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L band radar backscatter dependence upon surface wind stress - A summary of new Seasat-1 and aircraft observationsThe wind-scale relationships for L band radar wavelengths near 25 cm and 20 deg angle of incidence and HH polarization are reviewed using a number of aircraft and Seasat-1 SAR observations. The dependence of the L band backscatter coefficient from the ocean upon surface wind speed and direction is stated. The wind speed coefficient is 0.5 + or - 0.1 for a wide range of wind speeds. The wind direction coefficient is near zero for lower winds and stable marine boundary layers, but may be 0.20 + or - 0.05 for moderate wind speeds and an unstable marine boundary layer. These results are interpreted in terms of existing theoretical models for radar scattering from the ocean.
Document ID
19830043080
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Thompson, T. W.
(California Institute of Technology, Jet Propulsion Laboratory, Telecommunications Science and Engineering Div.; Science Applications, Inc. Pasadena, CA, United States)
Weissman, D. E.
(Hofstra University Hempstead, NY, United States)
Gonzalez, F. I.
(NOAA, Marine Environment Laboratory, Seattle WA, United States)
Date Acquired
August 11, 2013
Publication Date
February 28, 1983
Publication Information
Publication: Journal of Geophysical Research
Volume: 88
Subject Category
Oceanography
Accession Number
83A24298
Distribution Limits
Public
Copyright
Other

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