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

Author:

Briffa Keith R1,Shishov Vladimir V23,Melvin Thomas M1,Vaganov Eugene A4,Grudd Håken5,Hantemirov Rashit M6,Eronen Matti7,Naurzbaev Muktar M2

Affiliation:

1. Climatic Research Unit, School of Environmental Sciences, University of East AngliaNorwich NR4 7TJ, UK

2. Dendroecology Department, Sukachev Institute of Forest, Siberian Branch of Russian Academy of SciencesAkademgorodok Street, Krasnoyarsk 660036, Russia

3. IT and Mathematical Modelling Department, Krasnoyarsk State Trade-Economical InstituteL. Prushinskoi Street, Krasnoyarsk 660075, Russia

4. Siberian Federal University79 Svobodnji Avenue, Krasnoyarsk 660041, Russia

5. Department of Physical Geography and Quaternary Geology, Stockholm UniversityStockholm 10691, Sweden

6. Laboratory of Dendrochronology, Institute of Plant and Animal Ecology, Ural Branch of Russian Academy of Sciences8 Marta Street, Ekaterinburg 620144, Russia

7. Department of Geology, University of HelsinkiHelsinki 00014, Finland

Abstract

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.

Publisher

The Royal Society

Subject

General Agricultural and Biological Sciences,General Biochemistry, Genetics and Molecular Biology

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