Dendroclimatology in Fennoscandia – from past accomplishments to future potential
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 r...
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ftslunivuppsala:oai:pub.epsilon.slu.se:4591 2023-05-15T16:11:27+02:00 Dendroclimatology in Fennoscandia – from past accomplishments to future potential Linderholm , Hans W. Björklund , JA Seftigen, Kristina Gunnarson, Björn E. Grudd, Håkan Jeong, JH Drobyshev, Igor Liu, Y 2010 application/pdf https://pub.epsilon.slu.se/4591/ https://pub.epsilon.slu.se/4591/1/Linderholm_et_al_2010.pdf http://www.clim-past.net/6/93/2010/ swe eng swe eng https://pub.epsilon.slu.se/4591/1/Linderholm_et_al_2010.pdf Linderholm , Hans W. and Björklund , JA and Seftigen, Kristina and Gunnarson, Björn E. and Grudd, Håkan and Jeong, JH and Drobyshev, Igor and Liu, Y (2010). Dendroclimatology in Fennoscandia – from past accomplishments to future potential. Climate of the past. 6 , 93-114 [Research article] Wood fibre and forest products Research article PeerReviewed info:eu-repo/semantics/article 2010 ftslunivuppsala 2022-01-09T19:11:35Z 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. Article in Journal/Newspaper Fennoscandia Lapland Swedish University of Agricultural Sciences (SLU): Epsilon Open Archive Norway Torneträsk ENVELOPE(18.861,18.861,68.392,68.392) |
institution |
Open Polar |
collection |
Swedish University of Agricultural Sciences (SLU): Epsilon Open Archive |
op_collection_id |
ftslunivuppsala |
language |
Swedish English |
topic |
Wood fibre and forest products |
spellingShingle |
Wood fibre and forest products Linderholm , Hans W. Björklund , JA Seftigen, Kristina Gunnarson, Björn E. Grudd, Håkan Jeong, JH Drobyshev, Igor Liu, Y Dendroclimatology in Fennoscandia – from past accomplishments to future potential |
topic_facet |
Wood fibre and forest products |
description |
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. |
format |
Article in Journal/Newspaper |
author |
Linderholm , Hans W. Björklund , JA Seftigen, Kristina Gunnarson, Björn E. Grudd, Håkan Jeong, JH Drobyshev, Igor Liu, Y |
author_facet |
Linderholm , Hans W. Björklund , JA Seftigen, Kristina Gunnarson, Björn E. Grudd, Håkan Jeong, JH Drobyshev, Igor Liu, Y |
author_sort |
Linderholm , Hans W. |
title |
Dendroclimatology in Fennoscandia – from past accomplishments to future potential |
title_short |
Dendroclimatology in Fennoscandia – from past accomplishments to future potential |
title_full |
Dendroclimatology in Fennoscandia – from past accomplishments to future potential |
title_fullStr |
Dendroclimatology in Fennoscandia – from past accomplishments to future potential |
title_full_unstemmed |
Dendroclimatology in Fennoscandia – from past accomplishments to future potential |
title_sort |
dendroclimatology in fennoscandia – from past accomplishments to future potential |
publishDate |
2010 |
url |
https://pub.epsilon.slu.se/4591/ https://pub.epsilon.slu.se/4591/1/Linderholm_et_al_2010.pdf http://www.clim-past.net/6/93/2010/ |
long_lat |
ENVELOPE(18.861,18.861,68.392,68.392) |
geographic |
Norway Torneträsk |
geographic_facet |
Norway Torneträsk |
genre |
Fennoscandia Lapland |
genre_facet |
Fennoscandia Lapland |
op_relation |
https://pub.epsilon.slu.se/4591/1/Linderholm_et_al_2010.pdf Linderholm , Hans W. and Björklund , JA and Seftigen, Kristina and Gunnarson, Björn E. and Grudd, Håkan and Jeong, JH and Drobyshev, Igor and Liu, Y (2010). Dendroclimatology in Fennoscandia – from past accomplishments to future potential. Climate of the past. 6 , 93-114 [Research article] |
_version_ |
1765996588097863680 |