Hourly Downward Longwave Irradiance - GOES

Description

Estimation of the Downward Longwave Irradiance reaching the Earth surface, derived from the geostationary satellite GOES-E, produced by remapping over a 0.05° regular grid and expressed in W/m2. Algorithm is a bulk parameterization that uses NWP model outputs to calculate a clear sky Downward Longwave Irradiance (DLI), corrected according to satellite derived cloud information. An essential point is the calculation of products interpolated at rounded UT hours. A radiative flux calculated on a satellite image is not homogeneous in time (the pixel time varies from north to south, of about 24 minutes for GOES-E data).

Resources

Name Format Description Link
0 https://eoportal.eumetsat.int/userMgmt/protected/dataCentre.faces?acronym=OSIHDLI&satellite=GOES-09,GOES-10,GOES-11,GOES-12,GOES-13,GOES-14,GOES-15,GOES-16&id=EO:EUM:DAT:GOES:OSIHDLI

Tags

  • ocean
  • radiation

Topics

  • ENVI

Categories