[1]陈 峰,袁玉江,喻树龙.闽中北柳杉树轮指示的气候信号与季风区不同地域干湿变化关系[J].山地学报,2015,(06):690-695.[doi:10.16089/j.cnki.1008-2786.000083]
 CHEN Feng,YUAN Yujiang,YU Shulong.Drought Signals in the Tree-ring Width Record of Cedar(Cryptomeria fortunei)Trees from North Central Fujian: Linkages to the Monsoonal Regions[J].Mountain Research,2015,(06):690-695.[doi:10.16089/j.cnki.1008-2786.000083]
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闽中北柳杉树轮指示的气候信号与季风区不同地域干湿变化关系()
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2015年06期
页码:
690-695
栏目:
山地生态与环境
出版日期:
2015-12-01

文章信息/Info

Title:
Drought Signals in the Tree-ring Width Record of Cedar(Cryptomeria fortunei) Trees from North Central Fujian: Linkages to the Monsoonal Regions
作者:
陈 峰12袁玉江1喻树龙1
1.中国气象局乌鲁木齐沙漠气象研究所 中国气象局树木年轮理化研究重点实验室 新疆树轮生态实验室,新疆 乌鲁木齐 830002; 2. 兰州大学西部环境教育部重点实验室 资源环境学院,甘肃 兰州 730000
Author(s):
CHEN Feng12 YUAN Yujiang1 YU Shulong1
1. Xinjiang Laboratory of Tree Ring Ecology/Key Laboratory of Tree-ring Physical and Chemical Research of China Meteorological Administration, Institute of Desert Meteorology,China Meteorological Administration, Urumqi 830002,China; 2. MOE Key Laboratory of Western China's Environmental Systems, Collaborative Innovation Centre for Arid Environments and Climate Change, Lanzhou University, Lanzhou 730000, China
关键词:
福建中北部 柳杉 树木年轮 干湿变化
Keywords:
north central Fujian Cryptomeria fortunei tree rings dry and wet change
分类号:
P461,P467
DOI:
10.16089/j.cnki.1008-2786.000083
文献标志码:
A
摘要:
利用采自闽中北部柳杉树轮样芯,建立树轮宽度标准化年表,通过树轮气候响应分析, 发现柳杉树径向生长主要反映了该地上年7月至当年2月帕尔默干旱指数(PDSI)变化(r=0.6, p<0.001)。进一步研究发现,该年表与山东地区油松树轮年表有着良好相关,他们之间的第一主成分能够准确指示东部沿海季风区干湿变化(r=0.661, p<0.001),并揭示6个偏湿阶段和5个偏干阶段。该第一主成分序列所记录的一些极端干旱事件与中国北方干旱半干旱地区的极端干旱事件有着良好对应,这些极端干旱事件对中国社会有着重要影响。同时也发现该第一主成分序列与东亚夏季风尾闾区的兴隆山降水序列在低频变化上具有很好的一致性,并准确记录了最近30 a东亚夏季风变化趋势。
Abstract:
Based on the tree-ring cores of Cryptomeria fortunei collected from north central Fujian, China, the standardized tree-ring width chronology was developed. Growth-climate response analyses showed that the growth of Cryptomeria fortunei is mainly influenced by July-February PDSI variability. There is a reasonable agreement with wet/dry periods previously estimated from tree-ring record in Shandong. Based on the results of principal component analyses, June-February PDSI is the most important forces on the tree growth at the sites(r=0.661, p<0.001). Analyzing the first principal component of tree-ring series,we found that:1)During the last 138 years, 6 wet periods and 5 dry periods were happen in eastern China; 2)Drought events in the first principal component of tree-ring series are compared to the historical archives and other moisture-sensitive tree-ring width series in northern China. The results reveal common climatic extremes over much of China. Many of these events have had profound impacts on the peoples of China over the past several centuries; 3)The low-frequency change of the first principal component of tree-ring series is correlated positively with the precipitation reconstruction for the Xinglong Mountains of Lanzhou in the monsoonal tail region, and captures the current trend of East Asia summer monsoon.

参考文献/References:

[1] Cook E R, Anchukaitis K J, Buckley B M, et al. Asian monsoon failure and megadrought during the last millennium [J]. Science, 2010, 328:486-489
[2] Buckley B M, Anchukaitis K J, Penny D, et al. Climate as a contributing factor in the demise of Angkor [J]. Proceedings of the National Academy of Sciences of the United States of America, 2010, 107: 6748-6752
[3] Buckley B M, Palakit K, Duangsathaporn K, et al. Decadal scale droughts over northwestern Thailand over the past 448 years: Links to the tropical Pacific and Indian Ocean sectors [J]. Climate Dynamics, 2007, 29:63-71
[4] D'Arrigo R, Abram N, Ummenhofer C, et al. Reconstructed streamflow for Citarum River, Java, Indonesia: linkages to tropical climate dynamics [J]. Climate Dynamics, 2011, 23:451-462
[5] D'Arrigo R, Palmer J, Ummenhofer C C, et al. Three centuries of Myanmar monsoon climate variability inferred from teak tree rings [J]. Geophysical Research Letters 38, 2011, L24705, doi: 10.1029/2011GL049927
[6] Sano M, Buckley B M, Sweda T. Tree-ring based hydroclimate reconstruction over northern Vietnam from Fokienia hodginsii: eighteenth century mega-drought and tropical Pacific influence [J]. Climate Dynamics, 2009, 33:331-340
[7] Chen F, Yuan Y J, Wei W S, et al. Reconstructed temperature for Yong'an, Fujian, southeast China: Linkages to the Pacific Ocean climate variability [J]. Global and Planetary Change, 2012, 86-87:11-19
[8] Chen F, Yuan Y J, Wei W S, et al. Tree-ring based winter temperature reconstruction for Changting, Fujian, southeast China, since 1850 [J]. Theoretical and Applied Climatology, 2012, 109:141-151
[9] Shi J F, Cook E R, Lu H Y, et al. Tree-ring based winter temperature reconstruction for the lower reaches of the Yangtze River in southeast China [J]. Climate Reseach, 2010, 41:169-175
[10] Duan J P, Zhang Q B, Lv L X. Increased Variability in Cold-Season Temperature since the 1930s in Subtropical China [J]. Journal of Climate, 2013, 26:4749-4757
[11] Chen Feng, Yuan Yujiang, Wei Wenshou, et al. Correlation between the summer Asian Pacific oscillation index and the tree-ring width of Pinus massiniana from Sha county, Fujian province[J]. Quaternary Sciences, 2011, 31(1):96-103 [陈峰, 袁玉江, 魏文寿, 等. 福建沙县马尾松树轮宽度与夏季亚洲-太平洋涛动指数的关系 [J]. 第四纪研究, 2011, 31(1):96-103]
[12] Fritts H C. Tree Rings and Climate [M]. London: Academic Press, 1976.
[13] Holmes R L. Computer-assisted quality control in tree-ring dating and measurement [J]. Tree-ring Bulletin, 1983, 43:69-75
[14] Cook E R. A time series analysis approach to tree-ring standardization[D]. Tucson: The University of Arizona,1985.
[15] Cook E R, Kairiukstis L. Methods of dendrochronology: applications in the environmental sciences [M]. New York: Springer,1990.
[16] van der Schrier G, Jones P D, Briffa R. The sensitivity of the PDSI to the Thornthwaite and Penman-Monteith parameterizations for potential evapotranspiration [J]. Journal of Geophysical Research, 2011, 116(D3), doi:10.1029/2010JD015001
[17] Biondi F, Waikul K. DENDROCLIM2002: a C++ program for statistical calibration of climate signals in tree-ring chronologies[J]. Computers and Geosciences, 2004, 30:303-311
[18] Shen Changsi, Chen Jinmin, Zhang Zhihua, et al. Utlizing tree ring chronologies to reconstruct 200 years moisture index in Yi shan, Shandong province [J]. Geographical Reseach, 1998, 17(2): 150- 156 [沈长泗, 陈金敏, 张志华, 等. 利用树木年轮资料重建山东沂山地区200多年来的湿润指数[J]. 地理研究, 1998, 17(2): 150-156]
[19] Chen F, Wang H Q, Chen F H, et al. Tree-ring reconstruction of July-May precipitation(AD 1816—2010)in the northwestern marginal zone of the East Asian summer monsoon reveals the monsoon-related climate signals[J]. International Journal of Climatology, 2014, doi: 10.1002/joc.4110
[20] Hao Z X, Zheng J Y, Wu G F, et al. 1876-1878 severe drought in North China: Facts, impacts and climatic background[J]. Chinese Science Bulletin, 2010, 55:3001-3007
[21] Yuan Lin. Disaster history in Northwest China [M]. Lanzhou: The Gansu People's Press, 1994. [袁林. 西北灾荒史[M]. 兰州:甘肃人民出版社, 1994.]
[22] Chen Feng,Yuan Yujiang,Wei Wenshou,et al. Variation and prediction trend of precipitation series for the Tekes River Basin during the last 236 Years[J]. Mountain Research,2010,28(5):545-551 [陈峰, 袁玉江, 魏文寿, 等. 特克斯河流域近236a降水变化及其趋势预测[J]. 山地学报, 2010, 28(5):545-551]
[23] Liang Eryuan, Shao Xuemei, Huang Lei, et a1. Tree-ring records of the 1920s drought in central-western Chinese[J]. Progress in Natural Science,2004,14(4): 469-474 [梁尔源, 邵雪梅, 黄磊,等.中国中西部地区树木年轮对20世纪20年代干旱灾害的指示[J].自然科学进展, 2004, 14(4): 469-474]
[24] Wang HJ. The weakening of the Asian monsoon circulation after the end of 1970s [J]. Advances in Atmospheric Sciences. 2001, 18: 376-386

备注/Memo

备注/Memo:
收稿日期(Received date):2014-12-25; 修回日期(Accepted):2015-06-01。 基金项目(Foundation item):“国家重点基础研究发展规划(2012CB955301), 兰州大学西部环境教育部重点实验室开放基金(lzujbky-2011-t02),国家自然科学基金(41405081, U1203281)共同资助。[This study was supported by the National Basic Research Program of China(2012CB955301), Foundation of Key Laboratory of Western China's Environmental Systems(Ministry of Education)in Lanzhou University(lzujbky-2011-t02)and NSFC Project(41405081, U1203281).] 作者简介(Biography):陈峰(1982-),男,福建沙县人,副研究员,主要从事树木年轮与气候环境变化研究。[Chen Feng(1982-),male,was born in Sha County, Fujian,Associate Professor,work mainly about tree-ring and climate/environment change.] E-mail: feng653@163.com
更新日期/Last Update: 1900-01-01