globalchange  > 气候变化与战略
DOI: 10.1073/pnas.2013802117
论文题名:
Seasonal drought events in tropical East Asia over the last 60;000 y
作者: Zhang J.; Lu H.; Jia J.; Shen C.; Wang S.; Chu G.; Wang L.; Cui A.; Liu J.; Wu N.; Li F.
刊名: Proceedings of the National Academy of Sciences of the United States of America
ISSN: 0027-8424
出版年: 2020
卷: 117, 期:49
起始页码: 30988
结束页码: 30992
语种: 英语
英文关键词: Interstadial/stadial ; Phytolith ; Pollen ; Tropical SST gradient ; Walker and Hadley circulation
Scopus关键词: Article ; Asia ; atmosphere ; climate ; drought ; glaciation ; hydrology ; Northern Hemisphere ; oscillation ; precipitation ; priority journal ; sea ; vegetation
英文摘要: The cause of seasonal hydrologic changes in tropical East Asia during interstadial/stadial oscillations of the last glaciation remains controversial. Here, we show seven seasonal drought events that occurred during the relatively warm interstadials by phytolith and pollen records. These events are significantly manifested as high percentages of bilobate phytoliths and are consistent with the large zonal sea-surface temperature (SST) gradient from the western to eastern tropical Pacific, suggesting that the reduction in seasonal precipitation could be interpreted by westward shifts of the western Pacific subtropical high triggered by changes of zonal SST gradient over the tropical Pacific and Hadley circulation in the Northern Hemisphere. Our findings highlight that both zonal and meridional ocean-atmosphere circulations, rather than solely the Intertropical Convergence Zone or El Niño-Southern Oscillation, controlled the hydrologic changes in tropical East Asia during the last glaciation. © 2020 National Academy of Sciences. All rights reserved.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/163906
Appears in Collections:气候变化与战略

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作者单位: Zhang, J., Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China, Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences, Beijing, 100101, China; Lu, H., Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China, Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences, Beijing, 100101, China, College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing, 101408, China; Jia, J., Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China; Shen, C., Yunnan Key Laboratory of Plateau Geographical Processes and Environmental Changes, College of Tourism and Geographical Sciences, Yunnan Normal University, Kunming, 650500, China; Wang, S., Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China; Chu, G., Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China; Wang, L., Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China; Cui, A., Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China, College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing, 101408, China; Liu, J., Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China; Wu, N., Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China; Li, F., Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China

Recommended Citation:
Zhang J.,Lu H.,Jia J.,et al. Seasonal drought events in tropical East Asia over the last 60;000 y[J]. Proceedings of the National Academy of Sciences of the United States of America,2020-01-01,117(49)
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