Articles | Volume 13, issue 11
https://doi.org/10.5194/cp-13-1593-2017
https://doi.org/10.5194/cp-13-1593-2017
Research article
 | 
17 Nov 2017
Research article |  | 17 Nov 2017

Reconstructing Late Holocene North Atlantic atmospheric circulation changes using functional paleoclimate networks

Jasper G. Franke, Johannes P. Werner, and Reik V. Donner

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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 Jun 2017) by Hugues Goosse
AR by Jasper G. Franke on behalf of the Authors (25 Aug 2017)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (28 Aug 2017) by Hugues Goosse
RR by Anonymous Referee #2 (15 Sep 2017)
RR by Anonymous Referee #1 (20 Sep 2017)
ED: Publish subject to minor revisions (review by Editor) (21 Sep 2017) by Hugues Goosse
AR by Jasper G. Franke on behalf of the Authors (28 Sep 2017)  Author's response   Manuscript 
ED: Publish as is (09 Oct 2017) by Hugues Goosse
AR by Jasper G. Franke on behalf of the Authors (09 Oct 2017)
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Short summary
We apply evolving functional network analysis, a tool for studying temporal changes of the spatial co-variability structure, to a set of Late Holocene paleoclimate proxy records covering the last two millennia. The emerging patterns obtained by our analysis are related to long-term changes in the dominant mode of atmospheric circulation in the region, the North Atlantic Oscillation (NAO). We obtain a qualitative reconstruction of the NAO long-term variability over the entire Common Era.