Glacial-Interglacial Indian Summer Monsoon Dynamics

American Association for the Advancement of Science (AAAS) - Tập 333 Số 6043 - Trang 719-723 - 2011
Zhisheng An1,2, Steven C. Clemens3, Ji Shen4, Xiaoke Qiang2, Zhangdong Jin2, Youbin Sun2, Warren L Prell3, Jing‐Jia Luo5, Sumin Wang4, Hai Xu2, Yanjun Cai2, Weijian Zhou1,2, Xiaodong Liu2, Weiguo Liu2, Zhengguo Shi2, Libin Yan2, Xiayun Xiao4, Hong Chang2, Feng Wu2, Li Ai2, Fengyan Lu2
1Institute of Global Environmental Change, Xi'an Jiaotong University, Xi'an 710049, China
2State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710075, China
3Department of Geological Sciences, Brown University, Providence, RI 02912, USA
4Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China
5Research Institute for Global Change, Japan Agency for Marine-Earth Science and Technology, Kanagawa 236-0001, Japan.

Tóm tắt

Indian summer monsoon changes during the Pleistocene were influenced by dynamic effects originating in both hemispheres.

Từ khóa


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