No CrossRef data available.
Article contents
The generation of surface waves by an intense cyclone
Published online by Cambridge University Press: 17 February 2009
Abstract
Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.
Assuming a travelling oscillating pressure source model, this paper sets out to investigate the observation of surface gravity waves generated by a cyclone moving with constant speed v. It is shown that when the source frequency is near the critical resonant value g/4ν, large amplitude waves may be generated. There is some agreement with observations of waves from cyclone Pam of February, 1974.
- Type
- Research Article
- Information
- Copyright
- Copyright © Australian Mathematical Society 1983
References
[1]Abramowitz, M. and Stegun, I. A. (eds.), Handbook of mathematical functions (Dover, New York, 1965).Google Scholar
[2]Campbell, G. A. and Foster, R. M., Fourier integrals for practical applications (Van Nostrand, Princeton, 1948).Google Scholar
[3]Courant, R. and Hubert, D., Methods of mathematical physics, Volume 2 (Interscience, New York, 1953).Google Scholar
[4]Crapper, G. D., “Surface waves generated by a travelling pressure point”, Proc. Roy. Soc. London Ser. A 282 (1964), 547–558.Google Scholar
[5]Lighthill, M. J., “Studies on magneto-hydrodynamic waves and other anisotropic wave motions”, Phil. Trans. Roy. Soc. London Ser. A 252 (1960), 397–430.Google Scholar
[6]Lighthill, M. J., “On waves generated in dispersive systems by travelling forcing effects, with applications to the dynamics of rotating fluids”, J. Fluid Mech. 27 (1967), 725–752.Google Scholar
You have
Access