Radar scattering from modulated wind waves: proceedings of the Workshop on Modulation of Short Wind Waves in the Gravity-Capillary Range by Non-Uniform Currents


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Date added 2019-04-21
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Author G J Komen, W A Oost
Language English
ISBN 0792301463 9780792301462
Genre Conference papers and proceedings, Congresses
Available formats PDF, fb2, ePub, mobi, RTF, Doc, txt, LRF, AZW, DJVU

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Radar Scattering from Modulated Wind Waves. G.J. Komen,W.A. Oost — 2012-12-06 Science. Proceedings of the Workshop on Modulation of Short Wind Waves in the Gravity-Capillary Range by Non-Uniform Currents, held in Bergen aan Zee, The Netherlands, 24–26 May 1988.

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Workshop on Modulation of Short Wind Waves in the Gravity-Capillary Range by Non-Uniform Currents. & Komen, G. J. & Oost, W. A. (1989). Radar scattering from modulated wind waves : proceedings of the Workshop on Modulation of Short Wind Waves in the Gravity-Capillary Range by Non-Uniform Currents.

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Radar signal characteristics - Wikipedia

en.wikipedia.org/wiki/Radar_signal_characteristics

Carrier. The carrier is an RF signal, typically of microwave frequencies, which is usually (but not always) modulated to allow the system to capture the required data. In simple ranging radars, the carrier will be pulse modulated and in continuous wave systems, such as Doppler radar, modulation may not be required.Most systems use pulse modulation, with or without other supplementary ...

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Description. Proceedings of the Workshop on Modulation of Short Wind Waves in the Gravity-Capillary Range by Non-Uniform Currents, held in Bergen aan Zee, The Netherlands, May 24-26, 1988 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.

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During this workshop several models were presented to explain the modulation of short wind waves by non-uniform currents. For details on these models, see the contributions by Alpers, Thompson, Thomas & Edwards and Gastel. All models can be seen as limiting cases of the complete energy balance.

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Wave radar - Wikipedia

en.wikipedia.org/wiki/Wave_radar

The radar echo is generated by Bragg scattering, hence wind generated surface ripple (capillary waves) must be present. The backscattered signal will be modulated by the large surface gravity waves and the gravity wave information is derived from the modulation of the backscattered signal.

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