TL;DR
This study investigates how surface $CO_{2}$ condensation affects the long-term habitability of rocky planets around Sun-like stars, considering different initial thermal states and star types using an advanced energy balance model.
Contribution
It introduces an energy balance model to analyze $CO_{2}$ ice condensation on warm and cold planets across various star types, extending previous models to include diverse initial conditions.
Findings
Warm start planets have a reduced range of $CO_{2}$ ice condensation zones.
Star type does not significantly influence condensation zones, but hotter stars increase the habitable zone fraction affected.
Classical habitable zone limits remain valid for warm start scenarios.
Abstract
The habitable zone is the region around a star where standing bodies of liquid water can be stable on a planetary surface. Its width is often assumed to be dictated by the efficiency of the carbonate-silicate cycle, which has maintained habitable surface conditions on our planet for billions of years. This cycle may be inhibited by surface condensation of significant amounts of ice, which is likely to occur on distant planets containing high enough levels of atmospheric . Such a process could permanently trap ice within the planet, threatening its long-term habitability. Recent work has modeled this scenario for initially cold and icy planetary bodies orbiting the Sun. Here, we use an advanced energy balance model to consider both initially warm and cold rapidly-rotating planets orbiting F - K stars. We show that the range of orbital…
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