Atmospheres of low-mass planets: the "boil-off"
James E. Owen (IAS), Yanqin Wu (Toronto)

TL;DR
This paper proposes a 'boil-off' process where low-mass planets lose most of their primordial atmospheres shortly after disk dispersal, explaining the observed size distribution of Kepler planets.
Contribution
It introduces a new atmospheric mass-loss mechanism occurring immediately after disk dispersal, affecting planet radii and envelope retention.
Findings
Planets lose about 90% of their initial envelope within a million years.
The process explains the absence of planets larger than 2.5 Earth radii in Kepler data.
Atmospheric cooling and contraction halt mass-loss, leaving small residual envelopes.
Abstract
We show that, for a low-mass planet that orbits its host star within a few tenths of an AU (like the majority of the {\it Kepler} planets), the atmosphere it was able to accumulate while embedded in the proto-planetary disk may not survive unscathed after the disk disperses. This gas envelope, if more massive than a few percent of the core (with a mass below ), has a cooling time that is much longer than the time-scale on which the planet exits the disk. As such, it could not have contracted significantly from its original size, of order the Bondi radius. So a newly exposed proto-planet would be losing mass via a Parker wind that is catalyzed by the stellar continuum radiation. This represents an intermediate stage of mass-loss, occurring soon after the disc has dispersed, but before the EUV/X-ray driven photoevaporation becomes relevant. The surface mass-loss induces a…
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