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Day-night cloud asymmetry prevents early oceans on Venus but not on Earth.
Turbet, Martin; Bolmont, Emeline; Chaverot, Guillaume; Ehrenreich, David; Leconte, Jérémy; Marcq, Emmanuel.
Afiliação
  • Turbet M; Observatoire astronomique de l'Université de Genève, Versoix, Switzerland. martin.turbet@unige.ch.
  • Bolmont E; Observatoire astronomique de l'Université de Genève, Versoix, Switzerland.
  • Chaverot G; Observatoire astronomique de l'Université de Genève, Versoix, Switzerland.
  • Ehrenreich D; Observatoire astronomique de l'Université de Genève, Versoix, Switzerland.
  • Leconte J; Laboratoire d'astrophysique de Bordeaux, Université de Bordeaux, CNRS, B18N, Pessac, France.
  • Marcq E; LATMOS/IPSL, UVSQ, Université Paris-Saclay, Sorbonne Université, CNRS, Guyancourt, France.
Nature ; 598(7880): 276-280, 2021 10.
Article em En | MEDLINE | ID: mdl-34645997
ABSTRACT
Earth has had oceans for nearly four billion years1 and Mars had lakes and rivers 3.5-3.8 billion years ago2. However, it is still unknown whether water has ever condensed on the surface of Venus3,4 because the planet-now completely dry5-has undergone global resurfacing events that obscure most of its history6,7. The conditions required for water to have initially condensed on the surface of Solar System terrestrial planets are highly uncertain, as they have so far only been studied with one-dimensional numerical climate models3 that cannot account for the effects of atmospheric circulation and clouds, which are key climate stabilizers. Here we show using three-dimensional global climate model simulations of early Venus and Earth that water clouds-which preferentially form on the nightside, owing to the strong subsolar water vapour absorption-have a strong net warming effect that inhibits surface water condensation even at modest insolations (down to 325 watts per square metre, that is, 0.95 times the Earth solar constant). This shows that water never condensed and that, consequently, oceans never formed on the surface of Venus. Furthermore, this shows that the formation of Earth's oceans required much lower insolation than today, which was made possible by the faint young Sun. This also implies the existence of another stability state for present-day Earth the 'steam Earth', with all the water from the oceans evaporated into the atmosphere.

Texto completo: 1 Base de dados: MEDLINE Tipo de estudo: Prognostic_studies Idioma: En Ano de publicação: 2021 Tipo de documento: Article

Texto completo: 1 Base de dados: MEDLINE Tipo de estudo: Prognostic_studies Idioma: En Ano de publicação: 2021 Tipo de documento: Article