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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能量守恒

SAR Imaging of Ocean Waves in the Presence of Variable Currentsnear forcing (input from the wind, energy transfer by resonant nonlinear interactions, and dissipation) is given. Since many of the pertinent processes are quite complex and are areas of active research even today, the review is made as comprehensive as possible, but brief enough so as to bring the

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white-matter

Measurement of Short Wave Modulation by Long Waves Using Stereophotography and a Laser-Slope Sensor th the relaxation model introduced by Keller and Wright (1975). A comparison with the modulation transfer function obtained with a tower-based L-Band radar indicates that hydrodynamic modulation is only a fraction of the total modulation. The conclusion arrived at in this paper is that the mechanism

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The Surface Signatures of Internal Waves in the Ocean: Introduction and SystematicsThe emphasis initially was on surface currents induced by internal waves but the techniques involved are sufficiently general for them to apply to any current which can be represented satisfactorily by piecewise linear segmentation over the straining region. Thus tidal flows over bathymetric feature

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exclusice

The Modulation Transfer Function: Concept and Applicationsd to surface tilting and changes in range. The manner in which the modulation transfer function enters into the interpretation of real and synthetic aperture radar images, wave spectrometer outputs, scatterometer wind retrievals, and altimeter measurements is reviewed. Finally, limitations of the concept are discussed.

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CORE

The Surface Signatures of Internal Waves in the Ocean: Introduction and Systematics current which can be represented satisfactorily by piecewise linear segmentation over the straining region. Thus tidal flows over bathymetric features such as ridges and gulleys can be accommodated. The modelling is currently being extended to apply to shearing currents for comparison with observations of fronts and eddies.

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