Abstract

Ku-band backscatter from the Cowlitz River in southwestern Washington State was measured for incidence angles from 0/spl deg/ to 80/spl deg/. The measurements were made for light-wind conditions with and without rain. In rain-free conditions, Bragg scattering was the dominant scattering mechanism for both HH and VV polarizations out to 75/spl deg/, beyond which the signal-noise-ratio dropped very low at HH. When a light rain was falling on the river, the cross section increased substantially at moderate incidence angles. Doppler spectra taken during rain showed that VV polarized backscatter is primarily from Bragg scattering from ring waves while HH polarization scatters from both ring waves and stationary splash products, depending on the incidence angle. Finally, the effect of hail on the magnitude and spectral properties of backscatter was observed.

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