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

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NEEDY

Possible Mechanisms for Wave Breaking, by the dominant ones. We seek confirmation for this in the analysis of accurate wave records taken from an oceanographic platform in the Adriatic. Consistently with the forementioned mechanism, we find evidence of grouping of short waves just ahead of the dominant crests in the active wind cases,

BROOK

Plural Identities in the Age of Nationalismsnd . is a characteristic wind velocity. The other spectrum corresponds to an inverse cascade of energy in which wavelengths increase (“wave aging”) (Zakharov and Zaslavsky, 1981). It is realized at ω< ω.. The inverse cascade leads to the production of “aged waves” that are common in an open ocean (G

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Making Knowledge Management Clickable to wall layer scaling. In the intermediate region the dissipation decays more rapidly than z.. This may be viewed as a transition region between the deeper shear layer and the near surface region, with intense patches of breaking-imposed turbulence. In the absence of density stratification, dissipa

Spartan

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Leisure workshops for parents and carersetween the upper and lower sidebands but with the onset of breaking a smaller fraction of the initial energy was transferred to the upper sideband. The spectral behaviour of these evolving wave packets shows a number of features in common with that of wind waves observed in the open sea.

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Dependence of Wave-Breaking Statistics on Wind Stress and Wave Developmentcombination of.. and ../.. can be understood in physical terms. Furthermore, for the larger values of .. the dependence of wave breaking on wave age was stronger than at the low end of the values for .. and ../... Thus, both the level of wave development as determined by inverse wave age, which we m

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The Sideband Instability and the Onset of Wave Breakingetween the upper and lower sidebands but with the onset of breaking a smaller fraction of the initial energy was transferred to the upper sideband. The spectral behaviour of these evolving wave packets shows a number of features in common with that of wind waves observed in the open sea.