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Merge pull request #4593 from nasa-gibs/release
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Release to Main v4.12.0
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ryanweiler92 authored Aug 23, 2023
2 parents 075e51a + 0e7211e commit fb22e4c
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**NOTE: This layer is undergoing beta testing.**

This Reflectance imagery layer can be customized to display any available Red-Green-Blue (R-G-B) band combination. Select the desired combination in via the Options panel. The layer is dynamically generated, therefore it may take longer to display.

The Reflectance imagery layer from Landsat 8 and 9/OLI product (L30) is available through the HLS project from the Operational Land Imager (OLI) aboard the Landsat 8 and 9 satellites. The sensor resolution is 30 m, imagery resolution is 30 m, and the temporal resolution is daily with a 16 day revisit time. The imagery is available in Worldview/GIBS approximately 2 - 4 days after satellite overpass. There is a separate combined Sentinel 2A and Sentinel 2B imagery layer available.

This imagery layer is provided dynamically through the [NASA Interagency Implementation and Advanced Concepts Team (IMPACT)](https://earthdata.nasa.gov/esds/impact). As it is dynamically generated, it may take slightly longer to display than normal. The imagery is also only available at higher zoom levels.

References: HLSL30 v002 [doi:10.5067/HLS/HLSL30.002](https://doi.org/10.5067/HLS/HLSL30.002)
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**NOTE: This layer is undergoing beta testing.**

This Reflectance imagery layer can be customized to display any available Red-Green-Blue (R-G-B) band combination. Select the desired combination in via the Options panel. The layer is dynamically generated, therefore it may take longer to display.

The Reflectance imagery layer from Sentinel 2A and 2B/MSI product (S30) is available through the HLS project from the Multi-Spectral Instrument (MSI) aboard the European Union’s Copernicus Sentinel-2A and Sentinel-2B satellites. The sensor resolution is 10, 20, and 60 m, imagery resolution is resampled to 30 m, and the temporal resolution is daily with a 5 day revisit time. The imagery is available in Worldview/GIBS approximately 2 - 4 days after satellite overpass. There is a separate combined Landsat 8 and 9 imagery layer available.

This imagery layer is provided dynamically through the [NASA Interagency Implementation and Advanced Concepts Team (IMPACT)](https://earthdata.nasa.gov/esds/impact). As it is dynamically generated, it may take slightly longer to display than normal. The imagery is also only available at higher zoom levels.

References: HLSS30 v002 [doi:10.5067/HLS/HLSS30.002](https://doi.org/10.5067/HLS/HLSS30.002)
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**NOTE: This layer is undergoing beta testing.**

The dynamically generated Reflectance (Bands 5-4-3, False Color) imagery layer is a false color composite that is used to gauge plant health and assess plant density. Plants reflect in near infrared and green light, while absorbing in red. Areas with better vegetation health appear red, and denser plant growth is a darker red. Cities, urban areas, and exposed ground appear grey or tan and water is blue or black.

The Reflectance imagery layer from Landsat 8 and 9/OLI product (L30) is available through the HLS project from the Operational Land Imager (OLI) aboard the Landsat 8 and 9 satellites. The sensor resolution is 30 m, imagery resolution is 30 m, and the temporal resolution is daily with a 16 day revisit time. The imagery is available in Worldview/GIBS approximately 2 - 4 days after satellite overpass. There is a separate combined Sentinel 2A and Sentinel 2B imagery layer available.

This imagery layer is provided dynamically through the [NASA Interagency Implementation and Advanced Concepts Team (IMPACT)](https://earthdata.nasa.gov/esds/impact). As it is dynamically generated, it may take slightly longer to display than normal. The imagery is also only available at higher zoom levels.

References: HLSL30 v002 [doi:10.5067/HLS/HLSL30.002](https://doi.org/10.5067/HLS/HLSL30.002)
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**NOTE: This layer is undergoing beta testing.**

The dynamically generated Reflectance (Bands 8-4-3, False Color) imagery layer is a false color composite that is used to gauge plant health and assess plant density. Plants reflect in near infrared and green light, while absorbing in red. reas with better vegetation health appear red, and denser plant growth is a darker red. Cities, urban areas, and exposed ground appear grey or tan and water is blue or black.
The Reflectance imagery layer from Sentinel 2A and 2B/MSI product (S30) is available through the HLS project from the Multi-Spectral Instrument (MSI) aboard the European Union’s Copernicus Sentinel-2A and Sentinel-2B satellites. The sensor resolution is 10, 20, and 60 m, imagery resolution is resampled to 30 m, and the temporal resolution is daily with a 5 day revisit time. The imagery is available in Worldview/GIBS approximately 2 - 4 days after satellite overpass. There is a separate combined Landsat 8 and 9 imagery layer available.

This imagery layer is provided dynamically through the [NASA Interagency Implementation and Advanced Concepts Team (IMPACT)](https://earthdata.nasa.gov/esds/impact). As it is dynamically generated, it may take slightly longer to display than normal. The imagery is only available at higher zoom levels.

References: HLSS30 v002 [doi:10.5067/HLS/HLSS30.002](https://doi.org/10.5067/HLS/HLSS30.002)
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**NOTE: This layer is undergoing beta testing.**

The dynamically generated Reflectance (Bands 7-6-4, Urban False Color) imagery layer is useful for visualizing urban areas more clearly. Urban areas are white, grey, or purple and vegetation appear in shades of green. Snow and ice are dark blue, and water is black or blue. Flooded areas are very dark blue, sometimes black. Wildfires and lava in calderas of volcanoes display in shades of yellow and red.

The Reflectance imagery layer from Landsat 8 and 9/OLI product (L30) is available through the HLS project from the Operational Land Imager (OLI) aboard the Landsat 8 and 9 satellites. The sensor resolution is 30 m, imagery resolution is 30 m, and the temporal resolution is daily with a 16 day revisit time. The imagery is available in Worldview/GIBS approximately 2 - 4 days after satellite overpass. There is a separate combined Sentinel 2A and Sentinel 2B imagery layer available.

This imagery layer is provided dynamically through the [NASA Interagency Implementation and Advanced Concepts Team (IMPACT)](https://earthdata.nasa.gov/esds/impact). As it is dynamically generated, it may take slightly longer to display than normal. The imagery is also only available at higher zoom levels.

References: HLSL30 v002 [doi:10.5067/HLS/HLSL30.002](https://doi.org/10.5067/HLS/HLSL30.002)
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**NOTE: This layer is undergoing beta testing.**

The dynamically generated Reflectance (Bands 12-11-4, Urban False Color) imagery layer is useful for visualizing urban areas more clearly. Urban areas are white, grey, or purple and vegetation appear in shades of green. Snow and ice are dark blue, and water is black or blue. Flooded areas are very dark blue, sometimes black. Wildfires and lava in calderas of volcanoes display in shades of yellow and red.


The Reflectance imagery layer from Sentinel 2A and 2B/MSI product (S30) is available through the HLS project from the Multi-Spectral Instrument (MSI) aboard the European Union’s Copernicus Sentinel-2A and Sentinel-2B satellites. The sensor resolution is 10, 20, and 60 m, imagery resolution is resampled to 30 m, and the temporal resolution is daily with a 5 day revisit time. The imagery is available in Worldview/GIBS approximately 2 - 4 days after satellite overpass. There is a separate combined Landsat 8 and 9 imagery layer available.

This imagery layer is provided dynamically through the [NASA Interagency Implementation and Advanced Concepts Team (IMPACT)](https://earthdata.nasa.gov/esds/impact). As it is dynamically generated, it may take slightly longer to display than normal. The imagery is also only available at higher zoom levels.

References: HLSS30 v002 [doi:10.5067/HLS/HLSS30.002](https://doi.org/10.5067/HLS/HLSS30.002)
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**NOTE: This layer is undergoing beta testing.**

The dynamically generated Reflectance (Bands 6-5-4, Vegetative Analysis False Color) imagery layer is useful for looking at vegetation. Vegetation are in shades of green. Burned areas appear bright red, while bare ground appear light red/pink. Water is black.

The Reflectance imagery layer from Landsat 8 and 9/OLI product (L30) is available through the HLS project from the Operational Land Imager (OLI) aboard the Landsat 8 and 9 satellites. The sensor resolution is 30 m, imagery resolution is 30 m, and the temporal resolution is daily with a 16 day revisit time. The imagery is available in Worldview/GIBS approximately 2 - 4 days after satellite overpass. There is a separate combined Sentinel 2A and Sentinel 2B imagery layer available.

This imagery layer is provided dynamically through the [NASA Interagency Implementation and Advanced Concepts Team (IMPACT)](https://earthdata.nasa.gov/esds/impact). As it is dynamically generated, it may take slightly longer to display than normal. The imagery is also only available at higher zoom levels.

References: HLSL30 v002 [doi:10.5067/HLS/HLSL30.002](https://doi.org/10.5067/HLS/HLSL30.002)
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**NOTE: This layer is undergoing beta testing.**

The dynamically generated Reflectance (Bands 11-8A-4, Vegetative Analysis False Color) imagery layer is useful for looking at vegetation. Vegetation are in shades of green. Burned areas appear bright red, while bare ground appear light red/pink. Water is black.

The Reflectance imagery layer from Sentinel 2A and 2B/MSI product (S30) is available through the HLS project from the Multi-Spectral Instrument (MSI) aboard the European Union’s Copernicus Sentinel-2A and Sentinel-2B satellites. The sensor resolution is 10, 20, and 60 m, imagery resolution is resampled to 30 m, and the temporal resolution is daily with a 5 day revisit time. The imagery is available in Worldview/GIBS approximately 2 - 4 days after satellite overpass. There is a separate combined Landsat 8 and 9 imagery layer available.

This imagery layer is provided dynamically through the [NASA Interagency Implementation and Advanced Concepts Team (IMPACT)](https://earthdata.nasa.gov/esds/impact). As it is dynamically generated, it may take slightly longer to display than normal. The imagery is also only available at higher zoom levels.

References: HLSS30 v002 [doi:10.5067/HLS/HLSS30.002](https://doi.org/10.5067/HLS/HLSS30.002)
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**NOTE: This layer is undergoing beta testing.**

The dynamically generated Reflectance (Bands 7-5-4, Shortwave Infrared) imagery layer is useful looking at how much water is present in plants and soils, as water absorbs in shortwave infrared wavelengths. It can be used to distinguish between cloud types like water clouds versus ice clouds, snow and ice, which appear white. Vegetation is in shades of green, soils and urban areas are in shades of brown, and water is black. Freshly burned areas appear red.

The Reflectance imagery layer from Landsat 8 and 9/OLI product (L30) is available through the HLS project from the Operational Land Imager (OLI) aboard the Landsat 8 and 9 satellites. The sensor resolution is 30 m, imagery resolution is 30 m, and the temporal resolution is daily with a 16 day revisit time. The imagery is available in Worldview/GIBS approximately 2 - 4 days after satellite overpass. There is a separate combined Sentinel 2A and Sentinel 2B imagery layer available.

This imagery layer is provided dynamically through the [NASA Interagency Implementation and Advanced Concepts Team (IMPACT)](https://earthdata.nasa.gov/esds/impact). As it is dynamically generated, it may take slightly longer to display than normal. The imagery is also only available at higher zoom levels.

References: HLSL30 v002 [doi:10.5067/HLS/HLSL30.002](https://doi.org/10.5067/HLS/HLSL30.002)
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@@ -0,0 +1,9 @@
**NOTE: This layer is undergoing beta testing.**

The dynamically generated Reflectance (Bands 12-8A-4, Shortwave Infrared) imagery layer is useful looking at how much water is present in plants and soils, as water absorbs in shortwave infrared wavelengths. It can be used to distinguish between cloud types like water clouds versus ice clouds, snow and ice, which appear white. Vegetation is in shades of green, soils and urban areas are in shades of brown, and water is black. Freshly burned areas appear red.

The Reflectance imagery layer from Sentinel 2A and 2B/MSI product (S30) is available through the HLS project from the Multi-Spectral Instrument (MSI) aboard the European Union’s Copernicus Sentinel-2A and Sentinel-2B satellites. The sensor resolution is 10, 20, and 60 m, imagery resolution is resampled to 30 m, and the temporal resolution is daily with a 5 day revisit time. The imagery is available in Worldview/GIBS approximately 2 - 4 days after satellite overpass. There is a separate combined Landsat 8 and 9 imagery layer available.

This imagery layer is provided dynamically through the [NASA Interagency Implementation and Advanced Concepts Team (IMPACT)](https://earthdata.nasa.gov/esds/impact). As it is dynamically generated, it may take slightly longer to display than normal. The imagery is also only available at higher zoom levels.

References: HLSS30 v002 [doi:10.5067/HLS/HLSS30.002](https://doi.org/10.5067/HLS/HLSS30.002)
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**NOTE: This layer is undergoing beta testing.**

The dynamically generated Reflectance (Bands 4-3-2, True Color) imagery layer is a true-color or natural color image because this combination of wavelengths is similar to what the human eye would see. It consists of natural-looking images of land surface, oceanic and atmospheric features.

The Reflectance imagery layer from Landsat 8 and 9/OLI product (L30) is available through the HLS project from the Operational Land Imager (OLI) aboard the Landsat 8 and 9 satellites. The sensor resolution is 30 m, imagery resolution is 30 m, and the temporal resolution is daily with a 16 day revisit time. The imagery is available in Worldview/GIBS approximately 2 - 4 days after satellite overpass. There is a separate combined Sentinel 2A and Sentinel 2B imagery layer available.

This imagery layer is provided dynamically through the [NASA Interagency Implementation and Advanced Concepts Team (IMPACT)](https://earthdata.nasa.gov/esds/impact). As it is dynamically generated, it may take slightly longer to display than normal. The imagery is also only available at higher zoom levels.

References: HLSL30 v002 [doi:10.5067/HLS/HLSL30.002](https://doi.org/10.5067/HLS/HLSL30.002)
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@@ -0,0 +1,9 @@
**NOTE: This layer is undergoing beta testing.**

The dynamically generated Reflectance (Bands 4-3-2, True Color) imagery layer is a true-color or natural color image because this combination of wavelengths is similar to what the human eye would see. It consists of natural-looking images of land surface, oceanic and atmospheric features.

The Reflectance imagery layer from Sentinel 2A and 2B/MSI product (S30) is available through the HLS project from the Multi-Spectral Instrument (MSI) aboard the European Union’s Copernicus Sentinel-2A and Sentinel-2B satellites. The sensor resolution is 10, 20, and 60 m, imagery resolution is resampled to 30 m, and the temporal resolution is daily with a 5 day revisit time. The imagery is available in Worldview/GIBS approximately 2 - 4 days after satellite overpass. There is a separate combined Landsat 8 and 9 imagery layer available.

This imagery layer is provided dynamically through the [NASA Interagency Implementation and Advanced Concepts Team (IMPACT)](https://earthdata.nasa.gov/esds/impact). As it is dynamically generated, it may take slightly longer to display than normal. The imagery is also only available at higher zoom levels.

References: HLSS30 v002 [doi:10.5067/HLS/HLSS30.002](https://doi.org/10.5067/HLS/HLSS30.002)
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The Sea Ice Surface Temperature (Day) layer shows the "skin" temperature of the sea ice surface measured in Kelvin (K). It is derived from radiance data acquired by the Visible Infrared Imaging Radiometer Suite (VIIRS) aboard the joint NASA/NOAA Joint Polar Satellite System's first satellite (JPSS-1/NOAA-20). Following the approach used by MODIS, the algorithm converts VIIRS calibrated radiances into brightness temperature and computes Ice Surface Temperature (IST) using a split-window technique. Sea Ice Surface Temperature (IST) is an indicator of freeze/thaw processes on ice and has been used to separate thin ice from open water.

The Ice Surface Temperature product is available for the Suomi NPP (VNP29) and JPSS-1/NOAA-20 (VJ129) satellites. The sensor resolution is 750 m, imagery resolution is 1 km, and the temporal resolution is daily.

References: VJ130 [doi:10.5067/BW817SEFZ1TT](https://doi.org/10.5067/BW817SEFZ1TT)
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The Sea Ice Surface Temperature (Day) layer shows the "skin" temperature of the sea ice surface measured in Kelvin (K). It is derived from radiance data acquired by the Visible Infrared Imaging Radiometer Suite (VIIRS) aboard the joint NASA/NOAA Joint Polar Satellite System's first satellite (JPSS-1/NOAA-20). Following the approach used by MODIS, the algorithm converts VIIRS calibrated radiances into brightness temperature and computes Ice Surface Temperature (IST) using a split-window technique. Sea Ice Surface Temperature (IST) is an indicator of freeze/thaw processes on ice and has been used to separate thin ice from open water.

The Ice Surface Temperature product is available for the Suomi NPP (VNP29) and JPSS-1/NOAA-20 (VJ129) satellites. The sensor resolution is 750 m, imagery resolution is 1 km, and the temporal resolution is daily.

References: VJ130 [doi:10.5067/BW817SEFZ1TT](https://doi.org/10.5067/BW817SEFZ1TT)
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The Land Surface Temperature (Day) layer shows the temperature of the land surface in Kelvin (K), from the Visible Infrared Imaging Radiometer Suite (VIIRS) aboard the joint NASA/NOAA NOAA-20 satellite.

The VJ121 product is developed synergistically with the Moderate Resolution Imaging Spectroradiometer (MODIS) LST&E Version 6.1 product (MOD21) using the same input atmospheric products and algorithmic approach based on the ASTER Temperature Emissivity Separation (TES) technique. The VJ121 product uses a physics-based algorithm to dynamically retrieve both the LST and emissivity simultaneously for VIIRS thermal infrared bands M14 (8.55 µm), M15 (10.76 µm), and M16 (12 µm). The TES algorithm is combined with an improved Water Vapor Scaling (WVS) atmospheric correction scheme to stabilize the retrieval during very warm and humid conditions. The overall objective for NASA VIIRS products is to ensure the algorithms and products are compatible with the MODIS Terra and Aqua algorithms to promote the continuity of the Earth Observation System (EOS) mission.

The Land Surface Temperature (Day) layer is available from both the joint NASA/NOAA Suomi NPP (VNP21) and NOAA-20 (VJ121) satellites. The sensor resolution is 750 m, imagery resolution is 1 km, and the temporal resolution is daily.

References: VJ121 [doi:10.5067/VIIRS/VJ121.002](https://doi.org/10.5067/VIIRS/VJ121.002)
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