Long-term evolution of strongly nonlinear internal solitary waves in a rotating channel

被引:6
作者
Sanchez-Garrido, J. C. [1 ,2 ]
Vlasenko, V. [3 ]
机构
[1] Univ Malaga, Grp Oceanog Fis, Dpto Fis Aplicada 2, E-29071 Malaga, Spain
[2] Univ Granada, Grp Puertos & Costas, Ctr Andaluz Medio Ambiente, Granada, Spain
[3] Univ Plymouth, Sch Earth Ocean & Enviromental Sci, Plymouth PL8 4AA, Devon, England
关键词
KADOMTSEV-PETVIASHVILI EQUATION; KELVIN WAVES; OCEAN; TIDES; GENERATION; FLUID;
D O I
10.5194/npg-16-587-2009
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The evolution of internal solitary waves (ISWs) propagating in a rotating channel is studied numerically in the framework of a fully-nonlinear, nonhydrostatic numerical model. The aim of modelling efforts was the investigation of strongly-nonlinear effects, which are beyond the applicability of weakly nonlinear theories. Results reveal that small-amplitude waves and sufficiently strong ISWs evolve differently under the action of rotation. At the first stage of evolution an initially two-dimensional ISW transforms according to the scenario described by the rotation modified Kadomtsev-Petviashvili equation, namely, it starts to evolve into a Kelvin wave (with exponential decay of the wave amplitude across the channel) with front curved backwards. This transition is accompanied by a permanent radiation of secondary Poincar, waves attached to the leading wave. However, in a strongly-nonlinear limit not all the energy is transmitted to secondary radiated waves. Part of it returns to the leading wave as a result of nonlinear interactions with secondary Kelvin waves generated in the course of time. This leads to the formation of a slowly attenuating quasi-stationary system of leading Kelvin waves, capable of propagating for several hundreds hours as a localized wave packet.
引用
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页码:587 / 598
页数:12
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