Arid
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, Fahu1,2; Chen, Jianhui1; Huang, Wei1; Chen, Shengqian1; Huang, Xiaozhong1; Jin, Liya1; Jia, Jia1; Zhang, Xiaojian1; An, Chengbang1; Zhang, Jiawu1; Zhao, Yan3; Yu, Zicheng4; Zhang, Renhe5; Liu, Jianbao1,2; Zhou, Aifeng1; Feng, Song6
通讯作者Chen, Fahu
来源期刊EARTH-SCIENCE REVIEWS
ISSN0012-8252
EISSN1872-6828
出版年2019
卷号192页码:337-354
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.
英文关键词Holocene Westerlies Asia and Monsoonal Asia Westerlies-dominated climatic regime (WDCR) Core area of WDCR Silk Road pattern (SRP)
类型Review
语种英语
国家Peoples R China ; USA
收录类别SCI-E
WOS记录号WOS:000474499500013
WOS关键词MEDIEVAL-WARM-PERIOD ; ARID CENTRAL-ASIA ; NORTHWESTERN YUNNAN PROVINCE ; HOLOCENE MOISTURE EVOLUTION ; NORTH CENTRAL MONGOLIA ; OF-PHASE RELATIONSHIP ; LAST GLACIAL MAXIMUM ; TARIM RIVER-BASIN ; MID-LATE HOLOCENE ; SUMMER MONSOON
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
来源机构兰州大学 ; 中国科学院地理科学与资源研究所 ; 中国科学院青藏高原研究所
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/215111
作者单位1.Lanzhou Univ, Coll Earth & Environm Sci, Minist Educ, Key Lab Western Chinas Environm Syst, Lanzhou 730000, Gansu, Peoples R China;
2.Chinese Acad Sci, Inst Tibetan Plateau Res, CAS Ctr Excellence Tibetan Plateau Earth Sci, Key Lab Alpine Ecol LAE, Beijing 100101, Peoples R China;
3.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China;
4.Lehigh Univ, Dept Earth & Environm Sci, Bethlehem, PA 18015 USA;
5.Fudan Univ, Inst Atmospher Sci, Shanghai 200433, Peoples R China;
6.Univ Arkansas, Dept Geosci, Fayetteville, AR 72701 USA
推荐引用方式
GB/T 7714
Chen, Fahu,Chen, Jianhui,Huang, Wei,et al. Westerlies Asia and monsoonal Asia: Spatiotemporal differences in climate change and possible mechanisms on decadal to sub-orbital timescales[J]. 兰州大学, 中国科学院地理科学与资源研究所, 中国科学院青藏高原研究所,2019,192:337-354.
APA Chen, Fahu.,Chen, Jianhui.,Huang, Wei.,Chen, Shengqian.,Huang, Xiaozhong.,...&Feng, Song.(2019).Westerlies Asia and monsoonal Asia: Spatiotemporal differences in climate change and possible mechanisms on decadal to sub-orbital timescales.EARTH-SCIENCE REVIEWS,192,337-354.
MLA Chen, Fahu,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):337-354.
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