Identification of carbon dioxide in an exoplanet atmosphere.

Nature 614:7949 (2023) 649-652

Abstract:

Carbon dioxide (CO2) is a key chemical species that is found in a wide range of planetary atmospheres. In the context of exoplanets, CO2 is an indicator of the metal enrichment (that is, elements heavier than helium, also called 'metallicity')1-3, and thus the formation processes of the primary atmospheres of hot gas giants4-6. It is also one of the most promising species to detect in the secondary atmospheres of terrestrial exoplanets7-9. Previous photometric measurements of transiting planets with the Spitzer Space Telescope have given hints of the presence of CO2, but have not yielded definitive detections owing to the lack of unambiguous spectroscopic identification10-12. Here we present the detection of CO2 in the atmosphere of the gas giant exoplanet WASP-39b from transmission spectroscopy observations obtained with JWST as part of the Early Release Science programme13,14. The data used in this study span 3.0-5.5 micrometres in wavelength and show a prominent CO2 absorption feature at 4.3 micrometres (26-sigma significance). The overall spectrum is well matched by one-dimensional, ten-times solar metallicity models that assume radiative-convective-thermochemical equilibrium and have moderate cloud opacity. These models predict that the atmosphere should have water, carbon monoxide and hydrogen sulfide in addition to CO2, but little methane. Furthermore, we also tentatively detect a small absorption feature near 4.0 micrometres that is not reproduced by these models.

Testing 2D temperature models in Bayesian retrievals of atmospheric properties from hot Jupiter phase curves

Monthly notices of the Royal Astronomical Society

Authors:

Jingxuan Yang, Patrick G.J. Irwin, Joanna K. Barstow

Abstract:

Spectroscopic phase curves of transiting hot Jupiters are spectral measurements at multiple orbital phases, giving a set of disc-averaged spectra that probe multiple hemispheres. By fitting model phase curves to observations, we can constrain the atmospheric properties of hot Jupiters such as molecular abundance, aerosol distribution and thermal structure, which offer insights into their dynamics, chemistry, and formation. In this work, we propose a novel 2D temperature scheme consisting of a dayside and a nightside to retrieve information from near-infrared phase curves, and apply the scheme to phase curves of WASP-43b observed by HST/WFC3 and Spitzer/IRAC. In our scheme, temperature is constant on isobars on the nightside and varies with cos^n(longitude/ϵ) on isobars on the dayside, where n and ϵ are free parameters. We fit all orbital phases simultaneously using the radiative transfer package NEMESISPY coupled to a Bayesian inference code. We first validate the performance of our retrieval scheme with synthetic phase curves generated from a GCM, and find our 2D scheme can accurately retrieve the latitudinally-averaged thermal structure and constrain the abundance of H2O and CH4. We then apply our 2D scheme to the observed phase curves of WASP-43b and find: (1) the dayside temperature-pressure profiles do not vary strongly with longitude and are non-inverted; (2) the retrieved nightside temperatures are extremely low, suggesting significant nightside cloud coverage; (3) the H2O volume mixing ratio is constrained to 5.6×10^−5--4.0×10^−4, and we retrieve an upper bound for CH4 at ∼10^−6.

Detecting life outside our solar system with a large high-contrast-imaging mission

Experimental Astronomy Springer Nature 54:2-3 (2022) 1237-1274

Authors:

Ignas AG Snellen, F Snik, M Kenworthy, S Albrecht, G Anglada-Escudé, I Baraffe, P Baudoz, W Benz, J-L Beuzit, B Biller, JL Birkby, A Boccaletti, R van Boekel, J de Boer, Matteo Brogi, L Buchhave, L Carone, M Claire, R Claudi, B-O Demory, J-M Désert, S Desidera, BS Gaudi, R Gratton, M Gillon, JL Grenfell, O Guyon, T Henning, S Hinkley, E Huby, M Janson, C Helling, K Heng, M Kasper, CU Keller, O Krause, L Kreidberg, N Madhusudhan, A-M Lagrange, R Launhardt, TM Lenton, M Lopez-Puertas, A-L Maire, N Mayne, V Meadows, B Mennesson, G Micela, Y Miguel, J Milli, M Min, E de Mooij, D Mouillet, M N’Diaye, V D’Orazi, E Palle, I Pagano, G Piotto, D Queloz, H Rauer, I Ribas, G Ruane, F Selsis, A Sozzetti, D Stam, CC Stark, A Vigan, Pieter de Visser

99 oscillating red-giant stars in binary systems with NASA TESS and NASA Kepler identified from the SB9-Catalogue

Astronomy & Astrophysics EDP Sciences 667 (2022) a31

Authors:

PG Beck, S Mathur, K Hambleton, RA García, L Steinwender, NL Eisner, J-D do Nascimento, P Gaulme, S Mathis

CO2 ocean bistability on terrestrial exoplanets

Journal of Geophysical Research: Planets American Geophysical Union 127:10 (2022) e2022JE007456

Authors:

Robert J Graham, Tim Lichtenberg, Raymond T Pierrehumbert

Abstract:

Cycling of carbon dioxide between the atmosphere and interior of rocky planets can stabilize global climate and enable planetary surface temperatures above freezing over geologic time. However, variations in global carbon budget and unstable feedback cycles between planetary sub-systems may destabilize the climate of rocky exoplanets toward regimes unknown in the Solar System. Here, we perform clear-sky atmospheric radiative transfer and surface weathering simulations to probe the stability of climate equilibria for rocky, ocean-bearing exoplanets at instellations relevant for planetary systems in the outer regions of the circumstellar habitable zone. Our simulations suggest that planets orbiting G- and F-type stars (but not M-type stars) may display bistability between an Earth-like climate state with efficient carbon sequestration and an alternative stable climate equilibrium where CO2 condenses at the surface and forms a blanket of either clathrate hydrate or liquid CO2. At increasing instellation and with ineffective weathering, the latter state oscillates between cool, surface CO2-condensing and hot, non-condensing climates. CO2 bistable climates may emerge early in planetary history and remain stable for billions of years. The carbon dioxide-condensing climates follow an opposite trend in pCO2 versus instellation compared to the weathering-stabilized planet population, suggesting the possibility of observational discrimination between these distinct climate categories.