Articles | Volume 19, issue 5
Atmos. Chem. Phys., 19, 3417–3432, 2019
https://doi.org/10.5194/acp-19-3417-2019
Atmos. Chem. Phys., 19, 3417–3432, 2019
https://doi.org/10.5194/acp-19-3417-2019

Research article 18 Mar 2019

Research article | 18 Mar 2019

The importance of interactive chemistry for stratosphere–troposphere coupling

Sabine Haase and Katja Matthes

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Sabine Haase on behalf of the Authors (25 Jan 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (30 Jan 2019) by Farahnaz Khosrawi
RR by Anonymous Referee #2 (15 Feb 2019)
ED: Publish as is (15 Feb 2019) by Farahnaz Khosrawi
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Short summary
The Antarctic ozone hole influences surface climate in the Southern Hemisphere. Recent studies have shown that stratospheric ozone depletion in the Arctic can also affect the surface. We evaluate the importance of the direct and indirect representation of ozone variability in a climate model for this surface response. We show that allowing feedbacks between ozone chemistry, radiation, and dynamics enhances and prolongs the surface response to Northern Hemisphere spring ozone depletion.
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