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The dataset generation failed
Error code:   DatasetGenerationError
Exception:    TypeError
Message:      Couldn't cast array of type
struct<temporalExtentStart: string, seCorner: struct<crs: string, latitude: double, longitude: double, height: null>, cmrId: string, globalId: string, pagerank_publication_dataset: double, abstract: string, daac: string, nwCorner: struct<crs: string, latitude: double, longitude: double, height: null>, temporalFrequency: string, temporalExtentEnd: string, shortName: string, landingPageUrl: string, longName: string, doi: string, year: string, title: string, authors: string, url: string, Type: string>
to
{'temporalExtentStart': Value(dtype='string', id=None), 'seCorner': {'crs': Value(dtype='string', id=None), 'latitude': Value(dtype='float64', id=None), 'longitude': Value(dtype='float64', id=None), 'height': Value(dtype='null', id=None)}, 'cmrId': Value(dtype='string', id=None), 'globalId': Value(dtype='string', id=None), 'pagerank_publication_dataset': Value(dtype='float64', id=None), 'abstract': Value(dtype='string', id=None), 'daac': Value(dtype='string', id=None), 'nwCorner': {'crs': Value(dtype='string', id=None), 'latitude': Value(dtype='float64', id=None), 'longitude': Value(dtype='float64', id=None), 'height': Value(dtype='null', id=None)}, 'temporalFrequency': Value(dtype='string', id=None), 'temporalExtentEnd': Value(dtype='string', id=None), 'shortName': Value(dtype='string', id=None), 'landingPageUrl': Value(dtype='string', id=None), 'doi': Value(dtype='string', id=None), 'longName': Value(dtype='string', id=None)}
Traceback:    Traceback (most recent call last):
                File "/src/services/worker/.venv/lib/python3.9/site-packages/datasets/builder.py", line 1870, in _prepare_split_single
                  writer.write_table(table)
                File "/src/services/worker/.venv/lib/python3.9/site-packages/datasets/arrow_writer.py", line 622, in write_table
                  pa_table = table_cast(pa_table, self._schema)
                File "/src/services/worker/.venv/lib/python3.9/site-packages/datasets/table.py", line 2292, in table_cast
                  return cast_table_to_schema(table, schema)
                File "/src/services/worker/.venv/lib/python3.9/site-packages/datasets/table.py", line 2245, in cast_table_to_schema
                  arrays = [
                File "/src/services/worker/.venv/lib/python3.9/site-packages/datasets/table.py", line 2246, in <listcomp>
                  cast_array_to_feature(
                File "/src/services/worker/.venv/lib/python3.9/site-packages/datasets/table.py", line 1795, in wrapper
                  return pa.chunked_array([func(chunk, *args, **kwargs) for chunk in array.chunks])
                File "/src/services/worker/.venv/lib/python3.9/site-packages/datasets/table.py", line 1795, in <listcomp>
                  return pa.chunked_array([func(chunk, *args, **kwargs) for chunk in array.chunks])
                File "/src/services/worker/.venv/lib/python3.9/site-packages/datasets/table.py", line 2108, in cast_array_to_feature
                  raise TypeError(f"Couldn't cast array of type\n{_short_str(array.type)}\nto\n{_short_str(feature)}")
              TypeError: Couldn't cast array of type
              struct<temporalExtentStart: string, seCorner: struct<crs: string, latitude: double, longitude: double, height: null>, cmrId: string, globalId: string, pagerank_publication_dataset: double, abstract: string, daac: string, nwCorner: struct<crs: string, latitude: double, longitude: double, height: null>, temporalFrequency: string, temporalExtentEnd: string, shortName: string, landingPageUrl: string, longName: string, doi: string, year: string, title: string, authors: string, url: string, Type: string>
              to
              {'temporalExtentStart': Value(dtype='string', id=None), 'seCorner': {'crs': Value(dtype='string', id=None), 'latitude': Value(dtype='float64', id=None), 'longitude': Value(dtype='float64', id=None), 'height': Value(dtype='null', id=None)}, 'cmrId': Value(dtype='string', id=None), 'globalId': Value(dtype='string', id=None), 'pagerank_publication_dataset': Value(dtype='float64', id=None), 'abstract': Value(dtype='string', id=None), 'daac': Value(dtype='string', id=None), 'nwCorner': {'crs': Value(dtype='string', id=None), 'latitude': Value(dtype='float64', id=None), 'longitude': Value(dtype='float64', id=None), 'height': Value(dtype='null', id=None)}, 'temporalFrequency': Value(dtype='string', id=None), 'temporalExtentEnd': Value(dtype='string', id=None), 'shortName': Value(dtype='string', id=None), 'landingPageUrl': Value(dtype='string', id=None), 'doi': Value(dtype='string', id=None), 'longName': Value(dtype='string', id=None)}
              
              The above exception was the direct cause of the following exception:
              
              Traceback (most recent call last):
                File "/src/services/worker/src/worker/job_runners/config/parquet_and_info.py", line 1438, in compute_config_parquet_and_info_response
                  parquet_operations = convert_to_parquet(builder)
                File "/src/services/worker/src/worker/job_runners/config/parquet_and_info.py", line 1050, in convert_to_parquet
                  builder.download_and_prepare(
                File "/src/services/worker/.venv/lib/python3.9/site-packages/datasets/builder.py", line 924, in download_and_prepare
                  self._download_and_prepare(
                File "/src/services/worker/.venv/lib/python3.9/site-packages/datasets/builder.py", line 1000, in _download_and_prepare
                  self._prepare_split(split_generator, **prepare_split_kwargs)
                File "/src/services/worker/.venv/lib/python3.9/site-packages/datasets/builder.py", line 1741, in _prepare_split
                  for job_id, done, content in self._prepare_split_single(
                File "/src/services/worker/.venv/lib/python3.9/site-packages/datasets/builder.py", line 1897, in _prepare_split_single
                  raise DatasetGenerationError("An error occurred while generating the dataset") from e
              datasets.exceptions.DatasetGenerationError: An error occurred while generating the dataset

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type
string
id
string
labels
sequence
properties
dict
node
0
[ "Dataset" ]
{ "temporalExtentStart": "1992-01-01T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -79.7, "longitude": 180, "height": null }, "cmrId": "C2617226208-POCLOUD", "globalId": "dcf602c1-0e51-55f1-97fb-dbfb8a704c0f", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "This European Remote Sensing (ERS) Sigma-0 dataset is generated by the Scatterometer Climate Record Pathfinder (SCP) project at Brigham Young University (BYU) and is generated using a Scatterometer Image Reconstruction (SIR) technique developed by Dr. David Long at BYU. The dataset provides SIR processed Sigma-0 data from the ERS-1 C-band scatterometer, which is also known as the Active Microwave Instrument (AMI). AMI is a multimode radar operating at a frequency of 5.3 GHz (C-band), using vertically polarized antennas for both transmission and reception. The SIR technique results in an enhanced resolution image reconstruction and gridded on an equal-area grid (for non-polar regions) at 8.9 km pixel resolution stored in SIR files; polar regions are gridded at the same resolution using a polar-stereographic technique. A non-enhanced version is provided at 44.5 km pixel resolution in a format known as GRD (i.e., gridded) files. All files are produced in IEEE formatted binary. All data files are separated and organized by region, parameter, and sampling technique (i.e., SIR vs. GRD). The regions of China and Japan are combined into a single region. In addition to Sigma-0, various statistical parameters are provided for added guidance, including but not limited to: standard deviation, measurement counts, pixel time, Sigma-0 error, and average incidence angle. This dataset was once distributed on tape, but has been made available on FTP thanks to the BYU SCP.", "daac": "NASA/JPL/PODAAC", "nwCorner": { "crs": "wgs-84", "latitude": 88.2, "longitude": -180, "height": null }, "temporalFrequency": "Unknown", "temporalExtentEnd": "1996-05-17T23:59:59.000Z", "shortName": "ERS-1_BYU_L3_OW_SIGMA0_ENHANCED", "landingPageUrl": "https://archive.podaac.earthdata.nasa.gov/podaac-ops-cumulus-docs/ers1/open/L3/byu_scp/sigma0enhanced/docs/dLongERS1.html", "doi": "10.5067/ERS1B-SNEN0", "longName": "ERS-1 Gridded Level 3 Enhanced Resolution Sigma-0 from BYU" }
node
1
[ "Dataset" ]
{ "temporalExtentStart": "1996-09-15T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -89, "longitude": 180, "height": null }, "cmrId": "C2617226510-POCLOUD", "globalId": "592102e7-47ed-52f0-bde4-7a9bfa18ed5b", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "This NASA Scatterometer (NSCAT) satellite Sigma-0 dataset is generated by the Scatterometer Climate Record Pathfinder (SCP) project at Brigham Young University (BYU) and is generated using a Scatterometer Image Reconstruction (SIR) technique developed by Dr. David Long. The SIR technique results in an enhanced resolution image reconstruction and gridded on an equal-area grid (for non-polar regions) at 4.45 km pixel resolution stored in SIR files; polar regions are gridded using a polar-stereographic technique. A non-enhanced version is provided at 22.25 km pixel resolution in a format known as GRD files. All files are produced in IEEE formatted binary. All data files are separated and organized by region, polarization, parameter, and sampling technique (i.e., SIR vs. GRD). The regions of China and Japan are combined into a single region. In additional to Sigma-0, various statistical parameters are provided for added guidance, including but not limited to: standard deviation, measurement counts, pixel time, Sigma-0 error, and average incidence angle. For more information, please visti: http://www.scp.byu.edu/docs/NSCAT_user_notes.html", "daac": "NASA/JPL/PODAAC", "nwCorner": { "crs": "wgs-84", "latitude": 89, "longitude": -180, "height": null }, "temporalFrequency": "Unknown", "temporalExtentEnd": "1997-06-29T23:59:59.999Z", "shortName": "NSCAT_BYU_L3_OW_SIGMA0_ENHANCED", "landingPageUrl": "https://archive.podaac.earthdata.nasa.gov/podaac-ops-cumulus-docs/nscat/open/L3/byu_scp/sigma0enhanced/docs/dLongNscat.html", "doi": "10.5067/NSBYU-SNEN0", "longName": "NSCAT Gridded Level 3 Enhanced Resolution Sigma-0 from BYU" }
node
2
[ "Dataset" ]
{ "temporalExtentStart": "1996-06-03T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -79.7, "longitude": 180, "height": null }, "cmrId": "C2617226211-POCLOUD", "globalId": "9fa7db56-a9a2-5313-949e-4b30a3a2fbbf", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "This European Remote Sensing (ERS) Sigma-0 dataset is generated by the Scatterometer Climate Record Pathfinder (SCP) project at Brigham Young University (BYU) and is generated using a Scatterometer Image Reconstruction (SIR) technique developed by Dr. David Long at BYU. The dataset provides SIR processed Sigma-0 data from the ERS-2 C-band scatterometer, which is also known as the Active Microwave Instrument (AMI). AMI is a multimode radar operating at a frequency of 5.3 GHz (C-band), using vertically polarized antennas for both transmission and reception. The SIR technique results in an enhanced resolution image reconstruction and gridded on an equal-area grid (for non-polar regions) at 8.9 km pixel resolution stored in SIR files; polar regions are gridded at the same resolution using a polar-stereographic technique. A non-enhanced version is provided at 44.5 km pixel resolution in a format known as GRD (i.e., gridded) files. All files are produced in IEEE formatted binary. All data files are separated and organized by region, parameter, and sampling technique (i.e., SIR vs. GRD). The regions of China and Japan are combined into a single region. In addition to Sigma-0, various statistical parameters are provided for added guidance, including but not limited to: standard deviation, measurement counts, pixel time, Sigma-0 error, and average incidence angle. This dataset was once distributed on tape, but has been made available on FTP thanks to the BYU SCP. For more information, please visit: http://www.scp.byu.edu/docs/ERS_user_notes.html", "daac": "NASA/JPL/PODAAC", "nwCorner": { "crs": "wgs-84", "latitude": 88.2, "longitude": -180, "height": null }, "temporalFrequency": "Unknown", "temporalExtentEnd": "2001-12-30T23:59:59.000Z", "shortName": "ERS-2_BYU_L3_OW_SIGMA0_ENHANCED", "landingPageUrl": "https://archive.podaac.earthdata.nasa.gov/podaac-ops-cumulus-docs/ers2/open/L3/byu_scp/sigma0enhanced/docs/dLongERS2.html", "doi": "10.5067/ERS2B-SNEN0", "longName": "ERS-2 Gridded Level 3 Enhanced Resolution Sigma-0 from BYU" }
node
3
[ "Dataset" ]
{ "temporalExtentStart": "2013-08-01T13:09:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -68, "longitude": 0, "height": null }, "cmrId": "C2499940523-POCLOUD", "globalId": "99f70249-9d33-5647-8c57-e933c124e2e1", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "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.", "daac": "NASA/JPL/PODAAC", "nwCorner": { "crs": "wgs-84", "latitude": 68, "longitude": -155, "height": null }, "temporalFrequency": "hourly", "temporalExtentEnd": "2018-01-08T15:29:19.000Z", "shortName": "GOES13-OSPO-L2P-v1.0", "landingPageUrl": null, "doi": "10.5067/GHG13-2PO02", "longName": "GHRSST Level 2P Western Atlantic Regional Skin Sea Surface Temperature from the Geostationary Operational Environmental Satellites (GOES) Imager on the GOES-13 satellite (GDS version 2)" }
node
4
[ "Dataset" ]
{ "temporalExtentStart": "2013-08-01T09:32:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -80, "longitude": 180, "height": null }, "cmrId": "C2499940520-POCLOUD", "globalId": "52ee160f-d9ad-5481-8196-b475c3da166a", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "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'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.", "daac": "NASA/JPL/PODAAC", "nwCorner": { "crs": "wgs-84", "latitude": 79, "longitude": 64, "height": null }, "temporalFrequency": "hourly", "temporalExtentEnd": "2015-12-04T11:15:00.000Z", "shortName": "MTSAT2-OSPO-L2P-v1.0", "landingPageUrl": "http://www.star.nesdis.noaa.gov/sod/mecb/goes_validation/test/top_background.php", "doi": "10.5067/GHMT2-2PO02", "longName": "GHRSST Level 2P Western Pacific Regional Skin Sea Surface Temperature from the Multifunctional Transport Satellite 2 (MTSAT-2) (GDS version 2)" }
node
5
[ "Dataset" ]
{ "temporalExtentStart": "2010-01-01T14:30:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -60, "longitude": -15, "height": null }, "cmrId": "C2499940522-POCLOUD", "globalId": "2af067fb-a040-5e22-9d3e-f25267c07af0", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "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 realtime 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 multispectralalgorithm. Due to the lack of 12 micrometer channel in the GOES 13 imager, SST retrieval is not possiblein daytime conditions. Atmospheric profiles of water vapor and temperature from a numericalweather prediction model, together with a radiatiave transfer model, are used to correct themultispectral 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 thenproduced by remapping over a 0.05 degree regular grid (60S-60N and 135W-15W) SST fieldsobtained by aggregating 30 minute SST data available in one hour time, and the priority beinggiven to the value the closest in time to the product nominal hour. The product format is compliantwith the GHRSST Data Specification (GDS) version 2.", "daac": "NASA/JPL/PODAAC", "nwCorner": { "crs": "wgs-84", "latitude": 60, "longitude": -135, "height": null }, "temporalFrequency": "Unknown", "temporalExtentEnd": "2017-12-14T15:30:01.000Z", "shortName": "GOES13-OSISAF-L3C-v1.0", "landingPageUrl": "http://www.osi-saf.org", "doi": "10.5067/GHG13-3CO01", "longName": "GHRSST Level 3C sub-skin Sea Surface Temperature from the Geostationary Operational Environmental Satellites (GOES 13) Imager in East position (GDS V2) produced by OSI SAF" }
node
6
[ "Dataset" ]
{ "temporalExtentStart": "2013-06-04T10:25:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2491735309-POCLOUD", "globalId": "e5807c1a-4ed8-5e4b-a749-372104676cac", "pagerank_publication_dataset": 0.34411875000000003, "abstract": "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 realtime from Metop/AVHRR. Global AVHRR level 1b data are acquired at Meteo-France/Centre deMeteorologie Spatiale (CMS) through the EUMETSAT/EUMETCAST system. SST is retrievedfrom 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 forregional and seasonal biases due to changing atmospheric conditions. This product is delivered atfull resolution in satellite projection as metagranule corresponding to 3 minutes of acquisition. Theproduct format is compliant with the GHRSST Data Specification (GDS) version 2.", "daac": "NASA/JPL/PODAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "Unknown", "temporalExtentEnd": "2016-11-23T11:52:04.000Z", "shortName": "AVHRR_SST_METOP_A-OSISAF-L2P-v1.0", "landingPageUrl": "http://www.osi-saf.org", "doi": "10.5067/GHAMA-2PO02", "longName": "GHRSST Level 2P sub-skin Sea Surface Temperature from the Advanced Very High Resolution Radiometer (AVHRR) on Metop satellites (currently Metop-A) (GDS V2) produced by OSI SAF" }
node
7
[ "Dataset" ]
{ "temporalExtentStart": "2019-05-14T18:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": 53.8, "longitude": -146.1, "height": null }, "cmrId": "C2491772160-POCLOUD", "globalId": "ec4120b7-6e96-5d2f-a370-b8c3c906517e", "pagerank_publication_dataset": 0.5001857700892858, "abstract": "The Saildrone Arctic 2019 dataset presents a unique collection of high-quality, near real-time, multivariate surface ocean, and atmospheric observations obtained through the deployment of Saildrone, an innovative wind and solar-powered uncrewed surface vehicle (USV). Saildrone is capable of extended missions lasting up to 12 months, covering vast distances at typical speeds of 3-5 knots and operates autonomously, relying solely on wind propulsion, while its navigation can be remotely guided from land. The 2019 Saildrone Arctic campaign featured six Saildrone USVs (jointly funded by NOAA and NASA) deployed during a 150-day cruise in the Bering and Chukchi Seas, spanning from 14 May 2019 to 11 October 2019. The primary mission objective for 2019 was to gather comprehensive atmospheric and oceanographic data in Alaskan arctic waters, which could lead to significant improvements in modeling of diurnal warming and understanding of the marginal ice zones. Additionally, these new data will provide additional Arctic SST observations to benefit SST algorithm development and validation, and for studies of air- sea-ice interactions. Please see the cruise report: https://archive.podaac.earthdata.nasa.gov/podaac-ops-cumulus-docs/insitu/open/L2/saildrone/docs/Saildrone_2019_Arctic_Cruise_Report.pdf <p>\rDuring the Arctic campaign, NASA-funded Saildrones SD-1036 and SD-1037 undertook transects in the Chukchi Sea, approaching the sea ice edge to measure air-sea heat and momentum fluxes in the ocean near sea ice and to validate satellite sea-surface temperature measurements in the Arctic. Each Saildrone was equipped with a suite of instruments to measure various parameters, including air temperature, relative humidity, barometric pressure, surface skin temperature, wind speed and direction, wave height and period, seawater temperature and salinity, chlorophyll fluorescence, and dissolved oxygen. Additionally, both vehicles utilized 300 kHz acoustic Doppler current profilers (ADCP) to measure near-surface currents. Seven temperature data loggers positioned vertically along the hull enhanced understanding of thermal variability near the ocean surface.<p>\rThe Saildrone Arctic 2019 dataset, part of the Multi-sensor Improved Sea-Surface Temperature (MISST) project, encompasses three netCDF format files for each deployed Saildrone. The first file integrates saildrone platform telemetry and surface observational data at 1-minute temporal resolution including key parameters such as air temperature, sea surface skin, and bulk temperatures, salinity, oxygen and chlorophyll-a concentrations, barometric pressure, and wind speed and direction. The second file focuses on ADCP current vector data, providing depth-resolved information to 100m at 2m intervals and binned temporally at 5-minute resolution. The third file includes temperature logger measurements at various depths at 1-minute resolution. This project, funded by NASA through the National Ocean Partnership Program (NOPP), demonstrates a commitment to advancing scientific understanding of the Arctic environment through innovative and autonomous observational technologies. \r", "daac": "NASA/JPL/PODAAC", "nwCorner": { "crs": "wgs-84", "latitude": 75.5, "longitude": -168.7, "height": null }, "temporalFrequency": "Unknown", "temporalExtentEnd": "2019-10-11T18:30:01.000Z", "shortName": "SAILDRONE_ARCTIC", "landingPageUrl": "http://podaac.jpl.nasa.gov/saildrone", "doi": "10.5067/SDRON-NOPP0", "longName": "Saildrone Arctic field campaign surface and ADCP measurements for NOPP-MISST project" }
node
8
[ "Dataset" ]
{ "temporalExtentStart": "2020-01-17T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": 7.4, "longitude": -48.6, "height": null }, "cmrId": "C2491772162-POCLOUD", "globalId": "4a26c4bc-222a-5c74-b989-9cf4edb6b4d6", "pagerank_publication_dataset": 2.9791239928501647, "abstract": "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.", "daac": "NASA/JPL/PODAAC", "nwCorner": { "crs": "wgs-84", "latitude": 12.1, "longitude": -59.4, "height": null }, "temporalFrequency": "Unknown", "temporalExtentEnd": "2020-03-02T23:59:59.000Z", "shortName": "SAILDRONE_ATOMIC", "landingPageUrl": "http://podaac.jpl.nasa.gov/saildrone", "doi": "10.5067/SDRON-ATOM0", "longName": "Saildrone field campaign surface and ADCP measurements for the Atlantic Tradewind Ocean-Atmosphere Mesoscale Interaction Campaign (ATOMIC) project" }
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[ "Dataset" ]
{ "temporalExtentStart": "2018-04-11T18:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": 28.01, "longitude": -115.52, "height": null }, "cmrId": "C2491772165-POCLOUD", "globalId": "ca6e9b81-316e-5625-b26c-25655e067780", "pagerank_publication_dataset": 1.0126792840562429, "abstract": "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. \rThe saildrone Baja campaign was a 60-day cruise from San Francisco Bay, down along the US/Mexico coast to Guadalupe Island and back again over the period 11 April 2018 to 11 June 2018. Repeat surveys were taken around NDBC moored buoys, and during the final week of the cruise a targeted front was sampled. Scientific objectives included studies of upwelling and frontal region dynamics, air-sea interactions, and diurnal warming effects, while its validation objectives included establishing the utility of data from the saildrone platform for assessment of satellite data accuracy and model assimilation. During the Baja campaign, the single deployed saildrone was 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.\rThis Saildrone Baja dataset is comprised of one data file with the 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) for the entire cruise at 1 minute temporal resolution. A second file contains the ADCP current vector data that is depth-resolved to 100m at 2m intervals and binned temporally at 5 minute resolution. All data files are in netCDF format and CF/ACDD compliant consistent with the NOAA/NCEI specification.", "daac": "NASA/JPL/PODAAC", "nwCorner": { "crs": "wgs-84", "latitude": 37.82, "longitude": -125.55, "height": null }, "temporalFrequency": "Unknown", "temporalExtentEnd": "2018-06-11T20:17:26.000Z", "shortName": "SAILDRONE_BAJA_SURFACE", "landingPageUrl": "http://podaac.jpl.nasa.gov/saildrone", "doi": "10.5067/SDRON-SURF0", "longName": "Saildrone Baja field campaign surface and ADCP measurements" }
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[ "Dataset" ]
{ "temporalExtentStart": "1991-09-01T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2499940521-POCLOUD", "globalId": "102c01e1-bcd7-58b0-837d-102f90effbf0", "pagerank_publication_dataset": 5.387707046089298, "abstract": "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.", "daac": "NASA/JPL/PODAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "2017-03-18T00:00:00.000Z", "shortName": "CMC0.2deg-CMC-L4-GLOB-v2.0", "landingPageUrl": null, "doi": "10.5067/GHCMC-4FM02", "longName": "GHRSST Level 4 CMC0.2deg Global Foundation Sea Surface Temperature Analysis (GDS version 2)" }
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[ "Dataset" ]
{ "temporalExtentStart": "2000-02-16T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2540275683-LPCLOUD", "globalId": "ac139cfa-2b7a-5e1d-a995-1d2beefa5449", "pagerank_publication_dataset": 1.9237923719714907, "abstract": "The MCD43D62 Version 6.1 Bidirectional Reflectance Distribution Function and Albedo (BRDF/Albedo) Nadir BRDF-Adjusted Reflectance (NBAR) dataset is produced daily using 16 days of Terra and Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) data at 30 arc second (1,000 meter (m)) resolution. Data are temporally weighted to the ninth day which is reflected in the Julian date in the file name. This Climate Modeling Grid (CMG) product covers the entire globe for use in climate simulation models. Due to the large file size, each MCD43D product contains just one data layer. \r\rMCD43D62 through MCD43D68 are the NBAR products of the MCD43D BRDF/Albedo product suite for MODIS bands 1 through 7. 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.\r\rMCD43D62 is the NBAR for MODIS band 1. \r\rImprovements/Changes from Previous Versions\r\r* 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.\r* A polarization correction has been applied to the L1B Reflective Solar Bands (RSB).\r", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "MCD43D62", "landingPageUrl": "https://doi.org/10.5067/MODIS/MCD43D62.061", "doi": "10.5067/MODIS/MCD43D62.061", "longName": "MODIS/Terra+Aqua BRDF/Albedo Nadir BRDF-Adjusted Ref Band1 Daily L3 Global 30ArcSec CMG V061" }
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[ "Dataset" ]
{ "temporalExtentStart": "2000-03-03T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C1623882456-LPDAAC_ECS", "globalId": "750cff52-9834-585b-9773-bf5b680e77d6", "pagerank_publication_dataset": 0.5786374246413309, "abstract": "The Daily Moderate Resolution Imaging Spectroradiometer (MODIS) Bidirectional Reflectance Distribution Function and Albedo (BRDF/Albedo) 30 arc second, Global Gap-Filled, Snow-Free, (MCD43GF) Version 6 is derived from the 30 arc second Climate Modeling Grid (CMG) MCD43D Version 6 product suite, with additional processing to provide a gap-filled, snow-free product. The highest quality full inversion values were 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 quality layer for each band. To generate a snow-free product, pixels with ephemeral snow were removed using the MCD43D41 (https://doi.org/10.5067/MODIS/MCD43D41.006) snow flags. The underlying MCD43D utilizes a BRDF model derived from all available high quality cloud clear reflectance data over a 16 day moving window centered on and emphasizing the daily day of interest (the ninth day of each retrieval period as reflected in the Julian date in the filename). This 30 arc second BRDF model is then used to produce the Albedo and NBAR products (MCD43D). These BRDF model parameters are computed for MODIS spectral bands 1 through 7 (0.47 um, 0.55 um, 0.67 um, 0.86 um, 1.24 um, 1.64 um, 2.1 um), as well as the shortwave infrared band (0.3-5.0 um), visible band (0.3-0.7 um), and near-infrared (0.7-5.0 um) broad bands. The MCD43GF product includes 67 variables containing black-sky albedo (BSA) at local solar noon, isotropic model parameter (ISO), volumetric model parameter (VOL), geometric model parameter (GEO), quality (QA), Nadir BRDF-Adjusted Reflectance (NBAR) at local solar noon, and white-sky albedo (WSA). Due to the large file size, each data variable is distributed as a separate HDF file. Users are encouraged to download the quality variable for each of the 10 bands to check quality assessment information before using the BRDF/Albedo data.The MCD43 product is not recommended for solar zenith angles beyond 70 degrees.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 User Guide.Improvements/Changes from Previous Versions* Observations are weighted to estimate the BRDF/Albedo on the ninth day of the 16-day period.* MCD43 products use the snow status weighted to the ninth day instead of the majority snow/no-snow observations from the 16-day period.* Better quality at high latitudes from use of all available observations for the acquisition period. Collection 5 used only four observations per day.* The MCD43 products use L2G-lite surface reflectance as input.* When there are insufficient high quality reflectances, a database with archetypal BRDF parameters is used to supplement the observational data and perform a lower quality magnitude inversion. This database is continually updated with the latest full inversion retrieval for each pixel.* CMG Albedo is estimated using all the clear-sky observations within the 1,000 m grid for MCD43C as opposed to aggregating from the 500 m albedo.Important Quality InformationThe incorrect representation of the aerosol quantities (low average high) in the C6 MYD09 and MOD09 surface reflectance products may have impacted downstream products particularly over arid bright surfaces. This (and a few other issues) have been corrected for C6.1. Therefore users should avoid substantive use of the C6 MCD43 products and wait for the C6.1 products. In any event, users are always strongly encouraged to download and use the extensive QA data provided in MCD43A2, in addition to the briefer mandatory QAs provided as part of the MCD43A1, 3, and 4 products.", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "2017-12-31T23:59:59.999Z", "shortName": "MCD43GF", "landingPageUrl": "https://doi.org/10.5067/MODIS/MCD43GF.006", "doi": "10.5067/MODIS/MCD43GF.006", "longName": "MODIS/Terra+Aqua BRDF/Albedo Gap-Filled Snow-Free Daily L3 Global 30ArcSec CMG V006" }
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[ "Dataset" ]
{ "temporalExtentStart": "2000-02-24T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2565807733-LPCLOUD", "globalId": "63ae7d47-5577-5d4f-9a63-9f631d8901d3", "pagerank_publication_dataset": 0.5325000000000001, "abstract": "The MCD19A2CMG Version 6.1 data product is a Moderate Resolution Imaging Spectroradiometer (MODIS) Terra and Aqua combined Multi-Angle Implementation of Atmospheric Correction (MAIAC) Land Aerosol Optical Depth (AOD) and Water Vapor Level 3 product produced daily in a 0.05 degree (5,600 meters at the equator) Climate Modeling Grid (CMG). The MCD19A2CMG product provides the atmospheric properties and view geometry used to calculate the MAIAC Surface Reflectance data products (MCD19A1CMGL (https://doi.org/10.5067/MODIS/MCD19A1CMGL.061) and MCD19A1CMGO (https://doi.org/10.5067/MODIS/MCD19A1CMGO.061)). The MCD19A2CMG AOD data product contains the following Science Dataset (SDS) layers: blue band AOD at 0.47 µm, green band AOD at 0.55 µm, AOD uncertainty, column water vapor for Terra, column water vapor for Aqua, average cloud fraction, available AOD, satellite overpass times, line and sample number, offset, and number of AOD records. A low-resolution browse image is also included showing AOD of the blue band at 0.47 µm created using a composite of all available orbits. Known Issues* Known issues are described in Section 6 of the User Guide.* For complete information about known issues please refer to the MODIS/VIIRS Land Quality Assessment website (https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor=MODIS&sat=TerraAqua&as=61).", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "MCD19A2CMG", "landingPageUrl": "https://doi.org/10.5067/MODIS/MCD19A2CMG.061", "doi": "10.5067/MODIS/MCD19A2CMG.061", "longName": "MODIS/Terra+Aqua AOD and Water Vapor from MAIAC, Daily L3 Global 0.05Deg CMG V061" }
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[ "Dataset" ]
{ "temporalExtentStart": "1984-03-12T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2763261610-LPCLOUD", "globalId": "bf3e0ad8-3e3d-526e-8480-98e3d92ac4be", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "The Land Processes Distributed Active Archive Center (LP DAAC) archives and distributes Global Forest Cover Change (GFCC) data products through the NASA Making Earth System Data Records for Use in Research Environments (MEaSUREs) (https://earthdata.nasa.gov/about/competitive-programs/measures) Program. The GFCC Surface Reflectance Estimates Multi-Year Global dataset is derived from the enhanced Global Land Survey (GLS) datasets for epochs centered on the years 1990, 2000, 2005, and 2010. The GLS datasets are composed of Landsat 5 Thematic Mapper (TM) and Landsat 7 Enhanced Thematic Mapper Plus (ETM+) images at 30 meter resolution. Data available for this product represent the best available “leaf-on” date during the peak growing season. The original GLS datasets were enhanced with supplemental Landsat images when data were incomplete for the epoch or inadequate for analysis due to acquisition during “leaf-off” seasons. The enhanced GLS data were acquired June 1984 through August 2011. Atmospheric corrections were applied to seven visible bands to estimate surface reflectance by compensating for the scattering and absorption of radiance by atmospheric conditions. GFCC30SR is a multi-file data product. The surface reflectance data products are used as source data for other datasets in the GFCC collection.For each available date, data files are delivered in a zip folder that consists of six surface reflectance bands, a Top of Atmosphere temperature band, an Atmospheric Opacity layer, and the Landsat Surface Reflectance Quality layer. Data follow the Worldwide Reference System-2 tiling scheme. Additional details regarding the methodology used to create the data are available in the Algorithm Theoretical Basis Document (ATBD) (https://lpdaac.usgs.gov/documents/146/GFCC_ATBD.pdf). ", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "Unknown", "temporalExtentEnd": "2011-12-25T23:59:59.999Z", "shortName": "GFCC30SR", "landingPageUrl": "https://doi.org/10.5067/MEaSUREs/GFCC/GFCC30SR.001", "doi": "10.5067/MEASURES/GFCC/GFCC30SR.001", "longName": "Global Forest Cover Change Surface Reflectance Estimates Multi-Year Global 30m V001" }
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[ "Dataset" ]
{ "temporalExtentStart": "2000-02-16T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2540268566-LPCLOUD", "globalId": "ba90c3ad-6ad8-582b-bdde-ee853e3ac6bf", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "The MCD43D25 Version 6.1 Bidirectional Reflectance Distribution Function and Albedo (BRDF/Albedo) Model Parameter dataset is produced daily using 16 days of Terra and Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day which is reflected in the Julian date in the file name. This Climate Modeling Grid (CMG) product covers the entire globe for use in climate simulation models. Due to the large file size, each MCD43D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the MODIS bands 1 through 7 and the visible, near infrared (NIR), and shortwave bands included in MCD43C1 (https://doi.org/10.5067/MODIS/MCD43C1.061) are stored in a separate file as MCD43D01 through MCD43D30. \r\rMCD43D25 is the BRDF isotropic parameter for the MODIS NIR broadband. The isotropic parameter, in conjunction with the volumetric and geometric parameters, is used to derive the BRDF/Albedo values for the MODIS NIR broadband. \r\rImprovements/Changes from Previous Versions\r\r* 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.\r* A polarization correction has been applied to the L1B Reflective Solar Bands (RSB).", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "MCD43D25", "landingPageUrl": "https://doi.org/10.5067/MODIS/MCD43D25.061", "doi": "10.5067/MODIS/MCD43D25.061", "longName": "MODIS/Terra+Aqua BRDF/Albedo Parameter1 NIR Daily L3 Global 30ArcSec CMG V061" }
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[ "Dataset" ]
{ "temporalExtentStart": "2012-01-19T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C1607337482-LPDAAC_ECS", "globalId": "311380ae-3001-5be3-9edc-6e096386e625", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "The NASA/NOAA Suomi National Polar-orbiting Partnership (Suomi NPP) Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Black-Sky Albedo for ShortWave (VNP43D65) 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 VNP43D 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 VNP43D product contains just one data layer. \r\rVNP43D54 through VNP43D79 are the albedo products of the VNP43D 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 VNP43MA3 (https://doi.org/10.5067/VIIRS/VNP43MA3.001) product. In addition to the bands included in VNP43MA3, 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 VNP43MA3 product page and in the Algorithm Theoretical Basis Document (ATBD).\r\rVNP43D65 is the BSA for the VIIRS shortwave broadband (1.61 μm).", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "VNP43D65", "landingPageUrl": "https://doi.org/10.5067/VIIRS/VNP43D65.001", "doi": "10.5067/VIIRS/VNP43D65.001", "longName": "VIIRS/NPP BRDF/Albedo BSA at Solar Noon ShortWave Daily L3 Global 30ArcSec CMG V001" }
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[ "Dataset" ]
{ "temporalExtentStart": "2002-07-04T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2343109950-LPCLOUD", "globalId": "8ef7367e-8223-569b-b9c0-703f0591bd98", "pagerank_publication_dataset": 1.5489694073514624, "abstract": "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). \r\rValidation at stage 3 (https://modis-land.gsfc.nasa.gov/MODLAND_val.html) has been achieved for the MODIS Surface Reflectance products. Further details regarding MODIS land product validation for the MYD09 data product is available from the MODIS Land Team Validation site (https://modis-land.gsfc.nasa.gov/ValStatus.php?ProductID=MOD09).\r\rImprovements/Changes from Previous Versions\r\r* 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.\r* A polarization correction has been applied to the L1B Reflective Solar Bands (RSB).", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "MYD09GQ", "landingPageUrl": "https://doi.org/10.5067/MODIS/MYD09GQ.061", "doi": "10.5067/MODIS/MYD09GQ.061", "longName": "MODIS/Aqua Surface Reflectance Daily L2G Global 250m SIN Grid V061" }
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[ "Dataset" ]
{ "temporalExtentStart": "2012-01-19T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C1442270800-LPDAAC_ECS", "globalId": "af5e9dd9-c71d-5ed0-8a47-94d071c5dcb7", "pagerank_publication_dataset": 0.5477291666666667, "abstract": "The NASA/NOAA Suomi National Polar-orbiting Partnership (Suomi NPP) Visible Infrared Imaging Radiometer Suite (VIIRS) Land Surface Temperature and Emissivity (LST&E) Day Version 1 product (VNP21A1D) is compiled daily from daytime Level 2 Gridded (L2G) intermediate products. \r\rThe L2G process maps the daily (VNP21) (https://doi.org/10.5067/VIIRS/VNP21.001) swath granules onto a sinusoidal MODIS grid and stores all observations overlapping a gridded cell for a given day. The VNP21A1 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.\r\rThe VNP21A1D product is developed synergistically with the Moderate Resolution Imaging Spectroradiometer (MODIS) LST&E Version 6 product (MOD21A1D) (https://doi.org/10.5067/MODIS/MOD21A1D.006)) 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) (https://lpdaac.usgs.gov/documents/1332/VNP21_ATBD_V1.pdf). VIIRS LST&E products are available 2 months after acquisition due to latency of data inputs.\r\rThe VNP21A1D 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 VNP21A1D granule.\r", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "2024-05-01T23:59:59.999Z", "shortName": "VNP21A1D", "landingPageUrl": "https://doi.org/10.5067/VIIRS/VNP21A1D.001", "doi": "10.5067/VIIRS/VNP21A1D.001", "longName": "VIIRS/NPP Land Surface Temperature/Emissivity Daily L3 Global 1km SIN Grid Day V001" }
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[ "Dataset" ]
{ "temporalExtentStart": "2012-01-19T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C1607319544-LPDAAC_ECS", "globalId": "1e0a193d-c5b0-5307-ad50-59476aab41f7", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "The NASA/NOAA Suomi National Polar-orbiting Partnership (Suomi NPP) Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 1 Band M10 product (VNP43D22) 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 VNP43D 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 VNP43D 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 VNP43MA1 (https://doi.org/10.5067/VIIRS/VNP43MA1.001) product is stored in a separate file as VNP43D01 through VNP43D36. In addition to the bands included in VNP43MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VNP43D37 through VNP43D39. Details regarding methodology are available on the VNP43MA1 product page and in the Algorithm Theoretical Basis Document (ATBD).\r\rVNP43D22 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.", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "VNP43D22", "landingPageUrl": "https://doi.org/10.5067/VIIRS/VNP43D22.001", "doi": "10.5067/VIIRS/VNP43D22.001", "longName": "VIIRS/NPP BRDF/Albedo Parameter 1 Band M10 Daily L3 Global 30 ArcSec CMG V001" }
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[ "Dataset" ]
{ "temporalExtentStart": "2000-02-16T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2540268595-LPCLOUD", "globalId": "5274396c-c028-581a-a873-dabb6808074a", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "The MCD43D30 Version 6.1 Bidirectional Reflectance Distribution Function and Albedo (BRDF/Albedo) Model Parameter dataset is produced daily using 16 days of Terra and Aqua Moderate Resolution Imaging Sprectroradiometer (MODIS) data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day which is reflected in the Julian date in the file name. This Climate Modeling Grid (CMG) product covers the entire globe for use in climate simulation models. Due to the large file size, each MCD43D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the MODIS bands 1 through 7 and the visible, near infrared (NIR), and shortwave bands included in MCD43C1 (https://doi.org/10.5067/MODIS/MCD43C1.061) are stored in a separate file as MCD43D01 through MCD43D30. \r\rMCD43D30 is the BRDF geometric parameterfor the MODIS shortwave broadband. The geometric parameter, in conjunction with the isotropic and volumetric parameters, is used to derive the BRDF/Albedo values for the MODIS shortwave broadband.\r\rImprovements/Changes from Previous Versions\r\r* 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.\r* A polarization correction has been applied to the L1B Reflective Solar Bands (RSB).", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "MCD43D30", "landingPageUrl": "https://doi.org/10.5067/MODIS/MCD43D30.061", "doi": "10.5067/MODIS/MCD43D30.061", "longName": "MODIS/Terra+Aqua BRDF/Albedo Parameter3 Shortwave Daily L3 Global 30ArcSec CMG V061" }
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[ "Dataset" ]
{ "temporalExtentStart": "2013-01-01T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -60, "longitude": -20, "height": null }, "cmrId": "C2763261708-LPCLOUD", "globalId": "0b07a9ca-a72d-5199-b0b7-321bb5fff297", "pagerank_publication_dataset": 4.104749318632757, "abstract": "The NASA Making Earth System Data Records for Use in Research Environments (MEaSUREs) (https://earthdata.nasa.gov/about/competitive-programs/measures) Global Food Security-support Analysis Data (GFSAD) data product provides cropland extent data over South America for nominal year 2015 at 30 meter resolution (GFSAD30SACE). The monitoring of global cropland extent is critical for policymaking and provides important baseline data that are used in many agricultural cropland studies pertaining to water sustainability and food security. The GFSAD30SACE data product uses the pixel-based supervised classifier, Random Forest (RF), to retrieve cropland extent from a combination of Landsat 5 Thematic Mapper (TM), Landsat 7 Enhanced Thematic Mapper Plus (ETM+), Landsat 8 Operational Land Imager (OLI) data, and elevation derived from the Shuttle Radar Topography Mission (SRTM) Version 3 data products. Each GFSAD30SACE GeoTIFF file contains a cropland extent layer that defines areas of cropland, non-cropland, and water bodies over a 10° by 10° area.", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 15, "longitude": -110, "height": null }, "temporalFrequency": "Unknown", "temporalExtentEnd": "2016-12-31T23:59:59.999Z", "shortName": "GFSAD30SACE", "landingPageUrl": "https://doi.org/10.5067/MEaSUREs/GFSAD/GFSAD30SACE.001", "doi": "10.5067/MEaSUREs/GFSAD/GFSAD30SACE.001", "longName": "Global Food Security-support Analysis Data (GFSAD) Cropland Extent 2015 South America product 30 m V001" }
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[ "Dataset" ]
{ "temporalExtentStart": "2002-07-04T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2565794850-LPCLOUD", "globalId": "9a63b101-635c-5f3d-b011-e4f2c5c368f1", "pagerank_publication_dataset": 0.5544785714285715, "abstract": "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 (MYD17A2H)(https://doi.org/10.5067/MODIS/MYD17A2H.061) from the given year. The PSN value is the difference of the GPP and the Maintenance Respiration (MR).\r\rThe MYD17A3HGF will be generated at the end of each year when the entire yearly 8-day MYD15A2H (https://doi.org/10.5067/modis/myd15a2h.061) 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.\r\rStage 3 (https://landweb.modaps.eosdis.nasa.gov/cgi-bin/QA_WWW/newPage.cgi?fileName=maturity) validation has been achieved for MYD17 products.\r\rImprovements/Changes from Previous Versions\r* 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.\r* A polarization correction has been applied to the L1B Reflective Solar Bands (RSB).\r* The product uses Climatology LAI/FPAR as back up to the operational LAI/FPAR.\r\r\r\r", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "Unknown", "temporalExtentEnd": "", "shortName": "MYD17A3HGF", "landingPageUrl": "https://doi.org/10.5067/MODIS/MYD17A3HGF.061", "doi": "10.5067/MODIS/MYD17A3HGF.061", "longName": "MODIS/Aqua Net Primary Production Gap-Filled Yearly L4 Global 500m SIN Grid V061" }
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[ "Dataset" ]
{ "temporalExtentStart": "2000-02-16T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2218719731-LPCLOUD", "globalId": "21b38d33-e1f1-5520-8f88-beca75d6b8df", "pagerank_publication_dataset": 61.57966056240889, "abstract": "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 User Guide.The MCD43A4 provides NBAR and simplified mandatory quality layers for MODIS bands 1 through 7. Essential quality information provided in the corresponding MCD43A2 (https://doi.org/10.5067/MODIS/MCD43A2.061) data file should be consulted when using this product.Known Issues* For complete information about known issues please refer to the MODIS/VIIRS Land Quality Assessment website (https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor=MODIS&sat=TerraAqua&as=61).Improvements/Changes from Previous Versions* 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.* A polarization correction has been applied to the L1B Reflective Solar Bands (RSB).", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "MCD43A4", "landingPageUrl": "https://doi.org/10.5067/MODIS/MCD43A4.061", "doi": "10.5067/MODIS/MCD43A4.061", "longName": "MODIS/Terra+Aqua BRDF/Albedo Nadir BRDF-Adjusted Ref Daily L3 Global - 500m V061" }
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[ "Dataset" ]
{ "temporalExtentStart": "2000-02-24T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2343115666-LPCLOUD", "globalId": "b328d420-0866-547a-a3e4-05a110c434fc", "pagerank_publication_dataset": 12.297050728215911, "abstract": "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). \r\rValidation at stage 3 (https://modis-land.gsfc.nasa.gov/MODLAND_val.html) has been achieved for the MODIS Surface Reflectance products. Further details regarding MODIS land product validation for the MOD09 data product is available from the MODIS Land Team Validation site (https://modis-land.gsfc.nasa.gov/ValStatus.php?ProductID=MOD09).\r\rImprovements/Changes from Previous Versions\r\r* 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.\r* A polarization correction has been applied to the L1B Reflective Solar Bands (RSB).", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "MOD09GQ", "landingPageUrl": null, "doi": "10.5067/MODIS/MOD09GQ.061", "longName": "MODIS/Terra Surface Reflectance Daily L2G Global 250m SIN Grid V061" }
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[ "Dataset" ]
{ "temporalExtentStart": "2012-01-19T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C1607336296-LPDAAC_ECS", "globalId": "18a93a6f-482d-56cd-a054-1bded4bd0a34", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "The NASA/NOAA Suomi National Polar-orbiting Partnership (Suomi NPP) Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Black-Sky Albedo for NIR (VNP43D64) 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 VNP43D 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 VNP43D product contains just one data layer. \r\rVNP43D54 through VNP43D79 are the albedo products of the VNP43D 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 VNP43MA3 (https://doi.org/10.5067/VIIRS/VNP43MA3.001) product. In addition to the bands included in VNP43MA3, 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 VNP43MA3 product page and in the Algorithm Theoretical Basis Document (ATBD).\r\rVNP43D64 is the BSA for the VIIRS NIR broadband (0.865 μm).\r", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "VNP43D64", "landingPageUrl": "https://doi.org/10.5067/VIIRS/VNP43D64.001", "doi": "10.5067/VIIRS/VNP43D64.001", "longName": "VIIRS/NPP BRDF/Albedo BSA at Solar Noon NIR Daily L3 Global 30ArcSec CMG V001" }
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[ "Dataset" ]
{ "temporalExtentStart": "2000-02-16T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2532007810-LPCLOUD", "globalId": "39a7b3a8-3250-55a5-bd07-2d3d055dbd57", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "The MCD43D06 Version 6.1 Bidirectional Reflectance Distribution Function and Albedo (BRDF/Albedo) Model Parameter data set is a daily 16-day product. This product incorporates the Climate Modeling Grid (CMG) structure in which each file geographically covers the entire earth rather than the 10 degree x 10 degree latitude and longitude tiling system utilized by the standard MODIS land products. Unlike the standard CMG pixel resolution of 5600 meters the MCD43D products are 1000 meters, consequently, because of the large file size each product contains just one layer. The Julian date in the granule ID of each specific file represents the 9th day of the 16 day composite period, and consequently the observations are weighted to estimate the BRDF/Albedo for that day. The layer in the MCD43D06 is the Bidirectional Reflectance Distribution Function geometric parameter for MODIS band 2. This geometric parameter, in conjunction with the isotropic and volumetric parameters, is used to derive the Albedo and BRDF value for MODIS band 2. ", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "MCD43D06", "landingPageUrl": "https://doi.org/10.5067/MODIS/MCD43D06.061", "doi": "10.5067/MODIS/MCD43D06.061", "longName": "MODIS/Terra+Aqua BRDF/Albedo Parameter 3 Band 2 Daily L3 Global 30 ArcSec CMG V061" }
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[ "Dataset" ]
{ "temporalExtentStart": "2018-01-01T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2545310918-LPCLOUD", "globalId": "a530e2cb-b0d5-52e9-82e3-8aa685b9363d", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "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. \r\rThe 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 (VJ143IA4), 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).\r\rThe 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. \r", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "VJ143IA2", "landingPageUrl": "https://doi.org/10.5067/VIIRS/VJ143IA2.002", "doi": "10.5067/VIIRS/VJ143IA2.002", "longName": "VIIRS/JPSS1 BRDF/Albedo Quality Daily L3 Global 500m SIN Grid V002" }
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[ "Dataset" ]
{ "temporalExtentStart": "2002-07-04T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2565805789-LPCLOUD", "globalId": "a00df9d0-fe40-5391-84f9-89f0332db352", "pagerank_publication_dataset": 0.23234375000000002, "abstract": "A suite of Moderate Resolution Imaging Spectroradiometer (MODIS) Land Surface Temperature and Emissivity (LST&E) products are available in Collection 6.1. The MYD21 Land Surface Temperature (LST) algorithm differs from the algorithm of the MYD11 (https://doi.org/10.5067/modis/myd11_l2.061) 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 MYD21 (https://doi.org/10.5067/MODIS/MYD21.061) 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&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. Additional details regarding the methodology used to create this Level 3 (L3) product are available in the Algorithm Theoretical Basis Document (ATBD (https://lpdaac.usgs.gov/documents/1399/MOD21_ATBD.pdf)).Validation at stage 1 (https://modis-land.gsfc.nasa.gov/MODLAND_val.html) has been achieved for the MODIS Land Surface Temperature and Emissivity data products. Further details regarding MODIS land product validation for the MYD21 data products are available from the MODIS Land Team Validation site (https://modis-land.gsfc.nasa.gov/ValStatus.php?ProductID=MOD21).Improvements/Changes from Previous Versions* 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.* A polarization correction has been applied to the L1B Reflective Solar Bands (RSB).* The product utilizes GEOS data replacing MERRA2.* Three new CMG products are available in the MxD21 suite (MxD21C1/C2/C3).", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "MYD21A1N", "landingPageUrl": "https://doi.org/10.5067/MODIS/MYD21A1N.061", "doi": "10.5067/MODIS/MYD21A1N.061", "longName": "MODIS/Aqua Land Surface Temperature/3-Band Emissivity Daily L3 Global 1km SIN Grid Night V061" }
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[ "Dataset" ]
{ "temporalExtentStart": "1999-06-29T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2763261619-LPCLOUD", "globalId": "beb83473-9a5c-5810-bcd5-1bf2ca7ee3ad", "pagerank_publication_dataset": 1.3708125000000002, "abstract": "The Land Processes Distributed Active Archive Center (LP DAAC) archives and distributes Global Forest Cover Change (GFCC) data products through the NASA Making Earth System Data Records for Use in Research Environments (MEaSUREs) (https://earthdata.nasa.gov/about/competitive-programs/measures) Program. The GFCC Water Cover 2000 Global dataset provides surface-water information at 30 meter spatial resolution. This dataset was derived from waterbodies in the GFCC Tree Cover (GFCC30TC) (http://dx.doi.org/10.5067/MEaSUREs/GFCC/GFCC30TC.003) and Forest Cover Change (GFCC30FCC) (http://dx.doi.org/10.5067/MEaSUREs/GFCC/GFCC30FCC.001) products based on a classification-tree model. Data are available for selected dates between June 1999 and January 2003. GFCC30WC follows the Worldwide Reference System-2 tiling scheme. Additional details regarding the methodology used to create the data are available in the Algorithm Theoretical Basis Document (ATBD) (https://lpdaac.usgs.gov/documents/146/GFCC_ATBD.pdf). ", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "Unknown", "temporalExtentEnd": "2003-01-14T23:59:59.999Z", "shortName": "GFCC30WC", "landingPageUrl": "https://doi.org/10.5067/MEaSUREs/GFCC/GFCC30WC.001", "doi": "10.5067/MEASURES/GFCC/GFCC30WC.001", "longName": "Global Forest Cover Change Water Cover 2000 Global 30m V001" }
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[ "Dataset" ]
{ "temporalExtentStart": "2012-01-19T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C1607336273-LPDAAC_ECS", "globalId": "322e7a15-70bb-5a93-a3ad-7ee61e23ef0f", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "The NASA/NOAA Suomi National Polar-orbiting Partnership (Suomi NPP) Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Black-Sky Albedo for Band VIS (VNP43D63) 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 VNP43D 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 VNP43D product contains just one data layer. \r\rVNP43D54 through VNP43D79 are the albedo products of the VNP43D 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 VNP43MA3 (https://doi.org/10.5067/VIIRS/VNP43MA3.001) product. In addition to the bands included in VNP43MA3, 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 VNP43MA3 product page and in the Algorithm Theoretical Basis Document (ATBD).\r\rVNP43D63 is the BSA for the VIIRS visible broadband (0.64 μm).\r\r\r", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "VNP43D63", "landingPageUrl": "https://doi.org/10.5067/VIIRS/VNP43D63.001", "doi": "10.5067/VIIRS/VNP43D63.001", "longName": "VIIRS/NPP BRDF/Albedo BSA at Solar Noon Band VIS Daily L3 Global 30ArcSec CMG V001" }
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[ "Dataset" ]
{ "temporalExtentStart": "2000-02-11T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -56, "longitude": 180, "height": null }, "cmrId": "C2763266322-LPCLOUD", "globalId": "e8633c4e-23b0-5b9b-aac3-5664bf268dff", "pagerank_publication_dataset": 3.796858417980828, "abstract": "The Land Processes Distributed Active Archive Center (LP DAAC) is responsible for the archive and distribution of NASA Making Earth System Data Records for Use in Research Environments (MEaSUREs) Digital Elevation Model (DEM) version 1 (NASADEM_SHHP) dataset, which provides Shuttle Radar Topography Mission (SRTM) global elevation height data at 1 arc second spacing.NASADEM data products were derived from original telemetry data from SRTM, a collaboration between NASA and the National Geospatial-Intelligence Agency (NGA), as well as participation from the German and Italian space agencies. SRTM’s primary focus was to generate a near-global DEM of the Earth using radar interferometry. It was a primary component of the payload on space shuttle Endeavour during its STS-99 mission, which was launched on February 11, 2000, and flew for 11 days. In addition to Terra Advanced Spaceborne Thermal and Reflection Radiometer (ASTER) Global Digital Elevation Model (GDEM) Version 3 data, NASADEM also relied on Ice, Cloud, and Land Elevation Satellite (ICESat) Geoscience Laser Altimeter System (GLAS) ground control points of its lidar shots to improve surface elevation measurements that led to improved geolocation accuracy. Other reprocessing improvements include the conversion to geoid reference and the use of GDEMs and Advanced Land Observing Satellite Panchromatic Remote-sensing Instrument for Stereo Mapping (PRISM) AW3D30 DEM, and interpolation for void filling.NASADEM are distributed in 1 degree latitude by 1 degree longitude tiles and consist of all land between 60° N and 56° S latitude. This accounts for about 80% of Earth’s total landmass. NASADEM_SHHP data product layers include SRTM-only floating-point DEM and height error. A low-resolution browse image showing the SRTM-only elevation is also available for each NASADEM_SHHP granule.", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 60, "longitude": -180, "height": null }, "temporalFrequency": "Unknown", "temporalExtentEnd": "2000-02-21T23:59:59.000Z", "shortName": "NASADEM_SHHP", "landingPageUrl": "https://doi.org/10.5067/MEaSUREs/NASADEM/NASADEM_SHHP.001", "doi": "10.5067/MEASURES/NASADEM/NASADEM_SHHP.001", "longName": "NASADEM SRTM-only Height and Height Precision Mosaic Global 1 arc second V001" }
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[ "Dataset" ]
{ "temporalExtentStart": "2000-02-11T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -56, "longitude": 180, "height": null }, "cmrId": "C2763268444-LPCLOUD", "globalId": "901cb123-5ca1-5ac2-a2af-3ab4d0602a64", "pagerank_publication_dataset": 0.912290808982684, "abstract": "The Land Processes Distributed Active Archive Center (LP DAAC) is responsible for the archive and distribution of NASA Making Earth System Data Records for Use in Research Environments ([MEaSUREs](https://earthdata.nasa.gov/about/competitive-programs/measures)) Shuttle Radar Topography Mission (SRTM), which includes the global 1 arc second (~30 meter) swath (raw) image data product. (See [User Guide](https://lpdaac.usgs.gov/documents/179/SRTM_User_Guide_V3.pdf) Section 2.2.1)The SRTM swath image data set consists of radar image files containing brightness values, as well as quality assurance (incidence angle) files for each of four overlapping sub-swaths that passes through a 1 degree by 1 degree tile. Data from each sub-swath is included as a separate file. Some files may contain only partial data; however, every image pixel acquired by SRTM is included in this data set.The NASA SRTM data sets result from a collaborative effort by the National Aeronautics and Space Administration (NASA) and the National Geospatial-Intelligence Agency (NGA - previously known as the National Imagery and Mapping Agency, or NIMA), as well as the participation of the German and Italian space agencies. This collaboration aims to generate a near-global digital elevation model (DEM) of Earth using radar interferometry. SRTM was the primary (and virtually only) payload on the STS-99 mission of the Space Shuttle Endeavour, which launched February 11, 2000 and flew for 11 days.The SRTM swaths extended from ~30 degrees off-nadir to ~58 degrees off-nadir from an altitude of 233 kilometers (km), creating swaths ~225 km wide, and consisted of all land between 60° N and 56° S latitude to account for 80% of Earth’s total landmass. Improvements/Changes from Previous Versions * Voids in the Version 3.0 products have been filled with ASTER Global Digital Elevation Model (GDEM) Version 2.0, the Global Multi-resolution Terrain Elevation Data 2010 (GMTED2010), and the National Elevation Dataset (NED).", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 60, "longitude": -180, "height": null }, "temporalFrequency": "Unknown", "temporalExtentEnd": "2000-02-21T23:59:59.000Z", "shortName": "SRTMIMGR", "landingPageUrl": "https://doi.org/10.5067/MEaSUREs/SRTM/SRTMIMGR.003", "doi": "10.5067/MEASURES/SRTM/SRTMIMGR.003", "longName": "NASA Shuttle Radar Topography Mission Swath Image Data V003" }
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[ "Dataset" ]
{ "temporalExtentStart": "2018-07-09T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2076109886-LPCLOUD", "globalId": "55beff87-9492-50f9-8c10-5733e83cf4bc", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "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 ECOSTRESS website (https://ecostress.jpl.nasa.gov/science).The ECOSTRESS Gridded Water Use Efficiency Instantaneous L4 Global 70 m (ECO_L4G_WUE) Version 2 data product provides Water Use Efficiency (WUE) data generated by dividing the Breathing Earth System Simulator (BESS) Gross Primary Production (GPP) by the Priestley-Taylor Jet Propulsion Laboratory Soil Moisture (PT-JPL-SM) transpiration to estimate WUE, the ratio of grams of carbon that plants absorb to kilograms of water that plants release. The product provides a BESS GPP estimate that represents the amount of carbon surrounding the plants. The ECO_L4G_WUE Version 2 data product is available globally and projected to a globally snapped 0.0006 degree grid with a 70 meter spatial resolution and is distributed in HDF5. Each granule contains variables of Water Use Efficiency (WUE), Water Gross Primary Production (GPP), cloud mask, and water mask. A low-resolution browse is also available showing daily WUE as a stretched image with a color ramp in JPEG format.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, only Thermal Infrared (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.", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "ECO_L4G_WUE", "landingPageUrl": "https://doi.org/10.5067/ECOSTRESS/ECO_L4G_WUE.002", "doi": "10.5067/ECOSTRESS/ECO_L4G_WUE.002", "longName": "ECOSTRESS Gridded Water Use Efficiency Instantaneous L4 Global 70 m V002" }
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[ "Dataset" ]
{ "temporalExtentStart": "2018-07-09T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2074852168-LPCLOUD", "globalId": "b966e9c9-5905-5832-a92c-14d23206bffb", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "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 ECOSTRESS website (https://ecostress.jpl.nasa.gov/science).The ECOSTRESS Tiled Surface Energy Balance Instantaneous L3 Global 70 m (ECO_L3T_SEB) Version 2 data product provides estimated incoming surface radiation (Rg) and net radiation (Rn) aligned with each daytime ECOSTRESS overpass. The Rg was generated using the Forest Light Environmental Simulator (FLiES) radiative transfer model implemented in an artificial neural network using Cloud Optical Thickness (COT) and Aerosol Optical Thickness (AOT) from Goddard Earth Observing System Version 5 (GEOS-5) Forward Processing (FP) along with albedo from ECOSTRESS Tiled Ancillary NDVI and Albedo Level 2 Global 70 m (ECO_L2T_STARS) (https://doi.org/10.5067/ECOSTRESS/ECO_L2T_STARS.002) Version 2 as variables. The Rg output from the FLiES model was bias corrected to Rg from GEOS-FP. The Rn is an output from the Breathing Earth System Simulator (BESS) algorithm. This data product is tiled using a modified version of the Military Grid Reference System (MGRS) (https://hls.gsfc.nasa.gov/products-description/tiling-system/), which divides Universal Transverse Mercator (UTM) zones into square tiles that are 109.8 km by 109.8 km with a 70 meter (m) spatial resolution.The ECO_L3T_SEB Version 2 data product is provided in Cloud Optimized GeoTIFF (COG) format with each data layer distributed as a separate COG. This product contains four layers including Rg, Rn, cloud mask, and water mask.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.* Missing Cloud Layer Alert: All users of ECOSTRESS Tiled and Gridded L3 Soil Moisture and Surface Energy Balance v002 products (ECO_L3T_SM, ECO_L3G_SM, ECO_L3T_SEB, and ECO_L3G_SEB) should be aware that the ‘cloud mask’ layer may be unavailable for a select number of granules for the year 2023. Users are encouraged to get that information from the corresponding Level 2 Standard Cloud Mask products (ECO_L2_CLOUD and ECO_L2G_CLOUD) to assess if a pixel is clear or cloudy (see Section 3 of the User Guide).", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "Unknown", "temporalExtentEnd": "", "shortName": "ECO_L3T_SEB", "landingPageUrl": "https://doi.org/10.5067/ECOSTRESS/ECO_L3T_SEB.002", "doi": "10.5067/ECOSTRESS/ECO_L3T_SEB.002", "longName": "ECOSTRESS Tiled Surface Energy Balance Instantaneous L3 Global 70 m V002" }
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[ "Dataset" ]
{ "temporalExtentStart": "2013-01-01T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -45, "longitude": 180, "height": null }, "cmrId": "C2763261715-LPCLOUD", "globalId": "7a1103ae-2987-5d09-bed1-5eee725f2d88", "pagerank_publication_dataset": 3.6186205827308804, "abstract": "The NASA Making Earth System Data Records for Use in Research Environments (MEaSUREs) (https://earthdata.nasa.gov/about/competitive-programs/measures) Global Food Security-support Analysis Data (GFSAD) data product provides cropland extent data over Southeast and Northeast Asia for nominal year 2015 at 30 meter resolution (GFSAD30SEACE). The monitoring of global cropland extent is critical for policymaking and provides important baseline data that are used in many agricultural cropland studies pertaining to water sustainability and food security. The GFSAD30SEACE data product uses the pixel-based supervised classifiers, Random Forest (RF), to retrieve cropland extent from a combination of Landsat 8 Operational Land Imager (OLI), Landsat 7 Enhanced Thematic Mapper Plus (ETM+), and elevation derived from the Shuttle Radar Topography Mission (SRTM) Version 3 data products. Each GFSAD30SEACE GeoTIFF file contains a cropland extent layer that defines areas of cropland, non-cropland, and water bodies over a 10° by 10° area.", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 60, "longitude": 70, "height": null }, "temporalFrequency": "Unknown", "temporalExtentEnd": "2016-12-31T23:59:59.999Z", "shortName": "GFSAD30SEACE", "landingPageUrl": "https://doi.org/10.5067/MEaSUREs/GFSAD/GFSAD30SEACE.001", "doi": "10.5067/MEaSUREs/GFSAD/GFSAD30SEACE.001", "longName": "Global Food Security-support Analysis Data (GFSAD) Cropland Extent 2015 Southeast and Northeast Asia product 30 m V001" }
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[ "Dataset" ]
{ "temporalExtentStart": "2022-01-01T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2519119034-LPCLOUD", "globalId": "3e9e8dff-b011-5cff-b79b-c69868fda626", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "The Observational Products for End-Users from Remote Sensing Analysis (OPERA) Land Surface Disturbance Annual from Harmonized Landsat Sentinel-2 (HLS) product Version 1 summarizes the DIST-ALERT 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).\rThe 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. \r", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "Unknown", "temporalExtentEnd": "", "shortName": "OPERA_L3_DIST-ANN-HLS_V1", "landingPageUrl": "https://doi.org/10.5067/SNWG/OPERA_L3_DIST-ANN-HLS_V1.001", "doi": "10.5067/SNWG/OPERA_L3_DIST-ANN-HLS_V1.001", "longName": "OPERA Land Surface Disturbance Annual from Harmonized Landsat Sentinel-2 product (Version 1)" }
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[ "Dataset" ]
{ "temporalExtentStart": "2002-07-04T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2565794042-LPCLOUD", "globalId": "21b6906c-8a31-57c6-bf10-d60d5d2c957c", "pagerank_publication_dataset": 3.2830917769165224, "abstract": "The MYD11C2 Version 6.1 product provides Land Surface Temperature and Emissivity (LST&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&E values in the MYD11C2 product are derived by compositing and averaging the values from the corresponding eight MYD11C1 (https://doi.org/10.5067/MODIS/MYD11C1.061) 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. Validation at stage 2 (https://modis-land.gsfc.nasa.gov/MODLAND_val.html) has been achieved for all MODIS Land Surface Temperature and Emissivity products. Further details regarding MODIS land product validation for the MYD11 data products are available from the MODIS Land Team Validation site (https://modis-land.gsfc.nasa.gov/ValStatus.php?ProductID=MOD11).Improvements/Changes from Previous Versions* 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.* A polarization correction has been applied to the L1B Reflective Solar Bands (RSB).", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "MYD11C2", "landingPageUrl": "https://doi.org/10.5067/MODIS/MYD11C2.061", "doi": "10.5067/MODIS/MYD11C2.061", "longName": "MODIS/Aqua Land Surface Temperature/Emissivity 8-Day L3 Global 0.05Deg CMG V061" }
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[ "Dataset" ]
{ "temporalExtentStart": "2012-01-19T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C1607336236-LPDAAC_ECS", "globalId": "f82d51f3-98ef-5321-bdeb-1d3a097ec773", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "The NASA/NOAA Suomi National Polar-orbiting Partnership (Suomi NPP) Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Black-Sky Albedo for Band M10 (VNP43D61) 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 VNP43D 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 VNP43D product contains just one data layer. \r\rVNP43D54 through VNP43D79 are the albedo products of the VNP43D 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 VNP43MA3 (https://doi.org/10.5067/VIIRS/VNP43MA3.001) product. In addition to the bands included in VNP43MA3, 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 VNP43MA3 product page and in the Algorithm Theoretical Basis Document (ATBD).\r\rVNP43D61 is the BSA for VIIRS band M10 (1.61 μm). \r", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "VNP43D61", "landingPageUrl": "https://doi.org/10.5067/VIIRS/VNP43D61.001", "doi": "10.5067/VIIRS/VNP43D61.001", "longName": "VIIRS/NPP BRDF/Albedo BSA at Solar Noon Band M10 Daily L3 Global 30ArcSec CMG V001" }
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[ "Dataset" ]
{ "temporalExtentStart": "2011-06-30T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": 10, "longitude": -50, "height": null }, "cmrId": "C2763264748-LPCLOUD", "globalId": "c5c94c76-4648-58c0-a8a1-6a5e6b691d9a", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "Goddard’s LiDAR, Hyperspectral, and Thermal Imagery (G-LiHT) 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. ", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 73, "longitude": -170, "height": null }, "temporalFrequency": "Unknown", "temporalExtentEnd": "", "shortName": "GLTRAJECTORY", "landingPageUrl": "https://doi.org/10.5067/Community/GLIHT/GLTRAJECTORY.001", "doi": "10.5067/Community/GLIHT/GLTRAJECTORY.001", "longName": "G-LiHT Trajectory Data V001" }
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[ "Dataset" ]
{ "temporalExtentStart": "2012-01-19T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C1607316266-LPDAAC_ECS", "globalId": "8389d243-a731-5d00-8692-a222cf57c0f3", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "The NASA/NOAA Suomi National Polar-orbiting Partnership (Suomi NPP) Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 3 Band M4 product (VNP43D12) 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 VNP43D 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 VNP43D 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 VNP43MA1 (https://doi.org/10.5067/VIIRS/VNP43MA1.001) product is stored in a separate file as VNP43D01 through VNP43D36. In addition to the bands included in VNP43MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VNP43D37 through VNP43D39. Details regarding methodology are available on the VNP43MA1 product page and in the Algorithm Theoretical Basis Document (ATBD).\r\rVNP43D12 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.\r\r", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "VNP43D12", "landingPageUrl": "https://doi.org/10.5067/VIIRS/VNP43D12.001", "doi": "10.5067/VIIRS/VNP43D12.001", "longName": "VIIRS/NPP BRDF/Albedo Parameter 3 Band M4 Daily L3 Global 30 ArcSec CMG V001" }
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[ "Dataset" ]
{ "temporalExtentStart": "2008-12-01T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2763266354-LPCLOUD", "globalId": "854a37a3-b0e9-595e-a36a-0e71f75f0839", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "The NASA Making Earth System Data Records for Use in Research Environments (MEaSUREs) Global Web-Enabled Landsat Data Monthly (GWELDMO) Version 3 data product provides Landsat data at 30 meter (m) resolution for terrestrial non-Antarctica locations over monthly reporting periods for the 2010 epoch. GWELD data products are generated from all available Landsat 4 and 5 Thematic Mapper (TM) and Landsat 7 Enhanced Thematic Mapper Plus (ETM+) data in the U.S. Geological Survey (USGS) Landsat archive. The GWELD suite of products provide consistent data to derive land cover as well as geophysical and biophysical information for regional assessment of land surface dynamics.\r\rThe GWELD products include Nadir Bidirectional Reflectance Distribution Function (BRDF)-Adjusted Reflectance (NBAR) for the reflective wavelength bands and to top of atmosphere (TOA) brightness temperature for the thermal bands. The products are defined in the Sinusoidal coordinate system to promote continuity of NASA’s Moderate Resolution Imaging Spectroradiometer (MODIS) land tile grid.\r\rProvided in the GWELDMO product are layers for surface reflectance bands 1 through 5 and 7, TOA brightness temperature for thermal bands, Normalized Difference Vegetation Index (NDVI), day of year, ancillary angle, and data quality information. A low-resolution red, green, blue (RGB) browse image of bands 5, 4, 3 is also available for each granule.", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "monthly", "temporalExtentEnd": "2011-11-30T23:59:59.999Z", "shortName": "GWELDMO", "landingPageUrl": "https://doi.org/10.5067/MEaSUREs/GWELD/GWELDMO.003", "doi": "10.5067/MEaSUREs/GWELD/GWELDMO.003", "longName": "NASA Global Web-Enabled Landsat Data Monthly Global 30 m V003" }
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[ "Dataset" ]
{ "temporalExtentStart": "2012-01-19T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C1607327972-LPDAAC_ECS", "globalId": "81587273-aff7-523e-a32d-4ebdb7b8a965", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "The NASA/NOAA Suomi National Polar-orbiting Partnership (Suomi NPP) Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 3 Day-Night Band (DNB) product (VNP43D39) 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 VNP43D 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 VNP43D 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 VNP43MA1 (https://doi.org/10.5067/VIIRS/VNP43MA1.001) product is stored in a separate file as VNP43D01 through VNP43D36. In addition to the bands included in VNP43MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VNP43D37 through VNP43D39. Details regarding methodology are available on the VNP43MA1 product page and in the Algorithm Theoretical Basis Document (ATBD).\r\rVNP43D39 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.\r\r", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "VNP43D39", "landingPageUrl": "https://doi.org/10.5067/VIIRS/VNP43D39.001", "doi": "10.5067/VIIRS/VNP43D39.001", "longName": "VIIRS/NPP BRDF/Albedo Parameter 3 DNB Daily L3 Global 30 ArcSec CMG V001" }
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[ "Dataset" ]
{ "temporalExtentStart": "2000-02-16T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2540273183-LPCLOUD", "globalId": "bf07e850-0d94-58dc-bee2-01cc4af96a19", "pagerank_publication_dataset": 0.22423270089285716, "abstract": "The MCD43D59 Version 6.1 Bidirectional Reflectance Distribution Function and Albedo (BRDF/Albedo) White-Sky Albedo dataset is produced daily using 16 days of Terra and Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) data at 30 arc second (1,000 meter (m)) resolution. Data are temporally weighted to the ninth day which is reflected in the Julian date in the file name. This Climate Modeling Grid (CMG) product covers the entire globe for use in climate simulation models. Due to the large file size, each MCD43D product contains just one data layer. \r\rMCD43D42 through MCD43D61 are the albedo products of the MCD43D BRDF/Albedo product suite. There are 10 black-sky albedo and 10 white-sky albedo layers representing MODIS bands 1 through 7 and the visible, near infrared (NIR), and shortwave bands. 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. \r\rMCD43D59 is the white-sky albedo for the MODIS visible broadband. \r\rImprovements/Changes from Previous Versions\r\r* 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.\r* A polarization correction has been applied to the L1B Reflective Solar Bands (RSB).", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "MCD43D59", "landingPageUrl": "https://doi.org/10.5067/MODIS/MCD43D59.061", "doi": "10.5067/MODIS/MCD43D59.061", "longName": "MODIS/Terra+Aqua BRDF/Albedo White Sky Albedo VIS Daily L3 Global 30ArcSec CMG V061" }
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[ "Dataset" ]
{ "temporalExtentStart": "2002-01-01T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2565794824-LPCLOUD", "globalId": "7e127f29-be97-577e-ab9b-94dcfb73dfe9", "pagerank_publication_dataset": 0.6926389880952382, "abstract": "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 MYD15A2H (https://doi.org/10.5067/modis/myd15a2h.061) 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.Stage 3 (https://landweb.modaps.eosdis.nasa.gov/cgi-bin/QA_WWW/newPage.cgi?fileName=maturity) validation has been achieved for MYD17 products.Improvements/Changes from Previous Versions* 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.* A polarization correction has been applied to the L1B Reflective Solar Bands (RSB).* The product uses Climatology LAI/FPAR as back up to the operational LAI/FPAR.", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "Unknown", "temporalExtentEnd": "", "shortName": "MYD17A2HGF", "landingPageUrl": "https://doi.org/10.5067/MODIS/MYD17A2HGF.061", "doi": "10.5067/MODIS/MYD17A2HGF.061", "longName": "MODIS/Aqua Gross Primary Productivity Gap-Filled 8-Day L4 Global 500m SIN Grid V061" }
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[ "Dataset" ]
{ "temporalExtentStart": "2012-01-19T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C1607327355-LPDAAC_ECS", "globalId": "b614de1a-f029-53f6-ae3e-476ae144fb60", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "The NASA/NOAA Suomi National Polar-orbiting Partnership (Suomi NPP) Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 2 NIR product (VNP43D32) 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 VNP43D 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 VNP43D 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 VNP43MA1 (https://doi.org/10.5067/VIIRS/VNP43MA1.001) product is stored in a separate file as VNP43D01 through VNP43D36. In addition to the bands included in VNP43MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VNP43D37 through VNP43D39. Details regarding methodology are available on the VNP43MA1 product page and in the Algorithm Theoretical Basis Document (ATBD).\r\rVNP43D32 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.\r\r", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "VNP43D32", "landingPageUrl": "https://doi.org/10.5067/VIIRS/VNP43D32.001", "doi": "10.5067/VIIRS/VNP43D32.001", "longName": "VIIRS/NPP BRDF/Albedo Parameter 2 NIR Daily L3 Global 30 ArcSec CMG V001" }
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[ "Dataset" ]
{ "temporalExtentStart": "2012-01-19T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C1607330208-LPDAAC_ECS", "globalId": "34836681-5cf3-508d-9b06-a99bf395ebb5", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "The NASA/NOAA Suomi National Polar-orbiting Partnership (Suomi NPP) Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Valid Observation Band M3 product (VNP43D44) 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 VNP43D 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 VNP43D product contains just one data layer for each of the parameters included in the VNP43MA2 (https://doi.org/10.5067/VIIRS/VNP43MA2.001) product. VNP43D40 through VNP43D53 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 VNP43MA2 product page and in the Algorithm Theoretical Basis Document (ATBD). \r\rVNP43D44 contains the valid observation quality layer representing each of the 16 days of the retrieval period for VIIRS band M3.", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "VNP43D44", "landingPageUrl": "https://doi.org/10.5067/VIIRS/VNP43D44.001", "doi": "10.5067/VIIRS/VNP43D44.001", "longName": "VIIRS/NPP BRDF/Albedo Valid Observation Band M3 Daily L3 Global 30ArcSec CMG V001" }
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[ "Dataset" ]
{ "temporalExtentStart": "2002-07-04T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2565805805-LPCLOUD", "globalId": "f1f4725b-7ea3-53cc-8b94-5861ee008b5c", "pagerank_publication_dataset": 0.15796875000000002, "abstract": "A new suite of MODIS Land Surface Temperature and Emissivity (LST&E) products are available in Collection 6.1. The MYD21 LST algorithm differs from the algorithm of the MYD11 (https://doi.org/10.5067/modis/myd11_l2.061) 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 MYD21 (https://doi.org/10.5067/MODIS/MYD21.061) 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&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 (https://lpdaac.usgs.gov/documents/1399/MOD21_ATBD.pdf)).Validation at stage 1 (https://modis-land.gsfc.nasa.gov/MODLAND_val.html) has been achieved for the MODIS Land Surface Temperature and Emissivity data products. Further details regarding MODIS land product validation for the MYD21 data products are available from the MODIS Land Team Validation site (https://modis-land.gsfc.nasa.gov/ValStatus.php?ProductID=MOD21).Improvements/Changes from Previous Versions* 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.* A polarization correction has been applied to the L1B Reflective Solar Bands (RSB).* Three new CMG products are available in the MxD21 suite (MxD21C1/C2/C3).", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "MYD21C1", "landingPageUrl": "https://doi.org/10.5067/MODIS/MYD21C1.061", "doi": "10.5067/MODIS/MYD21C1.061", "longName": "MODIS/Aqua Land Surface Temperature/3-Band Emissivity Daily L3 Global 0.05Deg CMG V061" }
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[ "Dataset" ]
{ "temporalExtentStart": "2012-01-19T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C1607325920-LPDAAC_ECS", "globalId": "9b0cf045-78c8-5df7-9b87-2d966eada3d7", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "The NASA/NOAA Suomi National Polar-orbiting Partnership (Suomi NPP) Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 3 Band M10 product (VNP43D24) 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 VNP43D 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 VNP43D 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 VNP43MA1 (https://doi.org/10.5067/VIIRS/VNP43MA1.001) product is stored in a separate file as VNP43D01 through VNP43D36. In addition to the bands included in VNP43MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VNP43D37 through VNP43D39. Details regarding methodology are available on the VNP43MA1 product page and in the Algorithm Theoretical Basis Document (ATBD).\r\rVNP43D24 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.\r", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "VNP43D24", "landingPageUrl": "https://doi.org/10.5067/VIIRS/VNP43D24.001", "doi": "10.5067/VIIRS/VNP43D24.001", "longName": "VIIRS/NPP BRDF/Albedo Parameter 3 Band M10 Daily L3 Global 30 ArcSec CMG V001" }
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[ "Dataset" ]
{ "temporalExtentStart": "2018-07-09T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -54, "longitude": 180, "height": null }, "cmrId": "C1545228916-LPDAAC_ECS", "globalId": "f59c669a-ba6a-5242-85ae-8abe5c46b1f4", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "The ECO1BMAPRAD Version 1 data product was decommissioned on February 14, 2025. Users are encouraged to use the ECO_L1CT_RAD Version 2 data product (https://doi.org/10.5067/ECOSTRESS/ECO_L1CT_RAD.002).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 ECOSTRESS website (https://ecostress.jpl.nasa.gov/science).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 = 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.", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 54, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "2025-01-06T23:59:09.000Z", "shortName": "ECO1BMAPRAD", "landingPageUrl": "https://doi.org/10.5067/ECOSTRESS/ECO1BMAPRAD.001", "doi": "10.5067/ECOSTRESS/ECO1BMAPRAD.001", "longName": "ECOSTRESS Resampled Radiance Daily L1B Global 70m V001" }
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[ "Dataset" ]
{ "temporalExtentStart": "2000-04-01T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2763266343-LPCLOUD", "globalId": "06af93a5-5cab-5f12-8d77-599d1968ba79", "pagerank_publication_dataset": 0.6809471204229799, "abstract": "The NASA Making Earth System Data Records for Use in Research Environments (MEaSUREs) (https://earthdata.nasa.gov/about/competitive-programs/measures) Combined ASTER and MODIS Emissivity for Land (CAMEL) dataset provides monthly emissivity uncertainty at 0.05 degree (~5 kilometer) resolution (CAM5K30UC). CAM5K30UC is an estimation of total emissivity uncertainty, comprising 3 independent components of variability: temporal, spatial, and algorithm. Each measure of uncertainty is provided for all 13 hinge points of emissivity and each latitude-longitude point. Additional details regarding the methodology are available in the User Guide and Algorithm Theoretical Basis Document (ATBD) (https://lpdaac.usgs.gov/documents/219/cam5k30_v2_user_guide_atbd.pdf). Corresponding emissivity values can be found in the CAM5K30EM data product.Provided in the CAM5K30UC product are layers for algorithm uncertainty, spatial uncertainty, temporal uncertainty, total uncertainty, latitude, longitude, spectral wavelength, CAMEL quality, and total uncertainty quality information.", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "monthly", "temporalExtentEnd": "2017-01-01T00:00:00.000Z", "shortName": "CAM5K30UC", "landingPageUrl": "https://doi.org/10.5067/MEaSUREs/LSTE/CAM5K30UC.002", "doi": "10.5067/MEaSUREs/LSTE/CAM5K30UC.002", "longName": "Combined ASTER and MODIS Emissivity database over Land (CAMEL) Uncertainty Monthly Global 0.05Deg V002" }
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[ "Dataset" ]
{ "temporalExtentStart": "2002-07-04T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2307290656-LPCLOUD", "globalId": "df09e919-9c42-51a6-9f59-4c36f326a7b9", "pagerank_publication_dataset": 24.904334131991575, "abstract": "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. Validation at stage 3 (https://modis-land.gsfc.nasa.gov/MODLAND_val.html) has been achieved for the MODIS Vegetation Index product suite. Further details regarding MODIS land product validation for the MOD13 data products are available from the MODIS Land Team Validation site (https://modis-land.gsfc.nasa.gov/ValStatus.php?ProductID=MOD13).Improvements/Changes from Previous Versions* 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.* A polarization correction has been applied to the L1B Reflective Solar Bands (RSB).", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "Unknown", "temporalExtentEnd": "", "shortName": "MYD13Q1", "landingPageUrl": "https://doi.org/10.5067/MODIS/MYD13Q1.061", "doi": "10.5067/MODIS/MYD13Q1.061", "longName": "MODIS/Aqua Vegetation Indices 16-Day L3 Global 250m SIN Grid V061" }
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[ "Dataset" ]
{ "temporalExtentStart": "2012-01-19T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C1607340690-LPDAAC_ECS", "globalId": "242e3909-6ad1-554e-ba71-2e7cc525ff24", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "The NASA/NOAA Suomi National Polar-orbiting Partnership (Suomi NPP) Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo white-sky albedo for band M2 (VNP43D68) 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 VNP43D 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 VNP43D product contains just one data layer. \r\rVNP43D54 through VNP43D79 are the albedo products of the VNP43D 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 VNP43MA3 (https://doi.org/10.5067/VIIRS/VNP43MA3.001) product. In addition to the bands included in VNP43MA3, 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 VNP43MA3 product page and in the Algorithm Theoretical Basis Document (ATBD).\r\rVNP43D68 is the WSA for VIIRS band M2 (0.445 μm). ", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "VNP43D68", "landingPageUrl": "https://doi.org/10.5067/VIIRS/VNP43D68.001", "doi": "10.5067/VIIRS/VNP43D68.001", "longName": "VIIRS/NPP BRDF/Albedo WSA at Solar Noon Band M2 Daily L3 Global 30ArcSec CMG V001" }
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[ "Dataset" ]
{ "temporalExtentStart": "1984-03-01T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2763268458-LPCLOUD", "globalId": "e915f865-e5bd-5e97-bdaa-cf69b6087487", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "The NASA Making Earth System Data Records for Use in Research Environments (MEaSUREs) Global Web-Enabled Landsat Data Monthly (GWELDMO) Version 3.1 data product provides Landsat data at 30 meter (m) resolution for terrestrial non-Antarctica locations over monthly reporting periods for the 1985, 1990, and 2000 epochs. GWELD data products are generated from all available Landsat 4 and 5 Thematic Mapper (TM) and Landsat 7 Enhanced Thematic Mapper Plus (ETM+) data in the U.S. Geological Survey (USGS) Landsat archive. The GWELD suite of products provide consistent data to derive land cover as well as geophysical and biophysical information for regional assessment of land surface dynamics.\r\rThe GWELD products include Nadir Bidirectional Reflectance Distribution Function (BRDF)-Adjusted Reflectance (NBAR) for the reflective wavelength bands and to top of atmosphere (TOA) brightness temperature for the thermal bands. The products are defined in the Sinusoidal coordinate system to promote continuity of NASA’s Moderate Resolution Imaging Spectroradiometer (MODIS) land tile grid.\r\rProvided in the GWELDMO product are layers for surface reflectance bands 1 through 5 and 7, TOA brightness temperature for thermal bands, Normalized Difference Vegetation Index (NDVI), day of year, ancillary angle, and data quality information. A low-resolution red, green, blue (RGB) browse image of bands 5, 4, 3 is also available for each granule.\r\rVersion 3.1 products use Landsat Collection 1 products as input and have improved per-pixel cloud mask, new quality data, improved calibration information, and improved product metadata that enable view and solar geometry calculations.", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "monthly", "temporalExtentEnd": "2001-11-30T23:59:59.999Z", "shortName": "GWELDMO", "landingPageUrl": "https://doi.org/10.5067/MEaSUREs/GWELD/GWELDMO.031", "doi": "10.5067/MEaSUREs/GWELD/GWELDMO.031", "longName": "NASA Global Web-Enabled Landsat Data Monthly Global 30 m V031" }
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[ "Dataset" ]
{ "temporalExtentStart": "2000-03-04T20:34:04.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C1000000320-LPDAAC_ECS", "globalId": "783cfd5c-9ba8-54da-b75f-4e18e456e177", "pagerank_publication_dataset": 8.904023457237074, "abstract": "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) (https://doi.org/10.5067/ASTER/AST_L1B.003), 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) (https://doi.org/10.5067/ASTER/AST_L1A.003) 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.\r\rThe 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).\r\rFor 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 in both as a text file and a single band browse images with the valid GCPs overlaid.\r\rThis 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 (AST_L1A) (https://doi.org/10.5067/ASTER/AST_L1A.003) dataset. ", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "Unknown", "temporalExtentEnd": "", "shortName": "AST_L1T", "landingPageUrl": "https://doi.org/10.5067/ASTER/AST_L1T.003", "doi": "10.5067/ASTER/AST_L1T.003", "longName": "ASTER Level 1 precision terrain corrected registered at-sensor radiance V003" }
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[ "Dataset" ]
{ "temporalExtentStart": "2002-07-04T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2565794007-LPCLOUD", "globalId": "55cc527d-70a8-5d3a-87ba-c80387a4bf5a", "pagerank_publication_dataset": 0.9641383482142858, "abstract": "The MYD11B1 Version 6.1 product provides daily per pixel Land Surface Temperature and Emissivity (LST&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 MYD11_L2 (https://doi.org/10.5067/MODIS/MYD11_L2.061) swath product aggregated to the 6 km grid. Validation at stage 2 (https://modis-land.gsfc.nasa.gov/MODLAND_val.html) has been achieved for all MODIS Land Surface Temperature and Emissivity products. Further details regarding MODIS land product validation for the MYD11 data products are available from the MODIS Land Team Validation site (https://modis-land.gsfc.nasa.gov/ValStatus.php?ProductID=MOD11).Improvements/Changes from Previous Versions* 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.* A polarization correction has been applied to the L1B Reflective Solar Bands (RSB).", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "MYD11B1", "landingPageUrl": "https://doi.org/10.5067/MODIS/MYD11B1.061", "doi": "10.5067/MODIS/MYD11B1.061", "longName": "MODIS/Aqua Land Surface Temperature/Emissivity Daily L3 Global 6km SIN Grid V061" }
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[ "Dataset" ]
{ "temporalExtentStart": "2015-11-28T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C3246894861-LPCLOUD", "globalId": "53e40303-ed75-568c-be47-50079cf89937", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "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 HLSS30 Vegetation Indices (HLSS30_VI) product is derived from Sentinel-2A, Sentinel-2B, and Sentinel-2C MSI 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 (MGRS) tiling system, and thus are “stackable” for time series analysis.The HLSS30_VI product is provided in Cloud Optimized GeoTIFF (COG) format, and each band is distributed as a separate file. Nine indicators of vegetation health are included in the HLSS30_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 HLSS30_VI product.", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "HLSS30_VI", "landingPageUrl": "https://doi.org/10.5067/HLS/HLSS30_VI.002", "doi": "10.5067/HLS/HLSS30_VI.002", "longName": "HLS Sentinel-2 Multi-spectral Instrument Vegetation Indices Daily Global 30 m V2.0" }
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[ "Dataset" ]
{ "temporalExtentStart": "2022-08-09T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -54, "longitude": 180, "height": null }, "cmrId": "C2408009906-LPCLOUD", "globalId": "edf6438e-4782-5c36-87bf-eb53702b8f82", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "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 degrees N latitude and 52 degrees 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) EMIT Open Data Portal (https://earth.jpl.nasa.gov/emit/data/data-portal/coverage-and-forecasts/).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 kilometer (km) by 75 km, nominal at the equator, and 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.", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 54, "longitude": -180, "height": null }, "temporalFrequency": "Unknown", "temporalExtentEnd": "", "shortName": "EMITL1BRAD", "landingPageUrl": "https://doi.org/10.5067/EMIT/EMITL1BRAD.001", "doi": "10.5067/EMIT/EMITL1BRAD.001", "longName": "EMIT L1B At-Sensor Calibrated Radiance and Geolocation Data 60 m V001" }
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[ "Dataset" ]
{ "temporalExtentStart": "2018-07-15T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -54, "longitude": 180, "height": null }, "cmrId": "C1534731034-LPDAAC_ECS", "globalId": "48fc5c82-d216-58c9-a442-94bbe4333b06", "pagerank_publication_dataset": 0.16593750000000002, "abstract": "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 ECOSTRESS website (https://ecostress.jpl.nasa.gov/science).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.", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 54, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "2023-02-25T23:59:59.000Z", "shortName": "ECO4WUE", "landingPageUrl": "https://doi.org/10.5067/ECOSTRESS/ECO4WUE.001", "doi": "10.5067/ECOSTRESS/ECO4WUE.001", "longName": "ECOSTRESS Water Use Efficiency Daily L4 Global 70m V001" }
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[ "Dataset" ]
{ "temporalExtentStart": "2012-01-19T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2847929303-LPCLOUD", "globalId": "009a85d0-b220-59db-a0ac-4f872a7d16e8", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "The NASA/NOAA Suomi National Polar-orbiting Partnership (Suomi NPP) 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 VNP43DNBA4 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 VNP43 data products are designed after the Moderate Resolution Imaging Spectroradiometer (MODIS) BRDF/Albedo product suite.The VNP43 algorithm uses the RossThick/Li-Sparse-Reciprocal (RTLSR) semi-empirical kernel-driven BRDF model, with the three kernel weights from VNP43DNBA1 to reconstruct surface anisotropic effects, correcting the directional reflectance to a common view geometry (VNP43DNBA4), while also computing integrated black-sky albedo (BSA) at local solar noon and white-sky albedo (WSA) (VNP43DNBA3). 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 VNP43DNBA4 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.", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "VNP43DNBA4", "landingPageUrl": "https://doi.org/10.5067/VIIRS/VNP43DNBA4.002", "doi": "10.5067/VIIRS/VNP43DNBA4.002", "longName": "VIIRS/NPP DNB BRDF/Albedo Nadir BRDF-Adjusted Ref Daily L3 Global 1km SIN Grid V002" }
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[ "Dataset" ]
{ "temporalExtentStart": "2012-01-19T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C1607335278-LPDAAC_ECS", "globalId": "287f6f72-7a6a-53ee-ace6-a5337bee185b", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "The NASA/NOAA Suomi National Polar-orbiting Partnership (Suomi NPP) Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Black-Sky Albedo for Band M8 (VNP43D60) 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 VNP43D 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 VNP43D product contains just one data layer. \r\rVNP43D54 through VNP43D79 are the albedo products of the VNP43D 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 VNP43MA3 (https://doi.org/10.5067/VIIRS/VNP43MA3.001) product. In addition to the bands included in VNP43MA3, 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 VNP43MA3 product page and in the Algorithm Theoretical Basis Document (ATBD).\r\rVNP43D60 is the BSA for VIIRS band M8 (1.240 μm). \r", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "VNP43D60", "landingPageUrl": "https://doi.org/10.5067/VIIRS/VNP43D60.001", "doi": "10.5067/VIIRS/VNP43D60.001", "longName": "VIIRS/NPP BRDF/Albedo BSA at Solar Noon Band M8 Daily L3 Global 30ArcSec CMG V001" }
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[ "Dataset" ]
{ "temporalExtentStart": "2012-01-19T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C1607343322-LPDAAC_ECS", "globalId": "00e9b4bd-1055-5edf-87ee-2c1c096cbaea", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "The NASA/NOAA Suomi National Polar-orbiting Partnership (Suomi NPP) Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo white-sky albedo for band M7 (VNP43D72) 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 VNP43D 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 VNP43D product contains just one data layer. \r\rVNP43D54 through VNP43D79 are the albedo products of the VNP43D 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 VNP43MA3 (https://doi.org/10.5067/VIIRS/VNP43MA3.001) product. In addition to the bands included in VNP43MA3, 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 VNP43MA3 product page and in the Algorithm Theoretical Basis Document (ATBD).\r\rVNP43D72 is the WSA for VIIRS band M7 (0.865 μm). ", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "VNP43D72", "landingPageUrl": "https://doi.org/10.5067/VIIRS/VNP43D72.001", "doi": "10.5067/VIIRS/VNP43D72.001", "longName": "VIIRS/NPP BRDF/Albedo WSA at Solar Noon Band M7 Daily L3 Global 30ArcSec CMG V001" }
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[ "Dataset" ]
{ "temporalExtentStart": "2018-07-09T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -54, "longitude": 180, "height": null }, "cmrId": "C2595678497-LPCLOUD", "globalId": "665e0ff7-af56-5af0-81b1-846f40b3dc9c", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "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 ECOSTRESS website (https://ecostress.jpl.nasa.gov/science).The ECOSTRESS Gridded Top of Atmosphere Calibrated Radiance Instantaneous Level 1C Global 70 m (ECO_L1CG_RAD) Version 2 data product provides at-sensor calibrated radiance values retrieved for five thermal infrared (TIR) bands operating between 8 and 12.5 micons. This product is a gridded version of the ECO_L1B_RAD (https://doi.org/10.5067/ECOSTRESS/ECO_L1B_RAD.002) Version 2 data product that has been resampled by nearest neighbor, projected to a globally snapped 0.0006 degree grid, and repackaged as the ECO_L1CG_RAD data product.The ECO_L1CG_RAD Version 2 data product contains 12 layers distributed in an HDF5 format file containing radiance values for the five TIR bands, associated data quality indicators, and cloud and water masks. 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.* 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 ECO_L1B_RAD 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 ECO_L1B_RAD User Guide.* Scan flipping: Improvements to the visualization of the data to compensate for instrument orientation are discussed in Section 3.4 of the ECO_L1B_RAD User Guide.* 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.", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 54, "longitude": -180, "height": null }, "temporalFrequency": "Unknown", "temporalExtentEnd": "", "shortName": "ECO_L1CG_RAD", "landingPageUrl": "https://doi.org/10.5067/ECOSTRESS/ECO_L1CG_RAD.002", "doi": "10.5067/ECOSTRESS/ECO_L1CG_RAD.002", "longName": "ECOSTRESS Gridded Top of Atmosphere Calibrated Radiance Instantaneous L1C Global 70 m V002" }
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[ "Dataset" ]
{ "temporalExtentStart": "2016-01-01T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": 0, "longitude": 0, "height": null }, "cmrId": "C2102664483-LPDAAC_ECS", "globalId": "59471884-61a5-5ad4-a6a4-9e0cab0e024c", "pagerank_publication_dataset": 3.7643051105617866, "abstract": "The Multi-Source Land Surface Phenology (LSP) Yearly North America 30 meter (m) Version 1.1 product (MSLSP) provides a Land Surface Phenology product for North America derived from Harmonized Landsat Sentinel-2 (HLS) data. Data from the combined Landsat 8 Operational Land Imager (OLI) and Sentinel-2A and 2B Multispectral Instrument (MSI) provides the user community with dates of phenophase transitions, including the timing of greenup, maturity, senescence, and dormancy at 30m spatial resolution. These data sets are useful for a wide range of applications, including ecosystem and agro-ecosystem modeling, monitoring the response of terrestrial ecosystems to climate variability and extreme events, crop-type discrimination, and land cover, land use, and land cover change mapping. \r\rProvided in the MSLSP product are layers for percent greenness, onset greenness dates, Enhanced Vegetative Index (EVI2) amplitude, and maximum EVI2, and data quality information for up to two phenological cycles per year. For areas where the data values are missing due to cloud cover or other reasons, the data gaps are filled with good quality values from the year directly preceding or following the product year. A low resolution browse image representing maximum EVI is also available for each MSLSP30NA granule.\r", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "Unknown", "temporalExtentEnd": "2019-12-31T23:59:59.000Z", "shortName": "MSLSP30NA", "landingPageUrl": "https://doi.org/10.5067/Community/MuSLI/MSLSP30NA.011", "doi": "10.5067/Community/MuSLI/MSLSP30NA.011", "longName": "MuSLI Multi-Source Land Surface Phenology Yearly North America 30 m V011" }
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[ "Dataset" ]
{ "temporalExtentStart": "2011-06-30T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": 10, "longitude": -50, "height": null }, "cmrId": "C2763264728-LPCLOUD", "globalId": "f767ce75-214d-57db-90c6-f57e32ec0f89", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "Goddard’s LiDAR, Hyperspectral, and Thermal Imager (G-LiHT) 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.\r\rThe purpose of G-LiHT’s Hyperspectral Ancillary data product (GLHYANC) is to provide information related to aircraft attitude and altitude, view and solar angles, and other ancillary reflectance and radiance data. \r\rGLHYANC data are processed as a zipped raster data product (GeoTIFF) with associated header file (.hdr) at 1 meter spatial resolution over locally defined areas.\r", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 73, "longitude": -170, "height": null }, "temporalFrequency": "Unknown", "temporalExtentEnd": "", "shortName": "GLHYANC", "landingPageUrl": "https://doi.org/10.5067/Community/GLIHT/GLHYANC.001", "doi": "10.5067/Community/GLIHT/GLHYANC.001", "longName": "G-LiHT Hyperspectral Ancillary V001" }
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[ "Dataset" ]
{ "temporalExtentStart": "2020-01-01T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2801693973-LPDAAC_ECS", "globalId": "17240c85-c620-5468-ba84-a6820c3ad61f", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "LPJ-PROSAIL simulated data products are produced through the coupling of the Lund-Potsdam-Jena dynamic global vegetation model (LPJ) and PROSAIL, a radiative transfer model. The simulated imaging spectroscopy data were produced to aid in the development of workflows, algorithm testing, and other activities during the lead up to future global spaceborne imaging spectroscopy missions such as NASA’s Surface Biology and Geology (SBG). The LPJ-PROSAIL Level 2 Global Simulated Dynamic Surface Reflectance (LPJ_L2_SSREF) Version 1 data product provides simulated dynamic surface reflectance data in five Network Common Data Format 4 (netCDF4) files, each containing a different reflectance stream at a spatial resolution of 0.5 degrees (~50 kilometers): bidirectional (BDR), bi-hemispherical (BHR), hemispherical-directional (HDR), directional-hemispherical (DHR), and directional (DR). Each reflectance file within a granule contains simulated surface reflectance measurements of 211 bands with 10 nanometer (nm) spectral resolution across a spectral range of 400 to 2500 nm for the entire globe. The data are presented with four dimensions: latitude, longitude, bands (wavelength), and time. Each netCDF4 file holds a one-dimensional list for each of the four dimensions containing the values that are associated with those dimensions. LPJ_L2_SSREF Version 1 is composed of one granule containing data for the year 2020 with monthly time increments. \rData Usage Warning - Due to the simulated nature of these data, they should not be used for any real-world scientific analyses or conclusions. These data are meant to be used in development of workflows, algorithms, and other instances where large imaging spectroscopy datasets are needed for testing. These data are not intended for scientific use. ", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "monthly", "temporalExtentEnd": "2020-12-31T23:59:59.000Z", "shortName": "LPJ_L2_SSREF", "landingPageUrl": "https://doi.org/10.5067/Community/LPJ-PROSAIL/LPJ_L2_SSREF.001", "doi": "10.5067/Community/LPJ-PROSAIL/LPJ_L2_SSREF.001", "longName": "LPJ-PROSAIL L2 Global Simulated Dynamic Surface Reflectance V001" }
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[ "Dataset" ]
{ "temporalExtentStart": "2012-01-19T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C1607319156-LPDAAC_ECS", "globalId": "6c44ab46-dcf4-5b38-96cd-dc7259473525", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "The NASA/NOAA Suomi National Polar-orbiting Partnership (Suomi NPP) Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 1 Band M8 product (VNP43D19) 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 VNP43D 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 VNP43D 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 VNP43MA1 (https://doi.org/10.5067/VIIRS/VNP43MA1.001) product is stored in a separate file as VNP43D01 through VNP43D36. In addition to the bands included in VNP43MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VNP43D37 through VNP43D39. Details regarding methodology are available on the VNP43MA1 product page and in the Algorithm Theoretical Basis Document (ATBD).\r\rVNP43D19 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.\r\r", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "VNP43D19", "landingPageUrl": "https://doi.org/10.5067/VIIRS/VNP43D19.001", "doi": "10.5067/VIIRS/VNP43D19.001", "longName": "VIIRS/NPP BRDF/Albedo Parameter 1 Band M8 Daily L3 Global 30 ArcSec CMG V001" }
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[ "Dataset" ]
{ "temporalExtentStart": "1982-01-01T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2763266333-LPCLOUD", "globalId": "0c3b0b8b-40ce-5252-8553-884363ed00b8", "pagerank_publication_dataset": 6.2101456921624685, "abstract": "The NASA Making Earth System Data Records for Use in Research Environments (MEaSUREs) (https://earthdata.nasa.gov/community/community-data-system-programs/measures-projects) Vegetation Continuous Fields (VCF) Version 1 data product (VCF5KYR) provides global fractional vegetation cover at 0.05 degree (5,600 meter) spatial resolution at yearly intervals from 1982 to 2016. The VCF5KYR data product is derived from a bagged linear model algorithm using Long Term Data Record Version 4 (LTDR V4) data compiled from Advanced Very High Resolution Radiometer (AVHRR) observations. Fractional vegetation cover (FVC) is the ratio of the area of the vertical projection of green vegetation above ground to the total area, capturing the horizontal distribution and density of vegetation on the Earth’s surface. FVC is a primary means for measuring global forest cover change and is a key parameter for a variety of environmental and climate-related applications, including carbon land surface models and biomass measurements. The three bands included in each VCF5KYR Version 1 GeoTIFF are: percent of tree cover, non-tree vegetation, and bare ground. A water mask was applied with all pure water pixels (defined as ≥ 95% water coverage) set to zero.\r\rData from years 1994 and 2000 were excluded due to lack of data in the LTDR V4.", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "Unknown", "temporalExtentEnd": "2016-12-31T23:59:59.999Z", "shortName": "VCF5KYR", "landingPageUrl": "https://doi.org/10.5067/MEaSUREs/VCF/VCF5KYR.001", "doi": "10.5067/MEaSUREs/VCF/VCF5KYR.001", "longName": "MEaSUREs Vegetation Continuous Fields (VCF) Yearly Global 0.05 Deg V001" }
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[ "Dataset" ]
{ "temporalExtentStart": "2012-01-19T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C1607341867-LPDAAC_ECS", "globalId": "4812c58e-920b-55ce-bc43-53dc221decb6", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "The NASA/NOAA Suomi National Polar-orbiting Partnership (Suomi NPP) Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo white-sky albedo for band M4 (VNP43D70) 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 VNP43D 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 VNP43D product contains just one data layer. \r\rVNP43D54 through VNP43D79 are the albedo products of the VNP43D 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 VNP43MA3 (https://doi.org/10.5067/VIIRS/VNP43MA3.001) product. In addition to the bands included in VNP43MA3, 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 VNP43MA3 product page and in the Algorithm Theoretical Basis Document (ATBD).\r\rVNP43D70 is the WSA for VIIRS band M4 (0.555 μm). \r", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "VNP43D70", "landingPageUrl": "https://doi.org/10.5067/VIIRS/VNP43D70.001", "doi": "10.5067/VIIRS/VNP43D70.001", "longName": "VIIRS/NPP BRDF/Albedo WSA at Solar Noon Band M4 Daily L3 Global 30ArcSec CMG V001" }
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[ "Dataset" ]
{ "temporalExtentStart": "2000-02-24T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2484086031-LPCLOUD", "globalId": "282f7ac3-a2ca-592d-91df-1dc704438fb7", "pagerank_publication_dataset": 4.117172041153291, "abstract": "The MCD19A1 Version 6.1 data product is a Moderate Resolution Imaging Spectroradiometer (MODIS) Terra and Aqua combined Land Surface Bidirectional Reflectance Factor (BRF) gridded Level 2 product produced daily at 500 meter (m) and 1 kilometer (km) pixel resolutions. The MCD19A1 product is corrected for atmospheric gases and aerosols using a Multi-Angle Implementation of Atmospheric Correction (MAIAC) algorithm that is based on a time series analysis and a combination of pixel- and image-based processing. The MODIS MAIAC Land Surface BRF products provide an estimate of the surface spectral reflectance as it would be measured at ground-level in the absence of atmospheric scattering or absorption.The MCD19A1 MAIAC Surface Reflectance data product includes 31 Science Dataset (SDS) layers: surface reflectance for bands 1-12, BRF uncertainty for bands 1-2, Quality Assessment (QA) bits at 1 km, surface reflectance for bands 1-7 at 500 m, cosine of solar zenith angle, cosine of view zenith angle, relative azimuth angle, scattering angle, solar azimuth angle, view azimuth angle, glint angle, RossThick/Li-Sparse (RTLS) volumetric kernel, and RTLS geometric kernel at 5 km. A low-resolution browse image is also included showing surface reflectance band combination 1, 4, 3 created using a composite of all available orbits.Each SDS layer within each MCD19A1 Hierarchical Data Format 4 (HDF4) file contains a third dimension that represents the number of orbit overpasses. This factor could affect the total number of bands for each SDS layer.Known Issues* Known issues are described in Section 6 of the User Guide. * For complete information about known issues please refer to the MODIS/VIIRS Land Quality Assessment website (https://landweb.modaps.eosdis.nasa.gov/knownissue?sensor=MODIS&sat=TerraAqua&as=61).Improvements/Changes from Previous Versions* 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.* A polarization correction has been applied to the L1B Reflective Solar Bands (RSB).* The MCD19 Version 6.1 products have added 250 m resolution bands.* The previous BRDF product (MCD19A3) was reported once every eight days and the new MCD19A3D is a daily product.* MCD19A3D introduces gap-filled NDVI and gap-filled 250 m NBAR. * Snow Fraction, Snow Fit, and Snow Grain size layers were moved from MCD19A1 to the MCD19A3D.* There are four additional Climate Modeling Grid (CMG) products: MCD19A1CMGL, MCD19A1GO, MCD19A2CMG, and MCD19A3CMG.", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "MCD19A1", "landingPageUrl": "https://doi.org/10.5067/MODIS/MCD19A1.061", "doi": "10.5067/MODIS/MCD19A1.061", "longName": "MODIS/Terra+Aqua Land Surface BRF Daily L2G Global 500m and 1km SIN Grid V061" }
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[ "Dataset" ]
{ "temporalExtentStart": "2000-02-11T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -56, "longitude": 180, "height": null }, "cmrId": "C2763266360-LPCLOUD", "globalId": "420021f9-49ec-5272-80d7-b88a5800b175", "pagerank_publication_dataset": 147.9901580210313, "abstract": "The Land Processes Distributed Active Archive Center (LP DAAC) is responsible for the archive and distribution of the NASA Making Earth System Data Records for Use in Research Environments (MEaSUREs) (https://earthdata.nasa.gov/about/competitive-programs/measures) version SRTM, which includes the global 1 arc second (~30 meter) product.NASA Shuttle Radar Topography Mission (SRTM) datasets result from a collaborative effort by the National Aeronautics and Space Administration (NASA) and the National Geospatial-Intelligence Agency (NGA - previously known as the National Imagery and Mapping Agency, or NIMA), as well as the participation of the German and Italian space agencies. The purpose of SRTM was to generate a near-global digital elevation model (DEM) of the Earth using radar interferometry. SRTM was a primary component of the payload on the Space Shuttle Endeavour during its STS-99 mission. Endeavour launched February 11, 2000 and flew for 11 days.Each SRTMGL1 data tile contains a mosaic and blending of elevations generated by averaging all \"data takes\" that fall within that tile. These elevation files use the extension “.HGT”, meaning height (such as N37W105.SRTMGL1.HGT). The primary goal of creating the Version 3 data was to eliminate voids that were present in earlier versions of SRTM data. In areas with limited data, existing topographical data were used to supplement the SRTM data to fill the voids. The source of each elevation pixel is identified in the corresponding (SRTMGL1N) (https://doi.org/10.5067/MEaSUREs/SRTM/SRTMGL1N.003) product (such as N37W105.SRTMGL1N.NUM).SRTM collected data in swaths, which extend from ~30 degrees off-nadir to ~58 degrees off-nadir from an altitude of 233 kilometers (km). These swaths are ~225 km wide, and consisted of all land between 60° N and 56° S latitude. This accounts for about 80% of Earth’s total landmass. ", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 60, "longitude": -180, "height": null }, "temporalFrequency": "Unknown", "temporalExtentEnd": "2000-02-21T23:59:59.000Z", "shortName": "SRTMGL1", "landingPageUrl": "https://doi.org/10.5067/MEaSUREs/SRTM/SRTMGL1.003", "doi": "10.5067/MEASURES/SRTM/SRTMGL1.003", "longName": "NASA Shuttle Radar Topography Mission Global 1 arc second V003" }
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71
[ "Dataset" ]
{ "temporalExtentStart": "2000-02-16T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2539907962-LPCLOUD", "globalId": "5e8d279d-0912-55da-8455-9d392f0d63b5", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "The MCD43D20 Version 6.1 Bidirectional Reflectance Distribution Function and Albedo (BRDF/Albedo) Model Parameter dataset is produced daily using 16 days of Terra and Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) data at 30 arc second (1,000 meter) resolution. Data are temporally weighted to the ninth day which is reflected in the Julian date in the file name. This Climate Modeling Grid (CMG) product covers the entire globe for use in climate simulation models. Due to the large file size, each MCD43D product contains just one data layer. Each of the three model parameters (isotropic, volumetric, and geometric) for each of the MODIS bands 1 through 7 and the visible, near infrared (NIR), and shortwave bands included in MCD43C1 (https://doi.org/10.5067/MODIS/MCD43C1.061) are stored in a separate file as MCD43D01 through MCD43D30. \r\rMCD43D20 is the BRDF volumetric parameter for MODIS band 7. The volumetric parameter, in conjunction with the isotropic and geometric parameters, is used to derive the BRDF/Albedo values for MODIS band 7. \r\rImprovements/Changes from Previous Versions \r\r* 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.\r* A polarization correction has been applied to the L1B Reflective Solar Bands (RSB).\r", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "MCD43D20", "landingPageUrl": "https://doi.org/10.5067/MODIS/MCD43D20.061", "doi": "10.5067/MODIS/MCD43D20.061", "longName": "MODIS/Terra+Aqua BRDF/Albedo Parameter2 Band7 Daily L3 Global 30ArcSec CMG V061" }
node
72
[ "Dataset" ]
{ "temporalExtentStart": "2012-01-19T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C1607332800-LPDAAC_ECS", "globalId": "84f4d383-d876-5af9-80dc-af17370dea2c", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "The NASA/NOAA Suomi National Polar-orbiting Partnership (Suomi NPP) Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Valid Observation Day/Night Band (DNB) product (VNP43D51) 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 VNP43D 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 VNP43D product contains just one data layer for each of the parameters included in the VNP43MA2 (https://doi.org/10.5067/VIIRS/VNP43MA2.001) product. VNP43D40 through VNP43D53 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 VNP43MA2 product page and in the Algorithm Theoretical Basis Document (ATBD). \r\rVNP43D51 contains the valid observation quality layer representing each of the 16 days of the retrieval period for VIIRS DNB.", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "VNP43D51", "landingPageUrl": "https://doi.org/10.5067/VIIRS/VNP43D51.001", "doi": "10.5067/VIIRS/VNP43D51.001", "longName": "VIIRS/NPP BRDF/Albedo Valid Observation DNB Daily L3 Global 30ArcSec CMG V001" }
node
73
[ "Dataset" ]
{ "temporalExtentStart": "2012-01-19T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C1629258322-LPDAAC_ECS", "globalId": "2808c1ea-a762-52c1-a055-532d8f6a85ac", "pagerank_publication_dataset": 0.21375000000000002, "abstract": "The NASA/NOAA Suomi National Polar-orbiting Partnership (Suomi NPP) 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 1 product (VNP43C4) is derived from the 30 arc second CMG VNP43D Version 1 product suite. VNP43C3 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 VNP43 algorithm uses the RossThick/Li-Sparse-Reciprocal (RTLSR) semi-empirical kernel-driven BRDF model, with the three kernel weights from VNP43C1 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. \r\rThe VNP43C3 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.\r", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "VNP43C4", "landingPageUrl": "https://doi.org/10.5067/VIIRS/VNP43C4.001", "doi": "10.5067/VIIRS/VNP43C4.001", "longName": "VIIRS/NPP BRDF/Albedo Nadir BRDF-Adjusted Reflectance Daily L3 Global 0.05Deg CMG V001" }
node
74
[ "Dataset" ]
{ "temporalExtentStart": "2002-07-01T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2565794055-LPCLOUD", "globalId": "40f81b9b-4a21-5338-a803-a6a6a63e3c90", "pagerank_publication_dataset": 8.59762319815702, "abstract": "The 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 MYD13A2 (https://doi.org/10.5067/MODIS/MYD13A2.061) 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. Validation at stage 3 (https://modis-land.gsfc.nasa.gov/MODLAND_val.html) has been achieved for the MODIS Vegetation Index product suite. Further details regarding MODIS land product validation for the MOD13 data products are available from the MODIS Land Team Validation site (https://modis-land.gsfc.nasa.gov/ValStatus.php?ProductID=MOD13).Improvements/Changes from Previous Versions* 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.* A polarization correction has been applied to the L1B Reflective Solar Bands (RSB).", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "monthly", "temporalExtentEnd": "", "shortName": "MYD13C2", "landingPageUrl": "https://doi.org/10.5067/MODIS/MYD13C2.061", "doi": "10.5067/MODIS/MYD13C2.061", "longName": "MODIS/Aqua Vegetation Indices Monthly L3 Global 0.05Deg CMG V061" }
node
75
[ "Dataset" ]
{ "temporalExtentStart": "2000-02-16T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2540271835-LPCLOUD", "globalId": "92e7a001-f4ad-56d5-abf8-54a5e458f6f7", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "The MCD43D48 Version 6.1 Bidirectional Reflectance Distribution Function and Albedo (BRDF/Albedo) Black-Sky Albedo dataset is produced daily using 16 days of Terra and Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) data at 30 arc second (1,000 meter (m)) resolution. Data are temporally weighted to the ninth day which is reflected in the Julian date in the file name. This Climate Modeling Grid (CMG) product covers the entire globe for use in climate simulation models. Due to the large file size, each MCD43D product contains just one data layer. \r\rMCD43D42 through MCD43D61 are the albedo products of the MCD43D BRDF/Albedo product suite. There are 10 black-sky albedo and 10 white-sky albedo layers representing MODIS bands 1 through 7 and the visible, near infrared (NIR), and shortwave bands. 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. \r\rMCD43D48 is the black-sky albedo for MODIS band 7.\r\rImprovements/Changes from Previous Versions\r\r* 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.\r* A polarization correction has been applied to the L1B Reflective Solar Bands (RSB).", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "MCD43D48", "landingPageUrl": "https://doi.org/10.5067/MODIS/MCD43D48.061", "doi": "10.5067/MODIS/MCD43D48.061", "longName": "MODIS/Terra+Aqua BRDF/Albedo Black Sky Albedo Band7 Daily L3 Global 30ArcSec CMG V061" }
node
76
[ "Dataset" ]
{ "temporalExtentStart": "2012-01-19T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C1607315592-LPDAAC_ECS", "globalId": "77a18180-47b6-5cc9-a24d-5d64431c5557", "pagerank_publication_dataset": 0.15000000000000002, "abstract": "The NASA/NOAA Suomi National Polar-orbiting Partnership (Suomi NPP) Visible Infrared Imaging Radiometer Suite (VIIRS) Bidirectional Reflectance Distribution Function (BRDF) and Albedo Model Parameter 2 Band M3 product (VNP43D08) 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 VNP43D 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 VNP43D 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 VNP43MA1 (https://doi.org/10.5067/VIIRS/VNP43MA1.001) product is stored in a separate file as VNP43D01 through VNP43D36. In addition to the bands included in VNP43MA1, this product suite includes model parameters for the VIIRS Day/Night Band (DNB) as VNP43D37 through VNP43D39. Details regarding methodology are available on the VNP43MA1 product page and in the Algorithm Theoretical Basis Document [ATBD).\r\rVNP43D08 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.", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "", "shortName": "VNP43D08", "landingPageUrl": "https://doi.org/10.5067/VIIRS/VNP43D08.001", "doi": "10.5067/VIIRS/VNP43D08.001", "longName": "VIIRS/NPP BRDF/Albedo Parameter 2 Band M3 Daily L3 Global 30 ArcSec CMG V001" }
node
77
[ "Dataset" ]
{ "temporalExtentStart": "1981-01-01T00:00:00.000Z", "seCorner": { "crs": "wgs-84", "latitude": -90, "longitude": 180, "height": null }, "cmrId": "C2763268446-LPCLOUD", "globalId": "8ea7e8d7-fa0d-537c-97b4-c5a3e401bc99", "pagerank_publication_dataset": 0.19250000000000003, "abstract": "The NASA Making Earth System Data Records for Use in Research Environments (MEaSUREs) (https://earthdata.nasa.gov/about/competitive-programs/measures) Vegetation Index and Phenology (VIP) global datasets were created using Advanced Very High Resolution Radiometer (AVHRR) N07, N09, N11, and N14 datasets (1981 - 1999) and Moderate Resolution Imaging Spectroradiometer (MODIS)/Terra MOD09 surface reflectance data (2000 - 2014). The VIP Vegetation Index (VI) product was developed to provide consistent measurements of the Normalized Difference Vegetation Index (NDVI) and modified Enhanced Vegetation Index (EVI2) spanning more than 30 years of data from multiple sensors. The EVI2 is a backward extension of AVHRR. Vegetation indices such as NDVI and EVI2 are useful for assessing the biophysical properties of the land surface, and are used to characterize vegetation phenology. Phenology tracks the seasonal life cycle of vegetation, and provides information on the biotic response to environmental changes. The VIP01 VI data product is a daily global file at 0.05 degree (5600 meter (m)) spatial resolution in geographic (Lat/Lon) grid format. The data are stored in Hierarchical Data Format-Earth Observing System (HDF-EOS) file format. The VIP01 VI product contains 11 Science Datasets (SDS), which includes the calculated VIs (NDVI and EVI2) as well as information on the quality assurance/pixel reliability, the input Visible/Near Infrared (VNIR) surface reflectance data, and viewing geometry. The Blue and Middle Infrared (MIR) surface reflectance data are only available for the MODIS era (2000 - 2014). Gaps in the daily product are filled using long term mean VI records derived from the more than 30 year time series of data, and are indicated as gap-filled in the Pixel Reliability SDS. A low resolution browse image showing NDVI as a color map is also available.", "daac": "LP DAAC", "nwCorner": { "crs": "wgs-84", "latitude": 90, "longitude": -180, "height": null }, "temporalFrequency": "daily", "temporalExtentEnd": "2014-12-31T23:59:59.999Z", "shortName": "VIP01", "landingPageUrl": "https://doi.org/10.5067/MEaSUREs/VIP/VIP01.004", "doi": "10.5067/MEASURES/VIP/VIP01.004", "longName": "Vegetation Index and Phenology (VIP) Vegetation Indices Daily Global 0.05Deg CMG V004" }
End of preview.

NASA Knowledge Graph Dataset

Dataset Summary

The NASA Knowledge Graph Dataset is an expansive graph-based dataset designed to integrate and interconnect information about satellite datasets, scientific publications, instruments, platforms, projects, data centers, and science keywords. This knowledge graph is particularly focused on datasets managed by NASA's Distributed Active Archive Centers (DAACs), which are NASA's data repositories responsible for archiving and distributing scientific data. In addition to NASA DAACs, the graph includes datasets from 184 data providers worldwide, including various government agencies and academic institutions.

The primary goal of the NASA Knowledge Graph is to bridge scientific publications with the datasets they reference, facilitating deeper insights and research opportunities within NASA's scientific and data ecosystem. By organizing these interconnections within a graph structure, this dataset enables advanced analyses, such as discovering influential datasets, understanding research trends, and exploring scientific collaborations.


What's Changed (v1.1.0) - Feb 25th, 2025

1. Node Changes

  • Total Nodes: Increased from 135,764 to 145,678 (+9,914)
  • New Node Counts:
    • Dataset: Increased from 6,390 to 6,821 (+431)
    • DataCenter: Increased from 184 to 197 (+13)
    • Instrument: Increased from 867 to 897 (+30)
    • Platform: Increased from 442 to 451 (+9)
    • Project: Increased from 333 to 351 (+18)
    • Publication: Increased from 125,939 to 135,352 (+9,413)
    • ScienceKeyword: Remained the same at 1,609

2. Relationship Changes

  • Total Relationships: Increased from 365,857 to 406,515 (+40,658)
  • Updated Relationship Counts:
    • CITES: Decreased from 208,670 to 208,429 (-241)
    • HAS_APPLIED_RESEARCH_AREA: Increased from 89,039 to 119,695 (+30,656)
    • HAS_DATASET: Increased from 9,017 to 9,834 (+817)
    • HAS_INSTRUMENT: Increased from 2,469 to 2,526 (+57)
    • HAS_PLATFORM: Increased from 9,884 to 10,398 (+514)
    • HAS_SCIENCEKEYWORD: Increased from 20,436 to 21,571 (+1,135)
    • HAS_SUBCATEGORY: Remained the same at 1,823
    • OF_PROJECT: Increased from 6,049 to 6,378 (+329)
    • USES_DATASET: Increased from 18,470 to 25,861 (+7,391)

3. Property Changes

  • Removed Properties:
    • pagerank_global
    • fastrp_embedding_with_labels
  • Added Properties:
    • pagerank_publication_dataset (Float) for Dataset and Publication nodes

These changes reflect the addition of new datasets, publications, and relationships, alongside the streamlined properties to improve data efficiency and analysis potential.


Data Integrity

Each file in the dataset has a SHA-256 checksum to verify its integrity:

File Name SHA-256 Checksum
graph.cypher 99710792de412ce1977f1172d0458de1b0ea3d387e33adcd32adbec63c2238c1
graph.graphml 00f2848602104c073a97ca65ff7d3e10c5bdddcc1fe5ede69cb21d4bfbbe8a89
graph.json bb415c8579c31b2ec80cc83dedc5660ead6be2f5f2fcd3c162433ec73d6f5280

Verification

To verify the integrity of each file, calculate its SHA-256 checksum and compare it with the hashes provided above.

You can use the following Python code to calculate the SHA-256 checksum:

import hashlib

def calculate_sha256(filepath):
    sha256_hash = hashlib.sha256()
    with open(filepath, "rb") as f:
        for byte_block in iter(lambda: f.read(4096), b""):
            sha256_hash.update(byte_block)
    return sha256_hash.hexdigest()

Dataset Structure

Nodes and Properties

The knowledge graph consists of seven main node types, each representing a different entity within NASA's ecosystem:

Dataset Structure

Nodes and Properties

1. Dataset

  • Description: Represents satellite datasets, particularly those managed by NASA DAACs, along with datasets from other governmental and academic data providers. These nodes contain metadata and attributes specific to each dataset.
  • Properties:
    • globalId (String): Unique identifier for the dataset.
    • doi (String): Digital Object Identifier.
    • shortName (String): Abbreviated name of the dataset.
    • longName (String): Full name of the dataset.
    • abstract (String): Brief summary of the dataset.
    • cmrId (String): Common Metadata Repository ID.
    • daac (String): Distributed Active Archive Center associated with the dataset.
    • temporalFrequency (String): Frequency of data collection (e.g., daily, monthly).
    • temporalExtentStart (Date): Start date of the dataset's temporal coverage.
    • temporalExtentEnd (Date): End date of the dataset's temporal coverage.
    • nwCorner (Geo-Coordinate): Northwest corner coordinate of spatial coverage.
    • seCorner (Geo-Coordinate): Southeast corner coordinate of spatial coverage.
    • landingPageUrl (URL): Webpage link to the dataset.
    • pagerank_publication_dataset (Float): PageRank score based on dataset-publication influence.

2. Publication

  • Description: This node type captures publications that reference or use datasets, particularly those from NASA DAACs and other included data providers. By linking datasets and publications, this node type enables analysis of scientific impact and research usage of NASA’s datasets.
  • Properties:
    • globalId (String): Unique identifier for the publication.
    • DOI (String): Digital Object Identifier.
    • title (String): Title of the publication.
    • abstract (String): Summary of the publication's content.
    • authors (List): List of authors.
    • year (Integer): Year of publication.
    • pagerank_publication_dataset (Float): PageRank score based on publication-dataset influence.

3. ScienceKeyword

  • Description: Represents scientific keywords used to classify datasets and publications. Keywords provide topical context and aid in identifying research trends and related areas.
  • Properties:
    • globalId (String): Unique identifier.
    • name (String): Name of the science keyword.

4. Instrument

  • Description: Instruments used in data collection, often mounted on platforms like satellites. Instruments are linked to the datasets they help generate.
  • Properties:
    • globalId (String): Unique identifier.
    • shortName (String): Abbreviated name.
    • longName (String): Full name.

5. Platform

  • Description: Platforms, such as satellites or airborne vehicles, that host instruments for data collection.
  • Properties:
    • globalId (String): Unique identifier.
    • shortName (String): Abbreviated name.
    • longName (String): Full name.
    • Type (String): Type of platform.

6. Project

  • Description: NASA projects associated with datasets, often indicating a funding source or collaborative initiative for data collection and research.
  • Properties:
    • globalId (String): Unique identifier.
    • shortName (String): Abbreviated name.
    • longName (String): Full name.

7. DataCenter

  • Description: Represents data centers, primarily NASA DAACs, as well as other data providers in academia and government who manage and distribute datasets.
  • Properties:
    • globalId (String): Unique identifier.
    • shortName (String): Abbreviated name.
    • longName (String): Full name.
    • url (URL): Website of the data center.

Relationships

The knowledge graph includes several relationship types that define how nodes are interconnected.

1. HAS_DATASET

  • Description: Connects a DataCenter to its Dataset(s).
  • Properties: None.

2. OF_PROJECT

  • Description: Links a Dataset to a Project.
  • Properties: None.

3. HAS_PLATFORM

  • Description: Associates a Dataset with a Platform.
  • Properties: None.

4. HAS_INSTRUMENT

  • Description: Connects a Platform to an Instrument.
  • Properties: None.

5. HAS_SCIENCEKEYWORD

  • Description: Links a Dataset to a ScienceKeyword.
  • Properties: None.

6. HAS_SUBCATEGORY

  • Description: Defines hierarchical relationships between ScienceKeyword nodes.
  • Properties: None.

7. CITES

  • Description: Represents citation relationships between Publication nodes, indicating how research builds on previous work.
  • Properties: None.

8. HAS_APPLIED_RESEARCH_AREA

  • Description: Associates a Publication with a ScienceKeyword.
  • Properties: None.

Statistics

Data Statistics

Total Counts

Type Count
Total Nodes 145,678
Total Relationships 406,515

Node Label Counts

Node Label Count
Dataset 6,821
DataCenter 197
Project 351
Platform 451
Instrument 897
ScienceKeyword 1,609
Publication 135,352

Relationship Label Counts

Relationship Label Count
CITES 208,429
HAS_APPLIEDRESEARCHAREA 119,695
HAS_DATASET 9,834
HAS_INSTRUMENT 2,526
HAS_PLATFORM 10,398
HAS_SCIENCEKEYWORD 21,571
HAS_SUBCATEGORY 1,823
OF_PROJECT 6,378
USES_DATASET 25,861

Data Formats

The Knowledge Graph Dataset is available in three formats:

1. JSON

  • File: graph.json
  • Description: A hierarchical data format representing nodes and relationships. Each node includes its properties, such as globalId, doi, and pagerank_global.
  • Usage: Suitable for web applications and APIs, and for use cases where hierarchical data structures are preferred.

Loading the JSON Format

To load the JSON file into a graph database using Python and multiprocessing you can using the following script:

import json
from tqdm import tqdm
from collections import defaultdict
from multiprocessing import Pool, cpu_count
from neo4j import GraphDatabase

# Batch size for processing
BATCH_SIZE = 100

# Neo4j credentials (replace with environment variables or placeholders)
NEO4J_URI = "bolt://<your-neo4j-host>:<port>"  # e.g., "bolt://localhost:7687"
NEO4J_USER = "<your-username>"
NEO4J_PASSWORD = "<your-password>"


def ingest_data(file_path):
    # Initialize counters and label trackers
    node_label_counts = defaultdict(int)
    relationship_label_counts = defaultdict(int)
    node_count = 0
    relationship_count = 0

    with open(file_path, "r") as f:
        nodes = []
        relationships = []

        # Read and categorize nodes and relationships, and count labels
        for line in tqdm(f, desc="Reading JSON Lines"):
            obj = json.loads(line.strip())
            if obj["type"] == "node":
                nodes.append(obj)
                node_count += 1
                for label in obj["labels"]:
                    node_label_counts[label] += 1
            elif obj["type"] == "relationship":
                relationships.append(obj)
                relationship_count += 1
                relationship_label_counts[obj["label"]] += 1

    # Print statistics
    print("\n=== Data Statistics ===")
    print(f"Total Nodes: {node_count}")
    print(f"Total Relationships: {relationship_count}")
    print("\nNode Label Counts:")
    for label, count in node_label_counts.items():
        print(f"  {label}: {count}")
    print("\nRelationship Label Counts:")
    for label, count in relationship_label_counts.items():
        print(f"  {label}: {count}")
    print("=======================")

    # Multiprocess node ingestion
    print("Starting Node Ingestion...")
    node_batches = [nodes[i : i + BATCH_SIZE] for i in range(0, len(nodes), BATCH_SIZE)]
    with Pool(processes=cpu_count()) as pool:
        list(
            tqdm(
                pool.imap(ingest_nodes_batch, node_batches),
                total=len(node_batches),
                desc="Ingesting Nodes",
            )
        )

    # Multiprocess relationship ingestion
    print("Starting Relationship Ingestion...")
    relationship_batches = [
        relationships[i : i + BATCH_SIZE]
        for i in range(0, len(relationships), BATCH_SIZE)
    ]
    with Pool(processes=cpu_count()) as pool:
        list(
            tqdm(
                pool.imap(ingest_relationships_batch, relationship_batches),
                total=len(relationship_batches),
                desc="Ingesting Relationships",
            )
        )


def ingest_nodes_batch(batch):
    with GraphDatabase.driver(NEO4J_URI, auth=(NEO4J_USER, NEO4J_PASSWORD)) as driver:
        with driver.session() as session:
            for node in batch:
                try:
                    label = node["labels"][0]  # Assumes a single label per node
                    query = f"""
                    MERGE (n:{label} {{globalId: $globalId}})
                    SET n += $properties
                    """
                    session.run(
                        query,
                        globalId=node["properties"]["globalId"],
                        properties=node["properties"],
                    )
                except Exception as e:
                    print(
                        f"Error ingesting node with globalId {node['properties']['globalId']}: {e}"
                    )


def ingest_relationships_batch(batch):
    with GraphDatabase.driver(NEO4J_URI, auth=(NEO4J_USER, NEO4J_PASSWORD)) as driver:
        with driver.session() as session:
            for relationship in batch:
                try:
                    rel_type = relationship[
                        "label"
                    ]  # Use the label for the relationship
                    query = f"""
                    MATCH (start {{globalId: $start_globalId}})
                    MATCH (end {{globalId: $end_globalId}})
                    MERGE (start)-[r:{rel_type}]->(end)
                    """
                    session.run(
                        query,
                        start_globalId=relationship["start"]["properties"]["globalId"],
                        end_globalId=relationship["end"]["properties"]["globalId"],
                    )
                except Exception as e:
                    print(
                        f"Error ingesting relationship with label {relationship['label']}: {e}"
                    )


if __name__ == "__main__":
    # Path to the JSON file
    JSON_FILE_PATH = "<path-to-your-graph.json>"

    # Run the ingestion process
    ingest_data(JSON_FILE_PATH)

2. GraphML

  • File: graph.graphml
  • Description: An XML-based format well-suited for complex graph structures and metadata-rich representations.
  • Usage: Compatible with graph visualization and analysis tools, including Gephi, Cytoscape, and databases that support GraphML import.

Loading the GraphML Format

To import the GraphML file into a graph database with APOC support, use the following command:

CALL apoc.import.graphml("path/to/graph.graphml", {readLabels: true})

3. Cypher

  • File: graph.cypher
  • Description: A series of Cypher commands to recreate the knowledge graph structure.
  • Usage: Useful for recreating the graph in any Cypher-compatible graph database.

Loading the Cypher Format

To load the Cypher script, execute it directly using a command-line interface for your graph database:

neo4j-shell -file path/to/graph.cypher

4. Loading the Knowledge Graph into PyTorch Geometric (PyG)

This knowledge graph can be loaded into PyG (PyTorch Geometric) for further processing, analysis, or model training. Below is an example script that shows how to load the JSON data into a PyG-compatible HeteroData object.

The script first reads the JSON data, processes nodes and relationships, and then loads everything into a HeteroData object for use with PyG.

import json
import torch
from torch_geometric.data import HeteroData
from collections import defaultdict

# Load JSON data from file
file_path = "path/to/graph.json"  # Replace with your actual file path
graph_data = []
with open(file_path, "r") as f:
    for line in f:
        try:
            graph_data.append(json.loads(line))
        except json.JSONDecodeError as e:
            print(f"Error decoding JSON line: {e}")
            continue

# Initialize HeteroData object
data = HeteroData()

# Mapping for node indices per node type
node_mappings = defaultdict(dict)

# Temporary storage for properties to reduce concatenation cost
node_properties = defaultdict(lambda: defaultdict(list))
edge_indices = defaultdict(lambda: defaultdict(list))

# Process each item in the loaded JSON data
for item in graph_data:
    if item['type'] == 'node':
        node_type = item['labels'][0]  # Assuming first label is the node type
        node_id = item['id']
        properties = item['properties']

        # Store the node index mapping
        node_index = len(node_mappings[node_type])
        node_mappings[node_type][node_id] = node_index

        # Store properties temporarily by type
        for key, value in properties.items():
            if isinstance(value, list) and all(isinstance(v, (int, float)) for v in value):
                node_properties[node_type][key].append(torch.tensor(value, dtype=torch.float))
            elif isinstance(value, (int, float)):
                node_properties[node_type][key].append(torch.tensor([value], dtype=torch.float))
            else:
                node_properties[node_type][key].append(value)  # non-numeric properties as lists

    elif item['type'] == 'relationship':
        start_type = item['start']['labels'][0]
        end_type = item['end']['labels'][0]
        start_id = item['start']['id']
        end_id = item['end']['id']
        edge_type = item['label']

        # Map start and end node indices
        start_idx = node_mappings[start_type][start_id]
        end_idx = node_mappings[end_type][end_id]

        # Append to edge list
        edge_indices[(start_type, edge_type, end_type)]['start'].append(start_idx)
        edge_indices[(start_type, edge_type, end_type)]['end'].append(end_idx)

# Finalize node properties by batch processing
for node_type, properties in node_properties.items():
    data[node_type].num_nodes = len(node_mappings[node_type])
    for key, values in properties.items():
        if isinstance(values[0], torch.Tensor):
            data[node_type][key] = torch.stack(values)
        else:
            data[node_type][key] = values  # Keep non-tensor properties as lists

# Finalize edge indices in bulk
for (start_type, edge_type, end_type), indices in edge_indices.items():
    edge_index = torch.tensor([indices['start'], indices['end']], dtype=torch.long)
    data[start_type, edge_type, end_type].edge_index = edge_index

# Display statistics for verification
print("Nodes and Properties:")
for node_type in data.node_types:
    print(f"\nNode Type: {node_type}")
    print(f"Number of Nodes: {data[node_type].num_nodes}")
    for key, value in data[node_type].items():
        if key != 'num_nodes':
            if isinstance(value, torch.Tensor):
                print(f"  - {key}: {value.shape}")
            else:
                print(f"  - {key}: {len(value)} items (non-numeric)")

print("\nEdges and Types:")
for edge_type in data.edge_types:
    edge_index = data[edge_type].edge_index
    print(f"Edge Type: {edge_type} - Number of Edges: {edge_index.size(1)} - Shape: {edge_index.shape}")

Citation

Please cite the dataset as follows:

NASA Goddard Earth Sciences Data and Information Services Center (GES-DISC). (2024). Knowledge Graph of NASA Earth Observations Satellite Datasets and Related Research Publications [Data set]. DOI: 10.57967/hf/3463

BibTeX

@misc {nasa_goddard_earth_sciences_data_and_information_services_center__(ges-disc)_2024,
    author       = { {NASA Goddard Earth Sciences Data and Information Services Center (GES-DISC)} },
    title        = { nasa-eo-knowledge-graph },
    year         = 2024,
    url          = { https://huggingface.co/datasets/nasa-gesdisc/nasa-eo-knowledge-graph },
    doi          = { 10.57967/hf/3463 },
    publisher    = { Hugging Face }
}

References

For details on the process of collecting these publications, please refer to:

Gerasimov, I., Savtchenko, A., Alfred, J., Acker, J., Wei, J., & KC, B. (2024). Bridging the Gap: Enhancing Prominence and Provenance of NASA Datasets in Research Publications. Data Science Journal, 23(1). DOI: 10.5334/dsj-2024-001

For any questions or further information, please contact:

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