The physical and chemical structure of Titan’s upper atmosphere: energy balance, photochemistry and Jeans escape

Clicks: 12
ID: 332309
2026
Article Quality & Performance Metrics
Overall Quality
Not rated
Combines reader engagement with the AI quality analysis. This article has not been analysed, so there is no overall score — reader engagement is measured and shown alongside.
AI Quality Assessment
Not analyzed
Readership in this journal
Emerging

Ranked #1,182 of 1,339 articles by views in monthly notices of the royal astronomical society

Most read Least read

Bar heights use a square-root scale. Only the 120 most-read articles are drawn; the journal has 1,339 in total.

Mint this article as an NFT
Not yet minted

Create a permanent, verifiable on-chain record of this article on the Scimatic Network. The NFT is held in your Journament account, and you can withdraw it to your own wallet at any time.

5 SUSD one-off · no wallet required
Abstract
Abstract Titan’s upper atmospheric layers provide a unique opportunity to study how photochemistry, photoionisation, haze microphysics and escape processes shape its atmospheric chemical structure, providing a unique benchmark for understanding these processes in exoplanets. Using a 1D first-principles approach, we extend the Kompot model to simulate Titan’s upper atmosphere and investigate its thermal and chemical structure, and Jeans escape. We performed self-consistent simulations of Titan’s upper atmosphere, above the dense haze layer, over a 1D radial grid by solving the coupled hydrodynamics, thermal and photochemical kinetic, and energy balance equations. We considered heating by stellar X-ray and ultraviolet (XUV) and infrared (IR) radiation, and cooling due to radiative emission of methane (CH4) and hydrogen cyanide (HCN). We also included additional nineteen photochemical and 117 thermal reactions to Kompot’s standard chemical network. Our modelled atmospheric temperature structures lie within the observed variability of Titan’s atmospheric temperature profile. Our simulations reproduce observed nitrogen (N2) and CH4 densities in the upper atmosphere, and abundance of minor chemical species also broadly agree with observationally derived abundances. Near the exobase, our CH4 mixing ratio overlap with Cassini-Huygens results, and our model H2 mixing ratios also exhibit broad agreement with observations. Our simulations suggest no significant thermal loss of CH4, even under the conditions of an early Sun’s XUV environment.
Reference Key
openalex_W7221796604 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors
Journal monthly notices of the royal astronomical society
Year 2026
DOI
10.1093/mnras/stag1951
URL
Keywords Keywords not found

Citations

No citations found. To add a citation, contact the admin at info@scimatic.org

No comments yet. Be the first to comment on this article.