3rimg_l2b_sst

Sea Surface Temperature is derived from Split Thermal Window Channels (TIR1, Tir2) DURING DURING DURING DURING DURING DURING DURING DURING IR Wind IR Window Channel (MIR) DURING NIGHT TIME OORE CLOUD FREE OORE CHE The most important part of the sst retrieval from IR observations is the atmospheric correction, especially over tropics. This correction is determined through a suitable characterization of tropical atmospheres in radiative transfer model to simulate the brightness temperature of insat-3dr channels a

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