The Influence of Clouds and Deuterium-Burning on Brown Dwarf Habitable Zones
Kayla J. Smith, Mark S. Marley

TL;DR
This study uses advanced brown dwarf evolution models to analyze how clouds and deuterium burning influence the habitability duration of orbiting planets, revealing effects absent in previous analytic models.
Contribution
It introduces new equilibrium temperature evolution tracks incorporating clouds and deuterium burning, improving understanding of brown dwarf habitability zones.
Findings
Cloud presence extends habitable zones by slowing cooling.
Deuterium burning creates 'sweet spots' where habitability duration is similar across different brown dwarf masses.
Modern models reveal effects absent in prior analytic cooling approximations.
Abstract
To better understand the potential habitability of planets orbiting brown dwarfs, this work presents a new set of equilibrium temperature evolution tracks. Unlike most previous work that relied on analytic scaling relationships for brown dwarf luminosity evolution, we use the outputs of modern brown dwarf evolution models that account for the effects of deuterium burning, cloud formation and dissipation, and the most recent atmospheric opacities. While clouds are present, brown dwarfs cool more slowly than if they did not have clouds, allowing orbiting planets to remain in the habitable zone (HZ) for millions of years longer than previously estimated. Similarly, we find that during the deuterium-burning phase of brown dwarfs, which also slows the evolution, planets at the same orbital radius but orbiting brown dwarfs of different masses can remain in the HZ for the same duration,…
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