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Titlebook: Breaking Waves; IUTAM Symposium Sydn Michael L. Banner,Roger H. J. Grimshaw Conference proceedings 1992 Springer-Verlag, Berlin Heidelberg

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期刊全称Breaking Waves
期刊简称IUTAM Symposium Sydn
影响因子2023Michael L. Banner,Roger H. J. Grimshaw
视频video
学科分类IUTAM Symposia
图书封面Titlebook: Breaking Waves; IUTAM Symposium Sydn Michael L. Banner,Roger H. J. Grimshaw Conference proceedings 1992 Springer-Verlag, Berlin Heidelberg
影响因子Wave breaking is a commonly occurring phenomena associated with wave motion in fluids, often inducing significant effects which are of fundamental and technological importance, A familiar illustration is provided with white-capping and microbreaking of the wind-driven ocean sUrface waves, which is believed to play an important part in the transfers of momentum, mass and heat across the air-sea interface, as well as in the production of underwater ambient noise and augmented microwave backscatter. The enhanced hydrodynamic forces associated with the breaking of the more energetic ocean wave components constitute a significant challenge in ocean engineering, coastal engineering and naval architecture. Other less conspicuous but equally important manifestations are the breaking of internal waves and the fila mentation of vorticity interfaces. Despite recent theoretical and observational progress towards a more complete understanding of wave breaking, mathematical descriptions of its onset and consequences are presently lacking. The aim of this Symposium was to bring together theoretical and observational expertise, with the goal of determining the current state of knowledge of wave br
Pindex Conference proceedings 1992
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Capillary Rollers and Boresme phase speed. The dynamical theory of the generation of parasitic capillaries has been developed by Longuet-Higgins (1963), Crapper (1970) and Ruvinsky et al. (1981, 1985, 1991). This so far takes into account only the first-order effects of viscous damping.
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Effect of Breaking Waves on the Transport of Heat and Vapor Fluxes from the Oceanstent heat from the ocean. Field data reduced by the present model gives highly consistent results. During high-sea states, the vertical energy flux from the ocean was found to be more than four times larger than the existing formulation, in which the effect of water droplets was not taken into consideration.
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