paper

The Universal Aspect Ratio of Vortices in Rotating Stratified Flows: Theory and Simulation

arXiv:1203.1561 · doi:10.1017/jfm.2012.180

Abstract

We derive a relationship for the vortex aspect ratio (vertical half-thickness over horizontal length scale) for steady and slowly evolving vortices in rotating stratified fluids, as a function of the Brunt-Vaisala frequencies within the vortex and in the background fluid outside the vortex , the Coriolis parameter , and the Rossby number of the vortex: . This relation is valid for cyclones and anticyclones in either the cyclostrophic or geostrophic regimes; it works with vortices in Boussinesq fluids or ideal gases, and the background density gradient need not be uniform. Our relation for has many consequences for equilibrium vortices in rotating stratified flows. For example, cyclones must have ; weak anticyclones (with ) must have N_c^2 > \bar{N}^2ααα= f/\bar{N}$ in quasi-geostrophic vortices.

Submitted to the Journal of Fluid Mechanics. Also see the companion paper by Aubert et al. "The Universal Aspect Ratio of Vortices in Rotating Stratified Flows: Experiments and Observations" 2012

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