Abstract
The baroclinic quasigeostrophic equations describe the essential dynamics of large‐scale, low‐frequency atmospheric ocean flow. A nonlinear stability theorem is given based on a convexity argument of Arnold [Am. Math. Soc. Transl. 1 9, 267 (1969)], complementing a linear analysis by Blumen [J. Atmos. Sci. 2 5, 929 (1968)]. An a priori estimate bounding the growth of perturbation is derived.

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