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‎config/default/common/colormaps/orbits/OrbitTracks_EarthCARE_Ascending.xml

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<?xml version="1.0" encoding="utf-8"?>
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<ColorMaps xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance"
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xsi:noNamespaceSchemaLocation="http://gibs.earthdata.nasa.gov/schemas/ColorMap_v1.3.xsd">
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<ColorMap title="EarthCARE Orbital Track">
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<Entries>
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<ColorMapEntry rgb="3,42,17" sourceValue="200" transparent="false" ref="1" />
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</Entries>
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<Legend type="classification">
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<LegendEntry rgb="3,42,17" id="1" tooltip="Acquisition Time (UTC)" label="Acquisition Time (UTC)" showLabel="true" />
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</Legend>
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</ColorMap>
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</ColorMaps>

‎config/default/common/colormaps/orbits/OrbitTracks_EarthCARE_Descending.xml

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<?xml version="1.0" encoding="utf-8"?>
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<ColorMaps xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance"
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xsi:noNamespaceSchemaLocation="http://gibs.earthdata.nasa.gov/schemas/ColorMap_v1.3.xsd">
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<ColorMap title="EarthCARE Orbital Track">
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<Entries>
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<ColorMapEntry rgb="3,42,17" sourceValue="200" transparent="false" ref="1" />
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</Entries>
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<Legend type="classification">
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<LegendEntry rgb="3,42,17" id="1" tooltip="Acquisition Time (UTC)" label="Acquisition Time (UTC)" showLabel="true" />
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</Legend>
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</ColorMap>
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</ColorMaps>

‎config/default/common/config/metadata/layers/daymet/Daymet_Maximum_Air_Temp_Daily.md

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Daymet is a computer program that uses observations from ground weather stations to estimate weather conditions at locations that are not instrumented. Output from the Daymet model includes Daily Maximum Air Temperature: a gridded data set of daily maximum temperature (℃) for every 1-km x 1-km pixel within the mapped spatial extent; currently North America, Hawaii, Puerto Rico and Bermuda. Within the Daymet algorithm, each pixel in the continuous gridded coverage is estimated by interpolating from a sample of surrounding ground weather stations that record local 24-hr daily weather values, including daily maximum temperature. A digital elevation model (DEM) is also used in the temperature estimation to take into account temperature variation in elevation. There are between 9,000 to 10,000 weather stations, depending on the year, in North America that are archived by the National Oceanic and Atmospheric Administration (NOAA) that record daily temperature variables.
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Daymet is a computer program that uses observations from ground weather stations to estimate weather conditions at locations that are not instrumented. Output from the Daymet model includes Daily Maximum Air Temperature: a gridded data set of daily maximum temperature (℃) for every 1-km x 1-km pixel within the mapped spatial extent; currently North America, Hawaii, Puerto Rico and Bermuda. Within the Daymet algorithm, each pixel in the continuous gridded coverage is estimated by interpolating from a sample of surrounding ground weather stations that record local 24-hr daily weather values, including daily maximum temperature. A digital elevation model (DEM) is also used in the temperature estimation to take into account temperature variation in elevation. There are between 9,000 to 10,000 weather stations, depending on the year, in North America that are archived by the National Oceanic and Atmospheric Administration (NOAA) that record daily temperature variables.
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[Daymet](https://daymet.ornl.gov/) data products are used within a variety of studies that require daily continuous temperature data including, but not limited to, crop modelling, forest production, vector borne illnesses, and climate change adaptation.
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‎config/default/common/config/metadata/layers/daymet/Daymet_Minimum_Air_Temp_Daily.md

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Daymet is a computer program that uses observations from ground weather stations to estimate weather conditions at locations that are not instrumented. Output from the Daymet model includes Daily Minimum Air Temperature: a gridded data set of daily minimum temperature (℃) for every 1-km x 1-km pixel within the mapped spatial extent; currently North America, Hawaii, Puerto Rico and Bermuda. Within the Daymet algorithm, each pixel in the continuous gridded coverage is estimated by interpolating from a sample of surrounding ground weather stations that record local 24-hr daily weather values, including minimum temperature. A digital elevation model (DEM) is also used in the temperature estimation to take into account temperature variation with elevation. There are between 9,000 to 10,000 weather stations, depending on the year, in North America that are archived by the National Oceanic and Atmospheric Administration (NOAA) that record daily temperature variables.
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Daymet is a computer program that uses observations from ground weather stations to estimate weather conditions at locations that are not instrumented. Output from the Daymet model includes Daily Minimum Air Temperature: a gridded data set of daily minimum temperature (℃) for every 1-km x 1-km pixel within the mapped spatial extent; currently North America, Hawaii, Puerto Rico and Bermuda. Within the Daymet algorithm, each pixel in the continuous gridded coverage is estimated by interpolating from a sample of surrounding ground weather stations that record local 24-hr daily weather values, including minimum temperature. A digital elevation model (DEM) is also used in the temperature estimation to take into account temperature variation with elevation. There are between 9,000 to 10,000 weather stations, depending on the year, in North America that are archived by the National Oceanic and Atmospheric Administration (NOAA) that record daily temperature variables.
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[Daymet](https://daymet.ornl.gov/) data products are used within a variety of studies that require daily continuous temperature data including, but not limited to, crop modelling, forest production, vector borne illnesses, and climate change adaptation.
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‎config/default/common/config/metadata/layers/goes/GOES-West_ABI_Band2_Red_Visible_1km.md

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The Red Visible (0.64 um, Band 2) layer from the GOES-West Advanced Baseline Imager (ABI) is used primarily to monitor the evolution of clouds throughout the daylight hours. It is also useful for identifying small-scale features such as river fog/clear air boundaries, or overshooting tops of cumulus clouds. It can also be used to identify daytime snow and ice cover, diagnose low-level cloud-drift winds, assist with detections of volcanic ash and analysis of hurricanes and winter storms.
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The Geostationary Operational Environmental Satellites (GOES)-West satellite (currently, GOES-18) is centered on 137.2 degrees W, covering most of the Pacific Ocean, the USA, most of Canada, Central America, the western half of South America, and parts of Australasia. The GOES-West ABI imagery is available on a rolling 90-day basis at 10 minute intervals. The sensor resolution of Band 2 is 0.5 km, the imagery resolution in Worldview/Global Imagery Browse Services (GIBS) is 1 km, the temporal resolution is 10 minutes, and the latency (time from satellite acquisition to availability in GIBS) is approximately 40 minutes.
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The Geostationary Operational Environmental Satellites (GOES)-West satellite (currently, GOES-18) is centered on 137.2 degrees W, covering most of the Pacific Ocean, the USA, most of Canada, Central America, the western half of South America, and parts of Australasia. The GOES-West ABI imagery is available on a rolling 90-day basis at 10 minute intervals. The sensor resolution of Band 2 is 0.5 km, the imagery resolution in Worldview/Global Imagery Browse Services (GIBS) is 1 km, the temporal resolution is 10 minutes, and the latency (time from satellite acquisition to availability in GIBS) is approximately 40 minutes.
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References: [GOES-R: ABI Band 2 (0.64 um) Quick Guide](https://www.star.nesdis.noaa.gov/GOES/documents/ABIQuickGuide_Band02.pdf)

‎config/default/common/config/metadata/layers/goes/GOES-West_ABI_GeoColor.md

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Note: This layer is generally available for the **most recent 90 days**, though certain historical ranges are also preserved.
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The GeoColor (True Color (Day), Multispectral blended infrared (IR; at Night)) layer from the GOES-West Advanced Baseline Imager (ABI) provides an approximation to daytime True Color imagery. The combination of spectral bands yields an appearance similar to what the human eye would perceive for land surface, oceanic and atmospheric features, with atmospheric correction used to make the appearance of these features sharper. Thus it is used primarily for the intuitive interpretation of meteorological and surface-based features such as smoke, blowing dust, and vegetation types (forests, deserts, croplands, etc.). At night, the true color imagery gives way to IR-based blended multispectral imagery that provides differentiation between low liquid water clouds (shown in light blue) and higher ice clouds (shown in gray/white). It also includes a static city lights/night lights database derived from the VIIRS Day/Night Band, which aids in geo-referencing and can help determine the proximity of clouds (such as fog) or weather hazards (such as thunderstorms or tropical cyclones) to population centers. Please note that as these lights are static, they will not change even if, for example, a weather-induced power outage occurs.
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The GeoColor (True Color (Day), Multispectral blended infrared (IR; at Night)) layer from the GOES-West Advanced Baseline Imager (ABI) provides an approximation to daytime True Color imagery. The combination of spectral bands yields an appearance similar to what the human eye would perceive for land surface, oceanic and atmospheric features, with atmospheric correction used to make the appearance of these features sharper. Thus it is used primarily for the intuitive interpretation of meteorological and surface-based features such as smoke, blowing dust, and vegetation types (forests, deserts, croplands, etc.). At night, the true color imagery gives way to IR-based blended multispectral imagery that provides differentiation between low liquid water clouds (shown in light blue) and higher ice clouds (shown in gray/white). It also includes a static city lights/night lights database derived from the VIIRS Day/Night Band, which aids in geo-referencing and can help determine the proximity of clouds (such as fog) or weather hazards (such as thunderstorms or tropical cyclones) to population centers. Please note that as these lights are static, they will not change even if, for example, a weather-induced power outage occurs.
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The Geostationary Operational Environmental Satellites (GOES)-West satellite (currently, GOES-18) is centered on 137.2 degrees W, covering most of the Pacific Ocean, the USA, most of Canada, Central America, the western half of South America, and parts of Australasia. The GOES-West ABI imagery is available on a rolling 90-day basis at 10 minute intervals. The product resolution is 1 km, the imagery resolution in Worldview/Global Imagery Browse Services (GIBS) is 1 km, the temporal resolution is 10 minutes, and the latency (time from satellite acquisition to availability in GIBS) is approximately 40 minutes.
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‎config/default/common/config/metadata/layers/himawari/Himawari_AHI_Band13_Clean_Infrared.md

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Note: This layer is generally available for the **most recent 90 days**, though certain historical ranges are also preserved.
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The Clean Infrared (10.3 um, Band 13) layer from the Himawari-9 Advanced Himawari Imager (AHI) is useful for detecting clouds all times of day and night and is quite useful in retrievals of cloud top height. It is used to identify and classify cloud and other atmospheric features, estimate cloud-top brightness temperature and cloud particle size, convective severe weather signatures, and hurricane intensity. This infrared window is not strongly affected by atmospheric water vapor.
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The Clean Infrared (10.3 um, Band 13) layer from the Himawari-9 Advanced Himawari Imager (AHI) is useful for detecting clouds all times of day and night and is quite useful in retrievals of cloud top height. It is used to identify and classify cloud and other atmospheric features, estimate cloud-top brightness temperature and cloud particle size, convective severe weather signatures, and hurricane intensity. This infrared window is not strongly affected by atmospheric water vapor.
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The Himawari-9 satellite is centered on 140.7 degrees E, covering most of the Pacific Ocean, a portion of Eastern Asia, and parts of Australasia. The Himawari-9 AHI imagery is available on a rolling 90-day basis at 10 minute intervals. The sensor resolution is 2 km, the imagery resolution in Worldview/Global Imagery Browse Services (GIBS) is 2 km, the temporal resolution is 10 minutes, and the latency (time from satellite acquisition to availability in GIBS) is approximately 40 minutes.
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‎config/default/common/config/metadata/layers/ldas/NLDAS_Underground_Soil_Moisture_Noah_Monthly.md

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This NLDAS Soil Moisture is one of the model assimilated fields from the North America Land Data Assimilation System Phase 2 (NLDAS-2) Noah Land Surface Model (LSM). The NLDAS Soil Moisture monthly data are generated through temporal averaging of the hourly data. This NLDAS-2 Noah Soil Moisture parameter represents the 0 - 100 cm depth-averaged amount of water in unit “kg/m<sup>2</sup>” which is equivalent to “mm”.
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This NLDAS Soil Moisture is one of the model assimilated fields from the North America Land Data Assimilation System Phase 2 (NLDAS-2) Noah Land Surface Model (LSM). The NLDAS Soil Moisture monthly data are generated through temporal averaging of the hourly data. This NLDAS-2 Noah Soil Moisture parameter represents the 0 - 100 cm depth-averaged amount of water in unit “kg/m<sup>2</sup>” which is equivalent to “mm”.
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Soil Moisture is a science variable that controls the exchange of water and heat energy between the land surface and the atmosphere through evaporation and plant transpiration. As a result, soil moisture plays an important role in the development of weather patterns and the production of precipitation. The NLDAS Soil Moisture data can be used for supporting research and applications related to global water and energy cycle, drought and flood, and climatology, land surface assimilation, etc.
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‎config/default/common/config/metadata/layers/modis/aqua/MODIS_Aqua_L2_Chlorophyll_A.md

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The MODIS Chlorophyll *a* product is available from both the Terra and Aqua satellites. The sensor and imagery resolution is 1 km, and the temporal resolution is daily.
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References: MODISA_L2_OC_NRT [https://oceancolor.gsfc.nasa.gov/data/10.5067/AQUA/MODIS/L2/OC/2022]; MODISA_L2_OC [doi:10.5067/AQUA/MODIS/L2/OC/2022](https://doi.org/10.5067/AQUA/MODIS/L2/OC/2022)
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References: [MODISA_L2_OC_NRT](https://oceancolor.gsfc.nasa.gov/data/10.5067/AQUA/MODIS/L2/OC/2022); MODISA_L2_OC [doi:10.5067/AQUA/MODIS/L2/OC/2022](https://doi.org/10.5067/AQUA/MODIS/L2/OC/2022)

‎config/default/common/config/metadata/layers/modis/aqua/MODIS_Aqua_L2_Photosynthetically_Available_Radiation.md

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The Photosynthetically Available Radiation (L2) layer displays photosynthetically available radiation over oceans and large bodies of water and is measured in einstein/m²/day.
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References: MODISA_L2_OC_NRT [https://oceancolor.gsfc.nasa.gov/data/10.5067/AQUA/MODIS/L2/OC/2022]; MODISA_L2_OC [doi:10.5067/AQUA/MODIS/L2/OC/2022](https://doi.org/10.5067/AQUA/MODIS/L2/OC/2022)
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References: [MODISA_L2_OC_NRT](https://oceancolor.gsfc.nasa.gov/data/10.5067/AQUA/MODIS/L2/OC/2022); MODISA_L2_OC [doi:10.5067/AQUA/MODIS/L2/OC/2022](https://doi.org/10.5067/AQUA/MODIS/L2/OC/2022)

‎config/default/common/config/metadata/layers/modis/combined/MODIS_Combined_Thermal_Anomalies_All.md

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The MODIS Fire and Thermal Anomalies product is available from the Terra (MOD14) and Aqua (MYD14) satellites as well as a combined Terra and Aqua (MCD14) satellite product. The sensor resolution is 1 km, and the temporal resolution is daily. The thermal anomalies are represented as points (approximate center of a 1 km pixel) in Worldview/GIBS.
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References: References: MOD14.NRT [doi:10.5067/MODIS/MOD14.NRT.061](https://doi.org/10.5067/MODIS/MOD14.NRT.061); MOD14 [doi:10.5067/MODIS/MOD14.061](https://doi.org/10.5067/MODIS/MOD14.061); MYD14.NRT [doi:10.5067/MODIS/MYD14.NRT.061](https://doi.org/10.5067/MODIS/MYD14.NRT.061); MYD14 [doi:10.5067/MODIS/MYD14.061](https://doi.org/10.5067/MODIS/MYD14.061)
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References: MOD14.NRT [doi:10.5067/MODIS/MOD14.NRT.061](https://doi.org/10.5067/MODIS/MOD14.NRT.061); MOD14 [doi:10.5067/MODIS/MOD14.061](https://doi.org/10.5067/MODIS/MOD14.061); MYD14.NRT [doi:10.5067/MODIS/MYD14.NRT.061](https://doi.org/10.5067/MODIS/MYD14.NRT.061); MYD14 [doi:10.5067/MODIS/MYD14.061](https://doi.org/10.5067/MODIS/MYD14.061)

‎config/default/common/config/metadata/layers/modis/terra/MODIS_Terra_L2_Chlorophyll_A.md

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The MODIS Level 2 Chlorophyll *a* product is available from both the Terra and Aqua satellites. The sensor and imagery resolution is 1 km, and the temporal resolution is daily.
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References: MODISST_L2_OC_NRT [https://oceancolor.gsfc.nasa.gov/data/10.5067/TERRA/MODIS/L2/OC/2022]; MODIST_L2_OC [doi:10.5067/TERRA/MODIS/L2/OC/2022](https://dx.doi.org/10.5067/TERRA/MODIS/L2/OC/2022)
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References: [MODIST_L2_OC_NRT](https://oceancolor.gsfc.nasa.gov/data/10.5067/TERRA/MODIS/L2/OC/2022); MODIST_L2_OC [doi:10.5067/TERRA/MODIS/L2/OC/2022](https://dx.doi.org/10.5067/TERRA/MODIS/L2/OC/2022)

‎config/default/common/config/metadata/layers/modis/terra/MODIS_Terra_L2_Photosynthetically_Available_Radiation.md

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The Photosynthetically Available Radiation (L2) layer displays photosynthetically available radiation over oceans and large bodies of water and is measured in einstein/m²/day.
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References: References: MODISST_L2_OC_NRT [https://oceancolor.gsfc.nasa.gov/data/10.5067/TERRA/MODIS/L2/OC/2022]; MODIST_L2_OC [doi:10.5067/TERRA/MODIS/L2/OC/2022](https://dx.doi.org/10.5067/TERRA/MODIS/L2/OC/2022)
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References: [MODIST_L2_OC_NRT](https://oceancolor.gsfc.nasa.gov/data/10.5067/TERRA/MODIS/L2/OC/2022); MODIST_L2_OC [doi:10.5067/TERRA/MODIS/L2/OC/2022](https://dx.doi.org/10.5067/TERRA/MODIS/L2/OC/2022)

‎config/default/common/config/metadata/layers/oci/OCI_PACE_Photosynthetically_Available_Radiation.md

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The Photosynthetically Available Radiation layer displays photosynthetically available radiation over oceans and large bodies of water and is measured in einstein/m²/day.
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The Photosynthetically Available Radiation product is available from the Ocean Color Instrument (OCI) aboard the PACE satellite. The sensor resolution is 1.2 km, imagery resolution is 1 km, and the temporal resolution is daily.
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References: [PACE_OCI_L2_PAR_NRT](https://cmr.earthdata.nasa.gov/search/concepts/C3020920715-OB_CLOUD.html)

‎config/default/common/config/metadata/layers/reference/orbits/OrbitTracks_EarthCARE_Ascending.md

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The EarthCARE - Orbit Track & Time (Ascending/Night) layer is the path of ESA's (European Space Agency) Earth Cloud, Aerosol, and Radiation Explorer (EarthCARE) satellite on its ascending/night-time orbit. Overpass times are shown in Coordinated Universal Time (UTC).
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Orbital Track information from <https://www.space-track.org/>.

‎config/default/common/config/metadata/layers/reference/orbits/OrbitTracks_EarthCARE_Descending.md

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The EarthCARE - Orbit Track & Time (Descending/Day) layer is the path of ESA's (European Space Agency) Earth Cloud, Aerosol, and Radiation Explorer (EarthCARE) satellite on its descending/day-time orbit. Overpass times are shown in Coordinated Universal Time (UTC).
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Orbital Track information from <https://www.space-track.org/>.

‎config/default/common/config/metadata/layers/viirs/noaa20/VIIRS_NOAA20_CorrectedReflectance_BandsM11-I2-I1_Granule.md

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**NOTE: This layer is undergoing beta testing. Imagery is pixelated in certain areas and is currently being investigated.**
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Granule Corrected Reflectance imagery displays each 6-minute granule of imagery in near real-time. It is available on a 15 day rolling window basis. Each granule shows imagery as it was captured by the VIIRS instrument in that 6-minute time period and reveals areas that may have otherwise been obscured by the mosaicking of subsequent overpasses.
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Granule Corrected Reflectance imagery displays each 6-minute granule of imagery in near real-time. It is available on a 90 day rolling window basis. Each granule shows imagery as it was captured by the VIIRS instrument in that 6-minute time period and reveals areas that may have otherwise been obscured by the mosaicking of subsequent overpasses.
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For a daily overview, please refer to the associated Corrected Reflectance Mosaic/Composite image.
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