气候变化

云南丽江树轮δ18O记录的大气环流变化信息

展开
  • 中国科学院寒区旱区环境与工程研究所 冰冻圈科学国家重点实验室,兰州 730000
安文玲, 女。E-mail:wenlingan13@yahoo.com.cn

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

Expand
  • State Key Laboratory of Cryospheric Science,Cold and Arid Regions Environmental and Engineering Research Institute,CAS,Lanzhou 730000,China

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

摘要

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。

本文引用格式

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

Abstract

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.

参考文献


[1] Helle G. Interpreting Climate Proxies from Tree-rings. Berlin: Springer-Verlag, 2004. 129-148.

[2] Schweingruber F H. Tree Rings: Based and Application of Dendro-chronology. Dordrecht: Kluwer Press, 1988.

[3] Liu Xiaohong, Qin Dahe, Shao Xuemei et al. Temperature variations recovered from tree-rings in the middle Qilian Mountain over the last millennium. Science in China: Series D, 2005, 48(4): 521-529.

[4] Panek J A, Waring R H. Stable carbon isotopes as indicators of limitations to forest growth imposed by climate stress. Ecol. Appl., 1997, 7: 854-863.

[5] Loader N J, Robertson I, McCarroll D. Comparison of stable carbon isotope ratios in the wholewood, cellulose and lignin of oak tree-rings. Palaeogeography, Palaeoclimatology, Palaeoecology, 2003, 196: 395-407.

[6] Qian Junlong, Deng Ziwang, Tu Qipu et al. Climatic significance of δD time series in tree rings from Tianmu Mountain. Science in China: Series D, 2001, 44(12): 1140-1146.

[7] Liu Xiaohong, Shao Xuemei, Wang Lily et al. Climatic significance of the stable carbon isotope composition of tree-ring cellulose: Comparison of Chinese hemlock (Tsuga chinensis Pritz) and alpine pine (Pinus densata Mast) in a temperate-moist region of China. Science in China: Series D, 2007, 50(7): 1076-1085.

[8] Hiroyuki Tsuji. δ18O of tree-ring cellulose in two species (spruce and oak) as proxies of precipitation amount and relative humidity in northern Japan. Chemical Geology, 2006, 231: 67-76.

[9] Martine Reb Etez, Matthias Saure, Paolo Cherubini. To what extent can oxygen isotope in tree rings and precipitation be used to reconstruct past atmospheric temperature? A case study. Climate Change, 2003, 61: 237-248.

[10] Liu Xiaohong, Qin Dahe, Shao Xuemei et al. Variation and abrupt change of precipitation in Nyingchi Prefecture of Tibet Autonomous Region in past 350 years. Journal of Glaciology and Geocryology, 2003, 25(4): 375-379.
[刘晓宏, 秦大河, 邵雪梅 等. 西藏林芝地区近350a来降水变化及突变分析. 冰川冻土, 2003, 25(4): 375-379.]

[11] Qian Junlong, Lu Jun, Tu Qipu et al. Reconstruction of the climate in the Tianmu Mountain area, Zhejiang Province, in the last 160 years by δ13C sequence of tree ring δ-cellulose. Science in China: Series D, 2002, 45(5): 409-419.

[12] Liu Xiaohong, Qin Dahe, Shao Xuemei, et al. Climatic significance of stable carbon isotope in tree rings of Abies spectabibis in southern Tibet. Chinese Science Bulletin, 2003, 48(18): 2000-2004.

[13] James R Ehleringer, Anthony E Hall, Graham D. Farquhar. Stable isotope and plant carbon-water relations. San Diego: Academic Press Inc., 1993. 71-88.

[14] Robertson I, Waterhouse J S, Baker A C et al. Oxygen isotope ratios of oak in east England: Implications for reconstructing the isotopic composition of precipitation. Earth and Planetary Science Letters, 2001, 191(1/2): 21-31.

[15] Feng Xiahong, Cui Haiting, Tang Kuilian et al. Tree-ring δD as an indicator of Asian monsoon intensity. Quaternary Research, 1999, 51(3): 262-266.

[16] Burk R L and Stuiver M. Oxygen isotope ratios in trees reflect mean annual temperature and humidity. Science, 1981, 211: 1417-1419.

[17] Dansgaard W. Stable isotopes in precipitation. Tellus, 1964, 16B:436-438.

[18] John Gray, Peter Thompson. Climatic information from 18O/16O ratios of cellulose in tree rings. Nature, 1976, 262: 481-482.

[19] Libby L M, Pandolfi L J. Temperature dependence of isotope ratios in tree rings. Proc. Nat. Acad. Sci. USA, 1974, 71(6): 2482-2486.

[20] Liu Weiguo, Feng Xiahong, Liu Yu et al. δ18O values of tree rings as a proxy of monsoon precipitation in arid Northwest China. Chemical Geology, 2004, 206: 73-80.

[21] Liu Yu, Cai Qiufang, Liu Weiguo, et al. Monsoon precipitation variation recorded by tree-ring δ18O in arid Northwest China since AD 1878. Chemical Geology, 2008, 252(1/2): 56-61.

[22] Fritts H C. Tree Rings and Climate. London: Academic Press, 1976. 55-115.

[23] Raymond S Bradley. Paleoclimatology: Reconstructing Climates of the Quaternary. London: Academic Press, 1999: 397-439.

[24] Merela M, Pelicon P. Application of micro-PIXE, MRI and light microscopy for research in wood science and dendrochronology, 2009, 03.062. (Accepted).

[25] Buckley B M, Duangsathaporn K, Palakit K et al. Analyses of growth rings of Pinus merkusii from Lao P.D.R. Forest Ecology and Management, 2007, 253(1-3): 120-127.

[26] Li Zongxing, He Yuanqing, Jia Wenxiong et al. Chemical composition analysis of summer rainfalls in Lijiang. Environmental Science, 2009, 30(2): 362-367.
[李宗省, 何元庆, 贾文雄 等. 丽江市夏季降水化学组成分析. 环境科学, 2009, 30(2): 362-367.]

[27] Green J W. Wood cellulose. In: Whitler R L (ed.). Methods in Carbohydrate Chemistry. New York: Academic Press, 1963. 9-12.

[28] Loader N J, Robertson I, Barker A C et al. An improved technique for the batch processing of small whole wood samples to δ-cellulose. Chemical Geology, 1997, 136: 313-317.

[29] Wu Guanghe, Tian Lianshu, Hu Shuangxi et al. Physical Geography. 3rd ed. Beijing: Higher Education Press, 2000. 83.
[伍光和, 田连恕, 胡双熙 等. 自然地理学. 3版. 北京: 高等教育出版社, 2000. 83.]

[30] Roig F A, Siegwolf R, Boninsegna J A. Stable oxygen isotopes (δ18O) in Austrocedrus chilensis tree rings reflect climate variability in northwestern Patagonia, Argentina. Int. Biometeorol., 2006, 51: 97-105.

[31] Haurwitz M, Brier G W. A critique of the superposed epoch analysis method: Its application to solar weather relations. Monthly Weather Review, 1981, 109: 2074-2079.

[32] Duan Xu, Ju Jianhua, Xiao Ziniu et al. Climatic Anomaly of Physical Process and Research for Predicting Signal in Yunnan Province. Beijing: China Meteorological Press, 2000: 10-11.
[段旭, 踞建华, 肖子牛 等. 云南气候异常物理过程及预测信号的研究. 北京: 气象出版社, 2000: 10-11.]

[33] Evans M N, Schrag D P. A stable isotope-based approach to tropical dendroclimatology. Geochimica et Cosmchimica Acta, 2004, 68(16): 3295-3305.

[34] Louise E Cullen, Pauline F Grierson. A stable oxygen, but not carbon, isotope chronology of Callitris columellaris reflects recent climate change in north-western Australia. Climate Change, 2007, 85(1): 213-229

[35] Quinn W H, Neal V T. The historical record of El Nino events. In: Bradley R S, Jones P (eds.). Climate since 1500. London: Routledge, 1992. 623-648.

[36] Wang Shaowu, Gong Daoyi. ENSO events and intensity during the past century. Meteorological Monthly, 1999, 25(1): 9-13.
[王绍武, 龚道溢. 近百年来的ENSO事件及其强度. 气象, 1999, 25(1): 9-13.]

[37] Li J, Zeng Q. A new monsoon index, its interannual variability and relation with monsoon precipitation. Climatic and Environmental Research, 2005, 10(3): 351-365.

[38] Guo Qiyun, Cai Jingning, Shao Xuemei et al. Studies on the variations of East-Asia summer monsoon during AD 1873-2000. Chinese Journal of Atmospheric Science, 2004, 28(2): 206-215.
[郭其蕴, 蔡静宁, 邵雪梅 等. 1873-2000年东亚夏季风变化的研究. 大气科学, 2004, 28(2): 206-215.]

[39] Danny McCarroll, Neil J Loader. Stable isotopes in tree rings. Quaternary Science Reviews, 2004, 23: 771-801.

[40] Waterhouse J S, Switsur V R, Barker A C et al. Oxygen and hydrogen isotope ratios in tree rings: how well do models predict observed values? Earth and Planetary Science Letters, 2002, 201: 421-430.

[41] He Yuanqing, Yao Tandong, Kang Jiancheng, et al. Distribution features of stable oxygen isotopes in the typical monsoon temperate-glacier region, Mountain Yulong in China. Chinese Journal of Polar Science, 2001, 12(1): 31-38.

[42] Liu Zhongfang, Tian Lide, Chai Xurong et al. A model-based determination of spatial variation of precipitation δ18O over China. Chemical Geology, 2008, 249(1/2): 203-212.

[43] Pang Hongxi, He Yuanqing, Lu Aigang et al. Variation in δ18O of Lijiang precipitation in synoptic scale. Chinese Science Bulletin, 2006, 51(10): 1218-1224.
[庞洪喜, 何元庆, 卢爱刚 等. 天气尺度下丽江季风降水中δ18O变化. 科学通报, 2006, 51(10): 1218-1224.]

[44] Samuel Epstein, Peter Thompson, Crayton J Yapp. Oxygen and hydrogen isotopes ratios in plant cellulose. Science, 1977, 198: 1209-1215.

[45] John S Roden, Lin Guanghui, James R Ehleringer. A mechanistic model for interpretation of hydrogen and oxygen isotope ratios in tree-ring cellulose. Geochimica et Cosmochinica Acta, 2000, 64(1): 21-35.

[46] Ramesh R, Bhattacharya S K, Gopalan K. Climatic correlations in the stable isotope records of silver fir (Abies Pindrow) trees from Kashmir, India. Earth and Planetary Science Letters, 1986, 79: 66-74.

文章导航

/