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 language | English |
|---|---|
| Pages (from-to) | 329-344 |
| Number of pages | 16 |
| Journal | Journal of Mathematical Fluid Mechanics |
| Volume | 19 |
| Issue number | 2 |
| DOIs | |
| Publication status | Published - 1 Jun 2017 |
Keywords
- Hamiltonian system
- Internal waves
- KdV equation
- equatorial undercurrent
- shear flow