4.7 Article

A New Sedimentation Model for Greater Cloud Diversity in Giant Exoplanets and Brown Dwarfs

Journal

ASTROPHYSICAL JOURNAL
Volume 925, Issue 1, Pages -

Publisher

IOP Publishing Ltd
DOI: 10.3847/1538-4357/ac307a

Keywords

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Funding

  1. NASA
  2. NASA Astrophysics Division
  3. NASA Planetary Science Division

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The presence and distribution of atmospheric condensates play a critical role in the observed atmospheric spectrum of exoplanets and brown dwarfs. The Ackerman and Marley methodology, implemented in the open-source software Virga, is widely used to study cloudy atmospheres. However, comparisons with more complex models have revealed inconsistencies. In this study, the researchers extended the original methodology to allow for non-constant values of the input parameter f (sed), leading to better agreement with complex models.
The observed atmospheric spectrum of exoplanets and brown dwarfs depends critically on the presence and distribution of atmospheric condensates. The Ackerman and Marley methodology for predicting the vertical distribution of condensate particles is widely used to study cloudy atmospheres and has recently been implemented in an open-source python package, Virga. The model relies upon input parameter f (sed), the sedimentation efficiency, which until now has been held constant. The relative simplicity of this model renders it useful for retrieval studies due to its rapidly attainable solutions. However, comparisons with more complex microphysical models such as CARMA have highlighted inconsistencies between the two approaches, namely that the cloud parameters needed for radiative transfer produced by Virga are dissimilar to those produced by CARMA. To address these discrepancies, we have extended the original Ackerman and Marley methodology in Virga to allow for non-constant f (sed) values, in particular, those that vary with altitude. We discuss one such parameterization and compare the cloud mass mixing ratio produced by Virga with constant and variable f (sed) profiles to that produced by CARMA. We find that the variable f (sed) formulation better captures the profile produced by CARMA with heterogeneous nucleation, yet performs comparatively to constant f (sed) for homogeneous nucleation. In general, Virga has the capacity to handle any f (sed) with an explicit anti-derivative, permitting a plethora of alternative cloud profiles that are otherwise unattainable by constant f (sed) values. The ensuing flexibility has the potential to better agree with increasingly complex models and observed data.

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