Day-night cloud asymmetry prevents early oceans on Venus but not on Earth
Martin Turbet, Emeline Bolmont, Guillaume Chaverot, David Ehrenreich,, Jeremy Leconte, Emmanuel Marcq

TL;DR
This study uses 3D climate models to show that cloud asymmetry on early Venus prevented water condensation, explaining why Venus remained dry, while Earth’s conditions allowed oceans to form under lower insolation levels.
Contribution
It demonstrates the critical role of night-side cloud formation in inhibiting water condensation on Venus, a factor not captured by previous 1D models.
Findings
Water clouds on early Venus prevented surface water condensation.
Earth's oceans could form at lower insolation levels due to faint young Sun.
Venus likely remained dry because of cloud-induced warming effects.
Abstract
Earth has had oceans for nearly four billion years and Mars had lakes and rivers 3.5-3.8 billion years ago. 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…
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