with HHSearch, all according to procedures outlined in the supplement to the AlphaFold 2 Nature paper, &lt;a href&#x3D;&quot;https://www.nature.com/articles/s41586-021-03819-2&quot;&gt;Jumper et al. 2021&lt;/a&gt;. We expect the database to be broadly useful to structural biologists training or validating deep learning models for protein structure prediction and related tasks.</description>
    </item>
    <item>
      <title>OpenRoboCare Multi-Modal Expert Demonstration Dataset for Robot-Assisted Caregiving</title>
      <link>https://registry.opendata.aws/open-robo-care</link>
      <guid>https://registry.opendata.aws/open-robo-care</guid>
      <description>A comprehensive multimodal dataset capturing real-world caregiving routines from 21 occupational therapists performing 15 daily caregiving tasks. The dataset includes synchronized RGB-D video, tactile sensing, eye-gaze tracking, pose annotations, and action labels across 315 sessions totaling 19.8 hours of expert demonstrations. Data modalities include anonymized RGB images, depth maps, 44-sensor tactile readings, 2D/3D pose tracking, temporal action annotations, and first/third-person videos, enabling research in robot learning from demonstration, multimodal perception, and safe human-robot interaction for caregiving applications.</description>
    </item>
    <item>
      <title>PD12M</title>
      <link>https://registry.opendata.aws/pd12m</link>
      <guid>https://registry.opendata.aws/pd12m</guid>
      <description>PD12M is a collection of 12.4 million CC0/PD image-caption pairs for the purpose of training generative image models.</description>
    </item>
    <item>
      <title>Pohang Canal Dataset: A Multimodal Maritime Dataset for Autonomous Navigation in Restricted Waters</title>
      <link>https://registry.opendata.aws/pohang-canal-dataset</link>
      <guid>https://registry.opendata.aws/pohang-canal-dataset</guid>
      <description>This dataset presents a multi-modal maritime dataset acquired in restricted waters in Pohang, South Korea. The sensor suite is composed of three LiDARs (one 64-channel LiDAR and two 32-channel LiDARs), a marine radar, two visual cameras used as a stereo camera, an infrared camera, an omnidirectional camera with 6 directions, an AHRS, and a GPS with RTK. The dataset includes the sensor calibration parameters and SLAM-based baseline trajectory. It was acquired while navigating a 7.5 km route that includes a narrow canal area, inner and outer port areas, and a near-coastal area. The aim of this dataset is to facilitate research on autonomous surface vehicles.</description>
    </item>
    <item>
      <title>ProteinGym</title>
      <link>https://registry.opendata.aws/proteingym</link>
      <guid>https://registry.opendata.aws/proteingym</guid>
      <description>ProteinGym is a benchmark suite for assessing the performance of protein fitness prediction and design models. It comprises a large curated collection of 200+ high-throughput experimental assays (~3M mutated sequences), as well as clinical annotations from experts about the pathogenicity of mutants in over 3k human genes.</description>
    </item>
    <item>
      <title>QIIME 2 Tutorial Data</title>
      <link>https://registry.opendata.aws/qiime2</link>
      <guid>https://registry.opendata.aws/qiime2</guid>
      <description>QIIME 2 (pronounced “chime two”) is a microbiome multi-omics bioinformatics and data science platform that is trusted, free, open source, extensible, and community developed and supported.</description>
    </item>
    <item>
      <title>Rain over Africa</title>
      <link>https://registry.opendata.aws/roa</link>
      <guid>https://registry.opendata.aws/roa</guid>
      <description>The Rain over Africa (RoA) dataset consists of spaceborn estimates of precipitation of Rain over Africa using only geostationary imagery and obtained through a convolutional and quantile regression neural network. The dataset also contains some uncertainty estimates.</description>
    </item>
    <item>
      <title>SPaRCNet data:Seizures, Rhythmic and Periodic Patterns in ICU Electroencephalography</title>
      <link>https://registry.opendata.aws/bdsp-sparcnet</link>
      <guid>https://registry.opendata.aws/bdsp-sparcnet</guid>
      <description>The IIIC dataset includes  50,697 labeled EEG samples from 2,711 patients&amp;#39; and 6,095 EEGs that were annotated by physician experts from 18 institutions. These samples were used to train SPaRCNet (Seizures, Periodic and Rhythmic Continuum patterns Deep Neural Network), a computer program that classifies IIIC events with an accuracy matching clinical experts.</description>
    </item>
    <item>
      <title>STOIC2021 Training</title>
      <link>https://registry.opendata.aws/stoic2021-training</link>
      <guid>https://registry.opendata.aws/stoic2021-training</guid>
      <description>The STOIC project collected Computed Tomography (CT) images of 10,735 individuals suspected of being infected with SARS-COV-2 during the first wave of the pandemic in France, from March to April 2020. For each patient in the training set, the dataset contains binary labels for COVID-19 presence, based on RT-PCR test results, and COVID-19 severity, defined as intubation or death within one month from the acquisition of the CT scan. This S3 bucket contains the training sample of the STOIC dataset as used in the STOIC2021 challenge on grand-challenge.org.</description>
    </item>
    <item>
      <title>Sentinel-1</title>
      <link>https://registry.opendata.aws/sentinel-1</link>
      <guid>https://registry.opendata.aws/sentinel-1</guid>
      <description>&lt;a href&#x3D;&quot;https://sentinel.esa.int/web/sentinel/missions/sentinel-1&quot;&gt;Sentinel-1&lt;/a&gt; is a pair of European radar imaging (SAR) satellites launched in 2014 and 2016. Its 6 days revisit cycle and ability to observe through clouds makes it perfect for sea and land monitoring, emergency response due to environmental disasters, and economic applications. This dataset represents the global Sentinel-1 GRD archive, from beginning to the present, converted to &lt;a href&#x3D;&quot;https://www.cogeo.org/&quot;&gt;cloud-optimized GeoTIFF format&lt;/a&gt;.</description>
    </item>
    <item>
      <title>Sentinel-2 ACOLITE-DSF Aquatic Reflectance for the Conterminous United States</title>
      <link>https://registry.opendata.aws/usgs_aqr</link>
      <guid>https://registry.opendata.aws/usgs_aqr</guid>
      <description>Aquatic reflectance produced with the dark spectrum fitting (DSF) algorithm as implemented in the Atmospheric Correction for OLI “lite” (ACOLITE) software (version 20221114.0). Aquatic reflectance is defined here as unitless water-leaving radiance reflectance and represents the ratio of water-leaving radiance (units of watts per square meter per steradian per nanometer) to downwelling irradiance (units of watts per square meter per nanometer) multiplied by pi.</description>
    </item>
    <item>
      <title>Software Heritage Graph Dataset</title>
      <link>https://registry.opendata.aws/software-heritage</link>
      <guid>https://registry.opendata.aws/software-heritage</guid>
      <description>&lt;a href&#x3D;&quot;https://www.softwareheritage.org/&quot;&gt;Software Heritage&lt;/a&gt; is the largest
existing public archive of software source code and accompanying
development history. The Software Heritage Graph Dataset is a fully
deduplicated Merkle DAG representation of the Software Heritage archive.The dataset links together file content identifiers, source code
directories, Version Control System (VCS) commits tracking evolution over
time, up to the full states of VCS repositories as observed by Software
Heritage during periodic crawls. The dataset’s contents come from major
development forges (including GitHub and GitLab), FOSS distributions (e.g.,
Debian), and language-specific package managers (e.g., PyPI). Crawling
information is also included, providing timestamps about when and where all
archived source code artifacts have been observed in the wild.
Author and committer information is anonymized.</description>
    </item>
    <item>
      <title>Sophos/ReversingLabs 20 Million malware detection dataset</title>
      <link>https://registry.opendata.aws/sorel-20m</link>
      <guid>https://registry.opendata.aws/sorel-20m</guid>
      <description>A dataset intended to support research on machine learning
techniques for detecting malware.  It includes metadata and EMBER-v2
features for approximately 10 million benign and 10 million malicious
Portable Executable files, with disarmed but otherwise complete
files for all malware samples.  All samples are labeled using Sophos
in-house labeling methods, have features extracted using the
EMBER-v2 feature set, well as metadata obtained via the pefile
python library, detection counts obtained via ReversingLabs
telemetry, and additional behavioral tags that indicate the rough
behavior of the samples.</description>
    </item>
    <item>
      <title>State of Colorado Imagery</title>
      <link>https://registry.opendata.aws/colorado-imagery</link>
      <guid>https://registry.opendata.aws/colorado-imagery</guid>
      <description>The State of Colorado has gathered public historical imagery ranging from 2005 to 2021.</description>
    </item>
    <item>
      <title>TESS-GAIA Light Curve (TGLC)</title>
      <link>https://registry.opendata.aws/mast-tglc</link>
      <guid>https://registry.opendata.aws/mast-tglc</guid>
      <description>TESS-Gaia Light Curve (TGLC) is a PSF-based TESS full-frame image (FFI) light curve product. Using Gaia DR3 as priors, the team forward models the FFIs with the effective point spread function to remove contamination from nearby stars. The resulting light curves show a photometric precision closely tracking the pre-launch prediction of the noise level: TGLC&amp;#39;s photometric precision consistently reaches ≲2% at 16th TESS magnitude even in crowded fields, demonstrating excellent decontamination and deblending power.</description>
    </item>
    <item>
      <title>The Human Microbiome Project</title>
      <link>https://registry.opendata.aws/human-microbiome-project</link>
      <guid>https://registry.opendata.aws/human-microbiome-project</guid>
      <description>The NIH-funded Human Microbiome Project (HMP) is a collaborative effort of over 300 scientists from more than 80 organizations to comprehensively characterize the microbial communities inhabiting the human body and elucidate their role in human health and disease. To accomplish this task, microbial community samples were isolated from a cohort of 300 healthy adult human subjects at 18 specific sites within five regions of the body (oral cavity, airways, urogenital track, skin, and gut). Targeted sequencing of the 16S bacterial marker gene and/or whole metagenome shotgun sequencing was performed for thousands of these samples. In addition, whole genome sequences were generated for isolate strains collected from human body sites to act as reference organisms for analysis. Finally, 16S marker and whole metagenome sequencing was also done on additional samples from people suffering from several disease conditions.</description>
    </item>
    <item>
      <title>Transcriptomic MIT Licensed data and models</title>
      <link>https://registry.opendata.aws/biohub-transcriptomics-mit</link>
      <guid>https://registry.opendata.aws/biohub-transcriptomics-mit</guid>
      <description>This dataset contains a transcriptomics biological data and models. The models embed transcriptomic data and facilitate transcriptomic analysis. The data is sourced and curated by a team of experts at Biohub and is made available as part of these datasets only when it is not publicly accessible or requires transformations to support model training.</description>
    </item>
    <item>
      <title>UCSF Renal Mass CT Dataset</title>
      <link>https://registry.opendata.aws/ucsf-rmac</link>
      <guid>https://registry.opendata.aws/ucsf-rmac</guid>
      <description>This dataset provides a set of 831 3D Multiphase CT exams of renal masses, registered across phases with annotations identifying the masses</description>
    </item>
    <item>
      <title>Variant Effect Predictor (VEP) and the Loss-Of-Function Transcript Effect Estimator (LOFTEE) Plugin</title>
      <link>https://registry.opendata.aws/hail-vep-pipeline</link>
      <guid>https://registry.opendata.aws/hail-vep-pipeline</guid>
      <description>VEP determines the effect of genetic variants (SNPs, insertions, deletions, CNVs or structural variants) on genes, transcripts, and protein sequence, as well as regulatory regions. The European Bioinformatics Institute produces the VEP tool/db and releases updates every 1 - 6 months. The latest release contains 267 genomes from 232 species containing 5567663 protein coding genes. This dataset hosts the last 5 releases for human, rat, and zebrafish. Also, it hosts the required reference files for the Loss-Of-Function Transcript Effect Estimator (LOFTEE) plugin as it is commonly used with VEP.</description>
    </item>
    <item>
      <title>Vesuvius Challenge - CT Scans of Herculaneum Papyri</title>
      <link>https://registry.opendata.aws/vesuvius-challenge-herculaneum-scrolls</link>
      <guid>https://registry.opendata.aws/vesuvius-challenge-herculaneum-scrolls</guid>
      <description>This dataset contains reconstructed micro-CT volumes of carbonized Herculaneum papyri
produced as part of the Vesuvius Challenge. The scanned scroll library survived the
eruption of Mount Vesuvius in AD 79. It is the only intact library known to have
survived from antiquity.
The volumetric reconstructions are distributed as OME-Zarr multiscale datasets to support
research in virtual unwrapping, segmentation, and text recovery of ancient scrolls.
Deciphering these scrolls could forever change our understanding of Roman history.</description>
    </item>
    <item>
      <title>WIS2 Global Cache on AWS</title>
      <link>https://registry.opendata.aws/wis2-global-cache</link>
      <guid>https://registry.opendata.aws/wis2-global-cache</guid>
      <description>Global real-time Earth system data deemed by the World Meteorological Organisation (WMO) as essential for provision of services for the protection of life and property and for the well-being of all nations. Data is sourced from all WMO Member countries / territories and retained for 24-hours. Met Office and NOAA operate this Global Cache service curating and publishing the dataset on behalf of WMO.</description>
    </item>
    <item>
      <title>Wind AI Bench</title>
      <link>https://registry.opendata.aws/nrel-pds-windai</link>
      <guid>https://registry.opendata.aws/nrel-pds-windai</guid>
      <description>This data lake contains multiple datasets related to fundamental problems 
in wind energy research. This includes data for wind plant power production 
for various layouts/wind flow scenarios, data for two- and three-dimensional 
flow around different wind turbine airfoils/blades, wind turbine noise 
production, among others. The purpose of these datasets is to establish a 
standard benchmark against which new AI/ML methods can be tested, compared, 
and deployed. Details regarding the generation and formatting of the data for 
each dataset is included in the metadata as well as example notebooks and 
documentation that show how to access the data for ML modeling.</description>
    </item>
    <item>
      <title>run_dbcan CAZyme and CGC annotation database on AWS</title>
      <link>https://registry.opendata.aws/run_dbcan</link>
      <guid>https://registry.opendata.aws/run_dbcan</guid>
      <description>Database for use with run_dbcan (CAZyme and CGC annotation), including CAZyme, Transporter, Transcription factor, Signaling Transduction Protein, Sulfatase, Peptidase, and Polysaccharide utilization Loci.</description>
    </item>
    <item>
      <title>1940 Census Population Schedules, Enumeration District Maps, and Enumeration District Descriptions</title>
      <link>https://registry.opendata.aws/nara-1940-census</link>
      <guid>https://registry.opendata.aws/nara-1940-census</guid>
      <description>The 1940 Census population schedules were created by the Bureau of the Census in an attempt to enumerate every person living in the United States on April 1, 1940, although some persons were missed. The 1940 census population schedules were digitized by the National Archives and Records Administration (NARA) and released publicly on April 2, 2012.
The 1940 Census enumeration district maps contain maps of counties, cities, and other minor civil divisions that show enumeration districts, census tracts, and related boundaries and numbers used for each census. The coverage is nation wide and includes territorial areas.
The 1940 Census enumeration district descriptions contain written descriptions of census districts, subdivisions, and enumeration districts.</description>
    </item>
    <item>
      <title>1950 Census Population Schedules, Enumeration District Maps, and Enumeration District Descriptions</title>
      <link>https://registry.opendata.aws/nara-1950-census</link>
      <guid>https://registry.opendata.aws/nara-1950-census</guid>
      <description>The 1950 Census population schedules were created by the Bureau of the Census in an attempt to enumerate every person living in the United States on April 1, 1950, although some persons were missed. The 1950 census population schedules were digitized by the National Archives and Records Administration (NARA) and released publicly on April 1, 2022.
The 1950 Census enumeration district maps contain maps of counties, cities, and other minor civil divisions that show enumeration districts, census tracts, and related boundaries and numbers used for each census. The coverage is nation wide and includes territorial areas.
The 1950 Census enumeration district descriptions contain written descriptions of census districts, subdivisions, and enumeration districts.</description>
    </item>
    <item>
      <title>2010 Census Production Settings Redistricting Data (P.L. 94-171) Demonstration Noisy Measurement File</title>
      <link>https://registry.opendata.aws/census-2010-pl94-nmf</link>
      <guid>https://registry.opendata.aws/census-2010-pl94-nmf</guid>
      <description>The 2010 Census Production Settings Redistricting Data (P.L. 94-171) Demonstration Noisy Measurement File (2023-04-03) is an intermediate output of the 2020 Census Disclosure Avoidance System (DAS) TopDown Algorithm (TDA) (as described in Abowd, J. et al [2022] &lt;a href&#x3D;&quot;https://doi.org/10.1162/99608f92.529e3cb9&quot;&gt;https://doi.org/10.1162/99608f92.529e3cb9&lt;/a&gt; , and implemented in &lt;a href&#x3D;&quot;https://github.com/uscensusbureau/DAS_2020_Redistricting_Production_Code&quot;&gt;https://github.com/uscensusbureau/DAS_2020_Redistricting_Production_Code&lt;/a&gt;). The NMF was produced using the official “production settings,” the final set of algorithmic parameters and privacy-loss budget allocations, that were used to produce the 2020 Census Redistricting Data (P.L. 94-171) Summary File and the 2020 Census Demographic and Housing Characteristics File.
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The NMF consists of the full set of privacy-protected statistical queries (counts of individuals or housing units with particular combinations of characteristics) of confidential 2010 Census data relating to the redistricting data portion of the 2010 Demonstration Data Products Suite – Redistricting and Demographic and Housing Characteristics File – Production Settings (2023-04-03). These statistical queries, called “noisy measurements” were produced under the zero-Concentrated Differential Privacy framework (Bun, M. and Steinke, T [2016] &lt;a href&#x3D;&quot;https://arxiv.org/abs/1605.02065&quot;&gt;https://arxiv.org/abs/1605.02065&lt;/a&gt;; see also Dwork C. and Roth, A. [2014] &lt;a href&#x3D;&quot;https://www.cis.upenn.edu/~aaroth/Papers/privacybook.pdf&quot;&gt;https://www.cis.upenn.edu/~aaroth/Papers/privacybook.pdf&lt;/a&gt;) implemented via the discrete Gaussian mechanism (Cannone C., et al., [2023] &lt;a href&#x3D;&quot;https://arxiv.org/abs/2004.00010&quot;&gt;https://arxiv.org/abs/2004.00010&lt;/a&gt;), which added positive or negative integer-valued noise to each of the resulting counts. The noisy measurements are an intermediate stage of the TDA prior to the post-processing the TDA then performs to ensure internal and hierarchical consistency within the resulting tables. The Census Bureau has released these 2010 Census demonstration data to enable data users to evaluate the expected impact of disclosure avoidance variability on 2020 Census data. The 2010 Census Production Settings Redistricting Data (P.L.94-171) Demonstration Noisy Measurement File (2023-04-03) has been cleared for public dissemination by the Census Bureau Disclosure Review Board (CBDRB-FY22-DSEP-004).
&lt;br/&gt;
&lt;br/&gt;
The data includes zero-Concentrated Differentially Private (zCDP) (Bun, M. and Steinke, T [2016]) noisy measurements, implemented via the discrete Gaussian mechanism. These are estimated counts of individuals and housing units included in the 2010 Census Edited File (CEF), which includes confidential data initially collected in the 2010 Census of Population and Housing. The noisy measurements included in this file were subsequently post-processed by the TopDown Algorithm (TDA) to produce the 2010 Census Production Settings Privacy-Protected Microdata File - Redistricting (P.L. 94-171) and Demographic and Housing Characteristics File (2023-04-03) (&lt;a href&#x3D;&quot;https://www2.census.gov/programs-surveys/decennial/2020/program-management/data-product-planning/2010-demonstration-data-products/04-Demonstration_Data_Products_Suite/2023-04-03/&quot;&gt;https://www2.census.gov/programs-surveys/decennial/2020/program-management/data-product-planning/2010-demonstration-data-products/04-Demonstration_Data_Products_Suite/2023-04-03/&lt;/a&gt;). As these 2010 Census demonstration data are intended to support study of the design and expected impacts of the 2020 Disclosure Avoidance System, the 2010 CEF records were pre-processed before application of the zCDP framework. This pre-processing converted the 2010 CEF records into the input-file format, response codes, and tabulation categories used for the 2020 Census, which differ in substantive ways from the format, response codes, and tabulation categories originally used for the 2010 Census.
&lt;br/&gt;
&lt;br/&gt;
The NMF provides estimates of counts of persons in the CEF by various characteristics and combinations of characteristics including their reported race and ethnicity, whether they were of voting age, whether they resided in a housing unit or one of 7 group quarters types, and their census block of residence after the addition of discrete Gaussian noise (with the scale parameter determined by the privacy-loss budget allocation for that particular query under zCDP). Noisy measurements of the counts of occupied and vacant housing units by census block are also included. Lastly, data on constraints—information into which no noise was infused by the Disclosure Avoidance System (DAS) and used by the TDA to post-process the noisy measurements into the 2010 Census Production Settings Privacy-Protected Microdata File - Redistricting (P.L. 94-171) and Demographic and Housing Characteristics File (2023-04-03) —are provided.</description>
    </item>
    <item>
      <title>2020 Census Redistricting Data (P.L. 94-171) Noisy Measurement File</title>
      <link>https://registry.opendata.aws/census-2020-pl94-nmf</link>
      <guid>https://registry.opendata.aws/census-2020-pl94-nmf</guid>
      <description>The 2020 Census Redistricting Data (P.L. 94-171) Noisy Measurement File (NMF) is an intermediate output of the 2020 Census Disclosure Avoidance System (DAS) TopDown Algorithm (TDA) (as described in Abowd, J. et al [2022] &lt;a href&#x3D;&quot;https://doi.org/10.1162/99608f92.529e3cb9&quot;&gt;https://doi.org/10.1162/99608f92.529e3cb9&lt;/a&gt;, and implemented in the &lt;a href&#x3D;&quot;https://github.com/uscensusbureau/DAS_2020_Redistricting_Production_Code&quot;&gt;DAS 2020 Redistricting Production Code&lt;/a&gt;). The NMF was generated using &lt;a href&#x3D;&quot;https://github.com/uscensusbureau/DAS_2020_Redistricting_Production_Code/blob/289ee463936a6f0efcf2e378abe410ec01d0e140/source/programs/engine/primitives.py#L183&quot;&gt;the Census Bureau&amp;#39;s implementation&lt;/a&gt; of the &lt;a href&#x3D;&quot;https://arxiv.org/abs/2004.00010&quot;&gt;Discrete Gaussian Mechanism&lt;/a&gt;, calibrated to satisfy &lt;a href&#x3D;&quot;https://arxiv.org/abs/1605.02065&quot;&gt;zero-Concentrated Differential Privacy&lt;/a&gt; with &lt;a href&#x3D;&quot;https://dl.acm.org/doi/10.1145/1989323.1989345&quot;&gt;bounded neighbors&lt;/a&gt;.
&lt;br/&gt;
  &lt;br/&gt;
The NMF values, called &lt;strong&gt;noisy measurements&lt;/strong&gt; are the output of applying the Discrete Gaussian Mechanism to counts from the 2020 Census Edited File (CEF). They are generally inconsistent with one another (for example, in a county composed of two tracts, the noisy measurement for the county&amp;#39;s total population may not equal the sum of the noisy measurements of the two tracts&amp;#39; total population), and frequently negative (especially when the population being measured was small), but are integer-valued. The NMF was later post-processed as part of the DAS code to take the form of microdata and to satisfy various constraints. The NMF documented here contains both the noisy measurements themselves as well as the data needed to represent the DAS constraints; thus, the NMF could be used to reproduce the steps taken by the DAS code to produce microdata from the noisy measurements by applying &lt;a href&#x3D;&quot;https://github.com/uscensusbureau/DAS_2020_Redistricting_Production_Code/blob/289ee463936a6f0efcf2e378abe410ec01d0e140/source/&quot;&gt;the production code base&lt;/a&gt;.
&lt;br/&gt;
&lt;br/&gt;
The 2020 Census Redistricting Data (P.L. 94-171) Noisy Measurement File includes zero-Concentrated Differentially Private (zCDP) (Bun, M. and Steinke, T [2016]) noisy measurements, implemented via the discrete Gaussian mechanism. These are estimated counts of individuals and housing units included in the 2020 Census Edited File (CEF), which includes confidential data initially collected in the 2020 Census of Population and Housing. The noisy measurements included in this file were subsequently post-processed by the TopDown Algorithm (TDA) to produce the &lt;a href&#x3D;&quot;https://www.census.gov/programs-surveys/decennial-census/about/rdo/summary-files.html&quot;&gt;2020 Census Redistricting Data (P.L. 94-171) Summary File&lt;/a&gt;.
&lt;br/&gt;
&lt;br/&gt;
The NMF provides estimates of counts of persons in the CEF by various characteristics and combinations of characteristics including their reported race and ethnicity, whether they were of voting age, whether they resided in a housing unit or one of 7 group quarters types, and their census block of residence after the addition of discrete Gaussian noise (with the scale parameter determined by the privacy-loss budget allocation for that particular query under zCDP). Noisy measurements of the counts of occupied and vacant housing units by census block are also included. Lastly, data on constraints--information into which no noise was infused by the Disclosure Avoidance System (DAS) and used by the TDA to post-process the noisy measurements into the 2020 Census Redistricting Data (P.L. 94-171) Summary File --are provided.</description>
    </item>
    <item>
      <title>4D Nucleome (4DN)</title>
      <link>https://registry.opendata.aws/4dnucleome</link>
      <guid>https://registry.opendata.aws/4dnucleome</guid>
      <description>The goal of the National Institutes of Health (NIH) Common Fund’s 4D Nucleome (4DN) program
is to study the three-dimensional organization of the nucleus in space and time (the 4th dimension).
The nucleus of a cell contains DNA, the genetic “blueprint” that encodes all of the genes a living
organism uses to produce proteins needed to carry out life-sustaining cellular functions. Understanding
the conformation of the nuclear DNA and how it is maintained or changes in response to environmental
and cellular cues over time will provide insights into basic biology as well as aspects of human
health and disease. The 4DN is an international consortium of researchers who generate data that
include results from a variety of genomics and imaging assays with a focus on, but not exclusive to,
those that demonstrate close contact between chromatin loci that are non-adjacent on the linear DNA
sequence of chromosomes. Additional assays probe the nuclear landscape in the context of interactions
of chromatin with specific proteins, RNAs and epigenetic changes.</description>
    </item>
    <item>
      <title>A Global Drought and Flood Catalogue from 1950 to 2016</title>
      <link>https://registry.opendata.aws/global-drought-flood-catalogue</link>
      <guid>https://registry.opendata.aws/global-drought-flood-catalogue</guid>
      <description>Hydrological extremes, in the form of droughts and floods, have impacts on a wide range of sectors including water availability, food security, and energy production, among others. Given continuing large impacts of droughts and floods and the expectation for significant regional changes projected in the future, there is an urgent need to provide estimates of past events and their future risk, globally. However, current estimates of hydrological extremes are not robust and accurate enough, due to lack of long-term data records, standardized methods for event identification, geographical inconsistencies and data uncertainties. To tackle these challenges, we develop the first Global Drought and Flood Catalogue (GDFC) [He et al., 2020] for 1950-2016 by merging the latest in situ and remote-sensing datasets with state-of-the-art land surface and hydrodynamic modeling to provide a continuous and consistent estimate of the terrestrial water cycle and its extremes. This GDFC also includes an unprecedented level of detailed analysis of drought and large-scale flood events using a multivariate risk assessment framework, which incorporates regional spatial-temporal characteristics (i.e., duration, spatial extent, severity) and global hazard maps for different return periods. This catalogue forms a basis for analyzing the changing risk of droughts and floods and can underscore national and international climate change assessments and provide a key reference for climate change studies and climate model evaluations.</description>
    </item>
    <item>
      <title>ASL 1000</title>
      <link>https://registry.opendata.aws/asl_1000</link>
      <guid>https://registry.opendata.aws/asl_1000</guid>
      <description>This dataset provides a high-fidelity collection of American Sign Language (ASL) videos annotated with 2D landmarks for hands, pose, and face. The data is designed to train advanced research and development in ASL recognition, translation, gesture analysis, and computer animation. The annotations for this dataset were generated using an automated data pipeline to pre-annotate keyframes from the source videos. As a final, critical step, all automated annotations were subsequently reviewed and meticulously corrected by human labellers to ensure the highest level of accuracy and reliability, making it suitable for training production-grade machine learning models.</description>
    </item>
    <item>
      <title>Africa Soil Information Service (AfSIS) Soil Chemistry</title>
      <link>https://registry.opendata.aws/afsis</link>
      <guid>https://registry.opendata.aws/afsis</guid>
      <description>This dataset contains soil infrared spectral data and paired soil property
reference measurements for georeferenced soil samples that were collected
through the Africa Soil Information Service (AfSIS) project, which lasted
from 2009 through 2018. In this release, we include data collected during
Phase I (2009-2013.) Georeferenced samples were collected from 19 countries
in Sub-Saharan African using a statistically sound sampling scheme,
and their soil properties were analyzed using &lt;em&gt;both&lt;/em&gt; conventional soil
testing methods and spectral methods (infrared diffuse reflectance
spectroscopy). The two types of data can be paired to form a training
dataset for machine learning, such that certain soil properties can be
well-predicted through less expensive spectral techniques.</description>
    </item>
    <item>
      <title>AgricultureVision</title>
      <link>https://registry.opendata.aws/intelinair_agriculture_vision</link>
      <guid>https://registry.opendata.aws/intelinair_agriculture_vision</guid>
      <description>Agriculture-Vision aims to be a publicly available large-scale aerial agricultural image dataset that is high-resolution, multi-band, and with multiple types of patterns annotated by agronomy experts.  The original dataset affiliated with the 2020 CVPR paper includes 94,986 512x512images sampled from 3,432 farmlands with nine types of annotations: double plant, drydown, endrow, nutrient deficiency, planter skip, storm damage, water, waterway and weed cluster.  All of these patterns have substantial impacts on field conditions and the final yield. These farmland images were captured between 2017 and 2019 across multiple growing seasons in numerous farming locations in the US.  Each field image contains four color channels: Near-infrared (NIR), Red, Green and Blue.  We first randomly split the 3,432 farmland images with a 6/2/2 train/val/test ratio. We then assign each sampled image to the split of the farmland image they are cropped from. This guarantees that no cropped images from the same farmland will appear in multiple splits in the final dataset.  The generated (supervised) Agriculture-Vision dataset thus contains 56,944/18,334/19,708 train/val/test images.
Additionally, we continue to grow this dataset.  In 2021 as a part of the &lt;a href&#x3D;&quot;https://www.agriculture-vision.com/agriculture-vision-2021/prize-challenge-2021&quot;&gt;Prize Challenge at CVPR&lt;/a&gt;, we have added sequences of full-field imagery across 52 fields to promote the use of weakly supervised methods.</description>
    </item>
    <item>
      <title>Allen Institute for Brain Science - Synaptic Physiology Public Data Set</title>
      <link>https://registry.opendata.aws/allen-synphys</link>
      <guid>https://registry.opendata.aws/allen-synphys</guid>
      <description>This is a large-scale survey that describes the physiology (strength, kinetics, and short term plasticity) of thousands of synapses from patch clamp experiments in mouse visual cortex and human middle temporal gyrus.  </description>
    </item>
    <item>
      <title>Allen Institute for Neural Dynamics - Extracellular Electrophysiology Compression Benchmark</title>
      <link>https://registry.opendata.aws/allen-nd-ephys-compression</link>
      <guid>https://registry.opendata.aws/allen-nd-ephys-compression</guid>
      <description>Extracellular electrophysiology data is growing at a remarkable pace. This data, collected neuropixels probes by the Allen Institute and the International Brain Lab can be used to benchmark throughput rates and storage ratios of various data compression algorithms.</description>
    </item>
    <item>
      <title>Allen Institute for Neural Dynamics - Extracellular Electrophysiology Hybrid Evaluation Benchmark</title>
      <link>https://registry.opendata.aws/allen-nd-ephys-hybrid-evaluation</link>
      <guid>https://registry.opendata.aws/allen-nd-ephys-hybrid-evaluation</guid>
      <description>Evaluation of spike sorting methods is a challenging task, as it requires both ground-truth data and a variety of sorting algorithms to compare against. This dataset contains a set of hybrid data specifically designed for benchmarking spike sorting methods.</description>
    </item>
    <item>
      <title>Allen institute intratelencephalic neuron connectivity paper supplemental data</title>
      <link>https://registry.opendata.aws/allen-it-connectivity</link>
      <guid>https://registry.opendata.aws/allen-it-connectivity</guid>
      <description>organized and data files for plotting figures in the manuscript of VISp intratelencephalic (IT) neuron connectivity using MICrONS EM dataset</description>
    </item>
    <item>
      <title>Animal Tracking - Acoustic Telemetry - Quality controlled detections</title>
      <link>https://registry.opendata.aws/aodn_animal_acoustic_tracking_delayed_qc</link>
      <guid>https://registry.opendata.aws/aodn_animal_acoustic_tracking_delayed_qc</guid>
      <description>Since 2007, the Integrated Marine Observing System’s Animal Tracking Facility (formerly known as the Australian Animal Tracking And Monitoring System (AATAMS)) has established a permanent array of acoustic receivers around Australia to detect the movements of tagged marine animals in coastal waters. Simultaneously, the Animal Tracking Facility developed a centralised national database (&lt;a href&#x3D;&quot;https://animaltracking.aodn.org.au/&quot;&gt;https://animaltracking.aodn.org.au/&lt;/a&gt;) to encourage collaborative research across the Australian research community and provide unprecedented opportunities to monitor broad-scale animal movements. The resulting dataset comprises observations of tagged animals in Australian waters collected by IMOS infrastructure as well as receivers operated by independent research projects and  organisations. This dataset constitutes a valuable resource facilitating meta-analysis of animal movement, distributions, and habitat use, and is important for relating species distribution shifts with environmental covariates.This dataset comprises all available (2007 – ongoing) quality-controlled animal detections collected across the collaborative, continental IMOS network for a range of aquatic species (fish, sharks, rays, reptiles, and mammals). Here, raw animal detections collated via the IMOS Australian Animal Acoustic Telemetry Database have been quality-controlled as per Hoenner et al. (2018). This dataset is updated on a six-monthly basis.Note - There is a static snapshot of the database (up until 2017) (&lt;a href&#x3D;&quot;http://dx.doi.org/10.4225/69/5979810a7dd6f&quot;&gt;http://dx.doi.org/10.4225/69/5979810a7dd6f&lt;/a&gt;), and this has been documented in a Scientific Data Publication (Hoenner et al. 2018).</description>
    </item>
    <item>
      <title>Astrophysics Division Galaxy Segmentation Benchmark Dataset</title>
      <link>https://registry.opendata.aws/apd_galaxysegmentation</link>
      <guid>https://registry.opendata.aws/apd_galaxysegmentation</guid>
      <description>Pan-STARSS imaging data and associated labels for galaxy segmentation into galactic centers, galactic bars, spiral arms and foreground stars derived from citizen scientist labels from the Galaxy Zoo: 3D project.</description>
    </item>
    <item>
      <title>Atmospheric Models from Météo-France</title>
      <link>https://registry.opendata.aws/meteo-france-models</link>
      <guid>https://registry.opendata.aws/meteo-france-models</guid>
      <description>Global and high-resolution regional atmospheric models from Météo-France.&lt;ul&gt;
&lt;li&gt;ARPEGE World covers the entire world at a base horizontal resolution of 0.5° (~55km) between grid points, it predicts weather out up to 114 hours in the future.&lt;/li&gt;
&lt;li&gt;ARPEGE Europe covers Europe and North-Africa at a base horizontal resolution of 0.1° (~11km) between grid points, it predicts weather out up to 114 hours in the future.&lt;/li&gt;
&lt;li&gt;AROME France covers France at a base horizontal resolution of 0.025° (~2.5km) between grid points, it predicts weather out up to 42 hours in the future.&lt;/li&gt;
&lt;li&gt;AROME France HD covers France and neighborhood at a base horizontal resolution of 0.01° (~1.5km) between grid points, it predicts weather out up to 42 hours in the future.&lt;/li&gt;
&lt;/ul&gt;
Dozens of atmospheric variables are available through this datase: temperatures, winds, precipitation...Our work is based on open-data from Météo-France, but we are not affiliated or endorsed by Météo-France.</description>
    </item>
    <item>
      <title>Aurora Multi-Sensor Dataset</title>
      <link>https://registry.opendata.aws/aurora_msds</link>
      <guid>https://registry.opendata.aws/aurora_msds</guid>
      <description>The Aurora Multi-Sensor Dataset is an open, large-scale multi-sensor dataset with highly accurate localization ground truth, captured between January 2017 and February 2018 in the metropolitan area of Pittsburgh, PA, USA by Aurora (via Uber ATG) in collaboration with the University of Toronto. The de-identified dataset contains rich metadata, such as weather and semantic segmentation, and spans all four seasons, rain, snow, overcast and sunny days, different times of day, and a variety of traffic conditions.
&lt;br/&gt;
The Aurora Multi-Sensor Dataset contains data from a 64-beam Velodyne HDL-64E LiDAR sensor and seven 1920x1200-pixel resolution cameras including a forward-facing stereo pair and five wide-angle lenses covering a 360-degree view around the vehicle.
&lt;br/&gt;
This data can be used to develop and evaluate large-scale long-term approaches to autonomous vehicle localization. Its size and diversity make it suitable for a wide range of research areas such as 3D reconstruction, virtual tourism, HD map construction, and map compression, among others.
&lt;br/&gt;
The data was first presented at the International Conference on Intelligent Robots and Systems (IROS) in 2020, where it was nominated as a Finalist for Best Application Paper at the conference.</description>
    </item>
    <item>
      <title>Biodiversity Heritage Library Metadata and Page Images</title>
      <link>https://registry.opendata.aws/bhl-open-data</link>
      <guid>https://registry.opendata.aws/bhl-open-data</guid>
      <description>The Biodiversity Heritage Library (BHL) is the world’s largest open access digital library for biodiversity literature and archives. BHL operates as a worldwide consortium of natural history, botanical, research, and national libraries working together to digitize the natural history literature held in their collections and make it freely available for open access.</description>
    </item>
    <item>
      <title>Biological and Physical Sciences (BPS) Microscopy Benchmark Training Dataset</title>
      <link>https://registry.opendata.aws/bps_microscopy</link>
      <guid>https://registry.opendata.aws/bps_microscopy</guid>
      <description>Fluorescence microscopy images of individual nuclei from mouse fibroblast cells, irradiated with Fe particles or X-rays with fluorescent foci indicating 53BP1 positivity, a marker of DNA damage. These are maximum intensity projections of 9-layer microscopy Z-stacks.</description>
    </item>
    <item>
      <title>Biological and Physical Sciences (BPS) RNA Sequencing Benchmark Training Dataset</title>
      <link>https://registry.opendata.aws/bps_rnaseq</link>
      <guid>https://registry.opendata.aws/bps_rnaseq</guid>
      <description>RNA sequencing data from spaceflown and control mouse liver samples, sourced from NASA GeneLab and augmented with generative adversarial network.</description>
    </item>
    <item>
      <title>Brain Encoding Response Generator (BERG)</title>
      <link>https://registry.opendata.aws/brain-encoding-response-generator</link>
      <guid>https://registry.opendata.aws/brain-encoding-response-generator</guid>
      <description>Brain Encoding Response Generator (BERG) is a resource consisting of multiple pre-trained encoding models of the brain and an accompanying Python package to generate accurate in silico neural responses to arbitrary stimuli with just a few lines of code.</description>
    </item>
    <item>
      <title>Brain/MINDS Marmoset Connectivity Resource on AWS</title>
      <link>https://registry.opendata.aws/brainminds-marmoset-connectivity</link>
      <guid>https://registry.opendata.aws/brainminds-marmoset-connectivity</guid>
      <description>Brain/MINDS Marmoset Connectivity Resource (BMCR) is a resource that provides access to anterograde and retrograde neuronal tracer data, made available by Brain/MINDS project. It is currently restricted to injections into the prefrontal cortex of a marmoset brain but is planned to include injections into entire cortical areas and representative subcortical brain regions.</description>
    </item>
    <item>
      <title>BrainGlobe Atlases</title>
      <link>https://registry.opendata.aws/brainglobe</link>
      <guid>https://registry.opendata.aws/brainglobe</guid>
      <description>BrainGlobe provides an archive and standardised interface to anatomical atlases from multiple species. This dataset includes these atlases, and other data (e.g. sample neuroanatomy data) to allow the greatest use of the atlases.</description>
    </item>
    <item>
      <title>BrainSeq - Neurogenomics to Drive Novel Target Discovery for Neuropsychiatric Disorders</title>
      <link>https://registry.opendata.aws/brainseq</link>
      <guid>https://registry.opendata.aws/brainseq</guid>
      <description>This ambitious project seeks to characterize the genetic and epigenetic regulation of multiple facets of transcription in distinct brain regions across the human lifespan in samples of major neuropsychiatric disorders and controls. Initially focused on schizophrenia and mood disorders, the goal of this consortium is to elucidate the underlying molecular mechanisms of genetic associations with the goal of identifying novel therapeutic targets. The consortium currently consists of seven pharmaceutical companies and a not-for-profit medical research institution working as a precompetitive team to generate and analyze publicly available archival brain genomic data related to neuropsychiatric illness.</description>
    </item>
    <item>
      <title>Broad Genome References</title>
      <link>https://registry.opendata.aws/broad-references</link>
      <guid>https://registry.opendata.aws/broad-references</guid>
      <description>Broad maintained human genome reference builds hg19/hg38 and decoy references.</description>
    </item>
    <item>
      <title>COVID-19 Data Lake</title>
      <link>https://registry.opendata.aws/aws-covid19-lake</link>
      <guid>https://registry.opendata.aws/aws-covid19-lake</guid>
      <description>A centralized repository of up-to-date and curated datasets on or related to the spread and characteristics of the novel corona virus (SARS-CoV-2) and its associated illness, COVID-19. Globally, there are several efforts underway to gather this data, and we are working with partners to make this crucial data freely available and keep it up-to-date. Hosted on the AWS cloud, we have seeded our curated data lake with COVID-19 case tracking data from Johns Hopkins and The New York Times, hospital bed availability from Definitive Healthcare, and over 45,000 research articles about COVID-19 and related coronaviruses from the Allen Institute for AI.</description>
    </item>
    <item>
      <title>CanElevation - Canada Digital Elevation Models</title>
      <link>https://registry.opendata.aws/canelevation-dem</link>
      <guid>https://registry.opendata.aws/canelevation-dem</guid>
      <description>The Canadian DEM represents the current coverage of elevation data available. This dataset includes a Digital Terrain Model (DTM), a Digital Surface Model (DSM) and other derived products. This dataset includes a 1m, 2m and 30m DEM. The 1m and 2 m products are a combination of DEM data generated from airborne LiDAR and optical digital images. The 30 m DEM integrates data from the Copernicus DEM acquired during the TanDEM-X Mission, with the DEM data derived from airborne lidar and provides a complete coverage for Canada. 
&lt;br/&gt;
&lt;br/&gt;
Le modèle numérique d’élévation (MNE) canadien représente la couverture actuelle des données d’élévation disponibles. Ce jeu de données comprend un Modèle Numérique de Terrain (MNT), un Modèle Numérique de Surface (MNS) et d’autres produits dérivés. Ce jeu de données propose des MNE de résolution 1 m, 2 m et 30 m. Les produits 1 m et 2 m sont issus d’une combinaison de données MNE générées à partir de LiDAR aéroporté et d’images numériques optiques. Le MNE de 30 m intègre des données provenant du MNE Copernicus acquis lors de la mission TanDEM-X, ainsi que les données MNE issues du LiDAR aéroporté, ce qui permet d’assurer une couverture complète du Canada. </description>
    </item>
    <item>
      <title>Cancer Genome Characterization Initiatives - Burkitt Lymphoma, HIV+ Cervical Cancer</title>
      <link>https://registry.opendata.aws/cgci</link>
      <guid>https://registry.opendata.aws/cgci</guid>
      <description>The Cancer Genome Characterization Initiatives (CGCI) program supports cutting-edge genomics research of adult and pediatric cancers. CGCI investigators develop and apply advanced sequencing methods that examine genomes, exomes, and transcriptomes within various types of tumors. The program includes Burkitt Lymphoma Genome Sequencing Project (BLGSP) project and HIV+ Tumor Molecular Characterization Project - Cervical Cancer (HTMCP-CC) project.
The dataset contains open Clinical Supplement, Biospecimen Supplement, RNA-Seq Gene Expression Quantification, miRNA-Seq Isoform Expression Quantification, and miRNA Expression Quantification data.
This dataset also contains controlled WGS/Targeted Sequencing/RNA-Seq/miRNA-Seq Aligned Reads, and RNA-Seq Splice Junction Quantification</description>
    </item>
    <item>
      <title>Cell Painting Image Collection</title>
      <link>https://registry.opendata.aws/cell-painting-image-collection</link>
      <guid>https://registry.opendata.aws/cell-painting-image-collection</guid>
      <description>The Cell Painting Image Collection is a collection of freely
downloadable microscopy image sets. Cell Painting is an
unbiased high throughput imaging assay used to analyze
perturbations in cell models. In addition to the images
themselves, each set includes a description of the biological
application and some type of &amp;quot;ground truth&amp;quot; (expected results).
Researchers are encouraged to use these image sets as reference
points when developing, testing, and publishing new image
analysis algorithms for the life sciences. We hope that the
this data set will lead to a better understanding of which
methods are best for various biological image analysis
applications.</description>
    </item>
    <item>
      <title>Cloud Indexes for Bowtie, Kraken, HISAT, and Centrifuge</title>
      <link>https://registry.opendata.aws/jhu-indexes</link>
      <guid>https://registry.opendata.aws/jhu-indexes</guid>
      <description>Genomic tools use reference databases as indexes to operate quickly and efficiently, analogous to how web search engines use indexes for fast querying. Here, we aggregate genomic, pan-genomic and metagenomic indexes for analysis of sequencing data.</description>
    </item>
    <item>
      <title>Collection of open nation-scale LiDAR datasets</title>
      <link>https://registry.opendata.aws/open-lidar-data</link>
      <guid>https://registry.opendata.aws/open-lidar-data</guid>
      <description>The goal of this project is to collect all publicly available large scale LiDAR datasets and archive them in an
uniform fashion for easy access and use. Initial efforts to collect the datasets are concentrated on Europe and will
be in future expanded to USA and other regions, striving for global coverage. Every dataset includes files in original
data format and translated to COPC format. For faster browsing, we include an overview file that includes a small
subset of data points from every dataset file in a single COPC file.</description>
    </item>
    <item>
      <title>Consented Activities of People</title>
      <link>https://registry.opendata.aws/visym-cap</link>
      <guid>https://registry.opendata.aws/visym-cap</guid>
      <description>The Consented Activities of People (CAP) dataset is a fine grained activity dataset for visual AI research curated using the &lt;a href&#x3D;&quot;https://www.visym.com/collector/&quot;&gt;Visym Collector&lt;/a&gt; platform.</description>
    </item>
    <item>
      <title>Copernicus Digital Elevation Model (DEM)</title>
      <link>https://registry.opendata.aws/copernicus-dem</link>
      <guid>https://registry.opendata.aws/copernicus-dem</guid>
      <description>The Copernicus DEM is a Digital Surface Model (DSM) which represents the surface of the Earth including buildings, infrastructure and vegetation. We provide two instances of Copernicus DEM named GLO-30 Public and GLO-90. GLO-90 provides worldwide coverage at 90 meters. GLO-30 Public provides limited worldwide coverage at 30 meters because a small subset of tiles covering specific countries are not yet released to the public by the Copernicus Programme. Note that in both cases ocean areas do not have tiles, there one can assume height values equal to zero. Data is provided as Cloud Optimized GeoTIFFs and comes from Copernicus DEM 2021 release.</description>
    </item>
    <item>
      <title>CoversBR</title>
      <link>https://registry.opendata.aws/covers-br</link>
      <guid>https://registry.opendata.aws/covers-br</guid>
      <description>CoversBR is the first large audio database with, predominantly, Brazilian music for the tasks of Covers Song
Identification (CSI) and Live Song Identifications (LSI). Due to copyright restrictions audios of
the songs cannot be made available, however metadata and files of features have public access. Audio
streamings captured from radio and TV channels for the live song identification task will be made public.
CoversBR is composed of metadata and features extracted from 102298 songs, distributed in 26366
groups of covers/versions, with an average of 3.88 versions per group. The entire collection adds up to a total of
approximately 7070 hours and the average song length is 240 seconds (4 minutes).</description>
    </item>
    <item>
      <title>Covid Job Impacts - US Hiring Data Since March 1 2020</title>
      <link>https://registry.opendata.aws/us-hiring-rates-pandemic</link>
      <guid>https://registry.opendata.aws/us-hiring-rates-pandemic</guid>
      <description>This dataset provides daily updates on the volume of US job listings filtered by geography industry job family and role; normalized to pre-covid levels.These data files feed the business intelligence visuals at covidjobimpacts.greenwich.hr, a public-facing site hosted by Greenwich.HR and OneModel Inc.
Data is derived from online job listings tracked continuously, calculated daily and published nightly.  On average data from 70% of all new US jobs are captured,
and the dataset currently contains data from 3.3 million hiring organizations.Data for each filter segment is represented as the 7-day average of new job listings for a specific date, expressed as a percentage of the corresponding value 
on March 1, 2020.</description>
    </item>
    <item>
      <title>Cryo-EM SPA Workflow Records</title>
      <link>https://registry.opendata.aws/cryoem-spa-workflow-records</link>
      <guid>https://registry.opendata.aws/cryoem-spa-workflow-records</guid>
      <description>The “Cryo-EM SPA Workflow Records” contains all outputs of all processing steps involved in cryogenic electron microscopy (cryo-EM) single particle analysis (SPA), including both intermediate and final output data. The primary focus will be on data generated by RELION and CryoSPARC, two widely used software packages for :Cryo-EM SPA. These records will be archived systematically. To ensure the data remains reproducible while minimizing storage demands, large-sized files that can be regenerated will be excluded prior to registration. The aim is to retain only the essential metadata, processing parameters, and representative outputs that allow for full reconstruction of the analysis pipeline. This approach balances the need for long-term data preservation with practical considerations for storage capacity. Through this effort, we seek to enhance transparency and reproducibility in cryo-EM research by providing a structured and accessible record of the analysis process. Importantly, the use of this dataset is intended to facilitate the development of future AI algorithms in the field of Cryo-EM.</description>
    </item>
    <item>
      <title>DNAStack COVID19 SRA Data</title>
      <link>https://registry.opendata.aws/dnastack-covid-19-sra-data</link>
      <guid>https://registry.opendata.aws/dnastack-covid-19-sra-data</guid>
      <description>The &lt;a href&#x3D;&quot;https://www.ncbi.nlm.nih.gov/sra/&quot;&gt;Sequence Read Archive (SRA)&lt;/a&gt; is the primary archive of high-throughput sequencing data, hosted by the National Institutes of Health (NIH). The SRA represents the largest publicly available repository of SARS-CoV-2 sequencing data. This dataset was created by DNAstack using SARS-CoV-2 sequencing data sourced from the SRA. Where possible, raw sequence data were processed by DNAstack through a unified bioinformatics pipeline to produce genome assemblies and variant calls. The use of a standardized workflow to produce this harmonized dataset allows public data generated using different methodologies to be combined and compared for a more powerful global analysis of available SARS-CoV-2 data, allowing researchers rapid access to aggregated downstream results for accelerated insight generation. Methodology: Reads from the SRA were extracted in FASTQ format, then entered into a different pipeline depending on the sequencing technology used to create the reads: the &lt;a href&#x3D;&quot;https://artic.network/ncov-2019/ncov2019-bioinformatics-sop.html&quot;&gt;ARTIC protocol&lt;/a&gt; for Oxford Nanopore-derived reads; the &lt;a href&#x3D;&quot;https://github.com/jaleezyy/covid-19-signal&quot;&gt;SIGNAL pipeline&lt;/a&gt; for paired-end Illumina reads; and the &lt;a href&#x3D;&quot;https://github.com/PacificBiosciences/CoSA&quot;&gt;CoSA pipeline&lt;/a&gt; (using &lt;a href&#x3D;&quot;https://github.com/google/deepvariant&quot;&gt;DeepVariant&lt;/a&gt; for variant calling) for PacBio reads. Briefly, reads were primer-trimmed and aligned to the SARS-CoV-2 reference genome, following which contiguous regions were assembled and variant sites were called. &lt;a href&#x3D;&quot;https://github.com/cov-lineages/pangolin&quot;&gt;Pangolin&lt;/a&gt; was then used to assign viral lineage based on the assembled genome.</description>
    </item>
    <item>
      <title>Danish Meteorological Institute (DMI) Reanalysis dataset v0.5</title>
      <link>https://registry.opendata.aws/dmi-danra-05</link>
      <guid>https://registry.opendata.aws/dmi-danra-05</guid>
      <description>DANRA is a high-resolution meteorological reanalysis dataset for Denmark and Northwestern Europe covering the period September 1990 to December 2023</description>
    </item>
    <item>
      <title>Dendritic Consortium Multimodal Dataset</title>
      <link>https://registry.opendata.aws/dendritic-consortium</link>
      <guid>https://registry.opendata.aws/dendritic-consortium</guid>
      <description>The Dendritic Consortium provides a multimodal dataset integrating calcium and voltage imaging, electrophysiology, electron microscopy, proteomics, and computational models of Baz1a pyramidal neurons in the mouse primary visual cortex (V1).</description>
    </item>
    <item>
      <title>DigitalCorpora</title>
      <link>https://registry.opendata.aws/digitalcorpora</link>
      <guid>https://registry.opendata.aws/digitalcorpora</guid>
      <description>Disk images, memory dumps, network packet captures, and files for use in digital forensics research and education. All of this information is accessible through the digitalcorpora.org website, and made available at s3://digitalcorpora/. Some of these datasets implement scenarios that were performed by students, faculty, and others acting &lt;em&gt;in persona&lt;/em&gt;. As such, the information is synthetic and may be used without prior authorization or IRB approval. Details of these datasets can be found at &lt;a href&#x3D;&quot;http://www.simson.net/clips/academic/2009.DFRWS.Corpora.pdf&quot;&gt;http://www.simson.net/clips/academic/2009.DFRWS.Corpora.pdf&lt;/a&gt;</description>
    </item>
    <item>
      <title>Downscaled CMIP6 projections over CONUS at 30-arcsecond horizontal resolution</title>
      <link>https://registry.opendata.aws/nasa-nex-dcp30-cmip6</link>
      <guid>https://registry.opendata.aws/nasa-nex-dcp30-cmip6</guid>
      <description>The NEX-DCP30-CMIP6 dataset contains daily, monthly, and annual downscaled CMIP6 projections over CONUS at 30-arcsecond hoirzontal resolution for maximum temperature, minimum temperature, precipitation, and vapor pressure.  </description>
    </item>
    <item>
      <title>Downscaled Climate Data for Alaska (v1.1, August 2023)</title>
      <link>https://registry.opendata.aws/wrf-alaska-snap</link>
      <guid>https://registry.opendata.aws/wrf-alaska-snap</guid>
      <description>This dataset contains historical and projected dynamically downscaled climate data for the State of Alaska and surrounding regions at 20km spatial resolution and hourly temporal resolution. Select variables are also summarized into daily resolutions. This data was produced using the Weather Research and Forecasting (WRF) model (Version 3.5). We downscaled both ERA-Interim historical reanalysis data (1979-2015) and both historical and projected runs from 2 GCM’s from the Coupled Model Inter-comparison Project 5 (CMIP5): GFDL-CM3 and NCAR-CCSM4 (historical run: 1970-2005 and RCP 8.5: 2006-2100). Note - this dataset was updated in August, 2023 to retain the latitude and longitude grids as variables in the files.</description>
    </item>
    <item>
      <title>E11bio PRISM</title>
      <link>https://registry.opendata.aws/e11bio-prism</link>
      <guid>https://registry.opendata.aws/e11bio-prism</guid>
      <description>This dataset was generated using E11.bio&amp;#39;s PRISM technology (Protein Reconstruction and Identification through Multiplexing),
a platform that combines viral barcoding, expansion microscopy, and iterative immunolabeling for large-scale neuronal reconstruction.Neurons in the mouse hippocampal CA3 were transduced with a library of adeno-associated viruses (AAVs)
encoding diverse “protein bits”—small epitope tags that act as combinatorial barcodes. 
Tissue was then processed with an expansion microscopy protocol, physically enlarging the sample ~5×
to achieve an effective voxel size of ~35 × 35 × 80 nm.
Across multiple cycles of staining, imaging, and antibody stripping, the same expanded tissue was repeatedly labeled,
enabling iterative immunostaining for dozens of molecular targets.The dataset includes:&lt;ol&gt;
&lt;li&gt;Light microscopy data of multiplexed brain tissue&lt;/li&gt;
&lt;li&gt;Segmentations of cell morphology and protein expression in the tissue&lt;/li&gt;
&lt;li&gt;Files for faster visualization of the data (e.g. precomputed format)&lt;/li&gt;
&lt;li&gt;Additional supporting files (e.g. model predictions, manual annotations etc.)&lt;/li&gt;
&lt;/ol&gt;
</description>
    </item>
    <item>
      <title>ECMWF AIFS Single - dynamical.org Icechunk Zarr</title>
      <link>https://registry.opendata.aws/dynamical-ecmwf-aifs-single</link>
      <guid>https://registry.opendata.aws/dynamical-ecmwf-aifs-single</guid>
      <description>&lt;p&gt;The Artificial Intelligence Forecasting System (AIFS) is a data driven forecast model developed by the European Centre for Medium-Range Weather Forecasts (ECMWF). This is the non-ensemble configuration of AIFS that produces a single forecast trace. AIFS is trained on ECMWF&#x27;s ERA5 re-analysis and ECMWF&#x27;s operational numerical weather prediction (NWP) analyses.&lt;/p&gt;
&lt;p&gt;These datasets have been translated to cloud-optimized Icechunk Zarr format by &lt;a href&#x3D;&quot;https://dynamical.org&quot;&gt;dynamical.org&lt;/a&gt;.&lt;/p&gt;
&lt;ul&gt;
  &lt;li&gt;&lt;a href&#x3D;&quot;https://dynamical.org/catalog/ecmwf-aifs-single-forecast/&quot;&gt;ECMWF AIFS Single forecast&lt;/a&gt; - Weather forecasts from the ECMWF Artificial Intelligence Forecasting System (AIFS) Single model.&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>EMBER Open Datasets</title>
      <link>https://registry.opendata.aws/ember</link>
      <guid>https://registry.opendata.aws/ember</guid>
      <description>This is data from, Ecosystem for Multi-modal Brain-behavior Experimentation and Research (EMBER), It contains time series behavioral and neuroscience data from animal and deidentified human subjects across multiple modalities.</description>
    </item>
    <item>
      <title>EMory BrEast Imaging Dataset (EMBED)</title>
      <link>https://registry.opendata.aws/emory-breast-imaging-dataset-embed</link>
      <guid>https://registry.opendata.aws/emory-breast-imaging-dataset-embed</guid>
      <description>EMBED is a racially diverse mammography dataset containing 3.4M screening and diagnostic images from 110,000 patients collected from 2013-2020, with an
equal representation of black and white women. The dataset is comprised of 2D, synthetic 2D (C-view), and 3D (digital breast tomosynthesis, i.e. DBT)
images. It contains 60,000 annotated lesions linked to structured imaging descriptors and ground truth pathologic outcomes grouped into six severity
classes. This release represents 20% of the total 2D and C-view dataset and is available for research use. DBT, US, and MRI exams will be added at a
later date.&lt;/br&gt;&lt;/br&gt;
Acknowledgements - We would like to thank Glendor, Inc and MD.ai for assistance with image de-identification.</description>
    </item>
    <item>
      <title>Emory Knee Radiograph (MRKR) dataset</title>
      <link>https://registry.opendata.aws/mrkr</link>
      <guid>https://registry.opendata.aws/mrkr</guid>
      <description>The Emory Knee Radiograph (MRKR) dataset is a large, demographically diverse collection of
503,261 knee radiographs from 83,011 patients, 40% of which are African American. This dataset
provides imaging data in DICOM format along with detailed clinical information, including patient-
reported pain scores, diagnostic codes, and procedural codes, which are not commonly available in
similar datasets. The MRKR dataset also features imaging metadata such as image laterality, view type,
and presence of hardware, enhancing its value for research and model development. MRKR addresses
significant gaps in existing datasets by offering a more representative sample for studying osteoarthritis
and related outcomes, particularly among minority populations, thereby providing a valuable resource
for clinicians and researchers.
Acknowledgments - We would like to thank MD.ai for assistance with image de-identification.</description>
    </item>
    <item>
      <title>FLAb: Fitness Landscapes for Antibodies</title>
      <link>https://registry.opendata.aws/flab</link>
      <guid>https://registry.opendata.aws/flab</guid>
      <description>FLAb is the largest publicly available therapeutic antibody dataset designed to train and benchmark protein AI models. It provides open-access, high-quality developability data on diverse therapeutic properties, including expression, thermostability, immunogenicity, aggregation, polyreactivity, binding affinity, and pharmacokinetics.</description>
    </item>
    <item>
      <title>Ford Multi-AV Seasonal Dataset</title>
      <link>https://registry.opendata.aws/ford-multi-av-seasonal</link>
      <guid>https://registry.opendata.aws/ford-multi-av-seasonal</guid>
      <description>This research presents a challenging multi-agent seasonal dataset collected by a fleet of Ford autonomous vehicles at different days and times during 2017-18. The vehicles The vehicles were manually driven on an average route of 66 km in Michigan that included a mix of driving scenarios like the Detroit Airport, freeways, city-centres, university campus and suburban neighbourhood, etc. Each vehicle used in this data collection  is a Ford Fusion outfitted with an Applanix POS-LV inertial measurement unit (IMU), four HDL-32E Velodyne 3D-lidar scanners, 6 Point Grey 1.3 MP Cameras arranged on the rooftop for 360 degree coverage and 1 Pointgrey 5 MP camera mounted behind the windsheild for forward field of view. We present the seasonal variation in weather, lighting, construction and traffic conditions experienced in dynamic urban environments. This dataset can help design robust algorithms for autonomous vehicles and multi-agent systems. Each log in the dataset is time-stamped and contains raw data from all the sensors, calibration values, pose trajectory, ground truth pose, and 3D maps. All data is available in Rosbag format that can be visualized, modified and applied using the open-source Robot Operating System (ROS).</description>
    </item>
    <item>
      <title>GATK Structural Variation (SV) Data</title>
      <link>https://registry.opendata.aws/gatk-sv-data</link>
      <guid>https://registry.opendata.aws/gatk-sv-data</guid>
      <description>This dataset holds the data needed to run a &lt;a href&#x3D;&quot;https://github.com/broadinstitute/gatk-sv&quot;&gt;structural variation discovery pipeline&lt;/a&gt;
for Illumina short-read whole-genome sequencing (WGS) data in AWS.</description>
    </item>
    <item>
      <title>GEDI L2A Elevation and Height Metrics Data Global Footprint Level V002</title>
      <link>https://registry.opendata.aws/nasa-gedi02a</link>
      <guid>https://registry.opendata.aws/nasa-gedi02a</guid>
      <description>The Global Ecosystem Dynamics Investigation (&lt;a href&#x3D;&quot;https://gedi.umd.edu/&quot;&gt;GEDI&lt;/a&gt;) mission aims to characterize ecosystem structure and dynamics to enable radically improved quantification and understanding of the Earth’s carbon cycle and biodiversity. The GEDI instrument produces high resolution laser ranging observations of the 3-dimensional structure of the Earth. GEDI is attached to the International Space Station (ISS) and collects data globally between 51.6° N and 51.6° S latitudes at the highest resolution and densest sampling of any light detection and ranging (lidar) instrument in orbit to date. Each GEDI Version 2 granule encompasses one-fourth of an ISS orbit and includes georeferenced metadata to allow for spatial querying and subsetting.The GEDI instrument was removed from the ISS and placed into storage on March 17, 2023. No data were acquired during the hibernation period from March 17, 2023, to April 24, 2024. GEDI has since been reinstalled on the ISS and resumed operations as of April 26, 2024.The purpose of the GEDI Level 2A Geolocated Elevation and Height Metrics product (GEDI02_A) is to provide waveform interpretation and extracted products from each GEDI01_B received waveform, including ground elevation, canopy top height, and relative height (RH) metrics. The methodology for generating the GEDI02_A product datasets is adapted from the Land, Vegetation, and Ice Sensor (LVIS) algorithm. The GEDI02_A product is provided in HDF5 format and has a spatial resolution (average footprint) of 25 meters.The GEDI02_A data product contains 156 layers for each of the eight beams, including ground elevation, canopy top height, relative return energy metrics (e.g., canopy vertical structure), and many other interpreted products from the return waveforms. Additional information for the layers can be found in the GEDI Level 2A Dictionary.Known Issues&lt;ul&gt;
&lt;li&gt;Data acquisition gaps: GEDI data acquisitions were suspended on December 19, 2019 (2019 Day 353) and resumed on January 8, 2020 (2020 Day 8).&lt;/li&gt;
&lt;li&gt;Incorrect Reference Ground Track (RGT) number in the filename for select GEDI files: GEDI Science Data Products for six orbits on August 7, 2020, and November 12, 2021, had the incorrect RGT number in the filename. There is no impact to the science data, but users should reference this &lt;a href&#x3D;&quot;https://lpdaac.usgs.gov/documents/2236/GEDI_CORRECTED_RGT_FILENAMES.pptx&quot;&gt;document&lt;/a&gt; for the correct RGT numbers.&lt;/li&gt;
&lt;li&gt;Known Issues: Section 8 of the User Guide provides additional information on known issues.&lt;/li&gt;
&lt;/ul&gt;
Improvements/Changes from Previous Versions&lt;ul&gt;
&lt;li&gt;Metadata has been updated to include spatial coordinates.&lt;/li&gt;
&lt;li&gt;Granule size has been reduced from one full ISS orbit (&lt;del&gt;5.83 GB) to four segments per orbit (&lt;/del&gt;1.48 GB).&lt;/li&gt;
&lt;li&gt;Filename has been updated to include segment number and version number.&lt;/li&gt;
&lt;li&gt;Improved geolocation for an orbital segment.&lt;/li&gt;
&lt;li&gt;Added elevation from the SRTM digital elevation model for comparison.&lt;/li&gt;
&lt;li&gt;Modified the method to predict an optimum algorithm setting group per laser shot.&lt;/li&gt;
&lt;li&gt;Added additional land cover datasets related to phenology, urban infrastructure, and water persistence.&lt;/li&gt;
&lt;li&gt;Added selected_mode_flag dataset to root beam group using selected algorithm.&lt;/li&gt;
&lt;li&gt;Removed shots when the laser is not firing.&lt;/li&gt;
&lt;li&gt;Modified file name to include segment number and dataset version.
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&lt;/a&gt;&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>GHRSST Level 2P Global Sea Surface Skin Temperature from the MODIS on the NASA Terra satellite (GDS2)</title>
      <link>https://registry.opendata.aws/nasa-modis-t-jpl-l2p-v2019-0</link>
      <guid>https://registry.opendata.aws/nasa-modis-t-jpl-l2p-v2019-0</guid>
      <description>NASA produces skin sea surface temperature (SST) products from the Infrared (IR) channels of the Moderate-resolution Imaging Spectroradiometer (MODIS) onboard the Terra satellite. Terra was launched by NASA on December 18, 1999, into a sun synchronous, polar orbit with a daylight descending node at 10:30 am, to study the global dynamics of the Earth atmosphere, land and oceans. The MODIS captures data in 36 spectral bands at a variety of spatial resolutions.  Two SST products can be present in these files. The first is a skin SST produced for both day and night observations, derived from the long wave IR 11 and 12 micron wavelength channels, using a modified nonlinear SST algorithm intended to provide continuity with SST derived from heritage and current NASA sensors. At night, a second SST product is produced using the mid-infrared 3.95 and 4.05 micron channels which are unique to MODIS; the SST derived from these measurements is identified as SST4. The SST4 product has lower uncertainty, but due to sun glint can only be produced at night. MODIS L2P SST data have a 1 km spatial resolution at nadir and are stored in 288 five minute granules per day. Full global coverage is obtained every two days, with coverage poleward of 32.3 degree being complete each day. The production of MODIS L2P SST files is part of the Group for High Resolution Sea Surface Temperature (GHRSST) project, and is a joint collaboration between the NASA Jet Propulsion Laboratory (JPL), the NASA Ocean Biology Processing Group (OBPG), and the Rosenstiel School of Marine and Atmospheric Science (RSMAS). Researchers at RSMAS are responsible for SST algorithm development, error statistics and quality flagging, while the OBPG, as the NASA ground data system, is responsible for the production of daily MODIS ocean products. JPL acquires MODIS ocean granules from the OBPG and reformats them to the GHRSST L2P netCDF specification with complete metadata and ancillary variables, and distributes the data as the official Physical Oceanography Data Archive (PO.DAAC) for SST.  The R2019.0 supersedes the previous R2014.0 datasets which can be found at  &lt;a href&#x3D;&quot;https://doi.org/10.5067/GHMDT-2PJ02&quot;&gt;https://doi.org/10.5067/GHMDT-2PJ02&lt;/a&gt;
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://archive.podaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;https://archive.podaac.earthdata.nasa.gov/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>GPM DPR Precipitation Profile L2A 1.5 hours 5 km V07 (GPM_2ADPR) at GES DISC</title>
      <link>https://registry.opendata.aws/nasa-gpm2adpr</link>
      <guid>https://registry.opendata.aws/nasa-gpm2adpr</guid>
      <description>Version 07 is the current version of the data set. Older versions will no longer be available and have been superseded by Version 07.
.2ADPR provides single- and dual-frequency-derived precipitation estimates from the Ku and Ka radars of the Dual-Frequency Precipitation Radar (DPR) on the core GPM spacecraft. The output consists of three main classes of precipitation products: those derived from the Ku-band frequency over a wide swath (245 km), those derived from the Ka-band frequency over a narrow swath (125 km), and those derived from the dual-frequency data over the narrow swath. The Ka-band results are further divided into the standard and high-sensitivity estimates. In the standard sensitivity mode, the fields of view within the inner swath are matched to those of the Ku-band. Data from these matched-beam Ku- and Ka-band fields of view are used to derive the dual-frequency precipitation products. The retrievals are performed at each radar range bin along the slant path of the radar instrument field of view (IFOV).
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>Genomic Characterization of Metastatic Castration Resistant Prostate Cancer</title>
      <link>https://registry.opendata.aws/mcrpc</link>
      <guid>https://registry.opendata.aws/mcrpc</guid>
      <description>Biopsies of castration resistant prostate cancer metastases were subjected to whole genome sequencing (WGS), along with RNA-sequencing (RNA-Seq). The overarching goal of the study is to illuminate molecular mechanisms of acquired resistance to therapeutic agents, and particularly androgen signaling inhibitors, in the treatment of metastatic castration resistant prostate cancer (mCRPC). This study is made available on AWS via the NIH STRIDES Initiative.</description>
    </item>
    <item>
      <title>Genoxus Annotation</title>
      <link>https://registry.opendata.aws/genoxus-annotation</link>
      <guid>https://registry.opendata.aws/genoxus-annotation</guid>
      <description>Genoxus Annotation is a harmonized and curated collection of human genetic variant databases designed to support accurate and salable variant annotation. Variant annotation following genetic testing such as whole genome sequencing (WGS) or whole exome sequencing (WES) is a critical step in identifying and interpreting disease-associated genetic factors. As sequencing technologies continue to generate large volumes of genomic data, robust and well-structured annotation resources are essential for translating raw variant calls into clinically meaningful insights.
Genoxus Annotation v1.0 integrates data from NCBI ClinVar. ClinVar provides curated information on the clinical significance of a broad spectrum of genetic variants including single nucleotide variants (SNVs), insertions (INS), deletions (DEL), INDELs, copy number variations (CNVs), and structural variants (SVs) along with their associated diseases and traits.
GWAS catalog complements ClinVar by focusing primarily on SNVs identified through genome wide association studies, linking common variants to complex diseases and phenotype traits. (GWAS data is planned in a future release.) By harmonizing variant representations, standardizing disease terminology, and consolidating evidence across sources, Genoxus Annotation provides a unified framework that streamlines variant interpretation for research and clinical applications.</description>
    </item>
    <item>
      <title>Harvard Electroencephalography Database</title>
      <link>https://registry.opendata.aws/bdsp-harvard-eeg</link>
      <guid>https://registry.opendata.aws/bdsp-harvard-eeg</guid>
      <description>The Harvard EEG Database will encompass data gathered from four hospitals affiliated with Harvard University:Massachusetts General Hospital (MGH), Brigham and Women&amp;#39;s Hospital (BWH), Beth Israel Deaconess Medical Center (BIDMC), and Boston Children&amp;#39;s Hospital (BCH).</description>
    </item>
    <item>
      <title>Harvard-Emory ECG Database</title>
      <link>https://registry.opendata.aws/bdsp-heedb</link>
      <guid>https://registry.opendata.aws/bdsp-heedb</guid>
      <description>The Harvard-Emory ECG database (HEEDB) is a large collection of 12-lead electrocardiography (ECG) recordings, prepared through a collaboration between Harvard University and Emory University investigators.</description>
    </item>
    <item>
      <title>Hecatomb Databases</title>
      <link>https://registry.opendata.aws/hecatomb</link>
      <guid>https://registry.opendata.aws/hecatomb</guid>
      <description>Preprocessed databases for use with the Hecatomb pipeline for viral and phage sequence annotation.</description>
    </item>
    <item>
      <title>Human Cell Atlas</title>
      <link>https://registry.opendata.aws/humancellatlas</link>
      <guid>https://registry.opendata.aws/humancellatlas</guid>
      <description>The Human Cell Atlas (HCA) is a collaborative community of international scientists. Our mission is to create comprehensive reference maps of all the cells in the human body as a basis for both understanding human health and diagnosing, monitoring, and treating disease. The HCA registry has more than one thousand member scientists from hundreds of institutions around the world. The project is steered and governed by an Organizing Committee, co-chaired by Aviv Regev and Sarah Teichmann.</description>
    </item>
    <item>
      <title>IWMI DIWASA Blue ET for Africa</title>
      <link>https://registry.opendata.aws/blue_et</link>
      <guid>https://registry.opendata.aws/blue_et</guid>
      <description>Blue evapotranspiration (Blue ET) is the portion of ET derived from blue water sources, including surface water (rivers, lakes, reservoirs) and groundwater used for irrigation. It is a key component of blue water fluxes in water accounting. Blue ET consists of evaporation from irrigated fields, transpiration from irrigated crops, and water lost from artificial storage. It helps assess water productivity in irrigated agriculture, quantify consumptive water use, and support sustainable water resource management, particularly in water-scarce regions.</description>
    </item>
    <item>
      <title>Indexes for Kaiju</title>
      <link>https://registry.opendata.aws/kaiju-indexes</link>
      <guid>https://registry.opendata.aws/kaiju-indexes</guid>
      <description>This dataset comprises pre-built indexes for the bioinformatics software Kaiju, which is used for taxonomic classification of metagenomic sequencing data. Various indexes for different source reference databases are available.</description>
    </item>
    <item>
      <title>Indian Supreme Court Judgments</title>
      <link>https://registry.opendata.aws/indian-supreme-court-judgments</link>
      <guid>https://registry.opendata.aws/indian-supreme-court-judgments</guid>
      <description>This dataset contains judgements from the Indian Supreme Court, downloaded from ecourts website. It contains judgments from 1950 to 2025, along with raw metadata (in json format) and structured metadata in parquet format. Judgments are available in both English and regional Indian languages in zip format for easier download.</description>
    </item>
    <item>
      <title>Integrative Analysis of Lung Adenocarcinoma in Environment and Genetics Lung cancer Etiology (Phase 2)</title>
      <link>https://registry.opendata.aws/luad-eagle</link>
      <guid>https://registry.opendata.aws/luad-eagle</guid>
      <description>We performed whole genome sequencing and whole exome sequencing of 31 lung adenocarcinoma (LUAD) samples from the Environment And Genetics in Lung cancer Etiology (EAGLE) study. The EAGLE study is made available on AWS via the NIH STRIDES Initiative (&lt;a href&#x3D;&quot;https://aws.amazon.com/blogs/publicsector/aws-and-national-institutes-of-health-collaborate-to-accelerate-discoveries-with-strides-initiative/&quot;&gt;https://aws.amazon.com/blogs/publicsector/aws-and-national-institutes-of-health-collaborate-to-accelerate-discoveries-with-strides-initiative/&lt;/a&gt;).</description>
    </item>
    <item>
      <title>James Webb Space Telescope (JWST)</title>
      <link>https://registry.opendata.aws/mast-jwst</link>
      <guid>https://registry.opendata.aws/mast-jwst</guid>
      <description>The James Webb Space Telescope (JWST) is the world&amp;#39;s next flagship infrared observatory led by NASA with its partners, ESA (European Space Agency), and CSA (Canadian Space Agency). JWST offers scientists the opportunity to observe galaxy evolution, the formation of stars and planets, exoplanetary systems, and our own solar system, in ways never before possible.</description>
    </item>
    <item>
      <title>LEarning biOchemical Prostate cAncer Recurrence from histopathology sliDes challenge (LEOPARD) Dataset</title>
      <link>https://registry.opendata.aws/leopard</link>
      <guid>https://registry.opendata.aws/leopard</guid>
      <description>&amp;quot;This dataset contains the all data for the &lt;a href&#x3D;&quot;https://leopard.grand-challenge.org/&quot;&gt;LEarning biOchemical Prostate cAncer Recurrence from histopathology sliDes challenge or LEOPARD&lt;/a&gt;.Prostate cancer, impacting 1.4 million men annually, is a prevalent malignancy (&lt;a href&#x3D;&quot;https://acsjournals.onlinelibrary.wiley.com/doi/10.3322/caac.21660&quot;&gt;H. Sung et al., 2021&lt;/a&gt;). A substantial number of these individuals undergo prostatectomy as the primary curative treatment. The efficacy of this surgery is assessed, in part, by monitoring the concentration of prostate-specific antigen (PSA) in the bloodstream. While the role of PSA in prostate cancer screening is debatable (&lt;a href&#x3D;&quot;https://jamanetwork.com/journals/jama/fullarticle/2680553&quot;&gt;W. F. Clark et al., 2018;&lt;/a&gt; &lt;a href&#x3D;&quot;https://onlinelibrary.wiley.com/doi/full/10.1002/ijc.31102&quot;&gt;E. A. M. Heijnsdijk et al., 2018&lt;/a&gt;), it serves as a valuable biomarker for postprostatectomy follow-up in patients. Following successful surgery, PSA concentration is typically undetectable (&amp;lt;0.1 ng/mL) within 4-6 weeks (&lt;a href&#x3D;&quot;https://wchh.onlinelibrary.wiley.com/doi/abs/10.1002/tre.407&quot;&gt;S. S. Goonewardene et al., 2014&lt;/a&gt;). However, approximately 30% of patients experience biochemical recurrence, signifying the resurgence of prostate cancer cells. This recurrence serves as a prognostic indicator for progression to clinical metastases and eventual prostate cancer-related mortality (&lt;a href&#x3D;&quot;https://pubmed.ncbi.nlm.nih.gov/10840432/&quot;&gt;C. L. Amling, 2014;&lt;/a&gt; &lt;a href&#x3D;&quot;https://jamanetwork.com/journals/jama/fullarticle/201291&quot;&gt;S. J. Freedland et al., 2005;&lt;/a&gt; &lt;a href&#x3D;&quot;https://www.sciencedirect.com/science/article/abs/pii/S0094014305701634?via%3Dihub&quot;&gt;M. Han et al., 2001;&lt;/a&gt; &lt;a href&#x3D;&quot;https://www.sciencedirect.com/science/article/pii/S0302283818307528?via%3Dihub&quot;&gt;T. Van den Broeck et al., 2001&lt;/a&gt;. Current clinical practices gauge the risk of biochemical recurrence by considering the International Society of Urological Pathology (ISUP) grade, PSA value at diagnosis, and TNM staging criteria (&lt;a href&#x3D;&quot;https://journals.lww.com/ajsp/abstract/2016/02000/the_2014_international_society_of_urological.10.aspx&quot;&gt;J. I. Epstein et al., 2016&lt;/a&gt;). A recent European consensus guideline suggests categorizing patients into low-risk, intermediate-risk, and high-risk groups based on these factors (&lt;a href&#x3D;&quot;https://www.sciencedirect.com/science/article/abs/pii/S0302283820307697?via%3Dihub&quot;&gt;N. Mottet et al., 2021&lt;/a&gt;). Notably, a high ISUP grade independently assigns a patient to the intermediate (grade 2/3) or high-risk group (grade 4/5). The Gleason growth patterns, representing morphological patterns of prostate cancer, are used to categorize cancerous tissue into ISUP grade groups (&lt;a href&#x3D;&quot;https://www.auajournals.org/doi/10.1016/j.juro.2009.10.046&quot;&gt;J. I. Epstein, 2010;&lt;/a&gt; &lt;a href&#x3D;&quot;https://bjui-journals.onlinelibrary.wiley.com/doi/10.1111/j.1464-410X.2012.11611.x&quot;&gt;P. M. Pierorazio et al., 2013;&lt;/a&gt; &lt;a href&#x3D;&quot;https://journals.lww.com/ajsp/fulltext/2020/08000/the_2019_international_society_of_urological.1.aspx&quot;&gt;G. J. L. H. van Leenders et al., 2020;&lt;/a&gt; &lt;a href&#x3D;&quot;https://www.sciencedirect.com/science/article/abs/pii/S0302283815005576?via%3Dihub&quot;&gt;J. I. Epstein et al., 2016&lt;/a&gt;). However, the ISUP grade has limitations, such as grading disagreement among pathologists (&lt;a href&#x3D;&quot;https://www.sciencedirect.com/science/article/abs/pii/S0302283815005576?via%3Dihub&quot;&gt;J. I. Epstein et al., 2016&lt;/a&gt;) and coarse descriptors of tissue morphology. Recently, deep learning was shown (&lt;a href&#x3D;&quot;https://www.nature.com/articles/s43856-022-00126-3&quot;&gt;H. Pinckaers et al., 2022&lt;/a&gt;; &lt;a href&#x3D;&quot;https://www.nature.com/articles/s44303-023-00005-z&quot;&gt;O. Eminaga et. al., 2024&lt;/a&gt;) to be able to predict the biochemical recurrence of prostate cancer.  Hypothesizing that deep learning could uncover finer morphological features&amp;#39; prognostic value, we are organizing the LEarning biOchemical Prostate cAncer Recurrence from histopathology sliDes (LEOPARD) challenge. The goal of this challenge is to yield top-performance deep learning solutions to predict the time to biochemical recurrence from H&amp;amp;E-stained histopathological tissue sections, i.e. based on morphological features.</description>
    </item>
    <item>
      <title>Multi-Anatomy Post-Surgical Magnetic Resonance Dataset (MAPSMR)</title>
      <link>https://registry.opendata.aws/gehcai-mapsmr</link>
      <guid>https://registry.opendata.aws/gehcai-mapsmr</guid>
      <description>The MAPSMR dataset is a multi-organ, post-surgical MRI benchmark dataset focused on organ absence and altered anatomy after common abdominal and pelvic surgeries. The dataset includes cases such as cholecystectomy, prostatectomy, nephrectomy, colectomy, hepatectomy, and related procedures, with annotations identifying surgically absent organs and post-treatment anatomical changes.</description>
    </item>
    <item>
      <title>NASA Physical Sciences Informatics (PSI)</title>
      <link>https://registry.opendata.aws/nasa-psi</link>
      <guid>https://registry.opendata.aws/nasa-psi</guid>
      <description>NASA&amp;#39;s Physical Sciences Research Program, along with its predecessors, has conducted significant fundamental and applied research in the physical sciences. The International Space Station (ISS) is an orbiting laboratory that provides an ideal facility to conduct long-duration experiments in the near absence of gravity and allows continuous and interactive research similar to Earth-based laboratories. This enables scientists to pursue innovations and discoveries not currently achievable by other means. NASA&amp;#39;s Physical Sciences Research Program also benefits from collaborations with several of the ISS international partners—Europe, Russia, Japan, and Canada—and foreign governments with space programs, such as France, Germany and Italy. &lt;br/&gt;&lt;br/&gt; In fulfillment of the Open Science model, NASA&amp;#39;s Physical Sciences Research Program is pleased to offer the PSI data repository for physical science experiments performed in reduced-gravity environments such as the ISS, Space Shuttle flights, and Free-flyers. PSI also includes data from some related ground-based studies. The PSI system is accessible and open to the public. This provides the opportunity for researchers to data mine results from prior flight investigations, expanding on the research performed. This approach will allow numerous ground-based investigations to be conducted from one flight experiment’s data, exponentially increasing our body of knowledge. PSI is an Open Data initiative.</description>
    </item>
    <item>
      <title>NIH NLM NCBI PubMed Central (PMC) Article Datasets - Full-Text Biomedical and Life Sciences Journal Articles on AWS</title>
      <link>https://registry.opendata.aws/ncbi-pmc</link>
      <guid>https://registry.opendata.aws/ncbi-pmc</guid>
      <description>PubMed Central® (PMC) is a free full-text archive of biomedical and life sciences journal article at the U.S. National Institutes of Health&amp;#39;s National Library of Medicine (NIH/NLM). The PubMed Central (PMC) Article Datasets include full-text articles archived in PMC and made available under license terms that allow for text mining and other types of secondary analysis and reuse. The articles are organized on AWS based on PMCID and version number:&lt;br/&gt;&lt;br/&gt;
The PMC Open Access (OA) Subset, which includes all articles in PMC that are available for reuse based on terms specified by the publisher. The majority of available articles have machine-readable Creative Commons license&lt;br/&gt;&lt;br/&gt; The Author Manuscript Dataset, which includes all articles collected under a funder policy in PMC and made available in machine-readable formats for text mining. NOTEL Author manuscripts with Creative Commons licenses are also part of the PMC Open Access Subset.&lt;br/&gt;&lt;br/&gt; The Historical OCR Dataset, which includes historical articles, published in the 18th, 19th, and 20th centuries, scanned as part of an NLM digitization project, that have Creative Commons licenses. NOTE: These articles are also part of the PMC Open Access Subset.&lt;br/&gt;&lt;br/&gt;
These datasets collectively span more than half of PMC&amp;#39;s total collection of full-text articles. PMC enables access to these datasets to expand the impact of open access and publicly-funded research; enable greater machine learning across the spectrum of scientific research; reach new audiences; and open new doors for discovery. The bucket in this registry contains individual article versions in NISO Z39.96-2015 JATS XML format as well as in plain text as extracted from the XML and the full article PDF. Media files and supplementary material files are also available for all open access articles. The bucket is updated continuously with new and updated articles. Also includes JSON metadata objects for each article version and a CVS inventory file.</description>
    </item>
    <item>
      <title>NOAA Analysis of Record for Calibration (AORC) Dataset</title>
      <link>https://registry.opendata.aws/noaa-nws-aorc</link>
      <guid>https://registry.opendata.aws/noaa-nws-aorc</guid>
      <description>&lt;h4&gt;Announcements:&lt;/h4&gt;
April 2, 2026: The Office of Water Prediction (OWP) has identified some brittle components of the AORC data processing pipelines that, by our estimations, have resulted in 0.04% of all available rows being incorrectly masked. We&#x27;ve resolved the issue and we are currently regenerating the Zarr files to ensure a complete record. We will post an updated announcement once the corrected data is posted.
&lt;br/&gt;
&lt;br/&gt;
The Analysis Of Record for Calibration (AORC) is a gridded record of near-surface  weather conditions covering the continental United States and Alaska and their  hydrologically contributing areas. It is defined on a latitude/longitude spatial grid with a mesh length of 30 arc seconds (~800 m), and a temporal resolution of one hour.  Elements include hourly total precipitation, temperature, specific humidity, terrain-level  pressure, downward longwave and shortwave radiation, and west-east and south-north wind components. It spans the period from 1979 across the Continental U.S. (CONUS) and from 1981 across Alaska, to the near-present (at all locations). This suite of eight variables is sufficient to drive most land-surface and hydrologic models and is used as input to the National Water Model (NWM) retrospective simulation. While the native AORC process generates netCDF output, the data is post-processed to create a cloud optimized Zarr formatted equivalent for dissemination using cloud technology and infrastructure.
&lt;br/&gt;
&lt;br/&gt;
**AORC Version 1.1 dataset creation**
&lt;br/&gt;
The AORC dataset was created after reviewing, identifying, and processing multiple large-scale, observation, and analysis datasets. There are two versions of The Analysis Of Record for Calibration (AORC) data.
&lt;br/&gt;
&lt;br/&gt;
The initial AORC Version 1.0 dataset was completed in November 2019 and consisted of a grid with 8 elements at a resolution of 30 arc seconds.  The AORC version 1.1 dataset was created to address issues &quot;[see Table 1 in Fall et al., 2023](https://onlinelibrary.wiley.com/doi/10.1111/1752-1688.13143)&quot; in the version 1.0 CONUS dataset. Full documentation on version 1.1 of the AORC data and the related journal publication are provided below.
&lt;br/&gt;
&lt;br/&gt;
The native AORC version 1.1 process creates a dataset that consists of netCDF files with the following dimensions: 1 hour, 4201 latitude values (ranging from 25.0 to 53.0), and 8401 longitude values (ranging from -125.0 to -67).
&lt;br/&gt;
&lt;br/&gt;
The data creation runs with a 10-day lag to ensure the inclusion of any corrections to the input Stage IV and NLDAS data.
&lt;br/&gt;
&lt;br/&gt;
**Note** - The full extent of the AORC grid as defined in its data files exceed those cited above; those outermost rows and columns of data grids are filled with missing values and are the remnant of an early set of required AORC extents that have since been adjusted inward.
&lt;br/&gt;
&lt;br/&gt;
**AORC Version 1.1 Zarr Conversion**
&lt;br/&gt;
&lt;br/&gt;
The goal for converting the AORC data from netCDF to Zarr was to allow users to quickly and efficiently load/use the data.  For example, one year of data takes 28 mins to load via NetCDF while only taking 3.2 seconds to load via Zarr (resulting in a substantial increase in speed).  For longer periods of time, the percentage increase in speed using Zarr (vs NetCDF) is even higher.  Using Zarr also leads to less memory and CPU utilization.
&lt;br/&gt;
&lt;br/&gt;
It was determined that the optimal conversion for the data was 1 year worth of Zarr files with a chunk size of 18MB. The chunking was completed across all 8 variables.  The chunks consist of the following dimensions: 144 time, 128 latitude, and 256 longitude. To create the files in the Zarr format, the NetCDF files were rechunked using chunk() and &quot;[Xarray](https://docs.xarray.dev/en/stable/)&quot;.  After chunking the files, they were converted to a monthly Zarr file. Then, each monthly Zarr file was combined using &quot;[to_zarr](https://docs.xarray.dev/en/latest/generated/xarray.Dataset.to_zarr.html)&quot; to create a Zarr file that represents a full year
&lt;br/&gt;
&lt;br/&gt;
Users wanting more than 1 year of data will be able to utilize Zarr utilities/libraries to combine multiple years up to the span of the full data set.
&lt;br/&gt;
&lt;br/&gt;
There are eight variables representing the meteorological conditions
&lt;br/&gt;
**Total Precipitaion (APCP_surface)**
&lt;br/&gt;
1) Hourly total precipitation (kgm-2 or mm)  for Calibration (AORC) dataset
&lt;br/&gt;
**Air Temperature (TMP_2maboveground)**
1) Temperature (at 2 m above-ground-level (AGL)) (K)
&lt;br/&gt;
**Specific Humidity (SPFH_2maboveground)**
&lt;br/&gt;
1) Specific humidity (at 2 m AGL) (g g-1) 
&lt;br/&gt;
**Downward Long-Wave Radiation Flux (DLWRF_surface)**
&lt;br/&gt;
1) longwave (infrared)
2) radiation flux (at the  surface) (W m-2) 
&lt;br/&gt;
**Downward Short-Wave Radiation Flux (DSWRF_surface)**
&lt;br/&gt;
1) Downward shortwave (solar)
2) radiation flux (at the  surface) (W m-2)
&lt;br/&gt;
**Pressure (PRES_surface)**
&lt;br/&gt;
1) Air pressure (at the surface) (Pa)
&lt;br/&gt;
**U-Component of Wind (UGRD_10maboveground)&quot;
&lt;br/&gt;
1)U (west-east) - components of the wind (at 10 m AGL) (m s-1)
&lt;br/&gt;
**V-Component of Wind (VGRD_10maboveground)&quot;
&lt;br/&gt;
1) V (south-north) - components of the wind (at 10 m AGL) (m s-1)
&lt;br/&gt;
&lt;br/&gt;
**Precipitation and Temperature**
&lt;br/&gt;
&lt;br/&gt;
The gridded AORC precipitation dataset contains one-hour Accumulated Surface Precipitation (APCP) ending at the “top” of each hour, in liquid water-equivalent units  (kg m-2 to the nearest 0.1 kg m-2), while the gridded AORC temperature dataset is comprised of instantaneous, 2 m above-ground-level (AGL) temperatures at the top of each hour (in Kelvin, to the nearest 0.1).
&lt;br/&gt;
&lt;br/&gt;
**Specific Humidity, Pressure, Downward Radiation, Wind**
&lt;br/&gt;
&lt;br/&gt;
The development process for the six additional dataset components of the Conus AORC [i.e., specific humidity at 2m above ground (kg kg-1); downward  longwave and shortwave radiation fluxes at the surface (W m-2); terrain-level pressure (Pa); and west-east and south-north wind components at 10 m above ground (m s-1)] has  two distinct periods, based on datasets and methodology applied: 1979–2015 and 2016–present. 
</description>
    </item>
    <item>
      <title>NOAA Climate Forecast System (CFS)</title>
      <link>https://registry.opendata.aws/noaa-cfs</link>
      <guid>https://registry.opendata.aws/noaa-cfs</guid>
      <description>The Climate Forecast System (CFS) is a model representing the global interaction between Earth&amp;#39;s oceans, land, and atmosphere. Produced by several dozen scientists under guidance from the National Centers for Environmental Prediction (NCEP), this model offers hourly data with a horizontal resolution down to one-half of a degree (approximately 56 km) around Earth for many variables. CFS uses the latest scientific approaches for taking in, or assimilating, observations from data sources including surface observations, upper air balloon observations, aircraft observations, and satellite observations. &lt;br /&gt; Please note that the data in this bucket are the CFSv2 Operational Forecasts. To obtain other CFSv2 products such as the Operational Analysis, please visit our &lt;a href&#x3D;&quot;https://www.ncdc.noaa.gov/data-access/model-data/model-datasets/climate-forecast-system-version2-cfsv2&quot;&gt;website&lt;/a&gt;.</description>
    </item>
    <item>
      <title>NOAA GEFS - dynamical.org Icechunk Zarr</title>
      <link>https://registry.opendata.aws/dynamical-noaa-gefs</link>
      <guid>https://registry.opendata.aws/dynamical-noaa-gefs</guid>
      <description>&lt;p&gt;The Global Ensemble Forecast System (GEFS) is a National Oceanic and Atmospheric Administration (NOAA) National Centers for Environmental Prediction (NCEP) weather forecast model. GEFS creates 31 separate forecasts (ensemble members) to describe the range of forecast uncertainty.&lt;/p&gt;
&lt;p&gt;These datasets have been translated to cloud-optimized Icechunk Zarr format by &lt;a href&#x3D;&quot;https://dynamical.org&quot;&gt;dynamical.org&lt;/a&gt;.&lt;/p&gt;
&lt;ul&gt;
  &lt;li&gt;&lt;a href&#x3D;&quot;https://dynamical.org/catalog/noaa-gefs-forecast-35-day/&quot;&gt;NOAA GEFS forecast, 35 day&lt;/a&gt; - Weather forecasts from the Global Ensemble Forecast System (GEFS) operated by NOAA NWS NCEP.&lt;/li&gt;
  &lt;li&gt;&lt;a href&#x3D;&quot;https://dynamical.org/catalog/noaa-gefs-analysis/&quot;&gt;NOAA GEFS analysis&lt;/a&gt; - Weather analysis from the Global Ensemble Forecast System (GEFS) operated by NOAA NWS NCEP.&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>NOAA Global Forecast System (GFS) netCDF Formatted Data</title>
      <link>https://registry.opendata.aws/noaa-oar-arl-nacc-pds</link>
      <guid>https://registry.opendata.aws/noaa-oar-arl-nacc-pds</guid>
      <description>The Global Forecast System (GFS) is a weather forecast model produced by the National Centers for Environmental Prediction (NCEP). Dozens of atmospheric and land-soil variables are available through this dataset, from temperatures, winds, and precipitation to soil moisture and atmospheric ozone concentration. The GFS data files stored here can be immediately used for &lt;a href&#x3D;&quot;https://www.arl.noaa.gov/research/surface-atmosphere-exchange-home/tools-and-products/nacc-nacc-cloud/&quot;&gt;OAR/ARL’s NOAA-EPA Atmosphere-Chemistry Coupler Cloud (NACC-Cloud) tool&lt;/a&gt;, and are in a Network Common Data Form (netCDF), which is a very common format used across the scientific community. These particular GFS files contain a comprehensive number of global atmosphere/land variables at a relatively high spatiotemporal resolution (approximately 13x13 km horizontal, vertical resolution of 127 levels, and hourly), are not only necessary for the NACC-Cloud tool to adequately drive community air quality applications (e.g., U.S. EPA’s Community Multiscale Air Quality model; &lt;a href&#x3D;&quot;https://www.epa.gov/cmaq&quot;&gt;https://www.epa.gov/cmaq&lt;/a&gt;), but can be very useful for a myriad of other applications in the Earth system modeling communities (e.g., atmosphere, hydrosphere, pedosphere, etc.). While many other data file and record formats are indeed available for Earth system and climate research (e.g., GRIB, HDF, GeoTIFF), the netCDF files here are advantageous to the larger community because of the comprehensive, high spatiotemporal information they contain, and because they are more scalable, appendable, shareable, self-describing, and community-friendly (i.e., many tools available to the community of users).  Out of the four operational GFS forecast cycles per day (at 00Z, 06Z, 12Z and 18Z) this particular netCDF dataset is updated daily (/inputs/yyyymmdd/) for the 12Z cycle and includes 24-hr output for both 2D (gfs.t12z.sfcf$0hh.nc) and 3D variables (gfs.t12z.atmf$0hh.nc).
&lt;br/&gt;
&lt;br/&gt;
Also available are netCDF formatted Global Land Surface Datasets (GLSDs) developed by &lt;a href&#x3D;&quot;https://repository.library.noaa.gov/view/noaa/65705&quot;&gt;Hung et al&lt;/a&gt;. (2024).  The GLSDs are based on numerous satellite products, and have been gridded to match the GFS spatial resolution (~13x13 km).  These GLSDs contain vegetation canopy data (e.g., land surface type, vegetation clumping index, leaf area index, vegetative canopy height, and green vegetation fraction) that are supplemental to and can be combined with the GFS meteorological netCDF data for various applications, including &lt;a href&#x3D;&quot;https://github.com/noaa-oar-arl/canopy-app&quot;&gt;NOAA-ARL&amp;#39;s canopy-app&lt;/a&gt;.  The canopy data variables are climatological, based on satellite data from the year 2020, combined with GFS meteorology for the year 2022, and are created at a daily temporal resolution (/inputs/geo-files/gfs.canopy.t12z.2022mmdd.sfcf000.global.nc)
&lt;br/&gt;</description>
    </item>
    <item>
      <title>NOAA HRRR - dynamical.org Icechunk Zarr</title>
      <link>https://registry.opendata.aws/dynamical-noaa-hrrr</link>
      <guid>https://registry.opendata.aws/dynamical-noaa-hrrr</guid>
      <description>&lt;p&gt;The High-Resolution Rapid Refresh (HRRR) is a NOAA real-time 3-km resolution, hourly updated, cloud-resolving, convection-allowing atmospheric model, initialized by 3km grids with 3km radar assimilation. Radar data is assimilated in the HRRR every 15 min over a 1-h period adding further detail to that provided by the hourly data assimilation from the 13km radar-enhanced Rapid Refresh.&lt;/p&gt;
&lt;p&gt;These datasets have been translated to cloud-optimized Icechunk Zarr format by &lt;a href&#x3D;&quot;https://dynamical.org&quot;&gt;dynamical.org&lt;/a&gt;.&lt;/p&gt;
&lt;ul&gt;
  &lt;li&gt;&lt;a href&#x3D;&quot;https://dynamical.org/catalog/noaa-hrrr-forecast-48-hour/&quot;&gt;NOAA HRRR forecast, 48 hour&lt;/a&gt; - Weather forecasts from the High-Resolution Rapid Refresh (HRRR) model operated by NOAA NWS NCEP.&lt;/li&gt;
  &lt;li&gt;&lt;a href&#x3D;&quot;https://dynamical.org/catalog/noaa-hrrr-analysis/&quot;&gt;NOAA HRRR analysis&lt;/a&gt; - Analysis data from the High-Resolution Rapid Refresh (HRRR) model operated by NOAA NWS NCEP.&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>NOAA JISAO’s Seasonal Coastal Ocean Prediction of the Ecosystem (J-SCOPE)</title>
      <link>https://registry.opendata.aws/noaa-jscope</link>
      <guid>https://registry.opendata.aws/noaa-jscope</guid>
      <description>J-SCOPE (JISAO’s Seasonal Coastal Ocean Prediction of the Ecosystem) is funded by NOAA and presented by NANOOS. This project aims to provide experimental seasonal forecasts (six to nine months) of upper ocean properties, based on operational simulations by NOAA&amp;#39;s Climate Forecast System (CFS) model, and dynamical downscaling with a high-resolution version of the Regional Ocean Model System (ROMS) that includes a state-of-the-art biogeochemical module. Forecasts of specific oceanic properties crucial to the nearshore and coastal marine ecosystem such as upwelling, pH, mixed layer depth, oxygen concentration and plankton distributions are anticipated with updates on a monthly basis. For more information about the forecast system, please read &lt;a href&#x3D;&quot;https://www.nature.com/articles/srep27203&quot;&gt;Siedlecki et al. 2016&lt;/a&gt;.The Regional Ocean Modeling System (ROMS; Rutgers version 3) is configured for the Washington and Oregon coasts after &lt;a href&#x3D;&quot;https://agupubs.onlinelibrary.wiley.com/doi/full/10.1002/2013JC009622&quot;&gt;Giddings et al&lt;/a&gt;. More information about ROMS can be found &lt;a href&#x3D;&quot;https://www.myroms.org/&quot;&gt;here&lt;/a&gt;. The Cascadia domain was developed by the Coastal Modeling Group at the UW is roughly 1.5 km in resolution. More information about the model physics can be found &lt;a href&#x3D;&quot;https://scripps.ucsd.edu/iod&quot;&gt;here&lt;/a&gt;. Our implementation of ROMS includes 17 rivers forced with daily river discharge and temperature data from the USGS gauging stations and an Environment Canada gauging station for the Fraser River as described by &lt;a href&#x3D;&quot;https://agupubs.onlinelibrary.wiley.com/doi/full/10.1002/2013JC009622&quot;&gt;Giddings et al&lt;/a&gt;. Tides are included. Water entering the domain at the southern and western boundaries is supplied by CFS. Empirical relationships were derived relating nutrients and oxygen to salinity from the observations of Connolly et al (2010) as described by &lt;a href&#x3D;&quot;https://agupubs.onlinelibrary.wiley.com/doi/full/10.1002/2014JC010248&quot;&gt;Davis et al&lt;/a&gt; and &lt;a href&#x3D;&quot;https://agupubs.onlinelibrary.wiley.com/doi/full/10.1002/2014JC010254&quot;&gt;Siedlecki et al&lt;/a&gt;. The rivers enter the domain with constant saturated values of oxygen and a seasonal cycle for nutrients from a climatology of USGS gauging stations data described by &lt;a href&#x3D;&quot;https://agupubs.onlinelibrary.wiley.com/doi/full/10.1002/2014JC010248&quot;&gt;Davis et al&lt;/a&gt;. In the hindcast simulations, the rivers are based on observed streamflows, but in the re-forecast and forecast runs, the rivers are forced using a climatology of local river discharge data over seven years (2000-2007).
&lt;br&gt;&lt;br&gt;
The forecast system predicts the sea-surface temperature (SST), chlorophyll stock, dissolved oxygen concentration, carbon variables, and sardine as well as hake habitat. Each forecast is composed of three model runs that make up an ensemble. Each model run is initialized at a different time within the initialization month (for April, for example, April 6, April 15, April 25), and has complementary forcing files from the large scale model, &lt;a href&#x3D;&quot;https://www.nanoos.org/products/j-scope/about_the_model.php&quot;&gt;CFS&lt;/a&gt;. J-SCOPE produces January, April, and September initialized forecasts annually.
&lt;br&gt;&lt;br&gt;
The details of the wind forcing for each model run can be found on the California Current Indicators tab. For each of the predicted quantities listed above, we report the ensemble average anomaly as well as the relative uncertainty within the ensemble, which is defined as the standard deviation of the ensemble divided by the mean of the ensemble and is reported as a percentage of the mean. All of these quantities are reported as monthly averaged anomalies from our April-initialized reforecast &lt;a href&#x3D;&quot;https://www.nanoos.org/products/j-scope/climatology.php?climatology&#x3D;apr_init&quot;&gt;climatology&lt;/a&gt;, which spans 2009-2017. An anomaly is an indication of how different conditions are to what they have been in the past. For more information about anomalies, please see the &lt;a href&#x3D;&quot;https://nvs.nanoos.org/AveragesAnomalies&quot;&gt;NANOOS Climatology App&lt;/a&gt;. These predicted quantities are key indicators for the &lt;a href&#x3D;&quot;https://www.integratedecosystemassessment.noaa.gov/regions/california-current&quot;&gt;California Current Integrated Ecosystem Assessment report&lt;/a&gt;.
&lt;br&gt;&lt;br&gt;
J-SCOPE has also been run as a re-forecast and a hindcast each spanning 1998 to present and also rely on CFS forcing. The re-forecasts extend to 2013 when the true forecasts began.  The historical output is available daily while the re-forecasts and forecasts are available as monthly averages. The historical simulation is used to evaluate the Year-in Review and is released after the year is over in the early part of the following year. 
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NOAA S-104 Water Level Data</title>
      <link>https://registry.opendata.aws/noaa-s104</link>
      <guid>https://registry.opendata.aws/noaa-s104</guid>
      <description>S-104 is a data and metadata encoding specification that is part of the &lt;a href&#x3D;&quot;https://iho.int/en/s-100-universal-hydrographic-data-model&quot;&gt;S-100 Universal Hydrographic Data Model&lt;/a&gt;, an international standard for hydrographic data. This collection of data contains water level forecast guidance from &lt;a href&#x3D;&quot;https://polar.ncep.noaa.gov/estofs/&quot;&gt;NOAA&amp;#39;s Global Surge and Tide Operational Forecast System 2-D (STOFS-2D-Global)&lt;/a&gt;, an operational hydrodynamic nowcast and forecast modeling system for global water level conditions. These datasets are encoded as HDF-5 files conforming to the S-104 specification, and are geospatially subset into individual tiles conforming to the NOAA/OCS Nautical Product Tiling Scheme, with filenames indicating the corresponding NOAA Electronic Navigational Chart (ENC) Cell Identifier. A set of prototype S-104 tiles has been created for the Charleston, SC area for a select model run cycle. Each individual S-104 (HDF-5) file contains all forecast projections from a single model run for that geographic area. A single S-104 file will contain multiple gridded arrays each containing a forecast valid at a distinct time in the future, out to the forecast horizon of STOFS-2D-Global, which is 180 hours or 7.5 days. The water level forecast guidance includes the combined effects of storm surge (sub-tidal) and tides (astronomical tide predictions).</description>
    </item>
    <item>
      <title>NOAA Unified Forecast System Subseasonal to Seasonal Prototypes</title>
      <link>https://registry.opendata.aws/noaa-ufs-s2s</link>
      <guid>https://registry.opendata.aws/noaa-ufs-s2s</guid>
      <description>The Unified Forecast System Subseasonal to Seasonal prototypes consist of reforecast data from the UFS atmosphere-ocean coupled model experimental prototype version 5, 6, 7, and 8 produced by the Medium Range and Subseasonal to Seasonal Application team of the UFS-R2O project. The UFS prototypes are the first dataset released to the broader weather community for analysis and feedback as part of the development of the next generation operational numerical weather prediction system from NWS. The datasets includes all the major weather variables for atmosphere, land, ocean, sea ice, and ocean waves.
&lt;br/&gt;
&lt;br/&gt;
Acknowledgment - The Unified Forecast System (UFS) atmosphere-ocean coupled model experimental version # data used in this study are made available through the UFS Research to Operations (UFS-R2O) project sponsored by the National Weather Service (NWS) Office of Science and Technology Integration (OSTI) Modeling Program Division and the National Oceanic and Atmospheric Administration (NOAA) Oceanic and Atmospheric Research (OAR) Weather Program Office (WPO).</description>
    </item>
    <item>
      <title>NOAA World Ocean Database (WOD)</title>
      <link>https://registry.opendata.aws/noaa-wod</link>
      <guid>https://registry.opendata.aws/noaa-wod</guid>
      <description>The World Ocean Database (WOD) is the largest uniformly formatted, quality-controlled, publicly available historical subsurface ocean profile database. From Captain Cook&amp;#39;s second voyage in 1772 to today&amp;#39;s automated Argo floats, global aggregation of ocean variable information including temperature, salinity, oxygen, nutrients, and others vs. depth allow for study and understanding of the changing physical, chemical, and to some extent biological state of the World&amp;#39;s Oceans. Browse the bucket via the AWS S3 explorer: &lt;a href&#x3D;&quot;https://noaa-wod-pds.s3.amazonaws.com/index.html&quot;&gt;https://noaa-wod-pds.s3.amazonaws.com/index.html&lt;/a&gt;</description>
    </item>
    <item>
      <title>NUVIEW - Multi-State Geospatial Data</title>
      <link>https://registry.opendata.aws/nuview-state</link>
      <guid>https://registry.opendata.aws/nuview-state</guid>
      <description>NUVIEW hosts and manages a unified collection of geospatial datasets from multiple U.S. states and agencies
(LiDAR, orthophoto imagery, DEM/DSM, and derivative products). Data are organized in a
single S3 bucket with a logical sub-folder hierarchy: &lt;code&gt;/state_or_agency_product_type/acqusition_project_name/...&lt;/code&gt;. All assets
are cloud-optimized (COG GeoTIFFs, COPC (Cloud Optimized Point Cloud) LAZ point clouds, etc.) and available under open licenses.</description>
    </item>
    <item>
      <title>National Archives Catalog</title>
      <link>https://registry.opendata.aws/nara-national-archives-catalog</link>
      <guid>https://registry.opendata.aws/nara-national-archives-catalog</guid>
      <description>The National Archives Catalog dataset contains all of the descriptions; authority records; digitized and electronic records; and tags, transcriptions and comments for NARA’s archival holdings available in the Catalog.</description>
    </item>
    <item>
      <title>National Cancer Institute Center for Cancer Research - Diffuse Large B Cell Lymphoma (DLBCL) Genomics and Expression</title>
      <link>https://registry.opendata.aws/nciccr-dlbcl</link>
      <guid>https://registry.opendata.aws/nciccr-dlbcl</guid>
      <description>The study describes integrative analysis of genetic lesions in 574 diffuse large B cell lymphomas
(DLBCL) involving exome and transcriptome sequencing, array-based DNA copy number analysis and
targeted amplicon resequencing. The dataset contains open RNA-Seq Gene Expression Quantification
data.</description>
    </item>
    <item>
      <title>Nighttime-Fire-Flare</title>
      <link>https://registry.opendata.aws/black_marble_combustion</link>
      <guid>https://registry.opendata.aws/black_marble_combustion</guid>
      <description>Detection of nighttime combustion (fire and gas flaring) from daily top of atmosphere data from NASA&amp;#39;s Black Marble VNP46A1 product using VIIRS Day/Night Band and VIIRS thermal bands.</description>
    </item>
    <item>
      <title>OPERA Coregistered Single-Look Complex from Sentinel-1 Static Layers validated product (Version 1)</title>
      <link>https://registry.opendata.aws/nasa-operal2cslc-s1-staticv1</link>
      <guid>https://registry.opendata.aws/nasa-operal2cslc-s1-staticv1</guid>
      <description>The Observational Products for End-Users from Remote Sensing Analysis (OPERA) Coregistered Single-Look Complex (CSLC) from Sentinel-1 (S1) Static Layers (CSLC-S1-STATIC) validated product contains static radar geometry layers associated with the OPERA Coregistered Single-Look Complex (CSLC) from Sentinel-1 (S1) validated product. Due to the S1 mission’s narrow orbital tube, radar-geometry layers vary slightly over time for each position on the ground, and therefore are considered static. These static layers are provided separately from the OPERA CSLC-S1 product, as they are produced only once or a limited number of times, to account for changes in the DEM, in the S1 orbit, or in the static layers generation algorithm. Each OPERA CSLC-S1-STATIC product is distributed as a Hierarchical Data Format version 5 (HDF5) file following the CF-1.8 convention containing both data raster layers and product metadata and corresponds to matching CSLC-S1 products with the same burst ID. OPERA CSLC-S1 products are available over North America which includes the USA and U.S. Territories, Canada within 200 km of the U.S. border, and all mainland countries from the southern U.S. border down to and including Panama. The CSLC-S1 products are available in the associated OPERA Coregistered Single-Look Complex from Sentinel-1 validated product (Version 1) dataset.
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://cumulus.asf.alaska.edu/s3credentialsREADME&quot;&gt;https://cumulus.asf.alaska.edu/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>OPERA Coregistered Single-Look Complex from Sentinel-1 validated product (Version 1)</title>
      <link>https://registry.opendata.aws/nasa-operal2cslc-s1v1</link>
      <guid>https://registry.opendata.aws/nasa-operal2cslc-s1v1</guid>
      <description>The Observational Products for End-Users from Remote Sensing Analysis (OPERA) Coregistered Single-Look Complex (CSLC) from Sentinel-1 validated product consists of Single Look Complex (SLC) images which contain both amplitude and phase information of the complex radar return. The amplitude is primarily determined by ground surface properties (e.g., terrain slope, surface roughness, and physical properties), and phase primarily represents the distance between the radar and ground targets corrected for the geometrical distance between the two based on the knowledge from Digital Elevation Model and platform’s position, i.e., the CSLC phase represents residual geometrical distance between the sensor and target, the atmospheric propagation delay and the target movements. The CSLC-S1 product is derived from Copernicus Sentinel-1A and Sentinel-1B Interferometric Wide (IW) SLC data.  The CSLC images are precisely aligned or “coregistered” to a pre-defined UTM/Polar stereographic map projection systems and posted at 5x10 m spacing in east and north direction, respectively.  Each CSLC-S1 product corresponds to a single S1 burst and is distributed as a Hierarchical Data Format version 5 (HDF5) file following the CF-1.8 convention containing both data raster layers (e.g., geocoded complex backscatter, low-resolution correction look-up tables) and product metadata. OPERA CSLC-S1 products are available over North America which includes the USA and U.S. Territories, Canada within 200 km of the U.S. border, and all mainland countries from the southern U.S. border down to and including Panama.  The OPERA CSLC-S1 product contains modified Copernicus Sentinel data (2016-2025).Due to the S1 mission’s narrow orbital tube, radar-geometry layers vary slightly over time for each position on the ground, and therefore are considered static. These static layers are provided separately from the OPERA CLSLC-S1 product, as they are produced only once or a limited number of times. The static layers are available in the associated OPERA Coregistered Single-Look Complex from Sentinel-1 Static Layers validated product (Version 1).
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://cumulus.asf.alaska.edu/s3credentialsREADME&quot;&gt;https://cumulus.asf.alaska.edu/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>OPERA Dynamic Surface Water Extent from Sentinel-1 (Version 1)</title>
      <link>https://registry.opendata.aws/nasa-operal3dswx-s1v1</link>
      <guid>https://registry.opendata.aws/nasa-operal3dswx-s1v1</guid>
      <description>This dataset contains Level-3 Dynamic OPERA Surface Water Extent from Sentinel-1 (DSWx-S1) product version 1.  DSWx-S1 provides near-global geographical mapping of surface water extent over land at a spatial resolution of 30 meters over the Military Grid reference System (MGRS) grid system, with a temporal revisit frequency between 6-12 days. Using Sentinel-1 radar observations, DSWx-S1 maps open inland water bodies greater than 3 hectares and 200 meters in width, irrespective of cloud conditions and daylight illumination that often pose challenges to optical sensors. Forward production of the DSWx-S1 data record began in Sept 2024.  Each product is distributed as a set of 3 GeoTIFF (Geographic Tagged Image File Format) files including water classification and associated confidence layers.
&lt;br&gt;&lt;br&gt;
The OPERA DSWx-S1 product contains modified Copernicus Sentinel data (2024-2025).
&lt;br&gt;&lt;br&gt;
To access the calibration/validation database for OPERA Dynamic Surface Water Extent Products, please contact &lt;a href&#x3D;&quot;mailto:&amp;#x70;&amp;#x6f;&amp;#100;&amp;#97;&amp;#97;&amp;#99;&amp;#x40;&amp;#112;&amp;#x6f;&amp;#100;&amp;#97;&amp;#x61;&amp;#x63;&amp;#46;&amp;#106;&amp;#112;&amp;#108;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#x70;&amp;#x6f;&amp;#100;&amp;#97;&amp;#97;&amp;#99;&amp;#x40;&amp;#112;&amp;#x6f;&amp;#100;&amp;#97;&amp;#x61;&amp;#x63;&amp;#46;&amp;#106;&amp;#112;&amp;#108;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt; 
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://archive.podaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;https://archive.podaac.earthdata.nasa.gov/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>OPERA Land Surface Disturbance Alert from Harmonized Landsat Sentinel-2 product (Version 1)</title>
      <link>https://registry.opendata.aws/nasa-operal3dist-alert-hlsv1</link>
      <guid>https://registry.opendata.aws/nasa-operal3dist-alert-hlsv1</guid>
      <description>The Observational Products for End-Users from Remote Sensing Analysis (&lt;a href&#x3D;&quot;https://www.jpl.nasa.gov/go/opera&quot;&gt;OPERA&lt;/a&gt;) Land Surface Disturbance Alert from Harmonized Landsat Sentinel-2 (HLS) product Version 1 maps vegetation disturbance alerts that are derived from data collected by Landsat 8 and Landsat 9 Operational Land Imager (OLI) and Sentinel-2A, Sentinel-2B, and Sentinel-2C Multi-Spectral Instrument (MSI). A vegetation disturbance alert is detected at 30 meter (m) spatial resolution when there is an indicated decrease in vegetation cover within an HLS pixel. The Level-3 data product also provides additional information about more general disturbance trends and auxiliary generic disturbance information as determined from the variations of the reflectance through the HLS scenes. &lt;a href&#x3D;&quot;https://lpdaac.usgs.gov/product_search/?collections&#x3D;HLS&amp;amp;status&#x3D;Operational&amp;amp;view&#x3D;list&quot;&gt;HLS&lt;/a&gt; data represent the highest temporal frequency data available at medium spatial resolution. The combined observations will provide greater sensitivity to land changes, whether of large magnitude/short duration or small magnitude/long duration.The OPERA_L3_DIST-ALERT-HLS (or DIST-ALERT) data product is provided in Cloud Optimized GeoTIFF (COG) format, and each layer is distributed as a separate file. There are 19 layers contained within the DIST-ALERT product. The layers for both vegetation and generic disturbance include disturbance status, loss or anomaly, maximum loss anomaly, disturbance confidence layer, date of disturbance, count of observations with loss anomalies, days of ongoing anomalies, and day of last disturbance detection. Additional layers are vegetation cover percent, historical percent vegetation cover, and data mask. See the Product Specification Document (PSD) for a more detailed description of the individual layers provided in the DIST-ALERT product.The OPERA_L3_DIST-ALERT-HLS product contains modified Copernicus Sentinel data (2020-2025).Known Issues&lt;ul&gt;
&lt;li&gt;Additional usage constraints are provided under Section 5 of the Algorithm Theoretical Basis Document (ATBD).
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&lt;/a&gt;&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>OPERA Land Surface Disturbance Alert from Harmonized Landsat Sentinel-2 provisional product (Version 0)</title>
      <link>https://registry.opendata.aws/nasa-operal3dist-alert-hlsprovisionalv0</link>
      <guid>https://registry.opendata.aws/nasa-operal3dist-alert-hlsprovisionalv0</guid>
      <description>The OPERA_L3_DIST-ALERT-HLS Version 0 data product was decommissioned on April 25, 2025. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/SNWG/OPERA_L3_DIST-ALERT-HLS_V1.001&quot;&gt;OPERA_L3_DIST-ALERT-HLS V1&lt;/a&gt; data product which was released on March 14, 2024, and has achieved stage 1 validation.The Observational Products for End-Users from Remote Sensing Analysis (OPERA) Land Surface Disturbance Alert from Harmonized Landsat Sentinel-2 (HLS) provisional data product Version 0 maps vegetation disturbance alerts from data collected by Landsat 8 and Landsat 9 Operational Land Imager (OLI) and Sentinel-2A, Sentinel-2B, and Sentinel-2C Multi-Spectral Instrument (MSI). Vegetation disturbance alert is detected at 30 meter (m) spatial resolution when there is an indicated decrease in vegetation cover within an HLS pixel. The product also provides auxiliary generic disturbance information as determined from the variations of the reflectance through the HLS scenes to provide information about more general disturbance trends. HLS data represent the highest temporal frequency data available at medium spatial resolution. The combined observations will provide greater sensitivity to land changes, whether of large magnitude/short duration, or small magnitude/long duration. The OPERA_L3_DIST-ALERT-HLS (or DIST-ALERT) data product is provided in Cloud Optimized GeoTIFF (COG) format, and each layer is distributed as a separate file. There are 19 layers contained within in the DIST-ALERT product: vegetation disturbance status, current vegetation cover indicator, current vegetation anomaly value, historical vegetation cover indicator, max vegetation anomaly value, vegetation disturbance confidence layer, date of initial vegetation disturbance, number of detected vegetation loss anomalies, and vegetation disturbance duration. See the Product Specification for a more detailed description of the individual layers provided in the DIST-ALERT product. Known Issues&lt;ul&gt;
&lt;li&gt;Additional usage constraints are provided under Section 5 of the Algorithm Theoretical Basis Document (ATBD).
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&lt;/a&gt;&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>OS-Climate Physrisk</title>
      <link>https://registry.opendata.aws/os-climate-physrisk</link>
      <guid>https://registry.opendata.aws/os-climate-physrisk</guid>
      <description>Collection of adapted and derived hazard indicator datasets optimized for running physical climate risk analyses.</description>
    </item>
    <item>
      <title>Ocean Radar - Newcastle site - Sea water velocity - Delayed mode</title>
      <link>https://registry.opendata.aws/aodn_radar_newcastle_velocity_hourly_averaged_delayed_qc</link>
      <guid>https://registry.opendata.aws/aodn_radar_newcastle_velocity_hourly_averaged_delayed_qc</guid>
      <description>The Newcastle (NEWC) HF ocean radar system covers an area of the Central Coast, New South Wales, an area subject to the variability of the East Australian Current (EAC) and its coupling with coastal winds, tides, and waves. In this area the EAC separates from the coast and generates several eddies which control the larval species and the higher marine species and ecosystems in which they forage.The NEWC HF ocean radar system consists of two SeaSonde crossed loop direction finding stations located at Sea Rocks (32.441575 S 152.539022 E) and Red Head (33.010245 S 151.727059 E).  These radars operate at a frequency of 5.2625 MHz, with a bandwidth of 25 KHz, a maximum range of 200 Km and a range resolution of 6 Km.  Within the HF radar coverage area surface currents are measured.</description>
    </item>
    <item>
      <title>OpenCRAVAT</title>
      <link>https://registry.opendata.aws/open-cravat</link>
      <guid>https://registry.opendata.aws/open-cravat</guid>
      <description>OpenCRAVAT is a module variant annotation tool developed by KarchinLab at Johns Hopkins.
This dataset is a mirror of the OpenCRAVAT store available at &lt;a href&#x3D;&quot;https://store.opencravat.org&quot;&gt;https://store.opencravat.org&lt;/a&gt;.
You can configure OpenCRAVAT to use this mirror by editing the &amp;quot;cravat-system.yml&amp;quot; file.
The path to this file is in the first output line of the command &amp;quot;oc config system&amp;quot;. In that file,
change the value of &amp;quot;store_url&amp;quot; to &amp;quot;&lt;a href&#x3D;&quot;https://opencravat-store-aws.s3.amazonaws.com&amp;quot;&quot;&gt;https://opencravat-store-aws.s3.amazonaws.com&amp;quot;&lt;/a&gt;.</description>
    </item>
    <item>
      <title>Oregon Health &amp; Science University Chronic Neutrophilic Leukemia Dataset</title>
      <link>https://registry.opendata.aws/ohsu-cnl</link>
      <guid>https://registry.opendata.aws/ohsu-cnl</guid>
      <description>The OHSU-CNL study offers the whole exome and RNA-sequencing on a cohort of 100 cases with rare
hematologic malignancies such as Chronic neutrophilic leukemia (CNL), atypical chronic myeloid
leukemia (aCML), and unclassified myelodysplastic syndrome/myeloproliferative neoplasms
(MDS/MPN-U). This dataset contains open RNA-Seq Gene Expression Quantification data.</description>
    </item>
    <item>
      <title>PALSAR-2 ScanSAR Turkey &amp; Syria Earthquake (L2.1 &amp; L1.1)</title>
      <link>https://registry.opendata.aws/palsar2-scansar-turkey-syria</link>
      <guid>https://registry.opendata.aws/palsar2-scansar-turkey-syria</guid>
      <description>JAXA has responded to the Earthquake events in Turkey and Syria by conducting emergency disaster observations and providing data as requested by the Disaster and Emergency Management Authority (AFAD), Ministry of Interior in Turkey, through Sentinel Asia and the International Disaster Charter. Additional information on the event and dataset can be found &lt;a href&#x3D;&quot;https://earth.jaxa.jp/en/earthview/2023/02/14/7381/index.html&quot;&gt;here&lt;/a&gt;. The 25 m PALSAR-2 ScanSAR is normalized backscatter data of PALSAR-2 broad area observation mode with observation width of 350 km. Polarization data are stored as 16-bit digital numbers (DN). The DN values can be converted to gamma naught values in decibel unit (dB) using the following equation: γ0 &#x3D; 10*log10(DN2) - 83.0 dB. Included in this dataset are ALOS PALSAR Level 1.1 and 2.1 data. Level 1.1 is range and single look azimuth compressed data represented by complex I and Q channels to preserve the magnitude and phase information. Range coordinate is in slant range. In the case of ScanSAR mode, an image file is generated per each scan. Level 2.1 data is orthorectified from level 1.1 data by using digital elevation model. Pixel spacing is selectable depending on observation modes. Image coordinate in map projection is geocoded.</description>
    </item>
    <item>
      <title>Pancreatic Cancer Organoid Profiling</title>
      <link>https://registry.opendata.aws/organoid-pancreatic</link>
      <guid>https://registry.opendata.aws/organoid-pancreatic</guid>
      <description>This study generated a collection of patient-derived pancreatic normal and cancer organoids and it was sequenced using Whole Genome Sequencing (WGS), Whole Exome Sequencing (WXS) and RNA-Seq as well as matched tumor and normal tissue if available. The study provides a valuable resource for pancreatic cancer researchers.
The dataset contains open RNA-Seq Gene Expression Quantification data and controlled WGS/WXS/RNA-Seq Aligned Reads, WXS Annotated Somatic Mutation, WXS Raw Somatic Mutation, and RNA-Seq Splice Junction Quantification.</description>
    </item>
    <item>
      <title>RAPID NRT Flood Maps</title>
      <link>https://registry.opendata.aws/rapid-nrt-flood-maps</link>
      <guid>https://registry.opendata.aws/rapid-nrt-flood-maps</guid>
      <description>Near Real-time and archival data of High-resolution (10 m) flood inundation dataset over the Contiguous United States, developed based on the Sentinel-1 SAR imagery (2016-current) archive, using an automated Radar Produced Inundation Diary (RAPID) algorithm.</description>
    </item>
    <item>
      <title>REDASA COVID-19 Open Data</title>
      <link>https://registry.opendata.aws/redasa-covid-data</link>
      <guid>https://registry.opendata.aws/redasa-covid-data</guid>
      <description>The REaltime DAta Synthesis and Analysis (REDASA) COVID-19 snapshot contains the output of the curation protocol produced by our curator community. A detailed description can be found in &lt;a href&#x3D;&quot;https://www.jmir.org/2021/5/e25714&quot;&gt;our paper&lt;/a&gt;. The first S3 bucket listed in Resources contains a large collection of medical documents in text format extracted from the &lt;a href&#x3D;&quot;https://registry.opendata.aws/cord-19/&quot;&gt;CORD-19 dataset&lt;/a&gt;, plus other sources deemed relevant by the REDASA consortium.  The second S3 bucket contains a series of documents surfaced by &lt;a href&#x3D;&quot;https://aws.amazon.com/kendra/&quot;&gt;Amazon Kendra&lt;/a&gt; that were considered relevant for each medical question asked. The final S3 bucket contains the GroundTruth annotations created by our curator community.</description>
    </item>
    <item>
      <title>RNA structure by fragmentation frequency</title>
      <link>https://registry.opendata.aws/frag-struc</link>
      <guid>https://registry.opendata.aws/frag-struc</guid>
      <description>The fragSTRUC project devises a software to extract RNA secondary structure information from Illumina datasets, based on divalent ions in standard RNA-seq library preparation fragmenting sequences at non-base-paired regions of RNA.</description>
    </item>
    <item>
      <title>Reference Indexes for krepp</title>
      <link>https://registry.opendata.aws/kreppref</link>
      <guid>https://registry.opendata.aws/kreppref</guid>
      <description>krepp is an alignment-free method for estimating distances and phylogenetic placement of individual reads to many thousands of reference genomes in a scalable manner using k-mers. This dataset includes k-mer-based indexes consisting of ultra-large reference genome sets that can be efficiently analyzed using krepp.</description>
    </item>
    <item>
      <title>Reference data for HiFi human WGS</title>
      <link>https://registry.opendata.aws/pacbio-human-wgs-reference</link>
      <guid>https://registry.opendata.aws/pacbio-human-wgs-reference</guid>
      <description>Reference data bundle for analyzing HiFi human whole genome
sequencing data</description>
    </item>
    <item>
      <title>SatPM2.5</title>
      <link>https://registry.opendata.aws/surface-pm2-5-v6gl</link>
      <guid>https://registry.opendata.aws/surface-pm2-5-v6gl</guid>
      <description>Fine particulate matter (PM2.5) concentrations are estimated using information from satellite-, simulation- and monitor-based sources. Aerosol optical depth from multiple satellites (MODIS, VIIRS, MISR, SeaWiFS, and VIIRS) and their respective retrievals (Dark Target, Deep Blue, MAIAC) is combined with simulation (GEOS-Chem) based upon their relative uncertainties as determined using ground-based sun photometer (AERONET) observations to produce geophysical estimates that explain most of the variance in ground-based PM2.5 measurements. A subsequent statistical fusion incorporates additional information from ground-based PM2.5 measurements.</description>
    </item>
    <item>
      <title>Satellogic EarthView dataset</title>
      <link>https://registry.opendata.aws/satellogic-earthview</link>
      <guid>https://registry.opendata.aws/satellogic-earthview</guid>
      <description>Satellogic EarthView dataset includes high-resolution satellite images captured over all continents. The dataset is organized in Hive partition format and hosted by AWS. The dataset can be accessed via STAC browser or aws cli. Each item of the dataset corresponds to a specific region and date, with some of the regions revisited for additional data. The dataset provides Top-of-Atmosphere (TOA) reflectance values across four spectral bands (Red, Green, Blue, Near-Infrared) at a Ground Sample Distance (GSD) of 1 meter, accompanied by comprehensive metadata such as off-nadir angles, sun elevation, and other pertinent details. Users should note that due to an artifact in region delineation, a small number of regions present overlaps.</description>
    </item>
    <item>
      <title>SeeFar V0</title>
      <link>https://registry.opendata.aws/seefar</link>
      <guid>https://registry.opendata.aws/seefar</guid>
      <description>A collection of multi-resolution satellite images from both public and commercial satellites. The dataset is specifically curated for training geospatial foundation models.</description>
    </item>
    <item>
      <title>Sentinel-1 SLC dataset for South and Southeast Asia, Taiwan, Korea and Japan</title>
      <link>https://registry.opendata.aws/sentinel1-slc-seasia-pds</link>
      <guid>https://registry.opendata.aws/sentinel1-slc-seasia-pds</guid>
      <description>The S1 Single Look Complex (SLC) dataset contains Synthetic Aperture Radar (SAR) data in the C-Band wavelength. The SAR sensors are installed on a two-satellite (Sentinel-1A and Sentinel-1B) constellation orbiting the Earth with a combined revisit time of six days, operated by the European Space Agency. The S1 SLC data are a Level-1 product that collects radar amplitude and phase information in all-weather, day or night conditions, which is ideal for studying natural hazards and emergency response, land applications, oil spill monitoring, sea-ice conditions, and associated climate change effects.</description>
    </item>
    <item>
      <title>Somatic Mosaicism across Human Tissues (SMaHT)</title>
      <link>https://registry.opendata.aws/smaht</link>
      <guid>https://registry.opendata.aws/smaht</guid>
      <description>The Somatic Mosaicism across Human Tissues (SMaHT) project is an NIH Common
Fund consortium (2023-) aimed to comprehensively characterize somatic variation
(&amp;quot;mosaicism&amp;quot;) in normal human tissues. While most genetic studies have relied
on blood-derived DNA, SMaHT captures the full spectrum of DNA variation across
cell types, tissues, and organs from phenotypically normal individuals to
better understand the role of somatic mosaicism in human development, aging,
and disease progression.Researchers in the consortium develop and apply experimental and computational
methods, paired with the state-of-the-art sequencing technologies, to accurately
detect even rare mutations (frequency &amp;lt; 1%) in subpopulations of cells. In
addition to generating the production data across ~20 tissue types from 150
post-mortem donors, SMaHT also produces datasets from cell line and tissue
homogenate samples, to benchmark and develop new technologies and computational
tools for mosaic variant detection.The resulting data include high-coverage whole-genome and transcriptome data
using both short-read and long-read sequencing technologies from multiple platforms
(e.g., Illumina, PacBio, Oxford Nanopore Technologies, Ultima Genomics). SMaHT will
also generate comprehensive genome-wide catalogs of somatic variants. We anticipate
that this resource will be valuable not only for researchers studying somatic
mosaicism, but also for the broader scientific community interested in large-scale
WGS data from normal human tissues. More about the SMaHT project:
program announcement, &lt;a href&#x3D;&quot;https://commonfund.nih.gov/smaht&quot;&gt;https://commonfund.nih.gov/smaht&lt;/a&gt;, and &lt;a href&#x3D;&quot;https://smaht.org/&quot;&gt;https://smaht.org/&lt;/a&gt;.
More about the data portal: &lt;a href&#x3D;&quot;https://data.smaht.org/&quot;&gt;https://data.smaht.org/&lt;/a&gt; and types of data generated:
&lt;a href&#x3D;&quot;https://data.smaht.org/about/consortium/data&quot;&gt;https://data.smaht.org/about/consortium/data&lt;/a&gt;</description>
    </item>
    <item>
      <title>Sounds of Central African landscapes</title>
      <link>https://registry.opendata.aws/elp-nouabale-landscape</link>
      <guid>https://registry.opendata.aws/elp-nouabale-landscape</guid>
      <description>Archival soundscapes recorded in the rainforest landscapes of
Central Africa, with a focus on the vocalizations of African forest
elephants (Loxodonta cyclotis).</description>
    </item>
    <item>
      <title>State of Colorado Elevation Data</title>
      <link>https://registry.opendata.aws/colorado-elevation-data</link>
      <guid>https://registry.opendata.aws/colorado-elevation-data</guid>
      <description>The State of Colorado has gathered public historical elevation data.</description>
    </item>
    <item>
      <title>Sub-Meter Canopy Tree Height of California in 2020 by CTrees.org</title>
      <link>https://registry.opendata.aws/ctrees-california-vhr-tree-height</link>
      <guid>https://registry.opendata.aws/ctrees-california-vhr-tree-height</guid>
      <description>Canopy Tree Height maps for California in 2020. Created using a deep learning model on very-high-resolution airborne imagery from the National Agriculture Imagery Program (NAIP) by United States Department of Agriculture (USDA).</description>
    </item>
    <item>
      <title>TESS-SPOC</title>
      <link>https://registry.opendata.aws/mast-tess-spoc</link>
      <guid>https://registry.opendata.aws/mast-tess-spoc</guid>
      <description>The data products for the TESS-SPOC FFI targets are the same as for the &lt;a href&#x3D;&quot;https://archive.stsci.edu/missions-and-data/tess&quot;&gt;TESS&lt;/a&gt;
two-minute cadence targets: calibrated target pixel files, simple aperture photometry (SAP) flux time series, presearch data conditioning
corrected (PDCSAP) flux time series, and cotrending basis vectors (CBV). Since TESS-SPOC relies on FFIs, data are sampled at the FFI cadence.</description>
    </item>
    <item>
      <title>TIGER Training</title>
      <link>https://registry.opendata.aws/tiger</link>
      <guid>https://registry.opendata.aws/tiger</guid>
      <description>&amp;quot;This dataset contains the training data for the &lt;a href&#x3D;&quot;https://tiger.grand-challenge.org&quot;&gt;Tumor InfiltratinG lymphocytes in breast cancER or TIGER&lt;/a&gt; challenge. TIGER is the first challenge on fully automated assessment of tumor-infiltrating lymphocytes (TILs) in breast cancer histopathology slides. TILs are proving to be an important biomarker in cancer patients as they can play a part in killing tumor cells, particularly in some types of breast cancer. Identifying and measuring TILs can help to better target treatments, particularly immunotherapy, and may result in lower levels of other more aggressive treatments, including chemotherapy.&amp;quot;</description>
    </item>
    <item>
      <title>Tabula Sapiens</title>
      <link>https://registry.opendata.aws/tabula-sapiens</link>
      <guid>https://registry.opendata.aws/tabula-sapiens</guid>
      <description>Tabula Sapiens is a benchmark, first-draft human cell atlas of over 1.1M cells from 28 organs of 24 normal human subjects. 
This work is the product of the Tabula Sapiens Consortium. 
Taking the organs from the same individual controls for genetic background, age, environment, and epigenetic effects, 
and allows detailed analysis and comparison of cell types that are shared between tissues. 
Our work creates a detailed portrait of cell types as well as their distribution and variation in gene expression 
across tissues and within the endothelial, epithelial, stromal and immune compartments.
We have built directly on our unique skills, experience, and data infrastructure from Tabula Muris and Tabula Muris Senis 
to create a high-quality human reference dataset and portal at a 10-fold larger scale from these prior efforts.A critical factor in the Tabula projects is our large collaborative network of PIs with deep expertise at preparation of diverse organs, 
enabling all organs from a subject to be successfully processed within a single day. 
We have built the logistics and infrastructure capable of tracking hundreds of samples and thousands of 384-well plates 
from tissue through sample prep, library construction and on to sequencing and ultimately computational 
and expert cell annotation with tight quality control.Tabula Sapiens leverages our network of human tissue experts and a close collaboration with a Donor Network West, 
a not-for-profit organ procurement organization. We use their experience to balance and assign cell types 
from each tissue compartment and optimally mix high-quality plate-seq data and high-volume droplet-based data to 
provide a broad and deep benchmark atlas.The first version of Tabula Sapiens contained nearly 500,000 cells from 24 organs of 15 normal human subjects.
With the second version, Tabula Sapiens 2.0, we have built an integrated map of 28 tissues collected across 24 donors. 
Nine new donors and four new tissues were collected and analyzed together with the original Tabula Sapiens 1.0 dataset. 
All tissues and organs, with the exception of the respective reproductive organs, were profiled from both male (n&#x3D;11) and female (n&#x3D;13) donors. 
The donor&amp;#39;s age ranges from 22 to 74 years old, offering one of the most comprehensive molecular profiles of human tissues across the 
adult lifespan (7 donors under the age of 40, 11 donors between 40 and 60, and 6 donors over 60 years of age).Our goal is to make sequence data rapidly and broadly available to the scientific community as a community resource and 
we welcome collaborative interaction on the project and analyses. By accessing these data, you agree to cite our work as 
The Tabula Sapiens Consortium, Science 376, eabl4896 (2022) if using the original v1 dataset, or to cite our 
work as The Tabula Sapiens Consortium, biorxiv (2024) if you are using the Tabula Sapiens v2 data release. 
All processed data is available (see below) and the raw data is browsable from AWS. Redistribution of these data should 
include the full text of the data use policy.If you wish to gain access to the raw fastq files, please submit a request using the controlled access form to sign the data use agreement, 
upon which we may grant you access to the files. Raw fastq files should not be transferred to any third party.</description>
    </item>
    <item>
      <title>Terra Fusion Data Sampler</title>
      <link>https://registry.opendata.aws/terrafusion</link>
      <guid>https://registry.opendata.aws/terrafusion</guid>
      <description>The Terra Basic Fusion dataset is a fused dataset of the original Level 1 radiances
from the five Terra instruments. They have been fully validate to contain the original
Terra instrument Level 1 data. Each Level 1 Terra Basic Fusion file contains one full
Terra orbit of data and is typically 15 – 40 GB in size, depending on how much data was
collected for that orbit. It contains instrument radiance in physical units; radiance
quality indicator; geolocation for each IFOV at its native resolution; sun-view geometry;
bservation time; and other attributes/metadata. It is stored in HDF5, conformed to CF
conventions, and accessible by netCDF-4 enhanced models. It’s naming convention
follows: TERRA_BF_L1B_OXXXX_YYYYMMDDHHMMSS_F000_V000.h5. A concise description of the
dataset, along with links to complete documentation and available software tools, can
be found on the Terra Fusion project page: &lt;a href&#x3D;&quot;https://terrafusion.web.illinois.edu&quot;&gt;https://terrafusion.web.illinois.edu&lt;/a&gt;.&lt;/br&gt;&lt;/br&gt;Terra is the flagship satellite of NASA’s Earth Observing System (EOS). It was launched
into orbit on December 18, 1999 and carries five instruments. These are the
Moderate-resolution Imaging Spectroradiometer (MODIS), the Multi-angle Imaging
SpectroRadiometer (MISR), the Advanced Spaceborne Thermal Emission and Reflection
Radiometer (ASTER), the Clouds and Earth’s Radiant Energy System (CERES), and the
Measurements of Pollution in the Troposphere (MOPITT).&lt;/br&gt;&lt;/br&gt;The Terra Basic Fusion dataset is an easy-to-access record of the Level 1 radiances
for instruments on the Terra mission for selected WRS-2 paths covering the years
2000-2015. These paths are Paths 20-26 (e.g., US corn belt), 108 (e.g., Japan),
125 (e.g., China), 143 (e.g., India), 150 (e.g., Showa Station, Antarctica),
169 (e.g., Europe and Africa), 188 (e.g., Nigeria calibration site), and 233
(e.g., Greenland).</description>
    </item>
    <item>
      <title>Transiting Exoplanet Survey Satellite (TESS)</title>
      <link>https://registry.opendata.aws/mast-tess</link>
      <guid>https://registry.opendata.aws/mast-tess</guid>
      <description>The Transiting Exoplanet Survey Satellite (TESS) is a multi-year survey that has discovered exoplanets in orbit around bright stars across the entire sky using high-precision photometry. The survey also enables a wide variety of stellar astrophysics, solar system science, and extragalactic variability studies. More information about TESS is available at &lt;a href&#x3D;&quot;https://archive.stsci.edu/missions-and-data/tess&quot;&gt;MAST&lt;/a&gt; and the &lt;a href&#x3D;&quot;https://heasarc.gsfc.nasa.gov/docs/tess/&quot;&gt;TESS Science Support Center&lt;/a&gt;.</description>
    </item>
    <item>
      <title>Tropical Cyclone Precipitation, Infrared, Microwave, and Environmental Dataset (TC PRIMED)</title>
      <link>https://registry.opendata.aws/noaa-nesdis-tcprimed-pds</link>
      <guid>https://registry.opendata.aws/noaa-nesdis-tcprimed-pds</guid>
      <description>The Tropical Cyclone Precipitation, Infrared, Microwave and Environmental Dataset (TC PRIMED) is a dataset centered around passive microwave observations of global tropical cyclones from low-Earth-orbiting satellites. TC PRIMED is a compilation of tropical cyclone data from various sources, including 1) tropical cyclone information from the National Oceanic and Atmospheric Administration (NOAA) National Weather Service National Hurricane Center (NHC) and Central Pacific Hurricane Center (CPHC) and the U.S. Department of Defense Joint Typhoon Warning Center, 2) low-Earth-orbiting satellite observations and products from the National Aeronautics and Space Administration (NASA) Global Precipitation Measurement (GPM) mission constellation satellites, and 3) environmental fields and diagnostics calculated from the European Center for Medium-Range Weather Forecasts (ECMWF) fifth-generation reanalysis (ERA5).</description>
    </item>
    <item>
      <title>UMASSD-FVCOM-GOM3-Hindcast</title>
      <link>https://registry.opendata.aws/fvcom_gom3</link>
      <guid>https://registry.opendata.aws/fvcom_gom3</guid>
      <description>The Finite Volume Community Ocean Model (FVCOM) was used to simulate ocean water levels, velocity, temperature and salinity over a multi-decadal period (1984-present) in the waters of the Northeast US including the Gulf of Maine.  The model was configured and run by the Dr. Changshen Chen, Director of the Marine Ecosystems Dynamics Modeling Laboratory in the School for Marine Science &amp;amp; Technology at the University of Massachusetts Dartmouth.  The triangular mesh has a varying horizontal resolution from several hundred meters inshore to several kilometers offshore, and 45 terrain-following vertical layers.  The model output was saved at hourly intervals from 2009-08-21 to 2022-06-17.</description>
    </item>
    <item>
      <title>USGS COAWST (Coupled Ocean Atmosphere Wave and Sediment Transport) Forecast Model Archive, US East and Gulf Coasts</title>
      <link>https://registry.opendata.aws/coawst</link>
      <guid>https://registry.opendata.aws/coawst</guid>
      <description>The COAWST modeling system has been used to simulate ocean, wave and sediment transport processes along the of US East Coast and Gulf of Mexico. The grid has a horizontal resolution of approximately 5km and is resolved with 16 vertical terrain following levels. The model has been executed on a daily basis since August 2009 with outputs written every hour. This archive contains model output from 2009-08-21 to 2022-06-17.</description>
    </item>
    <item>
      <title>UniProt</title>
      <link>https://registry.opendata.aws/uniprot</link>
      <guid>https://registry.opendata.aws/uniprot</guid>
      <description>The Universal Protein Resource (UniProt) is a comprehensive resource for protein sequence and annotation data. The UniProt databases are the UniProt Knowledgebase (UniProtKB), the UniProt Reference Clusters (UniRef), and the UniProt Archive (UniParc). The UniProt consortium and host institutions &lt;a href&#x3D;&quot;https://www.ebi.ac.uk&quot;&gt;EMBL-EBI&lt;/a&gt;, &lt;a href&#x3D;&quot;https://www.sib.swiss&quot;&gt;SIB Swiss Institute of Bioinformatics&lt;/a&gt; and &lt;a href&#x3D;&quot;https://proteininformationresource.org/&quot;&gt;PIR&lt;/a&gt; are committed to the long-term preservation of the &lt;a href&#x3D;&quot;https://www.uniprot.org&quot;&gt;UniProt&lt;/a&gt; databases.</description>
    </item>
    <item>
      <title>Whiffle WINS50 Open Data on AWS</title>
      <link>https://registry.opendata.aws/whiffle-wins50</link>
      <guid>https://registry.opendata.aws/whiffle-wins50</guid>
      <description>Large Eddy Simulation (LES) data of the Winds of the North Sea in 2050 (WINS50) project.</description>
    </item>
    <item>
      <title>3-Band Cryo Data | Wide-field Infrared Survey Explorer (WISE)</title>
      <link>https://registry.opendata.aws/wise-cryo-3band</link>
      <guid>https://registry.opendata.aws/wise-cryo-3band</guid>
      <description>The Wide-field Infrared Survey Explorer (WISE) was a NASA Medium Explorer satellite in low-Earth orbit that conducted an all-sky astronomical imaging survey over four infrared bands from 2010-2011. The 3-Band Cryo Data Release contains 3.4, 4.6 and 12 micron (W1, W2, W3) imaging data that were acquired between 6 Aug and 29 Sept 2010 while the detectors were cooled by the inner cryogen tank following the exhaustion of the outer tank.</description>
    </item>
    <item>
      <title>3DCoMPaT: Composition of Materials on Parts of 3D Things</title>
      <link>https://registry.opendata.aws/3dcompat</link>
      <guid>https://registry.opendata.aws/3dcompat</guid>
      <description>3D CoMPaT is a richly annotated large-scale dataset of rendered compositions of Materials on Parts of thousands of unique 3D Models.
This dataset primarily focuses on stylizing 3D shapes at part-level with compatible materials.
Each object with the applied part-material compositions is rendered from four equally spaced views as well as four randomized views.
We introduce a new task, called Grounded CoMPaT Recognition (GCR), to collectively recognize and ground compositions of materials on parts of 3D objects.
We present two variations of this task and adapt state-of-art 2D/3D deep learning methods to solve the problem as baselines for future research.
We hope our work will help ease future research on compositional 3D Vision.</description>
    </item>
    <item>
      <title>A2D2: Audi Autonomous Driving Dataset</title>
      <link>https://registry.opendata.aws/aev-a2d2</link>
      <guid>https://registry.opendata.aws/aev-a2d2</guid>
      <description>An open multi-sensor dataset for autonomous driving research. This dataset comprises semantically segmented images, semantic point clouds, and 3D bounding boxes. In addition, it contains unlabelled 360 degree camera images, lidar, and bus data for three sequences. We hope this dataset will further facilitate active research and development in AI, computer vision, and robotics for autonomous driving.</description>
    </item>
    <item>
      <title>ABoVE: Bias-Corrected IMERG Monthly Precipitation for Alaska and Canada, 2000-2020</title>
      <link>https://registry.opendata.aws/nasa-imergprecipcanadaalaska2097</link>
      <guid>https://registry.opendata.aws/nasa-imergprecipcanadaalaska2097</guid>
      <description>This dataset is a modification to the Integrated Multi-satellitE Retrievals for GPM (IMERG) Final Run microwave-only, daily precipitation Version 06 data. It provides bias-corrected IMERG monthly precipitation data for Alaska and Canada from June 2000 through December 2020 in Cloud-Optimized GeoTIFF (*.tif) format. Data are provided in the units of mm/day. NASA&amp;#39;s IMERG data product is one of the most advanced satellite precipitation products with a 0.1-degree spatial resolution and near global coverage. This dataset bias-corrected IMERG&amp;#39;s HQprecipitation precipitation estimates, which are based on passive microwave (PMW)-only retrievals, using a linear regression method. This method utilizes empirical measurements from rain gauge stations from the Global Historical Climatology Network (GHCN) and a digital elevation model. This bias correction approach improves estimates at elevations above 500 m a.s.l., which are typically underestimated.
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.ornldaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;https://data.ornldaac.earthdata.nasa.gov/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>AI2 Diagram Dataset (AI2D)</title>
      <link>https://registry.opendata.aws/allenai-diagrams</link>
      <guid>https://registry.opendata.aws/allenai-diagrams</guid>
      <description>4,817 illustrative diagrams for research on diagram understanding and associated question answering.</description>
    </item>
    <item>
      <title>AI2 Meaningful Citations Data Set</title>
      <link>https://registry.opendata.aws/allenai-meaningful-citations</link>
      <guid>https://registry.opendata.aws/allenai-meaningful-citations</guid>
      <description>630 paper annotations</description>
    </item>
    <item>
      <title>AI2 Reasoning Challenge (ARC) 2018</title>
      <link>https://registry.opendata.aws/allenai-arc</link>
      <guid>https://registry.opendata.aws/allenai-arc</guid>
      <description>7,787 multiple choice science questions and associated corpora</description>
    </item>
    <item>
      <title>AIRS/Aqua L1B Infrared (IR) geolocated and calibrated radiances V005 (AIRIBRAD) at GES DISC</title>
      <link>https://registry.opendata.aws/nasa-airibrad</link>
      <guid>https://registry.opendata.aws/nasa-airibrad</guid>
      <description>WARNING: On 2021/09/23 the EOS Aqua executed a Deep Space Maneuver (DSM). In the DSM, the spacecraft is turned such that the normal Earth field of regard is deep space.The thermal impact of the DSM caused a shift of the centroids of spectral response functions (SRF) of about 1% of the width of the SRF, equivalent to a frequency shift of 9 parts per million. This shift is reflected in the “spectral_freq” parameter (observed frequencies) in the L1b v5 files for each 6 minute granule. The magnitude of the effect on brightness temperatures (BT) depends on the spectral gradient of each channel. Maximum BT shifts are approximately +- 0.5 K, although many channels experience far smaller BT shifts. Approximately 1803 channels have BT shifts of less than 0.1 K and 575 channels are now shifted in BT by more than 0.1 K, while 231 of these channels have BT shifts greater than 0.2 K.Users of the L1b v5 product who are concerned that these shifts may impact their science investigations and applications are encouraged to switch to the AIRS L1c v6.7.4 product, which, among many other improvements, converts the spectra to a fixed frequency grid.          END OF WARNING.The Atmospheric Infrared Sounder (AIRS) is a grating spectrometer (R &#x3D; 1200) aboard the second Earth Observing System (EOS) polar-orbiting platform, EOS Aqua. In combination with the Advanced Microwave Sounding Unit (AMSU) and the Humidity Sounder for Brazil (HSB), AIRS constitutes an innovative atmospheric sounding group of visible, infrared, and microwave sensors. The AIRS Infrared (IR) level 1B data set contains AIRS calibrated and geolocated radiances in milliWatts/m^2/cm^-1/steradian for 2378 infrared channels in the 3.74 to 15.4 micron region of t he spectrum. The AIRS instrument is co-aligned with AMSU-A so that successive blocks of 3 x 3 AIRS footprints are contained within one AMSU-A footprint. The AIRIBRAD_005 products are stored in files (often referred to as &amp;quot;granules&amp;quot;) that contain 6 minutes of data, 90 footprints across track by 135 lines along track.
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>ARCO-OCEAN</title>
      <link>https://registry.opendata.aws/ogs-arco-ocean</link>
      <guid>https://registry.opendata.aws/ogs-arco-ocean</guid>
      <description>ARCO-OCEAN is an analysis-ready cloud-optimized dataset providing physical properties of the ocean, waves, and sea ice for a period of about 28 years between the 1st of January 1993 and the 30th of June 2021. The dataset includes also atmospheric and hydrological variables that would be needed as boundary conditions and used to drive a numerical simulation. The dataset is the result of collecting, processing, merging and optimizing for the cloud different data sources, all retrospective analyses (reanalyses) or hindcasts of different Earth system components. The dataset has been designed with machine learning in mind, and takes inspiration from similar datasets derived from ERA5.</description>
    </item>
    <item>
      <title>ARPA-E PERFORM Forecast data</title>
      <link>https://registry.opendata.aws/arpa-e-perform</link>
      <guid>https://registry.opendata.aws/arpa-e-perform</guid>
      <description>The ARPA-E PERFORM Program is an ARPA-E funded program that aim to use
time-coincident power and load seeks to develop innovative management systems
that represent the relative delivery risk of each asset and balance the
collective risk of all assets across the grid. A risk-driven paradigm allows
operators to: (i) fully understand the true likelihood of maintaining a
supply-demand balance and system reliability, (ii) optimally manage the system,
and (iii) assess the true value of essential reliability services. This
paradigm shift is critical for all power systems and is essential for grids
with high levels of stochastic resources. Projects will propose methods to
quantify and manage risk at the asset level and at the system level.In support of the ARPA-E PERFORM project, NREL has produced a set of
time-coincident load, wind, and solar generation profiles, including actual and
forecasting time series. Both actuals and forecasts are provided in form of
time-series with high temporal and spatial fidelity. Both deterministic and
probabilistic forecasts are contained in the dataset.</description>
    </item>
    <item>
      <title>ASTER Level 1T Precision Terrain Corrected Registered At-Sensor Radiance V004</title>
      <link>https://registry.opendata.aws/nasa-astl1t</link>
      <guid>https://registry.opendata.aws/nasa-astl1t</guid>
      <description>The Terra Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) Level 1 Precision Terrain Corrected Registered At-Sensor Radiance (AST_L1T) data contains calibrated at-sensor radiance, which corresponds with the ASTER Level 1B (&lt;a href&#x3D;&quot;https://doi.org/10.5067/ASTER/AST_L1B.004&quot;&gt;AST_L1B&lt;/a&gt;) that has been geometrically corrected and rotated to a north-up UTM projection. The AST_L1T is created from a single resampling of the corresponding ASTER L1A (&lt;a href&#x3D;&quot;https://doi.org/10.5067/ASTER/AST_L1A.004&quot;&gt;AST_L1A&lt;/a&gt;) product. The bands available in the AST_L1T depend on the bands in the AST_L1A and can include up to three Visible and Near Infrared (VNIR) bands, six Shortwave Infrared (SWIR) bands, and five Thermal Infrared (TIR) bands. The AST_L1T dataset does not include the aft-looking VNIR band 3. The AST_L1T product has a spatial resolution of 15 meters (m) for the VNIR bands, 30 m for the SWIR bands, and 90 m for the TIR bands.The precision terrain correction process incorporates GLS2000 digital elevation data with derived ground control points (GCPs) to achieve topographic accuracy for all daytime scenes where correlation statistics reach a minimum threshold. Alternate levels of correction are possible (systematic terrain, systematic, or precision) for scenes acquired at night or that otherwise represent a reduced quality ground image (e.g., cloud cover).For daytime images, if the VNIR or SWIR telescope collected data and precision correction was attempted, each precision terrain corrected image will have an accompanying independent quality assessment. It will include the geometric correction available for distribution as both a text file and single band browse images with the valid GCPs overlaid.This multi-file product also includes georeferenced full resolution browse images. The number of browse images and the band combinations of the images depends on the bands available in the corresponding &lt;a href&#x3D;&quot;https://doi.org/10.5067/ASTER/AST_L1A.004&quot;&gt;AST_L1A&lt;/a&gt; dataset.Known Issues&lt;ul&gt;
&lt;li&gt;Since October 1, 2017, a correction addresses zero-filled scans in low-latitude, ascending orbit (nighttime) TIR data. Additional details are available in the ASTER L1T User Advisory.&lt;/li&gt;
&lt;li&gt;Data from the SWIR bands collected after April 2008 may show anomalous saturation and striping. See the ASTER SWIR User Advisory for further information.&lt;/li&gt;
&lt;/ul&gt;
Improvements/Changes from Previous Versions&lt;ul&gt;
&lt;li&gt;Enhanced Geolocation Accuracy: Version 4 uses Collection 2 Ground Control Points (GCPs) compared against Global Land Survey (GLS) 2000 standards to improve positional accuracy.&lt;/li&gt;
&lt;li&gt;Radiometric Calibration Update: Version 4 applies Radiometric Calibration Coefficient Version 5 (RCC V5) to improve the radiometric accuracy of the raw DNs, based on research by &lt;a href&#x3D;&quot;https://doi.org/10.3390/rs12030427&quot;&gt;Tsuchida and others (2020)&lt;/a&gt;, published in Remote Sensing.
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&lt;/a&gt;&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>ATLAS/ICESat-2 L2A Global Geolocated Photon Data V006</title>
      <link>https://registry.opendata.aws/nasa-atl03</link>
      <guid>https://registry.opendata.aws/nasa-atl03</guid>
      <description>This data set (ATL03) contains height above the WGS 84 ellipsoid (ITRF2014 reference frame), latitude, longitude, and time for all photons downlinked by the Advanced Topographic Laser Altimeter System (ATLAS) instrument on board the Ice, Cloud and land Elevation Satellite-2 (ICESat-2) observatory. The ATL03 product was designed to be a single source for all photon data and ancillary information needed by higher-level ATLAS/ICESat-2 products. As such, it also includes spacecraft and instrument parameters and ancillary data not explicitly required for ATL03.
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.nsidc.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;https://data.nsidc.earthdatacloud.nasa.gov/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>ATLAS/ICESat-2 L3A Land and Vegetation Height V006</title>
      <link>https://registry.opendata.aws/nasa-atl08</link>
      <guid>https://registry.opendata.aws/nasa-atl08</guid>
      <description>This data set (ATL08) contains along-track heights above the WGS84 ellipsoid (ITRF2014 reference frame) for the ground and canopy surfaces. The canopy and ground surfaces are processed in fixed 100 m data segments, which typically contain more than 100 signal photons. The data were acquired by the Advanced Topographic Laser Altimeter System (ATLAS) instrument on board the Ice, Cloud and land Elevation Satellite-2 (ICESat-2) observatory.
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.nsidc.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;https://data.nsidc.earthdatacloud.nasa.gov/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>Aging Mouse Brain Epigenetic</title>
      <link>https://registry.opendata.aws/salk-aging-mouse-brain-epigeneti</link>
      <guid>https://registry.opendata.aws/salk-aging-mouse-brain-epigeneti</guid>
      <description>Aging is a major risk factor for neurodegenerative diseases, yet underlying epigenetic mechanisms remain unclear. Here, we generated a comprehensive single-nucleus cell atlas of brain aging across multiple brain regions, comprising 132,551 single-cell methylomes and 72,666 joint chromatin conformation-methylome nuclei. Integration with companion transcriptomic and chromatin accessibility data yielded a cross-modality taxonomy of 36 major cell types.</description>
    </item>
    <item>
      <title>All-Sky Data | Wide-field Infrared Survey Explorer (WISE)</title>
      <link>https://registry.opendata.aws/wise-allsky</link>
      <guid>https://registry.opendata.aws/wise-allsky</guid>
      <description>The Wide-field Infrared Survey Explorer (WISE) was a NASA Medium Explorer satellite in low-Earth orbit that conducted an all-sky astronomical imaging survey over four infrared bands from 2010-2011. The All-Sky Release includes all data taken during the WISE full cryogenic mission phase, 7 January 2010 to 6 August 2010, in the 3.4, 4.6, 12, and 22 micron bands (i.e., W1, W2, W3, W4) that were processed with improved calibrations and reduction algorithms.</description>
    </item>
    <item>
      <title>AllWISE Data | Wide-field Infrared Survey Explorer (WISE)</title>
      <link>https://registry.opendata.aws/wise-allwise</link>
      <guid>https://registry.opendata.aws/wise-allwise</guid>
      <description>The Wide-field Infrared Survey Explorer (WISE) was a NASA Medium Explorer satellite in low-Earth orbit that conducted an all-sky astronomical imaging survey over four infrared bands from 2010-2011. The AllWISE Data Release combines data from all cryogenic and post-cryogenic survey phases and provides a comprehensive view of the mid-infrared sky. The Images Atlas includes 18,240 FITS image sets at 3.4, 4.6, 12 and 22 microns. The Source Catalog contains position, apparent motion, and flux information for over 747 million objects detected on the Atlas Images.</description>
    </item>
    <item>
      <title>Allen Brain Observatory - Visual Coding AWS Public Data Set</title>
      <link>https://registry.opendata.aws/allen-brain-observatory</link>
      <guid>https://registry.opendata.aws/allen-brain-observatory</guid>
      <description>The Allen Brain Observatory – Visual Coding is a large-scale, standardized survey of physiological activity across the mouse visual cortex, hippocampus, and thalamus. It includes datasets collected with both two-photon imaging and Neuropixels probes, two complementary techniques for measuring the activity of neurons in vivo. The two-photon imaging dataset features visually evoked calcium responses from GCaMP6-expressing neurons in a range of cortical layers, visual areas, and Cre lines. The Neuropixels dataset features spiking activity from distributed cortical and subcortical brain regions, collected under analogous conditions to the two-photon imaging experiments. We hope that experimentalists and modelers will use these comprehensive, open datasets as a testbed for theories of visual information processing.</description>
    </item>
    <item>
      <title>Allen Institute for Neural Dynamics - Mouse Neuroanatomy and Physiology Data</title>
      <link>https://registry.opendata.aws/allen-nd-open-data</link>
      <guid>https://registry.opendata.aws/allen-nd-open-data</guid>
      <description>The Allen Institute for Neural Dynamics (AIND) is committed to FAIR, Open, and Reproducible science. We therefore share all of the raw and derived data we collect publicly with rich metadata, including preliminary data collected during methods development, as near to the time of collection as possible.</description>
    </item>
    <item>
      <title>Analysis Ready Sentinel-1 Backscatter Imagery</title>
      <link>https://registry.opendata.aws/sentinel-1-rtc-indigo</link>
      <guid>https://registry.opendata.aws/sentinel-1-rtc-indigo</guid>
      <description>The &lt;a href&#x3D;&quot;https://sentinel.esa.int/web/sentinel/missions/sentinel-1&quot;&gt;Sentinel-1 mission&lt;/a&gt; is a constellation of
C-band Synthetic Aperature Radar (SAR) satellites from the European Space Agency launched since 2014.
These satellites collect observations of radar backscatter intensity day or night, regardless of the
weather conditions, making them enormously valuable for environmental monitoring.
These radar data have been processed from original Ground Range Detected (GRD) scenes into a Radiometrically
Terrain Corrected, tiled product suitable for analysis. This product is available over the Contiguous United States (CONUS)
since 2017 when Sentinel-1 data became globally available.</description>
    </item>
    <item>
      <title>Astrophysics Division Galaxy Morphology Benchmark Dataset</title>
      <link>https://registry.opendata.aws/apd_galaxymorph</link>
      <guid>https://registry.opendata.aws/apd_galaxymorph</guid>
      <description>Hubble Space Telescope imaging data and associated identification labels for galaxy morphology derived from citizen scientist labels from the Galaxy Zoo: Hubble project.</description>
    </item>
    <item>
      <title>CANOE (Canadian Aquatic Navigation for Observation of the Environment) Dataset</title>
      <link>https://registry.opendata.aws/canoe</link>
      <guid>https://registry.opendata.aws/canoe</guid>
      <description>This autonomous marine navigation dataset includes data from a 360-degree Navtech radar, a 128-beam Ouster OS1 lidar with integrated IMU, a Teledyne Bumblebee stereo camera, Oculus M3000d imaging sonar, motor inputs, and GNSS. This dataset was collected on a lake and reservoir in Ontario, Canada. The intended purpose of this dataset is to enable the development and benchmarking of autonomous navigation algorithms in aquatic environments. In the future, we hope to release localization and odometry benchmarks.</description>
    </item>
    <item>
      <title>CHIMERA</title>
      <link>https://registry.opendata.aws/chimera</link>
      <guid>https://registry.opendata.aws/chimera</guid>
      <description>This dataset contains the training data for the &lt;a href&#x3D;&quot;https://chimera.grand-challenge.org/&quot;&gt;CHIMERA - Combining HIstology, Medical imaging (radiology) and molEcular data for medical pRognosis and diAgnosis&lt;/a&gt; challenge. The CHIMERA Challenge aims to advance precision medicine in cancer care by addressing the critical need for multimodal data integration. Despite significant progress in AI, integrating transcriptomics, pathology, and radiology across clinical departments remains a complex challenge. Clinicians are faced with large, heterogeneous datasets that are difficult to analyze effectively. AI has the potential to unify multimodal data, but several technical barriers remain, such as defining appropriate fusion stages and handling missing modalities.</description>
    </item>
    <item>
      <title>CMS 2008-2010 Data Entrepreneurs’ Synthetic Public Use File (DE-SynPUF) in OMOP Common Data Model</title>
      <link>https://registry.opendata.aws/cmsdesynpuf-omop</link>
      <guid>https://registry.opendata.aws/cmsdesynpuf-omop</guid>
      <description>DE-SynPUF is provided here as a 1,000 person (1k), 100,000 person (100k), and 2,300,000 persom (2.3m) data sets in the &lt;a href&#x3D;&quot;https://www.ohdsi.org/data-standardization/&quot;&gt;OMOP Common Data Model&lt;/a&gt; format.  The DE-SynPUF was created with the goal of providing a realistic set of claims data in the public domain while providing the very highest degree of protection to the Medicare beneficiaries’ protected health information.  The purposes of the DE-SynPUF are to: &lt;ol&gt;
&lt;li&gt;allow data entrepreneurs to develop and create software and applications that may eventually be applied to actual CMS claims data;&lt;/li&gt;
&lt;li&gt;train researchers on the use and complexity of conducting analyses with CMS claims data prior to initiating the process to obtain access to actual CMS data; and,&lt;/li&gt;
&lt;li&gt;support safe data mining innovations that may reveal unanticipated knowledge gains while preserving beneficiary privacy.
The files have been designed so that programs and procedures created on the DE-SynPUF will function on CMS Limited Data Sets. The data structure of the Medicare DE-SynPUF is very similar to the CMS Limited Data Sets, but with a smaller number of variables.  The DE-SynPUF also provides a robust set of metadata on the CMS claims data that have not been previously available in the public domain.  Although the DE-SynPUF has very limited inferential research value to draw conclusions about Medicare beneficiaries due to the synthetic processes used to create the file, the Medicare DE-SynPUF does increase access to a realistic Medicare claims data file in a timely and less expensive manner to spur the innovation necessary to achieve the goals of better care for beneficiaries and improve the health of the population.&lt;/li&gt;
&lt;/ol&gt;
</description>
    </item>
    <item>
      <title>COVID-19 Genome Sequence Dataset</title>
      <link>https://registry.opendata.aws/ncbi-covid-19</link>
      <guid>https://registry.opendata.aws/ncbi-covid-19</guid>
      <description>This repository within the &lt;a href&#x3D;&quot;https://www.nih.gov/research-training/medical-research-initiatives/activ/tracking-resistance-coronavirus-evolution-trace&quot;&gt;ACTIV TRACE initiative&lt;/a&gt; houses a comprehensive collection of datasets related to SARS-CoV-2. The processing of SARS-CoV-2 Sequence Read Archive (SRA) files has been optimized to identify genetic variations in viral samples. This information is then presented in the Variant Call Format (VCF). Each VCF file corresponds to the SRA parent-run&amp;#39;s accession ID. Additionally, the data is available in the parquet format, making it easier to search and filter using the Amazon Athena Service. The SARS-CoV-2 Variant Calling Pipeline is designed to handle new data every six hours, with updates to the AWS ODP bucket occurring daily.</description>
    </item>
    <item>
      <title>COVID-19 Open Research Dataset (CORD-19)</title>
      <link>https://registry.opendata.aws/cord-19</link>
      <guid>https://registry.opendata.aws/cord-19</guid>
      <description>Full-text and metadata dataset of COVID-19 and coronavirus-related research articles optimized for machine readability.</description>
    </item>
    <item>
      <title>Common Screens</title>
      <link>https://registry.opendata.aws/comonscreens</link>
      <guid>https://registry.opendata.aws/comonscreens</guid>
      <description>A corpus of web screenshot and metadata data composed of over 70 million websites.</description>
    </item>
    <item>
      <title>Community Earth System Model v2 ARISE (CESM2 ARISE)</title>
      <link>https://registry.opendata.aws/ncar-cesm2-arise</link>
      <guid>https://registry.opendata.aws/ncar-cesm2-arise</guid>
      <description>Data from ARISE-SAI Experiments with CESM2</description>
    </item>
    <item>
      <title>Conformational Space of Short Peptides</title>
      <link>https://registry.opendata.aws/short_peptides</link>
      <guid>https://registry.opendata.aws/short_peptides</guid>
      <description>Co-managed by &lt;a href&#x3D;&quot;toyoko.io&quot;&gt;Toyoko&lt;/a&gt; and the &lt;a href&#x3D;&quot;http://ufq.unq.edu.ar/sbg/&quot;&gt;Structural Biology Group at the Universidad Nacional de Quilmes&lt;/a&gt;, this dataset allows us to explore the conformational space of all possible peptides using the 20 common amino acids. It consists of a collection of exhaustive molecular dynamics simulations of tripeptides and pentapeptides.</description>
    </item>
    <item>
      <title>Corn Kernel Counting Dataset</title>
      <link>https://registry.opendata.aws/intelinair_corn_kernel_counting</link>
      <guid>https://registry.opendata.aws/intelinair_corn_kernel_counting</guid>
      <description>Dataset associated with the March 2021 Frontiers in Robotics and AI paper &amp;quot;Broad Dataset and Methods for Counting and Localization of On-Ear Corn Kernels&amp;quot;, DOI: 10.3389/frobt.2021.627009</description>
    </item>
    <item>
      <title>Coupled Model Intercomparison Project Phase 5 (CMIP5) University of Wisconsin-Madison Probabilistic Downscaling Dataset</title>
      <link>https://registry.opendata.aws/noaa-uwpd-cmip5</link>
      <guid>https://registry.opendata.aws/noaa-uwpd-cmip5</guid>
      <description>The University of Wisconsin Probabilistic Downscaling (UWPD) is a statistically downscaled dataset based on the Coupled Model Intercomparison Project Phase 5 (CMIP5) climate models. UWPD consists of three variables, daily precipitation and maximum and minimum temperature. The spatial resolution is 0.1&lt;span&gt;&amp;#176;&lt;/span&gt;x0.1&lt;span&gt;&amp;#176;&lt;/span&gt; degree resolution for the United States and southern Canada east of the Rocky Mountains.
&lt;br/&gt;
&lt;br/&gt;
The downscaling methodology is not deterministic. Instead, to properly capture unexplained variability and extreme events, the methodology predicts a spatially and temporally varying Probability Density Function (PDF) for each variable. Statistics such as the mean, mean PDF and annual maximum statistics can be calculated directly from the daily PDF and these statistics are included in the dataset. In addition, “standard”, “raw” data is created by randomly sampling from the PDFs to create a “realization” of the local scale given the large-scale from the climate model. There are 3 realizations for temperature and 14 realizations for precipitation.
&lt;br/&gt;
&lt;br/&gt;
The directory structure of the data is as follows
&lt;br/&gt;
&lt;code&gt;[cmip_version]/[scenario]/[climate_model]/[ensemble_member]/&lt;/code&gt;
&lt;br/&gt;
The realizations are as follows
&lt;br/&gt;
&lt;code&gt;prcp_[realization_number]&lt;em&gt;[year].nc&lt;/code&gt;
&lt;code&gt;temp&lt;/em&gt;[realization_number]&lt;em&gt;[year].nc&lt;/code&gt;
&lt;br/&gt;
The time mean files averaged over certain year bounds are as follows
&lt;br/&gt;
&lt;code&gt;prcp_mean&lt;/em&gt;[year_bound_1]&lt;em&gt;[year_bound_2].nc&lt;/code&gt;
&lt;code&gt;temp_mean&lt;/em&gt;[year_bound_1]&lt;em&gt;[year_bound_2].nc&lt;/code&gt;
&lt;br/&gt;
The time-mean Cumulative Distribution Function (CDF) files are as follows
&lt;br/&gt;
&lt;code&gt;prcp_cdf&lt;/em&gt;[year_bound_1]&lt;em&gt;[year_bound_2].nc&lt;/code&gt;
&lt;code&gt;temp_cdf&lt;/em&gt;[year_bound_1]&lt;em&gt;[year_bound_2].nc&lt;/code&gt;
&lt;br/&gt;
The CDF of the annual maximum precipitation is given for each year in the record
&lt;code&gt;prcp_annual_max_cdf&lt;/em&gt;[start_year_of_scenario]_[end_year_of_scenario].nc&lt;/code&gt;
&lt;br /&gt;</description>
    </item>
    <item>
      <title>Crowdsourced Bathymetry</title>
      <link>https://registry.opendata.aws/noaa-dcdb-bathymetry-pds</link>
      <guid>https://registry.opendata.aws/noaa-dcdb-bathymetry-pds</guid>
      <description>Community provided bathymetry data collected in collaboration with the International Hydrographic Organization.</description>
    </item>
    <item>
      <title>DWD ICON-EU - dynamical.org Icechunk Zarr</title>
      <link>https://registry.opendata.aws/dynamical-dwd-icon-eu</link>
      <guid>https://registry.opendata.aws/dynamical-dwd-icon-eu</guid>
      <description>&lt;p&gt;ICON-EU is a regional weather forecast model operated by Deutscher Wetterdienst (DWD), Germany&#x27;s national meteorological service. ICON-EU is a nested configuration of DWD&#x27;s global ICON (Icosahedral Non-hydrostatic) model that provides high-resolution forecasts over Europe.&lt;/p&gt;
&lt;p&gt;These datasets have been translated to cloud-optimized Icechunk Zarr format by &lt;a href&#x3D;&quot;https://dynamical.org&quot;&gt;dynamical.org&lt;/a&gt;.&lt;/p&gt;
&lt;ul&gt;
  &lt;li&gt;&lt;a href&#x3D;&quot;https://dynamical.org/catalog/dwd-icon-eu-forecast-5-day/&quot;&gt;DWD ICON-EU forecast, 5 day&lt;/a&gt; - High-resolution weather forecasts for Europe from the ICON-EU model operated by Deutscher Wetterdienst (DWD).&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>Danish Meteorological Institute (DMI) Open Data Forecasts</title>
      <link>https://registry.opendata.aws/dmi-opendata</link>
      <guid>https://registry.opendata.aws/dmi-opendata</guid>
      <description>DMI forecast data consist of various models where each model contains different set of parameters relating to a specific domain like ocean (WAM), storm flooding (DKSS) or weather (HARMONIE)</description>
    </item>
    <item>
      <title>Defense Meteorology Satellite Program (DMSP) Auroral Particle Flux</title>
      <link>https://registry.opendata.aws/dmspssj</link>
      <guid>https://registry.opendata.aws/dmspssj</guid>
      <description>The United States Air Force (USAF) Defense Meteorological Satellite Program (DMSP) SSJ precipitating particle instrument measures in-situ total flux and energy distribution of electrons and ions at low earth orbit. These precipitating particles are of interest for space weather operations and research, in part because they produce aurora during normal and very strong geomagnetic storms. This dataset contains both sensor-level raw data (as detailed in Redmon et al. 2017) and a high-level machine-learning-ready data product.</description>
    </item>
    <item>
      <title>Discrete Reasoning Over the content of Paragraphs (DROP)</title>
      <link>https://registry.opendata.aws/allenai-drop</link>
      <guid>https://registry.opendata.aws/allenai-drop</guid>
      <description>The DROP dataset contains 96k Question and Answer pairs (QAs) over 6.7K paragraphs, split between train (77k QAs), development (9.5k QAs) and a hidden test partition (9.5k QAs).</description>
    </item>
    <item>
      <title>ECMWF AIFS ENS - dynamical.org Icechunk Zarr</title>
      <link>https://registry.opendata.aws/dynamical-ecmwf-aifs-ens</link>
      <guid>https://registry.opendata.aws/dynamical-ecmwf-aifs-ens</guid>
      <description>&lt;p&gt;The Artificial Intelligence Forecasting System (AIFS) is a data driven forecast model developed by the European Centre for Medium-Range Weather Forecasts (ECMWF). AIFS-ENS is the ensemble configuration of AIFS, containing 51 ensemble members. AIFS is trained on ECMWF&#x27;s ERA5 re-analysis and ECMWF&#x27;s operational numerical weather prediction (NWP) analyses.&lt;/p&gt;
&lt;p&gt;These datasets have been translated to cloud-optimized Icechunk Zarr format by &lt;a href&#x3D;&quot;https://dynamical.org&quot;&gt;dynamical.org&lt;/a&gt;.&lt;/p&gt;
&lt;ul&gt;
  &lt;li&gt;&lt;a href&#x3D;&quot;https://dynamical.org/catalog/ecmwf-aifs-ens-forecast/&quot;&gt;ECMWF AIFS ENS forecast&lt;/a&gt; - Ensemble weather forecasts from the ECMWF Artificial Intelligence Forecasting System (AIFS) ENS model.&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>ECMWF IFS ENS - dynamical.org Icechunk Zarr</title>
      <link>https://registry.opendata.aws/dynamical-ecmwf-ifs-ens</link>
      <guid>https://registry.opendata.aws/dynamical-ecmwf-ifs-ens</guid>
      <description>&lt;p&gt;The Integrated Forecasting System (IFS) is a global forecast model developed by ECMWF. ENS is an ensemble configuration of IFS, containing 51 ensemble members. IFS consists of a numerical model of the Earth system, which includes an atmospheric model at its heart, coupled with models of other Earth system components such as the ocean. The data assimilation system combines the latest weather observations with a recent forecast to obtain the best possible estimate of the current state of the Earth system.&lt;/p&gt;
&lt;p&gt;These datasets have been translated to cloud-optimized Icechunk Zarr format by &lt;a href&#x3D;&quot;https://dynamical.org&quot;&gt;dynamical.org&lt;/a&gt;.&lt;/p&gt;
&lt;ul&gt;
  &lt;li&gt;&lt;a href&#x3D;&quot;https://dynamical.org/catalog/ecmwf-ifs-ens-forecast-15-day-0-25-degree/&quot;&gt;ECMWF IFS ENS forecast, 15 day, 0.25 degree&lt;/a&gt; - Ensemble weather forecasts from the ECMWF Integrated Forecasting System (IFS).&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>ERA5-for-WRF Open Data on AWS</title>
      <link>https://registry.opendata.aws/era5-for-wrf</link>
      <guid>https://registry.opendata.aws/era5-for-wrf</guid>
      <description>ERA5 reanalysis data on AWS, preprocessed for use with the Weather Research and Forecasting (WRF) model.</description>
    </item>
    <item>
      <title>East Coast Community Ocean Forecast System (ECCOFS)</title>
      <link>https://registry.opendata.aws/noaa-nos-eccofs</link>
      <guid>https://registry.opendata.aws/noaa-nos-eccofs</guid>
      <description>The East Coast Community Ocean Forecast System (ECCOFS) is a data assimilating ocean analysis and forecast system being developed by Rutgers University, the University of California Santa Cruz, Fathom Science Inc., and the National Ocean Service (NOS) of NOAA for transition to operations at NCEP in 2028. The ECCOFS domain spans the eastern seaboard of North America and Intra-Americas Seas from the Grand Banks of Newfoundland in the north to the mouth of the Orinoco River, Venezuela, in the south. ECCOFS will complement the existing WCOFS (West Coast Operational Forecast System) to achieve complete forecast coverage of U.S. territorial seas adjacent to the 48 contiguous states and Puerto Rico. Each day ECCOFS generates an ocean analysis using the Regional Ocean Modeling System (ROMS) 4-Dimensional Variational (4D-Var) data assimilation (DA) system constrained by ocean observations. The forecast resolution is 3 km in the horizontal at 50 vertical terrain-following levels. A more detailed overview is presented &lt;a href&#x3D;&quot;https://github.com/myroms/roms_eccofs/wiki/Overview&quot;&gt;here&lt;/a&gt;. 
&lt;br&gt;&lt;br&gt;
The meteorological forcing data are marine boundary layer conditions (air temperature, humidity, pressure), net shortwave radiation, and downward longwave radiation at 1-hourly intervals from the NWS High Resolution Rapid Refresh (HRRR) 4-km, 48-hour forecast for the northwest Atlantic Ocean and western Caribbean Sea. In regions beyond the HRRR domain, and in forecast days 3 to 5, the NWS GFS (Global Forecast System) forecast is adopted.
&lt;br&gt;&lt;br&gt;
Sub-tidal frequency open boundary conditions are drawn from the Copernicus Marine Service Global Ocean Physics Analysis and Forecast (GLOBAL_ANALYSISFORECAST_PHY_001_024). These data are augmented by boundary harmonic barotropic tidal forcing from the Oregon State University TPXO analysis (12 harmonic constituents, adjusted for the 18.6-year nodal cycle). Luni-solar gravitational tide generating forces for 7 constituents are imposed in the ECCOFS domain interior.
&lt;br&gt;&lt;br&gt;
Daily average forecast river discharge data from the Global Flood Awareness System (GloFAS) river routing model of ECMWF precipitation set freshwaiter inflows at 93 rivers where annual mean discharge exceeds 50 m3/s. More details on the forward model configuration are presented &lt;a href&#x3D;&quot;https://github.com/myroms/roms_eccofs/wiki/Modeling-System-Configuration#Forward-Model-and-Forcing&quot;&gt;here&lt;/a&gt;.
&lt;br&gt;&lt;br&gt;
Observations presently assimilated include satellite sea level and temperature, and in situ temperature and salinity from moorings, drifters, profiling floats, autonomous underwater vehicles, ships of opportunity, and sensors affixed to fishing gear. When fully configured, ECCOFS will also assimilate satellite salinity, ocean surface currents measured by land-based high-frequency radars, and temperature data from animal tags.
&lt;br&gt;&lt;br&gt;
Recognizing that oceanic conditions that can be meaningfully constrained by existing observing networks have length scales much greater than the forecast model resolution of 3 km, ECCOFS employs a Mixed Resolution assimilation approach wherein the ocean forecast is computed on the 3-km grid, but the iterations of the Tangent Linear (TL) and Adjoint (AD) model inner loops of 4D-Var are computed on a lower resolution (6-km) grid that demands less time for execution.  The control variables of the assimilation are the initial conditions (at day 0 minus 3) and time varying boundary conditions (over 3 days). More details on the assimilation methodology are presented &lt;a href&#x3D;&quot;https://github.com/myroms/roms_eccofs/wiki/Modeling-System-Configuration#data-assimilation-methodology&quot;&gt;here&lt;/a&gt;. 
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>End of Term Web Archive Dataset</title>
      <link>https://registry.opendata.aws/eot-web-archive</link>
      <guid>https://registry.opendata.aws/eot-web-archive</guid>
      <description>The End of Term Web Archive (EOT) captures and saves U.S. Government websites at the end of presidential administrations.  The EOT has thus far preserved websites from administration changes in 2008, 2012, 2016, 2020  and 2024.  Data from these web crawls have been made openly available in several formats in this dataset.</description>
    </item>
    <item>
      <title>Ensemble Meteorological Dataset for Planet Earth, EM-Earth</title>
      <link>https://registry.opendata.aws/emearth</link>
      <guid>https://registry.opendata.aws/emearth</guid>
      <description>EM-Earth provides data for precipitation, mean air temperature, air temperature range, and dew-point temperature at 0.1° spatial resolution over global land areas from 1950 to 2019. EM-Earth provides hourly/daily deterministic estimates, and daily probabilistic estimates (25 ensemble members), to meet the diverse requirements of hydrometeorological applications.</description>
    </item>
    <item>
      <title>Essential-Web v1.0: 24T tokens of organized web data</title>
      <link>https://registry.opendata.aws/eai-essential-web-v1</link>
      <guid>https://registry.opendata.aws/eai-essential-web-v1</guid>
      <description>A 24-trillion-token dataset in which every document is annotated with a twelve-category taxonomy covering topic, format, content complexity, and quality.</description>
    </item>
    <item>
      <title>GEDI L4A Footprint Level Aboveground Biomass Density, Version 2.1</title>
      <link>https://registry.opendata.aws/nasa-gedil4aagbdensityv212056</link>
      <guid>https://registry.opendata.aws/nasa-gedil4aagbdensityv212056</guid>
      <description>This dataset contains Global Ecosystem Dynamics Investigation (GEDI) Level 4A (L4A) Version 2 predictions of the aboveground biomass density (AGBD; in Mg/ha) and estimates of the prediction standard error within each sampled geolocated laser footprint. In this version, the granules are in sub-orbits. The algorithm setting group selection used for GEDI02_A Version 2 has been modified for Evergreen Broadleaf Trees in South America to reduce false positive errors resulting from the selection of waveform modes above ground elevation as the lowest mode. The footprints are located within the global latitude band observed by the International Space Station (ISS), nominally 51.6 degrees N and S and reported for the period 2019-04-18 to 2024-11-27. No acquisitions occurred while the GEDI instrument was in storage on the International Space Station (ISS) from March 2023 to April 2024. The GEDI instrument consists of three lasers producing a total of eight beam ground transects, which instantaneously sample eight ~25 m footprints spaced approximately every 60 m along-track. The GEDI beam transects are spaced approximately 600 m apart on the Earth&amp;#39;s surface in the cross-track direction, for an across-track width of ~4.2 km. Footprint AGBD was derived from parametric models that relate simulated GEDI Level 2A (L2A) waveform relative height (RH) metrics to field plot estimates of AGBD. Height metrics from simulated waveforms associated with field estimates of AGBD from multiple regions and plant functional types (PFTs) were compiled to generate a calibration dataset for models representing the combinations of world regions and PFTs (i.e., deciduous broadleaf trees, evergreen broadleaf trees, evergreen needleleaf trees, deciduous needleleaf trees, and the combination of grasslands, shrubs, and woodlands). For each of the eight beams, additional data are reported with the AGBD estimates, including the associated uncertainty metrics, quality flags, model inputs, and other information about the GEDI L2A waveform for this selected algorithm setting group. Model inputs include the scaled and transformed GEDI L2A RH metrics, footprint geolocation variables and land cover input data including PFTs and the world region identifiers. Additional model outputs include the AGBD predictions for each of the six GEDI L2A algorithm setting groups with AGBD in natural and transformed units and associated prediction uncertainty for each GEDI L2A algorithm setting group. Providing these ancillary data products will allow users to evaluate and select alternative algorithm setting groups. Also provided are outputs of parameters and variables from the L4A models used to generate AGBD predictions that are required as input to the GEDI04_B algorithm to generate 1-km gridded products.
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.ornldaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;https://data.ornldaac.earthdata.nasa.gov/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>Geosnap Data, Center for Geospatial Sciences</title>
      <link>https://registry.opendata.aws/spatial-ucr</link>
      <guid>https://registry.opendata.aws/spatial-ucr</guid>
      <description>This bucket contains multiple datasets (as Quilt packages) created by the
Center for Geospatial Sciences (CGS) at the University of California-Riverside.
The data in this bucket contains the following:&lt;ol&gt;
&lt;li&gt;Tabular and geographic data from the US Census&lt;/li&gt;
&lt;li&gt;Land Cover imagery collected from &lt;a href&#x3D;&quot;https://www.mrlc.gov/&quot;&gt;Multi-Resolution Land Characteristics Consortium&lt;/a&gt;&lt;/li&gt;
&lt;li&gt;Road network data processed from OpenStreetMap&lt;/li&gt;
&lt;/ol&gt;
</description>
    </item>
    <item>
      <title>Global Biodiversity Information Facility (GBIF) Species Occurrences</title>
      <link>https://registry.opendata.aws/gbif</link>
      <guid>https://registry.opendata.aws/gbif</guid>
      <description>The Global Biodiversity Information Facility (GBIF) is an international network and data infrastructure funded by the world&amp;#39;s governments providing global data that document the occurrence of species. GBIF currently integrates datasets documenting over 1.6 billion species occurrences, growing daily. The GBIF occurrence dataset combines data from a wide array of sources including specimen-related data from natural history museums, observations from citizen science networks and environment recording schemes. While these data are constantly changing at GBIF.org, periodic snapshots are taken and made available on AWS.</description>
    </item>
    <item>
      <title>HLS Landsat Operational Land Imager Surface Reflectance and TOA Brightness Daily Global 30m v2.0</title>
      <link>https://registry.opendata.aws/nasa-hlsl30</link>
      <guid>https://registry.opendata.aws/nasa-hlsl30</guid>
      <description>The Harmonized Landsat Sentinel-2 (HLS) project provides consistent surface reflectance (SR) and top of atmosphere (TOA) brightness data from a virtual constellation of satellite sensors. The Operational Land Imager (OLI) is housed aboard the joint NASA/USGS Landsat 8 and Landsat 9 satellites, while the Multi-Spectral Instrument (MSI) is mounted aboard Europe’s Copernicus Sentinel-2A, Sentinel-2B, and Sentinel-2C satellites. The combined measurement enables global observations of the land every 2–3 days at 30-meter (m) spatial resolution. The HLS project uses a set of algorithms to obtain seamless products from OLI and MSI that include atmospheric correction, cloud and cloud-shadow masking, spatial co-registration and common gridding, illumination and view angle normalization, and spectral bandpass adjustment.The HLSL30 product provides 30-m Nadir Bidirectional Reflectance Distribution Function (BRDF)-Adjusted Reflectance (NBAR) and is derived from Landsat 8/9 OLI data products. The &lt;a href&#x3D;&quot;https://doi.org/10.5067/HLS/HLSS30.002&quot;&gt;HLSS30&lt;/a&gt; and HLSL30 products are gridded to the same resolution and Military Grid Reference System (&lt;a href&#x3D;&quot;https://hls.gsfc.nasa.gov/products-description/tiling-system/&quot;&gt;MGRS&lt;/a&gt;) tiling system and thus are “stackable” for time series analysis.The HLSL30 product is provided in Cloud Optimized GeoTIFF (COG) format, and each band is distributed as a separate file. There are 11 bands included in the HLSL30 product along with one quality assessment (QA) band and four angle bands. See the User Guide for a more detailed description of the individual bands provided in the HLSL30 product.Known Issues&lt;ul&gt;
&lt;li&gt;Unrealistically high aerosol and low surface reflectance over bright areas: The atmospheric correction over bright targets occasionally retrieves unrealistically high aerosol and thus makes the surface reflectance too low. High aerosol retrievals, both false high aerosol and realistically high aerosol, are masked when quality bits 6 and 7 are both set to 1 (see Table 9 in the &lt;a href&#x3D;&quot;https://lpdaac.usgs.gov/documents/1698/HLS_User_Guide_V2.pdf&quot;&gt;User Guide&lt;/a&gt;); the corresponding spectral data should be discarded from analysis.&lt;/li&gt;
&lt;li&gt;Issues over high latitudes: For scenes greater than or equal to 80 degrees north, multiple overpasses can be gridded into a single MGRS tile resulting in an L30 granule with data sensed at two different times. In this same area, it is also possible that Landsat overpasses that should be gridded into a single MGRS tile are actually written as separate data files. Finally, for scenes with a latitude greater than or equal to 65 degrees north, ascending Landsat scenes may have a slightly higher error in the BRDF correction because the algorithm is calibrated using descending scenes.&lt;/li&gt;
&lt;li&gt;Fmask omission errors: There are known issues regarding the Fmask band of this data product that impacts HLSL30 data prior to April of 2022. The HLS Fmask data band may have omission errors in water detection for cases where water detection using spectral data alone is difficult, and omission and commission errors in cloud shadow detection for areas with great topographic relief. This issue does not impact other bands in the dataset.&lt;/li&gt;
&lt;li&gt;Inconsistent snow surface reflectance between Landsat and Sentinel-2: The HLS snow surface reflectance can be highly inconsistent between Landsat and Sentinel-2. When assessed on same-day acquisitions from Landsat and Sentinel-2, Landsat reflectance is generally higher than Sentinel-2 reflectance in the visible bands.&lt;/li&gt;
&lt;li&gt;Unrealistically high snow surface reflectance in the visible bands: By design, the Land Surface Reflectance Code (LaSRC) atmospheric correction does not attempt aerosol retrieval over snow; instead, a default aerosol optical thickness (AOT) is used to drive the snow surface reflectance. If the snow detection fails, the full LaSRC is used in both AOT retrieval and surface reflectance derivation over snow, which produces surface reflectance values as high as 1.6 in the visible bands. This is a common problem for spring images at high latitudes.&lt;/li&gt;
&lt;li&gt;Unrealistically low surface reflectance surrounding snow/ice: Related to the above, the AOT retrieval over snow/ice is generally too high. When this artificially high AOT is used to derive the surface reflectance of the neighboring non-snow pixels, very low surface reflectance will result. These pixels will appear very dark in the visible bands. If the surface reflectance value of a pixel is below -0.2, a NO_DATA value of -9999 is used.&lt;/li&gt;
&lt;li&gt;Unrealistically low reflectance surrounding clouds: Like for snow, the HLS atmospheric correction does not attempt aerosol retrieval over clouds and a default AOT is used instead. But if the cloud detection fails, an artificially high AOT will be retrieved over clouds. If the high AOT is used to derive the surface reflectance of the neighboring cloud-free pixels, very low surface reflectance values will result. If the surface reflectance value of a pixel is below -0.2, a NO_DATA value of -9999 is used. &lt;/li&gt;
&lt;li&gt;Unusually low reflectance around other bright land targets: While the HLS atmospheric correction retrieves AOT over non-cloud, non-snow bright pixels, the retrieved AOT over bright targets can be unrealistically high in some cases, similar to cloud or snow. If this unrealistically high AOT is used to derive the surface reflectance of the neighboring pixels, very low surface reflectance values can result as shown in Figure 2. If the surface reflectance value of a pixel is below -0.2, a NO_DATA value of -9999 is used. These types of bright targets are mostly man-made, such as buildings, parking lots, and roads.  &lt;/li&gt;
&lt;li&gt;Dark plumes over water: The HLS atmospheric correction does not attempt aerosol retrieval over water. For water pixels, the AOT retrieved from the nearest land pixels is used to derive the surface reflectance, but if the retrieval is incorrect, e.g. from a cloud pixel, this high AOT will create dark stripes over water, as shown in Figure 3. This happens more often over large water bodies, such as lakes and bays, than over narrow rivers.  &lt;/li&gt;
&lt;li&gt;Landsat WRS-2 Path/Row boundary in L30 reflectance: HLS performs atmospheric correction on Landsat Level 1 images in the original Worldwide Reference System 2 (WRS2) path/row before the derived surface reflectance is reprojected into Military Grid Reference System (MGRS) tiles. If a WRS-2 Landsat image is very cloudy, the AOT from a few remaining clear pixels might be used for the atmospheric correction of the entire image. The AOT that is used can be quite different from the value for the adjacent row in the same path, which results in an artificial abrupt change from one row to the next, as shown in Figure 4. This occurrence is very rare.  &lt;/li&gt;
&lt;li&gt;Landsat WRS2 path/row boundary in cloud masks: The cloud mask algorithm Fmask creates mask labels by applying thresholds to the histograms of some metrics for each path/row independently. If two adjacent rows in the same path have distinct distributions within the metrics, abrupt changes in masking patterns can appear across the row boundary, as shown in Figure 5. This occurrence is very rare.  &lt;/li&gt;
&lt;li&gt;Fmask configuration was deficient for 2-3 months in 2021: The HLS installation of Fmask failed to include auxiliary digital elevation model (DEM) and European Space Agency (ESA) Global Surface Water Occurrence data for a 2-3 month run in 2021. This impacted the masking results over water and in mountainous regions. &lt;/li&gt;
&lt;li&gt;The reflectance “scale_factor” and “offset” for some L30 and S30 bands were not set: The HLS reflectance scaling factor is 0.0001 and offset is 0. However, this information was not set in the Cloud Optimized GeoTIFF (COG) files of some bands for a small number of granules. The lack of this information creates a problem for automatic conversion of the reflectance data, requiring explicit scaling in applications. The problem has been corrected, but the affected granules have not been reprocessed. &lt;/li&gt;
&lt;li&gt;Incomplete map projection information: For a time, HLS imagery was produced with an incomplete coordinate reference system (CRS). The metadata contains the Universal Transverse Mercator (UTM) zone and coordinates necessary to geolocate pixels within the image but might not be in a standard form, especially for granules produced early in the HLS mission. As a result, an error will occur in certain image processing packages due to the incomplete CRS. The simplest solution is to update to the latest version of Geospatial Data Abstraction Library (GDAL) and/or rasterio, which use the available information without error. &lt;/li&gt;
&lt;li&gt;False northing of 10^7 for the L30 angle data: The L30 and S30 products do not use a false northing for the UTM projection, and the angle data are supposed to follow the same convention. However, the L30 angle data incorrectly uses a false northing of 10^7. There is no problem with the angle data itself, but the false northing needs to be set to 0 for it to be aligned with the reflectance.&lt;/li&gt;
&lt;li&gt;L30 from Landsat L1GT scenes: Landsat L1GT scenes were not intended for HLS due to their poor geolocation. However, some scenes made it through screening for a short period of HLS production. L1GT L30 scenes mainly consist of extensive cloud or snow that can be eliminated using the Fmask quality bits layer. Users can also identify an L1GT-originated L30 granule by examining the HLS cmr.xml metadata file.&lt;/li&gt;
&lt;li&gt;The UTC dates in the L30/S30 filenames may not be the local dates: UTC dates are used by ESA and the U.S. Geological Survey (USGS) in naming their Level 1 images, and HLS processing retains this information to name the L30 and S30 products. Landsat and Sentinel-2 overpass eastern Australia and New Zealand around 10AM local solar time, but this area is in either UTC+10:00 or +11:00 zone; therefore, the UTC time for some orbits is in fact near the end of the preceding UTC day. For example, HLS.S30.T59HQS.2016117T221552.v2.0 was acquired in the 22nd hour of day 117 of year 2016 in UTC, but the time was 10:15:52 of day 118 locally. Approximately 100 minutes later HLS.S30.T56JML.2016117T235252.v2.0 was acquired in the next orbit in eastern Australia.    This issue also occurs for Landsat. For example, HLS.L30.T59HQS.2016117T221209.v2.0 was acquired on the same day as the first S30 example given above, but both on day 118 of 2016 locally. Adding to the confusion for L30, in the same region, Landsat 8 and 9 can each overpass once in one of the two adjacent WRS-2 Paths (91/92/93) over a two-day period on a local calendar, but based on UTC time, the two overpasses can appear to be on the same day. For example, in the following seemingly same-day pair, the second L30 is actually for day 168 locally:&lt;br&gt;   HLS.L30.T55GCN.2023167T000407.v2.0&lt;br&gt;   HLS.L30.T55GCN.2023167T235747.v2.0&lt;br&gt;   Bear in mind, the date peculiarity for the data occurs when the overpass time is during the late hours of a UTC day. &lt;/li&gt;
&lt;li&gt;The atmospheric ancillary data from the wrong date was used for LaSRC: Related to the above, for eastern Australia and New Zealand, L30 and S30 surface reflectance on certain days was created using the atmospheric ancillary data from a date that was one day too early. The exact geographic extent of the affected HLS products and the impact on the surface reflectance quality are under investigation. Practice caution when using data with overpass times during the late hours of a UTC day.&lt;/li&gt;
&lt;li&gt;Duplicates in L30: The Landsat 9 acquisitions from October 2021 to March 2023 in Landsat Collection 2 were reprocessed by USGS in March 2023. This reprocessing updated the overpass time by a fraction of a second for some scenes. Since HLS uses overpass time as part of the L30 filename, the older L30 granules were not automatically overwritten due to the different filenames. For example, the first L30 granule in the following pair originated from an older version of L1TP of Landsat 9 with the second granule originating from the reprocessed version.&lt;br&gt;HLS.L30.T11SLC.2022166T182646.v2.0&lt;br&gt;HLS.L30.T11SLC.2022166T182645.v2.0&lt;br&gt;There are other causes of duplicate L30 granules, but the overall number of duplicates is very small.&lt;/li&gt;
&lt;li&gt;Poor Geolocation: A large amount of granules that were processed for May through July 2023 were created with L1GT input scenes which were deemed undesirable due to a poor geolocation issue. These granules were removed from the archive. (see the full list of removed &lt;a href&#x3D;&quot;https://lpdaac.usgs.gov/documents/2161/L30_L1GT_granules_May_July_2023.csv&quot;&gt;granules&lt;/a&gt;)&lt;/li&gt;
&lt;/ul&gt;
Improvements/Changes from Previous Versions&lt;ul&gt;
&lt;li&gt;Aerosol QA bits from the USGS Land Surface Reflectance Code (LaSRC) model output have been added into the Function of Mask (Fmask) data layer. The added two bits indicate the aerosol levels: high, medium, low, and climatology aerosol.
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&lt;/a&gt;&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>HLS Sentinel-2 Multi-spectral Instrument Surface Reflectance Daily Global 30m v2.0</title>
      <link>https://registry.opendata.aws/nasa-hlss30</link>
      <guid>https://registry.opendata.aws/nasa-hlss30</guid>
      <description>The Harmonized Landsat Sentinel-2 (HLS) project provides consistent surface reflectance data from the Operational Land Imager (OLI) aboard the joint NASA/USGS Landsat 8 satellite and the Multi-Spectral Instrument (MSI) aboard Europe’s Copernicus Sentinel-2A, Sentinel-2B, and Sentinel-2C satellites. The combined measurement enables global observations of the land every 2–3 days at 30-meter (m) spatial resolution. The HLS project uses a set of algorithms to obtain seamless products from OLI and MSI that include atmospheric correction, cloud and cloud-shadow masking, spatial co-registration and common gridding, illumination and view angle normalization, and spectral bandpass adjustment. The HLSS30 product provides 30-m Nadir Bidirectional Reflectance Distribution Function (BRDF)-Adjusted Reflectance (NBAR) and is derived from Sentinel-2A, Sentinel-2B, and Sentinel-2C MSI data products. The HLSS30 and &lt;a href&#x3D;&quot;https://doi.org/10.5067/HLS/HLSL30.002&quot;&gt;HLSL30&lt;/a&gt; products are gridded to the same resolution and Military Grid Reference System (&lt;a href&#x3D;&quot;https://hls.gsfc.nasa.gov/products-description/tiling-system/&quot;&gt;MGRS&lt;/a&gt;) tiling system and thus are “stackable” for time series analysis.The HLSS30 product is provided in Cloud Optimized GeoTIFF (COG) format, and each band is distributed as a separate COG. There are 13 bands included in the HLSS30 product along with four angle bands and a quality assessment (QA) band. See the User Guide for a more detailed description of the individual bands provided in the HLSS30 product.Known Issues&lt;ul&gt;
&lt;li&gt;Unrealistically high aerosol and low surface reflectance over bright areas: The atmospheric correction over bright targets occasionally retrieves unrealistically high aerosol and thus makes the surface reflectance too low. High aerosol retrievals, both false high aerosol and realistically high aerosol, are masked when quality bits 6 and 7 are both set to 1 (see Table 9 in the &lt;a href&#x3D;&quot;https://lpdaac.usgs.gov/documents/1698/HLS_User_Guide_V2.pdf&quot;&gt;User Guide&lt;/a&gt;); the corresponding spectral data should be discarded from analysis.&lt;/li&gt;
&lt;li&gt;Issues over high latitudes: For scenes greater than or equal to 80 degrees north, multiple overpasses can be gridded into a single MGRS tile resulting in an L30 granule with data sensed at two different times. In this same area, it is also possible that Landsat overpasses that should be gridded into a single MGRS tile are actually written as separate data files. Finally, for scenes with a latitude greater than or equal to 65 degrees north, ascending Landsat scenes may have a slightly higher error in the BRDF correction because the algorithm is calibrated using descending scenes.&lt;/li&gt;
&lt;li&gt;Fmask omission errors: There are known issues regarding the Fmask band of this data product that impacts HLSL30 data prior to April of 2022. The HLS Fmask data band may have omission errors in water detection for cases where water detection using spectral data alone is difficult, and omission and commission errors in cloud shadow detection for areas with great topographic relief. This issue does not impact other bands in the dataset.&lt;/li&gt;
&lt;li&gt;Inconsistent snow surface reflectance between Landsat and Sentinel-2: The HLS snow surface reflectance can be highly inconsistent between Landsat and Sentinel-2. When assessed on same-day acquisitions from Landsat and Sentinel-2, Landsat reflectance is generally higher than Sentinel-2 reflectance in the visible bands.&lt;/li&gt;
&lt;li&gt;Unrealistically high snow surface reflectance in the visible bands: By design, the Land Surface Reflectance Code (LaSRC) atmospheric correction does not attempt aerosol retrieval over snow; instead, a default aerosol optical thickness (AOT) is used to drive the snow surface reflectance. If the snow detection fails, the full LaSRC is used in both AOT retrieval and surface reflectance derivation over snow, which produces surface reflectance values as high as 1.6 in the visible bands. This is a common problem for spring images at high latitudes.&lt;/li&gt;
&lt;li&gt;Unrealistically low surface reflectance surrounding snow/ice: Related to the above, the AOT retrieval over snow/ice is generally too high. When this artificially high AOT is used to derive the surface reflectance of the neighboring non-snow pixels, very low surface reflectance will result. These pixels will appear very dark in the visible bands. If the surface reflectance value of a pixel is below -0.2, a NO_DATA value of -9999 is used. In Figure 1, the pixels in front of the glaciers have surface reflectance values that are too low.  &lt;/li&gt;
&lt;li&gt;Unrealistically low reflectance surrounding clouds: Like for snow, the HLS atmospheric correction does not attempt aerosol retrieval over clouds and a default AOT is used instead. But if the cloud detection fails, an artificially high AOT will be retrieved over clouds. If the high AOT is used to derive the surface reflectance of the neighboring cloud-free pixels, very low surface reflectance values will result. If the surface reflectance value of a pixel is below -0.2, a NO_DATA value of -9999 is used. &lt;/li&gt;
&lt;li&gt;Unusually low reflectance around other bright land targets: While the HLS atmospheric correction retrieves AOT over non-cloud, non-snow bright pixels, the retrieved AOT over bright targets can be unrealistically high in some cases, similar to cloud or snow. If this unrealistically high AOT is used to derive the surface reflectance of the neighboring pixels, very low surface reflectance values can result as shown in Figure 2. If the surface reflectance value of a pixel is below -0.2, a NO_DATA value of -9999 is used. These types of bright targets are mostly man-made, such as buildings, parking lots, and roads.  &lt;/li&gt;
&lt;li&gt;Dark plumes over water: The HLS atmospheric correction does not attempt aerosol retrieval over water. For water pixels, the AOT retrieved from the nearest land pixels is used to derive the surface reflectance, but if the retrieval is incorrect, e.g. from a cloud pixel, this high AOT will create dark stripes over water, as shown in Figure 3. This happens more often over large water bodies, such as lakes and bays, than over narrow rivers.  &lt;/li&gt;
&lt;li&gt;Landsat WRS-2 Path/Row boundary in L30 reflectance: HLS performs atmospheric correction on Landsat Level 1 images in the original Worldwide Reference System 2 (WRS2) path/row before the derived surface reflectance is reprojected into Military Grid Reference System (MGRS) tiles. If a WRS-2 Landsat image is very cloudy, the AOT from a few remaining clear pixels might be used for the atmospheric correction of the entire image. The AOT that is used can be quite different from the value for the adjacent row in the same path, which results in an artificial abrupt change from one row to the next, as shown in Figure 4. This occurrence is very rare.  &lt;/li&gt;
&lt;li&gt;Landsat WRS2 path/row boundary in cloud masks: The cloud mask algorithm Fmask creates mask labels by applying thresholds to the histograms of some metrics for each path/row independently. If two adjacent rows in the same path have distinct distributions within the metrics, abrupt changes in masking patterns can appear across the row boundary, as shown in Figure 5. This occurrence is very rare.  &lt;/li&gt;
&lt;li&gt;Fmask configuration was deficient for 2-3 months in 2021: The HLS installation of Fmask failed to include auxiliary digital elevation model (DEM) and European Space Agency (ESA) Global Surface Water Occurrence data for a 2-3 month run in 2021. This impacted the masking results over water and in mountainous regions. &lt;/li&gt;
&lt;li&gt;The reflectance “scale_factor” and “offset” for some L30 and S30 bands were not set: The HLS reflectance scaling factor is 0.0001 and offset is 0. However, this information was not set in the Cloud Optimized GeoTIFF (COG) files of some bands for a small number of granules. The lack of this information creates a problem for automatic conversion of the reflectance data, requiring explicit scaling in applications. The problem has been corrected, but the affected granules have not been reprocessed. &lt;/li&gt;
&lt;li&gt;Incomplete map projection information: For a time, HLS imagery was produced with an incomplete coordinate reference system (CRS). The metadata contains the Universal Transverse Mercator (UTM) zone and coordinates necessary to geolocate pixels within the image but might not be in a standard form, especially for granules produced early in the HLS mission. As a result, an error will occur in certain image processing packages due to the incomplete CRS. The simplest solution is to update to the latest version of Geospatial Data Abstraction Library (GDAL) and/or rasterio, which use the available information without error. &lt;/li&gt;
&lt;li&gt;False northing of 10^7 for the L30 angle data: The L30 and S30 products do not use a false northing for the UTM projection, and the angle data are supposed to follow the same convention. However, the L30 angle data incorrectly uses a false northing of 10^7. There is no problem with the angle data itself, but the false northing needs to be set to 0 for it to be aligned with the reflectance.&lt;/li&gt;
&lt;li&gt;L30 from Landsat L1GT scenes: Landsat L1GT scenes were not intended for HLS due to their poor geolocation. However, some scenes made it through screening for a short period of HLS production. L1GT L30 scenes mainly consist of extensive cloud or snow that can be eliminated using the Fmask quality bits layer. Users can also identify an L1GT-originated L30 granule by examining the HLS cmr.xml metadata file.&lt;/li&gt;
&lt;li&gt;The UTC dates in the L30/S30 filenames may not be the local dates: UTC dates are used by ESA and the U.S. Geological Survey (USGS) in naming their Level 1 images, and HLS processing retains this information to name the L30 and S30 products. Landsat and Sentinel-2 overpass eastern Australia and New Zealand around 10AM local solar time, but this area is in either UTC+10:00 or +11:00 zone; therefore, the UTC time for some orbits is in fact near the end of the preceding UTC day. For example, HLS.S30.T59HQS.2016117T221552.v2.0 was acquired in the 22nd hour of day 117 of year 2016 in UTC, but the time was 10:15:52 of day 118 locally. Approximately 100 minutes later HLS.S30.T56JML.2016117T235252.v2.0 was acquired in the next orbit in eastern Australia.     This issue also occurs for Landsat. For example, HLS.L30.T59HQS.2016117T221209.v2.0 was acquired on the same day as the first S30 example given above, but both on day 118 of 2016 locally. Adding to the confusion for L30, in the same region, Landsat 8 and 9 can each overpass once in one of the two adjacent WRS-2 Paths (91/92/93) over a two-day period on a local calendar, but based on UTC time, the two overpasses can appear to be on the same day. For example, in the following seemingly same-day pair, the second L30 is actually for day 168 locally:&lt;br&gt;   HLS.L30.T55GCN.2023167T000407.v2.0&lt;br&gt;   HLS.L30.T55GCN.2023167T235747.v2.0&lt;br&gt;   Bear in mind, the date peculiarity for the data occurs when the overpass time is during the late hours of a UTC day.  &lt;/li&gt;
&lt;li&gt;The atmospheric ancillary data from the wrong date was used for LaSRC: Related to the above, for eastern Australia and New Zealand, L30 and S30 surface reflectance on certain days was created using the atmospheric ancillary data from a date that was one day too early. The exact geographic extent of the affected HLS products and the impact on the surface reflectance quality are under investigation. Practice caution when using data with overpass times during the late hours of a UTC day.&lt;/li&gt;
&lt;li&gt;Duplicates in L30: The Landsat 9 acquisitions from October 2021 to March 2023 in Landsat Collection 2 were reprocessed by USGS in March 2023. This reprocessing updated the overpass time by a fraction of a second for some scenes. Since HLS uses overpass time as part of the L30 filename, the older L30 granules were not automatically overwritten due to the different filenames. For example, the first L30 granule in the following pair originated from an older version of L1TP of Landsat 9 with the second granule originating from the reprocessed version.&lt;br&gt;HLS.L30.T11SLC.2022166T182646.v2.0&lt;br&gt;HLS.L30.T11SLC.2022166T182645.v2.0&lt;br&gt;There are other causes of duplicate L30 granules, but the overall number of duplicates is very small.&lt;/li&gt;
&lt;li&gt;Poor Geolocation: A large amount of granules that were processed for May through July 2023 were created with L1GT input scenes which were deemed undesirable due to a poor geolocation issue. These granules were removed from the archive. (see the full list of removed &lt;a href&#x3D;&quot;https://lpdaac.usgs.gov/documents/2161/L30_L1GT_granules_May_July_2023.csv&quot;&gt;granules&lt;/a&gt;)&lt;/li&gt;
&lt;/ul&gt;
Improvements/Changes from Previous Versions&lt;ul&gt;
&lt;li&gt;Aerosol QA bits from the USGS Land Surface Reflectance Code (LaSRC) model output have been added into the Function of Mask (Fmask) data layer. The added two bits indicate the aerosol levels: high, medium, low, and climatology aerosol.
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&lt;/a&gt;&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>Hawai&#x27;i Downscaled Climate Projections CMIP6</title>
      <link>https://registry.opendata.aws/nasa-nex-hidcp-cmip6</link>
      <guid>https://registry.opendata.aws/nasa-nex-hidcp-cmip6</guid>
      <description>The NEX-HIDCP-CMIP6 dataset contains high-resolution daily downscaled CMIP6 projections over Hawai&amp;#39;i for maximum temperature, minimum temperature, and precipitation. This dataset compliments the NEX-DCP30-CMIP6 collection of downscaled projections over CONUS.</description>
    </item>
    <item>
      <title>High Resolution Population Density Maps + Demographic Estimates by CIESIN and Meta</title>
      <link>https://registry.opendata.aws/dataforgood-fb-hrsl</link>
      <guid>https://registry.opendata.aws/dataforgood-fb-hrsl</guid>
      <description>Population data for a selection of countries, allocated to 1 arcsecond blocks and provided in a combination of CSV
and Cloud-optimized GeoTIFF files. This refines &lt;a href&#x3D;&quot;https://sedac.ciesin.columbia.edu/data/collection/gpw-v4&quot;&gt;CIESIN’s Gridded Population of the World&lt;/a&gt;
using machine learning models on high-resolution worldwide Maxar satellite imagery. CIESIN population counts aggregated from worldwide census
data are allocated to blocks where imagery appears to contain buildings.</description>
    </item>
    <item>
      <title>High-Order Accurate Direct Numerical Simulation of Flow over a MTU-T161 Low Pressure Turbine Blade</title>
      <link>https://registry.opendata.aws/pyfr-mtu-t161-dns-data</link>
      <guid>https://registry.opendata.aws/pyfr-mtu-t161-dns-data</guid>
      <description>The archive comprises snapshot, point-probe, and time-average data produced via a high-fidelity computational simulation of turbulent air flow over a low pressure turbine blade, which is an important component in a jet engine. The simulation was undertaken using the open source PyFR flow solver on over 5000 Nvidia K20X GPUs of the Titan supercomputer at Oak Ridge National Laboratory under an INCITE award from the US DOE. The data can be used to develop an enhanced understanding of the complex three-dimensional unsteady air flow patterns over turbine blades in jet engines. This could in turn lead to design of greener more fuel efficient aircraft. It could also be used to train a next-generation of Reynolds Averaged Navier-Stokes turbulence models via a machine learning approach, which would have broad applicability to a wide range of science and engineering problems.</description>
    </item>
    <item>
      <title>Human Cancer Models Initiative (HCMI) Cancer Model Development Center</title>
      <link>https://registry.opendata.aws/hcmi-cmdc</link>
      <guid>https://registry.opendata.aws/hcmi-cmdc</guid>
      <description>The Human Cancer Models Initiative (HCMI) is an international consortium that is generating novel,
next-generation, tumor-derived culture models annotated with genomic and clinical data.
HCMI-developed models and related data are available as a community resource. The NCI is
contributing to the initiative by supporting four Cancer Model Development Centers (CMDCs).  CMDCs
are tasked with producing next-generation cancer models from clinical samples. The cancer models
include tumor types that are rare, originate from patients from underrepresented populations, lack
precision therapy, or lack cancer model tools. Throughout the development process, the CMDCs
utilize stringent internal QC measures to ensure both clinical and molecular integrity. These
models are then annotated with clinical and genomic data and are available as a community
resource.</description>
    </item>
    <item>
      <title>Human PanGenomics Project</title>
      <link>https://registry.opendata.aws/hpgp-data</link>
      <guid>https://registry.opendata.aws/hpgp-data</guid>
      <description>This dataset includes sequencing data, assemblies, and analyses for the offspring of ten parent-offspring trios.</description>
    </item>
    <item>
      <title>ICEYE Synthetic Aperture Radar (SAR) Open Dataset</title>
      <link>https://registry.opendata.aws/iceye-opendata</link>
      <guid>https://registry.opendata.aws/iceye-opendata</guid>
      <description>ICEYE operates the world’s largest constellation of synthetic aperture radar (SAR) satellites, delivering unmatched access to persistent, high-resolution Earth observation data regardless of time of day or weather conditions. The ICEYE Open Dataset makes a curated selection of SAR imagery publicly available to promote research, innovation, and education in the geospatial community. ICEYE’s constellation enables rapid revisit rates and flexible imaging modes, unlocking insights into natural disasters, climate monitoring, infrastructure, and more.Learn more at &lt;a href&#x3D;&quot;https://www.iceye.com&quot;&gt;www.iceye.com&lt;/a&gt;.</description>
    </item>
    <item>
      <title>IGP Brick Kilns Bangladesh</title>
      <link>https://registry.opendata.aws/asset-data-igp-brick-kilns-ban</link>
      <guid>https://registry.opendata.aws/asset-data-igp-brick-kilns-ban</guid>
      <description>This dataset includes detailed information about brick kilns, their locations, capacities, emissions, and other relevant attributes around the Indian Gangetic Plain.</description>
    </item>
    <item>
      <title>IGP Brick Kilns India</title>
      <link>https://registry.opendata.aws/asset-data-igp-brick-kilns-ind</link>
      <guid>https://registry.opendata.aws/asset-data-igp-brick-kilns-ind</guid>
      <description>This dataset includes detailed information about brick kilns, their locations, capacities, emissions, and other relevant attributes around the Indian Gangetic Plain.</description>
    </item>
    <item>
      <title>IGP Brick Kilns Pakistan</title>
      <link>https://registry.opendata.aws/asset-data-igp-brick-kilns-pak</link>
      <guid>https://registry.opendata.aws/asset-data-igp-brick-kilns-pak</guid>
      <description>This dataset includes detailed information about brick kilns, their locations, capacities, emissions, and other relevant attributes around the Pakistann Gangetic Plain.</description>
    </item>
    <item>
      <title>IGP Cement Plants</title>
      <link>https://registry.opendata.aws/asset-data-igp-cement</link>
      <guid>https://registry.opendata.aws/asset-data-igp-cement</guid>
      <description>This dataset includes detailed information about cement plants, their locations, capacities, emissions, and other relevant attributes around the Indian Gangetic Plain.</description>
    </item>
    <item>
      <title>IGP Paper and Pulp Plant</title>
      <link>https://registry.opendata.aws/asset-data-igp-paper-and-pulp</link>
      <guid>https://registry.opendata.aws/asset-data-igp-paper-and-pulp</guid>
      <description>This dataset includes detailed information about paper and pulp plants, their locations, capacities, emissions, and other relevant attributes around the Indian Gangetic Plain.</description>
    </item>
    <item>
      <title>IGP Power Generation Plant</title>
      <link>https://registry.opendata.aws/asset-data-igp-power-generation</link>
      <guid>https://registry.opendata.aws/asset-data-igp-power-generation</guid>
      <description>This dataset includes detailed information about power generation plants, their locations, capacities, emissions, and other relevant attributes around the Indian Gangetic Plain.</description>
    </item>
    <item>
      <title>IGP Steel Plants</title>
      <link>https://registry.opendata.aws/asset-data-igp-steel</link>
      <guid>https://registry.opendata.aws/asset-data-igp-steel</guid>
      <description>This dataset includes detailed information about steel plants, their locations, capacities, emissions, and other relevant attributes around the Indian Gangetic Plain.</description>
    </item>
    <item>
      <title>IGP Waste Management Data</title>
      <link>https://registry.opendata.aws/asset-data-igp-waste</link>
      <guid>https://registry.opendata.aws/asset-data-igp-waste</guid>
      <description>This dataset includes detailed information about waste management sites, their locations, capacities, emissions, and other relevant attributes around the Indian Gangetic Plain.</description>
    </item>
    <item>
      <title>IWMI DIWASA Rainfed and Irrigated Cropland Map for Africa</title>
      <link>https://registry.opendata.aws/cropland_partitioining</link>
      <guid>https://registry.opendata.aws/cropland_partitioining</guid>
      <description>A framework integrating the Budyko model has been developed to distinguish between rainfed and irrigated cropland areas across Africa. This expands on remote sensing land cover products available for agricultural water studies in Africa and thereby helps address the need for deeper insights into cropland patterns. Validation against an independent dataset revealed an overall accuracy of 73% with high precision and specificity scores. These results validate the framework’s effectiveness in identifying irrigated areas while minimizing errors in misclassifying rainfed areas as irrigated.</description>
    </item>
    <item>
      <title>Image classification - fast.ai datasets</title>
      <link>https://registry.opendata.aws/fast-ai-imageclas</link>
      <guid>https://registry.opendata.aws/fast-ai-imageclas</guid>
      <description>Some of the most important datasets for image classification research, including
CIFAR 10 and 100, Caltech 101, MNIST, Food-101, Oxford-102-Flowers, Oxford-IIIT-Pets,
and Stanford-Cars.  This is part of the fast.ai datasets collection hosted by
AWS for convenience of fast.ai students. See documentation link for citation and
license details for each dataset.</description>
    </item>
    <item>
      <title>Japan Prefectures, 3D Point Cloud Data</title>
      <link>https://registry.opendata.aws/japan_pointcloud</link>
      <guid>https://registry.opendata.aws/japan_pointcloud</guid>
      <description>This dataset comprises high-precision 3D point cloud data that covers all prefectures throughout Japan.
The data is produced through aerial laser surveys, airborne laser bathymetry, and mobile mapping systems, representing the culmination of many years of dedicated effort.
This data will be visualized and analyzed for use in infrastructure maintenance, disaster prevention measures, and autonomous vehicle driving.</description>
    </item>
    <item>
      <title>Kanagawa, 3D Point Cloud Data</title>
      <link>https://registry.opendata.aws/kanagawa_pointcloud</link>
      <guid>https://registry.opendata.aws/kanagawa_pointcloud</guid>
      <description>This dataset comprises high-precision 3D point cloud data that encompasses the entire Kanagawa prefecture in Japan.
The data is produced through aerial laser survey, airborne laser bathymetry and mobile mapping systems, the culmination of many years of dedicated effort.
This data will be visualized and analyzed for use in infrastructure maintenance, disaster prevention measures and autonomous vehicle driving.</description>
    </item>
    <item>
      <title>Knowledge Portal Network Bottom-line Genetic Associations</title>
      <link>https://registry.opendata.aws/dig-open-analysis-data</link>
      <guid>https://registry.opendata.aws/dig-open-analysis-data</guid>
      <description>At the Knowledge Portal Network, we aggregate and analyze genetic association results for a wide range of diseases and traits. For any given disease, a large number of individual genetic association datasets may have been generated. To make these results more interpretable, we meta-analyze all datasets for each phenotype, using a method that we term &amp;quot;bottom-line integrative analysis&amp;quot;. Here we provide the bottom-line summary statistic files for public download.</description>
    </item>
    <item>
      <title>Korea Meteorological Administration (KMA) GK-2A Satellite Data</title>
      <link>https://registry.opendata.aws/noaa-gk2a-pds</link>
      <guid>https://registry.opendata.aws/noaa-gk2a-pds</guid>
      <description>The Geo-KOMPSAT-2A (GK2A) is the new generation geostationary meteorological satellite (located in 128.2°E) of the Korea Meteorological Administration (KMA). The main mission of the GK2A is to observe the atmospheric phenomena over the Asia-Pacific region. The Advance Meteorological Imager (AMI) on GK2A scan the Earth full disk every 10 minutes and the Korean Peninsula area every 2 minutes with a high spatial resolution of 4 visible channels and 12 infrared channels. In addition, the AMI has an ability of flexible target area scanning useful for monitoring severe weather events such as typhoon and volcanic eruption and so on. And for space weather mission, the Korea Space wEather Monitor (KSEM) on the GK2A observes the space environment with the particle detector, magnetometer and charging monitor. For questions regarding GK2A imagery specifications, visit the GK2A site at &lt;a href&#x3D;&quot;https://nmsc.kma.go.kr/enhome/html/base/cmm/selectPage.do?page&#x3D;satellite.gk2a.intro&quot;&gt;https://nmsc.kma.go.kr/enhome/html/base/cmm/selectPage.do?page&#x3D;satellite.gk2a.intro&lt;/a&gt;. To view the GK2A Fact Sheet please visit &lt;a href&#x3D;&quot;https://nmsc.kma.go.kr/enhome/html/base/cmm/selectPage.do?page&#x3D;satellite.gk2a.fact&quot;&gt;https://nmsc.kma.go.kr/enhome/html/base/cmm/selectPage.do?page&#x3D;satellite.gk2a.fact&lt;/a&gt;.
&lt;br/&gt;
&lt;br/&gt;
NOAA provides access to GK2A data on AWS in coordination with the Korean Meteorlogical Administration.
&lt;br/&gt;</description>
    </item>
    <item>
      <title>LGND Clay v1.5 Sentinel-2</title>
      <link>https://registry.opendata.aws/lgnd-clay-v1-5-sentinel2</link>
      <guid>https://registry.opendata.aws/lgnd-clay-v1-5-sentinel2</guid>
      <description>A global dataset of Clay v1.5 embeddings for Sentinel2.</description>
    </item>
    <item>
      <title>LOFAR ELAIS-N1 cycle 2 observations on AWS</title>
      <link>https://registry.opendata.aws/lofar-elais-n1</link>
      <guid>https://registry.opendata.aws/lofar-elais-n1</guid>
      <description>These data correspond to the &lt;a href&#x3D;&quot;http://www.lofar.org/&quot;&gt;International LOFAR Telescope&lt;/a&gt; observations of the sky field ELAIS-N1 (16:10:01 +54:30:36) during the cycle 2 of observations. There are 11 runs of about 8 hours each plus the corresponding observation of the calibration targets before and after the target field. The data are measurement sets (&lt;a href&#x3D;&quot;https://casa.nrao.edu/Memos/229.html&quot;&gt;MS&lt;/a&gt;) containing the cross-correlated data and metadata divided in 371 frequency sub-bands per target centred at ~150 MHz.</description>
    </item>
    <item>
      <title>Land/Sea static mask relevant to IMERG precipitation 0.1x0.1 degree V2 (GPM_IMERG_LandSeaMask) at GES DISC</title>
      <link>https://registry.opendata.aws/nasa-gpmimerglandseamask</link>
      <guid>https://registry.opendata.aws/nasa-gpmimerglandseamask</guid>
      <description>Version 2 is the current version of the data set. Older versions will no longer be available and have been superseded by Version 2.This land sea mask originated from the NOAA group at SSEC in the 1980s. It was originally produced at 1/6 deg resolution, and then regridded for the purposes of GPCP, TMPA, and IMERG precipitation products. NASA code 610.2, Terrestrial Information Systems Laboratory, restructured this land sea mask to match the IMERG grid, and converted the file to CF-compliant netCDF4. Version 2 was created in May, 2019 to resolve detected inaccuracies in coastal regions.Users should be aware that this is a static mask, i.e. there is no seasonal or annual variability, and it is due for update. It is not recommended to be used outside of the aforementioned precipitation data.
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>Legal Entity Identifier (LEI) and Legal Entity Reference Data (LE-RD)</title>
      <link>https://registry.opendata.aws/lei</link>
      <guid>https://registry.opendata.aws/lei</guid>
      <description>The Legal Entity Identifier (LEI) is a 20-character, alpha-numeric code based on the ISO 17442 standard developed by the International Organization for Standardization (ISO). It connects to key reference information that enables clear and unique identification of legal entities participating in financial transactions. Each LEI contains information about an entity’s ownership structure and thus answers the questions of &amp;#39;who is who’ and ‘who owns whom’. Simply put, the publicly available LEI data pool can be regarded as a global directory, which greatly enhances transparency in the global marketplace. The Financial Stability Board (FSB) has reiterated that global LEI adoption underpins “multiple financial stability objectives” such as improved risk management in firms as well as better assessment of micro and macro prudential risks. As a result, it promotes market integrity while containing market abuse and financial fraud. Last but not least, LEI rollout “supports higher quality and accuracy of financial data overall”. The publicly available LEI data pool is a unique key to standardized information on legal entities globally. The data is registered and regularly verified according to protocols and procedures established by the Regulatory Oversight Committee. In cooperation with its partners in the Global LEI System, the Global Legal Entity Identifier Foundation (GLEIF) continues to focus on further optimizing the quality, reliability and usability of LEI data, empowering market participants to benefit from the wealth of information available with the LEI population. The drivers of the LEI initiative, i.e. the Group of 20, the FSB and many regulators around the world, have emphasized the need to make the LEI a broad public good. The Global LEI Index, made available by GLEIF, greatly contributes to meeting this objective. It puts the complete LEI data at the disposal of any interested party, conveniently and free of charge. The benefits for the wider business community to be generated with the Global LEI Index grow in line with the rate of LEI adoption. To maximize the benefits of entity identification across financial markets and beyond, firms are therefore encouraged to engage in the process and get their own LEI. Obtaining an LEI is easy. Registrants simply contact their preferred business partner from the list of LEI issuing organizations available on the GLEIF website.</description>
    </item>
    <item>
      <title>LongBench - cross-platform reference dataset profiling cancer cell lines with bulk and single-cell approaches</title>
      <link>https://registry.opendata.aws/longbench</link>
      <guid>https://registry.opendata.aws/longbench</guid>
      <description>LongBench is a comprehensive benchmark dataset of the latest long-read transcriptomics technologies from Oxford Nanopore (ON) and Pacific Biosciences, alongside a comparison with next-generation sequencing from Illumina. We generated bulk and single-cell libraries from lung cancer cell lines which include different cancer subtypes to capture real biological variation. To further compare and assess sequencing platform performance, Sequins and SIRVs (Set 4) synthetic spike-ins have been included.</description>
    </item>
    <item>
      <title>Longitudinal Nutrient Deficiency</title>
      <link>https://registry.opendata.aws/intelinair_longitudinal_nutrient_deficiency</link>
      <guid>https://registry.opendata.aws/intelinair_longitudinal_nutrient_deficiency</guid>
      <description>Dataset associated with the 2021 AAAI Paper- Detection and Prediction of Nutrient Deficiency Stress using Longitudinal Aerial Imagery.  The dataset contains 3 image sequences of aerial imagery from 386 farm parcels which have been annotated for nutrient deficiency stress.</description>
    </item>
    <item>
      <title>MAN TruckScenes</title>
      <link>https://registry.opendata.aws/man-truckscenes</link>
      <guid>https://registry.opendata.aws/man-truckscenes</guid>
      <description>A large scale multimodal dataset for Autonomous Trucking. Sensor data was recorded with a heavy truck from MAN equipped with 6 lidars, 6 radars, 4 cameras and a high-precision GNSS. MAN TruckScenes allows the research community to come into contact with truck-specific challenges, such as trailer occlusions, novel sensor perspectives, and terminal environments for the first time.
It comprises more than 740 scenes of 20s each within a multitude of different environmental conditions. Bounding boxes are available for 27 object classes, 15 attributes, and a range of more than 230m. The scenes are tagged according to 34 distinct scene tags, and all objects are tracked throughout the scene to promote a wide range of applications.</description>
    </item>
    <item>
      <title>MODIS MYD13A1, MOD13A1, MYD11A1, MOD11A1, MCD43A4</title>
      <link>https://registry.opendata.aws/modis-astraea</link>
      <guid>https://registry.opendata.aws/modis-astraea</guid>
      <description>Data from the Moderate Resolution Imaging Spectroradiometer (MODIS), managed by
the U.S. Geological Survey and NASA. Five products are included:
MCD43A4 (MODIS/Terra and Aqua Nadir BRDF-Adjusted Reflectance Daily L3 Global 500 m SIN Grid),
MOD11A1 (MODIS/Terra Land Surface Temperature/Emissivity Daily L3 Global 1 km SIN Grid),
MYD11A1 (MODIS/Aqua Land Surface Temperature/Emissivity Daily L3 Global 1 km SIN Grid),
MOD13A1 (MODIS/Terra Vegetation Indices 16-Day L3 Global 500 m SIN Grid),
and MYD13A1 (MODIS/Aqua Vegetation Indices 16-Day L3 Global 500 m SIN Grid).
MCD43A4 has global coverage, all time (~21 years).
The other products have ~11 years of global coverage.  All data files are in single-band
cloud-optimized GeoTIFF (COG) format.</description>
    </item>
    <item>
      <title>MODIS/Aqua Surface Reflectance Daily L2G Global 1km and 500m SIN Grid V061</title>
      <link>https://registry.opendata.aws/nasa-myd09ga</link>
      <guid>https://registry.opendata.aws/nasa-myd09ga</guid>
      <description>The MYD09GA Version 6.1 product provides an estimate of the surface spectral reflectance of Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Bands 1 through 7, corrected for atmospheric conditions such as gasses, aerosols, and Rayleigh scattering. Provided along with the 500 meter (m) surface reflectance, observation, and quality bands are a set of ten 1 kilometer observation bands and geolocation flags. The reflectance layers from the MYD09GA are used as the source data for many of the MODIS land products. Known Issues&lt;ul&gt;
&lt;li&gt;Prior to the Aqua MODIS launch, Band 6 exhibited several anomalous detectors. Band 6 performance degraded seriously after launch and presently a majority of the Band 6 detectors are non-functional. Science users should read and use the non-functional detector flags and decide for themselves the optimum manner to handle non-functional detector &amp;quot;gaps&amp;quot; for their products. For complete information please refer to the &lt;a href&#x3D;&quot;https://mcst.gsfc.nasa.gov/time-dependent-list-non-functional-or-noisy-detector&quot;&gt;MODIS Characterization Support Team (MCST) website&lt;/a&gt;.&lt;/li&gt;
&lt;li&gt;For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.&lt;/li&gt;
&lt;/ul&gt;
Improvments/Changes from Previous Version&lt;ul&gt;
&lt;li&gt;The Version 6.1 Level-1B (L1B) products have been improved by undergoing various calibration changes that include: changes to the response-versus-scan angle (RVS) approach that affects reflectance bands for Aqua and Terra MODIS, corrections to adjust for the optical crosstalk in Terra MODIS infrared (IR) bands, and corrections to the Terra MODIS forward look-up table (LUT) update for the period 2012 - 2017.&lt;/li&gt;
&lt;li&gt;A polarization correction has been applied to the L1B Reflective Solar Bands (RSB).
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&lt;/a&gt;&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>MODIS/Aqua Surface Reflectance Daily L2G Global 250m SIN Grid V061</title>
      <link>https://registry.opendata.aws/nasa-myd09gq</link>
      <guid>https://registry.opendata.aws/nasa-myd09gq</guid>
      <description>The MYD09GQ Version 6.1 product provides an estimate of the surface spectral reflectance of Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) 250 meter (m) bands 1 and 2, corrected for atmospheric conditions such as gasses, aerosols, and Rayleigh scattering. Along with the 250 m bands are the Quality Assurance (QA) layer and five observation layers. This product is intended to be used in conjunction with the quality and viewing geometry information of the 500 m product (MYD09GA). Known Issues&lt;ul&gt;
&lt;li&gt;Prior to the Aqua MODIS launch, Band 6 exhibited several anomalous detectors. Band 6 performance degraded seriously after launch and presently a majority of the Band 6 detectors are non-functional. Science users should read and use the non-functional detector flags and decide for themselves the optimum manner to handle non-functional detector &amp;quot;gaps&amp;quot; for their products. For complete information please refer to the &lt;a href&#x3D;&quot;https://mcst.gsfc.nasa.gov/time-dependent-list-non-functional-or-noisy-detector&quot;&gt;MODIS Characterization Support Team (MCST) website&lt;/a&gt;.&lt;/li&gt;
&lt;li&gt;For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.&lt;/li&gt;
&lt;/ul&gt;
Improvments/Changes from Previous Version&lt;ul&gt;
&lt;li&gt;The Version 6.1 Level-1B (L1B) products have been improved by undergoing various calibration changes that include: changes to the response-versus-scan angle (RVS) approach that affects reflectance bands for Aqua and Terra MODIS, corrections to adjust for the optical crosstalk in Terra MODIS infrared (IR) bands, and corrections to the Terra MODIS forward look-up table (LUT) update for the period 2012 - 2017.&lt;/li&gt;
&lt;li&gt;A polarization correction has been applied to the L1B Reflective Solar Bands (RSB).
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&lt;/a&gt;&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>MODIS/Terra Calibrated Radiances 5-Min L1B Swath 500m</title>
      <link>https://registry.opendata.aws/nasa-mod02hkm</link>
      <guid>https://registry.opendata.aws/nasa-mod02hkm</guid>
      <description>The MODIS/Terra Calibrated Radiances 5Min L1B Swath 500m data set contains calibrated and geolocated at-aperture radiances for 7 discrete bands located in the 0.45 to 2.20 micron region of the electromagnetic spectrum. These data are generated from the MODIS Level 1A scans of raw radiance and in the process converted to geophysical units of W/(m^2 um sr). Additional data are provided including quality flags, error estimates and calibration data.Visible, shortwave infrared, and near infrared measurements are only made during the daytime (except band 26), while radiances for the thermal infrared region (bands 20-25, 27-36) are measured continuously.Channels 1 and 2 have 250 m resolution, channels 3 through 7 have 500 m resolution. However, for the MODIS L1B 500 m product, the 250 m band radiance data and their associated uncertainties have been aggregated to 500m resolution. Thus the entire channel data set has been co-registered to the same spatial scale in the 500 m product. Separate L1B products are available for the 250 m resolution channels (MOD02QKM) and 1 km resolution channels (MOD021KM). For the latter product, the 250 m and 500 m channel data (bands 1 through 7) have been aggregated into equivalent 1 km pixel values.Spatial resolution for pixels at nadir is 500 km, degrading to 2.4 km in the along-scan direction at the scan extremes. However, thanks to the overlapping of consecutive swaths and respectively pixels there, the resulting resolution at the scan extremes is about 1 km. A 55 degree scanning pattern at the EOS orbit of 705 km results in a 2330 km orbital swath width and provides global coverage every one to two days. A single MODIS Level 1B 500 m granule will contain a scene built from 203 scans sampled 2708 times in the cross-track direction, corresponding to approximately 5 minutes worth of data; thus 288 granules will be produced per day. Since an individual MODIS scan will contain 20 along-track spatial elements for the 500 m channels, the scene will be composed of (2708 x 4060) pixels, resulting in a spatial coverage of (2330 km x 2040 km). Due to the MODIS scan geometry, there will be increasing scan overlap beyond about 20 degrees scan angle.      To summarize, the MODIS L1B 500 m data product consists of:&lt;ol&gt;
&lt;li&gt;Calibrated radiances, uncertainties and number of samples for (2) 250 m reflected solar bands aggregated to 500 m resolution&lt;/li&gt;
&lt;li&gt;Calibrated radiances and uncertainties for (5) 500 m reflected solar bands&lt;/li&gt;
&lt;li&gt;Geolocation for 1km pixels, that must be interpolated to get 500 m pixel locations. For the relationship of 1km pixels to 500m pixels, see the Geolocation ATBD &lt;a href&#x3D;&quot;https://modis.gsfc.nasa.gov/data/atbd/atbd_mod28_v3.pdf&quot;&gt;https://modis.gsfc.nasa.gov/data/atbd/atbd_mod28_v3.pdf&lt;/a&gt;.&lt;/li&gt;
&lt;li&gt;Calibration data for all channels (scale and offset) &lt;/li&gt;
&lt;li&gt;Comprehensive set of file-level metadata summarizing the spatial, temporal and parameter attributes of the data, as well as auxiliary information pertaining to instrument status and data quality characterization users requiring all geolocation and solar/satellite geometry fields at 1km resolution can obtain the separate MODIS Level 1 Geolocation product (MOD03) from LAADS  &lt;a href&#x3D;&quot;https://ladsweb.modaps.eosdis.nasa.gov/&quot;&gt;https://ladsweb.modaps.eosdis.nasa.gov/&lt;/a&gt; .&lt;/li&gt;
&lt;/ol&gt;
The shortname for this product is MOD02HKM and is stored in the Earth Observing System Hierarchical Data Format (HDF-EOS). A typical MOD02HKM file size is approximately 135 MB.Environmental information derived from MODIS L1B measurements will offer a comprehensive and unprecedented look at terrestrial, atmospheric, and ocean phenomenology for a wide and diverse community of users throughout the world.See the MODIS Characterization Support Team webpage for more C6 product information at:&lt;a href&#x3D;&quot;https://mcst.gsfc.nasa.gov/l1b/product-information&quot;&gt;https://mcst.gsfc.nasa.gov/l1b/product-information&lt;/a&gt;or visit Science Team homepage at:
&lt;a href&#x3D;&quot;https://modis.gsfc.nasa.gov/data/dataprod/&quot;&gt;https://modis.gsfc.nasa.gov/data/dataprod/&lt;/a&gt;
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.laadsdaac.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;https://data.laadsdaac.earthdatacloud.nasa.gov/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>MODIS/Terra Net Evapotranspiration 8-Day L4 Global 500m SIN Grid V061</title>
      <link>https://registry.opendata.aws/nasa-mod16a2</link>
      <guid>https://registry.opendata.aws/nasa-mod16a2</guid>
      <description>The MOD16A2 Version 6.1 Evapotranspiration/Latent Heat Flux product is an 8-day composite dataset produced at 500 meter (m) pixel resolution. The algorithm used for the MOD16 data product collection is based on the logic of the Penman-Monteith equation, which includes inputs of daily meteorological reanalysis data along with Moderate Resolution Imaging Spectroradiometer (MODIS) remotely sensed data products such as vegetation property dynamics, albedo, and land cover. Provided in the MOD16A2 product are layers for composited Evapotranspiration (ET), Latent Heat Flux (LE), Potential ET (PET) and Potential LE (PLE) along with a quality control layer. Two low resolution browse images, ET and LE, are also available for each MOD16A2 granule.The pixel values for the two Evapotranspiration layers (ET and PET) are the sum of all eight days within the composite period and the pixel values for the two Latent Heat layers (LE and PLE) are the average of all eight days within the composite period. Note that the last acquisition period of each year is a 5 or 6-day composite period, depending on the year.Known Issues&lt;ul&gt;
&lt;li&gt;Operational and uncertainty issues are provided under Section 3 in the User Guide.&lt;/li&gt;
&lt;li&gt;For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Terra&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.&lt;/li&gt;
&lt;/ul&gt;
Improvements/Changes from Previous Versions&lt;ul&gt;
&lt;li&gt;The Version 6.1 Level-1B (L1B) products have been improved by undergoing various calibration changes that include: changes to the response-versus-scan angle (RVS) approach that affects reflectance bands for Aqua and Terra MODIS, corrections to adjust for the optical crosstalk in Terra MODIS infrared (IR) bands, and corrections to the Terra MODIS forward look-up table (LUT) update for the period 2012 - 2017.&lt;/li&gt;
&lt;li&gt;A polarization correction has been applied to the L1B Reflective Solar Bands (RSB).&lt;/li&gt;
&lt;li&gt;The product uses Climatology LAI/FPAR as back up to the operational LAI/FPAR.
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&lt;/a&gt;&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>MODIS/Terra Surface Reflectance 8-Day L3 Global 500m SIN Grid V061</title>
      <link>https://registry.opendata.aws/nasa-mod09a1</link>
      <guid>https://registry.opendata.aws/nasa-mod09a1</guid>
      <description>The  Moderate Resolution Imaging Spectroradiometer (MODIS) Terra MOD09A1 Version 6.1 product provides an estimate of the surface spectral reflectance of Terra MODIS Bands 1 through 7 corrected for atmospheric conditions such as gasses, aerosols, and Rayleigh scattering. Along with the seven 500 meter (m) reflectance bands are two quality layers and four observation bands. For each pixel, a value is selected from all the acquisitions within the 8-day composite period. The criteria for the pixel choice include cloud and solar zenith. When several acquisitions meet the criteria the pixel with the minimum channel 3 (blue) value is used. Known Issues&lt;ul&gt;
&lt;li&gt;For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Terra&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.&lt;/li&gt;
&lt;/ul&gt;
Improvements/Changes from Previous Versions&lt;ul&gt;
&lt;li&gt;The Version 6.1 Level-1B (L1B) products have been improved by undergoing various calibration changes that include: changes to the response-versus-scan angle (RVS) approach that affects reflectance bands for Aqua and Terra MODIS, corrections to adjust for the optical crosstalk in Terra MODIS infrared (IR) bands, and corrections to the Terra MODIS forward look-up table (LUT) update for the period 2012 - 2017.&lt;/li&gt;
&lt;li&gt;A polarization correction has been applied to the L1B Reflective Solar Bands (RSB).
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&lt;/a&gt;&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>MODIS/Terra Surface Reflectance Daily L2G Global 1km and 500m SIN Grid V061</title>
      <link>https://registry.opendata.aws/nasa-mod09ga</link>
      <guid>https://registry.opendata.aws/nasa-mod09ga</guid>
      <description>The MOD09GA Version 6.1 product provides an estimate of the surface spectral reflectance of Terra Moderate Resolution Imaging Spectroradiometer (MODIS) Bands 1 through 7, corrected for atmospheric conditions such as gasses, aerosols, and Rayleigh scattering. Provided along with the 500 meter (m) surface reflectance, observation, and quality bands are a set of ten 1 kilometer (km) observation bands and geolocation flags. The reflectance layers from the MOD09GA are used as the source data for many of the MODIS land products. Known Issues&lt;ul&gt;
&lt;li&gt;For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Terra&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.&lt;/li&gt;
&lt;/ul&gt;
Improvements/Changes from Previous Versions&lt;ul&gt;
&lt;li&gt;The Version 6.1 Level-1B (L1B) products have been improved by undergoing various calibration changes that include: changes to the response-versus-scan angle (RVS) approach that affects reflectance bands for Aqua and Terra MODIS, corrections to adjust for the optical crosstalk in Terra MODIS infrared (IR) bands, and corrections to the Terra MODIS forward look-up table (LUT) update for the period 2012 - 2017.&lt;/li&gt;
&lt;li&gt;A polarization correction has been applied to the L1B Reflective Solar Bands (RSB).
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&lt;/a&gt;&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>MODIS/Terra Surface Reflectance Daily L2G Global 250m SIN Grid V061</title>
      <link>https://registry.opendata.aws/nasa-mod09gq</link>
      <guid>https://registry.opendata.aws/nasa-mod09gq</guid>
      <description>The MOD09GQ Version 6.1 product provides an estimate of the surface spectral reflectance of Terra Moderate Resolution Imaging Spectroradiometer (MODIS) 250 meter (m) bands 1 and 2, corrected for atmospheric conditions such as gasses, aerosols, and Rayleigh scattering. Along with the 250 m surface reflectance bands are the Quality Assurance (QA) layer and five observation layers. This product is intended to be used in conjunction with the quality and viewing geometry information of the 500 m product (MOD09GA). Known Issues&lt;ul&gt;
&lt;li&gt;For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Terra&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.&lt;/li&gt;
&lt;/ul&gt;
Improvements/Changes from Previous Versions&lt;ul&gt;
&lt;li&gt;The Version 6.1 Level-1B (L1B) products have been improved by undergoing various calibration changes that include: changes to the response-versus-scan angle (RVS) approach that affects reflectance bands for Aqua and Terra MODIS, corrections to adjust for the optical crosstalk in Terra MODIS infrared (IR) bands, and corrections to the Terra MODIS forward look-up table (LUT) update for the period 2012 - 2017.&lt;/li&gt;
&lt;li&gt;A polarization correction has been applied to the L1B Reflective Solar Bands (RSB).
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&lt;/a&gt;&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>MODIS/Terra Vegetation Indices 16-Day L3 Global 250m SIN Grid V061</title>
      <link>https://registry.opendata.aws/nasa-mod13q1</link>
      <guid>https://registry.opendata.aws/nasa-mod13q1</guid>
      <description>The Terra Moderate Resolution Imaging Spectroradiometer (MODIS) Vegetation Indices (MOD13Q1) Version 6.1 data are generated every 16 days at 250 meter (m) spatial resolution as a Level 3 product. The MOD13Q1 product provides two primary vegetation layers. The first is the Normalized Difference Vegetation Index (NDVI) which is referred to as the continuity index to the existing National Oceanic and Atmospheric Administration-Advanced Very High Resolution Radiometer (NOAA-AVHRR) derived NDVI. The second vegetation layer is the Enhanced Vegetation Index (EVI), which has improved sensitivity over high biomass regions. The algorithm chooses the best available pixel value from all the acquisitions from the 16 day period. The criteria used is low clouds, low view angle, and the highest NDVI/EVI value.Along with the vegetation layers and the two quality layers, the HDF file will have MODIS reflectance bands 1 (red), 2 (near-infrared), 3 (blue), and 7 (mid-infrared), as well as four observation layers. Known Issues&lt;ul&gt;
&lt;li&gt;For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Terra&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.&lt;/li&gt;
&lt;/ul&gt;
Improvements/Changes from Previous Versions&lt;ul&gt;
&lt;li&gt;The Version 6.1 Level-1B (L1B) products have been improved by undergoing various calibration changes that include: changes to the response-versus-scan angle (RVS) approach that affects reflectance bands for Aqua and Terra MODIS, corrections to adjust for the optical crosstalk in Terra MODIS infrared (IR) bands, and corrections to the Terra MODIS forward look-up table (LUT) update for the period 2012 - 2017.&lt;/li&gt;
&lt;li&gt;A polarization correction has been applied to the L1B Reflective Solar Bands (RSB).
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&lt;/a&gt;&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>MODIS/Terra+Aqua BRDF/Albedo Albedo Daily L3 Global - 500m V061</title>
      <link>https://registry.opendata.aws/nasa-mcd43a3</link>
      <guid>https://registry.opendata.aws/nasa-mcd43a3</guid>
      <description>The Moderate Resolution Imaging Spectroradiometer (MODIS) MCD43A3 Version 6.1 Albedo Model dataset is produced daily using 16 days of Terra and Aqua MODIS data at 500 meter (m) resolution. Data are temporally weighted to the ninth day of the 16 day which is reflected in the Julian date in the file name.Users are urged to use the band specific quality flags to isolate the highest quality full inversion results for their own science applications as described in the &lt;a href&#x3D;&quot;https://www.umb.edu/spectralmass/modis-user-guide-v006-and-v0061/mcd43a3-albedo-product/&quot;&gt;User Guide&lt;/a&gt;.The MCD43A3 provides black-sky albedo (directional hemispherical reflectance) and white-sky albedo (bihemispherical reflectance) data at local solar noon for MODIS bands 1 through 7 and the visible, near infrared (NIR), and shortwave bands. Along with the albedo layers are the simplified mandatory quality layers for each of the 10 bands. Essential quality information provided in the corresponding &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MCD43A2.061&quot;&gt;MCD43A2&lt;/a&gt; data file should be consulted when using this product.Known Issues&lt;ul&gt;
&lt;li&gt;For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;TerraAqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.&lt;/li&gt;
&lt;/ul&gt;
Improvements/Changes from Previous Versions&lt;ul&gt;
&lt;li&gt;The Version 6.1 Level-1B (L1B) products have been improved by undergoing various calibration changes that include: changes to the response-versus-scan angle (RVS) approach that affects reflectance bands for Aqua and Terra MODIS, corrections to adjust for the optical crosstalk in Terra MODIS infrared (IR) bands, and corrections to the Terra MODIS forward look-up table (LUT) update for the period 2012 - 2017.&lt;/li&gt;
&lt;li&gt;A polarization correction has been applied to the L1B Reflective Solar Bands (RSB).
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&lt;/a&gt;&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>MODIS/Terra+Aqua BRDF/Albedo Model Parameters Daily L3 Global - 500m V061</title>
      <link>https://registry.opendata.aws/nasa-mcd43a1</link>
      <guid>https://registry.opendata.aws/nasa-mcd43a1</guid>
      <description>The Moderate Resolution Imaging Spectroradiometer (MODIS) MCD43A1 Version 6.1 Bidirectional Reflectance Distribution Function and Albedo (BRDF/Albedo) Model Parameters dataset is produced daily using 16 days of Terra and Aqua MODIS data at 500 meter (m) resolution. Data are temporally weighted to the ninth day of the retrieval period which is reflected in the Julian date in the file name. MCD43A1 provides the three model weighting parameters (isotropic, volumetric, and geometric) used to derive the Albedo (&lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MCD43A3.061&quot;&gt;MCD43A3&lt;/a&gt;) and Nadir BRDF-Adjusted Reflectance (NBAR) (&lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MCD43A4.061&quot;&gt;MCD43A4&lt;/a&gt;) products.Users are urged to use the band specific quality flags to isolate the highest quality full inversion results for their own science applications as described in the &lt;a href&#x3D;&quot;https://www.umb.edu/spectralmass/modis-user-guide-v006-and-v0061/mcd43a1-brdfalbedo-model-parameters-product/&quot;&gt;User Guide&lt;/a&gt;.The MCD43A1 provides the three model weighting parameters for MODIS spectral bands 1 through 7 as well as the visible, near infrared (NIR), and shortwave bands. Along with the three-dimensional parameter layers for these bands are the simplified mandatory quality layers for each of the 10 bands. Essential quality information provided in the corresponding &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MCD43A2.061&quot;&gt;MCD43A2&lt;/a&gt; data file should be consulted when using this product. Known Issues&lt;ul&gt;
&lt;li&gt;For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;TerraAqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.&lt;/li&gt;
&lt;/ul&gt;
Improvements/Changes from Previous Versions&lt;ul&gt;
&lt;li&gt;The Version 6.1 Level-1B (L1B) products have been improved by undergoing various calibration changes that include: changes to the response-versus-scan angle (RVS) approach that affects reflectance bands for Aqua and Terra MODIS, corrections to adjust for the optical crosstalk in Terra MODIS infrared (IR) bands, and corrections to the Terra MODIS forward look-up table (LUT) update for the period 2012 - 2017.&lt;/li&gt;
&lt;li&gt;A polarization correction has been applied to the L1B Reflective Solar Bands (RSB).
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&lt;/a&gt;&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>MODIS/Terra+Aqua BRDF/Albedo Nadir BRDF-Adjusted Ref Daily L3 Global - 500m V061</title>
      <link>https://registry.opendata.aws/nasa-mcd43a4</link>
      <guid>https://registry.opendata.aws/nasa-mcd43a4</guid>
      <description>The Moderate Resolution Imaging Spectroradiometer (MODIS) MCD43A4 Version 6.1 Nadir Bidirectional Reflectance Distribution Function (BRDF)-Adjusted Reflectance (NBAR) dataset is produced daily using 16 days of Terra and Aqua MODIS data at 500 meter (m) resolution. The view angle effects are removed from the directional reflectances, resulting in a stable and consistent NBAR product. Data are temporally weighted to the ninth day which is reflected in the Julian date in the file name.Users are urged to use the band specific quality flags to isolate the highest quality full inversion results for their own science applications as described in the &lt;a href&#x3D;&quot;https://www.umb.edu/spectralmass/modis-user-guide-v006-and-v0061/mcd43a4-nbar-product/&quot;&gt;User Guide&lt;/a&gt;.The MCD43A4 provides NBAR and simplified mandatory quality layers for MODIS bands 1 through 7. Essential quality information provided in the corresponding &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MCD43A2.061&quot;&gt;MCD43A2&lt;/a&gt; data file should be consulted when using this product.Known Issues&lt;ul&gt;
&lt;li&gt;For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;TerraAqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.&lt;/li&gt;
&lt;/ul&gt;
Improvements/Changes from Previous Versions&lt;ul&gt;
&lt;li&gt;The Version 6.1 Level-1B (L1B) products have been improved by undergoing various calibration changes that include: changes to the response-versus-scan angle (RVS) approach that affects reflectance bands for Aqua and Terra MODIS, corrections to adjust for the optical crosstalk in Terra MODIS infrared (IR) bands, and corrections to the Terra MODIS forward look-up table (LUT) update for the period 2012 - 2017.&lt;/li&gt;
&lt;li&gt;A polarization correction has been applied to the L1B Reflective Solar Bands (RSB).
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&lt;/a&gt;&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>Marginal Build Emissions Rates (MBERs) for Electricity</title>
      <link>https://registry.opendata.aws/mbers-open-data</link>
      <guid>https://registry.opendata.aws/mbers-open-data</guid>
      <description>The Climate TRACE coalition has developed and maintains free global hourly Build Margin data, also known as MBERs, that are compliant with the Greenhouse Gas Protocol&amp;#39;s Project Protocol electricity sector guidance, Guidelines for Grid-Connected Electricity Projects (&amp;quot;GHGP Guidelines&amp;quot;).</description>
    </item>
    <item>
      <title>Mars Spectrometry 2: Gas Chromatography for the Sample Analysis at Mars Data (SAM) Instrument</title>
      <link>https://registry.opendata.aws/nasa-gcms</link>
      <guid>https://registry.opendata.aws/nasa-gcms</guid>
      <description>NASA missions like the Curiosity and Perseverance rovers carry a rich array of instruments suited to collect data and build evidence towards answering if Mars ever had livable environmental conditions. These rovers can collect rock and soil samples and can take measurements that can be used to determine their chemical makeup. &lt;br/&gt;&lt;br/&gt;
Because communication between rovers and Earth is severely constrained, with limited transfer rates and short daily communication windows, scientists have a limited time to analyze the data and make difficult inferences about the chemistry in order to prioritize the next operations and send those instructions back to the rover. &lt;br/&gt;&lt;br/&gt;
This project aimed at building a model to automatically analyze gas chromatography mass spectrometry (GCMS) data collected for Mars exploration in order to help the scientists in their analysis of understanding the past habitability of Mars. &lt;br/&gt;&lt;br/&gt;
More information are available at &lt;a href&#x3D;&quot;https://mars.nasa.gov/msl/spacecraft/instruments/sam/&quot;&gt;https://mars.nasa.gov/msl/spacecraft/instruments/sam/&lt;/a&gt; and the data from Mars are available and described at &lt;a href&#x3D;&quot;https://pds-geosciences.wustl.edu/missions/msl/sam.htm&quot;&gt;https://pds-geosciences.wustl.edu/missions/msl/sam.htm&lt;/a&gt;. &lt;br/&gt;&lt;br/&gt;We request that you cite the following ackowledgement when using the data provided from this NASA Project: &amp;quot;NASA provided support for the development of SAM. The datasets for these 2 challenges were provided by NASA Goddard Space Flight Center and NASA Johnson Space Center. They have been collected by the Sample Analysis at Mars (SAM) scientists and specifically processed for these challenges with the help of the scientists from NASA: Doug Archer, Charles Malespin, Caroline Freissinet, Stephanie Getty, Luoth Chou, Eric Lyness, and Victoria Da Poian, and the DrivenData team. Data from all SAM experiments are archived in the Planetary Data System (pds.nasa.gov).&amp;quot;</description>
    </item>
    <item>
      <title>Mars Spectrometry: Detect Evidence for Past Habitability</title>
      <link>https://registry.opendata.aws/nasa-ega</link>
      <guid>https://registry.opendata.aws/nasa-ega</guid>
      <description>NASA missions like the Curiosity and Perseverance rovers carry a rich array of instruments suited to collect data and build evidence towards answering if Mars ever had livable environmental conditions. These rovers can collect rock and soil samples and can take measurements that can be used to determine their chemical makeup. &lt;br/&gt;&lt;br/&gt;
Because communication between rovers and Earth is severely constrained, with limited transfer rates and short daily communication windows, scientists have a limited time to analyze the data and make difficult inferences about the chemistry in order to prioritize the next operations and send those instructions back to the rover. &lt;br/&gt;&lt;br/&gt;
This project aimed at building a model to automatically analyze evolved gas analysis mass spectrometry (EGA-MS) data collected for Mars exploration in order to help the scientists in their analysis of understanding the past habitability of Mars. &lt;br/&gt;&lt;br/&gt;
More information are available at &lt;a href&#x3D;&quot;https://mars.nasa.gov/msl/spacecraft/instruments/sam/&quot;&gt;https://mars.nasa.gov/msl/spacecraft/instruments/sam/&lt;/a&gt; and the data from Mars are available and described at &lt;a href&#x3D;&quot;https://pds-geosciences.wustl.edu/missions/msl/sam.htm&quot;&gt;https://pds-geosciences.wustl.edu/missions/msl/sam.htm&lt;/a&gt;. &lt;br/&gt;&lt;br/&gt;
We request that you cite the following ackowledgement when using the data provided from this NASA Project: &amp;quot;NASA provided support for the development of SAM. The datasets for these 2 challenges were provided by NASA Goddard Space Flight Center and NASA Johnson Space Center. They have been collected by the Sample Analysis at Mars (SAM) scientists and specifically processed for these challenges with the help of the scientists from NASA: Doug Archer, Charles Malespin, Caroline Freissinet, Stephanie Getty, Luoth Chou, Eric Lyness, and Victoria Da Poian, and the DrivenData team. Data from all SAM experiments are archived in the Planetary Data System (pds.nasa.gov).&amp;quot;</description>
    </item>
    <item>
      <title>Met Office UK Earth System Model (UKESM1) ARISE-SAI geoengineering experiment data</title>
      <link>https://registry.opendata.aws/met-office-ukesm1-arise</link>
      <guid>https://registry.opendata.aws/met-office-ukesm1-arise</guid>
      <description>Data from the UK Earth System Model (UKESM1) ARISE-SAI experiment. The UKESM1 ARISE-SAI experiment explores the impacts of geoengineering via the injection of sulphur dioxide (SO2) into the stratosphere in order to keep global mean surface air temperature near 1.5 C above the pre-industrial climate. Data includes a five member ensemble of simulations with SO2 injection plus a five member ensemble of SSP2-4.5 simulations from CMIP6 to serve as a reference data set</description>
    </item>
    <item>
      <title>Met Office UK Land Surface Observations</title>
      <link>https://registry.opendata.aws/met-office-uk-land-observations</link>
      <guid>https://registry.opendata.aws/met-office-uk-land-observations</guid>
      <description>Land surface weather observations for 31 parameters from over 250 locations across the Met Office UK land observation network. The data is available as CSV files. You can use it to monitor the latest weather affecting a specific location so you can plan for your business or operations.
&lt;br&gt;&lt;br&gt;
The observations are produced every minute and transmitted to the Amazon Registry of Open Data every hour. They’re available for a rolling 7-day period (168 hours).
&lt;br&gt;
All locations in the observation network are within the bounding box:&lt;ul&gt;
&lt;li&gt;-15 (West)&lt;/li&gt;
&lt;li&gt;48 (South)&lt;/li&gt;
&lt;li&gt;5 (East)&lt;/li&gt;
&lt;li&gt;62 (North)
On average they are about 40km apart, distributed uniformly to detect as many weather features as possible.
&lt;br&gt;&lt;br&gt;
31 meteorological parameters are measured across the observation network. But not all locations record all parameters. Check the documentation for the full list of parameters.&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>Met Office UK Marine Observations</title>
      <link>https://registry.opendata.aws/met-office-uk-marine-observations</link>
      <guid>https://registry.opendata.aws/met-office-uk-marine-observations</guid>
      <description>Marine surface weather observations for 32 parameters from 69 locations across the Met Office marine observation network. Observations are available for a rolling 7-day period (168 hours). The data is available as CSV files.&lt;br&gt;&lt;br&gt;
The data comes from moored buoys, light vessels and ships with automatic weather stations onboard. Buoys and light vessels are static and you can view their locations on the &lt;a href&#x3D;&quot;https://weather.metoffice.gov.uk/specialist-forecasts/coast-and-sea/observations&quot;&gt;Met Office Marine Observations page&lt;/a&gt;. You can use the data to monitor the latest weather affecting a specific marine location so you can plan for your business or operations.&lt;br&gt;&lt;br&gt;
&lt;a href&#x3D;&quot;https://forms.office.com/Pages/ResponsePage.aspx?id&#x3D;YYHxF9cgRkeH_VD-PjtmGdxioYGoFbFIkZuB_q8Fb3VUQkoxRVQzTFdUMzNMVzczWVM5VTc3QTY3MC4u&quot;&gt;Join the Met Office research panel&lt;/a&gt; to help us understand how people interact with weather and climate data, uncover challenges and explore opportunities. </description>
    </item>
    <item>
      <title>Met Office UK Radar Observations on a 2-year rolling archive</title>
      <link>https://registry.opendata.aws/met-office-uk-radar-observations</link>
      <guid>https://registry.opendata.aws/met-office-uk-radar-observations</guid>
      <description>The United Kingdom Composite, Surface Rain Rate Estimate is an international radar composite produced by Met Office (UK). This is a composite, radar reflectivity derived, surface rain rate estimate product in HDF5 code from stations covering the United Kingdom.</description>
    </item>
    <item>
      <title>Multi-robot, Multi-Sensor, Multi-Environment Event Dataset (M3ED)</title>
      <link>https://registry.opendata.aws/m3ed</link>
      <guid>https://registry.opendata.aws/m3ed</guid>
      <description>M3ED is the first multi-sensor event camera (EC) dataset focused on high-speed dynamic motions in robotics applications. M3ED provides high-quality synchronized data from multiple platforms (car, legged robot, UAV), operating in challenging conditions such as off-road trails, dense forests, and performing aggressive flight maneuvers. M3ED also covers demanding operational scenarios for EC, such as high egomotion and multiple independently moving objects. M3ED includes high-resolution stereo EC (1280×720), grayscale and RGB cameras, a high-quality IMU, a 64-beam LiDAR, and RTK localization.</description>
    </item>
    <item>
      <title>MultiCoNER Datasets</title>
      <link>https://registry.opendata.aws/multiconer</link>
      <guid>https://registry.opendata.aws/multiconer</guid>
      <description>MultiCoNER 1 is a large multilingual dataset (11 languages) for Named Entity Recognition. It is designed to represent some of the contemporary challenges in NER, including low-context scenarios (short and uncased text), syntactically complex entities such as movie titles, and long-tail entity distributions. MultiCoNER 2 is a large multilingual dataset (12 languages) for fine grained Named Entity Recognition. Its fine-grained taxonomy contains 36 NE classes, representing real-world challenges for NER, where named entities, apart from the surface form, context represents a critical role in distinguishing between the different fine-grained types (e.g. Scientist vs. Athlete). Furthermore, the test data of MultiCoNER 2 contains noisy instances, where the noise has been applied to both context tokens as well as the entity tokens. The noise includes typing errors at character level based on keyboard layouts in the the different languages.</description>
    </item>
    <item>
      <title>My School Today</title>
      <link>https://registry.opendata.aws/sdgstoday-mst</link>
      <guid>https://registry.opendata.aws/sdgstoday-mst</guid>
      <description>This database provides estimates of walking travel time of school-aged populations to schools recorded in OpenStreetMap. Population counts of male and female students are sorted into 3 groups of travel time - under 30 minutes, 30-60 minutes, and over 60 minutes. It covers the African continent and is aggregated by first-level administrative divisions.</description>
    </item>
    <item>
      <title>NCBI SRA Gene Feature RNA-Seq counts</title>
      <link>https://registry.opendata.aws/ncbi-sra-rnaseq</link>
      <guid>https://registry.opendata.aws/ncbi-sra-rnaseq</guid>
      <description>The NIH Sequence Read Archive (SRA), hosted by the [National Center for Biotechnology Information (NCBI) at the National Library of Medicine (NLM) stores sequencing data and alignment information from high-throughput next-generation sequencing platforms. SRA has conducted gene expression analysis of publicly released human and mouse RNA-Seq experiments to process raw RNA-seq reads into concise formats that summarize the expression results. The un-normalized feature counts for each SRA record are available in tab-delimited (*.tsv) format. The tsv files include two columns, the gene id and count. These counts facilitate differential gene expression analyses, particularly across studies and the entirety of the SRA corpus.</description>
    </item>
    <item>
      <title>NCEP/CPC L3 Half Hourly 4km Global (60S - 60N) Merged IR V1 (GPM_MERGIR) at GES DISC</title>
      <link>https://registry.opendata.aws/nasa-gpmmergir</link>
      <guid>https://registry.opendata.aws/nasa-gpmmergir</guid>
      <description>These data originate from NOAA/NCEP.The NOAA Climate Prediction Center/NCEP/NWS is making the data available originally in binary format, in a weekly rotating archive. The NASA GES DISC is acquiring the binary files as they become available, converts them into CF (Climate and Forecast) -convention compliant netCDF-4 format, and stores the product in a permanent archive. The original record started from February, 2000, but in June, 2025 it was extended back to January, 1998.The leading edge of data availability is delayed by about 24 hours from real-time to abide by international data exchange agreements between NOAA and EUMETSAT (the METEOSAT data providers).The data contain globally-merged (60°S-60°N) 4-km pixel-resolution IR brightness temperature data (equivalent blackbody temps), merged from the European, Japanese, and U.S. geostationary satellites over the period of record (GOES-8/9/10/11/12/13/14/15/16/17/18/19, METEOSAT-5/7/8/9/10/11, and GMS-5/MTSat-1R/2/Himawari-8/9).The global geo-IR are dynamically calibrated to GOES East, using a 35 day trailing inter-calibration using time/space-matched IR Tb’s at the mid-point between sub-satellite positions.  In the event of duplicate data in a grid box, the value with the smaller zenith angle is taken. The data have been corrected for &amp;quot;zenith angle dependence&amp;quot;, in which IR temperatures for locations far from satellite nadir are erroneously cold due to a combination of geometric effects and radiometric path extinction effects (Joyce et al. 2001). Finally, the data are re-navigated for parallax, which shifts the geo-location of the GEO-IR footprints to approximately account for the cloud tops that the IR “sees” being displaced away from their actual geographic location when viewed along a slanted path. These corrections allow for the merging of the IR data from the various GEO-satellites with greatly reduced discontinuities at GEO-satellite data boundaries. In the event of duplicate data in a grid box, the value with the smaller zenith angle is taken.The NASA GES DISC is curating these data in a self-documenting, CF-compliant, netCDF-4 format, which allows a broad range of applications to access the data directly, without the need to cope with the original binary data format. In addition to the direct download of netCDF-4 data, the GES DISC provides data download in binary, ASCII, and netCDF-3 formats using the OPeNDAP interface.&lt;h2 id&#x3D;&quot;similarities-with-the-original&quot;&gt;Similarities with the original&lt;/h2&gt;
As in the original binaries, every netCDF-4 file covers one hour, and contains two half-hourly grids, at 4-km grid cell resolution. &lt;h2 id&#x3D;&quot;differences-from-the-original&quot;&gt;Differences from the original&lt;/h2&gt;
&lt;ol&gt;
&lt;li&gt;The data in the netCDF-4 files are already converted to real (float) values of Brightness Temperatures in Kelvin. There is no need to further scale these data. The netCDF-4 format is machine-independent and users need not worry about the endian-ness of their machines. &lt;/li&gt;
&lt;li&gt;To meet the requirements of collection spatial metadata, the grid is re-ordered from the original and now goes from -180 (West) to 180 (East). It is also starting from -60 (South).&lt;/li&gt;
&lt;/ol&gt;
The data and time units are reflected in the corresponding &amp;quot;units&amp;quot; attributes, and grid dimensions are described by longitude (&amp;quot;lon&amp;quot;), latitude (&amp;quot;lat&amp;quot;) and &amp;quot;time&amp;quot; vectors. Thus, any CF-compliant tool should automatically understand the setup in the data files and the starting time for each half-hourly grid. Even without such tools, simple &amp;quot;ncdump&amp;quot; or &amp;quot;h5dump&amp;quot; command line tools will easily disclose the netCDF-4 files configuration.&lt;h2 id&#x3D;&quot;acknowledgements&quot;&gt;Acknowledgements&lt;/h2&gt;
The creation of the original data at NOAA/NCEP is supported by funding from the NOAA Office of Global Programs for the Global Precipitation Climatology Project (GPCP) and by NASA via the Tropical Rainfall Measuring Mission (TRMM). The permanent archive at GES DISC is supported by NASA&amp;#39;s HQ Earth Science Data Systems (ESDS) Program. Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>NEOWISE Post-Cryo Data | Wide-field Infrared Survey Explorer (WISE)</title>
      <link>https://registry.opendata.aws/wise-postcryo</link>
      <guid>https://registry.opendata.aws/wise-postcryo</guid>
      <description>The Wide-field Infrared Survey Explorer (WISE) was a NASA Medium Explorer satellite in low-Earth orbit that conducted an all-sky astronomical imaging survey over four infrared bands from 2010-2011. The NEOWISE Post-Cryo Data Release contains 3.4 and 4.6 micron (W1 and W2) imaging data that were acquired between 29 September 2010 and 1 February 2011 following the exhaustion of the inner and outer cryogen tanks.</description>
    </item>
    <item>
      <title>NEOWISE Reactivation Data | Near-Earth Object Wide-field Infrared Survey Explorer (NEOWISE)</title>
      <link>https://registry.opendata.aws/wise-neowiser</link>
      <guid>https://registry.opendata.aws/wise-neowiser</guid>
      <description>The Near-Earth Object Wide-field Infrared Survey Explorer (NEOWISE) is a NASA Medium-class Explorer satellite in low-Earth orbit conducting an all-sky astronomical imaging survey over two infrared bands. The NEOWISE Reactivation mission began in 2013 when the original WISE satellite was brought out of hibernation to learn more about the population of near-Earth objects and comets that could pose an impact hazard to the Earth. The data is also used to study a wide range of astrophysical phenomena in the time domain including brown dwarfs, supernovae and active galactic nuclei.</description>
    </item>
    <item>
      <title>NOAA Coastal Lidar Data</title>
      <link>https://registry.opendata.aws/noaa-coastal-lidar</link>
      <guid>https://registry.opendata.aws/noaa-coastal-lidar</guid>
      <description>Lidar (light detection and ranging) is a technology that can measure the 3-dimentional location of objects, including the solid earth surface. The data consists of a point cloud of the positions of solid objects that reflected a laser pulse, typically from an airborne platform. In addition to the position, each point may also be attributed by the type of object it reflected from, the intensity of the reflection, and other system dependent metadata. The NOAA Coastal Lidar Data is a collection of lidar projects from many different sources and agencies, geographically focused on the coastal areas of the United States of America. The data is provided in Entwine Point Tiles (EPT; &lt;a href&#x3D;&quot;https://entwine.io&quot;&gt;https://entwine.io&lt;/a&gt;) format, which is a lossless streamable octree of the point cloud, and in LAZ format. Datasets are maintained in their original projects and care should be taken when merging projects. The coordinate reference system for the data is The NAD83(2011) UTM zone appropriate for the center of each data set for EPT and geographic coordinates for LAZ. Vertically they are in the orthometric datum appropriate for that area (for example, NAVD88 in the mainland United States, PRVD02 in Puerto Rico, or GUVD03 in Guam). The geoid model used is reflected in the data set resource name. &lt;br&gt;The data are organized under directories entwine and laz for the EPT and LAZ versions respectively. Some datasets are not in EPT format, either because the dataset is already in EPT on the USGS public lidar site, they failed to build or their content does not work well in EPT format. Topobathy lidar datasets using the topobathy domain profile do not translate well to EPT format.</description>
    </item>
    <item>
      <title>NOAA Global Surface Summary of Day</title>
      <link>https://registry.opendata.aws/noaa-gsod</link>
      <guid>https://registry.opendata.aws/noaa-gsod</guid>
      <description>Global Surface Summary of the Day is derived from The Integrated Surface Hourly (ISH) dataset. The ISH dataset includes global data obtained from the USAF Climatology Center, located in the Federal Climate Complex with NCDC. The latest daily summary data are normally available 1-2 days after the date-time of the observations used in the daily summaries. The online data files begin with 1929 and are at the time of this writing at the Version 8 software level. Over 9000 stations&amp;#39; data are typically available. The daily elements included in the dataset (as available from each station) are: &lt;br/&gt;
Mean temperature (.1 Fahrenheit) &lt;br/&gt;
Mean dew point (.1 Fahrenheit) &lt;br/&gt;
Mean sea level pressure (.1 mb) &lt;br/&gt;
Mean station pressure (.1 mb) &lt;br/&gt;
Mean visibility (.1 miles) &lt;br/&gt;
Mean wind speed (.1 knots) &lt;br/&gt;
Maximum sustained wind speed (.1 knots) &lt;br/&gt;
Maximum wind gust (.1 knots) &lt;br/&gt;
Maximum temperature (.1 Fahrenheit) &lt;br/&gt;
Minimum temperature (.1 Fahrenheit) &lt;br/&gt;
Precipitation amount (.01 inches) &lt;br/&gt;
Snow depth (.1 inches) &lt;br/&gt;
Indicator for occurrence of: Fog, Rain or Drizzle, Snow or Ice Pellets, Hail, Thunder, Tornado/Funnel Cloud.&lt;br/&gt;&lt;br/&gt;
Global summary of day data for 18 surface meteorological elements are derived from the synoptic/hourly observations contained in USAF DATSAV3 Surface data and Federal Climate Complex Integrated Surface Hourly (ISH). Historical data are generally available for 1929 to the present, with data from 1973 to the present being the most complete. For some periods, one or more countries&amp;#39; data may not be available due to data restrictions or communications problems. In deriving the summary of day data, a minimum of 4 observations for the day must be present (allows for stations which report 4 synoptic observations/day). Since the data are converted to constant units (e.g, knots), slight rounding error from the originally reported values may occur (e.g, 9.9 instead of 10.0). The mean daily values described below are based on the hours of operation for the station. For some stations/countries, the visibility will sometimes &amp;#39;cluster&amp;#39; around a value (such as 10 miles) due to the practice of not reporting visibilities greater than certain distances. The daily extremes and totals--maximum wind gust, precipitation amount, and snow depth--will only appear if the station reports the data sufficiently to provide a valid value. Therefore, these three elements will appear less frequently than other values. Also, these elements are derived from the stations&amp;#39; reports during the day, and may comprise a 24-hour period which includes a portion of the previous day. The data are reported and summarized based on Greenwich Mean Time (GMT, 0000Z - 2359Z) since the original synoptic/hourly data are reported and based on GMT.</description>
    </item>
    <item>
      <title>NOAA HYSPLIT-compatible meteorological data archives</title>
      <link>https://registry.opendata.aws/noaa-arl-hysplit</link>
      <guid>https://registry.opendata.aws/noaa-arl-hysplit</guid>
      <description>The HYSPLIT model is a complete system for computing simple air parcel trajectories, as well as complex transport, dispersion, chemical transformation, and deposition simulations. HYSPLIT continues to be one of the most extensively used atmospheric transport and dispersion models in the atmospheric sciences community. A common application is a back trajectory analysis to determine the origin of air masses and establish source-receptor relationships. HYSPLIT has also been used in a variety of simulations describing the atmospheric transport, dispersion, and deposition of pollutants and hazardous materials. Some examples of the applications include tracking and forecasting the release of radioactive material, wildfire smoke, windblown dust, pollutants from various stationary and mobile emission sources, allergens and volcanic ash.
The National Weather Service&amp;#39;s National Centers for Environmental Prediction (NCEP) runs a series of computer analyses and forecasts operationally. NOAA&amp;#39;s Air Resources Laboratory (ARL) routinely uses NCEP model data for use in air quality transport and dispersion modeling calculations. In 1989 ARL began to archive some of these datasets for future research studies. ARL has in the past, or is presently archiving the following NCEP datasets that are compatible with HYSPLIT. A few datasets that are created outside NOAA are also included. HYSPLIT-compatible meteorological datasets are required to run HYSPLIT for trajectory or dispersion simulations. The HYSPLIT-compatible meteorological datasets can also be used with HYSPLIT utilities to display and/or extract meteorological data from the datasets.</description>
    </item>
    <item>
      <title>NOAA Integrated Surface Database (ISD)</title>
      <link>https://registry.opendata.aws/noaa-isd</link>
      <guid>https://registry.opendata.aws/noaa-isd</guid>
      <description>The Integrated Surface Database (ISD) consists
of global hourly and synoptic observations
compiled from numerous sources into a gzipped
fixed width format. ISD was developed as a joint
activity within Asheville&amp;#39;s Federal Climate
Complex. The database includes over 35,000 stations
worldwide, with some having data as far back
as 1901, though the data show a substantial
increase in volume in the 1940s and again in
the early 1970s. Currently, there are over
14,000 &amp;quot;active&amp;quot; stations updated daily in the
database. The total uncompressed data volume is
around 600 gigabytes; however, it continues to
grow as more data are added. ISD includes
numerous parameters such as wind speed and
direction, wind gust, temperature, dew point,
cloud data, sea level pressure, altimeter setting,
station pressure, present weather, visibility,
precipitation amounts for various time periods,
snow depth, and various other elements as observed
by each station.</description>
    </item>
    <item>
      <title>NOAA MRMS - dynamical.org Icechunk Zarr</title>
      <link>https://registry.opendata.aws/dynamical-noaa-mrms</link>
      <guid>https://registry.opendata.aws/dynamical-noaa-mrms</guid>
      <description>&lt;p&gt;The NOAA Multi-Radar/Multi-Sensor System (MRMS) integrates data from multiple radars and radar networks, surface observations, numerical weather prediction (NWP) models, and climatology to generate seamless, high spatio-temporal resolution mosaics at low latency focused on hail, wind, tornado, quantitative precipitation estimations, convection, icing, and turbulence.&lt;/p&gt;
&lt;p&gt;These datasets have been translated to cloud-optimized Icechunk Zarr format by &lt;a href&#x3D;&quot;https://dynamical.org&quot;&gt;dynamical.org&lt;/a&gt;.&lt;/p&gt;
&lt;ul&gt;
  &lt;li&gt;&lt;a href&#x3D;&quot;https://dynamical.org/catalog/noaa-mrms-conus-analysis-hourly/&quot;&gt;NOAA MRMS CONUS analysis, hourly&lt;/a&gt; - Hourly precipitation analysis from the Multi-Radar Multi-Sensor (MRMS) system operated by NOAA NWS NCEP.&lt;/li&gt;
&lt;/ul&gt;
</description>
    </item>
    <item>
      <title>NOAA Multi-Year Reanalysis of Remotely Sensed Storms (MYRORSS)</title>
      <link>https://registry.opendata.aws/noaa-oar-myrorss-pds</link>
      <guid>https://registry.opendata.aws/noaa-oar-myrorss-pds</guid>
      <description>The Multi-Year Reanalysis of Remotely Sensed Storms (MYRORSS) consists of radar reflectivity data run through the Multi-Radar, Multi-Sensor (MRMS) framework to create a three-dimensional radar volume on a quasi-Cartesian latitude-longitude grid across the entire contiguous United States. The radar reflectivity grid is also combined with hourly forecast model analyses to produce derived products such as echo top heights and hail size estimates. Radar Doppler velocity data was also processed into two azimuthal shear layer products. The source radar data was from the &lt;a href&#x3D;&quot;https://registry.opendata.aws/noaa-nexrad/&quot;&gt;NEXRAD Level-II archive&lt;/a&gt; and the model analyses came from &lt;a href&#x3D;&quot;https://www.ncei.noaa.gov/has/HAS.FileAppRouter?datasetname&#x3D;RUCANL130&amp;amp;subqueryby&#x3D;STATION&amp;amp;applname&#x3D;&amp;amp;outdest&#x3D;FILE&quot;&gt;NOAA&amp;#39;s Rapid Update Cycle model&lt;/a&gt;. Radar reflectivity was quality controlled to remove non-weather echoes and the data set was manually quality contolled to remove errors as revealed through inspection of daily accumulations of the hail size product and the azimuthal shear products. MYRORSS contains data from April 1998 through December 2011. The horizontal resolution is 0.01&lt;span&gt;&amp;#176;&lt;/span&gt; by 0.01&lt;span&gt;&amp;#176;&lt;/span&gt; and the vertical spacing is stretched where at the lowest levels the spacing is 250-m and at the top of the domain 1000-m. The radar data was merged at imperfect timesteps, though in general the temporal spacing is around 5-min. </description>
    </item>
    <item>
      <title>NOAA National Digital Forecast Database (NDFD)</title>
      <link>https://registry.opendata.aws/noaa-ndfd</link>
      <guid>https://registry.opendata.aws/noaa-ndfd</guid>
      <description>&lt;br /&gt;
&lt;br /&gt;
The National Digital Forecast Database (NDFD) is a suite of gridded forecasts of sensible weather elements (e.g., cloud cover, maximum temperature).  Forecasts prepared by NWS field offices working in collaboration with the National Centers for Environmental Prediction (NCEP) are combined in the NDFD to create a seamless mosaic of digital forecasts from which operational NWS products are generated. The most recent data is under the opnl and expr prefixes. A copy is also placed under the wmo prefix. The wmo prefix is structured like so: wmo/&amp;lt;parameter&amp;gt;/&amp;lt;year&amp;gt;/&amp;lt;month&amp;gt;/&amp;lt;day&amp;gt;/&amp;lt;wmo-file-name&amp;gt; The wmo filename codes can be deciphered using the spreadsheet in the root of the bucket.
</description>
    </item>
    <item>
      <title>NOAA National Water Model Short-Range Forecast</title>
      <link>https://registry.opendata.aws/noaa-nwm-pds</link>
      <guid>https://registry.opendata.aws/noaa-nwm-pds</guid>
      <description>The National Water Model (NWM) is a water resources model that simulates and forecasts water
budget variables, including snowpack, evapotranspiration, soil moisture and streamflow, over
the entire continental United States (CONUS). The model, launched in August 2016, is designed
to improve the ability of NOAA to meet the needs of its stakeholders (forecasters, emergency
managers, reservoir operators, first responders, recreationists, farmers, barge operators, and
ecosystem and floodplain managers) by providing expanded accuracy, detail, and frequency of water
information. It is operated by NOAA’s Office of Water Prediction. This bucket contains a four-week
rollover of the Short Range Forecast model output and the corresponding forcing data for the
model. The model is forced with meteorological data from the High Resolution Rapid Refresh (HRRR)
and the Rapid Refresh (RAP) models. The Short Range Forecast configuration cycles hourly and produces
hourly deterministic forecasts of streamflow and hydrologic states out to 18 hours.</description>
    </item>
    <item>
      <title>NOAA S-111 Surface Water Currents Data</title>
      <link>https://registry.opendata.aws/noaa-s111</link>
      <guid>https://registry.opendata.aws/noaa-s111</guid>
      <description>S-111 is a data and metadata encoding specification that is part of the &lt;a href&#x3D;&quot;https://iho.int/en/s100-project&quot;&gt;S-100 Universal Hydrographic Data Model&lt;/a&gt;, an international standard for hydrographic data. This collection of data contains surface water currents forecast guidance from &lt;a href&#x3D;&quot;https://tidesandcurrents.noaa.gov/models.html&quot;&gt;NOAA/NOS Operational Forecast Systems&lt;/a&gt;, a set of operational hydrodynamic nowcast and forecast modeling systems, for various U.S. coastal waters and the great lakes. The collection also contains surface current forecast guidance output from the &lt;a href&#x3D;&quot;https://polar.ncep.noaa.gov/global/&quot;&gt;NCEP Global Real-Time Ocean Forecast System (GRTOFS)&lt;/a&gt; for some offshore areas. These datasets are encoded as HDF-5 files conforming to the S-111 specification, and are geospatially subset into individual tiles conforming to the NOAA/OCS Nautical Product Tiling Scheme, with filenames indicating the corresponding NOAA Electronic Navigational Chart (ENC) Cell Identifier.
A full set of S-111 tiles is created for each new model run cycle, which occurs four times per day for all models except for RTOFS, which updates only once per day. Files are organized using a path naming convention that includes the OFS identifier (e.g. &amp;#39;cbofs&amp;#39; corresponding with output from the Chesapeake Bay Operational Forecast System) as well as the year, month, day, and hour corresponding with each model run initialization time. Each individual S-111 (HDF-5) file contains all forecast projections from a single model run for that geographic area. In other words, a single S-111 file will contain multiple gridded arrays each containing a forecast valid at a distinct time in the future, out to the forecast horizon of the underlying modeling system. All surface currents forecasts in this collection are computed at a depth of 4.5 meters below water surface, or half the water column depth, whichever is shallower.</description>
    </item>
    <item>
      <title>NOAA U.S. Climate Normals</title>
      <link>https://registry.opendata.aws/noaa-climate-normals</link>
      <guid>https://registry.opendata.aws/noaa-climate-normals</guid>
      <description>The U.S. Climate Normals are a large suite of data products that provide information about typical climate conditions for thousands of locations across the United States. Normals act both as a ruler to compare today’s weather and tomorrow’s forecast, and as a predictor of conditions in the near future. The official normals are calculated for a uniform 30 year period, and consist of annual/seasonal, monthly, daily, and hourly averages and statistics of temperature, precipitation, and other climatological variables from almost 15,000 U.S. weather stations. &lt;br/&gt;&lt;br/&gt;
NCEI generates the official U.S. normals every 10 years in keeping with the needs of our user community and the requirements of the World Meteorological Organization (WMO) and National Weather Service (NWS). The 1991–2020 U.S. Climate Normals are the latest in a series of decadal normals first produced in the 1950s. These data allow travelers to pack the right clothes, farmers to plant the best crop varieties, and utilities to plan for seasonal energy usage. Many other important economic decisions that are made beyond the predictive range of standard weather forecasts are either based on or influenced by climate normals.</description>
    </item>
    <item>
      <title>NOAA Wave Ensemble Reforecast</title>
      <link>https://registry.opendata.aws/noaa-wave-ensemble-reforecast</link>
      <guid>https://registry.opendata.aws/noaa-wave-ensemble-reforecast</guid>
      <description>This is a 20-year global wave reforecast generated by WAVEWATCH III model (&lt;a href&#x3D;&quot;https://github.com/NOAA-EMC/WW3&quot;&gt;https://github.com/NOAA-EMC/WW3&lt;/a&gt;) forced by GEFSv12 winds (&lt;a href&#x3D;&quot;https://noaa-gefs-retrospective.s3.amazonaws.com/index.html&quot;&gt;https://noaa-gefs-retrospective.s3.amazonaws.com/index.html&lt;/a&gt;). The wave ensemble was run with one cycle per day (at 03Z), spatial resolution of 0.25°X0.25° and temporal resolution of 3 hours. There are five ensemble members (control plus four perturbed members) and, once a week (Wednesdays), the ensemble is expanded to eleven members. The forecast range is 16 days and, once a week (Wednesdays), it extends to 35 days. More information about the wave modeling, wave grids and calibration can be found in the WAVEWATCH III regtest ww3_ufs1.3 (&lt;a href&#x3D;&quot;https://github.com/NOAA-EMC/WW3/tree/develop/regtests/ww3_ufs1.3&quot;&gt;https://github.com/NOAA-EMC/WW3/tree/develop/regtests/ww3_ufs1.3&lt;/a&gt;).
&lt;br/&gt;&lt;br/&gt;
The 20 years of reforecast results were analyzed and quality-controlled. Three output types are available
&lt;br/&gt;&lt;br/&gt;&lt;ol&gt;
&lt;li&gt;Global wave fields, in grib2 format, with several variables including significant wave height, period, direction, and partitions;&lt;br/&gt;&lt;/li&gt;
&lt;li&gt;Point output tables, in netcdf format, containing time-series of significant wave height, period and direction, for 658 points (latitude/longitude informed) at the positions of wave buoys;  and,&lt;br/&gt;&lt;/li&gt;
&lt;li&gt;For the same positions, spectral outputs are available, in netcdf format, containing the full spectra (2D directional spectrum).&lt;br/&gt;
Each file refers to one forecast cycle with date (year, month, day) written in the file name.
&lt;br/&gt;
&lt;br/&gt;
This effort has been funded by a NOAA OAR/NWS Service Level Agreement (SLA) whereby NOAA/OAR supports R&amp;D and transition needed for mission delivery of climate
services within NWS. The SLA project is led by NWS/NCEP/Ocean Prediction Center in collaboration with NWS/NCEP/Environmental Modeling Center and NWS/NCEP/Climate 
Prediction Center. This is a project also in cooperation with NOAA’s Atlantic Oceanographic and Meteorological Laboratory (AOML) and the University of Miami’s 
Cooperative Institute for Marine and Atmospheric Studies (CIMAS).
&lt;br/&gt;
&lt;br/&gt;
The following github repository has examples and scripts to support users to download, visualize, and process the WAVEWATCH III output files
&lt;br/&gt;
&lt;br/&gt;
https://github.com/ricampos/gefswaves_reforecast
&lt;br/&gt;
&lt;br/&gt;
The reforecast simulations were generated on the supercomputer Orion, which is funded via a grant from NOAA to support research activities in environmental  
modeling, including weather modeling and simulation
&lt;br/&gt;
&lt;br/&gt;
https://www.noaa.gov/organization/information-technology/orion&lt;/li&gt;
&lt;/ol&gt;
</description>
    </item>
    <item>
      <title>NOAA nClimGrid and Livneh Gridded Historical Climate Observation Thresholds</title>
      <link>https://registry.opendata.aws/noaa-cris-hist</link>
      <guid>https://registry.opendata.aws/noaa-cris-hist</guid>
      <description>Livneh and nClimGrid are gridded observed historical climatology data that were used in the LOCA2 and STAR-ESDM downscaling process of global climate models as part of the 5th National Climate Assessment. The original Livneh and nClimGrid daily temperature and precipitation observations have been converted to a series of decision-relevant thresholds as part of the &lt;a href&#x3D;&quot;https://cris.climate.gov/pages/about&quot;&gt;(U.S. Climate Resilience Information System (CRIS))&lt;/a&gt;. These thresholds, such as days with extreme heat or precipitation, have been calculated to match the future projections from LOCA2 and STAR, also available in CRIS.</description>
    </item>
    <item>
      <title>NOAA/PMEL Ocean Climate Stations Moorings</title>
      <link>https://registry.opendata.aws/noaa-ocean-climate-stations</link>
      <guid>https://registry.opendata.aws/noaa-ocean-climate-stations</guid>
      <description>The mission of the Ocean Climate Stations (OCS) Project is to make meteorological and 
oceanic measurements from autonomous platforms.  Calibrated, quality-controlled, and well-documented 
climatological measurements are available on the OCS webpage and the OceanSITES Global Data
Assembly Centers (GDACs), with near-realtime data available prior to release of the complete, 
downloaded datasets.&lt;br/&gt;&lt;br/&gt;OCS measurements served through the Big Data Program come from OCS high-latitude moored buoys located in the Kuroshio 
Extension (32°N 145°E) and the Gulf of Alaska (50°N 145°W).  Initiated in 2004 and 2007, 
the respective moored buoys, KEO and Papa, measure a suite of surface and subsurface essential ocean variables.
The surface suite includes air temperature, relative humidity, shortwave and longwave radiation, barometric pressure, winds, and rain, 
while subsurface instrumentation includes temperature, salinity, and ocean currents.  Individual buoy deployments are stitched together into 
a continuous time-series, which is synced to the OceanSITES GDACs, and subsequently, to BDP.</description>
    </item>
    <item>
      <title>NSF NCAR Curated ECMWF Reanalysis 5 (ERA5)</title>
      <link>https://registry.opendata.aws/nsf-ncar-era5</link>
      <guid>https://registry.opendata.aws/nsf-ncar-era5</guid>
      <description>NSF NCAR is providing a NetCDF-4 structured version of the 0.25 degree atmospheric ECMWF Reanalysis 5 (ERA5) to the AWS ODSP. ERA5 is produced using high-resolution forecasts (HRES) at 31 kilometer resolution (one fourth the spatial resolution of the operational model) and a 62 kilometer resolution ten member 4D-Var ensemble of data assimilation (EDA) in CY41r2 of ECMWF&amp;#39;s Integrated Forecast System (IFS) with 137 hybrid sigma-pressure (model) levels in the vertical, up to a top level of 0.01 hPa. Atmospheric data on these levels are interpolated to 37 pressure levels (the same levels as in ERA-Interim). Surface or single level data are also available, containing 2D parameters such as precipitation, 2 meter temperature, top of atmosphere radiation and vertical integrals over the entire atmosphere. The IFS is coupled to a soil model, the parameters of which are also designated as surface parameters, and an ocean wave model. Generally, the data is available at an hourly frequency and consists of analyses and short (12 hour) forecasts, initialized twice daily from analyses at 06 and 18 UTC. Most analyses parameters are also available from the forecasts. The data are provided in CF-compliant NetCDF4 format files. ERA5 products are used to train ML/AI based weather forecast models and support retrospective climate research use cases, including where to locate solar and wind farms.</description>
    </item>
    <item>
      <title>NYUMets Brain Dataset</title>
      <link>https://registry.opendata.aws/nyumets-brain</link>
      <guid>https://registry.opendata.aws/nyumets-brain</guid>
      <description>This dataset contains 8,000+ brain MRIs of 2,000+ patients with brain metastases.</description>
    </item>
    <item>
      <title>National Herbarium of Israel</title>
      <link>https://registry.opendata.aws/huj-herbarium</link>
      <guid>https://registry.opendata.aws/huj-herbarium</guid>
      <description>Our collection encompasses approximately one million vascular plant specimens from the Mediterranean and Middle East biodiversity hotspot, representing flora from Israel, Jordan, Hermon, Sinai, Egypt, the Caucasus, Arabia, North Africa, and throughout the Mediterranean basin. This scientifically significant repository includes published voucher specimens, original specimens used for &amp;quot;Flora Palaestina&amp;quot; illustrations, and critical references for the Israeli gene bank collections. The ongoing digitization process captures high-resolution images of each specimen while systematically incorporating label information into our computerized catalog. This virtual herbarium will democratize access to these valuable botanical resources, enabling global researchers to examine specimens in exceptional detail from anywhere in the world. Beyond preservation, this digital transformation unlocks new research possibilities through computational analysis of both visual specimen characteristics and associated metadata. The dataset will serve as a foundational resource for advancing botanical research, ecological modeling, taxonomic investigation, historical analysis, and numerous other scientific disciplines concerned with plant biodiversity in this ecologically and historically significant region.</description>
    </item>
    <item>
      <title>Natural Earth</title>
      <link>https://registry.opendata.aws/naturalearth</link>
      <guid>https://registry.opendata.aws/naturalearth</guid>
      <description>Natural Earth is a public domain map dataset available at 1:10m, 1:50m, and 1:110 million scales. Featuring tightly integrated vector and raster data, with Natural Earth you can make a variety of visually pleasing, well-crafted maps with cartography or GIS software.</description>
    </item>
    <item>
      <title>New Jersey Statewide Digital Aerial Imagery Catalog</title>
      <link>https://registry.opendata.aws/nj-imagery</link>
      <guid>https://registry.opendata.aws/nj-imagery</guid>
      <description>The New Jersey Office of GIS, NJ Office of Information Technology manages a series of 11 digital orthophotography and scanned aerial photo maps collected at various years ranging from 1930 to 2017. Each year’s worth of imagery are available as Cloud Optimized GeoTIFF (COG) files and some years are available as compressed MrSID and/or JP2 files.  Additionally, each year of imagery is organized into a tile grid scheme covering the entire geography of New Jersey.  Many years share the same tiling grid while others have unique grids as defined by the project at the time.</description>
    </item>
    <item>
      <title>New Jersey Statewide LiDAR</title>
      <link>https://registry.opendata.aws/nj-lidar</link>
      <guid>https://registry.opendata.aws/nj-lidar</guid>
      <description>Elevation datasets in New Jersey have been collected over several years as several
discrete projects.  Each project covers a geographic area, which is a subsection of
the entire state, and has differing specifications based on the available technology
at the time and project budget.  The geographic extent of one project may overlap that
of a neighboring project. Each of the 18 projects contains deliverable products such
as LAS (Lidar point cloud) files, unclassified/classified, tiled to cover project area;
relevant metadata records or documents, most adhering to the Federal Geographic Data
Committee’s (FGDC) Content Standard for Digital Geospatial Metadata (CSDGM); tiling
index feature class or shapefile; flights lines feature class or shapefile; Digital
Elevation Model in image format or Esri grid format; other derivative data products
such as contour lines feature class or shapefile.</description>
    </item>
    <item>
      <title>OPERA Surface Displacement from Sentinel-1 validated product (Version 1)</title>
      <link>https://registry.opendata.aws/nasa-operal3disp-s1v1</link>
      <guid>https://registry.opendata.aws/nasa-operal3disp-s1v1</guid>
      <description>The Level-3 OPERA Sentinel-1 Surface Displacement (DISP) product is generated through interferometric time-series analysis of Level-2 Coregistered Sentinel-1 Single Look Complex (CSLC) datasets. Using a hybrid Persistent Scatterer (PS) and Distributed Scatterer (DS) approach, this product quantifies Earth&amp;#39;s surface displacement in the radar line-of-sight. The DISP products enable the detection of anthropogenic and natural surface changes, including subsidence, tectonic deformation, and landslides. The OPERA DISP suite comprises complementary datasets derived from Sentinel-1 and NISAR inputs, designated as DISP-S1 and DISP-NI, respectively. Each product, created per acquisition, adheres to a consistent structure, HDF5 file format, file-naming convention, and a 30 m spatial posting. This collection specifically includes DISP-S1 products, derived from Sentinel-1 data. DISP-S1 products provide spatial coverage across North America, encompassing the United States, U.S. territories within 200 km of the U.S. border, Canada, and mainland countries from the southern U.S. border to Panama. These products are generated from Sentinel-1 Interferometric Wide (IW) swath mode acquisitions starting in mid-2016. The OPERA DISP-S1 product contains modified Copernicus Sentinel data (2016-2025).
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://cumulus.asf.alaska.edu/s3credentialsREADME&quot;&gt;https://cumulus.asf.alaska.edu/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>Ohio State Cardiac MRI Raw Data (OCMR)</title>
      <link>https://registry.opendata.aws/ocmr_data</link>
      <guid>https://registry.opendata.aws/ocmr_data</guid>
      <description>OCMR is an open-access repository that provides multi-coil k-space data for cardiac cine.  The fully sampled MRI datasets are intended for quantitative comparison and evaluation of image reconstruction methods. The free-breathing, prospectively undersampled datasets are intended to evaluate their performance and generalizability qualitatively.</description>
    </item>
    <item>
      <title>OpenNeuro</title>
      <link>https://registry.opendata.aws/openneuro</link>
      <guid>https://registry.opendata.aws/openneuro</guid>
      <description>OpenNeuro is a database of openly-available brain imaging data. The data are shared according to a Creative Commons CC0 license, providing a broad range of brain imaging data to researchers and citizen scientists alike. The database primarily focuses on functional magnetic resonance imaging (fMRI) data, but also includes other imaging modalities including structural and diffusion MRI, electroencephalography (EEG), and magnetoencephalograpy (MEG). OpenfMRI is a project of the &lt;a href&#x3D;&quot;http://reproducibility.stanford.edu&quot;&gt;Center for Reproducible Neuroscience at Stanford University&lt;/a&gt;. Development of the OpenNeuro resource has been funded by the National Science Foundation, National Institute of Mental Health, National Institute on Drug Abuse, and the Laura and John Arnold Foundation.</description>
    </item>
    <item>
      <title>OpenSurfaces</title>
      <link>https://registry.opendata.aws/opensurfaces</link>
      <guid>https://registry.opendata.aws/opensurfaces</guid>
      <description>A large database of annotated surfaces created from real-world consumer photographs.</description>
    </item>
    <item>
      <title>OpenUniverse 2024 Simulated Roman &amp; Rubin Images</title>
      <link>https://registry.opendata.aws/openuniverse2024</link>
      <guid>https://registry.opendata.aws/openuniverse2024</guid>
      <description>This release consists of simulated data products designed to mimic observations of the same region of the sky as seen by two astronomical facilities: the Nancy Grace Roman Telescope and the Vera C. Rubin Observatory.</description>
    </item>
    <item>
      <title>Orcasound - bioacoustic data for marine conservation</title>
      <link>https://registry.opendata.aws/orcasound</link>
      <guid>https://registry.opendata.aws/orcasound</guid>
      <description>Live-streamed and archived audio data (~2018-present) from underwater microphones (hydrophones) containing marine biological signals as well as ambient ocean noise. Hydrophone placement and passive acoustic monitoring effort prioritizes detection of orca sounds (calls, clicks, whistles) and potentially harmful noise. Geographic focus is on the US/Canada critical habitat of Southern Resident killer whales (northern CA to central BC) with initial focus on inland waters of WA. In addition to the raw lossy or lossless compressed data, we provide a growing archive of annotated bioacoustic bouts.</description>
    </item>
    <item>
      <title>Oxford Nanopore Technologies Benchmark Datasets</title>
      <link>https://registry.opendata.aws/ont-open-data</link>
      <guid>https://registry.opendata.aws/ont-open-data</guid>
      <description>The ont-open-data registry provides reference sequencing data from Oxford Nanopore Technologies to support, 1) Exploration of the characteristics of nanopore sequence data. 2) Assessment and reproduction of performance benchmarks 3) Development of tools and methods. The data deposited showcases DNA sequences from a representative subset of sequencing chemistries. The datasets correspond to publicly-available reference samples (e.g. Genome In A Bottle reference cell lines). Raw data are provided with metadata and scripts to describe sample and data provenance.</description>
    </item>
    <item>
      <title>PALSAR-2 ScanSAR CARD4L (L2.2)</title>
      <link>https://registry.opendata.aws/jaxa-alos-palsar2-scansar</link>
      <guid>https://registry.opendata.aws/jaxa-alos-palsar2-scansar</guid>
      <description>The 25 m PALSAR-2 ScanSAR is normalized backscatter data of PALSAR-2 broad area observation mode with observation width of 350 km.
  The SAR imagery was ortho-rectificatied and slope corrected using the ALOS World 3D - 30 m (AW3D30) Digital Surface Model.
  Polarization data are stored as 16-bit digital numbers (DN).
  The DN values can be converted to gamma naught values in decibel unit (dB) using the following equation:
  γ0 &#x3D; 10*log10(DN2) - 83.0 dB
  CARD4L stands for CEOS Analysis Ready Data for Land (Level 2.2) data are ortho-rectified and radiometrically terrain-corrected.
  This dataset is compatible with the &lt;a href&#x3D;&quot;https://ceos.org/&quot;&gt;Committee on Earth Observation (CEOS)&lt;/a&gt; &lt;a href&#x3D;&quot;https://ceos.org/ard/files/PFS/NRB/v5.5/CARD4L-PFS_NRB_v5.5.pdf&quot;&gt;Analysis Ready Data for LAND (CARD4L)&lt;/a&gt; standard.&lt;br/&gt;&lt;br/&gt;</description>
    </item>
    <item>
      <title>PALSAR-2 ScanSAR Flooding in Rwanda (L2.1)</title>
      <link>https://registry.opendata.aws/palsar-2-scansar-flooding-in-rwanda</link>
      <guid>https://registry.opendata.aws/palsar-2-scansar-flooding-in-rwanda</guid>
      <description>Torrential rainfall triggered flooding and landslides in many parts of Rwanda. The hardest-hit districts were Ngororero, Rubavu, Nyabihu, Rutsiro and Karongi. According to reports, 14 people have died in Karongi, 26 in Rutsiro, 18 in Rubavu, 19 in Nyabihu and 18 in Ngororero.Rwanda National Police reported that the Mukamira-Ngororero and Rubavu-Rutsiro roads are impassable due to flooding and landslide debris. UNITAR on behalf of United Nations Office for the Coordination of Humanitarian Affairs (OCHA) / Regional Office for Southern &amp;amp; Eastern Africa in cooperation with Rwanda Space Agency (RSA) was activated International Disaster Charter. JAXA has responded to the flood event in Rwanda by conducting emergency disaster observations and providing data as requested by OCHA and RSA through the International Disaster Charter. The 25 m PALSAR-2 ScanSAR is normalized backscatter data of PALSAR-2 broad area observation mode with observation width of 350 km. Polarization data are stored as 16-bit digital numbers (DN). The DN values can be converted to gamma naught values in decibel unit (dB) using the following equation sigma zero &#x3D; 10*log10(DN2) - 83.0 dB. Included in this dataset are ALOS-2 PALSAR-2 ScanSAR 2.1 data. Level 2.1 data is orthorectified from level 1.1 data by using digital elevation model. Pixel spacing is selectable depending on observation modes. Image coordinate in map projection is geocoded.</description>
    </item>
    <item>
      <title>PALSAR-2 ScanSAR Tropical Cycolne Mocha (L2.1)</title>
      <link>https://registry.opendata.aws/palsar-2-scansar-flooding-in-bangladesh</link>
      <guid>https://registry.opendata.aws/palsar-2-scansar-flooding-in-bangladesh</guid>
      <description>Tropical Cyclone Mocha began to form in the Bay of Bengal on 11 May 2023 and continues to intensify as it moves towards Myanmar and Bangladesh.Cyclone Mocha is the first storm to form in the Bay of Bengal this year and is expected to hit several coastal areas in Bangladesh on 14 May with wind speeds of up to 175 km/h.After made its landfall in the coast between Cox’s Bazar (Bangladesh) and Kyaukphyu (Myanmar) near Sittwe (Myanmar). At most, Catastrophic Damage-causing winds was possible especially in the areas of Rakhine State and Chin State, and Severe Damage-causing winds is possible in the areas of Rakhine, Chin, Magway, and Sagaing ([source] TAOS Model, DisasterAWARE). Bangladesh were preparing to evacuate over 500,000 people as the World Meteorological Organisation (WMO) has warned of big humanitarian impacts once the storm makes landfall. Due to its intensity, Cyclone Mocha is expected to inundate several low-lying areas of the delta nation of Bangladesh which could consequently cause landslides.576 cyclone shelters are ready to provide refuge to those evacuated however damage to infrastructure and agriculture would be devastating.Myanmar ? POTENTIAL OF A CATASTROPHIC DISASTER. An estimated 8.7 Million people, 1.9M households, and $35.3 Billion (USD) of infrastructure (total replacement value) were potentially exposed to moderate to severe damaging winds in accordance with AHA Centre.JAXA has responded to the Tropical Cyclone MOCHA by conducting emergency disaster observations and providing data as requested through the International Disaster Charter and Sentinel Asia. The 25 m PALSAR-2 ScanSAR is normalized backscatter data of PALSAR-2 broad area observation mode with observation width of 350 km. Polarization data are stored as 16-bit digital numbers (DN). The DN values can be converted to gamma naught values in decibel unit (dB) using the following equation sigma zero &#x3D; 10*log10(DN2) - 83.0 dB. Included in this dataset are ALOS-2 PALSAR-2 ScanSAR 2.1 data. Level 2.1 data is orthorectified from level 1.1 data by using digital elevation model. Pixel spacing is selectable depending on observation modes. Image coordinate in map projection is geocoded.</description>
    </item>
    <item>
      <title>Quoref</title>
      <link>https://registry.opendata.aws/allenai-quoref</link>
      <guid>https://registry.opendata.aws/allenai-quoref</guid>
      <description>24K Question/Answer (QA) pairs over 4.7K paragraphs, split between train (19K QAs), development (2.4K QAs) and a hidden test partition (2.5K QAs).</description>
    </item>
    <item>
      <title>RSNA Abdominal Trauma Detection (RSNA-ABT)</title>
      <link>https://registry.opendata.aws/rsna-abdominal-trauma-detection</link>
      <guid>https://registry.opendata.aws/rsna-abdominal-trauma-detection</guid>
      <description>Blunt force abdominal trauma is among the most common types of traumatic injury, with the most frequent cause being motor vehicle accidents. Abdominal trauma may result in damage and internal bleeding of the internal organs, including the liver, spleen, kidneys, and bowel. Detection and classification of injuries are key to effective treatment and favorable outcomes. A large proportion of patients with abdominal trauma require urgent surgery. Abdominal trauma often cannot be diagnosed clinically by physical exam, patient symptoms, or laboratory tests. Prompt diagnosis of abdominal trauma using medical imaging is thus critical to patient care. AI tools that assist and expedite diagnosis of abdominal trauma have the potential to substantially improve patient care and health outcomes in the emergency setting. To create the ground truth dataset, RSNA collected imaging data sourced from 23 sites in 14 countries on six continents, including more than 4,000 CT exams with various abdominal injuries and a roughly equal number of cases without injury.</description>
    </item>
    <item>
      <title>RSNA Abdominal Traumatic Injury CT (RATIC)</title>
      <link>https://registry.opendata.aws/rsna-ratic</link>
      <guid>https://registry.opendata.aws/rsna-ratic</guid>
      <description>Blunt force abdominal trauma is among the most common types of traumatic injury, with the most frequent cause being motor vehicle accidents. Abdominal trauma may result in damage and internal bleeding of the internal organs, including the liver, spleen, kidneys, and bowel. Detection and classification of injuries are key to effective treatment and favorable outcomes. A large proportion of patients with abdominal trauma require urgent surgery. Abdominal trauma often cannot be diagnosed clinically by physical exam, patient symptoms, or laboratory tests. Prompt diagnosis of abdominal trauma using medical imaging is thus critical to patient care. AI tools that assist and expedite diagnosis of abdominal trauma have the potential to substantially improve patient care and health outcomes in the emergency setting. To create the ground truth dataset, RSNA collected imaging data sourced from 23 sites in 14 countries on six continents, including more than 4,000 CT exams with various abdominal injuries and a roughly equal number of cases without injury.</description>
    </item>
    <item>
      <title>RSNA Cervical Spine Fracture Detection (RSNA-CSF) Dataset</title>
      <link>https://registry.opendata.aws/rsna-cervical-spine-fracture-detection</link>
      <guid>https://registry.opendata.aws/rsna-cervical-spine-fracture-detection</guid>
      <description>Over 1.5 million spine fractures occur annually in the United States alone resulting in over 17,730 spinal cord injuries annually. The most common site of spine fracture is the cervical spine. There has been a rise in the incidence of spinal fractures in the elderly and in this population, fractures can be more difficult to detect on imaging due to degenerative disease and osteoporosis. Imaging diagnosis of adult spine fractures is now almost exclusively performed with computed tomography (CT). Quickly detecting and determining the location of any vertebral fractures is essential to prevent neurologic deterioration and paralysis after trauma. RSNA has teamed with the American Society of Neuroradiology (ASNR) and the American Society of Spine Radiology (ASSR) to create this ground truth dataset, collecting imaging data from twelve sites on six continents, including approximately 2,000 CT studies. Spine radiology specialists from the ASNR and ASSR provided expert image level annotations these studies to indicate the presence, vertebral level and location of any cervical spine fractures.</description>
    </item>
    <item>
      <title>RSNA Intracranial Aneurysm Detection Dataset (RSNA-ICA)</title>
      <link>https://registry.opendata.aws/rsna-intracranial-aneurysm-detection-dataset</link>
      <guid>https://registry.opendata.aws/rsna-intracranial-aneurysm-detection-dataset</guid>
      <description>The Radiological Society of North America Intracranial Aneurysm Detection (RSNA-ICA) dataset is a collection of over 4,000 CT brain scans annotated by a cohort of over 40 volunteer radiologists from RSNA and the American Society of Neuroradiology to show the presence and location of intracranial aneurysms. It also includes a set of about 200 imaging studies that are annotated with AI-generated segmentations highlighting abnormalities. The imaging data was provided by 18 institutions. Initially compiled in 2025 for the RSNA Intracranial Aneurysm Detection AI Challenge hosted on Kaggle competition platform (&lt;a href&#x3D;&quot;https://www.kaggle.com/competitions/rsna-intracranial-aneurysm-detection&quot;&gt;https://www.kaggle.com/competitions/rsna-intracranial-aneurysm-detection&lt;/a&gt;), it represents the largest publicly available collection of its kind. Additional information on the dataset and how to make use of it is provided in a forthcoming Data Resource Publication listed below, as well as on the Kaggle competition website, which also provides access to models developed during the competition.</description>
    </item>
    <item>
      <title>RSNA Intracranial Hemorrhage Detection</title>
      <link>https://registry.opendata.aws/rsna-intracranial-hemorrhage-detection</link>
      <guid>https://registry.opendata.aws/rsna-intracranial-hemorrhage-detection</guid>
      <description>RSNA assembled this dataset in 2019 for the RSNA Intracranial Hemorrhage Detection AI Challenge (&lt;a href&#x3D;&quot;https://www.kaggle.com/c/rsna-intracranial-hemorrhage-detection/&quot;&gt;https://www.kaggle.com/c/rsna-intracranial-hemorrhage-detection/&lt;/a&gt;). De-identified head CT studies were provided by four research institutions. A group of over 60 volunteer expert radiologists recruited by RSNA and the American Society of Neuroradiology labeled over 25,000 exams for the presence and subtype classification of acute intracranial hemorrhage.</description>
    </item>
    <item>
      <title>RSNA Lumbar Spine Degenerative Classification Dataset (RSNA-LSDD)</title>
      <link>https://registry.opendata.aws/rsna-lumbar-spine-degenerative-classification-dataset</link>
      <guid>https://registry.opendata.aws/rsna-lumbar-spine-degenerative-classification-dataset</guid>
      <description>The Radiological Society of North America Lumbar Spine Degenerative Classification dataset (RSNA-LSDD) is a collection of over 2,600 magnetic resonance imaging (MR) scans of the lumbar spine annotated by a cohort of about 60 volunteer radiologists recruited by the RSNA, the American Society for Spine Radiology and the American Society of Neuroradiology to identify the location and severity of five degenerative conditions across the five intervertebral disc levels (L1/L2, L2/L3, L3/L4, L4/L5, and L5/S1). The imaging data, comprising over 8,500 image series (Sagittal “T2”, Axial T2 and Sagittal T1), was provided by twelve institutions from across the globe. Initially compiled in 2024 for the RSNA Lumbar Spine Degenerative Classification AI Challenge hosted on Kaggle competition platform (&lt;a href&#x3D;&quot;https://www.kaggle.com/competitions/rsna-2024-lumbar-spine-degenerative-classification&quot;&gt;https://www.kaggle.com/competitions/rsna-2024-lumbar-spine-degenerative-classification&lt;/a&gt;), it represents the largest publicly available collection of its kind. Additional information on the dataset and how to make use of it is provided in the Data Resource Publication listed below, as well as on the Kaggle competition website, which also provides access to models developed during the competition.</description>
    </item>
    <item>
      <title>RSNA Pulmonary Embolism Detection</title>
      <link>https://registry.opendata.aws/rsna-pulmonary-embolism-detection</link>
      <guid>https://registry.opendata.aws/rsna-pulmonary-embolism-detection</guid>
      <description>RSNA assembled this dataset in 2020 for the RSNA STR Pulmonary Embolism Detection AI Challenge (&lt;a href&#x3D;&quot;https://www.kaggle.com/c/rsna-str-pulmonary-embolism-detection/&quot;&gt;https://www.kaggle.com/c/rsna-str-pulmonary-embolism-detection/&lt;/a&gt;). With more than 12,000 CT pulmonary angiography (CTPA) studies contributed by five international research centers, it is the largest publicly available annotated PE dataset. RSNA collaborated with the Society of Thoracic Radiology to recruit more than 80 expert thoracic radiologists who labeled the dataset with detailed clinical annotations.</description>
    </item>
    <item>
      <title>Reasoning Over Paragraph Effects in Situations (ROPES)</title>
      <link>https://registry.opendata.aws/allenai-ropes</link>
      <guid>https://registry.opendata.aws/allenai-ropes</guid>
      <description>14k QA pairs over 1.7K paragraphs, split between train (10k QAs), development (1.6k QAs) and a hidden test partition (1.7k QAs).</description>
    </item>
    <item>
      <title>SENTINEL-1A_DUAL_POL_GRD_HIGH_RES</title>
      <link>https://registry.opendata.aws/nasa-sentinel-1adpgrdhigh</link>
      <guid>https://registry.opendata.aws/nasa-sentinel-1adpgrdhigh</guid>
      <description>Sentinel-1A Dual-pol ground projected high and full resolution images
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://sentinel1.asf.alaska.edu/s3credentialsREADME&quot;&gt;https://sentinel1.asf.alaska.edu/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>SENTINEL-1A_SLC</title>
      <link>https://registry.opendata.aws/nasa-sentinel-1aslc</link>
      <guid>https://registry.opendata.aws/nasa-sentinel-1aslc</guid>
      <description>Sentinel-1A slant-range product
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://sentinel1.asf.alaska.edu/s3credentialsREADME&quot;&gt;https://sentinel1.asf.alaska.edu/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>SENTINEL-1B_DUAL_POL_GRD_HIGH_RES</title>
      <link>https://registry.opendata.aws/nasa-sentinel-1bdpgrdhigh</link>
      <guid>https://registry.opendata.aws/nasa-sentinel-1bdpgrdhigh</guid>
      <description>Sentinel-1B Dual-pol ground projected high and full resolution images
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://sentinel1.asf.alaska.edu/s3credentialsREADME&quot;&gt;https://sentinel1.asf.alaska.edu/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>SENTINEL-1B_SLC</title>
      <link>https://registry.opendata.aws/nasa-sentinel-1bslc</link>
      <guid>https://registry.opendata.aws/nasa-sentinel-1bslc</guid>
      <description>Sentinel-1B slant-range product
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://sentinel1.asf.alaska.edu/s3credentialsREADME&quot;&gt;https://sentinel1.asf.alaska.edu/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>SILAM Air Quality</title>
      <link>https://registry.opendata.aws/silam</link>
      <guid>https://registry.opendata.aws/silam</guid>
      <description>Air Quality is a global SILAM atmospheric composition and air quality forecast performed on a daily basis for &amp;gt; 100 species and covering the troposphere and the stratosphere. The output produces 3D concentration fields and aerosol optical thickness. The data are unique: 20km resolution for global AQ models is unseen worldwide.</description>
    </item>
    <item>
      <title>SPHEREx Quick Release (QR): An All-Sky Spectral Survey</title>
      <link>https://registry.opendata.aws/spherex-qr</link>
      <guid>https://registry.opendata.aws/spherex-qr</guid>
      <description>The Spectro-Photometer for the History of the Universe, Epoch of Reionization, and Ices Explorer (SPHEREx) is a NASA Astrophysics Medium-class Explorer (MIDEX) mission launched in March 2025. During its planned two-year mission, SPHEREx will perform the first ever all-sky spectral survey in the optical to near-infrared (0.75-5 microns). SPHEREx data will be used to probe inflation and the early universe, trace the history of galactic light production, and investigate the origin of planetary systems and biogenic ices, in addition to contributing to many other astrophysics research topics. IRSA began releasing SPHEREx QR2 data on a weekly basis in October 2025. QR2 features substantially improved calibrations and supersedes QR1.</description>
    </item>
    <item>
      <title>Safecast</title>
      <link>https://registry.opendata.aws/safecast</link>
      <guid>https://registry.opendata.aws/safecast</guid>
      <description>An ongoing collection of radiation and air quality measurements taken by devices involved in the Safecast project.</description>
    </item>
    <item>
      <title>Seattle Alzheimer&#x27;s Disease Brain Cell Atlas (SEA-AD)</title>
      <link>https://registry.opendata.aws/allen-sea-ad-atlas</link>
      <guid>https://registry.opendata.aws/allen-sea-ad-atlas</guid>
      <description>The Seattle Alzheimer&amp;#39;s Disease Brain Cell Atlas (SEA-AD) consortium strives to gain a deep molecular and cellular understanding of the early pathogenesis of Alzheimer&amp;#39;s disease and is funded by the National Institutes on Aging (NIA U19AG060909). The SEA-AD datasets available here comprise single cell profiling (transcriptomics and epigenomics) and quantitative neuropathology. To explore gene expression and chromatin accessibility information, the single-cell profiling data includes: snRNAseq and snATAC-seq data from the SEA-AD donor cohort (aged brains which span the spectrum of Alzheimer&amp;#39;s Disease pathology) and neurotypical reference brains. To explore key pathological proteins and cell types of interest to Alzheimer&amp;#39;s disease, the neuropathology data includes: full resolution brightfield images, images processed and segmented in HALO image analysis software, image annotations, and quantification summary files for the relevant stains including Abeta (6E10), IBA1, a-Synuclein, GFAP, H&amp;amp;E-LFB, NeuN, pTau(AT8), and pTDP43.</description>
    </item>
    <item>
      <title>Sentinel-1 SLC dataset for Germany</title>
      <link>https://registry.opendata.aws/sentinel1-slc</link>
      <guid>https://registry.opendata.aws/sentinel1-slc</guid>
      <description>The Sentinel1 Single Look Complex (SLC) unzipped dataset contains Synthetic Aperture Radar (SAR) data from the European Space Agency’s Sentinel-1 mission. Different from the zipped data provided by ESA, this dataset allows direct access to individual swaths required for a given study area, thus drastically minimizing the storage and downloading time requirements of a project. Since the data is stored on S3, users can utilize the boto3 library and s3 get_object method to read the entire content of the object into the memory for processing, without actually having to download it. The Sentinel-1 constellation consists of two satellites equipped with SAR sensors and a combined revisit time of six days. SAR imagery gets recorded regardless of weather conditions and daylight, which makes it ideally suited for monitoring land-use changes, surface deformations, land applications, oil spills, sea-ice, natural hazards, and for emergency response. In its current first stage, the dataset covers the entirety of Germany and is being updated continuously. As a next stage, the dataset will provide up-to-date coverage of the sentinel-1 SLC data over Europe.
This dataset is retrieved from Alaska Satellite Facility (ASF) and consists of all Sentinel1-SLC imagery from the beginning (2014) to present.</description>
    </item>
    <item>
      <title>Single-Cell Atlas of Human Blood During Healthy Aging</title>
      <link>https://registry.opendata.aws/singlecellhumanbloodatlas</link>
      <guid>https://registry.opendata.aws/singlecellhumanbloodatlas</guid>
      <description>Comprehensive, large-scale single-cell profiling of healthy human blood at different ages is one of the critical pending tasks required to establish a framework for systematic understanding of human aging. Here, using single-cell RNA/TCR/BCR-seq with protein feature barcoding (20 antibodies), we profiled 317 samples from 166 healthy individuals aged 25 to 85 years old drawn over 3-year period. Dataset spanning ~2 million cells describes 50 subpopulations of blood immune cells, with 14 subpopulations changing with age, including a novel NKG2C+ CD8 Tcm population that decreases with age. We describe age-associated accumulation of Th2 and HLA-DR+ memory CD4 T cells, CCR4+ CD8 Tcm cells and GZMK+ CD8 Tem cells. We validate key findings using 30-plex spectral cytometry panel. We characterize patterns of antigen receptor clonality across subpopulations of T and B cells and describe their age-dependence. Our work provides novel insights into healthy human aging and unique annotated resource of unprecedented depth.</description>
    </item>
    <item>
      <title>SpaceEye-T VVHR EO Open Data</title>
      <link>https://registry.opendata.aws/st-open-data</link>
      <guid>https://registry.opendata.aws/st-open-data</guid>
      <description>SpaceEye-T satellite collects the highest resolution optical imagery among the commercial satellites, 25 cm resolution. The Open Data features various satellite images around the world for end users to experience the power of VVHR optical data.</description>
    </item>
    <item>
      <title>Spitzer Enhanced Imaging Products (SEIP) Super Mosaics</title>
      <link>https://registry.opendata.aws/spitzer-seip</link>
      <guid>https://registry.opendata.aws/spitzer-seip</guid>
      <description>Spitzer was an infrared astronomy space telescope with imaging from 3 to 160 microns and spectroscopy from 5 to 37 microns, launched into an Earth-trailing solar orbit as the last of NASA&amp;#39;s Great Observatories. The SEIP Super Mosaics include data from the four channels of IRAC (3.6, 4.5, 5.8, 8 microns) and the 24 micron channel of MIPS. Data from multiple programs are combined where appropriate. Cryogenic Release v3.0 includes Spitzer data taken during commissioning and cryogenic operations, including calibration data.</description>
    </item>
    <item>
      <title>Sup3rCC</title>
      <link>https://registry.opendata.aws/nrel-pds-sup3rcc</link>
      <guid>https://registry.opendata.aws/nrel-pds-sup3rcc</guid>
      <description>Released to the public as part of the Department of Energy&amp;#39;s Open Energy Data Initiative, 
these data represent a serially complete collection of hourly 4km wind, solar, temperature, 
humidity, and pressure fields for the Continental United States under climate change scenarios.Sup3rCC is downscaled Global Climate Model (GCM) data. For example, the initial file set tagged
&amp;quot;sup3rcc_conus_mriesm20_ssp585_r1i1p1f1&amp;quot; is downscaled from MRI ESM 2.0 for climate change 
scenario SSP5 8.5 and variant label r1i1p1f1. The downscaling process is performed using a 
generative machine learning approach called sup3r: Super-Resolution for Renewable Energy 
Resource Data. The data includes both historical and future weather years, although the 
historical years represent the historical average climate, not true historical weather. The Sup3rCC data is intended to help researchers study the impact of climate change on energy 
systems with high levels of wind and solar power generation. Please note that all climate change 
data is only a representation of the &lt;em&gt;possible&lt;/em&gt; future climate and contains significant 
uncertainty. Analysis of multiple climate change scenarios and multiple climate models can help 
quantify this uncertainty.</description>
    </item>
    <item>
      <title>Swiss Public Transport Stops</title>
      <link>https://registry.opendata.aws/schweizer-haltestellen-oev</link>
      <guid>https://registry.opendata.aws/schweizer-haltestellen-oev</guid>
      <description>The basic geo-data set for public transport stops comprises public transport stops in Switzerland and additional selected geo-referenced public transport locations that are of operational or structural importance (operating points).</description>
    </item>
    <item>
      <title>Synthea Coherent Data Set</title>
      <link>https://registry.opendata.aws/synthea-coherent-data</link>
      <guid>https://registry.opendata.aws/synthea-coherent-data</guid>
      <description>This is a synthetic data set that includes FHIR resources, DICOM images, genomic data, physiological data (i.e., ECGs), and simple clinical notes. FHIR links all the data types together.</description>
    </item>
    <item>
      <title>Tabula Muris</title>
      <link>https://registry.opendata.aws/tabula-muris</link>
      <guid>https://registry.opendata.aws/tabula-muris</guid>
      <description>Tabula Muris is a compendium of single cell transcriptomic data from the model organism &lt;em&gt;Mus musculus&lt;/em&gt; comprising more than 100,000 cells from 20 organs and tissues. These data represent a new resource for cell biology, reveal gene expression in poorly characterized cell populations, and allow for direct and controlled comparison of gene expression in cell types shared between tissues, such as T-lymphocytes and endothelial cells from different anatomical locations. Two distinct technical approaches were used for most organs: one approach, microfluidic droplet-based 3’-end counting, enabled the survey of thousands of cells at relatively low coverage, while the other, FACS-based full length transcript analysis, enabled characterization of cell types with high sensitivity and coverage. The cumulative data provide the foundation for an atlas of transcriptomic cell biology. See: &lt;a href&#x3D;&quot;https://www.nature.com/articles/s41586-018-0590-4&quot;&gt;https://www.nature.com/articles/s41586-018-0590-4&lt;/a&gt;</description>
    </item>
    <item>
      <title>Tabula Muris Senis</title>
      <link>https://registry.opendata.aws/tabula-muris-senis</link>
      <guid>https://registry.opendata.aws/tabula-muris-senis</guid>
      <description>Tabula Muris Senis is a comprehensive compendium of single cell transcriptomic data from the model organism &lt;em&gt;Mus musculus&lt;/em&gt; comprising more than 500,000 cells from 18 organs and tissues across the mouse lifespan. We discovered cell-specific changes occurring across multiple cell types and organs, as well as age related changes in the cellular composition of different organs. Using single-cell transcriptomic data we were able to assess cell type specific manifestations of different hallmarks of aging, such as senescence, changes in the activity of metabolic pathways, depletion of stem-cell populations, genomic instability and the role of inflammation as well as other changes in the organism’s immune system. Tabula Muris Senis provides a wealth of new molecular information about how the most significant hallmarks of aging are reflected in a broad range of tissues and cell types.See: &lt;a href&#x3D;&quot;https://www.biorxiv.org/content/10.1101/661728v1&quot;&gt;https://www.biorxiv.org/content/10.1101/661728v1&lt;/a&gt;</description>
    </item>
    <item>
      <title>The JWST Advanced Extragalactic Survey JADES</title>
      <link>https://registry.opendata.aws/mast-jades</link>
      <guid>https://registry.opendata.aws/mast-jades</guid>
      <description>JADES is an infrared imaging and multi-object spectroscopy survey focused on two deep fields: the Hubble Deep Field (GOODS-N) 
and Hubble Ultra Deep Field (GOODS-S). JADES conducted NIRCam imaging in 8-10 bands, covering about 42 square arcminutes to very 
deep limits (fainter than 30th magnitude) with an average of about 100 hours of total exposure time, and then another 167 square arcminutes
to a typical exposure time of 25 hrs. Coordinated parallels with the MIRI instrument extend this imaging further into the infrared in smaller regions.
JADES then performed extensive NIRSpec spectroscopy with over 5000 targets on 31 separate pointings, including two deep exposures of
55 hrs spread across 5 dispersers. The JADES team added additional imaging and spectroscopy in Cycles 1, 2, and 3 from a number of 
affiliated guest observer programs.</description>
    </item>
    <item>
      <title>U.S. Census ACS PUMS</title>
      <link>https://registry.opendata.aws/census-dataworld-pums</link>
      <guid>https://registry.opendata.aws/census-dataworld-pums</guid>
      <description>U.S. Census Bureau American Community Survey (ACS) Public Use Microdata Sample (PUMS) available in a linked data format using the Resource Description Framework (RDF) data model.</description>
    </item>
    <item>
      <title>UCSF Primary Central Nervous System Lymphoma MRI Dataset</title>
      <link>https://registry.opendata.aws/ucsf-pcnsl</link>
      <guid>https://registry.opendata.aws/ucsf-pcnsl</guid>
      <description>This BIDS-formatted dataset provides multimodal brain MRI data from 150 patients with primary central nervous system lymphoma (PCNSL), including T1-weighted, contrast-enhanced T1-weighted, FLAIR, and ADC sequences. The dataset includes expert-annotated lesion segmentations with radiomic features, along with anonymized clinical data including demographics, diagnosis history, and medications.</description>
    </item>
    <item>
      <title>UK Biobank Pharma Proteomics Project (UKB-PPP)</title>
      <link>https://registry.opendata.aws/ukbppp</link>
      <guid>https://registry.opendata.aws/ukbppp</guid>
      <description>The UKB-PPP is a collaboration between the UK Biobank (UKB) and thirteen biopharmaceutical companies characterising the plasma proteomic profiles of 54,219 UKB participants. As part of a collaborative analysis across the thirteen UKB-PPP partners, we conducted comprehensive protein quantitative trait loci (pQTL) mapping of 2,923 proteins that identifies 14,287 primary genetic associations, of which 85% are newly discovered, in addition to ancestry-specific pQTL mapping in non-Europeans. We identify independent secondary associations in 87% of cis and 30% of trans loci, expanding the catalogue of genetic instruments for downstream analyses.</description>
    </item>
    <item>
      <title>Unblurred Coadds of the Wide-field Infrared Survey Explorer (unWISE)</title>
      <link>https://registry.opendata.aws/wise-unwise</link>
      <guid>https://registry.opendata.aws/wise-unwise</guid>
      <description>unWISE is a reprocessing of Wide-field Infrared Survey Explorer (WISE) data which preserves the native angular resolution and is optimized for forced photometry. WISE was a NASA satellite producing all-sky imaging in four infrared bands centered at 3.4, 4.6, 12 and 22 microns (W1, W2, W3, and W4) starting in 2010 until the coolant was exhausted in 2011. It was reactivated in 2013 as NEOWISE and continued imaging in W1 and W2 until 2024.</description>
    </item>
    <item>
      <title>Virtual Shizuoka, 3D Point Cloud Data</title>
      <link>https://registry.opendata.aws/virtual_shizuoka</link>
      <guid>https://registry.opendata.aws/virtual_shizuoka</guid>
      <description>This dataset comprises high-precision 3D point cloud data that encompasses the entire Shizuoka prefecture in Japan, covering 7,200 out of its 7,777 square kilometers. The data is produced through aerial laser survey, airborne laser bathymetry and mobile mapping systems, the culmination of many years of dedicated effort.This data will be visualized and analyzed for use in infrastructure maintenance, disaster prevention measures and autonomous vehicle driving.</description>
    </item>
    <item>
      <title>VitalDB</title>
      <link>https://registry.opendata.aws/vitaldb</link>
      <guid>https://registry.opendata.aws/vitaldb</guid>
      <description>VitalDB, a high-fidelity multi-parameter vital signs database in surgical patients.</description>
    </item>
    <item>
      <title>Voices Obscured in Complex Environmental Settings (VOiCES)</title>
      <link>https://registry.opendata.aws/lab41-sri-voices</link>
      <guid>https://registry.opendata.aws/lab41-sri-voices</guid>
      <description>VOiCES is a speech corpus recorded in acoustically challenging settings,
using distant microphone recording. Speech was recorded in real rooms with various
acoustic features (reverb, echo, HVAC systems, outside noise, etc.). Adversarial noise,
either television, music, or babble, was concurrently played with clean speech.
Data was recorded using multiple microphones strategically placed
throughout the room. The corpus includes audio recordings, orthographic transcriptions,
and speaker labels.</description>
    </item>
    <item>
      <title>World Bank Climate Change Knowledge Portal (CCKP)</title>
      <link>https://registry.opendata.aws/wbg-cckp</link>
      <guid>https://registry.opendata.aws/wbg-cckp</guid>
      <description>CCKP provides open access to a comprehensive suite of climate and climate change resources derived from the latest generation of climate data archives. Products are based on a consistent and transparent approach with a systematic way of pre-processing the raw observed and model-based projection data to enable inter-comparable use across a broad range of applications. Climate products consist of basic climate variables as well as a large collection (70+) of more specialized, application-orientated variables and indices across different scenarios. Precomputed data can be extracted per specified variables, select timeframes, climate projection scenarios, across ensembles or individual models, etc. CCKP adheres to data distributions standards defined under the Coupled Model Intercomparison Project (CMIP) and its contributions to the Intergovernmental Panel on Climate Change (IPCC) Assessment Reports and latest scientific methodologies identified by the World Meteorological Organization and climate science community. Climate products are available for the following collections. Downscaled CMIP6 global 0.25-degree – 1950-2100; ERA5 global 0.25-degree – 1950-2022; CRU global 0.50-degree – 1901-2022; Population global 0.25-degree – 1995-2100 (GPW v4).</description>
    </item>
    <item>
      <title>Xiph.Org Test Media</title>
      <link>https://registry.opendata.aws/xiph-media</link>
      <guid>https://registry.opendata.aws/xiph-media</guid>
      <description>Uncompressed video used for video compression and video processing research.</description>
    </item>
    <item>
      <title>ZINC Database</title>
      <link>https://registry.opendata.aws/zinc15</link>
      <guid>https://registry.opendata.aws/zinc15</guid>
      <description>3D models for molecular docking screens.</description>
    </item>
    <item>
      <title>iHART Whole Genome Sequencing Data Set</title>
      <link>https://registry.opendata.aws/ihart</link>
      <guid>https://registry.opendata.aws/ihart</guid>
      <description>iHART is the &lt;a href&#x3D;&quot;http://www.thehartwellfoundation.org/&quot;&gt;Hartwell Foundation&lt;/a&gt;’s Autism Research and Technology Initiative. This release contains whole genome data from over 1000 families with 2 or more children with autism, of which biomaterials were provided by the Autism Genetic Resource Exchange (&lt;a href&#x3D;&quot;http://research.agre.org/&quot;&gt;AGRE&lt;/a&gt;).</description>
    </item>
    <item>
      <title>recount3</title>
      <link>https://registry.opendata.aws/recount</link>
      <guid>https://registry.opendata.aws/recount</guid>
      <description>recount3 is an online resource consisting of RNA-seq gene, exon, and exon-exon junction counts as well as coverage bigWig files for 8,679 and 10,088 different studies for human and mouse respectively. It is the third generation of the ReCount project and part of recount.bio. recount2 is also included for historical purposes. The pipeline used to generate the data in recount3 (but not recount2) is available &lt;a href&#x3D;&quot;https://github.com/langmead-lab/monorail-external&quot;&gt;here&lt;/a&gt;.</description>
    </item>
    <item>
      <title>(EXPERIMENTAL) NOAA FourCastNet Global Forecast System (FourCastNetGFS) (EXPERIMENTAL)</title>
      <link>https://registry.opendata.aws/noaa-nws-fourcastnetgfs</link>
      <guid>https://registry.opendata.aws/noaa-nws-fourcastnetgfs</guid>
      <description>The FourCastNet Global Forecast System (FourCastNetGFS) is an experimental system set up by the National Centers for Environmental Prediction (NCEP) to produce medium range global forecasts. The model runs on a 0.25 degree latitude-longitude grid (about 28 km) and 13 pressure levels. The model produces forecasts 4 times a day at 00Z, 06Z, 12Z and 18Z cycles. Major atmospheric and surface fields including temperature, wind components, geopotential height, relative humidity and 2 meter temperature and 10 meter winds are available. The products are 6 hourly forecasts up to 10 days. The data format is GRIB2.
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&lt;br/&gt;
The FourCastNetGFS system is an experimental weather forecast model built upon the pre-trained Nvidia’s FourCastNet Machine Learning Weather Prediction (MLWP) model version 2. The FourCastNet (Bonev et al, 2023) was developed by Nvidia using Adaptive Fourier Neural Operators. It uses a Fourier transform-based token-mixing scheme with the vision transformer architecture. This model is pre-trained with ECMWF’s ERA5 reanalysis data. The FourCastNetGFS takes one model state as initial condition from NCEP 0.25 degree GDAS analysis data and runs FourCastNet with weights from the pretrained FourCastNet by Nvidia. Unit conversion to the GDAS data is conducted to match the input data required by FourCastNet and to generate forecast products consistent to GFS.
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&lt;br/&gt;
The input data generated from the GDAS data as FourCastNet input is provided under the forecast data directory. Example of file names is:
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&lt;br/&gt;
input_2024022000.npy
&lt;br/&gt;
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There are 40 files under each directory covering a 10 day forecast. An example of file name is listed below
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&lt;br/&gt;
fcngfs.t00z.pgrb2.0p25.f006
&lt;br/&gt;
&lt;br/&gt;
Please note that this NOAA GFS machine learning Model was produced using a code package released by ECMWF’s ai_models_fourcastnetv2 plugin. For information on ai_models_fourcastnetv2 plugin, please visit their github page listed in the documentation and license sections of this page.</description>
    </item>
    <item>
      <title>2020 Redistricting Data File Least Squares Estimates</title>
      <link>https://registry.opendata.aws/census-2020-pl94-gls</link>
      <guid>https://registry.opendata.aws/census-2020-pl94-gls</guid>
      <description>The 2020 Redistricting Data File Least Squares Estimates data product provides count estimates, and their standard deviations, for each tabulation that was published as part of the persons universe of the 2020 Redistricting Data File for the US, state, county, and tract geographic levels. These estimates are computed using the generalized least squares (GLS) estimator using as input the publicly available 2020 Census persons universe noisy measurement files for both &lt;a href&#x3D;&quot;https://registry.opendata.aws/census-2020-pl94-nmf/&quot;&gt;the Redistricting Data File&lt;/a&gt; and &lt;a href&#x3D;&quot;https://registry.opendata.aws/census-2020-dhc-nmf/&quot;&gt;the Demographic and Housing Characteristics File&lt;/a&gt;. The algorithm used to compute this estimate is described in more detail in &lt;a href&#x3D;&quot;https://arxiv.org/abs/2404.13164&quot;&gt;Least Squares Estimation For Hierarchical Data&lt;/a&gt;. As described in more detail in this paper and the README below, the primary goal of this data product is to provide the data required to compute confidence intervals for the 2020 Census Redistricting Data File published counts that account for the uncertainty in these published counts due to the disclosure avoidance methods applied to 2020 Census tabulations. In other words, these confidence intervals do not account for other sources of error, such as those due to enumeration errors.
&lt;br/&gt;
&lt;br/&gt;</description>
    </item>
    <item>
      <title>A Realistic Cyber Defense Dataset (CSE-CIC-IDS2018)</title>
      <link>https://registry.opendata.aws/cse-cic-ids2018</link>
      <guid>https://registry.opendata.aws/cse-cic-ids2018</guid>
      <description>This dataset is the result of a collaborative project between the Communications Security Establishment (CSE) and The Canadian Institute for Cybersecurity (CIC) that use the notion of profiles to generate cybersecurity dataset in a systematic manner. It incluides a detailed description of intrusions along with abstract distribution models for applications, protocols, or lower level network entities. The dataset includes seven different attack scenarios, namely Brute-force, Heartbleed, Botnet, DoS, DDoS, Web attacks, and infiltration of the network from inside. The attacking infrastructure includes 50 machines and the victim organization has 5 departments includes 420 PCs and 30 servers. This dataset includes the network traffic and log files of each machine from the victim side, along with 80 network traffic features extracted from captured traffic using CICFlowMeter-V3.
For more information on the creation of this dataset, see this paper by researchers at the Canadian Institute for Cybersecurity (CIC) and the University of New Brunswick (UNB): &lt;a href&#x3D;&quot;http://www.scitepress.org/Papers/2018/66398/66398.pdf&quot;&gt;Toward Generating a New Intrusion Detection Dataset and Intrusion Traffic Characterization&lt;/a&gt;.</description>
    </item>
    <item>
      <title>AI2 TabMCQ: Multiple Choice Questions aligned with the Aristo Tablestore</title>
      <link>https://registry.opendata.aws/allenai-tablestore-questions</link>
      <guid>https://registry.opendata.aws/allenai-tablestore-questions</guid>
      <description>9092 crowd-sourced science questions and 68 tables of curated facts</description>
    </item>
    <item>
      <title>AI2 Tablestore (November 2015 Snapshot)</title>
      <link>https://registry.opendata.aws/allenai-tablestore</link>
      <guid>https://registry.opendata.aws/allenai-tablestore</guid>
      <description>68 tables of curated facts</description>
    </item>
    <item>
      <title>Aristo Mini Corpus</title>
      <link>https://registry.opendata.aws/allenai-aristo-mini</link>
      <guid>https://registry.opendata.aws/allenai-aristo-mini</guid>
      <description>1,197,377 science-relevant sentences</description>
    </item>
    <item>
      <title>Aristo Tuple KB</title>
      <link>https://registry.opendata.aws/allenai-tuple-kb</link>
      <guid>https://registry.opendata.aws/allenai-tuple-kb</guid>
      <description>294,000 science-relevant tuples</description>
    </item>
    <item>
      <title>Australasian Genomes</title>
      <link>https://registry.opendata.aws/australasian-genomics</link>
      <guid>https://registry.opendata.aws/australasian-genomics</guid>
      <description>Australasian Genomes is the genomic data repository for the Threatened Species Initiative (TSI) and the ARC Centre for Innovations in Peptide and Protein Science (CIPPS). This repository contains reference genomes, transcriptomes, resequenced genomes and reduced representation sequencing data from Australasian species. Australasian Genomes is managed by the Australasian Wildlife Genomics Group (AWGG) at the University of Sydney on behalf of our collaborators within TSI and CIPPS.</description>
    </item>
    <item>
      <title>Baby Open Brains (BOBs) Repository on AWS</title>
      <link>https://registry.opendata.aws/bobsrepository</link>
      <guid>https://registry.opendata.aws/bobsrepository</guid>
      <description>Manually curated and reviewed infant brain segmentations and accompanying T1w and T2w images for a range of 1-9 month old participants from the Baby Connectome Project (BCP)</description>
    </item>
    <item>
      <title>BioLiP</title>
      <link>https://registry.opendata.aws/biolip</link>
      <guid>https://registry.opendata.aws/biolip</guid>
      <description>BioLiP is a semi-manually curated database for high-quality, biologically relevant ligand-protein binding interactions. The structure data are collected primarily from the Protein Data Bank (PDB), with biological insights mined from literature and other specific databases. BioLiP aims to construct the most comprehensive and accurate database for serving the needs of ligand-protein docking, virtual ligand screening and protein function annotation.</description>
    </item>
    <item>
      <title>Brain Data Science Database 1</title>
      <link>https://registry.opendata.aws/bdsp_open_projects</link>
      <guid>https://registry.opendata.aws/bdsp_open_projects</guid>
      <description>This collection unifies multiple brain datasets spanning critical care, sleep medicine, cardiopulmonary health, infectious diseases, and other aspects of clinical neuroscience. It includes a variety of types of clinical neuroscience data including electroencephalography (EEG) and polysomnography (PSG) recordings, and supporting data to enable research in diverse areas of clinical neuroscience such as epilepsy, delirium, coma, and sleep medicine. All data is de-identified and includes code to reproduce results in accompanying research publications. The data is available for non-commercial research use and is open access.</description>
    </item>
    <item>
      <title>Brain Data Science Database 2</title>
      <link>https://registry.opendata.aws/bdsp_restricted_projects</link>
      <guid>https://registry.opendata.aws/bdsp_restricted_projects</guid>
      <description>This collection unifies multiple brain datasets spanning critical care, sleep medicine, cardiopulmonary health, infectious diseases, and other aspects of clinical neuroscience. It includes large-scale electroencephalography (EEG) and polysomnography (PSG) recordings, brain imaging data (MRI, CT, PET), and supporting data to enable research in diverse areas of clinical neuroscience such as epilepsy, delirium, coma, sleep depth, sleep-related breathing disorders, meditation, subarachnoid hemorrhage, cardiac arrest, neuroinfectious diseases, and audiology. All data is de-identified and includes algorithmic tools and reproducible code. Access requires signing a data use agreement that prohibits re-identification, requires data security, restricts sharing, limits use to non-commercial research, and mandates reporting any potentially identifying information.</description>
    </item>
    <item>
      <title>Brain Data Science Database 3</title>
      <link>https://registry.opendata.aws/bdsp_credentialed_projects</link>
      <guid>https://registry.opendata.aws/bdsp_credentialed_projects</guid>
      <description>This collection unifies multiple brain datasets spanning critical care, sleep medicine, cardiopulmonary health, infectious diseases, and other aspects of clinical neuroscience. It includes large-scale electroencephalography (EEG) and polysomnography (PSG) recordings, brain imaging data (MRI, CT, PET), and electronic health records (EHR) data supporting research in areas such as epilepsy, delirium, coma, sleep depth, sleep-related breathing disorders, burst suppression, meditation, subarachnoid hemorrhage, cardiac arrest, and neuroinfectious diseases. All data is de-identified and includes algorithmic tools and reproducible code. Access requires (1) submitting proof of CITI training certification (research ethics training for human subjects research - see &lt;a href&#x3D;&quot;https://bdsp.io/about/citi-course/&quot;&gt;https://bdsp.io/about/citi-course/&lt;/a&gt;); (2) signing a data use agreement that prohibits re-identification, requires data security, restricts sharing, limits use to non-commercial research, and mandates reporting any potentially identifying information.</description>
    </item>
    <item>
      <title>CAFE60 reanalysis</title>
      <link>https://registry.opendata.aws/csiro-cafe60</link>
      <guid>https://registry.opendata.aws/csiro-cafe60</guid>
      <description>The CSIRO Climate retrospective Analysis and Forecast Ensemble system: version 1 (CAFE60v1) provides a large ensemble retrospective analysis of the global climate system from 1960 to present with sufficiently many realizations and at spatio-temporal resolutions suitable to enable probabilistic climate studies. Using a variant of the ensemble Kalman filter, 96 climate state estimates are generated over the most recent six decades. These state estimates are constrained by monthly mean ocean, atmosphere and sea ice observations such that their trajectories track the observed state while enabling estimation of the uncertainties in the approximations to the retrospective mean climate over recent decades. Strongly coupled data assimilation (SCDA) is implemented via an ensemble transform Kalman filter in order to constrain a general circulation climate model to observations. Satellite (altimetry, sea surface temperature, sea ice concentration) and in situ ocean temperature and salinity profiles are directly assimilated each month, whereas atmospheric observations are sub-sampled from the JRA55 atmospheric reanalysis. Strong coupling is implemented via explicit cross domain covariances between ocean, atmosphere, sea ice and ocean biogeochemistry. Atmospheric and surface ocean fields are available at daily resolution and monthly resolution for the land, subsurface ocean and sea ice. The system also produces a complete data archive of initial conditions potentially enabling individual forecasts for all members each month over the 60 year period. The size of the ensemble and application of strongly coupled data assimilation lead to new insights for future reanalyses. CAFE60v1 has been validated in comparison to empirical indices of the major climate teleconnections and blocking from various reanalysis products (ERA5, JRA55, NCEP NR1). Estimates of the large scale ocean structure and transports have been compared to those derived from gridded observational products (WOA18, HadISST, ERSSTv5) and climate model projections (CMIP). Sea ice (extent, concentration and variability) and land surface (precipitation and surface air temperatures) are also compared to a variety of model (ERA5, CMIP) and observational (GPCP, AWAP, HadCRU4, GIOMAS, NSIDC, HadISST) products. This analysis shows that CAFE60v1 is a useful, comprehensive and unique data resource for studying internal climate variability and predictability, including the recent climate response to anthropogenic forcing on multi-year to decadal time scales.</description>
    </item>
    <item>
      <title>CCAFS-Climate Data</title>
      <link>https://registry.opendata.aws/cgiardata</link>
      <guid>https://registry.opendata.aws/cgiardata</guid>
      <description>High resolution climate data to help assess the impacts of climate change primarily on agriculture. These open access datasets of climate projections will help researchers make climate change impact assessments.</description>
    </item>
    <item>
      <title>COCO - Common Objects in Context - fast.ai datasets</title>
      <link>https://registry.opendata.aws/fast-ai-coco</link>
      <guid>https://registry.opendata.aws/fast-ai-coco</guid>
      <description>COCO is a large-scale object detection, segmentation, and captioning dataset.
This is part of the fast.ai datasets collection hosted by AWS for convenience
of fast.ai students. If you use this dataset in your research please cite
arXiv:1405.0312 [cs.CV].</description>
    </item>
    <item>
      <title>COVID-19 Molecular Structure and Therapeutics Hub</title>
      <link>https://registry.opendata.aws/molssi-covid19-hub</link>
      <guid>https://registry.opendata.aws/molssi-covid19-hub</guid>
      <description>Aggregating critical information to accelerate drug discovery for the molecular modeling and simulation community.
A community-driven data repository and curation service for molecular structures, models, therapeutics, and
simulations related to computational research related to therapeutic opportunities for COVID-19
(caused by the SARS-CoV-2 coronavirus).</description>
    </item>
    <item>
      <title>CRC-SAS/SISSA historical seasonal and subseasonal forecast database</title>
      <link>https://registry.opendata.aws/sissa-forecast-database-dataset</link>
      <guid>https://registry.opendata.aws/sissa-forecast-database-dataset</guid>
      <description>En el marco del Sistema de Información de Sequías del Sur de Sudamérica (SISSA) se ha desarrollado una base de predicciones en escala subestacional y estacional con datos corregidos y sin corregir, con el propósito que permita estudiar predictibilidad en distintas escalas y también que sirva para alimentar modelos de sectores como agricultura e hidrología. 
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La base contiene datos en escala diaria entre 2000-2019 (sin corregir) y 2010-2019 (corregidos) para diversas variables incluyendo: temperatura media, máxima y mínima, así como también lluvia, viento medio y otras variables pensadas para alimentar modelos hidrológicos y de cultivo.
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La base de datos abarca toda el área del Centro Regional del Clima para el sur de sudamérica (CRC-SAS), abarcando desde Bolivia y centro-sur de Brasil hasta la Patagonia incluyendo los países miembros como Chile, Argentina, Brasil, Paraguay, Uruguay y Bolivia.
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La base fue generada a partir de datos de GEFSv12 para escala subestacional (&lt;a href&#x3D;&quot;https://www.ncei.noaa.gov/products/weather-climate-models/global-ensemble-forecast&quot;&gt;GEFS&lt;/a&gt;) y CFS2 para escala estacional (&lt;a href&#x3D;&quot;https://www.ncei.noaa.gov/access/metadata/landing-page/bin/iso?id&#x3D;gov.noaa.ncdc:C00878&quot;&gt;CFS2&lt;/a&gt;). Para la generación de los datos corregidos se utilizaron los datos del reanálisis de ERA5 (&lt;a href&#x3D;&quot;https://cds.climate.copernicus.eu/cdsapp#!/dataset/reanalysis-era5-single-levels?tab&#x3D;overview&quot;&gt;ERA5&lt;/a&gt;).
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Within the framework of the Southern South American Drought Information System (SISSA), a base of sub-seasonal and seasonal scale predictions has been developed with corrected and uncorrected data, with the purpose of studying predictability at different scales and also to be used to feed models for sectors such as agriculture and hydrology.
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The database contains daily scale data between 2000-2019 (uncorrected) and 2010-2019 (corrected) for several variables including: mean, maximum and minimum temperature, as well as rainfall, mean wind and other variables intended to feed hydrological and crop models.
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The database covers the entire area of the Regional Climate Center for Southern South America (CRC-SAS), from Bolivia and south-central Brazil to Patagonia, including member countries such as Chile, Argentina, Brazil, Paraguay, Uruguay and Bolivia.
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The base was generated from GEFSv12 data for subseasonal scale (&lt;a href&#x3D;&quot;https://www.ncei.noaa.gov/products/weather-climate-models/global-ensemble-forecast&quot;&gt;GEFS&lt;/a&gt;) and CFS2 for seasonal scale (&lt;a href&#x3D;&quot;https://www.ncei.noaa.gov/access/metadata/landing-page/bin/iso?id&#x3D;gov.noaa.ncdc:C00878&quot;&gt;CFS2&lt;/a&gt;). Data from the ERA5 reanalysis (&lt;a href&#x3D;&quot;https://cds.climate.copernicus.eu/cdsapp#!/dataset/reanalysis-era5-single-levels?tab&#x3D;overview&quot;&gt;ERA5&lt;/a&gt;) were used to generate the corrected data.</description>
    </item>
    <item>
      <title>CarbonPDF</title>
      <link>https://registry.opendata.aws/carbonpdf</link>
      <guid>https://registry.opendata.aws/carbonpdf</guid>
      <description>A carbon question-answering (QA) dataset specifically designed to facilitate the extraction and analysis of data from real-world carbon reports of computing products. The dataset features annotated metadata, a variety of numerical reasoning tasks, and structured derivations to ensure accurate processing of fragmented and inconsistent information.</description>
    </item>
    <item>
      <title>CartoStore</title>
      <link>https://registry.opendata.aws/cartostore</link>
      <guid>https://registry.opendata.aws/cartostore</guid>
      <description>Cross-Platform Repository for High-resolution Spatial Transcriptomics Datasets.</description>
    </item>
    <item>
      <title>Central Weather Administration OpenData</title>
      <link>https://registry.opendata.aws/cwa_opendata</link>
      <guid>https://registry.opendata.aws/cwa_opendata</guid>
      <description>Various kinds of weather raw data and charts from Central Weather Administration.</description>
    </item>
    <item>
      <title>Central Weather Bureau OpenData</title>
      <link>https://registry.opendata.aws/cwb_opendata</link>
      <guid>https://registry.opendata.aws/cwb_opendata</guid>
      <description>Various kinds of weather raw data and charts from Central Weather Bureau.</description>
    </item>
    <item>
      <title>Clinical Ultrasound Image Repository</title>
      <link>https://registry.opendata.aws/clinical-ultrasound-image-data</link>
      <guid>https://registry.opendata.aws/clinical-ultrasound-image-data</guid>
      <description>Generic Clinical Ultrasound Data from Random Subjects acquired for Clinical Reasons, to be used for Developing Artificial Intelligence Applications. This dataset is complete with 2000 studies from 2000 subjects (one third each from abdominal, cardiac, and OB/GYN cases)</description>
    </item>
    <item>
      <title>Cloud to Street - Microsoft Flood and Clouds Dataset</title>
      <link>https://registry.opendata.aws/c2smsfloods</link>
      <guid>https://registry.opendata.aws/c2smsfloods</guid>
      <description>This dataset consists of chips of Sentinel-1 and Sentinel-2 satellite data. Each Sentinel-1 chip contains a corresponding label for water and each Sentinel-2 chip contains a corresponding label for water and clouds. Data is stored in folders by a unique event identifier as the folder name. Within each event folder there are subfolders for Sentinel-1 (s1) and Sentinel-2 (s2) data. Each chip is contained in its own sub-folder with the folder name being the source image id, followed by a unique chip identifier consisting of a hyphenated set of 5 numbers. All bands of the satellite data, as well as the labels, and overview images are contained within the chip folder.</description>
    </item>
    <item>
      <title>Community Multiscale Air Quality (CMAQ) 2019 3D Gridded and Column data from the EPA&#x27;s Air Quality Time Series (EQUATES) Project</title>
      <link>https://registry.opendata.aws/epa-equates-v1</link>
      <guid>https://registry.opendata.aws/epa-equates-v1</guid>
      <description>The data are part of EPA’s Air Quality Time Series (EQUATES) Project.  The data consist of hourly gridded pollutant concentrations estimates by the Community Multiscale Air Quality (CMAQ) model version 5.3.2 (&lt;a href&#x3D;&quot;https://doi.org/10.15139/S3/F2KJSK&quot;&gt;https://doi.org/10.15139/S3/F2KJSK&lt;/a&gt;) for January 1 – December 31, 2019.  Model data is provided for two spatial domains :  the Northern Hemisphere (108 km x 108km horizontal grid spacing) and the Contiguous United States including parts of Canada and Mexico (12km x 12km horizontal grid spacing).  Two types of hourly data are provided: three-dimensional air pollutant concentrations and vertical column pollutant totals. Previous studies have used this type of CMAQ 3D and vertical column air quality data to evaluate the modeling system, created model-observed ‘fused’ surfaces, and to analyze spatial and temporal changes in air quality in the upper atmosphere, e.g., &lt;a href&#x3D;&quot;https://doi.org/10.1016/j.envint.2019.104909&quot;&gt;https://doi.org/10.1016/j.envint.2019.104909&lt;/a&gt;; &lt;a href&#x3D;&quot;https://doi.org/10.5194/acp-17-12449-2017&quot;&gt;https://doi.org/10.5194/acp-17-12449-2017&lt;/a&gt;; &lt;a href&#x3D;&quot;https://doi.org/10.1029/2006JD008085&quot;&gt;https://doi.org/10.1029/2006JD008085&lt;/a&gt;; &lt;a href&#x3D;&quot;https://doi.org/10.5194/acp-15-9997-2015&quot;&gt;https://doi.org/10.5194/acp-15-9997-2015&lt;/a&gt;.</description>
    </item>
    <item>
      <title>DARPA Invisible Headlights Dataset</title>
      <link>https://registry.opendata.aws/darpa-invisible-headlights</link>
      <guid>https://registry.opendata.aws/darpa-invisible-headlights</guid>
      <description>&amp;quot;The DARPA Invisible Headlights Dataset is a large-scale multi-sensor dataset annotated for autonomous, off-road navigation in challenging off-road environments. It features simultaneously collected off-road imagery from multispectral, hyperspectral, polarimetric, and broadband sensors spanning wave-lengths from the visible spectrum to long-wave infrared and provides aligned LIDAR data for ground-truth shape. Camera calibrations, LiDAR registrations, and traversability annotations for a subset of the data are available.&amp;quot;</description>
    </item>
    <item>
      <title>DHARANI Developing Human-Brain Atlas</title>
      <link>https://registry.opendata.aws/dharani-brain-dataset</link>
      <guid>https://registry.opendata.aws/dharani-brain-dataset</guid>
      <description>We introduce DHARANI, the first online platform with three-dimensional (3D) histological reconstructions of the developing human brain from 14 to 24 gestational weeks (GW) across the five fetal brains. DHARANI features 5132 Nissl, hematoxylin and eosin stained, 20 µm coronal and sagittal sections, postmortem MRI, and a neuroanatomical atlas with 466 annotated sections covering ∼500 brain structures. It is accessible online at &lt;a href&#x3D;&quot;https://brainportal.humanbrain.in/publicview/index.html&quot;&gt;https://brainportal.humanbrain.in/publicview/index.html&lt;/a&gt;. The 3D reconstruction enables a volumetric view of the fetal brain, allowing visualization in all three planes akin to MRI, previously unachievable with histological datasets from the fetal brain. This allowed qualitative assessment of the growth of brain regions and layers throughout the second trimester. “DHARANI” documents the initiation of sulci, with the lateral fissure, calcarine, parieto-occipital, and cingulate sulci, at 14 GW. The central and postcentral sulci appear by 24 GW; however, cytoarchitectonic boundaries become visible before sulcal patterns. Cortical plate (CP) lamination begins at 24 GW in the parietal and occipital cortices. The frontal cortex lacks lamination at 24 GW, although putative Betz cells are already visible and show early patterning in the intermediate zone. The cell-sparse layer between the CP and subplate, containing late migratory neurons, begins in the orbital cortex at 14 GW and reaches the frontal cortex by 17 GW. The appearance of the honeycomb pattern in the occipital and parietal cortex occurs after 14 GW. Additionally, we describe the development of the thalamic pregeniculate with the rotation of the lateral geniculate nucleus. Cerebellar nuclei and an early Purkinje cell layer appear by 21 GW in the already foliated cerebellar cortex. The collection of &amp;gt; 650,000 images have been made available in this Open Data bucket to enable efficient access and analysis of the this dataset.</description>
    </item>
    <item>
      <title>Department of Energy&#x27;s Marine Energy Data Lake</title>
      <link>https://registry.opendata.aws/marine-energy-data</link>
      <guid>https://registry.opendata.aws/marine-energy-data</guid>
      <description>Data released from projects funded by the Department of Energy&amp;#39;s Water Power Technologies Office (DOE WPTO) 
that are too large or complex to be conveniently accessed by traditional means. The Marine Energy data lake 
aims to improve and automate access of high-value MHK data sets, making data actionable and discoverable by 
researchers and industry to accelerate analysis and advance innovation. 
This data lake is a sister-data lake to the Department of Energy’s Open Energy Data Initiative (OEDI) data lake. </description>
    </item>
    <item>
      <title>District of Columbia - Classified Point Cloud LiDAR</title>
      <link>https://registry.opendata.aws/dc-lidar</link>
      <guid>https://registry.opendata.aws/dc-lidar</guid>
      <description>LiDAR point cloud data for Washington, DC is available for anyone to use on Amazon S3.
This dataset, managed by the Office of the Chief Technology Officer (OCTO), through the
direction of the District of Columbia GIS program, contains tiled point cloud data for
the entire District along with associated metadata.</description>
    </item>
    <item>
      <title>ENHANCE.PET 1.6k - Whole-/Total-Body [18F]FDG-PET/CT with CT-Derived Segmentations</title>
      <link>https://registry.opendata.aws/enhance-pet-1-6k</link>
      <guid>https://registry.opendata.aws/enhance-pet-1-6k</guid>
      <description>Open, multi-center dataset of 1,597 whole-/total-body FDG-PET/CT studies with 130 CT-derived, expert-verified anatomical segmentations per scan (~250 GB). Provided as anonymized NIfTI (PET, CT, labels) with spreadsheet metadata. Designed for segmentation benchmarking, multi-organ analysis, radiomics, and PET/CT AI research.</description>
    </item>
    <item>
      <title>EPA Dynamically Downscaled Ensemble (EDDE) Version 1</title>
      <link>https://registry.opendata.aws/epa-edde-v1</link>
      <guid>https://registry.opendata.aws/epa-edde-v1</guid>
      <description>The data are a subset of the EPA Dynamically Downscaled Ensemble (EDDE),  Version 1. EDDE is a collection of physics-based modeled data that represent 3D atmospheric conditions for historical and future periods under different scenarios. The EDDE Version 1 datasets cover the contiguous United States at a horizontal grid spacing of 36 kilometers at hourly increments. EDDE Version 1 includes simulations that have been dynamically downscaled from multiple global climate models (GCMs) under both mid- and high-emission scenarios from the Fifth Coupled Model Intercomparison Project (CMIP5) using the Weather Research and Forecasting (WRF) model. Scenarios were downscaled from the Community Earth System Model (CESM) and the Geophysical Fluid Dynamics Laboratory (GFDL) Coupled Model version 3 (CM3). Simulations followed the historical periods 1975-2005 (CESM only) and 1995-2005 (both CESM and CM3), and Representative Concentration Pathways (RCP) 4.5 for 2025-2100 (CESM only), RCP6.0 for 2025-2055 (CESM only), and RCP8.5 (both CESM and CM3). Data are in Network Common Data Form (netCDF) version 4, which is used in atmospheric modeling. The EDDE data in netCDF are further written to adhere to principles of Climate and Forecasting System (CF) Compliance to enhance portability and interoperability with data from other sources. The files are self-describing with metadata included in the netCDF header. Data reference: &lt;a href&#x3D;&quot;https://doi.org/10.23719/1530964&quot;&gt;https://doi.org/10.23719/1530964&lt;/a&gt; Some peer-reviewed publications that describe EDDE (without the name &amp;quot;EDDE&amp;quot;): &lt;a href&#x3D;&quot;https://doi.org/10.1080/10962247.2021.1970048&quot;&gt;https://doi.org/10.1080/10962247.2021.1970048&lt;/a&gt; &lt;a href&#x3D;&quot;https://doi.org/10.5194/acp-18-15471-2018&quot;&gt;https://doi.org/10.5194/acp-18-15471-2018&lt;/a&gt; &lt;a href&#x3D;&quot;https://doi.org/10.1080/10962247.2014.996270&quot;&gt;https://doi.org/10.1080/10962247.2014.996270&lt;/a&gt; &lt;a href&#x3D;&quot;https://doi.org/10.1175/JCLI-D-15-0233.1&quot;&gt;https://doi.org/10.1175/JCLI-D-15-0233.1&lt;/a&gt; &lt;a href&#x3D;&quot;https://doi.org/10.1002/2014JD021785&quot;&gt;https://doi.org/10.1002/2014JD021785&lt;/a&gt;</description>
    </item>
    <item>
      <title>EPA Dynamically Downscaled Ensemble (EDDE) Version 2</title>
      <link>https://registry.opendata.aws/epa-edde-v2</link>
      <guid>https://registry.opendata.aws/epa-edde-v2</guid>
      <description>The data are a subset of the EPA Dynamically Downscaled Ensemble (EDDE),  Version 2. EDDE is a collection of physics-based modeled data that represent 3D atmospheric conditions for historical and future periods under different scenarios. The EDDE Version 2 datasets cover the contiguous United States at a horizontal grid spacing of 12 kilometers at hourly increments. EDDE Version 2 will include simulations that have been dynamically downscaled from multiple global climate models (GCMs) under multiple emission scenarios from the Sixth Coupled Model Intercomparison Project (CMIP6) using the Weather Research and Forecasting (WRF) model. Scenarios were downscaled from the  Max Planck Institute (MPI) Earth System Model (ESM) version 1.2 High Resolution  (MPI-ESM1-2-HR), with plans to expand into additional GCMs in the future.  Simulations cover the historical period 1985-2014 and a future period of  2025-2100 under Shared Socioeconomic Pathway (SSP) 3-7.0. Data are in Network Common Data Form (netCDF) version 4, which is used in atmospheric modeling. The EDDE data in netCDF are further written to adhere to principles of Climate and Forecasting System (CF) Compliance to enhance portability and interoperability with data from other sources. The files are self-describing with metadata included in the netCDF header. Data reference: &lt;a href&#x3D;&quot;https://doi.org/10.23719/1531941&quot;&gt;https://doi.org/10.23719/1531941&lt;/a&gt; Some peer-reviewed publications that describe EDDE (without the name &amp;quot;EDDE&amp;quot;): &lt;a href&#x3D;&quot;https://doi.org/10.1080/10962247.2021.1970048&quot;&gt;https://doi.org/10.1080/10962247.2021.1970048&lt;/a&gt; &lt;a href&#x3D;&quot;https://doi.org/10.5194/acp-18-15471-2018&quot;&gt;https://doi.org/10.5194/acp-18-15471-2018&lt;/a&gt; &lt;a href&#x3D;&quot;https://doi.org/10.1080/10962247.2014.996270&quot;&gt;https://doi.org/10.1080/10962247.2014.996270&lt;/a&gt; &lt;a href&#x3D;&quot;https://doi.org/10.1175/JCLI-D-15-0233.1&quot;&gt;https://doi.org/10.1175/JCLI-D-15-0233.1&lt;/a&gt; &lt;a href&#x3D;&quot;https://doi.org/10.1002/2014JD021785&quot;&gt;https://doi.org/10.1002/2014JD021785&lt;/a&gt;</description>
    </item>
    <item>
      <title>EPA Hourly Prognostic Meteorological Data </title>
      <link>https://registry.opendata.aws/epa-hourly-prognostic-meteorology</link>
      <guid>https://registry.opendata.aws/epa-hourly-prognostic-meteorology</guid>
      <description>The data are hourly outputs from the Weather Research and Forecasting (WRF) model generated by the EPA&amp;#39;s Office of State Air Partnerships (OSAP), Air Quality Assessment Division, Air Quality Modeling Branch. These data were generated at a 12-km resolution over the Continental United States (12US), beginning for the year 2021 and continuing annually through 2023. These files are intended for use in a broad range of  air quality applications, but specifically may be used in dispersion modeling applications that would benefit from the use of the Mesoscale Model Interface (MMIF) tool  (&lt;a href&#x3D;&quot;https://www.epa.gov/scram/air-quality-dispersion-modeling-related-model-support-programs#mmif&quot;&gt;https://www.epa.gov/scram/air-quality-dispersion-modeling-related-model-support-programs#mmif&lt;/a&gt;) which translates prognostic meteorological data into formats suitable for use with AERMOD, CALPUFF, or SCICHEM. The individual files are less than 1GB in size, which allows for the use of the MMIF tool in a Windows environment. These data are anticipated to be updated annually so the 3 most-recent years are available for use. Additionally, model-observation paired files are included to aid in the performance evaluation that is necessary for use of these data in regulatory applications per Appendix W to 40 CFR Part 51. </description>
    </item>
    <item>
      <title>EPA Risk-Screening Environmental Indicators</title>
      <link>https://registry.opendata.aws/epa-rsei-pds</link>
      <guid>https://registry.opendata.aws/epa-rsei-pds</guid>
      <description>Detailed air model results from EPA’s Risk-Screening Environmental Indicators (RSEI) model.</description>
    </item>
    <item>
      <title>Epoch of Reionization Dataset</title>
      <link>https://registry.opendata.aws/epoch-of-reionization</link>
      <guid>https://registry.opendata.aws/epoch-of-reionization</guid>
      <description>The data are from observations with the Murchison Widefield Array (MWA) which is a
Square Kilometer Array (SKA) precursor in Western Australia.  This particular
dataset is from the Epoch of Reionization project which is a key science driver
of the SKA. Nearly 2PB of such observations have been recorded to date, this is
a small subset of that which has been exported from the MWA data archive in
Perth and made available to the public on AWS.  The data were taken to detect
signatures of the first stars and galaxies forming and the effect of these early
stars and galaxies on the evolution of the universe.</description>
    </item>
    <item>
      <title>GATK Test Data</title>
      <link>https://registry.opendata.aws/gatk-test-data</link>
      <guid>https://registry.opendata.aws/gatk-test-data</guid>
      <description>The GATK test data resource bundle is a collection of files for resequencing human genomic data with the
Broad Institute&amp;#39;s &lt;a href&#x3D;&quot;https://software.broadinstitute.org/gatk/&quot;&gt;Genome Analysis Toolkit (GATK)&lt;/a&gt;.</description>
    </item>
    <item>
      <title>GLAD Landsat ARD</title>
      <link>https://registry.opendata.aws/glad-landsat-ard</link>
      <guid>https://registry.opendata.aws/glad-landsat-ard</guid>
      <description>The Landsat Analysis Ready Data (ARD) created by the Global Land Analysis and Discovery Lab (GLAD) at the University of Maryland serves as a spatially and temporally consistent input for land cover mapping and change detection at global to local scales. The GLAD ARD represents a 16-day time series of globally consistent, tiled Landsat normalized surface reflectance from 1997 to the present operationally updated every 16 days. Only data from 2020 to present available on the AWS, older data is available through the UMD API.</description>
    </item>
    <item>
      <title>GX database for NCBI Foreign Contamination Screen (FCS) Tool Suite</title>
      <link>https://registry.opendata.aws/ncbi-fcs-gx</link>
      <guid>https://registry.opendata.aws/ncbi-fcs-gx</guid>
      <description>Sequence database used by FCS-GX (Foreign Contamination Screen - Genome Cross-species aligner) to detect contamination from foreign organisms in genome sequences.</description>
    </item>
    <item>
      <title>Galaxy Evolution Explorer Satellite (GALEX)</title>
      <link>https://registry.opendata.aws/mast-galex</link>
      <guid>https://registry.opendata.aws/mast-galex</guid>
      <description>The Galaxy Evolution Explorer Satellite (GALEX) was a NASA mission led by the California Institute of Technology, whose primary goal was to investigate how star formation in galaxies evolved from the early universe up to the present. GALEX used microchannel plate detectors to obtain direct images in the near-UV (NUV) and far-UV (FUV), and a grism to disperse light for low resolution spectroscopy.</description>
    </item>
    <item>
      <title>Genome Ark</title>
      <link>https://registry.opendata.aws/genomeark</link>
      <guid>https://registry.opendata.aws/genomeark</guid>
      <description>The Genome Ark hosts genomic information for the Vertebrate Genomes Project (VGP) and other related projects. The VGP is an international collaboration that aims to generate complete and near error-free reference genomes for all extant vertebrate species. These genomes will be used to address fundamental questions in biology and disease, to identify species most genetically at risk for extinction, and to preserve genetic information of life.</description>
    </item>
    <item>
      <title>Google Satellite Embedding V1</title>
      <link>https://registry.opendata.aws/aef-source</link>
      <guid>https://registry.opendata.aws/aef-source</guid>
      <description>COG (Cloud-Optimized GeoTIFF) files that together contain the AlphaEarth Foundations annual Satellite Embedding dataset. It contains the annual embeddings for the years from 2018 to 2024, inclusive.</description>
    </item>
    <item>
      <title>Gretel Synthetic Safety Alignment Dataset</title>
      <link>https://registry.opendata.aws/gretel-synthetic-safety-alignment-en-v1</link>
      <guid>https://registry.opendata.aws/gretel-synthetic-safety-alignment-en-v1</guid>
      <description>A comprehensive dataset designed for aligning language models with safety and ethical guidelines. Contains 8,361 curated triplets of prompts, responses, and safe responses across various risk categories. Each entry includes safety scores, judge reasoning, and harm probability assessments, making it valuable for model alignment, testing, and benchmarking.</description>
    </item>
    <item>
      <title>Grid Algorithms and Data Analytics Library (GADAL)</title>
      <link>https://registry.opendata.aws/gadal</link>
      <guid>https://registry.opendata.aws/gadal</guid>
      <description>The aim of this project is to create an easy-to-use platform where various types of analytics can be performed on a wide range of electrical grid datasets. The aim is to establish an open-source library of algorithms that universities, national labs and other developers can contribute to which can be used on both open-source and proprietary grid data to improve the analysis of electrical distribution systems for the grid modeling community. OEDI Systems Integration (SI) is a grid algorithms and data analytics API created to standardize how data is sent between different modules that are run as part of a co-simulation.</description>
    </item>
    <item>
      <title>Gulfwide Avian Colony Monitoring Survey Photos</title>
      <link>https://registry.opendata.aws/gulfwide-avian-monitoring</link>
      <guid>https://registry.opendata.aws/gulfwide-avian-monitoring</guid>
      <description>For this project, The Water Institute (the Institute) and subcontractor Colibri Ecological Consulting, LLC (Colibri) utilized established methods and protocols capable of assessing changes of colonial waterbird populations and their important habitats within individual states and the broader northern Gulf of Mexico region.  Data collection activities included:
    Aerial Photographic Nest Surveys: Implementation of fixed-wing aircraft surveys intended to assess waterbird colonies and document associated nesting within select portions of the northern Gulf of Mexico. Additional detail is provided on the Survey Protocols page of this portal. 
    Nest Dotting Analyses: Review and analysis of aerial photographic nest surveys (2010-2013, 2015, 2018, and 2021) with the intention of documenting the breeding population size and associated nesting for each species at each colony. Additional detail is provided on the Dotting Protocols page of this portal. </description>
    </item>
    <item>
      <title>Guy&#x27;s Breast Cancer Lymph Nodes (GRAPE)</title>
      <link>https://registry.opendata.aws/guys-breast-cancer-lymph-nodes</link>
      <guid>https://registry.opendata.aws/guys-breast-cancer-lymph-nodes</guid>
      <description>This is a retrospective dataset of 1523 H&amp;amp;E-stained whole slide images (WSI) of lymph nodes from breast cancer patients. The cohort consisted of 177 patients (122 LN-positive - metastasis was reported in at least 1 LN - and 55 LN-negative patients) with invasive breast carcinoma treated between 1984 and 2002 at Guy’s Hospital London, UK. Slides were scanned and digitised at 40x magnification (0.23 µm/pixel), NanoZoomer H.T2.0 2.0-HT (Hamamatsu Photonics UK, Ltd, Welwyn Garden City, UK). WSIs are in .ndpi format.</description>
    </item>
    <item>
      <title>HIRLAM Weather Model</title>
      <link>https://registry.opendata.aws/hirlam</link>
      <guid>https://registry.opendata.aws/hirlam</guid>
      <description>HIRLAM (High Resolution Limited Area Model) is an operational synoptic and mesoscale weather prediction model managed by the Finnish Meteorological Institute.</description>
    </item>
    <item>
      <title>High Resolution Downscaled Climate Data for Southeast Alaska</title>
      <link>https://registry.opendata.aws/wrf-se-alaska-snap</link>
      <guid>https://registry.opendata.aws/wrf-se-alaska-snap</guid>
      <description>This dataset contains historical and projected dynamically downscaled climate data for the Southeast region of the State of Alaska at 1 and 4km spatial resolution and hourly temporal resolution. Select variables are also summarized into daily resolutions. This data was produced using the Weather Research and Forecasting (WRF) model (Version 4.0). We downscaled both Climate Forecast System Reanalysis (CFSR) historical reanalysis data (1980-2019) and both historical and projected runs from two GCM’s from the Coupled Model Inter-comparison Project 5 (CMIP5): GFDL-CM3 and NCAR-CCSM4 (historical run: 1980-2010 and RCP 8.5: 2030-2060).</description>
    </item>
    <item>
      <title>Homeland Security and Infrastructure US Cities</title>
      <link>https://registry.opendata.aws/hsip-lidar-us-cities</link>
      <guid>https://registry.opendata.aws/hsip-lidar-us-cities</guid>
      <description>The U.S. Cities elevation data collection program supported the US Department of Homeland Security Homeland Security and Infrastructure Program (HSIP). As part of the HSIP Program, there were 133+ U.S. cities that had imagery and LiDAR collected to provide the Homeland Security, Homeland Defense, and Emergency Preparedness, Response and Recovery (EPR&amp;amp;R) community with common operational, geospatially enabled baseline data needed to analyze threat, support critical infrastructure protection and expedite readiness, response and recovery in the event of a man-made or natural disaster. As a part of that, for some time, recurring LiDAR data was also being collected by a joint agreement of NGA and other federal agencies and the HIFLDS Working Group. The publicly released data excluded US Military Installation coverage, but it is provided in as is. These collects were acquired by contract using commercial collection companies. Some metadata information about the collection can be found at USGS at &lt;a href&#x3D;&quot;https://rockyweb.usgs.gov/vdelivery/Datasets/Staged/Elevation/Non_Standard_Contributed/NGA_US_Cities/Topeka_KS/NGA%20133%20US%20Cities%20Data%20Disclaimer%20and%20Explanation%20Readme.pdf&quot;&gt;https://rockyweb.usgs.gov/vdelivery/Datasets/Staged/Elevation/Non_Standard_Contributed/NGA_US_Cities/Topeka_KS/NGA%20133%20US%20Cities%20Data%20Disclaimer%20and%20Explanation%20Readme.pdf&lt;/a&gt;</description>
    </item>
    <item>
      <title>Hubble Space Telescope</title>
      <link>https://registry.opendata.aws/mast-hst</link>
      <guid>https://registry.opendata.aws/mast-hst</guid>
      <description>The Hubble Space Telescope (HST) is one of the most productive scientific instruments ever created. This dataset contains calibrated and raw data for all currently active instruments on HST: ACS, COS, STIS, WFC3, and FGS.</description>
    </item>
    <item>
      <title>Hybrid statistical-dynamic downscaling based on multi-model ensembles in Southeast Asia</title>
      <link>https://registry.opendata.aws/cmip6-era5-hybrid-southeast-asia</link>
      <guid>https://registry.opendata.aws/cmip6-era5-hybrid-southeast-asia</guid>
      <description>GCMs under CMIP6 have been widely used to investigate climate change impacts and put forward associated adaptation and mitigation strategies. However, the relatively coarse spatial resolutions (usually 100~300km) preclude their direct applications at regional scales, which are exactly where the analysis (e.g., hydrological model simulation) is performed. To bridge this gap, a typical approach is to ‘refine’ the information from GCMs through regional climate downscaling experiments, which can be conducted statistically, dynamically, or a combination thereof. Statistical downscaling establishes relationships between large-scale climate indicators and small-scale climate variables in the reference (historical) period. Subsequently, these relationships are kept unchanged in the future and used to predict the future variables. On the other hand, dynamical downscaling operates based on the physical processes and the associated interactions in the climate systems and thus can produce a full set of regional climate simulations (e.g., temperature and precipitation fields) that are dynamically consistent. However, traditional dynamical downscaling contains significant biases that are transferred from GCMs and may be enhanced during the process of downscaling, thus degrading the downscaled results. One promising approach to remove these biases is the hybrid statistical-dynamical downscaling method, where GCMs are firstly bias-corrected, and subsequently used as lower and lateral boundary conditions to drive the regional climate models (RCMs).In this work, we apply a hybrid statistical-dynamical downscaling method, following the approach of Xu et al. 2021. The bias-corrected dataset is adjusted to resemble ERA5-based mean climate and interannual variance, and with a non-linear trend from the ensemble mean of the 14 CMIP6 models. The dataset spans a historical period of 1979–2014 and future scenarios (SSP585) of 2015–2100, with a temporal scale of six-hour.The main contributions of this dataset are twofold. First, we provide the open-source and high-resolution (12.5km: Southeast Asia; 2.5km:Southern Malay Peninsula; 500m: Singapore, as shown in the following Figures) datasets, including precipitation, wind, temperature, radiation, etc. Second, through our experiment, this bias-corrected and downscaled dataset is of exceptional quality compared to that of the existing dynamical scaling work (e.g., CORDEX) in southeast Asia in terms of its ability to reproduce regional climate extremes, spatial patterns, etc. This dataset will be useful for policy-makers and researchers to establish the necessary pathways for resilient planning in order to mitigate the dire impacts of climate change.</description>
    </item>
    <item>
      <title>ISERV</title>
      <link>https://registry.opendata.aws/iserv</link>
      <guid>https://registry.opendata.aws/iserv</guid>
      <description>ISS SERVIR Environmental Research and Visualization System (ISERV) was a fully-automated prototype camera aboard the International Space Station that was tasked to capture high-resolution Earth imagery of specific locations at 3-7 frames per second. In the course of its regular operations during 2013 and 2014, ISERV&amp;#39;s camera acquired images that can be used primaliry in use is environmental and disaster management.</description>
    </item>
    <item>
      <title>Image localization  - fast.ai datasets</title>
      <link>https://registry.opendata.aws/fast-ai-imagelocal</link>
      <guid>https://registry.opendata.aws/fast-ai-imagelocal</guid>
      <description>Some of the most important datasets for image localization  research, including
Camvid and PASCAL VOC (2007 and 2012). This is part of the fast.ai datasets
collection hosted by AWS for convenience of fast.ai students. See
documentation link for citation and license details for each dataset.</description>
    </item>
    <item>
      <title>Imaging BSD licensed data and models</title>
      <link>https://registry.opendata.aws/biohub-imaging-bsd</link>
      <guid>https://registry.opendata.aws/biohub-imaging-bsd</guid>
      <description>This dataset contains a diverse range of imaging biological data and models. The data is sourced and curated by a team of experts at Biohub and is made available as part of these datasets only when it is not publicly accessible or requires transformations to support model training.</description>
    </item>
    <item>
      <title>InRad COVID-19 X-Ray and CT Scans</title>
      <link>https://registry.opendata.aws/inlab-covid-19-images-dataset</link>
      <guid>https://registry.opendata.aws/inlab-covid-19-images-dataset</guid>
      <description>This dataset is a collection of anonymized thoracic radiographs (X-Rays) and computed tomography (CT) scans of patients with suspected COVID-19. Images are acommpanied by a positive or negative diagnosis for SARS-CoV2 infection via RT-PCR. These images were provided by Hospital das Clínicas da Universidade de São Paulo, Hospital Sirio-Libanes, and by Laboratory Fleury.</description>
    </item>
    <item>
      <title>K2 Mission Data</title>
      <link>https://registry.opendata.aws/mast-k2</link>
      <guid>https://registry.opendata.aws/mast-k2</guid>
      <description>The K2 mission observed 100 square degrees for 80 days each across 20 different pointings along the ecliptic, collecting high-precision photometry for a selection of targets within each field. The mission began when the original Kepler mission ended due to loss of the second reaction wheel in 2013.</description>
    </item>
    <item>
      <title>KITTI Vision Benchmark Suite</title>
      <link>https://registry.opendata.aws/kitti</link>
      <guid>https://registry.opendata.aws/kitti</guid>
      <description>Dataset and benchmarks for computer vision research in the context of autonomous driving. The dataset has been recorded in and around the city of Karlsruhe, Germany using the mobile platform AnnieWay (VW station wagon) which has been equipped with several RGB and monochrome cameras, a Velodyne HDL 64 laser scanner as well as an accurate RTK corrected GPS/IMU localization unit. The dataset has been created for computer vision and machine learning research on stereo, optical flow, visual odometry, semantic segmentation, semantic instance segmentation, road segmentation, single image depth prediction, depth map completion, 2D and 3D object detection and object tracking. In addition, several raw data recordings are provided. The datasets are captured by driving around the mid-size city of Karlsruhe, in rural areas and on highways. Up to 15 cars and 30 pedestrians are visible per image.</description>
    </item>
    <item>
      <title>Kepler Mission Data</title>
      <link>https://registry.opendata.aws/mast-kepler</link>
      <guid>https://registry.opendata.aws/mast-kepler</guid>
      <description>The Kepler mission observed the brightness of more than 180,000 stars near the Cygnus constellation at a 30 minute cadence for 4 years in order to find transiting exoplanets, study variable stars, and find eclipsing binaries.</description>
    </item>
    <item>
      <title>MIMIC-IV Clinical Database Demo</title>
      <link>https://registry.opendata.aws/mimic-iv-demo</link>
      <guid>https://registry.opendata.aws/mimic-iv-demo</guid>
      <description>The Medical Information Mart for Intensive Care (MIMIC)-IV&amp;nbsp;database is comprised&amp;nbsp;of&amp;nbsp;deidentified electronic health records for patients admitted to the Beth Israel Deaconess Medical Center. Access to MIMIC-IV is limited to credentialed users. Here, we have provided an openly-available demo of MIMIC-IV containing&amp;nbsp;a subset of&amp;nbsp;100 patients. The dataset includes similar content to MIMIC-IV, but excludes free-text clinical notes. The demo may be useful for running workshops&amp;nbsp;and for&amp;nbsp;assessing whether the MIMIC-IV is appropriate for a study before making an access request.</description>
    </item>
    <item>
      <title>MIMIC-IV-ECG: Diagnostic Electrocardiogram Matched Subset</title>
      <link>https://registry.opendata.aws/mimic-iv-ecg</link>
      <guid>https://registry.opendata.aws/mimic-iv-ecg</guid>
      <description>The MIMIC-IV-ECG module contains approximately 800,000 diagnostic electrocardiograms across nearly 160,000 unique patients. These diagnostic ECGs use 12 leads and are 10 seconds in length. They are sampled at 500 Hz. This subset contains all of the ECGs for patients who appear in the MIMIC-IV Clinical Database. When a cardiologist report is available for a given ECG, we provide the needed information to link the waveform to the report. The patients in MIMIC-IV-ECG have been matched against the MIMIC-IV Clinical Database, making it possible to link to information across the MIMIC-IV modules.</description>
    </item>
    <item>
      <title>MISR Level 1B2 Ellipsoid Data V004</title>
      <link>https://registry.opendata.aws/nasa-mi1b2e</link>
      <guid>https://registry.opendata.aws/nasa-mi1b2e</guid>
      <description>MI1B2E_004 is the Multi-angle Imaging SpectroRadiometer (MISR) Level 1B2 Ellipsoid Data Version 4 product. It contains Ellipsoid-projected Top-of-Atmosphere (TOA) Radiance, resampled at the surface and topographically corrected, as well as geometrically corrected by PGE22. Data collection for this product is ongoing.MISR itself is an instrument designed to view Earth with cameras pointed in 9 different directions. As the instrument flies overhead, each piece of Earth&amp;#39;s surface below is successively imaged by all 9 cameras, in each of 4 wavelengths (blue, green, red, and near-infrared). The goal of MISR is to improve our understanding of the affects of sunlight on Earth, as well as distinguish different types of clouds, particles and surfaces. Specifically, MISR monitors the monthly, seasonal, and long-term trends in three areas: 1) amount and type of atmospheric particles (aerosols), including those formed by natural sources and by human activities; 2) amounts, types, and heights of clouds, and 3) distribution of land surface cover, including vegetation canopy structure.
Read our doc on how to get AWS Credentials to retrieve this data: &lt;a href&#x3D;&quot;https://data.asdc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;https://data.asdc.earthdata.nasa.gov/s3credentialsREADME&lt;/a&gt;</description>
    </item>
    <item>
      <title>MegaScenes</title>
      <link>https://registry.opendata.aws/megascenes</link>
      <guid>https://registry.opendata.aws/megascenes</guid>
      <description>The MegaScenes Dataset is an extensive collection of around 430k scenes, featuring over 100k structure-from-motion reconstructions and over 2 million registered images. MegaScenes includes a diverse array of scenes, such as minarets, building interiors, statues, bridges, towers, religious buildings, and natural landscapes. The images of these scenes are captured under varying conditions, including different times of day, various weather and illumination, and from different devices with distinct camera intrinsics.</description>
    </item>
    <item>
      <title>MetaGraph Sequence Indexes</title>
      <link>https://registry.opendata.aws/metagraph</link>
      <guid>https://registry.opendata.aws/metagraph</guid>
      <description>The MetaGraph Sequence Indexes dataset comprises full-text searchable index files for raw sequencing data hosted in major public repositories. These include the European Nucleotide Archive (ENA) managed by the European Bioinformatics Institute (EMBL-EBI), the Sequence Read Archive (SRA) maintained by the National Center for Biotechnology Information (NCBI), and the DNA Data Bank of Japan (DDBJ) Sequence Read Archive (DRA).All index files can be used with the MetaGraph framework for sequence search. Indexes can be jointly used for aggregated search in the cloud or can be individually downloaded for search using local hardware. </description>
    </item>
    <item>
      <title>Metagenomic reference libraries for Slacken</title>
      <link>https://registry.opendata.aws/slacken</link>
      <guid>https://registry.opendata.aws/slacken</guid>
      <description>Metagenomic indexes for use with the Slacken taxonomic classification tool</description>
    </item>
    <item>
      <title>Model Benchmarking</title>
      <link>https://registry.opendata.aws/biohub-benchmarking</link>
      <guid>https://registry.opendata.aws/biohub-benchmarking</guid>
      <description>This dataset includes data and models relevant to benchmarking multimodal biological models. The data has been sourced and curated by a team of experts at Biohub and is provided as part of these datasets only when it is not publicly available or requires transformation to support effective model benchmarking.</description>
    </item>
    <item>
      <title>Multimedia Commons</title>
      <link>https://registry.opendata.aws/multimedia-commons</link>
      <guid>https://registry.opendata.aws/multimedia-commons</guid>
      <description>The Multimedia Commons is a collection of audio and visual features computed for the nearly 100 million Creative Commons-licensed Flickr images and videos in the YFCC100M dataset from Yahoo! Labs, along with ground-truth annotations for selected subsets. The International Computer Science Institute (ICSI) and Lawrence Livermore National Laboratory are producing and distributing a core set of derived feature sets and annotations as part of an effort to enable large-scale video search capabilities. They have released this feature corpus into the public domain, under Creative Commons License 0, so it is free for anyone to use for any purpose.</description>
    </item>
    <item>
      <title>NASA 1993_AN_NASA Project</title>
      <link>https://registry.opendata.aws/nasa-1993-an-nasa</link>
      <guid>https://registry.opendata.aws/nasa-1993-an-nasa</guid>
      <description>This data set contains spot elevation measurements of Arctic, Greenland, Antarctic, and Patagonia sea ice and ice surface acquired using the NASA Airborne Topographic Mapper (ATM) instrumentation.
&lt;br&gt;&lt;h4 id&#x3D;&quot;blatm2&quot;&gt;BLATM2&lt;/h4&gt;
This data set contains resampled and smoothed elevation measurements of Arctic and Antarctic sea ice, as well as Greenland, Arctic, Patagonia, and Antarctic region land ice surface acquired using the NASA Airborne Topographic Mapper (ATM) instrumentation.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.nsidc.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA 1993_GR_NASA Project</title>
      <link>https://registry.opendata.aws/nasa-1993-gr-nasa</link>
      <guid>https://registry.opendata.aws/nasa-1993-gr-nasa</guid>
      <description>This data set contains depth sounder measurements of ice elevation, ice surface, ice bottom, and ice thickness over Greenland and Antarctica, acquired by the Multichannel Coherent Radar Depth Sounder (MCoRDS).
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.nsidc.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA 2007_GR_NASA Project</title>
      <link>https://registry.opendata.aws/nasa-2007-gr-nasa</link>
      <guid>https://registry.opendata.aws/nasa-2007-gr-nasa</guid>
      <description>This data set contains surface elevation data over Greenland measured by the NASA Land, Vegetation, and Ice Sensor (LVIS), an airborne lidar scanning laser altimeter.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.nsidc.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA 2008_AN_UTIG Project</title>
      <link>https://registry.opendata.aws/nasa-2008-an-utig</link>
      <guid>https://registry.opendata.aws/nasa-2008-an-utig</guid>
      <description>This data set contains vertical acceleration values for Antarctica using the BGM-3 Gravimeter. The data were collected by scientists working on the International Collaborative Exploration of the Cryosphere through Airborne Profiling (ICECAP) project, which is funded by the National Science Foundation (NSF) and the Natural Environment Research Council (NERC) with additional support from NASA Operation IceBridge.
&lt;br&gt;&lt;h4 id&#x3D;&quot;igbgm2&quot;&gt;IGBGM2&lt;/h4&gt;
This data set contains free air anomaly measurements taken over Antarctica using the BGM-3 Gravimeter. The data were collected by scientists working on the Investigating the Cryospheric Evolution of the Central Antarctic Plate (ICECAP) project funded by the National Science Foundation (NSF) and the Natural Environment Research Council (NERC) with additional support from NASA Operation IceBridge.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ir1hi1b&quot;&gt;IR1HI1B&lt;/h4&gt;
This data set contains Antarctica radar sounder echo strength profiles from the Hi-Capability Radar Sounder (HiCARS) Version 1 instrument. The data were collected by scientists working on the Investigating the Cryospheric Evolution of the Central Antarctic Plate (ICECAP) project, which was funded by the National Science Foundation (NSF) and the Natural Environment Research Council (NERC) with additional support from NASA Operation IceBridge.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ir1hi2&quot;&gt;IR1HI2&lt;/h4&gt;
This data set contains ice thickness, surface and bed elevation, and echo strength measurements taken over Antarctica using the Hi-Capability Airborne Radar Sounder (HiCARS) instrument. The data were collected by scientists working on the Investigating the Cryospheric Evolution of the Central Antarctic Plate (ICECAP) project, which is funded by the National Science Foundation (NSF) and the Natural Environment Research Council (NERC) with additional support from NASA Operation IceBridge.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ir2hi1b&quot;&gt;IR2HI1B&lt;/h4&gt;
This data set contains Antarctica radar sounder echo strength profiles from the Hi-Capability Radar Sounder (HiCARS) Version 2 instrument. The data were collected by scientists working on the Investigating the Cryospheric Evolution of the Central Antarctic Plate (ICECAP) project, which was funded by the National Science Foundation (NSF) and the Natural Environment Research Council (NERC) with additional support from NASA Operation IceBridge.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ir2hi2&quot;&gt;IR2HI2&lt;/h4&gt;
This data set contains ice thickness, surface and bed elevation, and echo strength measurements taken over Antarctica using the Hi-Capability Airborne Radar Sounder (HiCARS) instrument. The data were collected by scientists working on the Investigating the Cryospheric Evolution of the Central Antarctic Plate (ICECAP) project, which was funded by the National Science Foundation (NSF) and the Natural Environment Research Council (NERC) with additional support from NASA Operation IceBridge.
&lt;br&gt;&lt;h4 id&#x3D;&quot;iaprs1b&quot;&gt;IAPRS1B&lt;/h4&gt;
This data set contains static pressure values for Antarctica using the Paroscientific Digiquartz Transmitter. The data were collected by scientists working on the Investigating the Cryospheric Evolution of the Central Antarctic Plate (ICECAP) project, which is funded by the National Science Foundation (NSF) and the Natural Environment Research Council (NERC) with additional support from NASA Operation IceBridge.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ilutp1b&quot;&gt;ILUTP1B&lt;/h4&gt;
This data set contains laser ranges, returned pulses, and deviation for returned pulses in Antarctica and Greenland using the Riegl Laser Altimeter. The data were collected by scientists working on the Investigating the Cryospheric Evolution of the Central Antarctic Plate (ICECAP) project, which is funded by the National Science Foundation (NSF) and the Natural Environment Research Council (NERC) with additional support from NASA&amp;#39;s Operation IceBridge.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ilutp2&quot;&gt;ILUTP2&lt;/h4&gt;
This data set contains surface range values for Antarctica and Greenland derived from measurements captured by the Riegl Laser Altimeter. The data were collected by scientists working on the Investigating the Cryospheric Evolution of the Central Antarctic Plate (ICECAP) project, which is funded by the National Science Foundation (NSF) and the Natural Environment Research Council (NERC) with additional support from NASA Operation IceBridge.
&lt;br&gt;&lt;h4 id&#x3D;&quot;imfgm1b&quot;&gt;IMFGM1B&lt;/h4&gt;
This data set contains time-registered Level-1B field readings taken over Antarctica using the Watson-Gyro Fluxgate Magnetometer instrument. The data were collected as part of Operation IceBridge funded aircraft survey campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;igzls1b&quot;&gt;IGZLS1B&lt;/h4&gt;
This data set contains vertical, cross body, and along body acceleration values for geophysical survey flights in Antarctica using the ZLS Dynamic Gravity Meter. The data were collected by scientists working on the International Collaborative Exploration of the Cryosphere through Airborne Profiling (ICECAP) project, which was funded by the National Science Foundation (NSF), the Antarctic Climate and Ecosystems Collaborative Research Center, and the Natural Environment Research Council (NERC) with additional support from NASA Operation IceBridge.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.nsidc.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA 2009_AK_NASA Project</title>
      <link>https://registry.opendata.aws/nasa-2009-ak-nasa</link>
      <guid>https://registry.opendata.aws/nasa-2009-ak-nasa</guid>
      <description>This data set represents a collection of orthorectified images that were created using the NASA Ames Stereo Pipeline. The final images were obtained by processing stereo images from the IceBridge DMS L0 Raw Imagery data set, along with NASA&amp;#39;s Land, Vegetation, and Ice Sensor (LVIS) and Airborne Topographic Mapper (ATM) lidar data from the IceBridge LVIS L2 Geolocated Surface Elevation Product and IceBridge ATM L1B Elevation and Return Strength data sets, respectively. The closely related data set IceBridge DMS L3 Ames Stereo Pipeline Photogrammetric DEM provides the corresponding digital elevation models (DEMs) in GeoTIFF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;iodem3&quot;&gt;IODEM3&lt;/h4&gt;
This data set represents a collection of digital elevation models (DEMs) that were created using the NASA Ames Stereo Pipeline. The final DEMs were obtained by processing stereo images from the IceBridge DMS L0 Raw Imagery data set, along with NASA&amp;#39;s Land, Vegetation, and Ice Sensor (LVIS) and Airborne Topographic Mapper (ATM) lidar data from the IceBridge LVIS L2 Geolocated Surface Elevation Product and IceBridge ATM L1B Elevation and Return Strength data sets, respectively. The closely related data set IceBridge DMS L3 Ames Stereo Pipeline Orthorectified Images provides the corresponding orthorectified images in GeoTIFF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;irwis2&quot;&gt;IRWIS2&lt;/h4&gt;
This data set contains depth sounder measurements of elevation, surface, bottom, and thickness for Alaska taken from the Warm Ice Sounding Explorer (WISE). The data were collected as part of Operation IceBridge funded aircraft survey campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.nsidc.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA 2009_AK_UAF Project</title>
      <link>https://registry.opendata.aws/nasa-2009-ak-uaf</link>
      <guid>https://registry.opendata.aws/nasa-2009-ak-uaf</guid>
      <description>This data set contains flight reports from NASA Operation IceBridge Greenland, Arctic, Antarctic, and Alaska missions. Flight reports contain information on region, mission, aircraft model, flight data, purpose of flight, and on-board sensors. The flight reports were collected as part of Operation IceBridge funded aircraft survey campaigns. The corresponding flight lines can be found in the IceBridge L1B Thinned Flight Lines (IPFLT1B) data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ilakp1b&quot;&gt;ILAKP1B&lt;/h4&gt;
This data set contains surface profiles of Alaska Glaciers acquired using the airborne University of Alaska Fairbanks (UAF) Glacier Lidar system. The data were collected as part of Operation IceBridge funded aircraft survey campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ilaks1b&quot;&gt;ILAKS1B&lt;/h4&gt;
This data set contains scanning laser altimetry data points of Alaskan glaciers and parts of East and West Antarctica acquired by the airborne University of Alaska Fairbanks (UAF) Glacier Lidar system. The data were collected as part of NASA Operation IceBridge funded campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.nsidc.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA 2009_AN_CRESIS Project</title>
      <link>https://registry.opendata.aws/nasa-2009-an-cresis</link>
      <guid>https://registry.opendata.aws/nasa-2009-an-cresis</guid>
      <description>This data set contains depth sounder measurements of ice elevation, ice surface, ice bottom, and ice thickness for Greenland and Antarctica taken from the Multichannel Coherent Radar Depth Sounder (MCoRDS). The data were collected as part of Operation IceBridge funded aircraft survey campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.nsidc.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA 2009_AN_NASA Project</title>
      <link>https://registry.opendata.aws/nasa-2009-an-nasa</link>
      <guid>https://registry.opendata.aws/nasa-2009-an-nasa</guid>
      <description>This data set contains radar echograms taken over Greenland and Antarctica using the Center for Remote Sensing of Ice Sheets (CReSIS) Accumulation Radar instrument. The data were collected as part of Operation IceBridge funded campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ilatm1b&quot;&gt;ILATM1B&lt;/h4&gt;
This data set contains spot elevation measurements of Arctic and Antarctic sea ice, and Greenland, Antarctic Peninsula, and West Antarctic region ice surface acquired using the NASA Airborne Topographic Mapper (ATM) instrumentation. The data were collected as part of Operation IceBridge funded aircraft survey campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ilatm2&quot;&gt;ILATM2&lt;/h4&gt;
This data set contains resampled and smoothed elevation measurements of Arctic and Antarctic sea ice, and Greenland, Antarctic Peninsula, and West Antarctic region land ice surface acquired using the NASA Airborne Topographic Mapper (ATM) instrumentation. The data were collected as part of Operation IceBridge funded aircraft survey campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;idhdt4&quot;&gt;IDHDT4&lt;/h4&gt;
This data set contains surface elevation rate of change measurements derived from IceBridge and Pre-IceBridge Airborne Topographic Mapper (ATM) widescan elevation measurements data for Arctic and Antarctic missions flown under NASA&amp;#39;s Operation IceBridge (OIB) and Arctic Ice Mapping (AIM) projects.
&lt;br&gt;&lt;h4 id&#x3D;&quot;iocam1b&quot;&gt;IOCAM1B&lt;/h4&gt;
This data set contains images taken with the Continuous Airborne Mapping By Optical Translator (CAMBOT) over Antarctica and Greenland.
&lt;br&gt;&lt;h4 id&#x3D;&quot;iodcc0&quot;&gt;IODCC0&lt;/h4&gt;
This data set contains camera calibration reports for IceBridge Digital Mapping System (DMS) missions flown over Antarctica and Greenland.
&lt;br&gt;&lt;h4 id&#x3D;&quot;iodms1b&quot;&gt;IODMS1B&lt;/h4&gt;
This data set contains Level-1B imagery taken from the Digital Mapping System (DMS) over Greenland and Antarctica. The data were collected as part of Operation IceBridge funded aircraft survey campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;iodms3&quot;&gt;IODMS3&lt;/h4&gt;
The IceBridge DMS L3 Photogrammetric DEM (IODMS3) data set contains gridded digital elevation models and orthorectified images of Greenland and Antarctica derived from the Digital Mapping System (DMS). The data were collected as part of Operation IceBridge funded campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;iakst1b&quot;&gt;IAKST1B&lt;/h4&gt;
This data set contains surface temperature measurements of Arctic and Antarctic sea ice and land ice acquired by the Heitronics KT19.85 Series II Infrared Radiation Pyrometer. For flights with the NASA DC-8 aircraft, the National Suborbital Research Center (NSRC) operated the instrument and created the data product. For flights with the NASA P-3 and other aircraft, the instrument was operated by the Wallops Flight Facility (WFF) as part of the ATM instrument suite. The data were collected as part of the Operation IceBridge funded survey campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;irkub1b&quot;&gt;IRKUB1B&lt;/h4&gt;
This data set contains elevation and surface measurements over Greenland, the Arctic, and Antarctica, as well as flight path charts and echogram images acquired using the Center for Remote Sensing of Ice Sheets (CReSIS) Ku-Band Radar Altimeter.
&lt;br&gt;&lt;h4 id&#x3D;&quot;idcsi4&quot;&gt;IDCSI4&lt;/h4&gt;
This data set contains derived geophysical data products including sea ice freeboard, snow depth, and sea ice thickness measurements in Greenland and Antarctica retrieved from IceBridge Snow Radar, Digital Mapping System (DMS), Continuous Airborne Mapping By Optical Translator (CAMBOT), and Airborne Topographic Mapper (ATM) data sets. The data were collected as part of Operation IceBridge funded campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ilvis0&quot;&gt;ILVIS0&lt;/h4&gt;
This data set contains raw Inertial Measurement Unit (IMU), Global Positioning System (GPS), and camera data over Greenland, Antarctica, and Alaska measured by the NASA Land, Vegetation, and Ice Sensor (LVIS), an airborne lidar scanning laser altimeter. The data were collected as part of Operation IceBridge funded campaigns, including the Arctic Radiation - IceBridge Sea and Ice Experiment (ARISE).
&lt;br&gt;&lt;h4 id&#x3D;&quot;iolvis1a&quot;&gt;IOLVIS1A&lt;/h4&gt;
This data set contains geotagged images taken over Greenland and Antarctica by the NASA Digital Mapping Camera paired with the Land, Vegetation, and Ice Sensor (LVIS), an airborne lidar scanning laser altimeter. The data were collected as part of Operation IceBridge funded campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ilvis1b&quot;&gt;ILVIS1B&lt;/h4&gt;
This data set contains return energy waveform data measured over Greenland, Alaska, and Antarctica by the NASA Land, Vegetation, and Ice Sensor (LVIS), an airborne lidar scanning laser altimeter. The data were collected as part of Operation IceBridge funded campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ilvis2&quot;&gt;ILVIS2&lt;/h4&gt;
This data set contains surface elevation data over Greenland, Alaska, and Antarctica, measured by the NASA Land, Vegetation, and Ice Sensor (LVIS), an airborne lidar scanning laser altimeter. The data were collected as part of NASA Operation IceBridge funded campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;iggrv1b&quot;&gt;IGGRV1B&lt;/h4&gt;
This data set contains gravity measurements, including acceleration data in three orthogonal directions, from the Sander Geophysics AIRGrav airborne gravity system. Gravity data include latitude and Eotvos-corrected values, as well as free air correction at various along-flight-line time filtering scales. The data were collected as part of Operation IceBridge funded campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;irsno1b&quot;&gt;IRSNO1B&lt;/h4&gt;
This data set contains radar echograms taken from the Center for Remote Sensing of Ice Sheets (CReSIS) ultra wide-band snow radar over land and sea ice in the Arctic and Antarctic. In addition, airborne snow measurements were taken during 10 flights over Alaska mountains, ice fields, and glaciers at the end of May 2018 by a compact CReSIS FMCW radar system installed on a Single Otter aircraft. The data were collected as part of Operation IceBridge funded campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.nsidc.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA 2009_GR_NASA Project</title>
      <link>https://registry.opendata.aws/nasa-2009-gr-nasa</link>
      <guid>https://registry.opendata.aws/nasa-2009-gr-nasa</guid>
      <description>This data set contains contains Greenland ice thickness measurements acquired using the Pathfinder Advanced Radar Ice Sounder (PARIS). The data were collected as part of Operation IceBridge funded campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.nsidc.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA 2010_AN_NASA Project</title>
      <link>https://registry.opendata.aws/nasa-2010-an-nasa</link>
      <guid>https://registry.opendata.aws/nasa-2010-an-nasa</guid>
      <description>This data set contains Level-3 tomographic ice thickness measurements and ice thickness errors over areas of Greenland and Antarctica. Two of the data files additionally provide bed elevation measurements. The data were derived from measurements taken by the Center for Remote Sensing of Ice Sheets (CReSIS) Multichannel Coherent Radar Depth Sounder (MCoRDS) instrument and were collected as part of NASA Operation IceBridge funded campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.nsidc.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA 2010_AN_UTIG Project</title>
      <link>https://registry.opendata.aws/nasa-2010-an-utig</link>
      <guid>https://registry.opendata.aws/nasa-2010-an-utig</guid>
      <description>This data set contains geolocated surface elevation measurements captured over Antarctica using the Sigma Space Mapping Photon Counting Lidar and Riegl Laser Altimeter. The data were collected by scientists working on the International Collaborative Exploration of the Cryosphere through Airborne Profiling (ICECAP) project, which was funded by the National Science Foundation (NSF), the Antarctic Climate and Ecosystems Collaborative Research Center, and the Natural Environment Research Council (NERC) with additional support from NASA Operation IceBridge.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ilsnp1b&quot;&gt;ILSNP1B&lt;/h4&gt;
This data set contains nadir photon counting data captured over Antarctica using the Sigma Space photon counting lidar. Position and orientation data are included. The data were collected by scientists working on the International Collaborative Exploration of the Cryosphere through Airborne Profiling (ICECAP) project, which was funded by the National Science Foundation (NSF), the Antarctic Climate and Ecosystems Collaborative Research Center, and the Natural Environment Research Council (NERC) with additional support from NASA Operation IceBridge.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.nsidc.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA 2010_GR_NASA Project</title>
      <link>https://registry.opendata.aws/nasa-2010-gr-nasa</link>
      <guid>https://registry.opendata.aws/nasa-2010-gr-nasa</guid>
      <description>This data set contains reprocessed images depicting labels that indicate the sea ice surface category, created by processing IceBridge DMS L0 Raw Imagery with the Open Source Sea-ice Processing Algorithm. The images are provided as TIFF files (.tif). Additional metadata are provided as CSV text files (.csv), which are available as a single zip file named RDSISC4_metadata.zip. An orthorectified version of this data set is available as IceBridge-Related DMS-Derived L4 Sea Ice Surface Cover Classification Orthorectified Images.
&lt;br&gt;&lt;h4 id&#x3D;&quot;rdsisco4&quot;&gt;RDSISCO4&lt;/h4&gt;
This data set contains reprocessed, orthorectified images depicting labels that indicate the sea ice surface category, created by processing IceBridge DMS L0 Raw Imagery (IODMS0) with the Open Source Sea-ice Processing Algorithm. Orthorectification was done using digital elevation models from the IceBridge DMS L3 Ames Stereo Pipeline Photogrammetric DEM (IODEM3) collection. The standard (non-orthorectified) images are available as IceBridge-Related DMS-Derived L4 Sea Ice Surface Cover Classification Images (RDSISC4).
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.nsidc.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA 2011_AN_NASA Project</title>
      <link>https://registry.opendata.aws/nasa-2011-an-nasa</link>
      <guid>https://registry.opendata.aws/nasa-2011-an-nasa</guid>
      <description>This data set contains surface temperature measurements of Arctic and Antarctic sea ice and land ice acquired by the Heitronics KT19.85 Series II Infrared Radiation Pyrometer. The instrument is operated by the Wallops Flight Facility (WFF) as part of the ATM instrument suite. The data were collected as part of the Operation IceBridge funded survey campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ilnsa1b&quot;&gt;ILNSA1B&lt;/h4&gt;
This data set contains spot elevation measurements of Greenland, Arctic, and Antarctic sea ice acquired using the NASA Airborne Topographic Mapper (ATM) 4CT3 narrow scan instrumentation. The data were collected as part of Operation IceBridge funded aircraft survey campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.nsidc.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA 2011_AN_UTIG Project</title>
      <link>https://registry.opendata.aws/nasa-2011-an-utig</link>
      <guid>https://registry.opendata.aws/nasa-2011-an-utig</guid>
      <description>This data set contains geolocated photon elevations captured over Antarctica using the Sigma Space photon counting lidar. The data were collected by scientists working on the International Collaborative Exploration of the Cryosphere through Airborne Profiling (ICECAP) project, which was funded by the National Science Foundation (NSF), the Antarctic Climate and Ecosystems Collaborative Research Center, and the Natural Environment Research Council (NERC) with additional support from NASA Operation IceBridge.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.nsidc.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA 2012_AN_NASA Project</title>
      <link>https://registry.opendata.aws/nasa-2012-an-nasa</link>
      <guid>https://registry.opendata.aws/nasa-2012-an-nasa</guid>
      <description>This data set contains radar echograms taken from the Center for Remote Sensing of Ice Sheets (CReSIS) ultra Multichannel Coherent Radar Depth Sounder (MCoRDS) over land and sea ice in the Arctic and Antarctic.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.nsidc.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA 2012_AN_UTIG Project</title>
      <link>https://registry.opendata.aws/nasa-2012-an-utig</link>
      <guid>https://registry.opendata.aws/nasa-2012-an-utig</guid>
      <description>This data set contains vertical acceleration values for Antarctica using the CMG 1A dynamic gravity meter. The data were collected by scientists working on the Investigating the Cryospheric Evolution of the Central Antarctic Plate (ICECAP) project, which is funded by the National Science Foundation (NSF) and the Natural Environment Research Council (NERC) with additional support from NASA Operation IceBridge.
&lt;br&gt;&lt;h4 id&#x3D;&quot;igcmg2&quot;&gt;IGCMG2&lt;/h4&gt;
This data set contains geolocated free air gravity disturbances derived from measurements taken over Antarctica using the GT-1A gravity meter S-019. The data were collected by scientists working on the Investigating the Cryospheric Evolution of the Central Antarctic Plate (ICECAP) project, which is funded by the National Science Foundation (NSF) and the Natural Environment Research Council (NERC) with additional support from NASA Operation IceBridge.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.nsidc.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA 2012_GR_GBMF Project</title>
      <link>https://registry.opendata.aws/nasa-2012-gr-gbmf</link>
      <guid>https://registry.opendata.aws/nasa-2012-gr-gbmf</guid>
      <description>This data set contains Greenland and Antarctica gravity measurements taken from the Sander Geophysics AIRGrav airborne gravity system.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.nsidc.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA 2013_AK_UAF Project</title>
      <link>https://registry.opendata.aws/nasa-2013-ak-uaf</link>
      <guid>https://registry.opendata.aws/nasa-2013-ak-uaf</guid>
      <description>This data set contains radar echograms acquired by the University of Alaska Fairbanks High-Frequency Radar Sounder over select glaciers in Alaska.
&lt;br&gt;&lt;h4 id&#x3D;&quot;iruafhf2&quot;&gt;IRUAFHF2&lt;/h4&gt;
This data set contains measurements of glacier surface elevation, bed elevation, and ice thickness for Alaska and Northwestern Canada. Glacier surface elevation is derived from IceBridge UAF Lidar Scanner L1B Geolocated Surface Elevation Triplets (ILAKS1B). Radar bed returns are sourced from IceBridge UAF L1B HF Geolocated Radar Echo Strength Profiles (IRUAFHF1B) to provide glacier bed elevation and ice thickness. Radar-derived ice thickness and glacier bed elevation are provided as per-trace measurements from the corresponding L1B radar echo strength profile (referencing the WGS 84 ellipsoid).
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.nsidc.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA 2013_AN_NASA Project</title>
      <link>https://registry.opendata.aws/nasa-2013-an-nasa</link>
      <guid>https://registry.opendata.aws/nasa-2013-an-nasa</guid>
      <description>This data set contains spot elevation measurements of Arctic and Antarctic sea ice, and Greenland, Antarctic Peninsula, and West Antarctic region ice surface acquired using the NASA Airborne Topographic Mapper (ATM) instrumentation. The data were collected as part of Operation IceBridge funded aircraft survey campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ilvgh1b&quot;&gt;ILVGH1B&lt;/h4&gt;
This data set contains energy waveform data measured by the NASA Land, Vegetation, and Ice Sensor (LVIS), an airborne lidar scanning laser altimeter, aboard the Global Hawk Unmanned Aerial Vehicle. The data were collected as part of NASA Operation IceBridge funded campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ilvgh2&quot;&gt;ILVGH2&lt;/h4&gt;
This data set contains surface elevation data measured by the NASA Land, Vegetation, and Ice Sensor (LVIS), an airborne lidar scanning laser altimeter, aboard the Global Hawk Unmanned Aerial Vehicle. The data were collected as part of NASA Operation IceBridge funded campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ilnsa1b&quot;&gt;ILNSA1B&lt;/h4&gt;
This data set contains spot elevation measurements of Greenland, Arctic, and Antarctic sea ice acquired using the NASA Airborne Topographic Mapper (ATM) narrow-swath instrumentation. The data were collected as part of Operation IceBridge funded aircraft survey campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;imcs31b&quot;&gt;IMCS31B&lt;/h4&gt;
This data set contains magnetic field readings taken over Antarctica using the Scintrex CS-3 Cesium Magnetometer instrument. The data were collected as part of Operation IceBridge funded aircraft survey campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.nsidc.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA 2015_AK_UAF Project</title>
      <link>https://registry.opendata.aws/nasa-2015-ak-uaf</link>
      <guid>https://registry.opendata.aws/nasa-2015-ak-uaf</guid>
      <description>This data set contains radar echograms acquired by the Arizona Radio-Echo Sounder (ARES) over select glaciers in Alaska.
&lt;br&gt;&lt;h4 id&#x3D;&quot;irares2&quot;&gt;IRARES2&lt;/h4&gt;
This data set contains glacier surface elevation, bed elevation, and ice thickness measurements for Alaska and Northwestern Canada. Glacier surface elevation is derived from IceBridge UAF Lidar Scanner L1B Geolocated Surface Elevation Triplets (ILAKS1B). Radar bed returns are taken from IceBridge ARES L1B Geolocated Radar Echo Strength Profiles (IRARES1B).
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.nsidc.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA 2015_AN_NASA Project</title>
      <link>https://registry.opendata.aws/nasa-2015-an-nasa</link>
      <guid>https://registry.opendata.aws/nasa-2015-an-nasa</guid>
      <description>This data set contains geotagged images captured by NASA Digital Mapping Cameras, which were mounted alongside the Land, Vegetation, and Ice Sensor (LVIS), an airborne lidar scanning laser altimeter.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.nsidc.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA 2017_AN_NASA Project</title>
      <link>https://registry.opendata.aws/nasa-2017-an-nasa</link>
      <guid>https://registry.opendata.aws/nasa-2017-an-nasa</guid>
      <description>This data set contains spot elevation measurements with corresponding waveforms of Arctic and Antarctic sea ice, and Greenland, Antarctic Peninsula, and West Antarctic region ice surface acquired using the NASA Airborne Topographic Mapper (ATM) instrumentation. The data were collected as part of Operation IceBridge funded aircraft survey campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ilatmgr&quot;&gt;ILATMGR&lt;/h4&gt;
This data set reports surface grain size estimates of snow and ice using waveform measurements from NASA&amp;#39;s Airborne Topographic Mapper (ATM) narrow-swath and wide-swath instrumentation over the Greenland ice sheet and surrounding sea ice.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ilnsaw1b&quot;&gt;ILNSAW1B&lt;/h4&gt;
This data set contains spot elevation measurements with corresponding waveforms of Greenland, Arctic, and Antarctic sea ice. The data complement the IceBridge ATM L1B Near-Infrared Waveforms data, which are measured at near-infrared wavelength. The data were acquired as part of aircraft survey campaigns funded by Operation IceBridge.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.nsidc.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA 2017_GR_NASA Project</title>
      <link>https://registry.opendata.aws/nasa-2017-gr-nasa</link>
      <guid>https://registry.opendata.aws/nasa-2017-gr-nasa</guid>
      <description>This data set contains gravity measurements taken over Greenland and Antarctica by the Lamont-Doherty Earth Observatory (LDEO) Gravimeter Suite. The data were collected as part of Operation IceBridge funded campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ilvis2&quot;&gt;ILVIS2&lt;/h4&gt;
This data set contains surface elevation data over parts of Greenland, measured by the NASA Land, Vegetation, and Ice Sensor (LVIS), an airborne lidar scanning laser altimeter. The data were collected as part of NASA Operation IceBridge funded campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.nsidc.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA 2018_AN_NASA Project</title>
      <link>https://registry.opendata.aws/nasa-2018-an-nasa</link>
      <guid>https://registry.opendata.aws/nasa-2018-an-nasa</guid>
      <description>This data set contains geolocated waveforms of Greenland, Arctic, and Antarctic sea ice measured by the Airborne Topographic Mapper (ATM) near-infrared (NIR) lidar. The data complement, and are intended to be used with, the IceBridge Narrow Swath ATM L1B Elevation and Return Strength with Waveforms data, which are measured at green wavelength. The data were acquired as part of aircraft survey campaigns funded by Operation IceBridge.
&lt;br&gt;&lt;h4 id&#x3D;&quot;iocam0&quot;&gt;IOCAM0&lt;/h4&gt;
This data set contains raw images and associated aircraft position and attitude data, taken over Antarctica and Greenland by the Continuous Airborne Mapping By Optical Translator (CAMBOT), part of the Airborne Topographic Mapper (ATM) instrument suite. The data were collected as part of Operation IceBridge funded aircraft survey campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;iocam1b&quot;&gt;IOCAM1B&lt;/h4&gt;
This data set contains high-resolution imagery taken with the Continuous Airborne Mapping By Optical Translator (CAMBOT) system over Antarctica and Greenland. The data were collected as part of Operation IceBridge funded aircraft survey campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.nsidc.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA ABLE-2 Project</title>
      <link>https://registry.opendata.aws/nasa-able-2</link>
      <guid>https://registry.opendata.aws/nasa-able-2</guid>
      <description>ABLE-2A_Aerosol_AircraftInSitu_Electra_Data is the in-situ aerosol data collected onboard the NASA Electra aircraft during the Amazon Boundary Layer Experiment - 2A (ABLE-2A) suborbital campaign. Data collection for this product is complete. From 1983-2001, NASA conducted a collection of field campaigns as part of the Global Tropospheric Experiment (GTE). Among those were the Amazon Boundary Layer Experiment (ABLE 2) campaigns. ABLE 2 was divided into two sub-campaigns, ABLE 2A (dry season) and ABLE 2B (wet season). ABLE 2A took place from July-August 1985, while ABLE 2B took place from April-May 1987. The goal of ABLE 2 was to better understand the role of tropics in global atmospheric chemistry and investigate processes which might lead to the enhanced concentrations of carbon monoxide (CO) in the tropical upper troposphere. ABLE 2 was a partnership with NASA and the Brazilian agency, Instituto Nacional de Pesquisas Espaciais (INPE), along with the Instituto Nacional de Pesquisas da Amazonia (INPA) providing facilities and logistical information. To accomplish its objectives, the ABLE 2 science team deployed the NASA Lockheed Electra aircraft, balloons, and free-flying sondes. Flights took place over the Amazon region in Brazil for both sub-campaigns. ABLE 2A consisted of 15 flights while ABLE 2B consisted of 21 flights with the fully equipped Electra. For most ABLE 2A flights, the data collected included in-situ measurements of CO2, CO, MHC, NO (nitric oxide), N2O, O3, DMS (dimethyl sulfide), aerosol composition, and meteorological parameters. ABLE 2B had the Electra instrumented with remote and in-situ techniques for measuring the atmospheric distribution of a variety of carbon, nitrogen, and sulfur gases; aerosol size and composition; and to measure ozone. The typical approach to flights involved high-altitude passes over research areas using the downward facing UV Differential Absorption Lidar (DIAL). The ABLE 2 campaign represents a modest advance in understanding the influence of the tropical rain forest ecosystem on the chemistry of the troposphere. Detailed descriptions related to the motivation, implementation, and instrument payloads are available in the ABLE 2A overview paper and the ABLE 2B overview paper. A collection of the publications based on ABLE 2A and 2B observation are available in the Journal of Geophysical Research special issues: Global Tropospheric Experiment/Chemical Instrumentation Test and Evaluation Results (GTE/ABLE 2A) and The Amazon Boundary Layer Experiment 2B.
&lt;br&gt;&lt;h4 id&#x3D;&quot;able-2a_tracegas_aircraftinsitu_electra_data&quot;&gt;ABLE-2A_TraceGas_AircraftInSitu_Electra_Data&lt;/h4&gt;
ABLE-2A_TraceGas_AircraftInSitu_Electra_Data is the in-situ trace gas data collected onboard the NASA Electra aircraft during the Amazon Boundary Layer Experiment - 2A (ABLE-2A) suborbital campaign. Data using chemiluminescence, gas traps, cryogenic air samples, and IR lasers are featured in this collection. Data collection for this product is complete. From 1983-2001, NASA conducted a collection of field campaigns as part of the Global Tropospheric Experiment (GTE). Among those were the Amazon Boundary Layer Experiment (ABLE 2) campaigns. ABLE 2 was divided into two sub-campaigns, ABLE 2A (dry season) and ABLE 2B (wet season). ABLE 2A took place from July-August 1985, while ABLE 2B took place from April-May 1987. The goal of ABLE 2 was to better understand the role of tropics in global atmospheric chemistry and investigate processes which might lead to the enhanced concentrations of carbon monoxide (CO) in the tropical upper troposphere. ABLE 2 was a partnership with NASA and the Brazilian agency, Instituto Nacional de Pesquisas Espaciais (INPE), along with the Instituto Nacional de Pesquisas da Amazonia (INPA) providing facilities and logistical information. To accomplish its objectives, the ABLE 2 science team deployed the NASA Lockheed Electra aircraft, balloons, and free-flying sondes. Flights took place over the Amazon region in Brazil for both sub-campaigns. ABLE 2A consisted of 15 flights while ABLE 2B consisted of 21 flights with the fully equipped Electra. For most ABLE 2A flights, the data collected included in-situ measurements of CO2, CO, MHC, NO (nitric oxide), N2O, O3, DMS (dimethyl sulfide), aerosol composition, and meteorological parameters. ABLE 2B had the Electra instrumented with remote and in-situ techniques for measuring the atmospheric distribution of a variety of carbon, nitrogen, and sulfur gases; aerosol size and composition; and to measure ozone. The typical approach to flights involved high-altitude passes over research areas using the downward facing UV Differential Absorption Lidar (DIAL). The ABLE 2 campaign represents a modest advance in understanding the influence of the tropical rain forest ecosystem on the chemistry of the troposphere. Detailed descriptions related to the motivation, implementation, and instrument payloads are available in the ABLE 2A overview paper and the ABLE 2B overview paper. A collection of the publications based on ABLE 2A and 2B observation are available in the Journal of Geophysical Research special issues: Global Tropospheric Experiment/Chemical Instrumentation Test and Evaluation Results (GTE/ABLE 2A) and The Amazon Boundary Layer Experiment 2B.
&lt;br&gt;&lt;h4 id&#x3D;&quot;able-2a_metnav_aircraftinsitu_electra_data&quot;&gt;ABLE-2A_MetNav_AircraftInSitu_Electra_Data&lt;/h4&gt;
ABLE-2A_MetNav_AircraftInSitu_Electra_Data is the in-situ meteorology and navigational data collected onboard the NASA Electra aircraft during the Amazon Boundary Layer Experiment - 2A (ABLE-2A) suborbital campaign. Data collection for this product is complete. From 1983-2001, NASA conducted a collection of field campaigns as part of the Global Tropospheric Experiment (GTE). Among those were the Amazon Boundary Layer Experiment (ABLE 2) campaigns. ABLE 2 was divided into two sub-campaigns, ABLE 2A (dry season) and ABLE 2B (wet season). ABLE 2A took place from July-August 1985, while ABLE 2B took place from April-May 1987. The goal of ABLE 2 was to better understand the role of tropics in global atmospheric chemistry and investigate processes which might lead to the enhanced concentrations of carbon monoxide (CO) in the tropical upper troposphere. ABLE 2 was a partnership with NASA and the Brazilian agency, Instituto Nacional de Pesquisas Espaciais (INPE), along with the Instituto Nacional de Pesquisas da Amazonia (INPA) providing facilities and logistical information. To accomplish its objectives, the ABLE 2 science team deployed the NASA Lockheed Electra aircraft, balloons, and free-flying sondes. Flights took place over the Amazon region in Brazil for both sub-campaigns. ABLE 2A consisted of 15 flights while ABLE 2B consisted of 21 flights with the fully equipped Electra. For most ABLE 2A flights, the data collected included in-situ measurements of CO2, CO, MHC, NO (nitric oxide), N2O, O3, DMS (dimethyl sulfide), aerosol composition, and meteorological parameters. ABLE 2B had the Electra instrumented with remote and in-situ techniques for measuring the atmospheric distribution of a variety of carbon, nitrogen, and sulfur gases; aerosol size and composition; and to measure ozone. The typical approach to flights involved high-altitude passes over research areas using the downward facing UV Differential Absorption Lidar (DIAL). The ABLE 2 campaign represents a modest advance in understanding the influence of the tropical rain forest ecosystem on the chemistry of the troposphere. Detailed descriptions related to the motivation, implementation, and instrument payloads are available in the ABLE 2A overview paper and the ABLE 2B overview paper. A collection of the publications based on ABLE 2A and 2B observation are available in the Journal of Geophysical Research special issues: Global Tropospheric Experiment/Chemical Instrumentation Test and Evaluation Results (GTE/ABLE 2A) and The Amazon Boundary Layer Experiment 2B.
&lt;br&gt;&lt;h4 id&#x3D;&quot;able-2a_ground_data&quot;&gt;ABLE-2A_Ground_Data&lt;/h4&gt;
ABLE-2A_Ground_Data is the ground site data collected during the Amazon Boundary Layer Experiment - 2A (ABLE-2A) suborbital campaign. Data collection for this product is complete. From 1983-2001, NASA conducted a collection of field campaigns as part of the Global Tropospheric Experiment (GTE). Among those were the Amazon Boundary Layer Experiment (ABLE 2) campaigns. ABLE 2 was divided into two sub-campaigns, ABLE 2A (dry season) and ABLE 2B (wet season). ABLE 2A took place from July-August 1985, while ABLE 2B took place from April-May 1987. The goal of ABLE 2 was to better understand the role of tropics in global atmospheric chemistry and investigate processes which might lead to the enhanced concentrations of carbon monoxide (CO) in the tropical upper troposphere. ABLE 2 was a partnership with NASA and the Brazilian agency, Instituto Nacional de Pesquisas Espaciais (INPE), along with the Instituto Nacional de Pesquisas da Amazonia (INPA) providing facilities and logistical information. To accomplish its objectives, the ABLE 2 science team deployed the NASA Lockheed Electra aircraft, balloons, and free-flying sondes. Flights took place over the Amazon region in Brazil for both sub-campaigns. ABLE 2A consisted of 15 flights while ABLE 2B consisted of 21 flights with the fully equipped Electra. For most ABLE 2A flights, the data collected included in-situ measurements of CO2, CO, MHC, NO (nitric oxide), N2O, O3, DMS (dimethyl sulfide), aerosol composition, and meteorological parameters. ABLE 2B had the Electra instrumented with remote and in-situ techniques for measuring the atmospheric distribution of a variety of carbon, nitrogen, and sulfur gases; aerosol size and composition; and to measure ozone. The typical approach to flights involved high-altitude passes over research areas using the downward facing UV Differential Absorption Lidar (DIAL). The ABLE 2 campaign represents a modest advance in understanding the influence of the tropical rain forest ecosystem on the chemistry of the troposphere. Detailed descriptions related to the motivation, implementation, and instrument payloads are available in the ABLE 2A overview paper and the ABLE 2B overview paper. A collection of the publications based on ABLE 2A and 2B observation are available in the Journal of Geophysical Research special issues: Global Tropospheric Experiment/Chemical Instrumentation Test and Evaluation Results (GTE/ABLE 2A) and The Amazon Boundary Layer Experiment 2B.
&lt;br&gt;&lt;h4 id&#x3D;&quot;able-2a_merge_data&quot;&gt;ABLE-2A_Merge_Data&lt;/h4&gt;
ABLE-2A_Merge_Data is the merge data collected onboard the NASA Electra aircraft during the Amazon Boundary Layer Experiment - 2A (ABLE-2A) suborbital campaign. Data collection for this product is complete. From 1983-2001, NASA conducted a collection of field campaigns as part of the Global Tropospheric Experiment (GTE). Among those were the Amazon Boundary Layer Experiment (ABLE 2) campaigns. ABLE 2 was divided into two sub-campaigns, ABLE 2A (dry season) and ABLE 2B (wet season). ABLE 2A took place from July-August 1985, while ABLE 2B took place from April-May 1987. The goal of ABLE 2 was to better understand the role of tropics in global atmospheric chemistry and investigate processes which might lead to the enhanced concentrations of carbon monoxide (CO) in the tropical upper troposphere. ABLE 2 was a partnership with NASA and the Brazilian agency, Instituto Nacional de Pesquisas Espaciais (INPE), along with the Instituto Nacional de Pesquisas da Amazonia (INPA) providing facilities and logistical information. To accomplish its objectives, the ABLE 2 science team deployed the NASA Lockheed Electra aircraft, balloons, and free-flying sondes. Flights took place over the Amazon region in Brazil for both sub-campaigns. ABLE 2A consisted of 15 flights while ABLE 2B consisted of 21 flights with the fully equipped Electra. For most ABLE 2A flights, the data collected included in-situ measurements of CO2, CO, MHC, NO (nitric oxide), N2O, O3, DMS (dimethyl sulfide), aerosol composition, and meteorological parameters. ABLE 2B had the Electra instrumented with remote and in-situ techniques for measuring the atmospheric distribution of a variety of carbon, nitrogen, and sulfur gases; aerosol size and composition; and to measure ozone. The typical approach to flights involved high-altitude passes over research areas using the downward facing UV Differential Absorption Lidar (DIAL). The ABLE 2 campaign represents a modest advance in understanding the influence of the tropical rain forest ecosystem on the chemistry of the troposphere. Detailed descriptions related to the motivation, implementation, and instrument payloads are available in the ABLE 2A overview paper and the ABLE 2B overview paper. A collection of the publications based on ABLE 2A and 2B observation are available in the Journal of Geophysical Research special issues: Global Tropospheric Experiment/Chemical Instrumentation Test and Evaluation Results (GTE/ABLE 2A) and The Amazon Boundary Layer Experiment 2B.
&lt;br&gt;&lt;h4 id&#x3D;&quot;able-2a_sondes_data&quot;&gt;ABLE-2A_Sondes_Data&lt;/h4&gt;
ABLE-2A_Sondes_Data is the radiosonde and rawinsonde data collected during the Amazon Boundary Layer Experiment - 2A (ABLE-2A) suborbital campaign. Data collection for this product is complete. From 1983-2001, NASA conducted a collection of field campaigns as part of the Global Tropospheric Experiment (GTE). Among those were the Amazon Boundary Layer Experiment (ABLE 2) campaigns. ABLE 2 was divided into two sub-campaigns, ABLE 2A (dry season) and ABLE 2B (wet season). ABLE 2A took place from July-August 1985, while ABLE 2B took place from April-May 1987. The goal of ABLE 2 was to better understand the role of tropics in global atmospheric chemistry and investigate processes which might lead to the enhanced concentrations of carbon monoxide (CO) in the tropical upper troposphere. ABLE 2 was a partnership with NASA and the Brazilian agency, Instituto Nacional de Pesquisas Espaciais (INPE), along with the Instituto Nacional de Pesquisas da Amazonia (INPA) providing facilities and logistical information. To accomplish its objectives, the ABLE 2 science team deployed the NASA Lockheed Electra aircraft, balloons, and free-flying sondes. Flights took place over the Amazon region in Brazil for both sub-campaigns. ABLE 2A consisted of 15 flights while ABLE 2B consisted of 21 flights with the fully equipped Electra. For most ABLE 2A flights, the data collected included in-situ measurements of CO2, CO, MHC, NO (nitric oxide), N2O, O3, DMS (dimethyl sulfide), aerosol composition, and meteorological parameters. ABLE 2B had the Electra instrumented with remote and in-situ techniques for measuring the atmospheric distribution of a variety of carbon, nitrogen, and sulfur gases; aerosol size and composition; and to measure ozone. The typical approach to flights involved high-altitude passes over research areas using the downward facing UV Differential Absorption Lidar (DIAL). The ABLE 2 campaign represents a modest advance in understanding the influence of the tropical rain forest ecosystem on the chemistry of the troposphere. Detailed descriptions related to the motivation, implementation, and instrument payloads are available in the ABLE 2A overview paper and the ABLE 2B overview paper. A collection of the publications based on ABLE 2A and 2B observation are available in the Journal of Geophysical Research special issues: Global Tropospheric Experiment/Chemical Instrumentation Test and Evaluation Results (GTE/ABLE 2A) and The Amazon Boundary Layer Experiment 2B.
&lt;br&gt;&lt;h4 id&#x3D;&quot;able-2b_aerosol_aircraftinsitu_electra_data&quot;&gt;ABLE-2B_Aerosol_AircraftInSitu_Electra_Data&lt;/h4&gt;
ABLE-2B_Aerosol_AircraftInSitu_Electra_Data is the in-situ aerosol data collected onboard the NASA Electra aircraft during the Amazon Boundary Layer Experiment - 2B (ABLE-2B) suborbital campaign. Data collection for this product is complete. From 1983-2001, NASA conducted a collection of field campaigns as part of the Global Tropospheric Experiment (GTE). Among those were the Amazon Boundary Layer Experiment (ABLE 2) campaigns. ABLE 2 was divided into two sub-campaigns, ABLE 2A (dry season) and ABLE 2B (wet season). ABLE 2A took place from July-August 1985, while ABLE 2B took place from April-May 1987. The goal of ABLE 2 was to better understand the role of tropics in global atmospheric chemistry and investigate processes which might lead to the enhanced concentrations of carbon monoxide (CO) in the tropical upper troposphere. ABLE 2 was a partnership with NASA and the Brazilian agency, Instituto Nacional de Pesquisas Espaciais (INPE), along with the Instituto Nacional de Pesquisas da Amazonia (INPA) providing facilities and logistical information. To accomplish its objectives, the ABLE 2 science team deployed the NASA Lockheed Electra aircraft, balloons, and free-flying sondes. Flights took place over the Amazon region in Brazil for both sub-campaigns. ABLE 2A consisted of 15 flights while ABLE 2B consisted of 21 flights with the fully equipped Electra. For most ABLE 2A flights, the data collected included in-situ measurements of CO2, CO, MHC, NO (nitric oxide), N2O, O3, DMS (dimethyl sulfide), aerosol composition, and meteorological parameters. ABLE 2B had the Electra instrumented with remote and in-situ techniques for measuring the atmospheric distribution of a variety of carbon, nitrogen, and sulfur gases; aerosol size and composition; and to measure ozone. The typical approach to flights involved high-altitude passes over research areas using the downward facing UV Differential Absorption Lidar (DIAL). The ABLE 2 campaign represents a modest advance in understanding the influence of the tropical rain forest ecosystem on the chemistry of the troposphere. Detailed descriptions related to the motivation, implementation, and instrument payloads are available in the ABLE 2A overview paper and the ABLE 2B overview paper. A collection of the publications based on ABLE 2A and 2B observation are available in the Journal of Geophysical Research special issues: Global Tropospheric Experiment/Chemical Instrumentation Test and Evaluation Results (GTE/ABLE 2A) and The Amazon Boundary Layer Experiment 2B.
&lt;br&gt;&lt;h4 id&#x3D;&quot;able-2b_tracegas_aircraftinsitu_electra_data&quot;&gt;ABLE-2B_TraceGas_AircraftInSitu_Electra_Data&lt;/h4&gt;
ABLE-2B_TraceGas_AircraftInSitu_Electra_Data is the in-situ trace gas data collected onboard the NASA Electra aircraft during the Amazon Boundary Layer Experiment - 2B (ABLE-2B) suborbital campaign. Data using chemiluminescence, gas traps, and grab samples are featured in this collection. Data collection for this product is complete. From 1983-2001, NASA conducted a collection of field campaigns as part of the Global Tropospheric Experiment (GTE). Among those were the Amazon Boundary Layer Experiment (ABLE 2) campaigns. ABLE 2 was divided into two sub-campaigns, ABLE 2A (dry season) and ABLE 2B (wet season). ABLE 2A took place from July-August 1985, while ABLE 2B took place from April-May 1987. The goal of ABLE 2 was to better understand the role of tropics in global atmospheric chemistry and investigate processes which might lead to the enhanced concentrations of carbon monoxide (CO) in the tropical upper troposphere. ABLE 2 was a partnership with NASA and the Brazilian agency, Instituto Nacional de Pesquisas Espaciais (INPE), along with the Instituto Nacional de Pesquisas da Amazonia (INPA) providing facilities and logistical information. To accomplish its objectives, the ABLE 2 science team deployed the NASA Lockheed Electra aircraft, balloons, and free-flying sondes. Flights took place over the Amazon region in Brazil for both sub-campaigns. ABLE 2A consisted of 15 flights while ABLE 2B consisted of 21 flights with the fully equipped Electra. For most ABLE 2A flights, the data collected included in-situ measurements of CO2, CO, MHC, NO (nitric oxide), N2O, O3, DMS (dimethyl sulfide), aerosol composition, and meteorological parameters. ABLE 2B had the Electra instrumented with remote and in-situ techniques for measuring the atmospheric distribution of a variety of carbon, nitrogen, and sulfur gases; aerosol size and composition; and to measure ozone. The typical approach to flights involved high-altitude passes over research areas using the downward facing UV Differential Absorption Lidar (DIAL). The ABLE 2 campaign represents a modest advance in understanding the influence of the tropical rain forest ecosystem on the chemistry of the troposphere. Detailed descriptions related to the motivation, implementation, and instrument payloads are available in the ABLE 2A overview paper and the ABLE 2B overview paper. A collection of the publications based on ABLE 2A and 2B observation are available in the Journal of Geophysical Research special issues: Global Tropospheric Experiment/Chemical Instrumentation Test and Evaluation Results (GTE/ABLE 2A) and The Amazon Boundary Layer Experiment 2B.
&lt;br&gt;&lt;h4 id&#x3D;&quot;able-2b_metnav_aircraftinsitu_electra_data&quot;&gt;ABLE-2B_MetNav_AircraftInSitu_Electra_Data&lt;/h4&gt;
ABLE-2B_MetNav_AircraftInSitu_Electra_Data is the in-situ meteorology and navigational data collected onboard the NASA Electra aircraft during the Amazon Boundary Layer Experiment - 2B (ABLE-2B) suborbital campaign. Data collection for this product is complete. From 1983-2001, NASA conducted a collection of field campaigns as part of the Global Tropospheric Experiment (GTE). Among those were the Amazon Boundary Layer Experiment (ABLE 2) campaigns. ABLE 2 was divided into two sub-campaigns, ABLE 2A (dry season) and ABLE 2B (wet season). ABLE 2A took place from July-August 1985, while ABLE 2B took place from April-May 1987. The goal of ABLE 2 was to better understand the role of tropics in global atmospheric chemistry and investigate processes which might lead to the enhanced concentrations of carbon monoxide (CO) in the tropical upper troposphere. ABLE 2 was a partnership with NASA and the Brazilian agency, Instituto Nacional de Pesquisas Espaciais (INPE), along with the Instituto Nacional de Pesquisas da Amazonia (INPA) providing facilities and logistical information. To accomplish its objectives, the ABLE 2 science team deployed the NASA Lockheed Electra aircraft, balloons, and free-flying sondes. Flights took place over the Amazon region in Brazil for both sub-campaigns. ABLE 2A consisted of 15 flights while ABLE 2B consisted of 21 flights with the fully equipped Electra. For most ABLE 2A flights, the data collected included in-situ measurements of CO2, CO, MHC, NO (nitric oxide), N2O, O3, DMS (dimethyl sulfide), aerosol composition, and meteorological parameters. ABLE 2B had the Electra instrumented with remote and in-situ techniques for measuring the atmospheric distribution of a variety of carbon, nitrogen, and sulfur gases; aerosol size and composition; and to measure ozone. The typical approach to flights involved high-altitude passes over research areas using the downward facing UV Differential Absorption Lidar (DIAL). The ABLE 2 campaign represents a modest advance in understanding the influence of the tropical rain forest ecosystem on the chemistry of the troposphere. Detailed descriptions related to the motivation, implementation, and instrument payloads are available in the ABLE 2A overview paper and the ABLE 2B overview paper. A collection of the publications based on ABLE 2A and 2B observation are available in the Journal of Geophysical Research special issues: Global Tropospheric Experiment/Chemical Instrumentation Test and Evaluation Results (GTE/ABLE 2A) and The Amazon Boundary Layer Experiment 2B.
&lt;br&gt;&lt;h4 id&#x3D;&quot;able-2b_ground_data&quot;&gt;ABLE-2B_Ground_Data&lt;/h4&gt;
ABLE-2B_Ground_Data is the ground data collected during the Amazon Boundary Layer Experiment - 2B (ABLE-2B) suborbital campaign. Data using grab samples are featured in this collection. Data collection for this product is complete. From 1983-2001, NASA conducted a collection of field campaigns as part of the Global Tropospheric Experiment (GTE). Among those were the Amazon Boundary Layer Experiment (ABLE 2) campaigns. ABLE 2 was divided into two sub-campaigns, ABLE 2A (dry season) and ABLE 2B (wet season). ABLE 2A took place from July-August 1985, while ABLE 2B took place from April-May 1987. The goal of ABLE 2 was to better understand the role of tropics in global atmospheric chemistry and investigate processes which might lead to the enhanced concentrations of carbon monoxide (CO) in the tropical upper troposphere. ABLE 2 was a partnership with NASA and the Brazilian agency, Instituto Nacional de Pesquisas Espaciais (INPE), along with the Instituto Nacional de Pesquisas da Amazonia (INPA) providing facilities and logistical information. To accomplish its objectives, the ABLE 2 science team deployed the NASA Lockheed Electra aircraft, balloons, and free-flying sondes. Flights took place over the Amazon region in Brazil for both sub-campaigns. ABLE 2A consisted of 15 flights while ABLE 2B consisted of 21 flights with the fully equipped Electra. For most ABLE 2A flights, the data collected included in-situ measurements of CO2, CO, MHC, NO (nitric oxide), N2O, O3, DMS (dimethyl sulfide), aerosol composition, and meteorological parameters. ABLE 2B had the Electra instrumented with remote and in-situ techniques for measuring the atmospheric distribution of a variety of carbon, nitrogen, and sulfur gases; aerosol size and composition; and to measure ozone. The typical approach to flights involved high-altitude passes over research areas using the downward facing UV Differential Absorption Lidar (DIAL). The ABLE 2 campaign represents a modest advance in understanding the influence of the tropical rain forest ecosystem on the chemistry of the troposphere. Detailed descriptions related to the motivation, implementation, and instrument payloads are available in the ABLE 2A overview paper and the ABLE 2B overview paper. A collection of the publications based on ABLE 2A and 2B observation are available in the Journal of Geophysical Research special issues: Global Tropospheric Experiment/Chemical Instrumentation Test and Evaluation Results (GTE/ABLE 2A) and The Amazon Boundary Layer Experiment 2B.
&lt;br&gt;&lt;h4 id&#x3D;&quot;able-2b_merge_data&quot;&gt;ABLE-2B_Merge_Data&lt;/h4&gt;
ABLE-2B_Merge_Data is the merge data collected onboard the NASA Electra aircraft during the Amazon Boundary Layer Experiment - 2B (ABLE-2B) suborbital campaign. Data using chemiluminescence, gas traps, and grab samples are featured in this collection. Data collection for this product is complete. From 1983-2001, NASA conducted a collection of field campaigns as part of the Global Tropospheric Experiment (GTE). Among those were the Amazon Boundary Layer Experiment (ABLE 2) campaigns. ABLE 2 was divided into two sub-campaigns, ABLE 2A (dry season) and ABLE 2B (wet season). ABLE 2A took place from July-August 1985, while ABLE 2B took place from April-May 1987. The goal of ABLE 2 was to better understand the role of tropics in global atmospheric chemistry and investigate processes which might lead to the enhanced concentrations of carbon monoxide (CO) in the tropical upper troposphere. ABLE 2 was a partnership with NASA and the Brazilian agency, Instituto Nacional de Pesquisas Espaciais (INPE), along with the Instituto Nacional de Pesquisas da Amazonia (INPA) providing facilities and logistical information. To accomplish its objectives, the ABLE 2 science team deployed the NASA Lockheed Electra aircraft, balloons, and free-flying sondes. Flights took place over the Amazon region in Brazil for both sub-campaigns. ABLE 2A consisted of 15 flights while ABLE 2B consisted of 21 flights with the fully equipped Electra. For most ABLE 2A flights, the data collected included in-situ measurements of CO2, CO, MHC, NO (nitric oxide), N2O, O3, DMS (dimethyl sulfide), aerosol composition, and meteorological parameters. ABLE 2B had the Electra instrumented with remote and in-situ techniques for measuring the atmospheric distribution of a variety of carbon, nitrogen, and sulfur gases; aerosol size and composition; and to measure ozone. The typical approach to flights involved high-altitude passes over research areas using the downward facing UV Differential Absorption Lidar (DIAL). The ABLE 2 campaign represents a modest advance in understanding the influence of the tropical rain forest ecosystem on the chemistry of the troposphere. Detailed descriptions related to the motivation, implementation, and instrument payloads are available in the ABLE 2A overview paper and the ABLE 2B overview paper. A collection of the publications based on ABLE 2A and 2B observation are available in the Journal of Geophysical Research special issues: Global Tropospheric Experiment/Chemical Instrumentation Test and Evaluation Results (GTE/ABLE 2A) and The Amazon Boundary Layer Experiment 2B.
&lt;br&gt;&lt;h4 id&#x3D;&quot;able-2b_sondes_data&quot;&gt;ABLE-2B_Sondes_Data&lt;/h4&gt;
ABLE-2B_Sondes_Data is the rawinsonde and tethered balloon data collected during the Amazon Boundary Layer Experiment - 2B (ABLE-2B) suborbital campaign. Data collection for this product is complete. From 1983-2001, NASA conducted a collection of field campaigns as part of the Global Tropospheric Experiment (GTE). Among those were the Amazon Boundary Layer Experiment (ABLE 2) campaigns. ABLE 2 was divided into two sub-campaigns, ABLE 2A (dry season) and ABLE 2B (wet season). ABLE 2A took place from July-August 1985, while ABLE 2B took place from April-May 1987. The goal of ABLE 2 was to better understand the role of tropics in global atmospheric chemistry and investigate processes which might lead to the enhanced concentrations of carbon monoxide (CO) in the tropical upper troposphere. ABLE 2 was a partnership with NASA and the Brazilian agency, Instituto Nacional de Pesquisas Espaciais (INPE), along with the Instituto Nacional de Pesquisas da Amazonia (INPA) providing facilities and logistical information. To accomplish its objectives, the ABLE 2 science team deployed the NASA Lockheed Electra aircraft, balloons, and free-flying sondes. Flights took place over the Amazon region in Brazil for both sub-campaigns. ABLE 2A consisted of 15 flights while ABLE 2B consisted of 21 flights with the fully equipped Electra. For most ABLE 2A flights, the data collected included in-situ measurements of CO2, CO, MHC, NO (nitric oxide), N2O, O3, DMS (dimethyl sulfide), aerosol composition, and meteorological parameters. ABLE 2B had the Electra instrumented with remote and in-situ techniques for measuring the atmospheric distribution of a variety of carbon, nitrogen, and sulfur gases; aerosol size and composition; and to measure ozone. The typical approach to flights involved high-altitude passes over research areas using the downward facing UV Differential Absorption Lidar (DIAL). The ABLE 2 campaign represents a modest advance in understanding the influence of the tropical rain forest ecosystem on the chemistry of the troposphere. Detailed descriptions related to the motivation, implementation, and instrument payloads are available in the ABLE 2A overview paper and the ABLE 2B overview paper. A collection of the publications based on ABLE 2A and 2B observation are available in the Journal of Geophysical Research special issues: Global Tropospheric Experiment/Chemical Instrumentation Test and Evaluation Results (GTE/ABLE 2A) and The Amazon Boundary Layer Experiment 2B.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.asdc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA ABLE-3 Project</title>
      <link>https://registry.opendata.aws/nasa-able-3</link>
      <guid>https://registry.opendata.aws/nasa-able-3</guid>
      <description>ABLE-3A_TraceGas_AircraftInSitu_Electra_Data is the in-situ trace gas data collected onboard the NASA Electra aircraft during the Arctic Boundary Layer Expedition - 3A (ABLE-3A) suborbital campaign. Data using grab samples, gas chromatography, and Laser Induced Fluorescence (LIF) are featured in this collection. Data collection for this product is complete. From 1983-2001, NASA conducted a collection of field campaigns as part of the Global Tropospheric Experiment (GTE). Among those were the Arctic Boundary Layer Expedition (ABLE 3) campaigns. ABLE 3 was broken into two sub-campaigns: ABLE 3A and ABLE 3B. ABLE 3A took place in the Arctic and subarctic regions of North America and Greenland, while ABLE 3B took place in the north central and northeastern regions of Canada. ABLE 3 was focused on understanding the “early warning” response of the near-surface, organic, active layer to climate variability with a special emphasis placed on identifying the range of variables which might have a significant influence on the tropospheric O3 budged in the Barrow region. The ABLE 3 campaigns took place in the summer since the summer is critical to an assessment of the full impact of accumulated winter/spring pollutant loadings. Observations in the summer months could also determine if significant long-range transport and injection of pollutants occur. ABLE 3A took place July-August 1988, and ABLE 3B took place July-August 1990. To accomplish its objectives, the ABLE 3 science team deployed the NASA Lockheed Electra aircraft on both sub-campaigns. With over 50 total flights, ABLE 3 aimed to utilize the Electra aircraft to take measurements of methane (CH4), carbon monoxide (CO), carbon dioxide (CO2), nonmethane hydrocarbons (NMHC), acetic acid (HA), formic acid (HFo), nitric oxide (NO), nitrogen dioxide (NO2), total “reactive” nitrogen gas (NOy), nitric acid (HNO3), peroxyacetyl nitrate (PAN), peroxypropionyl nitrate (PPN), ozone (O3), and aerosol chemical composition and size distribution. Onboard the Electra, airborne UV Differential Absorption Lidar (DIAL) provided remotely sense data on the two-dimensional distribution of aerosols and O3. The results of ABLE 3 indicate that atmospheric chemical changes in arctic and subarctic regions may serve as unique early warning indicators of global changes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;able-3a_metnav_aircraftinsitu_electra_data&quot;&gt;ABLE-3A_MetNav_AircraftInSitu_Electra_Data&lt;/h4&gt;
ABLE-3A_MetNav_AircraftInSitu_Electra_Data is the in-situ meteorology and navigational data collected onboard the NASA Electra aircraft during the Arctic Boundary Layer Expedition - 3A (ABLE-3A) suborbital campaign. Data collection for this product is complete. From 1983-2001, NASA conducted a collection of field campaigns as part of the Global Tropospheric Experiment (GTE). Among those were the Arctic Boundary Layer Expedition (ABLE 3) campaigns. ABLE 3 was broken into two sub-campaigns: ABLE 3A and ABLE 3B. ABLE 3A took place in the Arctic and subarctic regions of North America and Greenland, while ABLE 3B took place in the north central and northeastern regions of Canada. ABLE 3 was focused on understanding the “early warning” response of the near-surface, organic, active layer to climate variability with a special emphasis placed on identifying the range of variables which might have a significant influence on the tropospheric O3 budged in the Barrow region. The ABLE 3 campaigns took place in the summer since the summer is critical to an assessment of the full impact of accumulated winter/spring pollutant loadings. Observations in the summer months could also determine if significant long-range transport and injection of pollutants occur. ABLE 3A took place July-August 1988, and ABLE 3B took place July-August 1990. To accomplish its objectives, the ABLE 3 science team deployed the NASA Lockheed Electra aircraft on both sub-campaigns. With over 50 total flights, ABLE 3 aimed to utilize the Electra aircraft to take measurements of methane (CH4), carbon monoxide (CO), carbon dioxide (CO2), nonmethane hydrocarbons (NMHC), acetic acid (HA), formic acid (HFo), nitric oxide (NO), nitrogen dioxide (NO2), total “reactive” nitrogen gas (NOy), nitric acid (HNO3), peroxyacetyl nitrate (PAN), peroxypropionyl nitrate (PPN), ozone (O3), and aerosol chemical composition and size distribution. Onboard the Electra, airborne UV Differential Absorption Lidar (DIAL) provided remotely sense data on the two-dimensional distribution of aerosols and O3. The results of ABLE 3 indicate that atmospheric chemical changes in arctic and subarctic regions may serve as unique early warning indicators of global changes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;able-3a_aircraftremotesensing_electra_dial_data&quot;&gt;ABLE-3A_AircraftRemoteSensing_Electra_DIAL_Data&lt;/h4&gt;
ABLE-3A_AircraftRemoteSensing_Electra_DIAL_Data is the remotely sensed Differential Absorption Lidar (DIAL) data collected onboard the NASA Electra aircraft during the Arctic Boundary Layer Expedition - 3A (ABLE-3A) suborbital campaign. Data collection for this product is complete. From 1983-2001, NASA conducted a collection of field campaigns as part of the Global Tropospheric Experiment (GTE). Among those were the Arctic Boundary Layer Expedition (ABLE 3) campaigns. ABLE 3 was broken into two sub-campaigns: ABLE 3A and ABLE 3B. ABLE 3A took place in the Arctic and subarctic regions of North America and Greenland, while ABLE 3B took place in the north central and northeastern regions of Canada. ABLE 3 was focused on understanding the “early warning” response of the near-surface, organic, active layer to climate variability with a special emphasis placed on identifying the range of variables which might have a significant influence on the tropospheric O3 budged in the Barrow region. The ABLE 3 campaigns took place in the summer since the summer is critical to an assessment of the full impact of accumulated winter/spring pollutant loadings. Observations in the summer months could also determine if significant long-range transport and injection of pollutants occur. ABLE 3A took place July-August 1988, and ABLE 3B took place July-August 1990. To accomplish its objectives, the ABLE 3 science team deployed the NASA Lockheed Electra aircraft on both sub-campaigns. With over 50 total flights, ABLE 3 aimed to utilize the Electra aircraft to take measurements of methane (CH4), carbon monoxide (CO), carbon dioxide (CO2), nonmethane hydrocarbons (NMHC), acetic acid (HA), formic acid (HFo), nitric oxide (NO), nitrogen dioxide (NO2), total “reactive” nitrogen gas (NOy), nitric acid (HNO3), peroxyacetyl nitrate (PAN), peroxypropionyl nitrate (PPN), ozone (O3), and aerosol chemical composition and size distribution. Onboard the Electra, airborne UV Differential Absorption Lidar (DIAL) provided remotely sense data on the two-dimensional distribution of aerosols and O3. The results of ABLE 3 indicate that atmospheric chemical changes in arctic and subarctic regions may serve as unique early warning indicators of global changes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;able-3a_ground_data&quot;&gt;ABLE-3A_Ground_Data&lt;/h4&gt;
ABLE-3A_Ground_Data is the ground site data collected during the Arctic Boundary Layer Expedition - 3A (ABLE-3A) suborbital campaign. Data from the Harvard CO2 instrument and mist chambers are featured in this collection. Data collection for this product is complete. From 1983-2001, NASA conducted a collection of field campaigns as part of the Global Tropospheric Experiment (GTE). Among those were the Arctic Boundary Layer Expedition (ABLE 3) campaigns. ABLE 3 was broken into two sub-campaigns: ABLE 3A and ABLE 3B. ABLE 3A took place in the Arctic and subarctic regions of North America and Greenland, while ABLE 3B took place in the north central and northeastern regions of Canada. ABLE 3 was focused on understanding the “early warning” response of the near-surface, organic, active layer to climate variability with a special emphasis placed on identifying the range of variables which might have a significant influence on the tropospheric O3 budged in the Barrow region. The ABLE 3 campaigns took place in the summer since the summer is critical to an assessment of the full impact of accumulated winter/spring pollutant loadings. Observations in the summer months could also determine if significant long-range transport and injection of pollutants occur. ABLE 3A took place July-August 1988, and ABLE 3B took place July-August 1990. To accomplish its objectives, the ABLE 3 science team deployed the NASA Lockheed Electra aircraft on both sub-campaigns. With over 50 total flights, ABLE 3 aimed to utilize the Electra aircraft to take measurements of methane (CH4), carbon monoxide (CO), carbon dioxide (CO2), nonmethane hydrocarbons (NMHC), acetic acid (HA), formic acid (HFo), nitric oxide (NO), nitrogen dioxide (NO2), total “reactive” nitrogen gas (NOy), nitric acid (HNO3), peroxyacetyl nitrate (PAN), peroxypropionyl nitrate (PPN), ozone (O3), and aerosol chemical composition and size distribution. Onboard the Electra, airborne UV Differential Absorption Lidar (DIAL) provided remotely sense data on the two-dimensional distribution of aerosols and O3. The results of ABLE 3 indicate that atmospheric chemical changes in arctic and subarctic regions may serve as unique early warning indicators of global changes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;able-3a_merge_data&quot;&gt;ABLE-3A_Merge_Data&lt;/h4&gt;
ABLE-3A_Merge_Data is the merge data collected onboard the NASA Electra aircraft during the Arctic Boundary Layer Expedition - 3A (ABLE-3A) suborbital campaign. Data collection for this product is complete. From 1983-2001, NASA conducted a collection of field campaigns as part of the Global Tropospheric Experiment (GTE). Among those were the Arctic Boundary Layer Expedition (ABLE 3) campaigns. ABLE 3 was broken into two sub-campaigns: ABLE 3A and ABLE 3B. ABLE 3A took place in the Arctic and subarctic regions of North America and Greenland, while ABLE 3B took place in the north central and northeastern regions of Canada. ABLE 3 was focused on understanding the “early warning” response of the near-surface, organic, active layer to climate variability with a special emphasis placed on identifying the range of variables which might have a significant influence on the tropospheric O3 budged in the Barrow region. The ABLE 3 campaigns took place in the summer since the summer is critical to an assessment of the full impact of accumulated winter/spring pollutant loadings. Observations in the summer months could also determine if significant long-range transport and injection of pollutants occur. ABLE 3A took place July-August 1988, and ABLE 3B took place July-August 1990. To accomplish its objectives, the ABLE 3 science team deployed the NASA Lockheed Electra aircraft on both sub-campaigns. With over 50 total flights, ABLE 3 aimed to utilize the Electra aircraft to take measurements of methane (CH4), carbon monoxide (CO), carbon dioxide (CO2), nonmethane hydrocarbons (NMHC), acetic acid (HA), formic acid (HFo), nitric oxide (NO), nitrogen dioxide (NO2), total “reactive” nitrogen gas (NOy), nitric acid (HNO3), peroxyacetyl nitrate (PAN), peroxypropionyl nitrate (PPN), ozone (O3), and aerosol chemical composition and size distribution. Onboard the Electra, airborne UV Differential Absorption Lidar (DIAL) provided remotely sense data on the two-dimensional distribution of aerosols and O3. The results of ABLE 3 indicate that atmospheric chemical changes in arctic and subarctic regions may serve as unique early warning indicators of global changes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;able-3a_trajectory_data&quot;&gt;ABLE-3A_Trajectory_Data&lt;/h4&gt;
ABLE-3A_Trajectory_Data is the trajectory data collected during the Arctic Boundary Layer Expedition - 3A (ABLE-3A) suborbital campaign. Data collection for this product is complete. From 1983-2001, NASA conducted a collection of field campaigns as part of the Global Tropospheric Experiment (GTE). Among those were the Arctic Boundary Layer Expedition (ABLE 3) campaigns. ABLE 3 was broken into two sub-campaigns: ABLE 3A and ABLE 3B. ABLE 3A took place in the Arctic and subarctic regions of North America and Greenland, while ABLE 3B took place in the north central and northeastern regions of Canada. ABLE 3 was focused on understanding the “early warning” response of the near-surface, organic, active layer to climate variability with a special emphasis placed on identifying the range of variables which might have a significant influence on the tropospheric O3 budged in the Barrow region. The ABLE 3 campaigns took place in the summer since the summer is critical to an assessment of the full impact of accumulated winter/spring pollutant loadings. Observations in the summer months could also determine if significant long-range transport and injection of pollutants occur. ABLE 3A took place July-August 1988, and ABLE 3B took place July-August 1990. To accomplish its objectives, the ABLE 3 science team deployed the NASA Lockheed Electra aircraft on both sub-campaigns. With over 50 total flights, ABLE 3 aimed to utilize the Electra aircraft to take measurements of methane (CH4), carbon monoxide (CO), carbon dioxide (CO2), nonmethane hydrocarbons (NMHC), acetic acid (HA), formic acid (HFo), nitric oxide (NO), nitrogen dioxide (NO2), total “reactive” nitrogen gas (NOy), nitric acid (HNO3), peroxyacetyl nitrate (PAN), peroxypropionyl nitrate (PPN), ozone (O3), and aerosol chemical composition and size distribution. Onboard the Electra, airborne UV Differential Absorption Lidar (DIAL) provided remotely sense data on the two-dimensional distribution of aerosols and O3. The results of ABLE 3 indicate that atmospheric chemical changes in arctic and subarctic regions may serve as unique early warning indicators of global changes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;able-3b_aerosol_aircraftinsitu_electra_data&quot;&gt;ABLE-3B_Aerosol_AircraftInSitu_Electra_Data&lt;/h4&gt;
ABLE-3B_Aerosol_AircraftInSitu_Electra_Data is the in-situ aerosol data collected onboard the NASA Electra aircraft during the Arctic Boundary Layer Expedition - 3B (ABLE-3B) suborbital campaign. Data using mist chambers and teflon filters are featured in this collection. Data collection for this product is complete. From 1983-2001, NASA conducted a collection of field campaigns as part of the Global Tropospheric Experiment (GTE). Among those were the Arctic Boundary Layer Expedition (ABLE 3) campaigns. ABLE 3 was broken into two sub-campaigns: ABLE 3A and ABLE 3B. ABLE 3A took place in the Arctic and subarctic regions of North America and Greenland, while ABLE 3B took place in the north central and northeastern regions of Canada. ABLE 3 was focused on understanding the “early warning” response of the near-surface, organic, active layer to climate variability with a special emphasis placed on identifying the range of variables which might have a significant influence on the tropospheric O3 budged in the Barrow region. The ABLE 3 campaigns took place in the summer since the summer is critical to an assessment of the full impact of accumulated winter/spring pollutant loadings. Observations in the summer months could also determine if significant long-range transport and injection of pollutants occur. ABLE 3A took place July-August 1988, and ABLE 3B took place July-August 1990. To accomplish its objectives, the ABLE 3 science team deployed the NASA Lockheed Electra aircraft on both sub-campaigns. With over 50 total flights, ABLE 3 aimed to utilize the Electra aircraft to take measurements of methane (CH4), carbon monoxide (CO), carbon dioxide (CO2), nonmethane hydrocarbons (NMHC), acetic acid (HA), formic acid (HFo), nitric oxide (NO), nitrogen dioxide (NO2), total “reactive” nitrogen gas (NOy), nitric acid (HNO3), peroxyacetyl nitrate (PAN), peroxypropionyl nitrate (PPN), ozone (O3), and aerosol chemical composition and size distribution. Onboard the Electra, airborne UV Differential Absorption Lidar (DIAL) provided remotely sense data on the two-dimensional distribution of aerosols and O3. The results of ABLE 3 indicate that atmospheric chemical changes in arctic and subarctic regions may serve as unique early warning indicators of global changes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;able-3b_tracegas_aircraftinsitu_electra_data&quot;&gt;ABLE-3B_TraceGas_AircraftInSitu_Electra_Data&lt;/h4&gt;
ABLE-3B_TraceGas_AircraftInSitu_Electra_Data is the in-situ trace gas data collected onboard the NASA Electra aircraft during the Arctic Boundary Layer Expedition - 3B (ABLE-3B) suborbital campaign. Data using grab samples, gas chromatography, Laser Induced Fluorescence (LIF), and the Differential Absorption CO, CH4, N2O Measurements (DACOM) instrument are featured in this collection. Data collection for this product is complete. From 1983-2001, NASA conducted a collection of field campaigns as part of the Global Tropospheric Experiment (GTE). Among those were the Arctic Boundary Layer Expedition (ABLE 3) campaigns. ABLE 3 was broken into two sub-campaigns: ABLE 3A and ABLE 3B. ABLE 3A took place in the Arctic and subarctic regions of North America and Greenland, while ABLE 3B took place in the north central and northeastern regions of Canada. ABLE 3 was focused on understanding the “early warning” response of the near-surface, organic, active layer to climate variability with a special emphasis placed on identifying the range of variables which might have a significant influence on the tropospheric O3 budged in the Barrow region. The ABLE 3 campaigns took place in the summer since the summer is critical to an assessment of the full impact of accumulated winter/spring pollutant loadings. Observations in the summer months could also determine if significant long-range transport and injection of pollutants occur. ABLE 3A took place July-August 1988, and ABLE 3B took place July-August 1990. To accomplish its objectives, the ABLE 3 science team deployed the NASA Lockheed Electra aircraft on both sub-campaigns. With over 50 total flights, ABLE 3 aimed to utilize the Electra aircraft to take measurements of methane (CH4), carbon monoxide (CO), carbon dioxide (CO2), nonmethane hydrocarbons (NMHC), acetic acid (HA), formic acid (HFo), nitric oxide (NO), nitrogen dioxide (NO2), total “reactive” nitrogen gas (NOy), nitric acid (HNO3), peroxyacetyl nitrate (PAN), peroxypropionyl nitrate (PPN), ozone (O3), and aerosol chemical composition and size distribution. Onboard the Electra, airborne UV Differential Absorption Lidar (DIAL) provided remotely sense data on the two-dimensional distribution of aerosols and O3. The results of ABLE 3 indicate that atmospheric chemical changes in arctic and subarctic regions may serve as unique early warning indicators of global changes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;able-3b_metnav_aircraftinsitu_electra_data&quot;&gt;ABLE-3B_MetNav_AircraftInSitu_Electra_Data&lt;/h4&gt;
ABLE-3B_MetNav_AircraftInSitu_Electra_Data is the in-situ meteorological and navigational data collected onboard the NASA Electra aircraft during the Arctic Boundary Layer Expedition - 3B (ABLE-3B) suborbital campaign. Data from the Turbulent Air Motion Measurement System (TAMMS) instrument are featured in this collection. Data collection for this product is complete. From 1983-2001, NASA conducted a collection of field campaigns as part of the Global Tropospheric Experiment (GTE). Among those were the Arctic Boundary Layer Expedition (ABLE 3) campaigns. ABLE 3 was broken into two sub-campaigns: ABLE 3A and ABLE 3B. ABLE 3A took place in the Arctic and subarctic regions of North America and Greenland, while ABLE 3B took place in the north central and northeastern regions of Canada. ABLE 3 was focused on understanding the “early warning” response of the near-surface, organic, active layer to climate variability with a special emphasis placed on identifying the range of variables which might have a significant influence on the tropospheric O3 budged in the Barrow region. The ABLE 3 campaigns took place in the summer since the summer is critical to an assessment of the full impact of accumulated winter/spring pollutant loadings. Observations in the summer months could also determine if significant long-range transport and injection of pollutants occur. ABLE 3A took place July-August 1988, and ABLE 3B took place July-August 1990. To accomplish its objectives, the ABLE 3 science team deployed the NASA Lockheed Electra aircraft on both sub-campaigns. With over 50 total flights, ABLE 3 aimed to utilize the Electra aircraft to take measurements of methane (CH4), carbon monoxide (CO), carbon dioxide (CO2), nonmethane hydrocarbons (NMHC), acetic acid (HA), formic acid (HFo), nitric oxide (NO), nitrogen dioxide (NO2), total “reactive” nitrogen gas (NOy), nitric acid (HNO3), peroxyacetyl nitrate (PAN), peroxypropionyl nitrate (PPN), ozone (O3), and aerosol chemical composition and size distribution. Onboard the Electra, airborne UV Differential Absorption Lidar (DIAL) provided remotely sense data on the two-dimensional distribution of aerosols and O3. The results of ABLE 3 indicate that atmospheric chemical changes in arctic and subarctic regions may serve as unique early warning indicators of global changes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;able-3b_aircraftremotesensing_electra_dial_data&quot;&gt;ABLE-3B_AircraftRemoteSensing_Electra_DIAL_Data&lt;/h4&gt;
ABLE-3B_AircraftRemoteSensing_Electra_DIAL_Data is the remotely sensed Differential Absorption Lidar (DIAL) data collected onboard the NASA Electra aircraft during the Arctic Boundary Layer Expedition - 3B (ABLE-3B) suborbital campaign. Data collection for this product is complete. From 1983-2001, NASA conducted a collection of field campaigns as part of the Global Tropospheric Experiment (GTE). Among those were the Arctic Boundary Layer Expedition (ABLE 3) campaigns. ABLE 3 was broken into two sub-campaigns: ABLE 3A and ABLE 3B. ABLE 3A took place in the Arctic and subarctic regions of North America and Greenland, while ABLE 3B took place in the north central and northeastern regions of Canada. ABLE 3 was focused on understanding the “early warning” response of the near-surface, organic, active layer to climate variability with a special emphasis placed on identifying the range of variables which might have a significant influence on the tropospheric O3 budged in the Barrow region. The ABLE 3 campaigns took place in the summer since the summer is critical to an assessment of the full impact of accumulated winter/spring pollutant loadings. Observations in the summer months could also determine if significant long-range transport and injection of pollutants occur. ABLE 3A took place July-August 1988, and ABLE 3B took place July-August 1990. To accomplish its objectives, the ABLE 3 science team deployed the NASA Lockheed Electra aircraft on both sub-campaigns. With over 50 total flights, ABLE 3 aimed to utilize the Electra aircraft to take measurements of methane (CH4), carbon monoxide (CO), carbon dioxide (CO2), nonmethane hydrocarbons (NMHC), acetic acid (HA), formic acid (HFo), nitric oxide (NO), nitrogen dioxide (NO2), total “reactive” nitrogen gas (NOy), nitric acid (HNO3), peroxyacetyl nitrate (PAN), peroxypropionyl nitrate (PPN), ozone (O3), and aerosol chemical composition and size distribution. Onboard the Electra, airborne UV Differential Absorption Lidar (DIAL) provided remotely sense data on the two-dimensional distribution of aerosols and O3. The results of ABLE 3 indicate that atmospheric chemical changes in arctic and subarctic regions may serve as unique early warning indicators of global changes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;able-3b_ground_data&quot;&gt;ABLE-3B_Ground_Data&lt;/h4&gt;
ABLE-3B_Ground_Data is the ground site data collected during the Arctic Boundary Layer Expedition - 3B (ABLE-3B) suborbital campaign. Data from the High-Altitude Fast-Response CO2 Analyzer (Harvard CO2) instrument are featured in this collection. Data collection for this product is complete. From 1983-2001, NASA conducted a collection of field campaigns as part of the Global Tropospheric Experiment (GTE). Among those were the Arctic Boundary Layer Expedition (ABLE 3) campaigns. ABLE 3 was broken into two sub-campaigns: ABLE 3A and ABLE 3B. ABLE 3A took place in the Arctic and subarctic regions of North America and Greenland, while ABLE 3B took place in the north central and northeastern regions of Canada. ABLE 3 was focused on understanding the “early warning” response of the near-surface, organic, active layer to climate variability with a special emphasis placed on identifying the range of variables which might have a significant influence on the tropospheric O3 budged in the Barrow region. The ABLE 3 campaigns took place in the summer since the summer is critical to an assessment of the full impact of accumulated winter/spring pollutant loadings. Observations in the summer months could also determine if significant long-range transport and injection of pollutants occur. ABLE 3A took place July-August 1988, and ABLE 3B took place July-August 1990. To accomplish its objectives, the ABLE 3 science team deployed the NASA Lockheed Electra aircraft on both sub-campaigns. With over 50 total flights, ABLE 3 aimed to utilize the Electra aircraft to take measurements of methane (CH4), carbon monoxide (CO), carbon dioxide (CO2), nonmethane hydrocarbons (NMHC), acetic acid (HA), formic acid (HFo), nitric oxide (NO), nitrogen dioxide (NO2), total “reactive” nitrogen gas (NOy), nitric acid (HNO3), peroxyacetyl nitrate (PAN), peroxypropionyl nitrate (PPN), ozone (O3), and aerosol chemical composition and size distribution. Onboard the Electra, airborne UV Differential Absorption Lidar (DIAL) provided remotely sense data on the two-dimensional distribution of aerosols and O3. The results of ABLE 3 indicate that atmospheric chemical changes in arctic and subarctic regions may serve as unique early warning indicators of global changes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;able-3b_merge_data&quot;&gt;ABLE-3B_Merge_Data&lt;/h4&gt;
ABLE-3B_Merge_Data is the merge data collected onboard the NASA Electra aircraft during the Arctic Boundary Layer Expedition - 3B (ABLE-3B) suborbital campaign. Data collection for this product is complete. From 1983-2001, NASA conducted a collection of field campaigns as part of the Global Tropospheric Experiment (GTE). Among those were the Arctic Boundary Layer Expedition (ABLE 3) campaigns. ABLE 3 was broken into two sub-campaigns: ABLE 3A and ABLE 3B. ABLE 3A took place in the Arctic and subarctic regions of North America and Greenland, while ABLE 3B took place in the north central and northeastern regions of Canada. ABLE 3 was focused on understanding the “early warning” response of the near-surface, organic, active layer to climate variability with a special emphasis placed on identifying the range of variables which might have a significant influence on the tropospheric O3 budged in the Barrow region. The ABLE 3 campaigns took place in the summer since the summer is critical to an assessment of the full impact of accumulated winter/spring pollutant loadings. Observations in the summer months could also determine if significant long-range transport and injection of pollutants occur. ABLE 3A took place July-August 1988, and ABLE 3B took place July-August 1990. To accomplish its objectives, the ABLE 3 science team deployed the NASA Lockheed Electra aircraft on both sub-campaigns. With over 50 total flights, ABLE 3 aimed to utilize the Electra aircraft to take measurements of methane (CH4), carbon monoxide (CO), carbon dioxide (CO2), nonmethane hydrocarbons (NMHC), acetic acid (HA), formic acid (HFo), nitric oxide (NO), nitrogen dioxide (NO2), total “reactive” nitrogen gas (NOy), nitric acid (HNO3), peroxyacetyl nitrate (PAN), peroxypropionyl nitrate (PPN), ozone (O3), and aerosol chemical composition and size distribution. Onboard the Electra, airborne UV Differential Absorption Lidar (DIAL) provided remotely sense data on the two-dimensional distribution of aerosols and O3. The results of ABLE 3 indicate that atmospheric chemical changes in arctic and subarctic regions may serve as unique early warning indicators of global changes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;able-3b_trajectory_data&quot;&gt;ABLE-3B_Trajectory_Data&lt;/h4&gt;
ABLE-3B_Trajectory_Data is the trajectory data collected during the Arctic Boundary Layer Expedition - 3B (ABLE-3B) suborbital campaign. Data collection for this product is complete. From 1983-2001, NASA conducted a collection of field campaigns as part of the Global Tropospheric Experiment (GTE). Among those were the Arctic Boundary Layer Expedition (ABLE 3) campaigns. ABLE 3 was broken into two sub-campaigns: ABLE 3A and ABLE 3B. ABLE 3A took place in the Arctic and subarctic regions of North America and Greenland, while ABLE 3B took place in the north central and northeastern regions of Canada. ABLE 3 was focused on understanding the “early warning” response of the near-surface, organic, active layer to climate variability with a special emphasis placed on identifying the range of variables which might have a significant influence on the tropospheric O3 budged in the Barrow region. The ABLE 3 campaigns took place in the summer since the summer is critical to an assessment of the full impact of accumulated winter/spring pollutant loadings. Observations in the summer months could also determine if significant long-range transport and injection of pollutants occur. ABLE 3A took place July-August 1988, and ABLE 3B took place July-August 1990. To accomplish its objectives, the ABLE 3 science team deployed the NASA Lockheed Electra aircraft on both sub-campaigns. With over 50 total flights, ABLE 3 aimed to utilize the Electra aircraft to take measurements of methane (CH4), carbon monoxide (CO), carbon dioxide (CO2), nonmethane hydrocarbons (NMHC), acetic acid (HA), formic acid (HFo), nitric oxide (NO), nitrogen dioxide (NO2), total “reactive” nitrogen gas (NOy), nitric acid (HNO3), peroxyacetyl nitrate (PAN), peroxypropionyl nitrate (PPN), ozone (O3), and aerosol chemical composition and size distribution. Onboard the Electra, airborne UV Differential Absorption Lidar (DIAL) provided remotely sense data on the two-dimensional distribution of aerosols and O3. The results of ABLE 3 indicate that atmospheric chemical changes in arctic and subarctic regions may serve as unique early warning indicators of global changes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.asdc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA ABoVE Project</title>
      <link>https://registry.opendata.aws/nasa-above</link>
      <guid>https://registry.opendata.aws/nasa-above</guid>
      <description>This document presents the Concise Experiment Plan for NASA&amp;#39;s Arctic-Boreal Vulnerability Experiment (ABoVE) to serve as a guide to the Program as it identifies the research to be conducted under this study. Research for ABoVE will link field-based, process-level studies with geospatial data products derived from airborne and satellite remote sensing, providing a foundation for improving the analysis and modeling capabilities needed to understand and predict ecosystem responses and societal implications. The ABoVE Concise Experiment Plan (ACEP) outlines the conceptual basis for the Field Campaign and expresses the compelling rationale explaining the scientific and societal importance of the study. It presents both the science questions driving ABoVE research as well as the top-level requirements for a study design to address them.
&lt;br&gt;&lt;h4 id&#x3D;&quot;arctic_boreal_co2_flux_v2_2448&quot;&gt;Arctic_Boreal_CO2_Flux_V2_2448&lt;/h4&gt;
This dataset is a synthesis of terrestrial and freshwater CO2 and CH4 fluxes from the Arctic-Boreal region aggregated to monthly timesteps. The dataset, known as ABCFlux v2, includes 1,028 unique sites and spans 1984-2024 with the majority of observations occurring after 1999. ABCFlux v2 includes surface-atmosphere CO2 fluxes of net ecosystem exchange (NEE), gross primary production (GPP), and ecosystem respiration (Reco) alongside CH4 fluxes. For aquatic ecosystems, CH4 fluxes were split into diffusive and ebullitive flux pathways and included potential emissions from transient storage in the water column, alongside CO2 and CH4 concentrations dissolved in the surface water. Fluxes were measured through a variety of methods including chamber and eddy covariance techniques alongside bubble traps, ice-surveys, and concentration-based turbulence-driven modelling in aquatic ecosystems. Supporting variables include methodological metadata (e.g., gap-filling methods, number of chamber measurement days), environmental measurements (e.g., air, water, and soil temperatures), and site-level attributes (e.g., permafrost thaw status, disturbance history). Compared with version 1, this v2 dataset includes additional variables to represent detailed descriptions of plant functional types, deep soil temperatures (&amp;lt;10 cm), and permafrost thaw presence or absence in the top two meters. Data pertaining to CH4 fluxes were also added that were not included in previous version. The data are provided in comma separated values (CSV) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;abolvis1a&quot;&gt;ABOLVIS1A&lt;/h4&gt;
This data set contains geotagged images collected over Alaska and Western Canada. The images were taken by the NASA Digital Mapping Camera, paired with the Land, Vegetation, and Ice Sensor (LVIS), an airborne lidar scanning laser altimeter. The data were collected as part of NASA&amp;#39;s Terrestrial Ecology Program campaign, the Arctic-Boreal Vulnerability Experiment (ABoVE).
&lt;br&gt;&lt;h4 id&#x3D;&quot;ablvis1b&quot;&gt;ABLVIS1B&lt;/h4&gt;
This data set contains return energy waveform data over Alaska and Western Canada measured by the NASA Land, Vegetation, and Ice Sensor (LVIS), an airborne lidar scanning laser altimeter. The data were collected as part of NASA&amp;#39;s Terrestrial Ecology Program campaign, the Arctic-Boreal Vulnerability Experiment (ABoVE).
&lt;br&gt;&lt;h4 id&#x3D;&quot;ablvis2&quot;&gt;ABLVIS2&lt;/h4&gt;
This data set contains surface elevation data over Alaska and Western Canada measured by the NASA Land, Vegetation, and Ice Sensor (LVIS), an airborne lidar scanning laser altimeter. The data were collected as part of NASA&amp;#39;s Terrestrial Ecology Program campaign, the Arctic-Boreal Vulnerability Experiment (ABoVE).
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_ascends_xco2_2050&quot;&gt;ABoVE_ASCENDS_XCO2_2050&lt;/h4&gt;
This dataset provides in situ airborne measurements of atmospheric carbon dioxide (CO2), methane (CH4), and water vapor concentrations, plus air temperature, pressure, relative humidity, and wind speed values over Alaska and the Yukon and Northwest Territories of Canada during 2017-07-20 to 2017-08-08. Measurements were taken onboard a DC-8 aircraft during this Active Sensing of CO2 Emissions over Nights, Days and Seasons (ASCENDS) airborne deployment over portions of the Arctic-Boreal Vulnerability Experiment (ABoVE) domain. CO2 and CH4 were measured with NASA&amp;#39;s Atmospheric Vertical Observations of CO2 in the Earth&amp;#39;s Troposphere (AVOCET) instrument. Water vapor and relative humidity were measured with Diode Laser Hydrometer. Measurements of column-averaged dry-air mixing ratio CO2 measurements (XCO2) were taken with the CO2 Sounder Lidar instrument. The airborne CO2 Sounder is a pulsed, multi-wavelength Integrated Path Differential Absorption lidar. It estimates XCO2 in the nadir path from the aircraft to the scattering surface by measuring the shape of the 1572.33 nm CO2 absorption line. The data were collected in order to capture the spatial and temporal dynamics of the northern high latitude carbon cycle as part of ABoVE and are provided in ICARTT file format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_ascends_backscatter_2051&quot;&gt;ABoVE_ASCENDS_Backscatter_2051&lt;/h4&gt;
This dataset provides atmospheric backscattering coefficient profiles collected during Active Sensing of CO2 Emissions over Nights, Days, and Seasons (ASCENDS) deployments from 2017-07-20 to 2017-08-08 over Alaska, U.S., and the Yukon and Northwest Territories of Canada. These profiles were measured by the CO2 Sounder Lidar instrument carried on a DC-8 aircraft. The airborne CO2 Sounder is a pulsed, multi-wavelength Integrated Path Differential Absorption lidar that estimates column-averaged dry-air CO2 mixing ratio (XCO2) in the nadir path from the aircraft to the scattering surface. In addition to XCO2, the lidar receiver recorded the time-resolved atmospheric backscatter signal strength as the laser pulses propagated through the atmosphere. Raw lidar data were converted to the atmospheric backscatter cross-section product and the two-way atmosphere transmission, also known as attenuated backscatter profiles. These ASCENDS flights were coordinated with the 2017 Arctic-Boreal Vulnerability Experiment (ABoVE) campaign and are provided in ICARTT format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_ascends_merge_2114&quot;&gt;ABoVE_ASCENDS_Merge_2114&lt;/h4&gt;
This dataset provides in situ airborne measurements of atmospheric carbon dioxide (CO2), methane (CH4), water vapor concentrations, air temperature, pressure, and wind speed and direction as well as airborne remote sensing measurements of column average CO2 collected during Active Sensing of CO2 Emissions over Nights, Days, and Seasons (ASCENDS) deployments from 2017-07-20 to 2017-08-08 over Alaska, US, and the Yukon and Northwest Territories of Canada. CO2 and CH4 were measured with NASA&amp;#39;s Atmospheric Vertical Observations of CO2 in the Earth&amp;#39;s Troposphere (AVOCET) instrument. Water vapor and relative humidity were measured with Diode Laser Hydrometer. Measurements were taken onboard a DC-8 aircraft. The ASCENDS flights were coordinated with the 2017 Arctic-Boreal Vulnerability Experiment (ABoVE) campaign. The data are provided in ICARTT format along with an archive of flight videos.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_pband_sar_1657&quot;&gt;ABoVE_PBand_SAR_1657&lt;/h4&gt;
This dataset provides estimates of soil geophysical properties derived from Airborne Microwave Observatory of Subcanopy and Subsurface (AirMOSS) P-band polarimetric synthetic aperture radar (PolSAR) data collected in August and October of 2014, 2015, and 2017 over 12 study sites (with some exceptions) across Northern Alaska. Soil properties reported include the active layer thickness (ALT), dielectric constant, soil moisture profile, surface roughness, and their respective uncertainty estimates at 30-m spatial resolution over the 12 flight transects. Most of the study sites are located within the continuous permafrost zone and where the aboveground vegetation consisting mainly of dwarf shrub and tussock/sedge/moss tundra has a minimal impact on P-band radar backscatter.
&lt;br&gt;&lt;h4 id&#x3D;&quot;soil_activelayer_properties_ak_2315&quot;&gt;Soil_ActiveLayer_Properties_AK_2315&lt;/h4&gt;
This dataset provides soil active layer characteristics from nine locations across Alaska. Soil samples were collected in 2016 except for one site which was sampled in 2018. Soil cores were collected from each site using a steel barrel and plastic sample tube attached to a hand drill. At the majority of sites, samples were taken from each end of three 30-m transects (i.e. samples collected at the 0 m and 30 m location of each transect). The entire thawed horizon (active layer) was sampled where possible, and the length of cores varies among sites. Cores were kept frozen until analysis in the lab. Samples were sectioned by horizon (organic and mineral), and the organic horizon was split into subsections so that no section was longer than approximately 10 cm. Coarse roots were removed, dried and weighed. Soils were measured for gravimetric water content, percent soil organic matter (SOM), pH, and bulk density. Locations were selected to investigate fire disturbance, to span the range of permafrost regions from continuous to sporadic, and to cover vegetation types from boreal forests, tussock tundra, upland willow/herbaceous scrub, and lowland fen and wet tundra sites across Alaska. The data are provided in comma-separated values (CSV) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;permafrost_activelayer_nslope_1759&quot;&gt;Permafrost_ActiveLayer_NSlope_1759&lt;/h4&gt;
This dataset provides in situ soil measurements including soil dielectric properties, temperature, and moisture profiles, active layer thickness (ALT), and measurements of soil organic matter, bulk density, porosity, texture, and coarse root biomass. Samples were collected from the surface to permafrost table in soil pits at selected sites along the Dalton Highway in Northern Alaska. From North to South, the study sites include Franklin Bluffs, Sagwon, Happy Valley, Ice Cut, and Imnavait Creek. Measurements were made from August 22 to August 26, 2018. The purpose of the field campaign was to characterize the dielectric properties of permafrost active layer soils in support of the NASA Arctic and Boreal Vulnerability Experiment (ABoVE) Airborne Campaign.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_resalt_insar_polsar_v3_2004&quot;&gt;ABoVE_ReSALT_InSAR_PolSAR_V3_2004&lt;/h4&gt;
This dataset provides estimates of seasonal subsidence, active layer thickness (ALT), the vertical soil moisture profile, and uncertainties at a 30 m resolution for 51 sites across the ABoVE domain, including 39 sites in Alaska and 12 sites in Northwest Canada. The ALT and soil moisture profile retrievals simultaneously use L- and P-band synthetic aperture radar (SAR) data acquired by the NASA/JPL Uninhabited Aerial Vehicle Synthetic Aperture Radar (UAVSAR) instruments during the 2017 Arctic Boreal Vulnerability Experiment (ABoVE) airborne campaign. The data are provided in NetCDF Version 4 format along with a python script for estimating soil volumetric water content from data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sat_activelayer_thickness_maps_1760&quot;&gt;Sat_ActiveLayer_Thickness_Maps_1760&lt;/h4&gt;
This dataset provides annual estimates of active layer thickness (ALT) at 1 km resolution across Alaska from 2001-2015. The ALT was estimated using a remote sensing-based soil process model incorporating global satellite data from Moderate Resolution Imaging Spectroradiometer (MODIS) land surface temperature (LST) and snow cover extent (SCE), and Soil Moisture Active and Passive (SMAP) satellite soil moisture records. The study area covers the majority land area of Alaska except for areas of perennial ice/snow cover or open water. The ALT was defined as the maximum soil thawing depth throughout the year. The mean ALT and mean uncertainty from 2001 to 2015 are also provided.
&lt;br&gt;&lt;h4 id&#x3D;&quot;photos_thermokarstlakes_ak_1845&quot;&gt;Photos_ThermokarstLakes_AK_1845&lt;/h4&gt;
This dataset includes high resolution orthophotographs of 21 lakes in the region of Fairbanks, Alaska, USA. Aerial photographs were taken on October 8, 2014, three days after lake-ice formation. These photographs were used to identify open holes in lake ice that indicate the location of hotspot seeps associated with the releases of methane from thawing permafrost. Aerial photography can be used to measure changes in lake areas and to observe patterns in the formation of lake ice and other early winter lake conditions.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_open_water_map_1643&quot;&gt;ABoVE_Open_Water_Map_1643&lt;/h4&gt;
This dataset contains georeferenced three-band orthomosaics of green, red, and near-infrared (NIR) digital imagery at 1m resolution collected over selected surface waters across Alaska and Canada between July 9 and August 17, 2017. The orthomosaics were generated from individual images collected by a Cirrus Designs Digital Camera System (DCS) mounted on a Beechcraft Super King Air B200 aircraft from approximately 8-11 km altitude. Flights were over the following areas: Saskatchewan River, Saskatoon, Inuvik, Yukon River including Yukon Flats, Sagavanirktok River, Arctic Coastal Plain, Old Crow Flats, Peace-Athabasca Delta, Slave River, Athabasca River, Yellowknife, Great Slave Lake, Mackenzie River and Delta, Daring Lake, and other selected locations. Most locations were imaged twice during two flight campaigns in Canada and Alaska extending roughly SE-NW then NW-SE up to a month apart. The data were georeferenced using 303 ground control points (GCPs) across the study region.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_airswot_radar_data_1646&quot;&gt;ABoVE_AirSWOT_Radar_Data_1646&lt;/h4&gt;
This dataset provides AirSWOT (Surface Water and Ocean Topography) Ka-band (35.75 GHz) radar data products collected from an airborne platform over parts of Alaska and Canada during the period 2017-07-09 to 2017-08-17. Flights targeted specific surface water features, including rivers, lakes, ponds, and wetlands in the ABoVE domain. The radar data include six products: elevation (above the WGS84 ellipsoid), incidence angle, magnitude (backscatter), interferometric correlation (coherence), DHDPHI (incidence angle dependent height sensitivity), and error (estimated height random error, 1-sigma standard deviation). The flight lines were selected to span a full spectrum of permafrost conditions (permafrost-free to continuous permafrost, low to high ground ice content), ecosystems, climatic regions, topographic relief, and geological substrates across the ABoVE domain to investigate surface water responses to thawing permafrost and spatial and temporal variability in terrestrial water storage by measuring elevation and extent of surface waters. The data are provided in two forms: 1) the original output (outer-swath products only) at 3.6 m2 resolution in UTM coordinates from the AirSWOT processing group at the Jet Propulsion Laboratory (JPL), and 2) the ABoVE Projection at 3.6 m2 resolution, clipped to the ABoVE reference grid tiles using the C grid.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airswot_orthomosaic_watermask_1655&quot;&gt;AirSWOT_Orthomosaic_WaterMask_1655&lt;/h4&gt;
This dataset provides NASA AirSWOT Ka-band (35.75 GHz) radar interferometry data products for water surface elevation (WSE), a derived color-infrared (CIR) digital image orthomosaic, and derived lake/wetland and river channel water masks at 3.6 x 3.6 m resolution for a study area of ~3,300 km2 in the Yukon Flats Basin (YFB) in eastern interior Alaska. The data were collected during a flight over the region on June 15, 2015.These data were collected to validate AirSWOT WSE mappings and to improve the understanding of surface water flow through complex Arctic-Boreal wetland systems.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_airswot_water_mask_1707&quot;&gt;ABoVE_AirSWOT_Water_Mask_1707&lt;/h4&gt;
This dataset provides 1) a conservative open water mask for future water surface elevation (WSE) extraction from the co-registered AirSWOT Ka-band interferometry data, and 2) high-resolution (1 m) water body distribution maps for water bodies greater than 40 m2 along the NASA Arctic-Boreal Vulnerability Experiment (ABoVE) foundational flight lines. The masks and maps were derived from georeferenced three-band orthomosaics generated from individual images collected during the flights and a semi-automated water classification algorithm based on the Normalized Difference Water Index (NDWI). In total, 3,167 km2 of open water were mapped from 23,380 km2 of flight lines spanning 23 degrees of latitude. Detected water body sizes range from 40 m2 to 15 km2. The image tiles were georeferenced using manually selected ground control points (GCPs). Comparison with manually digitized open water boundaries yields an overall open-water classification accuracy of 98.0%.
&lt;br&gt;&lt;h4 id&#x3D;&quot;alaska_lake_pond_occurrence_2399&quot;&gt;Alaska_Lake_Pond_Occurrence_2399&lt;/h4&gt;
The Alaska Lake and Pond Occurrence Dataset (ALPOD) is a spatially explicit map of lakes and ponds across Alaska and their seasonal fluctuations. The core product is an open water occurrence raster that: (a) separates lakes and ponds from other components of the landscape (e.g., rivers and wetlands); (b) is built from Sentinel-2 imagery and has 10-m resolution; and (c) records the percentages of time that each pixel was open water and attached to a lake or pond during the 2016-2021 ice-free seasons at near-daily temporal resolution. The number of water bodies depends on the chosen occurrence threshold, but a conservative estimate is that ALPOD maps over 800,000 lakes and ponds larger than 0.001 km2. The lake occurrence rasters are tiled by UTM zone and latitude. ALPOD also includes a vector product defined using a 25% occurrence threshold. ALPOD was created using a U-Net lake identification model and manual inspection to produce a maximum possible lake extent mask. This mask serves as the region of interest for an adaptive NDWI threshold water classification algorithm written in Google Earth Engine (GEE), which was used to classify open water within the maximum lake mask in every available cloud- and ice-free Sentinel-2 image during the study period. ALPOD is suitable for investigations of individual water bodies as well as lake and pond patterns across Alaska. The data are provided in GeoTIFF and shapefile formats.
&lt;br&gt;&lt;h4 id&#x3D;&quot;alder_shrub_soil_alaska_v2_2300&quot;&gt;Alder_Shrub_Soil_Alaska_V2_2300&lt;/h4&gt;
This dataset holds measures of vegetative cover and soil characteristics for sites in interior Alaska, U.S., along the James W. Dalton Highway (Alaska Route 11). The field data were collected during August in 2018 and 2019 to study the expansion of shrub cover, particularly alders (Alnus spp.) in tundra ecosystems and the potential impact of shrubs on soil properties. Samples were measured along transects at 5- to 10-m intervals. Soil samples were collected and analyzed in the laboratory. Vegetation variables include percent cover of mosses, lichens, graminoid species, shrubs, alder, birch (Betula spp.), and willow (Salix spp.) along with the biomass, size, and age structure of alder. An allometric model to estimate alder biomass was developed. Soil metrics include moisture content, conductivity, bulk density, carbon and nitrogen content and isotope ratios. The data include the maximum annual Normalized Difference Vegetation Index (NDVI) for 2019 and the trend in maximum NDVI for 2000-2020. This is version 2 of this dataset.The data are provided in comma-separated values (CSV) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_modis_maiac_reflectance_1858&quot;&gt;ABoVE_MODIS_MAIAC_Reflectance_1858&lt;/h4&gt;
This dataset provides angular corrections of MODIS Multi-Angle Implementation of Atmospheric Correction algorithm (MAIAC) surface reflectances across the ABoVE domain in Alaska and western Canada from 2000 to 2017. Using random forests (RF), a machine-learning approach, the original MAIAC reflectance data were corrected to consistent view and illumination angles (0 degree view zenith angle and 45 degree of sun zenith angle) to reduce artifacts and variability due to angular effects. The original MAIAC data&amp;#39;s sub-daily temporal resolution and 1 km spatial resolution with seven land bands (bands 1-7) and five ocean bands (bands 8-12) were preserved. The resulting surface reflectance data are suitable for long-term studies on patterns, processes, and dynamics of surface phenomena. The data cover 11 different Terra and Aqua satellite MODIS MAIAC tiles.
&lt;br&gt;&lt;h4 id&#x3D;&quot;annual_30m_agb_1808&quot;&gt;Annual_30m_AGB_1808&lt;/h4&gt;
This dataset provides estimated annual aboveground biomass (AGB) density for live woody (tree and shrub) species and corresponding standard errors at a 30 m spatial resolution for the boreal forest biome portion of the Core Study Domain of NASA&amp;#39;s Arctic-Boreal Vulnerability Experiment (ABoVE) Project (Alaska and Canada) over the time period 1984-2014. The data were derived from a time series of Landsat-5 and Landsat-7 surface reflectance imagery and full-waveform lidar returns from the Geoscience Laser Altimeter System (GLAS) flown onboard IceSAT from 2004 to 2008. The Change Detection and Classification (CCDC) model-fitting algorithm was used to estimate the seasonal variability in surface reflectance, and AGB density data were produced by applying allometric equations to the GLAS lidar data. A Gradient Boosted Machines machine learning algorithm was used to predict annual AGB density across the study domain given the seasonal variability in surface reflectance and other predictors. The data received statistical smoothing to reduce noise and uncertainty was estimated at the pixel level. These data contribute to the characterization of how biomass stocks are responding to climate and disturbance in boreal forests.
&lt;br&gt;&lt;h4 id&#x3D;&quot;annual_seasonality_greenness_1698&quot;&gt;Annual_Seasonality_Greenness_1698&lt;/h4&gt;
This dataset provides annual maps of the timing of spring onset with leaf emergence, of autumn onset with leaf senescence, and of peak greenness for each 30 m pixel derived from Landsat time series of Thematic Mapper (TM) and Enhanced Thematic Mapper (ETM+) observations from 1984 to 2014. The ABoVE core domain includes 169 ABoVE grid tiles across Alaska, USA and Alberta, British Columbia, Northwest Territories, Nunavut, Saskatchewan, and Yukon, Canada. The data provided for deriving seasonality includes the total number of cloud-free observations, r-squared values between observed and spline-predicted Enhanced Vegetation Index (EVI), long-term average minimum EVI, long-term average maximum EVI, long-term average spring onset, long-term average autumn onset, annual spring onset, and annual autumn onset. The data provided for peak greenness includes annual peak Normalized Difference Vegetation Index (NDVI), Normalized Burn Ratio (NBR), annual composite red reflectance, annual composite NIR reflectance, annual composite shortwave infrared reflectance (band 6, SWIR1), annual composite shortwave infrared reflectance (band 7, SWIR2), number of dates used to calculate composites, and day of year of associated maximum composite.
&lt;br&gt;&lt;h4 id&#x3D;&quot;annual_thaw_slump_1724&quot;&gt;Annual_Thaw_Slump_1724&lt;/h4&gt;
This dataset provides a time series of spatial data showing the expansion of a thaw slump on the East Fork Chandalar River near the community of Venetie, Alaska, from 2008 through 2017. The erosion of vegetated areas along the river was documented by manually digitizing imagery from ESRI basemaps and Landsat 5 (TM), 7 (ETM+), and 8 (OLI), using the band combination of shortwave infrared 2, shortwave infrared 1, and red.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_atmospheric_flask_data_1717&quot;&gt;ABoVE_Atmospheric_Flask_Data_1717&lt;/h4&gt;
This dataset provides atmospheric carbon dioxide (CO2), methane (CH4), carbon monoxide (CO), molecular hydrogen (H2), nitrous oxide (N2O), sulfur hexafluoride (SF6), and other trace gas mole fractions (i.e. &amp;quot;concentrations&amp;quot;) from flights over Alaska and the Yukon and Northwest Territories of Canada during the Arctic Carbon Aircraft Profile (Arctic-CAP) monthly sampling campaigns from April-November 2017. The data were derived from laboratory measurements of whole air samples collected by Programmable Flask Packages (PFP) onboard the aircraft. During each of the six monthly campaigns, flights over the Arctic-Boreal Vulnerability Experiment (ABoVE) domain included 25 vertical profiles, from the surface up to 6 km altitude, at locations selected to complement regular long-term vertical profiles, remote sensing data, and ground-based flux tower measurements. Measurements were initiated by the aircraft pilot at predetermined locations within each profile in order to evenly distribute flask sampling points throughout each flight. A total of 408 flask samples were collected during 55 individual flights. The measurements included in this data set are crucial for understanding changes in Arctic carbon cycling and the potential threats posed by thawing of Arctic permafrost.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_arctic_cap_1658&quot;&gt;ABoVE_Arctic_CAP_1658&lt;/h4&gt;
This dataset provides in situ airborne measurements of atmospheric carbon monoxide (CO), carbon dioxide (CO2), methane (CH4), and water vapor concentrations, plus air temperature, pressure, relative humidity, and wind speed values over Alaska and the Yukon and Northwest Territories of Canada during the Arctic Carbon Aircraft Profile (Arctic-CAP) monthly sampling campaigns from April-November 2017. Observations have been averaged to a 10-second interval and are reported with the number of samples (N) and standard deviation. During each of the six monthly campaigns, flights over the Arctic-Boreal Vulnerability Experiment (ABoVE) domain included 25 vertical profiles, from the surface up to 6 km altitude, at locations selected to complement regular long-term vertical profiles, remote sensing data, and ground-based flux tower measurements.
&lt;br&gt;&lt;h4 id&#x3D;&quot;avhrr_fire_products_1545&quot;&gt;AVHRR_Fire_Products_1545&lt;/h4&gt;
This dataset provides annual forest fire burned area and daily hotspot products developed using data acquired from the Advanced Very-High-Resolution Radiometer (AVHRR) instruments carried aboard two NOAA polar-orbiting satellites (NOAA-11 and NOAA-14). The fire products were generated over 12 fire seasons (1st May - 31st October) from 1989-2000 across North America at 1-km resolution and subset to the ABoVE spatial domain of Alaska and Canada.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_airborne_av3_v1_2388&quot;&gt;ABoVE_Airborne_AV3_V1_2388&lt;/h4&gt;
This dataset includes L1B radiance and L2A surface reflectance imagery acquired by the Airborne Visible / Infrared Imaging Spectrometer-3 (AVIRIS-3) instrument over portions of Alaska and northwestern Canada in 2023. These data were collected for the Arctic-Boreal Vulnerability Experiment (ABoVE) project. NASA&amp;#39;s AVIRIS-3 is a spectral mapping system that measures reflected radiance at 7.4-nm intervals in the Visible to Shortwave Infrared (VSWIR) spectral range from 390-2500 nm. The AVIRIS-3 sensor has a 40 degree instantaneous field of view with 1234 pixels, providing altitude dependent ground sampling distances from 12 m to sub meter range. This dataset represents one part of a multi-sensor airborne sampling campaign conducted by eleven different aircraft teams for ABoVE. The imagery data are provided in ENVI format along with a GeoJSON showing imagery boundaries. These data were specifically processed for the ABoVE project.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_airborne_aviris_ng_v3_2362&quot;&gt;ABoVE_Airborne_AVIRIS_NG_V3_2362&lt;/h4&gt;
This dataset supersedes the previously published ABoVE AVIRIS-NG Level 2 surface reflectance files for 2017-2019 surveys of Alaska and northwestern Canada. It also includes previously unpublished L1 radiance and L2 reflectance for the 2021 surveys in Iceland when COVID-era policies prevented normal ABoVE flights, and the 2022 surveys, which returned to the ABoVE domain. The dataset comprises ~1700 individual flight lines covering ~120,000 km2 with a nominal spatial resolution of 5 m. Sampling includes individual transects to capture key gradients like the tundra-taiga ecotone and raster maps of key study areas like the CHARS Greiner watershed, the Mackenzie Delta, and the Utqiagvik/Point Barrow area. AVIRIS-NG measures reflected radiance in 425 bands at 5-nanometer (nm) intervals in the visible to shortwave infrared spectral range between 380 and 2510 nm. Measurements were radiometrically and geometrically calibrated. This dataset represents one part of a multi-sensor airborne sampling campaign conducted by eleven different aircraft teams for ABoVE. The imagery data are provided in ENVI format along with a RGB composite image for each flight line and shapefiles showing imagery boundaries.
&lt;br&gt;&lt;h4 id&#x3D;&quot;imerg_precip_canada_alaska_2097&quot;&gt;IMERG_Precip_Canada_Alaska_2097&lt;/h4&gt;
This dataset is a modification to the Integrated Multi-satellitE Retrievals for GPM (IMERG) Final Run microwave-only, daily precipitation Version 06 data. It provides bias-corrected IMERG monthly precipitation data for Alaska and Canada from June 2000 through December 2020 in Cloud-Optimized GeoTIFF (.tif) format. Data are provided in the units of mm/day. NASA&amp;#39;s IMERG data product is one of the most advanced satellite precipitation products with a 0.1-degree spatial resolution and near global coverage. This dataset bias-corrected IMERG&amp;#39;s HQprecipitation precipitation estimates, which are based on passive microwave (PMW)-only retrievals, using a linear regression method. This method utilizes empirical measurements from rain gauge stations from the Global Historical Climatology Network (GHCN) and a digital elevation model. This bias correction approach improves estimates at elevations above 500 m a.s.l., which are typically underestimated.
&lt;br&gt;&lt;h4 id&#x3D;&quot;boreal_forest_survey_fairbanks_2390&quot;&gt;Boreal_Forest_Survey_Fairbanks_2390&lt;/h4&gt;
This dataset includes five metrics of forest resilience (recruitment, invasives, permafrost change, tree damage, and radial growth) at five recently burned forest sites (2010-2019) near Fairbanks, Alaska. The sites were imaged by the Airborne Visible InfraRed Imaging Spectrometer (AVIRIS-NG) in 2017 and 2022 during the Arctic-Boreal Vulnerability Experiment (ABoVE). Field measurements were conducted in 2021. Random forest (RF) vegetation classification models constructed from key hyperspectral bands were validated with ground-truthing (GT) of 44 measured plots and 45 geotagged plots. GT included stem densities, understory cover, soil characteristics, radial growth of 51 spruce trees from cores, and visual damage assays of 668 conifers and deciduous trees. There are 10 data files in comma-separated values format (CSV) in this dataset.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nwt_burn_severity_maps_1694&quot;&gt;NWT_Burn_Severity_Maps_1694&lt;/h4&gt;
This dataset provides maps at 30-m resolution of landscape surface burn severity (surface litter and soil organic layers) from the 2014-2015 fires in the Northwest Territories and Northern Alberta, Canada. The maps were derived from Landsat 8 Operational Land Imager/Thermal Infrared Sensor (OLI/TIRS) imagery and two separate multiple linear regression models trained with field data; one for the Plains and a second for the Shield ecoregion. Field observations were used to estimate area burned in each of five severity classes (unburned, singed, light, moderate, severely burned) in six stratified randomly selected plots of 10 x 10-m in size across a 1-ha site. Using this five class scale a burn severity index (BSI) for each 1-ha site was calculated using multiple weighted and averaged field parameters. Pre- and post-fire phenologically paired Landsat 8 images were used to model the five discrete severity classes using midpoints as breaks.
&lt;br&gt;&lt;h4 id&#x3D;&quot;wildfires_nwt_canada_1548&quot;&gt;Wildfires_NWT_Canada_1548&lt;/h4&gt;
This data set provides a fire progression map for year 2015 and measures of burn severity and vegetation community biophysical data collected from areas that were burned by wildfires in 2014 and 2015 in the Northwest Territories, Canada. Field data collected in 2016 include an estimate of burn severity, woody seedling/sprouting data, soil moisture, peat depth, thaw depth, and vegetation cover for selected sites.
&lt;br&gt;&lt;h4 id&#x3D;&quot;wildfires_2014_nwt_canada_1307&quot;&gt;Wildfires_2014_NWT_Canada_1307&lt;/h4&gt;
This data set provides peatland landcover classification maps, fire progression maps, and vegetation community biophysical data collected from areas that were burned by wildfire in 2014 in the Northwest Territories, Canada. The peatland maps include peatland type (bog, fen, marsh, swamp) and level of biomass (open, forested). The fire progression maps enabled an assessment of wildfire progression rates at a daily time scale. Field data, collected in 2015, include an estimate of burn severity, woody seedling/sprouting data, soil moisture, and tree diameter and height of burned sites and similar vegetation characterization at landcover validation sites.
&lt;br&gt;&lt;h4 id&#x3D;&quot;burned_area_depth_ak_ca_2063&quot;&gt;Burned_Area_Depth_AK_CA_2063&lt;/h4&gt;
This dataset provides annual gridded estimates of fire locations and associated burn fraction per pixel for Alaska and Canada at approximately 500 m spatial resolution for the period 2001-2019. Gridded predictions of carbon combustion and burn depth for the same period within the ABoVE extended domain using the burn area maps and field data are also available. Fire locations and date of burn (DOB) were detected by MODIS-derived active fire products. Burned area was primarily estimated from finer-scale Landsat imagery using a differenced Normalized Burn Ratio (dNBR) algorithm and upscaled to an approximate 500 m MODIS resolution. Aboveground combustion, belowground combustion, and burn depth were statistically modeled at the pixel level for every mapped burned pixel in the ABoVE extended domain based on field observations across Alaska and western Canada. Predictor variables included remotely sensed indicators of fire severity, topography, soils, climate, and fire weather. Quality flags for burned area and combustion are available. Fire is the dominant disturbance agent in Alaskan and Canadian boreal ecosystems and releases large amounts of carbon into the atmosphere. These data are useful for studies of disturbance, fire ecology, and carbon cycling in boreal ecosystems.
&lt;br&gt;&lt;h4 id&#x3D;&quot;southern_boreal_plot_attribute_1740&quot;&gt;Southern_Boreal_Plot_Attribute_1740&lt;/h4&gt;
This dataset provides the results of field measurements and estimates of carbon stocks and combustion rates that characterize burned and unburned southern boreal forest stands near the La Ronge and Weyakwin communities in central Saskatchewan (SK), Canada. Measurements were completed in 2016 at 47 stands that burned in the 2015 Saskatchewan wildfires (Egg, Philion, and Brady) and at 32 unburned stands in comparable adjacent areas. Stands were characterized through field observations and sampling of the vegetative community (i.e., tree species, abundance, and biophysical measurements, stand age, coarse woody debris, history of fires or logging), soils (i.e., soil moisture class, unburned and burned soil organic layer depth, samples for bulk density and carbon analyses), and basic landscape geophysical traits. From these results, the pre-fire carbon stocks and carbon combustion values from both the above- and below-ground pools were estimated using a combination of linear and mixed-effects modeling and were calibrated against carbons stocks from the unburned stands. Estimates of uncertainty were generated for above- and below-ground carbon stocks and combustion values using a Monte Carlo framework paired with classic uncertainty propagation techniques.
&lt;br&gt;&lt;h4 id&#x3D;&quot;wildfire_effects_spruce_field_1595&quot;&gt;Wildfire_Effects_Spruce_Field_1595&lt;/h4&gt;
This dataset provides the results of field observations of soil characteristics and depth to permafrost, survey results for Composite Burn Index (CBI) determination, and Landsat-derived estimates of Relative Difference Normalized Burn Ratio (RdNBR) for 38 burned and unburned forest sites near Tanana, Alaska in 2017. Forests in the study area, at the confluence of the Yukon and Tanana Rivers about 200 km west of Fairbanks, are predominately black spruce on wetter soils and white spruce on drier soils. The burned areas were from wildfires that occurred in the summer of 2015.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_soil_radiocarbon_nwt_1664&quot;&gt;ABoVE_Soil_Radiocarbon_NWT_1664&lt;/h4&gt;
This dataset provides field data from boreal forests in the Northwest Territories (NWT), Canada, that were burned by wildfires in 2014. During fieldwork in 2015, 211 burned plots were established. From these plots, thirty-two forest plots were selected that were dominated by black spruce and were representative of the full moisture gradient across the landscape, ranging from xeric to sub-hygric. Plot observations included slope, aspect, and moisture. At each plot, one intact organic soil profile associated with a specific burn depth was selected and analyzed for carbon content and radiocarbon (14C) values at specific profile depth increments to assess legacy carbon presence and combustion. Vegetation observations included tree density. Stand age at the time of the fire was determined from tree-ring counts. Estimates of pre-fire below and aboveground carbon pools were derived. The percent of total NWT wildfire burned area comprising of &amp;quot;young&amp;quot; stands (less than 60 years old at time of fire) was estimated.
&lt;br&gt;&lt;h4 id&#x3D;&quot;seasonality_tundra_vegetation_1606&quot;&gt;Seasonality_Tundra_Vegetation_1606&lt;/h4&gt;
This dataset provides a summary of potential climate drivers of Arctic tundra vegetation productivity that have been compiled for growing seasons from 1982 to 2015. The scale of interest is the entire pan-arctic non-alpine tundra and the continental subdivisions of the North American and the Eurasian Arctic North of 70 degrees. These climate drivers include (1) maximum normalized difference vegetation index (MaxNDVI) and time-integrated NDVI (TI-NDVI), (2) summer sea ice concentrations, (3) oceanic heat content, (4) land surface temperature, and (5) summer warmth index (SWI). Data are provided variously as timeseries and weekly and bi-weekly averages over selected time ranges and study regions with calculated trends and trend significance. Data collected over 33 years were compiled to observe seasonal trends of vegetation productivity and to detect dynamics between arctic vegetation and climate drivers.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ak_north_slope_nee_ch4_flux_1562&quot;&gt;AK_North_Slope_NEE_CH4_Flux_1562&lt;/h4&gt;
This dataset provides CO2 and CH4 fluxes and meteorological parameters from five eddy covariance (EC) tower sites located at Barrow (three sites), Atqasuk (ATQ) and Ivotuk (IVO), Alaska. These locations form a 300-km north-south transect across Alaska&amp;#39;s North Slope. Flux measurements include CO2, CH4, and H2O fluxes plus sensible and latent heat fluxes. Meteorological data include air temperature, wind speed, rain, soil temperature, PAR, radiation, soil water content, RH, ground heat fluxes, and air pressure. All data are reported at half-hourly intervals and cover the period 2015-01-01 to 2017-03-09.
&lt;br&gt;&lt;h4 id&#x3D;&quot;modis_maiac_reflectance_1700&quot;&gt;MODIS_MAIAC_Reflectance_1700&lt;/h4&gt;
This dataset provides angular corrections of MODIS Multi-Angle Implementation of Atmospheric Correction algorithm (MAIAC) surface reflectances by two methods at each of 62 flux tower sites (1 km x 1 km area) across the ABoVE domain in Alaska and western Canada from 2000 to 2015/2016. The original MAIAC reflectance data were corrected to consistent view and illumination angles (0 degree view zenith angle and 45 degree of sun zenith angle) using two independent algorithms: the first based on the original BRDF (Bidirectional Reflectance Distribution Function) parameters provided by the MAIAC team, and the second based on a machine learning approach (random forests). The corrected data preserve the original MAIAC data&amp;#39;s sub-daily temporal resolution and 1 km spatial resolution with seven land bands (bands 1-7) and five ocean bands (bands 8-12). The resulting tower site sub-daily timeseries of angular corrected surface reflectances are suitable for long-term studies on patterns, processes, and dynamics of surface phenomena.
&lt;br&gt;&lt;h4 id&#x3D;&quot;dall_sheep_population_dynamics_1640&quot;&gt;Dall_Sheep_Population_Dynamics_1640&lt;/h4&gt;
This dataset contains estimated annual average Dall sheep (Ovis dalli dalli) lamb-to-ewe ratios for each year from 2000-2015 across the full species range in Alaska and Northwestern Canada. Sheep population data are from surveys conducted over the 14 major mountain ranges encompassing the range of Dall sheep. For this study, the mountain ranges were divided into 24 mountain units due to differing climate gradients. Estimated covariate environmental and climate data used to examine the relationship between environmental conditions and Dall sheep population performance (per mountain unit) are also provided and include precipitation, temperature, snow cover, elevation, and distance to the center of the range.
&lt;br&gt;&lt;h4 id&#x3D;&quot;dall_sheep_snowpack_1602&quot;&gt;Dall_Sheep_Snowpack_1602&lt;/h4&gt;
This dataset provides daily estimates of snow depth and snow density for the study area in Lake Clark National Park and Preserve (LCNPP), Alaska. The data were generated using SnowModel and used as snow covariates along with landscape covariates in modeling efforts to study Dall sheep movements in response to dynamic snow conditions. Thirty adult Dall sheep (12 male, 18 female) were captured and outfitted with global positioning system (GPS) collars programmed to acquire locations every seven hours. Given the individual sheep locations, their distances to land cover (e.g., shrub, forest, glacier), landscape characteristics (e.g., elevation, terrain ruggedness index (TRI), vector ruggedness measure (VRM), slope, and aspect), snow depth and density, MODIS normalized difference snow index (NDSI), and other covariates were determined and are provided in the environmental data file. The snow density and depth data are provided at 25-m, 100-m, 500-m, 2000-m, and 10000-m grid resolutions, at 1-day increments, and cover the period September 1, 2005 through August 31, 2008. The sheep, snow, and landscape data cover the years 2006, 2007, and 2008.
&lt;br&gt;&lt;h4 id&#x3D;&quot;snowpack_dall_sheep_track_1583&quot;&gt;Snowpack_Dall_Sheep_Track_1583&lt;/h4&gt;
This dataset contains Dall sheep (Ovis dalli dalli) hoof sinking depths in snow tracks, and snow depth, hardness, and density measurements in snow pits adjacent to the tracks. Snow measurements were collected between March 19-22, 2017 at sites on Jaeger Mesa in the Wrangell Mountains (WRST), Alaska. Estimated sheep age classes and track site coordinates are also provided.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_planning_field_sites_1582&quot;&gt;ABoVE_Planning_Field_Sites_1582&lt;/h4&gt;
This dataset provides a listing of the ~6,700 field sites used in planning the ABoVE Airborne Campaign (AAC) for 2017. The sites included point, polygon, and line locations that were used in determining the 2017 AAC flight paths. We intend this compilation to assist investigators in understanding the flight line choices and as a method for investigators to identify ground locations used in the airborne campaign. Data users may also search for the underlying data available at each of these locations. Site descriptors include name, coordinates, principal investigators with emails, data types, long-term archive locations, and links to project descriptions.
&lt;br&gt;&lt;h4 id&#x3D;&quot;frac_fuelcomponent_maps_tundra_1761&quot;&gt;Frac_FuelComponent_Maps_Tundra_1761&lt;/h4&gt;
This dataset provides maps of the distribution of three major wildland fire fuel types at 30 m spatial resolution covering the Alaskan arctic tundra, circa 2015. The three fuel components include woody (evergreen and deciduous shrubs), herbaceous (sedges and grasses), and nonvascular species (mosses and lichens). Multi-seasonal and multispectral mosaics were first developed at 30 m resolution using Landsat 8 surface reflectance data collected from 2013 to 2017. The spectral information from Landsat mosaics was combined with field observations from representative tundra vegetation plots collected during multiple field trips to model the fractional cover of fuel type components. An improved vegetation mask for shrub and graminoid-dominated tundra was developed using random forest classification and is also included. The final fractional cover maps were developed using the trained model with the multi-seasonal and multi-spectral Landsat mosaics across the entire Alaskan tundra.
&lt;br&gt;&lt;h4 id&#x3D;&quot;great_slave_lake_ecosystem_map_1695&quot;&gt;Great_Slave_Lake_Ecosystem_Map_1695&lt;/h4&gt;
This dataset provides an ecosystem type map at 12.5 meter pixel spacing and 0.2 ha minimum mapping unit for the area surrounding Great Slave Lake, Northwest Territories, Canada for the time period 1997 to 2011. The map includes nine classes for peatland, wetland, and upland areas derived from a Random Forest classification trained on multi-date, multi-sensor remote sensing images across the study extent, and using field data and high-resolution Worldview-2 image interpretation for training and validation. The nine classes are: Water, Marsh, Swamp, Open Fen, Treed Fen, Bog, Upland Deciduous, Upland Conifer, and Sparsely Vegetated. A tenth map class identifies areas of historical fires (prior to 2011) that are currently undergoing post-fire successional revegetation. This dataset provides an ecosystem type map of the area before the large fire season of 2014 to better understand the effects of fires in the area.
&lt;br&gt;&lt;h4 id&#x3D;&quot;end_of_season_snow_depth_1702&quot;&gt;End_of_Season_Snow_Depth_1702&lt;/h4&gt;
This dataset provides 20,582 snow depth measurements collected at six sites near Fairbanks, Alaska, USA. Measurements were made during March or April from 2014-2019. The sites were located at or near Goldstream, Creamer&amp;#39;s Field, APEX, the Permafrost Tunnel and Farmer&amp;#39;s Loop. The US Army Corps of Engineers, Cold Regions Research and Engineering Laboratory (CRREL) owns and operates facilities at the Permafrost Tunnel and Farmer&amp;#39;s Loop. The sites are suitable for manipulation experiments, installing permanent equipment, and establishing long-term measurements.
&lt;br&gt;&lt;h4 id&#x3D;&quot;environmental_disturbances_ak_1705&quot;&gt;Environmental_Disturbances_AK_1705&lt;/h4&gt;
This dataset provides descriptions and photos of environmental conditions that impacted availability to subsistence resources by residents in nine rural communities within the Yukon River basin of Interior Alaska. The data (photos) were collected by citizens (harvesters) residing in the communities while engaged in subsistence harvesting activities. The data include descriptions of the environmental condition captured in the photo, photo date, an explanation of how the condition influenced travel and access to resources, the subsistence activity when the photo was taken, effects of the environmental condition on the participant&amp;#39;s safety, and the participant&amp;#39;s observations regarding frequency and extent of the condition. A sensitivity metric was derived that incorporated the adaptive capacity of the participants to environmental conditions. The observations are for the period February 2016 - June 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;effect_environment_moose_1739&quot;&gt;Effect_Environment_Moose_1739&lt;/h4&gt;
This dataset provides daily and annual air temperature, river water level, and leaf drop dates coincident with the moose (Alces alces) hunting season (September) for the area surrounding the rural communities of Nulato, Koyukuk, Kaltag, Galena, Ruby, Huslia, and Hughes in interior Alaska, USA, over the period 2000-2016. The main objective of the study was to assess how the environmental conditions impacted the success of hunters who rely on moose as a subsistence resource.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_frac_open_water_1362&quot;&gt;ABoVE_Frac_Open_Water_1362&lt;/h4&gt;
This data set provides land surface fractional open water cover maps for two overlapping regions: the entire pan-Arctic region (latitude &amp;gt; 45 degrees) and the Arctic-Boreal Vulnerability Experiment (ABoVE) domain across Alaska and Canada. The data are a 10-day averaged time step at 5-km spatial resolution for the period 2002-2015. Data represent the aerial portion of a grid cell covered by open water. The data were produced using high frequency (89 GHz) brightness temperatures from the Advanced Microwave Scanning Radiometer for EOS (AMSR-E) and the Advanced Microwave Scanning Radiometer 2 (AMSR2), with other ancillary inputs from AMSR-E/AMSR2 25-km products and the Moderate Resolution Imaging Spectroradiometer (MODIS). The resulting data record for fractional water is suitable for documenting open water patterns and inundation dynamics in boreal-Arctic ecosystems experiencing rapid climate change.
&lt;br&gt;&lt;h4 id&#x3D;&quot;maps_agb_north_slope_ak_1565&quot;&gt;Maps_AGB_North_Slope_AK_1565&lt;/h4&gt;
This dataset includes 30-m gridded estimates of total plant aboveground biomass (AGB), the shrub AGB, and the shrub dominance (shrub/plant AGB) for non-water portions of the Beaufort Coastal Plain and Brooks Foothills ecoregions of the North Slope of Alaska. The estimates were derived by linking biomass harvests from 28 published field site datasets with NDVI from a regional Landsat mosaic derived from Landsat 5 and 7 satellite imagery. The data cover the period 2007-06-01 to 2016-08-31.
&lt;br&gt;&lt;h4 id&#x3D;&quot;snow_cover_extent_and_depth_1757&quot;&gt;Snow_Cover_Extent_and_Depth_1757&lt;/h4&gt;
This dataset provides estimates of maximum snow cover extent (SCE) and snow depth for each 8-day composite period from 2001 to 2017 at 1 km resolution across Alaska. The study area covers the majority land area of Alaska except for areas covered by perennial ice/snow or open water. A downscaling scheme was used in which Modern-Era Retrospective Analysis for Research and Applications, Version 2 (MERRA-2) global reanalysis 0.5 degree snow depth data were interpolated to a finer 1 km spatial grid. In the methods used, the downscaling scheme incorporated MODIS SCE (MOD10A2) to better account for the influence of local topography on the 1km snow distribution patterns. For MODIS cloud-contaminated pixels, persistent and patchy cloud cover conditions were improved by applying an elevation-based spatial filtering algorithm to predict snow occurrence. Cloud-free MODIS SCE data were then used to downscale MERRA-2 snow depth data. For each snow-covered 1 km pixel indicated by the MODIS data, the snow depth was estimated based on the snow depth of the neighboring MERRA-2 0.5 grid cell, with weights predicted using a spatial filter.
&lt;br&gt;&lt;h4 id&#x3D;&quot;historical_lake_shorelines_ak_1859&quot;&gt;Historical_Lake_Shorelines_AK_1859&lt;/h4&gt;
This dataset includes maps of historical lake shorelines with derived lake areas in the southern portion of the Goldstream Valley and the surrounding landscape north of Fairbanks, Alaska, USA. Historical lake margins were mapped for 1949, 1967, and 1985 using 1 m aerial photographs available through U.S. Geological Survey Earth Explorer, and for 2009 using 2.5 m SPOT satellite image mosaics. The study area was a 214 km&lt;sup&gt;2&lt;/sup&gt; area of Pleistocene-aged yedoma permafrost in the southern portion of the Goldstream Valley. An increasing number of thermokarst lakes and ponds, from 130&amp;ndash;275 per year, were identified over the entire study period. Anthropogenic lakes, formed by mining peat, gravel, and gold concentrated in the northwestern extent of Goldstream Valley, were excluded.
&lt;br&gt;&lt;h4 id&#x3D;&quot;icefraction_waterbodies_acp_ak_2451&quot;&gt;IceFraction_WaterBodies_ACP_AK_2451&lt;/h4&gt;
This dataset contains ice fraction data at 1-km spatial resolution and approximately 6-day temporal resolution for small water bodies (900 m2 to 25 km2) across the Arctic Coastal Plain of Alaska (ACP) from 2017 to 2023. The data were developed using Sentinel-1 Synthetic Aperture Radar (SAR) imagery, texture features, and temperature data. Ice fraction is summarized for 1-km grid cells. Ice cover of water bodies in the northern high latitudes (NHL) is highly sensitive to the changing climate, and its dynamics exert substantial impacts on the NHL ecosystems, hydrological processes, and carbon cycle. Compared with the Google Dynamic World (DW) product derived from Sentinel-2 observations, this dataset shows high consistency with DW (R &#x3D;0.91, RMSE &#x3D; 0.19) while having enhanced temporal coverage due to fewer constraints from solar illumination, cloud cover, and atmospheric conditions.
&lt;br&gt;&lt;h4 id&#x3D;&quot;fire_ignitions_locations_ak_ca_2316&quot;&gt;Fire_Ignitions_Locations_AK_CA_2316&lt;/h4&gt;
This dataset provides daily fire ignition locations and timing for boreal fires in Alaska, U.S., and Canada between 2001 and 2019. The fire ignition locations and timing are extracted from the ABoVE Fire Emission Database; however, the temperate prairies of Canada, the Atlantic Highlands, and Mixed Wood Plains were not included. Fires were detected from Landsat differenced normalized burn ratio (dNBR) and the daily MODIS burned area and active fire products. Detections by dNBR were limited to fire perimeters from national fire databases. Fire ignition locations were retrieved using a local minimum within the fire perimeters. However, when fire locations were confounded due to simultaneous active fire detections, the fire ignition location was set as the centroid of these pixels. A spatial uncertainty equaling the standard deviation of the pixels&amp;#39; coordinates and the nominal nadir of 1000 m was applied to the fire ignition location. The temporal resolution of the ignition timing is within one day. Data is provided in comma separated values (CSV) and shapefile formats.
&lt;br&gt;&lt;h4 id&#x3D;&quot;burnedarea_emissions_ak_yt_nwt_1812&quot;&gt;BurnedArea_Emissions_AK_YT_NWT_1812&lt;/h4&gt;
This dataset provides estimates of daily burned area, carbon emissions, and uncertainty, and daily fire ignition locations for boreal fires in Alaska, U.S., and in the Yukon and Northwest Territories, Canada. The data are at 500 m resolution for the 18-year period from 2001-2018. Burned area was retrieved from combining fire perimeter data from the Alaskan and Canadian Large Fire Databases with surface reflectance and active fire data from the Moderate Resolution Imaging Spectroradiometer (MODIS) Collection 6. Per-pixel carbon consumption was estimated based on a statistical relationship between field estimates of pyrogenic consumption and several environmental variables. To derive the carbon consumption estimates, the approach from Alaskan Fire Emissions Database (AKFED) was updated and extended for the period 2001-2018. Fire weather variables, temperature, and the drought code complemented remotely sensed tree cover and burn severity as model predictors. Fire ignition location and timing were extracted from the daily burned area maps.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_l1_p_sar_1800&quot;&gt;ABoVE_L1_P_SAR_1800&lt;/h4&gt;
This dataset provides Level 1 (L1) polarimetric radar backscattering coefficient (Sigma-0 or S-0), multi-look complex, polarimetrically calibrated, and georeferenced data products from the UAVSAR P-band SAR radar instrument collected over 74 study sites across Alaska, USA, and western Canada. The radar instrument is a fully polarimetric P-band (ultra-high frequency) SAR operating in the 420-440 MHz band. The flight campaigns took place periodically in May-August 2017 onboard a NASA Gulfstream-III aircraft. Each set of products was produced from a data take (i.e., acquisition) of the UAVSAR P-band SAR radar instrument, where one data take is equivalent to one flight line over a site. Two to four data takes were sought for each site, although for some sites as few as one or as many as six are provided. There were a total of 139 data takes over the 74 sites.
&lt;br&gt;&lt;h4 id&#x3D;&quot;alaska_lake_pond_maps_2134&quot;&gt;Alaska_Lake_Pond_Maps_2134&lt;/h4&gt;
This dataset provides polygon spatial files of lake and pond extents for three sub-regions of Interior Alaska&amp;#39;s boreal forest, and one tundra region located in Alaska&amp;#39;s Yukon-Kuskokwim Delta. Files provide lake and pond extents of standing water without wetland vegetation or other obstructions with a minimum area of 0.01 ha. Water extents were derived from Planet Labs PlanetScope imagery with resolution of 3.125 m. A deep learning model (U-Net) was applied to PlanetScope orthotile imagery from Planet Labs&amp;#39; Dove-R and Super Dove satellites. The U-Net model used the red, green, blue, and near-infrared bands along with a slope raster derived from a 30-m digital elevation model (DEM) as inputs. The U-Net detected water bodies in all available cloud-free images from the snow-free period (May-September) of 2019-2021. Water body data are provided as 3-year composites (2019-2021) for all four regions and monthly climatological composites (May-September) over 2019-2021 for the three boreal forest regions. The composite water files indicate the presence of open, standing water in &amp;gt;40% of valid PlanetScope observations for a given composite time-slice. Files are provided in shapefile format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lake_wetland_classes_uavsar_1883&quot;&gt;Lake_Wetland_Classes_UAVSAR_1883&lt;/h4&gt;
This dataset contains a high-resolution land cover classification focused on water and wetland vegetation classes over three NASA ABoVE Campaign regions: Yukon Flats, Alaska, USA; the Peace-Athabasca Delta, Alberta; and the Canadian Shield, Northwest Territories (NWT), Canada. The product was derived from L-band synthetic aperture radar (SAR) acquisitions from the airborne NASA UAVSAR instrument in 2017-2019. The classification was trained and validated from field visits, UAV images, satellite imagery as well as other ABoVE datasets. Classifications in all regions are provided as both preliminary 13-class versions and final, simplified 5-class versions. Training and test data used for the classifier are also included as well as characteristics of lakes in the study area. This land cover classification was developed to support a project focusing on potential methane emissions from the shallow near-shore, or littoral, regions of lakes. The emergent aquatic vegetation classes can be used as a proxy for these littoral zones. Wetland vegetation classifications are provided as gridded raster files with an approximately 5-meter spatial resolution and aligned with the original UAVSAR footprints. Composite mosaics that aggregate these UAVSAR scenes by region and day of acquisition, if applicable, are also provided. Classifications in all regions are provided as both preliminary 13-class versions and final 5-class versions.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_growingseason_lake_color_1866&quot;&gt;ABoVE_GrowingSeason_Lake_Color_1866&lt;/h4&gt;
This dataset provides an annual time series of Landsat green surface reflectance and the derived annual trend during the growing season (June and July) for 472,890 lakes across the ABoVE Extended Study Domain from 1984 to 2019. The reflectance data are from Landsat-5, Landsat-7, and Landsat-8 sensors for the green band (center wavelength 560 nm). Over 270,000 Landsat scenes were evaluated and quality assured to be cloud-free and over water. Lakes were selected from HydroLAKES, a global database of lakes of at least 10 ha. Lake surface reflectance was extracted from a 3-by-3-pixel area centered on each lake centroid from the selected Landsat scenes determined from lake polygons. This dataset demonstrates changes in lake color over time in the arctic and boreal regions of North America. Color is relevant for understanding physical, ecological, and biogeochemical processes in some of the world&amp;rsquo;s highest concentrations of lakes where climate change may have significant impacts.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lakes_ponds_weekly_occurrence_2430&quot;&gt;Lakes_Ponds_Weekly_Occurrence_2430&lt;/h4&gt;
This dataset provides weekly surface water occurrence across lakes and ponds in six study regions: the Alaskan Coastal Plain, Yukon Flats, Yukon Kuskokwim Delta, Mackenzie River Delta, Tuktoyaktuk Peninsula, and Anderson Plain. The study regions are in Alaska, US, and Yukon and Northwest Territories, Canada. This binary (water or not water) raster product is built from Sentinel-2 imagery and a maximum lake extent vector product also produced from Sentinel-2 imagery. When cloud-free imagery was available, raster files were produced at 10 m spatial resolution and weekly temporal resolution during the ice-free season (May-September) for the period 2016-2023. Open water was differentiated from land using an adaptive NDWI threshold water classification algorithm and then clipped to the lake and ponds vector product so that only lake and pond water is reported. The data are provided in netCDF format along with two Jupyter notebooks holding code used for this analysis.
&lt;br&gt;&lt;h4 id&#x3D;&quot;methane_flux_bigtrail_lake_2393&quot;&gt;Methane_Flux_BigTrail_Lake_2393&lt;/h4&gt;
This dataset provides field data and gridded land cover and terrain data for an area north of Big Trail Lake, an active thermokarst lake in Goldstream Valley (near Fairbanks, Alaska, USA). Field samples were collected at 56 locations across the study area in June 2021 and August 2022. Field data include chamber-based methane (CH4) and carbon dioxide (CO2) flux, soil moisture, soil temperature, soil pH, vegetation communities, meteorological data, and soil samples. The soil samples were used to conduct SIMPER microbial community analysis and soil chemical analyses and to quantify methanogen and methanotroph relative abundance. Land cover classifications (10 cm spatial resolution) were derived from supervised random forest classifications using RedEdge-MX and multiSPEC-4C multispectral drone imagery, normalized difference vegetation index (NDVI), and USGS 3D Elevation Program (3DEP) digital surface model (DSM) data. RedEdge-MX drone imagery was collected in July 2021 and multiSPEC-4C drone imagery was collected in August 2019. Gridded microtopography and slope estimates were derived at 1 m spatial resolution using USGS 3DEP digital terrain model (DTM) data. Gridded products are provided in cloud-optimized GeoTIFF format, field data are provided in comma-separated values format, and sample location photos in JPEG format are contained within a compressed file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tundra_greeness_temp_trends_1893&quot;&gt;Tundra_Greeness_Temp_Trends_1893&lt;/h4&gt;
This dataset provides annual tundra greenness and summer air temperatures at a resolution of 50 km over the pan-Arctic tundra biome above 31.5 degrees over the time period 1985 to 2016. Annual tundra greenness was assessed using the maximum Normalized Difference Vegetation Index (NDVImax) derived from surface reflectance measured by sensors on the Landsat satellites. Summer air temperatures were quantified using the Summer Warmth Index (SWI) derived from an ensemble of five global temperature datasets. Tabular data include NDVImax, SWI, and estimates of uncertainty using Monte Carlo simulations at 45,334 vegetated sampling sites. Raster data provide (1) annual SWI from 1985 to 2016; (2) temporal trends in annual NDVImax and SWI from 1985 to 2016 and from 2000 to 2016; and (3) temporal correlations between annual NDVImax - SWI during these two periods. Each raster also includes estimates of uncertainty that were generated using Monte Carlo simulations. This dataset provides a new pan-Arctic product for assessing inter-annual variability in tundra using moderate resolution observations from the Landsat satellites.
&lt;br&gt;&lt;h4 id&#x3D;&quot;borealforest_greenness_trends_2023&quot;&gt;BorealForest_Greenness_Trends_2023&lt;/h4&gt;
This dataset provides information on interannual trends in annual maximum vegetation greenness from 1985 to 2019 for recently undisturbed areas in the boreal forest biome. Multi-decadal changes in remotely sensed vegetation greenness provide evidence of an emerging boreal biome shift driven by climate warming. Annual maximum vegetation greenness was assessed at about 100,000 random sample locations using an ensemble of spectral vegetation indices (NDVI, EVI2, kNDVI, and NIRv) derived from Landsat products. The dataset provides raster data summarizing vegetation greenness trends for sample locations stratified by Ecological Land Unit in GeoTIFF format. These raster data span the circum-hemispheric boreal forest biome between 45 to 70 degrees north at 300 m resolution. Estimates of uncertainty were generated using Monte Carlo simulations. Interannual trends in annual maximum vegetation greenness from 1985 to 2019 and 2000 to 2019 are provided for sample locations with adequate data for time series analysis; these data are in comma-separated values (CSV) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_agbd_uncertainty_maps_2465&quot;&gt;ABoVE_AGBD_Uncertainty_Maps_2465&lt;/h4&gt;
This dataset provides annual aboveground biomass (AGB) maps and associated uncertainty maps for Alaska and Canada from 1984 to 2022 at ~30 m resolution (0.00027 degrees). The dataset was derived using predictors from synthetic spectral features from Landsat Collection 2 and Continuous Change Detection and Classification algorithm. Extensive collections of ground plots (n &#x3D; 45,002) and airborne lidar data (n &#x3D; 421,942) were compiled for reference AGB in order to calibrate AGB models using Extreme Gradient Boosting (XGBoost) per ecoregion. Fifty AGB predictions were derived, of which the mean and standard deviation was used as per-pixel AGB prediction and uncertainty, respectively. The dataset can promote better understanding of carbon dynamics across arctic and boreal regions of North America. The data are provided in cloud optimized GeoTIFF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_forestdisturbance_agents_1924&quot;&gt;ABoVE_ForestDisturbance_Agents_1924&lt;/h4&gt;
This dataset provides spatial data on disturbance agents of fire, insects, and logging in the Arctic Boreal Vulnerability Experiment (ABoVE) core domain at an annual time step from 1987-2012 and 30 m resolution. Using a time-series of Landsat data, the three disturbance types were identified by abrupt changes in Tasseled Cap (dTC) indices of brightness, greenness, and wetness. Disturbances were detected by a Continuous Change Detection and Classification (CCDC) harmonic regression model applied to the time series. The dTC indices and disturbance results are provided.
&lt;br&gt;&lt;h4 id&#x3D;&quot;annual_landcover_above_1691&quot;&gt;Annual_Landcover_ABoVE_1691&lt;/h4&gt;
This dataset provides two 30-m resolution time series products of annual land cover classifications over the Arctic Boreal Vulnerability Experiment (ABoVE) core domain for each year of the period 1984-2014. The data are the annual dominant plant functional type in a given 30-m pixel derived from Landsat surface reflectance, landcover training data mapped across the ABoVE domain (using Random Forests modeling, with clustering and interpretation of field photography) and very high resolution imagery to assign land cover classifications. One product has a 15-class land cover classification that breaks out forest and shrub types into several additional classes; the other product provides a simplified, 10-class approach. Classification accuracy assessment results are provided per year. Assessments were based on a probability-based random sample of reference data that supported statistically robust estimation of areas and uncertainties in mapped areas.
&lt;br&gt;&lt;h4 id&#x3D;&quot;boreal_landcoverclasses_ak_ca_2423&quot;&gt;Boreal_LandCoverClasses_AK_CA_2423&lt;/h4&gt;
This dataset contains a 30-m resolution time series of annual land cover classifications as the dominant plant functional type class for all of boreal Alaska and Canada from 1986 to 2020. The data were derived from a time series of Landsat Collection 2 Surface Reflectance and processed using the Continuous Change Detection and Classification (CCDC) algorithm. This dataset includes a nine-class land cover scheme. Classification accuracy was assessed using a probability-based random sample, ensuring statistically robust area estimates and uncertainty measures. The classifications were produced using a supervised Random Forest classification model and Canadian National Forest Inventory photo plot data. The data are provided in multiband GeoTIFF file format and distributed by tile in the ABoVE Level B grid.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_fire_severity_dnbr_1564&quot;&gt;ABoVE_Fire_Severity_dNBR_1564&lt;/h4&gt;
This dataset contains differenced Normalized Burned Ratio (dNBR) at 30-m resolution calculated for burn scars from fires that occurred within the Arctic Boreal and Vulnerability Experiment (ABoVE) Project domain in Alaska and Canada during 1985-2015. The fire perimeters were obtained from the Alaskan Interagency Coordination Center (AICC) and the Natural Resources Canada (NRC) fire occurrence datasets. Only burns with an area larger than 200-ha were included. The dNBR for each burn scar at 30-m pixel resolution was derived from pre- and post-burn Landsat 5, 7, and 8 scenes within a 5-km buffered area surrounding each burn scar using Landsat LEDAPS surface reflection image pairs.
&lt;br&gt;&lt;h4 id&#x3D;&quot;last_day_spring_snow_1528&quot;&gt;Last_Day_Spring_Snow_1528&lt;/h4&gt;
This dataset provides the last day of spring snow cover for most of Alaska and the Yukon Territory for 2000 through 2016. The data are based on the MODIS daily snow cover fraction product (MODSCAG) and are provided at 500-m resolution. Pixels in the daily snow cover fraction grids from April 1 through July 31 were flagged as &amp;quot;Snow&amp;quot; if the snow fraction exceeded 0.15, resulting in a time series of binary daily snow cover grids for each year. The annual last day of spring snow for each pixel was identified by day of the year ranging from 91 (April 1) to 183 (July 2).
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_footprints_wrf_ak_nwca_1896&quot;&gt;ABoVE_Footprints_WRF_AK_NWCa_1896&lt;/h4&gt;
This dataset provides Weather Research and Forecasting (WRF) Stochastic Time-Inverted Lagrangian Transport (STILT) Footprint data products for receptors (observations) located at positions along flight paths and at various fixed observing sites at circumpolar locations at northern latitudes during 2016-2019. Each aircraft and station position is treated as an independent receptor in the WRF-STILT model in order to simulate the land surface influence on observed atmospheric constituents. The footprints are independent of chemical species and can be applied to different flux models and incorporated into formal inversion frameworks. The particle trajectories that determine the footprint field are constrained only by the outer edges of the WRF modeling domain. The measurements included in this data set are crucial for understanding changes in Arctic carbon cycling and the potential threats posed by the thawing of Arctic permafrost.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_particles_wrf_ak_nwca_1895&quot;&gt;ABoVE_Particles_WRF_AK_NWCa_1895&lt;/h4&gt;
This dataset provides Weather Research and Forecasting (WRF) Stochastic Time-Inverted Lagrangian Transport (STILT) particle trajectory files for receptors located at positions along flight paths and at various fixed observing sites at circumpolar locations above 45 degrees North during 2016-2019. The particle files describe the motion of particles released backward in time over a 10-day period. The particle files are separated into archives by platform type (some platforms are combined) and can be characterized as either low resolution or high resolution depending on whether the subsequent footprint fields were generated on a circumpolar 0.5-degree grid (low-resolution) or both 0.5-degree and 0.1-degree grids (high-resolution). The platforms include flux towers at fixed sites, laboratory measurements of whole air samples collected by Programmable Flask Packages (PFP) onboard aircraft, and observations by NASA&amp;#39;s Orbiting Carbon Observatory-2 satellite. These particle files were thinned to retain particle location information only when the particles have non-zero contributions to the corresponding footprint field. These particle files are used to compute the footprint fields available in a companion dataset. The particle trajectories that determine the footprint field are constrained only by the outer edges of the WRF modeling domain. Likewise, the companion footprint files are provided on a regular latitude-longitude grid. This dataset extends previous research on the atmospheric transport of land-surface emissions of greenhouse gases by the Carbon in Arctic Reservoirs Vulnerability Experiment (CARVE) project. In particular, the content of the low-resolution particle files is similar to those for the CARVE dataset.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_forage_lichen_maps_1867&quot;&gt;ABoVE_Forage_Lichen_Maps_1867&lt;/h4&gt;
This dataset provides modeled estimates of lichen ground cover at 30 m resolution across the Fortymile study area in interior eastern Alaska, U.S., and the Yukon Territory, Canada, for the nominal year 2015. The mapped lichens are important winter forage for the nine resident caribou (Rangifer tarandus) herds in the region. A random forest modeling approach with vegetation inputs and environmental and spectral predictors was used to estimate lichen cover for 2015. Input data for the model were aggregated from historical in-situ vegetation plots, visual aerial surveys, and recent unmanned aerial system (UAS) imagery to align with 30 m resolution Landsat pixels over the 583,200 km2 study area. The model was also used to estimate lichen cover for the year 2000 by applying the trained model to historical Landsat imagery. An estimate of lichen volume in 2015, based on a published algorithm, is also provided. In addition, site-level presence-absence maps at &amp;lt;1 m resolution and site-level lichen cover maps at both 2 m and 30 resolution are provided. Site-level data were derived from high-resolution RGB imagery collected in summer 2017 from UASs at 22 forested and alpine sites across interior Alaska and western Yukon. Due to the use of two unique UAS imagers at 7 sites, there are 29 data collections across the 22 sites. Each UAS data collection is associated with three data files. These landscape-scale maps could be useful for understanding trends in lichen abundance and distribution, as well as for caribou research, management, and conservation.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpp_modis_alaska_canada_2024&quot;&gt;GPP_MODIS_Alaska_Canada_2024&lt;/h4&gt;
This dataset contains gridded estimations of daily ecosystem Gross Primary Production (GPP) in grams of carbon per day at a 1 km2 spatial resolution over Alaska and Canada from 2000-01-01 to 2018-01-01. Daily estimates of GPP were derived from a light-curve model that was fitted and validated over a network of ABoVE domain Ameriflux flux towers then upscaled using MODIS Multi-Angle Implementation of Atmospheric Correction (MAIAC) data to span the extended ABoVE domain. In general, the methods involved three steps; the first step involved collecting and processing mainly carbon-flux site-level data, the second step involved the analysis and correction of site-level MAIAC data, and the final step developed a framework to produce large-scale estimates of GPP. The light-curve parameter model was generated by upscaling from flux tower sub-daily temporal resolution by deconvolving the GPP variable into 3 components: the absorbed photosynthetically active radiation (aPAR), the maximum GPP or maximum photosynthetic capacity (GPPmax), and the photosynthetic limitation or amount of light needed to reach maximum capacity (PPFDmax). GPPmax and PPFDmax were related to satellite reflectance measurements sampled at the daily scale. GPP over the extended ABoVE domain was estimated at a daily resolution from the light-curve parameter model using MODIS MAIAC daily reflectance as input. This framework allows large-scale estimates of phenology and evaluation of ecosystem sensitivity to climate change.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_lvis_vegetationstructure_1923&quot;&gt;ABoVE_LVIS_VegetationStructure_1923&lt;/h4&gt;
This dataset provides Level 3 (L3) footprint-level gridded metrics and attributes collected from NASA&amp;#39;s Land, Vegetation, and Ice Sensor (LVIS)-Facility instrument for each flightline from 2017 and 2019. In 2017, the LVIS-Facility instrument was flown at a nominal flight altitude of 28,000 ft onboard a Dynamic Aviation Super King Air B200T. In 2019, the LVIS-Facility and LVIS-Classic instruments were flown at a nominal flight altitude of 41,000 feet onboard the NASA Gulfstream V. LVIS data are collected as waveforms over footprints of ~10-m diameter. The L3 data include grids of canopy relative height (RH), complexity, canopy cover (CC), ground elevation, and the number of LVIS footprints available to produce a pixel&amp;#39;s estimate.. These 30-m resolution grids describe the vertical column of the vegetation canopy in detail with relative canopy height metrics and are enriched with an additional set of canopy cover estimates at a variety of height thresholds. The LVIS-Facility instrument 2017 and 2019 acquisitions span Arctic, boreal, temperate, and sub-tropical landscapes in support of a variety of Arctic-Boreal Vulnerability Experiment (ABoVE)- and Global Ecosystem Dynamics Investigation (GEDI)-related science. In the ABoVE study domain of arctic and boreal Alaska and Western Canada, some of these acquisitions coincide spatially with legacy small-footprint airborne lidar. Data are included for the ABoVE domain and also for the continental U.S. and central America in support of GEDI calibration and validation. Data files are provided in GeoTIFF format and one geopackage file shows flightlines.
&lt;br&gt;&lt;h4 id&#x3D;&quot;methane_ebullition_lakes_ak_1861&quot;&gt;Methane_Ebullition_Lakes_AK_1861&lt;/h4&gt;
This dataset includes maps of the locations and number of methane ebullition hotspots in 15 frozen lakes in the southern portion of the Goldstream Valley and the surrounding landscape just north of Fairbanks, Alaska, USA. Hotspots were identified from early winter high resolution aerial photographs acquired three days after lake-ice formation in October 2014. Hotspot ebullition seeps are defined as point-sources of high ebullition that release methane from lake sediments year-round. High rates of bubbling impede ice formation. In early winter, bubbling leads to dark, round open holes in lake ice which were visible in the aerial photos. This project investigated the role of theromkarst lakes in thawing of permafrost and mobilization of organic carbon in frozen soils.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ch4_flux_bigtrail_goldstream_1778&quot;&gt;CH4_Flux_BigTrail_Goldstream_1778&lt;/h4&gt;
This dataset provides diffusive methane (CH4) fluxes collected from two thermokarst lakes in the Goldstream Valley, north of Fairbanks in interior Alaska. Fluxes were collected from the littoral zones, adjacent shoreline, and upland vegetation. The data were collected during July 2018. Measurements were made using a mobile, closed chamber technique where chamber air was recirculated through a Los Gatos Research (LGR) Ultraportable Cavity Ring-down Spectrometer. The chamber was large enough to enclose emergent and upland vegetation up to 1.5 m in height, allowing plant-facilitated fluxes to be measured. These in situ measurements were used to verify spatial patterns in methane flux (i.e., exponential decay with distance from water) detected by NASA&amp;#39;s Next Generation Airborne Visible/Infrared Imaging Spectrometer (AVIRIS-NG).
&lt;br&gt;&lt;h4 id&#x3D;&quot;ak_yukon_pft_topcover_2032&quot;&gt;AK_Yukon_PFT_TopCover_2032&lt;/h4&gt;
This dataset contains data files of modeled top cover estimates by plant functional type (PFT) for the Arctic and Boreal Alaska and Yukon regions. Estimates are presented for single years at 5-year intervals from 1985 to 2020. Also included are root mean square error (RMSE) and source year, which indicate the specific year from which pixels in the top cover maps were derived. Plant functional types include conifer trees, broadleaf trees, deciduous shrubs, evergreen shrubs, graminoids, forbs, and light macrolichens. Estimates were derived through the combination of two stochastic gradient-boosting models that used environmental and spectral covariates. Environmental covariates represented topographic, climatic, permafrost, hydrographic, and phenological gradients, and spectral covariates were based on Landsat Thematic Mapper (TM), Enhanced Thematic Mapper Plus (ETM+), and Operational Land Imager (OLI) data collected between 1984-2020. These maps catalog widespread changes in the distribution of PFTs occurring in the Arctic and boreal forest ecosystems, such as tundra shrub expansion, due to the intensification of disturbances such as fire and climate-driven vegetation dynamics.
&lt;br&gt;&lt;h4 id&#x3D;&quot;modis_ccan_ndvi_trends_alaska_1666&quot;&gt;MODIS_CCaN_NDVI_Trends_Alaska_1666&lt;/h4&gt;
This dataset provides the average Normalized Difference Vegetation Index (NDVI) at 1-km resolution over the north slope of Alaska, USA, for the growing season (June-August) of each year from 2000-2015, and NDVI trends for the same period. The dataset presents growing-season averages and trends from two sources: 1) derived from 1-km, 8-day data from the Moderate Resolution Imaging Spectroradiometer (MODIS) NDVI (MOD13A2) product, and 2) predicted by the Coupled Carbon and Nitrogen model (CCaN). CCaN is a mass balance carbon and nitrogen model that was driven by 1-km MODIS surface temperature and climate data for the North Slope of Alaska and parameterized using model-data fusion, where model predictions were ecologically constrained with historical ecological ground and satellite-based data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;albedo_boreal_north_america_1605&quot;&gt;Albedo_Boreal_North_America_1605&lt;/h4&gt;
This dataset contains MODIS-derived daily mean shortwave blue sky albedo for northern North America (i.e., Canada and Alaska) and a set of quality control flags for each albedo value to aid in user interpretation. The data cover the period of February 24, 2000 through April 22, 2017. The blue sky albedo data were derived from the MODIS 500-m version 6 Bidirectional Reflectance Distribution Function and Albedo (BRDF/Albedo) Model Parameters MCD43A1 dataset (MCD43A1.006, &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MCD43A1.006&quot;&gt;https://doi.org/10.5067/MODIS/MCD43A1.006&lt;/a&gt;) (Schaaf &amp;amp; Wang, 2015a, please refer to the MCD43 documentation and user guides for more information). Blue sky refers to albedo calculated under real-world conditions with a combination of both diffuse and direct lighting based on atmospheric and view-geometry conditions. Daily mean albedo was calculated by averaging hourly instantaneous blue sky albedo values weighted by the solar insolation for each time interval. Potter et al. (2019, &lt;a href&#x3D;&quot;https://doi.org/10.1111/gcb.14888&quot;&gt;https://doi.org/10.1111/gcb.14888&lt;/a&gt;) is the associated paper for this dataset. Note the actual extent of the dataset in Figure 1 of the User Guide. Users are encouraged to refer to the User Guide for further important information about the use of this dataset.
&lt;br&gt;&lt;h4 id&#x3D;&quot;alaska_yukon_ndvi_1614&quot;&gt;Alaska_Yukon_NDVI_1614&lt;/h4&gt;
This dataset provides the maximum Normalized Difference Vegetation Index (NDVI) at 1-km resolution over northern Alaska, USA and the Yukon Territory, Canada for each year from 2002-2017, as well as a 16 year maximum NDVI product. MODIS products MOD13Q1 and MYD13Q1 from Collection 6 were acquired at 250-m pixel size from June 1-August 30 of each year. Within each growing season from 2002-2017, the maximum NDVI was determined for each pixel. These maximum NDVI values were then aggregated to 1-km by selecting the maximum NDVI from the sixteen 250-m pixels values nested within each 1-km pixel. A long-term 16-year maximum NDVI was then derived from the time series of annual maximum NDVI values.
&lt;br&gt;&lt;h4 id&#x3D;&quot;monthly_hydrological_fluxes_1647&quot;&gt;Monthly_Hydrological_Fluxes_1647&lt;/h4&gt;
This dataset provides modeled estimates of monthly hydrological fluxes at 0.25-degree resolution over Alaska and Canada for the years 1979-2018. The estimates were derived from the Variable Infiltration Capacity (VIC) macroscale hydrological model version 4.1.2 with water and energy balance schemes at 0.25-degree spatial and daily temporal resolution for this 38-year period. The gridded output data products are monthly average water balance variables including precipitation (P), evapotranspiration (E), &amp;#39;P minus E&amp;#39;, evaporation, soil moisture in three soil layers, base flow and runoff, snow depth, snow water equivalent (SWE), and snow sublimation, and energy balance variables including surface temperature, albedo, latent and sensible heat flux, ground heat flux, short- and long-wave and other radiative fluxes. The daily modeled values for precipitation and evapotranspiration were also aggregated to water years and precipitation was also aggregated to a 30-year climate normal average.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_uncertainty_maps_1652&quot;&gt;ABoVE_Uncertainty_Maps_1652&lt;/h4&gt;
This dataset provides estimates of the uncertainty in components of the carbon cycle including: soil carbon stock, autotrophic respiration (Ra), heterotrophic respiration (Rh), net ecosystem exchange (NEE), net primary production (NPP), and gross primary productivity (GPP) across the entire ABoVE Study Domain at 0.5-degree resolution for the reference year 2003. The uncertainties were calculated from the multi-model (n &#x3D; 20) disagreement, i.e. standard deviation, from the Trends in Net Land Atmosphere Carbon Exchanges program (TRENDY) and the North American Carbon Program (NACP) regional synthesis model outputs averaged to annual means. This total uncertainty integrates both structural uncertainty of land-surface physics among models as well as inherent parametric uncertainty introduced within models, and uncertainty from forcing data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vegetation_greenness_trend_1576&quot;&gt;Vegetation_greenness_trend_1576&lt;/h4&gt;
This dataset provides the summer NDVI trend and trend significance for the period 1984-2012 over Alaska and Canada. The NDVI were calculated per-pixel from all available peak-summer 30-m Landsat 5 and 7 surface reflectance data for the period. NDVI time series were assembled for each 30-m land location (i.e., non-water, non-snow), from observations that were unaffected by clouds as indicated by data-quality masks and following additional processing to remove anomalous NDVI values. A simple linear regression via ordinary least squares was applied to the per-pixel NDVI time series. The slope of the regression was taken as the annual NDVI trend (unit NDVI change per year) and is reported in the &amp;quot;trend&amp;quot; data files. A Student&amp;#39;s t-test was used to assess the significance of the trend and the per-pixel significance is reported in the &amp;quot;trend_sig&amp;quot; data files. A significant positive slope indicates a greening trend, and a significant negative slope indicates a browning trend.
&lt;br&gt;&lt;h4 id&#x3D;&quot;chlorophyll_fluorescence_data_1785&quot;&gt;Chlorophyll_Fluorescence_Data_1785&lt;/h4&gt;
This dataset provides the results of in situ measurements of needle-level chlorophyll fluorescence (ChlF) obtained from a pulse amplitude modulated (PAM) fluorometer from evergreen needleleaf forested sites one in Alaska and one in Idaho. Measured light-adapted minimal fluorescence (Ft) is reported as the quantum yield of fluorescence and light-adapted variable fluorescence over maximal fluorescence (Fv/Fm) and is reported as the quantum yield of photosystem II. Also reported for both sites are two modeled irradiance products: (1) the top-of-canopy instantaneous irradiance (W/m2) and (2) needle-level irradiance (W/m2) that was modeled to account for shadow casting and canopy orientation in modulating direct radiation. Both products were modeled to be contemporaneous with ChlF observations. At the Idaho site only, needle-level irradiance (W/m2) was measured in situ with a handheld pyranometer. The Alaska field site is located in the northern latitudinal forest-tundra ecotone (FTE) near the Dalton Highway in Northern Alaska. Thirty-six Picea glauca (white spruce) trees were sampled on 2017-07-07 to 2017-07-08. The Idaho field site is located in a montane forest near McCall, Idaho. Ten selected Abies grandis (grand fir) trees were sampled on 2019-07-05 to 2019-07-06. Measurement of needle-level ChlF occurred during clear-sky conditions such that the canopies experienced a broad range of variability in sunlit-shading patterns across the day during these near-solstice periods.
&lt;br&gt;&lt;h4 id&#x3D;&quot;snowmeltduration_pmicrowave_1843&quot;&gt;SnowMeltDuration_PMicrowave_1843&lt;/h4&gt;
This dataset provides the annual period of snowpack melting (i.e., snow melt duration, SMD) across northwest Canada; Alaska, U.S.; and parts of far eastern Russia at 6.25 km resolution for the period 1988-2018. SMD is the number of days between the main melt onset date (MMOD) and the last day of seasonal snow cover when the melting of snow is complete. These dates were derived from the Making Earth Science Data Records for Use in Research Environments (MEaSUREs) Calibrated Enhanced-Resolution Passive Microwave (PMW) EASE-Grid Brightness Temperature (Tb) Earth System Data Record (ESDR). This dataset documents variability in SMD across space and the 31-year temporal period. The data from 1988-2016 included a coastal mask removing coastal pixels due to potential water contamination from coarse brightness temperature observations (Dersken et al., 2012). There is not a coastal mask for the 2017-2018 data. The full data are included, and data users should be aware that coastal values can be adversely affected by adjacent water bodies.
&lt;br&gt;&lt;h4 id&#x3D;&quot;main_melt_onset_dates_1841&quot;&gt;Main_Melt_Onset_Dates_1841&lt;/h4&gt;
This dataset provides the annual date of snowpack seasonal beginning melt (i.e., main melt onset date, MMOD) across northwest Canada, Alaska, US, and parts of far eastern Russia at 6.25-km resolution for the period 1988-2023. MMOD was derived from the daily 19V (K-band) and 37V (Ka-band) GHz bands from the Making Earth Science Data Records for Use in Research Environments (MEaSUREs) Calibrated Enhanced-Resolution Passive Microwave (PMW) EASE-Grid Brightness Temperature (Tb) Earth System Data Record (ESDR). The PMW MMOD dataset was validated using the transition date from Freeze Degree Days (FDD) to Thaw Degree Days (TDD) from in situ air temperature observations from 31 SNOw TELemetry network (SNOTEL) stations, and compared to an established Freeze-Thaw ESDR (FT-ESDR) spring onset date record. The resulting MMOD data record is suitable for documenting the spatial-temporal impacts of MMOD variability in ecosystem services, wildlife movements, and hydrologic processes within the ABoVE (Arctic Boreal Vulnerability Experiment) domain. The data from 1988-2016 included a coastal mask removing coastal pixels due to potential water contamination from coarse brightness temperature observations (Dersken et al., 2012). No coastal mask is used for the 2017-2023 data. The full data are included, and data users should be aware that values adjacent to large water bodies can be adversely affected.
&lt;br&gt;&lt;h4 id&#x3D;&quot;canada_boreal_forest_greenness_1587&quot;&gt;Canada_Boreal_Forest_Greenness_1587&lt;/h4&gt;
This dataset provides a 28-year time series of peak greenness (NDVI) data derived from Landsat 5 TM imagery over the boreal forest region of Canada. Landsat 5 TM scenes were collected for 46 selected sidelap sites along gradients in climate, tree cover, and disturbance history from 1984 to 2011. Peak-greenness reflectance was computed for 30-m Landsat pixels using the maximum normalized difference vegetation index (NDVI) along with the normalized burn ratio (NBR) during the period between days of the year (DOY) 180 and 204. To facilitate trend analysis at each site, the NDVI and NBR data of the 30-m Landsat pixels were regridded to the coarser MODIS 500-m (463.3-m) spatial scale to reduce the effects of missing data and to enhance the significance of the trend. The regridded NDVI and NBR 28-year time series data at 500-m resolution are provided for each of the 46 sites. Two trend analyses were run on the 500-m resolution data and are reported for each site. Supplemental site metadata are also provided, including the number of valid Landsat pixels, land cover composition, and disturbance history, for each 500-m pixel.
&lt;br&gt;&lt;h4 id&#x3D;&quot;permafrost_thaw_depth_yk_1598&quot;&gt;Permafrost_Thaw_Depth_YK_1598&lt;/h4&gt;
This dataset provides field observations of thaw depth and dominant vegetation types, a LiDAR-derived elevation map, and permafrost distribution and probability maps for an area on the coastal plain of the Yukon-Kuskokwim Delta (YKD), in western Alaska, USA. Field data were collected during July 8-17, 2016 to parameterize and to validate the derived permafrost maps. The YKD is in the sporadic to isolated permafrost zone where permafrost forms extensive elevated plateaus on abandoned floodplains. The region is extremely flat and vulnerable to eustatic sea-level rise and inland storm surges. These high-resolution permafrost maps support landscape change analyses and assessments of the impacts of climate change on permafrost in this region of high biological productivity, critical wildlife habitats, and subsistence-based human economy.
&lt;br&gt;&lt;h4 id&#x3D;&quot;radial_growth_pri_1781&quot;&gt;Radial_Growth_PRI_1781&lt;/h4&gt;
This dataset provides simultaneous in-situ measurements of the photochemical reflectance index (PRI) and radial tree growth of selected white spruce trees (Picea glauca (Moench) Voss) at the northern treeline in the Brooks Range of Alaska, south of Chandalar Shelf and Atigun Pass on the east side of the Dalton Highway. PRI and dendrometer measurements were simultaneously collected on 29 trees from six plots spaced along a 5.5 km transect from south to north where tree density becomes increasingly sparse. Measurements were made throughout the 2018 and 2019 growing seasons (May 1 to September 15) with a sampling interval of 5 minutes. The data were collected to better understand the suitability of the PRI to remotely track radial tree growth dynamics.
&lt;br&gt;&lt;h4 id&#x3D;&quot;veg_soil_tundra_burned_area_2119&quot;&gt;Veg_Soil_Tundra_Burned_Area_2119&lt;/h4&gt;
This dataset includes field measurements from 26 burned and unburned transects established in 2008 in the region of the Anaktuvuk River tundra fire on the Arctic Slope of Alaska, US. Measurements include plant cover by species, shrub and tussock density, thaw depth, and soil depth. This wildfire occurred in 2007, and sampling took place in 2008-2011 and in 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_nwt_2017_field_data_1771&quot;&gt;ABoVE_NWT_2017_Field_Data_1771&lt;/h4&gt;
This dataset provides vegetation community characteristics, soil moisture, and biophysical data collected in 2017 from 11 study sites in the ABoVE Study area. The 11 study areas contained 28 sites that were burned by wildfires in 2014 and 2015, and 10 unburned sites in the Northwest Territories (NWT), Canada. Burned sites included peatland and upland. These field data include assessment of burn severity, vegetation inventories, ground cover, diameter and height for trees and shrubs, seedling and sprouting cover, soil moisture, and depth of unfrozen soil. Plot sizes were 10 m x 10 m with smaller subplots for selected measurements. Similar data were collected for these sites in the years 2015-2019 and are available in related separate datasets. Field data are provided in CSV format. The dataset includes digital photographs (in JPEG format) of vegetation conditions at sampling sites.
&lt;br&gt;&lt;h4 id&#x3D;&quot;wildfires_nwt_canada_2018_1703&quot;&gt;Wildfires_NWT_Canada_2018_1703&lt;/h4&gt;
This dataset provides vegetation community characteristics and biophysical data collected in 2018 from areas that were burned by wildfire in 2014 and 2015, and from nine unburned validation sites in the Northwest Territories, Canada. The data include vegetation inventories, ground cover, regrowth, tree diameter and height, and woody seedling/sprouting data at burned sites, and similar vegetation community characterization at unburned validation sites. Additional measurements included soil moisture, collected for validation of the UAVSAR airborne collection, and depth to frozen ground at the nine unburned sites. This 2018 fieldwork completes four years of field sampling at the wildfire areas.
&lt;br&gt;&lt;h4 id&#x3D;&quot;wildfires_nwt_canada_2019_1900&quot;&gt;Wildfires_NWT_Canada_2019_1900&lt;/h4&gt;
This dataset provides vegetation community characteristics, soil moisture, and biophysical data collected in 2019 from 11 study areas, which contained 28 sites that were burned by wildfires in 2014 and 2015, and 14 unburned sites in the Northwest Territories (NWT), Canada. Burn sites included peatland and upland. These field data include vegetation inventories, ground cover, as well as diameter and height for trees and shrubs in the unburned sites. Similar data were collected for the unburned sites in the years 2015-18 and are available in related separate datasets. In 2019, the focus was on woody and non-woody seedling/sprouting regrowth data in the burned sites. Additional measurements collected at all sites included total peat depth, soil moisture, and active layer thickness (ALT). Soil moisture and ALT were collected for validation of the UAVSAR airborne collection and Radarsat-2 overpasses. This 2019 fieldwork completes five years of field sampling at the wildfire areas.
&lt;br&gt;&lt;h4 id&#x3D;&quot;rain-on-snow_data_v2_2415&quot;&gt;Rain-on-Snow_Data_V2_2415&lt;/h4&gt;
This dataset provides maps of rain-on-snow (ROS) events across Alaska for the individual cold season months from November to March using observations from two space-borne passive microwave radiometers: (a) the Advanced Microwave Scanning Radiometer for EOS and Advanced Microwave Scanning Radiometer 2 (AMSR-E/2) from 2002 to 2023; and (b) the Special Sensor Microwave Imager and the Special Sensor Microwave Imager Sounder (SSMI/S) from 1988 to 2020. Considering the differences in sensor overpass time, observation geometry, and ancillary snow cover data, the AMSR-E/2 and SSMI/S-based ROS records were generated separately. ROS events were defined as changes in surface snow wetness and isothermal states induced by atmospheric processes associated with winter rainfall or latent heat exchange. The data are summations of the number of days with ROS events per pixel at 6-km spatial resolution per month or per 5-month water year. Winter months are when snowmelt from solar illumination is minimal and snow cover is widespread and relatively consistent throughout the region. The data are provided in GeoTIFF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;reflectance_spectra_alaska_1685&quot;&gt;Reflectance_Spectra_Alaska_1685&lt;/h4&gt;
This dataset reports full-spectrum (350-2500 nm) reflectance measurements of diverse plant communities at the plot-level and individual plant species at the leaf-level, at multiple sites across northern Alaska during the 2017 and 2018 summer field seasons. Plot-level reflectance data (1 m2) include an assemblage of vascular and non-vascular species comprising tundra plant communities, while leaf-level scans are specific to one particular tundra species. Reflectance measurements were collected using a HR-1024i spectrometer and data were calibrated using a Spectralon white reference panel during sampling to correct for changing light conditions. Sampling methods and data and metadata structure follow that of the Ecological Spectral Information System (EcoSIS) Spectral Library.
&lt;br&gt;&lt;h4 id&#x3D;&quot;river_ice_breakup_freezeup_1697&quot;&gt;River_Ice_Breakup_Freezeup_1697&lt;/h4&gt;
This dataset provides estimates of river ice breakup and freeze-up stages along selected reaches of the Yukon and Tanana Rivers in the Yukon River Basin in interior Alaska from 1972-2016. Time series of Landsat satellite images were visually interpreted to identify the day of year and characteristics of the different stages of river ice seasonality. The stages of breakup or freeze-up were distinguished from one another based on the spatial extent and patterns of open water and ice cover. Images were displayed as false color composites, with the shortwave infrared (SWIR), near infrared (NIR), and green bands represented by red, green, and blue.
&lt;br&gt;&lt;h4 id&#x3D;&quot;erosion_vegetation_yukon_1616&quot;&gt;Erosion_Vegetation_Yukon_1616&lt;/h4&gt;
This dataset provides a time series of riverbank erosion and vegetation colonization along reaches of the Yukon River (3 study areas), Tanana and Nenana Rivers (1 area), and Chandalar River (1 area) in interior Alaska over the period 1984-2017. The change data were derived from selected 30-m images from Landsat TM, Landsat ETM+, and Landsat Operational Land Imager (OLI) surface reflectance products. Image classification used the Normalized Differenced Vegetation Index (NDVI) with an NDVI threshold of 0.2 to differentiate vegetated from non-vegetated pixels. Images were assigned to one of seven or eight multiyear intervals, within the 1984-2017 overall range, for each study area. Time intervals vary by study site. Change detection identified shifts from one time interval to the next: changes from vegetated to non-vegetated classes were considered riverbank erosion and changes from non-vegetated to vegetated classes were considered vegetation colonization.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sar_methane_ebullition_ak_1790&quot;&gt;SAR_Methane_Ebullition_AK_1790&lt;/h4&gt;
This dataset provides Synthetic Aperture Radar (SAR) estimates of lake-source methane ebullition flux in mg CH4/m2/d for thousands of lakes in five regions across Alaska. The study regions include the Atqasuk, Barrow Peninsula, Fairbanks, northern Seward Peninsula, and Toolik. L-band SAR backscatter values for early winter lake ice scenes were collected from 2007 to 2010 over 5,143 lakes using the Phased Array type L-band Synthetic Aperture Radar (PALSAR) instrument on the Advanced Land Observing Satellite (ALOS-1) satellite. The backscatter data were combined with field measurements of methane ebullition from 48 study lakes across the five regions to obtain a volumetric flux estimate for each lake. Mean methane gas-fractions from each region were applied to the SAR-based volumetric fluxes to obtain an estimate of methane ebullition mass flux per lake. The data files contain lake perimeters and the lake-specific attributes of lake area, SAR backscatter values and standard errors, volumetric flux with standard errors, mean percent of methane from gas samples, and methane ebullition mass flux.
&lt;br&gt;&lt;h4 id&#x3D;&quot;dissolved_gases_alaska_rivers_2360&quot;&gt;Dissolved_Gases_Alaska_Rivers_2360&lt;/h4&gt;
This dataset provides dissolved carbon dioxide (CO2) and methane (CH4) concentrations alongside their stable and radiocarbon isotopic compositions within the Arctic Sagavanirktok and Kuparuk River watersheds located on the North Slope of Alaska. The data were collected during the spring, fall, and summer seasons in 2022. In field separation of the bulk gaseous components (N2, CO2, and CH4) from the liquid phase was achieved using a degassing membrane contactor. Laboratory isotopic analyses were conducted at the W. M. Keck Carbon Cycle Accelerator Mass Spectrometer facility at UC Irvine. This collection aims to provide insights into the seasonal dynamics of greenhouse gas emissions in these critical Arctic environments, thereby contributing valuable information for climate change research and monitoring programs. The data are provided in comma separated values (CSV) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;active_layer_thaw_depths_1701&quot;&gt;Active_Layer_Thaw_Depths_1701&lt;/h4&gt;
This dataset provides soil active layer thaw depth measurements collected along transects at three sites near Fairbanks, Alaska, USA. Measurements were made during the late summers of 2014-2018. The sites were located at Creamer&amp;#39;s Field, the Permafrost Tunnel, and Farmer&amp;#39;s Loop (two transects). Vegetation ecotypes along the transects are also reported. The US Army Corps of Engineers, Cold Regions Research and Engineering Laboratory (CRREL) owns and operates facilities at the Permafrost Tunnel and Farmer&amp;#39;s Loop. The sites are suitable for manipulation experiments, installing permanent equipment, and establishing long-term measurements.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_soil_thawdepth_moisture_1903&quot;&gt;ABoVE_Soil_ThawDepth_Moisture_1903&lt;/h4&gt;
This dataset provides soil thaw depth and moisture (STDM) measurements and dielectric properties measured by different research teams at sites in Alaska, U.S., and the Northwest Territories, Canada. There are multiple observations per site and 352,719 total observations. The dataset includes 206,000 observations of active layer thickness measured by mechanical probing (6.0%) or ground penetrating radar (GPR) (94.0%). Approximately 16,000 volumetric water content measurements were collected using GPR (22.1%), Hydrosense I and II probes (75.3%), and DualEM (2.6%). Metadata includes the location, time, geospatial coordinates, technique, measurement teams. Measurements were typically collected in August and September near the end of the thaw season and cover the period 2008-06-22 to 2020-08-15.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_soil_thawmoisture_2369&quot;&gt;ABoVE_Soil_ThawMoisture_2369&lt;/h4&gt;
This dataset provides soil thaw depth and moisture measurements and dielectric properties measured by different research teams at sites in Alaska, U.S., and the Northwest Territories, Canada. There are multiple observations per site and 528,703 total observations. The dataset includes 223,230 observations of active layer thickness measured by mechanical probing (9.8%) or ground penetrating radar (GPR) (90.2%). Approximately 179,154 volumetric water content (VWC) measurements were collected using GPR (2.0%), HydroSense I and II probes (8.8%), in situ loggers (89.2%), and DualEM (&amp;lt;1.0%). Metadata includes the location, time, geospatial coordinates, sampling technique, measurement teams, and field team contact information. Measurements were typically collected in August and September near the end of the thaw season and cover the period from 2005 to 2022. This dataset, referred to as field measurements of Soil Moisture and Active layer Thickness (SMALT) (Schaefer et al., 2021), was developed for work in Clayton et al. (2021). It has been expanded in Version 2 to comprise a comprehensive dataset of NASA Arctic-Boreal Vulnerability Experiment (ABoVE) field campaign measurements of soil moisture and active layer thickness, including logger data of relevance to Uninhabited Aerial Vehicle Synthetic Aperture Radar (UAVSAR) acquisitions. The data are provided in comma separated values (CSV) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;alt_soil_collection_protocols_2373&quot;&gt;ALT_Soil_Collection_Protocols_2373&lt;/h4&gt;
This dataset contains soil moisture sampling protocols and calibration algorithms for Campbell Scientific Hydrosense-I and II units used at burned and unburned sites in the ABoVE project domain. The soil moisture sampling protocols document provides guidance for sampling in situ soil moisture to relate to synthetic aperture radar (SAR) data collections. Two additional documents describe algorithms for calibrating handheld Hydrosense units used to measure volumetric water content in soils. One calibration document applies to organic soils in fire-affected sites of the Northwest Territories and Alaska. A second document provides calibrations for samples collected in non-burned tundra, boreal bog, fen, upland deciduous and conifer sites located in Alberta and tundra sites in Alaska. The information is provided in portable document format (PDF).
&lt;br&gt;&lt;h4 id&#x3D;&quot;soil_temp_moisture_alaska_1869&quot;&gt;Soil_Temp_Moisture_Alaska_1869&lt;/h4&gt;
This dataset provides soil temperature and volumetric water content (VWC) measurements at 15 cm depth collected at 12 selected boreal and tundra sites located across Alaska. Each site is equipped with a HOBO MicroStation Data Logger that hosts two soil temperature sensors (HOBO S-TMB-M006 Temperature Smart Sensor), and two soil moisture sensors (HOBO S-SMD-M005 10HS Soil Moisture Smart Sensor). Each sensor was installed horizontally at a depth of 15 cm within the soil profile. Samples of soil from seven sites were taken to a laboratory for determination of site-specific soil moisture sensor calibration curves to correct raw measurements. Data were nominally recorded at an hourly frequency and downloaded from the sites at least annually for the period 2016-08-11 to 2023-09-02, but data coverage varies by site. These measurements were collected at the same sites as previously archived CO2 efflux and thaw depth data. The data are provided in comma-separated values (CSV) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;usarray_ground_temperature_1680&quot;&gt;USArray_Ground_Temperature_1680&lt;/h4&gt;
This dataset includes soil temperature profile measurements taken at 63 monitoring sites associated with the USArray program, located across the NASA ABoVE domain in interior Alaska. The measurement dates and depths vary per site as does measurement frequency (hourly or every 6 hours). Measurements were made from the soil surface to a maximum depth of 1.5 m from 2016-2021 using temperature sensors attached to HOBO data loggers. These measurement stations complement existing temperature monitoring networks allowing for better characterization of ground temperatures and permafrost conditions across Alaska. This station data complement an existing temperature monitoring network, allowing for better characterization of ground temperatures and permafrost conditions in northern and western Alaska. The temperature measurements are provided for each site in 64 data files in comma-separated values (.csv) format. Site descriptive data are also provided for soil, vegetation, and location.
&lt;br&gt;&lt;h4 id&#x3D;&quot;soil_temperature_profiles_ak_1767&quot;&gt;Soil_Temperature_Profiles_AK_1767&lt;/h4&gt;
This dataset includes soil temperature profile measurements taken at 16 monitoring sites in Alaska, USA, and at one site in Yukon, Canada. The six sites are collocated with seismic stations of the USArray program. The measurement dates and depths vary per site as does measurement frequency (hourly or every 6 hours). Measurements were made from the soil surface to a maximum depth of 1.5 m. Measurements were made from 2016-2018 at two sites, 2017-2019 at four sites, and 2018-2019 at 11 sites using temperature sensors attached to HOBO data loggers. These measurement stations complement existing temperature monitoring networks allowing for better characterization of ground temperatures and permafrost conditions across Alaska.
&lt;br&gt;&lt;h4 id&#x3D;&quot;post_fire_c_emissions_1787&quot;&gt;Post_Fire_C_Emissions_1787&lt;/h4&gt;
This dataset provides spatial estimates of carbon combustion from all 2015 wildfire burned areas across Saskatchewan, Canada, on a 30-m grid. Carbon combustion (kg C/m2) was derived from post-fire field measurements of carbon stocks completed in 2016 at 47 stands that burned during three 2015 Saskatchewan wildfires (Egg, Philion, and Brady) and at 32 unburned stands in adjacent areas. The study areas covered two ecozones (Boreal Plains and Boreal Shield), two stand-replacing history types (fire and timber harvest), three soil moisture classes (xeric, mesic, and subhygric), and three stand dominance classifications (coniferous, deciduous, and mixed). To spatially extrapolate estimates of combustion to all 2015 fires in Saskatchewan, a predictive radial support vector machine model was trained on the 47 burned stands with associated environmental variables and geospatial predictors and applied to historical fire areas. The dataset also includes uncertainty estimates represented as per pixel standard deviations of model estimates derived using a Monte Carlo analysis.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_reference_grid_1367&quot;&gt;ABoVE_reference_grid_1367&lt;/h4&gt;
The Arctic - Boreal Vulnerability Experiment (ABoVE) has developed two standardized spatial data products to expedite coordination of research activities and to facilitate data interoperability. First, the ABoVE Study Domain encompasses the Arctic and boreal regions of Alaska, USA, and the western provinces of Canada, North America. Core and Extended study regions have been designated within this Domain and are provided in both a vector representation (Shapefile) and a raster representation (GeoTIFF at 1,000-meter pixel resolution). Second, a Standard Reference Grid System has been developed to cover the entire Study Domain and also extends to the eastern portion of North America. This Reference Grid is provided as a nested pair of polygon grids at scales of 240- and 30-meter spatial resolution. A shapefile is provided for each grid. Note that the designated standard projection for the all ABoVE products is the Canadian Albers Equal Area projection.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_reference_grid_v2_1527&quot;&gt;ABoVE_reference_grid_v2_1527&lt;/h4&gt;
The Arctic - Boreal Vulnerability Experiment (ABoVE) has developed two standardized spatial data products to expedite coordination of research activities and to facilitate data interoperability. The ABoVE Study Domain encompasses the Arctic and boreal regions of Alaska, USA, and the western provinces of Canada, North America. Core and Extended study regions have been designated within this Domain and are provided in a vector representation (Shapefile), a raster representation (GeoTIFF at 1,000-meter spatial resolution), and a NetCDF file. A standard Reference Grid System has been developed to cover the entire Study Domain and extends to the eastern portion of North America. This Reference Grid is provided as nested polygon grids at scales of 240, 30, and 5-meter spatial resolution. The 5-meter grid is new in Version 2. Note that the designated standard projection for all ABoVE products is the Canadian Albers Equal Area projection.
&lt;br&gt;&lt;h4 id&#x3D;&quot;interior_alaska_subsistence_1725&quot;&gt;Interior_Alaska_Subsistence_1725&lt;/h4&gt;
This dataset provide maps to show the search and harvest areas used by community residents for all subsistence resources combined across Interior Alaska for the years 2011 through 2017. The maps show the extent of areas used by residents for those communities where data collection and research has occurred; it is not a comprehensive use map for the entire area. The maps are a composite of data collected by the Division of Subsistence, Alaska Department of Fish and Game using standardized methods where respondents indicated the search areas for species harvested, the amounts harvested, and the location and months of harvest. These data are important for research, analysis, and regulatory assessment.
&lt;br&gt;&lt;h4 id&#x3D;&quot;decadal_water_maps_1324&quot;&gt;Decadal_Water_Maps_1324&lt;/h4&gt;
This data set provides the location and extent of surface water (open water not including vegetated wetlands) for the entire Boreal and Tundra regions of North America for three epochs, centered on 1991, 2001, and 2011. Each of the products were generated with at least three years of ice-free Landsat imagery. The data are at 30-m resolution and were derived from time series of Landsat 4 and 5 Thematic Mapper (TM) data and Landsat 7 Enhanced Thematic Mapper (ETM+) covering all of Alaska and all provinces of Canada. The overall goal was to generate a map of the nominal extent of water for a given epoch, where nominal is neither the maximum nor the minimum but rather a representative extent for that time period.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_plot_data_burned_sites_1744&quot;&gt;ABoVE_Plot_Data_Burned_Sites_1744&lt;/h4&gt;
This dataset is a synthesis of field plot characterization data, derived above-ground and below-ground combusted carbon, and acquired Fire Weather Index (FWI) System components for burned boreal forest sites across Alaska, USA, the Northwest Territories, and Saskatchewan, Canada from 1983-2016. Unburned plot data are also included. Compiled plot-level characterization data include stand age, disturbance history, tree density, and tree biophysical measurements for calculation of the above-ground (ag) and below-ground (bg) biomass/carbon pools, pre-fire and residual post-fire soil organic layer (SOL) depths and estimates of combustion of tree structural classes. The measured slope and aspect for each site and an assigned moisture class based on topography are also provided. Data from 1019 burned and 152 unburned sites are included. From the estimates of combusted ag and bg carbon pools and SOL losses, the total carbon combusted, the proportion of pre-fire carbon combusted, and the proportion of total carbon combusted were calculated for each plot. FWI System components including moisture and drought codes and indices of fire danger were obtained for each plot from existing data sources based on the plot location, year of burn, and a dynamic start-up date (day of burn, DOB) from the global fire weather database. Data for soil characteristics are included in a separate file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;postfire_tree_regeneration_1955&quot;&gt;PostFire_Tree_Regeneration_1955&lt;/h4&gt;
This dataset is a synthesis of species-specific pre- and post-fire tree stem density estimates, field plot characterization data, and acquired climate moisture deficit data for sites from Alaska, USA eastward to Quebec, Canada in fires that burned between 1989 and 2014. Data are from 1,538 sites across 58 fire perimeters encompassing 4.52 Mha of forest and all major boreal ecozones in North America. To be included in this synthesis, a site had to contain information on species-specific post-fire seedling densities. This included sites where seedlings had been counted 2-13 years post-fire, a timeframe over which there was little change in relative dominance of species based on densities. Plot characterization data includes stand age, site drainage, disturbance history, crown combustion severity, seedbed conditions, and stand structural attributes. Gridded values of Hargreaves Climate Moisture Deficit (CMD) were obtained for each plot where plot coordinates were available. These values included 30-year normals (1981-2010) and CMD in the two years immediately following the fire year. CMD anomalies were calculated as the difference between the 30-year normal and the single year values for each of the first two years after a fire. These synthesis data are provided in comma-separated values (CSV) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lidar_tundra_forest_ak_1782&quot;&gt;LiDAR_Tundra_Forest_AK_1782&lt;/h4&gt;
This dataset provides terrestrial lidar scanning (TLS) point cloud data collected at 10 research plots along the forest-tundra ecotone (FTE) in the Brooks Range of Alaska, south of Chandalar Shelf and Atigun Pass on the east side of the Dalton Highway. Data were collected in mid-June 2016. Data were acquired for each plot from multiple scan positions with a Leica ScanStation C10 green wavelength laser instrument. After processing the point spacing is &amp;lt; 1 cm. TLS enables resolution of 3-dimensional landscape features that can be used to derive ecologically important metrics of canopy structure and surface topography at high spatial resolution.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_thaw_depth_1579&quot;&gt;ABoVE_Thaw_Depth_1579&lt;/h4&gt;
This dataset provides thaw depth measurements made at seven locations across Alaska, during August 2016, June and September 2017, and July-August 2018. Three of the locations are paired unburned-burned sites. At each site, three 30-meter transects were established and thaw depth was measured at 1-meter increments along each transect using a 1.15 m T-shaped thaw depth probe. Locations were selected to investigate fire disturbance, to span the range of permafrost regions from continuous to sporadic, and to cover vegetation types from boreal forests, tussock tundra, upland willow/herbaceous scrub, and lowland fen and wet tundra sites across Alaska. The data are provided in comma-separated values (CSV) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;boreal_canopycover_standage_2012&quot;&gt;Boreal_CanopyCover_StandAge_2012&lt;/h4&gt;
This dataset contains Landsat-derived locally-calibrated estimates of tree canopy cover (TCC) and forest stand age across global boreal forests from 1984-2020 in Cloud-Optimized GeoTIFF (.tif) format. These raster data span the circum-hemispheric boreal forest biome between 47 to 73 degrees north at 30 m resolution. Machine learning models calibrated with data from the World Reference System 2 were used to predict TCC from Landsat data at 30-m spatial resolution at annual temporal resolution. Through analysis of TCC time series, forest change estimates of stand age from 1984-2020 were developed. The broad spatial and temporal coverage of these data provide insight into forest and carbon dynamics of the global boreal forest system. Boreal forests store a large proportion of global soil and biomass carbon and have experienced disproportionately high levels of warming over the past century.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ak_tundra_pft_fractionalcover_1830&quot;&gt;AK_Tundra_PFT_FractionalCover_1830&lt;/h4&gt;
This dataset provides predicted continuous-field cover for tundra plant functional types (PFTs), across ~125,000 km2 of Alaska&amp;#39;s North Slope at 30-m resolution. The data cover the period 2010-07-01 to 2015-08-31. The data were derived using a random forest data-mining algorithm, predictors derived from Landsat satellite observations (surface reflectance composites for ~15-day periods from May-August), and field vegetation cover and site characterization data spanning bioclimatic and geomorphic gradients. The field vegetation cover was stratified by nine PFTs, plus open water, bare ground and litter, and using the cover metrics total cover (areal cover including the understory) and top cover (uppermost canopy or ground cover), resulting in a total of 19 field cover types. The field data and predictor values at the field sites are also included.
&lt;br&gt;&lt;h4 id&#x3D;&quot;northslope_nee_tvprm_1920&quot;&gt;NorthSlope_NEE_TVPRM_1920&lt;/h4&gt;
This dataset includes hourly net ecosystem exchange (NEE) simulated by the Tundra Vegetation Photosynthesis and Respiration Model (TVPRM) at 30 km horizontal resolution for the Alaskan North Slope for 2008-2017. TVPRM calculates tundra NEE from air temperature, soil temperature, photosynthetically active radiation (PAR), and solar-induced chlorophyll fluorescence (SIF) using functional relationships derived from eddy covariance tower measurements. These relationships were then scaled over the region using gridded meteorology and a vegetation map. The site-level CO2 fluxes fell into two distinct ecosystem groups: inland tundra (ICS, ICT, ICH, IVO) and coastal tundra (ATQ, BES, BEO, CMDL). The expanded modeling framework allowed for the easy substitution of ecological behaviors and environmental drivers, including the choice of representative inland tundra site, coastal tundra site, vegetation map (CAVM, RasterCAVM, or ABoVE-LC), meteorological reanalysis product (NARR or ERA5), and SIF product (GOME2, GOSIF, or CSIF). Using all of these variations generated an ensemble of 288 different TVPRM simulations of regional CO2 flux and one additional simulation option with added aquatic and zero curtain fluxes (AqZC).
&lt;br&gt;&lt;h4 id&#x3D;&quot;alt_maps_ak_ca_2332&quot;&gt;ALT_Maps_AK_CA_2332&lt;/h4&gt;
The dataset consists of maps of estimated Active Layer Thickness (ALT) at 30-m resolution throughout the northern half of Alaska for the years 2014, 2015, and 2017. The maps were generated by using a machine learning-based regression and a set of spatial data layers to upscale ALT from narrow swaths of ALT that were retrieved from airborne high-resolution P-band Polarimetric Synthetic Aperture Radar (PolSAR) imagery. The data are provided in cloud-optimized GeoTIFF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_izaviknek_field_data_1772&quot;&gt;ABoVE_Izaviknek_Field_Data_1772&lt;/h4&gt;
This dataset provides ecological field data that were collected during July 2017 and July 2018 from 43 plots spanning gradients of fire history in the upland tundra of the Yukon-Kuskokwim (Y-K) Delta, Alaska. Plot-level data include vegetation species composition and structure, leaf area index (LAI), topography, thaw-depth, and soil characteristics collected at plots burned in 1971-1972, 1985, 2006-2007, 2015, or unburned controls. Vegetation species were sampled along transects using the vegetation point-intercept (VPI) sampling approach and summarized by three metrics of vegetation cover: (1) top-hit cover, (2) any-hit cover, and (3) multi-hit cover. Each metric is the total number of hits for a species divided by the total number of sample points. The VPI any-hit cover metric data were combined with Landsat imagery to develop fractional maps of any-hit cover for four aggregated plant functional types (PFTs); bryophytes, herbs, lichen, and shrubs for the upland tundra area. Photographs of vegetation transects and soil pits are included as companion files.
&lt;br&gt;&lt;h4 id&#x3D;&quot;inundationmap_ykflats_peaceath_1901&quot;&gt;InundationMap_YkFlats_PeaceAth_1901&lt;/h4&gt;
This dataset provides time series of wetland inundation coverage maps and corresponding inundation frequency maps at ~10-meter resolution estimated every 12 days during the free-water period (May to October) for the years 2017-2019 over the Yukon Flats (YK) portion of the Yukon River, Alaska, USA, and the Peace-Athabasca Delta (PAD), Alberta, Canada. Wetland inundation coverage was determined by a two-step modified decision-tree classification approach that first used Sentinel-1 C-band SAR to identify likely inundated areas across a study site and was followed by a decision-tree classification step with C-band SAR backscatter statistics thresholds to distinguish among different inundation components. The result of this process was five classes for each inundation map, namely Open Water (OW), Floating Plants (FP), Emergent Plants (EP), Flooded Vegetation (FV), and Dry Land (DRY). After all the individual (every 12 days) inundation coverage maps were derived for a study site, they were generalized to two-class maps which maintained only inundation status. These generalized maps were then stacked and summarized to produce the inundation frequency map for the site. In these maps, higher values signify more frequently inundated areas, with the maximum value representing permanently inundated pixels. The Sentinel-1 inundation mapping capability demonstrated here provided frequent, broad-scale mapping of different wetland inundation components. Integration of such products with process-based methane (CH4) models would improve simulation of CH4 emissions from wetlands.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecosystem_map_srd_pad_1947&quot;&gt;Ecosystem_Map_SRD_PAD_1947&lt;/h4&gt;
This dataset provides ecosystem-types for the Slave River Delta (SRD) and Peace-Athabasca Delta (PAD), Canada, for the time periods circa 2007 and circa 2017. The image resolution is 12.5 m with 0.2-hectare minimum mapping unit. Included are an 18-class modified Enhanced Wetland Classification (EWC) scheme for wetland, peatland, and upland areas. Classes were derived from a Random Forest classification trained on multi-seasonal moderate-resolution images and synthetic aperture radar (SAR) imagery sourced from aerial and satellite sensors, field data, and calculated indices. Indices included Height Above Nearest Drainage (HAND) and Topographic Position Index (TPI), both derived from a digital elevation model, to differentiate between land cover types. The c. 2007 remote sensing data were comprised of early and late growing season Landsat-5, ERS2, L-Band PALSAR from 2006 to 2010 and growing season Landsat thermal composites. The c. 2017 remote sensing data were comprised of early and late growing season Landsat-8 and L-Band PALSAR-2 from 2017 to 2019, Sentinel-1 June VV and VH mean and standard deviations, and growing season Landsat thermal composites. Elevation indices from multi-resolution TPI and HAND were created from the Japan Aerospace Exploration Agency Advanced Land Observing Satellite 30 m Global Spatial Data Model. Also included are the images used for classification and the classification error matrices for each map and time period. Data are provided in GeoTIFF and GeoPackage file formats.
&lt;br&gt;&lt;h4 id&#x3D;&quot;wetland_vegclassification_pad_2069&quot;&gt;Wetland_VegClassification_PAD_2069&lt;/h4&gt;
This dataset contains land cover classification focused on water and wetland vegetation communities over the Peace-Athabasca Delta, Canada. Four classification maps with 5-m resolution were derived various combinations of Airborne Visible/Infrared Imaging Spectrometer-Next Generation (AVIRIS-NG) and Uninhabited Aerial Vehicle Synthetic Aperture Radar (UAVSAR) acquired in July and September 2019, and a historical LiDAR archive data. The maps include 10 land cover classes, including open water, emergent aquatic vegetation types, terrestrial vegetation, and forest. Based on field data, the best performing model, which combined all three data sources, achieved an overall accuracy of 93.5%. The land cover maps are provided in GeoTIFF format along with polygons of AVIRIS-NG, UAVSAR, and LiDAR footprints in shapefile and KML formats.
&lt;br&gt;&lt;h4 id&#x3D;&quot;whitespruce_leaf_traits_alaska_2124&quot;&gt;WhiteSpruce_Leaf_Traits_Alaska_2124&lt;/h4&gt;
This dataset provides measurements of gas exchange (light response curves, Kok curves and ACi curves), leaf traits (carbon, nitrogen, and specific leaf area), leaf pigments (Chlorophyll a, Chlorophyll b and Carotenoids), the photochemical reflectance index (PRI), and average photosynthetic photon flux density as collected from hemispherical photographs. Data were collected on white spruce trees (Picea glauca (Moench) Voss) growing at the northern edge of the species&amp;#39; distribution in Alaska and at the southern edge of the species&amp;#39; distribution in Black Rock Forest (BRF), New York. Measurements were taken at high and low canopy positions on each tree at both sites during the 2017 growing season (2017-06-19 to 2017-07-20). Gas exchange, leaf trait, pigment and spectral measurements were obtained using a portable photosynthesis system (LI-6800, LI-COR, Lincoln, NE). Photochemical reflectance index was determined using a spectroradiometer, and hemispherical photographs were taken with a digital camera. These data were collected to better understand how vertical canopy gradients in photosynthetic physiology change from the southernmost to the northernmost range extremes of white spruce. The data are provided in comma-separated value (CSV) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;fire_emissions_nwt_1561&quot;&gt;Fire_Emissions_NWT_1561&lt;/h4&gt;
This dataset provides estimates of wildfire carbon emissions and uncertainties at 30-m resolution, and measurements collected at burned and unburned field plots from the 2014 wildfire sites near Yellowknife, Northwest Territories (NWT), Canada. Field data were collected at 211 burned plots in 2015 and include site characteristics, tree cover and species, basal area, delta normalized burn ratio (dNBR), plot characteristics, soil carbon, and carbon combusted. Data were collected at 36 unburned plots with characteristics similar to the burned plots in 2016. The emission estimates were derived from a statistical modeling approach based on measurements of carbon consumption at the 211 burned field plots located in seven independent burn scars. Estimates include uncertainty of field observations of aboveground and belowground combustion, as well as prediction uncertainty from a multiplicative regression model. To apply the model across all 2014 NWT fire perimeters, the final model covariates were re-gridded to a common 30-m grid defined by the Arctic Boreal and Vulnerability Experiment (ABoVE) Project. The regression model was then applied to burned pixels defined by a threshold of Landsat-derived differenced Normalized Burn Ratio (dNBR) within fire perimeters. Derived carbon emissions and uncertainty in g/m2 are provided for each 30-m grid cell. The modeled NWT domain encompasses 29 tiles within the ABoVE 30-m reference grid system.
&lt;br&gt;&lt;h4 id&#x3D;&quot;wildfires_date_of_burning_1559&quot;&gt;Wildfires_Date_of_Burning_1559&lt;/h4&gt;
This dataset provides estimates of wildfire progression represented by date of burning (DoB) within fire scars across Alaska and Canada for the period 2001-2019. Burn scar locations were obtained from two datasets: the Alaskan Interagency Coordination Center (AICC) and the Natural Resources Canada (NRC) databases. All scars within these databases were used in this study. The estimated DoB was derived using an algorithm for identifying the first fire occurrence from the Moderate Resolution Imaging Spectroradiometer (MODIS) active fire detection product (MCD14ML, Collection 6) and to subsequently determine all dates of burning within fire scars. The DoB data are provided as polygons and map the daily progression of a fire within each burn scar. As a result, there is one polygon for each DoB detected within an identified burn scar boundary. The MODIS active fire points associated with the burn scar data are also provided. Data for the period 2001-2015 were first published in 2017 and data for the period 2016-2019 were added in January 2021.
&lt;br&gt;&lt;h4 id&#x3D;&quot;wolves_denning_pups_climate_1846&quot;&gt;Wolves_Denning_Pups_Climate_1846&lt;/h4&gt;
This dataset provides annual gray wolf (Canis lupus) denning spatial information and timing, associated climatic and phenologic metrics, and reproductive success (i.e., pup survival) in wolf populations across areas of western Canada and Alaska within the NASA ABoVE Core Domain. The study encompasses 18 years between the period 2000-2017. Wolves were captured from eight populations following standard animal care protocols and released with Global Positioning System (GPS) collars. Data from 388 wolves were used to estimate den initiation dates (n&#x3D;227 dens of 106 packs) and reproductive success in the eight populations. Each population was monitored from 1 to 12 years between 2000 and 2017. Denning parturition phenology was measured each year as the number of calendar days from January 1st to the initiation date of each documented denning event. Reproductive success was determined as to whether pups survived through the end of August following a reproductive event. To evaluate the effect of climate factors on reproductive phenology, aggregated seasonal climate metrics for temperature, precipitation, and snow water equivalent based on three biological seasons for seasonal wolf home ranges were produced. Normalized Difference Vegetation Index (NDVI) time-series data were used to estimate phenological metrics such as the start of the growing season (SOS), length of the growing season (LOS), and time-integrated NDVI (tiNDVI), and were summarized for the populations&amp;#39; home range.
&lt;br&gt;&lt;h4 id&#x3D;&quot;arctic_winter_respiration_v2_1762&quot;&gt;Arctic_Winter_Respiration_v2_1762&lt;/h4&gt;
This dataset provides soil-surface carbon dioxide (CO2) efflux derived from measurements of soil respiration with forced diffusion (FD) chambers. Soil Respiration Stations (SRS) were installed at 11 boreal and tundra sites along a broad south-to-north transect starting from near Fairbanks in interior Alaska and extending to Atqasuk in northern Alaska. Each SRS measures soil respiration and ambient atmospheric CO2 concentrations with a forced diffusion (FD) chamber to derive soil CO2 flux. The SRS also measures soil CO2 concentrations and temperatures using instrumented chambers buried at 5, 10, and 15 cm depths in the soil profile. At the highest measurement frequency, data are collected hourly, and during the lowest winter frequency, every 48 hours. The data include flux values and running median filtered values from the two or three FD chambers at each site. Soil CO2 and temperature profile data (beginning June 2017) were collected beginning 2016-08-18 through 2023-09-02. This dataset updates four sites with extended temporal coverage. As of this publication, sampling is continuing, and new data will be added as available.
&lt;br&gt;&lt;h4 id&#x3D;&quot;boreal_agb_density_icesat2_2186&quot;&gt;Boreal_AGB_Density_ICESat2_2186&lt;/h4&gt;
This dataset provides estimates of Aboveground dry woody Biomass Density (AGBD) for high northern latitude forests at a 30-m spatial resolution. It is designed both for boreal-wide mapping and filling the northern spatial data gap from NASA&amp;#39;s Global Ecosystem Dynamics Investigation (GEDI) project. Mapping forest aboveground biomass is essential for understanding, monitoring, and managing forest carbon stocks toward climate change mitigation. The AGBD estimates cover the extent of high latitude boreal forests and extend southward to 50 degrees latitude outside the boreal zone. AGBD was predicted using two modeling steps: 1) Ordinary Least Squares (OLS) regression related field plot measurements of AGBD to NASA&amp;#39;s ICESat-2 30-m lidar samples, and 2) random forest models were used to extend estimates beyond the field plots by relating ICESat-2 AGBD predictions to wall-to-wall covariate stacks from Harmonized Landsat Sentinel-2 (HLS) and the Copernicus DEM. Per-pixel uncertainties are estimated from bootstrapping both models. Non-vegetated areas (e.g. built up, water, rock, ice) were masked out. HLS composites and ICESat-2 data were from 2019-2021; three years of conditions were aggregated into the circa 2020 map. ICESat-2 data were filtered to include only strong beams, growing seasons (June through September), solar elevations less than 5 degrees, snow free land (snow flag set to 1), and &amp;quot;msw_flag&amp;quot; equal to 0 (clear skies and no observed atmospheric scattering). ICESat-2&amp;#39;s ATL08 product was resampled to a 30-m spatial resolution to better match both the field plots and mapped pixels. HLS data (L30HLS) were used to create a greenest pixel composite of growing season multispectral data, which was then used to compute a suite of vegetation indices: NDVI, NDWI, NBR, NBR2, TCW, TCG. These were then used, in combination with the slope and elevation data from the Copernicus DEM product, to predict 30-m AGBD per 90-km tile. Estimates of mean AGBD with standard deviation are provided in cloud-optimized GeoTIFF (CoG) format. Training data are in comma-separated values (CSV) format. A polygon map of data tiles is included as a GeoPackage file and a Shapefile.
&lt;br&gt;&lt;h4 id&#x3D;&quot;agb_great_slave_lake_nwt_2365&quot;&gt;AGB_Great_Slave_Lake_NWT_2365&lt;/h4&gt;
This dataset holds aboveground biomass (ABG) estimates for areas in the Great Slave Lake Region in the Northwest Territories of Canada for 2019. ABG was estimated from L-band synthetic aperture radar (SAR) data obtained from JAXA&amp;#39;s Advanced Land Observing Satellite-2 (ALOS-2/PALSAR-2) and supplemented with data from NASA&amp;#39;s airborne Uninhabited Aerial Vehicle SAR (UAVSAR) instrument. SAR data were collected from 2017 to 2021. In situ AGB measurements at 14 plots sampled in 2019 were used to calibrate a logarithmic regression to relate the radar datasets to in situ AGB data. Then, AGB was mapped over available ALOS-2 tiles. The estimates are provided in 20-Mg ha-1 bins at 100-m resolution in cloud optimized GeoTIFF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ykdelta_envchange_infoexchange_1894&quot;&gt;YKDelta_EnvChange_InfoExchange_1894&lt;/h4&gt;
This dataset provides a booklet documenting the discussions and outcomes from a knowledge-exchange meeting with Yup&amp;#39;ik elders from the Yukon-Kuskokwim Delta (YKD), western Alaska, community members, and natural scientist to discuss landscape and weather changes that have been observed in their homelands. The meeting was held during November 14-16, 2018. Yup&amp;#39;ik participants represented several YKD villages that occupy very different biophysical environments, and they have lifelong perspectives of environmental conditions and change that predate the era of Earth-observing satellites by many decades. Nearly 16 hours of discussion and testimonials from YKD elders were recorded during the meeting. The booklet is structured according to the environmental change processes that were discussed (e.g., coastal flooding, permafrost thaw, shrub expansion, climate change) and includes narrative summaries, quotations from participants, graphical illustrations, and examples of the field- and remote-sensing-based scientific findings, and map products developed as part of the larger ABoVE project.
&lt;br&gt;&lt;h4 id&#x3D;&quot;alaska_arctic_tundra_veg_map_1353&quot;&gt;Alaska_Arctic_Tundra_Veg_Map_1353&lt;/h4&gt;
This data set provides the spatial distributions of vegetation types, geobotanical characteristics, and physiographic features for the Arctic tundra region of Alaska for the period 1993-2005. Specific attributes include dominant vegetation, bioclimate subzones, floristic subprovinces, landscape types, lake coverage, and substrate chemistry. This data set generally includes areas North and West of the forest boundary and excludes areas that have a boreal flora such as the Aleutian Islands and alpine tundra regions south of treeline.
&lt;br&gt;&lt;h4 id&#x3D;&quot;arctic_boreal_burned_area_v2_2328&quot;&gt;Arctic_Boreal_Burned_Area_V2_2328&lt;/h4&gt;
This dataset provides annual cumulative end-of-season burned area in circumpolar boreal forests and tundra for the years 2002-2022. The data were generated using the Arctic Boreal Burned Area (ABBA) version 2 algorithm with MODIS collection 6 products. The algorithm is based on Normalized Burned Ratio differencing (dNBR) and is designed specifically to capture late season fires. The annual MODIS Vegetation Continuous Fields (VCF) 250-m Collection 5.1 (MOD44B) product allowed for additional vegetation-dependent dNBR thresholds within the algorithm&amp;#39;s processing steps. The spatial domain is circumpolar regions above 50 degrees north latitude. The data are provided in cloud-optimized GeoTIFF format with 463-m resolution.
&lt;br&gt;&lt;h4 id&#x3D;&quot;north_slope_veg_plots_1536&quot;&gt;North_Slope_Veg_Plots_1536&lt;/h4&gt;
This dataset provides vegetation cover and environmental plot and soil data collected at flux tower sites of the North Slope Arctic System Science/Land-Atmosphere-Ice Interactions (ARCSS/LAII) project in August of 1995 and 1996. The 19 ARCSS/LAII flux tower sites are located along a North-South transect from near Prudhoe Bay to the foothills of the Brooks Range on the North Slope of Alaska. At 17 of the flux tower sites, one or more vegetation plots (29 total) were established and measurements including (1) plant species cover for the major vegetation types using the Braun-Blanquet approach, (2) plot environmental data, and (3) soil profile descriptions were recorded. In addition, at all 19 sites, plant growth form composition and cover were surveyed using a point sampling technique along multiple transects within selected plots.
&lt;br&gt;&lt;h4 id&#x3D;&quot;arrigetch_peaks_veg_plots_1358&quot;&gt;Arrigetch_Peaks_Veg_Plots_1358&lt;/h4&gt;
This data set provides environmental and vegetation data collected between 1978 and 1981 from 439 study plots at Arrigetch Peaks research site, located in the Gates of the Arctic National Park and Preserve in the Endicott Mountains of the central Brooks Range, Alaska. Plots varied between 1 and 50 square meters in size and were located in 13 broad habitat types across the glaciated landscape. Environmental data include aspect, elevation, and cover of bare soil, rock, soil crust, and litter. Species data are described according to the Braun-Blanquet system. This product brings together for easy reference all the available information collected from the vegetation plots in the Arrigetch Peaks region of Alaska.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atqasuk_veg_plots_1371&quot;&gt;Atqasuk_Veg_Plots_1371&lt;/h4&gt;
This data set provides vegetation species abundance data collected in 1975 from 60 sites on the Arctic Coastal Plain near Atqasuk, Alaska, as well as environmental and species data for 31 of the sites that were revisited in 2000 and 2010. The study sites are located on Arctic tundra near the Meade River, about 60 miles southwest of Barrow. Data includes baseline plot information for vegetation and site factors for the study plots subjectively located in 9 plant communities. Specific attributes include: site characteristics such as altitude, slope, aspect, and topographic position; soil pH and organic layer depth; and dominant plant communities. This product brings together for easy reference all of the available information collected from the plots that has been used for the classification, mapping, and analysis of geo-botanical factors at the Atqasuk research sites and across Alaska.
&lt;br&gt;&lt;h4 id&#x3D;&quot;frost_boils_veg_plots_1361&quot;&gt;Frost_Boils_Veg_Plots_1361&lt;/h4&gt;
This data set describes the environment, soil, and vegetation on nonsorted circles and earth hummocks at seven study sites along a N-S-transect from the Arctic Ocean to the Arctic Foothills based on data collected from 2000 to 2006. The study sites are located along the Dalton Highway, beginning in Prudhoe Bay, on the North Slope of Alaska. These frost-boil features are important landscape components of the arctic tundra. Data include the baseline plot information for vegetation, soils, and site factors for 117 study plots subjectively located in areas of homogeneous, representative vegetation on frost-heave features surrounding stable tundra. Nine community types were identified in three bioclimate subzones. Vegetation was classified according to the Braun-Blanquet system.
&lt;br&gt;&lt;h4 id&#x3D;&quot;happy_valley_veg_plots_1354&quot;&gt;Happy_Valley_Veg_Plots_1354&lt;/h4&gt;
This dataset provides environmental, soil, and vegetation data collected in July 1994 from 56 study plots at the Happy Valley research site, located along the Sagavanirktok River in a glaciated valley of the northern Arctic Foothills of the Brooks Range. Data includes the baseline plot information for vegetation, soils, and site factors for the study plots subjectively located in 17 plant communities that occur in 5 broad habitat types across the glaciated landscape. Specific attributes include: dominant vegetation species, cover, indices, and biomass pools, soil chemistry, physical characteristics, moisture, and organic matter. This product brings together for easy reference all the available information collected from the plots that has been used for the classification, mapping, and analysis of geo-botanical factors in the Happy Valley region and across Alaska.
&lt;br&gt;&lt;h4 id&#x3D;&quot;imnavait_creek_veg_plots_1356&quot;&gt;Imnavait_Creek_Veg_Plots_1356&lt;/h4&gt;
This dataset provides environmental, soil, and vegetation data collected during the periods of August 1984 and August-September 1985 from 84 study plots at the Imnavait Creek research site. Imnavait Creek is located in a shallow basin at the foothills of the central Brooks Range. Data includes the baseline plot information for vegetation, soils, and site factors for the study plots subjectively located in 14 plant communities that occur in 19 broad habitat types across the glaciated landscape. Specific attributes include: dominant vegetation species, cover, indices, and biomass pools; soil chemistry, physical characteristics, moisture, and organic matter. This product brings together for easy reference all the available information collected from the plots that has been used for the classification, mapping, and analysis of geo-botanical factors in the Imnavait Creek region and across Alaska.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nome_veg_plots_1372&quot;&gt;Nome_Veg_Plots_1372&lt;/h4&gt;
This data set provides environmental, soil, and vegetation data collected in July and August 1951 from 80 study plots in the Nome River Valley about 10 miles northeast of Nome, Alaska on the Seward Peninsula. Data includes the baseline plot information for vegetation, soils, and site factors for the study plots subjectively located in plant communities that were found to occur in 5 broad habitat types across the glaciated landscape. Specific attributes include: dominant vegetation species and cover, and soil characteristics, moisture, and organic matter. This product brings together for easy reference all the available information collected from the plots that has been used for the classification, mapping and analysis of geo-botanical factors in the Nome River Valley and across Alaska.
&lt;br&gt;&lt;h4 id&#x3D;&quot;oumalik_veg_plots_1506&quot;&gt;Oumalik_Veg_plots_1506&lt;/h4&gt;
This data set provides environmental, soil, and vegetation data collected between 1983 and 1985 from 87 study plots near an abandoned test oil well in Oumalik, Alaska. Specific attributes include dominant vegetation, species, and cover, soil chemistry, physical characteristics, moisture, and organic matter, as well as site disturbance from various sources. The vegetation sampling sites were chosen to represent the full range of vegetation in the area with replication, and for uniformity in floristic composition and environmental conditions.
&lt;br&gt;&lt;h4 id&#x3D;&quot;prudhoe_bay_veg_plots_1360&quot;&gt;Prudhoe_Bay_Veg_Plots_1360&lt;/h4&gt;
This data set provides environmental, soil, and vegetation data collected between 1973 and 1980 from 89 study plots in the Prudhoe Bay region of Alaska. Data includes the baseline plot information for vegetation, soils, and site factors for study plots subjectively located in 43 plant communities and 4 broad habitat types across the glaciated landscape. Specific attributes include: dominant vegetation, species, and cover; soil chemistry, physical characteristics, moisture, and organic matter. This product brings together for easy reference all the available information collected from the plots that has been used for classification, mapping, and analysis of geobotanical factors in the Prudhoe Bay region and across Alaska.
&lt;br&gt;&lt;h4 id&#x3D;&quot;toolik_lake_veg_plots_1333&quot;&gt;Toolik_Lake_Veg_Plots_1333&lt;/h4&gt;
This dataset provides environmental, soil, and vegetation data collected in August 1989 from 81 study plots at the Toolik Lake research site, located in the southern Arctic Foothills of the Brooks Range, Alaska. Data includes the baseline plot information for vegetation, soils, and site factors for the study plots subjectively located in 26 communities and 4 broad habitat types across the glaciated landscape. Specific attributes include: dominant vegetation species, cover, indices, and biomass pools; soil chemistry, physical characteristics, moisture, and organic matter. This product brings together for easy reference all the available information collected from the plots that has been used for the classification, mapping, and analysis of geobotanical factors in the Toolik Lake region and across Alaska.
&lt;br&gt;&lt;h4 id&#x3D;&quot;umiat_veg_plots_1370&quot;&gt;Umiat_Veg_Plots_1370&lt;/h4&gt;
This data set provides vegetation cover and plot data collected during the periods of July and August, 1951, from 51 stands (areas of homogeneous vegetation communities) in the the Umiat region of Alaska, on the Colville River. The Umiat area is within the Northern Foothills section of the Arctic Foothills province on the slope north of the Brooks Range. Data include vegetation species, percent cover classes, soil moisture, topographic position, slope, aspect, and plot shape and size.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atlas_veg_plots_1541&quot;&gt;ATLAS_Veg_Plots_1541&lt;/h4&gt;
This data set provides environmental, soil, and vegetation data collected from study sites on the North Slope and Seward Peninsula of Alaska during the Arctic Transition in Land-Atmosphere System (ATLAS) project. ATLAS-1 sites on the North Slope, located in Barrow, Atqasuk, Oumalik, and Ivotuk, were sampled in 1998-1999. ATLAS-2 sites located at Council and Quartz Creek on the Seward Peninsula were sampled in 2000. Specific attributes include dominant vegetation species and cover, biomass, soil chemistry and moisture, leaf area index (LAI), normalized difference vegetation index (NDVI), topography and elevation, and plant cover abundance.
&lt;br&gt;&lt;h4 id&#x3D;&quot;barrow_tundra_veg_plots_1535&quot;&gt;Barrow_Tundra_Veg_Plots_1535&lt;/h4&gt;
This data set provides vegetation cover and environmental plot data collected as part of the International Biological Program (IBP), U. S. Tundra Biome Program, in Barrow, Alaska in 1972. Forty-three (43) plots were assessed for estimated percent land cover by species and plot data including moisture, topographic position, slope, aspect, shape, and soil data. In 1999, 2008, and 2010, 33 of the same plots were resampled for these same measures as part of the IPY &amp;quot;Back to the Future: Resampling old research sites to assess changes in high latitude terrestrial ecosystem structure and function&amp;quot; project. The tundra at Barrow is considered coastal tundra located in the most northern region of North Slope and is characterized by various microtopographic features such as polygons, as well as many ponds and lakes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;barrow_ngee_arctic_veg_plots_1505&quot;&gt;Barrow_NGEE_Arctic_Veg_Plots_1505&lt;/h4&gt;
This data set provides vegetation cover and environmental plot data collected on the Barrow Environmental Observatory (BEO), Barrow, Alaska in 2012. Forty-eight 1 x 1 m plots were established in homogenous plant communities along two perpendicular transects across ice wedge polygon geomorphic features on the BEO. Plots were distinguished as to their location within the polygons as center, edge, or trough. Vegetation data were originally collected by the U.S. Department of Energy (DOE) Next-Generation Ecosystem Experiment (NGEE) Arctic Project as part of a larger study to understand the response of Arctic terrestrial ecosystems to climate change.
&lt;br&gt;&lt;h4 id&#x3D;&quot;pingo_veg_plots_1507&quot;&gt;Pingo_Veg_Plots_1507&lt;/h4&gt;
This data set provides vegetation species and vegetation plot data collected between 1983 and 1985 from 293 study plots on 41 pingos on the North Slope of Alaska. The pingos were located within the Arctic Coastal Plain in the Kuparuk, Prudhoe Bay, Kadleroshilik, and Toolik River areas. Specific attributes include dominant vegetation species, cover, soil pH, moisture, and physical characteristics of the plots.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tundra_fire_veg_plots_1547&quot;&gt;Tundra_Fire_Veg_Plots_1547&lt;/h4&gt;
This dataset provides environmental and vegetation data collected in late June and July of 2011 and of 2012 from study plots located in tundra fire scars and adjacent unburned tundra areas on the Seward Peninsula and the northern foothills of the Brooks Range in Arctic Alaska. The surveys focused on upland tundra settings and provide information on vegetative differences between the burned and unburned sites. The sampling design established a chronosequence of sites that varied in time since last fire to better understand post-fire vegetation successional trajectories. Complete species lists and their cover abundance data are provided for both study areas. Environmental data include the baseline plot descriptive information for vegetation, soils, and site factors. No soil samples were collected.
&lt;br&gt;&lt;h4 id&#x3D;&quot;flux_tower_zona_veg_plots_1546&quot;&gt;Flux_Tower_Zona_Veg_Plots_1546&lt;/h4&gt;
This data set provides vegetation, environmental, and soil data collected from plots located in the footprints of eddy covariance flux towers along a 300 km north-south latitudinal gradient from Barrow, to Atqasuk, and to Ivotuk across the North Slope of Alaska in 2014. Within each of the five flux tower footprints, 1x1-m quadrats were placed subjectively within widespread habitat or micro-habitat types to map the dominant vegetation communities and site environmental factors. Specific attributes included species cover data and environmental, soil and spectral data (active layer thaw depth, moss layer depth, organic horizon layer depth, standing water depth, soil moisture status, vegetation height, LAI).
&lt;br&gt;&lt;h4 id&#x3D;&quot;canadian_west_arctic_veg_plots_1543&quot;&gt;Canadian_West_Arctic_Veg_Plots_1543&lt;/h4&gt;
This dataset provides vegetation, soil, and plot characteristics for 154 study plots located at three sites across the Richardson Mountains, Northwest Territories (NWT), and the British Mountains, Yukon Territory (YT). Study sites in the NWT included areas near Canoe Lake and Divided Lake; the study site in the YT was near Trout Lake. Specific attributes include dominant vegetation, species cover, and the physical characteristics of the plot areas. A soil pit was dug at each plot and the physical and chemical characteristics were determined for soil horizons. The data were collected in June, July, and August of 1965 and July and August of 1966.
&lt;br&gt;&lt;h4 id&#x3D;&quot;arctic_network_veg_plots_1542&quot;&gt;Arctic_Network_Veg_plots_1542&lt;/h4&gt;
This dataset provides environmental, soil, and vegetation data collected at selected locations in the parks and preserves of the National Park Service (NPS) Arctic Network (ARCN) between 2002 and 2008. The ARCN includes five national parks and preserves in northern Alaska encompassing 19.5 million acres and represents some of the wildest, most undisturbed areas left on earth: The Bering Land Bridge National Preserve, Cape Krusenstern National Monument, Gates of the Arctic National Park and Preserve, Kobuk Valley National Park, and the Noatak National Preserve. The sampling sites were chosen to represent the full range of vegetation in the area with replication, and for uniformity in floristic composition and environmental conditions and were positioned on transects along toposequences within major physiographic units (riverine, lacustrine, lowland, upland, subalpine and alpine). Specific attributes include dominant vegetation, species, and cover, soil chemistry, physical characteristics, moisture, and organic matter, as well as site disturbance from various sources.
&lt;br&gt;&lt;h4 id&#x3D;&quot;willow_veg_plots_1368&quot;&gt;Willow_Veg_Plots_1368&lt;/h4&gt;
This data set provides environmental, soil, and vegetation data collected in July and August 1997 from 85 study plots in willow shrub communities located along a north-south transect from the Brooks Range to Prudhoe Bay on the North Slope of Alaska. Data includes the baseline plot information for vegetation, soils, and site factors for the study plots subjectively located in three broad habitat types across the glaciated landscape. Specific attributes include: dominant vegetation species, cover, indices, and biomass pools; soil chemistry, physical characteristics, moisture, and organic matter. This product brings together for easy reference all the available information collected from the plots that has been used for the classification, mapping, and analysis of geobotanical factors in the region and across Alaska.
&lt;br&gt;&lt;h4 id&#x3D;&quot;barter_barrow_veg_plots_1534&quot;&gt;Barter_Barrow_Veg_Plots_1534&lt;/h4&gt;
This dataset provides vegetation cover and environmental plot and soil data collected at two U.S. Air Force sites at Barter Island (BI) and Point Barrow (B), on the coastal North Slope of Alaska, in 1994. At Barter Island, 31 plots, and 30 plots at Barrow, were subjectively located in 14 plant communities. The investigation was part of a larger study initiated by the United States Congress to provide an opportunity to enhance the stewardship of the natural and cultural resources land under Department of Defense jurisdiction. These two sites were characterized to build an inventory of the biotic communities to compare them to historic communities.
&lt;br&gt;&lt;h4 id&#x3D;&quot;unalaska_veg_plots_1375&quot;&gt;Unalaska_Veg_Plots_1375&lt;/h4&gt;
This data set provides environmental, soil, and vegetation data collected during August 2007 from 69 study plots at the Unalaska Island research site, and one plot on Amaknak Island. The study sites are within the eastern Aleutian Islands, Alaska, USA. Data includes the plot information for vegetation, soils, and site characteristics for the study plots subjectively located in 11 plant communities that occur in six broad habitat types. Specific attributes include: dominant vegetation species and cover, soil chemistry, moisture, organic matter, topography, and elevation. Cover-abundance was estimated for all vascular plants, bryophytes, and macrolichens according to the nine-point ordinal scale of Westhoff and van der Maarel (1973).
&lt;br&gt;&lt;h4 id&#x3D;&quot;poplar_veg_plots_1376&quot;&gt;Poplar_Veg_Plots_1376&lt;/h4&gt;
This data set provides vegetation cover and environmental plot data collected from 32 balsam poplar (Populus balsamifera L., Salicaceae) vegetation plots located on the Arctic Slope of Alaska and in the interior boreal forests of Alaska and the Yukon from 2003 to 2005. The estimated percent land cover by species per plot are according to the older Braun-Blanquet cover-abundance scale. Plot data includes moisture, topographic position, slope, aspect, shape, and soil data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;prudhoe_bay_arcsees_veg_plots_1555&quot;&gt;Prudhoe_Bay_ArcSEES_Veg_Plots_1555&lt;/h4&gt;
This dataset provides environmental, soil, and vegetation data collected from study plots in the vicinity of Lake Colleen off the Spine Road at Prudhoe Bay, Alaska, during August of 2014. Data include vegetation species, leaf area index (LAI), percent cover classes, soil moisture and color, and plot characteristics including geology, topographic position, slope, aspect, and plot disturbance.
&lt;br&gt;&lt;h4 id&#x3D;&quot;landcover_great_lakes_basin_2440&quot;&gt;LandCover_Great_Lakes_Basin_2440&lt;/h4&gt;
This dataset holds maps of land cover and wetland ecotype for the Great Lakes Basin (GLB) circa 2010. The data were derived from multi-season L-band SAR, Landsat 5 optical imagery, and thousands of field training data samples. The dataset includes detailed landcover maps of shorelines of each of five Great Lakes along with a land cover map of the entire GLB. This is the first binational map of the GLB that specifically depicts native wetland ecotypes and monocultures of invasive wetland plants (Phragmites australis and Typha spp.). The goal of the effort was to improve understanding of nutrient flow and transport of water across the landscape to the coasts and the processes at the land-water interface in wetland ecosystems that lead to the success of invasive species. The data are provided in Cloud-optimized GeoTIFF (COG), shapefile, comma separated values (CSV), and text file formats. An associated report is included in PDF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;plot_data_noatak_seward_ak_1919&quot;&gt;Plot_Data_Noatak_Seward_AK_1919&lt;/h4&gt;
This dataset includes field measurements from unburned and burned 10 m x 10 m and 1 m x 1 m plots in the Noatak, Seward, and North Slope regions of the Alaskan tundra during July through August in the years 2016-2018. The data include vegetation coverage, soil moisture, soil temperature, soil thickness, thaw depth, and weather measurements. Measurements were recorded using ocular assessments and standard equipment. Plot photographs are included.
&lt;br&gt;&lt;h4 id&#x3D;&quot;arctic_vegetation_maps_1323&quot;&gt;Arctic_Vegetation_Maps_1323&lt;/h4&gt;
This data set provides the spatial distributions of vegetation types, geobotanical characteristics, and physiographic features for the circumpolar Arctic tundra biome for the period 1982-2003. Specific attributes include dominant vegetation, bioclimate subzones, floristic subprovinces, landscape types, lake coverage, Arctic treeline, elevation, and substrate chemistry data. Vegetation indices, trends, and biomass estimate products for the circumpolar Arctic through 2010 are also provided.
&lt;br&gt;&lt;h4 id&#x3D;&quot;boreal_agb_density_icesat2_v3_2437&quot;&gt;Boreal_AGB_Density_ICESat2_V3_2437&lt;/h4&gt;
This dataset provides estimates of aboveground dry woody biomass density (AGBD) and vegetation height for high northern latitude forests at a 30-m spatial resolution for the year 2020, accounting for &amp;gt;30% of global forest area. The estimates were derived with state-of-the-art earth observation datasets collected from space, including lidar observations from NASA&amp;#39;s ICESat-2 and imagery from NASA&amp;#39;s Harmonized Landsat/Sentinel-2 project. They are designed for circumpolar boreal-wide mapping from local to global scales and provide the northern component of global forest structure estimates, to which complementary estimates from NASA&amp;#39;s Global Ecosystem Dynamics Investigation (GEDI) mission contribute temperate and tropical portions. The AGBD and height predictions cover the extent of high latitude boreal forests and shrublands, and while they extend southward outside the boreal domain nominally to ~50 degrees N they are intended to contribute to global estimates northward from 51.6 degrees N.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ch4_co2_waterbodies_yk_delta_2178&quot;&gt;CH4_CO2_WaterBodies_YK_Delta_2178&lt;/h4&gt;
This dataset provides estimates of carbon dioxide (CO2) and methane (CH4) diffusive fluxes from waterbodies, and watershed landcover data for the central-interior of the Yukon-Kuskokwim Delta (YK delta), Alaska. Dissolved concentrations of methane and carbon dioxide were predicted using an integrated terrestrial-aquatic approach to scale observations based on landscape and waterbody remote sensing drivers. The observations include &lt;del&gt;300 samples of surface water dissolved gases collected in July 2016-2019 from the central region of the YK Delta, Alaska. A machine learning model was used to generate estimated fluxes. Model inputs include Sentinel-2 MSI with derived normalized difference vegetation index (NDVI) and normalized difference water index (NDWI), an Arctic digital elevation model (DEM) with derived slope and flow accumulation, Sentinel-1 C-band July and December VV and VH composites, and a landcover map. Waterbody size, shape, and reflectance were determined using object-based image analysis in Google Earth Engine. Landscape-level input data were averaged in non-nested sub-basins calculated using the System for Automated Geoscientific Analyses (SAGA) &amp;quot;channel network&amp;quot; algorithm at three threshold sizes. Cross validation was used to tune and select variables for gradient boosting models. The trained gradient boosting models were then used to predict dissolved methane and carbon dioxide in all waterbodies (&lt;/del&gt;17,000) in the region. These aquatic concentrations were converted to fluxes using an average gas transfer velocity from observations (0.33 m/d). The data are provided in GeoTIFF and shapefile formats.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_snowmodel_data_2105&quot;&gt;ABoVE_SnowModel_Data_2105&lt;/h4&gt;
This dataset provides daily SnowModel simulation outputs on a 3-km grid for the period 1 September 1980 through 31 August 2020, covering the Core ABoVE Domain. The daily outputs include: air temperature (deg C), relative humidity (%), wind speed (m/s), wind direction (deg from True North), total precipitation (rain+snow) (m), rainfall (m), snowfall (m), snow melt (m), snow sublimation (m), runoff (m), surface temperature (deg C), bulk snowpack thermal resistance (K/W), snow depth (m), snow density (kg/m3), and snow-water-equivalent (SWE) depth (m). Model data inputs included land cover and topography, ground-based observations of snow, remote sensing observations of snow from satellites and aircraft, and meteorological forcing data from weather stations and reanalysis data. The SnowModel includes the processing modules MicroMet, Enbal, SnowDunes, SnowAssin, SnowPack, and SnowTran-3D. The data are provided in NetCDF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deciduousfractionl_canopycover_2296&quot;&gt;DeciduousFractionl_CanopyCover_2296&lt;/h4&gt;
This dataset holds deciduous fraction and tree canopy cover at 30-m resolution over the North American boreal domain for 1992 to 2015. Deciduous fraction is the areal percentage of deciduous trees relative to all tree canopy cover within a pixel, and tree canopy cover is the areal percentage of a pixel that is covered by tree canopy. Deciduous fraction values are valid only for pixels with tree canopy cover &amp;gt;25 percent. Normalized difference vegetation index (NDVI)-based median-value image composites were derived from Landsat 5, 7, and 8 Collection 1 surface reflectance datasets for years 1987-1997, 1998-2002, 2003-2007, 2008-2012, and 2013-2018 to create composites for nominal years 1992, 2000, 2005, 2010, and 2015, respectively. These image composites were prepared for early spring, mid-summer, and mid-to-late fall seasons to identify key differences in deciduous and evergreen green-up amplitudes. Random Forest (RF) regression models were used to derive deciduous fraction and tree canopy cover from the image composites. These models were trained with data from in-situ samples across Alaska and Canada from a variety of studies. Seventy percent of the in-situ samples were used for training and 30% for validation. Per-pixel uncertainty for both deciduous fraction and tree canopy cover are included and were based on one standard deviation of output values across all decision trees in the RF regression. These datasets were developed as part of NASA&amp;#39;s ABoVE project to capture forest composition changes over the North American boreal domain across the last several decades. The data are provided in GeoTIFF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;arctictreeline_dendrometry_env_2185&quot;&gt;ArcticTreeLine_Dendrometry_Env_2185&lt;/h4&gt;
This dataset provides in situ measurements of radial tree growth of selected white spruce (Picea glauca) and black spruce (Picea mariana) trees, as well as simultaneous in situ measurements of environmental variables (air temperature, air pressure, relative humidity, soil temperature, volumetric water content, and solar irradiance) at two Arctic treeline sites: one in the Brooks Range of Alaska (AK), USA, and the other near Inuvik, Northwest Territories (NWT), Canada. In AK, 36 trees were monitored from June 7, 2016 to September 13, 2019, and in NWT, 24 trees were monitored from July 5, 2017 to July 25, 2019 with a sampling interval of 5- or 20-minutes for radial tree growth and 5-minutes for all environmental variables. The dendrometer data included in this dataset are only those gathered from 2016-2017. Dendrometer data from 2018-2019 are available from a related dataset. The data were collected to better understand the influence of environmental variables on radial tree growth dynamics. The data are provided in comma-separated values (CSV) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;fielddata_alaska_tundra_2177&quot;&gt;FieldData_Alaska_Tundra_2177&lt;/h4&gt;
This dataset, titled the Synthesized Alaskan Tundra Field Database (SATFiD), provides a comprehensive collection of in-situ field data compiled from 37 existing datasets resulting from field surveys conducted at Alaska tundra sites between 1972 to 2020. The data were harmonized prior to being included in this dataset. The variables include active layer thickness, vegetation cover (by plant functional types), soil moisture and temperatures, as well as the wildfire history. SATFiD provides a unique lens into various long-term ecological processes within the tundra (such as the fire-permafrost-vegetation interactions) under a rapidly changing climate.
&lt;br&gt;&lt;h4 id&#x3D;&quot;prudhoe_bay_veg_maps_1387&quot;&gt;Prudhoe_Bay_Veg_Maps_1387&lt;/h4&gt;
This data set provides a collection of maps of geoecological characteristics of areas within the Beechey Point quadrangle near Prudhoe Bay on the North slope of Alaska: a geobotanical atlas of the Prudhoe Bay region, a land cover map of the Beechey Point quadrangle, and cumulative impact maps in the Prudhoe Bay Oilfield for ten dates from 1968 to 2010. The geobotanical atlas is based on aerial photographs and covers 145 square kilometers of the Prudhoe Bay Oilfield. The land cover map of the Beechey Point quadrangle was derived from the Landsat multispectral scanner, aerial photography, and other field and cartographic methods. The cumulative impact maps of the Prudhoe Bay Oilfield show historical infrastructure and natural changes digitized from aerial photos taken in each successive analysis year (1968, 1970, 1972, 1973, 1977, 1979, 1983, 1990, 2001, and 2010). Nine geoecological attributes are included: dominant vegetation, secondary vegetation, tertiary vegetation, percentage open water, landform, dominant surface form, secondary surface form, dominant soil, and secondary soil. These data document environmental changes in an Arctic region that is affected by both climate change and rapid industrial development.
&lt;br&gt;&lt;h4 id&#x3D;&quot;geocryoai_permafrostthaw_cflux_2371&quot;&gt;GeoCryoAI_PermafrostThaw_CFlux_2371&lt;/h4&gt;
This dataset provides model code, input data, sample results, and documentation for an artificial intelligence-driven model, GeoCryoAI. GeoCryoAI is a hybridized process-constrained ensemble learning framework consisting of stacked convolutionally layered long short-term memory-encoded recurrent neural networks. The purpose of GeoCryoAI is to quantify permafrost thaw dynamics and greenhouse gas emissions in Alaska. The dataset includes pre-processed input data (i.e., thaw depth, active layer thickness, thaw subsidence; CO2 flux, CH4 flux) acquired from in situ measurements (e.g., CALM, GTNP, ITEX, SMALT STDM, ReSALT, AmeriFlux, NEON), remote sensing platforms (e.g., UAVSAR, AVIRIS-NG), and process-based modeling products. Field data were included to quantify CO2 and CH4 flux (e.g., chamber, eddy-covariance, and tall-tower measurements via flux tower networks) and active layer thickness (e.g., mechanical probing, borehole temperatures, ground-penetrating radar). These measurements were resampled to a 1-km grid, standardized, transformed, and assimilated into GeoCryoAI, a framework that simultaneously ingests, scales, and analyzes input data after resolving disparate spatiotemporal sampling and data densities. Model outputs were generated from two process-based models: SIBBORK-TTE derived thaw subsidence and TCFM-Arctic generated carbon flux outputs. The objective was to quantify how the Arctic is changing in response to climate change and how evidence of the permafrost carbon feedback may contribute toward a better understanding of the uncertainty of nonlinear feedbacks and their impact on the earth system.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_co2_ch4_flux_estimates_2121&quot;&gt;ABoVE_CO2_CH4_Flux_Estimates_2121&lt;/h4&gt;
This dataset provides gridded estimates of gross primary productivity (GPP), ecosystem respiration (Reco), net ecosystem CO2 exchange (NEE &#x3D; Reco - GPP), and methane (CH4) emissions from tundra and boreal wetland soils, across the pan-Arctic and Boreal zone (&amp;gt;49 degrees north) at 1-km spatial resolution. The data were produced through simulations of the Arctic Terrestrial Carbon Flux Model (TCFM-Arctic) and are provided at the daily time step for the years 2003-2015. TCFM-Arctic uses a light-use efficiency approach driven by satellite estimates of FPAR (fraction of absorbed photosynthetically active radiation) to estimate GPP, and autotrophic respiration (Rauto) is estimated as a fraction of GPP. Heterotrophic respiration (Rhetero) is estimated using decomposition rates with environmental constraints applied to three near-surface soil organic carbon (SOC) pools, and Reco is determined as the sum of Ra and Rh. Methane production is estimated using optimal CH4 production rates with environmental constraints applied to the labile carbon pool, and transfer of CH4 from the soil to the atmosphere is modeled through vegetation, soil diffusion, and water ebullition pathways. The model estimates were calibrated and evaluated using &amp;gt;60 tower eddy covariance (EC) sites. Baseline carbon pools were initialized by continuously cycling (spinning-up) the model for 1,000 model years using recent climatology from 1985 to 2002 to reach a dynamic steady-state between estimated net primary productivity (NPP &#x3D; GPP - Rauto) and near-surface SOC pools. The TCFM-Arctic simulations were extended to the full Arctic-boreal domain at a 1-km spatial resolution using land cover maps representing high latitude vegetation communities. The data are provided in NetCDF and comma-separated values (CSV) formats.
&lt;br&gt;&lt;h4 id&#x3D;&quot;soil_carbon_flux_maps_1683&quot;&gt;Soil_Carbon_Flux_Maps_1683&lt;/h4&gt;
This dataset provides gridded estimates of soil CO2 flux (g C m-2 d-1) for the winter non-growing season (NGS) across pan-Arctic and Boreal permafrost regions (&amp;gt;49 Deg N), at 25 km spatial resolution. The data are the daily average flux over a monthly period for two climate periods: the baseline climate period represents 2003-2018 and the future climate scenarios period represents 2018-2100 under Representative Concentration Pathways (RCP) 4.5 and 8.5. The data were produced by applying a Boosted Regression Tree machine learning approach to create gridded estimates of emissions based on in situ observations of NGS fluxes provided in a related dataset. The resulting monthly average flux data records can be used to calculate annual NGS soil CO2 flux budgets from 2003-2100.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vegetation_photos_toolik_lake_1718&quot;&gt;Vegetation_Photos_Toolik_Lake_1718&lt;/h4&gt;
This dataset contains 731 ground-based nadir vegetation community and ground surface photographs of selected field plots taken as ground reference data for vegetation classification studies at three areas near Toolik Lake, Alaska during the summers of 2014 and 2015. The largest area, &amp;#39;Toolik&amp;#39;, (approximately 6 km2) covers research areas near Toolik Field Station at Toolik Lake, including Arctic LTER installations. The other two areas are each roughly 3 km2: the &amp;#39;Pipeline&amp;#39; area: a stretch of the Trans-Alaska Pipeline, and the &amp;#39;Imnavait&amp;#39; area: along Imnavait Creek roughly 10 km east of Toolik Lake.
&lt;br&gt;&lt;h4 id&#x3D;&quot;shrub_biomass_toolik_lake_ak_1573&quot;&gt;Shrub_Biomass_Toolik_Lake_AK_1573&lt;/h4&gt;
This dataset contains estimates for aboveground shrub biomass and uncertainty at high spatial resolution (0.80-m) across three research areas near Toolik Lake, Alaska. The estimates for August of 2013 were generated and mapped using Random Forest modeling with input variables of optimized LiDAR-derived canopy volume and height, mean NDVI from 4-band RGB color and near-IR orthophotographs, and harvested biomass data. Uncertainty in the final shrub biomass maps was quantified by producing separate maps showing the coefficient of variation (CV) of the Random Forest map estimates. Shrub biomass was harvested at Toolik Lake in 2014 and used to optimize inputs and validate the final model and these biomass data are also provided.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vegetation_maps_toolik_lake_1690&quot;&gt;Vegetation_Maps_Toolik_Lake_1690&lt;/h4&gt;
This dataset contains vegetation community maps at 20 cm resolution for three landscapes near the Toolik Lake research area in the northern foothills of the Brooks Range, Alaska, USA. The maps were built using a Random Forest modeling approach using predictor layers derived from airborne lidar data and high-resolution digital airborne imagery collected in 2013, and vegetation community training data collected from 800 reference field plots across the lidar footprints in 2014 and 2015. Vegetation community descriptions were based on the commonly used classifications of existing Toolik area vegetation maps.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lakebathymetry_model_nslope_ak_2243&quot;&gt;LakeBathymetry_Model_NSlope_AK_2243&lt;/h4&gt;
This dataset provides lake bathymetry maps derived from Landsat surface reflectance products for a portion of the North Slope area of Alaska. A random forest regression algorithm was used to generate depths for each point identified as being part of a lake, creating depth prediction files for each Landsat scene available for the study period: 2016-07-01 to 2018-08-31. These products are fitted to the ABoVE standard projection and reference grid to make them easily scalable and geometrically compatible with other products in the ABoVE study domain. The data are provided in cloud-optimized GeoTIFF (COG) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lakes_ponds_inundation_ykdelta_2450&quot;&gt;Lakes_Ponds_Inundation_YKDelta_2450&lt;/h4&gt;
This dataset provides high resolution (3 m) maps delineating open water and partial inundation in the Yukon-Kuskokwim Delta (YKD), Alaska, and a database that tracks rapid changes in surface area for individual lakes and ponds over 2019-2023. The dataset was built using daily PlanetScope imagery (3 m), allowing for tracking changes in surface water extent at high spatial and temporal resolutions. Two types of maps were produced; (1) open water lakes and ponds and (2) partial inundation, defined as areas that partially contain water (e.g. emergent vegetation, flooded vegetation, or saturated soil). Open water lakes and ponds were mapped using a convolutional neural network, and partial inundation was classified using a pixel-based thresholding approach. For both map categories, monthly climatological composites for the snow and ice-free period are provided. For open water lake and pond maps, monthly composites are provided as well. An accompanying database includes the geometry and surface area time series for each mapped water body.
&lt;br&gt;&lt;h4 id&#x3D;&quot;northern_alaska_veg_maps_1359&quot;&gt;Northern_Alaska_Veg_Maps_1359&lt;/h4&gt;
This data set provides four land cover and ecosystem classification maps for northern Alaska. The maps were produced for several projects and from different data sources including Landsat imagery and existing maps and models, and cover a range of ecosystem and vegetation classes. The data used to derive the maps covered the period 1976-08-04 to 2014-09-01.
&lt;br&gt;&lt;h4 id&#x3D;&quot;seward_peninsula_veg_maps_1363&quot;&gt;Seward_Peninsula_Veg_Maps_1363&lt;/h4&gt;
This data set provides two landcover and vegetation maps for the Seward Peninsula, Alaska. These maps were produced from existing maps, Landsat imagery, and color infrared aerial photography covering the period 1976-06-01 to 1999-09-01.
&lt;br&gt;&lt;h4 id&#x3D;&quot;arctic_wildlife_refuge_veg_map_1384&quot;&gt;Arctic_Wildlife_Refuge_Veg_Map_1384&lt;/h4&gt;
This data set provides a landcover map with 16 landcover classes for the northern coastal plain of the the Arctic National Wildlife Refuge (ANWR) on the North Slope of Alaska. The map was derived from Landsat Thematic Mapper (Landsat TM) data, Digital Elevation Models (DEMs), aerial photographs, existing maps, and extensive ground-truthing. The data used to derive the map cover the period 1982 to 1993.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_domain_projected_lulc_2353&quot;&gt;ABoVE_Domain_Projected_LULC_2353&lt;/h4&gt;
This dataset provides projections of land use and land cover (LULC) change within the Arctic Boreal Vulnerability Experiment (ABoVE) domain, spanning from 2015 to 2100 with a spatial resolution of 0.25 degrees. It includes LULC change under two Shared Socioeconomic Pathways (SSP126 and SSP585) derived from Global Change Analysis Model (GCAM) at an annual scale. The specific land types include: needleleaf evergreen tree-temperate, needleleaf evergreen tree-boreal, needleleaf deciduous tree-boreal, broadleaf evergreen tree-tropical, broadleaf evergreen tree-temperate, broadleaf deciduous tree-tropical, broadleaf deciduous tree-temperate, broadleaf deciduous tree-boreal, broadleaf evergreen shrub-temperate, broadleaf deciduous shrub-temperate, broadleaf deciduous shrub-boreal, C3 arctic grass, C3 grass, C4 grass, and C3 unmanaged rainfed crop. The data were generated by integrating regional LULC projections from GCAM with high-resolution MODIS land cover data and applying two alternative spatial downscaling models: FLUS and Demeter. Data are provided in NetCDF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lvisc1b&quot;&gt;LVISC1B&lt;/h4&gt;
This data set contains Level-1B geolocated return energy waveforms collected by the NASA Land, Vegetation, and Ice Sensor (LVIS) Facility, an imaging lidar and camera sensor suite.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lvisc2&quot;&gt;LVISC2&lt;/h4&gt;
This data set contains Level-2 geolocated surface elevation and canopy height measurements collected by the NASA Land, Vegetation, and Ice Sensor (LVIS) Facility, an imaging lidar and camera sensor suite.
&lt;br&gt;&lt;h4 id&#x3D;&quot;co2fluxes_arctic_boreal_domain_2377&quot;&gt;CO2Fluxes_Arctic_Boreal_Domain_2377&lt;/h4&gt;
This dataset provides gridded estimates of gross primary productivity (GPP), ecosystem respiration (Reco), and net ecosystem CO2 exchange (NEE) across the circumpolar terrestrial Arctic-boreal region at a 1-km spatial resolution. Monthly CO2 flux data from 2001 to 2020 were generated using terrestrial eddy covariance and chamber CO2 flux observations, combined with geospatial meteorological, remote sensing, topographical and soil data, all within a random forest modeling framework. Aggregated average annual NEE, average annual NEE with direct fire emissions added based on the Global Fire Emissions Database (GFED) product, and temporal trends in annual NEE rasters over 2002-2020 are also included. The data are provided in NetCDF and GeoTIFF formats.
&lt;br&gt;&lt;h4 id&#x3D;&quot;imnavait_creek_veg_maps_1385&quot;&gt;Imnavait_Creek_Veg_Maps_1385&lt;/h4&gt;
This dataset provides the spatial distribution of vegetation types, soil carbon, and physiographic features in the Imnavait Creek area, Alaska. Specific attributes include vegetation, percent water, glacial geology, soil carbon, a digital elevation model (DEM), surficial geology and surficial geomorphology. Data are also provided on the research grids for georeferencing. The map data are from a variety of sources and encompass the period 1970-06-01 to 2015-08-31.
&lt;br&gt;&lt;h4 id&#x3D;&quot;kuparuk_veg_maps_1378&quot;&gt;Kuparuk_Veg_Maps_1378&lt;/h4&gt;
This data set provides a collection of vegetation, landscape, geobotanical, elevation, hydrology, and geologic maps for the Kuparuk River Basin, North Slope, Alaska. The maps cover either (1) the entire Kuparuk River Basin, from the headwaters on the north side of the Brooks Range to the Beaufort Sea coast, or (2) the selected Upper Kuparuk River Region including the Toolik Lake and Imnavait Creek research areas. The maps were produced from imagery and existing geobotanical maps covering the period 1976-08-04 to 2008-12-31.
&lt;br&gt;&lt;h4 id&#x3D;&quot;toolik_lake_area_veg_maps_1380&quot;&gt;Toolik_Lake_Area_Veg_Maps_1380&lt;/h4&gt;
This data set provides the spatial distributions of vegetation types, soil carbon, and physiographic features in the Toolik Lake area, Alaska. Specific attributes include vegetation, percent water, glacial geology, soil carbon, a digital elevation model (DEM), surficial geology and surficial geomorphology.
&lt;br&gt;&lt;h4 id&#x3D;&quot;north_slope_transect_veg_maps_1386&quot;&gt;North_Slope_Transect_Veg_Maps_1386&lt;/h4&gt;
This dataset includes vegetation cover maps, Normalized Difference Vegetation Index (NDVI) maps, snow depth and thaw depth data that were obtained as part of a biocomplexity project on the North Slope of Alaska, USA, and the Northwest Territories (NWT), Canada. In Alaska, seven sites are located along the Dalton Highway and in the Prudhoe Bay Oilfield area, forming a transect across the climate gradient of the North Slope. From South to North, the sites are Happy Valley, Sagwon (an acidic and nonacidic site), Franklin Bluffs, Deadhorse, West Dock and Howe Island. Four sites are in the NWT, forming a latitudinal gradient from South to North; the sites include Inuvik, Green Cabin, Mould Bay, and Isachsen.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ch4_fluxes_thermokarstlakes_ak_1870&quot;&gt;CH4_Fluxes_ThermokarstLakes_AK_1870&lt;/h4&gt;
This dataset provides methane fluxes from hot-spot and non-hot spot differing surfaces at Big Trail Lake (BTL) in the Goldstream Valley near Fairbanks, AK, USA. Measurements were taken at a remotely-sensed methane hotspot on the shoreline of a pond, adjacent to BTL with a Los Gatos Ultra-Portable Greenhouse Gas Analyzer (UGGA), and from various non-hotspot surfaces representative of the broader thermokarst lake ecosystem with bucket chambers. All data were collected between 2019-07-04 and 2019-12-04 during the daytime hours of 09:35-17:32 local time. A ground-based CH4 enhancement survey was performed on 2019-07-06 between 13:25-17:15 Alaska Daylight Time (AKDT), approximately two hours following an AVIRIS-NG overflight and hotspot detection at the Eastside Pond. Methane flux is reported in units of both mmol CH4 m-2 hr-1 and mg CH4 m-2 d-1. Flux errors are quantified for each
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_annual_veg_resilience_2374&quot;&gt;ABoVE_Annual_Veg_Resilience_2374&lt;/h4&gt;
This dataset provides estimates of vegetation resilience in the Arctic Boreal Vulnerability Experiment (ABoVE) core domain at annual time steps for 2000-2019 and at 300-m spatial resolution. Vegetation resilience is defined as the recovery rate from deviations, due to climate perturbations or disturbances, to the equilibrium state. It is quantified as the negative temporal lag-1 autocorrelation of Enhanced Vegetation Index (EVI). Using a time series of MODIS EVI, the vegetation resilience was estimated using a Bayesian dynamic linear model. The mapped vegetation resilience was derived from Terra EVI products (MOD13Q1v061) across 175 ABoVE B grid tiles over the ABoVE core domain. The estimated mean resilience, upper boundary, and lower boundary results are provided for each tile in cloud optimized GeoTIFF (COG) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ndvi_forest_structure_1797&quot;&gt;NDVI_Forest_Structure_1797&lt;/h4&gt;
This dataset provides leaf area index (LAI), tree species and canopy cover, normalized difference vegetation index (NDVI), and NDVI trends for boreal forests in interior Alaska, U.S. These data were collected to investigate NDVI trends with forest structure and composition as influenced by disturbance and succession. The data are from 102 sites surveyed in 2017 and 2018 and include locations with and without a fire since 1940. A time series of NDVI was developed from Landsat (1999-2018) to measure NDVI trends. The field data cover the period 2017-08-29 to 2018-08-20. The surveyed forest stands spanned a distance of over 425 km across interior Alaska. The sites were selected before visiting the field to include locations with and without a fire since 1940. Recently burned sites were selected to span a range of years since fire, while sites without a recent fire were selected to include a range of Landsat NDVI trends. For each year, the median NDVI during the growing season was calculated. Then, a simple linear regression trend was calculated for years 1999-2018.
&lt;br&gt;&lt;h4 id&#x3D;&quot;passive_microwave_snowoff_data_1711&quot;&gt;Passive_Microwave_Snowoff_Data_1711&lt;/h4&gt;
This dataset provides annual maps of the snowoff (SO) date from 1988-2023 across Alaska and parts of Far East Russia and northwest Canada at a resolution of 6.25 km. SO date is defined as the last day of persistent snow and was derived from the MEaSUREs Calibrated Enhanced-Resolution Passive Microwave (PMW) EASE-Grid Brightness Temperature (Tb) Earth System Data Record (ESDR) product. The spatial domain was intended to match MODIS Alaska Snow Metrics and extend its temporal fidelity beyond the MODIS era. SO date estimates were compared to snow depth measurements collected at SNOTEL stations across Alaska and to three SO datasets derived from MODIS, Landsat, and the Interactive Multisensor Snow and Ice Mapping System (IMS). The data from 1988-2016 included a coastal mask removing coastal pixels due to potential water contamination from coarse brightness temperature observations (Dersken et al., 2012).
&lt;br&gt;&lt;h4 id&#x3D;&quot;post_fire_soc_nwt_2235&quot;&gt;Post_Fire_SOC_NWT_2235&lt;/h4&gt;
This dataset provides site moisture, soil organic layer thickness, soil organic carbon, nonvascular plant functional group, stand dominance, ecozone, time-after-fire, jack pine proportion, and deciduous proportion for 511 forested plots spanning ~140,000 km2 across two ecozones of the Northwest Territories, Canada (NWT). The plots were established during 2015-2018 across 41 wildfire scars and unburned areas (no burn history prior to 1965), with 317 plots in the Plains and 194 plots in the Shield regions. At each plot, two adjacent 30-m transects were established 2 m apart, running north from the plot origin. Soil organic layer (SOL) depth (cm) was measured every 3 m and the mean was taken from the 10 measurements to calculate a plot-level SOL thickness. Three soil organic layer profiles were destructively sampled at 0, 12, and 24 m using a corer that was custom designed for NWT soils. Within the transects, all stems taller than 1.37 m were identified to species to calculate tree density (stems / m2). Nonvascular plant percent cover was identified to functional group at five, 1-m2 quadrats spaced 6 m apart along the belt transect. A subset of 2,067 of 5,137 total increments from 1,803 profiles from 421 plots were analyzed for total percent C using a CHN analyzer. Time-after-fire was established using fire history records. For older plots where no known fire history is recorded, tree age was used. Data are for the period 2015-06-11 to 2018-08-24 and are provided in comma-separated values (CSV) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gas_seeps_lakes_fairbanks_sar_2394&quot;&gt;Gas_Seeps_Lakes_Fairbanks_SAR_2394&lt;/h4&gt;
This dataset includes maps and locations of potential gas seepage in lakes within the immediate and surrounding area around Fairbanks, Alaska, a region underlain by discontinuous permafrost and characterized by thermokarst lake formation. Gas bubbling from lakes in the Fairbanks area is usually rich in methane, a potent greenhouse gas that is difficult to quantify. A new remote sensing method was used for detecting potential gas seepage, defined as areas of suspected perennial ebullition, by using a previously ground-truthed seep that appeared as a high-backscatter perennial feature in winter L-band Synthetic Aperture Radar (SAR) data from 2006-2011. Based on threshold values determined by the sigma-naught backscatter of this training seep, 1,690 areas of potential seepage were detected in 459 lakes out of 658 lakes analyzed. Results were validated through a different ground-truthed seep. The data are provided in shapefile format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;alt_gpr_barrow_1355&quot;&gt;ALT_GPR_Barrow_1355&lt;/h4&gt;
This data set provides estimates of Active Layer Thickness (ALT) determined with ground-based measurements, and calculated soil volumetric water content (VWC) at four selected sites around Barrow, Alaska in August 2013. ALT was determined using a ground-penetrating radar (GPR) system and traditional mechanical probing. Calculated uncertainties are also included. GPR measurements were taken along four transects of varying length (approx. 1 to 7 km). Mechanical probing included several high-density surveys (every 1 m within 100-m survey line) along each GPR transect. VWC of the active layer soil was calculated at 3-8 calibration points per site where the probe measurement was exactly co-located with a GPR trace.
&lt;br&gt;&lt;h4 id&#x3D;&quot;alaska_l4_wrf_stilt_footprints_1544&quot;&gt;Alaska_L4_WRF_STILT_Footprints_1544&lt;/h4&gt;
This dataset provides Stochastic Time-Inverted Lagrangian Transport model outputs for receptors located at the NOAA Barrow Alaska Observatory for 12 selected years (15 August to 15 October) across the 30-year, 1982 to 2011, study timeframe. Meteorological fields from version 3.5.1 of the Weather Research and Forecasting model are used to drive STILT. STILT applies a Lagrangian particle dispersion model backwards in time from a measurement location (the &amp;quot;receptor&amp;quot; location), to create the adjoint of the transport model in the form of a &amp;quot;footprint&amp;quot; field. The footprint, with units of mixing ratio (ppm --- CO2; ppb --- CH4) per (umol m-2 s-1 --- CO2; nmol m-2 s-1 --- CH4), quantifies the influence of upwind surface fluxes on concentrations measured at the receptor and is computed by counting the number of particles in a surface-influenced volume and the time spent in that volume. The simulation results included in this dataset are crucial for understanding changes in Arctic carbon cycling and are part of a retrospective analysis to link changes in atmospheric composition at Arctic receptor sites with shifts in ecosystem structure and function. Each file provides the surface influence-function footprints on a lat/lon/time grid from WRF-STILT simulations for the receptor location.
&lt;br&gt;&lt;h4 id&#x3D;&quot;resalt_alt_gpr_1265&quot;&gt;ReSALT_ALT_GPR_1265&lt;/h4&gt;
This data set includes estimates of permafrost Active Layer Thickness (ALT; cm), and calculated uncertainties, derived using a ground-penetrating radar (GPR) system in the field in August 2014 near Toolik Lake and Happy Valley on the North Slope of Alaska. GPR measurements were taken along 10 transects of varying length (approx. 1 to 7 km). Traditional ALT estimates from mechanical probing every 100 to 500 m along each transect are also included. These data are suitable for future studies of how ALT varies over relatively large geological features, such as hills and valleys, wetland areas, and drained lake basins.
&lt;br&gt;&lt;h4 id&#x3D;&quot;preabove_airmoss_l1_alaska_1678&quot;&gt;PreABoVE_AirMOSS_L1_Alaska_1678&lt;/h4&gt;
This data set provides level 1 (L1) polarimetric radar backscattering coefficient (sigma-0), multi-look complex, polarimetrically calibrated, and georeferenced data products from the Airborne Microwave Observatory of Subcanopy and Subsurface (AirMOSS) radar instrument collected over 10 study sites across Northern Alaska, USA. Flight campaigns took place in August 2014, October 2014, April 2015, August 2015, September 2015, and October 2015. The acquired L1 P-band radar backscatter data will be used to derive estimates of soil water content and permafrost state at the study sites.
&lt;br&gt;&lt;h4 id&#x3D;&quot;resalt_insar_barrow_1266&quot;&gt;ReSALT_InSAR_Barrow_1266&lt;/h4&gt;
Active layer thickness (ALT) is a critical parameter for monitoring the status of permafrost that is typically measured at specific locations using probing, in situ temperature sensors, or other ground-based observations. The thickness of the active layer is the average annual thaw depth, in permafrost areas, due to solar heating of the surface. This data set includes the mean Remotely Sensed Active Layer Thickness (ReSALT) over years 2006 to 2011 for the region near Barrow, Alaska. The data were produced by an Interferometric Synthetic Aperture Radar (InSAR) technique that measures seasonal surface subsidence and infers ALT. ReSALT estimates were validated by comparison with ground-based ALT obtained using probing and Ground Penetrating Radar at multiple sites. These results indicate remote sensing techniques based on InSAR could be an effective way to measure and monitor ALT over large areas on the Arctic coastal plain. These data provide gridded (30-m) estimates of active layer thickness (cm; ALT) and seasonal subsidence (cm), as well as calculated uncertainty in each of these parameters. This data set was developed in support of NASA&amp;#39;s Arctic-Boreal Vulnerability Experiment (ABoVE) field campaign. The data are presented in one netCDF (.nc) file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;freeze_thaw_northernhemisphere_2323&quot;&gt;Freeze_Thaw_NorthernHemisphere_2323&lt;/h4&gt;
This dataset provides a probabilistic freeze/thaw (FT) data record from 2016 to 2020 for the Northern Hemisphere derived using a deep learning model (U-Net). The model was informed by satellite multi-frequency microwave brightness temperature retrievals from the NASA SMAP (Soil Moisture Active Passive) and JAXA AMSR2 (Advanced Microwave Scanning Radiometer 2) radiometers, and trained using daily soil temperature observations from Northern Hemisphere weather stations and global reanalysis data (ERA-5). Unlike other available FT data records that provide only a binary classification of frozen or non-frozen conditions, this product includes both binary FT and continuous variable estimates of the probability of thawed conditions. This product is designed to complement other established binary FT data records, including the NASA FT Earth System Data Record and SMAP Level 3 FT operational products, by providing a probabilistic FT variable with enhanced accuracy and sensitivity to near-surface (&amp;lt;&#x3D;5 cm depth) soil FT condition. The data are provided in cloud optimized GeoTIFF (COG) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;permafrostthaw_carbonemissions_1872&quot;&gt;PermafrostThaw_CarbonEmissions_1872&lt;/h4&gt;
This dataset consists of an ensemble of model projections from 1901 to 2299 for the northern hemisphere permafrost domain. The model projections include monthly average values for a common set of diagnostic outputs at a spatial resolution of 0.5 x 0.5 degrees latitude and longitude. The model simulations resulted from a synthesis effort organized by the Permafrost Carbon Network to evaluate the impacts of climate change on the carbon cycle in permafrost regions in the high northern latitudes. The model teams used different historical input weather data, but most used driver data developed by the Climate Research Unit - National Centers for Environmental Prediction (CRUNCEP) as modified for the Multiscale Terrestrial Model Intercomparison Project (MsTMIP). The teams scaled the driver data for the projections using output from global climate models from the fifth Coupled Model Intercomparison Project (CMIP5). The synthesis evaluated the terrestrial carbon cycle in the modern era and projected future emissions of carbon under two climate warming scenarios: Representative Concentration Pathways 4.5 and 8.5 (RCP45 and RCP85) from CMIP5. RCP45 represents emissions resulting in a global climate close to the target climate in the Paris Accord. RCP85 represents unconstrained greenhouse gas emissions.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpp_cos_conductance_soilfluxes_2324&quot;&gt;GPP_COS_Conductance_SoilFluxes_2324&lt;/h4&gt;
This dataset provides outputs from the Simple Biosphere Model (v 4.2). Products include hourly 0.5-degree gridded fluxes of gross primary productivity (GPP), respiration, carbonyl sulfide (COS) uptake by vegetation and soil, along with conductance of COS (apparent mesophyll and total), stomatal conductance of water and partial pressure of CO2 in the canopy air space, leaf surface, interior and chloroplast. The data are separated by plant functional type (PFT). Fluxes have dimensions of latitude, longitude, time, and plant functional type. Model output spans 53N to 90N latitude and 180W to 180E longitude over years 2000 to 2020. The data are provided in NetCDF version 4 format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;daily_fineparticulatematter_ak_2157&quot;&gt;Daily_FineParticulateMatter_AK_2157&lt;/h4&gt;
The dataset provides simulated PM2.5 concentration estimates over Alaska, U.S. PM2.5 (particulate matter with diameter &amp;lt;&#x3D; 2.5 microns) concentrations in air (micrograms m-3) are gridded at 0.1-degree resolution for May to September for the years 2001 through 2015. The data were created in a modeling process utilizing the Wildland Fire Emissions Inventory System (WFEIS), the Arctic-Boreal Vulnerability Experiment (ABoVE) Wildfire Date of Burning (WDoB) dataset, and multiple models including the Hybrid Single-Particle Lagrangian Integrated Trajectory (HYSPLIT) model. The data are provided in GeoTIFF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;snow_depth_data_images_1656&quot;&gt;Snow_Depth_Data_Images_1656&lt;/h4&gt;
This dataset includes data from late-March snow surveys and hourly digital camera images from two study areas within the Wrangell St Elias National Park, Alaska. These data comprise snow density, stratigraphy, and temperature profiles obtained by snow pits; and snow depth data obtained from transects between snow pits. Daily snow depths, adjacent to each pit, were derived from hourly camera images of snow stakes placed adjacent to each pit. These data were collected to constrain and validate a physically-based, spatially-distributed snow evolution model used to simulate snow conditions in Dall sheep habitat. The two study areas are both located within the Jacksina Park Unit (JPU). The first study area, surveyed in 2017, included the northern end of Jaeger Mesa and an area near Rambler mine in the North East of the JPU. The second study area, surveyed in 2018, was within the upper watershed of Pass Creek in the North of the JPU. The remote cameras operated from September 2016 to August 2017 on Jaeger Mesa/Rambler Mine and from September 2017 to July 2018 at Pass Creek.
&lt;br&gt;&lt;h4 id&#x3D;&quot;snow_wildlife_tracks_ak_wa_2188&quot;&gt;Snow_Wildlife_Tracks_AK_WA_2188&lt;/h4&gt;
This dataset contains three field seasons of snow-wildlife observations conducted at 707 sites from January 2021 to March 2023 in Washington and Alaska, spanning a broad range of snow conditions. Relatively fresh tracks (usually &amp;lt;24 h) of common large mammal predators (bobcats, coyotes, cougars, and wolves) and their ungulate prey (caribou, Dall sheep, moose, mule deer, and white-tailed deer) were investigated to determine how snow affects predator-prey interactions. The track sink depth and dimensions (width and length) of three consecutive footprints were measured from one individual. Age class was recorded for moose based either on visual confirmation of an individual creating snow tracks or based on track dimensions. The ability to differentiate age classes for smaller ungulates was more uncertain, so age classes for deer, caribou, or sheep were not specified. Animal gait was identified using a simple classification scheme. Data also include animal species, snow density, hardness, total ice, surface temperature, and vegetation type. To best capture snow hardness, surface penetrability and hand-hardness were measured throughout the snowpack. The data are provided in comma-separated values (CSV) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;arctic_soil_properties_2149&quot;&gt;Arctic_Soil_Properties_2149&lt;/h4&gt;
This dataset provides lab-measured soil properties, including soil water matric potential, soil dielectric properties, soil electrical conductivity, corresponding soil moisture. The dataset also includes the basic soil physical properties such as soil organic matter, bulk density, porosity, fiber content, root biomass, and mineral texture. Soil samples were collected from August 21 to August 27, 2018, from the surface to permafrost table in soil pits at nine sites along the Dalton Highway in northern and central regions of Alaska. Permittivity and soil electrical conductivity measurements were conducted using METER TEROS 12 probes. Soil moisture measurements were made with a TEROS 21 probe. The measurements were conducted in the lab over the span of three years. The purpose of soil collection and lab measurements was to develop an integrated framework that relates the hydrological properties to dielectric properties of permafrost active layer soil in support of the NASA Arctic and Boreal Vulnerability Experiment (ABoVE) Airborne Campaign.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_soil_respiration_maps_1935&quot;&gt;ABoVE_Soil_Respiration_Maps_1935&lt;/h4&gt;
This dataset provides gridded estimates of carbon dioxide (CO2) emissions from soil respiration occurring within permafrost-affected tundra and boreal ecosystems of Alaska and Northwest Canada at a 300 m spatial resolution for the period 2016-08-18 to 2018-09-12. The estimates include monthly average CO2 flux (gCO2 C m-2 d-1), daily average CO2 flux and error estimates by season (Autumn, Winter, Spring, Summer), estimates of annual offset of CO2 uptake (i.e., vegetation GPP), annual budgets of vegetation gross primary productivity (GPP; gCO2 C m-2 yr-1), and the fraction of open (non-vegetated) water within each 300 m grid cell. Belowground sources of respiration (i.e., root and microbial) are included. The gridded soil CO2 estimates were obtained using seasonal Random Forest models, information from remote sensing, and a new compilation of in-situ soil CO2 flux from Soil Respiration Stations and eddy covariance towers. The flux tower data are provided along with daily gap-filled flux observations for each Soil Respiration station forced diffusion (FD) chamber record. The data cover the NASA ABoVE Domain.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tundratransect_vegrefl_soil_2232&quot;&gt;TundraTransect_VegRefl_Soil_2232&lt;/h4&gt;
This dataset provides visible-near infrared spectral reflectance, descriptions of vegetation cover, surface temperature, the total fraction of absorbed photosynthetically active radiation (fAPAR, 2001 only), permafrost active layer depth, elevation, and soil temperature at 5 cm depth. Measurements were made at every meter along a 100-m transect aligned mainly in an east-west direction, located approximately 300 m southeast of the National Oceanic and Atmospheric Administration (NOAA) Global Monitoring Laboratory (GML) baseline observatory near Utqiagvik, Alaska. Reflectance measurements were collected at nearly weekly intervals through the growing seasons of 2000 to 2002 to describe characteristics of green-up, peak growth, and senescence. Reflectance measurements were also collected once near peak growth in 2022. Ancillary measurements were collected at intervals through the 2001 and 2002 growing seasons.
&lt;br&gt;&lt;h4 id&#x3D;&quot;arctictreeline_spruce_co2_wv_1948&quot;&gt;ArcticTreeLine_Spruce_CO2_WV_1948&lt;/h4&gt;
This dataset provides in situ measurements of needle-level gas-exchange and leaf traits from Picea glauca (white spruce) from a field site located in the northern latitudinal forest-tundra ecotone (FTE) near the Dalton Highway in northern Alaska, and from one study site located in Black Rock Forest, New York, USA. Measurements were collected with an open flow portable photosynthesis system (Li6400XT) and custom-built temperature-controlled cuvette. Respiration as a function of leaf temperature was measured continuously as the needle temperature was ramped from approximately 5 to 65 degrees C, at a constant rate of 1 degree C per minute. Additional data include tree diameter at breast height (dbh), leaf area, photosynthetic rate, intercellular C02, conductance to H20, tree height, and data from raw temperature curves. Results are reported on both a leaf area and leaf mass basis. The data are for the period 2018-06-06 to 2018-06-23 and are provided in comma-separated (CSV) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;above_sar_surveys_2150&quot;&gt;ABoVE_SAR_Surveys_2150&lt;/h4&gt;
This dataset contains tables containing Airborne flight metadata from synthetic aperture radar (SAR) surveys from 2012 to 2022 in Alaska and Canada. NASA&amp;#39;s Arctic Boreal Vulnerability Experiment (ABoVE) conducted airborne SAR surveys of over 120,000 km2 in Alaska and northwestern Canada during 2017, 2018, 2019, and 2022. Legacy lines acquired between 2012 and 2015 by other projects are included for completeness and to enable longer times series creation. The data files and companion file contain L-band and P-band airborne SAR metadata acquired during the ABoVE airborne campaigns. Included are detailed descriptions of ~80 SAR flight lines and how each fits into the ABoVE experimental design. Extensive maps, tables, and hyperlinks give direct access to every flight plan as well as individual flight lines. This entry is a guide to enable interested readers to fully explore the ABoVE L- and P-band SAR data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nongrowing_season_co2_flux_1692&quot;&gt;Nongrowing_Season_CO2_Flux_1692&lt;/h4&gt;
This dataset provides a synthesis of winter ( September-April) in situ soil CO2 flux measurement data from locations across pan-Arctic and Boreal permafrost regions. The in situ data were compiled from 66 published and 21 unpublished studies conducted from 1989-2017. The data sources (publication references) are provided. Sampling sites spanned pan-Arctic Boreal and tundra regions (&amp;gt;53 Deg N) in continuous, discontinuous, and isolated/sporadic permafrost zones. The CO2 flux measurements were aggregated at the monthly level, or seasonally when monthly data were not available, and are reported as the daily average (g C m-2 day-1) over the interval. Soil moisture and temperature data plus environmental and ecological model driver data (e.g., vegetation type and productivity, soil substrate availability) are also included based on gridded satellite remote sensing and reanalysis sources.
&lt;br&gt;&lt;h4 id&#x3D;&quot;arctic_boreal_co2_flux_1934&quot;&gt;Arctic_Boreal_CO2_Flux_1934&lt;/h4&gt;
This Arctic-Boreal CO2 fluxes (ABCflux) dataset contains monthly aggregates of terrestrial net ecosystem CO2 exchange and its derived partitioned component fluxes: gross primary productivity (GPP) and ecosystem respiration. Over 70 supporting variables describe key site conditions (e.g., vegetation and disturbance type), micrometeorological and environmental measurements (e.g., air and soil temperatures), and flux measurement techniques. The data contained in this ABCflux dataset form a standardized monthly database of Arctic-Boreal CO2 fluxes (i.e., ABCflux Database) and include 244 sites and 6,309 monthly observations; 136 sites and 2,217 monthly observations represent tundra, and 108 sites and 4,092 observations represent the boreal biome. The data are for the period 1989 to 2020.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cubesat_arctic_boreal_lakearea_1667&quot;&gt;CubeSat_Arctic_Boreal_LakeArea_1667&lt;/h4&gt;
This dataset provides near-daily lake area timeseries for 85,358 lakes across four study areas in Northern Canada and Alaska, USA, between May 1 and October 1, 2017. These lake area estimates were produced using digital images from newly developed Planet Labs CubeSats, small satellites with a 4-band (blue, green, red, near-infrared) camera payload. In constellation, CubeSats collected imagery at very high spatial (3-5m) and temporal (near-daily) resolution. From the imagery, each lake&amp;#39;s mean, minimum, and maximum areas and seasonal dynamism were derived. The dataset covers four Arctic-Boreal regions: the Yukon Flats Basin (YFB) in eastern interior Alaska, and the Mackenzie River Valley (MRV), Canadian Shield Transect (CST), and Hudson Bay Lowland (HBL) in Canada.
&lt;br&gt;&lt;h4 id&#x3D;&quot;towerbased_photospec_sif_sk_ca_1887&quot;&gt;TowerBased_PhotoSpec_SIF_SK_CA_1887&lt;/h4&gt;
This dataset includes daily averaged solar-induced chlorophyll fluorescence (SIF) in the red (680-686 nm) and far-red (745-758 nm) wavelength ranges, relative SIF (SIF/Intensity), chlorophyll-carotenoid index (CCI), photochemical reflectance index (PRI), near-infrared vegetation index (NIRv), and normalized difference vegetation index (NDVI) for both black spruce (Picea mariana) and larch (Larix laricina) targets. The study site (Southern Old Black Spruce, SOBS Fluxnet ID CA-Obs) is located near the southern limit of the boreal forest ecotone in Saskatchewan, Canada. Data were collected for the spring transition in both 2019 and 2020 using PhotoSpec. Species-specific averages were calculated over each 30-minute period, then averaged again to report daily averages of SIF relative and reflectance measurements for both black spruce and larch.
&lt;br&gt;&lt;h4 id&#x3D;&quot;circumarctic_trends_hotspots_2322&quot;&gt;CircumArctic_Trends_Hotspots_2322&lt;/h4&gt;
This dataset provides estimates of trends in temperature, moisture, and vegetation changes over the circumpolar Arctic. Time series trends were measured by the Theil-Sen slope and associated p-values for a variety of variables including 2-meter air temperature, precipitation, soil moisture, non-frozen season days, permafrost active layer thickness, snow cover, vapor pressure deficit, land surface water fraction, normalized difference vegetation index (NDVI), and vegetation optical depth. Trends were measured annually and over specific seasons of spring (March to May), summer (June to August), autumn (September to November) and winter (December to February), and for the 1980-2020 and 1997-2020 time periods, depending on the variable and original data availability. Emerging hotspots of change were identified for the same variables and seasons, but only over the 1997-2020 period. In addition, a multivariate ranking was used to create combined hotspot layers to show areas of substantial changes in the thermal environment, moisture, and vegetation; these themes reflect landscape changes considered to be detrimental (e.g., a threat) to ecosystems and human populations. Ancillary files provide the boundaries of study regions, Brown permafrost regions, and a land cover product. The data are provided in cloud optimized GeoTIFF (COG) and shapefile formats.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tundra_leaf_spectra_2005&quot;&gt;Tundra_Leaf_Spectra_2005&lt;/h4&gt;
This dataset provides leaf-level visible-near infrared spectral reflectance, chlorophyll fluorescence spectra, species, plant functional type (PFT), and chlorophyll content of common high latitude plant samples collected near Fairbanks, Utqiagvik, and Toolik, Alaska, U.S., during the summers of 2019, 2020, and 2021. A FluoWat leaf clip was used to measure leaf-level visible-near infrared spectral reflectance and chlorophyll fluorescence spectra. Fluorescence yield (Fyield) was calculated as the ratio of the emitted fluorescence divided by the absorbed radiation for the wavelengths from 400 nm up to the wavelength of the cut off for the FluoWat low pass filter (either 650 or 700 nm). Chlorophyll content of samples was measured using a CCM-300 Chlorophyll Content. The data are provided in comma-separated values (.csv) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tundraveg_reflectance_soil_co2_1960&quot;&gt;TundraVeg_Reflectance_Soil_CO2_1960&lt;/h4&gt;
This dataset provides measurements at tundra plots collected near Utqiagvik and Atqasuk, AK, including visible-near infrared spectral reflectance, chamber gas exchange measurements of CO2, pulse amplitude modulated (PAM) fluorometry, chlorophyll pigment contents, along with surface temperature, permafrost active layer depth, and soil temperature at 5 cm, through the growing seasons of 2001 and 2002. At all plots, spectral reflectance was measured using a portable spectrometer configured with a straight fiber optic foreoptic, surface temperatures were measured using a handheld Everest Infrared Thermometer, and thaw depth (or active layer depth) was measured using a metal rod graduated in centimeter intervals. At small plots (~15 cm) at Utqiagvik (referred to as Patch plots) chambers were constructed that enclosed an individual patch to determine photosynthetic rate and estimate respiration rate (made by covering the chamber in a dark cloth). Efficiency using PAM fluorometer, ambient yield estimations, and rapid light curve measurements were taken. Chlorophyll concentration was measured with a portable spectrometer configured as a spectrophotometer. At larger plots (approximately 1 m2) which were part of the International Tundra EXperiment (ITEX plots) at Utqiagvik (referred to as Barrow) and Atqasuk, a sub-sample of five control and five warmed plots at each site were fitted with 0.45 m diameter polyvinyl chloride collars for chamber flux measurements. To determine the total fraction of absorbed photosynthetically active radiation (fAPAR), a series of photosynthetically active radiation (PAR) measurements were made using a custom-made light bar consisting of a linear array of GaAsP sensors mounted within an aluminum U-bar under a white plastic diffuser. In addition, a visual estimate was made of the fraction of standing dead vegetation based on percent cover. The data are provided in comma-separated values (.csv) format. In addition, photographs of plots and instruments are provided.
&lt;br&gt;&lt;h4 id&#x3D;&quot;uavsar_wetland_peace-athabasca_2442&quot;&gt;UAVSAR_Wetland_Peace-Athabasca_2442&lt;/h4&gt;
This dataset holds UAVSAR imagery products for the Peace-Athabasca Delta region of Canada. UAVSAR data were collected for two flight lines on five dates from 2017 to 2022 and processed to NISAR-like products with spatial resolution of approximately 10 m. Products include double bounce, volume, odd, and helical scatter components. In addition, radiometrically terrain corrected HH backscatter, HV backscatter, and the ratio of HH to HV, as well as the local incidence angle in radians and a valid data mask are provided. These data can be used to estimate the extent of inundation of wetlands in this region. The data are provided in cloud optimized GeoTIFF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;understory_veg_biomass_alaska_2340&quot;&gt;Understory_Veg_Biomass_Alaska_2340&lt;/h4&gt;
This dataset provides measurements of vegetation biomass from 11 locations across Alaska during 2016 to 2018. Vegetation was harvested from plots that were located at the end of previously established 30-m transects at each site, except at one site where plots were randomly selected. Vascular vegetation was clipped from 50 cm x 50 cm plots, and non-vascular vegetation was clipped from 25 cm x 25 cm plots. All harvested vegetation was sorted by functional group or by species where identification was possible. The sorted vegetation was dried and then weighed to determine biomass. Locations were selected to investigate fire disturbance, to span the range of permafrost regions from continuous to sporadic, and to cover vegetation types from boreal forests, tussock tundra, upland willow/herbaceous scrub, and lowland fen and wet tundra sites across Alaska. The data are provided in comma separated values (CSV) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.ornldaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA ACCP Project</title>
      <link>https://registry.opendata.aws/nasa-accp</link>
      <guid>https://registry.opendata.aws/nasa-accp</guid>
      <description>An inventory of NASA&amp;#39;s airborne and field campaigns for Earth Science
&lt;br&gt;&lt;h4 id&#x3D;&quot;plotchem_420&quot;&gt;plotchem_420&lt;/h4&gt;
The purpose of these measurements was to determine plot-level average leaf concentrations of nitrogen, lignin, cellulose, etc. in order to investigate how AVIRIS reflectance measurements vary with chemistry. The plot-level leaf chemistry values were calculated from green leaf chemistry values and litterfall sample weights.
&lt;br&gt;&lt;h4 id&#x3D;&quot;leafchem_421&quot;&gt;leafchem_421&lt;/h4&gt;
As part of NASA&amp;#39;s Accelerated Canopy Chemistry Program (ACCP) analyses were performed for the determination of carbon constituents and nitrogen content in fresh forest foliage. Samples were analyzed using a series of extraction&amp;#39;s that yielded different carbon constituents: non-polar, polar, cellulose and lignin. Nitrogen analyses were conducted using a standard combustion procedure. Approximately 1000 leaf samples were collected from 5 geographically distinct sites and were analyzed at the University of New Hampshire to ensure consistency in analysis. Results were used as a calibration set for Visible/NIR reflectance and the estimation of canopy carbon and nitrogen concentrations.
&lt;br&gt;&lt;h4 id&#x3D;&quot;canopychem_422&quot;&gt;canopychem_422&lt;/h4&gt;
This data set describes the nitrogen and chlorophyll content of small, monospecific canopies formed from seedlings of Douglas-fir (Pseudotsuga menziesii) and bigleaf maple (Acer macrophyllum). The trees were provided different levels of fertilization in order to produce canopies with varying nitrogen and chlorophyll concentration. For the Douglas-fir, fertilization was provided during the dormant season, so there were no differences in growth or leaf area among canopies, and canopies were at a constant density with varying foliar chemistry. For the maple, seedlings were aggregated at various densities, producing a matrix of leaf area as well as chemistry variations. Before destructive analysis for foliar chemistry, canopy reflectance was measured under natural sunlight (see ACCP Seedling Canopy Reflectance Spectra Data).
&lt;br&gt;&lt;h4 id&#x3D;&quot;canopyspec_423&quot;&gt;canopyspec_423&lt;/h4&gt;
This is a data set of spectral reflectance (400-2500 nm) of small, monospecific canopies formed from seedlings of Douglas-fir (Pseudotsuga menziesii) and bigleaf maple (Acer macrophyllum). The trees were provided different levels of fertilization in order to produce canopies with varying nitrogen and chlorophyll concentration. For the Douglas-fir, fertilization was provided during the dormant season, so there were no differences in growth or leaf area among canopies, and canopies were at a constant density with varying foliar chemistry. For the maple, seedlings were aggregated at various densities, producing a matrix of leaf area as well as chemistry variations. Canopy reflectance was measured under natural sunlight, and canopies were then destructively analyzed for chemical content and leaf area (see ACCP Seedling Canopy Chemistry Data).
&lt;br&gt;&lt;h4 id&#x3D;&quot;plotspec_544&quot;&gt;plotspec_544&lt;/h4&gt;
AVIRIS image scenes were acquired in 1992 over ACCP sites. Pixels that coincided with field study plots were extracted and reflectance values were correlated with estimated canopy carbon and nitrogen content.
&lt;br&gt;&lt;h4 id&#x3D;&quot;leafspec_424&quot;&gt;leafspec_424&lt;/h4&gt;
The leaf spectra datasets contain visible and near infrared reflectance spectra data for both fresh and dry leaf samples collected in the ACCP. These samples are from Blackhawk Island, WI, Harvard Forest, MA, Howland, ME, Jasper Ridge, CA field sites and the Douglas fir and bigleaf maple seedling canopy study sites. Data reported for each sample is absorbance [log(1/Reflectance)] from 400-2498nm at 2nm intervals and a resolution of 10nm. These data were collected for the purpose of determining the relationship of foliar chemical concentrations with visible and near infrared wavelength reflectance spectra.. Both multiple linear regression and partial least square regression techniques have been used to relate lab chemistry data to spectral reflectance. ORNL DAAC maintains information on the entire ACCP.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.ornldaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA ACRIM III Project</title>
      <link>https://registry.opendata.aws/nasa-acrim-iii</link>
      <guid>https://registry.opendata.aws/nasa-acrim-iii</guid>
      <description>Launch and mission info for NASA&amp;#39;s AcrimSat Earth satellite, which for 14 years monitored solar radiation and its effects on Earth&amp;#39;s atmosphere and climate change.
&lt;br&gt;&lt;h4 id&#x3D;&quot;acr3l2dm&quot;&gt;ACR3L2DM&lt;/h4&gt;
ACR3L2DM_1 is the Active Cavity Radiometer Irradiance Monitor (ACRIM) III Level 2 Daily Mean Data version 1 product consists of Level 2 total solar irradiance in the form of daily means gathered by the ACRIM III instrument on the ACRIMSAT satellite. The daily means are constructed from the shutter cycle results for each day.
&lt;br&gt;&lt;h4 id&#x3D;&quot;acr3l2sc&quot;&gt;ACR3L2SC&lt;/h4&gt;
ACR3L2SC_1 is the Active Cavity Radiometer Irradiance Monitor (ACRIM) III Level 2 Shutter Cycle Data version 1 product contains Level 2 total solar irradiance in the form of shutter cycles gathered by the ACRIM instrument on the ACRIMSAT satellite.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.asdc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA ACT-America Project</title>
      <link>https://registry.opendata.aws/nasa-act-america</link>
      <guid>https://registry.opendata.aws/nasa-act-america</guid>
      <description>The ACT-America Campaign Catalog provides information about the airborne campaigns of the Atmospheric Carbon and Transport (ACT-America) project. ACT-America advanced atmospheric greenhouse gas inversions to a high level of accuracy and precision through new methods and models that improved knowledge of atmospheric transport, prior flux models, and space-based observations. The catalog compiles flight details for the five campaigns conducted during Summer 2016, Winter 2017, Fall 2017, Spring 2018, and Summer 2019 (2016-05-27 to 2019-07-26) across three regions of the eastern and central United States. Data include flight dates, regions, objectives, weather conditions, instrument status, aircraft flight paths, detailed weather reports, and measurement summary figures. A total of 121 research flights were conducted within the five six-week seasonal campaigns by each of the two instrumented aircraft platforms, the NASA Langley Beechcraft B-200 King Air and the NASA Wallops Flight Facility&amp;#39;s C-130 Hercules. During 1,140 flight hours remote and in situ sensors onboard the two research aircraft measured greenhouse gas mole fractions, trace gases, and thermodynamic variables across a variety of continental surfaces and atmospheric conditions to study the transport and fluxes of atmospheric carbon dioxide and methane. As noted in the Flight_patterns_staus field, there were flights when both aircraft flew directly under Orbiting Carbon Observatory-2 (OCO-2) overpasses to evaluate the ability of OCO-2 to observe high-resolution atmospheric CO2 variations. The C-130 aircraft was also equipped with active remote sensing instruments for planetary boundary layer height detection and column greenhouse gas measurements. The data are provided in comma separated values (CSV), compressed Keyhole Markup Language (KMZ) formats along with figures as JPEG and Portable Network Graphics images.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cpl_abl_top_height_1825&quot;&gt;CPL_ABL_Top_Height_1825&lt;/h4&gt;
This dataset consists of the atmospheric boundary layer (ABL) top heights and the altitudes of the two additional aerosol layers (in km above mean sea level) derived from Cloud Physics Lidar (CPL) measurements using the Haar wavelet transform method. The CPL instrument was deployed onboard NASA&amp;#39;s C-130 aircraft to obtain aerosol backscatter profiles during four ACT-America field campaigns (Summer 2016, Winter 2017, Fall 2017, and Spring 2018). CPL is a backscatter lidar designed to operate simultaneously at three wavelengths. The profiles were collected at 4-second temporal and 30 m vertical resolutions. The time resolution of the provided CPL-derived ABL top heights and other aerosol layers are 8 seconds.
&lt;br&gt;&lt;h4 id&#x3D;&quot;act_casa_ensemble_prior_fluxes_1675&quot;&gt;ACT_CASA_Ensemble_Prior_Fluxes_1675&lt;/h4&gt;
This data set provides gridded, model-derived gross primary productivity (GPP), ecosystem respiration (RECO), and net ecosystem exchange (NEE) of CO2 biogenic fluxes and their uncertainties at monthly and 3-hourly time scales over 2003-2019 on a 463-m spatial resolution grid for the conterminous United States (CONUS) and on both 5-km and half-degree spatial resolution grids for North America (NA). The biogeochemical model Carnegie Ames Stanford Approach (CASA) was used.
&lt;br&gt;&lt;h4 id&#x3D;&quot;halo_lidar_aop_ml_heights_1833&quot;&gt;HALO_LiDAR_AOP_ML_Heights_1833&lt;/h4&gt;
This dataset provides measurements from the High Altitude Lidar Observatory (HALO) instrument, an airborne multi-function Differential Absorption Lidar (DIAL) and High Spectral Resolution Lidar (HSRL), operating at 532 nm and 1064 nm wavelengths onboard a C-130 aircraft during the June and July 2019 ACT-America campaign. The flights took place over eastern and central North America based from Shreveport, Louisiana; Lincoln, Nebraska; and NASA Wallops Flight Facility located on the eastern shore of Virginia. HALO data were sampled at 0.5 s temporal and 1.25 m vertical resolutions. The data include profiles of aerosol optical properties (AOP), distributions of mixed layer heights (MLH), columns of tropospheric methane, and navigation parameters. The data are provided in HDF5 format along with PNG images and a companion files in Portable Document (.pdf) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;actamerica_mfll_l1_1817&quot;&gt;ACTAMERICA_MFLL_L1_1817&lt;/h4&gt;
This dataset provides Level 1 (L1) remotely sensed differential absorption optical depth (DAOD) measurements made through the Multi-Functional Fiber Laser Lidar (MFLL; Harris Corporation) during airborne campaigns in Summer 2016, Winter 2017, Fall 2017, and Spring 2018 conducted over central and eastern regions of the United States for the Atmospheric Carbon and Transport (ACT-America) project. DAOD were measured at 0.1 second frequency during flights of the C-130 Hercules aircraft at altitudes up to 8 km with MFLL. The MFLL is a set of Continuous-Wave (CW) lidar instruments consisting of an intensity modulated multi-frequency single-beam synchronous-detection Laser Absorption Spectrometer (LAS) operating at 1571 nm for measuring the column amount of CO2 number density and range between the aircraft and the surface or to cloud tops, and surface reflectance and a Pseudo-random Noise (PN) altimeter at 1596 nm for measuring the path length from the aircraft to the scattering surface and/or cloud tops. The MFLL was onboard all ACT-America seasonal campaigns, except Summer 2019. Complete aircraft flight information, interpolated to the 0.1 second column CO2 reporting frequency, are included, but not limited to, latitude, longitude, altitude, and attitude. Data users should note that a Level 2 (L2) MFLL data product is available (related dataset) that contains all data variables (plus the column-average CO2) included in this L1 MFLL data product but has undergone additional processing and calibrations and is recommended for most use cases.
&lt;br&gt;&lt;h4 id&#x3D;&quot;actamerica_hskping_1574&quot;&gt;ACTAMERICA_Hskping_1574&lt;/h4&gt;
This dataset provides aircraft navigational parameters and related meteorological data (often referred to as &amp;quot;housekeeping&amp;quot; data) in support of the research activities for the two aircrafts that flew for the NASA Atmospheric Carbon and Transport-America (ACT-America) project. ACT-America&amp;#39;s mission spans five years and includes five 6-week intensive field campaigns covering all 4 seasons and 3 regions of the central and eastern United States. Two instrumented aircraft platforms, the NASA Langley Beechcraft B200 King Air and the NASA Goddard Space Flight Center&amp;#39;s C-130H Hercules, were used to collect high-quality in situ measurements across a variety of continental surfaces and atmospheric conditions. During these flights, aircraft positional, meteorological, and environmental data are recorded by a variety of instruments. For this dataset, measurements include, but are not limited to: latitude, longitude, altitude, ground speed, air temperature, and wind speed and direction. These data are incorporated into related ACT-America flight-instrumented datasets to provide geotrajectory file information for position, attitude, and altitude awareness of instrumented sampling.
&lt;br&gt;&lt;h4 id&#x3D;&quot;insitu_tower_greenhouse_gas_1798&quot;&gt;Insitu_Tower_Greenhouse_Gas_1798&lt;/h4&gt;
This dataset provides Level 1 (L1) in situ atmospheric carbon dioxide (CO2), carbon monoxide (CO), and methane (CH4) concentrations as measured on a network of instrumented communications towers across the central and eastern USA operated by the Atmospheric Carbon and Transport-America (ACT-America) project. There were 11 towers instrumented with cavity ring-down spectrometers (CRDS; Picarro Inc.) with measurements beginning in January 2015 and continuing to October 2019. The measurement period varied by tower site. The Picarro analyzers continuously measured total CH4, isotopic ratio of CH4, CO2, CO, and other greenhouse gas concentrations. Not all species were measured at all sites. Complete tower location, elevation, instrument height, and date/time information are also provided. Determination of greenhouse gas fluxes and uncertainty bounds is essential for the evaluation of the effectiveness of mitigation strategies. These L1 data are raw instrument outputs from the Picarro instruments. A Level 2 (L2) product derived from this L1 data is available and generally would be the preferred data for most use cases.
&lt;br&gt;&lt;h4 id&#x3D;&quot;actamerica_picarro_1556&quot;&gt;ACTAMERICA_PICARRO_1556&lt;/h4&gt;
This dataset provides atmospheric carbon dioxide (CO2), carbon monoxide (CO), methane (CH4), water vapor (H2O), and ozone (O3) concentrations collected during airborne campaigns conducted by the Atmospheric Carbon and Transport-America (ACT-America) project. ACT-America&amp;#39;s mission spanned 4 years and included five 6-week airborne campaigns covering all 4 seasons and 3 regions of the central and eastern United States. This dataset provides results from all five campaigns, including Summer 2016, Winter 2017, Fall 2017, Spring 2018, and Summer 2019. Two instrumented aircraft platforms, the NASA Langley Beechcraft B200 King Air and the NASA Goddard Space Flight Center&amp;#39;s C-130H Hercules, were used to collect high-quality in situ measurements across a variety of continental surfaces and atmospheric conditions. CO2, CO, CH4, and H2O were collected with an infrared cavity ring-down spectrometer system (CRDS; Picarro Inc.). Ozone data were collected with a dual beam differential UV absorption ozone monitor (Model 205; 2B Technologies). Both aircraft hosted identical arrays of in situ sensors. Complete aircraft flight information including, but not limited to, latitude, longitude, altitude, and meteorological conditions are also provided.
&lt;br&gt;&lt;h4 id&#x3D;&quot;actamerica_pfp_1575&quot;&gt;ACTAMERICA_PFP_1575&lt;/h4&gt;
This dataset provides atmospheric carbon dioxide (CO2), methane (CH4), carbon monoxide (CO), molecular hydrogen (H2), nitrous oxide (N2O), sulfur hexafluoride (SF6), and other trace gas mole fractions (i.e., concentrations) from airborne campaigns over North America for the NASA Atmospheric Carbon and Transport - America (ACT-America) project. ACT-America&amp;#39;s mission spanned five years and included five six-week field campaigns covering all four seasons and three regions of the central and eastern United States. Two instrumented aircraft platforms, the NASA Langley Beechcraft B-200 King Air and the NASA Goddard Space Flight Center&amp;#39;s C-130 Hercules, were used to collect high-quality in situ measurements across a variety of continental surfaces and atmospheric conditions. The data were derived from laboratory measurements of whole air samples collected by Programmable Flask Packages (PFP) onboard the two ACT-America aircraft. Approximately 10 - 12 discrete flask samples were captured during each of the 195 flights. This dataset provides results from all five campaigns, including Summer 2016, Winter 2017, Fall 2017, Spring 2018, and Summer 2019.
&lt;br&gt;&lt;h4 id&#x3D;&quot;actamerica-picarro_ground_1568&quot;&gt;ACTAMERICA-PICARRO_Ground_1568&lt;/h4&gt;
This dataset provides atmospheric carbon dioxide (CO2), carbon monoxide (CO), and methane (CH4) concentrations as measured on a network of instrumented communications towers operated by the Atmospheric Carbon and Transport-America (ACT-America) project. ACT-America&amp;#39;s mission spans five years and includes five 6-week intensive field campaigns covering all 4 seasons and 3 regions of the central and eastern United States. Tower-based measurements began in early 2015 and are continuously collecting CO2, CO, and CH4 data to characterize ground-level (&amp;gt;100 m) carbon background conditions to support the periodic airborne measurement campaigns and transport modeling conducted by ACT-America. The towers are instrumented with infrared cavity ring-down spectrometer systems (CRDS; Picarro Inc.). Data are reported for the highest sampling port on each tower. The averaging interval standard deviation and uncertainty derived from periodic flask sample to in-situ measurement comparisons are provided. Complete tower location, elevation, instrument height, and date/time information are also provided.
&lt;br&gt;&lt;h4 id&#x3D;&quot;actamerica_mffll_1649&quot;&gt;ACTAMERICA_MFFLL_1649&lt;/h4&gt;
This dataset provides Level 2 (L2) remotely sensed column-average carbon dioxide (CO2) concentrations measured during airborne campaigns in Summer 2016, Winter 2017, Fall 2017, and Spring 2018 conducted over central and eastern regions of the United States for the Atmospheric Carbon and Transport (ACT-America) project. Column-average CO2 concentrations were measured at 0.1 second frequency during flights of the C-130 Hercules aircraft at altitudes up to 8 km with a Multi-functional Fiber Laser Lidar (MFLL; Harris Corporation). The MFLL is a set of Continuous-Wave (CW) lidar instruments consisting of an intensity modulated multi-frequency single-beam synchronous-detection Laser Absorption Spectrometer (LAS) operating at 1571 nm for measuring the column amount of CO2 number density and range between the aircraft and the surface or to cloud tops, and surface reflectance and a Pseudo-random Noise (PN) altimeter at 1596 nm for measuring the path length from the aircraft to the scattering surface and/or cloud tops. The MFLL was onboard all ACT-America seasonal campaigns, except Summer 2019. Complete aircraft flight information, interpolated to the 0.1 second column CO2 reporting frequency, are included, but not limited to, latitude, longitude, altitude, and attitude. Processing for this Level 2 (L2) product included additional processing and calibration procedures described in this document as applied to retrieval of column CO2 from L1 MFLL data. Data users should use this L2 data unless different CO2 retrieval criteria are preferred.
&lt;br&gt;&lt;h4 id&#x3D;&quot;mfll_xco2_range_10hz_1892&quot;&gt;MFLL_XCO2_Range_10Hz_1892&lt;/h4&gt;
This dataset provides a direct subset (i.e., the Lite version) of the Level 2 (L2) remotely sensed column-average carbon dioxide (CO2) concentrations measured during airborne campaigns in Summer 2016, Winter 2017, Fall 2017, and Spring 2018 conducted over central and eastern regions of the U.S. for the Atmospheric Carbon and Transport (ACT-America) project. Column-average CO2 concentrations were measured at a 0.1-second frequency during flights of the C-130 Hercules aircraft at altitudes up to 8 km with a Multi-functional Fiber Laser Lidar (MFLL; Harris Corporation). The MFLL is a set of Continuous-Wave (CW) lidar instruments consisting of an intensity-modulated multi-frequency single-beam synchronous-detection Laser Absorption Spectrometer (LAS) operating at 1571 nm for measuring the column amount of CO2 number density and range between the aircraft and the surface or to cloud tops, and surface reflectance and a Pseudo-random Noise (PN) altimeter at 1596 nm for measuring the path length from the aircraft to the scattering surface and/or cloud tops. The MFLL was onboard all ACT-America seasonal campaigns, except Summer 2019. Complete aircraft flight information, interpolated to the 0.1-second column CO2 reporting frequency, is included, but not limited to, latitude, longitude, altitude, and attitude.
&lt;br&gt;&lt;h4 id&#x3D;&quot;mfll_co2_weighting_functions_1891&quot;&gt;MFLL_CO2_Weighting_Functions_1891&lt;/h4&gt;
This dataset provides vertical weighting function coefficients of the Level 2 (L2) remotely sensed column-average carbon dioxide (CO2) concentrations measured during airborne campaigns in Summer 2016, Winter 2017, Fall 2017, and Spring 2018 conducted over central and eastern regions of the U.S. for the Atmospheric Carbon and Transport (ACT-America) project. Column-average CO2 concentrations were measured at a 0.1-second frequency during flights of the C-130 Hercules aircraft at altitudes up to 8 km with a Multi-functional Fiber Laser Lidar (MFLL; Harris Corporation). The MFLL is a set of Continuous-Wave (CW) lidar instruments consisting of an intensity-modulated multi-frequency single-beam synchronous-detection Laser Absorption Spectrometer (LAS) operating at 1571 nm for measuring the column amount of CO2 number density and range between the aircraft and the surface or to cloud tops, and surface reflectance and a Pseudo-random Noise (PN) altimeter at 1596 nm for measuring the path length from the aircraft to the scattering surface and/or cloud tops. The MFLL was onboard all ACT-America seasonal campaigns, except Summer 2019. The MFLL-measured column-averaged CO2 values have certain distinct vertical weights on CO2 profiles depending on the meteorological conditions and the wavelengths used at the measurement time and location. This product includes the instrument location at the time of measurement in geographic coordinates and altitude, along with a vector of weighting function values representing conditions along the nadir direction.
&lt;br&gt;&lt;h4 id&#x3D;&quot;actamerica_merge_1593&quot;&gt;ACTAMERICA_Merge_1593&lt;/h4&gt;
This dataset provides merged data products acquired during flights over the central and eastern United States as part of the Atmospheric Carbon and Transport - America (ACT-America) project. Two aircraft platforms, the NASA Langley Beechcraft B200 King Air and the NASA Goddard Space Flight Center&amp;#39;s C-130H Hercules, were used to collect high-quality in situ measurements across a variety of continental surfaces and atmospheric conditions. The merged data products are composed of continuous in situ measurements of atmospheric carbon dioxide (CO2), methane (CH4), carbon monoxide (CO), ozone (O3), and ethane (C2H6, B200 aircraft only) that were averaged to uniform intervals and merged with aircraft navigation and meteorological variables as well as trace gas concentrations from discrete flask samples collected with the Programmable Flask Package (PFP). These merged data products provide integrated measurements at intervals useful to the modeling community for studying the transport and fluxes of atmospheric carbon dioxide and methane across North America.
&lt;br&gt;&lt;h4 id&#x3D;&quot;profile_based_pbl_heights_1706&quot;&gt;Profile_based_PBL_heights_1706&lt;/h4&gt;
This dataset provides profile-based estimates of the height to the top of the planetary boundary layer (PBL), also known as the atmospheric boundary layer (ABL), in meters above mean sea level estimated from meteorological measurements acquired during ascending or descending vertical profile flight segments during NASA&amp;#39;s Atmospheric Carbon and Transport - America (ACT-America) airborne campaign. ACT-America flights sampled the atmosphere over the central and eastern United States seasonally from 2016 - 2019. Two aircraft platforms, the NASA Langley Beechcraft B-200 King Air and the NASA Goddard Space Flight Center&amp;#39;s C-130 Hercules, were used to collect high-quality in situ measurements across a variety of continental surfaces and atmospheric conditions.
&lt;br&gt;&lt;h4 id&#x3D;&quot;actamerica_wrf_chem_output_1884&quot;&gt;ACTAMERICA_WRF_Chem_Output_1884&lt;/h4&gt;
This dataset includes hourly output from the WRF-Chem simulation model for North America at a resolution of 27 km for 2016-06-29 through 2019-07-31. WRF-Chem is the Weather Research and Forecasting (WRF) model coupled with Chemistry. The output provides baseline conditions for comparison to data from ACT-America airborne campaigns conducted to study atmospheric CO2 and CH4 from 2016 to 2019. The WRF-Chem (v. 3.6.1) model was driven by meteorological conditions and sea-surface temperatures. The output includes 50 vertical layers up to atmospheric pressure of 50 hPa with 20 levels in the lowest 1 km. It provides information for understanding the fluxes and atmospheric transport of carbon dioxide (CO2), methane (CH4), and ethane (C2H6).
&lt;br&gt;&lt;h4 id&#x3D;&quot;flexpart_influence_functions_2018&quot;&gt;FLEXPART_Influence_Functions_2018&lt;/h4&gt;
This dataset contains a set of Lagrangian particle dispersion simulations of carbon dioxide concentrations using the FLEXible PARTicle (FLEXPART) model. FLEXPART quantified the source-receptor relationships, so-called &amp;quot;influence functions&amp;quot;, in a backward mode. The simulations were constructed for five Atmospheric Carbon and Transport America (ACT-America) deployments over the eastern U.S. that occurred in 2016-2019. Each receptor of the influence function is the 30-second or 10-minute interval along flight tracks, characterized by a box with boundaries between the maximum and minimum latitude/longitude as well as between the maximum and minimum altitudes during the interval. Each receptor box released 5,000 particles and simulated their transport and dispersion backward for 10 or 20 days. The simulations were driven by 27-km meteorology provided by the WRF-Chem simulation or by ERA-Interim data from the European Centre for Medium-Range Weather Forecasts (ECMWF). Background levels of carbon dioxide were obtained from CarbonTracker and OCO-2 v9 MIP. The data are provided in netCDF and FLEXPART binary formats.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.ornldaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA AEHYP Project</title>
      <link>https://registry.opendata.aws/nasa-aehyp</link>
      <guid>https://registry.opendata.aws/nasa-aehyp</guid>
      <description>The Airborne Hyperspectral Reflectance Indian Cave Nebraska Multi-Day (AEHYPICNE1M) data are from the Indian Cave Forest Global Earth Observatory (&lt;a href&#x3D;&quot;https://forestgeo.si.edu/&quot;&gt;ForestGeo&lt;/a&gt;) plot in Indian Cave State Park in southeastern Nebraska. The data have a spatial resolution of 1 meter (m) and fall in the spectral range of 400-1000 nanometers (nm). The data can be used by researchers in developing new capabilities for the remote sensing of forest diversity and function, as well as a global biodiversity monitoring system. The &lt;a href&#x3D;&quot;https://forestgeo.si.edu/sites/north-america/indian-cave&quot;&gt;Indian Cave ForestGeo&lt;/a&gt; plot airborne data were collected on September 6, 2019, and August 4, 2022. The images were collected by the Nebraska Earth Observatory (NEO), using an AisaKESTREL (Specim, Oulu, Finland) hyperspectral pushbroom sensor mounted on a Piper Saratoga fixed-wing aircraft. The AEHYPICNE1M product provides images with 178 hyperspectral bands that have been radiometrically, geometrically, and atmospherically corrected.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aehyp1tppok&quot;&gt;AEHYP1TPPOK&lt;/h4&gt;
The Airborne Hyperspectral Reflectance data are from The Nature Conservancy’s Tallgrass Prairie Preserve in northeastern Oklahoma. The data have a spatial resolution of 1 meter (m) and fall in the spectral range of 400-2450 nanometers (nm). These data can be used to develop approaches for studying grassland biodiversity. The Nature Conservancy’s Tallgrass Prairie Preserve airborne data were collected on three separate occasions: August 3, 2020, July 31, 2021, and July 23, 2022. The images were collected by SpecTIR Remote Sensing (SRS) Division, contracted by Oklahoma State University, using an AisaFENIX 1K (Specim, Oulu, Finland) pushbroom sensor mounted on a Twin Commander 500 fixed wing aircraft. The AEHYP1TPPOK product provides orthorectified individual flight lines of 323 hyperspectral bands that have been radiometrically, geometrically, and atmospherically corrected.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aehypccmn300mm&quot;&gt;AEHYPCCMN300MM&lt;/h4&gt;
The Airborne Hyperspectral Reflectance image mosaic is of the Long-Term Ecological Research (LTER) site at Cedar Creek Ecosystem Science Reserve (CCESR), Minnesota (AEHYPCCMN300MM). The image is at approximate 1 meter and resampled to 300 millimeter (0.3 meter) spatial resolution during processing in the 400 to 970 nanometer (nm) spectral range. This image can be used to understand the optical diversity-biodiversity relationship and investigate the spatial sensitivity of the relationship at local scales. Airborne data for the LTER Cedar Creek site were collected on August 2, 2014, using an AisaEAGLE airborne hyperspectral system mounted on a fixed-wing Piper Saratoga aircraft. The images were collected from a height of 1,540 m and spectral binning (approximately 10 nm) increased the signal-to-noise ratio of the data. Fast Line-of-sight Atmospheric Analysis of Hypercubes (FLAASH) software was used for atmospheric correction in converting radiance to reflectance. Airborne data covered all the prairie grassland plots in the biodiversity (BioDIV) experiment and the Biodiversity and Climate experiment. The data were mosaicked as one image. Provided in the AEHYPCCMN300MM product are 64 hyperspectral bands in an Environment for Visualizing Images (ENVI) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aehypwrne1m&quot;&gt;AEHYPWRNE1M&lt;/h4&gt;
The Airborne Hyperspectral Reflectance image mosaic is of the long-term prairie restoration and biodiversity study site led by the Nature Conservancy near Wood River, Nebraska (AEHYPWRNE1M). The approximately 1-meter (m) spatial resolution image was resampled in the 397 to 1004 nanometer (nm) spectral range. This image can be used to detect grassland biodiversity over time to help develop a regional biodiversity monitoring program. Airborne data for the long-term prairie restoration and biodiversity Wood River site were collected on four separate occasions: August 23, 2017; June 27, 2018; August 24, 2018; October 16, 2018. The images were collected using an AisaKESTREL compact hyperspectral pushbroom sensor. Provided in the AEHYPWRNE1M product are 178 hyperspectral bands that have been radiometrically, geometrically, and atmospherically corrected.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA AQUARIUS SAC-D Project</title>
      <link>https://registry.opendata.aws/nasa-aquarius-sac-d</link>
      <guid>https://registry.opendata.aws/nasa-aquarius-sac-d</guid>
      <description>The version 5.0 Aquarius CAP Level 2 product contains the fourth release of the AQUARIUS/SAC-D orbital/swath data based on the Combined Active Passive (CAP) algorithm. CAP is a P.I. produced dataset developed and provided by JPL. This Level 2 dataset contains sea surface salinity (SSS), wind speed and wind direction data derived from 3 different radiometers and the onboard scatterometer. The CAP algorithm simultaneously retrieves the salinity, wind speed and direction by minimizing the sum of squared differences between model and observations. The main improvements in CAP V5.0 relative to the previous version include: updates to the Geophysical Model Functions to 4th order harmonics with the inclusion of sea surface temperature (SST) and stability at air-sea interface effects; use of the Canadian Meteorological Center (CMC) SST product as the new source ancillary sea surface temperature data in place of NOAA OI SST. Each L2 data file covers one 98 minute orbit. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_raincorrected_cap_7day_v5&quot;&gt;AQUARIUS_L3_SSS_RAINCORRECTED_CAP_7DAY_V5&lt;/h4&gt;
Version 5.0 Aquarius CAP Level 3 products are the fourth release of the AQUARIUS/SAC-D mapped salinity and wind speed data based on the Combined Active Passive (CAP) algorithm. CAP Level 3 standard mapped image products contain gridded 1 degree spatial resolution salinity and wind speed data averaged over 7 day and monthly time scales. This particular dataset is the 7-Day running mean sea surface salinity (SSS) rain corrected V5.0 Aquarius CAP product. CAP is a P.I. produced dataset developed and provided by JPL. The CAP algorithm utilizes data from both the onboard radiometer and scatterometer to simultaneously retrieve salinity, wind speed and direction by minimizing the sum of squared differences between model and observations. The main improvements in CAP V5.0 relative to the previous version include: updates to the Geophysical Model Functions to 4th order harmonics with the inclusion of sea surface temperature (SST) and stability at air-sea interface effects; use of the Canadian Meteorological Center (CMC) SST product as the new source ancillary sea surface temperature data in place of NOAA OI SST. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_cap_7day_v5&quot;&gt;AQUARIUS_L3_SSS_CAP_7DAY_V5&lt;/h4&gt;
Version 5.0 Aquarius CAP Level 3 products are the fourth release of the AQUARIUS/SAC-D mapped salinity and wind speed data based on the Combined Active Passive (CAP) algorithm. Level 3 standard mapped image products contain gridded 1 degree spatial resolution salinity and wind speed data averaged over 7 day and monthly time scales. This particular dataset is the 7-Day running mean sea surface salinity (SSS) V5.0 Aquarius CAP product. CAP is a P.I. produced dataset developed and provided by JPL. The CAP algorithm utilizes data from both the onboard radiometer and scatterometer to simultaneously retrieve salinity, wind speed and direction by minimizing the sum of squared differences between model and observations. The main improvements in CAP V5.0 relative to the previous version include: updates to the Geophysical Model Functions to 4th order harmonics with the inclusion of sea surface temperature (SST) and stability at air-sea interface effects; use of the Canadian Meteorological Center (CMC) SST product as the new source ancillary sea surface temperature data in place of NOAA OI SST. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_ancillary_celestialsky_v1&quot;&gt;AQUARIUS_ANCILLARY_CELESTIALSKY_V1&lt;/h4&gt;
This datasets contains three maps of L-band (wavelength &#x3D; 21 cm) brightness temperature of the celestial sky (&amp;quot;Galaxy&amp;quot;) used in the processing of the NASA Aquarius instrument data. The maps report Sky brightness temperatures in Kelvin gridded on the Earth Centered Inertial (ECI) reference frame epoch J2000. They are sampled over 721 Declinations between -90 degrees and +90 degrees and 1441 Right Ascensions between 0 degrees and 360 degrees, all evenly spaced at 0.25 degrees intervals. The brightness temperatures are assumed temporally invariant and polarization has been neglected. They include microwave continuum and atomic hydrogen line (HI) emissions. The maps differ only in how the strong radio source Cassiopeia A has been included into the whole sky background surveys: 1/ TB_no_Cas_A does not include Cassiopeia A and reports only the whole Sky surveys. 2/ TB_Cas_A_1cell spread Cas A total flux homogeneously over 1 map grid cell (i.e. 9.8572E-6 sr). 3/ TB_Cas_A_beam spreads Cas A over surrounding grid cells using a convolution by a Gaussian beam with HPBW of 35 arcmin (equivalent to the instrument used for the Sky surveys). Cassiopeia A is a supernova remnant (SNR) in the constellation Cassiopeia and the brightest extra-solar radio source in the sky at frequencies above 1.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l2_sss_v5&quot;&gt;AQUARIUS_L2_SSS_V5&lt;/h4&gt;
The version 5.0 Aquarius Level 2 product is the official third release of the orbital/swath data from AQUARIUS/SAC-D mission. The Aquarius Level 2 data set contains sea surface salinity (SSS) and wind speed data derived from 3 different radiometers and the onboard scatterometer. Included also in the Level 2 data are the horizontal and vertical brightness temperatures (TH and TV) for each radiometer, ancillary data, flags, converted telemetry and navigation data. Each data file covers one 98 minute orbit. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath. Enhancements to the version 5.0 Level 2 data relative to v4.0 include: improvement of the salinity retrieval geophysical model for SST bias, estimates of SSS uncertainties (systematic and random components), and inclusion of a new spiciness variable.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_ancillary_sst_smi_28day-runningmean_v5&quot;&gt;AQUARIUS_L3_ANCILLARY_SST_SMI_28DAY-RUNNINGMEAN_V5&lt;/h4&gt;
Aquarius Level 3 ancillary sea surface temperature (SST) standard mapped image data are the ancillary SST data used in the Aquarius calibration for salinity retrieval. They are simply the daily SSTs from the Reynolds National Climatic Data Center (NCDC) 0.25 degree dataset, gridded and averaged using the Aquarius processing L2-L3 processing scheme to the same 1 degree spatial resolution and daily, 7 day, monthly, 7-Day, and annual time intervals as Aquarius L3 standard salinity and wind speed products. This particular data set is the 28-Day running mean, ancillary sea surface temperature product associated with version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_ancillary_sst_smi_7day-runningmean_v5&quot;&gt;AQUARIUS_L3_ANCILLARY_SST_SMI_7DAY-RUNNINGMEAN_V5&lt;/h4&gt;
Aquarius Level 3 ancillary sea surface temperature (SST) standard mapped image data are the ancillary SST data used in the Aquarius calibration for salinity retrieval. They are simply the daily SSTs from the Reynolds National Climatic Data Center (NCDC) 0.25 degree dataset, gridded and averaged using the Aquarius processing L2-L3 processing scheme to the same 1 degree spatial resolution and daily, 7 day, monthly, seasonal, and annual time intervals as Aquarius L3 standard salinity and wind speed products. This particular data set is the 7-Day running mean ancillary sea surface temperature product associated with version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_ancillary_sst_smi_annual_v5&quot;&gt;AQUARIUS_L3_ANCILLARY_SST_SMI_ANNUAL_V5&lt;/h4&gt;
Aquarius Level 3 ancillary sea surface temperature (SST) standard mapped image data are the ancillary SST data used in the Aquarius calibration for salinity retrieval. They are simply the daily SSTs from the Reynolds National Climatic Data Center (NCDC) 0.25 degree dataset, gridded and averaged using the Aquarius processing L2-L3 processing scheme to the same 1 degree spatial resolution and daily, 7 day, monthly, Annual, and annual time intervals as Aquarius L3 standard salinity and wind speed products. This particular data set is the Annual ancillary sea surface temperature product associated with version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_ancillary_sst_smia_daily_v5&quot;&gt;AQUARIUS_L3_ANCILLARY_SST_SMIA_DAILY_V5&lt;/h4&gt;
Aquarius Level 3 ancillary sea surface temperature (SST) standard mapped image data are the ancillary SST data used in the Aquarius calibration for salinity retrieval. They are simply the daily SSTs from the Reynolds National Climatic Data Center (NCDC) 0.25 degree dataset, gridded and averaged using the Aquarius processing L2-L3 processing scheme to the same 1 degree spatial resolution and daily, 7 day, monthly, Daily, and Daily time intervals as Aquarius L3 standard salinity and wind speed products. This particular data set is the Daily, ascending ancillary sea surface temperature product associated with version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss-rainflagged_sm_smia_monthly_v5&quot;&gt;AQUARIUS_L3_SSS-RainFlagged_SM_SMIA_MONTHLY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Monthly, Ascending rain-flagged sea surface salinity smoothed product for version 5.0 of the Aquarius data set. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss-rainflagged_sm_smid_monthly_v5&quot;&gt;AQUARIUS_L3_SSS-RainFlagged_SM_SMID_MONTHLY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Monthly, Descending rain-flagged sea surface salinity smoothed product for version 5.0 of the Aquarius data set. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss-rainflagged_sm_smi_monthly_v5&quot;&gt;AQUARIUS_L3_SSS-RainFlagged_SM_SMI_MONTHLY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Monthly rain-flagged sea surface salinity smoothed product for version 5.0 of the Aquarius data set. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss-rainflagged_smi_28day-runningmean_v5&quot;&gt;AQUARIUS_L3_SSS-RainFlagged_SMI_28DAY-RUNNINGMEAN_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) rain-flagged standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 28-Day running mean, rain-flagged rain-flagged sea surface salinity product for version 5.0 of the Aquarius data set. The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss-rainflagged_smi_7day_v5&quot;&gt;AQUARIUS_L3_SSS-RainFlagged_SMI_7DAY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) rain-flagged standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 7-Day rain-flagged rain-flagged sea surface salinity product for version 5.0 of the Aquarius data set. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss-rainflagged_smi_7day-runningmean_v5&quot;&gt;AQUARIUS_L3_SSS-RainFlagged_SMI_7DAY-RUNNINGMEAN_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) rain-flagged standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 7-Day running mean rain-flagged rain-flagged sea surface salinity product for version 5.0 of the Aquarius data set. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss-rainflagged_smi_annual_v5&quot;&gt;AQUARIUS_L3_SSS-RainFlagged_SMI_ANNUAL_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) rain-flagged standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Annual rain-flagged rain-flagged sea surface salinity product for version 5.0 of the Aquarius data set. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss-rainflagged_smia_28day-runningmean_v5&quot;&gt;AQUARIUS_L3_SSS-RainFlagged_SMIA_28DAY-RUNNINGMEAN_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) rain-flagged standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 28-Day running mean, Ascending rain-flagged rain-flagged sea surface salinity product for version 5.0 of the Aquarius data set. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss-rainflagged_smia_7day_v5&quot;&gt;AQUARIUS_L3_SSS-RainFlagged_SMIA_7DAY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) rain-flagged standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 7-Day, Ascending rain-flagged rain-flagged sea surface salinity product for version 5.0 of the Aquarius data set. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss-rainflagged_smia_annual_v5&quot;&gt;AQUARIUS_L3_SSS-RainFlagged_SMIA_ANNUAL_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) rain-flagged standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Annual, Ascending rain-flagged rain-flagged sea surface salinity product for version 5.0 of the Aquarius data set. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss-rainflagged_smia_daily_v5&quot;&gt;AQUARIUS_L3_SSS-RainFlagged_SMIA_DAILY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) rain-flagged standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Daily, Ascending rain-flagged rain-flagged sea surface salinity product for version 5.0 of the Aquarius data set. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss-rainflagged_smia_cumulative_v5&quot;&gt;AQUARIUS_L3_SSS-RainFlagged_SMIA_CUMULATIVE_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the mission cummulative, Ascending rain-flagged sea surface salinity product for version 5.0 of the Aquarius data set. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss-rainflagged_smia_monthly-climatology_v5&quot;&gt;AQUARIUS_L3_SSS-RainFlagged_SMIA_MONTHLY-CLIMATOLOGY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) rain-flagged standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the monthly climatology, Ascending rain-flagged rain-flagged sea surface salinity product for version 5.0. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss-rainflagged_smia_monthly_v5&quot;&gt;AQUARIUS_L3_SSS-RainFlagged_SMIA_MONTHLY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) rain-flagged standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Monthly, Ascending rain-flagged rain-flagged sea surface salinity product for version 5.0 of the Aquarius data set. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss-rainflagged_smia_seasonal-climatology_v5&quot;&gt;AQUARIUS_L3_SSS-RainFlagged_SMIA_SEASONAL-CLIMATOLOGY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) rain-flagged standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the seasonal climatology, Ascending rain-flagged rain-flagged sea surface salinity product for version 5.0 of the Aquarius data set. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss-rainflagged_smia_3month_v5&quot;&gt;AQUARIUS_L3_SSS-RainFlagged_SMIA_3MONTH_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) rain-flagged standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Seasonal, Ascending rain-flagged rain-flagged sea surface salinity product for version 5.0 of the Aquarius data set. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss-rainflagged_smi_daily_v5&quot;&gt;AQUARIUS_L3_SSS-RainFlagged_SMI_DAILY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) rain-flagged standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Daily rain-flagged rain-flagged sea surface salinity product for version 5.0 of the Aquarius data set. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss-rainflagged_smid_28day-runningmean_v5&quot;&gt;AQUARIUS_L3_SSS-RainFlagged_SMID_28DAY-RUNNINGMEAN_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) rain-flagged standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 28-Day running mean, Descending rain-flagged rain-flagged sea surface salinity product for version 5.0 of the Aquarius data set. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss-rainflagged_smid_7day_v5&quot;&gt;AQUARIUS_L3_SSS-RainFlagged_SMID_7DAY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) rain-flagged standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 7-Day, Descending rain-flagged rain-flagged sea surface salinity product for version 5.0 of the Aquarius data set. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss-rainflagged_smid_annual_v5&quot;&gt;AQUARIUS_L3_SSS-RainFlagged_SMID_ANNUAL_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) rain-flagged standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Annual, Descending rain-flagged sea surface salinity product for version 5.0 of the Aquarius data set. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss-rainflagged_smid_daily_v5&quot;&gt;AQUARIUS_L3_SSS-RainFlagged_SMID_DAILY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) rain-flagged standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Daily, Descending rain-flagged sea surface salinity product for version 5.0 of the Aquarius data set. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss-rainflagged_smid_cumulative_v5&quot;&gt;AQUARIUS_L3_SSS-RainFlagged_SMID_CUMULATIVE_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the mission cummulative, Descending rain-flagged sea surface salinity product for version 5.0 of the Aquarius data set. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss-rainflagged_smid_monthly-climatology_v5&quot;&gt;AQUARIUS_L3_SSS-RainFlagged_SMID_MONTHLY-CLIMATOLOGY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) rain-flagged standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the monthly climatology, Descending rain-flagged sea surface salinity product for version 5.0 of the Aquarius data set. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onbard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss-rainflagged_smid_monthly_v5&quot;&gt;AQUARIUS_L3_SSS-RainFlagged_SMID_MONTHLY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) rain-flagged standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Monthly, Descending rain-flagged sea surface salinity product for version 5.0 of the Aquarius data set. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss-rainflagged_smid_seasonal-climatology_v5&quot;&gt;AQUARIUS_L3_SSS-RainFlagged_SMID_SEASONAL-CLIMATOLOGY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) rain-flagged standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the seasonal climatology, Descending rain-flagged sea surface salinity product for version 5.0 of the Aquarius data set. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss-rainflagged_smid_3month_v5&quot;&gt;AQUARIUS_L3_SSS-RainFlagged_SMID_3MONTH_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) rain-flagged standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Seasonal, Descending rain-flagged rain-flagged sea surface salinity product for version 5.0 of the Aquarius data set. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss-rainflagged_smi_cumulative_v5&quot;&gt;AQUARIUS_L3_SSS-RainFlagged_SMI_CUMULATIVE_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the mission cummulative rain-flagged sea surface salinity product for version 5.0 of the Aquarius data set. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss-rainflagged_smi_monthly-climatology_v5&quot;&gt;AQUARIUS_L3_SSS-RainFlagged_SMI_MONTHLY-CLIMATOLOGY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) rain-flagged standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the monthly climatology rain-flagged rain-flagged sea surface salinity product for version 5.0 of the Aquarius data set. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss-rainflagged_smi_monthly_v5&quot;&gt;AQUARIUS_L3_SSS-RainFlagged_SMI_MONTHLY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) rain-flagged standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Monthly rain-flagged rain-flagged sea surface salinity product for version 5.0 of the Aquarius dataset. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss-rainflagged_smi_seasonal-climatology_v5&quot;&gt;AQUARIUS_L3_SSS-RainFlagged_SMI_SEASONAL-CLIMATOLOGY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) rain-flagged standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the seasonal climatology rain-flagged rain-flagged sea surface salinity product for version 5.0 of the Aquarius data set. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss-rainflagged_smi_3month_v5&quot;&gt;AQUARIUS_L3_SSS-RainFlagged_SMI_3MONTH_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) rain-flagged standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Seasonal rain-flagged rain-flagged sea surface salinity product for version 5.0 of the Aquarius data set. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_density_smi_28day-runningmean_v5&quot;&gt;AQUARIUS_L3_DENSITY_SMI_28DAY-RUNNINGMEAN_V5&lt;/h4&gt;
Aquarius Level 3 sea surface density standard mapped image data contains gridded 1 degree spatial resolution derived density averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 28-Day running mean, sea surface density product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Surface density estimates are based on TEOS-10 and derived using retrieved salinity from Aquarius and collocated ancillary SST (Reynolds OI 0.25 degree product). The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_density_smi_7day_v5&quot;&gt;AQUARIUS_L3_DENSITY_SMI_7DAY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface density standard mapped image data contains gridded 1 degree spatial resolution derived density averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 7-Day, sea surface density product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Surface density estimates are based on TEOS-10 and derived using retrieved salinity from Aquarius and collocated ancillary SST (Reynolds OI 0.25 degree product). The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_density_smi_7day-runningmean_v5&quot;&gt;AQUARIUS_L3_DENSITY_SMI_7DAY-RUNNINGMEAN_V5&lt;/h4&gt;
Aquarius Level 3 sea surface density standard mapped image data contains gridded 1 degree spatial resolution derived density averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 7-Day running mean, sea surface density product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Surface density estimates are based on TEOS-10 and derived using retrieved salinity from Aquarius and collocated ancillary SST (Reynolds OI 0.25 degree product). The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_density_smi_annual_v5&quot;&gt;AQUARIUS_L3_DENSITY_SMI_ANNUAL_V5&lt;/h4&gt;
Aquarius Level 3 sea surface density standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Annual, sea surface density product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Surface density estimates are based on TEOS-10 and derived using retrieved salinity from Aquarius and collocated ancillary SST (Reynolds OI 0.25 degree product). The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_density_smia_28day-runningmean_v5&quot;&gt;AQUARIUS_L3_DENSITY_SMIA_28DAY-RUNNINGMEAN_V5&lt;/h4&gt;
Aquarius Level 3 sea surface density standard mapped image data contains gridded 1 degree spatial resolution density data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 28-Day running mean, Ascending sea surface density product for version 5.0 of the Aquarius data set. Only retrieved values for Ascending passes have been used to create this product. Surface density estimates are based on TEOS-10 and derived using retrieved salinity from Aquarius and collocated ancillary SST (Reynolds OI 0.25 degree product). The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_density_smia_7day_v5&quot;&gt;AQUARIUS_L3_DENSITY_SMIA_7DAY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface density standard mapped image data contains gridded 1 degree spatial resolution density data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 7-Day, Ascending sea surface density product for version 5.0 of the Aquarius data set. Only retrieved values for Ascending passes have been used to create this product. Surface density estimates are based on TEOS-10 and derived using retrieved salinity from Aquarius and collocated ancillary SST (Reynolds OI 0.25 degree product). The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_density_smia_annual_v5&quot;&gt;AQUARIUS_L3_DENSITY_SMIA_ANNUAL_V5&lt;/h4&gt;
Aquarius Level 3 sea surface density standard mapped image data contains gridded 1 degree spatial resolution density data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Annual, Ascending sea surface density product for version 5.0 of the Aquarius data set. Only retrieved values for Ascending passes have been used to create this product. Surface density estimates are based on TEOS-10 and derived using retrieved salinity from Aquarius and collocated ancillary SST (Reynolds OI 0.25 degree product). The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_density_smia_daily_v5&quot;&gt;AQUARIUS_L3_DENSITY_SMIA_DAILY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface density standard mapped image data contains gridded 1 degree spatial resolution density data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Daily, Ascending sea surface density product for version 5.0 of the Aquarius data set. Only retrieved values for Ascending passes have been used to create this product. Surface density estimates are based on TEOS-10 and derived using retrieved salinity from Aquarius and collocated ancillary SST (Reynolds OI 0.25 degree product). The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_density_smia_cumulative_v5&quot;&gt;AQUARIUS_L3_DENSITY_SMIA_CUMULATIVE_V5&lt;/h4&gt;
Aquarius Level 3 sea surface density standard mapped image data contains gridded 1 degree spatial resolution density data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the mission series mean or cumulative, Ascending sea surface density product for version 5.0 of the Aquarius data set. Only retrieved values for Ascending passes have been used to create this product. Surface density estimates are based on TEOS-10 and derived using retrieved salinity from Aquarius and collocated ancillary SST (Reynolds OI 0.25 degree product). The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_density_smia_monthly-climatology_v5&quot;&gt;AQUARIUS_L3_DENSITY_SMIA_MONTHLY-CLIMATOLOGY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface density standard mapped image data contains gridded 1 degree spatial resolution density data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the monthly climatology, Ascending sea surface density product for version 5.0. Only retrieved values for Ascending passes have been used to create this product. Surface density estimates are based on TEOS-10 and derived using retrieved salinity from Aquarius and collocated ancillary SST (Reynolds OI 0.25 degree product). The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_density_smia_monthly_v5&quot;&gt;AQUARIUS_L3_DENSITY_SMIA_MONTHLY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface density standard mapped image data contains gridded 1 degree spatial resolution density data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Monthly, Ascending sea surface density product for version 5.0 of the Aquarius data set. Only retrieved values for Ascending passes have been used to create this product. Surface density estimates are based on TEOS-10 and derived using retrieved salinity from Aquarius and collocated ancillary SST (Reynolds OI 0.25 degree product). The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_density_smia_seasonal-climatology_v5&quot;&gt;AQUARIUS_L3_DENSITY_SMIA_SEASONAL-CLIMATOLOGY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface density standard mapped image data contains gridded 1 degree spatial resolution density data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the seasonal climatology, Ascending sea surface density product for version 5.0 of the Aquarius data set. Only retrieved values for Ascending passes have been used to create this product. Surface density estimates are based on TEOS-10 and derived using retrieved salinity from Aquarius and collocated ancillary SST (Reynolds OI 0.25 degree product). The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_density_smia_3month_v5&quot;&gt;AQUARIUS_L3_DENSITY_SMIA_3MONTH_V5&lt;/h4&gt;
Aquarius Level 3 sea surface density standard mapped image data contains gridded 1 degree spatial resolution density data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Seasonal, Ascending sea surface density product for version 5.0 of the Aquarius data set. Only retrieved values for Ascending passes have been used to create this product. Surface density estimates are based on TEOS-10 and derived using retrieved salinity from Aquarius and collocated ancillary SST (Reynolds OI 0.25 degree product). The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_density_smi_daily_v5&quot;&gt;AQUARIUS_L3_DENSITY_SMI_DAILY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface density standard mapped image data contains gridded 1 degree spatial resolution derived density averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Daily, sea surface density product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Surface density estimates are based on TEOS-10 and derived using retrieved salinity from Aquarius and collocated ancillary SST (Reynolds OI 0.25 degree product). The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_density_smid_28day-runningmean_v5&quot;&gt;AQUARIUS_L3_DENSITY_SMID_28DAY-RUNNINGMEAN_V5&lt;/h4&gt;
Aquarius Level 3 sea surface density standard mapped image data contains gridded 1 degree spatial resolution density data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 28-Day running mean, Descending sea surface density product for version 5.0 of the Aquarius data set. Only retrieved values for Descending passes have been used to create this product. Surface density estimates are based on TEOS-10 and derived using retrieved salinity from Aquarius and collocated ancillary SST (Reynolds OI 0.25 degree product). The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_density_smid_7day_v5&quot;&gt;AQUARIUS_L3_DENSITY_SMID_7DAY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface density standard mapped image data contains gridded 1 degree spatial resolution density data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 7-Day, Descending sea surface density product for version 5.0 of the Aquarius data set. Only retrieved values for Descending passes have been used to create this product. Surface density estimates are based on TEOS-10 and derived using retrieved salinity from Aquarius and collocated ancillary SST (Reynolds OI 0.25 degree product). The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_density_smid_annual_v5&quot;&gt;AQUARIUS_L3_DENSITY_SMID_ANNUAL_V5&lt;/h4&gt;
Aquarius Level 3 sea surface density standard mapped image data contains gridded 1 degree spatial resolution density data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Annual, Descending sea surface density product for version 5.0 of the Aquarius data set. Only retrieved values for Descending passes have been used to create this product. Surface density estimates are based on TEOS-10 and derived using retrieved salinity from Aquarius and collocated ancillary SST (Reynolds OI 0.25 degree product). The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_density_smid_daily_v5&quot;&gt;AQUARIUS_L3_DENSITY_SMID_DAILY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface density standard mapped image data contains gridded 1 degree spatial resolution density data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Daily, Descending sea surface density product for version 5.0 of the Aquarius data set. Surface density estimates are based on TEOS-10 and derived using retrieved salinity from Aquarius and collocated ancillary SST (Reynolds OI 0.25 degree product). The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_density_smid_cumulative_v5&quot;&gt;AQUARIUS_L3_DENSITY_SMID_CUMULATIVE_V5&lt;/h4&gt;
Aquarius Level 3 sea surface density standard mapped image data contains gridded 1 degree spatial resolution density data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the mission series mean or cumulative, Descending sea surface density product for version 5.0 of the Aquarius data set. Only retrieved values for Descending passes have been used to create this product. Surface density estimates are based on TEOS-10 and derived using retrieved salinity from Aquarius and collocated ancillary SST (Reynolds OI 0.25 degree product). The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_density_smid_monthly-climatology_v5&quot;&gt;AQUARIUS_L3_DENSITY_SMID_MONTHLY-CLIMATOLOGY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface density standard mapped image data contains gridded 1 degree spatial resolution density data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the monthly climatology, Descending sea surface density product for version 5.0 of the Aquarius data set. Only retrieved values for Descending passes have been used to create this product. Surface density estimates are based on TEOS-10 and derived using retrieved salinity from Aquarius and collocated ancillary SST (Reynolds OI 0.25 degree product). The Aquarius instrument is onbard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_density_smid_monthly_v5&quot;&gt;AQUARIUS_L3_DENSITY_SMID_MONTHLY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface density standard mapped image data contains gridded 1 degree spatial resolution density data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Monthly, Descending sea surface density product for version 5.0 of the Aquarius data set. Only retrieved values for Descending passes have been used to create this product. Surface density estimates are based on TEOS-10 and derived using retrieved salinity from Aquarius and collocated ancillary SST (Reynolds OI 0.25 degree product). The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_density_smid_seasonal-climatology_v5&quot;&gt;AQUARIUS_L3_DENSITY_SMID_SEASONAL-CLIMATOLOGY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface density standard mapped image data contains gridded 1 degree spatial resolution density data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the seasonal climatology, Descending sea surface density product for version 5.0 of the Aquarius data set. Only retrieved values for Descending passes have been used to create this product. Surface density estimates are based on TEOS-10 and derived using retrieved salinity from Aquarius and collocated ancillary SST (Reynolds OI 0.25 degree product). The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_density_smid_3month_v5&quot;&gt;AQUARIUS_L3_DENSITY_SMID_3MONTH_V5&lt;/h4&gt;
Aquarius Level 3 sea surface density standard mapped image data contains gridded 1 degree spatial resolution density data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Seasonal, Descending sea surface density product for version 5.0 of the Aquarius data set. Only retrieved values for Descending passes have been used to create this product. Surface density estimates are based on TEOS-10 and derived using retrieved salinity from Aquarius and collocated ancillary SST (Reynolds OI 0.25 degree product). The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_density_smi_cumulative_v5&quot;&gt;AQUARIUS_L3_DENSITY_SMI_CUMULATIVE_V5&lt;/h4&gt;
Aquarius Level 3 sea surface density standard mapped image data contains gridded 1 degree spatial resolution derived density averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the mission series mean or cumulative, sea surface density product for version 5.0 of the Aquarius data set. Surface density estimates are based on TEOS-10 and derived using retrieved salinity from Aquarius and collocated ancillary SST (Reynolds OI 0.25 degree product). The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_density_smi_monthly-climatology_v5&quot;&gt;AQUARIUS_L3_DENSITY_SMI_MONTHLY-CLIMATOLOGY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface density standard mapped image data contains gridded 1 degree spatial resolution derived density averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the monthly climatology, sea surface density product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Surface density estimates are based on TEOS-10 and derived using retrieved salinity from Aquarius and collocated ancillary SST (Reynolds OI 0.25 degree product). The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_density_smi_monthly_v5&quot;&gt;AQUARIUS_L3_DENSITY_SMI_MONTHLY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface density standard mapped image data contains gridded 1 degree spatial resolution derived density averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Monthly, sea surface density product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Surface density estimates are based on TEOS-10 and derived using retrieved salinity from Aquarius and collocated ancillary SST (Reynolds OI 0.25 degree product). The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_density_smi_seasonal-climatology_v5&quot;&gt;AQUARIUS_L3_DENSITY_SMI_SEASONAL-CLIMATOLOGY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface density standard mapped image data contains gridded 1 degree spatial resolution derived density averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the seasonal climatology, sea surface density product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Surface density estimates are based on TEOS-10 and derived using retrieved salinity from Aquarius and collocated ancillary SST (Reynolds OI 0.25 degree product). The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_density_smi_3month_v5&quot;&gt;AQUARIUS_L3_DENSITY_SMI_3MONTH_V5&lt;/h4&gt;
Aquarius Level 3 sea surface density standard mapped image data contains gridded 1 degree spatial resolution derived density averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Seasonal, sea surface density product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Surface density estimates are based on TEOS-10 and derived using retrieved salinity from Aquarius and collocated ancillary SST (Reynolds OI 0.25 degree product). The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_sm_smia_monthly_v5&quot;&gt;AQUARIUS_L3_SSS_SM_SMIA_MONTHLY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Monthly, Ascending sea surface salinity smoothed product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_sm_smid_monthly_v5&quot;&gt;AQUARIUS_L3_SSS_SM_SMID_MONTHLY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Monthly, Descending sea surface salinity smoothed product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_sm_smi_monthly_v5&quot;&gt;AQUARIUS_L3_SSS_SM_SMI_MONTHLY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Monthly sea surface salinity smoothed product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_smi_28day-runningmean_v5&quot;&gt;AQUARIUS_L3_SSS_SMI_28DAY-RUNNINGMEAN_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 28-Day running mean, sea surface salinity product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_smi_7day_v5&quot;&gt;AQUARIUS_L3_SSS_SMI_7DAY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 7-Day sea surface salinity product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_smi_7day-runningmean_v5&quot;&gt;AQUARIUS_L3_SSS_SMI_7DAY-RUNNINGMEAN_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 7-Day running mean sea surface salinity product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_smi_annual_v5&quot;&gt;AQUARIUS_L3_SSS_SMI_ANNUAL_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Annual sea surface salinity product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_smia_28day-runningmean_v5&quot;&gt;AQUARIUS_L3_SSS_SMIA_28DAY-RUNNINGMEAN_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 28-Day running mean, Ascending sea surface salinity product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_smia_7day_v5&quot;&gt;AQUARIUS_L3_SSS_SMIA_7DAY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 7-Day, Ascending sea surface salinity product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_smia_annual_v5&quot;&gt;AQUARIUS_L3_SSS_SMIA_ANNUAL_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Annual, Ascending sea surface salinity product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_smia_daily_v5&quot;&gt;AQUARIUS_L3_SSS_SMIA_DAILY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Daily, Ascending sea surface salinity product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_smia_cumulative_v5&quot;&gt;AQUARIUS_L3_SSS_SMIA_CUMULATIVE_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the mission series mean or cumulative, Ascending sea surface salinity product for version 5.0 of the Aquarius data set. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_smia_monthly-climatology_v5&quot;&gt;AQUARIUS_L3_SSS_SMIA_MONTHLY-CLIMATOLOGY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the monthly climatology, Ascending sea surface salinity product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_smia_monthly_v5&quot;&gt;AQUARIUS_L3_SSS_SMIA_MONTHLY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Monthly, Ascending sea surface salinity product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_smia_seasonal-climatology_v5&quot;&gt;AQUARIUS_L3_SSS_SMIA_SEASONAL-CLIMATOLOGY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the seasonal climatology, Ascending sea surface salinity product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_smia_3month_v5&quot;&gt;AQUARIUS_L3_SSS_SMIA_3MONTH_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Seasonal, Ascending sea surface salinity product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_smi_daily_v5&quot;&gt;AQUARIUS_L3_SSS_SMI_DAILY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Daily sea surface salinity product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_smid_28day-runningmean_v5&quot;&gt;AQUARIUS_L3_SSS_SMID_28DAY-RUNNINGMEAN_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 28-Day running mean, Descending sea surface salinity product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_smid_7day_v5&quot;&gt;AQUARIUS_L3_SSS_SMID_7DAY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 7-Day, Descending sea surface salinity product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_smid_annual_v5&quot;&gt;AQUARIUS_L3_SSS_SMID_ANNUAL_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Annual, Descending sea surface salinity product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_smid_daily_v5&quot;&gt;AQUARIUS_L3_SSS_SMID_DAILY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Daily, Descending sea surface salinity product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_smid_cumulative_v5&quot;&gt;AQUARIUS_L3_SSS_SMID_CUMULATIVE_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the mission series mean or cumulative, Descending sea surface salinity product for version 5.0 of the Aquarius data set. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_smid_monthly-climatology_v5&quot;&gt;AQUARIUS_L3_SSS_SMID_MONTHLY-CLIMATOLOGY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the monthly climatology, Descending sea surface salinity product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_smid_monthly_v5&quot;&gt;AQUARIUS_L3_SSS_SMID_MONTHLY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Monthly, Descending sea surface salinity product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_smid_seasonal-climatology_v5&quot;&gt;AQUARIUS_L3_SSS_SMID_SEASONAL-CLIMATOLOGY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the seasonal climatology, Descending sea surface salinity product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_smid_3month_v5&quot;&gt;AQUARIUS_L3_SSS_SMID_3MONTH_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Seasonal, Descending sea surface salinity product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_smi_cumulative_v5&quot;&gt;AQUARIUS_L3_SSS_SMI_CUMULATIVE_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the mission series mean or cumulative sea surface salinity product for version 5.0 of the Aquarius data set. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_smi_monthly-climatology_v5&quot;&gt;AQUARIUS_L3_SSS_SMI_MONTHLY-CLIMATOLOGY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the monthly climatology sea surface salinity product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_smi_monthly_v5&quot;&gt;AQUARIUS_L3_SSS_SMI_MONTHLY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Monthly sea surface salinity product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_smi_seasonal-climatology_v5&quot;&gt;AQUARIUS_L3_SSS_SMI_SEASONAL-CLIMATOLOGY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the seasonal climatology sea surface salinity product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_sss_smi_3month_v5&quot;&gt;AQUARIUS_L3_SSS_SMI_3MONTH_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity (SSS) standard mapped image data contains gridded 1 degree spatial resolution SSS averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Seasonal sea surface salinity product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_spiciness_smi_28day-runningmean_v5&quot;&gt;AQUARIUS_L3_SPICINESS_SMI_28DAY-RUNNINGMEAN_V5&lt;/h4&gt;
Aquarius Level 3 sea surface spiciness standard mapped image data contains gridded 1 degree spatial resolution spice data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 28-Day running mean, sea surface spiciness product for version 5.0 of the Aquarius data set. The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_spiciness_smi_7day_v5&quot;&gt;AQUARIUS_L3_SPICINESS_SMI_7DAY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface spiciness standard mapped image data contains gridded 1 degree spatial resolution spice data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 7-Day sea surface spiciness product for version 5.0 of the Aquarius data set. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_spiciness_smi_7day-runningmean_v5&quot;&gt;AQUARIUS_L3_SPICINESS_SMI_7DAY-RUNNINGMEAN_V5&lt;/h4&gt;
Aquarius Level 3 sea surface spiciness standard mapped image data contains gridded 1 degree spatial resolution spice data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 7-Day running mean sea surface spiciness product for version 5.0 of the Aquarius data set. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_spiciness_smi_annual_v5&quot;&gt;AQUARIUS_L3_SPICINESS_SMI_ANNUAL_V5&lt;/h4&gt;
Aquarius Level 3 sea surface spiciness standard mapped image data contains gridded 1 degree spatial resolution spice data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Annual sea surface spiciness product for version 5.0 of the Aquarius data set. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_spiciness_smia_28day-runningmean_v5&quot;&gt;AQUARIUS_L3_SPICINESS_SMIA_28DAY-RUNNINGMEAN_V5&lt;/h4&gt;
Aquarius Level 3 sea surface salinity spiciness standard mapped image data contains gridded 1 degree spatial resolution spice data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 28-Day running mean, Ascending sea surface spiciness product for version 5.0 of the Aquarius data set. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_spiciness_smia_7day_v5&quot;&gt;AQUARIUS_L3_SPICINESS_SMIA_7DAY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface spiciness standard mapped image data contains gridded 1 degree spatial resolution spice data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 7-Day, Ascending sea surface spiciness product for version 5.0 of the Aquarius data set. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_spiciness_smia_annual_v5&quot;&gt;AQUARIUS_L3_SPICINESS_SMIA_ANNUAL_V5&lt;/h4&gt;
Aquarius Level 3 sea surface spiciness standard mapped image data contains gridded 1 degree spatial resolution spice data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Annual, Ascending sea surface spiciness product for version 5.0 of the Aquarius data set. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_spiciness_smia_daily_v5&quot;&gt;AQUARIUS_L3_SPICINESS_SMIA_DAILY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface spiciness standard mapped image data contains gridded 1 degree spatial resolution spice data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Daily, Ascending sea surface spiciness product for version 5.0 of the Aquarius data set. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_spiciness_smia_cumulative_v5&quot;&gt;AQUARIUS_L3_SPICINESS_SMIA_CUMULATIVE_V5&lt;/h4&gt;
Aquarius Level 3 sea surface spiciness standard mapped image data contains gridded 1 degree spatial resolution spice data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the mission series mean or cumulative, Ascending sea surface spiciness product for version 5.0 of the Aquarius data set. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_spiciness_smia_monthly-climatology_v5&quot;&gt;AQUARIUS_L3_SPICINESS_SMIA_MONTHLY-CLIMATOLOGY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface spiciness standard mapped image data contains gridded 1 degree spatial resolution spice data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the monthly climatology, Ascending sea surface spiciness product for version 5.0. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_spiciness_smia_monthly_v5&quot;&gt;AQUARIUS_L3_SPICINESS_SMIA_MONTHLY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface spiciness standard mapped image data contains gridded 1 degree spatial resolution spice data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Monthly, Ascending sea surface spiciness product for version 5.0 of the Aquarius data set. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_spiciness_smia_seasonal-climatology_v5&quot;&gt;AQUARIUS_L3_SPICINESS_SMIA_SEASONAL-CLIMATOLOGY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface spiciness standard mapped image data contains gridded 1 degree spatial resolution spice data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the seasonal climatology, Ascending sea surface spiciness product for version 5.0 of the Aquarius data set. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_spiciness_smia_3month_v5&quot;&gt;AQUARIUS_L3_SPICINESS_SMIA_3MONTH_V5&lt;/h4&gt;
Aquarius Level 3 sea surface spiciness standard mapped image data contains gridded 1 degree spatial resolution spice data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Seasonal, Ascending sea surface spiciness product for version 5.0 of the Aquarius data set. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_spiciness_smi_daily_v5&quot;&gt;AQUARIUS_L3_SPICINESS_SMI_DAILY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface spiciness standard mapped image data contains gridded 1 degree spatial resolution spice data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Daily sea surface spiciness product for version 5.0 of the Aquarius data set. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_spiciness_smid_28day-runningmean_v5&quot;&gt;AQUARIUS_L3_SPICINESS_SMID_28DAY-RUNNINGMEAN_V5&lt;/h4&gt;
Aquarius Level 3 sea surface spiciness standard mapped image data contains gridded 1 degree spatial resolution spice data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 28-Day running mean, Descending sea surface spiciness product for version 5.0 of the Aquarius data set. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_spiciness_smid_7day_v5&quot;&gt;AQUARIUS_L3_SPICINESS_SMID_7DAY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface spiciness standard mapped image data contains gridded 1 degree spatial resolution spice data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 7-Day, Descending sea surface spiciness product for version 5.0 of the Aquarius data set. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_spiciness_smid_annual_v5&quot;&gt;AQUARIUS_L3_SPICINESS_SMID_ANNUAL_V5&lt;/h4&gt;
Aquarius Level 3 sea surface spiciness standard mapped image data contains gridded 1 degree spatial resolution spice data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Annual, Descending sea surface spiciness product for version 5.0 of the Aquarius data set. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_spiciness_smid_daily_v5&quot;&gt;AQUARIUS_L3_SPICINESS_SMID_DAILY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface spiciness standard mapped image data contains gridded 1 degree spatial resolution spice data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Daily, Descending sea surface spiciness product for version 5.0 of the Aquarius data set. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_spiciness_smid_cumulative_v5&quot;&gt;AQUARIUS_L3_SPICINESS_SMID_CUMULATIVE_V5&lt;/h4&gt;
Aquarius Level 3 sea surface spiciness standard mapped image data contains gridded 1 degree spatial resolution spice data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the mission series mean or cumulative, Descending sea surface spiciness product for version 5.0 of the Aquarius data set. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_spiciness_smid_monthly-climatology_v5&quot;&gt;AQUARIUS_L3_SPICINESS_SMID_MONTHLY-CLIMATOLOGY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface spiciness standard mapped image data contains gridded 1 degree spatial resolution spice data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the monthly climatology, Descending sea surface spiciness product for version 5.0 of the Aquarius data set. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onbard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_spiciness_smid_monthly_v5&quot;&gt;AQUARIUS_L3_SPICINESS_SMID_MONTHLY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface spiciness standard mapped image data contains gridded 1 degree spatial resolution spice data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Monthly, Descending sea surface spiciness product for version 5.0 of the Aquarius data set. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_spiciness_smid_seasonal-climatology_v5&quot;&gt;AQUARIUS_L3_SPICINESS_SMID_SEASONAL-CLIMATOLOGY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface spiciness standard mapped image data contains gridded 1 degree spatial resolution spice data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the seasonal climatology, Descending sea surface spiciness product for version 5.0 of the Aquarius data set. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_spiciness_smid_3month_v5&quot;&gt;AQUARIUS_L3_SPICINESS_SMID_3MONTH_V5&lt;/h4&gt;
Aquarius Level 3 sea surface spiciness standard mapped image data contains gridded 1 degree spatial resolution spice data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Seasonal, Descending sea surface spiciness product for version 5.0 of the Aquarius data set. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_spiciness_smi_cumulative_v5&quot;&gt;AQUARIUS_L3_SPICINESS_SMI_CUMULATIVE_V5&lt;/h4&gt;
Aquarius Level 3 sea surface spiciness standard mapped image data contains gridded 1 degree spatial resolution spice data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the mission series mean or cumulative sea surface spiciness product for version 5.0 of the Aquarius data set. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_spiciness_smi_monthly-climatology_v5&quot;&gt;AQUARIUS_L3_SPICINESS_SMI_MONTHLY-CLIMATOLOGY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface spiciness standard mapped image data contains gridded 1 degree spatial resolution spice data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the monthly climatology sea surface spiciness product for version 5.0 of the Aquarius data set. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_spiciness_smi_monthly_v5&quot;&gt;AQUARIUS_L3_SPICINESS_SMI_MONTHLY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface spiciness standard mapped image data contains gridded 1 degree spatial resolution spice data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Monthly sea surface spiciness product for version 5.0 of the Aquarius dataset. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_spiciness_smi_seasonal-climatology_v5&quot;&gt;AQUARIUS_L3_SPICINESS_SMI_SEASONAL-CLIMATOLOGY_V5&lt;/h4&gt;
Aquarius Level 3 sea surface spiciness standard mapped image data contains gridded 1 degree spatial resolution spice data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the seasonal climatology sea surface spiciness product for version 5.0 of the Aquarius data set. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_spiciness_smi_3month_v5&quot;&gt;AQUARIUS_L3_SPICINESS_SMI_3MONTH_V5&lt;/h4&gt;
Aquarius Level 3 sea surface spiciness standard mapped image data contains gridded 1 degree spatial resolution spice data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Seasonal sea surface spiciness product for version 5.0 of the Aquarius data set. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_wind_speed_smi_28day-runningmean_v5&quot;&gt;AQUARIUS_L3_WIND_SPEED_SMI_28DAY-RUNNINGMEAN_V5&lt;/h4&gt;
Aquarius Level 3 ocean surface wind speed standard mapped image data contains gridded 1 degree spatial resolution wind speed data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 28-Day running mean, wind speed product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_wind_speed_smi_7day_v5&quot;&gt;AQUARIUS_L3_WIND_SPEED_SMI_7DAY_V5&lt;/h4&gt;
Aquarius Level 3 ocean surface wind speed standard mapped image data contains gridded 1 degree spatial resolution wind speed data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 7-Day wind speed product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_wind_speed_smi_7day-runningmean_v5&quot;&gt;AQUARIUS_L3_WIND_SPEED_SMI_7DAY-RUNNINGMEAN_V5&lt;/h4&gt;
Aquarius Level 3 ocean surface wind speed standard mapped image data contains gridded 1 degree spatial resolution wind speed data averaged over daily, 7 day, monthly, and seasonaltime scales. This particular data set is the 7-Day running mean wind speed product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_wind_speed_smi_annual_v5&quot;&gt;AQUARIUS_L3_WIND_SPEED_SMI_ANNUAL_V5&lt;/h4&gt;
Aquarius Level 3 ocean surface wind speed standard mapped image data contains gridded 1 degree spatial resolution wind speed data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Annual wind speed product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_wind_speed_smia_28day-runningmean_v5&quot;&gt;AQUARIUS_L3_WIND_SPEED_SMIA_28DAY-RUNNINGMEAN_V5&lt;/h4&gt;
Aquarius Level 3 ocean surface wind speed standard mapped image data contains gridded 1 degree spatial resolution wind speed data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 28-Day running mean, Ascending wind speed product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_wind_speed_smia_7day_v5&quot;&gt;AQUARIUS_L3_WIND_SPEED_SMIA_7DAY_V5&lt;/h4&gt;
Aquarius Level 3 ocean surface wind speed standard mapped image data contains gridded 1 degree spatial resolution wind speed data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 7-Day, Ascending wind speed product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_wind_speed_smia_annual_v5&quot;&gt;AQUARIUS_L3_WIND_SPEED_SMIA_ANNUAL_V5&lt;/h4&gt;
Aquarius Level 3 ocean surface wind speed standard mapped image data contains gridded 1 degree spatial resolution wind speed data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Annual, Ascending wind speed product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_wind_speed_smia_daily_v5&quot;&gt;AQUARIUS_L3_WIND_SPEED_SMIA_DAILY_V5&lt;/h4&gt;
Aquarius Level 3 ocean surface wind speed standard mapped image data contains gridded 1 degree spatial resolution wind speed data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Daily, Ascending wind speed product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_wind_speed_smia_cumulative_v5&quot;&gt;AQUARIUS_L3_WIND_SPEED_SMIA_CUMULATIVE_V5&lt;/h4&gt;
Aquarius Level 3 ocean surface wind speed standard mapped image data contains gridded 1 degree spatial resolution wind speed data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the mission series mean or cumulative, Ascending wind speed product for version 5.0 of the Aquarius data set. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_wind_speed_smia_monthly-climatology_v5&quot;&gt;AQUARIUS_L3_WIND_SPEED_SMIA_MONTHLY-CLIMATOLOGY_V5&lt;/h4&gt;
Aquarius Level 3 ocean surface wind speed standard mapped image data contains gridded 1 degree spatial resolution wind speed data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the monthly climatology, Ascending wind speed product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_wind_speed_smia_monthly_v5&quot;&gt;AQUARIUS_L3_WIND_SPEED_SMIA_MONTHLY_V5&lt;/h4&gt;
Aquarius Level 3 ocean surface wind speed standard mapped image data contains gridded 1 degree spatial resolution wind speed data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Monthly, Ascending wind speed product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_wind_speed_smia_seasonal-climatology_v5&quot;&gt;AQUARIUS_L3_WIND_SPEED_SMIA_SEASONAL-CLIMATOLOGY_V5&lt;/h4&gt;
Aquarius Level 3 ocean surface wind speed standard mapped image data contains gridded 1 degree spatial resolution wind speed data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the seasonal climatology, Ascending wind speed product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_wind_speed_smia_3month_v5&quot;&gt;AQUARIUS_L3_WIND_SPEED_SMIA_3MONTH_V5&lt;/h4&gt;
Aquarius Level 3 ocean surface wind speed standard mapped image data contains gridded 1 degree spatial resolution wind speed data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Seasonal, Ascending wind speed product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Ascending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_wind_speed_smi_daily_v5&quot;&gt;AQUARIUS_L3_WIND_SPEED_SMI_DAILY_V5&lt;/h4&gt;
Aquarius Level 3 ocean surface wind speed standard mapped image data contains gridded 1 degree spatial resolution wind speed data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Daily wind speed product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_wind_speed_smid_28day-runningmean_v5&quot;&gt;AQUARIUS_L3_WIND_SPEED_SMID_28DAY-RUNNINGMEAN_V5&lt;/h4&gt;
Aquarius Level 3 ocean surface wind speed standard mapped image data contains gridded 1 degree spatial resolution wind speed data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 28-Day running mean, Descending wind speed product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_wind_speed_smid_7day_v5&quot;&gt;AQUARIUS_L3_WIND_SPEED_SMID_7DAY_V5&lt;/h4&gt;
Aquarius Level 3 ocean surface wind speed standard mapped image data contains gridded 1 degree spatial resolution wind speed data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the 7-Day, Descending wind speed product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_wind_speed_smid_annual_v5&quot;&gt;AQUARIUS_L3_WIND_SPEED_SMID_ANNUAL_V5&lt;/h4&gt;
Aquarius Level 3 ocean surface wind speed standard mapped image data contains gridded 1 degree spatial resolution wind speed data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Annual, Descending wind speed product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_wind_speed_smid_daily_v5&quot;&gt;AQUARIUS_L3_WIND_SPEED_SMID_DAILY_V5&lt;/h4&gt;
Aquarius Level 3 ocean surface wind speed standard mapped image data contains gridded 1 degree spatial resolution wind speed data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Daily, Descending wind speed product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_wind_speed_smid_cumulative_v5&quot;&gt;AQUARIUS_L3_WIND_SPEED_SMID_CUMULATIVE_V5&lt;/h4&gt;
Aquarius Level 3 ocean surface wind speed standard mapped image data contains gridded 1 degree spatial resolution wind speed data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the mission series mean or cumulative, Descending wind speed product for version 5.0 of the Aquarius data set. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_wind_speed_smid_monthly-climatology_v5&quot;&gt;AQUARIUS_L3_WIND_SPEED_SMID_MONTHLY-CLIMATOLOGY_V5&lt;/h4&gt;
Aquarius Level 3 ocean surface wind speed standard mapped image data contains gridded 1 degree spatial resolution wind speed data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the monthly climatology, Descending wind speed product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_wind_speed_smid_monthly_v5&quot;&gt;AQUARIUS_L3_WIND_SPEED_SMID_MONTHLY_V5&lt;/h4&gt;
Aquarius Level 3 ocean surface wind speed standard mapped image data contains gridded 1 degree spatial resolution wind speed data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Monthly, Descending wind speed product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_wind_speed_smid_seasonal-climatology_v5&quot;&gt;AQUARIUS_L3_WIND_SPEED_SMID_SEASONAL-CLIMATOLOGY_V5&lt;/h4&gt;
Aquarius Level 3 ocean surface wind speed standard mapped image data contains gridded 1 degree spatial resolution wind speed data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the seasonal climatology, Descending wind speed product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_wind_speed_smid_3month_v5&quot;&gt;AQUARIUS_L3_WIND_SPEED_SMID_3MONTH_V5&lt;/h4&gt;
Aquarius Level 3 ocean surface wind speed standard mapped image data contains gridded 1 degree spatial resolution wind speed data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Seasonal, Descending wind speed product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. Only retrieved values for Descending passes have been used to create this product. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_wind_speed_smi_cumulative_v5&quot;&gt;AQUARIUS_L3_WIND_SPEED_SMI_CUMULATIVE_V5&lt;/h4&gt;
Aquarius Level 3 ocean surface wind speed standard mapped image data contains gridded 1 degree spatial resolution wind speed data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the mission series mean or cumulative wind speed product for version 5.0 of the Aquarius data set. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_wind_speed_smi_monthly-climatology_v5&quot;&gt;AQUARIUS_L3_WIND_SPEED_SMI_MONTHLY-CLIMATOLOGY_V5&lt;/h4&gt;
Aquarius Level 3 ocean surface wind speed standard mapped image data contains gridded 1 degree spatial resolution wind speed data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the monthly climatology wind speed product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_wind_speed_smi_monthly_v5&quot;&gt;AQUARIUS_L3_WIND_SPEED_SMI_MONTHLY_V5&lt;/h4&gt;
Aquarius Level 3 ocean surface wind speed standard mapped image data contains gridded 1 degree spatial resolution wind speed data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Monthly wind speed product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_wind_speed_smi_seasonal-climatology_v5&quot;&gt;AQUARIUS_L3_WIND_SPEED_SMI_SEASONAL-CLIMATOLOGY_V5&lt;/h4&gt;
Aquarius Level 3 ocean surface wind speed standard mapped image data contains gridded 1 degree spatial resolution wind speed data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the seasonal climatology wind speed product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l3_wind_speed_smi_3month_v5&quot;&gt;AQUARIUS_L3_WIND_SPEED_SMI_3MONTH_V5&lt;/h4&gt;
Aquarius Level 3 ocean surface wind speed standard mapped image data contains gridded 1 degree spatial resolution wind speed data averaged over daily, 7 day, monthly, and seasonal time scales. This particular data set is the Seasonal wind speed product for version 5.0 of the Aquarius data set, which is the official end of mission public data release from the AQUARIUS/SAC-D mission. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_ancillary_rfi_v1&quot;&gt;AQUARIUS_ANCILLARY_RFI_V1&lt;/h4&gt;
Aquarius ancillary Radio Frequency Interference (RFI) product used in ADPS mission processing contains monthly-averaged Radio Frequency Interference (RFI) data for ascending/descending passes as detected by the Aquarius radiometers and scatterometer. The data is available for ascending (northward) and descending (southward) passes of the satellite only and ascending/descending passes combined. The values stored in this product are the percentage of radiometer and scatterometer measurements identified as corrupted by interference by the RFI detection algorithms [1,2] within each data point, averaged over one month. An additional RFI flag [3] is used to identify locations where the measured brightness temperature over land exceeds the expected limits of surface emissivity. This flag is not used to remove samples from further processing, but, in generating the radiometer RFI data, 100% RFI is assigned to points where this flag is raised. This product can be used to reproduce the RFI maps available on the Aquarius website at University of Maine (&lt;a href&#x3D;&quot;https://aquarius.umaine.edu/cgi/gal_radiometer.htm&quot;&gt;https://aquarius.umaine.edu/cgi/gal_radiometer.htm&lt;/a&gt; for the radiometer, and &lt;a href&#x3D;&quot;https://aquarius.umaine.edu/cgi/gal_scatterometer.htm&quot;&gt;https://aquarius.umaine.edu/cgi/gal_scatterometer.htm&lt;/a&gt; for the scatterometer), by plotting the variables Rad_RFI_percent_AscDes_AllBeams and Scat_RFI_percent_AscDes_AllBeams on the latitude/longitude grid. Additionally, the user can generate maps by using only a particular beam or only ascending passes, for example. All combinations of beams and ascending/descending passes are possible. This product contains information about RFI, but it is also relevant for the retrieved Sea Surface Salinity (SSS). Over the ocean, the RFI percentage in this product corresponds to the amount of raw measurements discarded due to RFI contamination before SSS retrieval. Therefore, maps of the RFI percentage can give the user an indication of where RFI is more likely to have affected the quality of SSS retrievals, for a particular month, or for a series of months.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aquarius_l4_oisss_iprc_7day_v5&quot;&gt;AQUARIUS_L4_OISSS_IPRC_7DAY_V5&lt;/h4&gt;
The IPRC/SOEST Aquarius OI-SSS v5 product is a level 4, near-global, 0.5 degree spatial resolution, 7-day, optimally interpolated salinity dataset based on version 5.0 of the AQUARIUS/SAC-D level 2 mission data. This is a PI led dataset produced at the International Pacific Research Center (IPRC) at the University of Hawaii (Manoa) School of Ocean and Earth Science and Technology. The optimal interpolation (OI) mapping procedure used to create this product corrects for systematic spatial biases in Aquarius SSS data with respect to near-surface in situ salinity observations and takes into account available statistical information about the signal and noise, specific to the Aquarius instrument. Bias fields are constructed by differencing in situ from Aquarius derived SSS fields obtained separately using ascending and descending satellite observations for each of the three Aquarius beams, and by removal of small-scale noise and low-pass filtering along-track using a two-dimensional Hanning window procedures prior to application of the OI algorithm. Additional enhancements for this new version of the product include: 1) The V5.0 (end-of mission) version of Aquarius Level-2 (swath) SSS data are used as input data for the OI SSS analysis. 2) The source of the first guess fields has changed from the APDRC Argo-derived SSS product to the average of four different in-situ based SSS products. 3) The bias correction algorithm has changed to adjust SSS retrievals for large-scale systematic biases on a repeat-track basis. 4) New, less restrictive thresholds are implemented to filter observations for land and ice contamination, thus improving coverage in the coastal areas and semi-enclosed seas. 5) Level-2 RFI masks for descending and ascending satellite passes are used to discard observations in specific geographic zones where excessive ascending-descending differences are observed due to contamination from undetected RFI. The Aquarius instrument is onboard the AQUARIUS/SAC-D satellite, a collaborative effort between NASA and the Argentinian Space Agency Comision Nacional de Actividades Espaciales (CONAE). The instrument consists of three radiometers in push broom alignment at incidence angles of 29, 38, and 46 degrees incidence angles relative to the shadow side of the orbit. Footprints for the beams are: 76 km (along-track) x 94 km (cross-track), 84 km x 120 km and 96km x 156 km, yielding a total cross-track swath of 370 km. The radiometers measure brightness temperature at 1.413 GHz in their respective horizontal and vertical polarizations (TH and TV). A scatterometer operating at 1.26 GHz measures ocean backscatter in each footprint that is used for surface roughness corrections in the estimation of salinity. The scatterometer has an approximate 390km swath. The Aquarius polar orbit is sun synchronous at 657 km with a 6 pm, ascending node, and has a 7-Day repeat cycle.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://archive.podaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA ARCSIX Project</title>
      <link>https://registry.opendata.aws/nasa-arcsix</link>
      <guid>https://registry.opendata.aws/nasa-arcsix</guid>
      <description>An inventory of NASA&amp;#39;s airborne and field campaigns for Earth Science
&lt;br&gt;&lt;h4 id&#x3D;&quot;arcsix_analysis_larc-g3_data&quot;&gt;ARCSIX_Analysis_LaRC-G3_Data&lt;/h4&gt;
ARCSIX_Analysis_LaRC-G3_Data is the analysis data collected onboard the LaRC G-III aircraft during the Arctic Radiation-Cloud-Aerosol-Surface Interaction EXperiment (ARCSIX) campaign. Data collection for this product is complete. The ARCSIX campaign is a NASA field investigation aimed at quantifying the contributions of surface properties, clouds, aerosol particles, and precipitation to the Arctic summer surface radiation budget and sea ice melt during the early melt season. Based out of Greenland, ARCSIX completed two deployments from May – June 2024 and July - August 2024 utilizing the NASA P-3B, LaRC G-III, and SPEC-Learjet aircraft. The P-3B was equipped with in situ and remote sensing payloads to acquire measurements of aerosols, cloud, and radiation properties. The high-flying LaRC G-III was equipped with remote sensing instrumentation, including the HALO, and HSRL, along with the AVAPS dropsonde system. The SPEC-Learjet acquired measurements of cloud microphysics. Data were also collected at the Thule High Arctic Atmospheric Observatory (THAAO) in Pituffik, Greenland. The primary objective of ARCSIX was to enhance long-term space-based monitoring and predictive capabilities of Arctic sea ice, cloud, and aerosols by validating and improving remote sensing algorithms and model parameterizations in the Arctic. ARCSIX science questions focused on examining the impact of the predominant summer Arctic cloud types on the radiative surface energy budget, what processes control the evolution and maintenance of the predominant cloud types in the summertime Arctic, and how do the two-way interactions between surface properties and atmospheric forcings affect sea ice evolution?
&lt;br&gt;&lt;h4 id&#x3D;&quot;arcsix_dropsondes_larc-g3_data&quot;&gt;ARCSIX_Dropsondes_LaRC-G3_Data&lt;/h4&gt;
ARCSIX_Dropsondes_LaRC-G3_Data is the dropsonde data collected onboard the LaRC G-III aircraft during the Arctic Radiation-Cloud-Aerosol-Surface Interaction EXperiment (ARCSIX) campaign. Data from the Airborne Vertical Atmosphere Profiling System (AVAPS) is featured in this collection. Data collection for this product is complete. The ARCSIX campaign is a NASA field investigation aimed at quantifying the contributions of surface properties, clouds, aerosol particles, and precipitation to the Arctic summer surface radiation budget and sea ice melt during the early melt season. Based out of Greenland, ARCSIX completed two deployments from May – June 2024 and July - August 2024 utilizing the NASA P-3B, LaRC G-III, and SPEC-Learjet aircraft. The P-3B was equipped with in situ and remote sensing payloads to acquire measurements of aerosols, cloud, and radiation properties. The high-flying LaRC G-III was equipped with remote sensing instrumentation, including the HALO, and HSRL, along with the AVAPS dropsonde system. The SPEC-Learjet acquired measurements of cloud microphysics. Data were also collected at the Thule High Arctic Atmospheric Observatory (THAAO) in Pituffik, Greenland. The primary objective of ARCSIX was to enhance long-term space-based monitoring and predictive capabilities of Arctic sea ice, cloud, and aerosols by validating and improving remote sensing algorithms and model parameterizations in the Arctic. ARCSIX science questions focused on examining the impact of the predominant summer Arctic cloud types on the radiative surface energy budget, what processes control the evolution and maintenance of the predominant cloud types in the summertime Arctic, and how do the two-way interactions between surface properties and atmospheric forcings affect sea ice evolution?
&lt;br&gt;&lt;h4 id&#x3D;&quot;arcsix_aircraftremotesensing_larc-g3_halo_data&quot;&gt;ARCSIX_AircraftRemoteSensing_LaRC-G3_HALO_Data&lt;/h4&gt;
ARCSIX_AircraftRemoteSensing_LaRC-G3_HALO_Data is the High Altitude Lidar Observatory (HALO) data collected onboard the LaRC G-III aircraft during the Arctic Radiation-Cloud-Aerosol-Surface Interaction EXperiment (ARCSIX) campaign. Data collection for this product is complete. The ARCSIX campaign is a NASA field investigation aimed at quantifying the contributions of surface properties, clouds, aerosol particles, and precipitation to the Arctic summer surface radiation budget and sea ice melt during the early melt season. Based out of Greenland, ARCSIX completed two deployments from May – June 2024 and July - August 2024 utilizing the NASA P-3B, LaRC G-III, and SPEC-Learjet aircraft. The P-3B was equipped with in situ and remote sensing payloads to acquire measurements of aerosols, cloud, and radiation properties. The high-flying LaRC G-III was equipped with remote sensing instrumentation, including the HALO, and HSRL, along with the AVAPS dropsonde system. The SPEC-Learjet acquired measurements of cloud microphysics. Data were also collected at the Thule High Arctic Atmospheric Observatory (THAAO) in Pituffik, Greenland. The primary objective of ARCSIX was to enhance long-term space-based monitoring and predictive capabilities of Arctic sea ice, cloud, and aerosols by validating and improving remote sensing algorithms and model parameterizations in the Arctic. ARCSIX science questions focused on examining the impact of the predominant summer Arctic cloud types on the radiative surface energy budget, what processes control the evolution and maintenance of the predominant cloud types in the summertime Arctic, and how do the two-way interactions between surface properties and atmospheric forcings affect sea ice evolution?
&lt;br&gt;&lt;h4 id&#x3D;&quot;arcsix_metnav_aircraftinsitu_larc-g3_data&quot;&gt;ARCSIX_MetNav_AircraftInSitu_LaRC-G3_Data&lt;/h4&gt;
ARCSIX_MetNav_AircraftInSitu_LaRC-G3_Data is the in-situ meteorology and navigation data collected onboard the LaRC G-III aircraft during the Arctic Radiation-Cloud-Aerosol-Surface Interaction EXperiment (ARCSIX) campaign. Data from the N520NA Meteorological and Navigation Facility Instrumentation is featured in this collection. Data collection for this product is complete. The ARCSIX campaign is a NASA field investigation aimed at quantifying the contributions of surface properties, clouds, aerosol particles, and precipitation to the Arctic summer surface radiation budget and sea ice melt during the early melt season. Based out of Greenland, ARCSIX completed two deployments from May – June 2024 and July - August 2024 utilizing the NASA P-3B, LaRC G-III, and SPEC-Learjet aircraft. The P-3B was equipped with in situ and remote sensing payloads to acquire measurements of aerosols, cloud, and radiation properties. The high-flying LaRC G-III was equipped with remote sensing instrumentation, including the HALO, and HSRL, along with the AVAPS dropsonde system. The SPEC-Learjet acquired measurements of cloud microphysics. Data were also collected at the Thule High Arctic Atmospheric Observatory (THAAO) in Pituffik, Greenland. The primary objective of ARCSIX was to enhance long-term space-based monitoring and predictive capabilities of Arctic sea ice, cloud, and aerosols by validating and improving remote sensing algorithms and model parameterizations in the Arctic. ARCSIX science questions focused on examining the impact of the predominant summer Arctic cloud types on the radiative surface energy budget, what processes control the evolution and maintenance of the predominant cloud types in the summertime Arctic, and how do the two-way interactions between surface properties and atmospheric forcings affect sea ice evolution?
&lt;br&gt;&lt;h4 id&#x3D;&quot;arcsix_cloud_aircraftinsitu_learjet_data&quot;&gt;ARCSIX_Cloud_AircraftInSitu_Learjet_Data&lt;/h4&gt;
ARCSIX_Cloud_AircraftInSitu_Learjet_Data is the in-situ cloud data collected onboard the Learjet aircraft during the Arctic Radiation-Cloud-Aerosol-Surface Interaction EXperiment (ARCSIX) campaign. Data from the 2D-Gray Particle Probe (2D-Gray), 2D-Stereo Particle Probe (2DS), Fast Cloud Droplet Probe (FCDP), High Volume Precipitation Spectrometer (HVPS), and the Nevzorov Water Vapor Probe are featured in this collection. Data collection for this product is complete. The ARCSIX campaign is a NASA field investigation aimed at quantifying the contributions of surface properties, clouds, aerosol particles, and precipitation to the Arctic summer surface radiation budget and sea ice melt during the early melt season. Based out of Greenland, ARCSIX completed two deployments from May – June 2024 and July - August 2024 utilizing the NASA P-3B, LaRC G-III, and SPEC-Learjet aircraft. The P-3B was equipped with in situ and remote sensing payloads to acquire measurements of aerosols, cloud, and radiation properties. The high-flying LaRC G-III was equipped with remote sensing instrumentation, including the HALO, and HSRL, along with the AVAPS dropsonde system. The SPEC-Learjet acquired measurements of cloud microphysics. Data were also collected at the Thule High Arctic Atmospheric Observatory (THAAO) in Pituffik, Greenland. The primary objective of ARCSIX was to enhance long-term space-based monitoring and predictive capabilities of Arctic sea ice, cloud, and aerosols by validating and improving remote sensing algorithms and model parameterizations in the Arctic. ARCSIX science questions focused on examining the impact of the predominant summer Arctic cloud types on the radiative surface energy budget, what processes control the evolution and maintenance of the predominant cloud types in the summertime Arctic, and how do the two-way interactions between surface properties and atmospheric forcings affect sea ice evolution?
&lt;br&gt;&lt;h4 id&#x3D;&quot;arcsix_metnav_aircraftinsitu_learjet_data&quot;&gt;ARCSIX_MetNav_AircraftInSitu_Learjet_Data&lt;/h4&gt;
ARCSIX_MetNav_AircraftInSitu_Learjet_Data is the in-situ meteorology and navigation data collected onboard the Learjet aircraft during the Arctic Radiation-Cloud-Aerosol-Surface Interaction EXperiment (ARCSIX) campaign. Data collection for this product is complete. The ARCSIX campaign is a NASA field investigation aimed at quantifying the contributions of surface properties, clouds, aerosol particles, and precipitation to the Arctic summer surface radiation budget and sea ice melt during the early melt season. Based out of Greenland, ARCSIX completed two deployments from May – June 2024 and July - August 2024 utilizing the NASA P-3B, LaRC G-III, and SPEC-Learjet aircraft. The P-3B was equipped with in situ and remote sensing payloads to acquire measurements of aerosols, cloud, and radiation properties. The high-flying LaRC G-III was equipped with remote sensing instrumentation, including the HALO, and HSRL, along with the AVAPS dropsonde system. The SPEC-Learjet acquired measurements of cloud microphysics. Data were also collected at the Thule High Arctic Atmospheric Observatory (THAAO) in Pituffik, Greenland. The primary objective of ARCSIX was to enhance long-term space-based monitoring and predictive capabilities of Arctic sea ice, cloud, and aerosols by validating and improving remote sensing algorithms and model parameterizations in the Arctic. ARCSIX science questions focused on examining the impact of the predominant summer Arctic cloud types on the radiative surface energy budget, what processes control the evolution and maintenance of the predominant cloud types in the summertime Arctic, and how do the two-way interactions between surface properties and atmospheric forcings affect sea ice evolution?
&lt;br&gt;&lt;h4 id&#x3D;&quot;arcsix_aircraftremotesensing_learjet_kpr_data&quot;&gt;ARCSIX_AircraftRemoteSensing_Learjet_KPR_Data&lt;/h4&gt;
ARCSIX_AircraftRemoteSensing_Learjet_KPR_Data is the Ka-Band Probe Radar-Radiometer (KPR) data collected onboard the Learjet aircraft during the Arctic Radiation-Cloud-Aerosol-Surface Interaction EXperiment (ARCSIX) campaign. Data collection for this product is complete. The ARCSIX campaign is a NASA field investigation aimed at quantifying the contributions of surface properties, clouds, aerosol particles, and precipitation to the Arctic summer surface radiation budget and sea ice melt during the early melt season. Based out of Greenland, ARCSIX completed two deployments from May – June 2024 and July - August 2024 utilizing the NASA P-3B, LaRC G-III, and SPEC-Learjet aircraft. The P-3B was equipped with in situ and remote sensing payloads to acquire measurements of aerosols, cloud, and radiation properties. The high-flying LaRC G-III was equipped with remote sensing instrumentation, including the HALO, and HSRL, along with the AVAPS dropsonde system. The SPEC-Learjet acquired measurements of cloud microphysics. Data were also collected at the Thule High Arctic Atmospheric Observatory (THAAO) in Pituffik, Greenland. The primary objective of ARCSIX was to enhance long-term space-based monitoring and predictive capabilities of Arctic sea ice, cloud, and aerosols by validating and improving remote sensing algorithms and model parameterizations in the Arctic. ARCSIX science questions focused on examining the impact of the predominant summer Arctic cloud types on the radiative surface energy budget, what processes control the evolution and maintenance of the predominant cloud types in the summertime Arctic, and how do the two-way interactions between surface properties and atmospheric forcings affect sea ice evolution?
&lt;br&gt;&lt;h4 id&#x3D;&quot;arcsix_aircraftremotesensing_p3b_marli_data&quot;&gt;ARCSIX_AircraftRemoteSensing_P3B_MARLi_Data&lt;/h4&gt;
ARCSIX_AircraftRemoteSensing_P3B_MARLi_Data contains data collected by the Multi-function Airborne Raman Lidar (MARLi) onboard the P-3B aircraft during the Arctic Radiation-Cloud-Aerosol-Surface Interaction EXperiment (ARCSIX) campaign. Data collection for this product is complete. The ARCSIX campaign is a NASA field investigation aimed at quantifying the contributions of surface properties, clouds, aerosol particles, and precipitation to the Arctic summer surface radiation budget and sea ice melt during the early melt season. Based out of Greenland, ARCSIX completed two deployments from May – June 2024 and July - August 2024 utilizing the NASA P-3B, LaRC G-III, and SPEC-Learjet aircraft. The P-3B was equipped with in situ and remote sensing payloads to acquire measurements of aerosols, cloud, and radiation properties. The high-flying LaRC G-III was equipped with remote sensing instrumentation, including the HALO, and HSRL, along with the AVAPS dropsonde system. The SPEC-Learjet acquired measurements of cloud microphysics. Data were also collected at the Thule High Arctic Atmospheric Observatory (THAAO) in Pituffik, Greenland. The primary objective of ARCSIX was to enhance long-term space-based monitoring and predictive capabilities of Arctic sea ice, cloud, and aerosols by validating and improving remote sensing algorithms and model parameterizations in the Arctic. ARCSIX science questions focused on examining the impact of the predominant summer Arctic cloud types on the radiative surface energy budget, what processes control the evolution and maintenance of the predominant cloud types in the summertime Arctic, and how do the two-way interactions between surface properties and atmospheric forcings affect sea ice evolution?
&lt;br&gt;&lt;h4 id&#x3D;&quot;arcsix_aircraftremotesensing_p3b_rsp_data&quot;&gt;ARCSIX_AircraftRemoteSensing_P3B_RSP_Data&lt;/h4&gt;
ARCSIX_AircraftRemoteSensing_P3B_RSP_Data contains data collected by the Research Scanning Polarimeter (RSP) onboard the P-3B aircraft during the Arctic Radiation-Cloud-Aerosol-Surface Interaction EXperiment (ARCSIX) campaign. Data collection for this product is complete. The ARCSIX campaign is a NASA field investigation aimed at quantifying the contributions of surface properties, clouds, aerosol particles, and precipitation to the Arctic summer surface radiation budget and sea ice melt during the early melt season. Based out of Greenland, ARCSIX completed two deployments from May – June 2024 and July - August 2024 utilizing the NASA P-3B, LaRC G-III, and SPEC-Learjet aircraft. The P-3B was equipped with in situ and remote sensing payloads to acquire measurements of aerosols, cloud, and radiation properties. The high-flying LaRC G-III was equipped with remote sensing instrumentation, including the HALO, and HSRL, along with the AVAPS dropsonde system. The SPEC-Learjet acquired measurements of cloud microphysics. Data were also collected at the Thule High Arctic Atmospheric Observatory (THAAO) in Pituffik, Greenland. The primary objective of ARCSIX was to enhance long-term space-based monitoring and predictive capabilities of Arctic sea ice, cloud, and aerosols by validating and improving remote sensing algorithms and model parameterizations in the Arctic. ARCSIX science questions focused on examining the impact of the predominant summer Arctic cloud types on the radiative surface energy budget, what processes control the evolution and maintenance of the predominant cloud types in the summertime Arctic, and how do the two-way interactions between surface properties and atmospheric forcings affect sea ice evolution?
&lt;br&gt;&lt;h4 id&#x3D;&quot;arcsix_analysis_p3b_data&quot;&gt;ARCSIX_Analysis_P3B_Data&lt;/h4&gt;
ARCSIX_Analysis_P3B_Data is the analysis data collected onboard the P-3B aircraft during the Arctic Radiation-Cloud-Aerosol-Surface Interaction EXperiment (ARCSIX) campaign. Data collection for this product is complete. The ARCSIX campaign is a NASA field investigation aimed at quantifying the contributions of surface properties, clouds, aerosol particles, and precipitation to the Arctic summer surface radiation budget and sea ice melt during the early melt season. Based out of Greenland, ARCSIX completed two deployments from May – June 2024 and July - August 2024 utilizing the NASA P-3B, LaRC G-III, and SPEC-Learjet aircraft. The P-3B was equipped with in situ and remote sensing payloads to acquire measurements of aerosols, cloud, and radiation properties. The high-flying LaRC G-III was equipped with remote sensing instrumentation, including the HALO, and HSRL, along with the AVAPS dropsonde system. The SPEC-Learjet acquired measurements of cloud microphysics. Data were also collected at the Thule High Arctic Atmospheric Observatory (THAAO) in Pituffik, Greenland. The primary objective of ARCSIX was to enhance long-term space-based monitoring and predictive capabilities of Arctic sea ice, cloud, and aerosols by validating and improving remote sensing algorithms and model parameterizations in the Arctic. ARCSIX science questions focused on examining the impact of the predominant summer Arctic cloud types on the radiative surface energy budget, what processes control the evolution and maintenance of the predominant cloud types in the summertime Arctic, and how do the two-way interactions between surface properties and atmospheric forcings affect sea ice evolution?
&lt;br&gt;&lt;h4 id&#x3D;&quot;arcsix_aerosol_aircraftinsitu_p3b_data&quot;&gt;ARCSIX_Aerosol_AircraftInSitu_P3B_Data&lt;/h4&gt;
ARCSIX_Aerosol_AircraftInSitu_P3B_Data is the in-situ aerosol data collected onboard the P-3B aircraft during the Arctic Radiation-Cloud-Aerosol-Surface Interaction EXperiment (ARCSIX) campaign. Data from the Nucleation Mode Aerosol Size Spectrometer, Portable Optical Particle Spetrometer (POPS), Ultra-High Sensitivity Aerosol Spectrometer (UHSAS), Time-of-Flight Aerosol Mass Spectrometer (ToF-AMS), Differential Aerosol Sizing and Hygroscopicity Spectrometer Probe (DASH-SP), Fast Integrated Mobility Spectrometer (FIMS), Aerodynamic Particle Sizer (APS), Cloud Condensation Nuclei Counter (CCN), TSI Condensation Particle Counter 3772 (TSI CPC-3772), TSI-3563 Nephelometer, and the Single Particle Soot Photometer (SP2) are featured in this collection. Data collection for this product is complete. The ARCSIX campaign is a NASA field investigation aimed at quantifying the contributions of surface properties, clouds, aerosol particles, and precipitation to the Arctic summer surface radiation budget and sea ice melt during the early melt season. Based out of Greenland, ARCSIX completed two deployments from May – June 2024 and July - August 2024 utilizing the NASA P-3B, LaRC G-III, and SPEC-Learjet aircraft. The P-3B was equipped with in situ and remote sensing payloads to acquire measurements of aerosols, cloud, and radiation properties. The high-flying LaRC G-III was equipped with remote sensing instrumentation, including the HALO, and HSRL, along with the AVAPS dropsonde system. The SPEC-Learjet acquired measurements of cloud microphysics. Data were also collected at the Thule High Arctic Atmospheric Observatory (THAAO) in Pituffik, Greenland. The primary objective of ARCSIX was to enhance long-term space-based monitoring and predictive capabilities of Arctic sea ice, cloud, and aerosols by validating and improving remote sensing algorithms and model parameterizations in the Arctic. ARCSIX science questions focused on examining the impact of the predominant summer Arctic cloud types on the radiative surface energy budget, what processes control the evolution and maintenance of the predominant cloud types in the summertime Arctic, and how do the two-way interactions between surface properties and atmospheric forcings affect sea ice evolution?
&lt;br&gt;&lt;h4 id&#x3D;&quot;arcsix_cloud_aircraftinsitu_p3b_data&quot;&gt;ARCSIX_Cloud_AircraftInSitu_P3B_Data&lt;/h4&gt;
ARCSIX_Cloud_AircraftInSitu_P3B_Data is the in-situ cloud data collected onboard the P-3B aircraft during the Arctic Radiation-Cloud-Aerosol-Surface Interaction EXperiment (ARCSIX) campaign. Data from the 2D-Stereo Particle Probe (2DS), Fast Cloud Droplet Probe (FCDP), High Volume Precipitation Spectrometer (HVPS), and the Continuous Flow Diffusion Chamber (CFDC) are featured in this collection. Data collection for this product is complete. The ARCSIX campaign is a NASA field investigation aimed at quantifying the contributions of surface properties, clouds, aerosol particles, and precipitation to the Arctic summer surface radiation budget and sea ice melt during the early melt season. Based out of Greenland, ARCSIX completed two deployments from May – June 2024 and July - August 2024 utilizing the NASA P-3B, LaRC G-III, and SPEC-Learjet aircraft. The P-3B was equipped with in situ and remote sensing payloads to acquire measurements of aerosols, cloud, and radiation properties. The high-flying LaRC G-III was equipped with remote sensing instrumentation, including the HALO, and HSRL, along with the AVAPS dropsonde system. The SPEC-Learjet acquired measurements of cloud microphysics. Data were also collected at the Thule High Arctic Atmospheric Observatory (THAAO) in Pituffik, Greenland. The primary objective of ARCSIX was to enhance long-term space-based monitoring and predictive capabilities of Arctic sea ice, cloud, and aerosols by validating and improving remote sensing algorithms and model parameterizations in the Arctic. ARCSIX science questions focused on examining the impact of the predominant summer Arctic cloud types on the radiative surface energy budget, what processes control the evolution and maintenance of the predominant cloud types in the summertime Arctic, and how do the two-way interactions between surface properties and atmospheric forcings affect sea ice evolution?
&lt;br&gt;&lt;h4 id&#x3D;&quot;arcsix_metnav_aircraftinsitu_p3b_data&quot;&gt;ARCSIX_MetNav_AircraftInSitu_P3B_Data&lt;/h4&gt;
ARCSIX_MetNav_AircraftInSitu_P3B_Data is the in-situ meteorology and navigation data collected onboard the P-3B aircraft during the Arctic Radiation-Cloud-Aerosol-Surface Interaction EXperiment (ARCSIX) campaign. Data from the Diode Laser Hygrometer (DLH) and the UNS-1Fw Flight Management System are featured in this collection. Data collection for this product is complete. The ARCSIX campaign is a NASA field investigation aimed at quantifying the contributions of surface properties, clouds, aerosol particles, and precipitation to the Arctic summer surface radiation budget and sea ice melt during the early melt season. Based out of Greenland, ARCSIX completed two deployments from May – June 2024 and July - August 2024 utilizing the NASA P-3B, LaRC G-III, and SPEC-Learjet aircraft. The P-3B was equipped with in situ and remote sensing payloads to acquire measurements of aerosols, cloud, and radiation properties. The high-flying LaRC G-III was equipped with remote sensing instrumentation, including the HALO, and HSRL, along with the AVAPS dropsonde system. The SPEC-Learjet acquired measurements of cloud microphysics. Data were also collected at the Thule High Arctic Atmospheric Observatory (THAAO) in Pituffik, Greenland. The primary objective of ARCSIX was to enhance long-term space-based monitoring and predictive capabilities of Arctic sea ice, cloud, and aerosols by validating and improving remote sensing algorithms and model parameterizations in the Arctic. ARCSIX science questions focused on examining the impact of the predominant summer Arctic cloud types on the radiative surface energy budget, what processes control the evolution and maintenance of the predominant cloud types in the summertime Arctic, and how do the two-way interactions between surface properties and atmospheric forcings affect sea ice evolution?
&lt;br&gt;&lt;h4 id&#x3D;&quot;arcsix_radiation_aircraftinsitu_p3b_data&quot;&gt;ARCSIX_Radiation_AircraftInSitu_P3B_Data&lt;/h4&gt;
ARCSIX_Radiation_AircraftInSitu_P3B_Data is the in-situ radiation data collected onboard the P-3B aircraft during the Arctic Radiation-Cloud-Aerosol-Surface Interaction EXperiment (ARCSIX) campaign. Data from the Broadband Radiometer (BBR), Hyper-Spectral Radiometer, Solar Spectral Flux Radiometers (SSFR), and the G-band Vapor Radiometer (GVR) are featured in this collection. Data collection for this product is complete. The ARCSIX campaign is a NASA field investigation aimed at quantifying the contributions of surface properties, clouds, aerosol particles, and precipitation to the Arctic summer surface radiation budget and sea ice melt during the early melt season. Based out of Greenland, ARCSIX completed two deployments from May – June 2024 and July - August 2024 utilizing the NASA P-3B, LaRC G-III, and SPEC-Learjet aircraft. The P-3B was equipped with in situ and remote sensing payloads to acquire measurements of aerosols, cloud, and radiation properties. The high-flying LaRC G-III was equipped with remote sensing instrumentation, including the HALO, and HSRL, along with the AVAPS dropsonde system. The SPEC-Learjet acquired measurements of cloud microphysics. Data were also collected at the Thule High Arctic Atmospheric Observatory (THAAO) in Pituffik, Greenland. The primary objective of ARCSIX was to enhance long-term space-based monitoring and predictive capabilities of Arctic sea ice, cloud, and aerosols by validating and improving remote sensing algorithms and model parameterizations in the Arctic. ARCSIX science questions focused on examining the impact of the predominant summer Arctic cloud types on the radiative surface energy budget, what processes control the evolution and maintenance of the predominant cloud types in the summertime Arctic, and how do the two-way interactions between surface properties and atmospheric forcings affect sea ice evolution?
&lt;br&gt;&lt;h4 id&#x3D;&quot;arcsix_tracegas_aircraftinsitu_p3b_data&quot;&gt;ARCSIX_TraceGas_AircraftInSitu_P3B_Data&lt;/h4&gt;
ARCSIX_TraceGas_AircraftInSitu_P3B_Data is the in-situ trace gas data collected onboard the P-3B aircraft during the Arctic Radiation-Cloud-Aerosol-Surface Interaction EXperiment (ARCSIX) campaign. Data from the PICARRO G2401-m Gas Concentration Analyzer and the 2B Technologies Model 205 Ozone Monitor are featured in this collection. Data collection for this product is complete. The ARCSIX campaign is a NASA field investigation aimed at quantifying the contributions of surface properties, clouds, aerosol particles, and precipitation to the Arctic summer surface radiation budget and sea ice melt during the early melt season. Based out of Greenland, ARCSIX completed two deployments from May – June 2024 and July - August 2024 utilizing the NASA P-3B, LaRC G-III, and SPEC-Learjet aircraft. The P-3B was equipped with in situ and remote sensing payloads to acquire measurements of aerosols, cloud, and radiation properties. The high-flying LaRC G-III was equipped with remote sensing instrumentation, including the HALO, and HSRL, along with the AVAPS dropsonde system. The SPEC-Learjet acquired measurements of cloud microphysics. Data were also collected at the Thule High Arctic Atmospheric Observatory (THAAO) in Pituffik, Greenland. The primary objective of ARCSIX was to enhance long-term space-based monitoring and predictive capabilities of Arctic sea ice, cloud, and aerosols by validating and improving remote sensing algorithms and model parameterizations in the Arctic. ARCSIX science questions focused on examining the impact of the predominant summer Arctic cloud types on the radiative surface energy budget, what processes control the evolution and maintenance of the predominant cloud types in the summertime Arctic, and how do the two-way interactions between surface properties and atmospheric forcings affect sea ice evolution?
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.asdc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA ASCENDS Airborne Project</title>
      <link>https://registry.opendata.aws/nasa-ascends-airborne</link>
      <guid>https://registry.opendata.aws/nasa-ascends-airborne</guid>
      <description>This dataset provides in situ airborne measurements of atmospheric carbon dioxide (CO2) over California and Nevada on February 10-11, 2016. Measurements were taken onboard a DC-8 aircraft during this Active Sensing of CO2 Emissions over Nights, Days and Seasons (ASCENDS) airborne deployment. CO2 was measured with NASA&amp;#39;s Atmospheric Vertical Observations of CO2 in the Earth&amp;#39;s Troposphere (AVOCET) instrument while over California and Nevada. The objective of this deployment was to assess the performance of the 2016 version of the CO2 Sounder LiDAR. The two flights were flown to compare results from an experimental LiDAR sensor with the AVOCET instrument. Aircraft navigation and flight meteorological data are also provided. The data are provided in ICARTT and comma-separated values (CSV) formats.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ascends_las_in_sept_2014_2116&quot;&gt;ASCENDS_LAS_IN_Sept_2014_2116&lt;/h4&gt;
This dataset provides in situ airborne measurements of atmospheric carbon dioxide (CO2) over Indianapolis, Indiana (IN) on September 3, 2014 during the morning commuter period with heavy traffic emissions. Stationary source emissions are also included. The observed CO2 plume downwind of the urban area, along with the prevailing wind speed and direction, enabled estimations of emission rates. CO2 was measured with an airborne CO2 Laser Absorption Spectrometer (JPL CO2LAS) developed at NASA&amp;#39;s Jet Propulsion Laboratory (JPL) to demonstrate the airborne Integrated Path Differential-Absorption (IPDA) lidar technique as a stepping stone to a capability for global measurements of CO2 concentrations from space. The CO2LAS measures the weighted, column averaged carbon dioxide between the aircraft and the ground using a continuous-wave heterodyne technique. The instrument operates at a 2.05 micron wavelength optimized for enhancing sensitivity to boundary layer carbon dioxide. Measurements were taken onboard a DC-8 aircraft during this Active Sensing of CO2 Emissions over Nights, Days and Seasons (ASCENDS) airborne deployment. The data are provided in HDF-5 format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.ornldaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA ASIA-AQ Project</title>
      <link>https://registry.opendata.aws/nasa-asia-aq</link>
      <guid>https://registry.opendata.aws/nasa-asia-aq</guid>
      <description>An inventory of NASA&amp;#39;s airborne and field campaigns for Earth Science
&lt;br&gt;&lt;h4 id&#x3D;&quot;asia-aq_analysis_dc8_data&quot;&gt;ASIA-AQ_Analysis_DC8_Data&lt;/h4&gt;
ASIA-AQ_Analysis_DC8_Data are analysis flag files derived from data products onboard the DC-8 aircraft during the Airborne and Satellite Investigation of Asian Air Quality (ASIA-AQ) campaign. Data flags identify plumes likely influenced by biomass burning and other combustion processes as well as identifies different air mass layers. Data collection for this product is complete. The ASIA-AQ campaign was an international cooperative field study designed to address local air quality challenges. Conducted from January-March 2024, ASIA-AQ deployed multiple aircraft to collect in situ and remote sensing measurements, along with numerous ground-based observations and modeling assessments. Data was collected over four countries including, the Philippines, Taiwan, South Korea and Thailand and flights were conducted in full partnership with local scientists and environmental agencies responsible for air quality monitoring and assessment. One of the primary goals of ASIA-AQ was to contribute improving integration of satellite observations with existing air quality ground monitoring and modeling efforts across Asia. Air quality observations from satellites are evolving with new capabilities from South Korea’s Geostationary Environment Monitoring Spectrometer (GEMS), which conducts hourly measurements to provide a new view of air quality conditions from space that complements and depends upon ground-based monitoring efforts of countries in its field of view. ASIA-AQ science goals focused on satellite validation and interpretation, emissions quantification and verification, model evaluation, aerosol chemistry, and ozone chemistry.
&lt;br&gt;&lt;h4 id&#x3D;&quot;asia-aq_aerosol_aircraftinsitu_dc8_data&quot;&gt;ASIA-AQ_Aerosol_AircraftInSitu_DC8_Data&lt;/h4&gt;
ASIA-AQ_Aerosol_AircraftInSitu_DC8_Data is the in-situ aerosol data collected onboard the DC-8 aircraft during the Airborne and Satellite Investigation of Asian Air Quality (ASIA-AQ) campaign. Data from the Transmission Electron Microscopy (TEM), Aerosol Mass Spectrometer (AMS), Single Particle Soot Photometer (DMT SP2), Ultra-High Sensitivity Aerosol Spectrometer (DMT UHSAS), Scanning Mobility Particle Sizer (SMPS), TSI-3563 Nephelometer, Cloud Condensation Nuclei (CCN) counter, and Condensation Particle Counter (CPC) are featured in this collection. Data collection for this product is complete. The ASIA-AQ campaign was an international cooperative field study designed to address local air quality challenges. Conducted from January-March 2024, ASIA-AQ deployed multiple aircraft to collect in situ and remote sensing measurements, along with numerous ground-based observations and modeling assessments. Data was collected over four countries including, the Philippines, Taiwan, South Korea and Thailand and flights were conducted in full partnership with local scientists and environmental agencies responsible for air quality monitoring and assessment. One of the primary goals of ASIA-AQ was to contribute improving integration of satellite observations with existing air quality ground monitoring and modeling efforts across Asia. Air quality observations from satellites are evolving with new capabilities from South Korea’s Geostationary Environment Monitoring Spectrometer (GEMS), which conducts hourly measurements to provide a new view of air quality conditions from space that complements and depends upon ground-based monitoring efforts of countries in its field of view. ASIA-AQ science goals focused on satellite validation and interpretation, emissions quantification and verification, model evaluation, aerosol chemistry, and ozone chemistry.
&lt;br&gt;&lt;h4 id&#x3D;&quot;asia-aq_cloud_aircraftinsitu_dc8_data&quot;&gt;ASIA-AQ_Cloud_AircraftInSitu_DC8_Data&lt;/h4&gt;
ASIA-AQ_Cloud_AircraftInSitu_DC8_Data is the in-situ cloud data collected onboard the DC-8 aircraft during the Airborne and Satellite Investigation of Asian Air Quality (ASIA-AQ) campaign. Data from the Cloud Droplet Probe (CDP), and Cloud Particle Spectrometer with Polarized Detection (CPSPD) are featured in this collection. Data collection for this product is complete. The ASIA-AQ campaign was an international cooperative field study designed to address local air quality challenges. Conducted from January-March 2024, ASIA-AQ deployed multiple aircraft to collect in situ and remote sensing measurements, along with numerous ground-based observations and modeling assessments. Data was collected over four countries including, the Philippines, Taiwan, South Korea and Thailand and flights were conducted in full partnership with local scientists and environmental agencies responsible for air quality monitoring and assessment. One of the primary goals of ASIA-AQ was to contribute improving integration of satellite observations with existing air quality ground monitoring and modeling efforts across Asia. Air quality observations from satellites are evolving with new capabilities from South Korea’s Geostationary Environment Monitoring Spectrometer (GEMS), which conducts hourly measurements to provide a new view of air quality conditions from space that complements and depends upon ground-based monitoring efforts of countries in its field of view. ASIA-AQ science goals focused on satellite validation and interpretation, emissions quantification and verification, model evaluation, aerosol chemistry, and ozone chemistry.
&lt;br&gt;&lt;h4 id&#x3D;&quot;asia-aq_metnav_aircraftinsitu_dc8_data&quot;&gt;ASIA-AQ_MetNav_AircraftInSitu_DC8_Data&lt;/h4&gt;
ASIA-AQ_MetNav_AircraftInSitu_DC8_Data is the in-situ meteorology and navigation data collected onboard the DC-8 aircraft during the Airborne and Satellite Investigation of Asian Air Quality (ASIA-AQ) campaign. Data from the Diode Laser Hygrometer (DLH) and the Meteorological Measurement System (MMS) are featured in this collection. Data collection for this product is complete. The ASIA-AQ campaign was an international cooperative field study designed to address local air quality challenges. Conducted from January-March 2024, ASIA-AQ deployed multiple aircraft to collect in situ and remote sensing measurements, along with numerous ground-based observations and modeling assessments. Data was collected over four countries including, the Philippines, Taiwan, South Korea and Thailand and flights were conducted in full partnership with local scientists and environmental agencies responsible for air quality monitoring and assessment. One of the primary goals of ASIA-AQ was to contribute improving integration of satellite observations with existing air quality ground monitoring and modeling efforts across Asia. Air quality observations from satellites are evolving with new capabilities from South Korea’s Geostationary Environment Monitoring Spectrometer (GEMS), which conducts hourly measurements to provide a new view of air quality conditions from space that complements and depends upon ground-based monitoring efforts of countries in its field of view. ASIA-AQ science goals focused on satellite validation and interpretation, emissions quantification and verification, model evaluation, aerosol chemistry, and ozone chemistry.
&lt;br&gt;&lt;h4 id&#x3D;&quot;asia-aq_tracegas_aircraftinsitu_dc8_data&quot;&gt;ASIA-AQ_TraceGas_AircraftInSitu_DC8_Data&lt;/h4&gt;
ASIA-AQ_TraceGas_AircraftInSitu_DC8_Data is the in-situ trace gas data collected onboard the DC-8 aircraft during the Airborne and Satellite Investigation of Asian Air Quality (ASIA-AQ) campaign. Data from the Trace Organic Gas Analyzer (TOGA), Whole Air Sampler (WAS), Quantum Cascade Tunable Infrared Differential Absorption Spectrometer (QC-TILDAS), Chemical Ionization Time-of-Flight Mass Spectrometer (CIT-ToF-CIMS), Differential Absorption CO, CH4, N2O Measurements (DACOM), LI-7000 Closed Path CO2/H2O Gas Analyzer (LI-7000), Los Gatos Research CO/CO2/H2O Analyzer (LGR), Airborne Cavity Enhanced Spectrometer (ACES), MIRO Multi-compound Gas Analyzer (MIRO MGA), Compact Airborne Nitrogen diOxide Experiment (CANOE), Rapid Ozone Experiment (ROZE), Proton Transfer Mass Spectrometer (PTR-MS), In Situ Airborne Formaldehyde (ISAF), and Open-Path Ammonia Laser Spectrometer (OPALS) are featured in this collection. Data collection for this product is complete. The ASIA-AQ campaign was an international cooperative field study designed to address local air quality challenges. Conducted from January-March 2024, ASIA-AQ deployed multiple aircraft to collect in situ and remote sensing measurements, along with numerous ground-based observations and modeling assessments. Data was collected over four countries including, the Philippines, Taiwan, South Korea and Thailand and flights were conducted in full partnership with local scientists and environmental agencies responsible for air quality monitoring and assessment. One of the primary goals of ASIA-AQ was to contribute improving integration of satellite observations with existing air quality ground monitoring and modeling efforts across Asia. Air quality observations from satellites are evolving with new capabilities from South Korea’s Geostationary Environment Monitoring Spectrometer (GEMS), which conducts hourly measurements to provide a new view of air quality conditions from space that complements and depends upon ground-based monitoring efforts of countries in its field of view. ASIA-AQ science goals focused on satellite validation and interpretation, emissions quantification and verification, model evaluation, aerosol chemistry, and ozone chemistry.
&lt;br&gt;&lt;h4 id&#x3D;&quot;asia-aq_jvalue_aircraftinsitu_dc8_data&quot;&gt;ASIA-AQ_jValue_AircraftInSitu_DC8_Data&lt;/h4&gt;
ASIA-AQ_jValue_AircraftInSitu_DC8_Data is the in-situ photolysis rates collected onboard the DC-8 aircraft during the Airborne and Satellite Investigation of Asian Air Quality (ASIA-AQ) campaign. Data from the CCD-based Actinic Flux Spectroradiometer (CAFS) is featured in this collection. Data collection for this product is complete. The ASIA-AQ campaign was an international cooperative field study designed to address local air quality challenges. Conducted from January-March 2024, ASIA-AQ deployed multiple aircraft to collect in situ and remote sensing measurements, along with numerous ground-based observations and modeling assessments. Data was collected over four countries including, the Philippines, Taiwan, South Korea and Thailand and flights were conducted in full partnership with local scientists and environmental agencies responsible for air quality monitoring and assessment. One of the primary goals of ASIA-AQ was to contribute improving integration of satellite observations with existing air quality ground monitoring and modeling efforts across Asia. Air quality observations from satellites are evolving with new capabilities from South Korea’s Geostationary Environment Monitoring Spectrometer (GEMS), which conducts hourly measurements to provide a new view of air quality conditions from space that complements and depends upon ground-based monitoring efforts of countries in its field of view. ASIA-AQ science goals focused on satellite validation and interpretation, emissions quantification and verification, model evaluation, aerosol chemistry, and ozone chemistry.
&lt;br&gt;&lt;h4 id&#x3D;&quot;asia-aq_aircraftremotesensing_larc-g3_gcas_data&quot;&gt;ASIA-AQ_AircraftRemoteSensing_LaRC-G3_GCAS_Data&lt;/h4&gt;
ASIA-AQ_AircraftRemoteSensing_LaRC-G3_GCAS_Data is the Geostationary Coastal and Air Pollution Event (GEO-CAPE) Airborne Simulator Data (GCAS) data collected onboard the NASA LaRC G-III aircraft during the Airborne and Satellite Investigation of Asian Air Quality (ASIA-AQ) campaign. Data collection for this product is complete. The ASIA-AQ campaign was an international cooperative field study designed to address local air quality challenges. Conducted from January-March 2024, ASIA-AQ deployed multiple aircraft to collect in situ and remote sensing measurements, along with numerous ground-based observations and modeling assessments. Data was collected over four countries including, the Philippines, Taiwan, South Korea and Thailand and flights were conducted in full partnership with local scientists and environmental agencies responsible for air quality monitoring and assessment. One of the primary goals of ASIA-AQ was to contribute improving integration of satellite observations with existing air quality ground monitoring and modeling efforts across Asia. Air quality observations from satellites are evolving with new capabilities from South Korea’s Geostationary Environment Monitoring Spectrometer (GEMS), which conducts hourly measurements to provide a new view of air quality conditions from space that complements and depends upon ground-based monitoring efforts of countries in its field of view. ASIA-AQ science goals focused on satellite validation and interpretation, emissions quantification and verification, model evaluation, aerosol chemistry, and ozone chemistry.
&lt;br&gt;&lt;h4 id&#x3D;&quot;asia-aq_aircraftremotesensing_larc-g3_hsrl2_data&quot;&gt;ASIA-AQ_AircraftRemoteSensing_LaRC-G3_HSRL2_Data&lt;/h4&gt;
ASIA-AQ_AircraftRemoteSensing_LaRC-G3_HSRL2_Data is the High Spectral Resolution Lidar (HSRL) data collected onboard the NASA LaRC G-III aircraft during the Airborne and Satellite Investigation of Asian Air Quality (ASIA-AQ) campaign. Data collection for this product is complete. The ASIA-AQ campaign was an international cooperative field study designed to address local air quality challenges. Conducted from January-March 2024, ASIA-AQ deployed multiple aircraft to collect in situ and remote sensing measurements, along with numerous ground-based observations and modeling assessments. Data was collected over four countries including, the Philippines, Taiwan, South Korea and Thailand and flights were conducted in full partnership with local scientists and environmental agencies responsible for air quality monitoring and assessment. One of the primary goals of ASIA-AQ was to contribute improving integration of satellite observations with existing air quality ground monitoring and modeling efforts across Asia. Air quality observations from satellites are evolving with new capabilities from South Korea’s Geostationary Environment Monitoring Spectrometer (GEMS), which conducts hourly measurements to provide a new view of air quality conditions from space that complements and depends upon ground-based monitoring efforts of countries in its field of view. ASIA-AQ science goals focused on satellite validation and interpretation, emissions quantification and verification, model evaluation, aerosol chemistry, and ozone chemistry.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.asdc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA ASTER GED Project</title>
      <link>https://registry.opendata.aws/nasa-aster-ged</link>
      <guid>https://registry.opendata.aws/nasa-aster-ged</guid>
      <description>The AG1kmB Version 3 dataset was decommissioned as of December 14, 2016. Users are encouraged to use the ASTER Global Emissivity Dataset 1-kilometer &lt;a href&#x3D;&quot;https://doi.org/10.5067/Community/ASTER_GED/AG1km.003&quot;&gt;AG1km&lt;/a&gt; dataset in HDF5. The Terra Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) Global Emissivity Dataset (GED) land surface temperature and emissivity (LST&amp;amp;E) data products are generated using the ASTER Temperature Emissivity Separation (TES) algorithm with a Water Vapor Scaling (WVS) atmospheric correction method using Moderate Resolution Imaging Spectroradiometer (MODIS) MOD07 atmospheric profiles and the MODerate spectral resolution TRANsmittance (MODTRAN) 5.2 radiative transfer model. This dataset is computed from all clear-sky pixels of ASTER scenes acquired from 2000 through 2008. The HDF5 version of the data are available for distribution, please see &lt;a href&#x3D;&quot;https://doi.org/10.5067/Community/ASTER_GED/AG1km.003&quot;&gt;AG1km&lt;/a&gt; for more information. The National Aeronautics and Space Administration’s (NASA) Jet Propulsion Laboratory (JPL), California Institute of Technology, developed the ASTER GED product. Knonw Issues * Known issues are provided in Section 4 of the User Guide.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ag100b&quot;&gt;AG100B&lt;/h4&gt;
The AG100B Version 3 dataset was decommissioned as of December 14, 2016. Users are encouraged to use the ASTER Global Emissivity Dataset 100-meter &lt;a href&#x3D;&quot;https://doi.org/10.5067/Community/ASTER_GED/AG100.003&quot;&gt;AG100 Version 3&lt;/a&gt; dataset in HDF5. The Terra Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) Global Emissivity Dataset (GED) land surface temperature and emissivity (LST&amp;amp;E) data products are generated using the ASTER Temperature Emissivity Separation (TES) algorithm with a Water Vapor Scaling (WVS) atmospheric correction method using Moderate Resolution Imaging Spectroradiometer (MODIS) MOD07 atmospheric profiles and the MODerate Spectral resolution TRANsmittance (MODTRAN) 5.2 radiative transfer model. This dataset is computed from all clear-sky pixels of ASTER scenes acquired from 2000 through 2008. The HDF5 version of the data are available for distribution, please see &lt;a href&#x3D;&quot;https://doi.org/10.5067/Community/ASTER_GED/AG100.003&quot;&gt;AG100&lt;/a&gt; for more information. The National Aeronautics and Space Administration’s (NASA) Jet Propulsion Laboratory (JPL), California Institute of Technology, developed the ASTER GED product. Known Issues: Known Issues are provided in Section 4 of the ASTER GED User Guide.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ag1km&quot;&gt;AG1km&lt;/h4&gt;
The Terra Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) Global Emissivity Dataset (GED) land surface temperature and emissivity (LST&amp;amp;E) data products are generated using the ASTER Temperature Emissivity Separation (TES) algorithm with a Water Vapor Scaling (WVS) atmospheric correction method using Moderate Resolution Imaging Spectroradiometer (MODIS) MOD07_L2 atmospheric profiles and the MODerate Spectral resolution TRANsmittance (MODTRAN 5.2) radiative transfer model. This dataset is computed from all clear-sky pixels of ASTER scenes acquired from 2000 through 2008. The National Aeronautics and Space Administration’s (NASA) Jet Propulsion Laboratory (JPL), California Institute of Technology, developed the ASTER GED product. Known Issues: Known issues are provided in Section 4 of the User Guide.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ag100&quot;&gt;AG100&lt;/h4&gt;
Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) Global Emissivity Dataset (GED) land surface temperature and emissivity (LST&amp;amp;E) data products are generated using the ASTER Temperature Emissivity Separation (TES) algorithm with a Water Vapor Scaling (WVS) atmospheric correction method using Moderate Resolution Imaging Spectroradiometer (MODIS) MOD07_L2 atmospheric profiles and the MODerate spectral resolution TRANsmittance (MODTRAN 5.2 radiative transfer model). This dataset is computed from all clear-sky pixels of ASTER scenes acquired from 2000 through 2008. AG100 data are available globally at spatial resolution of 100 meters. The National Aeronautics and Space Administration’s (NASA) Jet Propulsion Laboratory (JPL), California Institute of Technology, developed the ASTER GED product. Known Issues: Known issues are provided in Section 4, starting on page 8 of the User Guide.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ag5kmmoh&quot;&gt;AG5KMMOH&lt;/h4&gt;
The AG5KMMOH Version 4 dataset was decommissioned as of December 14, 2016. Users are encouraged to use &lt;a href&#x3D;&quot;https://doi.org/10.5067/Community/ASTER_GED/AG5KMMOH.041&quot;&gt;Version 4.1 ASTER Global Emissivity Dataset, Monthly, 0.05 degree, HDF5&lt;/a&gt;. The Terra Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) Global Emissivity Dataset (GED) is a collection of monthly files for each year of global emissivity. The ASTER GED data products are generated for 2000 through 2015 using the ASTER Temperature Emissivity Separation (TES) algorithm atmospheric correction method. This algorithm method uses Moderate Resolution Imaging Spectroradiometer (MODIS) Atmospheric Profiles product &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MOD07_L2.006&quot;&gt;MOD07&lt;/a&gt; and the MODTRAN 5.2 radiative transfer model along with the snow cover data from the standard monthly MODIS/Terra snow cover monthly global 0.05 degree product &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MOD10CM.006&quot;&gt;MOD10CM&lt;/a&gt;, and vegetation information from the MODIS monthly gridded Normalized Difference Vegetation Index (NDVI) product &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MOD13C2.006&quot;&gt;MOD13C2&lt;/a&gt;. The National Aeronautics and Space Administration’s (NASA) Jet Propulsion Laboratory (JPL), California Institute of Technology, developed the ASTER GED product.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ag5kmmoh-1&quot;&gt;AG5KMMOH&lt;/h4&gt;
The Terra Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) Global Emissivity Dataset (GED) is a collection of monthly files (see known issues for gaps) for each year of global emissivity. The ASTER GED data products are generated for 2000 through 2015 using the ASTER Temperature Emissivity Separation (TES) algorithm atmospheric correction method. This algorithm method uses Moderate Resolution Imaging Spectroradiometer (MODIS) Atmospheric Profiles product MOD07 and the MODerate spectral resolution TRANsmittance (MODTRAN) 5.2 radiative transfer model along with the snow cover data from the standard monthly MODIS/Terra snow cover monthly global 0.05 degree product &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MOD10CM.006&quot;&gt;MOD10CM&lt;/a&gt;, and vegetation information from the MODIS monthly gridded NDVI product &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MOD13C2.006&quot;&gt;MOD13C2&lt;/a&gt;. ASTER GED Monthly V041 data products are offered in Hierarchical Data Format 5 (HDF5). The National Aeronautics and Space Administration’s (NASA) Jet Propulsion Laboratory (JPL), California Institute of Technology, developed the ASTER GED product. Known Issues: Since ASTER GED Monthly V041 uses MOD10CM as an input, there will be some months that were unable to be created due to missing data. Please see the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?as&#x3D;61&quot;&gt;MODIS/Terra Data Outages Webpage&lt;/a&gt; for more information.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ag5kmmon&quot;&gt;AG5KMMON&lt;/h4&gt;
The AG5KMMOH Version 4 dataset was decommissioned as of December 14, 2016. Users are encouraged to use &lt;a href&#x3D;&quot;https://doi.org/10.5067/Community/ASTER_GED/AG5KMMOH.041&quot;&gt;Version 4.1 of ASTER Global Emissivity Dataset, Monthly, 0.05 degree, HDF5&lt;/a&gt;. The Terra Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) Global Emissivity Dataset (GED) is a collection of monthly files (see known issues for gaps) for each year of global emissivity. The ASTER GED data products are generated for 2000 through 2015 using the ASTER Temperature Emissivity Separation (TES) algorithm atmospheric correction method. This algorithm method uses Moderate Resolution Imaging Spectroradiometer (MODIS) Atmospheric Profiles product &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MOD07_L2.006&quot;&gt;MOD07&lt;/a&gt; and the MODerate spectral resolution TRANsmittance (MODTRAN) 5.2 radiative transfer model along with the snow cover data from the standard monthly MODIS/Terra snow cover monthly global 0.05 degree product &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MOD10CM.006&quot;&gt;MOD10CM&lt;/a&gt;, and vegetation information from the MODIS monthly gridded Normalized Difference Vegetation Index (NDVI) product &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MOD13C2.006&quot;&gt;MOD13C2&lt;/a&gt;. The National Aeronautics and Space Administration’s (NASA) Jet Propulsion Laboratory (JPL), California Institute of Technology, developed the ASTER GED product.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA ATDD Project</title>
      <link>https://registry.opendata.aws/nasa-atdd</link>
      <guid>https://registry.opendata.aws/nasa-atdd</guid>
      <description>This is a subset of AMSR-E rain rate product along CloudSat field of view track. The goal of the subset is to select and return AMSR-E data that are within -100 km across the CloudSat track. Thus resultant subset swath is 45 pixels cross-track. Apart from that, all efforts are made to preserve the original HDF-EOS formatting of the source full-sized data. The Advanced Microwave Scanning Radiometer - Earth Observing System (AMSR-E) instrument on the NASA EOS Aqua satellite provides global passive microwave measurements of terrestrial, oceanic, and atmospheric variables for the investigation of water and energy cycles. The original, full-sized, product is Level-2B swath product (AE_Rain), and it contains instantaneous measurements of rain rate and rain type (convective vs. stratiform), generated from Level-2A brightness temperatures (AE_L2A). The Goddard Space Flight Center (GSFC) Profiling algorithm determines rain rate and type over ocean areas, and a Modified GSFC Profiling algorithm over land. Data are stored in HDF-EOS (HDF4) format, and are available from 18 June 2002 until the AMSR-E instrument was turned off due to antenna problems in October 2011.
&lt;br&gt;&lt;h4 id&#x3D;&quot;mac04s0&quot;&gt;MAC04S0&lt;/h4&gt;
This is the narrow-swath MODIS/Aqua subset along CloudSat field of view track. The goal of the narrow-swath subset is to select and return MODIS data that are within +-5 km across the CloudSat track. I.e. the resultant MODIS subset swath is sought to be about 10 km cross-track.However, the original MYD04_L2 has 10-km pixels. Thus, MAC04S0 cross-track width is 2 pixels, the closest on either side of CloudSat track, and the resultant cross-track swath width is about 20 km.Along-track, all MODIS pixels from the original product are preserved. In the stardard product, the MODIS level-2 atmospheric aerosol product provides retrieved ambient aerosol optical properties (e.g., optical thickness and size distribution), mass concentration, look-up table derived reflected and transmitted fluxes, as well as quality assurance and other ancillary parameters, globally over ocean and near globally over land. (The shortname for this product is MAC04S0).
&lt;br&gt;&lt;h4 id&#x3D;&quot;mac04s1&quot;&gt;MAC04S1&lt;/h4&gt;
This is the wide-swath MODIS/Aqua subset along CloudSat field of view track. The goal of the wide-swath subset is to select and return MODIS data that are within +-100 km across the CloudSat track. I.e. the resultant MODIS subset swath is sought to be about 200 km cross-track. However, the original MYD04_L2 has 10-km pixels. Thus, MAC04S1 cross-track width is 21 pixels, and the resultant cross-track swath width is about 200 km. Along-track, all MODIS pixels from the original product are preserved. In the standard product, the MODIS level-2 atmospheric aerosol product provides retrieved ambient aerosol optical properties (e.g., optical thickness and size distribution), mass concentration, look-up table derived reflected and transmitted fluxes, as well as quality assurance and other ancillary parameters, globally over ocean and near globally over land. (The shortname for this product is MAC04S1).
&lt;br&gt;&lt;h4 id&#x3D;&quot;mam04s0&quot;&gt;MAM04S0&lt;/h4&gt;
This is the MODIS/Aqua subset along MLS field of view track. The goal of the subset is to select and return MODIS data that are within +-100 km across the MLS track. I.e. the resultant MODIS subset swath is sought to be about 200 km cross-track. However, the original MYD04_L2 has 10-km pixels. Thus, MAM04S0 cross-track width is 21 pixels, and the resultant cross-track swath width is about 200 km. Along-track, all MODIS pixels from the original product are preserved. In the stardard product, the MODIS level-2 atmospheric aerosol product provides retrieved ambient aerosol optical properties (e.g., optical thickness and size distribution), mass concentration, look-up table derived reflected and transmitted fluxes, as well as quality assurance and other ancillary parameters, globally over ocean and near globally over land. (The shortname for this product is MAM04S0).
&lt;br&gt;&lt;h4 id&#x3D;&quot;mam03s0&quot;&gt;MAM03S0&lt;/h4&gt;
This is the MODIS/Aqua subset along the Microwave Limb Sounder (MLS) field of view track. The goal of the subset is to select and return MODIS data that are within +-100 km across the MLS track. I.e. the resultant MODIS subset swath is about 200 km cross-track. Thus, MAM03S0 cross-track width is 201 pixels. Along-track, all MODIS pixels from the original product are preserved. In the standard product, geolocation fields are calculated for each 1 km MODIS Instantaneous Field of Views (IFOV) for all orbits daily. The locations and ancillary information corresponds to the intersection of the centers of each IFOV from 10 detectors in an ideal 1 km band on the Earth&amp;#39;s surface. A digital terrain model is used to model the Earth&amp;#39;s surface. The main inputs are the spacecraft attitude and orbit, the instrument telemetry and the digital elevation model. The geolocation fields include geodetic Latitude, Longitude, surface height above geoid, solar zenith and azimuth angles, satellite zenith and azimuth angles, and a land/sea mask for each 1 km sample. Additional information is included in the header to enable the calculation of the approximate location of the center of the detectors of any of the 36 MODIS bands. This product is used as input by a large number of subsequent MODIS products, particularly the products produced by the Land team. (The shortname for this product is MAM03S0).
&lt;br&gt;&lt;h4 id&#x3D;&quot;omcldo2_cpr&quot;&gt;OMCLDO2_CPR&lt;/h4&gt;
This the OMI/Aura Cloud Pressure and Fraction (O2-O2 Absorption) subset along CloudSat track, for the purposes of the A-Train mission. The original product uses the DOAS technique method. This level-2 global cloud product at the pixel resolution (13x24 km2 at nadir) is based on the spectral fitting of O2-O2 absorption band at 477 nm using DOAS technique. The goal of the subset is to select and return OMI data that are within +/-100 km across the CloudSat track. The resultant OMI subset swath is sought to be about 200 km cross-track. This product contains cloud pressure, cloud fraction, slant column O2-O2 and O3, ring coefficients, uncertainties in derived parameters, terrain and geolocation information, solar and satellite viewing angles, and quality flags. Even though collocated with CloudSat, this subset can serve many other A-Train applications. (The shortname for this Level-2 OMI cloud pressure and fraction (O2-O2 absorption) subset along CloudSat track product is OMCLDO2_CPR)
&lt;br&gt;&lt;h4 id&#x3D;&quot;omcldrr_cpr&quot;&gt;OMCLDRR_CPR&lt;/h4&gt;
This is the OMI/Aura Cloud Pressure and Fraction (Raman Scattering) subset along CloudSat tracks, for the purposes of the A-Train mission. The original data product uses the Rotational Raman Scattering method. This level-2 global cloud product provides effective cloud pressure and effective cloud fraction that is based on the least square fitting of the Ring spectrum (filling-in of Fraunhofer lines in the range 392 to 398 nm due to rotational Raman scattering). The goal of this subset is to select and return OMI data that are within +/-100 km across the CloudSat track. The resultant OMI subset swath is sought to be about 200 km cross-track. This product also contains many ancillary and derived parameters, terrain and geolocation information, solar and satellite viewing angles, and quality flags. Even though collocated with CloudSat, this subset can serve many other A-Train applications. (The shortname for this Level-2 OMI cloud pressure and fraction subset along CloudSat tracks product is OMCLDRR_CPR)
&lt;br&gt;&lt;h4 id&#x3D;&quot;omaeruv_cpr&quot;&gt;OMAERUV_CPR&lt;/h4&gt;
This is a CloudSat-collocated subset of the original OMI product OMAERUV, for the purposes of the A-Train mission. The goal of the subset is to select and return OMI data that are within +/-100 km across the CloudSat track. The resultant OMI subset swath is sought to be about 200 km cross-track of CloudSat. This product also contains many ancillary and derived parameters, terrain and geolocation information, solar and satellite viewing angles, and quality flags. Even though collocated with CloudSat, this subset can serve many other A-Train applications. (The shortname for this CloudSat-collocated OMI Level 2 near-UV aerosol subset is OMAERUV_CPR_003)
&lt;br&gt;&lt;h4 id&#x3D;&quot;omno2_cpr&quot;&gt;OMNO2_CPR&lt;/h4&gt;
This is a CloudSat-collocated subset of the original product OMNO2, for the purposes of the A-Train mission. The goal of the subset is to select and return OMI data that are within +/-100 km across the CloudSat track. The resultant OMI subset swath is sought to be about 200 km cross-track of CloudSat. This product also contains many ancillary and derived parameters, terrain and geolocation information, solar and satellite viewing angles, and quality flags. Even though collocated with CloudSat, this subset can serve many other A-Train applications. (The shortname for this CloudSat-collocated OMI Level 2 NO2 subset is OMNO2_CPR_V003)
&lt;br&gt;&lt;h4 id&#x3D;&quot;omto3_cpr&quot;&gt;OMTO3_CPR&lt;/h4&gt;
This is a CloudSat-collocated subset of the original product OMTO3, for the purposes of the A-Train mission. The goal of the subset is to select and return OMI data that are within +/-100 km across the CloudSat track. The resultant OMI subset swath is sought to be about 200 km cross-track of CloudSat. This product also contains many ancillary and derived parameters, terrain and geolocation information, solar and satellite viewing angles, and quality flags. Even though collocated with CloudSat, this subset can serve many other A-Train applications. (The shortname for this CloudSat-collocated OMI Level 2 Total Ozone Column subset is OMTO3_CPR_V003)
&lt;br&gt;&lt;h4 id&#x3D;&quot;omso2_cpr&quot;&gt;OMSO2_CPR&lt;/h4&gt;
This is a CloudSat-collocated subset of the original product OMSO2, for the purposes of the A-Train mission. The goal of the subset is to select and return OMI data that are within +/-100 km across the CloudSat track. The resultant OMI subset swath is sought to be about 200 km cross-track of CloudSat. Even though collocated with CloudSat, this subset can serve many other A-Train applications. (The shortname for this CloudSat-collocated subset of the original product OMSO2 Product is OMSO2_CPR_V003) This document describes the original OMI SO2 product (OMSO2) produced from global mode UV measurements of the Ozone Monitoring Instrument (OMI). OMI was launched on July 15, 2004 on the EOS Aura satellite, which is in a sun-synchronous ascending polar orbit with 1:45pm local equator crossing time. The data collection started on August 17, 2004 (orbit 482) and continues to this day with only minor data gaps. The minimum SO2 mass detectable by OMI is about two orders of magnitude smaller than the detection threshold of the legacy Total Ozone Mapping Spectrometer (TOMS) SO2 data (1978-2005) [Krueger et al 1995]. This is due to smaller OMI footprint and the use of wavelengths better optimized for separating O3 from SO2. The product file, called a data granule, covers the sunlit portion of the orbit with an approximately 2600 km wide swath containing 60 pixels per viewing line. During normal operations, 14 or 15 granules are produced daily, providing fully contiguous coverage of the globe. Currently, OMSO2 products are not produced when OMI goes into the &amp;quot;zoom mode&amp;quot; for one day every 452 orbits (~32 days). For each OMI pixel we provide 4 different estimates of the column density of SO2 in Dobson Units (1DU&#x3D;2.69x10^16 molecules/cm2) obtained by making different assumptions about the vertical distribution of the SO2. However, it is important to note that in most cases the precise vertical distribution of SO2 is unimportant. The users can use either the SO2 plume height, or the center of mass altitude (CMA) derived from SO2 vertical distribution, to interpolate between the 4 values: 1)Planetary Boundary Layer (PBL) SO2 column (ColumnAmountSO2_PBL), corresponding to CMA of 0.9 km. 2)Lower tropospheric SO2 column (ColumnAmountSO2_TRL), corresponding to CMA of 2.5 km. 3)Middle tropospheric SO2 column, (ColumnAmountSO2_TRM), usually produced by volcanic degassing, corresponding to CMA of 7.5 km, 4)Upper tropospheric and Stratospheric SO2 column (ColumnAmountSO2_STL), usually produced by explosive volcanic eruption, corresponding to CMA of 17 km. The accuracy and precision of the derived SO2 columns vary significantly with the SO2 CMA and column amount, observational geometry, and slant column ozone. OMI becomes more sensitive to SO2 above clouds and snow/ice, and less sensitive to SO2 below clouds. Preliminary error estimates are discussed below (see Data Quality Assessment). OMSO2 files are stored in EOS Hierarchical Data Format (HDF-EOS5). Each file contains data from the day lit portion of an orbit (53 minutes). There are approximately 14 orbits per day. The maximum file size for the OMSO2 data product is about 9 Mbytes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;parasolrb_cpr&quot;&gt;PARASOLRB_CPR&lt;/h4&gt;
This is the POLDER/Parasol Level-2 Radiation Budget Subset, collocated with the CloudSat track. The subset is processed at the A-Train Data Depot of the GES DISC, NASA. The algorithm first converts the original POLDER binary data, which is Level-2 but nevertheless in a sinusoidal grid, into HDF4 format, and thus stores the full-sized data in HDF4. Then, it calculates the CloudSat ground track coordinates, and proceeds to extract the closest POLDER grid cells. Along with the extraction, the algorithm re-orders the subset grid cells in a line-by-line fashion, so that the output subset is in array format and resembles a swath. This array has a cross-track dimension of 11 columns. That makes about 200-km-wide coverage. All original parameters are preserved in the subset. As it is collocated with CloudSat, the subset is automatically collocated with CALIPSO as well.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA ATLAS Project</title>
      <link>https://registry.opendata.aws/nasa-atlas</link>
      <guid>https://registry.opendata.aws/nasa-atlas</guid>
      <description>The Shuttle Solar Backscatter Ultraviolet (SSBUV) Level-2 Ozone data are available for eight space shuttle missions flown between 1989 and 1996. SSBUV, a successor to the SBUV flown on the Nimbus-7 satellite, is nearly identical to the SBUV/2 instruments flying on the NOAA satellites. Data are available in the ASCII AMES text format. Ozone profiles of the upper atmosphere and total column ozone values are available for the following time periods: Flight #1: 1989 October 19, 20, 21. Flight #2: 1990 October 7, 8, 9. Flight #3: 1991 August 3, 4, 5, 6. Flight #4: 1992 March 29, 31. Flight #5: 1993 April 9, 11, 13, 15, 16. Flight #6: 1994 March 14, 15, 17. Flight #7: 1994 November 5, 7, 10, 13. Flight #8: 1996 January 12, 16, 18. SSBUV measures spectral ultraviolet radiances backscattered by the earth&amp;#39;s atmosphere. For the ozone measurements the instrument steps over wavelengths between 252.2 and 339.99 nm while viewing the earth in the nadir position (50 km x 50 km footprint at nadir) at 19 pressure levels between 0.3 mb and 100 mb.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ssbuvirr&quot;&gt;SSBUVIRR&lt;/h4&gt;
The Shuttle Solar Backscatter Ultraviolet (SSBUV) level-2 irradiance data are available for eight space shuttle missions flown between 1989 and 1996. SSBUV, a successor to the SBUV flown on the Nimbus-7 satellite, is nearly identical to the SBUV/2 instruments flown on the NOAA polar orbiting satellites. Data are available in an ASCII text format. UV irradiance data are available for the following days from the eight missions: Flight #1: 1989 October 19, 20, 21 Flight #2: 1990 October 7, 8, 9 Flight #3: 1991 August 3, 4, 5, 6 Flight #4: 1992 March 29, 30 Flight #5: 1993 April 9, 11, 13, 15, 16 Flight #6: 1994 March 14, 15, 17 Flight #7: 1994 November 5, 7, 10, 13 Flight #8: 1996 January 12, 16, 18 The Shuttle SBUV (SSBUV) instrument measured solar spectral UV irradiance during the maximum and declining phase of solar cycle 22. The SSBUV data accurately represent the absolute solar UV irradiance between 200-405 nm, and also show the long-term variations during eight flights between October 1989 and January 1996. These data have been used to correct long-term sensitivity changes in the NOAA-11 SBUV/2 data, which provide a near-daily record of solar UV variations over the 170-400 nm region between December 1988 and October 1994. These data demonstrate the evolution of short-term solar UV activity during solar cycle 22.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA ATOMIC Project</title>
      <link>https://registry.opendata.aws/nasa-atomic</link>
      <guid>https://registry.opendata.aws/nasa-atomic</guid>
      <description>An inventory of NASA&amp;#39;s airborne and field campaigns for Earth Science
&lt;br&gt;&lt;h4 id&#x3D;&quot;saildrone_atomic&quot;&gt;SAILDRONE_ATOMIC&lt;/h4&gt;
Saildrone is a wind and solar powered unmanned surface vehicle (USV) capable of long distance deployments lasting up to 12 months and providing high quality, near real-time, multivariate surface ocean and atmospheric observations while transiting at typical speeds of 3-5 knots. The drone is autonomous in that it may be guided remotely from land while being completely wind driven. The saildrone ATOMIC (Atlantic Tradewind Ocean-Atmosphere Mesoscale Interaction Campaign) campaign involved the deployment of a fleet of saildrones, jointly funded by NASA and NOAA, in the Atlantic waters offshore of Barbados over a 45 day period from 17 January to 2 March 2020. The goal was to understand the Ocean-Atmosphere interaction particularly over the mesoscale ocean eddies in that region. The saildrones were equipped with a suite of instruments that included a CTD, IR pyrometer, fluorometer, dissolved oxygen sensor, anemometer, barometer, and Acoustic Doppler Current Profiler (ADCP). Additionally, four temperature data loggers were positioned vertically along hull to provide further information on thermal variability near the ocean surface. This Saildrone ATOMIC dataset is comprised of two data files for each of the three NASA-funded saildrones deployed, one for the surface observations and one for the ADCP measuements. The surface data files contain saildrone platform telemetry and near-surface observational data (air temperature, sea surface skin and bulk temperatures, salinity, oxygen and chlorophyll-a concentrations, barometric pressure, wind speed and direction) spanning the entire cruise at 1 minute temporal resolution. The ADCP files for each saildrone are at 5 minute resolution for the duration of the deployments. All data files are in netCDF format and CF/ACDD compliant consistent with the NOAA/NCEI specification.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://archive.podaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA ATom Project</title>
      <link>https://registry.opendata.aws/nasa-atom</link>
      <guid>https://registry.opendata.aws/nasa-atom</guid>
      <description>This dataset provides observations collected during eleven airborne campaigns from 2006&amp;ndash;2017 and associated input and output from nine widely used chemical transport models (CTMs). The airborne campaigns include ARCTAS-A, ARCTAS-B, ATom-1 and ATom-2, CalNex, DC3, INTEX-B, KORUS-AQ, MILAGRO, SEAC4RS, and WINTER, and they sampled mainly tropospheric air over the conterminous U.S. and the state of Alaska, Mexico, Canada, Greenland, and South Korea and remote areas over the Arctic, Pacific, Southern, and Atlantic Oceans. The CTMs are the AM4.1, CCSM4, GEOS-5, GEOS-Chem TOMAS, GEOS-Chem v10, GEOS-Chem v12, GISS-MATRIX, GISS-ModelE, and TM4-ECPL-F, and the output includes sulfate, nitrate, temperature, specific humidity, mixing ratio of ammonium, the volume mixing ratio of nitric acid, surface pressure, gas-phase ammonia, gas-phase nitric acid, pressure, total ammonium, etc. The observations were collected in-situ from a variety of instruments, including the Aerosol Microphysical Properties (AMP), HR Aerodyne Aerosol Mass Spectrometer (AMS), CIT Chemical Ionization Mass Spectrometer (CIMS), diode laser hygrometer (DLH), a mist chamber/ion chromatography system (MC/IC), Particle Analysis by Laser Mass Spectrometer (PALMS), Single Particle Soot Photometer (SP2), and UCI Whole Air Sampler (WAS). In-situ data also include latitude, longitude, and pressure. These observations were used to investigate how aerosol pH and ammonium balance change from polluted to remote regions, such as over oceans, and were compared to predictions from the CTMs.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_cafs_instrument_data_v2_1933&quot;&gt;ATom_CAFS_Instrument_Data_V2_1933&lt;/h4&gt;
This dataset contains actinic flux and photolysis frequencies for photodissociation reactions for a variety of chemical species during the four ATom campaigns. Spectrally resolved actinic flux was measured by the down- and up-welling Charged-coupled device Actinic Flux Spectroradiometers (CAFS) from approximately 280-650 nm. Photolysis frequencies were calculated from the actinic flux and published cross sections and quantum yield values for atmospherically relevant molecules. Solar radiation drives the chemistry of the atmosphere, including the evolution of ozone, greenhouse gases, biomass burning, and other anthropogenic and natural trace constituents.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_soap_instrument_data_1898&quot;&gt;ATom_SOAP_Instrument_Data_1898&lt;/h4&gt;
This dataset contains one-second aerosol extinction and absorption measurements from the Spectrometers for Optical Aerosol Properties (SOAP) instrument aboard the NASA DC-8 aircraft during the ATom-4 campaign that occurred in 2018. SOAP is a compact, low maintenance instrument that measures aerosol extinction and absorption at 532 nm. Aerosol extinction is measured by cavity ringdown spectroscopy and aerosol absorption by photoacoustic spectroscopy. Extinction is measured with sufficient precision and accuracy for the remote atmosphere. The absorption measurements are valid only in strongly absorbing cases, such as in dilute plumes from wildfire smoke. The absorption and extinction of visible light by aerosol particles is a major component of the earth&amp;#39;s radiation budget, strongly affecting climate. Highly absorbing particles directly heat the atmosphere, while particles that scatter light tend to cool the atmosphere. Extinction is the sum of absorption and scattering; in most cases scattering represents &amp;gt;90% of extinction, with absorption making up the remainder. These aerosol-radiation interactions also alter air temperature and the rates of photochemical reactions.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_hippo_orcas_1788&quot;&gt;ATom_HIPPO_ORCAS_1788&lt;/h4&gt;
This dataset provides calculated age of air (AoA) and the argon/nitrogen (Ar/N2) ratio (per meg) from stratospheric flask samples and simultaneous high-frequency measurements of nitrous oxide (N2O), carbon dioxide (CO2), ozone (O3), methane (CH4), and carbon monoxide (CO) compiled from three airborne projects. The trace gases were used to identify 235 flask samples with stratospheric influence collected by the Medusa Whole Air Sampler and to calculate AoA using a new N2O-AoA relationship developed using a Markov Chain Monte Carlo algorithm. The data span a wide range of latitudes poleward of 40 degrees in both the Northern and Southern Hemispheres and cover the period 2009-01-10 to 2018-05-21.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_nav_1613&quot;&gt;ATom_nav_1613&lt;/h4&gt;
This dataset provides flight track and aircraft navigation data from the NASA Atmospheric Tomography Mission (ATom). Flight track information is available for the four ATom campaigns: ATom-1, ATom-2, ATom-3, and ATom-4. Each ATom campaign consists of multiple individual flights and flight navigational information is recorded in 10-second intervals. Data available for each flight includes research flight number, date, and start and stop time of each 10-second interval. In addition, latitude, longitude, altitude, pressure and temperature is included at each 10-second interval. NASA&amp;#39;s ATom campaign deploys an extensive gas and aerosol payload on the NASA DC-8 aircraft for systematic, global-scale sampling of the atmosphere, profiling continuously from 0.2 to 12 km altitude. Flights occurred in each of 4 seasons from 2016 to 2018. During each campaign, flights originate from the Armstrong Flight Research Center in Palmdale, California, fly north to the western Arctic, south to the South Pacific, east to the Atlantic, north to Greenland, and return to California across central North America. ATom establishes a single, contiguous, global-scale dataset. One intended use of this flight track data is to facilitate to mapping model results from global models onto the precise ATom flight tracks for comparison.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_rad_measurements_armas_1906&quot;&gt;ATom_Rad_Measurements_ARMAS_1906&lt;/h4&gt;
This dataset contains Level 2 (L2) absorbed radiation dose rates in silicon from the Automated Radiation Measurements for Aerospace Safety (ARMAS) system along ATom flight paths for the ATom-1 campaign conducted in July and August 2016. Absorbed dose rates measure how much energy is deposited in matter by ionizing radiation per unit time. The radiation sources can be from galactic cosmic rays, solar energetic particles, or Van Allen radiation belt energetic particles. Radiation can have adverse effects on human tissue and aerospace electronics, as well as profound effects on chemical species in the atmosphere, making them important to consider in atmospheric modeling and analyses. In this context, the derived ambient equivalent dose rates are also provided and relate the absorbed dose in human tissue to the effective biological damage of the radiation through a radiation weighting factor. In addition, visualizations of absorbed radiation dose for ATom-1 flight paths are included. The visualizations show the absorbed dose rates in silicon in the upper panel and the 3D representation of the flight in the bottom panel.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_flighttrack_influences_1889&quot;&gt;ATom_FlightTrack_Influences_1889&lt;/h4&gt;
This dataset contains back trajectories, boundary layer influences, and convective influences of air parcels along NASA DC-8 aircraft&amp;#39;s flight tracks during the four ATom campaigns that occurred from 2016 to 2018. Back trajectories were interpolated using National Centers for Environmental Prediction (NCEP) Global Forecast System (GFS) and Modern-Era Retrospective analysis for Research and Applications, Version 2 (MERRA2) meteorology. Back trajectory analysis determines the origin of air masses by modeling the path of an air parcel backward in time. It can be used to better understand the sources of atmospheric compounds. Boundary layer Influences were determined based on 30 Day Back Trajectories. The atmospheric boundary layer is the lowest part of the troposphere that is directly influenced by earth&amp;#39;s surface. The boundary layer influences wind patterns and thus the dispersal of pollutants and other atmospheric compounds of interest. Convective influences were based on 10 Day Back Trajectories and NASA Langley cloud products. Convective influences model the effects of convection on the movement of water vapor through the atmosphere, which influences cloud behavior.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_carbon_aerosol_loadings_1618&quot;&gt;ATom_Carbon_Aerosol_Loadings_1618&lt;/h4&gt;
This dataset provides black carbon (BC) mass mixing ratios (in units of ng BC / kg air) measured during NASA&amp;#39;s Atmospheric Tomography (ATom)-1 flight campaign during July and August 2016. The BC-core masses of BC-containing aerosol particles were measured using a Single Particle Soot Photometer (SP2). Conversion to mass mixing ratio (MMR) is achieved by monitoring sample flow. Influences in air mass composition were determined using the Particle Analysis by Laser Mass Spectrometry (PALMS) instruments. Also included here are data from the Cloud, Aerosol and Precipitation Spectrometer (CAPS) instrument which are used to identify measurements taken while in clouds. Finally, the associated latitude, longitude, altitude, and the timestamp of each measurement are included. All data are at ten seconds resolution. ATom-1 flights originated from the Armstrong Flight Research Center in Palmdale, California, fly north to the western Arctic, south to the South Pacific, east to the Atlantic, north to Greenland, and return to California across central North America.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_cesm2_1878&quot;&gt;ATom_CESM2_1878&lt;/h4&gt;
This dataset contains CAM-chem (Community Atmosphere Model with Chemistry) model outputs along ATom flight tracks. CAM-chem is a component of the Community Earth System Model Version 2 (CESM2) and is used for simulations of global tropospheric and stratospheric atmospheric composition and for studies of chemistry-climate interactions. In general, CAM-chem uses the MOZART chemical mechanism, with various choices of complexity for tropospheric and stratospheric chemistry. For this dataset, CAM-chem used the MOZART-TS1 chemical mechanism, and the model was nudged to reanalysis meteorology from MERRA2.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_capsvienna_data_1981&quot;&gt;ATom_CAPSVienna_Data_1981&lt;/h4&gt;
This dataset contains cloud type and coarse aerosol contents measured by the University of Vienna&amp;#39;s second-generation Cloud Aerosol and Precipitation Spectrometer (CAPS) instrument mounted to the NASA DC-8 aircraft during the four ATom campaigns that occurred from 2016 to 2018. CAPS measures particle size distributions in a size range between nominally 0.5 micrometers and 960 micrometers. The sizes range between approximately 0.5 and 50 micrometers is covered by the optical particle counter component of CAPS-the Cloud and Aerosol Spectrometer with Depolarization Detection (CAS-DPOL). The sizes range from 15 to 930 micrometers is measured with the optical array probe called Cloud imaging Probe (CIP). Cloud types are determined using an algorithm developed to detect and classify clouds using measurements of CAPS. Relative humidity and temperature are considered by the algorithm. The cloud indicator provides a classification on a 1 Hz basis and separates data in cloud-free, aerosol-cloud transition regime (ACTR), liquid clouds, clouds in the mixed-phase temperature regime (MPTR), and cirrus clouds. The coarse aerosol product provides cloud and aerosol particle number concentrations at standard pressure (1013.25 hPa) and standard temperature (273.15 K) in selected size ranges. Particle sizes refer to ammonium sulfate optical equivalent diameter (m&#x3D;1.52 + 0.0i).
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_picarro_instrument_data_1732&quot;&gt;ATom_Picarro_Instrument_Data_1732&lt;/h4&gt;
This dataset contains atmospheric measurements of CO2, CH4, and CO mixing ratios made with a Picarro G2401 spectrometer during the four ATom campaigns. Picarro G2401 uses Wavelength-Scanned Cavity Ring Down Spectroscopy (WS-CRDS), a time-based measurement utilizing a near-infrared laser to measure a spectral signature of the molecule. For the ATom mission, the Picarro instrument was modified in the laboratory to operate across the full pressure altitude range of flight campaigns. The instrument was also modified to have a shorter measurement interval.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_mapping_oh_troposphere_1669&quot;&gt;ATom_Mapping_OH_Troposphere_1669&lt;/h4&gt;
This dataset provides profile-integrated column densities of formaldehyde (HCHO), hydroxyl (OH), and OH production rates, diel tropospheric mean OH concentrations, and uncertainties that were derived from direct observation data from selected profiles of NASA Atmospheric Tomography (ATom) mission 1 and 2 flights for the period July 29, 2016 to February 21, 2017. These calculated products were combined with coincident HCHO column retrievals from the Ozone Monitoring Instrument (OMI) to scale and extend the profile results to a global gridded (0.5 deg latitude x 0.625 deg longitude) product. In addition to OMI formaldehyde column data, model output products from the Global Modeling Initiative (GMI) including average tropopause height, scaling factor, column air mass, and column-average formaldehyde photolysis frequency are provided. The GMI model output products were used in calculations and are included for user convenience.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_aerosol_properties_v2_2111&quot;&gt;ATom_Aerosol_Properties_V2_2111&lt;/h4&gt;
This dataset contains comprehensive measurements of aerosol microphysical, chemical, and optical properties derived for both dry and ambient conditions from in situ measurements made during the four ATom campaigns. The dataset includes composition-resolved size distributions the integrated mass of sulfate, organics, nitrate, sea salt, dust, black carbon, and other compounds in coarse and fine fractions; extinction and absorption coefficients from each species at both dry and ambient conditions; asymmetry parameters; Angstrom exponents; and fitted lognormal functions to describe the size distribution. Optical parameters are calculated for 10 wavelengths from the near UV to the near IR, and size distributions range from 3 nm to 50 um in diameter. One file contains these data at 1-minute time intervals. Another file contains a subset of these data averaged into 1-km vertical bins for each vertical profile the aircraft made, as well as composition-resolved integrated aerosol optical depth derived from each profile. The concentration of cloud condensation nuclei is calculated for 5 supersaturations.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_fullmodel_datastream_1877&quot;&gt;ATom_FullModel_DataStream_1877&lt;/h4&gt;
This dataset provides Modeling Data Stream (MDS) and Reactivity Data Stream (RDS) products for each of the four ATom campaigns conducted from 2016 to 2018. MDS files contain the atmospheric constituents needed to model the RDS of the air parcels along ATom flight paths. The MDS is a continuous data stream (every 10 seconds) of the atmospheric content of these key chemical species derived from the in-situ measurements collected along ATom flight paths (as reported in the comprehensive related dataset ATom: Merged Atmospheric Chemistry, Trace Gases, and Aerosols). Values for chemical species measured by multiple instruments were selected from the instrument with better coverage and/or greater precision. Missing values were filled using interpolation for short gaps. For long gaps owing to instrument failure, values were estimated using multiple linear regressions from comparable parallel flights from other ATom campaigns. All species were flagged for instrument source and values were flagged for gap-filling status. In combination, MDS and RDS provide, in essence, a photochemical climatology for each air parcel along ATom flight paths containing the reactive species that control the loss of methane and the production and loss of ozone.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_forward_flight_videos_1938&quot;&gt;ATom_Forward_Flight_Videos_1938&lt;/h4&gt;
This dataset contains images taken from the front of the NASA DC-8 aircraft during the first three ATom campaigns from 2016-2017. Images were taken with an Axis P1357 High Definition camera with a Theia TH138A wide-angle lens. These images were then stitched together at a 10-second frequency into an MP4 (.mp4) video for each flight. The forward camera shows the visible atmosphere that DC-8 flew through, allowing the in situ measurements to be placed in the context of cloud fields, smoke and haze layers, and boundary layers.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_clouds_aerosols_2250&quot;&gt;ATom_Clouds_Aerosols_2250&lt;/h4&gt;
This dataset is the basis for the development of the Cloud Indicator, a novel algorithm that automatically detects and classifies measurement periods inside clouds. The included data were used in the analysis and development of figures for the related publication. The Cloud Indicator algorithm was developed based on particle size distribution measurements from a second-generation Cloud, Aerosol, and Precipitation Spectrometer (CAPS) combined with measurements of relative humidity and temperature from other sensors, to automatically detect flight sequences in clouds and classify the cloud type. Measurements were collected on 2016-08-20 as part of the Atmospheric Tomography Mission (ATom-1) Campaign and on 2017-04-20 as part of the Absorbing aerosol layers in a changing climate: aging, LIFEtime and dynamics (A-LIFE) project. As an additional criterion for the Cloud Indicator, a cloud-aerosol volume factor was established to ensure a precise and robust distinction between clouds and aerosol layers such as mineral dust or biomass burning to reduce misclassifications. Data are provided in netCDF (.nc) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_mineral_dust_cirrus_cloud_2006&quot;&gt;ATom_Mineral_Dust_Cirrus_Cloud_2006&lt;/h4&gt;
This dataset provides: (1) In situ dust aerosol concentration measurements over remote tropical Pacific and Atlantic Oceans by NOAA Particle Analysis by Laser Mass Spectrometry (PALMS) airborne single-particle mass spectrometer combined with Aerosol Microphysical Properties (AMP) aerosol size spectrometers. Measurements were made aboard the NASA DC8 aircraft during the four ATom campaigns that occurred from 2016 to 2018 (2) Model output of dust and meteorology from the CESM global transport model extracted at the time and location of the aircraft; (3) Model output of dust, other aerosol, and meteorology from the GEOS global transport model extracted at the time and location of the aircraft; (4) CESM model global output of dust and meteorology for dust emitted by specific source regions; (5) NCEP Global Forecast System forward trajectories of air parcels initiated at the time and location of the aircraft; and (6) The location and properties of cirrus clouds formed along the forward trajectories simulated using a parcel model. These data have been applied to better understand the role of mineral dust in cirrus cloud formation.
&lt;br&gt;&lt;h4 id&#x3D;&quot;flight_environment_parameters_1909&quot;&gt;Flight_Environment_Parameters_1909&lt;/h4&gt;
This dataset contains flight dynamics and environmental parameters (often referred to as housekeeping) specific to the DC-8 aircraft as collected from an assortment of instruments across all four ATom campaigns flown from 2016 through 2018. Measurements include aircraft position, altitude, speed, wind parameters, air temperature, and atmospheric and cabin pressure. These data can be used to understand the interior and exterior conditions and positioning of the DC-8 aircraft at 1-second resolution.
&lt;br&gt;&lt;h4 id&#x3D;&quot;interpolated_met_products_1876&quot;&gt;Interpolated_Met_Products_1876&lt;/h4&gt;
This dataset provides modeled meteorological conditions and tagged-CO tracer concentrations along ATom flight paths derived from the Goddard Earth Observing System Version 5 (GEOS-5) data assimilation products from the Global Modeling and Assimilation Office (GMAO) at NASA&amp;#39;s Goddard Space Flight Center. The GMAO &amp;quot;GEOS fp&amp;quot; forward processing system ingests satellite, ground-based, and airborne data, using a sophisticated model along with the data&amp;#39;s statistical properties to obtain global three-dimensional data gridded fields at regular time intervals. These data are from the GMAO model output that were fitted to the ATom flight tracks by interpolating the GMAO model output to the horizontal ATom flight tracks for each of the 4 ATom Deployments. The dataset also provides tagged-CO tracer concentrations, which represent the contribution of specific regional sources to the total simulated CO. The data products produced are consistent with both the original measurements and the physical laws governing the atmosphere. To provide some meteorological context for the ATom flights, the GEOS5 gridded data are interpolated in space and time to the flight tracks.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_photolysis_rates_1651&quot;&gt;ATom_Photolysis_Rates_1651&lt;/h4&gt;
This dataset provides the results from nine global chemistry-climate or chemistry-transport models that estimated gridded values of atmospheric photolytic rates (J values) for ozone (O3), designated J-O1D, and nitrogen dioxide (NO2), designated J-NO2, under cloudy and clear sky scenarios. Each model produced global 4-D fields (latitude by longitude by pressure for 24 hours) for one day in mid-August 2016 (nominally) of results from two simulations: first using their standard treatment of clouds (all sky or cloudy) and a second with clouds and aerosols removed (clear sky). Model resolution ranges from 0.5 to 2.5 degrees. Observed J-O1D and J-NO2 values from the first ATom deployment (29 July - 23 August 2016) were collected with the Charged-coupled device Actinic Flux Spectroradiometer (CAFS) instrument. The ATom CAFS measurements are 3-second averages along the flight path for selected remote areas over the tropical and northern Pacific Ocean. Both all-sky (cloudy) and synthesized clear-sky J values are provided. (3) Additional data are included for clouds and ozone column plus other cloudy and clear sky parameters for the same remote areas of the tropical and northern Pacific Ocean. These auxiliary data are provided for use with included MATLAB scripts to reproduce the plots and analyses performed in the related publication by Hall et al. (2018). Note that while the analyses in the related publication were limited to the Pacific basin, the global model data are archived with this dataset.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_globalmodelinitiative_ctm_1897&quot;&gt;ATom_GlobalModelInitiative_CTM_1897&lt;/h4&gt;
This dataset contains Global Modeling Initiative (GMI) Chemical Transport Model (CTM) outputs from the four Atom campaigns. GMI simulations of the ATom flight periods have a horizontal resolution of 1.0 x 1.25 degrees, with output every 15 minutes. The ICARTT files are generated by spatially and temporally interpolating the output to the ATom flight track. Vertical interpolation is linear in log-pressure. The netCDF files provide three-dimensional&amp;nbsp;(3D) GMI simulation output for the region surrounding the flight track every 15 minutes at the original model resolution. GMI is a 3-D CTM that includes full chemistry for both the troposphere and stratosphere. GMI simulates the concentrations of many of the species measured during ATom.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_dlh_instrument_data_v2_1937&quot;&gt;ATom_DLH_Instrument_Data_V2_1937&lt;/h4&gt;
This dataset provides the concentrations of water measured by the Diode Laser Hygrometer (DLH) flown on the NASA DC-8 during the ATom 1-4 campaigns from 2016 - 2018. The DLH measures the water vapor in the atmosphere by wavelength modulated differential absorption spectroscopy of an isolated rovibrational line. The measurements include water vapor mixing ratio in parts-per-million-by-volume (ppmv) and relative humidity in percent. Relative humidity, both with respect to liquid water and with respect to ice, are quantities derived from measurements of water vapor mixing ratio as well as ambient temperature and pressure.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_cit_instrument_data_v2_1927&quot;&gt;ATom_CIT_Instrument_Data_V2_1927&lt;/h4&gt;
This dataset provides the concentrations of gas-phase organic and inorganic analytes measured by the California Institute of Technology (CIT) Chemical Ionization Mass Spectrometer (CIMS), or CIT-CIMS, flown on the NASA DC-8 aircraft during the four ATom campaigns. The CIT-CIMS employs CF3O-ion chemistry with two independent mass spectrometers (compact time-of-flight and triple quadrupole) to enable sensitive and specific measurements of atmospheric trace gases. The measurements include hydrogen peroxide (H2O2), hydrogen cyanide (HCN), nitric acid (HNO3), methyl hydrogen peroxide (CH3OOH), peroxyacetic acid (C2O3H4), peroxynitric acid (HO2NO2), and sulfur dioxide (SO2), in units of parts-per-trillion-by-volume.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_aerosols_meteorology_1684&quot;&gt;ATom_Aerosols_Meteorology_1684&lt;/h4&gt;
This dataset provides (1) the results of in situ aerosol particle property measurements collected over remote tropical areas of both Pacific and Atlantic Oceans during the NASA airborne Atmospheric Tomography (ATom) campaigns for ATom-1 and ATom-2 and (2) modeled outputs of comparable aerosol properties, atmospheric chemistry and meteorology at 70 m resolution from four chemical-transport models matched to the location and time of the aircraft measurements.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airborne_insitu_measurements_1784&quot;&gt;Airborne_Insitu_Measurements_1784&lt;/h4&gt;
This dataset provides results of selected in-situ measurements of airflow and aerosol particles collected during the following airborne campaigns: NASA Atmospheric Tomography (ATom), Saharan Aerosol Long-range Transport and Aerosol-Cloud-interaction Experiment (SALTRACE), and Absorbing aerosol layers in a changing climate: aging, lifetime and dynamics (A-LIFE). The airborne campaigns were conducted between 2013-06-10 and 2018-05-21. Depending upon the aircraft instrumentation per flight and campaign, the data include aircraft position, relative humidity, temperature, pressure, angle of attack (AOA), the probe location, true and probe air speeds, and aerosol particle diameters as extracted from Cloud Imaging Probe (CIP) images for the ATom and A-LIFE flights. Also provided are the results of combining the airborne data with numerical modeling to simulate particle sampling efficiency. Simulations investigated how airflow around wing-mounted instruments affected sampling efficiency and the induced errors for different realistic flight conditions.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_was_instrument_data_1751&quot;&gt;ATom_WAS_Instrument_Data_1751&lt;/h4&gt;
This dataset provides atmospheric concentrations of halocarbons and hydrocarbons measured by the UC-Irvine Whole Air Sampler (WAS) during airborne campaigns conducted by NASA&amp;#39;s Atmospheric Tomography (ATom) mission. The analysis of samples from the UCI WAS provides measurements of more than 50 trace gases, including C2-C10 NMHCs, C1-C2 halocarbons, C1-C5 alkyl nitrates, and selected sulfur compounds. Species were identified and measured using an established technique of airborne whole air sampling followed by laboratory analysis using gas chromatography (GC) with flame ionization detection (FID), and mass spectrometric detection (MSD). The ATom mission deployed an extensive gas and aerosol payload on the NASA DC-8 aircraft for systematic, global-scale sampling of the atmosphere, profiling continuously from 0.2 to 12 km altitude. Flights occurred in each of 4 seasons from 2016 to 2018.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_noyo3_instrument_data_1734&quot;&gt;ATom_NOyO3_Instrument_Data_1734&lt;/h4&gt;
This dataset provides in situ concentrations of nitric oxide (NO), nitrogen dioxide (NO2), total reactive nitrogen oxides (NOy), and ozone (O3) measured by the NOAA Nitrogen Oxides and Ozone (NOyO3) 4-channel chemiluminescence (CL) instrument during airborne campaigns conducted by NASA&amp;#39;s Atmospheric Tomography (ATom) mission. NOyO3 provides fast-response, specific, high precision, and calibrated measurements of nitrogen oxides and ozone at a spatial resolution of better than 100 m. ATom deploys an extensive gas and aerosol payload on the NASA DC-8 aircraft for systematic, global-scale sampling of the atmosphere, profiling continuously from 0.2 to 12 km altitude. Flights occurred in each of 4 seasons from 2016 to 2018. Flights originate from the Armstrong Flight Research Center in Palmdale, California, fly north to the western Arctic, south to the South Pacific, east to the Atlantic, north to Greenland, and return to California across central North America. ATom establishes a single, contiguous, global-scale dataset. This comprehensive dataset will be used to improve the representation of chemically reactive gases and short-lived climate forcers in global models of atmospheric chemistry and climate.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_sp2_instrument_data_1672&quot;&gt;ATom_SP2_Instrument_Data_1672&lt;/h4&gt;
This dataset provides the refractory black carbon mass concentration at one-second resolution measured by the Single Particle Soot Photometer (NOAA SP2) instrument during airborne campaigns conducted by NASA&amp;#39;s Atmospheric Tomography (ATom) mission. The SP2 is a laser-induced incandescence instrument primarily used for measuring the black carbon mass content of individual particles.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_ao2_instrument_data_v2_1880&quot;&gt;ATom_AO2_Instrument_Data_V2_1880&lt;/h4&gt;
This dataset provides in situ atmospheric oxygen and carbon dioxide concentrations measured by the NCAR Airborne Oxygen Instrument (AO2) during airborne campaigns conducted by NASA&amp;#39;s Atmospheric Tomography (ATom) mission. The AO2 Instrument measures O2 concentration using a vacuum-ultraviolet absorption technique. ATom deploys an extensive gas and aerosol payload on the NASA DC-8 aircraft for a systematic, global-scale sampling of the atmosphere, profiling continuously from 0.2 to 12 km altitude. Flights occurred in each of 4 seasons from 2016 to 2018. Flights originate from the Armstrong Flight Research Center in Palmdale, California, fly north to the western Arctic, south to the South Pacific, east to the Atlantic, north to Greenland, and return to California across central North America. ATom establishes a single, contiguous, global-scale dataset. This comprehensive dataset will be used to improve the representation of chemically reactive gases and short-lived climate forcers in global models of atmospheric chemistry and climate.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_amp_instrument_data_1671&quot;&gt;ATom_AMP_Instrument_Data_1671&lt;/h4&gt;
This dataset provides the number, surface area, and volume concentrations and size distributions of dry aerosol particles measured by the Aerosol Microphysical Properties (AMP) instrument package during airborne campaigns conducted by NASA&amp;#39;s Atmospheric Tomography (ATom) mission. Five instruments--two nucleation-mode aerosol size spectrometers (NMASS), two ultra-high sensitivity aerosol spectrometers (UHSAS), and a laser aerosol spectrometer (LAS)--comprise the AMP package. The AMP payload provides size distributions with up to one-second time resolution for dry aerosol particles between 0.003 and 4.8 microns in diameter.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_gt_cims_instrument_data_1715&quot;&gt;ATom_GT_CIMS_Instrument_Data_1715&lt;/h4&gt;
This dataset provides measurements of two important components of photochemical smog - peroxyacetyl nitrate (PAN) and peroxyl propionyl nitrate (PPN)- measured by the Georgia Tech Chemical Ionization Mass Spectrometer (GT-CIMS) during airborne campaigns conducted by NASA&amp;#39;s Atmospheric Tomography (ATom) mission. The GT-CIMS measures reactive nitrogen species in the lower atmosphere. ATom deploys an extensive gas and aerosol payload on the NASA DC-8 aircraft for systematic, global-scale sampling of the atmosphere, profiling continuously from 0.2 to 12 km altitude. Flights occurred in each of 4 seasons from 2016 to 2018. Flights originate from the Armstrong Flight Research Center in Palmdale, California, fly north to the western Arctic, south to the South Pacific, east to the Atlantic, north to Greenland, and return to California across central North America. ATom establishes a single, contiguous, global-scale dataset. This comprehensive dataset will be used to improve the representation of chemically reactive gases and short-lived climate forcers in global models of atmospheric chemistry and climate.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_hr-ams_instrument_data_1716&quot;&gt;ATom_HR-AMS_Instrument_Data_1716&lt;/h4&gt;
This dataset provides the atmospheric concentrations of separated ions from inorganic and organic species measured by the High-Resolution Aerosol Mass Spectrometer (HR-AMS) collected during flights of the NASA ATom Mission. Data are available from all four ATom Campaigns. The HR-AMS detects non-refractory submicron aerosol composition by impaction on a vaporizer at 600 degrees C, followed by electron ionization and time-of-flight mass spectral analysis. The measurements include chemically speciated submicron non-refractory particulate mass at a one second and 60 second resolution, and the size distribution of chemically speciated submicron non-refractory particulate mass at 60 second resolution.
&lt;br&gt;&lt;h4 id&#x3D;&quot;noaa_tof_cims_instrument_data_1921&quot;&gt;NOAA_ToF_CIMS_Instrument_Data_1921&lt;/h4&gt;
This dataset provides the mixing ratios of reactive nitrogen and halogen species measured by the NOAA Iodide Ion Time-of-Flight Chemical Ionization Mass Spectrometer (NOAA CIMS) during airborne campaigns conducted by NASA&amp;#39;s Atmospheric Tomography (ATom) mission for ATom-3 and ATom-4 campaigns. The NOAA CIMS uses chemical ionization mass spectrometric detection of gas phase organic and inorganic analytes via I- adduct formation. Measurements for ATom include N2O5 (dinitrogen pentoxide), ClNO2 (chloro nitrite), Cl2 (Chlorine), HCOOH (formic acid), C2H4O3S (hydroperoxymethyl thioformate), BrCl (bromine monochloride), BrCN (cyanogen bromide), and BrO (bromine monoxide). ATom deploys an extensive gas and aerosol payload on the NASA DC-8 aircraft for systematic, global-scale sampling of the atmosphere, profiling continuously from 0.2-13 km altitude. This comprehensive dataset will be used to improve the representation of chemically reactive gases and short-lived climate forcers in global models of atmospheric chemistry and climate.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_pfp_instrument_data_1746&quot;&gt;ATom_PFP_Instrument_Data_1746&lt;/h4&gt;
This dataset provides mole fractions of atmospheric trace gases measured by the Programmable Flask Package (PFP) Whole Air Sampler during airborne campaigns conducted by NASA&amp;#39;s Atmospheric Tomography (ATom) mission. The PFP whole air sampler provides a means of automated or manual filling of glass flasks. The sampler is designed to remove excess water vapor from the sampled air and compress it without contamination into ~1-liter volumes. These flasks are analyzed at the NOAA&amp;#39;s Global Monitoring Division laboratory for trace gases and at the INSTAR&amp;#39;s Staple Isotope Lab laboratory for isotopes of methane. Analysis of standardized PFP samples can measure more than 60 trace gases including N2O, SF6, H2, CS2, OCS, CO2, CH4, CO, CFCs, HCFCs, HFCs, Solvents, Methyl Halides, Hydrocarbons and Perfluorocarbons. The ATom mission deployed an extensive gas and aerosol payload on the NASA DC-8 aircraft for systematic, global-scale sampling of the atmosphere, profiling continuously from 0.2 to 12 km altitude. Flights occurred in each of 4 seasons from 2016 to 2018.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_isaf_instrument_data_1730&quot;&gt;ATom_ISAF_Instrument_Data_1730&lt;/h4&gt;
This dataset provides the atmospheric volume mixing ratio of formaldehyde measured during airborne campaigns conducted by NASA&amp;#39;s Atmospheric Tomography (ATom) mission. ATom deploys an extensive gas and aerosol payload on the NASA DC-8 aircraft for systematic, global-scale sampling of the atmosphere, profiling continuously from 0.2 to 12 km altitude. Flights occurred in each of 4 seasons from 2016 to 2018. The NASA In Situ Airborne Formaldehyde (ISAF) instrument, based at the Goddard Space Flight Center, measures formaldehyde on high-altitude NASA aircraft. The instrument uses laser-induced fluorescence (LIF) to obtain the high detection sensitivity needed to detect formaldehyde in the upper troposphere and lower stratosphere where abundances are 10 parts per trillion. LIF also enables a fast time response needed to measure the abundance of formaldehyde in the finely structured outflow of convective storms. These measurements of formaldehyde will be used elucidate mechanisms of convective transport and quantify the effects of boundary layer pollutants on the ozone photochemistry and cloud microphysics of the upper atmosphere.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_particulate_iodine_1773&quot;&gt;ATom_Particulate_Iodine_1773&lt;/h4&gt;
This dataset provides mass concentrations of particulate iodine as measured by the High-Resolution Aerosol Mass Spectrometer (HR-AMS) during the first two deployments of the NASA Atmospheric Tomography airborne missions (ATom-1 and ATom-2) in 2016 and 2017, respectively. The data provided in this dataset result from a reanalysis of the initial HR-AMS data based on post-mission calibrations and are reported at 1-minute resolution. The dataset also includes the fractions of the main ions (I+, HI+, and I2+) that can be used to ascertain the oxidation state of iodine in particles. Each observation includes an air mass classification flag (tropospheric or stratospheric conditions) based on collocated in situ water vapor and ozone measurements and positional data from the HR-AMS data feed.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_medusa_instrument_data_v2_1881&quot;&gt;ATom_Medusa_Instrument_Data_V2_1881&lt;/h4&gt;
This dataset provides O2/N2, CO2, Ar/N2, and stable isotope ratios of CO2 measured in flasks collected by the Medusa Whole Air Sampler during airborne campaigns conducted by NASA&amp;#39;s Atmospheric Tomography (ATom) mission. ATom deployed an extensive gas and aerosol payload on the NASA DC-8 aircraft for a systematic, global-scale sampling of the atmosphere, profiling continuously from 0.2 to 12 km altitude. Flights occurred in each of 4 seasons from 2016 to 2018. Medusa collected 32 cryogenically dried, flow, and pressure-controlled samples per flight. The samples are collected by an automated sampler into 1.5 L glass flasks that integrate over 25 seconds. Medusa provides discretely-sampled comparisons for onboard in situ O2/N2 ratio and CO2 measurements and unique measurements of Ar/N2 and 13C, 14C, and 18O isotopologues of CO2. Medusa flasks are analyzed on a sector-magnet mass spectrometer and a LiCor non-dispersive infrared CO2 analyzer by the Scripps O2 Program at Scripps Institution of Oceanography.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_sp2_lam_feox_mmr_1828&quot;&gt;ATom_SP2_LAM_FeOx_MMR_1828&lt;/h4&gt;
This dataset provides mass mixing ratios and number density of light-absorbing metallic aerosols (LAM) in the size range 180-1290 nm obtained with the NOAA Single Particle Soot Photometer (SP2) during the four deployments of the NASA Atmospheric Tomography (ATom) airborne mission from 2016-2018. The NOAA SP2 detects light absorbing aerosols, such as black carbon (BC), via laser-induced incandescence to provide real-time in situ quantification of refractory aerosol mass and number density. The percent of LAM aerosols attributed to anthropogenic iron oxides (FeOx) by mass is also provided.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_athos_instrument_data_v2_1930&quot;&gt;ATom_ATHOS_Instrument_Data_V2_1930&lt;/h4&gt;
This dataset provides the mixing ratios of hydrogen oxides measured by the Airborne Tropospheric Hydrogen Oxides Sensor (ATHOS) during the ATom 1-4 campaigns. ATHOS uses laser-induced fluorescence (LIF) to measure hydroxide (OH) and hydroperoxyl (HO2) simultaneously. The measurements include OH and HO2 mixing ratios and the OH interference determined by chemical removal of OH. The reactivity of OH is measured by the OH Reactivity (OHR) instrument using the discharge flow method and is integrated into the ATHOS electronics. These data provide insights into the oxidative state of the global atmosphere. These data are useful for testing the oxidation chemistry in models and other analytical methods being developed to deduce the atmosphere&amp;#39;s oxidative state.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_mms_instrument_data_1731&quot;&gt;ATom_MMS_Instrument_Data_1731&lt;/h4&gt;
This dataset contains measurements from the Meteorological Measurement System (MMS) instrument from the four ATom campaigns. MMS is a state-of-the-art instrument for measuring accurate, high resolution in situ airborne state parameters (pressure, temperature, turbulence index, and the 3-dimensional wind vector). These key measurements enable our understanding of atmospheric dynamics, chemistry, and microphysical processes. The MMS is used to investigate atmospheric mesoscale (gravity and mountain lee waves) and microscale (turbulence) phenomena. An accurate characterization of the turbulence phenomenon is important for the understanding of dynamic processes in the atmosphere, such as the behavior of buoyant plumes within cirrus clouds, diffusions of chemical species within wake vortices generated by jet aircraft, and microphysical processes in breaking gravity waves. Accurate temperature and pressure data are needed to evaluate chemical reaction rates as well as to determine accurate mixing ratios. Accurate wind field data establish a detailed relationship with the various constituents and the measured wind also verifies numerical models used to evaluate air mass origin.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_palms_instrument_data_1733&quot;&gt;ATom_PALMS_Instrument_Data_1733&lt;/h4&gt;
This dataset contains single-particle aerosol composition as measured by the Particle Analysis by Laser Mass Spectrometry (PALMS) instrument during the four ATom campaigns from 2016-2018. Single aerosol particles are classified into several particle types, including: mixed sulfate/organic nitrate, biomass burning, elemental carbon, mineral/metallic, meteoric material, alkali salt, sea salt, heavy oil combustion, and others. Particle types are reported as raw number fractions and as absolute mass concentrations. PALMS measures aerosol composition for particles from diameter ~100 to 5000 nm, with most of the particle data in the size range ~150 to 3000 nm. Also included are absolute aerosol concentrations measured by a modified Laser Aerosol Spectrometer (LAS). Integrated number, surface area, and volume concentrations from LAS are reported over multiple size ranges.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_qcls_instrument_data_v2_1932&quot;&gt;ATom_QCLS_Instrument_Data_V2_1932&lt;/h4&gt;
This dataset provides atmospheric concentrations of CO2, CH4, CO, and N2O measured by the Harvard Quantum Cascade Laser System (QCLS) instruments during airborne campaigns conducted by NASA&amp;#39;s Atmospheric Tomography (ATom) mission. The QCLS (DUAL and CO2) instrument package contains two separate optical assemblies and calibration systems, and a common data system and power supply. The QCLS DUAL instrument simultaneously measures CO, CH4, and N2O concentrations, in situ, using two thermoelectrically cooled pulsed-quantum cascade lasers light sources, a multiple pass absorption cell, and two liquid nitrogen-cooled solid-state detectors. The QCLS CO2 instrument measures CO2 concentrations in situ using a thermoelectrically cooled pulsed-quantum cascade laser light source, gas cells, and liquid nitrogen cooled solid-state detectors. The CO2 mixing ratio of air flowing through the sample gas cell is determined by measuring absorption from a single infrared transition line at 4.32 microns relative to a reference gas of known concentration.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_ucats_instrument_data_1750&quot;&gt;ATom_UCATS_Instrument_Data_1750&lt;/h4&gt;
This dataset, collected with the Unmanned Aircraft Systems (UAS) Chromatograph for Atmospheric Trace Species (UCATS), provides atmospheric concentrations of nitrous oxide (N2O), sulfur hexafluoride (SF6), methane (CH4), hydrogen (H2), carbon monoxide (CO), water vapor (H2O), and ozone (O3). The UCATS system is three different instruments in one enclosure: a two-channel chromatograph with electron capture detectors (one measures N2O and SF6, the other measures CH4, H2 and CO), a tunable diode laser instrument for H2O, and a dual-beam O3 photometer.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_saga_instrument_data_1748&quot;&gt;ATom_SAGA_Instrument_Data_1748&lt;/h4&gt;
Soluble acidic gases and aerosols (SAGA) were collected with two related installations; a mist chamber/ion chromatography (MC/IC) system and a paired bulk aerosol system. The MC/IC system measures in situ atmospheric distributions of nitric acid (plus &amp;lt; 1 um NO3 aerosol) and fine (&amp;lt; 1 um) aerosol sulfate at an approximately 80-second interval. The paired bulk aerosol system collects particulates onto filters for subsequent analysis. Collected filters were first extracted with water to obtain the water-soluble (WS) constituents and then extracted again using methanol to collect the methanol soluble (MS) fraction. The light absorption of filtered extracts was measured from 300 to 700 nm. Ion chromatography on aqueous extracts of the bulk aerosol samples collected on Teflon filters were used to quantify soluble ions (Cl-, Br-, NO3-, SO42-, C2O42-, Na+, NH4+, K+, Ca+, and Mg+). The SAGA system is provided by the University of New Hampshire (UNH).
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_merge_1581&quot;&gt;ATom_merge_1581&lt;/h4&gt;
This dataset provides information on greenhouse gases and human-produced air pollution, including atmospheric concentrations of carbon dioxide (CO2), methane (CH4), tropospheric ozone (O3), and black carbon (BC) aerosols, collected during airborne campaigns conducted by NASA&amp;#39;s Atmospheric Tomography (ATom) mission. This dataset includes merged data from all instruments plus additional data such as numbered profiles and distance flown. Merged data have been created for seven different sampling intervals. In the case of data obtained over longer time intervals (e.g. flask data), the merge files provide (weighted) averages to match the sampling intervals. ATom deploys an extensive gas and aerosol payload on the NASA DC-8 aircraft for a systematic, global-scale sampling of the atmosphere, profiling continuously from 0.2 to 12 km altitude. Flights occurred in each of 4 seasons from 2016 to 2018. Flights originate from the Armstrong Flight Research Center in Palmdale, California, fly north to the western Arctic, south to the South Pacific, east to the Atlantic, north to Greenland, and return to California across central North America. ATom establishes a single, contiguous, global-scale dataset. This comprehensive dataset will be used to improve the representation of chemically reactive gases and short-lived climate forcers in global models of atmospheric chemistry and climate. Profiles of the reactive gases will also provide critical information for the validation of satellite data, particularly in remote areas where in situ data is lacking. Complete aircraft flight information including, but not limited to, latitude, longitude, and altitude are also provided. This data release provides results from all instruments on all four ATom flight campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_nmass_data_1607&quot;&gt;ATom_NMASS_Data_1607&lt;/h4&gt;
This dataset provides extensive calibration and in-flight performance data for two nucleation mode aerosol size spectrometer (NMASS) instruments utilized in the NASA Atmospheric Tomography Mission (ATom). Each NMASS has five condensation particle counters (CPCs) that detect particles above a different minimum size, determined by the maximum vapor supersaturation encountered by the particles. Operated in parallel, the CPCs provide continuous concentrations of particles in different cumulative size classes between 3 and 60 nm. Knowing the response function of each CPC, numerical inversion techniques were applied to recover size distributions from the continuous concentrations. Data provided include: NMASS counting efficiencies and diameters of calibration aerosols, inverted particle size distributions; comparisons of NMASS and Scanning Mobility Particle Sizer (SMPS) results; and performance at flows, temperatures, and pressures measured by both NMASSs and comparison with Ultra-High Sensitivity Aerosol Spectrometer (UHSAS) concentrations collected on board the NASA DC-8 aircraft during an ATom flight in February 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_co_geos_1604&quot;&gt;ATom_CO_GEOS_1604&lt;/h4&gt;
This dataset contains carbon monoxide (CO) observations at 10-second intervals from flights during the ATom-1 campaign in 2016 and simulated CO concentrations from the Goddard Earth Observing System version 5 (GEOS-5) model for the corresponding locations along the ATom flight tracks. The Atmospheric Tomography Mission (ATom) is a NASA Earth Venture Suborbital-2 mission studying the impact of human-produced air pollution on greenhouse gases and on chemically reactive gases in the atmosphere. The airborne observations were collected using the Quantum Cascade Laser System (QCLS) instrument, a high-frequency laser spectroscopy instrument for in situ atmospheric gas sampling. This dataset provides a direct comparison of observational and simulated CO that will be used to inform future atmospheric modeling experiments. The dataset also contains simulated tagged-CO tracer concentrations, which represent the contribution of specific regional sources to the total simulated CO. This dataset contributes to one of the ATom mission objectives to create an observation-based chemical climatology of important atmospheric constituents and their reactivity in the remote troposphere.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_organic_aerossols_1795&quot;&gt;ATom_Organic_Aerossols_1795&lt;/h4&gt;
This dataset provides airborne in situ observations of submicron organic aerosol (OA) mass concentrations during the first (mid-2016) and second (early-2017) global deployments of the Atmospheric Tomography Mission (ATom), as well as modeled submicron OA mass concentrations along the flight tracks from global chemistry models that implement a variety of commonly used representations of OA sources and chemistry. In situ observations include non-refractory submicron aerosols measured by the High-Resolution Aerosol Mass Spectrometer (HR-AMS), aerosol volume concentrations measured by the Aerosol Microphysical Properties package (AMP), black carbon mass content measured by the Single Particle Soot Photometer (NOAA SP2), and refractory and non-refractory aerosol composition measured by the Particle Analysis By Laser Mass Spectrometry (PALMS). Both observed and modeled data are provided at a 60-second temporal resolution. The data are provided in netCDF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_ozonesonde_instrumentdata_1910&quot;&gt;ATom_Ozonesonde_InstrumentData_1910&lt;/h4&gt;
This dataset contains ozone measurements from the Ozonesonde instrument in Antarctica, Hawaii, and Fiji taken during the Atom-4 campaign. The Electrochemical Concentration Cell (ECC) Ozonesonde is a balloon-borne instrument that collects ozone concentrations paired with a radiosonde to collect additional meteorological info along a vertical profile (as a result, unlike other ATom data, this dataset is not associated with DC-8). The balloon can ascend to altitudes of 35 km before bursting. Ozone in the stratosphere helps reduce UV radiation that reaches Earth&amp;#39;s surface; however, ozone at ground level can negatively influence respiratory health.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_simulated_data_1597&quot;&gt;ATom_Simulated_Data_1597&lt;/h4&gt;
This dataset provides a simulated data stream representative of an Atmospheric Tomography mission (ATom) data collection flight and also modeled reactivities for ozone (O3) production and loss and methane (CH4) loss from six global atmospheric chemistry models: CAM, GEOS-Chem, GFDL, GISS-E2.1, GMI, and UCI. The simulated data include concentrations of selected atmospheric trace gases for 14,880 air parcels along a simulated north-south ATom flight path along 180-degrees longitude over the Pacific basin. Each of the six models produced ozone production and loss and methane loss reactivities initialized using the simulated data beginning with five different days in August (8-01, 8-06, 8-11, 8-16, 8-21). Modeled years for each individual model varied from 1997 to 2016.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_so2_lif_instrument_data_1890&quot;&gt;ATom_SO2_LIF_Instrument_Data_1890&lt;/h4&gt;
This dataset provides concentrations of sulfur dioxide (SO2) measured by the Laser Induced Fluorescence Instrumentation for Sulfur Dioxide (SO2-LIF) on the ATom-4 campaign in April and May 2018. The LIF-SO2 instrument detects SO2 at the single-part per trillion level using red-shifted laser-induced fluorescence. Measurements are reported at 1-second intervals along the flight paths. Sources of SO2 atmosphere from natural sources include volcanic eruptions and wildfires; however, most anthropogenic sources, such as fossil fuel combustion, arise. SO2 influences some negative health and environmental impacts and is an important precursor of aerosols in the nucleation of new particles globally.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_panther_instrument_data_1914&quot;&gt;ATom_PANTHER_Instrument_Data_1914&lt;/h4&gt;
This dataset contains measurements of various trace gases from the PAN and Trace Hydrohalocarbon ExpeRiment (PANTHER) across the four ATom campaigns. PANTHER uses Electron Capture Detection and Gas Chromatography (ECD-GC) and Mass Selective Detection and Gas Chromatography (MSD-GC) to measure numerous trace gases, including methyl halides, HCFCs, PAN, N2O, SF6, CFC-12, CFC-11, Halon 1211, methyl chloroform, carbon tetrachloride.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_uhsas_data_1619&quot;&gt;ATom_UHSAS_Data_1619&lt;/h4&gt;
This dataset provides extensive calibration and in-flight performance data for two Ultra-High Sensitivity Aerosol Spectrometers (UHSAS) used for particle size distribution and volatility measurements during the NASA Atmospheric Tomography Mission (ATom) airborne campaign. UHSAS-1 was equipped with a compact thermodenuder operating at 300 degrees C and UHSAS-2 was operated without a thermodenuder to determine the number and volume fraction of volatile particles. Laboratory studies utilized aerosols from limonene ozonolysis (limon), atomization of ammonium sulfate (AS), and atomization of 2-diethylhexyl (dioctyl) sebacate (DOS). Data include: UHSAS detection efficiency, sizing calibration, performance at a range of pressures and at a range of thermodenuder temperatures, comparison of UHSAS-2 and condensation particle counter (CPC) particle number concentrations, comparisons of UHSAS-1 and UHSAS-2 for dry particle number concentration, surface area and volume collected onboard of a NASA DC-8 aircraft during August 2016, and dry aerosol size distributions for thermodenuded and non-thermodenuded instrument collected in February 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aerosol_sulfate_lowermoststrat_1868&quot;&gt;Aerosol_Sulfate_LowermostStrat_1868&lt;/h4&gt;
This dataset consists of (a) selected aerosol and gas-phase observations made on all four deployments of NASA Atmospheric Tomography Mission (ATom), (b) thermodynamic properties related to aerosol formation derived from these measurements, (c) 48-h back trajectories for ATom-4 observations, and (d) output from the Model of Aerosols and Ions in the Atmosphere (MAIA). ATom observations, thermodynamics, and back trajectories were inputs for MAIA model runs. MAIA runs focused on data from ATom-4 deployment, and output includes aerosol formation rates, and ultrafine particle size distributions and number concentrations in the lowermost stratosphere (LMS). ATom 1-4 deployments included all four seasons from 2016 to 2018. This investigation sought to understand how new particle formation (NPF) can occur in the LMS, factors influencing the amount of NPF, and other potential sources of ultrafine aerosols in this region of the atmosphere. The data are provided in comma-separated value (CSV) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atom_toga_instrument_data_v2_1936&quot;&gt;ATom_TOGA_Instrument_Data_V2_1936&lt;/h4&gt;
This dataset provides concentrations of volatile organic compounds (VOCs) measured by the Trace Organic Gas Analyzer (TOGA) during the four ATom campaigns. These data are relevant to the impact of human-produced air pollution on greenhouse gases and on chemically reactive gases in the atmosphere. Specific data were obtained for radical precursors, tracers of anthropogenic and biogenic activities, tracers of urban and biomass combustion emissions, products of oxidative processing, precursors to aerosol formation, and compounds important for aerosol modification and transformation. TOGA measures a wide range of VOCs with high sensitivity (ppt or lower), frequency (2-minutes), accuracy (often 15% or better), and precision (&amp;lt;3%).
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.ornldaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA AVIRIS Project</title>
      <link>https://registry.opendata.aws/nasa-aviris</link>
      <guid>https://registry.opendata.aws/nasa-aviris</guid>
      <description>This dataset provides attributed geospatial and tabular information for identifying and querying flight lines of interest for the Airborne Visible InfraRed Imaging Spectrometer-Classic (AVIRIS-C) and Airborne Visible InfraRed Imaging Spectrometer-Next Generation (AVIRIS-NG) Facility Instrument collections. It includes attributed shapefile and GeoJSON files containing polygon representation of individual flights lines for all years and separate KMZ files for each year. These files allow users to visualize and query flight line locations using Geographic Information System (GIS) software. Tables of AVIRIS-C and AVIRIS-NG flight lines with attributed information include dates, bounding coordinates, site names, investigators involved, flight attributes, associated campaigns, and corresponding file names for associated L1B (radiance) and L2 (reflectance) files in the AVIRIS-C and AVIRIS-NG Facility Instrument Collections. Tabular information is also provided in comma-separated values (CSV) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;av3_l1b_rdn_2356&quot;&gt;AV3_L1B_RDN_2356&lt;/h4&gt;
This dataset contains Level 1B (L1B) calibrated radiance images as well as observational geometry and illumination parameters from the Airborne Visible / Infrared Imaging Spectrometer-3 (AVIRIS-3) instrument. This is the NASA Earth Observing System Data and Information System (EOSDIS) facility instrument archive of these data. The NASA AVIRIS-3 is a spectral mapping system that measures reflected radiance at 7.4-nm intervals in the Visible to Shortwave Infrared (VSWIR) spectral range from 390-2500 nm. The AVIRIS-3 sensor has a 40 degree instantaneous field of view with 1234 pixels, providing altitude dependent ground sampling distances from 12 m to sub meter range. This spectrometer measures radiance from surface and atmosphere and is extremely similar in design to the orbital Earth Surface Mineral Dust Source Investigation (EMIT) spectrometer. AVIRIS-3 has been designed to fly on a variety of aircraft platforms including the King Air B-200, Gulfstream III, Gulfstream V, and ER-2. For each flight line, two file types are included: calibrated radiance (RDN) and orthocorrected observation geometry and illumination (ORT) in netCDF format. Both file types include a geolocation lookup table (GLT) for georeferencing pixels in UTM and geographic coordinates. A band mask file indicates whether wavelengths were interpolated on a per pixel basis. In addition, ancillary files for each flight line are provided, including a quick look image in JPEG format and text files in YAML format that document processing algorithms and parameters used during production.
&lt;br&gt;&lt;h4 id&#x3D;&quot;av3_l2a_rfl_2357&quot;&gt;AV3_L2A_RFL_2357&lt;/h4&gt;
This dataset contains Level 2A (L2A) surface reflectance images from the Airborne Visible / Infrared Imaging Spectrometer-3 (AVIRIS-3) instrument. This is the NASA Earth Observing System Data and Information System (EOSDIS) facility instrument archive of these data. The NASA AVIRIS-3 is a spectral mapping system that measures reflected radiance at 7.4-nm intervals in the Visible to Shortwave Infrared (VSWIR) spectral range from 390-2500 nm. Surface hemispherical directional reflectance was derived from calibrated radiance using an optimal estimation algorithm. For each flight line, two file types are included: orthocorrected surface reflectance (RFL_ORT) and orthocorrected reflectance uncertainty (UNC_ORT) in netCDF format. Both file types include data projected in a UTM coordinate system. In addition, ancillary files for each flight line are provided, including a quick look image in GeoTIFF format and text files in YAML format that document processing algorithms and parameters used during production.
&lt;br&gt;&lt;h4 id&#x3D;&quot;av3_l2b_ghg_2358&quot;&gt;AV3_L2B_GHG_2358&lt;/h4&gt;
This dataset contains Level 2B (L2b) enhancements of greenhouse gasses (GHG) derived from imagery collected by the Airborne Visible / Infrared Imaging Spectrometer-3 (AVIRIS-3) instrument. Products include methane and carbon dioxide enhancements, each with per-pixel uncertainties and sensitivities to the background. Concentration enhancements are estimated from radiance measurements using a column-wise adaptive matched filter approach, which searches each pixel&amp;#39;s radiance spectrum for deviations that are characteristic of a GHG&amp;#39;s absorption spectrum. This is the NASA Earth Observing System Data and Information System (EOSDIS) facility instrument archive of these data. The NASA AVIRIS-3 is a spectral mapping system that measures reflected radiance at 7.4-nm intervals in the Visible to Shortwave Infrared (VSWIR) spectral range from 390-2500 nm.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aviris-classic_l1b_radiance_2155&quot;&gt;AVIRIS-Classic_L1B_Radiance_2155&lt;/h4&gt;
This dataset contains Level 1B (L1B) orthocorrected, scaled radiance image files as well as files of observational geometry and illumination parameters and supporting sensor band information from the Airborne Visible / Infrared Imaging Spectrometer (AVIRIS-Classic) instrument. This is the NASA Earth Observing System Data and Information System (EOSDIS) facility instrument archive of these data. The NASA AVIRIS-Classic is a pushbroom spectral mapping system with high signal-to-noise ratio (SNR), designed and toleranced for high performance spectroscopy. AVIRIS-Classic measures reflected radiance in 224 contiguous bands at approximately 10-nm intervals in the Visible to Shortwave Infrared (VSWIR) spectral range from 400-2500 nm. The AVIRIS-Classic sensor has a 1 milliradian instantaneous field of view, providing altitude dependent ground sampling distances from 20 m to sub meter range. AVIRIS-Classic is flown on a variety of aircraft platforms including the Twin Otter, NASA&amp;#39;s WB-57, and NASA&amp;#39;s high altitude ER-2. Multiple file types are included for each flight line. The primary data files include: orthocorrected calibrated radiance image (img) files, geometric lookup table (glt) and orthocorrected observation geometry and illumination (obs_ort) files. Also included are unprojected files of input geometry (igm), and parameters relating to the geometry of observation and illumination (obs). Additional files provide information on spectral (spc) and radiometric calibration (rcc, gain), spatial resolution (geo), aircraft and sensor position (eph, nav), deployment notes (info), and data processing (plog). Quicklook images (jpeg) and polygon outlines of imagery footprints (kmz) are provided for each flight line. The primary AVIRIS-Classic L1B data are provided in ENVI binary format, which includes a flat binary file accompanied by a header (.hdr) file holding metadata in text format. The ancillary files include JPEG images, maps in Keyhole Markup Language (KML), and calibration files in binary and text formats. This archive currently includes data from 2004, and 2006 - 2025. Additional L1B data will be added as they become available. AVIRIS-Classic supports NASA Science and applications in many areas including plant composition and function, geology and soils, greenhouse gas mapping, and calibration of orbital platforms.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aviris-classic_l2_reflectance_2154&quot;&gt;AVIRIS-Classic_L2_Reflectance_2154&lt;/h4&gt;
This dataset contains Level 2 (L2) orthocorrected reflectance from the Airborne Visible / Infrared Imaging Spectrometer (AVIRIS-Classic) instrument. This is the NASA Earth Observing System Data and Information System (EOSDIS) facility instrument archive of these data. The NASA AVIRIS-Classic is a pushbroom spectral mapping system with high signal-to-noise ratio (SNR), designed and toleranced for high performance spectroscopy. AVIRIS-Classic measures reflected radiance in 224 contiguous bands at approximately 10-nm intervals in the Visible to Shortwave Infrared (VSWIR) spectral range from 400-2500 nm. The AVIRIS-Classic sensor has a 1 milliradian instantaneous field of view, providing altitude dependent ground sampling distances from 20 m to sub meter range. AVIRIS-Classic is flown on a variety of aircraft platforms including the Twin Otter, NASA&amp;#39;s WB-57, and NASA&amp;#39;s high altitude ER-2. For each flight line, two types of L2 data files may be included: (a) calibrated surface reflectance and (b) water vapor and optical absorption paths for liquid water and ice. The L2 data are provided in ENVI format, which includes a flat binary file accompanied by a header (.hdr) file holding metadata in text format. This archive currently includes data from 2008 - 2025. Additional AVIRIS-Classic facility instrument L2 data will be added as they become available. AVIRIS-Classic supports NASA Science and applications in many areas including plant composition and function, geology and soils, greenhouse gas mapping, and calibration of orbital platforms.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aviris-ng_l1b_radiance_2095&quot;&gt;AVIRIS-NG_L1B_radiance_2095&lt;/h4&gt;
This dataset contains Level 1B (L1B) orthocorrected, scaled radiance image files as well as files of observational geometry and illumination parameters and supporting sensor band information from the Airborne Visible / Infrared Imaging Spectrometer-Next Generation (AVIRIS-NG) instrument. This is the NASA Earth Observing System Data and Information System (EOSDIS) facility instrument archive of these data. The NASA AVIRIS-NG is a pushbroom spectral mapping system with high signal-to-noise ratio (SNR), designed and toleranced for high performance spectroscopy. AVIRIS-NG measures reflected radiance at 5-nm intervals in the Visible to Shortwave Infrared (VSWIR) spectral range from 380-2510 nm. The AVIRIS-NG sensor has a 1 milliradian instantaneous field of view, providing altitude dependent ground sampling distances from 20 m to sub-meter range. In this dataset, for each flight line, six file types are included: orthocorrected calibrated radiance image (img) files, geometric lookup table (glt) and orthocorrected observation geometry and illumination (obs_ort) files. Also included are unprojected files of input geometry (igm), parameters relating to the geometry of observation and illumination (obs), and orthocorrected locations of each pixel (loc). In addition, ancillary files for the flight line are provided, including quick look images and polygon outlines of imagery footprints. The AVIRIS-NG L1B data are provided in ENVI binary format, which includes a flat binary file accompanied by a header (.hdr) file holding metadata in text format. The ancillary files include JPEG images and maps in Keyhole Markup Language (KML). The AVIRIS-NG is flown on a variety of aircraft platforms including the Twin Otter, the King Air B-200, and NASA&amp;#39;s high altitude ER-2. This archive currently includes data from 2014 - 2022. Additional AVIRIS-NG facility instrument L1B data will be added as they become available. AVIRIS-NG supports NASA Science and applications in many areas including plant composition and function, geology and soils, greenhouse gas mapping, and calibration of orbital platforms.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aviris-ng_l2_reflectance_2110&quot;&gt;AVIRIS-NG_L2_Reflectance_2110&lt;/h4&gt;
This dataset contains Level 2 (L2) orthocorrected reflectance from the Airborne Visible / Infrared Imaging Spectrometer-Next Generation (AVIRIS-NG) instrument. This is the NASA Earth Observing System Data and Information System (EOSDIS) facility instrument archive of these data. The AVIRIS-NG is a pushbroom spectral mapping system with high signal-to-noise ratio (SNR), designed and toleranced for high performance spectroscopy. AVIRIS-NG measures reflected radiance at 5-nm intervals in the Visible to Shortwave Infrared (VSWIR) spectral range from 380-2510 nm. The AVIRIS-NG sensor has a 1 milliradian instantaneous field of view, providing altitude dependent ground sampling distances from 20 m to sub-meter range. For each flight line, two types of L2 data files may be included: (a) calibrated surface reflectance and (b) water vapor and optical absorption paths for liquid water and ice. The L2 data are provided in ENVI format, which includes a flat binary file accompanied by a header (.hdr) file holding metadata in text format. The AVIRIS-NG is flown on a variety of aircraft platforms including the Twin Otter, the King Air B-200, and NASA&amp;#39;s high altitude ER-2. This archive currently includes data from 2014 - 2022. Additional AVIRIS-NG facility instrument L2 data will be added as they become available. The AVIRIS-NG supports NASA Science and applications in many areas including plant composition and function, geology and soils, greenhouse gas mapping, and calibration of orbital platforms.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aviris-ng_ch4_co2_plumes_2406&quot;&gt;AVIRIS-NG_CH4_CO2_Plumes_2406&lt;/h4&gt;
This dataset contains enhanced column-integrated methane (CH4) and carbon dioxide (CO2) (concentration lengths) acquired from 211 flight lines across North America imaged by the Airborne Visible/Infrared Imaging Spectrometer-Next Generation (AVIRIS-NG) between June 26 and August 15, 2023 for NASA&amp;#39;s Synergistic TEMPO Air Quality Science (STAQS) campaign. Enhanced CH4 and CO2 concentrations were estimated from the L1B radiance measurements using a cluster matched filter approach. This algorithm searches each pixel&amp;#39;s radiance spectrum for deviations that are characteristic of a greenhouses gas&amp;#39;s absorption spectrum. A total of 177 greenhouse gas plumes were identified and delineated, of which 74 were CH4 and 103 were CO2. The data are provided in GeoTIFF and JSON formats.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.ornldaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA AVISO Project</title>
      <link>https://registry.opendata.aws/nasa-aviso</link>
      <guid>https://registry.opendata.aws/nasa-aviso</guid>
      <description>This dataset contains absolute dynamic topography (similar to sea level but with respect to the geoid) binned and averaged monthly on 1 degree grids. The coverage is from October 1992 to December 2010. These data were provided by AVISO (French space agency data provider) to support the CMIP5 (Coupled Model Intercomparison Project Phase 5) under the World Climate Research Program (WCRP) and was first made available via the JPL Earth System Grid. The dynamic topography are derived from sea surface height measured by several satellites including Envisat, TOPEX/Poseidon, Jason-1 and OSTM/Jason-2, and referenced to the geoid. Along with this dataset, two additional ancillary data files are included in the same directory which contain the number of observations and standard error co-located on the same 1 degree grids.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://archive.podaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA AVUELO Project</title>
      <link>https://registry.opendata.aws/nasa-avuelo</link>
      <guid>https://registry.opendata.aws/nasa-avuelo</guid>
      <description>An inventory of NASA&amp;#39;s airborne and field campaigns for Earth Science
&lt;br&gt;&lt;h4 id&#x3D;&quot;avuelo_av3_l2a_reflectance_2479&quot;&gt;AVUELO_AV3_L2A_Reflectance_2479&lt;/h4&gt;
This dataset contains Level 2A (L2A) orthocorrected surface reflectance and uncertainty estimates from the Airborne Visible / Infrared Imaging Spectrometer-3 (AVIRIS-3) instrument acquired for the Airborne Validation Unified Experiment: Land to Ocean (AVUELO) project in 2025. This L2A data product was generated with a provisional calibration algorithm. AVUELO aims to advance the validation and calibration of spaceborne imaging spectroscopy (hyperspectral) data for tropical ecosystems by combining airborne imaging spectroscopy for terrestrial and marine sites in Panama and Costa Rica with contemporaneous field measurements and data collected in February 2025. The NASA AVIRIS-3 is a spectral mapping system that measures reflected radiance at ~7.4-nm intervals in the Visible to Shortwave Infrared (VSWIR) spectral range from 390-2500 nm. The AVIRIS-3 sensor has a 40 degree instantaneous field of view with 1,234 pixels, providing altitude dependent ground sampling distances from 12 m to sub meter range. This spectrometer measures radiance from surface and atmosphere and is identical in design to the orbital Earth Surface Mineral Dust Source Investigation (EMIT) spectrometer. AVIRIS-3 was deployed on a King Air aircraft. Surface hemispherical directional reflectance was derived from calibrated radiance using an optimal estimation algorithm. For each flight scene, two file types are included: orthocorrected surface reflectance (RFL_ORT) and orthocorrected reflectance uncertainty (UNC_ORT) in netCDF format. Both file types include data projected in a UTM coordinate system. When available, a version 2 calibration Level 2A (L2A) of orthocorrected surface reflectance and uncertainty data for these same flight lines will be available in an AVIRIS-3 L2A Orthocorrected Surface Reflectance, Facility Instrument Collection, Version 2.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.ornldaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA AfriSAR Project</title>
      <link>https://registry.opendata.aws/nasa-afrisar</link>
      <guid>https://registry.opendata.aws/nasa-afrisar</guid>
      <description>This data set contains geotagged images collected over Gabon, Africa. The images were taken by the NASA Digital Mapping Camera paired with the Land, Vegetation, and Ice Sensor (LVIS), an airborne lidar scanning laser altimeter. The data were collected as part of a NASA campaign, in collaboration with the European Space Agency (ESA) mission AfriSAR.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aflvis1b&quot;&gt;AFLVIS1B&lt;/h4&gt;
This data set contains return energy waveform data over Gabon, Africa. The measurements were taken by the NASA Land, Vegetation, and Ice Sensor (LVIS), an airborne lidar scanning laser altimeter. The data were collected as part of a NASA campaign, in collaboration with the European Space Agency (ESA) mission AfriSAR.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aflvis2&quot;&gt;AFLVIS2&lt;/h4&gt;
This data set contains surface elevation data over Gabon, Africa. The measurements were taken by the NASA Land, Vegetation, and Ice Sensor (LVIS), an airborne lidar scanning laser altimeter. The data were collected as part of a NASA campaign, in collaboration with the European Space Agency (ESA) mission AfriSAR.
&lt;br&gt;&lt;h4 id&#x3D;&quot;afrisar_agb_maps_1681&quot;&gt;AfriSAR_AGB_Maps_1681&lt;/h4&gt;
This dataset provides gridded estimates of aboveground biomass (AGB) for four sites in Gabon at 0.25 ha (50 m) resolution derived with field measurements and airborne LiDAR data collected from 2010 to 2016. The sites represent a mix of forested, savannah, and some agricultural and disturbed landcover types: Lope site, within Lope National Park; Mabounie, mostly forested site; Mondah Forest, protected area; and the Rabi forest site, part of the Smithsonian Institution of Global Earth Observatories world-wide network of forest plots. Plot-level biophysical measurements of tree diameter and tree height (or estimated by allometry) were performed at 1 ha and 0.25 ha scales on multiple plots at each site and used to derive AGB for each tree and then summed for each plot. Aerial LiDAR scans were used to construct digital elevation models (DEM) and digital surface models (DSM), and then the DEM and DSM were used to construct a canopy height model (CHM) at 1 m resolution. After checking site-plot locations against the CHM, mean canopy height (MCH) was computed over each 0.25 ha. A single regression model relating MCH and AGB estimates, incorporating local height based on the trunk DBH (HD) relationships, was produced for all sites and combined with the CHM layer to construct biomass maps at 0.25 ha resolution.
&lt;br&gt;&lt;h4 id&#x3D;&quot;afrisar_lvis_footprint_cover_1591&quot;&gt;AfriSAR_LVIS_Footprint_Cover_1591&lt;/h4&gt;
This dataset includes footprint-level canopy structure products derived from data collected using NASA&amp;#39;s Land, Vegetation, and Ice Sensor (LVIS) during flights over five forested sites in Gabon during February and March 2016. Three types of canopy structure information are included for each flight: 1) vertical profiles of canopy cover fraction in 1-meter bins, 2) vertical profiles of plant area index (PAI) in 1-meter bins, and 3) footprint summary data of total recorded energy, leaf area index, canopy cover fraction, and vertical foliage profiles in 10-meter bins. Canopy structure metrics are provided for each waveform (20-m footprint) collected by the LVIS instrument. These data were collected by NASA as part of the AfriSAR project. AfriSAR is a NASA collaboration with the European Space Agency (ESA), German Aerospace Center (DLR), and the Gabonese Space Agency (AGEOS) that is collecting data useful for deriving forest canopy structure and will help prepare for and calibrate current and upcoming spaceborne missions that aim to gauge the role of forests in Earth&amp;#39;s carbon cycle.
&lt;br&gt;&lt;h4 id&#x3D;&quot;polarimetric_ct_1601&quot;&gt;Polarimetric_CT_1601&lt;/h4&gt;
This dataset contains forest vertical structure and associated uncertainty products derived by applying multi-baseline Polarimetric Interferometric Synthetic Aperture Radar (PolInSAR) and Polarimetric Coherence Tomographic SAR (PCT or PC-TomoSAR) techniques. The data were collected from multiple repeat-pass flights over Gabonese forests using the Uninhabited Aerial Vehicle Synthetic Aperture Radar (UAVSAR) instrument in February-March 2016. In addition, supplementary data products based on various intermediate parameters of the UAVSAR data are provided and include radar backscatter, coherence, and viewing and terrain geometry. These data were collected by NASA as part of the joint NASA/ESA AfriSAR campaign.
&lt;br&gt;&lt;h4 id&#x3D;&quot;afrisar_lvis_biomass_vprofiles_1775&quot;&gt;Afrisar_LVIS_Biomass_VProfiles_1775&lt;/h4&gt;
This dataset contains gridded forest characterization products derived from full-waveform lidar data acquired by NASA&amp;#39;s airborne Land, Vegetation, and Ice Sensor (LVIS) instrument for five forested sites in Gabon, Africa, during the 2016 NASA-ESA AfriSAR campaign. The LVIS lidar instrument was flown over study sites in Lope, Mondah/Akanda, Pongara, Rabi, and Mabouni from February to March 2016. Derived canopy cover, canopy heights, bare ground elevation, plant area index (PAI), and foliage height diversity (FHD), and respective uncertainties are provided at a 25 m resolution for each of the five study sites. Aboveground biomass density (AGBD) and uncertainty were modeled at 50 m and 100 m resolutions for the Lope, Mondah, and Mabounie sites using field inventory data and waveform height and cover metrics. Lidar grid cell data collection statistics (i.e., number of shots and flight lines) and a data mask are also included. This research leverages high-quality forest inventory datasets collected during the AfriSAR campaign for one of the least studied and most unique forest ecosystems in the world.
&lt;br&gt;&lt;h4 id&#x3D;&quot;afrisar_mondah_field_data_1580&quot;&gt;AfriSAR_Mondah_Field_Data_1580&lt;/h4&gt;
This dataset provides plot-level estimates of basal area, aboveground biomass, number of trees, maximum tree height, and basal-area-weighted wood specific gravity that were derived from observations of nearly 6,700 individual trees including tree family, species, DBH, the height of each tree, and their x, y location within 25 x 25 m subplots. These field data were collected from 15 1-hectare plots located across the Mondah Forest of Gabon as part of the AfriSAR Campaign in 2016. These biophysical and biomass data were used for training models to derive the AfriSAR remote sensing-based aboveground biomass products.
&lt;br&gt;&lt;h4 id&#x3D;&quot;polarimetric_height_profile_1577&quot;&gt;Polarimetric_height_profile_1577&lt;/h4&gt;
This dataset provides height profiles derived from UAVSAR (Uninhabited Aerial Vehicle Synthetic Aperture Radar; JPL) data acquired over Lope National Park and Rabi Forest in Gabon as part of the AfriSAR campaign in 2016. These data were produced using synthetic aperture radar tomography (TomoSAR), a method that reveals three-dimensional forest structures by extending the conventional two-dimensional imaging capabilities of radars using multiple images acquired from slightly different antenna positions. AfriSAR was an airborne campaign that collected radar, lidar, and field measurements of forests in Gabon, West Africa, as part of a collaborative mission between NASA, the European Space Agency, and the Gabonese Space Agency. These data will help prepare for and calibrate current and upcoming spaceborne missions that aim to gauge the role of forests in Earth&amp;#39;s carbon cycle, such as the Global Ecosystem Dynamics Investigation (GEDI).
&lt;br&gt;&lt;h4 id&#x3D;&quot;polinsar_canopy_height_1589&quot;&gt;PolInSAR_Canopy_Height_1589&lt;/h4&gt;
This dataset provides estimates of forest canopy height and canopy height uncertainty for study areas in the Pongara National Park and the Lope National Park, Gabon. Two canopy height products are included: 1) Canopy height was derived from multi-baseline Polarimetric Interferometric Synthetic Aperture Radar (PolInSAR) data using an inversion of the random volume over ground (RVoG) model and Kapok, an open source Python library. 2) Canopy height was derived from a fusion of PolInSAR and Land, Vegetation, and Ice Sensor (LVIS) Lidar data. This dataset also includes various intermediate parameters of the PolInSAR data (including radar backscatter, coherence, and viewing and terrain geometry) which provide additional insight into the input data used to invert the RVoG model and accuracy of the canopy height estimates. The AfriSAR campaign was flown from 2016-02-27 to 2016-03-08. AfriSAR data were collected by NASA, in collaboration with the European Space Agency (ESA) and the Gabonese Space Agency.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.nsidc.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA AirMOSS Project</title>
      <link>https://registry.opendata.aws/nasa-airmoss</link>
      <guid>https://registry.opendata.aws/nasa-airmoss</guid>
      <description>This dataset provides in situ measurements of soil temperature, moisture, conductivity, measured diameter of tree at breast height (DBH) and total height collected at the Harvard Forest, Petersham, Massachusetts, USA, during October 2012 and July - August 2013. These measurements were collected in support of the Airborne Microwave Observatory of Subcanopy and Subsurface (AirMOSS) project to validate root-zone soil measurements and carbon flux model estimates.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airmoss_l1_sigma0_berms_1406&quot;&gt;AirMOSS_L1_Sigma0_BERMS_1406&lt;/h4&gt;
This data set provides level 1 (L1) polarimetric radar backscattering coefficient (sigma-0), multilook complex, polarimetrically calibrated, and georeferenced data products from the Airborne Microwave Observatory of Subcanopy and Subsurface (AirMOSS) radar instrument collected over the BERMS (Boreal Ecosystem Research and Monitoring Sites), in Saskatchewan, Canada. The AirMOSS radar is a P-band (UHF) fully polarimetric synthetic aperture radar (SAR) currently operating in the 420-440 MHz band designed to measure root-zone soil moisture (RZSM) and is flown on a NASA Gulfstream-III aircraft. Flight campaigns took place at least biannually from 2012 to 2015 at 10 study sites across North America. The acquired L1 P-band radar backscatter data will be used to retrieve the RZSM at the study sites. Subsequent analyses will investigate both seasonal and inter-annual variability in soil moisture and the relationships to carbon fluxes and their associated uncertainties on a continental scale.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airmoss_l1_sigma0_chamel_1407&quot;&gt;AirMOSS_L1_Sigma0_Chamel_1407&lt;/h4&gt;
This data set provides level 1 (L1) polarimetric radar backscattering coefficient (sigma-0), multilook complex, polarimetrically calibrated, and georeferenced data products from the Airborne Microwave Observatory of Subcanopy and Subsurface (AirMOSS) radar instrument collected over the Chamela Biological Station, in Jalisco, Mexico. The AirMOSS radar is a P-band (UHF) fully polarimetric synthetic aperture radar (SAR) currently operating in the 420-440 MHz band designed to measure root-zone soil moisture (RZSM) and is flown on a NASA Gulfstream-III aircraft. Flight campaigns took place at least biannually from 2012 to 2015 at 10 study sites across North America. The acquired L1 P-band radar backscatter data will be used to retrieve the RZSM at the study sites. Subsequent analyses will investigate both seasonal and inter-annual variability in soil moisture and the relationships to carbon fluxes and their associated uncertainties on a continental scale.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airmoss_l1_sigma0_dukefr_1408&quot;&gt;AirMOSS_L1_Sigma0_DukeFr_1408&lt;/h4&gt;
This data set provides level 1 (L1) polarimetric radar backscattering coefficient (sigma-0), multilook complex, polarimetrically calibrated, and georeferenced data products from the Airborne Microwave Observatory of Subcanopy and Subsurface (AirMOSS) radar instrument collected over the Duke Forest site in North Carolina. The AirMOSS radar is a P-band (UHF) fully polarimetric synthetic aperture radar (SAR) currently operating in the 420-440 MHz band designed to measure root-zone soil moisture (RZSM) and is flown on a NASA Gulfstream-III aircraft. Flight campaigns took place at least biannually from 2012 to 2015 at 10 study sites across North America. The acquired L1 P-band radar backscatter data will be used to retrieve the RZSM at the study sites. Subsequent analyses will investigate both seasonal and inter-annual variability in soil moisture and the relationships to carbon fluxes and their associated uncertainties on a continental scale.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airmoss_l1_sigma0_harvrd_1409&quot;&gt;AirMOSS_L1_Sigma0_Harvrd_1409&lt;/h4&gt;
This data set provides level 1 (L1) polarimetric radar backscattering coefficient (sigma-0), multilook complex, polarimetrically calibrated, and georeferenced data products from the Airborne Microwave Observatory of Subcanopy and Subsurface (AirMOSS) radar instrument collected over the Harvard Forest site in Massachusetts. The AirMOSS radar is a P-band (UHF) fully polarimetric synthetic aperture radar (SAR) currently operating in the 420-440 MHz band designed to measure root-zone soil moisture (RZSM) and is flown on a NASA Gulfstream-III aircraft. Flight campaigns took place at least biannually from 2012 to 2015 at 10 study sites across North America. The acquired L1 P-band radar backscatter data will be used to retrieve the RZSM at the study sites. Subsequent analyses will investigate both seasonal and inter-annual variability in soil moisture and the relationships to carbon fluxes and their associated uncertainties on a continental scale.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airmoss_l1_sigma0_howlnd_1410&quot;&gt;AirMOSS_L1_Sigma0_Howlnd_1410&lt;/h4&gt;
This data set provides level 1 (L1) polarimetric radar backscattering coefficient (sigma-0), multilook complex, polarimetrically calibrated, and georeferenced data products from the Airborne Microwave Observatory of Subcanopy and Subsurface (AirMOSS) radar instrument collected over the Howland Forest site in Maine. The AirMOSS radar is a P-band (UHF) fully polarimetric synthetic aperture radar (SAR) currently operating in the 420-440 MHz band designed to measure root-zone soil moisture (RZSM) and is flown on a NASA Gulfstream-III aircraft. Flight campaigns took place at least biannually from 2012 to 2015 at 10 study sites across North America. The acquired L1 P-band radar backscatter data will be used to retrieve the RZSM at the study sites. Subsequent analyses will investigate both seasonal and inter-annual variability in soil moisture and the relationships to carbon fluxes and their associated uncertainties on a continental scale.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airmoss_l1_sigma0_laselv_1411&quot;&gt;AirMOSS_L1_Sigma0_LaSelv_1411&lt;/h4&gt;
This data set provides level 1 (L1) polarimetric radar backscattering coefficient (sigma-0), multilook complex, polarimetrically calibrated, and georeferenced data products from the Airborne Microwave Observatory of Subcanopy and Subsurface (AirMOSS) radar instrument collected over the La Selva Biological Station in Costa Rica. The AirMOSS radar is a P-band (UHF) fully polarimetric synthetic aperture radar (SAR) currently operating in the 420-440 MHz band designed to measure root-zone soil moisture (RZSM) and is flown on a NASA Gulfstream-III aircraft. Flight campaigns took place at least biannually from 2012 to 2015 at 10 study sites across North America. The acquired L1 P-band radar backscatter data will be used to retrieve the RZSM at the study sites. Subsequent analyses will investigate both seasonal and inter-annual variability in soil moisture and the relationships to carbon fluxes and their associated uncertainties on a continental scale.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airmoss_l1_sigma0_metoli_1412&quot;&gt;AirMOSS_L1_Sigma0_Metoli_1412&lt;/h4&gt;
This data set provides level 1 (L1) polarimetric radar backscattering coefficient (sigma-0), multilook complex, polarimetrically calibrated, and georeferenced data products from the Airborne Microwave Observatory of Subcanopy and Subsurface (AirMOSS) radar instrument collected over the Metolius site in Oregon. The AirMOSS radar is a P-band (UHF) fully polarimetric synthetic aperture radar (SAR) currently operating in the 420-440 MHz band designed to measure root-zone soil moisture (RZSM) and is flown on a NASA Gulfstream-III aircraft. Flight campaigns took place at least biannually from 2012 to 2015 at 10 study sites across North America. The acquired L1 P-band radar backscatter data will be used to retrieve the RZSM at the study sites. Subsequent analyses will investigate both seasonal and inter-annual variability in soil moisture and the relationships to carbon fluxes and their associated uncertainties on a continental scale.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airmoss_l1_sigma0_moisst_1413&quot;&gt;AirMOSS_L1_Sigma0_Moisst_1413&lt;/h4&gt;
This data set provides level 1 (L1) polarimetric radar backscattering coefficient (sigma-0), multilook complex, polarimetrically calibrated, and georeferenced data products from the Airborne Microwave Observatory of Subcanopy and Subsurface (AirMOSS) radar instrument collected over the MOISST site in Oklahoma. The AirMOSS radar is a P-band (UHF) fully polarimetric synthetic aperture radar (SAR) currently operating in the 420-440 MHz band designed to measure root-zone soil moisture (RZSM) and is flown on a NASA Gulfstream-III aircraft. Flight campaigns took place at least biannually from 2012 to 2015 at 10 study sites across North America. The acquired L1 P-band radar backscatter data will be used to retrieve the RZSM at the study sites. Subsequent analyses will investigate both seasonal and inter-annual variability in soil moisture and the relationships to carbon fluxes and their associated uncertainties on a continental scale.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airmoss_l1_sigma0_tonzir_1414&quot;&gt;AirMOSS_L1_Sigma0_TonziR_1414&lt;/h4&gt;
This data set provides level 1 (L1) polarimetric radar backscattering coefficient (sigma-0), multilook complex, polarimetrically calibrated, and georeferenced data products from the Airborne Microwave Observatory of Subcanopy and Subsurface (AirMOSS) radar instrument collected over the Tonzi Ranch site in California. The AirMOSS radar is a P-band (UHF) fully polarimetric synthetic aperture radar (SAR) currently operating in the 420-440 MHz band designed to measure root-zone soil moisture (RZSM) and is flown on a NASA Gulfstream-III aircraft. Flight campaigns took place at least biannually from 2012 to 2015 at 10 study sites across North America. The acquired L1 P-band radar backscatter data will be used to retrieve the RZSM at the study sites. Subsequent analyses will investigate both seasonal and inter-annual variability in soil moisture and the relationships to carbon fluxes and their associated uncertainties on a continental scale.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airmoss_l1_sigma0_walnut_1415&quot;&gt;AirMOSS_L1_Sigma0_Walnut_1415&lt;/h4&gt;
This data set provides level 1 (L1) polarimetric radar backscattering coefficient (sigma-0), multilook complex, polarimetrically calibrated, and georeferenced data products from the Airborne Microwave Observatory of Subcanopy and Subsurface (AirMOSS) radar instrument collected over the Walnut Gulch site in Arizona. The AirMOSS radar is a P-band (UHF) fully polarimetric synthetic aperture radar (SAR) currently operating in the 420-440 MHz band designed to measure root-zone soil moisture (RZSM) and is flown on a NASA Gulfstream-III aircraft. Flight campaigns took place at least biannually from 2012 to 2015 at 10 study sites across North America. The acquired L1 P-band radar backscatter data will be used to retrieve the RZSM at the study sites. Subsequent analyses will investigate both seasonal and inter-annual variability in soil moisture and the relationships to carbon fluxes and their associated uncertainties on a continental scale.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airmoss_l2_carbon_flux_1420&quot;&gt;AirMOSS_L2_Carbon_Flux_1420&lt;/h4&gt;
This data set contains carbon flux measurements recorded by an aircraft at the Duke, Harvard, and Howland Forest sites during the summers of 2012-2014 as part of the Airborne Microwave Observatory of Subcanopy and Subsurface (AirMOSS) project. Frequent measurements of CO2 and H2O were obtained using a cavity ring down spectrometer on board the Airborne Laboratory for Atmospheric Research, operated by Purdue University. Estimates of surface CO2 flux, sensible and latent heat fluxes, their corresponding uncertainties, and average wind speed and direction are provided for each of the 26 flights.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airmoss_l2_inground_soil_moist_1416&quot;&gt;AirMOSS_L2_Inground_Soil_Moist_1416&lt;/h4&gt;
This data set provides level 2 (L2) hourly volumetric (cm3/cm3) soil moisture profiles from in-ground sensors at seven North American sites as part of the Airborne Microwave Observatory of Subcanopy and Subsurface (AirMOSS) project. Three profiles were installed at each site, sampling at seven different depths per profile (2 cm to 80 cm). Initial sampling began at three sites in September 2011 and additional sites were added during 2012 and 2013. All sampling concluded in December 2015. The AirMOSS project used an airborne radar instrument to estimate root-zone soil moisture at 10 study sites across North America. These in-ground soil moisture data were collected to calibrate and validate the AirMOSS data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airmoss_l2_precipitation_1417&quot;&gt;AirMOSS_L2_Precipitation_1417&lt;/h4&gt;
This data set provides level 2 (L2) calibrated hourly precipitation (cm/hr) from rain gauges at seven North American sites as part of the Airborne Microwave Observatory of Subcanopy and Subsurface (AirMOSS) project. Three gauges were installed at each site. Initial sampling began at three sites in September 2011 and additional sites were added during 2012 and 2013. All sampling concluded in December 2015. The AirMOSS project used an airborne radar instrument to estimate root-zone soil moisture at 10 study sites across North America. These precipitation data were collected in conjunction with in-ground soil moisture data in order to calibrate and validate the AirMOSS data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airmoss_l2_3_rz_soil_moisture_1418&quot;&gt;AirMOSS_L2_3_RZ_Soil_Moisture_1418&lt;/h4&gt;
This data set provides level 2/3 root zone soil moisture (RZSM) estimates at multiple depths at 90-m spatial resolution from the Airborne Microwave Observatory of Subcanopy and Subsurface (AirMOSS) radar instrument collected over ten sites across North America. AirMOSS produces estimates of RZSM with data from a P-band synthetic aperture radar (SAR) flown on a NASA Gulfstream-III aircraft. The resulting soil moisture estimates capture the effects of gradients of soil, topography, and vegetation heterogeneity over an area of approximately 100km x 25km at each of the study sites. AirMOSS flight campaigns took place at least biannually from 2012 to 2015 at each site.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airmoss_l4_daily_nee_1422&quot;&gt;AirMOSS_L4_Daily_NEE_1422&lt;/h4&gt;
This data set provides Level 4 daily estimates of Net Ecosystem Exchange (NEE) of CO2 at a spatial resolution of 30 arc-seconds (~1 km) for seven of the sites covered by the Airborne Microwave Observatory of Subcanopy and Subsurface (AirMOSS) flights, each site spanning ~2500 km2. The daily NEE estimates are generally available from October 2012 through October 2014, although the exact time ranges vary by site. The AirMOSS L4 daily NEE were produced by the Ecosystem Demography Biosphere Model (ED2) augmented by the AirMOSS-derived L2/3 root zone soil moisture data as an additional input. The AirMOSS soil moisture data were used to estimate the sensitivity of carbon fluxes to soil moisture and to diagnose and improve estimation and prediction of NEE by constraining the model&amp;#39;s predictions of soil moisture and its impact on above- and below-ground fluxes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airmoss_l4_regional_nee_1423&quot;&gt;AirMOSS_L4_Regional_NEE_1423&lt;/h4&gt;
This data set provides Level 4 estimates of Net Ecosystem Exchange (NEE) of CO2 across the conterminous USA at a spatial resolution of 50 km. Modeled estimates are provided at hourly and monthly temporal resolutions, from January 2012 through October 2014. The AirMOSS L4 Regional NEE data were produced by the Ecosystem Demography Biosphere Model (ED2) augmented by the AirMOSS-derived L2/3 root zone soil moisture data as an additional input. The AirMOSS soil moisture data were used to estimate the sensitivity of carbon fluxes to soil moisture and to diagnose and improve estimation and prediction of NEE by constraining the model&amp;#39;s predictions of soil moisture and its impact on above- and below-ground fluxes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airmoss_l4_rz_soil_moisture_1421&quot;&gt;AirMOSS_L4_RZ_Soil_Moisture_1421&lt;/h4&gt;
This data set provides hourly gridded soil moisture estimates derived from hydrologic modeling at nine AirMOSS sites across North America. The AirMOSS L4 RZSM product represents a temporal interpolation of intermittent AirMOSS L2/3 RZSM retrievals into a temporally-continuous, multi-layer, hourly soil moisture product. The L4 RZSM data have the same spatial resolution (3-arcsecs or ~100 m), and the same temporal coverage (generally Fall 2012 through Fall 2015), as the underlying L2/3 RZSM data. The L4 RZSM data were produced by the integration of the Level 2/3 product and other ancillary information into the Penn State Integrated Hydrologic Model (PIHM). Many key applications for AirMOSS data products, including the calculation of net ecosystem exchange (NEE), require temporally continuous RZSM estimates such as those provided here.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.ornldaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA Applications Technology Satellite Project</title>
      <link>https://registry.opendata.aws/nasa-applications-technology-satellite</link>
      <guid>https://registry.opendata.aws/nasa-applications-technology-satellite</guid>
      <description>GVHRRATS6IMIR is the Geosynchronous Very High Resolution Radiometer (GVHRR) Black and White Infrared Images on 70mm Film data product from the sixth Applications Technology Satellite (ATS-6). This set of IR imagery (10.5 to 12.5 micrometer, with an 11 km footprint at the sub-satellite point) was originally produced on commercial image-generation equipment from digital tapes and was made available on 70-mm film, from which they were later scanned to digital TIFF image files. Each TIFF scan contains 2 or 3 pictures, and there are several hundred scans from an original 70 mm film roll which are combined into a ZIP file. Each picture contains a title at the bottom of the image and a gray scale on the right boundary that represents brightness temperatures. The title contains the satellite identification, receiving station, spectral band, picture number, picture type, pixel scale, sector number, and date. The ATS-6 satellite was in a geosynchronous orbit parked at 95W viewing the hemisphere below the satellite. The GVHRR experiment returned data from launch until August 15, 1974 when it became inoperable, The PI was William E. Shenk from NASA Goddard Space Flight Center. This product was previously available from the NSSDC with the identifier ESAD-00092 (old ID 74-039A-08B).
&lt;br&gt;&lt;h4 id&#x3D;&quot;gvhrrats6imvis&quot;&gt;GVHRRATS6IMVIS&lt;/h4&gt;
GVHRRATS6IMVIS is the Geosynchronous Very High Resolution Radiometer (GVHRR) Black and White Visible Images on Film data product from the sixth Applications Technology Satellite (ATS-6). This set of visible imagery (0.55 to 0.75 micrometer, with a 5.5 km footprint at the sub-satellite point) was originally produced on commercial image-generation equipment from digital tapes and was made available on 70-mm film, from which they were later scanned to digital TIFF image files. Each TIFF scan contains 2 or 3 pictures, and there are several hundred scans from an original 70 mm film roll which are combined into a ZIP file. Each picture contains a title at the bottom of the image and a gray scale on the right boundary that represents brightness temperatures. The title contains the satellite identification, receiving station, spectral band, picture number, picture type, pixel scale, sector number, and date. The ATS-6 satellite was in a geosynchronous orbit parked at 95W viewing the hemisphere below the satellite. The GVHRR experiment returned data from launch until August 15, 1974 when it became inoperable, The PI was William E. Shenk from NASA Goddard Space Flight Center. This product was previously available from the NSSDC with the identifier ESAD-00047 (old ID 74-039A-08A).
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA Aqua Project</title>
      <link>https://registry.opendata.aws/nasa-aqua</link>
      <guid>https://registry.opendata.aws/nasa-aqua</guid>
      <description>AIRS is a facility instrument whose goal is to support climate research and improve weather forecasting Launched into Earth-orbit on May 4, 2002, the Atmospheric Infrared Sounder, AIRS, moves climate research and weather prediction into the 21st century.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airxamap&quot;&gt;AIRXAMAP&lt;/h4&gt;
The Atmospheric Infrared Sounder (AIRS) is a grating spectrometer (R &#x3D; 1200) aboard the second Earth Observing System (EOS) polar-orbiting platform, EOS Aqua. In combination with the Advanced Microwave Sounding Unit (AMSU) and the Humidity Sounder for Brazil (HSB), AIRS constitutes an innovative atmospheric sounding group of visible, infrared, and microwave sensors. An AIRS granule has been set as 6 minutes of data, 30 footprints cross track by 45 lines along track. The AIRS Granule Map Product consists of images of granule coverage in PDF and JPG format. The images are daily ones but updated every 6 minutes to capture any new available granule. Granules are assembled by ascending, descending, in north and south hemisphere, and the maps are in global cylindrical projection and satellite projection for better view.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airibrad&quot;&gt;AIRIBRAD&lt;/h4&gt;
WARNING: On 2021/09/23 the EOS Aqua executed a Deep Space Maneuver (DSM). In the DSM, the spacecraft is turned such that the normal Earth field of regard is deep space. The thermal impact of the DSM caused a shift of the centroids of spectral response functions (SRF) of about 1% of the width of the SRF, equivalent to a frequency shift of 9 parts per million. This shift is reflected in the “spectral_freq” parameter (observed frequencies) in the L1b v5 files for each 6 minute granule. The magnitude of the effect on brightness temperatures (BT) depends on the spectral gradient of each channel. Maximum BT shifts are approximately +- 0.5 K, although many channels experience far smaller BT shifts. Approximately 1803 channels have BT shifts of less than 0.1 K and 575 channels are now shifted in BT by more than 0.1 K, while 231 of these channels have BT shifts greater than 0.2 K. Users of the L1b v5 product who are concerned that these shifts may impact their science investigations and applications are encouraged to switch to the AIRS L1c v6.7.4 product, which, among many other improvements, converts the spectra to a fixed frequency grid. END OF WARNING. The Atmospheric Infrared Sounder (AIRS) is a grating spectrometer (R &#x3D; 1200) aboard the second Earth Observing System (EOS) polar-orbiting platform, EOS Aqua. In combination with the Advanced Microwave Sounding Unit (AMSU) and the Humidity Sounder for Brazil (HSB), AIRS constitutes an innovative atmospheric sounding group of visible, infrared, and microwave sensors. The AIRS Infrared (IR) level 1B data set contains AIRS calibrated and geolocated radiances in milliWatts/m^2/cm^-1/steradian for 2378 infrared channels in the 3.74 to 15.4 micron region of t he spectrum. The AIRS instrument is co-aligned with AMSU-A so that successive blocks of 3 x 3 AIRS footprints are contained within one AMSU-A footprint. The AIRIBRAD_005 products are stored in files (often referred to as &amp;quot;granules&amp;quot;) that contain 6 minutes of data, 90 footprints across track by 135 lines along track.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airabrad_nrt&quot;&gt;AIRABRAD_NRT&lt;/h4&gt;
The AMSU-A Level 1B Near Real Time (NRT) product (AIRABRAD_NRT_005) differs from the routine product (AIRABRAD_005) in 2 ways to meet the three hour latency requirements of the Land Atmosphere NRT Capability Earth Observing System (LANCE): (1) The NRT granules are produced without previous or subsequent granules if those granules are not available within 5 minutes, (2) the predictive ephemeris/attitude data are used rather than the definitive ephemeris/attitude. The consequences of these differences are described in the AIRS Near Real Time (NRT) data products document. The Atmospheric Infrared Sounder (AIRS) is a grating spectrometer (R &#x3D; 1200) aboard the second Earth Observing System (EOS) polar-orbiting platform, EOS Aqua. In combination with the Advanced Microwave Sounding Unit (AMSU) and the Humidity Sounder for Brazil (HSB), AIRS constitutes an innovative atmospheric sounding group of visible, infrared, and microwave sensors. The AMSU-A instrument is co-aligned with AIRS so that successive blocks of 3 x 3 AIRS footprints are contained within one AMSU-A footprint. AMSU-A is primarily a temperature sounder that provides atmospheric information in the presence of clouds, which can be used to correct the AIRS infrared measurements for the effects of clouds. This is possible because non-precipitating clouds are for the most part transparent to microwave radiation, in contrast to visible and infrared radiation which are strongly scattered and absorbed by clouds. AMSU-A1 has 13 channels from 50 - 90 GHz and AMSU-A2 has 2 channels from 23 - 32 GHz. The AIRABRAD_NRT_005 products are stored in files (often referred to as &amp;quot;granules&amp;quot;) that contain 6 minutes of data, 30 footprints across track by 45 lines along track.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airibqap_nrt&quot;&gt;AIRIBQAP_NRT&lt;/h4&gt;
The AIRS Level 1B Near Real Time (NRT) product (AIRIBQAP_NRT_005) differs from the routine product (AIRIBQAP_005) in 2 ways to meet the three hour latency requirements of the Land Atmosphere NRT Capability Earth Observing System (LANCE): (1) The NRT granules are produced without previous or subsequent granules if those granules are not available within 5 minutes, (2) the predictive ephemeris/attitude data are used rather than the definitive ephemeris/attitude. The consequences of these differences are described in the AIRS Near Real Time (NRT) data products document. The Atmospheric Infrared Sounder (AIRS) is a facility instrument aboard the second Earth Observing System (EOS) polar-orbiting platform, EOS Aqua. In combination with the Advanced Microwave Sounding Unit (AMSU) and the Humidity Sounder for Brazil Humidity Sounder for Brazil (HSB), AIRS constitutes an innovative atmospheric sounding group of visible, infrared, and microwave sensors. AIRS data will be generated continuously. Global coverage will be obtained twice daily (day and night) on a 1:30pm sun synchronous orbit from a 705-km altitude. The AIRS IR Level 1B QA Subset contains Quality Assurance (QA) parameters that a user of may use to filter AIRS IR Level 1B radiance data to create a subset of analysis. QA parameters indicate quality of granule-per-channel, scan-per-channel, field of view, and channel and should be accessed before any data of analysis. It also contains &amp;quot;glintlat&amp;quot;, &amp;quot;glintlon&amp;quot;, and &amp;quot;sun_glint_distant&amp;quot; that users can use to check for possibility of solar glint contamination.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airvbrad_nrt&quot;&gt;AIRVBRAD_NRT&lt;/h4&gt;
The AIRS Visible/Near Infrared (VIS/NIR) Level 1B Near Real Time (NRT) product (AIRVBRAD_NRT_005) differs from the routine product (AIRVBRAD_005) in 2 ways to meet the three hour latency requirements of the Land Atmosphere NRT Capability Earth Observing System (LANCE): (1) The NRT granules are produced without previous or subsequent granules if those granules are not available within 5 minutes, (2) the predictive ephemeris/attitude data are used rather than the definitive ephemeris/attitude. The consequences of these differences are described in the AIRS Near Real Time (NRT) data products document. The AIRS VIS/NIR level 1B data set contains visible and near-infrared calibrated and geolocated radiances in W/m^2/micron/steradian for 4 channels in the 0.4 to 1.0 um region of the spectrum. The spectral range of the VIS/NIR channels are as follows: Channel 1 0.41 um - 0.44 um, Channel 2 0.58 um - 0.68 um, Channel 3 0.71 um - 0.92 um, Channel 4 0.49 um - 0.94 um. The AIRVBRAD_NRT_005 products are stored in files (often referred to as &amp;quot;granules&amp;quot;) that contain 6 minutes of data, 90 footprints across track by 135 lines along track. The VIS/NIR granules are only produced in the daytime so there will always be fewer VIS/NIR granules than Infrared or microwave granules.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airvbqap_nrt&quot;&gt;AIRVBQAP_NRT&lt;/h4&gt;
The AIRS Level 1B Near Real Time (NRT) product (AIRVBQAP_NRT_005) differs from the routine product (AIRVBQAP_005) in 2 ways to meet the three hour latency requirements of the Land Atmosphere NRT Capability Earth Observing System (LANCE): (1) The NRT granules are produced without previous or subsequent granules if those granules are not available within 5 minutes, (2) the predictive ephemeris/attitude data are used rather than the definitive ephemeris/attitude. The consequences of these differences are described in the AIRS Near Real Time (NRT) data products document. The Atmospheric Infrared Sounder (AIRS) Visible/Near Infrared (VIS/NIR) instrument in combination with the AIRS Infrared Spectrometer, the Advanced Microwave Sounding Unit (AMSU) and the Humidity Sounder for Brazil (HSB) constitute an innovative atmospheric sounding group aboard the Earth Observing System (EOS) Aqua platform in a near-polar Sun-synchronous orbit with a 1:30 AM/PM equator crossing time and an ~705 km altitude. The AIRS Visible/Near Infrared (VIS/NIR) Level 1B QA Subset contains Quality Assurance (QA) parameters that a may use of filter AIRS VIS/NIR Level 1B radiance data to create a subset of analysis. It includes &amp;quot;state&amp;quot; that user should check before using any VIS/NIR Level 1B data radiance and &amp;quot;glintlat&amp;quot;, &amp;quot;glintlon&amp;quot;, and &amp;quot;sun_glint_distant&amp;quot; that users can use to check for possibility of solar glint contamination. AIRS VIS/NIR Level 1B radiance data can be found in AIRVBRAD.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airs2ccf_nrt&quot;&gt;AIRS2CCF_NRT&lt;/h4&gt;
The Atmospheric Infrared Sounder (AIRS) Level 2 Near Real Time (NRT) Cloud-Cleared Infrared Radiances (AIRS-only) product (AIRS2CCF_NRT_006) differs from the routine product (AIRS2CCF_006) in four ways to meet the three hour latency requirements of the Land Atmosphere NRT Capability Earth Observing System (LANCE): (1) The NRT granules are produced without previous or subsequent granules if those granules are not available within 5 minutes, (2) the predictive ephemeris/attitude data are used rather than the definitive ephemeris/attitude, (3) if the forecast surface pressure is unavailable, a surface climatology is used, and (4) no ice cloud properties retrievals are performed. The consequences of these differences are described in the AIRS Near Real Time (NRT) data products document. The Atmospheric Infrared Sounder (AIRS) is a grating spectrometer (R &#x3D; 1200) aboard the second Earth Observing System (EOS) polar-orbiting platform, EOS Aqua. In combination with the Advanced Microwave Sounding Unit (AMSU) and the Humidity Sounder for Brazil (HSB), AIRS constitutes an innovative atmospheric sounding group of visible, infrared, and microwave sensors. This product is produced using AIRS IR only because the radiometric noise in AMSU channel 4 started to increase significantly (since June 2007). Cloud-Cleared Radiances contain calibrated, geolocated channel-by-channel AIRS infrared radiances (milliWatts/m2/cm-1/steradian) that would have been observed within each AMSU footprint if there were no clouds in the FOV and produced along with the AIRS Standard Product, as they are the radiances used to retrieve the Standard Product. Nevertheless, they are an order of magnitude larger in data volume than the remainder of the Standard Products and, many Standard Product users are expected to have little interest in the Cloud Cleared Radiance. For these reasons they are a separate output file. The AIRS2CCF_NRT_006 products are stored in files (often referred to as &amp;quot;granules&amp;quot;) that contain 6 minutes of data, 30 footprints across track by 45 lines along track.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airs2ret_nrt&quot;&gt;AIRS2RET_NRT&lt;/h4&gt;
The Atmospheric Infrared Sounder (AIRS) Level 2 Near Real Time (NRT) Standard Physical Retrieval (AIRS-only) product (AIRS2RET_NRT_006) differs from the routine product (AIRS2RET_006) in four ways to meet the three hour latency requirements of the Land Atmosphere NRT Capability Earth Observing System (LANCE): (1) The NRT granules are produced without previous or subsequent granules if those granules are not available within 5 minutes, (2) the predictive ephemeris/attitude data are used rather than the definitive ephemeris/attitude, (3) if the forecast surface pressure is unavailable, a surface climatology is used, and (4) no ice cloud properties retrievals are performed. The consequences of these differences are described in the AIRS Near Real Time (NRT) data products document. The Atmospheric Infrared Sounder (AIRS) is a grating spectrometer (R &#x3D; 1200) aboard the second Earth Observing System (EOS) polar-orbiting platform, EOS Aqua. In combination with the Advanced Microwave Sounding Unit (AMSU) and the Humidity Sounder for Brazil (HSB), AIRS constitutes an innovative atmospheric sounding group of visible, infrared, and microwave sensors. This product is produced using AIRS IR only because the radiometric noise in AMSU channel 4 started to increase significantly (since June 2007). The AIRS Standard Retrieval Product consists of retrieved estimates of cloud and surface properties, plus profiles of retrieved temperature, water vapor, ozone, carbon monoxide and methane. Estimates of the errors associated with these quantities is also part of the Standard Product. The temperature profile vertical resolution is 28 levels total between 1100 mb and 0.1 mb, while moisture profile is reported at 14 atmospheric layers between 1100 mb and 50 mb. The horizontal resolution is 50 km. An AIRS granule has been set as 6 minutes of data, 30 footprints cross track by 45 lines along track. There are 240 granules per day, with an orbit repeat cycle of approximately 16 day.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airs2sup_nrt&quot;&gt;AIRS2SUP_NRT&lt;/h4&gt;
The Atmospheric Infrared Sounder (AIRS) Level 2 Near Real Time (NRT) Support Retrieval (AIRS-only) product (AIRS2SUP_NRT_006) differs from the routine product (AIRS2SUP_006) in four ways to meet the three hour latency requirements of the Land Atmosphere NRT Capability Earth Observing System (LANCE): (1) The NRT granules are produced without previous or subsequent granules if those granules are not available within 5 minutes, (2) the predictive ephemeris/attitude data are used rather than the definitive ephemeris/attitude, (3) if the forecast surface pressure is unavailable, a surface climatology is used, and (4) no ice cloud properties retrievals are performed. The consequences of these differences are described in the AIRS Near Real Time (NRT) data products document. The Atmospheric Infrared Sounder (AIRS) is a grating spectrometer (R &#x3D; 1200) aboard the second Earth Observing System (EOS) polar-orbiting platform, EOS Aqua. In combination with the Advanced Microwave Sounding Unit (AMSU) and the Humidity Sounder for Brazil (HSB), AIRS constitutes an innovative atmospheric sounding group of visible, infrared, and microwave sensors. This product is product produced using AIRS IR only because the radiometric noise in AMSU channel 4 started to increase significantly (since June 2007). The Support Product includes higher vertical resolution profiles of the quantities found in the Standard Product, plus intermediate outputs (e.g., microwave-only retrieval), research products such as the abundance of trace gases, and detailed quality assessment information. The Support Product profiles contain 100 levels between 1100 and .016 mb; this higher resolution simplifies the generation of radiances using forward models, though the vertical information content is no greater than that in the Standard Product profiles. The intended users of the Support Product are researchers interested in generating forward radiance or in examining research products, and the AIRS algorithm development team. The Support Product is generated at all locations as Standard Products. An AIRS granule has been set as 6 minutes of data, 30 footprints cross track by 45 scanlines. There are 240 granules per day, with an orbit repeat cycle of approximately 16 day.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airg2ssd_ironly&quot;&gt;AIRG2SSD_IRonly&lt;/h4&gt;
The Atmospheric Infrared Sounder (AIRS) is a grating spectrometer (R &#x3D; 1200) aboard the second Earth Observing System (EOS) polar-orbiting platform, EOS Aqua. This precipitation estimate from AIRS IR only is using a TOVS-like algorithm, and is intended for merging into the precipitation product of the Global Precipitation Climatology Project (GPCP). The precipitation estimate from AIRS Level 2 Support product, which are 6-min swath granules (240 per day) are combined here into one daily &amp;quot;Level 2G&amp;quot; global grid with dimensions (24x1440x720). Thus every hour is a &amp;quot;layer&amp;quot;, and the resulting grid cell size is 0.25 degree (~25 km). Thus the grid size is made to fit TRMM products. Since AIRS precipitation is retrieved at AMSU footprint resolution, which is about 45 km at nadir, many grid cells in this 0.25-deg grid are &amp;quot;empty&amp;quot;. The data are stored such that the first line is the South Pole. The geolocation information for every hour-layer is also provided in the file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airx3c28&quot;&gt;AIRX3C28&lt;/h4&gt;
Atmospheric Infrared Sounder (AIRS) is a grating spectrometer (R &#x3D; 1200) aboard the second Earth Observing System (EOS) polar-orbiting platform, EOS Aqua. In combination with the Advanced Microwave Sounding Unit (AMSU) and the Humidity Sounder for Brazil (HSB), AIRS constitutes an innovative atmospheric sounding group of visible, infrared, and microwave sensors. This product is the AIRS mid-tropospheric Carbon Dioxide (CO2) Level 3 8-day Gridded Retrieval, from the AIRS and AMSU instruments on board of Aqua satellite. It is 8-day gridded data, at 2.5x2 deg (lon)x(lat) grid cell size. The data is in mole fraction units (data x 10^6 &#x3D;ppm in volume). This is a total tropospheric column property. The file format is HDF-EOS 2.12 corresponding to HDF4. This AIRS mid-tropospheric CO2 Level 3, 8-day, Gridded Retrieval Product contains standard retrieval means, standard deviations and input counts as well as the latitude and longitude arrays giving the centers of the grid boxes. Each file covers an 8-day period. The mean values are simply the arithmetic means of the individual CO2 retrievals which fall within that grid box over the 8-day period. The mid-tropospheric CO2 retrievals have been averaged and binned into 2.5 x 2 deg grid cells, from -180.0 to +180.0 deg longitude and from -60.0 to +90.0 deg latitude. For each grid map of 4-byte floating-point mean values there is a corresponding 4-byte floating-point map of standard deviation and a 2-byte integer grid map of counts. The counts map provides the user with the number of points per bin that were included in the mean.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lprm_amsre_soilm2&quot;&gt;LPRM_AMSRE_SOILM2&lt;/h4&gt;
AMSR-E/Aqua surface soil moisture (LPRM) L2B V002 is a Level 2 (swath) data set. Its land surface parameters, surface soil moisture, land surface (skin) temperature, and vegetation water content are derived from passive microwave remote sensing data from the Advanced Microwave Scanning Radiometer-Earth Observing System (AMSR-E), using the Land Parameter Retrieval Model (LPRM). Each swath is packaged with associated geolocation fields. The data set covers the period from June 2002 to October 2011 (when the AMSR-E on the NASA EOS Aqua satellite stopped producing data due to a problem with the rotation of its antenna), at the spatial resolution (nominally 56 and 38 km, respectively) of AMSR-E&amp;#39;s C and X bands (6.9 and 10.7 GHz, respectively). The LPRM is based on a forward radiative transfer model to retrieve surface soil moisture and vegetation optical depth. The land surface temperature is derived separately from the AMSR-E&amp;#39;s Ka-band (36.5 GHz). A unique feature of this method is that it can be applied at any microwave frequency, making it very suitable to exploit all the available passive microwave data from various satellites. Input data are from the AMSR-E resampled brightness temperatures (AE_L2A) product, archived at the National Snow and Ice Data Center (NSIDC).
&lt;br&gt;&lt;h4 id&#x3D;&quot;lprm_amsre_a_soilm3&quot;&gt;LPRM_AMSRE_A_SOILM3&lt;/h4&gt;
AMSR-E/Aqua surface soil moisture (LPRM) L3 1 day 25 km x 25 km ascending V002 is a Level 3 (gridded) data set. Its land surface parameters, surface soil moisture, land surface (skin) temperature, and vegetation water content, are derived from passive microwave remote sensing data from the Advanced Microwave Scanning Radiometer-Earth Observing System (AMSR-E), using the Land Parameter Retrieval Model (LPRM). There are two files per day, one ascending (daytime) and one descending (nighttime), archived as two different products. This document is for the daytime product. The data set covers the period from June 2002 to October 2011 (when the AMSR-E on the NASA EOS Aqua satellite stopped producing data due to a problem with the rotation of its antenna). The LPRM is based on a forward radiative transfer model to retrieve surface soil moisture and vegetation optical depth. The land surface temperature is derived separately from the AMSR-E&amp;#39;s Ka-band (36.5 GHz). A unique feature of this method is that it can be applied at any microwave frequency, making it very suitable to exploit all the available passive microwave data from various satellites. Input data are from the AMSR-E resampled brightness temperatures (AE_L2A) product, daytime passes, as processed using LPRM (i.e., LPRM/AMSR-E/Aqua L2B product, LPRM_AMSRE_SOILM2_V002).
&lt;br&gt;&lt;h4 id&#x3D;&quot;lprm_amsre_d_soilm3&quot;&gt;LPRM_AMSRE_D_SOILM3&lt;/h4&gt;
AMSR-E/Aqua surface soil moisture (LPRM) L3 1 day 25 km x 25 km descending V002 is a Level 3 (gridded) data set. Its land surface parameters, surface soil moisture, land surface (skin) temperature, and vegetation water content, are derived from passive microwave remote sensing data from the Advanced Microwave Scanning Radiometer-Earth Observing System (AMSR-E), using the Land Parameter Retrieval Model (LPRM). There are two files per day, one ascending (daytime) and one descending (nighttime), archived as two different products. This document is for the nighttime product. The data set covers the period from June 2002 to October 2011 (when the AMSR-E on the NASA EOS Aqua satellite stopped producing data due to a problem with the rotation of its antenna). The LPRM is based on a forward radiative transfer model to retrieve surface soil moisture and vegetation optical depth. The land surface temperature is derived separately from the AMSR-E&amp;#39;s Ka-band (36.5 GHz). A unique feature of this method is that it can be applied at any microwave frequency, making it very suitable to exploit all the available passive microwave data from various satellites. Input data are from the AMSR-E resampled brightness temperatures (AE_L2A) product, nighttime passes, as processed using LPRM (i.e., LPRM/AMSR-E/Aqua L2B product, LPRM_AMSRE_SOILM2_V002).
&lt;br&gt;&lt;h4 id&#x3D;&quot;sndraqil2jsfret&quot;&gt;SNDRAQIL2JSFRET&lt;/h4&gt;
The Joint Single Footprint Retrieval Algorithm (JoSFRA) Level-2 geophysical parameters include estimates of atmospheric temperature and water vapor profiles, cloud properties, and surface temperature. These are retrieved from infrared spectra observed by the Atmospheric Infrared Sounder (AIRS) instrument on the Aqua satellite. AIRS is a grating spectrometer aboard Aqua, the second Earth Observing System (EOS) polar-orbiting platform. AIRS is co-boresited with the Advanced Microwave Sounding Unit (AMSU) also on Aqua. Horizontal resolutions are 50 km for AMSU and 13.5 km for AIRS. The JoSFRA algorithm uses an optimal-estimation scheme and retrieves geophysical quantities from AIRS thermal infrared spectra at their native horizontal resolution. Cloud observations from MODIS are used in the forward model without recourse to a cloud-cleared state. JOSFRA retrievals provide improved spatial resolution (13.5 km vs 50 km for cloud-cleared retrievals) and information content quantification, making them well-suited for process studies. JoSFRA retrievals are particularly useful in cases where high resolution (finer than 45 km) is needed or is beneficial, such as regions of strong horizontal gradients in water vapor. Use of JoSFRA retrievals is recommended under medium to low cloud cover. AIRS observations provide near-global coverage twice daily (around 1:30 am and pm local time) since August 30, 2002. An AIRS granule includes 6 minutes of data, 90 AIRS (30 AMSU) footprints across the orbit track by 135 AIRS (45 AMSU) footprints along track. Each day includes 240 granules, with an orbit repeat cycle of approximately 16 days. For the initial release of Version 2 JoSFRA, a limited test data set is provided. Future releases will expand the dataset. The initial dataset includes full global coverage data for two 5-day periods: January 13-17, 2011 and July 13-17, 2011, the Marine ARM GPCI Investigation of Clouds (MAGIC) (Lewis and Teixeira, EOS, 2015) test campaign in the Pacific Ocean with all 6-minute granules that overlap the box bounded by 20-35 degrees North latitude and 120-160 West longitude, June 1, 2012 – September 30, 2013, select granules from the years 2002-2007 where correlative data were available. The locations include Dept. of Energy (DOE) Atmospheric Radiation Measurement (ARM) sites at the North Slope of Alaska (NSA), Southern Great Plains (SGP), and Tropical Western Pacific (TWP), as well as scientific field campaigns.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airsil3msolr&quot;&gt;AIRSIL3MSOLR&lt;/h4&gt;
This L3 Spectral Outgoing Longwave Radiation (OLR) is derived using the AIRS radiances to compute spectral fluxes based on an algorithm developed by Xianglei Huang at the University of Michigan. It uses data from the Atmospheric InfraRed Sounder (AIRS) instrument on the EOS-Aqua spacecraft. The Aqua AIRS Huang Level-3 Spectral OLR product contains OLR parameters derived from the AIRS version 6 data: all-sky and clear-sky OLR both spectrally resolved at 10 cm-1 bandwidth and integrated to a single value per grid square. This is monthly product on a 2x2 degree latitude/longitude grid.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aer_dbdt_d10km_l3_modis_aqua&quot;&gt;AER_DBDT_D10KM_L3_MODIS_AQUA&lt;/h4&gt;
This High-Resolution (0.1 x 0.1 degree) Level 3 daily Aerosol Optical Depth (AOD) product is generated by combining two Moderate Resolution Imaging Spectroradiometer (MODIS) operational algorithms, namely Deep Blue (DB) and Dark Target (DT), on board the AQUA satellite. This dataset is provided in daily files ranging from 2002-07-04 to the present. The spatial coverage is global and the dataset is gridded at 0.1 x 0.1 degree spatial resolution. The data are generated using Level 2 AOD retrieved using DT and DB algorithms. The product provides multiple options for using data either from DT or DB or combined. Depending on user need and application, they can choose one or more relevant parameter. The pixels with highest quality as recommended by science teams are only considered in these averaging. In addition to averaged AOD at 0.1 x 0.1 degree resolution, standard deviation and number of pixels averaged from each algorithm are also provided. Average sensor zenith angle is also provided for additional filtering of the data. If you have any questions, please read the README document first and post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#102;&amp;#99;&amp;#45;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#115;&amp;#102;&amp;#99;&amp;#45;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;aer_dbdt_m10km_l3_modis_aqua&quot;&gt;AER_DBDT_M10KM_L3_MODIS_AQUA&lt;/h4&gt;
This High-Resolution (0.1 x 0.1 degree) Level 3 monthly Aerosol Optical Depth (AOD) product is generated by combining two Moderate Resolution Imaging Spectroradiometer (MODIS) operational algorithms, namely Deep Blue (DB) and Dark Target (DT), on board the AQUA satellite. This dataset is provided in monthly files ranging from July 2002 to the present. The spatial coverage is global and the dataset is gridded at 0.1 x 0.1 degree spatial resolution. The data are generated using Level 2 AOD retrieved using DT and DB algorithms. The product provides multiple options for using data either from DT or DB or combined. Depending on user need and application, they can choose one or more relevant parameter. The pixels with highest quality as recommended by science teams are only considered in these averaging. In addition to averaged AOD at 0.1 x 0.1 degree resolution, standard deviation and number of pixels averaged from each algorithm are also provided. Average sensor zenith angle is also provided for additional filtering of the data. If you have any questions, please read the README document first and post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#97;&amp;#x73;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#118;&quot;&gt;&amp;#x67;&amp;#115;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#97;&amp;#x73;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;airx2ret&quot;&gt;AIRX2RET&lt;/h4&gt;
The Atmospheric Infrared Sounder (AIRS) is a grating spectrometer (R &#x3D; 1200) aboard the second Earth Observing System (EOS) polar-orbiting platform, EOS Aqua. The AIRS combination with the Advanced Microwave Sounding Unit (AMSU) constitutes an innovative atmospheric sounding group of infrared and microwave sensors. The AIRS Standard Retrieval Product consists of retrieved estimates of cloud and surface properties, plus profiles of retrieved temperature, water vapor, ozone, carbon monoxide and methane. Estimates of the errors associated with these quantities are also be part of the Standard Product. The temperature profile vertical resolution is 28 levels total between 1100 mb and 0.1 mb, while moisture profile is reported at 14 atmospheric layers between 1100 mb and 50 mb. The horizontal resolution is 50 km. An AIRS granule has been set as 6 minutes of data, 30 footprints cross track by 45 lines along track. There are 240 granules per day, with an orbit repeat cycle of approximately 16 day.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airx2sup&quot;&gt;AIRX2SUP&lt;/h4&gt;
The Atmospheric Infrared Sounder (AIRS) is a grating spectrometer (R &#x3D; 1200) aboard the second Earth Observing System (EOS) polar-orbiting platform, EOS Aqua. In combination with the Advanced Microwave Sounding Unit (AMSU), AIRS constitutes an innovative atmospheric sounding group of infrared and microwave sensors. The Support Product includes higher vertical resolution profiles of the quantities found in the Standard Product plus intermediate output (e.g., microwave-only retrieval), research products such as the abundance of trace gases, and detailed quality assessment information. The Support Product profiles contain 100 pressure levels between 1100 and .016 mb; this higher resolution simplifies the generation of radiances using forward models, though the vertical information content is no greater than in the Standard Product profiles. The horizontal resolution is 50 km. The intended users of the Support Product are researchers interested in generating forward radiance, or in examining research products, and the AIRS algorithm development team. The Support Product is generated at all locations as Standard Products. An AIRS granule has been set as 6 minutes of data, 30 footprints cross track by 45 lines along track. There are 240 granules per day, with an orbit repeat cycle of approximately 16 day.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airs2ccf_nrt-1&quot;&gt;AIRS2CCF_NRT&lt;/h4&gt;
The Atmospheric Infrared Sounder (AIRS) Level 2 Near Real Time (NRT) Cloud-Cleared Infrared Radiances (AIRS-only) product (AIRS2CCF_NRT_7.0) differs from the routine product (AIRS2CCF_7.0) in four ways to meet the three hour latency requirements of the Land Atmosphere NRT Capability Earth Observing System (LANCE): (1) The NRT granules are produced without previous or subsequent granules if those granules are not available within 5 minutes, (2) the predictive ephemeris/attitude data are used rather than the definitive ephemeris/attitude, (3) if the forecast surface pressure is unavailable, a surface climatology is used, and (4) no ice cloud properties retrievals are performed. The consequences of these differences are described in the AIRS Near Real Time (NRT) data products document. The Atmospheric Infrared Sounder (AIRS) is a grating spectrometer (R &#x3D; 1200) aboard the second Earth Observing System (EOS) polar-orbiting platform, EOS Aqua. In combination with the Advanced Microwave Sounding Unit (AMSU) and the Humidity Sounder for Brazil (HSB), AIRS constitutes an innovative atmospheric sounding group of visible, infrared, and microwave sensors. This product is produced using AIRS IR only because the radiometric noise in AMSU channel 4 started to increase significantly (since June 2007). Cloud-Cleared Radiances contain calibrated, geolocated channel-by-channel AIRS infrared radiances (milliWatts/m2/cm-1/steradian) that would have been observed within each AMSU footprint if there were no clouds in the FOV and produced along with the AIRS Standard Product, as they are the radiances used to retrieve the Standard Product. Nevertheless, they are an order of magnitude larger in data volume than the remainder of the Standard Products and, many Standard Product users are expected to have little interest in the Cloud Cleared Radiance. For these reasons they are a separate output file. The AIRS2CCF_NRT_7.0 products are stored in files (often referred to as &amp;quot;granules&amp;quot;) that contain 6 minutes of data, 30 footprints across track by 45 lines along track.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airs2ret_nrt-1&quot;&gt;AIRS2RET_NRT&lt;/h4&gt;
The Atmospheric Infrared Sounder (AIRS) Level 2 Near Real Time (NRT) Standard Physical Retrieval (AIRS-only) product (AIRS2RET_NRT_7.0) differs from the routine product (AIRS2RET_7.0) in four ways to meet the three hour latency requirements of the Land Atmosphere NRT Capability Earth Observing System (LANCE): (1) The NRT granules are produced without previous or subsequent granules if those granules are not available within 5 minutes, (2) the predictive ephemeris/attitude data are used rather than the definitive ephemeris/attitude, (3) if the forecast surface pressure is unavailable, a surface climatology is used, and (4) no ice cloud properties retrievals are performed. The consequences of these differences are described in the AIRS Near Real Time (NRT) data products document. The Atmospheric Infrared Sounder (AIRS) is a grating spectrometer (R &#x3D; 1200) aboard the second Earth Observing System (EOS) polar-orbiting platform, EOS Aqua. In combination with the Advanced Microwave Sounding Unit (AMSU) and the Humidity Sounder for Brazil (HSB), AIRS constitutes an innovative atmospheric sounding group of visible, infrared, and microwave sensors. This product is produced using AIRS IR only because the radiometric noise in several AMSU channels started to increase significantly (since June 2007). The AIRS Standard Retrieval Product consists of retrieved estimates of cloud and surface properties, plus profiles of retrieved temperature, water vapor, ozone, carbon monoxide and methane. Estimates of the errors associated with these quantities is also part of the Standard Product. The temperature profile vertical resolution is 28 levels total between 1100 mb and 0.1 mb, while moisture profile is reported at 14 atmospheric layers between 1100 mb and 50 mb. The horizontal resolution is 50 km. An AIRS granule has been set as 6 minutes of data, 30 footprints cross track by 45 lines along track. There are 240 granules per day, with an orbit repeat cycle of approximately 16 day.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airs2sup_nrt-1&quot;&gt;AIRS2SUP_NRT&lt;/h4&gt;
The Atmospheric Infrared Sounder (AIRS) Level 2 Near Real Time (NRT) Support Retrieval (AIRS-only) product (AIRS2SUP_NRT_7.0) differs from the routine product (AIRS2SUP_7.0) in four ways to meet the three hour latency requirements of the Land Atmosphere NRT Capability Earth Observing System (LANCE): (1) The NRT granules are produced without previous or subsequent granules if those granules are not available within 5 minutes, (2) the predictive ephemeris/attitude data are used rather than the definitive ephemeris/attitude, (3) if the forecast surface pressure is unavailable, a surface climatology is used, and (4) no ice cloud properties retrievals are performed. The consequences of these differences are described in the AIRS Near Real Time (NRT) data products document. The Atmospheric Infrared Sounder (AIRS) is a grating spectrometer (R &#x3D; 1200) aboard the second Earth Observing System (EOS) polar-orbiting platform, EOS Aqua. In combination with the Advanced Microwave Sounding Unit (AMSU) and the Humidity Sounder for Brazil (HSB), AIRS constitutes an innovative atmospheric sounding group of visible, infrared, and microwave sensors. This product is product produced using AIRS IR only because the radiometric noise in several AMSU channels started to increase significantly (since June 2007). The Support Product includes higher vertical resolution profiles of the quantities found in the Standard Product, plus intermediate outputs (e.g., microwave-only retrieval), research products such as the abundance of trace gases, and detailed quality assessment information. The Support Product profiles contain 100 levels between 1100 and .016 mb; this higher resolution simplifies the generation of radiances using forward models, though the vertical information content is no greater than that in the Standard Product profiles. The intended users of the Support Product are researchers interested in generating forward radiance or in examining research products, and the AIRS algorithm development team. The Support Product is generated at all locations as Standard Products. An AIRS granule has been set as 6 minutes of data, 30 footprints cross track by 45 scanlines. There are 240 granules per day, with an orbit repeat cycle of approximately 16 day.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airx3std&quot;&gt;AIRX3STD&lt;/h4&gt;
The Atmospheric Infrared Sounder (AIRS) is a grating spectrometer (R &#x3D; 1200) aboard the second Earth Observing System (EOS) polar-orbiting platform, EOS Aqua. In combination with the Advanced Microwave Sounding Unit (AMSU) AIRS constitutes an innovative atmospheric sounding group of infrared and microwave sensors. The AIRS Level 3 Daily Gridded Product contains standard retrieval means, standard deviations and input counts. Each file covers a temporal period of 24 hours for either the descending (equatorial crossing North to South at 1:30 AM local time) or ascending (equatorial crossing South to North at 1:30 PM local time) orbit. The data starts at the international dateline and progresses westward (as do the subsequent orbits of the satellite) so that neighboring gridded cells of data are no more than a swath of time apart (about 90 minutes). The two parts of a scan line crossing the dateline are included in separate L3 files, according to the date, so that data points in a grid box are always coincident in time. The edge of the AIRS Level 3 gridded cells is at the date line (the 180E/W longitude boundary). When plotted, this produces a map with 0 degrees longitude in the center of the image unless the bins are reordered. This method is preferred because the left (West) side of the image and the right (East) side of the image contain data farthest apart in time. The gridding scheme used by AIRS is the same as used by TOVS Pathfinder to create Level 3 products. The daily Level 3 products have gores between satellite paths where there is no coverage for that day. The geophysical parameters have been averaged and binned into 1 x 1 deg grid cells, from -180.0 to +180.0 deg longitude and from -90.0 to +90.0 deg latitude. The value for each grid box is the sum of the values that fall within the 1x1 area divided by the number of points in the box. For each grid map of 4-byte floating-point mean values there is a corresponding 4-byte floating-point map of standard deviation and a 2-byte integer grid map of counts. The counts map provides the user with the number of points per bin that were included in the mean and can be used to generate custom multi-day maps from the daily gridded products. The thermodynamic parameters are: Skin Temperature (land and sea surface), Air Temperature at the surface, Profiles of Air Temperature and Water Vapor, Tropopause Characteristics, Column Precipitable Water, Cloud Amount/Frequency, Cloud Height, Cloud Top Pressure, Cloud Top Temperature, Reflectance, Emissivity, Surface Pressure, Cloud Vertical Distribution. The trace gases parameters are: Total Amounts and Vertical Profiles of Carbon Monoxide, Methane, and Ozone. The actual names of the variables in the data files should be inferred from the Processing File Description document.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airs3std&quot;&gt;AIRS3STD&lt;/h4&gt;
The Atmospheric Infrared Sounder (AIRS) is a grating spectrometer (R &#x3D; 1200) aboard the second Earth Observing System (EOS) polar-orbiting platform, EOS Aqua. The AIRS Level 3 Daily Gridded Product contains standard retrieval means, standard deviations and input counts. Each file covers a temporal period of 24 hours for either the descending (equatorial crossing North to South at 1:30 AM local time) or ascending (equatorial crossing South to North at 1:30 PM local time) orbit. The data starts at the international dateline and progresses westward (as do the subsequent orbits of the satellite) so that neighboring gridded cells of data are no more than a swath of time apart (about 90 minutes). The two parts of a scan line crossing the dateline are included in separate L3 files, according to the date, so that data points in a grid box are always coincident in time. The edge of the AIRS Level 3 gridded cells is at the date line (the 180E/W longitude boundary). When plotted, this produces a map with 0 degrees longitude in the center of the image unless the bins are reordered. This method is preferred because the left (West) side of the image and the right (East) side of the image contain data farthest apart in time. The gridding scheme used by AIRS is the same as used by TOVS Pathfinder to create Level 3 products. The daily Level 3 products have gores between satellite paths where there is no coverage for that day. The geophysical parameters have been averaged and binned into 1 x 1 deg grid cells, from -180.0 to +180.0 deg longitude and from -90.0 to +90.0 deg latitude. For each grid map of 4-byte floating-point mean values there is a corresponding 4-byte floating-point map of standard deviation and a 2-byte integer grid map of counts. The counts map provides the user with the number of points per bin that were included in the mean and can be used to generate custom multi-day maps from the daily gridded products. The thermodynamic parameters are: Skin Temperature (land and sea surface), Air Temperature at the surface, Profiles of Air Temperature and Water Vapor, Tropopause Characteristics, Column Precipitable Water, Cloud Amount/Frequency, Cloud Height, Cloud Top Pressure, Cloud Top Temperature, Reflectance, Emissivity, Surface Pressure, Cloud Vertical Distribution. The trace gases parameters are: Total Amounts and Vertical Profiles of Carbon Monoxide, Methane, and Ozone. The actual names of the variables in the data files should be inferred from the Processing File Description document. The value for each grid box is the sum of the values that fall within the 1x1 area divided by the number of points in the box.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airs3stm&quot;&gt;AIRS3STM&lt;/h4&gt;
The Atmospheric Infrared Sounder (AIRS) is a grating spectrometer (R &#x3D; 1200) aboard the second Earth Observing System (EOS) polar-orbiting platform, EOS Aqua. The AIRS Only Level 3 Monthly Gridded Retrieval Product contains standard retrieval means, standard deviations and input counts. Each file covers a calendar month. The mean values are simply the arithmetic means of the daily products, weighted by the number of input counts for each day in that grid box. The geophysical parameters have been averaged and binned into 1 x 1 deg grid cells, from -180.0 to +180.0 deg longitude and from -90.0 to +90.0 deg latitude. For each grid map of 4-byte floating-point mean values there is a corresponding 4-byte floating-point map of standard deviation and a 2-byte integer grid map of counts. The counts map provides the user with the number of points per bin that were included in the mean and can be used to generate custom multi-day maps from the daily gridded products. The thermodynamic parameters are: Skin Temperature (land and sea surface), Air Temperature at the surface, Profiles of Air Temperature and Water Vapor, Tropopause Characteristics, Column Precipitable Water, Cloud Amount/Frequency, Cloud Height, Cloud Top Pressure, Cloud Top Temperature, Reflectance, Emissivity, Surface Pressure, Cloud Vertical Distribution. The trace gases parameters are: Total Amounts and Vertical Profiles of Carbon Monoxide, Methane, and Ozone. The actual names of the variables in the data files should be inferred from the Processing File Description document.
&lt;br&gt;&lt;h4 id&#x3D;&quot;airsac3mnh3&quot;&gt;AIRSAC3MNH3&lt;/h4&gt;
The mass concentration ammonia in the atmosphere, consists of products generated for the study of atmospheric ammonia. Atmospheric ammonia is an important component of the global nitrogen cycle. In the troposphere, ammonia reacts rapidly with acids such as sulfuric and nitric to form fine particulate matter. These ammonium containing aerosols affect Earth&amp;#39;s radiative balance, both directly by scattering incoming radiation and indirectly as cloud condensation nuclei. Major sources of atmospheric ammonia involve agricultural activities including animal husbandry, especially concentrated animal feeding operations and fertilizer use. Major sinks of atmospheric ammonia involve dry deposition and wet removal by precipitation, as well as conversion to particulate ammonium by reaction with acids. Measurements of ambient NH3 are sparse, but satellites provide a means to monitor atmospheric composition globally. Using the AIRS/AMSU satellite this algorithm provides monthly measurements of derived atmospheric NH3 for September 2002 through August 2016.
&lt;br&gt;&lt;h4 id&#x3D;&quot;mydfds_clm_glb_l3&quot;&gt;MYDFDS_CLM_GLB_L3&lt;/h4&gt;
Version 1 is the current version of the dataset. This collection MYDFDS_CLM_GLB_L3 provides level 3 climatological monthly frequency of dust storms (FDS) over land from 175°W to 175°E and 80°S to 80°N at a spatial resolution of 0.1˚ x 0.1˚. It is derived from Level 2, the Moderate Resolution Imaging Spectroradiometer (MODIS) Deep Blue aerosol products Collection 6.1 from Aqua (MYD04_L2). The dataset is the climatological monthly mean for each month averaged over 2003 to 2022. The FDS is calculated as the number of days per month when the daily dust optical depth is greater than a threshold optical depth (e.g., 0.025) with two quality flags: the lowest (1) and highest (3). It is advised to use flag 1, which is of lower quality, over dust source regions, and flag 3 over remote areas or polluted regions. Eight thresholds (0.025, 0.05, 0.1, 0.25, 0.5, 0.75, 1, 2) are saved separately in eight files. If you have any questions, please read the README document first and post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#x65;&amp;#108;&amp;#112;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#x65;&amp;#108;&amp;#112;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd04_l2&quot;&gt;MYD04_L2&lt;/h4&gt;
The MODIS/Aqua Aerosol 5-Min L2 Swath 10km product (MYD04_L2) provides full global coverage of aerosol properties from the Dark Target (DT) and Deep Blue (DB) algorithms. The DT algorithm is applied over ocean and dark land (e.g., vegetation), while the DB algorithm now covers the entire land areas including both dark and bright surfaces. Both results are provided on a 10x10 pixel scale (10 km at nadir). Each MYD04_L2 product file covers a five-minute time interval. The output grid is 135 pixels in width by 203 pixels in length. Every tenth file has an output grid size of 135 by 204 pixels. MYD04_L2 product files are stored in Hierarchical Data Format (HDF-EOS). The new Collection 6.1 (C61) MYD04_L2 product is an improved version based on algorithm changes in Dark Target (DT) Aerosol retrieval over urban areas and uncertainty estimates for Deep Blue (DB) Aerosol retrievals. The MODIS level-2 atmospheric aerosol product provides retrieved ambient aerosol optical properties, quality assurance, and other parameters, globally over ocean and land. In Collection 5 and in earlier collections, there was only one aerosol product (MYD04_L2) at 10km (at nadir) spatial resolution. Starting from C6, the Dark Target (DT) Aerosol algorithm team provided a new 3 km spatial resolution product (MYD04_3k) intended for the air quality community. For more information visit the MODIS Atmosphere website at: &lt;a href&#x3D;&quot;https://modis-atmos.gsfc.nasa.gov/products/aerosol&quot;&gt;https://modis-atmos.gsfc.nasa.gov/products/aerosol&lt;/a&gt; And, for C6.1 changes and updates, visit: &lt;a href&#x3D;&quot;https://modis-atmosphere.gsfc.nasa.gov/documentation/collection-61&quot;&gt;https://modis-atmosphere.gsfc.nasa.gov/documentation/collection-61&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd04_3k&quot;&gt;MYD04_3K&lt;/h4&gt;
The new Collection 6.1 (C61) MODIS/Aqua Aerosol 5 Min L2 Swath 3km (MYD04_3K) product is an improved version based on algorithm changes in Dark Target (DT) Aerosol retrieval over urban areas and uncertainty estimates for Deep Blue (DB) Aerosol retrievals. The MODIS level-2 atmospheric aerosol product provides retrieved ambient aerosol optical properties, quality assurance, and other parameters, globally over ocean and land. In Collection 5, and earlier collections, there was only one aerosol product (MYD04_L2) at 10km (at nadir) spatial resolution. Starting from C6, the Dark Target (DT) Aerosol algorithm team provided a new 3 km spatial resolution product (MYD04_3k) intended for the air quality community. The MYD04_3K product is based on the same algorithm and Look up Tables as the standard Dark Target aerosol product. Because of finer resolution, subtle differences are made in selecting pixels for retrieval and in determining QA. The only differences between the existing 10km algorithm and the new 3km algorithm are: 1) the size of the pixel-arrays defining each retrieval box ( 6x6 retrieval boxes of 36 pixels at 0.5km resolution for 3km algorithm as oppose to 20x20 retrieval boxes of 400 pixels at 0.5km resolution for 10km product); 2) the minimum percentage of &amp;quot;good&amp;quot; pixels required for a retrieval (a minimum of 5 pixels over ocean and 6 pixels over land instead of a minimum of 10 pixels over ocean or 12 pixels over land for 10km product retrieval); 3) the 10km algorithm attempts a &amp;quot;poor quality&amp;quot; retrieval while 3km algorithm does not. Everything else is the same between two products. For more information on C6.1 changes and updates, visit the MODIS Atmosphere website at: &lt;a href&#x3D;&quot;https://modis-atmosphere.gsfc.nasa.gov/documentation/collection-61&quot;&gt;https://modis-atmosphere.gsfc.nasa.gov/documentation/collection-61&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd08_e3&quot;&gt;MYD08_E3&lt;/h4&gt;
The MODIS/Aqua Aerosol Cloud Water Vapor Ozone 8-Day L3 Global 1Deg CMG product (MYD08_E3) contains 8-Day 1 degree x 1 degree grid average values of atmospheric parameters related to atmospheric aerosol particle properties, total ozone burden, atmospheric water vapor, cloud optical and physical properties, and atmospheric stability indices. This product also provides standard deviations, quality assurance weighted means and other statistically derived quantities for each parameter. The MYD08_E3 contains nearly 1000 statistical datasets (SDS&amp;#39;s) that are derived from the Level-3 MODIS Atmosphere Daily Global Product. Statistics are computed over a 1 degree equal-angle lat-lon grid that spans an 8-Day interval. Since the grid cells are 1 degree by 1 degree, the output grid is always 360 pixels in width and 180 pixels in length. MYD08_E3 product files are stored in Hierarchical Data Format (HDF-EOS). Each gridded global parameter is stored as Scientific Data Sets (SDS) within the file. The MODIS 8-Day Product will be used in the simultaneously study of clouds, water vapor, aerosol , trace gases, land surface and oceanic properties, as well as the interaction between them and their effect on the Earth&amp;#39;s energy budget and climate. This product will also be used to investigate seasonal and inter-annual changes in cirrus (semi-transparent) global cloud cover and cloud phase with multispectral observations at high spatial resolution. For more information about the MYD08_E3 product, please visit the MODIS-Atmosphere site at: &lt;a href&#x3D;&quot;https://modis-atmos.gsfc.nasa.gov/products/eight-day&quot;&gt;https://modis-atmos.gsfc.nasa.gov/products/eight-day&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd08_d3&quot;&gt;MYD08_D3&lt;/h4&gt;
The MODIS/Aqua Aerosol Cloud Water Vapor Ozone Daily L3 Global 1Deg CMG product (MYD08_D3) contains daily 1 x 1 degree grid average values of atmospheric parameters related to atmospheric aerosol particle properties, total ozone burden, atmospheric water vapor, cloud optical and physical properties, and atmospheric stability indices. This product also provides standard deviations, quality assurance weighted means and other statistically derived quantities for each parameter. The MYD08_D3 contains roughly 600 statistical datasets that are derived from approximately 80 scientific parameters from four Level-2 MODIS Atmosphere Products: MOD04_L2, MOD05_L2, MOD06_L2, and MOD07_L2. Statistics are computed over a 1 degree equal-angle lat-lon grid that spans a 24-hour (0000 to 2400 Greenwich Mean Time) interval. Since the grid cells are 1 degree by 1 degree, the output grid is always 360 pixels in width and 180 pixels in length. MYD08_D3 product files are stored in Hierarchical Data Format (HDF-EOS). Each gridded global parameter is stored as Scientific Data Sets (SDS) within the file. The MODIS Daily Product will be used in the simultaneously study of clouds, water vapor, aerosol , trace gases, land surface and oceanic properties, as well as the interaction between them and their effect on the Earth&amp;#39;s energy budget and climate. This product will also be used to investigate seasonal and inter-annual changes in cirrus (semi-transparent) global cloud cover and cloud phase with multispectral observations at high spatial resolution. For more information about the MYD08_D3 product, please visit the MODIS-Atmosphere site at: &lt;a href&#x3D;&quot;https://modis-atmos.gsfc.nasa.gov/products/daily&quot;&gt;https://modis-atmos.gsfc.nasa.gov/products/daily&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd08_m3&quot;&gt;MYD08_M3&lt;/h4&gt;
The MODIS/Aqua Aerosol Cloud Water Vapor Ozone Monthly L3 Global 1Deg CMG product (MYD08_M3) contains monthly 1 x 1 degree grid average values of atmospheric parameters related to atmospheric aerosol particle properties, total ozone burden, atmospheric water vapor, cloud optical and physical properties, and atmospheric stability indices. This product also provides standard deviations, quality assurance weighted means and other statistically derived quantities for each parameter. The MYD08_M3 contains roughly 800 statistical datasets that are derived from the Level-3 MODIS Atmosphere Daily Global Product. Statistics are sorted into 1x1 degree cells on an equal-angle grid that spans a (calendar) monthly interval and then summarized over the globe. MYD08_M3 product files are stored in Hierarchical Data Format (HDF-EOS). Each gridded global parameter is stored as Scientific Data Sets (SDS) within the file. The MODIS monthly Product will be used in the simultaneously study of clouds, water vapor, aerosol , trace gases, land surface and oceanic properties, as well as the interaction between them and their effect on the Earth&amp;#39;s energy budget and climate. This product will also be used to investigate seasonal and inter-annual changes in cirrus (semi-transparent) global cloud cover and cloud phase with multispectral observations at high spatial resolution. For more information about the MYD08_M3 product, please visit the MODIS-Atmosphere site at: &lt;a href&#x3D;&quot;https://modis-atmos.gsfc.nasa.gov/products/monthly&quot;&gt;https://modis-atmos.gsfc.nasa.gov/products/monthly&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;mydatml2&quot;&gt;MYDATML2&lt;/h4&gt;
The MODIS/Aqua Aerosol, Cloud and Water Vapor Subset 5-Min L2 Swath 5km and 10km (MYDATML2) product contains a combination of key high interest science parameters. The ATML2 product provides a subset of datasets from the suite of atmosphere team products on both a 10 km scale (aerosols) and 5km scale (native 5 km cloud properties and a 5x5 pixel sample of the 1km cloud datasets). The ATML2 product employs the same 5x5 pixel sampling scheme for the 1km native resolution Level 2 products as is used in the MOD08 Level 3 global aggregated product, an approach that has been shown to retain statistical integrity for multi-day aggregations. The C6 significantly increases the number of datasets included in the ATML2 product, including the full suite of QA datasets. Since the ATML2 data granule file size is significantly smaller than the combined size of the individual L2 products, and because the 1 km pixel sampling is consistent with the L3 algorithm, the ATML2 product is a more practical means for the user community to develop research L3 algorithms for their own specific purposes. For more information, visit the MODIS Atmosphere website at: &lt;a href&#x3D;&quot;https://modis-atmos.gsfc.nasa.gov/products/joint-atm&quot;&gt;https://modis-atmos.gsfc.nasa.gov/products/joint-atm&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd09&quot;&gt;MYD09&lt;/h4&gt;
The MODIS/Aqua Atmospherically Corrected Surface Reflectance 5-Min L2 Swath 250m, 500m, 1km (MYD09) product is computed from the MODIS Level 1B land bands 1, 2, 3, 4, 5, 6, and 7 (centered at 648 nm, 858 nm, 470 nm, 555 nm, 1240 nm, 1640 nm, and 2130 nm, respectively). The product is an estimate of the surface spectral reflectance for each band as it would have been measured at ground level if there were no atmospheric scattering or absorption. The surface-reflectance product is the input for product generation for several land products: vegetation Indices (VIs), Bidirectional Reflectance Distribution Function (BRDF), thermal anomaly, snow/ice, and Fraction of Photosynthetically Active Radiation/Leaf Area Index (FPAR/LAI).
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd021km&quot;&gt;MYD021KM&lt;/h4&gt;
The MODIS/Aqua Calibrated Radiances 5Min L1B Swath 1km data set contains calibrated and geolocated at-aperture radiances for 36 discrete bands located in the 0.4 to 14.4 micron region of the electromagnetic spectrum. These data are generated from the MODIS Level 1A scans of raw radiance which during processing are converted to geophysical units of W / (m^2 um sr). Additional data are provided including quality flags, error estimates and calibration data. Visible, shortwave infrared, and near infrared measurements are only made during the daytime (except band 26), while radiances for the thermal infrared region (bands 20-25, 27-36) are measured continuously. The shortname for this product is MYD021KM and is stored in the Earth Observing System Hierarchical Data Format (HDF-EOS). A typical file size is approximately 115 MB. Environmental information derived from MODIS L1B measurements will offer a comprehensive and unprecedented look at terrestrial, atmospheric, and ocean phenomenology for a wide and diverse community of users throughout the world. See the MODIS Characterization Support Team webpage for more C6 product information at: &lt;a href&#x3D;&quot;https://mcst.gsfc.nasa.gov/l1b/product-information&quot;&gt;https://mcst.gsfc.nasa.gov/l1b/product-information&lt;/a&gt; or visit Science Team homepage at: &lt;a href&#x3D;&quot;https://modis.gsfc.nasa.gov/data/dataprod/&quot;&gt;https://modis.gsfc.nasa.gov/data/dataprod/&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd02qkm&quot;&gt;MYD02QKM&lt;/h4&gt;
The MODIS/Terra Calibrated Radiances 5-Min L1B Swath 250m data set contains calibrated and geolocated at-aperture radiances for 2 discrete bands located in the 0.62 to 0.88 micron region of the electromagnetic spectrum. These data are generated from the MODIS Level 1A scans of raw radiance which during processing are converted to geophysical units of W / (m^2 um sr). Additional data are provided including quality flags, error estimates and calibration data. Separate L1B products are available for the five 500m resolution channels (MYD02HKM) and the twenty-nine 1km resolution channels (MYD021KM). For the 500m product, there are actually seven channels available since the data from the two 250 m channels have been aggregated to 500m resolution. Similarly, for the 1km product, all 36 MODIS channels are available since the data from the two 250m and five 500m channels have been aggregated into equivalent 1km pixel values. Spatial resolution for pixels at nadir is 250 m, degrading to 1.2 km in the along-scan direction and 0.5 km in the along-track direction for pixels located at the scan extremes. A 55 degree scanning pattern at the EOS orbit of 705 km results in a 2330 km orbital swath width and provides global coverage every one to two days. A single MODIS Level 1B 250 m granule will contain a scene built from 203 scans sampled 5416 times in the cross-track direction, corresponding to approximately 5 minutes worth of data; thus 288 granules will be produced per day. Since an individual MODIS scan will contain 40 along-track spatial elements for the 250 m channels, the scene will be composed of (5416 x 8120) pixels, resulting in a spatial coverage of (2330 km x 2040 km). Due to the MODIS scan geometry, there will be increasing scan overlap beyond about 17 degrees scan angle. The shortname for this product is MYD02QKM and is stored in the Earth Observing System Hierarchical Data Format (HDF-EOS). A typical file size will be approximately 140 MB and the total daily volume is around 22GB. Environmental information derived from MODIS L1B measurements will offer a comprehensive and unprecedented look at terrestrial, atmospheric, and ocean phenomenology for a wide and diverse community of users throughout the world. See the MODIS Characterization Support Team webpage for more C6.1 product information at: &lt;a href&#x3D;&quot;http://mcst.gsfc.nasa.gov/l1b/product-information&quot;&gt;http://mcst.gsfc.nasa.gov/l1b/product-information&lt;/a&gt; or visit Science Team homepage at: &lt;a href&#x3D;&quot;http://modis.gsfc.nasa.gov/data/dataprod/&quot;&gt;http://modis.gsfc.nasa.gov/data/dataprod/&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd02hkm&quot;&gt;MYD02HKM&lt;/h4&gt;
The MODIS/Aqua Calibrated Radiances 5Min L1B Swath 500m data set contains calibrated and geolocated at-aperture radiances for 7 discrete bands located in the 0.45 to 2.20 micron region of the electromagnetic spectrum. These data are generated from the MODIS Level 1A scans of raw radiance and in the process converted to geophysical units of W/(m^2 um sr). Additional data are provided including quality flags, error estimates and calibration data. Visible, shortwave infrared, and near infrared measurements are only made during the daytime (except band 26), while radiances for the thermal infrared region (bands 20-25, 27-36) are measured continuously. Channels 1 and 2 have 250 m resolution, channels 3 through 7 have 500 m resolution. However, for the MODIS L1B 500 m product, the 250 m band radiance data and their associated uncertainties have been aggregated to 500m resolution. Thus the entire channel data set has been co-registered to the same spatial scale in the 500 m product. Separate L1B products are available for the 250 m resolution channels (MYD02QKM) and 1 km resolution channels (MYD021KM). For the latter product, the 250 m and 500 m channel data (bands 1 through 7) have been aggregated into equivalent 1 km pixel values. Spatial resolution for pixels at nadir is 500 km, degrading to 2.4 km in the along-scan direction at the scan extremes. However, thanks to the overlapping of consecutive swaths and respectively pixels there, the resulting resolution at the scan extremes is about 1 km. A 55 degree scanning pattern at the EOS orbit of 705 km results in a 2330 km orbital swath width and provides global coverage every one to two days. A single MODIS Level 1B 500 m granule will contain a scene built from 203 scans sampled 2708 times in the cross-track direction, corresponding to approximately 5 minutes worth of data; thus 288 granules will be produced per day. Since an individual MODIS scan will contain 20 along-track spatial elements for the 500 m channels, the scene will be composed of (2708 x 4060) pixels, resulting in a spatial coverage of (2330 km x 2040 km). Due to the MODIS scan geometry, there will be increasing scan overlap beyond about 20 degrees scan angle. To summarize, the MODIS L1B 500 m data product consists of: 1. Calibrated radiances, uncertainties and number of samples for (2) 250 m reflected solar bands aggregated to 500 m resolution 2. Calibrated radiances and uncertainties for (5) 500 m reflected solar bands 3. Geolocation for 1km pixels, that must be interpolated to get 500 m pixel locations. For the relationship of 1km pixels to 500m pixels, see the Geolocation ATBD &lt;a href&#x3D;&quot;https://modis.gsfc.nasa.gov/data/atbd/atbd_mod28_v3.pdf&quot;&gt;https://modis.gsfc.nasa.gov/data/atbd/atbd_mod28_v3.pdf&lt;/a&gt;. 4. Calibration data for all channels (scale and offset) 5. Comprehensive set of file-level metadata summarizing the spatial, temporal and parameter attributes of the data, as well as auxiliary information pertaining to instrument status and data quality characterization users requiring all geolocation and solar/satellite geometry fields at 1km resolution can obtain the separate MODIS Level 1 Geolocation product (MYD03) from LAADS &lt;a href&#x3D;&quot;https://ladsweb.modaps.eosdis.nasa.gov/&quot;&gt;https://ladsweb.modaps.eosdis.nasa.gov/&lt;/a&gt; . The shortname for this product is MYD02HKM and is stored in the Earth Observing System Hierarchical Data Format (HDF-EOS). A typical MYD02HKM file size is approximately 135 MB. Environmental information derived from MODIS L1B measurements will offer a comprehensive and unprecedented look at terrestrial, atmospheric, and ocean phenomenology for a wide and diverse community of users throughout the world. See the MODIS Characterization Support Team webpage for more C6 product information at: &lt;a href&#x3D;&quot;https://mcst.gsfc.nasa.gov/l1b/product-information&quot;&gt;https://mcst.gsfc.nasa.gov/l1b/product-information&lt;/a&gt; or visit Science Team homepage at: &lt;a href&#x3D;&quot;https://modis.gsfc.nasa.gov/data/dataprod/&quot;&gt;https://modis.gsfc.nasa.gov/data/dataprod/&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;cldmsk_l2_modis_aqua&quot;&gt;CLDMSK_L2_MODIS_Aqua&lt;/h4&gt;
The MODIS-VIIRS Cloud Mask (MVCM) is designed to facilitate continuity in cloud detection between the MODIS (Moderate Resolution Imaging Spectroradiometer) on the Aqua and Terra platforms and the series of VIIRS (Visible Infrared Imaging Radiometer Suite) instruments, beginning with the Suomi NPP spacecraft. To establish continuity, this MODIS MVCM product does not use an algorithm identical to that used in the standard MODIS product (MOD35/MYD35). The MVCM-MODIS Cloud Mask product is Aqua MOIDS Level-2, 5-Min Swath product generated at 1000 m (at nadir) spatial resolution. The algorithm employs a series of visible through infrared threshold and consistency tests to specify confidence that an unobstructed view of the Earth&amp;#39;s surface has been observed. Radiometrically-accurate radiances are required, thus holes in the cloud mask will appear wherever the input radiances are incomplete or of poor quality. For more information consult Product Page at: &lt;a href&#x3D;&quot;https://cimss.ssec.wisc.edu/MVCM/&quot;&gt;https://cimss.ssec.wisc.edu/MVCM/&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd35_l2&quot;&gt;MYD35_L2&lt;/h4&gt;
The MODIS/Aqua Cloud Mask and Spectral Test Results 5-Min L2 Swath 250m and 1km product consists of global cloud mask quality assurance and other ancillary parameters. The algorithm employs a series of visible and infrared threshold and consistency tests to specify confidence levels that an unobstructed view of the Earth&amp;#39;s surface is observed. An indication of shadows affecting the scene is also provided. The 250-m cloud mask flags are based on the visible channel data only. Radiometrically accurate radiances are required, so holes in the cloud mask will appear wherever the input radiances are incomplete or of poor quality. The shortname for this Level-2 MODIS cloud mask product is MYD35_L2. The MYD35_L2 product files are stored in Hierarchical Data Format (HDF-EOS). This product consists of 9 parameters and each of these parameters are stored as a Scientific Data Set (SDS) within the HDF-EOS file. The Cloud Mask and Quality Assurance SDS&amp;#39;s are stored at 1 kilometer pixel resolution. All other SDS&amp;#39;s (those relating to time, geolocation, and viewing geometry) are stored at 5 kilometer pixel resolution. For more information about the MYD35_L2 product, visit the MODIS-Atmosphere site at: &lt;a href&#x3D;&quot;https://modis-atmos.gsfc.nasa.gov/products/cloud-mask&quot;&gt;https://modis-atmos.gsfc.nasa.gov/products/cloud-mask&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;cldprop_l2_modis_aqua&quot;&gt;CLDPROP_L2_MODIS_Aqua&lt;/h4&gt;
The MODIS/Aqua Cloud Properties 5-min L2 Swath 1km product is designed to facilitate continuity in cloud properties between the MODIS (Moderate Resolution Imaging Spectroradiometer) on the Aqua and Terra platforms and the series of VIIRS (Visible Infrared Imaging Radiometer Suite) instruments, beginning with the Suomi NPP spacecraft. To establish continuity, this MODIS Cloud Properties product does not use algorithms identical to those used in the standard MODIS product (MOD06/MYD06). The product consists of cloud optical and physical parameters derived using observations in visible through infrared spectral channels. MODIS infrared channels that are common with VIIRS are primarily used to derive cloud-top temperature, cloud-top height, effective emissivity, an infrared cloud phase product (ice vs. water, opaque vs. non-opaque), and cloud fraction under both daytime and nighttime conditions. The MODIS solar reflectances channels are primarily used to derive cloud optical thickness, particle effective radius, water path, and to inform the phase used in the optical retrievals. The MODIS Cloud Properties product is a Level-2 product generated at 1 km (at nadir) spatial resolution. The current version-1.1 of the Level-2 CLDPROP product collection is corrected to address an issue with the cloud optical properties’ thermodynamic phase that caused erroneous liquid water cloud phase results.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cldpropcosp_d3_modis_aqua&quot;&gt;CLDPROPCOSP_D3_MODIS_Aqua&lt;/h4&gt;
The MODIS/Aqua Cloud Properties COSP Level 3 daily, 1x1 degree grid product is a new L3 CLDPROP COSP Cloud product with short-name CLDPROPCOSP_D3_MODIS_Aqua. It contains MODIS Aqua cloud mask, cloud top, and cloud optical retrieval data over daily timeframe. It provides a set of custom cloud-related parameters for better comparison with climate model output. The “COSP” acronym in the short-name stands for Cloud Feedback Model Intercomparison Project (CFMIP) Observation Simulator Package. Provided in netCDF4 format, it contains 32 aggregated science data sets (SDS/parameters). Consult the CLDPROPCOSP User Guide for details regarding how the L3 daily statistics are computed, and to learn more about the gridding and sampling protocols specific to this product and a number of other topics germane to the user community. The collection of this product starts from July 4, 2002 and includes 365 granules each calendar year.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cldpropcosp_m3_modis_aqua&quot;&gt;CLDPROPCOSP_M3_MODIS_Aqua&lt;/h4&gt;
The MODIS/Aqua Cloud Properties COSP Level 3 monthly, 1x1 degree grid product is a new L3 CLDPROP COSP Cloud product with short-name CLDPROPCOSP_M3_MODIS_Aqua. It contains MODIS Aqua cloud mask, cloud top, and cloud optical retrieval data over monthly timeframe. It provides a set of custom cloud-related parameters for better comparison with climate model output. The “COSP” acronym in the short-name stands for Cloud Feedback Model Intercomparison Project (CFMIP) Observation Simulator Package. Provided in netCDF4 format, it contains 32 aggregated science data sets (SDS/parameters). Consult the CLDPROPCOSP User Guide for details regarding how the L3 daily statistics are computed, and to learn more about the gridding and sampling protocols specific to this product and a number of other topics germane to the user community. The collection of this product starts from August 1, 2002 and includes 12 granules each calendar year.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cldprop_d3_modis_aqua&quot;&gt;CLDPROP_D3_MODIS_Aqua&lt;/h4&gt;
The Cloud Properties Level-3 gridded product is designed to facilitate continuity in cloud property statistics between the MODIS on the Aqua and Terra platforms and the common continuity products generated for the VIIRS (Visible Infrared Imaging Radiometer Suite) and the MODIS Aqua instruments. CLDPROP Level-3 statistical routines include scalar and histograms (1-D and 2-D) that are calculated identically to statistical datasets in the MODIS standard Level-3 product (MOD08 and MYD08 for MODIS Terra and Aqua, respectively). In addition, the same dataset names are used for all common datasets provided in both the continuity and standard Level-3 files.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd06_l2&quot;&gt;MYD06_L2&lt;/h4&gt;
The MODIS/Aqua Clouds 5-Min L2 Swath 1km and 5km product consists of cloud optical and physical parameters. The cloud optical parameters are generated at 1km and cloud top (physical) parameters are generated at 5km resolution. These parameters are derived using remotely sensed infrared, visible and near infrared solar reflected radiances. MODIS infrared channel radiances are used to derive cloud top temperature, cloud top height, effective emissivity, cloud phase (ice vs. water, opaque vs. non-opaque), and cloud fraction under both daytime and nighttime conditions. MODIS visible radiances are used to derive cloud optical thickness and effective particle radius and cloud shadow effects. Near infrared solar reflected radiance provides additional information in the retrieval of cloud particle phase (ice vs. water, clouds vs. snow). The shortname for this level-2 MODIS cloud product is MYD06_L2. The MYD06_L2 consists of parameters at a spatial resolution of either 1- km or 5-km (at nadir). Each MYD06_L2 product file covers a five-minute time interval. This means that for 5-km resolution parameters, the output grid is 270 pixels in width by 406 pixels in length. C6.1 changes for the cloud optical property retrievals are low-impact, and are limited primarily to ancillary product usage, the Quality Assurance (QA), and handling of cloud top (CT) properties fill values; no updates to retrieval science are implemented. The MODIS Cloud Product is used to investigate seasonal and inter-annual changes in cirrus (semi-transparent) global cloud cover and cloud phase with multispectral observations at high spatial (1 kilometer) resolution. For more information about the MYD06_L2 product, visit the MODIS-Atmosphere site at: &lt;a href&#x3D;&quot;https://modis-atmos.gsfc.nasa.gov/products/cloud&quot;&gt;https://modis-atmos.gsfc.nasa.gov/products/cloud&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd03&quot;&gt;MYD03&lt;/h4&gt;
The MODIS/Aqua Geolocation Fields 5-Min L1A Swath 1km are calculated for each 1 km MODIS Instantaneous Field of Views (IFOV) for all orbits daily (in Collection 6 and later, information is provided to calculate 500m geolocation fields). The locations and ancillary information corresponds to the intersection of the centers of each IFOV from 10 detectors in an ideal 1 km band on the Earth&amp;#39;s surface. A digital terrain model is used to model the Earth&amp;#39;s surface. The main inputs are the spacecraft attitude and orbit, the instrument telemetry and the digital elevation model. The geolocation fields include geodetic Latitude, Longitude, surface height above geoid, solar zenith and azimuth angles, satellite zenith and azimuth angles, and a land/sea mask for each 1 km sample. Additional information is included in the header to enable the calculation of the approximate location of the center of the detectors of any of the 36 MODIS bands. This product is used as input by a large number of subsequent MODIS products, particularly the products produced by the Land team. The short name for this product is MYD03. Each file is roughly 30 MB in size, and the total data volume is approximately 8 GB/day. See the MODIS Science Team homepage for more data set information: &lt;a href&#x3D;&quot;https://modis.gsfc.nasa.gov/data/dataprod/&quot;&gt;https://modis.gsfc.nasa.gov/data/dataprod/&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd17a2h&quot;&gt;MYD17A2H&lt;/h4&gt;
The MYD17A2H Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD17A2H.061&quot;&gt;MYD17A2H Version 6.1&lt;/a&gt; data product. The MYD17A2H Version 6 Gross Primary Productivity (GPP) product is a cumulative 8-day composite of values with 500 meter (m) pixel size based on the radiation use efficiency concept that can be potentially used as inputs to data models to calculate terrestrial energy, carbon, water cycle processes, and biogeochemistry of vegetation. The data product includes information about GPP and Net Photosynthesis (PSN). The PSN band values are the GPP minus the Maintenance Respiration (MR). The data product also contains a PSN Quality Control (QC) layer. The quality layer contains quality information for both the GPP and the PSN. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd17a2h-1&quot;&gt;MYD17A2H&lt;/h4&gt;
The MYD17A2H Version 6.1 Gross Primary Productivity (GPP) product is a cumulative 8-day composite of values with 500 meter (m) pixel size based on the radiation use efficiency concept that can be potentially used as inputs to data models to calculate terrestrial energy, carbon, water cycle processes, and biogeochemistry of vegetation. The Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) data product includes information about GPP and Net Photosynthesis (PSN). The PSN band values are the GPP minus the Maintenance Respiration (MR). The data product also contains a PSN Quality Control (QC) layer. The quality layer contains quality information for both the GPP and the PSN. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd17a2hgf&quot;&gt;MYD17A2HGF&lt;/h4&gt;
The MYD17A2HGF Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD17A2HGF.061&quot;&gt;MYD17A2HGF Version 6.1&lt;/a&gt; data product. The MYD17A2HGF Version 6 Gross Primary Productivity (GPP) Gap-Filled product is a cumulative 8-day composite of values with 500 meter (m) pixel size based on the radiation use efficiency concept that can be potentially used as inputs to data models to calculate terrestrial energy, carbon, water cycle processes, and biogeochemistry of vegetation. The data product includes information about GPP and Net Photosynthesis (PSN). The PSN band values are the GPP less the Maintenance Respiration (MR). The data product also contains a PSN Quality Control (QC) layer. The quality layer contains quality information for both the GPP and the PSN. The MYD17A2HGF will be generated at the end of each year when the entire yearly 8-day &lt;a href&#x3D;&quot;https://doi.org/10.5067/modis/myd15a2h.006&quot;&gt;MYD15A2H&lt;/a&gt; is available. Hence, the gap-filled MYD17A2HGF is the improved MYD17, which has cleaned the poor-quality inputs from 8-day Leaf Area Index and Fraction of Photosynthetically Active Radiation (LAI/FPAR) based on the Quality Control (QC) label for every pixel. If any LAI/FPAR pixel did not meet the quality screening criteria, its value is determined through linear interpolation. However, users cannot get MYD17A2HGF in near-real time because it will be generated only at the end of a given year. Known Issues: Operational and uncertainty issues are provided under Section 2 in the User Guide. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd17a2hgf-1&quot;&gt;MYD17A2HGF&lt;/h4&gt;
The MYD17A2HGF Version 6.1 Gross Primary Productivity (GPP) Gap-Filled product is a cumulative 8-day composite of values with 500 meter (m) pixel size based on the radiation use efficiency concept that can be potentially used as inputs to data models to calculate terrestrial energy, carbon, water cycle processes, and biogeochemistry of vegetation. The Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) data product includes information about GPP and Net Photosynthesis (PSN). The PSN band values are the GPP less the Maintenance Respiration (MR). The data product also contains a PSN Quality Control (QC) layer. The quality layer contains quality information for both the GPP and the PSN. The MYD17A2HGF will be generated at the end of each year when the entire yearly 8-day &lt;a href&#x3D;&quot;https://doi.org/10.5067/modis/myd15a2h.061&quot;&gt;MYD15A2H&lt;/a&gt; is available. Hence, the gap-filled MYD17A2HGF is the improved MYD17, which has cleaned the poor-quality inputs from 8-day Leaf Area Index and Fraction of Photosynthetically Active Radiation (LAI/FPAR) based on the Quality Control (QC) label for every pixel. If any LAI/FPAR pixel did not meet the quality screening criteria, its value is determined through linear interpolation. However, users cannot get MYD17A2HGF in near-real time because it will be generated only at the end of a given year. Known Issues: Operational and uncertainty issues are provided under Section 2 in the User Guide. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd21&quot;&gt;MYD21&lt;/h4&gt;
The MYD21 Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD21.061&quot;&gt;MYD21 Version 6.1&lt;/a&gt; data product. The MYD21 Land Surface Temperature and Emissivity (LST&amp;amp;E) swath data product is produced daily in five minute temporal increments of satellite acquisition. The swath is approximately 2,030 pixels along track and 1,354 pixels per line, at a nadir resolution of 1,000 meters. The MYD21 Land Surface Temperature (LST) algorithm differs from the &lt;a href&#x3D;&quot;https://doi.org/10.5067/modis/myd11_l2.006&quot;&gt;MYD11&lt;/a&gt; algorithm in that the MYD21 LST algorithm is based on the ASTER Temperature/Emissivity Separation (TES) technique, whereas the MYD11 uses the split-window technique. The MYD21 TES algorithm uses a physics-based algorithm to dynamically retrieve both LST and spectral emissivity simultaneously from the MODIS thermal infrared bands 29, 31, and 32. The TES algorithm is combined with an improved Water Vapor Scaling (WVS) atmospheric correction scheme to stabilize the retrieval during very warm and humid conditions. MYD21 products are available two months after acquisition due to latency of data inputs. Additional details regarding the method used to create this Level 2 (L2) product are available in the Algorithm Theoretical Basis Document (ATBD). Known Issues: Users of MODIS LST products may notice an increase in occurrences of &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/displayissue?id&#x3D;117&quot;&gt;extreme high temperature outliers&lt;/a&gt; in the unfiltered MxD21 Version 6 and 6.1 products compared to the heritage MxD11 LST products. This can occur especially over desert regions like the Sahara where undetected cloud and dust can negatively impact both the MxD21 and MxD11 retrieval algorithms. * In the MxD11 LST products, these contaminated pixels are flagged in the algorithm and set to fill values in the output products based on differences in the band 32 and band 31 radiances used in the generalized split window algorithm. In the MxD21 LST products, values for the contaminated pixels are retained in the output products (and may result in overestimated temperatures), and users need to apply Quality Control (QC) filtering and other error analyses for filtering out bad values. High temperature outlier thresholds are not employed in MxD21 since it would potentially remove naturally occurring hot surface targets such as fires and lava flows. * High atmospheric aerosol optical depth (AOD) caused by vast dust outbreaks in the Sahara and other deserts highlighted in the example documentation are the primary reason for high outlier surface temperature values (and corresponding low emissivity values) in the MxD21 LST products. Future versions of the MxD21 product will include a dust flag from the MODIS aerosol product and/or brightness temperature look up tables to filter out contaminated dust pixels. It should be noted that in the MxD11B day/night algorithm products, more advanced cloud filtering is employed in the multi-day products based on a temporal analysis of historical LST over cloudy areas. This may result in more stringent filtering of dust contaminated pixels in these products. * In order to mitigate the impact of dust in the MxD21 V6 and 6.1 products, the science team recommends using a combination of the existing QC bits, emissivity values, and estimated product errors, to confidently remove bad pixels from analysis. For more details, refer to this dust and cloud contamination &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/data/userguide/MOD21_dust_QC_examples.pdf&quot;&gt;example documentation&lt;/a&gt;. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd21-1&quot;&gt;MYD21&lt;/h4&gt;
The MYD21 Version 6.1 Land Surface Temperature and Emissivity (LST&amp;amp;E) swath data product is produced daily in five minute temporal increments of satellite acquisition. The swath is approximately 2,030 pixels along track and 1,354 pixels per line, at a nadir resolution of 1,000 meters. The MYD21 Land Surface Temperature (LST) algorithm differs from the &lt;a href&#x3D;&quot;https://doi.org/10.5067/modis/myd11_l2.061&quot;&gt;MYD11&lt;/a&gt; algorithm in that the MYD21 LST algorithm is based on the ASTER Temperature/Emissivity Separation (TES) technique, whereas the MYD11 uses the split-window technique. The MYD21 TES algorithm uses a physics-based algorithm to dynamically retrieve both LST and spectral emissivity simultaneously from the MODIS thermal infrared bands 29, 31, and 32. The TES algorithm is combined with an improved Water Vapor Scaling (WVS) atmospheric correction scheme to stabilize the retrieval during very warm and humid conditions. Additional details regarding the method used to create this Level 2 (L2) product are available in the Algorithm Theoretical Basis Document (ATBD). Known Issues: Users of MODIS LST products may notice an increase in occurrences of &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/displayissue?id&#x3D;117&quot;&gt;extreme high temperature outliers&lt;/a&gt; in the unfiltered MxD21 Version 6 and 6.1 products compared to the heritage MxD11 LST products. This can occur especially over desert regions like the Sahara where undetected cloud and dust can negatively impact both the MxD21 and MxD11 retrieval algorithms. * In the MxD11 LST products, these contaminated pixels are flagged in the algorithm and set to fill values in the output products based on differences in the band 32 and band 31 radiances used in the generalized split window algorithm. In the MxD21 LST products, values for the contaminated pixels are retained in the output products (and may result in overestimated temperatures), and users need to apply Quality Control (QC) filtering and other error analyses for filtering out bad values. High temperature outlier thresholds are not employed in MxD21 since it would potentially remove naturally occurring hot surface targets such as fires and lava flows. * High atmospheric aerosol optical depth (AOD) caused by vast dust outbreaks in the Sahara and other deserts highlighted in the example documentation are the primary reason for high outlier surface temperature values (and corresponding low emissivity values) in the MxD21 LST products. Future versions of the MxD21 product will include a dust flag from the MODIS aerosol product and/or brightness temperature look up tables to filter out contaminated dust pixels. It should be noted that in the MxD11B day/night algorithm products, more advanced cloud filtering is employed in the multi-day products based on a temporal analysis of historical LST over cloudy areas. This may result in more stringent filtering of dust contaminated pixels in these products. * In order to mitigate the impact of dust in the MxD21 V6 and 6.1 products, the science team recommends using a combination of the existing QC bits, emissivity values, and estimated product errors, to confidently remove bad pixels from analysis. For more details, refer to this dust and cloud contamination &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/data/userguide/MOD21_dust_QC_examples.pdf&quot;&gt;example documentation&lt;/a&gt;. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd21c2&quot;&gt;MYD21C2&lt;/h4&gt;
A new suite of Moderate Resolution Imaging Spectroradiometer (MODIS) Land Surface Temperature and Emissivity (LST&amp;amp;E) products are available in Collection 6.1. The MYD21 Land Surface Temperature (LST) algorithm differs from the algorithm of the &lt;a href&#x3D;&quot;https://doi.org/10.5067/modis/myd11_l2.061&quot;&gt;MYD11&lt;/a&gt; LST products, in that the MYD21 algorithm is based on the ASTER Temperature/Emissivity Separation (TES) technique, whereas the MYD11 uses the split-window technique. The MYD21 TES algorithm uses a physics-based algorithm to dynamically retrieve both the LST and spectral emissivity simultaneously from the MODIS thermal infrared bands 29, 31, and 32. The TES algorithm is combined with an improved Water Vapor Scaling (WVS) atmospheric correction scheme to stabilize the retrieval during very warm and humid conditions. The MYD21C2 dataset is an 8-day composite LST product that uses an algorithm based on a simple averaging method. The algorithm calculates the average from all the cloud free &lt;a href&#x3D;&quot;http://doi.org/10.5067/MODIS/MYD21A1D.061&quot;&gt;MYD21A1D&lt;/a&gt; and &lt;a href&#x3D;&quot;http://doi.org/10.5067/MODIS/MYD21A1N.061&quot;&gt;MYD21A1N&lt;/a&gt; daily acquisitions from the 8-day period. Unlike the MOD21A1 data sets where the daytime and nighttime acquisitions are separate products, the MYD21A2 contains both daytime and nighttime acquisitions as separate Science Dataset (SDS) layers within a single Hierarchical Data Format (HDF) file. The LST, Quality Control (QC), view zenith angle, and viewing time have separate day and night SDS layers, while the values for the MODIS emissivity bands 29, 31, and 32 are the average of both the nighttime and daytime acquisitions. Additional details regarding the method used to create this Level 3 (L3) product are available in the Algorithm Theoretical Basis Document (ATBD). Known Issues: Users of MODIS LST products may notice an increase in occurrences of &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/displayissue?id&#x3D;117&quot;&gt;extreme high temperature outliers&lt;/a&gt; in the unfiltered MxD21 Version 6 and 6.1 products compared to the heritage MxD11 LST products. This can occur especially over desert regions like the Sahara where undetected cloud and dust can negatively impact both the MxD21 and MxD11 retrieval algorithms. * In the MxD11 LST products, these contaminated pixels are flagged in the algorithm and set to fill values in the output products based on differences in the band 32 and band 31 radiances used in the generalized split window algorithm. In the MxD21 LST products, values for the contaminated pixels are retained in the output products (and may result in overestimated temperatures), and users need to apply Quality Control (QC) filtering and other error analyses for filtering out bad values. High temperature outlier thresholds are not employed in MxD21 since it would potentially remove naturally occurring hot surface targets such as fires and lava flows. * High atmospheric aerosol optical depth (AOD) caused by vast dust outbreaks in the Sahara and other deserts highlighted in the example documentation are the primary reason for high outlier surface temperature values (and corresponding low emissivity values) in the MxD21 LST products. Future versions of the MxD21 product will include a dust flag from the MODIS aerosol product and/or brightness temperature look up tables to filter out contaminated dust pixels. It should be noted that in the MxD11B day/night algorithm products, more advanced cloud filtering is employed in the multi-day products based on a temporal analysis of historical LST over cloudy areas. This may result in more stringent filtering of dust contaminated pixels in these products. * In order to mitigate the impact of dust in the MxD21 V6 and 6.1 products, the science team recommends using a combination of the existing QC bits, emissivity values, and estimated product errors, to confidently remove bad pixels from analysis. For more details, refer to this dust and cloud contamination &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/data/userguide/MOD21_dust_QC_examples.pdf&quot;&gt;example documentation&lt;/a&gt;. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd21a2&quot;&gt;MYD21A2&lt;/h4&gt;
The MYD21A2 Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD21A2.061&quot;&gt;MYD21A2 Version 6.1&lt;/a&gt; data product. A new suite of Moderate Resolution Imaging Spectroradiometer (MODIS) Land Surface Temperature and Emissivity (LST&amp;amp;E) products are available in Collection 6. The MYD21 Land Surface Temperature (LST) algorithm differs from the algorithm of the &lt;a href&#x3D;&quot;https://doi.org/10.5067/modis/myd11_l2.006&quot;&gt;MYD11&lt;/a&gt; LST products, in that the MYD21 algorithm is based on the ASTER Temperature/Emissivity Separation (TES) technique, whereas the MYD11 uses the split-window technique. The MYD21 TES algorithm uses a physics-based algorithm to dynamically retrieve both the LST and spectral emissivity simultaneously from the MODIS thermal infrared bands 29, 31, and 32. The TES algorithm is combined with an improved Water Vapor Scaling (WVS) atmospheric correction scheme to stabilize the retrieval during very warm and humid conditions. The MYD21A2 dataset is an 8-day composite LST product that uses an algorithm based on a simple averaging method. The algorithm calculates the average from all the cloud free &lt;a href&#x3D;&quot;http://dx.doi.org/10.5067/MODIS/MYD21A1D.006&quot;&gt;MYD21A1D&lt;/a&gt; and &lt;a href&#x3D;&quot;http://dx.doi.org/10.5067/MODIS/MYD21A1N.006&quot;&gt;MYD21A1N&lt;/a&gt; daily acquisitions from the 8-day period. Unlike the MOD21A1 data sets where the daytime and nighttime acquisitions are separate products, the MYD21A2 contains both daytime and nighttime acquisitions as separate Science Dataset (SDS) layers within a single Hierarchical Data Format (HDF) file. The LST, Quality Control (QC), view zenith angle, and viewing time have separate day and night SDS layers, while the values for the MODIS emissivity bands 29, 31, and 32 are the average of both the nighttime and daytime acquisitions. MYD21A2 products are available two months after acquisition due to latency of data inputs. Additional details regarding the method used to create this Level 3 (L3) product are available in the Algorithm Theoretical Basis Document (ATBD). Known Issues: Users of MODIS LST products may notice an increase in occurrences of &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/displayissue?id&#x3D;117&quot;&gt;extreme high temperature outliers&lt;/a&gt; in the unfiltered MxD21 Version 6 and 6.1 products compared to the heritage MxD11 LST products. This can occur especially over desert regions like the Sahara where undetected cloud and dust can negatively impact both the MxD21 and MxD11 retrieval algorithms. * In the MxD11 LST products, these contaminated pixels are flagged in the algorithm and set to fill values in the output products based on differences in the band 32 and band 31 radiances used in the generalized split window algorithm. In the MxD21 LST products, values for the contaminated pixels are retained in the output products (and may result in overestimated temperatures), and users need to apply Quality Control (QC) filtering and other error analyses for filtering out bad values. High temperature outlier thresholds are not employed in MxD21 since it would potentially remove naturally occurring hot surface targets such as fires and lava flows. * High atmospheric aerosol optical depth (AOD) caused by vast dust outbreaks in the Sahara and other deserts highlighted in the example documentation are the primary reason for high outlier surface temperature values (and corresponding low emissivity values) in the MxD21 LST products. Future versions of the MxD21 product will include a dust flag from the MODIS aerosol product and/or brightness temperature look up tables to filter out contaminated dust pixels. It should be noted that in the MxD11B day/night algorithm products, more advanced cloud filtering is employed in the multi-day products based on a temporal analysis of historical LST over cloudy areas. This may result in more stringent filtering of dust contaminated pixels in these products. * In order to mitigate the impact of dust in the MxD21 V6 and 6.1 products, the science team recommends using a combination of the existing QC bits, emissivity values, and estimated product errors, to confidently remove bad pixels from analysis. For more details, refer to this dust and cloud contamination &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/data/userguide/MOD21_dust_QC_examples.pdf&quot;&gt;example documentation&lt;/a&gt;. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd21a2-1&quot;&gt;MYD21A2&lt;/h4&gt;
A suite of Moderate Resolution Imaging Spectroradiometer (MODIS) Land Surface Temperature and Emissivity (LST&amp;amp;E) products are available in Collection 6.1. The MYD21 Land Surface Temperature (LST) algorithm differs from the algorithm of the &lt;a href&#x3D;&quot;https://doi.org/10.5067/modis/myd11_l2.061&quot;&gt;MYD11&lt;/a&gt; LST products, in that the MYD21 algorithm is based on the ASTER Temperature/Emissivity Separation (TES) technique, whereas the MYD11 uses the split-window technique. The MYD21 TES algorithm uses a physics-based algorithm to dynamically retrieve both the LST and spectral emissivity simultaneously from the MODIS thermal infrared bands 29, 31, and 32. The TES algorithm is combined with an improved Water Vapor Scaling (WVS) atmospheric correction scheme to stabilize the retrieval during very warm and humid conditions. The MYD21A2 dataset is an 8-day composite LST product that uses an algorithm based on a simple averaging method. The algorithm calculates the average from all the cloud free &lt;a href&#x3D;&quot;http://doi.org/10.5067/MODIS/MYD21A1D.061&quot;&gt;MYD21A1D&lt;/a&gt; and &lt;a href&#x3D;&quot;http://doi.org/10.5067/MODIS/MYD21A1N.061&quot;&gt;MYD21A1N&lt;/a&gt; daily acquisitions from the 8-day period. Unlike the MOD21A1 data sets where the daytime and nighttime acquisitions are separate products, the MYD21A2 contains both daytime and nighttime acquisitions as separate Science Dataset (SDS) layers within a single Hierarchical Data Format (HDF) file. The LST, Quality Control (QC), view zenith angle, and viewing time have separate day and night SDS layers, while the values for the MODIS emissivity bands 29, 31, and 32 are the average of both the nighttime and daytime acquisitions. Additional details regarding the method used to create this Level 3 (L3) product are available in the Algorithm Theoretical Basis Document (ATBD). Known Issues: Users of MODIS LST products may notice an increase in occurrences of &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/displayissue?id&#x3D;117&quot;&gt;extreme high temperature outliers&lt;/a&gt; in the unfiltered MxD21 Version 6 and 6.1 products compared to the heritage MxD11 LST products. This can occur especially over desert regions like the Sahara where undetected cloud and dust can negatively impact both the MxD21 and MxD11 retrieval algorithms. * In the MxD11 LST products, these contaminated pixels are flagged in the algorithm and set to fill values in the output products based on differences in the band 32 and band 31 radiances used in the generalized split window algorithm. In the MxD21 LST products, values for the contaminated pixels are retained in the output products (and may result in overestimated temperatures), and users need to apply Quality Control (QC) filtering and other error analyses for filtering out bad values. High temperature outlier thresholds are not employed in MxD21 since it would potentially remove naturally occurring hot surface targets such as fires and lava flows. * High atmospheric aerosol optical depth (AOD) caused by vast dust outbreaks in the Sahara and other deserts highlighted in the example documentation are the primary reason for high outlier surface temperature values (and corresponding low emissivity values) in the MxD21 LST products. Future versions of the MxD21 product will include a dust flag from the MODIS aerosol product and/or brightness temperature look up tables to filter out contaminated dust pixels. It should be noted that in the MxD11B day/night algorithm products, more advanced cloud filtering is employed in the multi-day products based on a temporal analysis of historical LST over cloudy areas. This may result in more stringent filtering of dust contaminated pixels in these products. * In order to mitigate the impact of dust in the MxD21 V6 and 6.1 products, the science team recommends using a combination of the existing QC bits, emissivity values, and estimated product errors, to confidently remove bad pixels from analysis. For more details, refer to this dust and cloud contamination &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/data/userguide/MOD21_dust_QC_examples.pdf&quot;&gt;example documentation&lt;/a&gt;. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd21c1&quot;&gt;MYD21C1&lt;/h4&gt;
A new suite of MODIS Land Surface Temperature and Emissivity (LST&amp;amp;E) products are available in Collection 6.1. The MYD21 LST algorithm differs from the algorithm of the &lt;a href&#x3D;&quot;https://doi.org/10.5067/modis/myd11_l2.061&quot;&gt;MYD11&lt;/a&gt; LST products, in that the MYD21 algorithm is based on the ASTER Temperature/Emissivity Separation (TES) technique, whereas the MYD11 uses the split-window technique. The MYD21 TES algorithm uses a physics-based algorithm to retrieve dynamically both the LST and spectral emissivity simultaneously from the three MODIS thermal infrared bands 29, 31, and 32. The TES algorithm is combined with an improved Water Vapor Scaling (WVS) atmospheric correction scheme to stabilize the retrieval during very warm and humid conditions. The MYD21C1 Version 6.1 dataset is produced daily from daytime Level 2 Gridded (L2G) intermediate LST products. The L2G process maps the daily &lt;a href&#x3D;&quot;http://doi.org/10.5067/MODIS/MYD21.061&quot;&gt;MYD21&lt;/a&gt; swath granules onto a sinusoidal MODIS grid and stores all observations falling over a gridded cell for a given day. The MOD21C1 algorithm sorts through all these observations for each cell and estimates the final LST value as an average from all observations that are cloud free and have good LST&amp;amp;E accuracies. The daytime average is weighted by the observation coverage for that cell. Only observations having observation coverage more than a certain threshold (15%) are considered for this averaging. The MYD21C1 product contains seven Science Datasets (SDS), which include the calculated LST as well as quality control, the three emissivity bands, view zenith angle, and time of observation. Additional details regarding the methodology used to create this Level 3 (L3) product are available in the Algorithm Theoretical Basis Document (ATBD). Known Issues: Users of MODIS LST products may notice an increase in occurrences of &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/displayissue?id&#x3D;117&quot;&gt;extreme high temperature outliers&lt;/a&gt; in the unfiltered MxD21 Version 6 and 6.1 products compared to the heritage MxD11 LST products. This can occur especially over desert regions like the Sahara where undetected cloud and dust can negatively impact both the MxD21 and MxD11 retrieval algorithms. * In the MxD11 LST products, these contaminated pixels are flagged in the algorithm and set to fill values in the output products based on differences in the band 32 and band 31 radiances used in the generalized split window algorithm. In the MxD21 LST products, values for the contaminated pixels are retained in the output products (and may result in overestimated temperatures), and users need to apply Quality Control (QC) filtering and other error analyses for filtering out bad values. High temperature outlier thresholds are not employed in MxD21 since it would potentially remove naturally occurring hot surface targets such as fires and lava flows. * High atmospheric aerosol optical depth (AOD) caused by vast dust outbreaks in the Sahara and other deserts highlighted in the example documentation are the primary reason for high outlier surface temperature values (and corresponding low emissivity values) in the MxD21 LST products. Future versions of the MxD21 product will include a dust flag from the MODIS aerosol product and/or brightness temperature look up tables to filter out contaminated dust pixels. It should be noted that in the MxD11B day/night algorithm products, more advanced cloud filtering is employed in the multi-day products based on a temporal analysis of historical LST over cloudy areas. This may result in more stringent filtering of dust contaminated pixels in these products. * In order to mitigate the impact of dust in the MxD21 V6 and 6.1 products, the science team recommends using a combination of the existing QC bits, emissivity values, and estimated product errors, to confidently remove bad pixels from analysis. For more details, refer to this dust and cloud contamination &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/data/userguide/MOD21_dust_QC_examples.pdf&quot;&gt;example documentation&lt;/a&gt;. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd21a1d&quot;&gt;MYD21A1D&lt;/h4&gt;
The MYD21A1D Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD21A1D.061&quot;&gt;MYD21A1D Version 6.1&lt;/a&gt; data product. A new suite of MODIS Land Surface Temperature and Emissivity (LST&amp;amp;E) products are available in Collection 6. The MYD21 LST algorithm differs from the algorithm of the &lt;a href&#x3D;&quot;https://doi.org/10.5067/modis/myd11_l2.006&quot;&gt;MYD11&lt;/a&gt; LST products, in that the MYD21 algorithm is based on the ASTER Temperature/Emissivity Separation (TES) technique, whereas the MYD11 uses the split-window technique. The MYD21 TES algorithm uses a physics-based algorithm to retrieve dynamically both the LST and spectral emissivity simultaneously from the three MODIS thermal infrared bands 29, 31, and 32. The TES algorithm is combined with an improved Water Vapor Scaling (WVS) atmospheric correction scheme to stabilize the retrieval during very warm and humid conditions. The MYD21A1D dataset is produced daily from daytime Level 2 Gridded (L2G) intermediate LST products. The L2G process maps the daily &lt;a href&#x3D;&quot;http://doi.org/10.5067/MODIS/MYD21.006&quot;&gt;MYD21&lt;/a&gt; swath granules onto a sinusoidal MODIS grid and stores all observations falling over a gridded cell for a given day. The MOD21A1 algorithm sorts through all these observations for each cell and estimates the final LST value as an average from all observations that are cloud free and have good LST&amp;amp;E accuracies. The daytime average is weighted by the observation coverage for that cell. Only observations having observation coverage more than a certain threshold (15%) are considered for this averaging. The MYD21A1D product contains seven Science Datasets (SDS), which include the calculated LST as well as quality control, the three emissivity bands, view zenith angle, and time of observation. MYD21A1D products are available two months after acquisition due to latency of data inputs. Additional details regarding the methodology used to create this Level 3 (L3) product are available in the Algorithm Theoretical Basis Document [ATBD). Known Issues: Users of MODIS LST products may notice an increase in occurrences of &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/displayissue?id&#x3D;117&quot;&gt;extreme high temperature outliers&lt;/a&gt; in the unfiltered MxD21 Version 6 and 6.1 products compared to the heritage MxD11 LST products. This can occur especially over desert regions like the Sahara where undetected cloud and dust can negatively impact both the MxD21 and MxD11 retrieval algorithms. * In the MxD11 LST products, these contaminated pixels are flagged in the algorithm and set to fill values in the output products based on differences in the band 32 and band 31 radiances used in the generalized split window algorithm. In the MxD21 LST products, values for the contaminated pixels are retained in the output products (and may result in overestimated temperatures), and users need to apply Quality Control (QC) filtering and other error analyses for filtering out bad values. High temperature outlier thresholds are not employed in MxD21 since it would potentially remove naturally occurring hot surface targets such as fires and lava flows. * High atmospheric aerosol optical depth (AOD) caused by vast dust outbreaks in the Sahara and other deserts highlighted in the example documentation are the primary reason for high outlier surface temperature values (and corresponding low emissivity values) in the MxD21 LST products. Future versions of the MxD21 product will include a dust flag from the MODIS aerosol product and/or brightness temperature look up tables to filter out contaminated dust pixels. It should be noted that in the MxD11B day/night algorithm products, more advanced cloud filtering is employed in the multi-day products based on a temporal analysis of historical LST over cloudy areas. This may result in more stringent filtering of dust contaminated pixels in these products. * In order to mitigate the impact of dust in the MxD21 V6 and 6.1 products, the science team recommends using a combination of the existing QC bits, emissivity values, and estimated product errors, to confidently remove bad pixels from analysis. For more details, refer to this dust and cloud contamination &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/data/userguide/MOD21_dust_QC_examples.pdf&quot;&gt;example documentation&lt;/a&gt;. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd21a1d-1&quot;&gt;MYD21A1D&lt;/h4&gt;
A suite of MODIS Land Surface Temperature and Emissivity (LST&amp;amp;E) products are available in Collection 6.1. The MYD21 LST algorithm differs from the algorithm of the &lt;a href&#x3D;&quot;https://doi.org/10.5067/modis/myd11_l2.061&quot;&gt;MYD11&lt;/a&gt; LST products, in that the MYD21 algorithm is based on the ASTER Temperature/Emissivity Separation (TES) technique, whereas the MYD11 uses the split-window technique. The MYD21 TES algorithm uses a physics-based algorithm to retrieve dynamically both the LST and spectral emissivity simultaneously from the three MODIS thermal infrared bands 29, 31, and 32. The TES algorithm is combined with an improved Water Vapor Scaling (WVS) atmospheric correction scheme to stabilize the retrieval during very warm and humid conditions. The MYD21A1D dataset is produced daily from daytime Level 2 Gridded (L2G) intermediate LST products. The L2G process maps the daily &lt;a href&#x3D;&quot;http://doi.org/10.5067/MODIS/MYD21.061&quot;&gt;MYD21&lt;/a&gt; swath granules onto a sinusoidal MODIS grid and stores all observations falling over a gridded cell for a given day. The MOD21A1 algorithm sorts through all these observations for each cell and estimates the final LST value as an average from all observations that are cloud free and have good LST&amp;amp;E accuracies. The daytime average is weighted by the observation coverage for that cell. Only observations having observation coverage more than a certain threshold (15%) are considered for this averaging. The MYD21A1D product contains seven Science Datasets (SDS), which include the calculated LST as well as quality control, the three emissivity bands, view zenith angle, and time of observation. Additional details regarding the methodology used to create this Level 3 (L3) product are available in the Algorithm Theoretical Basis Document (ATBD). Known Issues: Users of MODIS LST products may notice an increase in occurrences of &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/displayissue?id&#x3D;117&quot;&gt;extreme high temperature outliers&lt;/a&gt; in the unfiltered MxD21 Version 6 and 6.1 products compared to the heritage MxD11 LST products. This can occur especially over desert regions like the Sahara where undetected cloud and dust can negatively impact both the MxD21 and MxD11 retrieval algorithms. * In the MxD11 LST products, these contaminated pixels are flagged in the algorithm and set to fill values in the output products based on differences in the band 32 and band 31 radiances used in the generalized split window algorithm. In the MxD21 LST products, values for the contaminated pixels are retained in the output products (and may result in overestimated temperatures), and users need to apply Quality Control (QC) filtering and other error analyses for filtering out bad values. High temperature outlier thresholds are not employed in MxD21 since it would potentially remove naturally occurring hot surface targets such as fires and lava flows. * High atmospheric aerosol optical depth (AOD) caused by vast dust outbreaks in the Sahara and other deserts highlighted in the example documentation are the primary reason for high outlier surface temperature values (and corresponding low emissivity values) in the MxD21 LST products. Future versions of the MxD21 product will include a dust flag from the MODIS aerosol product and/or brightness temperature look up tables to filter out contaminated dust pixels. It should be noted that in the MxD11B day/night algorithm products, more advanced cloud filtering is employed in the multi-day products based on a temporal analysis of historical LST over cloudy areas. This may result in more stringent filtering of dust contaminated pixels in these products. * In order to mitigate the impact of dust in the MxD21 V6 and 6.1 products, the science team recommends using a combination of the existing QC bits, emissivity values, and estimated product errors, to confidently remove bad pixels from analysis. For more details, refer to this dust and cloud contamination &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/data/userguide/MOD21_dust_QC_examples.pdf&quot;&gt;example documentation&lt;/a&gt;. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd21a1n&quot;&gt;MYD21A1N&lt;/h4&gt;
The MYD21A1N Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD21A1N.061&quot;&gt;MYD21A1N Version 6.1&lt;/a&gt; data product. A new suite of Moderate Resolution Imaging Spectroradiometer (MODIS) Land Surface Temperature and Emissivity (LST&amp;amp;E) products are available in Collection 6. The MYD21 Land Surface Temperature (LST) algorithm differs from the algorithm of the &lt;a href&#x3D;&quot;https://doi.org/10.5067/modis/myd11_l2.006&quot;&gt;MYD11&lt;/a&gt; LST products, in that the MYD21 algorithm is based on the ASTER Temperature/Emissivity Separation (TES) technique, whereas the MYD11 uses the split-window technique. The MYD21 TES algorithm uses a physics-based algorithm to dynamically retrieve both the LST and spectral emissivity simultaneously from the MODIS thermal infrared bands 29, 31, and 32. The TES algorithm is combined with an improved Water Vapor Scaling (WVS) atmospheric correction scheme to stabilize the retrieval during very warm and humid conditions. The MYD21A1N dataset is produced daily from nighttime Level 2 Gridded (L2G) intermediate LST products. The L2G process maps the daily &lt;a href&#x3D;&quot;http://dx.doi.org/10.5067/MODIS/MYD21.006&quot;&gt;MYD21&lt;/a&gt; swath granules onto a sinusoidal MODIS grid and stores all observations falling over a gridded cell for a given day. The MOD21A1 algorithm sorts through all these observations for each cell and estimates the final LST value as an average from all observations that are cloud free and have good LST&amp;amp;E accuracies. The nighttime average is weighted by the observation coverage for that cell. Only observations having an observation coverage greater than a 15% threshold are considered. The MYD21A1N product contains seven Science Datasets (SDS), which include the calculated LST as well as quality control, the three emissivity bands, view zenith angle, and time of observation. MYD21A1N products are available two months after acquisition due to latency of data inputs. Additional details regarding the methodology used to create this Level 3 (L3) product are available in the Algorithm Theoretical Basis Document (ATBD). Known Issues: Users of MODIS LST products may notice an increase in occurrences of &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/displayissue?id&#x3D;117&quot;&gt;extreme high temperature outliers&lt;/a&gt; in the unfiltered MxD21 Version 6 and 6.1 products compared to the heritage MxD11 LST products. This can occur especially over desert regions like the Sahara where undetected cloud and dust can negatively impact both the MxD21 and MxD11 retrieval algorithms. * In the MxD11 LST products, these contaminated pixels are flagged in the algorithm and set to fill values in the output products based on differences in the band 32 and band 31 radiances used in the generalized split window algorithm. In the MxD21 LST products, values for the contaminated pixels are retained in the output products (and may result in overestimated temperatures), and users need to apply Quality Control (QC) filtering and other error analyses for filtering out bad values. High temperature outlier thresholds are not employed in MxD21 since it would potentially remove naturally occurring hot surface targets such as fires and lava flows. * High atmospheric aerosol optical depth (AOD) caused by vast dust outbreaks in the Sahara and other deserts highlighted in the example documentation are the primary reason for high outlier surface temperature values (and corresponding low emissivity values) in the MxD21 LST products. Future versions of the MxD21 product will include a dust flag from the MODIS aerosol product and/or brightness temperature look up tables to filter out contaminated dust pixels. It should be noted that in the MxD11B day/night algorithm products, more advanced cloud filtering is employed in the multi-day products based on a temporal analysis of historical LST over cloudy areas. This may result in more stringent filtering of dust contaminated pixels in these products. * In order to mitigate the impact of dust in the MxD21 V6 and 6.1 products, the science team recommends using a combination of the existing QC bits, emissivity values, and estimated product errors, to confidently remove bad pixels from analysis. For more details, refer to this dust and cloud contamination &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/data/userguide/MOD21_dust_QC_examples.pdf&quot;&gt;example documentation&lt;/a&gt;. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd11_l2&quot;&gt;MYD11_L2&lt;/h4&gt;
The MYD11_L2 Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD11_L2.061&quot;&gt;MYD11_L2 Version 6.1&lt;/a&gt; data product. The MYD11_L2 Version 6 swath product provides per-pixel Land Surface Temperature and Emissivity (LST&amp;amp;E) with a pixel size of 1,000 meters (m). The product is produced daily in 5-minute temporal increments of satellite acquisition using the generalized split-window algorithm. MYD11_L2 is a Level 2 product which provides the input for the Level 3 products. Provided in each MYD11_L2 file are LST, quality control assessment, error estimates, bands 31 and 32 emissivities, zenith angle of the pixel view, observation time, and the geographic coordinates for every five scan lines and samples. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd11_l2-1&quot;&gt;MYD11_L2&lt;/h4&gt;
The Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Land Surface Temperature/Emissivity 5-Minute (MYD11_L2) Version 6.1 swath product provides per-pixel Land Surface Temperature and Emissivity (LST&amp;amp;E) with a pixel size of 1,000 meters (m). The product is produced daily in 5-minute temporal increments of satellite acquisition using the generalized split-window algorithm. MYD11_L2 is a Level 2 product which provides the input for the Level 3 products. Provided in each MYD11_L2 file are LST, quality control assessment, error estimates, bands 31 and 32 emissivities, zenith angle of the pixel view, observation time, and the geographic coordinates for every five scan lines and samples. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd11c2&quot;&gt;MYD11C2&lt;/h4&gt;
The MYD11C2 Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD11C2.061&quot;&gt;MYD11C2 Version 6.1&lt;/a&gt; data product. The MYD11C2 Version 6 product provides Land Surface Temperature and Emissivity (LST&amp;amp;E) values in a 0.05 degree (5,600 meters at the equator) latitude/longitude Climate Modeling Grid (CMG). A CMG granule follows a geographic grid with 7,200 columns and 3,600 rows, representing the entire globe. The LST&amp;amp;E values in the MYD11C2 product are derived by compositing and averaging the values from the corresponding eight &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD11C1.006&quot;&gt;MYD11C1&lt;/a&gt; daily files. The MYD11C2 granule consists of 17 layers. Each MYD11C2 product consists of the following layers for daytime and nighttime observations: LSTs, quality control assessments, observation times, view zenith angles, and number of clear-sky observations along with percentage of land in the grid and emissivities from bands 20, 22, 23, 29, 31, and 32. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd11c2-1&quot;&gt;MYD11C2&lt;/h4&gt;
The Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Land Surface Temperature/Emissivity 8-Day (MYD11C2) Version 6.1 product provides Land Surface Temperature and Emissivity (LST&amp;amp;E) values in a 0.05 degree (5,600 meters at the equator) latitude/longitude Climate Modeling Grid (CMG). A CMG granule follows a geographic grid with 7,200 columns and 3,600 rows, representing the entire globe. The LST&amp;amp;E values in the MYD11C2 product are derived by compositing and averaging the values from the corresponding eight &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD11C1.061&quot;&gt;MYD11C1&lt;/a&gt; daily files. The MYD11C2 granule consists of 17 layers. Each MYD11C2 product consists of the following layers for daytime and nighttime observations: LSTs, quality control assessments, observation times, view zenith angles, and number of clear-sky observations along with percentage of land in the grid and emissivities from bands 20, 22, 23, 29, 31, and 32. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd11a2&quot;&gt;MYD11A2&lt;/h4&gt;
The MYD11A2 Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD11A2.061&quot;&gt;MYD11A2 Version 6.1&lt;/a&gt; data product. The MYD11A2 Version 6 product provides an average 8-day per-pixel Land Surface Temperature and Emissivity (LST&amp;amp;E) with a 1 kilometer (km) spatial resolution in a 1,200 by 1,200 km grid. Each pixel value in the MYD11A2 is a simple average of all the corresponding &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD11A1.006&quot;&gt;MYD11A1&lt;/a&gt; LST pixels collected within that 8-day period. The 8-day compositing period was chosen because twice that period is the exact ground track repeat period of the Terra and Aqua platforms. Provided along with the daytime and nighttime surface temperature bands are associated quality control assessments, observation times, view zenith angles, and clear-sky coverages along with bands 31 and 32 emissivities from land cover types. Known Issues For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd11a2-1&quot;&gt;MYD11A2&lt;/h4&gt;
The Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Land Surface Temperature/Emissivity 8-Day (MYD11A2) Version 6.1 product provides an average 8-day per-pixel Land Surface Temperature and Emissivity (LST&amp;amp;E) with a 1 kilometer (km) spatial resolution in a 1,200 by 1,200 km grid. Each pixel value in the MYD11A2 is a simple average of all the corresponding &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD11A1.061&quot;&gt;MYD11A1&lt;/a&gt; LST pixels collected within that 8-day period. The 8-day compositing period was chosen because twice that period is the exact ground track repeat period of the Terra and Aqua platforms. Provided along with the daytime and nighttime surface temperature bands are associated quality control assessments, observation times, view zenith angles, and clear-sky coverages along with bands 31 and 32 emissivities from land cover types. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd11b2&quot;&gt;MYD11B2&lt;/h4&gt;
The MYD11B2 Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD11B2.061&quot;&gt;MYD11B2 Version 6.1&lt;/a&gt; data product. The MYD11B2 Version 6 product provides an average 8-day per pixel Land Surface Temperature and Emissivity (LST&amp;amp;E) in a 1,200 by 1,200 kilometer (km) tile with a pixel size of 5,600 meters (m). Each temperature and emissivity pixel value in the MYD11B2 is a simple average of all the corresponding values from the LST&amp;amp;E values from the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD11B1.006&quot;&gt;MYD11B1&lt;/a&gt; product collected during that 8-day period. Each MYD11B2 granule consists of 19 layers including daytime and nighttime layers for LSTs, quality control assessments, observation times, view zenith angles, and number of clear sky observations along with percentage of land in the tile and emissivities from bands 20, 22, 23, 29, 31, and 32. Unique to the MOD11B products are additional day and night LST layers generated from band 31 of the corresponding 1 km &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD11_L2.006&quot;&gt;MYD11_L2&lt;/a&gt; swath product aggregated to the 6 km grid. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd11b2-1&quot;&gt;MYD11B2&lt;/h4&gt;
The Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Land Surface Temperature/Emissivity 8-Day (MYD11B2) Version 6.1 product provides an average 8-day per pixel Land Surface Temperature and Emissivity (LST&amp;amp;E) in a 1,200 by 1,200 kilometer (km) tile with a pixel size of 5,600 meters (m). Each temperature and emissivity pixel value in the MYD11B2 is a simple average of all the corresponding values from the LST&amp;amp;E values from the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD11B1.061&quot;&gt;MYD11B1&lt;/a&gt; product collected during that 8-day period. Each MYD11B2 granule consists of 19 layers including daytime and nighttime layers for LSTs, quality control assessments, observation times, view zenith angles, and number of clear sky observations along with percentage of land in the tile and emissivities from bands 20, 22, 23, 29, 31, and 32. Unique to the MOD11B products are additional day and night LST layers generated from band 31 of the corresponding 1 km &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD11_L2.061&quot;&gt;MYD11_L2&lt;/a&gt; swath product aggregated to the 6 km grid. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd11c1&quot;&gt;MYD11C1&lt;/h4&gt;
The MYD11C1 Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD11C1.061&quot;&gt;MYD11C1 Version 6.1&lt;/a&gt; data product. The MYD11C1 Version 6 product provides daily Land Surface Temperature and Emissivity (LST&amp;amp;E) values in a 0.05 degree (5,600 meters at the equator) latitude/longitude Climate Modeling Grid (CMG). The MYD11C1 product is directly derived from the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD11B1.006&quot;&gt;MYD11B1&lt;/a&gt; product. A CMG granule follows a Geographic grid, having 7,200 columns and 3,600 rows, which represent the entire globe. Each MYD11C1 product consists of the following layers for daytime and nighttime observations: LSTs, quality control assessments, observation times, view zenith angles, number of clear-sky observations, and emissivities from bands 20, 22, 23, 29, 31, and 32 (bands 31 and 32 are daytime only) along with the percentage of land in the grid. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd11c1-1&quot;&gt;MYD11C1&lt;/h4&gt;
The Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Land Surface Temperature/Emissivity Daily (MYD11C1) Version 6.1 product provides daily Land Surface Temperature and Emissivity (LST&amp;amp;E) values in a 0.05 degree (5,600 meters at the equator) latitude/longitude Climate Modeling Grid (CMG). The MYD11C1 product is directly derived from the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD11B1.061&quot;&gt;MYD11B1&lt;/a&gt; product. A CMG granule follows a Geographic grid, having 7,200 columns and 3,600 rows, which represent the entire globe. Each MYD11C1 product consists of the following layers for daytime and nighttime observations: LSTs, quality control assessments, observation times, view zenith angles, number of clear-sky observations, and emissivities from bands 20, 22, 23, 29, 31, and 32 (bands 31 and 32 are daytime only) along with the percentage of land in the grid. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd11a1&quot;&gt;MYD11A1&lt;/h4&gt;
The MYD11A1 Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD11A1.061&quot;&gt;MYD11A1 Version 6.1&lt;/a&gt; data product. The MYD11A1 Version 6 product provides daily per-pixel Land Surface Temperature and Emissivity (LST&amp;amp;E) with 1 kilometer (km) spatial resolution in a 1,200 by 1,200 km grid. The pixel temperature value is derived from the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD11_L2.006&quot;&gt;MYD11_L2&lt;/a&gt; swath product. Above 30 degrees latitude, some pixels may have multiple observations where the criteria for clear-sky are met. When this occurs, the pixel value is a result of the average of all qualifying observations. Provided along with the daytime and nighttime surface temperature bands are associated quality control assessments, observation times, view zenith angles, and clear-sky coverages along with bands 31 and 32 emissivities from land cover types. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd11a1-1&quot;&gt;MYD11A1&lt;/h4&gt;
The Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Land Surface Temperature/Emissivity Daily (MYD11A1) Version 6.1 product provides daily per-pixel Land Surface Temperature and Emissivity (LST&amp;amp;E) with 1 kilometer (km) spatial resolution in a 1,200 by 1,200 km grid. The pixel temperature value is derived from the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD11_L2.061&quot;&gt;MYD11_L2&lt;/a&gt; swath product. Above 30 degrees latitude, some pixels may have multiple observations where the criteria for clear-sky are met. When this occurs, the pixel value is a result of the average of all qualifying observations. Provided along with the daytime and nighttime surface temperature bands are associated quality control assessments, observation times, view zenith angles, and clear-sky coverages along with bands 31 and 32 emissivities from land cover types. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd11b1&quot;&gt;MYD11B1&lt;/h4&gt;
The MYD11B1 Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD11B1.061&quot;&gt;MYD11B1 Version 6.1&lt;/a&gt; data product. The MYD11B1 Version 6 product provides daily per pixel Land Surface Temperature and Emissivity (LST&amp;amp;E) in a 1,200 by 1,200 kilometer (km) tile with a pixel size of 5,600 meters (m). Each MOD11B1 granule consists of the following layers for daytime and nighttime observations: LSTs, quality control assessments, observation times, view zenith angles, number of clear-sky observations, and emissivities from bands 20, 22, 23, 29, 31, and 32 (bands 31 and 32 are daytime only) along with the percentage of land in the tile. Unique to the MYD11B products are additional day and night LST layers generated from band 31 of the corresponding 1 km &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD11_L2.006&quot;&gt;MYD11_L2&lt;/a&gt; swath product aggregated to the 6 km grid. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd11b1-1&quot;&gt;MYD11B1&lt;/h4&gt;
The Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Land Surface Temperature/Emissivity Daily (MYD11B1) Version 6.1 product provides daily per pixel Land Surface Temperature and Emissivity (LST&amp;amp;E) in a 1,200 by 1,200 kilometer (km) tile with a pixel size of 5,600 meters (m). Each MOD11B1 granule consists of the following layers for daytime and nighttime observations: LSTs, quality control assessments, observation times, view zenith angles, number of clear-sky observations, and emissivities from bands 20, 22, 23, 29, 31, and 32 (bands 31 and 32 are daytime only) along with the percentage of land in the tile. Unique to the MYD11B products are additional day and night LST layers generated from band 31 of the corresponding 1 km &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD11_L2.061&quot;&gt;MYD11_L2&lt;/a&gt; swath product aggregated to the 6 km grid. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd11c3&quot;&gt;MYD11C3&lt;/h4&gt;
The MYD11C3 Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD11C3.061&quot;&gt;MYD11C3 Version 6.1&lt;/a&gt; data product. The MYD11C3 Version 6 product provides monthly Land Surface Temperature and Emissivity (LST&amp;amp;E) values in a 0.05 degree (5,600 meters at the equator) latitude/longitude Climate Modeling Grid (CMG). A CMG granule is a geographic grid with 7,200 columns and 3,600 rows representing the entire globe. The LST&amp;amp;E values in the MYD11C3 product are derived by compositing and averaging the values from the corresponding month of &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD11C1.006&quot;&gt;MYD11C1&lt;/a&gt; daily files. Each MYD11C3 product consists of the following layers for daytime and nighttime observations: LSTs, quality control assessments, observation times, view zenith angles, and number of clear-sky observations along with percentage of land in the grid and emissivities from bands 20, 22, 23, 29, 31, and 32. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd11c3-1&quot;&gt;MYD11C3&lt;/h4&gt;
The Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Land Surface Temperature/Emissivity Monthly (MYD11C3) Version 6.1 product provides monthly Land Surface Temperature and Emissivity (LST&amp;amp;E) values in a 0.05 degree (5,600 meters at the equator) latitude/longitude Climate Modeling Grid (CMG). A CMG granule is a geographic grid with 7,200 columns and 3,600 rows representing the entire globe. The LST&amp;amp;E values in the MYD11C3 product are derived by compositing and averaging the values from the corresponding month of &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD11C1.061&quot;&gt;MYD11C1&lt;/a&gt; daily files. Each MYD11C3 product consists of the following layers for daytime and nighttime observations: LSTs, quality control assessments, observation times, view zenith angles, and number of clear-sky observations along with percentage of land in the grid and emissivities from bands 20, 22, 23, 29, 31, and 32. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd11b3&quot;&gt;MYD11B3&lt;/h4&gt;
The MYD11B3 Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD11B3.061&quot;&gt;MYD11B3 Version 6.1&lt;/a&gt; data product. The MYD11B3 Version 6 product provides average monthly per pixel Land Surface Temperature and Emissivity (LST&amp;amp;E) in a 1,200 by 1,200 kilometer (km) tile with a pixel size of 5,600 meters (m). Each LST&amp;amp;E pixel value in the MYD11B3 is a simple average of all the corresponding values from the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD11B1.006&quot;&gt;MYD11B1&lt;/a&gt; collected during the month period. Each MYD11B3 granule consists of 19 layers including daytime and nighttime layers for LSTs, quality control assessments, observation times, view zenith angles, and number of clear sky observations along with percentage of land in the tile and emissivities from bands 20, 22, 23, 29, 31, and 32. Unique to the MYD11B products are additional day and night LST layers generated from band 31 of the corresponding 1 km &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD11_L2.006&quot;&gt;MYD11_L2&lt;/a&gt; swath product aggregated to the 6 km grid. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd11b3-1&quot;&gt;MYD11B3&lt;/h4&gt;
The Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Land Surface Temperature/Emissivity Monthly (MYD11B3) Version 6.1 product provides average monthly per pixel Land Surface Temperature and Emissivity (LST&amp;amp;E) in a 1,200 by 1,200 kilometer (km) tile with a pixel size of 5,600 meters (m). Each LST&amp;amp;E pixel value in the MYD11B3 is a simple average of all the corresponding values from the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD11B1.061&quot;&gt;MYD11B1&lt;/a&gt; collected during the month period. Each MYD11B3 granule consists of 19 layers including daytime and nighttime layers for LSTs, quality control assessments, observation times, view zenith angles, and number of clear sky observations along with percentage of land in the tile and emissivities from bands 20, 22, 23, 29, 31, and 32. Unique to the MYD11B products are additional day and night LST layers generated from band 31 of the corresponding 1 km &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD11_L2.061&quot;&gt;MYD11_L2&lt;/a&gt; swath product aggregated to the 6 km grid. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd15a2h&quot;&gt;MYD15A2H&lt;/h4&gt;
The MYD15A2H Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD15A2H.061&quot;&gt;MYD15A2H Version 6.1&lt;/a&gt; data product. The MYD15A2H Version 6 Moderate Resolution Imaging Spectroradiometer (MODIS) combined Leaf Area Index (LAI) and Fraction of Photosynthetically Active Radiation (FPAR) product is an 8-day composite dataset with 500 meter (m) pixel size. The algorithm chooses the “best” pixel available from all the acquisitions of the Aqua sensor from within the 8-day period. LAI is defined as the one-sided green leaf area per unit ground area in broadleaf canopies and as one-half the total needle surface area per unit ground area in coniferous canopies. FPAR is defined as the fraction of incident photosynthetically active radiation (400-700 nanometers (nm)) absorbed by the green elements of a vegetation canopy. Science Datasets (SDS) in the Level 4 (L4) MYD15A2H product include LAI, FPAR, two quality layers, and standard deviation for LAI and FPAR. Two low resolution browse images, LAI and FPAR, are also available for each MYD15A2H granule. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd15a2h-1&quot;&gt;MYD15A2H&lt;/h4&gt;
The MYD15A2H Version 6.1 Moderate Resolution Imaging Spectroradiometer (MODIS) combined Leaf Area Index (LAI) and Fraction of Photosynthetically Active Radiation (FPAR) product is an 8-day composite dataset with 500 meter (m) pixel size. The algorithm chooses the &amp;quot;best&amp;quot; pixel available from all the acquisitions of the Aqua sensor from within the 8-day period. LAI is defined as the one-sided green leaf area per unit ground area in broadleaf canopies and as one-half the total needle surface area per unit ground area in coniferous canopies. FPAR is defined as the fraction of incident photosynthetically active radiation (400-700 nanometers (nm)) absorbed by the green elements of a vegetation canopy. Science Datasets (SDS) in the Level 4 (L4) MYD15A2H product include LAI, FPAR, two quality layers, and standard deviation for LAI and FPAR. Two low resolution browse images, LAI and FPAR, are also available for each MYD15A2H granule. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd16a2&quot;&gt;MYD16A2&lt;/h4&gt;
The MYD16A2 Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD16A2.061&quot;&gt;MYD16A2 Version 6.1&lt;/a&gt; data product. The MYD16A2 Version 6 Evapotranspiration/Latent Heat Flux product is an 8-day composite dataset produced at 500 meter (m) pixel resolution. The improved algorithm is based on the logic of the Penman-Monteith equation, which includes inputs of daily meteorological reanalysis data along with Moderate Resolution Imaging Spectroradiometer (MODIS) remotely sensed data products such as vegetation property dynamics, albedo, and land cover. Provided in the MYD16A2 product are layers for composited Evapotranspiration (ET), Latent Heat Flux (LE), Potential ET (PET) and Potential LE (PLE) along with a quality control layer. Two low resolution browse images, ET and LE, are also available for each MYD16A2 granule. The pixel values for the two Evapotranspiration layers (ET and PET) are the sum of all eight days within the composite period, and the pixel values for the two Latent Heat layers (LE and PLE) are the average of all eight days within the composite period. Note that the last acquisition period of each year is a 5 or 6-day composite period depending on the year. Known Issues: Operational and uncertainty issues are provided under Section 3 in the User Guide. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd16a2-1&quot;&gt;MYD16A2&lt;/h4&gt;
The Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) MYD16A2 Version 6.1 Evapotranspiration/Latent Heat Flux product is an 8-day composite dataset produced at 500 meter (m) pixel resolution. The improved algorithm is based on the logic of the Penman-Monteith equation, which includes inputs of daily meteorological reanalysis data along with MODIS remotely sensed data products such as vegetation property dynamics, albedo, and land cover. Provided in the MYD16A2 product are layers for composited Evapotranspiration (ET), Latent Heat Flux (LE), Potential ET (PET) and Potential LE (PLE) along with a quality control layer. Two low resolution browse images, ET and LE, are also available for each MYD16A2 granule. The pixel values for the two Evapotranspiration layers (ET and PET) are the sum of all eight days within the composite period, and the pixel values for the two Latent Heat layers (LE and PLE) are the average of all eight days within the composite period. Note that the last acquisition period of each year is a 5 or 6-day composite period depending on the year. Known Issues: Operational and uncertainty issues are provided under Section 3 in the User Guide. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd16a2gf&quot;&gt;MYD16A2GF&lt;/h4&gt;
The MYD16A2GF Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD16A2GF.061&quot;&gt;MYD16A2GF Version 6.1&lt;/a&gt; data product. The MYD16A2GF Version 6 Evapotranspiration/Latent Heat Flux (ET/LE) product is a year-end gap-filled 8-day composite dataset produced at 500 meter (m) pixel resolution. The improved algorithm is based on the logic of the Penman-Monteith equation, which includes inputs of daily meteorological reanalysis data along with Moderate Resolution Imaging Spectroradiometer (MODIS) remotely sensed data products such as vegetation property dynamics, albedo, and land cover. The MYD16A2GF will be generated at the end of each year when the entire yearly 8-day &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD15A2H.006&quot;&gt;MYD15A2H&lt;/a&gt; is available. Hence, the gap-filled MYD16A2GF is the improved MYD16, which has cleaned the poor-quality inputs from 8-day Leaf Area Index and Fraction of Photosynthetically Active Radiation (LAI/FPAR) based on the Quality Control (QC) label for every pixel. If any LAI/FPAR pixel did not meet the quality screening criteria, its value is determined through linear interpolation. However, users cannot get MYD16A2GF in near-real time because it will be generated only at the end of a given year. Provided in the MYD16A2GF product are layers for composited ET, LE, Potential ET (PET), and Potential LE (PLE) along with a quality control layer. Two low resolution browse images, ET and LE, are also available for each MYD16A2GF granule. The pixel values for the two Evapotranspiration layers (ET and PET) are the sum of all eight days within the composite period, and the pixel values for the two Latent Heat layers (LE and PLE) are the average of all eight days within the composite period. The last acquisition period of each year is a 5- or 6-day composite period, depending on the year. Known Issues: Operational and uncertainty issues are provided on page 13 in the User Guide. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd16a2gf-1&quot;&gt;MYD16A2GF&lt;/h4&gt;
The Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) MYD16A2GF Version 6.1 Evapotranspiration/Latent Heat Flux (ET/LE) product is a year-end gap-filled 8-day composite dataset produced at 500 meter (m) pixel resolution. The improved algorithm is based on the logic of the Penman-Monteith equation, which includes inputs of daily meteorological reanalysis data along with MODIS remotely sensed data products such as vegetation property dynamics, albedo, and land cover. The MYD16A2GF will be generated at the end of each year when the entire yearly 8-day &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD15A2H.061&quot;&gt;MYD15A2H&lt;/a&gt; is available. Hence, the gap-filled MYD16A2GF is the improved MYD16, which has cleaned the poor-quality inputs from 8-day Leaf Area Index and Fraction of Photosynthetically Active Radiation (LAI/FPAR) based on the Quality Control (QC) label for every pixel. If any LAI/FPAR pixel did not meet the quality screening criteria, its value is determined through linear interpolation. However, users cannot get MYD16A2GF in near-real time because it will be generated only at the end of a given year. Provided in the MYD16A2GF product are layers for composited ET, LE, Potential ET (PET), and Potential LE (PLE) along with a quality control layer. Two low resolution browse images, ET and LE, are also available for each MYD16A2GF granule. The pixel values for the two Evapotranspiration layers (ET and PET) are the sum of all eight days within the composite period, and the pixel values for the two Latent Heat layers (LE and PLE) are the average of all eight days within the composite period. The last acquisition period of each year is a 5 or 6-day composite period, depending on the year. Known Issues: Operational and uncertainty issues are provided under Section 3 in the User Guide. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd16a3gf&quot;&gt;MYD16A3GF&lt;/h4&gt;
The MYD16A3GF Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD16A3GF.061&quot;&gt;MYD16A3GF Version 6.1&lt;/a&gt; data product. The MYD16A3GF Version 6 Evapotranspiration/Latent Heat Flux (ET/LE) product is a year-end gap-filled yearly composite dataset produced at 500 meter (m) pixel resolution. The improved algorithm is based on the logic of the Penman-Monteith equation, which includes inputs of daily meteorological reanalysis data along with Moderate Resolution Imaging Spectroradiometer (MODIS) remotely sensed data products such as vegetation property dynamics, albedo, and land cover. The MYD16A3GF will be generated at the end of each year when the entire yearly 8-day &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD15A2H.006&quot;&gt;MYD15A2H&lt;/a&gt; is available. Hence, the gap-filled MYD16A3GF is the improved MYD16, which has cleaned the poor-quality inputs from 8-day Leaf Area Index and Fraction Photosynthetically Active Radiation (LAI/FPAR) based on the Quality Control (QC) label for every pixel. If any LAI/FPAR pixel did not meet the quality screening criteria, its value is determined through linear interpolation. However, users cannot get MYD16A3GF in near-real time because it will be generated only at the end of a given year. Provided in the MYD16A3GF product are layers for composited ET, LE, Potential ET (PET), and Potential LE (PLE) along with a quality control layer. Two low resolution browse images, ET and LE, are also available for each MYD16A3GF granule. The pixel values for the two Evapotranspiration layers (ET and PET) are the sum for all days within the defined year, and the pixel values for the two Latent Heat layers (LE and PLE) are the average of all days within the defined year. Known Issues: Operational and uncertainty issues are provided under Section 3 in the User Guide. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd16a3gf-1&quot;&gt;MYD16A3GF&lt;/h4&gt;
The Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) MYD16A3GF Version 6.1 Evapotranspiration/Latent Heat Flux (ET/LE) product is a year-end gap-filled yearly composite dataset produced at 500 meter (m) pixel resolution. The improved algorithm is based on the logic of the Penman-Monteith equation, which includes inputs of daily meteorological reanalysis data along with MODIS remotely sensed data products such as vegetation property dynamics, albedo, and land cover. The MYD16A3GF will be generated at the end of each year when the entire yearly 8-day &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD15A2H.061&quot;&gt;MYD15A2H&lt;/a&gt; is available. Hence, the gap-filled MYD16A3GF is the improved MYD16, which has cleaned the poor-quality inputs from 8-day Leaf Area Index and Fraction Photosynthetically Active Radiation (LAI/FPAR) based on the Quality Control (QC) label for every pixel. If any LAI/FPAR pixel did not meet the quality screening criteria, its value is determined through linear interpolation. However, users cannot get MYD16A3GF in near-real time because it will be generated only at the end of a given year. Provided in the MYD16A3GF product are layers for composited ET, LE, Potential ET (PET), and Potential LE (PLE) along with a quality control layer. Two low resolution browse images, ET and LE, are also available for each MYD16A3GF granule. The pixel values for the two Evapotranspiration layers (ET and PET) are the sum for all days within the defined year, and the pixel values for the two Latent Heat layers (LE and PLE) are the average of all days within the defined year. Known Issues: Operational and uncertainty issues are provided under Section 3 in the User Guide. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd16a3&quot;&gt;MYD16A3&lt;/h4&gt;
The MYD16A3 Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD16A3GF.061&quot;&gt;MYD16A3GF Version 6.1&lt;/a&gt; data product. The MYD16A3 Version 6 Evapotranspiration/Latent Heat Flux product is a yearly composite dataset produced at 500 meter (m) pixel resolution. The improved algorithm is based on the logic of the Penman-Monteith equation, which includes inputs of daily meteorological reanalysis data along with Moderate Resolution Imaging Spectroradiometer (MODIS) remotely sensed data products such as vegetation property dynamics, albedo, and land cover. Provided in the MYD16A3 product are layers for yearly Evapotranspiration (ET), Latent Heat Flux (LE), Potential ET (PET) and Potential LE (PLE) along with a quality control layer. Two low resolution browse images, ET and LE, are also available for each MYD16A3 granule. The pixel values for the two Evapotranspiration layers (ET and PET) are the sum for all days within the defined year, and the pixel values for the two Latent Heat layers (LE and PLE) are the average of all days within the defined year. Known Issues: Operational and uncertainty issues are provided under Section 3 in the User Guide. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;. Improvements/Changes from Previous Versions * Spatial resolution of Version 6 products has increased to nominal 500 m from nominal 1,000 m in Version 5. * Version 5 data products were previously distributed by the Numerical Terradynamic Simulation Group at the University of Montana. The Version 6 products are a continuation of this project.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd17a3hgf&quot;&gt;MYD17A3HGF&lt;/h4&gt;
The MYD17A3HGF Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD17A3HGF.061&quot;&gt;MYD17A3HGF Version 6.1&lt;/a&gt; data product. The MYD17A3HGF Version 6 product provides information about annual Net Primary Production (NPP) at 500 meter (m) pixel resolution. Annual NPP is derived from the sum of all 8-day Net Photosynthesis (PSN) products (MYD17A2H) from the given year. The PSN value is the difference of the Gross Primary Productivity (GPP) and the Maintenance Respiration (MR). The MYD17A3HGF will be generated at the end of each year when the entire yearly 8-day &lt;a href&#x3D;&quot;https://doi.org/10.5067/modis/myd15a2h.006&quot;&gt;MYD15A2H&lt;/a&gt; is available. Hence, the gap-filled MYD17A3HGF is the improved MYD17, which has cleaned the poor-quality inputs from 8-day Leaf Area Index and Fraction of Photosynthetically Active Radiation (FPAR/LAI) based on the Quality Control (QC) label for every pixel. If any LAI/FPAR pixel did not meet the quality screening criteria, its value is determined through linear interpolation. However, users cannot get MYD17A3HGF in near-real time because it will be generated only at the end of a given year. Known Issues: Operational and uncertainty issues are provided under Section 2 in the User Guide. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd17a3hgf-1&quot;&gt;MYD17A3HGF&lt;/h4&gt;
The MYD17A3HGF Version 6.1 product provides information about annual Gross and Net Primary Production (GPP and NPP) at 500 meter (m) pixel resolution. Annual Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) GPP and NPP is derived from the sum of all 8-day GPP and Net Photosynthesis (PSN) products (&lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD17A2H.061&quot;&gt;MYD17A2H&lt;/a&gt;) from the given year. The PSN value is the difference of the GPP and the Maintenance Respiration (MR). The MYD17A3HGF will be generated at the end of each year when the entire yearly 8-day &lt;a href&#x3D;&quot;https://doi.org/10.5067/modis/myd15a2h.061&quot;&gt;MYD15A2H&lt;/a&gt; is available. Hence, the gap-filled MYD17A3HGF is the improved MYD17, which has cleaned the poor-quality inputs from 8-day Leaf Area Index and Fraction of Photosynthetically Active Radiation (FPAR/LAI) based on the Quality Control (QC) label for every pixel. If any LAI/FPAR pixel did not meet the quality screening criteria, its value is determined through linear interpolation. However, users cannot get MYD17A3HGF in near-real time because it will be generated only at the end of a given year. Known Issues: Operational and uncertainty issues are provided under Section 2 in the User Guide. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd17a3h&quot;&gt;MYD17A3H&lt;/h4&gt;
The MYD17A3H Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD17A3HGF.061&quot;&gt;MYD17A3HGF Version 6.1&lt;/a&gt; data product. The MYD17A3H Version 6 product provides information about annual Net Primary Production (NPP) at 500 meter (m) pixel resolution. Annual NPP is derived from the sum of all 8-day Net Photosynthesis (PSN) products (&lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD17A2H.006&quot;&gt;MYD17A2H&lt;/a&gt;) from the given year. The PSN value is the difference of the Gross Primary Productivity (GPP) and the Maintenance Respiration (MR). Knonw Issues * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;. * Forward processing of Aqua MODIS Net Primary Production Yearly L4 Global 500 m SIN Grid products was discontinued on January 3, 2004, due to unexpected errors in the input data. Users are encouraged to use the MYD17A3HGF Version 6.1 data product.
&lt;br&gt;&lt;h4 id&#x3D;&quot;mydocga&quot;&gt;MYDOCGA&lt;/h4&gt;
The MYDOCGA Version 6 data product was decommissioned on July 31, 2023. The MYDOCGA Version 6 Level 2 Gridded Lite (L2G-lite) Ocean Reflectance product provides an estimate of the surface spectral reflectance data from Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) bands 8 through 16. Data have been corrected for atmospheric conditions such as gasses, aerosols, and Rayleigh scattering. MYDOCGA is a daily land product with a pixel size of 1 kilometer (km). The product is referred to as ocean reflectance because bands 8 through 16 are used primarily to produce ocean products. The MYDOCGA, as with other L2G data sets, stores the “best available pixel” from all the qualifying observations in the first layer and any subsequent observations are stored in either a full or compact format layer within the Hierarchical Data Format (HDF) file. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;. Improvements/Changes from Previous Versions * New product for MODIS Version 6.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd09q1&quot;&gt;MYD09Q1&lt;/h4&gt;
The MYD09Q1 Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD09Q1.061&quot;&gt;MYD09Q1 Version 6.1&lt;/a&gt; data product. The MYD09Q1 Version 6 product provides an estimate of the surface spectral reflectance of Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Bands 1 and 2, corrected for atmospheric conditions such as gasses, aerosols, and Rayleigh scattering. Provided along with the 250 meter (m) surface reflectance bands are two quality layers. For each pixel, a value is selected from all the acquisitions within the 8-day composite period. The criteria for the pixel choice include cloud and solar zenith. When several acquisitions meet the criteria the pixel with the minimum channel 3 (blue) value is used. Known Issues: The Collection 6 MODIS Land Surface Reflectance product (MYD09) may &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/displayissue?id&#x3D;174&quot;&gt;incorrectly flag retrievals as ‘High Aerosol’&lt;/a&gt; over brighter surfaces and at higher view angles. This will impact the downstream MODIS BRDF/Albedo (MCD43) and Vegetation Index (MOD13 and MYD13) data products which use the aerosol quantity flag to screen out high aerosol values. * &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/data/userguide/LSRHighAerosolFlagFinal.pdf&quot;&gt;Corrections&lt;/a&gt; were implemented in Collection 6.1 reprocessing. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd09q1-1&quot;&gt;MYD09Q1&lt;/h4&gt;
The MYD09Q1 Version 6.1 product provides an estimate of the surface spectral reflectance of Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Bands 1 and 2, corrected for atmospheric conditions such as gasses, aerosols, and Rayleigh scattering. Provided along with the 250 meter (m) surface reflectance bands are two quality layers. For each pixel, a value is selected from all the acquisitions within the 8-day composite period. The criteria for the pixel choice include cloud and solar zenith. When several acquisitions meet the criteria the pixel with the minimum channel 3 (blue) value is used. Known Issues: Prior to the Aqua MODIS launch, Band 6 exhibited several anomalous detectors. Band 6 performance degraded seriously after launch and presently a majority of the Band 6 detectors are non-functional. Science users should read and use the non-functional detector flags and decide for themselves the optimum manner to handle non-functional detector &amp;quot;gaps&amp;quot; for their products. For complete information please refer to the &lt;a href&#x3D;&quot;https://mcst.gsfc.nasa.gov/time-dependent-list-non-functional-or-noisy-detector&quot;&gt;MODIS Characterization Support Team (MCST) website&lt;/a&gt;. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd09a1&quot;&gt;MYD09A1&lt;/h4&gt;
The MYD09A1 Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD09A1.061&quot;&gt;MYD09A1 Version 6.1&lt;/a&gt; data product. The Moderate Resolution Imaging Spectroradiometer (MODIS) Aqua MYD09A1 Version 6 product provides an estimate of the surface spectral reflectance of Aqua MODIS Bands 1 through 7 corrected for atmospheric conditions such as gasses, aerosols, and Rayleigh scattering. Along with the seven 500 meter (m) reflectance bands are a quality variable and four observation bands. For each pixel, a value is selected from all the acquisitions within the 8-day composite period. The criteria for the pixel choice include cloud and solar zenith. When several acquisitions meet the criteria the pixel with the minimum channel 3 (blue) value is used. Known Issues: The Collection 6 MODIS Land Surface Reflectance product (MYD09) may &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/displayissue?id&#x3D;174&quot;&gt;incorrectly flag retrievals as ‘High Aerosol’&lt;/a&gt; over brighter surfaces and at higher view angles. This will impact the downstream MODIS BRDF/Albedo (MCD43) and Vegetation Index (MOD13 and MYD13) data products which use the aerosol quantity flag to screen out high aerosol values. * &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/data/userguide/LSRHighAerosolFlagFinal.pdf&quot;&gt;Corrections&lt;/a&gt; were implemented in Collection 6.1 reprocessing. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd09a1-1&quot;&gt;MYD09A1&lt;/h4&gt;
The Moderate Resolution Imaging Spectroradiometer (MODIS) Aqua MYD09A1 Version 6.1 product provides an estimate of the surface spectral reflectance of Aqua MODIS Bands 1 through 7 corrected for atmospheric conditions such as gasses, aerosols, and Rayleigh scattering. Along with the seven 500 meter (m) reflectance bands are a quality layer and four observation bands. For each pixel, a value is selected from all the acquisitions within the 8-day composite period. The criteria for the pixel choice include cloud and solar zenith. When several acquisitions meet the criteria the pixel with the minimum channel 3 (blue) value is used. Known Issues: Prior to the Aqua MODIS launch, Band 6 exhibited several anomalous detectors. Band 6 performance degraded seriously after launch and presently a majority of the Band 6 detectors are non-functional. Science users should read and use the non-functional detector flags and decide for themselves the optimum manner to handle non-functional detector &amp;quot;gaps&amp;quot; for their products. For complete information please refer to the &lt;a href&#x3D;&quot;https://mcst.gsfc.nasa.gov/time-dependent-list-non-functional-or-noisy-detector&quot;&gt;MODIS Characterization Support Team (MCST) website&lt;/a&gt;. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd09ga&quot;&gt;MYD09GA&lt;/h4&gt;
The MYD09GA Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD09GA.061&quot;&gt;MYD09GA Version 6.1&lt;/a&gt; data product. The MYD09GA Version 6 product provides an estimate of the surface spectral reflectance of Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Bands 1 through 7, corrected for atmospheric conditions such as gasses, aerosols, and Rayleigh scattering. Provided along with the 500 meter (m) surface reflectance, observation, and quality bands are a set of ten 1 km observation bands and geolocation flags. The reflectance layers from the MYD09GA are used as the source data for many of the MODIS land products. Known Issues: The Collection 6 MODIS Land Surface Reflectance product (MYD09) may &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/displayissue?id&#x3D;174&quot;&gt;incorrectly flag retrievals as ‘High Aerosol’&lt;/a&gt; over brighter surfaces and at higher view angles. This will impact the downstream MODIS BRDF/Albedo (MCD43) and Vegetation Index (MOD13 and MYD13) data products which use the aerosol quantity flag to screen out high aerosol values. * &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/data/userguide/LSRHighAerosolFlagFinal.pdf&quot;&gt;Corrections&lt;/a&gt; were implemented in Collection 6.1 reprocessing. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd09ga-1&quot;&gt;MYD09GA&lt;/h4&gt;
The MYD09GA Version 6.1 product provides an estimate of the surface spectral reflectance of Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Bands 1 through 7, corrected for atmospheric conditions such as gasses, aerosols, and Rayleigh scattering. Provided along with the 500 meter (m) surface reflectance, observation, and quality bands are a set of ten 1 kilometer observation bands and geolocation flags. The reflectance layers from the MYD09GA are used as the source data for many of the MODIS land products. Known Issues: Prior to the Aqua MODIS launch, Band 6 exhibited several anomalous detectors. Band 6 performance degraded seriously after launch and presently a majority of the Band 6 detectors are non-functional. Science users should read and use the non-functional detector flags and decide for themselves the optimum manner to handle non-functional detector &amp;quot;gaps&amp;quot; for their products. For complete information please refer to the &lt;a href&#x3D;&quot;https://mcst.gsfc.nasa.gov/time-dependent-list-non-functional-or-noisy-detector&quot;&gt;MODIS Characterization Support Team (MCST) website&lt;/a&gt;. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd09gq&quot;&gt;MYD09GQ&lt;/h4&gt;
The MYD09GQ Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD09GQ.061&quot;&gt;MYD09GQ Version 6.1&lt;/a&gt; data product. The MYD09GQ Version 6 product provides an estimate of the surface spectral reflectance of Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) 250 meter (m) bands 1 and 2, corrected for atmospheric conditions such as gasses, aerosols, and Rayleigh scattering. Along with the 250 m bands are the Quality Assurance (QA) layer and five observation layers. This product is intended to be used in conjunction with the quality and viewing geometry information of the 500 m product (MYD09GA). Known Issues: The Collection 6 MODIS Land Surface Reflectance product (MYD09) may &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/displayissue?id&#x3D;174&quot;&gt;incorrectly flag retrievals as ‘High Aerosol’&lt;/a&gt; over brighter surfaces and at higher view angles. This will impact the downstream MODIS BRDF/Albedo (MCD43) and Vegetation Index (MOD13 and MYD13) data products which use the aerosol quantity flag to screen out high aerosol values. * &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/data/userguide/LSRHighAerosolFlagFinal.pdf&quot;&gt;Corrections&lt;/a&gt; were implemented in Collection 6.1 reprocessing. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd09gq-1&quot;&gt;MYD09GQ&lt;/h4&gt;
The MYD09GQ Version 6.1 product provides an estimate of the surface spectral reflectance of Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) 250 meter (m) bands 1 and 2, corrected for atmospheric conditions such as gasses, aerosols, and Rayleigh scattering. Along with the 250 m bands are the Quality Assurance (QA) layer and five observation layers. This product is intended to be used in conjunction with the quality and viewing geometry information of the 500 m product (MYD09GA). Known Issues: Prior to the Aqua MODIS launch, Band 6 exhibited several anomalous detectors. Band 6 performance degraded seriously after launch and presently a majority of the Band 6 detectors are non-functional. Science users should read and use the non-functional detector flags and decide for themselves the optimum manner to handle non-functional detector &amp;quot;gaps&amp;quot; for their products. For complete information please refer to the &lt;a href&#x3D;&quot;https://mcst.gsfc.nasa.gov/time-dependent-list-non-functional-or-noisy-detector&quot;&gt;MODIS Characterization Support Team (MCST) website&lt;/a&gt;. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd09cmg&quot;&gt;MYD09CMG&lt;/h4&gt;
The MYD09CMG Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD09CMG.061&quot;&gt;MYD09CMG Version 6.1&lt;/a&gt; data product. The MYD09CMG Version 6 product provides an estimate of the surface spectral reflectance of Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Bands 1 through 7, resampled to 5600 meter (m) pixel resolution and corrected for atmospheric conditions such as gasses, aerosols, and Rayleigh scattering. The MOD09CMG data product provides 25 layers including MODIS bands 1 through 7; Brightness Temperature data from thermal bands 20, 21, 31, and 32; along with Quality Assurance (QA) and observation bands. This product is based on a Climate Modeling Grid (CMG) for use in climate simulation models. Known Issues: The Collection 6 MODIS Land Surface Reflectance product (MYD09) may &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/displayissue?id&#x3D;174&quot;&gt;incorrectly flag retrievals as ‘High Aerosol’&lt;/a&gt; over brighter surfaces and at higher view angles. This will impact the downstream MODIS BRDF/Albedo (MCD43) and Vegetation Index (MOD13 and MYD13) data products which use the aerosol quantity flag to screen out high aerosol values. * &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/data/userguide/LSRHighAerosolFlagFinal.pdf&quot;&gt;Corrections&lt;/a&gt; were implemented in Collection 6.1 reprocessing. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd09cmg-1&quot;&gt;MYD09CMG&lt;/h4&gt;
The MYD09CMG Version 6.1 product provides an estimate of the surface spectral reflectance of Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Bands 1 through 7, resampled to 5600 meter (m) pixel resolution and corrected for atmospheric conditions such as gasses, aerosols, and Rayleigh scattering. The MOD09CMG data product provides 25 layers including MODIS bands 1 through 7; Brightness Temperature data from thermal bands 20, 21, 31, and 32; along with Quality Assurance (QA) and observation bands. This product is based on a Climate Modeling Grid (CMG) for use in climate simulation models. Known Issues: A &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/displayissue?id&#x3D;939&quot;&gt;striping anomaly in Band 5&lt;/a&gt; of the MYD09CMG V61 product has been identified, caused by a dead detector in the AQUA Band 5, affecting data accuracy throughout the Aqua MODIS mission. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd07_l2&quot;&gt;MYD07_L2&lt;/h4&gt;
The MODIS/Aqua Temperature and Water Vapor Profiles 5-Min L2 Swath 5km (MYD07_L2) product consists of a numbers of parameters related to atmospheric stability, atmospheric temperature and moisture profiles, total atmospheric water vapor, and total ozone. All of these parameters are produced for both daytime and nighttime conditions at 5-km pixel resolution when at least 9 Field Of View (FOV) are cloud free. The MODIS total-ozone burden is an estimate of the total-column tropospheric and stratospheric ozone content. The MODIS atmospheric stability consists of three daily Level 2 atmospheric stability indices. The Total Totals (TT), the Lifted Index (LI), and the K index (K) are each computed using the infrared temperature- and moisture-profile data, also derived as part of MYD07. The MODIS temperature and moisture profiles are produced at 20 vertical levels. The MODIS atmospheric water-vapor product is an estimate of the total tropospheric column water vapor made from integrated MODIS infrared retrievals of atmospheric moisture profiles in clear scenes. Additional information is available at: &lt;a href&#x3D;&quot;https://modis-atmos.gsfc.nasa.gov/products/atm-profile&quot;&gt;https://modis-atmos.gsfc.nasa.gov/products/atm-profile&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd14&quot;&gt;MYD14&lt;/h4&gt;
The MYD14 Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD14.061&quot;&gt;MYD14 Version 6.1&lt;/a&gt; data product. The Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Thermal Anomalies and Fire MYD14 Version 6 product is produced daily in 5-minute temporal satellite increments (swaths). The MYD14 product is used to generate all of the higher level fire products, but can also be used to identify fires and other thermal anomalies, such as volcanoes. Each swath of data is approximately 2,030 kilometers along track (long), and 2,300 kilometers across track (wide). Known Issues: Known issues are described on the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt; and in Section 7.2 of the User Guide which covers Pre-November 2000 Data Quality, Detection Confidence, Flagging of Static Sources, and the August 2020 MODIS Aqua Outage.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd14-1&quot;&gt;MYD14&lt;/h4&gt;
The Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Thermal Anomalies and Fire (MYD14) Version 6.1 product is produced daily in 5-minute temporal satellite increments (swaths). The MYD14 product is used to generate all of the higher level fire products, but can also be used to identify fires and other thermal anomalies, such as volcanoes. Each swath of data is approximately 2,030 kilometers along track (long), and 2,300 kilometers across track (wide). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd14a2&quot;&gt;MYD14A2&lt;/h4&gt;
The MYD14A2 Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD14A2.061&quot;&gt;MYD14A2 Version 6.1&lt;/a&gt; data product. The Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Thermal Anomalies and Fire 8-Day (MYD14A2) Version 6 data are generated at 1 kilometer (km) spatial resolution as a Level 3 product. The MYD14A2 gridded composite contains maximum value of individual fire pixel classes detected during the eight days of acquisition. The Science Dataset (SDS) layers include the fire mask and pixel quality indicators. Known Issues: Known issues are described on the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt; and in Section 7.2 of the User Guide which covers Pre-November 2000 Data Quality, Detection Confidence, Flagging of Static Sources, and the August 2020 MODIS Aqua Outage.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd14a2-1&quot;&gt;MYD14A2&lt;/h4&gt;
The Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Thermal Anomalies and Fire 8-Day (MYD14A2) Version 6.1 data are generated at 1 kilometer (km) spatial resolution as a Level 3 product. The MYD14A2 gridded composite contains maximum value of individual fire pixel classes detected during the eight days of acquisition. The Science Dataset (SDS) layers include the fire mask and pixel quality indicators. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd14a1&quot;&gt;MYD14A1&lt;/h4&gt;
The MYD14A1 Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD14A1.061&quot;&gt;MYD14A1 Version 6.1&lt;/a&gt; data product. The Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Thermal Anomalies and Fire Daily (MYD14A1) Version 6 data are generated every eight days at 1 kilometer (km) spatial resolution as a Level 3 product. MYD14A1 contains eight consecutive days of fire data conveniently packaged into a single file. The Science Dataset (SDS) layers include the fire mask, pixel quality indicators, maximum fire-radiative-power (MaxFRP), and the position of the fire pixel within the scan. Each layer consists of daily per pixel information for each of the eight days of data acquisition. Known Issues: Known issues are described on the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt; and in Section 7.2 of the User Guide which covers Pre-November 2000 Data Quality, Detection Confidence, Flagging of Static Sources, and the August 2020 MODIS Aqua Outage.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd14a1-1&quot;&gt;MYD14A1&lt;/h4&gt;
The Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Thermal Anomalies and Fire Daily (MYD14A1) Version 6.1 data are generated every eight days at 1 kilometer (km) spatial resolution as a Level 3 product. MYD14A1 contains eight consecutive days of fire data conveniently packaged into a single file. The Science Dataset (SDS) layers include the fire mask, pixel quality indicators, maximum fire-radiative-power (MaxFRP), and the position of the fire pixel within the scan. Each layer consists of daily per pixel information for each of the eight days of data acquisition. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;mydtbga&quot;&gt;MYDTBGA&lt;/h4&gt;
The MYDTBGA Version 6 data product was decommissioned on July 31, 2023. The MYDTBGA Version 6 Moderate Resolution Imaging Spectroradiometer (MODIS) Level 2 Gridded Lite (L2G-lite) Thermal Band product consists of brightness temperature data from Aqua MODIS bands 20, 31, and 32 and albedo data from band 20 along with the orbit and granule pointer fields. MYDTBGA is a daily product with a pixel size of 1 kilometer (km). The MYDTBGA, as with other L2G data sets, stores the “best available pixel” from all the qualifying observations in the first layer and any subsequent observations are stored in either full or a compact layers within the Hierarchical Data Format (HDF) file. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;. Improvements/Changes from Previous Versions * New product for MODIS Version 6.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd05_l2&quot;&gt;MYD05_L2&lt;/h4&gt;
The MODIS/Aqua Total Precipitable Water Vapor 5-Min L2 Swath 1km and 5km (MYD05_L2) product consists of atmospheric column water-vapor amounts. This product is derived from data collected by the Moderate-Resolution Imaging Spectroradiometer (MODIS) on board the Aqua satellite. There are two different algorithms used to derive total precipitable water vapor in this data product: a near-infrared algorithm and an infrared algorithm. The near-infrared algorithm relies on observations of reflected solar radiation in MODIS&amp;#39;s near-infrared channels, thus, the near-infrared retrievals are only produced during the daytime over surfaces that reflect near-infrared energy. As a result, the near-infrared algorithm is only applied over clear, cloud free land areas of the globe and above clouds over both the land and ocean. Over clear ocean areas, water-vapor estimates are provided over extended sun glint areas. Data produced by the near-infrared algorithm are generated at a 1-km spatial resolution. The other algorithm is the infrared algorithm which can be used to derive atmospheric precipitable water vapor profiles during both day and night. Data from the infrared algorithm are generated at a 5-km spatial resolution when at least nine field of views (FOVs) are cloud free. The infrared-derived precipitable water vapor is generated as a component of product MYD07, and is simply added to product MYD05 for convenience. There are two MODIS Precipitable Water Vapor products: MOD05_L2, containing data collected from the Terra platform; and MYD05_L2, containing data collected from the Aqua platform. This dataset has a short name of MYD05_L2 and provides data from the Aqua platform only. The MODIS Adaptive Processing System (MODAPS) is currently generating an improved version 6.1 (061) for all MODIS Level-1 (L1) and higher-level Level-2 (L2) &amp;amp; Level-3 (L3) Atmosphere Team products. The decision to create a new improved Collection 6.1 (061) was driven by the need to address a number of issues in the current Collection 6 (006) Level-1B (L1B) data, which have a negative impact in varying degrees in downstream products. It should be noted that the near-infrared algorithm refinement for this product is no longer being supported by NASA and as such there has been no update to this algorithm for Collection 6.1. For more information, visit the MODIS Atmosphere website at: &lt;a href&#x3D;&quot;https://modis-atmos.gsfc.nasa.gov/products/water-vapor&quot;&gt;https://modis-atmos.gsfc.nasa.gov/products/water-vapor&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd13c1&quot;&gt;MYD13C1&lt;/h4&gt;
The MYD13C1 Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD13C1.061&quot;&gt;MYD13C1 Version 6.1&lt;/a&gt; data product. The MYD13C1 Version 6 product provides a Vegetation Index (VI) value at a per pixel basis. There are two primary vegetation layers. The first is the Normalized Difference Vegetation Index (NDVI) which is referred to as the continuity index to the existing National Oceanic and Atmospheric Administration-Advanced Very High Resolution Radiometer (NOAA-AVHRR) derived NDVI. The second vegetation layer is the Enhanced Vegetation Index (EVI), which has improved sensitivity over high biomass regions. The Climate Modeling Grid (CMG) consists 3,600 rows and 7,200 columns of 5,600 meter (m) pixels. Global MYD13C1 data are cloud-free spatial composites of the gridded 16-day 1 kilometer &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD13A2.006&quot;&gt;MYD13A2&lt;/a&gt; data, and are provided as a Level 3 product projected on a 0.05 degree (5,600 m) geographic CMG. The MYD13C1 has data fields for NDVI, EVI, VI QA, reflectance data, angular information, and spatial statistics such as mean, standard deviation, and number of used input pixels at the 0.05 degree CMG resolution. Known Issues: The incorrect representation of the aerosol quantities (low, average, high) in the Collection 6 MYD09 surface reflectance products may have &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/displayissue?id&#x3D;174&quot;&gt;impacted&lt;/a&gt; MYD13 Vegetation Index data products particularly over arid bright surfaces. * &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/data/userguide/LSRHighAerosolFlagFinal.pdf&quot;&gt;Corrections&lt;/a&gt; were implemented in Collection 6.1 reprocessing. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd13c1-1&quot;&gt;MYD13C1&lt;/h4&gt;
The Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Vegetation Indices 16-Day (MYD13C1) Version 6.1 product provides a Vegetation Index (VI) value at a per pixel basis. There are two primary vegetation layers. The first is the Normalized Difference Vegetation Index (NDVI) which is referred to as the continuity index to the existing National Oceanic and Atmospheric Administration-Advanced Very High Resolution Radiometer (NOAA-AVHRR) derived NDVI. The second vegetation layer is the Enhanced Vegetation Index (EVI), which has improved sensitivity over high biomass regions. The Climate Modeling Grid (CMG) consists 3,600 rows and 7,200 columns of 5,600 meter (m) pixels. Global MYD13C1 data are cloud-free spatial composites of the gridded 16-day 1 kilometer &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD13A2.061&quot;&gt;MYD13A2&lt;/a&gt; data, and are provided as a Level 3 product projected on a 0.05 degree (5,600 m) geographic CMG. The MYD13C1 has data fields for NDVI, EVI, VI QA, reflectance data, angular information, and spatial statistics such as mean, standard deviation, and number of used input pixels at the 0.05 degree CMG resolution. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd13a2&quot;&gt;MYD13A2&lt;/h4&gt;
The MYD13A2 Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD13A2.061&quot;&gt;MYD13A2 Version 6.1&lt;/a&gt; data product. The MYD13A2 Version 6 product provides Vegetation Index (VI) values at a per pixel basis at 1 kilometer (km) spatial resolution. There are two primary vegetation layers. The first is the Normalized Difference Vegetation Index (NDVI), which is referred to as the continuity index to the existing National Oceanic and Atmospheric Administration-Advanced Very High Resolution Radiometer (NOAA-AVHRR) derived NDVI. The second vegetation layer is the Enhanced Vegetation Index (EVI), which has improved sensitivity over high biomass regions. The algorithm for this product chooses the best available pixel value from all the acquisitions from the 16 day period. The criteria used is low clouds, low view angle and the highest NDVI/EVI value. Provided along with the vegetation layers and the two quality assurance (QA) layers are reflectance bands 1 (red), 2 (near-infrared), 3 (blue), and 7 (mid-infrared), as well as four observation layers. Known Issues: The following issues have been detected: * Unexpected missing data in the last cycles of each year. * Incorrect instances of &amp;quot;NoData&amp;quot; and spikes in NDVI values. * VI Usefulness Bits are not correctly assigned. * For instances where the VI Quality (bits 0-1) is flagged as good and the VI Usefulness (bits 2-5) indicates the same pixels have the lowest usefulness score, users are advised to disregard the usefulness score. * The incorrect representation of the aerosol quantities (low, average, high) in the Collection 6 MYD09 surface reflectance products may have &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/displayissue?id&#x3D;174&quot;&gt;impacted&lt;/a&gt; MYD13 Vegetation Index data products particularly over arid bright surfaces. * &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/data/userguide/LSRHighAerosolFlagFinal.pdf&quot;&gt;Corrections&lt;/a&gt; were implemented in Collection 6.1 reprocessing. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd13a2-1&quot;&gt;MYD13A2&lt;/h4&gt;
The Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Vegetation Indices 16-Day (MYD13A2) Version 6.1 product provides Vegetation Index (VI) values at a per pixel basis at 1 kilometer (km) spatial resolution. There are two primary vegetation layers. The first is the Normalized Difference Vegetation Index (NDVI), which is referred to as the continuity index to the existing National Oceanic and Atmospheric Administration-Advanced Very High Resolution Radiometer (NOAA-AVHRR) derived NDVI. The second vegetation layer is the Enhanced Vegetation Index (EVI), which has improved sensitivity over high biomass regions. The algorithm for this product chooses the best available pixel value from all the acquisitions from the 16 day period. The criteria used is low clouds, low view angle and the highest NDVI/EVI value. Provided along with the vegetation layers and the two quality assurance (QA) layers are reflectance bands 1 (red), 2 (near-infrared), 3 (blue), and 7 (mid-infrared), as well as four observation layers. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd13q1&quot;&gt;MYD13Q1&lt;/h4&gt;
The MYD13Q1 Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD13Q1.061&quot;&gt;MYD13Q1 Version 6.1&lt;/a&gt; data product. The Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Vegetation Indices (MYD13Q1) Version 6 data are generated every 16 days at 250 meter (m) spatial resolution as a Level 3 product. The MYD13Q1 product provides two primary vegetation layers. The first is the Normalized Difference Vegetation Index (NDVI) which is referred to as the continuity index to the existing National Oceanic and Atmospheric Administration-Advanced Very High Resolution Radiometer (NOAA-AVHRR) derived NDVI. The second vegetation layer is the Enhanced Vegetation Index (EVI), which has improved sensitivity over high biomass regions. The algorithm chooses the best available pixel value from all the acquisitions from the 16 day period. The criteria used is low clouds, low view angle, and the highest NDVI/EVI value. Along with the vegetation layers and the two quality layers, the HDF file will have MODIS reflectance bands 1 (red), 2 (near-infrared), 3 (blue), and 7 (mid-infrared), as well as four observation layers. Known Issues: The following issues have been detected: * Unexpected missing data in the last cycles of each year. * Incorrect instances of &amp;quot;NoData&amp;quot; and spikes in NDVI values. * VI Usefulness Bits are not correctly assigned. * For instances where the VI Quality (bits 0-1) is flagged as good and the VI Usefulness (bits 2-5) indicates the same pixels have the lowest usefulness score, users are advised to disregard the usefulness score. * The incorrect representation of the aerosol quantities (low, average, high) in the Collection 6 MYD09 surface reflectance products may have &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/displayissue?id&#x3D;174&quot;&gt;impacted&lt;/a&gt; MYD13 Vegetation Index data products particularly over arid bright surfaces. * &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/data/userguide/LSRHighAerosolFlagFinal.pdf&quot;&gt;Corrections&lt;/a&gt; were implemented in Collection 6.1 reprocessing. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd13q1-1&quot;&gt;MYD13Q1&lt;/h4&gt;
The Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Vegetation Indices (MYD13Q1) Version 6.1 data are generated every 16 days at 250 meter (m) spatial resolution as a Level 3 product. The MYD13Q1 product provides two primary vegetation layers. The first is the Normalized Difference Vegetation Index (NDVI) which is referred to as the continuity index to the existing National Oceanic and Atmospheric Administration-Advanced Very High Resolution Radiometer (NOAA-AVHRR) derived NDVI. The second vegetation layer is the Enhanced Vegetation Index (EVI), which has improved sensitivity over high biomass regions. The algorithm chooses the best available pixel value from all the acquisitions from the 16 day period. The criteria used is low clouds, low view angle, and the highest NDVI/EVI value. Along with the vegetation layers and the two quality layers, the HDF file will have MODIS reflectance bands 1 (red), 2 (near-infrared), 3 (blue), and 7 (mid-infrared), as well as four observation layers. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd13a1&quot;&gt;MYD13A1&lt;/h4&gt;
The MYD13A1 Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD13A1.061&quot;&gt;MYD13A1 Version 6.1&lt;/a&gt; data product. The MYD13A1 Version 6 product provides Vegetation Index (VI) values at a per pixel basis at 500 meter (m) spatial resolution. There are two primary vegetation layers. The first is the Normalized Difference Vegetation Index (NDVI), which is referred to as the continuity index to the existing National Oceanic and Atmospheric Administration-Advanced Very High Resolution Radiometer (NOAA-AVHRR) derived NDVI. The second vegetation layer is the Enhanced Vegetation Index (EVI), which has improved sensitivity over high biomass regions. The algorithm for this product chooses the best available pixel value from all the acquisitions from the 16 day period. The criteria used is low clouds, low view angle, and the highest NDVI/EVI value. Provided along with the vegetation layers and two quality assurance (QA) layers are reflectance bands 1 (red), 2 (near-infrared), 3 (blue), and 7 (mid-infrared), as well as four observation layers. Known Issues: The following issues have been detected: * Unexpected missing data in the last cycles of each year. * Incorrect instances of &amp;quot;NoData&amp;quot; and spikes in NDVI values. * VI Usefulness Bits are not correctly assigned. * For instances where the VI Quality (bits 0-1) is flagged as good and the VI Usefulness (bits 2-5) indicates the same pixels have the lowest usefulness score, users are advised to disregard the usefulness score. * The incorrect representation of the aerosol quantities (low, average, high) in the Collection 6 MYD09 surface reflectance products may have &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/displayissue?id&#x3D;174&quot;&gt;impacted&lt;/a&gt; MYD13 Vegetation Index data products particularly over arid bright surfaces. * &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/data/userguide/LSRHighAerosolFlagFinal.pdf&quot;&gt;Corrections&lt;/a&gt; were implemented in Collection 6.1 reprocessing. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd13a1-1&quot;&gt;MYD13A1&lt;/h4&gt;
The Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Vegetation Indices 16-Day (MYD13A1) Version 6.1 product provides Vegetation Index (VI) values at a per pixel basis at 500 meter (m) spatial resolution. There are two primary vegetation layers. The first is the Normalized Difference Vegetation Index (NDVI), which is referred to as the continuity index to the existing National Oceanic and Atmospheric Administration-Advanced Very High Resolution Radiometer (NOAA-AVHRR) derived NDVI. The second vegetation layer is the Enhanced Vegetation Index (EVI), which has improved sensitivity over high biomass regions. The algorithm for this product chooses the best available pixel value from all the acquisitions from the 16 day period. The criteria used is low clouds, low view angle, and the highest NDVI/EVI value. Provided along with the vegetation layers and two quality assurance (QA) layers are reflectance bands 1 (red), 2 (near-infrared), 3 (blue), and 7 (mid-infrared), as well as four observation layers. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd13c2&quot;&gt;MYD13C2&lt;/h4&gt;
The MYD13C2 Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD13C2.061&quot;&gt;MYD13C2 Version 6.1&lt;/a&gt; data product. The MYD13C2 Version 6 product provides a Vegetation Index (VI) value at a per pixel basis. There are two primary vegetation layers. The first is the Normalized Difference Vegetation Index (NDVI) which is referred to as the continuity index to the existing National Oceanic and Atmospheric Administration-Advanced Very High Resolution Radiometer (NOAA-AVHRR) derived NDVI. The second vegetation layer is the Enhanced Vegetation Index (EVI), which has improved sensitivity over high biomass regions. The Climate Modeling Grid (CMG) consists of 3,600 rows and 7,200 columns of 5,600 meter (m) pixels. In generating this monthly product, the algorithm ingests all the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD13A2.006&quot;&gt;MYD13A2&lt;/a&gt; products that overlap the month and employs a weighted temporal average. Global MYD13C1 data are cloud-free spatial composites and are provided as a Level 3 product projected on a 0.05 degree (5,600 m) geographic CMG. The MYD13C2 has data fields for the NDVI, EVI, VI QA, reflectance data, angular information, and spatial statistics such as mean, standard deviation, and number of used input pixels at the 0.05 degree CMG resolution. Known Issues: The incorrect representation of the aerosol quantities (low, average, high) in the Collection 6 MYD09 surface reflectance products may have &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/displayissue?id&#x3D;174&quot;&gt;impacted&lt;/a&gt; MYD13 Vegetation Index data products particularly over arid bright surfaces. * &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/data/userguide/LSRHighAerosolFlagFinal.pdf&quot;&gt;Corrections&lt;/a&gt; were implemented in Collection 6.1 reprocessing. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd13c2-1&quot;&gt;MYD13C2&lt;/h4&gt;
The Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Vegetation Indices Monthly (MYD13C2) Version 6.1 product provides a Vegetation Index (VI) value at a per pixel basis. There are two primary vegetation layers. The first is the Normalized Difference Vegetation Index (NDVI) which is referred to as the continuity index to the existing National Oceanic and Atmospheric Administration-Advanced Very High Resolution Radiometer (NOAA-AVHRR) derived NDVI. The second vegetation layer is the Enhanced Vegetation Index (EVI), which has improved sensitivity over high biomass regions. The Climate Modeling Grid (CMG) consists of 3,600 rows and 7,200 columns of 5,600 meter (m) pixels. In generating this monthly product, the algorithm ingests all the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD13A2.061&quot;&gt;MYD13A2&lt;/a&gt; products that overlap the month and employs a weighted temporal average. Global MYD13C1 data are cloud-free spatial composites and are provided as a Level 3 product projected on a 0.05 degree (5,600 m) geographic CMG. The MYD13C2 has data fields for the NDVI, EVI, VI QA, reflectance data, angular information, and spatial statistics such as mean, standard deviation, and number of used input pixels at the 0.05 degree CMG resolution. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd13a3&quot;&gt;MYD13A3&lt;/h4&gt;
The MYD13A3 Version 6 data product was decommissioned on July 31, 2023. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD13A3.061&quot;&gt;MYD13A3 Version 6.1&lt;/a&gt; data product. The Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Vegetation Indices (MYD13A3) Version 6 data are provided monthly at 1 kilometer (km) spatial resolution as a gridded Level 3 product in the sinusoidal projection. In generating this monthly product, the algorithm ingests all the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD13A2.006&quot;&gt;MYD13A2&lt;/a&gt; products that overlap the month and employs a weighted temporal average. The MODIS Normalized Difference Vegetation Index (NDVI) complements NOAA&amp;#39;s Advanced Very High Resolution Radiometer (AVHRR) NDVI products and provides continuity for time series historical applications. MODIS also includes an Enhanced Vegetation Index (EVI) that minimizes canopy background variations and maintains sensitivity over dense vegetation conditions. The EVI uses the blue band to remove residual atmosphere contamination caused by smoke and sub-pixel thin clouds. The MODIS NDVI and EVI products are computed from surface reflectances corrected for molecular scattering, ozone absorption, and aerosols. Vegetation indices are used for global monitoring of vegetation conditions and are used in products displaying land cover and land cover changes. These data may be used as input for modeling global biogeochemical and hydrologic processes as well as global and regional climate. Additional applications include characterizing land surface biophysical properties and processes, such as primary production and land cover conversion. Provided along with the vegetation layers and the two quality assurance (QA) layers are reflectance bands 1 (red), 2 (near-infrared), 3 (blue), and 7 (mid-infrared), as well as three observation layers. Known Issues: The incorrect representation of the aerosol quantities (low, average, high) in the Collection 6 MYD09 surface reflectance products may have &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/displayissue?id&#x3D;174&quot;&gt;impacted&lt;/a&gt; MYD13 Vegetation Index data products particularly over arid bright surfaces. * &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/data/userguide/LSRHighAerosolFlagFinal.pdf&quot;&gt;Corrections&lt;/a&gt; were implemented in Collection 6.1 reprocessing. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;6&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd13a3-1&quot;&gt;MYD13A3&lt;/h4&gt;
The Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Vegetation Indices (MYD13A3) Version 6.1 data are provided monthly at 1 kilometer (km) spatial resolution as a gridded Level 3 product in the sinusoidal projection. In generating this monthly product, the algorithm ingests all the &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MYD13A2.061&quot;&gt;MYD13A2&lt;/a&gt; products that overlap the month and employs a weighted temporal average. The MODIS Normalized Difference Vegetation Index (NDVI) complements NOAA&amp;#39;s Advanced Very High Resolution Radiometer (AVHRR) NDVI products and provides continuity for time series historical applications. MODIS also includes an Enhanced Vegetation Index (EVI) that minimizes canopy background variations and maintains sensitivity over dense vegetation conditions. The EVI uses the blue band to remove residual atmosphere contamination caused by smoke and sub-pixel thin clouds. The MODIS NDVI and EVI products are computed from surface reflectances corrected for molecular scattering, ozone absorption, and aerosols. Vegetation indices are used for global monitoring of vegetation conditions and are used in products displaying land cover and land cover changes. These data may be used as input for modeling global biogeochemical and hydrologic processes as well as global and regional climate. Additional applications include characterizing land surface biophysical properties and processes, such as primary production and land cover conversion. Provided along with the vegetation layers and the two quality assurance (QA) layers are reflectance bands 1 (red), 2 (near-infrared), 3 (blue), and 7 (mid-infrared), as well as three observation layers. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd28c2&quot;&gt;MYD28C2&lt;/h4&gt;
The Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Water Reservoir 8-Day Level 3 (L3) Global (MYD28C2) Version 6.1 product provides current data for 151 man-made reservoirs and 13 regulated natural lakes for a total of 164 reservoirs. The MYD28C2 Version 6.1 data product provides an 8-day time series of surface area, elevation, and water storage. Datasets are combined with pre-established &lt;a href&#x3D;&quot;https://doi.org/10.1016/j.rse.2020.111831&quot;&gt;Area-Elevation (A-E) curves&lt;/a&gt; and image classifications of near-infrared (NIR) reflectance from the surface reflectance product acquired by the Aqua satellite (&lt;a href&#x3D;&quot;https://lpdaac.usgs.gov/products/myd09q1v061/&quot;&gt;MYD09Q1&lt;/a&gt;). The MYD28C2 data product contains a single layer with information about the reservoir identifier, dam location (longitude and latitude), reservoir area, elevation, and storage capacity. Known Issues: Water occurrence images generally show smaller surface area dynamics in high latitude regions, creating pixels with low occurrence values that have relatively large uncertainties. In addition, the quality of raw water area classification can be affected by lake ice coverage typically creating an overestimation of surface area in the enhancement algorithm. This issue will be addressed in a future release of the enhancement algorithm. For additional information about known issues, refer to Section 4 in the User Guide and &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;myd28c3&quot;&gt;MYD28C3&lt;/h4&gt;
The Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Water Reservoir Monthly Level 3 (L3) Global (MYD28C3) Version 6.1 product provides current data for 151 man-made reservoirs and 13 regulated natural lakes for a total of 164 reservoirs. The MYD28C3 Version 6.1 data product is a composite of the 8-day area classifications from &lt;a href&#x3D;&quot;https://lpdaac.usgs.gov/products/myd28c2v061/&quot;&gt;MYD28C2&lt;/a&gt;, which is converted to provide monthly elevation and water storage. &lt;a href&#x3D;&quot;https://doi.org/10.1016/j.rse.2020.112104&quot;&gt;Lake Temperature and Evaporation Model (LTEM)&lt;/a&gt; via MODIS Land Surface Temperature (LST) (&lt;a href&#x3D;&quot;https://lpdaac.usgs.gov/products/myd21v061/&quot;&gt;MYD21&lt;/a&gt;) and meteorological data from &lt;a href&#x3D;&quot;https://earth.gsfc.nasa.gov/hydro/data/gldas-global-land-data-assimilation-system-data&quot;&gt;Global Land Data Assimilation System (GLDAS)&lt;/a&gt; are used to produce monthly evaporation rates and volume losses. The MYD28C3 data product contains a single layer with information about the reservoir identifier, dam location (longitude and latitude), monthly reservoir area, elevation, storage capacity, evaporation rate, and evaporation volume. Known Issues: Water occurrence images generally show smaller surface area dynamics in high latitude regions, creating pixels with low occurrence values that have relatively large uncertainties. In addition, the quality of raw water area classification can be affected by lake ice coverage typically creating an overestimation of surface area in the enhancement algorithm. This issue will be addressed in a future release of the enhancement algorithm. For additional information about known issues, refer to Section 4 in the User Guide and &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;MODIS&amp;amp;sat&#x3D;Aqua&amp;amp;as&#x3D;61&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;mydfds_mon_glb_l3&quot;&gt;MYDFDS_MON_GLB_L3&lt;/h4&gt;
Version 1 is the current version of the dataset. This collection MYDFDS_MON_GLB_L3 provides level 3 monthly frequency of dust storms (FDS) over land from 175°W to 175°E and 80°S to 80°N at a spatial resolution of 0.1˚ x 0.1˚. It is derived from Level 2, the Moderate Resolution Imaging Spectroradiometer (MODIS) Deep Blue aerosol products Collection 6.1 from Aqua (MYD04_L2). The dataset covers the monthly mean from 2003 to 2022. The FDS is calculated as the number of days per month when the daily dust optical depth is greater than a threshold optical depth (e.g., 0.025) with two quality flags: the lowest (1) and highest (3). It is advised to use flag 1, which is of lower quality, over dust source regions, and flag 3 over remote areas or polluted regions. Eight thresholds (0.025, 0.05, 0.1, 0.25, 0.5, 0.75, 1, 2) are saved separately in eight files. If you have any questions, please read the README document first and post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;sndraqiml2ccpret&quot;&gt;SNDRAQIML2CCPRET&lt;/h4&gt;
WARNING: To users of the derived product “co_mmr_midtrop” (carbon monoxide mass mixing ratio to dry air [kg/kg] at ~500 hPa). This variable has a significant bias due to a conversion error: the molecular weight of carbon dioxide (CO2, 44.01 g/mol) was used instead of carbon monoxide (CO, 28.01 g/mol). To correct, simply multiply “co_mmr_midtrop” by 28.01/44.01. Alternatively, derive a profile of mass mixing ratio from scratch using the retrieved column density values (“mol_lay/co_mol_lay”) in the Level 2 files. For further questions or concerns please contact the Sounder SIPS at: &lt;a href&#x3D;&quot;mailto:&amp;#115;&amp;#111;&amp;#x75;&amp;#x6e;&amp;#100;&amp;#x65;&amp;#114;&amp;#x2e;&amp;#x73;&amp;#105;&amp;#112;&amp;#115;&amp;#x40;&amp;#x6a;&amp;#112;&amp;#108;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#115;&amp;#111;&amp;#x75;&amp;#x6e;&amp;#100;&amp;#x65;&amp;#114;&amp;#x2e;&amp;#x73;&amp;#105;&amp;#112;&amp;#115;&amp;#x40;&amp;#x6a;&amp;#112;&amp;#108;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt; The CLIMCAPS (Community Long-term Infrared Microwave Coupled Product System) algorithm is used to analyze data from the AIRS (Atmospheric Infrared Sounder) and AMSU (Advanced Microwave Sounding Unit). The AIRS instrument is a grating spectrometer (R &#x3D; 1200) aboard the second Earth Observing System (EOS) polar-orbiting platform, EOS Aqua. The AIRS in combination with the AMSU constitutes an innovative atmospheric sounding group of infrared and microwave sensors. The AIRS Standard Retrieval Product consists of retrieved estimates of cloud and surface properties, plus profiles of retrieved temperature, water vapor, ozone, carbon monoxide and methane. The temperature profile vertical resolution is 100 levels total between 1100 mb and 0.1 mb, while moisture profile is reported at atmospheric layers between 1100 mb and 300 mb. The horizontal resolution is 50 km. The CLIMCAPS algorithm uses an Optimal Estimation methodology and uses an a-priori first guess to start the process. A CLIMCAPS sounding is comprised of a set of parameters that characterizes the full atmospheric state and includes a variety of geophysical parameters derived from the CrIMSS data. These include surface temperature and infrared emissivity; full atmosphere profiles of temperature, water vapor and ozone; infrared effective cloud top characteristics; carbon monoxide, methane, carbon dioxide, sulfur dioxide, nitrous oxide, and nitric acid. An AIRS granule has been set as 6 minutes of data, 30 footprints cross track by 45 lines along track for each of the approximate 2378 channels. There are 240 granules per day, with an orbit repeat cycle of approximately 16 day.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sndraqiml2ccpccr&quot;&gt;SNDRAQIML2CCPCCR&lt;/h4&gt;
The CLIMCAPS (Community Long-term Infrared Microwave Coupled Product System) algorithm is used to analyze data from the AIRS (Atmospheric Infrared Sounder) and AMSU (Advanced Microwave Sounding Unit). The AIRS instrument is a grating spectrometer (R &#x3D; 1200) aboard the second Earth Observing System (EOS) polar-orbiting platform, EOS Aqua. The AIRS in combination with the AMSU constitutes an innovative atmospheric sounding group of infrared and microwave sensors. The AIRS Standard Retrieval Product consists of retrieved estimates of cloud and surface properties, plus profiles of retrieved temperature, water vapor, ozone, carbon monoxide and methane. The temperature profile vertical resolution is 100 levels total between 1100 mb and 0.1 mb, while moisture profile is reported at atmospheric layers between 1100 mb and 300 mb. The horizontal resolution is 50 km. Cloud-Cleared Radiances contain calibrated, geolocated channel-by-channel AIRS infrared radiances (milliWatts/m2/cm-1/steradian) that would have been observed within each AMSU footprint if there were no clouds in the FOV. An AIRS granule has been set as 6 minutes of data, 30 footprints cross track by 45 lines along track for each of the approximate 2378 channels. There are 240 granules per day, with an orbit repeat cycle of approximately 16 day.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sndraqiml2plevcps&quot;&gt;SNDRAQIML2PLEVCPS&lt;/h4&gt;
The CLIMCAPS (Community Long-term Infrared Microwave Coupled Product System) algorithm is used to analyze data from the AIRS (Atmospheric Infrared Sounder)/AMSU (Advanced Microwave Sounding Unit) instruments aboard the Earth Observing System (EOS) polar-orbiting platform, EOS Aqua. This file contains the fixed Pressure Level product (PLEV) variables derived from the CLIMCAPS algorithm using data. They include including gas mixing ratio profiles, column totals, surface values, tropopause properties, and relative humidity, together with per-field quality flagging. The profiles are specified at the surface and layer boundaries and are estimated from layer amounts using the L2 algorithm An AIRS granule has been set as 6 minutes of data, 30 footprints cross track by 45 lines along track. There are 240 granules per day, with an orbit repeat cycle of approximately 16 day. The CLIMCAPS algorithm uses data from the second Modern-Era Retrospective analysis for Research and Applications (MERRA-2) as a first-guess for the atmospheric state. Because MERRA-2 products typically have a latency from 3 to 7 weeks, so too do the CLIMCAPS products.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sndraqiml3sdccp&quot;&gt;SNDRAQIML3SDCCP&lt;/h4&gt;
WARNING: Users of the derived product “co_mmr_midtrop” (carbon monoxide mass mixing ratio to dry air [kg/kg] at ~500 hPa). This variable has a significant bias due to a conversion error: the molecular weight of carbon dioxide (CO2, 44.01 g/mol) was used instead of carbon monoxide (CO, 28.01 g/mol). To correct, simply multiply “co_mmr_midtrop” by 28.01/44.01. Alternatively, derive a profile of mass mixing ratio from scratch using the retrieved column density values (“mol_lay/co_mol_lay”) in the Level 2 files. For further questions or concerns please contact the Sounder SIPS at: &lt;a href&#x3D;&quot;mailto:&amp;#115;&amp;#x6f;&amp;#117;&amp;#x6e;&amp;#100;&amp;#x65;&amp;#114;&amp;#x2e;&amp;#x73;&amp;#x69;&amp;#112;&amp;#115;&amp;#x40;&amp;#x6a;&amp;#x70;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#115;&amp;#x6f;&amp;#117;&amp;#x6e;&amp;#100;&amp;#x65;&amp;#114;&amp;#x2e;&amp;#x73;&amp;#x69;&amp;#112;&amp;#115;&amp;#x40;&amp;#x6a;&amp;#x70;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt; The CLIMCAPS (Community Long-term Infrared Microwave Coupled Product System) algorithm is used to analyze data from the AIRS (Atmospheric Infrared Sounder) and AMSU (Advanced Microwave Sounding Unit). The AIRS instrument is a grating spectrometer (R &#x3D; 1200) aboard the second Earth Observing System (EOS) polar-orbiting platform, EOS Aqua. The AIRS in combination with the AMSU constitutes an innovative atmospheric sounding group of infrared and microwave sensors. The AIRS Standard Retrieval Product consists of retrieved estimates of cloud and surface properties, plus profiles of retrieved temperature, water vapor, ozone, carbon monoxide and methane. The temperature profile vertical resolution is 100 levels total between 1100 mb and 0.1 mb, while moisture profile is reported at atmospheric layers between 1100 mb and 300 mb. The horizontal resolution is 50 km. The CLIMCAPS algorithm uses an Optimal Estimation methodology and uses an a-priori first guess to start the process. A CLIMCAPS sounding is comprised of a set of parameters that characterizes the full atmospheric state and includes a variety of geophysical parameters derived from the CrIMSS data. These include surface temperature and infrared emissivity; full atmosphere profiles of temperature, water vapor and ozone; infrared effective cloud top characteristics; carbon monoxide, methane, carbon dioxide, sulfur dioxide, nitrous oxide, and nitric acid. This daily one degree latitude by one degree longitude level-3 product starts with level-2 retrieval products applying the specific quality control (QC) methodology. Specific QC accepts profile level from the top of the atmosphere down to the level where the QC determines that it is still good. Below this level, the data is rejected.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sndraqil2cps&quot;&gt;SNDRAQIL2CPS&lt;/h4&gt;
The CLIMCAPS (Community Long-term Infrared Microwave Coupled Product System) algorithm is used to analyze data from the AIRS (Atmospheric Infrared Sounder). The AIRS instrument is a grating spectrometer (R &#x3D; 1200) aboard the second Earth Observing System (EOS) polar-orbiting platform, EOS Aqua. The AIRS CLIMCAPS Retrieval Product consists of retrieved estimates of cloud and surface properties, plus profiles of retrieved temperature, water vapor, ozone, carbon monoxide and methane. The temperature profile vertical resolution is 100 levels total between 1100 mb and 0.1 mb, while moisture profile is reported at atmospheric layers between 1100 mb and 300 mb. The horizontal resolution is 50 km. The CLIMCAPS algorithm uses an Optimal Estimation methodology and uses an a-priori first guess to start the process. A CLIMCAPS sounding is comprised of a set of parameters that characterizes the full atmospheric state and includes a variety of geophysical parameters derived from the CrIMSS data. These include surface temperature and infrared emissivity; full atmosphere profiles of temperature, water vapor and ozone; infrared effective cloud top characteristics; carbon monoxide, methane, carbon dioxide, sulfur dioxide, nitrous oxide, and nitric acid. An AIRS level 2 granule has been set as 6 minutes of data, 30 footprints cross track by 45 lines along track. There are 240 granules per day, with an orbit repeat cycle of approximately 16 day.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sndraqil2plevcps&quot;&gt;SNDRAQIL2PLEVCPS&lt;/h4&gt;
The CLIMCAPS (Community Long-term Infrared Microwave Coupled Product System) algorithm is used to analyze data from the AIRS (Atmospheric Infrared Sounder) instrument aboard the Earth Observing System (EOS) polar-orbiting platform, EOS Aqua. This file contains the fixed Pressure Level product (PLEV) variables derived from the CLIMCAPS algorithm using data. They include including gas mixing ratio profiles, column totals, surface values, tropopause properties, and relative humidity, together with per-field quality flagging. The profiles are specified at the surface and layer boundaries and are estimated from layer amounts using the L2 algorithm An AIRS granule has been set as 6 minutes of data, 30 footprints cross track by 45 lines along track. There are 240 granules per day, with an orbit repeat cycle of approximately 16 day. The CLIMCAPS algorithm uses data from the second Modern-Era Retrospective analysis for Research and Applications (MERRA-2) as a first-guess for the atmospheric state. Because MERRA-2 products typically have a latency from 3 to 7 weeks, so too do the CLIMCAPS products.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sndraqiml1bcalsubsum&quot;&gt;SNDRAQIML1BCALSUBSUM&lt;/h4&gt;
The Atmospheric Infrared Sounder (AIRS) is a grating spectrometer (R &#x3D; 1200) aboard the second Earth Observing System (EOS) polar-orbiting platform, EOS Aqua. AIRS/Aqua Level-1C calibration subset including clear cases, special calibration sites, random nadir spots, and high clouds. Infrared temperature sounders generate a large amount of Level-1B spectral data. For example, the AIRS instrument with 2378 channels, its visible light component and AMSU with 15 channels create 3x240 files each day, for a total of over 500 MB of data. The purpose of the Calibration Data Subsets is extract key information from these data into a few daily files to: 1. Facilitate a quick evaluation of the absolute calibration of the instruments. 2. Facilitate an assessment of the instrument performance under clear, cloudy, and extreme hot and cold conditions. 3. Facilitate the evaluation of instrument trends and their significance relative to climate trends. 4. Facilitate the comparison of AIRS with CrIS using their equivalent data subsets. The output files are constructed from Level-1B or Level-1C IR and MW brightness or antenna temperatures. Each file contains selected observations taken from a nominal 24-hour period. The “summary” product includes a large set of cases of interest, including all identified spectra that match selection criteria detailed below for clear, special cloud classes, etc. These amount to about 10% of all spectra. But for each selected case only brightness temperatures (BTs) for selected key channels are saved.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sndr13chrp1&quot;&gt;SNDR13CHRP1&lt;/h4&gt;
The Climate Hyperspectral Infrared Radiance Product (CHIRP) is a Level 1 radiance product derived from Atmospheric Infrared Sounder (AIRS) on EOS-AQUA and the Cross-Track Infrared Sounders (CrIS) on the SNPP and JPSS-1+ platforms. (JPSS-1 is also called NOAA-20). CHIRP provides a consistent spectral response function (SRF) across all instruments. Inter-instrument radiometric offsets are removed with SNPP-CrIS chosen as the &amp;quot;standard&amp;quot;. CHIRP follows the original instrument storage, i.e., granule in, granule out, and contains all information needed for retrievals (including cross-track, along-track, fov id, etc.). This version of CHIRP, SNDR13CHRP1, is the primary CHIRP product which provides a full radiance record from 2002 onwards starting with AIRS from September 1, 2002 to August 30, 2016, switching to the SNPP CrIS instrument on September 1, 2016. The SNDR13CHRP1 product then switches to using JPSS-1 CrIS radiances starting September 1, 2018. This selection of time periods provides the best match to times when the microwave sounders on each of these platforms exhibited good performance and avoids long outages (such as SNPP CrIS in early Spring 2019). CHIRP is available for AIRS, CrIS-SNPP, and CrIS-JPSS-1 for time periods not used in the product distributed here, and are named SNDR13CHRP1AQCal, SNDR13CHRP1SNCal, and SNDR13CHRP1J1Cal respectively.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sndraqil3ssdfcnsat&quot;&gt;SNDRAQIL3SSDFCNSAT&lt;/h4&gt;
This data set provides an estimate of the surface air temperature. It infers a value for each grid point based on nearby and distant values of the input Level-2 datasets and estimates of the variance of those values, with lower variances given higher weight. The Spatial Statistical Data Fusion (SSDF) surface continental United States (CONUS) products, fuse data from the Atmospheric InfraRed Sounder (AIRS) instrument on the EOS-Aqua spacecraft with data from the Cross-track Infrared and Microwave Sounding Suite (CrIMSS) instruments on the Suomi-NPP spacecraft. The CrIMSS instrument suite consists of the Cross-track Infrared Sounder (CrIS) infrared sounder and the Advanced Technology Microwave Sounder (ATMS) microwave sounder. It infers a value for each grid point based on nearby and distant values of the input Level-2 datasets and estimates of the variance of those values, with lower variances given higher weight. These are all daily products on a ¼ x ¼ degree latitude/longitude grid covering the continental United States (CONUS). The SSDF algorithm infers a value for each grid point based on nearby and distant values of the input Level-2 datasets and estimates of the variance of those values, with lower variances given higher weight. Performing the data fusion of two (or more) remote sensing datasets that estimate the same physical state involves four major steps: (1) Filtering input data; (2) Matching the remote sensing datasets to an in situ dataset, taken as a truth estimate; (3) Using these matchups to characterize the input datasets via estimation of their bias and variance relative to the truth estimate; (4) Performing the spatial statistical data fusion. We note that SSDF can also be performed on a single remote sensing input dataset. The SSDF algorithm only ingests the bias-corrected estimates, their latitudes and longitudes, and their estimated variances; the algorithm is agnostic as to which dataset or datasets those estimates, latitudes, longitudes, and variances originated from.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sndraqil3ssdfcvpd&quot;&gt;SNDRAQIL3SSDFCVPD&lt;/h4&gt;
This data set provides an estimate of the vapor pressure deficit. It infers a value for each grid point based on nearby and distant values of the input Level-2 datasets and estimates of the variance of those values, with lower variances given higher weight. The Spatial Statistical Data Fusion (SSDF) surface continental United States (CONUS) products, fuse data from the Atmospheric InfraRed Sounder (AIRS) instrument on the EOS-Aqua spacecraft with data from the Cross-track Infrared and Microwave Sounding Suite (CrIMSS) instruments on the Suomi-NPP spacecraft. The CrIMSS instrument suite consists of the Cross-track Infrared Sounder (CrIS) infrared sounder and the Advanced Technology Microwave Sounder (ATMS) microwave sounder. These are all daily products on a ¼ x ¼ degree latitude/longitude grid covering the continental United States (CONUS). The SSDF algorithm infers a value for each grid point based on nearby and distant values of the input Level-2 datasets and estimates of the variance of those values, with lower variances given higher weight. Performing the data fusion of two (or more) remote sensing datasets that estimate the same physical state involves four major steps: (1) Filtering input data; (2) Matching the remote sensing datasets to an in situ dataset, taken as a truth estimate; (3) Using these matchups to characterize the input datasets via estimation of their bias and variance relative to the truth estimate; (4) Performing the spatial statistical data fusion. We note that SSDF can also be performed on a single remote sensing input dataset. The SSDF algorithm only ingests the bias-corrected estimates, their latitudes and longitudes, and their estimated variances; the algorithm is agnostic as to which dataset or datasets those estimates, latitudes, longitudes, and variances originated from.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sndr13iml3ssdfcvpd&quot;&gt;SNDR13IML3SSDFCVPD&lt;/h4&gt;
The Spatial Statistical Data Fusion (SSDF) surface continental United States (CONUS) products, fuse data from the Atmospheric InfraRed Sounder (AIRS) instrument on the EOS-Aqua spacecraft with data from the Cross-track Infrared and Microwave Sounding Suite (CrIMSS) instruments on the Suomi-NPP spacecraft. The CrIMSS instrument suite consists of the Cross-track Infrared Sounder (CrIS) infrared sounder and the Advanced Technology Microwave Sounder (ATMS) microwave sounder. This data set provides an estimate of the vapor pressure deficit. It infers a value for each grid point based on nearby and distant values of the input Level-2 datasets and estimates of the variance of those values, with lower variances given higher weight. These are all daily products on a ¼ x ¼ degree latitude/longitude grid covering the continental United States (CONUS). The SSDF algorithm infers a value for each grid point based on nearby and distant values of the input Level-2 datasets and estimates of the variance of those values, with lower variances given higher weight. Performing the data fusion of two (or more) remote sensing datasets that estimate the same physical state involves four major steps: (1) Filtering input data; (2) Matching the remote sensing datasets to an in situ dataset, taken as a truth estimate; (3) Using these matchups to characterize the input datasets via estimation of their bias and variance relative to the truth estimate; (4) Performing the spatial statistical data fusion. We note that SSDF can also be performed on a single remote sensing input dataset. The SSDF algorithm only ingests the bias-corrected estimates, their latitudes and longitudes, and their estimated variances; the algorithm is agnostic as to which dataset or datasets those estimates, latitudes, longitudes, and variances originated from.
&lt;br&gt;&lt;h4 id&#x3D;&quot;mydfds_sdv_glb_l3&quot;&gt;MYDFDS_SDV_GLB_L3&lt;/h4&gt;
Version 1 is the current version of the dataset. This collection MYDFDS_SDV_GLB_L3 provides level 3 standard deviation of climatological monthly frequency of dust storms (FDS) over land from 175°W to 175°E and 80°S to 80°N at a spatial resolution of 0.1˚ x 0.1˚. It is derived from Level 2, the Moderate Resolution Imaging Spectroradiometer (MODIS) Deep Blue aerosol products Collection 6.1 from Aqua (MYD04_L2). The dataset is the standard deviation of climatological monthly mean for each month over 2003 to 2022. The FDS is calculated as the number of days per month when the daily dust optical depth is greater than a threshold optical depth (e.g., 0.025) with two quality flags: the lowest (1) and highest (3). It is advised to use flag 1, which is of lower quality, over dust source regions, and flag 3 over remote areas or polluted regions. Eight thresholds (0.025, 0.05, 0.1, 0.25, 0.5, 0.75, 1, 2) are saved separately in eight files. If you have any questions, please read the README document first and post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#45;&amp;#100;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#97;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#45;&amp;#100;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#97;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA Aura Project</title>
      <link>https://registry.opendata.aws/nasa-aura</link>
      <guid>https://registry.opendata.aws/nasa-aura</guid>
      <description>Aura (Latin for breeze) obtains measurements of ozone, aerosols and key gases throughout the atmosphere.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omufpmet&quot;&gt;OMUFPMET&lt;/h4&gt;
The GEOS-5 FP-IT 3D Time-Averaged Model-Layer Assimilated Data Geo-Colocated to OMI/Aura UV2 1-Orbit L2 Swath 13x24km (OMUFPMET) product provides selected meteorlogical fields from the GEOS-5 Forward Processing for Instrument Teams (FP-IT) assimilated product produced by the Global Modeling and Assimilation Office (GMAO) co-located in space and time with the OMI UV-2 swath. The fields in this product include layer pressure thickness, surface pressure, vertical temperature profiles, surface potential, and mid-layer pressure along with geolocation info. The OMI team also provides a corresponding product for the OMI VIS swath, OMVFPMET. The OMI ancillary products were developed to provide supplementary information for use with the OMI collection 4 L1B data sets. The original GEOS-5 FP-IT data are reported on a 0.625 deg longitude by 0.5 deg latitude grid, whereas the OMI UV-2 spatial resolution is 13km x 24km at nadir. The OMUFPMET files are in netCDF4 format which is compatible with most netCDF and HDF5 readers and tools. Each file is approximately 45mb in size. The lead for this product is Zachary Fasnacht of SSAI. Joanna Joiner is the responsible NASA official.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omvfpmet&quot;&gt;OMVFPMET&lt;/h4&gt;
The GEOS-5 FP-IT 3D Time-Averaged Model-Layer Assimilated Data Geo-Colocated to OMI/Aura VIS 1-Orbit L2 Swath 13x24km (OMVFPMET) product provides selected meteorlogical fields from the GEOS-5 Forward Processing for Instrument Teams (FP-IT) assimilated product produced by the Global Modeling and Assimilation Office (GMAO) co-located in space and time with the OMI UV-2 swath. The fields in this product include layer pressure thickness, surface pressure, vertical temperature profiles, surface potential, and mid-layer pressure along with geolocation info. The OMI team also provides a corresponding product for the OMI UV2 swath, OMUFPMET. The OMI ancillary products were developed to provide supplementary information for use with the OMI collection 4 L1B data sets. The original GEOS-5 FP-IT data are reported on a 0.625 deg longitude by 0.5 deg latitude grid, whereas the OMI UV-2 spatial resolution is 13km x 24km at nadir. The OMVFPMET files are in netCDF4 format which is compatible with most netCDF and HDF5 readers and tools. Each file is approximately 45mb in size. The lead for this product is Zachary Fasnacht of SSAI. Joanna Joiner is the responsible NASA official.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omufpslv&quot;&gt;OMUFPSLV&lt;/h4&gt;
The GEOS-5 FP-IT 3D Time-Averaged Single-Level Diagnostics Geo-Colocated to OMI/Aura UV2 1-Orbit L2 Swath 13x24km (OMUFPSLV) provides selected parameters from GEOS-5 Forward Processing for Instrument Teams (FP-IT) assimilated product produced by the Global Modeling and Assimilation Office (GMAO) co-located in space and time with the OMI UV-2 swath. The fields in this product include boundary layer top pressure, tropopause pressure, surface pressure, surface skin temperature, and vertical wind profiles at 10m. The OMI team also provides a corresponding product for the OMI VIS swath, OMVFPSLV. The product has been generated for convenient use by the OMI/Aura team in their L2 algorithms, and for research where those L2 products are used. The original GEOS-5 FP-IT data are reported on a 0.625 deg longitude by 0.5 deg latitude grid, whereas the OMI UV-2 spatial resolution is 13km x 24km at nadir. The OMUFPSLV files are in netCDF4 format which is compatible with most netCDF and HDF5 readers and tools. Each file is approximately 45mb in size. The lead for this product is Zachary Fasnacht of SSAI. Joanna Joiner is the responsible NASA official.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omvfpslv&quot;&gt;OMVFPSLV&lt;/h4&gt;
The GEOS-5 FP-IT 3D Time-Averaged Single-Level Diagnostics Geo-Colocated to OMI/Aura VIS 1-Orbit L2 Swath 13x24km (OMVFPSLV) provides selected parameters from GEOS-5 Forward Processing for Instrument Teams (FP-IT) assimilated product produced by the Global Modeling and Assimilation Office (GMAO) co-located in space and time with the OMI UV-2 swath. The fields in this product include boundary layer top pressure, tropopause pressure, surface pressure, surface skin temperature, and vertical wind profiles at 10m. The OMI team also provides a corresponding product for the OMI UV2 swath, OMUFPSLV. The product has been generated for convenient use by the OMI/Aura team in their L2 algorithms, and for research where those L2 products are used. The original GEOS-5 FP-IT data are reported on a 0.625 deg longitude by 0.5 deg latitude grid, whereas the OMI UV-2 spatial resolution is 13km x 24km at nadir. The OMVFPSLV files are in netCDF4 format which is compatible with most netCDF and HDF5 readers and tools. Each file is approximately 45mb in size. The lead for this product is Zachary Fasnacht of SSAI. Joanna Joiner is the responsible NASA official.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omufpitmet&quot;&gt;OMUFPITMET&lt;/h4&gt;
The GEOS-5 FP-IT Assimilation Geo-colocated to OMI/Aura UV-2 1-Orbit L2 Support Swath 13x24km (OMUFPITMET) provides selected parameters from GEOS-5 Forward Processing for Instrument Teams (FP-IT) assimilated product produced by the Global Modeling and Assimilation Office (GMAO) co-located in space and time with the OMI UV-2 swath. The fields in this product include surface pressure, vertical temperature profiles, surface and vertical wind profiles, tropopause pressure, boundary layer top pressure, and surface geopotenial. The OMI team also provides a corresponding product for the OMI VIS swath, OMVFPITMET. The product has been generated for convenient use by the OMI/Aura team in their L2 algorithms, and for research where those L2 products are used. The original GEOS-5 FP-IT data are reported on a 0.625 deg longitude by 0.5 deg latitude grid, whereas the OMI UV-2 spatial resolution is 13km x 24km at nadir. To reduce the size of each orbital file, FP-IT data fields with a vertical dimension of 72 layers have been reduced to 47 layers in OMUFPITMET by combining layers above the troposphere. The OMUFPITMET files are in netCDF4 format which is compatible with most HDF5 readers and tools. Each file is approximately 45mb in size. The lead for this product is Zachary Fasnacht of SSAI. Joanna Joiner is the responsible NASA official.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omvfpitmet&quot;&gt;OMVFPITMET&lt;/h4&gt;
The GEOS-5 FP-IT Assimilation Geo-colocated to OMI/Aura VIS 1-Orbit L2 Support Swath 13x24km (OMVFPITMET) provides selected parameters from GEOS-5 Forward Processing for Instrument Teams (FP-IT) assimilated product produced by the Global Modeling and Assimilation Office (GMAO) co-located in space and time with the OMI VIS swath. The fields in this product include surface pressure, vertical temperature profiles, surface and vertical wind profiles, tropopause pressure, boundary layer top pressure, and surface geopotenial. The OMI team also provides a corresponding product for the OMI UV-2 swath, OMUFPITMET. The product has been generated for convenient use by the OMI/Aura team in their L2 algorithms, and for research where those L2 products are used. The original GEOS-5 FP-IT data are reported on a 0.625 deg longitude by 0.5 deg latitude grid, whereas the OMI VIS spatial resolution is 13km x 24km at nadir. To reduce the size of each orbital file, FP-IT data fields with a vertical dimension of 72 layers have been reduced to 47 layers in OMVFPITMET by combining layers above the troposphere. The OMVFPITMET files are in netCDF4 format which is compatible with most HDF5 readers and tools. Each file is approximately 45mb in size. The lead for this product is Zachary Fasnacht of SSAI. Joanna Joiner is the responsible NASA official.
&lt;br&gt;&lt;h4 id&#x3D;&quot;hirmls3iwc&quot;&gt;HIRMLS3IWC&lt;/h4&gt;
HIRMLS3IWC is the Joint EOS High Resolution Dynamics Limb Sounder (HIRDLS) and Microwave Limb Sounder (MLS) monthly 10 degreee lat x 20 degreee lon gridded product for ice water content (IWC) data. This is version 2 released to the public, with the original input coming from v3.3 MLS and v7 HIRDLS. The grid spatial coverage is near-global (-80 to +90 degrees latitude). The product contains HIRDLS and MLS IWC data for the time of the HIRDLS mission from February 1, 2005 through December 31, 2007. The useful vertical range of the data is from 215 to 82 hPa for both HIRDLS and MLS, and the vertical resolution is about 1.5 km for HIRDLS and 3 km for MLS. Users of the HIRMLS3IWC data product should read the Version 2 HIRDLS-MLS Level 3 IWC Data Description and Quality document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF5. The data file contains two grid objects (one with HIRDLS data, the other with MLS data), each with a set of data fields, attributes, and metadata. Each grid contains data fields with IWC values, and the HIRDLS grid includes data fields with volume density, cloud top pressure and frequency of clouds. Time, latitude and vertical pressure information are also included in each grid.
&lt;br&gt;&lt;h4 id&#x3D;&quot;hirdls2&quot;&gt;HIRDLS2&lt;/h4&gt;
The &amp;quot;HIRDLS/Aura Level 2 Geophysical Parameters&amp;quot; data product (HIRDLS2) contains an entire day&amp;#39;s worth of Level-2 vertical profiles of O3, HNO3, H2O, CFC-11, CFC-12, N2O, NO2, N2O5, ClONO2, temperature, geopotential height, and aerosol extinction at 12.1 and 8.3 microns, as well as cloud top pressure. HIRDLS measured infrared emissions in 21 channels ranging from 6.12 to 17.76 microns in the upper troposphere, stratosphere and mesosphere. Data are available for the ~3 year mission from January 29, 2005 until March 17, 2008. Observations of the Earth&amp;#39;s atmosphere were only made from the far azimuth scan (away from sun side) resulting in limited data coverage from +80 to -64 degrees latitude. The useful vertical range of the data depends on the measured species, and are provided on 24 levels per decade of pressure corresponding to about 1 km vertical resolution. The current and final version of this product is 7. Of the original targeted species, only CH4 was not retrieved in this version. The data are stored in the version 5 Hierarchical Data Format for the Earth Observing System (HDF-EOS5), which is an extension of the HDF5 format. Each file contains a single swath object with one day of data (measured species and species precision), geolocation fields (e.g. time, latitude, longitude, pressure), and swath attributes, along with file level metadata. Each file contains approximately 5600 profile scans.
&lt;br&gt;&lt;h4 id&#x3D;&quot;h3zfcclono2&quot;&gt;H3ZFCCLONO2&lt;/h4&gt;
The &amp;quot;HIRDLS/Aura Level 3 Chlorine Nitrate (ClONO2) Zonal Fourier Coefficients&amp;quot; version 7 data product (H3ZFCCLONO2) contains the entire mission (~3 years) of HIRDLS data expressed as zonal Fourier coefficients in 1 degree latitude bands from -64 to 80 degrees at 121 pressure levels. The coefficients are computed from the HIRDLS Level 2 profiles with a Kalman filter approach using both forward and backward passes in time. Expressed as the mean and up to 7 sine and cosine coefficients (4 waves for ascending and descending, 7 waves for combined), these coefficients may be used to compute values at any longitude. The data are provided on a pressure grid with 24 levels per decade, corresponding to about 1 km vertical resolution. The useful vertical range of the data is 100 to 1.0 hPa. The precision values are given by the root-mean square of the differences between the estimated fields and the input data. The data are stored in the version 5 Hierarchical Data Format for the Earth Observing System (HDF-EOS5), which is an extension of the HDF5 format. Each file contains a zonal object with data for the entire mission with separate data fields for ascending (daytime), descending (nighttime), and combined orbit node.
&lt;br&gt;&lt;h4 id&#x3D;&quot;h3zfccfc11&quot;&gt;H3ZFCCFC11&lt;/h4&gt;
The &amp;quot;HIRDLS/Aura Level 3 Chlorofluorocarbon-11 (CFC-11) Zonal Fourier Coefficients&amp;quot; version 7 data product (H3ZFCCFC11) contains the entire mission (~3 years) of HIRDLS data expressed as zonal Fourier coefficients in 1 degree latitude bands from -64 to 80 degrees at 121 pressure levels. The coefficients are computed from the HIRDLS Level 2 profiles with a Kalman filter approach using both forward and backward passes in time. Expressed as the mean and up to 7 sine and cosine coefficients (4 waves for ascending and descending, 7 waves for combined), these coefficients may be used to compute values at any longitude. The data are provided on a pressure grid with 24 levels per decade, corresponding to about 1 km vertical resolution. The useful vertical range of the CFC-11 data is 316 to 17.8 hPa. The precision values are given by the root-mean square of the differences between the estimated fields and the input data. The data are stored in the version 5 Hierarchical Data Format for the Earth Observing System (HDF-EOS5), which is an extension of the HDF5 format. Each file contains a zonal object with data for the entire mission with separate data fields for ascending (daytime), descending (nighttime), and combined orbit node.
&lt;br&gt;&lt;h4 id&#x3D;&quot;h3zfccfc12&quot;&gt;H3ZFCCFC12&lt;/h4&gt;
The &amp;quot;HIRDLS/Aura Level 3 Chlorofluorocarbon-12 (CFC-12) Zonal Fourier Coefficients&amp;quot; version 7 data product (H3ZFCCFC12) contains the entire mission (~3 years) of HIRDLS data expressed as zonal Fourier coefficients in 1 degree latitude bands from -64 to 80 degrees at 121 pressure levels. The coefficients are computed from the HIRDLS Level 2 profiles with a Kalman filter approach using both forward and backward passes in time. Expressed as the mean and up to 7 sine and cosine coefficients (4 waves for ascending and descending, 7 waves for combined), these coefficients may be used to compute values at any longitude. The data are provided on a pressure grid with 24 levels per decade, corresponding to about 1 km vertical resolution. The useful vertical range of the CFC-12 data is 316 to 8.3 hPa. The precision values are given by the root-mean square of the differences between the estimated fields and the input data. The data are stored in the version 5 Hierarchical Data Format for the Earth Observing System (HDF-EOS5), which is an extension of the HDF5 format. Each file contains a zonal object with data for the entire mission with separate data fields for ascending (daytime), descending (nighttime), and combined orbit node.
&lt;br&gt;&lt;h4 id&#x3D;&quot;hir3scol&quot;&gt;HIR3SCOL&lt;/h4&gt;
HIR3SCOL is the EOS High Resolution Dynamics Limb Sounder (HIRDLS/Aura) level 3 daily gridded 1 x 1 deg. stratospheric columns of NO2 (nitrogen dioxide) data product. The data are gridded at 1 x 1 degree resolution from +80 to -64 degrees latitude. The stratospheric column is computed from data at 57 to 1.0 hPa. The product consists of one file spanning the entire ~3 year HIRDLS mission from January 22, 2005 through March 17, 2008. Users of the HIR3SCOL data product should read the Version 7 HIRDLS Data Description and Quality document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF5. The data file contains one grid object with data fields, attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;h3zfcn2o5&quot;&gt;H3ZFCN2O5&lt;/h4&gt;
The &amp;quot;HIRDLS/Aura Level 3 Dinitrogen Pentoxide (N2O5) Zonal Fourier Coefficients&amp;quot; version 7 data product (H3ZFCN2O) contains the entire mission (~3 years) of HIRDLS data expressed as zonal Fourier coefficients in 1 degree latitude bands from -64 to 80 degrees at 121 pressure levels. The coefficients are computed from the HIRDLS Level 2 profiles with a Kalman filter approach using both forward and backward passes in time. Expressed as the mean and up to 7 sine and cosine coefficients (4 waves for ascending and descending, 7 waves for combined), these coefficients may be used to compute values at any longitude. The data are provided on a pressure grid with 24 levels per decade, corresponding to about 1 km vertical resolution. The useful vertical range of the data is 82.5 to 1.0 hPa. The precision values are given by the root-mean square of the differences between the estimated fields and the input data. The data are stored in the version 5 Hierarchical Data Format for the Earth Observing System (HDF-EOS5), which is an extension of the HDF5 format. Each file contains a zonal object with data for the entire mission with separate data fields for ascending (daytime), descending (nighttime), and combined orbit node.
&lt;br&gt;&lt;h4 id&#x3D;&quot;h3zfc12mext&quot;&gt;H3ZFC12MEXT&lt;/h4&gt;
The &amp;quot;HIRDLS/Aura Level 3 Extinction at 12.1 Microns Zonal Fourier Coefficients&amp;quot; version 7 data product (H3ZFC12MEXT) contains the entire mission (~3 years) of HIRDLS data expressed as zonal Fourier coefficients in 1 degree latitude bands from -64 to 80 degrees at 121 pressure levels. The coefficients are computed from the HIRDLS Level 2 profiles with a Kalman filter approach using both forward and backward passes in time. Expressed as the mean and up to 7 sine and cosine coefficients (4 waves for ascending and descending, 7 waves for combined), these coefficients may be used to compute values at any longitude. The data are provided on a pressure grid with 24 levels per decade, corresponding to about 1 km vertical resolution. The useful vertical range of the data is 215 to 20 hPa. The precision values are given by the root-mean square of the differences between the estimated fields and the input data. The data are stored in the version 5 Hierarchical Data Format for the Earth Observing System (HDF-EOS5), which is an extension of the HDF5 format. Each file contains a zonal object with data for the entire mission with separate data fields for ascending (daytime), descending (nighttime), and combined orbit node.
&lt;br&gt;&lt;h4 id&#x3D;&quot;h3zfc8mext&quot;&gt;H3ZFC8MEXT&lt;/h4&gt;
The &amp;quot;HIRDLS/Aura Level 3 Extinction at 8.3 Microns Zonal Fourier Coefficients&amp;quot; version 7 data product (H3ZFC8MEXT) contains the entire mission (~3 years) of HIRDLS data expressed as zonal Fourier coefficients in 1 degree latitude bands from -64 to 80 degrees at 121 pressure levels. The coefficients are computed from the HIRDLS Level 2 profiles with a Kalman filter approach using both forward and backward passes in time. Expressed as the mean and up to 7 sine and cosine coefficients (4 waves for ascending and descending, 7 waves for combined), these coefficients may be used to compute values at any longitude. The data are provided on a pressure grid with 24 levels per decade, corresponding to about 1 km vertical resolution. The useful vertical range of the data is 215 to 20 hPa. The precision values are given by the root-mean square of the differences between the estimated fields and the input data. The data are stored in the version 5 Hierarchical Data Format for the Earth Observing System (HDF-EOS5), which is an extension of the HDF5 format. Each file contains a zonal object with data for the entire mission with separate data fields for ascending (daytime), descending (nighttime), and combined orbit node.
&lt;br&gt;&lt;h4 id&#x3D;&quot;h3zfcgph&quot;&gt;H3ZFCGPH&lt;/h4&gt;
The &amp;quot;HIRDLS/Aura Level 3 Geopotential Height Zonal Fourier Coefficients&amp;quot; version 7 data product (H3ZFCGPH) contains the entire mission (~3 years) of HIRDLS data expressed as zonal Fourier coefficients in 1 degree latitude bands from -64 to 80 degrees at 121 pressure levels. The coefficients are computed from the HIRDLS Level 2 profiles with a Kalman filter approach using both forward and backward passes in time. Expressed as the mean and up to 7 sine and cosine coefficients (4 waves for ascending and descending, 7 waves for combined), these coefficients may be used to compute values at any longitude. The data are provided on a pressure grid with 24 levels per decade, corresponding to about 1 km vertical resolution. The useful vertical range of the data is 1000 to 0.01 hPa. The precision values are given by the root-mean square of the differences between the estimated fields and the input data. The data are stored in the version 5 Hierarchical Data Format for the Earth Observing System (HDF-EOS5), which is an extension of the HDF5 format. Each file contains a zonal object with data for the entire mission with separate data fields for ascending (daytime), descending (nighttime), and combined orbit node.
&lt;br&gt;&lt;h4 id&#x3D;&quot;h3zfchno3&quot;&gt;H3ZFCHNO3&lt;/h4&gt;
The &amp;quot;HIRDLS/Aura Level 3 Nitric Acid (HNO3) Zonal Fourier Coefficients&amp;quot; version 7 data product (H3ZFCHNO3) contains the entire mission (~3 years) of HIRDLS data expressed as zonal Fourier coefficients in 1 degree latitude bands from -64 to 80 degrees at 121 pressure levels. The coefficients are computed from the HIRDLS Level 2 profiles with a Kalman filter approach using both forward and backward passes in time. Expressed as the mean and up to 7 sine and cosine coefficients (4 waves for ascending and descending, 7 waves for combined), these coefficients may be used to compute values at any longitude. The data are provided on a pressure grid with 24 levels per decade, corresponding to about 1 km vertical resolution. The useful vertical range of the data is 215 to 5.1 hPa. The precision values are given by the root-mean square of the differences between the estimated fields and the input data. The data are stored in the version 5 Hierarchical Data Format for the Earth Observing System (HDF-EOS5), which is an extension of the HDF5 format. Each file contains a zonal object with data for the entire mission with separate data fields for ascending (daytime), descending (nighttime), and combined orbit node.
&lt;br&gt;&lt;h4 id&#x3D;&quot;h3zfcno2&quot;&gt;H3ZFCNO2&lt;/h4&gt;
The &amp;quot;HIRDLS/Aura Level 3 Nitrogen Dioxide (NO2) Zonal Fourier Coefficients&amp;quot; version 7 data product (H3ZFCNO2) contains the entire mission (~3 years) of HIRDLS data expressed as zonal Fourier coefficients in 1 degree latitude bands from -64 to 80 degrees at 121 pressure levels. The coefficients are computed from the HIRDLS Level 2 profiles with a Kalman filter approach using both forward and backward passes in time. Expressed as the mean and up to 7 sine and cosine coefficients (4 waves for ascending and descending, 7 waves for combined), these coefficients may be used to compute values at any longitude. The data are provided on a pressure grid with 24 levels per decade, corresponding to about 1 km vertical resolution. The useful vertical range of the data is 100 to 5.1 hPa. The precision values are given by the root-mean square of the differences between the estimated fields and the input data. The data are stored in the version 5 Hierarchical Data Format for the Earth Observing System (HDF-EOS5), which is an extension of the HDF5 format. Each file contains a zonal object with data for the entire mission with separate data fields for ascending (daytime), descending (nighttime), and combined orbit node.
&lt;br&gt;&lt;h4 id&#x3D;&quot;h3zfcn2o&quot;&gt;H3ZFCN2O&lt;/h4&gt;
The &amp;quot;HIRDLS/Aura Level 3 Nitrous Oxide (N2O) Zonal Fourier Coefficients&amp;quot; version 7 data product (H3ZFCN2O) contains the entire mission (~3 years) of HIRDLS data expressed as zonal Fourier coefficients in 1 degree latitude bands from -64 to 80 degrees at 121 pressure levels. The coefficients are computed from the HIRDLS Level 2 profiles with a Kalman filter approach using both forward and backward passes in time. Expressed as the mean and up to 7 sine and cosine coefficients (4 waves for ascending and descending, 7 waves for combined), these coefficients may be used to compute values at any longitude. The data are provided on a pressure grid with 24 levels per decade, corresponding to about 1 km vertical resolution. The useful vertical range of the data is 100 to 5.1 hPa. The precision values are given by the root-mean square of the differences between the estimated fields and the input data. The data are stored in the version 5 Hierarchical Data Format for the Earth Observing System (HDF-EOS5), which is an extension of the HDF5 format. Each file contains a zonal object with data for the entire mission with separate data fields for ascending (daytime), descending (nighttime), and combined orbit node.
&lt;br&gt;&lt;h4 id&#x3D;&quot;h3zfco3&quot;&gt;H3ZFCO3&lt;/h4&gt;
The &amp;quot;HIRDLS/Aura Level 3 Ozone (O3) Zonal Fourier Coefficients&amp;quot; version 7 data product (H3ZFCO3) contains the entire mission (~3 years) of HIRDLS data expressed as zonal Fourier coefficients in 1 degree latitude bands from -64 to 80 degrees at 121 pressure levels. The coefficients are computed from the HIRDLS Level 2 profiles with a Kalman filter approach using both forward and backward passes in time. Expressed as the mean and up to 7 sine and cosine coefficients (4 waves for ascending and descending, 7 waves for combined), these coefficients may be used to compute values at any longitude. The data are provided on a pressure grid with 24 levels per decade, corresponding to about 1 km vertical resolution. The useful vertical range of the data is 422 to 0.1 hPa. The precision values are given by the root-mean square of the differences between the estimated fields and the input data. The data are stored in the version 5 Hierarchical Data Format for the Earth Observing System (HDF-EOS5), which is an extension of the HDF5 format. Each file contains a zonal object with data for the entire mission with separate data fields for ascending (daytime), descending (nighttime), and combined orbit node.
&lt;br&gt;&lt;h4 id&#x3D;&quot;h3zfct&quot;&gt;H3ZFCT&lt;/h4&gt;
The &amp;quot;HIRDLS/Aura Level 3 Temperature Zonal Fourier Coefficients&amp;quot; version 7 data product (H3ZFCT) contains the entire mission (~3 years) of HIRDLS data expressed as zonal Fourier coefficients in 1 degree latitude bands from -64 to 80 degrees at 121 pressure levels. The coefficients are computed from the HIRDLS Level 2 profiles with a Kalman filter approach using both forward and backward passes in time. Expressed as the mean and up to 7 sine and cosine coefficients (4 waves for ascending and descending, 7 waves for combined), these coefficients may be used to compute values at any longitude. The data are provided on a pressure grid with 24 levels per decade, corresponding to about 1 km vertical resolution. The useful vertical range of the data is 1000 to 0.0042 hPa. The precision values are given by the root-mean square of the differences between the estimated fields and the input data. The data are stored in the version 5 Hierarchical Data Format for the Earth Observing System (HDF-EOS5), which is an extension of the HDF5 format. Each file contains a zonal object with data for the entire mission with separate data fields for ascending (daytime), descending (nighttime), and combined orbit node.
&lt;br&gt;&lt;h4 id&#x3D;&quot;h3zfch2o&quot;&gt;H3ZFCH2O&lt;/h4&gt;
The &amp;quot;HIRDLS/Aura Level 3 Water Vapor (H2O) Zonal Fourier Coefficients&amp;quot; version 7 data product (H3ZFCH2O) contains the entire mission (~3 years) of HIRDLS data expressed as zonal Fourier coefficients in 1 degree latitude bands from -64 to 80 degrees at 121 pressure levels. The coefficients are computed from the HIRDLS Level 2 profiles with a Kalman filter approach using both forward and backward passes in time. Expressed as the mean and up to 7 sine and cosine coefficients (4 waves for ascending and descending, 7 waves for combined), these coefficients may be used to compute values at any longitude. The data are provided on a pressure grid with 24 levels per decade, corresponding to about 1 km vertical resolution. The useful vertical range of the data is 200 to 10 hPa. The precision values are given by the root-mean square of the differences between the estimated fields and the input data. The data are stored in the version 5 Hierarchical Data Format for the Earth Observing System (HDF-EOS5), which is an extension of the HDF5 format. Each file contains a zonal object with data for the entire mission with separate data fields for ascending (daytime), descending (nighttime), and combined orbit node.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzmbro&quot;&gt;ML3DZMBRO&lt;/h4&gt;
ML3DZMBRO is the EOS Aura Microwave Limb Sounder (MLS) daily zonal mean product for bromine monoxide derived from radiances measured by the 640 GHz radiometer. The data version is 5.0. Data coverage is from August 2, 2005 to current. Spatial coverage is near-global (-85 degrees to 85 degrees latitude) spaced every 10 degrees in latitude. The recommended useful vertical range is between 10 and 4.64 hPa, and the vertical resolution is about 5 km. Users of the ML3DZMBRO data product should read the MLS Radiance Average Retrievals (RAR) BrO Product Guideline document, as well as section 3.2 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data are stored in the version 4 network Common Data Form (netCDF4), which is built on the version 5 Hierarchical Data Format, or HDF5. The netCDF4 files follow the Climate and Forecast (CF) metadata conventions. Each file contains two zonal means objects or groups, one with data from the ascending part of the MLS orbit, the other with the descending data. Each zonal means object contains the average, error (precision), solar zenith angle, and local solar time for each latitude band and pressure level. Files also contain metadata attributes describing the data and product.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzmho2&quot;&gt;ML3DZMHO2&lt;/h4&gt;
ML3DZMHO2 is the EOS Aura Microwave Limb Sounder (MLS) daily zonal mean product for hydroperoxy derived from radiances measured in two bands from the 640 GHz radiometer. The data version is 5.0. Data coverage is from August 2, 2005 to current. Spatial coverage is near-global (-85 degrees to 85 degrees latitude) spaced every 10 degrees in latitude. The recommended useful vertical range is between 21.5 to 0.0464 hPa, and the vertical resolution is about 5 km. Users of the ML3DZMHO2 data product should read the MLS Radiance Average Retrievals (RAR) Product Guideline document, as well as section 3.2 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data are stored in the version 4 network Common Data Form (netCDF4), which is built on the version 5 Hierarchical Data Format, or HDF5. The netCDF4 files follow the Climate and Forecast (CF) metadata conventions. Each file contains two zonal means objects or groups, one with data from the daytime part of the MLS orbit, the other with the nighttime data. Each zonal means object contains the average, error (precision), solar zenith angle, and local solar time for each latitude band and pressure level. Files also contain metadata attributes describing the data and product.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml1oa&quot;&gt;ML1OA&lt;/h4&gt;
ML1OA is the EOS Aura Microwave Limb Sounder (MLS) product containing the level 1 orbit attitude and tangent point geolocation data. The data version is 4.2. Data coverage is from August 8, 2004 to current. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), and files contain a full days worth of data (15 orbits). Users of the ML1OA data product should read the &amp;#39;A Short Guide to the Use and Interpretation of v4.2x Level 1 Data&amp;#39; document for additional information. The data are stored in the version 5 Hierarchical Data Format, or HDF-5. Each file contains orbital and attitude information written as HDF-5 dataset objects (n-dimensional arrays), along with file attributes and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml1oa-1&quot;&gt;ML1OA&lt;/h4&gt;
ML1OA is the EOS Aura Microwave Limb Sounder (MLS) product containing the level 1 orbit attitude and tangent point geolocation data. The data version is 5.0. Data coverage is from August 8, 2004 to current. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), and files contain a full days worth of data (15 orbits). Users of the ML1OA data product should read the &amp;#39;A Short Guide to the Use and Interpretation of v4.2x Level 1 Data&amp;#39; document for additional information. The data are stored in the version 5 Hierarchical Data Format, or HDF-5. Each file contains orbital and attitude information written as HDF-5 dataset objects (n-dimensional arrays), along with file attributes and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml1radd&quot;&gt;ML1RADD&lt;/h4&gt;
ML1RADD is the EOS Aura Microwave Limb Sounder (MLS) product containing the level 1 radiances from the digital autocorrelators. The data version is 4.2. Data coverage is from August 8, 2004 to current. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), and files contain a full days worth of data (15 orbits). Users of the ML1RADD data product should read the &amp;#39;A Short Guide to the Use and Interpretation of v4.2x Level 1 Data&amp;#39; document for additional information. The data are stored in the version 5 Hierarchical Data Format, or HDF-5. Each file contains radiances and ancillary information written as HDF-5 dataset objects (n-dimensional arrays), along with file attributes and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml1radd-1&quot;&gt;ML1RADD&lt;/h4&gt;
ML1RADD is the EOS Aura Microwave Limb Sounder (MLS) product containing the level 1 radiances from the digital autocorrelators. The data version is 5.0. Data coverage is from August 8, 2004 to current. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), and files contain a full days worth of data (15 orbits). Users of the ML1RADD data product should read the &amp;#39;A Short Guide to the Use and Interpretation of v4.2x Level 1 Data&amp;#39; document for additional information. The data are stored in the version 5 Hierarchical Data Format, or HDF-5. Each file contains radiances and ancillary information written as HDF-5 dataset objects (n-dimensional arrays), along with file attributes and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml1radg&quot;&gt;ML1RADG&lt;/h4&gt;
ML1RADG is the EOS Aura Microwave Limb Sounder (MLS) product containing the level 1 radiances from the filter banks for the GHz radiometers. The data version is 4.2. Data coverage is from August 8, 2004 to current. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), and files contain a full days worth of data (15 orbits). Users of the ML1RADG data product should read the &amp;#39;A Short Guide to the Use and Interpretation of v4.2x Level 1 Data&amp;#39; document for additional information. The data are stored in the version 5 Hierarchical Data Format, or HDF-5. Each file contains radiances and ancillary information written as HDF-5 dataset objects (n-dimensional arrays), along with file attributes and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml1radg-1&quot;&gt;ML1RADG&lt;/h4&gt;
ML1RADG is the EOS Aura Microwave Limb Sounder (MLS) product containing the level 1 radiances from the filter banks for the GHz radiometers. The data version is 5.0. Data coverage is from August 8, 2004 to current. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), and files contain a full days worth of data (15 orbits). Users of the ML1RADG data product should read the &amp;#39;A Short Guide to the Use and Interpretation of v4.2x Level 1 Data&amp;#39; document for additional information. The data are stored in the version 5 Hierarchical Data Format, or HDF-5. Each file contains radiances and ancillary information written as HDF-5 dataset objects (n-dimensional arrays), along with file attributes and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml1radt&quot;&gt;ML1RADT&lt;/h4&gt;
ML1RADT is the EOS Aura Microwave Limb Sounder (MLS) product containing the level 1 radiances from the filter banks for the GHz radiometers. The data version is 4.2. Data coverage is from August 8, 2004 to current. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), and files contain a full days worth of data (15 orbits). Users of the ML1RADG data product should read the &amp;#39;A Short Guide to the Use and Interpretation of v4.2x Level 1 Data&amp;#39; document for additional information. The data are stored in the version 5 Hierarchical Data Format, or HDF-5. Each file contains radiances and ancillary information written as HDF-5 dataset objects (n-dimensional arrays), along with file attributes and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml1radt-1&quot;&gt;ML1RADT&lt;/h4&gt;
ML1RADT is the EOS Aura Microwave Limb Sounder (MLS) product containing the level 1 radiances from the filter banks for the GHz radiometers. The data version is 5.0. Data coverage is from August 8, 2004 to current. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), and files contain a full days worth of data (15 orbits). Users of the ML1RADG data product should read the &amp;#39;A Short Guide to the Use and Interpretation of v4.2x Level 1 Data&amp;#39; document for additional information. The data are stored in the version 5 Hierarchical Data Format, or HDF-5. Each file contains radiances and ancillary information written as HDF-5 dataset objects (n-dimensional arrays), along with file attributes and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2bro&quot;&gt;ML2BRO&lt;/h4&gt;
ML2BRO is the EOS Aura Microwave Limb Sounder (MLS) standard product for bromine monoxide derived from radiances measured by the 640 GHz radiometer. The data version is 4.2. Data coverage is from August 8, 2004 to current. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is between 10 and 3.16 hPa, and the vertical resolution is about 5.5 km (6 km at 3.16 hPa). Users of the ML2BRO data product should read section 3.2 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2bro-1&quot;&gt;ML2BRO&lt;/h4&gt;
ML2BRO is the EOS Aura Microwave Limb Sounder (MLS) standard product for bromine monoxide derived from radiances measured by the 640 GHz radiometer. The data version is 5.0. Data coverage is from August 8, 2004 to current. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is between 10 and 3.16 hPa, and the vertical resolution is about 5.5 km (6 km at 3.16 hPa). Users of the ML2BRO data product should read section 3.2 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2co&quot;&gt;ML2CO&lt;/h4&gt;
ML2CO is the EOS Aura Microwave Limb Sounder (MLS) standard product for carbon monoxide derived from radiances measured by the 640 GHz radiometer. The data version is 4.2. Data coverage is from August 8, 2004 to current. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is between 215 and 0.00464 hPa, and the vertical resolution is about 6 km. Users of the ML2CO data product should read section 3.7 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2co-1&quot;&gt;ML2CO&lt;/h4&gt;
ML2CO is the EOS Aura Microwave Limb Sounder (MLS) standard product for carbon monoxide derived from radiances measured by the 640 GHz radiometer. The data version is 5.0. Data coverage is from August 8, 2004 to current. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is between 215 and 0.00564 hPa, and the vertical resolution is about 6 km. Users of the ML2CO data product should read section 3.7 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2clo&quot;&gt;ML2CLO&lt;/h4&gt;
ML2CLO is the EOS Aura Microwave Limb Sounder (MLS) standard product for chlorine monoxide derived from radiances measured primarily by the 640 GHz radiometer. The data version is 4.2. Data coverage is from August 8, 2004 to current. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is between 147 and 1.0 hPa, and the vertical resolution varies between 3 and 4.5 km. Users of the ML2CLO data product should read section 3.6 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2clo-1&quot;&gt;ML2CLO&lt;/h4&gt;
ML2CLO is the EOS Aura Microwave Limb Sounder (MLS) standard product for chlorine monoxide derived from radiances measured primarily by the 640 GHz radiometer. The data version is 5.0. Data coverage is from August 8, 2004 to current. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is between 147 and 1.0 hPa, and the vertical resolution varies between 3 and 4.5 km. Users of the ML2CLO data product should read section 3.6 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2iwc&quot;&gt;ML2IWC&lt;/h4&gt;
ML2IWC is the EOS Aura Microwave Limb Sounder (MLS) standard product for cloud ice water content derived from radiances measured by the 240 GHz radiometer. The data version is 4.2. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is from 215 to 82.5 hPa, and the vertical resolution is about 3 km. Users of the ML2IWC data product should read sections 3.15 and 3.16 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2iwc-1&quot;&gt;ML2IWC&lt;/h4&gt;
ML2IWC is the EOS Aura Microwave Limb Sounder (MLS) standard product for cloud ice water content derived from radiances measured by the 240 GHz radiometer. The data version is 5.0. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is from 215 to 82.5 hPa, and the vertical resolution is about 3 km. Users of the ML2IWC data product should read sections 3.15 and 3.16 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2dgg&quot;&gt;ML2DGG&lt;/h4&gt;
ML2DGG is the EOS Aura Microwave Limb Sounder (MLS) product containing geophysical diagnostic quantities pertaining directly to the standard geophysical data products, generally on a similar (or identical) grid, and at different spectral ranges. The data version is 4.2. Data coverage is from August 8, 2004 to current. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). Vertical resolution varies between species and typically ranges from 3 - 6 km. Users of the ML2DGG data product should read the EOS MLS Level 2 Version 4 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contain swaths objects for each diagnostics measurement. Each swath has a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2dgg-1&quot;&gt;ML2DGG&lt;/h4&gt;
ML2DGG is the EOS Aura Microwave Limb Sounder (MLS) product containing geophysical diagnostic quantities pertaining directly to the standard geophysical data products, generally on a similar (or identical) grid, and at different spectral ranges. The data version is 5.0. Data coverage is from August 8, 2004 to current. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). Vertical resolution varies between species and typically ranges from 3 - 6 km. Users of the ML2DGG data product should read the EOS MLS Level 2 Version 5 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contain swaths objects for each diagnostics measurement. Each swath has a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2dgm&quot;&gt;ML2DGM&lt;/h4&gt;
ML2DGM is the EOS Aura Microwave Limb Sounder (MLS) product containing the minor frame diagnostic quantities on a miscellaneous grid. These include items such as tangent pressure, chi-square describing various fits to the measured radiances, number of radiances used in various retrieval phases, etc. This product contains a second auxiliary file which includes cloud-induced radiances inferred for selected spectral channels. The data version is 4.2. Data coverage is from August 8, 2004 to current. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). Vertical resolution varies between species and typically ranges from 3 - 6 km. Users of the ML2DGM data product should read the EOS MLS Level 2 Version 4 Quality Document for more information. The data are stored in the version 5 Hierarchical Data Format, or HDF5. Each file contains sets of HDF5 dataset objects (n-dimensional arrays) for each diagnostics measurement. The dataset objects represent data and geolocation fields; included in the file are file attributes and metadata. There are two files per day (MLS-Aura_L2AUX-DGM* and MLS-Aura_L2AUX-Cloud*).
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2gph&quot;&gt;ML2GPH&lt;/h4&gt;
ML2GPH is the EOS Aura Microwave Limb Sounder (MLS) standard product for geopotential height derived from radiances measured by the 118 and 240 GHz radiometers. The data version is 4.2. Data coverage is from August 8, 2004 to current. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is between 261 and 0.001 hPa, and the vertical resolution varies between ~3.6 and 6 km. Users of the ML2GPH data product should read section 3.8 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2gph-1&quot;&gt;ML2GPH&lt;/h4&gt;
ML2GPH is the EOS Aura Microwave Limb Sounder (MLS) standard product for geopotential height derived from radiances measured by the 118 and 240 GHz radiometers. The data version is 5.0. Data coverage is from August 8, 2004 to current. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is between 261 and 0.001 hPa, and the vertical resolution varies between ~3.6 and 6 km. Users of the ML2GPH data product should read section 3.8 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2hcl&quot;&gt;ML2HCL&lt;/h4&gt;
ML2HCL is the EOS Aura Microwave Limb Sounder (MLS) standard product for hydrogen chloride derived from radiances measured primarily by the 640 GHz radiometer. The data version is 4.2. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is from 100 to 0.316 hPa, and the vertical resolution is between 3 and 6 km. Users of the ML2HCL data product should read section 3.10 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2hcl-1&quot;&gt;ML2HCL&lt;/h4&gt;
ML2HCL is the EOS Aura Microwave Limb Sounder (MLS) standard product for hydrogen chloride derived from radiances measured primarily by the 640 GHz radiometer. The data version is 5.0. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is from 100 to 0.316 hPa, and the vertical resolution is between 3 and 6 km. Users of the ML2HCL data product should read section 3.10 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2hcn&quot;&gt;ML2HCN&lt;/h4&gt;
ML2HCN is the EOS Aura Microwave Limb Sounder (MLS) standard product for hydrogen cyanide derived from radiances measured primarily by the 190 GHz radiometer. The data version is 4.2. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is from 21.5 to 0.1 hPa, and the vertical resolution is between 8 and 12 km. Users of the ML2HCN data product should read section 3.11 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2hcn-1&quot;&gt;ML2HCN&lt;/h4&gt;
ML2HCN is the EOS Aura Microwave Limb Sounder (MLS) standard product for hydrogen cyanide derived from radiances measured primarily by the 190 GHz radiometer. The data version is 5.0. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is from 21.5 to 0.1 hPa, and the vertical resolution is between 8 and 12 km. Users of the ML2HCN data product should read section 3.11 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2ho2&quot;&gt;ML2HO2&lt;/h4&gt;
ML2HO2 is the EOS Aura Microwave Limb Sounder (MLS) standard product for hydroperoxy derived from radiances measured in two bands from the 640 GHz radiometer. The data version is 4.2. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is from 21.5 to 0.0464 hPa, and the vertical resolution is about 5 km. Users of the ML2HO2 data product should read section 3.13 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2ho2-1&quot;&gt;ML2HO2&lt;/h4&gt;
ML2HO2 is the EOS Aura Microwave Limb Sounder (MLS) standard product for hydroperoxy derived from radiances measured in two bands from the 640 GHz radiometer. The data version is 5.0. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is from 21.5 to 0.0464 hPa, and the vertical resolution is about 5 km. Users of the ML2HO2 data product should read section 3.13 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2oh&quot;&gt;ML2OH&lt;/h4&gt;
ML2OH is the EOS Aura Microwave Limb Sounder (MLS) standard product for hydroxyl derived from radiances measured by the THz radiometer. The data version is 4.2. Data coverage is continuous from August 8, 2004 to December 12, 2009 when the THz radiometer was placed in standby mode. After this date OH data were collected for about 30 days in August/September of 2011, 2012, 2013 and 2014. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is from 31.6 to 0.00316 hPa, and the vertical resolution is about 3. Users of the ML2OH data product should read section 3.19 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2oh-1&quot;&gt;ML2OH&lt;/h4&gt;
ML2OH is the EOS Aura Microwave Limb Sounder (MLS) standard product for hydroxyl derived from radiances measured by the THz radiometer. The data version is 5.0. Data coverage is continuous from August 8, 2004 to December 12, 2009 when the THz radiometer was placed in standby mode. After this date OH data were collected for about 30 days in August/September of 2011, 2012, 2013 and 2014. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is from 31.6 to 0.00316 hPa, and the vertical resolution is about 3. Users of the ML2OH data product should read section 3.19 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2hocl&quot;&gt;ML2HOCL&lt;/h4&gt;
ML2HOCL is the EOS Aura Microwave Limb Sounder (MLS) standard product for hypochlorous acid derived from radiances measured primarily by the 640 GHz radiometer. The data version is 4.2. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is from 10 to 2.15 hPa, and the vertical resolution is about 6 km. Users of the ML2OHCL data product should read section 3.14 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2hocl-1&quot;&gt;ML2HOCL&lt;/h4&gt;
ML2HOCL is the EOS Aura Microwave Limb Sounder (MLS) standard product for hypochlorous acid derived from radiances measured primarily by the 640 GHz radiometer. The data version is 5.0. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is from 10 to 2.15 hPa, and the vertical resolution is about 6 km. Users of the ML2OHCL data product should read section 3.14 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2ch3oh&quot;&gt;ML2CH3OH&lt;/h4&gt;
At this time it is recommended that these data not be used pending further validation.ML2CH3OH is the EOS Aura Microwave Limb Sounder (MLS) standard product for methanol derived from radiances measured by the 640 GHz radiometer. The data version is 4.2. Data coverage is from August 8, 2004 to current. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is between 147 and 100 hPa, and the vertical resolution range is about 4-5 km. Users of the ML2CH3OH data product should read section 3.5 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains one swath object (profile data), with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2ch3oh-1&quot;&gt;ML2CH3OH&lt;/h4&gt;
At this time it is recommended that these data not be used pending further validation.ML2CH3OH is the EOS Aura Microwave Limb Sounder (MLS) standard product for methanol derived from radiances measured by the 640 GHz radiometer. The data version is 5.0. Data coverage is from August 8, 2004 to current. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is between 147 and 100 hPa, and the vertical resolution range is about 4-5 km. Users of the ML2CH3OH data product should read section 3.5 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains one swath object (profile data), with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2ch3cl&quot;&gt;ML2CH3CL&lt;/h4&gt;
ML2CH3CL is the EOS Aura Microwave Limb Sounder (MLS) standard product for methyl chloride derived from radiances measured by the 640 GHz radiometer. The data version is 4.2. Data coverage is from August 8, 2004 to current. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is between 147 and 4.64 hPa, and the vertical resolution ranges between 4-6 km in the lower stratosphere and 8-10 km above 14 hPa. Users of the ML2CH3CL data product should read section 3.3 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains one swath object (profile data), with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2ch3cl-1&quot;&gt;ML2CH3CL&lt;/h4&gt;
ML2CH3CL is the EOS Aura Microwave Limb Sounder (MLS) standard product for methyl chloride derived from radiances measured by the 640 GHz radiometer. The data version is 5.0. Data coverage is from August 8, 2004 to current. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is between 147 and 4.64 hPa, and the vertical resolution ranges between 4-6 km in the lower stratosphere and 8-10 km above 14 hPa. Users of the ML2CH3CL data product should read section 3.3 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains one swath object (profile data), with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2ch3cn&quot;&gt;ML2CH3CN&lt;/h4&gt;
ML2CH3CN is the EOS Aura Microwave Limb Sounder (MLS) standard product for methyl cyanide derived from radiances measured by the 640 GHz radiometer. The data version is 4.2. Data coverage is from August 8, 2004 to current. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is between 46.4 and 1.0 hPa, and the vertical resolution ranges between ~5 km in the lower stratosphere and ~10 km in the upper stratosphere. Users of the ML2CH3CN data product should read section 3.4 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains one swath object (profile data), with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2ch3cn-1&quot;&gt;ML2CH3CN&lt;/h4&gt;
ML2CH3CN is the EOS Aura Microwave Limb Sounder (MLS) standard product for methyl cyanide derived from radiances measured by the 640 GHz radiometer. The data version is 5.0. Data coverage is from August 8, 2004 to current. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is between 46.4 and 1.0 hPa, and the vertical resolution ranges between ~5 km in the lower stratosphere and ~10 km in the upper stratosphere. Users of the ML2CH3CN data product should read section 3.4 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains one swath object (profile data), with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2hno3&quot;&gt;ML2HNO3&lt;/h4&gt;
ML2HNO3 is the EOS Aura Microwave Limb Sounder (MLS) standard product for nitric acid derived from radiances measured by the 240 GHz radiometer at and below 10 hPa, and from the 190 GHz radiometer above 10 hPa. The data version is 4.2. Data coverage is from August 8, 2004 to current. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is from 215 to 1.47 hPa (1.0 hPa under enhanced conditions), and the vertical resolution is between about 3 and 5 km. Users of the ML2HNO3 data product should read section 3.12 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2hno3-1&quot;&gt;ML2HNO3&lt;/h4&gt;
ML2HNO3 is the EOS Aura Microwave Limb Sounder (MLS) standard product for nitric acid derived from radiances measured by the 240 GHz radiometer at and below 10 hPa, and from the 190 GHz radiometer above 10 hPa. The data version is 5.0. Data coverage is from August 8, 2004 to current. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is from 215 to 1.47 hPa (1.0 hPa under enhanced conditions), and the vertical resolution is between about 3 and 5 km. Users of the ML2HNO3 data product should read section 3.12 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2n2o&quot;&gt;ML2N2O&lt;/h4&gt;
ML2N2O is the EOS Aura Microwave Limb Sounder (MLS) standard product for nitrous oxide derived from radiances measured primarily by the 640 GHz radiometer (Band 12) until August 6, 2013, after this date using the 190 GHz radiometer (Band 3). The data version is 4.2. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is from 68.1 to 0.464 hPa, and the vertical resolution is between 4 and 6 km. Users of the ML2N2O data product should read section 3.17 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2n2o-1&quot;&gt;ML2N2O&lt;/h4&gt;
ML2N2O is the EOS Aura Microwave Limb Sounder (MLS) standard product for nitrous oxide derived from radiances measured primarily by the 640 GHz radiometer (Band 12) until August 6, 2013, after this date using the 190 GHz radiometer (Band 3). The data version is 5.0. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is from 68.1 to 0.464 hPa, and the vertical resolution is between 4 and 6 km. Users of the ML2N2O data product should read section 3.17 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2o3&quot;&gt;ML2O3&lt;/h4&gt;
ML2O3 is the EOS Aura Microwave Limb Sounder (MLS) standard product for ozone derived from radiances measured by the 240 GHz radiometer. The data version is 4.2. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is from 261 to 0.0215 hPa, and the vertical resolution is between 2.5 and 6 km. Users of the ML2O3 data product should read section 3.18 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2o3-1&quot;&gt;ML2O3&lt;/h4&gt;
ML2O3 is the EOS Aura Microwave Limb Sounder (MLS) standard product for ozone derived from radiances measured by the 240 GHz radiometer. The data version is 5.0. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is from 261 to 0.0215 hPa, and the vertical resolution is between 2.5 and 6 km. Users of the ML2O3 data product should read section 3.18 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2rhi&quot;&gt;ML2RHI&lt;/h4&gt;
ML2RHI is the EOS Aura Microwave Limb Sounder (MLS) standard product for relative humidity with respect to ice derived from radiances measured by the 118 and 190 GHz radiometers. The data version is 4.2. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is from 316 to 0.0215 hPa, and the vertical resolution is between 3 and 6 km. Users of the ML2RHI data product should read section 3.20 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2rhi-1&quot;&gt;ML2RHI&lt;/h4&gt;
ML2RHI is the EOS Aura Microwave Limb Sounder (MLS) standard product for relative humidity with respect to ice derived from radiances measured by the 118 and 190 GHz radiometers. The data version is 5.0. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is from 316 to 0.0215 hPa, and the vertical resolution is between 3 and 6 km. Users of the ML2RHI data product should read section 3.20 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2so2&quot;&gt;ML2SO2&lt;/h4&gt;
ML2SO2 is the EOS Aura Microwave Limb Sounder (MLS) standard product for sulfur dioxide derived from radiances measured by the 240 GHz radiometer. The data version is 4.2. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is from 215 to 10 hPa, and the vertical resolution is about 3 km. Users of the ML2SO2 data product should read section 3.21 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2so2-1&quot;&gt;ML2SO2&lt;/h4&gt;
ML2SO2 is the EOS Aura Microwave Limb Sounder (MLS) standard product for sulfur dioxide derived from radiances measured by the 240 GHz radiometer. The data version is 5.0. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is from 215 to 10 hPa, and the vertical resolution is about 3 km. Users of the ML2SO2 data product should read section 3.21 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2t&quot;&gt;ML2T&lt;/h4&gt;
ML2T is the EOS Aura Microwave Limb Sounder (MLS) standard product for temperature derived from radiances measured by the 118 and 240 GHz radiometers. The data version is 4.2. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is from 261 to 0.001 hPa, and the vertical resolution is between 3 and 6 km. Users of the ML2T data product should read section 3.22 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2t-1&quot;&gt;ML2T&lt;/h4&gt;
ML2T is the EOS Aura Microwave Limb Sounder (MLS) standard product for temperature derived from radiances measured by the 118 and 240 GHz radiometers. The data version is 5.0. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is from 261 to 0.001 hPa, and the vertical resolution is between 3 and 6 km. Users of the ML2T data product should read section 3.22 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2h2o&quot;&gt;ML2H2O&lt;/h4&gt;
ML2H2O is the EOS Aura Microwave Limb Sounder (MLS) standard product for water vapor derived from radiances measured primarily by the 190 GHz radiometer. The data version is 4.2. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is between 316 and 0.00215 hPa, and the vertical resolution is about 1.5 km at 316 hPa increasing to 3.5 km to 4.64 hPa, and degrades to 15 km above 0.1 hPa. Users of the ML2H2O data product should read section 3.9 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2h2o-1&quot;&gt;ML2H2O&lt;/h4&gt;
ML2H2O is the EOS Aura Microwave Limb Sounder (MLS) standard product for water vapor derived from radiances measured primarily by the 190 GHz radiometer. The data version is 5.0. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is between 316 and 0.00215 hPa, and the vertical resolution is about 1.5 km at 316 hPa increasing to 3.5 km to 4.64 hPa, and degrades to 15 km above 0.1 hPa. Users of the ML2H2O data product should read section 3.9 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5), which is based on the version 5 Hierarchical Data Format, or HDF-5. Each file contains two swath objects (profile and column data), each with a set of data and geolocation fields, swath attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzmbro-1&quot;&gt;ML3DZMBRO&lt;/h4&gt;
ML3DZMBRO is the EOS Aura Microwave Limb Sounder (MLS) daily zonal mean product for bromine monoxide derived from radiances measured by the 640 GHz radiometer. The data version is 4.2. Data coverage is from August 2, 2004 to current. Spatial coverage is near-global (-85 degrees to 85 degrees latitude) spaced every 10 degrees in latitude. The recommended useful vertical range is between 10 and 4.64 hPa, and the vertical resolution is about 5 km. Users of the ML3DZMBRO data product should read the MLS Radiance Average Retrievals (RAR) BrO Product Guideline document, as well as section 3.2 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data are stored in the version 4 network Common Data Form (netCDF4), which is built on the version 5 Hierarchical Data Format, or HDF5. The netCDF4 files follow the Climate and Forecast (CF) metadata conventions. Each file contains two zonal means objects or groups, one with data from the ascending part of the MLS orbit, the other with the descending data. Each zonal means object contains the average, error (precision), solar zenith angle, and local solar time for each latitude band and pressure level. Files also contain metadata attributes describing the data and product.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dbco&quot;&gt;ML3DBCO&lt;/h4&gt;
ML3DBCO is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for carbon monoxide (CO) derived from radiances measured by the 640 GHz radiometer. The data version is 4.2. Data coverage is from August 2, 2004 to current. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is between 215 and 0.00464 hPa, and the vertical resolution is about 6 km. Users of the ML3DBCO data product should read chapter 4 and section 3.7 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs theta, lat vs theta zonal mean, equivalent lat vs theta zonal mean, and vortex average vs theta. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dbco-1&quot;&gt;ML3DBCO&lt;/h4&gt;
ML3DBCO is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for carbon monoxide (CO) derived from radiances measured by the 640 GHz radiometer. The data version is 5.1. Data coverage is from August 2, 2005 to current. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is between 215 and 0.00464 hPa, and the vertical resolution is about 6 km. Users of the ML3DBCO data product should read chapter 4 and section 3.7 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs theta, lat vs theta zonal mean, equivalent lat vs theta zonal mean, and vortex average vs theta. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzco&quot;&gt;ML3DZCO&lt;/h4&gt;
ML3DZCO is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for carbon monoxide (CO) derived from radiances measured by the 640 GHz radiometer. The data version is 4.2. Data coverage is from August 2, 2004 to current. Spatial coverage is near-global (-82 to +82 degrees latitude) at 4 degree latitude zonal increments. The recommended useful vertical range is between 215 and 0.00464 hPa, and the vertical resolution is about 6 km. Users of the ML3DZCO data product should read chapter 4 and section 3.7 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzco-1&quot;&gt;ML3DZCO&lt;/h4&gt;
ML3DZCO is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for carbon monoxide (CO) derived from radiances measured by the 640 GHz radiometer. The data version is 5.1. Data coverage is from August 2, 2005 to current. Spatial coverage is near-global (-82 to +82 degrees latitude) at 4 degree latitude zonal increments. The recommended useful vertical range is between 215 and 0.00464 hPa, and the vertical resolution is about 6 km. Users of the ML3DZCO data product should read chapter 4 and section 3.7 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dbclo&quot;&gt;ML3DBCLO&lt;/h4&gt;
ML3DBCLO is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for chlorine monoxide (ClO) derived from radiances measured primarily by the 640 GHz radiometer. The data version is 4.2. Data coverage is from August 2, 2004 to current. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is between 147 and 1.0 hPa, and the vertical resolution varies between 3 and 4.5 km. Users of the ML3DBCLO data product should read chapter 4 and section 3.6 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs &amp;quot;potential temperature&amp;quot;, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. These are further subdivided into groups with all valid, ascending orbit, descending orbit, daytime (SZA &amp;lt; 90), and nighttime (SZA &amp;gt; 110) profiles. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dbclo-1&quot;&gt;ML3DBCLO&lt;/h4&gt;
ML3DBCLO is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for chlorine monoxide (ClO) derived from radiances measured primarily by the 640 GHz radiometer. The data version is 5.1. Data coverage is from August 2, 2005 to current. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is between 147 and 1.0 hPa, and the vertical resolution varies between 3 and 4.5 km. Users of the ML3DBCLO data product should read chapter 4 and section 3.6 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs &amp;quot;potential temperature&amp;quot;, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. These are further subdivided into groups with all valid, ascending orbit, descending orbit, daytime (SZA &amp;lt; 90), and nighttime (SZA &amp;gt; 110) profiles. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzclo&quot;&gt;ML3DZCLO&lt;/h4&gt;
ML3DZCLO is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for chlorine monoxide (ClO) derived from radiances measured primarily by the 640 GHz radiometer. The data version is 4.2. Data coverage is from August 2, 2004 to current. Spatial coverage is near-global (-82 to +82 degrees latitude) at 4 degree latitude zonal increments. The recommended useful vertical range is between 147 and 1.0 hPa, and the vertical resolution varies between 3 and 4.5 km. Users of the ML3DZCLO data product should read chapter 4 and section 3.6 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. These are further subdivided into groups with all valid, ascending orbit, descending orbit, daytime (SZA &amp;lt; 90), and nighttime (SZA &amp;gt; 110) profiles. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzclo-1&quot;&gt;ML3DZCLO&lt;/h4&gt;
ML3DZCLO is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for chlorine monoxide (ClO) derived from radiances measured primarily by the 640 GHz radiometer. The data version is 5.1. Data coverage is from August 2, 2005 to current. Spatial coverage is near-global (-82 to +82 degrees latitude) at 4 degree latitude zonal increments. The recommended useful vertical range is between 147 and 1.0 hPa, and the vertical resolution varies between 3 and 4.5 km. Users of the ML3DZCLO data product should read chapter 4 and section 3.6 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. These are further subdivided into groups with all valid, ascending orbit, descending orbit, daytime (SZA &amp;lt; 90), and nighttime (SZA &amp;gt; 110) profiles. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dbiwc&quot;&gt;ML3DBIWC&lt;/h4&gt;
ML3DBIWC is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for cloud ice water content (IWC) derived from radiances measured by the 240 GHz radiometer. The data version is 4.2. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 215 to 82.5 hPa, and the vertical resolution is about 3 km. Users of the ML3DBIWC data product should read chapter 4 and sections 3.15 and 3.16 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs &amp;quot;potential temperature&amp;quot;, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dbiwc-1&quot;&gt;ML3DBIWC&lt;/h4&gt;
ML3DBIWC is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for cloud ice water content (IWC) derived from radiances measured by the 240 GHz radiometer. The data version is 5.1. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 215 to 82.5 hPa, and the vertical resolution is about 3 km. Users of the ML3DBIWC data product should read chapter 4 and sections 3.15 and 3.16 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs &amp;quot;potential temperature&amp;quot;, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dziwc&quot;&gt;ML3DZIWC&lt;/h4&gt;
ML3DZIWC is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for cloud ice water content (IWC) derived from radiances measured by the 240 GHz radiometer. The data version is 4.2. Spatial coverage is near-global (-82 to +82 degrees latitude) at 4 degree latitude zonal increments. The recommended useful vertical range is from 215 to 82.5 hPa, and the vertical resolution is about 3 km. Users of the ML3DZIWC data product should read chapter 4 and sections 3.15 and 3.16 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dziwc-1&quot;&gt;ML3DZIWC&lt;/h4&gt;
ML3DZIWC is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for cloud ice water content (IWC) derived from radiances measured by the 240 GHz radiometer. The data version is 5.1. Spatial coverage is near-global (-82 to +82 degrees latitude) at 4 degree latitude zonal increments. The recommended useful vertical range is from 215 to 82.5 hPa, and the vertical resolution is about 3 km. Users of the ML3DZIWC data product should read chapter 4 and sections 3.15 and 3.16 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dbgph&quot;&gt;ML3DBGPH&lt;/h4&gt;
ML3DBGPH is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for geopotential height (GPH) derived from radiances measured by the 118 and 240 GHz radiometers. The data version is 4.2. Data coverage is from August 2, 2004 to current. Spatial coverage is near-global (-82 to +82 degrees latitude), with a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is between 261 and 0.001 hPa, and the vertical resolution varies between ~3.6 and 6 km. Users of the ML3DBGPH data product should read chapter 4 and section 3.8 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains two grid objects (profile and column data), each with a set of data and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dbgph-1&quot;&gt;ML3DBGPH&lt;/h4&gt;
ML3DBGPH is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for geopotential height (GPH) derived from radiances measured by the 118 and 240 GHz radiometers. The data version is 5.1. Data coverage is from August 2, 2005 to current. Spatial coverage is near-global (-82 to +82 degrees latitude), with a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is between 261 and 0.001 hPa, and the vertical resolution varies between ~3.6 and 6 km. Users of the ML3DBGPH data product should read chapter 4 and section 3.8 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains two grid objects (profile and column data), each with a set of data and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzgph&quot;&gt;ML3DZGPH&lt;/h4&gt;
ML3DZGPH is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for geopotential height (GPH) derived from radiances measured by the 118 and 240 GHz radiometers. The data version is 4.2. Data coverage is from August 2, 2004 to current. Spatial coverage is near-global (-82 to +82 degrees latitude) at 4 degree latitude zonal increments. The recommended useful vertical range is between 261 and 0.001 hPa, and the vertical resolution varies between ~3.6 and 6 km. Users of the ML3DZGPH data product should read chapter 4 and section 3.8 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzgph-1&quot;&gt;ML3DZGPH&lt;/h4&gt;
ML3DZGPH is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for geopotential height (GPH) derived from radiances measured by the 118 and 240 GHz radiometers. The data version is 5.1. Data coverage is from August 2, 2005 to current. Spatial coverage is near-global (-82 to +82 degrees latitude) at 4 degree latitude zonal increments. The recommended useful vertical range is between 261 and 0.001 hPa, and the vertical resolution varies between ~3.6 and 6 km. Users of the ML3DZGPH data product should read chapter 4 and section 3.8 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dbhcl&quot;&gt;ML3DBHCL&lt;/h4&gt;
ML3DBHCL is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for hydrogen chloride (HCl) derived from radiances measured primarily by the 640 GHz radiometer. The data version is 4.2. Spatial coverage is near-global (-82 to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is from 100 to 0.316 hPa, and the vertical resolution is between 3 and 6 km. Users of the ML3DBHCL data product should read chapter 4 and section 3.10 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains two grid objects (profile and column data), each with a set of data and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dbhcl-1&quot;&gt;ML3DBHCL&lt;/h4&gt;
ML3DBHCL is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for hydrogen chloride (HCl) derived from radiances measured primarily by the 640 GHz radiometer. The data version is 5.1. Spatial coverage is near-global (-82 to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is from 100 to 0.316 hPa, and the vertical resolution is between 3 and 6 km. Users of the ML3DBHCL data product should read chapter 4 and section 3.10 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains two grid objects (profile and column data), each with a set of data and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzhcl&quot;&gt;ML3DZHCL&lt;/h4&gt;
ML3DZHCL is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for hydrogen chloride (HCl) derived from radiances measured primarily by the 640 GHz radiometer. The data version is 4.2. Spatial coverage is near-global (-82 to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is from 100 to 0.316 hPa, and the vertical resolution is between 3 and 6 km. Users of the ML3DZHCL data product should read chapter 4 and section 3.10 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzhcl-1&quot;&gt;ML3DZHCL&lt;/h4&gt;
ML3DZHCL is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for hydrogen chloride (HCl) derived from radiances measured primarily by the 640 GHz radiometer. The data version is 5.1. Spatial coverage is near-global (-82 to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is from 100 to 0.316 hPa, and the vertical resolution is between 3 and 6 km. Users of the ML3DZHCL data product should read chapter 4 and section 3.10 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dbhcn&quot;&gt;ML3DBHCN&lt;/h4&gt;
ML3DBHCN is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for hydrogen cyanide (HCN) derived from radiances measured primarily by the 190 GHz radiometer. The data version is 4.2. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 21.5 to 0.1 hPa, and the vertical resolution is between 8 and 12 km. Users of the ML3DBHCN data product should read chapter 4 and section 3.11 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs &amp;quot;potential temperature&amp;quot;, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dbhcn-1&quot;&gt;ML3DBHCN&lt;/h4&gt;
ML3DBHCN is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for hydrogen cyanide (HCN) derived from radiances measured primarily by the 190 GHz radiometer. The data version is 5.1. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 21.5 to 0.1 hPa, and the vertical resolution is between 8 and 12 km. Users of the ML3DBHCN data product should read chapter 4 and section 3.11 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs &amp;quot;potential temperature&amp;quot;, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzhcn&quot;&gt;ML3DZHCN&lt;/h4&gt;
ML3DZHCN is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for hydrogen cyanide (HCN) derived from radiances measured primarily by the 190 GHz radiometer. The data version is 4.2. Spatial coverage is near-global (-82 to +82 degrees latitude) at 4 degree latitude zonal increments. The recommended useful vertical range is from 21.5 to 0.1 hPa, and the vertical resolution is between 8 and 12 km. Users of the ML3DZHCN data product should read chapter 4 and section 3.11 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzhcn-1&quot;&gt;ML3DZHCN&lt;/h4&gt;
ML3DZHCN is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for hydrogen cyanide (HCN) derived from radiances measured primarily by the 190 GHz radiometer. The data version is 5.1. Spatial coverage is near-global (-82 to +82 degrees latitude) at 4 degree latitude zonal increments. The recommended useful vertical range is from 21.5 to 0.1 hPa, and the vertical resolution is between 8 and 12 km. Users of the ML3DZHCN data product should read chapter 4 and section 3.11 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dboh&quot;&gt;ML3DBOH&lt;/h4&gt;
ML3DBOH is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for hydroxyl (OH) derived from radiances measured by the THz radiometer. The data version is 4.2. Data coverage is continuous from August 2, 2004 to December 12, 2009 when the THz radiometer was placed in standby mode. After this date OH data were collected for about 30 days in August/September of 2011, 2012, 2013 and 2014. Spatial coverage is near-global (-82 to +82 degrees latitude), with a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 31.6 to 0.00316 hPa, and the vertical resolution is about 3. Users of the ML3DBOH data product should read chapter 4 and section 3.19 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains two grid objects (profile and column data), each with a set of data and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dboh-1&quot;&gt;ML3DBOH&lt;/h4&gt;
ML3DBOH is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for hydroxyl (OH) derived from radiances measured by the THz radiometer. The data version is 5.1. Data coverage is continuous from August 2, 2005 to December 12, 2009 when the THz radiometer was placed in standby mode. After this date OH data were collected for about 30 days in August/September of 2011, 2012, 2013 and 2014. Spatial coverage is near-global (-82 to +82 degrees latitude), with a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 31.6 to 0.00316 hPa, and the vertical resolution is about 3. Users of the ML3DBOH data product should read chapter 4 and section 3.19 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains two grid objects (profile and column data), each with a set of data and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzoh&quot;&gt;ML3DZOH&lt;/h4&gt;
ML3DZOH is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for hydroxyl (OH) derived from radiances measured by the THz radiometer. The data version is 4.2. Data coverage is continuous from August 2, 2004 to December 12, 2009 when the THz radiometer was placed in standby mode. After this date OH data were collected for about 30 days in August/September of 2011, 2012, 2013 and 2014. Spatial coverage is near-global (-82 to +82 degrees latitude) at 4 degree latitude zonal increments. The recommended useful vertical range is from 31.6 to 0.00316 hPa, and the vertical resolution is about 3. Users of the ML3DZOH data product should read chapter 4 and section 3.19 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. These are further subdivided into groups with all valid, ascending orbit, descending orbit, daytime (SZA &amp;lt; 90), and nighttime (SZA &amp;gt; 110) profiles. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzoh-1&quot;&gt;ML3DZOH&lt;/h4&gt;
ML3DZOH is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for hydroxyl (OH) derived from radiances measured by the THz radiometer. The data version is 5.1. Data coverage is continuous from August 2, 2005 to December 12, 2009 when the THz radiometer was placed in standby mode. After this date OH data were collected for about 30 days in August/September of 2011, 2012, 2013 and 2014. Spatial coverage is near-global (-82 to +82 degrees latitude) at 4 degree latitude zonal increments. The recommended useful vertical range is from 31.6 to 0.00316 hPa, and the vertical resolution is about 3. Users of the ML3DZOH data product should read chapter 4 and section 3.19 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. These are further subdivided into groups with all valid, ascending orbit, descending orbit, daytime (SZA &amp;lt; 90), and nighttime (SZA &amp;gt; 110) profiles. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dbhocl&quot;&gt;ML3DBHOCL&lt;/h4&gt;
ML3DBHOCL is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for hypochlorous acid (HOCl) derived from radiances measured primarily by the 640 GHz radiometer. The data version is 4.2. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 10 to 2.15 hPa, and the vertical resolution is about 6 km. Users of the ML3DBOHCL data product should read chapter 4 and section 3.14 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs &amp;quot;potential temperature&amp;quot;, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. These are further subdivided into groups with all valid, ascending orbit, descending orbit, daytime (SZA &amp;lt; 90), and nighttime (SZA &amp;gt; 110) profiles. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dbhocl-1&quot;&gt;ML3DBHOCL&lt;/h4&gt;
ML3DBHOCL is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for hypochlorous acid (HOCl) derived from radiances measured primarily by the 640 GHz radiometer. The data version is 5.1. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 10 to 2.15 hPa, and the vertical resolution is about 6 km. Users of the ML3DBOHCL data product should read chapter 4 and section 3.14 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs &amp;quot;potential temperature&amp;quot;, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. These are further subdivided into groups with all valid, ascending orbit, descending orbit, daytime (SZA &amp;lt; 90), and nighttime (SZA &amp;gt; 110) profiles. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzhocl&quot;&gt;ML3DZHOCL&lt;/h4&gt;
ML3DZHOCL is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for hypochlorous acid (HOCl) derived from radiances measured primarily by the 640 GHz radiometer. The data version is 4.2. Spatial coverage is near-global (-82 to +82 degrees latitude) at 4 degree latitude zonal increments. The recommended useful vertical range is from 10 to 2.15 hPa, and the vertical resolution is about 6 km. Users of the ML3DZOHCL data product should read chapter 4 and section 3.14 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. These are further subdivided into groups with all valid, ascending orbit, descending orbit, daytime (SZA &amp;lt; 90), and nighttime (SZA &amp;gt; 110) profiles. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzhocl-1&quot;&gt;ML3DZHOCL&lt;/h4&gt;
ML3DZHOCL is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for hypochlorous acid (HOCl) derived from radiances measured primarily by the 640 GHz radiometer. The data version is 5.1. Spatial coverage is near-global (-82 to +82 degrees latitude) at 4 degree latitude zonal increments. The recommended useful vertical range is from 10 to 2.15 hPa, and the vertical resolution is about 6 km. Users of the ML3DZOHCL data product should read chapter 4 and section 3.14 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. These are further subdivided into groups with all valid, ascending orbit, descending orbit, daytime (SZA &amp;lt; 90), and nighttime (SZA &amp;gt; 110) profiles. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dbch3cl&quot;&gt;ML3DBCH3CL&lt;/h4&gt;
ML3DBCH3CL is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for methyl chloride (CH3Cl) derived from radiances measured by the 640 GHz radiometer. The data version is 4.2. Data coverage is from August 2, 2004 to current. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is between 147 and 4.64 hPa, and the vertical resolution ranges between 4-6 km in the lower stratosphere and 8-10 km above 14 hPa. Users of the ML3DBCH3CL data product should read chapter 4 and section 3.3 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs &amp;quot;potential temperature&amp;quot;, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dbch3cl-1&quot;&gt;ML3DBCH3CL&lt;/h4&gt;
ML3DBCH3CL is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for methyl chloride (CH3Cl) derived from radiances measured by the 640 GHz radiometer. The data version is 5.1. Data coverage is from August 2, 2005 to current. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is between 147 and 4.64 hPa, and the vertical resolution ranges between 4-6 km in the lower stratosphere and 8-10 km above 14 hPa. Users of the ML3DBCH3CL data product should read chapter 4 and section 3.3 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs &amp;quot;potential temperature&amp;quot;, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzch3cl&quot;&gt;ML3DZCH3CL&lt;/h4&gt;
ML3DZCH3CL is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for methyl chloride (CH3Cl) derived from radiances measured by the 640 GHz radiometer. The data version is 4.2. Data coverage is from August 2, 2004 to current. Spatial coverage is near-global (-82 to +82 degrees latitude) at 4 degree latitude zonal increments. The recommended useful vertical range is between 147 and 4.64 hPa, and the vertical resolution ranges between 4-6 km in the lower stratosphere and 8-10 km above 14 hPa. Users of the ML3DZCH3CL data product should read chapter 4 and section 3.3 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzch3cl-1&quot;&gt;ML3DZCH3CL&lt;/h4&gt;
ML3DZCH3CL is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for methyl chloride (CH3Cl) derived from radiances measured by the 640 GHz radiometer. The data version is 5.1. Data coverage is from August 2, 2005 to current. Spatial coverage is near-global (-82 to +82 degrees latitude) at 4 degree latitude zonal increments. The recommended useful vertical range is between 147 and 4.64 hPa, and the vertical resolution ranges between 4-6 km in the lower stratosphere and 8-10 km above 14 hPa. Users of the ML3DZCH3CL data product should read chapter 4 and section 3.3 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dbhno3&quot;&gt;ML3DBHNO3&lt;/h4&gt;
ML3DBHNO3 is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for nitric acid (HNO3) derived from radiances measured by the 240 GHz radiometer at and below 10 hPa, and from the 190 GHz radiometer above 10 hPa. The data version is 4.2. Data coverage is from August 2, 2004 to current. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 215 to 1.47 hPa (1.0 hPa under enhanced conditions), and the vertical resolution is between about 3 and 5 km. Users of the ML3DBHNO3 data product should read chapter 4 and section 3.12 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs &amp;quot;potential temperature&amp;quot;, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dbhno3-1&quot;&gt;ML3DBHNO3&lt;/h4&gt;
ML3DBHNO3 is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for nitric acid (HNO3) derived from radiances measured by the 240 GHz radiometer at and below 10 hPa, and from the 190 GHz radiometer above 10 hPa. The data version is 5.1. Data coverage is from August 2, 2005 to current. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 215 to 1.47 hPa (1.0 hPa under enhanced conditions), and the vertical resolution is between about 3 and 5 km. Users of the ML3DBHNO3 data product should read chapter 4 and section 3.12 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs &amp;quot;potential temperature&amp;quot;, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzhno3&quot;&gt;ML3DZHNO3&lt;/h4&gt;
ML3DZHNO3 is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for nitric acid (HNO3) derived from radiances measured by the 240 GHz radiometer at and below 10 hPa, and from the 190 GHz radiometer above 10 hPa. The data version is 4.2. Data coverage is from August 2, 2004 to current. Spatial coverage is near-global (-82 to +82 degrees latitude) at 4 degree latitude zonal increments. The recommended useful vertical range is from 215 to 1.47 hPa (1.0 hPa under enhanced conditions), and the vertical resolution is between about 3 and 5 km. Users of the ML3DZHNO3 data product should read chapter 4 and section 3.12 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzhno3-1&quot;&gt;ML3DZHNO3&lt;/h4&gt;
ML3DZHNO3 is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for nitric acid (HNO3) derived from radiances measured by the 240 GHz radiometer at and below 10 hPa, and from the 190 GHz radiometer above 10 hPa. The data version is 5.1. Data coverage is from August 2, 2005 to current. Spatial coverage is near-global (-82 to +82 degrees latitude) at 4 degree latitude zonal increments. The recommended useful vertical range is from 215 to 1.47 hPa (1.0 hPa under enhanced conditions), and the vertical resolution is between about 3 and 5 km. Users of the ML3DZHNO3 data product should read chapter 4 and section 3.12 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dbn2o&quot;&gt;ML3DBN2O&lt;/h4&gt;
ML3DBN2O is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for nitrous oxide (N2O) derived from radiances measured primarily by the 640 GHz radiometer (Band 12) until August 6, 2013, after this date using the 190 GHz radiometer (Band 3). The data version is 4.2. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 68.1 to 0.464 hPa, and the vertical resolution is between 4 and 6 km. Users of the ML3DBN2O data product should read chapter 4 and section 3.17 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs &amp;quot;potential temperature&amp;quot;, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dbn2o-1&quot;&gt;ML3DBN2O&lt;/h4&gt;
ML3DBN2O is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for nitrous oxide (N2O) derived from radiances measured primarily by the 640 GHz radiometer (Band 12) until August 6, 2013, after this date using the 190 GHz radiometer (Band 3). The data version is 5.1. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 68.1 to 0.464 hPa, and the vertical resolution is between 4 and 6 km. Users of the ML3DBN2O data product should read chapter 4 and section 3.17 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs &amp;quot;potential temperature&amp;quot;, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzn2o&quot;&gt;ML3DZN2O&lt;/h4&gt;
ML3DZN2O is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for nitrous oxide (N2O) derived from radiances measured primarily by the 640 GHz radiometer (Band 12) until August 6, 2013, after this date using the 190 GHz radiometer (Band 3). The data version is 4.2. Spatial coverage is near-global (-82 to +82 degrees latitude) at 4 degree latitude zonal increments. The recommended useful vertical range is from 68.1 to 0.464 hPa, and the vertical resolution is between 4 and 6 km. Users of the ML3DZN2O data product should read chapter 4 and section 3.17 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzn2o-1&quot;&gt;ML3DZN2O&lt;/h4&gt;
ML3DZN2O is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for nitrous oxide (N2O) derived from radiances measured primarily by the 640 GHz radiometer (Band 12) until August 6, 2013, after this date using the 190 GHz radiometer (Band 3). The data version is 5.1. Spatial coverage is near-global (-82 to +82 degrees latitude) at 4 degree latitude zonal increments. The recommended useful vertical range is from 68.1 to 0.464 hPa, and the vertical resolution is between 4 and 6 km. Users of the ML3DZN2O data product should read chapter 4 and section 3.17 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dbo3&quot;&gt;ML3DBO3&lt;/h4&gt;
ML3DBO3 is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for ozone (O3) derived from radiances measured by the 240 GHz radiometer. The data version is 4.2. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 261 to 0.0215 hPa, and the vertical resolution is between 2.5 and 6 km. Users of the ML3DBO3 data product should read chapter 4 and section 3.18 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs &amp;quot;potential temperature&amp;quot;, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. These are further subdivided into groups with all valid, ascending orbit, descending orbit, daytime (SZA &amp;lt; 90), and nighttime (SZA &amp;gt; 110) profiles. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dbo3-1&quot;&gt;ML3DBO3&lt;/h4&gt;
ML3DBO3 is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for ozone (O3) derived from radiances measured by the 240 GHz radiometer. The data version is 5.1. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 261 to 0.0215 hPa, and the vertical resolution is between 2.5 and 6 km. Users of the ML3DBO3 data product should read chapter 4 and section 3.18 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs &amp;quot;potential temperature&amp;quot;, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. These are further subdivided into groups with all valid, ascending orbit, descending orbit, daytime (SZA &amp;lt; 90), and nighttime (SZA &amp;gt; 110) profiles. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzo3&quot;&gt;ML3DZO3&lt;/h4&gt;
ML3DZO3 is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for ozone (O3) derived from radiances measured by the 240 GHz radiometer. The data version is 4.2. Spatial coverage is near-global (-82 to +82 degrees latitude) at 4 degree latitude zonal increments. The recommended useful vertical range is from 261 to 0.0215 hPa, and the vertical resolution is between 2.5 and 6 km. Users of the ML3DZO3 data product should read chapter 4 and section 3.18 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. These are further subdivided into groups with all valid, ascending orbit, descending orbit, daytime (SZA &amp;lt; 90), and nighttime (SZA &amp;gt; 110) profiles. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzo3-1&quot;&gt;ML3DZO3&lt;/h4&gt;
ML3DZO3 is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for ozone (O3) derived from radiances measured by the 240 GHz radiometer. The data version is 5.1. Spatial coverage is near-global (-82 to +82 degrees latitude) at 4 degree latitude zonal increments. The recommended useful vertical range is from 261 to 0.0215 hPa, and the vertical resolution is between 2.5 and 6 km. Users of the ML3DZO3 data product should read chapter 4 and section 3.18 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. These are further subdivided into groups with all valid, ascending orbit, descending orbit, daytime (SZA &amp;lt; 90), and nighttime (SZA &amp;gt; 110) profiles. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dbrhi&quot;&gt;ML3DBRHI&lt;/h4&gt;
ML3DBRHI is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for relative humidity with respect to ice (RHI) derived from radiances measured by the 118 and 190 GHz radiometers. The data version is 4.2. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 316 to 0.0215 hPa, and the vertical resolution is between 3 and 6 km. Users of the ML3DBRHI data product should read chapter 4 and section 3.20 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs theta, lat vs theta zonal mean, equivalent lat vs theta zonal mean, and vortex average vs theta. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dbrhi-1&quot;&gt;ML3DBRHI&lt;/h4&gt;
ML3DBRHI is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for relative humidity with respect to ice (RHI) derived from radiances measured by the 118 and 190 GHz radiometers. The data version is 5.1. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 316 to 0.0215 hPa, and the vertical resolution is between 3 and 6 km. Users of the ML3DBRHI data product should read chapter 4 and section 3.20 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs theta, lat vs theta zonal mean, equivalent lat vs theta zonal mean, and vortex average vs theta. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzrhi&quot;&gt;ML3DZRHI&lt;/h4&gt;
ML3DZRHI is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for relative humidity with respect to ice (RHI) derived from radiances measured by the 118 and 190 GHz radiometers. The data version is 4.2. Spatial coverage is near-global (-82 to +82 degrees latitude) at 4 degree latitude zonal increments. The recommended useful vertical range is from 316 to 0.0215 hPa, and the vertical resolution is between 3 and 6 km. Users of the ML3DZRHI data product should read chapter 4 and section 3.20 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzrhi-1&quot;&gt;ML3DZRHI&lt;/h4&gt;
ML3DZRHI is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for relative humidity with respect to ice (RHI) derived from radiances measured by the 118 and 190 GHz radiometers. The data version is 5.1. Spatial coverage is near-global (-82 to +82 degrees latitude) at 4 degree latitude zonal increments. The recommended useful vertical range is from 316 to 0.0215 hPa, and the vertical resolution is between 3 and 6 km. Users of the ML3DZRHI data product should read chapter 4 and section 3.20 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dbso2&quot;&gt;ML3DBSO2&lt;/h4&gt;
ML3DBSO2 is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for sulfur dioxide (SO2) derived from radiances measured by the 240 GHz radiometer. The data version is 4.2. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 215 to 10 hPa, and the vertical resolution is about 3 km. Users of the ML3DBSO2 data product should read chapter 4 and section 3.21 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs theta, lat vs theta zonal mean, equivalent lat vs theta zonal mean, and vortex average vs theta. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dbso2-1&quot;&gt;ML3DBSO2&lt;/h4&gt;
ML3DBSO2 is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for sulfur dioxide (SO2) derived from radiances measured by the 240 GHz radiometer. The data version is 5.1. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 215 to 10 hPa, and the vertical resolution is about 3 km. Users of the ML3DBSO2 data product should read chapter 4 and section 3.21 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs theta, lat vs theta zonal mean, equivalent lat vs theta zonal mean, and vortex average vs theta. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzso2&quot;&gt;ML3DZSO2&lt;/h4&gt;
ML3DZSO2 is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for sulfur dioxide (SO2) derived from radiances measured by the 240 GHz radiometer. The data version is 4.2. Spatial coverage is near-global (-82 to +82 degrees latitude) at 4 degree latitude zonal increments. The recommended useful vertical range is from 215 to 10 hPa, and the vertical resolution is about 3 km. Users of the ML3DZSO2 data product should read chapter 4 and section 3.21 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzso2-1&quot;&gt;ML3DZSO2&lt;/h4&gt;
ML3DZSO2 is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for sulfur dioxide (SO2) derived from radiances measured by the 240 GHz radiometer. The data version is 5.1. Spatial coverage is near-global (-82 to +82 degrees latitude) at 4 degree latitude zonal increments. The recommended useful vertical range is from 215 to 10 hPa, and the vertical resolution is about 3 km. Users of the ML3DZSO2 data product should read chapter 4 and section 3.21 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dbt&quot;&gt;ML3DBT&lt;/h4&gt;
ML3DBT is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for temperature derived from radiances measured by the 118 and 240 GHz radiometers. The data version is 4.2. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 261 to 0.001 hPa, and the vertical resolution is between 3 and 6 km. Users of the ML3DBT data product should read chapter 4 and section 3.22 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs theta, lat vs theta zonal mean, equivalent lat vs theta zonal mean, and vortex average vs theta. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dbt-1&quot;&gt;ML3DBT&lt;/h4&gt;
ML3DBT is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for temperature derived from radiances measured by the 118 and 240 GHz radiometers. The data version is 5.1. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 261 to 0.001 hPa, and the vertical resolution is between 3 and 6 km. Users of the ML3DBT data product should read chapter 4 and section 3.22 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs theta, lat vs theta zonal mean, equivalent lat vs theta zonal mean, and vortex average vs theta. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzt&quot;&gt;ML3DZT&lt;/h4&gt;
ML3DZT is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for temperature derived from radiances measured by the 118 and 240 GHz radiometers. The data version is 4.2. Spatial coverage is near-global (-82 to +82 degrees latitude) at 4 degree latitude zonal increments. The recommended useful vertical range is from 261 to 0.001 hPa, and the vertical resolution is between 3 and 6 km. Users of the ML3DZT data product should read chapter 4 and section 3.22 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzt-1&quot;&gt;ML3DZT&lt;/h4&gt;
ML3DZT is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for temperature derived from radiances measured by the 118 and 240 GHz radiometers. The data version is 5.1. Spatial coverage is near-global (-82 to +82 degrees latitude) at 4 degree latitude zonal increments. The recommended useful vertical range is from 261 to 0.001 hPa, and the vertical resolution is between 3 and 6 km. Users of the ML3DZT data product should read chapter 4 and section 3.22 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dbh2o&quot;&gt;ML3DBH2O&lt;/h4&gt;
ML3DBH2O is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for water vapor (H2O) derived from radiances measured primarily by the 190 GHz radiometer. The data version is 4.2. Spatial coverage is near-global (-82 to +82 degrees latitude), with a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is between 316 and 0.00215 hPa, and the vertical resolution is about 1.5 km at 316 hPa increasing to 3.5 km to 4.64 hPa, and degrades to 15 km above 0.1 hPa. Users of the ML3DBH2O data product should read chapter 4 and section 3.9 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains two grid objects (profile and column data), each with a set of data and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dbh2o-1&quot;&gt;ML3DBH2O&lt;/h4&gt;
ML3DBH2O is the EOS Aura Microwave Limb Sounder (MLS) daily binned on various vertical grids product for water vapor (H2O) derived from radiances measured primarily by the 190 GHz radiometer. The data version is 5.1. Spatial coverage is near-global (-82 to +82 degrees latitude), with a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is between 316 and 0.00215 hPa, and the vertical resolution is about 1.5 km at 316 hPa increasing to 3.5 km to 4.64 hPa, and degrades to 15 km above 0.1 hPa. Users of the ML3DBH2O data product should read chapter 4 and section 3.9 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains two grid objects (profile and column data), each with a set of data and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzh2o&quot;&gt;ML3DZH2O&lt;/h4&gt;
ML3DZH2O is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for water vapor (H2O) derived from radiances measured primarily by the 190 GHz radiometer. The data version is 4.2. Spatial coverage is near-global (-82 to +82 degrees latitude) at 4 degree latitude zonal increments. The recommended useful vertical range is between 316 and 0.00215 hPa, and the vertical resolution is about 1.5 km at 316 hPa increasing to 3.5 km to 4.64 hPa, and degrades to 15 km above 0.1 hPa. Users of the ML3DZH2O data product should read chapter 4 and section 3.9 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzh2o-1&quot;&gt;ML3DZH2O&lt;/h4&gt;
ML3DZH2O is the EOS Aura Microwave Limb Sounder (MLS) daily binned on zonal and assorted vertical grids product for water vapor (H2O) derived from radiances measured primarily by the 190 GHz radiometer. The data version is 5.1. Spatial coverage is near-global (-82 to +82 degrees latitude) at 4 degree latitude zonal increments. The recommended useful vertical range is between 316 and 0.00215 hPa, and the vertical resolution is about 1.5 km at 316 hPa increasing to 3.5 km to 4.64 hPa, and degrades to 15 km above 0.1 hPa. Users of the ML3DZH2O data product should read chapter 4 and section 3.9 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files contain one year of data and are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains four group objects: lat vs pressure zonal mean, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3dzmho2-1&quot;&gt;ML3DZMHO2&lt;/h4&gt;
ML3DZMHO2 is the EOS Aura Microwave Limb Sounder (MLS) daily zonal mean product for hydroperoxy derived from radiances measured in two bands from the 640 GHz radiometer. The data version is 4.2. Data coverage is from August 2, 2004 to current. Spatial coverage is near-global (-85 degrees to 85 degrees latitude) spaced every 10 degrees in latitude. The recommended useful vertical range is between 21.5 to 0.0464 hPa, and the vertical resolution is about 5 km. Users of the ML3DZMHO2 data product should read the MLS Radiance Average Retrievals (RAR) Product Guideline document, as well as section 3.2 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data are stored in the version 4 network Common Data Form (netCDF4), which is built on the version 5 Hierarchical Data Format, or HDF5. The netCDF4 files follow the Climate and Forecast (CF) metadata conventions. Each file contains two zonal means objects or groups, one with data from the daytime part of the MLS orbit, the other with the nighttime data. Each zonal means object contains the average, error (precision), solar zenith angle, and local solar time for each latitude band and pressure level. Files also contain metadata attributes describing the data and product.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mbco&quot;&gt;ML3MBCO&lt;/h4&gt;
ML3MBCO is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for carbon monoxide (CO) derived from radiances measured by the 640 GHz radiometer. The data version is 4.2. Data coverage is from August 2004 to current. Spatial coverage is near-global (-82 to +82 degrees latitude), with a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is between 215 and 0.00464 hPa, and the vertical resolution is about 6 km. Users of the ML3MBCO data product should read chapter 4 and section 3.7 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains two grid objects (profile and column data), each with a set of data and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mbco-1&quot;&gt;ML3MBCO&lt;/h4&gt;
ML3MBCO is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for carbon monoxide (CO) derived from radiances measured by the 640 GHz radiometer. The data version is 5.1. Data coverage is from August 2005 to current. Spatial coverage is near-global (-82 to +82 degrees latitude), with a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is between 215 and 0.00464 hPa, and the vertical resolution is about 6 km. Users of the ML3MBCO data product should read chapter 4 and section 3.7 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains two grid objects (profile and column data), each with a set of data and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mbclo&quot;&gt;ML3MBCLO&lt;/h4&gt;
ML3MBCLO is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for chlorine monoxide (ClO) derived from radiances measured primarily by the 640 GHz radiometer. The data version is 4.2. Data coverage is from August 2004 to current. Spatial coverage is near-global (-82 to +82 degrees latitude), with a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is between 147 and 1.0 hPa, and the vertical resolution varies between 3 and 4.5 km. Users of the ML3MBCLO data product should read chapter 4 and section 3.6 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains two grid objects (profile and column data), each with a set of data and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mbclo-1&quot;&gt;ML3MBCLO&lt;/h4&gt;
ML3MBCLO is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for chlorine monoxide (ClO) derived from radiances measured primarily by the 640 GHz radiometer. The data version is 5.1. Data coverage is from August 2005 to current. Spatial coverage is near-global (-82 to +82 degrees latitude), with a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is between 147 and 1.0 hPa, and the vertical resolution varies between 3 and 4.5 km. Users of the ML3MBCLO data product should read chapter 4 and section 3.6 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains two grid objects (profile and column data), each with a set of data and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mbiwc&quot;&gt;ML3MBIWC&lt;/h4&gt;
ML3MBIWC is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for cloud ice water content (IWC) derived from radiances measured by the 240 GHz radiometer. The data version is 4.2. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 215 to 82.5 hPa, and the vertical resolution is about 3 km. Users of the ML3MBIWC data product should read chapter 4 and sections 3.15 and 3.16 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs &amp;quot;potential temperature&amp;quot;, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mbiwc-1&quot;&gt;ML3MBIWC&lt;/h4&gt;
ML3MBIWC is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for cloud ice water content (IWC) derived from radiances measured by the 240 GHz radiometer. The data version is 5.1. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 215 to 82.5 hPa, and the vertical resolution is about 3 km. Users of the ML3MBIWC data product should read chapter 4 and sections 3.15 and 3.16 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs &amp;quot;potential temperature&amp;quot;, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mbgph&quot;&gt;ML3MBGPH&lt;/h4&gt;
ML3MBGPH is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for geopotential height (GPH) derived from radiances measured by the 118 and 240 GHz radiometers. The data version is 4.2. Data coverage is from August 2004 to current. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is between 261 and 0.001 hPa, and the vertical resolution varies between ~3.6 and 6 km. Users of the ML3MBGPH data product should read chapter 4 and section 3.8 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs theta, lat vs theta zonal mean, equivalent lat vs theta zonal mean, and vortex average vs theta. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mbgph-1&quot;&gt;ML3MBGPH&lt;/h4&gt;
ML3MBGPH is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for geopotential height (GPH) derived from radiances measured by the 118 and 240 GHz radiometers. The data version is 5.1. Data coverage is from August 2005 to current. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is between 261 and 0.001 hPa, and the vertical resolution varies between ~3.6 and 6 km. Users of the ML3MBGPH data product should read chapter 4 and section 3.8 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs theta, lat vs theta zonal mean, equivalent lat vs theta zonal mean, and vortex average vs theta. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mbhcl&quot;&gt;ML3MBHCL&lt;/h4&gt;
ML3MBHCL is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for hydrogen chloride (HCl) derived from radiances measured primarily by the 640 GHz radiometer. The data version is 4.2. Spatial coverage is near-global (-82 to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is from 100 to 0.316 hPa, and the vertical resolution is between 3 and 6 km. Users of the ML3MBHCL data product should read chapter 4 and section 3.10 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains two grid objects (profile and column data), each with a set of data and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mbhcl-1&quot;&gt;ML3MBHCL&lt;/h4&gt;
ML3MBHCL is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for hydrogen chloride (HCl) derived from radiances measured primarily by the 640 GHz radiometer. The data version is 5.1. Spatial coverage is near-global (-82 to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The recommended useful vertical range is from 100 to 0.316 hPa, and the vertical resolution is between 3 and 6 km. Users of the ML3MBHCL data product should read chapter 4 and section 3.10 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains two grid objects (profile and column data), each with a set of data and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mbhcn&quot;&gt;ML3MBHCN&lt;/h4&gt;
ML3MBHCN is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for hydrogen cyanide (HCN) derived from radiances measured primarily by the 190 GHz radiometer. The data version is 4.2. Spatial coverage is near-global (-82 to +82 degrees latitude), with a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 21.5 to 0.1 hPa, and the vertical resolution is between 8 and 12 km. Users of the ML3MBHCN data product should read chapter 4 and section 3.11 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains two grid objects (profile and column data), each with a set of data and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mbhcn-1&quot;&gt;ML3MBHCN&lt;/h4&gt;
ML3MBHCN is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for hydrogen cyanide (HCN) derived from radiances measured primarily by the 190 GHz radiometer. The data version is 5.1. Spatial coverage is near-global (-82 to +82 degrees latitude), with a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 21.5 to 0.1 hPa, and the vertical resolution is between 8 and 12 km. Users of the ML3MBHCN data product should read chapter 4 and section 3.11 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains two grid objects (profile and column data), each with a set of data and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mboh&quot;&gt;ML3MBOH&lt;/h4&gt;
ML3MBOH is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for hydroxyl (OH) derived from radiances measured by the THz radiometer. The data version is 4.2. Data coverage is continuous from August 2004 to December 12, 2009 when the THz radiometer was placed in standby mode. After this date OH data were collected for about 30 days in August/September of 2011, 2012, 2013 and 2014. Spatial coverage is near-global (-82 to +82 degrees latitude), with a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 31.6 to 0.00316 hPa, and the vertical resolution is about 3. Users of the ML3MBOH data product should read chapter 4 and section 3.19 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains two grid objects (profile and column data), each with a set of data and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mboh-1&quot;&gt;ML3MBOH&lt;/h4&gt;
ML3MBOH is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for hydroxyl (OH) derived from radiances measured by the THz radiometer. The data version is 5.1. Data coverage is continuous from August 2005 to December 12, 2009 when the THz radiometer was placed in standby mode. After this date OH data were collected for about 30 days in August/September of 2011, 2012, 2013 and 2014. Spatial coverage is near-global (-82 to +82 degrees latitude), with a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 31.6 to 0.00316 hPa, and the vertical resolution is about 3. Users of the ML3MBOH data product should read chapter 4 and section 3.19 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains two grid objects (profile and column data), each with a set of data and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mbhocl&quot;&gt;ML3MBHOCL&lt;/h4&gt;
ML3MBHOCL is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for hypochlorous acid (HOCl) derived from radiances measured primarily by the 640 GHz radiometer. The data version is 4.2. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 10 to 2.15 hPa, and the vertical resolution is about 6 km. Users of the ML3MBOHCL data product should read chapter 4 and section 3.14 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs &amp;quot;potential temperature&amp;quot;, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. These are further subdivided into groups with all valid, ascending orbit, descending orbit, daytime (SZA &amp;lt; 90), and nighttime (SZA &amp;gt; 110) profiles. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mbhocl-1&quot;&gt;ML3MBHOCL&lt;/h4&gt;
ML3MBHOCL is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for hypochlorous acid (HOCl) derived from radiances measured primarily by the 640 GHz radiometer. The data version is 5.1. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 10 to 2.15 hPa, and the vertical resolution is about 6 km. Users of the ML3MBOHCL data product should read chapter 4 and section 3.14 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs &amp;quot;potential temperature&amp;quot;, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. These are further subdivided into groups with all valid, ascending orbit, descending orbit, daytime (SZA &amp;lt; 90), and nighttime (SZA &amp;gt; 110) profiles. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mbch3cl&quot;&gt;ML3MBCH3CL&lt;/h4&gt;
ML3MBCH3CL is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for methyl chloride (CH3Cl) derived from radiances measured by the 640 GHz radiometer. The data version is 4.2. Data coverage is from August 2004 to current. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is between 147 and 4.64 hPa, and the vertical resolution ranges between 4-6 km in the lower stratosphere and 8-10 km above 14 hPa. Users of the ML3MBCH3CL data product should read chapter 4 and section 3.3 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs &amp;quot;potential temperature&amp;quot;, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mbch3cl-1&quot;&gt;ML3MBCH3CL&lt;/h4&gt;
ML3MBCH3CL is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for methyl chloride (CH3Cl) derived from radiances measured by the 640 GHz radiometer. The data version is 5.1. Data coverage is from August 2005 to current. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is between 147 and 4.64 hPa, and the vertical resolution ranges between 4-6 km in the lower stratosphere and 8-10 km above 14 hPa. Users of the ML3MBCH3CL data product should read chapter 4 and section 3.3 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs &amp;quot;potential temperature&amp;quot;, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mbhno3&quot;&gt;ML3MBHNO3&lt;/h4&gt;
ML3MBHNO3 is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for nitric acid (HNO3) derived from radiances measured by the 240 GHz radiometer at and below 10 hPa, and from the 190 GHz radiometer above 10 hPa. The data version is 4.2. Data coverage is from August 2004 to current. Spatial coverage is near-global (-82 to +82 degrees latitude), with a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 215 to 1.47 hPa (1.0 hPa under enhanced conditions), and the vertical resolution is between about 3 and 5 km. Users of the ML3MBHNO3 data product should read chapter 4 and section 3.12 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains two grid objects (profile and column data), each with a set of data and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mbhno3-1&quot;&gt;ML3MBHNO3&lt;/h4&gt;
ML3MBHNO3 is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for nitric acid (HNO3) derived from radiances measured by the 240 GHz radiometer at and below 10 hPa, and from the 190 GHz radiometer above 10 hPa. The data version is 5.1. Data coverage is from August 2005 to current. Spatial coverage is near-global (-82 to +82 degrees latitude), with a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 215 to 1.47 hPa (1.0 hPa under enhanced conditions), and the vertical resolution is between about 3 and 5 km. Users of the ML3MBHNO3 data product should read chapter 4 and section 3.12 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains two grid objects (profile and column data), each with a set of data and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mbn2o&quot;&gt;ML3MBN2O&lt;/h4&gt;
ML3MBN2O is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for nitrous oxide (N2O) derived from radiances measured primarily by the 640 GHz radiometer (Band 12) until August 6, 2013, after this date using the 190 GHz radiometer (Band 3). The data version is 4.2. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 68.1 to 0.464 hPa, and the vertical resolution is between 4 and 6 km. Users of the ML3MBN2O data product should read chapter 4 and section 3.17 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs &amp;quot;potential temperature&amp;quot;, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mbn2o-1&quot;&gt;ML3MBN2O&lt;/h4&gt;
ML3MBN2O is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for nitrous oxide (N2O) derived from radiances measured primarily by the 640 GHz radiometer (Band 12) until August 6, 2013, after this date using the 190 GHz radiometer (Band 3). The data version is 5.1. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 68.1 to 0.464 hPa, and the vertical resolution is between 4 and 6 km. Users of the ML3MBN2O data product should read chapter 4 and section 3.17 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs &amp;quot;potential temperature&amp;quot;, lat vs &amp;quot;potential temperature&amp;quot; zonal mean, &amp;quot;equivalent latitude&amp;quot; vs &amp;quot;potential temperature&amp;quot; zonal mean, and vortex average vs &amp;quot;potential temperature&amp;quot;. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mbo3&quot;&gt;ML3MBO3&lt;/h4&gt;
ML3MBO3 is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for ozone (O3) derived from radiances measured by the 240 GHz radiometer. The data version is 4.2. Spatial coverage is near-global (-82 to +82 degrees latitude), with a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 261 to 0.0215 hPa, and the vertical resolution is between 2.5 and 6 km. Users of the ML3MBO3 data product should read chapter 4 and section 3.18 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains two grid objects (profile and column data), each with a set of data and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mbo3-1&quot;&gt;ML3MBO3&lt;/h4&gt;
ML3MBO3 is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for ozone (O3) derived from radiances measured by the 240 GHz radiometer. The data version is 5.1. Spatial coverage is near-global (-82 to +82 degrees latitude), with a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 261 to 0.0215 hPa, and the vertical resolution is between 2.5 and 6 km. Users of the ML3MBO3 data product should read chapter 4 and section 3.18 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains two grid objects (profile and column data), each with a set of data and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mbrhi&quot;&gt;ML3MBRHI&lt;/h4&gt;
ML3MBRHI is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for relative humidity with respect to ice (RHI) derived from radiances measured by the 118 and 190 GHz radiometers. The data version is 4.2. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 316 to 0.0215 hPa, and the vertical resolution is between 3 and 6 km. Users of the ML3MBRHI data product should read chapter 4 and section 3.20 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs theta, lat vs theta zonal mean, equivalent lat vs theta zonal mean, and vortex average vs theta. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mbrhi-1&quot;&gt;ML3MBRHI&lt;/h4&gt;
ML3MBRHI is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for relative humidity with respect to ice (RHI) derived from radiances measured by the 118 and 190 GHz radiometers. The data version is 5.1. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 316 to 0.0215 hPa, and the vertical resolution is between 3 and 6 km. Users of the ML3MBRHI data product should read chapter 4 and section 3.20 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs theta, lat vs theta zonal mean, equivalent lat vs theta zonal mean, and vortex average vs theta. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mbso2&quot;&gt;ML3MBSO2&lt;/h4&gt;
ML3MBSO2 is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for sulfur dioxide (SO2) derived from radiances measured by the 240 GHz radiometer. The data version is 4.2. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 215 to 10 hPa, and the vertical resolution is about 3 km. Users of the ML3MBSO2 data product should read chapter 4 and section 3.21 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs theta, lat vs theta zonal mean, equivalent lat vs theta zonal mean, and vortex average vs theta. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mbso2-1&quot;&gt;ML3MBSO2&lt;/h4&gt;
ML3MBSO2 is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for sulfur dioxide (SO2) derived from radiances measured by the 240 GHz radiometer. The data version is 5.1. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 215 to 10 hPa, and the vertical resolution is about 3 km. Users of the ML3MBSO2 data product should read chapter 4 and section 3.21 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs theta, lat vs theta zonal mean, equivalent lat vs theta zonal mean, and vortex average vs theta. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mbt&quot;&gt;ML3MBT&lt;/h4&gt;
ML3MBT is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for temperature derived from radiances measured by the 118 and 240 GHz radiometers. The data version is 4.2. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 261 to 0.001 hPa, and the vertical resolution is between 3 and 6 km. Users of the ML3MBT data product should read chapter 4 and section 3.22 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs theta, lat vs theta zonal mean, equivalent lat vs theta zonal mean, and vortex average vs theta. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mbt-1&quot;&gt;ML3MBT&lt;/h4&gt;
ML3MBT is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for temperature derived from radiances measured by the 118 and 240 GHz radiometers. The data version is 5.1. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is from 261 to 0.001 hPa, and the vertical resolution is between 3 and 6 km. Users of the ML3MBT data product should read chapter 4 and section 3.22 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs theta, lat vs theta zonal mean, equivalent lat vs theta zonal mean, and vortex average vs theta. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mbh2o&quot;&gt;ML3MBH2O&lt;/h4&gt;
ML3MBH2O is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for water vapor (H2O) derived from radiances measured primarily by the 190 GHz radiometer. The data version is 4.2. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is between 316 and 0.00215 hPa, and the vertical resolution is about 1.5 km at 316 hPa increasing to 3.5 km to 4.64 hPa, and degrades to 15 km above 0.1 hPa. Users of the ML3MBH2O data product should read chapter 4 and section 3.9 of the EOS MLS Level 2 Version 4 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs theta, lat vs theta zonal mean, equivalent lat vs theta zonal mean, and vortex average vs theta. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml3mbh2o-1&quot;&gt;ML3MBH2O&lt;/h4&gt;
ML3MBH2O is the EOS Aura Microwave Limb Sounder (MLS) monthly binned on various vertical grids product for water vapor (H2O) derived from radiances measured primarily by the 190 GHz radiometer. The data version is 5.1. Spatial coverage is near-global (-82 to +82 degrees latitude) at a spatial resolution of 4 degrees latitude by 5 degrees longitude. The recommended useful vertical range is between 316 and 0.00215 hPa, and the vertical resolution is about 1.5 km at 316 hPa increasing to 3.5 km to 4.64 hPa, and degrades to 15 km above 0.1 hPa. Users of the ML3MBH2O data product should read chapter 4 and section 3.9 of the EOS MLS Level 2 Version 5 Quality Document for more information. The data files are archived in the netCDF4 format, which is also compatible with HDF5 readers and tools. Each file contains six group objects: lat-lon map vs pressure, lat vs pressure zonal mean, lat-lon map vs theta, lat vs theta zonal mean, equivalent lat vs theta zonal mean, and vortex average vs theta. Each group has a set of data (average, min, max, std dev, rms) and geolocation fields, grid attributes, and metadata.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2co_nrt&quot;&gt;ML2CO_NRT&lt;/h4&gt;
ML2CO_NRT is the EOS Aura Microwave Limb Sounder (MLS) Near-Real-Time (NRT) product for carbon monoxide (CO). This product contains CO profiles derived from the 240 GHz region. The NRT data are typically available within 3 hours of observation and are broken into files containing about 15 minutes of data. The most recent 7 days of data are available online. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The vertical coverage is from 215 to 0.1 hPa. The MLS NRT algorithm uses a simplified fast forward model to meet Near Real Time data latency requirements and are therefore not as accurate as the retrievals that constitute the standard MLS products. Nevertheless the results are scientifically useful in selected regions of the Earth&amp;#39;s atmosphere provided that the data are screened according to the recommendations in the MLS NRT User Guide and the MLS L2 Data Quality Document for Standard Products.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2hno3_nrt&quot;&gt;ML2HNO3_NRT&lt;/h4&gt;
ML2HNO3_NRT is the EOS Aura Microwave Limb Sounder (MLS) Near-Real-Time (NRT) product for nitric acid (HNO3). This product contains HNO3 profiles derived from the 190 and 240 GHz regions. The NRT data are typically available within 3 hours of observation and are broken into files containing about 15 minutes of data. The most recent 7 days of data are available online. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The vertical coverage is from 100 to 1.47 hPa. The MLS NRT algorithm uses a simplified fast forward model to meet Near Real Time data latency requirements and are therefore not as accurate as the retrievals that constitute the standard MLS products. Nevertheless the results are scientifically useful in selected regions of the Earth&amp;#39;s atmosphere provided that the data are screened according to the recommendations in the MLS NRT User Guide and the MLS L2 Data Quality Document for Standard Products.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2n2o_nrt&quot;&gt;ML2N2O_NRT&lt;/h4&gt;
ML2N2O_NRT is the EOS Aura Microwave Limb Sounder (MLS) Near-Real-Time (NRT) product for nitrous oxide (N2O). This product contains N2O profiles derived from the 190 GHz region. The NRT data are typically available within 3 hours of observation and are broken into files containing about 15 minutes of data. The most recent 7 days of data are available online. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The vertical coverage is from 100 to 1 hPa. The MLS NRT algorithm uses a simplified fast forward model to meet Near Real Time data latency requirements and are therefore not as accurate as the retrievals that constitute the standard MLS products. Nevertheless the results are scientifically useful in selected regions of the Earth&amp;#39;s atmosphere provided that the data are screened according to the recommendations in the MLS NRT User Guide and the MLS L2 Data Quality Document for Standard Products.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2o3_nrt&quot;&gt;ML2O3_NRT&lt;/h4&gt;
ML2O3_NRT is the EOS Aura Microwave Limb Sounder (MLS) Near-Real-Time (NRT) product for ozone (O3). This product contains O3 profiles derived from the 240 GHz region. The NRT data are typically available within 3 hours of observation and are broken into files containing about 15 minutes of data. The most recent 7 days of data are available online. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The vertical coverage is from 261 to 0.1 hPa. The MLS NRT algorithm uses a simplified fast forward model to meet Near Real Time data latency requirements and are therefore not as accurate as the retrievals that constitute the standard MLS products. Nevertheless the results are scientifically useful in selected regions of the Earth&amp;#39;s atmosphere provided that the data are screened according to the recommendations in the MLS NRT User Guide and the MLS L2 Data Quality Document for Standard Products.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2so2_nrt&quot;&gt;ML2SO2_NRT&lt;/h4&gt;
ML2SO2_NRT is the EOS Aura Microwave Limb Sounder (MLS) Near-Real-Time (NRT) product for sulfur dioxide (SO2). This product contains SO2 profiles derived from the 190 and 240 GHz regions. The NRT data are typically available within 3 hours of observation and are broken into files containing about 15 minutes of data. The most recent 7 days of data are available online. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The vertical coverage is from 215 to 10 hPa. The MLS NRT algorithm uses a simplified fast forward model to meet Near Real Time data latency requirements and are therefore not as accurate as the retrievals that constitute the standard MLS products. Nevertheless the results are scientifically useful in selected regions of the Earth&amp;#39;s atmosphere provided that the data are screened according to the recommendations in the MLS NRT User Guide and the MLS L2 Data Quality Document for Standard Products.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2t_nrt&quot;&gt;ML2T_NRT&lt;/h4&gt;
ML2T_NRT is the EOS Aura Microwave Limb Sounder (MLS) Near-Real-Time (NRT) product for temperature. This product contains temperature profiles derived from the 118 GHz region. The NRT data are typically available within 3 hours of observation and are broken into files containing about 15 minutes of data. The most recent 7 days of data are available online. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The vertical coverage is from 215 to 0.001 hPa. The MLS NRT algorithm uses a simplified fast forward model to meet Near Real Time data latency requirements and are therefore not as accurate as the retrievals that constitute the standard MLS products. Nevertheless the results are scientifically useful in selected regions of the Earth&amp;#39;s atmosphere provided that the data are screened according to the recommendations in the MLS NRT User Guide and the MLS L2 Data Quality Document for Standard Products.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ml2h2o_nrt&quot;&gt;ML2H2O_NRT&lt;/h4&gt;
ML2H2O_NRT is the EOS Aura Microwave Limb Sounder (MLS) Near-Real-Time (NRT) product for water vapor (H2O). This product contains H2O profiles derived from the 190 GHz region. The NRT data are typically available within 3 hours of observation and are broken into files containing about 15 minutes of data. The most recent 7 days of data are available online. Spatial coverage is near-global (-82 degrees to +82 degrees latitude), with each profile spaced 1.5 degrees or ~165 km along the orbit track (roughly 15 orbits per day). The vertical coverage is from 147 to 1 hPa. The MLS NRT algorithm uses a simplified fast forward model to meet Near Real Time data latency requirements and are therefore not as accurate as the retrievals that constitute the standard MLS products. Nevertheless the results are scientifically useful in selected regions of the Earth&amp;#39;s atmosphere provided that the data are screened according to the recommendations in the MLS NRT User Guide and the MLS L2 Data Quality Document for Standard Products.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omaeroz&quot;&gt;OMAEROZ&lt;/h4&gt;
The reprocessed OMI/Aura Level-2 Zoomed Aerosol data product OMAEROZ at 13x12 km resolution have been made available from the NASA Goddard Earth Sciences Data and Information Services Center (GES DISC) for public access in March 2012. There are two Level-2 Aura OMI aerosol products OMAERO and OMAERUV. The OMAERUV product uses the near-UV algorithm. The OMAERO (13x24 km resolution) and OMAEROZ (13x12 km resolution) is based on the multi-wavelength algorithm that uses up to 20 wavelength bands between 331 nm and 500 nm. The multi-wavelength retrieval algorithm is developed by the KNMI OMI Team Scientists. Drs. Deborah Stein-Zweers, Martin Sneep and Pepijn Veefkind are now the key investigators of this product. The OMAEROZ products contain Aerosol Optical Depths, Single Scattering Albedo, Aerosol Type, Aerosol Layer Height, and other intermediate and ancillary parameters and geolocation information. The OMAEROZ files are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5). Each file contains data from the day lit portion of an orbit (~53 minutes). OMAEROZ data files are based on Zoomed Level 1B radiance observations which are made once a month. Thus there is one day of zoomed data (approximately 14 orbits) per month. The maximum file size for the OMAEROZ data is about 11 Mbytes. A Readme document containing brief algorithm description and known data quality related issues and file specifications are provided by the OMAERO Algorithm lead.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ommydageo&quot;&gt;OMMYDAGEO&lt;/h4&gt;
The OMI/Aura and MODIS/Aqua Aerosol Geo-colocation Product 1-Orbit L2 Swath 13x24 km (OMMYDAGEO) is a Level-2 orbital data product that links the MODIS/Aqua aerosol geo-coordinates at 3 and 10 km with the OMI indices along the OMI orbital track. This product allows users to match up MODIS granules with the OMI orbit for analysis and validation. It co-locates MODIS and OMI cloud and radiance information onto the OMI pixel. The OMMYDAGEO data files are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5) using the swath model, and follows the same conventions used by the other OMI Level-2 data products. Each file contains data for 5 minutes, corresponding to the MODIS granule from the daylit side of the orbit. There are on the order of about 140 swath files per day. The file size for the OMMYDAGEO data product is about 12 Megabytes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ommydcld&quot;&gt;OMMYDCLD&lt;/h4&gt;
The OMI/Aura and MODIS/Aqua Merged Cloud Product 1-Orbit L2 Swath 13x24 km (OMMYDCLD) is a Level-2 orbital product that combines cloud parameters retrieved by the Ozone Mapping Instrument (OMI) on the Aura satellite with collocated statistical information for cloud parameters retrieved by the Moderate Resolution Imaging Spectrometer (MODIS) on the Aqua spacecraft. This product is designed to take advantage of the synergy between OMI and MODIS, which both fly on satellites in the NASA A-Train constellation of Earth-observing satellites that follow similar orbital tracks and collect near-simultaneous observations. This product can be used for cloud-clearing, detection of multi-layered clouds, and other applications that may exploit these multi-spectral measurements. The algorithm for the OMMYDCLD product co-locates daytime cloud parameters from MODIS onto the OMI visible (VIS) pixel for a given OMI orbit and generates statistical information from the collocated MODIS pixels. For each OMI granule, the orbit start and end times are used to select the corresponding 5-minute MODIS granules for processing. A contiguous list of MODIS granules spanning the full duration of the OMI orbit are selected based on the relative time lag between Aqua and Aura. The algorithm lead for this product is NASA OMI scientist Dr. Joanna Joiner. The OMMYDCLD data files are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5) using the swath model, and follows the same conventions used by the other OMI Level-2 data products. Each file contains data from the day lit portion of an orbit (about 53 minutes). There are approximately 14 orbits per day. The file size for the OMMYDCLD data product is about 8 Mbytes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ombro&quot;&gt;OMBRO&lt;/h4&gt;
The Aura Ozone Monitoring Instrument (OMI) collection-3 Bromine Monoxide Product OMBRO from the Aura-OMI, is now available from the NASA Goddard Earth Sciences Data and Information Services Center (GES DISC) for the public access. The shortname for this Level-2 OMI total column BrO product is OMBRO. The algorithm leads for this product are the US OMI scientists Dr. Kelly Chance and Dr. Thomas Kurosu from the Harvard-Smithsonian Center, Cambridge, MA. The OMBRO product contains total vertical column BrO, standard errors (rms and sigma), quality flags, geolocation and other ancillary information. The OMBRO files are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5). Each file contains data from the day lit portion of an orbit (~53 minutes). There are approximately 14 orbits per day. The average file size for the OMBRO data product is about 5 Mbytes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omoclo&quot;&gt;OMOCLO&lt;/h4&gt;
The Aura Ozone Monitoring Instrument (OMI) collection-3 Chlorine Dioxide Product OMOCLO is now available from the NASA Goddard Earth Sciences Data and Information Services Center (GES DISC) for public access. The shortname for this Level-2 OMI total column OClO product is OMOCLO. The algorithm leads for this product are the US OMI scientists Dr. Kelly Chance and Dr. Thomas Kurosu from the Harvard-Smithsonian Center, Cambridge, MA. The OMOCLO product contains slant column OClO, standard errors (rms and sigma), quality flags, geolocation and other ancillary information. The OMOCLO files are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5). Each file contains data from the day lit portion of an orbit (~53 minutes). There are approximately 14 orbits per day. The maximum file size for the OMOCLO data product is about 20 MB.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omcldo2&quot;&gt;OMCLDO2&lt;/h4&gt;
The reprocessed OMI/Aura Level-2 cloud data product OMCLDO2 is now available from the NASA GoddardEarth Sciences Data and Information Services Center (GES DISC) for the public access. It is the second release of Version 003 and was reprocessed in late 2011. OMI provides two cloud products based on two different algorithms, the Rotational Raman Scattering method, and O2-O2 absorption method using the DOAS technique. This level-2 global cloud product, with a pixel resolution of 13x24 km2at nadir, is based on the spectral fitting of O2-O2 absorption band at 477 nm using DOAS technique. This product contains cloud pressure, cloud fraction, slant column O2-O2, ozone, ring coefficients, uncertainties in derived parameters, terrain and geolocation information, solar and satellite viewing angles, and quality flags. The lead scientist for this product is Dr. Pepijn Veefkind. The OMCLDO2 product files are stored in the version 5 Hierarchical Data Format (HDF-EOS5). Each file contains data from the day lit portion of an orbit (~53 minutes) and is roughly 15.096 MB in size. There are approximately 14 orbits per day thus the total data volume is approximately 200 GB/day.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omcldo2g&quot;&gt;OMCLDO2G&lt;/h4&gt;
This Level-2G daily global gridded product OMCLDO2G is based on the pixel level OMI Level-2 CLDO2 product OMCLDO2. This level-2G global cloud product (OMCLDO2G) is based on the spectral fitting of O2-O2 absorption band at 477 nm using DOAS technique. This product contains cloud pressure, cloud fraction, slant column O2-O2 and Ozone, Ring coefficients, uncertainties in derived parameters, terrain and geolocation information, solar and satellite viewing angles, and quality flags. The short name for this Level-2 OMI cloud product is OMCLDO2G and the lead scientist for this product and for OMCLDO2 (the data source of OMCLDO2G) is KNMI scientist Dr. Pepijn Veefkind. OMCLDO2G data product is a special Level-2 Global Gridded Product where pixel level data (OMCLDO2) are binned into 0.25x0.25 degree global grids. It contains the OMCLDO2 data for all L2 scenes that have observation time between UTC times of 00:00:00 and 23:59:59.9999. All data pixels that fall in a grid are saved &amp;#39;Without Averaging&amp;#39;. Scientists can apply a data filtering scheme of their choice and create new gridded products. The OMCLDO2G product files are stored in the version 5 Hierarchical Data Format (HDF-EOS5). Each daily data file contains data from the day lit portion of the orbits (~14 orbits) and is roughly 85 MB in size.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omcldo2z&quot;&gt;OMCLDO2Z&lt;/h4&gt;
The reprocessed Aura Ozone Monitoring Instrument (OMI) Level-2 zoomed cloud data product OMCLDO2Z at 13x12 km resolution is now available from the NASA Goddard Earth Sciences Data and Information Services Center (GES DISC) for the public access. It is the second release of Version 003 and was reprocessed late 2011. OMI provides two cloud products based on two different algorithms, the Rotational Raman Scattering method and O2-O2 absorption method using the DOAS technique. This level-2 zoomed cloud product at the pixel resolution (13x12 km2 at nadir) is based on the spectral fitting of O2-O2 absorption band at 477 nm using DOAS technique. This product contains effective cloud pressure, effective cloud fraction, slant column O2-O2; uncertainties in derived, parameters, terrain and geolocation information, solar and satellite viewing angles, and quality flags. The shortname for this Level-2 OMI Zoomed cloud product is OMCLDO2Z. The lead scientist for this product is Dr. Pepijn Veefkind. The OMCLDO2Z files are stored in the version 5 Hierarchical Data Format (HDF-EOS5). Each file contains data from the day lit portion of an orbit (~53 minutes) and is roughly 20 MB in size. OMCLDO2Z data files are based on Zoomed Level 1B radiance observations which are made once a month. Thus there is one zoomed cloud product per month.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omdoao3&quot;&gt;OMDOAO3&lt;/h4&gt;
The second release of Aura Ozone Monitoring Instrument (OMI) Version 003 OMI/Aura Level-2 Total Column Ozone Data Product OMDOAO3 is now available from the NASA Goddard Earth Sciences Data and Information Services Center (GES DISC) for the public access. The data were processed in late 2011 using Algorithm or PGE version 1.2.3 and released in March 2012. OMI provides two total column ozone products based on two different algorithms. This level-2 global total column ozone product at the pixel resolution (13x24 km at nadir), is based on the Differential Absorption Spectroscopy (DOAS) fitting technique that essentially uses the OMI UV radiance values between 331.1 and 336.1 nm. In addition to the total ozone column this product also contains auxiliary , derived and ancillary input parameters e.g. ozone slant column density, ozone ghost column density, air mass factor, scene reflectivity, radiance over the DOAS fit window, root mean square of DAOS fit, cloud fraction, cloud radiance, cloud pressure, terrain height, geolocation, viewing angles and quality flags. The shortname for this Level-2 OMI total column ozone product is OMDOAO3. The lead scientist for this product is Dr. J. Pepijn Veefkind. The OMDOAO3 product files are stored in the version 5 Hierarchical Data Format (HDF-EOS5). Each file contains data from the day lit portion of an orbit (approximately 53 minutes) and is approximately 11 MB in size. There are approximately 14 orbits per day.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omdoao3z&quot;&gt;OMDOAO3Z&lt;/h4&gt;
The reprocessed Aura Ozone Monitoring Instrument (OMI) Level-2 Zoomed Ozone data product OMDOAO3Z at 13x12 km resolution is now available from the NASA Goddard Earth Sciences Data and Information Services Center (GES DISC) for the public access. It is the second release of Version 003 and was reprocessed late 2011. OMI provides two sets of total column ozone products OMTO3 and OMDOAO3 which are based on two different algorithms. OMTO3 product is based on TOMS like ozone retrieval algorithm whereas OMDOAO3 total column ozone product is based on the Differential Absorption Spectroscopy (DOAS) fitting technique that essentially uses the OMI visible radiance values between 331.1 and 336.1 nm. The DOAS retrieval algorithm is developed by the KNMI OMI Scientist, Dr Pepijn Veefkind. Based on spatial resolutions, there are two DOAS algorithm based ozone products, OMDOAO3 (at 13x24 km resolution) and OMDOAO3Z (13x12 km resolution). In addition to the total ozone column values these DOAS based ozone products also contain some auxiliary derived and ancillary input parameters e.g. ozone slant column density, ozone ghost column density, air mass factor, scene reflectivity, radiance over the DOAS fit window, root mean square of DAOS fit, cloud fraction, cloud radiance, cloud pressure, terrain height, geolocation, viewing angles and quality flags. The shortname for this Level-2 OMI Zoomed Ozone product is OMDOAO3Z. The OMDOAO3Z files are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5). Each file contains data from the day lit portion of an orbit (~53 minutes). OMDOAO3Z data files are based on Zoomed Level 1B radiance observations which are made once a month. Thus there is one day of zoomed data (approximately 14 orbits) per month. The maximum file size for the OMDOAO3Z data is approximately 30 MB.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omcldrr&quot;&gt;OMCLDRR&lt;/h4&gt;
The reprocessed Aura Ozone Monitoring Instrument (OMI) Version 003 Level 2 Cloud Data Product OMCLDRR is available to the public from the NASA Goddard Earth Sciences Data and Information Services Center (GES DISC). Aura OMI provides two Level-2 Cloud products (OMCLDRR and OMCLDO2) at pixel resolution (13 x 24 km at nadir) that are based on two different algorithms, the Rotational Raman Scattering method and the O2-O2 absorption method. This level-2 global cloud product, OMCLDRR, provides effective cloud pressure and effective cloud fraction that is based on the least square fitting of the Ring spectrum (filling-in of Fraunhofer lines in the range 392 to 398 nm due to rotational Raman scattering). This product also contains many ancillary and derived parameters, terrain and geolocation information, solar and satellite viewing angles, and quality flags. The shortname for this Level-2 OMI Cloud Pressure and Fraction product is OMCLDRR and the algorithm lead for this product is NASA OMI scientist Dr. Joanna Joinner. The OMCLDRR files are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5). Each file contains data from the day lit portion of an orbit (53 minutes). There are approximately 14 orbits per day. The maximum file size for the OMCLDRR data product is about 9 Mbytes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omcldrr-1&quot;&gt;OMCLDRR&lt;/h4&gt;
This is the Aura Ozone Monitoring Instrument (OMI) Version 004 Level 2 Cloud Data Product OMCLDRR. OMI provides two Level-2 Cloud products (OMCLDRR and OMCLDO2) at pixel resolution (13 x 24 km at nadir) that are based on two different algorithms, the Rotational Raman Scattering method and the O2-O2 absorption method. This level-2 global cloud product, OMCLDRR, provides effective cloud pressure and effective cloud fraction that is based on the least square fitting of the Ring spectrum (filling-in of Fraunhofer lines in the range 392 to 398 nm due to rotational Raman scattering). This product also contains many ancillary and derived parameters, terrain and geolocation information, solar and satellite viewing angles, and quality flags. The shortname for this Level-2 OMI Cloud Pressure and Fraction product is OMCLDRR and the algorithm lead for this product is NASA OMI scientist Dr. Joanna Joinner. The OMCLDRR files are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5). Each file contains data from the day lit portion of an orbit (53 minutes). There are approximately 14 orbits per day. The maximum file size for the OMCLDRR data product is about 9 Mbytes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omcldrrg&quot;&gt;OMCLDRRG&lt;/h4&gt;
This Level-2G daily global gridded product OMCLDRRG is based on the pixel level OMI Level-2 CLDRR product OMCLDRR. This level-2G global cloud product (OMCLDRRG) provides effective cloud pressure and effective cloud fraction that is based on the least square fitting of the Ring spectrum (filling-in of Fraunhofer lines in the range 392 to 398 nm due to rotational Raman scattering). This product also contains many ancillary and derived parameters, terrain and geolocation information, solar and satellite viewing angles, and quality flags. The algorithm lead for the products OMCLDRR and OMCLDRRG is NASA OMI scientist Dr. Joanna Joinner. OMCLDRRG data product is a special Level-2G Gridded Global Product where pixel level data (OMCLDRR)are binned into 0.25x0.25 degree global grids. It contains the OMCLDRR data for all L2 scenes that have observation time between UTC times of 00:00:00 and 23:59:59.9999. All data pixels that fall in a grid box are saved without Averaging. Scientists can apply a data filtering scheme of their choice and create new gridded products. The OMCLDRRG data products are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5). Each daily file contains data from the day lit portion of the orbits (~14 orbits). The average file size for the OMCLDRRG data product is about 75 Mbytes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omhcho&quot;&gt;OMHCHO&lt;/h4&gt;
The Aura Ozone Monitoring Instrument (OMI) Version-3 Formaldehyde Product OMHCHO is now available from the NASA Goddard Earth Sciences Data and Information Services Center (GES DISC) for the public access. The shortname for this Level-2 OMI total column Formaldehyde product is OMHCHO. The algorithm leads for this product are the US OMI scientists Dr. Kelly Chance and Dr. Thomas Kurosu from the Harvard-Smithsonian Center, Cambridge, MA. The OMHCHO product contains total vertical column HCHO, standard errors (rms and sigma), quality flags, geolocation and other ancillary information. The OMHCHO files are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5). Each file contains data from the day lit portion of an orbit (~53 minutes). There are approximately 14 orbits per day. The average file size for the OMHCHO data product is about 5 MB.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omhchog&quot;&gt;OMHCHOG&lt;/h4&gt;
This Level-2G daily global gridded product OMHCHOG is based on the pixel level OMI Level-2 HCHO product OMHCHO. OMHCHOG data product is a special Level-2 Global Gridded Product where pixel level data are binned into 0.25x0.25 degree grids. It contains data for all L2 scenes that have observation time between UTC times of 00:00:00 and 23:59:59.9999. All data pixels that fall in a grid box are saved without Averaging (third dimension provides indexing for the data points in each small grid). Scientists can apply a data filtering scheme of their choice and create Level-3 global gridded products. The OMHCHOG data product contains almost all parameters (e.g. total vertical column HCHO, standard errors, quality flags, geolocation and ancillary information) that are contained in the OMHCHO product. The OMHCHOG data are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5). Each file contains data from the day lit portions of 14 to 15 orbits that cover the globe in a day. The average file size for the OMGCHOG data product is about 55 Mbytes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omhchod&quot;&gt;OMHCHOd&lt;/h4&gt;
The OMI/Aura Formaldehyde (HCHO) Total Column Daily L3 Weighted Mean Global 0.1deg Lat/Lon Grid (OMHCHOd). The formaldehyde values in each file are the average for 0.1 x 0.1 degree grid cell of cloud-screened total HCHO columns for a single day. Other variables included in the files are the weight of each grid cell, the standard error of column averages, mean albedo, mean cloud fraction, mean cloud pressure, and surface height. The weight information is useful for combining data from several files and reducing the noise of the retrievals by co-adding in the temporal or spatial dimensions. The OMHCHOd files are in the netCDF4 format which is compatible with most HDF5 readers and tools. Each file contains daily data from approximately 15 orbits. The maximum file size for the OMHCHOd data product is about 80 Mbytes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omgler&quot;&gt;OMGLER&lt;/h4&gt;
The OMI/Aura Global Geometry-Dependent Surface LER 1-Orbit L2 Swath 13x24km product, or OMGLER, provides GLER, and the computed top-of-atmosphere (TOA) radiance from which GLER is derived, for the OMI field of view. The OMGLER data also contain a number of ancillary/input parameters for each OMI pixel used to compute TOA radiance. The primary intended use of the product is to provide surface reflectance information for OMI cloud, aerosol and trace gas algorithms. GLER is designed to easily replace commonly used LER climatologies within existing OMI algorithms. The product lead is Joanna J. Joiner (OMI US science team leader). The algorithm developer is Wenhan Qin. The OMGLER product file is produced in the version 5 Hierarchical Data Format (HDF-EOS5). Each file contains GLER data for the daylit portion of an orbit (~53 minutes). There are approximately 14 orbits per day. Files are roughly 9 MB in size.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ompixcor&quot;&gt;OMPIXCOR&lt;/h4&gt;
The Version-3 Aura Ozone Monitoring Instrument (OMI) Pixel Corner Product, OMPIXCOR, is now available from the NASA Goddard Earth Sciences Data and Information Services Center (GES DISC) for public access. The shortname for this Level-2 OMI product is OMPIXCOR. The algorithm lead for this product is the US OMI scientists Dr. Thomas Kurosu from the Harvard-Smithsonian Center, Cambridge, MA. The OMPIXCOR product contains ground locations of the OMI pixel corners in the global scanning mode. The motivation for the development of the OMI ground pixel corner products was the common need for: the visualization of derived OMI data products, the provision of ground pixel area for computations of trace gas emissions per area, the facilitation of the development of cross-platform pixel mapping applications (e.g., between OMI and MODIS), and to generally aid validation studies, to name just a few. The OMPIXCOR files are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5). Each file contains data from the day lit portion of an orbit (~53 minutes) . There are approximately 14 orbits per day. The average file size for the OMPIXCOR data product is about 5 Mbytes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;oml1birr&quot;&gt;OML1BIRR&lt;/h4&gt;
The Aura Ozone Monitoring Instrument (OMI) Level 1B (L1B) UV Averaged Solar Irradiances product (shortname OML1BIRR) contains the averaged radiometrically calibrated irradiance measurements from the UV and VIS detectors. The OMI UV Band 1 (264-311 nm) has 159 wavelength bins, the UV Band 2 (307-383 nm) has 559 wavelength bins, and the VIS Band 3 (349-504 nm) has 751 wavelength bins. The data files are written in netCDF version 4 format and are usually made once per day when the Sun is within the solar port field-of-view just before the spacecraft moves into the night shadow at the north end of an orbit. The lead algorithm scientist for this product is Quintus Kleipool from the Royal Netherlands Meteorological Institude (KNMI).
&lt;br&gt;&lt;h4 id&#x3D;&quot;oml1birr-1&quot;&gt;OML1BIRR&lt;/h4&gt;
The OMI Level 1B solar irradiance product is the radiometrically calibrated and geolocated measurements of the UV and Visible channels of the spectral solar irradiance. It is the averaged measurements of the solar irradiances over a single solar observation in the wavelength ranges of UV1 (264-311 nm, 159 channels), UV2 (307-383 nm, 557 channels) and VIS (349-504 nm, 751 channels). The data contain solar measurement products for both the global and the spatial zoom-in mode. This product only contains measurements obtained with the quartz volume diffuser and provides average of the individual measurements made along track to average out the solar elevation dependent bidirectional reflectance distribution function (BRDF) features of the diffuser. The shortname for this OMI Level-1B Product is OML1BIRR. The lead algorithm scientists for this product is Dr. Marcel Dobber from the Roayl Netherlands Meteorological Institude (KNMI). OMI calibrated and geolocated radiances for the UV and Visible channels, spectral irradiances, calibration measurements, and all derived geophysical atmospheric products are archived at the NASA Goddard Earth Sciences Data and Information Services Center (GES DISC). OML1BIRR files are stored in the HDF4 based EOS Hierarchical Data Format. The radiances for the earth measurements (also referred as signal) and its precision are stored as a 16 bit mantissa and an 8-bit exponent. The signal can be computed using the equation: signal &#x3D; mantissa x 10^exponent. For the precision, the same exponent is used as for the signal.
&lt;br&gt;&lt;h4 id&#x3D;&quot;oml1brug&quot;&gt;OML1BRUG&lt;/h4&gt;
The Aura Ozone Monitoring Instrument (OMI) Level-1B (L1B) Geo-located Earth View UV Radiance, Global-Mode (OML1BRUG) Version-3 product contains geo-located Earth view spectral radiances from the UV detectors in the wavelength range of 264 to 383 nm conducted in the global measurement mode. In the standard global measurement mode, OMI observes 60 ground pixels (13 km x 24 km at nadir) across the swath for each of the 557 channels of UV2 (307-383 nm) and 30 ground pixels (13 km x 48 km at nadir) for the 159 channels of UV1 (264-311 nm). Each file contains data from the day lit portion of an orbit (~53 minutes) and is roughly 180 MB in size. There are approximately 14 orbits per day. Once a month, in one orbit, OMI performs dark measurements, it does not perform radiance measurements. In addition, OMI performs spatial zoom measurements one day per month. For that day, this product also contains UV2 measurements that are rebinned from the spatial zoom-in measurements. In original spatial zoom mode the nadir ground pixel size is 13 x 12 km and measurements are available only for the UV2 and VIS wavelengths (306 to 432 nm). The shortname for this OMI Level-1B Product is OML1BRUG. The lead algorithm scientist for this product is Dr. Marcel Dobber from the Royal Netherlands Meteorological Institude (KNMI). The OML1BRUG files are stored in the HDF4 based EOS Hierarchical Data Format (HDF-EOS). The radiances for the earth measurements (also referred as signal) and its precision are stored as a 16 bit mantissa and an 8-bit exponent. The signal can be computed using the equation: signal &#x3D; mantissa x 10^exponent. For the precision, the same exponent is used as for the signal.
&lt;br&gt;&lt;h4 id&#x3D;&quot;oml1brug-1&quot;&gt;OML1BRUG&lt;/h4&gt;
The Aura Ozone Monitoring Instrument (OMI) Level 1B (L1B) Geolocated Earthshine UV Radiance, Global-mode (shortname OML1BRUG) Version 4 product contains geolocated Earth view spectral radiances from the UV detectors in the wavelength range of 264 to 383 nm taken in the global measurement mode. In the global mode, OMI observes 60 ground pixels (13 km x 24 km at nadir) across the swath (~2600 km) for each of the 557 channels of Band 2 (307-383 nm) and 30 ground pixels (13 km x 48 km at nadir) for the 159 channels of Band 1 (264-311 nm). There are approximately 14 files of orbital data per day. Each file contains data from the daylit portion of an orbit and is roughly 210 MB in size. This OML1BRUG global-mode product is occasionally unavailable when the instrument is collecting data in the zoom-mode or is making special calibration measurements. The data in the OML1BRUG files are stored in the Network Common Data Form (netCDF) format. The lead algorithm scientist for the OMI Level 1 products is Dr. Quintus Kleipool of the Royal Netherlands Meteorological Institude (KNMI).
&lt;br&gt;&lt;h4 id&#x3D;&quot;oml1bruz&quot;&gt;OML1BRUZ&lt;/h4&gt;
The Aura Ozone Monitoring Instrument (OMI) Level-1B (L1B) Geo-located Earth View UV Radiance, Zoom-in-Mode (OML1BRUZ) Version-3 product contains geo-located Earth view spectral radiances from the UV detectors in the wavelength range of 264 to 383 nm using spectral and spatial zoom-in measurement modes. In zoom-in measurement mode, OMI observes 60 ground pixels (13 km x 24 km at nadir) across the swath. Each file contains data from the day lit portion of an orbit (~60 minutes) and is roughly 215 MB in size. There are approximately 14 orbits per day. OMI performs spatial zoom-in measurements one day per month. For that day, this product also contains UV2 measurements that are rebinned from the spatial zoom-in measurements. The shortname for this OMI Level-1B Product is OML1BRUZ. The lead algorithm scientist for this product is Dr. Marcel Dobber from the Royal Netherlands Meteorological Institude (KNMI). The OML1BRUZ files are stored in HDF4 based EOS Hierarchical Data Format (HDF-EOS). The radiances for the earth measurements (also referred as signal) and its precision are stored as a 16 bit mantissa and an 8-bit exponent. The signal can be computed using the equation: signal &#x3D; mantissa x 10^exponent. For the precision, the same exponent is used as for the signal.
&lt;br&gt;&lt;h4 id&#x3D;&quot;oml1bruz-1&quot;&gt;OML1BRUZ&lt;/h4&gt;
The Aura Ozone Monitoring Instrument (OMI) Level 1B (L1B) Geolocated Earthshine UV Radiance, Zoom-mode (shortname OML1BRUZ) Version 4 product contains geolocated Earth view spectral radiances from the UV detectors in the wavelength range of 264 to 383 nm taken in the global measurement mode. In the zoom-in mode, OMI observes 60 ground pixels (13 km x 12 km at nadir) across the swath (&lt;del&gt;750 km width) for each of the 557 channels of Band 2 (307-383 nm) and 30 ground pixels (13 km x 24 km at nadir) across the swath (&lt;/del&gt;2600 km) for the 159 channels of Band 1 (264-311 nm). There are approximately 14 files of orbital data per day. Each file contains data from the daylit portion of an orbit and is roughly 210 MB in size. This OML1BRUZ zoom-in mode product is only available about once a month. The data in the OML1BRUZ files are stored in the Network Common Data Form (netCDF) format. The lead algorithm scientist for the OMI Level 1 products is Dr. Quintus Kleipool of the Royal Netherlands Meteorological Institude (KNMI).
&lt;br&gt;&lt;h4 id&#x3D;&quot;oml1brvg&quot;&gt;OML1BRVG&lt;/h4&gt;
The Aura Ozone Monitoring Instrument (OMI) Level-1B (L1B) Geo-located Earth View VIS Radiance, Global-Mode (OML1BRVG) Version-3 product contains geo-located Earth view spectral radiances from the VIS detector in the wavelength range of 349 to 504 nm conducted in the global measurement mode. In the standard global measurement mode, OMI observes 60 ground pixels (13 km x 24 km at nadir) across the swath (13 km x 48 km at nadir). Each file contains data from the day lit portion of an orbit (~60 minutes) and is roughly 200 MB in size. There are approximately 14 orbits per day. Once a month, in one orbit, OMI performs dark measurements, it does not perform radiance measurements. In addition, OMI performs spatial zoom measurements one day per month. For that day, this product also contains UV2 measurements that are rebinned from the spatial zoom-in measurements. In original spatial zoom mode the nadir ground pixel size is 13 x 12 km and measurements are available only for the UV2 and VIS wavelengths (306 to 432 nm). The shortname for this OMI Level-1B Product is OML1BRVG. The lead algorithm scientist for this product is Dr. Marcel Dobber from the Royal Netherlands Meteorological Institude (KNMI). The OML1BRVG files are stored in the HDF4 based EOS Hierarchical Data Format (HDF-EOS). The radiances for the earth measurements (also referred as signal) and its precision are stored as a 16-bit mantissa and an 8-bit exponent. The signal can be computed using the equation: signal &#x3D; mantissa x 10^exponent. For the precision, the same exponent is used as for the signal.
&lt;br&gt;&lt;h4 id&#x3D;&quot;oml1brvg-1&quot;&gt;OML1BRVG&lt;/h4&gt;
The Aura Ozone Monitoring Instrument (OMI) Level 1B (L1B) Geolocated Earthshine VIS Radiance, Global-mode (shortname OML1BRVG) Version 4 product contains geolocated Earth view spectral radiances from the VIS detectors in the wavelength range of 349 to 504 nm taken in the global measurement mode. In the global mode, OMI observes 60 ground pixels (13 km x 24 km at nadir) across the swath (~2600 km) for each of the 751 channels of Band 3 (349-504 nm). There are approximately 14 files of orbital data per day. Each file contains data from the daylit portion of an orbit and is roughly 240 MB in size. This OML1BRVG global-mode product is occasionally unavailable when the instrument is collecting data in the zoom-mode or is making special calibration measurements. The data in the OML1BRVG files are stored in the Network Common Data Form (netCDF) format. The lead algorithm scientist for the OMI Level 1 products is Dr. Quintus Kleipool of the Royal Netherlands Meteorological Institude (KNMI).
&lt;br&gt;&lt;h4 id&#x3D;&quot;oml1brvz&quot;&gt;OML1BRVZ&lt;/h4&gt;
The Aura Ozone Monitoring Instrument (OMI) Level-1B (L1B) Geo-located Earth View VIS Radiance, Zoom-in-Mode (OML1BRVZ) Version-3 product contains geo-located Earth view spectral radiances from the VIS detectors in the wavelength range of 349 to 504 nm using spectral and spatial zoom-in measurement modes. In zoom-in measurement mode, OMI observes 60 ground pixels (13 km x 24 km at nadir) across the swath. Each file contains data from the day lit portion of an orbit (~60 minutes) and is roughly 190 MB in size. There are approximately 14 orbits per day. OMI performs spatial zoom-in measurements one day per month. For that day, this product also contains VIS measurements that are rebinned from the spatial zoom-in measurements. The lead algorithm scientist for this product is Dr. Marcel Dobber from the Royal Netherlands Meteorological Institude (KNMI). The OML1BRVZ files are stored in the HDF4 based EOS Hierarchical Data Format (HDF-EOS). The radiances for the earth measurements (also referred as signal) and its precision are stored as a 16 bit mantissa and an 8-bit exponent. The signal can be computed using the equation: signal &#x3D; mantissa x 10^exponent. For the precision, the same exponent is used as for the signal.
&lt;br&gt;&lt;h4 id&#x3D;&quot;oml1brvz-1&quot;&gt;OML1BRVZ&lt;/h4&gt;
The Aura Ozone Monitoring Instrument (OMI) Level 1B (L1B) Zoom-in Earthshine UV Radiance, Zoom-mode (shortname OML1BRVZ) Version 4 product contains geolocated Earth view spectral radiances from the VIS detectors in the wavelength range of 349 to 504 nm taken in the zoom-in measurement mode. In the zoom-in mode, OMI observes 60 ground pixels (13 km x 12 km at nadir) across the swath (~750 km width) for each of the 751 channels of Band 3 (349-504 nm). There are approximately 14 files of orbital data per day. Each file contains data from the daylit portion of an orbit and is roughly 240 MB in size. This OML1BRVZ zoom-in mode product is only available about once a month. The data in the OML1BRVZ files are stored in the Network Common Data Form (netCDF) format. The lead algorithm scientist for the OMI Level 1 products is Dr. Quintus Kleipool of the Royal Netherlands Meteorological Institude (KNMI).
&lt;br&gt;&lt;h4 id&#x3D;&quot;omaero&quot;&gt;OMAERO&lt;/h4&gt;
The Level-2 Aura Ozone Monitoring Instrument (OMI) Aerosol Product (OMAERO) is now available from NASA Goddard Earth Sciences Data and Information Services Center (GES DISC) for public access. This is the second public release of version 003. The data was re-processed in late 2011 using an improved algorithm (processing version 1.2.3.1). After some quick validation the reprocessed data was released to the public in March 2012. The shortname for this Level-2 Aerosol Product is OMAERO_V003. There are two Level-2 Aura OMI aerosol products OMAERUV and OMAERO. The OMAERUV product uses the near-UV algorithm. The OMAERO product is based on the multi-wavelength algorithm and that uses up to 20 wavelength bands between 331 nm and 500 nm. OMAERO retrieval algorithm is developed by the KNMI OMI Team Scientists. Drs. Deborah Stein-Zweers, Martin Sneep and Pepijn Veefkind are now the key investigators of this product. The OMAERO product contains Aerosol Optical Depths, Single Scattering Albedo, and other ancillary and geolocation information. The OMAERO files are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5). Each file contains data from the day lit portion of an orbit (~53 minutes). There are approximately 14 orbits per day. The maximum file size for the OMAERO data product is about 6 Mbytes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omaerog&quot;&gt;OMAEROG&lt;/h4&gt;
This Level-2G daily global gridded product OMAEROG is based on the pixel level OMI Level-2 Aerosol product OMAERO, based on the multi-wavelength algorithm that uses up to 20 wavelength bands between 331 nm and 500 nm. OMAEROG is a special Level-2 gridded product where pixel level products are binned into 0.25 x 0.25 degree global grids. It contains the data for all scenes that have observation time between UTC times of 00:00:00 and 23:59:59.9999. All data pixels that fall in a grid box are saved without averaging. Scientists can apply a data filtering scheme of their choice and create new gridded products. The OMAEROG data product contains almost all parameters that are in OMAERO. For example, in addition to the extinction optical depth and single scattering albedo, it also contains aerosol indices, cloud fraction, cloud pressure, terrain height, geolocation, solar and satellite viewing angles, and extensive quality flags. The OMAEROG files are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5). Each file contains daily data from approximately 15 orbits. The maximum file size for the OMAEROG data product is about 78 Mbytes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omaeroe&quot;&gt;OMAEROe&lt;/h4&gt;
The OMI science team produces this Level-3 Aura/OMI Global Aerosol Data Products OMAEROe (0.25deg Lat/Lon grids). The OMAEROe product selects best aerosol value from the Level2G good quality data that are reported in each grid, based on the multi-wavelength algorithm that uses up to 20 wavelength bands between 331 nm and 500 nm. The selection criteria is based on the shortest optical path length (secant of solar zenith angle + secant of viewing zenith angle). The OMAEROe files are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5). Each file contains daily data from approximately 15 orbits. The maximum file size for the OMAEROe data product is about 7 Mbytes. (The shortname for this Level-3 Global Gridded Aerosol Product is OMAEROe)
&lt;br&gt;&lt;h4 id&#x3D;&quot;omaeruv&quot;&gt;OMAERUV&lt;/h4&gt;
The Aura Ozone Monitoring Instrument level-2 near UV Aerosol data product &amp;#39;OMAERUV&amp;#39;, recently re-processed using an enhanced algorithm, is now released (April 2012) to the public. The data are available from the NASA Goddard Earth Sciences Data and Information Services Center (GES DISC). The shortname for this Level-2 near-UV Aerosol Product is OMAERUV_V003. The OMAERUV retrieval algorithm is developed by the US OMI Team Scientists. Dr. Omar Torres (GSFC/NASA) is the principal investigator of this product. The OMAERUV product contains Aerosol Absorption and Aerosol Extinction Optical Depths, and Single Scattering Albedo at three different wavelengths (354, 388 and 500 nm), Aerosol Index, and other ancillary and geolocation parameters, in the OMI field of view (13x24 km). The OMAERUV files are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5). Each file contains data from the day lit portion of an orbit (~53 minutes). There are approximately 14 orbits per day. The maximum file size for the OMAERUV data product is about 6 Mbytes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omaeruv-1&quot;&gt;OMAERUV&lt;/h4&gt;
The Aura Ozone Monitoring Instrument level-2 near UV Aerosol data product OMAERUV (Version 004) is available from the NASA Goddard Earth Sciences Data and Information Services Center (GES DISC) for the public access. The OMAERUV retrieval algorithm is developed by the US OMI Team Scientists. Dr. Omar Torres (GSFC/NASA) is the principal investigator of this product. The OMAERUV product contains Aerosol Optical Depth, Aerosol Single Scattering Albedo, Absorption Optical Depth, UV Aerosol Index, and Aerosol Optical Depth over clouds at three wavelengths (354, 388, and 500 nm), and other ancillary and geolocation parameters, in the OMI field of view (13x24 km). The OMAERUV files are stored in the version 4.0 Network Common Data Form (NetCDF). Each file contains data from the day lit portion of an orbit (~53 minutes). There are approximately 14 orbits per day. The maximum file size for the OMAERUV data product is about 17 Mbytes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omaeruvg&quot;&gt;OMAERUVG&lt;/h4&gt;
This Level-2G daily global gridded product OMAERUVG is based on the pixel level OMI Level-2 AERUV product OMAERUV. This Level-2G daily global gridded product OMAERUVG is based on the pixel level OMI Level-2 Aerosol product OMAERUV. OMAERUVG data product is a special Level-2 gridded product where pixel level products are binned into 0.25x0.25 degree global grids. It contains the data for all scenes that have observation time between UTC times of 00:00:00 and 23:59:59.9999. All data pixels that fall in a grid box are saved without averaging. Scientists can apply a data filtering scheme of their choice and create new gridded products. The OMAERUVG files are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5). Each file contains daily data from approximately 15 orbits mapped on the Global 0.25x0.25 deg Grids. The maximum file size for the OMAERUVG data product is about 50 Mbytes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omaeruvd&quot;&gt;OMAERUVd&lt;/h4&gt;
The OMI science team produces this Level-3 daily global gridded product OMAERUVd (1 deg Lat/Lon grids). The OMAERUVd product is produced with all data pixels that fall in a grid box with quality filtered and then averaged, based on the pixel level OMI Level-2 Aerosol data product OMAERUV. The OMAERUV data product is based on the enhanced TOMS version-8 algorithm that essentially uses the ultraviolet radiance data. The OMAERUVd data product contains extinction and absorption optical depths at three wavelenghts (355 nm, 388 nm and 500 nm). The OMAERUVd files are stored in version 5 EOS Hierarchical Data Format (HDF-EOS5). Each file contains daily data from approximately 15 orbits. The maximum file size for the OMAERUVd data product is about 0.2 Mbytes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omno2&quot;&gt;OMNO2&lt;/h4&gt;
The Version 4.0 Aura Ozone Monitoring Instrument (OMI) Nitrogen Dioxide (NO2) Standard Product (OMNO2) is now available from the NASA Goddard Earth Sciences Data and Information Services Center. The major V4.0 updates include: (1) use of a new daily and OMI ﬁeld of view speciﬁc geometry dependent surface Lambertian Equivalent Reﬂectivity (GLER) product in both NO2 and cloud retrievals; (2) use of improved cloud parameters (eﬀective cloud fraction and cloud optical centroid pressure) from a new cloud algorithm (OMCDO2N) that are retrieved consistently with NO2 using a new algorithm for O2-O2 slant column data and the GLER product for terrain reﬂectivity; (3) use of a more accurate terrain pressure calculated using OMI ground pixel-averaged terrain height and monthly mean GMI terrain pressure; and (4) improved treatment over snow/ice surfaces by using the concept of scene LER and scene pressure. The details can be found in the updated OMNO2 readme document (see Documentation). The OMNO2 product contains slant column NO2 (total amount along the average optical path from the sun into the atmosphere, and then toward the satellite), the total NO2 vertical column density (VCD), the stratospheric and tropospheric VCDs, air mass factors (AMFs), scattering weights for calculation of AMFs, and other ancillary data. The short name for the Level-2 swath type column NO2 products is OMNO2. Other OMNO2-associated NO2 products include the Level-2 gridded column product, OMNO2G, and the Level-3 gridded column product, OMNO2d. The OMNO2 files are stored in version 5 EOS Hierarchical Data Format (HDF-EOS5). Each Level-2 file contains data from the day lit portion of an orbit (~53 minutes). There are approximately 14 orbits per day. The maximum file size for the OMNO2 is ~24 MB.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omno2-1&quot;&gt;OMNO2&lt;/h4&gt;
The Collection 4, Version 5.0, Aura Ozone Monitoring Instrument (OMI) Nitrogen Dioxide (NO2) Standard Product (OMNO2) is now available from the NASA Goddard Earth Sciences Data and Information Services Center. The major V5.0 updates include the use of: (1) improved Collection 4 Level-1B radiance and irradiance data in the retrieval of NO2 and O2-O2 slant columns; (2) a-priori NO2 profiles and other model-derived information from a high-resolution (&lt;del&gt;25 km) Global Modeling Initiative (GMI) simulation; (3) a new algorithm for improved de-striping and data flagging to correct for cross-track artifacts and row-anomaly; (4) updated geometry dependent surface Lambertian Equivalent Reﬂectivity (GLER) and consistently-retrieved O2-O2 cloud products; and (5) improved snow/ice database and treatment in the GLER, cloud, and NO2 algorithms. The details can be found in the updated OMNO2 readme document (see Documentation). The OMNO2 product contains NO2 slant column density (SCD), total NO2 vertical column density (VCD), the stratospheric and tropospheric VCDs, air mass factors (AMFs), scattering weights for AMF calculation, and other ancillary data used in the OMNO2 algorithm. The OMI NO2 files are stored in version 5 EOS Hierarchical Data Format (HDF-EOS5). The short name for the Level-2 swath type column NO2 products is OMNO2. Each Level-2 file contains data from the day lit portion of an orbit (&lt;/del&gt;53 minutes). There are approximately 14 orbits per day. The maximum file size for the OMNO2 is ~21 MB. Other OMNO2-associated NO2 products include the Level-2 gridded column product, OMNO2G, and the Level-3 gridded column product, OMNO2d.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omno2d&quot;&gt;OMNO2d&lt;/h4&gt;
This is Level-3 daily global gridded (0.25x0.25 degree) Nitrogen Dioxide Product (OMNO2d). OMNO2d data product is a Level-3 Gridded Product where pixel level data of good quality are binned and &amp;quot;averaged&amp;quot; into 0.25x0.25 degree global grids. This product contains Total column NO2 and Total Tropospheric Column NO2, for all atmospheric conditions, and for sky conditions where cloud fraction is less than 30 percent. Nitrogen dioxide is an important chemical species in both, the stratosphere where it plays a key role in ozone chemistry, and in the troposphere where it is a precursor to ozone production. In the troposphere, it is produced in various combustion processes and in lightning and is an indicator of poor air quality. The OMNO2d data are stored in version 5 EOS Hierarchical Data Format (HDF-EOS). Each file contains data from the day lit portion of the orbit (~14 orbits). The average file size for the OMNO2d data product is about 12 Mbytes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omno2g&quot;&gt;OMNO2G&lt;/h4&gt;
This Level-2G daily global gridded product OMNO2G is based on the pixel level OMI Level-2 NO2 product OMNO2. OMNO2G data product is a special Level-2 Gridded Product where pixel level data are binned into 0.25x0.25 degree global grids. It contains the data for all L2 scenes that have observation time between UTC times of 00:00:00 and 23:59:59.9999. All data pixels that fall in a rid box are saved Without Averaging. Nitrogen dioxide is an important chemical species in both the stratosphere, where it plays a key role in ozone chemistry, and in the troposphere, where it is a precursor to ozone production. In the troposphere, it is produced in various combustion processes and in lightning and is an indicator of poor air quality. The OMNO2G data product contains almost all parameters that are contained in OMNO2 product. The OMNO2G data are stored in version 5 EOS Hierarchical Data Format (HDF-EOS5). Each file contains data from the day lit portion of the orbit (~14 orbits). The average file size for the OMNO2G data product is about 115 Mbytes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omdoao3g&quot;&gt;OMDOAO3G&lt;/h4&gt;
This Level-2G daily global gridded product OMDOAO3G is based on the pixel level OMI Level-2 DOAO3 product OMDOAO3. This Level-2G global total column ozone product is derived from OMDOAO3 which is based on the Differential Absorption Spectroscopy (DOAS) fitting technique that essentially uses the OMI visible radiance values between 331.1 and 336.1 nm. In addition to the total ozone column this product also contains some auxiliary derived and ancillary input parameters, e.g. ozone slant column density, ozone ghost column density, etc. The short name for this Level-2 OMI ozone product is OMDOAO3G and the lead algorithm scientist for this product and for OMDOAO3 (the data source of OMDOAO3G) is Dr. Pepijn Veefkind from KNMI. The OMDOAO3G product files are stored in the version 5 Hierarchical Data Format (HDF-EOS5). Each daily file contains data from the day lit portion of the orbits (approximately 14 orbits) and is roughly 80 MB in size.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omdoao3e&quot;&gt;OMDOAO3e&lt;/h4&gt;
The OMI science team produces this Level-3 Aura/OMI Global OMDOAO3e Data Products (0.25deg Lat/Lon grids). This Level-3 global total column ozone product is derived from OMDOAO3 which is based on the Differential Absorption Spectroscopy (DOAS) fitting technique that essentially uses the OMI visible radiance values between 331.1 and 336.1 nm. In addition to the total ozone column (best quality data, satisfying the shortest path length) and its precision this product also contains some ancillary parameters such as cloud fraction, cloud height, etc. The short name for this Level-3 OMI ozone product is OMDOAO3e and the lead Algorithm scientist for this product and for OMDOAO3 (the data source of OMDOAO3e) is Dr. Pepijn Veefkind from KNMI. The OMDOAO3e product files are stored in the version 5 Hierarchical Data Format (HDF-EOS5). Each daily file contains data from the day lit portion of the orbits (approximately 14 orbits) and is roughly 8 MB in size.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omo3pr&quot;&gt;OMO3PR&lt;/h4&gt;
The Aura Ozone Monitoring Instrument Level-2 Ozone Profile data product OMO3PR (Version 003) is now available from the NASA Goddard Earth Sciences Data and Information Services Center (GES DISC) for the public access. OMI Level-2 ozone profile product, OMO3PR at the pixel resolution 13x 48 km (at nadir), is based on the optimal estimation algorithm (Rodgers, 2000) with climatological ozone profiles as a-priori information. The OMO3PR retrieval algorithm uses spectral radiance values from the UV1 channel (270 nm to 308.5 nm) and from the first part of the UV2 channel (311.5 nm to 33 0 nm). OMO3PR product provides ozone values (in Dobson unit) for 18 atmospheric layers. It also provides a-priori ozone profile values, error covariance matrix, averaging kernel and some ancillary information such as time, latitude, longitude, solar zenith and viewing zenith angles and quality flags. The short name for this Level-2 OMI ozone profile product is OMO3PR. The lead scientist for this product is Dr. Johan de Haan. The OMO3PR product files are stored in the version 5 Hierarchical Data Format (HDF-EOS5). Each file contains data from the day lit portion of an orbit (approximately 53 minutes). There are approximately 14 orbits per day thus the total data volume is approximately 150 GB/day.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omto3g&quot;&gt;OMTO3G&lt;/h4&gt;
This Level-2G daily global gridded product OMTO3G is based on the pixel level OMI Level-2 Total Ozone Product OMTO3. The OMTO3 product is from the enhanced TOMS version-8 algorithm that essentially uses the ultraviolet radiance data at 317.5 and 331.2 nm. The OMTO3G data product is a special Level-2 Global Gridded Product where pixel level data are binned into 0.25x0.25 degree global grids. It contains the data for all L2 scenes that have observation time for the 24-hour period beginning at 00:00:00 UTC. All data pixels that fall in a grid box are saved without averaging. Scientists can apply a data filtering scheme of their choice and create new gridded products. The OMTO3G data product contains almost all parameters that are contained in the OMTO3. For example, in addition to the total column ozone it also contains cloud fraction, cloud pressure, terrain height, geolocation, solar and satellite viewing angles, and quality flags. The OMTO3G files are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5). Each file contains daily data from approximately 15 orbits. The maximum file size for the OMTO3G data product is about 150 Mbytes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omto3&quot;&gt;OMTO3&lt;/h4&gt;
The Aura Ozone Monitoring Instrument (OMI) Level-2 Total Column Ozone Data Product OMTO3 (Version 003) is available from the NASA Goddard Earth Sciences Data and Information Services Center (GES DISC) for the public access. OMI provides two Level-2 (OMTO3 and OMDOAO3) total column ozone products at pixel resolution (13 x 24 km at nadir) that are based on two different algorithms. This level-2 global total column ozone product (OMTO3) is based on the enhanced TOMS version-8 algorithm that essentially uses the ultraviolet radiance data at 317.5 and 331.2 nm. OMI hyper-spectral measurements help in the corrections for the factors that induce uncertainty in ozone retrievals (e.g., cloud and aerosol, sea-glint effects, profile shape sensitivity, SO2 and other trace gas contamination). In addition to the total ozone values this product also contains some auxiliary derived and ancillary input parameters including N-values, effective Lambertian scene-reflectivity, UV aerosol index, SO2 index, cloud fraction, cloud pressure, ozone below clouds, terrain height, geolocation, solar and satellite viewing angles, and quality flags. The shortname for this Level-2 OMI total column ozone product is OMTO3. The algorithm lead for this product is NASA OMI scientist Dr. Pawan K. Bhartia. The OMTO3 files are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5). Each file contains data from the day lit portion of an orbit (~53 minutes). There are approximately 14 orbits per day. The maximum file size for the OMTO3 data product is approximately 35 MB.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omto3-1&quot;&gt;OMTO3&lt;/h4&gt;
The Aura Ozone Monitoring Instrument (OMI) Level-2 Total Column Ozone Data Product OMTO3 (Collection Version 004) is available from the NASA Goddard Earth Sciences Data and Information Services Center (GES DISC) for the public access. This level-2 global total column ozone product (OMTO3) is based on the enhanced TOMS version-8 algorithm that essentially uses the ultraviolet radiance data at 317.5 and 331.2 nm at a pixel resolution of 13 x 24 km at nadir. OMI hyper-spectral measurements help in the corrections for the factors that induce uncertainty in ozone retrievals (e.g., cloud and aerosol, sea-glint effects, profile shape sensitivity, SO2 and other trace gas contamination). In addition to the total ozone values this product also contains some auxiliary derived and ancillary input parameters including N-values, effective Lambertian scene-reflectivity, cloud fraction, cloud pressure, ozone below clouds, terrain height, geolocation, solar and satellite viewing angles, and quality flags. The shortname for this Level-2 OMI total column ozone product is OMTO3. The algorithm for this product was originally developed by a team led by Dr. Pawan K. Bhartia at NASA Goddard Space Flight Center. The current product lead is Dr. Can Li. The OMTO3 files are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5). Each file contains data from the day lit portion of an orbit (~53 minutes). There are approximately 14 orbits per day. The maximum file size for the OMTO3 data product is approximately 35 MB.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omso2e&quot;&gt;OMSO2e&lt;/h4&gt;
The OMI science team produces this Level-3 Aura/OMI Global OMSO2e Data Products (0.25 degree Latitude/Longitude grids). In this Level-3 daily global SO2 data product, each grid contains only one observation of Total Column Density of SO2 in the Planetary Boundary Layer (PBL), based on an improved Principal Component Analysis (PCA) Algorithm. This single observation is the &amp;quot;best pixel&amp;quot;, selected from all &amp;quot;good&amp;quot; L2 pixels of OMSO2 that overlap this grid and have UTC time between UTC times of 00:00:00 and 23:59:59.999. In addition to the SO2 Vertical column value some ancillary parameters, e.g., cloud fraction, terrain height, scene number, solar and satellite viewing angles, row anomaly flags, and quality flags have been also made available corresponding to the best selected SO2 data pixel in each grid. The OMSO2e files are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5) using the grid model.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omso2&quot;&gt;OMSO2&lt;/h4&gt;
The Aura Ozone Monitoring Instrument (OMI) level 2 sulphur dioxide (SO2) total column product (OMSO2) has been updated with a principal component analysis (PCA)-based algorithm (v2) with new SO2 Jacobian lookup tables and a priori profiles that significantly improve retrievals for anthropogenic SO2. The data files (or granules) contain different estimates of the vertical column density (VCD) of SO2 depending on the users investigating anthropogenic or volcanic sources. Files also contain quality flags, geolocation and other ancillary information. The lead scientist for the OMSO2 product is Can Li. The OMSO2 files are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5). Each file contains data from the daylit half of an orbit (~53 minutes). There are approximately 14 orbits per day. The resolution of the data is 13x24 km2 at nadir, with a swath width of 2600 km and 60 pixels per scan line every 2 seconds.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omso2g&quot;&gt;OMSO2G&lt;/h4&gt;
This Level-2G daily global gridded product OMSO2G is based on the pixel level OMI Level-2 SO2 product OMSO2. OMSO2G data product is a special Level-2 gridded product where pixel level products are binned into 0.125x0.125 degree global grids. It contains the data for all scenes that have observation time between UTC times of 00:00:00 and 23:59:59.9999 . All data pixels that fall in a grid box are saved without averaging. Scientists can apply a data filtering scheme of their choice and create new gridded products. The OMSO2G data product contains almost all parameters that are contained in OMSO2 files. For example, in addition to three values of SO2 Vertical column corresponding to three a-priori vertical profiles used in the retrieval algorithm, and ancillary parameters, e.g., UV aerosol index, cloud fraction, cloud pressure, geolocation, solar and satellite viewing angles, and quality flags. The OMSO2G files are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5). Each file contains daily data from approximately 15 orbits. The maximum file size for the OMTO3G data product is about 146 Mbytes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omler&quot;&gt;OMLER&lt;/h4&gt;
The OMI Earth Surface Reflectance Climatology product, OMLER (Global 0.5 degrees Lat/Lon grid) which is based on Version 003 Level-1B top of atmosphere upwelling radiance and incoming irradiance. OMI calibrated and geolocated radiances from 159 channels in UV1(264-311 nm), 557 channels in UV2 (307-383 nm) and 751 channels in VIS (349-504) spectral regions, spectral irradiances, calibration measurements, and all derived geophysical atmospheric products (Level-2 and 3) are archived at the NASA Goddard DAAC. OMLER spectral surface reflectance product contains monthly and yearly climatology of the Earth&amp;#39;s surface Lambert Equivalent Reflectance (LER) for 23 wavelengths in the spectral range 309 to 500 nm, at a spatial resolution of 0.5 by 0.5 degrees. This LER is defined as the required reflectance of an isotropic surface needed to match the observed top of the atmosphere (TOA) reflectance in a pure Rayleigh scattering atmosphere under cloud free conditions and no aerosols. The climatology is based on statistical analysis of the three years of OMI version 03 radiance data (Oct 2004-Oct 2007). This product also provides minimum spectral surface reflectivity observed during the three year period. The OMLER product file is produced in the version 5 Hierarchical Data Format (HDF-EOS5). It is roughly 300 MB in size.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omuvb&quot;&gt;OMUVB&lt;/h4&gt;
The Aura Ozone Monitoring Instrument (OMI) Version 003 Surface UV Irradiance Product (OMUVB) is now available from the NASA Goddard Earth Sciences Data and Information Services Center (GES DISC) for the public access. The shortname for this Level-2 OMI Surface UVB product is OMUVB. The algorithm scientists for this product are: Dr. Jari Hovila, Dr. Antii Arola and Dr. Johanna Taminnen. The OMUVB product contains erythemally weighted daily dose and dose rate, and spectral irradiances at 305, 310, 324, and 380 nm. It also contains quality flags, cloud optical depth, Lambertian Equivalent Reflectivity, Total Column Ozone amount, and other ancillary information. The OMUVB files are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5). Each file contains data from the day lit portion of an orbit (~53 minutes). There are approximately 14 orbits per day. The maximum file size for the OMUVB data product is about 10 Mbytes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omuvbg&quot;&gt;OMUVBG&lt;/h4&gt;
This is Level-2G daily global gridded Aura-OMI Spectral Surface UVB Irradiance and Erythemal Dose product (OMUVBG). The OMUVBG is a special Level-2 Global Gridded type data Product (referred as Level 2G or L2G) where Level-2 or swath pixel data are binned (but not averaged)into 0.25x0.25 degree global grids. It contains the data for all L2 scenes that have observation time between UTC times of 00:00:00 and 23:59:59.9999. All ancillary parameters such as latitude, longitude, time, solar and viewing angles are also saved for each pixel. First two dimensions of each parameter correspond to spatial (Lat/Lon based) Grid ID and third dimension identifies the pixel or observed scene (referred as &amp;#39;candidates&amp;#39; ID). Scientists can apply a data filtering scheme of their choice, average good quality pixels data in each grid and create their Level-3 products. The OMUVBG files are available in the version 5 EOS Hierarchical Data Format (HDF-EOS5). Each file contains daily data from the day lit portion of the globe. The maximum file size for the OMUVBG data product is about 128 MBytes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omuvbd&quot;&gt;OMUVBd&lt;/h4&gt;
This is Level-3 daily global gridded Aura-OMI Spectral Surface UVB Irradiance and Erythemal Dose product (OMUVBd). The OMUVBd product contains global erythemally weighted daily dose and erythemal dose rate at local solar noon at 1.0x1.0 deg grids. The OMUVBd files are available in the version 5 EOS Hierarchical Data Format (HDF-EOS5). Each file contains daily data from the day lit portion of the globe. The maximum file size for the OMUVBd data product is about 5 MBytes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omto3e&quot;&gt;OMTO3e&lt;/h4&gt;
The OMI science team produces this Level-3 Aura/OMI Global TOMS-Like Total Column Ozone gridded product OMTO3e (0.25deg Lat/Lon grids). The OMTO3e product selects the best pixel (shortest path length) data from the good quality filtered level-2 total column ozone data (OMTO3) that fall in the 0.25 x 0.25 degree global grids. Each file contains total column ozone, radiative cloud fraction and solar and viewing zenith angles. The OMTO3e files are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5). Each file contains daily data from approximately 15 orbits. The maximum file size for the OMTO3e data product is about 2.8 Mbytes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omto3d&quot;&gt;OMTO3d&lt;/h4&gt;
The OMI science team produces this Level-3 daily global TOMS-Like Total Column Ozone gridded product OMTO3d (1 deg Lat/Lon grids). The OMTO3d product is produced by gridding and averaging only good quality level-2 total column ozone orbital swath data (OMTO3, based on the enhanced TOMS version-8 algorithm) on the 1x1 degree global grids. The OMTO3d files are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5). Each file contains daily data from approximately 15 orbits. The maximum file size for the OMTO3d data product is about 0.65 Mbytes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ompixcorz&quot;&gt;OMPIXCORZ&lt;/h4&gt;
The Version-3 Aura Ozone Monitoring Instrument (OMI) Pixel Corner Product in zoom-in mode, OMPIXCORZ, is now available from the NASA Goddard Earth Sciences Data and Information Services Center (GES DISC) for public access. The shortname for this Level-2 OMI product is OMPIXCORZ. The algorithm lead for this product is the US OMI scientists Dr. Thomas Kurosu from the Harvard-Smithsonian Center, Cambridge, MA. The OMPIXCORZ product contains ground locations of the OMI pixel corners in the zoom-in scanning mode. The motivation for the development of the OMI ground pixel corner products was the common need for: the visualization of derived OMI data products, the provision of ground pixel area for computations of trace gas emissions per area, the facilitation of the development of cross-platform pixel mapping applications (e.g., between OMI and MODIS), and to generally aid validation studies, to name just a few. The OMPIXCORZ files are stored in the version 5 EOS Hierarchical Data Format (HDF-EOS5). Each file contains data from the day lit portion of an orbit (~53 minutes) . There are approximately 14 orbits approximately one day per month. The average file size for the OMPIXCORZ data product is about 8 Mbytes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omuanc&quot;&gt;OMUANC&lt;/h4&gt;
The Primary Ancillary Data Geo-Colocated to OMI/Aura UV2 1-Orbit L2 Swath 13x24km (OMUANC) provides selected parameters from GEOS-5 Forward Processing for Instrument Teams (FP-IT) assimilated product produced by the Global Modeling and Assimilation Office (GMAO) co-located in space and time with the OMI UV-2 swath. The fields in this product include snow cover, sea ice cover, land cover, terrain height, row anomaly flag, and pixel area. The OMI team also provides a corresponding product for the OMI VIS swath, OMVANC. This product has been generated for convenient use by the OMI/Aura team in their L2 algorithms, and for research where those L2 products are used. The original GEOS-5 FP-IT data are reported on a 0.625 deg longitude by 0.5 deg latitude grid, whereas the OMI UV-2 spatial resolution is 13km x 24km at nadir. The OMUANC files are in netCDF4 format which is compatible with most netCDF and HDF5 readers and tools. Each file is approximately 45mb in size. The lead for this product is Zachary Fasnacht of SSAI. Joanna Joiner is the responsible NASA official.
&lt;br&gt;&lt;h4 id&#x3D;&quot;omvanc&quot;&gt;OMVANC&lt;/h4&gt;
The Primary Ancillary Data Geo-Colocated to OMI/Aura VIS 1-Orbit L2 Swath 13x24km (OMVANC) provides selected parameters from GEOS-5 Forward Processing for Instrument Teams (FP-IT) assimilated product produced by the Global Modeling and Assimilation Office (GMAO) co-located in space and time with the OMI UV-2 swath. The fields in this product include snow cover, sea ice cover, land cover, terrain height, row anomaly flag, and pixel area. The OMI team also provides a corresponding product for the OMI UV2 swath, OMUANC. This product has been generated for convenient use by the OMI/Aura team in their L2 algorithms, and for research where those L2 products are used. The original GEOS-5 FP-IT data are reported on a 0.625 deg longitude by 0.5 deg latitude grid, whereas the OMI UV-2 spatial resolution is 13km x 24km at nadir. The OMVANC files are in netCDF4 format which is compatible with most netCDF and HDF5 readers and tools. Each file is approximately 45mb in size. The lead for this product is Zachary Fasnacht of SSAI. Joanna Joiner is the responsible NASA official.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA BOREAS Project</title>
      <link>https://registry.opendata.aws/nasa-boreas</link>
      <guid>https://registry.opendata.aws/nasa-boreas</guid>
      <description>An inventory of NASA&amp;#39;s airborne and field campaigns for Earth Science
&lt;br&gt;&lt;h4 id&#x3D;&quot;h9rgbl94_229&quot;&gt;h9rgbl94_229&lt;/h4&gt;
This data set contains the measurements from the Belfort rain gauges at the BOREAS NSA andSSA. These measurements were submitted in 15-minute and 1-hour intervals. Only the 15-minute interval data set was loaded into the data base tables. Data were collected from the Belfort gauges from mid-April until mid-October in 1994, 1995, and 1996.
&lt;br&gt;&lt;h4 id&#x3D;&quot;h9rgtb94_230&quot;&gt;h9rgtb94_230&lt;/h4&gt;
The BOREAS HYD-09 team collected several data sets containing precipitation and streamflow measurements over the BOREAS study areas. This data set contains the measurements from the tipping bucket rain gauges at the BOREAS NSA and SSA. These measurements were submitted in 15-minute and 1-hour intervals. Only the 15-minute interval data set was loaded into the data base tables. Data were collected from the tipping bucket gauges from mid-April until mid-October in 1994, 1995, and 1996.
&lt;br&gt;&lt;h4 id&#x3D;&quot;boreas_aeshrday_235&quot;&gt;boreas_aeshrday_235&lt;/h4&gt;
This data set contains hourly and daily meteorological data from 23 meteorological stations across Canada from January 1975 to January 1997. The surface meteorology parameters include: date, time, temperature, precipitation, snow, snow depth, sea level pressure, station pressure, dew point, wind direction, wind speed, dry and wet bulb temperature, relative humidity, cloud opacity and cloud amount.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aes5davg_236&quot;&gt;aes5davg_236&lt;/h4&gt;
The Canadian Atmospheric Environment Service (AES) provided BOREAS with hourly and daily surface meteorological data from 23 of the AES meteorological stations located across Canada and upper air data from 1 station at The Pas, Manitoba. Due to copyright restrictions on the full resolution surface meteorological data, this data set contains 5-day average values for the surface parameters. The upper air data are provided in their full resolution form. The 5-day averaging was performed in order to create a data set that could be publicly distributed at no cost. Temporally, the surface meteorological data cover the period of January 1975 to December 1996 and the upper air data cover the period of January 1961 to November 1996.
&lt;br&gt;&lt;h4 id&#x3D;&quot;mwlezflx_493&quot;&gt;mwlezflx_493&lt;/h4&gt;
This data set contains measurements from the NOAA/ATDD Long-EZ Aircraft collected during the 1994 IFCs at the SSA. These measurements were made from various instruments mounted on the aircraft. The data that were collected include: aircraft altitude, wind direction, wind speed, air temperature, potential temperature, water mixing ratio, U and V components of wind velocity, static pressure, surface radiative temperature, downwelling and upwelling total radiation, downwelling and upwelling longwave radiation, net radiation, downwelling and upwelling PAR, greenness index, CO2 concentration, O3 concentration, and CH4 concentration. There are also various columns that indicate the standard deviation, skewness, kurtosis, and trend of some of these data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;faamwdat_237&quot;&gt;faamwdat_237&lt;/h4&gt;
The BOREAS AFM-02 team collected pass-by-pass fluxes (and many other statistics) for a large number of level (constant altitude), straight line passes used in a variety of flight patterns. The data were collected by the University of Wyoming King Air in 1994 BOREAS IFCs 1-3. Most of these data were collected at 60-70 m above ground level, but a significant number of passes were also flown at various levels in the planetary boundary layer, up to about the inversion height. This documentation concerns only the data from the straight and level passes that are presented as original (over the NSA and SSA) and moving window values (over the Transect). Another archive of King Air data is also available, containing data from all the soundings flown by the King Air 1994 IFCs 1-3.
&lt;br&gt;&lt;h4 id&#x3D;&quot;afm2as94_494&quot;&gt;afm2as94_494&lt;/h4&gt;
The BOREAS AFM-02 team used the University of Wyoming King Air aircraft during IFCs 1, 2, and 3 in 1994 to collected pass-by-pass fluxes (and many other statistics) for the large number of level (constant altitude), straight line passes used in a variety of flight patterns. The data described here form a second set, namely soundings that were incorporated into nearly every research flight by the King Air in 1994. These soundings generally went from near the surface to above the inversion layer. Most were flown immediately after takeoff or immediately after finishing the last flux pattern of that particular day&amp;#39;s flights. The parameters that were measured include wind direction, wind speed, west wind component (u), south wind component (v), static pressure, air dry bulb temperature, potential temperature, dewpoint, temperature, water vapor mixing ratio, and CO2 concentration. Data on the aircraft&amp;#39;s location, attitude, and altitude during data collection are also provided.
&lt;br&gt;&lt;h4 id&#x3D;&quot;afm3mw94_495&quot;&gt;afm3mw94_495&lt;/h4&gt;
The BOREAS AFM-03 team used the NCAR Electra aircraft data to make measurements of the fluxes of momentum, sensible and latent heat, carbon dioxide, and ozone over the entire BOREAS region to tie together measurements made in both the SSA and the NSA. These data were also used to study the planetary boundary layer using both in situ and remote sensing measurements. This data set contains both the aircraft flux and the moving window data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;afm3as94_496&quot;&gt;afm3as94_496&lt;/h4&gt;
The BOREAS AFM-03 team used the NCAR Electra aircraft to make sounding measurements to study the planetary boundary layer using in situ and remote-sensing measurements. Measurements were made of wind speed and direction, air pressure and temperature, potential temperature, dewpoint, mixing ratio of H2O, CO2 concentration, and ozone concentration. Twenty-five research missions were flown over the NSA, SSA, and the transect during BOREAS IFCs 1, 2, and 3 during 1994. All missions had from 4 to 10 soundings through the top of the planetary boundary layer. This sounding data set contains all of the in situ vertical profiles through the boundary layer top that were made (with the exception of &amp;quot;porpoise&amp;quot; maneuvers). Data were recorded in 1-second time intervals.
&lt;br&gt;&lt;h4 id&#x3D;&quot;afm4tofx_497&quot;&gt;afm4tofx_497&lt;/h4&gt;
The BOREAS AFM-04 team used the NRC Twin Otter aircraft in 1994 and 1996 to make measurements in the boundary layer of the fluxes of sensible and latent heat, momentum, ozone, methane, and carbon dioxide, plus supporting meteorological parameters such as temperature, humidity, and wind speed and direction. Aircraft position, heading, and altitude were also recorded, as were several radiometric observations for use in interpretation of the data (greenness index, surface temperature, incoming and reflected radiation). Data were collected at both the NSA and SSA during the three 1994 IFCs and in July and August of 1996.
&lt;br&gt;&lt;h4 id&#x3D;&quot;afm4toas_498&quot;&gt;afm4toas_498&lt;/h4&gt;
The BOREAS AFM-04 team used the NRC Twin Otter aircraft to make sounding measurements through the boundary layer. These measurements included concentrations of carbon dioxide and ozone, atmospheric pressure, dry bulb temperature, potential temperature, dewpoint temperature, calculated mixing ratio, and wind speed and direction. Aircraft position, heading, and altitude were also recorded. Data were collected at both the NSA and the SSA in 1994 and 1996.
&lt;br&gt;&lt;h4 id&#x3D;&quot;aes_upl1_238&quot;&gt;aes_upl1_238&lt;/h4&gt;
The BOREAS AFM-05 team collected and processed data from the numerous radiosonde flights during the project. The goals of the AFM-05 team were to provide large scale definition of the atmosphere by supplementing the existing AES aerological network, both temporally and spatially. This data set includes basic upper-air parameters collected from the network of upper-air stations during the 1993, 1994, and 1996 field campaigns over the entire study region.
&lt;br&gt;&lt;h4 id&#x3D;&quot;afm06ihd_240&quot;&gt;afm06ihd_240&lt;/h4&gt;
The BOREAS AFM-06 team from the National Oceanic and Atmospheric Administration Environment Technology Laboratory (NOAA/ETL) operated a 915 MHz wind/Radio Acoustic Sounding System (RASS) profiler system in the Southern Study Area (SSA) near the Old Jack Pine (OJP) site. This data set provides boundary layer height information over the site. The data were collected from 21-May-1994 to 20-Sep-1994.
&lt;br&gt;&lt;h4 id&#x3D;&quot;afm06ptd_241&quot;&gt;afm06ptd_241&lt;/h4&gt;
The BOREAS AFM-06 team from the National Oceanic and Atmospheric Administration Environment Technology Laboratory (NOAA/ETL) operated a 915 MHz wind/Radio Acoustic Sounding System (RASS) profiler system in the Southern Study Area (SSA) near the Old Jack Pine (OJP) tower from 21-May-1994 to 20-Sep-1994. The data set provides temperature profiles at 15 heights, containing the variables of virtual temperature, vertical velocity, the speed of sound, and w-bar.
&lt;br&gt;&lt;h4 id&#x3D;&quot;afm06pwd_242&quot;&gt;afm06pwd_242&lt;/h4&gt;
The BOREAS AFM-06 team from the National Oceanic and Atmospheric Administration Environment Technology Laboratory (NOAA/ETL) operated a 915 MHz wind/Radio Acoustic Sounding System (RASS) profiler system in the Southern Study Area (SSA) near the Old Jack Pine (OJP) tower from 21-May-1994 to 20-Sep-1994. The data set provides wind profiles at 38 heights, containing the variables of wind speed, wind direction and the u-, v-, and w-components of the total wind.
&lt;br&gt;&lt;h4 id&#x3D;&quot;afm6gifs_433&quot;&gt;afm6gifs_433&lt;/h4&gt;
The BOREAS AFM-06 team from the National Oceanic and Atmospheric Administration Environmental Technology Laboratory (NOAA/ETL) operated a 35 GHz cloud-sensing radar in the Northern Study Area (NSA) near the Old Jack Pine (OJP) tower from 16-Jul-1994 to 08-Aug-1994. This data set contains a time series of GIF (Graphical Interchange Format) images that show the structure of the lower atmosphere. Companion files include (1) an image inventory listing to inform users of the images that are available and (2)example thumbnail images.
&lt;br&gt;&lt;h4 id&#x3D;&quot;afm06smd_243&quot;&gt;afm06smd_243&lt;/h4&gt;
The BOREAS AFM-06 team from the National Oceanic and Atmospheric Administration Environment Technology Laboratory (NOAA/ETL) collected surface meteorological data from 21-May to 20-Sep-1994 near the SSA-OJP tower site.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecmwf2_523&quot;&gt;ecmwf2_523&lt;/h4&gt;
The BOREAS AFM-08 team focused on modeling efforts to improve the understanding of the diurnal evolution of the convective boundary layer over the boreal forest. This data set contains hourly data from the ECMWF operational model from below the soil surface to the top of the atmosphere, including the model fluxes at the surface. Spatially, the data cover a pair of the points that enclose the rawinsonde sites at Candle Lake, Saskatchewan, in the SSA and Thompson, Manitoba, in the NSA. Temporally, the data include the two time periods of 13-May-1994 to 30-Sept-1994 and 01-Mar-1996 to 31-Mar-1997.
&lt;br&gt;&lt;h4 id&#x3D;&quot;afm11afr_244&quot;&gt;afm11afr_244&lt;/h4&gt;
This directory contains reports from the BOREAS AFM-11 team regarding quality control and sampling analysis of data collected by other AFM personnel using the Electra, Long-EZ, and Twin Otter aircraft. These reports are stored in Adobe Acrobat (.PDF) format and should be downloaded in binary mode.
&lt;br&gt;&lt;h4 id&#x3D;&quot;avhrrlc1_434&quot;&gt;avhrrlc1_434&lt;/h4&gt;
This regional land cover classification is based on the use of multitemporal 1-km Advanced Very High Resolution Radiometer (AVHRR) National Oceanic and Atmospheric Administration (NOAA 11) data that were analyzed in combination with selected Landsat Thematic Mapper (TM) and extensive field observations within a 619-km by 821-km subset of the 1,000-km by 1,000-km BOReal Ecosystem-Atmosphere Study (BOREAS) region (Steyaert et al., 1997). Following the approach developed by Loveland et al. (1991) for 1-km AVHRR land cover mapping in the conterminous United States, monthly Normalized Difference Vegetation Index (NDVI) image composites (April-September 1992) of this subset in the BOREAS region were used in an unsupervised image cluster analysis algorithm to develop an initial set of seasonal land cover classes. Extensive ground data with Global Positioning System (GPS) georeferencing, observations from low-level aerial flights over remote areas, and selected Landsat image composites for the study areas were analyzed to split, aggregate, and label the spectral-temporal clusters throughout the BOREAS region. Landsat TM image composites (bands 5, 4, and 3) were available for the 100-km by 100-km Northern Study Area (NSA) and Southern Study Area (SSA). This AVHRR land cover product was compared with Landsat TM land cover classifications for the BOREAS study areas (Steyaert et al., 1997). Companion files include example thumbnail images that may be viewed and the image data files downloaded using a convenient viewer utility.
&lt;br&gt;&lt;h4 id&#x3D;&quot;afm13afr_245&quot;&gt;afm13afr_245&lt;/h4&gt;
For the BOReal Ecosystem-Atmosphere Study (BOREAS) in 1994 and 1996, the Airborne Fluxes and Meteorology (AFM) group was involved in measurements (from different platforms and heights within the atmospheric boundary layer) of key atmospheric variables and several surface-related parameters that can be used to describe the evolution of the atmospheric boundary layer and the boundary layer fluxes of sensible heat, latent heat, momentum, and CO2. Specifically, the AFM-13 team was interested in analysis and interpretation of airborne flux observations over a 16-km by 16-km grid site in each of the BOREAS study areas. The primary data used in the investigation were collected using the Canadian Twin Otter aircraft, one among the many research aircraft flown in BOREAS. The main objectives of the AFM-13 investigations are to use the Twin Otter-based data with tower flux data to map spatial and temporal variations in the fluxes of heat, moisture, and CO2, and to define realistic footprint functions over the BOREAS sites, so that airborne observations are related to the correct ground surface with its biological and ecological characteristics. These maps are then compared to maps of remote sensing observations over the sites. It is hoped that these studies help to develop regional scale models of fluxes of sensible heat, latent heat, and CO2 for global monitoring of climate change. This document presents a brief summary of the Twin Otter grid sites, the measured data, the type of analysis carried out, and the preliminary results from the 1994 Intensive Field Campaigns (IFCs).
&lt;br&gt;&lt;h4 id&#x3D;&quot;saskatchewan_soils_125m_ssa_1346&quot;&gt;Saskatchewan_Soils_125m_SSA_1346&lt;/h4&gt;
This data set provides soil descriptions for forested areas in the BOREAS southern study area (SSA) in central Saskatchewan, Canada provided by Agriculture Canada. The data contain soil code, modifiers, extent, and soil names for the primary, secondary, and tertiary soil units within each polygon.
&lt;br&gt;&lt;h4 id&#x3D;&quot;calibgas_500&quot;&gt;calibgas_500&lt;/h4&gt;
In order to improve the comparability of trace gas measurements made by various science teams, the BOReal Ecosystem-Atmosphere Study (BOREAS) obtained several cylinders of carbon dioxide (CO2) and methane (CH4) that were used as calibration standards. The cylinders were stored in the field laboratories established in Paddockwood, Saskatchewan (Southern Study Area) (SSA) and in Thompson, Manitoba (Northern Study Area) (NSA) from May 1994 until November 1996.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cansis_regional_soils_1347&quot;&gt;CanSIS_Regional_Soils_1347&lt;/h4&gt;
This data set contains soils data from the Canada Soil Information System (CanSIS) in ESRI Shapefile format for the provinces of Saskatchewan and Manitoba. They are provided as part of the BOReal Ecosystem-Atmosphere Study (BOREAS) Staff Science GIS data collection program. Attribute tables provide the various soil data for the polygons. There is one attribute table for Saskatchewan and one for Manitoba. This data product may be useful to someone who is interested in studying this area at a regional scale.
&lt;br&gt;&lt;h4 id&#x3D;&quot;dtms0bil_247&quot;&gt;dtms0bil_247&lt;/h4&gt;
The level-0 Daedalus TMS imagery, along with the other remotely sensed images, was collected to provide spatially extensive information about radiant energy over the primary BOREAS study areas. This information includes detailed land cover and biophysical parameter maps such as FPAR and LAI. Two flights of the Daedalus TMS instrument were made onboard the ER-2 aircraft on September 16 and 17, 1994. Companion files include (1) an image inventory listing to inform users of the images that are available and (2) example thumbnail images that may be viewed and the image data files downloaded using a convenient viewer utility.
&lt;br&gt;&lt;h4 id&#x3D;&quot;n_s_dem_248&quot;&gt;n_s_dem_248&lt;/h4&gt;
These data were derived from the original DEMs produced by the BOREAS HYD-08 team. The original DEMs were in the UTM projection, while this product is projected in the AEAC projection (see Section 7 for further projection details). The pixel size of the data is 100 meters, which is appropriate for the 1:50,000- scale contours from which the DEMs were made. The original data were compiled from information available in the 1970s and 1980s. This data set covers the two MSAs that are contained within the SSA and the NSA.
&lt;br&gt;&lt;h4 id&#x3D;&quot;srfmetmd_249&quot;&gt;srfmetmd_249&lt;/h4&gt;
In 1995, the BOREAS science teams identified the need for a continuous surface meteorological and radiation data set to support flux and surface process modeling efforts. This data set contains actual, substituted, and interpolated 15-minute meteorological and radiation data compiled from several surface measurements sites over the BOREAS SSA and NSA. Temporally, the data cover 01-Jan-1994 to 31-Dec-1996.
&lt;br&gt;&lt;h4 id&#x3D;&quot;elev_arc_250&quot;&gt;elev_arc_250&lt;/h4&gt;
This data set was prepared by BORIS staff by reformatting the original data into the ARC/INFO Generate format. The original data were received in SIF at a scale of 1:50,000. BORIS staff could not find a format document or commercial software for reading SIF; the BOREAS HYD-08 team provided some C source code that could read some of the SIF files. The data cover the BOREAS NSA and SSA. The original data were compiled from information available in the 1970s and 1980s.
&lt;br&gt;&lt;h4 id&#x3D;&quot;er2flog_501&quot;&gt;er2flog_501&lt;/h4&gt;
During 1994 and 1996, digital and analog imaging instruments mounted on the NASA ER2 aircraft collected various remotely sensed data from the atmosphere and earth?s surface as part of the BOReal Ecosystem-Atmosphere Study (BOREAS) Intensive Field Campaigns (IFC). Personnel from the NASA Earth Resources Aircraft Program within the High-altitude Aircraft Branch at NASA Ames Research Center (ARC) compiled and published logs that document the BOREAS ER2 missions. These are standard flight reports that the ARC personnel produced routinely during their tenure.
&lt;br&gt;&lt;h4 id&#x3D;&quot;bfo_dsp01_ccrs_tm_landcover_588&quot;&gt;BFO_dsp01_ccrs_tm_landcover_588&lt;/h4&gt;
The objective of this land cover mosaic is to provide a data product that characterises the detailed land cover of a significant portion of the BOREAS Region. Seven Landsat-5 TM images have been assembled to completely cover the BOREAS Transect. Entire TM scenes were used to create this land cover map. A detailed classification scheme was employed, permitting the extraction of virtually all land cover information that can be discerned from digitally enhanced TM images. The data are provided in a binary image format file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;bfo_dsp01_ccrs_avhrr_landcover_589&quot;&gt;BFO_dsp01_ccrs_avhrr_landcover_589&lt;/h4&gt;
This land cover product was produced by NBIOME to generate an up-to-date, spatially and temporally consistent land cover map of the landmass of Canada for use by scientists and other users interested in environmental information at national and regional scales. The data were acquired by CCRS and were provided to BORIS for use. This data set is gridded and was produced from 10-day composite data of surface parameters. Temporally, the 10-day compositing periods begin 11-April-95 and ends 31-Oct-95. Spatially, the data cover the entire landmass of Canada. The data are stored in binary image format files.
&lt;br&gt;&lt;h4 id&#x3D;&quot;bfo_dsp04_ers_freeze-thaw_maps_590&quot;&gt;BFO_dsp04_ers_freeze-thaw_maps_590&lt;/h4&gt;
The BOREAS DSP-4 team acquired and analyzed imaging radar data from the ESA&amp;#39;s ERS-1 over a complete annual cycle at the BOREAS sites in Canada in 1994 to detect shifts in radar backscatter related to varying environmental conditions. Two independent transitions correlating with snow melt and soil thaw onset, and possible canopy thaw were revealed by the data. The results demonstrated that radar provides an ability to observe thaw transitions at the beginning of the growing season, which in turn helps constrain the length of the growing season. The data presented here are gridded maps of landscape freeze/thaw state derived from backscatter change maps. The backscatter change maps were computed from radar backscatter images covering the southern BOREAS sites. The freeze/thaw classifications were determined through application of a change detection threshold based on temporal backscatter change relative to a winter-time frozen reference state. The data are provided as both ASCII text and as binary image (.gif) format files.
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The BOREAS DSP-5 team generated a NPP image over the BOREAS region from a process-based ecosystem model, the Boreal Ecosystem Productivity Simulator (BEPS). The NPP image was created from a series of composited AVHRR images from April 11 - September 10, 1994. This document describes how the NPP is generated . The NPP data are stored in a binary image file.
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The LAI and canopy closure images over the BOREAS conifer flux tower sites were produced at a spatial resolution of 30 m using the Forest-Light Interaction Model. The data used were obtained by the CASI instrument in high spatial resolution mode in the winter of 1994. Additional high resolution LAI and canopy closure images were produced over the two black spruce flux tower sites using the FLIM-CLUS algorithm. The data are stored in binary image format.
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This data set contains maps of surface reflectance and ve getation parameters derived from imagery collected by the POLDER instrument over BOREAS conifer tower sites in the Southern Study Area(SSA) during 1994. The POLDER imagery proficed in this data set was collected on June 1, and July 21, 1994 from the NASA C-130 aircraft platform.
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BOREAS follow-on group DSP-9 mapped surface moss type at three scales (1 km, 30 m, and 10 m) based on observed associations between moss cover and land cover type. In the BOREAS Northern (NSA) and Southern (SSA) Study Areas, we utilized land cover derived from Landsat TM (30 m) and ground measurements/observations, soils maps, and field observations to establish associations between moss and land cover. At the BOREAS regional scale, the 1 km moss cover map was developed using a 1 km AVHRR land cover map for a 619 by 821 km subset of the BOREAS region. Our regional moss cover map is largely based on inferences from the 1 km land cover analysis and from ground observations in the study areas. The 30 m moss map covers the BOREAS Southern Study Area. The 10 m map covers the BOREAS NSA Old Black Spruce tower site.
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This data set contains a pair of raster images and a spreadsheet chronicling the most recent fire history of Saskatchewan from 1945 to 1996. This data set was developed from a series of ARC/INFO export files of annual fire data that were compiled and provided by the Saskatchewan Environment and Resource Management (SERM) Wildlife Branch.
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These images were produced by aggregating a reclassified version of the 30-m land cover Thematic Mapper classification by CCRS and are now available at multiple resolutions (10x5 minutes, and 30 minutes). These data were regridded for use by the BOREAS Follow-on Carbon and Hydro-Meteorological modeling groups. Characteristics of the individual products are described in the data set guide document.
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Existing BOREAS gridded data sets were processed into projections and scales required by the Follow-on modeling teams. Existing TM and AVHRR based landcover maps, AVHRR-FPAR maps, AVHRR-LAI maps, moss cover maps, and a new peatland distribution map were regridded to scales of 2 km, 10 by 5 minute, and half-degree grids for use by the BOREAS Follow-On Carbon and Hydro-Meteorological modeling groups.
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These images were produced by aggregating the 1-km land cover classification by Lou Steyaert at multiple resolutions (2 km, 10x5 minutes, and 0.5 degree). These data were regridded for use by the BOREAS Follow-on Carbon and Hydro-Meteorological modeling groups to have a number of data sets available in common grid projections and scales for intercomparison studies. Characteristics of the individual products are described in the data set guide document.
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Existing 1-km moss cover classifications were reprocessed and are now available at multiple resolutions (2 km, 10x5 minutes, and 0.5 degree). These data were regridded for use by the BOREAS Follow-on Carbon and Hydro-Meteorological modeling groups to have a number of data sets available in common grid projections and scales for intercomparison studies. Characteristics of the individual products are described in the data set guide document.
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These images were produced by averaging the 1-km FASIR-NDVI maps by Jing Chen to a 10&amp;#39; (horizontal) by 5&amp;#39; (vertical) pixel size in a straight latitude/longitude grid. Each pixel represents the average NDVI of the 1-km pixels that fall in each 10&amp;#39; by 5&amp;#39; pixel, where more than 50% of the 1-km pixels in the 10&amp;#39; by 5&amp;#39; area are not cloud and are not missing. If more than 50% of the 1-km pixels are missing or cloudy, a value of 0 is assigned to the 10&amp;#39; by 5&amp;#39; pixel.
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These images were produced by aggregating 1&amp;#39; gridded data layers derived from the polygon-based Peatlands of Canada Database (Tarnocai et al., 2000) to 10&amp;#39; (horizontal) by 5&amp;#39; (vertical) and to 0.5 degree by 0.5 degree (or 30&amp;#39; by 30&amp;#39;) pixel sizes in straight latitude/longitude grids. See the Peatlands Map of Canada data set for more information on the original data product that this is based on.
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Existing 30-m land cover Thematic Mapper classification by CCRS was aggregated and reprocessed and are now available at multiple resolutions (10x5 minutes and 30 minutes). These data were regridded for use by the BOREAS Follow-on Carbon and Hydro-Meteorological modeling groups. Characteristics of the individual products are described in the data set guide document.
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The BOREAS Follow-On FLX-01 team derived NEE, GEE, and Respiration using measured tower C02 flux measurements taken at the NSA-OBS site. The data provided contain half-hourly measurements as well as 4 and 5 day binned data sets. The derived data covers the period from March 1994 through the end of 1998.
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The BOREAS Follow-On FLX-01 team collected tower flux, surface meteorological, and soil temperature data at the BOREAS NSA-OBS site continuously from March 1994 through December 1998. Data from March 1994 through October 1996 are included in the BOREAS TF-03 effort while data from the end of October 1996 through December 1998 are included in the BOREAS Follow-on FLX-01 effort.
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Calculations of area-averaged fluxes using extracted flux data from BORIS.
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Tower flux and meteorological data were collected above 4 black spruce forest sites in the NSA that experienced stand-replacing wildfires in 1989,1981,1964 and 1930. At each site, 4-6 weeks of data were collected during the peak growing season (June-September) in either 1999 or 2000. Fluxes were measured using paired portable solar powered eddy flux systems. The data are part of an ongoing age sequence study that will result in year round eddy flux and meteorological measurements in seven sites that burned between 2 and 150 years ago.
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The BOREAS RSS-14 team collected and processed several Level-1 GOES-7 and GOES-8 image data sets for 1994-1996, and GOES-7 Level-2 for 1994 over the BOREAS study region. This data set contains shortwave and longwave radiation images at the surface and top of the atmosphere derived from collected GOES-8 data. These GOES-8 Level-2 data cover the period from 12-Feb-1996 to 22-Oct-1996. There are images missing from the temporal series. The main difference between this data set and 1994 data set is in the spatial coverage and the grid cell size.
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A gridded data set has been assembled over the BOREAS hydro-meteorological study region that combines a precipitation data set based on a rain gauge network with precipitation estimates based on SSM/I satellite images. The result is an hourly precipitation data set covering 122 consecutive days beginning on June 1, 1996.
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Phase II and III gridded data sets have been generated by an objective analysis scheme using all of the surface meteorological station data over BOREAS region for 1994-1996. Additionally, FSU GOES incoming solar radiation retrievals and BOREAS rain radar retrievals during portions of 1994 and 1996 were used when remote sensing products were available. Two Phase II, Northern Study Area (NSA) and Southern Study Area (SSA) grids, and one Phase III, Regional, gridded data sets have been assembled on a HOURLY time step. The meteorological variables in this data set are surface air pressure, air temperature, dew point temperature, wind speed, wind direction, precipitation, incoming solar (shortwave) radiation, and incoming infrared (longwave) radiation.
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Point data developed from in situ observations at four flux tower sites were combined to produce continuous, above the canopy, meteorological forcing data sets. Data from the OA and OBS sites in the SSA and the Fen and OBS sites in the NSA were used to create continuous time series with a time step of one hour, covering the period from 1-Jan-1994 through 1-Dec-1996. Meteorological variables of interest are surface air pressure, air temperature, dew point temperature, wind speed, wind direction, precipitation, incoming solar (shortwave) radiation, and incoming infrared (longwave) radiation.
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As part of the BOREAS Follow-on, an extended period of data collection was supported in the NSA because of the continued efforts at the NSA-OBS site. This data set contains near-surface meteorological data collected and averaged over 15 minute intervals from two sites in the NSA, the SRC tower at the Thompson airport (YTH) and a temporary walkup wooden tower at the Old Black Spruce (OBS) tower site.
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The Phase 3 gridded data sets provided by HMet-01 on an hourly time step have been converted to averaged daily files by the MOD-01 group to reduce the size and number of files used for input to some of the carbon models.
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This data set was prepared by BORIS staff by processing the original vector data into raster files. The original data were received as ARC/INFO coverages or as export files from SERM. The data include information on forest parameters for the BOREAS SSA MSA. The data are stored in binary, image format files.
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This data set was processed by BORIS staff from the original vector data of species, crown closure, cutting class, and site classification/subtype into raster files. The original polygon data were received from Linnet Graphics, the distributor of data for MNR. In the case of the species layer, the percentages of species composition were removed. This reduced the amount of information contained in the species layer of the gridded product, but it was necessary in order to make the gridded product easier to use. The original maps were produced from 1:15,840-scale aerial photography collected in 1988.
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The BOREAS HYD-01 team made several measurements related to soil moisture and soil properties. These soil hydraulic properties were determined at the flux tower sites based on analysis of in situ tension infiltrometer tests and laboratory determined water retention from soil cores collected during the 1994-95 field campaigns. Results from this analysis are saturated hydraulic conductivity, and fitting parameters for the van Genuchten-Mualem soil hydraulic conductivity and water retention function at flux tower sites.
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Under-canopy precipitation measurements were made by the BOREAS HYD-01 science team in 1994, 1995, and 1996 at various flux tower sites in the NSA and SSA. In 1994, these data were collected at the NSA-OJP, NSA-YJP, SSA-OJP, and SSA-YJP sites. Starting in 1995 and ending in 1997, data were collected at the NSA-OBS, NSA-OJP, NSA-YJP, and SSA-OA. These data were collected to support HYD-01 research by measuring the amount of water that falls through the canopy and is intercepted by the ground or moss. These data coincide with volumetric soil moisture measurements made by HYD-01.
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The BOREAS HYD-01 team made measurements of volumetric soil moisture at the SSA and NSA tower flux sites in 1994 and at selected tower flux sites in 1995-97. Different methods were used to collect these measurements, including neutron probe and manual and automated TDR. In 1994, the measurements were made every other day at the NSA-OJP, NSA-YJP, NSA-OBS, NSA-Fen, SSA-OJP, SSA-YJP, SSA-Fen, SSA-YA, and SSA-OBS sites. In 1995-97, when automated equipment was deployed at NSA-OJP, NSA-YJP, NSA-OBS, SSA-OBS, and SSA-OA, the measurements were made as often as every hour.
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The surface meteorological data collected at the BOREAS tower and ancillary sites are being used as inputs to an energy balance model to monitor the amount of snow storage in the boreal forest region. The BOREAS HYD-02 team used snow water equivalent (SWE) derived from an energy balance model and in situ observed SWE to compare the SWE inferred from airborne and spaceborne microwave data, and to assess the accuracy of microwave retrieval algorithms. The major external measurements that are needed are snowpack temperature profiles, and in situ snow areal extent and snow water equivalent data. The data in this data set were collected during February 1994 and cover portions of the SSA, NSA, and the transect areas.
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The BOREAS HYD-03 team collected several data sets related to the hydrology of forested areas. This data set contains measurements of stem density from a variety of sites. Stem density measurements were made during the FFC-W 1996 in the SSA only using standard techniques. This study was undertaken to predict spatial distributions of energy transfer, snow properties important to the hydrology, remote sensing signatures, and transmissivity of gases through the snow and their relation to forests in boreal ecosystems.
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The BOREAS HYD-03 team collected several data sets related to the hydrology of forested areas. This data set contains measurements of canopy density (closure) from a variety of sites. Canopy density measurements were made during the FFC-W and FFC-T 1994 in both the SSA and NSA using a forest densiometer. This study was undertaken to predict spatial distributions of energy transfer, snow properties important to the hydrology, remote sensing signatures, and transmissivity of gases through the snow and their relation to forests in boreal ecosystems.
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The BOREAS HYD-03 team collected several data sets related to the hydrology of forested areas. This data set contains measurements of snow depth, snow density in 3-cm intervals, an integrated snow pack density and snow water equivalent (SWE), and snow pack physical properties from snow pit evaluation taken in 1994 and 1996. The data were collected from several sites in both the SSA and the NSA. A variety of standard tools were used to measure the snowpack properties, including a meter stick (snow depth), a 100 cc snow density cutter, a dial stem thermometer and the Canadian snow sampler as used by HYD-04 to obtain a snow pack-integrated measure of SWE. This study was undertaken to predict spatial distributions of snow properties important to the hydrology, remote sensing signatures, and the transmissivity of gases through the snow.
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The BOREAS HYD-03 team collected several data sets related to the hydrology of forested areas. This data set contains measurements of tree diameter at breast height (DBH) from a variety of sites. This study was undertaken to predict spatial distributions of energy transfer, snow properties important to the hydrology, remote sensing signatures, and transmissivity of gases through the snow and their relation to forests in boreal ecosystems.
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The BOREAS HYD-03 team collected several data sets related to the hydrology of forested areas. This data set includes measurements of wind speed and direction; air temperature; relative humidity; and canopy, trunk, and snow surface temperatures within three forest types. The data were collected in the SSA-OJP (1994) and SSA-OBS and SSA-OA (1996). Measurements were taken for 3 days in 1994 and 4 days at each site in 1996. These measurements were intended to be short term to allow the relationship between subcanopy measurements and those collected above the forest canopy to be determined. The subcanopy estimates of wind speed were used in a snow melt model to help predict the timing of snow ablation.
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The BOREAS HYD-03 team collected several data sets related to the hydrology of forested areas. This data set contains solar radiation measurements from several pyranometers (solar radiometers) placed on the snow surface in jack pine (1994) and black spruce and aspen forests (1996). An array of radiometers was used to collect data for 3-4 consecutive days in each forest type to study the hypothesis that energy transfer and snow water equivalent would vary spatially as a function of canopy closure. The quality of the data is good, because the days were generally clear and the radiometers were checked daily to remove anything that landed on the radiometers.
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The BOREAS HYD-04 work was focused on collecting data during the winter field campaign (FFC-W) to improve the understanding of winter processes within the boreal forest. Airborne remote sensing data (gamma, passive microwave) were acquired along a series of flight lines established in the vicinity of the BOREAS study areas. Ground snow surveys were conducted along selected sections of these aircraft flight lines. These calibration segments were typically 10-20 km in length, and ground data were collected at 1- to 2-km intervals. The development and validation of remote sensing algorithms will provide the means to extend the knowledge of these processes and states from the local to the regional scale.
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The BOREAS HYD-04 work was focused on collecting data during the winter field campaign (FFC-W) to improve the understanding of winter processes within the boreal forest. Snow surveys were conducted at special snow courses throughout the 1993/94, 1994/95, 1995/96, and 1996/97 winter seasons. These snow courses were located in different boreal forest land cover types (i.e., old aspen, old black spruce, young jack pine, forest clearing, etc.) to document snow cover variations throughout the season as a function of different land cover. Measurements of snow depth, density, and water equivalent were acquired on or near the first and fifteenth of each month during the snow cover season. The development and validation of remote sensing algorithms will provide the means to extend the knowledge of these processes and states from the local to the regional scale. A specific thrust of the research is the development and validation of snow cover algorithms from airborne passive microwave measurements.
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The BOREAS HYD-05 team collected tower flux, surface meteorological, and surface temperature data on a frozen lake (Namekus Lake) and in a mature jack pine forest in the Beartrap Creek watershed. Both sites were located in the BOREAS SSA. The objective of this study was to characterize the winter energy and water vapor fluxes, as well as related properties (such as snow density, depth, temperature, and melt) for forested and nonforested areas of the boreal forest. Data were collected on Namekus Lake in the winters of 1994 and 1996, and at Beartrap Creek in the winter of 1994 only.
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This data set contains percent soil moisture (by weight) (and/or water content if there is a moss/humus layers measured from aircraft using a terrestrial gamma ray instrument. There is also data that indicates the location of the aircraft at the time it collected the terrestrial gamma ray data for the various flight lines and bins. The location information contains a list of coordinates that indicate the path of the aircraft for each bin. The data were collected during four time periods from September 1993 to September 1994 over the Southern Study Area (SSA) and two time periods from February to August 1994 over the Northern Study Area (NSA).
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This data set contains percent soil moisture ground measurements. These data were collected on the ground along the various flight lines flown in the Southern and Northern Study Areas (SSA and NSA) during 1994 by the gamma ray instrument. This data set contains information on the locations of field in-site measurements of soil moisture, depth of moss/humus layer, and water content of the moss/humus layer and contains information on soil conditions and vegetative cover around the sites.
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This data set contains water content measurements of the moss/humus layer, where it existed. These data were collected along various flight lines in the Southern and Northern Study Areas (SSA and NSA) during 1994.
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The BOREAS HYD-08 team made measurements of surface hydrological processes that were collected at the NSA OBS Tower Flux site in 1994 and at Joey Lake, Manitoba, to support their research into point hydrological processes and the spatial variation of these processes. The data collected may be useful in characterizing canopy interception, drip, throughfall, moss interception, drainage, evaporation, and capacity during the growing season at daily temporal resolution. This particular data set contains the gravimetric moss moisture measurements from June to September 1994. A nested spatial sampling plan was implemented to support research into spatial variations of the measured hydrological processes and ultimately the impact of these variations on modeled carbon and water budgets.
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The BOREAS HYD-08 team made measurements of surface hydrological processes that were collected at the SSA-OBS Tower Flux site in 1996 to support its research into point hydrological processes and the spatial variation of these processes. Data collected may be useful in characterizing canopy interception, drip, throughfall, moss interception, drainage, evaporation, and capacity during the growing season at daily temporal resolution. This particular data set contains the gravimetric moss moisture measurements from July to August 1996. To collect these data, a nested spatial sampling plan was implemented to support research into spatial variations of the measured hydrological processes and ultimately the impact of these variations on modeled carbon and water budgets.
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The BOREAS HYD-08 team made measurements of surface hydrological processes at the SSA-OBS Tower Flux site to support its research into point hydrological processes and the spatial variation of these processes. Data collected may be useful in characterizing canopy interception, drip, throughfall, moss interception, drainage, evaporation, and capacity during the growing season at daily temporal resolution. This particular data set contains the gross precipitation measurements for July to August 1996. Gross precipitation is the precipitation that falls that is not intercepted by tree canopies.
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These DEMs were produced from digitized contours at a cell resolution of 100 meters. Vector contours of the area were used as input to a software package that interpolates between contours to create a DEM representing the terrain surface. The vector contours had a contour interval of 25 feet. The data cover the BOREAS MSAs of the SSA and NSA and are given in a UTM map projection.
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The BOREAS HYD-08 team made measurements of surface hydrological processes at the SSA (1996) and NSA OBS (1994) Tower Flux sites, supporting its research into point hydrological processes and the spatial variation of these processes. These data were collected during the 1994 and 1996 field campaigns. Data collected may be useful in characterizing canopy interception, drip, throughfall, moss interception, drainage, evaporation, and capacity during the growing season at daily temporal resolution. This particular data set contains the measurements of throughfall, which is the amount of precipitation that fell through the canopy. A nested spatial sampling plan was implemented to determine spatial variations of the measured hydrological processes and ultimately the impact of these variations on modeled carbon and water budgets.
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The BOREAS HYD-09 team collected data on precipitation and streamflow over portions of the NSA and SSA. This data set contains Cartesian maps of rain accumulation for 1-hour and daily periods during the summer of 1994 over the SSA only (not the full view of the radar). A parallel set of 1-hour maps for the whole radar view has been prepared and is available upon request from the HYD-09 personnel. An incidental benefit of the areal selection was the elimination of some of the less accurate data, because for various reasons the radar rain estimates degrade considerably outside a range of about 100 km. The data are available in tabular ASCII files.
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These streamflow data were collected by the HYD-09 science team to support its research into meltwater supply to the soil during the spring melt period. These data were also collected for HYD-09&amp;#39;s research into the evolution of soil moisture, evaporation, and runoff from the end of the snowmelt period through freeze up. Data were collected in the BOREAS SSA and NSA from April until October in 1994, 1995, and 1996. Gauges SW1 and NW1 were operated year-round; however, data may not be available for both gauges for all 3 years.
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The Earth Resources Technology Satellite (ERTS) Program launched the first of a series of satellites (ERTS-1) in 1972. Part of the NASA Earth Resources Survey Program, the ERTS Program and the ERTS satellites were later renamed Landsat to better represent the civil satellite program&amp;#39;s prime emphasis on remote sensing of land resources. Landsat satellites 1 through 5 carry the MSS sensor. CCRS and BOREAS personnel gathered a set of MSS images from Landsat satellites 1, 2, 4 and 5 covering the dates of 21-Aug-1972 to 05-Sep-1988. The data are provided in binary image format files. Companion files include (1) an image inventory listing to inform users of the images that are available and (2) example thumbnail images that may be viewed and the image data files downloaded using a convenient viewer utility.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ltm_ii3a_280&quot;&gt;ltm_ii3a_280&lt;/h4&gt;
For BOREAS, the level-3a Landsat TM data, along with the other remotely sensed images, were collected in order to provide spatially extensive information over the primary study areas. This information includes radiant energy, detailed land cover, and biophysical parameter maps such as FPAR and LAI. Although very similar in content to the level-3s Landsat TM products, the level-3a images were created to provide users with a more usable BSQ format and to provide information that permitted direct determination of per-pixel latitude and longitude coordinates. Geographically, the level-3a images cover the BOREAS NSA and SSA. Temporally, the images cover the period of 22-Jun-1984 to 30-Jul-1996. The images are available in binary, image-format files. Companion files include (1) an image inventory listing to inform users of the images that are available and (2) example thumbnail images that may be viewed and the image data files downloaded using a convenient viewer utility.
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For BOREAS, the level-3b Landsat TM data, along with the other remotely sensed images, were collected in order to provide spatially extensive information over the primary study areas. This information includes radiant energy, detailed land cover, and biophysical parameter maps such as FPAR and LAI. Although very similar in content to the level-3a Landsat TM products, the level-3b images were created to provide users with a directly usable at-sensor radiance image. Geographically, the level-3b images cover the BOREAS NSA and SSA. Temporally, the images cover the period of 22-Jun-1984 to 30-Jul-1996. Companion files include (1) an image inventory listing to inform users of the images that are available and (2) example thumbnail images that may be viewed using a convenient viewer utility.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ltm_ii3p_426&quot;&gt;ltm_ii3p_426&lt;/h4&gt;
For BOREAS, the level-3p Landsat TM data were used to supplement the level-3s Landsat TM products. Along with the other remotely sensed images, the Landsat TM images were collected in order to provide spatially extensive information over the primary study areas. This information includes radiant energy, detailed land cover, and biophysical parameter maps such as FPAR and LAI. Although very similar to the level-3s Landsat TM products, the level-3p images were processed with ground control information which improved the accuracy of the geographic coordinates provided. Geographically, the level-3p images cover the BOREAS NSA and SSA. Temporally, the four images cover the period of 20-Aug-1988 to 07-Jun-1994. Except for the 07-Jun-1994 image which contains 7 bands, the other three only contain 3 bands. Companion files include (1)an image inventory listing to inform users of the images that are available and (2) example thumbnail images that may be viewed using a convenient viewer utility.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ltm_ii3s_427&quot;&gt;ltm_ii3s_427&lt;/h4&gt;
For BOREAS, the level-3s Landsat TM data, along with the other remotely sensed images, were collected in order to provide spatially extensive information over the primary study areas. This information includes radiant energy, detailed land cover, and biophysical parameter maps such as FPAR and LAI. CCRS collected and supplied the level-3s images to BOREAS for use in the remote sensing research activities. Geographically, the bulk of the level-3s images cover the BOREAS NSA and SSA with a few images covering the area between the NSA and SSA. Temporally, the images cover the period of 22-Jun-1984 to 30-Jul-1996. Companion files include (1) an image inventory listing to inform users of the images that are available and (2) example thumbnail images that may be viewed using a convenient viewer utility.
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The level-0 AOCI imagery, along with the other remotely sensed images, was collected to provide spatially extensive information about radiant energy over the primary BOREAS study areas. The AOCI was the only remote sensing instrument flown with wavelength bands specific to the investigation of various aquatic parameters such as chlorophyll content and turbidity. Only one flight of the AOCI instrument was made onboard the ER-2 aircraft on 21-Jul-1994 over the SSA. Companion files include (1) an image inventory listing to inform users of the images that are available and (2) example thumbnail images that may be viewed and the image data files downloaded using a convenient viewer utility.
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For BOREAS, the TIMS imagery, along with the other remotely sensed images, was collected to provide spatially extensive information over the primary study areas. The level-0 TIMS images cover the time periods of 16-Apr-1994 to 20-Apr-1994 and 06-Sep-1994 to 17-Sep-1994. The images are available in their original uncalibrated format. Companion files include (1) an image inventory listing to inform users of the images that are available and (2) example thumbnail images that may be viewed and the image data files downloaded using a convenient viewer utility.
&lt;br&gt;&lt;h4 id&#x3D;&quot;maslv1b_560&quot;&gt;maslv1b_560&lt;/h4&gt;
For BOREAS, the MAS images, along with the other remotely sensed data, were collected to provide spatially-extensive information over the primary study areas. This information includes detailed land cover and biophysical parameter maps such as fPAR (fraction of Photosynthetically Active Radiation), and LAI (Leaf Area Index). Collection of the MAS images occurred over the study areas during the 1994 field campaigns. The level-1B MAS data cover the dates of 21-Jul-1994, 24-Jul-1994, 04-Aug-1994 and 08-Aug-1994. The data are not geographically/geometrically corrected; however, files of relative X and Y coordinates for each image pixel were derived by using the C130 INS data in a MAS scan model.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tims1bsq_436&quot;&gt;tims1bsq_436&lt;/h4&gt;
The BOREAS Staff Science Aircraft Data Acquisition Program focused on providing the research teams with the remotely sensed satellite data products they needed to compare and spatially extend point results. For BOREAS, the TIMS imagery, along with other aircraft images, was collected to provide spatially extensive information over the primary study areas. The level-1B TIMS images cover the time periods of 16-Apr-1994 to 20-Apr-1994 and 06-Sep-1994 to 17-Sep-1994. The system calibrated images are stored in binary image format files. Companion files include (1) an image inventory listing to inform users of the images that are available and (2) example thumbnail images.
&lt;br&gt;&lt;h4 id&#x3D;&quot;mas_lv2_561&quot;&gt;mas_lv2_561&lt;/h4&gt;
The BOREAS Staff Science Aircraft Data Acquisition Program focused on providing the research teams with the remotely sensed aircraft data products they needed to compare and spatially extend point results. The MAS images, along with other remotely sensed data, were collected to provide spatially extensive information over the primary study areas. This information includes biophysical parameter maps such as surface reflectance and temperature. Collection of the MAS images occurred over the study areas during the 1994 field campaigns. The level-2 MAS data cover the dates of 21-Jul-1994, 24-Jul-1994, 04-Aug-1994 and 08-Aug-1994. The data are not geographically/geometrically corrected; however, files of relative X and Y coordinates for each image pixel were derived by using the C130 navigation data in a MAS scan model. The data are provided in binary image format files.
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The BOREAS Staff Science Satellite Data Acquisition Program focused on providing the research teams with the remotely sensed satellite data products they needed to compare and spatially extend point results. Data acquired from the AVHRR instrument on the NOAA-9, -11, -12, and -14 satellites were processed and archived for the BOREAS region by the MRSC and BORIS. The data were acquired by CCRS and were provided for use by BOREAS researchers. A few winter acquisitions are available, but the archive contains primarily growing season imagery. These gridded, at-sensor radiance image data cover the period of 30-Jan-1994 to 18-Sep-1996. Geographically, the data cover the entire 1000 km x 1000 km BOREAS Region. The data are stored in binary image format files.
&lt;br&gt;&lt;h4 id&#x3D;&quot;spot_3s_437&quot;&gt;spot_3s_437&lt;/h4&gt;
For BOREAS, the level-3s SPOT data, along with the other remotely sensed images, were collected in order to provide spatially extensive information over the primary study areas. This information includes radiant energy, detailed land cover, and biophysical parameter maps such as FPAR and LAI. The SPOT images acquired for the BOREAS project were selected primarily to fill temporal gaps in the Landsat TM image data collection. CCRS collected and supplied the level-3s images to BORIS for use in the remote sensing research activities. Spatially, the level-3s images cover 60-by 60-km portions of the BOREAS NSA and SSA. Temporally, the images cover the period of 17-Apr-1994 to 30-Aug-1996. The images are available in binary image format files. Companion files include (1) an image inventory listing to inform users of the images that are available and (2) example thumbnail images.
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The BOREAS Staff Science Satellite Data Acquisition Program focused on providing the research teams with the remotely sensed satellite data products they needed to compare and spatially extend point results. MRSC and BORIS personnel acquired, processed, and archived data from the AVHRR instruments on the NOAA-11 and -14 satellites. The AVHRR data were acquired by CCRS and were provided to BORIS for use by BOREAS researchers. These AVHRR level-4b data are gridded, 10-day composites of at-sensor radiance values produced from sets of single-day images. Temporally, the 10-day compositing periods begin 11-Apr-1994 and end 10-Sep-1994. Spatially, the data cover the entire BOREAS region. The data are stored in binary image format files. Companion files include example thumbnail images that may be viewed and the image data files downloaded using a convenient viewer utility.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ns001bil_440&quot;&gt;ns001bil_440&lt;/h4&gt;
For BOREAS, the NS001 TMS imagery, along with the other remotely sensed images, was collected in order to provide spatially extensive information over the primary study areas. This information includes detailed land cover and biophysical parameter maps such as fPAR and LAI. Data collections occurred over the study areas during the 1994 field campaigns.Companion files include (1) an image inventory listing to inform users of the images that are available and (2) example thumbnail images.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ns0012bq_482&quot;&gt;ns0012bq_482&lt;/h4&gt;
For BOREAS, the NS001 TMS images, along with the other remotely sensed data, were collected to provide spatially extensive information over the primary study areas. This information includes detailed land cover and biophysical parameter maps such as fPAR and LAI. Collection of the NS001 images occurred over the study areas during the 1994 field campaigns. The Level-2 NS001 data are atmospherically corrected versions of some of the best original NS001 imagery and cover the dates of 19-Apr-1994, 07-Jun-1994, 21-Jul-1994, 08-Aug-1994, and 16-Sep-1994. The data are not geographically/geometrically corrected; however, files of relative X and Y coordinates for each image pixel were derived by using the C130 INS data in an NS001 scan model. The data are provided in binary image format files. Note also that the top portion of the ASCII header file in each Level-2 NS001 image product indicates that the band 8 data are &amp;#39;Scaled Reflectance&amp;#39; when in fact they are &amp;#39;Scaled Temperatures.
&lt;br&gt;&lt;h4 id&#x3D;&quot;panpfcov_283&quot;&gt;panpfcov_283&lt;/h4&gt;
This data set provides detailed canopy, understory, and ground cover, height, density, and condition information for PANP in the western portion of the BOREAS SSA in vector form.
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This data set is based on the GTOPO30 DEM produced by the USGS EDC. The BOREAS region (1,000km x 1000km) was extracted from the GTOPO30 data and reprojected by BOREAS staff into the AEAC projection. The pixel size of these data is 1 km.
&lt;br&gt;&lt;h4 id&#x3D;&quot;regsoilr_285&quot;&gt;regsoilr_285&lt;/h4&gt;
This data set was gridded by BORIS staff from a vector data set received from Canadian Soil Information System (CanSIS). The original data came in two parts that covered Saskatchewan and Manitoba. The data were gridded and merged into one data set of 84 files covering the BOReal Ecosystem-Atmosphere Study (BOREAS) region. The data were gridded into the Albers Equal-Area Conic (AEAC) projection. Because the mapping of the two provinces was done separately in the original vector data, there may be discontinuities in some of the soil layers because of different interpretations of certain soil properties.
&lt;br&gt;&lt;h4 id&#x3D;&quot;rss1para_286&quot;&gt;rss1para_286&lt;/h4&gt;
The BOREAS RSS-01 team collected surface reflectance and transmittance data from three forested sites in the SSA. This data set contains averaged reflectance factors and transmitted radiances measured by the PARABOLA instrument at selected sites in the BOREAS SSA at different view angles and at three wavelength bands throughout the day. PARABOLA measurements were made during each of the three BOREAS IFCs during the growing season of 1994 at three SSA tower flux sites as well as during the FFC-T. Additional measurements were made in early and mid-1996 during the FFC-W and during IFC-2.
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Atmospherically-corrected bidirectional reflectance factor means for small homogeneous areas from several BOREAS sites were derived from multi-spectral, multi-angle imagery acquired by the Advanced Solidstate Array Spectroradiometer (ASAS) aboard the C-130 aircraft platform in 1994 and 1996.
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The BOREAS RSS-02 team used the ASAS instrument, mounted on the NASA C-130 aircraft, to create at-sensor radiance images of various sites as a function of spectral wavelength, view geometry (combinations of view zenith angle, view azimuth angle, solar zenith angle, and solar azimuth angle), and altitude. The level-1b ASAS images of the BOREAS study areas were collected from April to September 1994 and March to July 1996. The data are provided in binary image format files.
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The BOREAS RSS-03 team collected and processed helicopter-based measurements of atmospheric conditions to estimates of aerosol optical thickness and atmospheric water vapor. The automatic sun-tracking photometer for helicopters was deployed during all three IFC&amp;#39;s of 1994 at numerous tower and auxiliary sites in both the NSA and SSA. Seven spectral channels (440, 540, 613, 670, 870 and 1030 am) were chosen to span the visible and NIR wavelengths and to avoid gaseous absorption. One additional channel, 940 nm, was selected to measure the water column abundance above the helicopter platform.
&lt;br&gt;&lt;h4 id&#x3D;&quot;boreas_rss-03_snapshots_289&quot;&gt;BOREAS_RSS-03_Snapshots_289&lt;/h4&gt;
This data set provides images of boreal forests in central Canada collected over numerous tower and auxiliary sites during the BOREAS Intensive Field Campaigns (IFCs) in the Northern (NSA) and Southern Study Areas (SSA). The images were acquired by helicopter with VHS video cameras during the green-up, peak, and senescent stages of the growing season from May-September of 1994. These snapshots were generated from VHS imagery and converted to .jpg format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;rss3hmmr_290&quot;&gt;rss3hmmr_290&lt;/h4&gt;
The RSS-03 team acquired helicopter-based measurements of forested sites during BOREAS with a Barnes MMR. The data were collected in 1994 during the rhree BOREAS IFCs at numerous tower and auxiliary sites in both the NSA and SSA. The 15-degree FOV of the MMR yielded approximately 79 m from the 300 m altitude ground resolution. The MMR has seven spectral bands that are similar to the Landsat TM bands, ranging from the blue region to the thermal. Note:
&lt;br&gt;&lt;h4 id&#x3D;&quot;rs3se590_291&quot;&gt;rs3se590_291&lt;/h4&gt;
The BOREAS RSS-03 team collected multiple remotely sensed data sets from the NASA UH-1 helicopter. This data set includes helicopter-based radiometric measurements of forested sites acquired during BOREAS made with an SE-590 processed to reflectance factors. The data used in this analysis were collected in 1994 during the three BOREAS IFCs at numerous tower and auxiliary sites in both the NSA and the SSA. The 15-degree FOV of the SE-590 yielded a ground resolution of approximately 79 m at the 300-m nominal altitude.
&lt;br&gt;&lt;h4 id&#x3D;&quot;rss4lib_292&quot;&gt;rss4lib_292&lt;/h4&gt;
The BOREAS RSS-04 team focused its efforts on deriving estimates of LAI and leaf chlorophyll and nitrogen concentrations from remotely sensed data for input into the Forest BGC model. This data set contains measurements of jack pine (Pinus banksiana) needle biochemistry from the BOREAS SSA in July and August 1994. The data contain measurements of current and year-1 needle chlorophyll, nitrogen, lignin, cellulose, and water content for the OJP flux tower and nearby auxiliary sites. The data have been used to test a needle reflectance and transmittance model, LIBERTY (Dawson et al., in press). The source code for the model and modeled needle spectra for each of the sampled tower and auxiliary sites are provided as part of this data set. The LIBERTY model was developed and the predicted spectral data generated to parameterize a canopy reflectance model (North, 1996) for comparison with AVIRIS, POLDER, and PARABOLA data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;r04laifd_293&quot;&gt;r04laifd_293&lt;/h4&gt;
The RSS-04 team collected several data sets related to leaf, plant, and stand physical, optical, and chemical properties. This data set contains leaf area indices and FPAR measurements which were taken at the three conifer sites in the BOREAS SSA during August 1993 and at the jack pine tower flux and a subset of auxiliary sites during July and August 1994. The measurements were made with LAI-2000 and Ceptometer instruments. The measurements were taken for the purpose of model parameterization and to test empirical relationships that were hypothesized between biophysical parameters and remotely sensed data.
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The BOREAS RSS-07 team collected various data sets to develop and validate an algorithm to allow the retrieval of the spatial distribution of LAI from remotely sensed images. Ground measurements of LAI and FPAR absorbed by the plant canopy were made using the LAI-2000 and TRAC optical instruments during focused periods from 09-AUG-1993 to 19-SEP-1994. The measurements were intensive at the NSA and SSA tower sites, but were made just once or twice at auxiliary sites.
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The BOREAS RSS-07 team used Landsat TM images processed at CCRS to produce images of LAI for the BOREAS study areas. Two images acquired on June 6 and August 9, 1991 were used for the SSA, and one image acquired on June 9, 1994 was used for the NSA. The LAI images are based on ground measurements and Landsat TM RSR images. The data are stored in binary image-format files. Companion files include example thumbnail images that may be viewed and the image data files downloaded using a convenient viewer utility.
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The BOREAS RSS-07 team focused their efforts on developing and validating procedures and algorithms that would allow the retrieval of LAI from remotely sensed vegetation indices. This data set contains images of LAI and FPAR that were produced from the AVHRR Level-4c ten-day composite NDVI images produced at CCRS for the three summer IFCs in 1994. The algorithms were developed based on ground measurements and Landsat TM images (Chen and Cihlar, 1996; Chen, 1996b). The data are provided in binary image format files. Companion files include example thumbnail images that may be viewed and the image data files downloaded using a convenient viewer utility.
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BIOME-BGC is a general ecosystem process model designed to simulate biogeochemical and hydrologic processes across multiple scales (Running and Hunt, 1993). In this investigation, BIOME-BGC was used to estimate daily water and carbon budgets for the BOREAS tower flux sites for 1994. Carbon variables estimated by the model include gross primary production (i.e., net photosynthesis), maintenance and heterotrophic respiration, net primary production, and net ecosystem carbon exchange. Hydrologic variables estimated by the model include snowcover, evaporation, transpiration, evapotranspiration, soil moisture, and outflow. The information provided by the investigation includes input initialization and model output files for various sites in tabular ASCII format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;biomebg2_296&quot;&gt;biomebg2_296&lt;/h4&gt;
The BOREAS RSS-08 team performed research to evaluate the effect of seasonal weather and landcover heterogeneity on boreal forest regional water and carbon fluxes using a process level ecosystem model, BIOME-BGC, coupled with remote sensing-derived parameter maps of key state variables. This data set contains derived maps of landcover type and crown and stem biomass as model inputs to determine annual evapotranspiration, gross primary production, autotrophic respiration and net primary productivity within the BOREAS SSA-MSA, at a 30 m spatial resolution. Model runs were conducted over a 3 year period from 1994-1996, images are provided for each of those years.
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Ground BRDF measurements were acquired by the Remote Sensing Science (RSS)-08 team to aid in the development of advanced spectral vegetation indices. The RSS-08 team measured reflectances at the double-scaffold towers in the Southern Study Area (SSA) Old Black Spruce (OBS) and Old Aspen (OA) sites during IFC-3 in 1994. The RSS-08 team also acquired stereo photography at the SSA-OA, SSA-OJP, and SSA-OBS sites during IFC-3.
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The BOREAS RSS-08 team utilized Landsat TM images to perform mapping of snow extent over the SSA. This data set consists of two Landsat TM images which were used to determine the snow-covered pixels over the BOREAS SSA on 18-Jan-1993 and on 06-Feb-1994. Companion files include example thumbnail images that may be viewed using a convenient viewer utility.
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The RSS08 team acquired stereo photography from the double-scaffold towers at the Southern Study Area (SSA) Old Black Spruce (OBS), Old Aspen (OA), and Old Jack Pine (OJP) sites during IFC-3 in 1994. The imagery of the canopy was taken from various perspectives. The RSS08 team also measured BRDF at the SSA-OA and -OBS sites during IFC-3.
&lt;br&gt;&lt;h4 id&#x3D;&quot;rss10tom_443&quot;&gt;rss10tom_443&lt;/h4&gt;
The BOREAS RSS-10 team investigated the magnitude of daily, seasonal, and yearly variations of PAR from ground and satellite observations. This data set contains satellite estimates of surface-incident photosynthetically active radiation (PAR, 400-700 nm, MJ m-2) at 1 degree spatial resolution. The spatial coverage is circumpolar from latitudes of 41 to 66 degrees N latitude. The temporal coverage is from May through September for years 1979 through 1989. Eleven-year statistics are also provided: mean, standard deviation, and coefficient of variation for 1979-1989. The PAR estimates were derived from the global gridded ultraviolet reflectivity data product (average of 360, 380 nm) from the Nimbus-7 Total Ozone Mapping Spectrometer (TOMS). Image mask data are provided for identifying the boreal forest zone, and ocean/land and snow/ice covered areas. The data are available as binary image format data files. Companion files include example thumbnail images that may be viewed and the image data files downloaded using a convenient viewer utility.
&lt;br&gt;&lt;h4 id&#x3D;&quot;r11sunpd_297&quot;&gt;r11sunpd_297&lt;/h4&gt;
The BOREAS RSS-11 team operated a network of five automated (Cimel) and two hand-held (Miami) solar radiometers from 1994 to 1996 during the BOREAS field campaigns. The data provide aerosol optical depth measurements, size distribution, phase function, and column water vapor amounts over points in northern Saskatchewan and Manitoba, Canada. The data are useful for the correction of remotely sensed aircraft and satellite images. The data are provided in tabular ASCII files.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sunphair_298&quot;&gt;sunphair_298&lt;/h4&gt;
The BOREAS RSS-12 team collected both ground and airborne sunphotometer measurements for use in characterizing the aerosol optical properties of the atmosphere during the BOREAS data collection activities. These measurements are to be used to: 1) measure the magnitude and variability of the aerosol optical depth in both time and space; 2) determine the optical properties of the boreal aerosols; and 3) atmospherically correct remotely sensed data acquired during BOREAS. This data set contains airborne tracking sunphotometer data that were acquired from the C-130 aircraft during its flights over the BOREAS study areas. The data cover selected days and times from May to September 1994.
&lt;br&gt;&lt;h4 id&#x3D;&quot;r12sunpd_299&quot;&gt;r12sunpd_299&lt;/h4&gt;
The BOREAS RSS-12 team collected both ground and airborne sunphotometer measurements for use in characterizing the aerosol optical properties of the atmosphere during the BOREAS data collection activities. These measurements are to be used to: 1) measure the magnitude and variability of the aerosol optical depth in both time and space; 2) determine the optical properties of the boreal aerosols; and 3) atmospherically correct some remotely sensed data acquired during BOREAS. These data cover selected days and times from May to September 1994 and were taken from one of two ground sites near Candle Lake in the SSA. The data described in this document are from the field sunphotometer data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;goes71_444&quot;&gt;goes71_444&lt;/h4&gt;
The level-1 BOREAS GOES-7 image data were collected by Remote Sensing Science Team 14 (RSS-14) personnel at Florida State University (FSU) and delivered to BORIS. The data cover the period of 01-Jan-1994 through 08-Jul-1995, with partial to complete coverage on the majority of the days. The data include three bands with eight-bit pixel values. No major problems with the data have been identified. Companion files include (1) an image inventory listing to inform users of the images that are available and (2) example thumbnail images.
&lt;br&gt;&lt;h4 id&#x3D;&quot;goes71a_300&quot;&gt;goes71a_300&lt;/h4&gt;
The level-1a BOREAS GOES-7 image data was collected by Remote Sensing Science Team 14 (RSS-14) personnel at the Florida State University and processed to level-1a products by BORIS personnel. The primary objective for the GOES-7 images in 1994 was to collect visible, infrared (IR), and water vapor channel data covering the BOREAS region at a sufficiently high temporal frequency for subsequent use in analyzing weather events and deriving temporal surface radiation parameters and patterns that existed during the Focused and Intensive Field Campaigns (FFCs and IFCs). The transition and shifting of satellites from GOES-7 to GOES-8 in 1995 enabled good quality images to be acquired over the BOREAS region four times per day from January to June, giving a reasonable monitoring dataset. The data cover the period of 01-January-1994 through 08-July-1995 with partial to complete coverage on the majority of the days. The data include three-bands with eight-bit pixel values. No major problems with the data have been identified.
&lt;br&gt;&lt;h4 id&#x3D;&quot;goes72_554&quot;&gt;goes72_554&lt;/h4&gt;
The BOREAS RSS-14 team collected and processed several GOES-7 and GOES-8 image data sets that covered the BOREAS study region. This data set contains images of shortwave and longwave radiation at the surface and top of the atmosphere derived from collected GOES-7 data. The data cover the time period of 05-Feb-1994 to 20-Sep-1994. The images missing from the temporal series were zero-filled to create a consistent sequence of files. The data are stored in binary image format files.
&lt;br&gt;&lt;h4 id&#x3D;&quot;goes81_445&quot;&gt;goes81_445&lt;/h4&gt;
The BOREAS RSS-14 team collected and processed several GOES-7 and GOES-8 image data sets that covered the BOREAS study region. The level-1 BOREAS GOES-8 images are raw data values collected by RSS-14 personnel at FSU and delivered to BORIS. The data cover 14-Jul-1995 to 21-Sep-1995 and 01-Jan-1996 to 03-Oct-1996. The data start out containing three 8-bit spectral bands and end up containing five 10-bit spectral bands. No major problems with the data have been identified. The data are contained in binary image format files. Companion files include (1) an image inventory listing to inform users of the images that are available and (2) example thumbnail images.
&lt;br&gt;&lt;h4 id&#x3D;&quot;goes81a_446&quot;&gt;goes81a_446&lt;/h4&gt;
The BOREAS RSS-14 team collected and processed several GOES-7 and GOES-8 image data sets that covered the BOREAS study region. The level-1a GOES-8 images were created by BORIS personnel from the level-1 images delivered by FSU personnel. The data cover 14-Jul-1995 to 21-Sep-1995 and 12-Feb-1996 to 03-Oct-1996. The data start out as three bands with 8-bit pixel values and end up as five bands with 10-bit pixel values. No major problems with the data have been identified. The differences between the level-1 and level-1a GOES-8 data are the formatting and packaging of the data. The images missing from the temporal series of level-1 GOES-8 images were zero-filled by BORIS staff to create files consistent in size and format. In addition, BORIS staff packaged all the images of a given type from a given day into a single file, removed the header information from the individual level-1 files, and placed it into a single descriptive ASCII header file. The data are contained in binary image format files. Companion files include (1) an image inventory listing to inform users of the images that are available and (2) example thumbnail images.
&lt;br&gt;&lt;h4 id&#x3D;&quot;rss14srb_447&quot;&gt;rss14srb_447&lt;/h4&gt;
The BOREAS RSS-14 team collected and processed GOES-7 and -8 images of the BOREAS region as part of their effort to characterize the incoming, reflected and emitted radiation at regional scales. This data set contains surface radiation parameters, such as net radiation and net solar radiation, that have been interpolated from GOES-7 images and AMS data onto the standard BOREAS mapping grid at a resolution of 5 km N-S and E-W. While some parameters are taken directly from the AMS data set, others have been corrected according to calibrations carried out during the second 1994 IFC-2. The corrected values, as well as the uncorrected values are included. For example, two values of net radiation are provided: an uncorrected value (Rn), and a value that has been corrected according to the calibrations (Rn-COR). The data are provided in binary image format data files. Companion files include example thumbnail images that may be viewed and the image data files downloaded using a convenient viewer utility.
&lt;br&gt;&lt;h4 id&#x3D;&quot;rs15bmlc_483&quot;&gt;rs15bmlc_483&lt;/h4&gt;
As part of BOREAS, the RSS-15 team conducted an investigation using SIR-C , X-SAR and Landsat TM data for estimating total above-ground dry biomass for the SSA and NSA modeling grids and component biomass for the SSA. Relationships of backscatter to total biomass and total biomass to foliage, branch, and bole biomass were used to estimate biomass density across the landscape. The procedure involved image classification with SAR and Landsat TM data and development of simple mapping techniques using combinations of SAR channels. For the SSA, the SIR-C data used were acquired on 06-Oct-1994, and the Landsat TM data used were acquired on September 2, 1995. The maps of the NSA were developed from SIR-C data acquired on 13-Apr-1994.
&lt;br&gt;&lt;h4 id&#x3D;&quot;rs16cm61_563&quot;&gt;rs16cm61_563&lt;/h4&gt;
The BOREAS RSS-16 team used satellite and aircraft SAR data in conjunction with various ground measurements to determine the moisture regime of the boreal forest. RSS-16 assisted with the acquisition and ordering of NASA JPL AIRSAR data collected from the NASA DC-8 aircraft. The NASA JPL AIRSAR is a side-looking imaging radar system that utilizes the SAR principle to obtain high-resolution images that represent the radar backscatter of the imaged surface at different frequencies and polarizations. The information contained in each pixel of the AIRSAR data represents the radar backscatter for all possible combinations of horizontal and vertical transmit and receive polarizations (i.e., HH, HV, VH, and VV). Geographically, the data cover portions of the BOREAS SSA and NSA. Temporally, the data were acquired from 12-Aug-1993 to 31-Jul-1995. The level-3b AIRSAR CM data are in compressed Stokes matrix format, which has 10 bytes per pixel. From this data format, it is possible to synthesize a number of different radar backscatter measurements. The data are stored in binary image-format files.
&lt;br&gt;&lt;h4 id&#x3D;&quot;rss17fth_484&quot;&gt;rss17fth_484&lt;/h4&gt;
The BOREAS RSS-17 team acquired and analyzed imaging radar data from the ESA&amp;#39;s ERS-1 over a complete annual cycle at the BOREAS sites in Canada in 1994 to detect shifts in radar backscatter related to varying environmental conditions. Two independent transitions corresponding to soil thaw and possible canopy thaw were revealed by the data. The results demonstrated that radar provides an ability to observe thaw transitions at the beginning of the growing season, which in turn helps constrain the length of the growing season. The data set presented here includes change maps derived from radar backscatter images that were mosaicked together to cover the southern BOREAS sites. The image values used for calculating the changes are given relative to the reference mosaic image. Due to copyright issues, the 01-March-1994 reference image is not included on the CD-ROM and is not publically available. See the accompanying guide document for information about how to possibly acquire the data. The data are stored in binary image format files.
&lt;br&gt;&lt;h4 id&#x3D;&quot;rs17diel_301&quot;&gt;rs17diel_301&lt;/h4&gt;
The BOREAS RSS-17 team acquired and analyzed imaging radar data from the ESA&amp;#39;s ERS-1 over a complete annual cycle at the BOREAS sites in Canada in 1994 to detect shifts in radar backscatter related to varying environmental conditions. This data set consists of dielectric constant profile measurements from selected trees at various BOREAS flux tower sites. The relative dielectric constant was measured at C-band (frequency &#x3D; 5 GHz) as a function of depth into the trunk of three trees at each site. Measurements were made during April 1994 with an Applied Microwave Corporation field PDP fitted with a 0.358-cm (0.141-inch) diameter coaxial probe tip.
&lt;br&gt;&lt;h4 id&#x3D;&quot;rs7ssatd_302&quot;&gt;rs7ssatd_302&lt;/h4&gt;
The BOREAS RSS-17 team collected several data sets in support of its research in monitoring and analyzing environmental and phenological states using radar data. This data set consists of tree bole and soil temperature measurements from various BOREAS flux tower sites. Temperatures were measured with thermistors implanted in the hydroconductive tissue of the trunks of several trees at each site and at various depths in the soil. Data were stored on a data logger at intervals of either 1 or 2 hours. The majority of the data were acquired between early 1994 and early 1995. The primary product of this data set is the diurnal stem temperature measurements acquired for selected trees at five BOREAS tower sites.
&lt;br&gt;&lt;h4 id&#x3D;&quot;rss17xyf_303&quot;&gt;rss17xyf_303&lt;/h4&gt;
As part of its efforts to determine environmental and phenological states from radar imagery, the BOREAS RSS-17 team collected in situ tree xylem flow measurements for one growing season on five Picea mariana (black spruce) trees. The data were collected to obtain information on the temporal and spatial variability in water uptake by trees in the SSA-OBS (Picea mariana) stand in the BOREAS SSA. Temporally, the data were collected in 30-minute intervals for 120 days from 31-May-1994 until 27-September-1994.
&lt;br&gt;&lt;h4 id&#x3D;&quot;rss18_aviris_l1b_449&quot;&gt;RSS18_AVIRIS_L1B_449&lt;/h4&gt;
This dataset holds Level 1B (L1B) radiance data collected by the AVIRIS-Classic instrument near Prince Albert, Saskatchewan, Canada, on August 14, 1996. This imagery was acquired for the Boreal Ecosystem-Atmosphere Study (BOREAS) project in the boreal forests of central Canada. BOREAS focused on improving the understanding of exchanges of radiative energy, sensible heat, water, CO2 and trace gases between the boreal forest and the lower atmosphere. NASA&amp;#39;s AVIRIS-Classic is a pushbroom spectral mapping system with high signal-to-noise ratio (SNR), designed and toleranced for high performance spectroscopy. AVIRIS-Classic measures reflected radiance in 224 contiguous bands at approximately 10-nm intervals in the Visible to Shortwave Infrared (VSWIR) spectral range from 400-2500 nm. The AVIRIS-Classic sensor has a 1 milliradian instantaneous field of view, providing altitude dependent ground sampling distances from 20 m to sub meter range. For these data, AVIRIS-Classic was deployed on NASA&amp;#39;s ER-2 high altitude aircraft. These spectra are acquired as images with 20-meter spatial resolution, 11 km swath width, and flight lines up to 800 km in length. The measurements are spectrally, radiometrically, and geometrically calibrated. There are seven flight lines subdivided into 66 scenes. The dataset includes the radiance imagery cube for each scene along with calibration and navigation information. The radiance data are in instrument coordinates, georeferenced by center of each scan line, and provided in a binary file. Metadata are included in a mixture of binary and text file formats.
&lt;br&gt;&lt;h4 id&#x3D;&quot;rss18opt_503&quot;&gt;rss18opt_503&lt;/h4&gt;
The BOREAS RSS-18 team collected ground-based sunphotometer data in support of AVIRIS remote sensing activities at the SSA. The following information was compiled by staff members of the BOReal Ecosystem-Atmosphere Study (BOREAS) Information System (BORIS) as part of their data documentation efforts.
&lt;br&gt;&lt;h4 id&#x3D;&quot;r19cas94_537&quot;&gt;r19cas94_537&lt;/h4&gt;
The RSS-19 team collected CASI images from the Chieftain Navaho aircraft in order to observe the seasonal change in the radiometric reflectance properties of the boreal forest landscape. CASI was deployed as a site-specific optical sensor during BOREAS field campaigns. Image data were collected with CASI on 36 days during five field campaigns between February and September 1994, primarily at flux tower sites located at study sites near Thompson, Manitoba, and Prince Albert, Saskatchewan. A variety of CASI data collection strategies were used to meet the following scientific objectives: 1) canopy bidirectional reflectance, 2) canopy biochemistry, 3) spatial variability, and 4) estimates of up and downwelling PAR and spectral albedo, as well as changes along transects across lakes and transects NSA and SSA. The images are stored as binary image files.
&lt;br&gt;&lt;h4 id&#x3D;&quot;und_refl_304&quot;&gt;und_refl_304&lt;/h4&gt;
One objective of BOREAS is to further the understanding of the spectral bi-directional reflectance of typical boreal ecosystem stands in the visible/near-infrared regime. An essential input for any canopy BRDF model is an accurate estimate of the average understory reflectance, both for sunlit and shaded conditions. These variables can be expected to vary seasonally because of species-dependent differences in the phenological cycle of foliar display. In response to these requirements, the average understory reflectance for the flux tower sites of both the NSA (Thompson, Manitoba) and the SSA (Candle Lake, Saskatchewan) Study Areas (NSA and SSA) was observed throughout the year during five field campaigns. This was done by measuring the nadir reflectance (400 to 850 nm) of sunlit and shaded understory (vegetation and snow cover) along a surveyed LAI transect line (Chen, RSS-07) at each site near solar noon and documenting a average site reflectance. Comparisons between sites reveal differences in the green and infrared regions of the spectra, because of the differing species in the understory for each site. Temporal (seasonal) variation for each site was also observed, indicating the changing flora mixtures and changing spectral signatures as the understory matures during the growing season.
&lt;br&gt;&lt;h4 id&#x3D;&quot;r19cas96_538&quot;&gt;r19cas96_538&lt;/h4&gt;
The RSS-19 team collected CASI images from the Chieftain Navaho aircraft in order to observe the seasonal change in the radiometric reflectance properties of the boreal forest landscape. CASI was deployed as a site-specific optical sensor as part of BOREAS. The overall objective of the CASI deployment was to observe the seasonal change in the radiometric reflectance properties of the boreal forest landscape. In 1996, image data were collected with CASI on 15 days during a field campaign between 18-July and 01-August, primarily at flux tower sites located at study sites near Thompson, Manitoba, and Prince Albert, Saskatchewan. A subset of the data is available from the BOREAS Information System (BORIS). Radiance and at-ground modeled reflectance images have been provided. This subset of CASI-processed data corresponds to the data for CASI Mission 3 described in Section 4.1.3 of the complete guide document. A variety of CASI data collection strategies were used to meet the following scientific objectives: 1) canopy bidirectional reflectance, 2) canopy biochemistry, 3) spatial variability, and 4) estimates of up and downwelling PAR spectral albedo, as well as changes along transects across lakes at the southern site and transects between the NSA and SSA. The images are stored as binary image files.
&lt;br&gt;&lt;h4 id&#x3D;&quot;rs20c130_305&quot;&gt;rs20c130_305&lt;/h4&gt;
This data set contains measurements of surface BRDF made by the POLDER instrument over several surface types (pine, spruce, fen) of the BOREAS SSA during the 1994 IFCs. Single-point BRDF values were acquired either from the NASA ARC C-130 aircraft or from a NASA WFF helicopter. A related data set collected from the helicopter platform is available as is POLDER imagery acquired from the C-130.
&lt;br&gt;&lt;h4 id&#x3D;&quot;rs20helo_306&quot;&gt;rs20helo_306&lt;/h4&gt;
This data set contains measurements of surface BRDF made by the POLDER instrument over several sites (pine, spruce, fen) of the BOREAS study areas during 1994. Single-point BRDF values were acquired from NASA&amp;#39;s WFF helicopter. A related data set collected from the C-130 platform is available as is POLDER imagery acquired from the C-130.
&lt;br&gt;&lt;h4 id&#x3D;&quot;rs20prad_555&quot;&gt;rs20prad_555&lt;/h4&gt;
These data are a subset of images collected by the POLDER instrument over tower sites in the BOREAS study areas during the IFCs in 1994. The POLDER images presented here from the NASA/Ames C-130 aircraft are made available for illustration purposes only. The data are stored in binary image-format files.
&lt;br&gt;&lt;h4 id&#x3D;&quot;saskffcc_307&quot;&gt;saskffcc_307&lt;/h4&gt;
The Saskatchewan Forest Fire Control Centre (SFFCC) provided surface meteorological data to BOREAS from their archive. This data set contains hourly surface meteorological data from 18 of the meteorological stations located across Saskatchewan. Included in this data are parameters of date, time, temperature, relative humidity, wind direction, wind speed and precipitation. Temporally, the data cover the period of May through September of 1994 and 1995.
&lt;br&gt;&lt;h4 id&#x3D;&quot;boreas_slicer_508&quot;&gt;BOREAS_SLICER_508&lt;/h4&gt;
Scanning Lidar Imager of Canopies by Echo Recovery (SLICER) data were acquired in support of BOReal Ecosystem-Atmosphere Study (BOREAS) at all of the Tower Flux (TF) sites in the Southern and Northern Study Areas (SSA and NSA, respectively) and along transects between the study areas. Data were acquired on 5 days between 18 and 30 July 1996. Each coverage of a tower site is typically 40 km in length, with a minimum of 3 and a maximum of 10 lines across each tower oriented in a variety of azimuths. The SLICER data were acquired simultaneously with Advanced Solid-State Array Spectroradiometer (ASAS) hyperspectral, multiview angle images. The SLICER Level 3 products consist of binary files for each flight line with a data record for each laser shot composed of 13 parameters and a 600-byte waveform that is the raw record of the back scatter laser energy reflected from Earth&amp;#39;s surface.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ssafcovv_509&quot;&gt;ssafcovv_509&lt;/h4&gt;
The forest cover data provided by Saskatchewan Environment and Resource Management, Forestry Branch - Inventory Unit (SERM-FBIU) are basically a digital version of its 1:12,500 scale forest cover polygon maps. The data include information on forest parameters and cover the area in and near the BOREAS SSA, excluding the PANP. As a digital archive, however, changes within forest stands can be updated more readily. At the same time, it should be kept in mind that most of these digital forest cover data were acquired in 1993, and the data set has been static since that time.
&lt;br&gt;&lt;h4 id&#x3D;&quot;saskfc1m_510&quot;&gt;saskfc1m_510&lt;/h4&gt;
This data set is a condensed forest cover type digital map of Saskatchewan and is a product of the Saskatchewan Environment and Resource Management, Forestry Branch - Inventory Unit (SERM-FBIU). This map was generalized from SERM township maps of vegetation cover at an approximate scale of 1:63,000 (1 in. &#x3D; 1 mile). The cover information was iteratively generalized until it was compiled on a 1:1,000,000 scale map base. This data set was prepared by SERM-FBIU. The data is a condensed forest cover type map of Saskatchewan at a scale of 1:1,000,000.
&lt;br&gt;&lt;h4 id&#x3D;&quot;saskfire_308&quot;&gt;saskfire_308&lt;/h4&gt;
This data set is a series of ARC/INFO export files of the fire history of Saskatchewan by year from 1945 to 1996, with a few missing years. The data set was compiled and provided by the Saskatchewan Environment and Resource Management (SERM) to Wildlife Branch.
&lt;br&gt;&lt;h4 id&#x3D;&quot;geocoord_556&quot;&gt;geocoord_556&lt;/h4&gt;
In an effort to properly document the sites and areas where data were collected, personnel of the BOReal Ecosystem-Atmosphere Study (BOREAS) Information System (BORIS) obtained and compiled geographic coordinate and other site information from several sources throughout the experiment period. The final set of information is organized into two data sets that provide geographic coordinate and site characteristic information for single sites and corner coordinates for standard geographic areas. The data are stored in two text files as American Standard Code for Information Interchange (ASCII) characters.
&lt;br&gt;&lt;h4 id&#x3D;&quot;te1ch4fx_310&quot;&gt;te1ch4fx_310&lt;/h4&gt;
The BOREAS TE-01 team collected various data to characterize the soil-plant systems in the BOREAS SSA. Particular emphasis was placed on nutrient biochemistry, the stores and transfers of organic carbon and how the characteristics were related to measured methane fluxes. The overall transect in the Prince Albert National Park (Saskatchewan, Canada) included the major plant communities and related soils that occurred in that section of the boreal forest. Soil physical, chemical and biological measurements along the transect were used to characterize the static environment, which allowed them to be related to methane fluxes. Chamber techniques were used to provide a measure of methane production/uptake. Chamber measurements coupled with flask sampling were used to determine the seasonality of methane fluxes. This particular data set contains methane flux and soil profile methane concentration values from the SSA-OA site. The data were collected from 29-MAY to 17-SEP-1994.
&lt;br&gt;&lt;h4 id&#x3D;&quot;soilte1r_312&quot;&gt;soilte1r_312&lt;/h4&gt;
This data set was gridded from vector layers of soil maps that were received from Dr. Darwin Anderson TE-01 who did the original soil mapping in the field during 1994. The vector layers were gridded into raster files that cover approximately 1 square kilometer over each of the tower sites in the SSA.
&lt;br&gt;&lt;h4 id&#x3D;&quot;te01ssld_530&quot;&gt;te01ssld_530&lt;/h4&gt;
This data set was collected by TE-01 to provide a set of soil properties for BOREAS investigators in the SSA. The soil samples were collected at sets of soil pits. Each set of soil pits was in the vicinity of one of the five flux towers in the BOREAS SSA. The collected soil samples were sent to a lab, where the major soil properties were determined. These properties include, but are not limited to, soil horizon; dry soil color; pH; bulk density; total, organic, and inorganic carbon; electric conductivity; cation exchange capacity; exchangeable sodium, potassium, calcium, magnesium, and hydrogen; water content at 0.01, 0.033, and 1.5 MPascals; nitrogen; phosphorus; particle size distribution; texture; pH of the mineral soil and of the organic soil; extractable acid; and sulfur.
&lt;br&gt;&lt;h4 id&#x3D;&quot;te2wdrs2_314&quot;&gt;te2wdrs2_314&lt;/h4&gt;
The BOREAS TE-02 team collected several data sets in support of its efforts to characterize and interpret information on the respiration of the foliage, roots, and wood of boreal vegetation. This data set contains measurements of wood respiration measured continuously (about once per hour) in the NSA during the growing season of 1994.
&lt;br&gt;&lt;h4 id&#x3D;&quot;te2flrsp_315&quot;&gt;te2flrsp_315&lt;/h4&gt;
The BOREAS TE-02 team collected several data sets in support of its efforts to characterize and interpret information on the respiration of the foliage, roots, and wood of boreal vegetation. This data set contains measurements of foliar respiration conducted in the NSA during the growing season of 1994.
&lt;br&gt;&lt;h4 id&#x3D;&quot;te2rtrsp_316&quot;&gt;te2rtrsp_316&lt;/h4&gt;
The BOREAS TE-02 team collected several data sets in support of its efforts to characterize and interpret information on the respiration of the foliage, roots, and wood of boreal vegetation. This data set includes means of tree root respiration measurements on roots having diameters ranging from 0 to 2 mm conducted in the NSA during the growing season of 1994.
&lt;br&gt;&lt;h4 id&#x3D;&quot;te2stsap_317&quot;&gt;te2stsap_317&lt;/h4&gt;
The BOREAS TE-02 team collected several data sets in support of its efforts to characterize and interpret information on the respiration of the foliage, roots, and wood of boreal vegetation. This data set contains measurements of growth and sapwood of the stems conducted in the NSA during the growing season of 1994.
&lt;br&gt;&lt;h4 id&#x3D;&quot;te2wdrsp_318&quot;&gt;te2wdrsp_318&lt;/h4&gt;
The BOREAS TE-02 team collected several data sets in support of its efforts to characterize and interpret information on the respiration of the foliage, roots, and wood of boreal vegetation. This data set contains measurements of wood respiration conducted in the NSA during the growing season of 1994.
&lt;br&gt;&lt;h4 id&#x3D;&quot;te04bbag_319&quot;&gt;te04bbag_319&lt;/h4&gt;
The BOREAS TE-04 team collected continuous records of gas exchange under ambient conditions from intact boreal forest trees in the BOREAS NSA from 23-Jul-1996 until 14-Aug-1996. These measurements can be used to test models of photosynthesis, stomatal conductance, and leaf respiration, such as SiB2 (Sellers et al., 1996) or the leaf model (Collatz et al., 1991), and programs can be obtained from the investigators.
&lt;br&gt;&lt;h4 id&#x3D;&quot;te04gxda_320&quot;&gt;te04gxda_320&lt;/h4&gt;
Measurements of light, CO2, temperature, and humidity response curves were made by the BOREAS TE-04 team during the summary of 1994 using intact attached leaves of boreal forest species located in the BOREAS SSA. These measurements were conducted to calibrate models used to predict photosynthesis, stomatal conductance, and leaf respiration. The data can be used to construct plots of response functions or for parameterizing models. Parameter values suitable for application in SiB2 (Sellers et al., 1996) or the leaf model of Collatz et al. (1991) and programs can be obtained from the investigators.
&lt;br&gt;&lt;h4 id&#x3D;&quot;te5airs_321&quot;&gt;te5airs_321&lt;/h4&gt;
The BOREAS group TE-05 collected measurements in the NSA and SSA on gas exchange, gas composition and tree growth. This data set contains measurements of the concentration and stable carbon (13C/12C) and oxygen (18O/16O) isotope ratios of atmospheric CO2 in air samples collected at different heights within forest canopies. The data were collected to determine the influence of photosynthesis and respiration by the forest ecosystems on the concentration and stable isotope ratio of atmospheric CO2. These measurements were collected at the SSA during each IFC at OJP, OBS, and OA sites. Measurements were also collected at the NSA during each 1994 IFC at the OJP, T6R5S TE UBS, and T2Q6A TE OA sites. The stable isotope ratios are expressed using standard delta notation and in units of per mil. The isotope ratios are expressed relative to the international standard, PDB, for both carbon and oxygen samples.
&lt;br&gt;&lt;h4 id&#x3D;&quot;te5co2pd_322&quot;&gt;te5co2pd_322&lt;/h4&gt;
These data were collected by BOREAS TE-05 to provide detailed information within the canopy during times when TE-05 sampled canopy CO2 for carbon and oxygen isotope analysis. These measurements were made in both the NSA and SSA during each IFC at the OJP, OBS, UBS, and OA sites. CO2 profile data were not collected at SSA-OA during the first IFC.
&lt;br&gt;&lt;h4 id&#x3D;&quot;te5lciso_323&quot;&gt;te5lciso_323&lt;/h4&gt;
The BOREAS group TE-05 collected measurements in the NSA and SSA on gas exchange, gas composition and tree growth. This documentation describes leaf carbon isotope data that were collected in 1993 and 1994 at the NSA and SSA OJP, OBS and NSA UBS sites. In addition, leaf carbon isotope data were collected in 1994 only at the NSA and SSA OA sites. These data were collected to provide seasonal integrated physiological information for 10 to 15 common species at these 6 BOREAS sites.
&lt;br&gt;&lt;h4 id&#x3D;&quot;te5lgxd_324&quot;&gt;te5lgxd_324&lt;/h4&gt;
The BOREAS group TE-05 collected measurements in the NSA and SSA on gas exchange, gas composition and tree growth. The leaf photosynthetic gas exchange data were collected in the BOREAS NSA and the SSA using a Li-Cor 6200 portable photosynthesis system. The data were collected to compare the photosynthetic capacity, stomatal conductance and leaf intercellular CO2 concentrations among the major tree species at the BOREAS sites. The data are average values from diurnal measurements on the upper canopy foliage (sun leaves).
&lt;br&gt;&lt;h4 id&#x3D;&quot;te5soilr_325&quot;&gt;te5soilr_325&lt;/h4&gt;
The BOREAS group TE-05 collected measurements in the NSA and SSA on gas exchange, gas composition and tree growth. Soil respiration data collected in the BOREAS NSA and SSA to compare the soil respiration rates in different forest sites using a Li-Cor 6200 soil respiration chamber (model 6299).
&lt;br&gt;&lt;h4 id&#x3D;&quot;te5metd_326&quot;&gt;te5metd_326&lt;/h4&gt;
The BOREAS group TE-05 collected measurements in the NSA and SSA on gas exchange, gas composition and tree growth. Measurements of meteorological data, including air and soil temperature, RH, and PPFD were 30-minute intervals during the 1994 IFCs at various sites in the BOREAS NSA and SSA.
&lt;br&gt;&lt;h4 id&#x3D;&quot;te5treer_327&quot;&gt;te5treer_327&lt;/h4&gt;
These data include tree ring widths and cellulose carbon isotope data from coniferous trees collected at the BOREAS NSA and SSA by the BOREAS TE-05 team. Ring width data are provided for both Picea mariana and Pinus banksiana. The carbon isotope data are provided only for Pinus banksiana.
&lt;br&gt;&lt;h4 id&#x3D;&quot;te6satns_328&quot;&gt;te6satns_328&lt;/h4&gt;
The BOREAS TE-06 team collected several data sets to examine the influence of vegetation, climate, and their interactions on the major carbon fluxes for boreal forest species. This data set contains measurements of the air temperature at a single height and soil temperature at several depths in the NSA from 25-May to 8-Oct-1994. Chromel-Constantan thermocouple wires run by a miniprogrammable data logger (Model 21X, Campbell Scientific, Inc., Logan, UT) provided direct measurements of temperature.
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The BOREAS TE-06 team collected several data sets in support of its efforts to characterize and interpret information on the plant biomass, allometry, biometry, sapwood, leaf area index, net primatry production, soil temperature, leaf water potential, soil CO2 flux, and multivegetation imagery of boreal vegetation. This data set includes tree measurements conducted on the above gound biomass of trees in the BOREAS NSA and SSA during the growing seasons of 1994 and 1995 and the derived allometric relationships/equations.
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The BOREAS TE-06 team collected several data sets in support of its efforts to characterize and interpret information on the plant biomass, allometry, biometry, sapwood, leaf area index, net primary production, soil temperature, leaf water potential, soil CO2 flux, and multivegetation imagery of boreal vegetation. This data set contains measurements of estimates of the standing biomass and leaf area index for the plant species at the TF, CEV, and AUX sites in the SSA and NSA during the growing seasons of 1994 and 1995.
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A newly developed ground-based canopy imaging system called an MVI was tested and used by the BOREAS TE-06 team to collect measurements of the canopy gap fraction (sky fraction), canopy gap-size distribution (size and frequency of gaps between foliage in canopy), branch architecture, and leaf angle distribution (fraction of leaf area in specific leaf inclination classes assuming azimuthal symmetry). Measurements of the canopy gap-size distribution are used to derive canopy clumping indices that can be used to adjust indirect LAI measurements made in nonrandom forests. These clumping factors will also help to describe the radiation penetration in clumped canopies more accurately by allowing for simple adjustments to Beer&amp;#39;s law. Measurements of the above quantities were obtained at BOREAS NSA OJP site in IFC-2 in 1994, at the SSA OA in July 1995, and at the SSA OBS and SSA OA sites in IFC-2 in 1996. Modeling studies were also performed to further validate MVI measurements and to gain a more complete understanding of boreal forest canopy architecture. By using MVI measurements and Monte Carlo simulations, clumping indices as a function of zenith angle were derived for the three main boreal species studied during BOREAS.
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The BOREAS TE-06 team collected several data sets to examine the influence of vegetation, climate, and their interactions on the major carbon fluxes for boreal forest species. This data set contains estimates of the biomass produced by the plant species at the TF, CEV, and AUX sites in the SSA and NSA for a given year. Temporally, the data cover the years of 1985 to 1995. The plant biomass production (i.e., aboveground, belowground, understory, litterfall), spatial coverage, and temporal nature of measurements varied between the TF, CEV, and AUX sites as deemed necessary by BOREAS principal investigators.
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The BOREAS TE-06 team collected several data sets to examine the influence of vegetation, climate, and their interactions on the major carbon fluxes for boreal forest species. This data set contains summaries of predawn leaf water potentials and foliage moisture contents collected at the TF and CEV sites that had canopy access towers. The data was collected on a nearly weekly basis from early June to late August 1994 by TE-06, members of the BOREAS staff, and employees of Environment Canada.
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The BOREAS TE-07 team collected data sets in support of its efforts to characterize and interpret information on the sapflow and dendrology of boreal vegetation. This data set contains dendrology measurements, consisting of tree ring width and density taken at several points within each ring. Measurements were taken near the TE towers at the OJP and OBS sites in NSA. In the SSA, measurements were taken near the TE towers at the MIX, OBS, and OJP sites; at the AIM-13 and BMH-9 sites; and near the TF-YJP site. All data were collected during the summer of 1994. Note that the TE-07 dendrology data available for the ORNL DAAC are a summary and an inventoru of the full Canadian Forest Service (CFS) data set. Please see Section 1.5 of the complete data set reference document for information on obtaining the CFS data set.
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The BOREAS TE-07 team collected data sets in support of its efforts to characterize and interpret information on the sap flow of boreal vegetation. The heat pulse method was used to monitor sap flow and to estimate rates of transpiration from aspen, black spruce, and mixed wood forests at the SSA-OA, MIX, SSA-OBS, and Batoche sites in Saskatchewan, Canada. Measurements were made at the various sites from May to Oct 1994, May to Oct 1995, and Apr to Oct 1996. A scaling procedure was used to estimate canopy transpiration rates from the sap flow measurements.
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The BOREAS TE-08 team collected pigment density data from aspen bark and leaves from four sites within the BOREAS SSA from 24-May-1994 to 16-Jun-1994 (IFC-1), 19-Jul-1994 to 08-Aug-1994 (IFC 2), and 30-Aug-1994 to 19-Sep-1994 (IFC-3). One to nine trees from each site were sampled during the three IFCs. Each tree was sampled in five different locations for bark pigment properties: basal stem section, which was any bark sample taken below one-half the tree height; upper stem section, which was any bark sample taken from the main stem above one-half the tree height; bark taken from branches up to 3 years old; a 2-year old branch segment; and a 1-year old branch segment. Additionally, a limited number of leaves were collected. Bark samples were removed from the stem of the tree, placed in ziplock bags, and transported to UNH, where they were processed and analyzed by a spectrophotometer. In each data file, samples are identified by Site, date, Tree#, and Sample Location (see 1st paragraph above). Pigment density values are normalized to mg/m2. Density values for the following pigments are provided: Chl a, Chl b, Total Chl (Chl a+b), Carotenoids, Chl a to b ratio, and the Total Chl to carotenoids ratio.
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The BOREAS TE-08 team collected in-lab spectral reflectance data for aspen bark and leaves from three sites within the BOREAS SSA from 24-May-1994 to 16-Jun-1994 (IFC 1), 19-Jul-1994 to 08-Aug-1994 (IFC 2), and 30-Aug-1994 to 19-Sep-1994 (IFC 3). One to nine trees from each site were sampled during the three IFCs. Each tree was sampled in five different locations for bark spectral properties: BS, US, BR, BT, and BO. Additionally, a limited number of LV were collected. Bark samples were removed from the stem of the tree and placed in ziplock bags for transport to UNH, where they were scanned with a spectroradiometer in a controlled environment. Each sample was scanned twice: the first set of measurements was made with the bark surface moistened, and the second set was made with the bark surface air-dried for a period of 30 minutes. These data represent continuous spectra of bark reflectance. Each sample was scanned three times, rotating the sample when possible. The reported values for each sample are an average over the three scans.
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The gas exchange data of the Boreal Ecosystem-Atmosphere Study (BOREAS) Northern Study Area (NSA) were collected to characterize diurnal gas exchange and water potential of two canopy levels of five boreal canopy cover types: young and old jack pine (Pinus banksiana Lamb.), old aspen (Populus tremuloides Michx.), and lowland and upland black spruce (Picea mariana (Mill) B.S.P.). These data were collected between 27-May-1994 and 17-Sep-1994. The purpose of this study was threefold: 1) to provide in situ gas exchange data that will be used to validate models of photosynthetic responses to light, temperature, and carbon dioxide (CO2); 2) to compare the photosynthetic responses of different tree crown levels (upper and lower), and 3) to characterize the diurnal water potential curves for these sites to get an indication of the extent to which soil moisture supply to leaves might be limiting photosynthesis.
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Spectral reflectance of the forest understory at the ground level, in three boreal forest sites of Northern Manitoba (56 degrees N latitude and 98 degrees W longitude), were obtained and analyzed. The objective of the study was to estimate light levels inside the forest canopy and to link these estimates with airborne images taken above the canopy, in order to tie the photosynthetic experiments and models with the remotely sensed measurements. The Boreal Ecosystem-Atmospheric Study (BOREAS) Terrestrial Ecosystem (TE)-09 project contained several sub-projects designed to work together to meet this goal: a high-resolution canopy modeling component, extensive measurements of canopy architecture and structure, photometric measurements inside the canopy, and spectral measurements of both the canopy and the understory.
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The BOREAS TE-09 team collected several data sets related to chemical and photosynthetic properties of leaves. This data set contains canopy biochemistry data collected in 1994 in the NSA at the YJP, OJP, OBS, BS and OA sites including biochemistry lignin, nitrogen, cellulose, starch, and fiber concentrations. These data were collected to study the spatial and temporal changes in the canopy biochemistry of boreal forest cover types and how a high-resolution radiative transfer model in the mid-infrared could be applied in an effort to obtain better estimates of canopy biochemical properties using remote sensing.
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The Boreal Ecosystem-Atmosphere Study (BOREAS) Terrestrial Ecology Team #9 (TE-09) provided several data sets containing information about the state and response of boreal forest tree species. This data set contains information on the spatial density of chlorophyll in the leaves of three boreal tree species collected at five different sites at various times during 1994.
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The BOREAS TE-09 team collected several data sets related to chemical and photosynthetic properties of leaves in boreal forest tree species. This data set describes the relationship between Photosynthetically Active Radiation (PAR) levels and foliage nitrogen in samples from six sites in the BOREAS NSA. This information is useful for modeling the vertical distribution of carbon fixation for these different forest types in the boreal forest. The data were collected to quantify the relationship between PAR and leaf nitrogen of black spruce, jack pine, and aspen.
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The BOREAS TE-09 team collected several data sets related to chemical and photosynthetic properties of leaves in boreal forest tree species. This data set describes the spatial and temporal relationship between foliage nitrogen concentration and photosynthetic capacity in the canopies of black spruce, jack pine, and aspen. The data were collected from June to September 1994 and are useful for modeling the vertical distribution of carbon fixation for different forest types in the boreal forest.
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The BOREAS TE-09 team collected several data sets related to chemical and photosynthetic properties of leaves. This data set describes (1) the response of leaf and shoot-level photosynthesis to ambient and intercellular CO2 concentration, temperature, and incident PAR for black spruce, jack pine, and aspen during the three IFCs in 1994 in the NSA; (2) the response of stomatal conductance to vapor pressure difference throughout the growing season of 1994; and (3) a range of shoot water potentials (controlled in the laboratory) for black spruce and jack pine.
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The BOREAS TE-10 team collected several data sets in support of its efforts to characterize and interpret information on the reflectance, transmittance, gas exchange, chlorophyll content, carbon content, hydrogen content, and nitrogen content of boreal vegetation. This data set describes the relationship between sample location, age, chlorophyll content, and C-H-N concentrations at several sites in the SSA conducted during the growing seasons of 1994 and 1996.
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The BOREAS TE-10 team collected several data sets in support of its efforts to characterize and interpret information on the reflectance, transmittance, gas exchange, chlorophyll content, carbon content, hydrogen content, and nitrogen content of boreal vegetation. This data set contains measurements of assimilation, stomatal conductance, transpiration, internal CO2 concentration, and water use efficiency conducted in the SSA during the growing seasons of 1994 and 1996 using a portable gas exchange system.
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The BOREAS TE-10 team collected several data sets in support of its efforts to characterize and interpret information on the reflectance, transmittance, gas exchange, oxygen evolution, and biochemical properties of boreal vegetation. This data set describes the spectral optical properties (reflectance and transmittance) of boreal forest conifers and broadleaf tree leaves as measured with a Spectron Engineering SE590 spectroradiometer at the SSA OBS, OJP, YJP, OA, OA-AUX, YA-AUX, and YA sites. The data were collected during the growing seasons of 1994 and 1996.
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The BOREAS TE-10 team collected several data sets in support of its efforts to characterize and interpret information on the gas exchange, reflectance, transmittance, chlorophyll content, carbon content, hydrogen content, nitrogen content, and photosynthetic response of boreal vegetation. This data set contains measurements of quantitative parameters and leaf photosynthetic response to increases in light conducted in the SSA during the growing seasons of 1994 and 1996 using an oxygen electrode system. Leaf photosynthetic responses were not collected in 1996.
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The BOREAS TE-11 team collected several data sets in support of its efforts to characterize and interpret information on the sapflow, gas exchange, and lichen photosynthesis of boreal vegetation and meteorological data of the area studied. This data set contains measurements of assimilation and transpiration conducted at the OJP site during the growing seasons of 1993 and 1994.
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The BOREAS TE-11 team collected several data sets in support of its efforts to characterize and interpret information on the sap flow, gas exchange, and lichen photosynthesis of boreal vegetation and meteorological data of the area studied. This data set contains measurements of sap flow conducted at the SSA-OJP site in the growing seasons of 1993 and 1994.
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The BOReal Ecosystem-Atmosphere Study (BOREAS) Terrestrial Ecology (TE)-11 team collected several data sets in support of its efforts to characterize and interpret information on the sapflow, gas exchange, and lichen photosynthesis of boreal vegetation and meteorological data of the area studied. This data set contains the meteorological data taken in the BOREAS Southern Study Area (SSA) during 1994 and used by TE-11 for their sapflow and gas exchange data analysis.
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The BOREAS TE-12 team collected PAR data sets in support of its efforts to characterize and interpret information on shoot geometry, leaf optical properties, leaf water potential, and leaf gas exchange. The data were collected at the SSA-OBS site from 04-Jul-1996 to 25-Jul-1996.
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The BOREAS TE-12 team collected several data sets in support of its efforts to characterize and interpret information on the reflectance, transmittance, and gas exchange of boreal vegetation. This data set contains measurements of leaf gas exchange conducted in the SSA during the growing seasons of 1994 and 1995 using a portable gas exchange system.
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The BOREAS TE-12 team collected several data sets in support of its efforts to characterize and interpret information on the reflectance, transmittance, and gas exchange of boreal vegetation. This data set contains measurements of hemispherical spectral reflectance and transmittance factors of individual leaves, needles (ages: current and past 2 years&amp;#39; growth, i.e., for 1993, the growing seasons of 1993, 1992, and 1991 were measured; in 1994, the growing seasons of 1994, 1993, and 1992 were measured), twigs (reflectance only), and substrate at near-normal incidence measured using a LI-COR LI-1800-12 integrating sphere attached to a Spectron Engineering SE590 spectroradiometer. Procedures of Daughtry et al. (1989) were followed. These procedures permitted measurement of samples that: 1) filled the entire integrating sphere sample port, and 2) were narrow with a length greater than the sample port diameter. Optical properties were measured at the SSA Fen,YJP, YA, and OBS sites.
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The BOREAS TE-12 team collected shoot geometry data in 1993 and 1994 from Aspen, Jack Pine, and Black Spruce trees. Collections were made at the Southern Study Area FEN, YJP, OJP, OA, YA, MIX and OBS sites. A caliper was used to measure shoot and needle lengths and widths. A volume displacement procedure was used to measure the weight of the shoot or twig submerged in water.
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The BOREAS TE-12 team collected water potential data in 1993 and 1994 from aspen, jack pine and black spruce leaves/needles. Collections were made at the SSA FEN, YJP, YA, OA, and OBS sites. Measurements were made using a pressure chamber on a platform in the field.
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The Boreal Ecosystem-Atmosphere Study (BOREAS) Terrestrial Ecology (TE)-13 team collected data on site characteristics, soil profiles, woody debris, overstory vegetation, and understory vegetation from approximately 100 sites in the Southern Study Area (SSA), Northern Study Area (NSA), and Transect Areas in the boreal forest. This data sets provides 3 reports published by the Canadian Forest Service for the BOREAS project in pdf file format.
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A BOREAS version of the Global Production Efficiency Model (&lt;a href&#x3D;&quot;http://www.inform.umd.edu/glopem&quot;&gt;www.inform.umd.edu/glopem&lt;/a&gt;) was developed by TE-17 to generate maps of gross and net primary production, autotrophic respiration, and light use efficiency for the BOREAS region. This document provides basic information on the model and how the maps were generated. The data generated by the model are stored in binary image-format files.
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This biomass density image covers almost the entire BOREAS SSA. The pixels for which biomass density is computed include areas that are in conifer land cover classes only. The biomass density values represent the amount of overstory biomass (i.e. tree biomass only) per unit area. It is derived from a Landsat-5 TM image collected on 02-Sep-1994. The technique that was used to create this image is very similar to the technique that was used to create the physical classification of the SSA. The data are provided in a binary image file format. Companion files include (1) an image inventory listing to inform users of the images that are available and (2) example thumbnail images.
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The SAIL (Scattering from Arbitrarily Inclined Leaves) model was combined with the Jasinski geometric model to simulate canopy spectral reflectance and absorption of photosynthetically active radiation for discontinuous canopies. This model is called the GeoSail model. Tree shapes are described by cylinders or cones distributed over a plane. Spectral reflectance and transmittance of trees are calculated from the SAIL model to determine the reflectance of the three components used in the geometric model: illuminated canopy, illuminated background, shadowed canopy, and shadowed background. The model code is Fortran, sample input and output data are provided in ASCII text files.
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The objective of this classification is to provide the BOREAS investigators with a data product that characterizes the land cover of the NSA. A Landsat-5 TM image from 20-Aug-1988 was used to derive this classification. A standard supervised maximum likelihood approach was used to produce this classification. Companion files include example thumbnail images that may be viewed using a convenient viewer utility.
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A Landsat-5 TM image from 06-Aug-1990 was used to derive this classification. The objective of this classification is to provide the BOREAS investigators with a data product that characterizes the land cover of the SSA. A standard supervised maximum likelihood approach was used to produce this classification. Companion files include example thumbnail images that may be viewed using a convenient viewer utility.
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The objective of this classification is to provide the BOREAS investigators with a data product that characterizes the land cover of the NSA. A Landsat-5 TM image from 21-Jun-1995 was used to derive the classification. A technique was implemented that uses reflectances of various land cover types along with a geometric optical canopy model to produce spectral trajectories. These trajectories are used as training data to classify the image into the different land cover classes. Companion files include example thumbnail images that may be viewed and using a convenient viewer utility.
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The objective of this classification is to provide the BOREAS investigators with a data product that characterizes the land cover of the SSA. A Landsat-5 TM image from 02-Sep-1994 was used to derive the classification. A technique was implemented that uses reflectances of various land cover types along with a geometric optical canopy model to produce spectral trajectories. These trajectories are used as training data to classify the image into the different land cover classes. These data are provided in a binary image file format. Companion files include example thumbnail images that may be viewed and the image data files downloaded using a convenient viewer utility.
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The BOREAS TE-18 team used a radiometric rectification process to produce standardized digital number (DN) values for a series of Landsat TM images of the BOREAS SSA and NSA in order to compare images that were collected under different atmospheric conditions. The images for each study area were referenced to an image that had very clear atmospheric qualities. The reference image for the SSA was collected on 02-Sep-1994, while the reference image for the NSA was collected on 21-Jun-1995. The 23 rectified images cover the period of 07-Jul-1985 to 18-Sep-1994 in the SSA and from 22-Jun-1984 to 09-Jun-1994 in the NSA. Each of the reference scenes had coincident atmospheric optical thickness measurements made by RSS-11. The radiometric rectification process is described in more detail by Hall et al. (1991). The original Landsat TM data were received from CCRS for use in the BOREAS project. The data are stored in binary image-format files. Due to the nature of the radiometric rectification process and copyright issues, these full resolution images may not be publicly distributed. However, a spatially degraded 60-m resolution version of the images is available on the BOREAS CD-ROM series. Companion files include (1) an image inventory listing to inform users of the images that are available and (2) example thumbnail images that may be viewed and the image data files downloaded using a convenient viewer utility.
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The BOREAS TE-18 team used a radiometric rectification process to produce standardized digital number (DN) values for a series of Landsat TM images of the BOREAS SSA and NSA in order to compare images that were collected under different atmospheric conditions. The images for each study area were rectified by using a reference image that had clear atmospheric qualities. The reference image for the SSA was collected on 02-Sep-1994, while the reference image for the NSA was collected on 21-Jun-1995. The 23 rectified images cover the period of 07-Jul-1985 to 18-Sep-1994 in the SSA and 22-Jun-1984 to 09-Jun-1994 in the NSA.
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The BOREAS TE-19 team developed a model called the Spruce and Moss Model (SPAM) designed to simulate the daily carbon balance of a black spruce/moss boreal forest ecosystem. It is driven by daily weather conditions, and consists of four components: (1) soil climate; (2) tree photosynthesis and respiration; (3) moss photosynthesis and respiration; and (4) litter decomposition and associated heterotrophic respiration. The model simulates tree gross and net photosynthesis, wood respiration, live root respiration, moss gross and net photosynthesis, and heterotrophic respiration (decomposition of root litter, young needle and moss litter, and humus). These values can be combined to generate predictions of total site net ecosystem exchange of carbon (NEE), total soil dark respiration (live roots + heterotrophs + live moss), spruce and moss net productivity, and net carbon accumulation in the soil. The files include source code and sample input and output files in ASCII format.
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This data set contains the major soil properties of soil samples collected at the tower flux sites in the NSA. The soil samples were collected by Hugo Veldhuis and his staff from the University of Manitoba. The mineral soil samples were largely analyzed by Barry Goetz, under the supervision of Dr. Harold Rostad at the University of Saskatchewan. The organic soil samples were largely analyzed by Peter Haluschak, under the supervision of Hugo Veldhuis at the Centre for Land and Biological Resources Research in Winnipeg, Manitoba. During the course of field investigation and mapping, selected surface and subsurface soil samples were collected for laboratory analysis. These samples were used as benchmark references for specific soil attributes in general soil characterization. Detailed soil sampling, description and laboratory analysis were performed on selected modal soils to provide examples of common soil physical and chemical characteristics in the study area. The soil properties that were determined include soil horizon; dry soil color; pH; bulk density; total, organic, and inorganic carbon; electric conductivity; cation exchange capacity; exchangeable sodium, potassium, calcium, magnesium, and hydrogen; water content at 0.01, 0.033, and 1.5 MPascals; nitrogen; phosphorus; particle size distribution; texture; pH of the mineral soil and of the organic soil; extractable acid; and sulfur.
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The BOREAS TE-20 team collected several data sets for use in developing and testing models of forest ecosystem dynamics. This data set contains measurements of site characteristics conducted in the SSA from 18-Jul-1994 to 30-Jul-1994.
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This data set was gridded from vector layers of soil maps that were received from Dr. Hugo Veldhuis, who did the original mapping in the field during 1994. The vector layers were gridded into raster files that cover the NSA-MSA and tower sites.
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The BOREAS TE-20 team collected several data sets for use in developing and testing models of forest ecosystem dynamics. This data set contains vector layers of soil maps that were received from Dr. Hugo Veldhuis, who did the original mapping in the field during 1994. The vector layers were converted to ARC/INFO EXPORT files. These data cover 1-kilometer diameters around each of the NSA tower sites, and another layer covers the NSA-MSA.
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The BOREAS TE-20 team collected several data sets for use in developing and testing models of forest ecosystem dynamics. This data set and documentation were compiled from field notes and other information provided by Hugo Veldhuis, who did the original soils mapping in the field during 1994. The information here describes the soils and landscape characteristics of the NSA-MSA and tower sites.
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The BOREAS TE-21 team collected data sets in support of its efforts to characterize and interpret information on the meteorology of boreal forest areas. Daily meteorological data were derived from half-hourly BOREAS TF and AMS mesonet measurements collected in the SSA and NSA for the period of 01-Jan-1994 until 31-Dec-1994.
&lt;br&gt;&lt;h4 id&#x3D;&quot;te22allm_490&quot;&gt;te22allm_490&lt;/h4&gt;
The BOREAS TE-22 team collected data sets in support of its efforts to characterize and interpret information on the forest structure of boreal vegetation in the SSA and NSA during the 1994 growing season.
&lt;br&gt;&lt;h4 id&#x3D;&quot;te22ring_491&quot;&gt;te22ring_491&lt;/h4&gt;
The BOREAS TE-22 team collected complete tree cores at several sites in the SSA and NSA in order to perform historical growth studies and relate the information to their modeling activities. The cores were collected during the summer of 1994 in the Northern and Southern Study Areas. A sample of the file types resulting from the analysis of the tree cores are provided.
&lt;br&gt;&lt;h4 id&#x3D;&quot;te23arch_492&quot;&gt;te23arch_492&lt;/h4&gt;
The BOREAS TE-23 team collected hemispherical photographs in support of its efforts to characterize and interpret information on estimates of canopy architecture and radiative transfer properties for most BOREAS study sites. Various OA, OBS, OJP, YJP, and YA sites in the boreal forest were measured from May to August 1994. The hemispherical photographs were used to derive values of LAI, Leaf angle, Gap fraction, and Clumping index. This documentation describes these derived values. The derived data are stored in tabular ASCII files. The hemispherical photographs are stored in the original set of 42 CD-ROMs, that were supplied by TE-23.
&lt;br&gt;&lt;h4 id&#x3D;&quot;te23mapp_359&quot;&gt;te23mapp_359&lt;/h4&gt;
The BOREAS TE-23 team collected map plot data in support of its efforts to characterize and interpret information on canopy architecture and understory cover at the BOREAS tower flux sites and selected auxiliary sites from May to August 1994. Mapped plots (typical dimensions 50 m x 60 m) were set up and characterized at all BOREAS forested tower flux and selected auxiliary sites. Detailed measurement of the mapped plots included 1) stand characteristics (location, density, basal area); 2) map locations DBH of all trees; 3) detailed geometric measures of a subset of trees (height, crown dimensions); and 4) understory cover maps. The data are stored in tabular ASCII files.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tf01soil_511&quot;&gt;tf01soil_511&lt;/h4&gt;
The BOREAS TF-01 team collected several data sets in support of its efforts to characterize and interpret soil information at the SSA-OA tower site in 1994 as part of BOREAS. Data sets collected include soil respiration, temperature, moisture, and gravimetric data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tf01tflx_512&quot;&gt;tf01tflx_512&lt;/h4&gt;
The BOREAS TF-01 team collected energy, carbon dioxide, and momentum flux data above the canopy along with meteorological and soils data at the BOREAS SSA-OA site from mid-April to the end of the year for 1996.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tf01uflx_513&quot;&gt;tf01uflx_513&lt;/h4&gt;
The BOREAS TF-01 team collected energy, carbon dioxide, and momentum flux data under the canopy along with meteorological and soils data at the BOREAS SSA-OA site from mid-October to mid-November of 1993 and throughout all of 1994.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tf1ch4_514&quot;&gt;tf1ch4_514&lt;/h4&gt;
The BOREAS TF-01 team collected various trace gas and energy flux data in its efforts to characterize the temporal energy and gas exchanges that occurred over the SSA-OA site. This data set contains methane (CH4) and nitrous oxide (N2O) fluxes that were measured at the BOREAS SSA-OA site. These fluxes were measured from 16-Apr to 16-Sep-1994.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tf2met_504&quot;&gt;tf2met_504&lt;/h4&gt;
Members of the BOREAS TF-02 team collected meteorological and ozone measurements from instruments mounted below a tethered balloon. These data were collected at the SSA-OA site to extend meteorological and ozone measurements made from the flux tower to heights of 300 m. The tethersonde operated during the fall of 1993 and the spring, summer, and fall of 1994.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tf02tflx_515&quot;&gt;tf02tflx_515&lt;/h4&gt;
The BOREAS TF-02 team collected energy, carbon dioxide, water vapor, and momentum flux data above the canopy and in profiles through the canopy, along with meteorological data at the BOREAS SSA-OA site. Above-canopy measurements began in early February and ran through mid-September of 1994. Measurements were collected over a longer period of 1994 than most BOREAS flux sites. Daily precipitation data from several gauges were also collected.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tf3acco2_360&quot;&gt;tf3acco2_360&lt;/h4&gt;
The BOREAS TF-03 and TGB-01 teams collected automated CO2 chamber flux data in their efforts to fully describe the CO2flux at the NSA-OBS site. This data set contains fluxes of CO2 at the NSA-OBS site measured using automated chambers. In addition to reporting the CO2flux, it reports chamber air temperature, moss temperature, and light levels during each measurement. The data set covers the period from 23-Sep-1995 through 26-Oct-1995 and from 28-May-1996 through 21-Oct-1996.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tf3tflxd_361&quot;&gt;tf3tflxd_361&lt;/h4&gt;
The BOREAS TF-03 team collected tower flux, surface meterological, and soil temperature data at the BOREAS NSA-OBS site continuously from the March 1994 through October 1996.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tf4ssafx_362&quot;&gt;tf4ssafx_362&lt;/h4&gt;
The BOREAS TF-04 team measured fluxes of carbon dioxide (CO2) and methane (CH4) across the soil-air interface in four ages of jack pine forest at the Southern Study Area of the Boreal Ecosystem Atmosphere Study (BOREAS) during August 1993 to March 1995. Gross and net flux of CO2 and flux of CH4 between soil and air are presented for 24 chamber sites in mature jack pine forest, 20-year old, 4- year old, and clear cut areas.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tf4ssasp_363&quot;&gt;tf4ssasp_363&lt;/h4&gt;
The BOREAS TF-04 team measured distributions of carbon dioxide (CO2) and methane (CH4) concentrations for the upper 5 meters of soil and unsaturated zone at the mature stand, upper 6 m at the 20-year old stand, and the upper 1m at the 8-year old stand and clear cut area at the Southern Study Area of the Boreal Ecosystem Atmosphere Study (BOREAS) during August 1993 to March 1995. Particle size and carbon content of the unsaturated deposits, precipitation, soil temperature and moisture, carbon and oxygen isotopes of soil CO2 and soil water chemistry are also presented.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tf04flux_451&quot;&gt;tf04flux_451&lt;/h4&gt;
The BOREAS TF-04 team collected energy, carbon dioxide, and water vapor flux data at the BOREAS SSA-YJP site during the growing season of 1994. In addition, meteorological data were collected both above and within the canopy.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tf5tflxd_364&quot;&gt;tf5tflxd_364&lt;/h4&gt;
The BOREAS TF-05 team collected tower flux data at the BOREAS Southern Study Area Old Jack Pine (SSA-OJP) site through the growing season of 1994.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tf6fxmet_365&quot;&gt;tf6fxmet_365&lt;/h4&gt;
The BOREAS TF-06 team collected surface energy flux and meteorology data at the SSA-YA site. The data characterize the energy flux and meteorological conditions at the site from 18-Jul to 20-Sep-1994. The data set does not contain any trace gas exchange measurements.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tf07flux_452&quot;&gt;tf07flux_452&lt;/h4&gt;
The BOREAS TF-07 team collected meteorological data as well as energy, carbon dioxide, water vapor, methane, and nitrous oxide flux data at the BOREAS SSA-OBS site. The data were collected from May 24 to September 19, 1994.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tf08ceil_453&quot;&gt;tf08ceil_453&lt;/h4&gt;
The BOREAS TF-08 team used ceilometers to collect data on the fraction of the sky covered with clouds and the cloud height. Included with these data is the surface-based lifting condensation level, derived from temperature and humidity values acquired at the flux tower at the NSA-OJP site. Ceilometer data were collected at the NSA-OJP site in 1994 and at the NSA-OJP and SSA-OBS sites in 1996.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tf08tflx_516&quot;&gt;tf08tflx_516&lt;/h4&gt;
The BOREAS TF-08 team collected energy, CO2, and water vapor flux data at the BOREAS NSA-OJP site during the growing season of 1994 and most of the year for 1996.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tf9brflx_366&quot;&gt;tf9brflx_366&lt;/h4&gt;
The BOREAS TF-09 team collected data which describe carbon dioxide and water vapor fluxes from foliage at the BOREAS SSA-OBS site from 07-April through 23-November-1996.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tf9tflxd_367&quot;&gt;tf9tflxd_367&lt;/h4&gt;
The BOREAS TF-09 team collected energy, carbon dioxide and water vapor flux data at the BOREAS SSA-OBS site during the growing season of 1994 and most of the year for 1996. From the winter of 1995 to 1996, soil temperature data were also collected and provided.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tf10fxmt_368&quot;&gt;tf10fxmt_368&lt;/h4&gt;
The BOREAS TF-10 team collected tower flux and meteorological data at two sites, a fen and a young jack pine forest, near Thompson, Manitoba, Canada, as part of BOREAS. A preliminary data set was assembled in August 1993 while field testing the instrument packages, and at both sites data were collected from 15-Aug to 31-Aug. The main experimental period was in 1994, when continuous data were collected from 08-Apr to 23-Sept at the fen site. A very limited experiment was run in the spring/summer of 1995, when the fen site tower was operated from 08-Apr to 14-Jun in support of a hydrology experiment in an adjoining, feeder basin. Upon examination of the 1994 data set, it became clear that the behavior of the heat, water, and carbon dioxide fluxes throughout the whole growing season was an important scientific question, and that the 1994 data record was not sufficiently long to capture the character of the seasonal behavior of the fluxes. Thus, the fen site was operated in 1996 in order to collect data from spring melt to autumn freeze-up. Data were collected from 29-Apr to 05-Nov at the fen site. All variables are presented as 30-minute averages.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tf11biom_369&quot;&gt;tf11biom_369&lt;/h4&gt;
The BOREAS TF-11 team collected several data sets in their efforts to fully describe the flux and site characteristics at the SSA-Fen site. This data set contains plant cover, standing crop of plant biomass, and estimated net primary productivity at each chamber site at the end of the 1994 field season. The measurements were conducted as part of a 2x2 factorial experiment in which we added carbon (300 g m-2 as wheat straw) and nitrogen (6 g m-2 as urea) to four replicate locations in the vicinity of the TF-11 tower.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tf11conc_370&quot;&gt;tf11conc_370&lt;/h4&gt;
The BOREAS TF-11 team collected several data sets in their efforts to fully describe the flux and site characteristics at the SSA-Fen site. This data set contains temperature, pH, and concentration profiles of methane and carbon dioxide within the surface 50 cm of peat. The measurements were conducted as part of a 2x2 factorial experiment in which we added carbon (300 g m-2 as wheat straw) and nitrogen (6 g m-2 as urea) to four replicate locations in the vicinity of the TF-11 tower. The data set covers the period from the first week of June 1994 through the second week of September, 1994.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tf11flux_371&quot;&gt;tf11flux_371&lt;/h4&gt;
The BOREAS TF-11 team collected several data sets in their efforts to fully describe the flux and site characteristics at the SSA-Fen site. This data set contains fluxes of methane and carbon dioxide at the SSA fen site measured using static chambers. The measurements were conducted as part of a 2x2 factorial experiment in which we added carbon (300 g m-2 as wheat straw) and nitrogen (6 g m-2 as urea) to four replicate locations in the vicinity of the TF-11 tower. In addition to siting and treatment variables, it reports air temperature and water table height relative to the average peat surface during each measurement. The data set covers the period from the first week of June 1994 through the second week of September, 1994.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tf11dcom_372&quot;&gt;tf11dcom_372&lt;/h4&gt;
The BOREAS TF-11 team collected several data sets in their efforts to fully describe the flux and site characteristics at the SSA-Fen site. This data set contains decomposition rates of a standard substrate (wheat straw) across treatments. The measurements were conducted as part of a 2x2 factorial experiment in which we added carbon (300 g m-2 as wheat straw) and nitrogen (6 g m-2 as urea) to four replicate locations in the vicinity of the TF-11 tower.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tf11sflm_455&quot;&gt;tf11sflm_455&lt;/h4&gt;
The BOREAS TF-11 team gathered a variety of data to complement their tower flux measurements collected at the SSA Fen site. The data described in this document were made by the TF-11 team at the SSA Fen site to quantify the effect that the films observed to form on open water surfaces had on the transfer of carbon dioxide and methane from the water to the air. Measurements of fluxes of carbon dioxide and methane were made in 1994 and in 1996 using the chamber flux method. A gas chromatograph and a LI-COR LI-6200 were used to measure concentrations and to calculate the fluxes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tf11leaf_456&quot;&gt;tf11leaf_456&lt;/h4&gt;
The BOREAS TF-11 team gathered a variety of data to complement their tower flux measurements collected at the SSA Fen site. This data set contains single-leaf gas exchange data from the SSA Fen site during 1994 and 1995. These leaf gas exchange properties were measured for the dominant vascular plants using portable gas exchange systems.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tf11soil_457&quot;&gt;tf11soil_457&lt;/h4&gt;
The BOREAS TF-11 team gathered a variety of data to complement their tower flux measurements collected at the SSA Fen site. These data are soil surface CO2 flux data at the SSA Fen site from 27-May-1994 to 23-Sep-1994 and from 13-May-1995 to 3-Oct-1995. A portable gas exchange system was used to make these measurements.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tf11lai_458&quot;&gt;tf11lai_458&lt;/h4&gt;
The BOREAS TF-11 team gathered a variety of data to complement their tower flux measurements collected at the SSA Fen site. These data are LAI measurements made by the TF-11 team throughout the 1995 growing season. The data include the LAI of plants that fall into six categories: total, Carex spp., Betula pumila, Menyanthes trifoliata, Salix spp., and other vascular plants.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tf11tfx_373&quot;&gt;tf11tfx_373&lt;/h4&gt;
The BOREAS TF-11 team collected energy, carbon dioxide, and methane flux data at the BOREAS SSA-Fen site during the growing seasons of 1994 and 1995.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgb1ccfd_374&quot;&gt;tgb1ccfd_374&lt;/h4&gt;
Chamber flux measurements were taken at the Northern Study Area (NSA) Old Jack Pine (OJP), Young Jack Pine (YJP), Old Black Spruce (OBS), and Beaver Pond (BP) sites during the summer of 1994. The purpose of these measurements was to examine the trace gas exchange between the atmosphere and the boreal soils. The BOREAS TGB-01 team made methane (CH4) and carbon dioxide (CO2) dark chamber flux measurements from 16- May-1994 through 13-Sep-1994. Gas samples were extracted approximately every 7 days from dark chambers and analyzed at the NSA lab facility.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgb1cfd_375&quot;&gt;tgb1cfd_375&lt;/h4&gt;
The BOREAS TGB-01 team made numerous measurements of trace gas concentrations and fluxes at various NSA sites. This data set contains half-hourly averages of ambient methane (CH4) measurements and calculated fluxes for the NSA-TF in 1996 and the NSA-BP and NSA-OJP tower sites in 1994. The purpose of this study was to determine the CH4 flux from the study area by measuring ambient CH4 concentrations. This flux can then be compared to the chamber flux measurements taken at the same sites.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgb1sfd_376&quot;&gt;tgb1sfd_376&lt;/h4&gt;
Chamber flux measurements were taken at the Boreal Ecosystem Atmosphere Study (BOREAS) Northern Study Area (NSA) Old Jack Pine (OJP) and Young Jack Pine (YJP) sites during the summer of 1994. The purpose of these measurements was to examine the trace gas exchange between the atmosphere and the boreal soils. The following is a description of the acquisition of data and the final datasets. The BOREAS TGB-01 team made sulfur hexaflouride (SF6) dark chamber flux measurements 16-May through 13-Sep-1994. Gas samples were extracted approximately every 7 days from dark chambers and analyzed at the NSA lab facility.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgbfenfx_378&quot;&gt;tgbfenfx_378&lt;/h4&gt;
The BOREAS TGB-03 team collected methane (CH4) chamber flux measurements at the NSA fen site during May-September 1994 and June-October 1996. Gas samples were extracted approximately every 7 days from chambers and analyzed at the NSA lab facility.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgbfenne_379&quot;&gt;tgbfenne_379&lt;/h4&gt;
The BOREAS TGB-01 and TGB-03 teams collected several data sets that contributed to understanding the measured trace gas fluxes over sites in the NSA. This data set contains NEE measurements collected with chambers at the NSA fen in 1994 and 1996. Gas samples were extracted approximately every 7 days from chambers and analyzed at the NSA lab facility.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgb3wd_380&quot;&gt;tgb3wd_380&lt;/h4&gt;
The BOREAS TGB-01 and TGB-03 teams collected several data sets that contributed to understanding the measured trace gas fluxes over sites in the NSA. This data set contains continuous and manual measurements of water level, air and soil temperatures at the four subsites within the NSA Tower Fen site complex. The measurements were taken to understand the thermal and hydrological gradients associated with each plant community present in the fen. Measurements were taken from May to September 1994 and May to October 1996.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgb3cofd_381&quot;&gt;tgb3cofd_381&lt;/h4&gt;
The BOREAS TGB-03 team collected methane and carbon dioxide (CH4, CO2) chamber flux measurements at the NSA Fen site, OBS, YJP, and auxiliary sites along Gillam Road and the 1989 burn site. Gas samples were extracted from chambers and analyzed at the NSA lab facility approximately every 7 days during May to September 1994 and June to October 1996.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgb03doc_459&quot;&gt;tgb03doc_459&lt;/h4&gt;
The BOREAS TGB-03 team collected Dissolved Organic Carbon (DOC) data during the summer of 1994 in the Northern Study Area. The purpose of this work was to establish the major sources, sinks and fluxes of dissolved organic carbon (DOC) in the Northern Study Area. Data on DOC concentrations taken from samples representing the major sources and sinks were to be combined with hydrologic measurements (e.g. precipitation, stream flow etc.) to calculate DOC fluxes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgb3plsp_382&quot;&gt;tgb3plsp_382&lt;/h4&gt;
The BOREAS TGB-03 team collected several data sets that contributed to understanding the measured trace gas fluxes over sites in the NSA. This data set contains information about the composition of plant species that were within the collars used to measure NEE. The species composition was identified to understand the differences in NEE among the various plant communities in the NSA fen. The data were collected in July of 1994 and 1996.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgb4flux_460&quot;&gt;tgb4flux_460&lt;/h4&gt;
The BOREAS TGB-04 team measured the exchange of heat, water, and CO2 between a boreal forest beaver pond and the atmosphere in the NSA for the ice-free period of BOREAS. The data cover the period of May 28 to September 18, 1994.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgb4wsed_461&quot;&gt;tgb4wsed_461&lt;/h4&gt;
The BOREAS TGB-04 team collected several data sets in support of their flux tower measurements at the NSA Beaver Pond site. This data set contains water and sediment temperature data collected from May to September 1994.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgb5nnfd_383&quot;&gt;tgb5nnfd_383&lt;/h4&gt;
The BOREAS TGB-05 team made several measurements of trace gas concentrations and fluxes at various NSA sites. This data set contains biogenic soil emissions of nitric oxide and nitrous oxide that were measured over a wide range of spatial and temporal site parameters. Since very little is known about biogenic soil emissions of nitric oxide and nitrous oxide from the Boreal forest, the goal of the measurements was to characterize the biogenic soil fluxes of nitric oxide and nitrous oxide from black spruce and jack pine areas in the boreal forest. The diurnal variation and monthly variation of the emissions was examined as well as the impact of wetting through natural or artificial means. Temporally, the data cover mid-August 1993, June to August 1994, and mid-July 1995.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgb5cflx_384&quot;&gt;tgb5cflx_384&lt;/h4&gt;
The BOREAS TGB-05 team collected a variety of trace gas concentration and flux measurements at several NSA sites. This data set contains carbon dioxide (CO2), methane (CH4), and carbon monoxide (CO) chamber flux measurements conducted in 1994 at upland forest sites that experienced stand- replacement fires. These measurements were acquired to understand the impact of fires on soil biogeochemistry and related changes in trace gas exchange in boreal forest soils. Relevant ancillary data, including data concerning the soil temperature, solar irradiance, and information from nearby unburned control sites, are included to provide a basis for modeling the regional impacts of fire and climate changes on trace gas biogeochemistry.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgb5docd_385&quot;&gt;tgb5docd_385&lt;/h4&gt;
The BOREAS TGB-05 team collected several data sets related to carbon and trace gas fluxes and concentrations in the NSA. This data set contains concentrations of dissolved organic and inorganic carbon species from water samples collected at various NSA sites. In particular, this set covers the NSA Tower Beaver Pond Site and the NSA Gillam Road Beaver Pond Site, including data from all visits to open water sampling locations during the BOREAS field campaigns from April to September 1994.
&lt;br&gt;&lt;h4 id&#x3D;&quot;fhstmanr_386&quot;&gt;fhstmanr_386&lt;/h4&gt;
This raster format data set covers the province of Manitoba. The data were gridded into the AEAC projection from the original vector data. The original vector data were produced by Forestry Canada from hand-drawn boundaries of fires on photocopies of 1:250,000-scale maps. The locational accuracy of the data is considered fair to poor. When the locations of some fire boundaries were compared to Landsat TM images, they were found to be off by as much as a few kilometers. This problem should be kept in mind when using these data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;fhstmanv_387&quot;&gt;fhstmanv_387&lt;/h4&gt;
This vector format data set covers the province of Manitoba and was produced by Forestry Canada from hand-drawn boundaries of fires on photocopies of 1:250,000 scale maps. The locational accuracy of the data is considered fair to poor. When the locations of some fire boundaries were compared to Landsat TM images, they were found to be off by as much as a few kilometers.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgb6chrc_388&quot;&gt;tgb6chrc_388&lt;/h4&gt;
The BOREAS TGB-06 team collected soil methane measurements at several sites in the SSA and NSA. This data set contains soil methane consumption (bacterial CH4 oxidation) and associated 13C fractionation effects in samples that were collected at various sites in 1994 and 1996 from enclosures (chambers). Methane 13C data in soil gas samples from the NSA YJP and OJP sites for 1994 and 1996 are also given. Additional data on the isotopic composition of methane (carbon and hydrogen isotopes) produced in the NSA beaver ponds and fen bog in 1993 and 1994 are given as well.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgb7aaho_389&quot;&gt;tgb7aaho_389&lt;/h4&gt;
The BOREAS TGB-07 team measured the concentration and flux of several agricultural pesticides in air, rainwater, and dry deposition samples in order to determine the associated yearly deposition rates. This data set contains information on the ambient air concentration of seven herbicides [2,4-dichlorophenoxyacidic_acid (2,4-D), bromoxynil, dicamb, 2-methyl-4-chlorophenoxyacetic acid (MCPA), triallate, trifluralin, and diclop-methyl] known to appear in the atmosphere of the Canadian prairies. Also, the concentration of three herbicides (atrazine, alaclor and metolachlor), two groups of insecticides (lindane and breakdown products and dichlro-diphenyl-trichloroethane (DDT) and breakdown products), and several polychlorinated biphenyls commonly used in the central United States were measured. All of these chemicals are reported, in the literature, to be transported in the atmosphere. Many have been reported to occur in boreal and arctic food chains. The sampling was carried out from June 16 to August 13, 1993 and May 4 to July 20, 1994 at the BOREAS site in the Prince Albert National Park (Waskesiu).
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgb7ddho_390&quot;&gt;tgb7ddho_390&lt;/h4&gt;
The BOREAS TGB-07 team measured the concentration and flux of several agricultural pesticides in air, rainwater, and dry deposition samples in order to determine the associated yearly deposition rates. This data set contains information on the dry deposition flux of seven herbicides [2,4-dichlorophenoxyacidic_acid (2,4-D), bromoxynil, dicamb, 2-methyl-4-chlorophenoxyacetic acid (MCPA), triallate, trifluralin, and diclop-methyl] known to appear in the atmosphere of the Canadian prairies. Also, the concentration of three herbicides (atrazine, alaclor and metolachlor), two groups of insecticides (lindane and breakdown products and dichlro-diphenyl-trichloroethane (DDT) and breakdown products), and several polychlorinated biphenyls commonly used in the central United States were measured. All of these chemicals are reported, in the literature, to be transported in the atmosphere. Many have been reported to occur in boreal and arctic food chains. The sampling was carried out from June 16 to August 13, 1993 and May 4 to July 20, 1994 at the BOREAS site in the Prince Albert National Park (Waskesiu).
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgb7rwho_391&quot;&gt;tgb7rwho_391&lt;/h4&gt;
The BOREAS TGB-07 team measured the concentration and flux of several agricultural pesticides in air and rainwater samples in order to determine the associated yearly deposition rates. This data set contains information on the rainwater concentration of seven herbicides [2,4-dichlorophenoxyacidic_acid (2,4-D), bromoxynil, dicamb, 2-methyl-4-chlorophenoxyacetic acid (MCPA), triallate, trifluralin, and diclop-methyl] known to appear in the atmosphere of the Canadian prairies. Also, the concentration of three herbicides (atrazine, alaclor and metolachlor), two groups of insecticides (lindane and breakdown products and dichlro-diphenyl-trichloroethane (DDT) and breakdown products), and several polychlorinated biphenyls commonly used in the central United States were measured. All of these chemicals are reported, in the literature, to be transported in the atmosphere. Many have been reported to occur in boreal and arctic food chains. The sampling was carried out from June 16 to August 13, 1993 and May 4 to July 20, 1994 at the BOREAS site in the Prince Albert National Park (Waskesiu).
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgb8mono_392&quot;&gt;tgb8mono_392&lt;/h4&gt;
The TGB-08 team collected data to investigate the controls over non-methane hydrocarbon (NMHC) fluxes from boreal forest tree species. This data set contains measurements of monoterpene concentrations in collected foliar gas emissions and foliar samples. The data were collected at the Old Jack Pine (OJP) and Old Black Spruce(OBS) tower-flux sites in the SSA and were the locus for the monoterpene emission measurements. These areas contained mature stands of jack pine and black spruce and were the focal sites in the BOREAS program for studies of biosphere/atmosphere exchange from these two habitat types. The OBS site is situated in a black spruce/sphagnum bog with the largest trees 155 years old and 10-15 m. tall. The OJP site is in a jack pine forest, 80 to 120 years old, which lies on a sandy bench of glacial outwash with the largest tree standing 15 m. tall. Temporally, the data cover the period of 24-May-94 to 19-Sep-94.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgb8prds_393&quot;&gt;tgb8prds_393&lt;/h4&gt;
The TGB-08 team collected data to investigate the controls over non-methane hydrocarbon (NMHC) fluxes from boreal forest tree species. This data set includes measurements of photosynthetic rates at mature Jack Pine and Black spruce sites. The two areas used in this research were in the Southern Study Area (SSA) of the BOREAS region: the SSA Old Jack Pine (OJP) and Old Black Spruce(OBS) tower-flux locations. These areas contained mature stands of jack pine and black spruce and were the focal sites in the BOREAS program for studies of biosphere/atmosphere exchange from these two habitat types. The OBS site is situated in a black spruce/sphagnum bog with the largest trees 155 years old and 10-15 m. tall. The OJP site is in a jack pine forest, 80 to 120 years old, which lies on a sandy bench of glacial outwash with the largest tree standing 15 m. tall. Temporally, the data cover the period of 24-May-94 to 19-Sep-94.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgb8scds_394&quot;&gt;tgb8scds_394&lt;/h4&gt;
The TGB-08 team collected data to investigate the controls over non-methane hydrocarbon (NMHC) fluxes from boreal forest tree species. This data set includes measurements of starch concentrations in foliar samples at mature Jack Pine and Black spruce sites. The two areas used in this research were in the Southern Study Area (SSA) of the BOREAS region: the SSA Old Jack Pine (OJP) and Old Black Spruce(OBS) tower-flux locations. These areas contained mature stands of jack pine and black spruce and were the focal sites in the BOREAS program for studies of biosphere/atmosphere exchange from these two habitat types. The OBS site is situated in a black spruce/sphagnum bog with the largest trees 155 years old and 10-15 m. tall. The OJP site is in a jack pine forest, 80 to 120 years old, which lies on a sandy bench of glacial outwash with the largest tree standing 15 m. tall. Temporally, the data cover the period of 24-May-94 to 19-Sep-94.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgb9nmhc_395&quot;&gt;tgb9nmhc_395&lt;/h4&gt;
THE BOREAS TGB-09 team collected data in order to inventory and quantify the anthropogenic and biogenic NMHC&amp;#39;s over the BOREAS study areas. This data set contains concentration and mixing ratio values for several NMHC&amp;#39;s collected at the BOREAS SSA from 27-MAY-1994 to 15-SEP-1994.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgb10ocd_396&quot;&gt;tgb10ocd_396&lt;/h4&gt;
The BOREAS TGB-10 team collected several trace gas data sets in their efforts to determine the role of biogenic hydrocarbon emissions with respect to boreal forest carbon cycles. This data set contains measured peroxide (H2O2 and total organic peroxides (ROOH)) and ozone concentrations as well as, H2O2 and ROOH deposition velocities. These data were obtained at the SSA Old Jack Pine site from May to September 1994.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgb10ofd_397&quot;&gt;tgb10ofd_397&lt;/h4&gt;
The BOREAS TGB-10 team collected several trace gas data sets in their efforts to determine the role of biogenic hydrocarbon emissions with respect to boreal forest carbon cycles. This oxidant data set contains measured peroxide (H2O2 and total organic peroxides (ROOH)) and ozone concentrations as well as, H2O2 and ROOH deposition velocities. These data were obtained at the SSA Old Jack Pine site during the summer of 1994.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgb10voc_398&quot;&gt;tgb10voc_398&lt;/h4&gt;
The BOREAS TGB-10 team collected several trace gas data sets in their efforts to determine the role of biogenic hydrocarbon emissions with respect to boreal forest carbon cycles. This data set contains measured VOC concentrations. These data were obtained at the SSA Old Jack Pine site from May to September 1994.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgb12ci_399&quot;&gt;tgb12ci_399&lt;/h4&gt;
The BOREAS TGB-12 team made measurements of soil carbon inventories, carbon concentration in soil gases, and rates of soil respiration at several sites to estimate the rates of carbon accumulation and turnover in each of the major vegetation types. This data set contains information on the carbon isotopic content of carbon dioxide sampled from soils.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgb12rad_400&quot;&gt;tgb12rad_400&lt;/h4&gt;
The BOREAS TGB-12 team made measurements of soil carbon inventories, carbon concentration in soil gases, and rates of soil respiration at several sites to estimate the rates of carbon accumulation and turnover in each of the major vegetation types. Sampling strategies for soils were designed to take advantage of local fire chronosequences, so that the accumulation of C in regrowing mosses could be determined. All the data are used to (1) calculate the inventory of C and N in moss and mineral soil layers at NSA sites (2) determine the rates of input and turnover (using both accumulation since the last stand-killing fire and radiocarbon data) and (3) link changes in soil respiration rate to shifts in the 14C content of soil CO2 to determine the average &amp;#39;age&amp;#39; respired CO2. These 222Rn activity data were collected from 15-NOV-1993 to 16-AUG-1994 over the NSA sites.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgb12rfd_401&quot;&gt;tgb12rfd_401&lt;/h4&gt;
The BOREAS TGB-12 team made measurements of soil carbon inventories, carbon concentration in soil gases, and rates of soil respiration at several sites to estimate the rates of carbon accumulation and turnover in each of the major vegetation types. Sampling strategies for soils were designed to take advantage of local fire chronosequences, so that the accumulation of carbon in new moss growth could be determined. All the data are used to 1) calculate the inventory of carbon and nitrogen in moss and mineral soil layers at NSA sites, 2) determine the rates of input and turnover (using both accumulation since the last stand-killing fire and radiocarbon data), and 3) link changes in soil respiration rate to shifts in the 14C content of soil CO2 to determine the average &amp;#39;age&amp;#39; respired CO2. These 222Rn flux data were collected from 15-NOV-1993 to 16-AUG-1994 over the NSA sites.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgb12cfd_517&quot;&gt;tgb12cfd_517&lt;/h4&gt;
The BOREAS TGB-12 team made measurements of soil carbon inventories, carbon concentration in soil gases, and rates of soil respiration at several sites. This data set provides: (1) estimates of soil carbon stocks by horizon based on soil survey data and analyses of data from individual soil profiles; (2) estimates of soil carbon fluxes based on stocks, fire history, drainage, and soil C inputs and decomposition constants based on field work using radiocarbon analyses; (3) fire history data estimating age ranges of time since last fire; (4) a raster image and an associated soils table file from which area-weighted maps of soil carbon and fluxes and fire history may be generated. This data set was created from raster files, soil polygon data files, and detailed lab analysis of soils data that were received from Hugo Veldhuis who did the original mapping in the field during 1994. Also used were soils data from Susan Trumbore and Jennifer Harden (BOREAS TGB-12). The binary raster file covers a 733 km^2 area within the NSA-MSA.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgb12scd_402&quot;&gt;tgb12scd_402&lt;/h4&gt;
The BOREAS TGB-12 team made measurements of soil carbon inventories, carbon concentration in soil gases, and rates of soil respiration at several sites to estimate the rates of carbon accumulation and turnover in each of the major vegetation types. TGB-12 data sets include soil properties at tower and selected auxiliary sites in the BOREAS NSA and data on the seasonal variations in the radiocarbon content of CO2 in the soil atmosphere at NSA tower sites. The sampling strategies for soils were designed to take advantage of local fire chronosequences, so that the accumulation of C in areas of moss regrowth could be determined. These data are used to calculate the inventory of C and N in moss and mineral soil layers at NSA sites and to determine the rates of input and turnover (using both accumulation since the last stand-killing fire and radiocarbon data). This data set includes physical parameters needed to determine carbon and nitrogen inventory in soils. The data were collected discontinuously from August 1993 to July 1996.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgb12sci_558&quot;&gt;tgb12sci_558&lt;/h4&gt;
During 1993 and 1994, the BOReal Ecosystem-Atmosphere Study (BOREAS) Trace Gas and Biogeochemistry team #12 (TGB-12) collected several data sets to support their analysis of soil carbon content in the Northern Study Area (NSA). The primary data set (BOREAS TGB-12 Soil Carbon Data over the NSA) is described in some detail. Other ancillary information was stored and provided in two sets of soil pit description and surface vegetation transect files. In addition, a site description file provides more information on the positioning of the sampling sites. These files contain additional information that complements the data contained in the primary data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ams_cs93_403&quot;&gt;ams_cs93_403&lt;/h4&gt;
Canadian AES personnel collected data related to surface and atmospheric meteorological conditions over the BOREAS Region. This data set contains 15 minute meteorological data from 14 automated meteorology stations located across the BOREAS region. Included in this data are parameters of date, time, mean sea level pressure, station pressure, temperature, dewpoint, wind speed, resultant wind speed, resultant wind direction, peak wind, precipitation, maximum temperature in the last hour, minimum temperature in the last hour, pressure tendency, liquid precipitation in the last hour, relative humidity, precipitation from a weighing gauge, and snow depth. Temporally, the data cover the period of August 1993 to December 1996.
&lt;br&gt;&lt;h4 id&#x3D;&quot;marsii94_407&quot;&gt;marsii94_407&lt;/h4&gt;
Canadian AES personnel collected several data sets related to surface and atmospheric meteorological conditions over the BOREAS region. This data set contains 15-minute meteorological data from six MARSII meteorology stations in the BOREAS region in Canada. Parameters include site, time, temperature, dewpoint, visibility, wind speed, wind gust, wind direction, two cloud groups, precipitation, and station pressure. Temporarily, the data cover the period of May to September 1994. Geographically, the stations are spread across the provinces of Saskatchewan and Manitoba.
&lt;br&gt;&lt;h4 id&#x3D;&quot;readac_d_408&quot;&gt;readac_d_408&lt;/h4&gt;
Canadian AES personnel collected and processed data related to surface atmospheric meteorological conditions over the BOREAS region. This data set contains 15 minute meteorological data from one READAC meteorology station in Hudson Bay, Saskatchewan. Parameters include day, time, type of report, sky condition, visibility, mean sea level pressure, temperature, dewpoint, wind, altimeter, opacity, minimum and maximum visibility, station pressure, minimum and maximum air temperature, a wind group, precipitation, and precipitation in the last hour. The data were collected non-continuously from 24-May-1994 to 20-Sep-1994.
&lt;br&gt;&lt;h4 id&#x3D;&quot;samsa94d_462&quot;&gt;samsa94d_462&lt;/h4&gt;
The Saskatchewan Research Council (SRC) collected surface meteorological and radiation data from December, 1993 until Decemb er 1996. The data set is comprised of the Suite A (meteorological and energy balance measurements) and Suite B (diffuse sol ar and longwave measurements) components. Suite A measurements were taken at each of ten sites and suite B measurements were made at five of the suite A sites. These data cover an area of roughly 1000 km by 1000 km (a large portion of northern Man itoba and northern Saskatchewan). The measurement network was designed to provide researchers with a sufficient record of n ear-surface meteorological and radiation measurements.
&lt;br&gt;&lt;h4 id&#x3D;&quot;boreas_cds_1350&quot;&gt;BOREAS_CDS_1350&lt;/h4&gt;
This data set provides Boreal Ecosystem-Atmosphere Study (BOREAS) project information and data collected at selected sites in the boreal forest of Saskatchewan and Manitoba, Canada from 1993 through 1996. The data include surface, airborne, and satellite-based observations. Note that all of the data products on these CDs have been archived as separate BOREAS data sets by the ORNL DAAC and in many cases the published data are later versions. Users should search for BOREAS data among these individual data sets. These data were originally distributed on 12 CD-ROMs, but are now archived as 12 zip files to ensure historical completeness of the BOREAS data record.
&lt;br&gt;&lt;h4 id&#x3D;&quot;soil125r_309&quot;&gt;soil125r_309&lt;/h4&gt;
This data set consists of GIS layers that describe the soils of the BOREAS SSA. The original data were submitted as vector layers that were gridded by BOREAS staff to a 30-meter pixel size in the AEAC projection. These data layers include the soil code (which relates to the soil name), modifier (which also relates to the soil name), and extent (indicating the extent that this soil exists within the polygon). There are three sets of these layers representing the primary, secondary, and tertiary soil characteristics. Thus, there is a total of nine layers in this data set along with supporting files. The data are stored in binary, image format files.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tgb1ccsd_377&quot;&gt;tgb1ccsd_377&lt;/h4&gt;
The BOREAS TGB-01 team made numerous measurements of trace gas concentrations and fluxes at various NSA sites. This data set contains methane (CH4) and carbon dioxide (CO2) concentrations in soil profiles from the NSA-OJP, NSA-OBS, NSA-YJP, and NSA-BP sites during the period of 23-May to 20-Sep-1994. The soil gas sampling profiles of CH4 and CO2 were completed to quantify controls on CO2 and CH4 fluxes in the boreal forest.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.ornldaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA BigFoot Project</title>
      <link>https://registry.opendata.aws/nasa-bigfoot</link>
      <guid>https://registry.opendata.aws/nasa-bigfoot</guid>
      <description>The BigFoot project gathered field data for selected EOS Land Validation Sites in North America from 1999 to 2003. Data collected and derived for varying intervals at the BigFoot sites and archived with this data set include FPAR, nitrogen content, allometry equations, root biomass, LAI, tree biomass, soil respiration, NPP, landcover images, and vegetation inventories.Each site is representative of one or two distinct biomes, including the Arctic tundra; boreal evergreen needleleaf forest; temperate cropland, grassland, and deciduous broadleaf forest; desert grassland and shrubland. The project collected multi-year, in situ measurements of ecosystem structure and functional characteristics related to the terrestrial carbon cycle at the sites listed in Table 1. Companion files include documentation of measurement data, site and plot locations (Figure 2), and plot photographs for the SEVI and TUND sites (Figure 3).BigFoot Project Background: Reflectance data from MODIS, the Moderate Resolution Imaging Spectrometer onboard NASA&amp;#39;s Earth Observing System (EOS) satellites Terra and Aqua ( &lt;a href&#x3D;&quot;http://landval.gsfc.nasa.gov/MODIS/index.php&quot;&gt;http://landval.gsfc.nasa.gov/MODIS/index.php&lt;/a&gt; ), was used to produce several science products including land cover, leaf area index (LAI), gross primary production (GPP), and net primary production (NPP). The overall goal of the BigFoot Project was to provide validation of these products. To do this, BigFoot combined ground measurements, additional high-resolution remote-sensing data, and ecosystem process models at six flux tower sites representing different biomes to evaluate the effects of the spatial and temporal patterns of ecosystem characteristics on MODIS products. BigFoot characterized up to a 7 x 7 km area (49 1-km MODIS pixels) surrounding the CO2 flux towers located at six of the nine BigFoot sites. The sampling design allowed the Project to examine scales and spatial patterns of these properties, the inter-annual variability and validity of MODIS products, and provided for a field-based ecological characterization of the flux tower footprint. BigFoot was funded by NASA&amp;#39;s Terrestrial Ecology Program.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpp_surfaces_749&quot;&gt;GPP_surfaces_749&lt;/h4&gt;
The BigFoot project gathered Gross Primary Production (GPP) data for nine EOS Land Validation Sites located from Alaska to Brazil from 2000 to 2004. Each site is representative of one or two distinct biomes, including the Arctic tundra; boreal evergreen needleleaf forest; temperate cropland, grassland, evergreen needleleaf forest, and deciduous broadleaf forest; desert grassland and shrubland; and tropical evergreen broadleaf forest. At this time we are archiving Northern Old Black Spruce (NOBS - BOREAS NSA, Canada) and Harvard Forest LTER (HARV - Massachusetts, USA) data collected in 2001.The GPP surfaces were produced by a spatial version of an ecosystem process model named, Biome-BGC. Inputs to the model included Landsat ETM+ derived Land Cover and LAI, tower derived meteorological variables, and a set of site level ecophysical parameters. The model was calibrated using field measured NPP and validated by tower derived estimates of GPP. For an in depth discussion of methods used to produce these surfaces, please see Turner et al. (2003).Each BigFoot GPP product covers a 7 x 7 km extent and consists of the GPP surface in BIP format (280 rows by 280 columns by 365 bands at 25 meter resolution) and an accompanying text file which provides metadata specific to the image (such as projection, data type, etc). Additional information on GPP surface development can be found on the BigFoot website at &lt;a href&#x3D;&quot;http://www.fsl.orst.edu/larse/bigfoot/ovr_mthd.html.BigFoot&quot;&gt;http://www.fsl.orst.edu/larse/bigfoot/ovr_mthd.html.BigFoot&lt;/a&gt; Project Background: Reflectance data from MODIS, the Moderate Resolution Imaging Spectrometer onboard NASA&amp;#39;s Earth Observing System (EOS) satellite Terra (&lt;a href&#x3D;&quot;http://landval.gsfc.nasa.gov/MODIS/index.php&quot;&gt;http://landval.gsfc.nasa.gov/MODIS/index.php&lt;/a&gt;), is used to produce several science products including land cover, leaf area index (LAI), gross primary production (GPP) and net primary production (NPP). The overall goal of the BigFoot Project was to provide validation of these products. To do this, BigFoot combined ground measurements, additional high resolution remote sensing data, and ecosystem process models at nine flux tower sites representing different biomes to evaluate the effects of the spatial and temporal patterns of ecosystem characteristics on MODIS products. BigFoot characterized up to a 7 x 7 km area (49 MODIS pixels) surrounding the CO2 flux towers located at each of the nine sites. We collected multi-year, in situ measurements of ecosystem structure and functional characteristics related to the terrestrial carbon cycle. Our sampling design allowed us to examine scales and spatial pattern of these properties, the inter-annual variability and validity of MODIS products, and provided for a field-based ecological characterization of the flux tower footprint. BigFoot was funded by NASA&amp;#39;s Terrestrial Ecology Program.For more details on the BigFoot Project, please visit the website: &lt;a href&#x3D;&quot;http://www.fsl.orst.edu/larse/bigfoot/index.html&quot;&gt;http://www.fsl.orst.edu/larse/bigfoot/index.html&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;land_cover_surfaces_748&quot;&gt;Land_Cover_surfaces_748&lt;/h4&gt;
The BigFoot project gathered data for nine EOS Land Validation Sites located from Alaska to Brazil from 2000 to 2003. Each site is representative of one or two distinct biomes, including the Arctic tundra; boreal evergreen needleleaf forest; temperate cropland, grassland, evergreen needleleaf forest, and deciduous broadleaf forest; desert grassland and shrubland; and tropical evergreen broadleaf forest. These surfaces were produced from Landsat ETM+ imagery to explicitly characterize the land cover at the BigFoot Sites to provide validation of the MODIS land cover product. The land cover scheme is consistent with the categories defined by the MOD12 IGBP (&lt;a href&#x3D;&quot;http://geography.bu.edu/landcover/userguidelc/index.html&quot;&gt;http://geography.bu.edu/landcover/userguidelc/index.html&lt;/a&gt;) strategy. Each BigFoot land cover product covers approximately a 7 x 7 km extent and consists of the land cover surface image in standard geotiff format, an accompanying text file which provides metadata specific to the image (such as projection, data type, class names, etc), and associated auxiliary and world files. For an in depth discussion of methods used to produce these surfaces, please see references.Additional information on land cover surface development can be found on the BigFoot website at &lt;a href&#x3D;&quot;http://www.fsl.orst.edu/larse/bigfoot/ovr_mthd.html.BigFoot&quot;&gt;http://www.fsl.orst.edu/larse/bigfoot/ovr_mthd.html.BigFoot&lt;/a&gt; Project Background:Reflectance data from MODIS, the Moderate Resolution Imaging Spectrometer onboard NASA&amp;#39;s Earth Observing System (EOS) satellite Terra (&lt;a href&#x3D;&quot;http://landval.gsfc.nasa.gov/MODIS/index.php&quot;&gt;http://landval.gsfc.nasa.gov/MODIS/index.php&lt;/a&gt;), is used to produce several science products including land cover, leaf area index (LAI) and net primary production (NPP). The overall goal of the BigFoot Project was to provide validation of these products. To do this, BigFoot combined ground measurements, additional high resolution remote sensing data, and ecosystem process models at nine flux tower sites representing different biomes to evaluate the effects of the spatial and temporal patterns of ecosystem characteristics on MODIS products. BigFoot characterized up to a 7 x 7 km area (49 MODIS pixels) surrounding the CO2 flux towers located at each of the nine sites. We collected multi-year, in situ measurements of ecosystem structure and functional characteristics related to the terrestrial carbon cycle. Our sampling design allowed us to examine scales and spatial pattern of these properties, the inter-annual variability and validity of MODIS products, and provided for a field-based ecological characterization of the flux tower footprint. BigFoot was funded by NASA&amp;#39;s Terrestrial Ecology Program.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lai_surfaces_747&quot;&gt;LAI_surfaces_747&lt;/h4&gt;
The BigFoot project gathered leaf area index (LAI) data for nine EOS Land Validation Sites located from Alaska to Brazil from 2000 to 2003. Each site is representative of one or two distinct biomes, including the Arctic tundra; boreal evergreen needleleaf forest; temperate cropland, grassland, evergreen needleleaf forest, and deciduous broadleaf forest; desert grassland and shrubland; and tropical evergreen broadleaf forest. LAI was measured at plots within each site for at least two years using standard direct and optical methods at each site. Direct measurement approaches included periodic area harvest for non-forest sites and application of allometric equations to tree diameter data for forest sites. LAI was also estimated indirectly using the Li-Cor LAI-2000 Plant Canopy Analyzers (Gower et al. 1999). LAI was measured three times each year at the forest sites and four to six times at other sites depending upon the phenology of LAI development for a given ecosystem. To develop LAI surfaces at any given site, the Landsat ETM+ image closest in date to maximum LAI was chosen as a reference and images from other dates radiometrically normalized to it. Each LAI surface has a grain of 25 meters and covers a 7 x 7 km extent. The data set consists of the LAI surface images in standard geotiff format, an accompanying text file which provides metadata specific to the image (such as projection, data type, class names, etc), and associated auxiliary and world files. Additional information on LAI measurements and surface development can be found on the BigFoot website at &lt;a href&#x3D;&quot;http://www.fsl.orst.edu/larse/bigfoot/ovr_mthd.html&quot;&gt;http://www.fsl.orst.edu/larse/bigfoot/ovr_mthd.html&lt;/a&gt;. BigFoot Project Background: Reflectance data from MODIS, the Moderate Resolution Imaging Spectrometer onboard NASA&amp;#39;s Earth Observing System (EOS) satellite Terra (&lt;a href&#x3D;&quot;http://landval.gsfc.nasa.gov/MODIS/index.php&quot;&gt;http://landval.gsfc.nasa.gov/MODIS/index.php&lt;/a&gt;), is used to produce several science products including land cover, leaf area index (LAI) and net primary production (NPP). The overall goal of the BigFoot Project was to provide validation of these products. To do this, BigFoot combined ground measurements, additional high resolution remote sensing data, and ecosystem process models at nine flux tower sites representing different biomes to evaluate the effects of the spatial and temporal patterns of ecosystem characteristics on MODIS products. BigFoot characterized up to a 7 x 7 km area (49 MODIS pixels) surrounding the CO2 flux towers located at each of the nine sites. We collected multi-year, in situ measurements of ecosystem structure and functional characteristics related to the terrestrial carbon cycle. Our sampling design allowed us to examine scales and spatial pattern of these properties, the inter-annual variability and validity of MODIS products, and provided for a field-based ecological characterization of the flux tower footprint. BigFoot was funded by NASA&amp;#39;s Terrestrial Ecology Program.
&lt;br&gt;&lt;h4 id&#x3D;&quot;meteorological_1065&quot;&gt;Meteorological_1065&lt;/h4&gt;
The BigFoot Project has compiled daily meteorological measurements for nine EOS Land Validation Sites located from Alaska to Brazil from 1991 to 2004. Each site is representative of one or two distinct biomes, including the Arctic tundra; boreal evergreen needleleaf forest; temperate cropland, grassland, evergreen needleleaf forest, and deciduous broadleaf forest; desert grassland and shrubland; and tropical evergreen broadleaf forest. The BigFoot Project needed meteorological data to run the ecosystem process models used for scaling GPP and NPP products, for monitoring interannual variability, and for model testing. Meteorological data were obtained from various agencies collecting data in the vicinity of the BigFoot sites and for more recent years, collected on co-located CO2 flux measurement towers. A comparable set of original measurements from all sites were aggregated to a common daily time step for use in the BIOME-BGC model.
&lt;br&gt;&lt;h4 id&#x3D;&quot;npp_surfaces_750&quot;&gt;NPP_surfaces_750&lt;/h4&gt;
The BigFoot project gathered Net Primary Production (NPP) data for nine EOS Land Validation Sites located from Alaska to Brazil from 2000 to 2004. Each site is representative of one or two distinct biomes, including the Arctic tundra; boreal evergreen needleleaf forest; temperate cropland, grassland, evergreen needleleaf forest, and deciduous broadleaf forest; desert grassland and shrubland; and tropical evergreen broadleaf forest. At this time we are archiving Northern Old Black Spruce (NOBS - BOREAS NSA, Canada) and Harvard Forest LTER (HARV - Massachusetts, USA) data collected in 2001.The NPP surfaces were produced by a spatial version of an ecosystem process model named, Biome-BGC. Inputs to the model included Landsat ETM+ derived Land Cover and LAI, tower derived meteorological variables, and a set of site-level ecophysical parameters. The model was calibrated using field measured NPP and validated by tower derived estimates of GPP. Each BigFoot NPP product covers a 7 x 7 km extent and consists of the NPP surface in ASCII Raster (BIL - Band Interleaved by Line) format (280 rows by 280 columns at 25 meter resolution) and an accompanying text file which provides metadata specific to the image (such as projection, data type, etc).Additional information on NPP surface development can be found on the BigFoot website at &lt;a href&#x3D;&quot;http://www.fsl.orst.edu/larse/bigfoot/ovr_mthd.html.BigFoot&quot;&gt;http://www.fsl.orst.edu/larse/bigfoot/ovr_mthd.html.BigFoot&lt;/a&gt; Project Background: Reflectance data from MODIS, the Moderate Resolution Imaging Spectrometer onboard NASA&amp;#39;s Earth Observing System (EOS) satellite Terra (&lt;a href&#x3D;&quot;http://landval.gsfc.nasa.gov/MODIS/index.php&quot;&gt;http://landval.gsfc.nasa.gov/MODIS/index.php&lt;/a&gt;), is used to produce several science products including land cover, leaf area index (LAI), gross primary production (GPP) and net primary production (NPP). The overall goal of the BigFoot Project was to provide validation of these products. To do this, BigFoot combined ground measurements, additional high resolution remote sensing data, and ecosystem process models at nine flux tower sites representing different biomes to evaluate the effects of the spatial and temporal patterns of ecosystem characteristics on MODIS products. BigFoot characterized up to a 7 x 7 km area (49 MODIS pixels) surrounding the CO2 flux towers located at each of the nine sites. We collected multi-year, in situ measurements of ecosystem structure and functional characteristics related to the terrestrial carbon cycle. Our sampling design allowed us to examine scales and spatial pattern of these properties, the inter-annual variability and validity of MODIS products, and provided for a field-based ecological characterization of the flux tower footprint. BigFoot was funded by NASA&amp;#39;s Terrestrial Ecology Program.For more details on the BigFoot Project, please visit the website: &lt;a href&#x3D;&quot;http://www.fsl.orst.edu/larse/bigfoot/index.html&quot;&gt;http://www.fsl.orst.edu/larse/bigfoot/index.html&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.ornldaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA BioSCape Project</title>
      <link>https://registry.opendata.aws/nasa-bioscape</link>
      <guid>https://registry.opendata.aws/nasa-bioscape</guid>
      <description>BioSCape
&lt;br&gt;&lt;h4 id&#x3D;&quot;bioscape_estuaryveghabitats_2441&quot;&gt;BioSCape_EstuaryVegHabitats_2441&lt;/h4&gt;
This dataset provides vegetation information for 64 coastal wetland plots and coastal wetland extent maps for three habitat classes in 84 estuaries in South Africa. The vegetation plot data include vegetation species occurrence, percent cover, salinity, representative vegetation heights, porewater salinity, and ground temperature. In situ plot data were collected between October 27 and November 10, 2023, in Swartvlei Estuary, Wilderness Lakes, Knynsa Estuary, and Langebaan Lagoon within lands administered by the South African National Parks. The habitat extent maps were created for 84 estuaries across the Greater Cape Floristic Region. The classification is a single point in time representing the growing season when the plot data were collected (December 2023-January 2024). The habitat extent data were created with PlanetScope satellite classified with a U-Net semantic segmentation algorithm. The habitats classified are salt marsh, submerged aquatic vegetation, and reeds &amp;amp; sedges. Plot and habitat data were collected and created to inform analysis of the imaging spectroscopy and LiDAR data collected as part of the BioSCape field campaign. The data are provided in cloud optimized GeoTIFF, comma separated values, and geopackage formats.
&lt;br&gt;&lt;h4 id&#x3D;&quot;bioscape_vegplots_berg_eerste_2425&quot;&gt;BioSCape_VegPlots_Berg_Eerste_2425&lt;/h4&gt;
This dataset contains vegetation plot survey data collected at 36 sites across the Berg and Eerste River catchments in the Western Cape, South Africa collected during 2022 and again in 2023 during the 2023 BioSCape Field Collection season. Sampling protocols were designed by the BioSCape Leadership team for use by multiple teams to generate standardized and comparable vegetation plot data across sites. Each plot was circular, 10 m in diameter, and representative of the vegetation community. Species were identified at each 1-m mark along the N-S and W-E transects, totaling 42 identifications per plot. Fractional ground cover of the plot, fractional vegetation dominance, and rarefaction counts for each plot were recorded at all plots from 2023. Data from 2022 have fractional ground cover of the NE quadrant and fractional vegetation dominance. These data are provided in comma separated values (CSV) format. The boundaries of the patches where the vegetation plots were located were recorded as polygons in included Keyhole Markup Language (KML) files.
&lt;br&gt;&lt;h4 id&#x3D;&quot;bioscape_avng_l2b_brdf_gcfr_2385&quot;&gt;BioSCape_AVNG_L2B_BRDF_GCFR_2385&lt;/h4&gt;
This dataset holds corrected surface reflectance (L2B) from the Airborne Visible / Infrared Imaging Spectrometer-Next Generation (AVIRIS-NG) instrument flown on a NASA Gulfstream III aircraft during the Biodiversity Survey of the Cape (BioSCape) project. AVIRIS-NG imagery was acquired in October - November 2023 over the Greater Cape Floristic Region (GCFR), South Africa. BioSCape is a multi-agency, NASA-led research project that integrates airborne imaging spectroscopy and lidar with a suite of measurements of biodiversity. L2B surface reflectance was derived from L1B radiance data in 425 bands, and this enhanced L2B product includes topographic, glint, and bidirectional reflectance distribution function (BRDF) corrections. Data were georeferenced and projected into UTM coordinates. These files hold the original native ancillary information relevant to the image, as well as the ancillary masks used in the creation and parameterization of the topography, glint, and BRDF corrections applied to enhance these image products. The data are provided in netCDF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;bioscape_ang_v02_l3_rfl_mosaic_2427&quot;&gt;BioSCape_ANG_V02_L3_RFL_Mosaic_2427&lt;/h4&gt;
This dataset holds mosaics of resampled surface reflectance from the Airborne Visible / Infrared Imaging Spectrometer-Next Generation (AVIRIS-NG) instrument for Biodiversity Survey of the Cape (BioSCape) project. AVIRIS-NG imagery was acquired in October - November 2023 over the Greater Cape Floristic Region (GCFR), South Africa. L2B surface reflectance data from these AVIRIS-NG collections were resampled to 5-m spatial resolution and mosaiced into a regular tile system of 807 tiles. A given tile includes multiple AVIRIS-NG scenes from multiple flight lines spanning multiple days. BioSCape is a multi-agency, NASA-led research project that integrates airborne imaging spectroscopy and lidar with a suite of measurements of biodiversity. The dataset includes surface reflectance with uncertainty for each tile in netCDF format along with an RGB quicklook image in TIFF format. A spatial index of mosaic grid ties is included in GeoJSON format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;acoustic_data_cape_floristic_2372&quot;&gt;Acoustic_Data_Cape_Floristic_2372&lt;/h4&gt;
This dataset holds in situ sound recordings from sites in Greater Cape Floristic Region (GCFR), South Africa from June to December 2023. The recordings were collected as part of the Biodiversity Survey of the Cape (BioSCape) project, a multi-agency, NASA-led research project that integrates airborne imaging spectroscopy and lidar with a suite of measurements of biodiversity. BioSoundSCape is a BioSCape subproject seeking to relate ground-based measures of bioacoustic diversity to remote imagery. AudioMoth recorders were deployed at sites for 4 to 10 days of data collection (median &#x3D; 7), and programmed to record 1 min of every 10, thus providing temporal sampling through day and night. Each recording was saved in a waveform audio file format with 16-bit digitization depth and a 48 kHz sampling rate. The recordings contain a wide range of environmental sounds such as biophony (e.g., birds, frogs, insects), anthropophony (e.g,. automobiles, airplanes) and geophony (e.g,. wind, rain). Sampling locations were stratified with respect to elevation, broad land use/land cover types, and time since wildfire disturbance. Most sites were within protected fynbos and Afromontane forest ecosystems. There were 505 sites in the wet season and 489 sites in the dry season, with most sites co-located between seasons. All sites were located within AVIRIS-NG hyperspectral acquisitions and 61% of sites were in LVIS lidar acquisitions. The dataset includes site information in tabular form and photographs of field sites.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.ornldaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA Biodiversity Project</title>
      <link>https://registry.opendata.aws/nasa-biodiversity</link>
      <guid>https://registry.opendata.aws/nasa-biodiversity</guid>
      <description>This dataset contains vegetation canopy metrics for the Greater Kruger National Park region of South Africa for 2007-2010 and 2015-2024. Metrics include relative height 98th percentile (RH98), fractional canopy cover, and foliage height diversity. This dataset contains vegetation canopy metrics for the Greater Kruger National Park region of South Africa. Metrics include relative height 98th percentile (RH98), fractional canopy cover, and foliage height diversity. They were derived by modeling a sample of Global Ecosystem Dynamics Investigation (GEDI) Level 2A Elevation and Height Metrics and Level 2B Canopy Cover and Vertical Profile Metrics at the 25-m footprint level with wall-to-wall spatial datasets including Landsat, PALSAR, topography derived from NASADEM, and soils data from iSDAsoil. Maps for 2023 and 2024 were created by applying the model trained from 2007-2022 data to PALSAR and Landsat data for 2023 and 2024. The data are suitable for analyzing change in woody canopy structure within the savanna ecosystems of this region. The data are provided in cloud optimized GeoTIFF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;acoustic_data_sonomacounty_ca_2341&quot;&gt;Acoustic_Data_SonomaCounty_CA_2341&lt;/h4&gt;
This dataset holds in situ sound recordings from sites in Sonoma County, California, USA as part of the Soundscapes to Landscapes citizen science project. Recordings were collected from 2017 to 2022 during the bird breeding season (mid-March thru mid-July). Sites (n&#x3D;1399) were selected across the county; locations were stratified with respect to topographic position and broad land use/land cover types, such as forest, shrubland, herbaceous, urban, agriculture, and riparian areas. Two types of automated recorders were used: Android-based smartphones with attached microphones and AudioMoths. Recorders were deployed at sites for at least 3 days, and programmed to record 1 min of every 10, thus providing temporal sampling through day and night. Each recording was saved in a waveform audio file format (.wav) with 16-bit digitization depth and 44.1 kHz or 48 kHz sampling rate for smartphone and AudioMoth recorders, respectively. The dataset also includes site information including site location when so permitted by landowners in tabular form and photographs of field sites.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.ornldaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA CALIPSO Project</title>
      <link>https://registry.opendata.aws/nasa-calipso</link>
      <guid>https://registry.opendata.aws/nasa-calipso</guid>
      <description>Earth Orbiter
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_iir_l3_gewex_cloud-standard-v1-00&quot;&gt;CAL_IIR_L3_GEWEX_Cloud-Standard-V1-00&lt;/h4&gt;
CAL_IIR_L3_GEWEX_Cloud-Standard-V1-00 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) IIR Level 3 Global Energy and Water Cycle Experiment (GEWEX) Cloud, Standard Version 1-00 data product. Data for this product was collected using the CALIPSO Imaging Infrared Radiometer (IIR) instrument. This product reports global distributions of IIR cloud effective radius, water path averages, and histograms on a uniform 2-dimensional (2D) spatial grid. This product is designed to follow the general guidance of the GEWEX Cloud Assessment. Cloud amount, radiative temperature, effective emissivity, and optical depth characterize the cloud samples for which IIR microphysical retrievals are reported. Cloud properties are reported for ice clouds, liquid water clouds, and high ice clouds of layer pressure lower than 440 hPa. All level 3 parameters are derived from the IIR version 4 level 2 track products, with the temporal extent averaging one month. CALIPSO was launched on April 28, 2006, to study the impact of clouds and aerosols on the Earth&amp;#39;s radiation budget and climate. It flies in the international A-Train constellation for coincident Earth observations. The CALIPSO satellite comprises three instruments: The Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP), Imaging Infrared Radiometer (IIR), and Wide Field Camera (WFC). CALIPSO is a joint satellite mission between NASA and the French Agency, Centre National d&amp;#39;Etudes Spatiales (CNES).
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_iir_l3_gewex_cloud-standard-v2-00&quot;&gt;CAL_IIR_L3_GEWEX_Cloud-Standard-V2-00&lt;/h4&gt;
CAL_IIR_L3_GEWEX_Cloud-Standard-V2-00_V2-00 are Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) Infrared Imaging Radiometer (IIR) Level 3 Cloud products for the Global Energy and Water Cycle Experiment (GEWEX) Cloud Assessment. The IIR Level 3 GEWEX Cloud product reports global distributions of IIR cloud effective radius and water path averages and histograms on a uniform2-dimensional (2D) spatial grid. Cloud amount, radiative temperature, effective emissivity, and optical depth characterize the cloud samples for which IIR microphysical retrievals are reported. The statistics are reported for atmospheric columns containing only ice clouds, only liquid water clouds, and only high ice clouds of layer pressure lower than 440 hPa. CALIPSO was a partnership between NASA and the French Space Agency, CNES. CALIPSO was launched on April28, 2006 to study the many roles played by clouds and aerosols in Earth’s climate and weather. It flew in the international A-Train constellation for coincident Earth observations from launch until September 13, 2018, when CALIPSO began lowering its orbit from 705 km to 688 km (428 miles)above the Earth to resume formation flying with CloudSat as part of the “C-Train”. The CALIPSO satellite carried three remote sensing instruments: the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP), the Imaging Infrared Radiometer (IIR), and the Wide Field-of-View Camera(WFC). By mutual agreement between NASA and CNES, the CALIPSO science mission concluded on August 1, 2023.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_lid_l0_pivb-standard-v1-00&quot;&gt;CAL_LID_L0_PIVB-Standard-V1-00&lt;/h4&gt;
CAL_LID_L0_PIVB-Standard-V1-00 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Lidar Level 0 Payload Instrument Verification and Block (PIVB), Version 1-00 data product. These data were collected intermittently between August 2016 and June 2023 using the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP). The CALIPSO payload flight software, when commanded, creates Lidar Level 0 PIVB data packets for each of the three channels: 532 nm parallel, 532 nm perpendicular, and 1064 nm. These packets contain the altitude-dependent profiles (15 m resolution) of the raw backscatter signals acquired in the high and low gain channels over 15 consecutive laser pulses prior to being processed by CALIOP’s on-board profile averaging algorithm. Also included in the product are time and position information for each laser pulse, associated instrument engineering data, and an array containing the on-board measurement altitudes. No post-processing is done for the PIVB data, so the backscatter profiles have not been altitude-registered, geolocated, range-corrected, or calibrated. The PIVB data is not part of routine science data capture and is acquired only episodically throughout the latter portion of the CALIPSO mission. CALIPSO was a partnership between NASA and the French Space Agency, CNES. CALIPSO was launched on April 28, 2006 to study the many roles played by clouds and aerosols in Earth’s climate and weather. It flew in the international A-Train constellation for coincident Earth observations from launch until September 13, 2018, when CALIPSO began lowering its orbit from 705 km to 688 km (428 miles) above the Earth to resume formation flying with CloudSat as part of the “C-Train”. The CALIPSO satellite carried three remote sensing instruments: the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP), the ImagingInfrared Radiometer (IIR), and the Wide Field-of-View Camera (WFC). By mutual agreement between NASA and CNES, the CALIPSO science mission concluded on August 1, 2023.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_lid_l1-standard-v5-00&quot;&gt;CAL_LID_L1-Standard-V5-00&lt;/h4&gt;
CAL_LID_L1-Standard-V5-00 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Lidar Level 1B profile data product. This data product was collected using the Cloud-Aerosol Lidar with Orthogonal Polarization(CALIOP) instrument. The CALIOP Level 1B data product contains a half orbit (day or night) of calibrated and geolocated single-shot (highest resolution) lidar profiles, including 532 nm and1064 nm attenuated backscatter and depolarization ratio at 532 nm. CALIPSO was a partnership between NASA and the French Space Agency, CNES. CALIPSO was launched on April 28, 2006 to study the many roles played by clouds and aerosols in Earth’s climate and weather. It flew in the international A-Train constellation for coincident Earth observations from launch until September 13, 2018, when CALIPSO began lowering its orbit from 705 km to 688 km (428 miles)above the Earth to resume formation flying with CloudSat as part of the “C-Train”. The CALIPSO satellite carried three remote sensing instruments: the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP), the Imaging Infrared Radiometer (IIR), and the Wide Field-of-View Camera(WFC). By mutual agreement between NASA and CNES, the CALIPSO science mission concluded on August 1, 2023.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_lid_l2_01kmclay-standard-v4-51&quot;&gt;CAL_LID_L2_01kmCLay-Standard-V4-51&lt;/h4&gt;
CAL_LID_L2_01kmCLay-Standard-V4-51 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) Lidar Level 2 1 km Cloud Layer, Version 4-51 data product. Data for this product was collected using the CALIPSO Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) instrument. Within this layer product are two general classes of data: Column Properties (including position data and viewing geometry) and Layer Properties. The lidar layer products contain column descriptors associated with several layer descriptors. The column descriptors specify the temporal and geophysical location of the column of the atmosphere through which a given lidar pulse travels. Also included in the column descriptors are indicators of surface lighting conditions, information about the surface type, and the number of features (e.g., aerosol layers) identified within the column. The CALIPSO satellite comprises three instruments: CALIOP, Imaging Infrared Radiometer (IIR), and Wide Field Camera (WFC). CALIPSO is a joint satellite mission between NASA and the French Agency CNES (Centre National d&amp;#39;Etudes Spatiales). CALIPSO was launched on April 28, 2006, to study the impact of clouds and aerosols on the Earth&amp;#39;s radiation budget and climate. From June 13, 2006, to September 13, 2018, CALIPSO was part of the A-Train constellation for coincident Earth Observations. After September 13, 2018, the satellite was lowered from 705 to 688 km to resume flying in formation with CloudSat, called the C-Train.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_lid_l2_01kmclay-standard-v5-00&quot;&gt;CAL_LID_L2_01kmCLay-Standard-V5-00&lt;/h4&gt;
CAL_LID_L2_01kmCLay-Standard-V5-00 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Lidar Level 2 1 km Cloud Layer data product. This data product was collected using the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) instrument. Within this cloud layer product, generated at a horizontal resolution of 1 km, are two general classes of data: Column Properties (including position data and viewing geometry) and Layer Properties. The cloud layer products consist of a sequence of column descriptors, each associated with a variable number of cloud layer descriptors. The column descriptors specify the temporal and geophysical location of the column of the atmosphere through which a given lidar pulse travels. Also included in the column descriptors are indicators of surface lighting conditions, information about the surface type, and the number of features (e.g., cloud layers) identified within the column. For each feature within a column, a set of layer descriptors is reported. The layer descriptors provide information about the spatial and optical characteristics of a feature, such as base and top altitudes, integrated attenuated backscatter, and optical depth. CALIPSO was a partnership between NASA and the French Space Agency, CNES. CALIPSO was launched on April 28, 2006 to study the many roles played by clouds and aerosols in Earth’s climate and weather. It flew in the international A-Train constellation for coincident Earth observations from launch until September 13, 2018, when CALIPSO began lowering its orbit from 705 km to 688 km (428 miles) above the Earth to resume formation flying with CloudSat as part of the “C-Train”. The CALIPSO satellite carried three remote sensing instruments: the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP), the Imaging Infrared Radiometer (IIR), and the Wide Field-of-View Camera (WFC). By mutual agreement between NASA and CNES, the CALIPSO science mission concluded on August 1, 2023.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_lid_l2_333mmlay-standard-v5-00&quot;&gt;CAL_LID_L2_333mMLay-Standard-V5-00&lt;/h4&gt;
CAL_LID_L2_333mMLay-Standard-V5-00 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Lidar Level 2 333 m Merged Layer data product. This data product was collected using the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) instrument. Within this cloud and aerosol layer product, generated at a horizontal resolution of 333 m (single shot resolution), are two general classes of data: Column Properties (including position data and viewing geometry) and Layer Properties. The merged layer products consist of a sequence of column descriptors, each associated with a variable number of cloud and aerosol layer descriptors. The column descriptors specify the temporal and geophysical location of the column of the atmosphere through which a given lidar pulse travels. Also included in the column descriptors are indicators of surface lighting conditions, information about the surface type, and the number of features (e.g., cloud and aerosol layers) identified within the column. For each feature within a column, a set of layer descriptors is reported. The layer descriptors provide information about the spatial and optical characteristics of a feature, such as base and top altitudes, integrated attenuated backscatter, and optical depth. CALIPSO was a partnership between NASA and the French Space Agency, CNES. CALIPSO was launched on April 28, 2006 to study the many roles played by clouds and aerosols in Earth’s climate and weather. It flew in the international A-Train constellation for coincident Earth observations from launch until September 13, 2018, when CALIPSO began lowering its orbit from 705 km to 688 km (428 miles) above the Earth to resume formation flying with CloudSat as part of the “C-Train”. The CALIPSO satellite carried three remote sensing instruments: the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP), the Imaging Infrared Radiometer (IIR), and the Wide Field-of-View Camera (WFC). By mutual agreement between NASA and CNES, the CALIPSO science mission concluded on August 1, 2023.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_lid_l2_05kmalay-standard-v5-00&quot;&gt;CAL_LID_L2_05kmALay-Standard-V5-00&lt;/h4&gt;
CAL_LID_L2_05kmALay-Standard-V5-00 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Lidar Level 2 5 km Aerosol Layer data product. This data product was collected using the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) instrument. Within this aerosol layer product, generated at a horizontal resolution of 5 km, are two general classes of data: Column Properties (including position data and viewing geometry) and Layer Properties. The aerosol layer products consist of a sequence of column descriptors, each associated with a variable number of cloud layer descriptors. The column descriptors specify the temporal and geophysical location of the column of the atmosphere through which a given lidar pulse travels. Also included in the column descriptors are indicators of surface lighting conditions, information about the surface type, and the number of features (e.g., aerosol layers) identified within the column. For each feature within a column, a set of layer descriptors is reported. The layer descriptors provide information about the spatial and optical characteristics of a feature, such as base and top altitudes, integrated attenuated backscatter, and optical depth. CALIPSO was a partnership between NASA and the French Space Agency, CNES. CALIPSO was launched on April 28, 2006 to study the many roles played by clouds and aerosols in Earth’s climate and weather. It flew in the international A-Train constellation for coincident Earth observations from launch until September 13, 2018,when CALIPSO began lowering its orbit from 705 km to 688 km (428 miles) above the Earth to resume formation flying with CloudSat as part of the “C-Train”. The CALIPSO satellite carried three remote sensing instruments: the Cloud-Aerosol Lidar with Orthogonal Polarization(CALIOP), the Imaging Infrared Radiometer (IIR), and the Wide Field-of-View Camera (WFC). By mutual agreement between NASA and CNES, the CALIPSO science mission concluded on August1, 2023.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_lid_l2_05kmmlay-standard-v5-00&quot;&gt;CAL_LID_L2_05kmMLay-Standard-V5-00&lt;/h4&gt;
CAL_LID_L2_05kmMLay-Standard-V5-00 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Lidar Level 2 5 km Merged Layer data product. This data product was collected using the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) instrument. Within this cloud and aerosol layer product, generated at a horizontal resolution of 5 km, are two general classes of data: Column Properties(including position data and viewing geometry) and Layer Properties. The merged layer products consist of a sequence of column descriptors, each associated with a variable number of cloud or aerosol layer descriptors. The column descriptors specify the temporal and geophysical location of the column of the atmosphere through which a given lidar pulse travels. Also included in the column descriptors are indicators of surface lighting conditions, information about the surface type, and the number of features (e.g., cloud or aerosol layers) identified within the column. Foreach feature within a column, a set of layer descriptors is reported. The layer descriptors provide information about the spatial and optical characteristics of a feature, such as base and top altitudes, integrated attenuated backscatter, and optical depth. CALIPSO was a partnership between NASA and the French Space Agency, CNES. CALIPSO was launched on April 28, 2006 to study the many roles played by clouds and aerosols in Earth’s climate and weather. It flew in the international A-Train constellation for coincident Earth observations from launch until September 13, 2018, when CALIPSO began lowering its orbit from 705 km to 688 km (428 miles)above the Earth to resume formation flying with CloudSat as part of the “C-Train”. The CALIPSO satellite carried three remote sensing instruments: the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP), the Imaging Infrared Radiometer (IIR), and the Wide Field-of-View Camera(WFC). By mutual agreement between NASA and CNES, the CALIPSO science mission concluded on August 1, 2023.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_lid_l2_05kmclay-standard-v5-00&quot;&gt;CAL_LID_L2_05kmCLay-Standard-V5-00&lt;/h4&gt;
CAL_LID_L2_05kmCLay-Standard-V5-00 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Lidar Level 2 5 km Cloud Layer data product. This data product was collected using the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) instrument. Within this cloud layer product, generated at a horizontal resolution of 5 km, are two general classes of data: Column Properties (including position data and viewing geometry) and Layer Properties. The cloud layer products consist of a sequence of column descriptors, each associated with a variable number of cloud layer descriptors. The column descriptors specify the temporal and geophysical location of the column of the atmosphere through which a given lidar pulse travels. Also included in the column descriptors are indicators of surface lighting conditions, information about the surface type, and the number of features (e.g., cloud layers) identified within the column. For each feature within a column, a set of layer descriptors is reported. The layer descriptors provide information about the spatial and optical characteristics of a feature, such as base and top altitudes, integrated attenuated backscatter, and optical depth. CALIPSO was a partnership between NASA and the French Space Agency, CNES. CALIPSO was launched on April 28, 2006 to study the many roles played by clouds and aerosols in Earth’s climate and weather. It flew in the international A-Train constellation for coincident Earth observations from launch until September 13, 2018, when CALIPSO began lowering its orbit from 705 km to 688 km (428 miles) above the Earth to resume formation flying with CloudSat as part of the “C-Train”. The CALIPSO satellite carried three remote sensing instruments: the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP), the Imaging Infrared Radiometer (IIR), and the Wide Field-of-View Camera (WFC). By mutual agreement between NASA and CNES, the CALIPSO science mission concluded on August 1, 2023.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_lid_l2_05kmapro-standard-v5-00&quot;&gt;CAL_LID_L2_05kmAPro-Standard-V5-00&lt;/h4&gt;
CAL_LID_L2_05kmAPro-Standard-V5-00 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Lidar Level 2 5 km Aerosol Profile data product. This data product was collected using the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) instrument. This aerosol profile product reports vertical profiles of particulate extinction and backscatter, as well as additional information (e.g. particulate depolarization ratios) derived from these fundamental measurements. The aerosol profile products are reported at a uniform spatial resolution of 60 m vertically and 5 km horizontally, over a nominal altitude range from 30 km to -0.5 km. Due to constraints imposed by the on-board data averaging scheme, the vertical resolution of the aerosol profile data varies as a function of altitude. In the tropospheric region between 20 km to -0.5 km, the aerosol profile products are reported at a resolution of 60 m vertically, and in the stratospheric region(above 20-km), the aerosol profile products are reported at a resolution of 180 m vertically. CALIPSO was a partnership between NASA and the French Space Agency, CNES. CALIPSO was launched on April 28, 2006 to study the many roles played by clouds and aerosols in Earth’s climate and weather. It flew in the international A-Train constellation for coincident Earth observations from launch until September 13, 2018, when CALIPSO began lowering its orbit from705 km to 688 km (428 miles) above the Earth to resume formation flying with CloudSat as part of the “C-Train”. The CALIPSO satellite carried three remote sensing instruments: the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP), the Imaging Infrared Radiometer (IIR), and the Wide Field-of-View Camera (WFC). By mutual agreement between NASA and CNES, the CALIPSO science mission concluded on August 1, 2023.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_lid_l2_blowingsnow_antarctica-standard-v1-00&quot;&gt;CAL_LID_L2_BlowingSnow_Antarctica-Standard-V1-00&lt;/h4&gt;
CAL_LID_L2_BlowingSnow_Antarctica-Standard-V1-00 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) Lidar Level 2 Blowing Snow - Antarctica, Version 1-00 data product. This product was collected using the CALIPSO Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) instrument and reports the distribution of blowing snow properties based on back-scatter retrievals over Antarctica. Data collection for this product is complete. CALIPSO was launched on April 28, 2006, to study the impact of clouds and aerosols on the Earth&amp;#39;s radiation budget and climate. It flies in the international A-Train constellation for coincident Earth observations. The CALIPSO satellite comprises three instruments: CALIOP, Imaging Infrared Radiometer (IIR), and Wide Field Camera (WFC). CALIPSO is a joint satellite mission between NASA and the French Agency CNES (Centre National D&amp;#39;Etudes Spatiales).
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_lid_l2_blowingsnow_antarctica-standard-v1-01&quot;&gt;CAL_LID_L2_BlowingSnow_Antarctica-Standard-V1-01&lt;/h4&gt;
CAL_LID_L2_BlowingSnow_Antarctica-Standard-V1-01 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) Lidar Level 2 Blowing Snow - Antarctica, Version 1-01 data product. This product was collected using the CALIPSO Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) instrument and reports the distribution of blowing snow properties based on back-scatter retrievals over Antarctica. The version of this product was changed from 1-00 to 1-01 to account for a change in the operating system of the CALIPSO production cluster. Data collection for this product is complete. CALIPSO was launched on April 28, 2006, to study the impact of clouds and aerosols on the Earth&amp;#39;s radiation budget and climate. It flies in the international A-Train constellation for coincident Earth observations. The CALIPSO satellite comprises three instruments: CALIOP, Imaging Infrared Radiometer (IIR), and Wide Field Camera (WFC). CALIPSO is a joint satellite mission between NASA and the French Agency, Centre National d&amp;#39;Études Spatiales (CNES).
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_lid_l2_blowingsnow_greenland-standard-v1-00&quot;&gt;CAL_LID_L2_BlowingSnow_Greenland-Standard-V1-00&lt;/h4&gt;
CAL_LID_L2_BlowingSnow_Greenland-Standard-V1-00 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) Lidar Level 2 Blowing Snow - Greenland, Version 1-00 data product. This product was collected using the CALIPSO Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) instrument and reports the distribution of blowing snow properties based on back-scatter retrievals over Greenland. The CALIPSO satellite comprises three instruments: CALIOP, Imaging Infrared Radiometer (IIR), and Wide Field Camera (WFC). CALIPSO is a joint satellite mission between NASA and the French Agency CNES (Centre National d&amp;#39;Etudes Spatiales). CALIPSO was launched on April 28, 2006, to study the impact of clouds and aerosols on the Earth&amp;#39;s radiation budget and climate. From June 13, 2006, to September 13, 2018, CALIPSO was part of the A-Train constellation for coincident Earth Observations. After September 13, 2018, the satellite was lowered from 705 to 688 km to resume flying in formation with CloudSat, called the C-Train.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_lid_l2_05kmcpro-standard-v5-00&quot;&gt;CAL_LID_L2_05kmCPro-Standard-V5-00&lt;/h4&gt;
CAL_LID_L2_05kmCPro-Standard-V5-00 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Lidar Level 2 5 km Cloud Profile data product. This data product was collected using the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) instrument. This cloud profile product reports vertical profiles of particulate extinction and backscatter, as well as additional information (e.g. particulate depolarization ratios) derived from these fundamental measurements. The cloud profile products are reported at a uniform spatial resolution of 60 m vertically and 5 km horizontally, over a nominal altitude range from 30 km to -0.5 km. Due to constraints imposed by the on-board data averaging scheme, the vertical resolution of the cloud profile data varies as a function of altitude. In the tropospheric region between 20 km to -0.5 km, the cloud profile products are reported at a resolution of 60 m vertically, and in the stratospheric region (above20-km), the cloud profile products are reported at a resolution of 180 m vertically. CALIPSO was a partnership between NASA and the French Space Agency, CNES. CALIPSO was launched on April 28, 2006 to study the many roles played by clouds and aerosols in Earth’s climate and weather. It flew in the international A-Train constellation for coincident Earth observations from launch until September 13, 2018, when CALIPSO began lowering its orbit from 705 km to 688 km(428 miles) above the Earth to resume formation flying with CloudSat as part of the “C-Train”. The CALIPSO satellite carried three remote sensing instruments: the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP), the Imaging Infrared Radiometer (IIR), and the Wide Field-of-View Camera (WFC). By mutual agreement between NASA and CNES, the CALIPSO science mission concluded on August 1, 2023.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_lid_l2_mlay_diagnostic-beta-v5-00&quot;&gt;CAL_LID_L2_MLay_Diagnostic-Beta-V5-00&lt;/h4&gt;
CAL_LID_L2_MLay-Diagnostic-Beta-V5-00 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Lidar Level 2Merged Layer Diagnostic data product. This data product was collected using the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) instrument. The contents of this merged layer product contain information already in the CAL_LID_L2_05kmMLay-Standard-V5-00 andCAL_LID_L2_333mMLay-Standard-V5-00 data products, but with additional diagnostic flags and parameters that were used by the science algorithms. CALIPSO was a partnership between NASA and the French Space Agency, CNES. CALIPSO was launched on April 28, 2006 to study the many roles played by clouds and aerosols in Earth’s climate and weather. It flew in the international A-Train constellation for coincident Earth observations from launch until September 13, 2018, when CALIPSO began lowering its orbit from 705 km to 688 km (428 miles)above the Earth to resume formation flying with CloudSat as part of the “C-Train”. The CALIPSO satellite carried three remote sensing instruments: the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP), the Imaging Infrared Radiometer (IIR), and the Wide Field-of-View Camera(WFC). By mutual agreement between NASA and CNES, the CALIPSO science mission concluded on August 1, 2023.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_lid_l2_pscmask-standard-v3-00&quot;&gt;CAL_LID_L2_PSCMask-Standard-V3-00&lt;/h4&gt;
CAL_LID_L2_PSCMask-Standard-V3-00 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Lidar Level 2 Polar Stratospheric Clouds (PSC) data product. This data product was collected using the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) instrument and describes the spatial distribution, optical properties, and composition of PSC layers observed. The product contains profiles of PSC presence, composition, optical properties, and meteorological information on a uniform 5-km horizontal x 180-m vertical grid along CALIPSO orbit tracks. Aura Microwave Limb Sounder (MLS) measurements of the primary PSC condensable vapors HNO3 and H2O and a number of parameters from the Aura MLS V2 Derived Meteorological Products (DMPs) are also included in this product. CALIPSO was a partnership between NASA and the French Space Agency, CNES. CALIPSO was launched on April 28, 2006 to study the many roles played by clouds and aerosols in Earth’s climate and weather. It flew in the international A-Train constellation for coincident Earth observations from launch until September 13, 2018, when CALIPSO began lowering its orbit from 705 km to 688 km (428 miles) above the Earth to resume formation flying with CloudSat as part of the “C-Train”. The CALIPSO satellite carried three remote sensing instruments: the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP), the Imaging Infrared Radiometer (IIR), and the Wide Field-of-View Camera (WFC). By mutual agreement between NASA and CNES, the CALIPSO science mission concluded on August 1, 2023.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_lid_l2_vfm-standard-v5-00&quot;&gt;CAL_LID_L2_VFM-Standard-V5-00&lt;/h4&gt;
CAL_LID_L2_VFM-Standard-V5-00 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Lidar Level 2 Vertical Feature Mask (VFM) data product. This data product was collected using the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) instrument. The CALIOP Level 2 VFM data product contains scene classification and lidar lighting and land/water indicators. CALIPSO was a partnership between NASA and the French Space Agency, CNES. CALIPSO was launched on April28, 2006 to study the many roles played by clouds and aerosols in Earth’s climate and weather. It flew in the international A-Train constellation for coincident Earth observations from launch until September 13, 2018, when CALIPSO began lowering its orbit from 705 km to 688 km (428 miles)above the Earth to resume formation flying with CloudSat as part of the “C-Train”. The CALIPSO satellite carried three remote sensing instruments: the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP), the Imaging Infrared Radiometer (IIR), and the Wide Field-of-View Camera(WFC). By mutual agreement between NASA and CNES, the CALIPSO science mission concluded on August 1, 2023.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_lid_l3_cloud_occurrence-standard-v1-00&quot;&gt;CAL_LID_L3_Cloud_Occurrence-Standard-V1-00&lt;/h4&gt;
CAL_LID_L3_Cloud_Occurrence-Standard-V1-00 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Lidar Level 3 Cloud Occurrence Data, Standard Version 1-00 data product. This data product was collected using the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) instrument. The degradation of the laser energies that started in September 2016 had a negative impact on the product, and because of this, generation and distribution ended in December 2016. Updated Lidar Level 2 data products and changes to the Lidar Level 3 Cloud Occurrence algorithm will need to be completed before a new release of this product is released. This product reports global distributions of clouds on a uniform spatial grid. All level 3 parameters are derived from the CALIPSO level 2 data, with a temporal average of one month. CALIPSO was launched on April 28, 2006, and continues to collect data necessary to study the impact of clouds and aerosols on the Earth&amp;#39;s radiation budget and climate. It flies in the international A-Train constellation for coincident Earth observations. The CALIPSO satellite comprises three instruments: CALIOP, Imaging Infrared Radiometer (IIR), and Wide Field Camera (WFC). CALIPSO is a joint satellite mission between NASA and the French Agency CNES.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_lid_l3_cloud_occurrence-standard-v2-00&quot;&gt;CAL_LID_L3_Cloud_Occurrence-Standard-V2-00&lt;/h4&gt;
CAL_LID_L3_Cloud_Occurrence-Standard-V2-00_V2-00 are Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) Lidar(CALIOP) Level 3 Cloud Occurrence products. The Lidar Level 3 Cloud Occurrence product reports global distributions of cloud occurrence by counts on a uniform spatial grid. At each grid, the number of detected ice cloud samples is also reported as a histogram of ice cloud layer optical depth. CALIPSO was a partnership between NASA and the French Space Agency, CNES. CALIPSO was launched on April 28, 2006 to study the many roles played by clouds and aerosols in Earth’s climate and weather. It flew in the international A-Train constellation for coincident Earth observations from launch until September 13, 2018, when CALIPSO began lowering its orbit from 705 km to 688 km (428 miles) above the Earth to resume formation flying with CloudSat as part of the “C-Train”. The CALIPSO satellite carried three remote sensing instruments: the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP), the Imaging Infrared Radiometer (IIR), and the Wide Field-of-View Camera (WFC). By mutual agreement between NASA and CNES, the CALIPSO science mission concluded on August 1, 2023.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_lid_l3_gewex_cloud-standard-v1-00&quot;&gt;CAL_LID_L3_GEWEX_Cloud-Standard-V1-00&lt;/h4&gt;
CAL_LID_L3_GEWEX_Cloud-Standard-V1-00 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) Lidar Level 3 Global Energy and Water Cycle Experiment (GEWEX) Cloud, Standard Version 1-00 data product. Data for this product was collected using the CALIPSO Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) instrument. Data collection for this product is complete. This product is a reformatted version of the CALIPSO contribution to the GEWEX cloud assessment of global cloud datasets from satellites. The data submitted by the CALIPSO team for this project had to conform to a specific format: yearly netCDF files organized by parameter. To be compatible with another publicly orderable lidar level 3 CALIPSO aerosol and cloud products reported as monthly HDF files, this new lidar level 3 CALIPSO GEWEX cloud product was created. These files report global distributions of cloud amount and cloud top as averages and histograms on a uniform 2-dimensional (2D) spatial grid. All level 3 parameters are derived from the CALIPSO version 4. x Level 2, 5 km cloud merged layer products, with a temporal averaging of one month. CALIPSO was launched on April 28, 2006, to study the impact of clouds and aerosols on the Earth&amp;#39;s radiation budget and climate. It flies in the international A-Train constellation for coincident Earth observations. The CALIPSO satellite comprises three instruments: CALIOP, Imaging Infrared Radiometer (IIR), and Wide Field Camera (WFC). CALIPSO is a joint satellite mission between NASA and the French Agency CNES (Centre National D’Etudes Spatiales).
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_lid_l3_ice_cloud-standard-v1-00&quot;&gt;CAL_LID_L3_Ice_Cloud-Standard-V1-00&lt;/h4&gt;
CAL_LID_L3_Ice_Cloud-Standard-V1-00 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Lidar Level 3 Ice Cloud Data, Standard Version 1-00 data product. This data product was collected using the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) instrument. The degradation of the laser energies that started in September 2016 had a negative impact on the product, and because of this, generation and distribution ended in December 2016. Updated Lidar Level 2 data products and changes to the Lidar Level 3 Ice Cloud algorithm will need to be completed before a new release of this product is released. This product reports global distributions of ice cloud extinction and ice water content histograms on a uniform spatial grid. All level 3 parameters are derived from the CALIPSO level 2, 5km cloud profile products, with a temporal average of one month. CALIPSO was launched on April 28, 2006, and continues to collect data necessary to study the impact of clouds and aerosols on the Earth&amp;#39;s radiation budget and climate. It flies in the international A-Train constellation for coincident Earth observations. The CALIPSO satellite comprises three instruments: CALIOP, Imaging Infrared Radiometer (IIR), and Wide Field Camera (WFC). CALIPSO is a joint satellite mission between NASA and the French Agency CNES.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_lid_l3_stratospheric_apro-standard-v1-00&quot;&gt;CAL_LID_L3_Stratospheric_APro-Standard-V1-00&lt;/h4&gt;
CAL_LID_L3_Stratospheric_APro-Standard-V1-00 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Lidar Level 3 Stratospheric Aerosol Profiles Standard Version 1-00 data product. This data product was collected using the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) instrument. Data generation and distribution of this V1.00 product ended on July 1, 2020 to support a change in the operating system of the CALIPSO production clusters. The V1.01 data product covers July 1, 2020, to current. The CALIPSO Lidar Level 3 stratospheric aerosol reports global distributions of 532nm total attenuated backscatter, extinction, attenuated scattering ratios, and stratospheric aerosol optical depths on a uniform spatial grid. All level 3 parameters are derived from the CALIPSO version 4 level 1 and level 2 5 km merged layer and version 3 level 2 polar stratospheric cloud data products, with a temporal averaging of one month. The primary outputs are reported in terms of 1) background only and 2) all aerosol. All features identified by the level 2 algorithms have been removed for background only. Only aerosol layers are considered for all aerosols, while clouds and polar stratospheric clouds are removed. CALIPSO was launched on April 28, 2006, and continues to collect data necessary to study the impact of clouds and aerosols on the Earth&amp;#39;s radiation budget and climate. It flies in the international A-Train constellation for coincident Earth observations. The CALIPSO satellite comprises three instruments: CALIOP, Imaging Infrared Radiometer (IIR), and Wide Field Camera (WFC). CALIPSO is a joint satellite mission between NASA and the French Agency CNES (Centre national d&amp;#39;études spatiales).
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_lid_l3_stratospheric_apro-standard-v1-01&quot;&gt;CAL_LID_L3_Stratospheric_APro-Standard-V1-01&lt;/h4&gt;
CAL_LID_L3_Stratospheric_APro-Standard-V1-01 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Lidar Level 3 Stratospheric Aerosol Profiles Standard Version 1-01 data product. This data product was collected using the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) instrument. The version of this product was changed from 1-00 to 1-01 to account for a change in the operating system of the CALIPSO production cluster. Data collection for this product is ongoing. The CALIPSO Lidar Level 3 stratospheric aerosol reports global distributions of 532nm total attenuated backscatter, extinction, attenuated scattering ratios, and stratospheric aerosol optical depths on a uniform spatial grid. All level 3 parameters are derived from the CALIPSO version 4 level 1 and level 2 5 km merged layer and version 3 level 2 polar stratospheric cloud data products, with a temporal averaging of one month. The primary outputs are reported in terms of 1) background only and 2) all aerosol. All features identified by the level 2 algorithms have been removed for background only. Only aerosol layers are considered for all aerosols, while clouds and polar stratospheric clouds are removed. CALIPSO was launched on April 28, 2006, and continues to collect data necessary to study the impact of clouds and aerosols on the Earth&amp;#39;s radiation budget and climate. It flies in the international A-Train constellation for coincident Earth observations. The CALIPSO satellite comprises three instruments: CALIOP, Imaging Infrared Radiometer (IIR), and Wide Field Camera (WFC). CALIPSO is a joint satellite mission between NASA and the French Agency CNES (Centre national d&amp;#39;études spatiales).
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_lid_l3_stratospheric_apro-standard-v2-00&quot;&gt;CAL_LID_L3_Stratospheric_APro-Standard-V2-00&lt;/h4&gt;
CAL_LID_L3_Stratospheric_APro-Standard-V2-00 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Lidar Level 3 Stratospheric Aerosol data product. This data product was collected using the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) instrument. This data product reports global distributions of 532 nm total attenuated backscatter, particulate backscatter, extinction, attenuated scattering ratios, and stratospheric aerosol optical depths on a uniform spatial grid. All parameters are derived from the version 5.00 CALIOP Level 1 and Level 2 and V2.00 CALIOP Polar Stratospheric Mask data products. CALIPSO was a partnership between NASA and the French Space Agency, CNES. CALIPSO was launched on April 28, 2006 to study the many roles played by clouds and aerosols in Earth’s climate and weather. It flew in the international A-Train constellation for coincident Earth observations from launch until September 13, 2018, when CALIPSO began lowering its orbit from 705 km to 688 km (428 miles) above the Earth to resume formation flying with CloudSat as part of the “C-Train”. The CALIPSO satellite carried three remote sensing instruments: the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP), the Imaging Infrared Radiometer (IIR), and the Wide Field-of-View Camera (WFC). By mutual agreement between NASA and CNES, the CALIPSO science mission concluded on August 1, 2023.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_lid_l3_tropospheric_apro_allsky-standard-v4-20&quot;&gt;CAL_LID_L3_Tropospheric_APro_AllSky-Standard-V4-20&lt;/h4&gt;
CAL_LID_L3_Tropospheric_APro_AllSky-Standard-V4-20 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Lidar Level 3 Tropospheric Aerosol Profiles, All Sky Data, Standard Version 4-20 data product. This data product was collected using the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) instrument. Data generation and distribution of this V4.20 product ended on July 1, 2020, to support a change in the operating system of the CALIPSO production clusters. The V4.21 data product covers July 1, 2020, to current. The CALIPSO lidar level 3 aerosol data product reports monthly mean profiles of aerosol optical properties on a uniform spatial grid. It is intended to be a tropospheric product, so data are only reported below altitudes of 12 km. All level 3 parameters are derived from the version 4.20 CALIOP level 2 aerosol profile product and have been quality screened before averaging. The primary quantities reported are vertical profiles of the aerosol extinction coefficient at 532 nm and its vertical integral, the aerosol optical depth (AOD). Aerosol type and spatial distribution information are also included. Averaged profile data is reported for all aerosols, regardless of type, and for mineral dust aerosols only. Classification of dust is based on the aerosol-type flags in the level 2 profile product. To keep level 3 file sizes manageable, four different types of level 3 files are produced, depending on the sky condition and the temporal coverage of the data prior to averaging. Description of the Four Sky Conditions (Day, Night): 1) All Sky: All level 2 columns are averaged, regardless of cloud occurrence, 2) Cloud-Free: Only cloud-free level 2 columns are averaged, 3) Cloudy-Sky, Transparent: Only level 2 columns containing transparent clouds are averaged, and 4) Cloud-Sky, Opaque: Only level 2 columns containing opaque clouds are averaged CALIPSO was launched on April 28, 2006, and continues to collect data necessary to study the impact of clouds and aerosols on the Earth&amp;#39;s radiation budget and climate. It flies in the international A-Train constellation for coincident Earth observations. The CALIPSO satellite comprises three instruments: CALIOP, Imaging Infrared Radiometer (IIR), and Wide Field Camera (WFC). CALIPSO is a joint satellite mission between NASA and the French Agency CNES (Centre national d&amp;#39;études spatiales).
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_lid_l3_tropospheric_apro_allsky-standard-v5-00&quot;&gt;CAL_LID_L3_Tropospheric_APro_AllSky-Standard-V5-00&lt;/h4&gt;
CAL_LID_L3_Tropospheric_APro_AllSky-Standard-V5-00 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Lidar Level 3 Tropospheric Aerosol, All-Sky, data product. This data product was collected using the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) instrument. This data product, generated separately between day and night, reports monthly mean profiles of aerosol optical properties on a uniform spatial grid. It is a tropospheric product, so data are only reported below altitudes of 12 km. All parameters are derived from the version 5.00 CALIOP Level 2 data and have been quality screened prior to averaging. The primary quantities reported are vertical profiles of the aerosol extinction coefficient at 532 nm and its vertical integral, the aerosol optical depth (AOD). Aerosol type and spatial distributional information are also included. The All-Sky designate indicates that all level 2 columns are averaged, regardless of the occurrence of clouds. CALIPSO was a partnership between NASA and the French Space Agency, CNES. CALIPSO was launched on April 28, 2006 to study the many roles played by clouds and aerosols in Earth’s climate and weather. It flew in the international A-Train constellation for coincident Earth observations from launch until September 13, 2018, when CALIPSO began lowering its orbit from 705 km to 688 km (428 miles) above the Earth to resume formation flying with CloudSat as part of the “C-Train”. The CALIPSO satellite carried three remote sensing instruments: the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP), the Imaging Infrared Radiometer (IIR), and the Wide Field-of-View Camera (WFC). By mutual agreement between NASA and CNES, the CALIPSO science mission concluded on August 1, 2023.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_lid_l3_tropospheric_apro_cloudfree-standard-v4-20&quot;&gt;CAL_LID_L3_Tropospheric_APro_CloudFree-Standard-V4-20&lt;/h4&gt;
CAL_LID_L3_Tropospheric_APro_CloudFree-Standard-V4-20 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Lidar Level 3 Tropospheric Aerosol Profiles, Cloud Free Data, Standard Version 4-20 data product. This data product was collected using the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) instrument. Data generation and distribution of this V4.20 product ended on July 1, 2020, to support a change in the operating system of the CALIPSO production clusters. The V4.21 data product covers July 1, 2020, to current. The CALIPSO lidar level 3 aerosol data product reports monthly mean profiles of aerosol optical properties on a uniform spatial grid. It is intended to be a tropospheric product, so data are only reported below altitudes of 12 km. All level 3 parameters are derived from the version 4.20 CALIOP level 2 aerosol profile product and have been quality screened before averaging. The primary quantities reported are vertical profiles of the aerosol extinction coefficient at 532nm and its vertical integral, the aerosol optical depth (AOD). Aerosol type and spatial distribution information are also included. Averaged profile data is reported for all aerosols, regardless of type, and for mineral dust aerosols only. Classification of dust is based on the aerosol-type flags in the level 2 profile product. To keep level 3 file sizes manageable, four different types of level 3 files are produced, depending on the sky condition and the temporal coverage of the data prior to averaging. Description of the Four Sky Conditions (Day, Night) 1) All Sky: All level 2 columns are averaged, regardless of cloud occurrence 2) Cloud-Free: Only cloud-free level 2 columns are averaged 3) Cloudy-Sky, Transparent: Only level 2 columns containing transparent clouds are averaged 4) Cloud-Sky, Opaque: Only level 2 columns containing opaque clouds are averaged CALIPSO was launched on April 28, 2006, and continues to collect data necessary to study the impact of clouds and aerosols on the Earth&amp;#39;s radiation budget and climate. It flies in the international A-Train constellation for coincident Earth observations. The CALIPSO satellite comprises three instruments: CALIOP, Imaging Infrared Radiometer (IIR), and Wide Field Camera (WFC). CALIPSO is a joint satellite mission between NASA and the French Agency CNES (Centre National D’Etudes Spatiales).
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_lid_l3_tropospheric_apro_cloudyskyopaque-standard-v4-20&quot;&gt;CAL_LID_L3_Tropospheric_APro_CloudySkyOpaque-Standard-V4-20&lt;/h4&gt;
CAL_LID_L3_Tropospheric_APro_CloudySkyOpaque-Standard-V4-20 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Lidar Level 3 Tropospheric Aerosol Profiles, Cloudy Sky Opaque Data, Standard Version 4-20 data product. This data product was collected using the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) instrument. Data generation and distribution of this V4.20 product ended on July 1, 2020, to support a change in the operating system of the CALIPSO production clusters. The V4.21 data product covers July 1, 2020, to current. The CALIPSO lidar level 3 aerosol data product reports monthly mean profiles of aerosol optical properties on a uniform spatial grid. It is intended to be a tropospheric product, so data are only reported below altitudes of 12km. All level 3 parameters are derived from the version 4.20 CALIOP level 2 aerosol profile product and have been quality screened before averaging. The primary quantities reported are vertical profiles of the aerosol extinction coefficient at 532 nm and its vertical integral, the aerosol optical depth (AOD). Aerosol type and spatial distribution information are also included. Averaged profile data is reported for all aerosols, regardless of type, and for mineral dust aerosols only. Classification of dust is based on the aerosol-type flags in the level 2 profile product. To keep level 3 file sizes manageable, four different types of level 3 files are produced, depending on the sky condition and the temporal coverage of the data before averaging. Description of the Four Sky Conditions (Day, Night): 1) All Sky: All level 2 columns are averaged, regardless of cloud occurrence 2) Cloud-Free: Only cloud-free level 2 columns are averaged 3) Cloudy-Sky, Transparent: Only level 2 columns containing transparent clouds are averaged 4) Cloud-Sky, Opaque: Only level 2 columns containing opaque clouds are averaged CALIPSO was launched on April 28, 2006, and continues to collect data necessary to study the impact of clouds and aerosols on the Earth&amp;#39;s radiation budget and climate. It flies in the international A-Train constellation for coincident Earth observations. The CALIPSO satellite comprises three instruments: CALIOP, Imaging Infrared Radiometer (IIR), and Wide Field Camera (WFC). CALIPSO is a joint satellite mission between NASA and the French Agency CNES (Centre National D’Etudes Spatiales).
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_lid_l3_tropospheric_apro_cloudyskyopaque-standard-v5-00&quot;&gt;CAL_LID_L3_Tropospheric_APro_CloudySkyOpaque-Standard-V5-00&lt;/h4&gt;
CAL_LID_L3_Tropospheric_APro_CloudSkyOpaque-Standard-V5-00 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Lidar Level 3 Tropospheric Aerosol, Cloudy Sky Opaque, data product. This data product was collected using the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) instrument. This data product, generated separately between day and night, reports monthly mean profiles of aerosol optical properties on a uniform spatial grid. It is a tropospheric product, so data are only reported below altitudes of 12 km. All parameters are derived from the version 5.00 CALIOP Level 2 data and have been quality screened prior to averaging. The primary quantities reported are vertical profiles of the aerosol extinction coefficient at 532 nm and its vertical integral, the aerosol optical depth (AOD). Aerosol type and spatial distributional information are also included. The Cloudy Sky Opaque designate indicates that only level 2 columns containing opaque clouds are averaged. CALIPSO was a partnership between NASA and the French Space Agency, CNES. CALIPSO was launched on April28, 2006 to study the many roles played by clouds and aerosols in Earth’s climate and weather. It flew in the international A-Train constellation for coincident Earth observations from launch until September 13, 2018, when CALIPSO began lowering its orbit from 705 km to 688 km (428 miles)above the Earth to resume formation flying with CloudSat as part of the “C-Train”. The CALIPSO satellite carried three remote sensing instruments: the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP), the Imaging Infrared Radiometer (IIR), and the Wide Field-of-View Camera (WFC). By mutual agreement between NASA and CNES, the CALIPSO science mission concluded on August 1, 2023.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_lid_l3_tropospheric_apro_cloudyskytransparent-standard-v4-20&quot;&gt;CAL_LID_L3_Tropospheric_APro_CloudySkyTransparent-Standard-V4-20&lt;/h4&gt;
CAL_LID_L3_Tropospheric_APro_CloudySkyTransparent-Standard-V4-20 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Lidar Level 3 Tropospheric Aerosol Profiles, Cloudy Sky Transparent Data, Standard Version 4-20 data product. Data is collected using the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) instrument. Data generation and distribution of this V4.20 product ended on July 1, 2020, to support a change in the operating system of the CALIPSO production clusters. The V4.21 data product covers July 1, 2020, to current. The CALIPSO lidar level 3 aerosol data product reports monthly mean profiles of aerosol optical properties on a uniform spatial grid. It is intended to be a tropospheric product, so data are only reported below altitudes of 12 km. All level 3 parameters are derived from the version 4.20 CALIOP level 2 aerosol profile product and have been quality screened before averaging. The primary quantities reported are vertical profiles of the aerosol extinction coefficient at 532 nm and its vertical integral, the aerosol optical depth (AOD). Aerosol type and spatial distribution information are also included. Averaged profile data is reported for all aerosols, regardless of type, and for mineral dust aerosols only. Classification of dust is based on the aerosol-type flags in the level 2 profile product. To keep level 3 file sizes manageable, there are four different types of level 3 files produced, depending on the sky condition and the temporal coverage of the data before averaging: Description of the Four Sky Conditions (Day, Night) 1) All Sky: All level 2 columns are averaged, regardless of cloud occurrence, 2) Cloud-Free: Only cloud-free level 2 columns are averaged, 3) Cloudy-Sky, Transparent: Only level 2 columns containing transparent clouds are averaged, and 4) Cloud-Sky, Opaque: Only level 2 columns containing opaque clouds are averaged CALIPSO was launched on April 28, 2006, to study the impact of clouds and aerosols on the Earth&amp;#39;s radiation budget and climate. It flies in formation with five other satellites in the international &amp;quot;A-Train&amp;quot; (PDF) constellation for coincident Earth observations. The CALIPSO satellite comprises three instruments: the CALIOP, the Imaging Infrared Radiometer (IIR), and the Wide Field Camera (WFC). CALIPSO is a joint satellite mission between NASA and the French Agency CNES (Centre National D&amp;#39;Etudes Spatiales).
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_lid_l3_tropospheric_apro_cloudyskytransparent-standard-v5-00&quot;&gt;CAL_LID_L3_Tropospheric_APro_CloudySkyTransparent-Standard-V5-00&lt;/h4&gt;
CAL_LID_L3_Tropospheric_APro_CloudSkyTransparent-Standard-V5-00 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Lidar Level 3 Tropospheric Aerosol, Cloudy Sky Transparent, data product. This data product was collected using the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) instrument. This data product, generated separately between day and night, reports monthly mean profiles of aerosol optical properties on a uniform spatial grid. It is a tropospheric product, so data are only reported below altitudes of 12km. All parameters are derived from the version 5.00 CALIOP Level 2 data and have been quality screened prior to averaging. The primary quantities reported are vertical profiles of the aerosol extinction coefficient at 532 nm and its vertical integral, the aerosol optical depth (AOD). Aerosol type and spatial distributional information are also included. The Cloudy Sky Transparent designate indicates that only level 2 columns containing transparent clouds are averaged. CALIPSO was a partnership between NASA and the French Space Agency, CNES. CALIPSO was launched on April 28, 2006 to study the many roles played by clouds and aerosols in Earth’s climate and weather. It flew in the international A-Train constellation for coincident Earth observations from launch until September 13, 2018, when CALIPSO began lowering its orbit from705 km to 688 km (428 miles) above the Earth to resume formation flying with CloudSat as part of the “C-Train”. The CALIPSO satellite carried three remote sensing instruments: the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP), the Imaging Infrared Radiometer (IIR), and the Wide Field-of-View Camera (WFC). By mutual agreement between NASA and CNES, the CALIPSO science mission concluded on August 1, 2023.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_wfc_l1_asm-standard-v4-00&quot;&gt;CAL_WFC_L1_Asm-Standard-V4-00&lt;/h4&gt;
CAL_WFC_L1_Asm-Standard-V4-00 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Wide Field Camera (WFC)Level 1B Assembler Version 4-00 data product. The WFC Level 1B Assembler data products contain geolocated nighttime daily digital count and daily statistical data which comes from the calibration product. The Assembler takes the calibration data and calculates the statistics foreach pixel (mean, standard deviation, maximum, and minimum). CALIPSO was a partnership between NASA and the French Space Agency, CNES. CALIPSO was launched on April 28, 2006 to study the many roles played by clouds and aerosols in Earth’s climate and weather. It flew in the international A-Train constellation for coincident Earth observations from launch until September 13, 2018, when CALIPSO began lowering its orbit from 705 km to 688 km (428 miles)above the Earth to resume formation flying with CloudSat as part of the “C-Train”. The CALIPSO satellite carried three remote sensing instruments: the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP), the Imaging Infrared Radiometer (IIR), and the Wide Field-of-View Camera(WFC). By mutual agreement between NASA and CNES, the CALIPSO science mission concluded on August 1, 2023.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cal_wfc_l1_cal-standard-v4-00&quot;&gt;CAL_WFC_L1_Cal-Standard-V4-00&lt;/h4&gt;
CAL_WFC_L1_Cal-Standard-V4-00 is the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Wide Field Camera (WFC)Level 1B Calibration Version 4-00 data product. The WFC Level 1B Calibration data products contain geolocated nighttime digital count data. The calibration data is collected over a 25-second segment on the dark side of every orbit. CALIPSO was a partnership between NASA and the French Space Agency, CNES. CALIPSO was launched on April 28, 2006 to study the many roles played by clouds and aerosols in Earth’s climate and weather. It flew in the international A-Train constellation for coincident Earth observations from launch until September 13, 2018,when CALIPSO began lowering its orbit from 705 km to 688 km (428 miles) above the Earth to resume formation flying with CloudSat as part of the “C-Train”. The CALIPSO satellite carried three remote sensing instruments: the Cloud-Aerosol Lidar with Orthogonal Polarization(CALIOP), the Imaging Infrared Radiometer (IIR), and the Wide Field-of-View Camera (WFC). By mutual agreement between NASA and CNES, the CALIPSO science mission concluded on August1, 2023.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA CAR Project</title>
      <link>https://registry.opendata.aws/nasa-car</link>
      <guid>https://registry.opendata.aws/nasa-car</guid>
      <description>CAR will fly in 2022-2025 for the NASA’s Student Airborne Science Activation (SaSa) project. GSFC scientists and engineers will operate CAR together with
&lt;br&gt;&lt;h4 id&#x3D;&quot;car_arctas_l1c&quot;&gt;CAR_ARCTAS_L1C&lt;/h4&gt;
ARCTAS focuses on advancing understanding of the factors driving current changes in the Arctic region including transport of mid-latitude pollution, boreal forest fires, aerosol radiative forcing, and chemical processes. ARCTAS aimed to use detailed observations from aircraft to provide the validation, retrieval constraints, correlative data, and process information needed to better achieve the potential of satellites for Arctic research. The plan is for the combination of satellite and aircraft data to provide together powerful information for constraining and evaluating models of Arctic atmospheric composition and climate, and thus improve model projections of future change.
&lt;br&gt;&lt;h4 id&#x3D;&quot;car_armcas_brdf&quot;&gt;CAR_ARMCAS_BRDF&lt;/h4&gt;
The Arctic Radiation Measurement in Column Atmosphere-surface System (ARMCAS) was a collaborative research effort between the Cloud and Aerosol Research (CAR) Group, Department of Atmospheric Sciences, University of Washington (led by Professor Peter V. Hobbs) and Drs. Michael King and Si-Chee Tsay of NASA/Goddard. The field portion of ARMCAS was based out of Deadhorse, Alaska, from June 3-15, 1995. Flights of the University of Washington&amp;#39;s Convair C-131A research aircraft and NASA&amp;#39;s ER-2 aircraft took place over the tundra of the North Slope and over the partially ice-covered Beaufort Sea. Several of these flights were closely coordinated in order to provide simultaneous in situ and remote sensing measurements of arctic clouds. This data set consists of observations made with the CAR instrument and includes values for bidirectional reflectance factor at varying spectral bands.
&lt;br&gt;&lt;h4 id&#x3D;&quot;car_clams_brdf&quot;&gt;CAR_CLAMS_BRDF&lt;/h4&gt;
CLAMS is the Chesapeake Lighthouse and Aircraft Measurements for Satellites field campaign sponsored by CERES, MISR, MODIS-Atmospheres and the NASA/GEWEX Global Aerosol Climatology Project (GACP). The centerpiece of CLAMS is the Chesapeake Lighthouse sea platform 20 km east of Virginia Beach, at which NASA and NOAA make continuous, long-term measurements of radiation, meteorology, and ocean waves. Members of the CERES, MISR and MODIS instrument teams are collaborating to accomplish a common set of objectives tied to the validation of EOS data products. The CLAMS campaign took place in July-August 2001 to validate Terra data products from a shortwave closure experiment targeting clear (cloud-free) sky conditions and focused on obtaining: 1. more accurate spectral and broadband radiative fluxes at the surface and within the atmosphere, 2. characterization of ocean optics in the vicinity of the lighthouse, and 3. description of the atmospheric aerosol amounts, micro-physical and optical properties, and their variability. This data set consists of observations made with the CAR instrument and includes values for bidirectional reflectance factor at varying spectral bands.
&lt;br&gt;&lt;h4 id&#x3D;&quot;car_clasic_brdf&quot;&gt;CAR_CLASIC_BRDF&lt;/h4&gt;
CLASIC (Cloud and Land Surface Interaction Campaign) focuses on advancing the understanding of how land surface processes influence cumulus convection. CLASIC was conducted in the Southern Great Plains (SGP &amp;#8211; a region comprising Kansas, Oklahoma, and Texas) of the United States during June 2007. The SGP site consists of in situ and remote-sensing instrument clusters arrayed across approximately 55,000 square miles (143,000 square kilometers) in north-central Oklahoma, making it the largest and most extensive climate research field site in the world. The CAR flew aboard Sky Research Jetstream-31 and measured spectral and angular distribution of scattered light by clouds and aerosols, and provided bidirectional reflectance of various surfaces, and imagery of cloud and Earth surface features. By making such diverse measurements, our goal is to widen the audience of potential end-users and to foster collaborations among campaign participants and with outside users. This data set consists of observations made with the CAR instrument and includes values for bidirectional reflectance factor at varying spectral bands.
&lt;br&gt;&lt;h4 id&#x3D;&quot;car_clasic_l1c&quot;&gt;CAR_CLASIC_L1C&lt;/h4&gt;
CLASIC (Cloud and Land Surface Interaction Campaign) focuses on advancing the understanding of how land surface processes influence cumulus convection. The CAR flew aboard Sky Research Jetstream-31 and measured spectral and angular distribution of scattered light by clouds and aerosols, and provided bidirectional reflectance of various surfaces, and imagery of cloud and Earth surface features. By making such diverse measurements, our goal is to widen the audience of potential end-users and to foster collaborations among campaign participants and with outside users.
&lt;br&gt;&lt;h4 id&#x3D;&quot;car_discoveraq_l1c&quot;&gt;CAR_DISCOVERAQ_L1C&lt;/h4&gt;
DISCOVER-AQ, a NASA Earth Venture program funded mission, stands for Deriving Information on Surface Conditions from Column and Vertically Resolved Observations Relevant to Air Quality. In recent years, progress in reaching air quality goals has begun to plateau for many locations. Furthermore, near-surface pollution is one of the most challenging problems for Earth observations from space. However, with an improved ability to monitor pollution from satellites from DISCOVER-AQ, scientists could make better air quality forecasts, more accurately determine the sources of pollutants in the air and more closely determine the fluctuations in emissions levels. In short, the more accurate data scientists have at hand, the better society is able to deal effectively with lingering pollution problems.
&lt;br&gt;&lt;h4 id&#x3D;&quot;car_eco3d_l1c&quot;&gt;CAR_ECO3D_L1C&lt;/h4&gt;
This study promotes the understanding of vegetation response to changing forcing factors such as climate, storm frequency, and management practices, and is directly traceable to missions such as MODIS, MISR, and ICESat-2.
&lt;br&gt;&lt;h4 id&#x3D;&quot;car_eco3d_brdf&quot;&gt;CAR_ECO3D_BRDF&lt;/h4&gt;
This study provide critical measurements on 3-dimensional structure of vegetation, which is important for quantifying the amount of carbon stored in biomass. It promotes the understanding of vegetation response to changing forcing factors such as climate, storm frequency, and management practices, and is directly traceable to missions such as MODIS, MISR, and ICESat-2.During the ECO-3D mission in 2011, the CAR instrument was flown aboard the NASA P-3 and obtained measurements of bidirectional reflectance distribution function (BRDF) over forests ranging from Boreal to tropical wetlands covering sites from Quebec to Southern Florida. This data set consists of observations made with the CAR instrument and includes values for bidirectional reflectance factor at varying spectral bands.
&lt;br&gt;&lt;h4 id&#x3D;&quot;car_fireace_brdf&quot;&gt;CAR_FIREACE_BRDF&lt;/h4&gt;
The scientific objectives of FIRE/ACE are to study impact of Arctic clouds on radiation exchange between surface, atmosphere, and space, and the influence of surface characteristics of sea ice, leads, and ice melt ponds on these clouds. FIRE/ACE will attempt to document, understand, and predict the Arctic cloud-radiation feedbacks, including changes in cloud fraction and vertical distribution, water vapor cloud content, cloud particle concentration and size, and cloud phase as atmospheric temperature and chemical composition change. FIRE/ACE uses the data to focus on improving current climate model simulations of the Arctic climate, especially with respect to clouds and their effects on the surface energy budget. In addition, FIRE/ACE addresses a number of scientific questions dealing with radiation, cloud microphysics, and atmospheric chemistry. This data set consists of observations made with the CAR instrument and includes values for bidirectional reflectance factor at varying spectral bands.
&lt;br&gt;&lt;h4 id&#x3D;&quot;car_intexb_l1c&quot;&gt;CAR_INTEXB_L1C&lt;/h4&gt;
INTEX-B (Intercontinental Chemical Transport Experiment-Phase B) focuses on the long-range transport of pollution, global atmospheric photochemistry, and the effects of aerosols and clouds on radiation and climate. It has two phases: phase 1 of the study was performed in Mexico from March 1-20, 2006, and phase 2 was performed in April and May and focused on Asian City pollution outflow over the western Pacific.
&lt;br&gt;&lt;h4 id&#x3D;&quot;car_kuwaitoilfire_brdf&quot;&gt;CAR_KUWAITOILFIRE_BRDF&lt;/h4&gt;
CAR Kuwait Oil Fire mission measured bidirectional reflectance function of smoke from Kuwait oil fires during the Kuwait Oil Fire Smoke Experiment. Measurements were also taken over the Saudi Arabian desert with overlying desert dust, and Persian Gulf waters with some overlying aerosols. This experiment was a part of an international research effort in response to an environmental crisis, when over 600 oil wells in Kuwait were ignited by Iraqi forces in 1991. The resulting fires produced large plumes of smoke that had significant effects on the Persian Gulf region but limited global effects. Between May 16 and June 12, 1991, the Kuwait Oil Fire Smoke Experiment (KOFSE) was conducted in the Persian Gulf Region. The purpose of KOFSE was to determine the chemical and physical nature of the smoke and to investigate its potential effects on air quality, weather, and climate. This data set consists of observations made with the CAR instrument and includes values for bidirectional reflectance factor at varying spectral bands.
&lt;br&gt;&lt;h4 id&#x3D;&quot;car_leadex_brdf&quot;&gt;CAR_LEADEX_BRDF&lt;/h4&gt;
CAR LEADEX mission measured bidirectional reflectance functions for four common arctic surfaces: snow covered sea ice, melt season sea ice, snow covered tundra, and tundra shortly after snowmelt. The measurements show how the reflectance differs amongst the mentioned arctic surfaces and provides insights into the variability of albedo in the arctic. This data set consists of observations made with the CAR instrument and includes values for bidirectional reflectance factor at varying spectral bands.
&lt;br&gt;&lt;h4 id&#x3D;&quot;car_safari_brdf&quot;&gt;CAR_SAFARI_BRDF&lt;/h4&gt;
The Southern African Regional Science Initiative (SAFARI) 2000 is an international science field campaign aimed at developing a better understanding of the southern Africa earth-atmosphere-human system. The goal of SAFARI 2000 is to identify and understand the relationship between the physical, chemical, biological, and anthropogenic processes that underlie the biogeophysical and biogeochemical systems of southern Africa. Particular emphasis will be placed upon biogenic, pyrogenic, and anthropogenic emissions - their characterization and quantification, their transport and transformations in the atmosphere, their influence on regional climate and meteorology, their eventual deposition, and the effects of this deposition on ecosystems. This data set consists of observations made with the CAR instrument and includes values for bidirectional reflectance factor at varying spectral bands.
&lt;br&gt;&lt;h4 id&#x3D;&quot;car_scara_brdf&quot;&gt;CAR_SCARA_BRDF&lt;/h4&gt;
The objectives for the SCAR mission are to advance our knowledge of how the physical, chemical and radiative processes in our atmosphere are affected by sulfate aerosol and smoke from biomass burning; to improve our expertise at remotely sensing smoke, water vapor, clouds, vegetation and fires; and to assess the effects of deforestation and biomass burning on tropical landscapes. The SCAR-A campaign occurred in western Atlantic Ocean. This data set consists of observations made with the CAR instrument and includes values for bidirectional reflectance factor at varying spectral bands.
&lt;br&gt;&lt;h4 id&#x3D;&quot;car_scara_l1c&quot;&gt;CAR_SCARA_L1C&lt;/h4&gt;
The objectives for the SCAR mission are to advance our knowledge of how the physical, chemical and radiative processes in our atmosphere are affected by sulfate aerosol and smoke from biomass burning; to improve our expertise at remotely sensing smoke, water vapor, clouds, vegetation and fires; and to assess the effects of deforestation and biomass burning on tropical landscapes. The SCAR-B campaign occurred in western Atlantic Ocean.
&lt;br&gt;&lt;h4 id&#x3D;&quot;car_scarb_brdf&quot;&gt;CAR_SCARB_BRDF&lt;/h4&gt;
The objectives for the SCAR mission are to advance our knowledge of how the physical, chemical and radiative processes in our atmosphere are affected by sulfate aerosol and smoke from biomass burning; to improve our expertise at remotely sensing smoke, water vapor, clouds, vegetation and fires; and to assess the effects of deforestation and biomass burning on tropical landscapes. The SCAR-B campaign occurred in Brazil. This data set consists of observations made with the CAR instrument and includes values for bidirectional reflectance factor at varying spectral bands.
&lt;br&gt;&lt;h4 id&#x3D;&quot;car_skukuza_brdf&quot;&gt;CAR_SKUKUZA_BRDF&lt;/h4&gt;
CAR mission Skukuza measured bidirectional reflection functions over different natural surfaces and ecosystems in southern Africa. The measurements were conducted to characterize surface anisotropy in support of the CAR SAFARI mission and to validate products from NASA&amp;#39;s Earth Observing System satellites. This data set consists of observations made with the CAR instrument and includes values for bidirectional reflectance factor at varying spectral bands.
&lt;br&gt;&lt;h4 id&#x3D;&quot;car_skukuza_l1c&quot;&gt;CAR_SKUKUZA_L1C&lt;/h4&gt;
CAR mission Skukuza measured bidirectional reflection functions over different natural surfaces and ecosystems in southern Africa. The measurements were conducted to characterize surface anisotropy in support of the CAR SAFARI mission and to validate products from NASA’s Earth Observing System satellites.
&lt;br&gt;&lt;h4 id&#x3D;&quot;car_snowex17_brdf&quot;&gt;CAR_SNOWEX17_BRDF&lt;/h4&gt;
SnowEx is a multi-year airborne project to help advance capabilities, and plan for a near-future space mission to monitor global seasonal snow water equivalent - currently an inconsistently collected and difficult-to-obtain data point that scientists say is critical to understanding the world&amp;#39;s water resources. This data set consists of observations made with the CAR instrument and includes values for bidirectional reflectance factor at varying spectral bands.
&lt;br&gt;&lt;h4 id&#x3D;&quot;car_snowex17_l1c&quot;&gt;CAR_SNOWEX17_L1C&lt;/h4&gt;
SnowEx is a multi-year airborne project to help advance capabilities, and plan for a near-future space mission to monitor global seasonal snow water equivalent — currently an inconsistently collected and difficult-to-obtain data point that scientists say is critical to understanding the world’s water resources.
&lt;br&gt;&lt;h4 id&#x3D;&quot;car_tarfox_brdf&quot;&gt;CAR_TARFOX_BRDF&lt;/h4&gt;
CAR TARFOX mission collected data in the western Atlantic Ocean on the effects of tropospheric aerosols on radiation budgets in cloud free skies. The mission also measured the chemical, physical, and optical properties of aerosols. In July 1996, CAR data were collected aboard the University of Washington C-131A aircraft over the forested Great Dismal Swamp wetlands south of Norfolk, Virginia and the Atlantic Ocean approximately 340 km offshore of Richmond, Virginia. This data set consists of observations made with the CAR instrument and includes values for bidirectional reflectance factor at varying spectral bands.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA CARAFE Project</title>
      <link>https://registry.opendata.aws/nasa-carafe</link>
      <guid>https://registry.opendata.aws/nasa-carafe</guid>
      <description>An inventory of NASA&amp;#39;s airborne and field campaigns for Earth Science
&lt;br&gt;&lt;h4 id&#x3D;&quot;carafe_2016_2017_v2_2002&quot;&gt;CARAFE_2016_2017_v2_2002&lt;/h4&gt;
This dataset provides airborne eddy covariance (EC) fluxes of carbon dioxide, methane, sensible heat, and latent heat at high spatial resolution collected during the NASA Carbon Airborne Flux Experiment (CARAFE) airborne 2016 and 2017 campaigns. CARAFE utilized the NASA C-23 Sherpa aircraft with a suite of commercial and custom instrumentation. Deployment occurred across the Mid-Atlantic Region for the period 2016-09-07 through 2016-09-26 and 2017-05-03 through 2017-05-26. The data also include downwelling radiation, water vapor, pressure, temperature, wind, and aircraft navigation data. Airborne EC can quantify surface fluxes at local to regional scales, potentially helping to bridge gaps between top-down and bottom-up flux estimates and offering novel insights into biophysical and biogeochemical processes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.ornldaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA CARVE Project</title>
      <link>https://registry.opendata.aws/nasa-carve</link>
      <guid>https://registry.opendata.aws/nasa-carve</guid>
      <description>An inventory of NASA&amp;#39;s airborne and field campaigns for Earth Science
&lt;br&gt;&lt;h4 id&#x3D;&quot;polar-vprm_alaskan-nee_1314&quot;&gt;Polar-VPRM_Alaskan-NEE_1314&lt;/h4&gt;
This data set provides 3-hourly estimates of gross ecosystem CO2 exchange (GEE) and respiration (autotrophic and heterotrophic) for the state of Alaska from 2012 to 2014. The data were generated using the Polar Vegetation Photosynthesis and Respiration Model (PolarVPRM) and are provided at ~ 1 km2 [1/4-degree (longitude) by 1/6-degree (latitude)] pixel resolution. The PolarVPRM produces high-frequency estimates of GEE of CO2 for North American biomes from remotely-sensed data sets. For Alaska, the model used meteorological inputs from the North American regional re-analysis (NARR) and inputs of fractional snow cover and land surface water index (LSWI) from the Moderate Resolution Imaging Spectroradiometer (MODIS). Land surface greenness was factored into the model from three sources: 1) Enhanced Vegetation Index (EVI) from MODIS; 2) Solar Induced Florescence (SIF) from the Orbiting Carbon Observatory 2 (OCO-2); and 3) SIF from the Global Ozone Monitoring Experiment 2 (GOME-2). Three independent estimates of GEE are included in the data set, one for each source of greenness observations.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ch4_aircraft_stilt_footprints_1300&quot;&gt;CH4_Aircraft_STILT_footprints_1300&lt;/h4&gt;
This data set provides the results of (1) year-round measurements of methane (CH4) flux along with soil and air temperatures at five eddy covariance towers at sites located in the Alaskan Arctic tundra from June 2013 to December 2014 and (2) airborne CH4 and ozone (O3) measurements collected during Carbon in Arctic Reservoirs Vulnerability Experiment (CARVE) flight campaigns for years 2012 through 2014. The included site-level flux data at half-hourly intervals were calculated following standard eddy covariance data processing procedures. Also reported are daily mean methane flux, soil temperature with depth, and air temperature for each tower site. Also identified for each flux tower site were the &amp;quot;zero curtain&amp;quot; periods of extended cold when soil temperatures were poised near 0 degrees C. The reported CARVE airborne CH4 and O3 data were aggregated horizontally at 5 km intervals. Measurement heights are reported. These aircraft positions were treated as receptors in a Stochastic Time-Inverted Lagrangian Transport (STILT) model coupled with meteorology fields from the polar variant of the Weather and Research Forecasting model (WRF), in order to model the land surface influence on the aircraft-observed methane concentrations. The summed land surface influence on the aircraft data at each position is reported. For each airborne measurement, 2D surface influence fields (i.e. footprints) at two different spatial resolutions were derived using the WRF-STILT simulations. These gridded footprints are provided as netCDF formatted files. Regional C-CH4 fluxes were calculated from the CARVE CH4 data and footprints for the period 2012-2014 and are also included with this data set. Acknowledgements: Data collection efforts were funded by NSF ARCSS project &amp;quot;Methane Loss From Arctic&amp;quot; (ARCSS #1204263; &lt;a href&#x3D;&quot;http://www.nsf.gov/awardsearch/showAward?AWD_ID&#x3D;1204263&quot;&gt;http://www.nsf.gov/awardsearch/showAward?AWD_ID&#x3D;1204263&lt;/a&gt;) and by NASA&amp;#39;s Carbon in Arctic Reservoirs Vulnerability Experiment (CARVE).
&lt;br&gt;&lt;h4 id&#x3D;&quot;akfed_v1_1282&quot;&gt;AKFED_V1_1282&lt;/h4&gt;
This data set provides estimates of annual carbon emissions (kg carbon per square meter) from boreal fires at 450-m resolution for the state of Alaska between 2001 and 2013. To produce these data, daily burned area for 2001 to 2013 was mapped using imagery from the Moderate Resolution Imaging Spectroradiometer (MODIS) combined with perimeters from the Alaska Large Fire Database. Carbon consumption was calibrated using available field measurements from black spruce forests in Alaska. Above- and below-ground carbon consumption were modeled based on environmental variables including elevation, day of burning within the fire season, pre-fire tree cover and the differenced normalized burn ratio (dNBR). Modeled uncertainties in carbon consumption are included in the data set. The derived burn area and carbon emissions product, referred to as the Alaskan Fire Emissions Database (AKFED), provides a resource for study of the environmental controls on daily fire dynamics, boreal fire emissions in biogeochemical models, and potential feedbacks from changing fire regimes. There are 26 data files in GeoTIFF (.tif) format with this data set. There are 13 .tifs for carbon consumption, one for each year, and 13 .tifs for carbon consumption uncertainty, one for each year.
&lt;br&gt;&lt;h4 id&#x3D;&quot;alaskan_ch4_co2_fluxes_1316&quot;&gt;Alaskan_CH4_CO2_Fluxes_1316&lt;/h4&gt;
This data set provides hourly atmospheric concentrations of methane (CH4), carbon dioxide (CO2), and carbon monoxide (CO) as mole fractions, from January 2012 to December 2014 measured at the CARVE flux tower in Fox, Alaska (17 km north of Fairbanks) as part of NASA&amp;#39;s Carbon in Arctic Reservoirs Vulnerability Experiment (CARVE). High-resolution meteorological fields from the Polar Weather Research and Forecasting (WRF) model coupled with the Stochastic Time-Inverted Lagrangian Transport model (WRF- STILT), along with the Polar Vegetation Photosynthesis and Respiration Model (PolarVPRM) were used to determine the influence region of the tower site and investigate the inter-annual and seasonal variability of regional fluxes of CO2 and CH4 in boreal Alaska using the tower observations. Modeled estimates of CH4, CO2, and CO background concentrations are provided. The WRF-STILT model &amp;quot;footprints&amp;quot; for the CARVE tower are provided with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;carve_reports_1434&quot;&gt;CARVE_Reports_1434&lt;/h4&gt;
This dataset includes detailed daily flight reports from each of the airborne campaigns over the Alaskan and Canadian Arctic for the Carbon in Arctic Reservoirs Vulnerability Experiment (CARVE). The reports include plots of the flight path, altitude, wind and weather conditions, IR and visible light images, and initial analysis of the atmospheric gas concentrations encountered along the flight. Flight campaigns took place from 2012 to 2015 between the months of March and November to enable investigation of both seasonal and inter-annual variability in atmospheric gas content. The CARVE measurements are crucial for understanding changes in Arctic carbon cycling and the potential threats posed by thawing of Arctic permafrost.
&lt;br&gt;&lt;h4 id&#x3D;&quot;carve_land_thaw_state_1383&quot;&gt;CARVE_Land_Thaw_State_1383&lt;/h4&gt;
This data set provides daily 10 km resolution maps of the Alaskan and Arctic Boreal land surface state as either frozen, melting, or thawed. These data are generated from passive microwave radiometer observations made from 2003 through 2014 by the Advanced Microwave Scanning Radiometer (AMSR-E) and the Special Sensor Microwave Imager (SSM/I). Data products overlap with science data collections carried out during the Carbon in Arctic Reservoirs Vulnerability Experiment (CARVE).
&lt;br&gt;&lt;h4 id&#x3D;&quot;carve_ecosystem_ch4_flux_1558&quot;&gt;CARVE_Ecosystem_CH4_Flux_1558&lt;/h4&gt;
This dataset provides methane flux estimates derived from airborne measurements collected over Alaska and the western Yukon Territory during the Carbon in Arctic Reservoirs Vulnerability Experiment (CARVE) between 2012 and 2014. The state-scale methane fluxes were calculated using a combination of atmospheric profiles and lagrangian transport modeling. The methane flux estimates were used in a simple linear regression model to estimate the fluxes from the tundra and boreal ecosystems. Methane fluxes were also used with a combination of environmental variables to derive a statistical relationship between domain-wide flux and soil temperature. Soil temperature products from North American Regional Reanalysis and derived parameters from a Boltmann-Arrhenius model were used to model methane flux and related uncertainties within the domain at monthly and daily frequencies.
&lt;br&gt;&lt;h4 id&#x3D;&quot;bc_aerosol_dynamics_alaska_1340&quot;&gt;BC_Aerosol_Dynamics_Alaska_1340&lt;/h4&gt;
This data set provides measurements of the isotopic composition of black carbon and organic carbon aerosols collected at two locations in interior Alaska during the summer of 2013, as part of NASA&amp;#39;s Carbon in Arctic Reservoirs Vulnerability Experiment (CARVE). The delta14C end member of fire aerosol was derived and linked to soil elemental and isotopic composition in Alaskan boreal forests. Soil and aerosol measurements were used to estimate average depth of burn in Alaska during the summer of 2013.
&lt;br&gt;&lt;h4 id&#x3D;&quot;carve_photos_1435&quot;&gt;CARVE_Photos_1435&lt;/h4&gt;
This dataset contains photos taken by scientists aboard the CARVE aircraft during airborne campaigns over the Alaskan and Canadian Arctic for the Carbon in Arctic Reservoirs Vulnerability Experiment (CARVE). Flight campaigns took place from 2012 to 2015 between the months of March and November to enable investigation of both seasonal and inter-annual variability in atmospheric gas content.
&lt;br&gt;&lt;h4 id&#x3D;&quot;carve_videos_1433&quot;&gt;CARVE_Videos_1433&lt;/h4&gt;
This dataset contains videos captured by a camera mounted on the CARVE aircraft during airborne campaigns over the Alaskan and Canadian Arctic for the Carbon in Arctic Reservoirs Vulnerability Experiment (CARVE). Flight campaigns took place from 2012 to 2015 between the months of March and November to enable investigation of both seasonal and inter-annual variability in atmospheric gas content.
&lt;br&gt;&lt;h4 id&#x3D;&quot;carve_l1_infrared_1428&quot;&gt;CARVE_L1_Infrared_1428&lt;/h4&gt;
This data set provides earth referenced radiance counts measured by the Forward Looking Infrared (FLIR) camera aboard the CARVE aircraft between April 2013 and November 2015 for the Carbon in Arctic Reservoirs Vulnerability Experiment (CARVE). The FLIR camera records images of the surface temperature while measuring concentrations of atmospheric carbon dioxide, methane, and ozone. Thermal images from the FLIR camera will be used to characterize land surfaces underlain by permafrost during specific phases in the freeze-thaw cycle. The measurements included in this data set are crucial for understanding changes in Arctic carbon cycling and the potential threats posed by thawing of Arctic permafrost.
&lt;br&gt;&lt;h4 id&#x3D;&quot;carve_l1_flightpath_winds_1427&quot;&gt;CARVE_L1_FlightPath_Winds_1427&lt;/h4&gt;
This data set provides high-frequency wind speed and direction data for the C-23 Sherpa aircraft during airborne campaigns over the Alaskan and Canadian Arctic as part of the Carbon in Arctic Reservoirs Vulnerability Experiment (CARVE). The data were collected in situ using the Aventech AIMMS-30 Airborne Wind Sensor onboard the aircraft and are presented at 1-second intervals throughout each flight. The Winds instrument was available for flights in year 2015 only. The measurements included in this data set are most useful when paired with the scientific data collected by other CARVE airborne instruments.
&lt;br&gt;&lt;h4 id&#x3D;&quot;carve_l1_flightpath_1425&quot;&gt;CARVE_L1_FlightPath_1425&lt;/h4&gt;
This data set provides high-frequency geolocation, time, height, pitch, roll, and heading information for the C-23 Sherpa aircraft during airborne campaigns over the Alaskan and Canadian Arctic as part of the Carbon in Arctic Reservoirs Vulnerability Experiment (CARVE). The data were collected in situ using the Digital Air Data System (DADS) onboard the aircraft and are presented at 1-second intervals throughout each flight. Flight campaigns took place from 2012 to 2015 between the months of March and November to enable investigation of both seasonal and inter-annual variability in atmospheric gas content. The measurements included in this data set are useful for matching aircraft position with the scientific data collected by other CARVE airborne instruments.
&lt;br&gt;&lt;h4 id&#x3D;&quot;carve_l1_ground_flux_1424&quot;&gt;CARVE_L1_Ground_Flux_1424&lt;/h4&gt;
This data set provides ground in situ flux and meteorological science data from fixed instruments at three eddy covariance tower sites located in the Alaskan Arctic tundra. Real and gap-filled observations of carbon dioxide, methane, water vapor, and latent energy flux in addition to standard meteorological and environmental variables are reported at half-hourly intervals between 2011 and 2015 for sites at Atqasuk, Barrow, and Ivotuk, Alaska. The three sites form a 300-km north-south transect on the North Slope of Alaska, each site representing distinct Arctic vegetation communities. These tower measurements create a long-term record of one of the largest, most volatile carbon stocks on the planet. Observations from these towers are being used to determine the seasonal and inter-annual patterns of CO2 and CH4 flux, and their relationship to changes in environmental factors.
&lt;br&gt;&lt;h4 id&#x3D;&quot;carve_l1_fts_spectra_1426&quot;&gt;CARVE_L1_FTS_Spectra_1426&lt;/h4&gt;
This data set contains Level 1 spectral radiance data collected using the Fourier Transform Spectrometer (FTS) during airborne campaigns over the Alaskan and Canadian Arctic for the Carbon in Arctic Reservoirs Vulnerability Experiment (CARVE). Flight campaigns took place from 2012 to 2015 between the months of March and November to enable investigation of both seasonal and inter-annual variability in atmospheric gas content. The measurements included in this data set are crucial for understanding changes in Arctic carbon cycling and the potential threats posed by thawing of Arctic permafrost.
&lt;br&gt;&lt;h4 id&#x3D;&quot;carve_l2_atmosgas_harvard_1403&quot;&gt;CARVE_L2_AtmosGas_Harvard_1403&lt;/h4&gt;
This data set provides atmospheric carbon dioxide (CO2), methane (CH4), and carbon monoxide (CO) concentrations from airborne campaigns over the Alaskan and Canadian arctic for the Carbon in Arctic Reservoirs Vulnerability Experiment (CARVE). The data were collected in situ using a four-species cavity ring-down spectrometer system (CRDS; Picarro Inc.) provided by Harvard University and are presented at 5-second intervals throughout each flight. The Harvard CRDS instrument only collected data in 2012-2014; no Harvard data are available for year 2015. Aircraft latitude, longitude, and altitude are also provided. CARVE flight campaigns took place from 2012 to 2015 between the months of March and November to enable investigation of both seasonal and inter-annual variability in atmospheric gas content. The measurements included in this data set are crucial for understanding changes in Arctic carbon cycling and the potential threats posed by thawing of Arctic permafrost.
&lt;br&gt;&lt;h4 id&#x3D;&quot;carve_l2_atmosgas_noaa_1401&quot;&gt;CARVE_L2_AtmosGas_NOAA_1401&lt;/h4&gt;
This data set provides atmospheric carbon dioxide (CO2), methane (CH4), carbon monoxide (CO), and water vapor (H2O) concentrations from airborne campaigns over the Alaskan and Canadian arctic for the Carbon in Arctic Reservoirs Vulnerability Experiment (CARVE). The data were collected in situ using a cavity ring-down spectrometer (CRDS; Picarro Inc.) and are presented at 2-second intervals throughout each flight. Aircraft latitude, longitude, and altitude are also provided. Flight campaigns took place from 2012 to 2015 between the months of March and November to enable investigation of both seasonal and inter-annual variability in atmospheric gas content. The measurements included in this data set are crucial for understanding changes in Arctic carbon cycling and the potential threats posed by thawing of Arctic permafrost.
&lt;br&gt;&lt;h4 id&#x3D;&quot;carve_l2_atmosgas_ground_1419&quot;&gt;CARVE_L2_AtmosGas_Ground_1419&lt;/h4&gt;
This data set provides atmospheric methane (CH4), carbon dioxide (CO2), and carbon monoxide (CO) dry air mole fractions and water vapor mole fractions (H2O) from continuous in situ measurements at the CARVE flux tower in Fox, Alaska between October 2011 and May 2015 for the Carbon in Arctic Reservoirs Vulnerability Experiment (CARVE). Air was drawn from three different heights above the base of the tower (31.7 m, 17.1 m, and 4.9 m) and analyzed using a Picarro cavity ring-down spectrometer (CRDS). Measurements of ambient and sonic temperature, vertical and horizontal velocity, and atmospheric pressure are also included in the data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;carve_l2_flask_1404&quot;&gt;CARVE_L2_Flask_1404&lt;/h4&gt;
This data set provides atmospheric carbon dioxide (CO2), methane (CH4), carbon monoxide (CO), molecular hydrogen (H2), nitrous oxide (N2O), sulfur hexafluoride (SF6), and other trace gas mole fractions (i.e. &amp;quot;concentrations&amp;quot;) from airborne campaigns over the Alaskan and Canadian Arctic for the Carbon in Arctic Reservoirs Vulnerability Experiment (CARVE). The CARVE flight campaigns took place from 2012 to 2015 between the months of March and November to enable investigation of both seasonal and inter-annual variability in atmospheric gas abundances. The data were derived from laboratory measurements of whole air samples collected by a Programmable Flask Package (PFP) onboard the CARVE aircraft. Air samples were collected at strategic intervals to coincide with the overflight of a ground site of interest, or when interesting geophysical conditions were encountered. While most of these samples were collected near the surface in the planetary boundary layer (PBL), on almost every flight samples were also collected in the free troposphere. A minimum of 12 flask samples were collected per flight. Whole air samples collected in the PFPs were analyzed on automated systems at the NOAA Earth System Research Laboratory (ESRL) Global Monitoring Division in Boulder, CO, which also analyzes samples from the NOAA/ESRL Global Greenhouse Gas Reference Network. The measurements included in this data set are crucial for understanding changes in Arctic carbon cycling and the potential threats posed by thawing of Arctic permafrost.
&lt;br&gt;&lt;h4 id&#x3D;&quot;carve_l2_flask_ground_1405&quot;&gt;CARVE_L2_Flask_Ground_1405&lt;/h4&gt;
This data set provides atmospheric carbon dioxide, methane, carbon monoxide, molecular hydrogen, nitrous oxide, sulfur hexafluoride, and other trace gas mole fractions (i.e. &amp;quot;concentrations&amp;quot;) from a flask sampling system at the CARVE flux tower in Fox, Alaska for the Carbon in Arctic Reservoirs Vulnerability Experiment (CARVE). The data were derived from laboratory measurements of whole air samples collected by a Programmable Flask Package (PFP) from the top of the tower at 32 m above ground level during late evening multiple times per month since January 2012. Whole air samples collected in the PFPs were analyzed on automated systems at the NOAA Earth System Research Laboratory (ESRL) Global Monitoring Division in Boulder, CO, which also analyzes samples from the NOAA/ESRL Global Greenhouse Gas Reference Network. The measurements included in this data set are crucial for understanding changes in Arctic carbon cycling and the potential threats posed by thawing of Arctic permafrost.
&lt;br&gt;&lt;h4 id&#x3D;&quot;carve_l2_fts_columngas_1429&quot;&gt;CARVE_L2_FTS_ColumnGas_1429&lt;/h4&gt;
This data set provides total vertical column O2, CO2, CH4, CO, and H2O, as well as dry-air columns of CO2, CH4, CO, and H2O from airborne campaigns over the Alaskan and Canadian Arctic for the Carbon in Arctic Reservoirs Vulnerability Experiment (CARVE). The data represent the Level 2 Quick Retrieval (L2QR) data product collected using the CARVE Fourier Transform Spectrometer (FTS). Flight campaigns took place from 2012 to 2015 between the months of March and November to enable investigation of both seasonal and inter-annual variability in atmospheric gas content. The measurements included in this data set are crucial for understanding changes in Arctic carbon cycling and the potential threats posed by thawing of Arctic permafrost.
&lt;br&gt;&lt;h4 id&#x3D;&quot;carve_l2_atmosgas_merge_1402&quot;&gt;CARVE_L2_AtmosGas_Merge_1402&lt;/h4&gt;
This data set provides atmospheric carbon dioxide (CO2), methane (CH4), carbon monoxide (CO), ozone (O3), and water vapor (H2O) concentrations from airborne campaigns over the Alaskan and Canadian arctic for the Carbon in Arctic Reservoirs Vulnerability Experiment (CARVE). These data are merged and gap-filled outputs from two different cavity ring-down spectrometers (CRDS; Picarro Inc.) flown aboard the CARVE aircraft and are presented at 5-second intervals throughout each flight. Aircraft latitude, longitude, and altitude are also provided. Flight campaigns took place from 2012 to 2015 between the months of March and November to enable investigation of both seasonal and inter-annual variability in atmospheric gas content. The measurements included in this data set are crucial for understanding changes in Arctic carbon cycling and the potential threats posed by thawing of Arctic permafrost.
&lt;br&gt;&lt;h4 id&#x3D;&quot;carve_l4_wrf-stilt_footprint_1431&quot;&gt;CARVE_L4_WRF-STILT_Footprint_1431&lt;/h4&gt;
This data set provides Weather Research and Forecasting (WRF) Stochastic Time-Inverted Lagrangian Transport (STILT) Footprint data products for particle receptors located at positions along Carbon in Arctic Reservoirs Vulnerability Experiment (CARVE) flight paths (2012 - 2015) and various meteorological stations in Alaska and the Canadian Arctic. Each product consists of multiple NetCDF footprint files packaged as a TAR/GZIP file. These aircraft and station positions were treated as receptors in the WRF-STILT model in order to simulate the land surface influence on observed atmospheric constituents. The measurements included in this data set are crucial for understanding changes in Arctic carbon cycling and the potential threats posed by thawing of Arctic permafrost.
&lt;br&gt;&lt;h4 id&#x3D;&quot;carve_l4_wrf-stilt_particle_1430&quot;&gt;CARVE_L4_WRF-STILT_Particle_1430&lt;/h4&gt;
This data set provides Weather Research and Forecasting (WRF) Stochastic Time-Inverted Lagrangian Transport (STILT) model inputs for particle receptors located at positions along Carbon in Arctic Reservoirs Vulnerability Experiment (CARVE) flight paths (2012 - 2015) and various meteorological stations in Alaska and the Canadian Arctic. Each product consists of multiple NetCDF files packaged as a TAR/GZIP file. These data correspond to WRF-STILT model footprint data also generated by the CARVE science team.
&lt;br&gt;&lt;h4 id&#x3D;&quot;alaskan_co2_flux_1325&quot;&gt;Alaskan_CO2_Flux_1325&lt;/h4&gt;
This data set reports monthly averages of atmospheric CO2 concentration from satellite and airborne observations between 2009 and 2013 and simulated present and future monthly concentrations and land-atmosphere CO2 flux for periods between 1990 and 2200. Atmospheric CO2 concentration measurements were obtained from Carbon in Arctic Reservoirs Vulnerability Experiment (CARVE) and NOAA Arctic Coast Guard (ACG) flights, the Greenhouse Gases Observing Satellite (GOSAT), and NOAA/ESRL vertical profile measurements at Poker Flat, Alaska (PFA). Present and future monthly CO2 concentrations and fluxes were simulated using the GEOS-Chem global tracer model and the Community Land Model, Version 4.5, for multiple regional flux and permafrost thaw scenarios.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ak_regional_co2_flux_1389&quot;&gt;AK_Regional_CO2_Flux_1389&lt;/h4&gt;
This data set provides estimates of 3-hourly net ecosystem CO2 exchange (NEE) at 0.5-degree resolution over the state of Alaska for 2012-2014. The NEE estimates are the output are from Geostatistical Inverse Modeling of a subset of CARVE aircraft CO2 data, WRF-STILT footprints, and PVPRM-SIF data from flux towers (CRV: located in Fox, AK and BRW: located just outside Barrow, AK). Daily mean NEE is also provided as calculated for all of Alaska and for four sub-regions (0.5-degree resolution) that were defined across Alaska, based on general landcover type: North Slope Tundra, South and West Tundra, Boreal Forests, and Mixed (all other). Also provided are derived annual carbon budgets for (1) all of Alaska with defined contributions from biogenic, fossil fuel, and biomass burning sources and (2) annual biogenic carbon budgets for the four landcover-type regions of Alaska. Provided for completeness are the CARVE aircraft atmospheric measurement data used in estimating NEE.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.ornldaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA CERES Project</title>
      <link>https://registry.opendata.aws/nasa-ceres</link>
      <guid>https://registry.opendata.aws/nasa-ceres</guid>
      <description>CER_BDS_Terra-FM2_Edition4 is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) Bidirectional Scans (BDS) Terra Flight Model 2 (FM2) Edition 4 data product, which is collected using the CERES-FM2 instrument on the Terra platform. CER_BDS_Terra-FM2_Edition4 includes geolocated and calibrated Top of the Atmosphere (TOA) filtered radiances and other instrument data. Data collection for this product is ongoing. Each CERES BDS data product contains twenty-four hours of Level-1B data for each CERES scanner instrument mounted on each spacecraft. BDS includes samples of normal and short Earth scan elevation profiles in fixed and rotating azimuth modes (including space, internal calibration, and solar calibration views). BDS contains Level-0 raw (unconverted) and the geolocated converted science and instrument data. BDS contains additional data not found in the Level-0 input file, including converted satellite position and velocity data, celestial data, converted digital status data, and parameters used in the radiance count conversion equations. CERES is a key Earth Observing System (EOS) program component. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument, the proto flight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit onboard the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched onboard Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched onboard the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched onboard the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_syn1deg-1hour_terra-modis&quot;&gt;CER_SYN1deg-1Hour_Terra-MODIS&lt;/h4&gt;
CER_SYN1deg-1Hour_Terra-MODIS_Edition4A is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) and geostationary (GEO)-Enhanced Top-of-Atmosphere (TOA), Within-Atmosphere and Surface Fluxes, Clouds, and Aerosols 1-Hourly Terra Edition4A data product. Data was collected using several instruments on multiple platforms, including CERES Imaging Radiometers on Geostationary Satellites, CERES Flight Model 1 (FM1), FM2, CERES Scanner, and Moderate-Resolution Imaging Spectroradiometer on Terra. Data collection for this product is complete. The CERES Synoptic (SYN) 1 degree (SYN1deg) products provide CERES-observed temporally interpolated top-of-atmosphere (TOA) radiative fluxes and coincident MODIS-derived cloud and aerosol properties and include geostationary-derived cloud properties and broadband fluxes that have been carefully normalized with CERES fluxes to maintain the CERES calibration. They also contain computed initial TOA, in-atmosphere, surface fluxes, and computed fluxes adjusted or constrained to the CERES-observed TOA fluxes. The computed fluxes are produced using the Langley Fu-Liou radiative transfer model. Computations use MODIS and geostationary satellite cloud properties along with atmospheric profiles provided by GMAO. The adjustments to clouds and atmospheric properties are also provided. The computations are for all-sky, clear-sky, pristine (clear-sky without aerosols), and all-sky without aerosol conditions. This product provides parameters on a one-hourly temporal resolution and 1°-regional spatial scales. Fluxes are provided for clear-sky and all-sky conditions in the longwave (LW), shortwave (SW), and window (WN) regions. The CERES SYN1deg products use 1-hourly radiances and cloud property data from geostationary (GEO) imagers to model variability between CERES observations accurately. Several steps are involved in using GEO data to enhance diurnal sampling. First, GEO radiances are cross-calibrated with the MODIS imager using only data that is coincident in time and ray-matched in angle. Next, the GEO cloud retrievals are inferred from the calibrated GEO radiances. The GEO radiances are converted from narrow-band to broadband using empirical regressions and then to broadband GEO TOA fluxes using Angular Distribution Models (ADMs) and directional models. A normalization technique ensures GEO and CERES TOA fluxes are consistent. Instantaneous matched gridded fluxes from CERES and GEO are regressed against one another over a month from 5°x5 ° latitude-longitude regions. The regression relation is then applied to all GEO fluxes to remove biases that depend upon cloud amount, solar and view zenith angles, and regional dependencies. The regional means are determined for 1° equal-angle grid boxes calculated by first interpolating each parameter for any missing times of the CERES/GEO observations to produce a complete 1-hourly time series for the month. Monthly means are calculated using the combination of observed and interpolated parameters from all days containing at least one CERES observation. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument, the protoflight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched on board the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched on board the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_syn1deg-1hour_terra-aqua-modis&quot;&gt;CER_SYN1deg-1Hour_Terra-Aqua-MODIS&lt;/h4&gt;
CER_SYN1deg-1Hour_Terra-Aqua-MODIS_Edition4A is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) and geostationary (GEO) Top-of-Atmosphere (TOA) Within-Atmosphere and Surface Fluxes, Clouds, and Aerosols 1-Hourly Terra-Aqua Edition4A data product. Data was collected using several instruments on multiple platforms, including CERES Imaging Radiometers on Geostationary Satellites; CERES Flight Model 1 (FM1), FM2, CERES Scanner, and Moderate-Resolution Imaging Spectroradiometer (MODIS) on Terra; and FM3, FM4, CERES Scanner, and MODIS on Aqua. Data collection for this product is ongoing. The CERES Synoptic (SYN) 1 degree (SYN1deg) products provide CERES-observed temporally interpolated top-of-atmosphere (TOA) radiative fluxes and coincident MODIS-derived cloud and aerosol properties and include geostationary-derived cloud properties and broadband fluxes that have been carefully normalized with CERES fluxes to maintain the CERES calibration. They also contain computed initial TOA, in-atmosphere, surface fluxes, and computed fluxes adjusted or constrained to the CERES-observed TOA fluxes. The computed fluxes are produced using the Langley Fu-Liou radiative transfer model. Computations use MODIS, geostationary satellite cloud properties, and atmospheric profiles provided by the Global Modeling and Assimilation Office (GMAO). The adjustments to clouds and atmospheric properties are also provided. The computations are for all-sky, clear-sky, pristine (clear-sky without aerosols), and all-sky without aerosol conditions. This product provides parameters on a one-hourly temporal resolution and 1°-regional spatial scales. Fluxes are provided for clear-sky and all-sky conditions in the longwave (LW), shortwave (SW), and window (WN) regions. The CERES SYN1deg products use 1-hourly radiances and cloud property data from geostationary (GEO) imagers to model variability between CERES observations accurately. Several steps are involved in using GEO data to enhance diurnal sampling. First, GEO radiances are cross-calibrated with the MODIS imager using only data that is coincident in time and ray-matched in angle. Next, the GEO cloud retrievals are inferred from the calibrated GEO radiances. The GEO radiances are converted from narrow-band to broadband using empirical regressions and then to broadband GEO TOA fluxes using Angular Distribution Models (ADMs) and directional models. A normalization technique ensures GEO and CERES TOA fluxes are consistent. Instantaneous matched gridded fluxes from CERES and GEO are regressed against one another over a month from 5°x5 ° latitude-longitude regions. The regression relation is then applied to all GEO fluxes to remove biases that depend upon cloud amount, solar and view zenith angles, and regional dependencies. The regional means are determined for 1° equal-angle grid boxes calculated by first interpolating each parameter for any missing times of the CERES/GEO observations to produce a complete 1-hourly time series for the month. Monthly means are calculated using the combination of observed and interpolated parameters from all days containing at least one CERES observation. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument, the protoflight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched on board the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched on board the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_syn1deg-1hour_terra-noaa20&quot;&gt;CER_SYN1deg-1Hour_Terra-NOAA20&lt;/h4&gt;
CER_SYN1deg-1Hour_Terra-NOAA20-MODIS_Edition4A is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) and geostationary (GEO) Top-of-Atmosphere (TOA) Within-Atmosphere and Surface Fluxes, Clouds, and Aerosols 1-Hourly Terra-Aqua Edition4A data product. Data was collected using several instruments on multiple platforms, including CERES Imaging Radiometers on Geostationary Satellites; CERES Flight Model 1 (FM1), FM2, CERES Scanner, and Moderate-Resolution Imaging Spectroradiometer (MODIS) on Terra; and FM6, and VIIRS on NOAA-20. Data collection for this product is ongoing. The CERES Synoptic (SYN) 1 degree (SYN1deg) products provide CERES-observed temporally interpolated top-of-atmosphere (TOA) radiative fluxes and coincident MODIS-derived cloud and aerosol properties and include geostationary-derived cloud properties and broadband fluxes that have been carefully normalized with CERES fluxes to maintain the CERES calibration. They also contain computed initial TOA, in-atmosphere, surface fluxes, and computed fluxes adjusted or constrained to the CERES-observed TOA fluxes. The computed fluxes are produced using the Langley Fu-Liou radiative transfer model. Computations use MODIS, geostationary satellite cloud properties, and atmospheric profiles provided by the Global Modeling and Assimilation Office (GMAO). The adjustments to clouds and atmospheric properties are also provided. The computations are for all-sky, clear-sky, pristine (clear-sky without aerosols), and all-sky without aerosol conditions. This product provides parameters on a one-hourly temporal resolution and 1°-regional spatial scales. Fluxes are provided for clear-sky and all-sky conditions in the longwave (LW), shortwave (SW), and window (WN) regions. The CERES SYN1deg products use 1-hourly radiances and cloud property data from geostationary (GEO) imagers to model variability between CERES observations accurately. Several steps are involved in using GEO data to enhance diurnal sampling. First, GEO radiances are cross-calibrated with the MODIS imager using only data that is coincident in time and ray-matched in angle. Next, the GEO cloud retrievals are inferred from the calibrated GEO radiances. The GEO radiances are converted from narrow-band to broadband using empirical regressions and then to broadband GEO TOA fluxes using Angular Distribution Models (ADMs) and directional models. A normalization technique ensures GEO and CERES TOA fluxes are consistent. Instantaneous matched gridded fluxes from CERES and GEO are regressed against one another over a month from 5°x5 ° latitude-longitude regions. The regression relation is then applied to all GEO fluxes to remove biases that depend upon cloud amount, solar and view zenith angles, and regional dependencies. The regional means are determined for 1° equal-angle grid boxes calculated by first interpolating each parameter for any missing times of the CERES/GEO observations to produce a complete 1-hourly time series for the month. Monthly means are calculated using the combination of observed and interpolated parameters from all days containing at least one CERES observation. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument, the protoflight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched on board the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched on board the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_syn1deg-3hour_terra-modis&quot;&gt;CER_SYN1deg-3Hour_Terra-MODIS&lt;/h4&gt;
CER_SYN1deg-3Hour_Terra-MODIS_Edition4A is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) and geostationary (GEO)-Enhanced Top of Atmosphere (TOA), Within-Atmosphere and Surface Fluxes, Clouds and Aerosols 3-Hourly Terra Edition4A data product, which was collected using Imaging Radiometers on the Geostationary Satellites platform and CERES Flight Model 1 (FM1), CERES FM2, CERES Scanner, and MODIS on Terra. Data collection for this product is complete. The CERES Synoptic (SYN) 1 degree (SYN1deg) products provide CERES-observed temporally interpolated TOA radiative fluxes and coincident MODIS-derived cloud and aerosol properties and include geostationary-derived cloud properties and broadband fluxes that have been carefully normalized with CERES fluxes to maintain the CERES calibration. They also contain computed initial TOA, in-atmosphere, surface fluxes, and computed fluxes adjusted or constrained to the CERES-observed TOA fluxes. The calculated fluxes are produced using the Langley Fu-Liou radiative transfer model. Computations use MODIS, geostationary satellite cloud properties, and atmospheric profiles provided by the NASA Global Modeling and Assimilation Office (GMAO). The adjustments to clouds and atmospheric properties are also provided. The computations are for all-sky, clear-sky, pristine (clear-sky without aerosols), and all-sky without aerosol conditions. This product provides parameters on a three-hourly temporal resolution and 1°-regional spatial scales. Fluxes are provided for clear-sky and all-sky conditions in the longwave (LW), shortwave (SW), and window (WN) regions. CERES SYN1deg products use 1-hourly radiances and cloud property data from geostationary (GEO) imagers to accurately model variability between CERES observations. Several steps are involved in using GEO data to enhance diurnal sampling. First, GEO radiances are cross-calibrated with the MODIS imager using only data that is coincident in time and ray-matched in angle. Next, the GEO cloud retrievals are inferred from the calibrated GEO radiances. The GEO radiances are converted from narrowband to broadband using empirical regressions and then to broadband GEO TOA fluxes using Angular Distribution Models (ADMs) and directional models. A normalization technique ensures GEO and CERES TOA fluxes are consistent. Instantaneous matched gridded fluxes from CERES and GEO are regressed against one another over a month from 5°x5 ° latitude-longitude regions. The regression relation is then applied to all GEO fluxes to remove biases that depend upon cloud amount, solar and view zenith angles, and regional dependencies. The regional means are determined for 1° equal-angle grid boxes calculated by first interpolating each parameter for any missing times of the CERES/GEO observations to produce a complete 1-hourly time series for the month. Monthly means are calculated using the combination of observed and interpolated parameters from all days containing at least one CERES observation. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument, the protoflight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched on board the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched on board the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_syn1deg-3hour_terra-aqua-modis&quot;&gt;CER_SYN1deg-3Hour_Terra-Aqua-MODIS&lt;/h4&gt;
CER_SYN1deg-3Hour_Terra-Aqua-MODIS_Edition4A is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) and geostationary (GEO)-Enhanced Top of Atmosphere (TOA), Within-Atmosphere, and Surface Fluxes, Clouds and Aerosols 3-Hourly Terra-Aqua Edition4A data product. The instruments and platforms used to collect this data include Imaging Radiometers on the Geostationary Satellites platform; CERES Flight Model 1 (FM1), CERES FM2, CERES Scanner, and Moderate-Resolution Imaging Spectroradiometer (MODIS) on Terra; and CERES FM3, CERES FM4, CERES Scanner, and MODIS on Aqua. Data collection for this product is in progress. CERES Synoptic (SYN) 1-degree products provide CERES-observed temporally interpolated TOA radiative fluxes and coincident MODIS-derived cloud and aerosol properties and include geostationary-derived cloud properties and broadband fluxes that have been carefully normalized with CERES fluxes to maintain the CERES calibration. They also contain computed initial TOA, in-atmosphere, surface fluxes, and computed fluxes adjusted or constrained to the CERES-observed TOA fluxes. The calculated fluxes are produced using the Langley Fu-Liou radiative transfer model. Computations use MODIS, geostationary satellite cloud properties, and atmospheric profiles provided by the NASA Global Modeling and Assimilation Office (GMAO). The adjustments to clouds and atmospheric properties are also provided. The computations are for all-sky, clear-sky, pristine (clear-sky without aerosols), and all-sky without aerosol conditions. This product provides parameters on a three-hourly temporal resolution and 1°-regional spatial scales. Fluxes are provided for clear-sky and all-sky conditions in the longwave (LW), shortwave (SW), and window (WN) regions. CERES SYN1deg products use 1-hourly radiances and cloud property data from geostationary (GEO) imagers to accurately model variability between CERES observations. Several steps are involved in using GEO data to enhance diurnal sampling. First, GEO radiances are cross-calibrated with the MODIS imager using only data that is coincident in time and ray-matched in angle. Next, the GEO cloud retrievals are inferred from the calibrated GEO radiances. The GEO radiances are converted from narrowband to broadband using empirical regressions and then to broadband GEO TOA fluxes using Angular Distribution Models (ADMs) and directional models. A normalization technique ensures GEO and CERES TOA fluxes are consistent. Instantaneous matched gridded fluxes from CERES and GEO are regressed against one another over a month from 5°x5 ° latitude-longitude regions. The regression relation is then applied to all GEO fluxes to remove biases that depend upon cloud amount, solar and view zenith angles, and regional dependencies. The regional means are determined for 1° equal-angle grid boxes calculated by first interpolating each parameter for any missing times of the CERES/GEO observations to produce a complete 1-hourly time series for the month. Monthly means are calculated using the combination of observed and interpolated parameters from all days containing at least one CERES observation. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument, the protoflight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched on board the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched on board the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_syn1deg-day_terra-modis&quot;&gt;CER_SYN1deg-Day_Terra-MODIS&lt;/h4&gt;
CER_SYN1deg-Day_Terra-MODIS_Edition4A is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) and geostationary (GEO)-Enhanced Top-of-Atmosphere (TOA) and Surface Fluxes, Clouds and Aerosols Daily Terra Edition4A data product. Data was collected using CERES Imaging Radiometers on Geostationary Satellites as well as CERES Flight Model 1 (FM1), FM2, CERES Scanner, and Moderate-Resolution Imaging Spectroradiometer on Terra. Data collection for this product is complete. Note: It is highly recommended to use this product (CER_SYN1deg-Day_Terra-MODIS_Edition4A) in conjunction with CER_SYN1deg-Day_Terra-Aqua-MODIS_Edition4A when doing science-quality research. The CERES Synoptic Radiative Fluxes and Clouds (SYN) 1degree products provide CERES-observed temporally interpolated TOA radiative fluxes and coincident MODIS-derived cloud and aerosol properties and include geostationary-derived cloud properties and broadband fluxes that have been carefully normalized with CERES fluxes to maintain the CERES calibration. They also contain computed initial TOA, in-atmosphere, surface fluxes, and computed fluxes adjusted or constrained to the CERES-observed TOA fluxes. The calculated fluxes are produced using the Langley Fu-Liou radiative transfer model. Computations use MODIS, geostationary satellite cloud properties, and atmospheric profiles provided by the Global Modeling and Assimilation Office (GMAO). The adjustments to clouds and atmospheric properties are also provided. The computations are for all-sky, clear-sky, pristine (clear-sky without aerosols), and all-sky without aerosol conditions. This product provides parameters on a daily temporal resolution and 1°-regional spatial scales. Fluxes are provided for clear-sky and all-sky conditions in the longwave (LW), shortwave (SW), and window (WN) regions. The CERES SYN1deg products use 1-hourly radiances and cloud property data from GEO imagers to model variability between CERES observations accurately. Several steps are involved in using GEO data to enhance diurnal sampling. First, GEO radiances are cross-calibrated with the MODIS imager using only data that is coincident in time and ray-matched in angle. Next, the GEO cloud retrievals are inferred from the calibrated GEO radiances. The GEO radiances are converted from narrow-band to broadband using empirical regressions and then to broadband GEO TOA fluxes using Angular Distribution Models (ADMs) and directional models. A normalization technique ensures GEO and CERES TOA fluxes are consistent. Instantaneous matched gridded fluxes from CERES and GEO are regressed against one another over a month from 5°x5 ° latitude-longitude regions. The regression relation is then applied to all GEO fluxes to remove biases that depend upon cloud amount, solar and view zenith angles, and regional dependencies. The regional means are determined for 1° equal-angle grid boxes calculated by first interpolating each parameter for any missing times of the CERES/GEO observations to produce a complete 1-hourly time series for the month. Monthly means are calculated using the combination of observed and interpolated parameters from all days containing at least one CERES observation. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument, the protoflight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched on board the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched on board the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_syn1deg-day_terra-aqua-modis&quot;&gt;CER_SYN1deg-Day_Terra-Aqua-MODIS&lt;/h4&gt;
CER_SYN1deg-Day_Terra-Aqua-MODIS_Edition4A is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) and geostationary (GEO)-Enhanced Top-of-Atmosphere (TOA), Within-Atmosphere and Surface Fluxes, Clouds and Aerosols Daily Terra-Aqua Edition4A data product. Data was collected using several instruments on multiple platforms, including CERES Imaging Radiometers on Geostationary Satellites; CERES Flight Model 1 (FM1), FM2, CERES Scanner, and Moderate-Resolution Imaging Spectroradiometer on Terra; and FM3, FM4 CERES Scanner, and Moderate-Resolution Imaging Spectroradiometer (MODIS) on Aqua. Data collection for this product is ongoing. The CERES Synoptic Radiative Fluxes and Clouds (SYN) 1degree products provide CERES-observed temporally interpolated TOA radiative fluxes and coincident MODIS-derived cloud and aerosol properties and include geostationary-derived cloud properties and broadband fluxes that have been carefully normalized with CERES fluxes to maintain the CERES calibration. They also contain computed initial TOA, in-atmosphere, surface fluxes, and computed fluxes adjusted or constrained to the CERES-observed TOA fluxes. The computed fluxes are produced using the Langley Fu-Liou radiative transfer model. Computations use MODIS, geostationary satellite cloud properties, and atmospheric profiles provided by the Global Modeling and Assimilation Office (GMAO). The adjustments to clouds and atmospheric properties are also provided. The computations are for all-sky, clear-sky, pristine (clear-sky without aerosols), and all-sky without aerosol conditions. This product provides parameters on a daily temporal resolution and 1°-regional spatial scales. Fluxes are provided for clear-sky and all-sky conditions in the longwave (LW), shortwave (SW), and window (WN) regions. The CERES SYN1deg products use 1-hourly radiances and cloud property data from GEO imagers to model variability between CERES observations accurately. Several steps are involved in using GEO data to enhance diurnal sampling. First, GEO radiances are cross-calibrated with the MODIS imager using only data that is coincident in time and ray-matched in angle. Next, the GEO cloud retrievals are inferred from the calibrated GEO radiances. The GEO radiances are converted from narrowband to broadband using empirical regressions and then to broadband GEO TOA fluxes using Angular Distribution Models (ADMs) and directional models. A normalization technique ensures GEO and CERES TOA fluxes are consistent. Instantaneous matched gridded fluxes from CERES and GEO are regressed against one another over a month from 5°x5 ° latitude-longitude regions. The regression relation is then applied to all GEO fluxes to remove biases that depend upon cloud amount, solar and view zenith angles, and regional dependencies. The regional means are determined for 1° equal-angle grid boxes calculated by first interpolating each parameter for any missing times of the CERES/GEO observations to produce a complete 1-hourly time series for the month. Monthly means are calculated using the combination of observed and interpolated parameters from all days containing at least one CERES observation. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument, the protoflight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched on board the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched on board the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_syn1deg-day_terra-noaa20&quot;&gt;CER_SYN1deg-Day_Terra-NOAA20&lt;/h4&gt;
CER_SYN1deg-Day_Terra-NOAA20_Edition4A is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) and geostationary (GEO)-Enhanced Top-of-Atmosphere (TOA), Within-Atmosphere and Surface Fluxes, Clouds and Aerosols Daily Terra-NOAA20 Edition4A data product. Data was collected using the following instruments and platforms: Imaging Radiometers on the Geostationary Satellites platform, CERES Flight Model 1 (FM1), CERES FM2, CERES Scanner, and MODIS on Terra; and CERES FM6 and VIIRS on NOAA-20. Data collection for this product is ongoing. The CERES Synoptic Radiative Fluxes and Clouds (SYN) 1degree products provide CERES-observed temporally interpolated TOA radiative fluxes and coincident imager-derived cloud and aerosol properties and include geostationary-derived cloud properties and broadband fluxes that have been carefully normalized with CERES fluxes to maintain the CERES calibration. They also contain computed initial TOA, in-atmosphere, surface fluxes, and computed fluxes adjusted or constrained to the CERES-observed TOA fluxes. The calculated fluxes are produced using the Langley Fu-Liou radiative transfer model. Computations use MODIS, geostationary satellite cloud properties, and atmospheric profiles provided by the Global Modeling and Assimilation Office (GMAO). The adjustments to clouds and atmospheric properties are also provided. The computations are for all-sky, clear-sky, pristine (clear-sky without aerosols), and all-sky without aerosol conditions. This product provides parameters on a daily temporal resolution and 1°-regional spatial scales. Fluxes are provided for clear-sky and all-sky conditions in the longwave (LW), shortwave (SW), and window (WN) regions. The CERES SYN1deg products use 1-hourly radiances and cloud property data from GEO imagers to model variability between CERES observations accurately. Several steps are involved in using GEO data to enhance diurnal sampling. First, GEO radiances are cross-calibrated with the MODIS imager using only data that is coincident in time and ray-matched in angle. Next, the GEO cloud retrievals are inferred from the calibrated GEO radiances. The GEO radiances are converted from narrowband to broadband using empirical regressions and then to broadband GEO TOA fluxes using Angular Distribution Models (ADMs) and directional models. A normalization technique ensures GEO and CERES TOA fluxes are consistent. Instantaneous matched gridded fluxes from CERES and GEO are regressed against one another over a month from 5°x5 ° latitude-longitude regions. The regression relation is then applied to all GEO fluxes to remove biases that depend upon cloud amount, solar and view zenith angles, and regional dependencies. The regional means are determined for 1° equal-angle grid boxes calculated by first interpolating each parameter for any missing times of the CERES/GEO observations to produce a complete 1-hourly time series for the month. Daily means are calculated using the combination of observed and interpolated parameters from all days containing at least one CERES observation. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument, the protoflight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched on board the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched on board the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_syn1deg-day_terra-npp&quot;&gt;CER_SYN1deg-Day_Terra-NPP&lt;/h4&gt;
CER_SYN1deg-Day_Terra-NPP_Edition1A is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) and geostationary (GEO)-Enhanced Top-of-Atmosphere (TOA) and Surface Fluxes, Clouds and Aerosols Daily Terra-Suomi National Polar-orbiting Partnership (NPP) Edition1A data product. Data was collected using several instruments on multiple platforms, including CERES Imaging Radiometers on Geostationary Satellites; CERES Flight Model 1 (FM1), FM2, CERES Scanner, and Moderate-Resolution Imaging Spectroradiometer on Terra; and FM5, CERES Scanner, and Visible-Infrared Imager-Radiometer Suite (VIIRS) on Suomi-NPP. Data collection for this product is complete. The CERES Synoptic Radiative Fluxes and Clouds (SYN) 1degree products provide CERES-observed temporally interpolated TOA radiative fluxes and coincident MODIS-derived cloud and aerosol properties and include geostationary-derived cloud properties and broadband fluxes that have been carefully normalized with CERES fluxes to maintain the CERES calibration. They also contain computed initial TOA, in-atmosphere, surface fluxes, and computed fluxes adjusted or constrained to the CERES-observed TOA fluxes. The computed fluxes are produced using the Langley Fu-Liou radiative transfer model. Computations use MODIS, geostationary satellite cloud properties, and atmospheric profiles provided by the Global Modeling and Assimilation Office (GMAO). The adjustments to clouds and atmospheric properties are also provided. The computations are for all-sky, clear-sky, pristine (clear-sky without aerosols), and all-sky without aerosol conditions. This product offers parameters on a daily temporal resolution and 1°-regional spatial scales. Fluxes are provided for clear-sky and all-sky conditions in the longwave (LW), shortwave (SW), and window (WN) regions. The CERES SYN1deg products use 1-hourly radiances and cloud property data from GEO imagers to accurately model variability between CERES observations. Several steps are involved in using GEO data to enhance diurnal sampling. First, GEO radiances are cross-calibrated with the MODIS imager using only data that is coincident in time and ray-matched in angle. Next, the GEO cloud retrievals are inferred from the calibrated GEO radiances. The GEO radiances are converted from narrow-band to broadband using empirical regressions and then to broadband GEO TOA fluxes using Angular Distribution Models (ADMs) and directional models. A normalization technique ensures GEO and CERES TOA fluxes are consistent. Instantaneous matched gridded fluxes from CERES and GEO are regressed against one another over a month from 5°x5 ° latitude-longitude regions. The regression relation is then applied to all GEO fluxes to remove biases that depend upon cloud amount, solar and view zenith angles, and regional dependencies. The regional means are determined for 1° equal-angle grid boxes calculated by first interpolating each parameter for any missing times of the CERES/GEO observations to produce a complete 1-hourly time series for the month. Monthly means are calculated using the combination of observed and interpolated parameters from all days containing at least one CERES observation. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument, the protoflight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched on board the Suomi NPP satellite on October 28, 2011. The newest CERES instrument (FM6) was launched on board the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_syn1deg-month_terra-aqua-modis&quot;&gt;CER_SYN1deg-Month_Terra-Aqua-MODIS&lt;/h4&gt;
CER_SYN1deg-Month_Terra-Aqua-MODIS_Edition4A is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) and geostationary (GEO)-Enhanced Top of Atmosphere (TOA), Within-Atmosphere, and Surface Fluxes, Clouds and Aerosols Monthly Terra-Aqua Edition4A data product. Data was collected using the following instruments and platforms: Imaging Radiometers on Geostationary Satellites platform, CERES Flight Model 1 (FM1), CERES FM2, CERES Scanner, and MODIS on Terra; and CERES FM3, FM4, and MODIS on Aqua. Data collection for this product is ongoing. CERES Synoptic (SYN) 1-degree products provide CERES-observed temporally interpolated TOA radiative fluxes and coincident MODIS-derived cloud and aerosol properties and include geostationary-derived cloud properties and broadband fluxes that have been carefully normalized with CERES fluxes to maintain the CERES calibration. They also contain computed initial TOA, in-atmosphere, surface fluxes, and computed fluxes adjusted or constrained to the CERES-observed TOA fluxes. The computed fluxes are produced using the Langley Fu-Liou radiative transfer model. Computations use MODIS, geostationary satellite cloud properties, and atmospheric profiles provided by the NASA Global Modeling and Assimilation Office (GMAO). The adjustments to clouds and atmospheric properties are also provided. The computations are for all-sky, clear-sky, pristine (clear-sky without aerosols), and all-sky without aerosol conditions. This product offers parameters on a three-hourly temporal resolution and 1°-regional spatial scales. Fluxes are provided for clear-sky and all-sky conditions in the longwave (LW), shortwave (SW), and window (WN) regions. CERES SYN1deg products use 1-hourly radiances and cloud property data from geostationary (GEO) imagers to accurately model variability between CERES observations. Several steps are involved in using GEO data to enhance diurnal sampling. First, GEO radiances are cross-calibrated with the MODIS imager using only data that is coincident in time and ray-matched in angle. Next, the GEO cloud retrievals are inferred from the calibrated GEO radiances. The GEO radiances are converted from narrowband to broadband using empirical regressions and then to broadband GEO TOA fluxes using Angular Distribution Models (ADMs) and directional models. A normalization technique ensures GEO and CERES TOA fluxes are consistent. Instantaneous matched gridded fluxes from CERES and GEO are regressed against one another over a month from 5°x5 ° latitude-longitude regions. The regression relation is then applied to all GEO fluxes to remove biases that depend upon cloud amount, solar and view zenith angles, and regional dependencies. The regional means are determined for 1° equal-angle grid boxes calculated by first interpolating each parameter for any missing times of the CERES/GEO observations to produce a complete 1-hourly time series for the month. Monthly means are calculated using the combination of observed and interpolated parameters from all days containing at least one CERES observation. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument, the protoflight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched on board the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched on board the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_syn1deg-month_terra-noaa20&quot;&gt;CER_SYN1deg-Month_Terra-NOAA20&lt;/h4&gt;
CER_SYN1deg-Month_Terra-NOAA20_Edition4A is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) and geostationary (GEO)-Enhanced Top of Atmosphere (TOA), Within-Atmosphere, and Surface Fluxes, Clouds and Aerosols Monthly Terra-NOAA20 Edition4A data product. Data was collected using the following instruments and platforms: Imaging Radiometers on the Geostationary Satellites platform, CERES Flight Model 1 (FM1), CERES FM2, CERES Scanner, and MODIS on Terra; and CERES FM6 and VIIRS on NOAA-20. Data collection for this product is ongoing. CERES Synoptic (SYN) 1-degree products provide CERES-observed temporally interpolated TOA radiative fluxes and coincident MODIS-derived cloud and aerosol properties and include geostationary-derived cloud properties and broadband fluxes that have been carefully normalized with CERES fluxes to maintain the CERES calibration. They also contain computed initial TOA, in-atmosphere, surface fluxes, and computed fluxes adjusted or constrained to the CERES-observed TOA fluxes. The computed fluxes are produced using the Langley Fu-Liou radiative transfer model. Computations use MODIS, VIIRS, and geostationary satellite cloud properties along with atmospheric profiles provided by the NASA Global Modeling and Assimilation Office (GMAO). The adjustments to clouds and atmospheric properties are also provided. The computations are for all-sky, clear-sky, pristine (clear-sky without aerosols), and all-sky without aerosol conditions. This product provides parameters on a three-hourly temporal resolution and 1°-regional spatial scales. Fluxes are provided for clear-sky and all-sky conditions in the longwave (LW), shortwave (SW), and window (WN) regions. CERES SYN1deg products use 1-hourly radiances and cloud property data from geostationary (GEO) imagers to accurately model variability between CERES observations. Several steps are involved in using GEO data to enhance diurnal sampling. First, GEO radiances are cross-calibrated with the MODIS imager using only data that is coincident in time and ray-matched in angle. Next, the GEO cloud retrievals are inferred from the calibrated GEO radiances. The GEO radiances are converted from narrowband to broadband using empirical regressions and then to broadband GEO TOA fluxes using Angular Distribution Models (ADMs) and directional models. A normalization technique ensures GEO and CERES TOA fluxes are consistent. Instantaneous matched gridded fluxes from CERES and GEO are regressed against one another over a month from 5°x5 ° latitude-longitude regions. The regression relation is then applied to all GEO fluxes to remove biases that depend upon cloud amount, solar and view zenith angles, and regional dependencies. The regional means are determined for 1° equal-angle grid boxes calculated by first interpolating each parameter for any missing times of the CERES/GEO observations to produce a complete 1-hourly time series for the month. Monthly means are calculated using the combination of observed and interpolated parameters from all days containing at least one CERES observation. CERES is a critical Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument, the protoflight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched on board the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched on board the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_syn1deg-month_terra-npp&quot;&gt;CER_SYN1deg-Month_Terra-NPP&lt;/h4&gt;
CER_SYN1deg-Month_Terra-NPP_Edition1A is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) and geostationary (GEO)-Enhanced Top-of-Atmosphere (TOA) Within-Atmosphere and Surface Fluxes, Clouds and Aerosols Monthly Terra-Suomi National Polar-orbiting Partnership (NPP) Edition1A data product. Data was collected using the CERES Imaging Radiometers on Geostationary Satellites; CERES Flight Model 1 (FM1), FM2, CERES Scanner, and Moderate-Resolution Imaging Spectroradiometer (MODIS) on Terra; and FM5, CERES Scanner, and Visible-Infrared Imager-Radiometer Suite (VIIRS) on NPP. Data collection for this product is complete. The CERES SYN1deg products provide CERES-observed temporally interpolated TOA radiative fluxes and coincident MODIS-derived cloud and aerosol properties and include geostationary-derived cloud properties and broadband fluxes that have been carefully normalized with CERES fluxes to maintain the CERES calibration. They also contain computed initial TOA, in-atmosphere, surface fluxes, and computed fluxes adjusted or constrained to the CERES-observed TOA fluxes. The computed fluxes are produced using the Langley Fu-Liou radiative transfer model. Computations use MODIS, geostationary satellite cloud properties, and atmospheric profiles provided by the Global Modeling and Assimilation Office (GMAO). The adjustments to clouds and atmospheric properties are also provided. The computations are for all-sky, clear-sky, pristine (clear-sky without aerosols), and all-sky without aerosol conditions. This product provides parameters on a monthly temporal resolution on 1°-regional, zonal, and global spatial scales. Fluxes are provided for clear-sky and all-sky conditions in the longwave (LW), shortwave (SW), and window (WN) regions. The CERES SYN1deg products use 1-hourly radiances and cloud property data from geostationary (GEO) imagers to model variability between CERES observations accurately. Several steps are involved in using GEO data to enhance diurnal sampling. First, GEO radiances are cross-calibrated with the MODIS imager using only data that is coincident in time and ray-matched in angle. Next, the GEO cloud retrievals are inferred from the calibrated GEO radiances. The GEO radiances are converted from narrowband to broadband using empirical regressions and then to broadband GEO TOA fluxes using Angular Distribution Models (ADMs) and directional models. A normalization technique ensures GEO and CERES TOA fluxes are consistent. Instantaneous matched gridded fluxes from CERES and GEO are regressed against one another over a month from 5°x5 ° latitude-longitude regions. The regression relation is then applied to all GEO fluxes to remove biases that depend upon cloud amount, solar and view zenith angles, and regional dependencies. The regional means are determined for 1° equal-angle grid boxes calculated by first interpolating each parameter for any missing times of the CERES/GEO observations to produce a complete 1-hourly time series for the month. Monthly means are calculated using the combination of observed and interpolated parameters from all days containing at least one CERES observation. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument, the protoflight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched on board the Suomi NPP satellite on October 28, 2011. The newest CERES instrument (FM6) was launched on board the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_syn1deg-mhour_terra-modis&quot;&gt;CER_SYN1deg-MHour_Terra-MODIS&lt;/h4&gt;
CER_SYN1deg-MHour_Terra-MODIS_Edition4A is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) and geostationary (GEO)-Enhanced Top-of-Atmosphere (TOA), Within-Atmosphere and Surface Fluxes, Clouds and Aerosols Monthly-Averaged 1-Hourly Terra Edition4A data product. Data was collected using the CERES Imaging Radiometers on the Geostationary Satellites platform and CERES Flight Model 1 (FM1), FM2, CERES Scanner, and Moderate-Resolution Imaging Spectroradiometer (MODIS) on the Terra platform. Data collection for this product is complete. The CERES Synoptic (SYN) 1 degree (SYN1deg) products provide CERES-observed temporally interpolated TOA radiative fluxes and coincident MODIS-derived cloud and aerosol properties and include geostationary-derived cloud properties and broadband fluxes that have been carefully normalized with CERES fluxes to maintain the CERES calibration. They also contain computed initial TOA, in-atmosphere, and surface fluxes and computed fluxes that have been adjusted or constrained to the CERES-observed TOA fluxes. The computed fluxes are produced using the Langley Fu-Liou radiative transfer model. Computations use MODIS, geostationary satellite cloud properties, and atmospheric profiles provided by the Global Modeling and Assimilation Office (GMAO). The adjustments to clouds and atmospheric properties are also provided. The computations are made for all-sky, clear-sky, pristine (clear-sky without aerosols), and all-sky without aerosol conditions. This product provides parameters on a monthly-averaged one-hourly temporal resolution and 1°-regional spatial scales. Fluxes are provided for clear-sky and all-sky conditions in the longwave (LW), shortwave (SW), and window (WN) regions. The CERES SYN1deg products use 1-hourly radiances and cloud property data from geostationary (GEO) imagers to model variability between CERES observations accurately. Several steps are involved in using GEO data to enhance diurnal sampling. First, GEO radiances are cross-calibrated with the MODIS imager using only data that is coincident in time and ray-matched in angle. Next, the GEO cloud retrievals are inferred from the calibrated GEO radiances. The GEO radiances are converted from narrowband to broadband using empirical regressions and then to broadband GEO TOA fluxes using Angular Distribution Models (ADMs) and directional models. A normalization technique is used to ensure GEO and CERES TOA fluxes are consistent. Instantaneous matched gridded fluxes from CERES and GEO are regressed against one another over a month from 5°x5 ° latitude-longitude regions. The regression relation is then applied to all GEO fluxes to remove biases that depend upon cloud amount, solar and view zenith angles, and regional dependencies. The regional means are determined for 1° equal-angle grid boxes calculated by first interpolating each parameter for any missing times of the CERES/GEO observations to produce a complete 1-hourly time series for the month. Monthly means are calculated using the combination of observed and interpolated parameters from all days containing at least one CERES observation. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument, the proto flight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit onboard the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched onboard Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched onboard the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched onboard the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_syn1deg-mhour_terra-aqua-modis&quot;&gt;CER_SYN1deg-MHour_Terra-Aqua-MODIS&lt;/h4&gt;
CER_SYN1deg-MHour_Terra-Aqua-MODIS_Edition4A is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) and geostationary (GEO)-Enhanced Top-of-Atmosphere (TOA), Within-Atmosphere and Surface Fluxes, Clouds and Aerosols Monthly-Averaged 1-Hourly Terra-Aqua Edition4A data product. Data was collected using the CERES Imaging Radiometers on Geostationary Satellites; CERES Flight Model 1 (FM1), FM2, CERES Scanner, and Moderate-Resolution Imaging Spectroradiometer (MODIS) on Terra; and FM3, FM4 CERES Scanner, and Moderate-Resolution Imaging Spectroradiometer (MODIS) on Aqua. Data collection for this product is ongoing. The CERES Synoptic (SYN) 1 degree (SYN1deg) products provide CERES-observed temporally interpolated TOA radiative fluxes and coincident MODIS-derived cloud and aerosol properties and include geostationary-derived cloud properties and broadband fluxes that have been carefully normalized with CERES fluxes to maintain the CERES calibration. They also contain computed initial TOA, in-atmosphere, surface fluxes, and computed fluxes adjusted or constrained to the CERES-observed TOA fluxes. The computed fluxes are produced using the Langley Fu-Liou radiative transfer model. Computations use MODIS, geostationary satellite cloud properties, and atmospheric profiles provided by the Global Modeling and Assimilation Office (GMAO). The adjustments to clouds and atmospheric properties are also provided. The computations are for all-sky, clear-sky, pristine (clear-sky without aerosols), and all-sky without aerosol conditions. This product offers parameters on a monthly-averaged one-hourly temporal resolution and 1°-regional spatial scales. Fluxes are provided for clear-sky and all-sky conditions in the longwave (LW), shortwave (SW), and window (WN) regions. The CERES SYN1deg products use 1-hourly radiances and cloud property data from geostationary (GEO) imagers to model variability between CERES observations accurately. Several steps are involved in using GEO data to enhance diurnal sampling. First, GEO radiances are cross-calibrated with the MODIS imager using only data that is coincident in time and ray-matched in angle. Next, the GEO cloud retrievals are inferred from the calibrated GEO radiances. The GEO radiances are converted from narrowband to broadband using empirical regressions and then to broadband GEO TOA fluxes using Angular Distribution Models (ADMs) and directional models. A normalization technique ensures GEO and CERES TOA fluxes are consistent. Instantaneous matched gridded fluxes from CERES and GEO are regressed against one another over a month from 5°x5 ° latitude-longitude regions. The regression relation is then applied to all GEO fluxes to remove biases that depend upon cloud amount, solar and view zenith angles, and regional dependencies. The regional means are determined for 1° equal-angle grid boxes calculated by first interpolating each parameter for any missing times of the CERES/GEO observations to produce a complete 1-hourly time series for the month. Monthly means are calculated using the combination of observed and interpolated parameters from all days containing at least one CERES observation. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument, the protoflight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched on board the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched on board the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_syn1deg-mhour_terra-noaa20&quot;&gt;CER_SYN1deg-MHour_Terra-NOAA20&lt;/h4&gt;
CER_SYN1deg-MHour_Terra-NOAA20_Edition4A is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) and geostationary (GEO)-Enhanced Top-of-Atmosphere (TOA), Within-Atmosphere and Surface Fluxes, Clouds and Aerosols Monthly-Averaged 1-Hourly Terra-Aqua Edition4A data product. Data was collected using the CERES Imaging Radiometers on Geostationary Satellites; CERES Flight Model 1 (FM1), FM2, CERES Scanner, and Moderate-Resolution Imaging Spectroradiometer (MODIS) on Terra; and FM6 CERES Scanner, and VIIRS on NOAA-20. Data collection for this product is ongoing. The CERES Synoptic (SYN) 1 degree (SYN1deg) products provide CERES-observed temporally interpolated TOA radiative fluxes and coincident MODIS-derived cloud and aerosol properties and include geostationary-derived cloud properties and broadband fluxes that have been carefully normalized with CERES fluxes to maintain the CERES calibration. They also contain computed initial TOA, in-atmosphere, surface fluxes, and computed fluxes adjusted or constrained to the CERES-observed TOA fluxes. The computed fluxes are produced using the Langley Fu-Liou radiative transfer model. Computations use MODIS, geostationary satellite cloud properties, and atmospheric profiles provided by the Global Modeling and Assimilation Office (GMAO). The adjustments to clouds and atmospheric properties are also provided. The computations are for all-sky, clear-sky, pristine (clear-sky without aerosols), and all-sky without aerosol conditions. This product provides parameters on a monthly-averaged one-hourly temporal resolution and 1°-regional spatial scales. Fluxes are provided for clear-sky and all-sky conditions in the longwave (LW), shortwave (SW), and window (WN) regions. The CERES SYN1deg products use 1-hourly radiances and cloud property data from geostationary (GEO) imagers to model variability between CERES observations accurately. Several steps are involved in using GEO data to enhance diurnal sampling. First, GEO radiances are cross-calibrated with the MODIS imager using only data that is coincident in time and ray-matched in angle. Next, the GEO cloud retrievals are inferred from the calibrated GEO radiances. The GEO radiances are converted from narrowband to broadband using empirical regressions and then to broadband GEO TOA fluxes using Angular Distribution Models (ADMs) and directional models. A normalization technique ensures GEO and CERES TOA fluxes are consistent. Instantaneous matched gridded fluxes from CERES and GEO are regressed against one another over a month from 5°x5 ° latitude-longitude regions. The regression relation is then applied to all GEO fluxes to remove biases that depend upon cloud amount, solar and view zenith angles, and regional dependencies. The regional means are determined for 1° equal-angle grid boxes calculated by first interpolating each parameter for any missing times of the CERES/GEO observations to produce a complete 1-hourly time series for the month. Monthly means are calculated using the combination of observed and interpolated parameters from all days containing at least one CERES observation. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument, the protoflight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched on board the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched on board the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_syn1deg-month_terra-modis&quot;&gt;CER_SYN1deg-Month_Terra-MODIS&lt;/h4&gt;
CER_SYN1deg-Month_Terra-MODIS_Edition4A is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) and and geostationary (GEO)-Enhanced Top of Atmosphere (TOA), Within-Atmosphere and Surface Fluxes Clouds and Aerosols Monthly Terra Edition4A data product, which was collected using Imaging Radiometers on Geostationary Satellites platform as well as CERES Flight Model 1 (FM1), CERES FM2, and MODIS on Terra. Data collection for this product is complete. CERES Synoptic (SYN) 1-degree products provide CERES-observed temporally interpolated TOA radiative fluxes and coincident MODIS-derived cloud and aerosol properties and include geostationary-derived cloud properties and broadband fluxes that have been carefully normalized with CERES fluxes to maintain the CERES calibration. They also contain computed initial TOA, in-atmosphere, surface fluxes, and computed fluxes adjusted or constrained to the CERES-observed TOA fluxes. The computed fluxes are produced using the Langley Fu-Liou radiative transfer model. Computations use MODIS, geostationary satellite cloud properties, and atmospheric profiles provided by the NASA Global Modeling and Assimilation Office (GMAO). The adjustments to clouds and atmospheric properties are also provided. The computations are for all-sky, clear-sky, pristine (clear-sky without aerosols), and all-sky without aerosol conditions. This product offers parameters on a three-hourly temporal resolution and 1°-regional spatial scales. Fluxes are provided for clear-sky and all-sky conditions in the longwave (LW), shortwave (SW), and window (WN) regions. CERES SYN1deg products use 1-hourly radiances and cloud property data from geostationary (GEO) imagers to accurately model variability between CERES observations. Several steps are involved in using GEO data to enhance diurnal sampling. First, GEO radiances are cross-calibrated with the MODIS imager using only data that is coincident in time and ray-matched in angle. Next, the GEO cloud retrievals are inferred from the calibrated GEO radiances. The GEO radiances are converted from narrowband to broadband using empirical regressions and then to broadband GEO TOA fluxes using Angular Distribution Models (ADMs) and directional models. A normalization technique ensures GEO and CERES TOA fluxes are consistent. Instantaneous matched gridded fluxes from CERES and GEO are regressed against one another over a month from 5°x5 ° latitude-longitude regions. The regression relation is then applied to all GEO fluxes to remove biases that depend upon cloud amount, solar and view zenith angles, and regional dependencies. The regional means are determined for 1° equal-angle grid boxes calculated by first interpolating each parameter for any missing times of the CERES/GEO observations to produce a complete 1-hourly time series for the month. Monthly means are calculated using the combination of observed and interpolated parameters from all days containing at least one CERES observation. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument, the protoflight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched on board the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched on board the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_crs_terra-fm2-modis&quot;&gt;CER_CRS_Terra-FM2-MODIS&lt;/h4&gt;
CER_CRS_Terra-FM2-MODIS_Edition4A is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) Clouds and Radiative Swath (CRS) Terra Flight Model 2 (FM2) Moderate-Resolution Imaging Spectroradiometer (MODIS) Edition4A data product, which was collected using the CERES-FM2 instrument on the Terra platform. Please note that only a few variables from the SSF have been included and this product should be used in conjunction with the CER_SSF_Terra-FM2-MODIS_Edition4A product. The Clouds and Radiative Swath (CRS) product contains one hour of instantaneous CERES data for a single scanner instrument. The CRS contains geolocation, geometry, packet identification, and minimal cloud properties, and TOA fluxes from the CERES SSF product. For each CERES footprint on the Single Scanner Footprint (SSF), the CRS product also contains vertical flux profiles evaluated at six levels in the atmosphere: the surface, 850-, 500-, 200-, 70-, and 0.01-hPa for both clear-sky and total-sky. CERES is a key component of the Earth Observing System (EOS) program. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions are a follow-on to the successful Earth Radiation Budget Experiment (ERBE) mission. Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the Earth Observing System (EOS) flagship Terra on December 18, 1999.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_fluxbycldtyp-day_noaa20-viirs&quot;&gt;CER_FluxByCldTyp-Day_NOAA20-VIIRS&lt;/h4&gt;
CER_FluxByCldTyp-Day_NOAA20-VIIRS_Edition1B is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) Monthly Daytime Mean Regionally Averaged NOAA-20 Top-of-Atmosphere (TOA) Fluxes and Associated Cloud Properties Stratified by Optical Depth and Effective Pressure Edition 1B data product. Data was collected using CERES Flight Model 6 (FM6) and Visible Infrared Imaging Radiometer Suite (VIIRS) on NOAA-20. Data collection for this product is ongoing. CER_FluxByCldTyp-Day_NOAA20-VIIRS_Edition1B provides the monthly mean daytime CERES fluxes and CERES-VIIRS cloud properties that have been spatially gridded into 1° regions along both the NOAA-20 ground tracks where the TOA fluxes and cloud properties have been stratified by six cloud optical depth bins and seven cloud effective pressure layers. The CERES FluxByCldTyp-Day Edition1B product inputs Single Scanner Footprint (SSF) Edition1B footprint data. Within each footprint, all 1-km pixel-level VIIRS-retrieved cloud properties are stratified into three possible sub-footprint components: two cloud layers and a clear portion. The VIIRS channel radiances are converted to broadband (BB) radiances for each sub-footprint component. The CERES angular directional models are then applied to obtain BB fluxes. Each CERES sub-footprint cloud layer and associated fluxes are assigned to one of the 42 cloud types, similar to the stratification process in the CldTypHist product. FluxByCloudTyp is an hourly instantaneous gridded daytime-only product with a global extent. Each netCDF4 file covers a month. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument, the proto flight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit onboard the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched onboard Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched onboard the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched onboard the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_fluxbycldtyp-day_noaa20-viirs-1&quot;&gt;CER_FluxByCldTyp-Day_NOAA20-VIIRS&lt;/h4&gt;
CER_FluxByCldTyp-Day_NOAA20-VIIRS_Edition1C is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) Monthly Daytime Mean Regionally Averaged NOAA-20 Top-of-Atmosphere (TOA) Fluxes and Associated Cloud Properties Stratified by Optical Depth and Effective Pressure Edition 1C data product. Data was collected using CERES Flight Model 6 (FM6) and Visible Infrared Imaging Radiometer Suite (VIIRS) on NOAA-20 Data collection for this product is ongoing. CER_FluxByCldTyp-Day_NOAA20-VIIRS_Edition1C provides the monthly mean daytime CERES fluxes and CERES-VIIRS cloud properties that have been spatially gridded into 1° regions along both the NOAA-20 ground tracks where the TOA fluxes and cloud properties have been stratified by six cloud optical depth bins and seven cloud effective pressure layers. The CERES FluxByCldTyp-Day Edition1C product uses Single Scanner Footprint (SSF) Edition1C footprint data as input. Within each footprint, all 1-km pixel-level VIIRS-retrieved cloud properties are stratified into three possible sub-footprint components: two cloud layers and a clear portion. For each sub-footprint component, the VIIRS channel radiances are converted to broadband (BB) radiances. The CERES angular directional models are then applied to obtain BB fluxes. Each of the CERES sub-footprint cloud layers and associated fluxes are assigned to one of the 42 cloud types, similarly to the stratification process in the CldTypHist product. FluxByCloudTyp is an hourly instantaneous gridded daytime-only product with a global extent. Each netCDF4 file covers a month. CERES is a key component of the Earth Observing System (EOS) program. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions are a follow-on to the successful Earth Radiation Budget Experiment (ERBE) mission. The newest CERES instrument (FM6) was launched onboard the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ceres_ebaf&quot;&gt;CERES_EBAF&lt;/h4&gt;
CERES_EBAF_Edition4.1 is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) Energy Balanced and Filled (EBAF) Top-of-Atmosphere (TOA) and surface monthly means data in netCDF format Edition 4.1 data product. Data was collected using the CERES Scanner instruments on both the Terra and Aqua platforms. Data collection for this product is ongoing. CERES_EBAF_Edition4.1 data are monthly and climatological averages of TOA clear-sky (spatially complete) fluxes and all-sky fluxes, where the TOA net flux is constrained to the ocean heat storage. It also provides computed monthly mean surface radiative fluxes consistent with the CERES EBAF-TOA product and some basic cloud properties derived from MODIS. Cloud Radiative Effects are provided at both the TOA and surface as determined using a cloud-free profile in the Fu-Liou Radiative Transfer Model (RTM). Observed fluxes are obtained using cloud properties derived from narrow-band imagers onboard both EOS Terra and Aqua satellites, as well as geostationary satellites, to fully model the diurnal cycle of clouds. The computations are also based on meteorological assimilation data from the Goddard Earth Observing System (GEOS) Versions 5.4.1 models. Unlike other CERES Level 3 clear-sky regional data sets that contain clear-sky data gaps, the clear-sky fluxes in the EBAF-TOA product are regionally complete. The EBAF-TOA product is the CERES project&amp;#39;s best estimate of the fluxes based on all available satellite platforms and input data. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument, the proto flight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched on board the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched on board the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ceres_ebaf-1&quot;&gt;CERES_EBAF&lt;/h4&gt;
CERES_EBAF_Edition4.2 is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) Energy Balanced and Filled (EBAF) Top-of-Atmosphere (TOA) and surface monthly means data in netCDF format Edition 4.2 data product. Data was collected using the CERES Scanner instruments on the Terra, Aqua, and NOAA-20 platforms for various periods. Data collection for this product is ongoing. CERES_EBAF_Edition4.2 data are monthly and climatological averages of TOA clear-sky (spatially complete) fluxes and all-sky fluxes, where the TOA net flux is constrained to the ocean heat storage. It also provides computed monthly mean surface radiative fluxes consistent with the CERES EBAF-TOA product and some basic cloud properties derived from colocated imagers. Cloud Radiative Effects are provided at both the TOA and surface as determined using a cloud-free profile in the Fu-Liou Radiative Transfer Model (RTM). Observed fluxes are obtained using cloud properties derived from narrow-band imagers onboard both EOS Terra and Aqua satellites and NOAA-20, as well as geostationary satellites, to fully model the diurnal cycle of clouds. The computations are also based on meteorological assimilation data from the Goddard Earth Observing System (GEOS) Versions 5.4.1 models. Unlike other CERES Level 3 clear-sky regional data sets that contain clear-sky data gaps, the clear-sky fluxes in the EBAF-TOA product are regionally complete. The EBAF-TOA product is the CERES project&amp;#39;s best estimate of the fluxes based on all available satellite platforms and input data. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument, the protoflight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched on board the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched on board the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ceres_ebaf-2&quot;&gt;CERES_EBAF&lt;/h4&gt;
CERES_EBAF_Edition4.2.1 is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) Energy Balanced and Filled (EBAF) Top-of-Atmosphere (TOA) and surface monthly means data in netCDF format Edition 4.2.1 data product. Data was collected using the CERES Scanner instruments on the Terra, Aqua, and NOAA-20 platforms for various periods. Data collection for this product is ongoing. CERES_EBAF_Edition4.2.1 data are monthly and climatological averages of TOA clear-sky (spatially complete) fluxes and all-sky fluxes, where the TOA net flux is constrained to the ocean heat storage. It also provides computed monthly mean surface radiative fluxes consistent with the CERES EBAF-TOA product and some basic cloud properties derived from colocated imagers. Cloud Radiative Effects are supplied at the TOA and surface, as determined using a cloud-free profile in the Fu-Liou Radiative Transfer Model (RTM). Observed fluxes are obtained using cloud properties derived from narrow-band imagers onboard both EOS Terra and Aqua satellites and NOAA-20, as well as geostationary satellites, to model the diurnal cycle of clouds. The computations are also based on meteorological assimilation data from the Goddard Earth Observing System (GEOS) Versions 5.4.1 models. Unlike other CERES Level 3 clear-sky regional data sets that contain clear-sky data gaps, the clear-sky fluxes in the EBAF-TOA product are regionally complete. The EBAF-TOA product is the CERES project&amp;#39;s best estimate of the fluxes based on all available satellite platforms and input data. CERES is a key component of the Earth Observing System (EOS) program. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument, the protoflight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board the Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched on board the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched on board the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ceres_ebaf-toa&quot;&gt;CERES_EBAF-TOA&lt;/h4&gt;
CERES_EBAF-TOA_Edition4.1 is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) Energy Balanced and Filled (EBAF) Top-of-Atmosphere (TOA) Monthly means data in netCDF format Edition 4.1 data product. Data was collected using the CERES Scanner instruments on both the Terra and Aqua platforms. Data collection for this product is ongoing. CERES_EBAF-TOA_Edition4.1 data are monthly and climatological averages of TOA clear-sky (spatially complete) fluxes and all-sky fluxes, where the TOA net flux is constrained to the ocean heat storage. EBAF-TOA provides some basic cloud properties derived from Moderate-Resolution Imaging Spectroradiometer (MODIS) alongside TOA fluxes. Observed fluxes are obtained using cloud properties derived from narrow-band imagers onboard both Earth Observing System (EOS) Terra and Aqua satellites as well as geostationary satellites to more fully model the diurnal cycle of clouds. The computations are also based on meteorological assimilation data from the Goddard Earth Observing System (GEOS) Versions 5.4.1 models. Unlike other CERES Level 3 clear-sky regional data sets that contain clear-sky data gaps, the clear-sky fluxes in the EBAF-TOA product are regionally complete. The EBAF-TOA product is the CERES project&amp;#39;s best estimate of the fluxes based on all available satellite platforms and input data. CERES is a key component of the Earth Observing System (EOS) program. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions are a follow-on to the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument, the proto flight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit onboard the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched onboard Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched onboard the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched onboard the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ceres_ebaf-toa-1&quot;&gt;CERES_EBAF-TOA&lt;/h4&gt;
CERES_EBAF-TOA_Edition4.2 is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) Energy Balanced and Filled (EBAF) Top-of-Atmosphere (TOA) Monthly means data in netCDF format Edition 4.2 data product. Data was collected using the CERES Scanner instruments on the Terra, Aqua, and NOAA-20 platforms. Data collection for this product is ongoing. CERES_EBAF-TOA_Edition4.2 data are monthly and climatological averages of TOA clear-sky (spatially complete) fluxes and all-sky fluxes, where the TOA net flux is constrained to the ocean heat storage. EBAF-TOA provides some basic cloud properties derived from high-resolution imager data alongside TOA fluxes. The Moderate-Resolution Imaging Spectroradiometer (MODIS) imagers Terra and Aqua and the Visible Infrared Imaging Radiometer Suite (VIIRS) are used for NOAA-20. Observed fluxes are obtained using cloud properties derived from narrow-band imagers onboard Earth Observing System (EOS) Terra and Aqua and NOAA-20 satellites and geostationary satellites to fully model the diurnal cycle of clouds. The computations are also based on meteorological assimilation data from the Goddard Earth Observing System (GEOS) Versions 5.4.1 models. Unlike other CERES Level 3 clear-sky regional data sets that contain clear-sky data gaps, the clear-sky fluxes in the EBAF-TOA product are regionally complete. The EBAF-TOA product is the CERES project&amp;#39;s best estimate of the fluxes based on all available satellite platforms and input data. Only Terra data is used from March 2000 to June 2002; Terra and Aqua are combined from July 2002 until March 2022; and only NOAA-20 is used after March 2022. A correction created from an overlap period with time periods when both Terra and Aqua are available is used to adjust the single satellite periods. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument, the proto flight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit onboard the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched onboard Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched onboard the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched onboard the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ceres_ebaf-toa-2&quot;&gt;CERES_EBAF-TOA&lt;/h4&gt;
CERES_EBAF-TOA_Edition4.2.1 is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) Energy Balanced and Filled (EBAF) Top-of-Atmosphere (TOA) Monthly means data in netCDF format Edition 4.2.1 data product. Data was collected using the CERES Scanner instruments on the Terra, Aqua, and NOAA-20 platforms. Data collection for this product is ongoing. CERES_EBAF-TOA_Edition4.2.1 data are monthly and climatological averages of TOA clear-sky (spatially complete) fluxes and all-sky fluxes, where the TOA net flux is constrained to the ocean heat storage. EBAF-TOA provides some basic cloud properties derived from high-resolution imager data alongside TOA fluxes. The Moderate-Resolution Imaging Spectroradiometer (MODIS) imagers Terra and Aqua and the Visible Infrared Imaging Radiometer Suite (VIIRS) are used for NOAA-20. Observed fluxes are obtained using cloud properties derived from narrow-band imagers onboard Earth Observing System (EOS) Terra and Aqua and NOAA-20 satellites and geostationary satellites to fully model the diurnal cycle of clouds. The computations are also based on meteorological assimilation data from the Goddard Earth Observing System (GEOS) Versions 5.4.1 models until March 2022 and the Modern-Era Retrospective analysis for Research and Applications, Version 2 (MERRA-2). Unlike other CERES Level 3 clear-sky regional data sets that contain clear-sky data gaps, the clear-sky fluxes in the EBAF-TOA product are regionally complete. The EBAF-TOA product is the CERES project&amp;#39;s best estimate of the fluxes based on all available satellite platforms and input data. Only Terra data is used from March 2000 to June 2002; Terra and Aqua are combined from July 2002 until March 2022; and only NOAA-20 is used after March 2022. A correction created from an overlap period with time periods when both Terra and Aqua are available is used to adjust the single satellite periods. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. Two CERES instruments (FM1 and FM2) were launched into polar orbit onboard the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched onboard Earth Observing System (EOS) Aqua on May 4, 2002. The newest CERES instrument (FM6) was launched onboard the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_es9_npp-fm5&quot;&gt;CER_ES9_NPP-FM5&lt;/h4&gt;
The ERBE-like Monthly Regional Averages (ES-9) product contains a month of space and time-averaged Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) data for a single satellite using measurements from the primary cross-track instrument. All instantaneous shortwave and longwave fluxes at the Top-of-the-Atmosphere (TOA) from the CERES ES-8 product for a month are sorted by 2.5-degree spatial regions, by day number, and by the local hour of observation. The mean of the instantaneous fluxes for a given region-day-hour bin is determined and recorded on the ES-9, along with other flux statistics and scene information. For each region, the daily average flux is estimated from an algorithm that uses the available hourly data, scene identification data, and diurnal models. This algorithm is &amp;quot;like&amp;quot; the algorithm used for the Earth Radiation Budget Experiment (ERBE). The ES-9 also contains hourly average fluxes for the month and an overall monthly average for each region. These average fluxes are given for both clear-sky and total-sky scenes. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument (PFM) was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the EOS flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board EOS Aqua on May 4, 2002. The CERES instrument (FM5) was launched on board the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The last CERES instrument (FM6) was launched on board the Joint Polar Satellite System 1 (JPSS-1) satellite on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_es9_aqua-xtrk&quot;&gt;CER_ES9_Aqua-Xtrk&lt;/h4&gt;
CER_ES9_Aqua-Xtrk_Edition4 is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) Earth Radiation Budget Experiment (ERBE)-like Gridded Instantaneous Top-of-the-Atmosphere (TOA) Fluxes Aqua Cross-track Edition 4 data product, which was collected using the CERES-Flight Model (FM3) and FM4 instruments on the Aqua platform. Data collection for this product is ongoing. The ERBE-like Monthly Regional Averages (ES-9) products contain a month of space and time-averaged CERES data for a single satellite using measurements from the primary cross-track instrument. All instantaneous shortwave and longwave fluxes at the TOA from the CERES ES-8 product for a month are sorted by 2.5-degree spatial regions, by day number, and by the local hour of observation. The mean of the instantaneous fluxes for a given region-day-hour bin is determined and recorded on the ES-9, along with other flux statistics and scene information. For each region, the daily average flux is estimated from an algorithm that uses the available hourly data, scene identification data, and diurnal models. This algorithm is &amp;quot;like&amp;quot; the algorithm used for ERBE. ES-9 also contains hourly average fluxes for the month and an overall monthly average for each region. These average fluxes are given for both clear-sky and total-sky scenes. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions are a follow-on to the successful ERBE mission. The first CERES instrument, the protoflight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched on board the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched on board the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_es9_terra-xtrk&quot;&gt;CER_ES9_Terra-Xtrk&lt;/h4&gt;
CER_ES9_Terra-Xtrk_Edition4 is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) Earth Radiation Budget Experiment (ERBE)-like Gridded Instantaneous Top-of-the-Atmosphere (TOA) Fluxes Terra Cross-track Edition 4 data product, which was collected using the CERES Flight Model 1 (FM1) and FM2 instruments on the Terra platform. Data collection for this product is ongoing. The ERBE-like Monthly Regional Averages (ES-9) products contain a month of space and time-averaged CERES data for a single satellite using measurements from the primary cross-track instrument. All instantaneous shortwave and longwave fluxes at the TOA from the CERES ES-8 product for a month are sorted by 2.5-degree spatial regions, by day number, and by the local hour of observation. The mean of the instantaneous fluxes for a given region-day-hour bin is determined and recorded on the ES-9, along with other flux statistics and scene information. For each region, the daily average flux is estimated from an algorithm that uses the available hourly data, scene identification data, and diurnal models. This algorithm is &amp;quot;like&amp;quot; the algorithm used for ERBE. ES-9 also contains hourly average fluxes for the month and an overall monthly average for each region. These average fluxes are given for both clear-sky and total-sky scenes. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions are a follow-on to the successful ERBE mission. The first CERES instrument, the protoflight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched on board the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched on board the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_es4_trmm-pfm&quot;&gt;CER_ES4_TRMM-PFM&lt;/h4&gt;
CER_ES4_TRMM-PFM_Edition2 is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) Earth Radiation Budget Experiment (ERBE)-like Monthly Geographical Averages Tropical Rainfall Measuring Mission (TRMM) proto flight model (PFM) Edition 2 data product. Data for this product was collected by the CERES PFM instrument on the TRMM platform. Data collection for this product is complete. CER_ES4_TRMM-PFM_Edition2 data are CERES instrument Top-of-the-Atmosphere (TOA) fluxes that used algorithms identical to those used by ERBE, averaged regionally, zonally, and globally. The ERBE-like Monthly Geographical Averages (ES-4) product contains a month of space and time-averaged CERES data for a single scanner instrument. The ES-4 is also produced for combinations of scanner instruments. For each observed 2.5-degree spatial region, the daily average, the hourly average over the month, and the overall monthly average of shortwave and long-wave (LW) fluxes at the Top-of-the-Atmosphere (TOA) from the CERES ES-9 product are spatially nested up from 2.5-degree regions to 5- and 10-degree regions, to 2.5-, 5-, and 10-degree zonal averages, and to global monthly averages. For each nested area, the albedo and net flux are given. For each region, the daily average flux is estimated from an algorithm that uses the available hourly data, scene identification data, and diurnal models. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions are a follow-on to the successful ERBE mission. The first CERES instrument, PFM, was launched on November 27, 1997, as part of the TRMM. Two CERES instruments (FM1 and FM2) were launched into polar orbit onboard the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched onboard Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched onboard the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched onboard the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_es9_trmm-pfm&quot;&gt;CER_ES9_TRMM-PFM&lt;/h4&gt;
CER_ES9_TRMM-PFM_Edition2 is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) Earth Radiation Budget Experiment (ERBE)-like Monthly Regional Averages Tropical Rainfall Measuring Mission (TRMM) proto flight model (PFM) Edition 2 data product. Data for this product was collected by the CERES-PFM on the Tropical Rainfall Measuring Mission (TRMM) platform. Data collection for this product is complete. CER_ES9_TRMM-PFM_Edition2 data are CERES instrument Top-of-the-Atmosphere (TOA) fluxes that used algorithms identical to those used by ERBE, regional averages of instantaneous footprint TOA fluxes only for the hours of satellite overpass (from ES-8 Level 2 product). The ERBE-like Monthly Regional Averages (ES-9) product contains a month of space and time-averaged CERES data for a single scanner instrument. The ES-9 is also produced for combinations of scanner instruments. All instantaneous short-wave and long-wave (LW) fluxes at the TOA from the CERES ES-8 product for a month are sorted by 2.5-degree spatial regions, by day number, and by the local hour of observation. The mean of the instantaneous fluxes for a given region-day-hour bin is determined and recorded on the ES-9, along with other flux statistics and scene information. For each region, the daily average flux is estimated from an algorithm that uses the available hourly data, scene identification data, and diurnal models. This algorithm is like the algorithm used for the ERBE. The ES-9 also contains hourly average fluxes for the month and an overall monthly average for each region. These average fluxes are given for both clear-sky and total-sky scenes. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions are a follow-on to the successful ERBE mission. The first CERES instrument, PFM, was launched on November 27, 1997, as part of the TRMM. Two CERES instruments (FM1 and FM2) were launched into polar orbit onboard the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched onboard Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched onboard the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched onboard the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_es4_npp-fm5&quot;&gt;CER_ES4_NPP-FM5&lt;/h4&gt;
The ERBE-like Monthly Geographical Averages (ES-4) product contains a month of space and time-averaged Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) data for a single satellite using measurements from the primary cross-track instrument. For each observed 2.5-degree spatial region, the daily average, the hourly average over the month, and the overall monthly average of shortwave and longwave fluxes at the Top-of-the-Atmosphere (TOA) from the CERES ES-9 product are spatially nested up from 2.5-degree regions to 5- and 10-degree regions, to 2.5-, 5-, and 10-degree zonal averages, and to global monthly averages. For each nested area, the albedo and net flux are given. For each region, the daily average flux is estimated from an algorithm that uses the available hourly data, scene identification data, and diurnal models. This algorithm is &amp;quot;like&amp;quot; the algorithm used for the Earth Radiation Budget Experiment (ERBE). CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument (PFM) was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the EOS flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board EOS Aqua on May 4, 2002. The CERES instrument (FM5) was launched on board the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The last CERES instrument (FM6) was launched on board the Joint Polar Satellite System 1 (JPSS-1) satellite on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_es4_aqua-xtrk&quot;&gt;CER_ES4_Aqua-Xtrk&lt;/h4&gt;
CER_ES4_Aqua-Xtrk_Edition4 is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) Earth Radiation Budget Experiment (ERBE)-like Time-Interpolated Top-of-the-Atmosphere (TOA) Fluxes Aqua Crosstrack Edition4 data product, which was collected using the CERES-FM3 and CERES-FM4 instruments on the Aqua platform. Data collection for this product is complete. The ERBE-like Monthly Geographical Averages (ES-4) product contains a month of space and time averaged CERES data for a single satellite using measurements from the primary crosstrack instrument. For each observed 2.5-degree spatial region, the daily average, the hourly average over the month, and the overall monthly average of shortwave and longwave fluxes at the TOA from the CERES ES-9 product are spatially nested up from 2.5-degree regions to 5- and 10-degree regions, to 2.5-, 5-, and 10-degree zonal averages, and to global monthly averages. For each nested area, the albedo and net flux are given. For each region, the daily average flux is estimated from an algorithm that uses the available hourly data, scene identification data, and diurnal models. This algorithm is &amp;quot;like&amp;quot; the algorithm used for ERBE. CERES is a key component of the Earth Observing System (EOS) program. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions are a follow-on to the successful ERBE mission. The first CERES instrument, protoflight model (PFM), was launched on November 27, 1997 as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched on board the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched on board the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_es4_terra-xtrk&quot;&gt;CER_ES4_Terra-Xtrk&lt;/h4&gt;
CER_ES4_Terra-Xtrk_Edition4 is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) Earth Radiation Budget Experiment (ERBE)-like Time-Interpolated Top-of-the-Atmosphere (TOA) Fluxes Terra Cross-track Edition 4 data product, which was collected using the CERES-Flight Model (FM1) and FM2 instruments on the Terra platform. Data collection for this product is complete. The ERBE-like Monthly Geographical Averages (ES-4) product contains a month of space and time-averaged CERES data for a single satellite using measurements from the primary cross-track instrument. For each observed 2.5-degree spatial region, the daily average, the hourly average over the month, and the overall monthly average of shortwave and longwave fluxes at the TOA from the CERES ES-9 product are spatially nested up from 2.5-degree regions to 5- and 10-degree regions, to 2.5-, 5-, and 10-degree zonal averages, and to global monthly averages. For each nested area, the albedo and net flux are given. For each region, the daily average flux is estimated from an algorithm that uses the available hourly data, scene identification data, and diurnal models. This algorithm is &amp;quot;like&amp;quot; the algorithm used for ERBE. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions are a follow-on to the successful ERBE mission. The first CERES instrument, the protoflight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched on board the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched on board the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_fluxbycldtyp-month_noaa20-viirs&quot;&gt;CER_FluxByCldTyp-Month_NOAA20-VIIRS&lt;/h4&gt;
CER_FluxByCldTyp-Month_NOAA20-VIIRS_Edition1C is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) Monthly Daytime Mean Regionally Averaged NOAA-20 Top-of-Atmosphere (TOA) Fluxes and Associated Cloud Properties Stratified by Optical Depth and Effective Pressure Edition 1C data product. Data was collected using CERES Flight Model 6 (FM6) and Visible Infrared Imaging Radiometer Suite (VIIRS) on NOAA-20 Data collection for this product is ongoing. CER_FluxByCldTyp-Month_NOAA20-VIIRS_Edition1C provides the monthly mean daytime CERES fluxes and CERES-VIIRS cloud properties that have been spatially gridded into 1° regions along the NOAA-20 ground track where the TOA fluxes and cloud properties have been stratified by six cloud optical depth bins and seven cloud effective pressure layers. The CERES FluxByCldTyp-Month Edition1C product uses Single Scanner Footprint (SSF) Edition1C footprint data as input. Within each footprint, all 1-km pixel-level VIIRS-retrieved cloud properties are stratified into three possible sub-footprint components: two cloud layers and a clear portion. For each sub-footprint component, the VIIRS channel radiances are converted to broadband (BB) radiances. The CERES angular directional models are then applied to obtain BB fluxes. Each of the CERES sub-footprint cloud layers and associated fluxes are assigned to one of the 42 cloud types, similarly to the stratification process in the CldTypHist product. FluxByCloudTyp is a monthly instantaneous gridded and averaged daytime-only product with a global extent. Each netCDF4 file covers a single day. CERES is a key component of the Earth Observing System (EOS) program. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions are a follow-on to the successful Earth Radiation Budget Experiment (ERBE) mission. The newest CERES instrument (FM6) was launched onboard the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_fluxbycldtyp-month_terra-aqua-modis&quot;&gt;CER_FluxByCldTyp-Month_Terra-Aqua-MODIS&lt;/h4&gt;
CER_FluxByCldTyp-Month_Terra-Aqua-MODIS_Edition4A is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) Monthly Daytime Mean Regionally Averaged Terra and Aqua Top-of-Atmosphere (TOA) Fluxes and Associated Cloud Properties Stratified by Optical Depth and Effective Pressure Edition 4A data product. Data was collected using CERES Flight Model 1 (FM1), FM2, and Moderate-Resolution Imaging Spectroradiometer (MODIS) on Terra and FM3, FM4, and MODIS on Aqua. Data collection for this product is ongoing. CER_FluxByCldTyp-Month_Terra-Aqua-MODIS_Edition4A provides the monthly mean daytime CERES fluxes and CERES-Moderate-Resolution Imaging Spectroradiometer (MODIS) cloud properties that have been spatially gridded into 1° regions along both the Terra and Aqua ground tracks where the TOA fluxes and cloud properties have been stratified by six cloud optical depth bins and seven cloud effective pressure layers. The CERES FluxByCldTyp-Month Edition4A product inputs Single Scanner Footprint (SSF) Edition4A footprint data. All 1-km pixel-level MODIS-retrieved cloud properties within each footprint are stratified into three possible sub-footprint components: two cloud layers and a clear portion. The MODIS channel radiances are converted to broadband (BB) radiances for each sub-footprint component. The CERES angular directional models are then applied to obtain BB fluxes. Each CERES sub-footprint cloud layer and associated fluxes are assigned to one of the 42 cloud types, similar to the stratification process in the CldTypHist product. FluxByCloudTyp is an hourly instantaneous gridded daytime-only product with a global extent. Each netCDF4 file covers a single day. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument, the proto flight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit onboard the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched onboard Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched onboard the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched onboard the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_ssf1deg-hour_noaa20-viirs&quot;&gt;CER_SSF1deg-Hour_NOAA20-VIIRS&lt;/h4&gt;
The Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) Single Scanner Footprint One Degree (SSF1deg) Hour provides regional averages of CERES Top of Atmosphere (TOA) fluxes, clouds derived from a co-located imager and aerosols on a 1-degree latitude and longitude grid. This single satellite product uses the primary CERES instrument in cross-track mode. TOA fluxes are provided for clear-sky and all-sky conditions for longwave (LW), shortwave (SW), and window wavelength bands. The incoming daily solar irradiance is from the Solar Radiation and Climate Experiment (SORCE) and Total Solar Irradiance (TSI). The cloud properties are averaged for day and night (24-hour) and day-only periods. Cloud properties are stratified into four atmospheric layers (surface-700 hPa, 700 hPa - 500 hPa, 500 hPa - 300 hPa, 300 hPa - 100 hPa) and a total of all layers. The aerosols are averaged instantaneous values from the co-located imager. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument (PFM) was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the EOS flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board EOS Aqua on May 4, 2002. The CERES instrument (FM5) was launched on board the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched on board the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_ssf1deg-month_npp-viirs&quot;&gt;CER_SSF1deg-Month_NPP-VIIRS&lt;/h4&gt;
CER_SSF1deg-Month_NPP-VIIRS_Edition2A is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) Single Scanner Footprint One Degree (SSF1deg) Time-Interpolated Top-of-Atmosphere (TOA) Fluxes, Clouds and Aerosols Monthly Edition 2A data product, which was collected using the CERES-Flight Model 5 (FM5) and Visible-Infrared Imager-Radiometer Suite (VIIRS) instruments on the Suomi National Polar-orbiting Partnership (NPP) platform. Data collection for this product is in progress. CERES SSF1deg Month provides monthly averages of regional constant meteorology temporally interpolated CERES TOA fluxes, clouds derived from a co-located imager, and aerosols on a 1-degree latitude and longitude grid. One-degree zonally and global averaged values for the parameters are also provided. This single satellite product uses the primary CERES instrument in cross-track mode. TOA fluxes are provided for clear-sky and all-sky conditions for longwave (LW), shortwave (SW), and window (WN) wavelength bands. The incoming solar daily irradiance is from the Solar Radiation and Climate Experiment (SORCE) Total Solar Irradiance (TSI). The cloud properties are averaged for day and night (24-hour) and day-only periods. Cloud properties are stratified into four atmospheric layers (surface-700 hPa, 700 hPa, - 500 hPa, 500 hPa, - 300 hPa, 300 hPa, - 100 hPa) and a total of all layers. The aerosols are averaged instantaneous values from the co-located imager. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument, the protoflight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched on board the Suomi NPP satellite on October 28, 2011. The newest CERES instrument (FM6) was launched on board the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_ssf1deg-day_noaa20-viirs&quot;&gt;CER_SSF1deg-Day_NOAA20-VIIRS&lt;/h4&gt;
The Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) Single Scanner Footprint One Degree (SSF1deg) Day provides daily averages of regional constant meteorology temporally interpolated CERES Top of Atmosphere (TOA) fluxes, clouds derived from a co-located imager and aerosols on a 1-degree latitude and longitude grid. This single satellite product uses the primary CERES instrument in cross-track mode. TOA fluxes are provided for clear-sky and all-sky conditions for longwave (LW), shortwave (SW), and window wavelength bands. The incoming daily solar irradiance is from the Solar Radiation and Climate Experiment (SORCE) and Total Solar Irradiance (TSI). The cloud properties are averaged for day and night (24-hour) and day-only periods. Cloud properties are stratified into four atmospheric layers (surface-700 hPa, 700 hPa - 500 hPa, 500 hPa - 300 hPa, 300 hPa - 100 hPa) and all layers. The aerosols are averaged instantaneous values from the co-located imager. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument (PFM) was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the EOS flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board EOS Aqua on May 4, 2002. The CERES instrument (FM5) was launched on board the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched on board the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_ssf1deg-day_noaa20-viirs-1&quot;&gt;CER_SSF1deg-Day_NOAA20-VIIRS&lt;/h4&gt;
CER_SSF1deg-Day_NOAA20-VIIRS_Edition1C is the NOAA-20 Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) Level 3 Single Scanner Footprint (SSF) Edition1C Top of Atmosphere (ToA) flux data product. The SSF One Degree (SSF1deg) Day provides daily averages on a 1-degree latitude and longitude global grid from the NOAA-20 CERES Flight Model 6 (FM-6) data. The last CERES instrument, FM-6, was launched on board the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now known as NOAA-20, on November 18, 2017. The data product begins May 1, 2018. The product is distributed in monthly Hierarchical Data Format (HDF) 4 files. The file contains the daily mean for each day of the month and provides global coverage over a day. The SSF1deg-Day granule contains daily averages of regional CERES FM6 Earth-viewing Top of Atmosphere (ToA) shortwave and longwave fluxes. The fluxes are converted from the unfiltered CERES radiances at the footprint level using the co-located Visible Infrared Imaging Radiometer Suite (VIIRS) imager-defined scene. The footprint fluxes are gridded at hourly periods and then temporally interpolated assuming constant meteorology between measurements. The ToA fluxes are provided for both clear-sky and total sky conditions. The incoming daily solar irradiance is from the Solar Radiation and Climate Experiment (SORCE) and Total Solar Irradiance (TSI). The VIIRS radiances are used with CERES-specific cloud mask and cloud property retrievals and are stratified into four atmospheric layers: surface to 700 mb, 700 mb to 500 mb, 500 to 300 mb, and above 300 mb along with the total. Each cloud layer has properties such as amount, height, temperature, pressure, optical depth, emissivity, phase, water path, and water particle size. The cloud properties are averaged for day and night (24-hour) and day-only periods. This product uses the instantaneous gridded product, CER_SSF1deg-Hour_NOAA20-VIIRS_Edition1C, as input.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_ssf1deg-day_npp-viirs&quot;&gt;CER_SSF1deg-Day_NPP-VIIRS&lt;/h4&gt;
CER_SSF1deg-Day_NPP-VIIRS_Edition2A is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) Time-Interpolated Top of Atmosphere (TOA) Fluxes, Clouds and Aerosols Daily SUOMI National Polar-orbiting Partnership (NPP) Edition 2A data product, which was collected using the CERES-Flight Model 5 (FM5) and Visible-Infrared Imager-Radiometer Suite (VIIRS) instruments on the Suomi NPP platform. Data collection for this product is ongoing. The CERES Single Scanner Footprint One Degree (SSF1deg) Daily product provides daily averages of regional constant meteorology temporally interpolated CERES TOA fluxes, clouds derived from a co-located imager, and aerosols on a 1-degree latitude and longitude grid. This single satellite product uses the primary CERES instrument in cross-track mode. TOA fluxes are provided for clear-sky and all-sky conditions for longwave (LW), shortwave (SW), and window (WN) wavelength bands. The incoming solar daily irradiance is from the Solar Radiation and Climate Experiment (SORCE), Total Solar Irradiance (TSI). The cloud properties are averaged for day and night (24-hour) and day-only periods. Cloud properties are stratified into four atmospheric layers (surface-700 hPa, 700 hPa, - 500 hPa, 500 hPa, - 300 hPa, 300 hPa, - 100 hPa) and a total of all layers. The aerosols are averaged instantaneous values from the co-located imager. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions are a follow-on to the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument, the protoflight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched on board the Suomi NPP satellite on October 28, 2011. The newest CERES instrument (FM6) was launched on board the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_ssf1deg-month_noaa20-viirs&quot;&gt;CER_SSF1deg-Month_NOAA20-VIIRS&lt;/h4&gt;
The Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) Single Scanner Footprint One Degree (SSF1deg) Month provides monthly averages of regional constant meteorology temporally interpolated CERES Top of Atmosphere (TOA) fluxes, clouds derived from a co-located imager and aerosols on a 1-degree latitude and longitude grid. One-degree zonally and global averaged values for the parameters are also provided. This single satellite product uses the primary CERES instrument in cross-track mode. TOA fluxes are provided for clear-sky and all-sky conditions for longwave (LW), shortwave (SW), and window wavelength bands. The incoming daily solar irradiance is from the Solar Radiation and Climate Experiment (SORCE) and Total Solar Irradiance (TSI). The cloud properties are averaged for day and night (24-hour) and day-only periods. Cloud properties are stratified into four atmospheric layers (surface-700 hPa, 700 hPa - 500 hPa, 500 hPa - 300 hPa, 300 hPa - 100 hPa) and a total of all layers. The aerosols are averaged instantaneous values from the co-located imager.CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument (PFM) was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the EOS flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board EOS Aqua on May 4, 2002. The CERES instrument (FM5) was launched on board the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched on board the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_ssf1deg-month_noaa20-viirs-1&quot;&gt;CER_SSF1deg-Month_NOAA20-VIIRS&lt;/h4&gt;
CER_SSF1deg-Month_NOAA20-VIIRS_Edition1C is the NOAA-20 Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) Level 3 Single Scanner Footprint (SSF) Edition1C Top of Atmosphere (ToA) flux data product. The SSF One Degree (SSF1deg) Month provides monthly averages on a 1-degree latitude and longitude global grid from the NOAA-20 CERES Flight Model 6 (FM6) data. The last CERES instrument, FM-6, was launched on board the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now known as NOAA-20, on November 18, 2017. The data product begins May 1, 2018. The product is distributed in monthly Hierarchical Data Format (HDF) 4 files. The file contains the monthly mean and provides global coverage. The SSF1deg-Month granule contains the monthly averages of regional CERES FM6 Earth viewing Top of Atmosphere (ToA) shortwave and longwave fluxes. The fluxes are converted from the unfiltered CERES radiances at the footprint level using the co-located Visible Infrared Imaging Radiometer Suite (VIIRS) imager-defined scene. The footprint fluxes are gridded at hourly periods and then temporally interpolated assuming constant meteorology between measurements. The ToA fluxes are provided for both clear-sky and total sky conditions. The incoming daily solar irradiance is from the Solar Radiation and Climate Experiment (SORCE) and Total Solar Irradiance (TSI). The VIIRS radiances are used with CERES-specific cloud mask and cloud property retrievals and are stratified into four atmospheric layers: surface to 700 mb, 700 mb to 500 mb, 500 to 300 mb, and above 300 mb along with the total. Each cloud layer has properties such as amount, height, temperature, pressure, optical depth, emissivity, phase, water path, and water particle size. The cloud properties are averaged for day and night (24-hour) and day-only periods. This product uses the instantaneous gridded product, CER_SSF1deg-Hour_NOAA20-VIIRS_Edition1C, as input.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_ssf1deg-month_terra-modis&quot;&gt;CER_SSF1deg-Month_Terra-MODIS&lt;/h4&gt;
CER_SSF1deg-Month_Terra-MODIS_Edition4A is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) Time-Interpolated Top of Atmosphere (TOA) Fluxes, Clouds and Aerosols Monthly Terra Edition4A data product, which was collected using the CERES Flight Model 1 (FM1), FM2, and MODIS instruments on the Terra platform. Data collection for this product is in progress. CERES Single Scanner Footprint One Degree (SSF1deg) Day provides daily averages of regional constant meteorology temporally interpolated TOA fluxes, clouds derived from a co-located imager, and aerosols on a 1-degree latitude and longitude grid. This single satellite product uses the primary CERES instrument in cross-track mode. TOA fluxes are provided for clear-sky and all-sky conditions for longwave (LW), shortwave (SW), and window (WN) wavelength bands. The incoming solar daily irradiance is from the SOlar Radiation and Climate Experiment (SORCE) and Total Solar Irradiance (TSI). The cloud properties are averaged for day and night (24-hour) and day-only periods. Cloud properties are stratified into four atmospheric layers (surface-700 hPa, 700 hPa, - 500 hPa, 500 hPa, - 300 hPa, 300 hPa - 100 hPa) and a total of all layers. The aerosols are averaged instantaneous values from the co-located imager. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument, the protoflight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched on board the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched on board the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_cldtyphist_geo-modis-viirs&quot;&gt;CER_CldTypHist_GEO-MODIS-VIIRS&lt;/h4&gt;
CER_CldTypHist_GEO-MODIS-VIIRS_Edition4A is the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES)- Moderate-Resolution Imaging Spectroradiometer (MODIS) and Visible Infrared Imaging Radiometer Suite (VIIRS) and hourly geostationary cloud properties stratified by the International Satellite Cloud Climatology Project (ISCCP) cloud types for day and night Edition 4A data product. Data collection is ongoing. The CERES-MODIS-VIIRS and hourly geostationary cloud properties (CldTypHist) data product contain monthly and one-hourly gridded regional mean cloud properties as a function of 18 cloud types, where the cloud properties are stratified by pressure, optical depth, and phase. Data is available day and night. The CldTypHist product combines cloud properties from Terra-MODIS (10:30 AM local equator crossing time LECT), NOAA20-VIIRS (1:30 PM LECT), and geostationary satellites (GEO) to provide the most diurnally complete product. The GEO cloud properties have been normalized with MODIS for diurnal consistency. The CERES MODIS-derived cloud properties are not the official NASA MODIS cloud retrievals but are based on the CERES cloud working group retrievals that are also available in other CERES products. Likewise, CERES-VIIRS cloud properties are not the official NASA VIIRS cloud retrievals but are based on the CERES cloud working group retrievals that are also available in other CERES products. The CERES MODIS-derived and VIIRS-derived cloud properties provide coverage from pole to pole. The hourly GEO cloud properties come from five satellites at 8km nominal resolution with coverage limited to equatorward of 60 degrees. The GEO cloud retrievals incorporate additional channels as they become available on improved geostationary satellites that replaced earlier ones in the time period. The geostationary calibration is normalized to Terra-MODIS. Each CldTypHist file covers a single month. CERES is a key component of the Earth Observing System (EOS) program. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES missions are a follow-on to the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument, the proto flight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit onboard the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched onboard Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched onboard the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched onboard the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_geo_ed4_goe15_nh&quot;&gt;CER_GEO_Ed4_GOE15_NH&lt;/h4&gt;
CER_GEO_Ed4_GOE15_NH_V01.4 is the Satellite Cloud and Radiation Property retrieval System (SatCORPS) Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) Geostationary Satellite (GEO) Edition 4 Geostationary Operational Environmental Satellite 15 (GOES-15) over the Northern Hemisphere (NH) Version 1.4 data product. Data was collected using the GOES-15 Imager on the GOES-15 Platform. Note: Version 1.4 uses the Global Modeling and Assimilation Office (GMAO) Modern-Era Retrospective analysis for Research and Applications, Version 2 (MERRA-2) reanalysis for atmospheric input; Version 1.2 used GMAO&amp;#39;s GEOS-5.4.1. No changes have been made to the cloud retrieval algorithm. This data set comprises cloud micro-physical and radiation properties derived hourly from GOES-15 geostationary satellite imager data using the Langley Research Center (LaRC) SATCORPS algorithms supporting the CERES project. The data set is arranged as files for each hour in netCDF-4 format. The observations are at 4 km resolution (at nadir) and are sub-sampled to 8 km (taking every other line and pixel).
&lt;br&gt;&lt;h4 id&#x3D;&quot;cer_geo_ed4_goe17_nh&quot;&gt;CER_GEO_Ed4_GOE17_NH&lt;/h4&gt;
CER_GEO_Ed4_GOE17_NH_V01.4 is the Satellite Cloud and Radiation Property retrieval System (SatCORPS) Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) Geostationary Satellite (GEO) Edition 4 Geostationary Operational Environmental Satellite 17 (GOES-17) over the Northern Hemisphere (NH) Version 1.4 data product. Data was collected using the Advanced Baseline Imager (ABI) on the GOES-17 Platform. Note: Version 1.4 uses the Global Modeling and Assimilation Office (GMAO) Modern-Era Retrospective analysis for Research and Applications, Version 2 (MERRA-2) reanalysis for atmospheric input; Version 1.2 used GMAO&amp;#39;s GEOS-5.4.1. No changes have been made to the cloud retrieval algorithm. This data set comprises cloud micro-physical and radiation properties derived hourly from GOES-17 geostationary satellite imager data using the Langley Research Center (LaRC) SATCORPS algorithms supporting the CERES project. The data set is arranged as files for each hour in netCDF-4 format. The observations are at 2 km resolution (at nadir) and are sub-sampled to 6 km (taking every third line and pixel).
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA CIOSS Project</title>
      <link>https://registry.opendata.aws/nasa-cioss</link>
      <guid>https://registry.opendata.aws/nasa-cioss</guid>
      <description>The Gridded Altimeter Fields with Enhanced Coastal Coverage data product contains Sea Surface Height Anomalies (SSHA or SLA) and zonal and meridional geostrophic velocities for the US west coast encompassing 35.25 deg-48.5 deg N latitude and 227.75 deg-248.5 deg E longitude. This annually updated data product extends from October 14, 1992 through November 4, 2009. SSHA and current velocities are derived from the AVISO quarter degree DT UPD MSLA version 3.0 grids, 0.75 deg and greater away from the coast. Values within 0.75 deg of the coast are derived from tide gauge observations and interpolated out to the altimeter filled region. Details on how these data are derived can be found in: Saraceno, M., P. T. Strub, and P. M. Kosro (2008), Estimates of sea surface height and near-surface alongshore coastal currents from combinations of altimeters and tide gauges, J. Geophys. Res., 113, C11013, doi:10.1029/2008JC004756.
&lt;br&gt;&lt;h4 id&#x3D;&quot;alt_tide_gauge_l4_ost_sla_us_west_coast_daily&quot;&gt;ALT_TIDE_GAUGE_L4_OST_SLA_US_WEST_COAST_DAILY&lt;/h4&gt;
The Gridded Altimeter Fields with Enhanced Coastal Coverage data product contains Sea Surface Height Anomalies (SSHA or SLA) and zonal and meridional geostrophic velocities for the US west coast encompassing 35.25 deg-48.5 deg N latitude and 227.75 deg-248.5 deg E longitude. This annually updated data product extends from October 14, 1992 through January 19, 2011. SSHA and current velocities are derived from the AVISO quarter degree DT UPD MSLA version 3.0 grids, 0.75 deg and greater away from the coast. Values within 0.75 deg of the coast are derived from tide gauge observations and interpolated out to the altimeter filled region. Details on how these data are derived can be found in: Saraceno, M., P. T. Strub, and P. M. Kosro (2008), Estimates of sea surface height and near-surface alongshore coastal currents from combinations of altimeters and tide gauges, J. Geophys. Res., 113, C11013, doi:10.1029/2008JC004756.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://archive.podaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA CITE-2 Project</title>
      <link>https://registry.opendata.aws/nasa-cite-2</link>
      <guid>https://registry.opendata.aws/nasa-cite-2</guid>
      <description>CITE-2_Aerosol_AircraftInSitu_Electra_Data is the in-situ trace gas data collected onboard the NASA Electra aircraft Chemical Instrumentation Test and Evaluation - 2 (CITE-2) suborbital campaign. Data using forward scattering spectrometers are featured in this collection. Data collection for this product is complete. During 1983-2001, NASA conducted a collection of field campaigns as a part of the Global Tropospheric Experiment (GTE) to develop advanced instrumentation to measure critical atmospheric trace gases and quantify their sources, sinks, and distribution. Among those were the CITE missions, which had the overarching goal to test and evaluate the instruments developed for the GTE missions. To accomplish this objective, the CITE missions adopted the methodology of conducting intercomparisons of airborne measurements obtained for the same species by instruments utilizing fundamentally different detection principles (Hoell et al., 1990). The second phase of the CITE missions, CITE 2, was the first systematic evaluation of both instrumentation and photochemistry of odd nitrogen from an airborne platform (Hoell et al., 1990). Odd nitrogen is a crucial component of tropospheric chemistry. The common understanding of odd nitrogen chemistry at the time of GTE had come into question as being incomplete. Hoell et al. (1990) state that ground-based measurements showed there may be significant unidentified members of the NOy family and that “simple” odd nitrogen chemistry may not be fully understood, driving the objectives of CITE 2. CITE 2 was conducted in August 1986 with a focus on daytime odd nitrogen and the evaluation of instrumentation developed for measuring nitrogen species, specifically nitrogen dioxide (NO2), nitric acid (HNO3), and peroxyacetyl nitrate (PAN). Additional questions related to the abundance and partitioning among members of the odd nitrogen family were studied (Hoell et al., 1990). To accomplish its objectives, the CITE 2 team deployed the NASA Lockheed Electra aircraft equipped with a suite of instrumentation for the intercomparison of nitrogen species augmented with ancillary measurements such as temperature, dew point, wind velocity, aircraft position, CO, and ozone (O3). Ancillary measurements were added to the payload to answer questions related to tropospheric odd nitrogen budgets and photochemistry. Along with the airborne measurements, the CITE 2 campaign also relied on a ground-based evaluation of calibration standards for HNO3, NO2, PAN, and intercomparison of airborne ambient measurements of each species. Based at Moffett Field, California, CITE 2 took place over a four-week period conducting measurements over California and the eastern Pacific Ocean. While CITE 1 and CITE 2 used identical measurement techniques for NO2, the campaigns used different measurements techniques for the remaining species. Detailed descriptions related to the motivation, implementation, and instrument payloads are available in the CITE 2 overview paper. A collection of the publications based on CITE 2 observations are available in the Journal of Geophysical Research special issue: Global Tropospheric Experiment/Chemical Instrumentation Test &amp;amp; Evaluation.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cite-2_tracegas_aircraftinsitu_electra_data&quot;&gt;CITE-2_TraceGas_AircraftInSitu_Electra_Data&lt;/h4&gt;
CITE-2_TraceGas_AircraftInSitu_Electra_Data is the in-situ trace gas data collected onboard the NASA Electra aircraft Chemical Instrumentation Test and Evaluation - 2 (CITE-2) suborbital campaign. Data using grab samples, gas chromatography, chemiluminescence, and laser differential absorption are featured in this collection. Data collection for this product is complete. During 1983-2001, NASA conducted a collection of field campaigns as a part of the Global Tropospheric Experiment (GTE) to develop advanced instrumentation to measure critical atmospheric trace gases and quantify their sources, sinks, and distribution. Among those were the CITE missions, which had the overarching goal to test and evaluate the instruments developed for the GTE missions. To accomplish this objective, the CITE missions adopted the methodology of conducting intercomparisons of airborne measurements obtained for the same species by instruments utilizing fundamentally different detection principles (Hoell et al., 1990). The second phase of the CITE missions, CITE 2, was the first systematic evaluation of both instrumentation and photochemistry of odd nitrogen from an airborne platform (Hoell et al., 1990). Odd nitrogen is a crucial component of tropospheric chemistry. The common understanding of odd nitrogen chemistry at the time of GTE had come into question as being incomplete. Hoell et al. (1990) state that ground-based measurements showed there may be significant unidentified members of the NOy family and that “simple” odd nitrogen chemistry may not be fully understood, driving the objectives of CITE 2. CITE 2 was conducted in August 1986 with a focus on daytime odd nitrogen and the evaluation of instrumentation developed for measuring nitrogen species, specifically nitrogen dioxide (NO2), nitric acid (HNO3), and peroxyacetyl nitrate (PAN). Additional questions related to the abundance and partitioning among members of the odd nitrogen family were studied (Hoell et al., 1990). To accomplish its objectives, the CITE 2 team deployed the NASA Lockheed Electra aircraft equipped with a suite of instrumentation for the intercomparison of nitrogen species augmented with ancillary measurements such as temperature, dew point, wind velocity, aircraft position, CO, and ozone (O3). Ancillary measurements were added to the payload to answer questions related to tropospheric odd nitrogen budgets and photochemistry. Along with the airborne measurements, the CITE 2 campaign also relied on a ground-based evaluation of calibration standards for HNO3, NO2, PAN, and intercomparison of airborne ambient measurements of each species. Based at Moffett Field, California, CITE 2 took place over a four-week period conducting measurements over California and the eastern Pacific Ocean. While CITE 1 and CITE 2 used identical measurement techniques for NO2, the campaigns used different measurements techniques for the remaining species. Detailed descriptions related to the motivation, implementation, and instrument payloads are available in the CITE 2 overview paper. A collection of the publications based on CITE 2 observations are available in the Journal of Geophysical Research special issue: Global Tropospheric Experiment/Chemical Instrumentation Test &amp;amp; Evaluation.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cite-2_metnav_aircraftinsitu_electra_data&quot;&gt;CITE-2_MetNav_AircraftInSitu_Electra_Data&lt;/h4&gt;
CITE-2_MetNav_AircraftInSitu_Electra_Data is the in-situ meteorology and navigational data collected onboard the NASA Electra aircraft Chemical Instrumentation Test and Evaluation - 2 (CITE-2) suborbital campaign. Data collection for this product is complete. During 1983-2001, NASA conducted a collection of field campaigns as a part of the Global Tropospheric Experiment (GTE) to develop advanced instrumentation to measure critical atmospheric trace gases and quantify their sources, sinks, and distribution. Among those were the CITE missions, which had the overarching goal to test and evaluate the instruments developed for the GTE missions. To accomplish this objective, the CITE missions adopted the methodology of conducting intercomparisons of airborne measurements obtained for the same species by instruments utilizing fundamentally different detection principles (Hoell et al., 1990). The second phase of the CITE missions, CITE 2, was the first systematic evaluation of both instrumentation and photochemistry of odd nitrogen from an airborne platform (Hoell et al., 1990). Odd nitrogen is a crucial component of tropospheric chemistry. The common understanding of odd nitrogen chemistry at the time of GTE had come into question as being incomplete. Hoell et al. (1990) state that ground-based measurements showed there may be significant unidentified members of the NOy family and that “simple” odd nitrogen chemistry may not be fully understood, driving the objectives of CITE 2. CITE 2 was conducted in August 1986 with a focus on daytime odd nitrogen and the evaluation of instrumentation developed for measuring nitrogen species, specifically nitrogen dioxide (NO2), nitric acid (HNO3), and peroxyacetyl nitrate (PAN). Additional questions related to the abundance and partitioning among members of the odd nitrogen family were studied (Hoell et al., 1990). To accomplish its objectives, the CITE 2 team deployed the NASA Lockheed Electra aircraft equipped with a suite of instrumentation for the intercomparison of nitrogen species augmented with ancillary measurements such as temperature, dew point, wind velocity, aircraft position, CO, and ozone (O3). Ancillary measurements were added to the payload to answer questions related to tropospheric odd nitrogen budgets and photochemistry. Along with the airborne measurements, the CITE 2 campaign also relied on a ground-based evaluation of calibration standards for HNO3, NO2, PAN, and intercomparison of airborne ambient measurements of each species. Based at Moffett Field, California, CITE 2 took place over a four-week period conducting measurements over California and the eastern Pacific Ocean. While CITE 1 and CITE 2 used identical measurement techniques for NO2, the campaigns used different measurements techniques for the remaining species. Detailed descriptions related to the motivation, implementation, and instrument payloads are available in the CITE 2 overview paper. A collection of the publications based on CITE 2 observations are available in the Journal of Geophysical Research special issue: Global Tropospheric Experiment/Chemical Instrumentation Test &amp;amp; Evaluation.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.asdc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA CITE-3 Project</title>
      <link>https://registry.opendata.aws/nasa-cite-3</link>
      <guid>https://registry.opendata.aws/nasa-cite-3</guid>
      <description>CITE-3_Aerosol_AircraftInSitu_Electra_Data is the in-situ trace gas data collected onboard the NASA Electra aircraft Chemical Instrumentation Test and Evaluation - 3 (CITE-3) suborbital campaign. Data using chemiluminescence are featured in this collection. Data collection for this product is complete. During 1983-2001, NASA conducted a collection of field campaigns as a part of the Global Tropospheric Experiment (GTE) to develop advanced instrumentation to measure critical atmospheric trace gases and quantify their sources, sinks, and distribution. Among those were the Chemical Instrumentation Test and Evaluation (CITE) missions, which had the overarching goal to test and evaluate the instruments developed for the GTE missions. To accomplish this objective, the CITE missions adopted the methodology of conducting intercomparisons of airborne measurements obtained for the same species by instruments utilizing fundamentally different detection principles (Hoell et al., 1990). The third phase of the CITE mission, CITE 3, occurred in the North and tropical Atlantic Ocean from August-September 1989. Its primary objective was to test and evaluate the capacity to collect reliable measurements of the following sulfur species: sulfur dioxide (SO2), dimethyl sulfide (DMS), carbonyl sulfide (COS), carbon disulfide (CS2), and hydrogen sulfide (H2S). The secondary objective of CITE 3 was to determine the abundance and distribution of major sulfur species over a wide range of atmospheric conditions, including altitude, solar flux levels, atmospheric mixing ratios, and surface source strengths of sulfur in a predominantly marine environment (Hoell et al., 1993). CITE 3 utilized the NASA Electra research aircraft equipped with a suite of instruments for sulfur and ancillary measurements. The two main objectives were addressed through intercomparisons of airborne measurements obtained for the same species but utilizing fundamentally different detection principles in order to have multiple measurements of each of the sulfur species. In some instances, the same detection principle was used, but the method of sample collection and/or analysis procedures were different. A complete payload had the potential of five techniques for SO2, six techniques for DMS, and three techniques for H2S, CS2, and COS. However, due to operational problems or team decisions to focus on specific species during flights, not all measurement techniques were employed at all times (Hoell et al., 1993). There were three phases of field activity in this campaign: (1) intercomparison of sulfur calibration standards, (2) measurements in ambient air over the Northern Atlantic Ocean, and (3) measurements in ambient air over the tropical Atlantic Ocean. Cite 3 was based out of NASA Wallops Flight Facility in Virginia, USA and Natal, Brazil. Each base of operation provided a different environment for intercomparison. Air masses at NAS Wallops Flight Facility were influenced by anthropogenic emissions along the eastern United States compared to the relatively clean marine boundary layer over the ocean off the coast of Natal. As part of the Natal deployment, ozonesondes were launched from the Natal area to provide data on the general state of the atmosphere as well as serve as a frame of reference when compared to the seasonally averaged ozone data from this site. seasonally averaged ozone data from this site. Sulfur gases and their reaction products play important roles in the chemistry of the global troposphere as well as the biogeochemical sulfur cycle. The sulfur database from CITE 3, and the results from both intercomparison studies and photochemical budget studies, significantly enhanced the ability to evaluate the confidence in the existing databases. Detailed description related to the motivation, implementation, and instrument payloads are available in the CITE 3 overview paper. A collection of the publications based on CITE 3 observations are available in the Journal of Geophysical Research special issue: Chemical Instrumentation Test and Evaluation (CITE 3).
&lt;br&gt;&lt;h4 id&#x3D;&quot;cite-3_tracegas_aircraftinsitu_electra_data&quot;&gt;CITE-3_TraceGas_AircraftInSitu_Electra_Data&lt;/h4&gt;
CITE-3_TraceGas_AircraftInSitu_Electra_Data is the in-situ trace gas data collected onboard the NASA Electra aircraft Chemical Instrumentation Test and Evaluation - 3 (CITE-3) suborbital campaign. Data using gas chromatography, laser induced photofragmentation, and the Differential Absorption CO, CH4, N2O Measurements (DACOM) instrument are featured in this collection. Data collection for this product is complete. During 1983-2001, NASA conducted a collection of field campaigns as a part of the Global Tropospheric Experiment (GTE) to develop advanced instrumentation to measure critical atmospheric trace gases and quantify their sources, sinks, and distribution. Among those were the Chemical Instrumentation Test and Evaluation (CITE) missions, which had the overarching goal to test and evaluate the instruments developed for the GTE missions. To accomplish this objective, the CITE missions adopted the methodology of conducting intercomparisons of airborne measurements obtained for the same species by instruments utilizing fundamentally different detection principles (Hoell et al., 1990). The third phase of the CITE mission, CITE 3, occurred in the North and tropical Atlantic Ocean from August-September 1989. Its primary objective was to test and evaluate the capacity to collect reliable measurements of the following sulfur species: sulfur dioxide (SO2), dimethyl sulfide (DMS), carbonyl sulfide (COS), carbon disulfide (CS2), and hydrogen sulfide (H2S). The secondary objective of CITE 3 was to determine the abundance and distribution of major sulfur species over a wide range of atmospheric conditions, including altitude, solar flux levels, atmospheric mixing ratios, and surface source strengths of sulfur in a predominantly marine environment (Hoell et al., 1993). CITE 3 utilized the NASA Electra research aircraft equipped with a suite of instruments for sulfur and ancillary measurements. The two main objectives were addressed through intercomparisons of airborne measurements obtained for the same species but utilizing fundamentally different detection principles in order to have multiple measurements of each of the sulfur species. In some instances, the same detection principle was used, but the method of sample collection and/or analysis procedures were different. A complete payload had the potential of five techniques for SO2, six techniques for DMS, and three techniques for H2S, CS2, and COS. However, due to operational problems or team decisions to focus on specific species during flights, not all measurement techniques were employed at all times (Hoell et al., 1993). There were three phases of field activity in this campaign: (1) intercomparison of sulfur calibration standards, (2) measurements in ambient air over the Northern Atlantic Ocean, and (3) measurements in ambient air over the tropical Atlantic Ocean. Cite 3 was based out of NASA Wallops Flight Facility in Virginia, USA and Natal, Brazil. Each base of operation provided a different environment for intercomparison. Air masses at NAS Wallops Flight Facility were influenced by anthropogenic emissions along the eastern United States compared to the relatively clean marine boundary layer over the ocean off the coast of Natal. As part of the Natal deployment, ozonesondes were launched from the Natal area to provide data on the general state of the atmosphere as well as serve as a frame of reference when compared to the seasonally averaged ozone data from this site. seasonally averaged ozone data from this site. Sulfur gases and their reaction products play important roles in the chemistry of the global troposphere as well as the biogeochemical sulfur cycle. The sulfur database from CITE 3, and the results from both intercomparison studies and photochemical budget studies, significantly enhanced the ability to evaluate the confidence in the existing databases. Detailed description related to the motivation, implementation, and instrument payloads are available in the CITE 3 overview paper. A collection of the publications based on CITE 3 observations are available in the Journal of Geophysical Research special issue: Chemical Instrumentation Test and Evaluation (CITE 3).
&lt;br&gt;&lt;h4 id&#x3D;&quot;cite-3_metnav_aircraftinsitu_electra_data&quot;&gt;CITE-3_MetNav_AircraftInSitu_Electra_Data&lt;/h4&gt;
CITE-3_MetNav_AircraftInSitu_Electra_Data is the in-situ trace gas data collected onboard the NASA Electra aircraft Chemical Instrumentation Test and Evaluation - 3 (CITE-3) suborbital campaign. Data collection for this product is complete. During 1983-2001, NASA conducted a collection of field campaigns as a part of the Global Tropospheric Experiment (GTE) to develop advanced instrumentation to measure critical atmospheric trace gases and quantify their sources, sinks, and distribution. Among those were the Chemical Instrumentation Test and Evaluation (CITE) missions, which had the overarching goal to test and evaluate the instruments developed for the GTE missions. To accomplish this objective, the CITE missions adopted the methodology of conducting intercomparisons of airborne measurements obtained for the same species by instruments utilizing fundamentally different detection principles (Hoell et al., 1990). The third phase of the CITE mission, CITE 3, occurred in the North and tropical Atlantic Ocean from August-September 1989. Its primary objective was to test and evaluate the capacity to collect reliable measurements of the following sulfur species: sulfur dioxide (SO2), dimethyl sulfide (DMS), carbonyl sulfide (COS), carbon disulfide (CS2), and hydrogen sulfide (H2S). The secondary objective of CITE 3 was to determine the abundance and distribution of major sulfur species over a wide range of atmospheric conditions, including altitude, solar flux levels, atmospheric mixing ratios, and surface source strengths of sulfur in a predominantly marine environment (Hoell et al., 1993). CITE 3 utilized the NASA Electra research aircraft equipped with a suite of instruments for sulfur and ancillary measurements. The two main objectives were addressed through intercomparisons of airborne measurements obtained for the same species but utilizing fundamentally different detection principles in order to have multiple measurements of each of the sulfur species. In some instances, the same detection principle was used, but the method of sample collection and/or analysis procedures were different. A complete payload had the potential of five techniques for SO2, six techniques for DMS, and three techniques for H2S, CS2, and COS. However, due to operational problems or team decisions to focus on specific species during flights, not all measurement techniques were employed at all times (Hoell et al., 1993). There were three phases of field activity in this campaign: (1) intercomparison of sulfur calibration standards, (2) measurements in ambient air over the Northern Atlantic Ocean, and (3) measurements in ambient air over the tropical Atlantic Ocean. Cite 3 was based out of NASA Wallops Flight Facility in Virginia, USA and Natal, Brazil. Each base of operation provided a different environment for intercomparison. Air masses at NAS Wallops Flight Facility were influenced by anthropogenic emissions along the eastern United States compared to the relatively clean marine boundary layer over the ocean off the coast of Natal. As part of the Natal deployment, ozonesondes were launched from the Natal area to provide data on the general state of the atmosphere as well as serve as a frame of reference when compared to the seasonally averaged ozone data from this site. seasonally averaged ozone data from this site. Sulfur gases and their reaction products play important roles in the chemistry of the global troposphere as well as the biogeochemical sulfur cycle. The sulfur database from CITE 3, and the results from both intercomparison studies and photochemical budget studies, significantly enhanced the ability to evaluate the confidence in the existing databases. Detailed description related to the motivation, implementation, and instrument payloads are available in the CITE 3 overview paper. A collection of the publications based on CITE 3 observations are available in the Journal of Geophysical Research special issue: Chemical Instrumentation Test and Evaluation (CITE 3).
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.asdc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA CLASIC07 Project</title>
      <link>https://registry.opendata.aws/nasa-clasic07</link>
      <guid>https://registry.opendata.aws/nasa-clasic07</guid>
      <description>An inventory of NASA&amp;#39;s airborne and field campaigns for Earth Science
&lt;br&gt;&lt;h4 id&#x3D;&quot;cl07sm&quot;&gt;CL07SM&lt;/h4&gt;
This data set is comprised of several parameters from in situ measurements collected for the Cloud and Land Surface Interaction Campaign 2007 (CLASIC07).
&lt;br&gt;&lt;h4 id&#x3D;&quot;cl07v&quot;&gt;CL07V&lt;/h4&gt;
This data set includes in situ vegetation data collected during the Cloud and Land Surface Interaction Campaign 2007 (CLASIC07) campaign. Sampling was designed to coincide with satellite overpasses, such as Landsat&amp;#39;s Thematic Mapper (TM) 5 and the Moderate Resolution Imaging Spectroradiometer (MODIS) sensor on NASA&amp;#39;s Terra satellite (MODIS/Terra), which can be then used to estimate vegetation water content on the regional scale.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cl07lc&quot;&gt;CL07LC&lt;/h4&gt;
This data set consists of land cover classification data derived from satellite imagery as part of the Cloud and Land Surface Interaction Campaign 2007 (CLASIC07). ResourceSat-1 AWiFS images of the study area were retrieved for the period of April through August 2007. The land use classification image provides information about vegetation present in the study area at a resolution of 56 meters.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cl07plbk&quot;&gt;CL07PLBK&lt;/h4&gt;
This data set contains backscatter data obtained by the Passive Active L-band System (PALS) microwave aircraft radar instrument as part of the Cloud and Land Surface Interaction Campaign 2007 (CLASIC07).
&lt;br&gt;&lt;h4 id&#x3D;&quot;cl07pltb&quot;&gt;CL07PLTB&lt;/h4&gt;
This data set contains brightness temperature data obtained by the Passive Active L-band System (PALS) microwave aircraft radiometer instrument as part of the Cloud and Land Surface Interaction Campaign 2007 (CLASIC07).
&lt;br&gt;&lt;h4 id&#x3D;&quot;cl07st&quot;&gt;CL07ST&lt;/h4&gt;
This data set contains soil texture data obtained for the Cloud and Land Surface Interaction Campaign 2007 (CLASIC07). The original data were extracted from a multi-layer soil characteristics database for the conterminous United States called CONUS-Soil and generated for the regional study area. Data are representative of the conditions present in the regional study area during the general timeline of the CLASIC07 campaign.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cl07vwc&quot;&gt;CL07VWC&lt;/h4&gt;
The Vegetation Water Content (VWC) map for the Cloud and Land Surface Interaction Campaign 2007 (CLASIC07) was derived by calculating Normalized Difference Water Index (NDWI) from ResourceSat-1 satellite imagery.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.nsidc.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA CMS Project</title>
      <link>https://registry.opendata.aws/nasa-cms</link>
      <guid>https://registry.opendata.aws/nasa-cms</guid>
      <description>This dataset provides gridded estimates of aboveground biomass (AGB) for live dry woody vegetation density in the form of both stock for the baseline year 2003 and annual change in stock from 2003 to 2016. Data are at a spatial resolution of approximately 500 m (463.31 m; 21.47 ha) for three geographies: the biogeographical limit of the Amazon Basin, the country of Mexico, and a Pantropical belt from 40 degrees North to 30 degrees South latitudes. Estimates were derived from a multi-step modeling approach that combined field measurements with co-located LiDAR data from NASA ICESat Geoscience Laser Altimeter System (GLAS) to calibrate a machine-learning (ML) algorithm that generated spatially explicit annual estimates of AGB density. ML inputs included a suite of satellite and ancillary spatial predictor variables compiled as wall-to-wall raster mosaics, including MODIS products, WorldClim climate variables reflecting current (1960-1990) climatic conditions, and SoilGrids soil variables. The 14-year time series was analyzed at the grid cell (~500 m) level with a change point-fitting algorithm to quantify annual losses and gains in AGB. Estimates of AGB and change can be used to derive total losses, gains, and the net change in aboveground carbon density over the study period as well as annual estimates of carbon stock.
&lt;br&gt;&lt;h4 id&#x3D;&quot;salt_marsh_biomass_conus_2348&quot;&gt;Salt_Marsh_Biomass_CONUS_2348&lt;/h4&gt;
This dataset provides estimates of aboveground biomass (AGB) and salt marsh extent in the contiguous United States for 2020 and includes all coastal watersheds across the contiguous United States at 10-m resolution. Estimates were generated by XGBoost machine learning regression. Salt marsh extent was classified using an ensemble of XGBoost, random forests, and support vector machines, trained with salt marsh location identified with the National Wetland Inventory (NWI). The data are organized by Hydrologic Unit Code (HUC) 6-digit basin. Within each HUC, the spatial extent of salt marsh and its uncertainty were estimated by machine learning and input data from NWI maps, the National Elevation Dataset, along with Sentinel-1 and Sentinel-2 imagery. Estimates were compared to in situ biomass data from salt marshes in Georgia and Massachusetts. The data are provided in cloud-optimized GeoTIFF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;howland_forest_biomass_map_2434&quot;&gt;Howland_Forest_Biomass_Map_2434&lt;/h4&gt;
This dataset holds aboveground biomass (AGB) estimates at 10-m spatial resolution for the Howland Research Forest in central Maine for 2012, 2015, 2017, 2021, and 2023. Forest inventory data were collected using 50 fixed-area plot sampling during the summers of 2021, 2023, and 2024. Plots included permanent inventory plots around existing flux towers and additional plots to ensure representation of various forest conditions. Each plot had a radius of 7.98 m. In addition, leaf-off airborne LiDAR data were collected by the USGS 3DEP project in 2012, 2015, and 2023, and leaf-on data were obtained from the NASA G-LiHT project for 2017 and 2021. The LANDIS-II forest landscape model along with its Biomass Succession extension was used to simulate ecosystem dynamics in Howland Forest. Then, a random forest (RF) model was used to generate wall-to-wall biomass maps for the research forest from the LiDAR data. The RF model was calibrated from in situ AGB measurements from plots and simulated AGB values for the LiDAR acquisition years. Howland Research Forest is a low-elevation transitional forest dominated by spruce and hemlock, with conifer and northern hardwood species. The data are provided in cloud optimized GeoTIFF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tidal_marsh_biomass_us_v1-1_1879&quot;&gt;Tidal_Marsh_Biomass_US_V1-1_1879&lt;/h4&gt;
This dataset provides maps of aboveground tidal marsh biomass (g/m2) at 30 m resolution for six estuarine regions of the conterminous United States: Cape Cod, MA; Chesapeake Bay, MD, Everglades, FL; Mississippi Delta, LA; San Francisco Bay, CA; and Puget Sound, WA. Estuarine and palustrine emergent tidal marsh areas were based on a 2010 NOAA Coastal Change Analysis Program (C-CAP) map. Aboveground biomass maps were generated from a random forest model driven by Landsat vegetation indices and a national scale dataset of field-measured aboveground biomass. The final model, driven by six Landsat vegetation indices, with the soil adjusted vegetation index as the most important, successfully predicted biomass for a range of marsh plant functional types defined by height, leaf angle, and growth form. Biomass can be converted to carbon stocks using a mean plant carbon content of 44.1%.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_agb_landcover_indonesia_1645&quot;&gt;CMS_AGB_Landcover_Indonesia_1645&lt;/h4&gt;
This dataset provides estimates of aboveground biomass, percent canopy cover, mean canopy height, landcover, and forest degradation index products for forests in Kalimantan, Indonesia (Island of Borneo) representative of conditions in late 2014. Data were combined from several sources including field sampling, airborne lidar, satellite measurements, a forest-type land cover map, and integrated into a random forest algorithm to produce these estimates.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_iwed_v1_2452&quot;&gt;CMS_iWED_V1_2452&lt;/h4&gt;
This dataset provides an integrated Wildfire Event Dataset (iWED version 1) for wildfire events of 100 ha or more in area from 1992 to 2021 for the continental US. Fire information was compiled from a variety of state, regional, and federal-level agencies responsible for filing and archiving incident level reports. Additional information was obtained from the Monitoring Trends in Burn Severity (MTBS) program initiated in the mid-2000s. MTBS is being continuously updated as new satellite remote sensing data are collected and processed. The data are provided in comma separated values (CSV) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_agb_nw_usa_1719&quot;&gt;CMS_AGB_NW_USA_1719&lt;/h4&gt;
This dataset provides annual maps of aboveground biomass (AGB, Mg/ha) for forests in Washington, Oregon, Idaho, and western Montana, USA, for the years 2000-2016, at a spatial resolution of 30 meters. Tree measurements were summarized with the Fire and Fuels Extension of the Forest Vegetation Simulator (FFE-FVS) to estimate AGB in field plots contributed by stakeholders, then lidar was used to predict plot-level AGB using the Random Forests machine learning algorithm. The machine learning outputs were used to predict AGB from Landsat time series imagery processed through LandTrendr, climate metrics generated from 30-year climate normals, and topographic metrics generated from a 30-m Shuttle Radar Topography Mission (SRTM) digital elevation model (DEM). The non-forested pixels were masked using the PALSAR 2009 forest/nonforest mask.
&lt;br&gt;&lt;h4 id&#x3D;&quot;annual_burned_area_maps_1708&quot;&gt;Annual_Burned_Area_Maps_1708&lt;/h4&gt;
This dataset provides maps of annual burned area for the part of Mawas conservation program in Central Kalimantan, Indonesia from 1997 through 2015. Landsat imagery (TM, ETM+, OLI/TIR) at 30 m resolution was obtained for this 19-year period, including the variables surface reflectance, brightness temperature, and pixel quality assurance, plus the indices NDVI, NDMI, NBR, NBR2, SAVI, and MSAVI. The MODIS active fire product (MCD14) was used to define when fires occurred. Random Forest classifications were used to separate burned and unburned 30-m pixels with inputs of composites of Landsat indices and thermal bands, based on the pre- and post-fire values.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_wfeis_conus-ak_1306&quot;&gt;CMS_WFEIS_CONUS-AK_1306&lt;/h4&gt;
This data set contains annual modeled estimates of wildland fire emissions at 0.01 degree (~1-km) spatial resolution from the Wildland Fire Emissions Information System (WFEIS v0.5) for the conterminous U.S. (CONUS) and Alaska for 2001 through 2013. WFEIS is a web-based tool that provides resources to quantify emissions from past fires and output results as spatial data files (French et al., 2014). The data set includes emissions estimates of carbon (C), carbon monoxide (CO), carbon dioxide (CO2), methane (CH4), other non-methane hydrocarbons (NMHC), and particulate matter (PM) as well as estimates of above-ground biomass, total fuel availability, and consumption estimates.
&lt;br&gt;&lt;h4 id&#x3D;&quot;blue_carbon_tidal_wetland_maps_2091&quot;&gt;Blue_Carbon_Tidal_Wetland_Maps_2091&lt;/h4&gt;
This dataset contains shapefiles showing location of tidal wetland parcels with the potential for net greenhouse gas removal if restored from current mapped condition to unimpeded tidal wetlands. These maps focus on managed lands in the contiguous United States along the ocean coasts and show impounded wetlands where reconnecting tidal flow could diminish methane production. The maps include current dominant wetland type, restoration category, potential removal of atmospheric greenhouse gases in units of mass carbon dioxide with estimates of uncertainty.
&lt;br&gt;&lt;h4 id&#x3D;&quot;blueflux_airborneobs_florida_2327&quot;&gt;BlueFlux_AirborneObs_Florida_2327&lt;/h4&gt;
This dataset includes airborne in situ measurements of greenhouse gas mixing ratios, meteorological parameters, and fluxes (CO2, CH4, latent heat fluxes, friction velocity, and convective velocity scale) calculated with wavelet transforms. CO2, CH4, CO, O3, and water vapor mixing ratios, and meteorological variables were obtained from a Beechcraft A90 King Air aircraft. Flights occurred on April 19-26 2022, October 14-20 2022, February 5-13 2023, and April 13-19 2023 as part of the BlueFlux campaign, funded by NASA&amp;#39;s Carbon Monitoring System program. Measurements were made with several instruments, including a PICARRO 2401-m (0.5 Hz CO2/CH4/H2O/CO), PICARRO 2311-f (10 Hz CO2/CH4/H2O), NASA Rapid Ozone Experiment (ROZE, 10 Hz O3), and AIMMS-20 probe (3-D winds, meteorology, and aircraft location data). Flight lines span Everglades National Park (ENP) and Big Cypress National Preserve (BCNP) in southern Florida, USA. The measurements were used to calculate vertical fluxes of trace gases and heat via wavelet transform eddy covariance
&lt;br&gt;&lt;h4 id&#x3D;&quot;blueflux_tidal_river_water_2333&quot;&gt;BlueFlux_Tidal_River_Water_2333&lt;/h4&gt;
This dataset provides dissolved carbon (dissolved inorganic carbon and dissolved organic carbon), greenhouse gases, dissolved organic matter optical, and hydrological (water temperature, pH, alkalinity, dissolved oxygen) data collected from the Shark and Harney tidal rivers in the Everglades, Florida, USA. The data were collected as part of the NASA Carbon Monitoring System (CMS) BlueFlux field campaigns over the 2022 wet season (October 2022) and 2023 dry season (March 2023). Data includes single-collection samples collected from sites along both rivers and samples collected by an autosampler at one site over multiple tidal cycles. The data are provided in comma-separated values (.csv) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;blueflux_gridded_co2_ch4_2404&quot;&gt;BlueFlux_Gridded_CO2_CH4_2404&lt;/h4&gt;
This dataset contains gridded estimates of carbon dioxide (CO2) and methane (CH4) fluxes at daily resolution covering the Southern Florida region from 2000 to 2024. Gridded CO2 and CH4 flux prototype products at 500-m spatial resolution were derived from a machine learning model based on eddy covariance (EC) measurements from 1) airborne fluxes collected seasonally with the NASA Carbon Airborne Flux Experiment (CARAFE) over the region during five flight deployments and 2) regional EC tower networks representing long term wetland ecosystem fluxes since 2004. Multiscale flux measurements were upscaled with remote sensing observations of MODIS optical reflectance using a bootstrap ensemble random forest modeling approach to predict daily mean flux intensity and uncertainty from February 2000 to August 2024. Prototypes of modeled, gridded greenhouse gas fluxes were developed as part of the NASA Carbon Monitoring System (CMS) BlueFlux Project. The data are provided in netCDF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tls_lidar_blueflux_mangroves_2311&quot;&gt;TLS_Lidar_BlueFlux_Mangroves_2311&lt;/h4&gt;
This dataset contains point clouds of three-dimensional (3D) mangrove forest structure and volume collected from 10 sites in Everglades National Park, Florida. Data were collected during NASA CMS &amp;quot;Blueflux&amp;quot; campaigns in March 2022, October 2022, and March 2023. Products were acquired using a RIEGL VZ-400i terrestrial laser scanner (TLS). TLS is a non-destructive and quantitative method for in situ 3D forest structure measuring and monitoring. Data are provided in LAS (.las) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;boreal_arctic_wetland_ch4_2351&quot;&gt;Boreal_Arctic_Wetland_CH4_2351&lt;/h4&gt;
This dataset provides an upscaled estimate of Boreal-Arctic wetland CH4 emissions at a weekly time scale from 2002 to 2021 at 0.5 by 0.5-degree spatial resolution. Ground truth data on wetland CH4 emissions from eddy covariance towers (139 site years) and chambers (168 site years) were used to train and validate a causality-guided machine learning model. The trained model was then used to estimate CH4 emissions at grid cells that have wetlands and located above 44 degrees north. The data are provided in netCDF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cmsfluxfire&quot;&gt;CMSFluxFire&lt;/h4&gt;
This dataset provides the Carbon Flux for Fires. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cmsfluxfossilfuelprior&quot;&gt;CMSFluxFossilFuelPrior&lt;/h4&gt;
This dataset provides the Carbon Flux for Fossil Fuel Prior. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cmsfluxoceanprior&quot;&gt;CMSFluxOceanPrior&lt;/h4&gt;
This dataset provides the Carbon Flux for Ocean Carbon Prior. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cmsfluxfossilfuelprior-1&quot;&gt;CMSFluxFossilFuelPrior&lt;/h4&gt;
This dataset provides the Prior for the Fossil Fuel Carbon Flux. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cmsfluxnbe&quot;&gt;CMSFluxNBE&lt;/h4&gt;
This dataset provides the Carbon Flux from the Net Biome Exchange. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cmsfluxnbeprior&quot;&gt;CMSFluxNBEPrior&lt;/h4&gt;
This dataset provides the Carbon Flux from the Net Biome Exchange Prior. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cmsfluxlandprior&quot;&gt;CMSFluxLandPrior&lt;/h4&gt;
This dataset provides the Prior for the Land Carbon Flux. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cmsfluxnbe-1&quot;&gt;CMSFluxNBE&lt;/h4&gt;
This dataset provides the Carbon Flux for Posterior Net Biome Exchange (NBE). The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cmsfluxocean&quot;&gt;CMSFluxOcean&lt;/h4&gt;
This dataset provides the Posterior Carbon Flux for the Ocean. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cmsfluxoceanprior-1&quot;&gt;CMSFluxOceanPrior&lt;/h4&gt;
This dataset provides the Prior for the Carbon Flux for Ocean. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cmsfluxtotal&quot;&gt;CMSFluxTotal&lt;/h4&gt;
This dataset provides the Carbon Flux for Posterior Total Carbon. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cmsfluxtotalprior&quot;&gt;CMSFluxTotalPrior&lt;/h4&gt;
This dataset provides the Prior for Total Carbon Flux. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cmsfluxfossilfuel&quot;&gt;CMSFluxFossilfuel&lt;/h4&gt;
This dataset provides the Carbon Flux for Fossil Fuel. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cmsfluxocean-1&quot;&gt;CMSFluxOcean&lt;/h4&gt;
This dataset provides the Carbon Flux for Ocean Carbon. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cmsfluxtotalprior-1&quot;&gt;CMSFluxTotalprior&lt;/h4&gt;
This dataset provides the Carbon Flux for Prior Total Carbon. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cmsfluxmisc&quot;&gt;CMSFluxMISC&lt;/h4&gt;
This dataset provides the Carbon Flux for Shipping, Aviation, and Chemical Sources. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cmsfluxnee&quot;&gt;CMSFluxNEE&lt;/h4&gt;
This dataset provides the Carbon Flux from the Net Ecosystem Exchange. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cmslakehuronppm&quot;&gt;CMSLakeHuronPPM&lt;/h4&gt;
Monthly Average primary production/carbon fixation data for Lake Huron. The primary production data is derived using MODIS imagery with model data. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cmslakehuronppy&quot;&gt;CMSLakeHuronPPY&lt;/h4&gt;
Yearly Average primary production/carbon fixation data for Lake Huron. The primary production data is derived using MODIS imagery with model data. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cmslakemichiganppm&quot;&gt;CMSLakeMichiganPPM&lt;/h4&gt;
Monthly Average primary production/carbon fixation data for Lake Michigan. The primary production data is derived using MODIS imagery with model data. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cmslakemichiganppy&quot;&gt;CMSLakeMichiganPPY&lt;/h4&gt;
Yearly Average primary production/carbon fixation data for Lake Michigan. The primary production data is derived using MODIS imagery with model data. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cmslakesuperiorppm&quot;&gt;CMSLakeSuperiorPPM&lt;/h4&gt;
Monthly Average primary production/carbon fixation data for Lake Superior. The primary production data is derived using MODIS imagery with model data. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cmslakesuperiorppy&quot;&gt;CMSLakeSuperiorPPY&lt;/h4&gt;
Yearly Average primary production/carbon fixation data for Lake Superior. The primary production data is derived using MODIS imagery with model data. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_conus_biomass_1752&quot;&gt;CMS_CONUS_Biomass_1752&lt;/h4&gt;
This dataset provides annual estimates of six carbon pools, including forest aboveground live biomass, belowground biomass, aboveground dead biomass, belowground dead biomass, litter, and soil organic matter, across the conterminous United States (CONUS) for 2005, 2010, 2015, 2016, and 2017. Carbon stocks were estimated using a modified MaxEnt model. Measurements of pixel-specific site conditions from remote sensing data were combined with field inventory data from the U.S. Forest Service Forest Inventory and Analysis (FIA). Remote sensing data inputs included Thematic Mapper on Landsat 5, Operational Land Imager on Landsat 8, Moderate Resolution Imaging Spectroradiometer (MODIS) on Aqua, microwave radar measurements from Phased Array type L-band Synthetic Aperture Radar (PALSAR) on Advanced Land Observation Satellite (ALOS) and PALSAR-2 ALOS-2, airborne imagery from National Agriculture Imagery Program (NAIP), and the digital elevation model from the Shuttle Radar Topography Mission (SRTM). Data from satellite and airborne sources were co-registered on a common 100 m (1 ha) grid.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_ctl_na_gosat_footprints&quot;&gt;CMS_CTL_NA_GOSAT_FOOTPRINTS&lt;/h4&gt;
This data set provides Weather Research and Forecasting (WRF) Stochastic Time-Inverted Lagrangian Transport (STILT) particle trajectory data products for particle receptors co-located with atmospheric column observations from the GOSAT satellite. Meteorological fields from the WRF model are used to drive STILT. STILT applies a Lagrangian particle dispersion model backwards in time from a measurement location (the &amp;quot;receptor&amp;quot; location), to create the adjoint of the transport model in the form of a &amp;quot;footprint&amp;quot; field. The footprint, with units of mixing ratio per surface flux, quantifies the influence of upwind surface fluxes on greenhouse gas concentrations measured at the receptor and is computed by counting the number of particles in a surface-influenced volume and the time spent in that volume. For each column observation location, the receptors are located at 23 discrete vertical levels throughout the atmospheric column. The CMS program is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System uses NASA observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS data products are designed to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_ctl_na_oco2_footprints&quot;&gt;CMS_CTL_NA_OCO2_FOOTPRINTS&lt;/h4&gt;
This data set provides Weather Research and Forecasting (WRF) Stochastic Time-Inverted Lagrangian Transport (STILT) particle trajectory data products for particle receptors co-located with atmospheric column observations from the OCO-2 satellite. Meteorological fields from the WRF model are used to drive STILT. STILT applies a Lagrangian particle dispersion model backwards in time from a measurement location (the &amp;quot;receptor&amp;quot; location), to create the adjoint of the transport model in the form of a &amp;quot;footprint&amp;quot; field. The footprint, with units of mixing ratio per surface flux, quantifies the influence of upwind surface fluxes on greenhouse gas concentrations measured at the receptor and is computed by counting the number of particles in a surface-influenced volume and the time spent in that volume. For each column observation location, the receptors are located at 14 discrete vertical levels throughout the atmospheric column. The CMS program is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System uses NASA observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS data products are designed to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_ctl_na_tccon_footprints&quot;&gt;CMS_CTL_NA_TCCON_FOOTPRINTS&lt;/h4&gt;
This data set provides Weather Research and Forecasting (WRF) Stochastic Time-Inverted Lagrangian Transport (STILT) particle trajectory data products for particle receptors co-located with atmospheric column observations from the TCCON ground network. Meteorological fields from the WRF model are used to drive STILT. STILT applies a Lagrangian particle dispersion model backwards in time from a measurement location (the &amp;quot;receptor&amp;quot; location), to create the adjoint of the transport model in the form of a &amp;quot;footprint&amp;quot; field. The footprint, with units of mixing ratio per surface flux, quantifies the influence of upwind surface fluxes on greenhouse gas concentrations measured at the receptor and is computed by counting the number of particles in a surface-influenced volume and the time spent in that volume. For each column observation location, the receptors are located at 23 discrete vertical levels throughout the atmospheric column. The CMS program is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System uses NASA observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS data products are designed to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_global_forest_age_2345&quot;&gt;CMS_Global_Forest_Age_2345&lt;/h4&gt;
This dataset provides classes of global forests delineated by status/condition in 2020 at approximately 30-m resolution. The data support generating Tier 1 estimates for Aboveground dry woody Biomass Density (AGBD) in natural forests in the 2019 Refinement to the 2006 IPCC Guidelines for National Greenhouse Gas Inventories. Forest classes include primary, young secondary (&amp;lt;&#x3D;20 years), and old secondary forests (&amp;gt;20 years). Classification was based on a Boolean combination of a suite of existing Earth Observation (EO) products of forest tree cover, height, age, and land use classification layers representing years 2000 to 2020. This forest status/condition classification prioritizes the reduction of potential errors of commission in the delineations by minimizing the inclusion of ambiguous pixels. Hence, it provides a conservative estimate of global forest area, identifying approximately 3.26 billion ha of forests worldwide. The classification was created on the collaborative open-science cloud-computing system, the ESA-NASA Multi-mission Analysis and Algorithm Platform (MAAP). The data are provided in cloud-optimized GeoTIFF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_simulated_sif_niwotridge_1720&quot;&gt;CMS_Simulated_SIF_NiwotRidge_1720&lt;/h4&gt;
This dataset provides results for simulations of solar-induced chlorophyll fluorescence (SIF) implemented within the terrestrial biosphere Community Land Model (CLM 4.5) for Niwot Ridge, Colorado, USA, from 1998-2018. The data include outputs from three model simulations designed to test the importance of non-photochemical quenching (NPQ), that is, the absorbed light energy dissipated as heat, in determining seasonal SIF.
&lt;br&gt;&lt;h4 id&#x3D;&quot;c_fluxstocks_clm5_dart_westus_1856&quot;&gt;C_FluxStocks_CLM5_DART_WestUS_1856&lt;/h4&gt;
This dataset provides monthly estimates of biomass stocks and land-atmosphere carbon exchange across the western United States at 0.95 degrees longitude x 1.25 degrees latitude grid resolution from 1998 through 2010. The data include outputs from two types of model simulations: (1) a &amp;quot;free&amp;quot; simulation which used Community Land Model (CLM5.0) simulations forced with meteorology appropriate for complex mountainous terrain, and (2) &amp;quot;assimilation&amp;quot; runs using the land surface data assimilation system (CLM5-DART). In assimilation runs, the CLM5 vegetation state is constrained by remotely sensed observations of leaf area index and aboveground biomass, which influenced biomass stocks and carbon fluxes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_go_ch4_sec_tdyc_na&quot;&gt;CMS_GO_CH4_SEC_TDYC_NA&lt;/h4&gt;
Methane emissions are provided by sector in the contiguous United States (CONUS), Canada, and Mexico by inverse analysis of in situ (GLOBALVIEWplus CH4ObsPack) and satellite (GOSAT) atmospheric methane observations. The inversion uses as a prior estimate the national anthropogenic emission inventories for the three countries reported by the US Environmental Protection Agency (EPA), En- vironment and Climate Change Canada (ECCC), and the Instituto Nacional de Ecología y Cambio Climático (INECC) in Mexico to the United Nations Framework Convention on Climate Change (UNFCCC) and thus serves as an evaluation of these inventories in terms of their magnitudes and trends. Emissions are optimized with a Gaussian mixture model (GMM).
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_fluxestimates_aircraft_co2_2336&quot;&gt;CMS_FluxEstimates_Aircraft_CO2_2336&lt;/h4&gt;
This dataset provides gridded surface-atmosphere CO2 fluxes over North America from April 8 to November 18 during 2018 and 2019. Net ecosystem exchange (NEE) was estimated by the CMS-Flux-NA CO2 inversion system by assimilating in situ CO2 measurements and/or Orbiting Carbon Observatory (OCO-2) column-averaged CO2 retrievals. These data, along with imposed diurnal NEE variations, fossil fuel emissions, biomass burning, and biofuel emissions, are provided at 3-hour temporal resolution. The modeled co-samples of CO2 observed for aircraft flights are included for model evaluation. The data are provided in NetCDF version 4 format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_mangrove_biomass_zambezi_1522&quot;&gt;CMS_Mangrove_Biomass_Zambezi_1522&lt;/h4&gt;
This dataset provides several estimates of aboveground biomass from various regressions and allometries for mangrove forest in the Zambezi River Delta, Mozambique. Plot level estimates of aboveground biomass are based on extensive tree biophysical measurements from field campaigns conducted in September and October of 2012 and 2013. Aboveground biomass estimates for the larger area of mangrove coverage within the delta are based on (1) the plot level data and (2) canopy structure data derived from airborne LiDAR surveys in 2014. The high-resolution canopy height model for the delta region derived from the airborne LiDAR data is also included.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_lidar_agb_pef_2012_1318&quot;&gt;CMS_LiDAR_AGB_PEF_2012_1318&lt;/h4&gt;
This data set includes estimates of aboveground biomass (AGB) in 2012 from the Penobscot Experimental Forest (PEF) in Bradley, Maine. The AGB was modeled using LiDAR data gathered with the LiDAR Hyperspectral and Thermal Imager (G-LiHT) operated by Goddard Space Flight Center and field inventory data from 604 permanent Forest Inventory and Analysis (FIA) plots within the PEF. The estimates were produced through a novel modeling approach that accommodates temporal misalignment between field measurements and remotely sensed data by including multiple time-indexed measurements at plot locations to estimate changes in AGB.
&lt;br&gt;&lt;h4 id&#x3D;&quot;global_riverine_n2o_emissions_1791&quot;&gt;Global_Riverine_N2O_Emissions_1791&lt;/h4&gt;
This dataset provides modeled estimates of annual nitrous oxide (N2O) emissions at a coarse geographic scale (0.5 x 0.5 degree) for two sets of global rivers and streams covering the period of 1900-2016. Emissions (g N2O-N/yr) are provided for higher-order rivers and streams (&amp;gt;&#x3D;4th order) and headwater streams (&amp;lt;4th order). The estimates were derived from a water transport model, the Model for Scale Adaptive River Transport (MOSART), coupled with the Dynamic Land Ecosystem Model (DLEM) to link hydrology and ecosystem processes pertaining to N2O flux and transport. Factors driving the model included climate, land use and land cover, and nitrogen inputs (i.e., fertilizer, deposition, manure, and sewage). Nitrogen discharges from streams and rivers to the ocean were calibrated from observations from 50 river basins across the globe.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atmospheric_co2_california_1641&quot;&gt;Atmospheric_CO2_California_1641&lt;/h4&gt;
This dataset provides measurements of atmospheric CO2 concentrations, carbon isotopes d13C and D14C, and fossil fuel CO2 (ffCO2) estimates from nine observation sites in California over three month-long campaigns in separate seasons of 2014-2015. ffCO2 was quantified based on the CO2 concentration and D14C. Simulations of ffCO2 at the sites and times of the observations were conducted with the Vulcan v2.2 fossil fuel emissions estimate for 2002 and the Weather Research and Forecasting - Stochastic Time-Inverted Lagrangian Transport (WRF-STILT) atmospheric model. The observed and simulated ffCO2 were incorporated into Bayesian inverse estimates of ffCO2 to calculate California&amp;#39;s ffCO2 emissions during the campaign period.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_methane_emissions_boston_1291&quot;&gt;CMS_Methane_Emissions_Boston_1291&lt;/h4&gt;
This data set provides average hourly measured, modeled enhancements, and background methane (CH4) concentrations, atmospheric ethane (C2H6) measurements, prior CH4 flux fields by sector, and a spatial reconstruction of natural gas (NG) consumption in Boston, Massachusetts and the surrounding region. Atmospheric CH4 concentrations were measured continuously from September 2012 through August 2013 at four locations and atmospheric ethane was measured continuously for several months during 2012-2014 at one location. Spatial models of prior CH4 emissions and natural gas consumption are given for an ~18,000 km^2 area centered on Boston, MA.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_global_cropland_carbon_1279&quot;&gt;CMS_Global_Cropland_Carbon_1279&lt;/h4&gt;
This data set provides global estimates of carbon fluxes associate with annual crop net primary production (NPP) and harvested biomass, annual uptake and release by humans and livestock, and the total annual estimate of net carbon exchange (NCE) derived from these carbon fluxes. NCE estimates are for the combined crop plant harvest and consumption/expiration of fodder by livestock and of food by humans. Estimation of carbon uptake and release from global agricultural production and consumption required compilation and analysis of inventory data from various sources for the years 2005-2011. The flux estimates were spatially distributed to a global 0.05-degree resolution grid using MODIS land cover data. The quantities of carbon flux in each gridcell are represented in two ways: (1) where the quantities of carbon distributed to each gridcell were divided by the total gridcell area, resulting in average carbon fluxes per unit of total area (g C/m2/yr), and (2), where annual carbon fluxes associated with a source were summed over all types for the gridcell (Mg C/yr). The total surface area of the grid cells is provided. There are eight data files in netCDF format (.nc4) with this data set -- two files (per area and per gridcell) for each of the four flux source types. Data for all years are in each .nc4 file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_wrf_footprints_co2_signals_1381&quot;&gt;CMS_WRF_Footprints_CO2_Signals_1381&lt;/h4&gt;
This data set provides estimated CO2 emission signals for 16 regions (air quality basins) in California, USA, during the individual months of November 2010 and May 2011. The CO2 signals were predicted from simulated atmospheric CO2 observations and modeled fossil fuel emissions and biosphere CO2 fluxes. Data is also provided for the land surface in the larger modeling domain outside California. CO2 signals refer to the local enhancement or depletion in atmospheric CO2 concentration caused by fossil fuel emissions or biospheric exchange occurring within the region.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpp_conus_tropomi_1875&quot;&gt;GPP_CONUS_TROPOMI_1875&lt;/h4&gt;
This dataset includes estimates of gross primary production (GPP) for the conterminous U.S., for 2018-02-15 to 2021-10-15, based on measurements of solar-induced chlorophyll fluorescence from the TROPOspheric Monitoring Instrument (TROPOMI) on the Sentinel-5P satellite platform. GPP was estimated from rates of photosynthesis inferred from SIF using a linear model and ecosystem scaling factors from 102 AmeriFlux sites. Knowledge of the spatiotemporal patterns of GPP is necessary for understanding regional and global carbon budgets. Broad-scale estimates of GPP have typically relied upon carbon cycle models linking spatial patterns of vegetation with remotely sensed environmental data. SIF provides a means to directly estimate photosynthetic activity, and therefore, GPP. Recent deployments of satellite platforms that measure SIF provide near-real-time measurements and represent a breakthrough in measuring GPP on a global scale. Regular SIF measurements can detect spatially explicit ecosystem-level responses to climate events such as drought and flooding. This dataset includes spatially explicit estimates of GPP (g m-2 d-1), uncertainty in GPP, and related TROPOMI SIF measurements (mW m-2 sr-1 nm-1) at 500-m resolution. The data are provided in NetCDF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_pantropical_forest_biomass_1337&quot;&gt;CMS_Pantropical_Forest_Biomass_1337&lt;/h4&gt;
This data set provides estimates of pre-deforestation aboveground live woody biomass (AGLB) at 30-m resolution for deforested areas of tropical America, tropical Africa, and tropical Asia for the year 2000. The biomass estimates are only for areas where deforestation occurred during the period 2000 through 2012. These estimates represent biomass loss over this time period and can be used to derive average annual carbon emissions from tropical deforestation.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_daily_et_mexflux_1309&quot;&gt;CMS_Daily_ET_MexFlux_1309&lt;/h4&gt;
This data set provides daily average observations for evapotranspiration (measured and gap-filled), precipitation, net radiation, soil water content, air temperature, vapor pressure deficit, and normalized vegetation index (NDVI) from two water-limited shrubland sites for years 2008-2010. Both sites are located in the northwest part of Mexico and are part of the MexFlux network.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_fire_weather_data_ak_1509&quot;&gt;CMS_Fire_Weather_Data_AK_1509&lt;/h4&gt;
This dataset provides daily fire weather indices for interior Alaska during the active fire seasons from 2001 to 2010. Data are gridded at 60-m resolution. The active fire season is defined as May 24-September 18 (days of the year 144-261) in this dataset. Fire weather is the use of meteorological parameters such as relative humidity, wind speed and direction, cloud cover, mixing heights, and soil moisture to determine whether conditions are favorable for fire growth and smoke dispersion. The six indices provided in this dataset are defined and produced following the methodology of the Canadian Forest Fire Weather Index System: Fine Fuel Moisture Code, Duff Moisture Code, Drought Code, Initial Spread Index, Buildup Index, Fire Weather Index. The dataset was developed following point source data interpolation from weather station observations.
&lt;br&gt;&lt;h4 id&#x3D;&quot;fia_forest_biomass_estimates_1873&quot;&gt;FIA_Forest_Biomass_Estimates_1873&lt;/h4&gt;
This dataset provides forest biomass estimates for the conterminous United States based on data from the USDA Forest Inventory and Analysis (FIA) program. FIA maintains uniformly measured field plots across the conterminous U.S. This dataset, derived from field survey data from 2009-2019, includes statistical estimates of biomass at the finest scale (64,000-hectare hexagons) allowed by FIA&amp;#39;s sample density. Estimates include the mean (and standard error of the mean) biomass for both live and dead trees, calculated using three sets of allometric equations. There is also an estimate of the area of forestland in each hexagon. These data can be useful for assessing the accuracy of remotely sensed biomass estimates.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_forest_productivity_1221&quot;&gt;CMS_Forest_Productivity_1221&lt;/h4&gt;
Notice: This data set and guide were updated on June 30, 2014 to correct an error in the reported units. The data values were not changed.Spatially-gridded estimates of above ground biomass (AGB), net primary productivity (NPP), and net ecosystem productivity (NEP) are provided for forested areas of the conterminous United States (CONUS). Estimates of uncertainty are also provided for AGB and NEP. These data were derived by using Forest Inventory and Analysis (FIA) data to constrain forest growth rates in a Carnegie-Ames-Stanford Approach (CASA) carbon-cycle process model. Note that the data set does not include data for forests in the Northern Prairie States region (NPS; see Figure 3). These data provide a detailed estimate of carbon sources and sinks from recent forest disturbance and recovery across regions and forest types of the US. The data are presented as a series of ten NetCDF v4 (.nc4) files at two spatial scales (1-degree and 5-km spatial resolution) for the nominal year of 2005.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_forest_carbon_fluxes_1313&quot;&gt;CMS_Forest_Carbon_Fluxes_1313&lt;/h4&gt;
This data set provides maps of estimated carbon in forests of the 48 continental states of the US for the years 2005-2010. Carbon (termed committed carbon) stocks were estimated for forest aboveground biomass, belowground biomass, standing dead stems, and litter for the year 2005. Carbon emissions were estimated from land use conversion to agriculture, insect damage, logging, wind, and weather events in the forests for the years 2006 - 2010. Committed net carbon flux was estimated as the sum of carbon emissions and sequestration. The maps are provided at 100-m spatial resolution in GeoTIFF format. Average annual carbon estimates, by US county, for (1) emissions for the multiple disturbance sources, (2) sequestration, and (3) the committed net carbon flux are provided in an ESRI shapefile.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_landscapes_brazil_forests_1301&quot;&gt;CMS_Landscapes_Brazil_Forests_1301&lt;/h4&gt;
This data set provides measurements for diameter at breast height (DBH), commercial tree height, and total tree height for forest inventories taken at the Fazenda Cauaxi and the Fazenda Nova Neonita, Paragominas municipality, Para, Brazil. Also included for each tree are the common, family, and scientific name, coordinates, canopy position, crown radius, and for dead trees the decomposition status. These biophysical measurements were made at Fazenda Cauaxi during 2012 and 2014 and at the Fazenda Nova Neonita during 2013.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lidar_forest_canopy_heights_1271&quot;&gt;LIDAR_FOREST_CANOPY_HEIGHTS_1271&lt;/h4&gt;
This data set provides estimates of forest canopy height derived from the Geoscience Laser Altimeter System (GLAS) LiDAR instrument that was aboard the NASA Ice, Cloud, and land Elevation (ICESat) satellite. A global GLAS waveform data set (n&#x3D;12,336,553) from collection periods between October 2004 and March 2008 was processed to obtain canopy height estimates. Estimates of GLAS maximum canopy height and crown-area-weighted Lorey&amp;#39;s height are provided for 18,578 statistically-selected globally distributed forested sites in a point shapefile. Country is included as a site attribute. Also provided is the average canopy height for the forested area of each country, plus the number of GLAS data footprints (shots), number of selected sample sites, and estimates of the variance for each country.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_global_monthly_wetland_ch4_1502&quot;&gt;CMS_Global_Monthly_Wetland_CH4_1502&lt;/h4&gt;
This data set provides global monthly wetland methane (CH4) emissions and uncertainty data products derived from an ensemble of multiple terrestrial biosphere models, wetland extent scenarios, and CH4:C temperature dependencies. The data are at 0.5 by 0.5-degree resolution. Two model output data products are included in WetCHARTs v1.0: an output from the full ensemble for 2009-2010 and an output from a limited subset for 2001-2015. The intended use of the products is as a process-informed wetland CH4 emission and uncertainty data set for atmospheric chemistry and transport modelling (WetCHARTs).
&lt;br&gt;&lt;h4 id&#x3D;&quot;monthlywetland_ch4_wetchartsv2_2346&quot;&gt;MonthlyWetland_CH4_WetCHARTsV2_2346&lt;/h4&gt;
This dataset provides global monthly wetland methane (CH4) emissions estimates at 0.5 by 0.5-degree resolution for the period 2001-01-01 to 2022-08-31 that were derived from an ensemble of multiple terrestrial biosphere models, wetland extent scenarios, and CH4:C temperature dependencies that encompass the main sources of uncertainty in wetland CH4 emissions. There are 18 model configurations. WetCHARTs v1.3.3 is an updated product of WetCHARTs v1.3.1 dataset. The intended use of this product is as a process-informed wetland CH4 emission data set for atmospheric chemistry and transport modeling. Users can compare estimates by model configuration to explore variability and sensitivity with respect to ensemble members. The data are provided in netCDF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_global_livestock_ch4_co2_1329&quot;&gt;CMS_Global_Livestock_CH4_CO2_1329&lt;/h4&gt;
This data set provides global annual carbon flux estimates, at 0.05-degree resolution, associated with livestock feed intake, manure, manure management, respiration, and enteric fermentation, summed over all livestock types. These fluxes can be summed across multiple grid cells to obtain totals for any given areas. These 2000-2013 flux estimates were based on livestock populations reported by the Food and Agriculture Organization (FAO) and the United States Department of Agriculture National Agricultural Statistics Service (USDA NASS), on coefficients provided by the Intergovernmental Panel on Climate Change (IPCC), and on additional coefficients developed by the authors.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_global_mangrove_forest_ht_2251&quot;&gt;CMS_Global_Mangrove_Forest_Ht_2251&lt;/h4&gt;
This dataset characterizes canopy heights of mangrove-forested wetlands globally for 2015 at 12-m resolution. Estimates of maximum canopy height (height of the tallest tree) were derived from the German Space Agency&amp;#39;s TanDEM-X data that produced global digital surface models. Also provided are Lidar estimates of canopy height based on the GEDI instrument, which were used for training and validation of the TanDEM-X estimates of forest height. The coverage of these data follows Global Mangrove Watch&amp;#39;s mangrove extent maps. These spatially explicit maps of mangrove canopy height can be used to assess local-scale geophysical and environmental conditions that may regulate forest structure and carbon cycle dynamics. Maps revealed a wide range of canopy heights, including maximum values (&amp;gt;60 m) that surpass maximum heights of other forest types. Maps are provided in cloud optimized GeoTIFF format, and mangrove heights for individual GEDI tiles are compiled in a comma separated values (CSV) files.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_wrf_model_products_1338&quot;&gt;CMS_WRF_Model_Products_1338&lt;/h4&gt;
This data set contains estimated hourly CO2 atmospheric mole fractions and meteorological observations over North America for the year 2010 at a horizontal grid resolution of 27 km and vertical resolution from the surface to 50 hPa. The data are output from the Penn State WRF-Chem version of the Weather Research and Forecasting (WRF) model using lateral boundary conditions and surface fluxes from the CMS-Flux Inversion system.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gcam_land_cover_2005-2095_1216&quot;&gt;GCAM_Land_Cover_2005-2095_1216&lt;/h4&gt;
The data provided are annual land cover projections for years 2005 through 2095 generated by the Global Change Assessment Model (GCAM) Version 3.1. For the conterminous USA, the GCAM global gridded results were downscaled to &lt;del&gt;5.6 km (0.05 degree) resolution. For each 5.6 x 5.6 km area, the annual land cover percentage comprised by each of the nineteen different land cover classes/plant functional types (PFTs) of the Community Land Model (CLM) (Table 1) are provided. Results are reported for GCAM runs of three scenarios of future human efforts towards climate mitigation as related to global carbon emissions, radiative forcing, and land cover change. Specific scenario conditions were 1) a reference scenario with no explicit climate mitigation efforts that reaches a radiative forcing level of over 7 W/m2 in 2100, 2) the 2.6 mitigation pathway (MP) scenario which is a very low emission scenario with a mid-century peak in radiative forcing at ~3 W/m2, declining to 2.6 W/m2 in 2100, and 3) the 4.5 MP scenario which stabilizes radiative forcing at 4.5 W/m2 (&lt;/del&gt; 650 ppm CO2-equivalent) before 2100. These downscaled land cover projections can be used to derive spatially explicit estimates of potential shifts in croplands, grasslands, shrub lands, and forest lands in each future climate scenario. Data are presented as three NetCDF v4 files (.nc4), one for each future climate scenario -- 2.6 MP, 4.5 MP, and GCAM reference).
&lt;br&gt;&lt;h4 id&#x3D;&quot;landcover_colombian_amazon_1783&quot;&gt;Landcover_Colombian_Amazon_1783&lt;/h4&gt;
This dataset provides annual maps of land cover classes for the Colombian Amazon from 2001 through 2016 that were created by classifying time segments detected by the Continuous Change Detection and Classification (CCDC) algorithm. The CCDC algorithm detected changes in Landsat pixel surface reflectance across the time series, and the time segments were classified into land cover types using a Random Forest classifier and manually collected training data. Annual maps of land cover were created for each Landsat scene and then post-processed and mosaicked. Land cover types include unclassified, forest, natural grasslands, urban, pastures, secondary forest, water, or highly reflective surfaces. The training data are not included with this dataset.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sonoma_county_forest_agb_1764&quot;&gt;Sonoma_County_Forest_AGB_1764&lt;/h4&gt;
This data set provides estimates of above-ground woody biomass and uncertainty at 30-m spatial resolution for Sonoma County, California, USA, for the nominal year 2013. Biomass estimates, megagrams of biomass per hectare (Mg/ha), were generated using a combination of airborne LiDAR data and field plot measurements with a parametric modeling approach. The relationship between field estimated and airborne LiDAR estimated aboveground biomass density is represented as a parametric model that predicts biomass as a function of canopy cover and 50th percentile and 90th percentile LiDAR heights at a 30-m resolution. To estimate uncertainty, the biomass model was re-fit 1,000 times through a sampling of the variance-covariance matrix of the fitted parametric model. This produced 1,000 estimates of biomass per pixel. The 5th and 95th percentiles, and the standard deviation of these pixel biomass estimates, were calculated.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_landscapes_brazil_lidar_1302&quot;&gt;CMS_Landscapes_Brazil_LiDAR_1302&lt;/h4&gt;
This data set provides raw LiDAR point cloud data and derived Digital Terrain Models (DTMs) for five forested areas in the municipality of Paragominas, Para, Brazil, for the years 2012, 2013, and 2014. Data are included for two areas in Paragominas for 2013 and 2014, two areas for the Fazenda Cauaxi for 2012 and 2014, and for the Fazenda Andiroba for 2014. Shapefiles showing the LiDAR/DTM coverage areas are also provided for each of the areas.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_lidar_indonesia_1518&quot;&gt;CMS_LiDAR_Indonesia_1518&lt;/h4&gt;
This dataset provides airborne LiDAR data collected over 90 sites totaling approximately 100,000 hectares of forested land in Kalimantan, Indonesia on the island of Borneo in late 2014. The data were collected as part of an effort to establish a national forest monitoring system for Indonesia that uses a combination of remote sensing and ground-based forest carbon inventory approaches.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_lidar_point_cloud_zambezi_1521&quot;&gt;CMS_LiDAR_Point_Cloud_Zambezi_1521&lt;/h4&gt;
This data set provides high-resolution LiDAR point cloud data collected during surveys over mangrove forests in the Zambezi River Delta in Mozambique in May 2014. The data are arranged into 144 1- by 1-km tiles.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_maryland_agb_canopy_1320&quot;&gt;CMS_Maryland_AGB_Canopy_1320&lt;/h4&gt;
This data set provides 30-meter gridded estimates of aboveground biomass (AGB), canopy height, and canopy coverage for the state of Maryland in 2011. Leaf-off LiDAR data were combined with high-resolution leaf-on agricultural imagery to select 848 field sampling sites for biomass measurements. The field-based estimates were related to LiDAR height and volume metrics through random forests regression models across three physiographic regions of Maryland.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_lidar_biomass_canht_sonoma_1523&quot;&gt;CMS_LiDAR_Biomass_CanHt_Sonoma_1523&lt;/h4&gt;
This data set provides estimates of above-ground biomass (AGB), canopy height, and percent tree cover at 30-m spatial resolution for Sonoma County, California, USA, for the nominal year 2013. Biomass estimates, megagrams of biomass per hectare (Mg/ha) were generated using a combination of LiDAR data, field plot measurements, and random forest modeling approaches. Estimates of AGB uncertainty are also provided. Maximum canopy height and tree cover were derived from LiDAR data and high-resolution National Agriculture Imagery Program (NAIP) images.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_lidar_products_indonesia_1540&quot;&gt;CMS_LiDAR_Products_Indonesia_1540&lt;/h4&gt;
This dataset provides canopy height and elevation data products derived from airborne LiDAR data collected over 90 sites on the island of Borneo in late 2014. The sites cover approximately 100,000 hectares of forested land in Kalimantan, Indonesia. The data were produced as part of an effort to improve a national forest monitoring system for Indonesia that uses a combination of remote sensing and ground-based forest carbon inventory approaches.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_pilot_biomass_1257&quot;&gt;CMS_Pilot_Biomass_1257&lt;/h4&gt;
These data consist of high-resolution maps of aboveground biomass at four forested sites in the US: Garcia River Tract in California, Anne Arundel and Howard Counties in Maryland, Parker Tract in North Carolina, and Hubbard Brook Experimental Forest in New Hampshire. Biomass maps were generated using a combination of field data (forest inventory and Lidar) and modeling approaches. Estimates of uncertainty are also provided for the Maryland site using two different modeling methodologies. These data provide estimates of aboveground biomass for the nominal year of 2011 at 20-50 meter resolution in units of megagrams of carbon per hectare (or acre for the Garcia Tract site). The data are presented as a series of 11 GeoTIFF (.tif) files.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_pennsylvania_tree_cover_1334&quot;&gt;CMS_Pennsylvania_Tree_Cover_1334&lt;/h4&gt;
This data set provides high-resolution (1-m) tree canopy cover for states in the Northeast USA. State-level canopy cover data are currently available for Pennsylvania (data for nominal year 2008), Delaware (2014), and Maryland (2013). The data were derived with a rules-based expert system which facilitated integration of leaf-on LiDAR and imagery data into a single classification workflow, exploiting the spectral, height, and spatial information contained in the datasets. Additional states will be added as data processing is completed.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_mangrove_canht_stand_age_1377&quot;&gt;CMS_Mangrove_CanHt_Stand_Age_1377&lt;/h4&gt;
This data set provides canopy height, land cover change, and stand age estimates for mangrove forests in the Rufiji River Delta in Tanzania. The estimates were derived from a canopy height model (CHM) using TanDEM-X imagery and Polarimetric SAR interferometry (Pol-InSAR) techniques. Landsat imagery circa 1990 and circa 2014 was used to estimate stand age between 1994 and 2014 and for forest land cover change modeling.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_mangrove_canopy_ht_zambezi_1357&quot;&gt;CMS_Mangrove_Canopy_Ht_Zambezi_1357&lt;/h4&gt;
This data set provides high resolution canopy height estimates for mangrove forests in the Zambezi Delta, Mozambique, Africa. The estimates were derived from three separate canopy height models (CHM) using airborne Lidar data, stereophotogrammetry with WorldView 1 imagery, and Interferometric-Synthetic Aperture Radar (In-SAR) techniques with TanDEM-X imagery. The data cover the period 2011-10-14 to 2014-05-06.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_mangrove_canopy_height_1327&quot;&gt;CMS_Mangrove_Canopy_Height_1327&lt;/h4&gt;
This data set provides canopy height estimates for mangrove forests at 0.6 x 0.6 m resolution in three study sites located in southeastern Mozambique, Africa: two sites on Inhaca Island and one in the Maputo Elephant Reserve, located in the southern province of Maputo for September, 2012. The estimates were derived from WorldView1 (WV-1) very high resolution (VHR) stereo images processed using the Ames Stereo Pipeline (ASP) digital surface model (DSM) tool.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_mangrove_cover_1670&quot;&gt;CMS_Mangrove_Cover_1670&lt;/h4&gt;
This dataset provides estimates of mangrove extent for 2016, and mangrove change (gain or loss) from 2000 to 2016, in major river delta regions of eight countries: Bangladesh, Gabon, Jamaica, Mozambique, Peru, Senegal, Tanzania, and Vietnam. For mangrove extent, a combination of Landsat 8 OLI, Sentinel-1 C-SAR, and Shuttle Radar Topography Mission (SRTM) elevation data were used to create country-wide maps of mangrove landcover extent at a 30-m resolution. For mangrove change, the global mangrove map for 2000 (Giri et al., 2010) was used as the baseline. Normalized Difference Vegetation Indices (NDVI) were calculated for every cloud- and shadow-free pixel in the Landsat 5 TM, Landsat 7 ETM+, and Landsat 8 OLI collection and used to create an NDVI anomaly from 2000 to 2016. Areas of change (loss or gain) occurred at the extremes of the cumulative anomalies.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_co2_fluxes_tbmo_1315&quot;&gt;CMS_CO2_Fluxes_TBMO_1315&lt;/h4&gt;
This data set provides global, gridded, model-derived net ecosystem exchange (NEE) of CO2 flux between the land and atmosphere at 3-hourly time steps over seven years (2004-2010) at three different spatial resolutions: 0.5 x 0.5 degree, 2.0 x 2.5 degrees, and 4.0 x 5.0 degrees (latitude/longitude). The 3-hourly data were derived from monthly NEE outputs of 15 global land surface models and four ensemble products in the Multi-scale Synthesis and Terrestrial Model Intercomparison Project (MsTMIP).
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_sst_gpp_mexico_1310&quot;&gt;CMS_SST_GPP_Mexico_1310&lt;/h4&gt;
This data set provides data for MODIS-derived (1) gross primary productivity (GPP) for the years 2000-2010, (2) fraction of photosynthetically active radiation (fPAR) for the years 2003-2013, (3) sea surface temperature (SST) for the years 2003-2013, and (4) the NOAA-source Multivariate ENSO Index (MEI) data for the years 2003-2013 (as a measure of the El Nino/Southern Oscillation). The study areas were three transects on the Baja California Peninsula, Mexico, and the adjacent Pacific Ocean. The terrestrial transects, in order from North to South, West to East included Punta Colonet (three sites-PC1, PC2, PC3), Punta Abreojos (two sites-PA1, PA2), and Magdalena Bay (three sites-MB1, MB2, MB3).
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_great_basin_biomass_1755&quot;&gt;CMS_Great_Basin_Biomass_1755&lt;/h4&gt;
This dataset provides annual maps of live aboveground tree biomass (Mg/ha) for pinyon-juniper forests across the Great Basin of the Western USA for the years 2000-2016 at a spatial resolution of 30 meters. Biomass estimates are limited to areas of the Great Basin defined as a pinyon-juniper ecosystem type by the 2016 Landfire Existing Vegetation Type map. The estimates of biomass were based on a linear relationship with pinyon-juniper canopy cover and crown-based allometrics developed from field data in Nevada and Idaho. Canopy cover was estimated from remote sensing by using annual composites of Landsat imagery, which were temporally segmented with the LandTrendr algorithm, along with biologically-relevant climate variables, and topographic indices in a Random Forest regression model. Models of canopy cover were trained from semi-automatic extraction of tree crowns from 2011 - 2013 high resolution imagery (1 m) from the National Agriculture Imagery Program, which were validated with photo interpretation. Maps of the standard deviation of biomass estimates from decision trees in the Random Forest model are provided as an indicator of uncertainty. Biomass estimates were calibrated to estimates from the Forest Inventory and Analysis program (FIA) on an annual basis and corrections applied.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_sabgom_model_simulations_1510&quot;&gt;CMS_SABGOM_Model_Simulations_1510&lt;/h4&gt;
This dataset contains monthly mean ocean surface physical and biogeochemical data for the Gulf of America simulated by the South Atlantic Bight and Gulf of America (SABGOM) model on a 5-km grid from 2005 to 2010. The simulated data include ocean surface salinity, temperature, dissolved inorganic nitrogen (DIN), dissolved inorganic carbon (DIC), partial pressure of CO2 (pCO2), air-sea CO2 flux, surface currents, and primary production. The SABGOM model is a coupled physical-biogeochemical model for studying circulation and biochemical cycling for the entire Gulf of America to achieve an improved understanding of marine ecosystem variations and their relations with three-dimensional ocean circulation in a gulf-wide context.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_soil_co2_efflux_1298&quot;&gt;CMS_Soil_CO2_Efflux_1298&lt;/h4&gt;
This data set provides the results of (1) monthly measurements of soil CO2 efflux, volumetric water content, and temperature, and (2) seasonal measurements of soil (porosity, bulk density, nitrogen (N) and carbon (C) content) and vegetation (leaf area index (LAI), litter and fine root biomass) properties in a water-limited ecosystem in Baja California, Mexico. Measurements and samples were collected from August 2011 to August 2012.
&lt;br&gt;&lt;h4 id&#x3D;&quot;c_pools_fluxes_conus_1837&quot;&gt;C_Pools_Fluxes_CONUS_1837&lt;/h4&gt;
This dataset provides estimates of carbon pools, fluxes, and associated uncertainties across the contiguous USA (CONUS) at 0.5-degree resolution for all terrestrial land cover types. Carbon pools include labile carbon, foliar carbon, fine root, woody carbon, litter carbon, and soil organic carbon. Carbon fluxes include gross primary production (GPP), net primary production (NPP), net biome exchange, autotrophic respiration, and heterotrophic respiration. The modeled estimates are provided as monthly averages over the 16-year period, 2001 through 2016. The data were derived from the CARbon DAta MOdel fraMework (CARDAMOM) that included climate data, and above and below ground biomass maps of CONUS for the years 2005, 2010, 2015 and 2016 as input data sources to this model-data fusion framework. The input data were integrated into the CARDAMOM model to constrain on the terrestrial carbon and to specifically attribute changes of forest carbon stocks and spatial distributions of carbon emissions and removals across forested lands. United States Forest Service&amp;#39;s Forest Inventory and Analysis (FIA) plot data were used to train models for the prediction of forest above-ground biomass (AGB).
&lt;br&gt;&lt;h4 id&#x3D;&quot;vermont_highres_landcover_2072&quot;&gt;Vermont_HighRes_LandCover_2072&lt;/h4&gt;
This dataset contains estimates of tree canopy cover presence at high resolution (0.5m) across the state of Vermont for 2016 in Cloud-Optimized GeoTIFF (.tif) format. Tree canopy was derived from 2016 high-resolution remotely sensed data as part of the Vermont High-Resolution Land Cover mapping project. Object-based image analysis techniques (OBIA) were employed to extract potential tree canopy and trees using the best available remotely sensed and vector GIS datasets. OBIA systems work by grouping pixels into meaningful objects based on their spectral and spatial properties, while taking into account boundaries imposed by existing vector datasets. Within the OBIA environment a rule-based expert system was designed to effectively mimic the process of manual image analysis by incorporating the elements of image interpretation (color/tone, texture, pattern, location, size, and shape) into the classification process. A series of morphological procedures were employed to ensure that the end product is both accurate and cartographically pleasing. Following the automated OBIA mapping a detailed manual review of the dataset was carried out at a scale of 1:3000 and all observable errors were corrected. Tree canopy assessments have been conducted for numerous communities throughout the U.S. where the results have been instrumental in helping to establish tree canopy goals.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tree_canopy_cover_mexico_v2_2445&quot;&gt;Tree_Canopy_Cover_Mexico_V2_2445&lt;/h4&gt;
This dataset provides 20-year tree cover (TC) estimates at 30-m spatial resolution for Mexico from 2000 to 2019 using Landsat time series, airborne LiDAR, and machine learning. The TC data (hereafter, CMS-TC) offers accurate and consistent national-scale percent tree cover estimates with an overall coefficient of determination (R squared) of 0.81 and a root mean square error (RMSE) of 11.90%. The CMS-TC product is essential for tracking tree cover and aboveground biomass changes, monitoring land use dynamics, supporting biodiversity conservation, and informing climate and land use policy decisions. The data are provided in GeoTIFF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;continuous_lifeform_maps_conus_1809&quot;&gt;Continuous_Lifeform_Maps_CONUS_1809&lt;/h4&gt;
This dataset contains estimates of percent cover of tree, shrub, herb, and other (non-vegetation) lifeform classes and uncertainties for the conterminous U.S. (CONUS). The estimates were derived using quantile regression forest models and indicate the percent of ground covered by a vertical projection of each lifeform class ranging from 0 to 100 percent. Model input data included Landsat surface reflectance (SR) data and 165 airborne LiDAR datasets covering eight of the eleven terrestrial biomes of the conterminous U.S. and Alaska. Eighty-six of the LiDAR acquisitions are part of the NASA Goddard&amp;#39;s LiDAR, Hyperspectral, and Thermal Imager (G-LiHT) airborne imager data collection; the remaining 79 sites were acquired by the National Science Foundation&amp;#39;s National Ecological Observatory Network Airborne Observation Platform (NEON AOP). Acquisitions were selected based on the availability of the SR data for each G-LiHT and NEON dataset. The data are annual estimates from 1984 to 2018 and were tiled (425 tiles) using the CONUS Landsat Analysis Ready Data (ARD) grid scheme. Data are provided in GeoTIFF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;uncertainty_us_coastal_ghg_1650&quot;&gt;Uncertainty_US_Coastal_GHG_1650&lt;/h4&gt;
This dataset provides maps of coastal wetland carbon and methane fluxes and coastal wetland surface elevation from 2006 to 2011 at 30 m resolution for coastal wetlands of the conterminous United States. Total coastal wetland carbon flux per year per pixel was calculated by combining maps of wetland type and change with soil, biomass, and methane flux data from a literature review. Uncertainty in carbon flux was estimated from 10,000 iterations of a Monte Carlo analysis. In addition to the uncertainty analysis, this dataset also provides a probabilistic map of the extent of tidal elevation, as well as the geospatial files used to create that surface, and a land cover and land cover change map of the coastal zone from 2006 to 2011 with accompanying estimated median soil, biomass, methane, and total CO2 equivalent annual fluxes, each with reported 95% confidence intervals, at 30 m resolution. Land cover was quantified using the Coastal Change Analysis Program (C-CAP), a Landsat-based land cover mapping product.
&lt;br&gt;&lt;h4 id&#x3D;&quot;niwot_ridge_cnpam_fluorescence_1722&quot;&gt;Niwot_Ridge_CNPAM_Fluorescence_1722&lt;/h4&gt;
This dataset provides chlorophyll fluorescence measurements made on pine and spruce needle tissues at the Niwot Ridge AmeriFlux Core site (US-NR1) near Nederland, Colorado, USA, during the summers of 2017 and 2018. Two types of measurements were made using pulse-amplitude-modulation (PAM) fluorometry: the photosystem II (PSII) operating efficiency in the light (Fq&amp;#39;/Fm&amp;#39; at variable light levels), and the maximum quantum efficiency of PSII photochemistry (Fv/Fm) on dark-acclimated tissues. Chlorophyll fluorescence measurements were made to determine seasonality of photosynthetic performance at the needle level.
&lt;br&gt;&lt;h4 id&#x3D;&quot;niwot_ridge_pigment_1723&quot;&gt;Niwot_Ridge_Pigment_1723&lt;/h4&gt;
This dataset provides concentrations of pigments in pine and spruce needle tissues collected at the Niwot Ridge AmeriFlux Core site (US-NR1) near Nederland, Colorado, USA, during the summers of 2017 and 2018. Pigments measured included Chlorophyll A and B, Violaxanthin, Antheraxanthin, Zeaxanthin, Neoxanthin, Lutein, and beta-Carotene. Measurements were made on sun foliage from two canopy-access towers near the main flux tower, and in the laboratory on branches collected from those towers, every 4-8 weeks over the annual cycle. Due to canopy structure, a limited number of trees were accessible from the towers, preventing extensive replication. Pigments were extracted in acetone and analyzed by HPLC. The measurements were made to evaluate seasonal changes associated with the down-regulation of photosynthesis.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_darte_v2_1735&quot;&gt;CMS_DARTE_V2_1735&lt;/h4&gt;
This data set provides a 38-year, 1-km resolution inventory of annual on-road CO2 emissions for the conterminous United States based on roadway-level vehicle traffic data and state-specific emissions factors for multiple vehicle types on urban and rural roads as compiled in the Database of Road Transportation Emissions (DARTE). CO2 emissions from the on-road transportation sector are provided annually for 1980-2017 as a continuous surface at a spatial resolution of 1 km.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gcrw_dem_2016_1793&quot;&gt;GCRW_DEM_2016_1793&lt;/h4&gt;
This dataset contains four alternative digital elevation models (DEMs) at 1 m resolution and model performance statistical metrics for the Global Change Research Wetland (GCReW) site on the Rhode River, a tributary of the Chesapeake Bay in Maryland, USA, for the year 2016. Three DEMs were created by using different strategies for correcting positive biases in Light Detection and Ranging (LiDAR)-based DEMs that are common in tidal wetlands. These included (1) applying a single average offset based on a literature review, (2) using the LiDAR Elevation Correction with NDVI (LEAN)-method, and (3) applying plant community-specific offsets using a local vegetation cover map. Existing LiDAR data at 1 m resolution collected in 2011 was the basis for these DEMs. The fourth DEM was created by using Empirical Bayesian Kriging to extrapolate between measured ground points. The elevation is provided in meters relative to the North American Vertical Datum of 1988 (NAVD 88). To calibrate the four approaches, the elevation of the entire marsh complex was surveyed at 20 m x 20 m resolution to document the distribution of elevation relative to tidal datums from a single year. Two Trimble R8 real-time kinematic (RTK) GPS receivers were used to survey 525 points over the complex from July 26, 2016, to August 15, 2016. Relative plant cover was also documented. Tidal datums were calculated from the nearby Annapolis, MD tidal gauge located 13 km from GCReW.
&lt;br&gt;&lt;h4 id&#x3D;&quot;disturbance_biomass_maps_1679&quot;&gt;Disturbance_Biomass_Maps_1679&lt;/h4&gt;
This dataset provides derived disturbance history and predicted annual forest biomass maps at 30-m resolution for six selected Landsat scenes across the Conterminous United States (CONUS) for the period 1985-2014. The focus sites are in the following states: Colorado, Maine, Minnesota, Oregon, Pennsylvania, and South Carolina. These scenes were selected to represent a wide range of forest ecosystems, which ensured that a diversity of forest type groups and forest change processes (e.g., harvest, fire, insects, and urbanization) were included. Disturbance history was derived from a Landsat time-series for each site. Each disturbance is represented by year of detection, duration, and magnitude. The cause of the disturbance was not identified. Forest biomass was measured at field plots within each of the six sites and combined with airborne LiDAR data from each site to create land validation maps. Site biomass at 30-m resolution was estimated by developing Random Forest models that include site disturbance history with the land validation maps.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cropland_carbon_fluxes_2125&quot;&gt;Cropland_Carbon_Fluxes_2125&lt;/h4&gt;
This dataset contains daily estimates of carbon fluxes in croplands derived from the &amp;quot;ecosys&amp;quot; model covering a portion of the Midwestern US (Illinois, Indiana, and Iowa) at county-level resolution from 2001-2018. Ecosys simulates water, energy, carbon, and nutrient cycles simultaneously for various ecosystems, including agricultural systems at up to hourly resolution. Estimates include: gross primary productivity (GPP), net primary productivity (NPP), autotrophic respiration (Ra), heterotrophic respiration (Rh), or net ecosystem exchange (NEE). Data were generated by the ecosys model constrained by observational data, including USDA crop yield from USDA National Agricultural Statistics Service, and a remote-sensing-based SLOPE GPP product. Model performance was evaluated using observations from AmeriFlux towers at agricultural sites within the study area. Agriculture in the US Midwest produces significant quantities of corn and soybeans, which are key elements to the global food supply. The data are provided in shapefile format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ef_data_mexico_1693&quot;&gt;EF_Data_Mexico_1693&lt;/h4&gt;
This dataset provides a map of the distribution of ecosystem functional types (EFTs) at 0.05 degree resolution across Mexico for 2001 to 2014. EFTs are groupings of ecosystems based on their similar ecosystem functioning that are used to represent the spatial patterns and temporal variability of key ecosystem functional traits without prior knowledge of vegetation type or canopy architecture. Sixty-four EFTs were derived from the metrics of a 2001-2014 time-series of satellite images of the Enhanced Vegetation Index (EVI) from the Moderate Resolution Imaging Spectroradiometer (MODIS) product MOD13C2. EFT diversity was calculated as the modal (most repeated) EFT for each pixel.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_eft_conus_1659&quot;&gt;CMS_EFT_CONUS_1659&lt;/h4&gt;
This dataset provides maps of the distribution of ecosystem functional types (EFTs) and the interannual variability of EFTs at 0.05 degree resolution across the conterminous United States (CONUS) for 2001 to 2014. EFTs are groupings of ecosystems based on their similar ecosystem functioning that are used to represent the spatial patterns and temporal variability of key ecosystem functional traits without prior knowledge of vegetation type or canopy architecture. Sixty-four EFTs were derived from the metrics of a 2001-2014 time-series of satellite images of the Enhanced Vegetation Index (EVI) from the Moderate Resolution Imaging Spectroradiometer (MODIS) product MOD13C2. EFT diversity was calculated as the modal (most repeated) EFT and interannual variability was calculated as the number of unique EFTs for each pixel.
&lt;br&gt;&lt;h4 id&#x3D;&quot;dlem_c_n_export_1699&quot;&gt;DLEM_C_N_Export_1699&lt;/h4&gt;
This dataset provides estimates for export and leaching of dissolved inorganic carbon (DIC), dissolved organic carbon (DIC), total organic carbon (TOC), particulate organic carbon (POC), ammonium (NH4+), nitrate (NO3-), and total organic nitrogen (TON) from the Mississippi River Basin (MRB) to the Gulf of Mexico. The estimates are provided for a historical period of 1901-2014, and a future period of 2010-2099 (carbon estimates only) under two scenarios of high and low levels of population growth, economy, and energy consumption, respectively. The estimates are from the Dynamic Land Ecosystem Model 2.0 (DLEM 2.0). These data are applicable to studying how changes in multiple environmental factors (e.g., fertilizer application, land-use changes, climate variability, atmospheric CO2 and N deposition) affect the dynamics of leaching and export to the Gulf of Mexico.
&lt;br&gt;&lt;h4 id&#x3D;&quot;fire_emissions_indonesia_2118&quot;&gt;Fire_Emissions_Indonesia_2118&lt;/h4&gt;
This dataset provides 10-minute fire emissions within 0.1-degree regularly spaced intervals across Indonesia from July 2015 to December 2020. The dataset was produced with a top-down approach based on fire radiative energy (FRE) and smoke aerosol emission coefficients (Ce) derived from multiple new-generation satellite observations. Specifically, the Ce values of peatland, tropical forest, cropland, or savanna and grassland were derived from fire radiative power (FRP) and emission rates of smoke aerosols based on Visible Infrared Imaging Radiometer Suite (VIIRS) active fire and aerosol products. FRE for each 0.1-degree interval was calculated from the diurnal FRP cycle that was reconstructed by fusing cloud-corrected FRP retrievals from the high temporal-resolution (10 mins) Himawari-8 Advanced Himawari Imager (AHI) with those from high spatial-resolution (375 m) VIIRS. This new dataset was named the Fused AHI-VIIRS based fire Emissions (FAVE). Fire emissions data are provided in comma-separated values (CSV) format with one file per month from July 2015 to December 2020. Each file includes variables of fire observation time, fire geographic location, classification, fire radiative energy, various fire emissions and related standard deviations.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_forest_carbon_maryland_1660&quot;&gt;CMS_Forest_Carbon_Maryland_1660&lt;/h4&gt;
This dataset provides 90-m resolution maps of estimated forest aboveground biomass (Mg/ha) for nominal year 2011 and projections of carbon sequestration potential for the state of Maryland. Estimated biomass and sequestration potential were computed using the Ecosystem Demography (ED) model, which integrates data from multiple sources, including: climate variables from the North American Regional Reanalysis (NARR) Product, soil variables from the Soil Survey Geographic Database (SSURGO), land cover variables from airborne lidar, the National Agriculture Imagery Program (NAIP) and the National Land Cover Database (NLCD), and vegetation parameters from the Forest Inventory and Analysis (FIA) Program.
&lt;br&gt;&lt;h4 id&#x3D;&quot;agb_carbon_sequestration_rggi_1922&quot;&gt;AGB_Carbon_Sequestration_RGGI_1922&lt;/h4&gt;
This dataset provides 90 m estimates of forest aboveground biomass (Mg/ha) for nominal 2011 and projections of carbon sequestration potential for 11 states in the Regional Greenhouse Gas Initiative (RGGI) domain. The RGGI is a cooperative, market-based effort among States in the eastern United States. Estimated biomass and sequestration potential were computed using the Ecosystem Demography (ED) model. The ED Model integrates several key data including climate variables from Daymet and MERRA2 products; physical soil and hydraulic properties from Probabilistic Remapping of SSURGO (POLARIS) and CONUS-SOIL; land cover characteristics from airborne lidar, the National Agriculture Imagery Program (NAIP), and the National Land Cover Database (NLCD); and vegetation parameters from the Forest Inventory and Analysis (FIA) Program.
&lt;br&gt;&lt;h4 id&#x3D;&quot;maine_forest_biomass_map_2435&quot;&gt;Maine_Forest_Biomass_Map_2435&lt;/h4&gt;
This dataset holds estimates of forest aboveground biomass (AGB) for Maine, USA, in 2023. AGB was estimated using airborne LiDAR data from the USGS 3DEP project and a deep learning convolutional neural network (CNN) model. The airborne LiDAR datasets used in this mapping were collected in different years. The CNN model was calibrated using plot-level forest inventory data with precise location measurements and spectral indices derived from multiple remote sensing products. Stand-level biomass succession models, developed from the USDA Forest Service Forest Inventory and Analysis (FIA) data, were applied to project biomass estimates to the year 2023 with 10-m spatial resolution. The data are provided in GeoTIFF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;annual_forest_agb_maryland_2384&quot;&gt;Annual_Forest_AGB_Maryland_2384&lt;/h4&gt;
This dataset includes estimates of annual forest aboveground biomass over the state of Maryland, USA, for the period 1984-2023. It was generated by a modeling approach that linked an ecosystem model called Ecosystem Demography (ED) model, airborne lidar data of canopy height in circa 2010, and the remote sensing based land cover change dataset (NAFD).
&lt;br&gt;&lt;h4 id&#x3D;&quot;agb_nep_disturbance_us_forests_1829&quot;&gt;AGB_NEP_Disturbance_US_Forests_1829&lt;/h4&gt;
This dataset, derived from the National Forest Carbon Monitoring System (NFCMS), provides estimates of forest carbon stocks and fluxes in the form of aboveground woody biomass (AGB), total live biomass, total ecosystem carbon, aboveground coarse woody debris (CWD), and net ecosystem productivity (NEP) as a function of the number of years since the most recent disturbance (i.e., stand age) for forests of the conterminous U.S. at a 30 m resolution for the benchmark years 1990, 2000, and 2010. The data were derived from an inventory-constrained version of the Carnegie-Ames-Stanford Approach (CASA) carbon cycle process model that accounts for disturbance processes for each combination of forest type, site productivity, and pre-disturbance biomass. Also provided are the core model data inputs including the year of the most recent disturbance according to the North American Forest Dynamics (NAFD) and the Monitoring Trends in Burn Severity (MTBS) data products; the type of disturbance; biomass estimates from the year 2000 according to the National Biomass and Carbon Dataset (NBCD); forest-type group; a site productivity classification; and the number of years since stand-replacing disturbance. The data are useful for a wide range of applications including monitoring and reporting recent dynamics of forest carbon across the conterminous U.S., assessment of recent trends with attribution to disturbance and regrowth drivers, conservation planning, and assessment of climate change mitigation opportunities within the forest sector.
&lt;br&gt;&lt;h4 id&#x3D;&quot;forest_inventory_brazil_2007&quot;&gt;Forest_Inventory_Brazil_2007&lt;/h4&gt;
This dataset provides the complete catalog of forest inventory and biophysical measurements collected over selected forest research sites across the Amazon rainforest in Brazil between 2009 and 2018 for the Sustainable Landscapes Brazil Project. This dataset includes measurements for diameter at breast height (DBH), commercial tree height, and total tree height for forest inventories. Also included for each tree are the family, common and scientific names, coordinates, canopy position, crown radius, and for dead trees, the decomposition status. Aboveground biomass estimate is available for selected sites. The data are provided in comma-separated values (CSV) and shapefile formats. Sampling methodology for each site and year is described in companion files.
&lt;br&gt;&lt;h4 id&#x3D;&quot;geos_casagfed_3h_nee&quot;&gt;GEOS_CASAGFED_3H_NEE&lt;/h4&gt;
This product provides 3 hourly average net ecosystem exchange (NEE) and gross ecosystem exchange (GEE) of Carbon derived from the Carnegie-Ames-Stanford-Approach – Global Fire Emissions Database version 3 (CASA- GFED3) model. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;geos_casagfed_d_fire&quot;&gt;GEOS_CASAGFED_D_FIRE&lt;/h4&gt;
This product provides Daily average wildfire emissions (FIRE) and fuel wood burning emissions (FUEL) derived from the Carnegie-Ames-Stanford-Approach – Global Fire Emissions Database version 3 (CASA- GFED3) model. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;geos_casagfed_m_flux&quot;&gt;GEOS_CASAGFED_M_FLUX&lt;/h4&gt;
This product provides Monthly average Net Primary Production (NPP), heterotrophic respiration (Rh), wildfire emissions (FIRE), and fuel wood burning emissions (FUEL) derived from the Carnegie-Ames-Stanford-Approach – Global Fire Emissions Database version 3 (CASA- GFED3) model. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_global_fire_atlas_1642&quot;&gt;CMS_Global_Fire_Atlas_1642&lt;/h4&gt;
The Global Fire Atlas is a global dataset that tracks the day-to-day dynamics of individual fires to determine the timing and location of ignitions, fire size, duration, daily expansion, fire line length, speed, and direction of spread. These individual fire characteristics were derived based on the Global Fire Atlas algorithm and estimated day of burn information at 500-m resolution from the Moderate Resolution Imaging Spectroradiometer (MODIS) Collection 6 MCD64A1 burned area product. The algorithm identified 13.3 million individual fires (&amp;gt;&#x3D;21 ha or 0.21 km2; the size of one MODIS pixel) over the 2003-2016 study period.
&lt;br&gt;&lt;h4 id&#x3D;&quot;globfirecarbon&quot;&gt;GlobFireCarbon&lt;/h4&gt;
This dataset provides carbon monoxide and carbon dioxide flux from fires constrained by satellite observations. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_global_forest_agc_2180&quot;&gt;CMS_Global_Forest_AGC_2180&lt;/h4&gt;
This dataset provides global gridded estimates of forest aboveground carbon stocks and potential fluxes at a 0.01-degree resolution. It was derived by initializing a newly developed global Ecosystem Demography model (ED v3.0) with novel remote sensing observations of tree canopy height collected by GEDI and ICESat-2, two NASA spaceborne lidar missions. A total of 3.77 billion lidar samples were used to generate gridded canopy height histograms that were then linked to ED simulations of canopy height and carbon dynamics during ecosystem succession. This process constrained representation of contemporary forest conditions and associated carbon stocks and fluxes in the model. Inputs that drove these simulations included meteorology, carbon dioxide levels, and soil properties. The data are provided in cloud-optimized GeoTIFF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;methane_flaring_sites_viirs_1874&quot;&gt;Methane_Flaring_Sites_VIIRS_1874&lt;/h4&gt;
This dataset contains annual global flare site surveys from 2012-2019 derived from Visible Infrared Imaging Radiometer Suite (VIIRS) on the Suomi National Polar Partnership (SNPP) satellite. Gas flaring sites were identified from heat anomalies first estimated by the VIIRS Nightfire (VNF) algorithm from which high-temperature biomass burning and low-temperature gas flaring were separated based on temperature and persistence. Nightly observations for each flare site were drawn to determine their activity in the given calendar year. Data include flare location, temperature, and estimated flared gas volume; flaring data summarized by country; and KMZ files for viewing flaring locations in Google Earth. This dataset is valuable for measuring the current status of global gas flaring, which can have significant environmental impacts.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_global_soil_respiration_1736&quot;&gt;CMS_Global_Soil_Respiration_1736&lt;/h4&gt;
This dataset provides six global gridded products at 1-km resolution of predicted annual soil respiration (Rs) and associated uncertainty, maps of the lower and upper quartiles of the prediction distributions, and two derived annual heterotrophic respiration (Rh) maps. A machine learning approach was used to derive the predicted Rs and uncertainty data using a quantile regression forest (QRF) algorithm trained with observations from the global Soil Respiration Database (SRDB) version 3 spanning from 1961 to 2011. The two Rh maps were derived from the predicted Rs with two different empirical equations. These products were produced to support carbon cycle research at local- to global-scales, and highlight the immense spatial variability of soil respiration and our ability to predict it across the globe.
&lt;br&gt;&lt;h4 id&#x3D;&quot;soilresp_heterotrophicresp_1928&quot;&gt;SoilResp_HeterotrophicResp_1928&lt;/h4&gt;
This dataset provides global gridded estimates of annual soil respiration (Rs) and soil heterotrophic respiration (Rh) and associated uncertainties at 1 km resolution. Mean soil respiration was estimated using a quantile regression forest model utilizing data from the global Soil Respiration Database Version 5 (SRDB-V5) and covariates of mean annual temperature, seasonal precipitation, and vegetative cover. The SRDB holds results of field studies of soil respiration from around the globe. A total of 4,115 records from 1,036 studies were selected from SRDB-V5. SRDB-V5 features more soil respiration data published in Russian and Chinese scientific literature for better global spatio-temporal coverage and improved global climate-space representation. These soil respiration records were combined with global meteorological, land cover, and topographic data and then evaluated with variable selection using random forests. The standard deviation and coefficient of variation of Rs are included and were also derived from the same model. Global heterotrophic respiration was calculated from Rs estimates. The data are produced in part from SRDB-V5 inputs that cover the period 1961-2016.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gfei_ch4&quot;&gt;GFEI_CH4&lt;/h4&gt;
This is a global inventory of methane emissions from fuel exploitation (GFEI) created for the NASA Carbon Monitoring System (CMS). The emission sources represented in this dataset include fugitive emission sources from oil, gas, and coal exploitation following IPCC 2006 definitions and are estimated using bottom-up methods. The inventory emissions are based on individual country reports submitted in accordance with the United Nations Framework Convention on Climate Change (UNFCCC). For those countries that do not report, the emissions are estimated following IPCC 2006 methods. Emissions are allocated to infrastructure locations including mines, wells, pipelines, compressor stations, storage facilities, processing plants, and refineries. The purpose of the inventory is to be used as a prior estimate of fuel exploitation emissions in inverse modeling of atmospheric methane observations. GFEI only includes fugitive methane emissions from oil, gas, and coal exploitation activities and does not include any combustion emissions as defined in IPCC 2006 category 1A. The CMS program is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System uses NASA observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS data products are designed to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_global_map_mangrove_canopy_1665&quot;&gt;CMS_Global_Map_Mangrove_Canopy_1665&lt;/h4&gt;
This dataset characterizes the global distribution, biomass, and canopy height of mangrove-forested wetlands based on remotely sensed and in situ field measurement data. Estimates of (1) mangrove aboveground biomass (AGB), (2) maximum canopy height (height of the tallest tree), and (3) basal-area weighted height (individual tree heights weighted in proportion to their basal area) for the nominal year 2000 were derived across a 30-meter resolution global mangrove ecotype extent map using remotely-sensed canopy height measurements and region-specific allometric models. Also provided are (4) in situ field measurement data for selected sites across a wide variety of forest structures (e.g., scrub, fringe, riverine and basin) in mangrove ecotypes of the global equatorial region. Within designated plots, selected trees were identified to species and diameter at breast height (DBH) and tree height was measured using a laser rangefinder or clinometer. Tree density (the number of stems) can be estimated for each plot and expressed per unit area. These data were used to derive plot-level allometry among AGB, basal area weighted height (Hba), and maximum canopy height (Hmax) and to validate the remotely sensed estimates.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_global_mangrove_loss_1768&quot;&gt;CMS_Global_Mangrove_Loss_1768&lt;/h4&gt;
This dataset provides estimates of the extent of mangrove loss, land cover change, and its anthropogenic or climatic drivers in three time periods: 2000-2005, 2005-2010, and 2010-2016. Landsat-based Normalized Difference Vegetation Index (NDVI) anomalies were used to determine loss extent in each period. The drivers of mangrove loss were determined by examining land cover changes using a random forest machine learning technique that considered change from mangrove to wet soil, dry soil, and water at each loss pixel. A series of decision trees used several global-scale land-use datasets to identify the ultimate driver of the mangrove loss. Loss drivers include commodity production (agriculture, aquaculture), settlement, erosion, extreme climatic events, and non-productive conversion. Maps of loss extent per period, mangrove land cover changes, and loss drivers are provided for each of 39 mangrove holding nations.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cmsgch4f&quot;&gt;CMSGCH4F&lt;/h4&gt;
This dataset provides global methane fluxes optimized with GOSAT data for 2010-2018. It is supported by the Carbon Monitoring System project. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System uses NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS data products are designed to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;global_salt_marsh_change_2122&quot;&gt;Global_Salt_Marsh_Change_2122&lt;/h4&gt;
This dataset provides global salt marsh change, including loss and gain for five-year periods from 2000-2019. Loss and gain at a 30 m spatial resolution were estimated with Normalized Difference Vegetation Index (NDVI) anomaly algorithm using Landsat 5, 7, and 8 collections within the known extent of salt marshes. The data are provided in cloud-optimized GeoTIFF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;global_freshwater_ch4emissions_2253&quot;&gt;Global_Freshwater_CH4Emissions_2253&lt;/h4&gt;
This dataset provides monthly globally gridded freshwater wetland methane emissions from 2001-2018 in nmol CH4 m-2 s-1, g C-CH4 m-2 d-1, and TgCH4 grid cell-1 month-1. The data were derived from a six-predictor random forest upscaling model (UpCH4) trained on 119 site-years of eddy covariance CH4 flux data from 43 freshwater wetland sites covering bog (8), fen (8), marsh (10), swamp (6), and wet tundra (11) wetland classes and distributed across Arctic-boreal (20), temperate (16), and (sub)tropical (7) climate zones. Weekly mean CH4 fluxes were computed from half-hourly FLUXNET-CH4 Version 1.0 fluxes. Each grid cell CH4 flux prediction was weighted by fractional grid cell wetland extent to estimate CH4 emissions using the primary global dataset of Wetland Area and Dynamics for Methane Modeling (WAD2M) product and an alternate Global Inundation Estimate from Multiple Satellites GIEMS version 2 global wetland map. Both WAD2M and GIEMS-2 maps were modified with several correction data layers to represent the monthly area covered by vegetated wetlands, excluding open water and coastal wetlands. The data products are: mean daily fluxes with no adjustment for wetland area (i.e., flux densities assuming hypothetical 100% wetland cover); mean daily fluxes adjusting for WAD2M or GIEMS-2 wetland area; and by-pixel monthly sum of freshwater wetland methane emissions adjusting for WAD2M or GIEMS-2 wetland area. The data are provided in NetCDF4 format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tidal_marsh_vegetation_us_1608&quot;&gt;Tidal_Marsh_Vegetation_US_1608&lt;/h4&gt;
This dataset provides 30m resolution maps of the fraction of green vegetation within tidal marshes for six estuarine regions of the conterminous United States: Cape Cod, MA; Chesapeake Bay, MD; Everglades, FL; Mississippi Delta, LA; San Francisco Bay, CA; and Puget Sound, WA. Maps were derived from a 1m classification of 2013 to 2015 National Agriculture Imagery Program (NAIP) images as tidal marsh green vegetation, non-vegetation, and open water. Using this high-resolution map, the percent of each class within Landsat pixel extents was calculated to produce a 30m fraction of green vegetation map for each region.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cstocks_greenness_mangroves_mx_1853&quot;&gt;CStocks_Greenness_Mangroves_MX_1853&lt;/h4&gt;
This dataset provides estimates of greenness trends, above- and belowground carbon stocks, and climate variables of the persistent mangrove forests on the coasts of Mexico (PMFM) at a 1 km resolution from 2001 through 2015. Data are available as one-time estimates or across the temporal range; typically as monthly summaries. One-time estimates of aboveground carbon and soil organic carbon stocks for the PMFM derived from existing sources are provided. Also included are the monthly mean normalized difference vegetation index (NDVI) from MOD13A3 used to derive greenness trends, monthly mean air temperature, and total monthly precipitation from Daymet for 2001-2015 across the PMFM. Other files include the distribution and coverage of PMFM across Mexico. Distributions are provided as four categories of PMFM: (1) Arid mangroves with Surface Water as main input, along the Gulf of California and Pacific Coast (ARsw); (2) humid mangroves with surface water input along the Pacific Coast (HUsw-Pa); (3) humid mangroves with surface water input along the coast of the Gulf of Mexico (HUsw-Gf); (4) humid mangroves with groundwater input along the Gulf of Mexico and Caribbean Sea (HUgw). These data provide a baseline for national monitoring programs, carbon accounting models, and greenness trends in coastal wetlands.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tidal_wetland_gpp_conus_1792&quot;&gt;Tidal_Wetland_GPP_CONUS_1792&lt;/h4&gt;
This dataset provides mapped tidal wetland gross primary production (GPP) estimates (g C/m2/day) derived from multiple wetland types at 250-m resolution across the conterminous United States at 16-day intervals from March 5, 2000, through November 17, 2019. GPP was derived with the spatially explicit Blue Carbon (BC) model, which combined tidal wetland cover and field-based eddy covariance (EC) tower GPP data into a single Bayesian framework along with Moderate Resolution Imaging Spectroradiometer (MODIS) Enhanced Vegetation Index (EVI) datasets. Tidal wetlands are a critical component of global climate regulation. Tidal wetland-based carbon, or &amp;quot;blue carbon,&amp;quot; is a valued resource that is increasingly important for restoration and conservation purposes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sif_par_fpar_us_midwest_2018_1813&quot;&gt;SIF_PAR_fPAR_US_Midwest_2018_1813&lt;/h4&gt;
This dataset provides estimated solar-induced chlorophyll fluorescence (SIF) of specific vegetation types and total SIF under clear-sky and real/cloudy conditions at a resolution of 4 km for the Midwest USA. The estimates are 8-day averaged daily means over the 2018 crop growing season for the time period 2018-05-01 to 2018-09-29. SIF of a specific vegetation type (i.e., corn, soybean, grass/pasture, forest) was expressed as the product of photosynthetically active radiation (PAR), the fraction of photosynthetically active radiation absorbed by the canopy (fPAR), and canopy SIF yield (SIFyield) for each vegetation type. Uncertainty of each variable was also calculated and is provided. These components of the SIF model were derived using a TROPOspheric Monitoring Instrument (TROPOMI) dataset, the USDA National Agricultural Statistics Service Cropland Data Layer, and the MODIS MCD15A2H 8-day 500 m fPAR product. These data could be used to improve estimates of vegetation productivity and vegetation stress.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_hr_mna_ch4_flux&quot;&gt;CMS_HR_MNA_CH4_FLUX&lt;/h4&gt;
This data set contains estimates of methane emission in North America based on an inversion of the GEOS-Chem chemical transport model constrained by Greenhouse Gases Observing SATellite (GOSAT) observations. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_landcover_indonesia_1838&quot;&gt;CMS_Landcover_Indonesia_1838&lt;/h4&gt;
This dataset contains annual land use/cover (LUC) maps at 30 m resolution across Mawas, Central Kalimantan, Indonesia. There are six files, each representing a five-year interval over the period 1994-2019. An additional file for 2015 was created for accuracy assessment. A high-quality and low-cloud coverage image from Landsat 5 or Landsat 8 over each 5-year period was selected or composited for the January-August timeframe. Investigators used their knowledge to manually identify training polygons in these images for five LUC classes: peat swamp forest, tall shrubs/ secondary forest, low shrubs/ferns/grass, urban/bare land/open flooded areas, and river. Pixel values of Landsat Tier 1 surface reflectance products and selected indices were extracted for each LUC and used to predict LUC classes across the Mawas study area using the Classification and Regression Trees (CART) method. These data can be used to evaluate the relationship between fire occurrence and land cover type in the study site.
&lt;br&gt;&lt;h4 id&#x3D;&quot;estimated_biomass_stock_amazon_1648&quot;&gt;Estimated_Biomass_Stock_Amazon_1648&lt;/h4&gt;
This dataset provides estimates of forest aboveground biomass for three study areas and the entire Paragominas municipality, in Para, Brazil, in 2012. Aboveground biomass (in megagrams of carbon per hectare) was measured for inventory plots within the study (focal) areas, and then assimilated and modeled with LiDAR and PALSAR metrics using gradient boosting machines (GBM) to predict spatially explicit forest aboveground biomass and uncertainties for the entire focal areas. The PALSAR data across the three focal areas was combined and used in a GBM model to predict forest aboveground biomass across the entire Paragominas municipality.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_lidar_biomass_md_pa_de_1538&quot;&gt;CMS_LiDAR_Biomass_MD_PA_DE_1538&lt;/h4&gt;
This dataset provides 30-meter gridded estimates of aboveground biomass (AGB), forest canopy height, and canopy coverage for Maryland, Pennsylvania, and Delaware in 2011. Leaf-off LiDAR data were combined with high-resolution leaf-on agricultural imagery in a model-based stratification that was used to select 848 sampling sites for AGB estimation. Field-based estimates were then related to LiDAR height and volume metrics through random forest regression models across three physiographic regions. Spatial errors were estimated at the pixel level using standard prediction intervals to assess the accuracy of the modeling approach. Estimates of biomass were further validated against the permanent network of FIA plots and compared with existing coarse resolution national biomass maps.
&lt;br&gt;&lt;h4 id&#x3D;&quot;agb_canopyht_cover_newengland_1854&quot;&gt;AGB_CanopyHt_Cover_NewEngland_1854&lt;/h4&gt;
This dataset provides 30 m gridded estimates of aboveground biomass density (AGBD), forest canopy height, and tree canopy coverage for the New England Region of the U.S., including the state of Maine, Vermont, New Hampshire, Massachusetts, Connecticut, and Rhode Island, for the nominal year 2015. It is based on inputs from 1 m resolution Leaf-off LiDAR data collected from 2010 through 2015, high-resolution leaf-on agricultural imagery, and FIA plot-level measurements. Canopy height and tree cover were derived directly from LiDAR data while AGBD was estimated by statistical models that link remote sensing data and FIA plots at the pixel level. Error in AGBD was calculated at the 90% confidence interval. This approach can directly contribute to the formation of a cohesive forest carbon accounting system at national and even international levels, especially via future integrations with NASA&amp;#39;s spaceborne LiDAR missions.
&lt;br&gt;&lt;h4 id&#x3D;&quot;forest_agb_nw_usa_1766&quot;&gt;Forest_AGB_NW_USA_1766&lt;/h4&gt;
This dataset provides maps of aboveground forest biomass (AGB) of living trees and standing dead trees in Mg/ha across portions of Northwestern United States, including Washington, Oregon, Idaho, and Montana, at a spatial resolution of 30 m. Forest inventory data were compiled from 29 stakeholders that had overlapping lidar imagery. The collection totaled 3805 field plots with lidar imagery for 176 collections acquired between 2002 and 2016. Plot-level AGB estimates were calculated from tree measurements using the default allometric equations found in the Fire Fuels Extension (FFE) of the Forest Vegetation Simulator (FVS). The random forest algorithm was used to model AGB from lidar height and density metrics that were generated from the lidar returns within fixed-radius field plot footprints, gridded climate metrics obtained from the Climate-FVS Ready Data Server, and topographic estimates extracted from Shuttle Radar Topography Mission (SRTM) 1 Arc-Second Global elevation rasters. AGB was then mapped from the same lidar metrics gridded across the extent of the lidar collections at 30-m resolution. The standard deviation of estimated AGB of the terminal nodes from the random forest predictions was also mapped to show pixel-level model uncertainty. Note that the AGB estimates are, for the most part, a single snapshot in time and that the forest conditions are not necessarily representative of the larger study area.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lidar_forest_inventory_brazil_1644&quot;&gt;LiDAR_Forest_Inventory_Brazil_1644&lt;/h4&gt;
This dataset provides the complete catalog of point cloud data collected during LiDAR surveys over selected forest research sites across the Amazon rainforest in Brazil between 2008 and 2018 for the Sustainable Landscapes Brazil Project. Flight lines were selected to overfly key field research sites in the Brazilian states of Acre, Amazonas, Bahia, Goias, Mato Grosso, Para, Rondonia, Santa Catarina, and Sao Paulo. The point clouds have been georeferenced, noise-filtered, and corrected for misalignment of overlapping flight lines. They are provided in 1 km2 tiles. The data were collected to measure forest canopy structure across Amazonian landscapes to monitor the effects of selective logging on forest biomass and carbon balance, and forest recovery over time.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_lidar_agb_california_1537&quot;&gt;CMS_LiDAR_AGB_California_1537&lt;/h4&gt;
This dataset provides estimates of aboveground biomass and spatially explicit uncertainty from 53 airborne LiDAR surveys of locations throughout California between 2005 and 2014. Aboveground biomass was estimated by performing individual tree crown detection and applying a customized &amp;quot;remote sensing aware&amp;quot; allometric equation to these individual trees. Aboveground biomass estimates and their uncertainties for each study area are provided in per-tree and gridded format. The canopy height models used for the tree detection and biomass estimation are also provided.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_ch4_flx_ca&quot;&gt;CMS_CH4_FLX_CA&lt;/h4&gt;
This data set (CMS_CH4_FLX_CA) contains the yearly average methane (CH4) flux for Canada&amp;#39;s oil and gas systems based on a bottom up calculation of oil/gas emissions reported by ICF International in 2013. A related data set (CMS_CH4_FLX_MX) contains the yearly average methane (CH4) flux for Mexico&amp;#39;s oil and gas systems based on a bottom up calculation of oil/gas emissions reported by the Mexican Petrolium Institute in 2010. The Canadian emissions are concentrated in Alberta (gas production and processing) and the Mexican emissions are concentrated along the east coast (oil production). More details about the observations, algorithm, and scientific findings are described in Sheng et al. 2017. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_ch4_flx_mx&quot;&gt;CMS_CH4_FLX_MX&lt;/h4&gt;
This data set (CMS_CH4_FLX_MX) contains the yearly average methane (CH4) flux for Mexico&amp;#39;s oil and gas systems based on a bottom up calculation of oil/gas emissions reported by the Mexican Petrolium Institute in 2010. A related data set (CMS_CH4_FLX_CA) contains the yearly average methane (CH4) flux for Canada&amp;#39;s oil and gas systems based on a bottom up calculation of oil/gas emissions reported by ICF International in 2013. The Mexican emissions are concentrated along the east coast (oil production) and the Canadian emissions are concentrated in Alberta (gas production and processing). More details about the observations, algorithm, and scientific findings are described in Sheng et al. 2017. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_ch4_flx_nad&quot;&gt;CMS_CH4_FLX_NAD&lt;/h4&gt;
The CMS Methane (CH4) Flux for North America data set contains estimates of methane emission in North America based on an inversion of the GEOS-Chem chemical transport model constrained by Greenhouse Gases Observing SATellite (GOSAT) observations. The nested approach of the inversion enables large point sources to be resolved while aggregating regions with weak emissions and minimizing aggregation errors. The emission sources are separated into 12 different sectors as follows: Total, Oil/Gas, Coal, Cows, Waste (Landfills+ Wastewater), Biofuel, Rice, Other Anthropogenic, Biomass Burning, Wetlands, Soil Absorption, Other Natural. More details about the algorithm and error characterization can be found in Turner, Jacob, Wecht, et al. 2015. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;methane_ethane_ma_nh_1982&quot;&gt;Methane_Ethane_MA_NH_1982&lt;/h4&gt;
This dataset provides the hourly average of continuous atmospheric measurements of methane (CH4) from two urban sites and three boundary sites in and around Boston, Massachusetts, U.S., from September 2012-May 2020, measured with Picarro cavity ring down spectrometers (CRDS). Five-minute average atmospheric measurements of ethane (C2H6) and methane at Copley Square in Boston, MA, are also provided, with ethane measured with a laser spectrometer and methane measured with a Picarro CRDS. Background CH4 concentrations for the urban sites were determined using Hybrid Single-Particle Lagrangian Integrated Trajectory (HYSPLIT) model trajectories at the boundary of the study region based on measurements at three boundary sites and wind direction from the North American Mesoscale Forecast System (NAM) 12-kilometer meteorology.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ch4_plume_aviris-ng_1727&quot;&gt;CH4_Plume_AVIRIS-NG_1727&lt;/h4&gt;
This dataset provides maps of methane (CH4) plumes along flight lines over identified methane point-source emitting infrastructure across the State of California, USA collected during 2016 and 2017. Methane plume locations were derived from Next-Generation Airborne Visible Infrared Imaging Spectrometer (AVIRIS-NG) overflights during the California Methane Survey. The survey was designed to cover at least 60% of the methane point source infrastructure in California guided by the Vista-CA dataset of identified locations of potential methane emitting facilities and infrastructure in three primary sectors (energy, agriculture, and waste). The purpose of the survey was to detect, quantify, and attribute point source emissions to specific infrastructure elements to improve the scientific understanding of regional methane budgets and to inform policy and planning activities that reduce methane emissions.
&lt;br&gt;&lt;h4 id&#x3D;&quot;micasa_flux_3h&quot;&gt;MICASA_FLUX_3H&lt;/h4&gt;
MiCASA is an extensive revision of CASA-GFED3. CASA-GFED3 derives from Potter et al. (1993), diverging in development since Randerson et al. (1996). CASA is a light use efficiency model: NPP is expressed as the product of photosynthetically active solar radiation, a light use efficiency parameter, scalars that capture temperature and moisture limitations, and fractional absorption of photosynthetically active radiation (fPAR) by the vegetation canopy derived from satellite data. Fire parameterization was incorporated into the model by van der Werf et al. (2004) leading to CASA-GFED3 after several revisions (van der Werf et al., 2006, 2010). Development of the GFED module has continued, now at GFED5 (Chen et al., 2023) with less focus on the CASA module. MiCASA diverges from GFED development at version 3, although future reconciliation is possible. Input datasets include air temperature, precipitation, incident solar radiation, a soil classification map, and several satellite derived products. These products are primarily based on Moderate Resolution Imaging Spectroradiometer (MODIS) Terra and Aqua combined datasets including land cover classification (MCD12Q1), burned area (MCD64A1), Nadir BRDF-Adjusted Reflectance (NBAR; MCD43A4), from which fPAR is derived, and tree/herbaceous/bare vegetated fractions from Terra only (MOD44B). Emissions due to fire and burning of coarse woody debris (fuel wood) are estimated separately.
&lt;br&gt;&lt;h4 id&#x3D;&quot;slope_gpp_conus_1786&quot;&gt;SLOPE_GPP_CONUS_1786&lt;/h4&gt;
This dataset contains estimated gross primary productivity (GPP), photosynthetically active radiation (PAR), soil adjusted near infrared reflectance of vegetation (SANIRv), the fraction of C4 crops in vegetation (fC4), and their uncertainties for the conterminous United States (CONUS) from 2000 to 2019. The daily estimates are SatelLite Only Photosynthesis Estimation (SLOPE) products at 250-m resolution. There are three distinct features of the GPP estimation algorithm: (1) SLOPE couples machine learning models with MODIS atmosphere and land products to accurately estimate PAR, (2) SLOPE couples gap-filling and filtering algorithms with surface reflectance acquired by both Terra and Aqua MODIS satellites to derive a soil-adjusted NIRv (SANIRv) dataset, and (3) SLOPE couples a temporal pattern recognition approach with a long-term Crop Data Layer (CDL) product to predict dynamic C4 crop fraction. PAR, SANIRv and C4 fraction are used to drive a parsimonious model with only two parameters to estimate GPP, along with a quantitative uncertainty, on a per-pixel and daily basis. The slope GPP product has an R2 &#x3D; 0.84 and a root-mean-square error (RMSE) of 1.65 gC m-2 d-1.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nasmo_tiam_250m_2326&quot;&gt;NASMo_TiAM_250m_2326&lt;/h4&gt;
This NASMo-TiAM (North America Soil Moisture Dataset Derived from Time-Specific Adaptable Machine Learning Models) dataset holds gridded estimates of surface soil moisture (0-5 cm depth) at a spatial resolution of 250 meters over 16-day intervals from mid-2002 to December 2020 for North America. The model employed Random Forests to downscale coarse-resolution soil moisture estimates (0.25 deg) from the European Space Agency Climate Change Initiative (ESA CCI) based on their correlation with a set of static (terrain parameters, bulk density) and dynamic covariates (Normalized Difference Vegetation Index, land surface temperature). NASMo-TiAM 250m predictions were evaluated through cross-validation with ESA CCI reference data and independent ground-truth validation using North American Soil Moisture Database (NASMD) records. The data are provided in cloud optimized GeoTIFF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;bgc_glider_gnats&quot;&gt;BGC_glider_GNATS&lt;/h4&gt;
This dataset contains ocean biogeochemistry data from two Slocum gliders along the Gulf of Maine North Atlantic Time Series (GNATS) transect. The transect runs approximately east-west, with only a very minor change in latitude. The gliders are deployed on the western end of the transect, travel along the transect line to the eastern end, turn around and travel back along the transect to the western end, before being recovered. Each file contains data from one deployment (a glider “mission”), and thus contains both an eastbound and a westbound measurement of each variable. A full mission takes approximately 20 – 30 days. The data are gridded by longitude (0.01° intervals) and depth (1 m intervals). For more details on dataset preparation, see the Original Publication Citation and Data Processing Workflow below.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_oce_bgc_ccs&quot;&gt;CMS_OCE_BGC_CCS&lt;/h4&gt;
A coupled physical-biogeochemical ocean model (the MITgcm with BLING biogeochemistry) is a least squares fit to all available ocean observations in the region of the California Current System. This is accomplished iteratively through the adjoint method, using the methodology developed by the Consortium for Estimating the Circulation and Climate of the Ocean (ECCO). The result is a physically realistic estimate of the ocean state. The model domain extends from 28N to 40N and from 130W to 114W. It has a 1/16-degree horizontal resolution (~7km) and 72 vertical levels. The NASA Carbon Monitoring System (CMS) is designed to make significant contributions in characterizing, quantifying, understanding, and predicting the evolution of global carbon sources and sinks through improved monitoring of carbon stocks and fluxes. The System will use the full range of NASA satellite observations and modeling/analysis capabilities to establish the accuracy, quantitative uncertainties, and utility of products for supporting national and international policy, regulatory, and management activities. CMS will maintain a global emphasis while providing finer scale regional information, utilizing space-based and surface-based data and will rapidly initiate generation and distribution of products both for user evaluation and to inform near-term policy development and planning.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_monthly_co2_gulf_1668&quot;&gt;CMS_Monthly_CO2_Gulf_1668&lt;/h4&gt;
This dataset provides 1 km gridded monthly estimates of surface ocean partial pressure of CO2 (pCO2) and air-sea flux of CO2 (CO2 flux) for the northern Gulf of America for the period 2006 through 2010. Estimates of pCO2 were derived from MODIS/Aqua satellite imagery in combination with ship-based observations. Estimates of CO2 flux were derived from estimates of seawater pCO2, wind fields, and atmospheric pCO2.
&lt;br&gt;&lt;h4 id&#x3D;&quot;coastal_us_elevation_data_1844&quot;&gt;Coastal_US_Elevation_Data_1844&lt;/h4&gt;
This dataset provides maps of the elevation of coastal wetlands relative to tidal ranges for the conterminous United States (CONUS) at 30 m resolution for 2010. It also includes maps of tidal amplitude, relative sea-level rise for the period 1983-2001, and maps for coastal lands and low marsh areas based on the probability of being below the mean higher high tide water line for spring tides (MHHWS). Uncertainty layers for elevation maps are also provided.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_coastal_wetland_resilience_1839&quot;&gt;CMS_Coastal_Wetland_Resilience_1839&lt;/h4&gt;
This dataset provides information about the resilience of tidal wetlands to sea-level rise under three scenarios of global change. With rising seas, regularly inundated tidal wetlands may persist by vertical accretion of sediments (vertical resilience) and/or by migrating inland (lateral resilience), but local and regional conditions constrain these options. This dataset provides a vertical resilience index (VR) for coastal wetlands at 30 m resolution across the continental US predicted for 2100. The VR index was computed for current sea levels, local tidal dynamics, and coastal topography. It was also calculated for future sea levels predicted for 2100 by three IPCC Realized Concentration Pathway (RCP) scenarios: 2.5, 4.5, and 8.5. Moreover, the VR index incorporates estimated rates of sediment accretion. Relevant to lateral resiliency, the data include current and future tidal areas identified by mapping mean higher high water spring tide locations under the RCP scenarios. A shapefile outlining watershed units with tidal wetlands is included along with land cover classes for these areas for 1996 and 2011.
&lt;br&gt;&lt;h4 id&#x3D;&quot;satellitederived_forest_mexico_2320&quot;&gt;SatelliteDerived_Forest_Mexico_2320&lt;/h4&gt;
This dataset provides a comparison of forest extent agreement from seven remote sensing-based products across Mexico. These satellite-derived products include European Space Agency 2020 Land Cover Map for Mexico (ESA), Globeland30 2020 (Globeland30), Commission for Environmental Cooperation 2015 Land Cover Map (CEC), Impact Observatory 2020 Land Cover Map (IO), NAIP Trained Mean Percent Cover Map (NEX-TC), Global Land Analysis and Discovery Global 2010 Tree Cover (Hansen-TC), and Global Forest Cover Change Tree Cover 30 m Global (GFCC-TC). All products included data at 10-30 m resolution and represented the state of forest or tree cover from 2010 to 2020. These seven products were chosen based on: a) feedback from end-users in Mexico; b) availability and FAIR (findable, accessible, interoperable, and replicable) data principles; and c) products representing different methodological approaches from global to regional scales. The combined agreement map documents forest cover for each satellite-derived product at 30-m resolution across Mexico. The data are in cloud optimized GeoTIFF format and cover the period 2010-2020. A shapefile is included that outlines Mexico mainland areas.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sib4_global_halfdegree_daily_1849&quot;&gt;SiB4_Global_HalfDegree_Daily_1849&lt;/h4&gt;
This dataset provides global daily output predicted by the Simple Biosphere Model, Version 4.2 (SiB4), at a 0.5-degree spatial resolution covering the time period 2000 through 2018. SiB4 is a mechanistic land surface model that integrates heterogeneous land cover, environmentally responsive phenology, dynamic carbon allocation, and cascading carbon pools from live biomass to surface litter to soil organic matter. Daily output includes carbon, carbonyl sulfide, and energy fluxes; solar-induced fluorescence; carbon pools; soil moisture and temperatures in the top three layers; total column soil water and plant available water; and environmental potentials used to scale photosynthesis. The SiB4 output is per plant functional type (PFT) within each 0.5-degree grid cell. SiB4 partitions variable output to 15 PFTs in each grid cell that are indexed by the &amp;quot;npft&amp;quot; dimension (01-15) in each data file. The PFT three-character abbreviations (&amp;quot;pft_names&amp;quot; variable) are listed in the same order as the &amp;quot;npft&amp;quot; dimension. To combine the PFT-specific output into grid cell totals, users must compute the area-weighted mean across the vector of PFT-specific values for each cell. Fractional areal coverages are given in the &amp;quot;pft_area&amp;quot; variable for each cell.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sib4_global_halfdegree_hourly_1847&quot;&gt;SiB4_Global_HalfDegree_Hourly_1847&lt;/h4&gt;
This dataset provides global hourly output predicted from the Simple Biosphere Model, Version 4.2 (SiB4), at a 0.5-degree spatial resolution covering the time period 2000 through 2018. SiB4 is a mechanistic land surface model that integrates heterogeneous land cover, environmentally responsive phenology, dynamic carbon allocation, and cascading carbon pools from live biomass to surface litter to soil organic matter. Hourly output includes carbon fluxes, carbonyl sulfide (COS) fluxes, gross primary production, ecosystem respiration, solar-induced fluorescence (SIF), top-layer soil temperature and moisture, vegetation stress, photosynthetically active radiation (PAR), leaf and canopy-level carbon-dioxide partial pressures, and canopy conductance. The SiB4 output is per plant functional type (PFT) within each 0.5-degree grid cell. SiB4 partitions variable output to 15 PFTs in each grid cell that are indexed by the &amp;quot;npft&amp;quot; dimension (01-15) in each data file. The PFT three-character abbreviations (&amp;quot;pft_names&amp;quot; variable) are listed in the same order as the &amp;quot;npft&amp;quot; dimension. To combine the PFT-specific output into grid cell totals, users must compute the area-weighted mean across the vector of PFT-specific values for each cell. Fractional areal coverages are given in the &amp;quot;pft_area&amp;quot; variable for each cell.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sib4_global_halfdegree_monthly_1848&quot;&gt;SiB4_Global_HalfDegree_Monthly_1848&lt;/h4&gt;
This dataset provides global monthly output predicted by the Simple Biosphere Model, Version 4.2 (SiB4), at a 0.5-degree spatial resolution covering the time period 2000 through 2018. SiB4 is a mechanistic land surface model that integrates heterogeneous land cover, environmentally responsive phenology, dynamic carbon allocation, and cascading carbon pools from live biomass to surface litter to soil organic matter. Monthly output includes carbon, carbonyl sulfide (COS), and energy fluxes; solar-induced fluorescence (SIF); carbon pools; soil moisture and temperatures in the top three layers; total column soil water and plant available water; and environmental potentials used to scale photosynthesis. The SiB4 output is per plant functional type (PFT) within each 0.5-degree grid cell. SiB4 partitions variable output to 15 PFTs in each grid cell that are indexed by the &amp;quot;npft&amp;quot; dimension (01-15) in each data file. The PFT three-character abbreviations (&amp;quot;pft_names&amp;quot; variable) are listed in the same order as the &amp;quot;npft&amp;quot; dimension. To combine the PFT-specific output into grid cell totals, users must compute the area-weighted mean across the vector of PFT-specific values for each cell. Fractional areal coverages are given in the &amp;quot;pft_area&amp;quot; variable for each cell.
&lt;br&gt;&lt;h4 id&#x3D;&quot;crops_sif_vegindices_il_ne_2136&quot;&gt;Crops_SIF_VegIndices_IL_NE_2136&lt;/h4&gt;
This dataset contains half-hourly ground solar-induced chlorophyll fluorescence (SIF) and vegetation indices including NDVI, EVI, Red edge chlorophyll index, green chlorophyll index, and photochemical reflectance index at seven crop sites in Nebraska and Illinois for the period 2016-2021. Four sites were located at Eddy Covariance (EC) tower sites (sites US-Ne2, US-Ne3, US-UiB, and US-UiC), and three sites were located on private farms (sites Reifsteck, Rund, and Reinhart). The sites were either miscanthus, corn-soybean rotation or corn-corn-soybean rotation. The spectral data for SIF retrieval and hyperspectral reflectance for vegetation index calculation were collected by the FluoSpec2 system, installed near planting, and uninstalled after harvest to collect whole growing-season data. Raw nadir SIF at 760 nm from different algorithms (sFLD, 3FLD, iFLD, SFM) are included. SFM_nonlinear and SFM_linear represent the Spectral fitting method (SFM) with the assumption that fluorescence and reflectance change with wavelength non-linearly and linearly, respectively. Additional data include two SIF correction factors including calibration coefficient adjustment factor (f_cal_corr_QEPRO) and upscaling nadir SIF to eddy covariance footprint factor (ratio_EC footprint, SIF pixel), and measured FPAR from quantum sensors and Rededge NDVI calculated FPAR. The data are provided in comma-separated values (CSV) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;wetland_soil_carbonstocks_wa_2249&quot;&gt;Wetland_Soil_CarbonStocks_WA_2249&lt;/h4&gt;
This dataset contains estimates of soil organic carbon stocks and wetland intrinsic potential (WIP) across the Hoh River Watershed in the Olympic Peninsula, WA, USA in 2012-2013. Estimates were derived from an equation based on wetland intrinsic potential and geology type (Stewart et al., 2023). Wetland intrinsic potential estimates the likelihood that that an area is a wetland using a random forest model built on vegetation, hydrology, and soil data (Halabisky et al., 2022). SOC estimates at 1 m and 30 cm, SOC standard deviations, and WIP are presented in Cloud-Optimized GeoTIFF (.tif) format at 4-m resolution. Also included are 36 field observations of SOC collected from 2020-08-01 to 2022-06-29. These are contained in a comma separated (.csv) file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_soc_mexico_1754&quot;&gt;CMS_SOC_Mexico_1754&lt;/h4&gt;
This dataset provides an estimate of soil organic carbon (SOC) in the top one meter of soil across Mexico at a 90-m resolution for the period 1999-2009. Carbon estimates (kg/m2) are based on a field data collection of 2852 soil profiles by the National Institute for Statistics and Geography (INEGI). The profile data were used for the development of a predictive model along with a set of environmental covariates that were harmonized in a regular grid of 90x90 m2 across all Mexican states. The base of reference was the digital elevation model (DEM) of the INEGI at 90-m spatial resolution. A model ensemble of regression trees with a recursive elimination of variables explained 54% of the total variability using a cross-validation technique of independent samples. The error associated with the predictive model estimates of SOC is provided. A summary of the total estimated SOC per state, statistical description of the modeled SOC data, and the number of pixels modeled for each state are also provided.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cms_soc_mexico_conus_1737&quot;&gt;CMS_SOC_Mexico_CONUS_1737&lt;/h4&gt;
This dataset provides two sets of gridded estimates of estimated soil organic carbon (SOC) and associated uncertainties for 0-30 cm topsoil layer in kg SOC/m2 at 250-m resolution across Mexico and the conterminous USA (CONUS). The first set of gridded SOC estimates, for the period 1991-2010, were derived using multi-source SOC field data and multiple environmental variables representative of the soil forming environment coupled with a machine learning approach (i.e., simulated annealing) and regression tree ensemble modeling for optimized SOC prediction. Predictions of gridded SOC and uncertainty based on multiple bulk density (BD) pedotransfer functions (PFTs) are also included. The second set of gridded SOC estimates, for the period 2009-2011, were derived from two fully independent validation field datasets from across both countries. Note that the same environmental variables and modeling approach used for the first set of estimates were applied to the second set to assess the models&amp;#39; sensitivity to multiple SOC data sources. The SOC field data for the first set of estimates are provided in this dataset and the other data sources, including the two independent validation field datasets, are referenced.
&lt;br&gt;&lt;h4 id&#x3D;&quot;country_soc_latin_america_1615&quot;&gt;Country_SOC_Latin_America_1615&lt;/h4&gt;
This dataset provides 5 x 5 km gridded estimates of soil organic carbon (SOC) across Latin America that were derived from existing point soil characterization data and compiled environmental prediction factors for SOC. This dataset is representative for the period between 1980 to 2000s corresponding with the highest density of observations available in the WoSIS system and the covariates used as prediction factors for soil organic carbon across Latin America. SOC stocks (kg/m2) were estimated for the SOC and bulk density point measurements and a spatially explicit measure of the SOC estimation error was also calculated. A modeling ensemble, using a linear combination of five statistical methods (regression Kriging, random forest, kernel weighted nearest neighbors, partial least squared regression and support vector machines) was applied to the SOC stock data at (1) country-specific and (2) regional scales to develop gridded SOC estimates (kg/m2) for all of Latin America. Uncertainty estimates are provided for the two model predictions based on independent model residuals and their full conditional response to the SOC prediction factors.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tidal_wetland_soil_carbon_1612&quot;&gt;Tidal_Wetland_Soil_Carbon_1612&lt;/h4&gt;
This dataset provides modeled estimates of soil carbon stocks for tidal wetland areas of the Conterminous United States (CONUS) for the period 2006-2010. Wetland areas were determined using both 2006-2010 Coastal Change Analysis Program (C-CAP) raster maps and the National Wetlands Inventory (NWI) vector data. All 30 x 30-meter C-CAP pixels were extracted that are coded as estuarine emergent, scrub/shrub, or forested in either 2006 or 2010. A soil database for model fitting and validation was compiled from 49 different studies with spatially explicit empirical depth profile data and associated metadata, totaling 1,959 soil cores from 18 of the 22 coastal states. Reported estimates of carbon stocks were derived with modeling approaches that included (1) applying a single average carbon stock value from the compiled soil core data, (2) applying models fit using the empirical data and applied spatially using soil, vegetation and salinity maps, (3) relying on independently generated soil carbon maps from The United States Department of Agriculture (USDA)&amp;#39;s Soil Survey Geographic Database (SSURGO), and the NWI that intersected with mapped tidal wetlands, and (4) using a version of SSURGO bias-corrected for bulk density. Comparisons of uncertainty, precision, and accuracy among these four approaches are also provided.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tree_canopy_cover_mexico_2137&quot;&gt;Tree_Canopy_Cover_Mexico_2137&lt;/h4&gt;
The data set provides multi-year (2016-2018) percent tree cover (TC) estimates for entire Mexico at 30 m spatial resolution. The TC data (hereafter, NEX-TC) was derived from the 30 m Landsat Collection 1 product and a hierarchical deep learning approach (U-Net) developed in a previous CMS effort for the conterminous United States (CONUS) (Park et al., 2022). The hierarchical U-Net framework first developed a U-Net model for very high-resolution aerial images (NAIP) using training labels derived from previous work based on an interactive image segmentation tool and iterative updates with expert knowledge (Basu et al., 2015). The developed NAIP U-Net model and NAIP data produced 1-m NAIP TC across all lower 48 CONUS states. A Landsat U-Net model was developed for multi-year and large-scale TC mapping based on the very high-resolution NAIP TC made in the earlier stage. The Landsat U-Net model developed was adopted over the CONUS for testing its transferability, validation, and improvement across Mexico. This dataset provides national-scale percent tree cover estimates over Mexico and can be helpful for studies of carbon cycling, land cover and land use change, etc. The team has been working on improving temporal stability of the product and will update the product once the next version is ready to be shared.
&lt;br&gt;&lt;h4 id&#x3D;&quot;high_res_tidal_marsh_veg_1609&quot;&gt;High_Res_Tidal_Marsh_Veg_1609&lt;/h4&gt;
This dataset provides maps of tidal marsh green vegetation, non-vegetation, and open water for six estuarine regions of the conterminous United States: Cape Cod, MA; Chesapeake Bay, MD, Everglades, FL; Mississippi Delta, LA; San Francisco Bay, CA; and Puget Sound, WA. Maps were derived from current National Agriculture Imagery Program data (2013-2015) using object-based classification for estuarine and palustrine emergent tidal marshes as indicated by a modified NOAA Coastal Change Analysis Program (C-CAP) map. These 1m resolution maps were used to calculate the fraction of green vegetation within 30m Landsat pixels for the same tidal marsh regions and these data are provided in a related dataset.
&lt;br&gt;&lt;h4 id&#x3D;&quot;wetland_salinity_maps_2392&quot;&gt;Wetland_Salinity_Maps_2392&lt;/h4&gt;
This dataset provides gridded average annual wetland salinity concentrations in practical salinity units (PSU) at 30-meter resolution within 24 coastal estuary sites in the United States predicted for 2020. Salinity in estuaries can serve as a proxy for sulfate concentration, which can inhibit methanogenesis. Data were derived from a hybrid approach to mapping salinity as a continuous variable using a combination of physical watershed and stream characteristics, optical remote sensing based on vegetation characteristics, and climate variables. Data are provided in cloud-optimized GeoTIFF format covering 33 Hydrologic Unit Code 8-digit (HUC8) watersheds to the extent of palustrine and estuarine wetlands as defined by NOAA&amp;#39;s 2016 Coastal Change Analysis Program (C-CAP) Coastal Land Cover layer. Additionally, model outputs are provided in comma separated values (CSV) files, and code scripts are provided in a compressed (.zip) file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.ornldaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA COMEX Project</title>
      <link>https://registry.opendata.aws/nasa-comex</link>
      <guid>https://registry.opendata.aws/nasa-comex</guid>
      <description>An inventory of NASA&amp;#39;s airborne and field campaigns for Earth Science
&lt;br&gt;&lt;h4 id&#x3D;&quot;comex_amog_mobile_air_surveys_2387&quot;&gt;COMEX_AMOG_Mobile_Air_Surveys_2387&lt;/h4&gt;
This dataset provides AutoMObile trace Gas Surveyor (AMOG) in situ relevant datasets collected during the CO2 and Methane EXperiment (COMEX) field campaign and afterwards. COMEX was conducted in the summer and fall 2014 to study strong methane, CH4, sources in S. California including animal husbandry, fossil fuel industrial (FFI) production, petroleum refining, landfills, and natural geological formations. The AMOG Surveyor is a mobile air quality laboratory built into a passenger car. AMOG Surveyor uses an asynchronous logging system based on a NMEA tagging protocol, termed a tagstream. Analyzers provide data at rates from 5 Hz to 0.016 Hz. Tagstream data are timestamped based on the time of the analyzer measurement, which does not take into account the air sample travel time in sample tubes and analyzers, termed layback time. This dataset contains Level 0 (L0) and Level 1 (L1) data. L0 data were analyzed and sensor data interpolated to a uniform timebase of 5 Hz, correcting for the layback time, the time of flight for air samples in the sample tube and analyzers. L1 data include true winds (corrected for vehicle velocity), with filtering of outliers, non-physical data, and gap filling. The data files are in HDF-5 (.h5) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;comex_aviris_classic_flights_2343&quot;&gt;COMEX_AVIRIS_Classic_Flights_2343&lt;/h4&gt;
This dataset lists flight lines and provides data access links and contextual flight information for a subset of the AVIRIS-Classic Facility Instrument Collection that are associated with the CO2 and MEthane eXperiment (COMEX) Project. The COMEX Project was carried out May through September, 2014. AVIRIS-Classic Facility Instrument data are otherwise not replicated in this dataset. The COMEX Project utilized several measurement capabilities including the AVIRIS-Classic airborne facility instrument data to demonstrate that methane emissions associated with fossil fuel production activities in the Los Angeles, California area were of sufficient magnitude and size for space-based observations. These lists of the associated COMEX flights from the AVIRIS-Classic Facility Instrument provide flight lines and access information for the Level 1B Calibrated Radiance data and the Level 2 Calibrated Reflectance data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;comex_aviris_ng_flights_2342&quot;&gt;COMEX_AVIRIS_NG_Flights_2342&lt;/h4&gt;
This dataset lists flight lines and provides data access links and contextual flight information for a subset of the AVIRIS-NG Facility Instrument Collection that are associated with the CO2 and MEthane eXperiment (COMEX) Project. The COMEX Project was carried out May through September, 2014. AVIRIS-NG Facility Instrument data are otherwise not replicated in this dataset. The COMEX Project utilized several measurement capabilities including the AVIRIS-NG airborne facility instrument data to demonstrate that methane emissions associated with fossil fuel production activities in the Los Angeles, California area were of sufficient magnitude and size for space-based observations. These lists of the associated COMEX flights from the AVIRIS-NG Facility Instrument provide flight lines and access information for the Level 1B Calibrated Radiance data and the Level 2 Calibrated Reflectance data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;comex_ajax_co2_ch4_2347&quot;&gt;COMEX_AJAX_CO2_CH4_2347&lt;/h4&gt;
This dataset provides information to access NASA Earthdata published flight data and flight information collected by the Alpha Jet Atmospheric eXperiment (AJAX) and associated with the COMEX project in 2014-2015. The file lists information for COMEX-related datasets that has been subsetted from AJAX collections archived through NASA&amp;#39;s Atmospheric Science Data Center. AJAX data are not otherwise replicated in this dataset. AJAX is a partnership between NASA&amp;#39;s Ames Research Center and H211, L.L.C., which conducted in-situ measurements over California, Nevada, and the coastal Pacific in support of satellite validation. During COMEX data collection, a Picarro greenhouse gas (GHG) sensor was mounted on an Alpha Jet, a tactical strike fighter developed by Dassault-Breguet and Dornier through a German-French NATO collaboration. The GHG sensor made repeat measurements in California and Nevada. In situ data included measurements of CO2, CH4, and H2O at 2 Hz or CH4 and H2O at 10 Hz with a strategy of characterizing atmospheric structure over ocean and land, and vertical profiles to at least 5000 m. Ancillary data, including O3, formaldehyde, and meteorological profiles, were also collected. This dataset provides filenames, spatiotemporal bounds, and download URLs for accessing these in situ data. This information is provided in comma separated values (CSV) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;comex_longwaveinfrared_imagery_2331&quot;&gt;COMEX_LongwaveInfrared_Imagery_2331&lt;/h4&gt;
This dataset provides calibrated at-sensor radiance, retrieved surface brightness temperature, and adaptive coherence estimator (ACE) detection imagery of methane, and a limited number of auxiliary gases collected with the Aerospace Corporation&amp;#39;s Mako airborne longwave-IR hyperspectral imager flown during July 22-25, 2014 over a variety of methane generating sites in southern and central California (CA), U.S. These sites included animal husbandry and oil/gas production facilities. Specific study areas included the Coal Oil Point marine seep field off of Goleta, CA, the Kern River oil field complex at Bakersfield, CA, and the extensive stockyards in Chino, CA. The Kern River complex was acquired at 1-m ground sampling distance (GSD), while the other study areas were at 2-m GSD. Levels 1-3 data include single whisk data cubes (L1); at-sensor radiance and sensor performance (L2); surface brightness temperature and ACE detections for specific gases (L3). The data were collected in support of the NASA/ESA COMEX (CO2 and Methane EXperiment) campaign. The data are provided in ENVI and comma separated values (CSV) formats. Quicklook images are included for flight lines and molecule specific detections.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.ornldaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA COWVR-TEMPEST/STP-H8 Project</title>
      <link>https://registry.opendata.aws/nasa-cowvr-tempest-stp-h8</link>
      <guid>https://registry.opendata.aws/nasa-cowvr-tempest-stp-h8</guid>
      <description>This data set includes satellite-based observations of calibrated, geo-located antenna temperature and brightness temperatures, along with the sensor telemetry used to derive those values. Brightness temperatures are derived from the microwave band frequencies 18.7 GHz, 23.8 GHz, and 34.5 GHz. This product is best suited for a cal/val user or sensor expert. These level 1c measurements make up the temperature sensor data record (TSDR) from the COWVR (Compact Ocean Wind Vector Radiometer) sensor aboard the international space station (ISS), starting in January 2022 forward-streaming to PO.DAAC till the planned mission end in December 2024. Its swath width is 1012 km and spatial resolution is &amp;lt;35 km. Data files in HDF5 format are available at roughly hourly frequency (the ISS orbit period is ~90 minutes), although note that the coverage shown in the thumbnail is for a full day. Files include calibration and flag data in addition to brightness temperatures. Version 10.0 is the first public release, and is named as such to be consistent with the internal version numbers of the project team prior to release &lt;br&gt;&lt;br&gt; The COWVR sensor is a fully polarimetric, conically imaging microwave radiometer for measuring ocean surface wind vectors. It operates nominally on-orbit aboard the ISS and data are non-sun-synchronous. It was deployed as part of the Space Test Program - Houston 8 (STP-H8) technology demonstration mission. A successful COWVR mission will demonstrate a lower-cost sensor architecture (e.g. in comparison to WindSat) for providing imaging passive microwave data, including ocean surface vector wind products for the Department of Defense (DoD). COWVR was provided by the Jet Propulsion Laboratory and flown by the United States Space Force, Space Systems Command, Development Corps for Innovation and Prototyping.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cowvr_stph8_l2_edr_v100&quot;&gt;COWVR_STPH8_L2_EDR_V10.0&lt;/h4&gt;
This dataset includes satellite-based observations of geolocated surface wind vectors, precipitable water vapor, and integrated cloud liquid water, as well as the microwave brightness temperatures used to derive them. Theses measurements make up the environmental data record (EDR) from the COWVR (Compact Ocean Wind Vector Radiometer) sensor aboard the international space station (ISS), beginning in January 2022 with forward-streaming to PO.DAAC. Data over the satellite swath are available in HDF5 format with roughly one file per hour (the ISS orbit period is ~90 minutes), and coverage shown in the thumbnail is for a full day. Spatial resolution is roughly 35 km. The file metadata formats may be different than what an average user is familiar with – please see the User Guide to learn more. Version 10.0 is the first public release, and is named as such to be consistent with the internal version numbering of the project team prior to release. &lt;br&gt;&lt;br&gt; The COWVR sensor is a fully polarimetric, conically imaging microwave radiometer for measuring ocean surface wind vectors. It operates nominally on-orbit aboard the ISS and data are non-sun-synchronous. It was deployed as part of the Space Test Program - Houston 8 (STP-H8) technology demonstration mission. A successful COWVR mission will demonstrate a lower-cost sensor architecture (e.g. in comparison to WindSat) for providing imaging passive microwave data, including ocean surface vector wind products for the Department of Defense (DoD). COWVR was provided by the Jet Propulsion Laboratory and flown by the United States Space Force, Space Systems Command, Development Corps for Innovation and Prototyping.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tempest_stph8_l1_tsdr_v100&quot;&gt;TEMPEST_STPH8_L1_TSDR_V10.0&lt;/h4&gt;
This dataset includes satellite-based observations of calibrated, geo-located antenna temperature and brightness temperatures, along with the sensor telemetry used to derive those values. Brightness temperatures are derived from the microwave band frequencies 87, 164, 174, 178 and 181 GHz. This product is best suited for a cal/val user or sensor expert. These level 1c measurements make up the temperature sensor data record (TSDR) from the TEMPEST (Temporal Experiment for Storms and Tropical Systems) sensor aboard the international space station (ISS), starting in January 2022 forward-streaming to PO.DAAC till the planned mission end in December 2024. TEMPEST swath width is 1400 kilometers and resolution at nadir is 25 km for the 87 GHz channel and 13 km for the 180 GHz channels. Data files in HDF5 format are available at roughly hourly frequency (the ISS orbit period is ~90 minutes), although note that the coverage shown in the thumbnail is for a full day. Files include calibration and flag data in addition to brightness temperatures. Version 10.0 is the first public release, and is named as such to be consistent with the internal version numbering of the project team prior to release. &lt;br&gt;&lt;br&gt; The TEMPEST instrument is a microwave radiometer deployed as part of the Space Test Program - Houston 8 (STP-H8) technology demonstration mission, with the primary objective of tropical cyclone intensity tracking. It operates nominally on-orbit aboard the ISS and data are non-sun-synchronous. A successful mission will demonstrate a lower-cost, lighter-weight sensor architecture for providing microwave data. TEMPEST was provided by the Jet Propulsion Laboratory and flown by the United States Space Force, Space Systems Command, Development Corps for Innovation and Prototyping.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://archive.podaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA CSDA Project</title>
      <link>https://registry.opendata.aws/nasa-csda</link>
      <guid>https://registry.opendata.aws/nasa-csda</guid>
      <description>The GeoEye-1 Level 1B Multispectral 4-Band L1B Satellite Imagery collection contains satellite imagery acquired from Maxar Technologies (formerly known as DigitalGlobe) by the Commercial Smallsat Data Acquisition (CSDA) Program. Imagery is collected by the GeoEye-1 satellite using the GeoEye-1 Imaging System across the global land surface from September 2008 to the present. This satellite imagery is in the visible and near-infrared waveband range with data in the blue, green, red, and near-infrared wavelengths. The imagery has a spatial resolution of 1.84m at nadir (1.65m before summer 2013) and has a temporal resolution of approximately 3 days. The data are provided in National Imagery Transmission Format (NITF) and GeoTIFF formats. This level 1B data is sensor corrected and is an un-projected (raw) product. The data potentially serve a wide variety of applications that require high resolution imagery. Data access is restricted based on a National Geospatial-Intelligence Agency (NGA) license, and investigators must be approved by the CSDA Program.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ge01_pan_l1b&quot;&gt;GE01_Pan_L1B&lt;/h4&gt;
The GeoEye-1 Level 1B Panchromatic Imagery collection contains satellite imagery acquired from Maxar Technologies (formerly known as DigitalGlobe) by the Commercial Smallsat Data Acquisition (CSDA) Program. Imagery is collected by the GeoEye-1 satellite using the GeoEye-1 Imaging System across the global land surface from September 2008 to the present. This data product includes panchromatic imagery with a spatial resolution of 0.46m at nadir (0.41m before summer 2013) and a temporal resolution of approximately 3 days. The data are provided in National Imagery Transmission Format (NITF) and GeoTIFF formats. This level 1B data is sensor corrected and is an un-projected (raw) product. The data potentially serve a wide variety of applications that require high resolution imagery. Data access is restricted based on a National Geospatial-Intelligence Agency (NGA) license, and investigators must be approved by the CSDA Program.
&lt;br&gt;&lt;h4 id&#x3D;&quot;wv01_pan_l1b&quot;&gt;WV01_Pan_L1B&lt;/h4&gt;
The WorldView-1 Level 1B Panchromatic Imagery collection contains satellite imagery acquired from Maxar Technologies (formerly known as DigitalGlobe) by the Commercial Smallsat Data Acquisition (CSDA) Program. Panchromatic imagery is collected by the DigitalGlobe WorldView-1 satellite using the WorldView-60 camera across the global land surface from September 2007 to the present. Data have a spatial resolution of 0.5 meters at nadir and a temporal resolution of approximately 1.7 days. The data are provided in National Imagery Transmission Format (NITF) and GeoTIFF formats. This level 1B data is sensor corrected and is an un-projected (raw) product. The data potentially serve a wide variety of applications that require high resolution imagery. Data access is restricted based on a National Geospatial-Intelligence Agency (NGA) license, and investigators must be approved by the CSDA Program.
&lt;br&gt;&lt;h4 id&#x3D;&quot;wv02_msi_l1b&quot;&gt;WV02_MSI_L1B&lt;/h4&gt;
The WorldView-2 Level 1B Multispectral 8-Band Imagery collection contains satellite imagery acquired from Maxar Technologies (formerly known as DigitalGlobe) by the Commercial Smallsat Data Acquisition (CSDA) Program. Imagery is collected by the DigitalGlobe WorldView-2 satellite using the WorldView-110 camera across the global land surface from October 2009 to the present. This satellite imagery is in the visible and near-infrared waveband range with data in the coastal, blue, green, yellow, red, red edge, and near-infrared (2 bands) wavelengths. It has a spatial resolution of 1.85m at nadir and a temporal resolution of approximately 1.1 days. The data are provided in National Imagery Transmission Format (NITF) and GeoTIFF formats. This level 1B data is sensor corrected and is an un-projected (raw) product. The data potentially serve a wide variety of applications that require high resolution imagery. Data access is restricted based on a National Geospatial-Intelligence Agency (NGA) license, and investigators must be approved by the CSDA Program.
&lt;br&gt;&lt;h4 id&#x3D;&quot;wv02_pan_l1b&quot;&gt;WV02_Pan_L1B&lt;/h4&gt;
The WorldView-2 Level 1B Panchromatic Imagery collection contains satellite imagery acquired from Maxar Technologies (formerly known as DigitalGlobe) by the Commercial Smallsat Data Acquisition (CSDA) Program. Imagery is collected by the DigitalGlobe WorldView-2 satellite using the WorldView-110 camera across the global land surface from October 2009 to the present. This data product includes panchromatic imagery with a spatial resolution of 0.46m and a temporal resolution of approximately 1.1 days. The data are provided in National Imagery Transmission Format (NITF) and GeoTIFF formats. This level 1B data is sensor corrected and is an un-projected (raw) product. The data potentially serve a wide variety of applications that require high resolution imagery. Data access is restricted based on a National Geospatial-Intelligence Agency (NGA) license, and investigators must be approved by the CSDA Program.
&lt;br&gt;&lt;h4 id&#x3D;&quot;wv02_msi_l2a&quot;&gt;WV02_MSI_L2A&lt;/h4&gt;
The WorldView-2 Level 2A Multispectral 8-Band Imagery collection contains satellite imagery acquired from Maxar Technologies (formerly known as DigitalGlobe) by the Commercial Smallsat Data Acquisition (CSDA) Program. Imagery is collected by the DigitalGlobe WorldView-2 satellite using the WorldView-110 camera across the global land surface from October 2009 to the present. This satellite imagery is in the visible and near-infrared waveband range with data in the coastal, blue, green, yellow, red, red edge, and near-infrared (2 bands) wavelengths. It has a spatial resolution of 1.85m at nadir and a temporal resolution of approximately 1.1 days. The data are provided in National Imagery Transmission Format (NITF) and GeoTIFF formats. These level 2A data have been processed and undergone radiometric correction, sensor correction, projected to a plane using a map projection and datum, and has a coarse DEM applied. The data potentially serve a wide variety of applications that require high resolution imagery. Data access is restricted based on a National Geospatial-Intelligence Agency (NGA) license, and investigators must be approved by the CSDA Program.
&lt;br&gt;&lt;h4 id&#x3D;&quot;wv03_msi_l1b&quot;&gt;WV03_MSI_L1B&lt;/h4&gt;
The WorldView-3 Level 1B Multispectral 8-Band Imagery collection contains satellite imagery acquired from Maxar Technologies (formerly known as DigitalGlobe) by the Commercial Smallsat Data Acquisition (CSDA) Program. Imagery is collected by the DigitalGlobe WorldView-3 satellite using the WorldView-110 camera across the global land surface from August 2014 to the present. This satellite imagery is in a range of wavebands with data in the coastal, blue, green, yellow, red, red edge, and near-infrared (2 bands) wavelengths. The imagery has a spatial resolution of 1.24m at nadir and a temporal resolution of less than one day. The data are provided in National Imagery Transmission Format (NITF). This level 1B data is sensor corrected and is an un-projected (raw) product. The data potentially serve a wide variety of applications that require high resolution imagery. Data access is restricted based on a National Geospatial-Intelligence Agency (NGA) license, and investigators must be approved by the CSDA Program.
&lt;br&gt;&lt;h4 id&#x3D;&quot;wv03_msi_l2a&quot;&gt;WV03_MSI_L2A&lt;/h4&gt;
The WorldView-3 Level 2A Multispectral 8-Band Imagery collection contains satellite imagery acquired from Maxar Technologies (formerly known as DigitalGlobe) by the Commercial Smallsat Data Acquisition (CSDA) Program. Imagery is collected by the DigitalGlobe WorldView-3 satellite using the WorldView-110 camera across the global land surface from August 2014 to the present. This satellite imagery is in a range of wavebands with data in the coastal, blue, green, yellow, red, red edge, and near-infrared (2 bands) wavelengths. The imagery has a spatial resolution of 1.24m at nadir and a temporal resolution of less than one day. The data are provided in National Imagery Transmission Format (NITF). These level 2A data have been processed and undergone radiometric correction, sensor correction, projected to a plane using a map projection and datum, and has a coarse DEM applied. The data potentially serve a wide variety of applications that require high resolution imagery. Data access is restricted based on a National Geospatial-Intelligence Agency (NGA) license, and investigators must be approved by the CSDA Program.
&lt;br&gt;&lt;h4 id&#x3D;&quot;wv04_msi_l1b&quot;&gt;WV04_MSI_L1B&lt;/h4&gt;
The WorldView-4 Multispectral 4-Band Imagery collection contains satellite imagery acquired from Maxar Technologies (formerly known as DigitalGlobe) by the Commercial Smallsat Data Acquisition (CSDA) Program. Imagery was collected by the DigitalGlobe WorldView-4 satellite using the SpaceView-110 camera across the global land surface from December 2016 to January 2019. This satellite imagery is in the visible and near-infrared waveband range with data in the blue, green, red, and near-infrared wavelengths. The multispectral imagery has a spatial resolution of 1.24m at nadir and has a temporal resolution of approximately 1.1 days. The data are provided in National Imagery Transmission Format (NITF) and GeoTIFF formats. This level 1B data is sensor corrected and is an un-projected (raw) product. The data potentially serve a wide variety of applications that require high resolution imagery. Data access is restricted based on a Maxar End User License Agreement for Worldview 4 imagery and investigators must be approved by the CSDA Program.
&lt;br&gt;&lt;h4 id&#x3D;&quot;wv04_pan_l1b&quot;&gt;WV04_Pan_L1B&lt;/h4&gt;
The WorldView-4 Panchromatic Imagery collection contains satellite imagery acquired from Maxar Technologies (formerly known as DigitalGlobe) by the Commercial Smallsat Data Acquisition (CSDA) Program. Imagery was collected by the DigitalGlobe WorldView-4 satellite using the WorldView-110 camera across the global land surface from December 2016 to January 2019. This data product includes panchromatic imagery with a spatial resolution of 0.31m at nadir and a temporal resolution of approximately 1.1 days. The data are provided in National Imagery Transmission Format (NITF) and GeoTIFF formats. This level 1B data is sensor corrected and is an un-projected (raw) product. The data potentially serve a wide variety of applications that require high resolution imagery. Data access is restricted based on a Maxar End User License Agreement for Worldview 4 imagery and investigators must be approved by the CSDA Program.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.csdap.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA CWIC Project</title>
      <link>https://registry.opendata.aws/nasa-cwic</link>
      <guid>https://registry.opendata.aws/nasa-cwic</guid>
      <description>The The MODIS Near Real Time (NRT) product, MOD09Q1N provides Band 1 and 2 data at 250 meter resolution in a daily rolling 8-day gridded level-3 product in the Sinusoidal projection. Each MOD09Q1N pixel contains the best possible L2G observation during an 8-day period as selected on the basis of high observation coverage low view angle the absence of clouds or cloud shadow and aerosol loading. Science Data Sets provided for this product include reflectance values for Bands 1 and 2 and a quality rating.
&lt;br&gt;&lt;h4 id&#x3D;&quot;scamsn6im&quot;&gt;SCAMSN6IM&lt;/h4&gt;
The SCAMSN6IM data product consists of images of brightness temperatures, water vapor and temperature on 70 mm film strips from the Nimbus-6 Scanning Microwave Spectrometer. Each display contains eight vertical strips of data from one orbit. All strips have the same geographic coverage, but each represents a different parameter. The first three are brightness temperatures for channels 2 (31.65 GHz) and 3 (52.85 GHz) and their differences. The next two represent retrieved water vapor and liquid water from clouds or precipitation over the oceans, respectively. The remaining three strips on the right represent inverted mean temperatures for atmospheric layers 1000-500 mbar, 500-250 mbar, and 250-100 mbar, respectively. The first five parameters are displayed in 18-step gray levels, the values of which can be found in a table in each of the first five volumes of &amp;quot;The Nimbus 6 Data Catalog.&amp;quot; The last three parameters are displayed by contour bands (labeled on the side) that are spaced 4 K apart. Spatial resolution on the ground for the parameters varies from 145 km at nadir to 330 km at the scan extremes. The images are saved as TIFF digital files. About 3-5 months of images are archived into a ZIP file. Additional information can be found in section 2.4.1 of &amp;quot;The Nimbus 6 User&amp;#39;s Guide.&amp;quot; The SCAMS experiment on Nimbus-6 is a follow on to the successful Nimbus-5 NEMS experiment. SCAMS continuously monitored emitted microwave radiation at frequencies of 22.235, 31.65, 52.85, 53.85 and 55.45 GHz. The three channels near the 5.0-mm oxygen absorption band were used primarily to deduce atmospheric temperature profiles. The two channels near 10 mm permitted water vapor and cloud water content over calm oceans to be estimated separately. The instrument, a Dicke-superheterodyne type, scanned +/- 45 degrees normal to the orbital plane with a 10 degree field of view. The three oxygen channels shared common signal and reference antennas. Both water vapor channels had their own signals and reference antennas. The absolute rms accuracy of the oxygen channels was better than 2 Kelvin and that of the water vapor channels better than 1 Kelvin. The SCAMS Principal Investigator was Prof. David H. Staelin from MIT. The Nimbus-6 SCAMS images are available from June 15, 1975 (day of year 166) through May 31, 1976 (day of year 152). This product was previously available from the NSSDC with the identifier ESAD-00200 (old ID 75-052A-10B).
&lt;br&gt;&lt;h4 id&#x3D;&quot;tovsb5ng&quot;&gt;TOVSB5NG&lt;/h4&gt;
Level 3 parameters from HIRS/2 and MSU radiances using the Improved Initialization Inversion (3I) classification retrieval scheme by the Laboratoire de Meteorologie Dynamique (Ecole Polytechnique) averaged over 5 days and mapped on to a 1x1 degree grid. This data was run as part of the NASA TOVS Pathfinder project and designated as Path-B. This dataset contains data from the NOAA-10 satellite.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tovsbdng&quot;&gt;TOVSBDNG&lt;/h4&gt;
Level 3 parameters from HIRS/2 and MSU radiances using the Improved Initialization Inversion (3I) classification retrieval scheme by the Laboratoire de Meteorologie Dynamique (Ecole Polytechnique) averaged over 1 day and mapped on to a 1x1 degree grid. This data was run as part of the NASA TOVS Pathfinder project and designated as Path-B. This dataset contains data from the NOAA-10 satellite.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tovsbmng&quot;&gt;TOVSBMNG&lt;/h4&gt;
Level 3 parameters from HIRS/2 and MSU radiances using the Improved Initialization Inversion (3I) classification retrieval scheme by the Laboratoire de Meteorologie Dynamique (Ecole Polytechnique) averaged over 1 month and mapped on to a 1x1 degree grid. This data was run as part of the NASA TOVS Pathfinder project and designated as Path-B. This dataset contains data from the NOAA-10 satellite.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA CYGNSS Project</title>
      <link>https://registry.opendata.aws/nasa-cygnss</link>
      <guid>https://registry.opendata.aws/nasa-cygnss</guid>
      <description>This dataset contains the version 1.0 CYGNSS level 3 ocean microplastic concentration data record, which provides 18 netCDF files, each containing one month of daily gridded maps of microplastic number density (#/km^2). Microplastic concentration number density is indirectly estimated by an empirical relationship between ocean surface roughness and wind speed (Evans and Ruf, 2021). User caution is advised in regions containing independent, non-correlative factors affecting ocean surface roughness, such as anomalous atmospheric conditions within the Intertropical Convergence Zone, biogenic surfactants (such as algal blooms), oil spills, etc. This product reports microplastic concentration on a daily temporal and 0.25-degree latitude/longitude spatial grid with 30-day, 1 degree latitude/longitude feature resolution, as constrained by the binning and spatiotemporal averaging of the Mean Square Slope (MSS) anomaly (i.e., difference between measured and predicted ocean surface roughness for a given wind speed).
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l1_cal_raw_if_v10&quot;&gt;CYGNSS_L1_CAL_RAW_IF_V1.0&lt;/h4&gt;
The CYGNSS Level 1 Calibrated Raw IF Version 1.0 dataset is produced by the CYGNSS Science Team of the University of Michigan, and it contains the first release, Version 1.0, of the CYGNSS Calibrated Raw Intermediate Frequency (IF) based L1 Product. CYGNSS was launched on 15 December 2016, it is a NASA Earth System Science Pathfinder Mission that was launched with the purpose of collecting the first frequent space‐based measurements of surface wind speeds in the inner core of tropical cyclones. Originally made up of a constellation of eight micro-satellites, the observatories provide nearly gap-free Earth coverage using an orbital inclination of approximately 35° from the equator, with a mean (i.e., average) revisit time of seven hours and a median revisit time of three hours. &lt;br&gt;&lt;br&gt; This product includes several established signal coherence detectors, including the power-ratio P&lt;sub&gt;ratio&lt;/sub&gt;, complex zero-Doppler delay waveform and full entropy E&lt;sub&gt;full&lt;/sub&gt;, and a novel fast entropy detector E&lt;sub&gt;fast&lt;/sub&gt;. Both entropy detectors are provided with two temporal resolutions: 2 ms and 50 ms. Several scattered signal strength products are included: Signal-to-Noise Ratio SNR, reflected power P&lt;sub&gt;g&lt;/sub&gt;, reflectivity Γ, and Normalized Bistatic Radar Cross-Section NBRCS. Each of these products is derived using a coherent integration time of T&lt;sub&gt;c &lt;/sub&gt;&#x3D; 1 ms and incoherent integration times of N&lt;sub&gt;inc&lt;/sub&gt; &#x3D; 1000, 500, 250, 100, 50, and 2 ms. Signal strength time series at the shorter (2 and 50 ms) times provides excellent detection of land-water transitions in heterogeneous scenes. Delay Doppler Maps (DDMs) are also generated with high delay (∆τ &#x3D; 1/16 chip) and Doppler (∆f&#x3D; 50 Hz) resolution. This suite of coherence detection methods can be used to detect the presence of small inland water bodies.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l1_cdr_v10&quot;&gt;CYGNSS_L1_CDR_V1.0&lt;/h4&gt;
This Level 1 (L1) dataset contains the Version 1.0 Climate Data Record (CDR) of the geo-located Delay Doppler Maps (DDMs) calibrated into Power Received (Watts) and Bistatic Radar Cross Section (BRCS) expressed in units of m2 from the Delay Doppler Mapping Instrument aboard the CYGNSS satellite constellation. Other useful scientific and engineering measurement parameters include the DDM of Normalized Bistatic Radar Cross Section (NBRCS), the Delay Doppler Map Average (DDMA) of the NBRCS near the specular reflection point, and the Leading Edge Slope (LES) of the integrated delay waveform. The L1 dataset contains a number of other engineering and science measurement parameters, including sets of quality flags/indicators, error estimates, and bias estimates as well as a variety of orbital, spacecraft/sensor health, timekeeping, and geolocation parameters. At most, 8 netCDF data files (each file corresponding to a unique spacecraft in the CYGNSS constellation) are provided each day; under nominal conditions, there are typically 6-8 spacecraft retrieving data each day, but this can be maximized to 8 spacecraft under special circumstances in which higher than normal retrieval frequency is needed (i.e., during tropical storms and or hurricanes). Latency is approximately 2 months, depending on the availability of the MERRA wind speed reanalysis. The Version 1.0 CDR represents the first climate-quality release and is a collection of reanalysis products derived from the v2.1 Level 1 data. Calibration accuracy and long term stability are improved relative to the SDR v2.1 using a new trackwise correction algorithm which constrains the average value of the L1 data using MERRA-2 reanalysis wind speeds. Details of the algorithm are provide in the Trackwise Corrected CDR Algorithm Theoretical Basis Document. The CDR exhibits improved calibration accuracy and stability over v2.1. Trackwise correction is applied to the two primary CYGNSS L1 science data products the normalized bistatic radar cross section (NBRCS) and the leading edge slope of the Doppler-integrated delay waveform (LES). The correction compensates for variations in the transmit power level of the GPS signals measured by the CYGNSS bistatic radar receivers. By comparison, the v2.1 SDR L1 algorithm assumes a constant GPS transmit power, and variations in it can be misinterpreted as variations in the L1 data and in subsequent L2 science data products derived from them. The GPS constellation consists of several different satellite models (a.k.a. block types) and the level of transmit power variation differs between them. The more recent Block IIF models (which account for ~37% of the GPS constellation) have significantly larger variations than the older models and, for this reason, they have been screened out and not used to produce v2.1 L2 or L3 science data products. Trackwise correction eliminates the need for this screening so CDR L2 and L3 data products now include Block IIF samples. It should be noted that the trackwise correction algorithm cannot be successfully applied to all v2.1 SDR L1 data, so there is also some loss of samples that were present in v2.1. Overall, there is a significant increase in sampling and improvement in spatial coverage with the CDR products.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l1_cdr_v11&quot;&gt;CYGNSS_L1_CDR_V1.1&lt;/h4&gt;
This Level 1 (L1) dataset contains the Version 1.1 Climate Data Record (CDR) of the geo-located Delay Doppler Maps (DDMs) calibrated into Power Received (Watts) and Bistatic Radar Cross Section (BRCS) expressed in units of m2 from the Delay Doppler Mapping Instrument aboard the CYGNSS satellite constellation. Other useful scientific and engineering measurement parameters include the DDM of Normalized Bistatic Radar Cross Section (NBRCS), the Delay Doppler Map Average (DDMA) of the NBRCS near the specular reflection point, and the Leading Edge Slope (LES) of the integrated delay waveform. The L1 dataset contains a number of other engineering and science measurement parameters, including sets of quality flags/indicators, error estimates, and bias estimates as well as a variety of orbital, spacecraft/sensor health, timekeeping, and geolocation parameters. At most, 8 netCDF data files (each file corresponding to a unique spacecraft in the CYGNSS constellation) are provided each day; under nominal conditions, there are typically 6-8 spacecraft retrieving data each day, but this can be maximized to 8 spacecraft under special circumstances in which higher than normal retrieval frequency is needed (i.e., during tropical storms and or hurricanes). Latency is approximately 1 month, depending on the availability of the MERRA wind speed reanalysis. The Version 1.1 CDR is a collection of reanalysis products derived from the SDR v3.0 Level 1 data (&lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L1X30&quot;&gt;https://doi.org/10.5067/CYGNS-L1X30&lt;/a&gt; ). Calibration accuracy and long term stability are improved relative to SDR v3.0 using the same trackwise correction algorithm as was used by CDR v1.0 (&lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L1C10&quot;&gt;https://doi.org/10.5067/CYGNS-L1C10&lt;/a&gt; ), which was derived from SDR v2.1 Level 1 data (&lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L1X21&quot;&gt;https://doi.org/10.5067/CYGNS-L1X21&lt;/a&gt; ). Details of the algorithm are provided in the Trackwise Corrected CDR Algorithm Theoretical Basis Document. Trackwise correction is applied to the two primary CYGNSS L1 science data products, the normalized bistatic radar cross section (NBRCS) and the LES. The correction compensates for small errors in the Level 1 calibration, due e.g. to uncertainties in the GPS transmitting antenna gain patterns and the CYGNSS receiving antenna gain patterns. It should be noted that the trackwise correction algorithm cannot be successfully applied to all v3.0 SDR L1 data, so there is also some loss of samples that were present in v3.0.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l1_cdr_v12&quot;&gt;CYGNSS_L1_CDR_V1.2&lt;/h4&gt;
This Level 1 (L1) dataset contains the Version 1.2 Climate Data Record (CDR) of the geo-located Delay Doppler Maps (DDMs) calibrated into Power Received (Watts) and Bistatic Radar Cross Section (BRCS) expressed in units of m2 from the Delay Doppler Mapping Instrument aboard the CYGNSS satellite constellation. Other useful scientific and engineering measurement parameters include the DDM of Normalized Bistatic Radar Cross Section (NBRCS), the Delay Doppler Map Average (DDMA) of the NBRCS near the specular reflection point, and the Leading Edge Slope (LES) of the integrated delay waveform. The L1 dataset contains a number of other engineering and science measurement parameters, including sets of quality flags/indicators, error estimates, and bias estimates as well as a variety of orbital, spacecraft/sensor health, timekeeping, and geolocation parameters. At most, 8 netCDF data files (each file corresponding to a unique spacecraft in the CYGNSS constellation) are provided each day; under nominal conditions, there are typically 6-8 spacecraft retrieving data each day, but this can be maximized to 8 spacecraft under special circumstances in which higher than normal retrieval frequency is needed (i.e., during tropical storms and or hurricanes). Latency is approximately 1 week. The Version 1.2 CDR is a collection of reanalysis products derived from the SDR v3.1 Level 1 data (&lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L1X31&quot;&gt;https://doi.org/10.5067/CYGNS-L1X31&lt;/a&gt; ). Calibration accuracy and long term stability are improved relative to SDR v3.0 using the same trackwise correction algorithm as was used by CDR v1.1 (&lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L1C11&quot;&gt;https://doi.org/10.5067/CYGNS-L1C11&lt;/a&gt; ), which was derived from SDR v2.1 Level 1 data (&lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L1X21&quot;&gt;https://doi.org/10.5067/CYGNS-L1X21&lt;/a&gt; ). Details of the algorithm are provided in the Trackwise Corrected CDR Algorithm Theoretical Basis Document. Trackwise correction is applied to the two primary CYGNSS L1 science data products, the normalized bistatic radar cross section (NBRCS) and the LES. The correction compensates for small errors in the Level 1 calibration, due e.g. to uncertainties in the GPS transmitting antenna gain patterns and the CYGNSS receiving antenna gain patterns. It should be noted that the trackwise correction algorithm cannot be successfully applied to all v3.1 SDR L1 data, so there is also some loss of samples that were present in v3.1.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l1_full_ddm&quot;&gt;CYGNSS_L1_FULL_DDM&lt;/h4&gt;
This Level 1 (L1) dataset contains the Full Delay Doppler Map (DDM) sensor data from the Delay Doppler Mapping Instrument aboard the CYGNSS satellite constellation. The primary CYGNSS instrument, also known as the Delay-Doppler Mapping Instrument (DDMI), measures the incoming radio frequency (RF) streams from three input antenna channels (2 nadir oriented science antennas and one zenith oriented navigation antenna) and processes them in real time into DDMs, which are two-dimensional maps of the signal scattered from the Earth surface as a function of propagation time delay and Doppler frequency shift. DDMs are normally sampled over a restricted range of delay and Doppler values centered on the values at the specular point of reflection. The bit resolution of scattered signal strength is also truncated by a lossy data compression algorithm. Full DDMs are sampled over a wider range of delay and Doppler values and retain their full (lossless) bit resolution. Full DDM data records are typically 10-15 min in duration and are initiated by ground commands to coincide with an overpass by one of the spacecraft of a target area of interest.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l1_full_ddm_v30&quot;&gt;CYGNSS_L1_FULL_DDM_V3.0&lt;/h4&gt;
This Level 1 (L1) dataset contains the Version 3.0 (v3.0) Full Delay Doppler Map (DDM) sensor data from the Delay Doppler Mapping Instrument aboard the CYGNSS satellite constellation. The primary CYGNSS instrument, also known as the Delay-Doppler Mapping Instrument (DDMI), measures the incoming radio frequency (RF) streams from three input antenna channels (2 nadir oriented science antennas and one zenith oriented navigation antenna) and processes them in real time into DDMs, which are two-dimensional maps of the signal scattered from the Earth surface as a function of propagation time delay and Doppler frequency shift. DDMs are normally sampled over a restricted range of delay and Doppler values centered on the values at the specular point of reflection. The bit resolution of scattered signal strength is also truncated by a lossy data compression algorithm. Full DDMs are sampled over a wider range of delay and Doppler values and retain their full (lossless) bit resolution. Full DDM data records are typically 10-15 min in duration and are initiated by ground commands to coincide with an overpass by one of the spacecraft of a target area of interest. This version supersedes the Full DDM Version 1.0 (&lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L1FDD&quot;&gt;https://doi.org/10.5067/CYGNS-L1FDD&lt;/a&gt;) for data retrieved during or after August 2018. For data retrieved prior to August 2018, users will need to continue using the Full DDM Version 1.0. This version links the Full DDMs to the CYGNSS v3.0 L1 files (&lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L1X30&quot;&gt;https://doi.org/10.5067/CYGNS-L1X30&lt;/a&gt;) whereas the version 1.0 Full DDM linked the Full DDMs to the CYGNSS v2.1 L1 files (&lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L1X21&quot;&gt;https://doi.org/10.5067/CYGNS-L1X21&lt;/a&gt;). The calibration of the Full DDMs has not been modified for this release.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l1_raw_if&quot;&gt;CYGNSS_L1_RAW_IF&lt;/h4&gt;
This Level 1 (L1) dataset contains the Raw Intermediate Frequency (IF) sensor data from the Delay Doppler Mapping Instrument aboard the CYGNSS satellite constellation. The primary CYGNSS instrument, also known as the Delay-Doppler Mapping Instrument (DDMI), digitizes the incoming radio frequency (RF) streams from three input antenna channels (2 nadir oriented science antennas and one zenith oriented navigation antenna). The Raw IF data included in this data record are the raw sensor counts, retrieved prior to any digital signal processing, thus providing the highest possible resolution in delay and doppler space allowing for the construction of high resolution Delay Doppler Map (DDM) data. Raw IF data records are 30-90 sec in duration, with 60 sec being typical, and are initiated by ground commands to coincide with an overpass by one of the spacecraft of a target area of interest.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l1_v21&quot;&gt;CYGNSS_L1_V2.1&lt;/h4&gt;
This Level 1 (L1) dataset contains the Version 2.1 geo-located Delay Doppler Maps (DDMs) calibrated into Power Received (Watts) and Bistatic Radar Cross Section (BRCS) expressed in units of meters squared from the Delay Doppler Mapping Instrument aboard the CYGNSS satellite constellation. This version supersedes Version 2.0. Other useful scientific and engineering measurement parameters include the DDM of Normalized Bistatic Radar Cross Section (NBRCS), the Delay Doppler Map Average (DDMA) of the NBRCS near the specular reflection point, and the Leading Edge Slope (LES) of the integrated delay waveform. The L1 dataset contains a number of other engineering and science measurement parameters, including sets of quality flags/indicators, error estimates, and bias estimates as well as a variety of orbital, spacecraft/sensor health, timekeeping, and geolocation parameters. At most, 8 netCDF data files (each file corresponding to a unique spacecraft in the CYGNSS constellation) are provided each day; under nominal conditions, there are typically 6-8 spacecraft retrieving data each day, but this can be maximized to 8 spacecraft under special circumstances in which higher than normal retrieval frequency is needed (i.e., during tropical storms and or hurricanes). Latency is approximately 6 days (or better) from the last recorded measurement time. The Version 2.1 release represents the second science-quality release. Here is a summary of improvements that reflect the quality of the Version 2.1 data release: 1) data is now available when the CYGNSS satellites are rolled away from nadir during orbital high beta-angle periods, resulting in a significant amount of additional data; 2) correction to coordinate frames result in more accurate estimates of receiver antenna gain at the specular point; 3) improved calibration for analog-to-digital conversion results in better consistency between CYGNSS satellites measurements at nearly the same location and time; 4) improved GPS EIRP and transmit antenna pattern calibration results in significantly reduced PRN-dependence in the observables; 5) improved estimation of the location of the specular point within the DDM; 6) an altitude-dependent scattering area is used to normalize the scattering cross section (v2.0 used a simpler scattering area model that varied with incidence and azimuth angles but not altitude); 7) corrections added for noise floor-dependent biases in scattering cross section and leading edge slope of delay waveform observed in the v2.0 data. Users should also note that the receiver antenna pattern calibration is not applied per-DDM-bin in this v2.1 release.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l1_v30&quot;&gt;CYGNSS_L1_V3.0&lt;/h4&gt;
This Level 1 (L1) dataset contains the Version 3.0 geo-located Delay Doppler Maps (DDMs) calibrated into Power Received (Watts) and Bistatic Radar Cross Section (BRCS) expressed in units of m2 from the Delay Doppler Mapping Instrument aboard the CYGNSS satellite constellation. This version supersedes Version 2.1; &lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L1X21&quot;&gt;https://doi.org/10.5067/CYGNS-L1X21&lt;/a&gt; . Other useful scientific and engineering measurement parameters include the DDM of Normalized Bistatic Radar Cross Section (NBRCS), the Delay Doppler Map Average (DDMA) of the NBRCS near the specular reflection point, and the Leading Edge Slope (LES) of the integrated delay waveform. The L1 dataset contains a number of other engineering and science measurement parameters, including sets of quality flags/indicators, error estimates, and bias estimates as well as a variety of orbital, spacecraft/sensor health, timekeeping, and geolocation parameters. At most, 8 netCDF data files (each file corresponding to a unique spacecraft in the CYGNSS constellation) are provided each day; under nominal conditions, there are typically 6-8 spacecraft retrieving data each day, but this can be maximized to 8 spacecraft under special circumstances in which higher than normal retrieval frequency is needed (i.e., during tropical storms and or hurricanes). Latency is approximately 6 days (or better) from the last recorded measurement time. Here is a summary of improvements the calibration and processing changes to the Version 3.0 data: 1) the transmitted GPS signal strength in the direction of the DDM scattering surface is determined in real time from measurements of the direct signal from the GPS satellite to the CYGNSS navigation receiver, allowing for the BRCS calibration to be corrected for variations in GPS transmit power; 2) the NBRCS has been validated using comparisons with a large population of modeled values derived from coincident ocean surface roughness spectra produced by the NOAA WAVEWATCH-3 oceanographic wave model; 3) L1 calibration parameters have been adjusted to produce a best fit to the model population.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l1_v31&quot;&gt;CYGNSS_L1_V3.1&lt;/h4&gt;
This Level 1 (L1) dataset contains the Version 3.1 geo-located Delay Doppler Maps (DDMs) calibrated into Power Received (Watts) and Bistatic Radar Cross Section (BRCS) expressed in units of m2 from the Delay Doppler Mapping Instrument aboard the CYGNSS satellite constellation. This version supersedes Version 3.0; &lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L1X30&quot;&gt;https://doi.org/10.5067/CYGNS-L1X30&lt;/a&gt;. Other useful scientific and engineering measurement parameters include the DDM of Normalized Bistatic Radar Cross Section (NBRCS), the Delay Doppler Map Average (DDMA) of the NBRCS near the specular reflection point, and the Leading Edge Slope (LES) of the integrated delay waveform. The L1 dataset contains a number of other engineering and science measurement parameters, including sets of quality flags/indicators, error estimates, and bias estimates as well as a variety of orbital, spacecraft/sensor health, timekeeping, and geolocation parameters. At most, 8 netCDF data files (each file corresponding to a unique spacecraft in the CYGNSS constellation) are provided each day; under nominal conditions, there are typically 6-8 spacecraft retrieving data each day, but this can be maximized to 8 spacecraft under special circumstances in which higher than normal retrieval frequency is needed (i.e., during tropical storms and or hurricanes). Latency is approximately 6 days (or better) from the last recorded measurement time. Here is a summary of improvements the calibration and processing changes to the Version 3.1 data: The CYGNSS science antenna gain patterns have been adjusted to improve the accuracy of the ocean surface scattering cross section (a.k.a. the NBRCS) calibration. They are adjusted so that the annual average observed NBRCS matches the model-predicted average as derived from Wavewatch-3 estimates of the surface roughness with the appropriate spectral tail extension added to the roughness spectrum. The adjustment is made independently at each position in the science antenna pattern. A correction for coarse quantization effects by the on-board digital processor has also been added. This reduces the effects of radio frequency interference, which appeared as calibration biases in the v3.0 L1 NBRCS and retrieval biases in the v3.0 L2 wind speed that were persistent at certain locations.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l1_v32&quot;&gt;CYGNSS_L1_V3.2&lt;/h4&gt;
This CYGNSS Level 1 (L1) science data record dataset contains the version 3.2 geo-located Delay Doppler Maps (DDMs) calibrated into Power Received (Watts) and Bistatic Radar Cross Section (BRCS) expressed in units of m2 from the Delay Doppler Mapping Instrument aboard the CYGNSS satellite constellation. This version supersedes Version 3.1: &lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L1X31&quot;&gt;https://doi.org/10.5067/CYGNS-L1X31&lt;/a&gt;. Other useful scientific and engineering measurement parameters include the DDM of Normalized Bistatic Radar Cross Section (NBRCS), the Delay Doppler Map Average (DDMA) of the NBRCS near the specular reflection point, and the Leading Edge Slope (LES) of the integrated delay waveform. The L1 dataset contains a number of other engineering and science measurement parameters, including sets of quality flags/indicators, error estimates, and bias estimates as well as a variety of orbital, spacecraft/sensor health, timekeeping, and geolocation parameters. At most, 8 netCDF data files (each file corresponding to a unique spacecraft in the CYGNSS constellation) are provided each day; under nominal conditions, there are typically 6-8 spacecraft retrieving data each day, but this can be maximized to 8 spacecraft under special circumstances in which higher than normal retrieval frequency is needed (i.e., during tropical storms and or hurricanes). Latency is approximately 6 days (or better) from the last recorded measurement time. &lt;br&gt;&lt;br&gt; The correction for coarse quantization effects that was implemented in v3.1 for the signal portion of the DDM has been updated to include a correction to the noise floor portion of the DDM. This update is found to improve the sensitivity to soil moisture over land and to have a minimal effect on the sensitivity to wind speed over ocean. An update is made to the correction for the temperature dependence of the receiver electronics. This update reduces slow variations in calibration bias associated with a ~60 day oscillation in the mean temperature of the satellites. L1 variables over land and ocean are now combined in common netcdf data files, with additional details added regarding the specular point calculation over land. Nadir (science) antenna pattern and NBRCS rescaling has been updated to improve the inter-satellite consistency of the L1 calibration.&lt;br&gt;&lt;br&gt; The CYGNSS is a NASA Earth System Science Pathfinder Mission that is intended to collect the first frequent space‐based measurements of surface wind speeds in the inner core of tropical cyclones. Made up of a constellation of eight micro-satellites, the observatories provide nearly gap-free Earth coverage using an orbital inclination of approximately 35° from the equator, with a mean (i.e., average) revisit time of seven hours and a median revisit time of three hours. This inclination allows CYGNSS to measure ocean surface winds between approximately 38° N and 38° S latitude. This range includes the critical latitude band for tropical cyclone formation and movement.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l2_cdr_v10&quot;&gt;CYGNSS_L2_CDR_V1.0&lt;/h4&gt;
This dataset contains the Version 1.0 CYGNSS Level 2 Climate Data Record which provides the time-tagged and geolocated average wind speed (m/s) and mean square slope (MSS) with 25x25 kilometer resolution from the Delay Doppler Mapping Instrument aboard the CYGNSS satellite constellation. The reported sample locations are determined by the specular points corresponding to the Delay Doppler Maps (DDMs). A subset of DDM data used in the direct processing of the average wind speed and MSS is co-located inside of the Level 2 data files. Only one netCDF data file is produced each day (each file containing data from up to 8 unique CYGNSS spacecraft) with a latency of approximately 2 months (or better) from the last recorded measurement time. The Version 1.0 CDR represents the first climate-quality release and is a collection of reanalysis products derived from the SDR v2.1 Level 1 data. Calibration accuracy and long term stability are improved relative to the SDR v2.1 using a new trackwise correction algorithm which constrains the average value of the L1 data using MERRA-2 reanalysis wind speeds. Details of the algorithm are provided in the Trackwise Corrected CDR Algorithm Theoretical Basis Document. CDR Level 2 and 3 products (ocean surface wind speed, mean square slope, and latent and sensible heat flux) are generated from the CDR L1 data using the v2.1 SDR data processing algorithms. These products also exhibit improved calibration accuracy and stability over SDR v2.1. Trackwise correction is applied to the two primary CYGNSS L1 science data products the normalized bistatic radar cross section (NBRCS) and the leading edge slope of the Doppler-integrated delay waveform (LES). The correction compensates for variations in the transmit power level of the GPS signals measured by the CYGNSS bistatic radar receivers. The SDR v2.1 L1 algorithm assumes a constant GPS transmit power and variations in it can be misinterpreted as variations in the L1 data and in subsequent L2 science data products derived from them. The GPS constellation consists of several different satellite models (a.k.a. block types) and the level of transmit power variation differs between them. The more recent Block IIF models (which account for ~37% of the GPS constellation) have significantly larger variations than the older models and, for this reason, they have been screened out and not used to produce SDR v2.1 L2 or L3 science data products. Trackwise correction eliminates the need for this screening so CDR L2 and L3 data products now include Block IIF samples. It should be noted that the trackwise correction algorithm cannot be successfully applied to all SDR v2.1 L1 data so there is also some loss of samples that were present in SDR v2.1. Overall, there is a significant increase in sampling and improvement in spatial coverage with the CDR products.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l2_cdr_v11&quot;&gt;CYGNSS_L2_CDR_V1.1&lt;/h4&gt;
This dataset contains the Version 1.1 CYGNSS Level 2 Climate Data Record which provides the time-tagged and geolocated average wind speed (m/s) and mean square slope (MSS) with 25x25 kilometer resolution from the Delay Doppler Mapping Instrument aboard the CYGNSS satellite constellation. The reported sample locations are determined by the specular points corresponding to the Delay Doppler Maps (DDMs). A subset of DDM data used in the direct processing of the average wind speed and MSS is co-located inside of the Level 2 data files. Only one netCDF data file is produced each day (each file containing data from up to 8 unique CYGNSS spacecraft) with a latency of approximately 1 to 2 months from the last recorded measurement time. The Version 1.1 CDR represents is a collection of reanalysis products derived from the SDR v3.0 Level 1 data (&lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L1X30&quot;&gt;https://doi.org/10.5067/CYGNS-L1X30&lt;/a&gt; ). Calibration accuracy and long term stability are improved relative to SDR v3.0 (&lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L2X30&quot;&gt;https://doi.org/10.5067/CYGNS-L2X30&lt;/a&gt; ) using the same trackwise correction algorithm as was used by CDR v1.0 (&lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L2C10&quot;&gt;https://doi.org/10.5067/CYGNS-L2C10&lt;/a&gt; ), which was derived from SDR v2.1 Level 1 data (&lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L1X21&quot;&gt;https://doi.org/10.5067/CYGNS-L1X21&lt;/a&gt; ). Details of the algorithm are provided in the Trackwise Corrected CDR Algorithm Theoretical Basis Document. CDR Level 2 and 3 products (ocean surface wind speed, mean square slope, and latent and sensible heat flux) are generated from the CDR L1 data using the v3.0 SDR data processing algorithms. These products also exhibit improved calibration accuracy and stability over SDR v3.0. Trackwise correction is applied to the two primary CYGNSS L1 science data products, the normalized bistatic radar cross section (NBRCS) and the leading edge slope of the Doppler-integrated delay waveform (LES). The correction compensates for small errors in the Level 1 calibration, due e.g. to uncertainties in the GPS transmitting antenna gain patterns and the CYGNSS receiving antenna gain patterns. CDR v1.1 does not include a Young Seas with Limited Fetch (YSLF) wind speed product and investigators requiring wind speed measurements in and near the inner core of tropical cyclones should use the SDR v3.0 YSLF wind speed product. A YSLF wind speed product is omitted because the trackwise correction algorithm, which constrains the average value of the L1 data using MERRA-2 reanalysis wind speeds, is inherently biased toward fully developed sea state conditions. The constraint improves wind speed retrieval performance in fully developed seas but produces underestimates in YSLF conditions. It should also be noted that the trackwise correction algorithm cannot be successfully applied to all SDR v3.0 L1 data so there is also some loss of samples that were present in SDR v3.0.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l2_cdr_v12&quot;&gt;CYGNSS_L2_CDR_V1.2&lt;/h4&gt;
This dataset contains the Version 1.2 CYGNSS Level 2 Climate Data Record which provides the time-tagged and geolocated average wind speed (m/s) and mean square slope (MSS) with 25x25 kilometer resolution from the Delay Doppler Mapping Instrument aboard the CYGNSS satellite constellation. The reported sample locations are determined by the specular points corresponding to the Delay Doppler Maps (DDMs). A subset of DDM data used in the direct processing of the average wind speed and MSS is co-located inside of the Level 2 data files. Only one netCDF data file is produced each day (each file containing data from up to 8 unique CYGNSS spacecraft) with a latency of approximately 1 to 2 months from the last recorded measurement time. The Version 1.2 CDR represents is a collection of reanalysis products derived from the SDR v3.1 Level 1 data (&lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L1X31&quot;&gt;https://doi.org/10.5067/CYGNS-L1X31&lt;/a&gt; ). Calibration accuracy and long term stability are improved relative to SDR v3.1 (&lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L2X31&quot;&gt;https://doi.org/10.5067/CYGNS-L2X31&lt;/a&gt; ) using the same trackwise correction algorithm as was used by CDR v1.1 (&lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L2C11&quot;&gt;https://doi.org/10.5067/CYGNS-L2C11&lt;/a&gt; ), which was derived from SDR v2.1 Level 1 data (&lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L1X21&quot;&gt;https://doi.org/10.5067/CYGNS-L1X21&lt;/a&gt; ). Details of the algorithm are provided in the Trackwise Corrected CDR Algorithm Theoretical Basis Document. CDR Level 2 and 3 products (ocean surface wind speed, mean square slope, and latent and sensible heat flux) are generated from the CDR L1 data using the v3.1 SDR data processing algorithms. These products also exhibit improved calibration accuracy and stability over SDR v3.0. Trackwise correction is applied to the two primary CYGNSS L1 science data products, the normalized bistatic radar cross section (NBRCS) and the leading edge slope of the Doppler-integrated delay waveform (LES). The correction compensates for small errors in the Level 1 calibration, due e.g. to uncertainties in the GPS transmitting antenna gain patterns and the CYGNSS receiving antenna gain patterns. It should be noted that the trackwise correction algorithm cannot be successfully applied to all SDR v3.1 L1 data so there is also some loss of samples that were present in SDR v3.1.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l2_surface_flux_cdr_v10&quot;&gt;CYGNSS_L2_SURFACE_FLUX_CDR_V1.0&lt;/h4&gt;
This dataset contains the first release, Version 1.0, of the CYGNSS Level 2 Ocean Surface Heat Flux Climate Data Record (CDR), which provides the time-tagged and geolocated ocean surface heat flux parameters with 25x25 kilometer footprint resolution with 1-2 month latency from the Delay Doppler Mapping Instrument (DDMI) aboard the CYGNSS satellite constellation. The Cyclone Global Navigation Satellite System (CYGNSS) is a NASA Earth System Science Pathfinder Mission designed to collect the first frequent space-based measurements of surface wind speeds in the inner core of tropical cyclones. The Coupled Ocean-Atmosphere Response Experiment (COARE) version 3.5 algorithm combines CYGNSS L2 CDR v1.0 ocean surface wind speed estimates with the auxiliary parameters provided by the NASA Modern-Era Retrospective Analysis for Research and Applications Version 2 (MERRA-2) to produce latent and sensible heat fluxes and their respective transfer coefficients. More information on how the data is produced and validated can be found in the dataset user guide (see Documentation tab). More information on the CYGNSS mission, spacecraft, instrumentation and related datasets is available here: &lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/CYGNSS&quot;&gt;https://podaac.jpl.nasa.gov/CYGNSS&lt;/a&gt;. Additional information on the CYGNSS L2 CDR v1.0 wind speed dataset is available here: &lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L2C10&quot;&gt;https://doi.org/10.5067/CYGNS-L2C10&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l2_surface_flux_cdr_v11&quot;&gt;CYGNSS_L2_SURFACE_FLUX_CDR_V1.1&lt;/h4&gt;
This dataset contains the first release, Version 1.1, of the CYGNSS Level 2 Ocean Surface Heat Flux Climate Data Record (CDR), which provides the time-tagged and geolocated ocean surface heat flux parameters with 25x25 kilometer footprint resolution with 1-2 month latency from the Delay Doppler Mapping Instrument (DDMI) aboard the CYGNSS satellite constellation. The Cyclone Global Navigation Satellite System (CYGNSS) is a NASA Earth System Science Pathfinder Mission designed to collect the first frequent space-based measurements of surface wind speeds in the inner core of tropical cyclones. The Coupled Ocean-Atmosphere Response Experiment (COARE) version 3.5 algorithm combines CYGNSS L2 CDR v1.1 ocean surface wind speed estimates with the auxiliary parameters provided by the NASA Modern-Era Retrospective Analysis for Research and Applications Version 2 (MERRA-2) to produce latent and sensible heat fluxes and their respective transfer coefficients. More information on how the data is produced and validated can be found in the dataset user guide (see Documentation tab). More information on the CYGNSS mission, spacecraft, instrumentation and related datasets is available here: &lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/CYGNSS&quot;&gt;https://podaac.jpl.nasa.gov/CYGNSS&lt;/a&gt;. Additional information on the CYGNSS L2 CDR v1.1 wind speed dataset is available here: &lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L2C11&quot;&gt;https://doi.org/10.5067/CYGNS-L2C11&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l2_surface_flux_cdr_v12&quot;&gt;CYGNSS_L2_SURFACE_FLUX_CDR_V1.2&lt;/h4&gt;
This dataset contains the third release, Version 1.2, of the CYGNSS Level 2 Ocean Surface Heat Flux Climate Data Record (CDR), which provides the time-tagged and geolocated ocean surface heat flux parameters with 25x25 kilometer footprint resolution with 6-7 day latency from the Delay Doppler Mapping Instrument (DDMI) aboard the Cyclone Global Navigation Satellite System (CYGNSS) constellation. CYGNSS is a NASA Earth System Science Pathfinder Mission designed to collect the first frequent space-based measurements of surface wind speeds in the inner core of tropical cyclones. The Coupled Ocean-Atmosphere Response Experiment (COARE) version 3.5 algorithm combines CYGNSS L2 CDR v1.2 ocean surface wind speed estimates with the auxiliary parameters provided by the European Centre for Medium-Range Weather Forecasts Reanalysis Version 5 (ERA5) to produce latent and sensible heat fluxes and their respective transfer coefficients. More information on how the data is produced and validated can be found in the dataset user guide (see Documentation tab). More information on the CYGNSS mission, spacecraft, instrumentation and related datasets is available here: &lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/CYGNSS&quot;&gt;https://podaac.jpl.nasa.gov/CYGNSS&lt;/a&gt; . Additional information on the CYGNSS L2 CDR v1.2 wind speed dataset is available here: &lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L2C12&quot;&gt;https://doi.org/10.5067/CYGNS-L2C12&lt;/a&gt; .
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l2_surface_flux_v10&quot;&gt;CYGNSS_L2_SURFACE_FLUX_V1.0&lt;/h4&gt;
This dataset contains the Version 1.0 CYGNSS Level 2 Ocean Surface Heat Flux Science Data Record, which provides the time-tagged and geolocated ocean surface heat flux parameters with 25x25 kilometer footprint resolution from the Delay Doppler Mapping Instrument (DDMI) aboard the CYGNSS satellite constellation. The reported sample locations are determined by the specular points corresponding to the Delay Doppler Maps (DDMs). Only one netCDF-4 data file is produced each day (each file containing data from a combination of up to 8 unique CYGNSS spacecraft) with a latency of approximately 1 to 2 months from the last recorded measurement time. Version 1.0 represents the first release. The Cyclone Global Navigation Satellite System (CYGNSS), launched on 15 December 2016, is a NASA Earth System Science Pathfinder Mission that was launched with the purpose to collect the first frequent space-based measurements of surface wind speeds in the inner core of tropical cyclones. Made up of a constellation of eight micro-satellites, the CYGNSS observatories provide nearly gap-free Earth coverage with a mean (i.e., average) revisit time of seven hours and a median revisit time of three hours. The 35 degree orbital inclination allows CYGNSS to measure ocean surface winds between approximately 38 degrees North and 38 degrees South latitude using an innovative combination of all-weather performance Global Positioning System (GPS) L-band ocean surface reflectometry to penetrate the clouds and heavy precipitation. The Coupled Ocean-Atmosphere Response Experiment (COARE) algorithm is what is used in this dataset to estimate the latent and sensible heat fluxes and their respective transfer coefficients. While COARE&amp;#39;s initial intentions were for low to moderate wind speeds, the version used for this product, COARE 3.5, has been verified with direct in situ flux measurements for wind speeds up to 25 m/s. As CYGNSS does not provide air/sea temperature, humidity, surface pressure or density, the producer of this dataset obtains these values from the NASA Modern-Era Retrospective Analysis for Research and Applications Version 2 (MERRA-2), which uses data assimilation to combine all available in situ and satellite observation data with an initial estimate of the atmospheric state, provided by a global atmospheric model. Since the MERRA-2 data is only updated on monthly intervals, this corresponding heat flux dataset is likewise updated on a monthly interval to reflect the latest data available from MERRA-2, thus accounting for measurement latency, with respect to CYGNSS observables, ranging from 1 to 2 months. The data from this release compares well with in situ buoy data, including: Kuroshio Extension Observatory (KEO), National Data Buoy Center (NDBC), Ocean Sustained Interdisciplinary Time-series Environment observation System (OceanSITES), Prediction and Research Moored Array in the Tropical Atlantic (PIRATA), Research Moored Array for African-Asian-Australian Monsoon Analysis and Prediction (RAMA), and the Tropical Atmosphere Ocean (TAO) array. As this marks only the first data release, future work is expected to provide comparisons and validation with various field campaigns (e.g., PISTON, CAMP2Ex) as well as more buoy data, especially at higher flux estimates.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l2_surface_flux_v20&quot;&gt;CYGNSS_L2_SURFACE_FLUX_V2.0&lt;/h4&gt;
This dataset contains the Version 2.0 CYGNSS Level 2 Ocean Surface Heat Flux Science Data Record, which provides time-tagged and geolocated ocean surface heat flux parameters with 25x25 kilometer footprint resolution from the Delay Doppler Mapping Instrument (DDMI) aboard the CYGNSS satellite constellation. The reported sample locations are determined by the specular points corresponding to the Delay Doppler Maps (DDMs). Version 2.0 represents the second release of this product, which now uses CYGNSS Level 2 (L2) Science Data Record (SDR) Version 3.1 surface wind speeds and ECMWF Reanalysis, Version 5 (ERA5). Version 1.0 used CYGNSS L2 SDR Version 2.1 surface wind speeds and NASA Modern-Era Retrospective Analysis for Research and Applications Version 2 (MERRA-2). The Coupled Ocean-Atmosphere Response Experiment (COARE) algorithm is what is used in this dataset to estimate the latent and sensible heat fluxes and their respective transfer coefficients. While COARE&amp;#39;s initial intentions were for low to moderate wind speeds, the version used for this product, COARE 3.5, has been verified with direct in situ flux measurements for wind speeds up to 25 m/s. As CYGNSS does not provide air/sea temperature, humidity, surface pressure or density, the producer of this dataset obtains these values from this dataset obtains these values from ERA5. The Cyclone Global Navigation Satellite System (CYGNSS), launched on 15 December 2016, is a NASA Earth System Science Pathfinder Mission that was launched with the purpose to collect the first frequent space-based measurements of surface wind speeds in the inner core of tropical cyclones. Made up of a constellation of eight micro-satellites, the CYGNSS observatories provide nearly gap-free Earth coverage with a mean (i.e., average) revisit time of seven hours and a median revisit time of three hours. As a result of the CYGNSS constellation coverage, this data is made available from 1 August 2018 to present with an approximate 1 week latency in the netCDF-4 formatted data files, where each file contains data within a 24-hour UTC period from a combination of up to 8 unique CYGNSS spacecraft. More information on CYGNSS can be found on the CYGNSS mission page.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l2_surface_flux_v32&quot;&gt;CYGNSS_L2_SURFACE_FLUX_V3.2&lt;/h4&gt;
The CYGNSS level 2 ocean surface heat flux science data record version 3.2 dataset is provided as a service to the oceanographic and meteorological research communities on behalf of the CYGNSS Science Team in direct collaboration with the Cyclone Global Navigation Satellite System (CYGNSS) Mission. CYGNSS was launched on 15 December 2016, it is a NASA Earth System Science Pathfinder Mission that was launched with the purpose of collecting the first frequent space‐based measurements of surface wind speeds in the inner core of tropical cyclones. Originally made up of a constellation of eight micro-satellites, the observatories provide nearly gap-free Earth coverage using an orbital inclination of approximately 35° from the equator, with a mean (i.e., average) revisit time of seven hours and a median revisit time of three hours. &lt;br&gt;&lt;br&gt; This dataset provides time-tagged and geolocated ocean surface heat flux parameters with 25x25 kilometer footprint resolution from the Delay Doppler Mapping Instrument (DDMI) aboard the CYGNSS satellite constellation. The reported sample locations are determined by the specular points corresponding to the Delay Doppler Maps (DDMs). Version 3.2 uses CYGNSS Level 2 (L2) Science Data Record (SDR) Version 3.2 surface wind speeds and ECMWF Reanalysis, Version 5 (ERA5). The Coupled Ocean-Atmosphere Response Experiment (COARE) algorithm is what is used in this dataset to estimate the latent and sensible heat fluxes and their respective transfer coefficients. While COARE&amp;#39;s initial intentions were for low to moderate wind speeds, the version used for this product, COARE 3.5, has been verified with direct in situ flux measurements for wind speeds up to 25 m/s. As CYGNSS does not provide air/sea temperature, humidity, surface pressure or density, the producer of this dataset obtains these values from this dataset obtains these values from ERA5. This dataset is made available from 1 August 2018 to present with an approximate 1 week latency in the netCDF-4 formatted data files, where each file contains data within a 24-hour UTC period from a combination of up to 8 unique CYGNSS spacecraft. More information on CYGNSS can be found on the CYGNSS mission page.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l2_v21&quot;&gt;CYGNSS_L2_V2.1&lt;/h4&gt;
This dataset contains the Version 2.1 CYGNSS Level 2 Science Data Record which provides the time-tagged and geolocated average wind speed (m/s) and mean square slope (MSS) with 25x25 kilometer resolution from the Delay Doppler Mapping Instrument aboard the CYGNSS satellite constellation. This version supersedes Version 2.0. The reported sample locations are determined by the specular points corresponding to the Delay Doppler Maps (DDMs). A subset of DDM data used in the direct processing of the average wind speed and MSS is co-located inside of the Level 2 data files. Only one netCDF data file is produced each day (each file containing data from up to 8 unique CYGNSS spacecraft) with a latency of approximately 6 days (or better) from the last recorded measurement time. The Version 2.1 release represents the second science-quality release. Here is a summary of improvements that reflect the quality of the Version 2.1 data release: 1) revised Geophysical Model Functions (GMFs) for both Fully Developed Seas (FDS) and Young Seas with Limited Fetch conditions, to be consistent with the calibration changes made to the v2.1 Level 1 science data products.; 2) Revised covariance matrix between DDMA and LES versions of the FDS wind speed retrieval, used by the minimum variance estimator, resulting from changes made to the v2.1 Level 1 science data products; 3) Revised debiasing algorithm coefficients used by the FDS L2 retrieval algorithm, resulting from changes made to the v2.1 Level 2 science data products; 4) revised quality control (Q/C) flags related to the required level of consistency between DDMA and LES versions of the FDS wind speed retrieval (the errors in the two retrievals are now less correlated so larger discrepancies are allowed; if either retrieval is not available, the sample receives a fatal Q/C flag); 5) new Q/C flag related to the block type of the GPS satellite which provided the transmitted signal. Samples using block II-F signals receive a fatal Q/C flag due to the higher level of uncertainty in their radiated power; 6) revised wind speed uncertainty values as a function of RCG and wind speed, plus a new dependence of the uncertainty on GPS block type to reflect the higher uncertainty in GPS radiated power for block II-F satellites.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l2_v30&quot;&gt;CYGNSS_L2_V3.0&lt;/h4&gt;
This dataset contains the Version 3.0 CYGNSS Level 2 Science Data Record which provides the time-tagged and geolocated average wind speed (m/s) and mean square slope (MSS) with 25x25 kilometer resolution from the Delay Doppler Mapping Instrument aboard the CYGNSS satellite constellation. This version supersedes Version 2.1; &lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L2X21&quot;&gt;https://doi.org/10.5067/CYGNS-L2X21&lt;/a&gt;. The reported sample locations are determined by the specular points corresponding to the Delay Doppler Maps (DDMs). A subset of DDM data used in the direct processing of the average wind speed and MSS is co-located inside of the Level 2 data files. Only one netCDF data file is produced each day (each file containing data from up to 8 unique CYGNSS spacecraft) with a latency of approximately 6 days (or better) from the last recorded measurement time. Here is a summary of processing changes reflected in the v3.0 data: 1) the changes to calibration and validation of the Level 1 Normalized Bistatic Radar Cross Section (NBRCS) necessitated updates to the Geophysical Model Functions (GMFs) used to retrieve wind speed; 2) the GMF for fully developed seas (FDS) conditions was generating using matchups between NBRCS measurements and coincident wind speeds produced by NASAs Modern-Era Retrospective analysis for Research and Applications, version 2 (MERRA-2) reanalysis model; 3) the GMF for young seas with limited fetch (YSLF) was generated using matchups between NBRCS and coincident wind speeds produced by NOAAs Hurricane Weather Research and Forecast (HWRF) System; 4) YSLF wind speed is a tapered linear combination of wind speeds derived from the FDS and YSLF GMFs, where the taper gives more weight to FDS at low wind speeds and more to YSLF at high wind speeds and accounts for the transition from FDS to YSLF sea state conditions near cyclonic storms; 5) re-introduces measurements using transmissions from previously discarded GPS satellite block types; in prior versions, Block II-F was completely discarded due to large variations in GPS transmit power. The real time transmit power monitoring and correction implemented in Level 1 v3.0 data now allows Block II-F signals to be used.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l2_v31&quot;&gt;CYGNSS_L2_V3.1&lt;/h4&gt;
This dataset contains the Version 3.1 CYGNSS Level 2 Science Data Record which provides the time-tagged and geolocated average wind speed (m/s) and mean square slope (MSS) with 25x25 kilometer resolution from the Delay Doppler Mapping Instrument aboard the CYGNSS satellite constellation. This version supersedes Version 3.0; &lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L2X30&quot;&gt;https://doi.org/10.5067/CYGNS-L2X30&lt;/a&gt;. The reported sample locations are determined by the specular points corresponding to the Delay Doppler Maps (DDMs). A subset of DDM data used in the direct processing of the average wind speed and MSS is co-located inside of the Level 2 data files. Only one netCDF data file is produced each day (each file containing data from up to 8 unique CYGNSS spacecraft) with a latency of approximately 6 days (or better) from the last recorded measurement time. Here is a summary of processing changes reflected in the v3.1 data: The L2 Geophysical Model Functions (GMFs) that map L1 observables to ocean surface wind speed were rederived to be consistent with the v3.1 L1 calibration. The method used for deriving the GMFs is the same as for v3.0. A new correction has been added to both the Fully Developed Seas (FDS) and Young Seas Limited Fetch (YSLF) wind speed products that is a function of the Significant Wave Height (SWH) of the ocean surface. The correction is based on an observed correlation between the wind speed error and SWH. The SWH value used by the correction algorithm is the ERA5 reanalysis product, coincident in space and time with a CYGNSS measurement. The FDS and YSLF retrieval algorithms are otherwise the same as v3.0.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l3_cdr_v10&quot;&gt;CYGNSS_L3_CDR_V1.0&lt;/h4&gt;
This dataset contains the Version 1.0 CYGNSS Level 3 Climate Data Record which provides the average wind speed and mean square slope (MSS) on a 0.2x0.2 degree latitude by longitude equirectangular grid obtained from the Delay Doppler Mapping Instrument aboard the CYGNSS satellite constellation. The Level 2 Delay Doppler Map (DDM) data are used in the direct processing of the average wind speed and MSS data that are binned on the Level 3 grid. A subset of DDM data used in the direct processing of the average wind speed and MSS is co-located inside of the Level 2 data files. A single netCDF-4 data file is produced for each day of operation with an approximate 2 month latency. The reported sample locations are determined by the specular points corresponding to the Delay Doppler Maps (DDMs). The Version 1.0 CDR represents the first climate-quality release and is a collection of reanalysis products derived from the SDR v2.1 Level 1 data. Calibration accuracy and long term stability are improved relative to the SDR v2.1 using a new trackwise correction algorithm which constrains the average value of the L1 data using MERRA-2 reanalysis wind speeds. Details of the algorithm are provided in the Trackwise Corrected CDR Algorithm Theoretical Basis Document. CDR Level 2 and 3 products (ocean surface wind speed, mean square slope, and latent and sensible heat flux) are generated from the CDR L1 data using the v2.1 SDR data processing algorithms. These products also exhibit improved calibration accuracy and stability over SDR v2.1. Trackwise correction is applied to the two primary CYGNSS L1 science data products the normalized bistatic radar cross section (NBRCS) and the leading edge slope of the Doppler-integrated delay waveform (LES). The correction compensates for variations in the transmit power level of the GPS signals measured by the CYGNSS bistatic radar receivers. The SDR v2.1 L1 algorithm assumes a constant GPS transmit power and variations in it can be misinterpreted as variations in the L1 data and in subsequent L2 science data products derived from them. The GPS constellation consists of several different satellite models (a.k.a. block types) and the level of transmit power variation differs between them. The more recent Block IIF models (which account for ~37% of the GPS constellation) have significantly larger variations than the older models and, for this reason, they have been screened out and not used to produce SDR v2.1 L2 or L3 science data products. Trackwise correction eliminates the need for this screening so CDR L2 and L3 data products now include Block IIF samples. It should be noted that the trackwise correction algorithm cannot be successfully applied to all SDR v2.1 L1 data so there is also some loss of samples that were present in SDR v2.1. Overall, there is a significant increase in sampling and improvement in spatial coverage with the CDR products.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l3_cdr_v11&quot;&gt;CYGNSS_L3_CDR_V1.1&lt;/h4&gt;
This dataset contains the Version 1.1 CYGNSS Level 3 Climate Data Record which provides the average wind speed and mean square slope (MSS) on a 0.2x0.2 degree latitude by longitude equirectangular grid obtained from the Delay Doppler Mapping Instrument aboard the CYGNSS satellite constellation. The Level 2 Delay Doppler Map (DDM) data are used in the direct processing of the average wind speed and MSS data that are binned on the Level 3 grid. A subset of DDM data used in the direct processing of the average wind speed and MSS is co-located inside of the Level 2 data files. A single netCDF-4 data file is produced for each day of operation with an approximate 1 to 2 month latency. The reported sample locations are determined by the specular points corresponding to the Delay Doppler Maps (DDMs). The Version 1.1 CDR is a collection of reanalysis products derived from the SDR v3.0 Level 1 data (&lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L1X30&quot;&gt;https://doi.org/10.5067/CYGNS-L1X30&lt;/a&gt; ). Calibration accuracy and long term stability are improved relative to SDR v3.0 (&lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L3X30&quot;&gt;https://doi.org/10.5067/CYGNS-L3X30&lt;/a&gt; ) using the same trackwise correction algorithm as was used by CDR v1.0 (&lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L3C10&quot;&gt;https://doi.org/10.5067/CYGNS-L3C10&lt;/a&gt; ), which was derived from SDR v2.1 Level 1 data (&lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L1X21&quot;&gt;https://doi.org/10.5067/CYGNS-L1X21&lt;/a&gt; ). Details of the algorithm are provided in the Trackwise Corrected CDR Algorithm Theoretical Basis Document. CDR Level 2 and 3 products (ocean surface wind speed, mean square slope, and latent and sensible heat flux) are generated from the CDR L1 data using the v3.0 SDR data processing algorithms. These products also exhibit improved calibration accuracy and stability over SDR v3.0. Trackwise correction is applied to the two primary CYGNSS L1 science data products, the normalized bistatic radar cross section (NBRCS) and the leading edge slope of the Doppler-integrated delay waveform (LES). The correction compensates for small errors in the Level 1 calibration, due e.g. to uncertainties in the GPS transmitting antenna gain patterns and the CYGNSS receiving antenna gain patterns. CDR v1.1 does not include a Young Seas with Limited Fetch (YSLF) wind speed product and investigators requiring wind speed measurements in and near the inner core of tropical cyclones should use the SDR v3.0 YSLF wind speed product. A YSLF wind speed product is omitted because the trackwise correction algorithm, which constrains the average value of the L1 data using MERRA-2 reanalysis wind speeds, is inherently biased toward fully developed sea state conditions. The constraint improves wind speed retrieval performance in fully developed seas but produces underestimates in YSLF conditions. It should also be noted that the trackwise correction algorithm cannot be successfully applied to all SDR v3.0 L1 data so there is also some loss of samples that were present in SDR v3.0.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l3_cdr_v12&quot;&gt;CYGNSS_L3_CDR_V1.2&lt;/h4&gt;
This dataset contains the Version 1.2 CYGNSS Level 3 Climate Data Record which provides the average wind speed and mean square slope (MSS) on a 0.2x0.2 degree latitude by longitude equirectangular grid obtained from the Delay Doppler Mapping Instrument aboard the CYGNSS satellite constellation. The Level 2 Delay Doppler Map (DDM) data are used in the direct processing of the average wind speed and MSS data that are binned on the Level 3 grid. A subset of DDM data used in the direct processing of the average wind speed and MSS is co-located inside of the Level 2 data files. A single netCDF-4 data file is produced for each day of operation with an approximate 5 days latency. The reported sample locations are determined by the specular points corresponding to the Delay Doppler Maps (DDMs). The Version 1.2 CDR is a collection of reanalysis products derived from the SDR v3.1 Level 1 data (&lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L1X31&quot;&gt;https://doi.org/10.5067/CYGNS-L1X31&lt;/a&gt; ). Calibration accuracy and long term stability are improved relative to SDR v3.1 (&lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L3X31&quot;&gt;https://doi.org/10.5067/CYGNS-L3X31&lt;/a&gt; ) using the same trackwise correction algorithm as was used by CDR v1.1 (&lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L3C11&quot;&gt;https://doi.org/10.5067/CYGNS-L3C11&lt;/a&gt; ), which was derived from SDR v3.0 Level 1 data (&lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L1X30&quot;&gt;https://doi.org/10.5067/CYGNS-L1X30&lt;/a&gt; ). Details of the algorithm are provided in the Trackwise Corrected CDR Algorithm Theoretical Basis Document. CDR Level 2 and 3 products (ocean surface wind speed, mean square slope, and latent and sensible heat flux) are generated from the CDR L1 data using the v3.1 SDR data processing algorithms. These products also exhibit improved calibration accuracy and stability over SDR v3.1. Trackwise correction is applied to the two primary CYGNSS L1 science data products, the normalized bistatic radar cross section (NBRCS) and the leading edge slope of the Doppler-integrated delay waveform (LES). The correction compensates for small errors in the Level 1 calibration, due e.g. to uncertainties in the GPS transmitting antenna gain patterns and the CYGNSS receiving antenna gain patterns. It should be noted that the trackwise correction algorithm cannot be successfully applied to all SDR v3.1 L1 data so there is also some loss of samples that were present in SDR v3.1.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l3_mrg_nrt_v32&quot;&gt;CYGNSS_L3_MRG_NRT_V3.2&lt;/h4&gt;
This dataset contains the version 3.2 CYGNSS Level 3 Merged (MRG) Science Data Record Near Real Time (NRT) Storm Wind Speed derived from the Delay Doppler Mapping Instrument aboard the CYGNSS satellite constellation. It combines CYGNSS storm-centric gridded (SCG) wind speeds, which are derived from the L2 Young Seas Limited Fetch (YSLF) winds for a region surrounding a given tropical cyclone (TC), with L2 Fully Developed Seas (FDS) winds away from the TC center on a 0.2x0.2 degree latitude by longitude equirectangular grid. &lt;br&gt;&lt;br&gt; L3 MRG is a product which combines the L2 FDS and YSLF winds and eliminates the need to choose between them depending on sea state development and the proximity to storms. The data are provided in netCDF-4 format and starts from the June 11, 2024 through the present with an approximate latency between 2 and 24 hours . A tapered weighted averaging scheme is used centered on the 34-knot wind radius (R34) of the storm. The R34 value in each storm quadrant is also reported. The algorithm produces global (+/- 40 deg latitude) wind speeds reported on a 0.1x0.1 deg grid every 6 hours for each tropical cyclone, although some 6-hourly increments may be missing if there are an insufficient number of satellite overpasses of the storm during that time interval. The netCDF files are output on a storm-by-storm basis. &lt;br&gt;&lt;br&gt; The CYGNSS is a NASA Earth System Science Pathfinder Mission that is intended to collect the first frequent space‐based measurements of surface wind speeds in the inner core of tropical cyclones. Made up of a constellation of eight micro-satellites, the observatories provide nearly gap-free Earth coverage using an orbital inclination of approximately 35° from the equator, with a mean (i.e., average) revisit time of seven hours and a median revisit time of three hours. This inclination allows CYGNSS to measure ocean surface winds between approximately 38° N and 38° S latitude. This range includes the critical latitude band for tropical cyclone formation and movement
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l3_mrg_nrt_v321&quot;&gt;CYGNSS_L3_MRG_NRT_V3.2.1&lt;/h4&gt;
This dataset contains the version 3.2.1 CYGNSS Level 3 Merged (MRG) Science Data Record Near Real Time (NRT) Storm Wind Speed derived from the Delay Doppler Mapping Instrument aboard the CYGNSS satellite constellation. It combines CYGNSS storm-centric gridded (SCG) wind speeds, which are derived from the L2 Young Seas Limited Fetch (YSLF) winds for a region surrounding a given tropical cyclone (TC), with L2 Fully Developed Seas (FDS) winds away from the TC center on a 0.2x0.2 degree latitude by longitude equirectangular grid. &lt;br&gt;&lt;br&gt; L3 MRG is a product which combines the L2 FDS and YSLF winds and eliminates the need to choose between them depending on sea state development and the proximity to storms. The data are provided in netCDF-4 format and starts from the September 1, 2024 through the present with an approximate latency between 2 and 24 hours. A tapered weighted averaging scheme is used centered on the 25 m/s wind radius of the storm. The 34 knot wind radius (R34) algorithm has been updated for v3.2.1 release to center around the National Hurricane Center or the Joint Typhoon Warning Center (NHC/JTWC) reported storm center instead of the CYGNSS Vmax location The algorithm produces global (+/- 40 deg latitude) wind speeds reported on a 0.1x0.1 deg grid every 6 hours for each tropical cyclone, although some 6-hourly increments may be missing if there are an insufficient number of satellite overpasses of the storm during that time interval. The netCDF files are output on a storm-by-storm basis. &lt;br&gt;&lt;br&gt; The CYGNSS is a NASA Earth System Science Pathfinder Mission that is intended to collect the first frequent space‐based measurements of surface wind speeds in the inner core of tropical cyclones. Made up of a constellation of eight micro-satellites, the observatories provide nearly gap-free Earth coverage using an orbital inclination of approximately 35° from the equator, with a mean (i.e., average) revisit time of seven hours and a median revisit time of three hours. This inclination allows CYGNSS to measure ocean surface winds between approximately 38° N and 38° S latitude. This range includes the critical latitude band for tropical cyclone formation and movement.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l3_mrg_nrt_v322&quot;&gt;CYGNSS_L3_MRG_NRT_V3.2.2&lt;/h4&gt;
CYGNSS_L3_MRG_NRT_V3.2.2 This dataset contains the Near Real Time (NRT) version of the 3.2.2 CYGNSS Level 3 Merged (MRG) Science Data Record Wind Speed which combines CYGNSS storm-centric gridded (SCG) wind speeds, which are derived from the L2 Young Seas Limited Fetch (YSLF) winds for a region surrounding a given tropical cyclone (TC), with L3 Fully Developed Seas (FDS) winds away from the TC center. The L3 MRG wind speeds are obtained from the Delay Doppler Mapping Instrument aboard the CYGNSS satellite constellation and provided on a 0.1x0.1 degree latitude by longitude equirectangular grid. The NRT version of the L3 MRG product is intended to provide operational guidance via reduced latency compared to the standard CYGNSS L3 MRG product. In order to support this goal, as of v3.2.2 the averaging window has been reduced from the standard L3 MRG +/-6 hour window to +/-3 hours. &lt;br&gt;&lt;br&gt; The L3 MRG product was developed to eliminate the need to choose between the FDS and YSLF winds depending on sea state development and the proximity to storms by providing a product that merges winds in areas of YSLF and FDS conditions into a single wind field. The L3 MRG NRT data are provided in netCDF-4 format and will extend from the 2025 storm season through the present with an approximate latency between 2 and 24 hours, compared to an approximately 6 day latency for the standard product. A tapered weighted averaging scheme is used for the merging, centered on the 25 m/s wind radius of the storm. The algorithm produces global (+/- 40 deg latitude) wind speeds reported on a 0.1x0.1 deg grid using wind speeds collected over a 6 hour window, centered 3 hours back from the most recent sample in the wind field. In contrast to the standard L3 MRG product, the NRT netCDF files are output for a single time. New files are produced for a storm as more recent data becomes available instead of a single file containing all the available wind fields over a storm’s lifecycle. Changes from the previous v3.2.1 version include a new algorithm for determining the 34-knot wind radii and the inclusion of 50-knot wind radii. Additionally, the &amp;#39;epoch time&amp;#39; variable is now reported in &amp;#39;seconds since&amp;#39; the epoch instead of &amp;#39;hours since&amp;#39; the epoch. This change enables us to capture the exact timing of the L3 MRG Near Real Time (NRT) version time steps with full precision. &lt;br&gt;&lt;br&gt; The CYGNSS is a NASA Earth System Science Pathfinder Mission that is intended to collect the first frequent space‐based measurements of surface wind speeds in the inner core of tropical cyclones. Made up of a constellation of eight micro-satellites, the observatories provide nearly gap-free Earth coverage using an orbital inclination of approximately 35° from the equator, with a mean (i.e., average) revisit time of seven hours and a median revisit time of three hours. This inclination allows CYGNSS to measure ocean surface winds between approximately 38° N and 38° S latitude. This range includes the critical latitude band for tropical cyclone formation and movement.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l3_mrg_v32&quot;&gt;CYGNSS_L3_MRG_V3.2&lt;/h4&gt;
This dataset contains the version 3.2 CYGNSS level 3 science data record merged storm (MRG) wind speed which combines CYGNSS storm-centric gridded (SCG) wind speeds, which are derived from the L2 YSLF winds for a region surrounding a given tropical cyclone (TC), with L3 FDS winds away from the TC center on a 0.2x0.2 degree latitude by longitude equirectangular grid obtained from the Delay Doppler Mapping Instrument aboard the CYGNSS satellite constellation. &lt;br&gt;&lt;br&gt; L3 MRG is a new product which combines the L2 FDS and Young Seas Limited Fetch (YSLF) winds and eliminates the need to choose between them depending on sea state development and the proximity to storms. The data are provided in netCDF-4 format and extend from 1 August 2018 to the present with an approximate 6 day latency. A tapered weighted averaging scheme is used centered on the 34-knot wind radius (R34) of the storm. The R34 value in each storm quadrant is also reported. The algorithm produces global (+/- 40 deg latitude) wind speeds reported on a 0.1x0.1 deg grid every 6 hours for each tropical cyclone, although some 6-hourly increments may be missing if there are an insufficient number of satellite overpasses of the storm during that time interval. The netcdf files are output on a storm-by-storm basis.&lt;br&gt;&lt;br&gt; The CYGNSS is a NASA Earth System Science Pathfinder Mission that is intended to collect the first frequent space‐based measurements of surface wind speeds in the inner core of tropical cyclones. Made up of a constellation of eight micro-satellites, the observatories provide nearly gap-free Earth coverage using an orbital inclination of approximately 35° from the equator, with a mean (i.e., average) revisit time of seven hours and a median revisit time of three hours. This inclination allows CYGNSS to measure ocean surface winds between approximately 38° N and 38° S latitude. This range includes the critical latitude band for tropical cyclone formation and movement.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l3_mrg_v321&quot;&gt;CYGNSS_L3_MRG_V3.2.1&lt;/h4&gt;
This dataset contains the version 3.2.1 CYGNSS level 3 science data record merged storm (MRG) wind speed which combines CYGNSS storm-centric gridded (SCG) wind speeds, which are derived from the L2 Young Seas Limited Fetch (YSLF) winds for a region surrounding a given tropical cyclone (TC), with L3 Fully Developed Seas (FDS) winds away from the TC center on a 0.2x0.2 degree latitude by longitude equirectangular grid obtained from the Delay Doppler Mapping Instrument aboard the CYGNSS satellite constellation. &lt;br&gt;&lt;br&gt; L3 MRG combines the L2 FDS and Young Seas Limited Fetch (YSLF) winds and eliminates the need to choose between them depending on sea state development and the proximity to storms. The data are provided in netCDF-4 format and extend from 1 August 2018 to the present with an approximate 6 day latency. A tapered weighted averaging scheme is used centered on the 25 m/s wind radius of the storm. The 34 knot wind radius (R34) algorithm has been updated for v3.2.1 release to center around the National Hurricane Center or the Joint Typhoon Warning Center (NHC/JTWC) reported storm center instead of the CYGNSS Vmax location. The algorithm produces global (+/- 40 deg latitude) wind speeds reported on a 0.1x0.1 deg grid every 6 hours for each tropical cyclone, although some 6-hourly increments may be missing if there are an insufficient number of satellite overpasses of the storm during that time interval. The netCDF files are output on a storm-by-storm basis. &lt;br&gt;&lt;br&gt; The CYGNSS is a NASA Earth System Science Pathfinder Mission that is intended to collect the first frequent space‐based measurements of surface wind speeds in the inner core of tropical cyclones. Made up of a constellation of eight micro-satellites, the observatories provide nearly gap-free Earth coverage using an orbital inclination of approximately 35° from the equator, with a mean (i.e., average) revisit time of seven hours and a median revisit time of three hours. This inclination allows CYGNSS to measure ocean surface winds between approximately 38° N and 38° S latitude. This range includes the critical latitude band for tropical cyclone formation and movement.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l3_mrg_v322&quot;&gt;CYGNSS_L3_MRG_V3.2.2&lt;/h4&gt;
This dataset contains the version 3.2.2 CYGNSS level 3 science data record merged storm (MRG) wind speed which combines CYGNSS storm-centric gridded (SCG) wind speeds, which are derived from the L2 Young Seas Limited Fetch (YSLF) winds for a region surrounding a given tropical cyclone (TC), with L3 Fully Developed Seas (FDS) winds away from the TC center on a 0.2x0.2 degree latitude by longitude equirectangular grid obtained from the Delay Doppler Mapping Instrument aboard the CYGNSS satellite constellation. &lt;br&gt;&lt;br&gt; L3 MRG combines the L2 FDS and Young Seas Limited Fetch (YSLF) winds and eliminates the need to choose between them depending on sea state development and the proximity to storms. The data are provided in netCDF-4 format and extend from 1 August 2018 to the present with an approximate 6 day latency. A tapered weighted averaging scheme is used centered on the 25 m/s wind radius of the storm. The 34 knot wind radius (R34) algorithm was updated for the v3.2.1 release to center around the National Hurricane Center or the Joint Typhoon Warning Center (NHC/JTWC) reported storm center instead of the CYGNSS Vmax location. The algorithm produces global (+/- 40 deg latitude) wind speeds reported on a 0.1x0.1 deg grid every 6 hours for each tropical cyclone, although some 6-hourly increments may be missing if there are an insufficient number of satellite overpasses of the storm during that time interval. The netCDF files are output on a storm-by-storm basis. &lt;br&gt;&lt;br&gt; The CYGNSS is a NASA Earth System Science Pathfinder Mission that is intended to collect the first frequent space‐based measurements of surface wind speeds in the inner core of tropical cyclones. Made up of a constellation of eight micro-satellites, the observatories provide nearly gap-free Earth coverage using an orbital inclination of approximately 35° from the equator, with a mean (i.e., average) revisit time of seven hours and a median revisit time of three hours. This inclination allows CYGNSS to measure ocean surface winds between approximately 38° N and 38° S latitude. This range includes the critical latitude band for tropical cyclone formation and movement.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l3_microplastic_v32&quot;&gt;CYGNSS_L3_MICROPLASTIC_V3.2&lt;/h4&gt;
The CYGNSS L3 Ocean Microplastic Concentration V3.2 dataset is provided by the CYGNSS Science Team of the University of Michigan. CYGNSS was launched on 15 December 2016, it is a NASA Earth System Science Pathfinder Mission that was launched with the purpose of collecting the first frequent space‐based measurements of surface wind speeds in the inner core of tropical cyclones. Originally made up of a constellation of eight micro-satellites, the observatories provide nearly gap-free Earth coverage using an orbital inclination of approximately 35° from the equator, with a mean (i.e., average) revisit time of seven hours and a median revisit time of three hours. &lt;br&gt;&lt;br&gt; This dataset contains the version 3.2 CYGNSS Level 3 ocean microplastic concentration data record, which provides daily netCDF files, each file containing a gridded map of microplastic number density (#/km^2). Microplastic concentration number density is indirectly estimated by an empirical relationship between ocean surface roughness and wind speed (Evans and Ruf, 2021). User caution is advised in regions containing independent, non-correlative factors affecting ocean surface roughness, such as anomalous atmospheric conditions within the Intertropical Convergence Zone, biogenic surfactants (such as algal blooms), oil spills, etc. This product reports microplastic concentration on a daily temporal and 0.25-degree latitude/longitude spatial grid with 30-day, 1 degree latitude/longitude feature resolution, as constrained by the binning and spatial temporal averaging of the Mean Square Slope (MSS) anomaly (i.e., difference between measured and predicted ocean surface roughness for a given wind speed). Version 3.2 uses CYGNSS MSS measurements that are derived from updated v3.2 Level 1 scattering cross section data and has updated the parameterizations in the data processing algorithm to use v3.2 data correctly.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l3_v21&quot;&gt;CYGNSS_L3_V2.1&lt;/h4&gt;
This dataset contains the Version 2.1 CYGNSS Level 3 Science Data Record which provides the average wind speed and mean square slope (MSS) on a 0.2x0.2 degree latitude by longitude equirectangular grid obtained from the Delay Doppler Mapping Instrument aboard the CYGNSS satellite constellation. The Level 2 Delay Doppler Map (DDM) data are used in the direct processing of the average wind speed and MSS data that are binned on the Level 3 grid. A subset of DDM data used in the direct processing of the average wind speed and MSS is co-located inside of the Level 2 data files. A single netCDF-4 data file is produced for each day of operation with an approximate 6 day latency. This version supersedes Version 2.0. The reported sample locations are determined by the specular points corresponding to the Delay Doppler Maps (DDMs). The Version 2.1 release represents the second science-quality release. Here is a summary of improvements that reflect the quality of the Version 2.1 data release: 1) first time availability of wind speeds using the Geophysical Model Function (GMF) calibrated for Young Seas with Limited Fetch (YSLF) conditions; 2) inherits all other improvements made to the version 2.1 Level 2 data intended to improve the quality of the wind speed retrievals and uncertainty estimates. For a full list of improvements to the version 2.1 Level 2 data, please refer to the following dataset information page: &lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/CYGNSS_L2_V2.1&quot;&gt;https://podaac.jpl.nasa.gov/dataset/CYGNSS_L2_V2.1&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l3_v30&quot;&gt;CYGNSS_L3_V3.0&lt;/h4&gt;
This dataset contains the Version 3.0 CYGNSS Level 3 Science Data Record which provides the average wind speed and mean square slope (MSS) on a 0.2x0.2 degree latitude by longitude equirectangular grid obtained from the Delay Doppler Mapping Instrument aboard the CYGNSS satellite constellation. The Level 2 Delay Doppler Map (DDM) data are used in the direct processing of the average wind speed and MSS data that are binned on the Level 3 grid. A subset of DDM data used in the direct processing of the average wind speed and MSS is co-located inside of the Level 2 data files. A single netCDF-4 data file is produced for each day of operation with an approximate 6 day latency. This version supersedes Version 2.1; &lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L3X21&quot;&gt;https://doi.org/10.5067/CYGNS-L3X21&lt;/a&gt;. The reported sample locations are determined by the specular points corresponding to the Delay Doppler Maps (DDMs). The Version 3.0 release inherits all improvements made to the version 3.0 Level 2 data intended to improve the quality of the wind speed retrievals. For a full list of improvements to the version 3.0 Level 2 data, please refer to: &lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L2X30&quot;&gt;https://doi.org/10.5067/CYGNS-L2X30&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l3_v31&quot;&gt;CYGNSS_L3_V3.1&lt;/h4&gt;
This dataset contains the Version 3.1 CYGNSS Level 3 Science Data Record which provides the average wind speed and mean square slope (MSS) on a 0.2x0.2 degree latitude by longitude equirectangular grid obtained from the Delay Doppler Mapping Instrument aboard the CYGNSS satellite constellation. The Level 2 Delay Doppler Map (DDM) data are used in the direct processing of the average wind speed and MSS data that are binned on the Level 3 grid. A subset of DDM data used in the direct processing of the average wind speed and MSS is co-located inside of the Level 2 data files. A single netCDF-4 data file is produced for each day of operation with an approximate 6 day latency. This version supersedes Version 3.0; &lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L3X30&quot;&gt;https://doi.org/10.5067/CYGNS-L3X30&lt;/a&gt;. The reported sample locations are determined by the specular points corresponding to the Delay Doppler Maps (DDMs). The Version 3.1 release inherits all improvements made to the version 3.1 Level 2 data intended to improve the quality of the wind speed retrievals. For a full list of improvements to the version 3.1 Level 2 data, please refer to: &lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L2X31&quot;&gt;https://doi.org/10.5067/CYGNS-L2X31&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l3_soil_moisture_v32&quot;&gt;CYGNSS_L3_SOIL_MOISTURE_V3.2&lt;/h4&gt;
The CYGNSS Level 3 Soil Moisture V3.2 dataset is provided by the CYGNSS Science Team of the University of Michigan. It estimates volumetric water content for soils between 0-5 cm depth at a 6-hour discretization for most of the subtropics from the V3.2 reflectivity measurements provided in the CYGNSS L1 SDR dataset (&lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L1X32&quot;&gt;https://doi.org/10.5067/CYGNS-L1X32&lt;/a&gt;). CYGNSS was launched on 15 December 2016, it is a NASA Earth System Science Pathfinder Mission that was launched with the purpose of collecting the first frequent space‐based measurements of surface wind speeds in the inner core of tropical cyclones. Originally made up of a constellation of eight micro-satellites, the observatories provide nearly gap-free Earth coverage using an orbital inclination of approximately 35° from the equator, with a mean (i.e., average) revisit time of seven hours and a median revisit time of three hours. &lt;br&gt;&lt;br&gt; The soil moisture retrieval algorithm is an update of the previous version developed by UCAR-CU using a linear regression of CYGNSS angle-normalized effective surface reflectivity trained against collocated SMAP soil moisture during the calibration period 8/1/2018 to 11/15/2023. The data are archived in daily files in netCDF-4 format. Volumetric soil moisture water content in units of cm3/cm3 is provided with two gridding resolutions, 9x9 km and 36x36 km. The variable SM_subdaily contains data reported in six hour intervals. The variable SM_daily provides a daily average. The time series covers the period from August 2018 to present.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l3_s10&quot;&gt;CYGNSS_L3_S1.0&lt;/h4&gt;
This dataset contains the Version 1.0 Cyclone Global Navigation Satellite System (CYGNSS) Level 3 Storm Centric Grid (SCG) Science Data Record (SDR) which provides the average wind speed combined from aggregated wind speed measurements made by the entire CYGNSS constellation whose specular points are located near a storm of interest in latitude, longitude and time. Data are provided on both a 0.1x0.1 degree latitude by longitude equirectangular grid and storm centric coordinates obtained from the Delay Doppler Mapping Instrument (DDMI) aboard the CYGNSS satellite constellation. Storm centric coordinates are derived from the National Hurricane Center (NHC) Best Track dataset to produce a 6 hourly wind speed averaging window. A single netCDF-4 data file is produced for each storm. Each storm is uniquely identified by the year, storm basin, and a storm number. This dataset is intended for historical storm analysis, and as such, this dataset is periodically updated based on the availability of the NHC Best Track storm center information that is typically made available in April for the previous year&amp;#39;s hurricane season. SCG files are produced for named storms, as defined by the NHC, that reach hurricane strength (i.e., having a maximum sustained wind speed of at least 65 knots). Due to the dependency on NHC Best Track data, the SCG files produced in this dataset are confined to storms in the Northern Hemisphere within the North Atlantic and East Pacific ocean regions. Wind speed inputs are provided by the CYGNSS Level 2 SDR Version 3.0 (&lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L2X30&quot;&gt;https://doi.org/10.5067/CYGNS-L2X30&lt;/a&gt; ).
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_noaa_l2_swsp_25km_v12&quot;&gt;CYGNSS_NOAA_L2_SWSP_25KM_V1.2&lt;/h4&gt;
This dataset contains the Version 1.2 NOAA CYGNSS Level 2 Science Wind Speed Product Version 1.2 which provides the time-tagged and geolocated average wind speed (m/s) in 25x25 kilometer grid cells along the measurement tracks from the Delay Doppler Mapping Instrument (DDMI) aboard the CYGNSS satellite constellation. This version corresponds to the second science-quality released through the PO.DAAC, as produced by NOAA/NESDIS using a specific geophysical model function (GMF version 1.0) and a track-wise debiasing algorithm as part of the wind speed retrieval process. The reported retrieval locations are determined by averaging the specular point locations falling within each 25 km grid cell. Version 1.2 includes four major updates compared to Version 1.1 ( &lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNN-22511&quot;&gt;https://doi.org/10.5067/CYGNN-22511&lt;/a&gt; ), namely: 1) the inclusion of data associated to a spacecraft roll angle exceeding +/- 5 degrees; 2) an improved wind speed performance in the higher wind speed regime; 3) a full revision of the quality flags; 4) the inclusion of a wind speed retrieval error variable. Only one netCDF-4 data file is produced for each day (each file containing data from up to 8 unique CYGNSS spacecraft) with a latency of approximately 6 days (or better) from the last recorded measurement time. Formatting of the data variables and metadata designed to be consistent with the netCDF-4 formatting provided by the legacy CYGNSS mission Level 2 wind speed science data record (SDR).
&lt;br&gt;&lt;h4 id&#x3D;&quot;rongowai_l1_sdr_v10&quot;&gt;RONGOWAI_L1_SDR_V1.0&lt;/h4&gt;
The Rongowai Level 1 Science Data Record Version 1.0 dataset is generated by the University of Auckland (UoA) Rongowai Science Payloads Operations Centre in New Zealand. This initiative is supported by NASA and the New Zealand Space Agency. The data collection process is conducted using the Next-generation receiver (NgRx) mounted on the Air New Zealand domestic aircraft Q300.&lt;br&gt;&lt;br&gt; This Level 1 (L1) dataset contains the Version 1.0 geo-located Delay Doppler Maps (DDMs) calibrated into Power Received (Watts) and Bistatic Radar Cross Section (BRCS) expressed in units of meters squared from the Delay Doppler Mapping Instrument onboard an Air New Zealand domestic Q300 (tail number ZK-NFA). 20 DDMs are contained within a typical L1 netcdf corresponding to 10 Left-Hand-Circularly Polarized (LHCP) and 10 Right-Hand-Circularly Polarized (RHCP) channels. Other useful scientific and engineering measurement parameters include the co- and cross-polarized Normalized Bistatic Radar Cross Section (NBRCS) of the specular point, the Leading Edge Slope (LES) of the integrated delay waveform and the normalized waveforms. The L1 dataset contains a number of other engineering and science measurement parameters, including coherence detection and a coherence state metric, sets of quality flags/indicators, error estimates, Fresnel-zone geometry estimates (and thereby the estimated per-sample spatial resolution) as well as a variety of timekeeping, and geolocation parameters. Each netCDF data files corresponds to a single flight between airports within New Zealand (flight durations typically range between 45 min and 1hr 30min with a median of 7 flights/day) and measurements are reported at 1 second increments. Latency is approximately 1 days (or better) from the last recorded measurement time.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l3_uc_berkeley_watermask_daily_v32&quot;&gt;CYGNSS_L3_UC_BERKELEY_WATERMASK_DAILY_V3.2&lt;/h4&gt;
The CYGNSS Level 3 UC Berkeley Watermask Record Version 3.2 was developed by CYGNSS investigators in the Department of Civil and Environmental Engineering at the University of California, Berkeley. CYGNSS was launched on 15 December 2016, it is a NASA Earth System Science Pathfinder Mission that was launched with the purpose of collecting the first frequent space‐based measurements of surface wind speeds in the inner core of tropical cyclones. Originally made up of a constellation of eight micro-satellites, the observatories provide nearly gap-free Earth coverage using an orbital inclination of approximately 35° from the equator, with a mean (i.e., average) revisit time of seven hours and a median revisit time of three hours. &lt;br&gt;&lt;br&gt; This dataset is derived from version 3.2 of the CYGNSS L1 SDR dataset (&lt;href&gt;&lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L1X32&quot;&gt;https://doi.org/10.5067/CYGNS-L1X32&lt;/a&gt;&lt;/href&gt;). This is an update from the previous watermask monthly product (&lt;href&gt;&lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L3W31&quot;&gt;https://doi.org/10.5067/CYGNS-L3W31&lt;/a&gt;&lt;/href&gt;) which derived from the CYGNSS L1 SDR v3.1 (&lt;href&gt;&lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L1X31&quot;&gt;https://doi.org/10.5067/CYGNS-L1X31&lt;/a&gt;&lt;/href&gt;). The new product provides daily binary inland surface water classification data at a 0.01-degree (~1x1 kilometer) resolution with an approximate 6-day latency. The algorithm utilized data from up to 30 days prior to generate the daily map. This product, known as the UC Berkeley Random Walk Algorithm WaterMask from CYGNSS (Berkeley-RWAWC), generates water classification for a given location based on CYGNSS observations combined with a random walker algorithm. The watermask variable includes binary values indicating land (0), surface water (1), and no data/ocean (-99). The data product is archived in daily files in netCDF-4 format and covers the period from September 2018 to present. &lt;br&gt;&lt;br&gt; This product is recommended for operational use. For science applications, we recommend the use of the Berkeley-RWAWC monthly product instead: &lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/CYGNSS_L3_UC_BERKELEY_WATERMASK_V3.1&quot;&gt;https://podaac.jpl.nasa.gov/dataset/CYGNSS_L3_UC_BERKELEY_WATERMASK_V3.1&lt;/a&gt; Note that the daily product consist of maps constructed using the most recent 31 days of data to rapidly capture surface water dynamics without relying on historical data. While the oldest data within this 31 day-period is weighted less and replaced by newer observations as they become available, extreme flood events may still be detected with a delay due to the incorporation of prior days’ data into the algorithm. The incorporation of older data is necessary to maintain the spatial scale.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l3_uc_berkeley_watermask_v31&quot;&gt;CYGNSS_L3_UC_BERKELEY_WATERMASK_V3.1&lt;/h4&gt;
The CYGNSS Level 3 UC Berkeley Watermask Record Version 3.1 was developed by CYGNSS investigators in the Department of Civil and Environmental Engineering at the University of California, Berkeley. CYGNSS was launched on 15 December 2016, it is a NASA Earth System Science Pathfinder Mission that was launched with the purpose of collecting the first frequent space‐based measurements of surface wind speeds in the inner core of tropical cyclones. Originally made up of a constellation of eight micro-satellites, the observatories provide nearly gap-free Earth coverage using an orbital inclination of approximately 35° from the equator, with a mean (i.e., average) revisit time of seven hours and a median revisit time of three hours. &lt;br&gt;&lt;br&gt; This dataset is derived from version 3.1 of the CYGNSS L1 SDR dataset (&lt;a href&#x3D;&quot;https://doi.org/10.5067/CYGNS-L1X31&quot;&gt;https://doi.org/10.5067/CYGNS-L1X31&lt;/a&gt;), and provides monthly binary inland surface water classification data at a 0.01-degree (~1x1 kilometer) resolution with a 1-month latency. This product, known as the UC Berkeley Random Walk Algorithm WaterMask from CYGNSS (Berkeley-RWAWC), generates water classification for a given location based on CYGNSS observations combined with a random walker algorithm. The watermask variable includes binary values indicating land (0), surface water (1), and no data/ocean (-99). The data product is archived in monthly files in netCDF-4 format and covers the period from August 2018 to present.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cygnss_l3_soil_moisture_v10&quot;&gt;CYGNSS_L3_SOIL_MOISTURE_V1.0&lt;/h4&gt;
The CYGNSS Level 3 Soil Moisture Product provides volumetric water content estimates for soils between 0-5 cm depth at a 6-hour discretization for most of the subtropics. The data were produced by CYGNSS investigators at the University Corporation for Atmospheric Research (UCAR) and the University Colorado at Boulder (CU), and derive from version 2.1 of the CYGNSS L1 SDR. The soil moisture algorithm uses collocated soil moisture retrievals from SMAP to calibrate CYGNSS observations from the same day. For a given location, a linear relationship between the SMAP soil moisture and CYGNSS reflectivity is determined and used to transform the CYGNSS observations into soil moisture. The data are archived in daily files in netCDF-4 format. Two soil moisture variables report the volumetric water content in units of cm3/cm3. The variable SM_subdaily includes up to four soil moisture estimates per day. Another variable SM_daily provides a daily average. The time series covers the period from March 2017 to present.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://archive.podaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA Climate Project</title>
      <link>https://registry.opendata.aws/nasa-climate</link>
      <guid>https://registry.opendata.aws/nasa-climate</guid>
      <description>This dataset provides two 30-year climate normal data products for conditions during the last glacial maximum (LGM; ~18,000 years ago) and a modern time period (1975-2005) for the entire state of Alaska. The first set of products are monthly climate variable averages at 60 m resolution, including: minimum, maximum, and average temperatures, total precipitation, total surface radiation, rain, snow, potential evapotranspiration (PET), actual evapotranspiration (AET), and water deficit. The second set of products are annual summary climate variable averages for the same variables (excepting average temperature and rain) at 60m, 120m, 240m, 800m, 1km, 2km, 3km, 4km, 5km, 10km and 12km resolutions. The 30-year climate normal monthly averages were derived by topographically downscaling climate variables from existing coarse-resolution general circulation model outputs combined with local weather station data and digital surface models for Alaska for both the LGM and modern time periods at 60 m resolution. From this baseline, monthly averages for total surface radiation, rain, snow, potential evapotranspiration, actual evapotranspiration, and water deficit were also modeled. The annual averages are coarser resolution upsampled versions of the 60 m resolution monthly average data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nasasatellite_dev_applications_2293&quot;&gt;NASASatellite_Dev_Applications_2293&lt;/h4&gt;
This dataset provides a presentation that highlights the role NASA research and researchers played in developing a wide range of significant, quantitative ecological applications of satellite data. The presentation by Dr Diane E. Wickland, former NASA Terrestrial Ecology Program Manager and Lead for NASA Carbon Cycle and Ecosystems Focus Area, provides a top-level overview from her perspective of the development and evolution of the program. Dr Wickland joined NASA in 1985 to manage a newly formed Terrestrial Ecosystems Program. Along with other NASA program managers, she was charged with reorienting the program to be less empirical and have a greater focus on first principles, and to prepare for a next generation of earth-observing satellites. As an ecologist, she thought that focusing on important ecological questions and recruiting practicing ecologists to the program would facilitate such a change in directions. The presentation emphasizes the early years of U.S. satellite remote sensing and covers a few highlights after 2005.
&lt;br&gt;&lt;h4 id&#x3D;&quot;eastanglia10yearmean_549&quot;&gt;EastAnglia10YearMean_549&lt;/h4&gt;
This is a data set of 10-year mean monthly surface climate data over global land areas, excluding Antarctica, for the period 1901-1990. The data set is gridded at 0.5 degree latitude/longitude resolution and includes seven variables: precipitation, mean temperature, diurnal temperature range, wet-day frequency, vapour pressure, cloud cover, and ground-frost frequency. In constructing the monthly grids the authors used an anomaly approach which attempts to maximize station data in space and time (New et al., 2000). In this technique, grids of monthly historic anomalies are derived relative to a standard normal period. Station measurement data for the years 1961-1990, extracted from the monthly data holdings of the Climatic Research Unit and the Global Historic Climatology Network (GHCN), served as the normal period (New et al., 1999). The anomaly grids were then combined with high-resolution mean monthly climatology to arrive at fields of estimated historical monthly surface climate. Data users are encouraged to see the companion file New et al.(2000) for a complete description of this technique and potential applications and limitations of the data set. For additional information, refer to the IPCC Data Distribution Centre.
&lt;br&gt;&lt;h4 id&#x3D;&quot;eastanglia30yearmean_550&quot;&gt;EastAnglia30YearMean_550&lt;/h4&gt;
This is a data set of 30-year mean monthly surface climate data over global land areas, excluding Antarctica, for the period 1901-1960. The data set is gridded at 0.5 degree latitude/longitude resolution and includes seven variables: precipitation, mean temperature, diurnal temperature range, wet-day frequency, vapour pressure, cloud cover, and ground-frost frequency. In constructing the monthly grids the authors used an anomaly approach which attempts to maximize station data in space and time (New et al., 2000). In this technique, grids of monthly historic anomalies are derived relative to a standard normal period. Station measurement data for the years 1961-1990, extracted from the monthly data holdings of the Climatic Research Unit and the Global Historic Climatology Network (GHCN), served as the normal period (New et al., 1999). The anomaly grids were then combined with high-resolution mean monthly climatology to arrive at fields of estimated historical monthly surface climate. Data users are encouraged to see the companion file New et al.(2000) for a complete description of this technique and potential applications and limitations of the data set. For additional information, refer to the IPCC Data Distribution Centre.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cramerleemans_416&quot;&gt;CramerLeemans_416&lt;/h4&gt;
This database is a major update of the Leemans and Cramer database (Leemans and Cramer 1991). It currently contains monthly averages of mean temperature, temperature range, precipitation, rain days and sunshine hours for the terrestrial surface of the globe, gridded at 0.5 degree longitude/latitude resolution. It was generated from a large data base, using the partial thin-plate splining algorithm developed by Michael F. Hutchinson, Canberra (Hutchinson and Bischof 1983).
&lt;br&gt;&lt;h4 id&#x3D;&quot;eastangliaclimate_542&quot;&gt;EastAngliaClimate_542&lt;/h4&gt;
This is a dataset of mean monthly surface climate measurements over global land areas, excluding Antarctica, for the period 1961-1990. Values were interpolated from station data to a 0.5 degree latitude/longitude grid for several climatic parameters: precipitation and wet-day frequency, mean temperature and diurnal temperature range (from which maximum temperature and minimum temperature can be determined), vapour pressure, sunshine, cloud cover, ground-frost frequency and windspeed. A description of the data files is provided as a companion file. For a complete documentation of the dataset, see New et al, 1999. Also refer to IPCC Data Distribution Centre.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cdiac_ndp41_220&quot;&gt;CDIAC_NDP41_220&lt;/h4&gt;
This data set contains monthly temperature, precipitation, sea-level pressure, and station-pressure data for thousands of meteorological stations worldwide. The database was compiled from pre-existing national, regional, and global collections of data as part of the Global Historical Climatology Network (GHCN) project, the goal of which is to produce, maintain, and make available a comprehensive global surface baseline climate data set for monitoring climate and detecting climate change. It contains data from roughly 6000 temperature stations, 7500 precipitation stations, 1800 sea level pressure stations, and 1800 station pressure stations. Each station has at least 10 years of data, 40% have more than 50 years of data. Spatial coverage is good over most of the globe, particularly for the United States and Europe. Data gaps are evident over the Amazon rainforest, the Sahara Desert, Greenland, and Antarctica.
&lt;br&gt;&lt;h4 id&#x3D;&quot;global_n_deposition_maps_830&quot;&gt;global_N_deposition_maps_830&lt;/h4&gt;
This data set provides global gridded estimates of atmospheric deposition of total inorganic nitrogen (N), NHx (NH3 and NH4+), and NOy (all oxidized forms of nitrogen other than N2O), in mg N/m2/year, for the years 1860 and 1993 and projections for the year 2050. The data set was generated using a global three-dimensional chemistry-transport model (TM3) with a spatial resolution of 5 degrees longitude by 3.75 degrees latitude (Jeuken et al., 2001; Lelieveld and Dentener, 2000). Nitrogen emissions estimates (Van Aardenne et al., 2001) and projection scenario data (IPCC, 1996; 2000) were used as input to the model. The model output grids were subdivided into 50 km x 50 km sub-grids to create spatially defined deposition maps. The gridded data were assigned to continental and marine regions using boundaries delineated on a world data coverage from ESRI (1993).The data are stored as ASCII text files (.txt), in tab delimited format. The data can be used to produce maps that illustrate both the temporal and spatial variability of atmospheric deposition of N, NHx, and NOy as well as the degree of alteration and regional heterogeneity in deposition through time. Nine data files are provided to produce the following maps:Global N Deposition (1860, 1993, and 2050)Global NHx Deposition (1860, 1993, and 2050)Global NOy Deposition (1860, 1993, and 2050).
&lt;br&gt;&lt;h4 id&#x3D;&quot;gis_eastangliaclimatemonthly_551&quot;&gt;GIS_EastAngliaClimateMonthly_551&lt;/h4&gt;
This is a data set of mean monthly surface climate data over global land areas, excluding Antarctica, for nearly all of the twentieth century. The data set is gridded at 0.5 degree latitude/longitude resolution and includes seven variables: precipitation, mean temperature, diurnal temperature range, wet-day frequency, vapour pressure, cloud cover, and ground-frost frequency. All variables have mean monthly values for the period 1901-1995, several have data as recent as 1998, and more data will be added by the data originators. In constructing the monthly grids the authors used an anomaly approach which attempts to maximize station data in space and time (New et al., 2000). In this technique, grids of monthly historic anomalies are derived relative to a standard normal period. Station measurement data for the years 1961-1990, extracted from the monthly data holdings of the Climatic Research Unit and the Global Historic Climatology Network (GHCN), served as the normal period (New et al., 1999). The anomaly grids were then combined with high-resolution mean monthly climatology to arrive at fields of estimated historical monthly surface climate. Data users are encouraged to see the companion file New et al. (2000) for a complete description of this technique and potential applications and limitations of the data set. For additional information, refer to the IPCC Data Distribution Centre. Access to the complete year-by-year monthly data set or to data more recent than posted here can be achieved by making a request with the Climate Impacts LINK Project at the Climatic Research Unit (email: &lt;a href&#x3D;&quot;mailto:&amp;#x64;&amp;#46;&amp;#118;&amp;#105;&amp;#x6e;&amp;#x65;&amp;#x72;&amp;#x40;&amp;#x75;&amp;#101;&amp;#x61;&amp;#x2e;&amp;#x61;&amp;#x63;&amp;#46;&amp;#x75;&amp;#x6b;&quot;&gt;&amp;#x64;&amp;#46;&amp;#118;&amp;#105;&amp;#x6e;&amp;#x65;&amp;#x72;&amp;#x40;&amp;#x75;&amp;#101;&amp;#x61;&amp;#x2e;&amp;#x61;&amp;#x63;&amp;#46;&amp;#x75;&amp;#x6b;&lt;/a&gt;, web site: &lt;a href&#x3D;&quot;http://www.cru.uea.ac.uk/link&quot;&gt;www.cru.uea.ac.uk/link&lt;/a&gt; ).
&lt;br&gt;&lt;h4 id&#x3D;&quot;eastangliaprecip_417&quot;&gt;EastAngliaPrecip_417&lt;/h4&gt;
An historical monthly precipitation dataset for global land areas from 1900 to 1996, gridded at two different resolutions (2.5 degrees latitude by 3.75 degrees longitude and 5 degrees latitude/longitude).
&lt;br&gt;&lt;h4 id&#x3D;&quot;global_n_cycle_797&quot;&gt;global_N_cycle_797&lt;/h4&gt;
Nitrogen is a major nutrient in terrestrial ecosystems and an important catalyst in tropospheric photochemistry. Over the last century human activities have dramatically increased inputs of reactive nitrogen (Nr, the combination of oxidized, reduced and organically bound nitrogen) to the Earth system. Nitrogen cycle perturbations have compromised air quality and human health, acidified ecosystems, and degraded and eutrophied lakes and coastal estuaries [Vitousek et al., 1997a, 1997b; Rabalais, 2002; Howarth et al., 2003; Townsend et al., 2003; Galloway et al., 2004]. To begin to quantify the changes to the global N cycle, we have assembled key flux data and N2O mixing ratios from various sources. The data assembled from different sources includes fertilizer production from 1920-2004; manure production from 1860-2004; crop N fixation estimated for three time points, 1860, 1900, 1995; tropospheric N2O mixing ratios from ice core and firn measurements, and tropospheric concentrations to cover the time period from 1756-2004. The changing N2O concentrations provide an independent index of changes to the global N cycle, in much the same way that changing carbon dioxide concentrations provide an important constraint on the global carbon cycle. The changes to the global N cycle are driven by industrialization, as indicated by fossil fuel NOx emission, and by the intensification of agriculture, as indicted by fertilizer and manure production and crop N2 fixation. The data set and the science it reflects are by nature interdisciplinary. Making the data set available through the ORNL DAAC is an attempt to make the data set available to the considerable interdisciplinary community studying the N cycle.
&lt;br&gt;&lt;h4 id&#x3D;&quot;global_lakes_methane_2008&quot;&gt;Global_Lakes_Methane_2008&lt;/h4&gt;
This dataset provides global gridded information on lake surface area and open water CH4 emissions at a resolution of 0.25-degree x 0.25-degree for an annual climatology representative of the average conditions from 2003 to 2015. A compilation of flux data from 575 individual lake systems and 893 aggregated flux values were used, and each flux measurement was classified into one of seven ecoclimatic types. Ice-cover-regulated emission seasonality was derived from satellite microwave observations of ice cover phenology and freeze-thaw dynamics. Global lake area was determined from the merger of HydroLAKES and Climate Change Initiative Inland-Water (CCI-IW) remote-sensing data, and lakes were classified into ecoclimatic regions to facilitate linking these types with ecosystem-specific CH4 measurements in the flux compilation. Exploratory estimates of fluxes associated with ice melt and with spring and fall water-column turnover are also included. The data are provided in NetCDF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;em27_xco2_xch4_xco_ak_1831&quot;&gt;EM27_XCO2_XCH4_XCO_AK_1831&lt;/h4&gt;
This dataset provides ground-based column-averaged dry mole fractions (DMFs) of CO2 (xco2), CO (xco), CH4 (xch4), and N2O (xn2o) to supplement satellite-based observations of carbon dynamics of northern boreal ecosystems. Measurements were conducted with Bruker EM27/SUN Fourier transform spectrometers (FTS) at the University of Alaska Fairbanks (UAF) and two sites on the edges of the Tanana Flats wetlands to the south from 2016-08-04 to 2019-10-31. Single detectors were used during the first campaign at UAF in 2017, then two instruments were updated to dual detectors in early 2018 to allow retrieval of xco and xn2o. Data from additional FTS instruments, operated by Los Alamos National Laboratories (LANL), Karlsruhe Institute of Technology (KIT), and Jet Propulsion Laboratory (JPL), employed in these campaigns are included.
&lt;br&gt;&lt;h4 id&#x3D;&quot;new_england_ch4_1311&quot;&gt;New_England_CH4_1311&lt;/h4&gt;
This data set contains an inventory of natural and anthropogenic methane emissions for all counties in the six New England states of Connecticut, Rhode Island, Massachusetts, Vermont, New Hampshire, and Maine. The inventory represents a snapshot in time (circa 1990-1994) and provides emission estimates for multiple sources including wetlands, landfills, ruminant animals, residential wood combustion, fossil fuel combustion and use, animal manure, wastewater treatment, and natural gas transmission pipelines. Also included is the uptake or sink of methane in relatively well-drained upland soils.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nitrogen_deposition_730&quot;&gt;nitrogen_deposition_730&lt;/h4&gt;
This data set contains data for wet and dry nitrogen-species deposition for the United States and Western Europe. Deposition data were acquired directly from monitoring programs in the United States and Europe covering time periods from 1978-1994 for wet deposition and from 1989-1994 for dry deposition and evaluated using similar quality assurance criteria to ensure comparability. A standard geostatistical method (kriging) was used to interpolate data onto a 0.5 x 0.5 degree resolution map for wet and dry deposition. Analysis of N deposition for these regions was limited by sampling density, frequency, and coverage. These spatially explicit wet and dry N fluxes also provide a tool for verifying regional and global models of atmospheric chemistry and transport, and represent critical inputs into terrestrial models of biogeochemistry. These data can be used to construct continental scale N budgets and to evaluate recent modification of land-atmosphere N exchange and ecosystem function (Holland et al., 2004). Data files of the site monitoring locations and monthly deposition averages are available in ASCII space-delimited format, and 0.5 x 0.5 degree gridded deposition values are available in both ASCII space-delimited format and ASCII grid format. The 11 mapped data images are available in .jpg format as companion files (e.g., Figs. 1 and 2). The complete set of 11 derived nitrogen-species 0.5 x 0.5 degree deposition maps is also available in .pdf format in the companion file. Other companion files include quality assurance plans and operating manuals available from and maintained by the United States and European monitoring networks.
&lt;br&gt;&lt;h4 id&#x3D;&quot;snowmelt_timing_maps_v2_1712&quot;&gt;Snowmelt_timing_maps_V2_1712&lt;/h4&gt;
This data set provides snowmelt timing maps (STMs), cloud interference maps, and a map with the count of calculated snowmelt timing values for North America. The STMs are based on the Moderate Resolution Imaging Spectroradiometer (MODIS) standard 8-day composite snow-cover product MOD10A2 collection 6 for the period 2001-01-01 to 2018-12-31. The STMs were created by conducting a time-series analysis of the MOD10A2 snow maps to identify the DOY of snowmelt on a per-pixel basis. Snowmelt timing (no-snow) was defined as a snow-free reading following two consecutive snow-present readings for a given 500-m pixel. The count of STM values is also reported, which represents the number of years on record in the STMs from 2001-2018.
&lt;br&gt;&lt;h4 id&#x3D;&quot;african_rainfall_patterns_1263&quot;&gt;African_Rainfall_Patterns_1263&lt;/h4&gt;
This data set describes rainfall distribution statistics over the African continent, including Madagascar. The rainfall estimates are based on data from the NASA Tropical Rainfall Measuring Mission (TRMM) measured between 1998 and 2012. Rainfall patterns were quantified using a gamma-based function and two Markov chain parameters with the aim to summarize the rainfall pattern to a small number of parameters and processes. These summary statistics are suitable for temporal downscaling. These data provide gridded (0.25 x 0.25-degree) estimates of 14-year mean monthly rainfall total amount (mm), frequency (count), intensity (mm/hr), and duration (hrs) of rainfall, as well as Markov chain and gamma-distribution parameters for use in temporal downscaling. The data are presented as a series of 12 netCDF (.nc) files.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.ornldaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA DIS Project</title>
      <link>https://registry.opendata.aws/nasa-dis</link>
      <guid>https://registry.opendata.aws/nasa-dis</guid>
      <description>The ORNL DAAC Spatial Data Access Tool (SDAT) is a suite of Web-based applications that enable users to visualize and download spatial data in user-selected spatial/temporal extents, file formats, and projections. SDAT incorporates Open Geospatial Consortium (OGC) standard Web services, including Web Coverage Service (WCS), Web Map Service (WMS), and Web Feature Service (WFS). The SDAT provides ORNL DAAC-archived data sets and additional relevant data products including agriculture, atmosphere, biosphere, climate indicators, human dimensions, land surface, oceans, terrestrial hydrosphere data types, and related model output data sets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.ornldaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA DSCOVR Project</title>
      <link>https://registry.opendata.aws/nasa-dscovr</link>
      <guid>https://registry.opendata.aws/nasa-dscovr</guid>
      <description>Deep Space Climate Observatory (DSCOVR) DSCOVR National Institute of Standards and Technology Advanced Radiometer (NISTAR) was explicitly designed to measure the global daytime radiation budget for an entire hemisphere using active cavity radiometers for three channels: total (0.2 - 100 um), SW (0.2 - 4.0 um), and near-infrared (0.7 - 4.0 um). To derive the Earth Radiation Budget (ERB) from NISTAR measurements, the Short Wave (SW) radiances need to be unfiltered first before they can be subtracted from the total to yield the Long Wave (LW) (4 - 100 um) radiances. Additionally, the Earth&amp;#39;s surface and atmosphere are anisotropic reflectors and emitters, resulting in a relatively complex variation of radiance leaving the Earth as a function of viewing and illumination. Converting radiance to flux requires using angular distribution models (ADMs) to account for the emittance and reflectance anisotropies. The anisotropies are characterized for all Earth Polychromatic Imaging Camera (EPIC) pixels by using the Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) empirical angular distribution models (ADMs), which are functions of scene types which are defined using many variables including surface type, cloud amount, cloud phase, and optical depth, and water vapor. EPIC composite product is used to provide accurate scene-type information. The EPIC composites are generated from cloud property retrievals from Low Earth Orbit/Geostationary Equatorial Orbit (LEO/GEO) imagers mapped into the EPIC pixels. The EPIC composite also includes ancillary data (i.e., surface type, snow and ice map, skin temperature, precipitable water, etc.) needed for anisotropic factor selections. The anisotropies at the EPIC-pixel are then used to calculate the global mean SW and LW anisotropic factors, then convert the NISTAR SW and LW radiances to fluxes. This product contains the time series of the daytime Earth radiation budget derived from the NISTAR measurements.
&lt;br&gt;&lt;h4 id&#x3D;&quot;dscovr_nistar_l1a&quot;&gt;DSCOVR_NISTAR_L1A&lt;/h4&gt;
DSCOVR_NISTAR_L1A is the Deep Space Climate Observatory (DSCOVR) National Institute of Standards &amp;amp; Technology Advanced Radiometer (NISTAR) Level 1A Radiance, Version 3 data product. NISTAR is a 4-band radiometer onboard THE National Oceanic and Atmospheric Administration&amp;#39;s (NOAA) DSCOVR spacecraft located at the Earth-Sun Lagrange-1 (L-1) point, from which vantage it continuously measures the reflected and emitted radiances of the sunlit face of the Earth. These measurements provide an accurate energy balance measurement that improves our understanding of the Earth&amp;#39;s radiation budget. NISTAR employs three electrical substitution radiometers and a photodiode to measure reflected sunlight and infrared emission from the Earth. NISTAR measures the absolute irradiance integrated over the entire sunlit face of Earth in four broadband channels minute-by-minute. NISTAR has a 1º field of view (FOV) that acts as one large pixel that encompasses the entire sunlit side of the Earth and a 7º field of regard. The four measurement bands and their uses are: 1) Total Radiation – 0.2 µm to 100 µm: total radiant power in the UV, visible, and infrared wavelengths emerging from Earth. 2) Total Solar Reflected – 0.2 µm to 4 µm: reflected solar radiance in UV, visible, and near-infrared wavelengths from Earth. 3) Near Infrared Solar Reflected – 0.7 µm to 4 µm: reflected near-infrared solar radiation from Earth. 4) Photodiode – 0.2 µm to 1.1 µm: tracks the stability of the filters and verifies co-alignment of NISTAR and EPIC. The Level 1A products have been converted to engineering units but retain one-to-one associations with the items in the raw telemetry from which they were derived. These data products are in HDF5 format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;dscovr_epic_l2_o3so2ai&quot;&gt;DSCOVR_EPIC_L2_O3SO2AI&lt;/h4&gt;
Robust cloud products are critical for the Deep Space Climate Observatory (DSCOVR) to contribute significantly to climate studies. Building on our team’s track record in cloud detection, cloud property retrieval, oxygen band exploitation, and DSCOVR-related studies, we propose to develop a suite of algorithms for generating the operational Earth Polychromatic Imaging Camera (EPIC) cloud mask, cloud height, and cloud optical thickness products. Multichannel observations will be used for cloud masking; the cloud height will be developed with information from the oxygen A- and B- band pairs (780 nm vs. 779.5 nm and 680 nm vs. 687.75 nm); for the cloud optical thickness retrieval, we propose an approach that combines the EPIC 680 nm observations and numerical weather model outputs. Preliminary results from radiative transfer modeling and proxy data applications show that the proposed algorithms are viable. Product validation will be conducted by comparing EPIC observations/retrievals with counterparts from coexisting Low Earth Orbit (LEO) and Geosynchronous Earth Orbit (GEO) satellites. The proposed work will include a rigorous uncertainty analysis based on theoretical and computational radiative transfer modeling that complements standard validation activities with physics-based diagnostics. We also plan to evaluate and improve the calibration of the EPIC O2 A- and B-band absorption channels by tracking the instrument performance over known targets, such as cloud-free ocean and ice sheet surfaces. The deliverables for the proposed work include an Algorithm Theoretical Basis Document (ATBD) for peer review, products generated with the proposed algorithms, and supporting research articles. The data products, archived at the Atmospheric Science Data Center (ASDC) at the NASA Langley Research Center, will provide essential inputs needed for the community to apply EPIC observations to climate research and better interpret The National Institute of Standards and Technology Advanced Radiometer (NISTAR) observations. The proposed work directly responds to the solicitation to “develop and implement the necessary algorithms and processes to enable various data products from EPIC sunrise to sunset observations once on orbit” and improve “the calibration of EPIC based on in-flight data.”
&lt;br&gt;&lt;h4 id&#x3D;&quot;dscovr_epic_l1a_misc&quot;&gt;DSCOVR_EPIC_L1A_MISC&lt;/h4&gt;
The Deep Space Climate Observatory (DSCOVR) mission&amp;#39;s Earth Polychromatic Imaging Camera (EPIC) Level 1A miscellaneous data products capture unique images of the Moon transiting across the Earth&amp;#39;s disk, dark space or Jupiter from the spacecraft&amp;#39;s position at Lagrange point L1. These specialized observations, stored in HDF5 format, contain calibrated radiance measurements across 10 spectral bands ranging from 317 nm (ultraviolet) to 780 nm (near-infrared). The images of the Moon transiting across the Earth&amp;#39;s disk or appearing alongside Earth included in the miscellaneous dataset provide a distinctive perspective of the Earth-Moon system from approximately one million miles away, offering valuable information for Earth-Moon system dynamics.
&lt;br&gt;&lt;h4 id&#x3D;&quot;dscovr_epic_l2_to3&quot;&gt;DSCOVR_EPIC_L2_TO3&lt;/h4&gt;
DSCOVR_EPIC_L2_TO3_v03 is Level2 Total Ozone derived from the Deep Space Climate Observatory (DSCOVR) Earth Polychromatic Imaging Camera (EPIC) using Level 1b version 3 inputs and version 3 ozone retrieval algorithm. The measurements from four EPIC UV (ultraviolet) channels derive the global distributions of total ozone over the entire sunlit portion of the Earth. A new soft calibration technique developed based on scene matching with OMPS gives calibrated EPIC radiances. The calibrated EPIC radiances derive science-quality total ozone products from EPIC consistent with those from other UV instruments. The retrieval algorithm uses wavelength triplets and assumes that the scene reflectivity changes linearly with wavelength. Version 3 algorithm includes several key modifications aimed to improve total ozone retrievals: a) switch to Version 3 Level 1b product with improved geolocation registration, flat field, and dark counts corrections; b) replace OMI-based (Ozone Monitoring Instrument) cloud height climatology with the simultaneous EPIC A-Band cloud height; c) update absolute calibrations using polar orbiting the NASA OMPS SNPP ( Ozone Mapping and Profiler Suite / Suomi National Polar-orbiting Partnership Ozone); d) add corrections for ozone profile shape and temperature; e) update algorithm and error flags to filter data; f) add column weighting functions for each observation to facilitate error analysis. EPIC ozone retrievals accurately capture short-term synoptic changes in total column ozone. With EPIC measurements from DSCOVR&amp;#39;s vantage point, synoptic ozone maps can be derived every 1-2 hours. Scene Reflectivity (clouds, aerosols, and surface) is derived from ozone retrieval. In conjunction with ozone, the scene reflectivity has been used to derive the amount of UV solar radiation reaching the ground, and surface UV Erythemal is also reported in these files.
&lt;br&gt;&lt;h4 id&#x3D;&quot;dscovr_epic_l3_par&quot;&gt;DSCOVR_EPIC_L3_PAR&lt;/h4&gt;
DSCOVR_EPIC_L3_PAR_01 is the Deep Space Climate Observatory (DSCOVR) Earth Polychromatic Imaging Camera (EPIC) Level 3 photosynthetically available radiation (PAR) version 1 data product. The EPIC observations of the Earth’s surface lit by the Sun made 13 times during the day in spectral bands centered on 443, 551, and 680 nm are used to estimate daily mean PAR at the ice-free ocean surface. PAR is defined as the quantum energy flux from the Sun in the 400-700 nm range. Daily mean PAR is the 24-hour averaged planar flux in that spectral range reaching the surface. It is expressed in E.m-2.d-1 (Einstein per meter squared per day). The factor required to convert E.m-2 d-1 units to mW.cm-2.µm-1 units are equal to 0.838 to an inaccuracy of a few percent regardless of meteorological conditions. The EPIC daily mean PAR product is generated on Plate Carrée (equal-angle) grid with an 18.4 km resolution at the equator and on an 18.4 km equal-area grid, i.e., the product is compatible with Ocean Biology Processing Group ocean color products. The EPIC PAR algorithm uses a budget approach, in which the solar irradiance reaching the surface is obtained by subtracting from the irradiance arriving at the top of the atmosphere (known), the irradiance reflected space (estimated from the EPIC Level 1b radiance data), taking into account atmospheric transmission (modeled). Clear and cloudy regions within a pixel do not need to be distinguished. This dismisses the need for often-arbitrary assumptions about cloudiness distribution and is therefore adapted to the relatively large EPIC pixels. A daily mean PAR is estimated on the source grid for each EPIC instantaneous daytime observation, assuming no cloudiness changes during the day, and the individual estimates are remapped and weight-averaged using the cosine of the Sun zenith angle. In the computations, wind speed, surface pressure, and water vapor amount are extracted from NCEP (National Centers for Environmental Prediction) Reanalysis 2 data, aerosol optical thickness, and angstrom coefficient from MERRA-2 (Modern-Era Retrospective analysis for Research and Applications, Version 2) data, and ozone amount from EPIC Level 2 data. Areas contaminated by sun glint are excluded using a threshold on sun glint reflectance calculated using wind data. Ice masking is based on NSIDC (National Snow and Ice Data Center) near real-time ice fraction data. Additional information about the EPIC ocean surface PAR products can be found at the NASA DSCOVR: EPIC website: &lt;a href&#x3D;&quot;https://epic.gsfc.nasa.gov/&quot;&gt;https://epic.gsfc.nasa.gov/&lt;/a&gt;, under “Science -&amp;gt; Products -&amp;gt; Ocean Surface” (&lt;a href&#x3D;&quot;https://epic.gsfc.nasa.gov/science/products/ocean&quot;&gt;https://epic.gsfc.nasa.gov/science/products/ocean&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;dscovr_epic_l3_par-image&quot;&gt;DSCOVR_EPIC_L3_PAR-IMAGE&lt;/h4&gt;
DSCOVR_EPIC_L3_PAR-image_01 is a view image showing data from DSCOVR_EPIC_L3_PAR, which is the Deep Space Climate Observatory (DSCOVR) Earth Polychromatic Imaging Camera (EPIC) Level 3 photosynthetically available radiation (PAR) version 1 data product. The EPIC observations of the Earth’s surface lit by the Sun made 13 times during the day in spectral bands centered on 443, 551, and 680 nm are used to estimate daily mean PAR at the ice-free ocean surface. PAR is defined as the quantum energy flux from the Sun in the 400-700 nm range. Daily mean PAR is the 24-hour averaged planar flux in that spectral range reaching the surface. It is expressed in E.m-2.d-1 (Einstein per meter squared per day). The factor required to convert E.m-2 d-1 units to mW.cm-2.µm-1 units are equal to 0.838 to an inaccuracy of a few percent regardless of meteorological conditions. The EPIC daily mean PAR product is generated on Plate Carrée (equal-angle) grid with an 18.4 km resolution at the equator and on an 18.4 km equal-area grid, i.e., the product is compatible with Ocean Biology Processing Group ocean color products. The EPIC PAR algorithm uses a budget approach, in which the solar irradiance reaching the surface is obtained by subtracting from the irradiance arriving at the top of the atmosphere (known), the irradiance reflected space (estimated from the EPIC Level 1b radiance data), taking into account atmospheric transmission (modeled). Clear and cloudy regions within a pixel do not need to be distinguished. This dismisses the need for often-arbitrary assumptions about cloudiness distribution and is therefore adapted to the relatively large EPIC pixels. A daily mean PAR is estimated on the source grid for each EPIC instantaneous daytime observation, assuming no cloudiness changes during the day, and the individual estimates are remapped and weight-averaged using the cosine of the Sun zenith angle. In the computations, wind speed, surface pressure, and water vapor amount are extracted from NCEP (National Centers for Environmental Prediction) Reanalysis 2 data, aerosol optical thickness, and angstrom coefficient from MERRA-2 (Modern-Era Retrospective analysis for Research and Applications, Version 2) data, and ozone amount from EPIC Level 2 data. Areas contaminated by sun glint are excluded using a threshold on sun glint reflectance calculated using wind data. Ice masking is based on NSIDC (National Snow and Ice Data Center) near real-time ice fraction data. Additional information about the EPIC ocean surface PAR products can be found at the NASA DSCOVR: EPIC website: &lt;a href&#x3D;&quot;https://epic.gsfc.nasa.gov/&quot;&gt;https://epic.gsfc.nasa.gov/&lt;/a&gt;, under “Science -&amp;gt; Products -&amp;gt; Ocean Surface” (&lt;a href&#x3D;&quot;https://epic.gsfc.nasa.gov/science/products/ocean&quot;&gt;https://epic.gsfc.nasa.gov/science/products/ocean&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;dscovr_epic_l3_par-1&quot;&gt;DSCOVR_EPIC_L3_PAR&lt;/h4&gt;
EPIC Ocean Surface PAR The EPIC observations of the Earth’s surface lit by the Sun made 13 times during the day in spectral bands centered on 443, 551, and 680 nm are used to estimate daily mean photosynthetically available radiation (PAR) at the ice-free ocean surface. PAR is defined as the quantum energy flux from the Sun in the 400-700 nm range. Daily mean PAR is the 24-hour averaged planar flux in that spectral range reaching the surface. It is expressed in E.m-2.d-1 (Einstein per meter squared per day). The factor required to convert E.m-2 d-1 units to mW.cm-2.μm-1 units is equal to 0.838 to an inaccuracy of a few percent regardless of meteorological conditions. The EPIC daily mean PAR product is generated on Plate Carrée (equal-angle) grid with 18.4 km resolution at the equator and on 18.4 km equal-area grid, i.e., the product is compatible with Ocean Biology Processing Group ocean color products. The EPIC PAR algorithm uses a budget approach, in which the solar irradiance reaching the surface is obtained by subtracting from the irradiance arriving at the top of the atmosphere (known) the irradiance reflected to space (estimated from the EPIC Level 1b radiance data), taking into account atmospheric transmission (modeled). Clear and cloudy regions within a pixel do not need to be distinguished, which dismisses the need for often-arbitrary assumptions about cloudiness distribution and is therefore adapted to the relatively large EPIC pixels. A daily mean PAR is estimated on the source grid for each EPIC instantaneous daytime observation, assuming no cloudiness change during the day, and the individual estimates are remapped and weight-averaged using the cosine of the Sun zenith angle. In the computations, wind speed, surface pressure, and water vapor amount are extracted from NECP Reanalysis 2 data, aerosol optical thickness and angstrom coefficient fromMERRA-2 data, and ozone amount from EPIC Level 2 data. Areas contaminated by sun glint are excluded using a threshold on sun glint reflectance calculated using wind data. Ice masking is based on NSIDC near real time ice fraction data. Details about the algorithm are given in Frouinet al., (2018). Figure A1 gives an example of EPIC daily mean PAR product. Date is March 20, 2018(equinox); land is in black and sea ice in white. Values range from a few E.m-2.d-1at high latitudes to about 58 E.m-2.d-1 at equatorial and tropical latitudes, with atmospheric perturbances modulating the surface PAR field especially at middle latitudes. The EPIC ocean surface PAR products are available at the Atmospheric Science Data Center (ASDC) at NASA Langley Research Center: &lt;a href&#x3D;&quot;https://asdc.larc.nasa.gov&quot;&gt;https://asdc.larc.nasa.gov&lt;/a&gt;. 4. Reference Robert Frouin, Jing Tan, Didier Ramon, Bryan Franz, Hiroshi Murakami, 2018: Estimating photosynthetically available radiation at the ocean surface from EPIC/DSCOVR data, Proc. SPIE 10778, Remote Sensing of the Open and Coastal Ocean and Inland Waters, 1077806 (24 October 2018); doi: 10.1117/12.2501675. Changes from version 1 1) Algorithm (consistent with PACE) Updated the calculation of atmospheric reflectance, gaseous transmittance, and atmospheric transmittance using LUTs method so that calculations are accurate at high Sun and view zenith angles; Updated the calculation of surface albedo (based on Jin et al., 2011); Updated the calculation of cloud/surface layer albedo. 2)Ancillary data Changed the sources of the ancillary data including wind speed, surface pressure, and water vapor from NCEP to MERRA2; Added cloud fraction from MERRA2, which is needed for computing direct/diffuse ratio hence surface albedo.
&lt;br&gt;&lt;h4 id&#x3D;&quot;dscovr_epic_l2_composite&quot;&gt;DSCOVR_EPIC_L2_COMPOSITE&lt;/h4&gt;
In DSCOVR_EPIC_L2_composite_01, cloud property retrievals from multiple imagers on low Earth orbit (LEO) satellites (including MODIS, VIIRS, and AVHRR) and geostationary (GEO) satellites (including GOES-13 and -15, METEOSAT-7 and -10, MTSAT-2, and Himawari-8) are used to generate the composite. Based on the Ceres cloud detection and retrieval system, all cloud properties were determined using a standard set of algorithms, the Satellite ClOud and Radiation Property Retrieval System (SatCORPS). Cloud properties from these LEO/GEO imagers are optimally merged together to provide a seamless global composite product at 5-km resolution by using an aggregated rating that considers five parameters (nominal satellite resolution, pixel time relative to the Earth Polychromatic Imaging Camera (EPIC) observation time, viewing zenith angle, distance from day/night terminator, and sun glint factor) and selects the best observation at the time nearest to the EPIC measurements. About 72% of the LEO/GEO satellite overpass times are within one hour of the EPIC measurements, while 92% are within two hours of the EPIC measurements. The global composite data are then remapped into the EPIC Field of View (FOV) by convolving the high-resolution cloud properties with the EPIC point spread function (PSF) defined with a half-pixel accuracy to produce the EPIC composite. PSF-weighted radiances and cloud properties averages are computed separately for each cloud phase. Ancillary data (i.e., surface type, snow and ice map, skin temperature, precipitable water, etc.) needed for anisotropic factor selections are also included in the composite. These composite images are produced for each observation time of the EPIC instrument (typically 300 to 600 composites per month).
&lt;br&gt;&lt;h4 id&#x3D;&quot;dscovr_epic_l2_maiac-daily&quot;&gt;DSCOVR_EPIC_L2_MAIAC-DAILY&lt;/h4&gt;
DSOCVR EPIC_L2 MAIAC-Daily_01 contains plots of data generated from DSCOVR_EPIC_L2_MAIAC_03, the DSCOVR EPIC L2 Multi-Angle Implementation of Atmospheric Correction (MAIAC) Version 03 data product. Data collection for this product is ongoing. The datasets visualized include Aerosol Layer Height (ALH), Aerosol Optical Depth, and Single Scattering Albedo at 340nm, 388nm, 443nm, 551 nm, 680nm, and 780nm. Level 2 Multi-Angle Implementation of Atmospheric Correction (MAIAC) provides an interdisciplinary suite of products for the Deep Space Climate Observatory (DSCOVR) Earth Polychromatic Imaging Camera (EPIC). The current version 3 reports the following products: a) Atmosphere: cloud mask, global aerosol optical depth at 443nm and 551nm, fine mode fraction (over the ocean), aerosol layer height (ALH) globally, and spectral aerosol absorption for detected biomass burning or mineral dust aerosols. The absorption information includes single scattering albedo at 340-780nm range, imaginary refractive index at 680nm (k0), and Spectral Absorption Exponent (SAE) characterizing spectral increase of imaginary refractive index from Red towards UV wavelengths. The aerosol optical properties {AOD, ALH, k0, SAE} are retrieved simultaneously by matching EPIC measurements in the UV-NIR range, including atmospheric oxygen A- and B-bands. b) Land: atmospherically corrected spectral bidirectional reflectance factors (BRF) along with Lambertian surface reflectance and bidirectional reflectance distribution function (BRDF) for the backscattering view geometries of EPIC. The BRDF is represented by three parameters of the Ross-Thick Li-Sparse model. c) Ocean: Water leaving reflectance (non-dimensional) at Ultraviolet-Visible (UV-Vis) bands. The parameters are provided at 10 km resolution on a zonal sinusoidal grid with a 1—to 2-hour temporal frequency. MAIAC version 03 also provides gap-filled global composite products for the Normalized Difference Vegetation Index (NDVI) over land and water, leaving reflectance in 5 UV-Vis bands over the global ocean. The composite products represent a weighted running average where the weight of the latest observation is maximized towards the local noon and low aerosol conditions.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.asdc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA Daymet Project</title>
      <link>https://registry.opendata.aws/nasa-daymet</link>
      <guid>https://registry.opendata.aws/nasa-daymet</guid>
      <description>This dataset provides annual climate summaries derived from Daymet Version 4 R1 daily data at a 1 km x 1 km spatial resolution for five Daymet variables: minimum and maximum temperature, precipitation, vapor pressure, and snow water equivalent. Annual averages are provided for minimum and maximum temperature, vapor pressure, and snow water equivalent, and annual totals are provided for the precipitation variable. Each data file is provided as a single year by variable and covers the same period of record as the Daymet V4 R1 daily data. The annual climatology files are derived from the larger datasets of daily weather parameters produced on a 1 km x 1 km grid for North America (including Canada, the United States, and Mexico), Hawaii, and Puerto Rico. Separate annual files are provided for the land areas of continental North America, Hawaii, and Puerto Rico. Data are distributed in standardized Climate and Forecast (CF)-compliant netCDF (.nc) and Cloud Optimized GeoTIFF (.tif) file formats. In Version 4 R1, all 2020 and 2021 files (60 total) were updated to improve predictions especially in high-latitude areas. It was found that input files used for deriving 2020 and 2021 data had, for a significant portion of Canadian weather stations, missing daily variable readings for the month of January. NCEI has corrected issues with the Environment Canada ingest feed which led to the missing readings. The revised 2020 and 2021 Daymet V4 R1 files were derived with new GHCNd inputs. Files outside of 2020 and 2021 have not changed from the previous V4 release.
&lt;br&gt;&lt;h4 id&#x3D;&quot;daymet_daily_v4r1_2129&quot;&gt;Daymet_Daily_V4R1_2129&lt;/h4&gt;
This dataset provides Daymet Version 4 R1 data as gridded estimates of daily weather parameters for North America, Hawaii, and Puerto Rico. Daymet variables include the following parameters: minimum temperature, maximum temperature, precipitation, shortwave radiation, vapor pressure, snow water equivalent, and day length. The dataset covers the period from January 1, 1980, to December 31 (or December 30 in leap years) of the most recent full calendar year for the Continental North America and Hawaii spatial regions. Data for Puerto Rico is available starting in 1950. Each subsequent year is processed individually at the close of a calendar year. Daymet variables are provided as individual files, by variable and year, at a 1 km x 1 km spatial resolution and a daily temporal resolution. Areas of Hawaii and Puerto Rico are available as files separate from the continental North America. Data are in a North America Lambert Conformal Conic projection and are distributed in a standardized Climate and Forecast (CF)-compliant netCDF file format. In Version 4 R1, all 2020 and 2021 files were updated to improve predictions especially in high-latitude areas. It was found that input files used for deriving 2020 and 2021 data had, for a significant portion of Canadian weather stations, missing daily variable readings for the month of January. NCEI has corrected issues with the Environment Canada ingest feed which led to the missing readings. The revised 2020 and 2021 Daymet V4 R1 files were derived with new GHCNd inputs. Files outside of 2020 and 2021 have not changed from the previous V4 release.
&lt;br&gt;&lt;h4 id&#x3D;&quot;daymet_monthly_v4r1_2131&quot;&gt;Daymet_Monthly_V4R1_2131&lt;/h4&gt;
This dataset provides Daymet Version 4 R1 monthly climate summaries derived from Daymet Version 4 R1 daily data at a 1 km x 1 km spatial resolution for five Daymet variables: minimum and maximum temperature, precipitation, vapor pressure, and snow water equivalent. Monthly averages are provided for minimum and maximum temperature, vapor pressure, and snow water equivalent, and monthly totals are provided for the precipitation variable. Each data file is yearly by variable with 12 monthly time steps and covers the same period of record as the Daymet V4 R1 daily data. The monthly climatology files are derived from the larger datasets of daily weather parameters produced on a 1 km x 1 km grid for North America, Hawaii, and Puerto Rico. Separate monthly files are provided for the land areas of continental North America (Canada, the United States, and Mexico), Hawaii, and Puerto Rico. Data are distributed in standardized Climate and Forecast (CF)-compliant netCDF (.nc) and Cloud-Optimized GeoTIFF (.tif) formats. In Version 4 R1 (ver 4.1), all 2020 and 2021 files (60 total) were updated to improve predictions especially in high-latitude areas. It was found that input files used for deriving 2020 and 2021 data had, for a significant portion of Canadian weather stations, missing daily variable readings for the month of January. NCEI has corrected issues with the Environment Canada ingest feed which led to the missing readings. The revised 2020 and 2021 Daymet V4 R1 files were derived with new GHCNd inputs. Files outside of 2020 and 2021 have not changed from the previous V4 release.
&lt;br&gt;&lt;h4 id&#x3D;&quot;daymet_xval_v4r1_2132&quot;&gt;Daymet_xval_V4R1_2132&lt;/h4&gt;
This dataset reports the station-level daily weather observation data and the corresponding cross-validation results for three Daymet model parameters: minimum temperature (tmin), maximum temperature (tmax), and daily total precipitation (prcp) across continental North America (including Canada, the United States, and Mexico), Hawaii, and Puerto Rico. Each data file contains the daily observations and cross-validation results for one parameter for each modeled region and each year, that is, from 1980 to the current calendar year for stations across continental North America and Hawaii and from 1950 to the current year for Puerto Rico. Also included are corresponding station metadata files listing every surface weather station used in Daymet processing for each parameter, region, and year and containing the station name, station identification, latitude, and longitude. The data are provided in netCDF and text formats. In Version 4 R1, all 2020 and 2021 files were updated to improve predictions especially in high-latitude areas. It was found that input files used for deriving 2020 and 2021 data had, for a significant portion of Canadian weather stations, missing daily variable readings for the month of January. NCEI has corrected issues with the Environment Canada ingest feed which led to the missing readings. The revised 2020 and 2021 Daymet V4 R1 files were derived with new GHCNd inputs. Files outside of 2020 and 2021 have not changed from the previous V4 release.
&lt;br&gt;&lt;h4 id&#x3D;&quot;daymet_subdaily_puerto_rico_1977&quot;&gt;Daymet_SubDaily_Puerto_Rico_1977&lt;/h4&gt;
To support high spatial- and temporal-resolution land surface modeling, this dataset provides 3-hourly time step historic weather forcing at 1-km spatial resolution for Puerto Rico and surrounding islands. The latest Daymet V4 data provides gridded historic daily weather observation at 1-km spatial resolution from 1950 to present. Using sub-daily temporal information from two meteorological reanalysis datasets (GSWP3 and NARR), Daymet was further temporally downscaled to 3-hourly time steps and provided in the format required for land surface model simulations. The process of temporal downscaling preserves the relative magnitude in each sub-daily time step from GSWP3 and NARR while maintaining the total and average values from Daymet at each day. These result in two blended datasets: 1950-2014 Daymet-GSWP3 and 1979-2019 Daymet-NARR. Available variables include surface air temperature, precipitation, specific humidity, shortwave and longwave radiation, wind speed, and pressure. These data can be used as a high-resolution meteorological forcing dataset to support high-resolution land surface modeling where accurate meteorological forcing datasets built from historic observations and/or reanalysis datasets are desirable.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.ornldaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA Delta-X Project</title>
      <link>https://registry.opendata.aws/nasa-delta-x</link>
      <guid>https://registry.opendata.aws/nasa-delta-x</guid>
      <description>This dataset contains estimates of forest aboveground biomass (AGB) across the Atchafalaya and Terrebonne Basins, Louisiana, US. AGB was derived from AVIRIS-NG surface reflectance and UAVSAR products. L2B BRDF-adjusted surface reflectance was produced after applying atmospheric correction to L2 Hemispherical-Directional surface reflectance from NASA&amp;#39;s AVIRIS-NG instrument. A polarimetric decomposition of the UAVSAR Level 1 (L1) Single Look Complex (SLC) stack product was used. To estimate AGB, local pixel reflectance spectra and radar scattering component pixels coincident with in situ forest AGB plot data from Summer 2015 and Fall 2021 were used to generate a machine learning-based regression model. This model was then scaled to the AVIRIS-NG and UAVSAR mosaic data, in accordance with vegetation type, to map forest AGB across the Atchafalaya and Terrebonne Basins. The data are provided in cloud optimized GeoTIFF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_l3_aviris-ng_veg_types_2352&quot;&gt;DeltaX_L3_AVIRIS-NG_Veg_Types_2352&lt;/h4&gt;
This dataset provides maps of vegetation types for the Atchafalaya and Terrebonne basins in coastal Louisiana, U.S., derived from NASA&amp;#39;s Next Generation Airborne Visible Infrared Imaging Spectrometer (AVIRIS-NG) imagery acquired during spring and fall of 2021 for the Delta-X campaign. Vegetation types were classified from Level-2B BRDF-adjusted surface reflectance. Local pixel reflectance spectra coincident with herbaceous vegetation field samples and vegetation plot data from Louisiana&amp;#39;s Coastwide Reference Monitoring System were used to generate a machine learning-based model to classify vegetation types. This model was then applied to the AVIRIS-NG mosaic imagery to map vegetation types across the Atchafalaya and Terrebonne Basins. The data are provided in cloud optimized GeoTIFF (COG) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_agb_agn_v2_2237&quot;&gt;DeltaX_AGB_AGN_V2_2237&lt;/h4&gt;
This dataset contains total aboveground biomass (AGB) and necromass (AGN), and total carbon, total nitrogen, and total phosphorus content of aboveground biomass (AGB) and necromass (AGN) samples collected from herbaceous wetlands in the Atchafalaya and Terrebonne basins in southeastern coastal Louisiana during 2021. Field measurements were conducted at three sites in the Atchafalaya basin and three sites in the Terrebonne basin. Five of the sites are adjacent to sites from the Coastwide Reference Monitoring System (CRMS). The other site is located in Wax Lake Delta (WLD) without appropriate adjacent CRMS sites. All AGB and AGN plant material within each plot was clipped at soil level, stored in plastic bags, and transported to the laboratory for further analyses. Herbaceous wetland sites in both basins were chosen to represent a salinity gradient including freshwater, brackish, and saline ecosystems. These data cover the period 2021-03-19 to 2021-03-31 (spring) and 2021-08-19 to 2021-08-27 (fall).
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_vegetation_structure_v2_2240&quot;&gt;DeltaX_Vegetation_Structure_V2_2240&lt;/h4&gt;
This dataset provides mean stem diameter, mean height, dominant species, hydrogeomorphic zone (HGM), and stem density for vegetation in herbaceous wetlands collected in the Atchafalaya and Terrebonne basins in southeastern coastal Louisiana. The data were collected between 2021-03-21 to 2021-03-31 during the Delta-X Spring 2021 deployment, and from 2021-08-19 to 2021-08-27 during the Fall deployment. Field measurements were conducted at six sites in the Atchafalaya (N &#x3D; 3) and Terrebonne (N &#x3D; 3) basins. Five of the sites were adjacent to sites from the Coastwide Reference Monitoring System (CRMS), and the other site was in the Wax Lake Delta (WLD) without appropriate adjacent CRMS sites. Sites in both basins were chosen to represent a salinity gradient including freshwater, brackish, and saline ecosystems. At each herbaceous wetland site, duplicate sampling stations (30 m apart) were established parallel to the wetland edge at 25 and 50 m within the intertidal zone to capture within site variability in vegetation dynamics and soil properties. The data are provided in comma-separated values (.csv) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_adcp_measurements_v2_2081&quot;&gt;DeltaX_ADCP_Measurements_V2_2081&lt;/h4&gt;
This dataset provides river discharge measurements collected at selected locations in the Atchafalaya and Terrebonne Basins within the Mississippi River Delta (MRD) floodplain in coastal Louisiana, USA. The measurements were made during the Delta-X 2021 field efforts from 2021-03-25 to 2021-04-11 (spring) and 2021-08-16 to 2021-09-25 (fall). Channel surveys were conducted with a Teledyne RiverPro acoustic doppler current profiler (ADCP) or a Sontek M9 RiverSurveyor ADCP on selected wide channels (&amp;gt;100 m wide) and a few selected narrow channels (approximately 10 m wide) near the Delta-X intensive study sites. River discharge was measured on cross-channel transects. Reported data include bathymetry, discharge (m3 s-1), and flow velocity.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_l2_airswot_waterelev_v3_2350&quot;&gt;DeltaX_L2_AirSWOT_WaterElev_V3_2350&lt;/h4&gt;
This dataset contains Level 2 (L2) AirSWOT geocoded products, including estimated water surface elevation. The AirSWOT instrument is a Ka-band interferometer and for this study is flown on the King Air B200 platform. Data were collected during the DeltaX airborne campaign over the Atchafalaya and Terrebonne basins of the Mississippi River Delta, Louisiana, USA. Flights occurred during the Delta-X Spring 2021 deployment from 2021-03-26 to 2021-04-18 and the Delta-X Fall 2021 deployment from 2021-08-21 to 2021-09-12. AirSWOT is capable of producing high resolution (3.6 m) digital elevation models over land and water bodies using near-nadir wide-swath Ka-band radar interferometry to measure water-surface elevation and produce continuous gridded elevation data. The instrument includes six antennas that form multiple baseline pairs for along-track and across-track interferometry. AirSWOT elevation data are useful for calibrating elevation and slopes along the main channels, as well as tying observations to open ocean tidal conditions and is an airborne calibration and validation instrument for the Surface Water and Ocean Topography (SWOT) satellite. This Version 3 dataset provides updated data files due to an updated Calumet survey that changed the water level by 0.138 m. This resulted in all the AirSWOT water levels changing by that same amount. For these L2 products, only the estimated water surface elevation in respect to the WGS84 ellipsoid surface, and estimated height above the NAVD88 (GEOID12B) vertical datum files changed. Note that data acquired on September 1 and September 5, 2021 do not meet the expected MAE in-situ comparison and should be used with caution. This dataset contains cloud optimized GeoTIFF rasters in UTM map coordinates for each flight line. In addition, a text file provides basic metadata, including flight line ID, start and end UTC times of data acquisition, processor version number, and the date and time of different processing stages.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_l3_airswot_waterelev_v2_2349&quot;&gt;DeltaX_L3_AirSWOT_WaterElev_V2_2349&lt;/h4&gt;
This dataset contains water surface elevations at selected point locations generated from the AirSWOT data collected during the Spring and Fall 2021 Delta-X deployments over the Atchafalaya and Terrebonne basins in Louisiana, USA. AirSWOT uses near-nadir wide-swath Ka-band radar interferometry to measure water-surface elevation and produce continuous gridded elevation data. The Level 3 (L3) data were created by masking land areas out of the AirSWOT Level 2 products, then filtering and averaging to the AirSWOT heights to produce water surface elevations at selected points throughout the scene. The AirSWOT elevation data are useful for calibrating elevation and slopes along the main channels, as well as tying observations to open ocean tidal conditions. AirSWOT performance in the floodplain was limited by the presence of vegetation and the very small slope characteristic of two dimensional floodplain discharge. Therefore, the bulk of the AirSWOT data collections were targeted at the larger channels, since the channel discharge provides the necessary boundary conditions for potential overflow to islands and floodplains. The data are provided in comma-separated values (CSV) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_l1b_airswot_1996&quot;&gt;DeltaX_L1b_AirSWOT_1996&lt;/h4&gt;
This dataset contains AirSWOT interferogram products collected during the 2021 Delta-X Campaign over the Atchafalaya and Terrebonne Basins of the Mississippi River Delta, Louisiana, USA from 2021-03-26 to 2021-04-18 (Spring) and 2021-08-21 to 2021-09-12 (Fall). AirSWOT uses near-nadir wide-swath Ka-band radar interferometry to measure water-surface elevation and produce continuous gridded elevation data. AirSWOT elevation data is useful for calibrating elevation and slopes along the main channels, as well as tying observations to open ocean tidal conditions. The AirSWOT Level 1B (L1B) data products represent interferogram data in the radar coordinate system, not in georeferenced map coordinates. This is an earlier stage of data processing which is used to generate the later Level 2 and Level 3 data products which will contain georeferenced water heights and water height profiles for river channels in each basin. The data are provided in binary and text file formats.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_anuga_hydrodynamics_mrd_2310&quot;&gt;DeltaX_ANUGA_Hydrodynamics_MRD_2310&lt;/h4&gt;
This dataset comprises the primary inputs and outputs from the ANUGA hydrodynamic model for spring 2021 (2021-03-20 to 2021-04-04). These dates align with the 2021 Delta-X Spring Campaign. Data cover the Atchafalaya and Terrebonne basins of the Mississippi River Delta in southern Louisiana, USA. ANUGA is a 2D depth-integrated hydrodynamic model which uses the Finite Volume Method (FVM) to numerically solve the shallow water momentum and continuity equations for fluid flow in broad-scale geophysical systems. The inputs consist of a modified digital elevation (DEM) model, a spatial classification of the friction coefficient modified, and the model&amp;#39;s unstructured grid with boundary condition locations. The model&amp;#39;s outputs include two weeks of predictions of water levels and mean horizontal velocities at each mesh node at a 30-minute time step. Outputs are provided in NetCDF format, and inputs are provided in GeoTIFF and comma separated values (CSV) format. Also included are MP4 videos (.mp4) that provide visual summaries of the outputs.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_l2a_aviris-ng_brdf_v3_2355&quot;&gt;DeltaX_L2A_AVIRIS-NG_BRDF_V3_2355&lt;/h4&gt;
This data provides AVIRIS-NG Bidirectional Reflectance Distribution Function (BRDF) and sunglint-corrected surface spectral reflectance images over the Atchafalaya and Terrebonne basins of the Mississippi River Delta (MRD) of coastal Louisiana, USA. Flights were acquired during the Spring and Fall 2021 deployments of the Delta-X campaign. The imagery was acquired by the Airborne Visible/Infrared Imaging Spectrometer - Next Generation (AVIRIS-NG) from 2021-03-27 to 2021-04-06 and 2021-08-18 to 2021-09-25. Reflectance data are provided for each flight line. In addition, ten files of mosaicked flight lines, by time period and over four locations (labeled Terre, Atcha, TerreEast, and Bara), are included. Data are provided as binary ENVI image and header files. Only land pixels were corrected; mask files for the mosaic file coverage showing presence/absence of water and clouds are also included. For the Delta-X mission, these data serve to better understand rates of soil erosion, accretion, and creation in the delta system, with the goal of building better models of how river deltas will behave under relative sea level rise.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_l1_aviris_radiance_1987&quot;&gt;DeltaX_L1_AVIRIS_Radiance_1987&lt;/h4&gt;
This dataset provides Level 1B (L1B) radiance products from NASA&amp;#39;s Airborne Visible Infrared Imaging Spectrometer- Next Generation (AVIRIS-NG) instrument acquired over the Atchafalaya and Terrebonne basins of the Mississippi River Delta, Louisiana, USA during two deployments; spring and fall of 2021. All flights were flown on a Dynamic Aviation King Air B200. There are a combined 200 total flight lines for the spring and fall 2021 deployments; spring 2021 had 75 flight lines, fall 2021 had 175 flight lines. AVIRIS-NG measures reflected radiance at 5-nanometer (nm) intervals in the visible to shortwave infrared spectral range between 380 and 2510 nm. Level 1B data are orthorectified calibrated radiance values in units of spectral radiance in which raw digital numbers (DNs) are translated to units of radiant intensity measured at the sensor. Measurements are radiometrically and geometrically calibrated and provided at approximately 5-meter spatial resolution, dependent on aircraft altitude. Additional flight line files include band information of observational geometry and illumination parameters, as well as geographic pixel locations and elevation. These L1B data are provided in ENVI file format. AVIRIS-NG Cal/Val, Level 2 and Level 3 products for the Pre-Delta-X and Delta-X missions are provided in related datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_l2_aviris_reflectance_1988&quot;&gt;DeltaX_L2_AVIRIS_Reflectance_1988&lt;/h4&gt;
This dataset provides Level 2 (L2) atmospherically corrected surface reflectance data acquired from NASA&amp;#39;s Airborne Visible-Infrared Imaging Spectrometer-Next Generation (AVIRIS-NG) over regions of interest in the Atchafalaya and Terrebonne basins on the southern coast of Louisiana, United States. Data were collected as part of the Delta-X Spring and Fall 2021 deployments that occurred from 2021-03-27 to 2021-04-06 and from 2021-08-18 to 2021-08-25. Additionally, L2 data from flights flown specifically to capture the Significant Event of Hurricane Ida are provided. This includes 56 files from flights conducted following Hurricane Ida from 2021-09-23 to 2021-09-25. Hurricane Ida made landfall over this region on 2021-08-29. AVIRIS-NG is a pushbroom spectral mapping system with a high signal-to-noise ratio (SNR) designed for high performance imaging spectroscopy. AVIRIS-NG measures the wavelength range from 380 nm to 2510 nm with 5-nm sampling resolution. For this dataset, spatial resolution varies from 3.8-5.4 meters. For this campaign, the AVIRIS-NG instrument was deployed on the Dynamic Aviation King Air B200 platform. This dataset represents one part of a multisensor airborne sampling campaign conducted by different aircraft teams for the Delta-X Campaign. Data are provided in ENVI file format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_l2b_aviris-ng_fraccover_2407&quot;&gt;DeltaX_L2B_AVIRIS-NG_FracCover_2407&lt;/h4&gt;
This dataset provides estimates of fractional vegetation cover across the Atchafalaya and Terrebonne basins. Atmospheric correction was applied to a L2B BRDF-adjusted surface reflectance product from AVIRIS-NG imagery to produce L2 Hemispherical-Directional surface reflectance. A spectral library was compiled using in situ spectra in the USGS Spectral Library (v7) to represent green vegetation, non-photosynthetic vegetation, and soil. Linear spectral unmixing was then applied to mosaics of AVIRIS-NG reflectance using these spectra to estimate the fractional composition (scaled 0-1) of each endmember type for all terrestrial pixels. In addition to the AVIRIS-NG imagery and in situ field spectra, this analysis incorporated field images collected using a GoPro digital camera coincident with the AVIRIS-NG flight lines.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_l3_aviris-ng_agb_v3_2409&quot;&gt;DeltaX_L3_AVIRIS-NG_AGB_V3_2409&lt;/h4&gt;
This dataset includes high-resolution (~5 m) gridded estimates of aboveground biomass (AGB), aboveground necromass (AGN), and aboveground net primary productivity (ANPP) for herbaceous vegetation in the Atchafalaya and Terrebonne basins of the Mississippi River Delta in coastal Louisiana, USA, for the fall and spring seasons of 2021. AGB, AGN and ANPP were estimated from Bidirectional Reflectance Distribution Function (BRDF)-adjusted surface reflectance products from NASA&amp;#39;s Airborne Visible Infrared Imaging Spectrometer - Next Generation (AVIRIS-NG) acquired over the study area in April and August 2021. The BRDF-adjusted reflectance was derived from hemispherical-directional surface reflectance with atmospheric correction. Local pixel reflectance spectra coincident with herbaceous vegetation AGB field samples from both Spring and Fall 2021 collections were used to generate a machine learning-based regression model to estimate AGB. This model was then scaled to the AVIRIS-NG mosaic imagery in accordance with vegetation type to map herbaceous AGB across the Atchafalaya and Terrebonne Basins. The AGN field data, separated from the AGB samples, were also used in conjunction with AVIRIS-NG-derived fractional coverage to derive AGN maps again employing machine learning. The AGB and AGN products were used together to map ANPP across the Atchafalaya and Terrebonne Basins. The data are provided in cloud optimized GeoTIFF (COG) format. This Version 3 dataset replaces the files provided in Version 2.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_aviris-ng_l3_bgb_2456&quot;&gt;DeltaX_AVIRIS-NG_L3_BGB_2456&lt;/h4&gt;
This dataset contains high-resolution (~5 m) gridded estimates of belowground biomass (BGB) in the Atchafalaya and Terrebonne basins of southern Louisiana, U.S., in August 2021. The Level 3 (L3) AVIRIS-NG-derived herbaceous aboveground biomass (AGB) and necromass (AGN) Version 3 products were used to predict the BGB. The AGB estimates were derived from the L2B BRDF-adjusted surface reflectance product, following atmospheric correction to produce L2 Hemispherical-Directional surface reflectance. An Ordinary Least Squares Regression (OLSR) model was derived, trained on field sample measurements (n&#x3D;40) of aboveground biomass (AGB), aboveground necromass (AGN), and the natural logarithm-transformed total nitrogen (N). This dataset constitutes all available field samples where AGB, AGN, total N, and BGB were measured concurrently. Belowground biomass is an essential component of organic accretion but cannot be directly measured by airborne instruments. This model infers BGB from its relationships with aboveground plant mass and foliar N concentrations. This model was applied to landscape-scale maps derived from AVIRIS-NG data to estimate BGB for the August 2021 peak biomass collection period. The data are provided in cloud optimized GeoTIFF (COG) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_l3_aviris-ng_water_v3_2152&quot;&gt;DeltaX_L3_AVIRIS-NG_Water_V3_2152&lt;/h4&gt;
This dataset includes estimates of total suspended solids (TSS) concentration and turbidity for waters of the Atchafalaya River and Terrebonne Basins of the Mississippi River Delta (MRD) in coastal Louisiana. Estimates were derived from Level 2 (L2) BRDF-corrected imagery from NASA&amp;#39;s Next Generation Airborne Visible Infrared Imaging Spectrometer (AVIRIS-NG). AVIRIS-NG imagery was collected from March 27-April 6 (spring) and August 20-25 (fall), 2021, as part of the 2021 Delta-X campaign. Algorithms for TSS and turbidity estimation were developed using in-situ remote-sensing reflectance measured at field sampling stations paired with in-situ measures of turbidity from a water quality probe and TSS from water samples. Using the in-situ data, a partial least squares regression (PLSR) model was developed for each AVIRIS-NG wavelength. A subset of the in-situ data, collected during relatively clear AVIRIS-NG overflights, was held out to validate the PLSR model. The PLSR algorithm was then applied to AVIRIS-NG imagery to retrieve TSS and turbidity across the study area. The measurement units for TSS and turbidity estimates are mg L-1 and Formazin Nephelometric Units (FNU), respectively, and the spatial resolution is 3.8 to 5.4 m as determined by the AVIRIS-NG imagery. The dataset includes binary cloud and water masks. These data quantify the mesoscale (i.e., on the order of 1 ha) patterns of soil accretion that control land loss and gain and predict the resilience of deltaic floodplains under projected relative sea-level rise. Gridded estimates are provided in netCDF format, and regression coefficients are included in a comma-separated values (CSV) file. This is Version 3 of this dataset. All previously released data were updated to the latest available versions.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_sediment_grain_size_v3_2379&quot;&gt;DeltaX_Sediment_Grain_Size_V3_2379&lt;/h4&gt;
This dataset includes sediment concentration and grain size distribution measurements from suspended and bed sediment samples collected in the Atchafalaya River and Terrebonne Basins as part of the Delta-X Spring campaign between March 25 and April 2, 2021, and the Delta-X Fall campaign between August 17 and 22, 2021. In addition, ten samples were collected during a field campaign in October 2019. Samples were collected in the main channels and the interior of Mike Island in the Wax Lake Delta, Louisiana and at site CRMS0421 inside the Terrebonne Basin. Sediment samples were collected from a boat using a Van Dorn sampler (for suspended sediment samples) or a Ponar bed sampler (for bed samples). Suspended sediment samples were collected from a boat drifting at approximately the same velocity as the water flow. One sample was collected per drift. Bed samples were collected in a similar fashion. Data include measurements of sediment grain size distribution, total sediment concentration, water temperature, flow velocity, salinity, and depth. This Version 3 updates Version 2 to include data from more samples and reprocessed laser diffraction grain size distributions with optimized sediment optical properties. The data is provided in comma separated values (CSV) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_bgb_bgn_v2_2238&quot;&gt;DeltaX_BGB_BGN_V2_2238&lt;/h4&gt;
This dataset contains total belowground biomass (BGB) and necromass (BGN), and total carbon, total nitrogen, and total phosphorus content of samples collected from herbaceous wetlands in the Atchafalaya and Terrebonne basins of the Mississippi River Delta in southeastern coastal Louisiana, U.S., during March and August 2021. The data were collected during the Delta-X Spring and Fall deployments. Field measurements were conducted at three sites in the Atchafalaya basin and three sites in the Terrebonne basin. Five of the sites are adjacent to sites from the Coastwide Reference Monitoring System (CRMS). The other site is located in Wax Lake Delta (WLD) without appropriate adjacent CRMS sites. Herbaceous wetland sites in both basins were chosen to represent a salinity gradient including freshwater, brackish, and saline ecosystems. Root biomass samples were collected using a gouge soil auger.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_anuga_atchafalayabasin_2306&quot;&gt;DeltaX_ANUGA_AtchafalayaBasin_2306&lt;/h4&gt;
This dataset provides ANUGA hydrodynamic modeling results and input run-scripts for the Atchafalaya basin in the Mississippi River Delta in southern Louisiana, USA, during three windows of time corresponding to the Delta-X and Pre-Delta-X field campaigns in fall 2016, spring 2021, and fall 2021. ANUGA is a 2D depth-integrated hydrodynamic model which uses the Finite Volume Method (FVM) to numerically solve the shallow water momentum and continuity equations for fluid flow in broad-scale geophysical systems. Each iteration of the model was extensively calibrated using a database of in-situ and remotely-sensed observations, including about 54 water level gauges, numerous water surface profiles collected by AirSWOT or lidar, and water level change measurements derived from UAVSAR. The model was forced using observational data collected from NOAA and USGS, and the model mesh was specifically designed to capture channel-island connectivity using high-resolution Planet Labs imagery spanning over a decade. In total, over a month of simulation outputs are included in this dataset, covering different seasons and hydrological conditions in the Atchafalaya and Wax Lake Delta systems. These model outputs can be leveraged with other Delta-X datasets to provide contextual information about water levels or flow velocities at different times or locations within the Atchafalaya basin, and the model codes provided can be used to simulate additional time periods for further analysis in this region. Model outputs are presented in NetCDF (.nc) format and run-scripts are in Python (.py) or contained in compressed (.zip) file format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_delft3d_atchafalaya_mrd_2302&quot;&gt;DeltaX_Delft3D_Atchafalaya_MRD_2302&lt;/h4&gt;
This dataset contains the Delft3D model of the Atchafalaya Basin along the Mississippi River Delta (MRD) in coastal Louisiana. Simulations cover the Delta-X Spring and Fall campaigns in 2021 and include hydrodynamics, waves, and sediment transport. Bottom friction was calibrated using AirSWOT water elevation data, while sediment parameters were calibrated using AVIRIS-NG Total Suspended Solids (TSS) data. All files required to run the simulations are included. Model output of water levels, velocity, and depth-averaged sediment concentration are provided for both campaigns as netCDF files. The dataset includes a netCDF file containing the annual inorganic mass accumulation rates derived from simulations.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_delft3d_terrebonne_mrd_2301&quot;&gt;DeltaX_Delft3D_Terrebonne_MRD_2301&lt;/h4&gt;
This dataset contains the Delft3D model of the Terrebonne Basin along the Mississippi River Delta (MRD) in coastal Louisiana. Simulations cover the Delta-X Spring and Fall campaigns in 2021 and include hydrodynamics, waves, and sediment transport. Bottom friction was calibrated using AirSWOT water elevation data, while sediment parameters were calibrated using AVIRIS-NG Total Suspended Solids (TSS) data. All files required to run the simulations are included. The model&amp;#39;s output of water levels, velocity, and depth-averaged sediment concentrations are provided for both campaigns as netCDF files. The dataset includes a netCDF file containing the annual inorganic mass accumulation rates derived through a storms analysis and modelling.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_delft3d_fm_hydromodel_2464&quot;&gt;DeltaX_Delft3D_FM_HydroModel_2464&lt;/h4&gt;
This dataset contains Delft3D Flexible Mesh (FM) hydrodynamic model setup and results for the Atchafalaya and Terrebonne basins in coastal Louisiana, U.S.. The model domain spans from Bayou Lafourche in eastern Terrebonne Bay, encompasses Atchafalaya Bay, and extends westward to Vermilion Bay. Separate simulations were conducted for spring and fall, each covering a 31-day period. Both simulations were calibrated and validated using Delta-X airborne remote sensing data and in situ measurements. The dataset includes the full set of hydrodynamic model input files for each seasonal simulation, along with a netCDF output file for each model run. Using the provided input files, users can reproduce the simulations and obtain results identical to those in the output netCDF files included in this dataset.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_delft3d_fm_hydroperiod_2421&quot;&gt;DeltaX_Delft3D_FM_Hydroperiod_2421&lt;/h4&gt;
This dataset provides the weighted average hydroperiod derived from two Delft3D FM model simulations representing the low discharge (fall 2021) and high discharge (spring 2021) seasons. Each model was run for 31 days, excluding a 1-day warm-up period from the analysis. The weights for each model were derived from the long-term probability density function (PDF) of the Atchafalaya River discharge. Hydroperiod, which quantifies the frequency of inundation at each model grid cell, is computed by analyzing the water level time series and identifying periods when the water depth does not exceed the model-defined wet/dry threshold of 5 cm.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_delft3d_fm_salinity_2420&quot;&gt;DeltaX_Delft3D_FM_Salinity_2420&lt;/h4&gt;
This dataset provides the weighted averaged salinity derived from two Delft3D Flexible Mesh (FM) model simulations representing the low discharge (fall 2021) and high discharge (spring 2021) seasons. The weights for each model were determined using the probability density function of the Atchafalaya River discharge. Each model was run for 31 days, excluding a 1-day warm-up period from the analysis. Salinity is calculated by applying a weighted average to the salinity values at each grid cell in the final time step of each simulation. The data are provided in netCDF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_delft3d_294_terrebonne_2303&quot;&gt;DeltaX_Delft3D_294_Terrebonne_2303&lt;/h4&gt;
This dataset contains the Delft3D model of the intensive site 294 in the Terrebonne Basin along the Mississippi River Delta (MRD) in coastal Louisiana. Simulations cover the Delta-X Spring and Fall deployments in 2021 and include hydrodynamics and sediment transport. All files required to run the simulations are included. The model&amp;#39;s output of water velocity and depth-averaged sediment concentrations are provided for both deployments. The dataset includes annual inorganic mass accumulation rates derived through modelling intra-annual variability in water levels and suspended sediment concentrations. The data are provided in netCDF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_delft3d_322_terrebonne_2312&quot;&gt;DeltaX_Delft3D_322_Terrebonne_2312&lt;/h4&gt;
This dataset contains the Delft3D model of the intensive site 322 in the Terrebonne Basin along the Mississippi River Delta (MRD) in coastal Louisiana. Simulations cover the Delta-X Spring and Fall deployments in 2021 and include hydrodynamics and sediment transport. All files required to run the simulations are included. The model&amp;#39;s output of water velocity and depth-averaged sediment concentrations are provided for both deployments. The dataset includes annual inorganic mass accumulation rates derived through modelling intra-annual variability in water levels and suspended sediment concentrations. The data are provided in netCDF and ENVI formats.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_delft3d_396_terrebonne_2314&quot;&gt;DeltaX_Delft3D_396_Terrebonne_2314&lt;/h4&gt;
This dataset contains the Delft3D model of the intensive site 396 in the Terrebonne Basin along the Mississippi River Delta (MRD) in coastal Louisiana. Simulations cover the Delta-X Spring and Fall deployments in 2021 and include hydrodynamics and sediment transport. All files required to run the simulations are included. The model&amp;#39;s output of water velocity and depth-averaged sediment concentrations are provided for both deployments. The dataset includes annual inorganic mass accumulation rates derived through modelling intra-annual variability in water levels and suspended sediment concentrations. The data are provided in netCDF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_delft3d_399_terrebonne_2313&quot;&gt;DeltaX_Delft3D_399_Terrebonne_2313&lt;/h4&gt;
This dataset contains the Delft3D model of the intensive site 399 in the Terrebonne Basin along the Mississippi River Delta (MRD) in coastal Louisiana. Simulations cover the Delta-X Spring and Fall deployments in 2021 and include hydrodynamics and sediment transport. All files required to run the simulations are included. The model&amp;#39;s output of water velocity and depth-averaged sediment concentrations are provided for both deployments. The dataset includes annual inorganic mass accumulation rates derived through modelling intra-annual variability in water levels and suspended sediment concentrations. The data are provided in netCDF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_delft3d_421_terrebonne_2304&quot;&gt;DeltaX_Delft3D_421_Terrebonne_2304&lt;/h4&gt;
This dataset contains the Delft3D model of the intensive site 421 in the Terrebonne Basin along the Mississippi River Delta (MRD) in coastal Louisiana. Simulations cover the Delta-X Spring and Fall deployments in 2021 and include hydrodynamics and sediment transport. All files required to run the simulations are included. The model&amp;#39;s output of water velocity and depth-averaged sediment concentrations are provided for both deployments. The dataset includes annual inorganic mass accumulation rates derived through modelling intra-annual variability in water levels and suspended sediment concentrations. The data are provided in netCDF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_dem_mrd_la_2181&quot;&gt;DeltaX_DEM_MRD_LA_2181&lt;/h4&gt;
This dataset provides an updated digital elevation model (DEM) for the Atchafalaya and Terrebonne basins in coastal Louisiana, USA. The DEM is updated from the Pre-Delta-X DEM and extended to the full Delta-X study area. This DEM was developed from multiple data sources, including sonar data collected during Pre-Delta-X and Delta-X campaigns, bathymetric data from the Coastal Protection and Restoration Authority System-Wide Assessment and Monitoring System (CPRA SWAMP), and NOAA, and topography from the National Elevation Dataset and LiDAR from US Geological Survey (USGS). The provided data layers include the DEM, a binary water/land mask, data source flags, and eight layers with analysis weighting factors for each pixel. Elevation values are provided in meters with respect to the North American Vertical Datum of 1988 (NAVD88). The weighting factors indicate how each data source contributed to this multisource DEM. The data are provided in cloud-optimized GeoTIFF (CoG) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_ecogeomorphic_products_2108&quot;&gt;DeltaX_Ecogeomorphic_Products_2108&lt;/h4&gt;
This product delineates the Mississippi River Delta (MRD) landscape into distinct ecogeomorphic cells, which are small contiguous areas of land with similar ecological and geomorphological characteristics. The study area is the Atchafalaya and Terrebonne basins of the MRD in southern Louisiana, U.S., which was the focus of NASA&amp;#39;s 2021 Delta-X campaign. Each ecogeomorphic cell is a small homogeneous area of similar vegetation and elevation (or bathymetry). A &amp;quot;cell&amp;quot; typically consists of a cluster of contiguous pixels in a raster image, although cells of single pixels are present. The elevation was derived from the USGS Digital Elevation Model, and the vegetation was characterized by its spectral signature as measured by near infrared (NIR) reflectance and normalized difference vegetation index (NDVI). NIR and NDVI were computed from Sentinel-2 images acquired January through September 2021. The data are provided in shapefile and GeoTIFF formats. The vector shapefiles contain the distinct ecogeomorphic cells as polygons with unique labels (i.e., ID number). A raster image of these ecogeomorphic cells provided wherein the pixel values are the polygon labels from the shapefiles. The GeoTIFFs hold the mean and standard deviations of bathymetry, NIR, and NDVI spectral indices within each ecogeomorphic region (polygon). The raster data are provided with a spatial resolution of 0.000045 degrees (approximately 5 meters).
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_feldspar_sediment_v4_2381&quot;&gt;DeltaX_Feldspar_Sediment_V4_2381&lt;/h4&gt;
This dataset provides elevation, hydrogeomorphic zone classification, soil carbon content, bulk density, organic matter content, and sediment accretion measurements collected at feldspar stations established near Louisiana&amp;#39;s Coastwide Reference Monitoring Systems (CRMS) sites and on Mike Island in Wax Lake Delta (WLD). Feldspar stations were established to capture recent sediment deposition rates across hydrogeomorphic zones defined as discrete surface elevation ranges relative to NAVD88 (e.g., subtidal &amp;lt; -0.04 m, intertidal -0.04 m to 0.30 m, and supratidal &amp;gt; 0.30 m). Hydrogeomorphic zones classification was based on marsh surface elevation measurements acquired in November - December 2020 using a RTK GPS (Trible R12, using Geoid 18). Between two and four feldspar stations were deployed approximately 25 and 50 meters from a main channel to represent existing hydrogeomorphic zones in brackish and saline emergent marsh vegetation, brackish and saline ponds within emergent marshes, tidal freshwater emergent marshes, and forested swamps. Cryocore technique was used to determine recent sediment deposition. Soil samples were collected to determine organic and inorganic fractions and organic carbon content. The data cover the Delta-X field studies conducted from Fall 2020 through Fall 2023. The first feldspar markers were deployed in October of 2019. The data are provided in comma-separated values (CSV) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_foliar_stable_isotopes_2194&quot;&gt;DeltaX_Foliar_Stable_Isotopes_2194&lt;/h4&gt;
This dataset contains foliar tissue C and N bulk isotopic signatures (delta 13C, delta 15N) of dominant wetland herbaceous species collected at six sites in the Atchafalaya (N &#x3D; 3) and Terrebonne (N &#x3D; 3) basins in coastal Louisiana. Five of the sites are from the Coastwide Reference Monitoring System (CRMS) and one site is the Mike Island Site in the Wax Lake Delta (WLD). For the herbaceous wetland sites, Aboveground biomass (AGB) was harvested inside duplicate plots (0.25 m2), located 5 m apart at each sampling station. All plant material within each plot was clipped at soil level, stored in plastic bags, and transported to the laboratory for further analyses. In the lab, plant tissue (foliar) C and N bulk isotopic signatures were analyzed for two dominant plant species from each site using a Thermo Scientific Delta V Plus CF-IRMS coupled to a Carlo-Erba 1108 elemental analyzer via a ConFlo IV interface (Thermo Fisher Scientific, Waltham, MA, USA). The data were collected during 2021-08-19 to 2021-08-27 during the Delta-X Fall 2021 deployment.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_particle_size_lisst_v2_2077&quot;&gt;DeltaX_Particle_Size_LISST_V2_2077&lt;/h4&gt;
This dataset provides in situ measurements of beam attenuation coefficient at 670 nm, average suspended particle size, particle size distribution, and water temperature in surface waters (~0.5 m) of the Atchafalaya and Terrebonne Basins on the southern coast of Louisiana. The field studies were conducted in the Spring and Fall in support of the Delta-X mission and include measurements made in 2021 during March 25 - April 22 and August 14 - September 24. Measurements were made using the Sequoia Scientific Laser In-Situ Scattering and Transmissometer instrument (LISST-200X) in multiple channels of varying width (from a few meters to &amp;gt;100m), near Delta-X intensive study sites and in open bays and lakes and at a few locations in the nearshore Gulf of Mexico. The data are provided in comma-separated (CSV) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_insitu_wq_indicators_v2_2080&quot;&gt;DeltaX_Insitu_WQ_Indicators_V2_2080&lt;/h4&gt;
This dataset provides in situ measurements of water temperature (degrees C), salinity (PSU), turbidity (FNU), and chlorophyll-a fluorescence (RFU) in surface of the Atchafalaya River and Terrebonne Basins during the Spring (2021-03-25 to 2021-04-22) and Fall (2021-08-14 to 2021-09-24) field efforts by the Delta-X project. Field sampling was paused on August 25 and resumed on September 13, 2021, due to the landfall of Hurricane Ida on 2021-08-26 approximately 70 km east of the study site. Water quality changes caused by the hurricane were expected to be minimal. Measurements were collected in multiple channels of varying width (from a few meters to &amp;gt;100 m), near Delta-X intensive study sites, in open bays and lakes, and at a few locations in the nearshore Gulf of Mexico using either a YSI ProDSS water quality probe or a YSI EXO3 water quality probe.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_insitu_reflectance_v3_2153&quot;&gt;DeltaX_Insitu_Reflectance_V3_2153&lt;/h4&gt;
This dataset includes above water measurements of remote-sensing reflectance measured in situ at field sampling stations during the Delta-X 2021 field efforts. Measurements were collected in the Atchafalaya River and Terrebonne Basins on the southern coast of Louisiana from 2021-03-25 to 2021-04-22 (spring) and from 2021-08-14 to 2021-09-24 (fall). Field sampling was paused on 2021-08-25 and resumed on 2021-09-13 due to the landfall of Hurricane Ida on 2021-08-26 approximately 70 km east of the study site. Water quality changes caused by the hurricane were expected to be minimal. Reflectance was measured near-simultaneously with collection of field samples and in-water sediment parameters in multiple channels of varying width (from a few meters to &amp;gt;100 m), near Delta-X intensive study sites, in open bays and lakes, and at a few locations in the nearshore Gulf of Mexico. For each in situ collection, a handheld Portable SpectroRadiometer (PSR-1100f, Spectral Evolution) was used to measure radiance from: (a) a highly reflective (&amp;gt;99% reflectance) Lambertian Spectralon panel (b) from the sky, measured at 40 degrees from the solar zenith and at 135 degrees from the sun azimuthal plane, (c) from the water, measured at 40 degrees from nadir and at 135 degrees from the sun azimuthal plane. These measurements were used to calculate remote-sensing reflectance and the water-leaving radiance relative to downwelling irradiance, including a correction for the influence of reflected skylight. In Version 3, the data files with this dataset replace and update the data files in Version 2. A minor update was made to the code used to calculate the remote sensing reflectance (Rrs). These data are provided in comma-separated values (.csv) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_h2o_surface_elevation_2086&quot;&gt;DeltaX_H2O_Surface_Elevation_2086&lt;/h4&gt;
This dataset contains in situ water level measurements collected at 49 different locations across the Atchafalaya and Terrebonne basins in the Mississippi River Delta (MRD) floodplain, and 49 files with the in situ measurements from raw water level converted to absolute water surface elevation with respect to NAVD88 (GEOID12B). There were 65 sites included in the study, however, data from 16 of the sites were corrupted, unretrievable from the instrument or the instrument was lost during deployment. Additionally, it contains water surface elevations collected by GNSS mounted to a boat while underway, and a summary file with site information for all 65 sites. Relative water level measurements were recorded every 15-20 minutes using commercial pressure transducers (Levelogger, Solinst) to measure water depth. Water surface elevation was determined by measuring an absolute height conversion at each sensor location using AirSWOT or a survey-grade global navigation satellite system (GNSS). These water level measurements calibrate and validate the Delta-X campaign&amp;#39;s remote sensing observations and hydrodynamic models. The data are provided in comma separated values (CSV) and JPEG image formats.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_island_channel_model_2106&quot;&gt;DeltaX_Island_Channel_Model_2106&lt;/h4&gt;
This dataset includes model code and output for a model that simulates changes in islands and small water channels of river delta systems in response to dynamics of sediment deposit, erosion, and changing water levels. Simulations demonstrate developmental cycles of secondary channels and how sediment dynamics can allow islands to build land vertically to keep pace with rising sea levels rather than passively drowning. The model was applied to the Mississippi River Delta as part of NASA&amp;#39;s Delta-X project. Simulations were run for other river deltas, including the Amazon, Brahmputra, Danube, Magdalena, Nile, Orinoco, Parana, Rhine-Meuse, and Rhone rivers. The model code is provided in text format for MATLAB software. Files demonstrating initial model conditions and outputs are provided in binary MATLAB as well as NetCDF version 4 format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_totalsubsidencerate_mrd_2307&quot;&gt;DeltaX_TotalSubsidenceRate_MRD_2307&lt;/h4&gt;
This dataset provides estimates of land subsidence rates for the Delta-X domain area within the Atchafalaya and Terrebonne basins for 2021. The study area is a portion of the Mississippi River Delta in coastal Louisiana, U.S. The total subsidence is calculated as the sum of deep and shallow vertical elevation change rates. The deep subsidence rate is based on information from the Coastal Protection and Restoration Authority (CPRA) of Louisiana, documented in the Phase-4 subsidence trend report prepared for and provided by CPRA (2022). The shallow subsidence is calculated for the Delta-X study area by interpolation of publicly available data provided by CPRA for their coast-wide estimation of shallow subsidence in the 2023 Coastal Master Plan. The total subsidence rates and the estimated uncertainty in the total subsidence rates are provided as separate files in cloud optimized GeoTIFF (COG) format at 30-m (0.0003 decimal degrees) resolution.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_landaccretion_wld_2309&quot;&gt;DeltaX_LandAccretion_WLD_2309&lt;/h4&gt;
This dataset provides the Matlab sediment transport and land accretion model at Wax Lake Delta (WLD), Atchafalaya Basin, in coastal Louisiana. The data include the Matlab scripts that solve the advection and Exner equations to simulate the suspended sediment transport and accretion at WLD. The model requires modeled flow information from a separate ANUGA hydrodynamic model as inputs. For this study, ANUGA modeled flow information from the Delta-X Spring and Fall 2021 campaigns were used as inputs. The ANUGA output files are converted to variables used by this Matlab model using pre-processing tools. The main code calculates suspended sediment fluxes and accretion rates of mud and sand as a function of space and time. The cumulative sediment accretion from each campaign was then used to estimate an annualized land accretion map using a weighted-average formula presented. The final product, the one-yr upscaled land accretion map, is archived as a separate dataset.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_landaccretionmap_wld_2308&quot;&gt;DeltaX_LandAccretionMap_WLD_2308&lt;/h4&gt;
This dataset provides sediment transport and land accretion model results at Wax Lake Delta (WLD), Atchafalaya Basin, in coastal Louisiana, USA. Data were simulated over the Delta-X Spring 2021 (2021-03-21 to 2021-04-03) and Fall 2021 (2021-08-14 to 2021-08-27) campaigns and the results are presented as annualized land accretion rate map. The model results for these two short-term campaigns are used to calculate the 1-year upscale land accretion rate at WLD in post-processing, which is also provided in this dataset. Model results for these two short-term campaigns were derived using inputs from an ANUGA hydrodynamic model. The Matlab sediment transport and land accretion model used to derive these data employs sediment transport theory that models floc behavior using a non-cohesive sediment transport framework. Data are presented in NetCDF (.nc) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_marshaccretion_numar_2354&quot;&gt;DeltaX_MarshAccretion_NUMAR_2354&lt;/h4&gt;
This dataset provides input data and model code to run the Marsh Accretion Rates (NUMAR) process model used to predict soil accretion rates and chemical properties for marsh sites in the Mississippi River Delta. NUMAR is a modification of the NUMAN model by Chen and Twilley (1999) that was developed for mangrove environments. This dataset provides Python code, input data in comma separated values (CSV) format, and documentation for installing and running the model in Portable Document Format (PDF).
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_numar_soil_accretion_2368&quot;&gt;DeltaX_NUMAR_Soil_Accretion_2368&lt;/h4&gt;
This dataset holds modeled estimates of soil accretion for the Atchafalaya and Terrebonne basins in the Mississippi River Delta of coastal Louisiana, U.S. Soil accretion was predicted from 2021-2100 using the Numerical Understanding of Marsh Accretion Resilience (NUMAR) model. This process-based model is an adaptation of the NUMAN model that was modified for marsh environments. The input parameters were aggregated within ecogeomorphic cells, areas of similar vegetation and elevation. The dataset includes spatially explicit input values, description of important parameters, and a shapefile of model outputs.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_insitu_poc_2073&quot;&gt;DeltaX_Insitu_POC_2073&lt;/h4&gt;
This dataset provides measurements of particulate organic carbon (POC) concentrations made on water samples collected during 2021 in surface waters of the Atchafalaya River and Terrebonne Basins, portions of the Mississippi River Delta in coastal Louisiana. Water samples were collected at ~0.5 m depth from surface during the spring (2021-03-25 to 2021-04-22) and fall (2021-08-14 to 2021-09-24) field efforts. Field sampling was paused on August 25 and resumed on September 13 due to the landfall of Hurricane Ida on 2021-08-26 approximately 70 km east of the study sites. Water quality changes in this dataset caused by the hurricane are expected to be minimal. Samples were collected in multiple channels of varying width (from a few meters to &amp;gt;100 m) near Delta-X intensive study sites, in open bays and lakes, and a few locations in the nearshore Gulf of Mexico. For each sample, the water sample volume was filtered (in triplicate) through 25-mm glass microfiber (GF/F) filters to retain the suspended particles. The amount of organic carbon retained on each filter was measured using an elemental carbon, hydrogen and nitrogen (CHN) analyzer and normalized by the volume of sample water filtered. The reported values in this dataset include the mean and standard deviation of POC measurements from three replicate samples collected at each site.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_rtk_elevation_2071&quot;&gt;DeltaX_RTK_Elevation_2071&lt;/h4&gt;
This dataset provides real-time kinematic (RTK) GPS elevation measurements, along with horizontal and vertical precision errors, obtained along transects near Louisiana&amp;#39;s Coastwide Reference Monitoring Systems (CRMS) sites and on Mike Island in Wax Lake Delta (WLD). The data were collected during the Delta-X Spring Campaign from 2021-03-24 to 2021-04-02. The data are provided in comma-separated values (CSV) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_bg_root_stable_isotopes_2193&quot;&gt;DeltaX_BG_Root_Stable_Isotopes_2193&lt;/h4&gt;
This dataset contains carbon-13 (13C) and nitrogen-15 (15N) isotopic signatures of belowground root biomass samples from herbaceous wetlands in the Atchafalaya and Terrebonne basins of the Mississippi River Delta in coastal Louisiana, U.S., during August 2021. The data were collected during the Delta-X Fall deployment. Field measurements were conducted at three sites in the Atchafalaya basin and three sites in the Terrebonne basin. Five of the sites are adjacent to sites from the Coastwide Reference Monitoring System (CRMS). The other site is located in Wax Lake Delta (WLD) without appropriate adjacent CRMS sites. Herbaceous wetland sites in both basins were chosen to represent a salinity gradient including freshwater, brackish, and saline ecosystems. Root biomass samples were collected using a gouge soil auger. Bulk isotopic signatures in living fine roots were measured with a mass spectrometer coupled to an elemental analyzer.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_sediment_core_grainsize_2382&quot;&gt;DeltaX_Sediment_Core_GrainSize_2382&lt;/h4&gt;
This dataset provides grain size distribution measurements collected from sediment core samples on Mike Island in the Wax Lake Delta, Louisiana, as part of the Delta-X Spring campaign in March, 2021,and the Fall campaign during August, 2021. The data are for March 26 and 29, and August 18 and 24. Sediment cores were collected using a piston core, then volume-based grain size distribution for each sample was measured using a laser diffraction particle size analyzer. The data are provided in comma separated values (CSV) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_cs137_soilaccretionrate_2380&quot;&gt;DeltaX_Cs137_SoilAccretionRate_2380&lt;/h4&gt;
This dataset holds measurements of Cesium-137 (137Cs) activity sampled from sites in the Atchafalaya and Terrebonne Basins on the southern coast of Louisiana, USA. Sediment cores were taken to validate modeled estimates of soil accretion rates. The NUMAR model was designed to predict soil properties and corresponding accretion rates in marsh environments. This study explored whether the probabilistic outcomes generated by the model align with accretion rates determined through field-based measurements using 137Cs activity. The model&amp;#39;s probabilistic simulations were conducted for active and inactive basins, encompassing fresh, brackish, and saline sites. Aliquots of approximately 5-9 g of finely ground dry sediment were placed into vials of known geometry for direct gamma counting of 137Cs using high-purity Germanium (Ge) well detectors. The 137Cs dating technique is based on detecting the specific core section in which the radioactive isotope 137Cs peak activity occurs across a vertical soil profile. This peak corresponds to the peak fallout in 1963 deposited during the atmospheric nuclear testing and provides a timeline reference for estimating soil accumulation rates, sediment deposition, and marsh accretion. Therefore, to validate the NUMAR accretion results, 137Cs activity was measured at different core sections across a vertical soil profile to determine the peak corresponding to the peak fallout in 1963 due to atmospheric nuclear testing and estimate soil accretion rates. The data are provided in comma separated values (CSV) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_herb_wetlandsoil_v3_2239&quot;&gt;DeltaX_Herb_WetlandSoil_V3_2239&lt;/h4&gt;
This dataset contains properties of soil core samples for herbaceous wetlands collected in the Atchafalaya and Terrebonne basins in southeastern coastal Louisiana for the period 2021-03-21 to 2021-04-02 and on 2021-08-19. Field measurements were conducted at six sites in the Atchafalaya (N &#x3D; 3) and Terrebonne (N &#x3D; 3) basins. Five sites were adjacent to sites from the Coastwide Reference Monitoring System (CRMS). The other site is in the Wax Lake Delta (WLD) without appropriate adjacent CRMS sites. Herbaceous wetland sites in both basins were chosen to represent a salinity gradient including freshwater, brackish and saline ecosystems. Soil properties include bulk density, organic matter content, total densities of carbon, nitrogen, phosphorus, along with 13C and 15N isotopic signatures. The data are provided in comma-separated values (.csv) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_sonar_bathymetry_2085&quot;&gt;DeltaX_Sonar_Bathymetry_2085&lt;/h4&gt;
This dataset includes bathymetry data for water channels in a portion of the Mississippi River Delta (MRD) of coastal Louisiana. The data were collected using sonar during field efforts of the Delta-X Campaign taking place during 2021. In situ continuous surveys of channel bathymetry were conducted in the Atchafalaya and Terrebonne basins using either a Lowrance HDS-Live Fish Finder with Active Imaging 3-in-1 Transducer or a SonarMite Echo Sounder mounted on the side or back of the research boat. The sounder depth observations were delineated by the date, time, and location. These bathymetry measurements were used to generate a digital elevation model (DEM) through interpolation with ancillary DEMs. The data are provided in comma-separated values (CSV) format. A map of data collection routes is provided in compressed keyhole markup language (KMZ).
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_tss_concentration_v2_2075&quot;&gt;DeltaX_TSS_Concentration_V2_2075&lt;/h4&gt;
This dataset provides measurements of total suspended solids concentrations (TSS) of surface waters in the Atchafalaya River and Terrebonne Basins during the spring (2021-03-25 to 2021-04-22) and fall (2021-08-14 to 2021-09-24) field efforts by the Delta-X project. Field sampling was paused on August 25 and resumed on September 13, 2021, due to the landfall of Hurricane Ida on 2021-08-26 approximately 70 km east of the study site. Water quality changes caused by the hurricane were expected to be minimal. Samples were collected from ~0.5 m of surface in multiple channels of varying width (from a few meters to &amp;gt;100 m), near Delta-X intensive study sites, in open bays and lakes, and at few locations in the nearshore Gulf of Mexico. For each collection, the water sample volume was filtered, and the suspended particles retained on the filter were weighed after drying. The TSS concentration was calculated as the difference of the filter weight (before and after filtration) divided by the volume filtered.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_turbidity_data_v4_2241&quot;&gt;DeltaX_Turbidity_Data_V4_2241&lt;/h4&gt;
This dataset provides turbidity measurements with co-located water and air pressure and temperature measurements in portions of the Mississippi River Delta, coastal Louisiana, US. Data were collected at five sites in Atchafalaya River Basin in Spring (2021-03-24 to 2021-04-02) and eight sites in the Atchafalaya River and Terrebonne Basins in Fall 2021 (2021-08-16 to 2021-08-27). In order to sample various hydrodynamic conditions, sensors were deployed at island edges, island interior, and other portions of wetlands. Sensors recorded turbidity, absolute pressure, and temperature. The Delta-X mission is a 5-year NASA Earth Venture Suborbital-3 mission to study the Mississippi River Delta in the United States, which is growing and sinking in different areas. River deltas and their wetlands are drowning as a result of sea level rise and reduced sediment inputs. The Delta-X mission will determine which parts will survive and continue to grow, and which parts will be lost. Delta-X begins with airborne and in situ data acquisition and carries through data analysis, model integration, and validation to predict the extent and spatial patterns of future deltaic land loss or gain. The data are provided in comma-separated values (CSV) files.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_l1_uavsar_slc_stack_1984&quot;&gt;DeltaX_L1_UAVSAR_SLC_Stack_1984&lt;/h4&gt;
This dataset contains UAVSAR Level 1 (L1) Single Look Complex (SLC) stack products for Delta-X flight lines acquired during 2021-03-27 to 2021-04-18 (spring) and 2021-09-03 to 2021-09-13 (fall). The data were collected by Uninhabited Aerial Vehicle Synthetic Aperture Radar (UAVSAR), a polarimetric L-band synthetic aperture radar flown on the NASA Gulfstream-III (C20) aircraft as part of the Delta-X campaign. The study area includes the Atchafalaya Basin, in Southern Louisiana, USA, within the Mississippi River Delta (MRD) floodplain. Repeat pass interferometric synthetic aperture (InSAR) data are a standard UAVSAR product delivered by the UAVSAR processing team. These repeat pass SLC stack co-registered time series data were used as the underlying data for higher level data products. These higher level products provide a time series of water level changes and address a goal of the Delta-X campaign to measure water-level changes throughout wetlands. Data quality was assessed by comparing water elevation estimates with data from in situ water level gauges throughout the study area. These L1 data contain slant range single look complex (SLC), latitude/longitude/height, look vector, doppler, and metadata files. The data are provided in SLC stack format (.slc) with associated annotation (.ann), latitude-longitude-height (.llh), look vector (.lkv), and Doppler centroid-slant range (.dop) files. The single look complex (SLC) stacks are in the HH, HV, VH, and VV polarizations. The same area was sampled at approximately 30-minute intervals. The SLCs are not corrected for residual baseline (BU).
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_l1b_uavsar_waterlevels_1979&quot;&gt;DeltaX_L1B_UAVSAR_WaterLevels_1979&lt;/h4&gt;
This dataset contains UAVSAR Level 1B (L1B) interferometric products for Delta-X flight lines acquired during the 2021 Spring (2021-03-27 to 2021-04-18) and Fall (2021-09-03 to 2021-09-13) deployments. The data were collected by Uninhabited Aerial Vehicle Synthetic Aperture Radar (UAVSAR), a polarimetric L-band synthetic aperture radar flown on the NASA Gulfstream-III (C20) aircraft as part of the Delta-X campaign. The study area includes the Atchafalaya Basin, in Southern Louisiana, USA, within the Mississippi River Delta (MRD) floodplain. Repeat pass interferometric synthetic aperture (InSAR) data are a standard UAVSAR product delivered by the UAVSAR processing team. For this dataset, a set of nearest-neighbor (NN), NN+1, and NN+2 co-registered VV-polarization interferograms were generated from the quad-polarization SLC stack level-1 (L1) product using a combination of the InSAR Scientific Computing Environment (ISCE), the statistical-cost, network-flow algorithm for phase unwrapping (SNAPHU), and previously developed python code. Data quality was assessed by comparing water elevation estimates with data from in situ water level gauges throughout the study area. The data are provided in non-georeferenced ENVI file format and include interferometric amplitude, wrapped interferometric phase, interferometric coherence, and unwrapped interferometric phase products. Geometry files for each flight line per field campaign with latitude, longitude, height and incidence angle information are also included. The goal of this campaign was to measure water-level changes throughout wetlands, and these data may be used to generate time series of water levels. The data are provided in ENVI format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_l2_uavsar_waterlevels_2057&quot;&gt;DeltaX_L2_UAVSAR_WaterLevels_2057&lt;/h4&gt;
This dataset contains georeferenced UAVSAR Level 2 (L2) interferometric products for Delta-X flight lines acquired during the spring (2021-03-27 to 2021-04-18) and fall (2021-09-03 to 2021-09-13) deployments. This dataset provides water-level change observations throughout wetlands of the Atchafalaya and Terrebonne Basins, in Southern Louisiana, USA, within the Mississippi River Delta (MRD), and it may be used to generate time series analysis. The data were collected by Uninhabited Aerial Vehicle Synthetic Aperture Radar (UAVSAR), a polarimetric L-band synthetic aperture radar flown on the NASA Gulfstream-III (C20) aircraft as part of the Delta-X campaign. Water surface elevations were measured on multiple flights at 30-minute intervals. Data quality was assessed by comparing water elevation estimates with data from in situ water level gauges throughout the study area. The data include interferogram phase, interferogram amplitude, unwrapped interferogram phase, and coherence products. A series of quality assurance masks of troposphere-induced phase delay regions were generated for all SAR acquisition dates using a weather feature matching algorithm. Geometry files for each flight line per field campaign with latitude, longitude, height and incidence angle information are also included. The data are provided in ENVI format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_uavsar_l3_channelmap_v2_2344&quot;&gt;DeltaX_UAVSAR_L3_ChannelMap_V2_2344&lt;/h4&gt;
This dataset provides gridded estimates of water channels for the Atchafalaya and Terrebonne basins of the Mississippi River Delta in Louisiana, U.S.A. The data show channels with open water that are as narrow as 10 m. These channel estimates were generated from the Uninhabited Aerial Vehicle Synthetic Aperture Radar (UAVSAR) Level 1B interferometric products in radar coordinates acquired in the Spring and Fall Delta-X deployments of 2021, which have a spatial resolution of approximately 6 m. UAVSAR is a polarimetric L-band synthetic aperture radar (SAR) flown on the NASA Gulfstream-III aircraft. The data are provided in cloud-optimized GeoTIFF format. The channel estimates can be used to define open water paths in hydrodynamic models and to evaluate model performance.
&lt;br&gt;&lt;h4 id&#x3D;&quot;deltax_l3_uavsar_waterlevels_2058&quot;&gt;DeltaX_L3_UAVSAR_WaterLevels_2058&lt;/h4&gt;
This dataset contains georeferenced InSAR-derived water level change maps for Delta-X flight lines acquired during the spring (2021-03-27 to 2021-04-18) and fall (2021-09-03 to 2021-09-13) deployments. Water-level change observations are provided throughout wetlands of the Atchafalaya and Terrebonne Basins, in Southern Louisiana, USA, within the Mississippi River Delta (MRD). The data were collected by Uninhabited Aerial Vehicle Synthetic Aperture Radar (UAVSAR), a polarimetric L-band synthetic aperture radar flown on the NASA Gulfstream-III (C20) aircraft as part of the Delta-X campaign. Water surface elevations were measured on multiple flights at 30-minute intervals. There are three types of gridded products available: temporalcoherence (which provide an index measuring quality of phase unwrapping ranging from 0 (poor) to 1 (correctly unwrapped)), waterlevelchange in centimeters (which provide cumulative changes in water levels at approximately 30-minute intervals), and waterlevelchange_ramp in centimeters (which provide a 2-dimensional linear trend in water-level estimates not related to changing water levels). The water-level change maps were estimated using the phase unwrapping corrected interferograms generated for nearest-neighbor (NN), NN+1, and NN+2 pairs for data acquired within a single flight (one day). This analysis was done for all flight lines. Water level changes are relative to the first sampling flight for that study area. Data quality was assessed by comparing water elevation estimates with data from in situ water level gauges throughout the study area. A series of quality assurance masks of troposphere-induced phase delay regions were generated for all SAR acquisition dates using a weather feature matching algorithm.
&lt;br&gt;&lt;h4 id&#x3D;&quot;predeltax_l3_aviris_biomass_1821&quot;&gt;PreDeltaX_L3_AVIRIS_Biomass_1821&lt;/h4&gt;
This dataset includes aboveground biomass (AGB) and vegetation of herbaceous and forest wetland at 5.4 m resolution across the Wax Lake Delta (WLD) in Southern Louisiana, USA, within the Mississippi River Delta (MRD) floodplain. Vegetation classes were derived from Airborne Visible/Infrared Imaging Spectrometer-Next Generation (AVIRIS-NG) imagery acquired over the Atchafalaya Basin and the Terrebonne Basin in October 2016 in combination with a digital elevation model. The AVIRIS-NG surface reflectance data were also combined with L-band Uninhabited Airborne Vehicle Synthetic Aperture Radar (UAVSAR) HV backscatter and scattering component values from coincident vegetation sample sites to develop and test AGB models for emergent herbaceous and forested wetland vegetation. This study used the integrated airborne data from AVIRIS-NG and UAVSAR to assess the instruments&amp;#39; unique capabilities in combination for estimating AGB in coastal deltaic wetlands. The 5.4 m resolution vegetation classification map for the WLD study area was then used to apply the best models to estimate AGB across the WLD.
&lt;br&gt;&lt;h4 id&#x3D;&quot;predeltax_l3_aviris_sediment_1822&quot;&gt;PreDeltaX_L3_AVIRIS_Sediment_1822&lt;/h4&gt;
This dataset includes total suspended solids (TSS) at the water surface across the Atchafalaya and Terrebonne Basins in Southern Louisiana, USA, within the Mississippi River Delta (MRD) floodplain. AVIRIS-NG, the Next Generation Airborne Visible to Infrared Imaging Spectrometer, acquired data over the study area in 2015 and 2016. The remote imageries were combined with coincident field measurements to develop and validate spatially explicit estimates at 3.7-5.4 m resolution of the concentration (mg/L) of TSS.
&lt;br&gt;&lt;h4 id&#x3D;&quot;predeltax_sonar_bathymetry_1807&quot;&gt;PreDeltaX_Sonar_Bathymetry_1807&lt;/h4&gt;
This dataset provides water depths and water surface elevations collected during bathymetric surveys of the main channel of the Wax Lake Delta within the Mississippi River Delta (MRD) floodplain of coastal Louisiana, USA. The measurements were made during the Pre-Delta-X Campaign in Fall 2016. The in situ continuous (1 Hz) surveys of channel bathymetry were conducted using a SonarMite Hydrolite Single Beam Echo Sounder mounted on the side of the research boat. The sounder was located directly beneath the Septentrio global navigation satellite system (GNSS) antenna, about 30 cm below the water surface. The sounder depth observations were integrated with the GNSS location and elevation data into one data file per day for October 16-20. These bathymetry measurements were used to generate a merged digital elevation model (DEM) through interpolation with ancillary DEMs to expand the existing wetland DEM to include channels. The merged DEM product is distributed in GeoTIFF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;predeltax_uavsar_slc_1816&quot;&gt;PreDeltaX_UAVSAR_SLC_1816&lt;/h4&gt;
This Level 1 (L1) dataset includes single look complex (SLC) stack products and co-registered interferograms in the HH (horizontal transmit and horizontal receive) polarization for the Atchafalaya Basin, in Southern Louisiana, USA, within the Mississippi River Delta (MRD) floodplain. The data were collected in October 2016 by Uninhabited Aerial Vehicle Synthetic Aperture Radar (UAVSAR), a polarimetric L-band synthetic aperture radar flown on the NASA Gulfstream-III aircraft as part of the Pre-Delta-X campaign. A single study region, flight line &amp;quot;gulfco_12011&amp;quot;, was sampled six times at approximately 30-minute intervals to monitor changing water levels. The SLC stack product is a standard UAVSAR product delivered by the UAVSAR processing team. The L1 interferograms were generated from the SLC stacks.
&lt;br&gt;&lt;h4 id&#x3D;&quot;predeltax_l2_airswot_1818&quot;&gt;PreDeltaX_L2_AirSWOT_1818&lt;/h4&gt;
This dataset provides water surface elevations over the Wax Lake Delta in the Atchafalaya Basin in coastal Louisiana, USA, in May 2015. These Level 2 (L2) data were collected by AirSWOT, an airborne instrument employing near-nadir wide-swath Ka-band radar interferometry to measure water-surface elevation and produce continuous gridded elevation data at 3.6 m resolution. Along with elevation estimates, the dataset includes measures of estimation errors, sensitivity, incidence angle, backscatter, and interferometric correlation. For this application, in situ water level data were added into the AirSWOT phase calibration procedure. These L2 data consist of a set of rasters in Universal Transverse Mercator (UTM) map coordinates for each of the 39 AirSWOT flight lines. These elevation data were later used for calculating elevation and slopes along the main channels in this wetland system, as well as tying observations to ocean tidal conditions.
&lt;br&gt;&lt;h4 id&#x3D;&quot;predeltax_l2_aviris_sr_1826&quot;&gt;PreDeltaX_L2_AVIRIS_SR_1826&lt;/h4&gt;
This Level 2 (L2) dataset provides surface spectral reflectance data acquired over the Atchafalaya and Terrebonne basins of the Mississippi River Delta (MRD) of coastal Louisiana, USA, in 2015-2016. The data include georectified images with Lambertian-equivalent surface reflectance and composite mosaics with adjustments for Bidirectional Reflectance Distribution Function (BRDF) effects. The imagery was acquired by the Airborne Visible/Infrared Imaging Spectrometer - Next Generation (AVIRIS-NG), as part of the Pre-Delta-X campaign.
&lt;br&gt;&lt;h4 id&#x3D;&quot;predeltax_l3_airswot_wl_1819&quot;&gt;PreDeltaX_L3_AirSWOT_WL_1819&lt;/h4&gt;
This dataset contains water level profiles generated from the AirSWOT data collected in the Atchafalaya Basin in Southern Louisiana, USA, within the Mississippi River Delta (MRD) floodplain. Part of the Pre-Delta-X Campaign, AirSWOT used near-nadir wide-swath Ka-band radar interferometry to measure water-surface elevation and uncertainty in May 2015. This Level 3 (L3) AirSWOT dataset is in the form of numerous profiles of water level along the Wax Lake Outlet.
&lt;br&gt;&lt;h4 id&#x3D;&quot;predeltax_aso_lidar_waterlevel_1820&quot;&gt;PreDeltaX_ASO_LiDAR_WaterLevel_1820&lt;/h4&gt;
This dataset contains lidar-derived water surface elevation profiles for river channels between Wax Lake, in the Atchafalaya River Basin of the Mississippi River Delta, and the Gulf of Mexico. The provided elevation profiles (i.e., water levels) were estimated using remotely sensed lidar data in combination with in situ field measurements of water levels for elevation calibration and to quantify uncertainty in estimates. The lidar data were collected during the Fall 2016 Pre-Delta-X Campaign using an Airborne Snow Observatory (ASO) lidar instrument. The results are time-specific water levels measured as elevation in meters with respect to the North American Vertical Datum 1988 (NAVD 88) geoid (or orthometric height) and the World Geodetic System 1984 (WGS 84) ellipsoidal surface (or ellipsoidal/GPS height) along the water channels in this drainage system.
&lt;br&gt;&lt;h4 id&#x3D;&quot;predeltax_adcp_measurements_1806&quot;&gt;PreDeltaX_ADCP_Measurements_1806&lt;/h4&gt;
This dataset provides river discharge measurements collected at selected locations across the Atchafalaya River Basin, within the Mississippi River Delta (MRD) floodplain in coastal Louisiana, USA. The measurements were made during the Pre-Delta-X campaign on October 15 to 20, 2016. Seventy-five channel surveys were conducted with a SonTek RiverSurveyor M9 acoustic doppler current profiler (ADCP) on selected wide channels (&lt;del&gt;100 m) and a few selected (&lt;/del&gt;10 m) narrow channels. ADCP data provide near-instantaneous estimates of river discharge across the sampled channels. Sites coincided with AirSWOT swaths in the Atchafalaya River Basin and water level measurement locations. This in situ dataset was used to calibrate and validate Delta-X hydrodynamic models.
&lt;br&gt;&lt;h4 id&#x3D;&quot;predeltax_insitu_reflectance_1804&quot;&gt;PreDeltaX_Insitu_Reflectance_1804&lt;/h4&gt;
This dataset provides measurements of in situ remote-sensing reflectance (Rrs; per steradian) of surface water across Atchafalaya Basin, southern coastal Louisiana, USA within Mississippi River Delta (MRD) floodplain. The in situ spectral reflectance measurements were made during the Pre-Delta-X campaign in Fall 2016 (October 14 to 2). Hand-held spectrometer measurements were collected from a boat at 35 locations selected to represent a range of suspended sediment concentrations and properties from a variety of hydrodynamic and physical settings typically encountered across the Atchafalaya basin. These 35 spectral reflectance measurements were collected at 24 unique sites that coincide with measurements of total suspended solids (TSS). The data serves two main purposes, to ground-truth the remote-sensing reflectance derived from NASA&amp;#39;s Airborne Visible-Infrared Imaging Spectrometer - Next Generation (AVIRIS-NG) instrument, and to calibrate and validate algorithms for the retrieval of TSS from AVIRIS-NG.
&lt;br&gt;&lt;h4 id&#x3D;&quot;predeltax_tss_concentration_1802&quot;&gt;PreDeltaX_TSS_Concentration_1802&lt;/h4&gt;
This dataset contains the total suspended solids (TSS) concentration of in situ water samples collected at selected sites across the Atchafalaya and Terrebonne Basins within the Mississippi River Delta (MRD) floodplain of coastal Louisiana, USA. The measurements were made during the Pre-Delta-X campaign in Spring 2015 and Fall 2016. The sampling sites spanned large and small channels at locations chosen to cover a representative range of suspended sediment concentrations from a variety of hydrodynamic and physical settings typically encountered across the basins. Water samples were collected by bottle just beneath the surface and stored on ice until filtering. The TSS concentration was calculated as the difference of the filter weight (before and after filtration) divided by the volume of sample filtered. Both TSS and in situ spectral reflectance measurements were collected at some sampling sites. Pre-Delta-X sampling focused on surface waters, where the TSS data are used as inputs for hydrodynamic models for sediment transport and to calibrate the model to convert AVIRIS-NG spectral reflectance measurements into TSS.
&lt;br&gt;&lt;h4 id&#x3D;&quot;predeltax_uavsarchannelmaps_v2_2366&quot;&gt;PreDeltaX_UAVSARChannelMaps_V2_2366&lt;/h4&gt;
This dataset provides spatial data on water channels in the estuary of the Atchafalaya Basin of the Mississippi River Delta of coastal Louisiana. These Level-3 (L3) channel maps were developed from interferograms derived from Uninhabited Aerial Vehicle Synthetic Aperture Radar (UAVSAR) data collected on 2016-10-16 (low tides) and 2016-10-17 (high tides). The channel maps define open water paths in hydrodynamic models and are used to evaluate model performance. This is version 2 of this dataset. Data are provided in cloud optimized GeoTIFF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;predeltax_uavsar_waterlevel_1823&quot;&gt;PreDeltaX_UAVSAR_WaterLevel_1823&lt;/h4&gt;
This dataset contains five maps of cumulative changes in water levels at 30-minute intervals over a 150-minute period on 2016-10-16 in the Atchafalaya Basin in Southern Louisiana, USA, within the Mississippi River Delta (MRD) floodplain. Water surface elevations were measured on six flights at 30-minute intervals, with the Uninhabited Aerial Vehicle Synthetic Aperture Radar (UAVSAR), a polarimetric L-band synthetic aperture radar (SAR) flown on the NASA Gulfstream-III aircraft. The five georeferenced maps at 6 m resolution show the cumulative change of water levels (cm) every 30 minutes relative to the first sampling flight. These Level 3 maps were generated using the InSAR time series Small Baseline Subsets (SBAS) algorithm implemented in the Generic InSAR Analysis Toolbox (GIAnT) toolbox and served to evaluate and compare hydrodynamic models.
&lt;br&gt;&lt;h4 id&#x3D;&quot;predeltax_vegetation_structure_1805&quot;&gt;PreDeltaX_Vegetation_Structure_1805&lt;/h4&gt;
This dataset provides vegetation species, height, stem density and diameter, and species aboveground biomass (AGB) measurements collected at herbaceous and forested wetland sites across the Atchafalaya and Terrebonne basins within the Mississippi River Delta (MRD) floodplain in coastal Louisiana, USA. The measurements were made during the Pre-Delta-X campaign in Spring 2015 and Fall 2015. Vegetation height and density and diameter data are only provided for forested Atchafalaya sites during the spring collections. At the nine herbaceous wetland sites, a transect was established perpendicular to the wetland edge with replicate sample plots (0.25 m2, 5 m apart) located at 50, 100, and 150 m from the wetland edge to capture the range of vegetation structure, zonation, and composition. AGB was harvested inside the duplicate plots at each sampling location. At the six forested wetland sites, duplicate circular plots (10 m radius, 50 m apart) were established inside the forest approximately 30 m from the wetland edge. All trees with a diameter at breast height (DBH at 1.3 m) &amp;gt; 2.5 cm were measured within each plot and identified to species. The height of trees was measured with a laser range finder. AGB was estimated using species-specific allometric equations. Measurements were used to generate marsh and forested wetland coverage and biomass in response to seasonality within both basins. The data will be used to calibrate remote sensing data (e.g., UAVSAR, AVIRIS-NG) and hydrodynamics and sediment transport models.
&lt;br&gt;&lt;h4 id&#x3D;&quot;predeltax_water_level_data_1801&quot;&gt;PreDeltaX_Water_Level_Data_1801&lt;/h4&gt;
This dataset provides absolute water level elevations derived for 10 locations across the Wax Lake Delta, Atchafalaya Basin, in Southern Louisiana, USA, within the Mississippi River Delta (MRD) floodplain. Field measurements were made during the Pre-Delta-X campaign on October 13-20, 2016. Relative water level measurements were recorded every five minutes during a one-week period using in situ pressure transducers (Solinst) to measure water surface elevation change with millimeter accuracy. The Solinst system combines a total pressure transducer (TPT) and a temperature detector. Once underwater, the TPT measures the sum of the atmosphere and water pressure above the sensor. Atmospheric pressure fluctuations must be accounted for to obtain the height of the water column above the TPT. An absolute elevation correction was applied to the water level data using an iterative approach with the USGS Calumet Station water level height and Airborne Snow Observatory (ASO) lidar water level profiles. These Pre-Delta-X water level measurements served to calibrate and validate the campaign&amp;#39;s remote sensing observations and hydrodynamic models.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.ornldaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA ECCO Project</title>
      <link>https://registry.opendata.aws/nasa-ecco</link>
      <guid>https://registry.opendata.aws/nasa-ecco</guid>
      <description>This dataset provides ancillary data for the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate, and is intended for expert users to reproduce the state estimate. The ancillary data include documentation files, files required to initialize the model, forcing fields, binary input grid files, observational data used to constrain the model, model equivalent of observed profiles, files related to atmospheric flux-forced experiments, and some script files. Estimating the Circulation and Climate of the Ocean (ECCO) state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of a global, nominally 1-degree configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds].
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_atm_state_05deg_daily_v4r4&quot;&gt;ECCO_L4_ATM_STATE_05DEG_DAILY_V4R4&lt;/h4&gt;
This dataset contains daily-averaged atmosphere surface temperature, humidity, wind, and pressure interpolated to a regular 0.5-degree grid from the ECCO Version 4 revision 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g.,research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_atm_state_llc0090grid_daily_v4r4&quot;&gt;ECCO_L4_ATM_STATE_LLC0090GRID_DAILY_V4R4&lt;/h4&gt;
This dataset provides daily-averaged atmosphere surface temperature, humidity, winds, and pressure on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_atm_state_05deg_monthly_v4r4&quot;&gt;ECCO_L4_ATM_STATE_05DEG_MONTHLY_V4R4&lt;/h4&gt;
This dataset contains monthly-averaged atmosphere surface temperature, humidity, wind, and pressure interpolated to a regular 0.5-degree grid from the ECCO Version 4 revision 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g.,research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_atm_state_llc0090grid_monthly_v4r4&quot;&gt;ECCO_L4_ATM_STATE_LLC0090GRID_MONTHLY_V4R4&lt;/h4&gt;
This dataset provides monthly-averaged atmosphere surface temperature, humidity, winds, and pressure on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_ocean_bolus_streamfunction_llc0090grid_daily_v4r4&quot;&gt;ECCO_L4_OCEAN_BOLUS_STREAMFUNCTION_LLC0090GRID_DAILY_V4R4&lt;/h4&gt;
This dataset provides daily-averaged Gent-McWilliams ocean bolus transport streamfunction on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height and model sea level anomaly (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_ocean_bolus_streamfunction_llc0090grid_monthly_v4r4&quot;&gt;ECCO_L4_OCEAN_BOLUS_STREAMFUNCTION_LLC0090GRID_MONTHLY_V4R4&lt;/h4&gt;
This dataset provides monthly-averaged Gent-McWilliams ocean bolus transport streamfunction on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height and model sea level anomaly (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_bolus_05deg_daily_v4r4&quot;&gt;ECCO_L4_BOLUS_05DEG_DAILY_V4R4&lt;/h4&gt;
This dataset contains daily-averaged Gent-McWilliams ocean bolus velocity interpolated to a regular 0.5-degree grid from the ECCO Version 4 revision 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g.,research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_bolus_llc0090grid_daily_v4r4&quot;&gt;ECCO_L4_BOLUS_LLC0090GRID_DAILY_V4R4&lt;/h4&gt;
This dataset provides daily-averaged Gent-McWilliams ocean bolus velocity on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_bolus_05deg_monthly_v4r4&quot;&gt;ECCO_L4_BOLUS_05DEG_MONTHLY_V4R4&lt;/h4&gt;
This dataset contains monthly-averaged Gent-McWilliams ocean bolus velocity interpolated to a regular 0.5-degree grid from the ECCO Version 4 revision 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g.,research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_bolus_llc0090grid_monthly_v4r4&quot;&gt;ECCO_L4_BOLUS_LLC0090GRID_MONTHLY_V4R4&lt;/h4&gt;
This dataset provides monthly-averaged Gent-McWilliams ocean bolus ocean velocity on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_geometry_05deg_v4r4&quot;&gt;ECCO_L4_GEOMETRY_05DEG_V4R4&lt;/h4&gt;
This dataset provides geometric parameters for the regular 0.5-degree lat-lon grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Parameters include areas and lengths of grid cell sides and the horizontal and vertical coordinates of grid cell centers and corners. Additional information related to the global domain geometry (e.g., bathymetry and land/ocean masks) are also included. However, users should note these domain geometry fields are approximations because they have been interpolated from the ECCO lat-lon-cap 90 (llc90) native model grid. Users interested in exact budget closure calculations for volume, heat, salt, or momentum should use ECCO fields provided on the llc90 grid. Estimating the Circulation and Climate of the Ocean (ECCO) state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of a global, nominally 1-degree configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_geometry_llc0090grid_v4r4&quot;&gt;ECCO_L4_GEOMETRY_LLC0090GRID_V4R4&lt;/h4&gt;
This dataset provides geometric parameters for the lat-lon-cap 90 (llc90) native model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Parameters include areas and lengths of grid cell sides; horizontal and vertical coordinates of grid cell centers and corners; grid rotation angles; and global domain geometry including bathymetry and land/ocean masks. Estimating the Circulation and Climate of the Ocean (ECCO) state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of a global, nominally 1-degree configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_gmap_time_series_snapshot_v4r4&quot;&gt;ECCO_L4_GMAP_TIME_SERIES_SNAPSHOT_V4R4&lt;/h4&gt;
This dataset provides instantaneous hourly global mean atmospheric pressure from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height and model sea level anomaly (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_gmap_time_series_snapshot_v4r4b&quot;&gt;ECCO_L4_GMAP_TIME_SERIES_SNAPSHOT_V4R4B&lt;/h4&gt;
This dataset provides instantaneous hourly global mean atmospheric pressure from the ECCO Version 4 Release 4b (V4r4b) ocean and sea-ice state estimate. V4r4b is an errata for ECCO Version 4, Release 4 (V4r4). Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4b is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4b include sea surface height and model sea level anomaly (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4b covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_gmsl_time_series_daily_v4r4&quot;&gt;ECCO_L4_GMSL_TIME_SERIES_DAILY_V4R4&lt;/h4&gt;
This dataset provides daily-averaged global mean sea level from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height and model sea level anomaly (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_gmsl_time_series_monthly_v4r4&quot;&gt;ECCO_L4_GMSL_TIME_SERIES_MONTHLY_V4R4&lt;/h4&gt;
This dataset provides monthly-averaged global mean sea level from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height and model sea level anomaly (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_ocean_3d_mix_coeffs_05deg_v4r4&quot;&gt;ECCO_L4_OCEAN_3D_MIX_COEFFS_05DEG_V4R4&lt;/h4&gt;
This dataset provides 3D coefficients for the Gent-McWilliams and Redi parameterizations and background vertical diffusivity interpolated to a regular 0.5-degree grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Each of these three time-invariant, spatially-varying terms are estimated during the ECCO V4r4 optimization. Estimating the Circulation and Climate of the Ocean (ECCO) state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of a global, nominally 1-degree configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_ocean_3d_mix_coeffs_llc0090grid_v4r4&quot;&gt;ECCO_L4_OCEAN_3D_MIX_COEFFS_LLC0090GRID_V4R4&lt;/h4&gt;
This dataset provides 3D coefficients for the Gent-McWilliams and Redi parameterizations and background vertical diffusivity on the lat-lon-cap 90 (llc90) native model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Each of these three time-invariant, spatially-varying terms are estimated during the ECCO V4r4 optimization. Estimating the Circulation and Climate of the Ocean (ECCO) state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of a global, nominally 1-degree configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_fresh_flux_05deg_daily_v4r4&quot;&gt;ECCO_L4_FRESH_FLUX_05DEG_DAILY_V4R4&lt;/h4&gt;
This dataset contains daily-averaged ocean and sea-ice surface freshwater fluxes interpolated to a regular 0.5-degree grid from the ECCO Version 4 revision 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g.,research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_fresh_flux_llc0090grid_daily_v4r4&quot;&gt;ECCO_L4_FRESH_FLUX_LLC0090GRID_DAILY_V4R4&lt;/h4&gt;
This dataset provides daily-averaged ocean and sea-ice surface freshwater fluxes on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_fresh_flux_05deg_monthly_v4r4&quot;&gt;ECCO_L4_FRESH_FLUX_05DEG_MONTHLY_V4R4&lt;/h4&gt;
This dataset contains monthly-averaged ocean and sea-ice surface freshwater fluxes interpolated to a regular 0.5-degree grid from the ECCO Version 4 revision 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g.,research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_fresh_flux_llc0090grid_monthly_v4r4&quot;&gt;ECCO_L4_FRESH_FLUX_LLC0090GRID_MONTHLY_V4R4&lt;/h4&gt;
This dataset provides monthly-averaged ocean and sea-ice surface freshwater fluxes on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_heat_flux_05deg_daily_v4r4&quot;&gt;ECCO_L4_HEAT_FLUX_05DEG_DAILY_V4R4&lt;/h4&gt;
This dataset contains daily-averaged ocean and sea-ice surface heat fluxes interpolated to a regular 0.5-degree grid from the ECCO Version 4 revision 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g.,research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_heat_flux_llc0090grid_daily_v4r4&quot;&gt;ECCO_L4_HEAT_FLUX_LLC0090GRID_DAILY_V4R4&lt;/h4&gt;
This dataset provides daily-averaged ocean and sea-ice surface heat fluxes on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_heat_flux_05deg_monthly_v4r4&quot;&gt;ECCO_L4_HEAT_FLUX_05DEG_MONTHLY_V4R4&lt;/h4&gt;
This dataset contains monthly-averaged ocean and sea-ice surface heat fluxes interpolated to a regular 0.5-degree grid from the ECCO Version 4 revision 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g.,research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_heat_flux_llc0090grid_monthly_v4r4&quot;&gt;ECCO_L4_HEAT_FLUX_LLC0090GRID_MONTHLY_V4R4&lt;/h4&gt;
This dataset provides monthly-averaged ocean and sea-ice surface heat fluxes on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_stress_05deg_daily_v4r4&quot;&gt;ECCO_L4_STRESS_05DEG_DAILY_V4R4&lt;/h4&gt;
This dataset contains daily-averaged ocean and sea-ice surface stress interpolated to a regular 0.5-degree grid from the ECCO Version 4 revision 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g.,research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_stress_llc0090grid_daily_v4r4&quot;&gt;ECCO_L4_STRESS_LLC0090GRID_DAILY_V4R4&lt;/h4&gt;
This dataset provides daily-averaged ocean and sea-ice surface stress on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_stress_05deg_monthly_v4r4&quot;&gt;ECCO_L4_STRESS_05DEG_MONTHLY_V4R4&lt;/h4&gt;
This dataset contains monthly-averaged ocean and sea-ice surface stress interpolated to a regular 0.5-degree grid from the ECCO Version 4 revision 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g.,research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_stress_llc0090grid_monthly_v4r4&quot;&gt;ECCO_L4_STRESS_LLC0090GRID_MONTHLY_V4R4&lt;/h4&gt;
This dataset provides monthly-averaged ocean and sea-ice surface stress on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_obp_05deg_daily_v4r4&quot;&gt;ECCO_L4_OBP_05DEG_DAILY_V4R4&lt;/h4&gt;
This dataset contains daily-averaged ocean bottom pressure interpolated to a regular 0.5-degree grid from the ECCO Version 4 revision 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g.,research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_obp_05deg_daily_v4r4b&quot;&gt;ECCO_L4_OBP_05DEG_DAILY_V4R4B&lt;/h4&gt;
This dataset contains daily-averaged ocean bottom pressure interpolated to a regular 0.5-degree grid from the ECCO Version 4 revision 4b (V4r4b) ocean and sea-ice state estimate. V4r4b is an errata for ECCO Version 4, Release 4 (V4r4). Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4b is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4b include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g.,research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4b covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_obp_llc0090grid_daily_v4r4&quot;&gt;ECCO_L4_OBP_LLC0090GRID_DAILY_V4R4&lt;/h4&gt;
This dataset provides daily-averaged ocean bottom pressure and model ocean bottom pressure anomaly on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_obp_llc0090grid_daily_v4r4b&quot;&gt;ECCO_L4_OBP_LLC0090GRID_DAILY_V4R4B&lt;/h4&gt;
This dataset provides daily-averaged ocean bottom pressure and model ocean bottom pressure anomaly on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4b (V4r4b) ocean and sea-ice state estimate. V4r4b is an errata for ECCO Version 4, Release 4 (V4r4). Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4b is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4b include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4b covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_obp_05deg_monthly_v4r4&quot;&gt;ECCO_L4_OBP_05DEG_MONTHLY_V4R4&lt;/h4&gt;
This dataset contains monthly-averaged ocean bottom pressure interpolated to a regular 0.5-degree grid from the ECCO Version 4 revision 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g.,research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_obp_05deg_monthly_v4r4b&quot;&gt;ECCO_L4_OBP_05DEG_MONTHLY_V4R4B&lt;/h4&gt;
This dataset contains monthly-averaged ocean bottom pressure interpolated to a regular 0.5-degree grid from the ECCO Version 4 revision 4b (V4r4b) ocean and sea-ice state estimate. V4r4b is an errata for ECCO Version 4, Release 4 (V4r4). Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4b is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4b include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g.,research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4b covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_obp_llc0090grid_monthly_v4r4&quot;&gt;ECCO_L4_OBP_LLC0090GRID_MONTHLY_V4R4&lt;/h4&gt;
This dataset provides monthly-averaged ocean bottom pressure and model ocean bottom pressure anomaly on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_obp_llc0090grid_monthly_v4r4b&quot;&gt;ECCO_L4_OBP_LLC0090GRID_MONTHLY_V4R4B&lt;/h4&gt;
This dataset provides monthly-averaged ocean bottom pressure and model ocean bottom pressure anomaly on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4b (V4r4b) ocean and sea-ice state estimate. V4r4b is an errata for ECCO Version 4, Release 4 (V4r4). Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4b is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4b include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4b covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_obp_llc0090grid_snapshot_v4r4&quot;&gt;ECCO_L4_OBP_LLC0090GRID_SNAPSHOT_V4R4&lt;/h4&gt;
This dataset provides instantaneous ocean bottom pressure and model ocean bottom pressure anomaly on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_dens_strat_press_05deg_daily_v4r4&quot;&gt;ECCO_L4_DENS_STRAT_PRESS_05DEG_DAILY_V4R4&lt;/h4&gt;
This dataset contains daily-averaged ocean density, stratification, and hydrostatic pressure interpolated to a regular 0.5-degree grid from the ECCO Version 4 revision 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g.,research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_dens_strat_press_llc0090grid_daily_v4r4&quot;&gt;ECCO_L4_DENS_STRAT_PRESS_LLC0090GRID_DAILY_V4R4&lt;/h4&gt;
This dataset provides daily-averaged ocean density, stratification, and hydrostatic pressure on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_dens_strat_press_05deg_monthly_v4r4&quot;&gt;ECCO_L4_DENS_STRAT_PRESS_05DEG_MONTHLY_V4R4&lt;/h4&gt;
This dataset contains monthly-averaged ocean density, stratification, and hydrostatic pressure interpolated to a regular 0.5-degree grid from the ECCO Version 4 revision 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g.,research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_dens_strat_press_llc0090grid_monthly_v4r4&quot;&gt;ECCO_L4_DENS_STRAT_PRESS_LLC0090GRID_MONTHLY_V4R4&lt;/h4&gt;
This dataset provides monthly-averaged ocean density, stratification, and hydrostatic pressure on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_mixed_layer_depth_05deg_daily_v4r4&quot;&gt;ECCO_L4_MIXED_LAYER_DEPTH_05DEG_DAILY_V4R4&lt;/h4&gt;
This dataset contains daily-averaged ocean mixed layer depth interpolated to a regular 0.5-degree grid from the ECCO Version 4 revision 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g.,research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_mixed_layer_depth_llc0090grid_daily_v4r4&quot;&gt;ECCO_L4_MIXED_LAYER_DEPTH_LLC0090GRID_DAILY_V4R4&lt;/h4&gt;
This dataset provides daily-averaged ocean mixed layer depth on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_mixed_layer_depth_05deg_monthly_v4r4&quot;&gt;ECCO_L4_MIXED_LAYER_DEPTH_05DEG_MONTHLY_V4R4&lt;/h4&gt;
This dataset contains monthly-averaged ocean mixed layer depth interpolated to a regular 0.5-degree grid from the ECCO Version 4 revision 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g.,research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_mixed_layer_depth_llc0090grid_monthly_v4r4&quot;&gt;ECCO_L4_MIXED_LAYER_DEPTH_LLC0090GRID_MONTHLY_V4R4&lt;/h4&gt;
This dataset provides monthly-averaged ocean mixed layer depth on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_temp_salinity_05deg_daily_v4r4&quot;&gt;ECCO_L4_TEMP_SALINITY_05DEG_DAILY_V4R4&lt;/h4&gt;
This dataset contains daily-averaged ocean potential temperature and salinity interpolated to a regular 0.5-degree grid from the ECCO Version 4 revision 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g.,research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_temp_salinity_llc0090grid_daily_v4r4&quot;&gt;ECCO_L4_TEMP_SALINITY_LLC0090GRID_DAILY_V4R4&lt;/h4&gt;
This dataset provides daily-averaged ocean potential temperature and salinity on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Ocean and sea-ice state estimates from the &amp;#39;Estimating the Circulation and Climate of the Ocean&amp;#39; are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric state, FLUX, and transports. ECCO V4r4 is a free-running solution of 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. V4r4 data constraints include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean potential temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_temp_salinity_05deg_monthly_v4r4&quot;&gt;ECCO_L4_TEMP_SALINITY_05DEG_MONTHLY_V4R4&lt;/h4&gt;
This dataset contains monthly-averaged ocean potential temperature and salinity interpolated to a regular 0.5-degree grid from the ECCO Version 4 revision 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g.,research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_temp_salinity_llc0090grid_monthly_v4r4&quot;&gt;ECCO_L4_TEMP_SALINITY_LLC0090GRID_MONTHLY_V4R4&lt;/h4&gt;
This dataset provides monthly-averaged ocean potential temperature and salinity on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Ocean and sea-ice state estimates from the &amp;#39;Estimating the Circulation and Climate of the Ocean&amp;#39; are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric state, FLUX, and transports. ECCO V4r4 is a free-running solution of 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. V4r4 data constraints include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean potential temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_temp_salinity_llc0090grid_snapshot_v4r4&quot;&gt;ECCO_L4_TEMP_SALINITY_LLC0090GRID_SNAPSHOT_V4R4&lt;/h4&gt;
This dataset provides instantaneous ocean potential temperature and salinity on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Ocean and sea-ice state estimates from the &amp;#39;Estimating the Circulation and Climate of the Ocean&amp;#39; are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric state, FLUX, and transports. ECCO V4r4 is a free-running solution of 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. V4r4 data constraints include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean potential temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_ocean_3d_momentum_tend_llc0090grid_daily_v4r4&quot;&gt;ECCO_L4_OCEAN_3D_MOMENTUM_TEND_LLC0090GRID_DAILY_V4R4&lt;/h4&gt;
This dataset provides daily-averaged ocean three-dimensional momentum tendency on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height and model sea level anomaly (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_ocean_3d_momentum_tend_llc0090grid_monthly_v4r4&quot;&gt;ECCO_L4_OCEAN_3D_MOMENTUM_TEND_LLC0090GRID_MONTHLY_V4R4&lt;/h4&gt;
This dataset provides monthly-averaged ocean three-dimensional momentum tendency on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height and model sea level anomaly (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_ocean_3d_temperature_flux_llc0090grid_daily_v4r4&quot;&gt;ECCO_L4_OCEAN_3D_TEMPERATURE_FLUX_LLC0090GRID_DAILY_V4R4&lt;/h4&gt;
This dataset provides daily-averaged ocean three-dimensional potential temperature fluxes on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height and model sea level anomaly (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_ocean_3d_temperature_flux_llc0090grid_monthly_v4r4&quot;&gt;ECCO_L4_OCEAN_3D_TEMPERATURE_FLUX_LLC0090GRID_MONTHLY_V4R4&lt;/h4&gt;
This dataset provides monthly-averaged ocean three-dimensional potential temperature fluxes on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height and model sea level anomaly (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_ocean_3d_salinity_flux_llc0090grid_daily_v4r4&quot;&gt;ECCO_L4_OCEAN_3D_SALINITY_FLUX_LLC0090GRID_DAILY_V4R4&lt;/h4&gt;
This dataset provides daily-averaged ocean three-dimensional salinity fluxes on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height and model sea level anomaly (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_ocean_3d_salinity_flux_llc0090grid_monthly_v4r4&quot;&gt;ECCO_L4_OCEAN_3D_SALINITY_FLUX_LLC0090GRID_MONTHLY_V4R4&lt;/h4&gt;
This dataset provides monthly-averaged ocean three-dimensional salinity fluxes on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height and model sea level anomaly (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_ocean_3d_volume_flux_llc0090grid_daily_v4r4&quot;&gt;ECCO_L4_OCEAN_3D_VOLUME_FLUX_LLC0090GRID_DAILY_V4R4&lt;/h4&gt;
This dataset provides daily-averaged ocean three-dimensional volume fluxes on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height and model sea level anomaly (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_ocean_3d_volume_flux_llc0090grid_monthly_v4r4&quot;&gt;ECCO_L4_OCEAN_3D_VOLUME_FLUX_LLC0090GRID_MONTHLY_V4R4&lt;/h4&gt;
This dataset provides monthly-averaged ocean three-dimensional volume fluxes on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height and model sea level anomaly (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_ocean_vel_05deg_daily_v4r4&quot;&gt;ECCO_L4_OCEAN_VEL_05DEG_DAILY_V4R4&lt;/h4&gt;
This dataset contains daily-averaged ocean velocity interpolated to a regular 0.5-degree grid from the ECCO Version 4 revision 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g.,research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_ocean_vel_llc0090grid_daily_v4r4&quot;&gt;ECCO_L4_OCEAN_VEL_LLC0090GRID_DAILY_V4R4&lt;/h4&gt;
This dataset provides daily-averaged ocean velocity on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_ocean_vel_05deg_monthly_v4r4&quot;&gt;ECCO_L4_OCEAN_VEL_05DEG_MONTHLY_V4R4&lt;/h4&gt;
This dataset contains monthly-averaged ocean velocity interpolated to a regular 0.5-degree grid from the ECCO Version 4 revision 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g.,research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_ocean_vel_llc0090grid_monthly_v4r4&quot;&gt;ECCO_L4_OCEAN_VEL_LLC0090GRID_MONTHLY_V4R4&lt;/h4&gt;
This dataset provides monthly-averaged ocean velocity on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_sbo_core_time_series_snapshot_v4r4&quot;&gt;ECCO_L4_SBO_CORE_TIME_SERIES_SNAPSHOT_V4R4&lt;/h4&gt;
This dataset provides instantaneous hourly SBO core products from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height and model sea level anomaly (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_sbo_core_time_series_snapshot_v4r4b&quot;&gt;ECCO_L4_SBO_CORE_TIME_SERIES_SNAPSHOT_V4R4B&lt;/h4&gt;
This dataset provides instantaneous hourly SBO core products from the ECCO Version 4 Release 4b (V4r4b) ocean and sea-ice state estimate. V4r4b is an errata for ECCO Version 4, Release 4 (V4r4). Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4b is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4b include sea surface height and model sea level anomaly (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4b covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_ssh_05deg_daily_v4r4&quot;&gt;ECCO_L4_SSH_05DEG_DAILY_V4R4&lt;/h4&gt;
This dataset contains daily-averaged dynamic sea surface height interpolated to a regular 0.5-degree grid from the ECCO Version 4 revision 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g.,research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_ssh_05deg_daily_v4r4b&quot;&gt;ECCO_L4_SSH_05DEG_DAILY_V4R4B&lt;/h4&gt;
This dataset contains daily-averaged dynamic sea surface height interpolated to a regular 0.5-degree grid from the ECCO Version 4 revision 4b (V4r4b) ocean and sea-ice state estimate. V4r4b is an errata for ECCO Version 4, Release 4 (V4r4). Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4b is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4b include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g.,research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4b covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_ssh_llc0090grid_daily_v4r4&quot;&gt;ECCO_L4_SSH_LLC0090GRID_DAILY_V4R4&lt;/h4&gt;
This dataset provides daily-averaged dynamic sea surface height and model sea level anomaly on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height and model sea level anomaly (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_ssh_llc0090grid_daily_v4r4b&quot;&gt;ECCO_L4_SSH_LLC0090GRID_DAILY_V4R4B&lt;/h4&gt;
This dataset provides daily-averaged dynamic sea surface height and model sea level anomaly on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4b (V4r4b) ocean and sea-ice state estimate. V4r4b is an errata for ECCO Version 4, Release 4 (V4r4). Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4b is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4b include sea surface height and model sea level anomaly (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4b covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_ssh_05deg_monthly_v4r4&quot;&gt;ECCO_L4_SSH_05DEG_MONTHLY_V4R4&lt;/h4&gt;
This dataset contains monthly-averaged dynamic sea surface height interpolated to a regular 0.5-degree grid from the ECCO Version 4 revision 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g.,research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_ssh_05deg_monthly_v4r4b&quot;&gt;ECCO_L4_SSH_05DEG_MONTHLY_V4R4B&lt;/h4&gt;
This dataset contains monthly-averaged dynamic sea surface height interpolated to a regular 0.5-degree grid from the ECCO Version 4b revision 4 (V4r4b) ocean and sea-ice state estimate. V4r4b is an errata for ECCO Version 4, Release 4 (V4r4). Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4b is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4b include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g.,research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4b covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_ssh_llc0090grid_monthly_v4r4&quot;&gt;ECCO_L4_SSH_LLC0090GRID_MONTHLY_V4R4&lt;/h4&gt;
This dataset provides monthly-averaged dynamic sea surface height and model sea level anomaly on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height and model sea level anomaly (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_ssh_llc0090grid_monthly_v4r4b&quot;&gt;ECCO_L4_SSH_LLC0090GRID_MONTHLY_V4R4B&lt;/h4&gt;
This dataset provides monthly-averaged dynamic sea surface height and model sea level anomaly on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4b (V4r4b) ocean and sea-ice state estimate. V4r4b is an errata for ECCO Version 4, Release 4 (V4r4). Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4b is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4b include sea surface height and model sea level anomaly (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4b covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_ssh_llc0090grid_snapshot_v4r4&quot;&gt;ECCO_L4_SSH_LLC0090GRID_SNAPSHOT_V4R4&lt;/h4&gt;
This dataset provides instantaneous dynamic sea surface height and model sea level anomaly on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include dynamic sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; dynamic sea surface temperature (SST) from satellite radiometers [AVHRR], dynamic sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_sea_ice_conc_thickness_05deg_daily_v4r4&quot;&gt;ECCO_L4_SEA_ICE_CONC_THICKNESS_05DEG_DAILY_V4R4&lt;/h4&gt;
This dataset contains daily-averaged sea-ice and snow concentration and thickness interpolated to a regular 0.5-degree grid from the ECCO Version 4 revision 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g.,research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_sea_ice_conc_thickness_llc0090grid_daily_v4r4&quot;&gt;ECCO_L4_SEA_ICE_CONC_THICKNESS_LLC0090GRID_DAILY_V4R4&lt;/h4&gt;
This dataset provides daily-averaged sea-ice and snow concentration, thickness, and pressure loading on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_sea_ice_conc_thickness_05deg_monthly_v4r4&quot;&gt;ECCO_L4_SEA_ICE_CONC_THICKNESS_05DEG_MONTHLY_V4R4&lt;/h4&gt;
This dataset contains monthly-averaged sea-ice and snow concentration and thickness interpolated to a regular 0.5-degree grid from the ECCO Version 4 revision 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g.,research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_sea_ice_conc_thickness_llc0090grid_monthly_v4r4&quot;&gt;ECCO_L4_SEA_ICE_CONC_THICKNESS_LLC0090GRID_MONTHLY_V4R4&lt;/h4&gt;
This dataset provides monthly-averaged sea-ice and snow concentration, thickness, and pressure loading on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_sea_ice_conc_thickness_llc0090grid_snapshot_v4r4&quot;&gt;ECCO_L4_SEA_ICE_CONC_THICKNESS_LLC0090GRID_SNAPSHOT_V4R4&lt;/h4&gt;
This dataset provides instantaneous sea-ice and snow concentration, thickness, and pressure loading on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_sea_ice_horiz_volume_flux_llc0090grid_daily_v4r4&quot;&gt;ECCO_L4_SEA_ICE_HORIZ_VOLUME_FLUX_LLC0090GRID_DAILY_V4R4&lt;/h4&gt;
This dataset provides daily-averaged sea-ice and snow horizontal volume fluxes on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height and model sea level anomaly (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_sea_ice_horiz_volume_flux_llc0090grid_monthly_v4r4&quot;&gt;ECCO_L4_SEA_ICE_HORIZ_VOLUME_FLUX_LLC0090GRID_MONTHLY_V4R4&lt;/h4&gt;
This dataset provides monthly-averaged sea-ice and snow horizontal volume fluxes on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height and model sea level anomaly (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_sea_ice_salt_plume_flux_llc0090grid_daily_v4r4&quot;&gt;ECCO_L4_SEA_ICE_SALT_PLUME_FLUX_LLC0090GRID_DAILY_V4R4&lt;/h4&gt;
This dataset provides daily-averaged sea-ice salt plume fluxes on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height and model sea level anomaly (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_sea_ice_salt_plume_flux_llc0090grid_monthly_v4r4&quot;&gt;ECCO_L4_SEA_ICE_SALT_PLUME_FLUX_LLC0090GRID_MONTHLY_V4R4&lt;/h4&gt;
This dataset provides monthly-averaged sea-ice salt plume fluxes on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height and model sea level anomaly (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_sea_ice_velocity_05deg_daily_v4r4&quot;&gt;ECCO_L4_SEA_ICE_VELOCITY_05DEG_DAILY_V4R4&lt;/h4&gt;
This dataset contains daily-averaged sea-ice velocity interpolated to a regular 0.5-degree grid from the ECCO Version 4 revision 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g.,research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_sea_ice_velocity_llc0090grid_daily_v4r4&quot;&gt;ECCO_L4_SEA_ICE_VELOCITY_LLC0090GRID_DAILY_V4R4&lt;/h4&gt;
This dataset provides daily-averaged sea-ice velocity on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_sea_ice_velocity_05deg_monthly_v4r4&quot;&gt;ECCO_L4_SEA_ICE_VELOCITY_05DEG_MONTHLY_V4R4&lt;/h4&gt;
This dataset contains monthly-averaged sea-ice velocity interpolated to a regular 0.5-degree grid from the ECCO Version 4 revision 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g.,research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_sea_ice_velocity_llc0090grid_monthly_v4r4&quot;&gt;ECCO_L4_SEA_ICE_VELOCITY_LLC0090GRID_MONTHLY_V4R4&lt;/h4&gt;
This dataset provides monthly-averaged sea-ice velocity on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecco_l4_sea_ice_velocity_llc0090grid_snapshot_v4r4&quot;&gt;ECCO_L4_SEA_ICE_VELOCITY_LLC0090GRID_SNAPSHOT_V4R4&lt;/h4&gt;
This dataset provides instantaneous sea-ice velocity on the native Lat-Lon-Cap 90 (LLC90) model grid from the ECCO Version 4 Release 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g., research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://archive.podaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA ECOSTRESS Project</title>
      <link>https://registry.opendata.aws/nasa-ecostress</link>
      <guid>https://registry.opendata.aws/nasa-ecostress</guid>
      <description>The ECO1BRAD Version 1 data product was decommissioned on May 21, 2025. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/ECOSTRESS/ECO_L1CT_RAD.002&quot;&gt;ECO_L1CT_RAD&lt;/a&gt; Version 2 and &lt;a href&#x3D;&quot;https://doi.org/10.5067/ECOSTRESS/ECO_L1CG_RAD.002&quot;&gt;ECO_L1CG_RAD&lt;/a&gt; Version 2 data products. The ECOsystem Spaceborne Thermal Radiometer Experiment on Space Station (ECOSTRESS) mission measures the temperature of plants to better understand how much water plants need and how they respond to stress. ECOSTRESS is attached to the International Space Station (ISS) and collects data globally between 52 degrees N and 52 degrees S latitudes. . The ECO1BRAD Version 1 data product provides at-sensor calibrated radiance values retrieved for five thermal infrared (TIR) bands operating between 8 and 12.5 microns. Additionally, the digital numbers (DN) for the shortwave infrared (SWIR) band are provided. The TIR bands are spatially co-registered to produce a variable spatial resolution between 70 meters (m) to 90 m at the edge of the swath. The ECO1BRAD data product is provided as swath data and does not contain geolocation information. The corresponding &lt;a href&#x3D;&quot;https://doi.org/10.5067/ECOSTRESS/ECO1BGEO.001&quot;&gt;ECO1BGEO&lt;/a&gt; data product is required to georeference the ECO1BRAD data product. The geographic coverage of acquisitions for the ECO1BRAD Version 1 data product extends to areas outside of those indicated on the coverage map. However, corresponding higher-level products over these areas are not available at this time. The ECO1BRAD Version 1 data product contains variables of radiance values for the five TIR bands, DN values for the SWIR band, associated data quality indicators, and ancillary data. Known Issues: Cannot perform spatial query on ECO1BRAD in NASA Earthdata Search: ECO1BRAD does not contain spatial attributes, so granules cannot be searched by geographic location. Users should search for ECO1BRAD data products by orbit number instead. * Data acquisition gap: ECOSTRESS was launched on June 29, 2018, and moved to autonomous science operations on August 20, 2018, following a successful in-orbit checkout period. On September 29, 2018, ECOSTRESS experienced an anomaly with its primary mass storage unit (MSU). ECOSTRESS has a primary and secondary MSU (A and B). On December 5, 2018, the instrument was switched to the secondary MSU and science operations resumed. On March 14, 2019, the secondary MSU experienced a similar anomaly temporarily halting science acquisitions. On May 15, 2019, a new data acquisition approach was implemented and science acquisitions resumed. To optimize the new acquisition approach TIR bands 2, 4 and 5 are being downloaded. The data products are as previously, except the bands not downloaded contain fill values (L1 radiance and L2 emissivity). This approach was implemented from May 15, 2019, through April 28, 2023. * Data acquisition gap: From February 8 to February 16, 2020, an ECOSTRESS instrument issue resulted in a data anomaly that created striping in band 4 (10.5 micron). These data products have been reprocessed and are available for download. No ECOSTRESS data were acquired on February 17, 2020, due to the instrument being in SAFEHOLD. Data acquired following the anomaly have not been affected. * Missing scan data/striping features: During testing, an instrument artifact was encountered in ECOSTRESS bands 1 and 5, resulting in missing values. A machine learning algorithm has been applied to interpolate missing values. For more information on the missing scan filling techniques and outcomes, see Section 3.3.2 of the User Guide. * Scan overlap: An overlap between ECOSTRESS scans results in a clear line overlap and repeating data. Additional information is available in Section 3.2 of the User Guide. * Scan flipping: Improvements to the visualization of the data to compensate for instrument orientation are discussed in Section 3.4 of the User Guide. * Cold bias: ECOSTRESS Level-1 Radiance data shows high correlation with in-situ ground measurements (R2 &#x3D; 0.99 in all bands). Currently, ECOSTRESS has a cold bias of approximately 0.7 Kelvin (K), which will be corrected through calibration in future data releases. * Data acquisition: ECOSTRESS has now successfully returned to 5-band mode after being in 3-band mode since 2019. This feature was successfully enabled following a Data Processing Unit firmware update (version 4.1) to the payload on April 28, 2023. To better balance contiguous science data scene variables, 3-band collection is currently being interleaved with 5-band acquisitions over the orbital day/night periods.
&lt;br&gt;&lt;h4 id&#x3D;&quot;eco1batt&quot;&gt;ECO1BATT&lt;/h4&gt;
The ECO1BATT Version 1 data product was decommissioned on April 22, 2025. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/ECOSTRESS/ECO_L1B_ATT.002&quot;&gt;ECO_L1B_ATT&lt;/a&gt; Version 2 data product. The ECOsystem Spaceborne Thermal Radiometer Experiment on Space Station (ECOSTRESS) mission measures the temperature of plants to better understand how much water plants need and how they respond to stress. ECOSTRESS is attached to the International Space Station (ISS) and collects data globally between 52 degrees N and 52 degrees S latitudes. The ECO1BATT Version 1 data product provides both corrected and uncorrected attitude quaternions and spacecraft ephemeris data obtained from the ISS. The data are provided in 1 second intervals by the ISS, and each product file contains vectors from the duration of the orbit. The time elements are copied from the ISS raw data. The ECO1BATT Version 1 data product contains variables of corrected and uncorrected attitude quaternions, spacecraft ephemeris data including Earth-centered inertial (ECI) position and velocity, and associated time elements. Known Issues: Cannot perform spatial query on ECO1BATT in NASA Earthdata Search: ECO1BATT does not contain spatial attributes, so granules cannot be searched by geographic location. Users should search for ECO1BATT data products by orbit number instead. * Data acquisition gap: ECOSTRESS was launched on June 29, 2018, and moved to autonomous science operations on August 20, 2018, following a successful in-orbit checkout period. On September 29, 2018, ECOSTRESS experienced an anomaly with its primary mass storage unit (MSU). ECOSTRESS has a primary and secondary MSU (A and B). On December 5, 2018, the instrument was switched to the secondary MSU and science operations resumed. On March 14, 2019, the secondary MSU experienced a similar anomaly temporarily halting science acquisitions. On May 15, 2019, a new data acquisition approach was implemented and science acquisitions resumed. To optimize the new acquisition approach TIR bands 2, 4 and 5 are being downloaded. The data products are as previously, except the bands not downloaded contain fill values (L1 radiance and L2 emissivity). This approach was implemented from May 15, 2019, through April 28, 2023. * Data acquisition gap: From February 8 to February 16, 2020, an ECOSTRESS instrument issue resulted in a data anomaly that created striping in band 4 (10.5 micron). These data products have been reprocessed and are available for download. No ECOSTRESS data were acquired on February 17, 2020, due to the instrument being in SAFEHOLD. Data acquired following the anomaly have not been affected. * Data acquisition: ECOSTRESS has now successfully returned to 5-band mode after being in 3-band mode since 2019. This feature was successfully enabled following a Data Processing Unit firmware update (version 4.1) to the payload on April 28, 2023. To better balance contiguous science data scene variables, 3-band collection is currently being interleaved with 5-band acquisitions over the orbital day/night periods.
&lt;br&gt;&lt;h4 id&#x3D;&quot;eco2cld&quot;&gt;ECO2CLD&lt;/h4&gt;
The ECO2CLD Version 1 data product was decommissioned on May 21, 2025. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/ECOSTRESS/ECO_L2_CLOUD.002&quot;&gt;ECO_L2_CLOUD&lt;/a&gt; Version 2 and &lt;a href&#x3D;&quot;https://doi.org/10.5067/ECOSTRESS/ECO_L2G_CLOUD.002&quot;&gt;ECO_L2G_CLOUD&lt;/a&gt; Version 2 data products. The ECOsystem Spaceborne Thermal Radiometer Experiment on Space Station (ECOSTRESS) mission measures the temperature of plants to better understand how much water plants need and how they respond to stress. ECOSTRESS is attached to the International Space Station (ISS) and collects data globally between 52 degrees N and 52 degrees S latitudes. The ECO2CLD Version 1 data product provides a cloud mask that can be used to determine cloud cover for the ECO1BRAD, ECO2LSTE, ECO3ETPTJPL, ECO4ESIPTJPL, and ECO4WUE data products. The ECOSTRESS Level 2 cloud product is derived using the five calibrated thermal bands in a multispectral cloud-conservative thresholding approach. The details of the algorithm are provided in the Algorithm Theoretical Basis Document (ATBD). The corresponding &lt;a href&#x3D;&quot;https://doi.org/10.5067/ECOSTRESS/ECO1BGEO.001&quot;&gt;ECO1BGEO&lt;/a&gt; data product is required to georeference the ECO2CLD data product. The ECO2CLD Version 1 data product contains a single cloud mask layer. Information on how to interpret the bit fields in the cloud mask is provided in section 3.1 of the User Guide. Known Issues: Data acquisition gap: ECOSTRESS was launched on June 29, 2018, and moved to autonomous science operations on August 20, 2018, following a successful in-orbit checkout period. On September 29, 2018, ECOSTRESS experienced an anomaly with its primary mass storage unit (MSU). ECOSTRESS has a primary and secondary MSU (A and B). On December 5, 2018, the instrument was switched to the secondary MSU and science operations resumed. On March 14, 2019, the secondary MSU experienced a similar anomaly temporarily halting science acquisitions. On May 15, 2019, a new data acquisition approach was implemented and science acquisitions resumed. To optimize the new acquisition approach TIR bands 2, 4, and 5 are being downloaded. The data products are as previously, except the bands not downloaded contain fill values (L1 radiance and L2 emissivity). This approach was implemented from May 15, 2019, through April 28, 2023. * Data acquisition gap: From February 8 to February 16, 2020, an ECOSTRESS instrument issue resulted in a data anomaly that created striping in band 4 (10.5 micron). These data products have been reprocessed and are available for download. No ECOSTRESS data were acquired on February 17, 2020, due to the instrument being in SAFEHOLD. Data acquired following the anomaly have not been affected. * Data acquisition: ECOSTRESS has now successfully returned to 5-band mode after being in 3-band mode since 2019. This feature was successfully enabled following a Data Processing Unit firmware update (version 4.1) to the payload on April 28, 2023. To better balance contiguous science data scene variables, 3-band collection is currently being interleaved with 5-band acquisitions over the orbital day/night periods.
&lt;br&gt;&lt;h4 id&#x3D;&quot;eco4esialexi&quot;&gt;ECO4ESIALEXI&lt;/h4&gt;
The ECO4ESIALEXI Version 1 data product was decommissioned on January 30, 2026. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/ECOSTRESS/ECO_L4G_ESI_ALEXI.002&quot;&gt;ECO_L4G_ESI_ALEXI&lt;/a&gt; and &lt;a href&#x3D;&quot;https://doi.org/10.5067/ECOSTRESS/ECO_L4T_ESI_ALEXI.002&quot;&gt;ECO_L4T_ESI_ALEXI&lt;/a&gt; Version 2 data product(s). The ECOsystem Spaceborne Thermal Radiometer Experiment on Space Station (ECOSTRESS) mission measures the temperature of plants to better understand how much water plants need and how they respond to stress. ECOSTRESS is attached to the International Space Station (ISS) and collects data globally between 52 degrees N and 52 degrees S latitudes. The NASA Jet Propulsion Laboratory (JPL) ECO4ESIALEXI Version 1 data product provides the Evaporative Stress Index (ESI), which is computed from clear-sky estimates of the relative daily evapotranspiration (ET) fraction: ESI &#x3D; ET/ETo, where ET is ETdaily from the ECOSTRESS Level 3 product and ETo is the reference ET. A description of the major components of the ECOSTRESS algorithm implemented in Version 1 of the Atmosphere Land Exchange Inverse (ALEXI) Disaggregation algorithm (DisALEXI) ESI code is provided in the Algorithm Theoretical Basis Document (ATBD). ESI applications include indicating agricultural drought and observing vegetation stress. ECO4ESIALEXI is available for CONUS at 70-meter (m) pixel resolution. The ECO4ESIALEXI Version 1 data product contains variables of daily evaporative stress index, evaporative stress index uncertainty, and associated quality flags. A low-resolution browse is also available showing daily ESI as a stretched image with a color ramp in JPEG format. Known Issues: Data acquisition gaps: ECOSTRESS was launched on June 29, 2018, and moved to autonomous science operations on August 20, 2018, following a successful in-orbit checkout period. On September 29, 2018, ECOSTRESS experienced an anomaly with its primary mass storage unit (MSU). ECOSTRESS has a primary and secondary MSU (A and B). On December 5, 2018, the instrument was switched to the secondary MSU and science operations resumed. On March 14, 2019, the secondary MSU experienced a similar anomaly, temporarily halting science acquisitions. On May 15, 2019, a new data acquisition approach was implemented, and science acquisitions resumed. To optimize the new acquisition approach, only TIR bands 2, 4, and 5 are being downloaded. The data products are the same as before, but the bands not downloaded contain fill values (L1 radiance and L2 emissivity). This approach was implemented from May 15, 2019, through April 28, 2023. * Data acquisition gap: From February 8 to February 16, 2020, an ECOSTRESS instrument issue resulted in a data anomaly that created striping in band 4 (10.5 micron). These data products have been reprocessed and are available for download. No ECOSTRESS data were acquired on February 17, 2020, due to the instrument being in SAFEHOLD. Data acquired following the anomaly have not been affected. * Data acquisition: ECOSTRESS has now successfully returned to 5-band mode after being in 3-band mode since 2019. This feature was successfully enabled following a Data Processing Unit firmware update (version 4.1) to the payload on April 28, 2023. To better balance contiguous science data scene variables, 3-band collection is currently being interleaved with 5-band acquisitions over the orbital day/night periods.
&lt;br&gt;&lt;h4 id&#x3D;&quot;eco4esialexiu&quot;&gt;ECO4ESIALEXIU&lt;/h4&gt;
The ECOsystem Spaceborne Thermal Radiometer Experiment on Space Station (ECOSTRESS) mission measures the temperature of plants to better understand how much water plants need and how they respond to stress. ECOSTRESS is attached to the International Space Station (ISS) and collects data globally between 52 degrees N and 52 degrees S latitudes. The United States Department of Agriculture (USDA) ECO4ESIALEXIU Version 1 data product provides the Evaporative Stress Index (ESI), which is computed from clear-sky estimates of the relative daily evapotranspiration (ET) fraction: ESI &#x3D; ET/ETo, where ET is ETdaily from the ECOSTRESS Level 3 product and ETo is the reference ET. A description of the major components of the ECOSTRESS algorithm implemented in Version 1 of the Atmosphere Land Exchange Inverse (ALEXI) Disaggregation algorithm (DisALEXI) ESI code is provided in the Algorithm Theoretical Basis Document (ATBD). ESI applications include indicating agricultural drought and observing vegetation stress. The dis-ALEXI USDA ESI product is generated on a UTM grid at a spatial resolution of 30 meters. The ECO4ESIALEXIU Version 1 data product contains variables of daily evaporative stress index, evaporative stress index uncertainty, and associated quality flags. A low-resolution browse is also available showing daily ESI as a stretched image with a color ramp in JPEG format. Known Issues: Data acquisition gaps: ECOSTRESS was launched on June 29, 2018, and moved to autonomous science operations on August 20, 2018, following a successful in-orbit checkout period. On September 29, 2018, ECOSTRESS experienced an anomaly with its primary mass storage unit (MSU). ECOSTRESS has a primary and secondary MSU (A and B). On December 5, 2018, the instrument was switched to the secondary MSU and science operations resumed. On March 14, 2019, the secondary MSU experienced a similar anomaly temporarily halting science acquisitions. On May 15, 2019, a new data acquisition approach was implemented and science acquisitions resumed. To optimize the new acquisition approach TIR bands 2, 4 and 5 are being downloaded. The data products are as previously, except the bands not downloaded contain fill values (L1 radiance and L2 emissivity). This approach was implemented from May 15, 2019, through April 28, 2023. * Data acquisition gap: From February 8 to February 16, 2020, an ECOSTRESS instrument issue resulted in a data anomaly that created striping in band 4 (10.5 micron). These data products have been reprocessed and are available for download. No ECOSTRESS data were acquired on February 17, 2020, due to the instrument being in SAFEHOLD. Data acquired following the anomaly have not been affected. * Data acquisition: ECOSTRESS has now successfully returned to 5-band mode after being in 3-band mode since 2019. This feature was successfully enabled following a Data Processing Unit firmware update (version 4.1) to the payload on April 28, 2023. To better balance contiguous science data scene variables, 3-band collection is currently being interleaved with 5-band acquisitions over the orbital day/night periods.
&lt;br&gt;&lt;h4 id&#x3D;&quot;eco4esiptjpl&quot;&gt;ECO4ESIPTJPL&lt;/h4&gt;
The ECO4ESIPTJPL Version 1 data product was decommissioned on September 30, 2025. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/ECOSTRESS/ECO_L4T_ESI.002&quot;&gt;ECO_L4T_ESI&lt;/a&gt; and &lt;a href&#x3D;&quot;https://doi.org/10.5067/ECOSTRESS/ECO_L4G_ESI.002&quot;&gt;ECO_L4G_ESI&lt;/a&gt; Version 2 data products. The ECOsystem Spaceborne Thermal Radiometer Experiment on Space Station (ECOSTRESS) mission measures the temperature of plants to better understand how much water plants need and how they respond to stress. ECOSTRESS is attached to the International Space Station (ISS) and collects data globally between 52 degrees N and 52 degrees S latitudes. The ECO4ESIPTJPL Version 1 data product provides Evaporative Stress Index (ESI) data generated according to the Priestley-Taylor Jet Propulsion Laboratory (PT-JPL) algorithm described in the ECOSTRESS Level 4 (ESI_PT-JPL) Algorithm Theoretical Basis Document (ATBD). The ESI product is derived from the ratio of the Level 3 actual evapotranspiration (ET) to potential ET (PET) calculated as part of the algorithm. The ESI is an indicator of potential drought and plant water stress emphasizing areas of sub-optimal plant productivity. The ECO4ESIPTJPL Version 1 data product contains variables of ESI and PET. Known Issues: Data acquisition gaps: ECOSTRESS was launched on June 29, 2018, and moved to autonomous science operations on August 20, 2018, following a successful in-orbit checkout period. On September 29, 2018, ECOSTRESS experienced an anomaly with its primary mass storage unit (MSU). ECOSTRESS has a primary and secondary MSU (A and B). On December 5, 2018, the instrument was switched to the secondary MSU and science operations resumed. On March 14, 2019, the secondary MSU experienced a similar anomaly temporarily halting science acquisitions. On May 15, 2019, a new data acquisition approach was implemented and science acquisitions resumed. To optimize the new acquisition approach TIR bands 2, 4 and 5 are being downloaded. The data products are as previously, except the bands not downloaded contain fill values (L1 radiance and L2 emissivity). This approach was implemented from May 15, 2019, through April 28, 2023. * Data acquisition gap: From February 8 to February 16, 2020, an ECOSTRESS instrument issue resulted in a data anomaly that created striping in band 4 (10.5 micron). These data products have been reprocessed and are available for download. No ECOSTRESS data were acquired on February 17, 2020, due to the instrument being in SAFEHOLD. Data acquired following the anomaly have not been affected. * Data acquisition: ECOSTRESS has now successfully returned to 5-band mode after being in 3-band mode since 2019. This feature was successfully enabled following a Data Processing Unit firmware update (version 4.1) to the payload on April 28, 2023. To better balance contiguous science data scene variables, 3-band collection is currently being interleaved with 5-band acquisitions over the orbital day/night periods.
&lt;br&gt;&lt;h4 id&#x3D;&quot;eco3etalexi&quot;&gt;ECO3ETALEXI&lt;/h4&gt;
The ECO3ETALEXI Version 1 data product was decommissioned on January 30th, 2026. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/ECOSTRESS/ECO_L3T_ET_ALEXI.002&quot;&gt;ECO_L3T_ET_ALEXI&lt;/a&gt; and &lt;a href&#x3D;&quot;https://doi.org/10.5067/ECOSTRESS/ECO_L3G_ET_ALEXI.002&quot;&gt;ECO_L3G_ET_ALEXI&lt;/a&gt; Version 2 data product(s). The ECOsystem Spaceborne Thermal Radiometer Experiment on Space Station (ECOSTRESS) mission measures the temperature of plants to better understand how much water plants need and how they respond to stress. ECOSTRESS is attached to the International Space Station (ISS) and collects data globally between 52 degrees N and 52 degrees S latitudes. The NASA Jet Propulsion Laboratory (JPL) ECO3ETALEXI Version 1 data product provides estimates of daily evapotranspiration (ET) using the ECOSTRESS Level 2 (L2) land surface temperature and emissivity (LST&amp;amp;E) product, along with ancillary meteorological data and remotely sensed vegetation cover information. The ECO3ETALEXI data product is derived using a physics-based surface energy balance (SEB) algorithm, the Atmosphere Land Exchange Inverse (ALEXI) Disaggregation algorithm (DisALEXI). Described in the Algorithm Theoretical Basis Document (ATBD), DisALEXI is based on spatial disaggregation of regional-scale fluxes from the ALEXI SEB model. There are many approaches for spatially mapping ET; however, SEB methods are favored for remote sensing retrievals based on land-surface temperature. ALEXI was initially developed for managed landscapes and has now been evaluated in comparison with micrometeorological flux tower observations over crop, forest, grassland, wetland, and semiarid desert sites. Applications include crop water use, crop phenology monitoring, and drought early warning or water stress detection. ECO3ETALEXI is available for CONUS at 70-meter (m) pixel resolution. The ECO3ETALEXI Version 1 data product contains variables of daily ET, ET uncertainty, and associated quality flags. A low-resolution browse is also available showing daily ET as a stretched image with a color ramp in JPEG format. Known Issues: Data acquisition gaps: ECOSTRESS was launched on June 29, 2018, and moved to autonomous science operations on August 20, 2018, following a successful in-orbit checkout period. On September 29, 2018, ECOSTRESS experienced an anomaly with its primary mass storage unit (MSU). ECOSTRESS has a primary and secondary MSU (A and B). On December 5, 2018, the instrument was switched to the secondary MSU and science operations resumed. On March 14, 2019, the secondary MSU experienced a similar anomaly, temporarily halting science acquisitions. On May 15, 2019, a new data acquisition approach was implemented, and science acquisitions resumed. To optimize the new acquisition approach, only TIR bands 2, 4, and 5 are being downloaded. The data products are the same as before, but the bands not downloaded contain fill values (L1 radiance and L2 emissivity). This approach was implemented from May 15, 2019, through April 28, 2023. * Data acquisition gap: From February 8 to February 16, 2020, an ECOSTRESS instrument issue resulted in a data anomaly that created striping in band 4 (10.5 micron). These data products have been reprocessed and are available for download. No ECOSTRESS data were acquired on February 17, 2020, due to the instrument being in SAFEHOLD. Data acquired following the anomaly have not been affected. * Data acquisition: ECOSTRESS has now successfully returned to 5-band mode after being in 3-band mode since 2019. This feature was successfully enabled following a Data Processing Unit firmware update (version 4.1) to the payload on April 28, 2023. To better balance contiguous science data scene variables, 3-band collection is currently being interleaved with 5-band acquisitions over the orbital day/night periods.
&lt;br&gt;&lt;h4 id&#x3D;&quot;eco3etptjpl&quot;&gt;ECO3ETPTJPL&lt;/h4&gt;
ECO3ETPTJPL Version 1 was deprecated on September 30, 2025. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/ECOSTRESS/ECO_L3G_JET.002&quot;&gt;ECO_L3G_JET&lt;/a&gt; and &lt;a href&#x3D;&quot;https://doi.org/10.5067/ECOSTRESS/ECO_L3T_JET.002&quot;&gt;ECO_L3T_JET&lt;/a&gt; Version 2 data products. The ECOsystem Spaceborne Thermal Radiometer Experiment on Space Station (ECOSTRESS) mission measures the temperature of plants to better understand how much water plants need and how they respond to stress. ECOSTRESS is attached to the International Space Station (ISS) and collects data globally between 52 degrees N and 52 degrees S latitudes. ECO3ETPTJPL Version 1 is a Level 3 (L3) product that provides evapotranspiration (ET) generated from data acquired by the ECOSTRESS radiometer instrument according to the Priestly-Taylor Jet Propulsion Laboratory (PT-JPL) algorithm described in the Algorithm Theoretical Basis Document (ATBD). The ET product is generated from the Level 2 data products for surface temperature and emissivity, the Level 1 geolocation information, and a significant number of ancillary data inputs from other sources. ET is set by various controls, including radiative and atmospheric demand, and environmental sensitivity, productivity, vegetation physiology, and phenology. PT-JPL is best utilized for natural ecosystems. The L3 ET product is used for creating the Level 4 products, Evaporative Stress Index (ESI) and Water Use Efficiency (WUE). The ECO3ETPTJPL Version 1 data product contains variables of instantaneous ET, daily ET, canopy transpiration, soil evaporation, ET uncertainty, and interception evaporation. Known Issues: Data acquisition gaps: ECOSTRESS was launched on June 29, 2018, and moved to autonomous science operations on August 20, 2018, following a successful in-orbit checkout period. On September 29, 2018, ECOSTRESS experienced an anomaly with its primary mass storage unit (MSU). ECOSTRESS has a primary and secondary MSU (A and B). On December 5, 2018, the instrument was switched to the secondary MSU and science operations resumed. On March 14, 2019, the secondary MSU experienced a similar anomaly temporarily halting science acquisitions. On May 15, 2019, a new data acquisition approach was implemented and science acquisitions resumed. To optimize the new acquisition approach TIR bands 2, 4 and 5 are being downloaded. The data products are as previously, except the bands not downloaded contain fill values (L1 radiance and L2 emissivity). This approach was implemented from May 15, 2019, through April 28, 2023. * Data acquisition gap: From February 8 to February 16, 2020, an ECOSTRESS instrument issue resulted in a data anomaly that created striping in band 4 (10.5 micron). These data products have been reprocessed and are available for download. No ECOSTRESS data were acquired on February 17, 2020, due to the instrument being in SAFEHOLD. Data acquired following the anomaly have not been affected. * Data acquisition: ECOSTRESS has now successfully returned to 5-band mode after being in 3-band mode since 2019. This feature was successfully enabled following a Data Processing Unit firmware update (version 4.1) to the payload on April 28, 2023. To better balance contiguous science data scene variables, 3-band collection is currently being interleaved with 5-band acquisitions over the orbital day/night periods.
&lt;br&gt;&lt;h4 id&#x3D;&quot;eco1bgeo&quot;&gt;ECO1BGEO&lt;/h4&gt;
The ECO1BGEO Version 1 data product was decommissioned on January 30, 2026. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/ECOSTRESS/ECO_L1B_GEO.002&quot;&gt;ECO_L1B_GEO&lt;/a&gt; Version 2 data product. The ECOsystem Spaceborne Thermal Radiometer Experiment on Space Station (ECOSTRESS) mission measures the temperature of plants to better understand how much water plants need and how they respond to stress. ECOSTRESS is attached to the International Space Station (ISS) and collects data globally between 52 degrees N and 52 degrees S latitudes. The ECO1BGEO Version 1 data product provides the geolocation information for the radiance values retrieved in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/ecostress/eco1brad.001&quot;&gt;ECO1BRAD&lt;/a&gt; Version 1 data product. The ECO1BGEO data product should be used to georeference the ECO1BRAD, ECO2CLD, ECO2LSTE, ECO3ANCQA, ECO3ETPTJPL, ECO4ESIPTJPL, and ECO4WUE data products. The geolocation processing corrects the ISS-reported ephemeris and attitude data by image matching with a global ortho-base derived from Landsat data, and then assigns latitude and longitude values to each of the Level 1 radiance pixels. When image matching is successful, the data are geolocated to better than 50 meter (m) accuracy. The ECO1BGEO data product is provided as swath data. The ECO1BGEO data product contains data variables for latitude and longitude values, solar and view geometry information, surface height, and the fraction of pixel on land versus water. Known Issues: Geolocation accuracy: In cases where scenes were not successfully matched with the ortho-base, the geolocation error is significantly larger, with the worst-case geolocation error for uncorrected data being at 7 kilometers (km). Within the metadata of the ECO1BGEO file, if the field &amp;quot;L1GEOMetadata/OrbitCorrectionPerformed&amp;quot; is &amp;quot;True,&amp;quot; the data was corrected, and geolocation accuracy should be better than 50 m. If this is &amp;quot;False,&amp;quot; then the data was processed without correcting the geolocation and will have up to 7 km geolocation error. * Data acquisition gap: ECOSTRESS was launched on June 29, 2018, and moved to autonomous science operations on August 20, 2018, following a successful in-orbit checkout period. On September 29, 2018, ECOSTRESS experienced an anomaly with its primary mass storage unit (MSU). ECOSTRESS has a primary and secondary MSU (A and B). On December 5, 2018, the instrument was switched to the secondary MSU and science operations resumed. On March 14, 2019, the secondary MSU experienced a similar anomaly temporarily halting science acquisitions. On May 15, 2019, a new data acquisition approach was implemented and science acquisitions resumed. To optimize the new acquisition approach TIR bands 2, 4 and 5 are being downloaded. The data products are as previously, except the bands not downloaded contain fill values (L1 radiance and L2 emissivity). This approach was implemented from May 15, 2019, through April 28, 2023. * Data acquisition gap: From February 8 to February 16, 2020, an ECOSTRESS instrument issue resulted in a data anomaly that created striping in band 4 (10.5 micron). These data products have been reprocessed and are available for download. No ECOSTRESS data were acquired on February 17, 2020, due to the instrument being in SAFEHOLD. Data acquired following the anomaly have not been affected. * Data acquisition: ECOSTRESS has now successfully returned to 5-band mode after being in 3-band mode since 2019. This feature was successfully enabled following a Data Processing Unit firmware update (version 4.1) to the payload on April 28, 2023. To better balance contiguous science data scene variables, 3-band collection is currently being interleaved with 5-band acquisitions over the orbital day/night periods.
&lt;br&gt;&lt;h4 id&#x3D;&quot;eco_l2g_cloud&quot;&gt;ECO_L2G_CLOUD&lt;/h4&gt;
The ECOsystem Spaceborne Thermal Radiometer Experiment on Space Station (ECOSTRESS) mission measures the temperature of plants to better understand how much water plants need and how they respond to stress. ECOSTRESS is attached to the International Space Station (ISS) and collects data globally between 52° N and 52° S latitudes. The ECOSTRESS Gridded Cloud Mask Instantaneous L2 Global 70 m (ECO_L2G_CLOUD) Version 2 data product is derived using a single-channel Bayesian cloud threshold with a look-up-table (LUT) approach. The ECO_L2G_CLOUD product provides a cloud mask that can be used to determine cloud cover for accurate land surface temperature and evapotranspiration estimation. This data product is a gridded version of the &lt;a href&#x3D;&quot;https://doi.org/10.5067/ECOSTRESS/ECO_L2_CLOUD.002&quot;&gt;ECO_L2_CLOUD&lt;/a&gt; Version 2 product that was resampled using nearest neighbor, projected to a globally snapped 0.0006° grid, and repackaged as the ECO_L2G_CLOUD Version 2 data product. The ECO_L2G_CLOUD Version 2 data product contains two cloud mask layers: cloud confidence and final cloud mask. Information on how to interpret the cloud confidence and cloud mask layers is provided in Table 7 of the ECO_L2_CLOUD Version 2 User Guide. Known Issues: Data acquisition gap: ECOSTRESS was launched on June 29, 2018, and moved to autonomous science operations on August 20, 2018, following a successful in-orbit checkout period. On September 29, 2018, ECOSTRESS experienced an anomaly with its primary mass storage unit (MSU). ECOSTRESS has a primary and secondary MSU (A and B). On December 5, 2018, the instrument was switched to the secondary MSU and science operations resumed. On March 14, 2019, the secondary MSU experienced a similar anomaly, temporarily halting science acquisitions. On May 15, 2019, a new data acquisition approach was implemented, and science acquisitions resumed. To optimize the new acquisition approach TIR bands 2, 4, and 5 are being downloaded. The data products are as previously, except the bands not downloaded contain fill values (L1 radiance and L2 emissivity). This approach was implemented from May 15, 2019, through April 28, 2023. * Data acquisition gap: From February 8 to February 16, 2020, an ECOSTRESS instrument issue resulted in a data anomaly that created striping in band 4 (10.5 micron). These data products have been reprocessed and are available for download. No ECOSTRESS data were acquired on February 17, 2020, due to the instrument being in SAFEHOLD. Data acquired following the anomaly have not been affected. * Data acquisition: ECOSTRESS has now successfully returned to 5-band mode after being in 3-band mode since 2019. This feature was successfully enabled following a Data Processing Unit firmware update (version 4.1) to the payload on April 28, 2023. To better balance contiguous science data scene variables, 3-band collection is currently being interleaved with 5-band acquisitions over the orbital day/night periods. * Solar Array Obstruction: Some ECOSTRESS scenes may be affected by solar array obstructions from the International Space Station (ISS), potentially impacting data quality of obstructed pixels. The &amp;#39;FieldOfViewObstruction&amp;#39; metadata field is included in all Version 2 products to indicate possible obstructions: * Before October 24, 2024 (orbits prior to 35724): The field is present but was not populated and does not reliably identify affected scenes. * On or after October 24, 2024 (starting with orbit 35724): The field is populated and generally accurate, except for late December 2024, when a temporary processing error may have caused false positives. * A &lt;a href&#x3D;&quot;https://lpdaac.usgs.gov/documents/2249/obst_all_sort.txt&quot;&gt;list of scenes&lt;/a&gt; confirmed to be affected by obstructions is available and is recommended for verifying historical data (before October 24, 2024) and scenes from late December 2024. * The ISS native pointing information is coarse relative to ECOSTRESS pixels, so ECOSTRESS geolocation is improved through image matching with a basemap. Metadata in the L1B_GEO file shows the success of this geolocation improvement, using categorizations &amp;quot;best&amp;quot;, &amp;quot;good&amp;quot;, &amp;quot;suspect&amp;quot;, and &amp;quot;poor&amp;quot;. We recommend that users use only &amp;quot;best&amp;quot; and &amp;quot;good&amp;quot; scenes for evaluations where geolocation is important (e.g., comparison to field sites). For some scenes, this metadata is not reflected in the higher-level products (e.g., land surface temperature, evapotranspiration, etc.). While this metadata is always available in the geolocation product, to save users additional download, we have produced a &lt;a href&#x3D;&quot;https://lpdaac.usgs.gov/documents/2253/qa_20250423-present.txt&quot;&gt;summary text file&lt;/a&gt; that includes the geolocation quality flags for all scenes from launch to present. At a later date, all higher-level products will reflect the geolocation quality flag correctly (the field name is GeolocationAccuracyQA). *During the time period of May 15th, 2025, through July 1st, 2025, ECOSTRESS data was noisier than expected. Cycling the payload resolved the issue, but researchers should use all levels of ECOSTRESS data acquired during this time period with caution.
&lt;br&gt;&lt;h4 id&#x3D;&quot;eco3ancqa&quot;&gt;ECO3ANCQA&lt;/h4&gt;
The ECO3ANCQA Version 1 data product was decommissioned on September 30, 2025. The ECOsystem Spaceborne Thermal Radiometer Experiment on Space Station (ECOSTRESS) mission measures the temperature of plants to better understand how much water plants need and how they respond to stress. ECOSTRESS is attached to the International Space Station (ISS) and collects data globally between 52 degrees N and 52 degrees S latitudes. The ECO3ANCQA Version 1 is a Level 3 (L3) product that provides Quality Assessment (QA) fields for all ancillary data used in L3 and Level 4 (L4) products generated by Jet Propulsion Laboratory (JPL). No quality flags are generated for the L3 or L4 products. Instead, the quality flags of the source data products are resampled by nearest neighbor onto the geolocation of the ECOSTRESS scene. A quality flag array for each input dataset, when available, is collected into the combined QA product. The ECO3ANCQA Version 1 data product contains layers of quality flags for ECOSTRESS cloud mask, Landsat 8, land cover type, albedo, MODIS Terra aerosol, MODIS Terra Cloud 1 km, MODIS Terra Cloud 5 km, MODIS Terra atmospheric profile, vegetation indices, MODIS Terra gross primary productivity, and MODIS water mask. Known Issues: Data acquisition gaps: ECOSTRESS was launched on June 29, 2018, and moved to autonomous science operations on August 20, 2018, following a successful in-orbit checkout period. On September 29, 2018, ECOSTRESS experienced an anomaly with its primary mass storage unit (MSU). ECOSTRESS has a primary and secondary MSU (A and B). On December 5, 2018, the instrument was switched to the secondary MSU and science operations resumed. On March 14, 2019, the secondary MSU experienced a similar anomaly temporarily halting science acquisitions. On May 15, 2019, a new data acquisition approach was implemented and science acquisitions resumed. To optimize the new acquisition approach TIR bands 2, 4 and 5 are being downloaded. The data products are as previously, except the bands not downloaded contain fill values (L1 radiance and L2 emissivity). This approach was implemented from May 15, 2019, through April 28, 2023. * Data acquisition gap: From February 8 to February 16, 2020, an ECOSTRESS instrument issue resulted in a data anomaly that created striping in band 4 (10.5 micron). These data products have been reprocessed and are available for download. No ECOSTRESS data were acquired on February 17, 2020, due to the instrument being in SAFEHOLD. Data acquired following the anomaly have not been affected. * Data acquisition: ECOSTRESS has now successfully returned to 5-band mode after being in 3-band mode since 2019. This feature was successfully enabled following a Data Processing Unit firmware update (version 4.1) to the payload on April 28, 2023. To better balance contiguous science data scene variables, 3-band collection is currently being interleaved with 5-band acquisitions over the orbital day/night periods.
&lt;br&gt;&lt;h4 id&#x3D;&quot;eco2lste&quot;&gt;ECO2LSTE&lt;/h4&gt;
The ECO2LSTE Version 1 data product was decommissioned on May 21, 2025. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/ECOSTRESS/ECO_L2T_LSTE.002&quot;&gt;ECO_L2T_LSTE&lt;/a&gt; Version 2 and &lt;a href&#x3D;&quot;https://doi.org/10.5067/ECOSTRESS/ECO_L2G_LSTE.002&quot;&gt;ECO_L2G_LSTE&lt;/a&gt; Version 2 data products. The ECOsystem Spaceborne Thermal Radiometer Experiment on Space Station (ECOSTRESS) mission measures the temperature of plants to better understand how much water plants need and how they respond to stress. ECOSTRESS is attached to the International Space Station (ISS) and collects data globally between 52 degrees N and 52 degrees S latitudes. The ECO2LSTE Version 1 data product provides atmospherically corrected land surface temperature and emissivity (LST&amp;amp;E) values derived from five thermal infrared (TIR) bands. The ECO2LSTE data product was derived using a physics-based Temperature and Emissivity Separation (TES) algorithm. The ECO2LSTE is provided as swath data and has a spatial resolution of 70 meters (m). The corresponding &lt;a href&#x3D;&quot;https://doi.org/10.5067/ECOSTRESS/ECO1BGEO.001&quot;&gt;ECO1BGEO&lt;/a&gt; data product is required to georeference the ECO2LSTE data product. The ECO2LSTE Version 1 data product contains variables of LST, emissivity for bands 1 through 5, quality control for LST&amp;amp;E, LST error, emissivity error for bands 1 through 5, wideband emissivity, and Precipitable Water Vapor (PWV). Known Issues: Data acquisition gap: ECOSTRESS was launched on June 29, 2018, and moved to autonomous science operations on August 20, 2018, following a successful in-orbit checkout period. On September 29, 2018, ECOSTRESS experienced an anomaly with its primary mass storage unit (MSU). ECOSTRESS has a primary and secondary MSU (A and B). On December 5, 2018, the instrument was switched to the secondary MSU and science operations resumed. On March 14, 2019, the secondary MSU experienced a similar anomaly temporarily halting science acquisitions. On May 15, 2019, a new data acquisition approach was implemented and science acquisitions resumed. To optimize the new acquisition approach TIR bands 2, 4 and 5 are being downloaded. The data products are as previously, except the bands not downloaded contain fill values (L1 radiance and L2 emissivity). This approach was implemented from May 15, 2019, through April 28, 2023. * Data acquisition gap: From February 8 to February 16, 2020, an ECOSTRESS instrument issue resulted in a data anomaly that created striping in band 4 (10.5 micron). These data products have been reprocessed and are available for download. No ECOSTRESS data were acquired on February 17, 2020, due to the instrument being in SAFEHOLD. Data acquired following the anomaly have not been affected. * Data acquisition: ECOSTRESS has now successfully returned to 5-band mode after being in 3-band mode since 2019. This feature was successfully enabled following a Data Processing Unit firmware update (version 4.1) to the payload on April 28, 2023. To better balance contiguous science data scene variables, 3-band collection is currently being interleaved with 5-band acquisitions over the orbital day/night periods.
&lt;br&gt;&lt;h4 id&#x3D;&quot;eco1bmaprad&quot;&gt;ECO1BMAPRAD&lt;/h4&gt;
The ECO1BMAPRAD Version 1 data product was decommissioned on February 14, 2025. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/ECOSTRESS/ECO_L1CT_RAD.002&quot;&gt;ECO_L1CT_RAD&lt;/a&gt; Version 2 and &lt;a href&#x3D;&quot;https://doi.org/10.5067/ECOSTRESS/ECO_L1CG_RAD.002&quot;&gt;ECO_L1CG_RAD&lt;/a&gt; Version 2 data products. The ECOsystem Spaceborne Thermal Radiometer Experiment on Space Station (ECOSTRESS) mission measures the temperature of plants to better understand how much water plants need and how they respond to stress. ECOSTRESS is attached to the International Space Station (ISS) and collects data globally between 52 degrees N and 52 degrees S latitudes. A map of the acquisition coverage can be found in Figure 2 on the &lt;a href&#x3D;&quot;https://ecostress.jpl.nasa.gov/science&quot;&gt;ECOSTRESS website&lt;/a&gt;. The ECO1BMAPRAD Version 1 data product combines the at-sensor calibrated radiance values retrieved for the ECO1BRAD data product and the geolocation information provided in the ECO1BGEO data product to produce a geotagged, resampled radiance product. The ECO1BMAPRAD data product is produced as a map registered product that is in a rotated geographic projection with a spatial resolution of 70 meters (m). The ECO1BMAPRAD data product accounts for the overlap and variable pixel size in the ECO1BRAD data product. The ECO1BMAPRAD Version 1 data product contains data variables including the radiance values for the five thermal infrared (TIR) bands, digital number (DN) values for the shortwave infrared (SWIR) band, associated data quality indicators, latitude and longitude values, solar and view geometry information, and surface height. Known Issues: Data acquisition gap: ECOSTRESS was launched on June 29, 2018, and moved to autonomous science operations on August 20, 2018, following a successful in-orbit checkout period. On September 29, 2018, ECOSTRESS experienced an anomaly with its primary mass storage unit (MSU). ECOSTRESS has a primary and secondary MSU (A and B). On December 5, 2018, the instrument was switched to the secondary MSU and science operations resumed. On March 14, 2019, the secondary MSU experienced a similar anomaly temporarily halting science acquisitions. On May 15, 2019, a new data acquisition approach was implemented and science acquisitions resumed. To optimize the new acquisition approach TIR bands 2, 4 and 5 are being downloaded. The data products are as previously, except the bands not downloaded contain fill values (L1 radiance and L2 emissivity). This approach was implemented from May 15, 2019, through April 28, 2023. * Data acquisition gap: From February 8 to February 16, 2020, an ECOSTRESS instrument issue resulted in a data anomaly that created striping in band 4 (10.5 micron). These data products have been reprocessed and are available for download. No ECOSTRESS data were acquired on February 17, 2020, due to the instrument being in SAFEHOLD. Data acquired following the anomaly have not been affected. * Resampled data: The data has been resampled, so users interested in working with data closest to that acquired by the instrument may want to work with the swath products. * Missing scan data: During testing, an instrument artifact was encountered in ECOSTRESS bands 1 and 5, resulting in missing values. A machine learning algorithm has been applied to interpolate missing values. For more information on the missing scan filling techniques and outcomes, see Section 3.3.2 of the User Guide. * Cold bias: ECOSTRESS Level-1 Radiance data shows high correlation with in-situ ground measurements (R2 &#x3D; 0.99 in all bands). Currently, ECOSTRESS has a cold bias of approximately 0.7 Kelvin (K), which will be corrected through calibration in future data releases. * Data acquisition: ECOSTRESS has now successfully returned to 5-band mode after being in 3-band mode since 2019. This feature was successfully enabled following a Data Processing Unit firmware update (version 4.1) to the payload on April 28, 2023. To better balance contiguous science data scene variables, 3-band collection is currently being interleaved with 5-band acquisitions over the orbital day/night periods.
&lt;br&gt;&lt;h4 id&#x3D;&quot;eco4wue&quot;&gt;ECO4WUE&lt;/h4&gt;
The ECO4WUE Version 1 data product was deprecated on September 30, 2025. Users are encouraged to use the &lt;a href&#x3D;&quot;https://doi.org/10.5067/ECOSTRESS/ECO_L4T_WUE.002&quot;&gt;ECO_L4T_WUE&lt;/a&gt; and &lt;a href&#x3D;&quot;https://doi.org/10.5067/ECOSTRESS/ECO_L4G_WUE.002&quot;&gt;ECO_L4G_WUE&lt;/a&gt; Version 2 data products. The ECOsystem Spaceborne Thermal Radiometer Experiment on Space Station (ECOSTRESS) mission measures the temperature of plants to better understand how much water plants need and how they respond to stress. ECOSTRESS is attached to the International Space Station (ISS) and collects data globally between 52 degrees N and 52 degrees S latitudes. The ECO4WUE Version 1 data product provides Water Use Efficiency (WUE) data generated according to the Priestley-Taylor Jet Propulsion Laboratory (PT-JPL) algorithm described in the ECOSTRESS Level 4 WUE Algorithm Theoretical Basis Document (ATBD). WUE is the ratio of carbon stored by plants to water evaporated by plants. This ratio is given as grams of carbon stored per kilogram of water evaporated over the course of the day from sunrise to sunset on the day when the ECOSTRESS granule was acquired. The ECO4WUE Version 1 data product contains a single variable of water use efficiency. Known Issues: Data acquisition gaps: ECOSTRESS was launched on June 29, 2018, and moved to autonomous science operations on August 20, 2018, following a successful in-orbit checkout period. On September 29, 2018, ECOSTRESS experienced an anomaly with its primary mass storage unit (MSU). ECOSTRESS has a primary and secondary MSU (A and B). On December 5, 2018, the instrument was switched to the secondary MSU and science operations resumed. On March 14, 2019, the secondary MSU experienced a similar anomaly temporarily halting science acquisitions. On May 15, 2019, a new data acquisition approach was implemented and science acquisitions resumed. To optimize the new acquisition approach TIR bands 2, 4 and 5 are being downloaded. The data products are as previously, except the bands not downloaded contain fill values (L1 radiance and L2 emissivity). This approach was implemented from May 15, 2019, through April 28, 2023. * Data acquisition gap: From February 8 to February 16, 2020, an ECOSTRESS instrument issue resulted in a data anomaly that created striping in band 4 (10.5 micron). These data products have been reprocessed and are available for download. No ECOSTRESS data were acquired on February 17, 2020, due to the instrument being in SAFEHOLD. Data acquired following the anomaly have not been affected. * Data acquisition: ECOSTRESS has now successfully returned to 5-band mode after being in 3-band mode since 2019. This feature was successfully enabled following a Data Processing Unit firmware update (version 4.1) to the payload on April 28, 2023. To better balance contiguous science data scene variables, 3-band collection is currently being interleaved with 5-band acquisitions over the orbital day/night periods.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA EMIT Project</title>
      <link>https://registry.opendata.aws/nasa-emit</link>
      <guid>https://registry.opendata.aws/nasa-emit</guid>
      <description>The Earth Surface Mineral Dust Source Investigation (EMIT) instrument measures surface mineralogy, targeting the Earth’s arid dust source regions. EMIT is installed on the International Space Station (ISS) and uses imaging spectroscopy to take mineralogical measurements of sunlit regions of interest between 52° N latitude and 52° S latitude. An interactive map showing the regions being investigated, current and forecasted data coverage, and additional data resources can be found on the VSWIR Imaging Spectroscopy Interface for Open Science (VISIONS) &lt;a href&#x3D;&quot;https://earth.jpl.nasa.gov/emit/data/data-portal/coverage-and-forecasts/&quot;&gt;EMIT Open Data Portal&lt;/a&gt;. The EMIT Level 1B At-Sensor Calibrated Radiance and Geolocation (EMITL1BRAD) Version 1 data product provides at-sensor calibrated radiance values along with observation data in a spatially raw, non-orthocorrected format. Each EMITL1BRAD granule consists of two Network Common Data Format 4 (NetCDF4) files at a spatial resolution of 60 meters (m): Radiance (EMIT_L1B_RAD) and Observation (EMIT_L1B_OBS). The Radiance file contains the at-sensor radiance measurements of 285 bands with a spectral range of 381-2493 nanometers (nm) and with a spectral resolution of ~7.5 nm, which are held within a single science dataset layer (SDS). The Observation file contains viewing and solar geometries, timing, topographic, and other information related to the observation. Each NetCDF4 file holds a location group containing geometric lookup tables (GLT), which are orthorectified images that provide relative x and y reference locations from the raw scene to allow for projection of the data. Along with the GLT layers, the files also contain latitude, longitude, and elevation layers. The latitude and longitude coordinates are presented using the World Geodetic System (WGS84) ellipsoid. The elevation data was obtained from Shuttle Radar Topography Mission v3 (SRTM v3) data and resampled to EMIT’s spatial resolution. Each granule is approximately 75 kilometers (km) by 75 km, nominal at the equator, with some granules at the end of an orbit segment reaching 150 km in length. Known Issues: Data acquisition gap: From September 13, 2022, through January 6, 2023, a power issue outside of EMIT caused a pause in operations. Due to this shutdown, no data were acquired during that timeframe.
&lt;br&gt;&lt;h4 id&#x3D;&quot;emitl1batt&quot;&gt;EMITL1BATT&lt;/h4&gt;
The Earth Surface Mineral Dust Source Investigation (EMIT) instrument measures surface mineralogy, targeting the Earth’s arid dust source regions. EMIT is installed on the International Space Station (ISS). EMIT uses imaging spectroscopy to take mineralogical measurements of the sunlit regions of interest between 52° N latitude and 52° S latitude. An interactive map showing the regions being investigated, current and forecasted data coverage, and additional data resources can be found on the VSWIR Imaging Spectroscopy Interface for Open Science &lt;a href&#x3D;&quot;https://earth.jpl.nasa.gov/emit/data/data-portal/coverage-and-forecasts/&quot;&gt;(VISIONS): EMIT Open Data Portal&lt;/a&gt;. The EMIT Level 1B Corrected Spacecraft Attitude and Ephemeris (EMITL1BATT) Version 1 data product provides both corrected and uncorrected attitude quaternions and spacecraft ephemeris data obtained from the ISS, including Earth-centered inertial (ECI) position and velocity, and associated time elements. The data are provided in 1 second intervals, and each product file contains vectors from the duration of the orbit. The time elements are copied from the ISS raw data. The data for each EMITL1BATT granule are delivered in a single Network Common Data Format 4 (netCDF-4) file. Known Issues: Data acquisition gap: From September 13, 2022, through January 6, 2023, a power issue outside of EMIT caused a pause in operations. Due to this shutdown, no data were acquired during that timeframe.
&lt;br&gt;&lt;h4 id&#x3D;&quot;emitl2bco2enh&quot;&gt;EMITL2BCO2ENH&lt;/h4&gt;
The Earth Surface Mineral Dust Source Investigation (EMIT) instrument measures surface mineralogy, targeting the Earth’s arid dust source regions. EMIT is installed on the International Space Station (ISS) and uses imaging spectroscopy to take measurements of the sunlit regions of interest between 52° N latitude and 52° S latitude. An interactive map showing the regions being investigated, current and forecasted data coverage, and additional data resources can be found on the VSWIR Imaging Spectroscopy Interface for Open Science (VISIONS) &lt;a href&#x3D;&quot;https://earth.jpl.nasa.gov/emit/data/data-portal/coverage-and-forecasts/&quot;&gt;EMIT Open Data Portal&lt;/a&gt;. In addition to its primary objective described above, EMIT has demonstrated the capacity to characterize carbon dioxide (CO2) and methane (CH4) point-source emissions by measuring gas absorption features in the short-wave infrared bands. The EMIT Level 2B Greenhouse Gas (GHG) series of products can be used to identify and quantify point source emissions. The EMIT Level 2B Carbon Dioxide Enhancement Data (EMITL2BCO2ENH) Version 1 data product is a total vertical column enhancement estimate of CO2 in parts per million meter (ppm m) based on an adaptive matched filter approach. EMITL2BCO2ENH provides per-pixel CO2 enhancement data used to identify CO2 plume complexes. The initial release of the EMITL2BCO2ENH data product will only include granules where CO2 plume complexes have been identified. Each granule contains one Cloud Optimized GeoTIFF (COG) file at a spatial resolution of 60 meters (m): Carbon Dioxide Enhancement (EMIT_L2B_CO2ENH). The EMITL2BCO2ENH COG file contains methane enhancement data based primarily on &lt;a href&#x3D;&quot;https://doi.org/10.5067/EMIT/EMITL1BRAD.001&quot;&gt;EMITL1BRAD&lt;/a&gt; radiance values. Each granule is approximately 75 kilometers (km) by 75 km, nominal at the equator, with some granules near the end of an orbit segment reaching 150 km in length. Known Issues: Data acquisition gap: From September 13, 2022, through January 6, 2023, a power issue outside of EMIT caused a pause in operations. Due to this shutdown, no data were acquired during that timeframe.
&lt;br&gt;&lt;h4 id&#x3D;&quot;emitl2bco2enh-1&quot;&gt;EMITL2BCO2ENH&lt;/h4&gt;
The Earth Surface Mineral Dust Source Investigation (EMIT) instrument measures surface mineralogy, targeting the Earth’s arid dust source regions. EMIT is installed on the International Space Station. EMIT uses imaging spectroscopy to take measurements of sunlit regions of interest between 52° N latitude and 52° S latitude. An interactive map showing the regions being investigated, current and forecasted data coverage, and additional data resources can be found on the VSWIR Imaging Spectroscopy Interface for Open Science (VISIONS) &lt;a href&#x3D;&quot;https://earth.jpl.nasa.gov/emit/data/data-portal/coverage-and-forecasts/&quot;&gt;EMIT Open Data Portal&lt;/a&gt;. In addition to its primary objective described above, EMIT has demonstrated the capacity to characterize methane (CH4) and carbon dioxide (CO2) point-source emissions by measuring gas absorption features in the shortwave infrared bands. The EMIT Level 2B Carbon Dioxide Enhancement Data (EMITL2BCO2ENH) Version 2 data product is a total vertical column enhancement estimate of carbon dioxide in parts per million meter (ppm m) based on an adaptive matched filter approach. EMITL2BCO2ENH provides per-pixel carbon dioxide enhancement data used to identify carbon dioxide plume complexes, per-pixel carbon dioxide uncertainty due to sensor noise, and per-pixel carbon dioxide sensitivity that can be used to remove bias from the enhancement data. The EMITL2BCO2ENH Version 2 data product includes methane enhancement granules for all captured scenes, regardless of carbon dioxide plume complex identification. Each granule contains three Cloud Optimized GeoTIFF (COG) files at a spatial resolution of 60 meters (m): Carbon Dioxide Enhancement (EMIT_L2B_CO2ENH), Carbon Dioxide Uncertainty (EMIT_L2B_CO2UNCERT), and Carbon Dioxide Sensitivity (EMIT_L2B_CO2SENS). The EMITL2BCO2ENH COG files contain carbon dioxide enhancement data based primarily on &lt;a href&#x3D;&quot;https://doi.org/10.5067/EMIT/EMITL1BRAD.001&quot;&gt;EMITL1BRAD&lt;/a&gt; radiance values. Each granule is approximately 75 kilometers (km) by 75 km, nominal at the equator, with some granules near the end of an orbit segment reaching 150 km in length. Known Issues: Data acquisition gap: From September 13, 2022, through January 6, 2023, a power issue outside of EMIT caused a pause in operations. Due to this shutdown, no data were acquired during that timeframe.
&lt;br&gt;&lt;h4 id&#x3D;&quot;emitl2bmin&quot;&gt;EMITL2BMIN&lt;/h4&gt;
The Earth Surface Mineral Dust Source Investigation (EMIT) instrument measures surface mineralogy, targeting the Earth’s arid dust source regions. EMIT is installed on the International Space Station (ISS) and uses imaging spectroscopy to take mineralogical measurements of the sunlit regions of interest between 52° N latitude and 52° S latitude. An interactive map showing the regions being investigated, current and forecasted data coverage, and additional data resources can be found on the VSWIR Imaging Spectroscopy Interface for Open Science (VISIONS) &lt;a href&#x3D;&quot;https://earth.jpl.nasa.gov/emit/data/data-portal/coverage-and-forecasts/&quot;&gt;EMIT Open Data Portal&lt;/a&gt;. The EMIT Level 2B Estimated Mineral Identification and Band Depth and Uncertainty (EMITL2BMIN) Version 1 data product provides estimated mineral identification and band depths in a spatially raw, non-orthocorrected format. Each EMITL2BMIN granule contains two Network Common Data Format 4 (NetCDF4) files at a spatial resolution of 60 meters (m): Mineral Identification (EMIT_L2B_MIN) and Mineral Uncertainty (EMIT_L2B_MINUNCERT). The EMIT_L2B_MIN file contains the band depth (the depth of the identified spectral feature) and the identified mineral for each pixel. Two spectral groups, which correspond to different regions of the spectra, are identified independently and often co-occur. These estimates are generated using the &lt;a href&#x3D;&quot;https://www.usgs.gov/publications/tetracorder-user-guide-version-44&quot;&gt;Tetracorder system&lt;/a&gt; (&lt;a href&#x3D;&quot;https://github.com/PSI-edu/spectroscopy-tetracorder&quot;&gt;code&lt;/a&gt;) and are based on &lt;a href&#x3D;&quot;https://doi.org/10.5067/EMIT/EMITL2ARFL.001&quot;&gt;EMITL2ARFL&lt;/a&gt; reflectance values. The EMIT_L2B_MINUNCERT file provides band depth uncertainty estimates calculated using surface Reflectance Uncertainty values from the EMITL2ARFL data product. The band depth uncertainties are presented as standard deviations. The fit score for each mineral identification is also provided as the coefficient of determination (r&lt;sup&gt;2&lt;/sup&gt;) of the match between the continuum normalized library reference and the continuum normalized observed spectrum. Associated metadata indicates the name and reference information for each identified mineral, and additional information about aggregating minerals into different categories is available in the &lt;a href&#x3D;&quot;https://github.com/emit-sds/emit-sds-l2b&quot;&gt;emit-sds-l2b repository&lt;/a&gt; and will be available as subsequent data products. The EMITL2BMIN data product includes a total of 19 Science Dataset (SDS) layers. There are four layers for each of the Spectral Groups (Group 1 and Group 2): Mineral Identification, Band Depth, Band Depth Uncertainties, and Fit Score. Additional layers consist of geometric lookup table (GLT) x values, GLT y values, latitude, longitude, elevation, associated spectral library record, mineral name, URL for the spectral library description, spectral group, spectral library, and spectral group index. A browse image with Group 1 Band Depth, Group 2 Band Depth, Group 1 Band Depth Uncertainty, and Group 2 Band Depth Uncertainty is also included. Each granule is approximately 75 kilometers (km) by 75 km, nominal at the equator, with some granules at the end of an orbit segment reaching 150 km in length. Disclaimer This product is generated to support the EMIT mission objectives of constraining the sign of dust related radiative forcing. Ten mineral types are the core focus of this work: calcite, chlorite, dolomite, goethite, gypsum, hematite, illite+muscovite, kaolinite, montmorillonite, and vermiculite. A future product will aggregate these results for use in Earth System Models. Additional minerals are included in this product for transparency but were not the focus of this product. Further validation is required to use these additional mineral maps, particularly in the case of resource exploration. Similarly, the separation of minerals with similar spectral features, such as a fine-grained goethite and hematite, is an area of active research. The results presented here are an initial offering, but the precise categorization is likely to evolve over time, and the limits of what can and cannot be separated on the global scale is still being explored. The user is encouraged to read the Algorithm Theoretical Basis Document (ATBD) for more details. Known Issues: Data acquisition gap: From September 13, 2022, through January 6, 2023, a power issue outside of EMIT caused a pause in operations. Due to this shutdown, no data were acquired during that timeframe.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA EOS LAND VAL Project</title>
      <link>https://registry.opendata.aws/nasa-eos-land-val</link>
      <guid>https://registry.opendata.aws/nasa-eos-land-val</guid>
      <description>This data set provides field measurements of diameter, tree height, and crown dimensions for 1,513 trees in 30 plots at the La Selva Biological Station in Costa Rica. Fourteen of these plots were in undisturbed primary forest, six were in primary forest which had been selectively logged, seven were secondary forests, and three were abandoned pastures reverting to forest. The diameter and height data were used to calculate aboveground biomass for each of the 30 plots. The crown measurements were used to estimate a vertical profile for each plot, showing the vegetation volume in 1 meter increments from the ground to the top of the canopy. There are three comma-delimited data files and two shapefiles with this data set. The files contain the measurements and calculated biomass for the individual stems as well as the summary data at the plot level.
&lt;br&gt;&lt;h4 id&#x3D;&quot;maryland_temperature_humidity_1319&quot;&gt;Maryland_Temperature_Humidity_1319&lt;/h4&gt;
This data set describes the temperature and relative humidity at 12 locations around Goddard Space Flight Center in Greenbelt MD at 15 minute intervals between November 2013 and November 2015. These data were collected to study the impact of surface type on heating in a campus setting and to improve the understanding of urban heating and potential mitigation strategies on the campus scale. Sensors were mounted on posts at 2 m above surface and placed on 7 different surface types around the centre: asphalt parking lot, bright surface roof, grass field, forest, and stormwater mitigation features (bio-retention pond and rain garden). Data were also recorded in an office setting and a garage, both pre- and post-deployment, for calibration purposes. This dataset could be used to validate satellite-based study or could be used as a stand-alone study of the impact of surface type on heating in a campus setting.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lai_canada_816&quot;&gt;LAI_Canada_816&lt;/h4&gt;
This data set provides local LAI maps for the selected measured sites in Canada. These derived maps may also be useful for validating other LAI maps over these same sites given that the areas are protected from disturbance. The maps should be used for the given period of validity. The LAI data are suitable for use in modeling the carbon, water, energy, energy and trace gas exchange between the land surface and the atmosphere at regional scales. The data set may also be useful for monitoring changes in the land surface.The Leaf Area Index (LAI) maps are at 30-m resolution for the selected sites. LAI is defined here as half the total (all-sided) live foliage area per unit horizontal projected ground surface area. Overstory LAI corresponds to all tree foliage except for treeless areas where it corresponds to total foliage. The algorithms were developed from ground measurements and Landsat TM and ETM+ images (Fernandes et. al., 2003). A mask was developed using the Landsat ETM+/TM5 image and available land cover map to identify only those areas with land cover belonging to the sample land cover classes and with Landsat ETM+/TM5 spectral reflectance values that fell within the convex hull of the spectral reflectance values over the plots. LAI was mapped within the masked region using the Landsat ETM+/TM5 image and the developed transfer function. The final LAI map was scaled by a factor of 20 (offset 0). The LAI maps are in Tagged Image File Format (TIFF).
&lt;br&gt;&lt;h4 id&#x3D;&quot;lai_valeri_canada_829&quot;&gt;LAI_VALERI_Canada_829&lt;/h4&gt;
This data set provide local LAI maps for the Larose (Ontario) site in Canada. These derived maps may also be useful for validating other LAI maps over this same site given that the area is protected from disturbance. The maps should be used for the given period of validity. The LAI data are suitable for use in modeling the carbon, water, energy, energy and trace gas exchange between the land surface and the atmosphere at regional scales. The dataset may also be useful for monitoring changes in the land surface. A complete description of producing the maps for the Larose site and the ground measurement campaign is provide in the companion document (Larose2003FTReport.pdf (link)).The Leaf Area Index (LAI) maps are at 30-m resolution for the 3x3-km Larose site. LAI is defined here as half the total (all-sided) live foliage area per unit horizontal projected ground surface area. Overstory LAI corresponds to all tree foliage except for treeless areas where it corresponds to total foliage. The algorithms were developed from ground measurements and Landsat TM and ETM+ images (Fernandes et. al., 2003). A mask was developed using the Landsat ETM+/TM5 image and available land cover maps to identify only those areas with land cover belonging to the sample land cover classes and with Landsat ETM+/TM5 spectral reflectance values that fell within the convex hull of the spectral reflectance values over the plots. LAI was mapped within the masked region using the Landsat ETM+/TM5 image and the developed transfer function. The final LAI map was scaled by a factor of 20 (offset 0). The LAI maps are in Tagged Image File Format (TIFF).The VALERI project (Validation of Land European Remote sensing Instruments) is dedicated to the validation of the products derived from medium resolution satellite sensors ( &lt;a href&#x3D;&quot;http://www.avignon.inra.fr/valeri/&quot;&gt;http://www.avignon.inra.fr/valeri/&lt;/a&gt; ). The objectives of the VALERI project are: (1) to evaluate the absolute accuracy of the biophysical products (LAI, fAPAR, fCover) derived from large swath sensors (e.g., AVHRR, POLDER, VEGETATION, SEAWIFS, MSG, MERIS, AATSR, MODIS, MISR, GLI) using a range of possible algorithms; and (2) to inter-compare the products derived from different sensors and algorithms. For this purpose, the VALERI project has developed a network of sites distributed over the Earthâ€™s surface and a methodology designed to directly measure the biophysical variables of interest at proper spatial and temporal scales.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sar_subsets_993&quot;&gt;sar_subsets_993&lt;/h4&gt;
This data set provides Synthetic Aperture Radar (SAR) images for 42 selected sites from various terrestrial ecology and meteorological monitoring networks including FLUXNET, Ameriflux, Long Term Ecological Research (LTER), and the Greenland Climate Network (GC-Net). The data set contains at least one image for all 42 sites, and six sites have multiple images. See Table 1 for the sites and the temporal range of the available images. The scenes are in GeoTIFF format in Universal Transverse Mercator (UTM), WGS-84 projection, and 15-meter resolution. The SAR images are subset scenes of approximately 60 km x 70 km that include an established site in one of the monitoring networks. The spatial resolution of all scenes is 15 meters. These scenes are distributed as geotif files with appropriate projection information defined within the file.The acquisition mode for all data is the Fine Beam Double Polarization or FBD with the HH/HV polarization. The HH and HV channels are distributed as 3 channels to allow for an intuitive image display. The HH band is displayed in the red and blue channels and the HV band is displayed in the green channel. For some images only single polarization is available; these images are distributed as grayscale images. The source of the data is the PALSAR (Phased Array type L-band Synthetic Aperture Radar) sensor flying on the Advanced Land Observing Satellite (ALOS). The PALSAR data are in dual Polarization, HH+HV, mode. Bands HH (red and blue) and Band-HV (green) can be used to visualize land use patterns. The resulting images show vegetation in shades of green and barren land in shades of pink or purple.
&lt;br&gt;&lt;h4 id&#x3D;&quot;soilscape_1339&quot;&gt;SoilSCAPE_1339&lt;/h4&gt;
This data set contains in-situ soil moisture profile and soil temperature data collected at 20-minute intervals at SoilSCAPE (Soil moisture Sensing Controller and oPtimal Estimator) project sites in four states (California, Arizona, Oklahoma, and Michigan) in the United States. SoilSCAPE used wireless sensor technology to acquire high temporal resolution soil moisture and temperature data at up to 12 sites over varying durations since August 2011. At its maximum, the network consisted of over 200 wireless sensor installations (nodes), with a range of 6 to 27 nodes per site. The soil moisture sensors (EC-5 and 5-TM from Decagon Devices) were installed at three to four depths, nominally at 5, 20, and 50 cm below the surface. Soil conditions (e.g., hard soil or rocks) may have limited sensor placement. Temperature sensors were installed at 5 cm depth at six of the sites. Data collection started in August 2011 and continues at eight sites through the present. The data enables estimation of local-scale soil moisture at high temporal resolution and validation of remote sensing estimates of soil moisture at regional (airborne, e.g. NASA&amp;#39;s Airborne Microwave Observation of Subcanopy and Subsurface Mission - AirMOSS) and national (spaceborne, e.g. NASA&amp;#39;s Soil Moisture Active Passive - SMAP) scales.
&lt;br&gt;&lt;h4 id&#x3D;&quot;soilscape_v2_2049&quot;&gt;SoilSCAPE_V2_2049&lt;/h4&gt;
This dataset contains in-situ soil moisture profile and soil temperature data collected at 30-minute intervals at SoilSCAPE (Soil moisture Sensing Controller and oPtimal Estimator) project sites since 2021 in the United States and New Zealand. The SoilSCAPE network has used wireless sensor technology to acquire high temporal resolution soil moisture and temperature data over varying durations since 2011. Since 2021, the SoilSCAPE has upgraded the two previously active sites in Arizona and added several new sites in the United States and New Zealand. These new sites typically use the METER Teros-12 soil moisture sensor. At its maximum, the new network consisted of 57 wireless sensor installations (nodes), with a range of 6 to 8 nodes per site. Each SoilSCAPE site contains multiple wireless end-devices (EDs). Each ED supports up to five soil moisture probes typically installed at 5, 10, 20, and 30 cm below the surface. Sites in Arizona have soil moisture probes installed at up to 75 cm below the surface. Soil conditions (e.g., hard soil or rocks) may have limited sensor placement. The data enables estimation of local-scale soil moisture at high temporal resolution and validation of remote sensing estimates of soil moisture at regional and national (e.g. NASA&amp;#39;s Cyclone Global Navigation Satellite System - CYGNSS and Soil Moisture Active Passive - SMAP) scales. The data are provided in NetCDF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.ornldaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA EOS Project</title>
      <link>https://registry.opendata.aws/nasa-eos</link>
      <guid>https://registry.opendata.aws/nasa-eos</guid>
      <description>AM1EPHNE is the Terra Near Real Time (NRT) 2-hour spacecraft Extrapolated ephemeris data file in native format. The file name format is the following: AM1EPHNE.Ayyyyddd.hhmm.vvv.yyyydddhhmmss where from left to right: E &#x3D; Extrapolated; N &#x3D; Native format; A &#x3D; AM1 (Terra); yyyy &#x3D; data year, ddd &#x3D; Julian data day, hh &#x3D; data hour, mm &#x3D; data minute; vvv &#x3D; Version ID; yyyy &#x3D; production year, ddd &#x3D; Julian production day, hh &#x3D; production hour, mm &#x3D; production minute, and ss &#x3D; production second. Data set information:&lt;a href&#x3D;&quot;http://modis.gsfc.nasa.gov/sci_team/&quot;&gt;http://modis.gsfc.nasa.gov/sci_team/&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;modis_aqua_l3_sst_mid-ir_8day_4km_nighttime_v20190&quot;&gt;MODIS_AQUA_L3_SST_MID-IR_8DAY_4KM_NIGHTTIME_V2019.0&lt;/h4&gt;
Day and night spatially gridded (L3) global NASA skin sea surface temperature (SST) products from the Moderate-resolution Imaging Spectroradiometer (MODIS) onboard the Aqua satellite. Average daily, weekly (8 day), monthly and annual skin SST products at are available at both 4.63 and 9.26 km spatial resolution. Aqua was launched by NASA on May 4, 2002, into a sun synchronous, polar orbit with a daylight ascending node at 13:30, formation flying in the A-train with other Earth Observation Satellites (EOS), to study the global dynamics of the Earth atmosphere, land and oceans. MODIS captures data in 36 spectral bands at a variety of spatial resolutions. Two SST products can be present in these files. The first is a skin SST produced for both day and night (NSST) observations, derived from the long wave IR 11 and 12 micron wavelength channels, using a modified nonlinear SST algorithm intended to provide continuity of SST derived from heritage and current NASA sensors. At night, a second SST product is generated using the mid-infrared 3.95 and 4.05 micron wavelength channels which are unique to MODIS; the SST derived from these measurements is identified as SST4. The SST4 product has lower uncertainty, but due to sun glint can only be used at night. To generate the L3 products the L2 pixels are binned into an integerized sinusoidal area grid (ISEAG) and mapped into an equidistant cylindrical (also known as Platte Carre projection. Additional projection detailed can be found at &lt;a href&#x3D;&quot;https://oceancolor.gsfc.nasa.gov/docs/format/&quot;&gt;https://oceancolor.gsfc.nasa.gov/docs/format/&lt;/a&gt; The NASA MODIS L3 SST data products are generated by the NASA Ocean Biology Processing Group (OBPG) and Peter Minnett and his team at the Rosenstiel School of Marine and Atmospheric Science (RSMAS) are responsible for sea surface temperature algorithm development, error statistics and quality flagging. JPL acquires MODIS ocean L3 SST data from the OBPG and is the official Physical Oceanography Data Archive (PO.DAAC) for SST. The R2019.0 supersedes the previous v2014.1 datasets which can be found at &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODAM-8D4N4&quot;&gt;https://doi.org/10.5067/MODAM-8D4N4&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;modis_terra_l3_sst_thermal_daily_9km_daytime_v20190&quot;&gt;MODIS_TERRA_L3_SST_THERMAL_DAILY_9KM_DAYTIME_V2019.0&lt;/h4&gt;
Day and night spatially gridded (L3) global NASA skin sea surface temperature (SST) products from the Moderate-resolution Imaging Spectroradiometer (MODIS) onboard the Terra satellite. Average daily, weekly (8 day), monthly and annual skin SST products are available at both 4.63 and 9.26 km spatial resolution. Terra was launched by NASA on December 18, 1999, into a sun synchronous, polar orbit with a daylight descending node at 10:30 am, to study the global dynamics of the Earth atmosphere, land and oceans. The MODIS captures data in 36 spectral bands at a variety of spatial resolutions. Two SST products can be present in these files. The first is a skin SST produced for both day and night observations, derived from the long wave IR 11 and 12 micron wavelength channels, using a modified nonlinear SST algorithm intended to provide continuity with SST derived from heritage and current NASA sensors. At night, a second SST product is produced using the mid-infrared 3.95 and 4.05 micron channels which are unique to MODIS; the SST derived from these measurements is identified as SST4. The SST4 product has lower uncertainty, but due to sun glint can only be produced at night. To generate the L3 products the L2 pixels are binned into an integerized sinusoidal area grid (ISEAG) and mapped into an equidistant cylindrical (also known as Platte Carre) projection. Additional projection detailed can be found at &lt;a href&#x3D;&quot;https://oceancolor.gsfc.nasa.gov/docs/format/&quot;&gt;https://oceancolor.gsfc.nasa.gov/docs/format/&lt;/a&gt; The NASA MODIS L3 SST data products are generated by the NASA Ocean Biology Processing Group (OBPG) Peter Minnett and his team at the Rosenstiel School of Marine and Atmospheric Science (RSMAS) are responsible for sea surface temperature algorithm development, error statistics and quality flagging. JPL acquires and distributes MODIS ocean L3 SST data from the OBPG as the official Physical Oceanography Data Archive (PO.DAAC) for SST. The R2019 superseded the previous v2014.1 datasets which can be found at &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODST-1D9D4&quot;&gt;https://doi.org/10.5067/MODST-1D9D4&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;modis_terra_l3_sst_thermal_annual_9km_daytime_v20190&quot;&gt;MODIS_TERRA_L3_SST_THERMAL_ANNUAL_9KM_DAYTIME_V2019.0&lt;/h4&gt;
TDay and night spatially gridded (L3) global NASA skin sea surface temperature (SST) products from the Moderate-resolution Imaging Spectroradiometer (MODIS) onboard the Terra satellite. Average daily, weekly (8 day), monthly and annual skin SST products are available at both 4.63 and 9.26 km spatial resolution. Terra was launched by NASA on December 18, 1999, into a sun synchronous, polar orbit with a daylight descending node at 10:30 am, to study the global dynamics of the Earth atmosphere, land and oceans. The MODIS captures data in 36 spectral bands at a variety of spatial resolutions. Two SST products can be present in these files. The first is a skin SST produced for both day and night observations, derived from the long wave IR 11 and 12 micron wavelength channels, using a modified nonlinear SST algorithm intended to provide continuity with SST derived from heritage and current NASA sensors. At night, a second SST product is produced using the mid-infrared 3.95 and 4.05 micron channels which are unique to MODIS; the SST derived from these measurements is identified as SST4. The SST4 product has lower uncertainty, but due to sun glint can only be produced at night. To generate the L3 products the L2 pixels are binned into an integerized sinusoidal area grid (ISEAG) and mapped into an equidistant cylindrical (also known as Platte Carre) projection. Additional projection detailed can be found at &lt;a href&#x3D;&quot;https://oceancolor.gsfc.nasa.gov/docs/format/&quot;&gt;https://oceancolor.gsfc.nasa.gov/docs/format/&lt;/a&gt; The NASA MODIS L3 SST data products are generated by the NASA Ocean Biology Processing Group (OBPG) Peter Minnett and his team at the Rosenstiel School of Marine and Atmospheric Science (RSMAS) are responsible for sea surface temperature algorithm development, error statistics and quality flagging. JPL acquires and distributes MODIS ocean L3 SST data from the OBPG as the official Physical Oceanography Data Archive (PO.DAAC) for SST. The R2019 superseded the previous v2014.1 datasets which can be found at &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODST-AN9D4&quot;&gt;https://doi.org/10.5067/MODST-AN9D4&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;modis_terra_l3_sst_thermal_monthly_4km_daytime_v20190&quot;&gt;MODIS_TERRA_L3_SST_THERMAL_MONTHLY_4KM_DAYTIME_V2019.0&lt;/h4&gt;
Day and night spatially gridded global NASA skin sea surface temperature (SST) products from the Moderate-resolution Imaging Spectroradiometer (MODIS) onboard the Terra satellite. Average daily, weekly (8 day), monthly and annual skin SST products are available at both 4.63 and 9.26 km spatial resolution. Terra was launched by NASA on December 18, 1999, into a sun synchronous, polar orbit with a daylight descending node at 10:30 am, to study the global dynamics of the Earth atmosphere, land and oceans. The MODIS captures data in 36 spectral bands at a variety of spatial resolutions. Two SST products can be present in these files. The first is a skin SST produced for both day and night observations, derived from the long wave IR 11 and 12 micron wavelength channels, using a modified nonlinear SST algorithm intended to provide continuity with SST derived from heritage and current NASA sensors. At night, a second SST product is produced using the mid-infrared 3.95 and 4.05 micron channels which are unique to MODIS; the SST derived from these measurements is identified as SST4. The SST4 product has lower uncertainty, but due to sun glint can only be produced at night. To generate the L3 products the L2 pixels are binned into an integerized sinusoidal area grid (ISEAG) and mapped into an equidistant cylindrical (also known as Platte Carre) projection. Additional projection detailed can be found at &lt;a href&#x3D;&quot;https://oceancolor.gsfc.nasa.gov/docs/format/&quot;&gt;https://oceancolor.gsfc.nasa.gov/docs/format/&lt;/a&gt; The NASA MODIS L3 SST data products are generated by the NASA Ocean Biology Processing Group (OBPG) Peter Minnett and his team at the Rosenstiel School of Marine and Atmospheric Science (RSMAS) are responsible for sea surface temperature algorithm development, error statistics and quality flagging. JPL acquires and distributes MODIS ocean L3 SST data from the OBPG as the official Physical Oceanography Data Archive (PO.DAAC) for SST. The R2019 superseded the previous v2014.1 datasets which can be found at &lt;a href&#x3D;&quot;https://doi.org/10.5067/MODST-MO4D4&quot;&gt;https://doi.org/10.5067/MODST-MO4D4&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA EOSDIS Project</title>
      <link>https://registry.opendata.aws/nasa-eosdis</link>
      <guid>https://registry.opendata.aws/nasa-eosdis</guid>
      <description>This is the version 3 Atmospheric Trace Molecule Spectroscopy (ATMOS) Level 1 product containing spectra and runlog (i.e. ) information in a netCDF format. ATMOS is an infrared spectrometer (a Fourier transform interferometer) designed to derive vertical concentrations of various trace gases in the atmosphere, particularly the ozone depleting chlorine and fluorine based molecules. The transmission spectra are ratioed from ATMOS high sun observations, on a scale of 0 to 1. Data files also include time, geolocation and other information. The data were collected during four space shuttle missions: STS-51B/Spacelab 3 (April 30 to May 1, 1985), STS-45/ATLAS-1 (March 25 to April 2, 1992), STS-55/ATLAS-2 (April 8 to 16, 1993), and STS-66/ATLAS-3 (November 3 to 12, 1994). Data are written to separate files grouped by mission (sl3, at1, at2 or at3), and occultation type (sunrise or sunset) and number.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atmosl2af&quot;&gt;ATMOSL2AF&lt;/h4&gt;
This is the version 3 Atmospheric Trace Molecule Spectroscopy (ATMOS) Level 2 product containing trace gases on a vertical altitude (km) grid with data stored in an ASCII table using a FORTRAN friendly fixed field format. ATMOS is an infrared spectrometer (a Fourier transform interferometer) designed to derive vertical concentrations of various trace gases in the atmosphere, particularly the ozone depleting chlorine and fluorine based molecules. Measured species include: H2O, CO2, O3, N2O, CO, CH4, NO and NO2 (both diurnally and not diurnally corrected), HNO3, HF, HCl, OCS, H2CO, HOCl, H2O2, HO2NO2, N2O5, ClONO2, HCN, CH3F, CH3Cl, CF4, CCl2F2, CCl3F, CCl4, COF2, C2H6, C2H2, N2, CHF2Cl, HCOOH, HDO, SF6 and CH3D reported at 100 levels from 0.5 to 99.5 km. Data files also include time, geolocation and other information. The data were collected during four space shuttle missions: STS-51B/Spacelab 3 (April 30 to May 1, 1985), STS-45/ATLAS-1 (March 25 to April 2, 1992), STS-55/ATLAS-2 (April 8 to 16, 1993), and STS-66/ATLAS-3 (November 3 to 12, 1994). Data are written to separate files grouped by mission (sl3, at1, at2 or at3), and occultation type (sunrise or sunset) and number. A similar product (ATMOSL2AT) exists that contains these same data in a spreadsheet friendly tab delimited format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atmosl2at&quot;&gt;ATMOSL2AT&lt;/h4&gt;
This is the version 3 Atmospheric Trace Molecule Spectroscopy (ATMOS) Level 2 product containing trace gases on a vertical altitude (km) grid with data stored in an ASCII table using a spreadsheet friendly tab delimited format. ATMOS is an infrared spectrometer (a Fourier transform interferometer) designed to derive vertical concentrations of various trace gases in the atmosphere, particularly the ozone depleting chlorine and fluorine based molecules. Measured species include: H2O, CO2, O3, N2O, CO, CH4, NO and NO2 (both diurnally and not diurnally corrected), HNO3, HF, HCl, OCS, H2CO, HOCl, H2O2, HO2NO2, N2O5, ClONO2, HCN, CH3F, CH3Cl, CF4, CCl2F2, CCl3F, CCl4, COF2, C2H6, C2H2, N2, CHF2Cl, HCOOH, HDO, SF6 and CH3D reported at 100 levels from 0.5 to 99.5 km. Data files also include time, geolocation and other information. The data were collected during four space shuttle missions: STS-51B/Spacelab 3 (April 30 to May 1, 1985), STS-45/ATLAS-1 (March 25 to April 2, 1992), STS-55/ATLAS-2 (April 8 to 16, 1993), and STS-66/ATLAS-3 (November 3 to 12, 1994). Data are written to separate files grouped by mission (sl3, at1, at2 or at3), and occultation type (sunrise or sunset) and number. A similar product (ATMOSL2AF) exists that contains these same data in a FORTRAN friendly fixed field format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atmosl2tf&quot;&gt;ATMOSL2TF&lt;/h4&gt;
This is the version 3 Atmospheric Trace Molecule Spectroscopy (ATMOS) Level 2 product containing trace gases on a vertical potential temperature (theta) grid with data stored in an ASCII table using a FORTRAN friendly fixed field format. ATMOS is an infrared spectrometer (a Fourier transform interferometer) designed to derive vertical concentrations of various trace gases in the atmosphere, particularly the ozone depleting chlorine and fluorine based molecules. Measured species include: H2O, CO2, O3, N2O, CO, CH4, NO and NO2 (both diurnally and not diurnally corrected), HNO3, HF, HCl, OCS, H2CO, HOCl, H2O2, HO2NO2, N2O5, ClONO2, HCN, CH3F, CH3Cl, CF4, CCl2F2, CCl3F, CCl4, COF2, C2H6, C2H2, N2, CHF2Cl, HCOOH, HDO, SF6 and CH3D reported at 53 levels from 280 to 3950 K. Data files also include time, geolocation and other information. The data were collected during four space shuttle missions: STS-51B/Spacelab-3 (April 30 to May 1, 1985), STS-45/ATLAS-1 (March 25 to April 2, 1992), STS-55/ATLAS-2 (April 8 to 16, 1993), and STS-66/ATLAS-3 (November 3 to 12, 1994). Data are written to separate files grouped by mission (sl3, at1, at2 or at3), and occultation type (sunrise or sunset) and number. A similar product (ATMOSL2TT) exists that contains these same data in a spreadsheet friendly tab delimited format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atmosl2tt&quot;&gt;ATMOSL2TT&lt;/h4&gt;
This is the version 3 Atmospheric Trace Molecule Spectroscopy (ATMOS) Level 2 product containing trace gases on a vertical potential temperature (theta) grid with data stored in an ASCII table using a spreadsheet friendly tab delimited format. ATMOS is an infrared spectrometer (a Fourier transform interferometer) designed to derive vertical concentrations of various trace gases in the atmosphere, particularly the ozone depleting chlorine and fluorine based molecules. Measured species include: H2O, CO2, O3, N2O, CO, CH4, NO and NO2 (both diurnally and not diurnally corrected), HNO3, HF, HCl, OCS, H2CO, HOCl, H2O2, HO2NO2, N2O5, ClONO2, HCN, CH3F, CH3Cl, CF4, CCl2F2, CCl3F, CCl4, COF2, C2H6, C2H2, N2, CHF2Cl, HCOOH, HDO, SF6 and CH3D reported at 53 levels from 280 to 3950 K. Data files also include time, geolocation and other information. The data were collected during four space shuttle missions: STS-51B/Spacelab 3 (April 30 to May 1, 1985), STS-45/ATLAS-1 (March 25 to April 2, 1992), STS-55/ATLAS-2 (April 8 to 16, 1993), and STS-66/ATLAS-3 (November 3 to 12, 1994). Data are written to separate files grouped by mission (sl3, at1, at2 or at3), and occultation type (sunrise or sunset) and number. A similar product (ATMOSL2TF) exists that contains these same data in a FORTRAN friendly fixed field format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atmosl2pf&quot;&gt;ATMOSL2PF&lt;/h4&gt;
This is the version 3 Atmospheric Trace Molecule Spectroscopy (ATMOS) Level 2 product containing trace gases on a vertical pressure (atm) grid with data stored in an ASCII table using a FORTRAN friendly fixed field format. ATMOS is an infrared spectrometer (a Fourier transform interferometer) designed to derive vertical concentrations of various trace gases in the atmosphere, particularly the ozone depleting chlorine and fluorine based molecules. Measured species include: H2O, CO2, O3, N2O, CO, CH4, NO and NO2 (both diurnally and not diurnally corrected), HNO3, HF, HCl, OCS, H2CO, HOCl, H2O2, HO2NO2, N2O5, ClONO2, HCN, CH3F, CH3Cl, CF4, CCl2F2, CCl3F, CCl4, COF2, C2H6, C2H2, N2, CHF2Cl, HCOOH, HDO, SF6 and CH3D reported at 85 levels from 1 to 10-7 atm. Data files also include time, geolocation and other information. The data were collected during four space shuttle missions: STS-51B/Spacelab-3 (April 30 to May 1, 1985), STS-45/ATLAS-1 (March 25 to April 2, 1992), STS-55/ATLAS-2 (April 8 to 16, 1993), and STS-66/ATLAS-3 (November 3 to 12, 1994). Data are written to separate files grouped by mission (sl3, at1, at2 or at3), and occultation type (sunrise or sunset) and number. A similar product (ATMOSL2PT) exists that contains these same data in a spreadsheet friendly tab delimited format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atmosl2pt&quot;&gt;ATMOSL2PT&lt;/h4&gt;
This is the version 3 Atmospheric Trace Molecule Spectroscopy (ATMOS) Level 2 product containing trace gases on a vertical pressure (atm) grid with data stored in an ASCII table using a spreadsheet friendly tab delimited format. ATMOS is an infrared spectrometer (a Fourier transform interferometer) designed to derive vertical concentrations of various trace gases in the atmosphere, particularly the ozone depleting chlorine and fluorine based molecules. Measured species include: H2O, CO2, O3, N2O, CO, CH4, NO and NO2 (both diurnally and not diurnally corrected), HNO3, HF, HCl, OCS, H2CO, HOCl, H2O2, HO2NO2, N2O5, ClONO2, HCN, CH3F, CH3Cl, CF4, CCl2F2, CCl3F, CCl4, COF2, C2H6, C2H2, N2, CHF2Cl, HCOOH, HDO, SF6 and CH3D reported at 85 levels from 1 to 10-7 atm. Data files also include time, geolocation and other information. The data were collected during four space shuttle missions: STS-51B/Spacelab 3 (April 30 to May 1, 1985), STS-45/ATLAS-1 (March 25 to April 2, 1992), STS-55/ATLAS-2 (April 8 to 16, 1993), and STS-66/ATLAS-3 (November 3 to 12, 1994). Data are written to separate files grouped by mission (sl3, at1, at2 or at3), and occultation type (sunrise or sunset) and number. A similar product (ATMOSL2PF) exists that contains these same data in a FORTRAN friendly fixed field format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;eole1&quot;&gt;EOLE1&lt;/h4&gt;
The Eole 1 Raw Temperature, Pressure and Location Data Near 200 mbar product was obtained from the experimenter and originally consisted of a BCD tape generated on a CDC 6600 computer, subsequently converted to ASCII characters. The data are arranged sequentially by orbit. Data from each orbit are contained in a single record and consist of a heading giving the orbit number, the number of balloons contacted, and a control number. Following the heading, the balloon number, date of observation, location, and ambient temperature and pressure are listed. A maximum of 25 balloon contacts may appear in a single record. Empty records with no balloon contacts have been omitted. These data were obtained from balloons near 200 mbar and are for the region between 30 deg S and 60 deg S. The upper level wind speed and direction can be generated from these data by comparing individual balloon locations obtained from successive orbits. Eole, also known as the Cooperative Application Satellite (CAS-A), was the the second French experimental relay and meteorological satellite and the first launched by NASA under a cooperative agreement with the Centre National d&amp;#39;Etudes Spatiales (CNES).
&lt;br&gt;&lt;h4 id&#x3D;&quot;exp7l1trtwht&quot;&gt;EXP7L1TRTWHT&lt;/h4&gt;
Explorer-7 Thermal Radiation Experiment Selected White Sensor Temperature (Nighttime) Values product contains the temperatures measured by the white sensor at night. The white sensor was designed to measure terrestrial radiation. There is a single file for the entire mission (Nov. 15, 1959 to May 24, 1960). The data were originally written on IBM 7094 machines to magnetic tapes. In addition to the temperature values, the file contains radiance, geolocation and orbit information. The data have been restored and are archived in their original IBM EBCDIC text format. The Explorer-7 satellite was successfully launched on October 13, 1959. The radius of the circle of coverage was about 23 deg (&lt;del&gt;2500 km) at perigee and 31.5 deg (&lt;/del&gt;3500 km) at apogee. Half the radiation is received from an area below the satellite with a radius of 5.3 deg (545 km) at perigee and 9 deg (~1015 km) at apogee. The Thermal Radiation Experiment successfully returned the first set of Earth looking data from space. The instrument was operational from launch until Feb. 28, 1961. The Principal Investigator for these data was Verner E. Suomi from the University of Wisconsin. This product was previously available from the NSSDC with the identifier ESAD-00248 (old ID 59-009A-01A).
&lt;br&gt;&lt;h4 id&#x3D;&quot;exp7l1trtall&quot;&gt;EXP7L1TRTALL&lt;/h4&gt;
Explorer-7 Thermal Radiation Experiment Temperature Values from All Sensors product contains temperature readings from all five bolometers in order to measure solar, reflected and terrestrial radiation. There are two files for the entire mission (Oct. 19, 1959 to April 16, 1960 and April 16, 1960 to June 4, 1960. Note there is no geolocation information included with these data. The data were originally written on IBM 7094 machines on magnetic tapes. The data have been restored and are archived in their original IBM 36-bit word binary format. The Explorer-7 satellite was successfully launched on October 13, 1959. The radius of the circle of coverage was about 23 deg (&lt;del&gt;2500 km) at perigee and 31.5 deg (&lt;/del&gt;3500 km) at apogee. Half the radiation is received from an area below the satellite with a radius of 5.3 deg (545 km) at perigee and 9 deg (~1015 km) at apogee. The Thermal Radiation Experiment successfully returned the first set of Earth looking data from space. The instrument was operational from launch until Feb. 28, 1961. The Principal Investigator for these data was Verner E. Suomi from the University of Wisconsin. This product was previously available from the NSSDC with the identifier ESAD-00249 (old ID 59-009A-01B).
&lt;br&gt;&lt;h4 id&#x3D;&quot;geos2obsinputintl&quot;&gt;GEOS2OBSINPUTINTL&lt;/h4&gt;
GEOS2OBSINPUTINTL is the optical beacon system data product which contains reduced raw geodetic optical observations obtained by various international camera systems. These data were used as input to the Quality Control Program to create the product called the International Optical Beacon Pass Summary Data. The optical beacon system, used for geometric geodesy studies, consisted of four xenon flash tubes programmed to flash sequentially, in a series of five or seven flashes. Data are available for the time period from 1968-02-20 to 1968-10-03 in a single file with 1689 data records where each is a line of ASCII text.\n\nThe principal investigator for the Optical Beacon System experiment was R. E. Williston from APL. A previous version of this instrument flew on the first GEOS-1 satellite.
&lt;br&gt;&lt;h4 id&#x3D;&quot;geos3stst&quot;&gt;GEOS3STST&lt;/h4&gt;
GEOS3STST is the satellite-to-satellite tracking data product which contains observations, obtained from the S-band transponders on GEOS 3 relayed by the ATS 6 spacecraft to various ground stations, used for geodetic studies. Data are available for the time period from 1975-04-13 to 1976-04-28 in sixteen files, written in ASCII text, where each measurement is recorded as two lines of text.\n\nThe principal investigator for the Satellite-to-Satellite Tracking experiment was Indalecio Y. Galicinao from NASA/GSFC.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA ESDIS Project</title>
      <link>https://registry.opendata.aws/nasa-esdis</link>
      <guid>https://registry.opendata.aws/nasa-esdis</guid>
      <description>This is a global simulation of black carbon (BC) aerosol concentrations and daily deposition (wet+dry) from the FLEX-ible PARTicle (FLEXPART) Lagrangian particle dispersion model version 10.4. The FLEXPART model code are open source and freely available.
&lt;br&gt;&lt;h4 id&#x3D;&quot;dustflexpart&quot;&gt;DUSTFLEXPART&lt;/h4&gt;
This is a global simulation of mineral dust aerosol concentrations and daily deposition (wet+dry) from the FLEX-ible PARTicle (FLEXPART) Lagrangian particle dispersion model version 10.4. The FLEXPART model code are open source and freely available.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ocflexpart&quot;&gt;OCFLEXPART&lt;/h4&gt;
This is a global simulation of organic carbon (OC) aerosol concentrations and daily deposition (wet+dry) from the FLEX-ible PARTicle (FLEXPART) Lagrangian particle dispersion model version 10.4. The FLEXPART model code are open source and freely available.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA FIFE Project</title>
      <link>https://registry.opendata.aws/nasa-fife</link>
      <guid>https://registry.opendata.aws/nasa-fife</guid>
      <description>An inventory of NASA&amp;#39;s airborne and field campaigns for Earth Science
&lt;br&gt;&lt;h4 id&#x3D;&quot;fife_hydrology_strm_15m_1&quot;&gt;fife_hydrology_strm_15m_1&lt;/h4&gt;
The Fifteen Minute Stream Flow Data from the USGS Data Set contains 15 minute stream flow data from the USGS station located 2.9 miles upstream from the mouth of Kings Creek. The record extends from April 1, 1979 through September 2, 1988. The purpose of this data set was to provide accurate measurements of the stream flow from Kings Creek so that a water budget analysis for the northwest quadrant of the FIFE study area could be performed. The stilling pipe installed at the USGS station operates on the principle that the water level in a standpipe at a specific location within a stream bed can be converted to a volume of water in the stream bed. The tracking of the change in stream height with time then enables the calculation of stream flow.
&lt;br&gt;&lt;h4 id&#x3D;&quot;fife_sur_met_rain_30m_2&quot;&gt;fife_sur_met_rain_30m_2&lt;/h4&gt;
The FIFE Thirty Minute Rainfall Data Data Set contains data from thirty rain gauges located in the Kings Creek basin in the northwest corner of the FIFE study area during 1987. Reliability of the gauges were such that at any particular time, data from approximately 20 were recovered. The high temperatures and humidity, plus software problems in the loggers, resulted in data losses. The collected data were of high quality and sufficiently many gauges were working that the structure of the raincells can be observed from the gauge data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;fife_af_dtrnd_nae_3&quot;&gt;fife_AF_dtrnd_nae_3&lt;/h4&gt;
The purpose of this study was to develop alternatives to ground-based measurements in order to obtain information required to predict the effects of soil and land use on the fluxes of greenhouse gases, the surface energy balance, and the water balance. Satellite-based algorithms have been developed via flux measurements from an aircraft to estimate vegetation and soil conditions on a regional scale. The purpose of the Twin Otter FIFE flights was to make measurements in the boundary layer of the fluxes of sensible and latent heat, momentum, and carbon dioxide, plus supporting meteorological parameters such as temperature, humidity, wind speed, and direction. Aircraft position, heading, and altitude were also recorded, as were several radiometric observations for use in interpretation of these data. The Twin Otter aircraft allows steady flight trajectories at low airspeed (50-60 [m][sec^-1]) down to levels less than 10 m above the ground. The aircraft is instrumented to measure the contribution of flux densities of momentum, sensible, and latent heat, and CO2 over a frequency range of 0 to 5 Hz (MacPherson et al., 1981). All the flux measurements were obtained with the eddy-correlation method, wherein the aircraft is equipped with an inertial platform, accelerometers, and a gust probe for measurement of earth-relative gusts in the x, y, and z directions. Gusts in these dimensions are then correlated with each other for momentum fluxes and with fluctuations in other variables to obtain the various scalar fluxes, such as temperature (for sensible heat flux) and water vapor mixing ratio (for latent heat flux). The fluctuations in all variables were calculated with three different methods (the arithmetic means removed, the linear trends removed, or filtered with a high-pass recursive filter) prior to the eddy correlation calculations. This data set contains the linearly detrended data. Through this research, it is hoped that techniques can be developed to utilize satellite data for global monitoring of crop health and climate change.
&lt;br&gt;&lt;h4 id&#x3D;&quot;fife_af_dtrnd_wyo_4&quot;&gt;fife_AF_dtrnd_wyo_4&lt;/h4&gt;
The University of Wyoming (UW) King Air atmospheric boundary layer measurement missions were flown in 1987 during IFCs 3 and 4. This Boundary Layer Fluxes data set contains parameters that describe the environment in which the flux data were collected and the flux data itself . The fluctuations in all variables were calculated with three different methods (the arithmetic means removed, the linear trends removed, or filtered with a high-pass recursive filter) prior to the eddy correlation calculations. This data set contains the linearly detrended data. All the flux measurements were obtained with the eddy-correlation method, wherein the aircraft is equipped with an inertial platform, accelerometers, and a gust probe for measurement of earth-relative gusts in the x, y, and z directions. Gusts in these dimensions are then correlated with each other for momentum fluxes and with fluctuations in other variables to obtain the various scalar fluxes, such as temperature (for sensible heat flux) and water vapor mixing ratio (for latent heat flux). The summary of data calculated from each aircraft pass includes various statistics, correlations, and fluxes calculated after the time series for each variable with the linear trends removed.
&lt;br&gt;&lt;h4 id&#x3D;&quot;fife_af_dtrnd_ncar_5&quot;&gt;fife_AF_dtrnd_ncar_5&lt;/h4&gt;
The NCAR King Air participation in FIFE-1987 and FIFE-1989 was part of a coordinated atmospheric boundary layer component which included other aircraft, surface measurements, balloon-borne profiles, SODAR, and lidar remote sensing. The chief objective of the boundary layer component was to describe the structure of the atmospheric boundary layer over the FIFE study area, increase knowledge of the physical processes active in the daytime boundary layer, and explore the relationship of surface properties to the time and spatial variation in the structure of the boundary layer. The phenomena studied were the daytime convective boundary layer structure and physical processes. This study used airborne measurement of vertical and horizontal wind gusts, humidity, potential temperature, mean horizontal wind speed, and horizontal linear trends of temperature, humidity, radiation. Fluxes of sensible heat, moisture, and momentum were estimated from fast response wind gust, temperature, and humidity measurements; these fluxes were evaluated from data whose linear trend and mean were removed. In addition several radiation parameters were also measured.. Several radiation parameters were also measured (e.g., global short and longwave, upwelling, and downwelling). Altitude of the aircraft was measured by radar and pressure; radar was more accurate but was only valid below about 930 m. Geographical position was measured by an inertial navigation system. All level legs of a flight mission were flown at a constant pressure altitude, thus the altitude of the aircraft over the surface varied. In general, the detrended data set is of excellent overall quality with very little loss of data. Vertical winds were sampled at an effective rate of 5 samples per second instead of the customary 10 samples per second; this had negligible effect on the fluxes but could compromise estimates of turbulence dissipation. Fluxes were estimated using raw, detrended and high-pass filtered data. From extensive analysis the FIFE Boundary Layer Group recommends using the detrended data.
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The NCAR King Air participation in FIFE-1987 and FIFE-1989 was part of a coordinated atmospheric boundary layer component which included other aircraft, surface measurements, balloon-borne profiles, and SODAR and lidar remote sensing. The chief objective of the boundary layer component was to describe the structure of the atmospheric boundary layer over the FIFE study area, increase knowledge of the physical processes active in the daytime boundary layer, and explore the relationship of surface properties to the time and spatial variation in the structure of the boundary layer. The phenomena studied were the daytime convective boundary layer structure and physical processes. This study used airborne measurement of vertical and horizontal wind gusts, humidity, potential temperature, mean horizontal wind speed, and horizontal linear trends of temperature, humidity, radiation. Fluxes of sensible heat, moisture, and momentum were estimated from fast response wind gust, temperature, and humidity measurements; these fluxes were evaluated from data which had been high pass filtered with a third order algorithm with a break point set at 0.012 Hz (5 km wavelength). Several radiation parameters were also measured (e.g., global short and longwave, upwelling, and downwelling). Altitude of the aircraft was measured by radar and pressure; radar was more accurate but was only valid below about 930 m. Geographical position was measured by an inertial navigation system. All level legs of a flight mission were flown at a constant pressure altitude, thus the altitude of the aircraft over the surface varied. In general, the data set is of excellent overall quality with very little loss of data. Vertical winds were sampled at an effective rate of 5 samples per second instead of the customary 10 samples per second; this had negligible effect on the fluxes but could compromise estimates of turbulence dissipation. From extensive analysis the FIFE Boundary Layer Group recommends using the detrended data rather than the filtered data.
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The University of Wyoming (UW) King Air atmospheric boundary layer measurement missions were flown in 1987 during IFCs 3 and 4. This Raw Boundary Layer Fluxes data set contains parameters that describe the environment in which the flux data were collected and the flux data itself. The fluctuations in all variables were calculated with three different methods (the arithmetic means removed, the linear trends removed, or filtered with a high-pass recursive filter) prior to the eddy correlation calculations. This data set contains the data with the arithmetic means removed (i.e., RAW). All the flux measurements were obtained with the eddy-correlation method, wherein the aircraft is equipped with an inertial platform, accelerometers, and a gust probe for measurement of earth-relative gusts in the x, y, and z directions. Gusts in these dimensions are then correlated with each other for momentum fluxes and with fluctuations in other variables to obtain the various scalar fluxes, such as temperature (for sensible heat flux) and water vapor mixing ratio (for latent heat flux). The summary of data calculated from each aircraft pass includes various statistics, correlations, and fluxes calculated after the time series for each variable with the arithmetic means removed.
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As part of the FIFE staff science data collection effort, the FIFE Information System (FIS) processed and archived 5 minute, near-surface radiometric and meteorological information collected by the Automated Meteorological Stations (AMS) distributed over the FIFE study area. The FIFE AMS Data Set contains the two output products created. The level-1 product contains unpacked 5 minute data. The level-1a product contains 30 minute averages of these data. All AMS stations were equipped to measure air temperature, humidity, wind speed, soil temperature, reflected solar radiation, net radiation, surface temperature, and precipitation. Two stations were augmented with extra radiation sensors to become super-AMS (SAMS). These stations measured total radiation, direct solar radiation, diffuse solar radiation, photosynthetically active radiation, and downward longwave radiation.
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The NOAA Radiosonde Observations - 1989 (NCDC) Data Set contains radiosonde data obtained from the National Climatic Data Center (NCDC). These 396 days of data cover 13 months from October 1988 through October 1989. These data were collected using sondes released in Dodge City and Topeka Kansas, 337 km and 68 km, respectively, from the FIFE study area. Radiosonde observations were made to determine the pressure, temperature, and humidity from the surface to the point where the sounding was terminated. It is assumed that the use of these data is applicable to the FIFE study because these meteorological data are relatively stable in the horizontal domain. These data may be used as input to numerical models, as well as verification data for simulation studies.
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The FIFE Standard Pressure Level Radiosonde Data Set provides a set of standard level profiles (i.e., 5 mb pressure intervals) from over 450 radiosonde balloon flights, which occurred every one to three hours (daylight hours) during the FIFE IFCs. This derived profile data were computed to 5 mb pressure intervals through simple linear interpolation means. An assumption exists that a linear interpolation scheme may be used with sufficient accuracy to assign meteorological values at 5 mb pressure levels. Some errors are introduced using this method. Several new variables were computed from the original FIFE Radiosonde Data and are included in this derived data set. U (east-west) and V (north-south) winds have been computed from wind speed and direction, and potential temperature has been computed from pressure and temperature. These new parameters are desirable for initial conditions in numerical models as well as forcing functions in models, or as verification and comparison of numerical model&amp;#39;s results.
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The FIFE Radiosonde Data Set contains temperatures, wind speed, and temperature profiles in the atmospheric boundary layer measured by means of radiosondes that were analyzed in the framework of Monin-Obukhov similarity theory, with the objective of determining the regional surface heat flux. Profiles of temperature, humidity and wind velocity in the atmosphere were measured by means of intensive radiosoundings conducted approximately between 900 and 1800 CDST in northeastern Kansas during the five FIFE Intensive Field Campaigns in spring, summer and fall of 1987, and in the late summer of 1989. Some 445 radiosondes were released to generate the measurements needed to obtain profiles of wind velocity dry-bulb and wet-bulb temperature. The launch site was located near the northern edge of the experimental area to ensure that these profiles reflect surface conditions over the fetch of the experimental area in the general direction of the prevailing southerly wind. The raw radiosonde data described here have been corrected for sensor delays (see the FIFE Temperature and Humidity Profiles) and algorithm inconsistencies, (see the FIFE Radiosonde Wind Profiles) and have been interpolated to a set of standard pressure levels (see the FIFE Standard Pressure Level Radiosonde Data). These derived data sets are described separately.
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The TOVS data were acquired from NOAA/NESDIS to monitor atmospheric conditions that occurred over the FIFE study area during 1987. The TOVS data were obtained from NESDIS in the standard TOVS sounding product format containing atmospheric sounding data for NOAA-9 and NOAA-10 satellites over the FIFE study area. The TOVS sounding products information is derived from three sensors which measure the intensity of upwelling radiation in the various spectral intervals that occur at maxima over broad layers and depths of the atmosphere. These radiance measurements are processed into Earth-located, calibrated radiance values, &amp;quot;clear&amp;quot; radiances (radiances corrected for cloud effects and angle-of-view), estimates of water vapor in three atmospheric layers (converted to precipitable water in these layers), mean temperatures for selected atmospheric layers, tropopause height and temperature estimates, and geopotential thickness of selected atmospheric layers.
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The Volume Imaging LIDAR (VIL) system of the University of Wisconsin, operated during FIFE and all LIDAR return signals measured at a 90 degree elevation angle were averaged and stored in a file. From plots of those profiles, clouds up to 15 km AGL can be identified. By choosing appropriate reflectivity levels, the data from the University of Wisconsin LIDAR have been used to derive unique 2-D and 3-D views of the Atmospheric Boundary Layer (ABL) structure and the variations in that structure with time. Some of these views are available in the GRAB BAG directory on FIFE CD-ROM Volume 1. Color videos were also produced and are available from the Archive listed in Section 13.1. These views and videos provide important insights into many problems facing investigators in all aspects of FIFE, including scaling and the representativeness of point and line samples.
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The acoustic sounder (SODAR) maps the amplitude of backscattered acoustic energy associated with temperature fluctuations and thus thermal inversions in the atmosphere. The aim of the SODAR measurements was to provide estimates of the height of the mixed layer and the vertical dimensions of inversions within the lower kilometer of the atmosphere. A single, vertically pointing, conventional SODAR was operated at an acoustic frequency near 1500 Hz to detect the amplitude of backscattered acoustic energy. The thickness of an elevated inversion as seen by the SODAR is often smaller than the difference between the heights of the inversion top and bottom, because of oscillations in the heights that occur. The heights were estimated only for the inversions that were clearly associated with the active mixed layer. These data were collected at one location in the northwest quadrant of the FIFE study area during the first three Intensive Field Campaigns held in 1987.
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Surface flux measurements were made at selected sites within the FIFE area. Each surface flux station was capable of measuring the fluxes of net radiation, sensible heat, and latent heat. The Bowen ratio stations measured the soil heat flux as well. The surface flux and micrometeorological measurements available in this data set were collected from 15 locations within the FIFE study area between 1987 and 1989. Six automatic surface energy and radiation balance systems were operated continuously for 144 days from May 16 to October 16, 1987. Variables including net radiation, air temperature, vapor pressure and wind speed, were quite similar for the sites even though the sites were as much as 10 km apart and represented the four cardinal slopes and a top. The Bowen ratio was low during most of the season, increasing sharply toward the end of the season after a long dry spell. The average Bowen ratio was 0.35. About 72% of the available energy was converted into latent heat flux density. Since the data systems and instrumentation used were of similar design, the variability in results can be ascribed to treatment and locations. These results can be used to estimate the number of stations needed to represent a rolling prairie topography.
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The Bowen Ratio Surface Flux Observations (GSFC) Data Set contains data collected using the Bowen Ratio Techniques. The major data collection effort was conducted in 1987 when 16 stationary sites were equipped with Bowen ratio equipment by different groups. Surface flux measurements were made at selected sites within the FIFE area. All measurements are from a single upland site that was grazed. This station measured the fluxes of net radiation, sensible heat, and latent heat and several micrometeorological parameters.
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The Bowen Ratio Surface Flux Observations (KSU) Data Set contains surface flux measurements made at selected sites within the FIFE area. The sites were equipped with Bowen ratio equipment that was operated by several different groups. Each surface flux station was capable of measuring the fluxes of net radiation, latent heat and sensible heat. The Bowen ratio stations measured the soil heat flux as well. The components of the energy balance were determined with the Bowen Ratio Energy Balance (BREB) method. The BREB is a combination of the transport and the energy balance equations. The surface flux and micrometeorological measurements available in this data set were collected from 23 locations with 27 site identifiers from 1987 through 1989. Thirteen of these locations were instrumented with stationary bowen ratio systems which collected daily measurements for months. These systems were all located in the northwest quadrant of the FIFE study area within the Konza Prairie Natural Research Area. Ten locations were instrumented in 1987 for a few days at a time with a portable Bowen ratio system. This roving system visited all but the southeast quadrant of the FIFE study area.
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The Bowen Ratio Surface Flux Observations (Smith) Data Set contains surface flux measurements made at selected sites within the FIFE area. The collection effort was conducted in 1987, 1988, and 1989 from sites equipped with Bowen ratio equipment operated by several different groups. Each surface flux station was capable of measuring the fluxes of net radiation, sensible heat, and latent heat using. The Bowen ratio stations measured the soil heat flux as well. The surface flux and micrometeorological measurements available in this data set were collected from 2 locations within the FIFE study area. One of these sites was located at the bottom of a valley while the other was on the top of a ridge. During the IFC&amp;#39;s data were collected daily.
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The Bowen Ratio Surface Flux Observations (UNL) Data Set contains surface flux and micrometeorolgical measurements collected at one location located in a flat area of uniform surface vegetation approximately in the center of the FIFE study area. The data collection effort was during the four Intensive Field Campaigns in the spring, summer, and fall of 1987 (May 28 - Oct 17). The Bowen ratio system that collected these data was designed to retrieve all major components of the surface energy budget along with a large set of measured and derived parameters describing the dynamical, thermodynamical, hydrological, and radiative properties of the ground surface and atmosphere surface layer.
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The Bowen Ratio Surface Flux Observations (USGS) Data Set contains surface flux and micrometeorological collected from one location within the Northwest quadrant of the FIFE study area. Data were collected daily at this location only during the IFC&amp;#39;s during the period from late May through mid-October, 1987. Each Bowen ratio station was capable of measuring the fluxes of net radiation, sensible heat, and latent heat. The Bowen ratio stations measured the soil heat flux as well.
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The Canopy Photosynthesis Data Set data were collected from five sites within the FIFE study area during July 1, 1987 through October 12, 1987. The objectives of the study were to estimate canopy photosynthetic rates, respiration rates, and bulk stomatal resistance. Photosynthesis was measured by monitoring the net exchange of CO2 from the canopy to the atmosphere while the canopy is enclosed in a Plexiglas chamber equipped with a LI-COR CO2 gas analyzer. The rate of CO2 concentration change over intervals of 10 - 20 seconds is measured. This CO2 concentration rate of change is used along with other factors (e.g., the amount of canopy area enclosed, the volume of the enclosure, and temperature) to estimate the net photosynthesis rate. The stomatal resistance and conductance is calculated from the total leaf resistance (i.e., calculated via the transpiration rate along with the leaf and air temperatures) minus the boundary layer resistance. Stomatal resistance of selected species of the grass used to estimate the total canopy resistance were measured independently using a leaf diffusion porometer. The results showed that estimated values of net CO2 flux varied between about 0.25 and 1.0 [mg][m^-2][sec^-1] during IFC-2 and IFC-3, and around zero during IFC-4. Resistances ranged from 80 [sec][m^-1] to 300 [sec] [m^-1] during IFC-2 and IFC-3, rising to very high values (greater than 1000 [sec][m^-1]) during IFC-4.
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The FIFE Cloud Camera Data Data Set was collected to document distribution of clouds during FIFE, evaluate algorithms for identifying presence of thin cirrus, and popcorn cumulus clouds, and evaluate the impact of these clouds on retrieval of surface fluxes from satellite data. Clouds could be remotely sensed from both the surface and from satellites. Unlike surface properties, cloud parameters are incompletely retrieved from above or below; there is no ground truth for cloud retrieval algorithms. A camera fitted with a whole-sky (&amp;quot;fish-eye&amp;quot;) lens and positioned so that it points directly upwards can capture a full horizon-to-horizon image of the sky dome. Careful film and filter combinations permit differentiation of cloud types. The mathematical mapping of a spherical surface onto a flat surface uses nomenclature from the cartographic community, where the development of techniques for mapping the surface of the earth has a long history. Cartographic projections are precise, mathematically defined &amp;#39;mappings&amp;#39; and, as a consequence, this nomenclature has been adopted in describing whole-sky camera photographs (Herbert 1986; McGuffie and Henderson-Sellers 1989). Analysis of the camera data showed considerable temporal variability indicating that synoptic observation of cloud was not adequate. There is indication that the NOAA station report convention (clear, scattered, broken, and overcast) from the nearest synoptic NOAA surface stations (Manhattan Airport, and Fort Riley airfield) were used instead of true okta cloud observations, in the NOAA data.
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The FIFE Daily Rainfall Data Set contains daily precipitation values for 42 rain gauge stations within the Konza LTER portion of the FIFE site (i.e., Northwest quadrant). The data set is a composite of data collected by the LTER staff and the Princeton University group. The LTER staff collected daily precipitation data from 12 of the 42 rain gauge stations within this area with the Princeton University group collecting 30 minute precipitation data from the remaining 30 stations. LTER data was collected from April 1982 through December 1989. Data collected by the LTER staff was year round for some stations and from April 1 to October 31 for others. The Princeton University group collected data from May 1987 to October 1987. The Princeton University 30 minute precipitation data was converted to daily precipitation data by the FIS staff. At any particular time, data from approximately 20 of the 30 Princeton University stations were recovered. High temperatures and humidity, plus software problems in the rainfall data loggers, resulted in these data losses. The collected data were of high quality and enough gauges were working at all times so that rain cells could be observed using these data.
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The Eddy Correlation Surface Flux Observations (Argonne) Data Set contains surface flux measurements made at selected sites within the FIFE study area. The surface area and aerological data described here were located at 2 sites in the northwest quadrant of the study area within the Konza Prairie Natural Research area. Both sites were located on hill tops that were burnt on a regular cycle. These data were collected daily only during the five Intensive Field Campaigns which were held during the growing season of 1987 and the projected summer dry down in 1989. Data were also collected using a portable eddy correlation system that moved to a variety of locations within the FIFE study area. These data were collected for a day or two at each location sometime between June 1, 1987 and October 13, 1987. Argonne National Laboratory did not measure radiation but concentrated on observations of turbulence quantities, primarily covariances and standard deviations of winds, temperature, water vapor, and other quantities. The surface fluxes and standard deviations of carbon dioxide and ozone were measured by Argonne so that the fluxes of mass could be related to each other, surface biophysical conditions, vegetative parameters, and the optical characteristics of the surface that could be detected by remote sensing.
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The Eddy Correlations Surface Flux Observations (GSFC) Data Set contains surface flux measurements made at selected sites within the FIFE study area. The surface flux and micrometeorological measurements in this data set were collected from a single location located in the southwest quadrant on a upland, grazed area. The data set contains data collected daily from June 26 - October 17, 1987 during the three Intensive Field Campaigns. No data is available between the campaigns. Micrometeorological techniques of eddy correlation and Bowen ratio were used in determining the fluxes of sensible heat, latent heat, and carbon dioxide in FIFE. Eddy correlation is a well-established technique that has the primary advantage of measuring turbulent diffusive fluxes directly across a near-horizontal plane above the surface. It requires a rigid platform unencumbered by significant aerodynamic obstacles. The fluxes of sensible and latent heat are computed as covariances of the fluctuations of vertical wind velocity with fluctuations of temperature and vapor density at the same point and time.
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Surface flux measurements were made at selected sites within the FIFE study area. Each surface flux station was capable of measuring the fluxes of net radiation, sensible heat, and latent heat. The Eddy Correlation Surface Flux Observations (UK) Data Set contains surface flux and micrometeorological measurements collected from one location in the southwest quadrant of the FIFE study area. This location was grazed and had a gentle downhill slope to the southwest. Data were collected daily from May 14 - October 18, 1987, and from July 21 - August 16, 1989. The output from the Hydra sensors is sampled at 10 Hz and processed in real time to give hourly averages of sensible and latent heat flux and the friction velocity. The hourly mean values of net radiation, temperature, and of vapor pressure, provided in this data are a synthesis of the best measurements available for this site. The temperature measurement provided here is the preferred value for this site. This temperature was used to calculate the fluxes and some standard deviations. This is necessary because the sonic anemometer has a slightly temperature dependent calibration. The average soil heat flux measured at 5 mm depth is a weighted average value over three sample positions with dense, medium and sparse vegetation. A vegetation survey was made to assign weights to these three classes at this site. The spatial variability in this measurement at this (over) grazed site is particularly high and the three individual sensors commonly measure soil heat fluxes differing by factors of two or three. Some evidence suggests these data are providing a measurement of this component of the energy budget for this site which is biased low. Presumably this is because the limited number of sensors inadequately samples the points with low canopy density for this sparse crop cover.
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Surface flux and micrometeorological measurements were collected at one site within the northwest quadrant near the center of the FIFE study area during all five of the Intensive Field Campaigns (four in 1987 and one in 1989). This site had historically been ungrazed but had recently been exposed to grazing. The station was capable of measuring the fluxes of net radiation, sensible heat and latent heat using an eddy correlation system. In addition, measurements of soil heat flux and several micrometeorological parameters were made.
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This data set provides aircraft-based NS001 Thematic Mapper Simulator (TMS) images of the study area associated with The First ISLSCP (International Satellite Land Surface Climatology Project) Field Experiment (FIFE) project conducted on the Konza Prairie in Kansas. The images were acquired during June 1987 to August 1989. The images in this data set were originally provided on the FIFE CD-ROM Volume 3.
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Airborne soil moisture measurement is based on the difference between natural terrestrial gamma radiation flux measured for comparatively wet and dry soils. The presence of moisture in the soil causes an effective increase in the soil density resulting in an increased attenuation of the gamma flux for relatively wet soil and a correspondingly lower flux at the ground surface. As part of the FIFE experiment, natural terrestrial gamma radiation data over a network of 24 flight lines were collected. The data acquisition procedure was designed to accumulate and store spectral radiation data along a flight line from which estimates of soil moisture could be computed. Ground-based soil moisture measurements were used to make a one-time calibration of the natural terrestrial radioisotope signal over the flight line network. A time-series of airborne soil moisture measurements (to a depth of 20 cm) was compared to an extensive, independent data set of ground-based soil moisture measurements. Estimates for flight line segments were found to have an average RMS error of approximately 2.5 % soil moisture (Peck et al., 1990).
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During the 1989 Intensive Field Campaign a Russian spectroradiometer, the Gemma, was used to collect visible and near infrared spectra of a variety of FIFE sites from a helicopter. Gemma measurements of selected study sites and laboratory measurements of a portable calibration light sphere were made. The helicopter missions were designed to provide characterizations of each FIFE site while providing FIFE study area coverage, and to provide an intermediate scale of sampling between that of the surface measurements and the higher altitude aircraft and spacecraft multispectral imaging devices. The Gemma spectroradiometer was mounted on the helicopter to allow a comparison between it and the SE-590 spectroradiometer and Modular Multiband Radiometer (MMR) over a number of sites.
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The FIFE Historic Daily Meteorology Data Data Set is one of the historical data sets used for the FIFE project. The data set contains data back to January, 1900. This data set was prepared for input into models, therefore, no leap days (February 29) are included. Daily weather observations of air temperature and precipitation were made by Kansas State University. The observations are made according to the procedures outlined by the National Weather Service (Anonymous 1989).
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The FIFE Historic Monthly Meteorology Data Data Set is one of the historical data sets used for the FIFE project. This data set provides monthly precipitation values from January 1858 to December 1989 for Manhattan, Kansas adjacent to the FIFE study area. Daily weather observations of precipitation were made according to the procedures outlined by the National Weather Service by Kansas State University. The daily precipitation data were then summed to produce monthly precipitation.
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The purpose of the Leaf Area Index and PAR Determined from KSU Light Bar Measurements study was to collect extensive non-destructive measurements of Leaf Area Index (LAI) at the flux sites during IFC-5 (August 1989). These data were collected at thirteen locations which were coincident with the surface flux measurements within the FIFE study area from July 3, 1989 through August 18, 1989. The various fractions of the Photosynthetically Active Radiation (PAR) (i.e., diffuse, reflected, transmitted and total) were measured using a Line Quantum meter from LI-COR Inc. From these fractions the ratio of reflected to total incoming PAR was computed. LAI can be estimated from light bar measurements of PAR transmittance from measurements above and below a vegetation canopy. The use of the light bar allows rapid, multiple, and repeatable measurements of LAI at the FIFE sites. This type of measurements could not be done using destructive measurements of LAI.
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The Leaf Area Index and PAR Determined from the UNL Light Bar Data were collected in 1987, 1988, and 1989. Incoming, reflected, and transmitted photosynthetically active radiation (PAR) was measured with a LI-COR LI-191SA line quantum sensor. Absorbed and intercepted PAR calculated from these measurements. The objectives of this research were to characterize bi-directional reflectance factor distributions, estimate surface albedo, determine the variability of reflected and emitted fluxes in selected spectral wavebands as a function of topography, vegetative community and management practice, determine the influence of plant water status on surface reflectance factors, and determine sun angle affects on radiation fluxes.
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The prairie is inherently variable and large numbers of samples are needed to obtain reliable estimates of the prairie agronomic characteristics. For the Indirect Leaf Area Index Obtained from the KSU Light Wand Study a limited number of destructive samples were supplemented by large numbers of rapid non-destructive estimates. For the non-destructive measurements the LI-COR Inc. LAI-2000 Plant Canopy Analyzer (light-wand) was used. This instrument measures transmittance of the canopy in the blue region of the spectrum, at five different zenith angles. These measurements were inverted to provide estimates of leaf area index, and mean inclination angle of the leaves to the zenith. Verification studies conducted by LI-COR Inc. indicated that the LAI-2000 Canopy Analyzer measurements were generally within 15% of values obtained by destructive sampling and measurement with a leaf area meter. As a rough guess even the destructive measurements are accurate only to within about 25% of the true sample leaf area value. In the opinion of the study team, the non-destructive measurements with the LAI-2000 are as good as the destructive measurements, and provide a better estimate of the site mean, because many more non-destructive measurement can be made.
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The Leaf Angle Data Data Set contains leaf angle distributions (LAD) obtained during the 1987 growing season for ten types of plant canopies, from the Konza Long-Term Ecological Research (LTER) area. These data were collected using a direct measurement technique (i.e., a Spatial Coordinate Apparatus (SCA)). The species selected were major species common on the prairie with the leaves were of sufficient size to allow SCA measurement. The objective of this study was to obtain detailed LAD information on the major canopy species of the tallgrass prairie and selected agricultural crops. The LAD information for specific canopies can be used as input for a canopy radiation model. Canopy leaf orientation is an important parameter for plant growth modeling. Four categories of zenith angle distributions were found among the 14 species. These were planophile, plagiophile, erectophile, and uniform. Some canopies were found to have non-uniform leaf azimuth angle distribution. Also there were deferences between the upper and lower parts of the canopies for some species.
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The objective of the Leaf Photosynthesis study was to measure the response of leaf photosynthesis and stomatal conductance to light, temperature, vapor pressure deficit, carbon dioxide and water potential for the most abundant C4 species at the FIFE study area. To this end, photosynthesis measurements were made on 6 days in June, July and August of 1987 at three different locations in the northwest quadrant of the FIFE study area. Leaf photosynthetic rate is measured by enclosing a leaf in a closed, transparent chamber and measuring the decrease in carbon dioxide concentration as a function of time. Light flux density is measured outside of the chamber and must be corrected for the chamber transmittance, which is 0.9. These data can be fit to various models of leaf photosynthesis and stomatal conductance by providing the responses to light, temperature leaf water potential, and carbon dioxide under field conditions on intact plants.
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The Incoming Longwave Radiation Data from UNL Data Set was collected as part of a study of thermal radiant energy from vegetative canopies. These data were collected during the growing season of 1987 and 1989. The data measurements were made at 13 stations within 12 sitegrids scattered throughout the FIFE study area. Values for incoming longwave radiation were calculated using the radiometer chopper or detector temperature as a measure of air temperature. When determining surface temperatures from infrared thermometer measurements of the surface, the surface emissivity and the reflected component must be taken into account. The reflected component is dependent on the surface emissivity and the incoming longwave radiation.
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The MMR Calibration Data Set contains radiance data collected in the summer of 1987 and in July and August of 1989 via a Modular Multiband Radiometer (MMR) instrument. The MMR instrument monitored a nearly lambertian calibration panel stationed near the center of the FIFE study area. The radiances recorded from this instrument can be used to monitor solar insolation and clouds. In some cases, these data were also used to calculate the reflectance factor for reflective radiances measured over vegetation using other MMR instruments located at other FIFE sites or mounted on a helicopter.
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Surface reflectance factors, radiances, and temperatures were measured with a Mast-borne Modular Multiband Radiometer (MMR), predominantly in the solar principal plane, with nadir and off-nadir, view-zenith angles. The MMR was mounted on a portable mast in order to achieve a spatial sampling at a variety of sites as well as within each site. The portable mast alignment varied from the solar principal plane, to the azimuthal plane aligned perpendicular to the principal plane and aligned with the satellite azimuthal plane. Measurements were periodically collected with the MMR over a barium sulfate reference panel. Measurements were typically coordinated with aircraft and/or satellite overpasses. Solar radiation data at or near the specific site should be used to screen possible times of variable cloud cover.
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The Surface Reflectance Measured with a Helicopter-borne MMR Data Set contains surface reflectance measurements in Landsat-TM bands at low to intermediate altitudes. The helicopter operated during all Intensive Field Campaigns (IFCs) and was available to support all satellite overpasses. The average flight time was 2 hours, during which an average of 11 FIFE sites plus one special target were covered. The helicopter missions were designed to provide a rapid means of intensively spectrally characterizing each FIFE site while providing FIFE study area coverage, and to provide an intermediate scale of sampling between that of the surface measurements and the higher altitude aircraft and spacecraft multispectral imaging devices. The Modular Multiband Radiometer (MMR) instrumentation was chosen to provide compatibility with surface-based radiometers and TM spacecraft sensors. Off-nadir measurements were made as a means of providing more accurate estimates of hemispherical reflectance and for use with bi-directional reflectance models.
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The Leaf Optical Properties from UNL Data Set contains leaf-level spectral observations acquired in situ with the Nebraska Multiband Leaf Radiometer (NMLR) coupled with a LiCor LI-1800-12 integrating sphere. The NMLR measured leaf reflectance and transmittance in the seven MMR bands. Data were collected in 1987, 1988, and 1989. During 1987, measurements were always made on the most recently expanded leaf of the selected plant. Measurements were made on a variety of forbs and grasses. During 1988, measurements were made on the most recently expanded leaf of the selected plant unless specified. Measurements were also made of older green, yellow and brown leaves on a plant. Measurements were usually made on grasses (i.e., Indian grass, Switch grass and Big bluestem). A few forbs were measured. The same leaf was sometimes measured throughout the day. During 1989, measurements were usually made on the most recently expanded leaf of the selected plant unless specified. Typically, leaves of the dominant grass species at a site were measured. At least two samples of each species were measured. Typically, during all collections (i.e., 1987 - 1989) an external light source with a restricted beam spot (slitted illuminator) was used to restrict the illumination spot on narrow grass leaves so that only leaf material was illuminated.
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The Mowing Experiment Biophysical Measurements data set was collected to quantify the effects of grazing and nitrogen fertilization on primary productivity and plant chemistry. The data in this data set quantified the effects of foliage removal on plant net primary productivity (NPP), plant nutrient content and the effects of grazing pressure as simulated by mowing. Mean values and their variances are reported. Standing crop values reflect treatment effects of removing biomass periodically, but the productivity levels show the inverse effects, suggesting plant compensatory growth mechanisms. Grazing intensity was defined as the amount of leaf area remaining following defoliation. The latter was manipulated experimentally by mowing at several heights. Grazing frequency was defined as the number of times foliage removal occurred in each year and included grazing and mowing history as well as current mowing frequency.
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Light radiation striking a vegetative canopy interacts with individual phyto-elements (i.e., leaves, stems, branches) and the underlying substrate. The interaction depends on light quality, radiative form (direct or diffuse), illumination incidence angle, vegetative component optical properties and canopy architecture. Radiation is reflected, transmitted or absorbed. Mowing, grazing, and fertilization can affect the canopy architecture or optical properties of vegetation, thus changing the canopy reflectance. This study examined the response of spectral reflectance characteristics (using an Exotech radiometer) to canopies that were manipulated using simulated grazing and fertilization of plots. The spectral reflectance data set supports the original hypothesis of a curvilinear relationship between productivity and grazing intensity. Reflectances for the four MSS bands and the standard error for each are reported. These data were collected at two locations within the northwest quadrant of the FIFE study area during the growing season of 1987. Reflected radiation measurements were converted to radiances and reflectance factor. The reflectance factor is the ratio of the target reflected radiant flux to an ideal radiant flux reflected by an ideal Lambertian standard surface irradiated in exactly the same way as the target.
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The Upper Air Derivative Data from NMC Data Set was derived from National Meteorological Center global upper air models. These models use a 6 hours intermittent assimilation method. In this method, the objective analysis is performed every 6 hours using a 6 hours forecast as an initial guess (Kanamitsu 1989). The National Meteorological Center (NMC) gridded upper air data was extracted from the NOAA operational analysis system and transmitted to the FIS. This contained spatially interpolated NMC upper air data calculated for four grid points of 381 km polar-stereograph over the FIFE area. FIS considers this a derived data set (i.e., not from original measurements).
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The FIFE Staff Science effort included the acquisition, processing and archiving of meteorological parameters of the atmosphere above the FIFE study area, which would furnish surface meteorological parameters from hourly reporting network for the FIFE area, and provide input data and/or verification data for numerical simulation models. Though the measurements presented in this data set were not taken precisely at the FIFE site, it is hypothesized that they present a representative horizontal cross-section of meteorological variables and sky conditions in and around the site. It is also realized that many of the variables presented in this data set are somewhat subjective and dependent on the skill (and biases) of the observer, such as estimates of cloud amount and height. The NOAA regional surface reports were extracted from the NOAA operational analysis system and transmitted to the FIS. This contained hourly surface meteorological data from selected stations as received from NESDIS for FIFE.
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As part of the FIFE staff science data processing effort, the FIFE Information System (FIS) extracted site average radiances from the level-1 NS001-TMS products. Data were collected by the NS001 during each of the FIFE IFC&amp;#39;s. Selected flights were processed to level-1. The site averages were extracted from these processed images. Therefore, this data set contains a small number of observation dates for each site, but at the multiple angles provided by the grid pattern used during each flight. The data set can be used for canopy reflectance modeling studies. The site average radiances extracted from the NS001 imagery are instrument-corrected spectral radiances for each of the eight spectral bands. Geographic location and viewing and solar angles for each of 39 FIFE ground measurement sites are also included for each observation. The sensor calibrated radiance values were corrected using atmospheric aerosol optical thickness and gaseous absorption profile measurements, when available. The atmospheric correction algorithm of Fraser et al. (1989) was used to calculate reflectance in the visible and infrared channels. The thermal data are corrected using parameters derived from the Lowtran7 atmospheric path radiance model (Kneizys et al., 1988).
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The objective of the Optical Thickness Calibration study was to compare aerosol optical thickness measurements derived from three different groups. These groups measured atmospheric transmission, in particular, the aerosol optical thickness, using at least three different instruments (e.g., a solar transmissometer SXM-2, a Reagan sunphotometer, and an airborne tracking sunphotometer) and three different analysis procedures.
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The NIPS and Reagan Sunphotometer Optical Thickness study compared various ground and image-based techniques used to characterize the atmosphere. These data are used to remove atmospheric absorption and scattering from remote sensing scenes so that surface parameters can be retrieved. An evaluation of the effects of uncorrected atmospheric absorption and scattering on various vegetation indices and subsequent biophysical parameter estimations was also undertaken. These data can also be used to derive aerosol size distribution (King et al., 1978) and thereby estimate the phase function. Aerosol optical depths were recorded at various locations within the FIFE site. A Normal Incident Pyrheliometer (NIP) and a Reagan sunphotometer was used to collect data during the IFCs. These data showed that daily averages span a range of 0.05 to 0.28 in the mid-visible wavelength (Bruegge et al., 1992a). Diurnal variations were recorded. The afternoon optical depths are greater than those of the morning by as much as 0.07. These data are analyzed using the Langley technique. Rayleigh optical depth is subtracted, and aerosol, ozone, and water vapor abundance&amp;#39;s simultaneously measured. In retrieving ozone, a Junge aerosol model is assumed, thus, the natural log of aerosol optical depth is linear with wavelength (Bruegge et al., 1992a). This contrasts with other experimental approaches used by investigators in which an ozone abundance is assumed (Halthore and Markham 1992). This approach allows measurement of aerosol, but is limited by the accuracy of the ozone data.
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The data in the Sunphotometer Optical Thickness Data from C130 Aircraft data set were collected in June, July and August 1987, and in August 1989. The data was collected at selected locations within the FIFE study area. Atmospheric optical depths derived from measurements of solar radiation by the airborne suntracking sunphotometer are available in this data set. These data are necessary for atmospheric correction of data from Earth viewing airborne and satellite sensors in the visible and near infrared regions of the electromagnetic spectrum. The data show that atmospheric optical depth changes significantly both spatially and temporally. Variability in atmospheric optical properties and substantial differences in atmospheric optical properties during the data collection, emphasize the need to make quantitative measurements of atmospheric optical properties at the time of remote sensing data acquisition.
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The Solar Transmissometer Aerosol Optical Thickness Data Set contains optical thickness data that provide a measure of the effect of aerosols on the attenuation of radiation through the atmosphere at 8 discrete wavelength bands throughout the visible and near IR portion of the electromagnetic spectrum. These data were collected using a ground-based solar transmissometer in June and July of 1987, and July and August of 1989, at two stations in the FIFE study area. These data are used to provide atmospheric correction of remotely sensed data using radiative transfer models and to study aerosol particle size distribution (see Halthore and Markham 1992; King et al. 1978). These data are also used to infer the optical clarity of the atmosphere.
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Aerosol optical thickness in conjunction with an atmospheric model can provide estimates of atmospheric effects on transmitted and reflected solar radiation. These effects can then be used to correct aircraft and satellite radiometric data. In FIFE, three sunphotometers were used to track the sun through a range of airmasses during the period of February 6, 1987 through October 31, 1989. The Aerosol Optical Thickness from GSFC Data Set were analyzed using the Langley technique. Rayleigh optical depth was subtracted, and aerosol, ozone, and water vapor abundance&amp;#39;s simultaneously measured. In retrieving ozone a Junge aerosol model was assumed, thus the natural log of aerosol optical depth was linear with wavelength (Bruegge et al. 1992). This approach allows measurement of aerosol, but is limited by the accuracy of the ozone data.
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The Surface Reflectances Measured by the PARABOLA Data Set contains measurements from the Portable Apparatus or Rapid Acquisitions of Bi-directional Observations of Land and Atmosphere (PARABOLA) instrument. The focus of this research was to characterize the variation in vegetation reflectance as a function of solar and sensor viewing geometry, wavelength, and plant canopy biophysical characteristics. An understanding of these relationships is necessary for meaningful biophysical and ecological interpretations of measurements acquired from airborne and satellite sensors. The PARABOLA is able to measure these variations in reflectance because it measures at different viewing angles and at 3 spectral bands. The data are averaged reflectance factors of the Konza Prairie at different view angles and at 3 wavelength bands throughout the day. PARABOLA measurements were made during each of the 5 FIFE Intensive Field Campaigns from five locations within the FIFE study area.
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The focus of this study was to quantify the effects of foliage removal by cattle on plant net primary productivity (NPP). The Vegetation Biomass, Production and Consumption at Selected Sites Data Set contains mean values and their variances. During the growing season of 1987, portable cattle exclosures were used to quantify above-ground plant biomass dynamics at each of four sites. All sites had been grazed each year and burned frequently during the preceding 10 years. Biomass was measured inside portable exclosures, outside exclosures (in unprotected vegetation), and inside permanent exclosures. Exclosures were moved to previously unsampled locations within a distance of 10 m after samples were obtained, and these remained in place until the next sampling date.
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The Surface Radiant Temperature Measured with a Helicopter-borne Infrared Thermometer Data Set were collected for six days during July and August of 1989 to provide the radiant temperature of the FIFE sites and as a check of the thermal band on the MMR. The average and standard deviation of radiant temperature were measured with an Everest infrared thermometer. The Everest Series 4000 Infrared Thermometer (IRT) was mounted on the NASA Bell UH-1B helicopter in conjunction with the Barnes Multiband Modular Radiometer (MMR) and the Spectron Engineering SE590 Spectroradiometer for the 1989 field campaign. The IRT collected radiant temperature data as the helicopter hovered over individual sites within the FIFE study area.
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The Surface Temperatures Measured at Multiple Angles Data Set was collected at two locations within the northwest quadrant of the FIFE study area during July and August 1989. The data set contains hemispherical surface temperature, surface temperatures measured at several view zenith angles, and surface temperatures and at-view azimuth increments of 45 degrees. These data were collected using the Everest multiplexed infrared thermometers (IRT) Model 4000 and an Eppley Precision Infrared Radiometer Model PIR. Periodically measurements of the surface emissivity and incoming longwave radiation were also made. The purpose of this study was to characterize bi-directional reflectance factor distributions, estimate surface albedo from bi-directional reflectance factor and radiance data, determine the variability of reflected and emitted fluxes in selected spectral wavebands as a function of topography, vegetative community and management practice, determine the influence of plant water status on surface reflectance factors, and determine sun angle affects on radiation fluxes.
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The Surface Temperatures from UNL Data Set contains surface temperatures collected between July 15 and August 11, 1989 at three FIFE area sites. These surface temperatures were measured with an Everest multiplexed infrared thermometer (IRT) Model 4000 predominantly in the solar principal plane, with nadir and off-nadir, view-zenith angles (mounted on the portable mast with the Barnes Model 12-1000 Modular Multiband Radiometer (MMR)). The purpose of this study was to determine the variability of emitted fluxes as a function of topography, vegetative community and management practice. Spatial and temporal sampling at sites 906 (2133-EVN), 916 (4439-EVN), and 966 (2437-EVN) was achieved. Measurements were typically coordinated with aircraft and/or satellite overpasses.
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The NOAA Radiosonde Observations Data Set contains data that were extracted from the NOAA operational analysis system and transmitted to the FIS. Data are available from July 1985 to October 1988, there are 1123 days of data during this period with data at twelve hour intervals. These data were collected using sondes released in Dodge City and Topeka, Kansas, 337 km and 68 km, respectively, from the FIFE site. Radiosonde observations were made to determine the pressure, temperature, and humidity from the surface to the point where the sounding was terminated.
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The FIFE Root Biomass data were collected from 16 locations within the FIFE study area during the 1987 growing season. They provide a measure of the below-ground biomass for the study area. Biomass reported as grams per square m assumes that the depth of the core samples is sufficient to include all root biomass under the surface to an infinite depth. Prairie vegetation does possess roots deeper than the 20 cm coring, however, the fraction of total root biomass below 20 cm is minuscule and safely ignored in a study of biomass.
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The atmospheric effects on the transmitted and reflected solar radiation should be factored into the estimation of geophysical and biophysical parameters from remotely-sensed data, so that appropriate correction schemes can be employed to infer reflectivity of the ground from satellite radiometric data. Some of the correction techniques require derived coefficients as inputs in the algorithms that perform the atmospheric correction. As part of the FIFE staff science data collection effort, the FIFE Information System (FIS) utilized atmospheric correction and related algorithms to generate coefficients for deriving corrected values from the FIFE level-1 image products. These coefficients were used by FIFE staff in calculating site reflectances from pixel values extracted from the level-1 imagery. The Fraser (Fraser et al., 1992) and LOWTRAN 7 (Kneizys et al., 1988) models were used for computation of coefficients used to correct radiances of scattered radiation measured by aircraft and/or satellite during FIFE. The Fraser algorithm is designed to compute the surface reflectance for a given measured radiance, or alternatively, the upward radiance at an arbitrary height when the surface reflectance is given. LOWTRAN 7 is a low-resolution propagation model and computer code for predicting atmospheric transmittance and background radiance from 0 to 50,000 [cm^-1] at a resolution of 20 [cm^-1].
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The Advanced Very High Resolution Radiometer (AVHRR) is a four- or five-channel scanning radiometer capable of providing global daytime and nighttime sea-surface temperature and information about ice, snow, and clouds. The sensor measures emitted and reflected radiation in five channels (bands) of the electromagnetic spectrum. The Site Average Reflectances Extracted from AVHRR-LAC Imagery Data Set consists of averages of pixel extracts from AVHRR-LAC (1 km resolution) scenes that overlay the FIFE site. Average radiances for dates are available for the five sensor wavebands and average reflectance and exoatmospheric reflectances are available for wavebands 1 and 2. Site averages are clustered in 1987 and during the summer of 1989. Some data are also available for early 1988. The AVHRR is capable of operating in both real-time or recorded modes. Direct readout data were transmitted to ground stations of the automatic picture transmission (APT) class at low-resolution (4x4 km) and to ground stations of the high-resolution picture transmission (HRPT) class at high resolution (1x1 km). Data recorded on board were available for processing in the NOAA Central Computer Facility. They included local area coverage (LAC) data which were from selected portions of each orbit with a 1x1 km resolution. The precision of satellite remote sensing estimates of surface reflectance (Hall et al., 1992), calibrated and corrected for atmospheric effects, was no worse than about 1 percent absolute.
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The Thematic Mapper sensor system was used to collect the original data between February 1987 and October 1989 from which this data set was produced. Landsat TM extract data contains the average instrument corrected spectral radiances for each of the seven spectral bands. In addition, the associated view and solar angles are available for each of 39 FIFE ground measurement sites. The Site Reflectances Extracted from Landsat TM Imagery Data Set also contains reflectance values and exoatmospheric reflectance values for these seven spectral bands. These reflectances were derived using the sensor calibrated radiances which were corrected for exoatmospheric effects using atmospheric aerosol optical thickness and gaseous absorption profile measurements, when available. The atmospheric correction algorithm of Fraser et al. (1989) was used to calculate reflectance in the visible and infrared channels. The thermal data were corrected using parameters derived from the Lowtran-7 atmospheric path radiance model (Kneizys et al. 1988).
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The Site Reflectances Extracted from SPOT HRV Imagery Data Set contains the average instrument corrected spectral radiances for each of the spectral bands (3 in XS and 1 in PAN) collected during the growing seasons of 1987, 1988, and 1989. In addition, the associated view angles and solar angles are available for each of 39 FIFE ground measurement sites. The data set also contains reflectances and exoatmospheric reflectances for these spectral bands. These reflectances were derived using the sensor calibrated radiance values corrected using atmospheric aerosol optical thickness and gaseous absorption profile measurements, when available. The atmospheric correction algorithm of Fraser et al. (1989) was used to calculate reflectance in the visible and infrared channels.
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The SE-590 Spectroradiometer Reflectance Factors from GSFC Data Set contains spectral data collected with the Spectron SE-590 Spectral Radiometer at selected FIFE sites located primarily on the Konza Prairie. These measurements were acquired in conjunction with the Surface Reflectances measured by the PARABOLA bi-directional measurements. Ground SE-590 data were acquired in all four 1987 Intensive Field Campaigns and in the 1989 Intensive Field Campaign. The ground SE-590 data were collected at approximately every 10 degree change in solar zenith angle (SZA) to characterize diurnal variations and/or simultaneous observations acquired by helicopter, airplane, or satellite over flights. The data were collected as wavelength intensity values which were converted to spectral radiances with instrument and campaign-specific calibration coefficients.
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The SE-590 Reflectance Factors and Radiances from UNL Data Set contains surface reflectance and viewing angle data that was collected at three sites within the FIFE study area via a SE590 mounted on a portable mast. All measurements were made on eleven days between July 15 and August 11, 1989. Measurements were typically coordinated with aircraft and/or satellite overpasses. On days when measurements were not made the bare soil was covered with a plastic mulch that allowed moisture to penetrate the surface but hindered the regrowth of the vegetation. Solar radiation data at or near the specific site should be used to screen possible times of variable cloud cover. Canopy, illumination, and viewing geometry are critical in determining the amount of reflected radiation received at the sensor. The measurements were predominantly made in the solar principal plane since the greatest variation in observed reflected radiation is expected to occur in that plane due to extremes in sunlit and shaded portions of the canopy (Norman and Walthall 1985). Reflected radiation measurements were converted to radiances and reflectance factor. Reflected radiation from a field reference panel corrected for non-perfect reflectance and sun angle was used as an estimate of the ideal Lambertian standard surface (Walter-Shea and Biehl 1990).
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The SE-590 Leaf Level Spectral Observations from GSFC Data Set were acquired in situ with a Spectron SE590 spectroradiometer fitted with the 1 degree IFOV lens, and coupled with a LI-COR integrating sphere. The purpose in collecting SE590 leaf reflectance and transmittance data was to characterize the optical properties of the canopy components to gain a better understanding of how these optical properties contribute to canopy reflection and absorption of radiation. To measure the reflectance and transmittance of leaf surfaces an integrating sphere was used. The integrating sphere collected all of the radiation reflected from or transmitted through a surface. These data are the average spectral optical properties (i.e., reflectance, transmittance) and the standard deviations for the three dominant species found on each of three sites: 916 (i.e., Big Bluestem, Indiangrass, and Switchgrass), 906 (i.e., Big Bluestem, Indiangrass, and Switchgrass), and 26 (i.e., Big Bluestem, Lovegrass and Dropseed) during late July and early August, 1989. The average spectral reflectance and transmittance represent the mean values for the adaxial (top) and abaxial (bottom) sides of 4 - 10 leaves for wavelengths between 400 - 1050 nm at approximately 3 nm intervals.
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The SE-590 Reflectance Factors and Radiances Measured from a Helicopter Data Set were collected using the helicopter-borne SE-590 during Intensive Field Campaign 5 (IFC-5) in 1989. These data were collected at 17 different grid locations within the FIFE study area. Data were collected on 6 days from July 28, 1989 through August 8, 1989, when sky conditions were clear. The helicopter missions were designed to provide a means of spectrally characterizing each FIFE site and provide an intermediate scale of sampling between that of the surface measurements and the higher altitude aircraft and spacecraft multispectral imaging devices. The SE-590 instrumentation was chosen to provide compatibility with surface-based radiometers and TM spacecraft sensors. Off-nadir measurements were made as a means of providing more accurate estimates of hemispherical reflectance and for use with bi-directional reflectance models.
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The Site Averaged AMS Data: 1987 (Betts) Data Set contains the site averaged product of the Portable Automatic Meteorological Station (AMS) data acquired during the 1987-1989 FIFE experiment. Data are in 30 minute time intervals in 1987.
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The Site Averaged AMS Data: 1987 - 1989 (Betts) Data Set contains the site averaged product of the Portable Automatic Meteorological Station (AMS) data acquired during the 1987-1989 FIFE experiment. Data are in 30 minute time intervals in 1987.
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The Site Averaged AMS Data: 1988 (Betts) Data Set contains the site averaged product of the Portable Automatic Meteorological Station (AMS) data acquired during the 1987-1989 FIFE experiment. Data are in 30 minute time intervals in 1988.
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The Site Averaged AMS Data: 1989 (Betts) Data Set contains the site averaged product of the Portable Automatic Meteorological Station (AMS) data acquired during the 1987-1989 FIFE experiment. Data are in 30 minute time intervals in 1989.
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The Site Averaged Flux Data: 1987 (Betts) Data Set contains the site averaged product data collected by many PIs during the 1987-1989 FIFE experiment. This data set is a time series of 30-minute average variables for the periods May 27, 1987 - Oct 16, 1987.
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The Site Averaged Flux Data: 1987 (Betts) Data Set contains the site averaged product data collected by many PIs during the 1987-1989 FIFE experiment. Data are in 30 minute time intervals in 1987 and include the entire period 1987-1989.
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The Site Averaged Flux Data: 1988 (Betts) Data Set contains the site averaged product data collected by many PIs during the 1987-1989 FIFE experiment. Data are in 30 minute time intervals and include data only for 1988.
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The Site Averaged Flux Data: 1987 (Betts) Data Set contains the site averaged product data collected by many PIs during the 1987-1989 FIFE experiment. Data are in 30 minute time intervals and include data only for 1989.
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The Site Averaged Gravimetric Soil Moisture Data: 1987 (Betts) Data Set contains the site averaged product data collected during the 1987-1989 FIFE experiment. Samples were averaged for each site, then averaged for each day. This data set includes only 1987 data.
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The Site Averaged Gravimetric Soil Moisture Data: 1987 - 1989 (Betts) Data Set contains the site averaged product data collected during the 1987-1989 FIFE experiment. Samples were averaged for each site, then averaged for each day. This data set includes data from May 20, 1987 through August 12, 1989.
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The Site Averaged Gravimetric Soil Moisture Data: 1988 (Betts) Data Set contains the site averaged product data collected during the 1987-1989 FIFE experiment. Samples were averaged for each site, then averaged for each day. This data set includes only 1988 data.
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The Site Averaged Neutron Soil Moisture Data: 1987 (Betts) Data Set contains the site averaged product data of the neutron probe soil moisture collected during the 1987-1989 FIFE experiment. Samples were averaged for each site, then averaged for each day. This data set includes only 1987 data.
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The Site Averaged Neutron Soil Moisture Data: 1987 - 1989 (Betts) Data Set contains the site averaged product data of the neutron probe soil moisture collected during the 1987-1989 FIFE experiment. Samples were averaged for each site, then averaged for each day. This data set includes the 1987 - 1989 data.
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The Site Averaged Neutron Soil Moisture Data: 1988 (Betts) Data Set contains the site averaged product data of the neutron probe soil moisture collected during the 1987-1989 FIFE experiment. Samples were averaged for each site, then averaged for each day. This data set includes only 1988 data.
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The Site Averaged Neutron Soil Moisture Data: 1989 (Betts) Data Set contains the site averaged product data of the neutron probe soil moisture collected during the 1987-1989 FIFE experiment. Samples were averaged for each site, then averaged for each day. This data set includes only 1989 data.
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Soil bulk density is defined as the ratio of the mass of dry solids to the bulk volume of the soil occupied by those dry solids. Bulk density of the soil is an important site characterization parameter since it changes for a given soil. It varies with structural condition of the soil, particularly that related to packing. The Soil Bulk Density Data Set contains bulk density of the soil based on dry weight at two depths, 0-10 cm and 10-20 cm. Samples were collected at 31 different locations within the FIFE study area during the growing season of 1987. Samples were collected primarily in the northwest quadrant of the study area but at least one sitegrid is located in each of the quadrants of the study area.
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In the Soil Carbon Dioxide Flux study, a prototype gas exchange system and sensor were used to determine the soil surface flux of CO2 and associated parameters at the three FIFE supersites. The goal of this investigation was to characterize fluxes of carbon dioxide from the surface of the soil for a representative portion of the FIFE study area. These measurements are required to understand the carbon budget of the prairie and necessary for comparing vegetation models of photosynthesis with CO2 flux measurements by micrometeorological methods. The flux of the carbon dioxide from the surface of the soil is an important component of the carbon budget of a prairie ecosystem. The results from this study indicate that a soil chamber can be used to obtain reasonable estimates of soil surface carbon dioxide fluxes when operated in a closed system that is ported to the free atmosphere. Further, the flux of carbon dioxide from the soil surface of a grassland can be a large part of the carbon budget and should never be assumed to be negligible. Both soil temperature and soil water content are critical parameters for predicting soil surface CO2 flux, and leaf area index is a surrogate for the plant contribution through root respiration.
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Nitrogen gas fluxes are important to ecosystem productivity and atmospheric chemistry. Scaling of these microscale fluxes to landscape and regional scales relevant to ecosystem and atmosphere-biosphere exchange questions is difficult. For FIFE, two approaches were explored to accomplish scaling. First the relationships between hourly and daily gas fluxes and soil moisture were established and then large area estimates of soil moisture from simulation models or a push broom microwave radiometer were used to scale data from experimental sites to larger areas. The second approach was to establish relationships between annual gas fluxes and plant productivity and then use large area data on plant productivity derived from SPOT images as a scaling tool. Both approaches were based on hypotheses and previous studies that established strong relationships between soil moisture and plant productivity and gas fluxes. FIFE Soil Gas Fluxes Using Soil Cores Data Set contains the daily flux rates of denitrification, nitrous oxide flux and carbon dioxide flux obtained from 10 sites at four sampling dates during 1987. Soil gas fluxes were measured using an intact extracted core technique. The data set includes estimates of in situ fluxes as well as denitrification fluxes measured in cores amended with either water or water plus nitrate. Analysis of relationships between daily flux rates and soil moisture and between annual fluxes and plant productivity are reported elsewhere (Groffman and Turner submitted to Ecology, Groffman and Wood in preparation). Analysis of the denitrification data, and evaluation of denitrification fluxes in the context of the ecosystem ecology of the FIFE study area are presented in Groffman et al. (1992).
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The Soil Hydraulic Conductivity Data Set contains soil hydraulic conductivity, matric flux potential, and soil depth data collected during the 1989 FIFE soil properties investigation. The purpose of the 1989 FIFE soil properties investigation was to obtain more points on the soil moisture release curves for the soils at the FIFE stations, and provide values for the saturated hydraulic conductivity for the long-term water balance studies. In-situ measurements of field-saturated hydraulic conductivity were made using the constant well head permeameter method. These measurements were made at five sites, each representing a different soil series. The constant well head method for hydraulic conductivity involves augering a hole to the desired depth and measuring the steady state flow rate of water into the hole while maintaining a constant head of water inside the hole. Six measurements were made at each of the two soil depths at each site. The hydraulic conductivity measurements were made at the same depths and close to (less than 1 m away from) the location where samples for moisture release measurements were taken.
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The purpose of this research was to characterize the soil moisture distribution in the FIFE study area. Daily measurements of the soil dielectric properties were obtained at five locations throughout the FIFE study area during the 1987 Intensive Field Campaigns (IFC). Calculated soil volumetric water contents were compared with gravimetric soil moisture measurements collected at the same locations by the FIFE staff science team. Examination of the data revealed that the impedance probe is a more consistent source of time series information than traditional measurements, and is potentially more closely linked to the physical parameters. The dielectric constant of soil is a potentially sensitive indicator of soil moisture. Since, the magnetic permeability of all naturally occurring soils is near that of free space, dielectric measurements serve to fully characterize the electromagnetic response of soils. Many of the indirect methods of soil moisture measurement permit frequent or continuous measurements in the same place with only small expenditure of time. Thus, changes in water content with time can be approximated. The soil impedance is sensitive to the moisture content of the soil and can be used to calculate the volumetric water content of the soil. Soil impedence techniques using probes have been demonstrated to show small-scale diurnal variations that would be completely missed by small-scale spatial variations in the gravimetric sampling scheme. Furthermore, the basically non-destructive nature of the fixed probes minimize the impact of the sampling technique on the dynamic behavior of the region under study.
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Water content measurements by gravimetric methods involve weighing a wet sample, removing the water via drying in an oven, and reweighing the sample to determine the amount of water removed. Water content then is obtained by dividing the difference between wet and dry masses by the mass of the dry sample to obtain the ratio of the mass of water to the mass of dry soil. When multiplied by 100, this becomes the percentage of water in the sample on a dry-mass (or, as often expressed, on a dry-weight) basis. Soil moisture determined using the gravimetric method was measured at 800 sites along 24 transects. These transects were over flown by the airborne Gamma Radiation System used to measure soil moisture. These data are useful for comparison of airborne and ground soil moisture data. This analysis for the airborne Gamma Radiation System, using completely independent soil moisture data showed that the root mean square error of 97 flights was 3.02 percent soil moisture, with a bias of less than 0.5 percent soil moisture (Carroll et al., 1988).
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The gravimetrical soil moisture data were collected from many stations spread over the FIFE study area. These data were collected to characterize the spatial and temporal patterns of moisture content of the soils over this area during and between the FIFE Intensive Field Campaigns. The aim of the FIFE soil moisture work was to characterize spatial and temporal patterns of soil moisture at the FIFE site, to validate and calibrate remote sensing measurements of soil water, and to evaluate alternative methods of measuring soil moisture both from the air and on the ground. A further goal was to develop techniques for comparing point and spatially continuous measurements of soil moisture. The FIFE soil moisture research was designed to advance the technology for characterizing soil moisture and contribute useful data to other FIFE investigations.
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The neutron-probe data present a series of measurements of volumetric water content in the soil profile compiled using the neutron method. These data were collected from throughout the FIFE study area from May 1987 through August 1989. The neutron method of measuring soil water content uses the principle of neutron thermalization. When both hydrogen and oxygen are considered, water has a marked effect on slowing or thermalizing neutrons. Thermal neutron density is easily measured with a detector, if the capture cross-section remains constant then the thermal neutron density may be calibrated against water concentration on a volume basis.
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This data product was created based on the hypothesis that a variety of ground truth observations of soil moisture could be combined to estimate equal soil moisture contours across a large area (e.g., the FIFE area). A second stage required interpolating from these contours, using the methods of spatial statistics, to average soil moisture values at the nodes of a uniform grid. The grid node values in this product represent the average soil moisture of a 0.5 km x 0.5 km area centered at the node location. The correlation area method (CAM) was used to combine in situ measurements and airborne gamma remote sensing estimates to obtain areal averages of soil moisture. Information on biomass and the spatial distribution of vegetation in a model was also used to estimate soil moisture from PBMR measurements. Another simple method, using only ground soil moisture data, was also used to compute soil moisture from the PBMR measurements. All soil moisture data collected from the aircraft platforms and ground measurements were entered into the ARC/INFO GIS along with the UTM coordinates of each observation. All available and usable measurements of soil moisture were considered in an analysis that produced isolines of soil moisture.
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The aim of the FIFE soil moisture transect work was to characterize spatial and temporal patterns of soil moisture along selected transects at the FIFE study area. Two levels of ground data were collected to support the passive microwave (PBMR) flights over the Konza experimental area. The water content measurements were collected using gravimetric methods. Soil moisture measured along a transect is necessary to calibrate airborne moisture instruments or compare data obtained from them. Soil units in a landscape are inherently heterogeneous, which leads to variations in moisture content along an aircraft flight path on the ground. In order to reduce errors, values on the flight path were sampled at close intervals.
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Soil reflectance properties are an important factor in determining landscape reflectance characteristics. No soil reflectance data were collected as part of the FIFE experiment. Therefore, the FIS staff choose spectra from soils similar to those in the FIFE study area from the atlas of soil reflectance properties (Stoner et al., 1980). The atlas represents a wide range of soil types, and FIS staff choose spectra from soils similar to those in the FIFE study area. The selection of spectra was based on soil particle size, organic carbon content, taxonomic classification, and geography of soils found in the FIFE study area. All measurements were made on uniformly moist, sieved soils, which were equilibrated for 24 hours at a one-tenth bar moisture tension. Soil reflectance was measured using an Exotech Model 20 C spectroradiometer adapted for indoor use with a reflectometer equipped with an artificial illumination source, transfer optics, and sample stage. Spectral readings were taken in 0.01 micrometer increments over the 0.52 to 2.32 micrometer wavelength range.
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The objectives of this study were to collect soil survey information from the FIFE study area, determine the soil types at the FIFE sites, and characterize the physical and chemical properties of the soils. The Soil Properties Reference Information Data Set provide a description of the soils and their properties at the FIFE study sites as described by the U.S. Soil Conservation Service. Five stations representative of the Clime, Benfield, Dwight, Florence, and Tully soil types were selected, and a detailed description of the soil profile at each of these five sites was made. Soil samples from the surface down to bedrock were collected from the horizons and analyzed for bulk density, particle size distribution, moisture retention at 1/3 and 15 bar suctions, cation exchange capacity, and other chemical and physical properties, using standard procedures (Soil Survey Staff 1984).
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The purpose of the 1989 FIFE soil properties investigation was to obtain a description of the thermal properties of the soils within the FIFE study area. Soil thermal conductivity measurements describe the soil properties which govern the flow of heat through the soil. The thermal conductivity is defined as the quantity of heat that flows through a unit area in a unit time under a unit temperature gradient. These measurements were made using a hot wire probe in situ at two depths at twenty six FIFE sites during October 1987. The measurements were taken using a long electrically heated wire enclosed in a cylindrical probe . The probe is placed in the soil, the wire is heated by running a current through it, and the temperature rise is measured with a thermocouple placed next to the wire. A plot of temperature versus the log of time can be used to derive the thermal conductivity. The results may require a correction factor to account for the dimensions of the probe.
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During the 1989 FIFE field campaign, measurements were made of soil moisture release parameters and hydraulic conductivity. Bulk density and soil moisture release data were collected at five FIFE sites representing the major soil types in the FIFE study area. These data were used to model the porosity, saturated water potential, and the b-factor (the exponent of the power curve function) following the method of Clapp and Hormberger (1978). These soil moisture characteristics can be used to describe plant-available water and water movement through soils.
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The FIFE Standing Crop and Nitrogen Content Data Set contains biomass and nitrogen concentration data for live and dead above-ground plant material collected along transects in watersheds within the FIFE study area. The transects were in watersheds that had undergone burning and grazing treatments. Point physical descriptors (elevation, slope, and soil depth) are also included in the data set. Substantial variation in biomass, and N accumulation occurred over time, with topography, and as a result of grazing and previous burning (Schimel et al. 1991a, Kittel et al. 1990, Turner et al. 1992, Davis et al. 1992).
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The Daily Stream Flow Amounts Data Set contains daily measurements of stream flow for the four LTER stations and for the USGS stream-flow station located on tributaries to Kings Creek. This data set contains measurements from April 1979 to September 1988 for the USGS station, and from June 1985 to December 1987 for the 4 LTER stations. Five stream-flow gauges were placed across creeks in the Long-Term Ecological Research (LTER) section of the FIFE study area. Four of these five stations were maintained and monitored by the LTER staff while the fifth was part of the USGS network of stream flow gauges. The V-throated flume and standpipes used at the LTER weirs operated on the principle that the height of the water level in a standpipe at a specific location within a weir of known dimensions can be converted to volume of water in the stream. The change of this instantaneous volume with time could then be used to compute volumetric stream flow. The stilling pipe installation at the USGS stations operates on the principle that the height of the water level in a standpipe at a specific location within a streambed can be converted to volume of water in the stream. The tracking of the change in stream height with time then enables the calculation of stream flow.
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The Storm Event Stream Flow Data Set were collected during storm events from five treatment areas within the Konza Prairie Long-Term Ecological Research (LTER) site located within the northwest quadrant of the FIFE study area. These data were recorded so that the hydrology of the streams draining the tallgrass prairie could be studied. Moreover, these data were collected to determine the effect of burn frequency of a watershed upon runoff. Data are available from June 14, 1985 through December 31, 1987. The V-throated flume and standpipes used at the LTER weirs operated on the principle that the height of the water level in the standpipe at a specific location within a weir of known dimensions can be converted to volume of water in the stream. The change of this instantaneous volume with time could then be used to compute volumetric stream flow. The V-notch, sharp-crested weir used in watershed 1D operated on the principle that water flowing past a point of known dimensions per unit time could be converted through standard equations to volumetric flow.
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The FIFE Surface Flux Baseline 92 Derived Data Set was compiled from the original surface flux data collected during FIFE (i.e., no measurements were made specifically for this data set). This data set contains data collected from mid-May through mid-October, 1987 at 21 stations located within 19 sitegrids spread throughout the FIFE study area. For a description of the theory behind the original surface flux measurements see the documentation for each of the original surface flux data sets. Surface heat flux data routinely have erroneous jumps (i.e., spikes) in the latent and sensible heat flux time series in the early morning and evening hours due to small gradients in the measured data. A series of tests were developed to identify these spikes and flag them. Flux data obtained from Bowen ratio sites are also checked for energy imbalances. These data were also compared to model results. The consistency between these two methods is indicated in this data set.
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The NOAA Regional Surface Data - 1989 (NCDC) Data Set contains hourly surface meteorological data for the FIFE area. Though the measurements presented in this data set were not taken precisely at the FIFE study area, it is hypothesized that they present a representative horizontal cross-section of meteorological variables and sky conditions in and around the site. It is also realized that many of the variables presented in this data set are somewhat subjective and dependent on the skill (and biases) of the observer, such as estimates of cloud amount and height. This data may be used as input data and/or verification data for numerical simulation models.
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The Surface Temperatures, Reflected and Emitted Radiation, and PAR from UNL Data Set contains surface temperatures at different view zenith and azimuth angles, net radiation, incoming and reflected photosynthetically active radiation, incoming and reflected shortwave radiation, and reflected and emitted longwave radiation. Surface temperatures were measured at a 30 degree view zenith angle with an Everest infrared thermometer (IRT) Model 112C and at approximately a 60 degree view zenith angle with a Scheduler Plant Stress Monitor at 4 view azimuths (predominantly 90 degree increments from the solar azimuth). The Scheduler also measured air temperature, relative humidity, and vapor pressure deficit. Net radiation was measured with a Radiation and Energy Balance Systems (REBS) net radiometer Model Q*3. Incoming shortwave radiation was measured with a horizontally mounted Eppley Precision Pyranometer Model PSP. Reflected shortwave radiation was measured with two (2) Eppley Precision pyranometers Model PSP usually mounted horizontally (at site 966 (2437-PSP) one PSP was mounted horizontally and the other was inclined parallel to the slope). Reflected and emitted longwave radiation were measured with a horizontally mounted Eppley Precision Infrared Radiometer Model PIR.
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The temperature profile data included in this data set was derived from the FIFE radiosonde data collected during the summer and fall of 1987 and the late summer of 1989 by Dr. Wilfred H. Brutsaert. These intensive radiosonde flights allowed the measurement of the atmospheric profiles of potential temperature and specific humidity. These data have been corrected for sensor delays, algorithm inconsistencies and have been interpolated to a set of standard pressure levels.
&lt;br&gt;&lt;h4 id&#x3D;&quot;fife_biology_leaf_h2o_126&quot;&gt;fife_biology_leaf_h2o_126&lt;/h4&gt;
The Total Leaf Tissue Water Potential Data Set was collected during the summer months of 1988 and 1989. The objective of this study was to determine the influence of plant water status on surface reflectance factors. Measurements were made at six stations on Indian grass, switch grass, Big bluestem, little bluestem, and tall dropseed. Leaf water potential measurements were usually made on the same leaf that optical measurements were made and on leaves of surrounding plants. Measurements were made on the most recently expanded leaf of the selected plant unless specified. Measurements were also made of older green and yellow leaves on a plant. Leaf water potential measurements can be linked with the leaf optical properties data if the plant number in both sets of data are known. Plant water potential values measured just before dawn will provide the highest plant water potential (smallest negative value) during the day and also provides a reasonable estimate of the soil water potential. It is hypothesized that as the leaf water potential decreases (large negative value) that there may be some change in the internal structure of the leaf that would be detectable in one or more of the Nebraska Multiband Leaf Radiometer (NMLR - instrument used during leaf optical measurements) wavebands. It is also hypothesized that the amounts of water in a leaf will be lowest at low water potential and that this might also be detectable with the NMLR especially in the mid-IR wavebands.
&lt;br&gt;&lt;h4 id&#x3D;&quot;fife_biology_veg_biop_135&quot;&gt;fife_biology_veg_biop_135&lt;/h4&gt;
The Biophysical Properties of the Vegetation Data Set were collected as part of the larger FIFE Science effort to characterize the physical and biological properties of the sites within the FIFE study area over the life of the field experiment. These data were collected at 43 locations scattered throughout the FIFE study area between May 1987 and August 1989. The measurements of leaf area were based on an optical technique in which the area of the light beam obscured by the material under the beam is a measure of the surface area of that material relative to the total surface area that the beam covers. The resulting Leaf Area Indices (LAI) provide a relative measure of leaf area. These indices, when compared between plant samples provide an indirect and relative measure of plant biomass.
&lt;br&gt;&lt;h4 id&#x3D;&quot;fife_biology_veg_spec_136&quot;&gt;fife_biology_veg_spec_136&lt;/h4&gt;
The Vegetation Species and Cover Abundance Data Set documents the species present at the FIFE staff data measurement sites. Percent cover is estimated for each species at approximately the time of the IFC&amp;#39;s. Disturbances occur over a variety of spatial and temporal scales in North American grasslands, and interactions of these different disturbances affect community structure. Two types of disturbance commonly occur over large spatial scales in grasslands, namely, fire and grazing. Analysis of percent cover of dominant species indicated that composition and heterogeneity was significantly affected by grazing intensity and burning. The effects of disturbances on community structure are not additive, and may not be extrapolated from studies of single factors. The interpretation of patterns in natural communities is clearly scale dependent, and processes may act differently when viewed from different spatial or temporal scales. The effects of scale may not always be predictable; therefore, an understanding of pattern and process at one hierarchical level may not provide useful information about pattern and process at a different hierarchical level.
&lt;br&gt;&lt;h4 id&#x3D;&quot;fife_biology_veg_ref_137&quot;&gt;fife_biology_veg_ref_137&lt;/h4&gt;
The Konza Natural Research Area is a tallgrass prairie in a biologically heterogeneous environment that is rich in native plant species. Species composition is extremely variable over sites because of the effects of both natural and anthropological factors. The FIFE Vegetation Species Reference Data Set is used to associate the plant species found on the Konza Prairie with both their common and Latin names, and to translate the species codes found in the FIFE vegetation data sets to their Latin and common names.
&lt;br&gt;&lt;h4 id&#x3D;&quot;fife_atmos_wind_lid_138&quot;&gt;fife_atmos_wind_lid_138&lt;/h4&gt;
The aim of this wind profile study was to derive wind profiles and momentum fluxes from the National Oceanic and Atmospheric Administration (NOAA)/Wave Propagation Laboratory (WPL) Doppler LIDAR, and compare LIDAR and airborne measurements of mean wind, turbulent structure, momentum flux, and heat flux. Another objective was to compare profiles of mean wind and temperature obtained from aircraft, balloon sondes, and wind LIDAR. These data were collected at one location near the center of the FIFE study area but in the northwest quadrant. Data were acquired for a two week period during June and July 1987. Pulsed Doppler LIDAR measures the radial (along-beam) velocity as a function of range using light-scattering particles in the air as tracers. When the LIDAR beam is directed straight upward and the backscattered return as a function of height is recorded, vertical aerosol profiles may be determined. Various pointing and scanning schemes permit measurement of a variety of mean and turbulent quantities based on assumptions about the flow. The remote-sensing character of LIDAR offers the ability to measure flow parameters simultaneously at all the heights in a profile. The winds were obtained with the VAD (Velocity Azimuth Display) technique. The LIDAR only operates above 500 m, therefore the wind profile begins above the ground surface. Data in the planetary boundary layer are usually continuous, but gaps appear occasionally in profiles extending to several kilometers. Profiles were unsmoothed, and the LIDAR&amp;#39;s short pulse made adjacent data points almost independent.
&lt;br&gt;&lt;h4 id&#x3D;&quot;fife_atmos_wind_son_139&quot;&gt;fife_atmos_wind_son_139&lt;/h4&gt;
The wind profile data described in this document were derived from the raw radiosonde data collected during FIFE by Dr. Wilfred H. Brutsaert during the summer and fall of 1987 and the late summer of 1989 The objective of this study was to calculate wind velocity and wind direction from successive horizontal positions of a radiosonde. These data have allowed the measurement of the atmospheric profiles of wind velocity and direction. The raw data have also been corrected for sensor delays and have been interpolated to a set of standard pressure levels. Successive horizontal positions of the radiosonde balloon in relation to its release point was used to calculate average wind speed and direction. The variables used to make these calculations were obtained from the FIFE Radiosonde Data. The balloon height was calculated by adding 10 m (i.e., the length of the string) to the height of the sonde. The horizontal distance of the sonde, together with the measured azimuth angle (also obtained from the FIFE Radiosonde Data), produced the horizontal position of the sonde. Finally, successive horizontal positions allowed the calculation of average wind velocity and direction over the interval. Note, as a result of the addition of 10 m for most flights, the height of the wind measurements in this data set is 10 meters higher than the companion values in the original FIFE Radiosonde Data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.ornldaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA FLASHFLUX Project</title>
      <link>https://registry.opendata.aws/nasa-flashflux</link>
      <guid>https://registry.opendata.aws/nasa-flashflux</guid>
      <description>FLASH_SSF_Aqua-FM3-MODIS_Version4A is the Fast Longwave And Shortwave Radiative Fluxes (FLASHFlux) Clouds and Radiative Swath (SSF) Aqua-FM3-MODIS data in HDF Version 4A data product. This product consists of Low latency (&amp;lt; 5 days from observation) Top-of-Atmosphere (TOA) fluxes and parameterized surface radiative fluxes at Clouds and the Earth&amp;#39;s Radiant Energy System (CERES) Single Scanner Footprint (SSF) level for quick-look purposes. Data collection for this product is in progress. FLASHFlux data are a product line of the CERES project designed to process and release TOA and surface radiative fluxes for applied sciences and education uses. The FLASHFlux data product is a rapid-release product based on the algorithms developed for and data collected by the CERES project. CERES is currently producing world-class climate data products derived from measurements taken aboard NASA&amp;#39;s Terra and Aqua spacecraft. While of exceptional fidelity, these data products require considerable processing time to assure quality, verify accuracy, and assess precision. The result is that CERES data are typically released up to six months after acquiring the initial measurements. Such delays are of little consequence for climate studies, especially considering the improved quality of the released data products. Thus, FLASHFlux products are not intended to achieve climate quality. FLASHFlux data products were envisioned as a resource whereby CERES data could be provided to the community within a few days of the initial measurements, with some calibration accuracy requirements relaxed to gain speed. The SSF TOA/Surface Fluxes and Clouds product contains one hour of instantaneous FLASHFlux data for a single CERES scanner instrument. The SSF combines instantaneous CERES data with scene information from a higher-resolution imager, such as Moderate-Resolution Imaging Spectroradiometer (MODIS) on the Terra and Aqua satellites and meteorological and ozone information from The Goddard Earth Observing System GEOS-5 FP-IT Atmospheric Data Assimilation System (GEOS-5 ADAS). Scene identification and cloud properties are defined at the higher image resolution, and these data are averaged over the larger CERES footprint. For each CERES footprint, the SSF contains Top-of-Atmosphere fluxes in SW, LW, and NET, surface fluxes using the Langley parameterized shortwave and longwave algorithms, and cloud information. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES mission is a follow-up to the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument (PFM) was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the EOS flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board EOS Aqua on May 4, 2002. The newest CERES instrument Flight Model 5 (FM5), was launched on board the Suomi National Polar-orbiting Partnership (NPP) satellite.
&lt;br&gt;&lt;h4 id&#x3D;&quot;flash_ssf_terra-fm1-modis&quot;&gt;FLASH_SSF_Terra-FM1-MODIS&lt;/h4&gt;
FLASH_SSF_Terra-FM1-MODIS_Version4A is the Fast Longwave And Shortwave Radiative Fluxes (FLASHFlux) Clouds and Radiative Swath (SSF) TERRA-FM1 data in HDF Version 4A data product. This product consists of Low latency (&amp;lt; 5 days from observation) Top-of-Atmosphere (TOA) fluxes and parameterized surface radiative fluxes at Clouds and the Earth&amp;#39;s Radiant Energy Systems (CERES) Single Scanner Footprint (SSF) level for quick-look purposes. FLASHFlux data are a product line of the CERES project designed to process and release TOA and surface radiative fluxes for applied sciences and education uses. The FLASHFlux data product is a rapid-release product based on the algorithms developed for and data collected by the CERES project. CERES is currently producing world-class climate data products derived from measurements taken aboard NASA&amp;#39;s Terra and Aqua spacecraft. While of exceptional fidelity, these data products require considerable processing time to assure quality, verify accuracy, and assess precision. The result is that CERES data are typically released up to six months after acquiring the initial measurements. Such delays are of little consequence for climate studies, especially considering the improved quality of the released data products. Thus, FLASHFlux products are not intended to achieve climate quality. FLASHFlux data products were envisioned as a resource whereby CERES data could be provided to the community within a few days of the initial measurements, with some calibration accuracy requirements relaxed to gain speed. The SSF TOA/Surface Fluxes and Clouds product contains one hour of instantaneous FLASHFlux data for a single CERES scanner instrument. The SSF combines instantaneous CERES data with scene information from a higher-resolution imager, such as Moderate-Resolution Imaging Spectroradiometer (MODIS) on the Terra and Aqua satellites and meteorological and ozone information from The Goddard Earth Observing System (GEOS) GEOS-5 FP-IT Atmospheric Data Assimilation System (GEOS-5 ADAS). Scene identification and cloud properties are defined at the higher image resolution, and these data are averaged over the larger CERES footprint. For each CERES footprint, the SSF contains Top-of-Atmosphere fluxes in SW, LW, and NET, surface fluxes using the Langley parameterized shortwave and longwave algorithms, and cloud information. CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth&amp;#39;s atmosphere from three broadband channels. The CERES mission is a follow-up to the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument (PFM) was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the EOS flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board EOS Aqua on May 4, 2002. The newest CERES instrument, Flight Model 5 (FM5), was launched on board the Suomi National Polar-orbiting Partnership (NPP) satellite.
&lt;br&gt;&lt;h4 id&#x3D;&quot;flash_tisa_noaa20&quot;&gt;FLASH_TISA_NOAA20&lt;/h4&gt;
FLASH_TISA_NOAA20_Version1A is the Fast Longwave And SHortwave Fluxes (FLASHFlux) Daily Gridded Single Satellite Top-of-Atmosphere (TOA) and Surfaces/Clouds Version 1A data product. This product contains low latency (&amp;lt; 7 days from observations) NOAA-20 FLASHFlux Single Scanner Footprint (SSF) globally gridded TOA and parameterized surface radiative fluxes for applied science uses. Data collection for this product is in progress.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA FLDAS Project</title>
      <link>https://registry.opendata.aws/nasa-fldas</link>
      <guid>https://registry.opendata.aws/nasa-fldas</guid>
      <description>This dataset contains a series of land surface parameters simulated from the Noah 3.6.1 model in the Famine Early Warning Systems Network (FEWS NET) Land Data Assimilation System (FLDAS), adapted from Land Information System (LIS7). The dataset contains 28 parameters in a 0.10 degree spatial resolution and from January 2019 to present. The temporal resolution is monthly and the spatial coverage is global (60S, 180W, 90N, 180E). The simulation was forced by a combination of the Global Data Assimilation System (GDAS) data and Climate Hazards Group InfraRed Precipitation with Station Preliminary (CHIRPS-PRELIM) 6-hourly rainfall data that has been downscaled using the NASA Land Data Toolkit, restarted from CHIRPS-FINAL of the previous month. The simulation was initialized on January 1, 2019 using soil moisture and other state fields from a FLDAS/Noah model climatology for that day of the year.
&lt;br&gt;&lt;h4 id&#x3D;&quot;fldas_noah01_c_gl_m&quot;&gt;FLDAS_NOAH01_C_GL_M&lt;/h4&gt;
This dataset contains a series of land surface parameters simulated from the Noah 3.6.1 model in the Famine Early Warning Systems Network (FEWS NET) Land Data Assimilation System (FLDAS). The data are in 0.10 degree resolution and range from January 1982 to present. The temporal resolution is monthly and the spatial coverage is global (60S, 180W, 90N, 180E). The FLDAS regional monthly datasets will no longer be available and have been superseded by the global monthly dataset. The simulation was forced by a combination of the Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2) data and Climate Hazards Group InfraRed Precipitation with Station (CHIRPS) 6-hourly rainfall data that has been downscaled using the NASA Land Data Toolkit. The simulation was initialized on January 1, 1982 using soil moisture and other state fields from a FLDAS/Noah model climatology for that day of the year. In November 2020, all FLDAS data were post-processed with the MOD44W MODIS land mask. Previously, some grid boxes over inland water were considered as over land and, thus, had non-missing values. The post-processing corrected this issue and masked out all model output data over inland water; the post-processing did not affect the meteorological forcing variables. More information on this can be found in the FLDAS README document, and the MOD44W MODIS land mask is available on the FLDAS Project site. If you had downloaded any FLDAS data prior to November 2020, please download the data again to receive the post-processed data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;fldas_noah01_c_gl_ma&quot;&gt;FLDAS_NOAH01_C_GL_MA&lt;/h4&gt;
The monthly anomaly data set contains a series of land surface parameters simulated from the Noah 3.6.1 model in the Famine Early Warning Systems Network (FEWS NET) Land Data Assimilation System (FLDAS). The dataset comprises of monthly files, each representing how the month compares to the 35-year monthly climatology from 1982 to 2016, based on the FLDAS Noah Land Surface Model L4 Global Monthly 0.1 x 0.1 degree (MERRA-2 and CHIRPS) V001 (FLDAS_NOAH01_C_GL_M_001) monthly data. The data are in 0.10 degree resolution and the spatial coverage is global (60S, 180W, 90N, 180E). The FLDAS regional monthly anomaly datasets will no longer be available and have been superseded by the global monthly anomaly dataset. More information about the monthly FLDAS can be found from the dataset landing page for FLDAS_NOAH01_C_GL_M_001 and the FLDAS README document. In November 2020, all FLDAS data were post-processed with the MOD44W MODIS land mask. Previously, some grid boxes over inland water were considered as over land and, thus, had non-missing values. The post-processing corrected this issue and masked out all model output data over inland water; the post-processing did not affect the meteorological forcing variables. More information on this can be found in the FLDAS README document, and the MOD44W MODIS land mask is available on the FLDAS Project site. If you had downloaded any FLDAS data prior to November 2020, please download the data again to receive the post-processed data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;fldas_noah01_c_gl_mc&quot;&gt;FLDAS_NOAH01_C_GL_MC&lt;/h4&gt;
The monthly climatology dataset contains a series of land surface parameters simulated from the Noah 3.6.1 model in the Famine Early Warning Systems Network (FEWS NET) Land Data Assimilation System (FLDAS). The dataset comprises of 12 monthly files, each representing the monthly data averaged over 35 years from 1982 to 2016, based on the FLDAS Noah Land Surface Model L4 Global Monthly 0.1 x 0.1 degree (MERRA-2 and CHIRPS) V001 (FLDAS_NOAH01_C_GL_M_001) monthly data. The data are in 0.10 degree resolution and the spatial coverage is global (60S, 180W, 90N, 180E). The FLDAS regional monthly climatology datasets will no longer be available and have been superseded by the global monthly climatology dataset. More information about the monthly FLDAS can be found from the dataset landing page for FLDAS_NOAH01_C_GL_M_001 and the FLDAS README document. In November 2020, all FLDAS data were post-processed with the MOD44W MODIS land mask. Previously, some grid boxes over inland water were considered as over land and, thus, had non-missing values. The post-processing corrected this issue and masked out all model output data over inland water; the post-processing did not affect the meteorological forcing variables. More information on this can be found in the FLDAS README document, and the MOD44W MODIS land mask is available on the FLDAS Project site. If you had downloaded any FLDAS data prior to November 2020, please download the data again to receive the post-processed data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;fldas_noahmp001_g_ca_d&quot;&gt;FLDAS_NOAHMP001_G_CA_D&lt;/h4&gt;
This dataset contains land surface parameters simulated by the Famine Early Warning Systems Network (FEWS NET) Land Data Assimilation System version 2 (FLDAS2) Central Asia model. The FLDAS2 Central Asia model is a custom instance of the NASA Land Information System that has been adapted to work with domains, data streams, and monitoring and forecast requirements associated with food security assessment in data-sparse, developing country settings. The data are produced using the Noah Multi-Parameterization (Noah-MP) version 4.0.1 Land Surface Model (LSM) forced by Global Data Assimilation System (GDAS) meteorological data. The FLDAS2 Central Asia dataset is produced daily with a one-day latency. Data are available from October 1, 2000 to present. The dataset contains 27 parameters at a 0.01 degree spatial resolution over the Central Asia region (30-100°E, 21-56°N).
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA Fluxnet Project</title>
      <link>https://registry.opendata.aws/nasa-fluxnet</link>
      <guid>https://registry.opendata.aws/nasa-fluxnet</guid>
      <description>CO2 and water vapor fluxes and ecosystem characteristics were measured at 24 sites along a 317-km transect from the Arctic coast to the latitudinal treeline in Alaska during the growing seasons of 1994-1996. The sites were stratified to sample the ranges of climate, physiography, soil moisture, and vegetation type within the region. Our main objective was to understand what factors control variations in CO2 and water vapor exchange across the region. We therefore developed a spatially extensive approach of documenting fluxes for 1-2 weeks at each of the sites in order to study as many sites as possible during the middle of the short arctic growing season, when plant phenology is most comparable among different vegetation types and climatic regions. This allowed us to compare, with some replication, a given vegetation type across different provinces and climatic zones, as well as multiple vegetation types within a given geographic area.
&lt;br&gt;&lt;h4 id&#x3D;&quot;fluxnet_canada_1335&quot;&gt;FLUXNET_Canada_1335&lt;/h4&gt;
FLUXNET Canada is a Fluxnet research network comprised of the Fluxnet-Canada Research Network (FCRN) and the Canadian Carbon Program (CCP) operating from 1993 through 2014. It was a national research network of university and government scientists studying the influence of climate and disturbance on carbon cycling along an east-west transect of Canadian forest and peat land ecosystems. The data provided are measured and modeled results as obtained from the site investigators. They were not standardized and quality-controlled. Data include: atmospheric carbon dioxide (CO2) and water vapor fluxes and many ancillary meteorological variables; soil CO2 efflux and soil moisture; stable carbon isotopes; site soil and vegetation characteristics, plus documentation and descriptions for the 32 tower sites across 12 flux research stations. The time period is from 1993 - 2014; most reported data for a site does not cover the entire period.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gap_filled_marconi_811&quot;&gt;gap_filled_marconi_811&lt;/h4&gt;
Fluxes of carbon dioxide, water vapor, and energy exchange have been measured at 38 forest, grassland, and crop sites as part of the EUROFLUX and AmeriFlux projects. A total of 97 site-years of data were compiled, primarily between 1996 and 1998 but also for 1992-1995 and 1999-2000. Half-hour flux and meteorology measurements are included plus the gap-filled half-hour estimates and aggregations to day and night, weekly, monthly, and annual periods. The FLUXNET 2000 Synthesis Workshop was held at the Marconi Conference Center, Marshall, California, June 11-14, 2000. The Marconi Flux Data Collection was compiled to aid in exploring the interactions between the terrestrial biosphere and the overlying atmosphere through carbon, water, and energy exchanges. The workshop resulted in several studies to synthesize and interpret differences and similarities in long-term measurements of carbon dioxide, water vapor, and energy exchanges between vegetation and the atmosphere for a spectrum of ecosystems. A series of synthesis papers based on these data and studies was published in a special issue of the Agriculture and Forest Meteorology, Volume 113, 2002. The papers are listed in the reference section. This data product is being archived as a record of the data used the AFM special issue. Updates and revisions to the data are available at the FLUXNET web site.The eddy covariance technique is used for long-term continuous measurements of mass and energy fluxes to capture seasonal dynamics and allow for a meaningful scaling with respect to time. The equipment and methodology were standardized among sites by using common software and instrumentation. Comparisons of ecosystem fluxes among sites are usually performed on annual or monthly sums calculated on complete data records; however, the average site data coverage during a year was only 65%. Therefore, development and application of robust and consistent data gap-filling methods was required before fluxes could be calculated. One of the outcomes of the FLUXNET project was computer applications to process the data into complete, consistent, quality assured, and documented data sets (Falge et al. 2001a,b). Gap-filled flux data from four different filling methods are reported. Selected meteorological parameters were also gap filled to support flux estimating methods and are reported along with non-filled meteorological data. Note that the measured/estimated CO2 fluxes and storage fluxes were summed into net ecosystem exchange (NEE), and ONLY NEE data are reported.
&lt;br&gt;&lt;h4 id&#x3D;&quot;fluxnet_site_db_1530&quot;&gt;Fluxnet_site_DB_1530&lt;/h4&gt;
FLUXNET is a global network of micrometeorological tower sites that use eddy covariance methods to measure the exchanges of carbon dioxide, water vapor, and energy between terrestrial ecosystems and the atmosphere. This dataset provides information from the ORNL DAAC-hosted FLUXNET site database which was discontinued in 2016. The files provided contain a list of investigators associated with each tower site, site locations and environmental data, and a bibliography of papers that used FLUXNET data. For more up to date information on FLUXNET sites, see &lt;a href&#x3D;&quot;http://fluxnet.fluxdata.org/&quot;&gt;http://fluxnet.fluxdata.org/&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;fluxnet_website_archive_copy_1549&quot;&gt;Fluxnet_website_archive_copy_1549&lt;/h4&gt;
This dataset contains an archived copy of the fluxnet.ornl.gov website as of September 2017. This archived website is provided for informational purposes only. The last updates to the website and the underlying database were made in October 2016. Support for the Fluxnet project and website was transitioned to &lt;a href&#x3D;&quot;http://fluxnet.fluxdata.org&quot;&gt;http://fluxnet.fluxdata.org&lt;/a&gt; in September 2017. Please see &lt;a href&#x3D;&quot;http://fluxnet.fluxdata.org/&quot;&gt;http://fluxnet.fluxdata.org/&lt;/a&gt; for information on site locations, data availability, and to add or update a flux tower site.
&lt;br&gt;&lt;h4 id&#x3D;&quot;net_carbon_flux_662&quot;&gt;net_carbon_flux_662&lt;/h4&gt;
The variability of net surface carbon assimilation (Asmax), net ecosystem surface respiration (Rsmax), and net surface evapotranspiration (Etsmax) among and within vegetation types was examined based on a review of studies performed in either a micrometeorological setting or an enclosure setting. The majority of studies involved forests and C3 crops, particularly in the northern hemisphere; however, studies on tropical forests, C4 grasslands or wetlands were included. Data are presented for 133 published studies, although individual studies may not have measure all variables of interest.Despite large variations within a vegetation type, enclosure studies tended to give highest Asmax rates compared to micrometeorological techniques (Buchmann and Schulze 1999). Excluding enclosure studies, the investigators tested the effect of stand age and leaf area index (LAI) on net ecosystem gas exchange. The results from these analyses illustrate where gaps in scientific knowledge exist and how ecosystem properties affect the capacity of net ecosystem gas exchange.The information was collected from papers with publication dates from 1969-1998. Mean maximum flux rates for the period chosen by the authors were used instead of absolute maximum values for flux rates. Positive values stand for CO2 uptake by the vegetation and negative values represent CO2 release from the ecosystem. More information about the compilation can be found in Buchmann and Schultze (1999) or the individual studies cited in the data table.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.ornldaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA G-LiHT Project</title>
      <link>https://registry.opendata.aws/nasa-g-liht</link>
      <guid>https://registry.opendata.aws/nasa-g-liht</guid>
      <description>Goddard’s LiDAR, Hyperspectral, and Thermal Imager (&lt;a href&#x3D;&quot;https://gliht.gsfc.nasa.gov/&quot;&gt;G-LiHT&lt;/a&gt;) mission is a portable, airborne imaging system that aims to simultaneously map the composition, structure, and function of terrestrial ecosystems. G-LiHT primarily focuses on a broad diversity of forest communities and ecoregions in North America, mapping aerial swaths over the Conterminous United States (CONUS), Alaska, Puerto Rico, and Mexico. The purpose of G-LiHT’s Aerial Orthomosaic data product (GLORTHO) is to provide orthorectified high-resolution aerial photography. This data is provided as a supplement to other G-LiHT data products. GLORTHO data are processed as a raster data product (GeoTIFF) at 1 inch spatial resolution over locally defined areas. A low resolution browse is also provided with a color map applied in PNG format. Known Issues: Orthomosaics are automatically generated, and results may not be optimal.
&lt;br&gt;&lt;h4 id&#x3D;&quot;glchmk&quot;&gt;GLCHMK&lt;/h4&gt;
Goddard’s LiDAR, Hyperspectral, and Thermal Imager (&lt;a href&#x3D;&quot;https://gliht.gsfc.nasa.gov/&quot;&gt;G-LiHT&lt;/a&gt;) mission utilizes a portable, airborne imaging system that aims to simultaneously map the composition, structure, and function of terrestrial ecosystems. G-LiHT primarily focuses on a broad diversity of forest communities and ecoregions in North America, mapping aerial swaths over the Conterminous United States (CONUS), Alaska, Puerto Rico, and Mexico. The purpose of G-LiHT’s Canopy Height Model Keyhole Markup Language (KML) data product (GLCHMK) is to provide LiDAR-derived maximum canopy height and canopy variability information to aid in the study and analysis of biodiversity and climate change. Scientists at NASA’s Goddard Space Flight Center began collecting data over locally-defined areas in 2011 and that the collection will continue to grow as aerial campaigns are flown and processed. GLCHMK data are processed as a Google Earth overlay KML file at a nominal 1 meter spatial resolution over locally-defined areas. A low resolution browse is also provided showing the canopy height with a color map applied in JPEG format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gldsmt&quot;&gt;GLDSMT&lt;/h4&gt;
Goddard’s LiDAR, Hyperspectral, and Thermal Imagery (&lt;a href&#x3D;&quot;https://gliht.gsfc.nasa.gov/&quot;&gt;G-LiHT&lt;/a&gt;) mission is a portable, airborne imaging system that aims to simultaneously map the composition, structure, and function of terrestrial ecosystems. G-LiHT primarily focuses on a broad diversity of forest communities and ecoregions in North America, mapping aerial swaths over the Conterminous United States (CONUS), Alaska, Puerto Rico, and Mexico. The purpose of G-LiHT’s Digital Surface Model data product (GLDSMT) is to provide LiDAR-derived visualizations of elevation above bare earth. GLDSMT data is offered in multiple formats, including Digital Surface Model, Mean, Aspect, Rugosity, and Slope. GLDSMT data are processed as multiple raster data products (GeoTIFFs) at a nominal 1 meter spatial resolution over locally defined areas. A low resolution browse is also provided showing the digital surface model with a color map applied in PNG format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gltrajectory&quot;&gt;GLTRAJECTORY&lt;/h4&gt;
Goddard’s LiDAR, Hyperspectral, and Thermal Imagery (&lt;a href&#x3D;&quot;https://gliht.gsfc.nasa.gov/&quot;&gt;G-LiHT&lt;/a&gt;) mission is a portable, airborne imaging system that aims to simultaneously map the composition, structure, and function of terrestrial ecosystems. G-LiHT primarily focuses on a broad diversity of forest communities and ecoregions in North America, mapping aerial swaths over Conterminous United States (CONUS), Alaska, Puerto Rico, and Mexico. The purpose of G-LiHT’s Trajectory data product (GLTRAJECTORY) is to provide aircraft location and orientation to support and supplement other G-LiHT data products. GLTRAJECTORY data are processed as a Google Earth overlay Keyhole Markup Language (KML) file over the extent of an entire flight path. A low resolution browse is also provided to show the flight path.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA GCOM-W Project</title>
      <link>https://registry.opendata.aws/nasa-gcom-w</link>
      <guid>https://registry.opendata.aws/nasa-gcom-w</guid>
      <description>AMSR2/GCOM-W1 downscaled surface soil moisture (LPRM) L2B V001 is a Level 2 (swath) data set. Its land surface parameters, surface soil moisture, land surface (skin) temperature, and vegetation water content, are derived from passive microwave remote sensing data from the Advanced Microwave Scanning Radiometer 2 (AMSR2), using the Land Parameter Retrieval Model (LPRM). Each swath is packaged with associated geolocation fields. The data set covers the period from May 2012, when the Japan Aerospace Exploration Agency (JAXA) Global Change Observation Mission-1st Water GCOM-W1 satellite was launched, to the present. The spatial resolution of the data is based on a resampling of the nominally 46 and 31 km resolutions, respectively, of AMSR2&amp;#39;s C and X bands (6.9/7.3 and 10.7 GHz, respectively) to 25 km by 25 km and then a downscaling, using the smoothing filter-based intensity modulation (SFIM) technique, to 10 km by 10 km grids. The LPRM is based on a forward radiative transfer model to retrieve surface soil moisture and vegetation optical depth. The land surface temperature is derived separately from the AMSR2&amp;#39;s Ka-band (36.5 GHz). A unique feature of this method is that it can be applied at any microwave frequency, making it very suitable to exploit all the available passive microwave data from various satellites. Input data are from the AMSR2 spatial-resolution-matched brightness temperatures (L1SGRTBR) product, archived at JAXA.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lprm_amsr2_soilm2&quot;&gt;LPRM_AMSR2_SOILM2&lt;/h4&gt;
AMSR2/GCOM-W1 surface soil moisture (LPRM) L2B V001 is a Level 2 (swath) data set. Its land surface parameters, surface soil moisture, land surface (skin) temperature, and vegetation water content are derived from passive microwave remote sensing data from the Advanced Microwave Scanning Radiometer 2 (AMSR2), using the Land Parameter Retrieval Model (LPRM). Each swath is packaged with associated geolocation fields. The data set covers the period from May 2012, when the Japan Aerospace Exploration Agency (JAXA) Global Change Observation Mission-1st Water GCOM-W1 satellite was launched, to the present, at a spatial resolution (nominally 46 and 31 km, respectively) of AMSR2&amp;#39;s C and X bands (6.9/7.3 and 10.7 GHz, respectively). The LPRM is based on a forward radiative transfer model to retrieve surface soil moisture and vegetation optical depth. The land surface temperature is derived separately from the AMSR2&amp;#39;s Ka-band (36.5 GHz). A unique feature of this method is that it can be applied at any microwave frequency, making it very suitable to exploit all the available passive microwave data from various satellites. Input data are from the AMSR2 spatial-resolution-matched brightness temperatures (L1SGRTBR) product, archived at JAXA.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lprm_amsr2_ds_a_soilm3&quot;&gt;LPRM_AMSR2_DS_A_SOILM3&lt;/h4&gt;
AMSR2/GCOM-W1 surface soil moisture (LPRM) L3 1 day 10 km x 10 km ascending V001 is a Level 3 (gridded) data set. Its land surface parameters, surface soil moisture, land surface (skin) temperature, and vegetation water content, are derived from passive microwave remote sensing data from the Advanced Microwave Scanning Radiometer 2 (AMSR2), using the Land Parameter Retrieval Model (LPRM). There are two files per day, one ascending (daytime) and one descending (nighttime), archived as two different products. This document is for the daytime product. The data set covers the period from May 2012, when the Japan Aerospace Exploration Agency (JAXA) Global Change Observation Mission-1st Water GCOM-W1 satellite was launched, to the present. The LPRM is based on a forward radiative transfer model to retrieve surface soil moisture and vegetation optical depth. The land surface temperature is derived separately from the AMSR2&amp;#39;s Ka-band (36.5 GHz). A unique feature of this method is that it can be applied at any microwave frequency, making it very suitable to exploit all the available passive microwave data from various satellites. Input data are from the AMSR2 spatial-resolution-matched brightness temperatures (L1SGRTBR) product, daytime passes, as processed using LPRM (i.e., LPRM/AMSR2/GCOM-W1 Downscaled Level 2 product, LPRM_AMSR2_DS_SOILM2_V001).
&lt;br&gt;&lt;h4 id&#x3D;&quot;lprm_amsr2_ds_d_soilm3&quot;&gt;LPRM_AMSR2_DS_D_SOILM3&lt;/h4&gt;
AMSR2/GCOM-W1 surface soil moisture (LPRM) L3 1 day 10 km x 10 km descending V001 is a Level 3 (gridded) data set. Its land surface parameters, surface soil moisture, land surface (skin) temperature, and vegetation water content, are derived from passive microwave remote sensing data from the Advanced Microwave Scanning Radiometer 2 (AMSR2), using the Land Parameter Retrieval Model (LPRM). There are two files per day, one ascending (daytime) and one descending (nighttime), archived as two different products. This document is for the nighttime product. The data set covers the period from May 2012, when the Japan Aerospace Exploration Agency (JAXA) Global Change Observation Mission-1st Water GCOM-W1 satellite was launched, to the present. The LPRM is based on a forward radiative transfer model to retrieve surface soil moisture and vegetation optical depth. The land surface temperature is derived separately from the AMSR2&amp;#39;s Ka-band (36.5 GHz). A unique feature of this method is that it can be applied at any microwave frequency, making it very suitable to exploit all the available passive microwave data from various satellites. Input data are from the AMSR2 spatial-resolution-matched brightness temperatures (L1SGRTBR) product, nighttime passes, as processed using LPRM (i.e., LPRM/AMSR2/GCOM-W1 Downscaled Level 2 product, LPRM_AMSR2_DS_SOILM2_V001).
&lt;br&gt;&lt;h4 id&#x3D;&quot;lprm_amsr2_a_soilm3&quot;&gt;LPRM_AMSR2_A_SOILM3&lt;/h4&gt;
AMSR2/GCOM-W1 surface soil moisture (LPRM) L3 1 day 25 km x 25 km ascending V001 is a Level 3 (gridded) data set. Its land surface parameters, surface soil moisture, land surface (skin) temperature, and vegetation water content, are derived from passive microwave remote sensing data from the Advanced Microwave Scanning Radiometer 2 (AMSR2), using the Land Parameter Retrieval Model (LPRM). There are two files per day, one ascending (daytime) and one descending (nighttime), archived as two different products. This document is for the daytime product. The data set covers the period from May 2012, when the Japan Aerospace Exploration Agency (JAXA) Global Change Observation Mission-1st Water GCOM-W1 satellite was launched, to the present. The LPRM is based on a forward radiative transfer model to retrieve surface soil moisture and vegetation optical depth. The land surface temperature is derived separately from the AMSR2&amp;#39;s Ka-band (36.5 GHz). A unique feature of this method is that it can be applied at any microwave frequency, making it very suitable to exploit all the available passive microwave data from various satellites. Input data are from the AMSR2 spatial-resolution-matched brightness temperatures (L1SGRTBR) product, daytime passes, as processed using LPRM (i.e., LPRM/AMSR2/GCOM-W1 Level 2 product, LPRM_AMSR2_SOILM2_V001).
&lt;br&gt;&lt;h4 id&#x3D;&quot;lprm_amsr2_d_soilm3&quot;&gt;LPRM_AMSR2_D_SOILM3&lt;/h4&gt;
AMSR2/GCOM-W1 surface soil moisture (LPRM) L3 1 day 25 km x 25 km descending V001 is a Level 3 (gridded) data set. Its land surface parameters, surface soil moisture, land surface (skin) temperature, and vegetation water content, are derived from passive microwave remote sensing data from the Advanced Microwave Scanning Radiometer 2 (AMSR2), using the Land Parameter Retrieval Model (LPRM). There are two files per day, one ascending (daytime) and one descending (nighttime), archived as two different products. This document is for the nighttime product. The data set covers the period from May 2012, when the Japan Aerospace Exploration Agency (JAXA) Global Change Observation Mission-1st Water GCOM-W1 satellite was launched, to the present. The LPRM is based on a forward radiative transfer model to retrieve surface soil moisture and vegetation optical depth. The land surface temperature is derived separately from the AMSR2&amp;#39;s Ka-band (36.5 GHz). A unique feature of this method is that it can be applied at any microwave frequency, making it very suitable to exploit all the available passive microwave data from various satellites. Input data are from the AMSR2 spatial-resolution-matched brightness temperatures (L1SGRTBR) product, nighttime passes, as processed using LPRM (i.e., LPRM/AMSR2/GCOM-W1 Level 2 product, LPRM_AMSR2_SOILM2_V001).
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA GEDI Project</title>
      <link>https://registry.opendata.aws/nasa-gedi</link>
      <guid>https://registry.opendata.aws/nasa-gedi</guid>
      <description>GEDI Version 1 data products were decommissioned on February 15, 2022. Users are advised to use the improved &lt;a href&#x3D;&quot;https://doi.org/10.5067/GEDI/GEDI01_B.002&quot;&gt;GEDI01_B Version 2&lt;/a&gt; data product. The Global Ecosystem Dynamics Investigation (GEDI) mission aims to characterize ecosystem structure and dynamics to enable radically improved quantification and understanding of the Earth’s carbon cycle and biodiversity. The GEDI instrument produces high resolution laser ranging observations of the 3-dimensional structure of the Earth. GEDI is attached to the International Space Station and collects data globally between 51.6 degrees N and 51.6 degrees S latitudes at the highest resolution and densest sampling of any light detection and ranging (lidar) instrument in orbit to date. The GEDI Level 1B Geolocated Waveforms product (GEDI01_B) provides geolocated corrected and smoothed waveforms, geolocation parameters, and geophysical corrections for each laser shot for all eight GEDI beams. GEDI01_B data are created by geolocating the GEDI01_A raw waveform data. The GEDI01_B product is provided in HDF5 format and has a spatial resolution (average footprint) of 25 meters. The GEDI01 B data product contains 83 variables for each of the eight beams including the geolocated corrected and smoothed waveform datasets and parameters and the accompanying ancillary, geolocation, and geophysical correction. Additional information can be found in the GEDI L1B Product Data Dictionary. Known Issues: Known Issues: Section 6.1 of the User Guide provides additional information on known issues. * Data acquisition gaps: GEDI data acquisitions were suspended on December 19, 2019 (2019 Day 353) and resumed on January 8, 2020 (2020 Day 8).
&lt;br&gt;&lt;h4 id&#x3D;&quot;gedi01_b&quot;&gt;GEDI01_B&lt;/h4&gt;
The Global Ecosystem Dynamics Investigation (&lt;a href&#x3D;&quot;https://gedi.umd.edu/&quot;&gt;GEDI&lt;/a&gt;) mission aims to characterize ecosystem structure and dynamics to enable radically improved quantification and understanding of the Earth’s carbon cycle and biodiversity. The GEDI instrument produces high resolution laser ranging observations of the 3-dimensional structure of the Earth. GEDI is attached to the International Space Station (ISS) and collects data globally between 51.6° N and 51.6° S latitudes at the highest resolution and densest sampling of any light detection and ranging (lidar) instrument in orbit to date. Each GEDI Version 2 granule encompasses one-fourth of an ISS orbit and includes georeferenced metadata to allow for spatial querying and subsetting. The GEDI instrument was removed from the ISS and placed into storage on March 17, 2023. No data were acquired during the hibernation period from March 17, 2023, to April 24, 2024. GEDI has since been reinstalled on the ISS and resumed operations as of April 26, 2024. The GEDI Level 1B Geolocated Waveforms product (GEDI01_B) provides geolocated corrected and smoothed waveforms, geolocation parameters, and geophysical corrections for each laser shot for all eight GEDI beams. GEDI01_B data are created by geolocating the GEDI01_A raw waveform data. The GEDI01_B product is provided in HDF5 format and has a spatial resolution (average footprint) of 25 meters. The GEDI01_B data product contains 85 layers for each of the eight beams including the geolocated corrected and smoothed waveform datasets and parameters and the accompanying ancillary, geolocation, and geophysical correction. Additional information can be found in the GEDI L1B Product Data Dictionary. Known Issues: Data acquisition gaps: GEDI data acquisitions were suspended on December 19, 2019 (2019 Day 353) and resumed on January 8, 2020 (2020 Day 8). * Incorrect Reference Ground Track (RGT) number in the filename for select GEDI files: GEDI Science Data Products for six orbits on August 7, 2020, and November 12, 2021, had the incorrect RGT number in the filename. There is no impact to the science data, but users should reference this &lt;a href&#x3D;&quot;https://lpdaac.usgs.gov/documents/2236/GEDI_CORRECTED_RGT_FILENAMES.pptx&quot;&gt;document&lt;/a&gt; for the correct RGT numbers. * Known Issues: Section 8 of the User Guide provides additional information on known issues.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gedi02_a&quot;&gt;GEDI02_A&lt;/h4&gt;
GEDI Version 1 data products were decommissioned on February 15, 2022. Users are advised to use the improved &lt;a href&#x3D;&quot;https://doi.org/10.5067/GEDI/GEDI02_A.002&quot;&gt;GEDI02_A Version 2&lt;/a&gt; data product. The Global Ecosystem Dynamics Investigation (GEDI) mission aims to characterize ecosystem structure and dynamics to enable radically improved quantification and understanding of the Earth’s carbon cycle and biodiversity. The GEDI instrument produces high resolution laser ranging observations of the 3-dimensional structure of the Earth. GEDI is attached to the International Space Station and collects data globally between 51.6 degrees N and 51.6 degrees S latitudes at the highest resolution and densest sampling of any light detection and ranging (lidar) instrument in orbit to date. The purpose of the GEDI Level 2A Geolocated Elevation and Height Metrics product (GEDI02_A) is to provide waveform interpretation and extracted products from each GEDI01_B received waveform, including ground elevation, canopy top height, and relative height (RH) metrics. The methodology for generating the GEDI02_A product datasets is adapted from the Land, Vegetation, and Ice Sensor (LVIS) algorithm. The GEDI01_B product is provided in HDF5 format and has a spatial resolution (average footprint) of 25 meters. The GEDI02_A data product contains 156 variables for each of the eight beams, including ground elevation, canopy top height, relative return energy metrics (describing canopy vertical structure, for example), and many other interpreted products from the return waveforms. Additional information for the variables can be found in the GEDI Level 2A Dictionary. Known Issues: Known Issues: Section 7 of the User Guide provides additional information on known issues. * Data acquisition gaps: GEDI data acquisitions were suspended on December 19, 2019 (2019 Day 353) and resumed on January 8, 2020 (2020 Day 8).
&lt;br&gt;&lt;h4 id&#x3D;&quot;gedi02_b&quot;&gt;GEDI02_B&lt;/h4&gt;
GEDI Version 1 data products were decommissioned on February 15, 2022. Users are advised to use the improved GEDI02_B Version 2 (&lt;a href&#x3D;&quot;https://doi.org/10.5067/GEDI/GEDI02_B.002&quot;&gt;https://doi.org/10.5067/GEDI/GEDI02_B.002&lt;/a&gt;) data product. The Global Ecosystem Dynamics Investigation (GEDI) mission aims to characterize ecosystem structure and dynamics to enable radically improved quantification and understanding of the Earth’s carbon cycle and biodiversity. The GEDI instrument produces high resolution laser ranging observations of the 3-dimensional structure of the Earth. GEDI is attached to the International Space Station and collects data globally between 51.6 degrees N and 51.6 degrees S latitudes at the highest resolution and densest sampling of any light detection and ranging (lidar) instrument in orbit to date. The purpose of the GEDI Level 2B Canopy Cover and Vertical Profile Metrics product (GEDI02_B) is to extract biophysical metrics from each GEDI waveform. These metrics are based on the directional gap probability profile derived from the L1B waveform. Metrics provided include canopy cover, Plant Area Index (PAI), Plant Area Volume Density (PAVD), and Foliage Height Diversity (FHD). The GEDI02_B product is provided in HDF-5 format and has a spatial resolution (average footprint) of 25 meters. The GEDI02_B data product contains 96 variables for each of the eight-beam ground transects (or laser footprints located on the land surface). Variables provided include precise latitude, longitude, elevation, height, canopy cover, and vertical profile metrics. Additional information for the variables can be found in the GEDI Level 2B Data Dictionary. Known Issues: Known Issues: Section 7 of the User Guide provides additional information on known issues. * Data acquisition gaps: GEDI data acquisitions were suspended on December 19, 2019 (2019 Day 353) and resumed on January 8, 2020 (2020 Day 8).
&lt;br&gt;&lt;h4 id&#x3D;&quot;gedi_l3_land_surface_metrics_1865&quot;&gt;GEDI_L3_Land_Surface_Metrics_1865&lt;/h4&gt;
This dataset provides Global Ecosystem Dynamics Investigation (GEDI) Level 3 (L3) gridded mean canopy height, standard deviation of canopy height, mean ground elevation, standard deviation of ground elevation and counts of laser footprints per 1 km x 1 km grid cells globally within -52 and 52 degrees latitude. L3 gridded products can be used to characterize important carbon and water cycling processes, biodiversity, habitat and can also be of immense value for climate modeling, forest management, snow and glacier monitoring, and the generation of digital elevation models. This first release of L3 products are simple averages and standard deviations of the footprint profile metrics within each 1 sq. km cell. Future versions will optimally interpolate data to produce the best estimate of the mean and its error for each grid cell.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gedi_l3_landsurface_metrics_v2_1952&quot;&gt;GEDI_L3_LandSurface_Metrics_V2_1952&lt;/h4&gt;
This dataset provides Global Ecosystem Dynamics Investigation (GEDI) Level 3 (L3) gridded mean canopy height, standard deviation of canopy height, mean ground elevation, standard deviation of ground elevation, and counts of laser footprints per 1-km x 1-km grid cells globally within -52 and 52 degrees latitude. These L3 gridded products were derived from Level 2 (L2) geolocated laser footprint return profile metrics from the GEDI instrument onboard the International Space Station (ISS). Canopy height is provided as the mean height (in meters) above the ground of the received waveform signal that was the first reflection off the top of the canopy (RH100). Ground elevation is provided as the mean elevation (in meters) of the center of the lowest waveform mode relative to the WGS84 reference ellipsoid. L3 gridded products can be used to characterize important carbon and water cycling processes, biodiversity, habitat and can also be of immense value for climate modeling, forest management, snow and glacier monitoring, and the generation of digital elevation models. This dataset version uses Version 2 of the input L2 data, which includes improved geolocation of the footprints as well as a modified method to predict an optimum algorithm setting group.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gedi_l4a_agb_density_gw_2028&quot;&gt;GEDI_L4A_AGB_Density_GW_2028&lt;/h4&gt;
This dataset contains Global Ecosystem Dynamics Investigation (GEDI) Level 4A (L4A) predictions of the aboveground biomass density (AGBD; in Mg/ha) and estimates of the prediction standard error within each sampled geolocated laser footprint. The footprints are located within the global latitude band observed by the International Space Station (ISS), nominally 51.6 degrees N and S and reported for the mission weeks 19, 32, 34 and 38 (a.k.a. Golden Weeks). These weeks cover the range of instrument operating conditions important for calibration and validation of geolocation algorithms, and also include GEDI orbits that are coincident with underflights acquired by the LVIS (Land, Vegetation, and Ice Sensor) airborne lidar instrument. The GEDI instrument consists of three lasers producing a total of eight beam ground transects, which instantaneously sample eight ~25 m footprints spaced approximately every 60 m along-track. The GEDI beam transects are spaced approximately 600 m apart on the Earth&amp;#39;s surface in the cross-track direction, for an across-track width of ~4.2 km. Footprint AGBD was derived from parametric models that relate simulated GEDI Level 2A (L2A) waveform relative height (RH) metrics to field plot estimates of AGBD. Height metrics from simulated waveforms associated with field estimates of AGBD from multiple regions and plant functional types (PFT) were compiled to generate a calibration dataset for models representing the combinations of world regions and PFTs (i.e., deciduous broadleaf trees, evergreen broadleaf trees, evergreen needleleaf trees, deciduous needleleaf trees, and the combination of grasslands, shrubs, and woodlands).
&lt;br&gt;&lt;h4 id&#x3D;&quot;gedi_l4a_agb_density_1907&quot;&gt;GEDI_L4A_AGB_Density_1907&lt;/h4&gt;
This dataset contains Global Ecosystem Dynamics Investigation (GEDI) Level 4A (L4A) predictions of the aboveground biomass density (AGBD; in Mg/ha) and estimates of the prediction standard error within each sampled geolocated laser footprint. The footprints are located within the global latitude band observed by the International Space Station (ISS), nominally 51.6 degrees N and S and reported for the period 2019-04-18 to 2020-09-02. The GEDI instrument consists of three lasers producing a total of eight beam ground transects, which instantaneously sample eight ~25 m footprints spaced approximately every 60 m along-track. The GEDI beam transects are spaced approximately 600 m apart on the Earth&amp;#39;s surface in the cross-track direction, for an across-track width of ~4.2 km. Footprint AGBD was derived from parametric models that relate simulated GEDI Level 2A (L2A) waveform relative height (RH) metrics to field plot estimates of AGBD. Height metrics from simulated waveforms associated with field estimates of AGBD from multiple regions and plant functional types (PFT) were compiled to generate a calibration dataset for models representing the combinations of world regions and PFTs (i.e., deciduous broadleaf trees, evergreen broadleaf trees, evergreen needleleaf trees, deciduous needleleaf trees, and the combination of grasslands, shrubs, and woodlands).
&lt;br&gt;&lt;h4 id&#x3D;&quot;gedi_l4a_agb_density_v2_1986&quot;&gt;GEDI_L4A_AGB_Density_V2_1986&lt;/h4&gt;
This dataset contains Global Ecosystem Dynamics Investigation (GEDI) Level 4A (L4A) Version 2 predictions of the aboveground biomass density (AGBD; in Mg/ha) and estimates of the prediction standard error within each sampled geolocated laser footprint. In this version, the granules are in sub-orbits. The algorithm setting group selection used for GEDI02_A Version 2 has been modified for Evergreen Broadleaf Trees in South America to reduce false positive errors resulting from the selection of waveform modes above ground elevation as the lowest mode. The footprints are located within the global latitude band observed by the International Space Station (ISS), nominally 51.6 degrees N and S and reported for the period 2019-04-18 to 2021-08-05. The GEDI instrument consists of three lasers producing a total of eight beam ground transects, which instantaneously sample eight ~25 m footprints spaced approximately every 60 m along-track. The GEDI beam transects are spaced approximately 600 m apart on the Earth&amp;#39;s surface in the cross-track direction, for an across-track width of ~4.2 km. Footprint AGBD was derived from parametric models that relate simulated GEDI Level 2A (L2A) waveform relative height (RH) metrics to field plot estimates of AGBD. Height metrics from simulated waveforms associated with field estimates of AGBD from multiple regions and plant functional types (PFTs) were compiled to generate a calibration dataset for models representing the combinations of world regions and PFTs (i.e., deciduous broadleaf trees, evergreen broadleaf trees, evergreen needleleaf trees, deciduous needleleaf trees, and the combination of grasslands, shrubs, and woodlands). For each of the eight beams, additional data are reported with the AGBD estimates, including the associated uncertainty metrics, quality flags, model inputs, and other information about the GEDI L2A waveform for this selected algorithm setting group. Model inputs include the scaled and transformed GEDI L2A RH metrics, footprint geolocation variables and land cover input data including PFTs and the world region identifiers. Additional model outputs include the AGBD predictions for each of the six GEDI L2A algorithm setting groups with AGBD in natural and transformed units and associated prediction uncertainty for each GEDI L2A algorithm setting group. Providing these ancillary data products will allow users to evaluate and select alternative algorithm setting groups. Also provided are outputs of parameters and variables from the L4A models used to generate AGBD predictions that are required as input to the GEDI04_B algorithm to generate 1-km gridded products. Note that there are 351 granules in this release affected by duplicate GEDI shots for selected days (2020-297 to 2020-300, 2020-365, and 2021-106).
&lt;br&gt;&lt;h4 id&#x3D;&quot;gedi_l4b_country_biomass_2321&quot;&gt;GEDI_L4B_Country_Biomass_2321&lt;/h4&gt;
This dataset provides country-level estimates of land surface mean aboveground biomass density (AGBD), total aboveground biomass (AGB) stocks, and the associated standard errors of the mean calculated using different versions of the Global Ecosystem Dynamics Investigation (GEDI) Level-4B (L4B) product. The GEDI L4B product provides gridded (1 km x 1 km) estimates of AGBD within the GEDI orbital extent (between 51.6 degrees N and 51.6 degrees S). For comparison purposes, this dataset also includes national-scale National Forest Inventory (NFI) estimates of AGBD from the 2020 Global Forest Resources Assessment (FRA) published by the Food and Agriculture Organization (FAO, 2020) of the United Nations. The GEDI instrument produces high-resolution laser ranging observations of the 3-dimensional structure of the Earth&amp;#39;s surface. GEDI was launched on December 5, 2018, and is attached to the International Space Station (ISS). The GEDI instrument consists of three lasers producing a total of eight beam ground transects, which consist of ~25 m footprint samples spaced approximately every 60 m along-track. The GEDI beam transects are spaced approximately 600 m apart on the Earth&amp;#39;s surface in the cross-track direction, for an across-track width of ~4.2 km. The data are provided in comma-separated value (CSV) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gedi_l4b_gridded_biomass_2017&quot;&gt;GEDI_L4B_Gridded_Biomass_2017&lt;/h4&gt;
This Global Ecosystem Dynamics Investigation (GEDI) L4B product provides 1 km x 1 km (1 km, hereafter) estimates of mean aboveground biomass density (AGBD) based on observations from mission week 19 starting on 2019-04-18 to mission week 138 ending on 2021-08-04. The GEDI L4A Footprint Biomass product converts each high-quality waveform to an AGBD prediction, and the L4B product uses the sample present within the borders of each 1 km cell to statistically infer mean AGBD. The gridding procedure is described in the GEDI L4B Algorithm Theoretical Basis Document (ATBD). Patterson et al. (2019) describes the hybrid model-based mode of inference used in the L4B product. Corresponding 1 km estimates of the standard error of the mean are also provided in the L4B product. Uncertainty is due to both GEDI&amp;#39;s sampling of the 1 km area (as opposed to making wall-to-wall observations) and the fact that L4A biomass values are modeled in a process subject to error instead of measured in a process that may be assumed to be error-free.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gedi_l4b_gridded_biomass_v2_1_2299&quot;&gt;GEDI_L4B_Gridded_Biomass_V2_1_2299&lt;/h4&gt;
This Global Ecosystem Dynamics Investigation (GEDI) L4B product provides 1 km x 1 km (1 km, hereafter) estimates of mean aboveground biomass density (AGBD) based on observations from mission week 19 starting on 2019-04-18 to mission week 223 ending on 2023-03-16. The GEDI L4A Footprint Biomass product converts each high-quality waveform to an AGBD prediction, and the L4B product uses the sample present within the borders of each 1 km cell to statistically infer mean AGBD. The gridding procedure is described in the GEDI L4B Algorithm Theoretical Basis Document (ATBD). Patterson et al. (2019) describes the hybrid model-based mode of inference used in the L4B product. Corresponding 1 km estimates of the standard error of the mean are also provided in the L4B product. Uncertainty is due to both GEDI&amp;#39;s sampling of the 1 km area (as opposed to making wall-to-wall observations) and the fact that L4A biomass values are modeled in a process subject to error instead of measured in a process that may be assumed to be error-free.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gedi_l4c_wsci_2338&quot;&gt;GEDI_L4C_WSCI_2338&lt;/h4&gt;
This dataset contains Global Ecosystem Dynamics Investigation (GEDI) Level 4C (L4C) Version 2 predictions of the Waveform Structural Complexity Index (WSCI) and estimates of prediction intervals for each footprint estimate at 95% confidence. In this version, the granules are in sub-orbits. The algorithm setting group selection used for GEDI04_C is the same as in the GEDI02_A product. The footprints are located within the global latitude band observed by the International Space Station (ISS), nominally 51.6 degrees N and S and reported for the period 2019-04-17 to 2025-03-19. The GEDI instrument consists of three lasers producing a total of eight beam ground transects, which instantaneously sample eight ~25 m footprints spaced approximately every 60 m along-track. The GEDI beam transects are spaced approximately 600 m apart on the Earth&amp;#39;s surface in the cross-track direction, for an across-track width of ~4.2 km. Footprint WSCI was derived from XGBoost regression models relating simulated GEDI Level 2A (L2A) waveform relative height (RH) metrics to a 3D structural complexity metric calculated from matched Airborne laser Scanning (ALS) point clouds. Four global WSCI models were trained on a plant functional type (PFT) basis (i.e., deciduous broadleaf trees, evergreen broadleaf trees, evergreen needleleaf trees, and the combination of grasslands, shrubs, and woodlands). For each of the eight beams, additional data are reported with the WSCI estimates, including the associated uncertainty metrics, quality flags, and other information about the GEDI L2A waveform for this selected algorithm setting group. Additional model outputs include WSCI predictions for each of the six GEDI L2A algorithm setting groups and associated prediction intervals. Providing these ancillary data products will allow users to evaluate and select alternative algorithm setting groups. The data are provided in HDF5 format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gedi_l4c_wsci_gridded_2470&quot;&gt;GEDI_L4C_WSCI_Gridded_2470&lt;/h4&gt;
This dataset consists of gridded average estimates of Waveform Structural Complexity Index (WSCI) at 1-km resolution on a nearly global scale derived from the Global Ecosystem Dynamics Investigation (GEDI) Level 4C (L4C) footprint-level WSCI data covering the observations starting on 2019-04-18 to 2023-03-17. Mean WSCI values were computed from high quality GEDI shots over the land surface, according to the quality flags available in the GEDI L4C dataset. This dataset enables users to assess spatial patterns of forest structural complexity at a coarse scale anywhere within the GEDI domain without the need to acquire and process GEDI footprint data. The data are provided in cloud-optimized GeoTIFF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gedi_l4d_imputed_waveforms_2455&quot;&gt;GEDI_L4D_Imputed_Waveforms_2455&lt;/h4&gt;
This Global Ecosystem Dynamics Investigation (GEDI) L4D product provides a 30-m spatial elaboration of the mission&amp;#39;s sample of footprint-level L2A V002, L2B V002, and L4A Version 2.1 products. A nearest neighbor algorithm was used with Landsat time series data to impute high-quality GEDI shots identified using a combination of metrics. The data were collected between mission week 19 starting on 2019-04-18 to mission week 223 ending on 2023-03-16 to every 30-m pixel. A different nearest neighbor model was developed for every 10 x 10-km tile covering land between 51.6 degrees N and 51.6 degrees S, with &amp;quot;neighbors&amp;quot; (potentially imputed shots) drawn from a support area of at least 30 x 30 km centered on the tile. Nearest neighbor classifiers use a distance function to assign one or more reference observations (high-quality shots in this case) to each modeling unit based on multivariate similarity. Imputation of shots for the L4D product assigned the single nearest neighbor to Landsat time series imagery centering on the year 2023. The most basic 30-m output is the shot number of the imputed pixel (relayed in fragments across five fields), from which any shot-level quantity may be retrieved. Predictions for the following commonly used waveform attributes are also included: RH (relative height) 10, 20, ..., 90, 95, and 98 from the L2A product; canopy cover from L2B; and aboveground biomass density (AGBD) from L4A. Model diagnostics are delivered for each 10-km model in a separate product, which gives the root mean square error (RMSE) for each 30-m output as well as results of a Kolmogorov-Smirnov test comparing the 10-km distribution of GEDI observations and 30-m predictions.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gedi_fia_lidar_models_forests_2417&quot;&gt;GEDI_FIA_LIDAR_Models_Forests_2417&lt;/h4&gt;
This dataset includes interpolated cumulative waveforms, with uncertainties, over national forest inventory (FIA) field plots across the contiguous United States. The predicted waveforms are for the Global Ecosystem Dynamics Investigation (GEDI) instrument, which produces high resolution laser ranging observations of the 3D structure of the Earth. GEDI&amp;#39;s data provides precise measurements of forest canopy height, canopy vertical structure, and surface elevation. This dataset also provides R scripts to extract information from user-selected plots and for training linear regression models between GEDI lidar metrics and target forest attributes. The interpolated waveforms are provided in RData and JSON formats. A table of Forest Inventory and Analysis (FIA) plot information is included in comma separated values format
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA GEOS-3 Project</title>
      <link>https://registry.opendata.aws/nasa-geos-3</link>
      <guid>https://registry.opendata.aws/nasa-geos-3</guid>
      <description>These data consist of Geos-3 altimeter measurements produced by NOAA/NODC/Laboratory for Satellite Altimetry. The dataset contains 5,006,956 altimetric sea surface heights and supporting information such as sea state, wind speed, Schwiderski ocean tide height, and Cartwright solid-tide height. Corrections for altimeter bias, wet and dry troposheric delays, and electromagnetic bias are not included. The corrections in this dataset (tides and even orbit height) are old and not very accurate. This dataset should only be used by those with an expertise in altimetry. Measurements are compressed to a rate of 1 per second using a trim mean filter. Data values are written in binary format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://archive.podaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA GFSAD Project</title>
      <link>https://registry.opendata.aws/nasa-gfsad</link>
      <guid>https://registry.opendata.aws/nasa-gfsad</guid>
      <description>The Landsat-Derived Global Irrigated-Cropland Product Level 1 2020 (LGRIP30_L1_IRRI) Version 2 data provides high-resolution, 30 meter (m) cropland data to assist and address food and water security issues of the twenty-first century. As an extension of the Global Food Security-support Analysis Data (&lt;a href&#x3D;&quot;https://www.usgs.gov/centers/western-geographic-science-center/science/global-food-security-support-analysis-data-30-m&quot;&gt;GFSAD&lt;/a&gt;) project, LGRIP_L1_IRRI V2 maps agricultural lands by dividing them into 32 irrigated cropland types and calculates applicable cropland areas across the globe. LGRIP data are produced using Landsat 8 time-series satellite sensor data for the 2019 through 2021 time period to create a nominal 2020 product. Each LGRIP30 L1 V2 Irrigated 30 m resolution GeoTIFF file contains a layer that identifies areas of irrigated cropland (cropland that had at least one irrigation during the crop growing period) divided into 32 types, non-irrigated land (rainfed cropland and areas not classified as cropland), and water bodies over a 10° by 10° area, as well as an accuracy assessment of the product. A low-resolution browse image is also included. Currently, LGRIP30 V2 products contain data only for the conterminous United States (CONUS). LGRIP30 V2 data covering the rest of the globe will be added at a later date.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lgrip30_l2_irri&quot;&gt;LGRIP30_L2_IRRI&lt;/h4&gt;
The Landsat-Derived Global Irrigated-Cropland Product Level 2 2020 (LGRIP30_L2_IRRI) Version 2 data provides high-resolution, 30 meter (m) cropland data to assist and address food and water security issues of the twenty-first century. As an extension of the Global Food Security-support Analysis Data (&lt;a href&#x3D;&quot;https://www.usgs.gov/centers/western-geographic-science-center/science/global-food-security-support-analysis-data-30-m&quot;&gt;GFSAD&lt;/a&gt;) project, LGRIP_L2_IRRI V2 maps agricultural lands by dividing them into irrigated single crop, double crop, and continuous croplands, and calculates applicable cropland areas across the globe. LGRIP data are produced using Landsat 8 time-series satellite sensor data for the 2019 through 2021 time period to create a nominal 2020 product. Each LGRIP L2 Irrigated 30 m resolution GeoTIFF file contains a layer that identifies areas of irrigated cropland (cropland that had at least one irrigation during the crop growing period) divided into single, double, and continuous crop classifications, non-irrigated land (rainfed cropland and areas not classified as cropland), and water bodies over a 10° by 10° area, as well as an accuracy assessment of the product. A low-resolution browse image is also included. Currently, LGRIP30 V2 products only contain data for the conterminous United States (CONUS). LGRIP30 V2 data covering the rest of the globe will be added at a later date.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lgrip30_l3&quot;&gt;LGRIP30_L3&lt;/h4&gt;
The Landsat-derived Global Rainfed and Irrigated-Cropland Product Level 3 2020 (LGRIP30_L3) Version 2 data provides high-resolution, 30 meter (m) cropland data to assist and address food and water security issues of the twenty-first century. As an extension of the Global Food Security-support Analysis Data (&lt;a href&#x3D;&quot;https://www.usgs.gov/centers/western-geographic-science-center/science/global-food-security-support-analysis-data-30-m&quot;&gt;GFSAD&lt;/a&gt;) project, LGRIP L3 V2 maps agricultural croplands by dividing them into irrigated and rainfed croplands, and calculates irrigated and rainfed areas across the globe. LGRIP data are produced using Landsat 8 time-series satellite sensor data for the 2019 through 2021 time period to create a nominal 2020 product. Each LGRIP30 L3 V2 30 m resolution GeoTIFF file contains a layer that identifies areas of rainfed cropland (cropland areas that are purely dependent on direct precipitation without any artificial watering), irrigated cropland (cropland that had at least one irrigation during the crop growing period), non-cropland, and water bodies over a 10° by 10° area, as well as an accuracy assessment of the product. A low-resolution browse image is also included. Currently, LGRIP30 V2 products only contain data for the conterminous United States (CONUS). LGRIP30 V2 data covering the rest of the globe will be added at a later date.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lgrip30_l1_rain&quot;&gt;LGRIP30_L1_RAIN&lt;/h4&gt;
The Landsat-Derived Global Rainfed-Cropland Product Level 1 2020 (LGRIP30_L1_RAIN) Version 2 data provides high-resolution, 30 meter (m) cropland data to assist and address food and water security issues of the twenty-first century. As an extension of the Global Food Security-support Analysis Data (&lt;a href&#x3D;&quot;https://www.usgs.gov/centers/western-geographic-science-center/science/global-food-security-support-analysis-data-30-m&quot;&gt;GFSAD&lt;/a&gt;) project, LGRIP30_L1_RAIN V2 maps agricultural lands by dividing them into 24 types of rainfed croplands and calculates applicable cropland areas across the globe. LGRIP data are produced using Landsat 8 time-series satellite sensor data for the 2019 through 2021 time period to create a nominal 2020 product. Each LGRIP L1 Rainfed 30 m resolution GeoTIFF file contains a layer that identifies areas of rainfed cropland (cropland areas that are purely dependent on direct precipitation without any artificial watering) divided into 24 types, non-rainfed land (irrigated croplands and areas not classified as cropland), and water bodies over a 10° by 10° area, as well as an accuracy assessment of the product. A low-resolution browse image is also included. Currently, LGRIP30 V2 products only contain data for the conterminous United States (CONUS). LGRIP30 V2 data covering the rest of the globe will be added at a later date.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lgrip30_l2_rain&quot;&gt;LGRIP30_L2_RAIN&lt;/h4&gt;
The Landsat-Derived Global Rainfed-Cropland Product Level 2 2020 (LGRIP30_L2_RAIN) Version 2 data provides high-resolution, 30 meter (m) cropland data to assist and address food and water security issues of the twenty-first century. As an extension of the Global Food Security-support Analysis Data (&lt;a href&#x3D;&quot;https://www.usgs.gov/centers/western-geographic-science-center/science/global-food-security-support-analysis-data-30-m&quot;&gt;GFSAD&lt;/a&gt;) project, LGRIP_L2_RAIN V2 maps agricultural lands by dividing them into rainfed single croplands and rainfed single croplands mixed with natural vegetation, and calculates applicable cropland areas across the globe. LGRIP data are produced using Landsat 8 time-series satellite sensor data for the 2019 through 2021 time period to create a nominal 2020 product. Each LGRIP L2 Rainfed 30 m resolution GeoTIFF file contains a layer that identifies areas of rainfed cropland (cropland areas that are purely dependent on direct precipitation without any artificial watering) divided into single crop and single crop that is mixed with natural vegetation, non-rainfed land (irrigated croplands and areas not classified as cropland), and water bodies over a 10° by 10° area, as well as an accuracy assessment of the product. A low-resolution browse image is also included. Currently, LGRIP30 V2 products only contain data for the conterminous United States (CONUS). LGRIP30 V2 data covering the rest of the globe will be added at a later date.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA GHISA Project</title>
      <link>https://registry.opendata.aws/nasa-ghisa</link>
      <guid>https://registry.opendata.aws/nasa-ghisa</guid>
      <description>The Global Hyperspectral Imaging Spectral-library of Agricultural crops (GHISA) is a comprehensive compilation, collation, harmonization, and standardization of hyperspectral signatures of agricultural crops of the world. This hyperspectral library of agricultural crops is developed for all major world crops and was collected by United States Geological Survey (USGS) and partnering volunteer agencies from around the world. Crops include wheat, rice, barley, corn, soybeans, cotton, sugarcane, potatoes, chickpeas, lentils, and pigeon peas, which together occupy about 65% of all global cropland areas. The GHISA spectral libraries were collected and collated using spaceborne, airborne (e.g., aircrafts and drones), and ground based hyperspectral imaging spectroscopy. The GHISA for Central Asia (GHISACASIA) Version 1 product provides dominant crop data (wheat, rice, corn, alfalfa, and cotton) in different growth stages across the Galaba and Kuva farm fields in the Syr Darya river basin in Central Asia. The GHISA hyperspectral library for the two irrigated areas was developed using Earth Observing-1 (EO-1) Hyperion hyperspectral data acquired in 2007 and ASD (Analytical Spectral Devices, Inc.) Spectroradiometer data acquired in 2006 and 2007. GHISACASIA is extracted from three Hyperion hyperspectral images and several thousands of field ASD Spectroradiometer data. Measurements were taken from 1,232 randomly chosen points scattered across the two farm sites throughout the growing season. All the processing algorithms are coded in Statistical Analysis System (SAS) format and available for download. Provided in the .xlsx files are the spectral library including image information, plot IDs, study area, instrument, Julian or acquisition date, and crop type labels for Central Asia sample fields.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA GHRSST Project</title>
      <link>https://registry.opendata.aws/nasa-ghrsst</link>
      <guid>https://registry.opendata.aws/nasa-ghrsst</guid>
      <description>CNR MED Sea Surface Temperature provides daily gap-free maps (L4) at 0.0625 deg. x 0.0625 deg. horizontal resolution over the Black Sea. The data are obtained from infra-red measurements collected by satellite radiometers and statistical interpolation. It is the CMEMS sea surface temperature nominal operational product for the Black sea.
&lt;br&gt;&lt;h4 id&#x3D;&quot;oisst_uhr_nrt-gos-l4-blk-v20&quot;&gt;OISST_UHR_NRT-GOS-L4-BLK-v2.0&lt;/h4&gt;
CNR MED Sea Surface Temperature provides daily gap-free maps (L4) at 0.01 deg. x 0.01 deg. horizontal resolution over the Black Sea. The data are obtained from infra-red measurements collected by satellite radiometers and statistical interpolation. It is the CMEMS sea surface temperature nominal operational product for the Black sea.
&lt;br&gt;&lt;h4 id&#x3D;&quot;g18-abi-l2p-acspo-v290&quot;&gt;G18-ABI-L2P-ACSPO-v2.90&lt;/h4&gt;
The G18-ABI-L2P-ACSPO-v2.90 dataset produced by the NOAA ACSPO system is used to derive Subskin and Depth Sea Surface Temperature (SST) from the ABI onboard the G18 satellite. NOAA’s G18 (aka, GOES-T pre-launch) was launched on March 1, 2022, replacing the G17 as GOES West in Jan&amp;#39;2023. It is the third satellite in the US GOES–R Series, the Western Hemisphere’s most sophisticated weather-observing and environmental-monitoring system. The ABI is the primary instrument on the GOES-R Series for imaging Earth’s weather, oceans, and environment. &lt;br&gt;&lt;br&gt; G18/ABI maps SST in a Full Disk (FD) area from 163E-77W and 60S-60N, with a spatial resolution of 2km/nadir to 15km/VZA 67-deg, and 10-min temporal sampling. The 10-min FD data are subsequently collated in time, to produce the 1-hr product, with improved coverage and reduced cloud leakages and image noise. The L2P is produced in netCDF4 GDS2 format, with 24 granules per day, and a total data volume 0.8 GB/day. The near-real time (NRT) data are updated hourly, with several hours latency. The NRT files are replaced with Delayed Mode (DM) files, with a latency of ~2-months. File names remain unchanged, and DM vs NRT can be identified by different time stamps and global attributes inside the files (MERRA instead of GFS for atmospheric profiles, and same day CMC L4 analyses in DM instead of one-day delayed in NRT processing). &lt;br&gt;&lt;br&gt; Pixel earth locations are not reported in the granules, as they remain unchanged from granule to granule. Those can be obtained using a flat lat/lon file or a Python script available at Documents tab under How-To section. The ACSPO G18 ABI SSTs are validated against quality controlled in situ data from the NOAA iQuam system (Xu and Ignatov, 2014) and continuously monitored in NOAA SQUAM system (Dash et al, 2010). A 0.02-deg equal-angle gridded L3C product 0.7GB/day) is available at &lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/G18-ABI-L3C-ACSPO-v2.90&quot;&gt;https://podaac.jpl.nasa.gov/dataset/G18-ABI-L3C-ACSPO-v2.90&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;h09-ahi-l2p-acspo-v290&quot;&gt;H09-AHI-L2P-ACSPO-v2.90&lt;/h4&gt;
The H09-AHI-L2P-ACSPO-v2.90 dataset contains the Subskin Sea Surface Temperature (SST) produced by the NOAA ACSPO system from the Advanced Himawari Imager (AHI; largely identical to GOES-R/ABI) onboard the Himawari-9 (H09) satellite. The H09 is a Japanese weather satellite, the 9th of the Himawari geostationary weather satellite operated by the Japan Meteorological Agency. It was launched on November 2, 2016 into its nominal position at 140.7-deg E, and declared operational on December 13, 2022, replacing the Himawari-8. The AHI is the primary instrument on the Himawari Series for imaging Earth’s weather, oceans, and environment with high temporal and spatial resolutions. &lt;br&gt;&lt;br&gt; The H08/AHI maps SST in a Full Disk (FD) area from 80E-160W and 60S-60N, with spatial resolution 2km at nadir to 15km/VZA (view zenith angle) 67-deg, and 10-min temporal sampling. The 10-min FD data are subsequently collated in time, to produce the 1-hr product, with improved coverage and reduced cloud leakages and image noise. The L2P data is produced in GHRSST compliant netCDF4 GDS2 format, with 24 granules per day, and a total data volume 1.2 GB/day. The near-real time (NRT) data are updated hourly, with several hours latency. The NRT files are replaced with Delayed Mode (DM) files, with a latency of approximately 2-months. File names remain unchanged, and DM vs NRT can be identified by different time stamps and global attributes inside the files (MERRA instead of GFS for atmospheric profiles, and same day CMC L4 analyses in DM instead of one-day delayed in NRT processing). &lt;br&gt;&lt;br&gt; Pixel earth locations are not reported in the granules, as they remain unchanged from granule to granule. Pixel locations can be obtained using a flat lat/lon file or a Python script available via Documents tab from the dataset landing page. Climate and Forecast (CF) metadata aware software (e.g., Panoply, xarray) can detect and map the data as is via the granule CF projection attributes and variables. The ACSPO H09 HAI SSTs are validated against quality controlled in situ data from the NOAA iQuam system (Xu and Ignatov, 2014) and continuously monitored in the NOAA SQUAM system (Dash et al, 2010). A 0.02-deg equal-angle gridded L3C product 0.7GB/day) is available at &lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/H09-AHI-L3C-ACSPO-v2.90&quot;&gt;https://podaac.jpl.nasa.gov/dataset/H09-AHI-L3C-ACSPO-v2.90&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;avhrr_sst_metop_a_glb-osisaf-l3c-v10&quot;&gt;AVHRR_SST_METOP_A_GLB-OSISAF-L3C-v1.0&lt;/h4&gt;
A global Group for High Resolution Sea Surface Temperature (GHRSST) Level 3 Collated (L3C) dataset derived from the Advanced Very High Resolution Radiometer (AVHRR) on the European Meteorological Operational-A (MetOp-A) platform (launched 19 Oct 2006). The European Organization for the Exploitation of Meteorological Satellites (EUMETSAT), Ocean and Sea Ice Satellite Application Facility (OSI SAF) is producing SST products in near real time from Metop/AVHRR. Global AVHRR level 1b data are acquired at Meteo-France/Centre de Meteorologie Spatiale (CMS) through the EUMETSAT/EUMETCAST system. SST is retrieved from the AVHRR infrared channels (3.7, 10.8 and 12.0 micrometer) using a multispectral algorithm. Atmospheric profiles of water vapor and temperature from a numerical weather prediction model, together with a radiatiave transfer model, are used to correct the multispectral algorithm for regional and seasonal biases due to changing atmospheric conditions. This global L3C product is derived from full resolution AVHRR l1b data that are re-mapped onto a 0.05 degree grid twice daily. The product format is compliant with the GHRSST Data Specification (GDS) version 2.
&lt;br&gt;&lt;h4 id&#x3D;&quot;avhrr_sst_metop_b_glb-osisaf-l3c-v10&quot;&gt;AVHRR_SST_METOP_B_GLB-OSISAF-L3C-v1.0&lt;/h4&gt;
A global Group for High Resolution Sea Surface Temperature (GHRSST) Level 3 Collated (L3C) dataset derived from the Advanced Very High Resolution Radiometer (AVHRR) on the European Meteorological Operational-B (MetOp-B) platform (launched 17 Sep 2012). The European Organization for the Exploitation of Meteorological Satellites (EUMETSAT), Ocean and Sea Ice Satellite Application Facility (OSI SAF) is producing SST products in near real time from Metop/AVHRR. Global AVHRR level 1b data are acquired at Meteo-France/Centre de Meteorologie Spatiale (CMS) through the EUMETSAT/EUMETCAST system. SST is retrieved from the AVHRR infrared channels (3.7, 10.8 and 12.0 micrometer) using a multispectral algorithm. Atmospheric profiles of water vapor and temperature from a numerical weather prediction model, together with a radiatiave transfer model, are used to correct the multispectral algorithm for regional and seasonal biases due to changing atmospheric conditions. This global L3C product is derived from full resolution AVHRR l1b data that are re-mapped onto a 0.05 degree grid twice daily. The product format is compliant with the GHRSST Data Specification (GDS) version 2.
&lt;br&gt;&lt;h4 id&#x3D;&quot;goes16-sst-osisaf-l3c-v10&quot;&gt;GOES16-SST-OSISAF-L3C-v1.0&lt;/h4&gt;
The data is regional and part of the Group for High Resolution Sea Surface Temperature (GHRSST) Level 3 Collated (L3C) dataset covering the America Region based on retrievals from the Advanced Baseline Imager (ABI) on board the Geostationary Operational Environmental Satellite-16 (GOES-16). The European Organization for the Exploitation of Meteorological Satellites (EUMETSAT), Ocean and Sea Ice Satellite Application Facility (OSI SAF) is producing SST products in near real time from GOES-16 in the Eastern position. GOES-16 Imager level 1 data are acquired at Météo-France/Centre de Météorologie Spatiale (CMS) through the EUMETSAT/EUMETCast system. The GOES-16 ABI enables daytime SST calculations (whereas, previously, GOES East SST was restricted to nighttime conditions). The L3C SST is derived from a three-band (centered at 8.4, 10.3, and 12.3 um) algorithm. The ABI split-window configuration features three bands instead of the two found in heritage sensors (GOES-13). The 8.5-um is used in conjunction with the 10.3-um and 12.3-um bands for improved thin cirrus detection as well as for better atmospheric moisture correction in relatively dry atmospheres. Atmospheric profiles of water vapor and temperature from a numerical weather prediction model, together with a radiative transfer model, are used to correct the multispectral algorithm for regional and seasonal biases due to changing atmospheric conditions. Each 10-minute observation interval is processed at full satellite resolution. The operational products are then produced by remapping over a 0.05-degree regular grid (60S-60N and 135W-15W) SST fields obtained by aggregating the available10-minute SST data into hourly files-hour time, with priority being given to the value closest in time to the product nominal hour. The product format is compliant with the GHRSST Data Specification (GDS) version 2.
&lt;br&gt;&lt;h4 id&#x3D;&quot;seviri_sst_dr-osisaf-l3c-v10&quot;&gt;SEVIRI_SST_DR-OSISAF-L3C-v1.0&lt;/h4&gt;
A Group for High Resolution Sea Surface Temperature (GHRSST) dataset for the Eastern Atlantic Region from the Spinning Enhanced Visible and InfraRed Imager (SEVIRI) on the MSG satellites (Meteosat-8 and Meteosat-9). The European Organization for the Exploitation of Meteorological Satellites (EUMETSAT), Ocean and Sea Ice Satellite Application Facility (OSI SAF) has reprocessed SST products in (long) delayed-mode from MSG/SEVIRI. SST is retrieved from the SEVIRI infrared channels (10.8 and 12.0 micrometer) using a multispectral algorithm and the cloud mask (CM) from OSI SAF. Atmospheric profiles of water vapor and temperature from a numerical weather prediction (NWP) model, OSTIA Sea Surface Temperature re-analysis and analysis, together with a radiative transfer model (RTTOV), are used to correct the multispectral algorithm for regional and seasonal biases due to changing atmospheric conditions. Every 15-minute slot is processed at full satellite resolution. The products are then produced by remapping over a 0.05-degree regular grid (60S-60N and 60W-60E) SST fields obtained by aggregating all available 15-minute SST data into hourly files with priority being given to the value closest in time to the product nominal hour. The product format is compliant with the GHRSST Data Specification (GDS) version 2.
&lt;br&gt;&lt;h4 id&#x3D;&quot;g18-abi-l3c-acspo-v290&quot;&gt;G18-ABI-L3C-ACSPO-v2.90&lt;/h4&gt;
The G18-ABI-L3C-ACSPO-v2.90 dataset produced by the NOAA ACSPO system is used to derive Subskin and Depth Sea Surface Temperature (SST) from the ABI sensor onboard the G18 satellite. NOAA’s G18 (aka GOES-T before launch) was launched on March 1, 2022, replacing G17 as GOES West in Jan&amp;#39;2023. It is the third satellite in the US GOES–R Series, the Western Hemisphere’s most sophisticated weather-observing and environmental-monitoring system. The ABI is the primary instrument on the GOES-R Series for imaging Earth’s weather, oceans, and environment. &lt;br&gt;&lt;br&gt; The G18-ABI-L3C-ACSPO-v2.90 dataset is a gridded version of the G18-ABI-L2P-ACSPO-v2.90 dataset (&lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/G18-ABI-L2P-ACSPO-v2.90&quot;&gt;https://podaac.jpl.nasa.gov/dataset/G18-ABI-L2P-ACSPO-v2.90&lt;/a&gt;). The L3C (Level 3 Collated) outputs 24 hourly granules per day, with a daily volume of 0.7 GB/day. Valid SSTs are found over oceans, sea, lakes or rivers, with fill values reported elsewhere. All valid SSTs in L3C are recommended for users, although data over internal waters may not have enough in situ data to be adequately validated. Per GDS2 specifications, two additional Sensor-Specific Error Statistics layers (bias and standard deviation) are reported in each pixel with valid SST. &lt;br&gt;&lt;br&gt; The ACSPO G18/ABI L3C product is validated against iQuam in situ data (Xu and Ignatov, 2014) and continuously monitored in the NOAA SQUAM system (Dash et al, 2010). The NRT files are replaced with Delayed Mode (DM) files, with a latency of ~2-months. File names remain unchanged, and DM vs NRT can be identified by different time stamps and global attributes inside the files (MERRA instead of GFS for atmospheric profiles, and same day CMC L4 analyses in DM instead of one-day delayed in NRT processing).
&lt;br&gt;&lt;h4 id&#x3D;&quot;h09-ahi-l3c-acspo-v290&quot;&gt;H09-AHI-L3C-ACSPO-v2.90&lt;/h4&gt;
The H09-AHI-L3C-ACSPO-v2.90 dataset contains the Subskin Sea Surface Temperature (SST) produced by the NOAA ACSPO system from the Advanced Himawari Imager (AHI; largely identical to GOES-R/ABI) onboard the Himawari-9 (H09) satellite. The H09 is a Japanese weather satellite, the 9th of the Himawari geostationary weather satellite operated by the Japan Meteorological Agency. It was launched on November 2, 2016 into its nominal position at 140.7-deg E, and declared operational on December 13, 2022, replacing the Himawari-8. The AHI is the primary instrument on the Himawari Series for imaging Earth’s weather, oceans, and environment with high temporal and spatial resolutions. &lt;br&gt;&lt;br&gt; The H09-AHI-L3C-ACSPO-v2.90 dataset is a gridded version of the ACSPO H09-AHI-L2P-ACSPO-v2.90 dataset (&lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/AHI_H09-STAR-L2P-v2.90&quot;&gt;https://podaac.jpl.nasa.gov/dataset/AHI_H09-STAR-L2P-v2.90&lt;/a&gt;). The L3C (Level 3 Collated) data is mapped on 0.02-deg lat-lon grid and outputs 24 hourly granules per day, with a daily volume of 0.7 GB/day. Valid SSTs are found over oceans, sea, lakes or rivers, with fill values reported elsewhere. All valid SSTs in L3C are recommended for users, although data over internal waters may not have enough in situ data to be adequately validated. Per GDS2 specifications, two additional Sensor-Specific Error Statistics layers (bias and standard deviation) are reported in each pixel with valid SST. &lt;br&gt;&lt;br&gt; The ACSPO H09/AHI L3C product is validated against iQuam in situ data (Xu and Ignatov, 2014) and continuously monitored in the NOAA SQUAM system (Dash et al, 2010). The NRT files are replaced with Delayed Mode (DM) files, with a latency of approximately 2-months. File names remain unchanged, and DM vs NRT can be identified by different time stamps and global attributes inside the files (MERRA for DM instead of GFS for atmospheric profiles, and same day CMC L4 analyses in DM instead of one-day delayed in NRT processing).
&lt;br&gt;&lt;h4 id&#x3D;&quot;viirs_npp-navo-l2p-v10&quot;&gt;VIIRS_NPP-NAVO-L2P-v1.0&lt;/h4&gt;
A global Group for High Resolution Sea Surface Temperature (GHRSST) Level 2P dataset based on retrievals from the Visible Infrared Imaging Radiometer Suite (VIIRS). This sensor resides on the Suomi National Polar-orbiting Operational Environmental Satellite System (NPOESS) Preparatory Project (NPP) satellite launched on 28 October 2011. The VIIRS instrument is a a 22-band, multi-spectral scanning radiometer with a 3040-km swath width that builds on the heritage of the MODIS , AVHRR and SeaWIFS sensors for sea surface temperature (SST) and ocean color. For the infrared bands for SST the effective pixel size is 740 meters at nadir and the pixel size variation across the swath is constrained to no more than 1600 meters at the edge of the swath. However, the processing of this dataset aggregates two pixels into one so the resolution is 1500 meters at nadir. This dataset adheres to the GHRSST Data Processing Specification (GDS) version 2 format specifications.
&lt;br&gt;&lt;h4 id&#x3D;&quot;viirs_npp-navo-l2p-v30&quot;&gt;VIIRS_NPP-NAVO-L2P-v3.0&lt;/h4&gt;
A global Group for High Resolution Sea Surface Temperature (GHRSST) Level 2P dataset based on retrievals from the Visible Infrared Imaging Radiometer Suite (VIIRS). This sensor resides on the Suomi National Polar-orbiting Partnership (Suomi_NPP) satellite launched on 28 October 2011. VIIRS is a whiskbroom scanning radiometer which takes measurements in the cross-track direction within a field of regard of 112.56 degrees using 16 detectors and a double-sided mirror assembly. At a nominal altitude of 829 km, the swath width is 3060 km, providing full daily coverage both on the day and night side of the Earth. The VIIRS instrument is a 22-band, multi-spectral scanning radiometer that builds on the heritage of the MODIS , AVHRR and SeaWIFS sensors for sea surface temperature (SST) and ocean color. For the infrared bands for SST the effective pixel size is 750 meters at nadir and the pixel size variation across the swath is constrained to no more than 1600 meters at the edge of the swath. This L2P SST v3.0 is upgraded from the v2.0 with several significant improvements in processing algorithms, including contamination detection, cloud detection, and data format upgrades. It contains the global near daily-coverage Sea Surface Temperature at 1-meter depth with 750 m (along) x 750 m (cross) spatial resolution in swath coordinates. Each netCDF file has 768 x 3200 pixels in size, in compliance with the GHRSST Data Processing Specification (GDS) version 2 format specifications.
&lt;br&gt;&lt;h4 id&#x3D;&quot;msg03-ospo-l2p-v10&quot;&gt;MSG03-OSPO-L2P-v1.0&lt;/h4&gt;
The Meteosat Second Generation (MSG-3) satellites are spin stabilized geostationary satellites operated by the European Organization for the Exploitation of Meteorological Satellites (EUMETSAT) to provide accurate weather monitoring data through its primary instrument the Spinning Enhanced Visible and InfraRed Imager (SEVIRI), which has the capacity to observe the Earth in 12 spectral channels. Eight of these channels are in the thermal infrared, providing among other information, observations of the temperatures of clouds, land and sea surfaces at approximately 5 km resolution with a 15 minute duty cycle. This Group for High Resolution Sea Surface Temperature (GHRSST) dataset produced by the US National Oceanic and Atmospheric Administration (NOAA) National Environmental Satellite, Data, and Information Service (NESDIS) is derived from the SEVIRI instrument on the second MSG satellite (also known as Meteosat-9) that was launched on 22 December 2005. Skin sea surface temperature (SST) data are calculated from the infrared channels of SEVIRI at full resolution every 15 minutes. L2P data products with Single Sensor Error Statistics (SSES) are then derived following the GHRSST-PP Data Processing Specification (GDS) version 2.0.
&lt;br&gt;&lt;h4 id&#x3D;&quot;goes15-ospo-l2p-v10&quot;&gt;GOES15-OSPO-L2P-v1.0&lt;/h4&gt;
The Geostationary Operational Environmental Satellites (GOES) operated by the United States National Oceanic and Atmospheric Administration (NOAA) support weather forecasting, severe storm tracking, meteorology and oceanography research. Generally there are several GOES satellites in geosynchronous orbit at any one time viewing different earth locations including the GOES-15 launched 4 March 2010. The radiometer aboard the satellite, The GOES N-P Imager, is a five channel (one visible, four infrared) imaging radiometer designed to sense radiant and solar reflected energy from sampled areas of the earth. The multi-element spectral channels simultaneously sweep east-west and west-east along a north-to-south path by means of a two-axis mirror scan system retuning telemetry in 10-bit precision. For this Group for High Resolution Sea Surface Temperature (GHRSST) dataset, skin sea surface temperature (SST) measurements are calculated from the far IR channels of GOES-15 at full resolution on a half hourly basis. In native satellite projection, vertically adjacent pixels are averaged and read out at every pixel. L2P datasets including Single Sensor Error Statistics (SSES) are then derived following the GHRSST Data Processing Specification (GDS) version 2.0. The full disk image is subsetted into granules representing distinct northern and southern regions.
&lt;br&gt;&lt;h4 id&#x3D;&quot;avhrrmta_g-navo-l2p-v10&quot;&gt;AVHRRMTA_G-NAVO-L2P-v1.0&lt;/h4&gt;
A global Group for High Resolution Sea Surface Temperature (GHRSST) Level 2P dataset based on multi-channel sea surface temperature (SST) retrievals generated in real-time from the Advanced Very High Resolution Radiometer (AVHRR) on the European Meteorological Operational-A (MetOp-A; launched 19 Oct 2006) ) satellite produced and used operationally in oceanographic analyses and forecasts by the US Naval Oceanographic Office (NAVO). The MetOp satellite program is a European undertaking providing weather data services for monitoring climate and improving weather forecasts. It was jointly established by the European Space Agency (ESA) and the European Organisation for the Exploitation of Meteorological Satellites (EUMETSAT) with a contribution by the US National Oceanic and Atmospheric Administration (NOAA) of an AVHRR sensor identical to those flying on the family of Polar Orbiting Environmental Satellites (POES). AVHRR instruments measure the radiance of the Earth in 5 (or 6) relatively wide spectral bands. The first two are centered around the red (0.6 micrometer) and near-infrared (0.9 micrometer) regions, the third one is located around 3.5 micrometer, and the last two sample the emitted thermal radiation, around 11 and 12 micrometers, respectively. The legacy 5 band instrument is known as AVHRR/2 while the more recent version, the AVHRR/3 (first carried on the NOAA-15 platform), acquires data in a 6th channel located at 1.6 micrometer. Typically the 11 and 12 micron channels are used to derive SST sometimes in combination with the 3.5 micron channel. The MetOp-A platform is sun synchronous generally viewing the same earth location twice a day (latitude dependent) due to the relatively large AVHRR swath of approximately 2400 km. The highest ground resolution that can be obtained from the current AVHRR instruments is 1.1 km at nadir. This particular dataset is produced from Global Area Coverage (GAC) data that are derived from an on-board sample averaging of the full resolution global AVHRR data. Four out of every five samples along the scan line are used to compute on average value and the data from only every third scan line are processed, yielding an effective 4 km resolution at nadir. Further binning and averaging of these pixels results in a final dataset resolution of 8.8 km.
&lt;br&gt;&lt;h4 id&#x3D;&quot;avhrrmtb_g-navo-l2p-v10&quot;&gt;AVHRRMTB_G-NAVO-L2P-v1.0&lt;/h4&gt;
A global Group for High Resolution Sea Surface Temperature (GHRSST) Level 2P dataset based on multi-channel sea surface temperature (SST) retrievals generated in real-time from the Advanced Very High Resolution Radiometer (AVHRR) on the European Meteorological Operational-B (MetOp-B; launched 19 Oct 2006) ) satellite produced and used operationally in oceanographic analyses and forecasts by the US Naval Oceanographic Office (NAVO). The MetOp satellite program is a European undertaking providing weather data services for monitoring climate and improving weather forecasts. It was jointly established by the European Space Agency (ESA) and the European Organisation for the Exploitation of Meteorological Satellites (EUMETSAT) with a contribution by the US National Oceanic and Atmospheric Administration (NOAA) of an AVHRR sensor identical to those flying on the family of Polar Orbiting Environmental Satellites (POES). AVHRR instruments measure the radiance of the Earth in 5 (or 6) relatively wide spectral bands. The first two are centered around the red (0.6 micrometer) and near-infrared (0.9 micrometer) regions, the third one is located around 3.5 micrometer, and the last two sample the emitted thermal radiation, around 11 and 12 micrometers, respectively. The legacy 5 band instrument is known as AVHRR/2 while the more recent version, the AVHRR/3 (first carried on the NOAA-15 platform), acquires data in a 6th channel located at 1.6 micrometer. Typically the 11 and 12 micron channels are used to derive SST sometimes in combination with the 3.5 micron channel. The MetOp-A platform is sun synchronous generally viewing the same earth location twice a day (latitude dependent) due to the relatively large AVHRR swath of approximately 2400 km. The highest ground resolution that can be obtained from the current AVHRR instruments is 1.1 km at nadir. This particular dataset is produced from Global Area Coverage (GAC) data that are derived from an on-board sample averaging of the full resolution global AVHRR data. Four out of every five samples along the scan line are used to compute on average value and the data from only every third scan line are processed, yielding an effective 4 km resolution at nadir. Further binning and averaging of these pixels results in a final dataset resolution of 8.8 km.
&lt;br&gt;&lt;h4 id&#x3D;&quot;avhrr18_g-navo-l2p-v10&quot;&gt;AVHRR18_G-NAVO-L2P-v1.0&lt;/h4&gt;
A global Group for High Resolution Sea Surface Temperature (GHRSST) Level 2P dataset based on multi-channel sea surface temperature (SST) retrievals generated in real-time from the Advanced Very High Resolution Radiometer (AVHRR) on the NOAA-18 platform (launched 20 May 2005) produced and used operationally in oceanographic analyses and forecasts by the US Naval Oceanographic Office (NAVO). The AVHRR is a space-borne scanning sensor on the National Oceanic and Atmospheric Administration (NOAA) family of Polar Orbiting Environmental Satellites (POES) having a operational legacy that traces back to the Television Infrared Observation Satellite-N (TIROS-N) launched in 1978. AVHRR instruments measure the radiance of the Earth in 5 (or 6) relatively wide spectral bands. The first two are centered around the red (0.6 micrometer) and near-infrared (0.9 micrometer) regions, the third one is located around 3.5 micrometer, and the last two sample the emitted thermal radiation, around 11 and 12 micrometers, respectively. The legacy 5 band instrument is known as AVHRR/2 while the more recent version, the AVHRR/3 (first carried on the NOAA-15 platform), acquires data in a 6th channel located at 1.6 micrometer. Typically the 11 and 12 micron channels are used to derive SST sometimes in combination with the 3.5 micron channel. The NOAA platforms are sun synchronous generally viewing the same earth location twice a day (latitude dependent) due to the relatively large AVHRR swath of approximately 2400 km. The highest ground resolution that can be obtained from the current AVHRR instruments is 1.1 km at nadir. AVHRR data are acquired in three formats: High Resolution Picture Transmission (HRPT), Local Area Coverage (LAC), and Global Area Coverage (GAC). HRPT data are full resolution image data transmitted to a ground stations as they are collected. LAC are also full resolution data, but the acquisition is prescheduled and recorded with an on-board tape recorder for subsequent transmission during a station overpass. This particular dataset is produced from GAC data that are derived from an on-board sample averaging of the full resolution global AVHRR data. Four out of every five samples along the scan line are used to compute on average value and the data from only every third scan line are processed, yielding an effective 4 km resolution at nadir. Further binning and averaging of these pixels results in a final dataset resolution of 8.8 km.
&lt;br&gt;&lt;h4 id&#x3D;&quot;avhrr19_g-navo-l2p-v10&quot;&gt;AVHRR19_G-NAVO-L2P-v1.0&lt;/h4&gt;
A global Group for High Resolution Sea Surface Temperature (GHRSST) Level 2P dataset based on multi-channel sea surface temperature (SST) retrievals generated in real-time from the Advanced Very High Resolution Radiometer (AVHRR) on the NOAA-19 platform (launched 6 Feb 2009) produced and used operationally in oceanographic analyses and forecasts by the US Naval Oceanographic Office (NAVO). The AVHRR is a space-borne scanning sensor on the National Oceanic and Atmospheric Administration (NOAA) family of Polar Orbiting Environmental Satellites (POES) having a operational legacy that traces back to the Television Infrared Observation Satellite-N (TIROS-N) launched in 1978. AVHRR instruments measure the radiance of the Earth in 5 (or 6) relatively wide spectral bands. The first two are centered around the red (0.6 micrometer) and near-infrared (0.9 micrometer) regions, the third one is located around 3.5 micrometer, and the last two sample the emitted thermal radiation, around 11 and 12 micrometers, respectively. The legacy 5 band instrument is known as AVHRR/2 while the more recent version, the AVHRR/3 (first carried on the NOAA-15 platform), acquires data in a 6th channel located at 1.6 micrometer. Typically the 11 and 12 micron channels are used to derive SST sometimes in combination with the 3.5 micron channel. The NOAA platforms are sun synchronous generally viewing the same earth location twice a day (latitude dependent) due to the relatively large AVHRR swath of approximately 2400 km. The highest ground resolution that can be obtained from the current AVHRR instruments is 1.1 km at nadir. AVHRR data are acquired in three formats: High Resolution Picture Transmission (HRPT), Local Area Coverage (LAC), and Global Area Coverage (GAC). HRPT data are full resolution image data transmitted to a ground stations as they are collected. LAC are also full resolution data, but the acquisition is prescheduled and recorded with an on-board tape recorder for subsequent transmission during a station overpass. This particular dataset is produced from GAC data that are derived from an on-board sample averaging of the full resolution global AVHRR data. Four out of every five samples along the scan line are used to compute on average value and the data from only every third scan line are processed, yielding an effective 4 km resolution at nadir. Further binning and averaging of these pixels results in a final dataset resolution of 8.8 km.
&lt;br&gt;&lt;h4 id&#x3D;&quot;amsr2-remss-l2p_rt-v82&quot;&gt;AMSR2-REMSS-L2P_RT-v8.2&lt;/h4&gt;
This product provides a near-real-time (NRT) Level-2 Sea Surface Temperature (SST) (identified by &amp;quot;&lt;em&gt;rt&lt;/em&gt;&amp;quot; within the file name) for the Group for High Resolution Sea Surface Temperature (GHRSST) Project, which is derived from the Advanced Microwave Scanning Radiometer 2 (AMSR2) by Remote Sensing Systems (RSS, or REMSS). AMSR2 was launched on 18 May 2012, onboard the Global Change Observation Mission - Water (GCOM-W) satellite developed by the Japan Aerospace Exploration Agency (JAXA). The GCOM-W mission aims to establish the global and long-term observation system to collect data, which is needed to understand mechanisms of climate and water cycle variations, and demonstrate its utilization. AMSR2 onboard the first generation of the GCOM-W satellite will continue Aqua/AMSR-E observations of water vapor, cloud liquid water, precipitation, SST, sea surface wind speed, sea ice concentration, snow depth, and soil moisture. AMSR2 is a remote sensing instrument for measuring weak microwave emission from the surface and the atmosphere of the Earth. The antenna of AMSR2 rotates once per 1.5 seconds and obtains data over a 1450 km swath. This conical scan mechanism enables AMSR2 to acquire a set of daytime and nighttime data with more than 99% coverage of the Earth every 2 days. The NRT SST is made as available as soon as possible, generally within 3 hours latency. The v8.2 supersedes the previous v8a dataset which can be found at &lt;a href&#x3D;&quot;https://www.doi.org/10.5067/GHAM2-2TR8A&quot;&gt;https://www.doi.org/10.5067/GHAM2-2TR8A&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;viirs_npp-jpl-l2p-v20162&quot;&gt;VIIRS_NPP-JPL-L2P-v2016.2&lt;/h4&gt;
These files contain NASA produced skin sea surface temperature (SST) products from the Infrared (IR) channels of the Visible and Infrared Imager/Radiometer Suite (VIIRS) onboard the Suomi-NPP satellite. VIIRS is a multi-disciplinary instrument that is also being flown on the Joint Polar Satellite System (JPSS) series of spacecraft, of which NOAA-20 is the first. JPSS is a multi-agency program that consolidates the polar orbiting spacecraft of NASA and the National Oceanic and Atmospheric Administration (NOAA). Suomi-NPP is the initial spacecraft in this series, and VIIRS is the successor to MODIS for Earth science data. VIIRS has 22 spectral bands ranging from 412 nm to 12 micron . There are 16 moderate-resolution bands (750m at nadir), 5 image-resolution bands (375 m), and one day-night band (DNB). VIIRS uses on-board pixel aggregation to reduce the growth in size of pixels away from nadir. Two SST products are contained in these files. The first is a skin SST produced separately for day and night observations, derived from the long wave IR 11 and 12 micron wavelength channels, using a modified nonlinear SST algorithm intended to provide continuity of SST products from heritage and current NASA sensors. At night, a second triple channel SST product is generated using the 3.7 , 11 and 12 micron IR channels, identified as SST_triple. Due to the sun glint in the 3.7 micron SST_triple can only be used at night. VIIRS L2P SST data have a 750 spatial resolution at nadir and are stored in ~288 five minute granules per day. Full global coverage is obtained each day. The production of VIIRS NASA L2P SST files is part of the Group for High Resolution Sea Surface Temperature (GHRSST) project and is a joint collaboration between the NASA Jet Propulsion Laboratory (JPL), the NASA Ocean Biology Processing Group (OBPG), and the Rosenstiel School of Marine and Atmospheric Science (RSMAS). Researchers at RSMAS were responsible for sea surface temperature algorithm development, error statistics and quality flagging, while the OBPG, as the NASA ground data system, is responsible for the production of VIIRS ocean products. JPL acquires VIIRS ocean granules from the OBPG and reformats them to the GHRSST L2P netCDF specification with complete metadata and is the official Physical Oceanography Data Archive (PO.DAAC) for SST. In mid-August, 2018, the RSMAS involvement in the VIIRS SST project ceased, and the subsequent fields are not maintained.The R2016.2 supersedes the previous v2016.0 datasets which can be found at &lt;a href&#x3D;&quot;https://doi.org/10.5067/GHVRS-2PN16&quot;&gt;https://doi.org/10.5067/GHVRS-2PN16&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;modis_a-jpl-l2p-v20190&quot;&gt;MODIS_A-JPL-L2P-v2019.0&lt;/h4&gt;
NASA produces skin sea surface temperature (SST) products from the Infrared (IR) channels of the Moderate-resolution Imaging Spectroradiometer (MODIS) onboard the Aqua satellite. Aqua was launched by NASA on May 4, 2002, into a sun synchronous, polar orbit with a daylight ascending node at 1:30 pm, formation flying in the A-train with other Earth Observation Satellites (EOS), to study the global dynamics of the Earth atmosphere, land and oceans. MODIS captures data in 36 spectral bands at a variety of spatial resolutions. Two SST products can be present in these files. The first is a skin SST produced for both day and night (NSST) observations, derived from the long wave IR 11 and 12 micron wavelength channels, using a modified nonlinear SST algorithm intended to provide continuity of SST derived from heritage and current NASA sensors. At night, a second SST product is generated using the mid-infrared 3.95 and 4.05 micron wavelength channels which are unique to MODIS; the SST derived from these measurements is identified as SST4. The SST4 product has lower uncertainty, but due to sun glint can only be used at night. MODIS L2P SST data have a 1 km spatial resolution at nadir and are stored in 288 five minute granules per day. Full global coverage is obtained every two days, with coverage poleward of 32.3 degree being complete each day. The production of MODIS L2P SST files is part of the Group for High Resolution Sea Surface Temperature (GHRSST) project and is a joint collaboration between the NASA Jet Propulsion Laboratory (JPL), the NASA Ocean Biology Processing Group (OBPG), and the Rosenstiel School of Marine and Atmospheric Science (RSMAS). Researchers at RSMAS are responsible for SST algorithm development, error statistics and quality flagging, while the OBPG, as the NASA ground data system, is responsible for the production of daily MODIS ocean products. JPL acquires MODIS ocean granules from the OBPG and reformats them to the GHRSST L2P netCDF specification with complete metadata and ancillary variables, and distributes the data as the official Physical Oceanography Data Archive (PO.DAAC) for SST. The R2019.0 supersedes the previous R2014.0 datasets which can be found at &lt;a href&#x3D;&quot;https://doi.org/10.5067/GHMDA-2PJ02&quot;&gt;https://doi.org/10.5067/GHMDA-2PJ02&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;modis_t-jpl-l2p-v20190&quot;&gt;MODIS_T-JPL-L2P-v2019.0&lt;/h4&gt;
NASA produces skin sea surface temperature (SST) products from the Infrared (IR) channels of the Moderate-resolution Imaging Spectroradiometer (MODIS) onboard the Terra satellite. Terra was launched by NASA on December 18, 1999, into a sun synchronous, polar orbit with a daylight descending node at 10:30 am, to study the global dynamics of the Earth atmosphere, land and oceans. The MODIS captures data in 36 spectral bands at a variety of spatial resolutions. Two SST products can be present in these files. The first is a skin SST produced for both day and night observations, derived from the long wave IR 11 and 12 micron wavelength channels, using a modified nonlinear SST algorithm intended to provide continuity with SST derived from heritage and current NASA sensors. At night, a second SST product is produced using the mid-infrared 3.95 and 4.05 micron channels which are unique to MODIS; the SST derived from these measurements is identified as SST4. The SST4 product has lower uncertainty, but due to sun glint can only be produced at night. MODIS L2P SST data have a 1 km spatial resolution at nadir and are stored in 288 five minute granules per day. Full global coverage is obtained every two days, with coverage poleward of 32.3 degree being complete each day. The production of MODIS L2P SST files is part of the Group for High Resolution Sea Surface Temperature (GHRSST) project, and is a joint collaboration between the NASA Jet Propulsion Laboratory (JPL), the NASA Ocean Biology Processing Group (OBPG), and the Rosenstiel School of Marine and Atmospheric Science (RSMAS). Researchers at RSMAS are responsible for SST algorithm development, error statistics and quality flagging, while the OBPG, as the NASA ground data system, is responsible for the production of daily MODIS ocean products. JPL acquires MODIS ocean granules from the OBPG and reformats them to the GHRSST L2P netCDF specification with complete metadata and ancillary variables, and distributes the data as the official Physical Oceanography Data Archive (PO.DAAC) for SST. The R2019.0 supersedes the previous R2014.0 datasets which can be found at &lt;a href&#x3D;&quot;https://doi.org/10.5067/GHMDT-2PJ02&quot;&gt;https://doi.org/10.5067/GHMDT-2PJ02&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;avhrrmta_g-navo-l2p-v20&quot;&gt;AVHRRMTA_G-NAVO-L2P-v2.0&lt;/h4&gt;
A global Group for High Resolution Sea Surface Temperature (GHRSST) Level 2P data set containing multi-channel Sea Surface Temperature (SST) retrievals derived in real-time from the Advanced Very High Resolution Radiometer (AVHRR) level-1B data from the Meteorological Operational-A (MetOp-A) satellite. The SST data in this data set are used operationally in oceanographic analyses and forecasts by the US Naval Oceanographic Office (NAVO). The MetOp satellite program is a European multi-satellite program to provide weather data services for monitoring climate and improving weather forecasts. MetOp-A, MetOp-B and Metop-C were respectively launched on 19 Oct 2006, 17 September 2012 and 7 November 2018. The program was jointly established by the European Space Agency (ESA) and the European Organization for the Exploitation of Meteorological Satellites (EUMETSAT) with the US National Oceanic and Atmospheric Administration (NOAA) contributing the AVHRR sensor. AVHRR instruments measure the radiance of the Earth in 5 (or 6) relatively wide spectral bands. The first two are centered around the red (0.6 micron) and near-infrared (0.9 micron) regions, the third one is located around 4 (3.6) micron, and the last two sample the emitted thermal radiation, around 11 and 12 micron, respectively. The legacy 5 band instrument is known as AVHRR/2 while the more recent version, the AVHRR/3 (first carried on the NOAA-15 platform), acquires data in a 6th channel located at 1.6 micron. Typically, the 11 and 12 micron channels are used to derive SST sometimes in combination with the 3.5 micron channel. The swath of the AVHRR sensor is a relatively large 2400 km. All MetOp platforms are sun synchronous and generally view the same earth location twice a day (latitude dependent). The ground native resolution of the AVHRR instruments is approximately 1.1 km at nadir and degrades off nadir. This particular data set is produced from legacy Global Area Coverage (GAC) data that are derived from a sample averaging of the full resolution global AVHRR data. Four out of every five samples along the scan line are used to compute on average value and the data from only every third scan line are processed, yielding an effective 4 km spatial resolution at nadir. The v2.0 is the updated version from current v1.0 with extensive algorithm improvements and upgrades. The major improvements include: 1) Significant changes in contaminant/cloud detection; 2) Increased the spatial resolution from 9 km to 4 km; 3) Updated compliance with GDS2, ACDD 1.3, and CF 1.6; and 4) Removed the dependency on the High-resolution Infrared Radiation Sounder (HIRS) sensor (only available to MetOp-A/B), thus allowing for the consistent inter-calibration and the processing of MetOp-A/B/C data
&lt;br&gt;&lt;h4 id&#x3D;&quot;avhrrmtb_g-navo-l2p-v20&quot;&gt;AVHRRMTB_G-NAVO-L2P-v2.0&lt;/h4&gt;
A global Group for High Resolution Sea Surface Temperature (GHRSST) Level 2P data set containing multi-channel Sea Surface Temperature (SST) retrievals derived in real-time from the Advanced Very High Resolution Radiometer (AVHRR) level-1B data from the Meteorological Operational-B (MetOp-B) satellite. The SST data in this data set are used operationally in oceanographic analyses and forecasts by the US Naval Oceanographic Office (NAVO). The MetOp satellite program is a European multi-satellite program to provide weather data services for monitoring climate and improving weather forecasts. MetOp-A, MetOp-B and Metop-C were respectively launched on 19 Oct 2006, 17 September 2012 and 7 November 2018. The program was jointly established by the European Space Agency (ESA) and the European Organization for the Exploitation of Meteorological Satellites (EUMETSAT) with the US National Oceanic and Atmospheric Administration (NOAA) contributing the AVHRR sensor. AVHRR instruments measure the radiance of the Earth in 5 (or 6) relatively wide spectral bands. The first two are centered around the red (0.6 micron) and near-infrared (0.9 micron) regions, the third one is located around 4 (3.6) micron, and the last two sample the emitted thermal radiation, around 11 and 12 micron, respectively. The legacy 5 band instrument is known as AVHRR/2 while the more recent version, the AVHRR/3 (first carried on the NOAA-15 platform), acquires data in a 6th channel located at 1.6 micron. Typically, the 11 and 12 micron channels are used to derive SST sometimes in combination with the 3.5 micron channel. The swath of the AVHRR sensor is a relatively large 2400 km. All MetOp platforms are sun synchronous and generally view the same earth location twice a day (latitude dependent). The ground native resolution of the AVHRR instruments is approximately 1.1 km at nadir and degrades off nadir. This particular data set is produced from legacy Global Area Coverage (GAC) data that are derived from a sample averaging of the full resolution global AVHRR data. Four out of every five samples along the scan line are used to compute on average value and the data from only every third scan line are processed, yielding an effective 4 km spatial resolution at nadir. The v2.0 is the updated version from current v1.0 with extensive algorithm improvements and upgrades. The major improvements include: 1) Significant changes in contaminant/cloud detection; 2) Increased the spatial resolution from 9 km to 4 km; 3) Updated compliance with GDS2, ACDD 1.3, and CF 1.6; and 4) Removed the dependency on the High-resolution Infrared Radiation Sounder (HIRS) sensor (only available to MetOp-A/B), thus allowing for the consistent inter-calibration and the processing of MetOp-A/B/C data
&lt;br&gt;&lt;h4 id&#x3D;&quot;avhrrmtc_g-navo-l2p-v20&quot;&gt;AVHRRMTC_G-NAVO-L2P-v2.0&lt;/h4&gt;
A global Group for High Resolution Sea Surface Temperature (GHRSST) Level 2P data set containing multi-channel Sea Surface Temperature (SST) retrievals derived in real-time from the Advanced Very High Resolution Radiometer (AVHRR) level-1B data from the Meteorological Operational-C (MetOp-C) satellite. The SST data in this data set are used operationally in oceanographic analyses and forecasts by the US Naval Oceanographic Office (NAVO). The MetOp satellite program is a European multi-satellite program to provide weather data services for monitoring climate and improving weather forecasts. MetOp-A, MetOp-B and Metop-C were respectively launched on 19 Oct 2006, 17 September 2012 and 7 November 2018. The program was jointly established by the European Space Agency (ESA) and the European Organization for the Exploitation of Meteorological Satellites (EUMETSAT) with the US National Oceanic and Atmospheric Administration (NOAA) contributing the AVHRR sensor. AVHRR instruments measure the radiance of the Earth in 5 (or 6) relatively wide spectral bands. The first two are centered around the red (0.6 micron) and near-infrared (0.9 micron) regions, the third one is located around 4 (3.6) micron, and the last two sample the emitted thermal radiation, around 11 and 12 micron, respectively. The legacy 5 band instrument is known as AVHRR/2 while the more recent version, the AVHRR/3 (first carried on the NOAA-15 platform), acquires data in a 6th channel located at 1.6 micron. Typically, the 11 and 12 micron channels are used to derive SST sometimes in combination with the 3.5 micron channel. The swath of the AVHRR sensor is a relatively large 2400 km. All MetOp platforms are sun synchronous and generally view the same earth location twice a day (latitude dependent). The ground native resolution of the AVHRR instruments is approximately 1.1 km at nadir and degrades off nadir. This particular data set is produced from legacy Global Area Coverage (GAC) data that are derived from a sample averaging of the full resolution global AVHRR data. Four out of every five samples along the scan line are used to compute on average value and the data from only every third scan line are processed, yielding an effective 4 km spatial resolution at nadir. The v2.0 is the updated version from current v1.0 with extensive algorithm improvements and upgrades. The major improvements include: 1) Significant changes in contaminant/cloud detection; 2) Increased the spatial resolution from 9 km to 4 km; 3) Updated compliance with GDS2, ACDD 1.3, and CF 1.6; and 4) Removed the dependency on the High-resolution Infrared Radiation Sounder (HIRS) sensor (only available to MetOp-A/B), thus allowing for the consistent inter-calibration and the processing of MetOp-A/B/C data
&lt;br&gt;&lt;h4 id&#x3D;&quot;iasi_sst_metop_a-osisaf-l2p-v10&quot;&gt;IASI_SST_METOP_A-OSISAF-L2P-v1.0&lt;/h4&gt;
A global 1 km Group for High Resolution Sea Surface Temperature (GHRSST) Level 2P dataset based on multi-channel sea surface temperature (SST) retrievals generated in real-time from the Infrared Atmospheric Sounding Interferometer (IASI) on the European Meteorological Operational-A (MetOp-A&amp;#65289;satellite &amp;#65288;launched 19 Oct 2006). The European Organization for the Exploitation of Meteorological Satellites (EUMETSAT),Ocean and Sea Ice Satellite Application Facility (OSI SAF) is producing SST products in near realtime from METOP/IASI. The Infrared Atmospheric Sounding Interferometer (IASI) measures inthe infrared part of the electromagnetic spectrum at a horizontal resolution of 12 km at nadir up to40km over a swath width of about 2,200 km. With 14 orbits in a sun-synchronous mid-morningorbit (9:30 Local Solar Time equator crossing, descending node) global observations can beprovided twice a day. The SST retrieval is performed and provided by the IASI L2 processor atEUMETSAT headquarters. The product format is compliant with the GHRSST Data Specification(GDS) version 2.
&lt;br&gt;&lt;h4 id&#x3D;&quot;iasi_sst_metop_b-osisaf-l2p-v10&quot;&gt;IASI_SST_METOP_B-OSISAF-L2P-v1.0&lt;/h4&gt;
A Group for High Resolution Sea Surface Temperature (GHRSST) Level 2P dataset based on multi-channel sea surface temperature (SST) retrievals generated in real-time from the Infrared Atmospheric Sounding Interferometer (IASI) on the European Meteorological Operational-B (MetOp-B)satellite (launched 17 Sep 2012). The European Organization for the Exploitation of Meteorological Satellites (EUMETSAT),Ocean and Sea Ice Satellite Application Facility (OSI SAF) is producing SST products in near realtime from METOP/IASI. The Infrared Atmospheric Sounding Interferometer (IASI) measures inthe infrared part of the electromagnetic spectrum at a horizontal resolution of 12 km at nadir up to40km over a swath width of about 2,200 km. With 14 orbits in a sun-synchronous mid-morningorbit (9:30 Local Solar Time equator crossing, descending node) global observations can beprovided twice a day. The SST retrieval is performed and provided by the IASI L2 processor atEUMETSAT headquarters. The product format is compliant with the GHRSST Data Specification(GDS) version 2.
&lt;br&gt;&lt;h4 id&#x3D;&quot;amsre-remss-l2p-v7a&quot;&gt;AMSRE-REMSS-L2P-v7a&lt;/h4&gt;
The Advanced Microwave Scanning Radiometer (AMSR-E) was launched on 4 May 2002, aboard NASA&amp;#39;s Aqua spacecraft. The National Space Development Agency of Japan (NASDA) provided AMSR-E to NASA as an indispensable part of Aqua&amp;#39;s global hydrology mission. Over the oceans, AMSR-E is measuring a number of important geophysical parameters, including sea surface temperature (SST), wind speed, atmospheric water vapor, cloud water, and rain rate. A key feature of AMSR-E is its capability to see through clouds, thereby providing an uninterrupted view of global SST and surface wind fields. Remote Sensing Systems (RSS, or REMSS) is the provider of these SST data for the Group for High Resolution Sea Surface Temperature (GHRSST) Project, performs a detailed processing of AMSR-E instrument data in two stages. The first stage produces a near-real-time (NRT) product (identified by &amp;quot;&lt;em&gt;rt&lt;/em&gt;&amp;quot; within the file name) which is made as available as soon as possible. This is generally within 3 hours of when the data are recorded. Although suitable for many timely uses the NRT products are not intended to be archive quality. &amp;quot;Final&amp;quot; data (currently identified by &amp;quot;v7&amp;quot; within the file name) are processed when RSS receives the atmospheric model National Center for Environmental Prediction (NCEP) Final Analysis (FNL) Operational Global Analysis. The NCEP wind directions are particularly useful for retrieving more accurate SSTs and wind speeds. This dataset adheres to the GHRSST Data Processing Specification (GDS) version 2 format specifications.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tmi-remss-l2p-v4&quot;&gt;TMI-REMSS-L2P-v4&lt;/h4&gt;
GDS2 Version -The Tropical Rainfall Measuring Mission (TRMM) Microwave Imager (TMI) is a well calibrated passive microwave radiometer, similar to the Special Sensor Microwave Imager (SSM/I), that contains lower frequency channels required for sea surface temperature (SST) retrievals. The TRMM is part of the NASA&amp;#39;s mission to planet Earth, and is a joint venture between NASA and the Japan Aerospace Exploration Agency (JAXA) to measure precipitation, water vapor, SST and wind in the global tropical regions and was launched in 27 November 1997 from the Tanegashima Space Center in Tanegashima, Japan. The TRMM satellite travels west to east in a 402 km altitude semi-equatorial precessing orbit that results in day-to-day changes in the observation time of any given earth location between 38S and 38N. Remote Sensing Systems has produced a Version-4 TMI ocean SST dataset for the Group for High Resolution Sea Surface Temperature (GHRSST) by applying an algorithm to the 10.7 GHz channel through a removal of surface roughness effects. In contrast to infrared SST observations, microwave retrievals can be measured through clouds, which are nearly transparent at 10.7 GHz. Microwave retrievals are also insensitive to water vapor and aerosols. The algorithm for retrieving SSTs from radiometer data is described in &amp;quot;AMSR Ocean Algorithm.
&lt;br&gt;&lt;h4 id&#x3D;&quot;amsr2-remss-l2p-v82&quot;&gt;AMSR2-REMSS-L2P-v8.2&lt;/h4&gt;
This product provides a “Final” (Refined) Level-2 Sea Surface Temperature (SST) (currently identified by &amp;quot;v8.2&amp;quot; within the file name) for the Group for High Resolution Sea Surface Temperature (GHRSST) Project, which is derived from the Advanced Microwave Scanning Radiometer 2 (AMSR2) by Remote Sensing Systems (RSS, or REMSS). AMSR2 was launched on 18 May 2012, onboard the Global Change Observation Mission - Water (GCOM-W) satellite developed by the Japan Aerospace Exploration Agency (JAXA). The GCOM-W mission aims to establish the global and long-term observation system to collect data, which is needed to understand mechanisms of climate and water cycle variations, and demonstrate its utilization. AMSR2 onboard the first generation of the GCOM-W satellite will continue Aqua/AMSR-E observations of water vapor, cloud liquid water, precipitation, SST, sea surface wind speed, sea ice concentration, snow depth, and soil moisture. AMSR2 is a remote sensing instrument for measuring weak microwave emission from the surface and the atmosphere of the Earth. The antenna of AMSR2 rotates once per 1.5 seconds and obtains data over a 1450 km swath. This conical scan mechanism enables AMSR2 to acquire a set of daytime and nighttime data with more than 99% coverage of the Earth every 2 days. The “Final” SSTs are processed when RSS receives the atmospheric model National Center for Environmental Prediction (NCEP) Final Analysis (FNL) Operational Global Analysis. The NCEP wind directions are particularly useful for retrieving more accurate SSTs and wind speeds. The v8.2 supersedes the previous v8a dataset which can be found at &lt;a href&#x3D;&quot;https://www.doi.org/10.5067/GHAM2-2PR8A&quot;&gt;https://www.doi.org/10.5067/GHAM2-2PR8A&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;viirs_n20-navo-l2p-v30&quot;&gt;VIIRS_N20-NAVO-L2P-v3.0&lt;/h4&gt;
The VIIRS_N20-NAVO-L2P-v3.0 dataset produced by the Naval Oceanographic Office (NAVO) derives the 1-meter depth Sea Surface Temperature (SST) from the Visible Infrared Imaging Radiometer Suite (VIIRS) onboard the Joint Polar Satellite System (JPSS)-1 satellite, renamed as NOAA-20 (N20). N20 was launched on November 18, 2017, the 2nd satellite in the US NOAA JPSS series. &lt;br&gt;&lt;br&gt; VIIRS L2P SST products are derived at the native sensor resolution (~0.75 km at nadir, ~1.5 km at swath edge) using NAVO&amp;#39;s Level-2 SST processor version 3.0 (v3.0). Data contains the global near daily-coverage Sea Surface Temperature at 1-meter depth with 750 m (along) x 750 m (cross) spatial resolution in swath coordinates. Each netCDF file has 768 x 3200 pixels in size, in compliance with the Group for High Resolution Sea Surface Temperature (GHRSST) Data Specification version 2 (GDS2). The data record is available back to Feb. 20 2024. The L2P SST v3.0 is the first release at PO.DAAC derived from the L2P SST processor v3.0, which was upgraded from the v2.0 with several significant improvements in processing algorithms, including contamination detection, cloud detection, and data format upgrades.&lt;br&gt;&lt;br&gt; The product is comparable with the NPP VIIRS L2P (&lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/VIIRS_NPP-NAVO-L2P-v3.0&quot;&gt;https://podaac.jpl.nasa.gov/dataset/VIIRS_NPP-NAVO-L2P-v3.0&lt;/a&gt;) and the N21 VIIRS L2P (&lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/VIIRS_N21-NAVO-L2P-v3.0&quot;&gt;https://podaac.jpl.nasa.gov/dataset/VIIRS_N21-NAVO-L2P-v3.0&lt;/a&gt;) datasets. It also has similar coverage and quality as the NOAA ACSPO VIIRS L2P SST (&lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/N20-VIIRS-L2P-ACSPO-v2.80&quot;&gt;https://podaac.jpl.nasa.gov/dataset/N20-VIIRS-L2P-ACSPO-v2.80&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;viirs_n21-navo-l2p-v30&quot;&gt;VIIRS_N21-NAVO-L2P-v3.0&lt;/h4&gt;
The VIIRS_N21-NAVO-L2P-v3.0 dataset produced by the Naval Oceanographic Office (NAVO) derives the 1-meter depth Sea Surface Temperature (SST) from the Visible Infrared Imaging Radiometer Suite (VIIRS) onboard the Joint Polar Satellite System (JPSS)-2 satellite, renamed as NOAA-21 (N21). N21 was launched on November 10, 2022, the 3rd satellite in the US NOAA JPSS series. &lt;br&gt;&lt;br&gt; VIIRS L2P SST products are derived at the native sensor resolution (~0.75 km at nadir, ~1.5 km at swath edge) using NAVO&amp;#39;s Level-2 SST processor version 3.0 (v3.0). Data contains the global near daily-coverage Sea Surface Temperature at 1-meter depth with 750 m (along) x 750 m (cross) spatial resolution in swath coordinates. Each netCDF file has 768 x 3200 pixels in size, in compliance with the Group for High Resolution Sea Surface Temperature (GHRSST) Data Specification version 2 (GDS2). The data record is available back to Feb. 21 2024. The L2P SST v3.0 is the first release at PO.DAAC derived from the L2P SST processor v3.0, which was upgraded from the v2.0 with several significant improvements in processing algorithms, including contamination detection, cloud detection, and data format upgrades.&lt;br&gt;&lt;br&gt; The product is comparable with the NPP VIIRS L2P (&lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/VIIRS_NPP-NAVO-L2P-v3.0&quot;&gt;https://podaac.jpl.nasa.gov/dataset/VIIRS_NPP-NAVO-L2P-v3.0&lt;/a&gt;) and the N20 VIIRS L2P (&lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/VIIRS_N20-NAVO-L2P-v3.0&quot;&gt;https://podaac.jpl.nasa.gov/dataset/VIIRS_N20-NAVO-L2P-v3.0&lt;/a&gt;). It also has similar coverage and quality as the NOAA ACSPO VIIRS L2P SST (&lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/N21-VIIRS-L2P-ACSPO-v2.80&quot;&gt;https://podaac.jpl.nasa.gov/dataset/N21-VIIRS-L2P-ACSPO-v2.80&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;n21-viirs-l2p-acspo-v280&quot;&gt;N21-VIIRS-L2P-ACSPO-v2.80&lt;/h4&gt;
The N21-VIIRS-L2P-ACSPO-v2.80 dataset produced by the NOAA ACSPO system derives the Subskin Sea Surface Temperature (SST) from the Visible Infrared Imaging Radiometer Suite (VIIRS) onboard the The Joint Polar Satellite System (JPSS)-2 satellite, renamed as NOAA-21 (N21). N21 was launched on Nov. 10, 2022, the 3rd satellite in the US NOAA latest JPSS series. &lt;br&gt;&lt;br&gt; VIIRS L2P SST products are derived at the native sensor resolution (~0.75 km at nadir, ~1.5 km at swath edge) using NOAA&amp;#39;s Advanced Clear-Sky Processor for Ocean (ACSPO) system (Jonasson et al. 2022). Data are reported in 10-minute granules in netCDF4 format, compliant with the Group for High Resolution Sea Surface Temperature (GHRSST) Data Specification version 2 (GDS2). The ACSPO N21 VIIRS SST record is available back to 19 Mar 2023. In ACSPO products, SSTs are derived using the Non-Linear SST (NLSST) algorithms (Petrenko et al., 2014). An ACSPO clear-sky mask (ACSM) is provided in each pixel as part of variable l2p_flags, which also includes day/night, land, ice, twilight, and glint flags (Petrenko et al., 2010). Only ACSM confidently clear pixels with quality level QL&#x3D;5 are recommended. Per GDS2 specifications, two additional Sensor-Specific Error Statistics layers (SSES bias and standard deviation) are reported in each pixel with QL&#x3D;5. &lt;br&gt;&lt;br&gt; The ACSPO VIIRS L2P product is monitored and validated against quality controlled in situ data provided by NOAA in situ SST Quality Monitor system (iQuam) using another NOAA system, SST Quality Monitor (SQUAM). A reduced size (0.5GB/day), equal-angle gridded (0.02-deg resolution), ACSPO N21 VIIRS L3U product is also available (10.5067/GHV21-3U280) (Ignatov et al., 2017).
&lt;br&gt;&lt;h4 id&#x3D;&quot;viirs_n20-star-l2p-v280&quot;&gt;VIIRS_N20-STAR-L2P-v2.80&lt;/h4&gt;
NOAA-20 (N20/JPSS-1/J1) is the second satellite in the US NOAA latest generation Joint Polar Satellite System (JPSS), launched on November 18, 2017. NOAA is responsible for all JPSS products, including SST from the Visible Infrared Imaging Radiometer Suite (VIIRS). The L2P SST product is derived at the native sensor resolution (~0.75 km at nadir, ~1.5 km at swath edge) using NOAA&amp;#39;s Advanced Clear-Sky Processor for Ocean (ACSPO) system, and reported in 10-minute granules in netCDF4 format, compliant with the Group for High Resolution Sea Surface Temperature (GHRSST) Data Specification version 2 (GDS2). SSTs are derived from Brightness Temperatures (BTs) using the Non-Linear SST (NLSST) algorithms (Petrenko et al., 2014). An ACSPO clear-sky mask (ACSM) is provided in each pixel as part of variable l2p_flags, which also includes day/night, land, ice, twilight, and glint flags (Petrenko et al., 2010). Only ACSM confidently clear pixels are recommended (equivalent to GDS2 quality level&#x3D;5). Per GDS2 specifications, two additional Sensor-Specific Error Statistics layers (SSES bias and standard deviation) are reported in each pixel with QL&#x3D;5. The ACSPO VIIRS L2P product is monitored and validated against quality controlled in situ data provided by NOAA in situ SST Quality Monitor system (iQuam) using another NOAA system, SST Quality Monitor (SQUAM). A reduced size (0.5GB/day), equal-angle gridded (0.02-deg resolution), ACSPO L3U product is also available at &lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/VIIRS_N20-STAR-L3U-v2.80&quot;&gt;https://podaac.jpl.nasa.gov/dataset/VIIRS_N20-STAR-L3U-v2.80&lt;/a&gt;, where gridded L2P SSTs with QL&#x3D;5 only are reported. The v2.80 is an updated version from the v2.61 with several algorithm improvements including two added thermal front layers, reduced L2P SST data size, mitigated warm biases in the high latitudes, and improved clear-sky mask.
&lt;br&gt;&lt;h4 id&#x3D;&quot;viirs_npp-star-l2p-v280&quot;&gt;VIIRS_NPP-STAR-L2P-v2.80&lt;/h4&gt;
The Joint Polar Satellite System (JPSS), starting with S-NPP launched on 28 October 2011, is the new generation of the US Polar Operational Environmental Satellites (POES). NOAA is responsible for all JPSS products, including SST from the Visible Infrared Imaging Radiometer Suite (VIIRS). The L2P SST product is derived at the native sensor resolution (~0.75 km at nadir, ~1.5 km at swath edge) using NOAA&amp;#39;s Advanced Clear-Sky Processor for Ocean (ACSPO) system, and reported in 10-minute granules in netCDF4 format, compliant with the Group for High Resolution Sea Surface Temperature (GHRSST) Data Specification version 2 (GDS2). SSTs are derived from Brightness Temperatures (BTs) using the Non-Linear SST (NLSST) algorithms (Petrenko et al., 2014). An ACSPO clear-sky mask (ACSM) is provided in each pixel as part of variable l2p_flags, which also includes day/night, land, ice, twilight, and glint flags (Petrenko et al., 2010). Only ACSM confidently clear pixels are recommended (equivalent to GDS2 quality level&#x3D;5). Per GDS2 specifications, two additional Sensor-Specific Error Statistics layers (SSES bias and standard deviation) are reported in each pixel with QL&#x3D;5. The ACSPO VIIRS L2P product is monitored and validated against quality controlled in situ data provided by NOAA in situ SST Quality Monitor system (iQuam) using another NOAA system, SST Quality Monitor (SQUAM). A reduced size (0.5GB/day), equal-angle gridded (0.02-deg resolution), ACSPO L3U product is also available at &lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/VIIRS_NPP-STAR-L3U-v2.80&quot;&gt;https://podaac.jpl.nasa.gov/dataset/VIIRS_NPP-STAR-L3U-v2.80&lt;/a&gt;, where gridded L2P SSTs with QL&#x3D;5 only are reported. The v2.80 is an updated version from the v2.61 with several algorithm improvements including two added thermal front layers, reduced L2P SST data size, mitigated warm biases in the high latitudes, and improved clear-sky mask.
&lt;br&gt;&lt;h4 id&#x3D;&quot;avhrr19_l-navo-l2p-v10&quot;&gt;AVHRR19_L-NAVO-L2P-v1.0&lt;/h4&gt;
A regional Group for High Resolution Sea Surface Temperature (GHRSST) Level 2P dataset based on multi-channel sea surface temperature (SST) retrievals generated in real-time from the Advanced Very High Resolution Radiometer (AVHRR) on the NOAA-19 platform (launched 6 Feb 2009) produced and used operationally in oceanographic analyses and forecasts by the US Naval Oceanographic Office (NAVO). The AVHRR is a space-borne scanning sensor on the National Oceanic and Atmospheric Administration (NOAA) family of Polar Orbiting Environmental Satellites (POES) having a operational legacy that traces back to the Television Infrared Observation Satellite-N (TIROS-N) launched in 1978. AVHRR instruments measure the radiance of the Earth in 5 (or 6) relatively wide spectral bands. The first two are centered around the red (0.6 micrometer) and near-infrared (0.9 micrometer) regions, the third one is located around 3.5 micrometer, and the last two sample the emitted thermal radiation, around 11 and 12 micrometers, respectively. The legacy 5 band instrument is known as AVHRR/2 while the more recent version, the AVHRR/3 (first carried on the NOAA-15 platform), acquires data in a 6th channel located at 1.6 micrometer. Typically the 11 and 12 micron channels are used to derive SST sometimes in combination with the 3.5 micron channel. The NOAA platforms are sun synchronous generally viewing the same earth location twice a day (latitude dependent) due to the relatively large AVHRR swath of approximately 2400 km. The highest ground resolution that can be obtained from the current AVHRR instruments is 1.1 km at nadir. AVHRR data are acquired in three formats: High Resolution Picture Transmission (HRPT), Local Area Coverage (LAC), and Global Area Coverage (GAC). HRPT data are full resolution image data transmitted to a ground stations as they are collected. LAC are also full resolution data, but the acquisition is prescheduled and recorded with an on-board tape recorder for subsequent transmission during a station overpass. GAC data provide daily subsampled global coverage recorded on tape recorders and then transmitted to a ground station. This particular dataset is derived from LAC data. Further binning and averaging of the 1.1 km LAC pixels results in a final dataset resolution of 2.2 km. The coverage of the LAC data can vary but generally contains scenes over the oceans adjacent to Australia and the North Indian Ocean.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ewsg1-navo-l2p-v01&quot;&gt;EWSG1-NAVO-L2P-v01&lt;/h4&gt;
A Group for High Resolution Sea Surface Temperature (GHRSST) Level 2P sea surface temperature produced by The Naval Oceanographic Office (NAVO) from the GOES Imager sensor on the Electro-Optical Infrared Weather System – Geostationary satellite (EWS-G1). The EWS-G1, formerly GOES-13, is the first Department of Defense owned geostationary weather satellite, which has been repositioned over Indian Ocean (IO) region at 60.0° West longitude in January 2018 and fully operational since September 8, 2020, providing timely cloud characterization and theater weather imagery to DoD. The EWS-G1 L2P SST product is calculated based on the 4-micron (band 2) and 11-micron (band 4) channels, providing nighttime and daytime SST. However, daytime SSTs are not produced in areas where the 4-micron channel is strongly affected by Solar radiation, which is defined by solar reflection angle &amp;gt; 50 degree. The L2P data are packaged according to the GHRSST Data Specification version 2 (GDS2) in netCDF4 format at 0.04-degree spatial resolution and stored in 48 half-hour granules per day. The data will be continually updated with 24 hours latency.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ewsg2-navo-l2p-v01&quot;&gt;EWSG2-NAVO-L2P-v01&lt;/h4&gt;
A Group for High Resolution Sea Surface Temperature (GHRSST) Level 2P sea surface temperature dataset produced by the Naval Oceanographic Office (NAVO) from the GOES Imager sensor on the Electro-Optical Infrared Weather System – Geostationary satellite (EWS-G2). The EWS-G2, formerly GOES-15, is the second Department of Defense owned geostationary weather satellite, which has been repositioned over Indian Ocean (IO) region at 60.0° West longitude in September 2023 and fully operational since December 3, 2023, providing timely cloud characterization and theater weather imagery to DoD. The EWS-G2 L2P SST product is calculated based on the 4-micron (band 2) and 11-micron (band 4) channels, providing nighttime and daytime SST. However, daytime SSTs are not produced in areas where the 4-micron channel is strongly affected by Solar radiation, which is defined by solar reflection angle &amp;gt; 50 degrees. The L2P data are packaged according to the GHRSST Data Specification version 2 (GDS2) in netCDF4 format at 0.04-degree spatial resolution and stored in 104 partial disks per day. The data will be continually updated with 24 hours latency.
&lt;br&gt;&lt;h4 id&#x3D;&quot;avhrr_sst_metop_a-osisaf-l2p-v10&quot;&gt;AVHRR_SST_METOP_A-OSISAF-L2P-v1.0&lt;/h4&gt;
A global 1 km Group for High Resolution Sea Surface Temperature (GHRSST) Level 2P dataset based on multi-channel sea surface temperature (SST) retrievals generated in real-time from the Advanced Very High Resolution Radiometer (AVHRR) on the European Meteorological Operational-A (MetOp-A)satellite (launched 19 Oct 2006). The European Organization for the Exploitation of Meteorological Satellites (EUMETSAT), Ocean and Sea Ice Satellite Application Facility (OSI SAF) is producing SST products in near real time from Metop/AVHRR. Global AVHRR level 1b data are acquired at Meteo-France/Centre de Meteorologie Spatiale (CMS) through the EUMETSAT/EUMETCAST system. SST is retrieved from the AVHRR infrared channels (3.7, 10.8 and 12.0 micrometer) using a multispectral algorithm. Atmospheric profiles of water vapor and temperature from a numerical weather prediction model, together with a radiatiave transfer model, are used to correct the multispectral algorithm for regional and seasonal biases due to changing atmospheric conditions. This product is delivered at full resolution in satellite projection as metagranule corresponding to 3 minutes of acquisition. The product format is compliant with the GHRSST Data Specification (GDS) version 2.
&lt;br&gt;&lt;h4 id&#x3D;&quot;avhrr_sst_metop_b-osisaf-l2p-v10&quot;&gt;AVHRR_SST_METOP_B-OSISAF-L2P-v1.0&lt;/h4&gt;
A global 1 km Group for High Resolution Sea Surface Temperature (GHRSST) Level 2P dataset based on multi-channel sea surface temperature (SST) retrievals generated in real-time from the Advanced Very High Resolution Radiometer (AVHRR) on the European Meteorological Operational-B (MetOp-B) satellite (launched 17 Sep 2012). The European Organization for the Exploitation of Meteorological Satellites (EUMETSAT), Ocean and Sea Ice Satellite Application Facility (OSI SAF) is producing SST products in near real time from Metop/AVHRR. Global AVHRR level 1b data are acquired at Meteo-France/Centre de Meteorologie Spatiale (CMS) through the EUMETSAT/EUMETCAST system. SST is retrieved from the AVHRR infrared channels (3.7, 10.8 and 12.0 micrometer) using a multispectral algorithm. Atmospheric profiles of water vapor and temperature from a numerical weather prediction model, together with a radiatiave transfer model, are used to correct the multispectral algorithm for regional and seasonal biases due to changing atmospheric conditions. This product is delivered at full resolution in satellite projection as metagranule corresponding to 3 minutes of acquisition. The product format is compliant with the GHRSST Data Specification (GDS) version 2.
&lt;br&gt;&lt;h4 id&#x3D;&quot;goes13-ospo-l2p-v10&quot;&gt;GOES13-OSPO-L2P-v1.0&lt;/h4&gt;
The Geostationary Operational Environmental Satellites (GOES) operated by the United States National Oceanic and Atmospheric Administration (NOAA) support weather forecasting, severe storm tracking, meteorology and oceanography research. Generally there are several GOES satellites in geosynchronous orbit at any one time viewing different earth locations including the GOES-13 launched 24 May 2006. The radiometer aboard the satellite, The GOES N-P Imager, is a five channel (one visible, four infrared) imaging radiometer designed to sense radiant and solar reflected energy from sampled areas of the earth. The multi-element spectral channels simultaneously sweep east-west and west-east along a north-to-south path by means of a two-axis mirror scan system retuning telemetry in 10-bit precision. For this Group for High Resolution Sea Surface Temperature (GHRSST) dataset, skin sea surface temperature (SST) measurements are calculated from the far IR channels of GOES-13 at full resolution on a half hourly basis. In native satellite projection, vertically adjacent pixels are averaged and read out at every pixel. L2P datasets including Single Sensor Error Statistics (SSES) are then derived following the GHRSST Data Processing Specification (GDS) version 2.0. The full disk image is subsetted into granules representing distinct northern and southern regions.
&lt;br&gt;&lt;h4 id&#x3D;&quot;mtsat2-ospo-l2p-v10&quot;&gt;MTSAT2-OSPO-L2P-v1.0&lt;/h4&gt;
Multi-functional Transport Satellites (MTSAT) are a series of geostationary weather satellites operated by the Japan Meteorological Agency (JMA). MTSAT carries an aeronautical mission to assist air navigation, plus a meteorological mission to provide imagery over the Asia-Pacific region for the hemisphere centered on 140 East. The meteorological mission includes an imager giving nominal hourly full Earth disk images in five spectral bands (one visible, four infrared). MTSAT are spin stabilized satellites. With this system images are built up by scanning with a mirror that is tilted in small successive steps from the north pole to south pole at a rate such that on each rotation of the satellite an adjacent strip of the Earth is scanned. It takes about 25 minutes to scan the full Earth&amp;#39;s disk. This builds a picture 10,000 pixels for the visible images (1.25 km resolution) and 2,500 pixels (4 km resolution) for the infrared images. The MTSAT-2 (also known as Himawari 7) and its radiometer (MTSAT-2 Imager) was successfully launched on 18 February 2006. For this Group for High Resolution Sea Surface Temperature (GHRSST) dataset, skin sea surface temperature (SST) measurements are calculated from the IR channels of the MTSAT-2 Imager full resolution data in satellite projection on a hourly basis by using Bayesian Cloud Mask algorithm at the Office of Satellite and Product Operations (OSPO). L2P datasets including Single Sensor Error Statistics (SSES) are then derived following the GHRSST Data Processing Specification (GDS) version 2.0.
&lt;br&gt;&lt;h4 id&#x3D;&quot;seviri_sst-osisaf-l3c-v10&quot;&gt;SEVIRI_SST-OSISAF-L3C-v1.0&lt;/h4&gt;
A Group for High Resolution Sea Surface Temperature (GHRSST) dataset for the Eastern Atlantic Region from the Spinning Enhanced Visible and InfraRed Imager (SEVIRI) on the Meteosat Second Generation (MSG-3) satellites (launched 5 July 2012). The European Organization for the Exploitation of Meteorological Satellites (EUMETSAT), Ocean and Sea Ice Satellite Application Facility (OSI SAF) is producing SST products in near real time from MSG/SEVIRI. SEVIRI level 1.5 data are acquired at Meteo-France/Centre de Meteorologie Spatiale (CMS) through the EUMETSAT/EUMETCAST system. SST is retrieved from the SEVIRI infrared channels (10.8 and 12.0 micrometer) using a multispectral algorithm. Atmospheric profiles of water vapor and temperature from a numerical weather prediction model, together with a radiatiave transfer model, are used to correct the multispectral algorithm for regional and seasonal biases due to changing atmospheric conditions. Every 15 minutes slot is processed at full satellite resolution. The operational products are then produced by remapping over a 0.05 degree regular grid (60S-60N and 60W-60E) SST fields obtained by aggregating all 15 minute SST data available in one hour time, and the priority being given to the value the closest in time to the product nominal hour. The product format is compliant with the GHRSST Data Specification (GDS) version 2.
&lt;br&gt;&lt;h4 id&#x3D;&quot;seviri_io_sst-osisaf-l3c-v10&quot;&gt;SEVIRI_IO_SST-OSISAF-L3C-v1.0&lt;/h4&gt;
This dataset is produced by the Ocean and Sea Ice Satellite Application Facility (OSI SAF) from the Spinning Enhanced Visible and InfraRed Imager (SEVIRI) instrument onboard the Meteosat Second Generation (MSG-1), Meteosat-8 satellite (launched on 28 August 2002). The dataset covers the Indian Ocean region with latitude of 60S-60N and longitude of 101.5E-18.5W. Level-3C SST, in the NetCDF format recommended by Group for High Resolution Sea Surface Temperature (GHRSST), is identical to Level-2P GHRSST products, 3 refers to gridded products and C to the fact that hourly products result from compositing 15 minutes (MSG) or 30 minutes (GOES-E) data. The European Organization for the Exploitation of Meteorological Satellites (EUMETSAT), OSI SAF is producing SST products in near real time from MSG/SEVIRI. SEVIRI level 1.5 data are acquired at Meteo-France/Centre de Meteorologie Spatiale (CMS) through the EUMETSAT/EUMETCAST system. SST is retrieved from the SEVIRI infrared channels (10.8 and 12.0 micrometer) using a multispectral algorithm. Atmospheric profiles of water vapor and temperature from a numerical weather prediction model, together with a radiatiave transfer model, are used to correct the multispectral algorithm for regional and seasonal biases due to changing atmospheric conditions. Every 15 minutes slot is processed at full satellite resolution. The operational products are then produced by remapping over a 0.05-degree regular grid (60S-60N and 135W-15W) SST fields obtained by aggregating all 15-minute SST data available in one-hour time, and the priority being given to the value the closest in time to the product nominal hour. The product format is compliant with the GHRSST Data Specification (GDS) version 2.
&lt;br&gt;&lt;h4 id&#x3D;&quot;avhrr_sst_metop_b_nar-osisaf-l3c-v10&quot;&gt;AVHRR_SST_METOP_B_NAR-OSISAF-L3C-v1.0&lt;/h4&gt;
A Group for High Resolution Sea Surface Temperature (GHRSST) dataset for the North Atlantic Region (NAR) derived from the Advanced Very High Resolution Radiometer (AVHRR) on the European Meteorological Operational-B (MetOp-B) platform (launched 17 Sep 2012). The European Organization for the Exploitation of Meteorological Satellites (EUMETSAT), Ocean and Sea Ice Satellite Application Facility (OSI SAF) is producing SST products in near real time from Metop/AVHRR and SNPP/VIIRS. Global AVHRR level 1b data are acquired at Meteo- France/Centre de Meteorologie Spatiale (CMS) through the EUMETSAT/EUMETCAST system. NAR SNPP/VIIRS level 0 data are acquired through direct readout and converted into l1b at CMS. SST is retrieved from the AVHRR and VIIRS infrared channels using a multispectral algorithm. This product is delivered as four six hourly collated files per day on a regular 2km grid. The product format is compliant with the GHRSST Data Specification (GDS) version 2.
&lt;br&gt;&lt;h4 id&#x3D;&quot;viirs_sst_npp_nar-osisaf-l3c-v10&quot;&gt;VIIRS_SST_NPP_NAR-OSISAF-L3C-v1.0&lt;/h4&gt;
A regional Group for High Resolution Sea Surface Temperature (GHRSST) Level 3 Collated (L3C) dataset for the North Atlantic Region (NAR) based on retrievals from the Visible Infrared Imaging Radiometer Suite (VIIRS). The European Organization for the Exploitation of Meteorological Satellites (EUMETSAT), Ocean and Sea Ice Satellite Application Facility (OSI SAF) is producing SST products in near real time from Metop/AVHRR and SNPP/VIIRS. Global AVHRR level 1b data are acquired at Meteo-France/Centre de Meteorologie Spatiale (CMS) through the EUMETSAT/EUMETCAST system. NAR SNPP/VIIRS level 0 data are acquired through direct readout and converted into l1b at CMS. SST is retrieved from the AVHRR and VIIRS infrared channels using a multispectral algorithm. This product is delivered as four six hourly collated files per day on a regular 2km grid. The product format is compliant with the GHRSST Data Specification (GDS) version 2.
&lt;br&gt;&lt;h4 id&#x3D;&quot;avhrr_sst_metop_a_nar-osisaf-l3c-v10&quot;&gt;AVHRR_SST_METOP_A_NAR-OSISAF-L3C-v1.0&lt;/h4&gt;
A Group for High Resolution Sea Surface Temperature (GHRSST) dataset for the North Atlantic Region (NAR) derived from the Advanced Very High Resolution Radiometer (AVHRR) on the European Meteorological Operational-A (MetOp-A) platform (launched 19 Oct 2006). The European Organization for the Exploitation of Meteorological Satellites (EUMETSAT), Ocean and Sea Ice Satellite Application Facility (OSI SAF) is producing SST products in near real time from Metop/AVHRR and SNPP/VIIRS. Global AVHRR level 1b data are acquired at Meteo-France/Centre de Meteorologie Spatiale (CMS) through the EUMETSAT/EUMETCAST system. NAR SNPP/VIIRS level 0 data are acquired through direct readout and converted into l1b at CMS. SST is retrieved from the AVHRR and VIIRS infrared channels using a multispectral algorithm. This product is delivered as four six hourly collated files per day on a regular 2km grid. The product format is compliant with the GHRSST Data Specification (GDS) version 2.
&lt;br&gt;&lt;h4 id&#x3D;&quot;avhrr_sst_noaa19_nar-osisaf-l3c-v10&quot;&gt;AVHRR_SST_NOAA19_NAR-OSISAF-L3C-v1.0&lt;/h4&gt;
A Group for High Resolution Sea Surface Temperature (GHRSST) dataset for the North Atlantic Region (NAR) from the Advanced Very High Resolution Radiometer (AVHRR) on the NOAA-19 platform (launched 6 Feb 2009). This particular dataset is produced by the European Organization for the Exploitation of Meteorological Satellites (EUMETSAT), Ocean and Sea Ice Satellite Application Facility (OSI SAF) in France. The AVHRR is a space-borne scanning sensor on the National Oceanic and Atmospheric Administration (NOAA) family of Polar Orbiting Environmental Satellites (POES) having a operational legacy that traces back to the Television Infrared Observation Satellite-N (TIROS-N) launched in 1978. AVHRR instruments measure the radiance of the Earth in 5 (or 6) relatively wide spectral bands. The first two are centered around the red (0.6 micrometer) and near-infrared (0.9 micrometer) regions, the third one is located around 3.5 micrometer, and the last two sample the emitted thermal radiation, around 11 and 12 micrometers, respectively. The legacy 5 band instrument is known as AVHRR/2 while the more recent version, the AVHRR/3 (first carried on the NOAA-15 platform), acquires data in a 6th channel located at 1.6 micrometer. Typically the 11 and 12 micron channels are used to derive sea surface temperature (SST) sometimes in combination with the 3.5 micron channel. The highest ground resolution that can be obtained from the current AVHRR instruments is 1.1 km at nadir. The NOAA-19 platform is sun synchronous generally viewing the same earth location twice a day (latitude dependent) due to the relatively large AVHRR swath of approximately 2400 km. The NAR products are SST fields derived from 1km AVHRR data that are re-mapped onto a 0.02 degree equal angle grid. In the processing chain, global AVHRR level 1b data are acquired at Centre de Meteorologie Spatiale (CMS) through the EUMETSAT/EUMETCAST system. A cloud mask is applied and SST is retrieved from the AVHRR infrared (IR) channels by using a multispectral technique. This dataset adheres to the GHRSST Data Processing Specification (GDS) version 2 format specifications.
&lt;br&gt;&lt;h4 id&#x3D;&quot;goes13-osisaf-l3c-v10&quot;&gt;GOES13-OSISAF-L3C-v1.0&lt;/h4&gt;
A regional Group for High Resolution Sea Surface Temperature (GHRSST) Level 3 Collated (L3C) dataset for the America Region (AMERICAS) based on retrievals from the GOES-13 Imager on board GOES-13 satellite. The European Organization for the Exploitation of Meteorological Satellites (EUMETSAT), Ocean and Sea Ice Satellite Application Facility (OSI SAF) is producing SST products in near real time from GOES 13 in East position. GOES 13 imager level 1 data are acquired at Meteo- France/Centre de Meteorologie Spatiale (CMS) through the EUMETSAT/EUMETCAST system. SST is retrieved from the GOES 13 infrared channels (3.9 and 10.8 micrometer) using a multispectral algorithm. Due to the lack of 12 micrometer channel in the GOES 13 imager, SST retrieval is not possible in daytime conditions. Atmospheric profiles of water vapor and temperature from a numerical weather prediction model, together with a radiatiave transfer model, are used to correct the multispectral algorithm for regional and seasonal biases due to changing atmospheric conditions. Every 30 minutes slot is processed at full satellite resolution. The operational products are then produced by remapping over a 0.05 degree regular grid (60S-60N and 135W-15W) SST fields obtained by aggregating 30 minute SST data available in one hour time, and the priority being given to the value the closest in time to the product nominal hour. The product format is compliant with the GHRSST Data Specification (GDS) version 2.
&lt;br&gt;&lt;h4 id&#x3D;&quot;amsr2-remss-l3u_rt-v82&quot;&gt;AMSR2-REMSS-L3U_RT-v8.2&lt;/h4&gt;
This product contains a near-real-time (NRT) Level-3U Sea Surface Temperature (SST) (identified by &amp;quot;&lt;em&gt;rt&lt;/em&gt;&amp;quot; within the file name) for the Group for High Resolution Sea Surface Temperature (GHRSST) Project, which is derived from the Advanced Microwave Scanning Radiometer 2 (AMSR2) by Remote Sensing Systems (RSS, or REMSS). AMSR2 was launched on 18 May 2012, onboard the Global Change Observation Mission - Water (GCOM-W) satellite developed by the Japan Aerospace Exploration Agency (JAXA). The GCOM-W mission aims to establish the global and long-term observation system to collect data, which is needed to understand mechanisms of climate and water cycle variations, and demonstrate its utilization. AMSR2 onboard the first generation of the GCOM-W satellite will continue Aqua/AMSR-E observations of water vapor, cloud liquid water, precipitation, SST, sea surface wind speed, sea ice concentration, snow depth, and soil moisture. AMSR2 is a remote sensing instrument for measuring weak microwave emission from the surface and the atmosphere of the Earth. The antenna of AMSR2 rotates once per 1.5 seconds and obtains data over a 1450 km swath. This conical scan mechanism enables AMSR2 to acquire a set of daytime and nighttime data with more than 99% coverage of the Earth every 2 days. The NRT SST is made as available as soon as possible, generally within 3 hours latency. The v8.2 supersedes the previous v8a dataset which can be found at &lt;a href&#x3D;&quot;https://www.doi.org/10.5067/GHAM2-3TR8A&quot;&gt;https://www.doi.org/10.5067/GHAM2-3TR8A&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;amsr2-remss-l3u_rt-v8a&quot;&gt;AMSR2-REMSS-L3U_RT-v8a&lt;/h4&gt;
GDS2 Version -The Advanced Microwave Scanning Radiometer 2 (AMSR2) was launched on 18 May 2012, onboard the Golbal Change Observation Mission - Water (GCOM-W) satellite developed by the Japan Aerospace Exploration Agency (JAXA). The GCOM-W mission aims to establish the global and long-term observation system to collect data, which is needed to understand mechanisms of climate and water cycle variations, and demonstrate its utilization. AMSR2 onboard the first generation of the GCOM-W satellite will continue Aqua/AMSR-E observations of water vapor, cloud liquid water, precipitation, SST, sea surface wind speed, sea ice concentration, snow depth, and soil moisture. AMSR2 is a remote sensing instrument for measuring weak microwave emission from the surface and the atmosphere of the Earth. From about 700 km above the Earth, AMSR2 will provide us highly accurate measurements of the intensity of microwave emission and scattering. The antenna of AMSR2 rotates once per 1.5 seconds and obtains data over a 1450 km swath. This conical scan mechanism enables AMSR2 to acquire a set of daytime and nighttime data with more than 99% coverage of the Earth every 2 days. Remote Sensing Systems (RSS, or REMSS), providers of these SST data for the Group for High Resolution Sea Surface Temperature (GHRSST) Project, performs a detailed processing of AMSR-E instrument data in two stages. The first stage produces a near-real-time (NRT) product (identified by &amp;quot;rt&amp;quot; within the file name) which is made as available as soon as possible. This is generally within 3 hours of when the data are recorded. Although suitable for many timely uses the NRT products are not intended to be archive quality. &amp;quot;Final&amp;quot; data (currently identified by &amp;quot;v8&amp;quot; within the file name) are processed when RSS receives the atmospheric mode NCEP FNL analysis. The NCEP wind directions are particularly useful for retrieving more accurate SSTs and wind speeds. The final &amp;quot;v8&amp;quot; products will continue to accumulate new swaths (half orbits) until the maps are full, generally within 2 days.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gmi-remss-l3u-v82a&quot;&gt;GMI-REMSS-L3U-v8.2a&lt;/h4&gt;
The Global Precipitation Measurement (GPM) satellite was launched on February 27th, 2014 with the GPM Microwave Imager (GMI) instrument on board. The GPM mission is a joint effort between NASA, the Japan Aerospace Exploration Agency (JAXA) and other international partners. In march 2005, NASA has chosen the Ball Aerospace and Technologies Corp., Boulder, Colorado to build the GMI instrument on the continued success of the Tropical Rainfall Measuring Mission (TRMM) satellite by expanding current coverage of precipitation from the tropics to the entire world. GMI is a dual-polarization, multi-channel, conical-scanning, passive microwave radiometer with frequent revisit times. One of the primary differences between GPM and other satellites with microwave radiometers is the orbit, which is inclined 65 degrees, allowing a full sampling of all local Earth times repeated approximately every 2 weeks. The GPM platform undergoes yaw maneuvers approximately every 40 days to compensate for the sun&amp;#39;s changing position and prevent the side of the spacecraft facing the sun from overheating. Today, the GMI instrument plays an essential role in the worldwide measurement of precipitation and environmental forecasting. Sea Surface Temperature (SST) is one of its major products. The GMI data from the Remote Sensing System (REMSS) have been produced using an updated RTM, Version-8. The V8 brightness temperatures from GMI are slightly different from the V7 brightness temperatures; The SST datasets are available in near-real time (NRT) as they arrive, with a delay of about 3 to 6 hours, including the Daily, 3-Day, Weekly, and Monthly time series products.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tmi-remss-l3u-v71a&quot;&gt;TMI-REMSS-L3U-v7.1a&lt;/h4&gt;
The Tropical Rainfall Measuring Mission (TRMM) Microwave Imager (TMI) is a well calibrated passive microwave radiometer, similar to the Special Sensor Microwave Imager (SSM/I), that contains lower frequency channels required for sea surface temperature (SST) retrievals. The TRMM is part of the NASA&amp;#39;s mission to planet Earth, and is a joint venture between NASA and the Japan Aerospace Exploration Agency (JAXA) to measure precipitation, water vapor, sea surface temperature (SST) and surface wind in the global tropical regions and was launched in 27 November 1997 from the Tanegashima Space Center in Tanegashima, Japan. The TRMM satellite travels west to east in a 402 km altitude semi-equatorial processing orbit that results in day-to-day changes in the observation time of any given earth location between 38S and 38N. Remote Sensing Systems (REMSS) has produced a Version-7.1a TMI SST dataset for the Group for High Resolution Sea Surface Temperature (GHRSST) by applying an algorithm to the 10.7 GHz channel through a removal of surface roughness effects. In contrast to infrared SST observations, microwave retrievals can be measured through clouds, which are nearly transparent at 10.7 GHz. Microwave retrievals are also insensitive to water vapor and aerosols. The algorithm for retrieving SSTs from radiometer data is described in &amp;quot;AMSR Ocean Algorithm.
&lt;br&gt;&lt;h4 id&#x3D;&quot;amsr2-remss-l3u-v82&quot;&gt;AMSR2-REMSS-L3U-v8.2&lt;/h4&gt;
This product contains a “Final” (Refined) Level-3U Sea Surface Temperature (SST) (currently identified by &amp;quot;v8.2&amp;quot; within the file name) for the Group for High Resolution Sea Surface Temperature (GHRSST) Project, which is derived from the Advanced Microwave Scanning Radiometer 2 (AMSR2) by Remote Sensing Systems (RSS, or REMSS). AMSR2 was launched on 18 May 2012, onboard the Global Change Observation Mission - Water (GCOM-W) satellite developed by the Japan Aerospace Exploration Agency (JAXA). The GCOM-W mission aims to establish the global and long-term observation system to collect data, which is needed to understand mechanisms of climate and water cycle variations, and demonstrate its utilization. AMSR2 onboard the first generation of the GCOM-W satellite will continue Aqua/AMSR-E observations of water vapor, cloud liquid water, precipitation, SST, sea surface wind speed, sea ice concentration, snow depth, and soil moisture. AMSR2 is a remote sensing instrument for measuring weak microwave emission from the surface and the atmosphere of the Earth. The antenna of AMSR2 rotates once per 1.5 seconds and obtains data over a 1450 km swath. This conical scan mechanism enables AMSR2 to acquire a set of daytime and nighttime data with more than 99% coverage of the Earth every 2 days. The “Final” SSTs are processed when RSS receives the atmospheric model National Center for Environmental Prediction (NCEP) Final Analysis (FNL) Operational Global Analysis. The NCEP wind directions are particularly useful for retrieving more accurate SSTs and wind speeds. The final &amp;quot;v8.2&amp;quot; products will continue to accumulate new swaths (half orbits) until the maps are full, generally within 2 days. The v8.2 L3U SST supersedes the previous v8a dataset which can be found at &lt;a href&#x3D;&quot;https://www.doi.org/10.5067/GHAM2-3UR8A&quot;&gt;https://www.doi.org/10.5067/GHAM2-3UR8A&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;windsat-remss-l3u-v701a&quot;&gt;WindSat-REMSS-L3U-v7.0.1a&lt;/h4&gt;
The WindSat Polarimetric Radiometer, launched on January 6, 2003 aboard the Department of Defense Coriolis satellite, was designed to measure the ocean surface wind vector from space. It developed by the Naval Research Laboratory (NRL) Remote Sensing Division and the Naval Center for Space Technology for the U.S. Navy and the National Polar-orbiting Operational Environmental Satellite System (NPOESS) Integrated Program Office (IPO). In addition to wind speed and direction, the instrument can also measure sea surface temperature, soil moisture, ice and snow characteristics, water vapor, cloud liquid water, and rain rate. Unlike previous radiometers, the WindSat sensor takes observations during both the forward and aft looking scans. This makes the WindSat geometry of the earth view swath quite different and significantly more complicated to work with than the other passive microwave sensors. The Remote Sensing Systems (RSS, or REMSS) WindSat products are the only dataset available that uses both the fore and aft look directions. By using both directions, a wider swath and more complicated swath geometry is obtained. RSS providers of these SST data for the Group for High Resolution Sea Surface Temperature (GHRSST) Project, performs a detailed processing of WindSat instrument data in two stages. The first stage produces a near-real-time (NRT) product (identified by &amp;quot;rt&amp;quot; within the file name) which is made as available as soon as possible. This is generally within 3 hours of when the data are recorded. Although suitable for many timely uses the NRT products are not intended to be archive quality. &amp;quot;Final&amp;quot; data (currently identified by &amp;quot;v7.0.1a&amp;quot; within the file name) are processed when RSS receives the atmospheric mode NCEP FNL analysis. The NCEP wind directions are particularly useful for retrieving more accurate SSTs and wind speeds. The final &amp;quot;v7.0.1a&amp;quot; products will continue to accumulate new swaths (half orbits) until the maps are full, generally within 7 days. The version with letter &amp;quot;a&amp;quot; refers to the file incompliance with GHRSST format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;n21-viirs-l3u-acspo-v280&quot;&gt;N21-VIIRS-L3U-ACSPO-v2.80&lt;/h4&gt;
The N21-VIIRS-L3U-ACSPO-v2.80 dataset produced by the NOAA ACSPO system derives the Subskin Sea Surface Temperature (SST) from the Visible Infrared Imaging Radiometer Suite (VIIRS) onboard the Joint Polar Satellite System (JPSS)-2 satellite, renamed as NOAA-21 (N21). N21 was launched on Nov. 10, 2022, the 3rd satellite in the US NOAA latest JPSS series. &lt;br&gt;&lt;br&gt; The ACSPO N21 VIIRS L3U (Level 3 Uncollated) product is a gridded version of the ACSPO N21 VIIRS L2P product, also available at PO.DAAC (10.5067/GHV21-2P280). The L3U output files are 10-minute granules in netCDF4 format, compliant with the Group for High Resolution Sea Surface Temperature (GHRSST) Data Specification version 2 (GDS2). The ACSPO N21 VIIRS SST record is available back to 19 Mar 2023. There are 144 granules per 24 hour interval, with a total data volume of 0.6GB/day. Fill values are reported at all invalid pixels, including pixels &amp;gt;5 km inland. For each valid water pixel (defined as ocean, sea, lake or river, and up to 5 km inland), the following layers are reported: SST, a subset of variable l2p_flags (including day/night, land, ice, twilight, and glint flags), wind speed, and the SST minus reference CMC SST (Canadian Met Centre 0.1deg L4 SST, 10.5067/GHCMC-4FM03). Only L2P SSTs with QL&#x3D;5 were gridded, so all valid SSTs are recommended for the users. Per GDS2 specifications, two additional Sensor-Specific Error Statistics layers (SSES bias and standard deviation) are reported in each pixel with valid SST. &lt;br&gt;&lt;br&gt; The ACSPO VIIRS L3U product is monitored and validated against quality controlled in situ data provided by NOAA in situ SST Quality Monitor system (iQuam) using another NOAA system, SST Quality Monitor (SQUAM).
&lt;br&gt;&lt;h4 id&#x3D;&quot;viirs_n20-star-l3u-v280&quot;&gt;VIIRS_N20-STAR-L3U-v2.80&lt;/h4&gt;
NOAA-20 (N20/JPSS-1/J1) is the second satellite in the US NOAA latest generation Joint Polar Satellite System (JPSS), launched on November 18, 2017. The ACSPO N20/VIIRS L3U (Level 3 Uncollated) product is a gridded version of the ACSPO N20/VIIRS L2P product available here &lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/VIIRS_N20-STAR-L2P-v2.80&quot;&gt;https://podaac.jpl.nasa.gov/dataset/VIIRS_N20-STAR-L2P-v2.80&lt;/a&gt;. The L3U output files are 10-minute granules in netCDF4 format, compliant with the Group for High Resolution Sea Surface Temperature (GHRSST) Data Specification version 2 (GDS2). There are 144 granules per 24hr interval, with a total data volume of 0.5GB/day. Fill values are reported at all invalid pixels, including pixels with &amp;gt;5 km inland. For each valid water pixel (defined as ocean, sea, lake or river, and up to 5 km inland), the following layers are reported: SSTs, a subset of l2p_flags (including day/night, land, ice, twilight, and glint flags), wind speed, and ACSPO SST minus reference (Canadian Met Centre 0.1deg L4 SST; available at &lt;a href&#x3D;&quot;https://www.doi.org/10.5067/GHCMC-4FM03&quot;&gt;https://www.doi.org/10.5067/GHCMC-4FM03&lt;/a&gt;). Only L2P SSTs with QL&#x3D;5 were gridded, so all valid SSTs are recommended for the users. Per GDS2 specifications, two additional Sensor-Specific Error Statistics layers (SSES bias and standard deviation) are reported in each pixel with valid SST. The ACSPO VIIRS L3U product is monitored and validated against iQuam in situ data in SQUAM. The v2.80 is an updated version from the v2.61 with several L2P algorithm improvements including two added thermal front layers, mitigated warm biases in the high latitudes, and improved clear-sky mask.
&lt;br&gt;&lt;h4 id&#x3D;&quot;viirs_npp-star-l3u-v280&quot;&gt;VIIRS_NPP-STAR-L3U-v2.80&lt;/h4&gt;
The Joint Polar Satellite System (JPSS), starting with S-NPP launched on 28 October 2011, is the new generation of the US Polar Operational Environmental Satellites (POES). The ACSPO SNPP/VIIRS L3U (Level 3 Uncollated) product is a gridded version of the ACSPO NPP/VIIRS L2P product available here &lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/VIIRS_NPP-STAR-L2P-v2.80&quot;&gt;https://podaac.jpl.nasa.gov/dataset/VIIRS_NPP-STAR-L2P-v2.80&lt;/a&gt; . The L3U output files are 10-minute granules in netCDF4 format, compliant with the Group for High Resolution Sea Surface Temperature (GHRSST) Data Specification version 2 (GDS2). There are 144 granules per 24hr interval, with a total data volume of 0.5GB/day. Fill values are reported at all invalid pixels, including pixels with &amp;gt;5 km inland. For each valid water pixel (defined as ocean, sea, lake or river, and up to 5 km inland), the following layers are reported: SSTs, a subset of l2p_flags (including day/night, land, ice, twilight, and glint flags), wind speed, and ACSPO SST minus reference (Canadian Met Centre 0.1deg L4 SST; available at &lt;a href&#x3D;&quot;https://www.doi.org/10.5067/GHCMC-4FM03&quot;&gt;https://www.doi.org/10.5067/GHCMC-4FM03&lt;/a&gt;). Only L2P SSTs with QL&#x3D;5 were gridded, so all valid SSTs are recommended for the users. Per GDS2 specifications, two additional Sensor-Specific Error Statistics layers (SSES bias and standard deviation) are reported in each pixel with valid SST. The ACSPO VIIRS L3U product is monitored and validated against iQuam in situ data in SQUAM. The v2.80 is an updated version from the v2.61 with several L2P algorithm improvements including two added thermal front layers, mitigated warm biases in the high latitudes, and improved clear-sky mask.
&lt;br&gt;&lt;h4 id&#x3D;&quot;avhrr_oi-ncei-l4-glob-v20&quot;&gt;AVHRR_OI-NCEI-L4-GLOB-v2.0&lt;/h4&gt;
A Group for High Resolution Sea Surface Temperature (GHRSST) global Level 4 sea surface temperature analysis produced daily on a 0.25 degree grid at the NOAA National Centers for Environmental Information. This product uses optimal interpolation (OI) by interpolating and extrapolating SST observations from different sources, resulting in a smoothed complete field. The sources of data are satellite (AVHRR) and in situ platforms (i.e., ships and buoys), and the specific datasets employed may change over. At the marginal ice zone, sea ice concentrations are used to generate proxy SSTs. A preliminary version of this file is produced in near-real time (1-day latency), and then replaced with a final version after 2 weeks. Note that this is the AVHRR-ONLY (AVHRR-OI), available from September 1, 1981, but there is a companion SST product that includes microwave satellite data, available from June 2002.
&lt;br&gt;&lt;h4 id&#x3D;&quot;avhrr_oi-ncei-l4-glob-v21&quot;&gt;AVHRR_OI-NCEI-L4-GLOB-v2.1&lt;/h4&gt;
A Group for High Resolution Sea Surface Temperature (GHRSST) global Level 4 sea surface temperature dataset is produced daily on a 0.25 degree grid at the NOAA National Centers for Environmental Information. This product uses optimal interpolation (OI) by interpolating and extrapolating SST observations from different sources, resulting in a smoothed complete field. The sources of data are satellite (AVHRR) and in situ platforms (i.e., ships, buoys, and Argo floats above 5m depth), and the specific datasets employed may change over time. In the regions with sea-ice concentration higher than 30%, freezing points of seawater are used to generate proxy SSTs. A preliminary version of this dataset is produced in near-real time (1-day latency), and then replaced with a final version after 2 weeks. The v2.1 (Huang et al. 2021) is updated from the previous AVHRR_OI-NCEI-L4-GLOB-v2.0 data. Major improvements include: 1) In-situ ship and buoy data changed from the NCEP Traditional Alphanumeric Codes (TAC) to the NCEI merged TAC + Binary Universal Form for the Representation (BUFR) data, with large increases of buoy data included to correct satellite SST biases; 2) Addition of Argo float observed SST data as well, for further correction of satellite SST biases; 3) Satellite input from the METOP-A and NOAA-19 to METOP-A and METOP-B, removing degraded satellite data; 4) Revised ship-buoy SST corrections for improved accuracy; and 5) Revised sea-ice-concentration to SST conversion to remove warm biases in the Arctic region. These updates only apply to data after January 1st, 2016. The data pre 2016 are still the same as v2.0 except for metadata upgrades. NCEI has panned to update the entire dataset from 1982 to fix the In-Situ data ingest and bias correction which exist prior 2016.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cmc01deg-cmc-l4-glob-v30&quot;&gt;CMC0.1deg-CMC-L4-GLOB-v3.0&lt;/h4&gt;
A Group for High Resolution Sea Surface Temperature (GHRSST) Level 4 sea surface temperature (SST) analysis produced daily on an operational basis at the Canadian Meteorological Center. This dataset merges infrared satellite SST at varying points in the time series from the Advanced Very High Resolution Radiometer (AVHRR) from NOAA-18,19, the European Meteorological Operational-A (METOP-A) and Operational-B (METOP-B), and microwave data from the Advanced Microwave Scanning Radiometer 2 (AMSR2) onboard the GCOM-W satellite in conjunction with in situ observations of SST from drifting buoys and ships from the ICOADS program. It uses the previous days analysis as the background field for the statistical interpolation used to assimilate the satellite and in situ observations. This dataset adheres to the GHRSST Data Processing Specification (GDS) version 2 format specifications.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cmc02deg-cmc-l4-glob-v20&quot;&gt;CMC0.2deg-CMC-L4-GLOB-v2.0&lt;/h4&gt;
A Group for High Resolution Sea Surface Temperature (GHRSST) Level 4 sea surface temperature (SST) analysis produced daily on an operational basis at the Canadian Meteorological Center. This dataset merges infrared satellite SST at varying points in the time series from the (A)TSR series of radiometers from ERS-1, ERS-2 and Envisat, AVHRR from NOAA-16,17,18,19 and METOP-A, and microwave data from TMI, AMSR-E and Windsat in conjunction with in situ observations of SST from drifting buoys and ships from the ICOADS program. It uses the previous days analysis as the background field for the statistical interpolation used to assimilate the satellite and in situ observations. This dataset adheres to the GHRSST Data Processing Specification (GDS) version 2 format specifications.
&lt;br&gt;&lt;h4 id&#x3D;&quot;dmi_oi-dmi-l4-glob-v10&quot;&gt;DMI_OI-DMI-L4-GLOB-v1.0&lt;/h4&gt;
A Group for High Resolution Sea Surface Temperature (GHRSST) Level 4 sea surface temperature analysis produced daily on an operational basis by the Danish Meteorological Institute (DMI) using an optimal interpolation (OI) approach on a global 0.05 degree grid. The analysis is based upon nighttime GHRSST L2P skin and subskin SST observations from several satellites. The sensors include the Advanced Very High Resolution Radiometer (AVHRR), the Spinning Enhanced Visible and Infrared Imager (SEVIRI), the Advanced Microwave Scanning Radiometer 2 (AMSR2), the Visible Infrared Imager Radiometer Suite (VIIRS), and the Moderate Resolution Imaging Spectroradiometer (MODIS) on Aqua. An ice field from the EUMETSAT OSI-SAF is used to mask out areas with ice. This dataset adheres to the version 2 GHRSST Data Processing Specification (GDS).
&lt;br&gt;&lt;h4 id&#x3D;&quot;gamssa_28km-abom-l4-glob-v01&quot;&gt;GAMSSA_28km-ABOM-L4-GLOB-v01&lt;/h4&gt;
A Group for High Resolution Sea Surface Temperature (GHRSST) Level 4 sea surface temperature analysis, produced daily on an operational basis at the Australian Bureau of Meteorology (BoM) using optimal interpolation (OI) on a global 0.25 degree grid. This Global Australian Multi-Sensor SST Analysis (GAMSSA) v1.0 system blends satellite SST observations from passive infrared and passive microwave radiometers with in situ data from ships, drifting buoys and moorings from the Global Telecommunications System (GTS). SST observations that have experienced recent surface wind speeds less than 6 m/s during the day or less than 2 m/s during night are rejected from the analysis. The processing results in daily foundation SST estimates that are largely free of nocturnal cooling and diurnal warming effects. Sea ice concentrations are supplied by the NOAA/NCEP 12.7 km sea ice analysis. In the absence of observations, the analysis relaxes to the Reynolds and Smith (1994) Monthly 1 degree SST climatology for 1961 - 1990.
&lt;br&gt;&lt;h4 id&#x3D;&quot;k10_sst-navo-l4-glob-v01&quot;&gt;K10_SST-NAVO-L4-GLOB-v01&lt;/h4&gt;
This is a Group for High Resolution Sea Surface Temperature (GHRSST) Level 4 sea surface temperature (SST) analysis dataset produced daily on an operational basis by the Naval Oceanographic Office (NAVO) on a global 0.1x0.1 degree grid. The K10 (NAVO 10-km gridded SST analyzed product) L4 analysis uses SST observations from the following instruments: Advanced Very High Resolution Radiometer (AVHRR), Visible Infrared Imaging Radiometer Suite (VIIRS), and Spinning Enhanced Visible and InfraRed Imager (SEVIRI). The AVHRR data for this comes from the MetOp-A, MetOp-B, and NOAA-19 satellites; VIIRS data is sourced from the Suomi_NPP satellite; SEVIRI data comes from the Meteosat-8 and -11 satellites. The age (time-lag), reliability, and resolution of the data are used in the weighted average with the analysis tuned to represent SST at a reference depth of 1-meter. Input data from the AVHRR Pathfinder 9km climatology dataset (1985-1999) is used when no new satellite SST retrievals are available after 34 days. Comparing with its predecessor (DOI: &lt;a href&#x3D;&quot;https://doi.org/10.5067/GHK10-L4N01&quot;&gt;https://doi.org/10.5067/GHK10-L4N01&lt;/a&gt; ), this updated dataset has no major changes in Level-4 interpolated K10 algorithm, except for using different satellite instrument data, and updating metadata and file format. The major updates include: (a) updated and enhanced the granule-level metadata information, (b) converted the SST file from GHRSST Data Specification (GDS) v1.0 to v2.0, (c) added the sea_ice_fraction variable to the product, and (d) updated the filename convention to reflect compliance with GDS v2.0.
&lt;br&gt;&lt;h4 id&#x3D;&quot;mur25-jpl-l4-glob-v042&quot;&gt;MUR25-JPL-L4-GLOB-v04.2&lt;/h4&gt;
A Group for High Resolution Sea Surface Temperature (GHRSST) Level 4 sea surface temperature analysis produced as a retrospective dataset at the JPL Physical Oceanography DAAC using wavelets as basis functions in an optimal interpolation approach on a global 0.25 degree grid. The version 4 Multiscale Ultrahigh Resolution (MUR) L4 analysis is based upon nighttime GHRSST L2P skin and subskin SST observations from several instruments including the NASA Advanced Microwave Scanning Radiometer-EOS (AMSR-E), the JAXA Advanced Microwave Scanning Radiometer 2 on GCOM-W1, the Moderate Resolution Imaging Spectroradiometers (MODIS) on the NASA Aqua and Terra platforms, the US Navy microwave WindSat radiometer, the Advanced Very High Resolution Radiometer (AVHRR) on several NOAA satellites, and in situ SST observations from the NOAA iQuam project. The ice concentration data are from the archives at the EUMETSAT Ocean and Sea Ice Satellite Application Facility (OSI SAF) High Latitude Processing Center and are also used for an improved SST parameterization for the high-latitudes. The dataset also contains an additional SST anomaly variable derived from a MUR climatology (average between 2003 and 2014). This dataset was originally funded by the NASA MEaSUREs program (&lt;a href&#x3D;&quot;http://earthdata.nasa.gov/our-community/community-data-system-programs/measures-projects&quot;&gt;http://earthdata.nasa.gov/our-community/community-data-system-programs/measures-projects&lt;/a&gt; ) and the NASA CEOS COVERAGE project and created by a team led by Dr. Toshio M. Chin from JPL. It adheres to the GHRSST Data Processing Specification (GDS) version 2 format specifications.
&lt;br&gt;&lt;h4 id&#x3D;&quot;mur-jpl-l4-glob-v41&quot;&gt;MUR-JPL-L4-GLOB-v4.1&lt;/h4&gt;
A Group for High Resolution Sea Surface Temperature (GHRSST) Level 4 sea surface temperature analysis produced as a retrospective dataset (four day latency) and near-real-time dataset (one day latency) at the JPL Physical Oceanography DAAC using wavelets as basis functions in an optimal interpolation approach on a global 0.01 degree grid. The version 4 Multiscale Ultrahigh Resolution (MUR) L4 analysis is based upon nighttime GHRSST L2P skin and subskin SST observations from several instruments including the NASA Advanced Microwave Scanning Radiometer-EOS (AMSR-E), the JAXA Advanced Microwave Scanning Radiometer 2 on GCOM-W1, the Moderate Resolution Imaging Spectroradiometers (MODIS) on the NASA Aqua and Terra platforms, the US Navy microwave WindSat radiometer, the Advanced Very High Resolution Radiometer (AVHRR) on several NOAA satellites, and in situ SST observations from the NOAA iQuam project. The ice concentration data are from the archives at the EUMETSAT Ocean and Sea Ice Satellite Application Facility (OSI SAF) High Latitude Processing Center and are also used for an improved SST parameterization for the high-latitudes. The dataset also contains additional variables for some granules including the SST anomaly (variable sst_anomaly) derived from a MUR climatology, and the temporal distance in hours to the nearest IR measurement for each pixel (variable dt_1km_data). Variable dt_1km_data first appears in the time series on October 4, 2015, while sst_anomaly starts July 23, 2019. This dataset was originally funded by the NASA MEaSUREs program (&lt;a href&#x3D;&quot;http://earthdata.nasa.gov/our-community/community-data-system-programs/measures-projects&quot;&gt;http://earthdata.nasa.gov/our-community/community-data-system-programs/measures-projects&lt;/a&gt;), and created by a team led by Dr. Toshio M. Chin from JPL. It adheres to the GHRSST Data Processing Specification (GDS) version 2 format specifications. Use the file global metadata &amp;quot;history:&amp;quot; attribute to determine if a granule is near-realtime or retrospective.
&lt;br&gt;&lt;h4 id&#x3D;&quot;mw_ir_oi-remss-l4-glob-v50&quot;&gt;MW_IR_OI-REMSS-L4-GLOB-v5.0&lt;/h4&gt;
A Group for High Resolution Sea Surface Temperature (GHRSST) global Level 4 sea surface temperature analysis produced daily on a 0.09-degree grid at Remote Sensing Systems. This product uses optimal interpolation (OI) from both microwave (MW) sensors including the Global Precipitation Measurement (GPM) Microwave Imager (GMI), the Tropical Rainfall Measuring Mission (TRMM) Microwave Imager (TMI), the NASA Advanced Microwave Scanning Radiometer-EOS (AMSRE), the Advanced Microwave Scanning Radiometer 2 (AMSR2) onboard the GCOM-W1 satellite, and WindSat operates on the Coriolis satellite, and infrared (IR) sensors such as the Moderate Resolution Imaging Spectroradiometer (MODIS) on the NASA Aqua and Terra platform and the Visible Infrared Imaging Radiometer Suite (VIIRS) on board the Suomi-NPP satellite. The through-cloud capabilities of microwave radiometers provide a valuable picture of global sea surface temperature (SST) while infrared radiometers (i.e., MODIS) have a higher spatial resolution. This analysis does not use any in situ SST data such as drifting buoy SST. Comparing with previous version 4.0 dataset, the version 5.0 has made the updates in several areas, including the diurnal warming model, the sensor-specific error statistics (SSES) for each microwave sensor, the sensor correlation model, and the quality mask.
&lt;br&gt;&lt;h4 id&#x3D;&quot;mw_ir_oi-remss-l4-glob-v51&quot;&gt;MW_IR_OI-REMSS-L4-GLOB-v5.1&lt;/h4&gt;
A Group for High Resolution Sea Surface Temperature (GHRSST) global Level 4 sea surface temperature analysis produced daily on a 0.09-degree grid at Remote Sensing Systems. This product uses optimal interpolation (OI) from microwave (MW) sensors including the Tropical Rainfall Measuring Mission (TRMM) Microwave Imager (TMI), the NASA Advanced Microwave Scanning Radiometer-EOS (AMSR-E), the WindSat on the Coriolis satellite, the Global Precipitation Measurement (GPM) Microwave Imager (GMI), and the Advanced Microwave Scanning Radiometer 2 (AMSR2) onboard the GCOM-W1 satellite, as well as infrared (IR) sensors such as the Moderate Resolution Imaging Spectroradiometer (MODIS) on the NASA Aqua and Terra platforms and the Visible Infrared Imaging Radiometer Suite (VIIRS) on board the Suomi-NPP and NOAA-20 satellites. These MW sensors are used through the SST production based on the sensor data availability. The through-cloud capabilities of microwave radiometers provide a valuable picture of global sea surface temperature (SST) while infrared radiometers (i.e., MODIS) have a higher spatial resolution. This analysis does not use any in situ SST data such as drifting buoy SST. Compared with the previous version 5.0 dataset, version 5.1 is processed using updated input files, VIIRS on NOAA-20 is included, the sensor-specific error statistics (SSES) for each microwave sensor are updated, and deficiencies in the OI processing have been addressed.
&lt;br&gt;&lt;h4 id&#x3D;&quot;mw_oi-remss-l4-glob-v50&quot;&gt;MW_OI-REMSS-L4-GLOB-v5.0&lt;/h4&gt;
A Group for High Resolution Sea Surface Temperature (GHRSST) global Level 4 sea surface temperature analysis produced daily on a 0.25-degree grid at Remote Sensing Systems. This product uses optimal interpolation (OI) from microwave (MW) sensors including the Global Precipitation Measurement (GPM) Microwave Imager (GMI), the Tropical Rainfall Measuring Mission (TRMM) Microwave Imager (TMI), the NASA Advanced Microwave Scanning Radiometer-EOS (AMSRE), the Advanced Microwave Scanning Radiometer 2 (AMSR2) onboard the GCOM-W1 satellite, and WindSat operates on the Coriolis satellite. The through-cloud capabilities of microwave radiometers provide a valuable picture of global sea surface temperature (SST). This analysis does not use any in situ SST data such as drifting buoy SST. Comparing with previous version 4.0 dataset, the version 5.0 has made the updates in several areas, including the diurnal warming model, the sensor-specific error statistics (SSES) for each microwave sensor, the sensor correlation model, and the quality mask.
&lt;br&gt;&lt;h4 id&#x3D;&quot;mw_oi-remss-l4-glob-v51&quot;&gt;MW_OI-REMSS-L4-GLOB-v5.1&lt;/h4&gt;
A Group for High Resolution Sea Surface Temperature (GHRSST) global Level 4 sea surface temperature analysis produced daily on a 0.25-degree grid at Remote Sensing Systems. This product uses optimal interpolation (OI) from microwave (MW) sensors including the Tropical Rainfall Measuring Mission (TRMM) Microwave Imager (TMI), the NASA Advanced Microwave Scanning Radiometer-EOS (AMSR-E), the WindSat on the Coriolis satellite, the Global Precipitation Measurement (GPM) Microwave Imager (GMI), and the Advanced Microwave Scanning Radiometer 2 (AMSR2) onboard the GCOM-W1 satellite. These MW sensors are used through the SST production based on the sensor data availability. The through-cloud capabilities of microwave radiometers provide a valuable picture of global sea surface temperature (SST). This analysis does not use any in situ SST data such as drifting buoy SST. Compared with the previous version 5.0 dataset, version 5.1 is processed using updated input files, the sensor-specific error statistics (SSES) for each microwave sensor are updated, and deficiencies in the OI processing have been addressed.
&lt;br&gt;&lt;h4 id&#x3D;&quot;geo_polar_blended-ospo-l4-glob-v10&quot;&gt;Geo_Polar_Blended-OSPO-L4-GLOB-v1.0&lt;/h4&gt;
A Group for High Resolution Sea Surface Temperature (GHRSST) Level 4 sea surface temperature analysis produced daily on an operational basis at the Office of Satellite and Product Operations (OSPO) using optimal interpolation (OI) on a global 0.054 degree grid. The Geo-Polar Blended Sea Surface Temperature (SST) Analysis combines multi-satellite retrievals of sea surface temperature into a single analysis of SST. This analysis uses both daytime and nighttime data from sensors that include the Advanced Very High Resolution Radiometer (AVHRR), the Visible Infrared Imager Radiometer Suite (VIIRS), the Geostationary Operational Environmental Satellite (GOES) imager, the Japanese Advanced Meteorological Imager (JAMI) and in situ data from ships, drifting and moored buoys. This analysis was specifically produced to be used as a lower boundary condition in Numerical Weather Prediction (NWP) models. This dataset adheres to the GHRSST Data Processing Specification (GDS) version 2 format specifications.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ostia-ukmo-l4-glob-v20&quot;&gt;OSTIA-UKMO-L4-GLOB-v2.0&lt;/h4&gt;
A Group for High Resolution Sea Surface Temperature (GHRSST) Level 4 sea surface temperature analysis produced daily on an operational basis at the UK Met Office using optimal interpolation (OI) on a global 0.05x0.05 degree grid. The Operational Sea Surface Temperature and Sea Ice Analysis (OSTIA) analysis uses satellite data from over 10 unique sensors that include the Advanced Very High Resolution Radiometer (AVHRR), the Spinning Enhanced Visible and Infrared Imager (SEVIRI), the Geostationary Operational Environmental Satellite (GOES) imager, the Infrared Atmospheric Sounding Interferometer (IASI), the Tropical Rainfall Measuring Mission Microwave Imager (TMI) and in situ data from ships, drifting and moored buoys. This analysis was specifically produced to be used as a lower boundary condition in Numerical Weather Prediction (NWP) models. This dataset adheres to the GHRSST Data Processing Specification (GDS) version 2 format specifications and is updated daily with 24-hours nominal latency in a Near Real Time (NRT) mode. UKMO also produces the higher quality reprocessed OSTIA L4 SST using more sensors and data with a biannual latency (&lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/OSTIA-UKMO-L4-GLOB-REP-v2.0&quot;&gt;https://podaac.jpl.nasa.gov/dataset/OSTIA-UKMO-L4-GLOB-REP-v2.0&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;ostia-ukmo-l4-glob-rep-v20&quot;&gt;OSTIA-UKMO-L4-GLOB-REP-v2.0&lt;/h4&gt;
The Operational Sea Surface Temperature and Sea Ice Analysis Reprocessed (OSTIA-REP) is a GHRSST reprocessed Level-4 sea surface temperature and ice-concentration analysis produced by the UK Met Office (UKMO) using optimal interpolation (OI) on a global 0.05 degree grid. It is a sister product of the Near Real Time version (OSTIA-NRT), but incorporates satellite data from over 25 different SST sensors as well as in situ data from drifting and moored buoys. The OSTIA-REP is produced on a biannual frequency when more satellite and climatology observations are available from existing geostationary IR, and polar orbiting IR and MW satellites in addition to the data used in OSTIA-NRT. &lt;br&gt;&lt;br&gt; While OSTIA-NRT is produced to mainly serve as a lower boundary condition in Numerical Weather Prediction (NWP) models, this OSTIA-REP aims to provide a more accurate and consistent record of SST measurements over time, which is crucial for detecting long-term climate trends and variability. Both versions follow GHRSST Data Processing Specification (GDS) version 2 format guidelines.&lt;br&gt;&lt;br&gt; Data to June 2022 are also distributed through the E.U. Copernicus Marine Service Information (&lt;a href&#x3D;&quot;https://marine.copernicus.eu/&quot;&gt;https://marine.copernicus.eu/&lt;/a&gt;, DOI: &lt;a href&#x3D;&quot;https://doi.org/10.48670/moi-00168&quot;&gt;https://doi.org/10.48670/moi-00168&lt;/a&gt; with the following license). Please refer to the user guide for more information.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ramssa_09km-abom-l4-aus-v01&quot;&gt;RAMSSA_09km-ABOM-L4-AUS-v01&lt;/h4&gt;
A Group for High Resolution Sea Surface Temperature (GHRSST) Level 4 sea surface temperature analysis, produced daily on an operational basis at the Australian Bureau of Meteorology (BoM) using optimal interpolation (OI) on a regional 1/12 degree grid over the Australian region (20N - 70S, 60E - 170W). This Regional Australian Multi-Sensor SST Analysis (RAMSSA) v1.0 system blends satellite SST observations from passive infrared and passive microwave radiometers, with in situ data from ships, Argo floats, XBTs, CTDs, drifting buoys and moorings from the Global Telecommunications System (GTS). SST observations that have experienced recent surface wind speeds less than 6 m/s during the day or less than 2 m/s during night are rejected from the analysis. The processing results in daily foundation SST estimates that are largely free of nocturnal cooling and diurnal warming effects. Sea ice concentrations are supplied by the NOAA/NCEP 12.7 km sea ice analysis. In the absence of observations, the analysis relaxes to the BoM Global Weekly 1 degree OI SST analysis, which relaxes to the Reynolds and Smith (1994) Monthly 1 degree SST climatology for 1961 - 1990.
&lt;br&gt;&lt;h4 id&#x3D;&quot;remo_oi_sst_5km-ufrj-l4-samerica-v10&quot;&gt;REMO_OI_SST_5km-UFRJ-L4-SAMERICA-v1.0&lt;/h4&gt;
A Group for High Resolution Sea Surface Temperature (GHRSST) Level 4 sea surface temperature (SST) analysis produced daily on an operational basis by the Oceanographic Modeling and Observation Network (REMO) at Applied Meteorology Laboratory/Federal University of Rio de Janeiro (LMA/UFRJ) using the Barnes sub optimal interpolation (OI) technique on a regional 0.05 degree grid. REMO uses Advanced Very High Resolution Radiometer (AVHRR) data from National Oceanic and Atmospheric Administration (NOAA) satellites series (NOAA 15, NOAA 16, NOAA 17, NOAA 18 and NOAA 19) and Microwave Imager (TMI) data from Tropical Rainfall Measuring Mission (TRMM) which is a joint mission between NASA and the Japan Aerospace Exploration Agency (JAXA) to generate 0.05 degree daily cloud free blended (infrared and microwave) SST products (approximately 5.5 km). The data lies between latitudes 45 S and 15 N and longitudes 70 W and 15 W region and are fully validated by in situ measurements from eleven buoys of Prediction and Research Moored Array in the Tropical Atlantic (PIRATA).AVHRR is a scanning radiometer capable of detecting energy from land, ocean and atmosphere. It operates with six spectral bands arranged in the regions of visible and infrared region. TRMM was launched in December, 1997, having an orbital inclination of 53 degree and altitude 350 km, an equatorial orbit that ranges from 40 N to 40 S and a spatial resolution of 0.25 degree (&amp;#8764;27.75 km). Although infrared AVHRR SST data have high spatial resolution, they are contaminated by cloud cover and aerosols, while lower resolution microvwave TMI data are barely influenced by these.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sport-msfc-l4-glob-v10&quot;&gt;SPORT-MSFC-L4-GLOB-v1.0&lt;/h4&gt;
The GHRSST Level 4 SPoRT Global Foundation Sea Surface Temperature Analysis (v1.0) dataset is produced by the by the NASA Short-term Prediction Research and Transition (SPoRT) project to provide continuous high-resolution composited near global (80N – 80S) sea surface temperature fields twice daily at 2 km resolution for regional weather, maritime, and coastal applications. &lt;br&gt;&lt;br&gt; It was originally a regional L4 dataset based on MODIS Aqua/Terra Level 2 SST inputs. Currently, the SPoRT SST analysis composites seven-days of Visible Infrared Imaging Radiometer Suite (VIIRS) and Advanced Very High Resolution Radiometer (AVHRR) satellite L2 SST data, with additional data from OSTIA and Geo-Polar Blended L4 SST products into a single analysis. Two types of weighting are used in the compositing process. One weight is for the data latency and the other for the product type and spatial resolution. The VIIRS and AVHRR data, being at 750m and 1km resolution respectively, are given the most weight, while the L4 datasets are given weaker weights. &lt;br&gt;&lt;br&gt; This SPoRT SST dataset adheres to the GHRSST Data Specification (GDS) version 2 format specifications with full netCDF-4 and metadata compliance. The SPoRT project is funded by NASA and the data produced at the NASA Marshall Space Flight Center.
&lt;br&gt;&lt;h4 id&#x3D;&quot;l3s_leo_am-star-v280&quot;&gt;L3S_LEO_AM-STAR-v2.80&lt;/h4&gt;
NOAA STAR produces two lines of gridded 0.02 degree super-collated L3S LEO sub-skin Sea Surface Temperature (SST) datasets, one from the NOAA afternoon JPSS (L3S_LEO_PM) satellites and the other from the EUMETSAT mid-morning Metop (L3S_LEO_AM) satellites. The L3S_LEO_AM is derived from three Low Earth Orbiting (LEO) Metop-FG satellites: Metop-A, -B and -C . The Metop-FG satellite program was jointly established by the European Space Agency (ESA) and the European Organization for the Exploitation of Meteorological Satellites (EUMETSAT). The US National Oceanic and Atmospheric Administration (NOAA) under the joint NOAA/EUMETSAT Initial Joint Polar System Agreement, has contributed three Advanced Very High Resolution Radiometer (AVHRR) sensors capable of collecting and transmitting data in the Full Resolution Area Coverage (FRAC; 1km/nadir) format. The L3S_LEO_AM dataset is produced by aggregating three L3U datasets from MetOp-FG satellites (MetOp-A, -B and -C; all hosted in PO.DAAC) and covers from Dec 2006-present. The L3S_LEO_AM SST dataset is reported in two files per 24-hour interval, daytime and nighttime (nominal Metop local equator crossing times around 09:30/21:30, respectively), in NetCDF4 format, compliant with the GHRSST Data Specification version 2 (GDS2). The Near Real Time (NRT) L3S-LEO data are archived at PO.DAAC with approximately 6 hours latency, and then replaced by the Re-ANalysis (RAN) files about 2 months later, with identical file names. The dataset is validated against quality controlled in situ data, provided by the NOAA in situ SST Quality Monitor system (iQuam; Xu and Ignatov, 2014), and monitored in another NOAA system, SST Quality Monitor (SQUAM; Dash et al, 2010). The L3S SST imagery and local coverage are continuously evaluated, and checked for consistency with other Level 2, 3 and 4 datasets in the ACSPO Regional Monitor for SST (ARMS) system. NOAA plans to include data from other mid-morning platforms and sensors, such as MetOp-SG METImage and Terra MODIS, into L3S_LEO_AM. More information about the dataset can be found under the Documentation and Citation tabs.
&lt;br&gt;&lt;h4 id&#x3D;&quot;l3s_leo_dy-star-v281&quot;&gt;L3S_LEO_DY-STAR-v2.81&lt;/h4&gt;
The L3S_LEO_DY-STAR-v2.81 dataset produced by the NOAA Advanced Clear-Sky Processor for Ocean (ACSPO) system derives the Subskin Sea Surface Temperature (SST) from multiple instruments, including the VIIRS onboard the Suomi-NPP, NOAA-20 and NOAA-21 satellites, AVHRR onboard Metop-A, B , C satellites and MODIS onboard the Terra and Aqua satellites. The L3S-LEO is a family of multi-sensor super-collated (L3S) gridded 0.02º resolution SST products from low earth orbit (LEO) satellites. The L3S-LEO PM ( &lt;a href&#x3D;&quot;https://doi.org/10.5067/GHLPM-3S281&quot;&gt;https://doi.org/10.5067/GHLPM-3S281&lt;/a&gt; ) and AM ( &lt;a href&#x3D;&quot;https://doi.org/10.5067/GHLAM-3SS28&quot;&gt;https://doi.org/10.5067/GHLAM-3SS28&lt;/a&gt; ) data include SSTs from afternoon (&lt;del&gt;1:30 am/pm) and mid-morning (&lt;/del&gt;9:30 am/pm) satellites, respectively. The PM and AM SSTs, for both day (D) and night (N), and Terra MODIS SSTs, are further aggregated into a daily L3S-LEO-DY SST product. &lt;br&gt;&lt;br&gt; The L3S-DY-SST combines the both L3S-LEO-PM/AM SSTs into a single daily product. It covers from 2000-02-24 to present and is reported in one file per 24h interval. Data are in NetCDF4 format, compliant with the GHRSST Data Specification version 2 (GDS2). The v2.81 succeeds the v2.80 dataset (not available from the PO.DAAC) with the following improvements: (1) The L3S-LEO-PM input was updated from v2.80 to v2.81; and (2) ACSPO Terra MODIS SST is included from 2000-02-24 to 2021-12-31. The inclusion of Terra extends the availability of L3S-LEO-DY back to 2000-02-24 (from 2006-12-01 in v2.80). The SST diurnal warming effects from different daily observation times across the series of instruments have been corrected and are described in the publications by Jonasson et al., 2022 &lt;br&gt;&lt;br&gt; The Near Real Time (NRT) data are available with 6h latency, and replaced by the Re-ANalysis (RAN) files in 2 months, with identical file names. They can be differentiated by the file creation time and ancillary inputs. The data are validated against quality controlled in situ data from the NOAA in situ SST Quality Monitor (iQuam; &lt;a href&#x3D;&quot;https://www.star.nesdis.noaa.gov/socd/sst/iquam&quot;&gt;https://www.star.nesdis.noaa.gov/socd/sst/iquam&lt;/a&gt;), and monitored in another NOAA system, SST Quality Monitor (SQUAM; &lt;a href&#x3D;&quot;https://www.star.nesdis.noaa.gov/socd/sst/squam&quot;&gt;https://www.star.nesdis.noaa.gov/socd/sst/squam&lt;/a&gt;)
&lt;br&gt;&lt;h4 id&#x3D;&quot;l3s_leo_pm-star-v281&quot;&gt;L3S_LEO_PM-STAR-v2.81&lt;/h4&gt;
The L3S_LEO_PM-STAR-v2.81 dataset produced by the NOAA Advanced Clear-Sky Processor for Ocean (ACSPO) system derives the Subskin Sea Surface Temperature (SST) from the VIIRSs (Visible Infrared Imaging Radiometer Suite) onboard the Suomi-NPP, NOAA-20 and NOAA-21 satellites and MODIS (Moderate Resolution Imaging Spectroradiometer) onboard the Aqua satellite. The L3S-LEO is a family of multi-sensor super-collated (L3S) gridded 0.02º resolution SST products from low earth orbit (LEO) satellites. The L3S-LEO-PM ( &lt;a href&#x3D;&quot;https://doi.org/10.5067/GHLPM-3S281&quot;&gt;https://doi.org/10.5067/GHLPM-3S281&lt;/a&gt; ) and AM ( &lt;a href&#x3D;&quot;https://doi.org/10.5067/GHLAM-3SS28&quot;&gt;https://doi.org/10.5067/GHLAM-3SS28&lt;/a&gt; ) data include SSTs from afternoon (&lt;del&gt;1:30 am/pm) and mid-morning (&lt;/del&gt;9:30 am/pm) satellites, respectively. The PM and AM SSTs, for both day (D) and night (N), and Terra MODIS SSTs, are further aggregated into a daily L3S-LEO-DY SST product ( &lt;a href&#x3D;&quot;https://doi.org/10.5067/GHLDY-3S281&quot;&gt;https://doi.org/10.5067/GHLDY-3S281&lt;/a&gt; ). &lt;br&gt;&lt;br&gt; This PM SST product is derived by collating individual satellite ACSPO L3U data ( &lt;a href&#x3D;&quot;https://doi.org/10.5067/GHVRS-3UO61&quot;&gt;https://doi.org/10.5067/GHVRS-3UO61&lt;/a&gt;, &lt;a href&#x3D;&quot;https://doi.org/10.5067/GHV20-3UO61&quot;&gt;https://doi.org/10.5067/GHV20-3UO61&lt;/a&gt; and &lt;a href&#x3D;&quot;https://doi.org/10.5067/GHN21-3U280&quot;&gt;https://doi.org/10.5067/GHN21-3U280&lt;/a&gt; ). It covers from 2002-07-04 to present and is reported in 2 files daily, day and night, at 1:30am/pm local time. The SST is in NetCDF4 format, compliant with the GHRSST Data Specification version 2 (GDS2). The v2.81 is updated from the previous v2.80 ( &lt;a href&#x3D;&quot;https://doi.org/10.5067/GHLPM-3SS28&quot;&gt;https://doi.org/10.5067/GHLPM-3SS28&lt;/a&gt; ): (1) v2.81 includes 3 VIIRSs (NPP, N20, and N21 from 2023-03-19 - on); (2) Aqua MODIS SST included from 2002-07-04 to 2022-12-31; (3) Time series in v2.81 extended back to 2002-07-04 (from 2012-02-01 in v2.80); (4) recently uncovered VIIRS daytime SST drifts in NPP and N20 SSTs of approximately -0.1 K/decade mitigated. &lt;br&gt;&lt;br&gt; The Near Real Time (NRT) data are available with 6h latency, and replaced by the Re-ANalysis (RAN) files in 2 months, with identical file names. They can be differentiated by the file creation time and ancillary inputs. The data are validated against quality controlled in situ data from the NOAA in situ SST Quality Monitor (iQuam; &lt;a href&#x3D;&quot;https://www.star.nesdis.noaa.gov/socd/sst/iquam&quot;&gt;https://www.star.nesdis.noaa.gov/socd/sst/iquam&lt;/a&gt;), and monitored in another NOAA system, SST Quality Monitor (SQUAM; &lt;a href&#x3D;&quot;https://www.star.nesdis.noaa.gov/socd/sst/squam&quot;&gt;https://www.star.nesdis.noaa.gov/socd/sst/squam&lt;/a&gt;)
&lt;br&gt;&lt;h4 id&#x3D;&quot;abi_g16-star-l3c-v270&quot;&gt;ABI_G16-STAR-L3C-v2.70&lt;/h4&gt;
The ACSPO G16/ABI L3C (Level 3 Collated) product is a gridded version of the ACSPO G16/ABI L2P product available at &lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/ABI_G16-STAR-L2P-v2.70&quot;&gt;https://podaac.jpl.nasa.gov/dataset/ABI_G16-STAR-L2P-v2.70&lt;/a&gt;. The L3C output files are 1hr granules in netCDF4 format, compliant with the GHRSST Data Specification version 2 (GDS2). There are 24 granules per 24hr interval, with a total data volume of 0.2GB/day. Fill values are reported at all invalid pixels, including pixels with 5 km inland. For each valid water pixel (defined as ocean, sea, lake or river, and up to 5 km inland), the following layers are reported: SSTs, ACSPO clear-sky mask (ACSM; provided in each grid as part of l2p_flags, which also includes day/night, land, ice, twilight, and glint flags), NCEP wind speed, and ACSPO SST minus reference (Canadian Met Centre 0.1deg L4 SST; available at &lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/CMC0.1deg-CMC-L4-GLOB-v3.0&quot;&gt;https://podaac.jpl.nasa.gov/dataset/CMC0.1deg-CMC-L4-GLOB-v3.0&lt;/a&gt;). All valid SSTs in L3C are recommended for users. Per GDS2 specifications, two additional Sensor-Specific Error Statistics layers (SSES bias and standard deviation) are reported in each pixel with valid SST. The ACSPO VIIRS L3U product is monitored and validated against iQuam in situ data (Xu and Ignatov, 2014) in SQUAM (Dash et al, 2010).
&lt;br&gt;&lt;h4 id&#x3D;&quot;abi_g16-star-l2p-v270&quot;&gt;ABI_G16-STAR-L2P-v2.70&lt;/h4&gt;
GOES-16 (G16) is the first satellite in the US NOAA third generation of Geostationary Operational Environmental Satellites (GOES), a.k.a. GOES-R series (which will also include -S, -T, and -U). G16 was launched on 19 Nov 2016 and initially placed in an interim position at 89.5-deg W, between GOES-East and -West. Upon completion of Cal/Val in Dec 2018, it was moved to its permanent position at 75.2-deg W, and declared NOAA operational GOES-East on 18 Dec 2018. NOAA is responsible for all GOES-R products, including Sea Surface Temperature (SST) from the Advanced Baseline Imager (ABI). The ABI offers vastly enhanced capabilities for SST retrievals, over the heritage GOES-I/P Imager, including five narrow bands (centered at 3.9, 8.4, 10.3, 11.2, and 12.3 um) out of 16 that can be used for SST, as well as accurate sensor calibration, image navigation and co-registration, spectral fidelity, and sophisticated pre-processing (geo-rectification, radiance equalization, and mapping). From altitude 35,800 km, G16/ABI can accurately map SST in a Full Disk (FD) area from 15-135-deg W and 60S-60N, with spatial resolution 2km at nadir (degrading to 15km at view zenith angle, 67-deg) and temporal sampling of 10min (15min prior to 2 Apr 2019). The Level 2 Preprocessed (L2P) SST product is derived at the native sensor resolution using NOAA Advanced Clear-Sky Processor for Ocean (ACSPO) system. ACSPO first processes every 10min FD data SSTs are derived from BTs using the ACSPO clear-sky mask (ACSM; Petrenko et al., 2010) and Non-Linear SST (NLSST) algorithm (Petrenko et al., 2014). Currently, only 4 longwave bands centered at 8.4, 10.3, 11.2, and 12.3 um are used (the 3.9 microns was initially excluded, to minimize possible discontinuities in the diurnal cycle). The regression is tuned against quality controlled in situ SSTs from drifting and tropical mooring buoys in the NOAA iQuam system (Xu and Ignatov, 2014). The 10-min FD data are subsequently collated in time, to produce 1-hr L2P product, with improved coverage, and reduced cloud leakages and image noise, compared to each individual 10min image. In the collated L2P, SSTs and BTs are only reported in clear-sky water pixels (defined as ocean, sea, lake or river, and up to 5 km inland) and fill values elsewhere. The L2P is reported in netCDF4 GHRSST Data Specification version 2 (GDS2) format, 24 granules per day, with a total data volume of 0.6GB/day. In addition to SST, ACSPO files also include sun-sensor geometry, four BTs in ABI bands 11 (8.4um), 13 (10.3um), 14 (11.2um), and 15 (12.3um) and two reflectances in bands 2 and 3 (0.64um and 0.86um; used for cloud identification). The l2p_flags layer includes day/night, land, ice, twilight, and glint flags. Other variables include NCEP wind speed and ACSPO SST minus reference SST (Canadian Met Centre 0.1deg L4 SST; available at &lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/CMC0.1deg-CMC-L4-GLOB-v3.0&quot;&gt;https://podaac.jpl.nasa.gov/dataset/CMC0.1deg-CMC-L4-GLOB-v3.0&lt;/a&gt;). Pixel-level earth locations are not reported in the granules, as they remain unchanged from granule to granule. To obtain those, user has a choice of using a flat lat-lon file, or a Python script, both available at &lt;a href&#x3D;&quot;ftp://ftp.star.nesdis.noaa.gov/pub/socd4/coastwatch/sst/nrt/abi/nav/&quot;&gt;ftp://ftp.star.nesdis.noaa.gov/pub/socd4/coastwatch/sst/nrt/abi/nav/&lt;/a&gt;. Per GDS2 specifications, two additional Sensor-Specific Error Statistics layers (SSES bias and standard deviation) are reported in each pixel. The ACSPO VIIRS L2P product is monitored and validated against in situ data (Xu and Ignatov, 2014) using the Satellite Quality Monitor SQUAM (Dash et al, 2010), and BTs are validated against RTM simulation in MICROS (Liang and Ignatov, 2011). A reduced size (0.2GB/day), equal-angle gridded (0.02-deg resolution), ACSPO L3C product is also available at &lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/ABI_G16-STAR-L3C-v2.70&quot;&gt;https://podaac.jpl.nasa.gov/dataset/ABI_G16-STAR-L3C-v2.70&lt;/a&gt;, where gridded L2P SSTs are reported, and BT layers omitted.
&lt;br&gt;&lt;h4 id&#x3D;&quot;abi_g17-star-l3c-v271&quot;&gt;ABI_G17-STAR-L3C-v2.71&lt;/h4&gt;
The ACSPO G17/ABI L3C (Level 3 Collated) product is a gridded version of the ACSPO G17/ABI L2P product available at &lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/ABI_G17-STAR-L2P-v2.71&quot;&gt;https://podaac.jpl.nasa.gov/dataset/ABI_G17-STAR-L2P-v2.71&lt;/a&gt;. The L3C output files are 1hr granules in NetCDF4 format, compliant with the GHRSST Data Specification version 2 (GDS2). Due to the loop heat pipe (LHP) issue on G17 ABI, there are only 13 granules available per 24hr interval, from 20UTC to 08UTC, followed by a break from 09UTC to 19UTC, with a total data volume of 0.1GB/day. Valid SSTs are found over oceans, sea, lakes or rivers, with fill values reported elsewhere. The following additional layers are also reported: SST, ACSPO clear-sky mask (ACSM; provided in each grid as part of l2p_flags, which also includes day/night, land, ice, twilight, and glint flags), NCEP wind speed and ACSPO SST minus reference (Canadian Met Centre 0.1deg L4 SST; available at &lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/CMC0.1deg-CMC-L4-GLOB-v3.0&quot;&gt;https://podaac.jpl.nasa.gov/dataset/CMC0.1deg-CMC-L4-GLOB-v3.0&lt;/a&gt; ). All valid SSTs in L3C are recommended for users, although data over internal waters may not have enough in situ data to be adequately validated. Per GDS2 specifications, two additional Sensor-Specific Error Statistics layers (bias and standard deviation) are reported in each pixel with valid SST. The ACSPO VIIRS L3U product is monitored and validated against iQuam in situ data (Xu and Ignatov, 2014) in SQUAM (Dash et al, 2010).
&lt;br&gt;&lt;h4 id&#x3D;&quot;abi_g17-star-l2p-v271&quot;&gt;ABI_G17-STAR-L2P-v2.71&lt;/h4&gt;
GOES-17 (G17) is the second satellite in the US NOAA&amp;#39;s GOES-R series. It was launched on 1 Mar 2018 in an interim position at 89.5-deg W for initial Cal/Val, moved to its nominal position at 137.2-deg W in Nov 2018, and declared NOAA operational GOES-West satellite on 12 Feb 2019. Advanced Baseline Imager (ABI) is a 16 channel sensor, of which five (3.9, 8.4, 10.3, 11.2, 12.3 um) are suitable for SST. From altitude 35,800km, G17/ABI maps SST in a Full Disk (FD) area from 163E-77W and 60S-60N, with spatial resolution 2km/nadir to 15km/VZA 67-deg, and 10-min temporal sampling. The ABI L2P SST is derived at the native sensor resolution using NOAA ACSPO system. ACSPO processes every 10-min FD, identifies good-quality ocean pixels (Petrenko et al., 2010) and derives SST using Non-Linear SST (NLSST) algorithm (Petrenko et al., 2014). Unfortunately, the G17 ABI loop heat pipe (LHP) that should maintain the ABI at its intended temperature, is not operating at its designed capacity, which required mitigations to the ACSPO algorithms and releasing an updated ACSPO version 2.71 (Pennybacker et al, 2019). In particular, band 11.2um, most subject to calibration problems, is not used leading to a 3-band (8.4, 10.3, and 12.3um) NLSST, and increased calibration problems prevent SST retrievals at night. As a result, the G17 SST is only reported for 13 out of 24hrs/day, from 20UTC to 08UTC. The 10-min FD data are subsequently collated in time, to produce 1-hr product, with improved coverage and reduced cloud leakages and image noise. The collation algorithm also reduces G17 excessive sensor noise and striping to levels similar to G16. The collated SSTs are only reported over clear-sky water pixels. All pixels with valid SSTs are recommended for use. The L2P is reported in NetCDF4 GDS2 format, 13 granules per day, with a total data volume 0.3GB/day. ACSPO files also report sun-sensor geometry, wind speed and l2p_flags (day/night, land, ice, twilight, glint flags). Per GDS2 specifications, two Sensor-Specific Error Statistics (bias and standard deviation) are reported in each pixel (Petrenko et al., 2016). Pixel earth locations are not reported in the granules, as they remain unchanged from granule to granule. Those can be obtained using a flat lat/lon file or a Python script (see Documentation page). The ACSPO G17 ABI SSTs are continuously validated in SQUAM (Dash et al, 2010). A reduced size (0.1GB/day), 0.02-deg equal-angle gridded L3C product is available at &lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/ABI_G17-STAR-L3C-v2.71&quot;&gt;https://podaac.jpl.nasa.gov/dataset/ABI_G17-STAR-L3C-v2.71&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ahi_h08-star-l2p-v270&quot;&gt;AHI_H08-STAR-L2P-v2.70&lt;/h4&gt;
Himawari-8 (H08) was launched on 7 October 2014 into its nominal position at 140.7-deg E, and declared operational on 7 July 2015. The Advanced Himawari Imager (AHI; largely identical to GOES-R/ABI) is a 16 channel sensor, of which five (3.9, 8.4, 10.3, 11.2, and 12.3 um) are suitable for SST. Accurate sensor calibration, image navigation and (co)registration, high spectral fidelity, and sophisticated pre-processing (geo-rectification, radiance equalization, and mapping) offer vastly enhanced capabilities for SST retrievals, over the heritage GOES-I/P and MTSAT-2 Imagers. From altitude 35,800km, H08/AHI maps SST in a Full Disk (FD) area from 80E-160W and 60S-60N, with spatial resolution 2km at nadir to 15km at view zenith angle 67-deg, with a 10-min temporal sampling. The AHI L2P (swath) SST product is derived at the native sensor resolution using NOAA&amp;#39;s Advanced Clear-Sky Processor for Ocean (ACSPO) system. ACSPO processes every 10-min FD data, identifies good quality ocean pixels (Petrenko et al., 2010) and derives SST using the four-band (8.4, 10.3, 11.2 and 12.3um) Non-Linear SST (NLSST) regression algorithm (Petrenko et al., 2014), trained against in situ SSTs from drifting and tropical mooring buoys in the NOAA iQuam system (Xu and Ignatov, 2014). The 10-min data are subsequently collated in time, to produce 1-hr L2P product, with improved coverage, and reduced cloud leakages and image noise. The collated L2P reports SSTs and brightness temperatures (BTs) in clear-sky water pixels (defined as ocean, sea, lake or river), and fill values elsewhere. All pixels with valid SSTs are recommended for use. ACSPO files also include sun-sensor geometry, l2p_flags (day/night, land, ice, twilight, and glint flags), and NCEP wind speed. The L2P is reported in NetCDF4 GHRSST Data Specification version 2 (GDS2) format, 24 granules per day, with a total data volume 0.6GB/day. Pixel earth locations are not reported in the granules, as they remain unchanged from granule to granule. Those can be obtained using a flat lat/lon file or a Python script (see Documentation page). Per GDS2 specifications, two additional Sensor-Specific Error Statistics layers (SSES bias and standard deviation) are reported in each pixel (Petrenko et al., 2016). The H08 AHI SSTs and BTs are continuously validated against in situ data in SQUAM (Dash et al, 2010), and RTM simulation in MICROS (Liang and Ignatov, 2011). A reduced size (0.2GB/day), 0.02-deg equal-angle gridded ACSPO L3C product is available at &lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/AHI_H08-STAR-L3C-v2.70&quot;&gt;https://podaac.jpl.nasa.gov/dataset/AHI_H08-STAR-L3C-v2.70&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ahi_h08-star-l3c-v270&quot;&gt;AHI_H08-STAR-L3C-v2.70&lt;/h4&gt;
The ACSPO H08/AHI L3C (Level 3 Collated) product is a gridded version of the ACSPO H08/AHI L2P product available at &lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/AHI_H08-STAR-L2P-v2.70&quot;&gt;https://podaac.jpl.nasa.gov/dataset/AHI_H08-STAR-L2P-v2.70&lt;/a&gt;. The L3C output files are 1hr granules in NetCDF4 format, compliant with the GHRSST Data Specification version 2 (GDS2). There are 24 granules available per 24hr interval, with a total data volume of 0.2GB/day. Valid SSTs are found over clear-sky oceans, sea, lakes or rivers, with fill values reported elsewhere. The following layers are reported: SST, ACSPO clear-sky mask (ACSM; provided in each grid as part of l2p_flags, which also includes day/night, land, ice, twilight, and glint flags), NCEP wind speed and ACSPO SST minus reference (Canadian Met Centre 0.1deg L4 SST; available at &lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/CMC0.1deg-CMC-L4-GLOB-v3.0&quot;&gt;https://podaac.jpl.nasa.gov/dataset/CMC0.1deg-CMC-L4-GLOB-v3.0&lt;/a&gt; ). All valid SSTs in L3C are recommended for users, although data over internal waters may not have enough in situ data to be adequately validated. Per GDS2 specifications, two additional Sensor-Specific Error Statistics layers (bias and standard deviation) are reported in each pixel with valid SST (Petrenko et al., 2016). The ACSPO VIIRS L3U product is monitored and validated against iQuam in situ data (Xu and Ignatov, 2014) in SQUAM (Dash et al, 2010).
&lt;br&gt;&lt;h4 id&#x3D;&quot;avhrrf_ma-star-l3u-v280&quot;&gt;AVHRRF_MA-STAR-L3U-v2.80&lt;/h4&gt;
This L3U (Level 3 Uncollated) dataset contains global daily Sea Surface Temperature (SST) on a 0.02 degree grid resolution. It is produced by the National Oceanic and Atmospheric Administration (NOAA) Advanced Clear Sky Processor for Ocean (ACSPO) using L2P (Level 2 Preprocessed) product acquired from the Meteorological Operational satellite A (Metop-A) Advanced Very High Resolution Radiometer 3 (AVHRR/3) (&lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/AVHRRF_MA-STAR-L2P-v2.80&quot;&gt;https://podaac.jpl.nasa.gov/dataset/AVHRRF_MA-STAR-L2P-v2.80&lt;/a&gt; ) in Full Resolution Area Coverage (FRAC) mode as input. It is distributed as 10-minute granules in netCDF-4 format, compliant with the Group for High Resolution Sea Surface Temperature (GHRSST) Data Specification version 2 (GDS2). There are 144 granules per 24-hour interval. Fill values are reported in all invalid pixels, including land pixels with &amp;gt;5 km inland. For each valid water pixel (defined as ocean, sea, lake or river), and up to 5 km inland, the following major layers are reported: SSTs and ACSPO clear-sky mask (ACSM; provided in each grid as part of l2p_flags, which also includes day/night, land, ice, twilight, and glint flags). Only input L2P SSTs with QL&#x3D;5 were gridded, so all valid SSTs are recommended for the users. Per GDS2 specifications, two additional Sensor-Specific Error Statistics layers (SSES bias and standard deviation) are reported in each pixel with valid SST. Ancillary layers include wind speed and ACSPO minus reference Canadian Meteorological Centre (CMC) Level 4 (L4) SST. The ACSPO Metop-A AVHRR FRAC L3U product is monitored and validated against iQuam in situ data (Xu and Ignatov, 2014) in the NOAA SST Quality Monitor (SQUAM) system (Dash et al, 2010). SST imagery and clear-sky mask are evaluated, and checked for consistency with L2P and other satellites/sensors SST products, in the NOAA ACSPO Regional Monitor for SST (ARMS) system. More information about the dataset is found at AVHRRF_MA-STAR-L2P-v2.80 and in (Pryamitsyn et al., 2021).
&lt;br&gt;&lt;h4 id&#x3D;&quot;avhrrf_ma-star-l2p-v280&quot;&gt;AVHRRF_MA-STAR-L2P-v2.80&lt;/h4&gt;
The MetOp First Generation (FG) is a European multi-satellite program jointly established by ESA and EUMETSAT, comprising three satellites, MetOp-A, -B and -C. The primary sensor onboard MetOp-FG, the Advanced Very High Resolution Radiometer/3 (AVHRR/3) contributed by NOAA, measures Earth emissions and reflectances in 5 out of 6 available bands (centered at 0.63, 0.83, 1.61, 3.7, 11 and 12 microns), in a swath of 2,600km from an 817km altitude. These data are collected in a Full Resolution Area Coverage (FRAC) mode, with pixel size of 1.1km at nadir. MetOp-A launched on 19 October 2006 is the first in the MetOp-FG series. The NOAA Advanced Clear-Sky Processor for Ocean (ACSPO) Level 2 Preprocessed (L2P) SST product is derived at the full AVHRR FRAC resolution and reported in 10 minute granules in NetCDF4 format, compliant with the GHRSST Data Specification version 2 (GDS2). Subskin SSTs are derived using the regression Nonlinear SST (NLSST) algorithm, which employs three bands (3.7, 11 and 12 microns) at night and two bands (11 and 12 microns) during the day. The ACSPO AVHRR FRAC L2P product is monitored and validated against quality controlled in situ data, provided by the NOAA in situ SST Quality Monitor system (iQuam; Xu and Ignatov, 2014, &lt;a href&#x3D;&quot;https://doi.org/10.1175/JTECH-D-13-00121.1&quot;&gt;https://doi.org/10.1175/JTECH-D-13-00121.1&lt;/a&gt; ), in another NOAA system, SST Quality Monitor (SQUAM; Dash et al, 2010, &lt;a href&#x3D;&quot;https://doi.org/10.1175/2010JTECHO756.1&quot;&gt;https://doi.org/10.1175/2010JTECHO756.1&lt;/a&gt; ). SST imagery and clear-sky masking are continuously evaluated, and checked for consistency with other sensors and platforms, in the ACSPO Regional Monitor for SST (ARMS) system. MetOp-A orbital characteristics and AVHRR/3 sensor performance are tracked in the NOAA 3S system (He et al., 2016, &lt;a href&#x3D;&quot;https://doi.org/10.3390/rs8040346&quot;&gt;https://doi.org/10.3390/rs8040346&lt;/a&gt; ).The L2P Near Real Time (NRT) SST files are archived at PO.DAAC with 3-6 hours latency, and then replaced by the Re-ANalysis (RAN) SST after about 2 months later with identical file names. Two features can be used to identify them: different file name time stamps and netCDF global attribute metadata source&#x3D;NOAA-NCEP-GFS for NRT and source&#x3D;MERRA-2 for RAN. A reduced size (0.45GB/day), equal-angle gridded (0.02-deg resolution) ACSPO L3U product is available at &lt;a href&#x3D;&quot;https://doi.org/10.5067/GHMTA-3US28&quot;&gt;https://doi.org/10.5067/GHMTA-3US28&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;avhrrf_mb-star-l3u-v280&quot;&gt;AVHRRF_MB-STAR-L3U-v2.80&lt;/h4&gt;
This L3U (Level 3 Uncollated) dataset contains global daily Sea Surface Temperature (SST) on a 0.02 degree grid resolution. It is produced by the National Oceanic and Atmospheric Administration (NOAA) Advanced Clear Sky Processor for Ocean (ACSPO) using L2P (Level 2 Preprocessed) product acquired from the Meteorological Operational satellite B (Metop-B) Advanced Very High Resolution Radiometer 3 (AVHRR/3) (&lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/AVHRRF_MB-STAR-L2P-v2.80&quot;&gt;https://podaac.jpl.nasa.gov/dataset/AVHRRF_MB-STAR-L2P-v2.80&lt;/a&gt; ) in Full Resolution Area Coverage (FRAC) mode as input. It is distributed as 10-minute granules in netCDF-4 format, compliant with the Group for High Resolution Sea Surface Temperature (GHRSST) Data Specification version 2 (GDS2). There are 144 granules per 24-hour interval. Fill values are reported in all invalid pixels, including land pixels with &amp;gt;5 km inland. For each valid water pixel (defined as ocean, sea, lake or river), and up to 5 km inland, the following major layers are reported: SSTs and ACSPO clear-sky mask (ACSM; provided in each grid as part of l2p_flags, which also includes day/night, land, ice, twilight, and glint flags). Only input L2P SSTs with QL&#x3D;5 were gridded, so all valid SSTs are recommended for the users. Per GDS2 specifications, two additional Sensor-Specific Error Statistics layers (SSES bias and standard deviation) are reported in each pixel with valid SST. Ancillary layers include wind speed and ACSPO minus reference Canadian Meteorological Centre (CMC) Level 4 (L4) SST. The ACSPO Metop-B AVHRR FRAC L3U product is monitored and validated against iQuam in situ data (Xu and Ignatov, 2014) in the NOAA SST Quality Monitor (SQUAM) system (Dash et al, 2010). SST imagery and clear-sky mask are evaluated, and checked for consistency with L2P and other satellites/sensors SST products, in the NOAA ACSPO Regional Monitor for SST (ARMS) system. More information about the dataset is found at AVHRRF_MB-STAR-L2P-v2.80 and in (Pryamitsyn et al., 2021).
&lt;br&gt;&lt;h4 id&#x3D;&quot;avhrrf_mc-star-l3u-v280&quot;&gt;AVHRRF_MC-STAR-L3U-v2.80&lt;/h4&gt;
This L3U (Level 3 Uncollated) dataset contains global daily Sea Surface Temperature (SST) on a 0.02 degree grid resolution. It is produced by the National Oceanic and Atmospheric Administration (NOAA) Advanced Clear Sky Processor for Ocean (ACSPO) using L2P (Level 2 Preprocessed) product acquired from the Meteorological Operational satellite C (Metop-C) Advanced Very High Resolution Radiometer 3 (AVHRR/3) (&lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/AVHRRF_MC-STAR-L2P-v2.80&quot;&gt;https://podaac.jpl.nasa.gov/dataset/AVHRRF_MC-STAR-L2P-v2.80&lt;/a&gt; ) in Full Resolution Area Coverage (FRAC) mode as input. It is distributed as 10-minute granules in netCDF-4 format, compliant with the Group for High Resolution Sea Surface Temperature (GHRSST) Data Specification version 2 (GDS2). There are 144 granules per 24-hour interval. Fill values are reported in all invalid pixels, including land pixels with &amp;gt;5 km inland. For each valid water pixel (defined as ocean, sea, lake or river), and up to 5 km inland, the following major layers are reported: SSTs and ACSPO clear-sky mask (ACSM; provided in each grid as part of l2p_flags, which also includes day/night, land, ice, twilight, and glint flags). Only input L2P SSTs with QL&#x3D;5 were gridded, so all valid SSTs are recommended for the users. Per GDS2 specifications, two additional Sensor-Specific Error Statistics layers (SSES bias and standard deviation) are reported in each pixel with valid SST. Ancillary layers include wind speed and ACSPO minus reference Canadian Meteorological Centre (CMC) Level 4 (L4) SST. The ACSPO Metop-C AVHRR FRAC L3U product is monitored and validated against iQuam in situ data (Xu and Ignatov, 2014) in the NOAA SST Quality Monitor (SQUAM) system (Dash et al, 2010). SST imagery and clear-sky mask are evaluated, and checked for consistency with L2P and other satellites/sensors SST products, in the NOAA ACSPO Regional Monitor for SST (ARMS) system. More information about the dataset is found at AVHRRF_MC-STAR-L2P-v2.80 and in (Pryamitsyn et al., 2021).
&lt;br&gt;&lt;h4 id&#x3D;&quot;oisst_hr_nrt-gos-l4-med-v20&quot;&gt;OISST_HR_NRT-GOS-L4-MED-v2.0&lt;/h4&gt;
CNR MED Sea Surface Temperature provides daily gap-free maps (L4) at 0.0625deg. x 0.0625deg. horizontal resolution over the Mediterranean Sea. The data are obtained from infra-red measurements collected by satellite radiometers and statistical interpolation. It is the CMEMS sea surface temperature nominal operational product for the Mediterranean sea.
&lt;br&gt;&lt;h4 id&#x3D;&quot;oisst_uhr_nrt-gos-l4-med-v20&quot;&gt;OISST_UHR_NRT-GOS-L4-MED-v2.0&lt;/h4&gt;
CNR MED Sea Surface Temperature provides daily gap-free maps (L4) at 0.01 deg. x 0.01deg. horizontal resolution over the Mediterranean Sea. The data are obtained from infra-red measurements collected by satellite radiometers and statistical interpolation. It is the CMEMS sea surface temperature nominal operational product for the Mediterranean sea.
&lt;br&gt;&lt;h4 id&#x3D;&quot;msg04-ospo-l2p-v10&quot;&gt;MSG04-OSPO-L2P-v1.0&lt;/h4&gt;
The GHRSST L2P MSG04 SST v1.0 dataset is produced by the US National Oceanic and Atmospheric Administration (NOAA) National Environmental Satellite, Data, and Information Service (NESDIS) from the Spinning Enhanced Visible and InfraRed Imager (SEVIRI) onboard the Meteosat-11 (MSG4) satellite. It provides the full disk SEVIRI imagery covering the Atlantic Ocean region from its position at 0.0°E longitude. The L2P SST is produced at approximately 3 km resolution with a 15 minute duty cycle. On Feb. 2, 2018 the Meteosat-11 (MSG4) took over the Meteosat-10 (MSG3) (MSG03-OSPO-L2P-v1.0) and produced the L2P SST data from Sept 10. 2018 to March 24, 2023. In March 2023, Meteosat-10 and Meteosat-11 were swapped roles and orbital positions. The MSG03 has started to produce the L2P SST data again over the Atlantic Ocean region. Be aware that the granules before Dec. 1, 2022 contain some uncorrected metadata errors. &lt;br&gt;&lt;br&gt; The SST measurements from SEVIRI are parameters in study of the weather, atmosphere, climate and ocean environments. Meteosat satellites have been providing crucial data for weather forecasting since 1977. &lt;br&gt;&lt;br&gt; This L2P SST product which includes Single Sensor Error Statistics (i.e., uncertainty statistics) follows the GHRSST Data Processing Specification (GDS) version 2.0 format guidelines. Please refer to the user guide for more information.
&lt;br&gt;&lt;h4 id&#x3D;&quot;msg01-ospo-l2p-v10&quot;&gt;MSG01-OSPO-L2P-v1.0&lt;/h4&gt;
The GHRSST L2P MSG01 SST v1.0 dataset is produced by the US National Oceanic and Atmospheric Administration (NOAA) National Environmental Satellite, Data, and Information Service (NESDIS) from the Spinning Enhanced Visible and InfraRed Imager (SEVIRI) onboard the Meteosat-8 (MSG1) satellite. It provides the full disk SEVIRI imagery covering the Indian Ocean region from its position at 45.5°E longitude. The L2P SST is produced at approximately 3 km resolution with a 15 minute duty cycle. The full data records stretch from Sept. 18, 2018 to June 1, 2022. After June 1, 2022, the Meteosat-9 (MSG2) took over as the prime geostationary satellite for the Indian Ocean region (MSG02-OSPO-L2P-v1.0). Be aware that the granules before Dec. 1, 2022 contain some uncorrected metadata errors. &lt;br&gt;&lt;br&gt; The SST measurements from SEVIRI are key parameters in study of the weather, atmosphere, climate and ocean environments. Meteosat satellites have been providing crucial data for weather forecasting since 1977. &lt;br&gt;&lt;br&gt; This L2P SST product which includes Single Sensor Error Statistics (i.e., uncertainty statistics) follows the GHRSST Data Processing Specification (GDS) version 2.0 format guidelines. Please refer to the user guide for more information.
&lt;br&gt;&lt;h4 id&#x3D;&quot;msg02-ospo-l2p-v10&quot;&gt;MSG02-OSPO-L2P-v1.0&lt;/h4&gt;
The GHRSST L2P MSG02 SST v1.0 dataset is produced by the US National Oceanic and Atmospheric Administration (NOAA) National Environmental Satellite, Data, and Information Service (NESDIS) from the Spinning Enhanced Visible and InfraRed Imager (SEVIRI) onboard the Meteosat-9 (MSG2) satellite. It provides the full disk SEVIRI imagery covering the Indian Ocean region from its position at 45.5°E longitude. The L2P SST is produced at approximately 3 km resolution with a 15 minute duty cycle. On June 1, 2022, the Meteosat-9 (MSG2) replaced the Meteosat-8 (MSG1) (MSG01-OSPO-L2P-v1.0) and produced the L2P SST data from June 11. 2022 to the present. This dataset will be updated every 15 minutes as a forward data stream with 3-24 hours nominal latency. Be aware that the granules before Dec. 1, 2022 contain some uncorrected metadata errors.&lt;br&gt;&lt;br&gt; The SST measurements from SEVIRI are key parameters in study of the weather, atmosphere, climate and ocean environments. Meteosat satellites have been providing crucial data for weather forecasting since 1977. &lt;br&gt;&lt;br&gt; This L2P SST product which includes Single Sensor Error Statistics (i.e., uncertainty statistics) follows the GHRSST Data Processing Specification (GDS) version 2.0 format guidelines. Please refer to the user guide for more information.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://archive.podaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA GLDAS Project</title>
      <link>https://registry.opendata.aws/nasa-gldas</link>
      <guid>https://registry.opendata.aws/nasa-gldas</guid>
      <description>NASA Global Land Data Assimilation System Version 2 (GLDAS-2) has three components: GLDAS-2.0, GLDAS-2.1, and GLDAS-2.2. GLDAS-2.0 is forced entirely with the Princeton meteorological forcing input data and provides a temporally consistent series from 1948 through 2014. GLDAS-2.1 is forced with a combination of model and observation data from 2000 to present. GLDAS-2.2 product suites use data assimilation (DA), whereas the GLDAS-2.0 and GLDAS-2.1 products are &amp;quot;open-loop&amp;quot; (i.e., no data assimilation). The choice of forcing data, as well as DA observation source, variable, and scheme, vary for different GLDAS-2.2 products. GLDAS-2.1 data products are now available in two production streams: one stream is forced with combined forcing data including GPCP version 1.3 (the main production stream), and the other stream is processed without this forcing data (the early production stream). Since the GPCP Version 1.3 data have a 3-4 month latency, the GLDAS-2.1 data products are first created without it, and are designated as Early Products (EPs), with about 1.5 month latency. Once the GPCP Version 1.3 data become available, the GLDAS-2.1 data products are processed in the main production stream and are removed from the Early Products archive. This data product is an Early Product for GLDAS-2.1 Catchment 1.0 degree 3-hourly dataset. The GLDAS-2.1 3 hourly 1.0 degree product was simulated with the Catchment-F2.5 Land Surface Model in Land Information System (LIS) Version 7. The data product contains 34 land surface fields from January 2000 to present. The GLDAS-2.1 simulation started on January 1, 2000 using the conditions from the GLDAS-2.0 simulation. This simulation was forced with National Oceanic and Atmospheric Administration (NOAA)/Global Data Assimilation System (GDAS) atmospheric analysis fields (Derber et al., 1991), the disaggregated Global Precipitation Climatology Project (GPCP) V1.3 Daily Analysis precipitation fields (Adler et al., 2003; Huffman et al., 2001), and the Air Force Weather Agency&amp;#39;s AGRicultural METeorological modeling system (AGRMET) radiation fields. The simulation used with GDAS and GPCP only from 2000 to February 2001, followed by addition of AGRMET for March 1, 2001 onwards. The GLDAS-2.1 products supersede their corresponding GLDAS-1 products. The GLDAS-2.1 data are archived and distributed in NetCDF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA GOES Project</title>
      <link>https://registry.opendata.aws/nasa-goes</link>
      <guid>https://registry.opendata.aws/nasa-goes</guid>
      <description>The ABI G16 Deep Blue L3 Daily Aerosol Data, 1 x 1 degree grid product, short-name AERDB_D3_ABI_G16, derived from the L2 (AERDB_L2_ABI_G16) input data, each D3 ABI/GOES-16 product is produced daily at 1 x 1-degree horizontal resolution. In general, in this daily L3 (identified in the short-name as D3) aggregated product, each data field represents the arithmetic mean of all cells whose latitude and longitude places them within the bounds of each grid element. Another statistic like standard deviation is also provided in some cases. The final retrievals used in the aggregation process are Quality Assurance (QA)-filtered best-estimate values for cells that are measured on the day of interest. Further, at least three such retrievals are required to render the validity of a grid cell on any given day. This first release of these products spans from May 2019 through April 2020 with a potential to generate additional temporal coverage in the future. The Level-3 (L3) Advanced Baseline Imager (ABI) Geostationary Operational Environmental Satellite-16 (GOES-16) Deep Blue Daily Aerosol dataset is part of a 12-product suite produced by an Earth Science Research from Operational Geostationary Satellite Systems (ESROGSS)-funded project. The 12 products in this project include nine derived from three Geostationary Earth Observation (GEO) instruments and three from merged data from GEO and Low-Earth Orbit (LEO) instruments. The AERDB_D3_ABI_G16 product, in netCDF4 format, contains 48 Science Data Set (SDS) layers. For more information consult LAADS product description page at: &lt;a href&#x3D;&quot;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/products/AERDB_D3_ABI_G16&quot;&gt;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/products/AERDB_D3_ABI_G16&lt;/a&gt; Or, Deep Blue aerosol project webpage at: &lt;a href&#x3D;&quot;https://earth.gsfc.nasa.gov/climate/data/deep-blue&quot;&gt;https://earth.gsfc.nasa.gov/climate/data/deep-blue&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;aerdb_m3_abi_g16&quot;&gt;AERDB_M3_ABI_G16&lt;/h4&gt;
The ABI G16 Deep Blue L3 Monthly Aerosol Data, 1 x 1 degree grid product, short-name AERDB_M3_ABI_G16, derived by aggregating the L3 daily (AERDB_D3_ABI_G16) input data, each M3 ABI/GOES-16 product is produced monthly at 1 x 1-degree horizontal resolution. This monthly L3 (identified in the short-name as M3) product’s statistics that include mean and standard deviation of the daily means are derived from the arithmetic mean values of the L3 daily product. As a mechanism to filter out poorly sampled grid elements, at least three valid days of data in the month are required to populate the monthly grid element. This first release of these products spans from May 2019 through April 2020 with a potential to generate additional temporal coverage in the future. The Level-3 (L3) Advanced Baseline Imager (ABI) Geostationary Operational Environmental Satellite-16 (GOES-16) Deep Blue Monthly Aerosol dataset is part of a 12-product suite produced by an Earth Science Research from Operational Geostationary Satellite Systems (ESROGSS)-funded project. The 12 products in this project include nine derived from three Geostationary Earth Observation (GEO) instruments and three from merged data from GEO and Low-Earth Orbit (LEO)) instruments. The AERDB_D3_ABI_G16 product, in netCDF4 format, contains 48 Science Data Set (SDS) layers. For more information consult LAADS product description page at: &lt;a href&#x3D;&quot;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/products/AERDB_M3_ABI_G16&quot;&gt;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/products/AERDB_M3_ABI_G16&lt;/a&gt; Or, Deep Blue aerosol project webpage at: &lt;a href&#x3D;&quot;https://earth.gsfc.nasa.gov/climate/data/deep-blue&quot;&gt;https://earth.gsfc.nasa.gov/climate/data/deep-blue&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;aerdb_d3_abi_g17&quot;&gt;AERDB_D3_ABI_G17&lt;/h4&gt;
The ABI G17 Deep Blue L3 Daily Aerosol Data, 1 x 1 degree grid product, short-name AERDB_D3_ABI_G17, derived from the L2 (AERDB_L2_ABI_G17) input data, each D3 ABI/GOES-17 product is produced daily at 1 x 1-degree horizontal resolution. In general, in this daily L3 (identified in the short-name as D3) aggregated product, each data field represents the arithmetic mean of all cells whose latitude and longitude places them within the bounds of each grid element. Another statistic like standard deviation is also provided in some cases. The final retrievals used in the aggregation process are Quality Assurance (QA)-filtered best-estimate values for cells that are measured on the day of interest. Further, at least three such retrievals are required to render the validity of a grid cell on any given day. This first release of these products spans from May 2019 through April 2020 with a potential to generate additional temporal coverage in the future. The Level-3 (L3) Advanced Baseline Imager (ABI) Geostationary Operational Environmental Satellite-17 (GOES-17) Deep Blue Daily Aerosol dataset is part of a 12-product suite produced by an Earth Science Research from Operational Geostationary Satellite Systems (ESROGSS)-funded project. The 12 products in this project include nine derived from three Geostationary Earth Observation (GEO) instruments and three from merged data from GEO and Low-Earth Orbit (LEO) instruments. The AERDB_D3_ABI_G17 product, in netCDF4 format, contains 48 Science Data Set (SDS) layers. For more information consult LAADS product description page at: &lt;a href&#x3D;&quot;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/products/AERDB_D3_ABI_G17&quot;&gt;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/products/AERDB_D3_ABI_G17&lt;/a&gt; Or, Deep Blue aerosol project webpage at: &lt;a href&#x3D;&quot;https://earth.gsfc.nasa.gov/climate/data/deep-blue&quot;&gt;https://earth.gsfc.nasa.gov/climate/data/deep-blue&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;aerdb_m3_abi_g17&quot;&gt;AERDB_M3_ABI_G17&lt;/h4&gt;
The ABI G17 Deep Blue L3 Monthly Aerosol Data, 1 x 1 degree grid product, short-name AERDB_M3_ABI_G17, derived by aggregating the L3 daily (AERDB_D3_ABI_G17) input data, each M3 ABI/GOES-17 product is produced monthly at 1 x 1-degree horizontal resolution. This monthly L3 (identified in the shortname as M3) product’s statistics that include mean and standard deviation of the daily means are derived from the arithmetic mean values of the L3 daily product. As a mechanism to filter out poorly sampled grid elements, at least three valid days of data in the month are required to populate the monthly grid element. This first release of these products spans from May 2019 through April 2020 with a potential to generate additional temporal coverage in the future. The Level-3 (L3) Advanced Baseline Imager (ABI) Geostationary Operational Environmental Satellite-17 (GOES-17) Deep Blue Daily Aerosol dataset is part of a 12-product suite produced by an Earth Science Research from Operational Geostationary Satellite Systems (ESROGSS)-funded project. The 12 products in this project include nine derived from three Geostationary Earth Observation (GEO) instruments and three from merged data from GEO and Low-Earth Orbit (LEO) instruments. The AERDB_M3_ABI_G17 product, in netCDF4 format, contains 48 Science Data Set (SDS) layers. For more information consult LAADS product description page at: &lt;a href&#x3D;&quot;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/products/AERDB_M3_ABI_G17&quot;&gt;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/products/AERDB_M3_ABI_G17&lt;/a&gt; Or, Deep Blue aerosol project webpage at: &lt;a href&#x3D;&quot;https://earth.gsfc.nasa.gov/climate/data/deep-blue&quot;&gt;https://earth.gsfc.nasa.gov/climate/data/deep-blue&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;aerdb_l2g_geoleo_merged&quot;&gt;AERDB_L2G_GEOLEO_Merged&lt;/h4&gt;
The GEO-LEO Merged Deep Blue Aerosol 0.25x0.25 degree Gridded L2 product, short-name AERDB_L2G_GEOLEO_Merged contains gridded Aerosol Optical Thickness (AOT) at 550 nm reference wavelength, derived from seven merged GEO-LEO AOT layers (G16-ABI, G17-ABI, H08-AHI, SNPP-VIIRS, NOAA20-VIIRS, Terra MODIS and Aqua MODIS) and from each of the individual (three GEO and four LEO) instrument sources. Each L2G aggregated datafile is spatially comprised of a 0.25˚ x 0.25˚ horizontal grid that exists for every 30 minutes. This represents a 30-minute Deep Blue best-estimate AOT from each of the seven sources besides an error-weighted merged AOT layer. This first release of these products spans from May 2019 through April 2020 with a potential to generate additional temporal coverage in the future. The Level-2G (L2G) Geostationary Earth Orbit (GEO)-Low-Earth Orbit (LEO) Merged Deep Blue Aerosol 0.25 x 0.25-degree Gridded dataset is part of a 12-product suite produced by an Earth Science Research from Operational Geostationary Satellite Systems (ESROGSS)-funded project. The 12 products in this project include nine derived from three Geostationary Earth Observation (GEO) instruments and three from merged data from GEO and Low-Earth Orbit (LEO) instruments. The AERDB_L2G_GEOLEO_Merged product, in netCDF4 format, contains 16 GEO-LEO Merged Group Science Data Set (SDS) layers and 15 GEO and LEO SDSs. For more information consult LAADS product description page at: &lt;a href&#x3D;&quot;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/products/AERDB_L2G_GEOLEO_Merged&quot;&gt;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/products/AERDB_L2G_GEOLEO_Merged&lt;/a&gt; Or, Deep Blue aerosol project webpage at: &lt;a href&#x3D;&quot;https://earth.gsfc.nasa.gov/climate/data/deep-blue&quot;&gt;https://earth.gsfc.nasa.gov/climate/data/deep-blue&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;aerdb_d3_geoleo_merged&quot;&gt;AERDB_D3_GEOLEO_Merged&lt;/h4&gt;
The GEO-LEO Merged Deep Blue Aerosol Daily 1 x 1 degree Gridded L3 product, short-name AERDB_D3_GEOLEO_Merged contains gridded Aerosol Optical Thickness (AOT) at 550 nm reference wavelength that are composited from the L2G product (AERDB_L2G_GEOLEO_Merged) using best-estimate AOT values. Please note that while the individual standalone gridded data layer for each instrument is calculated as the arithmetic mean, the merged AOT layer is derived via an error-weighted average approach. The final retrievals used in the aggregation process are QA-filtered best-estimate values for cells that are measured on the day of interest. Further, at least three such retrievals are required to render the validity of a grid cell on any given day. Each L3 daily aggregated datafile is spatially comprised of a 1˚ x 1˚ horizontal grid that exists for every 30 minutes. This first release of these products spans from May 2019 through April 2020 with a potential to generate additional temporal coverage in the future. The Level-3 (L3) Geostationary Earth Orbit (GEO)-Low-Earth Orbit (LEO) Merged Deep Blue Aerosol Daily 1 x 1-degree Gridded dataset is part of a 12-product suite produced by an Earth Science Research from Operational Geostationary Satellite Systems (ESROGSS)-funded project. The 12 products in this project include nine derived from three Geostationary Earth Observation (GEO) instruments and three from merged data from GEO and Low-Earth Orbit (LEO) instruments. The AERDB_D3_GEOLEO_Merged product, in netCDF4 format, contains 16 GEO-LEO Merged Group Science Data Set (SDS) layers and 15 GEO and LEO SDSs. For more information consult LAADS product description page at: &lt;a href&#x3D;&quot;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/products/AERDB_D3_GEOLEO_Merged&quot;&gt;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/products/AERDB_D3_GEOLEO_Merged&lt;/a&gt; Or, Deep Blue aerosol project webpage at: &lt;a href&#x3D;&quot;https://earth.gsfc.nasa.gov/climate/data/deep-blue&quot;&gt;https://earth.gsfc.nasa.gov/climate/data/deep-blue&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;aerdb_m3_geoleo_merged&quot;&gt;AERDB_M3_GEOLEO_Merged&lt;/h4&gt;
The GEO-LEO Merged Deep Blue Aerosol Monthly 1 x 1 degree Gridded L3 product, short-name AERDB_M3_GEOLEO_Merged contains gridded Aerosol Optical Thickness (AOT) at 550 nm reference wavelength that are composited from the L3 daily product (AERDB_D3_GEOLEO_Merged). Please note that while the individual standalone gridded data layer for each instrument is calculated as the arithmetic mean, the merged AOT layer is derived via an error-weighted average approach. The final retrievals used in the aggregation process are QA-filtered best-estimate values for cells that are measured on the day of interest. Further, at least three such retrievals are required to render the validity of a grid cell on any given day. Each L3 daily aggregated datafile is spatially comprised of a 1˚ x 1˚ horizontal grid that exists for every 30 minutes. This first release of these products spans from May 2019 through April 2020 with a potential to generate additional temporal coverage in the future. The Level-3 (L3) Geostationary Earth Orbit (GEO)-Low-Earth Orbit (LEO) Merged Deep Blue Aerosol Daily 1 x 1-degree Gridded dataset is part of a 12-product suite produced by an Earth Science Research from Operational Geostationary Satellite Systems (ESROGSS)-funded project. The 12 products in this project include nine derived from three Geostationary Earth Observation (GEO) instruments and three from merged data from GEO and Low-Earth Orbit (LEO) instruments. The AERDB_M3_GEOLEO_Merged product, in netCDF4 format, contains 16 GEO-LEO Merged Group Science Data Set (SDS) layers and 15 GEO and LEO SDS layers. For more information consult LAADS product description page at: &lt;a href&#x3D;&quot;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/products/AERDB_M3_GEOLEO_Merged&quot;&gt;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/products/AERDB_M3_GEOLEO_Merged&lt;/a&gt; Or, Deep Blue aerosol project webpage at: &lt;a href&#x3D;&quot;https://earth.gsfc.nasa.gov/climate/data/deep-blue&quot;&gt;https://earth.gsfc.nasa.gov/climate/data/deep-blue&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;aerdb_l2_abi_g16&quot;&gt;AERDB_L2_ABI_G16&lt;/h4&gt;
The ABI G16 Deep Blue Aerosol 10-Min L2 Full Disk product, short-name AERDB_L2_ABI_G16 is produced every 30 minutes and contains full-disk observation data. The L2 data products comprise 10 x 10 native GEO pixels. Each spectral band with 0.5 km or 2 km resolution is downscaled or upscaled to a nominal ~1 km horizontal pixel size in the production process. To distinguish them from native instrument pixels, these 10 x 10 aggregated pixels are also called retrieval pixels. Therefore, the L2 products’ image dimensions are roughly 10 km x 10 km at the sub-satellite point and are larger away from that point because of the combined effects of the sensor’s scanning geometry and Earth’s curvature. This first release of these products spans from May 2019 through April 2020 with a potential to generate additional temporal coverage in the future. The Level-2 (L2) Advanced Baseline Imager (ABI) Geostationary Operational Environmental Satellite-16 (GOES-16) Deep Blue Aerosol Full-Disk dataset is part of a 12-product suite produced by an Earth Science Research from Operational Geostationary Satellite Systems (ESROGSS)-funded project. The 12 products in this project include nine derived from three Geostationary Earth Observation (GEO) instruments and three from merged data from GEO and Low-Earth Orbit (LEO) instruments. The AERDB_L2_ABI_G16 product, in netCDF4 format, contains 51 Science Data Set (SDS) layers. For more information consult LAADS product description page at: &lt;a href&#x3D;&quot;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/products/AERDB_L2_ABI_G16&quot;&gt;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/products/AERDB_L2_ABI_G16&lt;/a&gt; Or, Deep Blue aerosol project webpage at: &lt;a href&#x3D;&quot;https://earth.gsfc.nasa.gov/climate/data/deep-blue&quot;&gt;https://earth.gsfc.nasa.gov/climate/data/deep-blue&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;aerdb_l2_abi_g17&quot;&gt;AERDB_L2_ABI_G17&lt;/h4&gt;
The ABI G17 Deep Blue Aerosol 10-Min L2 Full Disk product, short-name AERDB_L2_ABI_G17 is produced every 30 minutes and contains full-disk observation data. The L2 data products comprise 10 x 10 native GEO pixels. Each spectral band with 0.5 km or 2 km resolution is downscaled or upscaled to a nominal ~1 km horizontal pixel size in the production process. To distinguish them from native instrument pixels, these 10 x 10 aggregated pixels are also called retrieval pixels. Therefore, the L2 products’ image dimensions are roughly 10 km x 10 km at the sub-satellite point and are larger away from that point because of the combined effects of the sensor’s scanning geometry and Earth’s curvature. This first release of these products spans from May 2019 through April 2020 with a potential to generate additional temporal coverage in the future. The Level-2 (L2) Advanced Baseline Imager (ABI) Geostationary Operational Environmental Satellite-17 (GOES-17) Deep Blue Aerosol Full-Disk dataset is part of a 12-product suite produced by an Earth Science Research from Operational Geostationary Satellite Systems (ESROGSS)-funded project. The 12 products in this project include nine derived from three Geostationary Earth Observation (GEO) instruments and three from merged data from GEO and Low-Earth Orbit (LEO) instruments. The AERDB_L2_ABI_G17 product, in netCDF4 format, contains 51 Science Data Set (SDS) layers. For more information consult LAADS product description page at: &lt;a href&#x3D;&quot;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/products/AERDB_L2_ABI_G17&quot;&gt;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/products/AERDB_L2_ABI_G17&lt;/a&gt; Or, Deep Blue aerosol project webpage at: &lt;a href&#x3D;&quot;https://earth.gsfc.nasa.gov/climate/data/deep-blue&quot;&gt;https://earth.gsfc.nasa.gov/climate/data/deep-blue&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;vissrgoes1imir&quot;&gt;VISSRGOES1IMIR&lt;/h4&gt;
VISSRGOES1IMIR is the Visible Infrared Spin-Scan Radiometer (VISSR) Infrared Imagery on 70mm Film data product from the first Geostationary Operational Environmental Satellite (GOES-1). This set of IR imagery (10.5 to 12.5 micrometer) was originally produced on commercial image-generation equipment from digital tapes and was made available on 70-mm film, from which they were later scanned to digital TIFF image files. Each TIFF scan contains 2 or 3 pictures, and there are several hundred scans from an original 70 mm film roll which are combined into a ZIP file. Each picture contains a title on the top boundary and a 33-level gray scale on the right boundary that represents brightness temperatures. It may have a combination of the following options: 1) contrast enhancement, 2) image sectorization, and 3) 1/16-size imagery. The maximum effective size covers 500 sq km, represented by 4000 by 3904 pixels. Each element has a maximum resolution of 3.7 km. The title contains the satellite identification, picture number, picture type, coordinate numbers of the top left pixel relative to the visible sensor, start time of sectorized image, and pixel scaling and sector size identification. The GOES-1 satellite was parked over the equator at longitude 115W on Dec 18, 1975 viewing the hemisphere below the satellite. The VISSR experiment was operated by the NOAA National Environmental Satellite Data and Information Service (NESDIS), as well as scientists from NASA Goddard Space Flight Center. This product was previously available from the NSSDC with the identifier ESAD-00247 (old ID 75-100A-01B).
&lt;br&gt;&lt;h4 id&#x3D;&quot;vissrgoes1imvis&quot;&gt;VISSRGOES1IMVIS&lt;/h4&gt;
VISSRGOES1IMVIS is the Visible Infrared Spin-Scan Radiometer (VISSR) Visible Imagery on 70mm Film data product from the first Geostationary Operational Environmental Satellite (GOES-1). This set of visible imagery (0.55 to 0.70 micrometer) was originally produced on commercial image-generation equipment from digital tapes and was made available on 70-mm film, from which they were later scanned to digital TIFF image files. Each TIFF scan contains 2 or 3 pictures, and there are several hundred scans from an original 70 mm film roll which are combined into a ZIP file. Each picture contains a title on the top boundary and a 33-level gray scale on the right boundary that represents brightness temperatures. It may have a combination of the following options: 1) contrast enhancement, 2) image sectorization, and 3) 1/16-size imagery. The maximum effective size covers 500 sq km, represented by 4000 by 3904 pixels. Each element has a maximum resolution of 3.7 km. The title contains the satellite identification, picture number, picture type, coordinate numbers of the top left pixel relative to the visible sensor, start time of sectorized image, and pixel scaling and sector size identification. The GOES-1 satellite was parked over the equator at longitude 115W on Dec 18, 1975 viewing the hemisphere below the satellite. The VISSR experiment was operated by the NOAA National Environmental Satellite Data and Information Service (NESDIS), as well as scientists from NASA Goddard Space Flight Center. This product was previously available from the NSSDC with the identifier ESAD-00247 (old ID 75-100A-01B).
&lt;br&gt;&lt;h4 id&#x3D;&quot;vissrgoes2imir&quot;&gt;VISSRGOES2IMIR&lt;/h4&gt;
VISSRGOES2IMIR is the Visible Infrared Spin-Scan Radiometer (VISSR) Infrared Imagery on 70mm Film data product from the second Geostationary Operational Environmental Satellite (GOES-2). This set of IR imagery (10.5 to 12.5 micrometer) was originally produced on commercial image-generation equipment from digital tapes and was made available on 70-mm film, from which they were later scanned to digital TIFF image files. Each TIFF scan contains 2 or 3 pictures, and there are several hundred scans from an original 70 mm film roll which are combined into a ZIP file. Each picture contains a title on the top boundary and a 33-level gray scale on the right boundary that represents brightness temperatures. It may have a combination of the following options: 1) contrast enhancement, 2) image sectorization, and 3) 1/16-size imagery. The maximum effective size covers 500 sq km, represented by 4000 by 3904 pixels. Each element has a maximum resolution of 3.7 km. The title contains the satellite identification, picture number, picture type, coordinate numbers of the top left pixel relative to the visible sensor, start time of sectorized image, and pixel scaling and sector size identification. The GOES-2 satellite was parked over the equator at longitude 75W from 1977 through 1978 viewing the hemisphere below the satellite. The VISSR experiment was operated by the NOAA National Environmental Satellite Data and Information Service (NESDIS), as well as scientists from NASA Goddard Space Flight Center. This product was previously available from the NSSDC with the identifier ESAD-00028 (old ID 77-048A-01C).
&lt;br&gt;&lt;h4 id&#x3D;&quot;vissrgoes2imvis&quot;&gt;VISSRGOES2IMVIS&lt;/h4&gt;
VISSRGOES2IMVIS is the Visible Infrared Spin-Scan Radiometer (VISSR) Visible Imagery on 70mm Film data product from the second Geostationary Operational Environmental Satellite (GOES-2). This set of visible imagery (0.55 to 0.70 micrometer) was originally produced on commercial image-generation equipment from digital tapes and was made available on 70-mm film, from which they were later scanned to digital TIFF image files. Each TIFF scan contains 2 or 3 pictures, and there are several hundred scans from an original 70 mm film roll which are combined into a ZIP file. Each picture contains a title on the top boundary and a 33-level gray scale on the right boundary that represents brightness temperatures. It may have a combination of the following options: 1) contrast enhancement, 2) image sectorization, and 3) 1/16-size imagery. The maximum effective size covers 500 sq km, represented by 4000 by 3904 pixels. Each element has a maximum resolution of 3.7 km. The title contains the satellite identification, picture number, picture type, coordinate numbers of the top left pixel relative to the visible sensor, start time of sectorized image, and pixel scaling and sector size identification. The GOES-2 satellite was parked over the equator at longitude 75W from 1977 through 1978 viewing the hemisphere below the satellite. The VISSR experiment was operated by the NOAA National Environmental Satellite Data and Information Service (NESDIS), as well as scientists from NASA Goddard Space Flight Center. This product was previously available from the NSSDC with the identifier ESAD-00087 (old ID 77-048A-01B).
&lt;br&gt;&lt;h4 id&#x3D;&quot;vissrgoes3imir&quot;&gt;VISSRGOES3IMIR&lt;/h4&gt;
VISSRGOES3IMIR is the Visible Infrared Spin-Scan Radiometer (VISSR) Infrared Imagery on 70mm Film data product from the third Geostationary Operational Environmental Satellite (GOES-3). This set of IR imagery (10.5 to 12.5 micrometer) was originally produced on commercial image-generation equipment from digital tapes and was made available on 70-mm film, from which they were later scanned to digital TIFF image files. Each TIFF scan contains 2 or 3 pictures, and there are several hundred scans from an original 70 mm film roll which are combined into a ZIP file. Each picture contains a title on the top boundary and a 33-level gray scale on the right boundary that represents brightness temperatures. It may have a combination of the following options: 1) contrast enhancement, 2) image sectorization, and 3) 1/16-size imagery. The maximum effective size covers 500 sq km, represented by 4000 by 3904 pixels. Each element has a maximum resolution of 3.7 km. The title contains the satellite identification, picture number, picture type, coordinate numbers of the top left pixel relative to the visible sensor, start time of sectorized image, and pixel scaling and sector size identification. The GOES-3 satellite was parked over the equator at longitude 135W from 1978 through 1981 viewing the hemisphere below the satellite. The VISSR experiment was operated by the NOAA National Environmental Satellite Data and Information Service (NESDIS), as well as scientists from NASA Goddard Space Flight Center. This product was previously available from the NSSDC with the identifier ESAD-00105 (old ID 75-100A-01C).
&lt;br&gt;&lt;h4 id&#x3D;&quot;vissrgoes3imvis&quot;&gt;VISSRGOES3IMVIS&lt;/h4&gt;
VISSRGOES3IMVIS is the Visible Infrared Spin-Scan Radiometer (VISSR) Visible Imagery on 70mm Film data product from the third Geostationary Operational Environmental Satellite (GOES-3). This set of visible imagery (0.55 to 0.70 micrometer) was originally produced on commercial image-generation equipment from digital tapes and was made available on 70-mm film, from which they were later scanned to digital TIFF image files. Each TIFF scan contains 2 or 3 pictures, and there are several hundred scans from an original 70 mm film roll which are combined into a ZIP file. Each picture contains a title on the top boundary and a 33-level gray scale on the right boundary that represents brightness temperatures. It may have a combination of the following options: 1) contrast enhancement, 2) image sectorization, and 3) 1/16-size imagery. The maximum effective size covers 500 sq km, represented by 4000 by 3904 pixels. Each element has a maximum resolution of 3.7 km. The title contains the satellite identification, picture number, picture type, coordinate numbers of the top left pixel relative to the visible sensor, start time of sectorized image, and pixel scaling and sector size identification. The GOES-3 satellite was parked over the equator at longitude 135W from 1978 through 1981 viewing the hemisphere below the satellite. It was moved to its final operational position at 135W on Dec 19, 1975. The VISSR experiment was operated by the NOAA National Environmental Satellite Data and Information Service (NESDIS), as well as scientists from NASA Goddard Space Flight Center. This product was previously available from the NSSDC with the identifier ESAD-00247 (old ID 75-100A-01B).
&lt;br&gt;&lt;h4 id&#x3D;&quot;vissrsms1imir&quot;&gt;VISSRSMS1IMIR&lt;/h4&gt;
VISSRSMS1IMIR is the Visible Infrared Spin-Scan Radiometer (VISSR) Infrared Imagery on 70mm Film data product from the first Synchronous Meteorological Satellite (SMS-1). This set of IR imagery (10.5 to 12.5 micrometer) was originally produced on commercial image-generation equipment from digital tapes and was made available on 70-mm film, from which they were later scanned to digital TIFF image files. Each TIFF scan contains 2 or 3 pictures, and there are several hundred scans from an original 70 mm film roll which are combined into a ZIP file. Each picture contains a title on the top boundary and a 33-level gray scale on the right boundary that represents brightness temperatures. It may have a combination of the following options: 1) contrast enhancement, 2) image sectorization, and 3) 1/16-size imagery. The maximum effective size covers 500 sq km, represented by 4000 by 3904 pixels. Each element has a maximum resolution of 3.7 km. The title contains the satellite identification, picture number, picture type, coordinate numbers of the top left pixel relative to the visible sensor, start time of sectorized image, and pixel scaling and sector size identification. The SMS-1 satellite was initially parked over the equator at longitude 45W on June 7, 1974 viewing the hemisphere below the satellite to support the GARP Atlantic Tropical Experiment (GATE). It was moved to its operational position at 75W on Nov 15, 1974 where it remained until GOES-1 was launched, after which SMS-1 was moved to 105W and placed in stand-by-mode as a backup to GOES-1 or SMS-2. The VISSR experiment was operated by the NOAA National Environmental Satellite Data and Information Service (NESDIS), as well as scientists from NASA Goddard Space Flight Center. This product was previously available from the NSSDC with the identifier ESAD-00068 (old ID 74-033A-01C).
&lt;br&gt;&lt;h4 id&#x3D;&quot;vissrsms1l1aoips&quot;&gt;VISSRSMS1L1AOIPS&lt;/h4&gt;
VISSRSMS1L1AOIPS is the Visible Infrared Spin-Scan Radiometer (VISSR) Level 1 Atmospheric and Oceanographic Image Processing System (AOIPS) data product from the first Synchronous Meteorological Satellite (SMS-1). There are typically three data files for a scene of the Earth with radiances that were measured in the visible (0.55 to 0.70 micrometer) and/or IR (10.5 to 12.6 micrometer) wavelengths with a spatial resolution of 0.9 and 8 km, respectively. Files also include time, geolocation, orbit, attitude, and telemetry information. There are three types of data files in this product: one contains IR data, one contains the IR grid information (blank before 1974/10/29), and another contains VIS data. Each data file is structured with an AOIPS label, followed by an IPD label, and then an optional 8 telemetry records followed by a set of data records. Visible data are typically 3904 pixels by either 4000 or 2000 scan lines (5 or 2.5 minute scenes respectively). IR data are typically 976 pixels by either 500 or 250 scan lines (5 or 2.5 minute scenes respectively). A full scan of the Earth was made every 20 minutes. The data were used to make 70mm film negatives and 9.5” positive prints on a Dicomed Image Recording System. Data for this product are available from 1974/07/01 through 1979/04/19 (with gaps plus no data between 1975/08/20 and 1979/02/17). The SMS-1 satellite was initially parked over the equator at longitude 45W on June 7, 1974 viewing the hemisphere below the satellite to support the GARP Atlantic Tropical Experiment (GATE). It was moved to its operational position at 75W on Nov 15, 1974 where it remained until GOES-1 was launched, after which SMS 1 was moved to 105W and placed in stand-by-mode as a backup to GOES-1 or SMS-2. The VISSR experiment was operated by the NOAA National Environmental Satellite Data and Information Service (NESDIS), as well as scientists from NASA Goddard Space Flight Center. This product was previously available from the NSSDC with the identifier ESAD-00018 (old ID 74-033A-01D).
&lt;br&gt;&lt;h4 id&#x3D;&quot;vissrsms1l1eht&quot;&gt;VISSRSMS1L1EHT&lt;/h4&gt;
VISSRSMS1L1EHT is the Visible Infrared Spin-Scan Radiometer (VISSR) Level 1 Experimenter History Tape (EHT) data product from the first Synchronous Meteorological Satellite (SMS-1). Each data file contains a segment of the Earth with radiances that were measured in the visible (0.55 to 0.70 micrometer) and/or IR (10.5 to 12.6 micrometer) wavelengths with a spatial resolution of 0.9 and 8 km, respectively. Files also include time, geolocation, orbit, attitude, and telemetry information. A data file is structured with a header, followed by an IR scan line and then 8 visible scan lines (although some files only contain IR scans). Visible scans are at full resolution of 15288 pixels and a file will contain several hundred scan lines. IR scans are at 3822 pixels and up to a hundred scan lines. A full scan of the Earth was made every 20 minutes. Data for this product are only available for 9 days: 1974/08/23 (IR only), 1974/08/27 (IR only), 1974/08/31, 1974/09/01, 1974/09/02, 1974/09/05, 1974/09/24 (IR only), 1975/01/10, and 1975/02/17. The SMS-1 satellite was initially parked over the equator at longitude 45W on June 7, 1974 viewing the hemisphere below the satellite to support the GARP Atlantic Tropical Experiment (GATE). It was moved to its operational position at 75W on Nov 15, 1974 where it remained until GOES-1 was launched, after which SMS 1 was moved to 105W and placed in stand-by-mode as a backup to GOES-1 or SMS-2. The VISSR experiment was operated by the NOAA National Environmental Satellite Data and Information Service (NESDIS), as well as scientists from NASA Goddard Space Flight Center. This product was previously available from the NSSDC with the identifier ESAD-00126 (old ID 74-033A-01A).
&lt;br&gt;&lt;h4 id&#x3D;&quot;vissrsms1imvis&quot;&gt;VISSRSMS1IMVIS&lt;/h4&gt;
VISSRSMS1IMVIS is the Visible Infrared Spin-Scan Radiometer (VISSR) Visible Imagery on 70mm Film data product from the first Synchronous Meteorological Satellite (SMS-1). This set of visible imagery (0.55 to 0.70 micrometer) was originally produced on commercial image-generation equipment from digital tapes and was made available on 70-mm film, from which they were later scanned to digital TIFF image files. Each TIFF scan contains 2 or 3 pictures, and there are several hundred scans from an original 70 mm film roll which are combined into a ZIP file. Each picture contains a title on the top boundary and a 33-level gray scale on the right boundary that represents brightness temperatures. It may have a combination of the following options: 1) contrast enhancement, 2) image sectorization, and 3) 1/16-size imagery. The maximum effective size covers 500 sq km, represented by 4000 by 3904 pixels. Each element has a maximum resolution of 3.7 km. The title contains the satellite identification, picture number, picture type, coordinate numbers of the top left pixel relative to the visible sensor, start time of sectorized image, and pixel scaling and sector size identification. The SMS-1 satellite was initially parked over the equator at longitude 45W on June 7, 1974 viewing the hemisphere below the satellite to support the GARP Atlantic Tropical Experiment (GATE). It was moved to its operational position at 75W on Nov 15, 1974 where it remained until GOES-1 was launched, after which SMS-1 was moved to 105W and placed in stand-by-mode as a backup to GOES-1 or SMS-2. The VISSR experiment was operated by the NOAA National Environmental Satellite Data and Information Service (NESDIS), as well as scientists from NASA Goddard Space Flight Center. This product was previously available from the NSSDC with the identifier ESAD-00040 (old ID 74-033A-01B).
&lt;br&gt;&lt;h4 id&#x3D;&quot;vissrsms2imir&quot;&gt;VISSRSMS2IMIR&lt;/h4&gt;
VISSRSMS2IMIR is the Visible Infrared Spin-Scan Radiometer (VISSR) Infrared Imagery on 70mm Film data product from the second Synchronous Meteorological Satellite (SMS-2). This set of IR imagery (10.5 to 12.5 micrometer) was originally produced on commercial image-generation equipment from digital tapes and was made available on 70-mm film, from which they were later scanned to digital TIFF image files. Each TIFF scan contains 2 or 3 pictures, and there are several hundred scans from an original 70 mm film roll which are combined into a ZIP file. Each picture contains a title on the top boundary and a 33-level gray scale on the right boundary that represents brightness temperatures. It may have a combination of the following options: 1) contrast enhancement, 2) image sectorization, and 3) 1/16-size imagery. The maximum effective size covers 500 sq km, represented by 4000 by 3904 pixels. Each element has a maximum resolution of 3.7 km. The title contains the satellite identification, picture number, picture type, coordinate numbers of the top left pixel relative to the visible sensor, start time of sectorized image, and pixel scaling and sector size identification. The SMS-2 satellite was initially parked over the equator at longitude 105W on Feb 22, 1975 viewing the hemisphere below the satellite. It was moved to its final operational position at 135W on Dec 19, 1975. The VISSR experiment was operated by the NOAA National Environmental Satellite Data and Information Service (NESDIS), as well as scientists from NASA Goddard Space Flight Center. This product was previously available from the NSSDC with the identifier ESAD-00038 (old ID 75-011A-04C).
&lt;br&gt;&lt;h4 id&#x3D;&quot;vissrsms2l1aoips&quot;&gt;VISSRSMS2L1AOIPS&lt;/h4&gt;
VISSRSMS2L1AOIPS is the Visible Infrared Spin-Scan Radiometer (VISSR) Level 1 Atmospheric and Oceanographic Image Processing System (AOIPS) data product from the second Synchronous Meteorological Satellite (SMS-2). There are typically three data files for a scene of the Earth with radiances that were measured in the visible (0.55 to 0.70 micrometer) and/or IR (10.5 to 12.6 micrometer) wavelengths with a spatial resolution of 0.9 and 8 km, respectively. Files also include time, geolocation, orbit, attitude, and telemetry information. There are three types of data files in this product: one contains IR data, one contains the IR grid information, and another contains VIS data. Each data file is structured with an AOIPS label, followed by an IPD label, and then an optional 8 telemetry records followed by a set of data records. Visible data are typically 3904 pixels by either 4000 or 2000 scan lines (5 or 2.5 minute scenes respectively). IR data are typically 976 pixels by either 500 or 250 scan lines (5 or 2.5 minute scenes respectively). A full scan of the Earth was made every 20 minutes. The data were used to make 70mm film negatives and 9.5” positive prints on a Dicomed Image Recording System. Data for this product are available from 1975/04/27 through 1980/08/22 (with gaps plus no data between 1975/07/31 and 1979/05/10). The SMS-2 satellite was initially parked over the equator at longitude 105W on Feb 22, 1975 viewing the hemisphere below the satellite. It was moved to its final operational position at 135W on Dec 19, 1975. The VISSR experiment was operated by the NOAA National Environmental Satellite Data and Information Service (NESDIS), as well as scientists from NASA Goddard Space Flight Center. This product was previously available from the NSSDC with the identifier ESAD-00095 (old ID 75-011A-04D).
&lt;br&gt;&lt;h4 id&#x3D;&quot;vissrsms2l1eht&quot;&gt;VISSRSMS2L1EHT&lt;/h4&gt;
VISSRSMS2L1EHT is the Visible Infrared Spin-Scan Radiometer (VISSR) Level 1 Experimenter History Tape (EHT) data product from the second Synchronous Meteorological Satellite (SMS-2). Each data file contains a segment of the Earth with radiances that were measured in the visible (0.55 to 0.70 micrometer) and/or IR (10.5 to 12.6 micrometer) wavelengths with a spatial resolution of 0.9 and 8 km, respectively. Files also include time, geolocation, orbit, attitude, and telemetry information. A data file is structured with a header, followed by an IR scan line and then 8 visible scan lines (although some files only contain IR scans). Visible scans are at full resolution of 15288 pixels and a file will contain several hundred scan lines. IR scans are at 3822 pixels and up to a hundred scan lines. A full scan of the Earth was made every 20 minutes. Data for this product are only available for 5 days: 1975/02/17, 1975/04/24, 1975/04/25, 1975/05/06, and 1975/08/28. The SMS-2 satellite was initially parked over the equator at longitude 105W on Feb 22, 1975 viewing the hemisphere below the satellite. It was moved to its final operational position at 135W on Dec 19, 1975. The VISSR experiment was operated by the NOAA National Environmental Satellite Data and Information Service (NESDIS), as well as scientists from NASA Goddard Space Flight Center. This product was previously available from the NSSDC with the identifier ESAD-00039 (old ID 75-011A-04A).
&lt;br&gt;&lt;h4 id&#x3D;&quot;vissrsms2imvis&quot;&gt;VISSRSMS2IMVIS&lt;/h4&gt;
VISSRSMS2IMVIS is the Visible Infrared Spin-Scan Radiometer (VISSR) Visible Imagery on 70mm Film data product from the second Synchronous Meteorological Satellite (SMS-2). This set of visible imagery (0.55 to 0.70 micrometer) was originally produced on commercial image-generation equipment from digital tapes and was made available on 70-mm film, from which they were later scanned to digital TIFF image files. Each TIFF scan contains 2 or 3 pictures, and there are several hundred scans from an original 70 mm film roll which are combined into a ZIP file. Each picture contains a title on the top boundary and a 33-level gray scale on the right boundary that represents brightness temperatures. It may have a combination of the following options: 1) contrast enhancement, 2) image sectorization, and 3) 1/16-size imagery. The maximum effective size covers 500 sq km, represented by 4000 by 3904 pixels. Each element has a maximum resolution of 3.7 km. The title contains the satellite identification, picture number, picture type, coordinate numbers of the top left pixel relative to the visible sensor, start time of sectorized image, and pixel scaling and sector size identification. The SMS-2 satellite was initially parked over the equator at longitude 105W on Feb 22, 1975 viewing the hemisphere below the satellite. It was moved to its final operational position at 135W on Dec 19, 1975. The VISSR experiment was operated by the NOAA National Environmental Satellite Data and Information Service (NESDIS), as well as scientists from NASA Goddard Space Flight Center. This product was previously available from the NSSDC with the identifier ESAD-00202 (old ID 75-011A-04B).
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.laadsdaac.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA GPCP Project</title>
      <link>https://registry.opendata.aws/nasa-gpcp</link>
      <guid>https://registry.opendata.aws/nasa-gpcp</guid>
      <description>These data are transitioned to a state of permanent preservation. They are available upon request. More advanced datasets have been developed since. One recommended replacement is the GPCP (doi: 10.5067/DBVUO4KQHXTK) product developed under the MEaSUREs project. The Arkin and Janowiak GPI (GOES Precipitation Index) was the infrared-based monthly rainfall estimate produced by the early GPCP (Global Precipitation Climatology Project) algorithms. The infrared observations from geostationary satellites (GOES, GMS, Meteosat) are used to produce these monthly mean rainfall totals on a 2.5 deg by 2.5 deg grid from 40 N to 40 S for the period Jan 1986 to Dec 1995.
&lt;br&gt;&lt;h4 id&#x3D;&quot;rain_jaeger&quot;&gt;RAIN_JAEGER&lt;/h4&gt;
The Jaeger Surface Rain Gauge Observations data set consists of gridded mean monthly global precipitation values for 1931 to 1960 over the continents and 1955 to 1965 over the oceans. In order to calculate monthly, seasonal, and annual variations of precipitation over the whole globe, both hemispheres, and various meridional zones, a gridding technique was used on data spanning 1931 to 1960 over the continents, and 1955 to 1965 over the oceans. For the continental regions, the grid point values were obtained as eye estimates from isopleth maps prepared from up-to-date climatic atlases containing annual and monthly rainfall values, supplemented by other data sets. Although it was initially intended to use data for the standard period 1931-1960, this did not prove possible for all regions. Moller&amp;#39;s (1951) method for estimating rainfall frequencies was adopted to provide ocean precipitation data. Monthly percentage frequencies were extracted from the mapped isolines of the US Marine Climatic Atlas (US Naval Weather Service 1955-1965) and interpolated to the grid points. After re-expressing the monthly frequencies as annual percentages, the values were scaled to rainfall depth units using Geiger&amp;#39;s (1965) precipitation map to yield monthly precipitation means.
&lt;br&gt;&lt;h4 id&#x3D;&quot;rain_legates&quot;&gt;RAIN_LEGATES&lt;/h4&gt;
The Legates Surface and Shipboard Rain Gauge Observations data set consists of a global climatology of monthly mean precipitation values. A global climatology of mean monthly precipitation was developed using traditional land-based gauge measurements as well as extrapolations of oceanic precipitation from coastal and island observations. Data were obtained from a variety of source archives. These data were screened for coding errors, merged, and redundant stations were removed. The resulting data base contains 24,635 independent terrestrial station records and 2223 oceanic gridpoint estimates. Precipitation gauge catches, however, are known to underestimate actual precipitation. Errors in the gauge catch result from wind-field deformation above the orifice of the gauge, wetting losses, and evaporation from the gauge and amount globally to nearly 8, 2, and 1 percent of the catch, respectively. A procedure was developed to estimate these errors and was used to obtain better estimates of global precipitation. Spatial variations in gauge type, air temperature, wind speed, and natural vegetation have been interpolated to the nodes of a 0.5 degrees of latitude by 0.5 degrees of longitude lattice using a spherically-based interpolation algorithm. The data set is used to validate general circulation model simulations of the present-day precipitation climate, for ground-based comparison with satellite-derived precipitation estimates, and as a basis for global water balance studies.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA GPM Project</title>
      <link>https://registry.opendata.aws/nasa-gpm</link>
      <guid>https://registry.opendata.aws/nasa-gpm</guid>
      <description>Version 07 is the current version of the data set. Older versions will no longer be available and have been superseded by Version 07. The &amp;#39;CLIM&amp;#39; products differ from their &amp;#39;regular&amp;#39; counterparts (without the &amp;#39;CLIM&amp;#39; in the name) by the ancillary data they use. They are Climate-Reference products, which requires homogeneous ancillary data over the climate time series. Hence, the ECMWF-Interim (European Centre for Medium-Range Weather Forecasts, 2-3 months lag behind the regular production) reanalysis is used as ancillary data to derive surface and atmospheric conditions required by the GPROF algorithm for the &amp;#39;CLIM&amp;#39; output. The GPROF databases are also adjusted accordingly for these climate-referenced retrievals. The 2AGPROF (also known as, GPM GPROF (Level 2)) algorithm retrieves consistent precipitation and related science fields from the following GMI and partner passive microwave sensors: + TMI (TRMM) + GMI, (GPM) + SSMI (DMSP F15), SSMIS (DMSP F16, F17, F18, F19) + AMSR2 (GCOM-W1) + MHS (NOAA 18,19) + MHS (METOP A,B) + ATMS (NPP) + SAPHIR (MT1) This provides the bulk of the 3-hour coverage achieved by GPM. For each sensor, there are near-realtime (NRT) products, standard products, and climate products. These differ only in the amount of data that are available within 3 hours, 48 hours, and 3 months of collection, as well as the ancillary data used. The NRT product uses GANAL forecast fields. Standard products use the GANAL analysis product, while the climate product uses ECMWF reanalysis in order to allow for consistent data records with earlier missions. These earlier data may be archived separately. The main strength of the product is the large sampling provided. The GPM radiometer algorithms are Bayesian-type algorithms. These algorithms search an a-priori database of potential rain profiles and retrieve a weighted average of these entries based upon the proximity of the observed brightness temperature (Tb) to the simulated Tb corresponding to each rain profile. By using the same a-priori database of rain profiles, with appropriate simulated Tb for each constellation sensor, the Bayesian method is completely parametric and thus well suited for GPM&amp;#39;s constellation approach. The a-priori information will be supplied by the combined algorithm supplied by GPM&amp;#39;s core satellite as soon after launch as feasible. Databases for V0 of the algorithm had to be constructed from various sources as described in the ATBD. The solution provides a mean rain rate as well as the vertical structure of cloud and precipitation hydrometeors and their uncertainty.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpm_1caquaamsre&quot;&gt;GPM_1CAQUAAMSRE&lt;/h4&gt;
All 1C products have a common L1C data structure, simple and generic. Each L1C swath includes scan time, latitude and longitude, scan status, quality, incidence angle, Sun glint angle, and the intercalibrated brightness temperature (Tc). One or more swaths are included in a product. The radiometer data are recalibrated to a common basis so that precipitation products derived from them are consistent. 1CSSMIS contains common calibrated brightness temperature from the SSMIS passive microwave instruments flown on the DMSP satellites. Swath S1 has 3 low frequency channels (19V 19H 22V). Swath S2 has 2 low frequency channels (37V 37H). Swath S3 has 4 high frequency channels (150H 183+/-1H 183+/-3H 183+/-7H). S4 has 2 high frequency channels (91V 91H). All the above frequencies are in GHz. Earth observations for all four swaths are taken during a 144o segment of the instrument rotation when SSMIS scans in the direction of foreward satellite motion. We define the spacecraft vector (v) at the center of this segment.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpm_2agprofnoaa15amsub_clim&quot;&gt;GPM_2AGPROFNOAA15AMSUB_CLIM&lt;/h4&gt;
The &amp;#39;CLIM&amp;#39; products differ from their &amp;#39;regular&amp;#39; counterparts (without the &amp;#39;CLIM&amp;#39; in the name) by the ancillary data they use. They are Climate-Reference products, which requires homogeneous ancillary data over the climate time series. Hence, the ECMWF-Interim (European Centre for Medium-Range Weather Forecasts, 2-3 months lag behind the regular production) reanalysis is used as ancillary data to derive surface and atmospheric conditions required by the GPROF algorithm for the &amp;#39;CLIM&amp;#39; output. The GPROF databases are also adjusted accordingly for these climate-referenced retrievals. The 2AGPROF (Goddard Profiling) algorithm retrieves consistent precipitation and related science fields from the following GMI and partner passive microwave sensors: + TMI (TRMM) + GMI, (GPM) + SSMI (DMSP F11, F13, F14, F15); SSMIS (DMSP F16, F17, F18, F19) + AMSR2 (GCOM-W1) + MHS (NOAA 18,19) + MHS (METOP A,B) + ATMS (NPP) + SAPHIR (MT1) This provides the bulk of the 3-hour coverage achieved by GPM. For each sensor, there are nearrealtime (NRT) products, standard products, and climate products. These differ only in the amount of data that are available within 3 hours, 48 hours, and 3 months of collection, as well as the ancillary data used. The NRT product uses GANAL forecast fields. Standard products use the GANAL analysis product, while the climate product uses ECMWF reanalysis in order to allow for consistent data records with earlier missions. These earlier data may be archived separately. The main strength of the product is the large sampling provided. The GPM radiometer algorithms are Bayesian-type algorithms. These algorithms search an apriori database of potential rain profiles and retrieve a weighted average of these entries based upon the proximity of the observed brightness temperature (Tb) to the simulated Tb corresponding to each rain profile. By using the same a-priori database of rain profiles, with appropriate simulated Tb for each constellation sensor, the Bayesian method is completely parametric and thus well suited for GPM&amp;#39;s constellation approach. The a-priori information will be supplied by the combined algorithm supplied by GPM&amp;#39;s core satellite as soon after launch as feasible. Databases for V0 of the algorithm had to be constructed from various sources as described in the ATBD. The solution provides a mean rain rate as well as the vertical structure of cloud and precipitation hydrometeors and their uncertainty
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpm_3gprofnoaa15amsub_day_clim&quot;&gt;GPM_3GPROFNOAA15AMSUB_DAY_CLIM&lt;/h4&gt;
The &amp;quot;CLIM&amp;quot; products differ from their &amp;quot;regular&amp;quot; counterparts (without the &amp;quot;CLIM&amp;quot; in the name) by the ancillary data they use. They are Climate-Reference products, which requires homogeneous ancillary data over the climate time series. Hence, the ECMWF-Interim (European Centre for Medium-Range Weather Forecasts, 2-3 months lag behind the regular production) reanalysis is used as ancillary data to derive surface and atmospheric conditions required by the GPROF algorithm for the &amp;quot;CLIM&amp;quot; output. The GPROF databases are also adjusted accordingly for these climate-referenced retrievals. 3GPROF products provide global gridded monthly/daily precipitation averages from multiple satellites that can be used for climate studies. The 3GPROF products are based on retrievals from high-quality microwave sensors, which are sensitive to liquid and ice-phase precipitation hydrometeors in the atmosphere.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpm_2agprofnoaa20atms_clim&quot;&gt;GPM_2AGPROFNOAA20ATMS_CLIM&lt;/h4&gt;
Version 07 is the current version of the data set. The &amp;quot;CLIM&amp;quot; products differ from their &amp;quot;regular&amp;quot; counterparts (without the &amp;quot;CLIM&amp;quot; in the name) by the ancillary data they use. They are Climate-Reference products, which requires homogeneous ancillary data over the climate time series. Hence, the ECMWF-Interim (European Centre for Medium-Range Weather Forecasts, 2-3 months lag behind the regular production) reanalysis is used as ancillary data to derive surface and atmospheric conditions required by the GPROF algorithm for the &amp;quot;CLIM&amp;quot; output. The GPROF databases are also adjusted accordingly for these climate-referenced retrievals. The 2AGPROF (also known as, GPM GPROF (Level 2)) algorithm retrieves consistent precipitation and related science fields from the following GMI and partner passive microwave sensors: GMI, SSMI (DMSP F15), SSMIS (DMSP F16, F17, F18) AMSR2 (GCOM-W1), TMI MHS (NOAA 18&amp;amp;19, METOP A&amp;amp;B), ATMS (SNPP and NOAA-20). This provides the bulk of the 3-hour coverage achieved by GPM. For each sensor, there are near-realtime (NRT) products, standard products, and climate products. These differ only in the amount of data that are available within 3 hours, 48 hours, and 3 months of collection, as well as the ancillary data used. The NRT product uses GANAL forecast fields. Standard products use the GANAL analysis product, while the climate product uses ECMWF reanalysis in order to allow for consistent data records with earlier missions. These earlier data may be archived separately. The main strength of the product is the large sampling provided. The GPM radiometer algorithms are Bayesian-type algorithms. These algorithms search an a-priori database of potential rain profiles and retrieve a weighted average of these entries based upon the proximity of the observed brightness temperature (Tb) to the simulated Tb corresponding to each rain profile. By using the same a-priori database of rain profiles, with appropriate simulated Tb for each constellation sensor, the Bayesian method is completely parametric and thus well suited for GPM&amp;#39;s constellation approach. The a-priori information will be supplied by the combined algorithm supplied by GPM&amp;#39;s core satellite as soon after launch as feasible. Databases for V0 of the algorithm had to be constructed from various sources as described in the ATBD. The solution provides a mean rain rate as well as the vertical structure of cloud and precipitation hydrometeors and their uncertainty.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpm_3gprofnoaa20atms_day_clim&quot;&gt;GPM_3GPROFNOAA20ATMS_DAY_CLIM&lt;/h4&gt;
Version 07 is the current version of the data set. Older versions are no longer available and have been superseded by Version 07. The &amp;quot;CLIM&amp;quot; products differ from their &amp;quot;regular&amp;quot; counterparts (without the &amp;quot;CLIM&amp;quot; in the name) by the ancillary data they use. They are Climate-Reference products, which requires homogeneous ancillary data over the climate time series. Hence, the ECMWF-Interim (European Centre for Medium-Range Weather Forecasts, 2-3 months lag behind the regular production) reanalysis is used as ancillary data to derive surface and atmospheric conditions required by the GPROF algorithm for the &amp;quot;CLIM&amp;quot; output. The GPROF databases are also adjusted accordingly for these climate-referenced retrievals. 3GPROF products provide global gridded monthly/daily precipitation averages from multiple satellites that can be used for climate studies. The 3GPROF products are based on retrievals from high-quality microwave sensors, which are sensitive to liquid and ice-phase precipitation hydrometeors in the atmosphere.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpm_2agprofnoaa20atms&quot;&gt;GPM_2AGPROFNOAA20ATMS&lt;/h4&gt;
Version 07 is the current version of the data set. The 2AGPROF (also known as, GPM GPROF (Level 2)) algorithm retrieves consistent precipitation and related science fields from the following GMI and partner passive microwave sensors: GMI, SSMI (DMSP F15), SSMIS (DMSP F16, F17, F18) AMSR2 (GCOM-W1), TMI MHS (NOAA 18&amp;amp;19, METOP A&amp;amp;B), ATMS (SNPP and NOAA-20). This provides the bulk of the 3-hour coverage achieved by GPM. For each sensor, there are near-realtime (NRT) products, standard products, and climate products. These differ only in the amount of data that are available within 3 hours, 48 hours, and 3 months of collection, as well as the ancillary data used. The NRT product uses GANAL forecast fields. Standard products use the GANAL analysis product, while the climate product uses ECMWF reanalysis in order to allow for consistent data records with earlier missions. These earlier data may be archived separately. The main strength of the product is the large sampling provided. The GPM radiometer algorithms are Bayesian-type algorithms. These algorithms search an a-priori database of potential rain profiles and retrieve a weighted average of these entries based upon the proximity of the observed brightness temperature (Tb) to the simulated Tb corresponding to each rain profile. By using the same a-priori database of rain profiles, with appropriate simulated Tb for each constellation sensor, the Bayesian method is completely parametric and thus well suited for GPM&amp;#39;s constellation approach. The a-priori information will be supplied by the combined algorithm supplied by GPM&amp;#39;s core satellite as soon after launch as feasible. Databases for V0 of the algorithm had to be constructed from various sources as described in the ATBD. The solution provides a mean rain rate as well as the vertical structure of cloud and precipitation hydrometeors and their uncertainty.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpm_3gprofnoaa20atms&quot;&gt;GPM_3GPROFNOAA20ATMS&lt;/h4&gt;
Version 07 is the current version of the data set. 3GPROF products provide global gridded monthly/daily precipitation averages from multiple satellites that can be used for climate studies. The 3GPROF products are based on retrievals from high-quality microwave sensors, which are sensitive to liquid and ice-phase precipitation hydrometeors in the atmosphere.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpm_2agprofnoaa21atms&quot;&gt;GPM_2AGPROFNOAA21ATMS&lt;/h4&gt;
Version 07 is the current version of the data set. The 2AGPROF (also known as, GPM GPROF (Level 2)) algorithm retrieves consistent precipitation and related science fields from the following GMI and partner passive microwave sensors: GMI, SSMI (DMSP F15), SSMIS (DMSP F16, F17, F18) AMSR2 (GCOM-W1), TMI MHS (NOAA 18&amp;amp;19, METOP A&amp;amp;B), ATMS (SNPP and NOAA-21). This provides the bulk of the 3-hour coverage achieved by GPM. For each sensor, there are near-realtime (NRT) products, standard products, and climate products. These differ only in the amount of data that are available within 3 hours, 48 hours, and 3 months of collection, as well as the ancillary data used. The NRT product uses GANAL forecast fields. Standard products use the GANAL analysis product, while the climate product uses ECMWF reanalysis in order to allow for consistent data records with earlier missions. These earlier data may be archived separately. The main strength of the product is the large sampling provided. The GPM radiometer algorithms are Bayesian-type algorithms. These algorithms search an a-priori database of potential rain profiles and retrieve a weighted average of these entries based upon the proximity of the observed brightness temperature (Tb) to the simulated Tb corresponding to each rain profile. By using the same a-priori database of rain profiles, with appropriate simulated Tb for each constellation sensor, the Bayesian method is completely parametric and thus well suited for GPM&amp;#39;s constellation approach. The a-priori information will be supplied by the combined algorithm supplied by GPM&amp;#39;s core satellite as soon after launch as feasible. Databases for V0 of the algorithm had to be constructed from various sources as described in the ATBD. The solution provides a mean rain rate as well as the vertical structure of cloud and precipitation hydrometeors and their uncertainty.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpm_3gprofnppatms&quot;&gt;GPM_3GPROFNPPATMS&lt;/h4&gt;
3GPROF products provide global gridded monthly/daily precipitation averages from multiple satellites that can be used for climate studies. The 3GPROF products are based on retrievals from high-quality microwave sensors, which are sensitive to liquid and ice-phase precipitation hydrometeors in the atmosphere.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpm_3gcsh&quot;&gt;GPM_3GCSH&lt;/h4&gt;
The Gridded Convective Stratiform Heating (3GCSH) products contain latent heating, Q1-QR and Q2 profiles from DPR raindata. Version 07 is the current version of the data set. Older versions will no longer be available and are superseded by Version 07.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpm_3hcsh&quot;&gt;GPM_3HCSH&lt;/h4&gt;
The Gridded Convective Stratiform Heating (3HCSH) products contain latent heating, Q1-QR and Q2 profiles from DPR raindata. Version 07 is the current version of the data set. Older versions will no longer be available and are superseded by Version 07.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpm_2hslh&quot;&gt;GPM_2HSLH&lt;/h4&gt;
Version 6B of these data were introduced in July, 2020. Please, see documentation tab for release notes. Latent heating variables are retrieved utilizing two separate algorithms for tropics and for mid-latitudes. First, location of each GPM KuPR pixel is assigned to either tropics or mid-latitudes, depending on monthly maps of precipitation types determined in a similar manner as described in Takayabu (2008). Then, three dimensional convective latent heating are retrieved, Q1-QR (Q1R), and Q2, applying either tropical/mid-latitude algorithms to precipitation data observed from GPM DPR (KuPR). Here, Q1 and Q2 are apparent heat source and apparent moisture sink, respectively, introduced by Yanai et al. (1973), and QR is radiative heating of the atmosphere.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpm_basegpmgmi&quot;&gt;GPM_BASEGPMGMI&lt;/h4&gt;
Version 07 is the current version of the data set. Older versions are no longer available and have been superseded by the current version. GMI is a multi-channel, conical- scanning, microwave radiometer. The BASEGPMGMI product contains unaltered data directly from the Global Microwave Imager (GMI) aboard the GPM core satellite. It is the standard GMI calibration product with full precision of all physical fields. It contains one full orbit with no overlaps to other orbits in the production, although up to 200 overlap scans may be used for multi-scan calibration in the process. If there is enough bandwidth, the entire circle of GMI samples will be sent down. The BASEGPMGMI product&amp;#39;s swaths 4 and 5 contain all of the samples that are sent down. Later products only use the subset of these data that contains the Earth view, hot load, and cold sky samples.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpm_3imerghhe&quot;&gt;GPM_3IMERGHHE&lt;/h4&gt;
Version 07B is the current version of the IMERG data sets. Older versions will no longer be available and have been superseded by Version 07. The Integrated Multi-satellitE Retrievals for GPM (IMERG) is the unified U.S. algorithm that provides the multi-satellite precipitation product for the U.S. GPM team. The precipitation estimates from the various precipitation-relevant satellite passive microwave (PMW) sensors comprising the GPM constellation are computed using the 2021 version of the Goddard Profiling Algorithm (GPROF2021), then gridded, intercalibrated to the GPM Combined Ku Radar-Radiometer Algorithm (CORRA) product, and merged into half-hourly 0.1°x0.1° (roughly 10x10 km) fields. Note that CORRA is adjusted to the monthly Global Precipitation Climatology Project (GPCP) Satellite-Gauge (SG) product over high-latitude ocean to correct known biases. The half-hourly intercalibrated merged PMW estimates are then input to both a Morphing-Kalman Filter (KF) Lagrangian time interpolation scheme based on work by the Climate Prediction Center (CPC) and the Precipitation Estimation from Remotely Sensed Information using Artificial Neural Networks (PERSIANN) Dynamic Infrared–Rain Rate (PDIR) re-calibration scheme. In parallel, CPC assembles the zenith-angle-corrected, intercalibrated merged geo-IR fields and forwards them to PPS for input to the PERSIANN-CCS algorithm (supported by an asynchronous re-calibration cycle) which are then input to the KF morphing (quasi-Lagrangian time interpolation) scheme. The KF morphing (supported by an asynchronous KF weights updating cycle) uses the PMW and IR estimates to create half-hourly estimates. Motion vectors for the morphing are computed by maximizing the pattern correlation of successive hours within each of the precipitation (PRECTOT), total precipitable liquid water (TQL), and vertically integrated vapor (TQV) data fields provided by the Modern-Era Retrospective Analysis for Research and Applications, Version 2 (MERRA-2) and Goddard Earth Observing System model Version 5 (GEOS-5) Forward Processing (FP) for the post-real-time (Final) Run and the near-real-time (Early and Late) Runs, respectively. The vectors from PRECTOT are chosen if available, else from TQL, if available, else from TQV. The KF uses the morphed data as the “forecast” and the IR estimates as the “observations”, with weighting that depends on the time interval(s) away from the microwave overpass time. The IR becomes important after about ±90 minutes away from the overpass time. Variable averaging in the KF is accounted for in a routine (Scheme for Histogram Adjustment with Ranked Precipitation Estimates in the Neighborhood, or SHARPEN) that compares the local histogram of KF morphed precipitation to the local histogram of forward- and backward-morphed microwave data and the IR. The IMERG system is run twice in near-real time: &amp;quot;Early&amp;quot; multi-satellite product ~4 hr after observation time using only forward morphing and &amp;quot;Late&amp;quot; multi-satellite product ~14 hr after observation time, using both forward and backward morphing and once after the monthly gauge analysis is received: &amp;quot;Final&amp;quot;, satellite-gauge product ~4 months after the observation month, using both forward and backward morphing and including monthly gauge analyses. In V07, the near-real-time Early and Late half-hourly estimates have a monthly climatological concluding calibration based on averaging the concluding calibrations computed in the Final, while in the post-real-time Final Run the multi-satellite half-hourly estimates are adjusted so that they sum to the Final Run monthly satellite-gauge combination. In all cases the output contains multiple fields that provide information on the input data, selected intermediate fields, and estimation quality. In general, the complete calibrated precipitation, precipitation, is the data field of choice for most users. Precipitation phase is a diagnostic variable computed using analyses of surface temperature, humidity, and pressure.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpm_2agprofmetopcmhs&quot;&gt;GPM_2AGPROFMETOPCMHS&lt;/h4&gt;
Version 07 is the current version of the data set. The 2AGPROF (also known as, GPM GPROF (Level 2)) algorithm retrieves consistent precipitation and related science fields from the following GMI and partner passive microwave sensors: GMI, SSMI (DMSP F15), SSMIS (DMSP F16, F17, F18) AMSR2 (GCOM-W1), TMI MHS (NOAA 18&amp;amp;19, METOP A;B;C), ATMS (NPP), SAPHIR (MT1) This provides the bulk of the 3-hour coverage achieved by GPM. For each sensor, there are near-realtime (NRT) products, standard products, and climate products. These differ only in the amount of data that are available within 3 hours, 48 hours, and 3 months of collection, as well as the ancillary data used. The NRT product uses GANAL forecast fields. Standard products use the GANAL analysis product, while the climate product uses ECMWF reanalysis in order to allow for consistent data records with earlier missions. These earlier data may be archived separately. The main strength of the product is the large sampling provided. The GPM radiometer algorithms are Bayesian-type algorithms. These algorithms search an a-priori database of potential rain profiles and retrieve a weighted average of these entries based upon the proximity of the observed brightness temperature (Tb) to the simulated Tb corresponding to each rain profile. By using the same a-priori database of rain profiles, with appropriate simulated Tb for each constellation sensor, the Bayesian method is completely parametric and thus well suited for GPM&amp;#39;s constellation approach. The a-priori information will be supplied by the combined algorithm supplied by GPM&amp;#39;s core satellite as soon after launch as feasible. Databases for V0 of the algorithm had to be constructed from various sources as described in the ATBD. The solution provides a mean rain rate as well as the vertical structure of cloud and precipitation hydrometeors and their uncertainty. ABSTRACT
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpm_1cmetopcmhs&quot;&gt;GPM_1CMETOPCMHS&lt;/h4&gt;
Version 07 is the current version of the data set. 1CAMSR2 contains common calibrated brightness temperature from the AMSR2 passive microwave instrument flown on the GCOMW1 satellite. This products contains 6 swaths. Swath 1 has channels 10.65V 10.65H. Swath 2 has channels 18.7V 18.7H. Swath 3 has channels 23.8V 23.8H. Swath 4 has channels 36.5V 36.5H. Swath S5 has 2 high frequency A-Scan channels (89V 89H). Swath S6 has 2 high frequency B-Scan channels (89V 89H). Data for all six swaths is observed in the same revolution of the instrument. High frequency A and high frequency B data are observed in separate feedhorns. All 1C products have a common L1C data structure, simple and generic. Each L1C swath includes scan time, latitude and longitude, scan status, quality, incidence angle, Sun glint angle, and the intercalibrated brightness temperature (Tc). One or more swaths are included in a product. The radiometer data are recalibrated to a common basis so that precipitation products derived from them are consistent.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpm_3cmb_trmm_day&quot;&gt;GPM_3CMB_TRMM_DAY&lt;/h4&gt;
This a new (GPM-formated) TRMM product, for the TRMM epoch (December 1997 - April 2015), created using GPM Algorithms. There is no equivalent in the old TRMM suite of products. This is the GPM-like formatted TRMM Combined Precipitation (TRMM Ku radar and microwave radiometer/imager), first released with the &amp;quot;V8&amp;quot; TRMM reprocessing. Combined Radar-Radiometer Algorithm performs two basic functions: First, it provides, in principle, the most accurate, high resolution estimates of surface rainfall rate and precipitation vertical distributions that can be achieved from a spaceborne platform, and it is therefore valuable for applications where information regarding instantaneous storm structure are vital. Second, a global, representative collection of combined algorithm estimates will yield a single common reference dataset that can be used to “cross-calibrate” rain rate estimates from all of the passive microwave radiometers in the TRMM and GPM constellations. The cross-calibration of radiometer estimates is crucial for developing a consistent, high time-resolution precipitation record for climate science and prediction model validation applications.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpm_3cmb_trmm&quot;&gt;GPM_3CMB_TRMM&lt;/h4&gt;
This is the new (GPM-formated) TRMM Combined product, using the GPM algorithms, for the TRMM epoch (December 1997 - April 2015). It replaces the old TRMM_3B31 This is the GPM-like formatted TRMM Combined Precipitation (TRMM Ku radar and microwave radiometer/imager), first released with the &amp;quot;V8&amp;quot; TRMM reprocessing. The corresponding GPM Combined product is archived under the name GPM_3CMB, with beginning date March 2014. Gombined Radar-Radiometer Algorithm performs two basic functions: First, it provides, in principle, the most accurate, high resolution estimates of surface rainfall rate and precipitation vertical distributions that can be achieved from a spaceborne platform, and it is therefore valuable for applications where information regarding instantaneous storm structure are vital. Second, a global, representative collection of combined algorithm estimates will yield a single common reference dataset that can be used to “cross-calibrate” rain rate estimates from all of the passive microwave radiometers in the TRMM and GPM constellations. The cross-calibration of radiometer estimates is crucial for developing a consistent, high time-resolution precipitation record for climate science and prediction model validation applications.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpm_2bcmb_trmm&quot;&gt;GPM_2BCMB_TRMM&lt;/h4&gt;
This is the new (GPM-formated) TRMM Combined product, using the GPM algorithms, for the TRMM epoch (December 1997 - April 2015). It replaces the old TRMM_2B31 This is the GPM-like formatted TRMM Combined Precipitation (TRMM Ku radar and microwave radiometer/imager), first released with the &amp;quot;V8&amp;quot; TRMM reprocessing. The corresponding GPM Combined product is archived under the name GPM_2BCMB, with beginning date March 2014. Gombined Radar-Radiometer Algorithm performs two basic functions: First, it provides, in principle, the most accurate, high resolution estimates of surface rainfall rate and precipitation vertical distributions that can be achieved from a spaceborne platform, and it is therefore valuable for applications where information regarding instantaneous storm structure are vital. Second, a global, representative collection of combined algorithm estimates will yield a single common reference dataset that can be used to “cross-calibrate” rain rate estimates from all of the passive microwave radiometers in the TRMM and GPM constellations. The cross-calibration of radiometer estimates is crucial for developing a consistent, high time-resolution precipitation record for climate science and prediction model validation applications.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpm_2aprpsmt1saphir_clim&quot;&gt;GPM_2APRPSMT1SAPHIR_CLIM&lt;/h4&gt;
Version 6 is the current version of this dataset. Older versions are no longer available and have been superseded by Version 6. The Precipitation Retrieval and Profiling Scheme (PRPS)is designed to provide a best estimate of precipitation based upon matched SAPHIR-DPR observations. This fulfils in part the essence of GPM (and its predecessor, TRMM) in which the core observatory acts as a calibrator of precipitation retrievals for the international constellation of passive microwave instruments. In doing so the retrievals from the partner constellation sensors are able to provide greater temporal sampling and great spatial coverage than is possible from the DPR instrument alone. However, the limitations of the DPR instrument are transferred through the retrieval scheme to the resulting precipitation products. Fundamental to the design of the PRPS is the independence from any dynamic ancillary data sets: the retrieval is based solely upon the satellite radiances, a static a priori radiance-rainrate database (and index), and (static) topographical data. Critically, the technique is independent of any model information, unlike the retrievals generated through the Goddard PROFiling (GPROF) scheme: this independence is advantageous when generating products across time scales from near real-time (inaccessibility to model data) to climatological scales (circumventing trends in model data). The algorithm is designed to generate instantaneous estimates of precipitation at a constant resolution (regardless of scan position), for all scan positions and scan lines. In addition to the actual precipitation estimate, an assessment of the error is made, and a measure of the ‘fit’ of the observations to the database provided. A quality flag is also provided, with any bad data generating a ‘missing flag’ in the retrieval.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpm_2agproff08ssmi_clim&quot;&gt;GPM_2AGPROFF08SSMI_CLIM&lt;/h4&gt;
Version 7 is the current version of the data set. Older versions will no longer be available and have been superseded by the current version. The &amp;#39;CLIM&amp;#39; products differ from their &amp;#39;regular&amp;#39; counterparts (without the &amp;#39;CLIM&amp;#39; in the name) by the ancillary data they use. They are Climate-Reference products, which requires homogeneous ancillary data over the climate time series. Hence, the ECMWF-Interim (European Centre for Medium-Range Weather Forecasts, 2-3 months lag behind the regular production) reanalysis is used as ancillary data to derive surface and atmospheric conditions required by the GPROF algorithm for the &amp;#39;CLIM&amp;#39; output. The GPROF databases are also adjusted accordingly for these climate-referenced retrievals. The 2AGPROF (Goddard Profiling) algorithm retrieves consistent precipitation and related science fields from the following GMI and partner passive microwave sensors: + TMI (TRMM) + GMI, (GPM) + SSMI (DMSP F11, F13, F14, F15); SSMIS (DMSP F16, F17, F18, F19) + AMSR2 (GCOM-W1) + MHS (NOAA 18,19) + MHS (METOP A,B) + ATMS (NPP) + SAPHIR (MT1) This provides the bulk of the 3-hour coverage achieved by GPM. For each sensor, there are nearrealtime (NRT) products, standard products, and climate products. These differ only in the amount of data that are available within 3 hours, 48 hours, and 3 months of collection, as well as the ancillary data used. The NRT product uses GANAL forecast fields. Standard products use the GANAL analysis product, while the climate product uses ECMWF reanalysis in order to allow for consistent data records with earlier missions. These earlier data may be archived separately. The main strength of the product is the large sampling provided. The GPM radiometer algorithms are Bayesian-type algorithms. These algorithms search an apriori database of potential rain profiles and retrieve a weighted average of these entries based upon the proximity of the observed brightness temperature (Tb) to the simulated Tb corresponding to each rain profile. By using the same a-priori database of rain profiles, with appropriate simulated Tb for each constellation sensor, the Bayesian method is completely parametric and thus well suited for GPM&amp;#39;s constellation approach. The a-priori information will be supplied by the combined algorithm supplied by GPM&amp;#39;s core satellite as soon after launch as feasible. Databases for V0 of the algorithm had to be constructed from various sources as described in the ATBD. The solution provides a mean rain rate as well as the vertical structure of cloud and precipitation hydrometeors and their uncertainty.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpm_2agproftrmmtmi_clim&quot;&gt;GPM_2AGPROFTRMMTMI_CLIM&lt;/h4&gt;
This is the new (GPM-formated) TRMM product. It replaces the old TRMM_2A12 Version 07 is the current version of the data set. Older versions will no longer be available and have been superseded by Version 07. The &amp;quot;CLIM&amp;quot; products differ from their &amp;quot;regular&amp;quot; counterparts (without the &amp;quot;CLIM&amp;quot; in the name) by the ancillary data they use. They are Climate-Reference products, which requires homogeneous ancillary data over the climate time series. Hence, the ECMWF-Interim (European Centre for Medium-Range Weather Forecasts, 2-3 months lag behind the regular production) reanalysis is used as ancillary data to derive surface and atmospheric conditions required by the GPROF algorithm for the &amp;quot;CLIM&amp;quot; output. The GPROF databases are also adjusted accordingly for these climate-referenced retrievals. The 2AGPROF (Goddard Profiling) algorithm retrieves consistent precipitation and related science fields from the following GMI and partner passive microwave sensors: + TMI (TRMM) + GMI, (GPM) + SSMI (DMSP F15), SSMIS (DMSP F16, F17, F18, F19) + AMSR2 (GCOM-W1) + MHS (NOAA 18,19) + MHS (METOP A,B) + ATMS (NPP) + SAPHIR (MT1) This provides the bulk of the 3-hour coverage achieved by GPM. For each sensor, there are nearrealtime (NRT) products, standard products, and climate products. These differ only in the amount of data that are available within 3 hours, 48 hours, and 3 months of collection, as well as the ancillary data used. The NRT product uses GANAL forecast fields. Standard products use the GANAL analysis product, while the climate product uses ECMWF reanalysis in order to allow for consistent data records with earlier missions. These earlier data may be archived separately. The main strength of the product is the large sampling provided. The GPM radiometer algorithms are Bayesian-type algorithms. These algorithms search an apriori database of potential rain profiles and retrieve a weighted average of these entries based upon the proximity of the observed brightness temperature (Tb) to the simulated Tb corresponding to each rain profile. By using the same a-priori database of rain profiles, with appropriate simulated Tb for each constellation sensor, the Bayesian method is completely parametric and thus well suited for GPM&amp;#39;s constellation approach. The a-priori information will be supplied by the combined algorithm supplied by GPM&amp;#39;s core satellite as soon after launch as feasible. Databases for V0 of the algorithm had to be constructed from various sources as described in the ATBD. The solution provides a mean rain rate as well as the vertical structure of cloud and precipitation hydrometeors and their uncertainty.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpm_3gproftrmmtmi_day_clim&quot;&gt;GPM_3GPROFTRMMTMI_DAY_CLIM&lt;/h4&gt;
This a new (GPM-formated) TRMM product. There is no equivalent in the old TRMM suite of products. Version 07 is the current version of the data set. Older versions will no longer be available and have been superseded by Version 07. The &amp;quot;CLIM&amp;quot; products differ from their &amp;quot;regular&amp;quot; counterparts (without the &amp;quot;CLIM&amp;quot; in the name) by the ancillary data they use. They are Climate-Reference products, which requires homogeneous ancillary data over the climate time series. Hence, the ECMWF-Interim (European Centre for Medium-Range Weather Forecasts, 2-3 months lag behind the regular production) reanalysis is used as ancillary data to derive surface and atmospheric conditions required by the GPROF algorithm for the &amp;quot;CLIM&amp;quot; output. The GPROF databases are also adjusted accordingly for these climate-referenced retrievals. 3GPROF products provide global gridded monthly/daily precipitation averages from multiple satellites that can be used for climate studies. The 3GPROF products are based on retrievals from high-quality microwave sensors, which are sensitive to liquid and ice-phase precipitation hydrometeors in the atmosphere.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpm_3gproftrmmtmi_clim&quot;&gt;GPM_3GPROFTRMMTMI_CLIM&lt;/h4&gt;
This is the new (GPM-formated) TRMM product. It replaces the old TRMM_3A12,3A11 Version 07 is the current version of the data set. Older versions will no longer be available and have been superseded by Version 07. The &amp;quot;CLIM&amp;quot; products differ from their &amp;quot;regular&amp;quot; counterparts (without the &amp;quot;CLIM&amp;quot; in the name) by the ancillary data they use. They are Climate-Reference products, which requires homogeneous ancillary data over the climate time series. Hence, the ECMWF-Interim (European Centre for Medium-Range Weather Forecasts, 2-3 months lag behind the regular production) reanalysis is used as ancillary data to derive surface and atmospheric conditions required by the GPROF algorithm for the &amp;quot;CLIM&amp;quot; output. The GPROF databases are also adjusted accordingly for these climate-referenced retrievals. 3GPROF products provide global gridded monthly/daily precipitation averages from multiple satellites that can be used for climate studies. The 3GPROF products are based on retrievals from high-quality microwave sensors, which are sensitive to liquid and ice-phase precipitation hydrometeors in the atmosphere.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpm_imerg_landseamask&quot;&gt;GPM_IMERG_LandSeaMask&lt;/h4&gt;
Version 2 is the current version of the data set. Older versions will no longer be available and have been superseded by Version 2. This land sea mask originated from the NOAA group at SSEC in the 1980s. It was originally produced at 1/6 deg resolution, and then regridded for the purposes of GPCP, TMPA, and IMERG precipitation products. NASA code 610.2, Terrestrial Information Systems Laboratory, restructured this land sea mask to match the IMERG grid, and converted the file to CF-compliant netCDF4. Version 2 was created in May, 2019 to resolve detected inaccuracies in coastal regions. Users should be aware that this is a static mask, i.e. there is no seasonal or annual variability, and it is due for update. It is not recommended to be used outside of the aforementioned precipitation data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpm_mergir&quot;&gt;GPM_MERGIR&lt;/h4&gt;
These data originate from NOAA/NCEP. The NOAA Climate Prediction Center/NCEP/NWS is making the data available originally in binary format, in a weekly rotating archive. The NASA GES DISC is acquiring the binary files as they become available, converts them into CF (Climate and Forecast) -convention compliant netCDF-4 format, and stores the product in a permanent archive. The original record started from February, 2000, but in June, 2025 it was extended back to January, 1998. The leading edge of data availability is delayed by about 24 hours from real-time to abide by international data exchange agreements between NOAA and EUMETSAT (the METEOSAT data providers). The data contain globally-merged (60°S-60°N) 4-km pixel-resolution IR brightness temperature data (equivalent blackbody temps), merged from the European, Japanese, and U.S. geostationary satellites over the period of record (GOES-8/9/10/11/12/13/14/15/16/17/18/19, METEOSAT-5/7/8/9/10/11, and GMS-5/MTSat-1R/2/Himawari-8/9). The global geo-IR are dynamically calibrated to GOES East, using a 35 day trailing inter-calibration using time/space-matched IR Tb’s at the mid-point between sub-satellite positions. In the event of duplicate data in a grid box, the value with the smaller zenith angle is taken. The data have been corrected for &amp;quot;zenith angle dependence&amp;quot;, in which IR temperatures for locations far from satellite nadir are erroneously cold due to a combination of geometric effects and radiometric path extinction effects (Joyce et al. 2001). Finally, the data are re-navigated for parallax, which shifts the geo-location of the GEO-IR footprints to approximately account for the cloud tops that the IR “sees” being displaced away from their actual geographic location when viewed along a slanted path. These corrections allow for the merging of the IR data from the various GEO-satellites with greatly reduced discontinuities at GEO-satellite data boundaries. In the event of duplicate data in a grid box, the value with the smaller zenith angle is taken. The NASA GES DISC is curating these data in a self-documenting, CF-compliant, netCDF-4 format, which allows a broad range of applications to access the data directly, without the need to cope with the original binary data format. In addition to the direct download of netCDF-4 data, the GES DISC provides data download in binary, ASCII, and netCDF-3 formats using the OPeNDAP interface which also provides remote data access. Similarities with the original ----------------------------- As in the original binaries, every netCDF-4 file covers one hour, and contains two half-hourly grids, at 4-km grid cell resolution. Differences from the original ----------------------------- 1. The data in the netCDF-4 files are already converted to physical values of Brightness Temperatures in Kelvin. Because the original data values are round with no decimal precision, the data type in the netCDF-4 files has been changed to 2-byte signed integer, a transition that took place in mid-August, 2025. This reduces the file size and speeds up data download and remote access. There is no need to further scale these data. The netCDF-4 format is machine-independent and users need not worry about the endian-ness of their machines. 2. To meet the requirements of collection spatial metadata, the grid is re-ordered from the original and now goes from -180 (West) to 180 (East). It is also starting from -60 (South). The data and time units are reflected in the corresponding &amp;quot;units&amp;quot; attributes, and grid dimensions are described by longitude (&amp;quot;lon&amp;quot;), latitude (&amp;quot;lat&amp;quot;) and &amp;quot;time&amp;quot; vectors. Thus, any CF-compliant tool should automatically understand the setup in the data files and the starting time for each half-hourly grid. Even without such tools, simple &amp;quot;ncdump&amp;quot; or &amp;quot;h5dump&amp;quot; command line tools will easily disclose the netCDF-4 files configuration. Acknowledgements ------------------ The creation of the original data at NOAA/NCEP is supported by funding from the NOAA Office of Global Programs for the Global Precipitation Climatology Project (GPCP) and by NASA via the Tropical Rainfall Measuring Mission (TRMM). The permanent archive at GES DISC is supported by NASA&amp;#39;s HQ Earth Science Data Systems (ESDS) Program.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA GRACE Project</title>
      <link>https://registry.opendata.aws/nasa-grace</link>
      <guid>https://registry.opendata.aws/nasa-grace</guid>
      <description>The monthly land mass grids contain water mass anomalies given as equivalent water thickness derived from GRACE &amp;amp; GRACE-FO time-variable gravity observations during the specified timespan, and relative to the specified time-mean reference period. The Equivalent water thickness represents the total terrestrial water storage anomalies from soil moisture, snow, surface water (incl. rivers, lakes, reservoirs etc.), as well as groundwater and aquifers. A glacial isostatic adjustment (GIA) correction has been applied, and standard corrections for geocenter (degree-1), C20 (degree-20) and C30 (degree-30) are incorporated. Post-processing filters have been applied to reduce correlated errors. Version 04 (v04) of the terrestrial water storage data uses updated and consistent C20 and Geocenter corrections (i.e., Technical Notes TN-14 and TN-13), as well as an ellipsoidal correction to account for the non-spherical shape of the Earth when mapping gravity anomalies to surface mass change. Data grids are provided in ASCII/netCDF/GeoTIFF formats. For the RL06 version, all GRACE products in the ASCII format have adopted the YAML encoding header, which is in full compliance with the PODAAC metadata best practices.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tellus_grac_l3_csr_rl06_ocn_v04&quot;&gt;TELLUS_GRAC_L3_CSR_RL06_OCN_v04&lt;/h4&gt;
The monthly ocean bottom pressure anomaly grids are given as equivalent water thickness changes derived from GRACE &amp;amp; GRACE-FO time-variable gravity observations during the specified timespan, and relative to the specified time-mean reference period. The Equivalent water thickness represent sea floor pressure changes due to the integral effect of ocean and atmosphere processes, including global mean ocean bottom pressure changes (mean ocean mass and mean atmosphere mass over the global oceans). The Level-2 GAD product has been added back, a glacial isostatic adjustment (GIA) correction has been applied, and standard corrections for geocenter (degree-1), C20 (degree-20) and C30 (degree-30) are incorporated. Post-processing filters (i.e., de-striping and spatial smoothing) have been applied to reduce correlated errors. Version 04 (v04) of the ocean bottom pressure data uses updated and consistent C20 and Geocenter corrections (i.e., Technical Notes TN-14 and TN-13), as well as an ellipsoidal correction to account for the non-spherical shape of the Earth when mapping gravity anomalies to surface mass change. Data grids are provided in ASCII/netCDF/GeoTIFF formats. For the RL06 version, all GRACE products in the ASCII format have adopted the YAML encoding header, which is in full compliance with the PODAAC metadata best practices.
&lt;br&gt;&lt;h4 id&#x3D;&quot;grace_aod1b_grav_gfz_rl06&quot;&gt;GRACE_AOD1B_GRAV_GFZ_RL06&lt;/h4&gt;
The GRACE Atmosphere and Ocean De-aliasing dataset contains spherical harmonic coefficients of combined barotropic or baroclinic sea level and vertical integrated pressure variations at 6-hour sample rate. It is used as a correction product for the Level 2 GRACE datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;grace_gsm_l2_grav_csr_rl06&quot;&gt;GRACE_GSM_L2_GRAV_CSR_RL06&lt;/h4&gt;
FOR EXPERT USE ONLY. This dataset contains estimates of static field geopotential of the Earth, derived from the Gravity Recovery and Climate Experiment (GRACE) mission measurements, produced by the Center for Space Research (CSR) at University of Texas at Austin. The data are in spherical harmonics averaged over approximately a month. The primary objective of the GRACE mission is to obtain accurate estimates of the mean and time-variable components of the gravity field variations. This objective is achieved by making continuous measurements of the change in distance between twin spacecraft, co-orbiting in about 500 km altitude, near circular, polar orbit, spaced approximately 200 km apart, using a microwave ranging system. In addition to these range change, the non-gravitional forces are measured on each satellite using a high accuracy electrostatic, room-temperature accelerometer. The satellite orientation and position (and timing) are precisely measured using twin star cameras and a GPS receiver, respectively. Spatial and temporal variations in the gravity field affect the orbits (or trajectories) of the twin spacecraft differently. These differences are manifested as changes in the distance between the spacecraft, as they orbit the Earth. This change in distance is reflected in the time-of-flight of microwave signals transmitted and received nearly simultaneously between the two spacecraft. The change in this time of fight is continuously measured by tracking the phase of the microwave carrier signals. The so called dual-one-way range change measurements can be reconstructed from these phase measurements. This range change (or its numerically derived derivatives), along with other mission and ancillary data, is subsequently analyzed to extract the parameters of an Earth gravity field model.
&lt;br&gt;&lt;h4 id&#x3D;&quot;grace_gsm_l2_grav_gfz_rl06&quot;&gt;GRACE_GSM_L2_GRAV_GFZ_RL06&lt;/h4&gt;
FOR EXPERT USE ONLY. This dataset contains estimates of static field geopotential of the Earth, derived from the Gravity Recovery and Climate Experiment (GRACE) mission measurements, produced by the German Research Centre for Geosciences (GFZ). The data are in spherical harmonics averaged over approximately a month. The primary objective of the GRACE mission is to obtain accurate estimates of the mean and time-variable components of the gravity field variations. This objective is achieved by making continuous measurements of the change in distance between twin spacecraft, co-orbiting in about 500 km altitude, near circular, polar orbit, spaced approximately 200 km apart, using a microwave ranging system. In addition to these range change, the non-gravitional forces are measured on each satellite using a high accuracy electrostatic, room-temperature accelerometer. The satellite orientation and position (and timing) are precisely measured using twin star cameras and a GPS receiver, respectively. Spatial and temporal variations in the gravity field affect the orbits (or trajectories) of the twin spacecraft differently. These differences are manifested as changes in the distance between the spacecraft, as they orbit the Earth. This change in distance is reflected in the time-of-flight of microwave signals transmitted and received nearly simultaneously between the two spacecraft. The change in this time of fight is continuously measured by tracking the phase of the microwave carrier signals. The so called dual-one-way range change measurements can be reconstructed from these phase measurements. This range change (or its numerically derived derivatives), along with other mission and ancillary data, is subsequently analyzed to extract the parameters of an Earth gravity field model.
&lt;br&gt;&lt;h4 id&#x3D;&quot;grace_gsm_l2_grav_jpl_rl06&quot;&gt;GRACE_GSM_L2_GRAV_JPL_RL06&lt;/h4&gt;
FOR EXPERT USE ONLY. This dataset contains estimates of static field geopotential of the Earth, derived from the Gravity Recovery and Climate Experiment (GRACE) mission measurements, produced by the NASA Jet Propulsion Laboratory (JPL). The data are in spherical harmonics averaged over approximately a month. The primary objective of the GRACE mission is to obtain accurate estimates of the mean and time-variable components of the gravity field variations. This objective is achieved by making continuous measurements of the change in distance between twin spacecraft, co-orbiting in about 500 km altitude, near circular, polar orbit, spaced approximately 200 km apart, using a microwave ranging system. In addition to these range change, the non-gravitional forces are measured on each satellite using a high accuracy electrostatic, room-temperature accelerometer. The satellite orientation and position (and timing) are precisely measured using twin star cameras and a GPS receiver, respectively. Spatial and temporal variations in the gravity field affect the orbits (or trajectories) of the twin spacecraft differently. These differences are manifested as changes in the distance between the spacecraft, as they orbit the Earth. This change in distance is reflected in the time-of-flight of microwave signals transmitted and received nearly simultaneously between the two spacecraft. The change in this time of fight is continuously measured by tracking the phase of the microwave carrier signals. The so called dual-one-way range change measurements can be reconstructed from these phase measurements. This range change (or its numerically derived derivatives), along with other mission and ancillary data, is subsequently analyzed to extract the parameters of an Earth gravity field model.
&lt;br&gt;&lt;h4 id&#x3D;&quot;grace_l1b_grav_jpl_rl02&quot;&gt;GRACE_L1B_GRAV_JPL_RL02&lt;/h4&gt;
FOR EXPERT USE ONLY. The GRACE Level 1B data provide all necessary inputs to derive monthly time variations in the Earth&amp;#39;s gravity field. Level 1B data are also used for GRACE orbit and mean gravity field determination. It contains K-Band Ranging Data Product (KBR1B), Star Camera Data Product (SCA1B), Accelerometer Data Product (ACC1B), GPS Data Product (GPS1B), Vector Products (VGN1B, VGO1B, VGB1B, VCM1B, VKB1B, VSL1B), Quaternion Products (QSA1B, QSB1B), and Housekeeping Products (AHK1B, IHK1B, THR1B, TNK1B, MAG1B, MAS1B, TIM1B)
&lt;br&gt;&lt;h4 id&#x3D;&quot;grace_gac_l2_grav_csr_rl06&quot;&gt;GRACE_GAC_L2_GRAV_CSR_RL06&lt;/h4&gt;
FOR EXPERT USE ONLY. This dataset contains estimates of geopotential field derived from the Gravity Recovery and Climate Experiment (GRACE) mission measurements and a non-tidal oceanic and atmospheric model produced by the Center for Space Research (CSR) at University of Texas at Austin. The data are in spherical harmonics averaged over approximately a month. The primary objective of the GRACE mission is to obtain accurate estimates of the mean and time-variable components of the gravity field variations. This objective is achieved by making continuous measurements of the change in distance between twin spacecraft, co-orbiting in about 500 km altitude, near circular, polar orbit, spaced approximately 200 km apart, using a microwave ranging system. In addition to these range change, the non-gravitional forces are measured on each satellite using a high accuracy electrostatic, room-temperature accelerometer. The satellite orientation and position (and timing) are precisely measured using twin star cameras and a GPS receiver, respectively. Spatial and temporal variations in the gravity field affect the orbits (or trajectories) of the twin spacecraft differently. These differences are manifested as changes in the distance between the spacecraft, as they orbit the Earth. This change in distance is reflected in the time-of-flight of microwave signals transmitted and received nearly simultaneously between the two spacecraft. The change in this time of fight is continuously measured by tracking the phase of the microwave carrier signals. The so called dual-one-way range change measurements can be reconstructed from these phase measurements. This range change (or its numerically derived derivatives), along with other mission and ancillary data, is subsequently analyzed to extract the parameters of an Earth gravity field model.
&lt;br&gt;&lt;h4 id&#x3D;&quot;grace_gac_l2_grav_gfz_rl06&quot;&gt;GRACE_GAC_L2_GRAV_GFZ_RL06&lt;/h4&gt;
FOR EXPERT USE ONLY. This dataset contains estimates of geopotential field derived from the Gravity Recovery and Climate Experiment (GRACE) mission measurements and a non-tidal oceanic and atmospheric model produced by the German Research Centre for Geosciences (GFZ). The data are in spherical harmonics averaged over approximately a month. The primary objective of the GRACE mission is to obtain accurate estimates of the mean and time-variable components of the gravity field variations. This objective is achieved by making continuous measurements of the change in distance between twin spacecraft, co-orbiting in about 500 km altitude, near circular, polar orbit, spaced approximately 200 km apart, using a microwave ranging system. In addition to these range change, the non-gravitional forces are measured on each satellite using a high accuracy electrostatic, room-temperature accelerometer. The satellite orientation and position (and timing) are precisely measured using twin star cameras and a GPS receiver, respectively. Spatial and temporal variations in the gravity field affect the orbits (or trajectories) of the twin spacecraft differently. These differences are manifested as changes in the distance between the spacecraft, as they orbit the Earth. This change in distance is reflected in the time-of-flight of microwave signals transmitted and received nearly simultaneously between the two spacecraft. The change in this time of fight is continuously measured by tracking the phase of the microwave carrier signals. The so called dual-one-way range change measurements can be reconstructed from these phase measurements. This range change (or its numerically derived derivatives), along with other mission and ancillary data, is subsequently analyzed to extract the parameters of an Earth gravity field model.
&lt;br&gt;&lt;h4 id&#x3D;&quot;grace_gac_l2_grav_jpl_rl06&quot;&gt;GRACE_GAC_L2_GRAV_JPL_RL06&lt;/h4&gt;
FOR EXPERT USE ONLY. This dataset contains estimates of geopotential field derived from the Gravity Recovery and Climate Experiment (GRACE) mission measurements and a non-tidal oceanic and atmospheric model produced by the NASA Jet Propulsion Laboratory (JPL). The data are in spherical harmonics averaged over approximately a month. The primary objective of the GRACE mission is to obtain accurate estimates of the mean and time-variable components of the gravity field variations. This objective is achieved by making continuous measurements of the change in distance between twin spacecraft, co-orbiting in about 500 km altitude, near circular, polar orbit, spaced approximately 200 km apart, using a microwave ranging system. In addition to these range change, the non-gravitional forces are measured on each satellite using a high accuracy electrostatic, room-temperature accelerometer. The satellite orientation and position (and timing) are precisely measured using twin star cameras and a GPS receiver, respectively. Spatial and temporal variations in the gravity field affect the orbits (or trajectories) of the twin spacecraft differently. These differences are manifested as changes in the distance between the spacecraft, as they orbit the Earth. This change in distance is reflected in the time-of-flight of microwave signals transmitted and received nearly simultaneously between the two spacecraft. The change in this time of fight is continuously measured by tracking the phase of the microwave carrier signals. The so called dual-one-way range change measurements can be reconstructed from these phase measurements. This range change (or its numerically derived derivatives), along with other mission and ancillary data, is subsequently analyzed to extract the parameters of an Earth gravity field model.
&lt;br&gt;&lt;h4 id&#x3D;&quot;grace_gaa_l2_grav_gfz_rl06&quot;&gt;GRACE_GAA_L2_GRAV_GFZ_RL06&lt;/h4&gt;
FOR EXPERT USE ONLY. This dataset contains estimates of geopotential field derived from the Gravity Recovery and Climate Experiment (GRACE) mission measurements and a non-tidal atmospheric model produced by the German Research Centre for Geosciences (GFZ). The data are in spherical harmonics averaged over approximately a month. The primary objective of the GRACE mission is to obtain accurate estimates of the mean and time-variable components of the gravity field variations. This objective is achieved by making continuous measurements of the change in distance between twin spacecraft, co-orbiting in about 500 km altitude, near circular, polar orbit, spaced approximately 200 km apart, using a microwave ranging system. In addition to these range change, the non-gravitional forces are measured on each satellite using a high accuracy electrostatic, room-temperature accelerometer. The satellite orientation and position (and timing) are precisely measured using twin star cameras and a GPS receiver, respectively. Spatial and temporal variations in the gravity field affect the orbits (or trajectories) of the twin spacecraft differently. These differences are manifested as changes in the distance between the spacecraft, as they orbit the Earth. This change in distance is reflected in the time-of-flight of microwave signals transmitted and received nearly simultaneously between the two spacecraft. The change in this time of fight is continuously measured by tracking the phase of the microwave carrier signals. The so called dual-one-way range change measurements can be reconstructed from these phase measurements. This range change (or its numerically derived derivatives), along with other mission and ancillary data, is subsequently analyzed to extract the parameters of an Earth gravity field model.
&lt;br&gt;&lt;h4 id&#x3D;&quot;grace_gaa_l2_grav_jpl_rl06&quot;&gt;GRACE_GAA_L2_GRAV_JPL_RL06&lt;/h4&gt;
FOR EXPERT USE ONLY. This dataset contains estimates of geopotential field derived from the Gravity Recovery and Climate Experiment (GRACE) mission measurements and a non-tidal atmospheric model produced by the NASA Jet Propulsion Laboratory (JPL). The data are in spherical harmonics averaged over approximately a month. The primary objective of the GRACE mission is to obtain accurate estimates of the mean and time-variable components of the gravity field variations. This objective is achieved by making continuous measurements of the change in distance between twin spacecraft, co-orbiting in about 500 km altitude, near circular, polar orbit, spaced approximately 200 km apart, using a microwave ranging system. In addition to these range change, the non-gravitional forces are measured on each satellite using a high accuracy electrostatic, room-temperature accelerometer. The satellite orientation and position (and timing) are precisely measured using twin star cameras and a GPS receiver, respectively. Spatial and temporal variations in the gravity field affect the orbits (or trajectories) of the twin spacecraft differently. These differences are manifested as changes in the distance between the spacecraft, as they orbit the Earth. This change in distance is reflected in the time-of-flight of microwave signals transmitted and received nearly simultaneously between the two spacecraft. The change in this time of fight is continuously measured by tracking the phase of the microwave carrier signals. The so called dual-one-way range change measurements can be reconstructed from these phase measurements. This range change (or its numerically derived derivatives), along with other mission and ancillary data, is subsequently analyzed to extract the parameters of an Earth gravity field model.
&lt;br&gt;&lt;h4 id&#x3D;&quot;grace_gab_l2_grav_gfz_rl06&quot;&gt;GRACE_GAB_L2_GRAV_GFZ_RL06&lt;/h4&gt;
FOR EXPERT USE ONLY. This dataset contains estimates of geopotential field derived from the Gravity Recovery and Climate Experiment (GRACE) mission measurements and a non-tidal oceanic model produced by the German Research Centre for Geosciences (GFZ). The data are in spherical harmonics averaged over approximately a month. The primary objective of the GRACE mission is to obtain accurate estimates of the mean and time-variable components of the gravity field variations. This objective is achieved by making continuous measurements of the change in distance between twin spacecraft, co-orbiting in about 500 km altitude, near circular, polar orbit, spaced approximately 200 km apart, using a microwave ranging system. In addition to these range change, the non-gravitional forces are measured on each satellite using a high accuracy electrostatic, room-temperature accelerometer. The satellite orientation and position (and timing) are precisely measured using twin star cameras and a GPS receiver, respectively. Spatial and temporal variations in the gravity field affect the orbits (or trajectories) of the twin spacecraft differently. These differences are manifested as changes in the distance between the spacecraft, as they orbit the Earth. This change in distance is reflected in the time-of-flight of microwave signals transmitted and received nearly simultaneously between the two spacecraft. The change in this time of fight is continuously measured by tracking the phase of the microwave carrier signals. The so called dual-one-way range change measurements can be reconstructed from these phase measurements. This range change (or its numerically derived derivatives), along with other mission and ancillary data, is subsequently analyzed to extract the parameters of an Earth gravity field model.
&lt;br&gt;&lt;h4 id&#x3D;&quot;grace_gab_l2_grav_jpl_rl06&quot;&gt;GRACE_GAB_L2_GRAV_JPL_RL06&lt;/h4&gt;
FOR EXPERT USE ONLY. This dataset contains estimates of geopotential field derived from the Gravity Recovery and Climate Experiment (GRACE) mission measurements and a non-tidal oceanic model produced by the Jet Propulsion Laboratory (JPL). The data are in spherical harmonics averaged over approximately a month. The primary objective of the GRACE mission is to obtain accurate estimates of the mean and time-variable components of the gravity field variations. This objective is achieved by making continuous measurements of the change in distance between twin spacecraft, co-orbiting in about 500 km altitude, near circular, polar orbit, spaced approximately 200 km apart, using a microwave ranging system. In addition to these range change, the non-gravitional forces are measured on each satellite using a high accuracy electrostatic, room-temperature accelerometer. The satellite orientation and position (and timing) are precisely measured using twin star cameras and a GPS receiver, respectively. Spatial and temporal variations in the gravity field affect the orbits (or trajectories) of the twin spacecraft differently. These differences are manifested as changes in the distance between the spacecraft, as they orbit the Earth. This change in distance is reflected in the time-of-flight of microwave signals transmitted and received nearly simultaneously between the two spacecraft. The change in this time of fight is continuously measured by tracking the phase of the microwave carrier signals. The so called dual-one-way range change measurements can be reconstructed from these phase measurements. This range change (or its numerically derived derivatives), along with other mission and ancillary data, is subsequently analyzed to extract the parameters of an Earth gravity field model.
&lt;br&gt;&lt;h4 id&#x3D;&quot;grace_gad_l2_grav_csr_rl06&quot;&gt;GRACE_GAD_L2_GRAV_CSR_RL06&lt;/h4&gt;
FOR EXPERT USE ONLY. This dataset contains estimates of ocean bottom pressure derived from the Gravity Recovery and Climate Experiment (GRACE) mission measurements, produced by the Center for Space Research (CSR) at University of Texas at Austin. The data are in spherical harmonics averaged over approximately a month. The primary objective of the GRACE mission is to obtain accurate estimates of the mean and time-variable components of the gravity field variations. This objective is achieved by making continuous measurements of the change in distance between twin spacecraft, co-orbiting in about 500 km altitude, near circular, polar orbit, spaced approximately 200 km apart, using a microwave ranging system. In addition to these range change, the non-gravitional forces are measured on each satellite using a high accuracy electrostatic, room-temperature accelerometer. The satellite orientation and position (and timing) are precisely measured using twin star cameras and a GPS receiver, respectively. Spatial and temporal variations in the gravity field affect the orbits (or trajectories) of the twin spacecraft differently. These differences are manifested as changes in the distance between the spacecraft, as they orbit the Earth. This change in distance is reflected in the time-of-flight of microwave signals transmitted and received nearly simultaneously between the two spacecraft. The change in this time of fight is continuously measured by tracking the phase of the microwave carrier signals. The so called dual-one-way range change measurements can be reconstructed from these phase measurements. This range change (or its numerically derived derivatives), along with other mission and ancillary data, is subsequently analyzed to extract the parameters of an Earth gravity field model.
&lt;br&gt;&lt;h4 id&#x3D;&quot;grace_gad_l2_grav_gfz_rl06&quot;&gt;GRACE_GAD_L2_GRAV_GFZ_RL06&lt;/h4&gt;
FOR EXPERT USE ONLY. This dataset contains estimates of ocean bottom pressure derived from the Gravity Recovery and Climate Experiment (GRACE) mission measurements, produced by the German Research Centre for Geosciences (GFZ). The data are in spherical harmonics averaged over approximately a month. The primary objective of the GRACE mission is to obtain accurate estimates of the mean and time-variable components of the gravity field variations. This objective is achieved by making continuous measurements of the change in distance between twin spacecraft, co-orbiting in about 500 km altitude, near circular, polar orbit, spaced approximately 200 km apart, using a microwave ranging system. In addition to these range change, the non-gravitional forces are measured on each satellite using a high accuracy electrostatic, room-temperature accelerometer. The satellite orientation and position (and timing) are precisely measured using twin star cameras and a GPS receiver, respectively. Spatial and temporal variations in the gravity field affect the orbits (or trajectories) of the twin spacecraft differently. These differences are manifested as changes in the distance between the spacecraft, as they orbit the Earth. This change in distance is reflected in the time-of-flight of microwave signals transmitted and received nearly simultaneously between the two spacecraft. The change in this time of fight is continuously measured by tracking the phase of the microwave carrier signals. The so called dual-one-way range change measurements can be reconstructed from these phase measurements. This range change (or its numerically derived derivatives), along with other mission and ancillary data, is subsequently analyzed to extract the parameters of an Earth gravity field model.
&lt;br&gt;&lt;h4 id&#x3D;&quot;grace_gad_l2_grav_jpl_rl06&quot;&gt;GRACE_GAD_L2_GRAV_JPL_RL06&lt;/h4&gt;
FOR EXPERT USE ONLY. This dataset contains estimates of ocean bottom pressure derived from the Gravity Recovery and Climate Experiment (GRACE) mission measurements, produced by the NASA Jet Propulsion Laboratory (JPL). The data are in spherical harmonics averaged over approximately a month. The primary objective of the GRACE mission is to obtain accurate estimates of the mean and time-variable components of the gravity field variations. This objective is achieved by making continuous measurements of the change in distance between twin spacecraft, co-orbiting in about 500 km altitude, near circular, polar orbit, spaced approximately 200 km apart, using a microwave ranging system. In addition to these range change, the non-gravitional forces are measured on each satellite using a high accuracy electrostatic, room-temperature accelerometer. The satellite orientation and position (and timing) are precisely measured using twin star cameras and a GPS receiver, respectively. Spatial and temporal variations in the gravity field affect the orbits (or trajectories) of the twin spacecraft differently. These differences are manifested as changes in the distance between the spacecraft, as they orbit the Earth. This change in distance is reflected in the time-of-flight of microwave signals transmitted and received nearly simultaneously between the two spacecraft. The change in this time of fight is continuously measured by tracking the phase of the microwave carrier signals. The so called dual-one-way range change measurements can be reconstructed from these phase measurements. This range change (or its numerically derived derivatives), along with other mission and ancillary data, is subsequently analyzed to extract the parameters of an Earth gravity field model.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tellus_grac-grfo_mascon_cri_grid_rl063_v4&quot;&gt;TELLUS_GRAC-GRFO_MASCON_CRI_GRID_RL06.3_V4&lt;/h4&gt;
This dataset contains gridded monthly global water storage/height anomalies relative to a time-mean, derived from GRACE and GRACE-FO and processed at JPL using the Mascon approach (RL06.3Mv04). A Coastal Resolution Improvement (CRI) filter has been applied to this data set to reduce signal leakage errors across coastlines. For most land hydrology, oceanographic as well as land-ice applications this is the recommend data set for the analysis of surface mass changes. The data are provided in a single data file in netCDF format, with water storage/height anomalies in equivalent water thickness units (cm). The data are derived from solving for monthly gravity field variations on geolocated spherical cap mass concentration functions, rather than global spherical harmonic coefficients. Additionally, realistic geophysical information is introduced during the computation to intrinsically remove correlated errors. Thus, these Mascon grids do not need to be de-correlated or smoothed, like traditional spherical harmonic gravity solutions. &lt;br&gt;&lt;br&gt; The complete Mascon solution consists of 4,551 independent estimates of surface mass change that have been derived using an equal-area 3-degree grid of individual mascons. A subset of these individual mascons span coastlines, and contain mixed land and ocean mass change signals. In a post-processing step, the CRI filter is applied to those mixed land/ocean Mascons to separate land and ocean mass. The land mask used to perform this separation is provided in the same directory as this dataset, as are uncertainty values, and the gridded mascon-ID number to enable further analysis. Since the individual mascons act as an inherent smoother on the gravity field, a set of optional gain factors (or scale factors) is provided within the netCDF and can be applied to the solution to study mass change signals at sub-mascon resolution (e.g. for continental hydrology applications). For use-case examples and further background on the gain factors, please see Wiese, Landerer &amp;amp; Watkins, 2016, &lt;a href&#x3D;&quot;https://doi.org/10.1002/2016WR019344&quot;&gt;https://doi.org/10.1002/2016WR019344&lt;/a&gt;. &lt;br&gt;&lt;br&gt; This RL06.3Mv04 is an updated version of the previous Tellus JPL Mascon RL06.1Mv03 (DOI, 10.5067/TEMSC-3JC63). For a detailed description on the Mascon solution, including the mathematical derivation, implementation of geophysical constraints, and solution validation, please see Watkins et al., 2015, doi: 10.1002/2014JB011547. For a detailed description of the CRI filter implementation, please see Wiese et al., 2016, doi:10.1002/2016WR019344.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tellus_grac-grfo_mascon_grid_rl063_v4&quot;&gt;TELLUS_GRAC-GRFO_MASCON_GRID_RL06.3_V4&lt;/h4&gt;
This dataset contains gridded monthly global water storage/height anomalies relative to a time-mean, derived from GRACE and GRACE-FO and processed at JPL using the Mascon approach (RL06.3Mv04). These data are provided in a single data file in netCDF format, and can be used for analysis for ocean, ice, and hydrology phenomena. The data are provided in a single data file in netCDF format, with water storage/height anomalies in equivalent water thickness units (cm). The data are derived from solving for monthly gravity field variations on geolocated spherical cap mass concentration functions, rather than global spherical harmonic coefficients. Additionally, realistic geophysical information is introduced during the computation to intrinsically remove correlated errors. Thus, these Mascon grids do not need to be de-correlated or smoothed, like traditional spherical harmonic gravity solutions. &lt;br&gt;&lt;br&gt; The complete Mascon solution consists of 4,551 independent estimates of surface mass change that have been derived using an equal-area 3-degree grid of individual mascons. Please note that this dataset does not correct for leakage errors across coastlines; it is therefore recommended only for users who want to apply their own algorithm to separate between land and ocean mass very near coastlines. &lt;br&gt;&lt;br&gt; This RL06.3Mv04 is an updated version of the previous Tellus JPL Mascon RL06.1Mv03. For more information, please visit &lt;a href&#x3D;&quot;https://grace.jpl.nasa.gov/data/get-data/jpl_global_mascons/&quot;&gt;https://grace.jpl.nasa.gov/data/get-data/jpl_global_mascons/&lt;/a&gt;. For a detailed description on the Mascon processing, including the mathematical derivation, implementation of geophysical constraints, and validation, please see Watkins et al., 2015, doi: 10.1002/2014JB011547. This product is intended for expert use only; other users are encouraged to use the CRI-filtered Mascon dataset, which is available here: &lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/TELLUS_GRAC-GRFO_MASCON_GRID_RL06.3_V4&quot;&gt;https://podaac.jpl.nasa.gov/dataset/TELLUS_GRAC-GRFO_MASCON_GRID_RL06.3_V4&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;grc-gfo_gridded_aod1b_jpl_1-deg_rl063&quot;&gt;GRC-GFO_GRIDDED_AOD1B_JPL_1-DEG_RL06.3&lt;/h4&gt;
GRACE non-tidal high-frequency atmospheric and oceanic mass variation models are routinely generated at GFZ as so-called Atmosphere and Ocean De-aliasing Level-1B (AOD1B) products (in terms of corresponding spherical harmonic geopotential coefficients) to be added to the background static gravity model during GRACE monthly gravity field determination. AOD1B products are 3-hourly series of spherical harmonic coefficients up to degree and order 180 which are routinely provided to the GRACE Science Data System and the user community with only a few days time delay. These products reflect spatio-temporal mass variations in the atmosphere and oceans deduced from an operational atmospheric model and corresponding ocean dynamics provided by an ocean model. The variability is derived by subtraction of a long-term mean of vertical integrated atmospheric mass distributions and a corresponding mean of ocean bottom pressure as simulated with the ocean model. &lt;br&gt;&lt;br&gt; The Gridded AOD1B data sets provided here contain the monthly mean AOD1B data in geolocated gridded form, smoothed or spatially aggregated to be consistent with the GRACE and GRACE-FO Tellus Level-3 data products of land and/or ocean mass anomalies. With these gridded AOD1B Level-3 products, users can remove or add the effects of the modeled mean monthly atmospheric and ocean bottom pressure change (e.g., to compare different models).
&lt;br&gt;&lt;h4 id&#x3D;&quot;tellus_gldas-noah-33_tws-anomaly_monthly&quot;&gt;TELLUS_GLDAS-NOAH-3.3_TWS-ANOMALY_MONTHLY&lt;/h4&gt;
The total land water storage anomalies are aggregated from the Global Land Data Assimilation System (GLDAS) NOAH model. GLDAS outputs land water content by using numerous land surface models and data assimilation. For more information on the GLDAS project and model outputs please visit &lt;a href&#x3D;&quot;https://ldas.gsfc.nasa.gov/gldas&quot;&gt;https://ldas.gsfc.nasa.gov/gldas&lt;/a&gt;. The aggregated land water anomalies (sum of soil moisture, snow, canopy water) provided here can be used for comparison against and evaluations of the observations of Gravity Recovery and Climate Experiment (GRACE) and GRACE-FO over land. The monthly anomalies are computed over the same days during each month as GRACE and GRACE-FO data, and are provided on monthly 1 degree lat/lon grids in NetCDF format. Currently, the days included in these monthly anomaly computation are same as GRACE-FO monthly Level-2 RL06.3 JPL solutions.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tellus_gia_l3_05-deg_v10&quot;&gt;TELLUS_GIA_L3_0.5-DEG_V1.0&lt;/h4&gt;
Glacial isostatic adjustment (GIA) is an ongoing geophysical process and is measured by gravimetry satellites like GRACE and GRACE-FO. To isolate signals of contemporary surface mass loss in the cumulative satellite gravimetry measurements, contemporary GIA rates are computed and subtracted from the satellite gravimetry observations. The GIA correction models provided here are filtered such that they are compatible with Level-3 post-processing filters applied to GRACE(-FO) data as indicated in the [product_id]. In this way, user can effectively assess the impact of the applied GIA correction, and substitute different GIA models should that be desired. This GIA dataset is mapped into 0.5-degree global grid compatible with the JPL Mascon solution, provided in netCDF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;antarctica_mass_tellus_mascon_cri_time_series_rl063_v4&quot;&gt;ANTARCTICA_MASS_TELLUS_MASCON_CRI_TIME_SERIES_RL06.3_V4&lt;/h4&gt;
This dataset is a time series of mass variability averaged over all of Antarctica. It provides the ice mass changes of Antarctica over time. The mass variability are derived from JPL GRACE Mascon Ocean, Ice, and Hydrology Equivalent Water Height CRI Filtered RL063Mv04 dataset, which can be found at &lt;a href&#x3D;&quot;https://doi.org/10.5067/TEMSC-3JC634&quot;&gt;https://doi.org/10.5067/TEMSC-3JC634&lt;/a&gt;. A more detailed description on the Mascon solution, including the mathematical derivation, implementation of geophysical constraints, and solution validation, please see Watkins et al., 2015, doi: 10.1002/2014JB011547. The mass variability are provided as an ASCII table.
&lt;br&gt;&lt;h4 id&#x3D;&quot;greenland_mass_tellus_mascon_cri_time_series_rl063_v4&quot;&gt;GREENLAND_MASS_TELLUS_MASCON_CRI_TIME_SERIES_RL06.3_V4&lt;/h4&gt;
This dataset is a time series of mass variability averaged over all of the global ocean. It provides the non-steric or mass only sea level changes over time. The mass variability are derived from JPL GRACE Mascon Ocean, Ice, and Hydrology Equivalent Water Height CRI Filtered RL06.3Mv04 dataset, which can be found at &lt;a href&#x3D;&quot;https://doi.org/10.5067/TEMSC-3JC634&quot;&gt;https://doi.org/10.5067/TEMSC-3JC634&lt;/a&gt;. A more detailed description on the Mascon solution, including the mathematical derivation, implementation of geophysical constraints, and solution validation, please see Watkins et al., 2015, doi: 10.1002/2014JB011547. The mass variability is provided as an ASCII table.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://archive.podaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA GRACE-DA-DM Project</title>
      <link>https://registry.opendata.aws/nasa-grace-da-dm</link>
      <guid>https://registry.opendata.aws/nasa-grace-da-dm</guid>
      <description>Scientists at NASA Goddard Space Flight Center generate groundwater and soil moisture drought indicators each week. They are based on terrestrial water storage observations derived from GRACE satellite data and integrated with other observations, using a sophisticated numerical model of land surface water and energy processes. This data product is GRACE Data Assimilation for Drought Monitoring (GRACE-DA-DM) U.S. Version 4.0 data product and supersedes the GRACE-DA-DM Version 2.0. The GRACE-DA-DM U.S. V4.0 is based on the Catchment Land Surface Model (CLSM) Fortuna 2.5 version simulation that was created within the Land Information System data assimilation framework (Kumar et al., 2016). This simulation used the latest GRACE RL06 (GRACE; 2002-2017) and GRACE Follow On (GRACE-FO; 2018-present) Mascon solutions version 2, at 0.25 degree resolution, from the University of Texas at Austin (Save et al., 2016; Save, 2020). The CLSM soil parameters were updated to address a soil moisture dry limit issue found near Zapata, Texas. Because the root zone soil moisture frequently reaches the dry limit there, drought conditions are often “normal” when the area should be in drought. The new soil parameters resolved the issue, and the root zone soil moisture now matches closely the in-situ observation near Zapata. In the data assimilation, the baseline for Terrestrial Water Storage anomaly computation was updated to the 2003-2019 mean, whereas previous simulations used the 2003-2016 mean. The percentile computation was switched to a 7-day moving average climatology, instead of monthly, to improve the temporal transition of drought/wetness conditions. The GRACE-DA-DM V1.0 was created by the stand alone CLSM (an older version) using the GRACE-Tellus 1 degree data from the Center for Space Research at University of Texas. The GRACE data assimilation (DA) is executed on a grid-to-grid basis in V2.0, while a basin scale average was used in V1.0 (Zaitchik et al. 2008). The V2.0 data were reprocessed (on June 14, 2017), using the GRACE RL05 Mascon solutions version 1 data set from UT CSR, for the entire period from April 1, 2002 to June 5, 2017. The reprocessing included fixes in the DA and increased the bedrock depth by 3 meters to enhance the drought indicator calculations. The GRACE-DA-DM U.S. V4.0 uses the same configuration as the V2.0 for the DA scheme and increased bedrock depth, with the updates previously mentioned, thus supersedes the previous versions. The GRACE-DA-DM U.S. V4.0 data product contains three drought indicators: Groundwater Percentile, Root Zone Soil Moisture Percentile, and Surface Soil Moisture Percentile. These drought indicators express wet or dry conditions as a percentile, indicating the probability of occurrence within the period of record from 1948 to 2014. The drought indicator data are daily, but available only one day (Monday) per week. The data have a spatial resolution of 0.125 x 0.125 degree over North America and range from April 1, 2002 to present (with a 3-6 months latency). The data are archived in NetCDF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gracedadm_clsm025gl_7d&quot;&gt;GRACEDADM_CLSM025GL_7D&lt;/h4&gt;
Scientists at NASA Goddard Space Flight Center generate groundwater and soil moisture drought indicators each week. They are based on terrestrial water storage observations derived from GRACE-FO satellite data and integrated with other observations, using a sophisticated numerical model of land surface water and energy processes. This data product is GRACE Data Assimilation for Drought Monitoring (GRACE-DA-DM) Global Version 3.0 from a global GRACE and GRACE-FO data assimilation and drought indicator product generation (Li et al., 2019). It varies from the other GRACE-DA-DM products which are from the U.S. GRACE-based drought indicator product generation (Houborg et al., 2012). The GRACE-DA-DM Global V3.0 is similar to the GRACE-DA-DM U.S. V4.0 product. Both products are based on the Catchment Land Surface Model (CLSM) Fortuna 2.5 version simulation that was created within the Land Information System data assimilation framework (Kumar et al., 2016). GRACE-DA-DM Global V3.0 drought indicator maps are derived from the GLDAS_CLSM025_DA1_D product, at 0.25 degree resolution, forced by ECMWF meteorological data, and assimilated RL06 GRACE and GRACE-FO data from the University of Texas at Austin (Save et al., 2016; Save, 2020). The GRACE-DA-DM U.S. V4.0 is at 0.125 degree, which is based on a model simulation (not published at GES DISC) forced by NLDAS-2 meteorological data and assimilated with RL06 GRACE/GRACE-FO data. More information on GRACE-DA-DM U.S. V4.0 and previous versions of the data can be found in the README. The GRACE-DA-DM Global V3.0 data product contains three drought indicators: Groundwater Percentile, Root Zone Soil Moisture Percentile, and Surface Soil Moisture Percentile. These drought indicators express wet or dry conditions as a percentile, indicating the probability of occurrence within the period of record from 1948 to 2014. The drought indicator data are daily, but available only one day (Monday) per week. The data have a spatial resolution of 0.25 x 0.25 degree with global coverage (60S, 180W, 90N, 180E), and a temporal range from February 2003 to present (with a 3-6 month latency). The data are archived in NetCDF format. The GRACE-DA-DM is an operational project which produces groundwater and soil moisture drought indicators each week. The operational data is available weekly with a 2-9 day latency from the NASA GRACE project home page found under the Documentation tab. The GRACE-DA-DM data distributed here at GESDISC is the final archive version, which is generated after the latest GRACE-FO data are available.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA GRACE-FO Project</title>
      <link>https://registry.opendata.aws/nasa-grace-fo</link>
      <guid>https://registry.opendata.aws/nasa-grace-fo</guid>
      <description>This data set is produced by the Center for Space Research (CSR) GRACE-FO (Gravity Recovery and Climate Experiment Follow-On) program and derives the terrestrial water storage anomaly given as equivalent water thickness. These monthly grids are derived from GRACE-FO time-variable gravity observations during the specified timespan, and relative to the specified time-mean reference period. This quantity represents the total terrestrial water storage anomalies from soil moisture, snow, surface water (incl. rivers, lakes, reservoirs etc.), as well as groundwater and aquifers. A glacial isostatic adjustment (GIA) correction has been applied, and standard corrections for geocenter (degree-1), C20 (degree-20) and C30 (degree-30) are incorporated. Post-processing filters have been applied to reduce correlated errors. Data grids are provided in ASCII/netCDF/GeoTIFF formats. &lt;br&gt;&lt;br&gt; GRACE-FO was launched on 22 May 2018, and extends the original GRACE mission (2002 – 2017) and expands its legacy of scientific achievements in tracking earth surface mass changes. Version 04 (v04) of the terrestrial water storage data uses updated and consistent C20 and Geocenter corrections (i.e., Technical Notes TN-14 and TN-13), as well as an ellipsoidal correction to account for the non-spherical shape of the Earth when mapping gravity anomalies to surface mass change. Additionally, this release 06.3 is an updated version of the Level 3 products in coordination with the release of the analogous Level 2 products used to generate them. It differs from RL06.1 only in the Level-1B accelerometer transplant data that is used for the GF2 (GRACE-FO 2) satellite; see respective L-2 data descriptions. RL06.3 uses the ACX2-L1B data products. All GRACE-FO RL06.3 Level-3 fields are fully compatible with the GRACE RL06 data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tellus_grfo_l3_csr_rl063_ocn_v04&quot;&gt;TELLUS_GRFO_L3_CSR_RL06.3_OCN_v04&lt;/h4&gt;
This data set is produced by the Center for Space Research (CSR) GRACE-FO (Gravity Recovery and Climate Experiment Follow-On) program and derives the ocean bottom pressure (OBP) anomaly given as equivalent water thickness. These monthly grids are derived from GRACE-FO time-variable gravity observations during the specified timespan, and relative to the specified time-mean reference period. This quantity represents sea floor pressure changes due to the integral effect of ocean and atmosphere processes, including global mean ocean bottom pressure changes (mean ocean mass and mean atmosphere mass over the global oceans). A glacial isostatic adjustment (GIA) correction has been applied, and standard corrections for geocenter (degree-1), C20 (degree-20) and C30 (degree-30) are incorporated. Post-processing filters have been applied to reduce correlated errors. Data grids are provided in ASCII/netCDF/GeoTIFF formats. &lt;br&gt;&lt;br&gt; GRACE-FO was launched on 22 May 2018, and extends the original GRACE mission (2002 – 2017) and expands its legacy of scientific achievements in tracking earth surface mass changes. Version 04 (v04) of the ocean bottom pressure data uses updated and consistent C20 and Geocenter corrections (i.e., Technical Notes TN-14 and TN-13), as well as an ellipsoidal correction to account for the non-spherical shape of the Earth when mapping gravity anomalies to surface mass change. Additionally, this release 06.3 is an updated version of the Level 3 products in coordination with the release of the analogous Level 2 products used to generate them. It differs from RL06.1 only in the Level-1B accelerometer transplant data that is used for the GF2 (GRACE-FO 2) satellite; see respective L-2 data descriptions. RL06.3 uses the ACX2-L1B data products. All GRACE-FO RL06.3 Level-3 fields are fully compatible with the GRACE RL06 data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tellus_grfo_l3_gfz_rl063_lnd_v04&quot;&gt;TELLUS_GRFO_L3_GFZ_RL06.3_LND_v04&lt;/h4&gt;
This data set is produced by the German Research Centre for Geosciences (GFZ) as part of the GRACE-FO (Gravity Recovery and Climate Experiment Follow-On) program and derives the terrestrial water storage anomaly given as equivalent water thickness. These monthly grids are derived from GRACE-FO time-variable gravity observations during the specified timespan, and relative to the specified time-mean reference period. This quantity represents the total terrestrial water storage anomalies from soil moisture, snow, surface water (incl. rivers, lakes, reservoirs etc.), as well as groundwater and aquifers. A glacial isostatic adjustment (GIA) correction has been applied, and standard corrections for geocenter (degree-1), C20 (degree-20) and C30 (degree-30) are incorporated. Post-processing filters have been applied to reduce correlated errors. Data grids are provided in ASCII/netCDF/GeoTIFF formats. &lt;br&gt;&lt;br&gt; GRACE-FO was launched on 22 May 2018, and extends the original GRACE mission (2002 – 2017) and expands its legacy of scientific achievements in tracking earth surface mass changes. Version 04 (v04) of the terrestrial water storage data uses updated and consistent C20 and Geocenter corrections (i.e., Technical Notes TN-14 and TN-13), as well as an ellipsoidal correction to account for the non-spherical shape of the Earth when mapping gravity anomalies to surface mass change. Additionally, this release 06.3 is an updated version of the Level 3 products in coordination with the release of the analogous Level 2 products used to generate them. It differs from RL06.1 only in the Level-1B accelerometer transplant data that is used for the GF2 (GRACE-FO 2) satellite; see respective L-2 data descriptions. RL06.3 uses the ACX2-L1B data products. All GRACE-FO RL06.3 Level-3 fields are fully compatible with the GRACE RL06 data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tellus_grfo_l3_gfz_rl063_ocn_v04&quot;&gt;TELLUS_GRFO_L3_GFZ_RL06.3_OCN_v04&lt;/h4&gt;
This data set is produced by the German Research Centre for Geosciences (GFZ) as part of the GRACE-FO (Gravity Recovery and Climate Experiment Follow-On) program and derives the ocean bottom pressure (OBP) anomaly given as equivalent water thickness. These monthly grids are derived from GRACE-FO time-variable gravity observations during the specified timespan, and relative to the specified time-mean reference period. This quantity represents sea floor pressure changes due to the integral effect of ocean and atmosphere processes, including global mean ocean bottom pressure changes (mean ocean mass and mean atmosphere mass over the global oceans). A glacial isostatic adjustment (GIA) correction has been applied, and standard corrections for geocenter (degree-1), C20 (degree-20) and C30 (degree-30) are incorporated. Post-processing filters have been applied to reduce correlated errors. Data grids are provided in ASCII/netCDF/GeoTIFF formats. &lt;br&gt;&lt;br&gt; GRACE-FO was launched on 22 May 2018, and extends the original GRACE mission (2002 – 2017) and expands its legacy of scientific achievements in tracking earth surface mass changes. Version 04 (v04) of the ocean bottom pressure data uses updated and consistent C20 and Geocenter corrections (i.e., Technical Notes TN-14 and TN-13), as well as an ellipsoidal correction to account for the non-spherical shape of the Earth when mapping gravity anomalies to surface mass change. Additionally, this release 06.3 is an updated version of the Level 3 products in coordination with the release of the analogous Level 2 products used to generate them. It differs from RL06.1 only in the Level-1B accelerometer transplant data that is used for the GF2 (GRACE-FO 2) satellite; see respective L-2 data descriptions. RL06.3 uses the ACX2-L1B data products. All GRACE-FO RL06.3 Level-3 fields are fully compatible with the GRACE RL06 data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gracefo_l1a_ascii_grav_jpl_rl04&quot;&gt;GRACEFO_L1A_ASCII_GRAV_JPL_RL04&lt;/h4&gt;
FOR EXPERT USE ONLY. The GRACE-FO Level-1A data contains telemetry data that has been converted to engineering units, from which Level-1B data products are derived. For a detailed description, please see the GRACE-FO Level-1 documentation (&lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/gravity/gracefo-documentation&quot;&gt;https://podaac.jpl.nasa.gov/gravity/gracefo-documentation&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;gracefo_l1b_ascii_grav_jpl_rl04&quot;&gt;GRACEFO_L1B_ASCII_GRAV_JPL_RL04&lt;/h4&gt;
FOR EXPERT USE ONLY. The GRACE-FO Level-1B data provide all necessary inputs to derive monthly time variations in the Earth gravity field. Level-1B data are also used for GRACE orbit and mean gravity field determination. For a detailed description, please see the GRACE-FO Level-1 documentation (&lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/gravity/gracefo-documentation&quot;&gt;https://podaac.jpl.nasa.gov/gravity/gracefo-documentation&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;gracefo_l2_jpl_monthly_0063&quot;&gt;GRACEFO_L2_JPL_MONTHLY_0063&lt;/h4&gt;
FOR EXPERT USE ONLY. This dataset contains estimates of the total month-by-month geopotential of the Earth, derived from the Gravity Recovery and Climate Experiment Follow-On (GRACE-FO) mission measurements, produced by the NASA Jet Propulsion Laboratory (JPL). The data are provided as spherical harmonic coefficients, averaged over approximately a month, and available from 2018 onward. These coefficients are derived from the Microwave Instrument (MWI) measured intersatellite range changes between the twin spacecraft of the GRACE-FO (Gravity Recovery and Climate Experiment Follow-On) mission. The GRACE-FO mission, a joint partnership between NASA and the German Research Centre for Geosciences (GFZ), launched on 22 May 2018. It uses twin satellites to accurately map variations in the Earth&amp;#39;s gravity field and surface mass distribution. It is designed as a successor to the Gravity Recovery and Climate Experiment (GRACE) mission. &lt;br&gt;&lt;br&gt; This GRACE-FO RL06.3 data is an updated version of the GRACE-FO RL06.1 Level-2 data products. RL06.3 differs from RL06.1 only in the Level-1B accelerometer transplant data that is used for the GF2 satellite: Level-2 RL06.3 uses ACH1B RL04 that is contained within the ACX2 Level-1 bundle, which replaces ACH1B RL04 contained within the ACX Level-1 bundle that was used for Level-2 RL06.1 (note: ACX2-L1B is only applicable for 01/2023 onwards in wide-pointing operational mode; from 6/2018 through 12/2022, RL06.1 and RL06.3 GRACE-FO data are identical and based on ACX; ACX2 is not available for 03/2023-06/2023 as the satellites were not in wide-pointing mode during that period). All GRACE-FO RL06.3 Level-2 products are fully compatible with the GRACE RL06 level-2 fields. Refer to the mission page for more information.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gracefo_l2_csr_monthly_0063&quot;&gt;GRACEFO_L2_CSR_MONTHLY_0063&lt;/h4&gt;
FOR EXPERT USE ONLY. This dataset contains estimates of the total month-by-month geopotential of the Earth, derived from the Gravity Recovery and Climate Experiment Follow-On (GRACE-FO) mission measurements, produced by the University of Texas (at Austin) Center for Space Research (CSR). The data are provided as spherical harmonic coefficients, averaged over approximately a month, and available from 2018 onward. These coefficients are derived from the Microwave Instrument (MWI) measured intersatellite range changes between the twin spacecraft of the GRACE-FO (Gravity Recovery and Climate Experiment Follow-On) mission. The GRACE-FO mission, a joint partnership between NASA and the German Research Centre for Geosciences (GFZ), launched on 22 May 2018. It uses twin satellites to accurately map variations in the Earth&amp;#39;s gravity field and surface mass distribution. It is designed as a successor to the Gravity Recovery and Climate Experiment (GRACE) mission. &lt;br&gt;&lt;br&gt; This GRACE-FO RL06.3 data is an updated version of the GRACE-FO RL06.1 Level-2 data products. RL06.3 differs from RL06.1 only in the Level-1B accelerometer transplant data that is used for the GF2 satellite: Level-2 RL06.3 uses ACH1B RL04 that is contained within the ACX2 Level-1 bundle, which replaces ACH1B RL04 contained within the ACX Level-1 bundle that was used for Level-2 RL06.1 (note: ACX2-L1B is only applicable for 01/2023 onwards in wide-pointing operational mode; from 6/2018 through 12/2022, RL06.1 and RL06.3 GRACE-FO data are identical and based on ACX; ACX2 is not available for 03/2023-06/2023 as the satellites were not in wide-pointing mode during that period). All GRACE-FO RL06.3 Level-2 products are fully compatible with the GRACE RL06 level-2 fields. Refer to the mission page for more information.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gracefo_l2_gfz_monthly_0063&quot;&gt;GRACEFO_L2_GFZ_MONTHLY_0063&lt;/h4&gt;
FOR EXPERT USE ONLY. This dataset contains estimates of the total month-by-month geopotential of the Earth, derived from the Gravity Recovery and Climate Experiment Follow-On (GRACE-FO) mission measurements, produced by the German Research Centre for Geosciences (GFZ). The data are provided as spherical harmonic coefficients, averaged over approximately a month. These coefficients are derived from the Microwave Instrument (MWI) measured intersatellite range changes between the twin spacecraft of the GRACE-FO mission. Refer to the mission page for more information. &lt;br&gt;&lt;br&gt; This GRACE-FO RL06.3 data is an updated version of the GRACE-FO RL06.1 Level-2 data products. RL06.3 differs from RL06.1 only in the Level-1B accelerometer transplant data that is used for the GF2 satellite: Level-2 RL06.3 uses ACH1B RL04 that is contained within the ACX2 Level-1 bundle, which replaces ACH1B RL04 contained within the ACX Level-1 bundle that was used for Level-2 RL06.1 (note: ACX2-L1B is only applicable for 01/2023 onwards in wide-deadband operational mode; from 6/2018 through 12/2022, RL06.1 and RL06.3 GRACE-FO data are identical). All GRACE-FO RL06.3 Level-2 products are fully compatible with the GRACE RL06 level-2 fields. Refer to the mission page for more information.
&lt;br&gt;&lt;h4 id&#x3D;&quot;grace_abpr_fo_l2_v10&quot;&gt;GRACE_ABPR_FO_L2_V1.0&lt;/h4&gt;
This dataset provides hourly ocean bottom pressure measurements at the North Pole from the Arctic Bottom Pressure Recorder - Follow On (ABPR-FO) from August 2022 to August 2023. Based around a Paroscientific Digiquartz pressure sensor, the ABPR-FO was designed and powered to collect and transmit data which was then collected, quality-controlled and updated at PO.DAAC on a yearly basis. The full time series is provided as a single netCDF file, and reports both bottom pressure (reported as liquid water equivalent thickness) and temperature. This dataset aims to serve as in situ validation for GRACE-FO data products in the central Arctic. This project is funded by NASA’s GRACE and GRACE-FO Science Team and supported by PONANT Science.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tellus_grfo_l3_jpl_rl063_lnd_v04&quot;&gt;TELLUS_GRFO_L3_JPL_RL06.3_LND_v04&lt;/h4&gt;
This data set is produced by the Jet Propulsion Laboratory (JPL) as part of the GRACE-FO (Gravity Recovery and Climate Experiment Follow-On) program and derives the terrestrial water storage anomaly given as equivalent water thickness. These monthly grids are derived from GRACE-FO time-variable gravity observations during the specified timespan, and relative to the specified time-mean reference period. This quantity represents the total terrestrial water storage anomalies from soil moisture, snow, surface water (incl. rivers, lakes, reservoirs etc.), as well as groundwater and aquifers. A glacial isostatic adjustment (GIA) correction has been applied, and standard corrections for geocenter (degree-1), C20 (degree-20) and C30 (degree-30) are incorporated. Post-processing filters have been applied to reduce correlated errors. Data grids are provided in ASCII/netCDF/GeoTIFF formats. &lt;br&gt;&lt;br&gt; GRACE-FO was launched on 22 May 2018, and extends the original GRACE mission (2002 – 2017) and expands its legacy of scientific achievements in tracking earth surface mass changes. Version 04 (v04) of the terrestrial water storage data uses updated and consistent C20 and Geocenter corrections (i.e., Technical Notes TN-14 and TN-13), as well as an ellipsoidal correction to account for the non-spherical shape of the Earth when mapping gravity anomalies to surface mass change. Additionally, this RL06.3 is an updated release of the previous RL06.1. It differs from RL06.1 only in the Level-1B accelerometer transplant data that is used for the GF2 (GRACE-FO 2) satellite; see respective L-2 data descriptions. RL06.3 uses the ACX2-L1B data products. All GRACE-FO RL06.3 Level-3 fields are fully compatible with the GRACE RL06 data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://archive.podaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA GSESA Project</title>
      <link>https://registry.opendata.aws/nasa-gsesa</link>
      <guid>https://registry.opendata.aws/nasa-gsesa</guid>
      <description>The Global Surface Emissivity Spectral Atlas (GSESA) database contains global, monthly climatology infrared emissivity functional Empirical Orthogonal Function (EOF) scores in 0.25 x 0.25 latitude-longitude resolution. An eigenvector file and a reader file allow customers to produce emissivity spectra. The emissivity functional EOF scores were developed using the Infrared Atmospheric Sounding Interferometer (IASI) instrument on the METOP-A, METOP-B, and METOP-C satellites for the period 2007-07-01 to 2025-01-31. An inversion scheme, dealing with cloudy as well as cloud-free radiances observed with ultraspectral infrared (IR) sounders, was developed to simultaneously retrieve atmospheric thermodynamic and surface or cloud microphysical parameters. This inversion scheme was applied to the IASI instrument. Rapidly produced surface spectral emissivity (SSE) is initially evaluated through quality control checks on the retrievals of other impacted surface and atmospheric parameters. The GSESA data are provided in binary format, with sample reader files that can be used in a Fortan IDE to read a functional emissivity EOF compressed file (e.g., MFEMI_MONTH01_A_V5P.bin) and its EOF eigenvector file (IASI_B_EV_FUNC_GLOBAL_V4.bin) to produce spectral emissivity at a certain location (latitude and longitude). A sample reader file can be used in a Matlab IDE is also provided. These data were created with funding from the NASA Internal Scientist Funding Model for the National Airborne Sounder Testbed-Interferometer (NAST-I).
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.asdc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA HAQAST Project</title>
      <link>https://registry.opendata.aws/nasa-haqast</link>
      <guid>https://registry.opendata.aws/nasa-haqast</guid>
      <description>Our mission is to put the power of NASA’s satellites down to earth and in your hands. HAQAST is a collaborative team that works in partnership with public health and air quality agencies to use NASA data and tools for the public benefit. Here, you can learn about our team, partnerships, and newsworthy achievements. You…
&lt;br&gt;&lt;h4 id&#x3D;&quot;alan_viirs_conus&quot;&gt;ALAN_VIIRS_CONUS&lt;/h4&gt;
This product provides detailed information about the satellite-based data on artificial light at night (ALAN). The Suomi National Polar-orbiting Partnership (S-NPP) Visible Infrared Imaging Radiometer Suite (VIIRS) Day/Night Band (DNB) nighttime lights (NTL) product (VNP46A4, DOI: 10.5067/VIIRS/VNP46A4.001 ) in NASA’s Black Marble suite is used to derive annual summary of ALAN levels throughout the CONUS at both county and tract level for the period of 2012-2020. The PI Dr. Qian Xiao is a member of NASA Heath and Air Quality Applied Sciences Team (HAQAST).
&lt;br&gt;&lt;h4 id&#x3D;&quot;haq_tropomi_no2_conus_a_l3&quot;&gt;HAQ_TROPOMI_NO2_CONUS_A_L3&lt;/h4&gt;
This product provides level 3 annual averages of tropospheric Nitrogen dioxide (NO2) vertical column density derived from the level 2 Tropospheric Monitoring Instrument (TROPOMI) across the Continental United States oversampled to a spatial resolution of 0.01˚ x 0.01˚ (&lt;del&gt;1 km2) using a consistent algorithm from the European Space Agency (ESA) version 2.4 that can be used for trend analysis of air pollution. The dataset record began in 2019 and continues to the present. This L3 product was developed by the George Washington University Air, Climate and Health Laboratory as part of the NASA Health Air Quality Applied Science Team (HAQAST) using Level 2 version 2.4 TROPOMI NO2 files from the ESA. The TROPOMI instrument on Sentinel-5 Precursor acquires tropospheric NO2 column contents from low Earth orbit (&lt;/del&gt;824 km above ground level) once per day globally at approximately 13:30 local time. NO2 is an air pollutant that adversely affects the human respiratory system and leads to premature mortality. NO2 is also an important precursor for ozone and fine particulates, which also have severe health impacts. In urban areas, the majority of NO2 originates from anthropogenic NOx (&#x3D;NO+NO2; most NOx is emitted as NO, which rapidly cycles to NO2) emissions during high-temperature fossil fuel combustion. Tropospheric NO2 vertical column contents are qualitatively representative of near-surface NO2 concentrations and NOx emissions in urban/polluted locations.
&lt;br&gt;&lt;h4 id&#x3D;&quot;haq_tropomi_no2_conus_m_l3&quot;&gt;HAQ_TROPOMI_NO2_CONUS_M_L3&lt;/h4&gt;
This product provides level 3 monthly averages of tropospheric Nitrogen dioxide (NO2) vertical column density derived from the level 2 Tropospheric Monitoring Instrument (TROPOMI) across the Continental United States oversampled to a spatial resolution of 0.01˚ x 0.01˚ (&lt;del&gt;1 km2) using a consistent algorithm from the European Space Agency (ESA) version 2.4 that can be used for trend analysis of air pollution. The dataset record began in May 2018 and continues to the present. This L3 product was developed by the George Washington University Air, Climate and Health Laboratory as part of the NASA Health Air Quality Applied Science Team (HAQAST) using Level 2 version 2.4 TROPOMI NO2 files from the ESA. The TROPOMI instrument on Sentinel-5 Precursor acquires tropospheric NO2 column contents from low Earth orbit (&lt;/del&gt;824 km above ground level) once per day globally at approximately 13:30 local time. NO2 is an air pollutant that adversely affects the human respiratory system and leads to premature mortality. NO2 is also an important precursor for ozone and fine particulates, which also have severe health impacts. In urban areas, the majority of NO2 originates from anthropogenic NOx (&#x3D;NO+NO2; most NOx is emitted as NO, which rapidly cycles to NO2) emissions during high-temperature fossil fuel combustion. Tropospheric NO2 vertical column contents are qualitatively representative of near-surface NO2 concentrations and NOx emissions in urban/polluted locations.
&lt;br&gt;&lt;h4 id&#x3D;&quot;haq_tropomi_no2_conus_s_l3&quot;&gt;HAQ_TROPOMI_NO2_CONUS_S_L3&lt;/h4&gt;
This product provides level 3 seasonal averages of tropospheric Nitrogen dioxide (NO2) vertical column density derived from the level 2 Tropospheric Monitoring Instrument (TROPOMI) across the Continental United States oversampled to a spatial resolution of 0.01˚ x 0.01˚ (&lt;del&gt;1 km2) using a consistent algorithm from the European Space Agency (ESA) version 2.4 that can be used for trend analysis of air pollution. The dataset record began in June-August 2018 and continues to the present. This L3 product was developed by the George Washington University Air, Climate and Health Laboratory as part of the NASA Health Air Quality Applied Science Team (HAQAST) using Level 2 version 2.4 TROPOMI NO2 files from the ESA. The TROPOMI instrument on Sentinel-5 Precursor acquires tropospheric NO2 column contents from low Earth orbit (&lt;/del&gt;824 km above ground level) once per day globally at approximately 13:30 local time. NO2 is an air pollutant that adversely affects the human respiratory system and leads to premature mortality. NO2 is also an important precursor for ozone and fine particulates, which also have severe health impacts. In urban areas, the majority of NO2 originates from anthropogenic NOx (&#x3D;NO+NO2; most NOx is emitted as NO, which rapidly cycles to NO2) emissions during high-temperature fossil fuel combustion. Tropospheric NO2 vertical column contents are qualitatively representative of near-surface NO2 concentrations and NOx emissions in urban/polluted locations.
&lt;br&gt;&lt;h4 id&#x3D;&quot;haq_tropomi_no2_global_a_l3&quot;&gt;HAQ_TROPOMI_NO2_GLOBAL_A_L3&lt;/h4&gt;
This product provides level 3 annual averages of tropospheric Nitrogen dioxide (NO2) vertical column density derived from the level 2 Tropospheric Monitoring Instrument (TROPOMI) across the globe oversampled to a spatial resolution of 0.1˚ x 0.1˚ (&lt;del&gt;10 km2) using a consistent algorithm from the European Space Agency (ESA) version 2.4 that can be used for trend analysis of air pollution. The dataset record began in January 2019 and continues to the present. This L3 product was developed by the George Washington University Air, Climate and Health Laboratory as part of the NASA Health Air Quality Applied Science Team (HAQAST) using Level 2 version 2.4 TROPOMI NO2 files from the ESA. The TROPOMI instrument on Sentinel-5 Precursor acquires tropospheric NO2 column contents from low Earth orbit (&lt;/del&gt;824 km above ground level) once per day globally at approximately 13:30 local time. NO2 is an air pollutant that adversely affects the human respiratory system and leads to premature mortality. NO2 is also an important precursor for ozone and fine particulates, which also have severe health impacts. In urban areas, the majority of NO2 originates from anthropogenic NOx (&#x3D;NO+NO2; most NOx is emitted as NO, which rapidly cycles to NO2) emissions during high-temperature fossil fuel combustion. Tropospheric NO2 vertical column contents are qualitatively representative of near-surface NO2 concentrations and NOx emissions in urban/polluted locations.
&lt;br&gt;&lt;h4 id&#x3D;&quot;haq_tropomi_no2_global_m_l3&quot;&gt;HAQ_TROPOMI_NO2_GLOBAL_M_L3&lt;/h4&gt;
This product provides level 3 monthly averages of tropospheric Nitrogen dioxide (NO2) vertical column density derived from the level 2 Tropospheric Monitoring Instrument (TROPOMI) across the globe oversampled to a spatial resolution of 0.1˚ x 0.1˚ (&lt;del&gt;10 km2) using a consistent algorithm from the European Space Agency (ESA) version 2.4 that can be used for trend analysis of air pollution. The dataset record began in January 2019 and continues to the present. This L3 product was developed by the George Washington University Air, Climate and Health Laboratory as part of the NASA Health Air Quality Applied Science Team (HAQAST) using Level 2 version 2.4 TROPOMI NO2 files from the ESA. The TROPOMI instrument on Sentinel-5 Precursor acquires tropospheric NO2 column contents from low Earth orbit (&lt;/del&gt;824 km above ground level) once per day globally at approximately 13:30 local time. NO2 is an air pollutant that adversely affects the human respiratory system and leads to premature mortality. NO2 is also an important precursor for ozone and fine particulates, which also have severe health impacts. In urban areas, the majority of NO2 originates from anthropogenic NOx (&#x3D;NO+NO2; most NOx is emitted as NO, which rapidly cycles to NO2) emissions during high-temperature fossil fuel combustion. Tropospheric NO2 vertical column contents are qualitatively representative of near-surface NO2 concentrations and NOx emissions in urban/polluted locations.
&lt;br&gt;&lt;h4 id&#x3D;&quot;haqes_na_pm25_bc_census&quot;&gt;HAQES_NA_PM25_BC_CENSUS&lt;/h4&gt;
This product provides HAQES 3-hourly ensemble mean surface PM2.5 Black Carbon concentration at the census level over the continental United States (CONUS). The Hazardous Air Quality Ensemble System (HAQES) is a real-time ensemble forecast of hazardous air quality events, such as wildfires, dust storms, and Volcanic eruptions. Both regional and global models from multiple agencies are used to create the ensemble, including the Goddard Earth Observing System (GEOS) from the National Aeronautics and Space Administration (NASA), the Navy Aerosol Analysis and Prediction System (NAAPS) from Naval Research Laboratory, the Global Ensemble Forecast System Aerosols (GEFS), High-Resolution Rapid Refresh (HRRR), and National Oceanic and Atmospheric Administration-U.S. Environmental Protection Agency (NOAA-EPA) Atmosphere-Chemistry Coupler-Community Multiscale Air Quality model (NACC-CMAQ) from NOAA. The prototypes of HAQES products were developed by the George Mason University Air Quality Laboratory as part of the NASA Health Air Quality Applied Science Team (HAQAST).
&lt;br&gt;&lt;h4 id&#x3D;&quot;haqes_na_pm25_bc_county&quot;&gt;HAQES_NA_PM25_BC_COUNTY&lt;/h4&gt;
This product provides HAQES 3-hourly ensemble mean surface PM2.5 Black Carbon concentration at the county level over the continental United States (CONUS). The Hazardous Air Quality Ensemble System (HAQES) is a real-time ensemble forecast of hazardous air quality events, such as wildfires, dust storms, and Volcanic eruptions. Both regional and global models from multiple agencies are used to create the ensemble, including the Goddard Earth Observing System (GEOS) from the National Aeronautics and Space Administration (NASA), the Navy Aerosol Analysis and Prediction System (NAAPS) from Naval Research Laboratory, the Global Ensemble Forecast System Aerosols (GEFS), High-Resolution Rapid Refresh (HRRR), and National Oceanic and Atmospheric Administration-U.S. Environmental Protection Agency (NOAA-EPA) Atmosphere-Chemistry Coupler-Community Multiscale Air Quality model (NACC-CMAQ) from NOAA. The prototypes of HAQES products were developed by the George Mason University Air Quality Laboratory as part of the NASA Health Air Quality Applied Science Team (HAQAST).
&lt;br&gt;&lt;h4 id&#x3D;&quot;haqes_na_pm25_bc&quot;&gt;HAQES_NA_PM25_BC&lt;/h4&gt;
This product provides HAQES 3-hourly ensemble mean surface PM2.5 Black Carbon concentration over the continental United States (CONUS) and surrounding regions. The data is mapped on Lambert projection. The Hazardous Air Quality Ensemble System (HAQES) is a real-time ensemble forecast of hazardous air quality events, such as wildfires, dust storms, and Volcanic eruptions. Both regional and global models from multiple agencies are used to create the ensemble, including the Goddard Earth Observing System (GEOS) from the National Aeronautics and Space Administration (NASA), the Navy Aerosol Analysis and Prediction System (NAAPS) from Naval Research Laboratory, the Global Ensemble Forecast System Aerosols (GEFS), High-Resolution Rapid Refresh (HRRR), and National Oceanic and Atmospheric Administration-U.S. Environmental Protection Agency (NOAA-EPA) Atmosphere-Chemistry Coupler-Community Multiscale Air Quality model (NACC-CMAQ) from NOAA. The prototypes of HAQES products were developed by the George Mason University Air Quality Laboratory as part of the NASA Health Air Quality Applied Science Team (HAQAST).
&lt;br&gt;&lt;h4 id&#x3D;&quot;haqes_na_pm25_oc_census&quot;&gt;HAQES_NA_PM25_OC_CENSUS&lt;/h4&gt;
This product provides HAQES 3-hourly ensemble mean surface PM2.5 Organic Carbon concentration at the census level over the continental United States (CONUS). The Hazardous Air Quality Ensemble System (HAQES) is a real-time ensemble forecast of hazardous air quality events, such as wildfires, dust storms, and Volcanic eruptions. Both regional and global models from multiple agencies are used to create the ensemble, including the Goddard Earth Observing System (GEOS) from the National Aeronautics and Space Administration (NASA), the Navy Aerosol Analysis and Prediction System (NAAPS) from Naval Research Laboratory, the Global Ensemble Forecast System Aerosols (GEFS), High-Resolution Rapid Refresh (HRRR), and National Oceanic and Atmospheric Administration-U.S. Environmental Protection Agency (NOAA-EPA) Atmosphere-Chemistry Coupler-Community Multiscale Air Quality model (NACC-CMAQ) from NOAA. The prototypes of HAQES products were developed by the George Mason University Air Quality Laboratory as part of the NASA Health Air Quality Applied Science Team (HAQAST).
&lt;br&gt;&lt;h4 id&#x3D;&quot;haqes_na_pm25_oc_county&quot;&gt;HAQES_NA_PM25_OC_COUNTY&lt;/h4&gt;
This product provides HAQES 3-hourly ensemble mean surface PM2.5 Organic Carbon concentration at the county level over the continental United States (CONUS). The Hazardous Air Quality Ensemble System (HAQES) is a real-time ensemble forecast of hazardous air quality events, such as wildfires, dust storms, and Volcanic eruptions. Both regional and global models from multiple agencies are used to create the ensemble, including the Goddard Earth Observing System (GEOS) from the National Aeronautics and Space Administration (NASA), the Navy Aerosol Analysis and Prediction System (NAAPS) from Naval Research Laboratory, the Global Ensemble Forecast System Aerosols (GEFS), High-Resolution Rapid Refresh (HRRR), and National Oceanic and Atmospheric Administration-U.S. Environmental Protection Agency (NOAA-EPA) Atmosphere-Chemistry Coupler-Community Multiscale Air Quality model (NACC-CMAQ) from NOAA. The prototypes of HAQES products were developed by the George Mason University Air Quality Laboratory as part of the NASA Health Air Quality Applied Science Team (HAQAST).
&lt;br&gt;&lt;h4 id&#x3D;&quot;haqes_na_pm25_oc&quot;&gt;HAQES_NA_PM25_OC&lt;/h4&gt;
This product provides HAQES 3-hourly ensemble mean surface PM2.5 Organic Carbon concentration over the continental United States (CONUS) and surrounding regions. The data is mapped on Lambert projection. The Hazardous Air Quality Ensemble System (HAQES) is a real-time ensemble forecast of hazardous air quality events, such as wildfires, dust storms, and Volcanic eruptions. Both regional and global models from multiple agencies are used to create the ensemble, including the Goddard Earth Observing System (GEOS) from the National Aeronautics and Space Administration (NASA), the Navy Aerosol Analysis and Prediction System (NAAPS) from Naval Research Laboratory, the Global Ensemble Forecast System Aerosols (GEFS), High-Resolution Rapid Refresh (HRRR), and National Oceanic and Atmospheric Administration-U.S. Environmental Protection Agency (NOAA-EPA) Atmosphere-Chemistry Coupler-Community Multiscale Air Quality model (NACC-CMAQ) from NOAA. The prototypes of HAQES products were developed by the George Mason University Air Quality Laboratory as part of the NASA Health Air Quality Applied Science Team (HAQAST).
&lt;br&gt;&lt;h4 id&#x3D;&quot;haqes_na_pm25_tot_census&quot;&gt;HAQES_NA_PM25_TOT_CENSUS&lt;/h4&gt;
This product provides HAQES 3-hourly ensemble mean surface total PM2.5 concentration at the census level over the continental United States (CONUS). The Hazardous Air Quality Ensemble System (HAQES) is a real-time ensemble forecast of hazardous air quality events, such as wildfires, dust storms, and Volcanic eruptions. Both regional and global models from multiple agencies are used to create the ensemble, including the Goddard Earth Observing System (GEOS) from the National Aeronautics and Space Administration (NASA), the Navy Aerosol Analysis and Prediction System (NAAPS) from Naval Research Laboratory, the Global Ensemble Forecast System Aerosols (GEFS), High-Resolution Rapid Refresh (HRRR), and National Oceanic and Atmospheric Administration-U.S. Environmental Protection Agency (NOAA-EPA) Atmosphere-Chemistry Coupler-Community Multiscale Air Quality model (NACC-CMAQ) from NOAA. The prototypes of HAQES products were developed by the George Mason University Air Quality Laboratory as part of the NASA Health Air Quality Applied Science Team (HAQAST).
&lt;br&gt;&lt;h4 id&#x3D;&quot;haqes_na_pm25_tot_county&quot;&gt;HAQES_NA_PM25_TOT_COUNTY&lt;/h4&gt;
This product provides HAQES 3-hourly ensemble mean surface total PM2.5 concentration at the county level over the continental United States (CONUS). The Hazardous Air Quality Ensemble System (HAQES) is a real-time ensemble forecast of hazardous air quality events, such as wildfires, dust storms, and Volcanic eruptions. Both regional and global models from multiple agencies are used to create the ensemble, including the Goddard Earth Observing System (GEOS) from the National Aeronautics and Space Administration (NASA), the Navy Aerosol Analysis and Prediction System (NAAPS) from Naval Research Laboratory, the Global Ensemble Forecast System Aerosols (GEFS), High-Resolution Rapid Refresh (HRRR), and National Oceanic and Atmospheric Administration-U.S. Environmental Protection Agency (NOAA-EPA) Atmosphere-Chemistry Coupler-Community Multiscale Air Quality model (NACC-CMAQ) from NOAA. The prototypes of HAQES products were developed by the George Mason University Air Quality Laboratory as part of the NASA Health Air Quality Applied Science Team (HAQAST).
&lt;br&gt;&lt;h4 id&#x3D;&quot;haqes_na_pm25_tot&quot;&gt;HAQES_NA_PM25_TOT&lt;/h4&gt;
This product provides HAQES 3-hourly ensemble mean surface total PM2.5 concentration over the continental United States (CONUS) and surrounding regions. The data is mapped on Lambert projection. The Hazardous Air Quality Ensemble System (HAQES) is a real-time ensemble forecast of hazardous air quality events, such as wildfires, dust storms, and Volcanic eruptions. Both regional and global models from multiple agencies are used to create the ensemble, including the Goddard Earth Observing System (GEOS) from the National Aeronautics and Space Administration (NASA), the Navy Aerosol Analysis and Prediction System (NAAPS) from Naval Research Laboratory, the Global Ensemble Forecast System Aerosols (GEFS), High-Resolution Rapid Refresh (HRRR), and National Oceanic and Atmospheric Administration-U.S. Environmental Protection Agency (NOAA-EPA) Atmosphere-Chemistry Coupler-Community Multiscale Air Quality model (NACC-CMAQ) from NOAA. The prototypes of HAQES products were developed by the George Mason University Air Quality Laboratory as part of the NASA Health Air Quality Applied Science Team (HAQAST).
&lt;br&gt;&lt;h4 id&#x3D;&quot;merra2_cnn_haqast_pm25&quot;&gt;MERRA2_CNN_HAQAST_PM25&lt;/h4&gt;
This product provides MERRA-2 bias-corrected global hourly surface total PM2.5 mass concentration with the same horizontal spatial resolution as MERRA-2, covering a temporal range from 2000 to 2024. It is derived using a machine learning (ML) approach with a convolutional neural network (CNN) method and is specifically developed for the NASA Health and Air Quality Applied Sciences Team (HAQAST). The dataset consists of two parameters: MERRA2_CNN_Surface_PM25 and QFLAG. MERRA2_CNN_Surface_PM25, a 3-dimensional variable (time, latitude, longitude), represents the surface PM2.5 concentrations in µg/m³. QFLAG denotes the quality of data at each grid point, where 4 indicates the highest quality and 1 indicates the lowest quality. It is recommended to use QFLAG values of 3 and 4 for quantitative analysis.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sfc_nitrogen_dioxide_conc&quot;&gt;SFC_NITROGEN_DIOXIDE_CONC&lt;/h4&gt;
The Nitrogen Dioxide Surface-Level Annual Average Concentrations Product (SFC_NITROGEN_DIOXIDE_CONC) contains estimated global NO2 surface values derived using a Land Use Regression (LUR) model (based on 5220 NO2 monitors in 58 countries and land use variables) for the years 2010-2012. NO2 column densities from the Ozone Monitoring Instrument and MERRA-2 scale the concentrations to other years between 1990 and 2020. This product is part of NASA&amp;#39;s Health and Air Quality Applied Sciences Team (HAQAST) effort. The data are global over land and span the latitude range between 60 south and 75 north, gridded at 0.0083 degree resolution (array size is 43080 x 16200). Data variables include surface NO2, as well as latitude and longitude values. The data are written to files using the new version 4 netCDF format. The average file size is about 150 Megabytes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA HLS Project</title>
      <link>https://registry.opendata.aws/nasa-hls</link>
      <guid>https://registry.opendata.aws/nasa-hls</guid>
      <description>The HLSL30 V1.5 data product was decommissioned on January 4, 2022. Users are encouraged to use the improved &lt;a href&#x3D;&quot;https://doi.org/10.5067/HLS/HLSL30.002&quot;&gt;HLSL30 V2&lt;/a&gt; data product. The Harmonized Landsat Sentinel-2 (HLS) project provides consistent surface reflectance (SR) and top of atmosphere (TOA) brightness data from the Operational Land Imager (OLI) aboard the joint NASA/USGS Landsat 8 satellite and the Multi-Spectral Instrument (MSI) aboard Europe’s Copernicus Sentinel-2A and Sentinel-2B satellites. The combined measurement enables global observations of the land every 2–3 days at 30-meter (m) spatial resolution. The HLS project uses a set of algorithms to obtain seamless products from OLI and MSI that include atmospheric correction, cloud and cloud-shadow masking, spatial co-registration and common gridding, illumination and view angle normalization, and spectral bandpass adjustment. The HLSL30 product provides 30-m Nadir Bidirectional Reflectance Distribution Function (BRDF)-Adjusted Reflectance (NBAR) and is derived from Landsat 8 OLI data products. The &lt;a href&#x3D;&quot;https://doi.org/10.5067/HLS/HLSS30.015&quot;&gt;HLSS30&lt;/a&gt; and HLSL30 products are gridded to the same resolution and Military Grid Reference System (&lt;a href&#x3D;&quot;https://hls.gsfc.nasa.gov/products-description/tiling-system/&quot;&gt;MGRS&lt;/a&gt;) tiling system and thus are “stackable” for time series analysis. The HLSL30 product is provided in Cloud Optimized GeoTIFF (COG) format, and each band is distributed as a separate file. There are 10 bands included in the HLSL30 product along with one quality assessment (QA) band and four angle bands. For a more detailed description of the individual bands provided in the HLSL30 product, please see the User Guide. The HLS project is funded by NASA’s Satellite Needs Working Group (SNWG) which provides data products developed to meet the needs of stakeholders from US government agencies. Known Issues: HLSL30.015 products are based on input Landsat 8 L1TP (precision terrain corrected) products, which require identification of ground control targets for precision geometric correction. Images where ground control is not available (e.g., very cloudy images) cannot be processed to L1TP and are not included in the HLSL30 dataset. * Interruptions in data service occurred during a restaging of backlogged data between June 1 and June 15, 2021 for both HLSS30 and HLSL30 version 1.5 data products. During this time period increased errors in the processing workflow resulted in a significant number of data ingestion failures and thus, significant gaps in data availability. Given the pending release of the version 2.0, science quality HLS products, these missing data will not be filled for version 1.5. Users of the provisional version 1.5 products should be aware of the significant data gap in this two week window. The version 2.0 products will incorporate these data back into the archive. If you have any feedback or questions on the data please contact &lt;a href&#x3D;&quot;https://www.earthdata.nasa.gov/centers/lp-daac/contact&quot;&gt;Customer Services&lt;/a&gt; or join our HLS conversion on the &lt;a href&#x3D;&quot;https://forum.earthdata.nasa.gov/viewtopic.php?f&#x3D;7&amp;amp;t&#x3D;618&amp;amp;hilit&#x3D;hls&amp;amp;sid&#x3D;95750d868b6448e0f4360a1473def234&quot;&gt;Earthdata Forum&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;hlsl30_vi&quot;&gt;HLSL30_VI&lt;/h4&gt;
The Harmonized Landsat and Sentinel-2 (HLS) project provides consistent data products from the Operational Land Imager (OLI) aboard the joint NASA/USGS Landsat 8 and Landsat 9 satellites and the Multi-Spectral Instrument (MSI) aboard Europe’s Copernicus Sentinel-2A, Sentinel-2B, and Sentinel-2C satellites. The combined measurement enables global observations of the land every 2–3 days at 30 meter (m) spatial resolution. The HLSL30 Vegetation Indices (HLSL30_VI) product is derived from Landsat 8 and Landsat 9 OLI data products. Vegetation indices combine specific bands of satellite data to quantify various aspects of vegetation. Analysis of vegetation indices allows for tracking changes in vegetation over time, identifying areas of stress or deforestation, and assessing crop health. Vegetation indices provide a reliable and efficient means of understanding the complex dynamics of vegetation health. The HLSS30_VI and HLSL30_VI products are gridded to the same resolution and Military Grid Reference System (&lt;a href&#x3D;&quot;https://hls.gsfc.nasa.gov/products-description/tiling-system/&quot;&gt;MGRS&lt;/a&gt;) tiling system and thus are “stackable” for time series analysis. The HLSL30_VI product is provided in Cloud Optimized GeoTIFF (COG) format, and each variable is distributed as a separate file. Nine indicators of vegetation health are included in the HLSL30_VI product: Normalized Difference Vegetation Index (NDVI), Enhanced Vegetation Index (EVI), Soil Adjusted Vegetation Index (SAVI), Modified Soil Adjusted Vegetation Index (MSAVI), Normalized Difference Moisture Index (NDMI), Normalized Difference Water Index (NDWI), Normalized Burn Ratio (NBR), Normalized Burn Ratio 2 (NBR2), and Triangular Vegetation Index (TVI). See the User Guide for a more detailed description of the individual vegetation health variables provided in the HLSL30_VI product. The HLS project is funded by NASA’s Satellite Needs Working Group (SNWG) which provides data products developed to meet the needs of stakeholders from US government agencies.
&lt;br&gt;&lt;h4 id&#x3D;&quot;hlss30&quot;&gt;HLSS30&lt;/h4&gt;
The HLSS30 V1.5 data product was decommissioned on January 4, 2022. Users are encouraged to use the improved &lt;a href&#x3D;&quot;https://doi.org/10.5067/HLS/HLSS30.002&quot;&gt;HLSS30 V2&lt;/a&gt; data product. The Harmonized Landsat Sentinel-2 (HLS) project provides consistent surface reflectance data from the Operational Land Imager (OLI) aboard the joint NASA/USGS Landsat 8 satellite and the Multi-Spectral Instrument (MSI) aboard the European Union’s Copernicus Sentinel-2A and Sentinel-2B satellites. The combined measurement enables global observations of the land every 2-3 days at 30 meter (m) spatial resolution. The HLS project uses a set of algorithms to obtain seamless products from OLI and MSI that include atmospheric correction, cloud and cloud-shadow masking, spatial co-registration and common gridding, illumination and view angle normalization, and spectral bandpass adjustment. The HLSS30 product provides 30 m Nadir Bidirectional Reflectance Distribution Function (BRDF)-Adjusted Reflectance (NBAR) and is derived from Sentinel-2A and Sentinel-2B MSI data products. The HLSS30 and &lt;a href&#x3D;&quot;https://doi.org/10.5067/HLS/HLSL30.015&quot;&gt;HLSL30&lt;/a&gt; products are gridded to the same resolution and Military Grid Reference System (&lt;a href&#x3D;&quot;https://hls.gsfc.nasa.gov/products-description/tiling-system/&quot;&gt;MGRS&lt;/a&gt;) tiling system and thus are “stackable” for time series analysis. The HLSS30 product is provided in Cloud Optimized GeoTIFF (COG) format, and each band is distributed as a separate COG. There are 13 bands included in the HLSS30 product along with four angle bands and a quality assessment (QA) band. For a more detailed description of the individual bands provided in the HLSS30 product, please see the User Guide. The HLS project is funded by NASA’s Satellite Needs Working Group (SNWG) which provides data products developed to meet the needs of stakeholders from US government agencies. Known Issues: Interruptions in data service occurred during a restaging of backlogged data between June 1 and June 15, 2021 for both HLSS30 and HLSL30 version 1.5 data products. During this time period increased errors in the processing workflow resulted in a significant number of data ingestion failures and thus, significant gaps in data availability. Given the pending release of the version 2.0, science quality HLS products, these missing data will not be filled for version 1.5. Users of the provisional version 1.5 products should be aware of the significant data gap in this two week window. The version 2.0 products will incorporate these data back into the archive. If you have any feedback or questions on the data please contact &lt;a href&#x3D;&quot;https://www.earthdata.nasa.gov/centers/lp-daac/contact&quot;&gt;Customer Services&lt;/a&gt; or join our HLS conversion on the &lt;a href&#x3D;&quot;https://forum.earthdata.nasa.gov/viewtopic.php?f&#x3D;7&amp;amp;t&#x3D;618&amp;amp;hilit&#x3D;hls&amp;amp;sid&#x3D;95750d868b6448e0f4360a1473def234&quot;&gt;Earthdata Forum&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;hlss30-1&quot;&gt;HLSS30&lt;/h4&gt;
The Harmonized Landsat Sentinel-2 (HLS) project provides consistent surface reflectance data from the Operational Land Imager (OLI) aboard the joint NASA/USGS Landsat 8 satellite and the Multi-Spectral Instrument (MSI) aboard Europe’s Copernicus Sentinel-2A, Sentinel-2B, and Sentinel-2C satellites. The combined measurement enables global observations of the land every 2–3 days at 30-meter (m) spatial resolution. The HLS project uses a set of algorithms to obtain seamless products from OLI and MSI that include atmospheric correction, cloud and cloud-shadow masking, spatial co-registration and common gridding, illumination and view angle normalization, and spectral bandpass adjustment. The HLSS30 product provides 30-m Nadir Bidirectional Reflectance Distribution Function (BRDF)-Adjusted Reflectance (NBAR) and is derived from Sentinel-2A, Sentinel-2B, and Sentinel-2C MSI data products. The HLSS30 and &lt;a href&#x3D;&quot;https://doi.org/10.5067/HLS/HLSL30.002&quot;&gt;HLSL30&lt;/a&gt; products are gridded to the same resolution and Military Grid Reference System (&lt;a href&#x3D;&quot;https://hls.gsfc.nasa.gov/products-description/tiling-system/&quot;&gt;MGRS&lt;/a&gt;) tiling system and thus are “stackable” for time series analysis. The HLSS30 product is provided in Cloud Optimized GeoTIFF (COG) format, and each band is distributed as a separate COG. There are 13 bands included in the HLSS30 product along with four angle bands and a quality assessment (QA) band. See the User Guide for a more detailed description of the individual bands provided in the HLSS30 product. The HLS project is funded by NASA’s Satellite Needs Working Group (SNWG) which provides data products developed to meet the needs of stakeholders from US government agencies. Known Issues: Unrealistically high aerosol and low surface reflectance over bright areas: The atmospheric correction over bright targets occasionally retrieves unrealistically high aerosol and thus makes the surface reflectance too low. High aerosol retrievals, both false high aerosol and realistically high aerosol, are masked when quality bits 6 and 7 are both set to 1 (see Table 9 in the &lt;a href&#x3D;&quot;https://lpdaac.usgs.gov/documents/1698/HLS_User_Guide_V2.pdf&quot;&gt;User Guide&lt;/a&gt;); the corresponding spectral data should be discarded from analysis. * Issues over high latitudes: For scenes greater than or equal to 80 degrees north, multiple overpasses can be gridded into a single MGRS tile resulting in an L30 granule with data sensed at two different times. In this same area, it is also possible that Landsat overpasses that should be gridded into a single MGRS tile are actually written as separate data files. Finally, for scenes with a latitude greater than or equal to 65 degrees north, ascending Landsat scenes may have a slightly higher error in the BRDF correction because the algorithm is calibrated using descending scenes. * Fmask omission errors: There are known issues regarding the Fmask band of this data product that impacts HLSL30 data prior to April of 2022. The HLS Fmask data band may have omission errors in water detection for cases where water detection using spectral data alone is difficult, and omission and commission errors in cloud shadow detection for areas with great topographic relief. This issue does not impact other bands in the dataset. * Inconsistent snow surface reflectance between Landsat and Sentinel-2: The HLS snow surface reflectance can be highly inconsistent between Landsat and Sentinel-2. When assessed on same-day acquisitions from Landsat and Sentinel-2, Landsat reflectance is generally higher than Sentinel-2 reflectance in the visible bands. * Unrealistically high snow surface reflectance in the visible bands: By design, the Land Surface Reflectance Code (LaSRC) atmospheric correction does not attempt aerosol retrieval over snow; instead, a default aerosol optical thickness (AOT) is used to drive the snow surface reflectance. If the snow detection fails, the full LaSRC is used in both AOT retrieval and surface reflectance derivation over snow, which produces surface reflectance values as high as 1.6 in the visible bands. This is a common problem for spring images at high latitudes. * Unrealistically low surface reflectance surrounding snow/ice: Related to the above, the AOT retrieval over snow/ice is generally too high. When this artificially high AOT is used to derive the surface reflectance of the neighboring non-snow pixels, very low surface reflectance will result. These pixels will appear very dark in the visible bands. If the surface reflectance value of a pixel is below -0.2, a NO_DATA value of -9999 is used. In Figure 1, the pixels in front of the glaciers have surface reflectance values that are too low. * Unrealistically low reflectance surrounding clouds: Like for snow, the HLS atmospheric correction does not attempt aerosol retrieval over clouds and a default AOT is used instead. But if the cloud detection fails, an artificially high AOT will be retrieved over clouds. If the high AOT is used to derive the surface reflectance of the neighboring cloud-free pixels, very low surface reflectance values will result. If the surface reflectance value of a pixel is below -0.2, a NO_DATA value of -9999 is used. * Unusually low reflectance around other bright land targets: While the HLS atmospheric correction retrieves AOT over non-cloud, non-snow bright pixels, the retrieved AOT over bright targets can be unrealistically high in some cases, similar to cloud or snow. If this unrealistically high AOT is used to derive the surface reflectance of the neighboring pixels, very low surface reflectance values can result as shown in Figure 2. If the surface reflectance value of a pixel is below -0.2, a NO_DATA value of -9999 is used. These types of bright targets are mostly man-made, such as buildings, parking lots, and roads. * Dark plumes over water: The HLS atmospheric correction does not attempt aerosol retrieval over water. For water pixels, the AOT retrieved from the nearest land pixels is used to derive the surface reflectance, but if the retrieval is incorrect, e.g. from a cloud pixel, this high AOT will create dark stripes over water, as shown in Figure 3. This happens more often over large water bodies, such as lakes and bays, than over narrow rivers. * Landsat WRS-2 Path/Row boundary in L30 reflectance: HLS performs atmospheric correction on Landsat Level 1 images in the original Worldwide Reference System 2 (WRS2) path/row before the derived surface reflectance is reprojected into Military Grid Reference System (MGRS) tiles. If a WRS-2 Landsat image is very cloudy, the AOT from a few remaining clear pixels might be used for the atmospheric correction of the entire image. The AOT that is used can be quite different from the value for the adjacent row in the same path, which results in an artificial abrupt change from one row to the next, as shown in Figure 4. This occurrence is very rare. * Landsat WRS2 path/row boundary in cloud masks: The cloud mask algorithm Fmask creates mask labels by applying thresholds to the histograms of some metrics for each path/row independently. If two adjacent rows in the same path have distinct distributions within the metrics, abrupt changes in masking patterns can appear across the row boundary, as shown in Figure 5. This occurrence is very rare. * Fmask configuration was deficient for 2-3 months in 2021: The HLS installation of Fmask failed to include auxiliary digital elevation model (DEM) and European Space Agency (ESA) Global Surface Water Occurrence data for a 2-3 month run in 2021. This impacted the masking results over water and in mountainous regions. * The reflectance “scale_factor” and “offset” for some L30 and S30 bands were not set: The HLS reflectance scaling factor is 0.0001 and offset is 0. However, this information was not set in the Cloud Optimized GeoTIFF (COG) files of some bands for a small number of granules. The lack of this information creates a problem for automatic conversion of the reflectance data, requiring explicit scaling in applications. The problem has been corrected, but the affected granules have not been reprocessed. * Incomplete map projection information: For a time, HLS imagery was produced with an incomplete coordinate reference system (CRS). The metadata contains the Universal Transverse Mercator (UTM) zone and coordinates necessary to geolocate pixels within the image but might not be in a standard form, especially for granules produced early in the HLS mission. As a result, an error will occur in certain image processing packages due to the incomplete CRS. The simplest solution is to update to the latest version of Geospatial Data Abstraction Library (GDAL) and/or rasterio, which use the available information without error. * False northing of 10^7 for the L30 angle data: The L30 and S30 products do not use a false northing for the UTM projection, and the angle data are supposed to follow the same convention. However, the L30 angle data incorrectly uses a false northing of 10^7. There is no problem with the angle data itself, but the false northing needs to be set to 0 for it to be aligned with the reflectance. * L30 from Landsat L1GT scenes: Landsat L1GT scenes were not intended for HLS due to their poor geolocation. However, some scenes made it through screening for a short period of HLS production. L1GT L30 scenes mainly consist of extensive cloud or snow that can be eliminated using the Fmask quality bits layer. Users can also identify an L1GT-originated L30 granule by examining the HLS cmr.xml metadata file. * The UTC dates in the L30/S30 filenames may not be the local dates: UTC dates are used by ESA and the U.S. Geological Survey (USGS) in naming their Level 1 images, and HLS processing retains this information to name the L30 and S30 products. Landsat and Sentinel-2 overpass eastern Australia and New Zealand around 10AM local solar time, but this area is in either UTC+10:00 or +11:00 zone; therefore, the UTC time for some orbits is in fact near the end of the preceding UTC day. For example, HLS.S30.T59HQS.2016117T221552.v2.0 was acquired in the 22nd hour of day 117 of year 2016 in UTC, but the time was 10:15:52 of day 118 locally. Approximately 100 minutes later HLS.S30.T56JML.2016117T235252.v2.0 was acquired in the next orbit in eastern Australia. This issue also occurs for Landsat. For example, HLS.L30.T59HQS.2016117T221209.v2.0 was acquired on the same day as the first S30 example given above, but both on day 118 of 2016 locally. Adding to the confusion for L30, in the same region, Landsat 8 and 9 can each overpass once in one of the two adjacent WRS-2 Paths (91/92/93) over a two-day period on a local calendar, but based on UTC time, the two overpasses can appear to be on the same day. For example, in the following seemingly same-day pair, the second L30 is actually for day 168 locally: HLS.L30.T55GCN.2023167T000407.v2.0 HLS.L30.T55GCN.2023167T235747.v2.0 Bear in mind, the date peculiarity for the data occurs when the overpass time is during the late hours of a UTC day. * The atmospheric ancillary data from the wrong date was used for LaSRC: Related to the above, for eastern Australia and New Zealand, L30 and S30 surface reflectance on certain days was created using the atmospheric ancillary data from a date that was one day too early. The exact geographic extent of the affected HLS products and the impact on the surface reflectance quality are under investigation. Practice caution when using data with overpass times during the late hours of a UTC day. * Duplicates in L30: The Landsat 9 acquisitions from October 2021 to March 2023 in Landsat Collection 2 were reprocessed by USGS in March 2023. This reprocessing updated the overpass time by a fraction of a second for some scenes. Since HLS uses overpass time as part of the L30 filename, the older L30 granules were not automatically overwritten due to the different filenames. For example, the first L30 granule in the following pair originated from an older version of L1TP of Landsat 9 with the second granule originating from the reprocessed version. HLS.L30.T11SLC.2022166T182646.v2.0 HLS.L30.T11SLC.2022166T182645.v2.0 There are other causes of duplicate L30 granules, but the overall number of duplicates is very small. * Poor Geolocation: A large amount of granules that were processed for May through July 2023 were created with L1GT input scenes which were deemed undesirable due to a poor geolocation issue. These granules were removed from the archive. (see the full list of removed &lt;a href&#x3D;&quot;https://lpdaac.usgs.gov/documents/2161/L30_L1GT_granules_May_July_2023.csv&quot;&gt;granules&lt;/a&gt;)
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA HRAC Project</title>
      <link>https://registry.opendata.aws/nasa-hrac</link>
      <guid>https://registry.opendata.aws/nasa-hrac</guid>
      <description>This is a dataset that enhances the TMPA monthly product (3B43) in its accuracy and spatial resolution, in hydrometeorological applications. About 9,200 gauge measurement are used to compare with the 3B43 product at 0.25° x 0.25° spatial resolution across the CONUS. Observed is a strong relationship between the bias and land surface elevation, in which 3B43 underestimates the true precipitation at the elevations above 1,500 m amsl. Satellite data is resampled to elevation data at ~1km grid size and applied a correction function to reduce bias in the data. Accordingly, a High-Resolution Altitude-Corrected product is constructed, based on 3B43 and covering the entire CONUS at 1-km resolution. This product is verified against 9,200 gauges across the country. The results showed a substantial improvement in the satellite-gauge data accuracy as well as spatial resolution.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA HWHYP Project</title>
      <link>https://registry.opendata.aws/nasa-hwhyp</link>
      <guid>https://registry.opendata.aws/nasa-hwhyp</guid>
      <description>The Headwall Hyperspectral Reflectance data are for the Long-Term Ecological Research (LTER) at Cedar Creek Ecosystem Science Reserve (CCESR), Minnesota (HWHYPCCMN1MM). The reflectance products are at 1 millimeter (mm) spatial resolution in the 400 to 1,000 nanometer spectral range. This dataset can be used to understand the optical diversity-biodiversity relationship and investigate the spatial sensitivity of the relationship at local scales. A Headwall Series E imaging spectrometer was mounted on a tram system to collect designated plots for the biodiversity (BioDIV) experiment at the LTER Cedar Creek site. The imaging spectrometer, located 3 meters above the ground surface, obtained 1 mm ground pixel size of hyperspectral field image cubes that are among the finest spatial resolution available. The fine-scale images were acquired at a prairie grassland ecosystem during June/July 2014 and July 2015. Provided in the HWHYPCCMN1MM product are 920 to 924 hyperspectral bands in an Environment for Visualizing Images (ENVI) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA Hydroclimatology Project</title>
      <link>https://registry.opendata.aws/nasa-hydroclimatology</link>
      <guid>https://registry.opendata.aws/nasa-hydroclimatology</guid>
      <description>The Global Monthly River Discharge Data Set (RivDIS) contains monthly averaged discharge measurements for 1,018 stations located throughout the world from 1807-1991. The period of record varies widely from station to station with a mean of 21.5 years. The data are derived from the published UNESCO archives for river discharge, and checked against information obtained from the Global Runoff Center in Koblenz, Germany through the U.S. National Geophysical Data Center in Boulder, Colorado.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sahel_water_bodies_1269&quot;&gt;Sahel_Water_Bodies_1269&lt;/h4&gt;
This data set provides an estimate of the spatial and temporal extent of surface water at 250-m resolution over nine years (2003-2011) for the African Sahel region (10-20 degrees N) using imagery from the Moderate-resolution Imaging Spectroradiometer (MODIS). Water bodies were identified by a spectral analysis of MODIS vegetation indices with the aim to improve existing regional to global mapping products. This data set can be used to enhance the understanding of Earth system processes, and to support global change studies, agricultural planning, and disease prevention. These data provide a gridded (250-m) estimate of the number of years (during 2003-2011) that a pixel was covered by water. The data are presented in a single netCDF (.nc) file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;hcdn_810&quot;&gt;HCDN_810&lt;/h4&gt;
Time series of monthly minimum and maximum temperature, precipitation, and potential evapotranspiration were derived for 1,469 watersheds in the conterminous United States for which stream flow measurements were also available from the national streamflow database, termed the Hydro-Climatic Data Network (HCDN), developed by Slack et al. (1993a,b). Monthly climate estimates were derived for the years 1951-1990. The climate characteristic estimates of temperature and precipitation were estimated using the PRISM (Daly et al. 1994, 1997) climate analysis system as described in Vogel, et al. 1999. Estimates of monthly potential evaporation were obtained using a method introduced by Hargreaves and Samani (1982) which is based on monthly time series of average minimum and maximum temperature data along with extraterrestrial solar radiation. Extraterrestrial solar radiation was estimated for each basin by computing the solar radiation over 0.1 degree grids using the method introduced by Duffie and Beckman (1980) and then summing those estimates for each river basin. This process is described in Sankarasubramanian, et al. (2001). Revision Notes: This data set has been revised to update the number of watersheds included in the data set and to updated the units for the potential evapotranspiration variable. Please see the Data Set Revisions section of this document for detailed information.
&lt;br&gt;&lt;h4 id&#x3D;&quot;pad_935&quot;&gt;PAD_935&lt;/h4&gt;
The Peace-Athabasca Delta (PAD) is a large boreal wetland located in northeastern Alberta, Canada at the confluence of the Peace and Athabasca Rivers with Lake Athabasca (Figures 1 and 2). A Ramsar Convention wetland and UNESCO World Heritage Site, it is among the world&amp;#39;s most ecologically significant wetlands. This data set contains four comma-delimited ASCII files, two of which contain water surface elevation site and measurement information and two contain water quality and ancillary parameter location and measurement data for 120 sites within the PAD. Data archived include water surface elevation and water quality parameters measured at points throughout the Delta during summers 2006 and 2007. These data sets were originally collected to improve understanding of hydrologic recharge processes in low-relief environments and to provide ground-based measurements to validate satellite observations of inundation and sediment transport. All work was supported by the NASA Terrestrial Hydrology Program under grant NNG06GE05G to the Department of Geography, University of California-Los Angeles, Los Angeles, California.
&lt;br&gt;&lt;h4 id&#x3D;&quot;pad_2011_1133&quot;&gt;PAD_2011_1133&lt;/h4&gt;
The Peace-Athabasca Delta (PAD) is a hydrologically complex and ecologically diverse freshwater delta formed by the confluence of the Peace, Athabasca, and Birch Rivers near the western end of Lake Athabasca. This data set includes 3 comma-delimited ASCII files: one containing water quality data and site characteristics from June and July 2010, a second containing water quality data and site characteristics for June and July 2011, and a third containing spectral reflectance of the water surface for 2011. The 2010 data file has measurements from 62 unique sites, the majority of which were revisited in 2011. Both of the 2011 data files have measurements from 99 unique sites visited 1-4 times.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.ornldaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA INTEXB Project</title>
      <link>https://registry.opendata.aws/nasa-intexb</link>
      <guid>https://registry.opendata.aws/nasa-intexb</guid>
      <description>INTEX-NA is a two phase experiment that aims to understand the transport and transformation of gases and aerosols on transcontinental/intercontinental scales and assess their impact on air quality and climate. The primary constituents of interest are ozone and precursors, aerosols and precursors, and the long-lived greenhouse gases. The first phase (INTEX-A) was completed in the summer of 2004 and the second phase (INTEX-B) is to be performed in the spring of 2006. This document is intended to provide an update on the goals of INTEX-B and define its implementation strategy. The scientific goals envisioned here are based on the joint implementation of INTEX-B, MIRAGE-Mex and DLR/IMPACT studies and their coordination with satellite observations. In collaboration with these partners, the main goals of INTEX-B are to:- Quantify the transpacific transport and evolution of Asian pollution to North America and assess its implications for regional air quality and climate; - Quantify the outflow and evolution of gases and aerosols from the Mexico City Megaplex; - Investigate the transport of Asian and North America pollution to the eastern Atlantic and assess its implications for European air quality; - Validate and refine satellite observations of tropospheric composition; - Map emissions of trace gases and aerosols and relate atmospheric composition to sources and sinks.The INTEX-B field study is to be performed during an approximate 8-week period from March 1 to April 30, 2006.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ixbmigeo&quot;&gt;IXBMIGEO&lt;/h4&gt;
IXBMIGEO_2 is the Multi-angle Imaging SpectroRadiometer (MISR) Geometric Parameters subset for the INTEX-B region version 2. It contains the Geometric Parameters that measure the sun and view angles at the reference ellipsoid for the region covered by the INTEXB_2006 theme. MISR is designed to view Earth with cameras in 9 different directions. As the instrument flies overhead, all nine cameras successfully imaged each piece of Earth&amp;#39;s surface below in 4 wavelengths (blue, green, red, and near-infrared). MISR aims to improve our understanding of the effects of sunlight on Earth and distinguish different types of clouds, particles, and surfaces. Specifically, MISR monitors the monthly, seasonal, and long-term trends in three areas: 1) amount and type of atmospheric particles (aerosols), including those formed by natural sources and by human activities; 2) amounts, types, and heights of clouds, and 3) distribution of land surface cover, including vegetation canopy structure.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ixbmib2e&quot;&gt;IXBMIB2E&lt;/h4&gt;
IXBMIB2E_3 is the Multi-angle Imaging SpectroRadiometer (MISR) Level 1B2 Ellipsoid Product subset for the INTEX-B region V003. It contains Ellipsoid-projected TOA Radiance, resampled at the surface and topographically corrected and geometrically corrected by PGE22 for the region covered by the INTEXB_2006 theme. MISR is designed to view Earth with cameras in 9 different directions. As the instrument flies overhead, all nine cameras successfully imaged each piece of Earth&amp;#39;s surface below in 4 wavelengths (blue, green, red, and near-infrared). MISR aims to improve our understanding of the effects of sunlight on Earth and distinguish different types of clouds, particles, and surfaces. Specifically, MISR monitors the monthly, seasonal, and long-term trends in three areas: 1) amount and type of atmospheric particles (aerosols), including those formed by natural sources and by human activities; 2) amounts, types, and heights of clouds, and 3) distribution of land surface cover, including vegetation canopy structure.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ixbmib2t&quot;&gt;IXBMIB2T&lt;/h4&gt;
IXBMIB2T_3 is the Multi-angle Imaging SpectroRadiometer (MISR) Level 1B2 Terrain Product subset for the INTEX-B region version 3. It contains Terrain-projected TOA Radiance, resampled at the surface and topographically corrected, and geometrically corrected by PGE22 for the region covered by the INTEXB_2006 theme. MISR is designed to view Earth with cameras in 9 different directions. As the instrument flies overhead, all nine cameras successfully imaged each piece of Earth&amp;#39;s surface below in 4 wavelengths (blue, green, red, and near-infrared). MISR aims to improve our understanding of the effects of sunlight on Earth and distinguish different types of clouds, particles, and surfaces. Specifically, MISR monitors the monthly, seasonal, and long-term trends in three areas: 1) amount and type of atmospheric particles (aerosols), including those formed by natural sources and by human activities; 2) amounts, types, and heights of clouds, and 3) distribution of land surface cover, including vegetation canopy structure.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ixbmi2ae&quot;&gt;IXBMI2AE&lt;/h4&gt;
MISR Level 2 Aerosol Product containing aerosol optical depth and particle type, with associated atmospheric data for the INTEXB_2006 theme.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ixbmi2ls&quot;&gt;IXBMI2LS&lt;/h4&gt;
IXBMI2LS_002 is the Multi-angle Imaging SpectroRadiometer (MISR) Level 2 Land Surface Product subset for the INTEX-B region. It contains information on land directional reflectance properties, albedos(spectral and PAR integrated), FPAR, associated radiation parameters, and terrain-referenced geometric parameters for the region covered by the INTEXB_2006 theme. The MISR instrument consists of nine push-broom cameras that measure radiance in four spectral bands. Global coverage is achieved in nine days. The cameras are arranged with one camera pointing toward the nadir, four forward, and four aftward. It takes seven minutes for all nine cameras to view the same surface location. The view angles relative to the surface reference ellipsoid are 0, 26.1, 45.6, 60.0, and 70.5 degrees. The spectral band shapes are nominally Gaussian, centered at 443, 555, 670, and 865 nm.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ixbmi2st&quot;&gt;IXBMI2ST&lt;/h4&gt;
IXBMI2ST_2 is the Multi-angle Imaging SpectroRadiometer (MISR) L2 TOA/Cloud Stereo Product subset for the INTEX-B region V002. It contains the Stereoscopically Derived Cloud Mask (SDCM), cloud winds, and Reflecting Level Reference Altitude (RLRA), with associated data for the region covered by the INTEXB_2006 theme. MISR is designed to view Earth with cameras in 9 different directions. As the instrument flies overhead, all nine cameras successfully imaged each piece of Earth&amp;#39;s surface below in 4 wavelengths (blue, green, red, and near-infrared). MISR aims to improve our understanding of the effects of sunlight on Earth and distinguish different types of clouds, particles, and surfaces. Specifically, MISR monitors the monthly, seasonal, and long-term trends in three areas: 1) amount and type of atmospheric particles (aerosols), including those formed by natural sources and by human activities; 2) amounts, types, and heights of clouds, and 3) distribution of land surface cover, including vegetation canopy structure.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA ISLSCP II Project</title>
      <link>https://registry.opendata.aws/nasa-islscp-ii</link>
      <guid>https://registry.opendata.aws/nasa-islscp-ii</guid>
      <description>This data set contains the calculated net ocean-air carbon dioxide (CO2) flux and sea-air CO2 partial pressure (pCO2) difference. The estimates are based on approximately one million measurements made for the pCO2 in surface waters of the global ocean since the International Geophysical Year, 1956-1959. Only the ocean water pCO2 values measured using direct gas-seawater equilibration methods were used. The results represent the climatological distributions under non-El Nino conditions. Since the measurements were made in different years, during which the atmospheric pCO2 was increasing, they were corrected to a single reference year (arbitrarily chosen to be 1995) on the basis of the following assumptions: -Surface waters in subtropical gyres mix vertically at slow rates with subsurface waters due to the presence of strong stratification at the base of the mixed layer. This will allow a long contact time with the atmosphere to exchange CO2. Therefore, their CO2 chemistry tends to follow the atmospheric CO2 increase. Accordingly, the pCO2 measured in a given month and year is corrected to the same month of the reference year 1995 using changes in the atmospheric CO2 concentration occurred during this period. -Oceanic pCO2 measurements made after the beginning of 1979 have been corrected to 1995 using the atmospheric CO2 concentration data from the GLOBALVIEW-CO2 database (2000), in which the zonal mean atmospheric concentrations (for each 0.05 in sine of latitude) within the planetary boundary layer are summarized for each month since 1979 to 2000. -Pre-1979 oceanic pCO2 data were corrected to 1979 using the annual mean trend for the global mean atmospheric CO2 concentration constructed from the Mauna Loa data of Keeling and Whorf (2000), and then from 1979 to 1995 using the GLOBALVIEW-CO2 database. -Measurements for pCO2 made in the following areas have been corrected for the time of observation; 45 degrees N, 50 degrees S, in the Atlantic Ocean, north of 50 degrees S in the Indian Ocean, 40 degrees N, 50 degrees S in the western Pacific west of the date line, and 40 degrees N, 60 degrees S, in the eastern Pacific east of the date line.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atmos_co2_by_erosion_xdeg_1019&quot;&gt;atmos_co2_by_erosion_xdeg_1019&lt;/h4&gt;
The Continental Atmospheric CO2 Consumption data set represents gridded estimates for the riverine export of carbon and of sediments based on empirical models. All data exist for the overall continental area in a spatial resolution of 0.5 x 0.5 degree longitude/ latitude. The units are tC/km2/yr for all carbon species, and t/km2/yr for sediment fluxes. There are two data files (.zip) with this data set which describe the following: dissolved organic carbon (DOC) export, particulate organic carbon (POC) export, bicarbonate export, export of bicarbonate being of atmospheric origin (also called atmospheric CO2 consumption by rock weathering), and sediment export.
&lt;br&gt;&lt;h4 id&#x3D;&quot;avhrr_albedo_1995_xdeg_928&quot;&gt;avhrr_albedo_1995_xdeg_928&lt;/h4&gt;
This Albedo and BRDF (Bidirectional Reflectance Distribution Function) data set contains three files containing BRDF parameters, white- sky albedo and black-sky albedo at solar noon for three bands ((350-680nm, 680-3000nm, and 350-30000nm)derived from AVHRR (Advanced Very High Resolution Radiometer). These data are available at spatial resolutions of quarter, half, and one degree. Black-sky albedo (direct beam contribution) and white-sky (Completely diffuse contribution) can be linearly combined as a function of the fraction of diffuse skylight (itself a function of optical depth) to provide an actual or instantaneous albedo at local solar noon.
&lt;br&gt;&lt;h4 id&#x3D;&quot;c4_percent_1deg_932&quot;&gt;c4_percent_1deg_932&lt;/h4&gt;
The photosynthetic composition (C3 or C4) of vegetation on the land surface is essential for accurate simulations of biosphere-atmosphere exchanges of carbon, water, and energy. C3 and C4 plants have different responses to light, temperature, CO2, and nitrogen; they also differ in physiological functions like stomatal conductance and isotope fractionation. A fine-scale distribution of these plant types is essential for earth science modeling. The C4 percentage is determined from datasets that describe the continuous distribution of plant growth forms (i.e., the percent of a grid cell covered by herbaceous or woody vegetation), climate classifications, the fraction of a grid cell covered in croplands, and national crop type harvest area statistics. The staff from the International Satellite Land Surface Climatology Project (ISLSCP) Initiative II have made the original data set consistent with the ISLSCP-2 land/water mask. This data set contains a single file in ArcInfo ASCIIGRID format. This data set is one of the products of the International Satellite Land-Surface Climatology Project, Initiative II (ISLSCP II) data collection which contains 50 global time series data sets for the ten-year period 1986 to 1995. Selected data sets span even longer periods. ISLSCP II is a consistent collection of data sets that were compiled from existing data sources and algorithms, and were designed to satisfy the needs of modelers and investigators of the global carbon, water and energy cycle. The data were acquired from a number of U.S. and international agencies, universities, and institutions. The global data sets were mapped at consistent spatial (1, 0.5 and 0.25 degrees) and temporal (monthly, with meteorological data at finer (e.g., 3-hour)) resolutions and reformatted into a common ASCII format. The data and documentation have undergone two peer reviews. ISLSCP is one of several projects of Global Energy and Water Cycle Experiment (GEWEX) [&lt;a href&#x3D;&quot;http://www.gewex.org/%5D&quot;&gt;http://www.gewex.org/]&lt;/a&gt; and has the lead role in addressing land-atmosphere interactions -- process modeling, data retrieval algorithms, field experiment design and execution, and the development of global data sets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;co2_emissions_1deg_1021&quot;&gt;co2_emissions_1deg_1021&lt;/h4&gt;
This data set contains decadal (1950, 1960, 1970, 1980, 1990 and 1995) estimates of gridded fossil-fuel emissions, expressed in 1,000 metric tons C per year per one degree latitude by one degree longitude. The CO2 emissions are the summed emissions from fossil-fuel burning, hydraulic cement production and gas flaring. The years 1950 to 1990 were developed and compiled using somewhat different procedures and information than the 1995 data. The national annual estimates (Boden et al., 1996) from 1950 to 1990 were allocated to one degree grid cells based on gridded information on national boundaries and political units, and a 1984 gridded human population map (Andres et al., 1996). For the 1995 data, the population data base developed by Li (1996a) and documented by CDIAC (DB1016: Li, 1996b) was used as proxy to grid the 1995 emission estimates. There is one .zip data file with this data set at 1.0 degree spatial resolution.
&lt;br&gt;&lt;h4 id&#x3D;&quot;fluxnet_point_1029&quot;&gt;fluxnet_point_1029&lt;/h4&gt;
This International Satellite Land Surface Climatology Project (ISLSCP II) data set, ISLSCP II Carbon Dioxide Flux at Harvard Forest and Northern BOREAS Sites, contains gapp-filled flux and meterological data for half-hourly, daily, weekly, monthly, and annual time intervals presented for each site and year. The 1992-1995 Harvard Forest, MA site, and the 1994-95 Old Black Spruce, Alberta, Canada site are members of the FLUXNET global network of micrometeorological towers that use eddy covariance methods to measure the excahanges of carbon dioxide (CO2), water vapor, and energy between terrestrial ecosystem and atmosphere. There are 6 .zip files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cru_monthly_mean_xdeg_1015&quot;&gt;cru_monthly_mean_xdeg_1015&lt;/h4&gt;
This data set contains a mean monthly climatology for several climate variables averaged over the period from 1961 to 1990, and constructed from a data set of station 1961-1990 climatological normals, numbering between 19,800 (precipitation) and 3,615 (windspeed; see New et al, 1999 for details). The station data were interpolated as a function of latitude, longitude and elevation using thin-plate splines. The data comprise a suite of climate elements: precipitation, mean, maximum, and minimum temperature, frost frequency, diurnal temperature range, radiation, wet-day frequency, vapor pressure, wind, and cloud cover. There are 23 files in this data set provided at 0.5 and 1.0 degree spatial resolutions.
&lt;br&gt;&lt;h4 id&#x3D;&quot;srb_clouds_1deg_1073&quot;&gt;srb_clouds_1deg_1073&lt;/h4&gt;
This data set contains cloud and meteorology data on a 1.0 degree x 1.0 degree spatial resolution. There are eight data files (.zip) with this data set for several cloud parameters (monthly only) and meteorological parameters including monthly surface skin temperature, monthly total column ozone, and water vapor burdens for the period 1986-1995. All monthly parameters include files with a monthly mean value, a monthly standard deviation, and monthly minimum and maximum values.
&lt;br&gt;&lt;h4 id&#x3D;&quot;veg_continuous_fields_xdeg_931&quot;&gt;veg_continuous_fields_xdeg_931&lt;/h4&gt;
The objective of this study was to derive continuous fields of vegetation cover from multi-temporal Advanced Very High Resolution Radiometer (AVHRR) data using all available bands and derived Normalized Difference Vegetation Index (NDVI). The continuous fields describe sub-pixel proportions of cover for tree, herbaceous, bare ground and water cover types. For tree cover, additional fields describing leaf longevity (evergreen and deciduous) and leaf morphology (broadleaf and needleleaf) were also generated. The modeling of carbon dynamics and climate require knowing tree characteristics such as these. These products were resampled and aggregated to 0.25, 0.5 and 1.0 degree grids for the International Satellite Land Surface Climatology Project (ISLSCP) data initiative II. The data set describes the geographic distributions of three fundamental vegetation characteristics: tree, herbaceous and bare ground cover, plus a water layer. For tree cover, leaf longevity and morphology layers were produced. This data set is one of the products of the International Satellite Land-Surface Climatology Project, Initiative II (ISLSCP II) data collection which contains 50 global time series data sets for the ten-year period 1986 to 1995. Selected data sets span even longer periods. ISLSCP II is a consistent collection of data sets that were compiled from existing data sources and algorithms, and were designed to satisfy the needs of modelers and investigators of the global carbon, water and energy cycle. The data were acquired from a number of U.S. and international agencies, universities, and institutions. The global data sets were mapped at consistent spatial (1, 0.5 and 0.25 degrees) and temporal (monthly, with meteorological data at finer (e.g., 3-hour)) resolutions and reformatted into a common ASCII format. The data and documentation have undergone two peer reviews. ISLSCP is one of several projects of Global Energy and Water Cycle Experiment (GEWEX) [&lt;a href&#x3D;&quot;http://www.gewex.org/%5D&quot;&gt;http://www.gewex.org/]&lt;/a&gt; and has the lead role in addressing land-atmosphere interactions -- process modeling, data retrieval algorithms, field experiment design and execution, and the development of global data sets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cru_monthly_climate_xdeg_1014&quot;&gt;cru_monthly_climate_xdeg_1014&lt;/h4&gt;
This data set contains monthly climate time series data created by the Climatic Research Unit (CRU) at the University of East Anglia, U.K., for every year covering the period 1986 to 1995. This time series is a subset of a larger CRU monthly data set that covers the period of 1901 to 1996. The data comprise a suite of six climate elements: precipitation, mean temperature, diurnal temperature range, wet-day frequency, vapor pressure, and cloud cover. There are 13 files in this data set provided at 0.5 and 1.0 degree spatial resolutions.
&lt;br&gt;&lt;h4 id&#x3D;&quot;erbe_albedo_monthly_xdeg_957&quot;&gt;erbe_albedo_monthly_xdeg_957&lt;/h4&gt;
This data set, ISLSCP II Earth Radiation Budget Experiment (ERBE) Monthly Albedo, 1986-1990, contains both the original ERBE albedo data at 2.5 degree spatial resolution, and the International Land Surface Climatology Project Initative II (ISLSCP Initiative II) albedo product re-gridded to 1 degree resolution. The goals of the ERBE were (1) to understand the radiation balance between the Sun, Earth, atmosphere, and space and (2) to establish an accurate, long-term baseline data set for detection of climate changes. Earth Radiation Budget (ERB) data are fundamental to the development of realistic climate models and to the understanding of natural and anthropogenic perturbations of the climate system. As part of ERBE, measurements of broadband shortwave radiation reflected from the Earth-atmosphere system were obtained, from which top of atmosphere albedo values were calculated. In addition, values from scenes determined to be free of clouds were analyzed separately and clear-sky albedos were derived. For this study, only the clear-sky albedos are included. The ERBE data sets for ISLSCP Initiative II contain global, top of atmosphere, clear sky albedo data from January 1986 to February 1990.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecmwf_met_1deg_1222&quot;&gt;ecmwf_met_1deg_1222&lt;/h4&gt;
This data set for the ISLSCP Initiative II data collection provides meteorology data with fixed, monthly, monthly-6-hourly, 6-hourly, and 3-hourly temporal resolutions. The data were derived from the European Centre for Medium-range Weather Forecasts (ECMWF) near-surface meteorology data set, 40-year re-analysis, or ERA-40 (Simmons and Gibson, 2000), which covers the years 1957 to 2001. The data were processed onto the ISLSCP II Earth grid with a spatial resolution of 1-degree in both latitude and longitude, and span the common ISLSCP II period from 1986 to 1995. The ECMWF forecast system is called the Integrated Forecasting System (IFS) and was developed in co-operation with Meteo-France. For ERA40 it is used with 60 levels from the top of the model at 10 Pa to the lowest level at about 10 m above the surface. There are 46 compressed (.tar.gz) data files with this data set. Each uncompressed file contains space-delimited text (.asc) data files.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ecosystem_roots_1deg_929&quot;&gt;ecosystem_roots_1deg_929&lt;/h4&gt;
The goal of this study was to predict the global distribution of plant rooting depths based on data about global aboveground vegetation structure and climate. Vertical root distributions influence the fluxes of water, carbon, and soil nutrients and the distribution and activities of soil fauna. Roots transport nutrients and water upwards, but they are also pathways for carbon and nutrient transport into deeper soil layers and for deep water infiltration. Roots also affect the weathering rates of soil minerals. For calculating such processes on a global scale, data on vertical root distributions are needed as inputs to global biogeochemistry and vegetation models. In the Project for Intercomparison of Land Surface Parameterization Schemes (PILPS), rooting depth and vertical soil characteristics were the most important factors explaining scatter for simulated transpiration among 14 land-surface models. Recently, the Terrestrial Observation Panel for Climate of the Global Climate Observation System (GCOS) identified the 95% rooting depth as a key variable needed to quantify the interactions between the climate, soil, and plants, stating that the main challenge was to find the correlation between rooting depth and soil and climate features (GCOS/GTOS Terrestrial Observation Panel for Climate 1997). In response to this challenge, a data set of vertical rooting depths was collected from the literature in order to construct maps of global ecosystem rooting depths. The parameters included in these data sets are estimates for the soil depths containing 50% and 95% of all roots, termed 50% and 95% rooting depths (D50 and D95, respectively). Together, these variables can be used to calculate estimates for vertical root distributions, using a logistic equation provided in this documentation. The data represent mean ecosystem rooting depths for 1 by 1 degree grid cells. Related data sets:Â The ORNL DAAC offers related data sets by Jackson et al. (2003), Gordon and Jackson (2003), Schenk and Jackson (2003), and Gill and Jackson (2003). This data set is one of the products of the International Satellite Land-Surface Climatology Project, Initiative II (ISLSCP II) data collection which contains 50 global time series data sets for the ten-year period 1986 to 1995. Selected data sets span even longer periods. ISLSCP II is a consistent collection of data sets that were compiled from existing data sources and algorithms, and were designed to satisfy the needs of modelers and investigators of the global carbon, water and energy cycle. The data were acquired from a number of U.S. and international agencies, universities, and institutions. The global data sets were mapped at consistent spatial (1, 0.5 and 0.25 degrees) and temporal (monthly, with meteorological data at finer (e.g., 3-hour)) resolutions and reformatted into a common ASCII format. The data and documentation have undergone two peer reviews. ISLSCP is one of several projects of Global Energy and Water Cycle Experiment (GEWEX) [&lt;a href&#x3D;&quot;http://www.gewex.org/%5D&quot;&gt;http://www.gewex.org/]&lt;/a&gt; and has the lead role in addressing land-atmosphere interactions -- process modeling, data retrieval algorithms, field experiment design and execution, and the development of global data sets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;edgar_atmos_emissions_1deg_1022&quot;&gt;edgar_atmos_emissions_1deg_1022&lt;/h4&gt;
The EDGAR (Emission Database for Global Atmospheric Research) database project is a comprehensive task carried out jointly by the National Institute for Public Health (RIVM) and the Netherlands Organization for Applied Scientific Research (TNO) and stores global emission inventories of direct and indirect greenhouse gases from anthropogenic sources including halocarbons and aerosols both on a per country and region basis as well as on a grid (see &lt;a href&#x3D;&quot;http://www.rivm.nl/edgar/&quot;&gt;http://www.rivm.nl/edgar/&lt;/a&gt;). For the ISLSCP Initiative II data collection, gridded global annual anthropogenic emissions for the greenhouse gases CO2, CH4, N2O are provided on a 1.0 degree by 1.0 degree grid for the years 1970, 1980, 1990, and 1995 and for the tropospheric ozone precursor gases CO, NOx, NMVOC (Non-Methane Volatile Organic Compounds) and SO2 for the years 1990 and 1995. There are 2 .zip data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;fasir_biophys_monthly_xdeg_970&quot;&gt;fasir_biophys_monthly_xdeg_970&lt;/h4&gt;
The Fourier-Adjusted, Sensor and Solar zenith angle corrected, Interpolated, Reconstructed (FASIR) adjusted Normalized Difference Vegetation Index (NDVI) data set and derived biophysical parameter fields were generated to provide a 17-year, satellite record of monthly changes in the photosynthetic activity of terrestrial vegetation. This multiple resolution (1/4, 1/2 and 1 degree in latitude and longitude) biophysical parameter data set contains essential variables for the calculation of photosynthesis, and the energy and water exchange between the Earth&amp;#39;s surface (in particular of vegetation) and the lower boundary layer of the atmosphere. The Fraction of Absorbed Photosynthetically Active Radiation (FAPAR) is related to the light absorption and the photosynthetic capacity of vegetation. It also serves as an intermediate variable to calculate vegetation cover fraction (Vcover), total Leaf Area Index (LAI_T), green leaf area index (LAI_G), roughness length (z0), zero plane displacement (d), and snow-free albedo. The biophysical parameters were derived assuming one canopy layer. The production of the FASIR NDVI data set and its associated biophysical parameters was funded by NASA&amp;#39;s Land Surface Hydrology program and the Higher Education Funding Council for Wales (HEFCW) as a core component of the International Satellite Land Surface Climatology Project (ISLSCP) Initiative II Data Collection.
&lt;br&gt;&lt;h4 id&#x3D;&quot;fasir_ndvi_monthly_xdeg_972&quot;&gt;fasir_ndvi_monthly_xdeg_972&lt;/h4&gt;
The Fourier-Adjusted, Sensor and Solar zenith angle corrected, Interpolated, Reconstructed (FASIR) adjusted Normalized Difference Vegetation Index (NDVI) data sets were generated to provide a 17-year, satellite record of monthly changes in the photosynthetic activity of terrestrial vegetation. FASIR-NDVI data are also used in climate models and biogeochemical models to calculate photosynthesis, the exchange of CO2 between the atmosphere and the land surface, land-surface evapotranspiration and the absorption and release of energy by the land surface. There are three data files provided at spatial resolutions of 0.25, 0.5 and 1.0 degree in latitude and longitude. FASIR adjustments concentrated on reducing NDVI variations arising from atmospheric, calibration, view and illumination geometries and other effects not related to actual vegetation change. FASIR NDVI was also generated to provide inputs for computing a 17-year time series of associated biophysical parameters, provided as a separate data set in this data collection. The production of the FASIR NDVI data set and its associated biophysical parameters was funded by NASA&amp;#39;s Land Surface Hydrology program and the Higher Education Funding Council for Wales (HEFCW) as a core component of the International Satellite Land Surface Climatology Project (ISLSCP) Initiative II Data Collection.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gts_precip_daily_xdeg_1001&quot;&gt;gts_precip_daily_xdeg_1001&lt;/h4&gt;
The objective of this work was to construct a long-term data set of daily precipitation on half degree and one degree latitude/longitude grids over the global land areas. The analyses are defined by interpolating station observations from GTS (Global Telecommunications System) gauges using the algorithm of Shepard (1968). The algorithm of Shepard (1968) has been widely used to interpolate gauge observations of monthly, pentad, and daily precipitation (Rudolf 1993, Xie et al. 1996). This algorithm is used to interpolate the irregularly distributed station observations onto grid points. The weighting coefficients are inversely proportional to the gauge-grid point distance and are adjusted by a cosine function taking into account the directional isolation of each gauge relative to all other nearby gauges. There are 6 data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gimms_ndvi_monthly_xdeg_973&quot;&gt;gimms_ndvi_monthly_xdeg_973&lt;/h4&gt;
The Global Inventory Modelling and Mapping Studies (GIMMS) Normalized Difference Vegetation Index (NDVI) data sets were generated to provide a 22-year satellite record of monthly changes in terrestrial vegetation. This data set contains three data files provided at spatial resolutions of 0.25, 0.5 and 1.0 degree in latitude and longitude with data from July 1981 through December 2002. New features include reduced NDVI variations arising from calibration, view geometry, volcanic aerosols, and other effects not related to actual vegetation change. In particular, NOAA-9 descending node data from September 1994 to January 1995, volcanic stratospheric aerosol correction for 1982-1984 and 1991-1994, and improved NDVI using empirical mode decomposition/reconstruction (EMD) to minimize effects of orbital drift. Global NDVI was generated to provide inputs for computing the time series of biophysical parameters contained in the International Satellite Land Surface Climatology Project (ISLSCP) Initiative II collection. NDVI is used in climate models and biogeochemical models to calculate photosynthesis, the exchange of CO2 between the atmosphere and the land surface, land-surface evapotranspiration and the absorption and release of energy by the land surface.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gdp_xdeg_974&quot;&gt;gdp_xdeg_974&lt;/h4&gt;
The data sets in this directory were provided by Mr. Gregory Yetman and Drs. Stuart Gaffin and Deborah Balk from the Center for International Earth Science Information Network (CIESIN) at Columbia University. There are three data files at three spatial resolutions of 0.25, 0.5 and 1.0 degree in both latitude and longitude and for the reference year of 1990. Estimates of Gross Domestic Product (GDP) are commonly given for nations as a single aggregated number. This data set generates estimates of GDP density distributed subnationally to facilitate the integration of GDP with other data at a sub-national level and to promote interdisciplinary studies that include socioeconomic aspects. This is one of two coarse resolution Socioeconomic data sets included in the International Satellite Land Surface Climatology Project (ISLSCP) Initiative II data collection, the other being the Gridded Population of the World (GPW), also produced by CIESIN.
&lt;br&gt;&lt;h4 id&#x3D;&quot;islscp2_soils_1deg_1004&quot;&gt;islscp2_soils_1deg_1004&lt;/h4&gt;
This data set provides gridded data for selected soil parameters derived from data and methods developed by the Global Soil Data Task, an international collaborative project with the objective of making accurate and appropriate data relating to soil properties accessible to the global change research community. The task was coordinated by the International Geosphere-Biosphere Programme (IGBP-DIS). The data in this data set were produced by the International Satellite Land-Surface Climatology Project, Initiative II (ISLSCP II) staff from data obtained from the Oak Ridge National Laboratory Distributed Active Archive Center (ORNL DAAC, &lt;a href&#x3D;&quot;http://daac.ornl.gov/&quot;&gt;http://daac.ornl.gov/&lt;/a&gt;). See the related data sets section below. Two-dimensional gridded maps of selected soil parameters, including soil texture, at a 1.0 by 1.0 degree spatial resolution and for two soil depths are provided. All data layers have been adjusted to match the ISLSCP II land/water mask. There are 36 data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;global_population_xdeg_975&quot;&gt;global_population_xdeg_975&lt;/h4&gt;
Global Population of the World (GPW) translates census population data to a latitude-longitude grid so that population data may be used in cross-disciplinary studies. There are three data files with this data set for the reference years 1990 and 1995. Over 127,000 administrative units and population counts were collected and integrated from various sources to create the gridded data. In brief, GPW was created using the following steps: * Population data were estimated for the product reference years, 1990 and 1995, either by the data source or by interpolating or extrapolating the given estimates for other years. * Additional population estimates were created by adjusting the source population data to match UN national population estimates for the reference years. * Borders and coastlines of the spatial data were matched to the Digital Chart of the World where appropriate and lakes from the Digital Chart of the World were added. * The resulting data were then transformed into grids of UN-adjusted and unadjusted population counts for the reference years. * Grids containing the area of administrative boundary data in each cell (net of lakes) were created and used with the count grids to produce population densities. As with any global data set based on multiple data sources, the spatial and attribute precision of GPW is variable. The level of detail and accuracy, both in time and space, vary among the countries for which data were obtained.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpcc_precip_monthly_xdeg_995&quot;&gt;gpcc_precip_monthly_xdeg_995&lt;/h4&gt;
The Global Precipitation Climatology Centre (GPCC), which is operated by the Deutscher Wetterdienst (National Meteorological Service of Germany), is a component of the Global Precipitation Climatology Project (GPCP) with the main emphasis on the treatment of the global in-situ observations. The GPCC simultaneously contributes to the Global Climate Observing System (GCOS) and other international research and climate monitoring projects. This rain gauge-only data set was acquired from GPCC and resampled to 0.5 degree grid boxes for use in the International Satellite Land Surface Climatology Project (ISLSCP) Initiative II. The GPCC collects precipitation data which are locally observed at rain gauge stations and distributed as CLIMAT and SYNOP reports via the Global Telecommunication System of the World Weather Watch (GTS) of the World Meteorological Organization (WMO). The Centre acquires additional monthly precipitation data from meteorological and hydrological networks which are operated by national services.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpcp_precip_pentad_xdeg_1002&quot;&gt;gpcp_precip_pentad_xdeg_1002&lt;/h4&gt;
The Global Precipitation Climatology Project (GPCP) pentad version 1 precipitation data set includes global precipitation rates for 5-day, or pentad, periods. The data sets are derived from measured rain gauge data and merged with satellite estimates of rainfall. This is a portion of the version 1 GPCP pentad data set and covers the ISLSCP II period from 1986 to 1995. The original precipitation rates at 2.5 degrees were re-gridded to a 1 degree spatial resolution by the ISLSCP II staff.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gpcp_precip_monthly_xdeg_1003&quot;&gt;gpcp_precip_monthly_xdeg_1003&lt;/h4&gt;
The Global Precipitation Climatology Project (GPCP) Version 2 data set includes global, monthly precipitation rates and associated random errors (RMSE), and a monthly precipitation climatology derived as an average from all GPCP data sets from January 1979 to December 1999. The data are derived from measured gauge data and merged with satellite estimates of rainfall. This is a portion of the version 2 GPCP data and covers the ISLSCP II period from 1986 to 1995. There are six data files included with this data set: the original precipitation rates, errors and climatology at 2.5 degrees spatial resolution, and the same data re-gridded to a 1 degree spatial resolution by the ISLSCP II staff.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gppdi_npp_gridded_xdeg_1023&quot;&gt;gppdi_npp_gridded_xdeg_1023&lt;/h4&gt;
Net Primary Production (NPP) is an important component of the carbon cycle and, among the pools and fluxes that make up the cycle, it is one of the steps that are most accessible to field measurement. Direct measurement of NPP is not practical for large areas and so models are generally used to study the carbon cycle at a global scale. This data set contains 2 .zip files for above ground and total NPP data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;river_carbon_flux_xdeg_1028&quot;&gt;river_carbon_flux_xdeg_1028&lt;/h4&gt;
The River Carbon Flux data set represents estimates for the riverine export of carbon and of sediments. This data set includes the amounts of carbon and of sediments that are discharged to the oceans by rivers for each coastal grid point which receives river inputs. This data set contains three compressed (.zip) files: the original data at 2.5 x 2.0 degrees, and global maps at spatial resolutions of 0.5 and 1.0 degree which the ISLSCP II staff has created from the original data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sea_ice_extent_xdeg_981&quot;&gt;sea_ice_extent_xdeg_981&lt;/h4&gt;
This International Satellite Land Surface Climatology Project (ISLSCP) Initiative II data set, ISLSCP II Global Sea Ice Concentration, is based on the Goddard Space Flight Center (GSFC) Sea Ice Concentrations from Nimbus-7 Scanning Multichannel Microwave Radiometer (SMMR) and the Defense Meteorological Satellites Program (DMSP) Special Sensor Microwave/Imager (SSM/I) Passive Microwave Data. This data set contains four zip files which includes sea ice concentration (in percentage of ocean area covered by sea ice), table data and map data. These original data were re-gridded by the National Snow and Ice Data Center (NSIDC) from their original 25-km spatial resolution and EASE-Grid into equal angle Earth grids with quarter, half and one degree spatial resolutions in latitude/longitude. The ISLSCP II staff have taken the one degree resolution original data provided by the Principal Investigator and created global maps of monthly sea ice concentration on a global one degree grid using the latitude and longitude coordinates that were provided. Individual monthly files were created and written to the ASCII format. The re-gridded one degree original data were also adjusted to match the one degree ISLSCP II land/water mask.
&lt;br&gt;&lt;h4 id&#x3D;&quot;globalview_co2_point_1111&quot;&gt;globalview_co2_point_1111&lt;/h4&gt;
The GlobalView Carbon Dioxide (CO2) data product contains synchronized and smoothed time series of atmospheric CO2 concentrations at selected sites that were created using the data extension and integration techniques described by Masarie and Tans, (1995). The information needed to derive this time series is also in this data set, along with extensive documentation. The longest period of coverage is from 1979 to 2001 with some sites having longer or shorter temporal coverage. Note that the GlobalView CO2 data products are derived from measurements but contain no actual data. To facilitate heterogeneous CO2 data use in carbon cycle modeling studies, the measurements have been processed (smoothed, interpolated, and extrapolated) resulting in extended records that are evenly incremented in time. There are 92 files with this data set which includes 89 .zip data files. The other three files include 2 files with site information, one comma-delimited ASCII file (.csv), and one .dat file, and one .dat file which is a single reference marine boundary layer matrix file which contains CO2 mixing ratios as a function of time and sine of latitude and is a by-product of the data extension procedure.
&lt;br&gt;&lt;h4 id&#x3D;&quot;globalview_ch4_point_1109&quot;&gt;globalview_ch4_point_1109&lt;/h4&gt;
The GlobalView Methane (CH4) data product contains synchronized and smoothed time series of atmospheric CH4 concentrations at selected sites that were created using the data extension and integration techniques described by Masarie and Tans (1995). The information needed to derive this time series is also in this data set, along with extensive documentation. The longest period of coverage is from 1984 to 1998 with some sites having shorter or longer temporal coverage. Note that the GlobalView-CH4 data products are derived from measurements but contain no actual data. To facilitate heterogeneous CH4 data use in carbon cycle modeling studies, the measurements have been processed (smoothed, interpolated, and extrapolated) resulting in extended records that are evenly incremented in time. There are 74 files with this data set which includes 71 .zip data files. The other three files include 2 files with site information, one comma-delimited ASCII file (.csv), and one .dat file, and one .dat file which is a single reference marine boundary layer matrix file containing CH4 mixing ratios as a function of time and sine of latitude and is a by-product of the data extension procedure.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gppdi_npp_point_1033&quot;&gt;gppdi_npp_point_1033&lt;/h4&gt;
The Global Primary Production Data Initiative (GPPDI) was set up as a Focus 1 activity of the IGBP Data and Information System, a coordinated international program to improve worldwide estimates of terrestrial net primary productivity (NPP) for parameterization, calibration, and validation of NPP models at various scales. The GPPDI data collection contains documented field measurements of NPP for global terrestrial sites compiled from published literature and other extant data sources. The point measurements of NPP were categorized as either Class A, representing intensively studied or well-documented study sites (e.g., with site-specific climate, soils information, etc.), Class B, representing more numerous “extensive” sites with less documentation and site-specific information available, or Class C, representing regional collections of half-degree latitude-longitude grid cells. This data set in the ISLSCP II collection represents the GPPDI Class B NPP data. The Class B NPP data file contains biomass dynamics, climate, and site-characteristics data georeferenced to each site. There is one ASCII data file with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;historic_cropland_xdeg_966&quot;&gt;historic_cropland_xdeg_966&lt;/h4&gt;
The Historical Croplands Cover data set was developed to understand the consequences of historical changes in land use and land cover for ecosystem goods and services. In particular, this data set can be used to study how global changes in cultivated area has influenced climate, biogeochemical cycles, biodiversity, etc. This data set can be used directly within spatially-explicit climate and biogeochemical models. This is a gridded data set describing the fraction of each grid cell in the globe that is occupied by cultivated land from 1700 to 1992. Data layers are provided for every 50 years from 1700 to 1850, every 10 years from 1850 to 1980, and every year from 1986 to 1992. There are two sources of global land cover/land use data. The most recent estimates are derived from satellite measurements, and are available in a spatially-explicit fashion for roughly the last 30 years. The other estimate is based on ground-based sources such as census statistics, land surveys, estimates by historical geographers, etc. These land inventory data are only available at the scale of political units, but have the advantage of being historical. Ramankutty and Foley (1998) derived a spatially-explicit data set of croplands in 1992 by synthesizing remotely-sensed land cover data with contemporary land inventory data. Furthermore, Ramankutty and Foley (1999) extended this data set into the past (back to 1700) using historical land inventory data. The data set should only be used for continental-to-global scale analysis and modeling. The data set captures the broad patterns of cropland change over history, but not necessarily the fine details at local to regional scales - please check the data quality before using it at fine spatial scales. The quality of historical data for the Russian Federation is poor. The quality of data prior to 1850 is poor -- only continental-scale historical data were used for that period.
&lt;br&gt;&lt;h4 id&#x3D;&quot;historic_landcover_xdeg_967&quot;&gt;historic_landcover_xdeg_967&lt;/h4&gt;
The Historical Land Cover and Land Use data set was developed to provide the global change community with historical land use estimates. The data set describes historical land use changes over a 300-year historical period (1700-1990). Testing against historical data is an important step for validating integrated models of global environmental change. Owing to long time lags in the climate and biogeochemical systems, these models should aim to simulate the land use dynamics for long periods, i.e., spanning decades to centuries. Developing such models requires an understanding of past and current trends and is therefore strongly data dependent. For this purpose, a historical database of the global environment has been developed: HYDE. Historical statistical inventories on agricultural land (census data, tax records, land surveys, etc) and different spatial analysis techniques were used to create a geographically-explicit data set of land use change, with a regular time interval. The data set can be used to test integrated models of global change. Continental-scale historical data were used for that period.
&lt;br&gt;&lt;h4 id&#x3D;&quot;hydro1k_elevation_xdeg_1007&quot;&gt;hydro1k_elevation_xdeg_1007&lt;/h4&gt;
This data set contains coarse scale elevation and elevation-based parameters at 1.0 and 0.5-degree spatial resolutions that were developed to support a wide variety of global modeling activities through the International Satellite Land Surface Climatology Project (ISLSCP) Initiative II data collection. These coarse scale data have sufficient statistical information (up to fourth moment) to allow a good statistical description of the sub-cell distribution of any particular elevation parameter (i.e. elevation, slope and aspect). The database used in the development effort was the HYDRO1k product (&lt;a href&#x3D;&quot;http://eros.usgs.gov/#/Find_Data/Products_and_Data_Available/HYDRO1K&quot;&gt;http://eros.usgs.gov/#/Find_Data/Products_and_Data_Available/HYDRO1K&lt;/a&gt;) with a native spatial resolution of 1 km, the highest resolution database of global coverage of standard elevation-based derivatives (slope, aspect, elevation, compound topographic index, etc.).
&lt;br&gt;&lt;h4 id&#x3D;&quot;edc_landcover_xdeg_930&quot;&gt;edc_landcover_xdeg_930&lt;/h4&gt;
This data set describes the geographic distributions of 17 classes of land cover based on the International Geosphere-Biosphere DISCover land cover legend (Loveland and Belward 1997) and the 15 classes of the SiB model processed at the USGS EROS Data Center (EDC). Specifically, the resampled DISCover datasets were derived from the 1km DISCover data set compiled by the USGS. The 1km data sets for each classification scheme were aggregated to 1, 0.5 and 0.25 degree spatial resolutions for this ISLSCP II data collection. Each layer of the aggregated products corresponds to a single DISCover land cover category and the values represent the percentage of the coarse resolution cell (1 degree, etcâï¿½¦) occupied by that land cover category. The dominant class data show the land cover category that occupies the majority of the cell and is derived from the percentage files for each cover type. The objective of this study was to create a land cover map derived from 1 kilometer AVHRR data using a full year of data (April 1992-March 1993). This thematic map was resampled to 0.25, 0.5 and 1.0 degree grids for the International Satellite Land Surface Climatology Project (ISLSCP) data initiative II. During this re-processing, the original EDC land cover type and fraction maps were adjusted to match the water/land fraction of the ISLSCP II land/water mask. These maps were generated for use by global modelers and others. This data set is one of the products of the International Satellite Land-Surface Climatology Project, Initiative II (ISLSCP II) data collection which contains 50 global time series data sets for the ten-year period 1986 to 1995. Selected data sets span even longer periods. ISLSCP II is a consistent collection of data sets that were compiled from existing data sources and algorithms, and were designed to satisfy the needs of modelers and investigators of the global carbon, water and energy cycle. The data were acquired from a number of U.S. and international agencies, universities, and institutions. The global data sets were mapped at consistent spatial (1, 0.5 and 0.25 degrees) and temporal (monthly, with meteorological data at finer (e.g., 3-hour)) resolutions and reformatted into a common ASCII format. The data and documentation have undergone two peer reviews. ISLSCP is one of several projects of Global Energy and Water Cycle Experiment (GEWEX) [&lt;a href&#x3D;&quot;http://www.gewex.org/%5D&quot;&gt;http://www.gewex.org/]&lt;/a&gt; and has the lead role in addressing land-atmosphere interactions -- process modeling, data retrieval algorithms, field experiment design and execution, and the development of global data sets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;model_npp_xdeg_1027&quot;&gt;model_npp_xdeg_1027&lt;/h4&gt;
This data set contains modeled annual net primary production (NPP) for the land biosphere from seventeen different global models. Annual NPP is defined as the net difference of annual carbon uptake (grams CO2/m2/yr) from the atmosphere through photosynthesis by the land vegetation and that lost back to the atmosphere through autotrophic and maintenance respiration. NPP is also related to the Net Ecosystem Exchange (NEE) of carbon accumulated by or lost from the surface by its vegetation and soils. NPP is NEE plus heterotrophic (decomposition) respiration of the vegetation and soils. Only NPP values are included in this data set as some models did not estimate NEE. Data for the mean, standard deviation and coefficient of variation of NPP for the 17 models are provided at spatial resolutions of 1.0 degree and 0.5 degrees. There are two compressed (.zip) data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;combined_ancillary_xdeg_1200&quot;&gt;combined_ancillary_xdeg_1200&lt;/h4&gt;
This data set contains the ISLSCP II fixed land/water masks and percentages of land or water in each cell. There are seven zip data files: four produced from a 1-km land/water mask compiled at the Jet Propulsion Laboratory (JPL) in support of NASA&amp;#39;s Earth Observing System; two files of a land outline overlay created from the land/water mask files created at NASA&amp;#39;s Goddard Space Flight Center; and one file which is a latitude grid coordinate file and longitude grid coordinate file produced by the ISLSCP II staff. All of these data are provided at three spatial resolutions of .25, 0.5 and 1-degree in latitude and longitude and on a common Earth grid.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ornl_lai_point_971&quot;&gt;ornl_lai_point_971&lt;/h4&gt;
Leaf Area Index (LAI) data from the scientific literature, covering the period from 1932-2000, have been compiled at the Oak Ridge National Laboratory (ORNL) Distributed Active Archive Center (DAAC) to support model development and validation for products from the MODerate Resolution Imaging Spectroradiometer (MODIS) instrument. There is one data file which consists of a spreadsheet table, together with a bibliography of more than 300 original-source references. Although the majority of measurements are from natural or semi-natural ecosystems, some LAI values have been included from crops (limited to a sub-set representing different crops at different stages of development under a range of treatments). Like Net Primary Productivity (NPP), Leaf Area Index (LAI) is a key parameter for global and regional models of biosphere/atmosphere exchange. Modeling and validation of coarse scale satellite measurements both require field measurements to constrain LAI values for different biomes (typical minimum, maximum values, phenology, etc.). Maximum values for point measurements are unlikely to be approached or exceeded by area-weighted LAI, which is what satellites and true spatial models are measuring or modeling.
&lt;br&gt;&lt;h4 id&#x3D;&quot;modis_albedo_2002_xdeg_958&quot;&gt;modis_albedo_2002_xdeg_958&lt;/h4&gt;
This International Satellite Land Surface Climatology Project (ISLSCP II) MODerate resolution Image Spectroradiometer (MODIS) dataset, ISLSCP II MODIS (Collection 4) Albedo 2002, provides albedo data for the period January 2002 through December 2002.The MODIS bidirectional reflectance distribution function (BRDF) albedo product (MOD43B) provides measures of clear sky surface albedo every 16 days. Both white-sky albedo (bihemispherical reflectance) and black-sky albedo (directional hemispherical reflectance) at local solar noon are provided for 7 spectral bands and 3 broadbands. Since black-sky albedo represents the direct beam contribution while white-sky represents the completely diffuse contribution, these measures can be linearly combined as a function of the fraction of diffuse skylight (itself a function of optical depth) to provide an actual or instantaneous albedo at local solar noon.
&lt;br&gt;&lt;h4 id&#x3D;&quot;modis_landcover_xdeg_968&quot;&gt;modis_landcover_xdeg_968&lt;/h4&gt;
This data set, ISLSCP II MODIS (Collection 4) IGBP Land Cover, 2000-2001, contains global land cover classifications (dominant type, classification confidence and fractional cover) generated using a full year of MODerate Resolution Imaging Spectroradiometer (MODIS) data covering the period from October 2000 to October 2001. The objective of the MODIS Land Cover Product is to provide a suite of land cover types useful to global system science modelers by exploiting the information content of MODIS data in the spectral, temporal, spatial, and directional domains. These products describe the geographic distribution of the 17 land cover classification scheme proposed by the International Geosphere-Biosphere Programme (IGBP).
&lt;br&gt;&lt;h4 id&#x3D;&quot;snowfree_albedo_1deg_956&quot;&gt;snowfree_albedo_1deg_956&lt;/h4&gt;
This data set contains monthly average snow-free surface shortwave albedo calculated for the period 1982-1998 and estimates of background soil/litter reflectances in the visible (0.4-0.7 Î¼m) and near-infrared (NIR) (0.7-1.0 Î¼m) wavelengths. Biophysical Parameters derived from the FASIR-NDVI (Fourier Adjusted, Solar zenith angle correction, Interpolation, and Reconstruction of Normalized Difference Vegetation Index) data set developed for the ISLSCP Initiative II data collection for the months of January 1982 through December 1998 were used to calculate monthly mean surface albedos at 1 X 1 degree spatial resolution for vegetated land surfaces (Sellers et al, 1996b) for the wavelength interval from 0.4 to 3.0 Âµm. The instantaneous albedo is a function of the properties of the land surface and the solar zenith angle. The monthly mean albedo is an average weighted over time weighted by the incident radiation. NDVI data are used to generate the biophysical parameters leaf area index (LAI) and green fraction of vegetation (Greenness) used by the canopy radiative transfer model of the Simple Biosphere (SiB2) model (Sellers et al, 1996a), which computes the instantaneous albedo. This is coupled to the Colorado State University (CSU) General Circulation Model (GCM) (Randall et al, 1989) which integrates the SiB2 radiative transfer through time. The incident radiation for weighting the time-averaged albedo was provided by a previous run of the GCM using the atmospheric radiation parameterization of Harshvardhan et al (1987). The Harshvardhan parameterization models radiative transfer through the atmosphere in both the longwave and shortwave bands, including the effects of cloudiness and water vapor, carbon dioxide and ozone. The shortwave radiation distinguishes between the direct and diffuse components of the solar beam.
&lt;br&gt;&lt;h4 id&#x3D;&quot;noaa_albedo_5year-av_xdeg_959&quot;&gt;noaa_albedo_5year-av_xdeg_959&lt;/h4&gt;
The objective of this work was to produce a monthly climatology of broadband surface albedos for use in global numerical weather prediction models at the National Centers for Environmental Prediction (NCEP). Monthly means of clear-sky, surface, broadband, snow-free albedos for overhead sun illumination angle were determined using data from a five-year period from April 1985-December 1987 and January 1989-March 1991. The data set is compatible in temporal coverage and spatial resolution with a monthly climatology of green vegetation fraction (Gutman and Ignatov, 1998) delivered earlier and currently in use at NCEP. Files showing the differences between the original data set and the Land/water mask used in the International Satellite land Surface Climatology Project (ISLSCP) Initiative II are also provided.
&lt;br&gt;&lt;h4 id&#x3D;&quot;snow_cover_xdeg_982&quot;&gt;snow_cover_xdeg_982&lt;/h4&gt;
This ISLSCP data set is derived from the National Snow and Ice Data Center (NSIDC) Northern Hemisphere EASE-Grid Weekly Snow Cover and Sea Ice Extent product which combines snow cover and sea ice extent at weekly intervals for October 1978 through June 2001, and snow cover alone from 1966 through June 2001. The original data set was the first representation of combined snow and sea ice measurements derived from satellite observations for the period of record. Designed to facilitate study of Northern Hemisphere seasonal fluctuations of snow cover and sea ice extent, the original NSIDC data set also includes monthly climatologies describing average extent, probability of occurrence, and variance. This data set shows the extent of snow on the land at a variety of scales (1.0 degree, 0.5 degree, 0.25 degree). The values represent the percentage of days in each month where snow was present -- 100 means 100% of the month, 80 means 80% of the month, etc. There are 4 .zip files provided. Missing data is represented by -99 for water and -88 for land. The data were originally in a yearly tabular format. The file was converted to multi-scale maps by plotting each point in the tabular data onto a map of -99 (water) and -88 (land) created from the standard ISLSCP II Land/Sea Mask.
&lt;br&gt;&lt;h4 id&#x3D;&quot;potential_veg_xdeg_961&quot;&gt;potential_veg_xdeg_961&lt;/h4&gt;
This data set was developed to describe the state of the global land cover in terms of 15 major vegetation types, plus water, before alteration by humans. It forms a complement to the historical croplands data set developed by Ramankutty and Foley (1999). By overlaying the two, one can determine the extent to which natural vegetation has been cleared for cultivation. This data set can be used directly within spatially-explicit climate and biogeochemical models. There are four total files in this data set. Two files contain the land cover types representing potential natural vegetation before human alteration, and two other files contain those points in the original data set submitted by the Principal Investigator that have been modified in order to match the land/water mask of the ISLSCP Initiative II. The geographic distribution of contemporary land cover types can be derived from remotely-sensed data. However, humans now dominate much of the world and there is little evidence of the pre-human-settlement natural vegetation or Potential Natural Vegetation (PNV). PNV, as defined here, does not necessarily represent the world&amp;#39;??s natural pre-human-disturbance vegetation. Rather, our definition of PNV represents the world&amp;#39;s vegetation cover that would most likely exist now in equilibrium with present-day climate and natural disturbance, in the absence of human activities.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ncep_met_1deg_1226&quot;&gt;ncep_met_1deg_1226&lt;/h4&gt;
This data set for the ISLSCP Initiative II data collection provides near surface meteorological variables, fluxes of heat, moisture and momentum at the surface, and land surface state variables, all with a spatial resolution of 1 degree in both latitude and longitude. There are four temporal categories of data: time invariant and monthly mean annual cycle fields (together referred to as &amp;quot;fixed&amp;quot; fields), monthly mean fields, monthly 3-hourly diurnal, and 3-hourly fields. Two types of variables exist in this data; instantaneous fields (primarily state variables), and average fields (primarily flux fields expressed as a rate). The Center for Ocean-Land Atmosphere Studies (COLA) near-surface data set for ISLSCP II was derived from the National Centers for Environmental Prediction (NCEP)/Department of Energy (DOE) Atmospheric Model Inter-comparison Project (AMIP-II) reanalysis (&lt;a href&#x3D;&quot;http://www.cpc.ncep.noaa.gov/products/wesley/reanalysis2/&quot;&gt;http://www.cpc.ncep.noaa.gov/products/wesley/reanalysis2/&lt;/a&gt;), covering the years from 1979-2003. The data set for ISLSCP II covers the period from 1986 to 1995. The purpose of the reanalysis was to provide an improved version of the original NCEP/National Center for Atmospheric Research (NCAR) reanalysis for General Circulation Model (GCM) validation. To co-register the NCEP/DOE reanalysis on the ISLSCP 1-degree grid, the reanalysis data set was regridded from its native T62 Gaussian grid) resolution (192 x 94 grid boxes globally) to 1-degree ISLSCP II required resolution. There are 136 compressed (.tar.gz) data files with this data set. When extrapolated, the individual data files are in ASCII (.asc) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;river_routing_stn_xdeg_1005&quot;&gt;river_routing_stn_xdeg_1005&lt;/h4&gt;
The Simulated Topological Network (STN-30p) data set provides the large-scale hydrological modeling community an accurate representation of the global river system at 0.5 degree and 1.0 degree spatial resolutions. STN-30p represents the potential connectivity of the continental land mass by assigning one of eight (E, SE, S, SW, W, NW, N, NE) possible flow directions to each continental grid cell (Jenson 1988, Band 1993). The potentiality of STN-30p reflects the fact that flow direction is assigned to every land cell regardless of the existence of actively flowing rivers. STN-30p can be viewed as a river network which would exist if sufficient surface runoff was available to form river channels everywhere. There are two data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sea_surface_temp_1deg_980&quot;&gt;sea_surface_temp_1deg_980&lt;/h4&gt;
Sea surface temperature (SST) is an important indicator of the state of the earth climate system as well as a key variable in the coupling between the atmosphere and the ocean. Accurate knowledge of SST is essential for climate monitoring, prediction and research. It is also a key surface boundary condition for numerical weather prediction and for other atmospheric simulations using atmospheric general circulation models and regional models. SST also is important in gas exchange between the ocean and atmosphere, including the air-sea flux of carbon. Gridded SST products have been developed to satisfy these needs. There are 3 .zip files provided with this data set. Gridded monthly and weekly sea surface temperature (SST) and long term SST monthly climatology for the period 1971-2000 are provided here. Weekly normalized error variance fields are also provided with the weekly data. The data are derived using the National Oceanic and Atmospheric Administration (NOAA) Optimum Interpolation (OI) global sea surface temperature analyses that use seven days of in situ (ship and buoy) and satellite SST observations and SST values derived from sea ice concentration. These analyses are produced weekly using optimum interpolation (OI) on a 1-degree grid. The data sets included in the ISLSCP II data collection are produced using version 2 of the OI analyses, called OIv2. In this data set, the ISLSCP II staff have masked land areas based on the ISLSCP II land/water mask. A file describing the differences between the ISLSCP II mask and the original mask used is provided.
&lt;br&gt;&lt;h4 id&#x3D;&quot;modis_albedo_2002_filled_xdeg_960&quot;&gt;modis_albedo_2002_filled_xdeg_960&lt;/h4&gt;
This data set, ISLSCP II Snow-Free, Spatially Complete, 16 Day Albedo, 2002, contains 9 files for snow-free, spatially complete 16-day global black-sky albedos at local solar noon, white-sky albedos and quality information based on MODerate Resolution Imaging Spectroradiometer (MODIS) Collection 4 Albedo Products (MOD43B3). Data are provided for 7 spectral bands and 3 broad bands for a full year of MODIS data (2002). An ecosystem-dependent temporal interpolation technique was developed to fill any missing or seasonally snow-covered data in the official MOD43B3 albedo product. The resulting data set maintains the original resolution and data of the MOD43B3 product while replacing fill values to provide snow-free spatially complete maps.
&lt;br&gt;&lt;h4 id&#x3D;&quot;srb_radiation_1deg_1201&quot;&gt;srb_radiation_1deg_1201&lt;/h4&gt;
This data set contains global Surface Radiation Budget (SRB) and a few top-of-atmosphere (TOA) radiation budget parameters on a 1-degree x 1-degree spatial resolution. These parameters are provided as monthly, monthly-3 hourly (i.e. monthly average for a particular 3 hourly period) and 3-hourly averages. All monthly parameters include files with a monthly mean value, a monthly standard deviation, and monthly minimum and maximum values. The surface and TOA Shortwave (SW) radiative parameters were computed with the Pinker and Laszlo (1992) radiation model. The Longwave (LW) SRB parameters were derived with the Gupta et al. (1992) model. Meteorological inputs for all processing were taken from the Goddard Earth Observing System version 1 (GEOS-1) reanalysis data sets (Schubert et al., 1993) from the Data Assimilation Office (DAO), at NASA Goddard Space Flight Center (GSFC). Required cloud parameters were derived at NASA Langley Research Center (LaRC) from International Satellite Cloud Climatology Project (ISCCP) DX data using the algorithms developed at the NASA Goddard Institute for Space Studies (GISS) (Rossow et al., 1996). Surface albedos are derived internally in the Pinker and Laszlo SW model. There are 30 compressed data files (.zip) with this data set. When the .zip files are expanded, there are 114,912 3-hourly files, 42,064 diurnal files, and 6,254 monthly files.
&lt;br&gt;&lt;h4 id&#x3D;&quot;root_water_storage_1deg_1006&quot;&gt;root_water_storage_1deg_1006&lt;/h4&gt;
This data set provides two estimates of the geographic distribution of the total plant-available soil water storage capacity of the rooting zone (&amp;quot;rooting zone water storage size&amp;quot;) on a 1.0 degree global grid. Two inverse modeling methods were used. The first modeling approach (optimization) was based on the assumption that vegetation has adapted to the environment such that it makes optimum use of water (Kleidon and Heimann 1998). The second method (assimilation) was based on the assumption that green vegetation indicates sufficient available water for transpiration (Knorr 1997). The data set was developed to provide alternative means to describe rooting characteristics of the global vegetation cover for land surface and climate models in support of the ISLSCP Initiative II data collection. There are three files in this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;comp_runoff_monthly_xdeg_994&quot;&gt;comp_runoff_monthly_xdeg_994&lt;/h4&gt;
The University of New Hampshire (UNH)/Global Runoff Data Centre (GRDC) composite runoff data combines simulated water balance model runoff estimates derived from climate forcing with monitored river discharge. It can be viewed as a data assimilation applied in a water balance model context (conceptually similar to the commonly used 4DDA techniques used in meteorological modeling). Such a data assimilation scheme preserves the spatial specificity of the water balance calculations while constrained by the more accurate discharge measurement. There are 11 data files in this data set and 1 changemap file which shows the differences between the ISLSCP II land/water mask and the original data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;umd_landcover_xdeg_969&quot;&gt;umd_landcover_xdeg_969&lt;/h4&gt;
The objective of the International Satellite Land Surface Climatology Project (ISLSCP II) study that produced this data set, ISLSCP II University of Maryland Global Land Cover Classifications 1992-1993, was to create a land cover map derived from 1 kilometer Advanced Very High Resolution Radiometer (AVHRR) data using all available bands, derived Normalized Difference Vegetation Index (NDVI), and a full year of data (April 1992-March 1993). This thematic map was resampled to 0.25, 0.5 and 1.0 degree grids. During this re-processing, the original University of Maryland (UMD) land cover type and fraction maps were adjusted to match the water/land fraction of the ISLSCP II land/water mask. These maps were generated for use by modelers of global biogeochemical cycles and others in need of an internally consistent, global depiction of land cover. This 1km map was also one of the MODerate resolution Imaging Spectroradiometer (MODIS) at-launch land cover maps. This product describes the geographic distributions of 13 classes of vegetation cover (plus water and unclassified classes) based on a modified International Geosphere-Biosphere Programme (IGBP) legend. The data set also provides the fraction of each of the 15 classes within the coarser resolution cells, at three spatial resolutions of 0.25, 0.5 and 1.0 degrees in latitude and longitude.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.ornldaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA ISS_RapidScat Project</title>
      <link>https://registry.opendata.aws/nasa-iss-rapidscat</link>
      <guid>https://registry.opendata.aws/nasa-iss-rapidscat</guid>
      <description>This dataset contains the ISS-RapidScat Version 2.0 Level 1B geo-located Sigma-0 measurements and antenna pulse &amp;quot;egg&amp;quot; and &amp;quot;slice&amp;quot; geometries as derived from ephemeris and the Level 1A dataset. The pulse &amp;quot;egg&amp;quot; represents the complete footprint of the pulse, which has a spatial geometry of approximately 25 km by 35 km. There are 8 slices that constitute the range-binned components of a pulse each of which has a spatial geometry of approximately 25 km by 7 km. The orientation of the long dimension of the slices varies with the rotation of the antenna and thus does not align with the along/across track orientation of the wind vector grid in the L2B/L2A products. Version 2.0 represents a complete historical re-processing of the L1B data record and provides a calibration which is consistent across the several signal to noise ratio states experienced by RapidScat throughout its operation period (see the technical note for Version 2.0 under Documentation). The Version 2.0 is also the dataset used to derive the Version 2.0 wind products (L2B). Data are provided in single-orbit files in HDF-4 format. This dataset is intended for expert use only. If you must use RapidScat Sigma-0 data but you are unsure about how to use the L1B data record, please consider using either of the following L2A datasets: 1) &lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/RSCAT_L2A_25KM_V2.0&quot;&gt;https://podaac.jpl.nasa.gov/dataset/RSCAT_L2A_25KM_V2.0&lt;/a&gt; or 2) &lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/dataset/RSCAT_L2A_12KM_V2.0&quot;&gt;https://podaac.jpl.nasa.gov/dataset/RSCAT_L2A_12KM_V2.0&lt;/a&gt;. RapidScat is a Ku-band dual beam circular rotating scatterometer retaining much of the same hardware and functionality of QuikSCAT, with exception of the antenna sub-system and digital interface to the ISS Columbus module, which is where RapidScat is mounted. The NASA mission is officially referred to as ISS-RapidScat. Unlike QuikSCAT, ISS-RapidScat is not in sun-synchronous orbit, and flies at roughly half the altitude with a low inclination angle that restricts data coverage to the tropics and mid-latitude regions; the extent of latitudinal coverage stretches from approximately 61 degrees North to 61 degrees South. Furthermore, there is no consistent local time of day retrieval.
&lt;br&gt;&lt;h4 id&#x3D;&quot;rscat_l2a_12km_v20&quot;&gt;RSCAT_L2A_12KM_V2.0&lt;/h4&gt;
This dataset contains the Version 2.0 ISS-RapidScat on Level 2A 12.5 km science data record, which provides surface-flagged sigma-0 in 12.5 km Wind Vector Cells processed using the pulse &amp;quot;slice&amp;quot; Sigma-0 data provided by the Level 1B dataset. Due to the circular scan of the RapidScat instrument the expected number of Sigma-0 cells per WVC is not constant. To minimize the L2A data volume, the Sigma-0 cell data are stored as &amp;quot;lists&amp;quot; for each WVC row, with each list indexed by a &amp;quot;cell_index&amp;quot; array to indicate the cross-track WVC membership of the data. Each cell is then checked for land or ice and flagged accordingly. Attenuation corrections for each Sigma-0 measurement are also provided. Version 2.0 represents a complete historical re-processing of the L2A data record and provides a calibration which is consistent across the several signal to noise ratio states experienced by RapidScat throughout its operation period (see the technical note for Version 2.0 under Documentation). It is also derived from the same L1B V2.0 product that was used to generate Version 2.0 wind products (L2B). Data are provided in single-orbit files in HDF-4 format. RapidScat is a Ku-band dual beam circular rotating scatterometer retaining much of the same hardware and functionality of QuikSCAT, with exception of the antenna sub-system and digital interface to the International Space Station (ISS) Columbus module, which is where RapidScat is mounted. The NASA mission is officially referred to as ISS-RapidScat. Unlike QuikSCAT, ISS-RapidScat is not in sun-synchronous orbit, and flies at roughly half the altitude with a low inclination angle that restricts data coverage to the tropics and mid-latitude regions; the extent of latitudinal coverage stretches from approximately 61 degrees North to 61 degrees South. Furthermore, there is no consistent local time of day retrieval.
&lt;br&gt;&lt;h4 id&#x3D;&quot;rscat_l2a_25km_v20&quot;&gt;RSCAT_L2A_25KM_V2.0&lt;/h4&gt;
This dataset contains the Version 2.0 ISS-RapidScat Level 2A 25km science data record, which provides surface-flagged sigma-0 in 25km Wind Vector Cells processed using the pulse &amp;quot;egg&amp;quot; Sigma-0 data provided by the Level 1B dataset. Due to the circular scan of the SeaWinds instrument the expected number of Sigma-0 cells per WVC is not constant. To minimize the L2A data volume, the Sigma-0 cell data are stored as &amp;quot;lists&amp;quot; for each WVC row, with each list indexed by a &amp;quot;cell_index&amp;quot; array to indicate the cross-track WVC membership of the data. Each cell is then checked for land or ice and flagged accordingly. Attenuation corrections for each Sigma-0 measurement are also provided. Version 2.0 represents a complete historical re-processing of the L2A data record and provides a calibration which is consistent across the several signal to noise ratio states experienced by RapidScat throughout its operation period (see the technical note for Version 2.0 under Documentation). It is also derived from the same L1B V2.0 product that was used to generate Version 2.0 wind products (L2B). Data are provided in single-orbit files in HDF-4 format. RapidScat is a Ku-band dual beam circular rotating scatterometer retaining much of the same hardware and functionality of QuikSCAT, with exception of the antenna sub-system and digital interface to the International Space Station (ISS) Columbus module, which is where RapidScat is mounted. The NASA mission is officially referred to as ISS-RapidScat. Unlike QuikSCAT, ISS-RapidScat is not in sun-synchronous orbit, and flies at roughly half the altitude with a low inclination angle that restricts data coverage to the tropics and mid-latitude regions; the extent of latitudinal coverage stretches from approximately 61 degrees North to 61 degrees South. Furthermore, there is no consistent local time of day retrieval.
&lt;br&gt;&lt;h4 id&#x3D;&quot;rscat_level_2b_owv_clim_12_v1&quot;&gt;RSCAT_LEVEL_2B_OWV_CLIM_12_V1&lt;/h4&gt;
This dataset contains the RapidScat Level 2B 12.5km Version 1.0 Climate quality ocean surface wind vectors. The Level 2B wind vectors are binned on a 12.5 km Wind Vector Cell (WVC) grid and processed using the using the &amp;quot;full aperture&amp;quot; normalized radar cross-section (NRCS, a.k.a. Sigma-0) from the L1B dataset. RapidScat is a Ku-band dual beam circular rotating scatterometer retaining much of the same hardware and functionality of QuikSCAT, with exception of the antenna sub-system and digital interface to the International Space Station (ISS) Columbus module, which is where RapidScat is mounted. The NASA mission is officially referred to as ISS-RapidScat. Unlike QuikSCAT, ISS-RapidScat is not in sun-synchronous orbit, and flies at roughly half the altitude with a low inclination angle that restricts data coverage to the tropics and mid-latitude regions; the extent of latitudinal coverage stretches from approximately 61 degrees North to 61 degrees South. Furthermore, there is no consistent local time of day retrieval. This dataset is provided in a netCDF-3 file format that follows the netCDF-4 classic model (i.e., generated by the netCDF-4 API) and made available via Direct Download and OPeNDAP. For data access, please click on the &amp;quot;Data Access&amp;quot; tab above. This climate quality data set differs from the nominal &amp;quot;slice&amp;quot; L2B dataset as follows: 1) it uses full antenna footprint measurements (&lt;del&gt;20-km) without subdividing by range (&lt;/del&gt;7-km) and 2) the absolute calibration has been modified for the two different low signal-to-noise ratio (SNR) mode data sets: LowSNR1 14 August 2015 to 18 September 2015; LowSNR2 6 October 2015 to 7 February 2016. The above enhancements allow this dataset to provide consistent calibration across all SNR states. Low SNR periods and other key quality control (QC) issues are tracked and kept up-to-date in PO.DAAC Drive at &lt;a href&#x3D;&quot;https://archive.podaac.earthdata.nasa.gov/podaac-ops-cumulus-docs/rapidscat/open/L1B/docs/revtime.csv&quot;&gt;https://archive.podaac.earthdata.nasa.gov/podaac-ops-cumulus-docs/rapidscat/open/L1B/docs/revtime.csv&lt;/a&gt;. If you have any questions, please visit our user forums: &lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/forum/&quot;&gt;https://podaac.jpl.nasa.gov/forum/&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;rscat_level_2b_owv_clim_12_v2&quot;&gt;RSCAT_LEVEL_2B_OWV_CLIM_12_V2&lt;/h4&gt;
This dataset contains the RapidScat Level 2B 12.5km Version 2.0 Climate quality ocean surface wind vectors. The Level 2B wind vectors are binned on a 12.5 km Wind Vector Cell (WVC) grid and processed using the using the &amp;quot;full aperture&amp;quot; normalized radar cross-section (NRCS, a.k.a. Sigma-0) from the L1B dataset. RapidScat is a Ku-band dual beam circular rotating scatterometer retaining much of the same hardware and functionality of QuikSCAT, with exception of the antenna sub-system and digital interface to the International Space Station (ISS) Columbus module, which is where RapidScat is mounted. The NASA mission is officially referred to as ISS-RapidScat. Unlike QuikSCAT, ISS-RapidScat is not in sun-synchronous orbit, and flies at roughly half the altitude with a low inclination angle that restricts data coverage to the tropics and mid-latitude regions; the extent of latitudinal coverage stretches from approximately 61 degrees North to 61 degrees South. Furthermore, there is no consistent local time of day retrieval. The new version has two important improvements over the previous version 1.0. First, an SST-dependent GMF developed by Lucrezia Ricciardulli of Remote Sensing Systems is used in wind retrieval in order to fix persistent speed biases in Ku-band data over cold ocean. Second, flagging is simplified and extra flags are provided. All the previously existing flags are still there and still reflect the same meaning and purpose. A new single bit wind_retrieval_likely_corrupted_flag specifies the approximately 3% of the data which is known to have suboptimal performance due to rain, ice, or a few other rare anomalous cases. Another bit wind_retrieval_possibly_corrupted_flag specifies the approximately 15% of the data near rain, near ice, or near the coast, that is thought to be high quality but may not match up well with numerical wind models due to either remaining rain/ice/land contamination or variability in the winds near ice, rain, and coasts that are not reflected in the NWPs. In addition to these two new bits, copious quality information is provided in the data to allow users to tailor flags to meet their own needs. There is also an added a global attribute called rev_status that specifies whether the RapidScat Instrument was in the original (highest data quality) high SNR mode, or one of the four low SNR time periods, the latter of which indicates the accuracy of winds below 5 m/s is degraded. This attribute also serves to identify MARGINAL orbits in which there are large gaps in the data record due to suboptimal spacecraft attitude. Other than gaps in the data, the accuracy of the winds in the MARGINAL orbits are similar to other orbits. This dataset is provided in netCDF-4 format and made available via FTP and OPeNDAP. For data access, please click on the &amp;quot;Data Access&amp;quot; tab above.
&lt;br&gt;&lt;h4 id&#x3D;&quot;rscat_level_2b_owv_comp_12_v11&quot;&gt;RSCAT_LEVEL_2B_OWV_COMP_12_V1.1&lt;/h4&gt;
This dataset contains the RapidScat Level 2B 12.5km Version 1.1 science-quality ocean surface wind vectors. The Level 2B wind vectors are binned on a 12.5 km Wind Vector Cell (WVC) grid and processed using the Level 2A Sigma-0 dataset. RapidScat is a Ku-band dual beam circular rotating scatterometer retaining much of the same hardware and functionality of QuikSCAT, with exception of the antenna sub-system and digital interface to the International Space Station (ISS) Columbus module, which is where RapidScat is mounted. The NASA mission is officially referred to as ISS-RapidScat. Unlike QuikSCAT, ISS-RapidScat is not in sun-synchronous orbit, and flies at roughly half the altitude with a low inclination angle that restricts data coverage to the tropics and mid-latitude regions; the extent of latitudinal coverage stretches from approximately 61 degrees North to 61 degrees South. Furthermore, there is no consistent local time of day retrieval. This dataset is provided in a netCDF-3 file format that follows the netCDF-4 classic model (i.e., generated by the netCDF-4 API) and made available via FTP and OPeNDAP. For data access, please click on the &amp;quot;Data Access&amp;quot; tab above. This Version 1.1 dataset differs from the previous Version 1 dataset as follows: 1) A new neural network approach for high wind speeds provided rain corrections for the &amp;quot;retrieve_wind_speed&amp;quot; variable for wind speeds in excess of 15 m/s. 2) The data variables containing the number of measurements of each type for each wind vector cell have been corrected; these variables include &amp;quot;number_in_aft&amp;quot;, &amp;quot;number_in_fore&amp;quot;, &amp;quot;number_out_aft&amp;quot;, and &amp;quot;number_out_fore&amp;quot;. 3) The &amp;quot;wind_obj&amp;quot; data variable has been corrected to include the proper data for the conditional probability for the objective DIRTH function values. It is advised for users to avoid using the &amp;quot;wind_obj&amp;quot; variable in this dataset since it is minimally applicable and meant primarily for quality assurance; for users who wish to access the objective function values for each ambiguity, it is suggested to use only the &amp;quot;ambiguity_obj&amp;quot; variable. The &amp;quot;wind_obj&amp;quot; variable contains DIRTH probabilities (which are derived form the &amp;quot;ambiguity_obj&amp;quot; objective function values) in the range of 0 to 1 indicating the conditional probability that the true direction is within + or - 2.5 degrees of the retrieved wind direction given the observed backscatter measurements in the cell. If you have any questions, please contact &lt;a href&#x3D;&quot;mailto:&amp;#x70;&amp;#111;&amp;#x64;&amp;#97;&amp;#97;&amp;#x63;&amp;#x40;&amp;#112;&amp;#x6f;&amp;#100;&amp;#97;&amp;#x61;&amp;#x63;&amp;#x2e;&amp;#x6a;&amp;#112;&amp;#x6c;&amp;#46;&amp;#110;&amp;#x61;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#x70;&amp;#111;&amp;#x64;&amp;#97;&amp;#97;&amp;#x63;&amp;#x40;&amp;#112;&amp;#x6f;&amp;#100;&amp;#97;&amp;#x61;&amp;#x63;&amp;#x2e;&amp;#x6a;&amp;#112;&amp;#x6c;&amp;#46;&amp;#110;&amp;#x61;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;rscat_level_2b_owv_comp_12_v12&quot;&gt;RSCAT_LEVEL_2B_OWV_COMP_12_V1.2&lt;/h4&gt;
This dataset contains the RapidScat Level 2B 12.5km Version 1.2 science-quality ocean surface wind vectors, which are intended as a replacement and continuation of the Version 1.1 data forward from orbital revolution number 5127, corresponding to 19 August 2015; the overlapping time period starting on 19 August 2015 corresponds to the first time period of the recorded low signal-to-noise ratio (SNR). The Level 2B wind vectors are binned on a 12.5 km Wind Vector Cell (WVC) grid and processed using the Level 2A Sigma-0 dataset. RapidScat is a Ku-band dual beam circular rotating scatterometer retaining much of the same hardware and functionality of QuikSCAT, with exception of the antenna sub-system and digital interface to the International Space Station (ISS) Columbus module, which is where RapidScat is mounted. The NASA mission is officially referred to as ISS-RapidScat. Unlike QuikSCAT, ISS-RapidScat is not in sun-synchronous orbit, and flies at roughly half the altitude with a low inclination angle that restricts data coverage to the tropics and mid-latitude regions; the extent of latitudinal coverage stretches from approximately 61 degrees North to 61 degrees South. Furthermore, there is no consistent local time of day retrieval. This dataset is provided in a netCDF-3 file format that follows the netCDF-4 classic model (i.e., generated by the netCDF-4 API) and made available via FTP and OPeNDAP. For data access, please click on the &amp;quot;Data Access&amp;quot; tab above. This Version 1.2 dataset differs from the previous Version 1.1 dataset as follows: 1) L1B sigma-0 has been re-calibrated during the periods of low signal-to-noise ratio (SNR) and 2) during low SNR periods the L1B sigma-0 calibration is determined using re-pointed L1B QuikSCAT data. It is advised for users to avoid using the &amp;quot;wind_obj&amp;quot; variable in this dataset since it is minimally applicable and meant primarily for quality assurance; for users who wish to access the objective function values for each ambiguity, it is suggested to use only the &amp;quot;ambiguity_obj&amp;quot; variable. The &amp;quot;wind_obj&amp;quot; variable contains DIRTH probabilities (which are derived form the &amp;quot;ambiguity_obj&amp;quot; objective function values) in the range of 0 to 1 indicating the conditional probability that the true direction is within + or - 2.5 degrees of the retrieved wind direction given the observed backscatter measurements in the cell. If you have any questions or concerns, please visit our Forum at &lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/forum/&quot;&gt;https://podaac.jpl.nasa.gov/forum/&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;rscat_level_2b_owv_comp_12_v13&quot;&gt;RSCAT_LEVEL_2B_OWV_COMP_12_V1.3&lt;/h4&gt;
This dataset contains the RapidScat Level 2B 12.5km Version 1.3 science-quality ocean surface wind vectors, which are intended as a replacement and continuation of the Version 1.1 and 1.2 data forward from orbital revolution number 7873, corresponding to 11 February 2016; on 11 Feb 2016, RapidScat entered it&amp;#39;s 3rd low signal to noise ratio (SNR) state and the initial calibration of low SNR 3 was preliminary during the Version 1.2 release. The fundamental difference between Version 1.3 and the previous Version 1.2 datasets is that the L1B sigma-0 has been re-calibrated during the periods of low SNR states 3 and 4 using re-pointed QuikSCAT data. The Version 1.1 should still be considered valid up to the first rev of version 1.2 (5127), and similarly version 1.2 shall be considered valid up to the first rev of version 1.3 (7873). The Level 2B wind vectors are binned on a 12.5 km Wind Vector Cell (WVC) grid and processed using the Level 2A Sigma-0 dataset. RapidScat is a Ku-band dual beam circular rotating scatterometer retaining much of the same hardware and functionality of QuikSCAT, with exception of the antenna sub-system and digital interface to the International Space Station (ISS) Columbus module, which is where RapidScat is mounted. The NASA mission is officially referred to as ISS-RapidScat. Unlike QuikSCAT, ISS-RapidScat is not in sun-synchronous orbit, and flies at roughly half the altitude with a low inclination angle that restricts data coverage to the tropics and mid-latitude regions; the extent of latitudinal coverage stretches from approximately 61 degrees North to 61 degrees South. Furthermore, there is no consistent local time of day retrieval. This dataset is provided in a netCDF-3 file format that follows the netCDF-4 classic model (i.e., generated by the netCDF-4 API) and made available via FTP and OPeNDAP. For data access, please click on the &amp;quot;Data Access&amp;quot; tab above. It is advised for users to avoid using the &amp;quot;wind_obj&amp;quot; variable in this dataset since it is minimally applicable and meant primarily for quality assurance; for users who wish to access the objective function values for each ambiguity, it is suggested to use only the &amp;quot;ambiguity_obj&amp;quot; variable. The &amp;quot;wind_obj&amp;quot; variable contains DIRTH probabilities (which are derived form the &amp;quot;ambiguity_obj&amp;quot; objective function values) in the range of 0 to 1 indicating the conditional probability that the true direction is within + or - 2.5 degrees of the retrieved wind direction given the observed backscatter measurements in the cell. If you have any questions or concerns, please visit our Forum at &lt;a href&#x3D;&quot;https://podaac.jpl.nasa.gov/forum/&quot;&gt;https://podaac.jpl.nasa.gov/forum/&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;rscat_colocated_rss_radiometer_level_2b_v1&quot;&gt;RSCAT_COLOCATED_RSS_RADIOMETER_LEVEL_2B_V1&lt;/h4&gt;
This dataset contains the multi-sourced microwave radiometer wind speed, rain and cloud liquid water data collocated to RapidScat Level 2B wind vector cell (WVC) locations. The corresponding NASA mission is officially referred to as ISS-RapidScat. This dataset is produced by Remote Sensing Systems (RSS) with direct funding from the JPL RapidScat project. All of the collocated radiometer data is produced by RSS. The co-located radiometer sources include: 1) DMSP SSM/I (F15) and SSMIS (F16/F17), 2) Coriolis WindSat, 3) GCOM-W1 AMSR2 and 4) GPM Core GMI; more details on these radiometer sources and sensors can be extracted by scrolling down to the &amp;quot;Platform/Sensor&amp;quot; section below this description. RapidScat is a Ku-band dual beam circular rotating scatterometer retaining much of the same hardware and functionality of QuikSCAT, with exception of the antenna sub-system and digital interface to the International Space Station (ISS) Columbus module, which is where RapidScat is mounted. Unlike QuikSCAT, ISS-RapidScat is not in sun-synchronous orbit, and flies at roughly half the altitude with a low inclination angle that restricts data coverage to the tropics and mid-latitude regions; the extent of latitudinal coverage stretches from approximately 61 degrees North to 61 degrees South. Furthermore, there is no consistent local time of day retrieval. This dataset is provided in a netCDF-4 file format that follows the netCDF &amp;quot;classic&amp;quot; model and made available via FTP and OPeNDAP. For data access, please click on the &amp;quot;Data Access&amp;quot; tab above.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://archive.podaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA JASON-1 Project</title>
      <link>https://registry.opendata.aws/nasa-jason-1</link>
      <guid>https://registry.opendata.aws/nasa-jason-1</guid>
      <description>The enhanced Jason-1 Microwave Radiometer (JMR) corrections contains better wet tropospheric path delay corrections along with better land, rain and ice flagging for coastal regions than that found in the Jason-1 Geophysical Data Records (GDR). The enhanced corrections can be used in place of the GDR wet troposphere correction to provide more accurate Sea Surface Height Anomalies for coastal regions.
&lt;br&gt;&lt;h4 id&#x3D;&quot;jason-1_l2_ost_gpr_e&quot;&gt;JASON-1_L2_OST_GPR_E&lt;/h4&gt;
These Sea Surface Height Anomalies (SSHA) are derived from the Jason-1 Geophysical Data Record (GDR). Jason-1 is an altimetric mission whose instruments make direct observations of the following quantities: altimeter range, significant wave height, ocean radar backscatter cross-section (a measure of wind speed), ionospheric electron content (derived by a simple formula), tropospheric water content, and position relative to the GPS satellite constellation. Using the various parameter the SSHA can be calculated and are provided in this dataset. The data are in NetCDF format. This dataset only contains the parameters that are directly related to SSHA.
&lt;br&gt;&lt;h4 id&#x3D;&quot;jason-1_l2_ost_gpr_e_geodetic&quot;&gt;JASON-1_L2_OST_GPR_E_GEODETIC&lt;/h4&gt;
These Sea Surface Height Anomalies (SSHA) are derived from the Jason-1 Geophysical Data Record (GDR) Geodetic Mission. Jason-1 is an altimetric mission whose instruments make direct observations of the following quantities: altimeter range, significant wave height, ocean radar backscatter cross-section (a measure of wind speed), ionospheric electron content (derived by a simple formula), tropospheric water content, and position relative to the GPS satellite constellation. Using the various parameter the SSHA can be calculated and are provided in this dataset. The data are in NetCDF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;jason-1_l2_ost_gpn_e&quot;&gt;JASON-1_L2_OST_GPN_E&lt;/h4&gt;
The Jason-1 Geophysical Data Records (GDR) contain full accuracy altimeter data to measure sea surface height, with a high precision orbit (accuracy ~1.5 cm). The instruments on Jason-1 make direct observations of the following quantities: altimeter range, significant wave height, ocean radar backscatter cross-section (a measure of wind speed), ionospheric electron content (derived by a simple formula), tropospheric water content, mean sea surface, and position relative to the GPS satellite constellation. The GDR contain all relevant corrections needed to calculate the sea surface height. Sea surface height anomalies calculation and recommended data edit criteria are specified in the Jason-1 GDR User Handbook at &lt;a href&#x3D;&quot;https://archive.podaac.earthdata.nasa.gov/podaac-ops-cumulus-docs/jason1/open/L2/gdr_netcdf_e/docs/Handbook_Jason-1_v5.1_April2016.pdf&quot;&gt;https://archive.podaac.earthdata.nasa.gov/podaac-ops-cumulus-docs/jason1/open/L2/gdr_netcdf_e/docs/Handbook_Jason-1_v5.1_April2016.pdf&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;jason-1_l2_ost_gpn_e_geodetic&quot;&gt;JASON-1_L2_OST_GPN_E_GEODETIC&lt;/h4&gt;
The Jason-1 Geophysical Data Records (GDR) Geodetic Mission contain full accuracy altimeter data, with a high precision orbit, provided approximately 35 days after data collection. The data are sorted into cycles that are approximately 11 days long and contain 280 pass files. The instruments on Jason-1 make direct observations of the following quantities: altimeter range, significant wave height, ocean radar backscatter cross-section (a measure of wind speed), ionospheric electron content (derived by a simple formula), tropospheric water content, mean sea surface, and position relative to the GPS satellite constellation. The GDR contain all relevant corrections needed to calculate the sea surface height.
&lt;br&gt;&lt;h4 id&#x3D;&quot;jason-1_l2_ost_gps_e&quot;&gt;JASON-1_L2_OST_GPS_E&lt;/h4&gt;
The Sensory Geophysical Data Record (SGDR) files contain full accuracy altimeter data, with a high precision orbit (accuracy ~1.5 cm). The instruments on Jason-1 make direct observations of the following quantities: altimeter range, significant wave height, ocean radar backscatter cross-section (a measure of wind speed), ionospheric electron content (derived by a simple formula), tropospheric water content, mean sea surface, and position relative to the GPS satellite constellation. The SGDR contain all relevant corrections needed to calculate the sea surface height. It also contains the 20Hz waveforms that are required for retracking. The SGDR is an expert level product, if you do not require the waveforms then the GDR/GPN or GPR will be more suited for your needs.
&lt;br&gt;&lt;h4 id&#x3D;&quot;jason-1_l2_ost_gps_e_geodetic&quot;&gt;JASON-1_L2_OST_GPS_E_GEODETIC&lt;/h4&gt;
The Sensory Geophysical Data Record (SGDR) files from the Geodetic Mission contain full accuracy altimeter data, with a high precision orbit. The instruments on Jason-1 make direct observations of the following quantities: altimeter range, significant wave height, ocean radar backscatter cross-section (a measure of wind speed), ionospheric electron content (derived by a simple formula), tropospheric water content, mean sea surface, and position relative to the GPS satellite constellation. The SGDR contain all relevant corrections needed to calculate the sea surface height. It also contains the 20Hz waveforms that are required for retracking. The SGDR is an expert level product, if you do not require the waveforms then the GDR will be more suited for your needs.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://archive.podaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA JASON-3 Project</title>
      <link>https://registry.opendata.aws/nasa-jason-3</link>
      <guid>https://registry.opendata.aws/nasa-jason-3</guid>
      <description>This is a near real time dataset that provides a GPS based orbit and Sea Surface Height Anomalies (SSHA) from that orbit. It is similar to the Jason-3 Operation Geophysical Data Record (OGDR) that is distributed at NOAA (&lt;a href&#x3D;&quot;http://www.nodc.noaa.gov/sog/jason/&quot;&gt;http://www.nodc.noaa.gov/sog/jason/&lt;/a&gt;), but includes the GPS orbit and SSHA as two additional variables. It has a 5 hour time lag due to the time needed to calculate the GPS orbit and SSHA. The GPS orbits have been shown to be more accurate than the DORIS orbits on a near real time scale and therefore produces a more accurate SSHA.&lt;br&gt; Forward stream transitioned from processing baseline/version &amp;quot;F&amp;quot; to &amp;quot;G&amp;quot; in January 2025. The change is reflected in the product filename: JA3_GPSOPR_2P&lt;b&gt;f&lt;/b&gt;S* -&amp;gt; JA3_GPSOPR_2P&lt;b&gt;g&lt;/b&gt;S*
&lt;br&gt;&lt;h4 id&#x3D;&quot;jason_3_pd_correction&quot;&gt;JASON_3_PD_CORRECTION&lt;/h4&gt;
This dataset provides supplementary wet tropospheric corrections for historical Jason-3 observations (&lt;a href&#x3D;&quot;https://www.ncei.noaa.gov/archive/accession/Jason3-xGDR&quot;&gt;https://www.ncei.noaa.gov/archive/accession/Jason3-xGDR&lt;/a&gt;). Recent assessments of the global sea level budget have resulted in increased scrutiny of estimates of global sea level change based on Jason-3. After a careful assessment of the wet tropospheric correction derived from the Advanced Microwave Radiometer (AMR) instrument, it was determined that further improvements to the accuracy of the historical Jason-3 observations could be made. Since this assessment was only completed after Jason-3 data was reprocessed to GDR-F (Geophysical Data Record – Version F) standards, it was not included in the GDR-F product release. For this reason, this supplementary correction product has been created using the method of Brown et al. (2012) to allow users to correct path delay and sea surface height observations, reducing errors in estimates of global sea level change by 2-3 mm over 8 years.&lt;br&gt;&lt;br&gt; The correction was computed based on comparison of the AMR-observed brightness temperatures with independent satellite observations from the Special Sensor Microwave Imager Sounder (SSMI), F16, F17 and F18, Fundamental Climate Data Records. SSMI data was obtained from the NOAA Climate Data Record (CDR) of SSMIS Microwave Brightness Temperatures, RSS Version 8 (Wentz et al., 2019, &lt;a href&#x3D;&quot;https://www.ncei.noaa.gov/metadata/geoportal/rest/metadata/item/gov.noaa.ncdc:C01567/html&quot;&gt;https://www.ncei.noaa.gov/metadata/geoportal/rest/metadata/item/gov.noaa.ncdc:C01567/html&lt;/a&gt;). The method described in Brown et al. (2012) to map SSMI Brightness Temperatures to AMR equivalent brightness temperatures (TBs) was used. Although it was found that it made little difference to the result, a bias was removed between SSMI equivalent AMR TBs and AMR TBs with respect to latitude for all data prior to computing temporal trends. In addition, only rain free, mostly clear data (TB18.7 GHz &amp;lt; 160K) data were considered.&lt;br&gt;&lt;br&gt; The correction is supplied on a pass-by-pass basis in a 4-column text file. See the product documentation for guidance on how to apply it to Jason-3 observations.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://archive.podaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA JPSS Project</title>
      <link>https://registry.opendata.aws/nasa-jpss</link>
      <guid>https://registry.opendata.aws/nasa-jpss</guid>
      <description>This High-Resolution (0.1 x 0.1 degree) Level 3 daily Aerosol Optical Depth (AOD) product is generated by combining two Visible Infrared Imaging Radiometer Suite (VIIRS) operational algorithms, namely Deep Blue (DB) and Dark Target (DT), on board the NOAA-20 satellite. This dataset is provided in daily files ranging from 2018-02-17 to the present. The spatial coverage is global and the dataset is gridded at 0.1 x 0.1 degree spatial resolution. The data are generated using Level 2 AOD retrieved using DT and DB algorithms. The product provides multiple options for using data either from DT or DB or combined. Depending on user need and application, they can choose one or more relevant parameter. The pixels with highest quality as recommended by science teams are only considered in these averaging. In addition to averaged AOD at 0.1 x 0.1 degree resolution, standard deviation and number of pixels averaged from each algorithm are also provided. Average sensor zenith angle is also provided for additional filtering of the data. If you have any questions, please read the README document first and post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#x66;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#108;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#115;&amp;#x66;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#108;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;aer_dbdt_m10km_l3_viirs_noaa20&quot;&gt;AER_DBDT_M10KM_L3_VIIRS_NOAA20&lt;/h4&gt;
This High-Resolution (0.1 x 0.1 degree) Level 3 monthly Aerosol Optical Depth (AOD) product is generated by combining two Visible Infrared Imaging Radiometer Suite (VIIRS) operational algorithms, namely Deep Blue (DB) and Dark Target (DT), on board the NOAA-20 satellite. This dataset is provided in monthly files ranging from February 2018 to the present. The spatial coverage is global and the dataset is gridded at 0.1 x 0.1 degree spatial resolution. The data are generated using Level 2 AOD retrieved using DT and DB algorithms. The product provides multiple options for using data either from DT or DB or combined. Depending on user need and application, they can choose one or more relevant parameter. The pixels with highest quality as recommended by science teams are only considered in these averaging. In addition to averaged AOD at 0.1 x 0.1 degree resolution, standard deviation and number of pixels averaged from each algorithm are also provided. Average sensor zenith angle is also provided for additional filtering of the data. If you have any questions, please read the README document first and post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;omps_n21_lp_l1g_ev&quot;&gt;OMPS_N21_LP_L1G_EV&lt;/h4&gt;
The OMPS-N21 L1G LP Radiance EV Wavelength-Altitude Grid swath orbital 3slit product contains the calibrated earth-viewing radiances measured by the Ozone Mapping and Profiling Suite (OMPS) Limb-Profiler (LP) sensor on the NOAA 21 (JPSS-2) satellite. The LP L1G product measures radiances in the wavelength region from 280 nm to 1000 nm. Each granule contains data from the daylight portion of each orbit measured for a full day. Spatial coverage is global (-90 to 90 degrees latitude), and there are about 14.5 orbits per day each measuring three limb profiles spaced approximately 250 km in the cross-track direction. The profiles are measured from the ground up to about 80 km with a vertical resolution of the retrieved profiles of approximately 1-2 km. The data are written using the Hierarchical Data Format Version 5 or HDF5.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sndrj1atmsmap&quot;&gt;SNDRJ1ATMSMAP&lt;/h4&gt;
The Advanced Technology Microwave Sounder (ATMS) Level 1B data files contain brightness temperature measurements along with ancillary spacecraft, instrument, and geolocation data of the ATMS instrument on the Joint Polar Satellite System-1 (JPSS-1) platform. This platform is also known as NOAA-20 (National Oceanic and Atmospheric Administration). The ATMS is a 22-channel mm-wave radiometer. The ATMS will measure upwelling radiances in six frequency bands centered at 23 GHz, 31 GHz, 50-58 GHz, 89 GHz, 66 GHz, and 183 GHz. The ATMS is a total power radiometer, with &amp;quot;through-the-antenna&amp;quot; radiometric calibration. Radiometric data is collected by a pair of antenna apertures, scanned by rotating flat plate reflectors. Scanning is performed cross-track to the satellite motion from sun to anti-sun, using the &amp;quot;integrate-while-scan&amp;quot; type data collection. The scan period is 8/3 second, synchronized to the Cross-track Infrared Sounder (CrIS) using a spacecraft provided scan synchronization pulse. Since the JPSS-1 satellite is orbiting at an altitude of about 830 km, the instantaneous spatial resolution on the ground at nadir is about 16 km, 32 km, or 75 km depending upon the channel. The brightness temperature data are contained in an array with 135 rows in the along-track direction, 96 columns in the cross-track direction, and a 3rd dimension for each of the 22 channels. The ATMS cross-track scan interval is 0.018 seconds and the along-track scan period is 8/3 seconds.. Data products are constructed on six minute boundaries. The Granule Map Product consists of daily images of granule coverage in PDF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sndrj1ml2rms&quot;&gt;SNDRJ1ML2RMS&lt;/h4&gt;
This level 2 product is generated by the RAMSES (Retrieval Algorithm for Microwave Sounders in Earth Science II algorithm.The RAMSES II algorithm is a microwave only retrieval algorithm using observations from the NOAA-20 (National Oceanic and Atmospheric Administration) also know as Joint Polar Satellite System (JPSS-1) Advanced Technology Microwave Sounder (ATMS) instrument. The ATMS instrument used for this product is a cross-track scanner with 22 channels in spectral bands from 23 GHz through 183 GHz. The RAMSES II Level-2 retrieval products contain a variety of geophysical parameters retrieved from ATMS measurements, including profiles of temperature, water in all phases as well as surface properties for six minutes of instrument observation at a time. The RAMSES II algorithm doesn&amp;#39;t have a cloud clearing process and produces all weather retrieval A level 2 granule has been set as 6 minutes of data. There are 240 granules per day, with an orbit repeat cycle of approximately 16 day.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sndrj1ml2rmssup&quot;&gt;SNDRJ1ML2RMSSUP&lt;/h4&gt;
This level 2 support product is generated by the RAMSES (Retrieval Algorithm for Microwave Sounders in Earth Science) II algorithm.The RAMSES II algorithm is a microwave only retrieval algorithm using observations from the NOAA-20 (National Oceanic and Atmospheric Administration) also know as Joint Polar Satellite System (JPSS-1) Advanced Technology Microwave Sounder (ATMS) instrument. The ATMS instrument used for this product is a cross-track scanner with 22 channels in spectral bands from 23 GHz through 183 GHz. The RAMSES II Level-2 retrieval products contain a variety of geophysical parameters retrieved from ATMS measurements, including profiles of temperature, water in all phases as well as surface properties for six minutes of instrument observation at a time. The RAMSES II algorithm doesn&amp;#39;t have a cloud clearing process and produces all weather retrieval A level 2 granule has been set as 6 minutes of data. There are 240 granules per day, with an orbit repeat cycle of approximately 16 day.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sndrj1ml3drms&quot;&gt;SNDRJ1ML3DRMS&lt;/h4&gt;
This level 3 daily product is generated from the RAMSES (Retrieval Algorithm for Microwave Sounders in Earth Science) II algorithm.The RAMSES II algorithm is a microwave only retrieval algorithm using observations from the NOAA-20 (National Oceanic and Atmospheric Administration) also know as Joint Polar Satellite System (JPSS-1) Advanced Technology Microwave Sounder (ATMS) instrument. The ATMS instrument used for this product is a cross-track scanner with 22 channels in spectral bands from 23 GHz through 183 GHz. The RAMSES II retrieval products contain a variety of geophysical parameters retrieved from ATMS measurements, including profiles of temperature, water in all phases as well as surface properties. The RAMSES II algorithm doesn&amp;#39;t have a cloud clearing process and produces all weather retrieval This daily one degree latitude by one degree longitude level-3 product starts with level-2 retrieval products with QC values of 0 (best), 1 (good), and 2 (don&amp;#39;t use) which are provided for each variable.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sndrj1ml3mrms&quot;&gt;SNDRJ1ML3MRMS&lt;/h4&gt;
This level 3 monthly product is generated from the RAMSES (Retrieval Algorithm for Microwave Sounders in Earth Science) II algorithm.The RAMSES II algorithm is a microwave only retrieval algorithm using observations from the NOAA-20 (National Oceanic and Atmospheric Administration) also know as Joint Polar Satellite System (JPSS-1) Advanced Technology Microwave Sounder (ATMS) instrument. The ATMS instrument used for this product is a cross-track scanner with 22 channels in spectral bands from 23 GHz through 183 GHz. The RAMSES II retrieval products contain a variety of geophysical parameters retrieved from ATMS measurements, including profiles of temperature, water in all phases as well as surface properties. The RAMSES II algorithm doesn&amp;#39;t have a cloud clearing process and produces all weather retrieval This monthly one degree latitude by one degree longitude level-3 product starts with level-2 retrieval products with QC values of 0 (best), 1 (good), and 2 (don&amp;#39;t use) which are provided for each variable.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sndrj1iml2cps&quot;&gt;SNDRJ1IML2CPS&lt;/h4&gt;
The CLIMCAPS (Community Long-term Infrared Microwave Coupled Product System) algorithm is used to analyze data from the Cross-track Infrared Sounder/Advanced Technology Microwave Sounder (CrIS/ATMS) instruments, also known as CrIMSS (Cross-track Infrared and Microwave Sounding Suite). The CrIS/ATMS instruments used for this product are on board the NOAA-20 platform, also known as JPSS-1. The CrIS instrument is a Fourier transform spectrometer with a total of 2211 FSR (Full Spectral Resolution) infrared sounding channels covering the longwave (645-1095 cm-1), midwave (1210-1750 cm-1), and shortwave (2100-2550 cm-1) spectral regions. The ATMS instrument is a cross-track scanner with 22 channels in spectral bands from 23 GHz through 183 GHz. The CLIMCAPS algorithm uses an Optimal Estimation methodology and uses an a-priori first guess to start the process. A CLIMCAPS sounding is comprised of a set of parameters that characterizes the full atmospheric state and includes a variety of geophysical parameters derived from the CrIMSS data. These include surface temperature and infrared emissivity; full atmosphere profiles of temperature, water vapor and ozone; infrared effective cloud top characteristics; carbon monoxide, methane, carbon dioxide, sulfur dioxide, nitrous oxide, and nitric acid. The CLIMCAPS algorithm uses data from the second Modern-Era Retrospective analysis for Research and Applications (MERRA-2) as a first-guess for the atmospheric state. Because MERRA-2 products typically have a latency from 3 to 7 weeks, so too do the CLIMCAPS products. A level 2 granule has been set as 6 minutes of data, 30 footprints cross track by 45 lines along track. There are 240 granules per day, with an orbit repeat cycle of approximately 16 day.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sndrj1iml2plevcps&quot;&gt;SNDRJ1IML2PLEVCPS&lt;/h4&gt;
The CLIMCAPS (Community Long-term Infrared Microwave Coupled Product System) algorithm is used to analyze data from the Cross-track Infrared Sounder/Advanced Technology Microwave Sounder (CrIS/ATMS) instruments, also known as CrIMSS (Cross-track Infrared and Microwave Sounding Suite). This file contains the fixed Pressure Level product (PLEV) variables derived from the CLIMCAPS algorithm using data from the JPSS-1 (Joint Polar Satellite System). They include including gas mixing ratio profiles, column totals, surface values, tropopause properties, and relative humidity, together with per-field quality flagging. The profiles are specified at the surface and layer boundaries and are estimated from layer amounts using the L2 algorithm An level 2 granule has been set as 6 minutes of data, 30 footprints cross track by 45 lines along track. There are 240 granules per day, with an orbit repeat cycle of approximately 16 day. The CLIMCAPS algorithm uses data from the second Modern-Era Retrospective analysis for Research and Applications (MERRA-2) as a first-guess for the atmospheric state. Because MERRA-2 products typically have a latency from 3 to 7 weeks, so too do the CLIMCAPS products.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sndrj1iml2ccpret&quot;&gt;SNDRJ1IML2CCPRET&lt;/h4&gt;
WARNING: To users of the derived product “co_mmr_midtrop” (carbon monoxide mass mixing ratio to dry air [kg/kg] at ~500 hPa). This variable has a significant bias due to a conversion error: the molecular weight of carbon dioxide (CO2, 44.01 g/mol) was used instead of carbon monoxide (CO, 28.01 g/mol). To correct, simply multiply “co_mmr_midtrop” by 28.01/44.01. Alternatively, derive a profile of mass mixing ratio from scratch using the retrieved column density values (“mol_lay/co_mol_lay”) in the Level 2 files. For further questions or concerns please contact the Sounder SIPS at: &lt;a href&#x3D;&quot;mailto:&amp;#115;&amp;#111;&amp;#x75;&amp;#110;&amp;#100;&amp;#101;&amp;#114;&amp;#46;&amp;#115;&amp;#105;&amp;#x70;&amp;#x73;&amp;#64;&amp;#x6a;&amp;#112;&amp;#x6c;&amp;#46;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#115;&amp;#111;&amp;#x75;&amp;#110;&amp;#100;&amp;#101;&amp;#114;&amp;#46;&amp;#115;&amp;#105;&amp;#x70;&amp;#x73;&amp;#64;&amp;#x6a;&amp;#112;&amp;#x6c;&amp;#46;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#x76;&lt;/a&gt; The CLIMCAPS (Community Long-term Infrared Microwave Coupled Product System) algorithm is used to analyze data from the Cross-track Infrared Sounder/Advanced Technology Microwave Sounder (CrIS/ATMS) instruments, also known as CrIMSS (Cross-track Infrared and Microwave Sounding Suite). The CrIS/ATMS instruments used for this product are on board the NOAA-20 platform, also known as JPSS-1. The CrIS instrument is a Fourier transform spectrometer with a total of 2211 FSR (Full Spectral Resolution) infrared sounding channels covering the longwave (645-1095 cm-1), midwave (1210-1750 cm-1), and shortwave (2100-2550 cm-1) spectral regions. The ATMS instrument is a cross-track scanner with 22 channels in spectral bands from 23 GHz through 183 GHz. The CLIMCAPS algorithm uses an Optimal Estimation methodology and uses an a-priori first guess to start the process. A CLIMCAPS sounding is comprised of a set of parameters that characterizes the full atmospheric state and includes a variety of geophysical parameters derived from the CrIMSS data. These include surface temperature and infrared emissivity; full atmosphere profiles of temperature, water vapor and ozone; infrared effective cloud top characteristics; carbon monoxide, methane, carbon dioxide, sulfur dioxide, nitrous oxide, and nitric acid. The CLIMCAPS algorithm uses data from the second Modern-Era Retrospective analysis for Research and Applications (MERRA-2) as a first-guess for the atmospheric state. Because MERRA-2 products typically have a latency from 3 to 7 weeks, so too do the CLIMCAPS products. A level 2 granule has been set as 6 minutes of data, 30 footprints cross track by 45 lines along track. There are 240 granules per day, with an orbit repeat cycle of approximately 16 day.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj114img&quot;&gt;VJ114IMG&lt;/h4&gt;
The Visible Infrared Imaging Radiometer Suite (VIIRS) Active Fires (VJ114IMG) Version 2 product is produced in 6-minute temporal satellite increments (swaths) at 375 meter resolution from the VIIRS sensor aboard the NOAA-20 satellite. This product is designed after the Terra and Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Thermal Anomalies and Fire data products to promote the continuity of the Earth Observation System (EOS) mission. This data product can enable users to understand the location and intensity of fire events as well as thermal anomalies. The VJ114IMG product includes 26 science dataset layers to analyze key factors in fire detection, including atmospheric conditions (e.g., radiance, solar zenith angle, brightness temperature) and fuel type for the event. The fire mask layer in the VJ114IMG product is the primary layer and can be used to identify fires and other thermal anomalies such as volcanoes. Each swath of data is approximately 3,060 kilometers along track (long) and 3,060 kilometers across track (wide). The VJ114IMG product is also used to generate higher-level fire data products. Use of the &lt;a href&#x3D;&quot;https://doi.org/10.5067/viirs/vJ103modll.021&quot;&gt;VJ103MODLL&lt;/a&gt; data product is required to apply accurate geolocation information to the VNP14IMG Science Datasets (SDS). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj109&quot;&gt;VJ109&lt;/h4&gt;
The VIIRS/JPSS1 Atmospherically Corrected Surface Reflectance 6-Min L2 Swath 375m, 750m product, with short name VJ109, are estimates of surface reflectance in each of the Visible Infrared Imaging Radiometer Suite (VIIRS) reflective bands I1-I3, M1-M5, M7, M8, M10, and M11. The VJ109 contains approximately 6 minutes&amp;#39; worth of data. Surface reflectance for each moderate-resolution (750m) or imagery-resolution (375m) pixel is retrieved separately for the Level-2 products. Surface reflectance is obtained by adjusting top-of-atmosphere reflectance to compensate for atmospheric effects. Corrections are made for the effects of molecular gases, including ozone and water vapor, and for the effects of atmospheric aerosols. All surface reflectance products are produced for daytime conditions only. The product is produced under all atmospheric conditions except for night and oceans.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143c3&quot;&gt;VJ143C3&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Albedo Daily Global 0.05 Degree Climate Modeling Grid (CMG) Version 2 product (VJ143C3) is derived from the 30 arc second CMG VJ143D Version 2 product suite. VJ143C3 is generated daily from all available high-quality reflectance data over a 16-day moving window emphasizing the ninth day of the retrieval period, which is reflected in the Julian date in the filename. The VJ143 algorithm uses the RossThick/Li-Sparse-Reciprocal (RTLSR) semi-empirical kernel-driven BRDF model, with the three kernel weights from &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143C1.002&quot;&gt;VJ143C1&lt;/a&gt; to compute white-sky albedos and the black-sky albedos at local solar noon for the VIIRS Day/Night band (DNB), moderate resolution bands M1 through M5, M7, M8, M10, and M11, as well as the shortwave band, visible band, and near-infrared (NIR) broadbands. The quality and inversion status of the majority of the underlying 30 arc second pixels is provided as well as the percentage of the underlying pixels that were present or were snow covered. Users are encouraged to assess the quality information before using the BRDF/Albedo data. This 0.05 degree (5,600 meters at the equator) CMG product covers the entire globe for use in climate simulation models. The VJ143C3 product includes 26 layers containing white-sky albedos and the black-sky albedos for the VIIRS DNB, moderate resolution bands M1 through M5, M7, M8, M10, and M11, as well as the shortwave band, visible band, and NIR broadbands. Along with the albedo data for the 13 bands are five ancillary layers for uncertainty, quality, local solar noon, percent finer resolution inputs, and snow cover. A low-resolution image is also available showing retrievals of WSA for the shortwave broadband in JPEG format. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143ma3&quot;&gt;VJ143MA3&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo (VJ143MA3) Version 2 product provides albedo values at 1 kilometer (km) resolution for the bihemispherical reflectance white-sky albedo (WSA) and directional hemispherical reflectance black-sky albedo (BSA) at local solar noon. The VJ143MA3 product is produced daily using 16 days of VIIRS data and is weighted temporally to the ninth day, which is reflected in the file name. The VJ143 data products are designed to promote the continuity of NASA’s Moderate Resolution Imaging Spectroradiometer (MODIS) BRDF/Albedo data product suite. The VJ143 algorithm uses the RossThick/Li-Sparse-Reciprocal (RTLSR) semi-empirical kernel-driven BRDF model, with the three kernel weights from &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; to reconstruct surface anisotropic effects, correcting the directional reflectance to a common view geometry (&lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA4.002&quot;&gt;VJ143MA4&lt;/a&gt;), while also computing integrated black-sky albedo (BSA) at local solar noon and white-sky albedo (WSA) (VJ143MA3). Researchers can use the BRDF model parameters with a simple polynomial, to obtain black-sky albedo at any solar illumination angle. Likewise, both the BSA and WSA Science Dataset (SDS) layers can be used with a simple polynomial, to manually estimate instantaneous actual albedo (blue-sky albedo). Additional details regarding the methodology are available in the Algorithm Theoretical Basis Document (ATBD). The VJ143MA3 product provides a total of 36 SDS layers including: BSA; WSA; and mandatory quality layers for nine VIIRS moderate bands M1-M5, M7-M8, and M10-M11; as well as near-infrared (NIR); shortwave; and visible broadbands. A low-resolution image is also available showing retrievals of WSA for band M1 in JPEG format. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143ia3&quot;&gt;VJ143IA3&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo (VJ143IA3) Version 2 product provides albedo values at 500 meter (m) resolution for the bihemispherical reflectance white-sky albedo (WSA) and directional hemispherical reflectance black-sky albedo (BSA) at local solar noon. The VJ143IA3 product is produced daily using 16 days of VIIRS data and is weighted temporally to the ninth day, which is reflected in the file name. The VJ143 data products are designed to promote the continuity of NASA’s Moderate Resolution Imaging Spectroradiometer (MODIS) BRDF/Albedo data product suite. The VJ143 algorithm uses the RossThick/Li-Sparse-Reciprocal (RTLSR) semi-empirical kernel-driven BRDF model, with the three kernel weights from &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143IA1.002&quot;&gt;VJ143IA1&lt;/a&gt; to reconstruct surface anisotropic effects, correcting the directional reflectance to a common view geometry (&lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143IA4.002&quot;&gt;VJ143IA4&lt;/a&gt;), while also computing integrated black-sky albedo (BSA) at local solar noon and white-sky albedo (WSA) (VJ143IA3). Researchers can use the BRDF model parameters with a simple polynomial, to obtain black-sky albedo at any solar illumination angle. Likewise, both the BSA and WSA Science Dataset (SDS) layers can be used with a simple polynomial, to manually estimate instantaneous actual albedo (blue-sky albedo). Additional details regarding the methodology are available in the Algorithm Theoretical Basis Document (ATBD). The VJ143IA3 product provides a total of 9 SDS layers including: BSA, WSA, and mandatory quality layers for VIIRS imagery bands I1, I2, and I3. A low-resolution browse image is also available showing retrievals of WSA for band I1 in JPEG format. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d54&quot;&gt;VJ143D54&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Black-Sky Albedo for Band M1 (VJ143D54) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D54 through VJ143D79 are the albedo products of the VJ143D BRDF/Albedo product suite. Black-sky albedo (BSA) and white-sky albedo (WSA) values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA3.002&quot;&gt;VJ143MA3&lt;/a&gt; product. In addition to the bands included in VJ143MA3, this product suite includes albedo values for the VIIRS Day/Night Band (DNB). The black-sky albedo (directional hemispherical reflectance) is defined as albedo in the absence of a diffuse component and is a function of solar zenith angle. White-sky albedo (bihemispherical reflectance) is defined as albedo in the absence of a direct component when the diffuse component is isotropic. Details regarding methodology are available on the VJ143MA3 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D54 is the BSA for VIIRS band M1 (0.412 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d61&quot;&gt;VJ143D61&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Black-Sky Albedo for Band M10 (VJ143D61) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D54 through VJ143D79 are the albedo products of the VJ143D BRDF/Albedo product suite. Black-sky albedo (BSA) and white-sky albedo (WSA) values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA3.002&quot;&gt;VJ143MA3&lt;/a&gt; product. In addition to the bands included in VJ143MA3, this product suite includes albedo values for the VIIRS Day/Night Band (DNB). The black-sky albedo (directional hemispherical reflectance) is defined as albedo in the absence of a diffuse component and is a function of solar zenith angle. White-sky albedo (bihemispherical reflectance) is defined as albedo in the absence of a direct component when the diffuse component is isotropic. Details regarding methodology are available on the VJ143MA3 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D61 is the BSA for VIIRS band M10 (1.61 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d62&quot;&gt;VJ143D62&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Black-Sky Albedo for Band M11 (VJ143D62) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D54 through VJ143D79 are the albedo products of the VJ143D BRDF/Albedo product suite. Black-sky albedo (BSA) and white-sky albedo (WSA) values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA3.002&quot;&gt;VJ143MA3&lt;/a&gt; product. In addition to the bands included in VJ143MA3, this product suite includes albedo values for the VIIRS Day/Night Band (DNB). The black-sky albedo (directional hemispherical reflectance) is defined as albedo in the absence of a diffuse component and is a function of solar zenith angle. White-sky albedo (bihemispherical reflectance) is defined as albedo in the absence of a direct component when the diffuse component is isotropic. Details regarding methodology are available on the VJ143MA3 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D62 is the BSA for VIIRS band M11 (2.25 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d55&quot;&gt;VJ143D55&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Black-Sky Albedo for Band M2 (VJ143D55) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D54 through VJ143D79 are the albedo products of the VJ143D BRDF/Albedo product suite. Black-sky albedo (BSA) and white-sky albedo (WSA) values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA3.002&quot;&gt;VJ143MA3&lt;/a&gt; product. In addition to the bands included in VJ143MA3, this product suite includes albedo values for the VIIRS Day/Night Band (DNB). The black-sky albedo (directional hemispherical reflectance) is defined as albedo in the absence of a diffuse component and is a function of solar zenith angle. White-sky albedo (bihemispherical reflectance) is defined as albedo in the absence of a direct component when the diffuse component is isotropic. Details regarding methodology are available on the VJ143MA3 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D55 is the BSA for VIIRS band M2 (0.445 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d56&quot;&gt;VJ143D56&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Black-Sky Albedo for Band M3 (VJ143D56) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D54 through VJ143D79 are the albedo products of the VJ143D BRDF/Albedo product suite. Black-sky albedo (BSA) and white-sky albedo (WSA) values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA3.002&quot;&gt;VJ143MA3&lt;/a&gt; product. In addition to the bands included in VJ143MA3, this product suite includes albedo values for the VIIRS Day/Night Band (DNB). The black-sky albedo (directional hemispherical reflectance) is defined as albedo in the absence of a diffuse component and is a function of solar zenith angle. White-sky albedo (bihemispherical reflectance) is defined as albedo in the absence of a direct component when the diffuse component is isotropic. Details regarding methodology are available on the VJ143MA3 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D56 is the BSA for VIIRS band M3 (0.488 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d57&quot;&gt;VJ143D57&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Black-Sky Albedo for Band M4 (VJ143D57) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D54 through VJ143D79 are the albedo products of the VJ143D BRDF/Albedo product suite. Black-sky albedo (BSA) and white-sky albedo (WSA) values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA3.002&quot;&gt;VJ143MA3&lt;/a&gt; product. In addition to the bands included in VJ143MA3, this product suite includes albedo values for the VIIRS Day/Night Band (DNB). The black-sky albedo (directional hemispherical reflectance) is defined as albedo in the absence of a diffuse component and is a function of solar zenith angle. White-sky albedo (bihemispherical reflectance) is defined as albedo in the absence of a direct component when the diffuse component is isotropic. Details regarding methodology are available on the VJ143MA3 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D57 is the BSA for VIIRS band M4 (0.555 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d58&quot;&gt;VJ143D58&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Black-Sky Albedo for Band M5 (VJ143D58) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D54 through VJ143D79 are the albedo products of the VJ143D BRDF/Albedo product suite. Black-sky albedo (BSA) and white-sky albedo (WSA) values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA3.002&quot;&gt;VJ143MA3&lt;/a&gt; product. In addition to the bands included in VJ143MA3, this product suite includes albedo values for the VIIRS Day/Night Band (DNB). The black-sky albedo (directional hemispherical reflectance) is defined as albedo in the absence of a diffuse component and is a function of solar zenith angle. White-sky albedo (bihemispherical reflectance) is defined as albedo in the absence of a direct component when the diffuse component is isotropic. Details regarding methodology are available on the VJ143MA3 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D58 is the BSA for VIIRS band M5 (0.672 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d59&quot;&gt;VJ143D59&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Black-Sky Albedo for Band M7 (VJ143D59) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D54 through VJ143D79 are the albedo products of the VJ143D BRDF/Albedo product suite. Black-sky albedo (BSA) and white-sky albedo (WSA) values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA3.002&quot;&gt;VJ143MA3&lt;/a&gt; product. In addition to the bands included in VJ143MA3, this product suite includes albedo values for the VIIRS Day/Night Band (DNB). The black-sky albedo (directional hemispherical reflectance) is defined as albedo in the absence of a diffuse component and is a function of solar zenith angle. White-sky albedo (bihemispherical reflectance) is defined as albedo in the absence of a direct component when the diffuse component is isotropic. Details regarding methodology are available on the VJ143MA3 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D59 is the BSA for VIIRS band M7 (0.865 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d60&quot;&gt;VJ143D60&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Black-Sky Albedo for Band M8 (VJ143D60) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D54 through VJ143D79 are the albedo products of the VJ143D BRDF/Albedo product suite. Black-sky albedo (BSA) and white-sky albedo (WSA) values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA3.002&quot;&gt;VJ143MA3&lt;/a&gt; product. In addition to the bands included in VJ143MA3, this product suite includes albedo values for the VIIRS Day/Night Band (DNB). The black-sky albedo (directional hemispherical reflectance) is defined as albedo in the absence of a diffuse component and is a function of solar zenith angle. White-sky albedo (bihemispherical reflectance) is defined as albedo in the absence of a direct component when the diffuse component is isotropic. Details regarding methodology are available on the VJ143MA3 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D60 is the BSA for VIIRS band M8 (1.240 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d63&quot;&gt;VJ143D63&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Black-Sky Albedo for Band VIS (VJ143D63) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VNJ143D product contains just one data layer. VJ143D54 through VJ143D79 are the albedo products of the VJ143D BRDF/Albedo product suite. Black-sky albedo (BSA) and white-sky albedo (WSA) values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) along with the visible (VIS), near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA3.002&quot;&gt;VJ143MA3&lt;/a&gt; product. In addition to the bands included in VJ143MA3, this product suite includes albedo values for the VIIRS Day/Night Band (DNB). The black-sky albedo (directional hemispherical reflectance) is defined as albedo in the absence of a diffuse component and is a function of solar zenith angle. White-sky albedo (bihemispherical reflectance) is defined as albedo in the absence of a direct component when the diffuse component is isotropic. Details regarding methodology are available on the VJ143MA3 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D63 is the BSA for the VIIRS visible broadband (0.64 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d66&quot;&gt;VJ143D66&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Black-Sky Albedo for DNB (VJ143D66) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D54 through VJ143D79 are the albedo products of the VJ143D BRDF/Albedo product suite. Black-sky albedo (BSA) and white-sky albedo (WSA) values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA3.002&quot;&gt;VJ143MA3&lt;/a&gt; product. In addition to the bands included in VJ143MA3, this product suite includes albedo values for the VIIRS Day/Night Band (DNB). The black-sky albedo (directional hemispherical reflectance) is defined as albedo in the absence of a diffuse component and is a function of solar zenith angle. White-sky albedo (bihemispherical reflectance) is defined as albedo in the absence of a direct component when the diffuse component is isotropic. Details regarding methodology are available on the VJ143MA3 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D66 is the BSA for the VIIRS DNB (0.7 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d64&quot;&gt;VJ143D64&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Black-Sky Albedo for NIR (VJ143D64) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D54 through VJ143D79 are the albedo products of the VJ143D BRDF/Albedo product suite. Black-sky albedo (BSA) and white-sky albedo (WSA) values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA3.002&quot;&gt;VJ143MA3&lt;/a&gt; product. In addition to the bands included in VJ143MA3, this product suite includes albedo values for the VIIRS Day/Night Band (DNB). The black-sky albedo (directional hemispherical reflectance) is defined as albedo in the absence of a diffuse component and is a function of solar zenith angle. White-sky albedo (bihemispherical reflectance) is defined as albedo in the absence of a direct component when the diffuse component is isotropic. Details regarding methodology are available on the VJ143MA3 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D64 is the BSA for the VIIRS NIR broadband (0.865 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d65&quot;&gt;VJ143D65&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Black-Sky Albedo for ShortWave (VJ143D65) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D54 through VJ143D79 are the albedo products of the VJ143D BRDF/Albedo product suite. Black-sky albedo (BSA) and white-sky albedo (WSA) values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA3.002&quot;&gt;VJ143MA3&lt;/a&gt; product. In addition to the bands included in VJ143MA3, this product suite includes albedo values for the VIIRS Day/Night Band (DNB). The black-sky albedo (directional hemispherical reflectance) is defined as albedo in the absence of a diffuse component and is a function of solar zenith angle. White-sky albedo (bihemispherical reflectance) is defined as albedo in the absence of a direct component when the diffuse component is isotropic. Details regarding methodology are available on the VJ143MA3 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D65 is the BSA for the VIIRS shortwave broadband (1.61 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d41&quot;&gt;VJ143D41&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Local Solar Noon product (VJ143D41) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer for each of the parameters included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA2.002&quot;&gt;VJ143MA2&lt;/a&gt; product. VJ143D40 through VJ143D53 are the 30 arc second BRDF/Albedo Quality values, the Local Solar Noon values, the Valid Observations of the moderate resolution bands (M1 through M5, M7, M8, M10, and M11) plus the Day/Night Band (DNB), the Snow Status, and the Uncertainty. Details regarding methodology are available on the VJ143MA2 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D41 contains the local solar zenith angle at the local solar noon of the representative pixel for the retrieval period. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;. Improvements/Changes from Previous Versions The NOAA-20 VIIRS algorithms include the same improvements as the S-NPP VIIRS V002 * Improved calibration algorithm and better coefficients for entire NOAA-20 mission * Improved geolocation accuracy and updates to fix outliers around maneuver periods and other events * Corrections to the aerosol quantity flag (low, average, high) mainly over brighter surfaces in the mid to high latitudes such as desert and tropical vegetation areas. This has an impact on the retrieval of other downstream data products such as VJ113 Vegetation Indices and VJ143 BRDF/Albedo. * Improved cloud mask input product for corrections along coastlines and artifacts from use of coarse resolution climatology data * Replaced the land/water mask input product with MODIS heritage seven class land/water mask
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143c1&quot;&gt;VJ143C1&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameters Daily Global 0.05 Degree Climate Modeling Grid (CMG) Version 2 product (VJ143C1) is derived from the 30 arc second CMG VJ143D Version 2 product suite. VJ143C1 is generated daily from all available high-quality reflectance data over a 16-day moving window emphasizing the ninth day of the retrieval period, which is reflected in the Julian date in the filename. VJ143C1 supplies the weighting parameters associated with the RossThick/Li-Sparse-Reciprocal BRDF model that best describes the anisotropy of each pixel, which is used to produce the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143C3.002&quot;&gt;VJ143C3&lt;/a&gt; Albedo and &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143C4.002&quot;&gt;VJ143C4&lt;/a&gt; Nadir BRDF-Adjusted Reflectance (NBAR) products. The highest quality full inversion values are used for the temporal fitting effort and supplemented with lower quality pixels, spatial fitting, and spatial smoothing as needed. The status of each pixel can be found in the ancillary layers. Users are encouraged to assess the quality information before using the BRDF/Albedo data. This 0.05 degree (5,600 meters at the equator) CMG product covers the entire globe for use in climate simulation models. The VJ143C1 product includes 39 layers containing the three parameters (fiso, fvol, and fgeo) for the VIIRS Day/Night band (DNB), moderate resolution bands M1 through M5, M7, M8, M10, and M11, as well as the shortwave band, visible band, and near-infrared (NIR) broadbands. Along with the parameter data for the 13 bands are five ancillary layers for uncertainty, quality, local solar noon, percent finer resolution inputs, and snow cover. A low-resolution browse is also provided showing BRDF/Albedo parameters for bands M5, M4, and M3 as a red, green, blue (RGB) image in JPEG format. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143ma1&quot;&gt;VJ143MA1&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameters (VJ143MA1) Version 2 product provides BRDF/Albedo model parameters at 1 kilometer (km) resolution. The VJ143MA1 product is produced daily using 16-day VIIRS data and is weighted temporally to the 9th day, which is reflected in the file name. The VJ143 data products are designed to promote the continuity of NASA’s Moderate Resolution Imaging Spectroradiometer (MODIS) BRDF/Albedo data product suite. The VJ143 algorithm uses the RossThick/Li-Sparse-Reciprocal (RTLSR) semi-empirical kernel-driven BRDF model, with the three kernel weights from VJ143MA1 to reconstruct surface anisotropic effects, correcting the directional reflectance to a common view geometry (&lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA4.002&quot;&gt;VJ143MA4&lt;/a&gt;), while also computing integrated black-sky albedo (BSA) at local solar noon and white-sky albedo (WSA) (&lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA3.002&quot;&gt;VJ143MA3&lt;/a&gt;). Researchers can use the BRDF model parameters with a simple polynomial, to obtain black-sky albedo at any solar illumination angle. Likewise, both the BSA and WSA Science Dataset (SDS) layers can be used with a simple polynomial, to manually estimate instantaneous actual albedo (blue-sky albedo). Additional details regarding the methodology are available in the Algorithm Theoretical Basis Document (ATBD). The VJ143MA1 data product provides a total of 24 SDS layers including: mandatory quality bands and three multi-dimensional model parameter bands representing fiso, fvol, and fgeo for VIIRS moderate resolution bands M1-M5, M7-M8, and M10-M11. A low-resolution browse is also provided showing BRDF/Albedo parameters for bands M5, M7, and M5 as an RGB image in JPEG format. Known Issues: Known issues for VIIRS BRDF/Albedo data products can be found on the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143ia1&quot;&gt;VJ143IA1&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameters (VJ143IA1) Version 2 product provides kernel weights (parameters) at 500 meter (m) resolution. The VJ143IA1 product is produced daily using 16 days of VIIRS data, temporally weighted to the ninth day, which is reflected in the file name. The VJ143IA1 product provides three spectrally dependent kernel weights, also known as model parameters: isotropic (fiso), volumetric (fvol), and geometric (fgeo), which can be used to model anisotropic effects of the Earth’s surface. All VJ143 data products are designed to promote the continuity of NASA’s Moderate Resolution Imaging Spectroradiometer (MODIS) BRDF/Albedo data product suite. The VJ143 algorithm uses the RossThick/Li-Sparse-Reciprocal (RTLSR) semi-empirical kernel-driven BRDF model, with the three kernel weights from VJ143IA1 to reconstruct surface anisotropic effects, correcting the directional reflectance to a common view geometry (&lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143IA4.002&quot;&gt;VJ143IA4&lt;/a&gt;), while also computing integrated black-sky albedo (BSA) at local solar noon and white-sky albedo (WSA) (&lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143IA3.002&quot;&gt;VJ143IA3&lt;/a&gt;). Researchers can use the BRDF model parameters with a simple polynomial, to obtain black-sky albedo at any solar illumination angle. Likewise, both the BSA and WSA Science Dataset (SDS) layers can be used with a simple polynomial, to manually estimate instantaneous actual albedo (blue-sky albedo). Additional details regarding the methodology are available in the Algorithm Theoretical Basis Document (ATBD). The VNP43IA1 data product provides a total of six SDS layers including: three mandatory quality layers for bands I1, I2, and I3 and three multi-dimensional model parameter bands representing fiso, fvol, and fgeo for each imagery band. Each data product file is provided in HDF-EOS5 format. A low-resolution browse is also available showing BRDF/Albedo parameters for VIIRS imagery bands: I1, I2, and I1 as an RGB (red, green, blue) image in JPEG format. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143ma4&quot;&gt;VJ143MA4&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Nadir Bidirectional Reflectance Distribution Function (BRDF) Adjusted Reflectance (NBAR) Version 2 product provides NBAR estimates at 1 kilometer (km) resolution. The VJ143MA4 product is produced daily using 16-day VIIRS data and is weighted temporally to the 9th day, which is reflected in the file name. The view angle effects are removed from the directional reflectances resulting in a stable and consistent NBAR product. The VJ143 data products are designed after the Moderate Resolution Imaging Spectroradiometer (MODIS) BRDF/Albedo product suite to promote the continuity of the Earth Observation System (EOS) mission. The VJ143 data products are designed to promote the continuity of NASA’s Moderate Resolution Imaging Spectroradiometer (MODIS) BRDF/Albedo data product suite. The VJ143 algorithm uses the RossThick/Li-Sparse-Reciprocal (RTLSR) semi-empirical kernel-driven BRDF model, with the three kernel weights from &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; to reconstruct surface anisotropic effects, correcting the directional reflectance to a common view geometry (VJ143MA4), while also computing integrated black-sky albedo (BSA) at local solar noon and white-sky albedo (WSA) (&lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA3.002&quot;&gt;VJ143MA3&lt;/a&gt;). Researchers can use the BRDF model parameters with a simple polynomial, to obtain black-sky albedo at any solar illumination angle. Likewise, both the BSA and WSA Science Dataset (SDS) layers can be used with a simple polynomial, to manually estimate instantaneous actual albedo (blue-sky albedo). Additional details regarding the methodology are available in the Algorithm Theoretical Basis Document (ATBD). The VJ143MA4 product includes 18 SDS layers for BRDF/Albedo mandatory quality and nadir reflectance for VIIRS nine moderate bands M1-M5, M7-M8, and M10-M11. A low-resolution browse image is also available showing NBAR bands M5, M7, and M5 as an RGB image in JPEG format. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143ia4&quot;&gt;VJ143IA4&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Nadir Bidirectional Reflectance Distribution Function (BRDF) Adjusted Reflectance (NBAR) Version 2 product provides NBAR estimates at 500 meter (m) resolution. The VJ143IA4 product is produced daily using 16 days of VIIRS data and is weighted temporally to the ninth day, which is reflected in the file name. The view angle effects are removed from the directional reflectances, resulting in a stable and consistent NBAR product. The VJ143 data products are designed to promote the continuity of NASA’s Moderate Resolution Imaging Spectroradiometer (MODIS) BRDF/Albedo data product suite. The VJ143 algorithm uses the RossThick/Li-Sparse-Reciprocal (RTLSR) semi-empirical kernel-driven BRDF model, with the three kernel weights from &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143IA1.002&quot;&gt;VJ143IA1&lt;/a&gt; to reconstruct surface anisotropic effects, correcting the directional reflectance to a common view geometry (VJ143IA4), while also computing integrated black-sky albedo (BSA) at local solar noon and white-sky albedo (WSA) (&lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143IA3.002&quot;&gt;VJ143IA3&lt;/a&gt;). Researchers can use the BRDF model parameters with a simple polynomial, to obtain black-sky albedo at any solar illumination angle. Likewise, both the BSA and WSA Science Dataset (SDS) layers can be used with a simple polynomial, to manually estimate instantaneous actual albedo (blue-sky albedo). Additional details regarding the methodology are available in the Algorithm Theoretical Basis Document (ATBD). The VJ143IA4 product includes six SDS layers for BRDF/Albedo mandatory quality and nadir reflectance for VIIRS imagery bands I1, I2, and I3. A low-resolution browse image is also available showing NBAR bands I1, I2, and I1 as an RGB (red, green, blue) image in JPEG format. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143c4&quot;&gt;VJ143C4&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Nadir BRDF-Adjusted Reflectance Daily Global 0.05 Degree Climate Modeling Grid (CMG) Version 2 product (VJ143C4) is derived from the 30 arc second CMG VJ143D Version 2 product suite. VJ143C3 is generated daily from all available high-quality reflectance data over a 16-day moving window emphasizing the ninth day of the retrieval period, which is reflected in the Julian date in the filename. The VJ143 algorithm uses the RossThick/Li-Sparse-Reciprocal (RTLSR) semi-empirical kernel-driven BRDF model, with the three kernel weights from &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143C1.002&quot;&gt;VJ143C1&lt;/a&gt; to compute NBAR values for the VIIRS Day/Night band (DNB), and moderate resolution bands M1 through M5, M7, M8, M10, and M11. The algorithm removes view angle effects from directional reflectances to model the values as if they were collected from a nadir view at local solar noon. The quality and inversion status of the majority of the underlying 30 arc second pixels is provided as well as the percentage of the underlying pixels that were present or were snow covered. Users are encouraged to assess the quality information before using the BRDF/Albedo data. This 0.05 degree (5,600 meters at the equator) CMG product covers the entire globe for use in climate simulation models. The VJ143C4 product includes 10 layers containing NBAR values for VIIRS DNB and moderate resolution bands M1 through M5, M7, M8, M10, and M11. Along with the NBAR data for the 10 bands are five ancillary layers for uncertainty, quality, local solar noon, percent finer resolution inputs, and snow cover. A low-resolution browse image is also available showing NBAR bands M5, M4, and M3 as a red, green, blue (RGB) image in JPEG format. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d80&quot;&gt;VJ143D80&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Nadir BRDF-Adjusted Reflectance (NBAR) for Band M1 (VJ143D80) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D80 through VJ143D89 are the NBAR products of the VJ143D BRDF/Albedo product suite. NBAR values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA4.002&quot;&gt;VJ143MA4&lt;/a&gt; product. In addition to the bands included in VJ143MA4, this product suite includes NBAR values for the VIIRS Day/Night Band (DNB). The NBAR algorithm removes view angle effects from directional reflectances to model the values as if they were collected from a nadir view at local solar noon. Details regarding methodology are available on the VJ143MA4 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D80 is the NBAR for VIIRS band M1 (0.412 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d87&quot;&gt;VJ143D87&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Nadir BRDF-Adjusted Reflectance (NBAR) for Band M10 (VJ143D87) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D80 through VJ143D89 are the NBAR products of the VJ143D BRDF/Albedo product suite. NBAR values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA4.002&quot;&gt;VJ143MA4&lt;/a&gt; product. In addition to the bands included in VJ143MA4, this product suite includes NBAR values for the VIIRS Day/Night Band (DNB). The NBAR algorithm removes view angle effects from directional reflectances to model the values as if they were collected from a nadir view at local solar noon. Details regarding methodology are available on the VJ143MA4 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D87 is the NBAR for VIIRS band M10 (1.61 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d88&quot;&gt;VJ143D88&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Nadir BRDF-Adjusted Reflectance (NBAR) for Band M11 (VJ143D88) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D80 through VJ143D89 are the NBAR products of the VJ143D BRDF/Albedo product suite. NBAR values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA4.002&quot;&gt;VJ143MA4&lt;/a&gt; product. In addition to the bands included in VJ143MA4, this product suite includes NBAR values for the VIIRS Day/Night Band (DNB). The NBAR algorithm removes view angle effects from directional reflectances to model the values as if they were collected from a nadir view at local solar noon. Details regarding methodology are available on the VJ143MA4 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D88 is the NBAR for VIIRS band M11 (2.25 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d81&quot;&gt;VJ143D81&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Nadir BRDF-Adjusted Reflectance (NBAR) for Band M2 (VJ143D81) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D80 through VJ143D89 are the NBAR products of the VJ143D BRDF/Albedo product suite. NBAR values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA4.002&quot;&gt;VJ143MA4&lt;/a&gt; product. In addition to the bands included in VJ143MA4, this product suite includes NBAR values for the VIIRS Day/Night Band (DNB). The NBAR algorithm removes view angle effects from directional reflectances to model the values as if they were collected from a nadir view at local solar noon. Details regarding methodology are available on the VJ143MA4 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D81 is the NBAR for VIIRS band M2 (0.445 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d82&quot;&gt;VJ143D82&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Nadir BRDF-Adjusted Reflectance (NBAR) for Band M3 (VJ143D82) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D80 through VJ143D89 are the NBAR products of the VJ143D BRDF/Albedo product suite. NBAR values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA4.002&quot;&gt;VJ143MA4&lt;/a&gt; product. In addition to the bands included in VJ143MA4, this product suite includes NBAR values for the VIIRS Day/Night Band (DNB). The NBAR algorithm removes view angle effects from directional reflectances to model the values as if they were collected from a nadir view at local solar noon. Details regarding methodology are available on the VJ143MA4 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D82 is the NBAR for VIIRS band M3 (0.488 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d83&quot;&gt;VJ143D83&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Nadir BRDF-Adjusted Reflectance (NBAR) for Band M4 (VJ143D83) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D80 through VJ143D89 are the NBAR products of the VJ143D BRDF/Albedo product suite. NBAR values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA4.002&quot;&gt;VJ143MA4&lt;/a&gt; product. In addition to the bands included in VJ143MA4, this product suite includes NBAR values for the VIIRS Day/Night Band (DNB). The NBAR algorithm removes view angle effects from directional reflectances to model the values as if they were collected from a nadir view at local solar noon. Details regarding methodology are available on the VJ143MA4 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D83 is the NBAR for VIIRS band M4 (0.555 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d84&quot;&gt;VJ143D84&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Nadir BRDF-Adjusted Reflectance (NBAR) for Band M5 (VJ143D84) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D80 through VJ143D89 are the NBAR products of the VJ143D BRDF/Albedo product suite. NBAR values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA4.002&quot;&gt;VJ143MA4&lt;/a&gt; product. In addition to the bands included in VNP43MA4, this product suite includes NBAR values for the VIIRS Day/Night Band (DNB). The NBAR algorithm removes view angle effects from directional reflectances to model the values as if they were collected from a nadir view at local solar noon. Details regarding methodology are available on the VJ143MA4 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D84 is the NBAR for VIIRS band M5 (0.672 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d85&quot;&gt;VJ143D85&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Nadir BRDF-Adjusted Reflectance (NBAR) for Band M7 (VJ143D85) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D80 through VJ143D89 are the NBAR products of the VJ143D BRDF/Albedo product suite. NBAR values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA4.002&quot;&gt;VJ143MA4&lt;/a&gt; product. In addition to the bands included in VJ143MA4, this product suite includes NBAR values for the VIIRS Day/Night Band (DNB). The NBAR algorithm removes view angle effects from directional reflectances to model the values as if they were collected from a nadir view at local solar noon. Details regarding methodology are available on the VJ143MA4 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D85 is the NBAR for VIIRS band M7 (0.865 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d86&quot;&gt;VJ143D86&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Nadir BRDF-Adjusted Reflectance (NBAR) for Band M8 (VJ143D86) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D80 through VJ143D89 are the NBAR products of the VJ143D BRDF/Albedo product suite. NBAR values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA4.002&quot;&gt;VJ143MA4&lt;/a&gt; product. In addition to the bands included in VJ143MA4, this product suite includes NBAR values for the VIIRS Day/Night Band (DNB). The NBAR algorithm removes view angle effects from directional reflectances to model the values as if they were collected from a nadir view at local solar noon. Details regarding methodology are available on the VJ143MA4 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D86 is the NBAR for VIIRS band M8 (1.240 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d89&quot;&gt;VJ143D89&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Nadir BRDF-Adjusted Reflectance (NBAR) for DNB (VJ143D89) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D80 through VJ143D89 are the NBAR products of the VJ143D BRDF/Albedo product suite. NBAR values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA4.002&quot;&gt;VJ143MA4&lt;/a&gt; product. In addition to the bands included in VJ143MA4, this product suite includes NBAR values for the VIIRS Day/Night Band (DNB). The NBAR algorithm removes view angle effects from directional reflectances to model the values as if they were collected from a nadir view at local solar noon. Details regarding methodology are available on the VJ143MA4 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D89 is the NBAR for VIIRS DNB (0.7 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d01&quot;&gt;VJ143D01&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 1 Band M1 product (VJ143D01) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D01 is the BRDF isotropic parameter for VIIRS band M1 (0.412 μm). The isotropic parameter, in conjunction with the volumetric and geometric parameters, is used to derive the BRDF/Albedo values for VIIRS band M1. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d22&quot;&gt;VJ143D22&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 1 Band M10 product (VJ143D22) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D22 is the BRDF isotropic parameter for VIIRS band M10 (1.61 μm). The isotropic parameter, in conjunction with the volumetric and geometric parameters, is used to derive the BRDF/Albedo values for VIIRS band M10. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d25&quot;&gt;VJ143D25&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 1 Band M11 product (VJ143D25) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D25 is the BRDF isotropic parameter for VIIRS band M11 (2.25 μm). The isotropic parameter, in conjunction with the volumetric and geometric parameters, is used to derive the BRDF/Albedo values for VIIRS band M11. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;. Improvements/Changes from Previous Versions The NOAA-20 VIIRS algorithms include the same improvements as the S-NPP VIIRS V002 * Improved calibration algorithm and better coefficients for entire NOAA-20 mission * Improved geolocation accuracy and updates to fix outliers around maneuver periods and other events * Corrections to the aerosol quantity flag (low, average, high) mainly over brighter surfaces in the mid to high latitudes such as desert and tropical vegetation areas. This has an impact on the retrieval of other downstream data products such as VJ113 Vegetation Indices and VJ143 BRDF/Albedo. * Improved cloud mask input product for corrections along coastlines and artifacts from use of coarse resolution climatology data * Replaced the land/water mask input product with MODIS heritage seven class land/water mask
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d04&quot;&gt;VJ143D04&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 1 Band M2 product (VJ143D04) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D04 is the BRDF isotropic parameter for VIIRS band M2 (0.445 μm). The isotropic parameter, in conjunction with the volumetric and geometric parameters, is used to derive the BRDF/Albedo values for VIIRS band M2. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d07&quot;&gt;VJ143D07&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 1 Band M3 product (VJ143D07) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D07 is the BRDF isotropic parameter for VIIRS band M3 (0.488 μm). The isotropic parameter, in conjunction with the volumetric and geometric parameters, is used to derive the BRDF/Albedo values for VIIRS band M3. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d10&quot;&gt;VJ143D10&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 1 Band M4 product (VJ143D10) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D10 is the BRDF isotropic parameter for VIIRS band M4 (0.555 μm). The isotropic parameter, in conjunction with the volumetric and geometric parameters, is used to derive the BRDF/Albedo values for VIIRS band M4. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d13&quot;&gt;VJ143D13&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 1 Band M5 product (VJ143D13) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D13 is the BRDF isotropic parameter for VIIRS band M5 (0.672 μm). The isotropic parameter, in conjunction with the volumetric and geometric parameters, is used to derive the BRDF/Albedo values for VIIRS band M5. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d16&quot;&gt;VJ143D16&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 1 Band M7 product (VJ143D16) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D16 is the BRDF isotropic parameter for VIIRS band M7 (0.865 μm). The isotropic parameter, in conjunction with the volumetric and geometric parameters, is used to derive the BRDF/Albedo values for VIIRS band M7. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d19&quot;&gt;VJ143D19&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 1 Band M8 product (VJ143D19) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D19 is the BRDF isotropic parameter for VIIRS band M8 (1.240 μm). The isotropic parameter, in conjunction with the volumetric and geometric parameters, is used to derive the BRDF/Albedo values for VIIRS band M8. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d37&quot;&gt;VJ143D37&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 1 Day/Night Band (DNB) product (VJ143D37) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D37 is the BRDF isotropic parameter for the VIIRS DNB (0.7 μm). The isotropic parameter, in conjunction with the volumetric and geometric parameters, is used to derive the BRDF/Albedo values for the VIIRS DNB. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d31&quot;&gt;VJ143D31&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 1 NIR product (VJ143D31) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D31 is the BRDF isotropic parameter for the VIIRS NIR broadband (0.865 μm). The isotropic parameter, in conjunction with the volumetric and geometric parameters, is used to derive the BRDF/Albedo values for the VIIRS NIR broadband. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d34&quot;&gt;VJ143D34&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 1 Shortwave product (VJ143D34) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D34 is the BRDF isotropic parameter for the VIIRS shortwave broadband (1.61 μm). The isotropic parameter, in conjunction with the volumetric and geometric parameters, is used to derive the BRDF/Albedo values for the VIIRS shortwave broadband. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d28&quot;&gt;VJ143D28&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 1 VIS product (VJ143D28) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible (VIS), near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D28 is the BRDF isotropic parameter for the VIIRS visible broadband (0.64 μm). The isotropic parameter, in conjunction with the volumetric and geometric parameters, is used to derive the BRDF/Albedo values for the VIIRS visible broadband. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d02&quot;&gt;VJ143D02&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 2 Band M1 product (VJ143D02) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D02 is the BRDF volumetric parameter for VIIRS band M1 (0.412 μm). The volumetric parameter, in conjunction with the isotropic and geometric parameters, is used to derive the BRDF/Albedo values for VIIRS band M1. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d23&quot;&gt;VJ143D23&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 2 Band M10 product (VJ143D23) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D23 is the BRDF volumetric parameter for VIIRS band M10 (1.61 μm). The volumetric parameter, in conjunction with the isotropic and geometric parameters, is used to derive the BRDF/Albedo values for VIIRS band M10. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d26&quot;&gt;VJ143D26&lt;/h4&gt;
The NOAA-20 Suomi National Polar-orbiting Partnership (Suomi NPP) Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 2 Band M11 product (VJ143D26) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document [ATBD). VJ143D26 is the BRDF volumetric parameter for VIIRS band M11 (2.25 μm). The volumetric parameter, in conjunction with the isotropic and geometric parameters, is used to derive the BRDF/Albedo values for VIIRS band M11. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d05&quot;&gt;VJ143D05&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 2 Band M2 product (VJ143D05) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D05 is the BRDF volumetric parameter for VIIRS band M2 (0.445 μm). The volumetric parameter, in conjunction with the isotropic and geometric parameters, is used to derive the BRDF/Albedo values for VIIRS band M2. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d08&quot;&gt;VJ143D08&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 2 Band M3 product (VJ143D08) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document [ATBD). VJ143D08 is the BRDF volumetric parameter for VIIRS band M3 (0.488 μm). The volumetric parameter, in conjunction with the isotropic and geometric parameters, is used to derive the BRDF/Albedo values for VIIRS band M3. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d11&quot;&gt;VJ143D11&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 2 Band M4 product (VJ143D11) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D11 is the BRDF volumetric parameter for VIIRS band M4 (0.555 μm). The volumetric parameter, in conjunction with the isotropic and geometric parameters, is used to derive the BRDF/Albedo values for VIIRS band M4. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d14&quot;&gt;VJ143D14&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 2 Band M5 product (VJ143D14) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D14 is the BRDF volumetric parameter for VIIRS band M5 (0.672 μm). The volumetric parameter, in conjunction with the isotropic and geometric parameters, is used to derive the BRDF/Albedo values for VIIRS band M5. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d17&quot;&gt;VJ143D17&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 2 Band M7 product (VJ143D17) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D17 is the BRDF volumetric parameter for VIIRS band M7 (0.865 μm). The volumetric parameter, in conjunction with the isotropic and geometric parameters, is used to derive the BRDF/Albedo values for VIIRS band M7. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;. Improvements/Changes from Previous Versions The NOAA-20 VIIRS algorithms include the same improvements as the S-NPP VIIRS V002 * Improved calibration algorithm and better coefficients for entire NOAA-20 mission * Improved geolocation accuracy and updates to fix outliers around maneuver periods and other events * Corrections to the aerosol quantity flag (low, average, high) mainly over brighter surfaces in the mid to high latitudes such as desert and tropical vegetation areas. This has an impact on the retrieval of other downstream data products such as VJ113 Vegetation Indices and VJ143 BRDF/Albedo. * Improved cloud mask input product for corrections along coastlines and artifacts from use of coarse resolution climatology data * Replaced the land/water mask input product with MODIS heritage seven class land/water mask
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d20&quot;&gt;VJ143D20&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 2 Band M8 product (VJ143D20) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D20 is the BRDF volumetric parameter for VIIRS band M8 (1.240 μm). The volumetric parameter, in conjunction with the isotropic and geometric parameters, is used to derive the BRDF/Albedo values for VIIRS band M8. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d38&quot;&gt;VJ143D38&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 2 Day/Night Band (DNB) product (VJ143D38) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D38 is the BRDF volumetric parameter for the VIIRS DNB (0.7 μm). The volumetric parameter, in conjunction with the isotropic and geometric parameters, is used to derive the BRDF/Albedo values for the VIIRS DNB. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d32&quot;&gt;VJ143D32&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 2 NIR product (VJ143D32) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D32 is the BRDF volumetric parameter for the VIIRS NIR broadband (0.865 μm). The volumetric parameter, in conjunction with the isotropic and geometric parameters, is used to derive the BRDF/Albedo values for the VIIRS NIR broadband. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d35&quot;&gt;VJ143D35&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 2 Shortwave product (VJ143D35) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D35 is the BRDF volumetric parameter for VIIRS shortwave broadband (1.61 μm). The volumetric parameter, in conjunction with the isotropic and geometric parameters, is used to derive the BRDF/Albedo values for the VIIRS shortwave broadband. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d29&quot;&gt;VJ143D29&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 2 VIS product (VJ143D29) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible (VIS), near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D29 is the BRDF volumetric parameter for the VIIRS visible broadband (0.64 μm). The volumetric parameter, in conjunction with the isotropic and geometric parameters, is used to derive the BRDF/Albedo values for the VIIRS visible broadband. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d03&quot;&gt;VJ143D03&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 3 Band M1 product (VJ143D03) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D03 is the BRDF geometric parameter for VIIRS band M1 (0.412 μm). The geometric parameter, in conjunction with the isotropic and volumetric parameters, is used to derive the BRDF/Albedo values for VIIRS band M1. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d24&quot;&gt;VJ143D24&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 3 Band M10 product (VJ143D24) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D24 is the BRDF geometric parameter for VIIRS band M10 (1.61 μm). The geometric parameter, in conjunction with the isotropic and volumetric parameters, is used to derive the BRDF/Albedo values for VIIRS band M10. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d27&quot;&gt;VJ143D27&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 3 Band M11 product (VJ143D27) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D27 is the BRDF geometric parameter for VIIRS band M11 (2.25 μm). The geometric parameter, in conjunction with the isotropic and volumetric parameters, is used to derive the BRDF/Albedo values for VIIRS band M11. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d06&quot;&gt;VJ143D06&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 3 Band M2 product (VJ143D06) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D06 is the BRDF geometric parameter for VIIRS band M2 (0.445 μm). The geometric parameter, in conjunction with the isotropic and volumetric parameters, is used to derive the BRDF/Albedo values for VIIRS band M2. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d09&quot;&gt;VJ143D09&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 3 Band M3 product (VJ143D09) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D09 is the BRDF geometric parameter for VIIRS band M3 (0.488 μm). The geometric parameter, in conjunction with the isotropic and volumetric parameters, is used to derive the BRDF/Albedo values for VIIRS band M3. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d12&quot;&gt;VJ143D12&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 3 Band M4 product (VJ143D12) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D12 is the BRDF geometric parameter for VIIRS band M4 (0.555 μm). The geometric parameter, in conjunction with the isotropic and volumetric parameters, is used to derive the BRDF/Albedo values for VIIRS band M4. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d15&quot;&gt;VJ143D15&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 3 Band M5 product (VJ143D15) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D15 is the BRDF geometric parameter for VIIRS band M5 (0.672 μm). The geometric parameter, in conjunction with the isotropic and volumetric parameters, is used to derive the BRDF/Albedo values for VIIRS band M5. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d18&quot;&gt;VJ143D18&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 3 Band M7 product (VJ143D18) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D18 is the BRDF geometric parameter for VIIRS band M7 (0.865 μm). The geometric parameter, in conjunction with the isotropic and volumetric parameters, is used to derive the BRDF/Albedo values for VIIRS band M7. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d21&quot;&gt;VJ143D21&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 3 Band M8 product (VJ143D21) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D21 is the BRDF geometric parameter for VIIRS band M8 (1.240 μm). The geometric parameter, in conjunction with the isotropic and volumetric parameters, is used to derive the BRDF/Albedo values for VIIRS band M8. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d39&quot;&gt;VJ143D39&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 3 Day-Night Band (DNB) product (VJ143D39) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D39 is the BRDF geometric parameter for the VIIRS DNB (0.7 μm). The geometric parameter, in conjunction with the isotropic and volumetric parameters, is used to derive the BRDF/Albedo values for the VIIRS DNB. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d33&quot;&gt;VJ143D33&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 3 NIR product (VJ143D33) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D33 is the BRDF geometric parameter for the VIIRS NIR broadband (0.865 μm). The geometric parameter, in conjunction with the isotropic and volumetric parameters, is used to derive the BRDF/Albedo values for the VIIRS NIR broadband. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d36&quot;&gt;VJ143D36&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 3 Shortwave product (VJ143D36) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D36 is the BRDF geometric parameter for VIIRS shortwave broadband (1.61 μm). The geometric parameter, in conjunction with the isotropic and volumetric parameters, is used to derive the BRDF/Albedo values for the VIIRS shortwave broadband. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d30&quot;&gt;VJ143D30&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 3 VIS product (VJ143D30) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the nine VIIRS moderate resolution bands along with the visible (VIS), near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; product is stored in a separate file as VJ143D01 through VJ143D36. In addition to the bands included in VJ143MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VJ143D37 through VJ143D39. Details regarding methodology are available on the VJ143MA1 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D30 is the BRDF geometric parameter for the VIIRS visible broadband (0.64 μm). The geometric parameter, in conjunction with the isotropic and volumetric parameters, is used to derive the BRDF/Albedo values for the VIIRS visible broadband. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143ma2&quot;&gt;VJ143MA2&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Quality (VJ143MA2) Version 2 product provides BRDF and Albedo quality at 1 kilometer (km) resolution. The VJ143MA2 product is produced daily using 16 days of VIIRS data and is weighted temporally to the ninth day, which is reflected in the file name. The VJ143MA2 product gives information regarding band quality and days of valid observation within a 16-day period for nine VIIRS moderate resolution bands and three broadbands. The VJ143 data products are designed to promote the continuity of NASA’s Moderate Resolution Imaging Spectroradiometer (MODIS) BRDF/Albedo data product suite. The VJ143 algorithm uses the RossThick/Li-Sparse-Reciprocal (RTLSR) semi-empirical kernel-driven BRDF model, with the three kernel weights from &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA1.002&quot;&gt;VJ143MA1&lt;/a&gt; to reconstruct surface anisotropic effects, correcting the directional reflectance to a common view geometry (&lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA4.002&quot;&gt;VJ143MA4&lt;/a&gt;), while also computing integrated black-sky albedo (BSA) at local solar noon and white-sky albedo (WSA) (&lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA3.002&quot;&gt;VJ143MA3&lt;/a&gt;). Researchers can use the BRDF model parameters with a simple polynomial, to obtain black-sky albedo at any solar illumination angle. Likewise, both the BSA and WSA Science Dataset (SDS) layers can be used with a simple polynomial, to manually estimate instantaneous actual albedo (blue-sky albedo). Additional details regarding the methodology are available in the Algorithm Theoretical Basis Document (ATBD). The VNP43MA2 data product provides a total of 23 SDS layers including: BRDF/Albedo band quality and days of valid observation within a 16-day period for VIIRS moderate resolution bands M1-M5, M7-M8, and M10-M11; as well as land water type class flag; snow BRDF albedo class flag; local solar noon; albedo uncertainty and the platform name. Known Issues: Known issues for VIIRS BRDF/Albedo data products can be found on the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d40&quot;&gt;VJ143D40&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Quality product (VJ143D40) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer for each of the parameters included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA2.002&quot;&gt;VJ143MA2&lt;/a&gt; product. VJ143D40 through VJ143D53 are the 30 arc second BRDF/Albedo Quality values, the Local Solar Noon values, the Valid Observations of the moderate resolution bands (M1 through M5, M7, M8, M10, and M11) plus the Day/Night Band (DNB), the Snow Status, and the Uncertainty. Details regarding methodology are available on the VJ143MA2 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D40 consists of BRDF/Albedo quality information representing the overall quality of each pixel for VIIRS moderate resolution bands M1 through M5, M7, M8, M10, M11, and DNB. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143ia2&quot;&gt;VJ143IA2&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Quality (VJ143IA2) Version 2 product provides BRDF and Albedo quality at 500 meter (m) resolution. The VJ143IA2 product is produced daily using 16 days of VIIRS data and is weighted temporally to the ninth day, which is reflected in the file name. The VJ143IA2 product provides information regarding band quality and days of valid observation within a 16-day period for the VIIRS imagery bands. The VJ143 data products are designed to promote the continuity of NASA’s Moderate Resolution Imaging Spectroradiometer (MODIS) BRDF/Albedo data product suite. The VJ143 algorithm uses the RossThick/Li-Sparse-Reciprocal (RTLSR) semi-empirical kernel-driven BRDF model, with the three kernel weights from &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143IA1.002&quot;&gt;VJ143IA1&lt;/a&gt; to reconstruct surface anisotropic effects, correcting the directional reflectance to a common view geometry (&lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143IA4.002&quot;&gt;VJ143IA4&lt;/a&gt;), while also computing integrated black-sky albedo (BSA) at local solar noon and white-sky albedo (WSA) (&lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143IA3.002&quot;&gt;VJ143IA3&lt;/a&gt;). Researchers can use the BRDF model parameters with a simple polynomial, to obtain black-sky albedo at any solar illumination angle. Likewise, both the BSA and WSA Science Dataset (SDS) layers can be used with a simple polynomial, to manually estimate instantaneous actual albedo (blue-sky albedo). Additional details regarding the methodology are available in the Algorithm Theoretical Basis Document (ATBD). The VJ143IA2 data product provides a total of 11 SDS layers including: BRDF/Albedo band quality (inversion information) and days of valid observation within a 16-day period for VIIRS imagery bands I1, I2, and I3, as well as land water type class flag, snow BRDF albedo class flag, local solar noon, albedo uncertainty and the platform name. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d52&quot;&gt;VJ143D52&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Snow Status product (VJ143D52) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer for each of the parameters included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA2.002&quot;&gt;VJ143MA2&lt;/a&gt; product. VJ143D40 through VJ143D53 are the 30 arc second BRDF/Albedo Quality values, the Local Solar Noon values, the Valid Observations of the moderate resolution bands (M1 through M5, M7, M8, M10, and M11) plus the Day/Night Band (DNB), the Snow Status, and the Uncertainty. Details regarding methodology are available on the VJ143MA2 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D52 contains the snow status quality layer, which identifies each pixel as either “Snow-free Albedo Retrieved” or “Snow Albedo Retrieved” for the acquisition period. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143c2&quot;&gt;VJ143C2&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Snow-free Model Parameters Daily Global 0.05 Degree Climate Modeling Grid (CMG) Version 2 product (VJ143C2) is derived from the 30 arc second CMG VJ143D Version 2 product suite. VJ143C2 is generated daily from all available snow-free acquisitions over a 16-day moving window emphasizing the ninth day of the retrieval period, which is reflected in the Julian date in the filename. VJ143C2 supplies the weighting parameters associated with the RossThick/Li-Sparse-Reciprocal BRDF model, which is used to produce the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143C3.002&quot;&gt;VJ143C3&lt;/a&gt; Albedo and &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143C4.002&quot;&gt;VJ143C4&lt;/a&gt; Nadir BRDF-Adjusted Reflectance (NBAR) products. The highest quality full inversion values are used for the temporal fitting effort and supplemented with lower quality pixels, spatial fitting, and spatial smoothing as needed. The status of each pixel can be found in the ancillary layers. Users are encouraged to assess the quality information before using the BRDF/Albedo data. This 0.05 degree (5,600 meters at the equator) CMG product covers the entire globe for use in climate simulation models. The VJ143C2 product includes 39 layers containing the three parameters (fiso, fvol, and fgeo) for the VIIRS Day/Night band (DNB), moderate resolution bands M1 through M5, M7, M8, M10, and M11, as well as the shortwave band, visible band, and near-infrared (NIR) broadbands. Along with the parameter data for the 13 bands are four ancillary layers for uncertainty, quality, local solar noon, and percent finer resolution inputs. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d53&quot;&gt;VJ143D53&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Uncertainty product (VJ143D53) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer for each of the parameters included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA2.002&quot;&gt;VJ143MA2&lt;/a&gt; product. VJ143D40 through VJ143D53 are the 30 arc second BRDF/Albedo Quality values, the Local Solar Noon values, the Valid Observations of the moderate resolution bands (M1 through M5, M7, M8, M10, and M11) plus the Day/Night Band (DNB), the Snow Status, and the Uncertainty. Details regarding methodology are available on the VJ143MA2 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D53 contains the uncertainty range of each BRDF/Albedo pixel for the retrieval period. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d42&quot;&gt;VJ143D42&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Valid Observation Band M1 product (VJ143D42) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer for each of the parameters included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA2.002&quot;&gt;VJ143MA2&lt;/a&gt; product. VJ143D40 through VJ143D53 are the 30 arc second BRDF/Albedo Quality values, the Local Solar Noon values, the Valid Observations of the moderate resolution bands (M1 through M5, M7, M8, M10, and M11) plus the Day/Night Band (DNB), the Snow Status, and the Uncertainty. Details regarding methodology are available on the VJ143MA2 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D42 contains the valid observation quality layer representing each of the 16 days of the retrieval period for VIIRS band M1. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d49&quot;&gt;VJ143D49&lt;/h4&gt;
The NOAA-20 Suomi National Polar-orbiting Partnership (Suomi NPP) Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Valid Observation Band M10 product (VJ143D49) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer for each of the parameters included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA2.002&quot;&gt;VJ143MA2&lt;/a&gt; product. VJ143D40 through VJ143D53 are the 30 arc second BRDF/Albedo Quality values, the Local Solar Noon values, the Valid Observations of the moderate resolution bands (M1 through M5, M7, M8, M10, and M11) plus the Day/Night Band (DNB), the Snow Status, and the Uncertainty. Details regarding methodology are available on the VJ143MA2 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D49 contains the valid observation quality layer representing each of the 16 days of the retrieval period for VIIRS band M10. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d50&quot;&gt;VJ143D50&lt;/h4&gt;
The NOAA-20 Suomi National Polar-orbiting Partnership (Suomi NPP) Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Valid Observation Band M11 product (VJ143D50) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer for each of the parameters included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA2.002&quot;&gt;VJ143MA2&lt;/a&gt; product. VJ143D40 through VJ143D53 are the 30 arc second BRDF/Albedo Quality values, the Local Solar Noon values, the Valid Observations of the moderate resolution bands (M1 through M5, M7, M8, M10, and M11) plus the Day/Night Band (DNB), the Snow Status, and the Uncertainty. Details regarding methodology are available on the VJ143MA2 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D50 contains the valid observation quality layer representing each of the 16 days of the retrieval period for VIIRS band M11. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d43&quot;&gt;VJ143D43&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Valid Observation Band M2 product (VJ143D43) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer for each of the parameters included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA2.002&quot;&gt;VJ143MA2&lt;/a&gt; product. VJ143D40 through VJ143D53 are the 30 arc second BRDF/Albedo Quality values, the Local Solar Noon values, the Valid Observations of the moderate resolution bands (M1 through M5, M7, M8, M10, and M11) plus the Day/Night Band (DNB), the Snow Status, and the Uncertainty. Details regarding methodology are available on the VJ143MA2 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D43 contains the valid observation quality layer representing each of the 16 days of the retrieval period for VIIRS band M2. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d44&quot;&gt;VJ143D44&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Valid Observation Band M3 product (VJ143D44) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer for each of the parameters included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA2.002&quot;&gt;VJ143MA2&lt;/a&gt; product. VJ143D40 through VJ143D53 are the 30 arc second BRDF/Albedo Quality values, the Local Solar Noon values, the Valid Observations of the moderate resolution bands (M1 through M5, M7, M8, M10, and M11) plus the Day/Night Band (DNB), the Snow Status, and the Uncertainty. Details regarding methodology are available on the VJ143MA2 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D44 contains the valid observation quality layer representing each of the 16 days of the retrieval period for VIIRS band M3. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d45&quot;&gt;VJ143D45&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Valid Observation Band M4 product (VJ143D45) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer for each of the parameters included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA2.002&quot;&gt;VJ143MA2&lt;/a&gt; product. VJ143D40 through VJ143D53 are the 30 arc second BRDF/Albedo Quality values, the Local Solar Noon values, the Valid Observations of the moderate resolution bands (M1 through M5, M7, M8, M10, and M11) plus the Day/Night Band (DNB), the Snow Status, and the Uncertainty. Details regarding methodology are available on the VJ143MA2 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D45 contains the valid observation quality layer representing each of the 16 days of the retrieval period for VIIRS band M4. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d46&quot;&gt;VJ143D46&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Valid Observation Band M5 product (VJ143D46) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer for each of the parameters included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA2.002&quot;&gt;VJ143MA2&lt;/a&gt; product. VJ143D40 through VJ143D53 are the 30 arc second BRDF/Albedo Quality values, the Local Solar Noon values, the Valid Observations of the moderate resolution bands (M1 through M5, M7, M8, M10, and M11) plus the Day/Night Band (DNB), the Snow Status, and the Uncertainty. Details regarding methodology are available on the VJ143MA2 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D46 contains the valid observation quality layer representing each of the 16 days of the retrieval period for VIIRS band M5. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d47&quot;&gt;VJ143D47&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Valid Observation Band M7 product (VJ143D47) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer for each of the parameters included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA2.002&quot;&gt;VJ143MA2&lt;/a&gt; product. VJ143D40 through VJ143D53 are the 30 arc second BRDF/Albedo Quality values, the Local Solar Noon values, the Valid Observations of the moderate resolution bands (M1 through M5, M7, M8, M10, and M11) plus the Day/Night Band (DNB), the Snow Status, and the Uncertainty. Details regarding methodology are available on the VJ143MA2 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D47 contains the valid observation quality layer representing each of the 16 days of the retrieval period for VIIRS band M7. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d48&quot;&gt;VJ143D48&lt;/h4&gt;
The NOAA-20 Suomi National Polar-orbiting Partnership (Suomi NPP) Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Valid Observation Band M8 product (VJ143D48) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer for each of the parameters included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA2.002&quot;&gt;VJ143MA2&lt;/a&gt; product. VJ143D40 through VJ143D53 are the 30 arc second BRDF/Albedo Quality values, the Local Solar Noon values, the Valid Observations of the moderate resolution bands (M1 through M5, M7, M8, M10, and M11) plus the Day/Night Band (DNB), the Snow Status, and the Uncertainty. Details regarding methodology are available on the VJ143MA2 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D48 contains the valid observation quality layer representing each of the 16 days of the retrieval period for VIIRS band M8. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d51&quot;&gt;VJ143D51&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Valid Observation Day/Night Band (DNB) product (VJ143D51) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer for each of the parameters included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA2.002&quot;&gt;VJ143MA2&lt;/a&gt; product. VJ143D40 through VJ143D53 are the 30 arc second BRDF/Albedo Quality values, the Local Solar Noon values, the Valid Observations of the moderate resolution bands (M1 through M5, M7, M8, M10, and M11) plus the Day/Night Band (DNB), the Snow Status, and the Uncertainty. Details regarding methodology are available on the VJ143MA2 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D51 contains the valid observation quality layer representing each of the 16 days of the retrieval period for VIIRS DNB. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d67&quot;&gt;VJ143D67&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo white-sky albedo for band M1 (VJ143D67) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D54 through VJ143D79 are the albedo products of the VJ143D BRDF/Albedo product suite. Black-sky albedo (BSA) and white-sky albedo (WSA) values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA3.002&quot;&gt;VJ143MA3&lt;/a&gt; product. In addition to the bands included in VJ143MA3, this product suite includes albedo values for the VIIRS Day/Night Band (DNB). The black-sky albedo (directional hemispherical reflectance) is defined as albedo in the absence of a diffuse component and is a function of solar zenith angle. White-sky albedo (bihemispherical reflectance) is defined as albedo in the absence of a direct component when the diffuse component is isotropic. Details regarding methodology are available on the VJ143MA3 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D67 is the WSA for VIIRS band M1 (0.412 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d74&quot;&gt;VJ143D74&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo white-sky albedo for band M10 (VJ143D74) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D54 through VJ143D79 are the albedo products of the VJ143D BRDF/Albedo product suite. Black-sky albedo (BSA) and white-sky albedo (WSA) values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA3.002&quot;&gt;VJ143MA3&lt;/a&gt; product. In addition to the bands included in VJ143MA3, this product suite includes albedo values for the VIIRS Day/Night Band (DNB). The black-sky albedo (directional hemispherical reflectance) is defined as albedo in the absence of a diffuse component and is a function of solar zenith angle. White-sky albedo (bihemispherical reflectance) is defined as albedo in the absence of a direct component when the diffuse component is isotropic. Details regarding methodology are available on the VJ143MA3 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D74 is the WSA for VIIRS band M10 (1.61 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d75&quot;&gt;VJ143D75&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo white-sky albedo for band M11 (VJ143D75) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D54 through VJ143D79 are the albedo products of the VJ143D BRDF/Albedo product suite. Black-sky albedo (BSA) and white-sky albedo (WSA) values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA3.002&quot;&gt;VJ143MA3&lt;/a&gt; product. In addition to the bands included in VJ143MA3, this product suite includes albedo values for the VIIRS Day/Night Band (DNB). The black-sky albedo (directional hemispherical reflectance) is defined as albedo in the absence of a diffuse component and is a function of solar zenith angle. White-sky albedo (bihemispherical reflectance) is defined as albedo in the absence of a direct component when the diffuse component is isotropic. Details regarding methodology are available on the VJ143MA3 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D75 is the WSA for VIIRS band M11 (2.25 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d68&quot;&gt;VJ143D68&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo white-sky albedo for band M2 (VJ143D68) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D54 through VJ143D79 are the albedo products of the VJ143D BRDF/Albedo product suite. Black-sky albedo (BSA) and white-sky albedo (WSA) values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA3.002&quot;&gt;VJ143MA3&lt;/a&gt; product. In addition to the bands included in VJ143MA3, this product suite includes albedo values for the VIIRS Day/Night Band (DNB). The black-sky albedo (directional hemispherical reflectance) is defined as albedo in the absence of a diffuse component and is a function of solar zenith angle. White-sky albedo (bihemispherical reflectance) is defined as albedo in the absence of a direct component when the diffuse component is isotropic. Details regarding methodology are available on the VJ143MA3 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D68 is the WSA for VIIRS band M2 (0.445 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d69&quot;&gt;VJ143D69&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo white-sky albedo for band M3 (VJ143D69) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D54 through VJ143D79 are the albedo products of the VJ143D BRDF/Albedo product suite. Black-sky albedo (BSA) and white-sky albedo (WSA) values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA3.002&quot;&gt;VJ143MA3&lt;/a&gt; product. In addition to the bands included in VJ143MA3, this product suite includes albedo values for the VIIRS Day/Night Band (DNB). The black-sky albedo (directional hemispherical reflectance) is defined as albedo in the absence of a diffuse component and is a function of solar zenith angle. White-sky albedo (bihemispherical reflectance) is defined as albedo in the absence of a direct component when the diffuse component is isotropic. Details regarding methodology are available on the VJ143MA3 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D69 is the WSA for VIIRS band M3 (0.488 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d70&quot;&gt;VJ143D70&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo white-sky albedo for band M4 (VJ143D70) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D54 through VJ143D79 are the albedo products of the VJ143D BRDF/Albedo product suite. Black-sky albedo (BSA) and white-sky albedo (WSA) values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA3.002&quot;&gt;VJ143MA3&lt;/a&gt; product. In addition to the bands included in VJ143MA3, this product suite includes albedo values for the VIIRS Day/Night Band (DNB). The black-sky albedo (directional hemispherical reflectance) is defined as albedo in the absence of a diffuse component and is a function of solar zenith angle. White-sky albedo (bihemispherical reflectance) is defined as albedo in the absence of a direct component when the diffuse component is isotropic. Details regarding methodology are available on the VJ143MA3 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D70 is the WSA for VIIRS band M4 (0.555 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d71&quot;&gt;VJ143D71&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo white-sky albedo for band M5 (VJ143D71) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D54 through VJ143D79 are the albedo products of the VJ143D BRDF/Albedo product suite. Black-sky albedo (BSA) and white-sky albedo (WSA) values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA3.002&quot;&gt;VJ143MA3&lt;/a&gt; product. In addition to the bands included in VJ143MA3, this product suite includes albedo values for the VIIRS Day/Night Band (DNB). The black-sky albedo (directional hemispherical reflectance) is defined as albedo in the absence of a diffuse component and is a function of solar zenith angle. White-sky albedo (bihemispherical reflectance) is defined as albedo in the absence of a direct component when the diffuse component is isotropic. Details regarding methodology are available on the VJ143MA3 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D71 is the WSA for VIIRS band M5 (0.672 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d72&quot;&gt;VJ143D72&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo white-sky albedo for band M7 (VJ143D72) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D54 through VJ143D79 are the albedo products of the VJ143D BRDF/Albedo product suite. Black-sky albedo (BSA) and white-sky albedo (WSA) values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA3.002&quot;&gt;VJ143MA3&lt;/a&gt; product. In addition to the bands included in VJ143MA3, this product suite includes albedo values for the VIIRS Day/Night Band (DNB). The black-sky albedo (directional hemispherical reflectance) is defined as albedo in the absence of a diffuse component and is a function of solar zenith angle. White-sky albedo (bihemispherical reflectance) is defined as albedo in the absence of a direct component when the diffuse component is isotropic. Details regarding methodology are available on the VJ143MA3 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D72 is the WSA for VIIRS band M7 (0.865 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d73&quot;&gt;VJ143D73&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo white-sky albedo for band M8 (VJ143D73) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D54 through VJ143D79 are the albedo products of the VJ143D BRDF/Albedo product suite. Black-sky albedo (BSA) and white-sky albedo (WSA) values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA3.002&quot;&gt;VJ143MA3&lt;/a&gt; product. In addition to the bands included in VJ143MA3, this product suite includes albedo values for the VIIRS Day/Night Band (DNB). The black-sky albedo (directional hemispherical reflectance) is defined as albedo in the absence of a diffuse component and is a function of solar zenith angle. White-sky albedo (bihemispherical reflectance) is defined as albedo in the absence of a direct component when the diffuse component is isotropic. Details regarding methodology are available on the VJ143MA3 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D73 is the WSA for VIIRS band M8 (1.240 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d76&quot;&gt;VJ143D76&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo white-sky albedo for band VIS (VJ143D76) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D54 through VJ143D79 are the albedo products of the VJ143D BRDF/Albedo product suite. Black-sky albedo (BSA) and white-sky albedo (WSA) values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) along with the visible (VIS), near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA3.002&quot;&gt;VJ143MA3&lt;/a&gt; product. In addition to the bands included in VJ143MA3, this product suite includes albedo values for the VIIRS Day/Night Band (DNB). The black-sky albedo (directional hemispherical reflectance) is defined as albedo in the absence of a diffuse component and is a function of solar zenith angle. White-sky albedo (bihemispherical reflectance) is defined as albedo in the absence of a direct component when the diffuse component is isotropic. Details regarding methodology are available on the VJ143MA3 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D76 is the WSA for the VIIRS visible broadband (0.64 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d79&quot;&gt;VJ143D79&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo white-sky albedo for DNB (VJ143D79) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D54 through VJ143D79 are the albedo products of the VJ143D BRDF/Albedo product suite. Black-sky albedo (BSA) and white-sky albedo (WSA) values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA3.002&quot;&gt;VJ143MA3&lt;/a&gt; product. In addition to the bands included in VJ143MA3, this product suite includes albedo values for the VIIRS Day/Night Band (DNB). The black-sky albedo (directional hemispherical reflectance) is defined as albedo in the absence of a diffuse component and is a function of solar zenith angle. White-sky albedo (bihemispherical reflectance) is defined as albedo in the absence of a direct component when the diffuse component is isotropic. Details regarding methodology are available on the VJ143MA3 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D79 is the WSA for the VIIRS DNB (0.7 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d77&quot;&gt;VJ143D77&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo white-sky albedo for band NIR (VJ143D77) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D54 through VJ143D79 are the albedo products of the VJ143D BRDF/Albedo product suite. Black-sky albedo (BSA) and white-sky albedo (WSA) values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA3.002&quot;&gt;VJ143MA3&lt;/a&gt; product. In addition to the bands included in VJ143MA3, this product suite includes albedo values for the VIIRS Day/Night Band (DNB). The black-sky albedo (directional hemispherical reflectance) is defined as albedo in the absence of a diffuse component and is a function of solar zenith angle. White-sky albedo (bihemispherical reflectance) is defined as albedo in the absence of a direct component when the diffuse component is isotropic. Details regarding methodology are available on the VJ143MA3 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D77 is the WSA for the VIIRS NIR broadband (0.865 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143d78&quot;&gt;VJ143D78&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo white-sky albedo for ShortWave (VJ143D78) is produced daily using 16 days of data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day, which is reflected in the file name. The VJ143D product suite is provided in a Climate Modeling Grid (CMG), which covers the entire globe for use in climate simulation models. Due to the large file size, each VJ143D product contains just one data layer. VJ143D54 through VJ143D79 are the albedo products of the VJ143D BRDF/Albedo product suite. Black-sky albedo (BSA) and white-sky albedo (WSA) values are provided for the nine VIIRS moderate resolution bands (M1 through M5, M7, M8, M10, and M11) along with the visible, near-infrared (NIR), and shortwave bands included in the &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143MA3.002&quot;&gt;VJ143MA3&lt;/a&gt; product. In addition to the bands included in VJ143MA3, this product suite includes albedo values for the VIIRS Day/Night Band (DNB). The black-sky albedo (directional hemispherical reflectance) is defined as albedo in the absence of a diffuse component and is a function of solar zenith angle. White-sky albedo (bihemispherical reflectance) is defined as albedo in the absence of a direct component when the diffuse component is isotropic. Details regarding methodology are available on the VJ143MA3 product page and in the Algorithm Theoretical Basis Document (ATBD). VJ143D78 is the WSA for the VIIRS shortwave broadband (1.61 μm). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj146a1&quot;&gt;VJ146A1&lt;/h4&gt;
The NOAA-20 VIIRS Daily Gridded Day Night Band 15 arc-second Linear Lat Lon Grid Night product, short-name VJ146A1 is a daily, top-of-atmosphere, at-sensor nighttime radiance product. This product is available at 15 arc-second spatial resolution from January 2018 onward. The VJ146A1 product contains 26 Science Data Sets (SDS) that include sensor radiance, zenith and azimuth angles (at-sensor, solar, and lunar), cloud-mask flags, time, shortwave IR radiance, brightness temperatures, VIIRS quality flags, moon phase angle, and moon illumination fraction. It also provides Quality Flag (QF) information specific to the cloud-mask, VIIRS moderate-resolution bands M10, M11, M12, M13, M15, M16, and DNB. The current v2.0 collection contains several changes and differences relative to the previous v1.0 collection. These include radiance data format change from unsigned integer to floating-point, from exclusively for land surfaces coverage to both land and water surfaces, updated Mandatory_Quality_Flag layer, and others. Consult the v2.0-specific Black Marble User Guide for additional details at: &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/data/userguide/BlackMarbleUserGuide_Collection2.0_20241203.pdf&quot;&gt;https://landweb.modaps.eosdis.nasa.gov/data/userguide/BlackMarbleUserGuide_Collection2.0_20241203.pdf&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj102dnb&quot;&gt;VJ102DNB&lt;/h4&gt;
The VIIRS/JPSS1 Day/Night Band 6-Min L1B Swath 750 m, short-name VJ102DNB is platform-derived single NASA VIIRS panchromatic Day-Night band (DNB) calibrated radiance product. The DNB is one of the M-bands with an at-nadir spatial resolution of 750 meters (across the entire scan). The panchromatic DNB’s spectral wavelength ranges from 0.5 µm to 0.9 µm. It facilitates measuring night lights, reflected solar/lunar lights with a large dynamic range between a low of a quarter moon illumination to the brightest daylight. The spatial resolution of the instrument at viewing nadir is approximately 750 m for the DNB and the Moderate-resolution Bands and 375m for the Imagery bands. The DNB is aggregated to maintain nearly constant horizontal spatial resolution across the swath.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj103dnb&quot;&gt;VJ103DNB&lt;/h4&gt;
The VIIRS/JPSS1 Day/Night Band Resolution Terrain Corrected Geolocation 6-Min L1 Swath 750m product contains the derived line-of-sight (LOS) vectors for the single panchromatic Day-Night band (DNB). The geolocation algorithm uses a number of inputs that include an Earth ellipsoid, geoid, and a digital terrain model along with the SNPP platform’s ephemeris and attitude data, and knowledge of the VIIRS sensor and satellite geometry. It provides geodetic coordinates (latitude and longitude), and related parameters for each VIIRS L1 pixel. The VJ103DNB product includes geodetic latitude, longitude, surface height above the geoid, solar zenith and azimuth angles, lunar zenith and azimuth angles, sensor zenith and azimuth angles, land/water mask, moon illumination fraction and phase angle, and quality flag for every pixel location.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143dnba3&quot;&gt;VJ143DNBA3&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Day/Night Band (DNB) Bidirectional Reflectance Distribution Function (BRDF) and Albedo (VJ143DNBA3) Version 2 product provides albedo values at 1 kilometer (km) resolution for the bihemispherical reflectance white-sky albedos (WSA) and directional hemispherical reflectance black-sky albedos (BSA) at local solar noon. The VJ143DNBA3 product is produced daily using 16 days of VIIRS data and is weighted temporally to the ninth day, which is reflected in the file name. The VJ143 data products are designed to promote the continuity of NASA’s Moderate Resolution Imaging Spectroradiometer (MODIS) BRDF/Albedo data product suite. The VJ143 algorithm uses the RossThick/Li-Sparse-Reciprocal (RTLSR) semi-empirical kernel-driven BRDF model, with the three kernel weights from &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143DNBA1.002&quot;&gt;VJ143DNBA1&lt;/a&gt; to reconstruct surface anisotropic effects, correcting the directional reflectance to a common view geometry (&lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143DNBA4.002&quot;&gt;VJ143DNBA4&lt;/a&gt;), while also computing integrated black-sky albedo (BSA) at local solar noon and white-sky albedo (WSA) (VJ143DNBA3). Researchers can use the BRDF model parameters with a simple polynomial to obtain black-sky albedo at any solar illumination angle. Likewise, both the BSA and WSA Science Dataset (SDS) layers can be used with a simple polynomial to manually estimate instantaneous actual albedo (blue-sky albedo). Additional details regarding the methodology are available in the Algorithm Theoretical Basis Document (ATBD). The VJ143DNBA3 product provides BSA, WSA, and mandatory quality layers for the VIIRS DNB. A low-resolution image is also available showing retrievals of WSA for the shortwave broadband in JPEG format. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143dnba1&quot;&gt;VJ143DNBA1&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Day/Night Band (DNB) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameters (VJ143DNBA1) Version 2 product provides BRDF/Albedo model parameters at 1 kilometer (km) resolution. The VJ143DNBA1 product is produced daily using 16 days of VIIRS data and is weighted temporally to the ninth day, which is reflected in the file name. The VJ143 data products are designed to promote the continuity of NASA’s Moderate Resolution Imaging Spectroradiometer (MODIS) BRDF/Albedo data product suite. The VJ143 algorithm uses the RossThick/Li-Sparse-Reciprocal (RTLSR) semi-empirical kernel-driven BRDF model, with the three kernel weights from VJ143DNBA1 to reconstruct surface anisotropic effects, correcting the directional reflectance to a common view geometry (&lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143DNBA4.002&quot;&gt;VJ143DNBA4&lt;/a&gt;), while also computing integrated black-sky albedo (BSA) at local solar noon and white-sky albedo (WSA) (&lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143DNBA3.002&quot;&gt;VJ143DNBA3&lt;/a&gt;). Researchers can use the BRDF model parameters with a simple polynomial to obtain black-sky albedo at any solar illumination angle. Likewise, both the BSA and WSA Science Dataset (SDS) layers can be used with a simple polynomial to manually estimate instantaneous actual albedo (blue-sky albedo). Additional details regarding the methodology are available in the Algorithm Theoretical Basis Document (ATBD). The VJ143DNBA1 data product provides two SDS layers for mandatory quality and model parameters representing fiso, fvol, and fgeo for the VIIRS DNB. A low-resolution browse is also available showing BRDF/Albedo parameters for the DNB as a red, green, blue (RGB) image in JPEG format. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143dnba4&quot;&gt;VJ143DNBA4&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Day/Night Band (DNB) Nadir Bidirectional Reflectance Distribution Function (BRDF) Adjusted Reflectance (NBAR) Version 2 product provides NBAR estimates at 1 kilometer (km) resolution. The VJ143DNBA4 product is produced daily using 16 days of VIIRS data and is weighted temporally to the ninth day, which is reflected in the file name. The view angle effects are removed from the directional reflectance resulting in a stable and consistent NBAR product. The VJ143 data products are designed after the Moderate Resolution Imaging Spectroradiometer (MODIS) BRDF/Albedo product suite. The VJ143 algorithm uses the RossThick/Li-Sparse-Reciprocal (RTLSR) semi-empirical kernel-driven BRDF model, with the three kernel weights from &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143DNBA1.002&quot;&gt;VJ143DNBA1&lt;/a&gt; to reconstruct surface anisotropic effects, correcting the directional reflectance to a common view geometry (VJ143DNBA4), while also computing integrated black-sky albedo (BSA) at local solar noon and white-sky albedo (WSA) (&lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143DNBA3.002&quot;&gt;VJ143DNBA3&lt;/a&gt;). Researchers can use the BRDF model parameters with a simple polynomial to obtain black-sky albedo at any solar illumination angle. Likewise, both the BSA and WSA Science Dataset (SDS) layers can be used with a simple polynomial to manually estimate instantaneous actual albedo (blue-sky albedo). Additional details regarding the methodology are available in the Algorithm Theoretical Basis Document (ATBD). The VJ143DNBA4 product includes BRDF/Albedo mandatory quality and nadir reflectance for the VIIRS DNB. A low-resolution browse image is also available showing NBAR of the DNB as a red, green, blue (RGB) image in JPEG format. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj143dnba2&quot;&gt;VJ143DNBA2&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Day/Night Band (DNB) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Quality (VJ143DNBA2) Version 2 product provides BRDF and Albedo quality at 1 kilometer (km) resolution. The VJ143DNBA2 product is produced daily using 16 days of VIIRS data and is weighted temporally to the ninth day, which is reflected in the file name. The VJ143DNBA2 product gives information regarding band quality and days of valid observation within a 16-day period for the VIIRS DNB. The VJ143 data products are designed to promote the continuity of NASA’s Moderate Resolution Imaging Spectroradiometer (MODIS) BRDF/Albedo data product suite. The VJ143 algorithm uses the RossThick/Li-Sparse-Reciprocal (RTLSR) semi-empirical kernel-driven BRDF model, with the three kernel weights from &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143DNBA1.002&quot;&gt;VJ143DNBA1&lt;/a&gt; to reconstruct surface anisotropic effects, correcting the directional reflectance to a common view geometry (&lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143DNBA4.002&quot;&gt;VJ143DNBA4&lt;/a&gt;), while also computing integrated black-sky albedo (BSA) at local solar noon and white-sky albedo (WSA) (&lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ143DNBA3.002&quot;&gt;VJ143DNBA3&lt;/a&gt;). Researchers can use the BRDF model parameters with a simple polynomial to obtain black-sky albedo at any solar illumination angle. Likewise, both the BSA and WSA Science Dataset (SDS) layers can be used with a simple polynomial to manually estimate instantaneous actual albedo (blue-sky albedo). Additional details regarding the methodology are available in the Algorithm Theoretical Basis Document (ATBD). The VJ143DNBA2 data product provides a total of seven SDS layers, including BRDF/Albedo band quality and days of valid observation within a 16-day period for the VIIRS DNB, as well as land water type class flag, snow BRDF albedo class flag, local solar noon, and the platform name. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj147img&quot;&gt;VJ147IMG&lt;/h4&gt;
The Visible Infrared Imaging Radiometer Suite (VIIRS) FIre Light Detection Algorithm-2 (FILDA-2) Modified Combustion Efficiency (MCE) Version 2 swath product (VJ147IMG) is produced in 6-minute orbit segments 375 meter (m) resolution from the VIIRS sensor aboard the NOAA-20 satellite. The VJ147IMG product takes advantage of the rich information that visible band observation conveys at night to assess fire combustion efficiency and enhance fire detection. It also utilizes improvements made in fire detection algorithms to detect smaller and cooler fires. The VJ147IMG product includes 83 layers containing fire detection and retrievals of Radiative Power (FRP), fire Visible Energy Fraction (VEF), and Modified Combustion Efficiency (MCE). Known Issues: Known issues can be found in Section 5 of the User Guide. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&amp;amp;as&#x3D;5200&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj146a2&quot;&gt;VJ146A2&lt;/h4&gt;
The NOAA-20 VIIRS Gap-Filled Lunar BRDF-Adjusted Nighttime Lights Daily L3 Global 15 arc-second Linear Lat Lon Grid product, short-name VJ146A2 is a daily moonlight- and atmosphere-corrected Nighttime Lights (NTL) product. This product is available at 15 arc-second resolution and contains seven Science Data Sets (SDS) that include DNB BRDF-Corrected NTL, Gap-Filled DNB BRDF-Corrected NTL, DNB Lunar Irradiance, Latest High-Quality Retrieval, Mandatory Quality Flag, Cloud Mask Quality Flag, and Snow Flag. The VJ146A2 product files are provided in standard Hierarchical Data Format–Earth Observing System (HDF-EOS5) format. The current v2.0 collection contains several changes and differences relative to the previous v1.0 collection. These include radiance data format change from unsigned integer to floating-point, from exclusively for land surfaces coverage to both land and water surfaces, updated Mandatory_Quality_Flag layer, and others. Consult the v2.0-specific Black Marble User Guide for additional details at: &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/data/userguide/BlackMarbleUserGuide_Collection2.0_20241203.pdf&quot;&gt;https://landweb.modaps.eosdis.nasa.gov/data/userguide/BlackMarbleUserGuide_Collection2.0_20241203.pdf&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj102img&quot;&gt;VJ102IMG&lt;/h4&gt;
The VIIRS/JPSS1 Imagery Resolution 6-Min L1B Swath 375m, short-name VJ102IMG product that comprise five image-resolution or I-bands, which have a 375-meter resolution at nadir. These I-bands comprise three reflective solar bands (RSB) and two thermal emissive bands (TEB). Ranging in wavelengths from 0.6 µm to 12.4 µm, the I-bands are sensitive to visible/reflective, near-, shortwave-, mediumwave-, and longwave-infrared wavelengths. Derived from the NASA VIIRS L1A raw radiances, this product includes calibrated and geolocated radiance and reflectance data, quality flags, and granule- and collection-level metadata. In contrast to a MODIS L1B product, which temporally spans 5 minutes, the VIIRS L1B calibrated radiances product contains a nominal temporal duration of 6 minutes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj103img&quot;&gt;VJ103IMG&lt;/h4&gt;
The VIIRS/JPSS1 Imagery Resolution Terrain Corrected Geolocation 6-Min L1 Swath 375m product, short-name VJ103IMG, contains the derived line- of-sight (LOS) vectors for each of the 375-m image-resolution or I-bands. The geolocation algorithm uses a number of inputs that include an Earth ellipsoid, geoid, and a digital terrain model along with the SNPP platform’s ephemeris and attitude data, and knowledge of the VIIRS sensor and satellite geometry. It produces geodetic coordinates (latitude and longitude), and related parameters for each VIIRS L1 pixel. The VJ103IMG product includes geodetic latitude, longitude, surface height above the geoid, solar zenith and azimuth angles, sensor zenith and azimuth angles, land/water mask, and quality flag for every pixel location.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj121&quot;&gt;VJ121&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Land Surface Temperature and Emissivity (LST&amp;amp;E) Version 2 swath product (VJ121) is produced daily in 6-minute temporal increments of satellite acquisition. The VJ121 product uses a physics-based algorithm to dynamically retrieve both the LST and emissivity simultaneously for VIIRS thermal infrared bands M14 (8.55 µm), M15 (10.76 µm), and M16 (12 µm) at a spatial resolution of 750 meters. The VJ121 product is developed developed synergistically with the Moderate Resolution Imaging Spectroradiometer (MODIS) LST&amp;amp;E Version 6.1 product (&lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MOD21.061&quot;&gt;MOD21&lt;/a&gt;) using the same input atmospheric products and algorithmic approach based on the ASTER Temperature Emissivity Separation (TES) technique. The TES algorithm is combined with an improved Water Vapor Scaling (WVS) atmospheric correction scheme to stabilize the retrieval during very warm and humid conditions. The overall objective for NASA VIIRS products is to ensure the algorithms and products are compatible with the MODIS Terra and Aqua algorithms to promote the continuity of the Earth Observation System (EOS) mission. VIIRS LST&amp;amp;E products are available two months after acquisition due to latency of data inputs. Additional details regarding the method used to create this Level 2 (L2) product are available in the Algorithm Theoretical Basis Document (ATBD). Provided in the VJ121 product are layers for LST, quality control, emissivity for bands M14, M15, and M16, LST&amp;amp;E errors, view angle, ASTER Global Emissivity Dataset (GED), Precipitable Water Vapor (PWV), ocean-land mask, latitude, and longitude. A low-resolution browse image for LST is also available for each VJ121 granule. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt; and the User Guide.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj121c2&quot;&gt;VJ121C2&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Land Surface Temperature and Emissivity (LST&amp;amp;E) 8-day Climate Modeling Grid Version 2 product (VJ121C2) combines the daily &lt;a href&#x3D;&quot;http://doi.org/10.5067/VIIRS/VJ121A1D.002&quot;&gt;VJ121A1D&lt;/a&gt; and &lt;a href&#x3D;&quot;http://doi.org/10.5067/VIIRS/VJ121A1N.002&quot;&gt;VJ121A1N&lt;/a&gt; products over an 8-day compositing period into a single product. The VJ121C2 dataset is an 8-day composite LST&amp;amp;E product at 0.05 degree (~5,600 meter) resolution that uses an algorithm based on a simple-averaging method and is formatted as a CMG for use in climate simulation models. The algorithm calculates the average from all the cloud-free VJ121A1D and VJ121A1N daily acquisitions from the 8-day period. Unlike the VJ121A1 datasets where the daytime and nighttime acquisitions are separate products, the VJ121C2 contains both daytime and nighttime acquisitions as separate science dataset (SDS) layers within a single Hierarchical Data Format (HDF) file. The overall objective for NASA VIIRS products is to ensure the algorithms and products are compatible with the MODIS Terra and Aqua algorithms to promote the continuity of the Earth Observation System (EOS) mission. Additional details regarding the method used to create this Level 3 (L3) product are available in the Algorithm Theoretical Basis Document (ATBD). The VJ121C2 product contains 25 Science Datasets (SDS): LST, quality control, view zenith angle, and time of observation for both day and night observations along with emissivity for bands M14, M15, and M16. Low-resolution browse images for day and night LST are also available for each VJ121C2 granule. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt; and the User Guide.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj121a2&quot;&gt;VJ121A2&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Land Surface Temperature and Emissivity (LST&amp;amp;E) 8-day product (VJ121A2) combines the daily &lt;a href&#x3D;&quot;http://doi.org/10.5067/VIIRS/VJ121A1D.002&quot;&gt;VJ121A1D&lt;/a&gt; and &lt;a href&#x3D;&quot;http://doi.org/10.5067/VIIRS/VJ121A1N.002&quot;&gt;VJ121A1N&lt;/a&gt; products over an 8-day compositing period into a single product. The VJ121A2 dataset is an 8-day composite LST&amp;amp;E product at 1 kilometer resolution that uses an algorithm based on a simple-averaging method. The algorithm calculates the average from all the cloud-free VJ121A1D and VJ121A1N daily acquisitions from the 8-day period. Unlike the VJ121A1 datasets where the daytime and nighttime acquisitions are separate products, the VJ121A2 contains both daytime and nighttime acquisitions as separate science dataset (SDS) layers within a single Hierarchical Data Format (HDF) file. The VJ121A2 product is developed synergistically with the Moderate Resolution Imaging Spectroradiometer (MODIS) LST&amp;amp;E Version 6.1 product (&lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MOD21A2.061&quot;&gt;MOD21A2&lt;/a&gt;) using the same input atmospheric products and algorithmic approach. The overall objective for NASA VIIRS products is to ensure the algorithms and products are compatible with the MODIS Terra and Aqua algorithms to promote the continuity of the Earth Observation System (EOS) mission. Additional details regarding the method used to create this Level 3 (L3) product are available in the Algorithm Theoretical Basis Document (ATBD). The VJ121A2 product contains 11 Science Datasets (SDS): LST, quality control, view zenith angle, and time of observation for both day and night observations along with emissivity for bands M14, M15, and M16. Low-resolution browse images for day and night LST are also available for each VJ121A2 granule. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt; and the User Guide.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj121c1&quot;&gt;VJ121C1&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Land Surface Temperature and Emissivity (LST&amp;amp;E) Climate Modeling Grid Version 2 product (VJ121C) is compiled daily from daytime Level 2 Gridded (L2G) intermediate products. The L2G process maps the daily &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ121.002&quot;&gt;VJ121&lt;/a&gt; swath granules onto a sinusoidal MODIS grid and stores all observations overlapping a gridded cell for a given day. The VJ121C1 algorithm sorts through all these observations for each cell and estimates the final LST value as an average from all cloud-free observations that have good LST accuracies. The 0.05 degree (5,600 m) dataset is derived through resampling the native 750 meter VIIRS resolution in the input product. The overall objective for NASA VIIRS products is to ensure the algorithms and products are compatible with the MODIS Terra and Aqua algorithms to promote the continuity of the Earth Observation System (EOS) mission. Additional details regarding the method used to create this Level 3 (L3) product are available in the Algorithm Theoretical Basis Document (ATBD). The VJ121C1 product contains 25 Science Datasets (SDS): LST, quality control, view zenith angle, and time of observation for both day and night observations along with emissivity for bands M14, M15, and M16. Low-resolution browse images for day and night LST are also available for each VJ121C1 granule. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt; and the User Guide.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj121a1d&quot;&gt;VJ121A1D&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Land Surface Temperature and Emissivity (LST&amp;amp;E) Day Version 2 product (VJ121A1D) is compiled daily from daytime Level 2 Gridded (L2G) intermediate products. The L2G process maps the daily &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ121.002&quot;&gt;VJ121&lt;/a&gt; swath granules onto a sinusoidal MODIS grid and stores all observations overlapping a gridded cell for a given day. The VJ121A1 algorithm sorts through all these observations for each cell and estimates the final LST value as an average from all cloud-free observations that have good LST accuracies. The daytime average is weighted by the observation coverage for that cell. Only observations having observation coverage more than a certain threshold (15%) are considered for this averaging. The 1 kilometer dataset is derived through resampling the native 750 meter VIIRS resolution in the input product. The VJ121A1D product is developed synergistically with the Moderate Resolution Imaging Spectroradiometer (MODIS) LST&amp;amp;E Version 6.1 product (&lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MOD21A1D.061&quot;&gt;MOD21A1D&lt;/a&gt;) using the same input atmospheric products and algorithmic approach. The overall objective for NASA VIIRS products is to ensure the algorithms and products are compatible with the MODIS Terra and Aqua algorithms to promote the continuity of the Earth Observation System (EOS) mission. Additional details regarding the method used to create this Level 3 (L3) product are available in the Algorithm Theoretical Basis Document (ATBD). The VJ121A1D product contains seven Science Datasets (SDS): LST, quality control, emissivity for bands M14, M15, and M16, view zenith angle, and time of observation. A low-resolution browse image for LST is also available for each VJ121A1D granule. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt; and the User Guide.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj121a1n&quot;&gt;VJ121A1N&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Land Surface Temperature and Emissivity (LST&amp;amp;E) Night Version 2 product (VJ121A1N) is compiled daily from nighttime Level 2 Gridded (L2G) intermediate products. The L2G process maps the daily &lt;a href&#x3D;&quot;https://doi.org/10.5067/VIIRS/VJ121.002&quot;&gt;VJ121&lt;/a&gt; swath granules onto a sinusoidal MODIS grid and stores all observations overlapping a gridded cell for a given night. The VJ121A1 algorithm sorts through all these observations for each cell and estimates the final LST value as an average from all cloud-free observations that have good LST accuracies. The nighttime average is weighted by the observation coverage for that cell. Only observations having observation coverage more than a certain threshold (15%) are considered for this averaging. The 1 kilometer dataset is derived through resampling the native 750 meter VIIRS resolution in the input product. The VJ121A1N product is developed synergistically with the Moderate Resolution Imaging Spectroradiometer (MODIS) LST&amp;amp;E Version 6.1 product (&lt;a href&#x3D;&quot;https://doi.org/10.5067/MODIS/MOD21A1N.061&quot;&gt;MOD21A1N&lt;/a&gt;) using the same input atmospheric products and algorithmic approach. The overall objective for NASA VIIRS products is to ensure the algorithms and products are compatible with the MODIS Terra and Aqua algorithms to promote the continuity of the Earth Observation System (EOS) mission. Additional details regarding the method used to create this Level 3 (L3) product are available in the Algorithm Theoretical Basis Document (ATBD). The VJ121A1N product contains seven Science Datasets (SDS): LST, quality control, emissivity for bands M14, M15, and M16, view zenith angle, and time of observation. A low-resolution browse image for LST is also available for each VJ121A1N granule. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt; and the User Guide.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj121c3&quot;&gt;VJ121C3&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Land Surface Temperature and Emissivity (LST&amp;amp;E) monthly Climate Modeling Grid Version 2 product (VJ121C3) provides LST&amp;amp;E by a process of selecting the best available pixel over a monthly acquisition period at 0.05 degree (~5,600 meter) resolution. The VJ121C3 dataset is a monthly composite LST&amp;amp;E product that uses an algorithm based on a simple averaging method and is formatted as a CMG for use in climate simulation models. The algorithm calculates the average from all the cloud free &lt;a href&#x3D;&quot;http://doi.org/10.5067/VIIRS/VJ121A1D.002&quot;&gt;VJ121A1D&lt;/a&gt; and &lt;a href&#x3D;&quot;http://doi.org/10.5067/VIIRS/VJ121A1N.002&quot;&gt;VJ121A1N&lt;/a&gt; daily acquisitions from the monthly period. Unlike the VJ121A1 data sets where the daytime and nighttime acquisitions are separate products, the VJ121C3 contains both daytime and nighttime acquisitions as separate Science Dataset (SDS) layers within a single Hierarchical Data Format (HDF) file. Additional details regarding the method used to create this Level 3 (L3) product are available in the Algorithm Theoretical Basis Document (ATBD). The VJ121C3 product contains 25 Science Datasets (SDS): LST, quality control, view zenith angle, and time of observation for both day and night observations along with emissivity for bands M14, M15, and M16. Low-resolution browse images for day and night LST are also available for each VJ121C3 granule. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt; and the User Guide.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj115a2h&quot;&gt;VJ115A2H&lt;/h4&gt;
The Visible Infrared Imaging Radiometer Suite (VIIRS) Leaf Area Index (LAI) and Fraction of Photosynthetically Active Radiation (FPAR) Version 2 data product (VJ115A2H) provides information about the vegetative canopy layer at 500 meter resolution. The VIIRS sensor is located aboard the NOAA-20 satellite. LAI is an index that quantifies the one-sided leaf area of a canopy, while FPAR is the fraction of incoming solar energy absorbed through photosynthesis at 400 to 700 nanometers. This product is intentionally designed after the Terra and Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) LAI/FPAR operational algorithm to promote the continuity of the Earth Observation System (EOS) mission. The VJ115A2H product includes six Science Data Set Layers for the analysis of key factors in LAI/FPAR measurements. These include the LAI and FPAR measurements, quality detail for LAI/FPAR, extra quality detail for FPAR, and the standard deviation for LAI and FPAR. Two low resolution browse images are also available for each VJ115A2H granule: LAI and FPAR. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj102mod&quot;&gt;VJ102MOD&lt;/h4&gt;
The VIIRS/JPSS1 Moderate Resolution 6-Min L1B Swath 750 m, short-name VJ102MOD is VIIRS Level-1B calibrated radiances product that comprise sixteen moderate-resolution or M-bands, which have a spatial resolution of 750-meters at nadir. These M-bands comprise eleven reflective solar bands (RSB) and five thermal emissive bands (TEB). Each of the M-bands has 16 detectors in the along-track direction with 16 rows of pixels per scan that provide a 750-m resolution. Ranging in wavelengths from 0.402 µm to 12.49 µm, the M-bands are sensitive to visible, near-, shortwave-, mediumwave-, and longwave-infrared wavelengths. Derived from the NASA VIIRS L1A raw radiances, this product includes calibrated and geolocated radiance and reflectance data, quality flags, and granule- and collection-level metadata. In contrast to a MODIS L1B product, which temporally spans 5 minutes, the VIIRS L1B calibrated radiances product contains a nominal temporal duration of 6 minutes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj103modll&quot;&gt;VJ103MODLL&lt;/h4&gt;
The Visible Infrared Imaging Radiometer Suite (VIIRS) Moderate Resolution Terrain Correction Geolocation (VJ103MODLL) Version 2.1 product from the NOAA-20 VIIRS sensor is produced in 6 minute temporal satellite increments (swaths) at 750 meter resolution. Intersecting the VIIRS line of sight vector with Earth’s geoid and the World Geodetic System (WGS) ellipsoid, this product is based on the SRTM30 Version 2 digital elevation model (DEM), which uses GTOPO30 data for areas from 60° North to 60° South. VJ103MODLL is a terrain correction geolocation product that provides the spatial location for various VIIRS data products. Each swath of data is approximately 3,060 kilometers along track (long) and 3,060 kilometers across track (wide). Provided in the VJ103MODLL product are layers for height, latitude, and longitude. These Science Data Sets (SDS) layers are used in conjunction with the (&lt;a href&#x3D;&quot;https://doi.org/10.5067/viirs/vj114.002&quot;&gt;VJ114&lt;/a&gt;) swath product for accurate geolocation information. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj103mod&quot;&gt;VJ103MOD&lt;/h4&gt;
The VIIRS/JPSS1 Moderate Resolution Terrain Corrected Geolocation 6-Min L1 Swath 750m product, short-name VJ103MOD contains the derived line-of-sight (LOS) vectors for each of the 750-m moderate-resolution, or M-bands. The geolocation algorithm uses a number of inputs that include an Earth ellipsoid, geoid, and a digital terrain model along with the SNPP platform’s ephemeris and attitude data, and knowledge of the VIIRS sensor and satellite geometry. It produces geodetic coordinates (latitude and longitude), and related parameters for each VIIRS L1 pixel. The VJ103MOD product includes geodetic latitude, longitude, surface height above the geoid, solar zenith and azimuth angles, sensor zenith and azimuth angles, land/water mask, and quality flag for every pixel location.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj109a1&quot;&gt;VJ109A1&lt;/h4&gt;
The 8-day Visible Infrared Imaging Radiometer Suite (VIIRS) surface reflectance (VJ109A1) Version 2 composite product provides an estimate of land surface reflectance from the NOAA-20 VIIRS sensor for nine moderate resolution bands (M1 - M5, M7, M8, M10, M11) at nominal 1 kilometer resolution (~926 meter). The 1 kilometer dataset is derived through resampling the native 750 meter VIIRS resolution in the Level 2 input product. The data are corrected for atmospheric conditions such as the effects of molecular gases, including ozone and water vapor, and for the effects of atmospheric aerosols. Each pixel represents the best possible Level 2G observation during an 8-day period that is selected on the basis of high observation coverage, low sensor angle, the absence of clouds or cloud shadow, and aerosol loading. Included in the product along with the nine reflectance bands are day of year, reflectance band quality, control, reflectance state quality assurance, relative azimuth angle, sensor zenith angle, and solar zenith angle layers. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt; and in Section 4.0 of the User Guide.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj109h1&quot;&gt;VJ109H1&lt;/h4&gt;
The 8-day Visible Infrared Imaging Radiometer Suite (VIIRS) Surface Reflectance (VJ109H1) Version 2 composite product provides an estimate of land surface reflectance from the NOAA-20 VIIRS sensor for three imagery bands (I1, I2, I3) at nominal 500 meter resolution (~463 meter). The 500 meter dataset is derived through resampling the native 375 meter VIIRS resolution in the L2 input product. The data are corrected for atmospheric conditions such as the effects of molecular gases, including ozone and water vapor, and for the effects of atmospheric aerosols. Each pixel represents the best possible Level 2G observation during an 8-day period, which is selected on the basis of high observation coverage, low sensor angle, the absence of clouds or cloud shadow, and aerosol loading. In addition to the three reflectance bands, this product includes a state quality assurance (QA) layer and a reflectance band quality layer. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt; and in Section 4.0 of the User Guide.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj109ga&quot;&gt;VJ109GA&lt;/h4&gt;
The Visible Infrared Imaging Radiometer Suite (VIIRS) daily surface reflectance (VJ109GA) Version 2 product provides an estimate of land surface reflectance from the NOAA-20 VIIRS sensor. Data are provided for three imagery bands (I1-I3) at nominal 500 meter resolution (&lt;del&gt;463 meter) and nine moderate resolution bands (M1-M5, M7, M8, M10, M11) at nominal 1 kilometer (&lt;/del&gt;926 meter) resolution. The 500 meter and 1 kilometer datasets are derived through resampling the native 375 meter and 750 meter VIIRS resolutions, respectively, in the Level 2 input product. These bands are corrected for atmospheric conditions such as the effects of molecular gases, including ozone and water vapor, and for the effects of atmospheric aerosols. The inputs to the surface reflectance algorithm are top-of-atmosphere reflectance for the VIIRS visible bands, the VIIRS cloud mask and aerosol product, aerosol optical thickness and atmospheric data obtained from the NOAA National Centers for Environmental Prediction (NCEP) reanalysis system. Along with the twelve reflectance bands are reflectance band quality, sensor azimuth angle, solar azimuth angle, sensor zenith angle, solar zenith angle, and observations layers. The reflectance layers from the VJ109GA data product are used as input data for many of the VIIRS land products. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt; and in Section 4.0 of the User Guide.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj109cmg&quot;&gt;VJ109CMG&lt;/h4&gt;
The Visible Infrared Imaging Radiometer Suite (VIIRS) daily surface reflectance Climate Modeling Grid (VJ109CMG) Version 2 product provides an estimate of land surface reflectance from the NOAA-20 VIIRS sensor. Data are provided for three imagery bands (I1-I3) and nine moderate resolution bands (M1-M5, M7, M8, M10, M11) at 0.05 degree (~5,600 meter) resolution. The data are corrected for atmospheric conditions such as the effects of molecular gases, including ozone and water vapor, and for the effects of atmospheric aerosols. This product uses a weighted average of the best quality observation and is formatted as a CMG for use in climate simulation models. This product includes the twelve reflectance bands, five moderate resolution brightness temperature bands (M12-M16) and information layers representing relative azimuth angle, sensor zenith angle, solar zenith angle, reflectance band quality, time of day, and number mapping. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt; and in Section 4.0 of the User Guide.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj114a1&quot;&gt;VJ114A1&lt;/h4&gt;
The daily NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Thermal Anomalies and Fire (VJ114A1) Version 2 data product provides daily information about active fires and other thermal anomalies. The VJ114A1 data product is a global, 1 kilometer (km) gridded composite of fire pixels detected from VIIRS 750 meter (m) bands over a daily (24-hour) period. The VJ114 data products are designed after the Moderate Resolution Imaging Spectroradiometer (MODIS) Thermal Anomalies/Fire product suite. The VJ114A1 product provides a total of four Science Dataset (SDS) layers for the confidence of fire, maximum fire radiative power (FRP), quality assessment (QA), and position of fire within scan. Each data product file is provided in HDF-EOS5 format. A low resolution browse is also provided showing the fire mask layer with a color map applied in JPEG format. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt; and in Section 5.0 “Frequently Asked Questions” of the User Guide.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj114&quot;&gt;VJ114&lt;/h4&gt;
The Visible Infrared Imaging Radiometer Suite (VIIRS) Thermal Anomalies (VJ114) Version 2 product is produced in 6-minute temporal satellite increments (swaths) at 750 meter resolution from the VIIRS sensor located on the NOAA-20 satellite. This product is designed after the Terra and Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) Thermal Anomalies and Fire data products to promote the continuity of the Earth Observation System (EOS) mission. This data product can enable users to understand the location and intensity of fire events as well as identifying thermal anomalies. The VJ114 product includes 31 science dataset layers to analyze key factors in fire detection, including atmospheric conditions (e.g., atmospheric reflectance, solar zenith angle, brightness temperature) and fuel type for the event. The fire mask layer in the VJ114 product is the primary layer and can be used to identify fires and other thermal anomalies such as volcanoes. In addition to the fire mask, brightness temperature is provided for VIIRS channels M5, M7, M11, M13, M15, and M16. Each swath of data is approximately 3,060 kilometers along track (long) and 3,060 kilometers across track (wide). The VJ114 product is also used to generate higher-level fire data products. Use of the &lt;a href&#x3D;&quot;https://doi.org/10.5067/viirs/vj103modll.021&quot;&gt;VJ103MODLL&lt;/a&gt; data product is required to apply accurate geolocation information to the VJ114 Science Datasets (SDS). Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt; and in Section 5.0 “Frequently Asked Questions” of the User Guide.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj113c1&quot;&gt;VJ113C1&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Vegetation Indices (VJ113C1) Version 2 data product provides vegetation indices by a process of selecting the best available pixel over a 16-day acquisition period at 0.05 degree resolution. The VNP13 data products are designed after the Moderate Resolution Imaging Spectroradiometer (MODIS) Terra and Aqua Vegetation Indices product suite to promote the continuity of the Earth Observation System (EOS) mission. The VJ113 algorithm process produces three vegetation indices: The Normalized Difference Vegetation Index (NDVI), the Enhanced Vegetation Index (EVI), and the Enhanced Vegetation Index-2 (EVI2). NDVI is one of the longest continual remotely sensed time series observations, using both the red and near-infrared (NIR) bands. EVI is a slightly different vegetation index that is more sensitive to canopy cover, while NDVI is more sensitive to chlorophyll. EVI2 is a reformation of the standard 3-band EVI, using the red band and NIR band. This reformation addresses arising issues when comparing VIIRS EVI to other EVI models that do not include a blue band. EVI2 will eventually become the standard EVI. Along with the three Vegetation Indices layers, this product also includes layers for the standard deviations of each Vegetation Index; NIR reflectance; three shortwave infrared (SWIR) reflectance; red, blue, and green reflectance; number of pixels, number of pixels used; pixel reliability; average sun angle, and a quality layer. Two low resolution browse images are also available for each VJ113C1 product: EVI and NDVI. Known Issues: Due to missing critical inputs, this product lacks coverage for tiles h33v07 and h18v14, which are located over water. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt; and the User Guide and ATBD.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj113a2&quot;&gt;VJ113A2&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Vegetation Indices (VJ113A2) Version 2 data product provides vegetation indices by a process of selecting the best available pixel over a 16-day acquisition period at 1 kilometer (km) resolution. The VJ113 data products are designed after the Moderate Resolution Imaging Spectroradiometer (MODIS) Terra and Aqua Vegetation Indices product suite to promote the continuity of the Earth Observation System (EOS) mission. The VJ113 algorithm process produces three vegetation indices: The Normalized Difference Vegetation Index (NDVI), the Enhanced Vegetation Index (EVI), and the Enhanced Vegetation Index-2 (EVI2). NDVI is one of the longest continual remotely sensed time series observations, using both the red and near-infrared (NIR) bands. EVI is a slightly different vegetation index that is more sensitive to canopy cover, while NDVI is more sensitive to chlorophyll. EVI2 is a reformation of the standard 3-band EVI, using the red band and NIR band. This reformation addresses arising issues when comparing VIIRS EVI to other EVI models that do not include a blue band. EVI2 will eventually become the standard EVI. Along with the three Vegetation Indices layers, this product also includes layers for NIR reflectance; three shortwave infrared (SWIR) reflectance; red, blue, and green reflectance; composite day of year; pixel reliability; relative azimuth, view, and sun angles, and a quality layer. Two low resolution browse images are also available for each VJ113A2 product: EVI and NDVI. Known Issues: Due to missing critical inputs, this product lacks coverage for tiles h33v07 and h18v14, which are located over water. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt; and the User Guide and ATBD.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj113a1&quot;&gt;VJ113A1&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Vegetation Indices (VJ113A1) Version 2 data product provides vegetation indices by a process of selecting the best available pixel over a 16-day acquisition period at 500 meter (m) resolution. The VJ113 data products are designed after the Moderate Resolution Imaging Spectroradiometer (MODIS) Terra and Aqua Vegetation Indices product suite to promote the continuity of the Earth Observation System (EOS) mission. The VJ113 algorithm process produces three vegetation indices: Normalized Difference Vegetation Index (NDVI), the Enhanced Vegetation Index (EVI), and Enhanced Vegetation Index-2 (EVI2). NDVI is one of the longest continual remotely sensed time series observations, using both the red and near-infrared (NIR) bands. EVI is a slightly different vegetation index that is more sensitive to canopy cover, while NDVI is more sensitive to chlorophyll. EVI2 is a reformation of the standard 3-band EVI, using the red band and NIR band. This reformation addresses arising issues when comparing VIIRS EVI to other EVI models that do not include a blue band. EVI2 will eventually become the standard EVI. Along with the three Vegetation Indices layers, this product also includes layers for NIR reflectance; three shortwave infrared (SWIR) reflectance; red, blue, and green reflectance; composite day of year; pixel reliability; relative azimuth, view, and sun angles; and a quality layer. Two low resolution browse images are also available for each VJ113A1 product: EVI and NDVI. Known Issues: Due to missing critical inputs, this product lacks coverage for tiles h33v07 and h18v14, which are located over water. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt; and the User Guide and ATBD.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj113c2&quot;&gt;VJ113C2&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Vegetation Indices (VJ113C2) Version 2 data product provides vegetation indices by a process of selecting the best available pixel over a monthly acquisition period at 0.05 degree resolution. The VNP13 data products are designed after the Moderate Resolution Imaging Spectroradiometer (MODIS) Terra and Aqua Vegetation Indices product suite to promote the continuity of the Earth Observation System (EOS) mission. The VNP13 algorithm process produces three vegetation indices: The Normalized Difference Vegetation Index (NDVI), the Enhanced Vegetation Index (EVI), and the Enhanced Vegetation Index-2 (EVI2). NDVI is one of the longest continual remotely sensed time series observations, using both the red and near-infrared (NIR) bands. EVI is a slightly different vegetation index that is more sensitive to canopy cover, while NDVI is more sensitive to chlorophyll. EVI2 is a reformation of the standard 3-band EVI, using the red band and NIR band. This reformation addresses arising issues when comparing VIIRS EVI to other EVI models that do not include a blue band. EVI2 will eventually become the standard EVI. Along with the three Vegetation Indices layers, this product also includes layers for the standard deviations of each Vegetation Index; NIR reflectance; three shortwave infrared (SWIR) reflectance; red, blue, and green reflectance; number of pixels, number of pixels used; pixel reliability; average sun angle, and a quality layer. Two low resolution browse images are also available for each VJ113C2 product: EVI and NDVI. Known Issues: Due to missing critical inputs, this product lacks coverage for tiles h33v07 and h18v14, which are located over water. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt; and the User Guide and ATBD.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj113a3&quot;&gt;VJ113A3&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Vegetation Indices (VJ113A3) Version 2 data product provides vegetation indices by a process of selecting the best available pixel over a monthly acquisition period at 1 kilometer (km) resolution. The VJ113 data products are designed after the Moderate Resolution Imaging Spectroradiometer (MODIS) Terra and Aqua Vegetation Indices product suite to promote the continuity of the Earth Observation System (EOS) mission. The VJ113 algorithm process produces three vegetation indices: The Normalized Difference Vegetation Index (NDVI), the Enhanced Vegetation Index (EVI), and the Enhanced Vegetation Index-2 (EVI2). NDVI is one of the longest continual remotely sensed time series observations, using both the red and near-infrared (NIR) bands. EVI is a slightly different vegetation index that is more sensitive to canopy cover, while NDVI is more sensitive to chlorophyll. EVI2 is a reformation of the standard 3-band EVI, using the red band and NIR band. This reformation addresses arising issues when comparing VIIRS EVI to other EVI models that do not include a blue band. EVI2 will eventually become the standard EVI. Along with the three Vegetation Indices layers, this product also includes layers for NIR reflectance; three shortwave infrared (SWIR) reflectance; red, blue, and green reflectance; pixel reliability; pixel reliability; relative azimuth, view, and sun angles; and a quality layer. Two low resolution browse images are also available for each VJ113A3 product: EVI and NDVI. Known Issues: Due to missing critical inputs, this product lacks coverage for tiles h33v07 and h18v14, which are located over water. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt; and the User Guide and ATBD.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj128c2&quot;&gt;VJ128C2&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Water Reservoir 8-day Level 3 (L3) Global (VJ128C2) Version 2 product provides current data for 151 man-made reservoirs and 13 regulated natural lakes for a total of 164 reservoirs. The VJ128C2 data product provides an 8-day time series of surface area, elevation, and water storage. Datasets are combined with pre-established &lt;a href&#x3D;&quot;https://doi.org/10.1016/j.rse.2020.111831&quot;&gt;Area-Elevation (A-E) curves&lt;/a&gt; and image classifications of near-infrared (NIR) reflectance from the surface reflectance product acquired by the VIIRS satellite (&lt;a href&#x3D;&quot;https://lpdaac.usgs.gov/products/vj109h1v002/&quot;&gt;VJ109H1&lt;/a&gt;). The VJ128C2 data product consists of a single layer with information about the reservoir identifier, dam location (longitude and latitude), reservoir surface area, elevation, and water storage capacity. Known Issues: Water occurrence images generally show smaller surface area dynamics in high latitude regions, creating pixels with low occurrence values that have relatively large uncertainties. In addition, the quality of raw water area classification can be affected by lake ice coverage typically creating an overestimation of surface area in the enhancement algorithm. This issue will be addressed in a future release of the enhancement algorithm. For additional information about known issues, refer to Section 4 in the User Guide.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj128c3&quot;&gt;VJ128C3&lt;/h4&gt;
The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) Water Reservoir Monthly Level 3 (L3) Global (VJ128C3) Version 2 product provides current data for 151 man-made reservoirs and 13 regulated natural lakes for a total of 164 reservoirs. The VJ128C3 data product is a composite of the 8-day area classifications from &lt;a href&#x3D;&quot;https://lpdaac.usgs.gov/products/vj128c2v002/&quot;&gt;VJ128C2&lt;/a&gt; which is converted to provide monthly elevation and water storage. The Lake Temperature and Evaporation Model (&lt;a href&#x3D;&quot;https://doi.org/10.1016/j.rse.2020.112104&quot;&gt;LTEM&lt;/a&gt;) with input from VIIRS Land Surface Temperature and Emissivity (&lt;a href&#x3D;&quot;https://lpdaac.usgs.gov/products/vj121a2v002/&quot;&gt;VJ121A2&lt;/a&gt;) and meteorological data from Global Land Data Assimilation System (&lt;a href&#x3D;&quot;https://earth.gsfc.nasa.gov/hydro/data/gldas-global-land-data-assimilation-system-data&quot;&gt;GLDAS&lt;/a&gt;) are used to produce monthly evaporation rates and volume losses. The VJ128C3 data product provides a monthly time series that consists of a single layer with information about the reservoir identifier, dam location (longitude and latitude), reservoir surface area, elevation, water storage capacity, evaporation rate, and evaporation volume. Known Issues: Water occurrence images generally show smaller surface area dynamics in high latitude regions, creating pixels with low occurrence values that have relatively large uncertainties. In addition, the quality of raw water area classification can be affected by lake ice coverage typically creating an overestimation of surface area in the enhancement algorithm. This issue will be addressed in a future release of the enhancement algorithm. For additional information about known issues, refer to Section 4 in the User Guide.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj147mod&quot;&gt;VJ147MOD&lt;/h4&gt;
The Visible Infrared Imaging Radiometer Suite (VIIRS) FIre Light Detection Algorithm-2 (FILDA-2) Modified Combustion Efficiency (MCE) Version 2 swath product (VJ147MOD) is produced in 6-minute orbit segments 750 meter (m) resolution from the VIIRS sensor aboard the NOAA-20 satellite. The VJ147MOD product takes advantage of the rich information that visible band observation conveys at night to assess fire combustion efficiency and enhance fire detection. It also utilizes improvements made in fire detection algorithms to detect smaller and cooler fires. The VJ147MOD product includes 85 layers containing fire detection and retrievals of Radiative Power (FRP), fire Visible Energy Fraction (VEF), and Modified Combustion Efficiency (MCE). Known Issues: Known issues can be found in Section 5 of the User Guide. * For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&amp;amp;as&#x3D;5200&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj202dnb&quot;&gt;VJ202DNB&lt;/h4&gt;
The VIIRS/JPSS2 Day/Night Band 6-Min L1B Swath 750 m, short-name VJ202DNB, of the Joint Polar-orbiting Satellite System-2 (JPSS-2/NOAA-21; referred to hereafter as J2) platform-derived single NASA VIIRS panchromatic Day-Night band (DNB) calibrated radiance product. The DNB is one of the M-bands with an at-nadir spatial resolution of 750 meters (across the entire scan). The panchromatic DNB’s spectral wavelength ranges from 0.5 micrometer to 0.9 micrometer. It facilitates measuring night lights, reflected solar/lunar lights with a large dynamic range between a low of a quarter moon illumination to the brightest daylight. The J2 VIIRS radiometric calibration Level-1B reprocessing includes a few calibration updates for the reflective solar bands (RSB), but no significant changes for the day-night band (DNB) or thermal emissive bands (TEB). For more information and for users guide, visit: &lt;a href&#x3D;&quot;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/products/VJ202DNB&quot;&gt;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/products/VJ202DNB&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj203dnb&quot;&gt;VJ203DNB&lt;/h4&gt;
The VIIRS/JPSS2 Day/Night Band Resolution Terrain Corrected Geolocation 6-Min L1 Swath 750 m, short-name VJ203DNB product is the Joint Polar-orbiting Satellite System-2 (JPSS-2/NOAA-21) platform-based NASA Visible Infrared Imaging Radiometer Suite (VIIRS) L1 terrain-corrected geolocation product, and contains the derived line-of-sight (LOS) vectors for the single panchromatic Day-Night band (DNB). The geolocation algorithm uses a number of inputs that include an Earth ellipsoid, geoid, and a digital terrain model along with the SNPP platform’s ephemeris and attitude data, and knowledge of the VIIRS sensor and satellite geometry. It provides geodetic coordinates (latitude and longitude), and related parameters for each VIIRS L1 pixel. The VJ203DNB product includes geodetic latitude, longitude, surface height above the geoid, solar zenith and azimuth angles, lunar zenith and azimuth angles, sensor zenith and azimuth angles, land/water mask, moon illumination fraction and phase angle, and quality flag for every pixel location. The J2 VIIRS geolocation underwent an on-orbit validation. Geolocation errors of about 350 m in the along-scan direction and about 165 m in the along-track direction were corrected for the image-resolution bands and moderate-resolution bands. The Day-Night band (DNB) geolocation error of about 2000 m was corrected. For more information and documents, visit LAADS product page at: &lt;a href&#x3D;&quot;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/products/VJ203DNB&quot;&gt;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/products/VJ203DNB&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj202img&quot;&gt;VJ202IMG&lt;/h4&gt;
The VIIRS/JPSS2 Imagery Resolution 6-Min L1B Swath 375m, short-name VJ202IMG is the Joint Polar-orbiting Satellite System-2 (JPSS-2/NOAA-21; referred to hereafter as J2) platform-derived NASA Visible Infrared Imaging Radiometer Suite (VIIRS) L1B calibrated radiances product that comprise five image-resolution or I-bands, which have a 375-meter resolution at nadir. These I-bands comprise three reflective solar bands (RSB) and two thermal emissive bands (TEB). Each of the I-bands has 32 detectors in the along-track direction with 32 rows of pixels per scan that offer a resolution that is twice finer than that of the moderate (M) and Day-Night bands (DNB). Ranging in wavelengths from 0.6 µm to 12.4 µm, the I-bands are sensitive to visible/reflective, near-, shortwave-, mediumwave-, and longwave-infrared wavelengths. The J2 VIIRS radiometric calibration Level-1B reprocessing includes a few calibration updates for the reflective solar bands (RSB), but no significant changes for the day-night band (DNB) or thermal emissive bands (TEB). For more information and documents, visit LAADS product page at: &lt;a href&#x3D;&quot;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/products/VJ202IMG&quot;&gt;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/products/VJ202IMG&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj203img&quot;&gt;VJ203IMG&lt;/h4&gt;
The VIIRS/JPSS2 Imagery Resolution Terrain Corrected Geolocation 6-Min L1 Swath 375 m, short-name VJ203IMG is the Joint Polar-orbiting Satellite System-2 (JPSS-2/NOAA-21) platform-derived NASA Visible-Infrared Imaging-Radiometer Suite (VIIRS) L1 terrain-corrected geolocation product and contains the derived line-of-sight (LOS) vectors for each of the 375-m image-resolution or I-bands. The geolocation algorithm uses a number of inputs that include an Earth ellipsoid, geoid, and a digital terrain model along with the SNPP platform’s ephemeris and attitude data, and knowledge of the VIIRS sensor and satellite geometry. It produces geodetic coordinates (latitude and longitude), and related parameters for each VIIRS L1 pixel. The VJ203IMG product includes geodetic latitude, longitude, surface height above the geoid, solar zenith and azimuth angles, sensor zenith and azimuth angles, land/water mask, and quality flag for every pixel location. VJ203IMG provides a fundamental input to derive a number of VIIRS I-band higher-level products. The J2 VIIRS geolocation underwent an on-orbit validation. Geolocation errors of about 350 m in the along-scan direction and about 165 m in the along-track direction were corrected for the image-resolution bands and moderate-resolution bands. The Day-Night band (DNB) geolocation error of about 2000 m was corrected. Further, the geolocation biases in the scan profile were also corrected. For more information and documents, visit LAADS product page at: &lt;a href&#x3D;&quot;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/products/VJ203IMG&quot;&gt;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/products/VJ203IMG&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj202mod&quot;&gt;VJ202MOD&lt;/h4&gt;
The VIIRS/JPSS2 Moderate Resolution 6-Min L1B Swath 750m, short-name VJ202MOD is the Joint Polar-orbiting Satellite System-2 (JPSS-2/NOAA-21; referred to hereafter as J2) platform-derived NASA Visible Infrared Imaging Radiometer Suite (VIIRS) L1B calibrated radiances product that comprise sixteen moderate-resolution or M-bands, which have a spatial resolution of 750-meters at nadir. These M-bands comprise eleven reflective solar bands (RSB) and five thermal emissive bands (TEB). Each of the M-bands has 16 detectors in the along-track direction with 16 rows of pixels per scan that provide a 750-m resolution. Ranging in wavelengths from 0.402 µm to 12.49 µm, the M-bands are sensitive to visible, near-, shortwave-, mediumwave-, and longwave-infrared wavelengths. Derived from the NASA VIIRS L1A raw radiances, this product includes calibrated and geolocated radiance and reflectance data, quality flags, and granule- and collection-level metadata. The J2 VIIRS radiometric calibration Level-1B reprocessing includes a few calibration updates for the reflective solar bands (RSB), but no significant changes for the day-night band (DNB) or thermal emissive bands (TEB). For more information and documentation, visit LAADS product page at: &lt;a href&#x3D;&quot;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/products/VJ202MOD&quot;&gt;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/products/VJ202MOD&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj203mod&quot;&gt;VJ203MOD&lt;/h4&gt;
The VIIRS/JPSS2 Moderate Resolution Terrain Corrected Geolocation 6-Min L1 Swath 750 m, short-name VJ203MOD is the Joint Polar-orbiting Satellite System-2 (JPSS-2/NOAA-21) platform-based NASA Visible-Infrared Imaging-Radiometer Suite (VIIRS) L1 terrain-corrected geolocation product, and contains the derived line-of-sight (LOS) vectors for each of the 750-m moderate-resolution, or M-bands. The geolocation algorithm uses a number of inputs that include an Earth ellipsoid, geoid, and a digital terrain model along with the SNPP platform’s ephemeris and attitude data, and knowledge of the VIIRS sensor and satellite geometry. It produces geodetic coordinates (latitude and longitude), and related parameters for each VIIRS L1 pixel. The VJ203MOD product includes geodetic latitude, longitude, surface height above the geoid, solar zenith and azimuth angles, sensor zenith and azimuth angles, land/water mask, and quality flag for every pixel location. VJ203MOD provides a fundamental input to derive a number of VIIRS M-band higher-level products. The J2 VIIRS geolocation underwent an on-orbit validation. Geolocation errors of about 350 m in the along-scan direction and about 165 m in the along-track direction were corrected for the image-resolution bands and moderate-resolution bands. The Day-Night band (DNB) geolocation error of about 2000 m was corrected. For more information and documents, visit LAADS product page at: &lt;a href&#x3D;&quot;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/products/VJ203MOD&quot;&gt;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/products/VJ203MOD&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj209a1&quot;&gt;VJ209A1&lt;/h4&gt;
The 8-day Visible Infrared Imaging Radiometer Suite (VIIRS) surface reflectance (VJ209A1) Version 2 composite product provides an estimate of land surface reflectance from the NOAA-21 VIIRS sensor for nine moderate resolution bands (M1 - M5, M7, M8, M10, M11) at nominal 1 kilometer resolution (~926 meter). The 1 kilometer dataset is derived through resampling the native 750 meter VIIRS resolution in the Level 2 input product. The data are corrected for atmospheric conditions such as the effects of molecular gases, including ozone and water vapor, and for the effects of atmospheric aerosols. Each pixel represents the best possible Level 2G observation during an 8-day period that is selected on the basis of high observation coverage, low sensor angle, the absence of clouds or cloud shadow, and aerosol loading. Included in the product along with the nine reflectance bands are day of year, reflectance band quality, control, reflectance state quality assurance, relative azimuth angle, sensor zenith angle, and solar zenith angle layers. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&amp;amp;sat&#x3D;J2&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj209h1&quot;&gt;VJ209H1&lt;/h4&gt;
The 8-day Visible Infrared Imaging Radiometer Suite (VIIRS) Surface Reflectance (VJ209H1) Version 2 composite product provides an estimate of land surface reflectance from the NOAA-21 VIIRS sensor for three imagery bands (I1, I2, I3) at nominal 500 meter resolution (~463 meter). The 500 meter dataset is derived through resampling the native 375 meter VIIRS resolution in the L2 input product. The data are corrected for atmospheric conditions such as the effects of molecular gases, including ozone and water vapor, and for the effects of atmospheric aerosols. Each pixel represents the best possible Level 2G observation during an 8-day period, which is selected on the basis of high observation coverage, low sensor angle, the absence of clouds or cloud shadow, and aerosol loading. In addition to the three reflectance bands, this product includes a state quality assurance (QA) layer and a reflectance band quality layer. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&amp;amp;sat&#x3D;J2&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj209ga&quot;&gt;VJ209GA&lt;/h4&gt;
The Visible Infrared Imaging Radiometer Suite (VIIRS) daily surface reflectance (VJ209GA) Version 2 product provides an estimate of land surface reflectance from the NOAA-21 VIIRS sensor. Data are provided for three imagery bands (I1-I3) at nominal 500 meter resolution (&lt;del&gt;463 meter) and nine moderate resolution bands (M1-M5, M7, M8, M10, M11) at nominal 1 kilometer (&lt;/del&gt;926 meter) resolution. The 500 meter and 1 kilometer datasets are derived through resampling the native 375 meter and 750 meter VIIRS resolutions, respectively, in the Level 2 input product. These bands are corrected for atmospheric conditions such as the effects of molecular gases, including ozone and water vapor, and for the effects of atmospheric aerosols. The inputs to the surface reflectance algorithm are top-of-atmosphere reflectance for the VIIRS visible bands, the VIIRS cloud mask and aerosol product, aerosol optical thickness and atmospheric data obtained from the NOAA National Centers for Environmental Prediction (NCEP) reanalysis system. Along with the twelve reflectance bands are reflectance band quality, sensor azimuth angle, solar azimuth angle, sensor zenith angle, solar zenith angle, and observations layers. The reflectance layers from the VJ209GA data product are used as input data for many of the VIIRS land products. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&amp;amp;sat&#x3D;J2&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vj209cmg&quot;&gt;VJ209CMG&lt;/h4&gt;
The Visible Infrared Imaging Radiometer Suite (VIIRS) daily surface reflectance Climate Modeling Grid (VJ209CMG) Version 2 product provides an estimate of land surface reflectance from the NOAA-21 VIIRS sensor. Data are provided for three imagery bands (I1-I3) and nine moderate resolution bands (M1-M5, M7, M8, M10, M11) at 0.05 degree (~5,600 meter) resolution. The data are corrected for atmospheric conditions such as the effects of molecular gases, including ozone and water vapor, and for the effects of atmospheric aerosols. This product uses a weighted average of the best quality observation and is formatted as a CMG for use in climate simulation models. This product includes the twelve reflectance bands, five moderate resolution brightness temperature bands (M12-M16) and information layers representing relative azimuth angle, sensor zenith angle, solar zenith angle, reflectance band quality, time of day, and number mapping. Known Issues: For complete information about known issues please refer to the &lt;a href&#x3D;&quot;https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor&#x3D;VIIRS&amp;amp;sat&#x3D;J2&quot;&gt;MODIS/VIIRS Land Quality Assessment website&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA LANCE Project</title>
      <link>https://registry.opendata.aws/nasa-lance</link>
      <guid>https://registry.opendata.aws/nasa-lance</guid>
      <description>ATL13QL is the quick look version of ATL13 and is based on the same algorithms that generate the ATL13 final data products. Once final ATL13 files are available, the corresponding ATL13QL files are removed. ATL13QL provides along-track surface water products for inland water bodies, defined as lakes, reservoirs, bays, estuaries, rivers, and a 7 km near-shore buffer. Data parameters include surface water height statistics and related parameters including significant wave height, transect slope, subsurface signal attenuation, and shallow water bathymetry. Water surface heights are provided as both orthometric height and height referencing the WGS84 ellipsoid.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atl09ql&quot;&gt;ATL09QL&lt;/h4&gt;
ATL09QL is the quick look version of ATL09 and is based on the same algorithms that generate the ATL09 final data products. Once final ATL09 files are available, the corresponding ATL09QL files are removed. ATL09QL contains calibrated, attenuated backscatter profiles (CAB), layer-integrated attenuated backscatter, blowing snow, and other parameters including cloud and aerosol layer height and atmospheric characteristics. The data were acquired by the Advanced Topographic Laser Altimeter System (ATLAS) instrument on board the ICESat-2 observatory.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atl08ql&quot;&gt;ATL08QL&lt;/h4&gt;
ATL08QL is the quick look version of ATL08 and is based on the same algorithms that generate the ATL08 final data products. Once final ATL08 files are available, the corresponding ATL08QL files are removed. ATL08QL contains along-track estimates of terrain height, canopy height, and canopy cover, as well as beam and reference parameters. Data were acquired by the Advanced Topographic Laser Altimeter System (ATLAS) instrument on board the ICESat-2 observatory.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atl10ql&quot;&gt;ATL10QL&lt;/h4&gt;
ATL10QL is the quick look version of ATL10 and is based on the same algorithms that generate the ATL10 final data products. Once final ATL10 files are available, the corresponding ATL10QL files are removed. ATL10 contains along-track sea ice freeboard calculated for 10 km swath segments. The data were acquired by the Advanced Topographic Laser Altimeter System (ATLAS) instrument on board the ICESat-2 observatory.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atl07ql&quot;&gt;ATL07QL&lt;/h4&gt;
ATL07QL is the quick look version of ATL07 and is based on the same algorithms that generate the ATL07 final data products. Once final ATL07 files are available, the corresponding ATL07QL files are removed. ATL07 contains along-track sea surface height and sea ice height for segments of variable lengths for all beams as well as fixed 10-meter segments for strong beams. Heights are also computed using the DDA-Bifurcation algorithm for strong beams. The data were acquired by the Advanced Topographic Laser Altimeter System (ATLAS) instrument on board the ICESat-2 observatory.
&lt;br&gt;&lt;h4 id&#x3D;&quot;spl1btb_nrt&quot;&gt;SPL1BTB_NRT&lt;/h4&gt;
This Near Real-Time (NRT) data set corresponds to the standard SMAP L1B Radiometer Half-Orbit Time-Ordered Brightness Temperatures (SPL1BTB) product. The data provide calibrated estimates of time-ordered geolocated brightness temperature data measured by the Soil Moisture Active Passive (SMAP) passive microwave radiometer, the SMAP L-band radiometer. These Near Real-Time data are available within three hours of satellite observation. The data are created using the latest available ancillary data and spacecraft and antenna attitude data to reduce latency. The SMAP satellite orbits Earth every two to three days, providing half-orbit, ascending and descending, coverage from 86.4°S to 86.4°N in swaths 1000 km across. Data are stored for approximately two to three weeks. Thus, at any given time, users have access to at least fourteen consecutive days of Near Real-Time data through the NSIDC DAAC. Users deciding between the NRT and standard SMAP products should consider the immediacy of their needs versus the quality of the data required. Near real-time data are provided for operational needs whereas standard products meet the quality needs of scientific research. If latency is not a primary concern, users are encouraged to use the standard science product, SPL1BTB (&lt;a href&#x3D;&quot;https://doi.org/10.5067/ZHHBN1KQLI20&quot;&gt;https://doi.org/10.5067/ZHHBN1KQLI20&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;spl2smp_nrt&quot;&gt;SPL2SMP_NRT&lt;/h4&gt;
This Near Real-Time (NRT) data set corresponds to the standard SMAP L2 Radiometer Half-Orbit 36 km EASE-Grid Soil Moisture (SPL2SMP) product. The data provide estimates of global land surface conditions measured by the Soil Moisture Active Passive (SMAP) passive microwave radiometer, the SMAP L-band radiometer. These Near Real-Time data are available within three hours of satellite observation. The data are created using the latest available ancillary data and spacecraft and antenna attitude data to reduce latency. The SMAP satellite orbits Earth every two to three days, providing half-orbit, ascending and descending, coverage from 86.4°S to 86.4°N in swaths 1000 km across. Data are stored for approximately two to three weeks. Thus, at any given time, users have access to at least fourteen consecutive days of Near Real-Time data through the NSIDC DAAC. Users deciding between the NRT and standard SMAP products should consider the immediacy of their needs versus the quality of the data required. Near real-time data are provided for operational needs whereas standard products meet the quality needs of scientific research. If latency is not a primary concern, users are encouraged to use the standard science product SPL2SMP (&lt;a href&#x3D;&quot;https://doi.org/10.5067/LPJ8F0TAK6E0&quot;&gt;https://doi.org/10.5067/LPJ8F0TAK6E0&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.nsidc.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA LBA-ECO Project</title>
      <link>https://registry.opendata.aws/nasa-lba-eco</link>
      <guid>https://registry.opendata.aws/nasa-lba-eco</guid>
      <description>This data set provides measurements from the Amazonian Aerosol Characterization Experiment (AMAZE-08) carried out during the wet season from February 4 to March 21, 2008 in the central Amazon Basin. Aerosol and atmospheric samples and measurements were collected at Tower TT34 located 60 km NNW of downtown Manaus, and at Tower K34, located 1.6 km from the TT34 site. Physical characterization of aerosols included size, mass, and number distributions and light scattering properties. Chemical characterization included mass concentrations of organics, major anions and cations, and trace metals. Aerosol sources were estimated with measurements of black carbon and biogenic particles. Meteorological and atmospheric conditions including relative humidity, temperature, wind speed and direction, rain, photosynthetically active radiation (PAR), downward and upward solar irradiance, and condensation nuclei were measured. Atmospheric trace gases and volatile organic compounds (VOCs) were sampled and analyzed.
&lt;br&gt;&lt;h4 id&#x3D;&quot;amazon_precip_228&quot;&gt;amazon_precip_228&lt;/h4&gt;
The Amazon River Basin precipitation grids were derived from data which was collected daily by the gauging network operated by the Divisao Nacional de Aguas e Energia Eletrica (DNAEE, SGAN 603 Modulo J, Anexo DNC, CEP 70.830-030 Brasilia DF, Brazil). The DNAEE provided the Earth Observing System (EOS) Regional Amazon Model (EOSRAM) project with this data for cooperative analysis. The project includes both empirical and modeling studies of rainfall and runoff from sample hillslopes to the entire Amazon basin. The precipitation data is 0.2 degree gridded monthly precipitation data. The data spans the period from January 1972 to December 1992.
&lt;br&gt;&lt;h4 id&#x3D;&quot;jers-1_sar_grfm_amazon_mosaics_1280&quot;&gt;JERS-1_SAR_GRFM_Amazon_Mosaics_1280&lt;/h4&gt;
This data set provides ~100-m resolution image mosaics of South America acquired during the low flood season between September and December 1995 and during the high flood season between May and July of 1996. The images cover the same areas during both seasons and were obtained from the Japanese Earth Resources Satellite 1 (JERS-1) Synthetic Aperture Radar (SAR) of the National Space Development Agency of Japan (NASDA). The data were mosaicked into 34 tiles for each season, each consisting of about 50 JERS-1 scenes. This data set constitutes the first-ever high-resolution and single season coverage of the entire Amazon River Basin, made possible by the cloud penetrating properties of the radar sensor. The images are from the original JERS-1 SAR Global Rain Forest Mapping Project. This data set contains 66 files in GeoTIFF (.tiff) format. There are 32 files for the low flood season and 34 files for the high flood season.
&lt;br&gt;&lt;h4 id&#x3D;&quot;basin_border_670&quot;&gt;basin_border_670&lt;/h4&gt;
This data set is an expanded version of the Costa et al. (2000) data set and consists of a single grid with values of 1 for cells within the basins and 0 for cells outside. The resolution of the data set is 5 x 5 min (approximately 9 x 9 km). The area of this data set is consistent with the study area of the Large Scale Biosphere-Atmosphere Experiment in Amazonia (LBA) in South America. The data file is in ASCII GRID format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;legal_amazon_mask_671&quot;&gt;legal_amazon_mask_671&lt;/h4&gt;
The Legal Amazon of Brazil is defined by law to include the states of Acre, Amapá, Amazonas, Pará, Rondônia, Roraima, Mato Grosso, Maranhão, and Tocantins [Fundãcao Instituto Brasileiro de Geografia e Estatística (IBGE) 1991]. This is the definition used in generating the Legal Amazon mask. The 8-km Legal Amazon mask was generated by Christopher Potter at the Ecosystem Science and Technology Branch of the Earth Science Division at NASA Ames Research Center (Potter and Brooks-Genovese 1999). The mask was generated from the Digital Chart of the World available from Environmental Systems Research Institute, Inc. (ESRI). The mask is available in ASCII GRID format. The README file accompanying the mask has more information regarding data format. More information can be found at &lt;a href&#x3D;&quot;ftp://daac.ornl.gov/data/lba/human_dimensions/legal_amazon_mask/comp/legamazon_readme.pdf&quot;&gt;ftp://daac.ornl.gov/data/lba/human_dimensions/legal_amazon_mask/comp/legamazon_readme.pdf&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;olson_672&quot;&gt;olson_672&lt;/h4&gt;
This data set is a subset of Olson et al. (1985, 2000) &amp;quot;Major World Ecosystem Complexes Ranked by Carbon in Live Vegetation.&amp;quot; This subset was created for the study area of the Large Scale Biosphere-Atmosphere Experiment in Amazonia (LBA) in South America (i.e., latitude 10° N to 25° S, longitude 30° to 85° W). The data are in ASCII GRID format. &amp;quot;Major World Ecosystem Complexes Ranked by Carbon in Live Vegetation&amp;quot; is a computerized database used to generate a global vegetation map of 44 different land ecosystem complexes (mosaics of vegetation or landscapes) comprising seven broad groups. The map is derived from patterns of preagricultural vegetation, modern areal surveys, and intensive biomass data from research sites. Work on the database was begun in 1960 and completed in 1980. Ecosystem complexes are defined for each 0.5-degree grid cell, reflecting the major climatic, topographic, and land-use patterns. Numeric codes are assigned to each vegetation type. Classifications include natural as well as human managed/modified complexes such as mainly cropped, residential, commercial, and park. The complexes are ranked by estimated organic carbon in the mass of live plants given in units of kilograms of carbon per square meter. Counting the cells of each type and adding their areas give total area estimates for the ecosystem complexes. Multiplying by carbon estimates gives corresponding estimates of carbon by ecosystem complex with in the LBA study area. The results help define the role of the terrestrial biosphere in the global carbon cycle. Information about the ecosystem classifications, as well as the procedure used to create the LBA subset can be found at &lt;a href&#x3D;&quot;ftp://daac.ornl.gov/data/lba/carbon_dynamics/olson/comp/olson_readme.pdf&quot;&gt;ftp://daac.ornl.gov/data/lba/carbon_dynamics/olson/comp/olson_readme.pdf&lt;/a&gt;. LBA was a cooperative international research initiative led by Brazil. NASA was a lead sponsor for several experiments. LBA was designed to create the new knowledge needed to understand the climatological, ecological, biogeochemical, and hydrological functioning of Amazonia; the impact of land use change on these functions; and the interactions between Amazonia and the Earth system. More information about LBA can be found at &lt;a href&#x3D;&quot;http://www.daac.ornl.gov/LBA/misc_amazon.html&quot;&gt;http://www.daac.ornl.gov/LBA/misc_amazon.html&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;willmott_673&quot;&gt;willmott_673&lt;/h4&gt;
This data set is a subset of a 0.5-degree gridded temperature and precipitation data set for South America (Willmott and Webber 1998). This subset was created for the study area of the Large Scale Biosphere-Atmosphere Experiment in Amazonia (LBA), defined as 10° N to 25° S, 30° to 85° W. The data are in ASCII GRID format. The data consist of the following: Monthly mean air temperature time series (1960-1990), in degrees C: monthly mean air temperatures for 1960-1990 cross validation errors associated with time series monthly mean air temperatures for 1960-1990, DEM assisted interpolation cross validation errors associated with DEM assisted interpolation time series Monthly mean air temperature climatology, in degrees C: climatic means of monthly and annual air temperatures cross validation errors associated with climatic means climatic means of monthly and annual mean air temperatures, DEM assisted interpolation cross validation errors associated with DEM assisted interpolation climatic means Monthly total precipitation time series (1960-1990), in millimeters: monthly precipitation totals for 1960-1990 cross validation errors associated with time series monthly precipitation totals for 1960-1990, climatologically aided interpolation cross validation errors associated with climatologically aided interpolation time series Monthly total precipitation climatology, in millimeters: climatic means of monthly and annual precipitation totals cross validation errors associated with climatic means More information about the full data set can be found at &amp;quot;Willmott, Matsuura, and Collaborators&amp;#39; Global Climate Resource Pages&amp;quot; (&lt;a href&#x3D;&quot;http://climate.geog.udel.edu/~climate&quot;&gt;http://climate.geog.udel.edu/~climate&lt;/a&gt;) at the University of Delaware. To obtain the original documentation and data, follow the link for &amp;quot;Available Climate Data,&amp;quot; register or sign in, and follow the link for &amp;quot;South American Climate Data.&amp;quot; Information on the LBA subset can be found at &lt;a href&#x3D;&quot;ftp://daac.ornl.gov/data/lba/physical_climate/willmott/comp/willmott_readme.pdf&quot;&gt;ftp://daac.ornl.gov/data/lba/physical_climate/willmott/comp/willmott_readme.pdf&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lba_isric_wise_701&quot;&gt;lba_isric_wise_701&lt;/h4&gt;
The data set consists of a subset of the ISRIC-WISE global data set of derived soil properties for the study area of the Large Scale Biosphere-Atmosphere Experiment in Amazonia (LBA) in South America (i.e., longitude 85 to 30 degrees W, latitude 25 degrees S to 10 degrees N).The World Inventory of Soil Emission Potentials (WISE) database currently contains data for over 4300 soil profiles collected mostly between 1950 and 1995. This database has been used to generate a series of uniform data sets of derived soil properties for each of the 106 soil units considered in the Soil Map of the World (FAO-UNESCO, 1974). These data sets were then linked to a 1/2 degree longitude by 1/2 degree latitude version of the edited and digital Soil Map of the World (FAO, 1995) to generate GIS raster image files for the following variables:Total available water capacity (mm water per 1 m soil depth)Soil organic carbon density (kg C/m&lt;strong&gt;2 for 0-30 cm depth range)Soil organic carbon density (kg C/m&lt;/strong&gt;2 for 0-100 cm depth range)Soil carbonate carbon density (kg C/m**2 for 0-100 cm depth range)Soil pH (0-30 cm depth range)Soil pH (30-100 cm depth range)LBA was designed to create the new knowledge needed to understand the climatological, ecological, biogeochemical, and hydrological functioning of Amazonia; the impact of land use change on these functions; and the interactions between Amazonia and the Earth system. LBA was a cooperative international research initiative led by Brazil and NASA was a lead sponsor for several experiments. More information about LBA and links to other LBA project sites can be found at &lt;a href&#x3D;&quot;http://www.daac.ornl.gov/LBA/misc_amazon.html&quot;&gt;http://www.daac.ornl.gov/LBA/misc_amazon.html&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;soller_wetlands_674&quot;&gt;soller_wetlands_674&lt;/h4&gt;
This data set consists of a subset of a 1-degree gridded global freshwater wetlands database (Stillwell-Soller et al. 1995). This subset was created for the study area of the Large Scale Biosphere-Atmosphere Experiment in Amazonia (LBA) in South America (i.e., 10° N to 25° S, 30° to 85° W). The data are in ASCII GRID format. The global freshwater wetlands database was assembled from two data sets: Aselman and Crutzen&amp;#39;s (1989) wetlands data set and Klinger&amp;#39;s political Alaska data set (pers. comm. to L. M. Stillwell-Soller, 1995). The aim of Stillwell-Soller&amp;#39;s global data set was to provide an accurate, comprehensive and uniform set of files for convenient specification of wetlands in global climate models. The main source of data was Aselman and Crutzen&amp;#39;s global maps of percent cover for a variety of wetlands categories at 2.5-degree latitude by 5-degree longitude resolution. There was some reorganization for seasonally varying categories. Aselman and Crutzen&amp;#39;s data were interpolated to a standard 1-degree by 1-degree grid through bilinear interpolation. Their data were geographically complete except for the Alaskan region, for which Klinger&amp;#39;s data set provided values. More information can be found at &lt;a href&#x3D;&quot;ftp://daac.ornl.gov/data/lba/land_use_land_cover_change/soller_wetlands/comp/soller_readme.pdf&quot;&gt;ftp://daac.ornl.gov/data/lba/land_use_land_cover_change/soller_wetlands/comp/soller_readme.pdf&lt;/a&gt;. LBA was a cooperative international research initiative led by Brazil. NASA was a lead sponsor for several experiments. LBA was designed to create the new knowledge needed to understand the climatological, ecological, biogeochemical, and hydrological functioning of Amazonia; the impact of land use change on these functions; and the interactions between Amazonia and the Earth system. More information about LBA can be found at &lt;a href&#x3D;&quot;http://www.daac.ornl.gov/LBA/misc_amazon.html&quot;&gt;http://www.daac.ornl.gov/LBA/misc_amazon.html&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lba_ghcn_702&quot;&gt;lba_ghcn_702&lt;/h4&gt;
This data set consists of a subset of the Global Historical Climatology Network (GHCN) Version 1 database for the study area of the Large Scale Biosphere-Atmosphere Experiment in Amazonia (LBA) in South America (i.e., longitude 85 to 30 degrees W, latitude 25 degrees S to 10 degrees N). There are three files available, one each for precipitation, temperature, and pressure data. Within this subset the oldest data date from 1832 and the most recent from 1990.The GHCN V1 database contains monthly temperature, precipitation, sea-level pressure, and station-pressure data for thousands of meteorological stations worldwide. The database was compiled from pre-existing national, regional, and global collections of data as part of the Global Historical Climatology Network (GHCN) project, the goal of which was to produce, maintain and make available a comprehensive global surface baseline climate data set for monitoring climate and detecting climate change. It contains data from roughly 6000 temperature stations, 7500 precipitation stations, 1800 sea-level pressure stations, and 1800 station-pressure stations. Each station has at least 10 years of data; 40% have more than 50 years of data. Spatial coverage is good over most of the globe, particularly for the United States and Europe. Data gaps are evident over the Amazon rainforest, the Sahara desert, Greenland, and Antarctica. The earliest station data are from 1697; the most recent are from 1990. The database was created from 15 source data sets including:The National Climatic Data Center&amp;#39;s (NCDC&amp;#39;s) World Weather Records,CAC&amp;#39;s Climate Anomaly Monitoring System (CAMS),NCAR&amp;#39;s World Monthly Surface Station Climatology,CIRES&amp;#39; (Eischeid/Diaz) Global precipitation data set,P. Jones&amp;#39; Temperature data base for the world, andS. Nicholson&amp;#39;s African precipitation database. Quality Control of the GHCN V1 database included visual inspection of graphs of all station time series, tests for precipitation digitized 6 months out of phase, tests for different stations having identical data, and other tests. This detailed analysis has revealed that most stations (95% for temperature and precipitation, 75% for pressure) contain high-quality data. However, gross data-processing errors (e.g., keypunch problems) and discontinuous inhomogeneities (e.g., station relocations and instrumentation changes) do characterize a small number of stations. All major data processing problems have been flagged (or corrected, when possible). Similarly, all major inhomogeneities have been flagged, although no homogeneity corrections were applied.LBA was designed to create the new knowledge needed to understand the climatological, ecological, biogeochemical, and hydrological functioning of Amazonia; the impact of land use change on these functions; and the interactions between Amazonia and the Earth system. LBA was a cooperative international research initiative led by Brazil and NASA was a lead sponsor for several experiments. More information about LBA and links to other LBA project sites can be found at &lt;a href&#x3D;&quot;http://www.daac.ornl.gov/LBA/misc_amazon.html&quot;&gt;http://www.daac.ornl.gov/LBA/misc_amazon.html&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;historical_croplands_675&quot;&gt;historical_croplands_675&lt;/h4&gt;
This data set is a subset of a global croplands data set (Ramankutty and Foley 1999a). The subset was created for the study area of the Large Scale Biosphere-Atmosphere Experiment in Amazonia (LBA) in South America (i.e., 10° N to 25° S, 30° to 85° W). The data are in ASCII GRID format at 5-min resolution. Navin Ramankutty and Jonathan Foley, of the Center for Sustainability and the Global Environment (SAGE) at the University of Wisconsin, developed a global, spatially explicit data set of reconstructed historical croplands from 1700 to 1992. The method for historical reconstruction used a simple algorithm that linked contemporary satellite data and historical cropland inventory data. A spatially explicit croplands data set for 1992 was first derived by calibrating a satellite-derived land cover classification data set against cropland inventory data for 1992. This derived data set was then used within a simple land cover change model, along with historical cropland inventory data, to derive spatially explicit maps of historical croplands. The global data set was restricted to a representation of permanent croplands (i.e., excluding shifting cultivation), which follows the Food and Agriculture Organization (FAO) definition of arable lands and permanent crops. Data values represent fraction of grid cell in croplands. Data for the LBA study area are available for the years 1900, 1910, 1920, 1930, 1940, 1950, 1960, 1970, 1980, 1990, and 1992. Although the global croplands data set contains data representing croplands since 1700, essentially no croplands were in the LBA study area until 1900. Data from previous years were excluded at the suggestion of the data originator. More information can be found at &lt;a href&#x3D;&quot;ftp://daac.ornl.gov/data/lba/land_use_land_cover_change/historical_croplands/comp/uwcrop_readme.pdf&quot;&gt;ftp://daac.ornl.gov/data/lba/land_use_land_cover_change/historical_croplands/comp/uwcrop_readme.pdf&lt;/a&gt;. LBA was a cooperative international research initiative led by Brazil. NASA was a lead sponsor for several experiments. LBA was designed to create the new knowledge needed to understand the climatological, ecological, biogeochemical, and hydrological functioning of Amazonia; the impact of land use change on these functions; and the interactions between Amazonia and the Earth system. More information about LBA can be found at &lt;a href&#x3D;&quot;http://www.daac.ornl.gov/LBA/misc_amazon.html&quot;&gt;http://www.daac.ornl.gov/LBA/misc_amazon.html&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gghydro_676&quot;&gt;gghydro_676&lt;/h4&gt;
This subset of the Global Hydrographic data set (GGHYDRO) Release 2.2 for the study area of the Large Scale Biosphere-Atmosphere Experiment in Amazonia (LBA) in South America (i.e., longitude 85 deg to 30 deg W, latitude 25 deg S to 10 deg N) is organized into 19 files containing terrain type, stream frequency counts, major drainage basins, main features of the cryosphere surface, and ice/water runoff per year for the entire Earth&amp;#39;s surface at a spatial resolution of 1- degree longitude by 1-degree latitude. The data are provided in both ASCII GRID and binary image file formats.More information and selected thumbnails images can be found at: &lt;a href&#x3D;&quot;ftp://daac.ornl.gov/data/lba/surf_hydro_and_water_chem/gghydro/comp/README&quot;&gt;ftp://daac.ornl.gov/data/lba/surf_hydro_and_water_chem/gghydro/comp/README&lt;/a&gt;. Exposed land not covered by swamp, intermittent water bodies, glacier ice, sand dunes, saltmarsh or salt flats (LAND)2. Perennial freshwater lakes (FLAK)3. Swamp, marsh and other wetlands(SWMP)4. Saltwater, whether marine or terrestrial (SLTW)5. Intermittent water bodies (ILAK)6. Glacier ice, including shelf ice but excluding pack ice (GLAC)7. Sand dunes (DUNE)8. Saltmarsh (SMRS)9. Salt flats (SFLT)10. Land + Swamp + Sand dunes + Saltmarsh (DSRF)11. Perennial rivers (FRIV)12. Intermittent rivers (IRIV)13. Land mask (MS05)14. Major drainage basins (BAS1)15. Smaller drainage basins (BAS2)16. Main features of the cryosphere (CRYO)17. Surface runoff of water (kg/m&lt;strong&gt;2/yr) (RNOF)18. Estimated root-mean-square error of RNOF (%) (RNER)19. Runoff of ice ( kg/m&lt;/strong&gt;2/yr ) (RICE)
&lt;br&gt;&lt;h4 id&#x3D;&quot;land_cover_data_1deg_677&quot;&gt;land_cover_data_1deg_677&lt;/h4&gt;
This data set consists of a subset for the study area of the Large Scale Biosphere-Atmosphere Experiment in Amazonia (LBA) in South America (i.e., longitude 85 deg to 30 deg W, latitude 25 deg S to 10 deg N) of the University of Maryland (UMD) 1-degree Global Land Cover product in ASCII GRID and binary image formats.The UMD 1-degree Global Land Cover product was produced by researchers at the Laboratory for Global Remote Sensing Studies (LGRSS) at UMD. The product is based on Advanced Very High Resolution Radiometer (AVHRR) maximum monthly composites for 1987 of Normalized Difference Vegetation Index (NDVI) values at approximately 8-km resolution, averaged to one-by-one degree resolution. This coarse- resolution data set was used as the basis for a supervised classification of eleven cover types that broadly represent the major biomes of the world. Because of missing values at high latitudes, the Pathfinder AVHRR data set for 1987 for summer monthly NDVI and red reflectance values were used to distinguish the following cover types: tundra, high latitude deciduous forest and woodland, coniferous evergreen forest and woodland.The 1-degree global land cover product is available for download from the Global Land Cover Facility (GLCF)[&lt;a href&#x3D;&quot;http://glcf.umiacs.umd.edu/data/landcover/index.shtml%5D&quot;&gt;http://glcf.umiacs.umd.edu/data/landcover/index.shtml]&lt;/a&gt; web site. The data are available as a global coverage in both binary and ASCII format. Additional information and references on this data set can be found at the GLCF web site as well as at the LGRSS web site (link provided at the GLCF web site ) and in the readme file found along with the data [ &lt;a href&#x3D;&quot;ftp://daac.ornl.gov/data/lba/land_use_change/land_cover_data_1deg/comp/README%5D&quot;&gt;ftp://daac.ornl.gov/data/lba/land_use_change/land_cover_data_1deg/comp/README]&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;land_cover_data_1km_678&quot;&gt;land_cover_data_1km_678&lt;/h4&gt;
This data set is a subset of Hansen et al. (1999), &amp;quot;1 km Global Land Cover Data Set Derived from AVHRR,&amp;quot; which was developed at the Laboratory for Global Remote Sensing Studies (LGRSS) at the University of Maryland. This subset was created for the study area of the Large Scale Biosphere-Atmosphere Experiment in Amazonia (LBA) in South America (i.e., latitude 10 N to 25 S, longitude 30 to 85 W). The data are in ASCII GRID file format. In recent years, researchers have increasingly turned to remotely sensed data to improve the accuracy of data sets that describe the geographic distribution of land cover at regional and global scales. To develop improved methodologies for global land cover classifications as well as to provide global land cover products for immediate use in global change research, LGRSS researchers have employed the NASA/NOAA Pathfinder AVHRR Land (PAL) data set with a spatial resolution of 1 km. The PAL data set has a record length of 14 years (1981-1994), providing the ability to test the stability of classification algorithms. The PAL data set includes red, infrared, and thermal bands in addition to the Normalized Difference Vegetation Index (NDVI). Inclusion of these additional bands improves discrimination between cover types. The LGRSS researchers&amp;#39; aim was to develop and validate global land cover data sets and to develop advanced methodologies for more realistically describing the vegetative land surface based on satellite data. The 1-km global land cover product was created from 1992-1993 local area coverage (LAC) AVHRR data. The global land cover product is available for download from the University of Maryland&amp;#39;s Global Land Cover Facility (GLCF) Web site (&lt;a href&#x3D;&quot;http://glcf.umiacs.umd.edu/data/landcover/index.shtml&quot;&gt;http://glcf.umiacs.umd.edu/data/landcover/index.shtml&lt;/a&gt;). Forty-one metrics were developed to describe global vegetation phenology, and these data were used to make the 1-km land cover map. The final product contains 13 land cover classes. More information can be found at &lt;a href&#x3D;&quot;ftp://daac.ornl.gov/data/lba/land_use_land_cover_change/land_cover_data_1km/comp/glcf1km_readme.pdf&quot;&gt;ftp://daac.ornl.gov/data/lba/land_use_land_cover_change/land_cover_data_1km/comp/glcf1km_readme.pdf&lt;/a&gt;. LBA was a cooperative international research initiative led by Brazil. NASA was a lead sponsor for several experiments. LBA was designed to create the new knowledge needed to understand the climatological, ecological, biogeochemical, and hydrological functioning of Amazonia; the impact of land use change on these functions; and the interactions between Amazonia and the Earth system. More information about LBA can be found at &lt;a href&#x3D;&quot;http://www.daac.ornl.gov/LBA/misc_amazon.html&quot;&gt;http://www.daac.ornl.gov/LBA/misc_amazon.html&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;discover_land_cover_679&quot;&gt;DISCover_land_cover_679&lt;/h4&gt;
The data set consists of a LBA study area subset of the IGBP DISCover Data Set. The DISCover data set is one data set contained within the Global Land Cover Characteristics Data Base. The U.S. Geological Survey (USGS), the University of Nebraska-Lincoln (UNL), and the European Commission&amp;#39;s Joint Research Centre (JRC) have generated a 1-km resolution global land cover characteristics data base for use in a wide range of environmental research and modeling applications. The global land cover characteristics data base was developed on a continent-by-continent basis. All continental data bases share the same map projections (Interrupted Goode Homolosine and Lambert Azimuthal Equal Area), have 1-km nominal spatial resolution, and are based on 1-km Advanced Very High Resolution Radiometer (AVHRR) data spanning April 1992 through March 1993. Each data base contains unique elements based on the geographic aspects of the specific continent. In addition, a core set of derived thematic maps produced through the aggregation of seasonal land cover regions are included in each continental data base. The continental data bases are combined to make six global data sets, each representing a different landscape based on a particular classification legend. The following derived data sets are included in the global land cover data base: * Global Ecosystems (Olson, 1994a, 1994b) * IGBP Land Cover Classification (Belward, 1996) * U.S. Geological Survey Land Use/Land Cover System(Anderson &amp;amp; others, 1976) * Simple Biosphere Model (Sellers and others, 1986) * Simple Biosphere 2 Model (Sellers and others, 1996) * Biosphere-Atmosphere Transfer Scheme (Dickinson and others, 1986) The legends for each of these derived data sets can be found in the documentation accompanying the data. For a description of the methodology for the global data base, see the global readme file found under the EROS Data Center DAAC home page (&lt;a href&#x3D;&quot;http://edcwww.cr.usgs.gov/landdaac/glcc/glcc.html&quot;&gt;http://edcwww.cr.usgs.gov/landdaac/glcc/glcc.html&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;land_cover_data_8km_680&quot;&gt;land_cover_data_8km_680&lt;/h4&gt;
This data set is a subset of an 8-km global land cover product (DeFries et al. 1998). This subset was created for the study area of the Large Scale Biosphere-Atmosphere Experiment in Amazonia (LBA) in South America (i.e., latitude 10° N to 25° S, longitude 30° to 85° W). The data are in ASCII GRID file format. To develop improved methodologies for global land cover classifications as well as to provide global land cover products for immediate use in global change research, researchers at the Laboratory for Global Remote Sensing Studies at the University of Maryland employed the NASA/NOAA Pathfinder AVHRR Land (PAL) data set with a spatial resolution of 8 km. The PAL data set has a length of record of 14 years (1981-1994), providing the ability to test the stability of classification algorithms. Furthermore, the data set includes red, infrared, and thermal bands in addition to the Normalized Difference Vegetation Index (NDVI). Inclusion of these additional bands improves discrimination between cover types. The project&amp;#39;s aim was to develop and validate global land cover data sets and to develop advanced methodologies for more realistically describing the vegetative land surface based on satellite data. The global land cover product (Defries et al. 1998) was derived by testing several metrics that describe the temporal dynamics of vegetation over an annual cycle. These metrics were applied to 1984 PAL data at 8-km resolution to derive a global land cover classification product using a decision tree classifier. The final product contains 13 land cover classes. The original 8-km global land cover product is available for download from the University of Maryland&amp;#39;s Global Land Cover Facility (GLCF) Web site (&lt;a href&#x3D;&quot;http://glcf.umiacs.umd.edu/data/landcover/index.shtml&quot;&gt;http://glcf.umiacs.umd.edu/data/landcover/index.shtml&lt;/a&gt;). Additional information and references on this data set can be found at the GLCF Web site, as well as at the LGRSS Web site (&lt;a href&#x3D;&quot;http://www.geog.umd.edu/LGRSS/intro.html&quot;&gt;http://www.geog.umd.edu/LGRSS/intro.html&lt;/a&gt;). More information can be found at &lt;a href&#x3D;&quot;ftp://daac.ornl.gov/data/lba/land_use_land_cover_change/comp/land_cover_data_8km/glcf8km_readme.pdf&quot;&gt;ftp://daac.ornl.gov/data/lba/land_use_land_cover_change/comp/land_cover_data_8km/glcf8km_readme.pdf&lt;/a&gt;. LBA was a cooperative international research initiative led by Brazil. NASA was a lead sponsor for several experiments. LBA was designed to create the new knowledge needed to understand the climatological, ecological, biogeochemical, and hydrological functioning of Amazonia; the impact of land use change on these functions; and the interactions between Amazonia and the Earth system. More information about LBA can be found at &lt;a href&#x3D;&quot;http://www.daac.ornl.gov/LBA/misc_amazon.html&quot;&gt;http://www.daac.ornl.gov/LBA/misc_amazon.html&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;leemans_cramer_681&quot;&gt;leemans_cramer_681&lt;/h4&gt;
This data set is a subset of Cramer and Leemans&amp;#39; (2001) global database of mean monthly climatology, which contains monthly averages of mean temperature, temperature range, precipitation, rain days, and sunshine hours for terrestrial areas during 1931-1960. This subset was created for the Large Scale Biosphere-Atmosphere Experiment in Amazonia (LBA) in South America (i.e., latitude 10° N to 25° S, longitude 30° to 85° W). The data are presented at 0.5-degree latitude/longitude resolution in ASCII GRID file format. Cramer and Leemans (2001, Version 2.1) constituted a major update of an earlier database, Leemans and Cramer (1991). The new version was generated from a larger database by means of the partial thin-plate splining algorithm developed by Michael F. Hutchinson, Canberra (Hutchinson and Bischof 1983). Version 2.1 has been used widely, notably by all groups participating in the International Geosphere-Biosphere Programme&amp;#39;s Net Primary Productivity (NPP) model intercomparison (Olsen et al. 2001). More information about the data can be found at &lt;a href&#x3D;&quot;ftp://daac.ornl.gov/data/lba/physical_climate/leemans_cramer/comp/cramer_lmns_readme.pdf&quot;&gt;ftp://daac.ornl.gov/data/lba/physical_climate/leemans_cramer/comp/cramer_lmns_readme.pdf&lt;/a&gt;. LBA was a cooperative international research initiative led by Brazil. NASA was a lead sponsor for several experiments. LBA was designed to create the new knowledge needed to understand the climatological, ecological, biogeochemical, and hydrological functioning of Amazonia; the impact of land use change on these functions; and the interactions between Amazonia and the Earth system. More information about LBA be found at &lt;a href&#x3D;&quot;http://www.daac.ornl.gov/LBA/misc_amazon.html&quot;&gt;http://www.daac.ornl.gov/LBA/misc_amazon.html&lt;/a&gt;. tabase is a major update of the Leemans and Cramer database (Leemans and Cramer 1991). It contains long-term monthly averages, for the period 1931-1960, of mean temperature, temperature range, precipitation, rain days and sunshine hours for the terrestrial surface of the globe, gridded at 0.5-degree longitude/latitude resolution. It was generated from a larger database, using the partial thin-plate splining algorithm developed by Michael F. Hutchinson, Canberra (Hutchinson and Bischof 1983). The current version is 2.1--this is the same version that is currently used widely around the globe, notably by all groups participating in the IGBP NPP model intercomparison.More information can be found at: &lt;a href&#x3D;&quot;ftp://daac.ornl.gov/data/lba/physical_climate/leemans_cramer/comp/README&quot;&gt;ftp://daac.ornl.gov/data/lba/physical_climate/leemans_cramer/comp/README&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;zinke_soil_683&quot;&gt;Zinke_soil_683&lt;/h4&gt;
The data set contains a subset of a global organic soil carbon and nitrogen data set (Zinke et al. 1986). The subset was created for the study area of the Large Scale Biosphere-Atmosphere Experiment in Amazonia (LBA) in South America (i.e., 10 N to 25 S, 30 to 85 W). The point data are available in three formats: a comma-delimited ASCII file (.csv), an ESRI shapefile, and an ESRI export file (.e00). The data for the global data set (Zinke et al. 1986) were obtained from soil surveys conducted by Zinke in 1965-1984 and from soil survey literature. The main samples for laboratory analyses were collected at uniform soil increments and included bulk density determinations. Many samples reported in the literature did not have uniform soil increments or bulk density determinations. Only soil profiles that had been sampled either to a meter in depth or to actual depth were included in this database from soil survey literature. When carbon content was known but bulk densities were absent from soil samples reported in the literature, densities were estimated by regression analysis on the basis of the relationship between organic carbon content and measured bulk density in 1800 soil profiles for which bulk densities were known. Further information can be found at &lt;a href&#x3D;&quot;ftp://daac.ornl.gov/data/lba/carbon_dynamics/Zinke_soil/comp/zinke_readme.pdf&quot;&gt;ftp://daac.ornl.gov/data/lba/carbon_dynamics/Zinke_soil/comp/zinke_readme.pdf&lt;/a&gt;. LBA was a cooperative international research initiative led by Brazil. NASA was a lead sponsor for several experiments. LBA was designed to create the new knowledge needed to understand the climatological, ecological, biogeochemical, and hydrological functioning of Amazonia; the impact of land use change on these functions; and the interactions between Amazonia and the Earth system. More information about LBA can be found at &lt;a href&#x3D;&quot;http://www.daac.ornl.gov/LBA/misc_amazon.html&quot;&gt;http://www.daac.ornl.gov/LBA/misc_amazon.html&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;potential_vegetation_684&quot;&gt;potential_vegetation_684&lt;/h4&gt;
The data set consists of a subset for the study area of the Large Scale Biosphere-Atmosphere Experiment in Amazonia (LBA) in South America (i.e., longitude 85 deg to 30 deg W, latitude 25 deg S to 10 deg N) of the 5-min resolution Global Potential Vegetation data set developed by Navin Ramankutty and Jon Foley at the University of Wisconsin. Data are available in both ASCII GRID and binary image file formats.The original map was derived at a 5-min resolution and contains natural vegetation classified into 15 types. This data set is derived mainly from the DISCover land cover data set, with the regions dominated by land use filled using the vegetation data set of Haxeltine and Prentice (1996). The data set represents the world&amp;#39;s potential vegetation (i.e., vegetation that would most likely exist now in the absence of human activities), and not necessarily natural pre-settlement vegetation. This is because human activities such as fire suppression have modified the stages of succession at which vegetation communities exist.More information can be found at: &lt;a href&#x3D;&quot;ftp://daac.ornl.gov/data/lba/land_use_change/potential_vegetation/comp/README&quot;&gt;ftp://daac.ornl.gov/data/lba/land_use_change/potential_vegetation/comp/README&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sage_685&quot;&gt;sage_685&lt;/h4&gt;
This data set is a subset of a global river discharge data set by Coe and Olejniczak (1999). The subset was created for the study area of the Large Scale Biosphere-Atmosphere Experiment in Amazonia (LBA) in South America (i.e., 10° N to 25° S, 30° to 85° W). The global river discharge data set (Coe and Olejniczak 1999), formerly known as the &amp;quot;Climate, People, and Environment Program (CPEP) Global River Discharge Database,&amp;quot; is a compilation of monthly mean discharge data for more than 2600 sites worldwide. The data were compiled from RivDIS Version 1.1 (Vorosmarty et al. 1998), the U.S. Geological Survey, and the Brazilian National Department of Water and Electrical Energy. The period of record for the sites varies from 3 years to greater than 100. The purpose of the global compilation is to provide detailed hydrographic information for the climate research community in as general a format as possible. Data are given in units of meters cubed per second (m**3/sec) and are in ASCII format. Data from stations that had less than 3 years of information or that had a basin area less than 5000 square kilometers were excluded from the global data set. Thus, the data sources may include more sites than the data set by Coe and Olejniczak (1999). Users should refer to the data originators for further documentation on the source data. More information, a map of discharge sites, and a clickable site data table can be found at &lt;a href&#x3D;&quot;ftp://daac.ornl.gov/data/lba/surf_hydro_and_water_chem/sage/comp/sagedischarge_readme.pdf&quot;&gt;ftp://daac.ornl.gov/data/lba/surf_hydro_and_water_chem/sage/comp/sagedischarge_readme.pdf&lt;/a&gt;. LBA was a cooperative international research initiative led by Brazil. NASA was a lead sponsor for several experiments. LBA was designed to create the new knowledge needed to understand the climatological, ecological, biogeochemical, and hydrological functioning of Amazonia; the impact of land use change on these functions; and the interactions between Amazonia and the Earth system. Further information about LBA can be found at &lt;a href&#x3D;&quot;http://www.daac.ornl.gov/LBA/misc_amazon.html&quot;&gt;http://www.daac.ornl.gov/LBA/misc_amazon.html&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lba_tree_cover-1km_686&quot;&gt;lba_tree_cover-1km_686&lt;/h4&gt;
The data set consists of a subset for the study area of the Large Scale Biosphere-Atmosphere Experiment in Amazonia (LBA) in South America (i.e., longitude 85 deg to 30 deg W, latitude 25 deg S to 10 deg N) of the 1km Global Tree Cover Data Set developed at the Laboratory for Global Remote Sensing Studies (LGRSS) at the University of Maryland. Data are available in both ASCII GRID and binary image files formats.Characterization of terrestrial vegetation from the Advanced Very High Resolution Radiometer (AVHRR) on the global to regional scale has traditionally been accomplished using classification schemes with discrete numbers of vegetation classes. Representation of vegetation into a limited number of homogeneous classes does not account for the variability within land cover, nor does the portrayal recognize transition zones between adjacent cover types. An alternative paradigm to describing land cover as discrete classes is to represent land cover as continuous fields of vegetation characteristics using a linear mixture model approach. This prototype data set, created by researchers at the Laboratory for Global Remote Sensing Studies (LGRSS) at the University of Maryland, contains 1-km cells estimating: 1) Percent tree cover; 2) Percentage cover for two layers representing leaf longevity (evergreen and deciduous); and 3) Percentage cover for two layers estimating leaf type (broadleaf and needleleaf).Data acquired in 1992-93 from NOAA&amp;#39;s AVHRR at a 1-km spatial resolution and processed under the guidance of the International Geosphere Biosphere Programme (IGBP) were used to derive the tree cover, leaf type and leaf longevity maps. Each pixel in the layers has a value between 10 and 80 percent. These layers can be directly used as parameters in models or aggregated into more conventional land cover maps. For the latter, the product offers the flexibility to derive land cover maps based on user&amp;#39;s requirements for a particular application. The product is intended for use in terrestrial carbon cycle models, in conjunction with other spatial data sets such as climate and soil type, to obtain more consistent and reliable estimates of carbon stocks.
&lt;br&gt;&lt;h4 id&#x3D;&quot;wilhend_687&quot;&gt;wilhend_687&lt;/h4&gt;
This data set is a subset of a global vegetation and soils data set by Wilson and Henderson-Sellers (1985a). The subset was created for the study area of the Large Scale Biosphere-Atmosphere Experiment in Amazonia (LBA) in South America (i.e., 10° N to 25° S, 30° to 85° W). The data are in ASCII GRID format. The original global data set (Wilson and Henderson-Sellers 1985a) is an archive of soil type and land cover data derived for use in general circulation models (GCMs). The data were collated from maps depicting natural vegetation, forestry, agriculture, land use, and soil, and they were archived at a resolution of 1° latitude by 1° longitude. The data set indicates soil type, soil data reliability, primary vegetation, secondary vegetation, and land cover data reliability. Approximately 50 land cover classifications are used, including categories for agricultural and urban uses. The inclusion of secondary vegetation type is particularly useful in areas with cover types that may have a fragmented distribution, such as in areas of urban development. The soil type data are classified according to climatically important properties for GCMs, and they indicate color (light, medium, or dark), texture, and drainage quality of the soil. The land cover data are compatible with the soils data, forming a coherent and consistent data set. The reliability of the land cover data is ranked on a scale of 1 to 5 (high to low). The reliability of the soil data is ranked as high, good, moderate, fair, or poor. Recommendations for the use of these data, as well as more detailed information can be found in Wilson and Henderson-Sellers (1985b). Further data set information can be found at &lt;a href&#x3D;&quot;ftp://daac.ornl.gov/data/lba/land_use_land_cover_change/wilhend/comp/wilhend_readme.pdf&quot;&gt;ftp://daac.ornl.gov/data/lba/land_use_land_cover_change/wilhend/comp/wilhend_readme.pdf&lt;/a&gt;. LBA was a cooperative international research initiative led by Brazil. NASA was a lead sponsor for several experiments. LBA was designed to create the new knowledge needed to understand the climatological, ecological, biogeochemical, and hydrological functioning of Amazonia; the impact of land use change on these functions; and the interactions between Amazonia and the Earth system. More information about LBA can be found at &lt;a href&#x3D;&quot;http://www.daac.ornl.gov/LBA/misc_amazon.html&quot;&gt;http://www.daac.ornl.gov/LBA/misc_amazon.html&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lba_gisswetlands_688&quot;&gt;lba_gisswetlands_688&lt;/h4&gt;
This database, compiled by Matthews and Fung (1987), provides information on the distribution and environmental characteristics of natural wetlands. The database was developed to evaluate the role of wetlands in the annual emission of methane from terrestrial sources. The original data consists of five global 1-degree latitude by 1-degree longitude arrays. This subset, for the study area of the Large Scale Biosphere-Atmosphere Experiment in Amazonia (LBA) in South America, retains all five arrays at the 1-degree resolution but only for the area of interest (i.e., longitude 85 deg to 30 deg W, latitude 25 deg S to 10 deg N). The arrays are (1) wetland data source, (2) wetland type, (3) fractional inundation, (4) vegetation type, and (5) soil type. The data subsets are in both ASCII GRID and binary image file formats.The data base is the result of the integration of three independent digital sources: (1) vegetation classified according to the United Nations Educational Scientific and Cultural Organization (UNESCO) system (Matthews, 1983), (2) soil properties from the Food and Agriculture Organization (FAO) soil maps (Zobler, 1986), and (3) fractional inundation in each 1-degree cell compiled from a global map survey of Operational Navigation Charts (ONC). With vegetation, soil, and inundation characteristics of each wetland site identified, the data base has been used for a coherent and systematic estimate of methane emissions from wetlands and for an analysis of the causes for uncertainties in the emission estimate.The complete global data base is available from NASA/GISS [&lt;a href&#x3D;&quot;http://www.giss.nasa.gov%5D&quot;&gt;http://www.giss.nasa.gov]&lt;/a&gt; and NCAR data set ds765.5 [&lt;a href&#x3D;&quot;http://www.ncar.ucar.edu%5D&quot;&gt;http://www.ncar.ucar.edu]&lt;/a&gt;; the global vegetation types data are available from ORNL DAAC [&lt;a href&#x3D;&quot;http://www.daac.ornl.gov%5D&quot;&gt;http://www.daac.ornl.gov]&lt;/a&gt;.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd01_cirsan_meteorology_2001_1114&quot;&gt;CD01_CIRSAN_Meteorology_2001_1114&lt;/h4&gt;
This data set contains meteorological data collected around the confluence of the Tapajos River with the Amazon River in the Amazon Basin near Santarem, Brazil, in July and August 2001. Boundary layer and upper air measurements were collected with an acoustic sounder-sodar instrument, pilot balloons with optical theodolites, and radiosondes. Radiosondes also measured pressure, temperature, and relative humidity in addition to wind speed and direction. Measurements were made from five local stations at varying frequencies. There are 41 comma-delimited data files with this data set. Supporting information provided with the data set as companion files include: Weather forecasts: Weather forecasts were used to determine the presence of favorable conditions for the balloon flights during the CIRSAN experiment, as well as to help decide the radiosonde launch frequency. The daily observed and forecast weather descriptions for the study period (Weather_forecasts_Santarem.txt) are included. Satellite images: All the satellite images during the CIRSAN period are provided. This is a compilation of images from various instruments and satellite platforms. (See readme_sat.txt). There are 42 images in .gif format. CPTEC Analysis files: The CIRSAN measurement data were used in the CPTEC Global Analysis modeling activity. Model output results for the Pacific and South American region are provided in GRIB format. (See readme_GPSA.txt)
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd01_brams_907&quot;&gt;CD01_BRAMS_907&lt;/h4&gt;
We have investigated mesoscale variations of atmospheric CO2 over a heterogeneous landscape of forests, pastures, and large rivers during the Santarem Mesoscale Campaign (SMC) of August 2001. The variations of atmospheric CO2 concentration were simulated using the Colorado State University (CSU) Regional Atmospheric Modeling System (RAMS) with four nested grids that included a 1-km finest grid centered on the Flona Tapajos. Surface fluxes of CO2 were prescribed in the model using idealized diurnal cycles over forest and pasture vegetation derived from flux tower observations, and over surface water using a value suggested by in situ measurements in the Amazon region. The distribution of vegetation types was derived from the 1-km International Geosphere-Biosphere Programme (IGBP) land-cover dataset version 2.0. Our simulation ran from the 1st through the 15th of August 2001, which was concurrent with the SMC. Evaluation against flux tower observations and the SMC field measurements shows that, in many respects, the model captures observed meteorological variables and CO2 concentrations reasonably well. The results also suggest that the local topography, differences in roughness length between water and land, the T shape juxtaposition of Amazon and Tapajos Rivers, and the resulting horizontal and vertical wind shears, all facilitated the generation of local mesoscale circulations. Possible mechanisms producing a lower level convergence line near the east bank of the Tapajos River during strong trade-wind conditions are also explored. Our modeling study is helping us to understand observed patterns of CO2 fluxes and concentration distribution obtained from flux towers and light aircraft.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd02_c_n_isotopes_1097&quot;&gt;CD02_C_N_Isotopes_1097&lt;/h4&gt;
This data set reports delta 13C/12C results for leaf tissues and atmospheric carbon dioxide (CO2), 15N/14N ratios for leaf tissue, and leaf carbon and nitrogen concentrations along a topographical gradient in old-growth forests in the ZF2 Reserve (km 34), Instituto Nacional de Pesquisas da Amazonia (INPA), near Manaus, Amazonas, Brazil. During the dry seasons of 2004 and 2006, leaves were sampled at various heights within the canopy and atmospheric air flask samples were also collected at various heights at three locations along this gradient. Also included are coincident meteorological, atmospheric CO2, and CO2 flux measurements from the plateau KM34 tower. There are 3 comma-delimited data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd02_atmosphere_co2_isotopes_1011&quot;&gt;CD02_Atmosphere_CO2_Isotopes_1011&lt;/h4&gt;
This data set reports carbon and oxygen stable isotope ratios of atmospheric carbon dioxide (CO2) collected at several forest and pasture sites and in the free troposphere over Amazonia. There are three comma-delimited ASCII files with this data set. Atmospheric CO2 concentrations and isotope signatures were measured at ten different forest and pasture canopy sites across the states of Amazonas, Para, and Rondonia within the Brazilian Amazon between March 1999 and March 2004. Both daytime and nighttime profile samples were collected. Samples of CO2 in the troposphere were collected during aircraft flights over the Amazon/Tapajos Rivers, FLONA Tapajos, and pasture/agriculture areas during five days in May 2003 (wet season). Samples were analyzed for carbon and oxygen isotopes of atmospheric CO2. Flights ranged from low altitudes to above the diurnal tropospheric boundary layer. Measurements of carbon and oxygen stable isotope ratios of atmospheric carbon dioxide (CO2) are a powerful indicator of large-scale CO2 exchange on land across multiple spatial scales. Stable carbon isotope composition of leaf tissue and CO2 released by respiration (delta r) can be used as an estimate of changes in ecosystem isotopic discrimination that occur in response to seasonal and interannual changes in environmental conditions, and land-use change (forest-pasture conversion). Understanding of carbon dioxide stable isotope composition can play a central role in influencing our understanding of the extent to which terrestrial ecosystems are carbon sinks.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd02_c_n_o_organic_983&quot;&gt;CD02_C_N_O_Organic_983&lt;/h4&gt;
This data set reports the measurement of stable carbon, nitrogen, and oxygen isotope ratios in organic material (plant, litter and soil samples) in forest canopy profiles and pasture (grasses and shrubs) as well as corresponding carbon and nitrogen tissue concentrations in a number of different sites across Brazil. The sampling design captured the temporal variation in rainfall over the course of several years. Carbon and nitrogen isotope ratios can act as a proxy for interpreting aspects of the carbon and nitrogen cycles in Amazonian rainforests. Data are in three comma-delimited ASCII files.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd02_forest_canopy_structure_1009&quot;&gt;CD02_Forest_Canopy_Structure_1009&lt;/h4&gt;
This data set reports on Leaf Area Index (LAI) and Specific Leaf Area (SLA) measurements collected from forest and pasture sites in or near the Tapajos National Forest (TNF), 80 km south of the city of Santarem, Para, Brazil. The collections were between October 1999 and June 2003 from tower sites accessed via the km 67 forest entrance. There are 2 comma-delimited ASCII data files with this data set, and 1 companion data file which provides site descriptions.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd02_leaf_level_gas_exchange_1010&quot;&gt;CD02_Leaf_Level_Gas_Exchange_1010&lt;/h4&gt;
This data set reports leaf gas flux and leaf properties from samples collected from trees, liana, pasture saplings, and pasture grass located at eight different sampling locations in the states of Para (south of Santarem) and Amazonas (near Manaus) from November 1999 through December 2003. Data are reported on photosynthesis measurements, CO2 response curves, light response curves, humidity response curves, and stomatal responses to variations of the leaf-to-air water vapor mole fraction deficit. Leaf weight, carbon and nitrogen concentrations as well as stable isotope signatures for 13C and 15N are reported for a subset of the samples. There is one comma-delimited ASCII data file with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd02_leaf_water_potential_1100&quot;&gt;CD02_Leaf_Water_Potential_1100&lt;/h4&gt;
Data are reported for leaf water potential of leaves of seven species of trees and lianas from the primary forest at the km 67 Tower Site, Tapajos National Forest, and measurements of five sapling tree species and the grass Brachiaria brizantha from a pasture site located near the km 77 Pasture Tower Site, approximately 10 km from the primary forest site. The research area is situated within the Tapajos National Forest reserve, south of the city of Santarem, Para, Brazil. Measurements were made quarterly between March 2000 and March 2001. There is one comma-delimited data file with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd02_o_h_isotopes_1008&quot;&gt;CD02_O_H_Isotopes_1008&lt;/h4&gt;
This data set reports the oxygen isotope signatures of water extracted from plant tissue (xylem from the stems and leaf tissue) and of atmospheric water vapor from twelve different sites (including both pasture and forest) throughout the Amazon region of Brazil. Samples were collected approximately every 4 months between 1999 and 2003 with additional samples collected monthly between January and May of 2003. In 2004 the collection of water samples from plant tissue continued at two sites, though water vapor collections were discontinued, and measurements of deuterium signatures were added to the analyses. In addition, water vapor from the troposphere was collected during a series of aircraft flights over the Tapajos National Forest in May of 2003 and analyzed for oxygen isotopes using the same methodology. There is one comma-delimited ASCII data file with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd03_ceilometer_km67_942&quot;&gt;CD03_Ceilometer_Km67_942&lt;/h4&gt;
A Vaisala CT-25K ceilometer was installed at an old-growth forest site located at the km 67 Eddy Flux Tower site in the Tapajos National Forest, Para, Brazil, off Kilometer 67 of BR-163 south of Santarem in April 2001 and remained operational through December 2003, with reliable data being collected between May 2001 and June 2003. Annual, 2001 to 2003, 30-minute average cloud base and backscatter profile data and measurement statistics (sample count, variance, skewness, and kurtosis) are presented in 15 ASCII comma-delineated files. In addition, the cloud base values (m) and measurement statistics for the three reported cloud base levels have been consolidated in 3 annual comma-separated files. The ceilometer provides 15-second measurements of cloud base (three levels up to 7500 m), echo intensity, and a 30-m resolution backscatter profile. The ceilometer reports vertical visibility during periods when the sky is obscured but a cloud base is not detectable. The ceilometer was operational for a sufficient amount of time to examine wet-to-dry season variations in cloud cover fraction and cloud base height.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd03_pasture_flux_962&quot;&gt;CD03_Pasture_Flux_962&lt;/h4&gt;
Eddy correlation and micrometeorological measurements began in 2001 and continued through 2005 at the pasture site at km 77 on BR-163 just south of the city of Santarem, Para, Brazil. Measurements included turbulent fluxes (momentum, heat, water vapor, and CO2) using the eddy covariance (EC) approach. Other measurements included the CO2 profile, air temperature, humidity, wind speed profile, downward and upward solar and terrestrial radiation, downward and upward photosynthetically active radiation (PAR), atmospheric pressure, rainfall, soil temperature, soil moisture, and soil heat flux. Data are presented in 5 comma-separated ASCII value (csv) files each corresponding roughly to one calendar year. At the beginning of the measurements, in September 2000, the field was a pasture. In November 2001, the pasture was burned, plowed, and planted in upland (non-irrigated) rice. Land use practices during the study period were recorded and are included in a table in Section 5 of this guide. The EC system was composed of a 3D sonic anemometer (ATI 3D) and an infrared analyzer (LICOR 6262) installed on a 20m tower in the agricultural field. The methodology to calculate the flux is described in detail in Sakai et al. (2004) and a companion file is included that describes in detail the formulae used to calculate the eddy flux variables (CD03_Pasture_Flux_Calculations.pdf).
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd03_mesoscale_meteorology_944&quot;&gt;CD03_Mesoscale_Meteorology_944&lt;/h4&gt;
We analyzed rainfall obtained in a network of 38 rain gauges located near the confluence of the Tapajos and Amazon rivers in the eastern Amazon Basin. We found that tipping bucket rain gauges work adequately in the Amazon rainfall regime, but careful field calibration and comparison with collocated conventional rain gauges was essential to incorporate daily totals from operational array into regional maps. Near-river stations miss the afternoon convective rain as expected as the river breeze promotes subsidence over the river, but paradoxically, this deficiency is more than compensated for by additional nocturnal rainfall at these locations. The 0.25-degree CMORPH passive infrared inferred rainfall data do an adequate job of describing medium scale variability in this region, but some localized breeze effects are not resolved. For inland areas away from the breezes, the nocturnal period precipitation contributes less than half of total precipitation. The large-scale rainfall increase just to the west of Santarem manifests itself locally as a &amp;#39;tongue&amp;#39; of enhanced rain from along the wide area of open water at the Tapajos-Amazon confluence The breeze circulations associated with the Amazon River (which lies parallel to the mean flow) affects rainfall more than does the Tapajos breeze (normal to the predominant wind). The Tapajos breeze influence extends only a few kilometers inland east of the riverbank. Rainfall increases to the north of the Amazon, possibly the result of orographic effects. Dry season rainfall increases by up to 30% going away from the Amazon River, as would be expected given breeze subsidence over the river.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd03_tethered_balloon_1108&quot;&gt;CD03_Tethered_Balloon_1108&lt;/h4&gt;
This data set contains measurements of nocturnal meteorological profiles collected from tethered balloon platforms during July 2001, October 2001, and November 2003. Measurements were made near the pasture/agricultural tower site at km 77 on BR-163 just south of the city of Santarem, and the near the Tapajos National Forest, km 83 tower site, Santarem, Para, Brazil. Measurements collected include air temperature, wind speed and direction, and specific humidity. The 2003 measurements also included CO2 concentrations. Sites were near enough to allow comparison between sounding profiles and tower data. There are three comma-delimited ASCII files with this data set. Profiles were obtained from sunset until the first hours after sunrise. Each sounding provided information on temperature, humidity, horizontal wind magnitude and direction as the balloon went up and down. Typical soundings went up to 300 to 400 m. During most of the night, soundings were performed hourly. The balloon rose at a rate of 0.5 m per second in the first 100 m, and 2 m per second above it. The time between successive samplings was 10 s. Intensive periods of shallow, successive soundings were performed starting at dawn, to catch the early development of the convective boundary layer (CBL). These early morning soundings went up only to the capping inversion.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd04_biomass_990&quot;&gt;CD04_Biomass_990&lt;/h4&gt;
This data set contains the results of a biometric tree survey of a 19.25 ha area adjacent to the eddy flux tower at the km 83 logged forest tower site in Tapajos National Forest, Para, Brazil. The survey was done in March 2000. All measurements reported here were taken before the logging began. Diameters of all trees &amp;gt; 35 cm DBH within the 19.25 ha survey area were recorded and trees with DBH between 10 and 35 cm DBH were recorded along three transects with a total area of 2.3 ha (Miller et al., 2004). These data were used to calculate net ecosystem productivity (NEP) and the role of this forest as a carbon source or sink. Biometric data are reported in one comma-delimited ASCII file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd04_tower_flux_gap_978&quot;&gt;CD04_Tower_Flux_Gap_978&lt;/h4&gt;
This data set reports 30-minute values for above-canopy meteorology and fluxes of momentum, heat, and carbon dioxide, and within-canopy carbon dioxide and water vapor concentrations collected at 12 levels between 10 cm and 64 m at the tower located within a logging gap at km 83 Tower Site in the Tapajos National Forest, Para, Brazil. Data were collected over 1.5 years between June 3, 2002 and January 30, 2004. All of the data are contained in one comma separated file. Two towers are located at the km 83 site. The first tower was installed in an intact forest area at this site in June 2000 (the &amp;#39;intact&amp;#39; tower). In September 2001, the area adjacent to the tower was selectively logged (Bruno et al., 2006). The second tower (the &amp;#39;gap tower&amp;#39;) was installed and operating in June 2002, 400 m east of the intact tower. The gap tower was installed in the middle of a 50 m x 50 m log landing.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd04_co2_profiles_947&quot;&gt;CD04_CO2_Profiles_947&lt;/h4&gt;
We used two independent approaches, biometry and micrometeorology, to determine the net ecosystem production (NEP) of an old growth forest in Para, Brazil. Biometric inventories indicated that the forest was either a source or, at most, a modest sink of carbon from 1984 to 2000 (+0.8 +/- 2 Mg C(.)ha(-1.)yr(-1); a positive flux indicates carbon loss by the forest, a negative flux indicates carbon gain). Eddy covariance measurements of CO2 exchange were made from July 2000 to July 2001 using both open- and closed-path gas analyzers. The annual eddy covariance flux-calculated without correcting for the underestimation of flux on calm nights indicated that the forest was a large carbon sink (-3.9 Mg C.ha(-1.)yr(-1)). This annual uptake is comparable to past reports from other Amazonian forests, which also were calculated without correcting for calm nights. The magnitude of the annual integral was relatively insensitive to the selection of open- versus closed-path gas analyzer, averaging time, detrending, and high-frequency correction. In contrast, the magnitude of the annual integral was highly sensitive to the treatment of calm nights, changing by over 4 Mg C(.)ha(-1.)yr(-1) when a filter was used to replace the net ecosystem exchange (NEE) during nocturnal periods with u* &amp;lt; 0.2 m/s. Analyses of the relationship between nocturnal NEE and u* confirmed that the annual sum needs to be corrected for the effect of calm nights, which resulted in our best estimate of the annual flux (+0.4 Mg C(.)ha(-1.)yr(-1)). The observed sensitivity of the annual sum to the u* filter is far greater than has been previously reported for temperate and boreal forests. The annual carbon balance determined by eddy covariance is therefore less certain for tropical than temperate forests. Nonetheless, the biometric and micrometeorological measurements in tandem provide strong evidence that the forest was not a strong, persistent carbon sink during the study interval.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd04_dendrometry_989&quot;&gt;CD04_Dendrometry_989&lt;/h4&gt;
A dendrometry study was conducted at the logged forest tower site, km 83 site, Tapajos National Forest, Para, Brazil over a period of 4 years following the implementation of a reduced impact logging management regime. Dendrometer bands were installed to measure diameter growth increments for 234 trees in an 18 ha plot adjacent to the eddy flux tower at the km 83 site. In addition to trees randomly selected for measurements within the plot prior to logging, a set of smaller diameter trees within or adjacent to gaps created during the logging treatment were added to the study in 2002. Selective logging is a major land use in the Amazon Basin. An accurate accounting of the effect of logging on regional carbon balances requires better information on the rates at which the logged forest recovers biomass. There is one comma-delimited data file with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd04_lai_estimates_1103&quot;&gt;CD04_LAI_Estimates_1103&lt;/h4&gt;
This data set contains summary data for monthly leaf area index (LAI) and plant area index (PAI) at the km 83 Tower Site, in the Tapajos National Forest, Para, Brazil. LAI was estimated for hemispherical photographs of leaves collected between 2000 and 2003, using the histogram and gap-fraction analysis methods. There are two data files with this data set: one comma-delimited ASCII data file with this data set which contains the monthly summary LAI and PAI data, and one compressed (.zip) file that contains hemispherical photo images (.bmp) for 2000-2001. The images include those taken pre-logging and post-logging at the measurement site for the purpose of comparing LAI. In addition, there is a companion file containing a program code developed for LAI analysis provided as an ASCII text file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd04_lai_992&quot;&gt;CD04_LAI_992&lt;/h4&gt;
Leaf area index was estimated in an 18 ha plot at the logged forest tower site, km 83, Tapajos National Forest, Para, Brazil. The plot was adjacent to the eddy flux tower at km 83, Tapajos National Forest, Para, Brazil. Thirty litter traps were placed at 25-m intervals along two east–west transects in the 18 ha block. Litter samples were collected biweekly from the traps and returned to the lab where they were sorted, air dried, and weighed. The leaf area of a subsample of air-dried leaves was determined using a computer scanner and image processing software. The subsample was then dried in an oven and the air-dried weights were corrected to oven-dried weight. The area of leaf litter collected during each sampling was calculated using the relationship between weight and area measured for the subsample (Goulden et al., 2004). There is one comma-delimited data file with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd04_leaf_litter_991&quot;&gt;CD04_Leaf_Litter_991&lt;/h4&gt;
Above-ground litter productivity was measured in a 18 ha plot adjacent to the eddy flux tower at the logged forest tower site, km 83, Tapajos National Forest, Para, Brazil. Thirty litter baskets distributed within the grid were visited bi-weekly (Goulden et al., 2004). Oven dry mass of leaves, wood, reproductive parts and miscellaneous components of the collected litter was determined for each collection. Collections covered a pre-harvest period (Sept 2000 - July 2001) and a post- harvest period (Aug 2001-Mar 2003). There is one comma-delimited data file with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd04_leaf_level_gas_exchange_1060&quot;&gt;CD04_Leaf_Level_Gas_Exchange_1060&lt;/h4&gt;
This data set reports the results of measurements of (1) leaf-level photosynthesis response curves for the effects of temperature, leaf age, warming, irradiation, and circadian rhythm and (2) leaf-level photorespiration rates at 30 and 37 degrees C. Measurements were made between June 2000 and February 2006 at the km 83 Logged Forest Tower site, the km 67 Primary Forest Tower site, and the control site at Seca Floresta, all in the Tapajos National Forest, Para, Brazil. There are 7 comma delimited ASCII data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd04_logging_damage_1038&quot;&gt;CD04_Logging_Damage_1038&lt;/h4&gt;
This data set contains the results of a survey of logging damage in a 18 ha plot (300 m N-S, 600 m E-W) east (upwind) of the eddy flux tower at km 83, Tapajos National Forest, Para, Brazil. Data collected include type of damage, snap height, and log dimensions, as well as calculated biomass of stems and canopy either damaged or removed in logging. There are two comma-delimited data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd04_soil_moisture_km83_979&quot;&gt;CD04_Soil_Moisture_Km83_979&lt;/h4&gt;
This data set reports continuous high-resolution frequency-domain reflectometry measurements of soil moisture to 10 m depth and precipitation data near each of the two towers located at the km 83 tower site (logged forest site) in the Tapajos National Forest in the state of Para, Brazil. Measurements were made during 2002 and 2003. Soil moisture and precipitation data are provided in two comma-delimited ASCII files. The first tower was installed in an intact forest area at this site in June 2000 (the &amp;#39;intact&amp;#39; tower) and instrumented for eddy flux and micrometerological measurements and operated 15 months prior to any logging in the area (Goulden et al., 2004; Miller et al., 2004; Rocha et al., 2004). In September 2001, the area adjacent to the tower was selectively logged (Bruno et al., 2006). The second tower (the &amp;#39;gap tower&amp;#39; tower) was installed and operating in June 2002, 400 m east of the intact tower. The gap tower was installed in the middle of a 50 m x 50 m log landing. Soil moisture measurements were made in 10 m deep vertical pits (1 x 1 m2) approximately 20 m from the micrometerological tower sites in undisturbed forest patches. Reflectometers were inserted horizontally into shaft walls at 0.15, 0.30, 0.60, 1, 2, 3, 4, 6, 8, and 10 meters beneath the surface. These data were used to determine how soil moisture varies on diel, seasonal and multi-year timescales and to better understand the quantitative and mechanistic relationships between soil moisture and forest evapotranspiration.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd04_soil_respiration_1039&quot;&gt;CD04_Soil_Respiration_1039&lt;/h4&gt;
This data set reports on the flux of carbon dioxide from logged forest soils near the eddy flux tower at the km 83 site, Para, Brazil. The automated soil respiration measurements were collected using 15 chambers, installed August 2001 in primary forest. Data were collected between December 19, 2001 and March 1, 2002. There is one comma-delimited data file with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd05_fuel_loads_1233&quot;&gt;CD05_Fuel_Loads_1233&lt;/h4&gt;
This data set contains estimates of understory fuel loads (forest litter) at six locations near Paragominas in Northeastern Amazonia. Samples were collected from three different forest conditions: primary forest, logged forest, and burned forest. Volumes and weights are provided by size and condition class based on the planar transect method of estimating understory fuel loads (Brown 1971). Means and standard errors are reported from 3 transects in each forest x condition class. There is one comma-delimited data file (.csv) with this data set. DATA QUALITY STATEMENT: The Data Center has determined that there are questions about the quality of the data reported in this data set. The data set has missing or incomplete data, metadata, or other documentation that diminishes the usability of the products.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd05_micromet_1169&quot;&gt;CD05_Micromet_1169&lt;/h4&gt;
This data set reports soil moisture expressed as volumetric water content (VWC), daily precipitation, air temperature, relative humidity, and dew point measurements conducted at the Seca Floresta site, km 67, Tapajos National Forest, Brazil. The measurements were part of the Rainfall Exclusion Experiment (REE) established to study the response of a humid Amazonian forest to severe drought. VWC was measured with continuous high-resolution frequency-domain reflectometry to 11-m depth in two 1-ha plots from 1999 to 2007. One plot was subjected to ~75 percent throughfall exclusion during the rainy season (exclusion) and another monitored under normal conditions (control). Daily precipitation was measured in the control plot and in a nearby clearing between 1999 and 2006 using wedge rain gauges. Air temperature, relative humidity, and dew point were measured along the vertical forest profile of the control and dry plots of the site between 2000 and 2003. There are three comma-delimited data files (.csv) with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd05_ree_fuel_sticks_moisture_1232&quot;&gt;CD05_REE_Fuel_Sticks_Moisture_1232&lt;/h4&gt;
This data set contains moisture content measurements for fuel sticks located in the forest understory of the rainfall exclusion experimental site, Tapajos National Forest, Para, Brazil. The mean and standard errors are reported for control and treatment plot measurements. The measurements were taken on various dates and times of day between 1998 and 2000 during the dry season. The rainfall exclusion treatment began in late January 2000 and continued through December 2004. About 60% of throughfall (equivalent to approximately half the rainfall) was diverted from a 1-hectare plot (i.e., dry) using plastic panels installed in the understory. The comparable 1-hectare control plot (i.e., wet) was unaltered. The purpose was to observe the potential effects of severe water stress on a humid Amazonian forest (Nepstad et al., 2002). There is one comma-separated (.csv) data file with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd06_camrex_1086&quot;&gt;CD06_Camrex_1086&lt;/h4&gt;
This data set provides high-resolution (~500 m) gridded land and stream drainage direction maps for the Amazon River basin, excluding the Rio Tocantins basin. These maps are the result of a new topography-independent analysis method (Mayorga et al., 2005) using the vector river network from the Digital Chart of the World (DCW, Danko, 1992) to create a high-resolution flow direction map. The data products include (1) a stream network coverage with stream order assigned to each reach; (2) the basin boundaries of the major tributaries to the Amazon mainstem; (3) the mouths; and (4) the source points of these tributaries. There are 7 ESRI ArcGIS shapefiles provided in compressed .zip format and 4 GeoTiff image files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd06_bgc_jiparana_1227&quot;&gt;CD06_BGC_JiParana_1227&lt;/h4&gt;
This data set provides spatially extensive and temporally intensive surveys of the river biogeochemistry of the Ji-Parana River Basin in Western Amazonia, Rondonia, Brazil. The concentrations of major nutrient ions, dissolved organic and inorganic carbon, pH, temperature, dissolved oxygen, and conductivity were measured in Ji-Parana River and tributary samples at the defined seasonal or monthly intervals. Dominant landuse/landcover classes, slope, and soil cation exchange capacity are included for each of the extensive sampling locations derived from river basin and sub-basin characteristics. Water samples were collected from 1999 to 2003 along the main stem of the Ji-Parana River as well as from the major tributaries including the Urupa. Shapefiles with the boundaries of the major sub-basins of the study area as well as the location of the sample collection points are included for the intensive and extensive sampling campaigns as well as the Urupa River campaign. There are six comma-separated data files (.csv) and five compressed shapefiles (.zip) with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd06_carbon_respiration_1125&quot;&gt;CD06_Carbon_respiration_1125&lt;/h4&gt;
This data set provides measured and calculated variables describing the carbon pools in river waters, CO2 respired from the water and total amount of CO2 evaded, dissolved oxygen isotopes (delta 18O-O2), and concentration of bacterial cells in river water. Samples were collected from 10 white-water rivers, two clear-water streams (one each in Amazonas and Acre), and two black-water rivers in Amazonas from July to September 2005, which coincided with a severe drought in the western and southern regions of the Amazon Basin (Zeng et al. 2008). Eight of these sites were resampled during August through September 2006 of the following year (no drought).
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd06_c02_exchange_1136&quot;&gt;CD06_C02_Exchange_1136&lt;/h4&gt;
This data set provides measurements of carbon dioxide flux rates (FCO2), gas transfer velocity (k), and partial pressures (pCO2) at 75 sites on rivers and streams of the Amazon River system in South America for the period beginning July 1, 2004, and ending January 23, 2007. Several fieldwork campaigns occurred between June 2004 and January 2007 in the Amazon River basin, with discharge conditions ranging from low to high flow. The sampled areas span the spectrum of chemical characteristics observed across the entire basin, including, for example, both low and high pH values and suspended sediment loads. There is one comma-delimited data file in this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd06_outgassing_1151&quot;&gt;CD06_Outgassing_1151&lt;/h4&gt;
This data set provides estimates of monthly carbon dioxide (CO2) flux from the Amazon mainstem rivers, tributary stream networks, and their associated varzeas (floodplains). CO2 flux was calculated using two aggregation approaches: for defined river basins (data file #2) and for defined river reaches (figure 2). Flux was calculated from (1) estimated surface water area by month for the Amazon mainstem rivers, associated varzeas, and tributary stream networks, (2) mean daily partial pressures of CO2 (pCO2) concentrations for the mainstem rivers, and (3) calculated mean pCO2 values for the varzea waters. Mean monthly discharge data for 11 mainstem rivers are also included. There are five comma-delimited data files with this data set. Amazon mainstem is a region covering the Amazon/Solimoes River mainstem from 70 degrees W to 54 degrees W. Data from the Japanese Earth Resources Satellite-1 (JERS-1) L-band synthetic aperture radar were used to estimate the areal coverage and inundation status of rivers and floodplains over 100 m in width and compiled into mosaics for periods of high and low water. For each mosaic, the study area was classified into either flooded or non-flooded areas. Data for the seasonal and spatial distributions of pCO2 within each hydrographic region were utilized from over 1,800 samples taken on 13 Carbon in the Amazon River Experiment (CAMREX) expeditions at different water stages throughout a 2,000 km reach of the central Amazon mainstem, tributary, and floodplain waters (Degens et al., 1991, Devol et al., 1995, Richey et al., 1988).
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd06_c_isotopes_1120&quot;&gt;CD06_C_Isotopes_1120&lt;/h4&gt;
This data set includes measurements of standard geochemical variables, dissolved CO2, dissolved inorganic carbon (DIC), dissolved organic carbon (DOC), fine particulate organic carbon (FPOC), and coarse particulate organic carbon (CPOC) in samples taken from 60 Amazonian river locations across the Amazon Basin from 1991 to 2003 (Mayorga et al., 2005). The 14C and 13C isotopic composition of DIC was measured on samples collected between 1991 and 2003. The 14C composition of organic carbon fractions was measured on samples collected from 1995 through 1996. There are four comma-delimited data files with this data set. Note that site descriptions include a categorization of each site by topography according to the percentage of the drainage area above 1,000 m elevation (Mayorga et al., 2005). Only means of geochemical and carbon-fraction results are provided. Both individual 13C and 14C measurements and mean results are provided.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd06_lulc_map_jiparana_1087&quot;&gt;CD06_LULC_Map_JiParana_1087&lt;/h4&gt;
This data set provides a land use/land cover map of the Ji-Parana River Basin in the state of Rondonia, Brazil produced from the digital classification of eight Landsat 7-ETM+ scenes from 1999 acquired from the Tropical Rain Forest Information Center (TRFIC) at Michigan State University. Nine land cover classes covering the Ji-Parana Basin were identified. There is one GeoTiff file with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd06_landuse_timeseries_jiparana_844&quot;&gt;CD06_Landuse_Timeseries_JiParana_844&lt;/h4&gt;
This data set contains four land use/land cover maps (1986, 1992, 1996 and 2001) for the Ji-Parana River Basin, derived from the digital classification of 8 Landsat images obtained from The Tropical Rain Forest Information Center (TRFIC).
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd06_physical_template_jiparana_1090&quot;&gt;CD06_Physical_Template_JiParana_1090&lt;/h4&gt;
This data set contains physical, hydrologic, political, demographic, and societal maps for the Ji-Parana River Basin, in the state of Rondonia, Brazil. These data were used as base information in subsequent investigations of land use/land cover, biogeochemistry, soils, and water balance processes (Ballester et al., 2003). This data set includes a Digital Elevation Model (DEM), river networks and morphometric characteristics of the region (derived from the DEM), and a number of social and demographic vector sets (roads as of 2001, county borders, population change from 1970-2000, and settlement projects). The DEM is provided in GeoTIFF format. Other files are provided as shapefiles.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd06_soils_jiparana_1088&quot;&gt;CD06_Soils_JiParana_1088&lt;/h4&gt;
This data set provides a digital map of soil orders for the Ji-Parana River Basin, in the state of Rondonia, Brazil (Western Amazonia). Soil orders wereÂ manually digitized from a 1:500,000 map from EMBRAPA originally published in 1983. Oxisols and Ultisols are the predominant soil types in the basin, encompassing 47% and 24% of the total drainage area, respectively. Entisols cover 14%, Alfisols 13% and Eptisols 2% of the basin (Ballester et al., 2003). One data file is provided in ESRI ArcGIS Shapefile format compressed into a single zip file (.zip).
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd06_water_balance_jiparana_1132&quot;&gt;CD06_Water_Balance_JiParana_1132&lt;/h4&gt;
This data set provides simulated minimum, average, and maximum monthly rainfall, potential evapotranspiration, water deficit, and water surplus values for the Ji-Parana River basin, Rondonia, Brazil. The Thornthwaite-??Mather climatological model integrated into a Geographic Information System (GIS) was used to derive the data by utilizing Advanced Very High Resolution Radar (AVHRR) images for temperatures, rainfall amounts from gauges within and around the basin, soil profiles, and land cover maps as model inputs. The monthly water balance for the Ji-Parana river basin is simulated from February 1995 through December 1996 (Victoria et al., 2007). Data are also provided from the Ji-Parana subbasin stations for total basin rainfall, basin discharge and basin evapotranspiration. This data was used to check the results of the water balance model. There are 2 comma-delimited data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd07_goes_l3_gridded_srb_831&quot;&gt;CD07_GOES_L3_Gridded_SRB_831&lt;/h4&gt;
High resolution downwelling solar, PAR, infrared radiation and rain rates retrieved from GOES-8 imager. The data set covers primarily Amazon watershed area. It has 8km and half hourly resolution. Data covers two periods in 1999: March 1 - April 30 and September 1 - October 31. Files are available in compressed binary format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd08_c_isotopes_belowground_1025&quot;&gt;CD08_C_Isotopes_Belowground_1025&lt;/h4&gt;
This data set contains carbon isotope signatures from soil organic matter collected from the following sites: the forests of the ZF-2 INPA reserve approximately 80 km north of the city of Manaus, Amazon; the Tapajos National Forest approximately 83 km south of the city of Santarem, Para; and the Fazenda Vitoria, a ranch near the city of Paragominas, Para. Samples from the Fazenda Vitoria were from degraded and managed pasture sites as well as mature and secondary forests. In addition,carbon isotope signatures from roots sorted by size class, hand-picked from soil pits in the Flona Tapajos and Fazenda Vitoria, are included, as are carbon isotope signatures from soil gases from samples collected at the Fazenda Vitoria. There are 4 ASCII data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd08_cwd_res_and_decomp_manaus_911&quot;&gt;CD08_CWD_Res_and_Decomp_Manaus_911&lt;/h4&gt;
Respiration from coarse litter (trunks and large branches &amp;gt; 10 cm diameter) was studied in central Amazon forests. Respiration rates varied over almost two orders of magnitude (1.003-0.014 mug C g(-1) C min(-1), n &#x3D; 61), and were significantly correlated with wood density (r(adj)(2) &#x3D; 0.42), and moisture content (r(adj)(2) &#x3D; 0.39). Additional samples taken from a nearby pasture indicated that wood moisture content was the most important factor controlling respiration rates across sites (r(adj)(2) &#x3D; 0.65). Based on average coarse litter wood density and moisture content, the mean long-term carbon loss rate due to respiration was estimated to be 0.13 yr(-1) (range of 95% prediction interval (PI) &#x3D; 0.11-0.15 yr(-1)). Comparing mean respiration rate with mean mass loss (decomposition) rate from a previous study, respiratory emissions to the atmosphere from coarse litter were predicted to be 76% (95% PI &#x3D; 65-88%) of total carbon loss, or about 1.9 (95% PI &#x3D; 1.6-2.2) Mg C ha(- 1) yr(-) (1). Optimum respiration activity corresponded to about 2.5 g H2O g(-1) dry wood, and severely restricted respiration to &amp;lt; 0.5 g H2O g(-1) dry wood. Respiration from coarse litter in central Amazon forests is comparable in magnitude to decomposing fine surface litter (e.g. leaves, twigs) and is an important carbon cycling component when characterizing heterotrophic respiration budgets and net ecosystem exchange (NEE).
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd08_leaf_isotopes_manaus_1245&quot;&gt;CD08_Leaf_Isotopes_Manaus_1245&lt;/h4&gt;
This data set provides measurements for carbon (C), nitrogen (N), leaf area index (LAI), and carbon isotope ratio data (13C and 14C) of leaves sampled at the Manaus ZF2 Jacaranda transect area, Amazonas, Brazil, in 2001. Leaf tips and the petioles from the youngest and oldest leaves from a sampled branch were analyzed for nine different species. There is one comma-delimited data file (.csv) with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd08_radiocarbon_dates_manaus_996&quot;&gt;CD08_Radiocarbon_Dates_Manaus_996&lt;/h4&gt;
This data set reports the ages and growth rates of trees as determined by radiocarbon dating (14C), selected from a logging operation near the city of Itacoatiara, about 250 km east of Manaus, Brazil in 1997. Samples were collected from forty-four trees from 15 species with a basal diameter greater than 100 cm and prepared for radiocarbon dating by Accelerator Mass Spectrometry (AMS) at Lawrence Livermore National Laboratory. There is one comma-separated ASCII data file with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd08_radiocarbon_dates_997&quot;&gt;CD08_Radiocarbon_Dates_997&lt;/h4&gt;
This data set reports the ages and growth rates of trees determined by radiocarbon dating (14C) in three Amazonia forests. Tree samples were collected from permanent research plots at ZF2 km 34, Manaus, Amazonas, the Catuaba Experimental Farm, Acre, and the km 83 tower site (logged forest site) in the Tapajos National Forest, Para, between 2001-2003. Samples from 97 individual trees were either tree cores (Manaus and Acre) or a combination of tree cores and slabs cut from stems as part of the logging in the Tapajos National Forest (Para). Radiocarbon dating (14C) was used to determine the age and the mean diameter growth increment of samples from individual trees in various diameter size classes. These measurements can be used to verify and extend short-term diameter increment measurements done with dendrometers and to constrain models of tree demography. There is one comma-separated ASCII data file with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd08_tree_growth_manaus_1194&quot;&gt;CD08_Tree_Growth_Manaus_1194&lt;/h4&gt;
This data set provides diameter at breast height (DBH) measurements made of trees in a dense terra-firme tropical moist forest at the ZF-2 Experimental Station, 90 km north of Manaus, Brazil. DBH was measured over two transects (East to West and North to South) which were established in 1996 by the Jacaranda Project (agreement between the National Institute for Research in the Amazon (INPA) and the Japan International Cooperation Agency, JICA). For each tree, a metal dendrometer band was fixed to the trunk and growth in circumference was measured monthly with digital calipers. The transects measured 20-m x 2500-m, and were stratified by plateau, slope, and baixio (lowland areas near small streams). Topography location, distance along the transect, height at which the band was installed, local tree name, and field notes are also provided in the data files. Measurements were taken between June 1999 and December 2001.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd08_tree_inventory_ducke_910&quot;&gt;CD08_Tree_Inventory_Ducke_910&lt;/h4&gt;
This data set includes in one data file the common names, base diameters, and calculated tree masses for almost 3,000 trees on a 5 hectare plot (20 x 2,500 m) located in the Ducke Reserve near Manaus, Brazil in the central Amazon. Measurements were taken during October-December 1999. All diameter measurements were taken at 1.3 meters in height (DBH), or above the buttresses or other stem anomalies. Forest structure characteristics such as biomass density, stem density, diameter class distribution, and taxonomic information at the family and perhaps genus level, can be derived from these data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd08_ecosystem_resp_manaus_912&quot;&gt;CD08_Ecosystem_Resp_Manaus_912&lt;/h4&gt;
Understanding how tropical forest carbon balance will respond to global change requires knowledge of individual heterotrophic and autotrophic respiratory sources, together with factors that control respiratory variability. We measured leaf, live wood (tree stem), and soil respiration, along with additional environmental factors over a 1-yr period in a Central Amazon terra firme forest. Scaling these fluxes to the ecosystem, and combining our data with results from other studies, we estimated an average total ecosystem respiration (R-eco) of 7.8 mumol(.)m(-2.)s(-1). Average estimates (per unit ground area) for leaf, wood, soil, total heterotrophic, and total autotrophic respiration were 2.6, 1.1, 3.2, 5.6, and 2.2 mumol(.)m(-2.)s(-1), respectively. Comparing autotrophic respiration with net primary production (NPP) estimates indicated that only similar to30% of carbon assimilated in photosynthesis was used to construct new tissues, with the remaining 70% being respired back to the atmosphere as autotrophic respiration. This low ecosystem carbon use efficiency (CUE) differs considerably from the relatively constant CUE of similar to0.5 found for temperate forests. Our R-eco estimate was comparable to the above-canopy flux (F-ac) from eddy covariance during defined sustained high turbulence conditions (when presumably F-ac &#x3D; R-eco) of 8.4 (95% CI &#x3D; 7.59.4). Multiple regression analysis demonstrated that similar to50% of the nighttime variability in Fa, was accounted for by friction velocity (u*, a measure of turbulence) variables. After accounting for u* variability, mean F-ac varied significantly with seasonal and daily changes in precipitation. A seasonal increase in precipitation resulted in a decrease in F-ac similar to our soil respiration response to moisture. The effect of daily changes in precipitation was complex: precipitation after a dry period resulted in a large increase in F-ac whereas additional precipitation after a rainy period had little effect. This response was similar to that of surface litter (coarse and fine), where respiration is greatly reduced when moisture is limiting, but increases markedly and quickly saturates with an increase in moisture.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd09_soils_veg_tapajos_1104&quot;&gt;CD09_Soils_Veg_Tapajos_1104&lt;/h4&gt;
This data set reports the results of soil and vegetation surveys at four distinct areas within the Tapajos National Forest (TNF), 50 to 100 km south of Santarem, Para, Brazil, in November 1999. At 13 individual sites across the four areas, all located in primary forest, core soil samples at 10, 30 and 50 cm depths were collected and analyzed for dry mass, bulk density, texture, percentage carbon (C), percentage organic matter, and percentage nitrogen (N). At these 13 sites, vegetation was characterized for 250 m long by 10 m wide transects. Biomass was estimated for all stems over 10 cm DBH from allometric relationships for species, measured height, canopy dimension, and diameter. LAI was measured along the transect at 26 points with a LICOR LAI-2000. Canopy foliage samples were collected with a shotgun at dawn and leaf water potential was determined with a pressure chamber. Samples of foliage, wood, bark, fine roots, and litter were analyzed for %N, % C, delta 13C, and delta 15N. There are five comma-delimited ASCII data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd10_co_tapajos_856&quot;&gt;CD10_CO_Tapajos_856&lt;/h4&gt;
This data set contains half-hourly average CO mixing ratios measured from 2001/04/18 to 2003/08/29 in the old-growth upland forest at the Para Western (Santarem) - km 67, Primary Forest Tower Site. This site is in the Tapajos National Forest located in north central Brazil.CO concentrations were measured in air drawn from above the canopy top of tower (approx. 64 meters) using a TEI 48CTL instrument modified for increased stability and sensitivity. The sensor was frequently zeroed by passing ambient air over a CO oxidation catalyst. The span was checked 4 times daily by sampling calibration gases at 100 and 500 ppb. Time in the file is given in UTC (decimal date) at the start of each half hour interval.Associated meteorological parameters, CO2 concentrations and micrometerological fluxes are available in LBA-ECO CD-10 CO2 and H2O Eddy Flux Data at km 67 Tower Site, Tapajos National Forest.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd10_co_co2_maxaranguape_1012&quot;&gt;CD10_CO_CO2_Maxaranguape_1012&lt;/h4&gt;
This data set reports the concentrations of carbon monoxide (CO) and carbon dioxide (CO2), wind direction, wind speed, and air temperature measured at the Maxaranguape Atmospheric Observatory in northeast Brazil, January 4, 2003 - December 27, 2006. The data are 30-minute averages. The concentrations observed at Maxaranguape are representative of upstream atmospheric boundary conditions for the Amazon basin and could be used in conjunction with Santarem data and other data sets to estimate regional budgets for these gasses (Kirchhoff et al., 2003). There is one comma-delimited ASCII text file with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd10_eddyflux_tapajos_860&quot;&gt;CD10_EddyFlux_Tapajos_860&lt;/h4&gt;
This data set reports eddy flux measurements of CO2 and H2O exchange and associated meteorological measurements at the Para Western (Santarem) - km 67, Primary Forest Tower Site. This site is in the Tapajos National Forest located in north central Brazil. Measurements extend from January 2002 through January 2006.Eddy fluxes of CO2 and H2O were measured at two levels (58m and 47m) using tower-mounted closed-path Licor 6262 gas analyzers and Campbell CSAT3 sonic anemometers (Figure 1). Eddy-flux measurements were made at a sampling rate of 8 Hz and averaged over a 1 hour interval.. A comprehensive set of meteorological parameters (air temperature, pressure, PAR, net radiation, precipitation, etc) were also measured.Co-located measurements included a third Licor gas analyzer that measured (a) the CO2 and H2O concentration profiles at 8 levels in and above the canopy (1 level every 2 minutes) and (b) the instantaneous integrated canopy storage of CO2 and H2O, using a design that pulled air simultaneously through all 8 inlets (once every 20 minutes). See related data sets.With the permission of the author, Hutyra, L.R. 2007. Carbon and water exchange in Amazonian rainforests. Ph.D. Thesis, Department of Earth and Planetary Sciences, Harvard University, Cambridge, Massachusetts., is included as a companion file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd10_co2_profiles_tapajos_855&quot;&gt;CD10_CO2_Profiles_Tapajos_855&lt;/h4&gt;
Eddy fluxes of CO2 and H2O are measured at two levels (58m and 47m) using tower-mounted closed-path Licor 6262 analyzers and Campbell CSAT3 sonic anemometers. A third Licor gas analyzer measures (a) the CO2/H2O concentration profile (1 of 8 levels every 2 minutes) and (b) the instantaneous integrated canopy storage of CO2/H2O, using a design pulling air simultaneously through 8 inlets (once every 20 minutes). Comprehensive meteorological data (air temperature, PAR, net radiation, etc) are also included. Pressure and temperature of the Licor cells are controlled to 500 torr and 48 degrees C. Eddy licors are automatically zeroed every 2 hours and the profile licor every 20 minutes. All Licors are automatically calibrated with span gases (at 325, 400, and 475 ppm) every 6 hours.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd10_cwd_tapajos_858&quot;&gt;CD10_CWD_Tapajos_858&lt;/h4&gt;
This data sets reports properties of fallen course woody debris in an old-growth upland forest at the Para Western (Santarem) - km 67, Primary Forest Tower Site. This site is in the Tapajos National Forest located in north central Brazil. Measurements extend from April 2001 through July 2001.Standing and Fallen coarse woody debris (CWD), or necromass were measured in a series of ecological plots at the km 67 eddy flux tower site in the Tapajos National Forest (Figure 2). The data set includes different size classes of debris measured in different plot sizes. Size classes were: 2-10cm (in 64 m2 subplots) , 10-30cm (in 1600 m2 subplots), 30cm (in 38400 m2 subplots), standing (in entire 50m by 1000m transects).
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd10_litter_tapajos_862&quot;&gt;CD10_Litter_Tapajos_862&lt;/h4&gt;
This data set reports litter type and mass in the old-growth upland forest at the Para Western (Santarem) - km 67, Primary Forest Tower Site. This site is in the Tapajos National Forest located in north central Brazil. Measurements extend from July 2000 through June 2005.Litter collection began in July 2000 using 40 circular, mesh screen traps (0.43 m diameter, 0.156 m2) randomly located throughout the 19.75-ha tree-survey area (Rice et al., 2004). Approximately every 14 days, litter was collected, sorted, oven dried at 60 degrees C, and weighed. The litterfall from each trap was sorted into (1) leaves, (2) fruits and flowers, (3) wood , &amp;lt;2 cm diameter, and (4) miscellaneous. Data values reported are the mean and standard error of the 40 mass measurements of each of the litter components and the combined total, that have been converted to the reporting units of Mg/ha/yr.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd10_biometry_tapajos_854&quot;&gt;CD10_Biometry_Tapajos_854&lt;/h4&gt;
This data sets reports biometry measurements of the old-growth upland forest at the Para¡ Western (Santarrem)km 67, Primary Forest Tower Site. This site is in the Tapajos National Forest located in north central Brazil. Measurements extend from July 1999 through March 2005.To monitor tree woody increment, metal dendrometer bands (Figure 1) were placed on a sub-sample of 1000 trees in December 1999. The data set contains estimates of tree diameter at breast height (cm) based on caliper measurements made approximately every six weeks. The first column of data refers to the tree identification number. For a more detailed description of the biometry study refer to Rice et al. 2004.The data file contains a time series of DBH (cm) values from July 1999 through March 2005.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd10_h2o_profiles_tapajos_861&quot;&gt;CD10_H2O_Profiles_Tapajos_861&lt;/h4&gt;
This data set reports vertical profiles of H2O vapor concentrations measured at the Para Western (Santarem) - km 67, Primary Forest Tower Site (Figure 1). This site is in the Tapajos National Forest located in north central Brazil. Measurements extend from January 2002 through January 2006.H2O concentrations were measured at 8 levels on the tower (62.2, 50, 39.4, 28.7, 19.6, 10.4, and 0.91 m). Sample air was drawn at 1000 sccm (standard cubic centimeters per minute) through 8 profile inlets in sequence (2 minutes at each level) and then a mixed air sample was simultaneously drawn from all 8 levels to obtain a total column integral (once every 20 minutes) and analyzed with an infrared gas analyzer (IRGA, LI-6262, Licor, Lincoln, NE). Data were averaged over a 1 hour interval. Calibration for H2O used two independent calibrations for the IRGA concentration measurements: (a) the nighttime relationship between ambient temperature measurements and sonic temperature measurements; (b) a chilled mirror dew point hygrometer mounted on the tower. See Appendix A of Hutyra (2007) for addition details about calibration methods. Co-located measurements included eddy fluxes of CO2 and H2O were measured at two levels (58m and 47m) using tower-mounted closed-path Licor 6262 gas analyzers and Campbell CSAT3 sonic anemometers. And a comprehensive set of meteorological parameters (air temperature, pressure, PAR, net radiation, precipitation, etc) were also measured. With the permission of the author, Hutyra, L.R. 2007. Carbon and water exchange in Amazonian rainforests. Ph.D. Thesis, Department of Earth and Planetary Sciences, Harvard University, Cambridge, Massachusetts., is included as a companion file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd10_temperature_profiles_tapajos_863&quot;&gt;CD10_Temperature_Profiles_Tapajos_863&lt;/h4&gt;
This data set reports temperature measurements at the Para Western (Santarem) - km 67, Primary Forest Tower Site. This site is in the Tapajos National Forest located in north central Brazil. Measurements extend from January 2002 through January 2006 (Figure 1).Air temperature measurements were collected at 8 levels on the tower (61.9, 49.8, 39.1, 28.4, 18.3, 10.1, 2.8, and 0.6 m). Temperature measurements were made with aspirated thermistors (Met One 076B-4 aspiration with YSI 44032 thermistors) and averaged over a 1 hour interval.Co-located measurements included a Licor gas analyzer that measured (a) the CO2 and H2O concentration profiles at 8 levels in and above the canopy (1 level every 2 minutes), (b) the instantaneous integrated canopy storage of CO2 and H2O, using a design that pulled air simultaneously through all 8 inlets (once every 20 minutes), and (c) eddy fluxes of CO2 and H2O were measured at two levels (58m and 47m) using tower-mounted closed-path Licor 6262 gas analyzers and Campbell CSAT3 sonic anemometers. A comprehensive set of meteorological parameters (air pressure, PAR, net radiation, precipitation, etc) were also measured. See related data sets.With the permission of the author, Hutyra, L.R. 2007. Carbon and water exchange in Amazonian rainforests. Ph.D. Thesis, Department of Earth and Planetary Sciences, Harvard University, Cambridge, Massachusetts., is included as a companion file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd10_dbh_tapajos_859&quot;&gt;CD10_DBH_Tapajos_859&lt;/h4&gt;
This data sets reports diameter at breast height (DBH) measurements in the old-growth upland forest at the Para Western (Santarem) - km 67, Primary Forest Tower Site. This site is in the Tapajos National Forest located in north central Brazil. Measurements were made periodically from July 1999 through August 2005.Trees with DBH &amp;gt;35cm were measured for ~2600 trees in four 5ha transects. Trees &amp;gt;10cm were measured in a smaller area (Rice et al., 2004). Measurements were made in 1999, 2001, and 2005. Trees are identified by local common names. A cross reference to scientific names is provided as a companion file.Coarse woody debris and litter samples and measurements were collected same area. See related data sets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd11_forest_degradation_1118&quot;&gt;CD11_Forest_Degradation_1118&lt;/h4&gt;
This data set reports the results of vegetation field surveys that measured tree height and diameter at breast height (DBH) in defined size classes at three study sites -- Santarem, Para; Paragominas, Para; and Alo Brasil, Mato Grosso, Brazil, from 2001-2003. At each site, plots and transects within plots, were defined that represented different types of logging and fire treatments, each including one primary forest plot used as a control. Along each transect all trees with more than 30 cm DBH were measured. Dead standing trees were also measured and classified in three classes of decomposition. A 4 m wide transect was used to measure individuals between 10 and 30 cm DBH. Six small subplots were set along each transect to measure regeneration individuals from 2-10 cm DBH and 0-2 cm DBH. DBH is also provided for stumps found in each of the logged forest plots. There are ten comma-delimited data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd15_productivity_1167&quot;&gt;CD15_Productivity_1167&lt;/h4&gt;
This data set provides mean leaf area index (LAI), dendrometry band measurements, and litterfall mass from samples collected at the km 67 research site, Topajos National Forest, Para, Brazil. Litterfall collections were from January 23, 2004 through December 3, 2004, dendrometer measurements were monthly between December 2003 and December 2004, and LAI measurements were collected from January 26, 2004 through November 3, 2004. All measurements were taken at the km 67 site in the Tapajos National Forest. This site is situated in an area of Amazonian primary tropical forest belonging to the municipality of Belterra, Para, Brazil. The forest is mostly evergreen with a few deciduous species. The canopy is characterized by large emergent trees up to 55-m tall, with a closed canopy at approximately 40-m; there are few indications of recent anthropogenic disturbance other than hunting trails. Measurement plots (50) were established along 4 transects at the site and within each plot, 5 subplots were established. The longest transect (25 m x 500 m) was the location of 20 (25 m x 25 m) plots. The other 3 transects (25 m x 250 m) contain 10 plots per transect. Note that the assignment of plots to transects is not provided. There are four comma-delimited data files (.csv) with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd17_forest_survey_1254&quot;&gt;CD17_Forest_Survey_1254&lt;/h4&gt;
This data set provides measurements for diameter at breast height (DBH), tree height, distance from tree stems to the furthest canopy element, and a species survey of secondary forests in Para and Rondonia, Brazil, from 2002-2003. The forest areas were defined as Type A and Type B stands. Measurements were made in the overstory, understory, and midstory of each stand. Type A stands were sampled intensively, with the goal of providing high-fidelity spatial information about the 3-dimensional structure of the stand. These stands were 60 x 60-m (0.36-ha) areas divided into 10 x 10-m grids of uniform clearing and abandonment history and were identifiable from Landsat images. Type B stands were sampled extensively, with the goal of providing unbiased estimates of biomass, along with some information about the vertical structure of the stand and of spatial variability. These stands were polygons of uniform clearing and afforestation history based on multitemporal Landsat imagery, and varied in size and shape. The Landsat files provide classified land cover for each scene and can be used as a time series to evaluate land cover change over time. Each file is a geolocated land cover map based on 30-m Landsat data. NOTE: There were additional files which could not be archived due to file problems. Data Quality Statement: The Data Center has determined that this data set has missing or incomplete data, metadata, or other documentation resulting in diminished usability of this product. Known Problems: Some unresolved issues remain where data values are inconsistent with the variable descriptions provided with the data set. The site identification and plot identification values are not consistently used in all three data files. The variables are not adequately described.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd32_fluxes_brazil_1842&quot;&gt;CD32_Fluxes_Brazil_1842&lt;/h4&gt;
This dataset is a compilation of carbon and energy eddy covariance flux, meteorology, radiation, canopy temperature, humidity, CO2 profiles and soil moisture and temperature profile data that were collected at nine towers across the Brazilian Amazon. Independent investigators provided the data from a variety of flux tower projects over the period 1999 thru 2006. This is Version 2 of the tower data compilation, where the data have been harmonized across projects, additional quality control checks were performed, and have been aggregated to hourly, daily, 16-day, and monthly timesteps. This integrated dataset is intended to facilitate integrative studies and data-model synthesis from a common reference point.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd32_lba_mip_drivers_1177&quot;&gt;CD32_LBA_MIP_Drivers_1177&lt;/h4&gt;
The source meteorological observations for the forcing data, from the nine Brazilian flux towers, were recently published as Saleska, et al. (2013). See related data sets. These source data were gap-filled according to the LBA-MIP standard protocol. Note that the CAX forest tower was not included in the MIP. See the companion file driver_data.pdf for additional gap-filling information. There are 34 data products with this data set and they are provided in both text (.txt) and ALMA-compliant NetCDF (.nc) formats. The files have been compressed into nine .zip files according to site.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd34_amazon_hyperion_1064&quot;&gt;CD34_Amazon_Hyperion_1064&lt;/h4&gt;
This data set contains 20 multispectral surface reflectance images collected by the EO-1 satellite Hyperion sensor at 30-m resolution and covering the entire Amazon Basin for 2002 - 2005. All images were converted to GeoTiff format for distribution. The respective ENVI .hdr files are included as companion files and contain image projection and band information. The selected multispectral images were processed using ENVI software as described in Chambers et al. (2009). Bands with uncalibrated wavelengths and those with low spectral response were removed leaving a spectral subset of generally 196 bands (some images have fewer). A cloud mask was developed using 2-d scatter plots of variable reflectance bands to highlight clouds as regions of interest (ROIs), allowing clouds and cloud edges to be masked. A de-streaking algorithm was then applied to the image to reduce variance in balance between the vertical columns. Apparent surface reflectance was calculated for this balanced image using the atmospheric correction algorithm ACORN in 1.5pb mode (AIG-LLC, Boulder, CO). The images (18 of the 20) were georeferenced using the corresponding Advanced Land Imager (ALI) satellite images.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd34_amazon_landsat_1176&quot;&gt;CD34_Amazon_Landsat_1176&lt;/h4&gt;
This data set provides the results of fractional land cover analysis for nonphotosynthetic vegetation (NPV) from two Landsat images of Manaus, Brazil, for October 14, 2004, and for July 29, 2005. Both images are from Landsat 5, path 231, row 62. The Manauas area experienced a squall line with intense downbursts from January 16-18, 2005, that resulted in widespread blowdown and tree mortality. The pre- and post-disturbance Landsat images were obtained and processed using spectral mixture analysis (SMA) in order to investigate forest disturbance and tree mortatility resulting from the downburst. SMA was based on scene-derived end-members of green vegetation (GV, photosynthetically active vegetation), NPV ( wood, dead vegetation, and surface litter), soil, and shade obtained using a pixel purity index (PPI) algorithm (Negron-Juarez et al., 2010). Changes in NPV due to disturbance were calculated by subtracting the 2004 NPV image from the 2005 NPV image. This NPV difference image is provided. There are three image files (.tif) with this data set: The two Landsat images that were georectified and converted to reflectance values and the NPV difference image. DATA QUALITY STATEMENT: The Data Center has determined that there are questions about the quality of the data reported in this data set. The data set has missing or incomplete data, metadata, or other documentation that diminishes the usability of the products. KNOWN PROBLEMS: Four additional images were needed to make this data set complete but are unavailable. Specifically, the two images resulting from SMA as applied to the Landsat images collected on the 14th of October, 2004 and the 29th of July, 2005 to determine per-pixel fractional abundance of GV, NPV (wood, dead vegetation, and surface litter), soil, and shade and the 2004 NPV and 2005 NPV images that were used to derive the ??NPV changes? image (which we do provide) (Negron-Juarez, et al., 2010).
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd36_saldas_1162&quot;&gt;CD36_SALDAS_1162&lt;/h4&gt;
This data set provides South American Land Data Assimilation System (SALDAS) forcing data including atmospheric fields necessary for land surface modeling for South America which are derived by combining modeled and observation based sources. The forcing data cover the entire continent of South America at 0.125 degree resolution and are built around the model-calculated values of air temperature, wind speed and specific humidity at two meters, surface pressure, downward shortwave and longwave surface radiation, and precipitation from the South American Regional Reanalysis (SARR). These SARR data (Aravequia et al. 2007), which were released in 2006 by INPE/CPTEC, are a medium-term, dynamically consistent, high-resolution (0.125 degree), high-frequency, atmospheric dataset covering South America. The forcing data are available at a 3-hourly time step for a 5-year period from 2000 to 2004. There are 60 monthly .zip files with each zipped file containing ~240 3-hourly time step data files for that particular month in NetCDF format. Each zipped file is approximately one GB in size.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cd37_biomass_landsat_glas_1145&quot;&gt;CD37_Biomass_Landsat_Glas_1145&lt;/h4&gt;
This data set provides tree age, forest formation, and land cover classification maps, and estimates of landscape-level above-ground live woody biomass (AGLB) for secondary forests in Rondonia, Brazil. The Threshold Age Mapping Algorithm (TAMA) was applied to a densely spaced time series of Landsat images (1975 to 2003) to derive forest type and age classification maps. The AGLB of the secondary forest was estimated by combining the forest classification map with coincident biomass estimates from the Geoscience Laser Altimeter System (GLAS). There are five raster images and three comma-delimited data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc01_cities_communities_roads_1058&quot;&gt;LC01_Cities_Communities_Roads_1058&lt;/h4&gt;
This data set contains the boundaries of the four major cities in the Northern Ecuadorian Amazon, the locations of primary communities in the colonist settlement area, and the locations of the road network, circa 2002. This area in northeastern Ecuador, know as the northern Oriente of Ecuador, borders the Andes Mountains and contains the headwaters of the Amazon River. The road network was originally digitized from 1:50,000 scale topographic maps from 1990. The surface attributes for the majority of the roads have been updated based on later remote sensing and field observations from 1999 and 2002. There are three compressed (.zip) files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc01_hydrography_edaphology_nec_1059&quot;&gt;LC01_Hydrography_Edaphology_NEC_1059&lt;/h4&gt;
This data set provides map images of hydrographic, morphologic, and edaphic features for the northern Amazon Basin in eastern Ecuador. The hydrographic data are available at two scales based on the 1:50,000 and 1:250,000-scale topographic source maps that were generated in 1990 and 1993, respectively. Morphological and edaphological data were digitized from a 1:500,000 map published in 1983. There are 3 compressed (.zip) data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc01_landsat_1187&quot;&gt;LC01_Landsat_1187&lt;/h4&gt;
This data set contains a time series of early Landsat-4 MSS satellite imagery as well as Landsat-5 TM and Landsat-7 ETM+ satellite imagery of the northern Ecuadorian Amazon. Some of the TM and ETM images have been georectified to UTM Zone 18 South, WGS84 Datum. Not all of the images have been georectified.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc01_lulc_classes_ecuador_isa_1084&quot;&gt;LC01_LULC_Classes_Ecuador_ISA_1084&lt;/h4&gt;
This data set contains Landsat TM imagery for the years 1986, 1989, 1996, and 1999, that have been classified into four land use/land cover (LULC) classes: Forest, Non-Forest Vegetation, Urban/Barren, and Water; and a fifth class of Clouds/Shadows. The areas of interest were the four Intensive Study Areas (ISA) of the University of North Carolina&amp;#39;s Carolina Population Center (CPC) Ecuador Projects: Eastern Intensive Study Area; Northern Intensive Study Area; Southern Intensive Study Area, and Southwestern Intensive Study Area. These areas are in the Northern Ecuadorian Amazon, in the area known as the northern Oriente of Ecuador. The resolution of the data is 30 meters. There are 12 image files (.tif) with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc01_boundaries_ecuador_1057&quot;&gt;LC01_Boundaries_Ecuador_1057&lt;/h4&gt;
This data set contains the national and provincial boundaries of Ecuador as well as the boundaries of two national parks: the Cuyabeno Wildlife Reserve and the Yasuni National Park. There are four data files in ESRI ARCGIS Shapefile format within this data set. Each shape file has been compressed into a single compressed file (.zip).
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc01_households_nec_1052&quot;&gt;LC01_Households_NEC_1052&lt;/h4&gt;
This data set reports summary statistics from socioeconomic and demographic surveys administered to the male and female heads of household on 767 farm plots. The surveys were performed in the provinces of Sucumbios and Napo/Orellana, in the northern Ecuadorian Amazon colonist settlements (Oriente) in 1999 (Pan and Bilsborrow, 2005). In addition, perception of, and opinions about local climate, soil quality, and environmental contamination were assessed for both the male and female heads of household. There are two comma-delimited (csv) ASCII data files. One file provides summary data from male respondents; the other data file provides summary responses from the female household survey (generally the spousal respondent). The original questionnaire forms are included as companion files (PDF format).
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc01_srtm_dem_90m_nec_1083&quot;&gt;LC01_SRTM_DEM_90m_NEC_1083&lt;/h4&gt;
This data set provides 90-meter resolution Digital Elevation Model data used in the University of North Carolina&amp;#39;s Carolina Population Center (CPC) Ecuador Projects. The topographic data were derived from Shuttle Radar Topography Mission (SRTM) C-band and X-band interferometric synthetic aperture radars (IFSARs) data that were acquired over 80% of Earth&amp;#39;s land mass in February 2000. This data set includes one image in GeoTiff format that is a subset for the Northern Ecuadorian Amazon region.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc01_topography_ecuador_isa_1082&quot;&gt;LC01_Topography_Ecuador_ISA_1082&lt;/h4&gt;
This data set contains topographic/geomorphological data associated with the four Intensive Study Areas (ISAs) in the Northern Ecuadorian Amazon (northern Oriente) that are part of the University of North Carolina&amp;#39;s Carolina Population Center (CPC) Ecuador Projects study. Study area boundaries were developed directly from 1:50,000 topographical maps. Point elevation features and 20-meter elevation contours were digitized from these same maps. Digital elevation models (DEMs) were derived from these elevation data and, in turn, terrain aspect and terrain slope were derived from the digital elevation models. Only boundary data were provided for the southwestern ISA. These data are provided in ESRI shapefile format and GeoTiff. There are six compressed (.zip) data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc02_permplot_acre_1237&quot;&gt;LC02_PermPlot_Acre_1237&lt;/h4&gt;
This data set provides diameter at breast height (DBH) measurements for 1,063 trees located at the Catuaba Experimental Farm, and 812 trees located in the Humaita Forest Reserve. Both sites are in the state of Acre, southwest Amazonia, Brazil. Measurements were made on individuals with DBH between 10 and 35 cm and individuals with DBH &amp;gt; 35 cm. The Catuaba Experimental Farm is part of a forest fragment of approximately 800 ha. The Humaita Forest Reserve is located in a 1,500-ha forest band with dominant bamboo characteristic. Ten-ha areas were inventoried at both sites. There is one data file in comma-delimited (.csv) format with this data set. There is also one companion data file with supplemental Catuaba site tree height and biomass data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc02_meteorology_acre_1091&quot;&gt;LC02_Meteorology_Acre_1091&lt;/h4&gt;
This data set provides meteorological measurements collected from 3 different meteorological stations within a radius of 8 km in Rio Branco, Acre Brazil, for the periods of June of 1970 to 1974, December of 1974 to 1980, and May of 1980 thru May 31, 2001. Daily average values for rainfall, relative humidity, evapotranspiration, maximum and minimum temperature, pressure, wind direction and speed, solar radiation, and cloud cover are reported. There is one comma-delimited data file with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc02_forest_flammability_acre_1089&quot;&gt;LC02_Forest_Flammability_Acre_1089&lt;/h4&gt;
This data set provides the results of controlled burns conducted to assess the flammability of mature forests on the Catuaba Experimental Farm of the Federal University of Acre - Rio Branco, Acre, Brazil. Controlled burns were conducted in 1998, and the rate of fire spread was calculated based on the duration of the fire and the measured extent of the burned area. Environmental variables measured included type of forest, canopy openness, leaf area index, number of days without rainfall, precipitation, height of litter, litter humidity, brushwood humidity, amount of water in the ground, air temperature, and relative humidity. Results from 50 fires set in 1998 are reported. There is one comma-delimited data file with this data set. These data are part of a larger study reported in the thesis by Elsa Renee HuamÃ¡n Mendoza, Susceptibility of primary forest to fire in 1998 and 1999: A case study in Acre, south-eastern Amazonia, Brazil. The thesis, in Portuguese, is included as a companion file with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc02_goes8_hotpixel_acre_1092&quot;&gt;LC02_GOES8_Hotpixel_Acre_1092&lt;/h4&gt;
This data set provides hot pixel data, as an indicator of fires that were detected by the GOES-8 satellite for the state of Acre, Brazil. Image data were collected for extended periods over the course of 3 years (1998, 2000 and 2001). Data were filtered to select only pixels identified and processed by the GOES-8 Automated Biomass Burning Algorithm (ABBA), where estimates of sub-pixel fire characteristics including size and temperature were able to be determined. There are three comma-delimited ASCII data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc02_water_table_acre_1062&quot;&gt;LC02_Water_Table_Acre_1062&lt;/h4&gt;
This data set reports bi-weekly or monthly depth-to-water measurements for three wells located in a ~1,500 ha forest fragment on the Catuaba Experimental Farm, which is the property of the Federal University of Acre, Brazil. Data were collected between February 1999 and December 2004. There is one comma-delimited ASCII data file with this data set. DATA QUALITY STATEMENT: The Data Center has determined that there are questions about the quality of the data reported in this data set. The data set has missing or incomplete data, metadata, or other documentation that diminishes the usability of the products. KNOWN PROBLEMS: The depth-to-water measurements for the three wells lack ground surface elevation reference points, therefore, the groundwater table elevation for the site cannot be determined. The depth-to-water measurements are of limited use unless paired with other site data for precipitation, tree growth, etc.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc02_map_fire_indicators_1044&quot;&gt;LC02_MAP_Fire_Indicators_1044&lt;/h4&gt;
This data set provides hot pixel data, as an indicator of fires, that were detected by various satellites in the tri-national MAP region (Madre de Dios-Peru, Acre-Brazil, and Pando-Bolivia) in 2003, 2004, 2005, and 2006. Data from the following satellites/sensors were compiled: NOAA-12, NOAA-14, NOAA-15, and NOAA-16, which transports the AVHRR sensor; GOES-8 and GOES- 12, which transports the GOES Imager; and AQUA and TERRA, both which transport the MODIS sensor. These data were made available by the Centro de PrevisÃ£o do Tempo e Estudos ClimÃ¡ticos (CPTEC) of the Instituto Nacional de Pesquisas Espaciais (INPE) via the internet (&lt;a href&#x3D;&quot;http://sigma.cptec.inpe.br/queimadas/&quot;&gt;http://sigma.cptec.inpe.br/queimadas/&lt;/a&gt;). This data set contains 12 comma-delimited ASCII data files. Hot pixel data from satellites can be used as an indicator of fires and for the understanding of fire frequency in remote areas. The publication by Vasconcelos and Brown, 2007, which has been included as a companion file, describes the application of these data in the MAP region. In addition to the the hot pixel data, each observation has a derived vegetation type, susceptibility to fire, recent and past precipitation amounts, and a calculated fire risk value. These data are described in the Fire Risk Factor companion file, by Alberto W. Setzer and Raffi A. Sismanoglu, Version 5, February 2006.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc02_streams_acre_1243&quot;&gt;LC02_Streams_Acre_1243&lt;/h4&gt;
This data set provides coordinates for points at the mouth of tributaries of the Acre River in the Tri-national River Basin in South America. Three Global Positioning System (GPS) readings were made at the outlet of each tributary and the average of the three readings is reported. The Tri-national River Basin is located in the tri-national frontier region of Madre de Dios, Peru, Acre, Brazil, and Pando, Bolivia (known as the MAP region). The MAP region is approximately 300,000 km2. The Acre River flows through Brazil, Bolivia, and Peru. Data on the basin drainage network from the Digital Elevation Model (DEM) Shuttle Radar Topography Mission (SRTM) was obtained as a source of information for the border areas. The GPS readings were part of an assessment of the reliability of the DEM/SRTM drainage network data (Maldonado and Brown, 2003). There is one data file in comma-delimited (.csv) format and one compamion file (.pdf) with this data set. DATA QUALITY STATEMENT: This data set provides GPS coordinates only and is not associated with any additional measurements. There is no associated research documentation.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc03_hypsography_dem_1094&quot;&gt;LC03_Hypsography_DEM_1094&lt;/h4&gt;
This data set provides four related spatial data products for four study areas across the Brazilian Amazon: Manaus, Amazonas; Tapajos National Forest, Para Western (Santarem); Rio Branco, Acre; and Rondonia, Rondonia. Products include vector data showing (1) roads, (2) rivers, and (3) hypsography and (4) digital elevation model (DEM) images that were encoded from the hypsography vectors. There are 15 data files with this data set which includes 12 compressed .zip files containing ArcInfo shape files and 3 GeoTIFFS. This data set contains vector data showing roads, rivers, and hypsography for each study area in ESRI ArcGIS shapefile format. The vectors were hand-digitized by the Images Company in Brazil from paper maps produced by the Brazilian government. Depending on the scale of the original maps, the digitization errors vary. For some maps, some vectors are missing. Data were manually checked for duplicate or extra vectors. These data sets were derived from several map sheets produced from aerial coverages dating from 1974 to 1978. The DEM images were encoded from the hypsography vectors and are provided in GeoTIFF format. The attribute value associated with each line and point in the vector segment is encoded into the image channel; the image channel is then filled in by interpolating image data between encoded vector data. For each DEM: 1 image channel with pixel resolution &#x3D; 25m x 25m. DEM images are provided for Manaus, Tapajos National Forest, and Rondonia. The files for Rio Branco were unusable due to a documentation error. DATA QUALITY STATEMENT: The Data Center has determined that there are questions about the quality of the data reported in this data set. The data set has missing or incomplete data, metadata, or other documentation that diminishes the usability of the products. KNOWN PROBLEMS: The data providers note that due to limited resources, these data have been neither validated nor quality-assured for general use. For that reason, extreme caution is advised when considering the use of these data. - Any use of the derived data is not recommended because the results have not been validated. - However, the DEM, vectors, and orthorectified SAR data (related data set) can be used if the user understands how these were produced and accepts the limitations.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc03_sar_lc_biomass_1093&quot;&gt;LC03_SAR_LC_Biomass_1093&lt;/h4&gt;
This data set provides three related land cover products for four study areas across the Brazilian Amazon: Manaus, Amazonas; Tapajos National Forest, Para Western (Santarem); Rio Branco, Acre; and Rondonia, Rondonia. Products include (1) orthorectified JERS-1 and RadarSat images, (2) land cover classifications derived from the SAR data, and (3) biomass estimates in tons per hectare based on the land cover classification. There are 12 image files (.tif) with this data set. Orthorectified JERS-1 and RadarSat images are provided as GeoTIFF images - one file for each study area. For the Manaus and Tapajos sites: The images are orthorectified at 12.5-meter resolution and then re-sampled at 25-meter resolution. For the Rondonia and Rio Branco sites: The images from 1978 are orthorectified at 25-meter resolution and then re-sampled at 90-meter resolution. Each GeoTIFF file contains 3 image channels: - 2 L-band JERS-1 data in Fall and Spring seasons and - 1 C-band RadarSat data. Land cover classifications are based on two JERS-1 images and one RadarSat image and provided as GeoTIFFs - one file for each study area. Four major land cover classes are distinguished: (1) Flat surface; (2) Regrowth area; (3) Short vegetation; and (4) Tall vegetation. The biomass estimates in tons per hectare are based on the land cover classification results and are reported in one GeoTIFF file for each study area. DATA QUALITY STATEMENT: The Data Center has determined that there are questions about the quality of the data reported in this data set. The data set has missing or incomplete data, metadata, or other documentation that diminishes the usability of the products. KNOWN PROBLEMS: The data providers note that due to limited resources, these data have been neither validated nor quality-assured for general use. For that reason, extreme caution is advised when considering the use of these data. Any use of the derived data is not recommended because the results have not been validated. However, the DEM and vectors (related data set), and orthorectified SAR data can be used if the user understands how these were produced and accepts the limitations.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc04_ibis_model_1139&quot;&gt;LC04_IBIS_Model_1139&lt;/h4&gt;
The provided data were generated by the Integrated BIosphere Simulator (IBIS) terrestrial ecosystem model (Foley et al. 1996, Kucharik et al. 2000) using data from the CRU05 climate record for the years 1921-1998 (New et al. 2000). Data are included for the annual net ecosystem exchange of the surface, microbial respiration, root respiration, total soil respiration, soil moisture, leaf area index, drainage, and surface and subsurface runoff, for the entire Amazon and Tocantins basins. The data files are provided in netCDF format and standard ESRI ARCGIS ARC/INFO ASCIIGRID format. The netCDF files consist of either annual or monthly means from 1921 to 1998. The ASCII files are available only for the annual mean files.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc04_macrohydrology_1048&quot;&gt;LC04_Macrohydrology_1048&lt;/h4&gt;
This data set provides continental-scale hydrological river flow routing parameter data for the Amazon and Tocantins River basins at 5 minute (~9 km) resolution (Costa et al., 2002). The data set includes four geospatial data files (in standard ESRI Arc/Info ASCII Grid format): (1) the river network (flow direction); (2) sinuosity of each of the main rivers, measured at 111 river sections in the basins; (3) depth to the water table; and (4) transmissivity of the aquifer. The latter two parameters were derived from measurements taken at 81 wells located throughout the basins. There is also a compressed file (.zip) which contains the time series of monthly mean river discharge and long-term climatology (monthly mean) for the period of record at each of 122 fluviometric stations located throughout the basin. These files are provided in ASCII common-separated (.csv) format. Also included in this data set are two data files in .csv format; one containing river discharge station location and drainage area information and one containing original well data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc04_land_use_5min_906&quot;&gt;LC04_Land_Use_5min_906&lt;/h4&gt;
Amazonia has been under considerable development pressure as croplands and pasture are established in areas formerly occupied by tropical forest and cerrado. Although this region is an important part of several important planetary biogeochemical cycles, the location and impact of human land use are not well understood. In particular, there is no existing satellite-based map of agriculture across the Amazon or Tocantins river drainage basins. Recent efforts have classified land cover across this vast region, although they disagree on the location and amount of cropland and do not directly address pasture, a land use that has grown in importance in the last 2 decades. Here we present an analysis of land cover and land use practices over the Amazon and Tocantins basins of South America. In this study, we demonstrate how satellite imagery and agricultural censuses can be merged in order to provide a geographically explicit, fine- scale description of land cover and land use practices. The result depicts the fraction of each 5-min (9 x 9 km) grid cell that was devoted to agricultural activity during the mid-1990s. The resultant map retains many of the characteristics of the agricultural census data, but with a much finer spatial resolution. During the mid-1990s, cultivated area is estimated to have been 1.7 x 10(7) ha (2.5% of the basin), natural pasture is estimated at 3.3 x 10(7) ha (4.9% of the basin), and planted pasture is estimated to cover 3.3 x 10(7) ha (4.9% of the basin). Perhaps more important than the quantities, however, is that these data sets provide a new blend of ground- based and satellite-based spatially explicit data. This snapshot can be used as a basis to project either forward or backward in time, as a new check of finer scale land use classifications or as a driver of ecosystem models.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc04_thmb-hydra_model_1138&quot;&gt;LC04_THMB-HYDRA_Model_1138&lt;/h4&gt;
The model output data provided were generated by the THMB 1.2 (Terrestrial Hydrology Model with Biogeochemistry) model which simulates the flow of water through groundwater systems, rivers, lakes and wetlands. The model operates at a 5-minute latitude-by-longitude grid with a 1-hour time step and requires as boundary conditions: topography, evaporation from water surfaces, surface runoff, base flow, and precipitation. Data are included for the mean monthly simulated water height above flood stage, mean monthly simulated river discharge, and mean monthly inundated area for the period 1939-1998 for the entire Amazon and Tocantins River basins. There are three netCDF files (.nc) with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc05_bdff_biomass_soils_1040&quot;&gt;LC05_BDFF_Biomass_Soils_1040&lt;/h4&gt;
This data set reports (1) total aboveground dry biomass based on detailed estimates of all live and dead plant material, (2) results from repeated surveys of aboveground biomass allowing the calculation of above-ground productivity, and (3) soil chemical and physical characteristics for 50 1-ha plots of undisturbed and fragmented central Amazonian rainforest within the Biological Dynamics of Forest Fragments Project (BDFFP) study area. The reported data are plot-level summaries based on plant and soil samples and measurements obtained over the 1997 to 2001 timeframe. The BDFFP study area is an experimentally fragmented landscape spanning 1,000 km2 located 70-90 km north of Manaus, Amazonas, Brazil. For additional information about the BDFFP and research conducted at the site, please visit their web site at &lt;a href&#x3D;&quot;http://pdbff.inpa.gov.br/index.html&quot;&gt;http://pdbff.inpa.gov.br/index.html&lt;/a&gt;. There are six comma-separated ASCII data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc07_lake_chlorophyll_modis_1000&quot;&gt;LC07_Lake_Chlorophyll_MODIS_1000&lt;/h4&gt;
This data set contains chlorophyll concentration maps of the Amazon River floodplain region from Parintins (Amazonas) to Almeirim (Para). These chlorophyll fraction maps were derived from the Moderate Resolution Imaging Spectroradiometer (MODIS) surface reflectance product (MOD09) for 19 months from April 2002 to December 2003. The study was conducted in a floodplain reach upstream from Santarem, Para, in order to assess seasonal changes in phytoplanktonic chlorophyll-a distributions in the floodplain Lake Curuai. MODIS reflectance data were acquired at four river stages: rising (April), high (June), decreasing (September), and low (November). Chlorophyll maps were derived and used to compute the weighted average of chlorophyll concentration from MODIS images in the region. Field measurements of suspended inorganic matter and chlorophyll-a in Lake Curuai were made almost concurrently with satellite overpasses (Barbosa, 2005). The images and the estimated chlorophyll concentrations were compared to measured chlorophyll concentrations at control points for different hydrological states. This data set may be applied to better understand the seasonal dynamics of primary production of the Amazon floodplains. The maps of chlorophyll-a concentration may be used to model spatial and temporal variations of primary production in this region. The monthly chlorophyll-a maps are provided as GeoTIFF files. There are two formats: (1) color-mapped pixels and (2) pixels as chlorophyll-a concentrations. These latter images are not intended for browsing. These images have pixel values that are the chlorophyll-a concentration in mg/m3 and need to be download and opened in GIS software.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc07_biomass_lgrande_1127&quot;&gt;LC07_Biomass_LGrande_1127&lt;/h4&gt;
This data set reports measurements of aquatic macrophyte biomass, phenology, leaf characteristics, and length and diameter of stems of both submerged and unsubmerged macrophytes. Data were collected from sites in the Monte Alegre Lake region on the eastern Amazon River floodplain in Para, Brazil. Ten field surveys were made at approximately monthly intervals from December 2003 to November 2004. There is one comma-delimited data file with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc07_bathymetry_curuai_999&quot;&gt;LC07_Bathymetry_Curuai_999&lt;/h4&gt;
The bathymetry data provided represent a continuous surface of interpolated point measurements of depth values of Lago Curuai, an Amazon River floodplain lake, upstream from Santarem, Para, Brazil, from measurements made in June of 2004. The first product contains the actual depth values (in meters) of the interpolated continuous surface saved as real numbers in both ENVI and GeoTIFF formats. Also available is a color scaled depth GeoTIFF image which has an embedded color scale bar. This secondary file is meant only for viewing but has the unique advantage of being a GeoTIFF file. Therefore, this map can be a background image with other projected files of interest in the area. Data provided in this data set were used to develop a methodology for processing and applying high resolution bathymetric data acquired with a Lowrance-480M ecosounder in the Amazon floodplain. This research was supported by the addition of Landast/TM images for planning and executing the survey. 4600 km of transects were processed semi-automatically and integrated into a georeferenced database. A digital elevation model with 15 m horizontal resolution and 1 cm vertical resolution was generated for the floodplain. The changes in inundated area and volume of water on the floodplain were estimated. Regression models were constructed to predict flood area and water stored volume from water level. The results of this research show that water level and flooded area mapped from images are good enough for estimating water stored volume in the Lago Grande de Curuai (Barbosa et al., 2006).
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc07_wetlands_fluxes_1209&quot;&gt;LC07_Wetlands_fluxes_1209&lt;/h4&gt;
This data set provides estimates of daily and monthly carbon dioxide (CO2) and methane (CH4) diffusive and ebullitive flux for dry and flooded areas from two study sites, Cuini and Itu, in the interfluvial wetlands of the upper Negro River basin, Brazil. CO2 (ebullitive and diffusive) and CH4 diffusive flux measurements were made one day each month from February 2005 through January 2006 in both permanently and seasonally flooded areas. For the remaining days of each month, fluxes were calculated as the mean of the two measurements bracketing that time period, times the area flooded each day. Total site area, dry area, and seasonally varying flooded area estimates for the two wetlands were determined through analysis of synthetic aperture radar data from Radarsat images. From these estimates, the total flux of CO2 and CH4 for the sites was calculated. Values for CH4 ebullitive flux were determined from a constant for each area based on whether the water was rising or falling and the area flooded. Hydrologic measurements were taken from April 2004 through January, 2006. There are three comma-separated (.csv) data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc07_lake_nutrient_sediments_1050&quot;&gt;LC07_Lake_Nutrient_Sediments_1050&lt;/h4&gt;
This data set reports lake sediment texture and porosity, carbon (C), nitrogen (N), and phosphorus (P) content of surficial sediments, 210Pb-derived nutrient accumulation rates in sediments, and burial rates of C, N, and P in sediments at eleven locations in Lake Calado, Amazonas, Brazil. Field samples were collected between February 1982 and August 1984. There are eight comma-delimited ASCII data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc07_reservoir_ghg_1143&quot;&gt;LC07_Reservoir_GHG_1143&lt;/h4&gt;
This data set provides flux measurements of methane (CH4) and carbon dioxide (CO2) from surface waters to the atmosphere. It also provides CH4, CO2, and oxygen (O2) concentrations of surface water, and concentrations measured at several depths of the Balbina Reservoir in the central Amazon Basin, Amazonas, Brazil. The Balbina Reservoir was formed by impounding the Uatuma River in 1987. Reservoir surface water samples, bottom water samples, and gas samples from static flux enclosures were collected at 10 to 14 sites at monthly intervals between April and November of 2005, and 6 times in February, 2006. Water samples to determine the vertical profiles of temperature, dissolved O2, CH4, and CO2 were collected during the rainy and dry seasons immediately above the dam between September 2004 and February 2006. Water samples were collected downstream from the dam from July 2004 - November 2005 for analysis of CH4 and CO2 concentrations. There are three comma-delimited data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc07_reservoir_methane_emissions_1047&quot;&gt;LC07_Reservoir_Methane_Emissions_1047&lt;/h4&gt;
This data set reports methane (CH4) fluxes at the water-air interface and concentrations and isotopic signals of CH4 in the bubbles stirred up from the sediment in Tucurui and Samuel reservoirs in 2000 and 2001. Tucurui (deep) reservoir is located near Belem city in the Tocantins-Araguaia basin in the eastern Amazon. Samuel (shallow) reservoir is situated near Porto Velho city in the Jamari River, a tributary of the Madeira River in the western Amazon. Field samples were collected between June 2000 and September 2001. There are two comma-delimited ASCII data files in this data set. This study was carried out to identify differences in methane cycling between deep and shallow reservoirs (Lima, 2005). Isotopic and concentration analyses of methane in bubbles, dissolved in the water column, and emitted to the atmosphere demonstrate that water depth is critical regarding methane emissions from hydroreservoirs in the Amazon. Methanotrophic activities are greater in Tucurui (deep) while light isotopic methane is directly released from Samuel (shallow). Therefore, the methanotrophic layer of the deep reservoir is more efficient in oxidizing methane before reaching the atmosphere, since the quantity of methane in the sediments of the reservoirs were equivalent.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc07_smmr_inundated_area_1051&quot;&gt;LC07_SMMR_Inundated_Area_1051&lt;/h4&gt;
This data set reports the monthly record of inundated area, in square km, for six floodplain and open water regions in South America. The following floodplains were analyzed: (1) mainstem Amazon River floodplain in Brazil; (2) Llanos de Mojos (Beni and Mamore rivers) in Bolivia; (3) Bananal Island (Araguaia River) in Brazil; (4) Roraima savannas (Branco and Rupununi rivers) in Brazil and Guyana; (5) Llanos del Orinoco (Apure and Meta rivers) in Venezuela and Colombia; and (6) Pantanal wetland (Paraguay River) in Brazil. Flooded area was estimated at monthly intervals from December 1978 through August 1987 for the Amazon mainstem region and from January 1979 through August 1987 for the other five regions. Inundated area was determined from SMMR (Scanning Multichannel Microwave Radiometer) passive microwave data. Area estimates include permanent open water as well as land subject to seasonal inundation. This data set contains five data files: two comma-delimited (.csv) ASCII data files providing the monthly inundation area values for six floodplain and open water regions in South America; a compressed (.zip) file providing seventeen ESRI Shape files for the region bounding polygons; and two .csv files providing information about the region bounding polygons and latitude/longitude verticies.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc07_monthly_inundated_areas_1049&quot;&gt;LC07_Monthly_Inundated_Areas_1049&lt;/h4&gt;
This data set reports monthly mean inundation areas (square kilometers) for four cover classes of Central Amazon wetlands habitat: Open water (OW), river channel (RC) class, macrophyte (MA) class, and a flooded forest (FF) class, which also incorporates a flooded shrub class. The full study area was a 1.77 million km2 quadrant covering the Central Amazon Basin. Inundation was also calculated from three subsets of this area: (1) covering only the Amazon/Solimoes River mainstem and (2) the Eastern and (3) the Western halves of this mainstem area. There is one comma-delimited ASCII data file in this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc07_spectroradiometry_1144&quot;&gt;LC07_Spectroradiometry_1144&lt;/h4&gt;
This data set includes bidirectional reflectance (BDR) spectra and water-quality data of floodplain lakes of the Solimoes and Negro Rivers in the central Amazon basin, Amazonas, Brazil. Samples and measurements were collected during July 2000 to August 2000. Bidirectional reflectance factors were recorded, at 3 nm intervals from 400 to 900 nm, concurrently with in situ measurements of water temperature and Secchi depth, and collection of samples for analysis of optically active components including total suspended solids, chlorophyll, and dissolved organic carbon (DOC). The lakes sampled were in the low-lying varzea of the Solimoes River (&amp;quot;varzea&amp;quot; is the local name for the floodplain formed by the overflow of white-water rivers) and igapo (&amp;quot;igapo&amp;quot; is the local name for the floodplain formed by the overflow of black-water rivers) of the Negro River. There are two comma-delimited data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc07_airborne_rasters_1274&quot;&gt;LC07_Airborne_Rasters_1274&lt;/h4&gt;
This data set includes high-resolution geocoded mosaics derived from the Validation Overflight for Amazon Mosaics (VOAM) aerial video surveys as part of the Large-Scale Biosphere-Atmosphere (LBA) Experiment in the Amazon. The VOAM flights were carried out in the wet-season (June) 1999 in the Brazilian Amazon to provide ground verification for mapping of wetland cover in the Amazon Basin conducted by the Global Rain Forest Mapping (GRFM) Project JERS-1 (Japanese Earth Remote Sensing Satellite). Digital camcorder systems were installed in a Bandeirante survey plane operated by Brazil&amp;#39;s National Institute for Space Research. The VOAM99 surveys circumscribed the Brazilian Amazon, documenting ground conditions at resolutions on the order of 1-m resolution for wetlands, forests, savannas, and human-impacted areas. Geocoded mosaics were generated by processing the aerial videography into GeoTIFF format, maximizing its usefulness for environmental monitoring applications. Other applications of the VOAM99 videography include acquisition of ground control points for image geolocation, forest biomass estimation, and rapid assessment of fire damage. Geocoded digital videography provides a cost-effective means of compiling a high-resolution validation data set for land cover mapping in remote, cloud-covered regions.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc07_airborne_videography_1272&quot;&gt;LC07_Airborne_Videography_1272&lt;/h4&gt;
This data set presents georeferenced digital video files from Validation Overflight for Amazon Mosaics (VOAM) aerial video surveys as part of the Large-Scale Biosphere-Atmosphere Experiment in the Amazon. The VOAM flights were carried out in the wet-season (June) 1999 in the Brazilian Amazon to provide ground verification for mapping of wetland cover with the Global Rain Forest Mapping (GRFM) Project JERS-1 (Japanese Earth Remote Sensing Satellite) mosaics of the Amazon basin. Digital camcorder systems were installed in a Bandeirante survey plane operated by Brazil&amp;#39;s National Institute for Space Research. The VOAM99 surveys circumscribed the Brazilian Amazon, documenting ground conditions at resolutions on the order of 1-m (wide-angle format) and 10-cm (zoom format) for wetlands, forests, savannas, and human-impacted areas. Other applications of the VOAM videography include acquisition of ground control points for image geolocation, creation of a high-resolution geocoded mosaic of a forest study area, forest biomass estimation, and rapid assessment of fire damage. Geocoded digital videography provides a cost-effective means of compiling a high-resolution validation data set for land cover mapping in remote, cloud-covered regions.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc07_curuai_chl_1134&quot;&gt;LC07_Curuai_chl_1134&lt;/h4&gt;
This data set reports (1) concentrations of total, organic, and inorganic suspended solids; dissolved inorganic, and organic carbon; chlorophyll-a and (2) measurements of turbidity, ph, temperature, transparency, conductivity, and calculated carbon dioxide (CO2) in water samples collected from Lago Curuai (Lake Curuai), in the floodplain of the Amazon River south of Obidos, Para, Brazil. Approximately 70 stations were sampled during four phases of the hydrological cycle: receding (September 2003), low (November 2003), rising (February 2004), and high water (June 2004). There is one comma-delimited data file with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc07_amazon_wetlands_1284&quot;&gt;LC07_Amazon_Wetlands_1284&lt;/h4&gt;
This data set provides a map of wetland extent, vegetation type, and dual-season flooding state of the entire lowland Amazon basin. As described in Hess et al. (2015), the classified image was derived from the Global Rain Forest Mapping Project (GRFM) Amazon mosaics (Rosenqvist et al 2000; Siqueira et al. 2002) acquired during Oct.-Nov. 1995 and May-June 1996, corresponding to the low-flood and high-flood seasons for much of the central Amazon. Hess et al. (2003) mapped wetland extent, vegetative cover, and flooding state for an 18 degree × 8 degree portion of the central Amazon using the dual-season GRFM mosaics. This study extends the previous wetlands mapping to report the first validated estimate of wetland extent, cover, and flooding for the lowland Amazon basin. A wetlands mask was created by segmentation of the mosaics and clustering of the resulting polygons; a rules set was then applied to classify wetland areas into five land cover classes and two flooding classes using dual-season backscattering values. The mapped wetland area of 8.4 × 105 km2 is equivalent to 14 % of the total basin area (5.83 × 106 km2) and 17% of the lowland basin (5.06 × 106 km2). The mapped flooding extent is representative of average high and low-flood conditions for latitudes north of 6 degrees S; flooding conditions were less well captured for the southern part of the basin. The wetlands map is provided in GeoTIFF format using two coordinate systems: unprojected (Geographic) with pixel size of 3 arcseconds, and Albers Conical Equal Area with pixel size of 100 m.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc08_ecosystem_demography_model_1102&quot;&gt;LC08_Ecosystem_Demography_Model_1102&lt;/h4&gt;
This data set provides Ecosystem Demography Model (ED) estimates of potential above-ground net primary production (NPP) (kg C/m2/y), potential average live biomass (kg C/m2), and potential average soil carbon (kg C/m2) for the Brazilian Amazon at 1 degree resolution. Ecosystem Demography Model predicts both ecosystem structure (e.g. above and below-ground biomass, vegetation height and basal area, and soil carbon stocks) and corresponding ecosystem fluxes (e.g. NPP, NEP, and evapotranspiration) from climate, soil, and land-use inputs. Estimates for the Brazilian Amazon include the effects of natural disturbances such as windthrow and fire, but do not include the effects of human land use. To produce these estimates, ED was forced with ISLSCP I data for 1987 and 1988 and averaged into a single average year (Moorcroft et al., 2001). The data are provided for the three estimates in both ASCII text and in NetCDF formatted files.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc08_fire_observations_1095&quot;&gt;LC08_Fire_Observations_1095&lt;/h4&gt;
This data set reports observations of fires in the vicinity of Maraba, Para, Brazil, from November 3-5th, 2001, and in Mato Grosso, Brazil, between Cuiaba and Alta Floresta, for July 12-15th, 2002. These ground-based data were collected by visual inspection from roads primarily during daylight hours. Data include fire position and time, estimates of fire size, and type of vegetation burned. There is one comma-delimited ASCII file with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc08_eos_maps_1155&quot;&gt;LC08_EOS_Maps_1155&lt;/h4&gt;
This data set provides (1) soil maps for Brazil that are digital versions of the MAPA DE SOLOS DO BRASIL (EMBRAPA, 1981) classified at three levels of detail, 19-class, 70-class and 249-class; (2) vegetation maps for Brazil that are digital versions of the MAPA DE VEGETACAO DO BRASIL (IBGE, 1988) classified at three levels of detail, 13-class, 59-class, and an overprint (combination) class; and (3) a land cover map for all of South America that was derived from National Oceanic and Atmospheric Administration (NOAA) Advanced Very High Resolution Radiometer (AVHRR) data over the time period 1987 through 1991 (Stone et al., 1994). The seven soil, vegetation, and general land cover classification maps are provided as GeoTIFF files (.tif) files. There are also three companion files (.pdf), one each, for the soil, vegetation, and land cover maps, with information on map units, class values, codes, and descriptions.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc09_precipitation_940&quot;&gt;LC09_Precipitation_940&lt;/h4&gt;
This data set reports daily total precipitation data retrieved from Brazilian National Institute of Meteorology (INMET) network for three stations near two Amazonian research sites: Altamira, and Santarem, from 1961-1998. Daily precipitation totals are provided in one comma-separated ASCII file for three stations in Para, including two sites in Altamira: Altamira City and on the Transamazon Highway at Km 100 near Medicilandia (operated by EMBRAPA); and, one site in Santarem: Taperinha. Data availability varies by station (sublocation): Altamira City from 1961-1990, Transamazon Km 100 from 1982-1998, and Taperinha from 1983-1992.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc09_transition_matricies_1098&quot;&gt;LC09_Transition_Matricies_1098&lt;/h4&gt;
This data set includes classified land cover transition maps at 30-m resolution derived from Landsat TM, MSS, ETM+ imagery and aerial photos of Altamira, Santarem, and Ponta de Pedras, in the state of Para, Brazil. The Landsat images were classified into several types of land use (e.g., forest, secondary succession, pasture, annual crops, perennial crops, and water) and subjected to change detection analysis to create transition matrices of land cover change. Dates of acquired images represent the most cloud-free image retrievals from 1970-2001 for each site and are therefore not continuous. There are 3 GeoTIFF files (.tif) with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc09_landsat_987&quot;&gt;LC09_Landsat_987&lt;/h4&gt;
This data set includes 15 zipped archives of rectified .tif format Landsat 5 TM and Landsat 7 ETM+ scenes from near the study sites of Altamira, Santarem, Ponta de Pedras, and Bragantina in the state of Para, Brazil and Machadinho D&amp;#39;Oeste in Rondonia, Brazil. Dates represent the most cloud-free image retrievals from 1985-2004 and are therefore not continuous. These images may be useful to evaluate potential environmental impacts resulting from the establishment of colonization projects in the Amazon.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc09_gis_study_areas_986&quot;&gt;LC09_GIS_Study_Areas_986&lt;/h4&gt;
This data set includes 16 zipped archives of shapefiles of cities, rivers and streams, roads, and study area boundaries of several Amazonian study sites: Altamira, Santarem, Bragantina, and Ponta de Pedras, in the state of Para, and 1 site at Machadinho D&amp;#39;Oeste, in the state of Rondonia. Data from Brazil were digitized from Instituto Nacional de Colonizacao e Reforma Agraria (INCRA) maps and other data from Instituto Brasileiro de Geografia e Estatistica (IBGE). These products were prepared in the 2000-2004 time period. The data of creation for the source material is unknown.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc09_soil_composition_938&quot;&gt;LC09_Soil_Composition_938&lt;/h4&gt;
This data set reports basic soil structure and composition information for five Amazonian research sites: Altamira, Bragantina, Tome-Acu, and Ponta de Pedras, all four in the state of Para, Brazil; and one site in Yapu, Colombia. Soil characteristics reported for all five study sites include cation information (e.g., H, Al, Mg, K, Na, S), percent of soil C, N, and organic matter, soil texture/composition and color, pH, and land use history. Soil bulk density and tons of carbon/ha are reported for only three of the study sites: Altamira, Bragantina, and Tome-Acu. All of the data are provided in one comma-separated data file. The five study areas represent characteristic differences in soil fertility and a range of land uses typical of the Amazon region. One of these areas, Altamira, is characterized by above average pH, nutrients, and texture. The other four areas are more typical of the 75 percent of the Amazon that is characterized by Oxisols and Ultisols, with well-drained but low pH and low levels of nutrients. Ponta de Pedras in Marajo Island, located in the estuary, is composed of upland Oxisols and floodplain alluvial soils. Igarape-Acu in the Bragantina region is characterized by both nutrient-poor Spodosols and Oxisols. Tome-Acu, south of Igarape-Acu, represents a mosaic of Oxisols and Ultisols. Yapu, in the Colombian Vaupes, is composed of patches of Spodosols and Oxisols. Three of the areas are colonization regions at various degrees of development: Altamira is a colonization front that opened up in 1971, whereas Tome-Acu was settled by a Japanese population in the 1930s, and Bragantina was settled in the early part of the twentieth century. Marajo (Ponta de Pedras) is the home of caboclos, whereas Yapu is home to Tukanoan Native American populations. In these study areas slash-and-burn cultivation as well as plantation agriculture and mechanized agriculture are employed. Length of fallows vary in these communities. The two indigenous areas leave their land in longer fallow than do the three colonization areas, and the proportion of land prepared from secondary forests increases with length of settlement as the stock of mature forest declines over time.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc09_vegetation_composition_939&quot;&gt;LC09_Vegetation_Composition_939&lt;/h4&gt;
No abstract available.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc10_landsat_tm_852&quot;&gt;LC10_Landsat_TM_852&lt;/h4&gt;
This data set includes Landsat TM scenes from across the Legal Amazon region. A single image is provided for each spatial tile, representing the most cloud-free retrieval from 9/21/86 to 9/17/94. All files are in a single directory, including one band-sequential (bsq) file and one database (ddr) file for each scene.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc10_landsat_etm_846&quot;&gt;LC10_Landsat_ETM_846&lt;/h4&gt;
This data set includes orthorectified Landsat ETM+ scenes across the Legal Amazon region. At least one scene is provided for each spatial tile, representing the most cloud-free retrievals from mid-1999 through late 2001 (Fig. 1). Dates are therefore not continuous but include scenes from July 8, 1999 to November 13, 2001. Data have been atmospherically corrected and orthorectified. The individual images should be highly useful as they include very little cloud cover, but they should not be mosaicked together since retrieval dates vary.Data files (and format) included for each scene are: six multispectral bands (tif), two thermal bands (tif), one panchromatic band (tif), two preview files (jpg), and one metadata file (txt). The individual Geotiff files have been g-zipped and subsequently all of the files for a scene have been g-zipped together for ordering convenience.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc13_gis_cauaxi_890&quot;&gt;LC13_GIS_Cauaxi_890&lt;/h4&gt;
We combined a detailed field study of canopy gap fraction with spectral mixture analysis of Landsat ETM+ satellite imagery to assess landscape and regional dynamics of canopy damage following selective logging in an eastern Amazon forest. Our field studies encompassed measurements of ground damage and canopy gap fractions along multi-temporal sequences of post-harvest regrowth of 0.5-3.5 yr. Areas used to stage harvested logs prior to transport, called log decks, had the largest forest gap fractions, but their contribution to the landscape-level gap dynamics was minor. Tree falls were spatially the most extensive form of canopy damage following selective logging, but the canopy gap fractions resulting from them were small. Reduced-impact logging resulted in consistently less damage to the forest canopy than did conventional logging practices. This was true at the level of individual landscape strata such as roads, skids, and tree falls as well as at the area-integrated scale. A spectral mixture model was employed that utilizes bundles of field and image spectral reflectance measurements with a Monte Carlo analysis to estimate high spatial resolution (sub-pixel) cover of forest canopies, exposed non-photosynthetic vegetation, and soils in the Landsat imagery. The method proved highly useful for quantifying forest canopy cover fraction in the log decks, roads, skids, tree fall, and intact forest areas, and it tracked canopy damage up to 3.5 yr post-harvest. Forest canopy cover fractions derived from satellite observations were highly and inversely correlated with field- and satellite-based measurements. A 450-km^2 study of gap fraction showed that approximately one-half of the canopy opening caused by logging is closed within one year of regrowth following timber harvests. This is the first regional-scale study utilizing field measurements, satellite observations, and models to quantify forest canopy damage and recovery following selective logging in the Amazon.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc13_gis_juruena_888&quot;&gt;LC13_GIS_Juruena_888&lt;/h4&gt;
We combined a detailed field study of canopy gap fraction with spectral mixture analysis of Landsat ETM+ satellite imagery to assess landscape and regional dynamics of canopy damage following selective logging in an eastern Amazon forest. Our field studies encompassed measurements of ground damage and canopy gap fractions along multitemporal sequences of post-harvest regrowth of 0.5-3.5 yr. Areas used to stage harvested logs prior to transport, called log decks, had the largest forest gap fractions, but their contribution to the landscape-level gap dynamics was minor. Tree falls were spatially the most extensive form of canopy damage following selective logging, but the canopy gap fractions resulting from them were small. Reduced-impact logging resulted in consistently less damage to the forest canopy than did conventional logging practices. This was true at the level of individual landscape strata such as roads, skids, and tree falls as well as at the area-integrated scale. A spectral mixture model was employed that utilizes bundles of field and image spectral reflectance measurements with a Monte Carlo analysis to estimate high spatial resolution (subpixel) cover of forest canopies, exposed nonphotosynthetic vegetation, and soils in the Landsat imagery. The method proved highly useful for quantifying forest canopy cover fraction in the log decks, roads, skids, tree fall, and intact forest areas, and it tracked caopy damage up to 3.5 yr post-harvest. Forest canopy cover fractions derived from satellite observations were highly and inversely correlated with field- and satellite-based measurements. A 450-km^2 study of gap fraction showed that approximately one-half of the canopy opening caused by logging is closed within one year of regrowth following timber harvests. This is the first regional-scale study utilizing field measurements, satellite observations, and models to quantify forest canopy damage and recovery following selective logging in the Amazon.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc14_aboveground_prod_1196&quot;&gt;LC14_Aboveground_Prod_1196&lt;/h4&gt;
This data set reports forest biophysical measurements from a rainfall exclusion experiment conducted at the km 67 Seca Floresta site, Tapajos National Forest, Brazil from 1998 to 2006. The purpose was to observe the potential effects of severe water stress on a humid Amazonian forest (Nepstad 2002). Data are reported for stem inventory, tree diameter at breast height (DBH) and height, dendrometer measurements of tree diameter growth increments, canopy density, leaf area index (LAI), and coarse and fine litter mass. The measurements were made monthly from September 28, 1998 through November 10, 2006. There are six comma-delimited data files (.csv), one text file (.txt), and two companion files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc14_amazon_scenarios_1153&quot;&gt;LC14_Amazon_Scenarios_1153&lt;/h4&gt;
This data set provides the results of the two modeled scenarios for future patterns of deforestation across the Amazon Basin from 2002 to 2050. This larger defined Amazon Basin (PanAmazon area) includes the Amazon River watershed, the Legal Amazon in Brazil, and the Guiana region. The model SimAmazonia was used to simulate monthly deforestation in the Amazon Basin from 2002 to 2050 for two scenarios: (1) a &amp;quot;Business-as-Usual&amp;quot; scenario, which considered the deforestation trends across the basin and projected the rates by using historical images and their variations from 1997 to 2002 and then added to that the effect of paving a set of major roads, and (2) a &amp;quot;Governance&amp;quot; scenario, that also considered the current deforestation trends, but assumed a 50% limit imposed for deforested land within each basin&amp;#39;s subregion, and that existing and proposed Protected Areas (PAs), play a decisive role in limiting deforestation as well (Soares et al., 2006). The provided data products include one GeoTiff (.tif) for each year (2002 to 2050) for both model scenarios for a total of 98 files. The files have been compressed in two .zip files, one for each model scenario. There is also one comma-delimited file that contains the model input data derived from satellite deforestation maps.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc14_risque_1147&quot;&gt;LC14_RISQUE_1147&lt;/h4&gt;
A simple GIS soil-water balance model for the Amazon Basin, called RisQue (Risco de Queimadasa -- Fire Risk), was used to conduct an analysis of spatial and temporal patterns of drought in moist tropical forests and the complex relationships between patterns of drought and forest fire regimes from 1995 through 2001. The provided data products are the model output estimates of maximum plant-available soil water (PAWmax) at 10 m depth at 8 km resolution and model data inputs of monthly precipitation and evapotranspiration. RisQue estimates PAWmax at 10 m depth starting with a map of PAWmax (1-2 m depth) developed using 1,565 RADAMBRASIL soil texture profiles and empirical relationships between soil texture and critical soil water parameters and then interpolated to 8 km resolution. In RisQue, plant-available soil water (PAW) is depleted by monthly evapotranspiration estimated using the Penman Monteith equation and satellite-derived radiation and recharged by monthly precipitation. There are three data files with this data set, two .zip, and one GeoTIFF image (.tif). The .zip files expand to 83 .asc files of evapotranspiration and 89 .asc files for precipitation data. The image (.tif) is a map of maximum percent available water at 10 m depth. All the files in this data set are in standard arc/info asciigrid format at 8 km resolution.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc14_surface_roots_phenology_1268&quot;&gt;LC14_Surface_Roots_Phenology_1268&lt;/h4&gt;
This data set contains biomass estimates for coarse roots measured on the forest floor and measurements of fine root growth down to 2-m depth at the km 67 Rainfall Exclusion Experiment site, Tapajos National Forest, Brazil. The study site was part of a rainfall exclusion experiment that was conducted from 1999-2006 to develop an understanding of the physical processes driving the observed soil water dynamics at the site. All surface roots intersected along three 1000-m long x 1-m wide transects were identified to species, measured, and biomass calculated. The collections were made on January 26, 2001 during the experimental rain exclusion period. The fine root growth was measured from 0.5-m to 2-m depth with a rhizotron. The rhizotron tubes were inserted into deep soil pits in the control and treatment plots. Average root growth measurements are provided by depth interval on a monthly basis from July 25, 2000 to December 14, 2003. DATA QUALITY STATEMENT: The Data Center has determined that there are questions about the quality of the data reported in this data set. The data set has missing or incomplete data, metadata, or other documentation that diminishes the usability of the products. KNOWN PROBLEMS: There are discrepancies with the documentation, collection dates reported and collection method for fine roots utilizing rhizotrons.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc14_ree_sla_1211&quot;&gt;LC14_REE_SLA_1211&lt;/h4&gt;
This data set provides measurements of specific leaf area and monthly phenological observations for selected tree and vine species at the km 67 Seca Floresta site, Tapajos National Forest, Para, Brazil. The study site was part of a rainfall exclusion experiment that was conducted from 1999-2006 to develop an understanding of the physical processes driving the observed soil water dynamics at the site. Phenological observations were made from 2001-2004 in rainfall exclusion and control plots. In total, 3,224 leaves were observed across 223 individuals and 56 species. The phenological observations included the month and year when a given leaf was first observed fully expanded and last observed alive. Starting in July 2004 and continuing through January 2006, leaves that had been followed in the phenology study were sampled and leaf area and mass were determined and the specific leaf area was calculated. There are two comma-delimited data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc15_roughness_map_1182&quot;&gt;LC15_Roughness_Map_1182&lt;/h4&gt;
This data set provides physical roughness maps of vegetation canopies in the Amazon Basin. The images are estimates of aerodynamic roughness length (Z0) and zero plane displacement height (D0) at 1-km spatial resolution. The aerodynamic roughness length (Z0) is an important parameter to determine the vertical gradients of mean wind speed and the conditions for momentum transfer over a vegetated or bare rough surface. The maps were produced from a multivariate regression model algorithm developed from field-measured vegetation structure and remote-sensing data. The data input sources included Shuttle Radar Topography Mission (SRTM) (Saatchi, 2013), JERS-1, MODIS, and field data from vegetation biomass plots over the Amazon basin, as well as tower-based wind profile measurements, and roughness parameters from LBA tower sites. There are two GeoTIFF (.tif) files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc15_aglb_distribution_map_908&quot;&gt;LC15_AGLB_Distribution_Map_908&lt;/h4&gt;
The amount and spatial distribution of forest biomass in the Amazon basin is a major source of uncertainty in estimating the flux of carbon released from land-cover and landuse change. Direct measurements of aboveground live biomass (AGLB) are limited to small areas of forest inventory plots and site-specific allometric equations that cannot be readily generalized for the entire basin. Furthermore, there is no space-borne remote sensing instrument that can measure tropical forest biomass directly. To determine the spatial distribution of forest biomass of the Amazon basin, we report a method based on remote sensing metrics representing various forest structural parameters and environmental variables, and more than 500 plot measurements of forest biomass distributed over the basin. A decision tree approach was used to develop the spatial distribution of AGLB for seven distinct biomass classes of lowland old-growth forests with more than 80% accuracy. AGLB for other vegetation types, such as the woody and herbaceous savanna and secondary forests, was directly estimated with a regression based on satellite data. Results show that AGLB is highest in Central Amazonia and in regions to the east and north, including the Guyanas. Biomass is generally above 300 Mg ha-1 here except in areas of intense logging or open floodplains. In Western Amazonia, from the lowlands of Peru, Ecuador, and Colombia to the Andean mountains, biomass ranges from 150 to 300 Mg ha-1. Most transitional and seasonal forests at the southern and northwestern edges of the basin have biomass ranging from 100 to 200 Mg ha-1. The AGLB distribution has a significant correlation with the length of the dry season. We estimate that the total carbon in forest biomass of the Amazon basin, including the dead and belowground biomass, is 86 Pg C with +/- 20% uncertainty.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc15_grfm_jers1_mosaic_1024&quot;&gt;LC15_GRFM_JERS1_Mosaic_1024&lt;/h4&gt;
This data set contains two image mosaics of L-band radar backscatter and two image mosaics of first order texture. The two backscatter images are mosaics of L-band Radar Backscatter at Horizontal-Horizontal (HH) Polarization created from 1,500 images collected by the Japanese Earth Resources Satellite-1 (JERS-1) Synthetic Aperture Radar (SAR) over the Amazon River Basin as part of the Global Rainforest Mapping Project (GRMP). These backscatter image mosaics were developed using data collected over 62 days from August to November of 1995 for the peak of the dry season and for 62 days from May to June of 1996 during the peak of the wet season. The two image mosaics are at 3 arc-sec resolution. Data provided under this project are resampled images at 30 arc-sec resolution (or about 1 km resolution). For each radar backscatter image, first order texture statistical information was derived and is distributed along with the image mosaic. This data set contains four images each in both geotiff and ENVI formats, provided in eight zip files. The four files in ENVI file format contain “_envi” in their file name and when extrapolated contain an envi image (*_envi.dat) and an envi image header file (_envi.hdr). The four files in geotiff format contain “_geotiff” in their file name and when extrapolated contain .tif and .tfw file pairs. See Section 2 for more information about the characteristics of these data files.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc15_spot_metrics_1239&quot;&gt;LC15_SPOT_Metrics_1239&lt;/h4&gt;
This data set provides Normalized Difference Vegetation Index (NDVI) composite images of the Amazon Basin for the years 1999-2000 at approximately1-km spatial resolution. The images were from the VEGETATION 1 sensor, aboard the SPOT 4 satellite. Ten day composite images were reprocessed through several filters for cloud removal. Monthly NDVI data were used to create five metrics: maximum NDVI, minimum of 6 greenest months, range of NDVI between min and max, mean NDVI dry months, and mean NDVI wet months. There are five GeoTIFF (.tif) files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc15_srtm_topography_1181&quot;&gt;LC15_SRTM_Topography_1181&lt;/h4&gt;
This dataset provides a subset of the SRTM30 Digital Elevation Model (DEM) elevation and standard deviation data for the Amazon Basin. SRTM30 is a near-global digital elevation model (DEM) comprising a combination of data from the Shuttle Radar Topography Mission (SRTM), flown in February, 2000, and the earlier U.S. Geological Survey&amp;#39;s GTOPO30 data set. The SRTM30 resolution is 30 arc-sec or about 1 km. In processing the SRTM data, to combine with GTOPO30, the data were resampled from 3 arc-sec to 30 arc-sec. Provided here are the mean elevation and the standard deviation (STD) of the data points used in the averaging. The STD is thus an indication of topographic roughness useful in some applications.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc15_modis_treecover_1035&quot;&gt;LC15_MODIS_TreeCover_1035&lt;/h4&gt;
This data set contains proportional estimates for the vegetative cover types of woody vegetation, herbaceous vegetation, and bare ground over the Amazon Basin for the period 2000-2001. These products were derived from all seven bands of the Moderate-resolution Imaging Spectroradiometer (MODIS) sensor onboard NASA&amp;#39;s Terra satellite. A set of MODIS 32-day composites were used to create the vegetation cover types using the Vegetation Continuous Fields (VCF) (Hansen et al., 2002) approach which shows how much of a land cover such as &amp;quot;forest&amp;quot; or &amp;quot;grassland&amp;quot; exists anywhere on the land surface. The VCF product may depict areas of heterogeneous land cover better than traditional discrete classification schemes which shows where land cover types are concentrated. The original MODIS products are 500-m spatial resolution and are derived from 2000-2001 data products. The data were resampled to 1-km resolution for the regional study under this project, and provided as 3 separate cover type files in ENVI and GeoTIFF file formats that are provided in six zipped files. These products are registered to the rest of the regional data sets over the Amazon basin. These data are also available for download from the Global Land Cover Facility Website (&lt;a href&#x3D;&quot;http://modis.umiacs.umd.edu/&quot;&gt;http://modis.umiacs.umd.edu/&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc18_hyperion_889&quot;&gt;LC18_Hyperion_889&lt;/h4&gt;
This image was collected by the Hyperion sensor on 10-July-2004 at 13:16:16 GMT. It was calibrated to apparent surface reflectance using the ACORN atmospheric model. The Hyperion imager has a spectral range of 400-2500 nm, a spectral resolution of 10 nm, spatial resolution of 30 m, and a swath width of 7.8 km. Sampling is scene based (256 samples, 512 lines) (&lt;a href&#x3D;&quot;http://eo1.usgs.gov/sensors.php&quot;&gt;http://eo1.usgs.gov/sensors.php&lt;/a&gt;). Through these large number of spectral bands, complex land ecosystems can be imaged and accurately classified. Data from the EO-1 Hyperion imaging spectrometer may greatly increase our ability to estimate the presence and structural attributes of selective logging in the Amazon Basin using four biogeophysical indicators not yet derived simultaneously from any satellite sensor: 1) green canopy leaf area index; 2) degree of shadowing; 3) presence of exposed soil and; 4) non-photosynthetic vegetation material. Airborne, field and modeling studies have shown that the optical reflectance continuum (400-2500 nm) contains sufficient information to derive estimates of each of these indicators. Our ongoing studies in the eastern Amazon basin also suggest that these four indicators are sensitive to logging intensity. Satellite-based estimates of these indicators should provide a means to quantify both the presence and degree of structural disturbance caused by various logging regimes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc19_field_2002_1261&quot;&gt;LC19_Field_2002_1261&lt;/h4&gt;
This data set provides measurements for soil physical and chemical properties, rooting depth and weight, leaf area index (LAI), plant area index (PAI), biomass, fraction of photosynthetically active radiation (fPAR), and ground-based reflectance measurements of soil and litter samples. The samples were collected from 23 areas within the Brazilian research sites of the Brasilia National Park (BNP) and Aguas Emnendadas Ecological Station (AE), Brasilia; Cangacu Research Center, Tocantins; and Tapajos National Forest, Para. The research areas were in the most intensely stressed areas in Brazil, with rapid and aggressive land use conversions in forested and cerrado-transition areas. These field measurements were conducted from June to July 2002. There are 61 comma-delimited (.csv) data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc21_fractional_cover_1152&quot;&gt;LC21_Fractional_Cover_1152&lt;/h4&gt;
This data set provides Landsat Enhanced Thematic Mapper Plus (ETM+) imagery, derived classified land cover products, and cloud-water masks for selected Brazilian states (Acre, Amapa, Amazonas, Maranhao, Mato Grosso, Para, Rondonia, and Roraima) for the years 1999-2002. The Landsat ETM+ images were processed to derive fractional land cover types (photosynthetic vegetation [PV], non-photosynthetic vegetation [NPV], and bare substrate) by application of the Carnegie Landsat Analysis System (CLAS) methodology (Asner et al., 2005). CLAS utilizes a quantitative determination of fractional land cover at the subpixel scale (e.g., within each Landsat 30 x 30 m pixel). The resulting images display estimates of subpixel land cover fraction values including free of clouds, cloud shadows, and water. There are 584 .zip files in this data set which when expanded, contain a total of 1,717 (.tif) images files (GeoTiff Standard format).
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc21_foliar_nutrients_1234&quot;&gt;LC21_Foliar_Nutrients_1234&lt;/h4&gt;
This data set provides measurements for foliar nutrients from logging blocks in the Tapajos National Forest, Para Western Santarem, Brazil. Data are included for calcium (Ca), phosphorus (P), magnesium (Mg), nitrogen (N), and potassium (K) concentrations. In March 2003 foliar samples were collected from the cover types remaining after selective logging in 2002: forest, tree-fall gaps, skids, roads, and deck areas. Fresh foliage was also collected in March 2003, from 192 upper canopy species at an intact forest site 17 km from the logging area. There are two data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc21_selective_logging_1172&quot;&gt;LC21_Selective_Logging_1172&lt;/h4&gt;
This data set provides the results of analyses of Landsat Enhanced Thematic Mapper Plus (ETM+) images for selective logging activity in the Brazilian states of Para, Mato Gross, Rondonia, Roraima, and Acre over the years 1999 through 2001. Images were analyzed using the Carnegie Landsat Analysis System (CLAS) to detect and to quantify the amount of damage due to selective logging in the major timber-production states of the Brazilian Amazon. This approach provided automated image analysis using atmospheric modeling for detection of forest canopy openings, surface debris, and bare soil exposed by forest disturbances; and pattern-recognition techniques. CLAS provides detailed measurements of forest-canopy damage at a spatial resolution of 30 x 30m. Fifteen GeoTiff format files are included -- one for each of the three years from 1999-2001 for each of the five states. Each GeoTiff is a single band image where each pixel represents if logging activity was or was not detected. A zero (0) value indicates that no logging was detected, while a value of one (1) indicates that damage from logging was detected. The 15 GeoTiff (.tif) files have been compressed into one .zip file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc21_soil_characteristics_1236&quot;&gt;LC21_Soil_Characteristics_1236&lt;/h4&gt;
This data set provides measurements for soil nutrients from areas that were selectively logged and from control areas in the Tapajos National Forest, Para Western Santarem, Brazil. Data are included for calcium (Ca), phosphorus (P), magnesium (Mg), nitrogen (N), aluminum (Al), iron (Fe), silicon (Si), carbon 13, nitrogen 15, and potassium (K) concentrations. In addition, data are included for Phosphorus fractionation which was performed on a subset of the soils, and soil bulk density measurements. The samples were from clay-dominated (oxisols) soils.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc22_modis_field_val_2004_1262&quot;&gt;LC22_MODIS_Field_Val_2004_1262&lt;/h4&gt;
This data set contains field observations, corresponding GPS points, and point and polygons of deforested areas in the state of Mato Grosso, Brazil, for the period August 2003 to July 2004. The field observations were conducted in the forested areas between Nova Mutum and Sinop, MT. These data were part of a study to validate Moderate Resolution Imaging Spectroradiometer (MODIS) data at 250-m resolution for the detection of deforested areas. There are 16 data files with this data set. This includes 10 shapefile (.shp) and six comma-separated files (.csv).
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc22_modis_field_val_2005_1260&quot;&gt;LC22_MODIS_Field_Val_2005_1260&lt;/h4&gt;
This data set contains field observations, corresponding GPS points, and point and polygons of deforested areas in the state of Mato Grosso, Brazil, for the period March 17-24,2005. Fieldwork was conducted in the regions surrounding Sinop, Mato Grosso, with specific emphasis on large clearings occurring in the Xingu Basin. The field campaign was designed to validate preliminary MODIS deforestation products designed to detect deforestation during the wet season. There are five data files with this data set: four shapefiles (.shp) and one comma-separated file (.csv).
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc22_modis_phenology_mato_grosso_1185&quot;&gt;LC22_MODIS_Phenology_Mato_Grosso_1185&lt;/h4&gt;
This data set, LBA-ECO LC-22 Land Cover from MODIS Vegetation Indices, Mato Grosso, Brazil, provides land cover classifications for Mato Grosso, Brazil, for the years 2000-2001 and 2003-2004. The classifications were derived from annual vegetation phenology information from a time series of Collection 4, 16-day MODerate Resolution Imaging Spectroradiometer (MODIS) Normalized Difference Vegetation Index (NDVI), and the Enhanced Vegetation Index (EVI) vegetation data, at 250-m resolution. A decision tree classifier was trained using field observations and Landsat TM data of land cover from 2003-2004 to identify seven land-cover classes. The classifier was applied to the 2000-2001 and 2003-2004 MODIS ENVI and EVI data. There are two GeoTIFF (.tif) files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc22_post_deforestation_lulc_1099&quot;&gt;LC22_Post_Deforestation_LULC_1099&lt;/h4&gt;
This data set provides (1) areal estimates of deforestation events (&amp;gt;25 ha) that were identified from 2001-2004 in Mato Grosso by the Brazilian Institute for Space Research (INPE) as part of the Program for the Estimation of Deforestation in the Brazilian Amazon (PRODES) and (2) the classification of the post-deforestation land use as either cropland, cattle pasture, or not in production (deforested areas that were never fully cleared or returned immediately to secondary forest) in the years after the large deforestation events from 2001-2005. Data are provided in ESRI shapefile format. There are five compressed (.zip) data files with this data set. Each shapefile represents one year of post-deforestation land use. Land use in the years following deforestation was estimated using annual time series of MODIS NDVI (normalized difference vegetation index) and EVI (enhanced vegetation index). Metrics of vegetation phenology derived annual time series of MODIS NDVI and EVI data were analyzed using a decision-tree classifier to characterize the major cover type in each area of new deforestation. Post-deforestation land use for each large deforestation event was classified based on the classification of MODIS phenology metrics for all years following deforestation during 2002-2005.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc22_modis_vcf_tree_cover_1112&quot;&gt;LC22_MODIS_VCF_Tree_Cover_1112&lt;/h4&gt;
This data set contains proportional estimates for the vegetative cover types of tree cover, herbaceous vegetation, and bare ground over South America for the period 2000-2001. These products were derived from all seven bands of the Moderate-resolution Imaging Spectroradiometer (MODIS) sensor onboard NASA&amp;#39;s Terra satellite. A set of 500-m MOD09A1 Surface Reflectance 8-day minimum blue reflectance composites were used as input data. To reduce the presence of cloud shadows, The data were converted to 40-day composites using a second darkest albedo (sum of blue, green, and red bands), and the Vegetation Continuous Fields (VCF) algorithmn was utilized (Hansen et al., 2002). The VCF shows how much of a land cover such as forest or grassland exists anywhere on the land surface. The VCF product may depict areas of heterogeneous land cover better than traditional discrete classification schemes which shows where land cover types are concentrated. There are three images provided in GeoTIFF format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc23_modis_aster_fire_comparisons_839&quot;&gt;LC23_MODIS_ASTER_Fire_Comparisons_839&lt;/h4&gt;
This data set contains data associated with MODIS fire maps generated using two different algorithms and compared against fire maps produced by ASTER. These data relate to a paper (Morisette et al., 2005) that describes the use of high spatial resolution ASTER data to evaluate the characteristics of two fire detection algorithms, both applied to MODIS-Terra data and both operationally producing publicly available fire locations. The two algorithms are NASA&amp;#39;s operational Earth Observing System MODIS fire detection product and Brazil&amp;#39;s National Institute for Space Research (INPE) algorithm. These data are the ASCII files used in the logistic regression and error matrices presented in the paper.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc23_vegetation_fire_dynamics_843&quot;&gt;LC23_Vegetation_Fire_Dynamics_843&lt;/h4&gt;
Satellite fire detection was determined from two sensorsâ€”the Advanced Very High Resolution Radiometer (AVHRR) on NOAA-12 and the Moderate Resolution Imaging Spectroradiometer (MODIS) on both the Terra and Aqua platforms, for 2001- 2003 to characterize fire activity in Brazil, giving special emphasis to the Amazon region. Active fire data for AVHRR/NOAA-12 was produced using a fixed threshold fire detection technique based on the algorithm developed by the Centro de Previsao do Tempo e Estudos Climaticos (CPTEC/INPE) (Setzer and Pereira, 1991; Setzer et al., 1994; Setzer and Malingreau, 1996). Active fire data for MODIS/Terra and MODIS/Aqua was produced using a contextual fire detection technique based on NASA-University of Maryland algorithm (Justice et al., 2003; Giglio et al.2003).Resulting fire counts were compared for major biomes of Brazil (Figure 1), the nine states of the Legal Amazon (e.g., Tocantins, Figure 2), and two important road corridors in the Amazon region (Figure 3). In evaluating the daily fire counts, there is a dependence on variations in satellite viewing geometry, overpass time, atmospheric conditions, and fire characteristics (Schroeder et al., 2005). The data provided are the coordinates of daily active vegetation fires in Brazil for 2001 through 2003 at 1km resolution for both AVHRR and MODIS sensors. Data are provided in both Arcview (shape file format) and ASCII comma separated file formats. Vector files for the major biomes of Brazil, the nine states of the Legal Amazon, and two important road corridors in the Amazon region are also included.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc23_vegetation_fires_2003_887&quot;&gt;LC23_Vegetation_Fires_2003_887&lt;/h4&gt;
The ASTER high resolution satellite data are available for visible-near infrared (15m resolution), short wave infrared (30m), and thermal infrared (90m) bands. Two sets of imagery were collected over Roraima state - Brazil covering a strip of approximately 180 X 60 km each on January 19 and 28, 2003. Each date has one prescribed burn and many other opportunistic fires. Data format is ASTER L1B HDF. There is a corresponding .met file (metadata file) for each hdf file. These files can be opened using any standard hdf viewer, ENVI can recognize the bands and georegistration automatically. The companion document, ASTER_GeoRef_FINAL.pdf, gives a good description of how to georeference ASTER L1B data and to open the files in ERDAS Imagine and also older ENVI versions.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc24_basin_scale_hot_pixels_2001_882&quot;&gt;LC24_Basin_Scale_Hot_Pixels_2001_882&lt;/h4&gt;
This data set provides the number of hot spots detected across the legal Amazon Basin at 5- km resolution by the AVHRR (Advanced Very High Resolution Radiometer) on NOAA 12, 14, 15, 16, 17, and 18 satellites for the entirety of 2001 (January 1 - December 31). Only hot spots detected at night are included. This data is useful for modeling fire events and evaluating human impacts on the Amazon Basin using fire as an indicator of anthropogenic disturbance (Arima et al., 2007).
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc24_cadastral_property_map_para_1042&quot;&gt;LC24_Cadastral_Property_Map_Para_1042&lt;/h4&gt;
This data set contains a shapefile of a digitized map of the land parcel information of the original properties of the Uruara colonization site, Para, Brazil, acquired from the Instituto de Colonizacao e Reforma Agraria, or the Colonization and Agrarian Reform Institute (INCRA). The Uruara settlement geometry was initially designed by INCRA, and consists of mostly 100 hectare lots (400 x 2500 meters, and 500 x 2000 meters), running north and south of the Trans-Amazon Highway, as a fine network of small, narrow rectangles. The other parcels in the landscape are the so-called glebas that range up to 3,000 hectares. The map was in the form of a paper map without a projection (a spherical geographic coordinate system) in the South American 1969 datum (SAD 1969). This paper map was digitized in Environmental Science Research Institute (ESRI) ArcInfo 8.1 using a digitizing table, and the digital cadastral data were geo-referenced and projected to match the Universal Transverse Mercator projection (Zone 22 South, World Geodetic System 1984 datum) of Landsat imagery (Landsat.org). There is one compressed (.zip) file with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc24_modis_forest_cover_500-m_1056&quot;&gt;LC24_MODIS_Forest_Cover_500-m_1056&lt;/h4&gt;
This data set, LBA-ECO LC-24 Forest Cover Map from MODIS, 500-m, South America: 2001, contains forest cover information for 2001 for all of South America. The data were collected by the MODerate Resolution Imaging Spectroradiometer (MODIS) sensor onboard the Earth Observing System, TERRA (AM-1) satellite platform and released by the MODIS science team as an image showing percent canopy cover. This information was then reclassified so that all pixels with a percent canopy cover greater than 40% (40% after the 1973 UNESCO standard) were classified as forest (a value of 1), and all other pixels were classified as non-forest (a value of 2). Water features were given a value of 3. This data has a pixel resolution of 500 meters and is unprojected with the WGS-1984 datum (Hansen et al. 2006). There is one GeoTIFF data file for this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc24_historical_roads_amazon_1043&quot;&gt;LC24_Historical_Roads_Amazon_1043&lt;/h4&gt;
Understanding the impact of road investments on deforestation is part of a complete evaluation of the expansion of infrastructure for development.We find evidence of spatial spillovers from roads in the Brazilian Amazon: deforestation rises in the census tracts that lack roads but are in the same county as and within 100 km of a tract with a new paved or unpaved road. At greater distances from the new roads the evidence is mixed, including negative coefficients of inconsistent significance between 100 and 300km, and if anything, higher neighbor deforestation at distances over 300 km.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc24_land_cover_uruara_para_1053&quot;&gt;LC24_Land_Cover_Uruara_Para_1053&lt;/h4&gt;
This data set provides course land cover classifications derived from Landsat TM images for 1986, 1988, and 1991 for the area surrounding the municipality of Uruara, Para, Brazil. Five land cover classes (Water, Clouds/Shadow, Forest, Not Forest, and Background) were derived (Aldrich et al. 2006). The Land Cover is in a compressed (.zip) GeoTIFF file for each year.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc24_etm_deforestation_map_para_1999_1054&quot;&gt;LC24_ETM_Deforestation_Map_Para_1999_1054&lt;/h4&gt;
This data set contains a 1999 Landsat ETM+ mosaic image land of cover classification showing forested and deforestation areas in Uruara, Para, Brazil. This image may be overlain with the cadastral property map of the same area (see related data set LBA-ECO LC-24 Cadastral Property Map of Uruara, Para, Brazil: ca.1975). This data sets contains a single geotiff image distributed as deforested_large.zip.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc24_land_cover_southern_para_1055&quot;&gt;LC24_Land_Cover_Southern_Para_1055&lt;/h4&gt;
This data set is a five-class land cover for Southern Para for the years 1984 (Landsat MSS), 1988 (Landsat TM), 1996, and 2003 (Landsat ETM+). The final classification shows five classes derived using visual comparison (Water, Clouds/Shadow, Forest, Not Forest, Background). These data were used in 2007 to illustrate the nature of deforestation in Southern Para, Brazil over the past twenty years (Simmons et al. 2007). There are four annual GeoTIFF files distributed with this data set. Each GeoTIFF file and accompanying .tfw file have been compressed into a single .zip file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc31_amz_historical_lu_1170&quot;&gt;LC31_AMZ_Historical_LU_1170&lt;/h4&gt;
This data set provides annual spatial patterns of cropland, natural pasture, and planted pasture land uses across Amazonia for the period 1940/1950-1995. Two series of 5-minute grid cell historical maps were generated starting from land use classification products for 1995. Annual data are the fraction of natural pasture, planted pasture, and cropland in each 5-min grid cell. The annual maps are provided in two NetCDF (.nc) format file at 5-minute resolution. The AMZ-C.nc file covers the Brazilian portion of Amazon and Tocantins Rivers basins, and is based on the 1995 land use classification of Cardille et al. (2002), generated through the fusion of remote sensing (AVHRR) and agricultural census data. The second file, AMZ-R.nc, covers the entire Legal Amazon region and adjacent areas and is based on the 1995 land use classification by Ramankutty et al. (2008). The land use classification was generated by the fusion of satellite imagery (MODIS and VEGETATION-SPOT) and data from the agricultural census. A historical land-use reconstruction algorithm was used to generate the annual spatial patterns (based on work from Ramunkutty and Foley, 1999).
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc31_site_1173&quot;&gt;LC31_SITE_1173&lt;/h4&gt;
This model product provides the Fortran source code and input data for the Simple Tropical Ecosystem Model (SITE). SITE is a simplified point model of vegetation dynamics that uses an integration interval of one hour to estimate the fluxes of CO2, water, and energy. Model forcing data are hourly meteorological parameters. SITE is a simplified model of vegetation dynamics for tropical ecosystems developed by Santos and Costa (2004). Model input data measurements of temperature, wind velocity, precipitation, latent heat, sensible heat, downward incident solar flux, and downward incident infrared flux were collected at the km 67 Tapajos National Forest site, Para, Brazil, from 2002 to 2003. SITE is structured with a canopy layer and two soil layers, and incorporates the following processes: *infrared radiation balance in the canopy and balance of solar radiation *aerodynamic processes *plant physiology *transpiration *balance of water intercepted by the canopy *transport of mass and energy fluxes *soil heat flux and soil moisture *carbon balance There are five files provided with this data set: the Fortran source code (version 1.1-0d), one file for the main program that declares variables and input parameters, one file that initializes vegetation parameters, one file used to compile the SITE model, and the km 67 input data file in comma-delimited (.csv) format. The four SITE files are provided in the compressed file SITE_Model.zip. One companion file is also provided that describes the collection and processing of the meteorological and flux measurements at the km 67 Tapajos National Forest site and the use of the data to calibrate SITE.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc35_goes_wf_abba_1180&quot;&gt;LC35_GOES_WF_ABBA_1180&lt;/h4&gt;
This data set is an active fire detection product resulting from the application of The Wildfire Automated Biomass Burning Algorithm (WF_ABBA) to Geostationary Environmental Operational Satellite (GOES) imager data for all of South America from 2000 through 2005. GOES imager data are available at 30 minute intervals with a nominal 4 x 4-km resolution. The data provided are the latitude/longitude, brightness temperature, estimates of sub-pixel fire size and temperature, Global Land Cover Characterization (GLCC) ecosystem type, and a pixel-fire flag (0-5, information regarding the probability of a fire or processing characteristics) for each active fire detected by WF_ABBA for a 30 minute imager interval. Spatial area coverage data files are provided as a complement to individual fire detection data files because the area of the latter varied according to the GOES imager scan mode in use. Versions 5.9 and 6.0 WF_ABBA data are provided. Differences between the two versions are assumed to be small though (typically less than 10%). An in-line temporal filter has been added to the algorithm to screen out false alarms associated with noise in the imagery and cloud edge issues in version 6.0. This is especially important for screening false alarms due to reflection off clouds at extreme view angles and at sunrise and sunset. There are nine compressed (.zip) files with this data set which expand to the filtered ASCII text data files (.filt), and seven coverage files text (.txt).
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc35_landsat7_fire_masks_1071&quot;&gt;LC35_Landsat7_Fire_Masks_1071&lt;/h4&gt;
This data set provides active fire detection images and associated summary information derived from Landsat 7 Enhanced Thematic Mapper Plus (ETM+) images for various locations in Brazilian Amazonia during 2001-2003. There are two image types: (1) GeoTiff images (masks) of active fire pixels, and (2) GeoTiff images (masks) of clustered active fire pixels where a distinct cluster identification number has been assigned to each individual group of contiguous active fire pixels. There are 122 GeoTiff format files of each type of fire mask; a total of 244 images. The spatial resolution of the fire mask images is 30 meters. ETM+ images were selected based on data quality, availability, as well as on the occurrence of vegetation fires. In addition to the two image types, there are also two types of fire pixel summary information provided in text files: (1) one file of active fire pixel summary information derived from the active fire pixel images, and (2) 122 files of clustered active fire pixel information derived from individual clustered fire pixel masks, each of which correspond to a clustered image.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc39_decaf_model_1190&quot;&gt;LC39_DECAF_Model_1190&lt;/h4&gt;
This data set contains modeled estimates of carbon flux, biomass, and annual burning emissions across the Brazilian state of Mato Grosso from 2000-2006. The model, DEforestation CArbon Flux (DECAF), was used to provide annual carbon fluxes from large deforestation events (&amp;gt;25 ha) based on post-deforestation land use, and the frequency and duration of active fires during the deforestation process. Carbon fluxes associated with the conversion of Cerrado to mechanized crop production, fires in Cerrado, and managed pasture cover types were also estimated. Model data outputs provided include: * Estimated aboveground live biomass from DECAF in 2000 and 2004. * Annual biomass burning emissions estimates for 2001-2005 from low, middle, and high emissions scenarios with DECAF. There are 15 GeoTIFF files for annual emissions which represent the carbon emissions per pixel in grams of carbon per m2 (g C m-2). Model data inputs provided include: * Annual burn trajectories for 2001 - 2005, including deforestation, Cerrado land cover conversion, and fires in pasture and Cerrado ecosystems unrelated to agricultural expansion. These data were assembled from three sources: MODIS 500-m burned area maps, annual deforestation based on data from the INPE PRODES program, and the conversion of Cerrado savannah/woodland to cropland estimated from land cover information from MODIS phenology metrics. * Annual land cover data 2001-2004 for the portion of Mato Grosso covered by MODIS phenology metrics, tile h12v10, updated based on annual land cover changes in Amazon forest and Cerrado cover types. * Monthly Normalized Difference Vegetation Index (NDVI) for MODIS tile h12v10 from 10/2000 - 09/2006, based on cloud and gap-filled 16-day NDVI data from MODIS Collection 4 16-day NDVI composites MOD13 product (Huete et al., 2002). There are six compressed (.gz) files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;lc39_modis_fire_sa_1186&quot;&gt;LC39_MODIS_Fire_SA_1186&lt;/h4&gt;
This data set provides active fire locations and estimates of annual fire frequencies for South America from 2000-2007. Data from the Moderate Resolution Imaging Spectroradiometer (MODIS) sensors aboard the Terra (2000-??2007) and Aqua (2003-2007) satellite platforms were analyzed to determine spatial and temporal patterns in satellite fire detections. The analysis considered a high-confidence subset of all MODIS fire detections to reduce the influence of false fire detections over small forest clearings in Amazonia (Schroeder et al., 2008). The number of unique days on which the active fire detections were recorded within a 1 km radius was estimated from the subset of active fire detections and the ArcGIS neighborhood variety algorithm. There are 14 data files with this data set: 7 GeoTIFF (.tif) files of fire frequency at MODIS 250 m resolution, where each grid cell value represents the number of days in that year on which active fires were detected, and 7 shape files of active fire locations for the years 2001-2007.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd01_pasture_nutrients_1135&quot;&gt;ND01_Pasture_Nutrients_1135&lt;/h4&gt;
This data set provides soil physical and chemical properties, and grass nutrient measurements of samples collected from 17 pasture sites located within the state of Rondonia in the southwestern Brazilian Amazon. Soil data includes bulk density, class, texture, and measurements of carbon (C), phosphorus (P), calcium (Ca), magnesium (mg), and potassium (K) concentrations. Foliar data includes nitrogen (N), P, Ca, Mg, and K concentrations. The 17 pasture sites were cattle ranches selected within the region between Porto Velho and Presidente Medici of Rondonia. Four of the ranches with Ultisols support dairy cattle, and the rest have beef cattle pastures dispersed across three soil orders: Oxisols, Ultisols, and Alfisols. Nearby primary forest sites were also sampled to provide data on the original soil properties for each soil order. Soil samples were collected in May 2003, July through August 2003, and May 2004, which covered the late rainy season (May) and the dry season (July through August). Grass species sampled included Brachiaria brizantha, Brachiaria decumbens, B. brizantha, and Pennestum clandestinum, and represented three phenologically distinct grass materials: wet-season live grass, collected in May 2004, dry-season live grass and dry-season senesced grass, both collected between the end of July and the beginning of August 2003. There are 4 comma-delimited data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd01_spectral_mixture_models_1188&quot;&gt;ND01_Spectral_Mixture_Models_1188&lt;/h4&gt;
This data set provides fractional land cover type images for shade, green vegetation (GV), non-photosynthetic vegetation (NPV), and soil for the regions of JiParana, PortoVelho, Luiza, Ariquemes, and Cacoal in the state of Rondonia, Brazil, for the period 1984 to 2000. The images were derived with a spectral mixture analysis (SMA) of Landsat Thematic Mapper (TM) time series scenes for each of these areas. There were 249 TM scenes and one Landsat Multispectral Scanner (MSS) scene acquired for these analyses. The images are 30-m Landsat resolution and were georectified to the Brazilian space agency 1998 and 1999 PRODES imagery. There are 250 GeoTIIF image files (.tif) in this data set. Files are grouped by region and year/month/day scene was taken.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd01_registered_tm_mss_1197&quot;&gt;ND01_Registered_TM_MSS_1197&lt;/h4&gt;
This data set provides a time series of Landsat Multispectral Scanner (MSS), Thematic Mapper (TM), and Enhanced Thematic Mapper Plus (ETM+) scenes for five (Path/Row) areas in Rondonia, Brazil. The scenes are from the period June 1975 through June 2000, but all areas do not have scenes for all the years. The areas and Landsat Path/Rows included are as follows: Ariquemes (P232,R67), Ji-Parana (P231, R67), Luiza (P231, R68), Cacoal (P230, R68), and Porto Velho (P232, R66). TM images are available for all five areas. Because of a paucity of digital Landsat MSS imagery from the 1970s, only two scenes could be included, a 1975 scene from Ariquemes and a 1978 scene from Ji-Parana. Each of the Landsat scenes has been coregistered to a Path/Row-specific georectified PRODES Landsat file obtained from the Brazilian Government&amp;#39;s National Institute for Space Research (INPE) program. For each scene, the coregistration is accurate to within (plus or minus)1 pixel (30-m Landsat resolution) in most places. The five INPE PRODES Landsat scenes used in the georectification process are included with this data set. There are five compressed files (tar.gz format) with this data set. When expanded, each compressed file (which corresponds to one of the five areas) contains a directory for each scene with GeoTIFF files for individual Landsat bands, a text file of tie points, and another text file of slope and intercept values for converting radiance to reflectance. There are two dates for Landsat MSS scenes, 45 dates for TM scenes, and six dates for ETM+ scenes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd01_land_cover_maps_1259&quot;&gt;ND01_Land_Cover_Maps_1259&lt;/h4&gt;
This data set provides a time series of land cover classifications for Ariquemes, Ji-Parana, and Luiza, research sites in Rondonia, Brazil. The land cover classifications are derived from the Landsat Multispectral Scanner (MSS), Thematic Mapper (TM), and Enhanced Thematic Mapper Plus (ETM+) sensors. The time period ranges from June 1975 through June 2000, but all areas do not have images for all the years. The images were classified into the following categories: 1. Primary upland forest, representing the dominant natural vegetation in the area; 2. Pasture and green pasture; 3. Second growth, dominated by small trees and shrubs with low species diversity and biomass relative to primary forest; 4. Soil/urban; 5. Rock/savanna; 6. Water; and 7. Cloud and smoke obscured. In addition, areas covered by rock and savanna were mapped and all areas outside of the overlap zone between all dates within a scene, and scene edges, were masked. There are 75 GeoTIFF files (.tif) with this data set which includes: classified images (*ful.tif) and a corresponding image mask (*ful_mask .tif) for each date (with the exception of 1978 and 1996 images for Ji-Parana, for which there are only ful_mask.tif files), and three mask files for rock, savannah, and scene edges, for each area. By area, there are 31 images for Ariquemes, 23 images for Ji-Parana, and 21 images for Luiza.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd01_georectified_products_1165&quot;&gt;ND01_Georectified_Products_1165&lt;/h4&gt;
This data set provides a 27-year land cover time series of 28.5-m resolution products derived from Landsat images for 80% of Rondonia, Brazil, for the period 1984 to 2010. Selected Landsat Thematic Mapper (TM) and Landsat Multispectral Scanner (MSS) images from the years 1984 through 2010, for seven path/row scenes (PortoVelho, Ariquemes, Jiparana, Luiza (or Urupa), Cacoal, Chapuingaia, and Vilhena) were mosaicked for each year. Each mosaicked image was georectified and classified into seven land-cover classes--savanna/rock, pasture, secondary forest, primary forest, cloud, urban, or water. This 27-year time series allows the long-term assessment of land-cover variation across the state. There are 27 GeoTIFF image files (.tif) and one accompanying .xml file for each GeoTIFF file, compressed and available as .zip files, one file for each year for the period 1984-2010, with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd01_age_maps_1184&quot;&gt;ND01_Age_Maps_1184&lt;/h4&gt;
This data set provides classified land cover transition images (maps) derived from Landsat Thematic Mapper (TM) and Multispectral Scanner (MSS) imagery for Ariquemes, Luiza, and Ji-Parana¡ areas in Rondonia, Brazil, at 30-m resolution. Images depict the age relative to the year 2000, of cleared land from the date the land was cut, to the date when primary forests transitioned into nonforest class (for example, 25 &#x3D; cut by 1975, or 25 years before the year 2000). Temporal changes in three regions are represented by 31 TM scenes acquired between 1984 and 1999, and a pair of MSS scenes from 1975 and 1978. Data are provided as three GeoTiff (.tif) images, one for each of the three areas.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd01_pasture_spectra_1154&quot;&gt;ND01_Pasture_Spectra_1154&lt;/h4&gt;
This data set provides the results of spectral reflectance (350 to 2,500 nm at 1-nm increments) and biophysical measurements on grass pastures in eight cattle ranches in the state of Rondonia, located in the southwestern Brazilian Amazon. The ranches are located near the cities of Porto Velho, Ariquemes, Ouro Preto, Ji-Parana, and Presidente Medici. Field measurements were collected in July and August 2003. The primary grass species sampled were Brachiaria brizantha and Brachiaria decumbens. Spectrometer measurements were taken at 5-m intervals along 100 m transects on the pastures - fourteen total transects. Vegetation was sampled at 20-m intervals along the transects. All standing biomass and litter on the soil surface were collected and separated into live and senesced biomass and then dried to calculate water content. Sixty-eight reflectance spectra coincided with grass biophysical samples. Note that the research was done on private lands in Rondonia, and to protect the privacy of those land owners no geographic information is associated with the reported measurements. Three data files are included: an ENVI spectral library file with reflectance data for 484 pasture sampling points, an ASCII comma-separated file with reflectance data for the 484 pasture sampling points, and an ASCII comma-separated file with the biophysical measurements.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd01_stream_chemistry_1119&quot;&gt;ND01_Stream_Chemistry_1119&lt;/h4&gt;
This data set provides the results of (1) synoptic streamwater sampling and analyses from numerous sites across Rondonia and (2) corresponding watershed characteristics derived from remote sensing and historical/available data sources. Sixty streams, in both forested and non-forested sites, were sampled once during the dry season in August of 1998 and 49 of the same streams were sampled again during the wet season in January-February of 1999. Analyses included sodium (Na), calcium (Ca), magnesium (Mg), potassium (K), silica (Si), chloride (Cl), sulfate, pH, and acid neutralizing capacity. Watershed characteristics, including soil cation content, pH, watershed lithology, area, percent deforested, and urban watershed population density, were derived and calculated from digitized soil maps and available soil profile analyses, digitized topographic maps, land use mosaics from Landsat Thematic Mapper (TM) images, and Brazilian census data. The objective of the study was to determine the relative influence of watershed soil exchangeable cation content, rock type, deforestation, and urban population density on stream concentrations of base cations, dissolved silicon, chloride and sulfate in both the dry and wet seasons in a humid tropical region undergoing regional land use transformation. There are three comma-delimited data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd01_watershed_defor_1159&quot;&gt;ND01_Watershed_Defor_1159&lt;/h4&gt;
This data set provides estimates of watershed deforestation, as a proportion of the total area of watersheds, in Rondonia, Brazil for 1999. Deforestation maps were determined for the main agricultural and surrounding forested areas of Rondonia using multiple Landsat TM scenes (Biggs et al. 2008). Cumulative deforestation estimates were derived from this time series of Landsat scenes from 1975 to 1999. To obtain watershed-level estimates of deforestation, watershed boundaries and stream networks were delineated by a flow accumulation algorithm using a 90-m resolution digital elevation model (DEM) from NASA&amp;#39;s Shuttle Radar Topography Mission (SRTM). The results were watersheds of seven Strahler stream orders (1-7) with stream networks that closely matched those of the 1:100,000 topographic maps for the area. The watershed boundaries, classified by stream order, were overlain on the time series of deforestation maps to determine the cumulative deforestation extent in 1999. This data set contains six ESRI ArcGIS shapefiles of the watershed boundaries for streams orders 2-7, the smallest watershed (second order) to the largest inclusive watershed (seventh order). The cumulative deforestation estimates, as a proportion of total area for each watershed, are available as a comma-delimited text file that can be related to the individual watershed boundary shapefiles. Cumulative deforestation data are available for first order streams, although not as a shapefile. There are six zipped ESRI ArcGIS shapefiles (.zip) and one ASCII comma separated file with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd02_mulching_experiment_950&quot;&gt;ND02_Mulching_Experiment_950&lt;/h4&gt;
Fires set for slash-and-burn agriculture contribute to the current unsustainable accumulation of atmospheric greenhouse gases, and they also deplete the soil of essential nutrients, which compromises agricultural sustainability at local scales. Integrated assessments of greenhouse gas emissions have compared intensive cropping systems in industrialized countries, but such assessments have not been applied to common cropping systems of smallholder farmers in developing countries. We report an integrated assessment of greenhouse gas emissions in slash-and-burn agriculture and an alternative chop-and-mulch system in the Amazon Basin. The soil consumed atmospheric methane under slash-and-burn treatment and became a net emitter of methane to the atmosphere under the mulch treatment. Mulching also caused about a 50% increase in soil emissions of nitric oxide and nitrous oxide and required greater use of fertilizer and fuel for farm machinery. Despite these significantly higher emissions of greenhouse gases during the cropping phase under the alternative chop-and-mulch system, calculated pyrogenic emissions in the slash-and-burn system were much larger, especially for methane. The global warming potential CO2-equivalent emissions calculated for the entire crop cycles were at least five times lower in chop-and-mulch compared to slash-and-burn. The crop yields were similar for the two systems. While economic and logistical considerations remain to be worked out for alternatives to slash-and-burn, these results demonstrate a potential win-win strategy for maintaining soil fertility and reducing net greenhouse gas emissions, thus simultaneously contributing to sustainability at both spatial scales.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd02_soil_co2_extracts_1074&quot;&gt;ND02_Soil_CO2_Extracts_1074&lt;/h4&gt;
This data set provides a time series of calcium, magnesium, and potassium concentrations extracted from soil samples from a laboratory column extraction study conducted in 2002. Soils used in the columns were originally collected in 1998 in Fazenda Vitoria, a cattle ranch 6 km north of the town of Paragominas, Para, Brazil. The soils were from contrasting land uses of primary forest (mata), secondary forest (capoeira), or pasture (pasto). Water equilibrated with increasing concentrations of CO2 was used to extract cations from the soil columns. Data represent the time series of cation concentrations in the extract solutions as well as the total content of cations removed from the soils. There is one comma-delimited ASCII file with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd02_soil_co2_flux_1066&quot;&gt;ND02_Soil_CO2_Flux_1066&lt;/h4&gt;
This data set reports soil CO2 flux and results of This data set reports soil CO2 flux and results of physical and chemical characterization of soils from pastures, secondary forests, and mature forests near Rio Branco, Acre, Brazil. CO2 flux measurements were made in the field on a monthly basis at 16 sites from June of 1999 to January 2001. In addition, litter was collected monthly from 2001-2002 at each of the mature forest sites and at 4 of the secondary forest sites, and mean litter mass is reported. Soil samples were collected and analyzed from several land cover types at two sites during this same time period. There are four comma-delimited ASCII data files with this data set. and chemical characterization of soils from pastures, secondary forests, and mature forests near Rio Branco, Acre, Brazil. CO2 flux measurements were made in the field on a monthly basis at 16 sites from June of 1999 to January 2001. In addition, litter was collected monthly from 2001-2002 at each of the mature forest sites and at 4 of the secondary forest sites, and mean litter mass is reported. Soil samples were collected and analyzed from several land cover types at two sites during this same time period. There are four comma-delimited ASCII data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd02_landsat_tm_mss_para_1156&quot;&gt;ND02_Landsat_TM_MSS_Para_1156&lt;/h4&gt;
This data set provides Landsat images of the county of Sao Francisco do Para located in the Bragantina region of Para, Brazil, the oldest agriculture frontier in Amazonia. These images are subsets for the municipio (county) and immediate region. There are seven GeoTIFF files (.tif) with this data set which includes two for July 24, 1984 multispectral scanner (MSS), one for June 21, 1994 thematic mapper Landsat 5 (TM5), three for July 13, 1999 thematic mapper Landsat 7 (TM7), and one TM for June 21, 1994.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd02_soil_hydraulic_conductivity_1075&quot;&gt;ND02_Soil_Hydraulic_Conductivity_1075&lt;/h4&gt;
This data set reports field estimated saturated hydraulic conductivity measurements from June 12 through June 20, 2001. This study was part of a rainfall exclusion experiment that was conducted from 1999-2001 at the km 67 Seca Floresta site, Tapajos National Forest, Para, Brazil. The objective of this component of the study was to develop an understanding of the physical processes driving the observed soil water dynamics at the site. There is one comma-delimited ASCII data file with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd02_non_woody_biomass_1115&quot;&gt;ND02_Non_Woody_Biomass_1115&lt;/h4&gt;
This data set reports biomass from small stems and non-woody vegetation measured from 1999 to 2005 in plots of a secondary-growth forest fertilization experiment. The study location was Fazenda Vitoria, 6.5-km northwest of the town of Paragominas, Para, Brazil, in a 6-year old secondary-growth forest. Vegetation life-forms with diameters less than or equal to 2 cm (grasses, herbs, vines and dead material) were destructively sampled in November 1999, June 2000, June 2001, July 2003, July 2004, and July 2005. All data are provided in a single comma-separated file. The site was divided into three blocks with four treatment plots (each 20m x 20m) located in each block (3 reps x 4 treatments &#x3D; 12 plots). Three of the twelve plots were fertilized with nitrogen (100 kg N/ha as urea), three were fertilized with phosphorus (50 kg P/ha as superphosphate), three were fertilized with both nitrogen and phosphorus. The remaining three plots were not fertilized and served as the experimental control.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd02_tree_heights_dbh_951&quot;&gt;ND02_Tree_Heights_DBH_951&lt;/h4&gt;
Understanding secondary successional processes in Amazonian terrestrial ecosystems is becoming increasingly important as continued deforestation expands the area that has become secondary forest, or at least has been through a recent phase of secondary forest growth. Most Amazonian soils are highly weathered and relatively nutrient poor, but the role of nutrients as a factor determining successional processes is unclear. Soils testing and chronosequence studies have yielded equivocal results regarding the possible role of nutrient limitation. The objective of this paper is to report the first two years&amp;#39; results of a nitrogen (N) and phosphorus (P) fertilization experiment in a 6-yr-old secondary forest growing on an abandoned cattle pasture on a clayey Oxisol. Growth of remnant grasses responded significantly to the N + P treatment, whereas tree biomass increased significantly following N-only and N + P treatments. The plants took up about 10% of the 50 kg P/ha of the first year&amp;#39;s application, and recovery in soil fractions could account for the rest. The trees took up about 20% of the 100 kg N/ha of the first year&amp;#39;s application. No changes in soil inorganic N, soil microbial biomass N, or litter decomposition rates have been observed so far, but soil faunal abundances increased in fertilized plots relative to the control in the second year of the study. A pulse of nitric oxide and nitrous oxide emissions was measured in the N-treated plots only shortly after the second year&amp;#39;s application. Net N mineralization and net nitrification assays demonstrated strong immobilization potential, indicating that much of the N was probably retained in the large soil organic-N pool. Although P availability is low in these soils and may partially limit biomass growth, the most striking result of this study so far is the significant response of tree growth to N fertilization. Repeated fire and other losses of N from degraded pastures may render tree growth N limited in some young Amazonian forests. Changes in species composition and monitoring of long-term effects on biomass accumulation will be addressed as this experiment is continued.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd02_soil_gases_ree_1117&quot;&gt;ND02_Soil_Gases_REE_1117&lt;/h4&gt;
This data set reports soil carbon dioxide (CO2) and nitrous oxide (N2O) concentrations and soil volumetric water content (VWC) from a rainfall exclusion experiment that was conducted at the km 67 Seca Floresta site, Tapajos National Forest, Brazil. Samples were collected every two to three months. The purpose was to observe the potential effects of severe water stress on a humid Amazonian forest (Nepstad 2002). Data provided are from December 9, 1999, and April 2, 2000-June 14, 2002. There is one comma-delimited data file with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd02_ree_trace_gas_tapajos_955&quot;&gt;ND02_REE_Trace_Gas_Tapajos_955&lt;/h4&gt;
Moist tropical forests in Amazonia and elsewhere are subjected to increasingly severe drought episodes through the El Nino-Southern Oscillation (ENSO) and possibly through deforestation-driven reductions in rainfall. The effects of this trend on tropical forest canopy dynamics, emissions of greenhouse gases, and other ecological functions are potentially large but poorly understood. We established a throughfall exclusion experiment in an east-central Amazon forest (Tapajos National Forest, Brazil) to help understand these effects. After 1-year intercalibration period of two 1-ha forest plots, we installed plastic panels and wooden gutters in the understory of one of the plots, thereby excluding similar to 890 mm of throughfall during the exclusion period of 2000 (late January to early August) and similar to680 mm thus far in the exclusion period of 2001 (early January to late May). Average daily throughfall reaching the soil during the exclusion period in 2000 was 4.9 and 8.3 mm in the treatment and control plots and was 4.8 and 8.1 mm in 2001, respectively. During the first exclusion period, surface soil water content (0-2 m) declined by similar to100 mm, while deep soil water (2-11 m) was unaffected. During the second exclusion period, which began shortly after the dry season when soil water content was low, surface and deep soil water content declined by similar to140 and 160 mm, respectively. Although this depletion of soil water provoked no detectable increase in leaf drought stress (i.e., no reduction in predawn leaf water potential), photosynthetic capacity declined for some species, the canopy thinned (greater canopy openness and lower leaf area index) during the second exclusion period, stem radial growth of trees &amp;lt;15 m tall declined, and fine litterfall declined in the treatment plot, as did tree fruiting. Aboveground net primary productivity (NPP) (stemwood increment and fine litter production) declined by one fourth, from 15.1 to 11.4 Mg ha(-1) yr(-1), in the treatment plot and decreased slightly, from 11.9 to 11.5 Mg ha(-1) yr(-1), in the control plot. Stem respiration varied seasonally and was correlated with stem radial growth but showed no treatment response. The fastest response to the throughfall exclusion, and the surface soil moisture deficits that it provoked, was found in the soil itself. The treatment reduced N2O emissions and increased CH4 consumption relative to the control plot, presumably in response to the improved soil aeration that is associated with soil drying. Our hypothesis that NO emissions would increase following exclusion was not supported. The conductivity and alkalinity of water percolating through the litter layer and through the mineral soil to a depth of 200 cm was higher in the treatment plot, perhaps because of the lower volume of water that was moving through these soil layers in this plot. Decomposition of the litter showed no difference between plots. In sum, the small soil water reductions provoked during the first 2 years of partial throughfall exclusion were sufficient to lower aboveground NPP, including the stemwood increment that determines the amount of carbon stored in the forest. These results suggest that the net accumulation of carbon in mature Amazon forests indicated by recent permanent plot and eddy covariance studies may be very sensitive to small reductions in rainfall. The soil water reductions were also sufficient to increase soil emissions of N2O and to increase soil consumption of CH4-both radiatively important gases in the atmosphere.The possible reduction of tree reproductive activity points to potentially important effects of drought on the long-term species composition of Amazon forests.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd02_soil_gas_flux_apeu_953&quot;&gt;ND02_Soil_Gas_Flux_Apeu_953&lt;/h4&gt;
Changes in land-use and climate are likely to alter moisture and substrate availability in tropical forest soils, but quantitative assessment of the role of resource constraints as regulators of soil trace gas fluxes is rather limited. The primary objective of this study was to quantify the effects of moisture and substrate availability on soil trace gas fluxes in an Amazonian regrowth forest. We measured the efflux of carbon dioxide (CO2), nitric oxide (NO), nitrous oxide (N2O), and methane (CH4) from soil in response to two experimental manipulations. In the first, we increased soil moisture availability during the dry season by irrigation; in the second, we decreased substrate availability by continuous removal of aboveground litter. In the absence of irrigation, soil CO2 efflux decreased during the dry season while irrigation maintained soil CO2 efflux levels similar to the wet season. Large variations in soil CO2 efflux consistent with a significant moisture constraint on respiration were observed in response to soil wet-up and dry-down events. Annual soil C efflux for irrigated plots was 27 and 13% higher than for control plots in 2001 and 2002, respectively. Litter removal significantly reduced soil CO2 efflux; annual soil C efflux in 2002 was 28% lower for litter removal plots compared to control plots. The annual soil C efflux: litterfall C ratio for the control treatment (4.0-5.2) was consistent with previously reported values for regrowth forests that indicate a relatively large belowground C allocation. In general, fluxes of N2O and CH4 were higher during the wet season and both fluxes increased during dry-season irrigation. There was no seasonal effect on NO fluxes. Litter removal had no significant impact on N oxide or CH4 emissions. Net soil nitrification did not respond to dry-season irrigation, but was somewhat reduced by litter removal. Overall, these results demonstrate significant soil moisture and substrate constraints on soil trace gas emissions, particularly for CO2, and suggest that climate and land-use changes that alter moisture and substrate availability are therefore likely to have an impact on atmosphere chemistry.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd02_ree_soil_vwc_1061&quot;&gt;ND02_REE_Soil_VWC_1061&lt;/h4&gt;
This data set reports monthly measured soil volumetric water content (VWC) from a rainfall exclusion experiment that was conducted from 1999-2001 at the km 67 Seca Floresta site, Tapajos National Forest, Brazil. The purpose was to observe the potential effects of severe water stress on a humid Amazonian forest (Nepstad 2002). There are two ASCII comma delimited files with measured VWC, one for the control plot and one for the rainfall exclusion plot. These measured values were used by the authors to develop a model of daily changes in the distribution of water through the soil layers. The simulated daily VWC values are also provided in the file with the measured VWC. For comparison, results of VWC simulation for the control and treatment plots using a STELLA model which incorporates rainfall and plant water uptake are provided. There are two ASCII comma delimited files of simulated results. See Belk et. al., 2007 for details.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd02_water_chemistry_paragominas_1067&quot;&gt;ND02_Water_Chemistry_Paragominas_1067&lt;/h4&gt;
This data set includes measurements of dissolved nutrient and organic carbon concentrations, as well as dissolved oxygen, alkalinity, conductivity, turbidity, pH, and discharge from three streams located in mixed land use (crop fields, pastures, secondary vegetation, and forest) and two streams in entirely forested landscapes near Paragominas in the state of Para, Brazil. Stream water samples were collected during two different periods: 1) weekly from August 1999 to July 2001 at location Igarape 54, Station 5 and 2) monthly from April 2003 through October 2005 at all of the stations. The exact start date and suite of measurements vary by location. In addition, samples from precipitation collectors at the Paragominas Meteorological Station were measured for nutrient concentrations every two weeks from 1999 to 2001. There are two comma delimited ASCII data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd03_flowpath_chemistry_1076&quot;&gt;ND03_Flowpath_Chemistry_1076&lt;/h4&gt;
This data set consists of water chemistry data from streams, wells, rainwater, and canopy throughfall samples. The field measurements were carried out at Rancho Grande in the Brazilian state of Rondonia, in the southwestern Brazilian Amazon basin, at two adjacent watersheds, a forest (1.37 ha), and pasture (0.73 ha). Samples were collected during one entire rainy season starting in August 2004 and ending in April 2005. There is one comma-delimited data file with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd03_streams_soilwater_1113&quot;&gt;ND03_Streams_Soilwater_1113&lt;/h4&gt;
This data set provides the results of (1) the physical and chemical characterization of streams and (2) comparable chemical analyses of extracted soil water in the Aldeia River basin at Fazenda Nova Vida, a large cattle ranch 50 km from the city of Ariquemes, in central Rondonia, Brazil, from 1994-2001. Data are provided on the stream beds including cross-sectional depth and stream bed surface type. Stream discharge is reported. Streamwater was sampled and analyzed periodically over the eight year duration of the study at numerous steam locations. Soil solution samples were collected at the same frequency with lysimeters placed at 30 cm and 100 cm depths on the floodplain and at upland forest and pasture sites in the Aldeia River watershed. There are five comma-delimited data files in this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd04_soil_h2o_manaus_1246&quot;&gt;ND04_Soil_H2O_Manaus_1246&lt;/h4&gt;
This data set contains soil water measurements to a depth of 3 meters for the years 1999, 2000, and 2001, and total monthly precipitation data for 1999-2000. The data were collected from a pasture site located at the Embrapa Pasture Research Site, a former cattle research station 54 km north of Manaus on the highway BR 174 Manaus-Boa Vista, Brazil. There are three comma-separated data files (.csv) with this data set. DATA QUALITY STATEMENT: The Data Center has determined that there are questions about the quality of the data reported in this data set. The data set has missing or incomplete data, metadata, or other documentation that diminishes the usability of the products. KNOWN PROBLEMS: There is no associated research documentation and the units were not provided with the data.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd04_c_nutrient_stocks_1069&quot;&gt;ND04_C_Nutrient_Stocks_1069&lt;/h4&gt;
This data set reports the carbon and nutrient stocks of above-ground vegetation and soil pools at three locations where post-pasture secondary forest recovery ranged from 0 to 14 years since abandonment. These sites are located in the state of Amazonas, Brazil, along the road BR-174 north of the city of Manaus within three fazendas (cattle ranches) now in various stages of grazing, pasture abandonment, or pasture reclamation: Fazenda Rodao (km 46), Embrapa-District of SUFRAMA (DAS) pasture research site (km 53) and Fazenda Dimona (km 72). From September 2000 to July 2001, measurements were obtained for aboveground biomass (cite ND-04 Sec For Recovery), foliage and wood samples were collected and analyzed for total nutrient (C, N, P, K, Ca and Mg) concentrations, and soil samples from 0 to 45 cm depth were collected and analyzed for total nutrient (C, N, P, K, Ca and Mg) concentrations. Total carbon (C) and nutrient stocks were calculated for various vegetation and soil pools to gain an understanding of the dynamics of nutrient and C buildup in regenerating secondary forests in central Amazonia (Feldpausch et al., 2004). There are 2 comma-delimited ASCII data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd04_secondary_forest_recovery_1068&quot;&gt;ND04_Secondary_Forest_Recovery_1068&lt;/h4&gt;
This data set reports measurements of the canopy and structure of secondary forests regenerating from abandoned pastures. These secondary forests are located in the state of Amazonas, Brazil, along the road BR-174 north of the city of Manaus within three fazendas (cattle ranches) now in various stages of grazing, pasture abandonment, or pasture reclamation: Fazenda Rodao (km 46), Embrapa-District of SUFRAMA (DAS) pasture research site (km 53), and Fazenda Dimona (km 72). Ten secondary forest study sites were selected within the three fazendas where post-pasture forest recovery ranged from 0 to 14 years since abandonment. From 2000-2001 estimates of leaf area index (LAI) and canopy cover were derived from hemispherical canopy digital photographs, and estimates of aboveground biomass and basal area were derived utilizing allometric equations from diameter at breast height (DBH) measurements. Estimates were classified by growth-form and diameter class. See Feldpausch et al. (2005) for more information. There are four comma-delimited data files with this data set and one companion file with information regarding the allometric equations relating diameter at breast height (for dbh &amp;gt; 5 cm) to dry weight for biomass calculations.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd04_termite_mounds_1072&quot;&gt;ND04_Termite_Mounds_1072&lt;/h4&gt;
This data set reports the results of a comprehensive study of mound building termites at the Embrapa research station in the Distrito Agropecuario da SUFRAMA, located at km 53 of the federal highway BR 174 outside Manaus, Amazonas, Brazil. Study areas included a primary forest site, an adjacent 7-8 year old secondary forest site, and two abandoned pasture sites which were being used for agroforest purposes. Reported are (1) the termite species occurrence and areal abundance of mounds, (2) characterization of the mound soil microbiological community, root biomass, seedling emergence success, soil respiration, nitrogen mineralization, and (3) the characterization of the termite mound soil physical, chemical, and hydraulic properties. Analyses were also performed on samples from adjacent control soils for comparison. This data set contains 15 comma-delimited data files.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd06_landuse_studies_1130&quot;&gt;ND06_LandUse_Studies_1130&lt;/h4&gt;
This data set provides measurements of soil properties compiled from 39 studies on nutrient dynamics in natural forests and forest-derived land uses (pasture, shifting cultivation and tree plantations) conducted in Amazonia over the period of 1950-2001. The initial literature survey for the data consisted of more than 100 studies conducted during this period. The objectives of this project were to compare soil data from major land uses across Amazonia and identify gaps in present knowledge that offer direction for future research. Five widely cited hypotheses were tested concerning the effects of land-use change on soil properties by analyzing data compiled from 39 studies in multi-factorial ANOVA models: ?¢ effective cation exchange capacity (ECEC), and exchangeable calcium (Ca) concentrations rise and remain elevated following the slash-and-burn conversion of forest to pasture or crop fields ¢ soil contents of total carbon (C), nitrogen (N), and inorganic readily (i.e., Bray, Mehlich I or resin) extractable phosphorus (Pi) decline following forest-to-pasture conversion ?¢ soil concentrations of total C, N, and Pi increase in secondary forests with time since abandonment from agricultural activities ?¢ soil nutrient conditions under all tree-dominated land-use systems (natural or not) remain the same ?¢ higher efficiencies of nutrient utilization occur where soil nutrient pools are lower There is one comma-delimited ASCII file (.csv) with this data set and a list of the 39 studies used in this data set provided as a companion file in text format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd07_15n_leaves_soils_1121&quot;&gt;ND07_15N_Leaves_Soils_1121&lt;/h4&gt;
This data set provides (1) delta 15N ratios and nitrogen concentrations for foliar samples and (2) delta 13C and delta 15N ratios as well as carbon and nitrogen concentrations for soil samples collected from cerrado sites within the Ecological Reserve of the Brazilian Institute of Geography and Statistic (IBGE), Brasilia, Brazil. Foliar samples, collected from 320 individuals representing 45 woody tree and shrub species, and soil samples were collected from 5 cerrado locations (2 in campo sujo, 2 in cerrado denso and 1 in cerrado). Soil samples were collected to 450 cm depth in the campo sujo and 800 cm depth elsewhere. Samples were collected during the period December 1999 to September 2000. Eiten (1972) described campo sujo as an open savanna with scattered trees and shrubs, cerrado sensu stricto as a savanna woodland with abundant evergreen and deciduous trees and shrubs and an herbaceous understory, and cerrado denso as medium to tall woodlands with closed or semiclosed canopies (Bustamante et al., 2004). There are two comma-delimited data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd07_stream_chemistry_brasilia_1018&quot;&gt;ND07_Stream_Chemistry_Brasilia_1018&lt;/h4&gt;
This data set reports on dissolved nutrient concentrations, as well as dissolved oxygen, alkalinity, conductivity, turbidity, and pH measured in water samples collected from nine streams located in the state of Brasilia, Brazil, between September, 2004 and December, 2006. Streams were located in different land cover types including natural (forest), rural (agricultural), and developed landscapes. In addition, water samples from wells, lysimeters, surface runoff, and precipitation were collected from four sites, 2 natural and 2 rural, and analyzed for nutrient concentrations. Streams were sampled every 2-4 weeks; rain water was collected approximately monthly during the wet season and once during a dry season; wells and lysimeters were sampled monthly; and surface runoff collections were event based. There are three comma-delimited data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd07_plfa_soils_microbial_biomass_1017&quot;&gt;ND07_PLFA_Soils_Microbial_Biomass_1017&lt;/h4&gt;
This data set reports the microbial biomass in soil samples collected from the Cerrado, a woodlands-savannah area, in Brasilia, Brazil. Microbial biomass was determined as the total concentration of phospholipid fatty acids (PLFAs). Soil samples (0-5 cm) were collected from June, 2000 to June, 2001 in two native areas of Cerrado that were subjected to a range of fire regimes. Two plots were protected from fire since 1973, another two plots were subjected to prescribed fires every two years since 1992, and a fifth plot was in a 20 year-old active pasture (Brachiaria brizantha). The analyses were conducted to determine the effects of fire regimes and changes in vegetation cover on the microbial communities of Cerrada soils. There is one comma-separated ASCII data file with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd07_no_flux_cerrado_1124&quot;&gt;ND07_NO_Flux_Cerrado_1124&lt;/h4&gt;
This data set reports the results of soil nitric oxide (NO) flux, soil moisture, and soil nitrate (NO3) and ammonium (NH4) concentration measurements on Cerrado soils receiving nitrogen fertilization. Measurements and samples were collected from control and fertillized experimental plots on Cerrado soils within the Ecological Reserve of the Brazilian Institute of Geography and Statistic (IBGE), Brasilia, Brazil. Sampling dates were from March 26, 2004 to November 25, 2004. The soils had received nitrogen and phosphorus fertilization treatments which began in 1998. The objective of this project was to determine the long-term effects of nutrient addition (N and N+P) in native Cerrado area on N oxide fluxes from soil to the atmosphere. There is one comma delimited (.csv) ASCII file with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd07_trace_gas_land_use_1016&quot;&gt;ND07_Trace_Gas_Land_Use_1016&lt;/h4&gt;
This data set reports on soil-atmosphere fluxes of trace carbon dioxide, carbon monoxide, nitrous oxide, and nitric oxide (CO2, CO, N2O, NO) under various natural and manipulated land use conditions. The studies were conducted near Brasilia, Brazil in pastures and agricultural areas under a variety of management regimes and in more natural areas of cerrado (20-50% canopy cover) and campo sujo (open, grass-dominated), which were either burned every 2 years or protected from fire. Results provide data and relationships needed for regional trace gas models. There are nine comma-separated ASCII data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd08_biomass_jari_1148&quot;&gt;ND08_Biomass_Jari_1148&lt;/h4&gt;
This data set reports the concentrations of the nutrients nitrogen (N), phosphorus (P), magnesium (Mg), calcium (Ca), and potassium (K) in roots, litterfall, leaves, and twigs, biomass of fine roots and litterfall, and the decomposition of leaves and twigs in samples that were collected on the property of Jari Celulose, Monte Dourado, Para, Brazil, from 1999-2001. Samples were collected from two study sites, a eucalyptus plantation and an adjacent primary forest, during both rainy and dry seasons. Roots were sampled from three depths (0-15 cm, 35-50 cm, and 85-100 cm). There are five comma-delimited data files with this data set. DATA QUALITY STATEMENT: The Data Center has determined that there are questions about the quality of the data reported in this data set. The data set has missing or incomplete data, metadata, or other documentation that diminishes the usability of the products. KNOWN PROBLEMS: The data files do not identify the year in which samples were collected. The methods for nutrient, decomposition, and biomass sampling and analyses were not provided. The data file descriptions indicate that samples were collected from two soil types (sandy and clay) but there is no documentation of which data field provides that information. Also, there is no documentation for the Location or Block fields in the data files.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd08_soil_respiration_1250&quot;&gt;ND08_Soil_Respiration_1250&lt;/h4&gt;
This data set provides (1) carbon (C) and nitrogen (N) concentration measurements of two soil aggregate fractions (250-2000 micon, small macro-aggregates (SMAG)), and (53-250 micron (micro-aggregates (mico)) and (2) in situ soil respiration measurements (January-March 2003) on sand and clay soils from a Eucalyptus plantation and an adjacent primary forest. The soils for fractionation were sampled in July 2001 from 0-20 cm and 30-50 cm depths. The research site was on the property of Jari Celulose, Monte Dourado, Para, Brazil. There are two files with this data set in comma-delimited (.csv) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd10_soil_chemistry_1171&quot;&gt;ND10_Soil_Chemistry_1171&lt;/h4&gt;
This data set provides the results of soil physical property and chemical measurements of samples collected from two pasture chronosequences (years since conversion from primary forest) located on two ranches south of Santarem, Para, Brazil, and east of the Tapajos River. Soil data includes soil classification, bulk density, texture, and mean concentrations of total nitrogen (N), carbon (C), phosphorus (P), and P fractions. The soils were high clay oxisols and highly sandy entisols. One chronosequence of sites was established on oxisol soils dating 2, 7, and 15 years since conversion from primary forest. A second set of sites, 1, 7, and 15 years old was established on the sandy entisols. Five of the six pasture sites were on a single ranch; the 2-year-old oxisol pasture was the exception. Ten soil samples per site were collected from 0-10 cm depth along random intervals within 100-m transects in August 1997. There are two comma-delimited (.csv) data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd11_veg_biomass_mt_964&quot;&gt;ND11_Veg_Biomass_MT_964&lt;/h4&gt;
Not available.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd11_logging_damage_mt_977&quot;&gt;ND11_Logging_Damage_MT_977&lt;/h4&gt;
Data were collected in the logging concession at the Fazenda Rohsamar in the municipality of Juruena in northwestern Mato Grosso. Estimates of damage associated with logging operations were made after logging operations were complete in 2003 and 2004. Damage associated with gaps created by felling single trees was estimated in 54 individual gaps. Characteristics of the single harvested tree were recorded and included species, DBH, commercial height, total height, and canopy proportions. Damage to all surrounding trees was recorded. Stratified transects in two logging blocks were used to estimate damage associated with road building and skid trails. Twenty-six transects were established in Block 5 and 21 transects in Block 18 to assess the frequency of damage by log skidders and tree felling. The boundaries between different types of damage were noted along the transect and the length in meters of that damage type along the transect was recorded. From this information, the area of the logging block affected by road building and skid trails was determined. The Gap Survey and the Logging Damage Transects Survey data are provided in comma-separated ASCII files. A third file provides the coordinates of the starting points for the Survey Transects.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd11_soil_nitrate_moisture_mt_976&quot;&gt;ND11_Soil_Nitrate_Moisture_MT_976&lt;/h4&gt;
This data set reports the results of the analysis of soil samples for Nitrate (NO3) and physical properties that were collected for one year following reduced impact logging in logging concessions at the Fazenda Rohsamar in the municipality of Juruena in northwestern Mato Grosso. Sample locations were randomly selected from stratified regions of the 1,400 ha Block 5 to account for local scale soil variability. Soil samples were collected to 8-m depth in (1) nine gaps formed by single tree removal and (2) nine areas of undisturbed primary forest. Areas of undisturbed forest were confined to patches of forest within Block 5 that were protected from logging. An additional 3 forested areas were sampled to 3-m depth that contained high sand content. These results quantified the effects of reduced impact logging, to test whether nitrogen (N) loss from leaves and coarse woody debris under reduced impact logging results in a significant accumulation of subsoil nitrate (Feldpausch et al., 2009). One comma separated data file contains the soil moisture results and a second file the soil NO3 content and soil physical properties.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd11_nitrogen_transfer_leaf_litter_915&quot;&gt;ND11_Nitrogen_Transfer_Leaf_Litter_915&lt;/h4&gt;
It has been proposed that the C/N ratio, or quality, of litter or mulch mixtures affects N release. Although total N release from these mixtures and the effects on soil N are relatively well understood, a mechanistic understanding of the interactions between litter species with respect to their N release is still lacking. This study examines decomposition and N dynamics in mixtures of high-quality leguminous mulch, gliricidia [Gliricidia sepium (Jacq.) Kunth. ex Walp.] with a C/N ratio of 13, and low-quality cupuacu [Theobroma grandiflorum (Wild. ex Spring) Schumann] litter with a C/N ratio of 42, which occur in combination in agroforestry systems. Ratios of 100:0, 80:20, 50:50, 20:80, 0:100 of fresh 15N-enriched gliricidia leaves and senescent cupuacu leaves, totaling the same dry weight of 6.64 t ha-1, were applied to an Oxisol and sampled at 6, 14, 38, and 96 days after application. After more than 40% of the N in the gliricidia leaves had been released and the microbial biomass N reached its peak, a significant increase in available soil N occurred at day 14, which was more pronounced with greater amounts of gliricidia in the leaf mixture. However, relative to the N applied in the leaf mixture, there was no significant difference in available soil N with greater proportions of gliricidia. Total N release from the mixtures corresponded to the total N applied by gliricidia. Until day 38, cupuaÃƒÂ§u C mineralization was significantly faster in the presence of the highest proportion of gliricidia compared to lower proportions. This faster C mineralization of more than 0.5% per day, however, did not increase total C loss or N release from cupuaÃƒÂ§u leaves after 96 days. The use of 15N tracers identified an N transfer from gliricidia leaves and the soil to cupuaÃƒÂ§u leaves and consequently, a lower N release from gliricidia to the soil in the presence of cupuaÃƒÂ§u leaves. Though we expected that available N in the soil would also decrease with greater amounts of cupuaÃƒÂ§u litter in the mixture, our results indicated an additive effect of the two species on N release and soil mineral N, with gross interactions between them canceling net interactive effects. Therefore, N release of leaf mixtures behaved as predicted from a calculated sum of individual release patterns, in spite of a transfer of N from the high- to the low-quality leaves.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd11_carbon_export_cpom_913&quot;&gt;ND11_Carbon_Export_CPOM_913&lt;/h4&gt;
Resolving the carbon (C) balance in the Amazonian forest depends on an improved quantification of production and losses of particulate C from forested landscapes via stream export. The main goal of this work was to quantify litterfall, the lateral movement of litter, and the export of coarse organic particulate matter (&amp;gt;2 mm) in four small watersheds (1-2 ha) under native forest in southern Amazonia near Juruena, Mato Grosso, Brazil (10Â°25 S, 58Â°46 W). Mean litterfall production was 11.8 Mg ha-1 y-1 (5.7 Mg C ha-1 y-1). Litterfall showed strong seasonality, with the highest deposition in the driest months of the year. About two times more C per month was deposited on the forest floor during the 6-mo dry season (0.65 Mg C ha-1 mo-1) compared to the rainy season (0.3 Mg C ha-1 mo-1). The measured C concentration of the litterfall samples was greater in the dry season than in the rainy season (49% vs. 46%, P &amp;lt; 0.05). The lateral movement of litter increased from the plateau (upper landscape position) towards the riparian zone. However, the trend in C concentration of laterally transported litter samples was the opposite, being highest on the plateau (44%) and lowest in the riparian zone (42%) (P &amp;lt; 0.05). Stream-water exports of particulate C were positively correlated with streamflow, increasing in the rainiest months. The export of particulate C in streamflow was found to be very small (less than 1%) in relation to the amount of litterfall produced.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd11_tree_vine_biomass_mt_922&quot;&gt;ND11_Tree_Vine_Biomass_MT_922&lt;/h4&gt;
The purpose of this study was to determine if spatially-explicit commercial timber inventories (CTI) could be used in conjunction with satellite imagery to improve timber assessments and forest biomass estimates in Amazonia. As part of a CTI, all commercial trees &amp;gt;&#x3D; 45 cm DBH were measured and georeferenced in 3500 ha of a logging concession in NW Mato Grosso, Brazil. A scientific inventory was conducted of all trees and palms &amp;gt;&#x3D; 10 cm DBH in 11.1 ha of this area. A total of &amp;gt; 20,000 trees were sampled for both inventories. To characterize vegetation radiance and topographic features, regional LANDSAT TM and ASTER images were obtained. Using a stream network derived from the ASTER-based 30 m digital elevation model (DEM), a procedure was developed to predict areas excluded from logging based on reduced impact logging (RIL) criteria. A topographic index (TI) computed from the DEM was used to identify areas with similar hydrologic regimes and to distinguish upland and lowland areas. Some timber species were associated with convergent landscape positions (i.e., higher TI values). There were significant differences in timber density and aboveground biomass (AGB) in upland (6.0 stems ha(-1), 33 Mg ha(-1)) versus lowland (5.4 stems ha(-1), 29 Mg ha(-1)) areas. Upland and lowland, and timber and non-timber areas could be distinguished through single and principal component analysis of LANDSAT bands. However, radiance differences between areas with and without commercial timber on a sub-hectare scale were small, indicating LANDSAT images would have limited utility for assessing commercial timber distribution at this scale. Assuming a 50 m stream buffer, areas protected from logging ranged from 7% (third order streams and above) to 28% (first order and above) of the total area. There was a strong positive relationship between AGB based on the scientific inventory of all trees and from the commercial timber, indicating that the CTI could be used in conjunction with limited additional sampling to predict total AGB (276 Mg ha(-1)). The methods developed in this study could be useful for facilitating commercial inventory practices, understanding the relationship of tree species distribution to landscape features, and improving the novel use of CTIs to estimate AGB.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd11_soil_spatial_variability_914&quot;&gt;ND11_Soil_Spatial_Variability_914&lt;/h4&gt;
The northwestern region of Mato Grosso State consists of complex landscapes due to ongoing geomorphologic activity that contributes to the occurrence of different soil classes over small distances, which complicates soil sampling strategies. This study was conducted in Juruena (MT), with the objective of identifying pedologic classes in undisturbed forested headwater catchments by examining the spatial variability of soil texture and color, and taking elevation and topographic position into consideration. The spatial variability of soil texture and color were determined for 185 georeferenced sample points from a 20 x 20 m grid over the four headwater catchments. By sampling each location at depths of 0-20 and 40-60 cm it was possible to distinguish and map the principle soil classes found in the study area to the 2nd category level of the Brazilian System of Soil Classification, associated with the topographic relief. A satisfactory relationship between the redness index of the diagnostic horizons and the soil class colors was also found. The small headwater catchments contained the soil classes Plintossolos and Argissolos (of plinthic character) at altitudes below 280 m, and Latossolos at higher elevations. In this way, the use of geostatistics to map soil classes proved effective, as well as to estimate the precision of the resulting maps. Nevertheless, pedologic knowledge and a follow-up field validation of the resulting maps are necessary for an application as well as adjustments to the geostatistical models.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd11_soil_water_pressure_851&quot;&gt;ND11_Soil_Water_Pressure_851&lt;/h4&gt;
This data set contains information that can be used to examine water fluxes in soils beneath tree crops in an Amazonian agroforest. The data consists of repeated measurements of soil matrix pressure and soil moisture content at several depths. The study was carried out at the Empresa Brasileira de Pesquisa Agropecuaria (Embrapa)-AmazÃƒÂ´nia Ocidental, 29 km North of Manaus, Brazil (3Â° 8&amp;#39; S, 59Â° 52&amp;#39; W, 40 - 50 m above sea level), in 1998 and 1999.Microaggregated tropical soils have shown high water conductivity even under unsaturated conditions in laboratory experiments. It is not clear, however, what depth the infiltrating soil water reaches during storm events under humid tropical conditions. Dynamics and fluxes of water were determined with high temporal resolution to a depth of 5 m in a Xanthic Hapludox of central Amazonia, Brazil. The soil water percolated to a depth of 0.9 m within 2 h of a rainfall event of 48 mm. Water fluxes were significantly slower below 0.9 m (17% of infiltration at 0 - 0.9 m) due to higher bulk densities. Percolation not only started rapidly after a rainfall event when soil water suction reached a certain threshold (ca. 20 - 30 hPa) but was also reduced to background levels less than 1 h after the rain had ended. The demonstrated extremely short-term dynamics of water fluxes have implications for measurement design of water availability and solute leaching in microaggregated tropical soil that require correct time integrals of solution concentrations and soil water dynamics. Measurement intervals of 30 min or less were necessary in our study. Rapid water flows may explain the observed high nutrient losses from the topsoil of microaggregated tropical soil and the large accumulation of nutrients in the deep soil (&amp;gt; 5 m).
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd11_stream_nutrients_921&quot;&gt;ND11_Stream_Nutrients_921&lt;/h4&gt;
This data set contains baseflow streamwater concentrations of pH, specific conductivity, base cations, carbon (dissolved organic carbon (DOC), particulate organic carbon (POC) and bicarbonate alkalinity) and silica for four headwater streams in the seasonally dry Amazon (Johnson et al. (2006a) and Johnson et al. (2006b). Data are provided in one comma-separated ASCII file. This hydrologic study of four headwater watersheds was conducted in an undisturbed forest near Juruena, Mato Grosso in the seasonally dry, southern Amazon. The small catchments range in size from 0.85 to 1.9 ha. Stream water samples were collected weekly during rainy seasons and biweekly during the dry seasons. Baseflow stream water concentrations of base cations, silica, electrical conductivity, DOC, and alkalinity varied inversely with discharge. While there was variation among the watersheds, the concentration-discharge patterns were consistent for each of the four watersheds. Baseflow discharge data are not included in this data set and will be archived separately.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd30_pasture_degradation_1164&quot;&gt;ND30_Pasture_Degradation_1164&lt;/h4&gt;
This data set contains images of fractional cover estimates of photosynthetic vegetation (PV) canopy, nonphotosynthetic vegetation (NPV), and exposed soils (S) derived from Landsat images (30-m resolution) obtained for two ranches in the Brazilian Amazon from 1996 to 2002. The Fazenda Vitoria ranch is located in eastern Para near the city of Paragominas and is a mosaic of primary forest, logged forest, secondary forest, and pasture with moderately dissected topography. The Fazenda Nova Vida ranch is located in the state of Rondonia in western Amazonia and is a mosaic of primary forest, logged forest, and pastures. For Fazenda Vitoria, two dry-season Landsat images were obtained, subset, and analyzed. For Nova Vida three dry-season images and one end-of-wet-season image were obtained, subset, and analyzed. Spectral mixture analysis, which decomposes individual satellite pixels into constituent cover fractions of surface materials, was used with a general probabilistic modeling approach to derive subpixel cover fractions of PV, NPV, and S. There are six GeoTIFF (.tif) files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd30_litter_para_1129&quot;&gt;ND30_Litter_Para_1129&lt;/h4&gt;
This data set provides fine litterfall mass and nutrient concentrations from samples collected at chronosequences established at Sao Francisco do Para and Capitao Poco, Para, Brazil. Nitrogen (N) and phosphorus (P) concentrations were determined for litterfall samples from the Sao Francisco do Para, and N, P, potassium (K), calcium (Ca), and magnesium (Mg) concentrations are reported for samples from the Capitao Poco. In addition, carbon (C), N, delta C13, and delta N15 values were determined for leaves from the dominant species of the forests at Sao Francisco do Para; soil physical and chemical characteristics were determined for a subset of the chronosequence plots at the two study sites; and soil trace gas fluxes were determined from the Sao Francisco do Para site. All samples were collected between March 2001-February 2005. Trace gas fluxes were measured 10 times between October 2000 and June 2002 with 5 sample periods in dry season and 5 in wet season months. There are five comma-delimited data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;nd30_ree_water_chemistry_1131&quot;&gt;ND30_REE_Water_Chemistry_1131&lt;/h4&gt;
This data set reports the results of chemical analyses of rainfall, throughfall, litter leachate, and soil water samples collected before, during, and after a rainfall exclusion experiment conducted at the km 67 Seca Floresta site, Tapajos National Forest, Brazil. Samples were collected every two weeks from May 17, 1999 through May 10, 2006. Measurements included alkalinity, conductivity, pH, and selected anions and cations analyzed by ion chromatography. The exclusion treatment, began in late January 2000 and continued through December 2004, involved diverting about 60% of throughfall (equivalent to approximately half the rainfall) from a 1-hectare plot using plastic panels installed in the understory. The comparable 1-hectare control plot was unaltered. The purpose was to observe the potential effects of severe water stress on a humid Amazonian forest (Nepstad et al., 2002 and Nepstad et al., 2007). There are five comma-delimited data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tg02_balloon_voc_1110&quot;&gt;TG02_Balloon_VOC_1110&lt;/h4&gt;
This data set reports concentrations of biogenic volatile organic compounds (BVOCs) collected from tethered balloon-sampling platforms above selected forest and pasture sites in the Brazilian Amazon in March 1998, February 1999, and February 2000. The air samples were collected from forested sites in Brazil: the Tapajos forest (Para) in the Tapajos/Xingu moist forest; Balbina (Amazonas) in the Uatuma moist forest; and Jaru (Rondonia) in the Purus/Madeira moist forest. Two other sites were also located in Rondonia: at a forest reserve (Rebio Jaru) and a pasture (Fazenda Nossa Senhora Aparecida). The BVOCs measured included isoprene, alpha and beta pinene, camphene, sabinene, myrcene, limonene, and other monoterpenes. Approximately 24 to 40 soundings, including as many as four VOC samples collected simultaneously at various altitudes, were made at each site. There is one comma-delimited data file with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tg03_aeronet_aot_1128&quot;&gt;TG03_AERONET_AOT_1128&lt;/h4&gt;
This data set includes aerosol optical thickness measurements from the CIMEL sunphotometer for 22 sites in Brazil during the period from 1993-2005. The AERONET (AErosol RObotic NETwork) program is an inclusive federation of ground-based remote sensing aerosol networks established by AERONET and the PHOtomÃ©trie pour le Traitement OpÃ©rationnel de Normalisation Satellitaire (PHOTONS) and greatly expanded by AEROCAN (the Canadian sunphotometer network) and other agency, institute and university partners. The goal is to assess aerosol optical properties and validate satellite retrievals of aerosol optical properties. The network imposes standardization of instruments, calibration, and processing. Data from this collaboration provides globally distributed observations of spectral aerosol optical depths, inversion products, and precipitable water in geographically diverse aerosol regimes. Three levels of data are available from the AERONET website: Level 1.0 (unscreened), Level 1.5 (cloud-screened), and Level 2.0 (cloud-screened and quality-assured). Data provided here are Level 2.0. There are 22 comma-delimited data files with this data set and one companion text file which contains the latitude, longitude, and elevation of the 22 sites.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tg03_aeronet_solar_flux_1137&quot;&gt;TG03_Aeronet_Solar_Flux_1137&lt;/h4&gt;
This data set includes solar surface irradiance from Kipp and Zonen CM-21 pyranometers, both total unfiltered and filtered (RG695), and photosynthetically active radiation (PAR) from Skye-Probetech SKE-510 PAR sensors. Measurements were made at six sites acrosss the Brazilian Amazon during the period from 1999 to 2004. These sites were co-located with AERONET (AErosol RObotic NETwork) program sites. There are 17 comma-delimited data files (.csv) with this data set. The AERONET program is an inclusive federation of ground-based remote sensing aerosol networks established by AERONET and the PHOtometrie pour le Traitement Operationnel de Normalisation Satellitaire (PHOTONS) and greatly expanded by AEROCAN (the Canadian sunphotometer network) and other agency, institute and university partners. The goal is to assess aerosol optical properties and validate satellite retrievals of those properties. The network imposes standardization of instruments, calibration, and processing.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tg05_casa_1199&quot;&gt;TG05_CASA_1199&lt;/h4&gt;
This data set provides maps produced from model output data from the National Aeronautics and Space Administration-Carnegie Ames Stanford Approach (NASA-CASA) model and other modeling approaches. The maps include estimated annual Net Primary Production (ANPP), leaf (live) biomass carbon, wood (live) biomass carbon, fine root (live) biomass carbon, metabolic leaf litter (dead) carbon, structural leaf litter (dead) carbon, woody detritus (dead) carbon, and slow soil carbon, gridded at half-degree spatial resolution for the years 1982-1998, and 2001 (NPP data) for Brazil. Maps are provided at one-degree resolution for monthly soil emissions and soil uptake of N2O, NO, CO, and CH4. In addition, there are maps in 8-km resolution for soil texture, soil carbon, soil pH, soil maximum plant available water (paw), and net primary productivity (NPP). There are three files with this data set in tar.gz format. The files are in half-degree, one-degree, and 8-km resolution. When expanded, the half degree and one degree files contain 83 map files in GeoTIFF (.tif) format. The third file (8-km resolution) contains the soil and productivity maps. When expanded, this file contains 22 files in GeoTIFF (.tif) format.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tg06_vertical_profiles_1175&quot;&gt;TG06_Vertical_Profiles_1175&lt;/h4&gt;
This data set contains measurements of atmospheric carbon dioxide (CO2), methane (CH4), carbon monoxide (CO), hydrogen (H2), nitrous oxide (N2O), and sulfur hexafluoride (SF6) collected from December 2000-November 2005 as vertical profiles above three sites in Brazil: Fortaleza, Santarem, and Manaus. At Santarem, ascending profiles were made above the Tapajos National Forest, near the km 67 Tower Site. At Manaus, ascending profiles were made above the K34 flux tower (aka, ZF2 km 34 tower) to the northwest of the city of Manaus. Descending profiles were flown nearby, but at locations upwind of population centers to avoid possible pollution. Fortaleza samples were collected off the coast, over the Atlantic Ocean to sample background air before it flows over the Amazon Basin. Air samples were collected as discrete samples aboard light aircraft and shipped to laboratories for analysis relative to internationally accepted calibration standards. There are three comma-delimited (.csv) data files with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tg07_fallen_standing_necromass_998&quot;&gt;TG07_Fallen_Standing_Necromass_998&lt;/h4&gt;
This data set reports the characterization of fallen necromass as the volume and density of coarse woody debris (CWD), and standing necromass as the volume and density of standing dead trees. Measurements were made in undisturbed and logged forest areas of the Tapajos National Forest, and Cauaxi Forest, Para, Brazil, and Juruena Forest, Mato Grosso, Brazil from 2002-2004. Fallen and standing necromass were classified into one of five categories according to its state of decomposition. There are two comma-delimited ASCII data files with this data set: two files contain the sampling information, decomposition state, and DBH measurements. There are also two files provided as companion data files which provide sampling transect descriptions.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tg07_soil_nutrients_1085&quot;&gt;TG07_Soil_Nutrients_1085&lt;/h4&gt;
This data set reports phosphorus (P), carbon (C), and nitrogen (N) nutrient pool concentrations for forest soils and roots and P pool concentrations for forest floor litter, soil solutions, and microbial extracts. Soils samples were also extracted using the Hedley sequential fractionation method and the extracts analyzed for P. Nutrient pool concentrations are presented on an areal basis of 1 hectare to a depth of 10 cm, as calculated from soil bulk densities and respective pool biomass quantities. There is one comma-delimited ASCII file with this data set. These measurements were made during a soil P addition fertilization experiment conducted at the km 83 site, Tapajos National Forest, Para, Brazil. Control and fertilized plots were established in both sandy loam and clay soils. Soil cores were collected every 4 months from August 1999 through April 2000 (McGroddy et al. 2008).
&lt;br&gt;&lt;h4 id&#x3D;&quot;tg07_stm_glas_836&quot;&gt;TG07_STM_GLAS_836&lt;/h4&gt;
This data set provides the results of a GLAS (the Geoscience Laser Altimeter System) forest structure validation survey conducted in Santarem and Sao Jorge, Para during November 2004 (Lefsky et al., 2005). DBH, total height, commercial height, canopy width and canopy class description were measured for 11 primary forest sites in Santarem along two 75m transects per GLAS measurement. For 10 secondary forest sites in Sao Jorge, the number of stems 0-2cm, 2-5cm, 5-10cm, and greater than 10cm were measured. For all stems greater than 10cm the DBH was measured, and for all sites, the maximum height was recorded. The basal area was calculated for all trees with DBH greater than 10cm within our transects, and biomass was calculated using the Brown, 1997 formula.Exchange of carbon between forests and the atmosphere is a vital component of the global carbon cycle. Satellite laser altimetry has a unique capability for estimating forest canopy height, which has a direct and increasingly well understood relationship to aboveground carbon storage.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tg07_fft_survey_km83_923&quot;&gt;TG07_FFT_Survey_Km83_923&lt;/h4&gt;
Changes in the biomass of Amazon region forests represent an important component of the global carbon cycle but the biomass of these forests remains poorly quantified. We examined forest survey data for trees with a diameter at breast height (DBH) greater than 35 cm from 4 plots with a total area of 392 ha in the Tapajos National Forest near Santarem, Para, Brazil (S 3.04, W 54.95). The average frequency of trees greater than 35 cm DBH was approximately 55 ha^-1. Based on tree diameter data, allometric relations, and published relations for biomass in other compartments besides trees of DBH &amp;gt; 35 cm, we estimated a total biomass density of 372 Mg ha^-1. Trees with diameters greater than 35 cm DBH accounted for about half of the total biomass. This estimate includes all live and dead plant material above and below ground with the exception of soil organic matter. We propagated errors in sampling and those associated with allometric relations and other ratios used to estimate biomass of roots, lianas and epiphytes, and necromass. The major sources of uncertainty in our estimate were found in the allometric relations for trees with DBH greater than 35 cm, in the estimates of numbers of trees with DBH less than 35 cm, and in root biomass. In the worst case, we estimate an uncertainty in this value of about 40%. Simulated sampling based on our full survey, suggests that we could have estimated mean biomass per hectare for trees (DBH greater than 35 cm) to within 20% with 95% confidence by sampling 21 randomly selected 0.25 ha plots in our study area.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tg07_litter_decomposition_925&quot;&gt;TG07_Litter_Decomposition_925&lt;/h4&gt;
Once the weathering of parent material ceases to supply significant inputs of phosphorus (P), vegetation depends largely on the decomposition of litter and soil organic matter and the associated mineralization of organic P forms to provide an adequate supply of this essential nutrient. At the same time, the decomposition of litter is often characterized by the immobilization of nutrients, suggesting that nutrient availability is a limiting factor for this process. Immobilization temporally decouples nutrient mineralization from decomposition and may play an important role in nutrient retention in low-nutrient ecosystems. In this study, we used a common substrate to study the effects of native soil P availability as well as artificially elevated P availability on litter decomposition rates in a lowland Amazonian rain forest on highly weathered soils. Although both available and total soil P pools varied almost three fold across treatments, there was no significant difference in decomposition rates among treatments. Decomposition was rapid in all treatments, with approximately 50% of the mass lost over the 11-month study period. Carbon (C) and nitrogen (N) remaining and C:N ratios were the most effective predictors of amount of mass remaining at each time point in all treatments. Fertilized treatments showed significant amounts of P immobilization (P &amp;lt; 0.001). By the final collection point, the remaining litter contained a quantity equivalent to two-thirds of the initial P and N, even though only half of the original mass remained. In these soils, immobilization of nutrients in the microbial biomass, late in the decomposition process, effectively prevents the loss of essential nutrients through leaching or occlusion in the mineral soil.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tg07_root_mortality_longterm_1116&quot;&gt;TG07_Root_Mortality_Longterm_1116&lt;/h4&gt;
This data set reports measurements of trace gas fluxes of methane (CH4), nitric oxide (N2O), nitrous oxide (NO), carbon dioxide (CO2) from soils at a study site in the Tapajos National Forest (TNF), near the km 83 on the Santarem-Cuiaba Highway south of Santarem, Para, Brazil. Data for root mass and carbon content, soil nitrogen (N), nitrification, and moisture content are also provided. There are five comma-delimited data files with this data set. The research was conducted to test the effects of root mortality on the soil-atmosphere trace-gas fluxes over the course of one year. Root mortality was induced by isolating blocks of land to 1 m depth using trenching and root exclusion screening. Gas fluxes were measured weekly for ten weeks following the trenching treatment and monthly for the remainder of the year. Note: The related data set LBA-ECO TG-07 Soil Trace Gas Flux and Root Mortality, Tapajos National Forest contains the same flux data that were measured weekly for ten weeks following the trenching treatment. This data set also provides the monthly data for the remainder of the year.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tg07_trace_gas_profiles_1107&quot;&gt;TG07_Trace_Gas_Profiles_1107&lt;/h4&gt;
This data set provides concentrations of carbon dioxide (CO2), methane (CH4), and nitrous oxide (N2O) from air samples collected at several heights on towers at three locations in upland old growth forests in the Brazilian Amazon during the wet and dry seasons of 2004 and 2005. Towers are located in the Caxiuana National Forest, in the state of Amazonas; the Manaus, Para, site in the Cuieiras Reserve; and the Sinop site, located north of that city in the state of Mato Grosso. Two sampling campaigns were conducted at each location. Samples were collected from each height 3-5 times on several nights and at least once during well-mixed daytime conditions during each campaign for a total of 75 profiles on 19 dates. There is one comma-delimited ASCII file with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tg07_autochamber_soil_co2_flux_km67_927&quot;&gt;TG07_Autochamber_Soil_CO2_Flux_Km67_927&lt;/h4&gt;
The net ecosystem exchange of carbon dioxide was measured by eddy covariance methods for 3 years in two old-growth forest sites near Santarem, Brazil. Carbon was lost in the wet season and gained in the dry season, which was opposite to the seasonal cycles of both tree growth and model predictions. The 3-year average carbon loss was 1.3 (confidence interval: 0.0 to 2.0) megagrams of carbon per hectare per year. Biometric observations confirmed the net loss but imply that it is a transient effect of recent disturbance superimposed on long-term balance. Given that episodic disturbances are characteristic of old-growth forests, it is likely that carbon sequestration is lower than has been inferred from recent eddy covariance studies at undisturbed sites.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tg07_root_mortality_experiment_924&quot;&gt;TG07_Root_Mortality_Experiment_924&lt;/h4&gt;
We conducted an experiment on sand and clay tropical forest soils to test the short-term effect of root mortality on the soil-atmosphere flux of nitrous oxide, nitric oxide, methane, and carbon dioxide. We induced root mortality by isolating blocks of land to 1 m using trenching and root exclusion screening. Gas fluxes were measured weekly for ten weeks following the trenching treatment. For nitrous oxide there was a highly significant increase in soil-atmosphere flux over the ten weeks following treatment for trenched plots compared to control plots. N2O flux averaged 37.5 and 18.5 ng N cm-2 h-1 from clay trenched and control plots and 4.7 and 1.5 ng N cm-2 h-1 from sand trenched and control plots. In contrast, there was no effect for soil-atmosphere flux of nitric oxide, carbon dioxide, or methane.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tg07_manual_flux_km67_1026&quot;&gt;TG07_Manual_Flux_Km67_1026&lt;/h4&gt;
Trace gas fluxes of carbon dioxide, methane, nitrous oxide, and nitric oxide (CO2, CH4, N2O, and NO) from surface soil were measured manually in an undisturbed forest at the Tapajos National Forest Seca-Floresta Site, which is within the footprint of the km 67 eddy flux tower. Measurements were made in January 2000 through April 2004, approximately twice per month. On each sampling date, up to four sets of 30-m lines were established off the existing transects at the Seca-Floresta site. Along each line eight chambers were installed for gas collection. In addition soil samples were collected for analysis of soil moisture as water-filled pore space (WFPS). There is one comma-delimited ASCII file with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tg07_soil-atmosphere_flux_km83_926&quot;&gt;TG07_Soil-Atmosphere_Flux_Km83_926&lt;/h4&gt;
Selective logging is an extensive land use in the Brazilian Amazon region. We studied the soil-atmosphere fluxes of nitrous oxide (N2O), nitric oxide (NO), methane (CH4), and carbon dioxide (CO2) on two soil types (clay Oxisol and sandy loam Ultisol) over two years (2000-2001)in both undisturbed forest and forest recently logged using reduced impact forest management in the Tapajos National Forest, near Santarem, Para, Brazil. In undisturbed forest, annual soil-atmosphere fluxes of N2O (mean +/- standard error) were 7.9 +/- 0.7 and 7.0 +/- 0.6 ng N cm-2 h-1 for the Oxisol and 1.7 +/- 0.1 and 1.6 +/- 0.3 ng N cm-2 h-1 for the Ultisol for 2000 and 2001 respectively. The annual fluxes of NO from undisturbed forest soil in 2001 was 9.0 +/- 2.8 ng N cm-2 h-1 for the Oxisol and 8.8 +/- 5.0 ng N cm-2 h-1 for the Ultisol. Consumption of CH4 from the atmosphere dominated over production on undisturbed forest soils. Fluxes averaged -0.3 +/- 0.2 and -0.1 +/- 0.9 mg CH4 m-2 d-1 on the Oxisol and -1.0 +/- 0.2 and -0.9 +/- 0.3 mg CH4 m-2 d-1 on the Ultisol for years 2000 and 2001. For CO2 in 2001, the annual fluxes averaged 3.6 +/- 0.4 :mol m-2 s-1 on the Oxisol and 4.9 +/- 1.1 :mol m-2 s-1 on the Ultisol. We measured fluxes over one year each from two recently logged forests on the Oxisol in 2000 and on the Ultisol in 2001. Sampling in logged areas was stratified from greatest to least ground disturbance covering log decks, skid trails, tree-fall gaps, and forest matrix. Areas of strong soil compaction, especially the skid trails and logging decks were prone to significantly greater emissions of N2O, NO, and especially CH4. In the case of CH4, estimated annual emissions from decks reached extremely high rates of 531 +/- 419 and 98 +/- 41 mg CH4 m-2 d-1, for Oxisol and Ultisol sites respectively, comparable to wetland emissions in the region. We calculated excess fluxes from logged areas by subtraction of a background forest matrix or undisturbed forest flux and adjusted these fluxes for the proportional area of ground disturbance. Our calculations suggest that selective logging increases emissions of N2O and NO from 30% to 350% depending upon conditions. While undisturbed forest was a CH4 sink, logged forest tended to emit methane at moderate rates. Soil-atmosphere CO2 fluxes were only slightly affected by logging. The regional effects of logging cannot be simply extrapolated based upon one site. We studied sites where reduced impact harvest management was used while in typical conventional logging ground damage is twice as great. Even so, our results indicate that for N2O, NO, and CH4, logging disturbance may be as important for regional budgets of these gases as other extensive land use changes in the Amazon such as the conversion of forest to cattle pasture.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tg07_dbh_cauaxi_1063&quot;&gt;TG07_DBH_Cauaxi_1063&lt;/h4&gt;
Canopy measurements in an undisturbed eastern Amazon forest (Cauxi, Para, Brazil. See Figure 1) were derived from a one-time event in 2000 using a hand-held laser range finder, and diameter at breast height (DBH) was determined manually. Parameters reported include: Crown Width, Crown Depth, Tree Height, and DBH. There is one comma-delimited ASCII data file with this data set. In addition, these manually derived measurements were compared to the IKONOS satellite data of crown dimensions that were acquired on 2 November 2000, from an orbital altitude of 680 km. The data from a 600 x 600 m block of undisturbed forest, including the 50 ha area surveyed in the field, were analyzed in a combined image processing and geographic information system environment. DATA QUALITY STATEMENT: The Data Center has determined that there are questions about the quality of the data reported in this data set. The data set has missing or incomplete data, metadata, or other documentation that diminishes the usability of the products. KNOWN PROBLEMS: Only the general location for this study was identified -- Cauaxi, Para, Brazil. The tree measurement data are of limited use because coordinates for the study site, coordinates of the beginning and end of the transects, and coordinates of the measured trees were not provided. Also, the area that the IKONOS image captured was not provided and the IKONOS image is not available due to restricted distribution.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tg08_soil_gas_fertilization_1105&quot;&gt;TG08_Soil_Gas_Fertilization_1105&lt;/h4&gt;
This data set provides nitric oxide (NO), nitrous oxide (N2O), carbon dioxide (CO2) flux measurements, nitrogen (N) and phosphorus (P) pools, net N mineralization and nitrification rates, and measurements of soil moisture, in response to nitrogen and phosphorus soil fertilization treatments. The research was conducted in a mature moist tropical forest and an 11-year pasture at Nova Vida in Rondonia, in the Brazilian Amazon, in 1998 and 1999. There is one comma-delimited ASCII data file with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tg08_soil_gas_wetting_1101&quot;&gt;TG08_Soil_Gas_Wetting_1101&lt;/h4&gt;
This data set includes the results of measurements of the soil gas fluxes of nitric oxide (NO), nitrous oxide (N2O), and carbon dioxide (CO2), soil moisture, soil temperature, and soil pools of ammonium and nitrate in response to a simulated rain event. Study sites were soils in mature forests and pastures of two ages (11 and 26 yrs old). The study took place during the dry season in August 1998 at Fazenda Nova Vida, Rondonia in the Brazilian Amazon. There is one comma-delimited ASCII file with this data set. This study investigated how changes in soil moisture (i.e., rains at the end of the dry season) affected the fluxes of NO, N20 and CO2 from forest and pasture soils in the southwestern Brazilian Amazon (Garcia-Montiel, et al., 2003). The main objectives were to measure the short-term dynamics of soil emissions of NO, N20, and CO2 in forest and pasture soils associated with soil wetting after prolonged dryness; and quantify the contribution of the pulses of N oxide fluxes resulting from soil wetting to dry season and annual fluxes.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tg09_n2o_soils_1013&quot;&gt;TG09_N2O_Soils_1013&lt;/h4&gt;
This data set reports the results of carbon, nitrogen, and oxygen isotopic analyses of soil, soil water, and N2O soil gas samples; total soil carbon and nitrogen concentrations; and soil texture and bulk density. Samples were collected from the km 83 Logged Forest Tower Site and the km 67 Seca-Floresta Site in the Tapajos National Forest (TNF) near Santarem, Para, Brazil. Soil samples were collected in July of 2000 and soil gas samples were collected in 2001 and 2002. Soil and gas samples were collected from various soil types at each site and from several depths in specially constructed pits. There is one comma-delimited ASCII data file with this data set.
&lt;br&gt;&lt;h4 id&#x3D;&quot;tg10_troffee_1195&quot;&gt;TG10_TROFFEE_1195&lt;/h4&gt;
This data set provides derived emission factors (EFs), reported in grams of compound emitted per kilogram of dry fuel (g/kg), for PM10 (particulate matter up to 10 micrometers in size), O3, CO2, CO, NO, NO2, HONO, HCN, NH3, OCS, DMS, CH4, and up to 48 non-methane organic compounds (NMOC) from the Tropical Forest and Fire Emissions Experiment (TROFFEE). TROFFEE used laboratory measurements followed by airborne and ground based field campaigns in Mato Grosso, Para, and Amazonas, Brazil during the 2004 Amazon dry season to quantify the emissions from pristine tropical forest and several plantations as well as the emissions, fuel consumption, and fire ecology of tropical deforestation fires. EFs were determined for 19 tropical deforestation fires in August and September, 2004. The combined output of these fires created a massive megaplume more than 500-km wide and covered a large area in Brazil, Bolivia, and Paraguay for about one month. For the megaplume, the EFs (reported in grams of compound emitted per kilogram of dry fuel (g/kg)) represented the effective emissions factor measured downwind from the source. There are two comma-delimited data files (.csv) and one text file (.txt) with this data set. The text file contains information regarding the fuel/fire sources, latitude and longitudes (also provided in the data files).
&lt;br&gt;&lt;h4 id&#x3D;&quot;pc06_ecmwf_lba_1141&quot;&gt;PC06_ECMWF_LBA_1141&lt;/h4&gt;
This data set provides the mean diurnal cycle of precipitation, near-surface thermodynamics, and surface fluxes generated from short-term forecasts from the European Centre for Medium-Range Weather Forecasts (ECMWF) model. The model outputs were 12- to 36-hour short-range forecasts, run at a triangular truncation of T319 and a vertical resolution of 60 levels, from each daily 1200 (UTC) analysis. The version of the forecast model used to prepare this data product was the operational ECMWF model in fall 2000, which included the tiled land-surface scheme (TESSEL) (Van den Hurk et al., 2000) and recent revisions to the convection, radiation, and cloud schemes described by Gregory et al., (2000). The ECMWF model was run for two Large-Scale Biosphere-Atmosphere Experiment in Amazonia (LBA) campaigns conducted in Rondonia, Brazil, during January and February of 1999: the Wet Season Atmospheric Mesoscale Campaign (WETAMC) and the Tropical Rainfall Measuring Mission (TRMM). See Silva Dias et al.,(2002) for additional information regarding the WETAMAC and TRMM campaigns. There are two comma-delimited data files with this data set: the ECMWF model output data and a file containing the mean hourly precipitation observations used to check the model output for biases.
&lt;br&gt;&lt;h4 id&#x3D;&quot;able_897&quot;&gt;ABLE_897&lt;/h4&gt;
The ABLE 2A and 2B (Atmospheric Boundary Layer Experiments) data consists of estimates of the rate of exchange of a wide variety of aerosols and gases between the Amazon Basin and its atmospheric boundary layer, and the processes by which these aerosols and gases are moved between the boundary layer and the free troposphere. The data are presented in gzipped ASCII text files in Global Tropospheric Experiment (GTE) format. The ABLE-2 project consisted of two expeditions: the first in the Amazonian dry season (ABLE-2A, July-August 1985); and the second in the wet season (ABLE-2B, April-May 1987). The ABLE-2 core research data were gathered by NASA Electra aircraft flights that stretched from Belem, at the mouth of the Amazon River, west to Tabatinga, on the Brazil-Colombia border, from a base at Manaus in the heart of the forest. See Figure 1. These observations were supplemented by ground based chemical and meteorological measurements in the dry forest, the Amazon floodplain, and the tributary rivers through use of enclosures, an instrumented tower in the jungle, a large tethered balloon, and weather and ozone sondes. This study showed air above the Amazon jungle to be extremely clean during the wet season but air quality deteriorated dramatically during the dry season as the result of biomass burning, performed mostly at the edges of the forest. Biomass burning is also a source of greenhouse gases carbon dioxide and methane, as well as other pollutants (carbon monoxide and oxides of nitrogen). Amazonian ozone deposition rates were found to be 5 to 50 times higher than those previously measured over pine forests and water surfaces. The Amazon River floodplain is a globally significant source of methane, supplying about 12% of the estimated worldwide total from all wetlands sources. Over Amazonia, carbon monoxide is enhanced by factors ranging from 1.2 to 2.7 by comparison with adjacent regions due to isoprene oxidation and biomass burning. Over the rainforest individual convective storms transport 200 megatons of air per hour, of which 3 megatons is water vapor that releases 100,000 megawatts of energy into the atmosphere through condensation into rain. The ABLE was a collaboration of U.S. and Brazilian scientists sponsored by NASA and Instituto Nacional de Pesquisas Espaciais (INPE) and supported by the Global Tropospheric Experiment (GTE) component of the NASA Tropospheric Chemistry Program.
&lt;br&gt;&lt;h4 id&#x3D;&quot;arme_898&quot;&gt;ARME_898&lt;/h4&gt;
The Amazonian Region Micrometeorological Experiment (ARME) data contain micrometeorological data (climate, interception of precipitation, mircometeorology and soil moisture) on the elements of the energy balance and evapotranspiration for the Amazonian forest. ASCII text data files for each of the four data types have been zipped toghether. One of the many scientific findings of this experiment was that tropical forest does not experience water stress due to the lack of precipitation, during periods when evapotranspiration is at the potential rate (Shuttleworth, 1988). ARME data types include climate (meteorological), interception of precipitation, micrometeorology, and soil moisture. These data are described in the Data Description section below.
&lt;br&gt;&lt;h4 id&#x3D;&quot;pre_lba_abracos_899&quot;&gt;Pre_LBA_ABRACOS_899&lt;/h4&gt;
The data set presents the principal data from the Anglo-BRazilian Amazonian Climate Observation Study (ABRACOS) (Gash et al, 1996) and provides quality controlled information from five of the study topics considered by the project in five zipped files containing ASCII text data. The five study topics include Micrometeorology, Climate, Carbon Dioxide and Water Vapor, Plant Physiology, and Soil Moisture. The objectives of the ABRACOS were to monitor Amazonian climate and improve the understanding of the consequences of deforestation and to provide data for the calibration and validation of GCMs and GCM sub-models of Amazonian forest and post-deforestation pasture (Shuttleworth et al, 1991). Three areas were instrumented, each with different soils, dry season intensities and deforestation densities (Gash et al, 1996). In each area, an automatic weather station and soil moisture measurement equipment were installed: in a primary forest site and in nearby cattle pasture, for monitoring climate and soil status throughout the year. Additional intensive periods of study (or Missions), of varying duration, were operated at these sites: for calibration purposes, to understand the physical processes relevant to each site, and for detailed comparisons between sites. These data were collected under the ABRACOS project and made available by the UK Institute of Hydrology and the Instituto Nacional de Pesquisas Espaciais (Brazil). ABRACOS is a collaboration between the Agencia Brasileira de Cooperacao and the UK Overseas Development Administration. The processed, quality controlled and integrated data in the documented Pre-LBA data sets were originally published as a set of three CD_ROMs (Marengo and Victoria, 1998) but are now archived individually.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cabare_918&quot;&gt;CABARE_918&lt;/h4&gt;
Surface parameter digital maps of vegetation, soil, and topography were obtained for Rondonia, Brazil, covering the 5x5 degree region bounded by 13-8 degrees S and 65-60 degrees W. Numerical maps of the natural landscape structure were prepared by digitizing existing 1:1,000,000 maps. Satellite data give information about the most recent modifications of the surface due to human activities. This mapping work was the first step of a mesoscale meteorological modeling program (Calvet et al., 1997) in forested and deforested Southwestern Amazonia (Rondonia, Brazil). This work was performed in the framework of a research program (CABARE) supported by the European Union, CEC Environment Program. Data are provided in ArcGIS ArcInfo grid ascii format for the following surface parameters: Elevation of terrain of the Rondonia region (altitude.txt) LANDSAT-derived vegetation classification of the Rondonia region in 1993-1994 (classify.txt) Soil classification of the Rondonia region (soil.txt) Sand and Clay of the Rondonia region (sand.txt and clay.txt) Vegetation classification of the Rondonia region from RADAMBRASIL (Macedo et al., 1979) (vegetation.txt)
&lt;br&gt;&lt;h4 id&#x3D;&quot;camrex_904&quot;&gt;CAMREX_904&lt;/h4&gt;
The objective of CAMREX (Carbon in the Amazon River Experiment) project which was conducted from 1982 through 1991, was been to define by mass balances and direct measurements those processes which control the distribution of bioactive elements (C, N, P and O) in the mainstem of the Amazon River in Brazil. The CAMREX dataset represents a time series unique in its length and detail for very large river systems. The central sampling strategy has been to obtain representative flux-weighted water samples for comprehensive chemical analysis and to make rate measurements over 18 different sites within a 2000 km reach of the Brazilian Amazon mainstem, including major intervening tributaries. Samples have now been collected on 13 different cruises (1982-1991) during contrasting hydrographic stages. Data or images are provided for (1) water chemistry, (2) daily river discharge, (3) monthly estimates for 1989 of some model drivers and structure including NPP, Evapotranspiration, Precipitation, Temperature, and AVHRR data, (4) daily precipitation, and (5) air temperature anomalies. The processed, quality controlled and integrated data in the documented Pre-LBA Data sets were originally published as a set of three CD_ROMs (Marengo and Victoria, 1998) but are now archived individually.
&lt;br&gt;&lt;h4 id&#x3D;&quot;floodama_903&quot;&gt;FLOODAMA_903&lt;/h4&gt;
This data set provides a digital mosaic of the Amazon River floodplain that was compiled using Landsat TM images. This mosaic was planned in July 1995 as an activity of the EOS-IDS Project that was developed with cooperation among INPE, CENA, University of Washington in Seattle (UW), University of California in Santa Barbara (UCSB), and NASA. The mosaic is composed by 29 Landsat TM images covering a period from 1986 to 1995 that were selected with minimum cloud cover and within the July to September high water season of the Amazon River. These images were geometrically corrected using ground control points extracted from topographic charts and image charts at the 1:250,000 scale. In addition, these images were radiometrically rectified to 231/062 (Manaus region) TM image using the method developed by Hall et al. (1991). The radiometric rectification applied had a good performance for bands 3, 5, and 7, for most of the scenes. For bands 1 and 2 the radiometric rectification was limited, especially for scenes with intense haze. Nevertheless, the overall performance of radiometric normalization allowed the production of a uniform data set for the entire Brazilian Amazon River mainstem floodplain. The mosaic was then built using the best bands (rectified or non-rectified) of the TM images with 90 meter spatial resolution. The mosaic data are provided in geoTIFF-formatted files, rectified and geocoded, for six TM bands (1 to 5 and 7) with 90-meter spatial resolution. The mosaic is divided in two parts: Part 1, from the mouth of the Amazon river in Brazil to the Brazil/Peru boundary and Part 2, from the Brazil/Peru boundary to its spring. There is also a 500-meter resolution mosaic covering all the Amazon river (from spring to the mouth) with geoTIFF-formatted data files for TM bands 3, 4, and 5. The processed, quality controlled and integrated data in the documented Pre-LBA Data sets were originally published as a set of three CD_ROMs (Marengo and Victoria, 1998) but are now archived individually.
&lt;br&gt;&lt;h4 id&#x3D;&quot;fluamazon_896&quot;&gt;FLUAMAZON_896&lt;/h4&gt;
The FLUAMAZON Experiment data set includes meteorological data collected with radiosondes to examine the moisture flux from the northern coast of South America (near the mouth of the Amazon River) into central Amazonia. The measurements were collected from November 23, to December 21, 1989 during the period of transition between the dry and humid seasons in the region. Some of the studies performed with data from FLUAMAZON were related to the atmospheric thermodynamic structure over Amazonia. During FLUAMAZON, radiosonde measurements were made simultaneously in five different locations: Alcantara, Belem, Oiapoque, Manaus, and Alta Floresta. ASCII text data files for each location have been compiled and compressed into site-specific zipped files.
&lt;br&gt;&lt;h4 id&#x3D;&quot;islscp_919&quot;&gt;ISLSCP_919&lt;/h4&gt;
This data set contains hydrology, soils, radiation, cloud, and vegetation data from the International Satellite Land Surface Climatology Project (ISLSCP) Initiative I. The ISLSCP data sets should provide LBA modelers with many of the fields required to describe boundary conditions, and to initialize and force a wide range of land-biosphere-atmosphere models. All of the data have been processed to the same global spatial resolution (1 deg. x 1 deg.), using the same land/sea mask and steps have been taken to ensure spatial and temporal continuity of the data. The data sets cover the period 1987-1988 at 1-month time resolution for most of the seasonally varying quantities. For this pre-LBA data set, the ISLSCP I data are provided as global coverages. The companion file illustrations were subset over the LBA study area, from 35-85 deg. W longitude and 20 deg. S to 10 deg. N latitude, as shown in Figure 1. The data files and illustrations are organized into the three groups listed below. 1. Hydrology and Soils 2. Radiation and Clouds 3. Vegetation The data within each of these areas were acquired from a variety of sources including model output, satellites, and ground measurements. The individual data sets were provided in a variety of forms. In some cases, this required the data publication team to regrid and reformat data sets and in others to produce monthly averages from finer resolution data. The specific processing for each data set is detailed in the documentation. The processed, quality controlled and integrated data in the documented Pre-LBA Data sets were originally published as a set of three CD-ROMs (Marengo and Victoria, 1998) but are now archived individually.
&lt;br&gt;&lt;h4 id&#x3D;&quot;radambrasil_941&quot;&gt;RADAMBrasil_941&lt;/h4&gt;
The RADAMBRASIL project extensively mapped the Amazon soils using a combination of soil pit information, aerial photography, and geologic maps. During the project, 1,153 soil pits, distributed basin-wide, were described and sampled by horizon and analyzed for texture and chemical composition. This data set, which consists of one file in ASCII comma separated format, contains soil profile descriptions for locations throughout Brazilian Amazonia. These data are based on RADAMBRASIL surveys from the Soil Profiles of Amazonia (Source: IPAM, Brazil/WHRC, USA). See the companion file Soil Profiles of Amazonia.pdf
&lt;br&gt;&lt;h4 id&#x3D;&quot;rble_917&quot;&gt;RBLE_917&lt;/h4&gt;
The atmospheric boundary layer (ABL) is the layer of air closest to the ground which is directly influenced on a daily basis by the heating and cooling of the earth&amp;#39;s surface. The exact depth of the ABL varies according synoptic weather conditions and the time of day. During the daytime it is usually between 1 and 3 km; during the night it is much shallower. The ABL is important because it links the fluxes of heat and water vapor observed at the surface to the general circulation of the atmosphere. To model climate correctly, it is necessary for the ABL to be well understood and represented in the model. Because the air in the ABL is turbulent, small scale variations (about 1 km or less) in evaporation and heat flux at the surface are smoothed, with the temperature, humidity and depth of the ABL being uniform over the entire area. Larger scale variations (on the scale of 10 km or more) may lead to differences in ABL properties between the different surface types. Such differences may cause local atmospheric circulations to develop which may be important for the local climate of an area. During ABRACOS, three ABL measurement campaigns were carried out. These campaigns were called the Rondonia Boundary Layer Experiment (RBLE) 1, 2 and 3 and were held at Ji-Parana where the scale of the forested and deforested areas is large enough for each surface type to develop its own ABL. Refer to the related data set, Pre-LBA Anglo-Brazilian Amazonian Climate Observation Study (ABRACOS) Data, for additional information. The processed, quality controlled and integrated data in the documented Pre-LBA Data sets were originally published as a set of three CD_ROMs (Marengo and Victoria, 1998) but are now archived individually. The campaigns were held during the dry season when the difference in evaporation between the two surfaces types, forest and pasture, is at its greatest. Measurements were made with both free-flying radiosondes which measure temperature, humidity, and wind up to about 12 km and with a tethered balloon which makes more detailed measurements in the lowest 1 km of the atmosphere. Measurements were made at both the forest and clearing sites. Profiles of potential temperature measured during RBLE2 show that the daytime ABL was deeper over the clearing than the forest. The data have been used to test several models of ABL development. It appears that the ABL over pastures or over clearings grows more rapidly than predicted by the models, possibly because of the increased turbulence generated by the strips of forest typical of this area. The data have also been used to initialize one-dimensional climate models used in experiments to investigate the sensitivity of climate to land surface parameters, and to initialize a mesoscale model which can predict local effects on climate caused by the pattern of deforestation in this area.
&lt;br&gt;&lt;h4 id&#x3D;&quot;scar-b_916&quot;&gt;SCAR-B_916&lt;/h4&gt;
This data set contains meteorological data, reanalysis data, remote sensing images, and data on atmospheric composition collected during the Smoke, Clouds, and Radiation - Brazil (SCAR-B) experiment. The SCAR-B examined the effects of biomass burning on atmospheric processes with four primary goals: (1) improving techniques for remote sensing of these process from space, (2) obtain measurements of the rates of emissions of trace gases and particles from biomass burning, (3) observe the influence of atmospheric processes on the emission products was to obtain measurements of the rates of emissions of trace gases and particles from biomass burning, and to observe the influence of atmospheric processes on these emission products, and (4) characterize the physical and radiative properties of smoke particles from biomass burning. SCAR-B was conducted during biomass burning in the cerrado ( dry savannah) and Amazonia rainforest to understand the influence of land cover type on smoke, clouds, and radiation. Selected archived data and images from SCAR-B are described in the Data Description section table. Extensive background information on SCAR-B is provided following the Data Description. The processed, quality controlled and integrated data in the documented Pre-LBA Data sets were originally published as a set of three CD_ROMs (Marengo and Victoria, 1998) but are now archived individually.
&lt;br&gt;&lt;h4 id&#x3D;&quot;trace-a_920&quot;&gt;TRACE-A_920&lt;/h4&gt;
This data set contains atmospheric chemistry and meteorological data from the NASA Transport and Atmospheric Chemistry near the Equator-Atlantic (TRACE-A) field study. The NASA TRACE-A study took place in August 1992 to determine the cause and source of high concentrations of ozone that accumulate over the Atlantic ocean between southern Africa and South America during the months of August through October. The processed, quality controlled and integrated data in the documented Pre-LBA Data sets were originally published as a set of three CD-ROMs (Marengo and Victoria, 1998) but have now been archived individually.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.ornldaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA LPJ Project</title>
      <link>https://registry.opendata.aws/nasa-lpj</link>
      <guid>https://registry.opendata.aws/nasa-lpj</guid>
      <description>Exploring Greenhouse Gas Data; Driving Sustainable Strategies through Powerful Analysis
&lt;br&gt;&lt;h4 id&#x3D;&quot;lpj_eosim_l2_dch4e_ll&quot;&gt;LPJ_EOSIM_L2_DCH4E_LL&lt;/h4&gt;
The Lund-Potsdam-Jena Earth Observation SIMulator (LPJ-EOSIM) model estimates global wetland methane (CH4) emissions using simulated wetland extent and characteristics including soil moisture, temperature, and carbon content. For this dataset, wetlands are defined as land areas that are either permanently or seasonally saturated, excluding small ponds, lakes, and coastal wetlands. These wetland CH4 flux data will be used to support the United States Greenhouse Gas Center (&lt;a href&#x3D;&quot;https://earth.gov/ghgcenter&quot;&gt;GHGC&lt;/a&gt;) and its mission to study natural GHG fluxes. The model will also be used to facilitate improved rapid detection and attribution of climate-carbon feedback and help with strategic placement of measurement campaigns and monitoring systems as they relate to predicted biogeochemical hotspots. The LPJ-EOSIM Level 2 Global Simulated Daily Wetland Methane Flux Low Latency (LPJ_EOSIM_L2_DCH4E_LL) Version 1 data product provides simulated daily wetland CH4 flux globally at a spatial resolution of 0.5 degrees. The daily data are presented in four Cloud Optimized GeoTIFF (COG) files: two based on the forcing datasets Modern-Era Retrospective analysis for Research and Applications Version 2 (MERRA-2) and European Centre for Medium-Range Weather Forecasts (ECMWF) Re-Analysis (ERA5), and two containing the mean and standard deviation values. Due to the latency of global carbon dioxide (CO2) concentration estimates required for computation of LPJ-EOSIM simulated daily CH4 flux data products, low latency (LPJ_EOSIM_L2_DCH4E_LL) and high latency (&lt;a href&#x3D;&quot;https://doi.org/10.5067/Community/LPJ-EOSIM/LPJ_EOSIM_L2_DCH4E.001&quot;&gt;LPJ_EOSIM_L2_DCH4E&lt;/a&gt;) collections are available. Low latency data are delivered on a two-month cadence throughout the year. Granules will also be updated as new CO2 input data become available. Please refer to Section 2.0.1 of the User Guide for a more detailed explanation of CO2 estimate inputs and timing for scheduled updates to the collections.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.lpdaac.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA Landslide Project Project</title>
      <link>https://registry.opendata.aws/nasa-landslide-project</link>
      <guid>https://registry.opendata.aws/nasa-landslide-project</guid>
      <description>The Landslide Hazard Assessment for Situational Awareness (LHASA) model identifies locations with high potential for landslide occurrence at a daily temporal resolution. LHASA combines satellite‐based precipitation estimates with a landslide susceptibility map derived from information on slope, geology, road networks, fault zones, and forest loss. When rainfall is considered to be extreme and susceptibility values are moderate to very high, a “nowcast” is issued to indicate the times and places where landslides are more probable. Although the model could be run every half hour, this archive contains a daily record derived from a retrospective model run and spatial coverage is from 60°N to 60°S .
&lt;br&gt;&lt;h4 id&#x3D;&quot;global_landslide_nowcast&quot;&gt;Global_Landslide_Nowcast&lt;/h4&gt;
The Global Landslide Nowcast addresses the need for real-time situational awareness of landslide hazard. The Landslide Hazard Assessment for Situational Awareness model (LHASA) combines satellite rainfall estimates from the Global Precipitation Measurement mission (GPM) with soil moisture estimates from the Soil Moisture Active Passive (SMAP) satellite and other factors to produce a map of locations where rainfall-triggered landslide activity is probable. Due to the latency of the rainfall data, the nowcast is a near-real time product with a minimum latency of 5 hours. Although the model could be run every half hour, this archive contains a daily record derived from a retrospective model run. The Global Landslide Nowcast version 2.0.0 retains replaces the heuristic decision tree from version 1.0 with a machine learning model. Instead of merging all factors other than precipitation into a susceptibility map, LHASA 2.0 takes in each variable as a separate input layer. The most important change is the replacement of the categorical nowcast with a probabilistic output. This will enable users to adjust the threshold to suit their specific application and geographic location.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA Low-Cost Sensor AQ Project</title>
      <link>https://registry.opendata.aws/nasa-low-cost-sensor-aq</link>
      <guid>https://registry.opendata.aws/nasa-low-cost-sensor-aq</guid>
      <description>Low-Cost-Sensors-AQ_AirQino is the ground site data collected by the AirQino sensor network as part of the Low-Cost Air Quality Sensor Harmonization Database. Data collection for this product is ongoing. The Low-Cost Sensor AQ Harmonization aims to harmonize sensor networks by amalgamating measurements from a multitude of networks into one open access framework. Currently, data from 10 unique US-based sensor networks have been collected for redistribution in the archive. Data from each network is reformatted in a common data format with metadata embedded to streamline data processing. A key feature is a tier system in which the team critically reviews each sensor network by their calibration efforts and subsequent data quality, providing data quality flags to help end users determine which sensor data best meets their target application. The framework allows users to search based on calibration criteria in addition to location, date range, and pollutant of interest. The sensor database is aimed at scientific end users seeking ground-based validation data for satellites and models alike but is also accessible to community scientists. The team is currently accepting new submissions! If you maintain a sensor network that you would like included, please contact the PI.
&lt;br&gt;&lt;h4 id&#x3D;&quot;low-cost-sensors-aq_beaco2n&quot;&gt;Low-Cost-Sensors-AQ_BEACO2N&lt;/h4&gt;
Low-Cost-Sensors-AQ_BEACO2N is the ground site data collected by the Berkeley Environmental Air-quality &amp;amp; CO2 Network (BEACO2N) as part of the Low-Cost Air Quality Sensor Harmonization Database. Data collection for this product is ongoing. The Low-Cost Sensor AQ Harmonization aims to harmonize sensor networks by amalgamating measurements from a multitude of networks into one open access framework. Currently, data from 10 unique US-based sensor networks have been collected for redistribution in the archive. Data from each network is reformatted in a common data format with metadata embedded to streamline data processing. A key feature is a tier system in which the team critically reviews each sensor network by their calibration efforts and subsequent data quality, providing data quality flags to help end users determine which sensor data best meets their target application. The framework allows users to search based on calibration criteria in addition to location, date range, and pollutant of interest. The sensor database is aimed at scientific end users seeking ground-based validation data for satellites and models alike but is also accessible to community scientists. The team is currently accepting new submissions! If you maintain a sensor network that you would like included, please contact the PI.
&lt;br&gt;&lt;h4 id&#x3D;&quot;low-cost-sensors-aq_haqpods&quot;&gt;Low-Cost-Sensors-AQ_HAQPods&lt;/h4&gt;
Low-Cost-Sensors-AQ_HAQPods is the ground site data collected by the Hannigan Air Quality Pods (HAQ Pods) sensor network as part of the Low-Cost Air Quality Sensor Harmonization Database. Data collection for this product is ongoing. The Low-Cost Sensor AQ Harmonization aims to harmonize sensor networks by amalgamating measurements from a multitude of networks into one open access framework. Currently, data from 10 unique US-based sensor networks have been collected for redistribution in the archive. Data from each network is reformatted in a common data format with metadata embedded to streamline data processing. A key feature is a tier system in which the team critically reviews each sensor network by their calibration efforts and subsequent data quality, providing data quality flags to help end users determine which sensor data best meets their target application. The framework allows users to search based on calibration criteria in addition to location, date range, and pollutant of interest. The sensor database is aimed at scientific end users seeking ground-based validation data for satellites and models alike but is also accessible to community scientists. The team is currently accepting new submissions! If you maintain a sensor network that you would like included, please contact the PI.
&lt;br&gt;&lt;h4 id&#x3D;&quot;low-cost-sensors-aq_instep&quot;&gt;Low-Cost-Sensors-AQ_INSTEP&lt;/h4&gt;
Low-Cost-Sensors-AQ_INSTEP is the ground site data collected by the Inexpensive Network Sensor Technology Exploring Pollution (INSTEP) sensor network as part of the Low-Cost Air Quality Sensor Harmonization Database. Data collection for this product is ongoing. The Low-Cost Sensor AQ Harmonization aims to harmonize sensor networks by amalgamating measurements from a multitude of networks into one open access framework. Currently, data from 10 unique US-based sensor networks have been collected for redistribution in the archive. Data from each network is reformatted in a common data format with metadata embedded to streamline data processing. A key feature is a tier system in which the team critically reviews each sensor network by their calibration efforts and subsequent data quality, providing data quality flags to help end users determine which sensor data best meets their target application. The framework allows users to search based on calibration criteria in addition to location, date range, and pollutant of interest. The sensor database is aimed at scientific end users seeking ground-based validation data for satellites and models alike but is also accessible to community scientists. The team is currently accepting new submissions! If you maintain a sensor network that you would like included, please contact the PI.
&lt;br&gt;&lt;h4 id&#x3D;&quot;low-cost-sensors-aq_love-my-air-denver&quot;&gt;Low-Cost-Sensors-AQ_Love-my-Air-Denver&lt;/h4&gt;
Low-Cost-Sensors-AQ_Love-my-Air-Denver is the ground site data collected by the Love my Air Denver sensor network as part of the Low-Cost Air Quality Sensor Harmonization Database. Data collection for this product is ongoing. The Low-Cost Sensor AQ Harmonization aims to harmonize sensor networks by amalgamating measurements from a multitude of networks into one open access framework. Currently, data from 10 unique US-based sensor networks have been collected for redistribution in the archive. Data from each network is reformatted in a common data format with metadata embedded to streamline data processing. A key feature is a tier system in which the team critically reviews each sensor network by their calibration efforts and subsequent data quality, providing data quality flags to help end users determine which sensor data best meets their target application. The framework allows users to search based on calibration criteria in addition to location, date range, and pollutant of interest. The sensor database is aimed at scientific end users seeking ground-based validation data for satellites and models alike but is also accessible to community scientists. The team is currently accepting new submissions! If you maintain a sensor network that you would like included, please contact the PI.
&lt;br&gt;&lt;h4 id&#x3D;&quot;low-cost-sensors-aq_love-my-air-wisconsin&quot;&gt;Low-Cost-Sensors-AQ_Love-my-Air-Wisconsin&lt;/h4&gt;
Low-Cost-Sensors-AQ_Love-my-Air-Wisconsin is the ground site data collected by the Love my Air Wisconsin sensor network as part of the Low-Cost Air Quality Sensor Harmonization Database. Data collection for this product is ongoing. The Low-Cost Sensor AQ Harmonization aims to harmonize sensor networks by amalgamating measurements from a multitude of networks into one open access framework. Currently, data from 10 unique US-based sensor networks have been collected for redistribution in the archive. Data from each network is reformatted in a common data format with metadata embedded to streamline data processing. A key feature is a tier system in which the team critically reviews each sensor network by their calibration efforts and subsequent data quality, providing data quality flags to help end users determine which sensor data best meets their target application. The framework allows users to search based on calibration criteria in addition to location, date range, and pollutant of interest. The sensor database is aimed at scientific end users seeking ground-based validation data for satellites and models alike but is also accessible to community scientists. The team is currently accepting new submissions! If you maintain a sensor network that you would like included, please contact the PI.
&lt;br&gt;&lt;h4 id&#x3D;&quot;low-cost-sensors-aq_mke-fresh-air&quot;&gt;Low-Cost-Sensors-AQ_MKE-Fresh-Air&lt;/h4&gt;
Low-Cost-Sensors-AQ_MKE-Fresh-Air is the ground site data collected by the MKE Fresh Air Collective sensor network as part of the Low-Cost Air Quality Sensor Harmonization Database. Data collection for this product is ongoing. The Low-Cost Sensor AQ Harmonization aims to harmonize sensor networks by amalgamating measurements from a multitude of networks into one open access framework. Currently, data from 10 unique US-based sensor networks have been collected for redistribution in the archive. Data from each network is reformatted in a common data format with metadata embedded to streamline data processing. A key feature is a tier system in which the team critically reviews each sensor network by their calibration efforts and subsequent data quality, providing data quality flags to help end users determine which sensor data best meets their target application. The framework allows users to search based on calibration criteria in addition to location, date range, and pollutant of interest. The sensor database is aimed at scientific end users seeking ground-based validation data for satellites and models alike but is also accessible to community scientists. The team is currently accepting new submissions! If you maintain a sensor network that you would like included, please contact the PI.
&lt;br&gt;&lt;h4 id&#x3D;&quot;low-cost-sensors-aq_ramp&quot;&gt;Low-Cost-Sensors-AQ_RAMP&lt;/h4&gt;
Low-Cost-Sensors-AQ_RAMP is the ground site data collected by the Real-Time Multi-Pollutant (RAMP) sensor network as part of the Low-Cost Air Quality Sensor Harmonization Database. Data collection for this product is ongoing. The Low-Cost Sensor AQ Harmonization aims to harmonize sensor networks by amalgamating measurements from a multitude of networks into one open access framework. Currently, data from 10 unique US-based sensor networks have been collected for redistribution in the archive. Data from each network is reformatted in a common data format with metadata embedded to streamline data processing. A key feature is a tier system in which the team critically reviews each sensor network by their calibration efforts and subsequent data quality, providing data quality flags to help end users determine which sensor data best meets their target application. The framework allows users to search based on calibration criteria in addition to location, date range, and pollutant of interest. The sensor database is aimed at scientific end users seeking ground-based validation data for satellites and models alike but is also accessible to community scientists. The team is currently accepting new submissions! If you maintain a sensor network that you would like included, please contact the PI.
&lt;br&gt;&lt;h4 id&#x3D;&quot;low-cost-sensors-aq_stair&quot;&gt;Low-Cost-Sensors-AQ_STAIR&lt;/h4&gt;
Low-Cost-Sensors-AQ_STAIR is the ground site data collected by the Smart and Trustworthy AIR quality network (STAIR) as part of the Low-Cost Air Quality Sensor Harmonization Database. Data collection for this product is ongoing. The Low-Cost Sensor AQ Harmonization aims to harmonize sensor networks by amalgamating measurements from a multitude of networks into one open access framework. Currently, data from 10 unique US-based sensor networks have been collected for redistribution in the archive. Data from each network is reformatted in a common data format with metadata embedded to streamline data processing. A key feature is a tier system in which the team critically reviews each sensor network by their calibration efforts and subsequent data quality, providing data quality flags to help end users determine which sensor data best meets their target application. The framework allows users to search based on calibration criteria in addition to location, date range, and pollutant of interest. The sensor database is aimed at scientific end users seeking ground-based validation data for satellites and models alike but is also accessible to community scientists. The team is currently accepting new submissions! If you maintain a sensor network that you would like included, please contact the PI.
&lt;br&gt;&lt;h4 id&#x3D;&quot;low-cost-sensors-aq_upc&quot;&gt;Low-Cost-Sensors-AQ_UPC&lt;/h4&gt;
Low-Cost-Sensors-AQ_UPC is the ground site data collected by the Universitat Politècnica of Catalunya (UPC), Spain sensor network as part of the Low-Cost Air Quality Sensor Harmonization Database. Data collection for this product is ongoing. The Low-Cost Sensor AQ Harmonization aims to harmonize sensor networks by amalgamating measurements from a multitude of networks into one open access framework. Currently, data from 10 unique US-based sensor networks have been collected for redistribution in the archive. Data from each network is reformatted in a common data format with metadata embedded to streamline data processing. A key feature is a tier system in which the team critically reviews each sensor network by their calibration efforts and subsequent data quality, providing data quality flags to help end users determine which sensor data best meets their target application. The framework allows users to search based on calibration criteria in addition to location, date range, and pollutant of interest. The sensor database is aimed at scientific end users seeking ground-based validation data for satellites and models alike but is also accessible to community scientists. The team is currently accepting new submissions! If you maintain a sensor network that you would like included, please contact the PI.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.asdc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA MASTER Project</title>
      <link>https://registry.opendata.aws/nasa-master</link>
      <guid>https://registry.opendata.aws/nasa-master</guid>
      <description>This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during 7 flights aboard a DOE B-200 aircraft over Baja California, Mexico, and Nevada, U.S., on 1999-04-23 to 1999-05-05. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 20-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rsl_october_2010_2127&quot;&gt;MASTER_RSL_October_2010_2127&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during six flights aboard a DOE B-200 aircraft over California, Arizona, and New Mexico, U.S., from 2010-10-04 to 2010-10-13. Objectives included mapping for California Fire-Burn Area Emergency Response (BAER) and Jornada Experimental Range in southern New Mexico (JORNEX). This deployment was coordinated by the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 10-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_houston_2011_1972&quot;&gt;MASTER_Houston_2011_1972&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during 16 flights aboard a NASA ER-2 aircraft over portions of California, Colorado, Wisconsin, Michigan, Louisiana, Mississippi, the central Mississippi River basin, and the Gulf of Mexico from 2011-07-19 to 2011-08-18. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes the flight path, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rsl_august_2007_2020&quot;&gt;MASTER_RSL_August_2007_2020&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during seven flights aboard a DOE B-200 aircraft over Nevada and California, U.S., from 2007-08-30 to 2007-09-02. This data collection focused on mapping earthquake faults in southern California. This deployment was coordinated by the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 10-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_dfrc_rsl_august_2002_2066&quot;&gt;MASTER_DFRC_RSL_August_2002_2066&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during three flights aboard a NASA ER-2 and two flights on a DOE B-200 aircraft over California and Nevada U.S. from 2002-08-09 to 2002-08-20. This deployment was coordinated by NASA&amp;#39;s Dryden Flight Research Center (DRFC), renamed Armstrong Flight Research Center in 2014, located in Edwards, California, and the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at spatial resolution of 10 to 50 m. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rsl_august_2004_2036&quot;&gt;MASTER_RSL_August_2004_2036&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during one flight aboard a DOE B-200 aircraft over California and Nevada, U.S., on 2004-08-18 to 2004-08-29. Objectives of this deployment included mapping geological faults in southern California. This deployment was coordinated by the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 20-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_dfrc_fall_2005_2030&quot;&gt;MASTER_DFRC_Fall_2005_2030&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during three flights aboard a NASA ER-2 aircraft over California and Nevada, U.S., from 2005-10-19 to 2005-12-09. This deployment was coordinated by NASA&amp;#39;s Dryden Flight Research Center (DRFC), renamed Armstrong Flight Research Center in 2014, located in Edwards, California. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rsl_june_2001_2090&quot;&gt;MASTER_RSL_June_2001_2090&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during seven flights aboard a DOE B-200 aircraft over California and Nevada, U.S., on 2001-06-06 to 2001-06-16. This deployment was coordinated by the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 20-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rsl_march_2000_2094&quot;&gt;MASTER_RSL_March_2000_2094&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during five flights aboard a DOE B-200 aircraft over California and Nevada, U.S., on 2000-03-10 to 2000-03-14. This deployment was coordinated by the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 20-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rsl_march_2002_2068&quot;&gt;MASTER_RSL_March_2002_2068&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during six flights aboard a DOE B-200 aircraft over California and Nevada, U.S., on 2002-03-08 to 2002-04-07. This deployment was coordinated by the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 10-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_dfrc_may-june_2008_2011&quot;&gt;MASTER_DFRC_May-June_2008_2011&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected as part of the Hyperspectral Infrared Imager (HyspIRI) mission&amp;#39;s preparatory airborne campaign during four flights aboard a NASA ER-2 aircraft over California and Nevada, U.S., from 2008-05-29 to 2008-06-19. This deployment was coordinated by NASA&amp;#39;s Dryden Flight Research Center (DRFC), renamed Armstrong Flight Research Center in 2014, located in Edwards, California. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rsl_may_1999_2101&quot;&gt;MASTER_RSL_May_1999_2101&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during a single flight aboard a DOE B-200 aircraft over California, Nevada, and Arizona, U.S., on 1999-05-11. This deployment was coordinated by the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 10-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rsl_may_2002_v2_2148&quot;&gt;MASTER_RSL_May_2002_V2_2148&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during seven flights aboard a DOE B-200 aircraft over California, New Mexico, and Nevada, U.S., on 2002-05-14 to 2002-05-24. This deployment was coordinated by the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 10-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rsl_june_2002_2067&quot;&gt;MASTER_RSL_June_2002_2067&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during seven flights aboard a DOE B-200 aircraft over California, Nevada and Utah, U.S., on 2002-06-07 to 2002-06-18. This deployment was coordinated by the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 20-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rsl_may_2001_v2_2145&quot;&gt;MASTER_RSL_May_2001_V2_2145&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during two flights aboard a DOE B-200 aircraft over California and New Mexico, U.S., on 2001-05-11 to 2001-05-12. This deployment was coordinated by the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 10-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rsl_october_2005_2031&quot;&gt;MASTER_RSL_October_2005_2031&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during one flight aboard a DOE B-200 aircraft over Catalina Island, California, U.S., on 2005-10-31. This deployment was coordinated by the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 7-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_hawaii_october_2001_v2_2142&quot;&gt;MASTER_Hawaii_October_2001_V2_2142&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during 19 flights aboard a NASA ER-2 aircraft over Hawaii, eastern Pacific Ocean, and western U.S. from 2001-10-14 to 2001-11-14. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes the flight path, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rsl_july_2003_2047&quot;&gt;MASTER_RSL_July_2003_2047&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during three flights aboard a DOE B-200 aircraft over Nevada, U.S., on 2003-07-14 to 2003-07-22. This deployment was coordinated by the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 20-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rsl_july_2004_2038&quot;&gt;MASTER_RSL_July_2004_2038&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during one functional check flight aboard a DOE B-200 aircraft over Nevada, U.S., on 2004-07-29. This deployment was coordinated by the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 5-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rsl_may_2006_2029&quot;&gt;MASTER_RSL_May_2006_2029&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during five flights aboard a DOE B-200 aircraft over Nevada, U.S., from 2006-05-26 to 2006-06-01. This deployment was coordinated by the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 10-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_sky_2006_2026&quot;&gt;MASTER_Sky_2006_2026&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during two flights aboard a Cessna Caravan aircraft over Oregon and Wyoming, U.S., from 2006-08-01 to 2006-08-03. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 10-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rsl_august_2006_2027&quot;&gt;MASTER_RSL_August_2006_2027&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during 18 flights aboard a DOE B-200 aircraft over Nevada, California and Colorado, U.S., from 2006-08-21 to 2006-09-06. This data collection focused on mapping geological faults. This deployment was coordinated by the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 10-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_dfrc_june_2011_1976&quot;&gt;MASTER_DFRC_June_2011_1976&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during 6 flights aboard a NASA ER-2 aircraft over southwestern U.S. and northern Mexico, from 2011-06-08 to 2011-06-20. The purposes of these flights include collecting data for wildfire mapping, airborne science initiatives, and calibration data for AVIRIS. This deployment was coordinated by NASA&amp;#39;s Dryden Flight Research Center (DRFC), renamed Armstrong Flight Research Center in 2014, located in Edwards, California. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes the flight path, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_dfrc_may_2011_1985&quot;&gt;MASTER_DFRC_May_2011_1985&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during five flights aboard a NASA ER-2 aircraft over southwestern U.S., from 2011-05-15 to 2011-05-23. This deployment was coordinated by NASA&amp;#39;s Dryden Flight Research Center (DRFC), renamed Armstrong Flight Research Center in 2014, located in Edwards, California. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes the flight path, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_dfrc_november_2011_1973&quot;&gt;MASTER_DFRC_November_2011_1973&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during seven flights aboard a NASA ER-2 aircraft over southwestern U.S. from 2011-11-02 to 2011-11-16. This deployment was coordinated by NASA&amp;#39;s Dryden Flight Research Center (DRFC), renamed Armstrong Flight Research Center in 2014, located in Edwards, California. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. The L1B file formats are HDF-4 and KMZ. In addition, the dataset includes the flight path, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rsl_september_2005_2037&quot;&gt;MASTER_RSL_September_2005_2037&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during two flights aboard a DOE B-200 aircraft over Arizona, California, and Nevada, U.S., on 2005-09-27 to 2005-09-29. This deployment was coordinated by the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 5-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rsl_june_2000_2096&quot;&gt;MASTER_RSL_June_2000_2096&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during 12 flights aboard a DOE B-200 aircraft over California, Nevada, Arizona, and New Mexico, U.S., on 2000-06-01 to 2000-06-17. This deployment was coordinated by the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 20-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_dfrc_september_2002_2064&quot;&gt;MASTER_DFRC_September_2002_2064&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during 11 flights aboard a NASA ER-2 aircraft over southwestern U.S. from 2002-09-10 to 2002-09-26. This deployment was coordinated by NASA&amp;#39;s Dryden Flight Research Center (DRFC), renamed Armstrong Flight Research Center in 2014, located in Edwards, California. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_dfrc_april_2004_2043&quot;&gt;MASTER_DFRC_April_2004_2043&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during four flights aboard a NASA ER-2 aircraft over western U.S. and Pacific Ocean from 2004-04-01 to 2004-04-13. This deployment was coordinated by NASA&amp;#39;s Dryden Flight Research Center (DRFC), renamed Armstrong Flight Research Center in 2014, located in Edwards, California. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rsl_august_2001_v2_2143&quot;&gt;MASTER_RSL_August_2001_V2_2143&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during 11 flights aboard a DOE B-200 aircraft over California, Nevada, Oregon, and Washington, U.S., on 2001-08-22 to 2001-08-31. This deployment was coordinated by the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 20-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_dfrc_july-aug_2001_v2_2144&quot;&gt;MASTER_DFRC_July-Aug_2001_V2_2144&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during three flights aboard a NASA ER-2 aircraft over California, Nevada, Oregon, Washington, U.S., and British Columbia, Canada, from 2001-07-20 to 2001-08-18. This deployment was coordinated by NASA&amp;#39;s Dryden Flight Research Center (DRFC), renamed Armstrong Flight Research Center in 2014, located in Edwards, California. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rsl_june_1999_2098&quot;&gt;MASTER_RSL_June_1999_2098&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during 10 flights aboard a DOE B-200 aircraft over California, Nevada, Arizona, New Mexico, and Texas, U.S., on 1999-05-28 to 1999-06-10. This deployment was coordinated by the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 20-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rsl_may_2004_2041&quot;&gt;MASTER_RSL_May_2004_2041&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during five flights aboard a DOE B-200 aircraft over New Mexico, California, Utah, and Colorado, U.S., on 2004-05-20 to 2004-05-25. This deployment was coordinated by the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 15-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_dfrc_october_2003_2044&quot;&gt;MASTER_DFRC_October_2003_2044&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during eight flights aboard a NASA ER-2 aircraft over western U.S. and Pacific Ocean on 2003-10-03 to 2003-11-01. This deployment was coordinated by NASA&amp;#39;s Dryden Flight Research Center (DRFC), renamed Armstrong Flight Research Center in 2014, located in Edwards, California. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_sky_2004_2035&quot;&gt;MASTER_Sky_2004_2035&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during 11 flights aboard a Cessna Caravan aircraft over California, Oregon, Washington, and Colorado, U.S., from 2004-09-15 to 2004-10-14. A focus of this deployment involved mapping volcanic landforms. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 10-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_dfrc_september_2006_2022&quot;&gt;MASTER_DFRC_September_2006_2022&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during two flights aboard a NASA ER-2 aircraft over California, Nevada, Wyoming, Utah, Colorado, Nebraska, South Dakota, Wisconsin, and Minnesota, U.S., from 2006-09-19 to 2006-10-13. This deployment was coordinated by NASA&amp;#39;s Dryden Flight Research Center (DRFC), renamed Armstrong Flight Research Center in 2014, located in Edwards, California. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_b200_fall_1999_2099&quot;&gt;MASTER_B200_Fall_1999_2099&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during 18 flights aboard a DOE B-200 aircraft over California, Nevada, Arizona, New Mexico, Washington, Colorado, and Texas, U.S., on 1999-09-13 to 1999-10-06. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 20-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_houston_2010_2126&quot;&gt;MASTER_Houston_2010_2126&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The raw data were collected during 9 flights aboard a NASA ER-2 aircraft over the Gulf of America and portions of California, Colorado, Arizona, Utah, Idaho, New Mexico, Texas, Arkansas, Illinois, Wisconsin, Michigan, Louisiana, Mississippi, and Florida from 2010-07-31 to 2010-09-01. A primary purpose of this deployment was to collect imagery related to the Deepwater Horizon-BP Oil Spill that occurred in late April 2010 in the Gulf of America. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes the flight path, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_dfrc_june_1999_2100&quot;&gt;MASTER_DFRC_June_1999_2100&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during two flights aboard a DC-8 aircraft and one flight on a NASA ER-2 aircraft over California, Nevada, and eastern Pacific Ocean on 1999-06-18 to 1999-06-30. The objectives of this deployment included validation and cross-calibration of the instrument on the two airborne platforms. This deployment was coordinated by NASA&amp;#39;s Dryden Flight Research Center (DRFC), renamed Armstrong Flight Research Center in 2014, located in Edwards, California. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at spatial resolution of 7 to 50 meters. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rsl_april_2008_2016&quot;&gt;MASTER_RSL_April_2008_2016&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected as part of the Hyperspectral Infrared Imager (HyspIRI) mission&amp;#39;s preparatory airborne campaign during four flights aboard a DOE B-200 aircraft over California, U.S., 2008-04-14 to 2008-04-26. The locations sampled include areas affected by wildfires in 2007. This deployment was coordinated by the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 10-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rsl_august_2008_2010&quot;&gt;MASTER_RSL_August_2008_2010&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during four flights aboard a DOE B200 aircraft over California, U.S., from 2008-08-20 to 2008-08-27. Objectives included mapping for California Fire-Burn Area Emergency Response (BAER). This deployment was coordinated by the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 10-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rsl_november_2007_2015&quot;&gt;MASTER_RSL_November_2007_2015&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during six flights aboard a DOE B-200 aircraft over California, U.S., from 2007-11-05 to 2007-11-15. This data collection focused on mapping area affected by wildfires in southern California. This deployment was coordinated by the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 10-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_clasic_2007_2019&quot;&gt;MASTER_CLASIC_2007_2019&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during two flights aboard a NASA ER-2 aircraft over California, Arizona, New Mexico, Texas, and Oklahoma, U.S., from 2007-09-20 to 2007-09-21. This data collection supported the Cloud And Land Surface Interaction Campaign (CLASIC), a cross-disciplinary interagency research effort to study cumulus convection as an important component in the atmospheric radiation budget and hydrologic cycle of the Southern Great Plains (SGP). Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_carta_2005_2034&quot;&gt;MASTER_CARTA_2005_2034&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during 23 flights aboard a NASA WB-57 aircraft over Costa Rica on 2005-03-01 to 2005-04-06. The CARTA-2005 project was a collaborative effort between the Centro Nacional de Alta Tecnologia (CENAT) of Costa Rica and NASA. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 10-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_carta_2003_2054&quot;&gt;MASTER_CARTA_2003_2054&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during 14 flights aboard a NASA WB-57 aircraft over Texas, U.S., Gulf of Mexico, and Costa Rica on 2003-03-06 to 2003-03-29. The CARTA-2003 project was a collaborative effort between the Centro Nacional de Alta Tecnologia (CENAT) of Costa Rica and NASA. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 30-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_dfrc_august_2003_2046&quot;&gt;MASTER_DFRC_August_2003_2046&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during eight flights aboard a NASA ER-2 aircraft over California, U.S., on 2003-08-05 to 2003-08-11. The objective of this deployment was farmland mapping. This deployment was coordinated by NASA&amp;#39;s Dryden Flight Research Center (DRFC), renamed Armstrong Flight Research Center in 2014, located in Edwards, California. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_firesense_spring_2025_2439&quot;&gt;MASTER_FireSense_Spring_2025_2439&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected as part of the FireSense project during 7 flights aboard a NASA B200 aircraft over California, Alabama, Georgia and Florida, U.S., 2025-03-17 to 2025-04-18. The FireSense project is focused on delivering NASA&amp;#39;s unique Earth science and technological capabilities to operational agencies, striving towards measurable improvement in US wildland fire management. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 10-meter spatial resolution. The L1B file format is HDF-4, and L2 products are provided in HDF-5 and KMZ formats. In addition, the dataset includes the flight path, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_firesense_2023_2330&quot;&gt;MASTER_FireSense_2023_2330&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected as part of the FireSense project during 11 flights aboard a NASA B200 aircraft over California, Nevada, Utah, and Arizona, U.S., 2023-10-16 to 2023-10-26. The FireSense project is focused on delivering NASA&amp;#39;s unique Earth science and technological capabilities to operational agencies, striving towards measurable improvement in US wildland fire management. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 10-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_firex_aq_julysept_2019_1941&quot;&gt;MASTER_FIREX_AQ_JulySept_2019_1941&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected as part of the Fire Influence on Regional to Global Environments and Air Quality (FIREX-AQ) program during 21 flights aboard a NASA DC-8 aircraft over the central and western U.S. from 2019-07-22 to 2019-09-03. The purpose of these flights was to measure emissions and to characterize the aerosols in the smoke plume above and downwind of the fire, and to determine the overall spatial extent of wildfires and prescribed fires. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 20-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes the flight path, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_flightline_locator_2151&quot;&gt;MASTER_Flightline_Locator_2151&lt;/h4&gt;
This dataset provides resources for identifying flight lines of interest for the MODIS/ASTER Airborne Simulator (MASTER) instrument based on spatial and temporal criteria. MASTER first flew in 1998 and has ongoing deployments as a Facility Instrument in the NASA Airborne Science Program (ASP). MASTER is a joint project involving the Airborne Sensor Facility (ASF) at the Ames Research Center, the Jet Propulsion Laboratory (JPL), and the Earth Resources Observation and Science Center (EROS). The primary goal of these airborne campaigns is to demonstrate important science and applications research that is uniquely enabled by the full suite of MASTER thermal infrared bands as well as the contiguous spectroscopic measurements of the AVIRIS (also flown in similar campaigns), or combinations of measurements from both instruments. This dataset includes a table of flight lines with dates, bounding coordinates, site names, investigators involved, flight attributes, and associated campaigns for the MASTER Facility Instrument Collection. A shapefile containing flights for all years, a GeoJSON version of the shapefile, and separate KMZ files for all years allow users to visualize flight line locations using GIS software.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_sky_2003_2052&quot;&gt;MASTER_Sky_2003_2052&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during a single flight aboard a Cessna Caravan aircraft over California and Nevada, U.S., on 2003-05-31. The purpose of this deployment was a functional check flight. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 10-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for the flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_gemx_summer_2023_2319&quot;&gt;MASTER_GEMx_Summer_2023_2319&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during 13 flights aboard a NASA ER-2 aircraft over California, Oregon, Nevada, and Arizona, US, from 2023-04-25 to 2023-09-26. The Geological Earth Mapping Experiment (GEMx) research project used NASA&amp;#39;s Airborne Visible/Infrared Imaging Spectrometer (AVIRIS), Hyperspectral Thermal Emission Spectrometer (HyTES), and MODIS/ASTER Airborne Simulator (MASTER) instruments to collect the measurements over the country&amp;#39;s arid and semi-arid regions, including parts of California, Nevada, Arizona, and New Mexico, to map portions of southwest US for critical minerals. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in five bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes the flight path, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_gemx_spring_2024_2370&quot;&gt;MASTER_GEMx_Spring_2024_2370&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during 26 flights aboard a NASA ER-2 aircraft over California, Oregon, Nevada, and Arizona, US, from 2024-04-02 to 2024-06-24. The Geological Earth Mapping Experiment (GEMx) research project used NASA&amp;#39;s Airborne Visible/Infrared Imaging Spectrometer (AVIRIS), Hyperspectral Thermal Emission Spectrometer (HyTES), and MODIS/ASTER Airborne Simulator (MASTER) instruments to collect the measurements over the country&amp;#39;s arid and semi-arid regions, including parts of California, Nevada, Arizona, and New Mexico, to map portions of southwest US for critical minerals. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in five bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes the flight path, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_gemx_summer_2025_2472&quot;&gt;MASTER_GEMx_Summer_2025_2472&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during 29 flights aboard a NASA ER-2 aircraft over California, Oregon, Nevada, and Arizona, US, from 2025-05-23 to 2025-09-23. The Geological Earth Mapping Experiment (GEMx) research project used NASA&amp;#39;s Airborne Visible/Infrared Imaging Spectrometer (AVIRIS), Hyperspectral Thermal Emission Spectrometer (HyTES), and MODIS/ASTER Airborne Simulator (MASTER) instruments to collect the measurements over the country&amp;#39;s arid and semi-arid regions, including parts of California, Nevada, Arizona, and New Mexico, to map portions of southwest US for critical minerals. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in five bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in HDF-5 and KMZ formats. In addition, the dataset includes the flight path, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rsl_october_2003_2048&quot;&gt;MASTER_RSL_October_2003_2048&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during six flights aboard a DOE B-200 aircraft over California and Nevada, U.S., on 2003-10-05 to 2003-10-12. An objective of this deployment was geological fault mapping. This deployment was coordinated by the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 10-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rsl_june_2004_2042&quot;&gt;MASTER_RSL_June_2004_2042&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during two flights aboard a DOE B-200 aircraft over Colorado and Utah, U.S., on 2004-07-01. Objectives of this deployment included mapping geological substrates and their mineral content. This deployment was coordinated by the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 10-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rslphoenix_2011_1975&quot;&gt;MASTER_RSLPhoenix_2011_1975&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during five flights aboard a B-200 aircraft over Phoenix, Arizona, and Lake Mead, Nevada from 2011-07-11 to 2011-07-16 as part of a study on urban heat islands. This deployment was coordinated by the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 5-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes the flight path, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_hyspiri_summer_2016_1913&quot;&gt;MASTER_HyspIRI_Summer_2016_1913&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The data were collected as part of the Hyperspectral Infrared Imager (HyspIRI) mission&amp;#39;s preparatory airborne campaign during 6 flights aboard a NASA ER-2 aircraft over California and Nevada, U.S., from 2016-06-09 to 2016-06-21. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes the flight path, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_hyspiri_fall_2015_1956&quot;&gt;MASTER_HyspIRI_Fall_2015_1956&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected as part of the Hyperspectral Infrared Imager (HyspIRI) mission&amp;#39;s preparatory airborne campaign during seven flights aboard a NASA ER-2 aircraft over California and Nevada, U.S., from 2015-08-24 to 2015-10-26. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes the flight path, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_hyspiri_summer_2015_1959&quot;&gt;MASTER_HyspIRI_Summer_2015_1959&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected as part of the Hyperspectral Infrared Imager (HyspIRI) mission&amp;#39;s preparatory airborne campaign during six flights aboard a NASA ER-2 aircraft over California and Nevada, U.S., from 2015-05-28 to 2015-06-11. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_hyspiri_summer_2017_1950&quot;&gt;MASTER_HyspIRI_Summer_2017_1950&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected as part of the Hyperspectral Infrared Imager (HyspIRI) airborne campaign during 9 flights aboard a NASA ER-2 aircraft over southern California and western Nevada, U.S., from 2017-06-07 to 2017-06-28. Two flights on 2017-06-26 and 2017-06-28 were flown jointly for the Student Airborne Research Program (SARP). SARP was an eight-week summer program for junior and senior undergraduate students to acquire hands-on research experience in all aspects of a scientific campaign using airborne science laboratories. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_hyspiri_earlys2013_v2_2146&quot;&gt;MASTER_HyspIRI_EarlyS2013_V2_2146&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected as part of the Hyperspectral Infrared Imager (HyspIRI) mission&amp;#39;s preparatory airborne campaign during 6 flights aboard a NASA ER-2 aircraft over California and Nevada, U.S., from 2013-03-26 to 2013-04-19. An additional purpose of this campaign was an underpass of Landsat 8. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes the flight path, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_hyspiri_earlyspring2014_1965&quot;&gt;MASTER_HyspIRI_EarlySpring2014_1965&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected as part of the Hyperspectral Infrared Imager (HyspIRI) mission&amp;#39;s preparatory airborne campaign during 10 flights aboard a NASA ER-2 aircraft over California and Nevada, U.S., from 2014-03-31 to 2014-05-07. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes the flight path, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_hyspiri_fall_2013_1966&quot;&gt;MASTER_HyspIRI_Fall_2013_1966&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The raw data were collected as part of the Hyperspectral Infrared Imager (HyspIRI) mission&amp;#39;s preparatory airborne campaign during 11 flights aboard a NASA ER-2 aircraft over California and Nevada, U.S., from 2013-09-13 to 2013-12-05. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes the flight path, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_hyspiri_fall_2014_1962&quot;&gt;MASTER_HyspIRI_Fall_2014_1962&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected as part of the Hyperspectral Infrared Imager (HyspIRI) mission&amp;#39;s preparatory airborne campaign during seven flights aboard a NASA ER-2 aircraft over California and Nevada, U.S., from 2014-09-19 to 2014-11-24. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes the flight path, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_hyspiri_latespring_2013_1968&quot;&gt;MASTER_HyspIRI_LateSpring_2013_1968&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The raw data were collected as part of the Hyperspectral Infrared Imager (HyspIRI) mission&amp;#39;s preparatory airborne campaign during 7 flights aboard a NASA ER-2 aircraft over California and Nevada, U.S., from 2013-05-02 to 2013-06-26. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_hyspiri_latespring_2014_1963&quot;&gt;MASTER_HyspIRI_LateSpring_2014_1963&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected as part of the Hyperspectral Infrared Imager (HyspIRI) mission&amp;#39;s preparatory airborne campaign during seven flights aboard a NASA ER-2 aircraft over California and Nevada, U.S., from 2014-05-28 to 2014-06-13. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_hyspiri_spring_2015_1957&quot;&gt;MASTER_HyspIRI_Spring_2015_1957&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected as part of the Hyperspectral Infrared Imager (HyspIRI) mission&amp;#39;s preparatory airborne campaign during six flights aboard a NASA ER-2 aircraft over California and Nevada, U.S., from 2015-04-16 to 2015-05-05. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_hyspiri_summer_2014_1964&quot;&gt;MASTER_HyspIRI_Summer_2014_1964&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected as part of the Hyperspectral Infrared Imager (HyspIRI) mission&amp;#39;s preparatory airborne campaign during four flights aboard a NASA ER-2 aircraft over California, U.S., from 2014-08-18 to 2014-08-29. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_hyspiri_hawaii_2017_1951&quot;&gt;MASTER_HyspIRI_Hawaii_2017_1951&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected as part of the Hyperspectral Infrared Imager (HyspIRI) airborne campaign during 18 flights aboard a NASA ER-2 aircraft over Hawaii, California and Nevada, U.S., from 2016-12-14 to 2017-03-03. This deployment includes imagery of Hawaii&amp;#39;s volcanoes. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_hyspiri_hawaii_2018_1945&quot;&gt;MASTER_HyspIRI_Hawaii_2018_1945&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected as part of the Hyperspectral Infrared Imager (HyspIRI) airborne campaign during 12 flights aboard a NASA ER-2 aircraft over Hawaii and southern California, U.S., from 2018-01-11 to 2018-02-20. This campaign includes imagery of Hawaii&amp;#39;s volcanoes. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes the flight path, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_hyspiri_summer_2018_1942&quot;&gt;MASTER_HyspIRI_Summer_2018_1942&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected as part of the Hyperspectral Infrared Imager (HyspIRI) mission&amp;#39;s preparatory airborne campaign during 15 flights aboard a NASA ER-2 aircraft over California, Arizona, Oregon, and Nevada, U.S., from 2018-06-19 to 2018-09-06. Two flights on 2018-06-20 and 2018-06-27 were flown jointly with Student Airborne Research Program (SARP). SARP was an eight-week summer program for junior and senior undergraduate students to acquire hands-on research experience in all aspects of a scientific campaign using airborne science laboratories. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes the flight path, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rsl_january_1999_2103&quot;&gt;MASTER_RSL_January_1999_2103&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during a single flight aboard a DOE B-200 aircraft over California, U.S., on 1999-01-17. A primary objective of this deployment was instrument validation. This deployment was coordinated by the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 20-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rsl_december_1998_2104&quot;&gt;MASTER_RSL_December_1998_2104&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during a single flight aboard a DOE B-200 aircraft over California and Nevada, U.S., on 1998-12-02. A primary objective of this deployment was instrument validation. This deployment was coordinated by the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 10-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_ames_august_2003_2045&quot;&gt;MASTER_Ames_August_2003_2045&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during a single flight aboard a NASA WB-57 aircraft over California, Nevada, Oregon, and Washington, U.S., on 2003-08-27. This deployment was an instrument validation flight. Imagery was collected over the Cascade Mountains and Lake Tahoe. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 25-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight path, spectral band information, instrument configuration, ancillary notes, and summary information for the flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rsl_oct_2002_v2_2147&quot;&gt;MASTER_RSL_Oct_2002_V2_2147&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during nine flights aboard a DOE B-200 aircraft over Arizona, California, Nevada and New Mexico, U.S., on 2002-10-01 to 2002-10-08. Flights included coverage of the Jornada Experimental Range (JORNEX) in New Mexico. This deployment was coordinated by the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 15-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rsl_april_2003_2053&quot;&gt;MASTER_RSL_April_2003_2053&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during three flights aboard a DOE B-200 aircraft over Phoenix, Arizona, and the Jornada Experimental Range (JORNEX) in New Mexico, U.S., on 2003-04-28 to 2003-05-02. These data were used to evaluate theÃƒÂƒÃ‚Â‚ÃƒÂ‚Ã‚Â Temperature Emissivity Separation (TES) algorithm for extracting land surface temperature and emissivity data from thermal infrared data from ASTER. This deployment was coordinated by the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 10-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rsl_october_2007_2013&quot;&gt;MASTER_RSL_October_2007_2013&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during four flights aboard a DOE B-200 aircraft over Nevada, Arizona, and New Mexico, U.S., from 2007-10-01 to 2007-10-04. A focus of this data collection was the USDA Jornada Experimental Range (Jornada) in southern New Mexico. To complement the programs of ground measurements, JORNEX (JORNada EXperiment) began in 1995 to collect remotely sensed data from aircraft and satellite platforms to provide spatial and temporal data on physical and biological states of the Jornada rangeland. JORNEX uses remote sensing techniques to study arid rangeland and the responses of vegetation to changing hydrologic fluxes and atmospheric driving forces. This deployment was coordinated by the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 10-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_rsl-dfrc_october_2008_2014&quot;&gt;MASTER_RSL-DFRC_October_2008_2014&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected as part of the Hyperspectral Infrared Imager (HyspIRI) mission&amp;#39;s preparatory airborne campaign during four flights aboard a DOE B-200 and a NASA ER-2 aircraft over California and New Mexico, U.S., 2008-10-20 to 2008-10-29. A focus of this data collection was the USDA Jornada Experimental Range (Jornada) in southern New Mexico. To complement the programs of ground measurements, JORNEX (JORNada EXperiment) began in 1995 to collect remotely sensed data from aircraft and satellite platforms to provide spatial and temporal data on physical and biological states of the Jornada rangeland. JORNEX uses remote sensing techniques to study arid rangeland and the responses of vegetation to changing hydrologic fluxes and atmospheric driving forces. This deployment was coordinated by NASA&amp;#39;s Dryden Flight Research Center (DRFC), renamed Armstrong Flight Research Center in 2014, located in Edwards, California, and the U.S. Department of Energy&amp;#39;s Remote Sensing Laboratory (RSL) located at Nellis Air Force Base near Las Vegas, Nevada. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 30-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_pacificrim_2000_2093&quot;&gt;MASTER_PacificRim_2000_2093&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during 46 flights aboard a NASA DC-8 aircraft over sites encompassing the Pacific Rim, including Alaska, California, Hawaii, islands of the south and western Pacific Ocean, New Zealand, Australia, Polynesia, southeast Asia, South Korea, and Japan. Flights took place on 2000-07-21 to 2000-10-23. The Pacific Rim 2000 (PacRim II) Campaign gathered geographic and atmospheric data for coastal analysis, oceanography, forestry, geology, hydrology and archaeology of various regions using data from the Airborne Synthetic Aperture Radar (AirSAR) and MODIS/ASTER Airborne Simulator (MASTER) instruments. This was the first campaign to operate both the AIRSAR and MASTER instruments simultaneously, providing scientists with additional insight on how topography affects the vegetation and land surface temperature as seen in the MASTER data. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 25-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_sarp_2009_1990&quot;&gt;MASTER_SARP_2009_1990&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument collected and developed by the Student Airborne Research Program (SARP). The spectral data were collected from flights flown on 2009-07-22 to 2009-07-24 over southern California, U.S., in a NASA DC-8 aircraft. SARP was an eight-week summer program for junior and senior undergraduate students to acquire hands-on research experience in all aspects of a scientific campaign using airborne science laboratories. The SARP 2009 deployment included two flights with 11 flight tracks. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 20-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_sarp_2010_1989&quot;&gt;MASTER_SARP_2010_1989&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument collected and developed by the Student Airborne Research Program (SARP). The spectral data were collected from flights flown on 2010-06-28 to 2010-07-01 over southern California, U.S., in a NASA DC-8 aircraft. SARP was an eight-week summer program for junior and senior undergraduate students to acquire hands-on research experience in all aspects of a scientific campaign using airborne science laboratories. The SARP 2010 deployment included three flights with 21 flight tracks. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 10-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_sarp_2011_1974&quot;&gt;MASTER_SARP_2011_1974&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument collected and developed by the Student Airborne Research Program (SARP). The spectral data were collected from flights flown on 2011-06-27 to 2011-06-30 over southern California, U.S., in a NASA DC-8 aircraft. SARP was an eight-week summer program for junior and senior undergraduate students to acquire hands-on research experience in all aspects of a scientific campaign using airborne science laboratories. The SARP 2011 deployment included five flights with 23 flight tracks. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 10-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes the flight path, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_sarp_2012_1983&quot;&gt;MASTER_SARP_2012_1983&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument collected and developed by the Student Airborne Research Program (SARP). The spectral data were collected from flights flown on 2012-06-25 to 2012-06-27 over southern California, U.S., in a Lockheed P-3B Orion aircraft. SARP was an eight-week summer program for junior and senior undergraduate students to acquire hands-on research experience in all aspects of a scientific campaign using airborne science laboratories. The SARP 2012 deployment included five flights with 19 flight tracks. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 20-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_sarp_2013_1967&quot;&gt;MASTER_SARP_2013_1967&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument collected and developed by the Student Airborne Research Program (SARP). The spectral data were collected from flights flown on 2013-06-17 to 2013-06-19 over southern California, U.S., in a NASA DC-8 aircraft. The SARP 2013 deployment included four flights with 21 flight tracks. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 20-meter spatial resolution. The L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_sarp_2014_1961&quot;&gt;MASTER_SARP_2014_1961&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument collected and developed by the Student Airborne Research Program (SARP). The spectral data were collected from flights flown on 2014-06-23 to 2014-06-25 over southern California, U.S., in a NASA DC-8 aircraft. SARP was an eight-week summer program for junior and senior undergraduate students to acquire hands-on research experience in all aspects of a scientific campaign using airborne science laboratories. The SARP 2014 deployment included three flights with 17 flight tracks. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 20-meter spatial resolution, and the L1B file format is HDF-4. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_sarp_2015_1958&quot;&gt;MASTER_SARP_2015_1958&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument collected and developed by the Student Airborne Research Program (SARP). The raw spectral data were collected from flights flown on 2015-06-23 to 2015-06-24 over southern California, U.S., in a NASA DC-8 aircraft. SARP was an eight-week summer program for junior and senior undergraduate students to acquire hands-on research experience in all aspects of a scientific campaign using airborne science laboratories. The SARP 2015 deployment included three flights with 25 flight tracks. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 20-meter spatial resolution, and the L1B file format is HDF-4. In addition, the dataset includes the flight path, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_sarp_2016_1912&quot;&gt;MASTER_SARP_2016_1912&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument collected and developed by the Student Airborne Research Program (SARP). The spectral data were collected from flights flown on 2016-06-17 in a NASA ER-2 aircraft over Santa Barbara, California. SARP was an eight-week summer program for junior and senior undergraduate students to acquire hands-on research experience in all aspects of a scientific campaign using airborne science laboratories. The SARP 2016 deployment included one flight with 5 flight tracks. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_suominpp_2013_1969&quot;&gt;MASTER_SuomiNPP_2013_1969&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected for the Suomi National Polar-orbiting Partnership (Suomi-NPP) instrument validation airborne campaign during 11 flights aboard a NASA ER-2 aircraft over California, Texas, and Oklahoma, U.S.; Baja California, Mexico; and eastern Pacific Ocean from 2013-05-07 to 2013-06-01. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_suominpp_2015_1970&quot;&gt;MASTER_SuomiNPP_2015_1970&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected for the Suomi National Polar-orbiting Partnership (Suomi-NPP) instrument validation airborne campaign during 10 flights aboard a NASA ER-2 aircraft over Greenland, portions of the conterminous U.S., and Canada from 2015-02-23 to 2015-03-31. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_tc4_2007_2021&quot;&gt;MASTER_TC4_2007_2021&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during seven flights aboard a NASA ER-2 aircraft over California, Nevada, Central America, and eastern Pacific Ocean from 2007-07-29 to 2007-08-18. This deployment supported the Tropical Composition, Cloud and Climate Coupling Campaign (TC4), which investigated the atmospheric structure, properties, and processes in the Eastern Pacific Tropics. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_wh2ymsie_2024_2402&quot;&gt;MASTER_WH2yMSIE_2024_2402&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected as part of the Westcoast &amp;amp; Heartland Hyperspectral Microwave Sensor Intensive Experiment (WH2yMSIE) airborne campaign during 10 flights aboard a NASA ER-2 aircraft across the central US from Arkansas to California, U.S., and along the west coast and eastern Pacific Ocean. Flights occurred from 2024-10-18 to 2024-11-13. WH2yMSIE demonstrates the first-of-its-kind hyperspectral microwave airborne measurements and is complemented by other passive (infrared, visible) and active (lidar) sensors onboard the aircraft. It serves as a future NASA planetary boundary-layer (PBL) mission prototype and aims to capture a wide variety of thermodynamic, moisture, and PBL regimes across a variety of surface types. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in five bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in HDF-5 and KMZ formats. In addition, the dataset includes the flight path, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_wdts_septoct_2020_1940&quot;&gt;MASTER_WDTS_SeptOct_2020_1940&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected as part of the Western Diversity Time Series (WDTS, formerly HyspIRI) program during nine flights aboard a NASA ER-2 aircraft over selected areas of California, U.S, from 2020-09-17 to 2020-10-15. The WDTS program will observe California&amp;#39;s ecosystems and provide critical information on natural disasters such as volcanoes, wildfires, and drought. MASTER products can identify vegetation type and health and provide a benchmark for the state of the ecosystems against which future changes can be assessed. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes the flight path, spectral band information, instrument configuration, ancillary notes, and summary information for each deployment, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_wdts_spring_2021_1953&quot;&gt;MASTER_WDTS_Spring_2021_1953&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected as part of the Western Diversity Time Series (WDTS, formerly HyspIRI) airborne campaign during nine flights aboard a NASA ER-2 aircraft over selected areas of California and Nevada, U.S., from 2021-02-09 to 2021-04-02. The WDTS campaign will observe California&amp;#39;s ecosystems and provide critical information on natural disasters such as volcanoes, wildfires, and drought. MASTER products can identify vegetation type and health and provide a benchmark for the state of the ecosystems against which future changes can be assessed. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes the flight path, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_wdts_fall_2022_2141&quot;&gt;MASTER_WDTS_Fall_2022_2141&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected as part of the Western Diversity Time Series (WDTS, formerly HyspIRI) airborne campaign during five flights aboard a NASA ER-2 aircraft over California and Nevada, U.S., from 2022-09-02 to 2022-09-09. The WDTS campaign will observe California&amp;#39;s ecosystems and provide critical information on natural disasters such as volcanoes, wildfires, and drought. MASTER products can identify vegetation type and health and provide a benchmark for the state of the ecosystems against which future changes can be assessed. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes the flight path, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_wdts_spring_2023_2252&quot;&gt;MASTER_WDTS_Spring_2023_2252&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected as part of the Western Diversity Time Series (WDTS, formerly HyspIRI) airborne campaign during 12 flights aboard a NASA ER-2 aircraft over California and Nevada, U.S., from 2023-03-31 to 2023-05-02. The WDTS campaign will observe California&amp;#39;s ecosystems and provide critical information on natural disasters such as volcanoes, wildfires, and drought. MASTER products can identify vegetation type and health and provide a benchmark for the state of the ecosystems against which future changes can be assessed. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in five bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes the flight path, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_wdts_spring_2024_2383&quot;&gt;MASTER_WDTS_Spring_2024_2383&lt;/h4&gt;
This dataset includes Level 1B (L1B) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected as part of the Western Diversity Time Series (WDTS, formerly HyspIRI) airborne campaign during four flights aboard a NASA ER-2 aircraft over California and Nevada, U.S., from 2024-06-04 to 2024-06-28. The WDTS campaign will observe California&amp;#39;s ecosystems and provide critical information on natural disasters such as volcanoes, wildfires, and drought. MASTER products can identify vegetation type and health and provide a benchmark for the state of the ecosystems against which future changes can be assessed. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in five bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes the flight path, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_wdts_spring_2025_2471&quot;&gt;MASTER_WDTS_Spring_2025_2471&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected as part of the Western Diversity Time Series (WDTS, formerly HyspIRI) airborne campaign during seven flights aboard a NASA ER-2 aircraft over California and Nevada, U.S., from 2025-05-27 to 2025-07-17. The WDTS campaign will observe California&amp;#39;s ecosystems and provide critical information on natural disasters such as volcanoes, wildfires, and drought. MASTER products can identify vegetation type and health and provide a benchmark for the state of the ecosystems against which future changes can be assessed. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in five bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in HDF-5 and KMZ formats. In addition, the dataset includes the flight path, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;master_dfrc_july_2004_2039&quot;&gt;MASTER_DFRC_July_2004_2039&lt;/h4&gt;
This dataset includes Level 1B (L1B) and Level 2 (L2) data products from the MODIS/ASTER Airborne Simulator (MASTER) instrument. The spectral data were collected during two flights aboard a NASA ER-2 aircraft over California, U.S., from 2004-07-20 to 2004-07-21. The primary objective of this deployment was mapping of farmland and sites of recent wildfires. This deployment was coordinated by NASA&amp;#39;s Dryden Flight Research Center (DRFC), renamed Armstrong Flight Research Center in 2014, located in Edwards, California. Data products include L1B georeferenced multispectral imagery of calibrated radiance in 50 bands covering wavelengths of 0.460 to 12.879 micrometers at approximately 50-meter spatial resolution. Derived L2 data products are emissivity in 5 bands in thermal infrared range (8.58 to 12.13 micrometers) and land surface temperature. The L1B file format is HDF-4, and L2 products are provided in ENVI and KMZ formats. In addition, the dataset includes flight paths, spectral band information, instrument configuration, ancillary notes, and summary information for each flight, and browse images derived from each L1B data file.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.ornldaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA MAS_eMAS Project</title>
      <link>https://registry.opendata.aws/nasa-mas-emas</link>
      <guid>https://registry.opendata.aws/nasa-mas-emas</guid>
      <description>The Enhanced Moderate Resolution Imaging Spectroradiometer (MODIS) Airborne Simulator (eMAS)instrument is maintained and operated by the Airborne Sensor Facility at NASA Ames Research Center in Mountain View, California, under the oversight of the EOS Project Science Office at NASA Goddard. Prior to 1995, the MAS was deployed on the NASA&amp;#39;s ER-2 and C-130 aircraft platforms using a 12-channel, 8-bit data system that somewhat constrained the full benefit of having a 50-channel scanning spectrometer. Beginning in January 1995, a 50-channel, 16-bit digitizer was used on the ER-2 platform, which greatly enhanced the capability of MAS to simulate MODIS data over a wide range of environmental conditions. Recently, it has undergone extensive upgrades to the optics and other components. New detectors have been installed and the spectral bands have been streamlined. The eMAS instrument is now a 38-channel instrument, sensing in the range from 0.445 to 13.844 um. For more information and for a list of MAS campaign flights visit ladsweb at: &lt;a href&#x3D;&quot;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/mas/&quot;&gt;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/mas/&lt;/a&gt; or, visit the eMAS Homepage at: &lt;a href&#x3D;&quot;https://asapdata.arc.nasa.gov/emas/&quot;&gt;https://asapdata.arc.nasa.gov/emas/&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;emasl2aer&quot;&gt;eMASL2AER&lt;/h4&gt;
The Enhanced Moderate Resolution Imaging Spectroradiometer (MODIS) Airborne Simulator (eMAS)instrument is maintained and operated by the Airborne Sensor Facility at NASA Ames Research Center in Mountain View, California, under the oversight of the EOS Project Science Office at NASA Goddard. The eMAS instrument is now a 38-channel instrument, sensing in the range from 0.445 to 13.844 um. The Enhanced MODIS Airborne Simulator (eMAS) L2 Aerosol Data product (eMASL2AER) consists of in-situ measurements of trace gas and aerosol emissions for wildfires and prescribed fires in great detail, relate them to fuel and fire conditions at the point of emission, characterize the conditions relating to plume rise, follow plumes downwind to understand chemical transformation and air quality impacts, and assess the efficacy of satellite detections for estimating the emissions from sampled fires. These measurements were collected onboard the DC-8 aircraft during FIREX-AQ, during summer 2019. The DC-8 aircraft had a comprehensive instrument payload capable of measuring over 200 trace gases as well as aerosol microphysical, optical, and chemical properties. The eMASL2AER product files are stored in Hierarchical Data Format (HDF-EOS). All gridded cloud parameters are stored as Scientific Data Sets (SDS) within the file. For more information and for a list of MAS campaign flights visit ladsweb at: &lt;a href&#x3D;&quot;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/mas/&quot;&gt;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/mas/&lt;/a&gt; or, visit the eMAS Homepage at: &lt;a href&#x3D;&quot;https://asapdata.arc.nasa.gov/emas/&quot;&gt;https://asapdata.arc.nasa.gov/emas/&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;masl1b&quot;&gt;MASL1B&lt;/h4&gt;
The Moderate Resolution Imaging Spectroradiometer (MODIS) Airborne Simulator (MAS) sensor was developed for NASA&amp;#39;s high-altitude ER-2 research aircraft by Daedalus Enterprises, Inc., in support of the MODIS remote sensing algorithm development. The overall goal was to modify the spectral coverage and gains of the MAS to emulate as many of the MODIS spectral channels as possible. With its much higher spatial resolution (50 m vs. 250-1000 m for MODIS), MAS is able to provide unique information on the small-scale distribution of various geophysical parameters. The MAS instrument has been deployed on multiple platforms for many field campaigns since its first mission in 1991, as the prototype Wildfire Spectrometer. For more information and for a list of MAS campaign flights visit ladsweb at: &lt;a href&#x3D;&quot;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/mas/&quot;&gt;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/mas/&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;masl2cld&quot;&gt;MASL2CLD&lt;/h4&gt;
The MODIS Airborne Simulator (MAS) Level-2 Cloud Data product (MASL2CLD) consists of cloud optical and physical parameters. These parameters are derived using remotely sensed infrared and near infrared solar reflected radiances. Multispectral images of the reflectance and brightness temperature at 10 wavelengths between 0.66 and 13.98nm were used to derive the probability of clear sky (or cloud), cloud thermodynamic phase, and the optical thickness and effective radius of liquid water and ice clouds. MASL2CLD product files are stored in Hierarchical Data Format (HDF-EOS). All gridded cloud parameters are stored as Scientific Data Sets (SDS) within the file. For more information and for a list of MAS campaign flights visit ladsweb at: &lt;a href&#x3D;&quot;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/mas/&quot;&gt;https://ladsweb.modaps.eosdis.nasa.gov/missions-and-measurements/mas/&lt;/a&gt;
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.laadsdaac.earthdatacloud.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA MERRA-2 Observation Project</title>
      <link>https://registry.opendata.aws/nasa-merra-2-observation</link>
      <guid>https://registry.opendata.aws/nasa-merra-2-observation</guid>
      <description>Global Modeling and Assimilation Office Research
&lt;br&gt;&lt;h4 id&#x3D;&quot;gmao_m2scream_inst3_chem&quot;&gt;GMAO_M2SCREAM_INST3_CHEM&lt;/h4&gt;
The MERRA-2 Stratospheric Composition Reanalysis of Aura MLS (M2-SCREAM) products produced at NASA’s Global Modeling and Assimilation Office (GMAO) are generated by assimilating MLS and OMI retrievals into the GEOS Constituent Data Assimilation System (CoDAS) driven by meteorological fields from MERRA-2. M2-SCREAM assimilates hydrochloric acid (HCl), nitric acid (HNO3), stratospheric water vapor (H2O), nitrous oxide (N2O) and ozone with a system equipped with a version of the GEOS general circulation model and a stratospheric chemistry model, StratChem. Assimilated fields are provided globally at 0.5° by 0.625° resolution at three-hourly frequencies from 2004/09/01 to 2024/09/30. Assimilation uncertainties for each of the assimilated constituents are calculated from the CoDAS statistical output (Wargan et al., 2022) and provided as global full-resolution three-dimensional monthly files. Data product updates in March 2024, as a result of Aura MLS “duty cycle” of 190-GHz measurements, include reduced availability of H2O, N2O and HNO3 retrievals resulting in expected M2-SCREAM data quality degradation. However, preliminary analysis shows that the GEOS CoDAS handles the reduced temporal data coverage well, indicating that the GEOS model accurately propagates information from past observations. Data product updates in June 2024 resulting from MLS version upgrade to v5.0 include discontinuities in assimilated H2O (throughout the stratosphere) and N2O (in the lower stratosphere). To note: MLS water vapor is about 0.5 ppmv lower in v5.0, and the vertical range of assimilated N2O data is 100 hPa, extended down from 68 hPa. GMAO is not aware of discontinuities in HCl, HNO3, and ozone related to the version switch.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA MERRA-2 Project</title>
      <link>https://registry.opendata.aws/nasa-merra-2</link>
      <guid>https://registry.opendata.aws/nasa-merra-2</guid>
      <description>Global Modeling and Assimilation Office Research
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2_tmax_pm25&quot;&gt;M2_TMAX_PM25&lt;/h4&gt;
M2_TMAX_PM25 is a value-added product derived from the MERRA-2 aerosol monthly product M2TMNXAER_5.12.4 (or tavgM_2d_aer_Nx). The surface concentration of fine particulate matter (PM2.5) is calculated as the sum of individual aerosol components (organic carbon, black carbon, sulfate, sea salt, and dust) (Buchard et al., 2017) and is recast from the native MERRA-2 model grid. This data collection includes separate files for country-level (and territories) PM2.5 concentrations with and without population weighting applied. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#97;&amp;#46;&amp;#x67;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#97;&amp;#46;&amp;#x67;&amp;#111;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#45;&amp;#100;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#45;&amp;#100;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2c0nxasm&quot;&gt;M2C0NXASM&lt;/h4&gt;
M2C0NXASM (or const_2d_asm_Nx) is a data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of 2-dimensional constant model parameters, such as the fraction of lake, land, and ocean within a model grid cell. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#108;&amp;#45;&amp;#104;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#100;&amp;#105;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#108;&amp;#45;&amp;#104;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#100;&amp;#105;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#100;&amp;#108;&amp;#45;&amp;#x68;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#100;&amp;#108;&amp;#45;&amp;#x68;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2c0nxctm&quot;&gt;M2C0NXCTM&lt;/h4&gt;
M2C0NXCTM (or const_2d_ctm_Nx) is a data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of 2-dimensional constant model parameters for usage by the chemistry transport model (CTM), such as the fraction of lake, land, ice, or ocean within a model grid cell. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#99;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#99;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#100;&amp;#x69;&amp;#x73;&amp;#99;&amp;#64;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#110;&amp;#x61;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#100;&amp;#x69;&amp;#x73;&amp;#99;&amp;#64;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#110;&amp;#x61;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2c0nxlnd&quot;&gt;M2C0NXLND&lt;/h4&gt;
M2C0NXLND (or const_2d_lnd_Nx) is a data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of 2-dimensional constant land surface parameters, such as thickness of the predefined soil layers, soil porosity, and soil wilting point. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#112;&amp;#45;&amp;#x64;&amp;#105;&amp;#115;&amp;#99;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#115;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#112;&amp;#45;&amp;#x64;&amp;#105;&amp;#115;&amp;#99;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#115;&amp;#97;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#115;&amp;#97;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2i1nxasm&quot;&gt;M2I1NXASM&lt;/h4&gt;
M2I1NXASM (or inst1_2d_asm_Nx) is an instantaneous 2-dimensional hourly data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of meteorological diagnostic parameters at the single levels, such as temperature at 2-meter and 10-meter; wind components at 2-meter, 10-meter, and 50-meter; surface pressure, and total precipitable water. The timestamp of a data field is on each hour starting from 00:00 UTC, e.g.: 00:00, 01:00, … , 23:00 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#99;&amp;#45;&amp;#x64;&amp;#108;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#112;&amp;#45;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#99;&amp;#45;&amp;#x64;&amp;#108;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#112;&amp;#45;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#108;&amp;#45;&amp;#104;&amp;#x65;&amp;#108;&amp;#112;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#108;&amp;#45;&amp;#104;&amp;#x65;&amp;#108;&amp;#112;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2i1nxint&quot;&gt;M2I1NXINT&lt;/h4&gt;
M2I1NXINT (or inst1_2d_int_Nx) is an instantaneous 2-dimensional hourly data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of vertically integrated diagnostics, such as kinetic energy, virtual potential temperature, and total precipitable water (or ice, liquid, and vapor). The timestamp of a data field is on each hour starting from 00:00 UTC, e.g.: 00:00, 01:00, … , 23:00 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#115;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#115;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#102;&amp;#99;&amp;#45;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#x65;&amp;#108;&amp;#112;&amp;#45;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#111;&amp;#118;&quot;&gt;&amp;#103;&amp;#115;&amp;#102;&amp;#99;&amp;#45;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#x65;&amp;#108;&amp;#112;&amp;#45;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#111;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2i1nxlfo&quot;&gt;M2I1NXLFO&lt;/h4&gt;
M2I1NXLFO (or inst1_2d_lfo_Nx) is an instantaneous 2-dimensional hourly data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of land surface forcing parameters, such as height, specific humidity, wind, and air temperature of the model surface layer. The timestamp of a data field is on each hour starting from 00:00 UTC, e.g.: 00:00, 01:00, … , 23:00 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#99;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#99;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2i3nxgas&quot;&gt;M2I3NXGAS&lt;/h4&gt;
M2I3NXGAS (or inst3_3d_gas_Nx) is an instantaneous 2-dimensional 3-hourly data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilation of aerosol optical depth analysis and aerosol optical depth analysis increment. The data field is available every three hour starting from 00:00 UTC, e.g.: 00:00, 03:00, … , 21:00 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#97;&amp;#105;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#97;&amp;#105;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2i3nvaer&quot;&gt;M2I3NVAER&lt;/h4&gt;
M2I3NVAER (or inst3_3d_aer_Nv) is an instantaneous 3-dimensional 3-hourly data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of aerosol mixing ratio parameters at 72 model layers, such as dust, sulphur dioxide, sea salt, black carbon, and organic carbon. The data field is available every three hour starting from 00:00 UTC, e.g.: 00:00, 03:00, … , 21:00 UTC. Section 4.2 of the MERRA-2 File Specification document provides pressure values nominal for a 1000 hPa surface pressure and refers to the top edge of the layer. The lev&#x3D;1 is for the top layer, and lev&#x3D;72 is for the bottom (or surface) model layer. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#108;&amp;#112;&amp;#45;&amp;#100;&amp;#105;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#108;&amp;#112;&amp;#45;&amp;#100;&amp;#105;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#97;&amp;#46;&amp;#x67;&amp;#111;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#97;&amp;#46;&amp;#x67;&amp;#111;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2i3npasm&quot;&gt;M2I3NPASM&lt;/h4&gt;
M2I3NPASM (or inst3_3d_asm_Np) is an instantaneous 3-dimensional 3-hourly data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of meteorological parameters at 42 pressure levels, such as temperature, wind components, vertical pressure velocity, water vapor, ozone mass mixing ratio, and layer height. The data field is available every three hours starting from 00:00 UTC, e.g.: 00:00, 03:00, … , 21:00 UTC. The information on the pressure levels can be found in the section 4.2 of the MERRA-2 File Specification document. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#102;&amp;#99;&amp;#45;&amp;#x64;&amp;#108;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#103;&amp;#111;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#102;&amp;#99;&amp;#45;&amp;#x64;&amp;#108;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#103;&amp;#111;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#97;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#115;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#97;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2i3nvasm&quot;&gt;M2I3NVASM&lt;/h4&gt;
M2I3NVASM (or inst3_3d_asm_Nv) is an instantaneous 3-dimensional 3-hourly data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of meteorological parameters at 72 model layers, such as temperature, wind components, vertical pressure velocity, water vapor, and layer height. The data field is available every three hour starting from 00:00 UTC, e.g.: 00:00, 03:00, … , 21:00 UTC. Section 4.2 of the MERRA-2 File Specification document provides pressure values nominal for a 1000 hPa surface pressure and refers to the top edge of the layer. The lev&#x3D;1 is for the top layer, and lev&#x3D;72 is for the bottom (or surface) model layer. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#104;&amp;#101;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#104;&amp;#101;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2i3nvchm&quot;&gt;M2I3NVCHM&lt;/h4&gt;
M2I3NVCHM (or inst3_3d_chm_Nv) is an instantaneous 3-dimensional 3-hourly data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of carbon monoxide and ozone mixing ratio at 72 model layers. The data is available every three hour starting from 00:00 UTC, e.g.: 00:00, 03:00, … , 21:00 UTC. Section 4.2 of the MERRA-2 File Specification document provides pressure values nominal for a 1000 hPa surface pressure and refers to the top edge of the layer. The lev&#x3D;1 is for the top layer, and lev&#x3D;72 is for the bottom (or surface) model layer. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#111;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#111;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#108;&amp;#112;&amp;#45;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#110;&amp;#97;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#103;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#108;&amp;#112;&amp;#45;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#110;&amp;#97;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2i3nvgas&quot;&gt;M2I3NVGAS&lt;/h4&gt;
M2I3NVGAS (or inst3_3d_gas_Nv) is an instantaneous 3-dimensional 3-hourly data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of aerosol mixing ratio analysis increments at 72 model layers, such as mixing ratio analysis increments of black carbon, dust, organic carbon, sea salt, and sulfate. The data field is available every three hour starting from 00:00 UTC, e.g.: 00:00, 03:00, … , 21:00 UTC. Section 4.2 of the MERRA-2 File Specification document provides pressure values nominal for a 1000 hPa surface pressure and refers to the top edge of the layer. The lev&#x3D;1 is for the top layer, and lev&#x3D;72 is for the bottom (or surface) model layer. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#102;&amp;#99;&amp;#45;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#115;&amp;#102;&amp;#99;&amp;#45;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2i6npana&quot;&gt;M2I6NPANA&lt;/h4&gt;
M2I6NPANA (or inst6_3d_ana_Np) is an instantaneous 3-dimensional 6-hourly data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of analyzed meteorological fields at 42 pressure levels, such as temperature, wind components, specific humidity, ozone mixing ratio, and geopotential height. The data field is available every six hour starting from 00:00 UTC, e.g.: 00:00, 06:00, … , 18:00 UTC. The information on the pressure levels can be found in the section 4.2 of the MERRA-2 File Specification document. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#108;&amp;#45;&amp;#x68;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#x73;&amp;#99;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#108;&amp;#45;&amp;#x68;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#x73;&amp;#99;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#108;&amp;#112;&amp;#45;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#108;&amp;#112;&amp;#45;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2i6nvana&quot;&gt;M2I6NVANA&lt;/h4&gt;
M2I6NVANA (or inst6_3d_ana_Nv) is an instantaneous 3-dimensional 6-hourly data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of analized meteorological fields at 72 model layers, such as temperature, wind components,specific humidity, and layer pressure thickness. The data field is available every six hour starting from 00:00 UTC, e.g.: 00:00, 06:00, … , 18:00 UTC. Section 4.2 of the MERRA-2 File Specification document provides pressure values nominal for a 1000 hPa surface pressure and refers to the top edge of the layer. The lev&#x3D;1 is for the top layer, and lev&#x3D;72 is for the bottom (or surface) model layer. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#x66;&amp;#99;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#x66;&amp;#99;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#108;&amp;#x70;&amp;#45;&amp;#100;&amp;#x69;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#115;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#108;&amp;#x70;&amp;#45;&amp;#100;&amp;#x69;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2imnxasm&quot;&gt;M2IMNXASM&lt;/h4&gt;
M2IMNXASM (or instM_2d_asm_Nx) is an instantaneous 2-dimensional monthly mean data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of meteorological diagnostic parameters at the single levels, such as temperature at 2-meter and 10-meter; wind components at 2-meter, 10-meter, and 50-meter; surface pressure, and total precipitable water. The collection also includes variance of certain parameters. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#108;&amp;#45;&amp;#104;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#115;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#115;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#108;&amp;#45;&amp;#104;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#115;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#115;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2imnxgas&quot;&gt;M2IMNXGAS&lt;/h4&gt;
M2IMNXGAS (or instM_3d_gas_Nx) is an instantaneous 2-dimensional monthly mean data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilation of aerosol optical depth analysis and aerosol optical depth analysis increment. The collection also includes the variance of parameters. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#108;&amp;#112;&amp;#45;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#108;&amp;#112;&amp;#45;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#100;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#97;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#100;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#97;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2imnxint&quot;&gt;M2IMNXINT&lt;/h4&gt;
M2IMNXINT (or instM_2d_int_Nx) is an instantaneous 2-dimensional monthly mean data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of vertically integrated diagnostics, such as kinetic energy, virtual potential temperature, and total precipitable water (or ice, liquid, and vapor). The collection also includes variance of certain variables. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#105;&amp;#x73;&amp;#99;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#105;&amp;#x73;&amp;#99;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#45;&amp;#100;&amp;#108;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#97;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#111;&amp;#118;&quot;&gt;&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#45;&amp;#100;&amp;#108;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#97;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#111;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2imnxlfo&quot;&gt;M2IMNXLFO&lt;/h4&gt;
M2IMNXLFO (or instM_2d_lfo_Nx) is an instantaneous 2-dimensional monthly mean data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of land surface forcing parameters, such as height, specific humidity, wind, and air temperature of the model surface layer. The collection also includes variance of certain parameters. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#100;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#100;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2imnpana&quot;&gt;M2IMNPANA&lt;/h4&gt;
M2IMNPANA (or instM_3d_ana_Np) is an instantaneous 3-dimensional monthly mean data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of analyzed meteorological fields at 42 pressure levels, such as temperature, wind components, specific humidity, ozone mixing ratio, and geopotential height. The information on the pressure levels can be found in the section 4.2 of the MERRA-2 File Specification document. The collection also includes certain quadratic information (such as the variance and covariance of certain parameters). MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#102;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#x73;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#115;&amp;#102;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#x73;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#99;&amp;#45;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#97;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#99;&amp;#45;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#97;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2imnpasm&quot;&gt;M2IMNPASM&lt;/h4&gt;
M2IMNPASM (or instM_3d_asm_Np) is an instantaneous 3-dimensional monthly mean data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of meteorological parameters at 42 pressure levels, such as temperature, wind components, vertical pressure velocity, water vapor, ozone mass mixing ratio, and layer height. The information on the pressure levels can be found in the section 4.2 of the MERRA-2 File Specification document. The collection also includes certain quadratic information (such as the variance and covariance of certain parameters). MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#100;&amp;#x69;&amp;#x73;&amp;#99;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#100;&amp;#x69;&amp;#x73;&amp;#99;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#108;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#108;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2iunxasm&quot;&gt;M2IUNXASM&lt;/h4&gt;
M2IUNXASM (or instU_2d_asm_Nx) is an instantaneous 2-dimensional monthly diurnal means data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of meteorological diagnostic parameters at the single levels, such as temperature at 2-meter and 10-meter; wind components at 2-meter, 10-meter, and 50-meter; surface pressure, and total precipitable water. The data consists of the monthly mean of the data field at each hour of a day, e.g., 00:00, 01:00, …, 23:00 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#112;&amp;#45;&amp;#100;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#112;&amp;#45;&amp;#100;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#110;&amp;#97;&amp;#115;&amp;#97;&amp;#46;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#110;&amp;#97;&amp;#115;&amp;#97;&amp;#46;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2iunxgas&quot;&gt;M2IUNXGAS&lt;/h4&gt;
M2IUNXGAS (or instU_3d_gas_Nx) is an instantaneous 2-dimensional monthly diurnal means data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilation of aerosol optical depth analysis and aerosol optical depth analysis increment. It consists of the monthly mean of the data fields every three hour starting from 00:00 UTC, e.g.: 00:00, 03:00, … , 21:00 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#x66;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#99;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#115;&amp;#x66;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#99;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#101;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#x73;&amp;#99;&amp;#64;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#101;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#x73;&amp;#99;&amp;#64;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2iunxint&quot;&gt;M2IUNXINT&lt;/h4&gt;
M2IUNXINT (or instU_2d_int_Nx) is an instantaneous 2-dimensional monthly diurnal means data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of vertically integrated diagnostics, such as kinetic energy, virtual potential temperature, and total precipitable water (or ice, liquid, and vapor). It consists of the monthly mean of the data fields on each hour starting from 00:00 UTC, e.g.: 00:00, 01:00, … , 23:00 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#x6c;&amp;#46;&amp;#110;&amp;#97;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#x6c;&amp;#46;&amp;#110;&amp;#97;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#45;&amp;#100;&amp;#105;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#110;&amp;#97;&amp;#x73;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#115;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#45;&amp;#100;&amp;#105;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#110;&amp;#97;&amp;#x73;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2iunxlfo&quot;&gt;M2IUNXLFO&lt;/h4&gt;
M2IUNXLFO (or instU_2d_lfo_Nx) is an instantaneous 2-dimensional monthly diurnal means data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of land surface forcing parameters, such as height, specific humidity, wind, and air temperature of the model surface layer. It consists of the monthly mean of the data fields on each hour starting from 00:00 UTC, e.g.: 00:00, 01:00, … , 23:00 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#99;&amp;#x2d;&amp;#100;&amp;#108;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#100;&amp;#105;&amp;#115;&amp;#99;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#99;&amp;#x2d;&amp;#100;&amp;#108;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#100;&amp;#105;&amp;#115;&amp;#99;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2iunpana&quot;&gt;M2IUNPANA&lt;/h4&gt;
M2IUNPANA (or instU_3d_ana_Np) is an instantaneous 3-dimensional monthly diurnal means data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of analyzed meteorological fields at 42 pressure levels, such as temperature, wind components, specific humidity, ozone mixing ratio, and geopotential height. It is the monthly mean of data fields every six hour starting from 00:00 UTC, e.g.: 00:00, 06:00, … , 18:00 UTC. The information on the pressure levels can be found in the section 4.2 of the MERRA-2 File Specification document. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#45;&amp;#100;&amp;#x69;&amp;#x73;&amp;#99;&amp;#x40;&amp;#109;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#45;&amp;#100;&amp;#x69;&amp;#x73;&amp;#99;&amp;#x40;&amp;#109;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#104;&amp;#101;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#x73;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#115;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#104;&amp;#101;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#x73;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#115;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2iunpasm&quot;&gt;M2IUNPASM&lt;/h4&gt;
M2IUNPASM (or instU_3d_asm_Np) is an instantaneous 3-dimensional monthly diurnal means data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of meteorological parameters at 42 pressure levels, such as temperature, wind components, vertical pressure velocity, water vapor, ozone mass mixing ratio, and layer height. The data collection is the monthly mean of data fields every three hours starting from 00:00 UTC, e.g.: 00:00, 03:00, … , 21:00 UTC. The information on the pressure levels can be found in the section 4.2 of the MERRA-2 File Specification document. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#102;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#97;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#115;&amp;#102;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#97;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2sdnxslv&quot;&gt;M2SDNXSLV&lt;/h4&gt;
M2SDNXSLV (or statD_2d_slv_Nx) is a 2-dimensional daily data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of daily statistics, such as daily mean (or daily minimum and maximum) air temperature at 2-meter, and maximum precipitation rate during the period. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#x64;&amp;#105;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#x64;&amp;#105;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#97;&amp;#105;&amp;#x6c;&amp;#46;&amp;#110;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#97;&amp;#105;&amp;#x6c;&amp;#46;&amp;#110;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2smnxedi&quot;&gt;M2SMNXEDI&lt;/h4&gt;
M2SMNXEDI (or statM_2d_edi_Nx) is a 2-dimensional monthly data collection for extreme detection indices derived from daily Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2) datasets within each month. V2 of this extreme detection indices data collection is computed based on the 1991-2020 climatology, covering the time period from January 1980 to present. In contrast, V1, the original version, is computed based on an earlier 30-year climatology (1981-2010). This collection consists of indices used to identify or characterize extreme weather events associated with temperature, such as heatwaves and cold spells (e.g., their frequency, duration, and intensity), as well as events associated with precipitation, such as dry days and wet days (e.g., their frequency, duration, and intensity). MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by the NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present, with a latency of ~3 weeks after the end of the previous month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes”, linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original filename. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changes to tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#102;&amp;#99;&amp;#x2d;&amp;#100;&amp;#108;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#102;&amp;#99;&amp;#x2d;&amp;#100;&amp;#108;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read the &amp;quot;MERRA-2 File Specification Document&amp;#39;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page for more information. If these documents do not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#110;&amp;#97;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#110;&amp;#97;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2smnxedi-1&quot;&gt;M2SMNXEDI&lt;/h4&gt;
M2SMNXEDI (or statM_2d_edi_Nx) is a 2-dimensional monthly data collection for extreme detection indices derived from daily Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2) datasets within each month. V1, the original version of this extreme detection indices data collection, is computed based on the 1981-2010 climatology, covering the period from January 1980 to December 2022. In contrast, V2, the second version, is calculated based on a 30-year climatology (1991-2020), covering the period from January 1980 to the present. This collection consists of indices used to identify or characterize extreme weather events associated with temperature, such as heatwaves and cold spells (e.g., their frequency, duration, and intensity), as well as events associated with precipitation, such as dry days and wet days (e.g., their frequency, duration, and intensity). MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by the NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present, with a latency of ~3 weeks after the end of the previous month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes”, linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original filename. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changes to tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#x73;&amp;#99;&amp;#64;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#110;&amp;#97;&amp;#115;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#x73;&amp;#99;&amp;#64;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#110;&amp;#97;&amp;#115;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read the &amp;quot;MERRA-2 File Specification Document&amp;#39;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page for more information. If these documents do not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#45;&amp;#100;&amp;#105;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#45;&amp;#100;&amp;#105;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2smnxpct&quot;&gt;M2SMNXPCT&lt;/h4&gt;
M2SMNXPCT (or statM_2d_pct_Nx) is a 2-dimensional monthly data collection for percentile statistics derived from monthly Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2) datasets. V2 of this percentile data collection is computed based on the 1991-2020 climatology, covering the time period from January 1980 to present. In contrast, V1, the original version, is computed based on an earlier 30-year climatology (1981-2010). This collection consists of percentiles used to identify or characterize extreme weather events associated with temperature (maximum, mean, and minimum 2-m air temperature), as well as with precipitation (total precipitation). MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by the NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present, with a latency of ~3 weeks after the end of the previous month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes”, linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original filename. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changes to tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read the &amp;quot;MERRA-2 File Specification Document&amp;#39;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page for more information. If these documents do not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#100;&amp;#105;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#100;&amp;#105;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2smnxpct-1&quot;&gt;M2SMNXPCT&lt;/h4&gt;
M2SMNXPCT (or statM_2d_pct_Nx) is a 2-dimensional monthly data collection for percentile statistics derived from monthly Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2) datasets. V1, the original version of this percentile data collection, is computed based on the 1981-2010 climatology, covering the period from January 1980 to December 2022. In contrast, V2, the second version, is calculated based on a 30-year climatology (1991-2020), covering the period from January 1980 to the present. This collection consists of percentiles used to identify or characterize extreme weather events associated with temperature (maximum, mean, and minimum 2-m air temperature), as well as with precipitation (total precipitation). MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by the NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present, with a latency of ~3 weeks after the end of the previous month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes”, linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original filename. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changes to tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#x66;&amp;#99;&amp;#45;&amp;#100;&amp;#108;&amp;#45;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#110;&amp;#97;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#115;&amp;#x66;&amp;#99;&amp;#45;&amp;#100;&amp;#108;&amp;#45;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#110;&amp;#97;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read the &amp;quot;MERRA-2 File Specification Document&amp;#39;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page for more information. If these documents do not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#45;&amp;#x64;&amp;#108;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#x61;&amp;#x69;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#103;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#45;&amp;#x64;&amp;#108;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#x61;&amp;#x69;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2smnxslv&quot;&gt;M2SMNXSLV&lt;/h4&gt;
M2SMNXSLV (or statM_2d_slv_Nx) is a 2-dimensional monthly mean data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of monthly mean of daily statistics, such as daily mean (or daily minimum and maximum) air temperature at 2-meter, and maximum precipitation rate during the period. The collection also includes the variance of parameters. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#x64;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#103;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#x64;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#102;&amp;#99;&amp;#45;&amp;#100;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#103;&amp;#115;&amp;#102;&amp;#99;&amp;#45;&amp;#100;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2t1nxadg&quot;&gt;M2T1NXADG&lt;/h4&gt;
M2T1NXADG (or tavg1_2d_adg_Nx) is an hourly time-averaged 2-dimensional data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilated aerosol diagnostics (extended), such as dry and wet deposition of each aerosol component, dust emission and sedimentation for each sized bin, and organic carbon convective scavenging. The data fields are time-stamped with the central time of an hour starting from 00:30 UTC, e.g.: 00:30, 01:30, … , 23:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#111;&amp;#118;&quot;&gt;&amp;#x67;&amp;#115;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#111;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2t1nxaer&quot;&gt;M2T1NXAER&lt;/h4&gt;
M2T1NXAER (or tavg1_2d_aer_Nx) is an hourly time-averaged 2-dimensional data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilated aerosol diagnostics, such as column mass density of aerosol components (black carbon, dust, sea salt, sulfate, and organic carbon), surface mass concentration of aerosol components, and total extinction (and scattering ) aerosol optical thickness (AOT) at 550 nm. The total PM1.0, PM2.5, and PM10 may be derived with the formula described in the FAQs under the Documentation tab of this page. The data field is time-stamped with the central time of an hour starting from 00:30 UTC, e.g.: 00:30, 01:30, … , 23:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#110;&amp;#97;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#110;&amp;#97;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#97;&amp;#105;&amp;#108;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#118;&quot;&gt;&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#97;&amp;#105;&amp;#108;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2t1nxchm&quot;&gt;M2T1NXCHM&lt;/h4&gt;
M2T1NXCHM (or tavg1_2d_chm_Nx) is an hourly time-averaged 2-dimensional data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilated carbon monoxide and ozone diagnostics, such as properties of carbon monoxide (column burden, emission, chemical production, and surface concentration), and total column ozone. The data field is time-stamped with the central time of an hour starting from 00:30 UTC, e.g.: 00:30, 01:30, … , 23:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#100;&amp;#108;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#45;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#118;&quot;&gt;&amp;#x67;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#100;&amp;#108;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#45;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2t1nxcsp&quot;&gt;M2T1NXCSP&lt;/h4&gt;
M2T1NXCSP (or tavg1_2d_csp_Nx) is an hourly time-averaged 2-dimensional data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of parameters from CFMIP Observations Simulator Package(COSP), such as ISCCP total cloud area fraction, MODIS cloud fraction water (ice) mean, MODIS cloud fraction low (mid,high) mean, modis cloud particle size water (ice) mean. CFMIP is the abbreviation of Cloud Feedback Model Intercomparison Project. The data field is time-stamped with the central time of an hour starting from 00:30 UTC, e.g.: 00:30, 01:30, … , 23:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#97;&amp;#46;&amp;#103;&amp;#111;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#97;&amp;#46;&amp;#103;&amp;#111;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2t1nxflx&quot;&gt;M2T1NXFLX&lt;/h4&gt;
M2T1NXFLX (or tavg1_2d_flx_Nx) is an hourly time-averaged 2-dimensional data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilated surface flux diagnostics, such as total precipitation, bias corrected total precipitation, surface air temperature, surface specific humidity, surface wind speed, and evaporation from turbulence. The “surface” in this data collection is the model surface layer. The heights of the model surface layer (HLML) vary with time and location, with the value of ~60 meter above ground. The data field is time-stamped with the central time of an hour starting from 00:30 UTC, e.g.: 00:30, 01:30, … , 23:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#105;&amp;#115;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#118;&quot;&gt;&amp;#103;&amp;#115;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#105;&amp;#115;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#x65;&amp;#108;&amp;#x70;&amp;#45;&amp;#x64;&amp;#105;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#103;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#x65;&amp;#108;&amp;#x70;&amp;#45;&amp;#x64;&amp;#105;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2t1nxint&quot;&gt;M2T1NXINT&lt;/h4&gt;
M2T1NXINT (or tavg1_2d_int_Nx) is an hourly time-averaged 2-dimensional data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of vertically Integrated diagnostics of water and energy, such as autoconversion loss of cloud water, convective source of cloud ice (water), eastward (nothward) flux of atmospheric ice (liquid, vapor), total potential energy tendency, vertically integrated potential energy tendency, and vertically integrated kinetic energy tendency. The data field is time-stamped with the central time of an hour starting from 00:30 UTC, e.g.: 00:30, 01:30, … , 23:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#99;&amp;#x40;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#99;&amp;#x40;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#115;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2t1nxlfo&quot;&gt;M2T1NXLFO&lt;/h4&gt;
M2T1NXLFO (or tavg1_2d_lfo_Nx) is an hourly time-averaged 2-dimensional data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of land surface forcing parameters, such as bias corrected precipitation, shortwave and longwave radiation at surface. The data field is time-stamped with the central time of an hour starting from 00:30 UTC, e.g.: 00:30, 01:30, … , 23:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#100;&amp;#108;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#100;&amp;#108;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2t1nxlnd&quot;&gt;M2T1NXLND&lt;/h4&gt;
M2T1NXLND (or tavg1_2d_lnd_Nx) is an hourly time-averaged 2-dimensional data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of land surface diagnostics, such as baseflow flux, runoff, surface soil wetness, root zone soil wetness, water at surface layer, water at root zone layer, and soil temperature at six layers. The data field is time-stamped with the central time of an hour starting from 00:30 UTC, e.g.: 00:30, 01:30, … , 23:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#100;&amp;#108;&amp;#45;&amp;#x68;&amp;#x65;&amp;#108;&amp;#x70;&amp;#45;&amp;#100;&amp;#105;&amp;#x73;&amp;#99;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#100;&amp;#108;&amp;#45;&amp;#x68;&amp;#x65;&amp;#108;&amp;#x70;&amp;#45;&amp;#100;&amp;#105;&amp;#x73;&amp;#99;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#102;&amp;#99;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#99;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#115;&amp;#102;&amp;#99;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#99;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2t1nxocn&quot;&gt;M2T1NXOCN&lt;/h4&gt;
M2T1NXOCN (or tavg1_2d_ocn_Nx) is an hourly time-averaged 2-dimensional data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of ocean surface diagnostics, such as open water skin temperature (sea surface temperature), open water latent energy flux, open water upward sensible heat flux, and open water net downward longwave ( or shortwave ) flux . The data field is time-stamped with the central time of an hour starting from 00:30 UTC, e.g.: 00:30, 01:30, … , 23:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#100;&amp;#105;&amp;#115;&amp;#99;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#x6c;&amp;#46;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#100;&amp;#105;&amp;#115;&amp;#99;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#x6c;&amp;#46;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#99;&amp;#45;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#x40;&amp;#109;&amp;#97;&amp;#105;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#99;&amp;#45;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#x40;&amp;#109;&amp;#97;&amp;#105;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2t1nxrad&quot;&gt;M2T1NXRAD&lt;/h4&gt;
M2T1NXRAD (or tavg1_2d_rad_Nx) is an hourly time-averaged 2-dimensional data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of radiation diagnostics, such as surface albedo, cloud area fraction, in cloud optical thickness, surface incoming shortwave flux (i.e. solar radiation), surface net downward shortwave flux, and upwelling longwave flux at toa (top of atmosphere) (i.e. outgoing longwave radiation (OLR) at toa). The data field is time-stamped with the central time of an hour starting from 00:30 UTC, e.g.: 00:30, 01:30, … , 23:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#108;&amp;#46;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#115;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#108;&amp;#46;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#102;&amp;#99;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#105;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#x2e;&amp;#110;&amp;#97;&amp;#x73;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#115;&amp;#102;&amp;#99;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#105;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#x2e;&amp;#110;&amp;#97;&amp;#x73;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2t1nxslv&quot;&gt;M2T1NXSLV&lt;/h4&gt;
M2T1NXSLV (or tavg1_2d_slv_Nx) is an hourly time-averaged 2-dimensional data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of meteorology diagnostics at popularly used vertical levels, such as air temperature at 2-meter (or at 10-meter, 850hPa, 500 hPa, 250hPa), wind components at 50-meter (or at 2-meter, 10-meter, 850 hPa, 500hPa, 250 hPa), sea level pressure, surface pressure, and total precipitable water vapor (or ice water, liquid water). The data field is time-stamped with the central time of an hour starting from 00:30 UTC, e.g.: 00:30, 01:30, … , 23:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#x65;&amp;#108;&amp;#112;&amp;#45;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#115;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#x65;&amp;#108;&amp;#112;&amp;#45;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#99;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#99;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2t3nxglc&quot;&gt;M2T3NXGLC&lt;/h4&gt;
M2T3NXGLC (or tavg3_2d_glc_Nx) is a 2-dimensional 3-hourly time-averaged data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilated land ice surface diagnostics at the single levels, such as fractional area of glaciated surface snow cover, snow mass over glaciated surface, snow depth over glaciated surface, and total snow mass residual due to densification. The data field is available every three hour starting from 01:30 UTC, e.g.: 01:30, 04:30, … , 22:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#110;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#x67;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#110;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#x67;&amp;#111;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2t3nvasm&quot;&gt;M2T3NVASM&lt;/h4&gt;
M2T3NVASM (or tavg3_3d_asm_Nv) is a 3-dimensional 3-hourly time averaged data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of meteorological parameters at 72 model layers, such as air temperature, wind components, vertical pressure velocity, water vapor, and layer height. The data field is available every three hour starting from 01:30 UTC, e.g.: 01:30, 04:30, … , 22:30 UTC. Section 4.2 of the MERRA-2 File Specification document provides pressure values nominal for a 1000 hPa surface pressure and refers to the top edge of the layer. The lev&#x3D;1 is for the top layer, and lev&#x3D;72 is for the bottom (or surface) model layer. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#115;&amp;#99;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#115;&amp;#99;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#x64;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#x73;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#x64;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2t3npcld&quot;&gt;M2T3NPCLD&lt;/h4&gt;
M2T3NPCLD (or tavg3_3d_cld_Np) is a 3-dimensional 3-hourly time averaged data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of cloud diagnostics on the 42 pressure levels, such as updraft areal fraction, cloud fraction for radiation , in-cloud cloud liquid (or ice) for radiation, and mass fraction of cloud liquid (or ice) water. The data field is available every three hour starting from 01:30 UTC, e.g.: 01:30, 04:30, … , 22:30 UTC. The information on the pressure levels can be found in the section 4.2 of the MERRA-2 File Specification document. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#115;&amp;#97;&amp;#46;&amp;#103;&amp;#111;&amp;#118;&quot;&gt;&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#115;&amp;#97;&amp;#46;&amp;#103;&amp;#111;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#101;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#97;&amp;#46;&amp;#x67;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#101;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#97;&amp;#46;&amp;#x67;&amp;#111;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2t3nvcld&quot;&gt;M2T3NVCLD&lt;/h4&gt;
M2T3NVCLD (or tavg3_3d_cld_Nv) is a 3-dimensional 3-hourly time averaged data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of cloud diagnostics at 72 model layers, such as cloud fraction for radiation, pressure thickness, in cloud cloud ice (or liquid) for radiation, and relative humidity. The data field is available every three hour starting from 01:30 UTC, e.g.: 01:30, 04:30, … , 22:30 UTC. Section 4.2 of the MERRA-2 File Specification document provides pressure values nominal for a 1000 hPa surface pressure and refers to the top edge of the layer. The lev&#x3D;1 is for the top layer, and lev&#x3D;72 is for the bottom (or surface) model layer. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#x64;&amp;#105;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#115;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#x64;&amp;#105;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#108;&amp;#112;&amp;#45;&amp;#100;&amp;#105;&amp;#x73;&amp;#99;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#x73;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#108;&amp;#112;&amp;#45;&amp;#100;&amp;#105;&amp;#x73;&amp;#99;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2t3nemst&quot;&gt;M2T3NEMST&lt;/h4&gt;
M2T3NEMST (or tavg3_3d_mst_Ne) is a 3-dimensional 3-hourly time-averaged data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of moisture processes diagnostics at the 73 model layer edges. The parameters include cumulative mass flux, 3D flux of liquid (or ice) convective (or nonconvective) precipitation, and model layer edge pressure. The data field is available every three hour starting from 01:30 UTC, e.g.: 01:30, 04:30, … , 22:30 UTC. Section 4.2 of the MERRA-2 File Specification document provides pressure values nominal for a 1000 hPa surface pressure and refers to the top edge of the layer. The lev&#x3D;1 is for the top layer, and lev&#x3D;73 is for the bottom (or surface) model layer edge. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#115;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2t3npmst&quot;&gt;M2T3NPMST&lt;/h4&gt;
M2T3NPMST (or tavg3_3d_mst_Np) is a 3-dimensional 3-hourly time averaged data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of moist processes diagnostics on the 42 pressure levels, such as convective rainwater source, 3D flux of ice convective (or nonconvective) precipitation, and 3D flux of liquid convective (or nonconvective) precipitation. The data field is available every three hour starting from 01:30 UTC, e.g.: 01:30, 04:30, … , 22:30 UTC. The information on the pressure levels can be found in the section 4.2 of the MERRA-2 File Specification document. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#115;&amp;#99;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#115;&amp;#99;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#100;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#97;&amp;#46;&amp;#x67;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#100;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#97;&amp;#46;&amp;#x67;&amp;#111;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2t3nvmst&quot;&gt;M2T3NVMST&lt;/h4&gt;
M2T3NVMST (or tavg3_3d_mst_Nv) is a 3-dimensional 3-hourly time averaged data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilated moist processes diagnostics at 72 model layers, such as convective rainwater source, large scale rainwater source, evap subl of convective precipitation, and evap subl of non convective precipitation. The data field is available every three hour starting from 01:30 UTC, e.g.: 01:30, 04:30, … , 22:30 UTC. Section 4.2 of the MERRA-2 File Specification document provides pressure values nominal for a 1000 hPa surface pressure and refers to the top edge of the layer. The lev&#x3D;1 is for the top layer, and lev&#x3D;72 is for the bottom (or surface) model layer. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#x64;&amp;#105;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#x64;&amp;#105;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#102;&amp;#99;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#97;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#115;&amp;#102;&amp;#99;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#97;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2t3nenav&quot;&gt;M2T3NENAV&lt;/h4&gt;
M2T3NENAV (or tavg3_3d_nav_Ne) is a 3-dimensional 3-hourly time-averaged data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of vertical coordinates of the 73 model layer edges. The parameters include edge pressure and edge heights. The data field is available every three hour starting from 01:30 UTC, e.g.: 01:30, 04:30, … , 22:30 UTC. Section 4.2 of the MERRA-2 File Specification document provides pressure values nominal for a 1000 hPa surface pressure and refers to the top edge of the layer. The lev&#x3D;1 is for the top layer, and lev&#x3D;73 is for the bottom (or surface) model layer edge. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#x66;&amp;#99;&amp;#45;&amp;#100;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#105;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#x66;&amp;#99;&amp;#45;&amp;#100;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#105;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#111;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#111;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2t3npodt&quot;&gt;M2T3NPODT&lt;/h4&gt;
M2T3NPODT (or tavg3_3d_odt_Np) is a 3-dimensional 3-hourly time averaged data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of ozone tendencies on the 42 pressure levels, such as total ozone analysis tendency, tendency of odd oxygen mixing ratio due to chemistry, tendency of odd oxygen due to moist processes, and tendency of ozone due to dynamics. The data field is available every three hour starting from 01:30 UTC, e.g.: 01:30, 04:30, … , 22:30 UTC. The information on the pressure levels can be found in the section 4.2 of the MERRA-2 File Specification document. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#102;&amp;#99;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#115;&amp;#102;&amp;#99;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2t3npqdt&quot;&gt;M2T3NPQDT&lt;/h4&gt;
M2T3NPQDT (or tavg3_3d_qdt_Np) is a 3-dimensional 3-hourly time averaged data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of moist tendencies on the 42 pressure levels, such as tendency of ice (or liquid) water due to dynamics, total ice (or liquid) water tendency due to moist, total specific humidity analysis tendency, and specific humidity tendency due to moist. The data field is available every three hour starting from 01:30 UTC, e.g.: 01:30, 04:30, … , 22:30 UTC. The information on the pressure levels can be found in the section 4.2 of the MERRA-2 File Specification document. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#102;&amp;#99;&amp;#45;&amp;#x64;&amp;#108;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#115;&amp;#102;&amp;#99;&amp;#45;&amp;#x64;&amp;#108;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#108;&amp;#45;&amp;#104;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#118;&quot;&gt;&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#108;&amp;#45;&amp;#104;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2t3nprad&quot;&gt;M2T3NPRAD&lt;/h4&gt;
M2T3NPRAD (or tavg3_3d_rad_Np) is a 3-dimensional 3-hourly time averaged data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of radiation diagnostics on 42 pressure levels, such as cloud fraction for radiation, and air temperature tendency due to longwave (or shortwave). The data field is available every three hour starting from 01:30 UTC, e.g.: 01:30, 04:30, … , 22:30 UTC. The information on the pressure levels can be found in the section 4.2 of the MERRA-2 File Specification document. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#102;&amp;#x63;&amp;#45;&amp;#100;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#108;&amp;#112;&amp;#45;&amp;#100;&amp;#x69;&amp;#x73;&amp;#99;&amp;#x40;&amp;#109;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#110;&amp;#x61;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#115;&amp;#102;&amp;#x63;&amp;#45;&amp;#100;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#108;&amp;#112;&amp;#45;&amp;#100;&amp;#x69;&amp;#x73;&amp;#99;&amp;#x40;&amp;#109;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#110;&amp;#x61;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#99;&amp;#45;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#112;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#99;&amp;#45;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#112;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2t3nvrad&quot;&gt;M2T3NVRAD&lt;/h4&gt;
M2T3NVRAD (or tavg3_3d_rad_Nv) is a 3-dimensional 3-hourly time averaged data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilated radiation diagnostics at 72 model layers, such as air temperature tendency due to longwave and air temperature tendency due to shortwave. The data field is available every three hour starting from 01:30 UTC, e.g.: 01:30, 04:30, … , 22:30 UTC. Section 4.2 of the MERRA-2 File Specification document provides pressure values nominal for a 1000 hPa surface pressure and refers to the top edge of the layer. The lev&#x3D;1 is for the top layer, and lev&#x3D;72 is for the bottom (or surface) model layer. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#100;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#111;&amp;#118;&quot;&gt;&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#100;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#111;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#99;&amp;#45;&amp;#100;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#100;&amp;#105;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#97;&amp;#46;&amp;#x67;&amp;#111;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#99;&amp;#45;&amp;#100;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#100;&amp;#105;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#97;&amp;#46;&amp;#x67;&amp;#111;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2t3nptdt&quot;&gt;M2T3NPTDT&lt;/h4&gt;
M2T3NPTDT (or tavg3_3d_tdt_Np) is a 3-dimensional 3-hourly time averaged data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of air temperature tendencies on 42 pressure levels, such as total temperature analysis tendency, and tendency of air temperature due to dynamics (or friction, moisture, radiation, and physics). The data field is available every three hour starting from 01:30 UTC, e.g.: 01:30, 04:30, … , 22:30 UTC. The information on the pressure levels can be found in the section 4.2 of the MERRA-2 File Specification document. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#115;&amp;#99;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#115;&amp;#99;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#105;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#105;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2t3netrb&quot;&gt;M2T3NETRB&lt;/h4&gt;
M2T3NETRB (or tavg3_3d_trb_Ne) is a 3-dimensional 3-hourly time-averaged data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilated turbulence diagnostics at the 73 model layer edges. The parameters include total scalar diffusivity, total momentum diffusivity, momentum diffusivity from Louis, Richardson number from Louis, and more. The data field is available every three hour starting from 01:30 UTC, e.g.: 01:30, 04:30, … , 22:30 UTC. Section 4.2 of the MERRA-2 File Specification document provides pressure values nominal for a 1000 hPa surface pressure and refers to the top edge of the layer. The lev&#x3D;1 is for the top layer, and lev&#x3D;73 is for the bottom (or surface) model layer edge. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#103;&amp;#x73;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#115;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2t3nptrb&quot;&gt;M2T3NPTRB&lt;/h4&gt;
M2T3NPTRB (or tavg3_3d_trb_Np) is a 3-dimensional 3-hourly time averaged data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of turbulence diagnostics on 42 pressure levels, such as total scalar diffusivity, total momentum diffusivity, momentum diffusivity from Louis, and Richardson number from Louis. The data field is available every three hour starting from 01:30 UTC, e.g.: 01:30, 04:30, … , 22:30 UTC. The information on the pressure levels can be found in the section 4.2 of the MERRA-2 File Specification document. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#108;&amp;#45;&amp;#x68;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#115;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#103;&amp;#115;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#108;&amp;#45;&amp;#x68;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#115;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2t3npudt&quot;&gt;M2T3NPUDT&lt;/h4&gt;
M2T3NPUDT (or tavg3_3d_udt_Np) is a 3-dimensional 3-hourly time averaged data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of wind tendencies on 42 pressure levels, such as total eastward (or northward) wind analysis tendency, tendency of eastward (or northward) wind due to dynamics, and tendency of eastward (or northward) wind due to turbulence. The data field is available every three hour starting from 01:30 UTC, e.g.: 01:30, 04:30, … , 22:30 UTC. The information on the pressure levels can be found in the section 4.2 of the MERRA-2 File Specification document. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#45;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#45;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#115;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tcnxltm&quot;&gt;M2TCNXLTM&lt;/h4&gt;
M2TCNXLTM (or tavgC_2d_ltm_Nx) is a 2-dimensional monthly data collection for climatological long term mean and standard deviation representing the interannual variability on a monthly timescale, derived from monthly Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2) datasets. V2 of this data collection is calculated with data from January 1991 to December 2020. In contrast, V1, the original version, is computed with data from an earlier 30-year time of 1981-2010. This collection consists of meteorological diagnostics, such as air temperature (maximum, mean, and minimum at 2-meter), wind components at different vertical levels (2-meter, 10-meter, 50-meter, 850 hPa, 500hPa, and 250 hPa), sea level pressure, surface pressure, and total precipitation, evaporation, and total precipitable water vapor. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by the NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present, with a latency of ~3 weeks after the end of the previous month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes”, linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original filename. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changes to tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#102;&amp;#99;&amp;#x2d;&amp;#100;&amp;#108;&amp;#x2d;&amp;#104;&amp;#101;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#102;&amp;#99;&amp;#x2d;&amp;#100;&amp;#108;&amp;#x2d;&amp;#104;&amp;#101;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read the &amp;quot;MERRA-2 File Specification Document&amp;#39;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page for more information. If these documents do not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#97;&amp;#46;&amp;#x67;&amp;#111;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#115;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#97;&amp;#46;&amp;#x67;&amp;#111;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tcnpltm&quot;&gt;M2TCNPLTM&lt;/h4&gt;
M2TCNPLTM (or tavgC_3d_ltm_Np) is a 3-dimensional monthly data collection for climatological long term mean and standard deviation representing the interannual variability on a monthly timescale, derived from monthly Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2) datasets. V2 of this data collection is calculated with data from January 1991 to December 2020. In contrast, V1, the original version, is computed with data from an earlier 30-year time of 1981-2010. This collection consists of meteorological diagnostics at 12 vertical pressure levels (e.g.,850 hPa, 500hPa, and 200 hPa), such as air temperature, wind components, and both relative and specific humidity. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by the NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present, with a latency of ~3 weeks after the end of the previous month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes”, linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original filename. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changes to tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#115;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read the &amp;quot;MERRA-2 File Specification Document&amp;#39;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page for more information. If these documents do not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#x66;&amp;#x63;&amp;#45;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#115;&amp;#x66;&amp;#x63;&amp;#45;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tmnxadg&quot;&gt;M2TMNXADG&lt;/h4&gt;
M2TMNXADG (or tavgM_2d_adg_Nx) is a time-averaged 2-dimensional monthly mean data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilated aerosol diagnostics (extended), such as dry and wet deposition of each aerosol component, dust emission and sedimentation for each sized bin, and organic carbon convective scavenging. The collection also includes variance of certain parameters. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#102;&amp;#99;&amp;#45;&amp;#100;&amp;#108;&amp;#45;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#105;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#102;&amp;#99;&amp;#45;&amp;#100;&amp;#108;&amp;#45;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#105;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#102;&amp;#x63;&amp;#45;&amp;#100;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#x73;&amp;#99;&amp;#x40;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#115;&amp;#102;&amp;#x63;&amp;#45;&amp;#100;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#x73;&amp;#99;&amp;#x40;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tmnxaer&quot;&gt;M2TMNXAER&lt;/h4&gt;
M2TMNXAER (or tavgM_2d_aer_Nx) is a time-averaged 2-dimensional monthly mean data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilated aerosol diagnostics, such as column mass density of aerosol components (black carbon, dust, sea salt, sulfate, and organic carbon), surface mass concentration of aerosol components, and total extinction (and scattering ) aerosol optical thickness (AOT) at 550 nm. The total PM1.0, PM2.5, and PM10 may be derived with the formula described in the FAQs under the Documentation tab of this page. The collection also includes variance of certain parameters. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#105;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#118;&quot;&gt;&amp;#x67;&amp;#115;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#105;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#100;&amp;#105;&amp;#x73;&amp;#99;&amp;#x40;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#100;&amp;#105;&amp;#x73;&amp;#99;&amp;#x40;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tmnxchm&quot;&gt;M2TMNXCHM&lt;/h4&gt;
M2TMNXCHM (or tavgM_2d_chm_Nx) is a time-averaged 2-dimensional monthly mean data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilated carbon monoxide and ozone diagnostics, such as properties of carbon monoxide (column burden, emission, chemical production, and surface concentration), and total column ozone. The collection also includes variance of certain parameters. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#97;&amp;#105;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#97;&amp;#105;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#99;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#x67;&amp;#111;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#99;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#x67;&amp;#111;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tmnxcsp&quot;&gt;M2TMNXCSP&lt;/h4&gt;
M2TMNXCSP (or tavgM_2d_csp_Nx) is a time-averaged 2-dimensional monthly mean data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of parameters from CFMIP Observations Simulator Package(COSP), such as ISCCP total cloud area fraction, MODIS cloud fraction water (ice) mean, MODIS cloud fraction low (mid,high) mean, modis cloud particle size water (ice) mean. CFMIP is the abbreviation of Cloud Feedback Model Intercomparison Project. The collection also includes variance of certain parameters. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#x64;&amp;#x69;&amp;#115;&amp;#99;&amp;#x40;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#x64;&amp;#x69;&amp;#115;&amp;#99;&amp;#x40;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#x64;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#x64;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tmnxflx&quot;&gt;M2TMNXFLX&lt;/h4&gt;
M2TMNXFLX (or tavgM_2d_flx_Nx) is a time-averaged 2-dimensional monthly mean data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilated surface flux diagnostics, such as total precipitation, bias corrected total precipitation, surface air temperature, surface specific humidity, surface wind speed, and evaporation from turbulence. The “surface” in this data collection is the model surface layer. The heights of the model surface layer (HLML) vary with time and location, with the value of ~60 meter above ground. The collection also includes variance of certain parameters. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#97;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#97;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tmnxglc&quot;&gt;M2TMNXGLC&lt;/h4&gt;
M2TMNXGLC (or tavgM_2d_glc_Nx) is a 2-dimensional monthly mean data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilated land ice surface diagnostics at the single levels, such as fractional area of glaciated surface snow cover, snow mass over glaciated surface, snow depth over glaciated surface, and total snow mass residual due to densification. The collection also includes variance of certain parameters. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#112;&amp;#45;&amp;#100;&amp;#105;&amp;#x73;&amp;#x63;&amp;#64;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#112;&amp;#45;&amp;#100;&amp;#105;&amp;#x73;&amp;#x63;&amp;#64;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#110;&amp;#97;&amp;#x73;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#110;&amp;#97;&amp;#x73;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tmnxint&quot;&gt;M2TMNXINT&lt;/h4&gt;
M2TMNXINT (or tavgM_2d_int_Nx) is a time-averaged 2-dimensional monthly mean data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of water and energy related vertically Integrated diagnostics, such as autoconversion loss of cloud water, convective source of cloud ice (water), eastward (nothward) flux of atmospheric ice (liquid, vapor), total potential energy tendency, vertically integrated potential energy tendency, and vertically integrated kinetic energy tendency. The collection also includes variance of certain parameters. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#100;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#118;&quot;&gt;&amp;#x67;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#100;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#97;&amp;#46;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#97;&amp;#46;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tmnxlfo&quot;&gt;M2TMNXLFO&lt;/h4&gt;
M2TMNXLFO (or tavgM_2d_lfo_Nx) is a time-averaged 2-dimensional monthly mean data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of land surface forcing parameters, such as bias corrected precipitation, shortwave and longwave radiation at surface. The collection also includes variance of certain parameters. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#112;&amp;#45;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#105;&amp;#x6c;&amp;#46;&amp;#110;&amp;#97;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#112;&amp;#45;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#105;&amp;#x6c;&amp;#46;&amp;#110;&amp;#97;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#101;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#x73;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#108;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#115;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#101;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#x73;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#108;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tmnxlnd&quot;&gt;M2TMNXLND&lt;/h4&gt;
M2TMNXLND (or tavgM_2d_lnd_Nx) is a time-averaged 2-dimensional monthly mean data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of land surface diagnostics, such as baseflow flux, runoff, surface soil wetness, root zone soil wetness, water at surface layer, water at root zone layer, and soil temperature at six layers. The collection also includes variance of certain parameters. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#101;&amp;#108;&amp;#112;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#99;&amp;#64;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#103;&amp;#111;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#101;&amp;#108;&amp;#112;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#99;&amp;#64;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#103;&amp;#111;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#110;&amp;#97;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#115;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#110;&amp;#97;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tmnxocn&quot;&gt;M2TMNXOCN&lt;/h4&gt;
M2TMNXOCN (or tavgM_2d_ocn_Nx) is a time-averaged 2-dimensional monthly mean data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of ocean surface diagnostics, such as open water skin temperature (sea surface temperature), open water latent energy flux, open water upward sensible heat flux, and open water net downward longwave ( or shortwave ) flux . The collection also includes variance of certain parameters. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#102;&amp;#99;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#111;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#102;&amp;#99;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#111;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#102;&amp;#99;&amp;#45;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#115;&amp;#102;&amp;#99;&amp;#45;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tmnxrad&quot;&gt;M2TMNXRAD&lt;/h4&gt;
M2TMNXRAD (or tavgM_2d_rad_Nx) is a time-averaged 2-dimensional monthly mean data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of radiation diagnostics, such as surface albedo, cloud area fraction, in cloud optical thickness, surface incoming shortwave flux (i.e. solar radiation), surface net downward shortwave flux, and upwelling longwave flux at toa (top of atmosphere) (i.e. outgoing longwave radiation (OLR) at toa). The collection also includes variance of certain parameters. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#108;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#108;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#108;&amp;#112;&amp;#45;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#108;&amp;#112;&amp;#45;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tmnxslv&quot;&gt;M2TMNXSLV&lt;/h4&gt;
M2TMNXSLV (or tavgM_2d_slv_Nx) is a time-averaged 2-dimensional monthly mean data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of meteorology diagnostics at popularly used vertical levels, such as air temperature at 2-meter (or at 10-meter, 850hPa, 500 hPa, 250hPa), wind components at 50-meter (or at 2-meter, 10-meter, 850hPa, 500hPa, 250 hPa), sea level pressure, surface pressure, and total precipitable water vapor (or ice water, liquid water). The collection also includes variance of certain parameters. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#103;&amp;#115;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#99;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#99;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tmnpcld&quot;&gt;M2TMNPCLD&lt;/h4&gt;
M2TMNPCLD (or tavgM_3d_cld_Np) is a 3-dimensional monthly mean data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of cloud diagnostics on 42 the pressure levels, such as updraft areal fraction, cloud fraction for radiation, in-cloud cloud liquid (or ice) for radiation, and mass fraction of cloud liquid (or ice) water. The information on the pressure levels can be found in the section 4.2 of the MERRA-2 File Specification document. The collection also includes variance of certain parameters. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#108;&amp;#45;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#108;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#118;&quot;&gt;&amp;#103;&amp;#115;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#108;&amp;#45;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#108;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#45;&amp;#x64;&amp;#105;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#45;&amp;#x64;&amp;#105;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tmnpmst&quot;&gt;M2TMNPMST&lt;/h4&gt;
M2TMNPMST (or tavgM_3d_mst_Np) is a 3-dimensional monthly mean data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of moist processes diagnostics on the 42 pressure levels, such as convective rainwater source, 3D flux of ice convective (or nonconvective) precipitation, and 3D flux of liquid convective (or nonconvective) precipitation. The information on the pressure levels can be found in the section 4.2 of the MERRA-2 File Specification document. The collection also includes variance of certain parameters. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#115;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#115;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#108;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#109;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#108;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#109;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tmnpodt&quot;&gt;M2TMNPODT&lt;/h4&gt;
M2TMNPODT (or tavgM_3d_odt_Np) is a 3-dimensional monthly mean data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of ozone tendencies on the 42 pressure levels, such as total ozone analysis tendency, tendency of odd oxygen mixing ratio due to chemistry, tendency of odd oxygen due to moist processes, and tendency of ozone due to dynamics. The information on the pressure levels can be found in the section 4.2 of the MERRA-2 File Specification document. The collection also includes variance of certain parameters. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#x66;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#x61;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#103;&amp;#115;&amp;#x66;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#x61;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#108;&amp;#112;&amp;#45;&amp;#100;&amp;#105;&amp;#x73;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#97;&amp;#46;&amp;#103;&amp;#111;&amp;#118;&quot;&gt;&amp;#x67;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#108;&amp;#112;&amp;#45;&amp;#100;&amp;#105;&amp;#x73;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#97;&amp;#46;&amp;#103;&amp;#111;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tmnpqdt&quot;&gt;M2TMNPQDT&lt;/h4&gt;
M2TMNPQDT (or tavgM_3d_qdt_Np) is a 3-dimensional monthly mean data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of moist tendencies on the 42 pressure levels, such as tendency of ice (or liquid) water due to dynamics, total ice (or liquid) water tendency due to moist, total specific humidity analysis tendency, and specific humidity tendency due to moist. The information on the pressure levels can be found in the section 4.2 of the MERRA-2 File Specification document. The collection also includes variance of certain parameters. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#x40;&amp;#109;&amp;#97;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#x40;&amp;#109;&amp;#97;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tmnprad&quot;&gt;M2TMNPRAD&lt;/h4&gt;
M2TMNPRAD (or tavgM_3d_rad_Np) is a 3-dimensional monthly mean data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of radiation diagnostics on 42 pressure levels, such as cloud fraction for radiation, and air temperature tendency due to longwave (or shortwave). The information on the pressure levels can be found in the section 4.2 of the MERRA-2 File Specification document. The collection also includes variance of certain parameters. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#x66;&amp;#x63;&amp;#45;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#45;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#115;&amp;#x66;&amp;#x63;&amp;#45;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#45;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#102;&amp;#99;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#64;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#115;&amp;#102;&amp;#99;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#64;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tmnptdt&quot;&gt;M2TMNPTDT&lt;/h4&gt;
M2TMNPTDT (or tavgM_3d_tdt_Np) is a 3-dimensional monthly mean data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of air temperature tendencies on 42 pressure levels, such as total temperature analysis tendency, and tendency of air temperature due to dynamics (or friction, moisture, radiation, and physics). The information on the pressure levels can be found in the section 4.2 of the MERRA-2 File Specification document. The collection also includes variance of certain parameters. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#x64;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#115;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#x64;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#105;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#105;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tmnptrb&quot;&gt;M2TMNPTRB&lt;/h4&gt;
M2TMNPTRB (or tavgM_3d_trb_Np) is a 3-dimensional monthly mean data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of turbulence diagnostics on 42 pressure levels, such as total scalar diffusivity, total momentum diffusivity, momentum diffusivity from Louis, and Richardson number from Louis. The information on the pressure levels can be found in the section 4.2 of the MERRA-2 File Specification document. The collection also includes variance of certain parameters. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#x66;&amp;#99;&amp;#45;&amp;#100;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#x66;&amp;#99;&amp;#45;&amp;#100;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#100;&amp;#105;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#x73;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#100;&amp;#105;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tmnpudt&quot;&gt;M2TMNPUDT&lt;/h4&gt;
M2TMNPUDT (or tavgM_3d_udt_Np) is a 3-dimensional monthly mean data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of wind tendencies on 42 pressure levels, such as total eastward (or northward) wind analysis tendency, tendency of eastward (or northward) wind due to dynamics, and tendency of eastward (or northward) wind due to turbulence. The information on the pressure levels can be found in the section 4.2 of the MERRA-2 File Specification document. The collection also includes variance of certain parameters. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#111;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#111;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tunxadg&quot;&gt;M2TUNXADG&lt;/h4&gt;
M2TUNXADG (or tavgU_2d_adg_Nx) is a time-averaged 2-dimensional monthly diurnal means data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilated aerosol diagnostics (extended), such as dry and wet deposition of each aerosol component, dust emission and sedimentation for each sized bin, and organic carbon convective scavenging. This data collection is the monthly mean of data fields for each hour and is time-stamped with the central time of an hour starting from 00:30 UTC, e.g.: 00:30, 01:30, … , 23:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#108;&amp;#x2d;&amp;#104;&amp;#101;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#108;&amp;#x2d;&amp;#104;&amp;#101;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#115;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#x69;&amp;#108;&amp;#46;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#115;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#115;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#x69;&amp;#108;&amp;#46;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tunxaer&quot;&gt;M2TUNXAER&lt;/h4&gt;
M2TUNXAER (or tavgU_2d_aer_Nx) is a time-averaged 2-dimensional monthly diurnal means data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilated aerosol diagnostics, such as column mass density of aerosol components (black carbon, dust, sea salt, sulfate, and organic carbon), surface mass concentration of aerosol components, and total extinction (and scattering ) aerosol optical thickness (AOT) at 550 nm. The total PM1.0, PM2.5, and PM10 may be derived with the formula described in the FAQs under the Documentation tab of this page. This data collection is the monthly mean of data fields for each hour and is time-stamped with the central time of an hour starting from 00:30 UTC, e.g.: 00:30, 01:30, … , 23:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#45;&amp;#100;&amp;#105;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#115;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#45;&amp;#100;&amp;#105;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#102;&amp;#99;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#115;&amp;#102;&amp;#99;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tunxchm&quot;&gt;M2TUNXCHM&lt;/h4&gt;
M2TUNXCHM (or tavgU_2d_chm_Nx) is a time-averaged 2-dimensional monthly diurnal means data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilated carbon monoxide and ozone diagnostics, such as properties of carbon monoxide (column burden, emission, chemical production, and surface concentration), and total column ozone. This data collection is the monthly mean of data fields for each hour and time-stamped with the central time of an hour starting from 00:30 UTC, e.g.: 00:30, 01:30, … , 23:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#102;&amp;#99;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#112;&amp;#45;&amp;#x64;&amp;#105;&amp;#x73;&amp;#99;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#118;&quot;&gt;&amp;#103;&amp;#115;&amp;#102;&amp;#99;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#112;&amp;#45;&amp;#x64;&amp;#105;&amp;#x73;&amp;#99;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#45;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#x73;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#111;&amp;#118;&quot;&gt;&amp;#103;&amp;#115;&amp;#x66;&amp;#99;&amp;#45;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#x73;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#111;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tunxcsp&quot;&gt;M2TUNXCSP&lt;/h4&gt;
M2TUNXCSP (or tavgU_2d_csp_Nx) is a time-averaged 2-dimensional monthly diurnal means data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of parameters from CFMIP Observations Simulator Package(COSP), such as ISCCP total cloud area fraction, MODIS cloud fraction water (ice) mean, MODIS cloud fraction low (mid,high) mean, modis cloud particle size water (ice) mean. CFMIP is the abbreviation of Cloud Feedback Model Intercomparison Project. This data collection is the monthly mean of data fields for each hour and time-stamped with the central time of an hour starting from 00:30 UTC, e.g.: 00:30, 01:30, … , 23:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#99;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#99;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#101;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#x73;&amp;#99;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#x66;&amp;#99;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#101;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#x73;&amp;#99;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tunxflx&quot;&gt;M2TUNXFLX&lt;/h4&gt;
M2TUNXFLX (or tavgU_2d_flx_Nx) is a time-averaged 2-dimensional monthly diurnal means data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilated surface flux diagnostics, such as total precipitation, bias corrected total precipitation, surface air temperature, surface specific humidity, surface wind speed, and evaporation from turbulence. The “surface” in this data collection is the model surface layer. The heights of the model surface layer (HLML) vary with time and location, with the value of ~60 meter above ground. This data collection is the monthly mean of data fields for each hour and time-stamped with the central time of an hour starting from 00:30 UTC, e.g.: 00:30, 01:30, … , 23:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#x73;&amp;#99;&amp;#x40;&amp;#109;&amp;#97;&amp;#105;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#115;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#x73;&amp;#99;&amp;#x40;&amp;#109;&amp;#97;&amp;#105;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#102;&amp;#99;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#100;&amp;#105;&amp;#115;&amp;#99;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#102;&amp;#99;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#100;&amp;#105;&amp;#115;&amp;#99;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tunxglc&quot;&gt;M2TUNXGLC&lt;/h4&gt;
M2TUNXGLC (or tavgU_2d_glc_Nx) is a 2-dimensional monthly diurnal means data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilated land ice surface diagnostics at the single levels, such as fractional area of glaciated surface snow cover, snow mass over glaciated surface, snow depth over glaciated surface, and total snow mass residual due to densification. This data collection is the monthly mean of data fields for each 3-hour and time-stamped at the central time starting from 01:30 UTC, e.g.: 01:30, 04:30, … , 22:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#100;&amp;#x69;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#97;&amp;#105;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#100;&amp;#x69;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#97;&amp;#105;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tunxint&quot;&gt;M2TUNXINT&lt;/h4&gt;
M2TUNXINT (or tavgU_2d_int_Nx) is a time-averaged 2-dimensional monthly diurnal means data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of water and energy related vertically Integrated diagnostics, such as autoconversion loss of cloud water, convective source of cloud ice (water), eastward (nothward) flux of atmospheric ice (liquid, vapor), total potential energy tendency, vertically integrated potential energy tendency, and vertically integrated kinetic energy tendency. This data collection is the monthly mean of data fields for each hour and time-stamped with the central time of an hour starting from 00:30 UTC, e.g.: 00:30, 01:30, … , 23:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#x66;&amp;#99;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#109;&amp;#97;&amp;#105;&amp;#x6c;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#115;&amp;#x66;&amp;#99;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#109;&amp;#97;&amp;#105;&amp;#x6c;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#x66;&amp;#x63;&amp;#45;&amp;#x64;&amp;#108;&amp;#45;&amp;#104;&amp;#101;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#115;&amp;#99;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#115;&amp;#x66;&amp;#x63;&amp;#45;&amp;#x64;&amp;#108;&amp;#45;&amp;#104;&amp;#101;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#115;&amp;#99;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tunxlfo&quot;&gt;M2TUNXLFO&lt;/h4&gt;
M2TUNXLFO (or tavgU_2d_lfo_Nx) is a time-averaged 2-dimensional monthly diurnal means data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of land surface forcing parameters, such as bias corrected precipitation, shortwave and longwave radiation at surface. This data collection is the monthly mean of data fields for each hour and time-stamped with the central time of an hour starting from 00:30 UTC, e.g.: 00:30, 01:30, … , 23:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#46;&amp;#110;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#115;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#46;&amp;#110;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#102;&amp;#99;&amp;#45;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#100;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#115;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#115;&amp;#102;&amp;#99;&amp;#45;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#100;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#115;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tunxlnd&quot;&gt;M2TUNXLND&lt;/h4&gt;
M2TUNXLND (or tavgU_2d_lnd_Nx) is a time-averaged 2-dimensional monthly diurnal means data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of land surface diagnostics, such as baseflow flux, runoff, surface soil wetness, root zone soil wetness, water at surface layer, water at root zone layer, and soil temperature at six layers. This data collection is the monthly mean of data fields for each hour and time-stamped with the central time of an hour starting from 00:30 UTC, e.g.: 00:30, 01:30, … , 23:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#99;&amp;#64;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#x73;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#99;&amp;#64;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#112;&amp;#45;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#115;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#112;&amp;#45;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tunxocn&quot;&gt;M2TUNXOCN&lt;/h4&gt;
M2TUNXOCN (or tavgU_2d_ocn_Nx) is a time-averaged 2-dimensional monthly diurnal means data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of ocean surface diagnostics, such as open water skin temperature (sea surface temperature), open water latent energy flux, open water upward sensible heat flux, and open water net downward longwave ( or shortwave ) flux . This data collection is the monthly mean of data fields for each hour and time-stamped with the central time of an hour starting from 00:30 UTC, e.g.: 00:30, 01:30, … , 23:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#x73;&amp;#99;&amp;#x40;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#105;&amp;#x73;&amp;#99;&amp;#x40;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#112;&amp;#45;&amp;#x64;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#112;&amp;#45;&amp;#x64;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tunxrad&quot;&gt;M2TUNXRAD&lt;/h4&gt;
M2TUNXRAD (or tavgU_2d_rad_Nx) is a time-averaged 2-dimensional monthly diurnal means data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of radiation diagnostics, such as surface albedo, cloud area fraction, in cloud optical thickness, surface incoming shortwave flux (i.e. solar radiation), surface net downward shortwave flux, and upwelling longwave flux at toa (top of atmosphere) (i.e. outgoing longwave radiation (OLR) at toa). This data collection is the monthly mean of data fields for each hour and time-stamped with the central time of an hour starting from 00:30 UTC, e.g.: 00:30, 01:30, … , 23:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#103;&amp;#115;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#97;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#103;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tunxslv&quot;&gt;M2TUNXSLV&lt;/h4&gt;
M2TUNXSLV (or tavgU_2d_slv_Nx) is a time-averaged 2-dimensional monthly diurnal means data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of meteorology diagnostics at popularly used vertical levels, such as air temperature at 2-meter (or at 10-meter, 850 hPa, 500 hPa, 250hPa), wind components at 50-meter (or at 2-meter, 10-meter, 850hPa, 500hPa, 250 hPa), sea level pressure, surface pressure, and total precipitable water vapor (or ice water, liquid water). This data collection is the monthly mean of data fields for each hour and time-stamped with the central time of an hour starting from 00:30 UTC, e.g.: 00:30, 01:30, … , 23:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#99;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#108;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#99;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#100;&amp;#x69;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#100;&amp;#x69;&amp;#x73;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tunpcld&quot;&gt;M2TUNPCLD&lt;/h4&gt;
M2TUNPCLD (or tavgU_3d_cld_Np) is a 3-dimensional monthly diurnal means data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of cloud diagnostics on 42 the pressure levels, such as updraft areal fraction, cloud fraction for radiation, in-cloud cloud liquid (or ice) for radiation, and mass fraction of cloud liquid (or ice) water. The information on the pressure levels can be found in the section 4.2 of the MERRA-2 File Specification document. This data collection is the monthly mean of data fields for each 3-hour and time-stamped at the central time starting from 01:30 UTC, e.g.: 01:30, 04:30, … , 22:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#102;&amp;#99;&amp;#45;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#115;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#118;&quot;&gt;&amp;#x67;&amp;#115;&amp;#102;&amp;#99;&amp;#45;&amp;#x64;&amp;#108;&amp;#45;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#112;&amp;#45;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#115;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#111;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#x6c;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#97;&amp;#x2e;&amp;#103;&amp;#111;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tunpmst&quot;&gt;M2TUNPMST&lt;/h4&gt;
M2TUNPMST (or tavgU_3d_mst_Np) is a 3-dimensional monthly diurnal means data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of moist processes diagnostics on the 42 pressure levels, such as convective rainwater source, 3D flux of ice convective (or nonconvective) precipitation, and 3D flux of liquid convective (or nonconvective) precipitation. The information on the pressure levels can be found in the section 4.2 of the MERRA-2 File Specification document. This data collection is the monthly mean of data fields for each 3-hour and time-stamped at the central time starting from 01:30 UTC, e.g.: 01:30, 04:30, … , 22:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#97;&amp;#105;&amp;#x6c;&amp;#46;&amp;#110;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#111;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#x66;&amp;#99;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#97;&amp;#105;&amp;#x6c;&amp;#46;&amp;#110;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#111;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#100;&amp;#108;&amp;#45;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#100;&amp;#108;&amp;#45;&amp;#104;&amp;#x65;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#109;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tunpodt&quot;&gt;M2TUNPODT&lt;/h4&gt;
M2TUNPODT (or tavgU_3d_odt_Np) is a 3-dimensional monthly diurnal means data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of ozone tendencies on the 42 pressure levels, such as total ozone analysis tendency, tendency of odd oxygen mixing ratio due to chemistry, tendency of odd oxygen due to moist processes, and tendency of ozone due to dynamics. The information on the pressure levels can be found in the section 4.2 of the MERRA-2 File Specification document. This data collection is the monthly mean of data fields for each 3-hour and time-stamped at the central time starting from 01:30 UTC, e.g.: 01:30, 04:30, … , 22:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#108;&amp;#112;&amp;#45;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#110;&amp;#97;&amp;#x73;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#103;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#104;&amp;#x65;&amp;#108;&amp;#112;&amp;#45;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#110;&amp;#97;&amp;#x73;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#108;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#99;&amp;#64;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#118;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#108;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#99;&amp;#64;&amp;#x6d;&amp;#97;&amp;#x69;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tunpqdt&quot;&gt;M2TUNPQDT&lt;/h4&gt;
M2TUNPQDT (or tavgU_3d_qdt_Np) is a 3-dimensional monthly diurnal means data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of moist tendencies on the 42 pressure levels, such as tendency of ice (or liquid) water due to dynamics, total ice (or liquid) water tendency due to moist, total specific humidity analysis tendency, and specific humidity tendency due to moist. The information on the pressure levels can be found in the section 4.2 of the MERRA-2 File Specification document. This data collection is the monthly mean of data fields for each 3-hour and time-stamped at the central time starting from 01:30 UTC, e.g.: 01:30, 04:30, … , 22:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#102;&amp;#99;&amp;#45;&amp;#100;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#x67;&amp;#115;&amp;#102;&amp;#99;&amp;#45;&amp;#100;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#x73;&amp;#x63;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#108;&amp;#x2e;&amp;#110;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#108;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#115;&amp;#x66;&amp;#x63;&amp;#45;&amp;#100;&amp;#108;&amp;#45;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#45;&amp;#x64;&amp;#105;&amp;#x73;&amp;#x63;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#x2e;&amp;#110;&amp;#97;&amp;#115;&amp;#x61;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tunprad&quot;&gt;M2TUNPRAD&lt;/h4&gt;
M2TUNPRAD (or tavgU_3d_rad_Np) is a 3-dimensional monthly diurnal means data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of radiation diagnostics on 42 pressure levels, such as cloud fraction for radiation, and air temperature tendency due to longwave (or shortwave). The information on the pressure levels can be found in the section 4.2 of the MERRA-2 File Specification document. This data collection is the monthly mean of data fields for each 3-hour that is time-stamped at the central time starting from 01:30 UTC, e.g.: 01:30, 04:30, … , 22:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#45;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#110;&amp;#x61;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#x6f;&amp;#118;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#108;&amp;#112;&amp;#45;&amp;#100;&amp;#105;&amp;#x73;&amp;#99;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#x68;&amp;#101;&amp;#108;&amp;#112;&amp;#45;&amp;#100;&amp;#105;&amp;#x73;&amp;#99;&amp;#x40;&amp;#109;&amp;#x61;&amp;#105;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tunptdt&quot;&gt;M2TUNPTDT&lt;/h4&gt;
M2TUNPTDT (or tavgU_3d_tdt_Np) is a 3-dimensional monthly diurnal means data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of air temperature tendencies on 42 pressure levels, such as total temperature analysis tendency, and tendency of air temperature due to dynamics (or friction, moisture, radiation, and physics). The information on the pressure levels can be found in the section 4.2 of the MERRA-2 File Specification document. This data collection is the monthly mean of data fields for each 3-hour and time-stamped at the central time starting from 01:30 UTC, e.g.: 01:30, 04:30, … , 22:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#x73;&amp;#102;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#45;&amp;#x68;&amp;#101;&amp;#108;&amp;#x70;&amp;#45;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#x61;&amp;#x2e;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#108;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#64;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#108;&amp;#46;&amp;#x6e;&amp;#x61;&amp;#x73;&amp;#97;&amp;#46;&amp;#x67;&amp;#x6f;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tunptrb&quot;&gt;M2TUNPTRB&lt;/h4&gt;
M2TUNPTRB (or tavgU_3d_trb_Np) is a 3-dimensional monthly diurnal means data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of turbulence diagnostics on 42 pressure levels, such as total scalar diffusivity, total momentum diffusivity, momentum diffusivity from Louis, and Richardson number from Louis. The information on the pressure levels can be found in the section 4.2 of the MERRA-2 File Specification document. This data collection is the monthly mean of data fields for each 3-hour and time-stamped at the central time starting from 01:30 UTC, e.g.: 01:30, 04:30, … , 22:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#115;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#104;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#115;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#x64;&amp;#x6c;&amp;#45;&amp;#104;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#99;&amp;#x40;&amp;#x6d;&amp;#97;&amp;#105;&amp;#108;&amp;#x2e;&amp;#x6e;&amp;#x61;&amp;#115;&amp;#x61;&amp;#46;&amp;#x67;&amp;#111;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#110;&amp;#97;&amp;#x73;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&quot;&gt;&amp;#103;&amp;#115;&amp;#102;&amp;#x63;&amp;#45;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#104;&amp;#101;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#x64;&amp;#x69;&amp;#x73;&amp;#99;&amp;#64;&amp;#109;&amp;#97;&amp;#x69;&amp;#x6c;&amp;#46;&amp;#110;&amp;#97;&amp;#x73;&amp;#x61;&amp;#46;&amp;#103;&amp;#x6f;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;m2tunpudt&quot;&gt;M2TUNPUDT&lt;/h4&gt;
M2TUNPUDT (or tavgU_3d_udt_Np) is a 3-dimensional monthly diurnal means data collection in Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2). This collection consists of assimilations of wind tendencies on 42 pressure levels, such as total eastward (or northward) wind analysis tendency, tendency of eastward (or northward) wind due to dynamics, and tendency of eastward (or northward) wind due to turbulence. The information on the pressure levels can be found in the section 4.2 of the MERRA-2 File Specification document. This data collection is the monthly mean of data fields for each 3-hour and time-stamped at the central time starting from 01:30 UTC, e.g.: 01:30, 04:30, … , 22:30 UTC. MERRA-2 is the latest version of global atmospheric reanalysis for the satellite era produced by NASA Global Modeling and Assimilation Office (GMAO) using the Goddard Earth Observing System Model (GEOS) version 5.12.4. The dataset covers the period of 1980-present with the latency of ~3 weeks after the end of a month. Data Reprocessing: Please check “Records of MERRA-2 Data Reprocessing and Service Changes” linked from the “Documentation” tab on this page. Note that a reprocessed data filename is different from the original file. MERRA-2 Mailing List: Sign up to receive information on reprocessing of data, changing of tools and services, as well as data announcements from GMAO. Contact the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#103;&amp;#115;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&quot;&gt;&amp;#103;&amp;#115;&amp;#102;&amp;#99;&amp;#x2d;&amp;#x64;&amp;#108;&amp;#x2d;&amp;#104;&amp;#x65;&amp;#x6c;&amp;#x70;&amp;#x2d;&amp;#100;&amp;#x69;&amp;#115;&amp;#99;&amp;#64;&amp;#109;&amp;#x61;&amp;#105;&amp;#108;&amp;#46;&amp;#x6e;&amp;#97;&amp;#115;&amp;#x61;&amp;#46;&amp;#103;&amp;#111;&amp;#x76;&lt;/a&gt;) to be added to the list. Questions: If you have a question, please read &amp;quot;MERRA-2 File Specification Document&amp;quot;, “MERRA-2 Data Access – Quick Start Guide”, and FAQs linked from the ”Documentation” tab on this page. If that does not answer your question, you may post your question to the NASA Earthdata Forum (forum.earthdata.nasa.gov) or email the GES DISC Help Desk (&lt;a href&#x3D;&quot;mailto:&amp;#x67;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#x76;&quot;&gt;&amp;#x67;&amp;#x73;&amp;#x66;&amp;#x63;&amp;#x2d;&amp;#100;&amp;#x6c;&amp;#x2d;&amp;#x68;&amp;#x65;&amp;#x6c;&amp;#112;&amp;#x2d;&amp;#100;&amp;#105;&amp;#115;&amp;#x63;&amp;#x40;&amp;#x6d;&amp;#x61;&amp;#x69;&amp;#x6c;&amp;#x2e;&amp;#x6e;&amp;#97;&amp;#x73;&amp;#97;&amp;#x2e;&amp;#x67;&amp;#111;&amp;#x76;&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://data.gesdisc.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA MEaSUREs/HOMaGE Project</title>
      <link>https://registry.opendata.aws/nasa-measures-homage</link>
      <guid>https://registry.opendata.aws/nasa-measures-homage</guid>
      <description>This data set contains the monthly Global Ocean Mass Anomalies (goma) since 04/2002, as measured by the GRACE and GRACE Follow-On (G/GFO) satellite missions. The data are averaged over the global ocean domain, at monthly intervals (note: data gaps exist). This file contains the goma time series based on the spherical harmonic gravity fields provided by the G/GFO SDS centers: JPL, CSR, GFZ. The data are frequently updated as new monthly observations are acquired by the GFO mission. The processing of the spherical harmonics gravity field coefficients is as follows: (1) GAD + GSM: the monthly de-aliasing product GAD is added back to the GSM L2 gravity fields; (2) [GSM + GAD] coefficients are averaged over the global ocean with a coastal buffer of 300 km (to avoid land-ocean leakage); (3) the spatial mean of atmospheric loading of the entire global ocean domain is removed (via the GAA L2 data product). A GIA correction using the ICE-6GD model (Peltier et al., 2018) is applied.
&lt;br&gt;&lt;h4 id&#x3D;&quot;homage_ggfo_msc_cri_salgrd_v01&quot;&gt;HOMAGE_GGFO_MSC_CRI_SALGRD_v01&lt;/h4&gt;
This data set contains global gridded, monthly solutions of the sea level equation (gravitational-rotational-deformational GRD components) using surface mass data from the GRACE and GRACE Follow-On (G/GFO) satellite missions, beginning in April 2002. The sea level components are provided for separate land domains to allow users the local contributions from various ice melt sources (e.g., Greenland, Antarctica, mountain glaciers), as well as non-glaciated land regions. The full record for each component is given in a separate netCDF file, and includes gridded data of radial deformation, geoid height and relative sea level, as well as timeseries of global mean barystatic sea level. The data are frequently updated as new monthly observations are acquired by the GFO mission. &lt;br&gt;&lt;br&gt; These data are based on the gridded JPL CRI-filtered mascons (e.g., &lt;a href&#x3D;&quot;https://doi.org/10.5067/TEMSC-3JC634&quot;&gt;https://doi.org/10.5067/TEMSC-3JC634&lt;/a&gt;), and thus inherit all processing steps from those fields. For more information on GRD definitions and related terminology, please refer to Gregory et al., 2019 (&lt;a href&#x3D;&quot;https://doi.org/10.1007/s10712-019-09525-z&quot;&gt;https://doi.org/10.1007/s10712-019-09525-z&lt;/a&gt;).
&lt;br&gt;&lt;h4 id&#x3D;&quot;homage_steric_ohc_time_series_v01&quot;&gt;HOMAGE_STERIC_OHC_TIME_SERIES_v01&lt;/h4&gt;
The [HOMAGE_STERIC_OHC_TIME_SERIES_v01] dataset contains monthly global mean ocean heat content (OHC) anomalies as well as thermosteric, halosteric and total steric sea level anomalies computed from various gridded ocean data sets of sub-temperature and salinity profiles as provided by different institutions: Scripps Institution of Oceanography (SIO); Institute of Atmospheric Physics (IAP); Barnes objective analysis (BOA from CSIO, MNR); Jamstec / Ishii et al. 2017 (I17); and Met Office Hadley Centre: EN4_c13, EN4_c14, EN4_g10, and EN4_I09. The data are averaged over the quasi-global ocean domain (i.e., where valid values are defined; note that gaps exist, in particular towards polar latitudes), at monthly intervals. The input profiling data (i.e, temperature and salinity profiles at depth levels), editing, quality flags and processing schemes vary across the different gridded products, please refer to the documentation for each institution’s data product for details. Since 2005, the profiling data are dominated by the observations from the global Argo network (e.g., &lt;a href&#x3D;&quot;https://argo.ucsd.edu/&quot;&gt;https://argo.ucsd.edu/&lt;/a&gt;), which comprises nearly 4000 active floats (as of 08/2022). Before 2005, non-Argo data such as XBT profilers were used, and the global ocean coverage was significantly more sparse. Data sets from SIO and BOA are Argo-only, while the others also include other observations, such as expendable bathythermographs (XBTs) and Conductivity-Temperature-Depth (CTD) observations. The data are active forward stream data files and will be frequently updated as new observations are acquired by Argo, and processed by the data centers.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://archive.podaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA MEaSUREs/OSWV Project</title>
      <link>https://registry.opendata.aws/nasa-measures-oswv</link>
      <guid>https://registry.opendata.aws/nasa-measures-oswv</guid>
      <description>This dataset contains model output interpolated in space and time to observations from the MetOp-A ASCAT (ASCAT-A) instrument (a satellite-based scatterometer), representing the first science quality release of these data (post-provisional after v1.0) funded under the MEaAUREs program. These auxiliary fields are included to complement those scatterometer observations, specifically for the ASCATA_ESDR_L2_WIND_STRESS_V1.1 dataset. Model variables include: i) ocean surface wind fields from ERA-5 short-term forecast (removed from the analyses times to reduce impacts from assimilated scatterometer retrievals at the beginning of the forecast); ii) estimations of precipitation from the GPM IMERG product; iii) estimation of the surface currents from the GlobCurrent project. The fields are provided on a non-uniform grid within the sampled locations of the ASCAT-A Level 2 product, and at a nominal 12.5 km pixel resolution. Each file corresponds to a specific orbital revolution number, which begins at the southernmost point of the ascending orbit. The thumbnail shows data for two orbits - using all orbits for a single day will provide global coverage. &lt;br&gt;&lt;br&gt; The dataset represents the first science quality release of this product with funding from the MEaSUREs (Making Earth System Data Records for Use in Research Environments) program. Version 1.1 provides a set of updates and improvements from version 1.0, including: 1) cleaned up ancillary data points in between the left/right swaths for improved collocation with available satellite data, 2) improved variable metadata, 3) removed the GlobCurrent stokes drift variables, and 4) provided data source metadata including DOIs for the ERA-5, IMERGE, and GlobCurrent data sources. The primary purpose of this Version 1.1 release is for science evaluation by the NASA International Ocean Vector Winds Science Team (IOVWST).
&lt;br&gt;&lt;h4 id&#x3D;&quot;ascata_esdr_l2_wsderiv_v10&quot;&gt;ASCATA_ESDR_L2_WSDERIV_V1.0&lt;/h4&gt;
This dataset contains the curl and divergence of ocean surface equivalent neutral wind and wind stress, derived from satellite-based scatterometer observations (the MetOp-A ASCAT scatterometer), representing the first science quality release of these data funded under the MEaSUREs program. This product from MetOp-A ASCAT has been intercalibrated with similar scatterometer measurements from instruments on the MetOp-B, ScatSat-1, and QuikScat satellites, all of which can be found on the MEaSUREs OSVW Project Page. These Level 2 data are provided on a non-uniform grid within the satellite swath at ~12.5 km pixel resolution. Each L2 file corresponds to a specific orbital revolution number, which begins at the southernmost point of the ascending orbit - the thumbnail preview shows data for all orbits over a day (typically 14 orbits). Estimates for the curls and divergences are computed over several spatial domains with varying radii from the point of interest, and included as separate variables. &lt;br&gt;&lt;br&gt; The dataset represents the first science quality release funded under the MEaSUREs (Making Earth System Data Records for Use in Research Environments) program. The primary purpose of this release is for science evaluation by the NASA International Ocean Vector Winds Science Team (IOVWST). This V1.0 of the data was derived from V1.1 of the L2 wind and stress product.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ascata_esdr_l2_wind_stress_v11&quot;&gt;ASCATA_ESDR_L2_WIND_STRESS_V1.1&lt;/h4&gt;
This dataset contains ocean surface wind vectors (equivalent neutral and true 10m) and wind stress vectors derived from satellite-based scatterometer observations (the MetOp-A ASCAT scatterometer), representing the first science quality release of these data (post-provisional after v1.0) funded under the MEaSUREs program. This product from MetOp-A ASCAT has been intercalibrated with similar scatterometer measurements from instruments on the MetOp-B, ScatSat-1, and QuikScat satellites (all of which can be found on the MEaSUREs OSVW Project Page), and if used together create an unbroken record of winds from 1999 to 2022. The wind vector and stress retrievals are provided on a non-uniform grid within the swath (Level 2 products) at 12.5 km pixel resolution. Each L2 file corresponds to a specific orbital revolution number, which begins at the southernmost point of the ascending orbit. The thumbnail shows data for two orbits - using all orbits for a single day will provide global coverage. &lt;br&gt;&lt;br&gt; The dataset represents the first science quality release funded under the MEaSUREs (Making Earth System Data Records for Use in Research Environments) program. Version 1.1 provides a set of updates and improvements from version 1.0, including: 1) increased data coverage, 2) improved quality control, and 3) new global metadata attributes featuring revolution number, equator crossing longitude, and equator crossing time (UTC). The primary purpose of this release is for science evaluation by the NASA International Ocean Vector Winds Science Team (IOVWST).
&lt;br&gt;&lt;h4 id&#x3D;&quot;ascata_esdr_l3_wind_stress_v10&quot;&gt;ASCATA_ESDR_L3_WIND_STRESS_V1.0&lt;/h4&gt;
This dataset contains gridded ocean surface wind vectors (equivalent neutral and true 10m) and wind stress vectors derived from satellite-based scatterometer observations (the MetOp-A ASCAT scatterometer), representing the first science quality release of these data funded under the MEaSUREs program. This product from MetOp-A ASCAT has been intercalibrated with similar scatterometer measurements from instruments on the MetOp-B, ScatSat-1, and QuikScat satellites, all of which can be found on the MEaSUREs OSVW Project Page. The wind vector and stress retrievals are provided on a global grid (one per file) at 12.5 km pixel resolution. Data exist only over areas of the globe that fell within one of the satellite swaths/orbits for that day (see thumbnail). &lt;br&gt;&lt;br&gt; The dataset represents the first science quality release funded under the MEaSUREs (Making Earth System Data Records for Use in Research Environments) program. Note that this is the first version of the Level 3 data (V1.0) but they were derived from V1.1 of the Level 2 product. The primary purpose of this release is for science evaluation by the NASA International Ocean Vector Winds Science Team (IOVWST).
&lt;br&gt;&lt;h4 id&#x3D;&quot;ascatb_esdr_ancillary_l2_v11&quot;&gt;ASCATB_ESDR_ANCILLARY_L2_V1.1&lt;/h4&gt;
This dataset contains model output interpolated in space and time to observations from the MetOp-B ASCAT (ASCAT-B) instrument (a satellite-based scatterometer), representing the first science quality release of these data (post-provisional after v1.0) funded under the MEaAUREs program. These auxiliary fields are included to complement those scatterometer observations, specifically for the ASCATB_ESDR_L2_WIND_STRESS_V1.1 dataset. Model variables include: i) ocean surface wind fields from ERA-5 short-term forecast (removed from the analyses times to reduce impacts from assimilated scatterometer retrievals at the beginning of the forecast); ii) estimations of precipitation from the GPM IMERG product; iii) estimation of the surface currents from the GlobCurrent project. The fields are provided on a non-uniform grid within the sampled locations of the ASCAT-B Level 2 product, and at a nominal 12.5 km pixel resolution. Each file corresponds to a specific orbital revolution number, which begins at the southernmost point of the ascending orbit. The thumbnail shows data for two orbits - using all orbits for a single day will provide global coverage. &lt;br&gt;&lt;br&gt; The dataset represents the first science quality release of this product with funding from the MEaSUREs (Making Earth System Data Records for Use in Research Environments) program. Version 1.1 provides a set of updates and improvements from version 1.0, including: 1) cleaned up ancillary data points in between the left/right swaths for improved collocation with available satellite data, 2) improved variable metadata, 3) removed the GlobCurrent stokes drift variables, and 4) provided data source metadata including DOIs for the ERA-5, IMERGE, and GlobCurrent data sources. The primary purpose of this Version 1.1 release is for science evaluation by the NASA International Ocean Vector Winds Science Team (IOVWST).
&lt;br&gt;&lt;h4 id&#x3D;&quot;ascatb_esdr_l2_wsderiv_v10&quot;&gt;ASCATB_ESDR_L2_WSDERIV_V1.0&lt;/h4&gt;
This dataset contains the curl and divergence of ocean surface equivalent neutral wind and wind stress, derived from satellite-based scatterometer observations (the MetOp-B ASCAT scatterometer), representing the first science quality release of these data (post-provisional after v1.0) funded under the MEaSUREs program. This product from MetOp-B ASCAT has been intercalibrated with similar scatterometer measurements from instruments on the MetOp-A, ScatSat-1, and QuikScat satellites, all of which can be found on the MEaSUREs OSVW Project Page. These Level 2 data are provided on a non-uniform grid within the satellite swath at ~12.5 km pixel resolution. Each L2 file corresponds to a specific orbital revolution number, which begins at the southernmost point of the ascending orbit - the thumbnail preview shows data for all orbits over a day (typically 14 orbits). Estimates for the curls and divergences are computed over several spatial domains with varying radii from the point of interest, and included as separate variables. &lt;br&gt;&lt;br&gt; The dataset represents the first science quality release funded under the MEaSUREs (Making Earth System Data Records for Use in Research Environments) program. The primary purpose of this release is for science evaluation by the NASA International Ocean Vector Winds Science Team (IOVWST). This V1.0 of the data was derived from V1.1 of the L2 wind and stress product.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ascatb_esdr_l2_wind_stress_v11&quot;&gt;ASCATB_ESDR_L2_WIND_STRESS_V1.1&lt;/h4&gt;
This dataset contains ocean surface wind vectors (equivalent neutral and true 10m) and wind stress vectors derived from satellite-based scatterometer observations (the MetOp-B ASCAT scatterometer), representing the first science quality release of these data (post-provisional after v1.0) funded under the MEaAUREs program. This product from MetOp-B ASCAT has been intercalibrated with similar scatterometer measurements from instruments on the MetOp-A, ScatSat-1, and QuikScat satellites (all of which can be found on the MEaSUREs OSVW Project Page), and if used together create an unbroken record of winds from 1999 to 2022. The wind vector and stress retrievals are provided on a non-uniform grid within the swath (Level 2 (L2) products) at 12.5 km pixel resolution. Each L2 file corresponds to a specific orbital revolution number, which begins at the southernmost point of the ascending orbit. The thumbnail shows data for two orbits - using all orbits for a single day will provide global coverage. &lt;br&gt;&lt;br&gt; The dataset represents the first science quality release funded under the MEaSUREs (Making Earth System Data Records for Use in Research Environments) program. Version 1.1 provides a set of updates and improvements from version 1.0, including: 1) increased data coverage, 2) improved quality control, and 3) new global metadata attributes featuring revolution number, equator crossing longitude, and equator crossing time (UTC). The primary purpose of this release is for science evaluation by the NASA International Ocean Vector Winds Science Team (IOVWST).
&lt;br&gt;&lt;h4 id&#x3D;&quot;ascatb_esdr_l3_wind_stress_v10&quot;&gt;ASCATB_ESDR_L3_WIND_STRESS_V1.0&lt;/h4&gt;
This dataset contains gridded ocean surface wind vectors (equivalent neutral and true 10m) and wind stress vectors derived from satellite-based scatterometer observations (the MetOp-B ASCAT scatterometer), representing the first science quality release of these data funded under the MEaSUREs program. This product from MetOp-B ASCAT has been intercalibrated with similar scatterometer measurements from instruments on the MetOp-A, ScatSat-1, and QuikScat satellites, all of which can be found on the MEaSUREs OSVW Project Page. The wind vector and stress retrievals are provided on a global grid (one per file) at 12.5 km pixel resolution, but data exist only over areas of the globe that fell within one of the satellite swaths/orbits for that day (see thumbnail). &lt;br&gt;&lt;br&gt; The dataset represents the first science quality release funded under the MEaSUREs (Making Earth System Data Records for Use in Research Environments) program. Note that this is the first version of the Level 3 data (V1.0) but they were derived from V1.1 of the Level 2 product. The primary purpose of this release is for science evaluation by the NASA International Ocean Vector Winds Science Team (IOVWST).
&lt;br&gt;&lt;h4 id&#x3D;&quot;quikscat_esdr_ancillary_l2_v11&quot;&gt;QUIKSCAT_ESDR_ANCILLARY_L2_V1.1&lt;/h4&gt;
This dataset contains model output interpolated in space and time to the ESDR product from the scatterometer on the QuikSCAT satellite, representing the first science quality release of these data (post-provisional after v1.0) funded under the MEaAUREs program. These auxiliary fields are included to complement the scatterometer observations, specifically for the QUIKSCAT_ESDR_L2_WIND_STRESS_V1.1 dataset.. Model variables include: i) ocean surface wind fields from ERA-5 short-term forecast (removed from the analyses times to reduce impacts from assimilated scatterometer retrievals at the beginning of the forecast); ii) estimations of precipitation from the GPM IMERG product; iii) estimation of the surface currents from the GlobCurrent project. The modeled ocean surface auxiliary fields are provided on a non-uniform grid within the native L2 QuikSCAT sampled locations at a nominal 12.5 km pixel resolution. Each file corresponds to a specific orbital revolution (rev) number, which begins at the southernmost point of the ascending orbit. The thumbnail shows data for two orbits - using all orbits for a single day will provide global coverage. &lt;br&gt;&lt;br&gt; Version 1.1 provides a set of updates and improvements from version 1.0, including: 1) improved variable metadata, 2) removed the GlobCurrent stokes drift variables, and 3) provided data source metadata including DOIs for the ERA-5, IMERGE, and GlobCurrent data sources. The primary purpose of this release is for science evaluation by the NASA International Ocean Vector Winds Science Team (IOVWST).
&lt;br&gt;&lt;h4 id&#x3D;&quot;quikscat_esdr_l2_wsderiv_v10&quot;&gt;QUIKSCAT_ESDR_L2_WSDERIV_V1.0&lt;/h4&gt;
This dataset contains the curl and divergence of ocean surface equivalent neutral wind and wind stress, derived from satellite-based scatterometer observations aboard QuikScat, representing the first science quality release of these data funded under the MEaSUREs program. This product from QuikScat has been intercalibrated with similar scatterometer measurements from instruments on the MetOp-A, MetOp-B ASCAT, and ScatSat-1 satellites, all of which can be found on the MEaSUREs OSVW Project Page. These Level 2 data are provided on a non-uniform grid within the satellite swath at ~12.5 km pixel resolution. Each L2 file corresponds to a specific orbital revolution number, which begins at the southernmost point of the ascending orbit - the thumbnail preview shows data for all orbits over a day (typically 14 orbits). Estimates for the curls and divergences are computed over several spatial domains with varying radii from the point of interest, and included as separate variables. &lt;br&gt;&lt;br&gt; The dataset represents the first science quality release funded under the MEaSUREs (Making Earth System Data Records for Use in Research Environments) program. The primary purpose of this release is for science evaluation by the NASA International Ocean Vector Winds Science Team (IOVWST). This V1.0 of the data was derived from V1.1 of the L2 wind and stress product.
&lt;br&gt;&lt;h4 id&#x3D;&quot;quikscat_esdr_l2_wind_stress_v11&quot;&gt;QUIKSCAT_ESDR_L2_WIND_STRESS_V1.1&lt;/h4&gt;
This dataset contains ocean surface wind vectors (equivalent neutral and true 10m) and wind stress vectors derived from satellite-based scatterometer observations aboard QuikScat, representing the first science quality release of these data (post-provisional after v1.0) funded under the MEaAUREs program. This product from QuikScat has been intercalibrated with similar scatterometer measurements from instruments on the MetOp-A, MetOp-B, and ScatSat-1 satellites (all of which can be found on the MEaSUREs OSVW Project Page), and if used together create an unbroken record of winds from 1999 to 2022. The wind vector and stress retrievals are provided on a non-uniform grid within the swath (Level 2 (L2) products) at 12.5 km pixel resolution. Each L2 file corresponds to a specific orbital revolution number, which begins at the southernmost point of the ascending orbit. The thumbnail shows data for two orbits - using all orbits for a single day will provide global coverage. &lt;br&gt;&lt;br&gt; The dataset represents the first science quality release funded under the MEaSUREs (Making Earth System Data Records for Use in Research Environments) program. Version 1.1 provides a set of updates and improvements from version 1.0, including: 1) increased data coverage, 2) improved quality control, and 3) new global metadata attributes featuring revolution number, equator crossing longitude, and equator crossing time (UTC). The primary purpose of this release is for science evaluation by the NASA International Ocean Vector Winds Science Team (IOVWST).
&lt;br&gt;&lt;h4 id&#x3D;&quot;quikscat_esdr_l3_wind_stress_v10&quot;&gt;QUIKSCAT_ESDR_L3_WIND_STRESS_V1.0&lt;/h4&gt;
This dataset contains gridded ocean surface wind vectors (equivalent neutral and true 10m) and wind stress vectors derived from satellite-based scatterometer observations aboard QuikScat, representing the first science quality release of these data funded under the MEaSUREs program. This product from QuikScat has been intercalibrated with similar scatterometer measurements from instruments on the MetOp-A, MetOp-B, and ScatSat-1, all of which can be found on the MEaSUREs OSVW Project Page. The wind vector and stress retrievals are provided on a global grid (one per file) at 12.5 km pixel resolution, but data exist only over areas of the globe that fell within one of the satellite swaths/orbits for that day (see thumbnail). &lt;br&gt;&lt;br&gt; The dataset represents the first science quality release funded under the MEaSUREs (Making Earth System Data Records for Use in Research Environments) program. Note that this is the first version of the Level 3 data (V1.0) but they were derived from V1.1 of the Level 2 product. The primary purpose of this release is for science evaluation by the NASA International Ocean Vector Winds Science Team (IOVWST).
&lt;br&gt;&lt;h4 id&#x3D;&quot;scatsat1_esdr_ancillary_l2_v11&quot;&gt;SCATSAT1_ESDR_ANCILLARY_L2_V1.1&lt;/h4&gt;
This dataset contains the first science quality release (post-provisional after v1.0) of the MEaSUREs-funded Earth Science Data Record (ESDR) of ancillary data corresponding to the SCATSAT-1 Level 2 (L2) data products, interpolated in space and time to the scatterometer observations. These auxiliary fields are included to complement those scatterometer observations, specifically for the SCATSAT_ESDR_L2_WIND_STRESS_V1.1 dataset. The fields include: i) ocean surface wind fields from ERA-5 short-term forecast (removed from the analyses times to reduce impacts from assimilated scatterometer retrievals at the beginning of the forecast); ii) collocated in space and time estimations of precipitation from the GPM IMERG product; iii) estimation of the surface currents from the GlobCurrent project. These auxiliary fields are included to complement the scatterometer observation fields and to help in the evaluation process. They are provided on a non-uniform grid within the native L2 SCATSAT-1 sampled locations at a nominal 12.5 km pixel resolution. Each file corresponds to a specific orbital revolution (rev) number, which begins at the southernmost point of the ascending orbit. The thumbnail shows data for two orbits - using all orbits for a single day will provide global coverage. &lt;br&gt;&lt;br&gt; The dataset represents the first science quality release of this product with funding from the MEaSUREs (Making Earth System Data Records for Use in Research Environments) program. Version 1.1 provides a set of updates and improvements from version 1.0, including: 1) improved variable metadata, 2) removed the GlobCurrent stokes drift variables, and 3) provided data source metadata including DOIs for the ERA-5, IMERGE, and GlobCurrent data sources. The primary purpose of this release is for science evaluation by the NASA International Ocean Vector Winds Science Team (IOVWST).
&lt;br&gt;&lt;h4 id&#x3D;&quot;scatsat1_esdr_l2_wsderiv_v10&quot;&gt;SCATSAT1_ESDR_L2_WSDERIV_V1.0&lt;/h4&gt;
This dataset contains the curl and divergence of ocean surface equivalent neutral wind and wind stress, derived from satellite-based scatterometer observations aboard SCATSAT-1, representing the first science quality release of these data funded under the MEaSUREs program. This product from SCATSAT-1 has been intercalibrated with similar scatterometer measurements from instruments on the MetOp-A, MetOp-B, and QuikScat satellites, all of which can be found on the MEaSUREs OSVW Project Page. These Level 2 data are provided on a non-uniform grid within the satellite swath at ~12.5 km pixel resolution. Each L2 file corresponds to a specific orbital revolution number, which begins at the southernmost point of the ascending orbit. There are typically 14 orbits per day, and the thumbnail preview shows coverage for the first ten orbits in an example day. Estimates for the curls and divergences are computed over several spatial domains with varying radii from the point of interest, and included as separate variables. &lt;br&gt;&lt;br&gt; The dataset represents the first science quality release funded under the MEaSUREs (Making Earth System Data Records for Use in Research Environments) program. The primary purpose of this release is for science evaluation by the NASA International Ocean Vector Winds Science Team (IOVWST). This V1.0 of the data was derived from V1.1 of the L2 wind and stress product.
&lt;br&gt;&lt;h4 id&#x3D;&quot;scatsat1_esdr_l2_wind_stress_v11&quot;&gt;SCATSAT1_ESDR_L2_WIND_STRESS_V1.1&lt;/h4&gt;
This dataset contains ocean surface wind vectors (equivalent neutral and true 10m) and wind stress vectors derived from satellite-based scatterometer observations aboard ScatSat-1, representing the first science quality release of these data (post-provisional after v1.0) funded under the MEaAUREs program. This product from ScatSat-1 has been intercalibrated with similar scatterometer measurements from instruments on the MetOp-A, MetOp-B, and QuikScat satellites (all of which can be found on the MEaSUREs OSVW Project Page), and if used together create an unbroken record of winds from 1999 to 2022. The wind vector and stress retrievals are provided on a non-uniform grid within the swath (Level 2 (L2) products) at 12.5 km pixel resolution. Each L2 file corresponds to a specific orbital revolution number, which begins at the southernmost point of the ascending orbit. The thumbnail shows data for two orbits - using all orbits for a single day will provide global coverage.&lt;br&gt;&lt;br&gt; The dataset represents the first science quality release funded under the MEaSUREs (Making Earth System Data Records for Use in Research Environments) program. Version 1.1 provides a set of updates and improvements from version 1.0, including: 1) increased data coverage, 2) improved quality control, and 3) new global metadata attributes featuring revolution number, equator crossing longitude, and equator crossing time (UTC). The primary purpose of this release is for science evaluation by the NASA International Ocean Vector Winds Science Team (IOVWST).
&lt;br&gt;&lt;h4 id&#x3D;&quot;scatsat1_esdr_l3_wind_stress_v10&quot;&gt;SCATSAT1_ESDR_L3_WIND_STRESS_V1.0&lt;/h4&gt;
This dataset contains gridded ocean surface wind vectors (equivalent neutral and true 10m) and wind stress vectors derived from satellite-based scatterometer observations aboard SCATSAT-1, representing the first science quality release of these data funded under the MEaSUREs program. This product from SCATSAT-1 has been intercalibrated with similar scatterometer measurements from instruments on the MetOp-A, MetOp-B, and QuikScat satellites, all of which can be found on the MEaSUREs OSVW Project Page. The wind vector and stress retrievals are provided on a global grid (one per file) at 12.5 km pixel resolution, but data exist only over areas of the globe that fell within one of the satellite swaths/orbits for that day (see thumbnail). &lt;br&gt;&lt;br&gt; The dataset represents the first science quality release funded under the MEaSUREs (Making Earth System Data Records for Use in Research Environments) program. Note that this is the first version of the Level 3 data (V1.0) but they were derived from V1.1 of the Level 2 product. The primary purpose of this release is for science evaluation by the NASA International Ocean Vector Winds Science Team (IOVWST).
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-discovery&quot;&gt;Data Discovery&lt;/h4&gt;
Explore this data using NASA&amp;#39;s &lt;a href&#x3D;&quot;https://search.earthdata.nasa.gov/&quot;&gt;Earthdata Search&lt;/a&gt;, a comprehensive tool for discovering and visualizing Earth science datasets.
&lt;br&gt;&lt;h4 id&#x3D;&quot;data-access&quot;&gt;Data Access&lt;/h4&gt;
Access requires an &lt;a href&#x3D;&quot;https://urs.earthdata.nasa.gov/&quot;&gt;Earthdata Login&lt;/a&gt; account. &lt;a href&#x3D;&quot;https://archive.podaac.earthdata.nasa.gov/s3credentialsREADME&quot;&gt;Read our guide on obtaining AWS credentials&lt;/a&gt; to retrieve this data from AWS.
&lt;br&gt;&lt;br&gt;</description>
    </item>
    <item>
      <title>NASA MISR Project</title>
      <link>https://registry.opendata.aws/nasa-misr</link>
      <guid>https://registry.opendata.aws/nasa-misr</guid>
      <description>MIANACP_1 is the Multi-angle Imaging SpectroRadiometer (MISR) Aerosol Climatology Product version 1. It is 1) the microphysical and scattering characteristics of pure aerosol upon which routine retrievals are based, 2) mixtures of pure aerosol to be compared with MISR observations, and 3) the likelihood value assigned to each mode geographically. The ACP describes mixtures of up to three component aerosol types from a list of eight components in varying proportions. ACP component aerosol particle data quality depends on the ACP input data, which are based on aerosol particles described in the literature and consider MISR-specific sensitivity to particle size, single-scattering albedo, and shape, and shape - roughly: small, medium, and large; dirty and clean; spherical and nonspherical [Kahn et al., 1998; 2001]. Also reported in the ACP are the mixtures of these components used by the retrieval algorithm. The MISR instrument consists of nine push-broom cameras that measure radiance in four spectral bands. Global coverage is achieved in nine days. The cameras are arranged with one camera pointing toward the nadir, four forward, and four aftward. It takes seven minutes for all nine cameras to view the same surface location. The view angles relative to the surface reference ellipsoid are 0, 26.1, 45.6, 60.0, and 70.5 degrees. The spectral band shapes are nominally Gaussian, centered at 443, 555, 670, and 865 nm.
&lt;br&gt;&lt;h4 id&#x3D;&quot;miancagp&quot;&gt;MIANCAGP&lt;/h4&gt;
MIANCAGP_1 is the Multi-angle Imaging SpectroRadiometer (MISR) Ancillary Geographic Product version 1. It is a set of 233 pre-computed files. Each AGP file pertains to a single Terra orbital path. MISR production software relies on information in the AGP, such as digital terrain elevation, as input to the algorithms that generate MISR products. The AGP contains eleven fields of geographical data. This product consists primarily of geolocation data on a Space Oblique Mercator (SOM) Grid. It has 233 parts, corresponding to the 233 repeat orbits of the EOS-AM1 Spacecraft. The MISR instrument consists of nine push-broom cameras that measure radiance in four spectral bands. Global coverage is achieved in nine days. The cameras are arranged with one camera pointing toward the nadir, four forward, and four aftward. It takes seven minutes for all nine cameras to view the exact surface location. The view angles relative to the surface reference ellipsoid are 0, 26.1, 45.6, 60.0, and 70.5 degrees. The spectral band shapes are nominally Gaussian, centered at 443, 555, 670, and 865 nm.
&lt;br&gt;&lt;h4 id&#x3D;&quot;miancarp&quot;&gt;MIANCARP&lt;/h4&gt;
MIANCARP_2 is the Multi-angle Imaging SpectroRadiometer (MISR) Ancillary Radiometric Product version 2. It is composed of 4 files covering instrument characterization data, pre-flight calibration data, in-flight calibration data, and configuration parameters. The MISR instrument consists of nine pushbroom cameras which measure radiance in four spectral bands. Global coverage is achieved in nine days. The cameras are arranged with one camera pointing toward the nadir, four cameras pointing forward, and four cameras pointing aftward. It takes seven minutes for all nine cameras to view the same surface location. The view angles relative to the surface reference ellipsoid, are 0, 26.1, 45.6, 60.0, and 70.5 degrees. The spectral band shapes are nominally Gaussian, centered at 443, 555, 670, and 865 nm.
&lt;br&gt;&lt;h4 id&#x3D;&quot;misbr&quot;&gt;MISBR&lt;/h4&gt;
This is the browse data associated with a particular granule. MISBR_005 is the Multi-angle Imaging SpectroRadiometer (MISR) Browse data version 5. It consists of Ellipsoid color images obtained by each camera resampled to 2. 2 km resolution. The MISR instrument consists of nine pushbroom cameras which measure radiance in four spectral bands. Global coverage is achieved in nine days. The cameras are arranged with one camera pointing toward the nadir, four forward, and four aftward. It takes seven minutes for all nine cameras to view the same surface location. The view angles relative to the surface reference ellipsoid are 0, 26.1, 45.6, 60.0, and 70.5 degrees. The spectral band shapes are nominally Gaussian, centered at 443, 555, 670, and 865 nm.
&lt;br&gt;&lt;h4 id&#x3D;&quot;mirccmf&quot;&gt;MIRCCMF&lt;/h4&gt;
MIRCCMF_001 is the Multi-angle Imaging SpectroRadiometer (MISR) FIRSTLOOK radiometric camera-by-camera Cloud Mask (RCCM) version 1 data product. It was produced using ancillary inputs from the previous time period, such as Radiometric Camera-by-camera Cloud mask Threshold (RCCT). It is used to determine whether a scene is clear, cloudy, or dusty (over the ocean). Data collection for this product is ongoing. FIRSTLOOK processing uses the new time dependence of the Atmospheric and Surface Climatology (TASC) from the same month/previous year. The TASC data set now contains snow-ice and ocean surface wind speed values that are updated on a monthly basis. Therefore, these data sets cannot be generated until the end of the month. Products generated are distinguished by the presence of FIRSTLOOK in the file names. The MISR instrument consists of nine push-broom cameras that measure radiance in four spectral bands. Global coverage is achieved in nine days. The cameras are arranged with one camera pointing toward the nadir, four cameras pointing forward, and four cameras pointing aftward. It takes seven minutes for all nine cameras to view the same surface location. The view angles relative to the surface reference ellipsoid are 0, 26.1, 45.6, 60.0, and 70.5 degrees. The spectral band shapes are nominally Gaussian, centered at 443, 555, 670, and 865 nm. MISR is designed to view Earth with cameras in 9 different directions. As the instrument flies overhead, all nine cameras successfully imaged each piece of Earth&amp;#39;s surface below in 4 wavelengths (blue, green, red, and near-infrared). MISR aims to improve our understanding of the effects of sunlight on Earth and distinguish different types of clouds, particles, and surfaces. Specifically, MISR monitors the monthly, seasonal, and long-term trends in three areas: 1) amount and type of atmospheric particles (aerosols), including those formed by natural sources and by human activities; 2) amounts, types, and heights of clouds, and 3) distribution of land surface cover, including vegetation canopy structure.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atsmigeo&quot;&gt;ATSMIGEO&lt;/h4&gt;
ATSMIGEO_002 is the Multi-angle Imaging SpectroRadiometer (MISR) Geometric Parameters subset for the ARCTAS region version 2. It measures the sun and view angles at the reference ellipsoid. MISR is designed to view Earth with cameras in 9 different directions. As the instrument flies overhead, all nine cameras successfully imaged each piece of Earth&amp;#39;s surface below in 4 wavelengths (blue, green, red, and near-infrared). MISR aims to improve our understanding of the effects of sunlight on Earth and distinguish different types of clouds, particles, and surfaces. Specifically, MISR monitors the monthly, seasonal, and long-term trends in three areas: 1) amount and type of atmospheric particles (aerosols), including those formed by natural sources and by human activities; 2) amounts, types, and heights of clouds, and 3) distribution of land surface cover, including vegetation canopy structure.
&lt;br&gt;&lt;h4 id&#x3D;&quot;gomigeo&quot;&gt;GOMIGEO&lt;/h4&gt;
GOMIGEO_002 is the Multi-angle Imaging SpectroRadiometer (MISR) Geometric Parameters subset for the GoMACCS region version 2. It contains the Geometric Parameters, which measure the sun and view angles at the reference ellipsoid. MISR is designed to view Earth with cameras in 9 different directions. As the instrument flies overhead, all nine cameras successfully imaged each piece of Earth&amp;#39;s surface below in 4 wavelengths (blue, green, red, and near-infrared). MISR aims to improve our understanding of the effects of sunlight on Earth and distinguish different types of clouds, particles, and surfaces. Specifically, MISR monitors the monthly, seasonal, and long-term trends in three areas: 1) amount and type of atmospheric particles (aerosols), including those formed by natural sources and by human activities; 2) amounts, types, and heights of clouds, and 3) distribution of land surface cover, including vegetation canopy structure.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sammigeo&quot;&gt;SAMMIGEO&lt;/h4&gt;
SAMMIGEO_2 is the Multi-angle Imaging SpectroRadiometer (MISR) Geometric Parameters subset for the SAMUM region version 2. It contains the Stereoscopically Derived Cloud Mask (SDCM), cloud winds, and Reflecting Level Reference Altitude (RLRA), with associated data for the SAMUM_2006 theme. The MISR instrument consists of nine push-broom cameras that measure radiance in four spectral bands. Global coverage is achieved in nine days. The cameras are arranged with one camera pointing toward the nadir, four forward, and four aftward. It takes seven minutes for all nine cameras to view the same surface location. The view angles relative to the surface reference ellipsoid are 0, 26.1, 45.6, 60.0, and 70.5 degrees. The spectral band shapes are nominally Gaussian, centered at 443, 555, 670, and 865 nm.
&lt;br&gt;&lt;h4 id&#x3D;&quot;vbemigeo&quot;&gt;VBEMIGEO&lt;/h4&gt;
VBEMIGEO_002 is the Multi-angle Imaging SpectroRadiometer (MISR) Geometric Parameters subset for the VBBE region version 2. It contains the Geometric Parameters that measure the sun and view angles at the reference ellipsoid. The MISR instrument consists of nine push-broom cameras that measure radiance in four spectral bands. Global coverage is achieved in nine days. The cameras are arranged with one camera pointing toward the nadir, four forward, and four aftward. It takes seven minutes for all nine cameras to view the same surface location. The view angles relative to the surface reference ellipsoid are 0, 26.1, 45.6, 60.0, and 70.5 degrees. The spectral band shapes are nominally Gaussian, centered at 443, 555, 670, and 865 nm. MISR is designed to view Earth with cameras in 9 different directions. As the instrument flies overhead, all nine cameras successfully imaged each piece of Earth&amp;#39;s surface below in 4 wavelengths (blue, green, red, and near-infrared). MISR aims to improve our understanding of the effects of sunlight on Earth and distinguish different types of clouds, particles, and surfaces. Specifically, MISR monitors the monthly, seasonal, and long-term trends in three areas: 1) amount and type of atmospheric particles (aerosols), including those formed by natural sources and by human activities; 2) amounts, types, and heights of clouds, and 3) distribution of land surface cover, including vegetation canopy structure.
&lt;br&gt;&lt;h4 id&#x3D;&quot;mib2geop&quot;&gt;MIB2GEOP&lt;/h4&gt;
Multi-angle Imaging SpectroRadiometer (MISR) is designed to view Earth with cameras pointed in 9 different directions. As the instrument flies overhead, each piece of Earth&amp;#39;s surface below is successfully imaged by all nine cameras in 4 wavelengths (blue, green, red, and near-infrared). The goal of MISR is to improve our understanding of the fate of sunlight in Earth&amp;#39;s environment and distinguish different types of clouds, particles, and surfaces. Specifically, MISR monitors the monthly, seasonal, and long-term trends in three areas: 1) amount and type of atmospheric particles (aerosols), including those formed by natural sources and by human activities; 2) amounts, types, and heights of clouds, and 3) distribution of land surface cover, including vegetation canopy structure. MISR Geometric Parameters V002 contains the Geometric Parameters which measure the sun and view angles at the reference ellipsoid
&lt;br&gt;&lt;h4 id&#x3D;&quot;mib2geop-1&quot;&gt;MIB2GEOP&lt;/h4&gt;
MIB2GEOP_003 is the Multi-angle Imaging SpectroRadiometer (MISR) Geometric Parameters Version 3 product. It contains the Geometric Parameters which measure the sun and view angles at the reference ellipsoid. Data collection for this product is ongoing. The distribution format of this product is NetCDF-4 which is a migration from the previous version&amp;#39;s format of HDF-EOS2. MISR itself is an instrument designed to view Earth with cameras pointed in 9 different directions. As the instrument flies overhead, each piece of Earth&amp;#39;s surface below is successively imaged by all 9 cameras, in each of 4 wavelengths (blue, green, red, and near-infrared). The goal of MISR is to improve our understanding of the affects of sunlight on Earth, as well as distinguish different types of clouds, particles and surfaces. Specifically, MISR monitors the monthly, seasonal, and long-term trends in three areas: 1) amount and type of atmospheric particles (aerosols), including those formed by natural sources and by human activities; 2) amounts, types, and heights of clouds, and 3) distribution of land surface cover, including vegetation canopy structure.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atsmib2e&quot;&gt;ATSMIB2E&lt;/h4&gt;
ATSMIB2E_003 is the Multi-angle Imaging SpectroRadiometer (MISR) Level 1B2 Ellipsoid Product subset for the ARCTAS region. It contains an Ellipsoid-projected TOA Radiance subset for the ARCTAS region, resampled at the surface and topographically corrected and geometrically corrected by PGE22. MISR is designed to view Earth with cameras in 9 different directions. As the instrument flies overhead, all nine cameras successfully imaged each piece of Earth&amp;#39;s surface below in 4 wavelengths (blue, green, red, and near-infrared). MISR aims to improve our understanding of the effects of sunlight on Earth and distinguish different types of clouds, particles, and surfaces. Specifically, MISR monitors the monthly, seasonal, and long-term trends in three areas: 1) amount and type of atmospheric particles (aerosols), including those formed by natural sources and by human activities; 2) amounts, types, and heights of clouds, and 3) distribution of land surface cover, including vegetation canopy structure.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ricmib2e&quot;&gt;RICMIB2E&lt;/h4&gt;
RICMIB2E_002 is the Multi-angle Imaging SpectroRadiometer (MISR) Level 1B2 Ellipsoid Product subset for the RICO region version 2. It contains the ellipsoid projected TOA Radiance over the RICO region, resampled to WGS84 ellipsoid corrected, and it requires the radiances from all nine cameras of MISR to be projected to a surface defined by the reference WGS84 ellipsoid. On this surface, the camera-to-camera stereo matching will be performed to determine cloud altitude. Topographic distortions are removed. Corrections due to errors in the supplied Navigation and attitude data are obtained during Terrain-projected parameter processing and are applied to these parameters. The MISR instrument consists of nine push-broom cameras that measure radiance in four spectral bands. Global coverage is achieved in nine days. The cameras are arranged with one camera pointing toward the nadir, four forward, and four aftward. It takes seven minutes for all nine cameras to view the same surface location. The view angles relative to the surface reference ellipsoid are 0, 26.1, 45.6, 60.0, and 70.5 degrees. The spectral band shapes are nominally Gaussian, centered at 443, 555, 670, and 865 nm.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sammib2e&quot;&gt;SAMMIB2E&lt;/h4&gt;
SAMMIB2E_3 is the Multi-angle Imaging SpectroRadiometer (MISR) Level 1B2 Ellipsoid Product subset for the SAMUM region version 1. It contains Ellipsoid-projected TOA Radiance, resampled at the surface and topographically corrected and geometrically corrected by PGE22 for the SAMUM_2006 theme. The MISR instrument consists of nine push-broom cameras that measure radiance in four spectral bands. Global coverage is achieved in nine days. The cameras are arranged with one camera pointing toward the nadir, four forward, and four aftward. It takes seven minutes for all nine cameras to view the same surface location. The view angles relative to the surface reference ellipsoid are 0, 26.1, 45.6, 60.0, and 70.5 degrees. The spectral band shapes are nominally Gaussian, centered at 443, 555, 670, and 865 nm.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atsmib2t&quot;&gt;ATSMIB2T&lt;/h4&gt;
ATSMIB2T_003 is the Multi-angle Imaging SpectroRadiometer (MISR) Level 1B2 Terrain Product subset for the ARCTAS region version 3. It contains a Terrain-projected TOA Radiance subset for the ARCTAS region, resampled at the surface and topographically corrected and geometrically corrected by PGE22. MISR is designed to view Earth with cameras in 9 different directions. As the instrument flies overhead, all nine cameras successfully imaged each piece of Earth&amp;#39;s surface below in 4 wavelengths (blue, green, red, and near-infrared). MISR aims to improve our understanding of the effects of sunlight on Earth and distinguish different types of clouds, particles, and surfaces. Specifically, MISR monitors the monthly, seasonal, and long-term trends in three areas: 1) amount and type of atmospheric particles (aerosols), including those formed by natural sources and by human activities; 2) amounts, types, and heights of clouds, and 3) distribution of land surface cover, including vegetation canopy structure.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sammib2t&quot;&gt;SAMMIB2T&lt;/h4&gt;
SAMMIB2T_3 is the Multi-angle Imaging SpectroRadiometer (MISR) Level 1B2 Terrain Product subset for the SAMUM region version 3. It contains Terrain-projected TOA Radiance, resampled at the surface and topographically corrected, as well as geometrically corrected by PGE22 for the SAMUM_2006 theme. The MISR instrument consists of nine push-broom cameras that measure radiance in four spectral bands. Global coverage is achieved in nine days. The cameras are arranged with one camera pointing toward the nadir, four forward, and four aftward. It takes seven minutes for all nine cameras to view the same surface location. The view angles relative to the surface reference ellipsoid are 0, 26.1, 45.6, 60.0, and 70.5 degrees. The spectral band shapes are nominally Gaussian, centered at 443, 555, 670, and 865 nm.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ricmircm&quot;&gt;RICMIRCM&lt;/h4&gt;
RICMIRCM_004 is the Multi-angle Imaging SpectroRadiometer (MISR) Level 1B3 Radiometric Camera-by-camera Cloud Mask Product subset for the RICO region version 4. This file contains the Radiometric camera-by-camera Cloud Mask dataset over the RICO region. It is used during geophysical parameter retrievals to determine whether a scene is classified as clear or cloudy. A new parameter has been added to indicate dust over ocean. This version of the ESDT is used by MISR PGE 13. In the TOA/Cloud Product, RCCM is combined with a stereoscopically derived cloud mask to 1) establish values of the Reflecting Level Reference Altitude, 2) determine how a scene is classified for choosing angular integration coefficients for establishing TOA albedos, and 3) calculate regional scene classifiers. Retrieval of Aerosol/Surface Product properties requires the absence of clouds for retrieval assumptions to be valid. The MISR instrument consists of nine push-broom cameras that measure radiance in four spectral bands. Global coverage is achieved in nine days. The cameras are arranged with one camera pointing toward the nadir, four forward, and four aftward. It takes seven minutes for all nine cameras to view the same surface location. The view angles relative to the surface reference ellipsoid are 0, 26.1, 45.6, 60.0, and 70.5 degrees. The spectral band shapes are nominally Gaussian, centered at 443, 555, 670, and 865 nm.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cmrmiaae&quot;&gt;CMRMIAAE&lt;/h4&gt;
CMRMIAAE_2 is the Multi-angle Imaging SpectroRadiometer (MISR) Level 2 Aerosol Product subset for the C-MARE Region version 2. It contains aerosol optical depth, ancillary meteorological data, and related parameters on a 17.6 km grid for the CMARE_2004 theme. To study the magnitude and natural variability in space and time of sunlight and cloud interactions with aerosols in the earth&amp;#39;s atmosphere and to determine their effect on climate; to improve knowledge of sources, sinks, and regional budgets of aerosols; and to provide atmospheric correction inputs for surface imaging data acquired by MISR and other instruments that are simultaneously viewing the same portion of the Earth, to make better quantitative estimates of surface reflectance. MISR is designed to view Earth with cameras in 9 different directions. As the instrument flies overhead, all nine cameras successfully imaged each piece of Earth&amp;#39;s surface below in 4 wavelengths (blue, green, red, and near-infrared). MISR aims to improve our understanding of the effects of sunlight on Earth and distinguish different types of clouds, particles, and surfaces. Specifically, MISR monitors the monthly, seasonal, and long-term trends in three areas: 1) amount and type of atmospheric particles (aerosols), including those formed by natural sources and by human activities; 2) amounts, types, and heights of clouds, and 3) distribution of land surface cover, including vegetation canopy structure.
&lt;br&gt;&lt;h4 id&#x3D;&quot;carmiaae&quot;&gt;CARMIAAE&lt;/h4&gt;
CARMIAAE_002 is the MISR L2 Aerosol Product subset for the ICARTT region V002 product. It contains aerosol optical depth and particle type, with associated atmospheric data over the region covered by the ICARTT_2004 theme. MISR is designed to view Earth with cameras in 9 different directions. As the instrument flies overhead, all nine cameras successfully imaged each piece of Earth&amp;#39;s surface below in 4 wavelengths (blue, green, red, and near-infrared). MISR aims to improve our understanding of the effects of sunlight on Earth and distinguish different types of clouds, particles, and surfaces. Specifically, MISR monitors the monthly, seasonal, and long-term trends in three areas: 1) amount and type of atmospheric particles (aerosols), including those formed by natural sources and by human activities; 2) amounts, types, and heights of clouds, and 3) distribution of land surface cover, including vegetation canopy structure.
&lt;br&gt;&lt;h4 id&#x3D;&quot;ricmiaae&quot;&gt;RICMIAAE&lt;/h4&gt;
RICMIAAE_002 is the Multi-angle Imaging SpectroRadiometer (MISR) Level 2 Aerosol Product subset for the RICO region version 2. It contains Aerosol optical depth and particle type, with associated atmospheric data over the RICO region. The MISR instrument consists of nine push-broom cameras that measure radiance in four spectral bands. Global coverage is achieved in nine days. The cameras are arranged with one camera pointing toward the nadir, four forward, and four aftward. It takes seven minutes for all nine cameras to view the same surface location. The view angles relative to the surface reference ellipsoid are 0, 26.1, 45.6, 60.0, and 70.5 degrees. The spectral band shapes are nominally Gaussian, centered at 443, 555, 670, and 865 nm.
&lt;br&gt;&lt;h4 id&#x3D;&quot;sammi2ae&quot;&gt;SAMMI2AE&lt;/h4&gt;
SAMMI2AE_002 is the Multi-angle Imaging SpectroRadiometer (MISR) Level 2 Aerosol Product subset for the SAMUM region Version 2. It contains Aerosol optical depth and particle type, with associated atmospheric data for the SAMUM_2006 theme. The MISR instrument consists of nine push-broom cameras that measure radiance in four spectral bands. Global coverage is achieved in nine days. The cameras are arranged with one camera pointing toward the nadir, four forward, and four aftward. It takes seven minutes for all nine cameras to view the same surface location. The view angles relative to the surface reference ellipsoid are 0, 26.1, 45.6, 60.0, and 70.5 degrees. The spectral band shapes are nominally Gaussian, centered at 443, 555, 670, and 865 nm.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atsm2aef&quot;&gt;ATSM2AEF&lt;/h4&gt;
ATSM2AEF_001 is the Multi-angle Imaging SpectroRadiometer (MISR) Level 2 FIRSTLOOK Aerosol Product subset for the ARCTAS region version 1 data product. It contains Aerosol optical depth and particle type, with associated atmospheric data produced using ancillary inputs from the previous time period. Data collection for this product is complete. FIRSTLOOK processing uses the new time dependence of the Atmospheric and Surface Climatology (TASC) from the same month/previous year. The TASC data set now contains snow-ice and ocean surface wind speed values that are updated on a monthly basis. Therefore, these data sets cannot be generated until the end of the month. Products generated are distinguished by the presence of FIRSTLOOK in the file names. The MISR instrument consists of nine push-broom cameras that measure radiance in four spectral bands. Global coverage is achieved in nine days. The cameras are arranged with one camera pointing toward the nadir, four forward, and four aftward. It takes seven minutes for all nine cameras to view the same surface location. The view angles relative to the surface reference ellipsoid are 0, 26.1, 45.6, 60.0, and 70.5 degrees. The spectral band shapes are nominally Gaussian, centered at 443, 555, 670, and 865 nm. MISR is designed to view Earth with cameras in 9 different directions. As the instrument flies overhead, each piece of Earth&amp;#39;s surface below is successfully imaged by all nine cameras in 4 wavelengths (blue, green, red, and near-infrared). The goal of MISR is to improve our understanding of the fate of sunlight in Earth&amp;#39;s environment and distinguish different types of clouds, particles, and surfaces. Specifically, MISR monitors the monthly, seasonal, and long-term trends in three areas: 1) amount and type of atmospheric particles (aerosols), including those formed by natural sources and by human activities; 2) amounts, types, and heights of clouds, and 3) distribution of land surface cover, including vegetation canopy structure.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atsm2lsf&quot;&gt;ATSM2LSF&lt;/h4&gt;
ATSM2LSF_001 is the Multi-angle Imaging SpectroRadiometer (MISR) Level 2 FIRSTLOOK Land Surface Product subset for the ARCTAS region version 1. It contains directional reflectance properties, albedo (spectral and PAR integrated), FPAR, radiation parameters, and terrain-referenced geometric parameters produced using ancillary input from the previous time period. Data collection for this product is complete. FIRSTLOOK processing uses the new time dependence of the Atmospheric and Surface Climatology (TASC) from the same month/previous year. The TASC data set now contains snow-ice and ocean surface wind speed values that are updated on a monthly basis. Therefore, these data sets cannot be generated until the end of the month. Products generated are distinguished by the presence of FIRSTLOOK in the file names. The MISR instrument consists of nine push-broom cameras that measure radiance in four spectral bands. Global coverage is achieved in nine days. The cameras are arranged with one camera pointing toward the nadir, four forward, and four aftward. It takes seven minutes for all nine cameras to view the same surface location. The view angles relative to the surface reference ellipsoid are 0, 26.1, 45.6, 60.0, and 70.5 degrees. The spectral band shapes are nominally Gaussian, centered at 443, 555, 670, and 865 nm. MISR is designed to view Earth with cameras in 9 different directions. As the instrument flies overhead, all nine cameras successfully imaged each piece of Earth&amp;#39;s surface below in 4 wavelengths (blue, green, red, and near-infrared). MISR aims to improve our understanding of the effects of sunlight on Earth and distinguish different types of clouds, particles, and surfaces. Specifically, MISR monitors the monthly, seasonal, and long-term trends in three areas: 1) amount and type of atmospheric particles (aerosols), including those formed by natural sources and by human activities; 2) amounts, types, and heights of clouds, and 3) distribution of land surface cover, including vegetation canopy structure.
&lt;br&gt;&lt;h4 id&#x3D;&quot;atsm2stf&quot;&gt;ATSM2STF&lt;/h4&gt;
ATSM2STF_001 is the Multi-angle Imaging SpectroRadiometer (MISR) Level 2 FIRSTLOOK TOA/Cloud Stereo Product subset for the ARCTAS region version 1. It contains the Stereoscopically Derived winds, heights, and cloud mask, along with associated data, produced using ancillary inputs (TASC) from the previous time period. Data collection for this product is complete. FIRSTLOOK processing uses the new time dependence of the Atmospheric and Surface Climatology (TASC) from the same month/previous year. The TASC data set now contains snow-ice and ocean surface wind speed values that are updated on a monthly basis. Therefore, these data sets cannot be generated until the end of the month. Products generated are distinguished by the presence of FIRSTLOOK in the file names. The MISR instrument consists of nine push-broom cameras that measure radiance in four spectral bands. Global coverage is achieved in nine days. The cameras are arranged with one camera pointing toward the nadir, four forward, and four aftward. It takes seven minutes for all nine cameras to view the same surface location. The view angles relative to the surface reference ellipsoid are 0, 26.1, 45.6, 60.0, and 70.5 degrees. The spectral band shapes are nominally Gaussian, centered at 443, 555, 670, and 865 nm. MISR is designed to view Earth with cameras in 9 different directions. As the instrument flies overhead, all nine cameras successfully imaged each piece of Earth&amp;#39;s surface below in 4 wavelengths (blue, green, red, and near-infrared). MISR aims to improve our understanding of the effects of sunlight on Earth and distinguish different types of clouds, particles, and surfaces. Specifically, MISR monitors the monthly, seasonal, and long-term trends in three areas: 1) amount and type of atmospheric particles (aerosols), including those formed by natural sources and by human activities; 2) amounts, types, and heights of clouds, and 3) distribution of land surface cover, including vegetation canopy structure.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cmrmigeo&quot;&gt;CMRMIGEO&lt;/h4&gt;
CMRMIGEO_2 is the Multi-angle Imaging SpectroRadiometer (MISR) Level 2 Geometric Parameters subset for the C-MARE Region version 2. It contains the geometric parameters which measure the sun and view angles at the reference ellipsoid for the region covered by the CMARE_2004 theme. MISR is designed to view Earth with cameras in 9 different directions. As the instrument flies overhead, all nine cameras successfully imaged each piece of Earth&amp;#39;s surface below in 4 wavelengths (blue, green, red, and near-infrared). MISR aims to improve our understanding of the effects of sunlight on Earth and distinguish different types of clouds, particles, and surfaces. Specifically, MISR monitors the monthly, seasonal, and long-term trends in three areas: 1) amount and type of atmospheric particles (aerosols), including those formed by natural sources and by human activities; 2) amounts, types, and heights of clouds, and 3) distribution of land surface cover, including vegetation canopy structure.
&lt;br&gt;&lt;h4 id&#x3D;&quot;cmrmials&quot;&gt;CMRMIALS&lt;/h4&gt;
CMRMIALS_2 is the MISR L2 Land Surface Product subset for the C-MARE Region V002. It contains albedo and BRF data for the region covered by the CMARE_2004 t