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Dendroclimatology in Fennoscandia – from past accomplishments to future potential

Journal article
Authors Hans W. Linderholm
Jesper Björklund
Kristina Seftigen
Björn E Gunnarson
Håkan Grudd
Jee-Hoon Jeong
Igor Drobyshev
Yu Liu
Published in Climate of the Past
Volume 6
Pages 93-114.
ISSN 1814-9324
Publication year 2010
Published at Department of Earth Sciences
Pages 93-114.
Language en
Subject categories Earth and Related Environmental Sciences, Climate Research


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 Tornetr¨ask 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.

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