Articles | Volume 16, issue 6
https://doi.org/10.5194/cp-16-2239-2020
https://doi.org/10.5194/cp-16-2239-2020
Research article
 | 
19 Nov 2020
Research article |  | 19 Nov 2020

Synergy of the westerly winds and monsoons in the lake evolution of global closed basins since the Last Glacial Maximum and implications for hydrological change in central Asia

Yu Li and Yuxin Zhang

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Cited articles

An, C. B. and Chen, F. H.: The pattern of Holocene climate change in the arid central Asia: a case study based on lakes, Journal of Lake Sciences, 21, 329–334, https://doi.org/10.18307/2009.0303, 2009. 
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Bacon, S. N., Burke, R. M., Pezzopane, S. K., and Jayko, A. S.: Last glacial maximum and Holocene lake levels of Owens Lake, eastern California, USA, Quaternary Sci. Rev., 25, 1264–1282, https://doi.org/10.1016/j.quascirev.2005.10.014, 2006. 
Baker, P. A., Rigsby, C. A., Seltzer, G. O., Fritz, S. C., Lowenstein, T. K., Bacher, N. P., and Veliz, C.: Tropical climate changes at millennial and orbital timescales on the Bolivian Altiplano, Nature, 409, 698–701, https://doi.org/10.1038/35055524, 2001. 
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Short summary
Monsoons and westerly winds interact with each other in the middle to low latitudes. We track millennial-scale evolution characteristics of monsoons and westerly winds over the past 21 000 years. In the monsoon-dominated regions of Asia, a humid climate prevails in the past 6000–10 000 years, while in the westerly-wind-dominated regions of Asia, the climate is relatively humid around 21 000 years and 6000 years ago.