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.
An empirical investigation of source term balance of small scale surface waves,
2 Pith papers cite this work. Polarity classification is still indexing.
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Wind-wave spectra in the cmDm range exhibit variable slopes indicating nonequilibrium conditions, quantified via LPMSS data combined with a variable-slope spectrum model.
citing papers explorer
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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.
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Variable Spectral Slope and Nonequilibrium Surface Wave Spectrum
Wind-wave spectra in the cmDm range exhibit variable slopes indicating nonequilibrium conditions, quantified via LPMSS data combined with a variable-slope spectrum model.