Habitable Planets Around White and Brown Dwarfs: The Perils of a Cooling Primary
Rory Barnes, Rene Heller

TL;DR
This paper explores the challenges of habitability for planets around white and brown dwarfs, emphasizing the risks of water loss and greenhouse effects due to their cooling nature and UV radiation, which may prevent life from developing.
Contribution
It provides a detailed analysis of the habitability prospects of planets orbiting white and brown dwarfs, highlighting the effects of their cooling and UV emission on planetary water retention and climate stability.
Findings
Planets around white dwarfs are unlikely to retain water due to UV-driven photolysis.
Tidal heating may trigger greenhouse effects even with minimal orbital eccentricity.
The specific planets KOI 55.01 and 55.02 are unlikely to become habitable.
Abstract
White and brown dwarfs are astrophysical objects that are bright enough to support an insolation habitable zone (IHZ). Unlike hydrogen-burning stars, they cool and become less luminous with time, and hence their IHZ moves in with time. The inner edge of the IHZ is defined as the orbital radius at which a planet may enter a moist or runaway greenhouse, phenomena that can remove a planet's surface water forever. Thus, as the IHZ moves in, planets that enter it may no longer have any water, and are still uninhabitable. Additionally, the close proximity of the IHZ to the primary leads to concern that tidal heating may also be strong enough to trigger a runaway greenhouse, even for orbital eccentricities as small as 10^-6. Water loss occurs due to photolyzation by UV photons in the planetary stratosphere, followed by hydrogen escape. Young white dwarfs emit a large amount of these photons as…
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