Magnetic Scaling Laws for the Atmospheres of Hot Giant Exoplanets
Kristen Menou

TL;DR
This paper develops scaling laws for magnetic effects in hot giant exoplanet atmospheres, linking ohmic dissipation and magnetic drag to temperature and magnetic field strength, with implications for planetary radius inflation.
Contribution
It introduces new scaling laws for magnetic drag and ohmic dissipation in hot Jupiter atmospheres, considering weak thermal ionization and magnetic field effects.
Findings
Ohmic dissipation increases rapidly with temperature above 1000 K.
Magnetic drag can significantly reduce atmospheric winds at high temperatures.
Peak ohmic dissipation occurs around 1600 K, potentially inflating planetary radii.
Abstract
We present scaling laws for advection, radiation, magnetic drag and ohmic dissipation in the atmospheres of hot giant exoplanets. In the limit of weak thermal ionization, ohmic dissipation increases with the planetary equilibrium temperature (T_eq >~ 1000 K) faster than the insolation power does, eventually reaching values >~ 1% of the insolation power, which may be sufficient to inflate the radii of hot Jupiters. At higher T_eq values still, magnetic drag rapidly brakes the atmospheric winds, which reduces the associated ohmic dissipation power. For example, for a planetary field strength B=10G, the fiducial scaling laws indicate that ohmic dissipation exceeds 1% of the insolation power over the equilibrium temperature range T_eq ~ 1300-2000 K, with a peak contribution at T_eq ~ 1600 K. Evidence for magnetically dragged winds at the planetary thermal photosphere could emerge in the…
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