Japan Geoscience Union Meeting 2025

Presentation information

[E] Oral

P (Space and Planetary Sciences ) » P-AE Astronomy & Extrasolar Bodies

[P-AE18] Exoplanets

Fri. May 30, 2025 9:00 AM - 10:30 AM 304 (International Conference Hall, Makuhari Messe)

convener:Takanori Kodama(Earth-Life Science Institute, Institute of Science Tokyo), Yui Kawashima(Kyoto University), Shota Notsu(Earth and Planetary System Science Group, Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo), Mayuko Mori(Astrobiology Center), Chairperson:Yuichi Ito(National Astronomical Observatory of Japan, Division of Science), Takanori Kodama(Earth-Life Science Institute, Institute of Science Tokyo)


9:15 AM - 9:30 AM

[PAE18-02] MIRI-LRS spectrum of a cold exoplanet around a white dwarf: water, ammonia, and methane measurements.

*Mael Milan Voyer1, Quentin Changeat2, Pierre-Olivier Lagage3 (1.Paris-Cite University / CEA, 2.Kapteyn Instutite, Groningen University / UCL, 3.CEA)


Keywords:Exoplanets, Atmospheric retrievals, White dwarf exoplanets, Bayesian statistics

The study of the atmosphere of exoplanets orbiting white dwarfs is a largely unexplored field. With WD 0806-661 b, we present the first deep dive into the atmospheric physics and chemistry of a cold exoplanet around a white dwarf. We observed WD 0806-661 b using JWST's Mid-InfraRed Instrument Low-Resolution Spectrometer (MIRI-LRS), covering the wavelength range from 5 -- 12 microns, and the Imager, providing us with 12.8, 15, 18 and 21 microns photometric measurements. We carried the data reduction of those datasets, tackling second-order effects to ensure a reliable retrieval analysis. Using the TauREx retrieval code, we inferred the pressure-temperature structure, atmospheric chemistry, mass, and radius of the planet. The spectrum of WD 0806-661 b is shaped by molecular absorption of water, ammonia, and methane, consistent with a cold Jupiter atmosphere, allowing us to retrieve their abundances. From the mixing ratio of water, ammonia and methane we derive C/O C/N N/O and the ratio of detected metals as proxy for metallicity. We also derive upper limits for the abundance of CO and CO_2 which were not detected by our retrieval models. While our interpretation of WD 0806-661 b's atmosphere is mostly consistent with our theoretical understanding, some results -- such as the lack of evidence for water clouds, an apparent increase in the mixing ratio of ammonia at low pressure, or the retrieved mass at odds with the supposed age -- remain surprising and require follow-up observational and theoretical studies to be confirmed.