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When studying the propagation and evolution of internal solitary waves in stratified fluids, seawater is typically simplified as two homogeneous, immiscible fluid layers. Existing two-layer theoretical models are based on potential flow theory, assuming irrotational, incompressible flow with upper and lower layer depths set as \({h}_{1}\) and \({h}_{2}\) , fluid densities set as \({\rho }_{1}\) and \({\rho }_{2}\) , with total water depth \(H={h}_{1}+{h}_{2}\) .

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Internal Wave Theory

  • 章节

  • 发表日期：

    2026年

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  • Peng Du,
  • Chao Wang,
  • Sen Zhao,
  • Jun Wen,
  • Luo Xie,
  • Haibao Hu

摘要

When studying the propagation and evolution of internal solitary waves in stratified fluids, seawater is typically simplified as two homogeneous, immiscible fluid layers. Existing two-layer theoretical models are based on potential flow theory, assuming irrotational, incompressible flow with upper and lower layer depths set as \({h}_{1}\) and \({h}_{2}\) , fluid densities set as \({\rho }_{1}\) and \({\rho }_{2}\) , with total water depth \(H={h}_{1}+{h}_{2}\) .