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Merge branch 'develop' into WV-3474-esri-reference-layer
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PatchesMaps authored Feb 13, 2025
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6 changes: 3 additions & 3 deletions config/default/common/brand/about/imagery.md
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<h2>Imagery Use</h2>
<p>NASA supports an <a
href="https://www.earthdata.nasa.gov/engage/open-data-services-software-policies/data-information-policy"
target="_blank" rel="noopener noreferrer">open data policy</a> and we encourage publication of imagery
<p>NASA promotes <a
href="https://www.earthdata.nasa.gov/engage/open-data-services-software-policies/data-information-guidance"
target="_blank" rel="noopener noreferrer">full and open sharing of data</a> and we encourage publication of imagery
from
Worldview; when doing so for image captions, please cite it as "NASA Worldview" and also consider including a
direct link to the imagery in Worldview to allow others to explore the imagery.</p>
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### About MODIS
MODIS (or Moderate Resolution Imaging Spectroradiometer) is a key instrument aboard the Terra (EOS AM) and Aqua (EOS PM) satellites. Terra's orbit around the Earth is timed so that it passes from north to south across the equator in the morning, while Aqua passes south to north over the equator in the afternoon. Terra MODIS and Aqua MODIS are viewing the entire Earth's surface every 1 to 2 days, acquiring data in 36 spectral bands, or groups of wavelengths (see MODIS Technical Specifications). These data will improve our understanding of global dynamics and processes occurring on the land, in the oceans, and in the lower atmosphere. MODIS is playing a vital role in the development of validated, global, interactive Earth system models able to predict global change accurately enough to assist policy makers in making sound decisions concerning the protection of our environment.
MODIS (or Moderate Resolution Imaging Spectroradiometer) is a key instrument aboard the Terra (EOS AM) and Aqua (EOS PM) satellites. Terra's orbit around the Earth is timed so that it passes from north to south across the equator in the morning, while Aqua passes south to north over the equator in the afternoon. Terra MODIS and Aqua MODIS are viewing the entire Earth's surface every 1 to 2 days, acquiring data in 36 spectral bands, or groups of wavelengths (see MODIS Technical Specifications). These data will improve our understanding of global dynamics and processes occurring on the land, in the oceans, and in the lower atmosphere. MODIS is playing a vital role in the development of validated, global, interactive Earth system models able to predict global change accurately enough to assist decision makers concerning the protection of our environment.
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The Sea Surface Temperature (Day) layer displays level 2 11µm sea surface temperature in Celsius (C). MODIS (or Moderate Resolution Imaging Spectroradiometer) is a key instrument aboard the Terra (EOS AM) and Aqua (EOS PM) satellites. Terra's orbit around the Earth is timed so that it passes from north to south across the equator in the morning, while Aqua passes south to north over the equator in the afternoon. Terra MODIS and Aqua MODIS are viewing the entire Earth's surface every 1 to 2 days, acquiring data in 36 spectral bands, or groups of wavelengths (see MODIS Technical Specifications). These data will improve our understanding of global dynamics and processes occurring on the land, in the oceans, and in the lower atmosphere. MODIS is playing a vital role in the development of validated, global, interactive Earth system models able to predict global change accurately enough to assist policy makers in making sound decisions concerning the protection of our environment.
The Sea Surface Temperature (Day) layer displays level 2 11µm sea surface temperature in Celsius (C). MODIS (or Moderate Resolution Imaging Spectroradiometer) is a key instrument aboard the Terra (EOS AM) and Aqua (EOS PM) satellites. Terra's orbit around the Earth is timed so that it passes from north to south across the equator in the morning, while Aqua passes south to north over the equator in the afternoon. Terra MODIS and Aqua MODIS are viewing the entire Earth's surface every 1 to 2 days, acquiring data in 36 spectral bands, or groups of wavelengths (see MODIS Technical Specifications). These data will improve our understanding of global dynamics and processes occurring on the land, in the oceans, and in the lower atmosphere. MODIS is playing a vital role in the development of validated, global, interactive Earth system models able to predict global change accurately enough to assist decision makers concerning the protection of our environment.

References: [MODISA_L2_SST_NRT](https://cmr.earthdata.nasa.gov/search/concepts/C1641945527-OB_DAAC.html) and [MODISA_L2_SST](https://cmr.earthdata.nasa.gov/search/concepts/C1615905765-OB_DAAC.html)
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The Sea Surface Temperature (Night) layer displays level 2 11µm sea surface temperature in Celsius (C). MODIS (or Moderate Resolution Imaging Spectroradiometer) is a key instrument aboard the Terra (EOS AM) and Aqua (EOS PM) satellites. Terra's orbit around the Earth is timed so that it passes from north to south across the equator in the morning, while Aqua passes south to north over the equator in the afternoon. Terra MODIS and Aqua MODIS are viewing the entire Earth's surface every 1 to 2 days, acquiring data in 36 spectral bands, or groups of wavelengths (see MODIS Technical Specifications). These data will improve our understanding of global dynamics and processes occurring on the land, in the oceans, and in the lower atmosphere. MODIS is playing a vital role in the development of validated, global, interactive Earth system models able to predict global change accurately enough to assist policy makers in making sound decisions concerning the protection of our environment.
The Sea Surface Temperature (Night) layer displays level 2 11µm sea surface temperature in Celsius (C). MODIS (or Moderate Resolution Imaging Spectroradiometer) is a key instrument aboard the Terra (EOS AM) and Aqua (EOS PM) satellites. Terra's orbit around the Earth is timed so that it passes from north to south across the equator in the morning, while Aqua passes south to north over the equator in the afternoon. Terra MODIS and Aqua MODIS are viewing the entire Earth's surface every 1 to 2 days, acquiring data in 36 spectral bands, or groups of wavelengths (see MODIS Technical Specifications). These data will improve our understanding of global dynamics and processes occurring on the land, in the oceans, and in the lower atmosphere. MODIS is playing a vital role in the development of validated, global, interactive Earth system models able to predict global change accurately enough to assist decision makers concerning the protection of our environment.

References: [MODISA_L2_SST_NRT](https://cmr.earthdata.nasa.gov/search/concepts/C1641945527-OB_DAAC.html) and [MODISA_L2_SST](https://cmr.earthdata.nasa.gov/search/concepts/C1615905765-OB_DAAC.html)
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The Sea Surface Temperature (Day, L2) layer displays level 2 11µm sea surface temperature in Celsius (C). MODIS (or Moderate Resolution Imaging Spectroradiometer) is a key instrument aboard the Terra (EOS AM) and Aqua (EOS PM) satellites. Terra's orbit around the Earth is timed so that it passes from north to south across the equator in the morning, while Aqua passes south to north over the equator in the afternoon. Terra MODIS and Aqua MODIS are viewing the entire Earth's surface every 1 to 2 days, acquiring data in 36 spectral bands, or groups of wavelengths (see MODIS Technical Specifications). These data will improve our understanding of global dynamics and processes occurring on the land, in the oceans, and in the lower atmosphere. MODIS is playing a vital role in the development of validated, global, interactive Earth system models able to predict global change accurately enough to assist policy makers in making sound decisions concerning the protection of our environment.
The Sea Surface Temperature (Day, L2) layer displays level 2 11µm sea surface temperature in Celsius (C). MODIS (or Moderate Resolution Imaging Spectroradiometer) is a key instrument aboard the Terra (EOS AM) and Aqua (EOS PM) satellites. Terra's orbit around the Earth is timed so that it passes from north to south across the equator in the morning, while Aqua passes south to north over the equator in the afternoon. Terra MODIS and Aqua MODIS are viewing the entire Earth's surface every 1 to 2 days, acquiring data in 36 spectral bands, or groups of wavelengths (see MODIS Technical Specifications). These data will improve our understanding of global dynamics and processes occurring on the land, in the oceans, and in the lower atmosphere. MODIS is playing a vital role in the development of validated, global, interactive Earth system models able to predict global change accurately enough to assist decision makers concerning the protection of our environment.

References: [MODIST_L2_SST_NRT](https://cmr.earthdata.nasa.gov/search/concepts/C1641917076-OB_DAAC.html) and [MODIST_L2_SST](https://cmr.earthdata.nasa.gov/search/concepts/C1615934250-OB_DAAC.html)
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The Sea Surface Temperature (Night, L2) layer displays level 2 11µm sea surface temperature in Celsius (C). MODIS (or Moderate Resolution Imaging Spectroradiometer) is a key instrument aboard the Terra (EOS AM) and Aqua (EOS PM) satellites. Terra's orbit around the Earth is timed so that it passes from north to south across the equator in the morning, while Aqua passes south to north over the equator in the afternoon. Terra MODIS and Aqua MODIS are viewing the entire Earth's surface every 1 to 2 days, acquiring data in 36 spectral bands, or groups of wavelengths (see MODIS Technical Specifications). These data will improve our understanding of global dynamics and processes occurring on the land, in the oceans, and in the lower atmosphere. MODIS is playing a vital role in the development of validated, global, interactive Earth system models able to predict global change accurately enough to assist policy makers in making sound decisions concerning the protection of our environment.
The Sea Surface Temperature (Night, L2) layer displays level 2 11µm sea surface temperature in Celsius (C). MODIS (or Moderate Resolution Imaging Spectroradiometer) is a key instrument aboard the Terra (EOS AM) and Aqua (EOS PM) satellites. Terra's orbit around the Earth is timed so that it passes from north to south across the equator in the morning, while Aqua passes south to north over the equator in the afternoon. Terra MODIS and Aqua MODIS are viewing the entire Earth's surface every 1 to 2 days, acquiring data in 36 spectral bands, or groups of wavelengths (see MODIS Technical Specifications). These data will improve our understanding of global dynamics and processes occurring on the land, in the oceans, and in the lower atmosphere. MODIS is playing a vital role in the development of validated, global, interactive Earth system models able to predict global change accurately enough to assist decision makers concerning the protection of our environment.

References: [MODIST_L2_SST_NRT](https://cmr.earthdata.nasa.gov/search/concepts/C1641917076-OB_DAAC.html) and [MODIST_L2_SST](https://cmr.earthdata.nasa.gov/search/concepts/C1615934250-OB_DAAC.html)
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Expand Up @@ -4,6 +4,10 @@ The dynamically generated Reflectance (Bands 5-4-3, False Color) imagery layer i

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 an 8 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://www.earthdata.nasa.gov/about/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.
Landsat 9 launched on September 21, 2021 and was subsequently added to the HLS product, availability of imagery from Landsat 8 and Landsat 9 is as follows:
- Landsat 8: April 11, 2013 - Present
- Landsat 9: May 31, 2022 - Present

This imagery layer is provided dynamically through the [NASA Interagency Implementation and Advanced Concepts Team (IMPACT)](https://www.earthdata.nasa.gov/about/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: HLSL30 v002 [doi:10.5067/HLS/HLSL30.002](https://doi.org/10.5067/HLS/HLSL30.002)
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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.
The Reflectance imagery layer from Sentinel-2\/MSI product (S30) is available through the HLS project from the Multi-Spectral Instrument (MSI) aboard the European Union’s Copernicus Sentinel-2A, Sentinel-2B, and Sentinel-2C 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://www.earthdata.nasa.gov/about/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.
On January 21, 2025, the Sentinel-2C satellite replaced Sentinel-2A satellite. This layer contains a mix of imagery from Sentinel-2A, Sentinel-2B, and Sentinel-2C.
- Sentinel-2A: November 28, 2015 to January 22, 2025
- Sentinel-2B: September 18, 2017 to Present
- Sentinel-2C: January 21, 2025 to Present

This imagery layer is provided dynamically through the [NASA Interagency Implementation and Advanced Concepts Team (IMPACT)](https://www.earthdata.nasa.gov/about/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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Expand Up @@ -4,6 +4,10 @@ This Reflectance imagery layer can be customized to display any available Red-Gr

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 an 8 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://www.earthdata.nasa.gov/about/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.
Landsat 9 launched on September 21, 2021 and was subsequently added to the HLS product, availability of imagery from Landsat 8 and Landsat 9 is as follows:
- Landsat 8: April 11, 2013 - Present
- Landsat 9: May 31, 2022 - Present

This imagery layer is provided dynamically through the [NASA Interagency Implementation and Advanced Concepts Team (IMPACT)](https://www.earthdata.nasa.gov/about/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: HLSL30 v002 [doi:10.5067/HLS/HLSL30.002](https://doi.org/10.5067/HLS/HLSL30.002)
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Expand Up @@ -4,6 +4,11 @@ This Reflectance imagery layer can be customized to display any available Red-Gr

The Reflectance imagery layer from Sentinel-2A and Sentinel-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://www.earthdata.nasa.gov/about/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.
On January 21, 2025, the Sentinel-2C satellite replaced Sentinel-2A satellite. This layer contains a mix of imagery from Sentinel-2A, Sentinel-2B, and Sentinel-2C.
- Sentinel-2A: November 28, 2015 to January 22, 2025
- Sentinel-2B: September 18, 2017 to Present
- Sentinel-2C: January 21, 2025 to Present

This imagery layer is provided dynamically through the [NASA Interagency Implementation and Advanced Concepts Team (IMPACT)](https://www.earthdata.nasa.gov/about/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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