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Hydraulic control of zonal currents on a β-plane

Published online by Cambridge University Press:  26 April 2006

Laurence Armi
Affiliation:
Scripps Institution of Oceanography, La Jolla, CA 92093, USA

Abstract

Eastward-flowing zonal currents on a thin rotating shell, such as a planetary atmosphere or ocean, have integral properties analogous to open channel flows, the latitudinal width of the zonal current being the analogue of the depth of an open channel flow. The purpose here is to apply the formalism and some of the concepts of open channel flow hydraulics to zonal flows and demonstrate the results with laboratory experiments. In particular a critical relationship is found between a representative zonal velocity, U, and the half-width of the current, a. A dimensionless parameter (Ua2), the Froude/Rossby number, is found analogous to the Froude number of open channel flow. Westward-flowing currents do not have an equivalent analogue.

Type
Research Article
Copyright
© 1989 Cambridge University Press

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References

Armi, L. 1974 An energy minimization principle for oceanic currents and atmospheric jet streams. Geophys. Fluid Dyn. Notes, WHOI Ref. 74–63 (2), 114.Google Scholar
Baker, D. J. 1966 A technique for the precise measurment of small fluid velocities. J. Fluid Mech. 26, 573575.Google Scholar
Ball, F. K. 1959 Long waves, lee waves and gravity waves. Q. J. R. Met. Soc. 85, 2430.Google Scholar
Berggren, R., Bolin, B. & Rossby, C.-G. 1949 An aerological study of zonal motion, its perturbations and breakdown. Tellus 1, 1437.Google Scholar
Faller, A. J. 1960 Further examples of stationary planetary flow patterns in bounded basins. Tellus 12, 159171.Google Scholar
Fultz, D. 1961 Developments in controlled experiments on larger scale geophysical problems. Adv. Geophys. 7, 1103.Google Scholar
Gadgil, S. 1971 Structure of jets in rotating systems. J. Fluid Mech. 47, 417436.Google Scholar
Grimshaw, R. H. J. 1975 A note on the beta-plane approximation. Tellus 27, 351357.Google Scholar
Henderson, F. M. 1966 Open Channel Flow, pp. 522. Macmillan.
Ibbetson, A. & Phillips, N. 1967 Some laboratory experiments on Rossby waves in a rotating annulus. Tellus 19, 8187.Google Scholar
Ippen, A. T. 1950 Channel transitions and controls. Engineering Hydraulics, Proc. Fourth Hydraulics Conference, Iowa Inst. of Hydraulic Res., June 12-15, 1949 (ed. H. Rouse), pp. 496588. Wiley.
Long, R. R. 1955 Some aspects of the flow of stratified fluids. III. Continuous density gradients. Tellus 7, 341357.Google Scholar
Phillips, N. A. 1966 The equations of motion for a shallow rotating atmosphere and “the traditional approximation”. J. Atmos. Sci. 23, 626628.Google Scholar
Rex, D. F. 1950 Blocking action in the middle troposphere and its effect upon regional climate. I. An aerological study of blocking action. Tellus 2, 196211.Google Scholar
Rhines, P. B. 1975 Waves and turbulence on a beta-plane. J. Fluid Mech. 69, 417443.Google Scholar
Rossby, C.-G. 1950 On the dynamics of certain types of blocking waves. J. Chinese Geophys. Soc. 2, 113.Google Scholar
Rouse, H. 1950 Fundamental principles of flow, Engineering Hydraulics, Proc. Fourth Hydraulics Conference, Iowa Inst. of Hydraulic Res., June 12-15, 1949 (ed. H. Rouse), pp. 1135. Wiley.
Veronis, G. 1963 On the approximations involved on transforming the equations of motion from a spherical surface to the beta-plane. I. Barotropic systems. J. Mar. Res. 21, 110124.Google Scholar
Veronis, G. 1973 Large scale ocean circulation. Adv. Appl. Mech. 13, 192.Google Scholar
Yih, C. S. 1980 Stratified flows. Academic. 418 pp.