Oceanic waves have been found to contribute enhanced backscattering in the
direction of the illumination source in studies that assumed the ocean surf
ace to be a random sum of waves. Here we investigate enhanced back-scatteri
ng by coherent capillary-gravity wave trains that coexist near the crests o
f short gravity waves in the ocean. We find that the enhanced back-scatteri
ng effect is intensified relative to that of a random surface and that the
effect is observed at larger angles. This effect may not only affect active
sensors such as lidar, which have a viewing angle close to that of the sou
rce but possibly passive sensors as well. This effect is likely to result i
n biases when attempting closure between radiative transfer models that do
not include realistic representation of the ocean surface and observed wate
r leaving radiance. (C) 2001 Optical Society of America.