Ku-band backscatter from the Cowlitz River: Bragg scattering with and without rain

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.

[1]  Christophe Craeye,et al.  Rain generated ring-waves: Measurements and modelling for remote sensing , 1997 .

[2]  Christophe Craeye,et al.  Ring-waves generated by water drops impacting on water surfaces at rest , 1999 .

[3]  William J. Plant,et al.  The dependence of microwave backscatter from the sea on illuminated area: Correlation times and lengths , 1994 .

[4]  James C. West,et al.  Two-scale treatment of low-grazing-angle scattering from spilling breaker water waves , 2002 .

[5]  David Atlas,et al.  Footprints of storms on the sea: A view from spaceborne synthetic aperture radar , 1994 .

[6]  W. Plant A stochastic, multiscale model of microwave backscatter from the ocean , 2002 .

[7]  M. Gade,et al.  Investigation of multifrequency/multipolarization radar signatures of rain cells over the ocean using SIR‐C/X‐SAR data , 1998 .

[8]  William J. Plant,et al.  Bound waves and bragg scattering in a wind-wave tank , 1999 .

[9]  K. L. Beach,et al.  What are the mechanisms for non‐Bragg scattering from water wave surfaces? , 1999 .

[10]  Martin Gade,et al.  Radar backscattering measurements of artificial rain impinging on a water surface at different wind speeds , 1999, IEEE 1999 International Geoscience and Remote Sensing Symposium. IGARSS'99 (Cat. No.99CH36293).

[11]  William J. Plant,et al.  A model for microwave Doppler sea return at high incidence angles: Bragg scattering from bound, tilted waves , 1997 .

[12]  Christophe Craeye,et al.  Drop size effects on rain-generated ring-waves with a view to remote sensing applications , 2002 .

[13]  William J. Plant,et al.  Effects of rain on Ku‐band backscatter from the ocean , 2003 .

[14]  William J. Plant,et al.  Microwave sea return at moderate to high incidence angles , 2003 .

[15]  William J. Plant,et al.  A new interpretation of sea-surface slope probability density functions , 2003 .

[16]  William J. Plant,et al.  measuring stream discharge by non‐contact methods: A Proof‐of‐Concept Experiment , 2000 .

[17]  J. P. Hansen Rain backscatter tests dispel old theories , 1986 .

[18]  Murray J. Smith,et al.  Doppler radar backscatter from ring waves , 1998 .

[19]  C. Craeye,et al.  Scatterometric signatures of multivariate drop impacts on fresh and salt water surfaces , 1999 .