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Twentieth-century warming preserved in a Geladaindong mountain ice core, central Tibetan Plateau
Zhang, YL (Zhang, Yulan)1,4; Kang, SC (Kang, Shichang)1,2; Grigholm, B (Grigholm, Bjorn)5,6; Zhang, YJ (Zhang, Yongjun)3; Kaspari, S (Kaspari, Susan)7; Morgenstern, U (Morgenstern, Uwe)8; Ren, JW (Ren, Jiawen)1; Qin, DH (Qin, Dahe)1; Mayewski, PA (Mayewski, Paul A.)5,6; Zhang, QG (Zhang, Qianggong)2,3; Cong, ZY (Cong, Zhiyuan)2,3; Sillanpaa, M (Sillanpaa, Mika)4; Schwikowski, M (Schwikowski, Margit)9; Chen, F (Chen, Feng)3; Kang, SC
Source PublicationANNALS OF GLACIOLOGY
2016
Volume57Issue:71Pages:70-80
DOI10.3189/2016AoG71A001
AbstractHigh-resolution delta O-18 records from a Geladaindong mountain ice core spanning the period 1477-1982 were used to investigate past temperature variations in the Yangtze River source region of the central Tibetan Plateau (TP). Annual ice-core delta O-18 records were positively correlated with temperature data from nearby meteorological stations, suggesting that the delta O-18 record represented the air temperature in the region. A generally increasing temperature trend over the past 500 years was identified, with amplified warming during the 20th century. A colder stage, spanning before the 1850s, was found to represent the Little Ice Age with colder periods occurring during the 1470s-1500s, 1580s-1660s, 1700s-20s and 1770s-1840s. Compared with other temperature records from the TP and the Northern Hemisphere, the Geladaindong ice-core record suggested that the regional climate of the central TP experienced a stronger warming trend during the 20th century than other regions. In addition, a positive relationship between the Geladaindong delta O-18 values and the North Atlantic Oscillation index, combined with a wavelet analysis of delta O-18 records, indicated that there was a potential atmospheric teleconnection between the North Atlantic and the central TP.
Subject Area自然地理学
WOS IDWOS:000384891500009
Language英语
Indexed BySCI
KeywordNorth-atlantic Oscillation Glacier Variations Rapid Decrease Mass-balance Alpine Firn Tree-rings Climate Record Precipitation South
Cooperation Status国际
Department环境
Citation statistics
Cited Times:3[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.itpcas.ac.cn/handle/131C11/7857
Collection图书馆
Corresponding AuthorKang, SC
Affiliation1.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, State Key Lab Cryospher Sci, Lanzhou, Peoples R China
2.Chinese Acad Sci, CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China
3.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Surface Proc, Beijing, Peoples R China
4.Lappeenranta Univ Technol, Lab Green Chem, Mikkeli, Finland
5.Univ Maine, Climate Change Inst, Orono, ME USA
6.Univ Maine, Dept Earth Sci, Orono, ME USA
7.Cent Washington Univ, Dept Geol Sci, Ellensburg, WA USA
8.Natl Isotope Ctr, Inst Geol & Nucl Sci, Lower Hutt, New Zealand
9.Paul Scherrer Inst, Lab Radiochem & Environm Chem, Villigen, Switzerland
Recommended Citation
GB/T 7714
Zhang, YL ,Kang, SC ,Grigholm, B ,et al. Twentieth-century warming preserved in a Geladaindong mountain ice core, central Tibetan Plateau[J]. ANNALS OF GLACIOLOGY,2016,57(71):70-80.
APA Zhang, YL .,Kang, SC .,Grigholm, B .,Zhang, YJ .,Kaspari, S .,...&Kang, SC.(2016).Twentieth-century warming preserved in a Geladaindong mountain ice core, central Tibetan Plateau.ANNALS OF GLACIOLOGY,57(71),70-80.
MLA Zhang, YL ,et al."Twentieth-century warming preserved in a Geladaindong mountain ice core, central Tibetan Plateau".ANNALS OF GLACIOLOGY 57.71(2016):70-80.
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