Exoplanetology: Exoplanets & Exomoons

A New Convection Scheme For GCMs Of Temperate Sub-Neptunes

By Keith Cowing
Status Report
astro-ph.EP
February 19, 2025
Filed under , , , , , , , , ,
A New Convection Scheme For GCMs Of Temperate Sub-Neptunes
K2-18 b vertical velocity πœ” at the 0.01 bar level. Negative (positive) πœ” indicates upwards (downwards) motion. The global overturning circulation is clearly visible. Irradiation concentrated on the dayside heats and expands these atmospheric regions, driving upwards motion. There is corresponding subsidence on the nightside. — astro-ph.EP

Atmospheric characterisation of temperate sub-Neptunes is the new frontier of exoplanetary science with recent JWST observations of possible Hycean world K2-18b.

Accurate modelling of atmospheric processes is essential to interpreting high-precision spectroscopic data given the wide range of possible conditions in the sub-Neptune regime, including on potentially habitable planets. Notably, convection is an important process which can operate in different modes across sub-Neptune conditions.

Convection can act very differently in atmospheres with a high condensible mass fraction (non-dilute atmospheres) or with a lighter background gas, e.g. water convection in a H2-rich atmosphere, and can be much weaker or even shut down entirely in the latter case.

We present a new mass-flux scheme which can capture these variations and simulate convection over a wide range of parameter space for use in 3D general circulation models (GCMs). We validate our scheme for two representative cases, a terrestrial-like atmosphere and a mini-Neptune atmosphere.

In the terrestrial case, considering TRAPPIST-1e with an Earth-like atmosphere, the model performs near-identically to Earth-tuned models in an Earth-like convection case.

In the mini-Neptune case, considering the bulk properties of K2-18b and assuming a deep H2-rich atmosphere, we demonstrate the capability of the scheme to reproduce non-condensing convection. We find convection occurring at pressures greater than 0.3 bar and the dynamical structure shows high-latitude prograde jets.

Our convection scheme will aid in the 3D climate modelling of a wide range of exoplanet atmospheres, and enable further exploration of temperate sub-Neptune atmospheres.

Edouard F. L. Barrier, Nikku Madhusudhan

Comments: Accepted for publication in MNRAS
Subjects: Earth and Planetary Astrophysics (astro-ph.EP)
Cite as: arXiv:2502.12234 [astro-ph.EP] (or arXiv:2502.12234v1 [astro-ph.EP] for this version)
https://doi.org/10.48550/arXiv.2502.12234
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Submission history
From: Edouard Barrier
[v1] Mon, 17 Feb 2025 19:00:00 UTC (1,167 KB)
https://arxiv.org/abs/2502.12234
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Explorers Club Fellow, ex-NASA Space Station Payload manager/space biologist, Away Teams, Journalist, Lapsed climber, Synaesthete, Na’Vi-Jedi-Freman-Buddhist-mix, ASL, Devon Island and Everest Base Camp veteran, (he/him) πŸ––πŸ»