The Ku-band dual-polarized backscatter signatures of ocean surfaces are des
cribed in this paper with the airborne scatterometer measurements collected
in the Hurricane Ocean Wind Experiment:in September 1997, The data collect
ed from flights over:Hurricane Erika provide a direct evidence that there a
re wind direction signals in the vertically and horizontally polarized Ku-b
and backscatter of ocean surfaces under the influence of hurricane-force wi
nds. At 46 degrees incidence angle, the vertically polarized backscatter ac
quired at the upwind direction increases by about I dB as the wind speed in
creases from 22 m.s(-1) to 35 m.s(-1), while the horizontally polarized bac
kscatter appears to he twice as sensitive with a change of about 2 dB. At 3
5 m.s(-1) wind speeds, the difference between upwind and crosswind observat
ions of vertically polarized backscatter is about 1.5 dB, smaller than the
2 dB difference for the horizontally polarized backscatter. This demonstrat
es that the horizontal polarization has a greater sensitivity to wind speed
and direction than the vertical polarization in the high wind regime. The
data also suggest that the upwind and downwind asymmetry of Ku-band backsca
tter decreases with increasing wind speed and can fall below 0 dB at small
incidence-angles (<35 degrees) for the vertical polarization. A combined in
teraction of the geometric optics scattering and the short wave modulation
by long waves is proposed to interpret this phenomenonn and appears to agre
e with the dependence of the signature on incidence, wind speed, and polari
zation. The aircraft flight data-support the feasibility of dual-polarized
Ku-band radar for hurricane ocean wind measurements, although the data do s
uggest a reduced wind speed and direction sensitivity in the high wind regi
me. Also, the differing polarization backscatter signatures suggest the rel
ative contributions of various surface scattering mechanisms. An improved K
u-band GMF is described.