Habitability of waterworlds: runaway greenhouses, atmospheric expansion and multiple climate states of pure water atmospheres
Colin Goldblatt

TL;DR
This paper explores the stable climate states of water-rich planets, showing how atmospheric expansion and planet size influence habitability and runaway greenhouse thresholds, revealing a narrow habitable zone for pure water atmospheres.
Contribution
It maps the stable climate states of pure water atmospheres across different planet sizes and solar constants, incorporating atmospheric expansion effects.
Findings
Four stable climate states identified for pure water atmospheres.
Habitable zone width depends on planet mass and atmospheric properties.
Venus-sized planets are most susceptible to runaway greenhouse effects.
Abstract
There are four different stable climate states for pure water atmospheres, as might exist on so-called "waterworlds". I map these as a function of solar constant for planets ranging in size from Mars size to 10 Earth-mass. The states are: globally ice covered (Ts< 245K), cold and damp (270 < Ts< 290K), hot and moist (350< Ts< 550K) and very hot and dry (Ts< 900K). No stable climate exists for 290< Ts < 350K or 550 < Ts < 900K. The union of hot moist and cold damp climates describe the liquid water habitable zone, the width and location of which depends on planet mass. At each solar constant, two or three different climate states are stable. This is a consequence of strong non-linearities in both thermal emission and the net absorption of sunlight. Across the range of planet sizes, I account for the atmospheres expanding to high altitudes as they warm. The emitting and absorbing…
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