Diversity in the haziness and chemistry of temperate sub-Neptunes
Pierre-Alexis Roy, Björn Benneke, Marylou Fournier-Tondreau, Louis-Philippe Coulombe, Caroline Piaulet-Ghorayeb, David Lafrenière, Romain Allart, Nicolas B. Cowan, Lisa Dang, Doug Johnstone, Adam B. Langeveld, Stefan Pelletier, Michael Radica, Jake Taylor, Loïc Albert, René Doyon, Laura Flagg, Ray Jayawardhana, Ryan J. MacDonald, Jake D. Turner
TL;DR
This study reveals substantial diversity among temperate sub-Neptunes by presenting JWST/NIRSpec PRISM transmission spectroscopy of LP 791-18 c, which shows a haze-dominated, methane-rich, metal-enriched atmosphere with no CO$_2$ detection, contrasting with earlier temperate sub-Neptunes that appear relatively clear and CO$_2$-rich. Using SCARLET atmosphere retrievals across free-chemistry and chemically consistent frameworks, the authors infer a metallicity of roughly 250–400× solar and a CH$_4$/CO$_2$ ratio exceeding unity, while also exploring a potential miscible-envelope scenario via coupled SCARLET–VULCAN models. They carefully address instrumental systematics (NIN, saturation), spot-crossing events, and stellar contamination, concluding that hazes plus methane dominate LP 791-18 c’s spectrum and that the atmosphere is not uniquely determined by temperature alone. The results demonstrate intrinsic diversity among sub-Neptunes and highlight the role of aerosols and interior-derived chemistry in shaping observable upper atmospheres, informing formation histories and guiding future JWST observations. $
Abstract
Recent transit observations of K2-18b and TOI-270d revealed strong molecular absorption signatures, lending credence to the idea that temperate sub-Neptunes (T$_\mathrm{eq}$=250-400K) have upper atmospheres mostly free of aerosols. These observations also indicated higher-than-expected CO$_2$ abundances on both planets, implying bulk compositions with high water mass fractions. However, it remains unclear whether these findings hold true for all temperate sub-Neptunes. Here, we present the JWST NIRSpec/PRISM 0.7-5.4$\mathbfμ$m transmission spectrum of a third temperate sub-Neptune, the 2.4R$_\oplus$ planet LP 791-18c (T$_\mathrm{eq}$=355K), which is even more favorable for atmospheric characterization thanks to its small M6 host star. Intriguingly, despite LP 791-18c's radius, mass, and equilibrium temperature being in between those of K2-18b and TOI-270d, we find a drastically different transmission spectrum. While we also detect methane on LP 791-18c, its transit spectrum is dominated by strong haze scattering and there is no discernible CO$_2$ absorption. Overall, we infer a deep metal-enriched atmosphere (246-415$\times$solar) for LP 791-18c, with a CO$_2$-to-CH$_4$ ratio smaller than 0.07 (at 2$σ$), indicating less H$_2$O in the deep envelope of LP 791-18c and implying a relatively dry formation inside the water ice-line. These results show that sub-Neptunes that are near-analogues in density and temperature can show drastically different aerosols and envelope chemistry, and are intrinsically diverse beyond a simple temperature dependence.
