Trends in recent temperature and radial tree growth spanning 2000 years across northwest Eurasia

被引:119
作者
Briffa, Keith R. [1 ]
Shishov, Vladimir V. [2 ,3 ]
Melvin, Thomas M. [1 ]
Vaganov, Eugene A. [7 ]
Grudd, Haken [4 ]
Hantemirov, Rashit M. [5 ]
Eronen, Matti [6 ]
Naurzbaev, Muktar M. [2 ]
机构
[1] Univ E Anglia, Sch Environm Sci, Climat Res Unit, Norwich NR4 7TJ, Norfolk, England
[2] Russian Acad Sci, Siberian Branch, Sukachev Inst Forest, Dendroecol Dept, Krasnoyarsk 660036, Russia
[3] Krasnoyarsk State Trade Econ Inst, IT & Math Modelling Dept, Krasnoyarsk 660075, Russia
[4] Stockholm Univ, Dept Phys Geog & Quaternary Geol, S-10691 Stockholm, Sweden
[5] Russian Acad Sci, Ural Branch, Inst Plant & Anim Ecol, Lab Dendrochronol, Ekaterinburg 620144, Russia
[6] Univ Helsinki, Dept Geol, FIN-00014 Helsinki, Finland
[7] Siberian Fed Univ, Krasnoyarsk 660041, Russia
基金
英国自然环境研究理事会;
关键词
climate change; Eurasia; tree-ring chronology; temperature;
D O I
10.1098/rstb.2007.2199
中图分类号
Q [生物科学];
学科分类号
07 ; 0710 ; 09 ;
摘要
This paper describes variability in trends of annual tree growth at several locations in the high latitudes of Eurasia, providing a wide regional comparison over a 2000-year period. The study focuses on the nature of local and widespread tree-growth responses to recent warming seen in instrumental observations, available in northern regions for periods ranging from decades to a century. Instrumental temperature data demonstrate differences in seasonal scale of Eurasian warming and the complexity and spatial diversity of tree-growing-season trends in recent decades. A set of long tree-ring chronologies provides empirical evidence of association between inter-annual tree growth and local, primarily summer, temperature variability at each location. These data show no evidence of a recent breakdown in this association as has been found at other high-latitude Northern Hemisphere locations. Using Kendall's concordance, we quantify the time-dependent relationship between growth trends of the long chronologies as a group. This provides strong evidence that the extent of recent widespread warming across northwest Eurasia, with respect to 100- to 200-year trends, is unprecedented in the last 2000 years. An equivalent analysis of simulated temperatures using the HadCM3 model fails to show a similar increase in concordance expected as a consequence of anthropogenic forcing.
引用
收藏
页码:2271 / 2284
页数:14
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