Articles | Volume 16, issue 1
Clim. Past, 16, 315–324, 2020
Clim. Past, 16, 315–324, 2020

Research article 14 Feb 2020

Research article | 14 Feb 2020

Centennial- to millennial-scale monsoon changes since the last deglaciation linked to solar activities and North Atlantic cooling

Xingxing Liu et al.


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: Publish subject to minor revisions (review by editor) (19 Dec 2019) by Qiuzhen Yin
AR by Xingxing Liu on behalf of the Authors (27 Dec 2019)  Author's response    Manuscript
ED: Publish as is (08 Jan 2020) by Qiuzhen Yin
Short summary
The East Asian summer monsoon and winter monsoon are anticorrelated on a centennial timescale during 16–1 ka. The centennial monsoon variability is connected to changes of both solar activity and North Atlantic cooling events during the Early Holocene. Then, North Atlantic cooling became the major forcing of events during the Late Holocene. This work presents the great challenge and potential to understand the response of the monsoon system to global climate changes in the past and the future.