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Titlebook: Wave Dynamics and Radio Probing of the Ocean Surface; O. M. Phillips,Klaus Hasselmann Book 1986 Springer Science+Business Media New York 1

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An Experimental Study of the Statistical Properties of Wind-Generated Gravity Waves ratio of the rms wave height to the wavelength corresponding to the waves at the spectral peak. The significant slope is also found to be the controlling factor in determining the spectral shape and evolution. Thus, the present set of detailed observational data could be used as the base to link th
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On Finite-Depth Wind-Wave Generation and Dissipationt shift in the forward face and peak of the spectrum to lower frequencies and a reduction in the peak spectral density in the manner suggested by Phillips (1977). This overshoot, furthermore, occurred when k.h ≈ 0.67 [where the resonant response rate has been calculated by Hasselmann and Hasselmann
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The Instability and Breaking of a Deep-Water Wave Trains’s (1978) breaking instabihty. For . 0.31 a full three-dimensional instability dominates the Benjamin-Feir instability and leads rapidly to breaking. Preliminary measurements of this instability agree very well with the results of McLean .. (1981). Continuous measurements of the velocity field at t
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Experimental Studies of Strong Nonlinear Interactions of Deep-Water Gravity Wavesed. The experimental investigations plus analyses of other oceanic measurements and theoretical computations seem to imply that the classical view of weak-in-the-mean interactions of ocean waves can also be explained conceptually by combined effects of intermittent processes of strong three-dimensio
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The Instability and Breaking of a Deep-Water Wave Trains’s (1978) breaking instabihty. For . 0.31 a full three-dimensional instability dominates the Benjamin-Feir instability and leads rapidly to breaking. Preliminary measurements of this instability agree very well with the results of McLean .. (1981). Continuous measurements of the velocity field at t
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natural that Sir George Deacon would be invited to serve as honorary chairman for the meeting, and the entire waves community was delighted at his acceptance. The present volume contains reviewed and edited papers given at this second meeting, held this time in Miami, Florida, May 13-20, 1981, with the gener978-1-4684-8982-8978-1-4684-8980-4
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