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《Journal of Glaciolgy and Geocryology》 2002-05
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The Maximum Glaciation and Desert Expansion in China during MIS16

WU Guang\|jian~ 1, 2,\ PAN Bao\|tian~ 2,\ GUAN Qing\|yu~ 2,\ GAO Hong\|shan~ 2 (1.Key Laboratory of Ice Core and Cold Regions Environment, CAREERI, CAS, Lanzhou Gansu 730000, China; 2.Department of Geography, National Laboratory of Western China  
The Shagou loess section, which is situated in the border between the Tibetan Plateau and northwest arid region of China, records the detail of climate changes and desert evolution over the past 0\^83 Ma BP. Median grain size and sand content in the L6 loess layer indicate that winter monsoon greatly enhanced and desert extremely expanded at that time. During the MIS16, ice sheets in the Northern Hemisphere extended largely, and the global ice volume reached the Maximum since the mid\|Pleistocene climate transition. The expansion of northern Siberian ice sheet also reinforced the Siberian High during MIS16. At the same time, the Maximum glaciation developed in the Tibetan Plateau greatly adjusted the westerly and amplified winter monsoon via the Siberian High. Responding to the maximum of global ice volume, as a climate background, and the Maximum Glaciation in the Tibetan Plateau, as an amplifier of the winter monsoon and westerly, deserts in East China expanded extremely. Global ice volume and the Tibetan Plateau are the two important factors influencing desert evolution among others.
【Fund】: 国家自然科学基金项目 (4 0 1710 10 );; 中国科学院寒区旱区环境与工程研究所冰芯与寒区环境重点实验室知识创新项目资助
【CateGory Index】: P532
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