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  3. Revisiting the Scattering Greenhouse Effect of CO2 Ice Clouds

Revisiting the Scattering Greenhouse Effect of CO2 Ice Clouds

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DOI
10.7892/boris.87727
Publisher DOI
10.3847/2041-8205/817/2/L18
Abstract
Carbon dioxide ice clouds are thought to play an important role for cold terrestrial planets with thick CO2 dominated atmospheres. Various previous studies showed that a scattering greenhouse effect by carbon dioxide ice clouds could result in a massive warming of the planetary surface. However, all of these studies only employed simplified two-stream radiative transfer schemes to describe the anisotropic scattering. Using accurate radiative transfer models with a general discrete ordinate method, this study revisits this important effect and shows that the positive climatic impact of carbon dioxide clouds was strongly overestimated in the past. The revised scattering greenhouse effect can have important implications for the early Mars, but also for planets like the early Earth or the position of the outer boundary of the habitable zone.
Date Issued
2016-02
Publication Type
Article
Subject(s)
500 Science > 520 Astronomy
Language(s)
en
Author(s)
Kitzmann, Daniel  orcid-logo
Center for Space and Habitability (CSH)  
Additional Credits
Center for Space and Habitability (CSH)  
Journal
Astrophysical Journal Letters
Publisher
Institute of Physics Publishing IOP
ISSN
2041-8205
Access(Rights)
open.access
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