- 1Université Paris Cité, Université Paris-Saclay, CEA, CNRS, AIM, F-91191 Gif-sur-Yvette, France (mael.voyer@u-paris.fr)
- 2Kapteyn Institute, University of Groningen, 9747 AD Groningen, NL
- 3Université Paris-Saclay, Université Paris Cité, CEA, CNRS, AIM, F-91191 Gif-sur-Yvette, France
The study 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 to 12 microns, and the Imager, providing us with 12.8, 15, 18 and 21 microns photometric measurements. We carried out a robust 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 and N/O and the ratio of detected metals as proxy for metallicity. We also derive upper limits for the abundance of CO and CO2 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.
How to cite: Voyer, M., Changeat, Q., and Lagage, P.-O.: MIRI-LRS spectrum of a cold exoplanet around a white dwarf: water, ammonia, and methane measurements., EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-2157, https://doi.org/10.5194/egusphere-egu25-2157, 2025.