| 引用本文: | 郑紫薇,赵兴云,商志远,王建,成瑞琴,陈振举.2014.利用黑松树轮δ13C 重建山东塔山地区近七十年来冬春季节的平均气温[J].地球环境学报,(1):10-15 |
| ZHENG Zi-wei,ZHAO Xing-yun,SHANG Zhi-yuan,WANG Jian,CHENG Rui-qin,CHEN Zhen-ju.2014.The winter and spring average temperature reconstruction based on tree ring δ13C in recent 70 years in Tashan, Shandong Province[J].Journal of Earth Environment,(1):10-15 |
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| 利用黑松树轮δ13C 重建山东塔山地区近七十年来冬春季节的平均气温 |
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郑紫薇1,2,赵兴云2,3,商志远4,王建4,成瑞琴1,2,陈振举5
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1. 山东师范大学 人口、资源与环境学院，济南 250000;2. 临沂大学 资源环境学院，临沂 276000;3. 山东省水土保持与环境保育重点实验室，临沂 276000;4. 南京师范大学 地理科学学院，南京210023;5. 沈阳农业大学 林学院，沈阳 110866
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| 摘要: |
| 对采自山东塔山的黑松(Pinus thunbergii Parl) 树芯样本进行交叉定年后建立树轮稳定碳同位素序列（δ13C 序列）。将得到的树轮δ13C 序列进行校正以去除大气CO2的影响，提取其高频部分分析与气候要素的响应关系，发现黑松树轮δ13C 的高频序列与对应年份平均气温的响应比对降水量的响应显著。气温和降水对树轮δ13C 的影响均有滞后效应，即塔山地区树轮δ13C 能记录冬季气候变化。在相关分析基础上用回归方程重建了山东塔山地区近七十年冬春季节（即上年12 月— 当年5 月）的平均气温，分析发现重建序列有明显的冷暖交替上升的变化趋势。 |
| 关键词: 塔山 树轮 δ13C 平均气温 |
| DOI：10.7515/JEE201401002 |
| CSTR：32259.14.JEE201401002 |
| 分类号:P467 |
基金项目:国家自然科学基金项目(41072139)；山东省自然科学基金项目(Y2008E15)
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| 英文基金项目: |
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| The winter and spring average temperature reconstruction based on tree ring δ13C in recent 70 years in Tashan, Shandong Province |
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ZHENG Zi-wei1,2, ZHAO Xing-yun2,3, SHANG Zhi-yuan4, WANG Jian4, CHENG Rui-qin1,2, CHEN Zhen-ju5
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1. College of Population, Resources and Environment, Shandong Normal University, Jinan 250000, China; 2. College of Resources and Environment, Linyi University, Linyi 276000, China; 3. Shandong Provincial Key Laboratory of Water and Soil Conservation and Environmental Protection, Linyi 276000, China; 4. College of Geographical Science, Nanjing Normal University, Nanjing 210023, China; 5. Forestry College, Shenyang Agricultural University, Shenyang 110866, China
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| Abstract: |
| Tree-ring samples of Pinus thunbergii Parl at eastern Tashan in Shandong Province were collected to integrate the tree-ring stable carbon isotope series. In order to remove the influence of atmospheric CO2, extract the high frequency part of the tree ring δ13C. Analysis the response of tree ring δ13C series and climate factors, found that the response between tree ring δ13C and temperature is obvious than precipitation. There exists a lagging effect of the influence of both temperature and precipitation on tree-ring δ13C in some extent. This results indicated that tree ring δ13C in Tashan can record the winter climate change. On the basis of correlation analysis, utilize the regression equation to reconstruct near seventy years' average temperature in winter and spring season (i.e., from December last year to May current year). Analysis found that the rebuilding temperature series shows an obviously rise trend which cold and warm temperature change alternately. |
| Key words: Tashan tree-ring δ13C average temperature |
