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Автор Joyce, Terrence M.
Дата выпуска 1974
dc.description A laboratory study has been undertaken to measure the energy transfer from two surface waves to one internal gravity wave in a nonlinear, resonant interaction. The interacting waves form triads for which \[ \sigma_{1s} - \sigma_{2s} \pm\sigma_1 = 0\quad {\rm and}\quad \kappa_{1s} - \kappa_2s} \pm \kappa_I = 0; \] σj and κj being the frequency and wavenumber of the jth wave. Unlike previously published results involving single triplets of interacting waves, all waves here considered are standing waves. For both a diffuse, two-layer density field and a linearly increasing density with depth, the growth to steady state of a resonant internal wave is observed while two deep water surface eigen-modes are simultaneously forced by a paddle. Internal-wave amplitudes, phases and initial growth rates are compared with theoretical results derived assuming an arbitrary Boussinesq stratification, viscous dissipation and slight detuning of the internal wave. Inclusion of viscous dissipation and slight detuning permit predictions of steady-state amplitudes and phases as well as initial growth rates. Satisfactory agreement is found between predicted and measured amplitudes and phases. Results also suggest that the internal wave in a resonant triad can act as a catalyst, permitting appreciable energy transfer among surface waves.
Издатель Cambridge University Press
Название Nonlinear interactions among standing surface and internal gravity wavesContribution no. 3209, Woods Hole Oceanographic Institution.
DOI 10.1017/S0022112074002205
Electronic ISSN 1469-7645
Print ISSN 0022-1120
Журнал Journal of Fluid Mechanics
Том 63
Первая страница 801
Последняя страница 825
Аффилиация Joyce Terrence M.; Massachusetts Institute of Technology; Woods Hole Oceanographic Institution
Выпуск 4

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