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Автор Brucks, John T.
Автор Jones, W. Linwood
Автор Leming, Thomas D.
Дата выпуска 1980
dc.description Sea surface wind stress measurements recorded by a sonic anemometer are correlated with airborne scatterometer measurements of ocean roughness (cross section of radar backscatter) to establish the accuracy of remotely sensed data and assist in the definition of geophysical algorithms for the scatterometer sensor aboard Seasat A. Results of this investigation are as follows: (1) Comparison of scatterometer and sonic anemometer wind stress (u<sub>*</sub>) measurements are good for the majority of cases; however, a tendency exists for scatterometer u<sub>*</sub> to be somewhat high for higher wind conditions experienced in this experiment (6–9 m/s). (2) The scatterometer wind speed algorithm tends to overcompute the higher wind speeds by approximately 0.5 m/s. This is a direct result of the scatterometer overestimate of u<sub>*</sub>, from which wind speeds are derived. (3) Algorithmic derivations of wind speed and direction are, in most comparisons, within accuracies defined by Seasat A scatterometer sensor specifications.
Формат application.pdf
Копирайт This paper is not subject to U.S. copyright. Published in 1980 by the American Geophysical Union.
Тема West Coast Experiment and Marineland Experiment
Тема ELECTROMAGNETICS
Тема Electromagnetics: Radio oceanography
Название Comparison of surface wind stress measurements: Airborne radar scatterometer versus sonic anemometer
Тип article
DOI 10.1029/JC085iC09p04967
Electronic ISSN 2156-2202
Print ISSN 0148-0227
Журнал Journal of Geophysical Research: Oceans
Том 85
Первая страница 4967
Последняя страница 4976
Выпуск C9
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