Abstract
The turbulent flow at the periphery of the Great Red Spot (GRS) contains many fine-scale filamentary structures, while the more quiescent core: bounded by a narrow high-velocity ring, exhibits organized, possibly counterrotating, motion. Past studies have neither been able to capture this complexity nor adequately study the effects of vertical stratification L-R(z) on the GRS. We present results from a series of high-resolution, three-dimensional simulations that advect the dynamical tracer, potential vorticity. The detailed flow is successfully captured with a characteristic value of L-R approximate to 2000 km, independent of the precise vertical stratification profile.
| Original language | English |
|---|---|
| Pages (from-to) | 5099-5105 |
| Number of pages | 7 |
| Journal | Journal of Geophysical Research |
| Volume | 106 |
| Issue number | E3 |
| DOIs | |
| Publication status | Published - 25 Mar 2001 |
Keywords
- NUMERICAL-SIMULATION
- POTENTIAL VORTICITY
- OUTER PLANETS
- ATMOSPHERE
- FLOW
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