Articles | Volume 15, issue 13
https://doi.org/10.5194/bg-15-4245-2018
https://doi.org/10.5194/bg-15-4245-2018
Research article
 | 
13 Jul 2018
Research article |  | 13 Jul 2018

Large but decreasing effect of ozone on the European carbon sink

Rebecca J. Oliver, Lina M. Mercado, Stephen Sitch, David Simpson, Belinda E. Medlyn, Yan-Shih Lin, and Gerd A. Folberth

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Interactive discussion

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
ED: Reconsider after major revisions (05 Mar 2018) by Xinming Wang
AR by Rebecca Oliver on behalf of the Authors (07 Mar 2018)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (08 Apr 2018) by Xinming Wang
RR by Anonymous Referee #2 (12 Apr 2018)
ED: Reconsider after major revisions (24 Apr 2018) by Xinming Wang
AR by Lorena Grabowski on behalf of the Authors (06 Jun 2018)  Author's response
ED: Referee Nomination & Report Request started (08 Jun 2018) by Xinming Wang
RR by Anonymous Referee #2 (08 Jun 2018)
ED: Publish subject to minor revisions (review by editor) (12 Jun 2018) by Xinming Wang
AR by Rebecca Oliver on behalf of the Authors (17 Jun 2018)  Author's response    Manuscript
ED: Publish as is (01 Jul 2018) by Xinming Wang
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Short summary
Potential gains in terrestrial carbon sequestration over Europe from elevated CO2 can be partially offset by concurrent rises in tropospheric O3. The land surface model JULES was run in a factorial suite of experiments showing that by 2050 simulated GPP was reduced by 4 to 9 % due to plant O3 damage. Large regional variations exist with larger impacts identified for temperate compared to boreal regions. Plant O3 damage was greatest over the twentieth century and declined into the future.
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