Airy worlds or barren rocks? On the survivability of secondary atmospheres around the TRAPPIST-1 planets

Fuente: arXiv
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Main Authors: Van Looveren, Gwenaël, Güdel, Manuel, Saikia, Sudeshna Boro, Kislyakova, Kristina
Format: Preprint
Published: 2024
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author Van Looveren, Gwenaël
Güdel, Manuel
Saikia, Sudeshna Boro
Kislyakova, Kristina
author_facet Van Looveren, Gwenaël
Güdel, Manuel
Saikia, Sudeshna Boro
Kislyakova, Kristina
contents In this work we aim to determine the atmospheric survivability of the TRAPPIST-1 planets by modelling the response of the upper atmosphere to incoming stellar high-energy radiation. Through this case study, we also aim to learn more about rocky planet atmospheres in the habitable zone around low-mass M dwarfs. We simulated the upper atmospheres using the Kompot code, a self-consistent thermo-chemical code. Specifically, we studied the atmospheric mass loss due to Jeans escape induced by stellar high-energy radiation. This was achieved through a grid of models that account for the differences in planetary properties, irradiances, and atmospheric properties, allowing the exploration of the different factors influencing atmospheric loss. The present-day irradiance of the TRAPPIST-1 planets would lead to the loss of an Earth's atmosphere within just some 100 Myr. Taking into account the much more active early stages of a low-mass M dwarf, the planets undergo a period of even more extreme mass loss, regardless of planetary mass or atmospheric composition. This indicates that it is unlikely that any significant atmosphere could survive for any extended amount of time around any of the TRAPPIST-1 planets. The assumptions used here allow us to generalise the results, and we conclude that the results tentatively indicate that this conclusion applies to all Earth-like planets in the habitable zones of low-mass M dwarfs.
format Preprint
id arxiv_https___arxiv_org_abs_2401_16490
institution arXiv
publishDate 2024
record_format arxiv
spellingShingle Airy worlds or barren rocks? On the survivability of secondary atmospheres around the TRAPPIST-1 planets
Van Looveren, Gwenaël
Güdel, Manuel
Saikia, Sudeshna Boro
Kislyakova, Kristina
Earth and Planetary Astrophysics
In this work we aim to determine the atmospheric survivability of the TRAPPIST-1 planets by modelling the response of the upper atmosphere to incoming stellar high-energy radiation. Through this case study, we also aim to learn more about rocky planet atmospheres in the habitable zone around low-mass M dwarfs. We simulated the upper atmospheres using the Kompot code, a self-consistent thermo-chemical code. Specifically, we studied the atmospheric mass loss due to Jeans escape induced by stellar high-energy radiation. This was achieved through a grid of models that account for the differences in planetary properties, irradiances, and atmospheric properties, allowing the exploration of the different factors influencing atmospheric loss. The present-day irradiance of the TRAPPIST-1 planets would lead to the loss of an Earth's atmosphere within just some 100 Myr. Taking into account the much more active early stages of a low-mass M dwarf, the planets undergo a period of even more extreme mass loss, regardless of planetary mass or atmospheric composition. This indicates that it is unlikely that any significant atmosphere could survive for any extended amount of time around any of the TRAPPIST-1 planets. The assumptions used here allow us to generalise the results, and we conclude that the results tentatively indicate that this conclusion applies to all Earth-like planets in the habitable zones of low-mass M dwarfs.
title Airy worlds or barren rocks? On the survivability of secondary atmospheres around the TRAPPIST-1 planets
topic Earth and Planetary Astrophysics
url https://arxiv.org/abs/2401.16490