Arid
DOI10.1016/j.quascirev.2010.01.005
Moisture changes over the last millennium in arid central Asia: a review, synthesis and comparison with monsoon region
Chen, Fa-Hu1; Chen, Jian-Hui1; Holmes, Jonathan2; Boomer, Ian3; Austin, Patrick2; Gates, John B.4; Wang, Ning-Lian5; Brooks, Stephen J.6; Zhang, Jia-Wu1
通讯作者Chen, Fa-Hu
来源期刊QUATERNARY SCIENCE REVIEWS
ISSN0277-3791
出版年2010
卷号29期号:7-8页码:1055-1068
英文摘要

There is a strong chance that 20th century warming will cause differences in precipitation distribution, hydrological cycle and effective moisture changes over the globe Arid central Asia (ACA), a unique dry-land area whose atmospheric circulation is dominated today by the westerlies, is one of the specific regions that are likely to be strongly impacted by global warming. An understanding of past variations in effective moisture in such regions is an important prerequisite for the prediction of future hydrological change. Here we evaluate spatial and temporal patterns of effective moisture variations documented by different proxies from 17 records in ACA, and synthesize a decadal-resolution moisture curve for ACA over the past millennium, using 5 of the 17 records selected on the basis of reliable chronologies and robust proxies The high- and low-resolution data all show that, over the past millennium, ACA has been characterized by a relatively dry Medieval Warm Period (MWP: the period from similar to 1000 to 1350 AD), a wet Little Ice Age (LIA. from similar to 1500 to 1850 AD) and increasing moisture during recent decades As a whole, the LIA in the ACA was not only relatively humid but also had high precipitation. Over the past millennium, the multi-centennial moisture changes in ACA show a generally inverse relationship with the temperature changes in the Northern Hemisphere, China, and western central Asia The effective moisture history in ACA also shows an out-of-phase relationship with that in monsoon Asia (especially during the LIA). We propose that the humid LIA in ACA, possibly extending to Mediterranean Sea and Western Europe, may have resulted from increased precipitation due to more frequent mid-latitude cyclone activities as a result of the strengthening and equator-ward shift of the westerly jet stream, and the predominantly negative North Atlantic Oscillation conditions, coupled with a decrease in evapo-transpiration caused by the cooling at that time (C) 2010 Elsevier Ltd. All rights reserved


类型Article
语种英语
国家Peoples R China ; England ; USA
收录类别SCI-E
WOS记录号WOS:000276749200017
WOS关键词NORTHERN-HEMISPHERE TEMPERATURES ; BASIN WESTERN TIBET ; GULIYA ICE CORE ; ARAL SEA ; GROUNDWATER RECHARGE ; CLIMATE VARIABILITY ; HOLOCENE CLIMATE ; SUMMER MONSOON ; BOSTEN LAKE ; ENVIRONMENTAL-CHANGES
WOS类目Geography, Physical ; Geosciences, Multidisciplinary
WOS研究方向Physical Geography ; Geology
来源机构兰州大学 ; 中国科学院西北生态环境资源研究院 ; University of London
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/166178
作者单位1.Lanzhou Univ, MOE Key Lab Western Chinas Environm Syst, Lanzhou 730000, Peoples R China;
2.UCL, Dept Geog, Environm Change Res Ctr, London WC1E 6BT, England;
3.Univ Birmingham, Sch Geog Earth & Environm Sci, Birmingham B15 2TT, W Midlands, England;
4.Univ Nebraska, Dept Geosci, Lincoln, NE 68588 USA;
5.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Lanzhou 730000, Peoples R China;
6.Nat Hist Museum, Dept Entomol, London SW7 5BD, England
推荐引用方式
GB/T 7714
Chen, Fa-Hu,Chen, Jian-Hui,Holmes, Jonathan,et al. Moisture changes over the last millennium in arid central Asia: a review, synthesis and comparison with monsoon region[J]. 兰州大学, 中国科学院西北生态环境资源研究院, University of London,2010,29(7-8):1055-1068.
APA Chen, Fa-Hu.,Chen, Jian-Hui.,Holmes, Jonathan.,Boomer, Ian.,Austin, Patrick.,...&Zhang, Jia-Wu.(2010).Moisture changes over the last millennium in arid central Asia: a review, synthesis and comparison with monsoon region.QUATERNARY SCIENCE REVIEWS,29(7-8),1055-1068.
MLA Chen, Fa-Hu,et al."Moisture changes over the last millennium in arid central Asia: a review, synthesis and comparison with monsoon region".QUATERNARY SCIENCE REVIEWS 29.7-8(2010):1055-1068.
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