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Observations of Sea Surface Mean Square Slope During the Southern Ocean Waves ExperimentFor the Southern Ocean Waves Experiment (SOWEX), conducted in June 1992 out of Hobart, Tasmania, the NASA Scanning Radar Altimeter (SRA) was shipped to Australia and installed on a CSIRO Fokker F-27 research aircraft instrumented to make comprehensive surface layer measurements of air-sea interaction fluxes. The SRA sweeps a radar beam of P (two-way) half-power width across the aircraft ground track over a swath equal to 0.8 of the aircraft height, simultaneously measuring the backscattered power at its 36 GHz (8.3 mm) operating frequency and the range to the sea surface at 64 cross-track positions. In realtime, the slant ranges are multiplied by the cosine of the off-nadir incidence angles (including the effect of aircraft roll attitude) to determine the vertical distances from the aircraft to the sea surface. These distances are subtracted from the aircraft height to produce a sea-surface elevation map, which is displayed on a monitor in the aircraft to enable real-time assessments of data quality and wave properties. The sea surface mean square slope (mss), which is predominantly caused by the short waves, was determined from the backscattered power falloff with incidence angle measured by the SRA in the plane normal to the aircraft heading. On each flight, data were acquired at 240 m altitude while the aircraft was in a 7 degree roll attitude, interrogating off-nadir incidence angles from -15 degrees through nadir to +29 degrees. The aircraft turned azimuthally through 810 degrees in this attitude, mapping the azimuthal dependence of the backscattered power falloff with incidence angle. Two sets of turning data were acquired on each day, before and after the aircraft measured wind stress at low altitude (12 meters to 65 meters). Wave topography and backscattered power for mss were also acquired during those level flight segments whenever the aircraft altitude was above the SRA minimum range of 35 m. Data were collected over a wide range of wind and sea conditions, from quiescent to gale force winds with 9 meter wave height.
Document ID
20020022887
Acquisition Source
Goddard Space Flight Center
Document Type
Conference Paper
Authors
Walsh, E. J.
(NASA Goddard Space Flight Center Greenbelt, MD United States)
Vandemark, D. C.
(NASA Goddard Space Flight Center Greenbelt, MD United States)
Wright, C. W.
(NASA Goddard Space Flight Center Greenbelt, MD United States)
Banner, M. L.
(New South Wales Univ. Sydney, Australia)
Chen, W.
(New South Wales Univ. Sydney, Australia)
Swift, R. N.
(EG and G, Inc. Wallops Island, VA United States)
Scott, J. F.
(EG and G, Inc. Wallops Island, VA United States)
Hines, D. E.
(EG and G, Inc. Wallops Island, VA United States)
Jensen, J.
(Commonwealth Scientific and Industrial Research Organization Aspendale, Australia)
Lee, S.
(Commonwealth Scientific and Industrial Research Organization Aspendale, Australia)
Gerlach, John C.
Date Acquired
August 20, 2013
Publication Date
January 1, 2001
Subject Category
Oceanography
Meeting Information
Meeting: IGARSS 2001
Location: Sydney
Country: Australia
Start Date: July 9, 2001
End Date: July 13, 2001
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.

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