Pre-monsoon precipitation signal in tree rings of timberline Betula utilis in the central Himalayas

被引:84
作者
Dawadi, Binod [1 ,3 ]
Liang, Eryuan [1 ]
Tian, Lide [1 ]
Devkota, Lochan Prasad [2 ]
Yao, Tandong [1 ]
机构
[1] Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing 100101, Peoples R China
[2] Tribhuvan Univ, Cent Dept Hydrol & Meteorol, Kathmandu, Nepal
[3] Chinese Acad Sci, Grad Univ, Beijing 100049, Peoples R China
基金
中国国家自然科学基金;
关键词
TIBETAN PLATEAU; CLIMATIC RESPONSE; LOW-FREQUENCY; WIDTH; TEMPERATURE; MOUNTAINS; CHRONOLOGIES; SOUTHERN; HISTORY; GROWTH;
D O I
10.1016/j.quaint.2012.05.039
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Himalayan birch (Betula utilis D. Don) is a long-lived, broadleaf tree species native to the Himalayas. However, it has received limited attention for dendroclimatological studies. Based on 49 tree-ring cores from 41 Himalayan birch trees at two sites in the Langtang National Park, central Nepal, a 458-year chronology (back to AD 1552) was developed. To date, this is the longest for this species in the Himalayas despite a low sample depth before AD 1785. The chronology statistics show the potential of Himalayan birch for dendroclimatology, as indicated by a positive correlation with precipitation in May and March May (p < 0.001) and an inverse relationship with temperature in May and precipitation in August (p < 0.05). The Himalayan birch ring-width chronology is thus an indicator for pre-monsoon precipitation variations in the central Himalayas. The wide distribution of Himalayan birch in High Asia presents an outstanding opportunity for developing a large-scale, single-species tree-ring network. (C) 2012 Elsevier Ltd and INQUA. All rights reserved.
引用
收藏
页码:72 / 77
页数:6
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