Dendroclimatology in Fennoscandia - from past accomplishments to future potential
(2010) In Climate of the Past 6(1). p.93-114- Abstract
- 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 Tornetrask 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... (More)
- 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 Tornetrask 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. (Less)
Please use this url to cite or link to this publication:
https://lup.lub.lu.se/record/4448869
- author
- Linderholm, HW ; Bjorklund, JA ; Seftigen, K ; Gunnarson, BE ; Grudd, H ; Jeong, JH ; Drobyshev, Igor LU and Liu, Y
- publishing date
- 2010
- type
- Contribution to journal
- publication status
- published
- subject
- in
- Climate of the Past
- volume
- 6
- issue
- 1
- pages
- 93 - 114
- publisher
- Copernicus GmbH
- external identifiers
-
- scopus:77649111726
- ISSN
- 1814-9332
- DOI
- 10.5194/cp-6-93-2010
- language
- English
- LU publication?
- no
- id
- e907beae-860f-4a6c-adb3-c7493180fd5d (old id 4448869)
- date added to LUP
- 2016-04-01 11:05:00
- date last changed
- 2024-10-01 12:08:19
@article{e907beae-860f-4a6c-adb3-c7493180fd5d, abstract = {{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 Tornetrask 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.}}, author = {{Linderholm, HW and Bjorklund, JA and Seftigen, K and Gunnarson, BE and Grudd, H and Jeong, JH and Drobyshev, Igor and Liu, Y}}, issn = {{1814-9332}}, language = {{eng}}, number = {{1}}, pages = {{93--114}}, publisher = {{Copernicus GmbH}}, series = {{Climate of the Past}}, title = {{Dendroclimatology in Fennoscandia - from past accomplishments to future potential}}, url = {{http://dx.doi.org/10.5194/cp-6-93-2010}}, doi = {{10.5194/cp-6-93-2010}}, volume = {{6}}, year = {{2010}}, }