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Modulation of the amplitude of steep wind waves

Published online by Cambridge University Press:  19 April 2006

M. S. Longuet-Higgins
Affiliation:
Department of Applied Mathematics and Theoretical Physics, Silver Street, Cambridge, England, and Institute of Oceanographic Sciences, Wormley, Godalming, Surrey

Abstract

Lake & Yuen (1978) have suggested that in very steep wind waves the modulation-frequency of the wave amplitude may correspond to the frequency of the fastest-growing subharmonic instability of a uniform train of waves whose amplitude equals the mean wave amplitude $\overline{a}$. The approximate theory of Benjamin & Feir (1967) gives this frequency as $(\overline{a}k)f_d$, where κ is the wavenumber and fd the frequency of the unperturbed waves. This expression applies strictly only to very small values of the wave steepness $\overline{a}k$.

More recently (Longuet-Higgins 1978) the present author calculated accurately all the normal-mode instabilities of steep gravity waves on deep water. In this note these calculations are used to determine the frequency of the fastest-growing sub-harmonic instabilities precisely. When compared with the experimental data of Lake & Huen, these frequencies show even closer agreement.

Type
Research Article
Copyright
© 1980 Cambridge University Press

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References

Benjamin, T. B. & Feir, J. E. 1967 The disintegration of wave trains in deep water. Part I. Theory. J. Fluid Mech. 27, 417430.Google Scholar
Ewing, J. A. 1973 Mean length of runs of high waves. J. Geophys. Res. 78, 19331936.Google Scholar
Goda, Y. 1970 Numerical experiments on wave statistics with spectral simulation. Rep., Port Harbour Res. Inst., Min. Transport, Yokosuka 9, 3.Google Scholar
Hasselmann, K. 1973 Measurements of wind-wave growth and swell decay during the joint North Sea Wave Project (JONSWAP). Deut. Hydrogr. Z. Suppl. A 8 (12).Google Scholar
Lake, B. M. & Yuen, H. C. 1978 A new model for nonlinear wind waves. Part 1. Physical model and experimental evidence. J. Fluid Mech. 88, 3362.Google Scholar
Longuet-Higgins, M. S. 1952 On the statistical distribution of the heights of sea waves. J. Mar. Res. 11, 245266.Google Scholar
Longuet-Higgins, M. S. 1956 The statistical analysis of a random, moving surface. Phil. Trans. Roy. Soc. A 249, 321000.Google Scholar
Longuet-Higgins, M. S. 1975 Integral properties of periodic gravity waves of finite amplitude. Proc. Roy. Soc. A 342, 157174.Google Scholar
Longuet-Higgins, M. S. 1978 The instabilities of gravity waves of finite amplitude in deep water. Proc. Roy. Soc. A 360, 471505.Google Scholar
Longuet-Higgins, M. S. & Cokelet, E. D. 1978 The deformation of steep surface waves on water. II. Growth of normal-mode instabilities. Proc. Roy. Soc. A 364, 128.Google Scholar
Sverdrup, H. U. & Munk, W. H. 1947 Wind, sea and swell: Theory of relations for forecasting. U.S. Hydrographic Office, Publ. no. 601.