Articles | Volume 16, issue 2
Clim. Past, 16, 475–485, 2020
https://doi.org/10.5194/cp-16-475-2020
Clim. Past, 16, 475–485, 2020
https://doi.org/10.5194/cp-16-475-2020

Research article 10 Mar 2020

Research article | 10 Mar 2020

Hydrological variations in central China over the past millennium and their links to the tropical Pacific and North Atlantic oceans

Fucai Duan et al.

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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 (07 Nov 2019) by Qiuzhen Yin
ED: Reconsider after major revisions (07 Nov 2019) by Qiuzhen Yin
AR by Fucai Duan on behalf of the Authors (12 Nov 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (21 Nov 2019) by Qiuzhen Yin
RR by Anonymous Referee #1 (20 Dec 2019)
ED: Publish subject to minor revisions (review by editor) (09 Jan 2020) by Qiuzhen Yin
AR by Fucai Duan on behalf of the Authors (16 Jan 2020)  Author's response
ED: Publish as is (05 Feb 2020) by Qiuzhen Yin
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Short summary
We reconstruct a detailed history of the East Asian summer monsoon (EASM) using stalagmite records in central China during the last millennium. We estimate responses of the EASM to anthropogenic global warming by comparing its relative intensity between the Current Warm Period and Medieval Climate Anomaly, two recent warm periods. We also study potential links of the EASM to the tropical Pacific and North Atlantic oceans. This work advances our understanding of EASM dynamics.