Arid
呼伦贝尔沙地樟子松年轮生长对气候变化的响应
其他题名Response of tree-ring width of Pinus sylvestris var.mongolica to climate change in Hulunbuir sand land,China
尚建勋1; 时忠杰2; 高吉喜3; 徐丽宏4; 吕世海5; 冯朝阳5; 王鲁秀6
来源期刊生态学报
ISSN1000-0933
出版年2012
卷号32期号:4页码:1077-1084
中文摘要以内蒙古呼伦贝尔地区沙地樟子松为样本,建立了樟子松树木年轮宽度年表,应用相关分析和响应函数分析等年轮气候学方法,研究了樟子松径向生长对气候变化的响应。结果表明,樟子松年轮宽度与4月和69月平均温度呈显著负相关关系(P<0.05);与各月降水量多呈正相关关系,特别是与当年58月的月降水量呈显著正相关关系(P<0.05);树轮年表与前一年10月至当年10月的PDSI均呈显著正相关关系(P<0.05),其中与5月份PDSI的相关性最高。响应函数分析表明,年表与当年67月的平均气温、上一年10月和当年57月份的降雨存在显著的相关性,与57月份PDSI存在较显著的正相关性;综合来看,呼伦贝尔沙地樟子松生长同时受降水和温度的影响,其径向生长与气候因子间的关系属于降水敏感型,为区域降水重建提供了科学基础。
英文摘要In order to analyze the response of tree radial growth on the climate change in the semi-arid area,the tree-ring width chronology of Pinus sylvestris var.mongolica in Hulunbuir,Inner Mongolia,including the standard chronology(STD),residual chronology(RES) and autoregressive chronology(ARS),was developed by fitting a negative exponential in this paper.According to the analysis on statistical characteristics,STD chronology showed quite well correlation between samples of different trees(correlation coefficient between trees,namely r = 0.520,P <0.01),indicating good consistency of variance characteristics of the ring-width among different trees,and thus the climate information recorded by those sampled trees can be regarded as reliable.The relationship between ring width and climate factors such as monthly mean precipitation and temperature from the previous October to current October was analyzed by correlation analysis and response function analysis during the observation period(19522008).The results indicate that the tree-ring width is negatively correlated to the monthly mean temperature,and the data shows a significant negative correlation from June to September in the current year(P <0.05).The mean temperature,especially the maximum temperature from June to August may constrain tree growth indirectly due to the enhanced evapotranspiration and decreased availability of soil moisture.The tree-ring width is significantly positively correlated to the monthly precipitation from May to August in the current year(P <0.05),and the highest correlation coefficient is observed between tree-ring width and the precipitation of current July(r=0.394,P<0.05).Low total annual precipitation is generally regarded as the main factor to constrain the growth of trees,indicating a clear physiological sense for the notable positive correlation between tree-ring width index and precipitation.There is no significant correlation between the tree-ring width and the precipitation from previous December to current April,but in general they were positively correlated.The tree-ring width chronology is significantly positively correlated with the Palmer Drought Severity Index(PDSI) from last October to current October during 19512005,which comprehensively reflects the effect of available soil moisture,precipitation and temperature,especially during May.The response function analysis showed that the chronology is significantly correlated with the average temperature from June to July,the amount of precipitation from May to July of the current year,and that of last October,and positively related to the PDSI from May to July.These results show that the tree-ring width of Pinus sylvestris var.mongolica in Hulunbuir is affected by the temperature and precipitation in the growing seasons simultaneously,but the effect of precipitation on the tree radial growth is much greater than that of temperature on the yearly scale.In general,precipitation is a direct limiting factor to the radial growth of Pinus sylvestris var.mongolica in Hulunbuir area,while the temperature is an indirect limiting factor.Namely,the radial growth of Pinus sylvestris var.mongolica is more sensitive to precipitation.This study will be helpful for the precipitation and temperature reconstruction of Hulunbuir region.
中文关键词呼伦贝尔 ; 沙地樟子松 ; 年轮宽度 ; 气候变化 ; 响应
英文关键词Hulunbuir sandy Pinus sylvestris var.mongolica tree-ring width climate change response
语种中文
国家中国
收录类别CSCD
WOS类目FORESTRY
WOS研究方向Forestry
CSCD记录号CSCD:4446443
来源机构中国林业科学研究院荒漠化研究所
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/228431
作者单位1.水利部松辽水利委员会水土保持处, 长春, 吉林 130021, 中国;
2.中国林业科学研究院荒漠化研究所, 北京 100091, 中国;
3.环境保护部南京环境科学研究所, 南京, 江苏 210042, 中国;
4.中国林业科学研究院森林生态环境与保护研究所, 国家林业局森林生态环境重点试验室, 北京 100091, 中国;
5.中国环境科学研究院生态所, 北京 100012, 中国;
6.中国人民大学环境学院, 北京 100872, 中国
推荐引用方式
GB/T 7714
尚建勋,时忠杰,高吉喜,等. 呼伦贝尔沙地樟子松年轮生长对气候变化的响应[J]. 中国林业科学研究院荒漠化研究所,2012,32(4):1077-1084.
APA 尚建勋.,时忠杰.,高吉喜.,徐丽宏.,吕世海.,...&王鲁秀.(2012).呼伦贝尔沙地樟子松年轮生长对气候变化的响应.生态学报,32(4),1077-1084.
MLA 尚建勋,et al."呼伦贝尔沙地樟子松年轮生长对气候变化的响应".生态学报 32.4(2012):1077-1084.
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