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ACP | Articles | Volume 18, issue 22
Atmos. Chem. Phys., 18, 16499–16513, 2018
https://doi.org/10.5194/acp-18-16499-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Atmos. Chem. Phys., 18, 16499–16513, 2018
https://doi.org/10.5194/acp-18-16499-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 21 Nov 2018

Research article | 21 Nov 2018

Response of Arctic ozone to sudden stratospheric warmings

Alvaro de la Cámara et al.

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Alvaro de la Camara on behalf of the Authors (22 Oct 2018)  Author's response    Manuscript
ED: Publish subject to minor revisions (review by editor) (23 Oct 2018) by Peter Haynes
AR by Alvaro de la Camara on behalf of the Authors (23 Oct 2018)  Author's response    Manuscript
ED: Publish as is (05 Nov 2018) by Peter Haynes
AR by Alvaro de la Camara on behalf of the Authors (05 Nov 2018)  Author's response    Manuscript
Publications Copernicus
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Short summary
Long chemistry–climate runs are used to investigate the changes that sudden stratospheric warmings (extreme and fast disruptions of the wintertime stratospheric polar vortex) induce on Arctic ozone. Ozone increases rapidly during the onset of the events, driven by deep changes in the stratospheric transport circulation. These anomalies decay slowly, particularly in the lower stratosphere where they can last up to 2 months. Irreversible mixing makes an important contribution to this behavior.
Long chemistry–climate runs are used to investigate the changes that sudden stratospheric...
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