Exoplanetology: Exoplanets & Exomoons

Pursuing Truth: Improving Retrievals on Mid-Infrared Exo-Earth Spectra with Physically Motivated Water Abundance Profiles and Cloud Models

By Keith Cowing
Status Report
astro-ph.EP
August 20, 2024
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Pursuing Truth: Improving Retrievals on Mid-Infrared Exo-Earth Spectra with Physically Motivated Water Abundance Profiles and Cloud Models
Ground truths and disk-integrated MIR spectra for the NP, SP, and EqC Earth views introduced in Section 2.3.2. Solid lines indicate the data for January and dashed lines represent the month July. Color-shaded areas indicate the uncertainties on the data. Left column: Ground truth P−T profiles. Center column: Ground truth abundance profiles for CO2,O3,CH4, and H2O. Right column: R = 50 disk-integrated monthly averaged Earth spectra. The color-shaded areas indicate the S/N = 10 LIFEsim-noise level. — astro-ph.EP

Atmospheric retrievals are widely used to constrain exoplanet properties from observed spectra. We investigate how the common nonphysical retrieval assumptions of vertically constant molecule abundances and cloud-free atmospheres affect our characterization of an exo-Earth (an Earth-twin orbiting a Sun-like star).

Specifically, we use a state-of-the-art retrieval framework to explore how assumptions for the H2O profile and clouds affect retrievals. In a first step, we validate different retrieval models on a low-noise simulated 1D mid-infrared (MIR) spectrum of Earth. Thereafter, we study how these assumptions affect the characterization of Earth with the Large Interferometer For Exoplanets (LIFE).

We run retrievals on LIFE mock observations based on real disk-integrated MIR Earth spectra. The performance of different retrieval models is benchmarked against ground truths derived from remote sensing data. We show that assumptions for the H2O abundance and clouds directly affect our characterization.

Overall, retrievals that use physically motivated models for the H2O profile and clouds perform better on the empirical Earth data. For observations of Earth with LIFE, they yield accurate estimates for the radius, pressure-temperature structure, and the abundances of CO2, H2O, and O3. Further, at R=100, a reliable and bias-free detection of the biosignature CH4 becomes feasible.

We conclude that the community must use a diverse range of models for temperate exoplanet atmospheres to build an understanding of how different retrieval assumptions can affect the interpretation of exoplanet spectra. This will enable the characterization of distant habitable worlds and the search for life with future space-based instruments.

Björn S. Konrad, Sascha P. Quanz, Eleonora Alei, Robin Wordsworth

Comments: Re-submitted to ApJ after a first iteration with referee; 17 pages (main text incl. 9 figures and 5 tables) + appendix; comments are welcome
Subjects: Earth and Planetary Astrophysics (astro-ph.EP); Instrumentation and Methods for Astrophysics (astro-ph.IM)
Cite as: arXiv:2408.09129 [astro-ph.EP] (or arXiv:2408.09129v1 [astro-ph.EP] for this version)
https://doi.org/10.48550/arXiv.2408.09129
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Submission history
From: Björn S. Konrad
[v1] Sat, 17 Aug 2024 07:54:46 UTC (3,942 KB)
https://arxiv.org/abs/2408.09129
Astrobiology,

Explorers Club Fellow, ex-NASA Space Station Payload manager/space biologist, Away Teams, Journalist, Lapsed climber, Synaesthete, Na’Vi-Jedi-Freman-Buddhist-mix, ASL, Devon Island and Everest Base Camp veteran, (he/him) 🖖🏻