R. Sabia, D. Fernández-Prieto, M. Portabella, J. Gourrion, J. Font, M. Talone, Adriano Camps
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SMOS L3 salinity performances at decreasing sea surface temperature
A study of the latitudinal trend of the retrieved salinity performances along a Southwards transect has been performed, analyzing the trade-off between geophysical effects in cold seawater and the concomitant temporal oversampling under various processing configurations. Quantitative sensitivity with respect to sea surface temperature gradient has been evaluated.