Titlebook: Breaking Ocean Waves; Geometry, Structure Eugene A. Sharkov Book 2007 Springer-Verlag Berlin Heidelberg 2007 Air-sea interactions on sea s

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SEVER

,Spatial stochastic breaking wave fields in the atmosphere—ocean system, techniques and instruments for optically surveying a disturbed sea surface are diverse: both small-scale surveys from ships, and large-scale ones from air- and space-based carriers. The experimental data, obtained as a result of ship-based investigations, possess some natural limitations (spatial l

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The lifetime dynamics of sea wave breakings,ng. Investigations have taken various directions—namely, spatiotemporal estimations of breaking parameters using dimensional considerations (Phillips, 1977); simplified numerical models (Vinje and Brevig, 1981; Krasilnikov, 1987); wave breaking, carried out under laboratory conditions, which certain

Surgeon

The drop-spray phase over a rough sea surface,breaking of steep crests of wind gravity waves. However, this generally trivial conclusion is far removed from understanding what actually is the physical mechanism involved in production and separation of drops from the water surface. This process, widely used in technological facilities and called

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induct

蚊子

,Field optical—microwave remote sensing of the air—sea transition zone in the atmosphere—ocean systetion and a rough sea surface. In spite of the fact that investigations over the last 25–30 years have demonstrated, in general, the validity of the two-scale radiophysical scattering model for signals with vertical polarization (in transmission-reception mode) (Moor and Fung, 1979; Alpers and Hassel

用樹(shù)皮

Conclusions,ical remote diagnostics of a rough sea surface when the single-boundedness of the surface is broken and when an intermediate density zone arises, which represents a polydisperse mixture of finite volumes of air and water with highly fluctuating (in space and time) transition characteristics.

白楊

https://doi.org/10.1057/9780230250772ical remote diagnostics of a rough sea surface when the single-boundedness of the surface is broken and when an intermediate density zone arises, which represents a polydisperse mixture of finite volumes of air and water with highly fluctuating (in space and time) transition characteristics.