How does downward planetary wave coupling affect polar stratospheric ozone in the Arctic winter stratosphere?

Lubis, Sandro W.; Silverman, Vered; Matthes, Katja; Harnik, Nili; Omrani, Nour-Eddine; Wahl, Sebastian

doi:https://doi.org/10.5194/acp-17-2437-2017

Articles | Volume 17, issue 3

https://doi.org/10.5194/acp-17-2437-2017

© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

https://doi.org/10.5194/acp-17-2437-2017

© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 17, issue 3

Research article

|

15 Feb 2017

Research article |

| 15 Feb 2017

How does downward planetary wave coupling affect polar stratospheric ozone in the Arctic winter stratosphere?

Sandro W. Lubis, Vered Silverman, Katja Matthes, Nili Harnik, Nour-Eddine Omrani, and Sebastian Wahl

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Final revised paper (published on 15 Feb 2017)
Supplement to the final revised paper
Preprint (discussion started on 12 Aug 2016)
Supplement to the preprint

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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- Supplement

RC1: 'Review', Anonymous Referee #1, 30 Aug 2016
- AC1: 'Response to reviewer 1', Sandro Lubis, 12 Dec 2016
RC2: 'Review of the manuscript entitled ‘How does Downward Planetary Wave coupling affect Polar Stratospheric Ozone in the Arctic Winter Stratosphere?’ by S. W. Lubis et al. submitted to Atmospheric Chemistry and Dynamics.', Anonymous Referee #3, 08 Sep 2016
- AC2: 'Response to reviewer 3', Sandro Lubis, 12 Dec 2016
RC3: 'Review', Anonymous Referee #4, 15 Sep 2016
- AC3: 'Response to reviewer 4', Sandro Lubis, 12 Dec 2016
AC4: 'General response to editor and all referees', Sandro Lubis, 12 Dec 2016

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

AR by Sandro Lubis on behalf of the Authors (20 Dec 2016) Author's response Manuscript

ED: Publish as is (26 Jan 2017) by Timothy J. Dunkerton

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Short summary

Downward wave coupling (DWC) events impact high-latitude stratospheric ozone in two ways: (1) reduced dynamical transport of ozone from low to high latitudes during individual events and (2) enhanced springtime chemical destruction of ozone via the cumulative impact of DWC events on polar stratospheric temperatures. The results presented here broaden the scope of the impact of wave–mean flow interaction on stratospheric ozone by highlighting the key role of wave reflection.