Articles | Volume 7, issue 4
https://doi.org/10.5194/esd-7-877-2016
https://doi.org/10.5194/esd-7-877-2016
Research article
 | 
11 Nov 2016
Research article |  | 11 Nov 2016

Response of the AMOC to reduced solar radiation – the modulating role of atmospheric chemistry

Stefan Muthers, Christoph C. Raible, Eugene Rozanov, and Thomas F. Stocker

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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 (22 Jul 2016) by Rui A. P. Perdigão
AR by Stefan Muthers on behalf of the Authors (29 Aug 2016)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (30 Aug 2016) by Rui A. P. Perdigão
RR by Anonymous Referee #3 (06 Sep 2016)
RR by Anonymous Referee #1 (08 Sep 2016)
RR by Anonymous Referee #4 (19 Sep 2016)
ED: Publish subject to minor revisions (review by Editor) (23 Sep 2016) by Rui A. P. Perdigão
AR by Stefan Muthers on behalf of the Authors (30 Sep 2016)  Author's response   Manuscript 
ED: Publish as is (22 Oct 2016) by Rui A. P. Perdigão
AR by Stefan Muthers on behalf of the Authors (25 Oct 2016)  Manuscript 
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Short summary
The Atlantic Meridional Overturning Circulation (AMOC) is an important oceanic circulation system which transports large amounts of heat from the tropics to the north. This circulation is strengthened when less solar irradiance reaches the Earth, e.g. due to reduced solar activity or geoengineering techniques. In climate models, however, this response is overestimated when chemistry–climate interactions and the following shift in the atmospheric circulation systems are not considered.
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