Development of tree-ring width chronologies and tree-growth response to climate in the mountains surrounding the Issyk-Kul Lake, Central Asia

被引:26
作者
Zhang, Tongwen [1 ,2 ,3 ]
Yuan, Yujiang [1 ,2 ,3 ]
He, Qing [1 ,2 ,3 ]
Wei, Wenshou [1 ,2 ,3 ]
Diushen, Mamatkanov [4 ]
Shang, Huaming [1 ,2 ,3 ]
Zhang, Ruibo [1 ,2 ,3 ]
机构
[1] China Meteorol Adm, Inst Desert Meteorol, Urumqi 830002, Peoples R China
[2] China Meteorol Adm, Key Lab Tree Ring Phys & Chem Res, Urumqi 830002, Peoples R China
[3] Key Lab Tree Ring Ecol Uigur Autonomous Reg, Urumqi 830002, Peoples R China
[4] Natl Acad Sci Kyrgyz Republ, Inst Water Problem & Hydropower, Bishkek 720033, Kyrgyzstan
关键词
Issyk-Kul Lake; Picea schrenkiana; Tree-ring width; Climatic responses; TIEN-SHAN MOUNTAINS; TIBETAN PLATEAU; PRECIPITATION RECONSTRUCTION; TEMPERATURE RECONSTRUCTION; INNER-MONGOLIA; CHINA; VARIABILITY; QINGHAI; REGION;
D O I
10.1016/j.dendro.2014.03.002
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
Three tree-ring width chronologies were developed from 75 Picea schrenkiana trees ranging from low-to high-elevation in the mountains surrounding the Issyk-Kul Lake, Northeast Kyrgyzstan. The reliable chronologies extend back to the mid-18th and late-19th centuries. Spatial correlation analysis indicates that the chronologies for the relatively high-elevation trees contain large-scale climatic signals, while the chronology at relatively low elevation may reflect the local climate variability. The results of the response of tree growth to climate show that these chronologies contain an annual precipitation signal. Furthermore, the influence of temperature indicates mainly moisture stress that is enhanced with rising elevation. The tree-ring records also captured a wetting trend in eastern Central Asia over the past decades. These new tree-ring width chronologies provide reliable proxies of precipitation variability in Central Asia and contribute to the International Tree-Ring Data Bank. (C) 2014 Elsevier GmbH. All rights reserved.
引用
收藏
页码:230 / 236
页数:7
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