Airborne ocean backscatter measurements at C and Ku band wavelengths obtained in low to moderate‐wind conditions are presented. The differences between the low‐wind backscatter data and the CMOD4 and SASS‐II models are reported. The measurements show that the upwind/crosswind backscatter ratio is greater than predicted. These large upwind/crosswind backscatter ratios are attributed to a rapid decrease in the crosswind backscatter at low winds. Qualitative agreement with the composite surface model proposed by Donelan and Pierson suggests the rapid decrease in the crosswind backscatter may be caused by viscous dampening of the Bragg‐resonant capillary‐gravity waves. We show that for larger antenna footprints typical of satellite‐based scatterometers, the variability in the observed wind field smooths out the backscatter response such that the rapid decrease in the crosswind direction is not observed.
