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Three-dimensional circulation driving chemical disequilibrium in WASP-43b

Three-dimensional circulation driving chemical disequilibrium in WASP-43b
Three-dimensional circulation driving chemical disequilibrium in WASP-43b
Spectral features in the observed spectra of exoplanets depend on the composition of their atmospheres. A good knowledge of the main atmospheric processes that drive the chemical distribution is therefore essential to interpret exoplanetary spectra. An atmosphere reaches chemical equilibrium if the rates of the forward and backward chemical reactions converge to the same value. However, there are atmospheric processes, such as atmospheric transport, that destabilize this equilibrium. In this work we study the changes in composition driven by a 3D wind field in WASP-43b using our Global Circulation Model, THOR. Our model uses validated temperature- and pressure-dependent chemical timescales that allow us to explore the disequilibrium chemistry of CO, CO2, H2O, and CH4. In WASP-43b the formation of the equatorial jet has an important impact on the chemical distribution of the different species across the atmosphere. At low latitudes the chemistry is longitudinally quenched, except for CO2 at solar abundances. The polar vortexes have a distinct chemical distribution since these are regions with lower temperature and atmospheric mixing. Vertical and latitudinal mixing have a secondary impact on the chemical transport. We determine graphically the effect of disequilibrium on the observed emission spectra. Our results do not show any significant differences in the emission spectra between the equilibrium and disequilibrium solutions for C/O = 0.5. However, if C/O is increased to 2.0, differences in the spectra due to the disequilibrium chemistry of CH4 become non-negligible. In some spectral ranges the emission spectra can have more than 15% departure from the equilibrium solution.
0004-637X
Mendonça, João M.
cb29fe08-eb94-4fad-8eba-eac1c5de491b
Tsai, Shang-min
fd5f43d2-042b-44a2-bf50-c556b74ad84e
Malik, Matej
3be444ea-4bfd-4f60-81d7-310298714867
Grimm, Simon L.
2e304876-a102-4be9-a7d0-cd58bc71bd5b
Heng, Kevin
11e4460d-9575-412c-b350-53e2ef459056
Mendonça, João M.
cb29fe08-eb94-4fad-8eba-eac1c5de491b
Tsai, Shang-min
fd5f43d2-042b-44a2-bf50-c556b74ad84e
Malik, Matej
3be444ea-4bfd-4f60-81d7-310298714867
Grimm, Simon L.
2e304876-a102-4be9-a7d0-cd58bc71bd5b
Heng, Kevin
11e4460d-9575-412c-b350-53e2ef459056

Mendonça, João M., Tsai, Shang-min, Malik, Matej, Grimm, Simon L. and Heng, Kevin (2018) Three-dimensional circulation driving chemical disequilibrium in WASP-43b. The Astrophysical Journal, 869 (2), [107]. (doi:10.3847/1538-4357/aaed23).

Record type: Article

Abstract

Spectral features in the observed spectra of exoplanets depend on the composition of their atmospheres. A good knowledge of the main atmospheric processes that drive the chemical distribution is therefore essential to interpret exoplanetary spectra. An atmosphere reaches chemical equilibrium if the rates of the forward and backward chemical reactions converge to the same value. However, there are atmospheric processes, such as atmospheric transport, that destabilize this equilibrium. In this work we study the changes in composition driven by a 3D wind field in WASP-43b using our Global Circulation Model, THOR. Our model uses validated temperature- and pressure-dependent chemical timescales that allow us to explore the disequilibrium chemistry of CO, CO2, H2O, and CH4. In WASP-43b the formation of the equatorial jet has an important impact on the chemical distribution of the different species across the atmosphere. At low latitudes the chemistry is longitudinally quenched, except for CO2 at solar abundances. The polar vortexes have a distinct chemical distribution since these are regions with lower temperature and atmospheric mixing. Vertical and latitudinal mixing have a secondary impact on the chemical transport. We determine graphically the effect of disequilibrium on the observed emission spectra. Our results do not show any significant differences in the emission spectra between the equilibrium and disequilibrium solutions for C/O = 0.5. However, if C/O is increased to 2.0, differences in the spectra due to the disequilibrium chemistry of CH4 become non-negligible. In some spectral ranges the emission spectra can have more than 15% departure from the equilibrium solution.

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More information

Accepted/In Press date: 29 October 2018
Published date: 17 December 2018

Identifiers

Local EPrints ID: 496768
URI: http://eprints.soton.ac.uk/id/eprint/496768
ISSN: 0004-637X
PURE UUID: 58b92c85-ef1a-44e5-8818-7e706804e676
ORCID for João M. Mendonça: ORCID iD orcid.org/0000-0002-6907-4476

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Date deposited: 08 Jan 2025 05:21
Last modified: 10 Jan 2025 03:21

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Contributors

Author: João M. Mendonça ORCID iD
Author: Shang-min Tsai
Author: Matej Malik
Author: Simon L. Grimm
Author: Kevin Heng

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