Articles | Volume 15, issue 4
https://doi.org/10.5194/acp-15-2019-2015
https://doi.org/10.5194/acp-15-2019-2015
Research article
 | 
24 Feb 2015
Research article |  | 24 Feb 2015

Contribution of liquid, NAT and ice particles to chlorine activation and ozone depletion in Antarctic winter and spring

O. Kirner, R. Müller, R. Ruhnke, and H. Fischer

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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 Oliver Kirner on behalf of the Authors (13 Nov 2014)
ED: Referee Nomination & Report Request started (08 Dec 2014) by Mathias Palm
RR by Anonymous Referee #2 (12 Dec 2014)
ED: Reconsider after minor revisions (Editor review) (22 Dec 2014) by Mathias Palm
AR by Oliver Kirner on behalf of the Authors (14 Jan 2015)  Manuscript 
ED: Publish as is (21 Jan 2015) by Mathias Palm
AR by Oliver Kirner on behalf of the Authors (21 Jan 2015)
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Short summary
We use multi-year simulations of the chemistry--climate model EMAC to investigate the impact that the various types of PSCs have on Antarctic chlorine activation and ozone loss. Heterogeneous chemistry on liquid particles is responsible for more than 90% of the ozone depletion in Antarctic spring in the model simulations. In high southern latitudes, heterogeneous chemistry on ice particles causes only up to 5 DU of additional ozone depletion and chemistry on NAT particles less than 0.5 DU.
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