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Limiting amplitudes of fully nonlinear interfacial tides and solitons
2016
Nonlinear Processes in Geophysics Discussions
A new two-fluid layer model consisting of forced rotation-modified Boussinesq equations is derived for studying tidally-generated fully nonlinear, weakly nonhydrostatic dispersive interfacial waves. This set is a generalization of the Choi-Camassa equations, extended here with forcing terms and Coriolis effects. The forcing is represented by a horizontally oscillating sill, mimicking a barotropic tidal flow over topography. Solitons are generated by a disintegration of the interfacial tide.
doi:10.5194/npg-2016-1
fatcat:nzu2ld7yjbezpnk2wgd6tsaxfm