Habitability of Terrestrial-Mass Planets in the HZ of M Dwarfs. I. H/He-Dominated Atmospheres
James E. Owen, Subhanjoy Mohanty

TL;DR
This study models atmospheric escape on terrestrial planets in M dwarf habitable zones, finding that only low-mass cores can lose thick H/He envelopes to become potentially habitable.
Contribution
It improves hydrodynamic escape modeling by including radiative cooling and transition to ballistic escape, refining predictions of atmospheric loss.
Findings
Lower mass-loss rates than previous estimates.
Planets with cores less than 0.9 M⊕ can lose enough H/He to be habitable.
Cores ≥1 M⊕ with 1% H/He envelopes remain uninhabitable.
Abstract
The ubiquity of M dwarfs, combined with the relative ease of detecting terrestrial-mass planets around them, has made them prime targets for finding and characterising planets in the "Habitable Zone" (HZ). However, Kepler finds that terrestrial-mass exoplanets are often born with voluminous H/He envelopes, comprising mass-fractions () %. If these planets retain such envelopes over Gyr timescales, they will not be "habitable" even within the HZ. Given the strong X-ray/UV fluxes of M dwarfs, we study whether sufficient envelope mass can be photoevaporated away for these planets to become habitable. We improve upon previous work by using hydrodynamic models that account for radiative cooling as well as the transition from hydrodynamic to ballistic escape. Adopting a template active M dwarf XUV spectrum, including stellar evolution, and considering both…
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