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Wave-induced longitudinal-vortex instability in shear flows

Published online by Cambridge University Press:  20 April 2006

A. D. D. Craik
A. D. D. Craik
Affiliation:
Department of Applied Mathematics, University of St. Andrews, St. Andrews, Fife KY16 9SS, Scotland
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Abstract

The instability of two-dimensional periodic flows to spanwise-periodic ‘longitudinal- vortex’ modes is examined. The undisturbed state comprises a parallel shear flow and a two-dimensional O(ε) wave field as encountered in, say, water-wave or hydrodynamic-stability theories.

When the mean shear is weak, of order ε2, the present theory reduces to that of Craik (1977) and Leibovich (1977b, 1980). For stronger but still weak shear, of order ε, it is established that the Craik-Leibovich instability mechanism is essentially unchanged, apart from scaling factors. For strong O(1) shear flows, the governing equations are derived by using, in part, a generalized Lagrangian-mean formulation. The resultant eigenvalue problem for the longitudinal-vortex instability is then more complex, but simplifies in the case of small spanwise spacing of the vortices, in the inviscid limit. An example is given of flows that exhibit instability in this limiting case. Such instability seems likely to occur for a wide class of periodic shear flows. Complementary physical interpretations of the instability mechanism are discussed.

Information

Type
Research Article
Information
Journal of Fluid Mechanics , Volume 125 , December 1982 , pp. 37 - 52
Copyright
© 1982 Cambridge University Press

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