2021
DOI: 10.3847/2041-8213/ac0fec
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Observational Consequences of Shallow-water Magnetohydrodynamics on Hot Jupiters

Abstract: We use results of shallow-water magnetohydrodynamics to place estimates on the minimum magnetic field strengths required to cause atmospheric wind variations (and therefore westward-venturing hotspots) for a data set 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 whi… Show more

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Cited by 13 publications
(11 citation statements)
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“…As a result of this assumption, we apply the drag only in the zonal (east-west) direction. This assumption remains reasonable when the magnetic Reynolds number is less than 1 (Menou 2012;Hindle et al 2021bHindle et al , 2021a. The magnetic Reynolds number can be approximated by et al 2021a), where U is the zonal wind speed, H is the pressure scale height, and η is the magnetic resistivity.…”
Section: Our Magnetic Drag Treatmentmentioning
confidence: 99%
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“…As a result of this assumption, we apply the drag only in the zonal (east-west) direction. This assumption remains reasonable when the magnetic Reynolds number is less than 1 (Menou 2012;Hindle et al 2021bHindle et al , 2021a. The magnetic Reynolds number can be approximated by et al 2021a), where U is the zonal wind speed, H is the pressure scale height, and η is the magnetic resistivity.…”
Section: Our Magnetic Drag Treatmentmentioning
confidence: 99%
“…The quintessential category of these planets is ultrahot Jupiters (UHJs), which orbit so close to their host star that their equilibrium temperatures exceed ∼2200 K. The extreme temperatures of these planets warrant a careful consideration of the relevant physical processes included in the models, as the increased irradiation results in different dominant mechanisms than those of their cooler cousins, "normal" hot Jupiters. While magnetic effects may begin to alter the circulation patterns of gas giant planets that reach temperatures ≈1500 K (Menou 2012;Rogers & Komacek 2014), it is not until planets reach an equilibrium temperature 2000 K that nonideal MHD effects are predicted to become very strong due to the coupling between the circulation and atmospheric magnetic field, potentially resulting in effects such as hot spot reversals (Hindle et al 2021a). Since no solar system analog exists for these planets, intricate multidimensional atmospheric modeling is critical for understanding and interpreting observations of their atmospheres.…”
Section: Introductionmentioning
confidence: 99%
“…from Parmentier et al (2021), suggesting even warmer daysides than expected from current theory. In our ∼1300 K sample, the hotter than expected dayside temperatures are further interesting due to their equilibrium temperature being below the threshold where MHD effects begin to affect the day-night heat transport (Menou 2012;Rogers & Komacek 2014;Hindle et al 2021aHindle et al , 2021b. As a result, unconsidered MHD effects cannot explain why Qatar-1b and WASP-52b have warmer than expected daysides compared to the Parmentier et al (2021) models.…”
Section: Population Trendsmentioning
confidence: 76%
“…This could drive the observed variability in wind dynamics in addition to the standard gyres, vortices, and other hydrodynamic instabilities predicted by hydrodynamic GCMs (Fromang et al 2016;Tan & Komacek 2019). MHD simulations also predict variability of winds, especially of zonal winds in the hottest HJs which can entirely reverse from eastward to westward (Rogers & Komacek 2014;Hindle et al 2021). Our measured scale of variability motivates further exploration of these models and their predictions for the day-to-nightside winds typically observed with high-resolution transmission spectroscopy in addition to the zonal winds commonly studied by theorists.…”
Section: Expectations From Gcmsmentioning
confidence: 91%