Water loss from Earth-sized planets in the habitable zones of ultracool dwarfs: Implications for the planets of TRAPPIST-1
Emeline Bolmont, Franck Selsis, James E. Owen, Ignasi Ribas, Sean N., Raymond, J\'er\'emy Leconte, Michael Gillon

TL;DR
This study models water loss in Earth-sized planets within the habitable zones of ultracool dwarfs, revealing that planets can retain significant water despite early hot phases, especially in the 0.04-0.06 solar mass range, with implications for habitability.
Contribution
It provides the first detailed modeling of water retention considering recent XUV emission limits, focusing on the TRAPPIST-1 system and the entire UCD mass range.
Findings
Planets in the 0.04-0.06 solar mass range can retain substantial water.
TRAPPIST-1b and c may have lost up to 15 Earth Oceans of water.
Planet d might have lost less than 1 Earth Ocean, remaining potentially habitable.
Abstract
Ultracool dwarfs (UCD; K) cool to settle on the main sequence after 1 Gyr. For brown dwarfs, this cooling never stops. Their habitable zone (HZ) thus sweeps inward at least during the first Gyr of their lives. Assuming they possess water, planets found in the HZ of UCDs have experienced a runaway greenhouse phase too hot for liquid water prior to entering the HZ. It has been proposed that such planets are desiccated by this hot early phase and enter the HZ as dry worlds. Here we model the water loss during this pre-HZ hot phase taking into account recent upper limits on the XUV emission of UCDs and using 1D radiation-hydrodynamic simulations. We address the whole range of UCDs but also focus on the planets recently found around the dwarf TRAPPIST-1. Despite assumptions maximizing the FUV-photolysis of water and the XUV-driven escape of…
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