密云山区油松树轮δ13C对气温和降水量变化的响应

doi:10.11707/j.1001-7488.20180301

摘要/Abstract

摘要： [目的]探究北京市密云山区油松树轮δ¹³C对气温和降水量变化的响应，重建1947-2014年密云山区气候资料，以期为揭示该地区的气候变化规律提供依据。[方法]测定密云山区红门川流域油松树轮δ¹³C值，建立1947-2014年的树轮δ¹³C序列，并剔除序列值中受大气CO₂碳同位素值影响产生的下降趋势，之后获得油松树轮δ¹³C去趋势序列（DS），然后结合当地气象站资料分析油松树轮δ¹³C值对降水和气温变化的响应，构建δ¹³C与降水和气温的关系方程，进而重建1947-2014年的降水和气温资料。[结果]1947-2014年，密云山区油松树轮δ¹³C呈下降趋势，其中，1995-2014年波动较大，剔除大气CO₂背景值的DS序列呈现二次曲线的走势，拐点出现在1980年附近；油松树轮δ¹³C值DS序列与7月平均气温等极显著正相关（r=0.719 7，P<0.01），利用回归方法重建1947-2014年密云山区7月份平均气温，平均值为25.67℃，重建曲线显示该地区气温呈先下降后上升趋势；油松树轮δ¹³C值DS序列与夏季降水量极显著负相关（r=-0.696 7， P<0.01），利用回归方法重建了1947-2014年密云山区夏季降水量，平均值为450.3 mm，自1980年以后，降水量年际变化出现较大波动，并且下降趋势明显。[结论]油松树轮δ¹³C对7月份气温和夏季降水量响应极为显著；1947-2014年密云山区气候变化呈现波动性变暖变干趋势。

关键词: 密云山区, 树木年轮, δ¹³C, 气温, 降水, 气候变化

Abstract: [Objective]To reconstruct the history of climate change and reveal climatic characteristics from 1947 to 2014 in Miyun mountainous area, based on stable carbon isotope (δ¹³C) of tree-ring in Pinus tabulaeformis.[Method]In this paper, tree-ring samples of Pinus tabulaeformis in Miyun mountain area were collected to analyze tree-ring δ¹³C. Moreover, we eliminated the effect of atmospheric CO₂ from original δ¹³C series and establish the de-trend series (DS) of tree-rings. Then, regression equations were established based on analysis of the correlation of δ¹³C DS combined with temperature and precipitation, and further reconstructed the temperature and precipitation histories from 1947 to 2014.[Results] From 1947 to 2014:tree-ring δ¹³C series had a downward trend with a big fluctuation from 1997 to 2014. A quadric curve trend was found in tree-ring DS. Tree-ring δ¹³C DS is extremely and positively correlated with July temperature (r=0.719 7,P<0.01). The average temperature of July from 1947 to 2014 were reconstructed with regression method. Results showed that the average temperature of July firstly declined and then increased since 1980 with an average of 25.67℃. The tree-ring δ¹³C DS was extremely and negatively correlated with summer precipitation (r=-0.696 7,P<0.01). Summer precipitation data from 1947 to 2014 were reconstructed with regression method. Results showed that the average summer precipitation was 450.3 mm. After 1980, summer precipitation fluctuated sharply with an evident declining trend.[Conclusion]The response of tree-rings δ¹³C in Pinus tabulaeformis to July temperature was extremely and positively significant. The tree-ring δ¹³C values were extremely and negatively influenced by summer precipitation. Overall, the climate in Miyun mountainous area showed a fluctuated warming and drying trend from 1947 to 2014.

Key words: Miyun mountain area, tree-ring, δ¹³C, temperature, precipitation, climate change

中图分类号:

S718.5
X173

路伟伟, 余新晓, 贾国栋, 李瀚之, 刘自强. 密云山区油松树轮δ¹³C对气温和降水量变化的响应[J]. 林业科学, 2018, 54(3): 1-7.

Lu Weiwei, Yu Xinxiao, Jia Guodong, Li Hanzhi, Liu Ziqiang. Response of Stable Carbon Isotope of Tree-Ring to Temperature and Precipitation Changes in Pinus tabulaeformis in Miyun Mountain Area[J]. Scientia Silvae Sinicae, 2018, 54(3): 1-7.

参考文献

阿多, 赵文吉, 宫兆宁,等. 2017. 1981-2013华北平原气候时空变化及其对植被覆盖度的影响. 生态学报, 37(2):576-592.
(A D, Zhao W J, Gong Z N, et al. 2017. Temporal analysis of climate change and its relationship with vegetation cover on the north China plain from 1981 to 2013.Acta Ecologica Sinica, 37(2):576-592.[in Chinese])
陈拓, 秦大河, 何元庆,等. 2002. 从树轮δ¹³C序列中提取大气δ¹³C信息的可行性研究. 海洋地质与第四纪地质, 22(4):79-83.
(Chen T, Qin D H, He Y Q, et al. 2002. Study on the feasibility of extracting information on δ¹³C of atmospheric CO₂ from tree-ring δ¹³C. Marine Geology and Quaternary Geology, 22(4):79-83.[in Chinese])
陈向军, 袁玉江, 陈峰, 等. 2008. 天山北坡东部地区树轮宽度年表特征分析. 中国沙漠, 28(5):833-841.
(Chen X J, Yuan Y J, Chen F, et al. 2008.Analysis of tree-ring width chronology characteristics from eastern area on north slope of Tianshan Mountains. Journal of Desert Research, 28(5):833-841.[in Chinese])
靳翔, 徐庆, 刘世荣,等. 2014. 川西亚高山森林岷江冷杉树轮碳稳定同位素对气候要素的响应. 生态学报, 34(7):1831-1840.
(Jin X, Xu Q, Liu S R, et al. 2014. Relationship of stable carbon isotope of Abies faxoniana tree-rings to climate in sub-alpine forest in western Sichuan. Acta Ecological Sinica, 34(7):1831-1840.[in Chinese])
刘贤赵, 张勇, 宿庆, 等. 2014. 现代陆生植物碳同位素组成对气候变化的响应研究进展. 地球科学进展, 29(12):1341-1354.
(Liu X Z, Zhang Y, Su Q, et al. 2014. Research progress in responses of modern terrestrial plant carbon isotope composition to climate change. Advances in Earth Science, 29(12):1341-1354.[in Chinese])
刘晓宏, 秦大河, 邵雪梅, 等. 2004. 祁连山中部过去近千年温度变化的树轮记录. 中国科学:地球科学,34(1):89-95.
(Liu X H, Qin D H, Shao X M, et al. 2004. The middle section of Qilian mountain temperature variations in the last millennium tree-ring records. Scientia Sinica(Terrae),34(1):89-95.[in Chinese])
刘旭辉, 余新晓, 赵阳. 2013. 北京山区典型小流域景观格局变化对径流的影响. 水土保持研究, 20(5):39-44.
(Liu X H, Yu X X, Zhao Y. 2013. Impact of landscape pattern on runoff in small watershed of Beijing mountain region. Research of Soil and Water Conservation, 20(5):39-44.[in Chinese])
刘禹, 马利民, 蔡秋芳,等. 2002. 采用树轮稳定碳同位素重建贺兰山1890年以来夏季(6~8月)气温. 中国科学:地球科学, 32(8):667-674.
(Liu Y, Ma L M, Cai Q F, et al. 2002. Reconstruct summer (6-8) temperature of Helan Mountain since 1890 using tree-ring stable carbon isotope values. Scientia Sinica(Terrae), 32(8):667-674.[in Chinese])
尚华明, 魏文寿, 袁玉江,等. 2010. 天山北坡东部树轮宽度和稳定碳同位素的环境响应分析. 沙漠与绿洲气象, 4(5):6-10.
(Shang H M, Wei W S, Yuan Y J, et al. 2010. Environmental response of tree-ring width and stable carbon isotope at north slope of eastern Tianshan mountains. Desert and Oasis Meteorology, 4(5):6-10.[in Chinese])
谭方颖, 王建林, 宋迎波. 2010.华北平原近45年气候变化特征分析. 气象, 36(5):40-45.
(Tan F Y, Wang J L, Song Y B. 2010. Characteristics of climate change in the North China Plain for recent 45 years. Meteorological Monthly, 36(5):40-45.[in Chinese])
吴祥定. 1990. 树木年轮与气候变化. 北京:气象出版社.
(Wu X D. 1990. Tree-ring and climatic change. Beijing:China Meteorological Press.[in Chinese])
张瑞波, 尚华明, 魏文寿,等. 2014.树轮δ¹³C记录的阿勒泰地区近160a夏季气温变化. 沙漠与绿洲气象, 8(2):34-40.
(Zhang R B, Shang H M, Wei W S, et al. 2014. Summer temperature history in Altay during the last 160 years recorded by δ¹³C in tree rings. Desert and Oasis Meteorology, 8(2):34-40.[in Chinese])
张瑞波, 尚华明, 袁玉江,等. 2015. 基于树轮δ¹³C的阿尔泰山南坡夏季降水变化分析. 中国沙漠, 35(1):106-112.
(Zhang R B, Shang H M, Yuan Y J, et al. 2015. Summer precipitation variation in the southern slope of the Altay mountains recorded by tree-ring δ¹³C. Journal of Desert Research, 35(1):106-112.[in Chinese])
张瑞波, 袁玉江, 魏文寿,等. 2012. 西伯利亚落叶松树轮稳定碳同位素对气候的响应. 干旱区研究, 29(2):328-334.
(Zhang R B, Yuan Y J, Wei W S, et al. 2012. Response of stable carbon isotope of Larix sibirica Ledeb. tree-rings to climate change. Arid Zone Research, 29(2):328-334.[in Chinese])
赵兴云, 成瑞琴. 2009. 树轮稳定碳同位素研究进展与未来趋势. 临沂师范学院学报, 31(6):107-114.
(Zhao X Y, Cheng R Q. 2009. Progress and prospect of stable carbon isotopes in tree-rings. Journal of Linyi Normal University, 31(6):107-114.[in Chinese])
朱丽, 秦富仓, 姚云峰. 2010. 北京市红门川流域径流对防护林结构变化的响应. 水土保持通报, 30(4):63-67.
(Zhu L, Qin F C, Yao Y F. 2010. Response of runoff to changes of shelter forest structure in Hongmenchuan basin of Beijing city. Bulletin of Soil and Water Conservation, 30(4):63-67.[in Chinese])
Fritts H C. 1976.Tree rings and climate. Scientific American, 226(5):95-99.
Mann H B. 1945. Non-parametric test against trend. Econometrika, 13(3):245-259.
McCarroll D, Loader N J. 2004. Stable isotopes in tree rings. Quaternary Science Reviews, 23(7):771-801.
Robertson I, Loader N J, Mccarroll D, et al. 2004. δ¹³C of tree-ring lignin as an indirect measure of climate change. Water Air & Soil Pollution Focus, 4(2):531-544.
Shi Y, Shen Y, Kang E, et al. 2007. Recent and future climate change in northwest China. Climatic change, 80(3/4):379-393.
Sidorova O V, Siegwolf R T W, Myglan V S, et al. 2013. The application of tree-rings and stable isotopes for reconstructions of climate conditions in the Russian Altai. Climatic Change, 120(1/2):153-167.
Stuiver M, Burk R L, Quay P D. 1984. ¹³C/¹²C ratios in tree rings and the transfer of biospheric carbon to the atmosphere. Journal of Geophysical Research Atmospheres, 891(D7):11731-11748.

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密云山区油松树轮δ¹³C对气温和降水量变化的响应

Response of Stable Carbon Isotope of Tree-Ring to Temperature and Precipitation Changes in Pinus tabulaeformis in Miyun Mountain Area

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