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The periodic quasigeostrophic equations: existence and uniqueness of strong solutions

Published online by Cambridge University Press:  14 November 2011

A. F. Bennett
Affiliation:
Department of Mathematics, Monash University, Clayton 3168, Victoria, Australia
P. E. Kloeden
Affiliation:
School of Mathematical and Physical Sciences, Murdoch University, Murdoch 6153, Western Australia

Synopsis

The periodic quasigeostrophic equations are a coupled system of a second order elliptic equation for a streamfunction and first order hyperbolic equations for the relative potential vorticity and surface potential temperatures, on a three-dimensional domain which is periodic in both horizontal spatial co-ordinates. Such equations are used in both numerical and theoretical studies in meteorology and oceanography. In this paper Schauder estimates and a Schauder fixed point theorem are used to prove the existence and uniqueness of strong, that is classical, solutions of the periodic quasigeostrophic equations for a finite interval of time, which is inversely proportional to the sum of the norms of the initial vorticity and surface temperatures.

Type
Research Article
Copyright
Copyright © Royal Society of Edinburgh 1982

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References

1Adams, R. A.. Sobolev Spaces (New York: Academic Press, 1975).Google Scholar
2Bennett, A. F. and Kloeden, P. E.. The quasigeostrophic equations: approximation, predictability and equilibrium spectra of solutions. Quart. J. Roy. Met. Soc. 107 (1981), 121136.Google Scholar
3Bretherton, F. P. and Karweit, M.. Mid-ocean mesoscale modelling. In Numerical Models of Ocean Circulation (Proc. Symp. Durham, New Hampshire 1972) (Washington, D.C.: National Academy of Sciences, 1975).Google Scholar
4Charney, J. G.. Geostrophic turbulence. J. Atmospheric Sci. 28 (1971), 10871095.2.0.CO;2>CrossRefGoogle Scholar
5Hartman, P.. Ordinary Differential Equations (Baltimore: Hartman, 1973).Google Scholar
6Kato, T.. On classical solutions of the two-dimensional non-stationary Euler equations.Arch. Rational Mech. Anal. 25 (1967), 188200.CrossRefGoogle Scholar
7Miranda, C.. Sul problema misto per le equazioni lineari ellittiche. Ann. Mat. Pura Appl. 39 (1955), 279303.CrossRefGoogle Scholar
8Pedlosky, J.. The stability of currents in the atmosphere and ocean: Part I. J. Atmospheric Sci. 21 (1964), 201209.2.0.CO;2>CrossRefGoogle Scholar
9Smart, D. R.. Fixed Point Theorems (Edinburgh: Cambridge Univ. Press, 1974).Google Scholar