C. Melsheimer et al., IMAGING OF OCEAN WAVES ON BOTH SIDES OF AN ATMOSPHERIC FRONT BY THE SIR-C X-SAR MULTIFREQUENCY SYNTHETIC-APERTURE RADAR/, J GEO RES-O, 103(C9), 1998, pp. 18839-18849
Radar images of an ocean scene containing an atmospheric front and alm
ost range-propagating ocean waves which were acquired by the multifreq
uency/multipolarization synthetic aperture radar (SAR) aboard the spac
e shuttle Endeavour during the spaceborne imaging radar-C/X-band synth
etic aperture radar (SIR-C/X-SAR) mission over the North Atlantic in 1
994 are analyzed. The L-band SAR image spectra calculated from two are
as located on opposite sides of the atmospheric front age quite simila
r, whereas the corresponding X- and C-band SAR image spectra differ si
gnificantly. It is shown that this is, a consequence of the SAR imagin
g mechanism; at L band the SAR imaging mechanism depends weakly on the
local wind field, and at X and C band it depends strongly on the loca
l wind field. This is in agreement with earlier results obtained from
the analysis of airborne multifrequency/multipolarization SAR images a
cquired over the North Sea during the SAR and X-Band Ocean Nonlinearit
ies - Forschungsplattform Nordsee (SAXON-FPN) experiment. In this inve
stigation it was found that at X and C band the phase of the real aper
ture radar modulation transfer function (RAR MTF) changes by almost 90
degrees, when in the reference system moving with the group velocity
of the dominant wave, the component of the wind velocity in the direct
ion of the wave propagation changes sign. However, at L band such a ch
ange in local wind direction affects the phase of the RAR MTF only sli
ghtly. Using this phase behavior of the RAR MTF in simulations of the
SIR-C/X-SAR image spectra, we show that the observed differences of th
e X- and C-band SAR image spectra measured on both sides of the atmosp
heric front are consistent with a change in wind speed and direction a
cross the front. From this we conclude that for inverting X- or C-band
SAR image spectra into ocean wave spectra that contain ocean waves pr
opagating near the range direction, it is quite important to have a go
od knowledge of the local wind field, whereas for L-band SAR image spe
ctra this is of minor importance.