Tree-ring based precipitation variability since AD 1828 in northwestern Liaoning, China

被引：12
|
作者：
Peng, Junjie [1 ]
Sun, Yu [1 ]
Chen, Ming [2 ]
He, Xingyuan [1 ]
Davi, Nicole K. [3 ]
Zhang, Xianliang [1 ]
Li, Teng [1 ]
Zhu, Cuiying [2 ]
Cai, Chao [2 ]
Chen, Zhenju [1 ,4 ]
机构：
[1] Chinese Acad Sci, Inst Appl Ecol, State Key Lab Forest & Soil Ecol, Shenyang 110164, Peoples R China
[2] Yiwulv Mt Natl Nat Reserve, Beizhen 121300, Peoples R China
[3] Columbia Univ, Lamont Doherty Earth Observ, Tree Ring Lab, Palisades, NY 10964 USA
[4] Shenyang Agr Univ, Res Stn Liaohe River Plain Forest Ecosyst, Changtu 112500, Peoples R China
来源：
QUATERNARY INTERNATIONAL | 2013年 / 283卷
基金：
中国国家自然科学基金; 美国国家科学基金会;
关键词：
NORTH-CENTRAL CHINA; CHANGBAI MOUNTAIN; INNER-MONGOLIA; RECONSTRUCTION; FORESTS; INDEX; RIVER;
D O I：
10.1016/j.quaint.2012.07.007
中图分类号：
P9 [自然地理学];
学科分类号：
0705 ; 070501 ;
摘要：
A 183-year record of total precipitation from September to current July was reconstructed using tree rings from Chinese pine (Pinus tabulaeformis) to explore regional moisture variations in northwestern Liaoning province. The reconstruction accounts for 35.4% of the total variance of the instrumental precipitation from 1957 to 2010. The reconstruction shows eleven persistent dry periods (e.g. 1856-1866, 1886-1891, 1898-1905), and eleven persistent wet periods (e.g. 1835-1855, 1867-1878, 1892-1897). Spectral analysis of the reconstruction shows several significant spectral peaks in the ca. 2-4-year periodicity band, suggesting inter-annual variability of El Nino-Southern Oscillation (ENSO). The precipitation reconstruction shows correlations related to the East Asian Monsoon and possible teleconnection of regional moisture variations to Pacific Ocean signals, such as El Nino and La Nina. (C) 2012 Elsevier Ltd and INQUA. All rights reserved.
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收藏
页码：63 / 71
页数：9
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