Irradiated Atmospheres IV: Effect of Mixing Heat Flux on Chemistry

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Irradiated Atmospheres IV: Effect of Mixing Heat Flux on Chemistry

The mixing ratios of CH4, H2O, CO, NH3, NO and CO2 across varying intensities of vertical mixing. The dotted line (Case 0) corresponds to the case where there is no vertical mixing in the atmosphere. The solid lines (Case K) represent the scenarios where only the effect of material transport due to vertical mixing is considered, without accounting for the mixing heat flux. The dashed lines (Case KT) consider both the material mixing and the heat flux brought about by vertical mixing. The different colors correspond to different values of Kzz, with the temperature profile displayed in Figure 1. — astro-ph.EP

Vertical mixing disrupts the thermochemical equilibrium and introduces additional heat flux that alters exoplanetary atmospheric temperatures. We investigate how this mixing-induced heat flux affects atmospheric chemistry.

Temperature increase in the lower atmosphere by the mixing-induced heat flux alters species abundances there and modifies those in the upper atmosphere through vertical transport. In the lower atmosphere, most species follow thermodynamic equilibrium with temperature changes. In the upper layers, species mixing ratios depend on the positions of quenching levels relative to the regions exhibiting significant mixing-induced temperature variations.

When the quenching level resides within such region (e.g. CO, CH4, and H2O with strong mixing), the mixing ratios in the upper atmosphere are modified due to changes in the quenched ratios affected by the temperature variation in the lower atmosphere. This alters the mixing ratio of other species (e.g. NO and CO2) through the chemical reaction network, whose quenching occurs in the region without much temperature change.

The mixing ratios of CH4, H2O, and NH3 decrease in the lower atmosphere with increasing mixing heat flux, similarly reducing these ratios in the upper atmosphere. Conversely, the mixing ratios of CO, CO2, and NO rise in the lower atmosphere, with CO and CO2 also increasing in the upper levels, although NO decreases.

Weaker host star irradiation lowers the overall temperature of the planet, allowing a smaller mixing to have a similar effect. We conclude that understanding the vertical mixing heat flux is essential for accurate atmospheric chemistry modeling and retrieval.

Zhen-Tai Zhang, Wei Zhong, Wei Wang, Jianheng Guo, Xianyu Tan, Bo Ma, Ruyi Wei, Cong Yu

Comments: 11 pages, 3 figures. APJ accepted
Subjects: Earth and Planetary Astrophysics (astro-ph.EP)
Cite as: arXiv:2510.21543 [astro-ph.EP] (or arXiv:2510.21543v1 [astro-ph.EP] for this version)
https://doi.org/10.48550/arXiv.2510.21543
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Submission history
From: Zhen Tai Zhang
[v1] Fri, 24 Oct 2025 15:04:27 UTC (493 KB)
https://arxiv.org/abs/2510.21543

Astrobiology

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