Brominated VSLS and their influence on ozone under a changing climate

Falk, Stefanie; Sinnhuber, Björn-Martin; Krysztofiak, Gisèle; Jöckel, Patrick; Graf, Phoebe; Lennartz, Sinikka T.

doi:https://doi.org/10.5194/acp-17-11313-2017

Articles | Volume 17, issue 18

https://doi.org/10.5194/acp-17-11313-2017

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

Special issue:

The Modular Earth Submodel System (MESSy) (ACP/GMD inter-journal...

https://doi.org/10.5194/acp-17-11313-2017

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

Articles | Volume 17, issue 18

Research article

|

25 Sep 2017

Research article |

| 25 Sep 2017

Brominated VSLS and their influence on ozone under a changing climate

Stefanie Falk, Björn-Martin Sinnhuber, Gisèle Krysztofiak, Patrick Jöckel, Phoebe Graf, and Sinikka T. Lennartz

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Final revised paper (published on 25 Sep 2017)
Preprint (discussion started on 03 Mar 2017)

Interactive discussion

Status: closed

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

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- Supplement

RC1: 'Reviewer' comments on Brominated VSLS and their influence on ozone under a changing climate by Flat et al.', Anonymous Referee #2, 31 Mar 2017
- AC1: 'Reviewer comment anonymous referee #2 (31 March 2017)', Stefanie Falk, 27 Apr 2017
RC2: 'Review of Falk et al.', Anonymous Referee #1, 18 Jul 2017

Peer-review completion

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

AR by Stefanie Falk on behalf of the Authors (10 Aug 2017) Author's response Manuscript

ED: Publish as is (02 Sep 2017) by Michel Van Roozendael

AR by Stefanie Falk on behalf of the Authors (02 Sep 2017)

Short summary

Brominated very short-lived source gases (VSLS) contribute significantly to the tropospheric and stratospheric bromine loading. We find an increase of future ocean–atmosphere flux of brominated VSLS of 8–10 % compared to present day. A decrease in the tropospheric mixing ratios of VSLS and an increase in the lower stratosphere are attributed to changes in atmospheric chemistry and transport. Bromine impact on stratospheric ozone at the end of the 21st century is reduced compared to present day.