Articles | Volume 3, issue 1
https://doi.org/10.5194/wcd-3-139-2022
https://doi.org/10.5194/wcd-3-139-2022
Research article
 | 
01 Feb 2022
Research article |  | 01 Feb 2022

Twenty-first-century Southern Hemisphere impacts of ozone recovery and climate change from the stratosphere to the ocean

Ioana Ivanciu, Katja Matthes, Arne Biastoch, Sebastian Wahl, and Jan Harlaß

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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 wcd-2021-43', Anonymous Referee #1, 16 Aug 2021
  • RC2: 'Comment on wcd-2021-43', Anonymous Referee #2, 11 Sep 2021
  • AC1: 'Author response to the comments of the referees', Ioana Ivanciu, 30 Oct 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Ioana Ivanciu on behalf of the Authors (30 Oct 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (15 Nov 2021) by Thomas Birner
RR by Anonymous Referee #1 (22 Nov 2021)
RR by Anonymous Referee #2 (07 Dec 2021)
ED: Publish subject to minor revisions (review by editor) (09 Dec 2021) by Thomas Birner
AR by Ioana Ivanciu on behalf of the Authors (16 Dec 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (21 Dec 2021) by Thomas Birner
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Short summary
Greenhouse gas concentrations continue to increase, while the Antarctic ozone hole is expected to recover during the twenty-first century. We separate the effects of ozone recovery and of greenhouse gases on the Southern Hemisphere atmospheric and oceanic circulation, and we find that ozone recovery is generally reducing the impact of greenhouse gases, with the exception of certain regions of the stratosphere during spring, where the two effects reinforce each other.