GPS signal scattering from sea surface: Wind speed retrieval using experimental data and theoretical model

Global Positioning System (GPS) signals reflected from the ocean surface have potential use for various remote sensing purposes. Some possibilities are measurements of surface roughness characteristics from which wave height, wind speed, and direction could be determined. For this paper; GPS-reflected signal measurements collected at aircraft altitudes of 2 km to 5 km with delay-Doppler mapping GPS receiver are used to explore the possibility of determining wind speed. To interpret the GPS data, a theoretical model has been developed that describes the power. of the reflected CPS signals for different time delays and Doppler frequencies as a function of geometrical and environmental parameters. The results indicate a good agreement between the measured and the modeled normalized signal power waveforms during changing surface wind conditions. The estimated rr,ind spc en using surface-reflected GPS data, obtained by comparing actual and modeled waveforms, shows good ;agreement (within 2 m/s) with delta obtained from a nearby buoy and independent wind speed measurements derived from the TOPEX/Poseidon altimetric satellite. (C)Elsevier Science Inc., 2000.