Articles | Volume 25, issue 21
https://doi.org/10.5194/acp-25-14719-2025
https://doi.org/10.5194/acp-25-14719-2025
Research article
 | 
05 Nov 2025
Research article |  | 05 Nov 2025

Thermospheric nitric oxide is modulated by the ratio of atomic to molecular oxygen and thermospheric dynamics during solar minimum

Miriam Sinnhuber, Christina Arras, Stefan Bender, Bernd Funke, Hanli Liu, Daniel R. Marsh, Thomas Reddmann, Eugene Rozanov, Timofei Sukhodolov, Monika E. Szelag, and Jan Maik Wissing

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2024-2256', Anonymous Referee #1, 12 Sep 2024
  • RC2: 'Comment on egusphere-2024-2256', Anonymous Referee #2, 02 Mar 2025

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Miriam Sinnhuber on behalf of the Authors (11 May 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to minor revisions (review by editor) (28 Jul 2025) by William Ward
AR by Miriam Sinnhuber on behalf of the Authors (13 Sep 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (22 Sep 2025) by William Ward
AR by Miriam Sinnhuber on behalf of the Authors (26 Sep 2025)  Manuscript 
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Short summary
Nitric oxide in the upper atmosphere varies with solar activity. Observations show that this starts a chain of processes affecting the ozone layer and climate system. This is often underestimated in models. We compare five models which show large differences in simulated NO. Analysis of these discrepancies identify two processes which interact with each other: the balance between atomic and molecular oxygen in the thermosphere, and a poleward - downward transport in the winter thermosphere. 
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