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M. Evonuk, G. A. Glatzmaier (UCSC)
It is likely that some of the giant extrasolar gaseous planets, and possibly Jupiter, do not possess solid cores. To gain a preliminary understanding of the influence a solid core has on the convective patterns in the deep interior of these planets and their effect on the surface zonal flow of the planet, we use a 2D finite volume code to simulate thermal convection in a rapidly rotating density-stratified fluid disk with and without a solid core. The results of the three cases are compared: two with cores of different sizes and one case without a core. We find higher kinetic energy densities in the cases with a small core or no core than in the case with a larger core suggesting possible correlation between surface zonal wind velocities and structure at depth.
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Bulletin of the American Astronomical Society, 37 #3
© 2004. The American Astronomical Soceity.