Observational Consequences of Shallow-water Magnetohydrodynamics on Hot Jupiters
arXiv:2107.10848 · doi:10.3847/2041-8213/ac0fec
Abstract
We use results of shallow-water magnetohydrodynamics (SWMHD) to place estimates on the minimum magnetic field strengths required to cause atmospheric wind variations (and therefore westward venturing hotspots) for a dataset of hot Jupiters (HJs), including HAT-P-7b, CoRoT-2b, Kepler-76, WASP-12b, and WASP-33b, on which westward hotspots have been observationally inferred. For HAT-P-7b and CoRoT-2b our estimates agree with past results; for Kepler-76b we find that the critical dipolar magnetic field strength, over which the observed wind variations can be explained by magnetism, lies between $4\mbox{ G}$ and $19\mbox{ G}$; for WASP-12b and WASP-33b westward hotspots can be explained by $1\mbox{ G}$ and $2\mbox{ G}$ dipolar fields respectively. Additionally, to guide future observational missions, we identify further HJs that are likely to exhibit magnetically-driven atmospheric wind variations and predict these variations are highly-likely in of the hottest HJs.
10 pages, 3 figures, 2 tables
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