中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
North Atlantic cooling triggered a zonal mode over the Indian Ocean during Heinrich Stadial 1

文献类型:期刊论文

作者Du, Xiaojing1,13; Russell, James M.1,13; Liu, Zhengyu12; Otto-Bliesner, Bette L.11; Oppo, Delia W.10; Mohtadi, Mahyar9; Zhu, Chenyu8; Galy, Valier V.7; Schefu?, Enno9; Yan, Yan6
刊名SCIENCE ADVANCES
出版日期2023
卷号9期号:1页码:eadd4909
关键词PACIFIC WARM POOL HEMISPHERE CONTROLS LAST DEGLACIATION CENTRAL INDONESIA HIGH-RESOLUTION SEA-LEVEL CLIMATE MONSOON RECORD VARIABILITY
ISSN号2375-2548
DOI10.1126/sciadv.add4909
英文摘要Abrupt changes in the Atlantic meridional overturning circulation (AMOC) are thought to affect tropical hydroclimate through adjustment of the latitudinal position of the intertropical convergence zone (ITCZ). Heinrich Stadial 1 (HS1) involves the largest AMOC reduction in recent geological time; however, over the tropical Indian Ocean (IO), proxy records suggest zonal anomalies featuring intense, widespread drought in tropical East Africa versus generally wet but heterogeneous conditions in the Maritime Continent. Here, we synthesize proxy data and an isotope-enabled transient deglacial simulation and show that the southward ITCZ shift over the eastern IO during HS1 strengthens IO Walker circulation, triggering an east-west precipitation dipole across the basin. This dipole reverses the zonal precipitation anomalies caused by the exposed Sunda and Sahul shelves due to glacial lower sea level. Our study illustrates how zonal modes of atmosphere-ocean circulation can amplify or reverse global climate anomalies, highlighting their importance for future climate change. Copyright ? 2023 The Authors, some rights reserved;
WOS研究方向Multidisciplinary Sciences
语种英语
WOS记录号WOS:000936020700013
源URL[http://ir.gig.ac.cn/handle/344008/80214]  
专题同位素地球化学国家重点实验室
作者单位1.Institute at Brown for Environment and Society, Brown University, Providence; RI, United States
2.Department of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing, China
3.Department of Earth Sciences, ETH Zürich, Zürich, Switzerland
4.Department of Surface Waters Research and Management, Eawag, Dübendorf, Switzerland
5.Department of Marine and Coastal Sciences, Department of Earth and Planetary Sciences, Rutgers, State University of New Jersey, New Brunswick; NJ, United States
6.State Key Laboratory of Isotope Geochemistry, CAS Center for Excellence in Deep Earth Science, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, China
7.Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole; MA, United States
8.Frontier Science Center for Deep Ocean Multispheres and Earth System (FDOMES), Physical Oceanography Laboratory, Ocean University of China, Qingdao, China
9.MARUM-Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany
10.Geology and Geophysics Department, Woods Hole Oceanographic Institution, Woods Hole; MA, United States
推荐引用方式
GB/T 7714
Du, Xiaojing,Russell, James M.,Liu, Zhengyu,et al. North Atlantic cooling triggered a zonal mode over the Indian Ocean during Heinrich Stadial 1[J]. SCIENCE ADVANCES,2023,9(1):eadd4909.
APA Du, Xiaojing.,Russell, James M..,Liu, Zhengyu.,Otto-Bliesner, Bette L..,Oppo, Delia W..,...&Gao, Yu.(2023).North Atlantic cooling triggered a zonal mode over the Indian Ocean during Heinrich Stadial 1.SCIENCE ADVANCES,9(1),eadd4909.
MLA Du, Xiaojing,et al."North Atlantic cooling triggered a zonal mode over the Indian Ocean during Heinrich Stadial 1".SCIENCE ADVANCES 9.1(2023):eadd4909.

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来源:广州地球化学研究所

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