Weakly nonlinear internal waves in a two-fluid system

Author:

Choi Wooyoung,Camassa Roberto

Abstract

We derive general evolution equations for two-dimensional weakly nonlinear waves at the free surface in a system of two fluids of different densities. The thickness of the upper fluid layer is assumed to be small compared with the characteristic wavelength, but no restrictions are imposed on the thickness of the lower layer. We consider the case of a free upper boundary for its relevance in applications to ocean dynamics problems and the case of a non-uniform rigid upper boundary for applications to atmospheric problems. For the special case of shallow water, the new set of equations reduces to the Boussinesq equations for two-dimensional internal waves, whilst, for great and infinite lower-layer depth, we can recover the well-known Intermediate Long Wave and Benjamin–Ono models, respectively, for one-dimensional uni-directional wave propagation. Some numerical solutions of the model for one-dimensional waves in deep water are presented and compared with the known solutions of the uni-directional model. Finally, the effects of finite-amplitude slowly varying bottom topography are included in a model appropriate to the situation when the dependence on one of the horizontal coordinates is weak.

Publisher

Cambridge University Press (CUP)

Subject

Mechanical Engineering,Mechanics of Materials,Condensed Matter Physics

Reference26 articles.

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3. Kubota, T. , Ko, D. R. S. & Dobbs, L. D. 1978 Propagation of weakly nonlinear internal waves in a stratified fluid of finite depth.AIAA J. Hydrodyn. 12,157–165.

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5. Matsuno, Y. 1993b Nonlinear evolution of surface gravity waves over an uneven bottom.J. Fluid Mech. 249,121–133.

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