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Research article - Peer-reviewed, 2010

Dendroclimatology in Fennoscandia – from past accomplishments to future potential

Linderholm HW, Björklund JA, Seftigen K, Gunnarson BE, Drobyshev Igor, Grudd H, Jeong J-H, Stridbeck P, Liu Y


Fennoscandia has a strong tradition in dendrochronology, and its large tracts of boreal forest make the region well suited for the development of tree-ring chronologies that extend back several thousands of years. Two of the world's longest continuous (most tree-ring chronologies are annually resolved) tree-ring width chronologies are found in northern Fennoscandia, with records from Torneträsk and Finnish Lapland covering the last ca. 7500 yr. In addition, several chronologies between coastal Norway and the interior of Finland extend back several centuries. Tree-ring data from Fennoscandia have provided important information on regional climate variability during the mid to late Holocene and have played major roles in the reconstruction of hemispheric and global temperatures. Tree-ring data from the region have also been used to reconstruct large-scale atmospheric circulation patterns, regional precipitation and drought. Such information is imperative when trying to reach better understanding of natural climate change and variability and its forcing mechanisms, and placing recent climate change within a long-term context


dendrochronology; climate; climatic variation; reconstructions

Published in

Climate of the Past
2010, volume: 6, number: 1, pages: 93-114

Authors' information

Linderholm, Hans W.
Björklund, Jesper A.
Seftigen, Kristina
Gunnarson, Björn
Swedish University of Agricultural Sciences, Department of Forest Ecology and Management
Gunnarson, Björn
Stockholm University
Grudd, Håkan
Jeong, Jee-Hoon
University of Gothenburg
Swedish University of Agricultural Sciences, Southern Swedish Forest Research Centre
Liu, Yimin
Chinese Academy of Sciences

UKÄ Subject classification

Environmental Sciences related to Agriculture and Land-use
Forest Science

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