Hamiltonian model for coupled surface and internal waves in the presence of currents

Abstract

We examine a two dimensional fluid system consisting of a lower medium bounded underneath by a flatbed and an upper medium with a free surface. The two media are separated by a free common interface. The gravity driven surface and internal water waves (at the common interface between the media) in the presence of a depth-dependent current are studied under certain physical assumptions. Both media are considered incompressible and with prescribed vorticities. Using the Hamiltonian approach the Hamiltonian of the system is constructed in terms of 'wave' variables and the equations of motion are calculated. The resultant equations of motion are then analysed to show that wave-current interaction is influenced only by the current profile in the 'strips' adjacent to the surface and the interface. Small amplitude and long-wave approximations are also presented.

arXiv comment33 pages, 1 figure

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Cited by in corpus (9)

• A nonlocal shallow-water model arising from the full water waves with the Coriolis effect
• Azimuthal equatorial flows in spherical coordinates with discontinuous stratification
• On the intermediate long wave propagation for internal waves in the presence of currents
• Hamiltonian approach to modelling interfacial internal waves over variable bottom
• Hamiltonian description of internal ocean waves with Coriolis force
• Modelling surface waves on shear current with quadratic depth-dependence
• Hamiltonian model for coupled surface and internal waves over currents and uneven bottom
• Modelling intermediate internal waves with currents and variable bottom
• Solitary Wave Solution of Flat Surface Internal Geophysical Waves with Vorticity