2015
DOI: 10.1146/annurev-astro-082214-122522
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On the Cool Side: Modeling the Atmospheres of Brown Dwarfs and Giant Planets

Abstract: The atmosphere of a brown dwarf or extrasolar giant planet controls the spectrum of radiation emitted by the object and regulates its cooling over time. While the study of these atmospheres has been informed by decades of experience modeling stellar and planetary atmospheres, the distinctive characteristics of these objects present unique challenges to forward modeling. In particular, complex chemistry arising from molecule-rich atmospheres, molecular opacity line lists (sometimes running to 10 billion absorpt… Show more

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Cited by 208 publications
(189 citation statements)
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References 200 publications
(226 reference statements)
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“…However, as the atmosphere cools and becomes more neutral, the ability of the atmosphere to sustain these magnetic features becomes less clear. Concurrently, the low temperature of the atmospheres allows for the formation of dust condensates and clouds that influence the emergent stellar flux (e.g., Marley & Robinson 2015). Thus, in UCD atmospheres, there is some ambiguity with regard to the dominant processes generating photometric variability, especially at the M/ L transition, whether magnetic spots or clouds (Gizis et al 2015).…”
Section: Photometric Variabilitymentioning
confidence: 99%
“…However, as the atmosphere cools and becomes more neutral, the ability of the atmosphere to sustain these magnetic features becomes less clear. Concurrently, the low temperature of the atmospheres allows for the formation of dust condensates and clouds that influence the emergent stellar flux (e.g., Marley & Robinson 2015). Thus, in UCD atmospheres, there is some ambiguity with regard to the dominant processes generating photometric variability, especially at the M/ L transition, whether magnetic spots or clouds (Gizis et al 2015).…”
Section: Photometric Variabilitymentioning
confidence: 99%
“…The evolution of brown dwarfs and the substellar boundary itself are largely understood based on theoretical work over the last two decades (e.g., Saumon et al 1994;Baraffe et al 1995;Burrows et al 1997;Chabrier & Baraffe 1997;Lodders 1999;Chabrier et al 2000;Burrows et al 2001;Baraffe et al 2003;Saumon & Marley 2008;MacDonald & Mullan 2009;Baraffe et al 2015). Broadly speaking, the interior physics of evolutionary models over this time has remained the same, while the treatment of the surface boundary conditions has advanced greatly due to improved molecular line lists, chemistry, and cloud modeling (see a recent review by Marley & Robinson 2015). Clouds in particular have long thought to be the key to explaining major variations in the emergent flux of brown dwarfs, especially in the change from L to T spectral types (the L/T transition).…”
Section: Introductionmentioning
confidence: 99%
“…gas and cloud opacities, gas-phase chemistry (kinetic or LTE), hydrodynamics (HD), magnetohydrodynamics (MHD), and cloud formation. The radiative transfer problem and the gas-phase chemical abundances have achieved rather high standards as core problems of atmosphere modelling and data analysis (see review by Marley & Robinson 2015, also Benneke 2015. HD and MHD have a long standing tradition in meteorology and in solar physics, respectively.…”
Section: Introductionmentioning
confidence: 99%