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

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Observations of the Enhancement of Kinetic Energy Dissipation Beneath Breaking Wind Wavesonal to the cube of the friction velocity .. and inversely proportional to depth, ∈αu...With a concomitant logarithmic velocity profile, this is consistent with a total kinetic energy flux from the wind of . . However, in fully rough flow and strongly forced waves the energy input may be one to two

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Microwave Backscattering from Laboratory Wind-Wave Surfaces and its Relation to Wave Breaking with Bnsity of the backscattered signature is in phase with the surface displacement. Variation of the Doppler velocity also corresponds to the phase of the individual waves. High Doppler velocity observed at the crests of the individual waves coincides with the propagating speed of the crests. It is conc

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LAP

2否定

Sound Production and Air Entrainment by Breaking Waves: A Review of Recent Laboratory Experimentscatter from individual breaking events are found to correlate with the important kinematic and dynamic properties of the breaking waves. Air entrainment measurements show that the bubble plume characteristics evolve as simple functions of time. A large fraction (30% to 50%) of the surface wave energ

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Wave Breaking in the Presence of Wind Drift and Opposed Swellopagating against the wind. It is shown that the growth of the wind waves is much intensified by swell propagating against the wind, when the swell steepness increases. This phenomenon shows clear contrast to the attenuation of the wind waves by swell propagating in the direction of the wind. Anothe

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