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宁夏罗山油松(Pinus tabulaeformis)树轮宽度对气候因子的响应分析
引用本文:王亚军,马玉贞,郑影华,鲁瑞洁,桑艳礼,蒙红卫.宁夏罗山油松(Pinus tabulaeformis)树轮宽度对气候因子的响应分析[J].中国沙漠,2009,29(5):971-976.
作者姓名:王亚军  马玉贞  郑影华  鲁瑞洁  桑艳礼  蒙红卫
作者单位:1. 北京师范大学,环境演变与自然灾害教育部重点实验室,沙漠与沙区资源研究所,北京,100875;河北工程大学,资源学院,河北,邯郸,056038
2. 北京师范大学,环境演变与自然灾害教育部重点实验室,沙漠与沙区资源研究所,北京,100875
3. 兰州大学,资源环境学院,甘肃,兰州,730000
基金项目:国家自然科学基金,高等学校博士学科点专项科研基金 
摘    要: 树轮样本采自宁夏罗山油松纯林的下限和上限。建立了下限和上限的树轮宽度标准化年表,分析了树轮宽度与降水、气温、湿润指数(P/T)的相关关系,结果显示,下限和上限树轮宽度指数都与当年3月、5月、春季以及年降水量显著正相关,与7月气温显著负相关;下限树轮宽度标准化年表与气候要素的相关系数一般大于上限的相关系数,而且下限树轮宽度与前一年9月、秋季降水以及夏季气温的相关也达到显著水平,表明下限树轮宽度标准化序列对降水和气温单一气候要素的变化较敏感;下限和上限的树轮宽度指数和湿润指数(P/T)呈正相关关系,而且上限树轮宽度和3—8月湿润指数的正相关达到99%的置信水平,说明罗山油松纯林上限树轮宽度标准化序列对水热组合的响应较敏感。

关 键 词:罗山  树木年轮  响应关系
收稿时间:2008-9-27
修稿时间:2009-5-4

Response of Tree-Ring Width of Pinus tabulaeformis to Climate Factors in Luoshan Mountains of Ningxia
WANG Ya-jun,MA Yu-zhen,ZHENG Ying-hua,LU Rui-jie,SANG Yan-li,MENG Hong-wei.Response of Tree-Ring Width of Pinus tabulaeformis to Climate Factors in Luoshan Mountains of Ningxia[J].Journal of Desert Research,2009,29(5):971-976.
Authors:WANG Ya-jun  MA Yu-zhen  ZHENG Ying-hua  LU Rui-jie  SANG Yan-li  MENG Hong-wei
Institution:1.Key Laboratory of Environmental Changes and Natural Disaster under the Ministry of Education of China in Beijing Normal University; China Center of Desert Research of Beijing Normal University, Beijing 100875, China; 2.The Resource College of Hebei University of Engineering, Handan 056038, Hebei, China; 3.College of Earth and Environmental Science, Lanzhou University, Laznhou 730000, China
Abstract:Tree-ring cores are sampled at lower and upper forest border of pure forests of Pinus tabulaeformis in Luoshan Mountains of Ningxia. The authors develop the tree-ring width index standard chronologies and analyze the statistical characters of two sites chronologies. After anglicizing the response relationship between tree-ring width and precipitation, temperature and moisture index (P/T), it is found out that the standard chronologies of two sites are all significantly related to March, May, spring and the annual precipitation and July temperature. There is a significant relation between the tree-ring width and the prior September precipitation, autumn precipitation and summer temperature at lower forest border. Based on the size of the correlation coefficient and the number of significant factors, it is pointed out that the tree-ring width index standard chronology at lower forest border is relatively sensitive to the precipitation and temperature than that at upper forest border. Furthermore the tree-ring width trends are all positively correlative with the humid index, and the correlation coefficient between the tree-ring width standard chronology at upper forest border and March to August moisture index reaches 99% level. The standard chronology at upper forest border is relatively sensitive to the combination of water and heat.
Keywords:Luoshan Mountains  tree-ring width  response relationship
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