The asymmetric balance (AB) theory is valid for large Rossby number; it makes no formal restriction on the magnitude of the divergence or vertical advection, which need not be small. The AB is an ordered expansion in the square of the ratio of orbital to inertial frequencies, the square of a local Rossby number. The approximation filters gravity and inertial waves from the system. Advantage is taken of the weak asymmetries near the vortex core as well as the tendency for low azimuthal wavenumber asymmetries to dominate. Linearization about a symmetric balanced vortex allows the three-dimensional asymmetric dynamics to be deduced properly. It includes the full inertial dynamics of the vortex core, and reduces to Eliassen's formulation for purely axisymmetric flow. It has a full set of conservation laws on fluid parcels analogous to those for primitive equations, including conservation of potential temperature, potential vorticity, three-dimensional vorticity, and energy. A weakly nonlinear extension of the formulation in the near-vortex region is presented. Appropriate physical applications for the AB system, as well as its limitations, are discussed. -from Authors
CITATION STYLE
Shapiro, L. J., & Montgomery, M. T. (1993). A three-dimensional balance theory for rapidly rotating vortices. Journal of the Atmospheric Sciences, 50(19), 3322–3335. https://doi.org/10.1175/1520-0469(1993)050<3322:ATDBTF>2.0.CO;2
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