The Dynamics of Flat Surface Internal Geophysical Waves with Currents

Alan Compelli, Rossen I. Ivanov

Research output: Contribution to journalArticlepeer-review

Abstract

A two-dimensional water wave system is examined consisting of two discrete incompressible fluid domains separated by a free common interface. In a geophysical context this is a model of an internal wave, formed at a pycnocline or thermocline in the ocean. The system is considered as being bounded at the bottom and top by a flatbed and wave-free surface respectively. A current profile with depth-dependent currents in each domain is considered. The Hamiltonian of the system is determined and expressed in terms of canonical wave-related variables. Limiting behaviour is examined and compared to that of other known models. The linearised equations as well as long-wave approximations are presented.

Original languageEnglish
Pages (from-to)329-344
Number of pages16
JournalJournal of Mathematical Fluid Mechanics
Volume19
Issue number2
DOIs
Publication statusPublished - 1 Jun 2017

Keywords

  • Hamiltonian system
  • Internal waves
  • KdV equation
  • equatorial undercurrent
  • shear flow

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