The Ice Cap Zone: A Unique Habitable Zone for Ocean Worlds
Ramses M. Ramirez, Amit Levi

TL;DR
This paper proposes a new habitable zone concept called the Ice Cap Zone, where ocean worlds with subpolar sea ice can sustain habitability through a CO2 cycle, especially around certain star types and planetary conditions.
Contribution
It models a novel CO2 mobilization mechanism on ocean worlds, extending habitable zone boundaries and predicting observable atmospheric C/O ratios for JWST.
Findings
The mechanism can operate on rapidly rotating ocean worlds.
Habitable zones extend from 0.0428 to 1.65 AU depending on star type.
C/O ratios around 0.5 are predicted for atmospheres, testable by JWST.
Abstract
Traditional definitions of the habitable zone assume that habitable planets contain a carbonate-silicate cycle that regulates CO2 between the atmosphere, surface, and the interior. Such theories have been used to cast doubt on the habitability of ocean worlds. However, Levi et al (2017) have recently proposed a mechanism by which CO2 is mobilized between the atmosphere and the interior of an ocean world. At high enough CO2 pressures, sea ice can become enriched in CO2 clathrates and sink after a threshold density is achieved. The presence of subpolar sea ice is of great importance for habitability in ocean worlds. It may moderate the climate and is fundamental in current theories of life formation in diluted environments. Here, we model the Levi et al. mechanism and use latitudinally-dependent non-grey energy balance and single-column radiative-convective climate models and find that…
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