Conjugate flows for waves with trapped cores

DOI10.1063/1.1811551zbMath1187.76293OpenAlexW1966549430MaRDI QIDQ3554773

K. G. Lamb, Kathleen P. Wilkie

Publication date: 22 April 2010

Published in: Physics of Fluids (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1063/1.1811551

zbMATH Keywords

waveswave propagationtwo-phase flowsolitonsvorticesflow simulation

Mathematics Subject Classification ID

Fluid mechanics (76-XX)

Related Items (10)

Asymmetric internal solitary waves with a trapped core in deep fluids ⋮ Convectively induced shear instability in large amplitude internal solitary waves ⋮ Breathers in a three-layer fluid ⋮ On symmetric intrusions in a linearly stratified ambient: a revisit of Benjamin's steady-state propagation results ⋮ Gravity currents and internal waves in a stratified fluid ⋮ Internal solitary waves with subsurface cores ⋮ Numerical simulation of supercritical trapped internal waves over topography ⋮ Instability in internal solitary waves with trapped cores ⋮ A general description of a gravity current front propagating in a two-layer stratified fluid ⋮ Breather interactions in a three-layer fluid

Cites Work

• A Computational Method for Solitary Internal Waves in a Continuously Stratified Fluid
• Conjugate flows for a three-layer fluid
• Broadening of interfacial solitary waves
• Large Amplitude Internal Waves of Permanent Form
• The transition from density-driven to wave-dominated isolated flows
• A numerical investigation of solitary internal waves with trapped cores formed via shoaling
• An integral equation approach to internal (2-layer) solitary waves
• Breaking and broadening of internal solitary waves
• Numerical simulations of internal solitary waves with vortex cores
• Internal waves of finite amplitude and permanent form
• Solitary internal waves in deep water
• Solitary waves with a vortex core in a shallow layer of stratified fluid
• Conjugate flows and flat solitary waves for a continuously stratified fluid
• Fully nonlinear solitary waves in continuously stratified incompressible Boussinesq fluids

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