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WV-3403: Update 404 links, sentinel-3 orbit track images, copyright y…
…ear (#5632) * Update 404 links * Update outdated links * Update copyright year
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# Disclaimer | ||
The information presented through this interface is provided "as is" and users bear all responsibility and liability for their use of the data. Please read the [full disclaimer](https://earthdata.nasa.gov/earth-observation-data/near-real-time/citation#ed-lance-disclaimer). | ||
The information presented through this interface is provided "as is" and users bear all responsibility and liability for their use of the data. Please read the [full disclaimer](https://www.earthdata.nasa.gov/data/projects/lance). | ||
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config/default/common/config/metadata/layers/modis/CorrectedReflectance.md
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### MODIS Corrected Reflectance vs. MODIS Surface Reflectance | ||
The MODIS Corrected Reflectance algorithm utilizes MODIS Level 1B data (the calibrated, geolocated radiances). It is not a standard, science quality product. The purpose of this algorithm is to provide natural-looking images by removing gross atmospheric effects, such as Rayleigh scattering, from MODIS visible bands 1-7. The algorithm was developed by the original MODIS Rapid Response team to address the needs of the fire monitoring community who want to see smoke. Corrected Reflectance shows smoke more clearly than the standard Surface Reflectance product. In contrast, the MODIS Land Surface Reflectance product (MOD09) is a more complete atmospheric correction algorithm that includes aerosol correction, and is designed to derive land surface properties. In clear atmospheric conditions the Corrected Reflectance product is very similar to the MOD09 product, but they depart from each other in presence of aerosols. If you wish to perform a complete atmospheric correction, please do not use the Corrected Reflectance algorithm. An additional difference is that the Land Surface Reflectance product is only tuned for calculating the reflectance over land surfaces. | ||
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References: [NASA Earthdata - Creating Reprojected True Color MODIS Images: A Tutorial](https://earthdata.nasa.gov/s3fs-public/2022-02/MODIS_True_Color.pdf); [NASA Earthdata - LANCE FAQ](https://earthdata.nasa.gov/faq/lance-faq#ed-CRvsSR) | ||
References: [NASA Earthdata - Creating Reprojected True Color MODIS Images: A Tutorial](https://earthdata.nasa.gov/s3fs-public/2022-02/MODIS_True_Color.pdf); [NASA Earthdata Forum - LANCE FAQ](https://forum.earthdata.nasa.gov/viewtopic.php?t=5203) | ||
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NOTE: We are reprocessing the entire MODIS Land imagery archive to collection 6.1 but currently the imagery is a mix of collection 6 and collection 6.1. Most of the imagery from mid-May 2021 onwards is collection 6.1 and older imagery is collection 6. |
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config/default/common/config/metadata/layers/modis/LandSurfaceReflectance.md
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### MODIS Corrected Reflectance vs. MODIS Surface Reflectance | ||
The MODIS Corrected Reflectance algorithm utilizes MODIS Level 1B data (the calibrated, geolocated radiances). It is not a standard, science quality product. The purpose of this algorithm is to provide natural-looking images by removing gross atmospheric effects, such as Rayleigh scattering, from MODIS visible bands 1-7. The algorithm was developed by the original MODIS Rapid Response team to address the needs of the fire monitoring community who want to see smoke. Corrected Reflectance shows smoke more clearly than the standard Surface Reflectance product. In contrast, the MODIS Land Surface Reflectance product (MOD09) is a more complete atmospheric correction algorithm that includes aerosol correction, and is designed to derive land surface properties. In clear atmospheric conditions the Corrected Reflectance product is very similar to the MOD09 product, but they depart from each other in presence of aerosols. If you wish to perform a complete atmospheric correction, please do not use the Corrected Reflectance algorithm. An additional difference is that the Land Surface Reflectance product is only tuned for calculating the reflectance over land surfaces. | ||
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References: [NASA Earthdata - Creating Reprojected True Color MODIS Images: A Tutorial](https://earthdata.nasa.gov/s3fs-public/2022-02/MODIS_True_Color.pdf); [NASA Earthdata - LANCE FAQ](https://earthdata.nasa.gov/faq/lance-faq#ed-CRvsSR) | ||
References: [NASA Earthdata - Creating Reprojected True Color MODIS Images: A Tutorial](https://earthdata.nasa.gov/s3fs-public/2022-02/MODIS_True_Color.pdf); [NASA Earthdata Forum - LANCE FAQ](https://forum.earthdata.nasa.gov/viewtopic.php?t=5203) | ||
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NOTE: We are reprocessing the entire MODIS Land imagery archive to collection 6.1 but currently the imagery is a mix of collection 6 and collection 6.1. Most of the imagery from mid-May 2021 onwards is collection 6.1 and older imagery is collection 6. |
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...adata/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 [doi:10.5067/AQUA/MODIS/L2/OC/2018](https://doi.org/10.5067/AQUA/MODIS/L2/OC/2018) | ||
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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...n/config/metadata/layers/modis/aqua/MODIS_Aqua_L3_SST_MidIR_4km_Night_Annual.md
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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 annual. | ||
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References: MODIS_AQUA_L3_SST_MID-IR_ANNUAL_4KM_NIGHTTIME_V2019.0 [doi:10.5067/MODAM-AN4N9](https://doi.org/10.5067/MODAM-AN4N9); 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_ANNUAL_4KM_NIGHTTIME_V2019.0 [doi:10.5067/MODAM-AN4N9](https://doi.org/10.5067/MODAM-AN4N9); Details of the [algorithm](https://oceancolor.gsfc.nasa.gov/resources/atbd/sst4/) can be found at Ocean Biology Processing Group (OBPG/OB.DAAC) website. | ||
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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). |
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