Future changes in the stratosphere-to-troposphere ozone mass flux and the contribution from climate change and ozone recovery

Meul, Stefanie; Langematz, Ulrike; Kröger, Philipp; Oberländer-Hayn, Sophie; Jöckel, Patrick

doi:https://doi.org/10.5194/acp-18-7721-2018

Articles | Volume 18, issue 10

https://doi.org/10.5194/acp-18-7721-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Special issue:

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

https://doi.org/10.5194/acp-18-7721-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 18, issue 10

Research article

|

01 Jun 2018

Research article |

| 01 Jun 2018

Future changes in the stratosphere-to-troposphere ozone mass flux and the contribution from climate change and ozone recovery

Stefanie Meul, Ulrike Langematz, Philipp Kröger, Sophie Oberländer-Hayn, and Patrick Jöckel

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Final revised paper (published on 01 Jun 2018)
Preprint (discussion started on 31 Jan 2018)

Interactive discussion

Status: closed

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

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RC1: 'Referee', Anonymous Referee #1, 05 Mar 2018
- AC1: 'Reply to Anonymous Referee #1', Ulrike Langematz, 30 Apr 2018
RC2: 'Review manuscript by Meul et al', Anonymous Referee #2, 07 Mar 2018
- AC2: 'Reply to Anonymous Referee #2', Ulrike Langematz, 30 Apr 2018

Peer-review completion

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

AR by Ulrike Langematz on behalf of the Authors (30 Apr 2018) Author's response Manuscript

ED: Publish as is (04 May 2018) by Jens-Uwe Grooß

Short summary

Using a chemistry--climate model future changes in the stratosphere-to-troposphere ozone mass flux, their drivers, and the future distribution of stratospheric ozone in the troposphere are investigated. In an extreme greenhouse gas (GHG) scenario, the global influx of stratospheric ozone into the troposphere is projected to grow between 2000 and 2100 by 53%. The increase is due to the recovery of stratospheric ozone owing to declining halogens and GHG induced circulation and temperature changes.