A numerical investigation of the stability of isolated vortices beyond the quasi-geostrophic regime

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Abstract

Motivated by observational data and recent numerical simulations showing that ageostrophic effects may play an important role in the dynamics and transport of large-scale vortices in the atmosphere and the oceans, the authors examine the stability of a family of isolated vortices, numerically, using the contour-advective semi-Lagrangian algorithm. The full shallow-water equations (1 1/2-layer model) are integrated in order to investigate vortices over a wide range of parameters. In order to characterize the cyclone-anticyclone asymmetry, the stability of a couple of vortices having velocity profiles of opposite sign is compared. It is found that ageostrophic effects (finite Rossby number) tend to stabilize anticyclones but destabilize cyclones. On the other hand, large-scale effects (small Burger number) are shown to stabilize all vortices for this reduced-gravity model. Here again, the anticyclones tend to be favored in this restabilization process. These results are compared with a linear stability analysis performed in the framework of the standard quasigeostrophic model that predicts a symmetric evolution for cyclones and anticyclones. The authors have shown that a significant departure from QG dynamics, due to ageostrophic and large-scale effects, appears in a range of parameters relevant to large-scale coherent structures in nature.

Original languageEnglish
Pages (from-to)2562-2573
Number of pages12
JournalJournal of Physics Oceanography
Volume30
Issue number10
DOIs
Publication statusPublished - Oct 2000

Keywords

  • F-PLANE
  • GEOSTROPHIC VORTICES
  • OCEANIC RINGS
  • INSTABILITY
  • ALGORITHM
  • EQUATIONS
  • EVOLUTION
  • TRIPOLES
  • DYNAMICS
  • FLUID

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