The Stability of Oscillatory Stokes Layers

DOI10.1002/sapm1972513239zbMath0257.76042OpenAlexW2605543313MaRDI QIDQ5672371

Stephen H. Davis, Christian von Kerczek

Publication date: 1972

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

Full work available at URL: https://doi.org/10.1002/sapm1972513239

Mathematics Subject Classification ID

Parallel shear flows in hydrodynamic stability (76E05)

Related Items (9)

The stability of uniformly accelerated flows with application to convection driven by surface tension ⋮ Linear stability theory of oscillatory Stokes layers ⋮ Energy method in the theory of convective stability of a non-Newtonian liquid ⋮ Global stability of time-dependent flows. Part 2. Modulated fluid layers ⋮ Casi di non validità di una riformulazione del metodo dell'energia ⋮ Coriolis instability of pulsed flow ⋮ On magnetohydrodynamic motions in unbounded domains: Stability and uniqueness ⋮ An application of the invariance principle to a non-linear, first order evolution problem: Asymptotic stability in non-isothermal magnetohydrodynamics ⋮ Particle image velocimetry as a teaching with technology resource in oscillatory laminar fluid flow

Cites Work

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• The stability of time-dependent laminar flow. Parallel flows
• The stability of time-dependent laminar flow. Flow with curved streamlines
• Nonlinear stability of the Boussines q equations by the method of energy
• Contributions to the nonlinear theory of stability of viscous flow in pipes and between rotating cylinders
• Instability of unsteady flows or configurations Part 1. Instability of a horizontal liquid layer on an oscillating plane
• Centrifugal instability of time-dependent flows. Part 1. Inviscid, periodic flows
• The stability of steady and time-dependent plane Poiseuille flow
• The effects of gravity modulation on the stability of a heated fluid layer
• ON THE STABILITY OF OSCILLATING, PLANE COUETTE FLOW
• Instability of Time-Periodic Flows of Stratified Fluids
• Energy stability of the buoyancy boundary layer

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