Long Eddies in Sheared Flows

DOI10.1002/sapm1983682103zbMath0515.76025OpenAlexW1674185422MaRDI QIDQ3662819

P. A. Blythe, E. Varley

Publication date: 1983

Published in: Studies in Applied Mathematics (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1002/sapm1983682103

zbMATH Keywords

steadycritical levelthin layer of fluidbarotropic and baroclinic flowseffect of shear gradientslarge amplitude long waveslateral boundaries rigid, flexible or freepropagation of eddieswaves containing single peakwaves containing single trough

Mathematics Subject Classification ID

Vortex flows for incompressible inviscid fluids (76B47) Water waves, gravity waves; dispersion and scattering, nonlinear interaction (76B15) Shear flows and turbulence (76F10)

Related Items (9)

On the nonlinear critical layer below a nonlinear unsteady surface wave ⋮ Applications of exact solutions to the Navier–Stokes equations: free shear layers ⋮ Nonlinear instability and break-up of separated flow ⋮ Solutions to the Navier‐Stokes Equations Describing Local Flows of Stratified and Compressible Fluids ⋮ Exact Simple Waves on Shear Flows in a Compressible Barotropic Medium ⋮ ANALYTICAL AND NUMERICAL SOLUTIONS OF THE SHALLOW WATER EQUATIONS FOR 2D ROTATIONAL FLOWS ⋮ Sub- and supercritical horizontal-shear flows in an open channel of variable cross-section ⋮ Is Landau Damping Possible in a Shear Fluid Flow? ⋮ Stability Of Shear Shallow Water Flows with Free Surface

Cites Work

• Unnamed Item
• The interaction of large amplitude barotropic waves with an ambient shear flow: critical flows
• On the high Reynolds number flow over a wavy boundary
• A New Class of Nonlinear Waves in Parallel Flows
• The interaction of large amplitude shallow-water waves with an ambient shear flow: non-critical flows
• Critical Layers m Parallel Flows

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