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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https://doi.org/10.1057/9780230250772e wind, as well as intensive near-surface thermal convection, causes the appearance of an aerodisperse high-velocity medium over the sea surface, the parameters of the medium highly fluctuating both in particle concentration and spectrum, and in its turbulence (see Chapter 5 and Plate 2 in the Preli

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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.

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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.

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Burkhard Schwenker,Stefan B?tzelle) to be obtained, which is required for detailed analysis of foam structures. Analysis of the possibilities of the means of remote sensing required for experimental solution of these problems has led us to the conclusion of the expediency of using two types of optical surveying: the large-scale, m

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