Interactions of currents and weakly nonlinear water waves in shallow water
- 1 August 1989
- journal article
- research article
- Published by Cambridge University Press (CUP) in Journal of Fluid Mechanics
- Vol. 205 (-1), 397-419
- https://doi.org/10.1017/s0022112089002089
Abstract
Two-dimensional Boussinesq-type depth-averaged equations are derived for describing the interactions of weakly nonlinear shallow-water waves with slowly varying topography and currents. The current velocity varies appreciably within a characteristic wavelength. The effects of vorticity in the current field are considered. The wave field is decomposed into Fourier time harmonics. A set of evolution equations for the wave amplitude functions of different harmonics is derived by adopting the parabolic approximation. Numerical solutions are obtained for shallow-water waves propagating over rip currents on a plane beach and an isolated vortex ring. Numerical results show that the wave diffraction and nonlinearity are important in the examples considered.Keywords
This publication has 13 references indexed in Scilit:
- Wave refraction by warm core ringsJournal of Geophysical Research: Oceans, 1985
- Nonlinear refraction–diffraction of waves in shallow waterJournal of Fluid Mechanics, 1985
- A note on linear surface wave‐current interaction over slowly varying topographyJournal of Geophysical Research: Oceans, 1984
- Giant wavesJournal of Fluid Mechanics, 1976
- Stationary gravity waves on non-uniform free streams: jet-like streamsMathematical Proceedings of the Cambridge Philosophical Society, 1975
- Wavetrains in inhomogeneous moving mediaProceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences, 1968
- Long waves on a beachJournal of Fluid Mechanics, 1967
- The changes in amplitude of short gravity waves on steady non-uniform currentsJournal of Fluid Mechanics, 1961
- Changes in the form of short gravity waves on long waves and tidal currentsJournal of Fluid Mechanics, 1960
- Refraction of shallow water waves: The combined effect of currents and underwater topographyEOS, Transactions American Geophysical Union, 1950