Articles | Volume 18, issue 2
https://doi.org/10.5194/acp-18-1079-2018
https://doi.org/10.5194/acp-18-1079-2018
Research article
 | 
26 Jan 2018
Research article |  | 26 Jan 2018

Climate impact of idealized winter polar mesospheric and stratospheric ozone losses as caused by energetic particle precipitation

Katharina Meraner and Hauke Schmidt

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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 Katharina Meraner on behalf of the Authors (13 Oct 2017)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (16 Oct 2017) by Thomas von Clarmann (deceased)
RR by Anonymous Referee #1 (25 Oct 2017)
RR by Anonymous Referee #2 (30 Oct 2017)
RR by Anonymous Referee #3 (13 Nov 2017)
ED: Publish subject to minor revisions (review by editor) (27 Nov 2017) by Thomas von Clarmann (deceased)
AR by Katharina Meraner on behalf of the Authors (19 Dec 2017)  Author's response   Manuscript 
ED: Publish as is (21 Dec 2017) by Thomas von Clarmann (deceased)
AR by Katharina Meraner on behalf of the Authors (22 Dec 2017)
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Short summary
Using a coupled Earth system model and radiative transfer modeling we show that the radiative forcing of a winter polar mesospheric ozone loss due to energetic particle precipitation is negligible. A climate impact of a mesospheric ozone loss as suggested by Andersson et al. (2014, Nature Communications) seems unlikely. A winter polar stratospheric ozone loss due to energetic particle precipitation leads to a small warming of the stratosphere, but only a few statistically significant changes.
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