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hal.structure.identifierLaboratoire d'Astrophysique de Bordeaux [Pessac] [LAB]
dc.contributor.authorKODAMA, T.
dc.contributor.authorGENDA, H.
dc.contributor.authorLECONTE, J.
dc.contributor.authorABE-OUCHI, A.
dc.date.issued2021
dc.identifier.issn2169-9097
dc.description.abstractEnThe climates of terrestrial planets with a small amount of water on their surface, called land planets, are significantly different from the climates of planets having a large amount of surface water. Land planets have a higher runaway greenhouse threshold than aqua planets, which extends the inner edge of the habitable zone inward. Land planets also have the advantage of avoiding global freezing due to drier tropics, leading to a lower planetary albedo. In this study, we systematically investigate the complete freezing limit for various surface water distributions using a three-dimensional dynamic atmospheric model. As in a previous study, we found that a land planet climate has dry tropics that result in less snow and fewer clouds. The complete freezing limit decreases from that for aqua planets (92% S<SUB>0</SUB>, where S<SUB>0</SUB> is Earth's present insolation) to that for land planets (77% S<SUB>0</SUB>) with an increasing dry area. Values for the complete freezing limit for zonally uniform surface water distributions are consistently lower than those for meridionally uniform surface water distribution. This is because the surface water distribution in the tropics in the meridionally uniform cases causes ice-albedo feedback until a planet lapses into the complete freezing state. For a surface water distribution using the topographies of the terrestrial planets, the complete freezing limit has values near those for the meridionally uniform cases. Our results indicate that the water distribution is important for the onset of a global ice-covered state for Earth-like exoplanets.
dc.language.isoen
dc.publisherWiley-Blackwell
dc.rights.urihttp://hal.archives-ouvertes.fr/licences/copyright/
dc.subject.enexoplanets
dc.subject.enhabitable planets
dc.subject.enGCM
dc.subject.enfreezing limit
dc.subject.ensnowball state
dc.title.enThe Onset of a Globally Ice-Covered State for a Land Planet
dc.typeArticle de revue
dc.identifier.doi10.1029/2021JE006975
dc.subject.halPlanète et Univers [physics]
dc.identifier.arxiv2111.12913
bordeaux.journalJournal of Geophysical Research. Planets
bordeaux.volume126
bordeaux.peerReviewedoui
hal.identifierinsu-03678876
hal.version1
hal.popularnon
hal.audienceInternationale
hal.origin.linkhttps://hal.archives-ouvertes.fr//insu-03678876v1
bordeaux.COinSctx_ver=Z39.88-2004&amp;rft_val_fmt=info:ofi/fmt:kev:mtx:journal&amp;rft.jtitle=Journal%20of%20Geophysical%20Research.%20Planets&amp;rft.date=2021&amp;rft.volume=126&amp;rft.eissn=2169-9097&amp;rft.issn=2169-9097&amp;rft.au=KODAMA,%20T.&amp;GENDA,%20H.&amp;LECONTE,%20J.&amp;ABE-OUCHI,%20A.&amp;rft.genre=article


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