IMIS | Flanders Marine Institute
 

Flanders Marine Institute

Platform for marine research

IMIS

Publications | Institutes | Persons | Datasets | Projects | Maps
[ report an error in this record ]basket (0): add | show Print this page

Day–night cloud asymmetry prevents early oceans on Venus but not on Earth
Turbet, M.; Bolmont, E.; Chaverot, G.; Ehrenreich, D.; Leconte, J.; Marcq, E. (2021). Day–night cloud asymmetry prevents early oceans on Venus but not on Earth. Nature (Lond.) 598(7880): 276-280. https://dx.doi.org/10.1038/s41586-021-03873-w
In: Nature: International Weekly Journal of Science. Nature Publishing Group: London. ISSN 0028-0836; e-ISSN 1476-4687, more
Peer reviewed article  

Available in  Authors 

Authors  Top 
  • Turbet, M.
  • Bolmont, E., more
  • Chaverot, G.
  • Ehrenreich, D.
  • Leconte, J.
  • Marcq, E.

Abstract
    Earth has had oceans for nearly four billion years1 and Mars had lakes and rivers billion years ago2. However, it is still unknown whether water has ever condensed on the surface of Venus because the planet—now completely dry has undergone global resurfacing events that obscure most of its history. 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 models 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.

All data in the Integrated Marine Information System (IMIS) is subject to the VLIZ privacy policy Top | Authors