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Numerical Simulation of Whitecaps and Foam Effects on Satellite Altimeter Response
2014
Remote Sensing
The determination of wave height by active satellite remote sensing, be it Synthetic Aperture Radar (SAR) or altimeter, has been a common practice for many years and is now imbedded on many meteorological and oceanographic forecasting systems. Despite their differences, all active sensors are based on the measurement of the Normalized Radar Cross Section (NRCS) of the sea surface, i.e., of its backscattering properties, which in turn depend on the wind velocity. At small and moderate wind
doi:10.3390/rs6053681
fatcat:ioyr6b7rkbda7kkojdcoekegbi