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Titlebook: Air-Sea Exchange: Physics, Chemistry and Dynamics; G. L. Geernaert Book 1999 Springer Science+Business Media Dordrecht 1999 Coast.Ocean.at

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期刊全稱Air-Sea Exchange: Physics, Chemistry and Dynamics
影響因子2023G. L. Geernaert
視頻videohttp://file.papertrans.cn/152/151863/151863.mp4
學(xué)科分類Atmospheric and Oceanographic Sciences Library
圖書封面Titlebook: Air-Sea Exchange: Physics, Chemistry and Dynamics;  G. L. Geernaert Book 1999 Springer Science+Business Media Dordrecht 1999 Coast.Ocean.at
影響因子During the 1980‘s a wealth of information was reported from field and laboratory experiments in order to validate andlor modify various aspects of the surface layer Monin-Obukhov (M-O) similarity theory for use over the sea, and to introduce and test new concepts related to high resolution flux magnitudes and variabilities. For example, data from various field experiments conducted on the North Sea, Lake Ontario, and the Atlantic experiments, among others, yielded information on the dependence of the flux coefficients on wave state. In all field projects, the usual criteria for satisfying M-O similarity were applied. The assumptions of stationarity and homogeneity was assumed to be relevant over both small and large scales. In addition, the properties of the outer layer were assumed to be "correlated" with properties of the surface layer. These assumptions generally required that data were averaged for spatial footprints representing scales greater than 25 km (or typically 30 minutes or longer for typical windspeeds). While more and more data became available over the years, and the technology applied was more reliable, robust, and durable, the flux coefficients and other turbulent
Pindex Book 1999
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Effect of Surface Gravity Waves on Near-Surface Atmospheric Turbulence,nduced pressure component is far from satisfactory because very little is known about the structure of the wavw-induced flow in the atmospheric surface layer or how this flow affects the structure of the surface-layer turbulence.
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Engineering Spectra Over Water,l on deep waters are sensitive to slow variation in the direction of the wind. Thus various engineering structures are sensitive to various components of wind fluctuations at a wide range of frequencies and also to the spatial correlations of these fluctuations.
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