Articles | Volume 16, issue 18
Atmos. Chem. Phys., 16, 12159–12176, 2016
https://doi.org/10.5194/acp-16-12159-2016
Atmos. Chem. Phys., 16, 12159–12176, 2016
https://doi.org/10.5194/acp-16-12159-2016

Research article 28 Sep 2016

Research article | 28 Sep 2016

Future Arctic ozone recovery: the importance of chemistry and dynamics

Ewa M. Bednarz et al.

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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 Ewa Bednarz on behalf of the Authors (30 Jun 2016)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (01 Jul 2016) by Martin Dameris
RR by Anonymous Referee #2 (06 Jul 2016)
ED: Reconsider after minor revisions (Editor review) (07 Jul 2016) by Martin Dameris
AR by Anna Wenzel on behalf of the Authors (28 Jul 2016)  Author's response    Manuscript
ED: Publish as is (28 Jul 2016) by Martin Dameris
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Short summary
Future trends in springtime Arctic ozone, and its chemical dynamical and radiative drivers, are analysed using a 7-member ensemble of chemistry–climate model integrations, allowing for a detailed assessment of interannual variability. Despite the future long-term recovery of Arctic ozone, there is large interannual variability and episodic reductions in springtime Arctic column ozone. Halogen chemistry will become a smaller but non-negligible driver of Arctic ozone variability over the century.
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