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千山油松年轮宽度年表的建立及其与气候的关系
引用本文:陈振举,孙雨,何兴元,陈玮,邵雪梅,张华宇,王忠钰,刘筱彧.千山油松年轮宽度年表的建立及其与气候的关系[J].应用生态学报,2007,18(10):2191-2201.
作者姓名:陈振举  孙雨  何兴元  陈玮  邵雪梅  张华宇  王忠钰  刘筱彧
作者单位:1. 中国科学院沈阳应用生态研究所,沈阳,110016
2. 中国科学院地理科学与资源研究所,北京,100101;中国科学院青藏高原研究所,北京,100085
3. 千山风景名胜区管理委员会,辽宁鞍山,114045
基金项目:国家自然科学基金;中国科学院知识创新工程项目;中国科学院知识创新工程项目;辽宁省省院合作项目;中国科学院知识创新工程项目;鞍山市科学技术局千山风景名胜区名木古树扶壮研究项目
摘    要:以千山油松为样本,建立了年轮宽度标准化年表、差值年表和自回归年表.结果表明,油松年轮宽度与5—7和9—11月温度指标的相关性较高,且与低温呈正相关,其中与7月的极端最低温、9月的平均最低温显著相关.3种年表与上年12月和当年1月的极端最低温、1月的平均最低温呈显著相关,且其与全年、上年12月、当年5月的降水量显著相关,与4月的降水量极显著相关.油松与水汽压、相对湿度的月和年指标均有较强的相关性.蒸发的年指标和绝大部分月指标对油松生长具有负效应,其中4—7月最明显.油松年表的窄化突变佐证了1800年以来的30次主要的旱灾年历史记录.千山油松的生长受全球或半球尺度气候变化的影响.年表与太阳活动存在显著的11、23和50年左右的公共周期,与地磁指标在10、20和45年左右存在共同的周期变化.

关 键 词:千山  油松  年轮宽度年表  气候
文章编号:1001-9332(2007)10-2191-11
修稿时间:2006-10-09

Chinese pine tree ring width chronology and its relations to climatic conditions in Qianshan Mountains
CHEN Zhen-ju,SUN Yu,HE Xing-yuan,CHEN Wei,SHAO Xue-mei,ZHANG Hua-yu,WANG Zhong-yu,LIU Xiao-yu.Chinese pine tree ring width chronology and its relations to climatic conditions in Qianshan Mountains[J].Chinese Journal of Applied Ecology,2007,18(10):2191-2201.
Authors:CHEN Zhen-ju  SUN Yu  HE Xing-yuan  CHEN Wei  SHAO Xue-mei  ZHANG Hua-yu  WANG Zhong-yu  LIU Xiao-yu
Institution:1 Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China ; 2Institute of Geographical Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China ; 3Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100085, China; 4Administration Committee of Qianshan Mountain Scenic Spot, Anshan 114045, Liaoning, China
Abstract:Taking Chinese pine in Qianshan Mountains as a sample,the tree ring width chronology including standard,residual,and Arstan chronologies was established.The results showed that the tree ring width of Chinese pine had a higher correlation with the temperature in May-July and in September-November,and significant positive correlations were observed between the tree ring width and the extreme minimum temperature in July and mean minimum temperature in September.The chronology had significant or very significant correlations with the extreme minimum temperature in December and next January,mean minimum temperature in January,annual precipitation,and the precipitation in April,May and last December.Chinese pine had stronger responses to the monthly/yearly water vapor pressure and relative humidity.The yearly and most monthly evaporation had negative effects on the growth,being most significant for the evaporation in April-July.The narrowed tree rings recorded by the chronology demonstrated the 30 times of extreme drought since 1 800.The growth of Chinese pine in Qianshan Mountains was also affected by the climate changes on global and hemisphere scales.There existed 11-,23-and 50-year-common periodicity between the chronology and solar activity,and 10-,20-and 45-year-common periodicity between the chronology and geomagnetic activity.
Keywords:Qianshan Mountains  Chinese pine  tree ring width chronology  climate
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