The mineral clouds on HD 209458b and HD189733b
Ch. Helling (1), G. Lee (1), I. Dobbs-Dixon (2), N. Mayne (3), D. S., Amundsen (3), J. Khaimova (4,1), A.A. Unger (1), J. Manners (3), D. Acreman, (5), C. Smith (5) (1 - University of St Andrews, 2 - NYU Abu Dhabi, 3 -, University of Exeter, 4 - Brooklyn College New York

TL;DR
This study uses 3D atmosphere models to analyze mineral cloud formation in HD 209458b and HD 189733b, revealing complex, height-dependent mineral clouds and their impact on atmospheric composition and observed water features.
Contribution
It provides the first detailed comparison of mineral cloud formation in these two exoplanets using kinetic, non-equilibrium models, highlighting the importance of cloud modeling in interpreting observations.
Findings
Both planets are covered in mineral clouds throughout their atmospheres.
Cloud composition and location influence water feature strength in spectra.
Cloud formation modeling can resolve degeneracies in atmospheric retrievals.
Abstract
3D atmosphere model results are used to comparatively study the kinetic, non-equilibrium cloud formation in the atmospheres of two example planets guided by the giant gas planets HD209458b and HD189733b. Rather independently of hydrodynamic model differences, our cloud modelling suggests that both planets are covered in mineral clouds throughout the entire modelling domain. Both planets harbour chemically complex clouds that are made of mineral particles that have a height-dependent material composition and size. The remaining gas-phase element abundances strongly effects the molecular abundances of the atmosphere in the cloud forming regions. Hydrocarbon and cyanopolyyne molecules can be rather abundant in the inner, dense part of the atmospheres of HD189733b and HD209458b. No one value for metallicity and the C/O ratio can be used to describe an extrasolar planet. Our results…
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