Answers are grounded in this paper and cite their sources.
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. 19, 267 (1969)], complementing a linear analysis by Blumen [J. Atmos. Sci. 25, 929 (1968)]. An a priori estimate bounding the growth of perturbation is derived.
No takes yet. Share an insight, caveat, or question.
Gordon E. Swaters (1986) studied this question.
Synapse has enriched 5 related papers. Consider them for comparative context: