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Generation of mode-2 internal waves in a two-dimensional stratification by a mode-1 internal wave
Institution:1. Satellite Oceanography Laboratory (SOLab), Russian State Hydrometeorological University, Malookhtinsky Prospect 98, St. Petersburg 195196, Russian Federation;2. Klaip?da University, H. Manto g. 84, LT-92291 Klaip?da, Lithuania;3. St. Petersburg Branch of P. P. Shirshov Institute of Oceanology RAS, St. Petersburg, Russian Federation;4. Institute Francais de Recherche pour I''Exploitation de la Mer, BP 70, 29280 Plouzane, France
Abstract:The generation of mode-2 nonlinear internal waves (IWs) by the evolution of a mode-1 IW in a two-dimensional stratification is investigated. A generation model accounting for intermodal interaction is derived based on a multi-modal approach in a weakly nonlinear and non-hydrostatic configuration. The generation model is numerically solved to simulate the evolution of mode-1 and mode-2 IWs in an inhomogeneous pycnocline. The numerical experiments confirm that mode-2 IWs are generated due to linear and nonlinear intermodal interaction. The mode-2 IW continues growing and gradually separates with the mode-1 IW during the generation process. The numerical results suggest that the pycnocline strength or thickness prominently affects the generation of mode-2 IWs, followed by pycnocline depth. A weakening or thinning pycnocline favors the generation of mode-2 IWs by evidently enhancing linear and nonlinear intermodal interaction, whereas a shoaling pycnocline favors a rapid growth rate mainly by enhancing linear intermodal interaction. The wave amplitude of an initial mode-1 IW strongly affects the generation of mode-2 IWs and increasing it can noticeably enlarge mode-2 IWs.
Keywords:Mode-2 internal wave  Two-dimensional stratification  Generation  Favorable environmental conditions
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