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Quantitative temperature reconstruction based on growth rate of annually-layered stalagmite: a case study from central China
Tan, LC (Tan, Liangcheng)[ 1 ]; Yi, L (Yi, Liang)[ 2 ]; Cai, YJ (Cai, Yanjun)[ 1 ]; Shen, CC (Shen, Chuan-Chou)[ 3 ]; Cheng, H (Cheng, Hai)[ 4,5 ]; An, ZS (An, Zhisheng)[ 1 ]
2013-07-15
发表期刊QUATERNARY SCIENCE REVIEWS
卷号72页码:137-145
文章类型期刊论文
摘要

We used the annual growth rate of a stalagmite (XL21) collected from Xianglong Cave, central China, to quantitatively reconstruct regional terrestrial temperature changes over the last 95 years (1912-2006 AD). Based on a significant positive correlation between the growth rate and the observed temperature, a transfer function was designed, and the temperature from the previous September to May (P-9-5) was reconstructed, with an explained variance of 43.5%. Our results show an increasing trend in temperature during the last century, and especially over the last 30 years. The temperature variability from central China recorded here bears a striking similarity to that in the Northern Hemisphere, and also to global trends. However, the cooling between the 1980s and the early 1990s seen in the stalagmite record, which interrupted the warming trend that began in the 1960s, is not observed in the mean conditions found in China, the Northern Hemisphere, neither globally. This methodology for reconstructing historical temperature from stalagmite growth rates overcomes the limitation of the short meteorological observation period and supports the potential of stalagmite lamina climatology.

关键词Stalagmite Annual Layer Growth Rate Temperature Modern Process Central China
DOI10.1016/j.quascirev.2013.04.022
收录类别SCI ; EI
语种英语
引用统计
被引频次:15[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.ieecas.cn/handle/361006/9993
专题现代环境研究室
通讯作者Tan, LC (Tan, Liangcheng)[ 1 ]
作者单位1.State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710075, China;
2.State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China;
3.High-precision Mass Spectrometry and Environment Change Laboratory (HISPEC), Department of Geosciences, National Taiwan University,Taipei 106, Taiwan;
4.Institute of Global Environmental Change, Xi’an Jiaotong University, Xi’an 710049, China;
5.Department of Earth Sciences, University of Minnesota, Minneapolis 55455, USA
推荐引用方式
GB/T 7714
Tan, LC ,Yi, L ,Cai, YJ ,et al. Quantitative temperature reconstruction based on growth rate of annually-layered stalagmite: a case study from central China[J]. QUATERNARY SCIENCE REVIEWS,2013,72:137-145.
APA Tan, LC ,Yi, L ,Cai, YJ ,Shen, CC ,Cheng, H ,&An, ZS .(2013).Quantitative temperature reconstruction based on growth rate of annually-layered stalagmite: a case study from central China.QUATERNARY SCIENCE REVIEWS,72,137-145.
MLA Tan, LC ,et al."Quantitative temperature reconstruction based on growth rate of annually-layered stalagmite: a case study from central China".QUATERNARY SCIENCE REVIEWS 72(2013):137-145.
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