Scattering experiments from breaking gravity waves conducted at a wave
tank facility at small grazing angles in the absence of wind are anal
yzed, Breaking gravity waves are studied using a fully plane polarimet
ric horizontal (HH), vertical (VV), vertically transmitted and horizon
tally received polarization (VH), and horizontally transmitted and ver
tically received polarization (HV) pulse-chirped X-band radar in conju
nction with optical instruments: the plane polarimetric optical specul
ar event detector (OSED) and side-looking camera(SLC), Spatially and t
emporally resolved radar backscatter has been measured and temporally
correlated to the data obtained from the optical diagnostics. The expe
riments yield the following results: 1) enhanced scattering compared t
o Bragg scattering levels occurs throughout the evolutionary process o
f wave-breaking, i.e., the radar scatters strongly from both the unbro
ken and broken surfaces; 2) an explanation is found for the observatio
n that the scatterer Doppler frequency is slightly less than the Doppl
er frequency corresponding to the fundamental wave phase speed; 3) a r
epresentative non-Bragg cross section of a breaking wave can be obtain
ed; and 4) a breaking wave surface is found to be an efficient depolar
izer.