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Drastically different sea states result for a growing, decaying, or a fully-developed sea due to the presence of a wind field. In addition, the sea state is altered by the superposition of oceanic currents on the wave field created by the wind. This study presents a numerical analysis of the change in the sea surface brightness temperature at L-band computed using the SSA model and a modified Kitaigorodskii-Pierson-Moskowitz...
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