IMOS - Satellite Remote Sensing - NOAA20 - 01 day - Diffuse attenuation coefficient (k490)
The NOAA20 satellite platform carries a VIIRS sensor that observes sunlight reflected from within the ocean surface layer at multiple wavelengths. These multi-spectral measurements are used to infer the diffuse attenuation coefficient (Kd) at 490nm wavelength which provides information on how light is attenuated in the water column. It is defined as the scaling length of the exponential decrease of the downwelling irradiance, and has units (m^-1). The VIIRS K490 product estimates Kd at 490nm wavelength, using a semi-empirical model based on the ratio of water leaving radiances at 490nm and 555nm. The algorithm is described at https://oceancolor.gsfc.nasa.gov/atbd/kd/.
Data and resources
-
HTML Open
-
HTML Open
-
SRS - K490 - WMS layerHTML Open
-
The GoGoDuck subsets and aggregates gridded data. Data is returned as a NetCDF file.HTML Open
-
HTML Open
-
HTML Open
-
HTML Open
-
HTML Open
-
License GraphicPNG Open
-
HTML Open
Additional information
| Temporal extent | 2022-05-21 – ongoing |
|---|---|
| Date (creation) | 2025-02-07 |
| Status | onGoing |
| Update frequency | asNeeded |
| Metadata language | en |
| License | Data, products and services from IMOS are provided "as is" without any warranty as to fitness for a particular purpose. |
| Source metadata | ISO 19115 XML |
| Last updated | 2026-11-05 |
| Created | 2026-11-05 |
| API | package_show |