Exoplanets under consideration for the Rocky Worlds DDT. Planets above the cosmic shoreline are expected to have lost their atmosphere. The circled exoplanets have already been observed in emission during JWST’s first three cycles. The exoplanets for which the observations concluded there is no atmosphere are in red. We also added the Solar System terrestrial planets. The XUV irradiation is computed from Zahnle & Catling (2017). — astro-ph.EP
JWST observations of the secondary eclipse of TRAPPIST-1 b at 12.8 and 15 microns revealed a very bright dayside. These measurements are consistent with an absence of atmosphere. Previous 1D atmospheric modeling also excludes — at first sight — CO2-rich atmospheres.
However, only a subset of the possible atmosphere types has been explored and ruled out to date. Recently, a full thermal phase curve of the planet at 15 microns with JWST has also been observed, allowing for more information on the thermal structure of the planet. We first looked for atmospheres capable of producing a dayside emission compatible with secondary eclipse observations. We then tried to determine which of these are compatible with the observed thermal phase curve.
We used a 1D radiative-convective model and a 3D global climate model (GCM) to simulate a wide range of atmospheric compositions and surface pressures. We then produced observables from these simulations and compared them to available emission observations.
We found several families of atmospheres compatible at 2-sigma with the eclipse observations. Among them, some feature a flat phase curve and can be ruled out with the observation, and some produce a phase curve still compatible with the data (i.e., thin N2-CO2 atmospheres, and CO2 atmospheres rich in hazes). We also highlight different 3D effects that could not be predicted from 1D studies (redistribution efficiency, atmospheric collapse).
The available observations of TRAPPIST-1 b are consistent with an airless planet, which is the most likely scenario. A second possibility is a thin CO2-poor residual atmosphere. However, our study shows that different atmospheric scenarios can result in a high eclipse depth at 15 microns. It may therefore be hazardous, in general, to conclude on the presence of an atmosphere from a single photometric point.
Sketches of the different atmospheric scenarios studied in depth in this work, as seen from the North pole. — astro-ph.EP
Alice Maurel, Martin Turbet, Elsa Ducrot, Jérémy Leconte, Guillaume Chaverot, Gwenael Milcareck, Alexandre Revol, Benjamin Charnay, J. Thomas Fauchez, Michaël Gillon, Alexandre Mechineau, Emeline Bolmont, Ehouarn Millour, Franck Selsis, Jean-Philippe Beaulieu, Pierre Drossart
Comments: 26 pages, 24 figures, accepted for publication in Astronomy and Astrophysics
Subjects: Earth and Planetary Astrophysics (astro-ph.EP)
Cite as: arXiv:2509.02120 [astro-ph.EP] (or arXiv:2509.02120v1 [astro-ph.EP] for this version)
https://doi.org/10.48550/arXiv.2509.02120
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Submission history
From: Alice Maurel
[v1] Tue, 2 Sep 2025 09:16:33 UTC (4,472 KB)
https://arxiv.org/abs/2509.02120
Astrobiology,