Articles | Volume 22, issue 16
Atmos. Chem. Phys., 22, 10425–10441, 2022
https://doi.org/10.5194/acp-22-10425-2022
Atmos. Chem. Phys., 22, 10425–10441, 2022
https://doi.org/10.5194/acp-22-10425-2022
Research article
16 Aug 2022
Research article | 16 Aug 2022

Ozone–gravity wave interaction in the upper stratosphere/lower mesosphere

Axel Gabriel

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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 acp-2021-1066', Anonymous Referee #1, 01 Feb 2022
    • AC1: 'Reply on RC1', Axel Gabriel, 10 Feb 2022
      • RC3: 'Reply on AC1', Anonymous Referee #1, 11 Feb 2022
        • AC3: 'Reply on RC3', Axel Gabriel, 13 Feb 2022
  • RC2: 'Comment on acp-2021-1066', Anonymous Referee #2, 02 Feb 2022
    • AC2: 'Reply on RC2', Axel Gabriel, 12 Feb 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Axel Gabriel on behalf of the Authors (14 Mar 2022)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (04 Apr 2022) by Mathias Palm
RR by Andreas Dörnbrack (25 Apr 2022)
RR by Anonymous Referee #1 (11 May 2022)
ED: Reconsider after major revisions (24 May 2022) by Mathias Palm
AR by Axel Gabriel on behalf of the Authors (11 Jul 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (21 Jul 2022) by Mathias Palm
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Short summary
Recent measurements show some evidence that the amplitudes of atmospheric gravity waves (horizontal wavelengths of 100–2000 km), which propagate from the troposphere (0–10 km) to the stratosphere and mesosphere (10–100 km), increase more strongly with height during daytime than during nighttime. This study shows that ozone–temperature coupling in the upper stratosphere can principally produce such an amplification. The results will help to improve atmospheric circulation models.
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