Atmospheric variability driven by radiative cloud feedback in brown dwarfs and directly imaged extrasolar giant planets
Xianyu Tan, Adam P. Showman

TL;DR
This study demonstrates that radiative cloud feedback can spontaneously cause atmospheric variability in brown dwarfs and directly imaged exoplanets, affecting their thermal and spectral properties on short timescales.
Contribution
It introduces a self-consistent, time-dependent one-dimensional model showing radiative cloud feedback as a natural driver of atmospheric variability in these objects.
Findings
Variability periods range from one to tens of hours.
Amplitude of temperature variability can reach hundreds of Kelvins.
The mechanism is robust across a wide parameter space.
Abstract
Growing observational evidence has suggested active meteorology in atmospheres of brown dwarfs (BDs) and directly imaged extrasolar giant planets (EGPs). In particular, a number of surveys have shown that near-IR brightness variability is common among L and T dwarfs. Despite initial understandings of atmospheric dynamics which is the major cause of the variability by previous studies, the detailed mechanism of variability remains elusive, and we need to seek a natural, self-consistent mechanism. Clouds are important in shaping the thermal structure and spectral properties of these atmospheres via large opacity, and we expect the same for inducing atmospheric variability. In this work, using a time-dependent one-dimensional model that incorporates a self-consistent coupling between the thermal structure, convective mixing, cloud radiative heating/cooling and condensation/evaporation of…
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