Investigating aerosols as a way to reconcile K2-18 b JWST MIRI and NIRISS/NIRSpec observations
Adam Yassin Jaziri, Thomas Drant
TL;DR
This work tackles the apparent tension between JWST NIRISS/NIRSpec and MIRI transmission spectra of the temperate sub-Neptune K2-18 b. Using TauREx 3 retrievals that incorporate free chemistry, non-equilibrium chemistry, and aerosol models with laboratory-derived haze refractive indices, the authors test whether photochemical hazes can reconcile the two datasets. They find that CH4-dominated, nitrogen-poor tholins (exo1) can explain the NIRISS slope through scattering and the MIRI 7 μm absorption feature, while simultaneously reducing the inferred metallicity from $19.63$ to $0.29$ and lowering CH4 abundance from $6.3\times 10^{-2}$ to $3.0\times 10^{-4}$, illustrating strong degeneracies between metallicity, composition, and aerosol properties. However, none of the models are decisively preferred over a flat spectrum for the combined data, underscoring the importance of aerosol absorption in temperate sub-Neptune atmospheres and the need for further JWST observations and laboratory haze measurements to break these degeneracies.
Abstract
Recent JWST observations of the temperate sub-Neptune K2-18 b with NIRISS SOSS/NIRSpec G395H and MIRI LRS have yielded apparently inconsistent results: the MIRI spectra exhibit spectral features nearly twice as large as those seen at shorter wavelengths, challenging the high-metallicity, CH4-rich non-equilibrium model that fits the NIRISS/NIRSpec data. We perform a suite of atmospheric retrievals on both datasets, including free-chemistry, non-equilibrium, and aerosol models, using laboratory-derived complex refractive indices for a variety of photochemical haze analogues. Free retrievals systematically return lower metallicities than inferred by self-consistent chemical disequilibrium models, and the inclusion of absorbing aerosols, especially CH4-dominated, nitrogen-poor tholins, can further reduce the inferred metallicity by over an order of magnitude. These hazes reproduce the observed NIRISS slope through scattering and match MIRI features via C-H bending absorption near 7 um, while yielding particle properties consistent with photochemical production in H2-rich atmospheres. Although their inclusion improves the joint fit and reduces tension between datasets, it also significantly lowers the retrieved CH4 abundance, highlighting degeneracies between metallicity, composition, and aerosol properties. Our results underscore the importance of aerosol absorption in interpreting temperate sub-Neptune spectra, and motivate future JWST observations and laboratory work to break these degeneracies.
