Merge pull request #4907 from nasa-gibs/release

Release to Main v4.23.0

LICENSE.md

@@ -3,7 +3,7 @@
 This code was originally developed at NASA/Goddard Space Flight Center for
 the Earth Science Data and Information System (ESDIS) project.
 
-Copyright © 2013 - 2023 United States Government as represented by the
+Copyright © 2013 - 2024 United States Government as represented by the
 Administrator of the National Aeronautics and Space Administration.
 All Rights Reserved.
 
@@ -131,7 +131,7 @@ customarily used for software exchange.
 **B.** Each Recipient must ensure that the following copyright notice appears
 prominently in the Subject Software:
 
-    Copyright © 2012-2023 United States Government
+    Copyright © 2012-2024 United States Government
     as represented by the Administrator of the
     National Aeronautics and Space Administration.
     All Rights Reserved.

README.md

@@ -76,7 +76,6 @@ To update Worldview, pull down any branch or tag from GitHub. From the `main` br
 - [Custom Branding](doc/branding.md)
 - [Optional Features](doc/features.md)
 - [Developing](doc/developing.md)
-- [Deployment](doc/deployment.md)
 - [Testing](doc/testing.md)
 - [URL Parameters](doc/url_parameters.md)
 - [Uploading](doc/upload.md)

config/default/common/brand/about/license.md

@@ -1,11 +1,11 @@
 <h2>License</h2>
-<p>Copyright © 2013 - 2023 United States Government as represented by the Administrator of the National Aeronautics
+<p>Copyright © 2013 - 2024 United States Government as represented by the Administrator of the National Aeronautics
     and Space Administration. All Rights Reserved. This software is licensed under the <a
-        href="https://ti.arc.nasa.gov/opensource/nosa/" target="_blank" rel="noopener noreferrer">NASA Open Source
+        href="https://opensource.gsfc.nasa.gov/nosa.php" target="_blank" rel="noopener noreferrer">NASA Open Source
         Software Agreement, Version 1.3</a>. Source code is available on the <a
         href="https://github.com/nasa-gibs/worldview" target="_blank" rel="noopener noreferrer">NASA GIBS
         GitHub</a>.</p>
 <hr>
 <p>@BUILD_TIMESTAMP@<br> Responsible NASA Official: <a href="mailto:[email protected]">Ryan
         Boller</a><br>
-<a href="https://www.nasa.gov/about/highlights/HP_Privacy.html" target="_blank">Web Privacy Policy</a></p>
+<a href="https://www.nasa.gov/privacy/#privacy-policy" target="_blank">Web Privacy Policy</a></p>

config/default/common/config/metadata/layers/amsre/LPRM_AMSRE_Surface_Soil_Moisture_C_Band_Day_Daily.md

@@ -0,0 +1,5 @@
+The Surface Soil Moisture C-band (Day, Daily) layer displays level 3, daily, gridded surface soil moisture from the daytime (ascending) overpass. The surface soil moisture is derived from passive microwave remote sensing data from the Advanced Microwave Scanning Radiometer-Earth Observing System (AMSR-E), using the Land Parameter Retrieval Model (LPRM). The LPRM is based on a forward radiative transfer model to retrieve surface soil moisture and vegetation optical depth.
+
+The spatial resolution is 25 km x 25 km, the imagery resolution is 2 km and temporal availability is daily, covering the period from June 2002 to October 2011.
+
+References: LPRM_AMSRE_A_SOILM3 [doi:10.5067/X3K5V3NNLYAV](https://doi.org/10.5067/X3K5V3NNLYAV)

config/default/common/config/metadata/layers/amsre/LPRM_AMSRE_Surface_Soil_Moisture_C_Band_Night_Daily.md

@@ -0,0 +1,5 @@
+The Surface Soil Moisture C-band (Night, Daily) layer displays level 3, daily, gridded surface soil moisture from the nighttime (descending) overpass. The surface soil moisture is derived from passive microwave remote sensing data from the Advanced Microwave Scanning Radiometer-Earth Observing System (AMSR-E), using the Land Parameter Retrieval Model (LPRM). The LPRM is based on a forward radiative transfer model to retrieve surface soil moisture and vegetation optical depth.
+
+The spatial resolution is 25 km x 25 km, the imagery resolution is 2 km and temporal availability is daily, covering the period from June 2002 to October 2011.
+
+References: LPRM_AMSRE_D_SOILM3 [doi:10.5067/MXL0MFDHWP07](https://doi.org/10.5067/MXL0MFDHWP07)

config/default/common/config/metadata/layers/modis/Chlorophyll_a.md

@@ -1,4 +1,4 @@
 ### About Chlorophyll *a*
 Chlorophyll is a light harvesting pigment found in most photosynthetic organisms. In the ocean, phytoplankton all contain the chlorophyll pigment, which has a greenish color. Derived from the Greek words _phyto_ (plant) and _plankton_ (made to wander or drift), _phytoplankton_ are microscopic organisms that live in watery environments, both salty and fresh. Some phytoplankton are bacteria, some are protists, and most are single-celled plants. The concentration of chlorophyll *a* is used as an index of phytoplankton biomass. Phytoplankton fix carbon through photosynthesis, taking in dissolved carbon dioxide in the sea water and producing oxygen, enabling phytoplankton to grow. Changes in the amount of phytoplankton indicate the change in productivity of the ocean and as marine phytoplankton capture almost an equal amount of carbon as does photosynthesis by land vegetation, it provides an ocean link to global climate change modeling. The MODIS Chlorophyll *a* product is therefore a useful product for assessing the “health” of the ocean. The presence of phytoplankton indicates sufficient nutrient conditions for phytoplankton to flourish, but harmful algal blooms (HABs) can result when high concentrations of phytoplankton produced toxins build up. Known as red tides, blue-green algae or cyanobacteria, harmful algal blooms have severe impacts on human health, aquatic ecosystems and the economy. Chlorophyll features can also be used to trace oceanographic currents, atmospheric jets/streams and upwelling/downwelling/river plumes. Chlorophyll concentration is also useful for studying the Earth’s climate system as it is plays an integral role in the Global Carbon Cycle. More phytoplankton in the ocean may result in a higher capture rate of carbon dioxide into the ocean and help cool the planet.
 
-References: [OceanColor Web - Level 1&2 Browsers](https://oceancolor.gsfc.nasa.gov/cgi/browse.pl?sen=am); [OceanColor Web - Chlorophyll a](https://oceancolor.gsfc.nasa.gov/atbd/chlor_a/); [NASA Earth Observations - Chlorophyll Concentration](https://neo.gsfc.nasa.gov/view.php?datasetId=MY1DMM_CHLORA)
+References: [OceanColor Web - Level 1&2 Browsers](https://oceancolor.gsfc.nasa.gov/cgi/browse.pl?sen=am); [Earthdata Algorithm Publication Tool - Chlorophyll a](https://www.earthdata.nasa.gov/apt/documents/chlor-a/v1.0); [NASA Earth Observations - Chlorophyll Concentration](https://neo.gsfc.nasa.gov/view.php?datasetId=MY1DMM_CHLORA)

config/default/common/config/metadata/layers/modis/aqua/MODIS_Aqua_L3_SST_MidIR_4km_Night_8Day.md

@@ -1,5 +1,5 @@
 The MODIS L3 SST 4km layer shows global nighttime sea surface temperature (SST) at a depth of a few micrometers with ranges from -1.8 to 32 degree Celsius. The SST is derived with a Mid-Infrared (Short–Wave) SST Algorithm that uses MODIS bands 22 and 23 at 3.959 and 4.050 μm. This Level 3 product is derived from native 1 km Level 2 SST observations that are mapped to a global 4.63 km grid. The temporal resolution of this MODIS L3 SST is 8-Day.
 
-References: MODIS_AQUA_L3_SST_MID-IR_8DAY_4KM_NIGHTTIME_V2019.0 [doi:10.5067/MODAM-8D4N9](https://doi.org/10.5067/MODAM-8D4N9); Details of the [algorithm](https://oceancolor.gsfc.nasa.gov/atbd/sst4/) can be found at Ocean Biology Processing Group (OBPG/OB.DAAC) website.
+References: MODIS_AQUA_L3_SST_MID-IR_8DAY_4KM_NIGHTTIME_V2019.0 [doi:10.5067/MODAM-8D4N9](https://doi.org/10.5067/MODAM-8D4N9); Details of the [algorithm](https://oceancolor.gsfc.nasa.gov/resources/atbd/sst4/) can be found at Ocean Biology Processing Group (OBPG/OB.DAAC) website.
 
 P. J. Minnett et al., "Sea-surface temperature measurements from the Moderate-Resolution Imaging Spectroradiometer (MODIS) on Aqua and Terra," IGARSS 2004. 2004 IEEE International Geoscience and Remote Sensing Symposium, Anchorage, AK, 2004, pp. 4576-4579 vol.7. [doi:10.1109/IGARSS.2004.1370173](https://doi.org/10.1109/IGARSS.2004.1370173).

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

@@ -2,4 +2,4 @@ The MODIS Cloud Water Path (PCL) indicates the amount of water in the atmosphere
 
 The MODIS Cloud Water Path layers are available from both the Terra (MOD06) and Aqua (MYD06) satellites for daytime overpasses. The sensor/algorithm resolution is 1 km, imagery resolution is 1 km, and the temporal resolution is daily.
 
-References: [MODIS Atmosphere - Cloud (06_L2)](https://modis-atmos.gsfc.nasa.gov/products/cloud); [NCAR|UCAR Climate Date Guide: Cloud Water Path](https://climatedataguide.ucar.edu/climate-data/liquid-water-path-overview); [GES DISC: Cloud Water Path](https://disc.gsfc.nasa.gov/information/glossary?title=Cloud%20Water%20Path)
+References: [MODIS Atmosphere - Cloud (06_L2)](https://modis-atmos.gsfc.nasa.gov/products/cloud); [NCAR|UCAR Climate Date Guide: Cloud Dataset Overview](https://climatedataguide.ucar.edu/climate-data/cloud-dataset-overview); [GES DISC: Cloud Water Path](https://disc.gsfc.nasa.gov/information/glossary?title=Cloud%20Water%20Path)

config/default/common/config/metadata/layers/multi-mission/hls/HLS_MGRS_Granule_Grid.md

@@ -4,4 +4,4 @@ The UTM system divides the Earth’s surface into 60 longitude zones, each 6° o
 
 The MGRS/HLS Grid layer is a reference layer and does not change over time.
 
-References: [Harmonized Landsat Sentinel-2 (HLS) Product User Guide](https://lpdaac.usgs.gov/documents/1326/HLS_User_Guide_V2.pdf)
+References: [Harmonized Landsat Sentinel-2 (HLS) Product User Guide](https://lpdaac.usgs.gov/documents/1698/HLS_User_Guide_V2.pdf)

config/default/common/config/metadata/layers/multi-mission/hls/Reflectance.md

@@ -1,5 +1,5 @@
 ### About HLS
 The Harmonized Landsat and Sentinel-2 (HLS) project provides consistent surface reflectance data from the Operational Land Imager (OLI) aboard the joint NASA/USGS Landsat 8 and 9 satellites and the Multi-Spectral Instrument (MSI) aboard the European Union’s Copernicus Sentinel-2A and Sentinel-2B satellites. The combined measurements between Landsat 8, Landsat 9, Sentinel-2A, and Sentinel-2B enable global observations of the land every 2-3 days at 30 meter (m) spatial resolution. The HLS project uses a set of algorithms to obtain seamless products from OLI and MSI that include atmospheric correction, cloud and cloud-shadow masking, spatial co-registration and common gridding, illumination and view angle normalization, and spectral bandpass adjustment.
 
-References: [Harmonized Landsat Sentinel-2 (HLS) Product User Guide](https://lpdaac.usgs.gov/documents/1326/HLS_User_Guide_V2.pdf)
+References: [Harmonized Landsat Sentinel-2 (HLS) Product User Guide](https://lpdaac.usgs.gov/documents/1698/HLS_User_Guide_V2.pdf)
 

config/default/common/config/metadata/layers/smap/SMAP_L1_Passive_Brightness_Temp_Aft_H.md

@@ -2,6 +2,6 @@ The Soil Moisture Active Passive (SMAP) "Uncorrected Brightness Temperature 36 k
 
 The SMAP spacecraft carries two instruments, a radar (active) and a radiometer (passive), that together make global measurements of land surface soil moisture and freeze/thaw state. It is useful for monitoring and predicting natural hazards such as floods and droughts, understanding the linkages between Earth’s water, energy and carbon cycles, and reducing uncertainties in predicting weather and climate.
 
-References: SPL1CTB [doi: 10.5067/JJ5FL7FRLKJI](https://doi.org/10.5067/JJ5FL7FRLKJI)
+References: SPL1CTB [doi:10.5067/DV7IX2DQ681Y](https://doi.org/10.5067/DV7IX2DQ681Y)
 
 Data field: `cell_tb_h_aft`

config/default/common/config/metadata/layers/smap/SMAP_L1_Passive_Brightness_Temp_Aft_H_QA.md

@@ -2,6 +2,6 @@ The Soil Moisture Active Passive (SMAP) "Uncorrected Brightness Temperature 36 k
 
 Within the image, green indicates that TB observations have acceptable quality for science use, yellow indicates that caution should be used with the TB observations as one or more quality-impacting conditions have been identified, and red indicates that TB observations are flagged as bad due to unacceptable quality.
 
-References: SPL1CTB [doi: 10.5067/JJ5FL7FRLKJI](https://doi.org/10.5067/JJ5FL7FRLKJI)
+References: SPL1CTB [doi:10.5067/DV7IX2DQ681Y](https://doi.org/10.5067/DV7IX2DQ681Y)
 
 Data field: `cell_tb_qual_flag_h_aft`

config/default/common/config/metadata/layers/smap/SMAP_L1_Passive_Brightness_Temp_Aft_H_RFI.md

@@ -2,6 +2,6 @@ The Soil Moisture Active Passive (SMAP) "Uncorrected Brightness Temperature 36 k
 
 Within the image, green indicates that TB observations are free of RFI and approved for science use, yellow indicates that caution should be used with the TB observations as RFI was detected but mitigated, and red indicates that TB observations are flagged as bad due to RFI.
 
-References: SPL1CTB [doi: 10.5067/JJ5FL7FRLKJI](https://doi.org/10.5067/JJ5FL7FRLKJI)
+References: SPL1CTB [doi:10.5067/DV7IX2DQ681Y](https://doi.org/10.5067/DV7IX2DQ681Y)
 
 Data field: `cell_tb_qual_flag_h_aft`

config/default/common/config/metadata/layers/smap/SMAP_L1_Passive_Brightness_Temp_Aft_V.md

@@ -2,6 +2,6 @@ The Soil Moisture Active Passive (SMAP) "Uncorrected Brightness Temperature 36 k
 
 The SMAP spacecraft carries two instruments, a radar (active) and a radiometer (passive), that together make global measurements of land surface soil moisture and freeze/thaw state. It is useful for monitoring and predicting natural hazards such as floods and droughts, understanding the linkages between Earth’s water, energy and carbon cycles, and reducing uncertainties in predicting weather and climate.
 
-References: SPL1CTB [doi: 10.5067/JJ5FL7FRLKJI](https://doi.org/10.5067/JJ5FL7FRLKJI)
+References: SPL1CTB [doi:10.5067/DV7IX2DQ681Y](https://doi.org/10.5067/DV7IX2DQ681Y)
 
 Data field: `cell_tb_v_aft`

config/default/common/config/metadata/layers/smap/SMAP_L1_Passive_Brightness_Temp_Aft_V_QA.md

@@ -2,6 +2,6 @@ The Soil Moisture Active Passive (SMAP) "Uncorrected Brightness Temperature 36 k
 
 Within the image, green indicates that TB observations have acceptable quality for science use, yellow indicates that caution should be used with the TB observations as one or more quality-impacting conditions have been identified, and red indicates that TB observations are flagged as bad due to unacceptable quality.
 
-References: SPL1CTB [doi: 10.5067/JJ5FL7FRLKJI](https://doi.org/10.5067/JJ5FL7FRLKJI)
+References: SPL1CTB [doi:10.5067/DV7IX2DQ681Y](https://doi.org/10.5067/DV7IX2DQ681Y)
 
 Data field: `cell_tb_qual_flag_v_aft`

config/default/common/config/metadata/layers/smap/SMAP_L1_Passive_Brightness_Temp_Aft_V_RFI.md

@@ -2,6 +2,6 @@ The Soil Moisture Active Passive (SMAP) "Uncorrected Brightness Temperature 36 k
 
 Within the image, green indicates that TB observations are free of RFI and approved for science use, yellow indicates that caution should be used with the TB observations as RFI was detected but mitigated, and red indicates that TB observations are flagged as bad due to RFI.
 
-References: SPL1CTB [doi: 10.5067/JJ5FL7FRLKJI](https://doi.org/10.5067/JJ5FL7FRLKJI)
+References: SPL1CTB [doi:10.5067/DV7IX2DQ681Y](https://doi.org/10.5067/DV7IX2DQ681Y)
 
 Data field: `cell_tb_qual_flag_v_aft`

config/default/common/config/metadata/layers/smap/SMAP_L1_Passive_Brightness_Temp_Fore_H.md

@@ -2,6 +2,6 @@ The Soil Moisture Active Passive (SMAP) "Uncorrected Brightness Temperature 36 k
 
 The SMAP spacecraft carries two instruments, a radar (active) and a radiometer (passive), that together make global measurements of land surface soil moisture and freeze/thaw state. It is useful for monitoring and predicting natural hazards such as floods and droughts, understanding the linkages between Earth’s water, energy and carbon cycles, and reducing uncertainties in predicting weather and climate.
 
-References: SPL1CTB [doi: 10.5067/JJ5FL7FRLKJI](https://doi.org/10.5067/JJ5FL7FRLKJI)
+References: SPL1CTB [doi:10.5067/DV7IX2DQ681Y](https://doi.org/10.5067/DV7IX2DQ681Y)
 
 Data field: `cell_tb_h_fore`

config/default/common/config/metadata/layers/smap/SMAP_L1_Passive_Brightness_Temp_Fore_H_QA.md

@@ -2,6 +2,6 @@ The Soil Moisture Active Passive (SMAP) "Uncorrected Brightness Temperature 36 k
 
 Within the image, green indicates that TB observations have acceptable quality for science use, yellow indicates that caution should be used with the TB observations as one or more quality-impacting conditions have been identified, and red indicates that TB observations are flagged as bad due to unacceptable quality.
 
-References: SPL1CTB [doi: 10.5067/JJ5FL7FRLKJI](https://doi.org/10.5067/JJ5FL7FRLKJI)
+References: SPL1CTB [doi:10.5067/DV7IX2DQ681Y](https://doi.org/10.5067/DV7IX2DQ681Y)
 
 Data field: `cell_tb_qual_flag_h_fore`

config/default/common/config/metadata/layers/smap/SMAP_L1_Passive_Brightness_Temp_Fore_H_RFI.md

@@ -2,6 +2,6 @@ The Soil Moisture Active Passive (SMAP) "Uncorrected Brightness Temperature 36 k
 
 Within the image, green indicates that TB observations are free of RFI and approved for science use, yellow indicates that caution should be used with the TB observations as RFI was detected but mitigated, and red indicates that TB observations are flagged as bad due to RFI.
 
-References: SPL1CTB [doi: 10.5067/JJ5FL7FRLKJI](https://doi.org/10.5067/JJ5FL7FRLKJI)
+References: SPL1CTB [doi:10.5067/DV7IX2DQ681Y](https://doi.org/10.5067/DV7IX2DQ681Y)
 
 Data field: `cell_tb_qual_flag_h_fore`

config/default/common/config/metadata/layers/smap/SMAP_L1_Passive_Brightness_Temp_Fore_V.md

@@ -2,6 +2,6 @@ The Soil Moisture Active Passive (SMAP) "Uncorrected Brightness Temperature 36 k
 
 The SMAP spacecraft carries two instruments, a radar (active) and a radiometer (passive), that together make global measurements of land surface soil moisture and freeze/thaw state. It is useful for monitoring and predicting natural hazards such as floods and droughts, understanding the linkages between Earth’s water, energy and carbon cycles, and reducing uncertainties in predicting weather and climate.
 
-References: SPL1CTB [doi: 10.5067/JJ5FL7FRLKJI](https://doi.org/10.5067/JJ5FL7FRLKJI)
+References: SPL1CTB [doi:10.5067/DV7IX2DQ681Y](https://doi.org/10.5067/DV7IX2DQ681Y)
 
 Data field: `cell_tb_v_fore`

config/default/common/config/metadata/layers/smap/SMAP_L1_Passive_Brightness_Temp_Fore_V_QA.md

@@ -2,6 +2,6 @@ The Soil Moisture Active Passive (SMAP) "Uncorrected Brightness Temperature 36 k
 
 Within the image, green indicates that TB observations have acceptable quality for science use, yellow indicates that caution should be used with the TB observations as one or more quality-impacting conditions have been identified, and red indicates that TB observations are flagged as bad due to unacceptable quality.
 
-References: SPL1CTB [doi: 10.5067/JJ5FL7FRLKJI](https://doi.org/10.5067/JJ5FL7FRLKJI)
+References: SPL1CTB [doi:10.5067/DV7IX2DQ681Y](https://doi.org/10.5067/DV7IX2DQ681Y)
 
 Data field: `cell_tb_qual_flag_v_fore`

config/default/common/config/metadata/layers/smap/SMAP_L1_Passive_Brightness_Temp_Fore_V_RFI.md

@@ -2,6 +2,6 @@ The Soil Moisture Active Passive (SMAP) "Uncorrected Brightness Temperature 36 k
 
 Within the image, green indicates that TB observations are free of RFI and approved for science use, yellow indicates that caution should be used with the TB observations as RFI was detected but mitigated, and red indicates that TB observations are flagged as bad due to RFI.
 
-References: SPL1CTB [doi: 10.5067/JJ5FL7FRLKJI](https://doi.org/10.5067/JJ5FL7FRLKJI)
+References: SPL1CTB [doi:10.5067/DV7IX2DQ681Y](https://doi.org/10.5067/DV7IX2DQ681Y)
 
 Data field: `cell_tb_qual_flag_v_fore`

config/default/common/config/metadata/layers/smap/SMAP_L1_Passive_Enhanced_Brightness_Temp_Aft_H.md

@@ -2,6 +2,6 @@ The Soil Moisture Active Passive (SMAP) "Uncorrected Brightness Temperature 9 km
 
 The SMAP spacecraft carries two instruments, a radar (active) and a radiometer (passive), that together make global measurements of land surface soil moisture and freeze/thaw state. It is useful for monitoring and predicting natural hazards such as floods and droughts, understanding the linkages between Earth’s water, energy and carbon cycles, and reducing uncertainties in predicting weather and climate.
 
-References: SPL1CTB_E [doi:10.5067/XB8K63YM4U8O](https://doi.org/10.5067/XB8K63YM4U8O)
+References: SPL1CTB_E [doi:10.5067/99LHDR3NUM47](https://dx.doi.org/10.5067/99LHDR3NUM47)
 
 Data field: `cell_tb_h_aft`

config/default/common/config/metadata/layers/smap/SMAP_L1_Passive_Enhanced_Brightness_Temp_Aft_H_QA.md

@@ -2,6 +2,6 @@ The Soil Moisture Active Passive (SMAP) "Uncorrected Brightness Temperature 9 km
 
 Within the image, green indicates that TB observations have acceptable quality for science use, yellow indicates that caution should be used with the TB observations as one or more quality-impacting conditions have been identified, and red indicates that TB observations are flagged as bad due to unacceptable quality.
 
-References: SPL1CTB_E [doi:10.5067/XB8K63YM4U8O](https://doi.org/10.5067/XB8K63YM4U8O)
+References: SPL1CTB_E [doi:10.5067/99LHDR3NUM47](https://dx.doi.org/10.5067/99LHDR3NUM47)
 
 Data field: `cell_tb_qual_flag_h_aft`

config/default/common/config/metadata/layers/smap/SMAP_L1_Passive_Enhanced_Brightness_Temp_Aft_H_RFI.md

@@ -2,6 +2,6 @@ The Soil Moisture Active Passive (SMAP) "Uncorrected Brightness Temperature 9 km
 
 Within the image, green indicates that TB observations are free of RFI and approved for science use, yellow indicates that caution should be used with the TB observations as RFI was detected but mitigated, and red indicates that TB observations are flagged as bad due to RFI.
 
-References: SPL1CTB_E [doi:10.5067/XB8K63YM4U8O](https://doi.org/10.5067/XB8K63YM4U8O)
+References: SPL1CTB_E [doi:10.5067/99LHDR3NUM47](https://dx.doi.org/10.5067/99LHDR3NUM47)
 
 Data field: `cell_tb_qual_flag_h_aft`