DocumentCode :
1485077
Title :
Free and bound capillary waves as microwave scatterers: laboratory studies
Author :
Rozenberg, Anatol D. ; Ritter, Michael J. ; Melville, W. Kendall ; Gottschall, Christopher C. ; Smirnov, Andre V.
Author_Institution :
Scripps Inst. of Oceanogr., California Univ., San Diego, La Jolla, CA, USA
Volume :
37
Issue :
2
fYear :
1999
fDate :
3/1/1999 12:00:00 AM
Firstpage :
1052
Lastpage :
1065
Abstract :
Laboratory measurements of the fine space-time structure of short gravity-capillary waves, as well as Ku-band scattering at grazing and moderate incidence from wind waves in the large Delft Hydraulics Laboratory wind-wave channel are presented. This study was stimulated by the need to verify the processes that significantly contribute to scattering at grazing and moderate incidence. A scanning laser slope gauge was used for measuring capillary waves from 2-mm to 2-cm wavelengths and frequencies ranging up to 100 Hz. A dual-polarized (vertical, VV, and horizontal, HH), coherent, pulsed Ku-band scatterometer with good temporal resolution (3 ns) was used to obtain simultaneous Doppler spectra and the absolute cross section of scattered signals for grazing angles 6 and 25° and for winds in the range 2.5-12.5 m/s. Two-dimensional (2D) filtering and bispectral analyses were used to separate and study the influence of free and bound surface waves. The results of this study demonstrate that the frequency-wavenumber spectra of capillary waves consist of two parts. The first corresponds to free capillary waves, which satisfy the dispersion relationship. The second corresponds to bound parasitic capillary waves, which are located near the crests of steep wind waves. The phase velocity of these capillary waves is approximately equal to the phase velocity of the steep waves. Measurements of the Doppler frequency of the scattered signals show that the Doppler spectra also have a bimodal structure. While the first low-frequency part of the spectrum corresponds to the Bragg scattering from the free capillary waves, the highfrequency part is associated with Bragg scattering from the bound capillary waves on the crests of the steep waves. This type of scattering is predominant for the upwind direction of illumination (especially for HH-polarization)
Keywords :
backscatter; capillary waves; ocean waves; oceanographic techniques; radar cross-sections; remote sensing by radar; 2 mm to 2 cm; Ku-band; SHF; backscatter; bound capillary wave; bound surface wave; capillary wave; free capillary wave; free surface wave; frequency-wavenumber spectra; gravity-capillary wave; grazing incidence; measurement technique; microwave scatterer; moderate incidence; ocean wave; radar remote sensing; radar scattering; sea surface; Frequency measurement; Laboratories; Laser modes; Optical pulses; Pulse measurements; Radar measurements; Scattering; Signal resolution; Spaceborne radar; Wavelength measurement;
fLanguage :
English
Journal_Title :
Geoscience and Remote Sensing, IEEE Transactions on
Publisher :
ieee
ISSN :
0196-2892
Type :
jour
DOI :
10.1109/36.752223
Filename :
752223
Link To Document :
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