Three-dimensional transport-induced chemistry on temperate sub-Neptune K2-18b, Part II: the combined effects of atmospheric dynamics and chemical reactions
Jiachen Liu, Duncan Christie, Jun Yang, Krisztian Kohary

TL;DR
This study uses a 3D general circulation model to explore how atmospheric dynamics influence chemical disequilibrium and mixing in the atmosphere of the temperate sub-Neptune K2-18b, with implications for interpreting JWST observations.
Contribution
It provides the first 3D modeling of transport-induced chemistry on K2-18b, estimating vertical mixing parameters and comparing synthetic spectra with JWST data.
Findings
Vertical transport significantly increases CO$_2$ and CO in the upper atmosphere.
Horizontal winds homogenize chemical composition zonally.
The model's synthetic spectra fit JWST observations comparably to existing data.
Abstract
The upper atmospheres of temperate sub-Neptunes are strongly influenced by atmospheric dynamics due to their cool equilibrium temperature and thereby longer chemical timescales than the atmospheric dynamical timescales. In this study, we used a three-dimensional (3D) general circulation model to investigate the transport-induced disequilibrium chemistry and vertical mixing on temperate gas-rich mini-Neptunes, using K2-18b as an example. We model K2-18b assuming 180 times solar metallicity and consider it as either a synchronous or an asynchronous rotator, exploring spin-orbit resonances of 2:1, 6:1, and 10:1. We find that the vertical transport affects the chemical structure significantly, making CO and CO more abundant (10) in the upper atmosphere compared to the chemical equilibrium abundance (<10), and horizontal winds further homogenize the chemical…
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