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NONLINEAR INERTIA—GRAVITY INTERNAL WAVE IN STRATIFIED FLUID

NONLINEAR INERTI A-GRAVITY INTERNAL WAVE IN STRATIFIED FLUID*
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摘要 Based on the fundamental equations of geophysical fluid dynamics and on the consequence of verticaldensity stratification,travelling wave coordinates are used in this work to study the geometric topologicalstructures of nonlinear permanent wave in phase plane.Rigorous mathematical mechanics demonstratethat the solution of permanent solitary wave does not exist.Hamilton functions and 'action-angle' varia-bles are used to express the travelling wave system in the simplest form and the analytic solution of the nonlinear inertia-gravity internal wave is obtained. Based on the fundamental equations of geophysical fluid dynamics and on the consequence of vertical density stratification, travelling wave coordinates are used in this work to study the geometric topological structures of nonlinear permanent wave in phase plane. Rigorous mathematical mechanics demonstrate that the solution of permanent solitary wave does not exist. Hamilton functions and 'action-angle' varia-bles are used to express the travelling wave system in the simplest form and the analytic solution of the nonlinear inertia-gravity internal wave is obtained.
出处 《Chinese Journal of Oceanology and Limnology》 SCIE CAS CSCD 1995年第1期13-20,共8页 中国海洋湖沼学报(英文版)
基金 Project supported by NSFC for Youtb(No.B909920106)
关键词 NONLINEAR inertia-gravity INTERNAL wave STRATIFIED FLUID nonlinear inertia-gravity internal wave, stratified fluid
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参考文献2

  • 1刘式适,刘式达,卜玉康.层结切变流体非线性惯性重力内波的稳定性[J]气象学报,1984(01). 被引量:1
  • 2巢纪平,黄瑞新.THE CNOIDAL WAVES OF ROTATING BAROTROPIC ATMOSPHERE[J]Science in ChinaSerA,1980(10). 被引量:1

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