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DOI10.1016/j.earscirev.2019.03.005
Westerlies Asia and monsoonal Asia: Spatiotemporal differences in climate change and possible mechanisms on decadal to sub-orbital timescales
Chen F.; Chen J.; Huang W.; Chen S.; Huang X.; Jin L.; Jia J.; Zhang X.; An C.; Zhang J.; Zhao Y.; Yu Z.; Zhang R.; Liu J.; Zhou A.; Feng S.
发表日期2019
ISSN00128252
起始页码337
结束页码354
卷号192
英文摘要The ‘westerlies-dominated climatic regime’ (WDCR) in the present interglacial period was proposed because precipitation/moisture variations between arid central Asia and mid-latitude monsoonal Asia are out-of-phase or anti-phased on different timescales during the Holocene. In this study. we first review the development of the theoretical framework of the WDCR, and then outline the boundary of its core area: from the Caspian Sea in the west to the western Hexi Corridor in the east, with the northern and southern limits coinciding with the domain of arid central Asia. Next, we present a synthesis of multiple lines of evidence for the occurrence of the WDCR on multi-millennial (‘sub-orbital’ herein) to decadal timescales during the Holocene. Finally, we examine the possible physical mechanisms responsible for the WDCR. We find that external factors (insolation changes induced by orbital factors) generated the WDCR on a sub-orbital timescale, whereas a circum-global teleconnection/Silk Road pattern was the most significant factor responsible for the WDCR on centennial and decadal timescales. The study provides a comprehensive summary of the development of our knowledge of the WDCR over the past several decades, together with a tentative theoretical framework for understanding climatic and environmental changes within its region of influence. In addition, it forms a scientific basis for environmental management and ecological restoration in this arid region in the context of global warming. © 2019 Elsevier B.V.
关键词Core area of WDCRHoloceneSilk Road pattern (SRP)Westerlies Asia and Monsoonal AsiaWesterlies-dominated climatic regime (WDCR)
英文关键词climate variation; decadal variation; Holocene; interglacial; monsoon; paleoclimate; paleoenvironment; spatiotemporal analysis; theoretical study; timescale; westerly; Caspian Sea; China; Gansu; Hexi Corridor
语种英语
来源期刊Earth Science Reviews
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/203402
作者单位Key Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou, 730000, China; Key Laboratory of Alpine Ecology (LAE), CAS Center for Excellence in Tibetan Plateau Earth Sciences, Institute of Tibetan Plateau Research, Chinese Academy of Sciences (CAS), Beijing, 100101, China; Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences (CAS), Beijing, 100101, China; Department of Earth and Environmental Sciences, Lehigh University, Bethlehem, PA 18015, United States; Institute of Atmospheric Sciences, Fudan University, Shanghai, 200433, China; Department of Geosciences, University of Arkansas, Fayetteville, AR 72701, United States
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Chen F.,Chen J.,Huang W.,et al. Westerlies Asia and monsoonal Asia: Spatiotemporal differences in climate change and possible mechanisms on decadal to sub-orbital timescales[J],2019,192.
APA Chen F..,Chen J..,Huang W..,Chen S..,Huang X..,...&Feng S..(2019).Westerlies Asia and monsoonal Asia: Spatiotemporal differences in climate change and possible mechanisms on decadal to sub-orbital timescales.Earth Science Reviews,192.
MLA Chen F.,et al."Westerlies Asia and monsoonal Asia: Spatiotemporal differences in climate change and possible mechanisms on decadal to sub-orbital timescales".Earth Science Reviews 192(2019).
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