This work was financially funded by projects from the State Key Laboratory of Loess and Quaternary Geology in the Institute of Earth Environment of the Chinese Academy of Sciences (Y652001589 and Y651031589), the West Light Foundation of The Chinese Academy of Sciences (XAB2016B01), the gs3:National Science Foundation of China (NSFC) (41522305 and 41403018), the Major State Basic Research Development Program of China (973 Program) (2013CB955900), and the Chinese Academy of Sciences (QYZDB-SSW-DQC001, 132B61KYSB20160003, and 55ZZBS1304101).
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an, China; School of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney, Australia; Department of Geography and International Centre for China Development Study, The University of Hong Kong, Pokfulam Road, Hong Kong; School of Geographic and Oceanographic Sciences, Nanjing University, Nanjing, China; Institute of Nihewan Archaeology, Hebei Normal University, Shijiazhuang, China; Department of Social Sciences, The Education University of Hong Kong, 10 Lo Ping Road, Tai Po, Hong Kong; College of Urban and Environmental Sciences, Central China Normal University, Wuhan, China; State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing, China; College of Chemistry and Life Sciences, Zhejiang Normal University, Jinhua, China; College of Earth Sciences, University of Chinese Academy of Sciences, 19A Yuquan Rd, Shijingshan District, Beijing, China; Department of Earth Sciences, The University of Hong Kong, Hong Kong; Guangzhou Institute of Geography, Guangzhou, China
Recommended Citation:
Li J.,Dodson J.,Yan H.,et al. Quantifying climatic variability in monsoonal northern China over the last 2200 years and its role in driving Chinese dynastic changes[J]. Quaternary Science Reviews,2017-01-01,159