Articles | Volume 12, issue 7
https://doi.org/10.5194/cp-12-1583-2016
https://doi.org/10.5194/cp-12-1583-2016
Research article
 | 
28 Jul 2016
Research article |  | 28 Jul 2016

Quantification of southwest China rainfall during the 8.2 ka BP event with response to North Atlantic cooling

Yuhui Liu and Chaoyong Hu

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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 (03 May 2016) by Dominik Fleitmann
AR by Yuhui Liu on behalf of the Authors (08 Jun 2016)  Author's response   Manuscript 
ED: Publish subject to minor revisions (review by Editor) (20 Jun 2016) by Dominik Fleitmann
AR by Yuhui Liu on behalf of the Authors (26 Jun 2016)
ED: Publish as is (07 Jul 2016) by Dominik Fleitmann
AR by Yuhui Liu on behalf of the Authors (10 Jul 2016)  Manuscript 
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Short summary
The 8.2 ka BP event, a global climate anomaly that occurred 8200 years ago, could provide climate teleconnection information for the simulation of abrupt climate changes, but there are few quantitative reconstructions of this event. This paper provides a 10-year resolution rainfall record from the East Asian monsoon area during the event, showing the reduced rainfall in southwest China during the 8.2 ka BP period was coupled with Greenland cooling with a possible response rate of 110 ± 30 mm/℃.