The Temporal Onset of Habitability For Earth-Like Planets
Johnny Seales, Adrian Lenardic

TL;DR
This paper models how the timing of habitability for Earth-like planets depends on planetary and stellar evolution, revealing that planets of the same age can differ significantly in habitability due to tectonic and energy factors.
Contribution
It introduces a comprehensive model integrating planetary cooling, tectonics, and climate to predict the variable timing of habitability for Earth-like exoplanets.
Findings
Habitability onset varies by billions of years among similar planets.
Planets can become habitable later if early conditions are unfavorable.
Tectonic efficiency influences whether planets reside in the habitable zone.
Abstract
The ability of a planet to maintain surface water, key to life as we know it, depends on solar and planetary energy. As a star ages, it delivers more energy to a planet. As a planet ages it produces less internal heat, which leads to cooling. For the Earth, interior cooling connects to plate tectonics - the surface manifestation of convection within the Earth's interior. This process cycles volatiles (CO2 and water) between surface and interior reservoirs, which affects planetary climate. Cycling rates depend on the efficiency of plate tectonic cooling. That efficiency remains debated and multiple hypotheses have been put forth. Geological proxy data allow us to validate these hypotheses accounting for model and data uncertainty. Multiple models pass the validation test. Those models define a distribution for terrestrial exoplanets akin to Earth, accounting for variations in tectonic…
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Taxonomy
TopicsAstro and Planetary Science · Scientific Research and Discoveries · Stellar, planetary, and galactic studies
