Drivers for Asynchronous Patterns of Dust Accumulation in Central and Eastern Asia and in Greenland During the Last Glacial Maximum

• Published in: Geophysical Research Letters
• Main Authors: Cheng, Liangqing, Song, Yougui, Wu, Yubin, Liu, Yonggang, Liu, Huifang, Chang, Hong, Zong, Xiulan, Kang, Shugang
• Format: Report
• Language: English
• Published: AMER GEOPHYSICAL UNION 2021
• Subjects: dust accumulation; Last Glacial Maximum; obliquity; precession; Siberian High; westerlies; CHINESE LOESS; MINERAL-DUST; ICE CORE; WINTER MONSOON; GRAIN-SIZE; MIS 2; CLIMATE; INSOLATION; VARIABILITY; INSIGHTS; Geology; Geosciences; Multidisciplinary; Greenland; ice core
• Online Access: http://ir.ieecas.cn/handle/361006/16210; http://ir.ieecas.cn/handle/361006/16211; https://doi.org/10.1029/2020GL091194

We collected 143 loess optically stimulated luminescence (OSL) ages between 10 ka and 30 ka from Central Asia (CA), and analyzed their probability density functions (PDFs). The PDFs show dust accumulation was greater during the late Last Glacial Maximum (LGM) (23-19 ka) than that during the early LGM (26.5-23 ka). The temporal variability of dust accumulation of CA loess is generally similar to that of Chinese Loess Plateau (CLP) loess, following precession. In contrast, dust accumulation in Greenland was stronger during the early LGM than that during the late LGM, following obliquity. Supported by numerical modeling experiments and our newly dating OSL ages, we conclude dust accumulation in CA and CLP during the LGM was controlled by Siberian High forced by precession, while dust accumulation in Greenland was closely related to both intensity of summer westerlies forced by obliquity, and to intensity of dust emissions at source forced by precession.