150 likes | 230 Views
USING SMOS POLARIMETRIC BRIGHTNESS TEMPERATURES TO CORRECT FOR ROUGH SURFACE EMISSION BEFORE SALINITY INVERSION. COMBINING HORIZONTALLY AND VERTICALLY POLARIZED BRIGHTNESS TEMPERATURES TO REMOVE SSS DEPENDENCE.
E N D
USING SMOS POLARIMETRIC BRIGHTNESS TEMPERATURES TO CORRECT FOR ROUGH SURFACE EMISSION BEFORE SALINITY INVERSION
COMBINING HORIZONTALLY AND VERTICALLY POLARIZED BRIGHTNESS TEMPERATURES TO REMOVE SSS DEPENDENCE
COMBINING HORIZONTALLY AND VERTICALLY POLARIZED BRIGHTNESS TEMPERATURES TO REMOVE SSS DEPENDENCE The relative sensitivities of horizontally and verticallypolarizedbrightnesstemperatures to changes in salinity and wind speed are differentat large incidence angles. Wewill exploit thisdifferenceto derive the windfrom a linearcombination of Th and Tv thatisinsensitive to salinity changes and then use thiswind to derivesalinityusing the first Stokes parameter.
IMPACT OF USING SMOS-DERIVED WIND SPEED 2011 mean surface windfieldfrom ECMWF modeling system
IMPACT OF USING SMOS-DERIVED WIND SPEED 2011 mean surface windfieldderivedfrom SMOS polarimetry. Wind speeds are lower by up to several m/s than ECMWF along the equator.
IMPACT OF USING SMOS-DERIVED WIND SPEED 2011 Retrieved SSS – Climatologyusing ECMWF 10-m wind speed Ascending Passes Only
IMPACT OF USING SMOS-DERIVED WIND SPEED 2011 Retrieved SSS – Climatologyusing SMOS-derivedwind speed Ascending Passes Only
IMPACT OF USING SMOS-DERIVED WIND SPEED 2011 mean surface windfieldfrom ECMWF modeling system
IMPACT OF USING SMOS-DERIVED WIND SPEED 2011 mean surface windfieldderivedfrom SMOS polarimetry. Wind speeds are lower by up to several m/s than ECMWF along the equator.
IMPACT OF USING SMOS-DERIVED WIND SPEED When ECMWF windisused to correct for rough surface emissiontoomuchbrightnessissubtracted, resulting in retrievedsalinitythatisbiased high.
IMPACT OF USING SMOS-DERIVED WIND SPEED This biasisremoved by using the wind speed derivedfrom SMOS brightnesstemperatures: