The Abundance of Atmospheric CO2 in Ocean Exoplanets: A Novel CO2 Deposition Mechanism

We consider super-Earth sized planets which have a water mass fraction that is large enough to form an external mantle composed of high pressure water ice polymorphs and that lack a substantial H/He atmosphere. We consider such planets in their habitable zone so that their outermost condensed mantle...

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Main Authors: Levi, Amit, Sasselov, Dimitar, Podolak, Morris
Format: Text
Language:unknown
Published: arXiv 2016
Subjects:
Online Access:https://dx.doi.org/10.48550/arxiv.1609.08185
https://arxiv.org/abs/1609.08185
id ftdatacite:10.48550/arxiv.1609.08185
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spelling ftdatacite:10.48550/arxiv.1609.08185 2023-05-15T18:18:32+02:00 The Abundance of Atmospheric CO2 in Ocean Exoplanets: A Novel CO2 Deposition Mechanism Levi, Amit Sasselov, Dimitar Podolak, Morris 2016 https://dx.doi.org/10.48550/arxiv.1609.08185 https://arxiv.org/abs/1609.08185 unknown arXiv https://dx.doi.org/10.3847/1538-4357/aa5cfe arXiv.org perpetual, non-exclusive license http://arxiv.org/licenses/nonexclusive-distrib/1.0/ Earth and Planetary Astrophysics astro-ph.EP FOS Physical sciences article-journal Article ScholarlyArticle Text 2016 ftdatacite https://doi.org/10.48550/arxiv.1609.08185 https://doi.org/10.3847/1538-4357/aa5cfe 2022-04-01T11:14:04Z We consider super-Earth sized planets which have a water mass fraction that is large enough to form an external mantle composed of high pressure water ice polymorphs and that lack a substantial H/He atmosphere. We consider such planets in their habitable zone so that their outermost condensed mantle is a global deep liquid ocean. For these ocean planets we investigate potential internal reservoirs of CO2; the amount of CO2 dissolved in the ocean for the various saturation conditions encountered, and the ocean-atmosphere exchange flux of CO2. We find that in steady state the abundance of CO2 in the atmosphere has two possible states. When the wind-driven circulation is the dominant CO2 exchange mechanism, an atmosphere of tens of bars of CO2 results, where the exact value depends on the subtropical ocean surface temperature and the deep ocean temperature. When sea-ice formation, acting on these planets as a CO2 deposition mechanism, is the dominant exchange mechanism, an atmosphere of a few bars of CO2 is established. The exact value depends on the subpolar surface temperature. Our results suggest the possibility of a negative feedback mechanism, unique to water planets, where a reduction in the subpolar temperature drives more CO2 into the atmosphere to increase the greenhouse effect. : 114 pages, 55 figures, submitted to the astrophysical journal Text Sea ice DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Earth and Planetary Astrophysics astro-ph.EP
FOS Physical sciences
spellingShingle Earth and Planetary Astrophysics astro-ph.EP
FOS Physical sciences
Levi, Amit
Sasselov, Dimitar
Podolak, Morris
The Abundance of Atmospheric CO2 in Ocean Exoplanets: A Novel CO2 Deposition Mechanism
topic_facet Earth and Planetary Astrophysics astro-ph.EP
FOS Physical sciences
description We consider super-Earth sized planets which have a water mass fraction that is large enough to form an external mantle composed of high pressure water ice polymorphs and that lack a substantial H/He atmosphere. We consider such planets in their habitable zone so that their outermost condensed mantle is a global deep liquid ocean. For these ocean planets we investigate potential internal reservoirs of CO2; the amount of CO2 dissolved in the ocean for the various saturation conditions encountered, and the ocean-atmosphere exchange flux of CO2. We find that in steady state the abundance of CO2 in the atmosphere has two possible states. When the wind-driven circulation is the dominant CO2 exchange mechanism, an atmosphere of tens of bars of CO2 results, where the exact value depends on the subtropical ocean surface temperature and the deep ocean temperature. When sea-ice formation, acting on these planets as a CO2 deposition mechanism, is the dominant exchange mechanism, an atmosphere of a few bars of CO2 is established. The exact value depends on the subpolar surface temperature. Our results suggest the possibility of a negative feedback mechanism, unique to water planets, where a reduction in the subpolar temperature drives more CO2 into the atmosphere to increase the greenhouse effect. : 114 pages, 55 figures, submitted to the astrophysical journal
format Text
author Levi, Amit
Sasselov, Dimitar
Podolak, Morris
author_facet Levi, Amit
Sasselov, Dimitar
Podolak, Morris
author_sort Levi, Amit
title The Abundance of Atmospheric CO2 in Ocean Exoplanets: A Novel CO2 Deposition Mechanism
title_short The Abundance of Atmospheric CO2 in Ocean Exoplanets: A Novel CO2 Deposition Mechanism
title_full The Abundance of Atmospheric CO2 in Ocean Exoplanets: A Novel CO2 Deposition Mechanism
title_fullStr The Abundance of Atmospheric CO2 in Ocean Exoplanets: A Novel CO2 Deposition Mechanism
title_full_unstemmed The Abundance of Atmospheric CO2 in Ocean Exoplanets: A Novel CO2 Deposition Mechanism
title_sort abundance of atmospheric co2 in ocean exoplanets: a novel co2 deposition mechanism
publisher arXiv
publishDate 2016
url https://dx.doi.org/10.48550/arxiv.1609.08185
https://arxiv.org/abs/1609.08185
genre Sea ice
genre_facet Sea ice
op_relation https://dx.doi.org/10.3847/1538-4357/aa5cfe
op_rights arXiv.org perpetual, non-exclusive license
http://arxiv.org/licenses/nonexclusive-distrib/1.0/
op_doi https://doi.org/10.48550/arxiv.1609.08185
https://doi.org/10.3847/1538-4357/aa5cfe
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