Analysis of geophysical model functions from three radar bands shows nonmonotonic wind-speed dependence in directional roughness parameters and derives a similarity relationship requiring both upwind-downwind and upwind-crosswind terms for accurate backscattering models.
The elevation, slope, and curvature spectra of a wind roughened sea surface
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Directional Distribution of Ocean Surface Roughness Observed in Microwave Radar Backscattering
Analysis of geophysical model functions from three radar bands shows nonmonotonic wind-speed dependence in directional roughness parameters and derives a similarity relationship requiring both upwind-downwind and upwind-crosswind terms for accurate backscattering models.