Articles | Volume 16, issue 1
Clim. Past, 16, 315–324, 2020
https://doi.org/10.5194/cp-16-315-2020
Clim. Past, 16, 315–324, 2020
https://doi.org/10.5194/cp-16-315-2020
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.

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Cited articles

Alley, R. B., Mayewski, P. A., Sowers, T., Stuiver, M., Taylor, K. C., and Clark, P. U.: Holocene climatic instability: A prominent, widespread event 8200 yr ago, Geology, 25, 483–486, 1997. 
An, Z. S., Kukla, G., Porter, S. C., and Xiao, J. L.: Late Quaternary dust flow on the Chinese loess plateau, Catena, 18, 125–132, 1991. 
Berger, A.: Long term variations of daily insolations and quaternary climatic changes, J. Atmos. Sci., 35, 2362–2367, 1978. 
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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.