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Generation of TOA Radiative Fluxes from the Geostationary Earth Radiation Budget (GERB) Instrument Data I) Methods. Steven Dewitte and GERB team Royal Meteorological Institute of Belgium EUMETSAT users conference – Weimar - September 2003. Meteosat Second Generation. SEVIRI
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Generation of TOA Radiative Fluxes from the Geostationary Earth Radiation Budget (GERB) Instrument DataI) Methods Steven Dewitte and GERB team Royal Meteorological Institute of Belgium EUMETSAT users conference – Weimar - September 2003
Meteosat Second Generation SEVIRI Spinning Enhanced Visible and InfraRed Imager GERB Geostationary Earth Radiation Budget
Overview • The GERB measurements • Validation of GERB radiances • GERB/SEVIRI synergy • Conclusions
The GERB measurements • 2 channel radiometer: shortwave and total • 1 pair of images in 5’. shortwave total
Radiances Measured: radiances filtered by spectral response • LTOT,LSW Calculated: longwave radiance • LLW = LTOT -A LSW Wanted: unfiltered radiances • Lsol = reflected solar radiance • Lth = emitted thermal radiance
GERB radiance validation • comparison with Clouds and the Earth’s Radiant Energy System (CERES) measurements • CERES on TERRA in flight since 2000 • special CERES mode : Rotating Azimuth Plane Scan (RAPS) allows co-angular views with all GERB detectors
95% confidence intervals • Reflected solar radiance:GERB/CERES=0.990 +/- 0.017 =[0.974 - 1.007]target uncertainty = 2*0.01 = 0.02 -> OK ! • Emitted thermal radiance:GERB/CERES=0.982 +/- 0.016 =[0.966 - 0.998] target uncertainty = 2*0.005 = 0.01 -> OK
GERB/SEVIRI synergy GERB derived spectral correction factor for SEVIRI based flux estimate SEVIRI derived unfilter factor for GERB measurement SEVIRI derived unfilter and angular conversion factor for GERB measurement
Conclusions • The GERB instrument performs well in space. • The GERB broadband radiances have been validated by comparison with CERES. • Next step: validate GERB fluxes.