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Dipolar mode of precipitation changes between north China and the Yangtze River Valley existed over the entire Holocene: Evidence from the sediment record of Nanyi Lake
Key Laboratory of Alpine Ecology (LAE), Institute of Tibetan Plateau Research, Chinese Academy of Sciences
CAS Center for Excellence in Tibetan Plateau Earth System Sciences, Chinese Academy of Sciences
Key Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Science, Center for Pan Third Pole Environment (Pan‐TPE), Lanzhou University
Key Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Science, Center for Pan Third Pole Environment (Pan‐TPE), Lanzhou University
State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology and Center for Excellence in Life and Paleoenvironment, Chinese Academy of Sciences
Key Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Science, Center for Pan Third Pole Environment (Pan‐TPE), Lanzhou University
CAS Center for Excellence in Tibetan Plateau Earth System Sciences, Chinese Academy of Sciences
Key Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Science, Center for Pan Third Pole Environment (Pan‐TPE), Lanzhou University
Key Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Science, Center for Pan Third Pole Environment (Pan‐TPE), Lanzhou University
Key Laboratory of Alpine Ecology (LAE), Institute of Tibetan Plateau Research, Chinese Academy of Sciences
CAS Center for Excellence in Tibetan Plateau Earth System Sciences, Chinese Academy of Sciences
Key Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Science, Center for Pan Third Pole Environment (Pan‐TPE), Lanzhou University