Self-similar multi-layer exchange flow through a contraction

DOI10.1017/S0022112096008646zbMath0890.76088MaRDI QIDQ4358966

Anders Engqvist

Publication date: 7 October 1997

Published in: Journal of Fluid Mechanics (Search for Journal in Brave)

zbMATH Keywords

decoupling principlebidirectional flowsgravitationally driven flowshydraulic control conditionstable Boussinesq type of stratificationstagnant layer

Mathematics Subject Classification ID

Hydrology, hydrography, oceanography (86A05) Reaction effects in flows (76V05)

Related Items (3)

Critical conditions and composite Froude numbers for layered flow with transverse variations in velocity ⋮ Viscous effects in two-layer, unidirectional hydraulic flow ⋮ Buoyancy-driven exchange flows in inclined ducts

Cites Work

• Maximal two-layer exchange through a contraction with barotropic net flow
• Maximal two-layer exchange over a sill and through the combination of a sill and contraction with barotropic flow
• A general method for determining upstream effects in stratified flow of finite depth over long two-dimensional obstacles
• Steady flows drawn from a stably stratified reservoir
• On hydraulic control in a stratified fluid
• Hydraulic jumps in an incompressible stratified fluid
• The hydraulics of rotating-channel flow
• Two-layer hydraulics: a functional approach

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