Distinguishing between wet and dry atmospheres of TRAPPIST-1 e and f
Fabian Wunderlich, Markus Scheucher, Mareike Godolt, John Lee, Grenfell, Franz Schreier, P. Christian Schneider, David J. Wilson, Alejandro, S\'anchez L\'opez, Manuel L\'opez Puertas, Heike Rauer

TL;DR
This study develops a coupled photochemical and radiative-convective model to analyze TRAPPIST-1 e and f atmospheres, proposing observational strategies to infer surface conditions and biosignatures with upcoming telescopes.
Contribution
It introduces a novel coupled atmospheric model validated against Solar System planets and applies it to TRAPPIST-1, suggesting methods to detect oceans and biospheres via transmission spectra.
Findings
Detection of CO could indicate an ocean.
Presence of CH₄ may suggest biosphere activity.
Combining 30 transits with ELT/JWST can reveal surface conditions.
Abstract
The nearby TRAPPIST-1 planetary system is an exciting target for characterizing the atmospheres of terrestrial planets. The planets e, f and g lie in the circumstellar habitable zone and could sustain liquid water on their surfaces. During the extended pre-main sequence phase of TRAPPIST-1, however, the planets may have experienced extreme water loss, leading to a desiccated mantle. The presence or absence of an ocean is challenging to determine with current and next generation telescopes. Therefore, we investigate whether indirect evidence of an ocean and/or a biosphere can be inferred from observations of the planetary atmosphere. We introduce a newly developed photochemical model for planetary atmospheres, coupled to a radiative-convective model and validate it against modern Earth, Venus and Mars. The coupled model is applied to the TRAPPIST-1 planets e and f, assuming different…
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