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On the instability of sheared disturbances

Published online by Cambridge University Press:  21 April 2006

Peter H. Haynes
Affiliation:
Joint Institute for the Study of the Atmosphere and the Ocean, University of Washington, Seattle. WA 98195, USA Present address: Department of Applied Mathematics and Theoretical Physics, University of Cambridge, Silver Street, Cambridge, CB3 9EW, UK.

Abstract

The equation for small-amplitude disturbances to an unbounded flow of constant shear on a beta-plane has well-known solutions of a particularly simple form. In physical terms such solutions represent a flow in which absolute-vorticity contours, initially taking a wavy configuration, are deformed by the basic-state shear. Here it is shown that, at least in cases where the initial disturbance has long wavelength, the vorticity distribution predicted by such solutions eventually becomes barotropically unstable, as the shearing over of material contours leads to local reversals in the cross-stream gradient of absolute vorticity.

Type
Research Article
Copyright
© 1987 Cambridge University Press

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References

Abramowitz, M. & Stegun, I. A. 1964 Handbook of Mathematical Functions. U.S. National Bureau of Standards.
Boyd, J. P. 1983 The continuous spectrum of linear Couette flow with the beta-effect. J. Atmos. Sci. 40, 23042308.Google Scholar
Case, K. M. 1960 Stability of inviscid plane Couette flow. Phys. Fluids 3, 143148.Google Scholar
Cox, M. D. 1985 An eddy-resolving numerical model of the ventilated thermocline. J. Phys. Oceanogr. 15, 13121324.Google Scholar
Dickinson, R. E. 1970 Development of a Rossby wave critical level. J. Atmos. Sci. 27, 627633.Google Scholar
Farrell, B. F. 1982 The initial growth of disturbances in a baroclinic flow. J. Atmos. Sci. 39, 16631686.Google Scholar
Haynes, P. H. 1985 Nonlinear instability of a Rossby-wave critical layer. J. Fluid Mech. 161, 493511.Google Scholar
Killworth, P. D. & McIntyre, M. E. 1985 Do Rossby-wave critical layers absorb, reflect or over-reflect?. J. Fluid Mech. 161, 449491.Google Scholar
Orr, W. M. F. 1907 The stability or instability of the steady motions of a perfect liquid and a viscous liquid: Parts I and II. Proc. R. Irish Acad. A27, 9–68; 69–138.Google Scholar
Phillips, O. M. 1966 Dynamics of the Upper Ocean, 1st edn. Cambridge University Press.
Shepherd, T. G. 1985 On the time development of small disturbances to plane Couette flow. J. Atmos. Sci. 42, 18681871.Google Scholar
Thomson, W. 1887 Stability of fluid motion - rectilineal motion of viscous fluid between two parallel planes. Phil. Mag. 24, 188196.Google Scholar
Tung, K. K. 1983 Initial-value problems for Rossby waves in a shear flow with critical level. J. Fluid Mech. 133, 443469.Google Scholar
Warn, T. & Warn, H. 1976 On the development of a Rossby wave critical level. J. Atmos. Sci. 33, 20212024.Google Scholar
Yamagata, T. 1976 On trajectories of Rossby-wave packets released in a lateral shear flow. J. Oceanogr. Soc. Japan 32, 162168.Google Scholar