Abstract
Based on the microwave radiative transfer theory, this thesis simulates the brightness temperature measured by Microwave Radiation Imager(MWRI) flown aboard Chinese FY-3B meteorological satellite, a new semi-statistical model for the development of the inversion algorithm is established through comparison of the simulated results with the simultaneous satellite measurements, and the MWRI five channels are log-linearly combined to inverse the real-time sea surface wind speeds under conditions of no precipitation. The results are compared to the ocean buoy measurements during June to August in 2011, shows small differences.
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