云南丽江树轮δ18O记录的大气环流变化信息
收稿日期: 2009-06-02
修回日期: 2009-07-09
网络出版日期: 2009-09-25
基金资助
中国科学院方向性项目 (KZCX2-YW-317); 国家重点基础研究发展规划 (2007CB411506); 国家自然科学基金 (40871002)
Atmospheric Circulation Information Recorded in Tree-ring δ18O at Lijiang, Yunnan Province
Received date: 2009-06-02
Revised date: 2009-07-09
Online published: 2009-09-25
Supported by
Knowledge Innovation Project of Chinese Acadamy of Sciences, No.KZCX2-YW-317;National Basic Research Program of China (973 Program), No.2007CB411506;National Natural Science Foundation of China, No.40871002
通过对云南玉龙雪山丽江冷杉年轮晚材纤维素氧同位素 (δ18O) 的分析，建立了1902-2004时段年分辨率的树轮δ18O序列。将所得序列与相邻的丽江市气象站记录的气候资料对比，分析了树轮δ18O对气候要素的响应。结果表明，丽江冷杉年轮晚材中的δ18O与其生长季气候因子密切相关。主要与季风期 (8-10月) 的降水和相对湿度、6-10月总云量、5-6月平均温度显著相关，尤其和总云量相关性最高 (r = -0.45，P = 0.01)。同时，树轮δ18O年际变化与南亚季风指数、东亚夏季风指数呈反相关关系，并与1-5月南方涛动指数负相关显著，在一定程度上反映了大尺度的大气环流影响。
安文玲,刘晓宏,陈拓,徐国保,侯书贵,孙维贞 . 云南丽江树轮δ18O记录的大气环流变化信息[J]. 地理学报, 2009 , 64(9) : 1103 -1112 . DOI: 10.11821/xb200909008
In this paper, tree-ring latewood stable oxygen isotope composition (δ18O) of Lijiang fir (Abies forrestii) was used to estimate the climatic response of tree-ring δ18O by comparing the δ18O values with meteorological records from Lijiang meteorological station. The annually resolved tree-ring δ18O chronology spans the period of 1902-2004. Results indicate that tree-ring δ18O values of latewood were significantly correlated with climate conditions during the growth season. Tree-ring δ18O was mainly correlated with precipitation and relative humidity of the wet season in summer (August to October). Temperature had a weak influence on the tree-ring δ18O, indicating a relatively high correlation with δ18O in May and June (r = 0.35), prior to the rainy season. The strongest correlation was found between the total cloud cover and tree-ring δ18O covering the whole wet season (June to October). Furthermore, tree-ring δ18O shows negative and significant correlations with South Asia monsoon index and East Asia monsoon index in different periods. Meanwhile, a strong correlation between tree-ring δ18O and SOI during the period of 1902-2004, to some degree, indicates that the tree-ring δ18O recorded a large amount of atmospheric circulation information.
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