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Titlebook: Radar Scattering from Modulated Wind Waves; Proceedings of the W G. J. Komen,W. A. Oost Conference proceedings 1989 Kluwer Academic Publish

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發(fā)表于 2025-3-21 19:02:04 | 只看該作者 |倒序瀏覽 |閱讀模式
書目名稱Radar Scattering from Modulated Wind Waves
副標題Proceedings of the W
編輯G. J. Komen,W. A. Oost
視頻videohttp://file.papertrans.cn/821/820394/820394.mp4
圖書封面Titlebook: Radar Scattering from Modulated Wind Waves; Proceedings of the W G. J. Komen,W. A. Oost Conference proceedings 1989 Kluwer Academic Publish
描述Ten years ago, de Loor and co-workers at TNO, The Netherlands, were the first to report bottom topography patterns in real aperture radar (RAR) images of the southern North Sea. At that time, this was a real puzzle. The skin depth of microwaves for sea water is only of the order of centimeters while the sea bottom is about 20 meters below the surface. Electromagnetic radiation therefore cannot probe the bottom directly. Similar phenomena were found in radar imagery from SEASAT and SIR-AlB synthetic aperture radars (SAR‘s) of Nantucket Shoals, the English Channel and many other coastal areas. Since then theory and ocean field experiments (Le., Phelps Bank, Georgia Straits, SARSEX, TOWARD, FASINEX, etc.) have advanced our understanding considerably. We now know that these surface signatures are the results of surface currents, perturbed by the bottom topography, which refract the propagation and modulate the energy of (short) surface waves so as to cause microwave backscatter power variations. Hence, any large scale ocean features containing nonuniform surface currents (i.e. internal waves, eddies, fronts, etc.) will cause similar manifestations in the radar imagery by means of curre
出版日期Conference proceedings 1989
關(guān)鍵詞Ocean; Scale; Wind speed; image processing; wind; remote sensing/photogrammetry
版次1
doihttps://doi.org/10.1007/978-94-009-2309-6
isbn_softcover978-94-010-7537-4
isbn_ebook978-94-009-2309-6
copyrightKluwer Academic Publishers 1989
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https://doi.org/10.1007/978-94-009-2309-6Ocean; Scale; Wind speed; image processing; wind; remote sensing/photogrammetry
板凳
發(fā)表于 2025-3-22 02:00:50 | 只看該作者
Studies of the Sea Surface with Radar in The Netherlands a Short HistoryA short survey is given of the studies of the sea with radar in the Netherlands. Topics of research are the study of waves, the radar backscatter, bathymetry, and internal waves.
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The Energy Balance in Short Gravity WavesEarlier results on the energy balance in gravity waves (Komen, Hasselmann and Hasselmann, 1985) are discussed. It is shown that these can be used to describe the evolution of short gravity waves, provided wind speeds are low enough. For higher wind speeds equilibrium range ideas are considered.
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AR) images of the southern North Sea. At that time, this was a real puzzle. The skin depth of microwaves for sea water is only of the order of centimeters while the sea bottom is about 20 meters below the surface. Electromagnetic radiation therefore cannot probe the bottom directly. Similar phenomen
8#
發(fā)表于 2025-3-22 22:26:27 | 只看該作者
Determining the Currents Over Phelps Bankd area model showed signs of instability that were damped out with a horizontal eddy viscosity. Agreement of this model with data from the one available current meter mooring was worse. Different options are available to go from model predictions to the currents necessary for calibration of microwave data obtained over Phelps Bank.
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Temporal and Spatial Variability of the Wind Stress Vectors concerned with shorter time or length scales, the variation of the stress vector according to phase of the long wave must be considered; such problems include the long wave phase dependent growth rates of short waves and wave/current interactions.
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