Venus as an Exoplanet: I. An Initial Exploration of the 3-D Energy Balance for a CO$_{2}$ Exoplanetary Atmosphere Around an M-Dwarf Star

TL;DR

This study uses a 3-D model to explore the energy balance and atmospheric dynamics of a Venus-like exoplanet orbiting an M-dwarf star, revealing how stellar radiation influences temperature and wind patterns.

Contribution

It provides the first 3-D simulation of a Venus-like exoplanet's atmosphere around an M-dwarf, analyzing the effects of stellar radiation on energy balance and atmospheric dynamics.

Findings

EUV-UV heating significantly impacts zonal winds and temperature profiles.

CO₂ 15-μm cooling balances EUV/UV and NIR heating at specific altitudes.

Changes in NIR heating cause notable temperature variations in the upper and middle atmosphere.

Abstract

The chemical evolution of an exoplanetary Venus-like atmosphere is dependent upon the ultraviolet to near ultraviolet (FUV-NUV) radiation ratio from the parent star, the balance between CO$_{2}$ photolysis and recombination via reactions that depend on the water abundance, and various catalytic chemical cycles. In this study, we use a three-dimensional (3-D) model to simulate conditions for a Venus-like exoplanet orbiting the M-dwarf type star GJ 436 by varying the star/planet distance and considering the resultant effects on heating/cooling and dynamics. The simulation includes the middle and upper atmosphere (<40 mbar). Overall, these model comparisons reveal that the impact of extreme ultraviolet to ultraviolet (EUV-UV) heating on the energy balance shows both radiative and dynamical processes are responsible for driving significant variations in zonal winds and global temperature profiles at < 10$^{-5}$ mbar. More specifically, CO$_{2}$ 15-${\mu}$m cooling balances EUV/UV and Near InfraRed (NIR) heating at altitudes below 10$^{-7}$ mbar pressure with a strong maximum balance for pressures at ~10$^{-5}$ mbar, thus explaining the invariance of the temperature distribution at altitudes below 10$^{-5}$mbar pressure for all cases. Our model comparisons also show that moderate changes in NIR heating result in relatively small changes in neutral temperature in the upper atmosphere, and virtually no change in the middle atmosphere. However, with larger changes in the NIR heating profile, much greater changes in neutral temperature occur in the entire upper and middle atmosphere studied.