During the joint U.K./U.S.A. experiment conducted in the Loch Linnhe,
Scotland, U.K., in 1989, the Jet Propulsion Laboratory (JPL) multifreq
uency airborne synthetic aperture radar (SAR) was deployed to investig
ate the relation between the SAR images and ship-generated internal wa
ves. One of the intriguing results, consistent throughout the experime
nt, was the striking difference in phase (position) between the images
of internal wave wakes in the P-band (similar or equal to 68 cm) wave
length and those in L-band (similar or equal to 24 cm) and C-band (sim
ilar or equal to 6 cm) wavelengths. An explanation for this difference
is found in the sensitivity of different radar wavelengths to oceanic
surface waves in different ranges of wavelengths, that are perturbed
by varying surface currents by different amounts and at different posi
tions, depending on the wavelength of surface waves.