The oscillating fringe and paleo-intensity of the East Asian monsoon reconstructed using closed-basin lake-area and dDwax
Yonaton Goldsmith1, Wallace S Broecker2, Pratigya J Polissar3, Hai Xu4, Jianghu Lan5, Weijian Zhou6, Zhisheng An7 and Peter B deMenocal3, (1)Columbia University of New York, Palisades, NY, United States, (2)Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY, United States, (3)Lamont-Doherty Earth Observatory, Palisades, United States, (4)State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Xi’an, China, (5)State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Xian, China, (6)Institute of Earth Environment, Chinese Academy of Sciences, Xi'an, China, (7)IEE Institute of Earth Environment, Chinese Academy of Sciences, Xi'an, China
