Two centuries-long dendroclimatic reconstruction based on Low Arctic Betula pubescens from Tromso Region, Northern Norway

This study presents the results of dendrochronological and dendroclimatological research of Betula pubescens from four sites in northern Norway (Kvaløya Island, Tromsøya Island and Storelva Valley), which provided a 193-year chronology. Our results highlight the importance of the site selection in d...

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Published in:Polish Polar Research
Main Authors: Opała-Owczarek, Magdalena, Migała, Krzysztof, Owczarek, Piotr
Format: Article in Journal/Newspaper
Language:English
Published: 2016
Subjects:
Online Access:https://hdl.handle.net/20.500.12128/496
https://doi.org/10.1515/popore-2016-0024
id ftunivsilesia:oai:rebus.us.edu.pl:20.500.12128/496
record_format openpolar
spelling ftunivsilesia:oai:rebus.us.edu.pl:20.500.12128/496 2024-09-15T18:17:10+00:00 Two centuries-long dendroclimatic reconstruction based on Low Arctic Betula pubescens from Tromso Region, Northern Norway Opała-Owczarek, Magdalena Migała, Krzysztof Owczarek, Piotr 2016 https://hdl.handle.net/20.500.12128/496 https://doi.org/10.1515/popore-2016-0024 en eng Polish Polar Research Polish Polar Research, Vol. 37, iss. 4 (2016), s. 457-476 0138-0338 http://hdl.handle.net/20.500.12128/496 doi:10.1515/popore-2016-0024 Uznanie autorstwa-Użycie niekomercyjne-Bez utworów zależnych 3.0 Polska http://creativecommons.org/licenses/by-nc-nd/3.0/pl/ Arctic Birch Dendroclimatology Temperature reconstruction Tree-ring chronology info:eu-repo/semantics/article 2016 ftunivsilesia https://doi.org/20.500.12128/49610.1515/popore-2016-0024 2024-06-25T03:11:26Z This study presents the results of dendrochronological and dendroclimatological research of Betula pubescens from four sites in northern Norway (Kvaløya Island, Tromsøya Island and Storelva Valley), which provided a 193-year chronology. Our results highlight the importance of the site selection in dendroclimatological studies. We demonstrated that activity of geomorphic processes connected with local topography could led to reduced strength of climatic signal embedded in tree-ring data. Negative pointer years, triggered mainly by unfavourable climatic conditions and insect outbreaks, were common for all site chronologies in 1945, 1955, 1965, 1975, 1986, 2004. However, some site-specific differences were also distinguished. Response function analysis confirmed that June, July and August temperatures were positively correlated with tree-ring widths. This climate-growth relationship was stable throughout the years 1925-2000. From summer temperature reconstruction back to AD 1820, two colder (c. 1835-1850 and 1890-1920) and two warmer (c. 1825-1835 and 1920-1940) periods were identified. The tree-ring record from the Tromsø Region, well correlated between series, sites and climate variables, is an important element of a large-scale reconstruction of pre-instrumental climate variation in the northeastern part of the Atlantic Ocean. Our dendroclimatic reconstruction corresponds well with other climate proxy data, like fluctuations of mountain glaciers in Scandinavia or sea ice extent. Article in Journal/Newspaper Kvaløya Northern Norway Polar Research Sea ice Tromso Tromso Tromsø The Repository of the University of Silesia (RE-BUŚ) Polish Polar Research 37 4 457 476
institution Open Polar
collection The Repository of the University of Silesia (RE-BUŚ)
op_collection_id ftunivsilesia
language English
topic Arctic
Birch
Dendroclimatology
Temperature reconstruction
Tree-ring chronology
spellingShingle Arctic
Birch
Dendroclimatology
Temperature reconstruction
Tree-ring chronology
Opała-Owczarek, Magdalena
Migała, Krzysztof
Owczarek, Piotr
Two centuries-long dendroclimatic reconstruction based on Low Arctic Betula pubescens from Tromso Region, Northern Norway
topic_facet Arctic
Birch
Dendroclimatology
Temperature reconstruction
Tree-ring chronology
description This study presents the results of dendrochronological and dendroclimatological research of Betula pubescens from four sites in northern Norway (Kvaløya Island, Tromsøya Island and Storelva Valley), which provided a 193-year chronology. Our results highlight the importance of the site selection in dendroclimatological studies. We demonstrated that activity of geomorphic processes connected with local topography could led to reduced strength of climatic signal embedded in tree-ring data. Negative pointer years, triggered mainly by unfavourable climatic conditions and insect outbreaks, were common for all site chronologies in 1945, 1955, 1965, 1975, 1986, 2004. However, some site-specific differences were also distinguished. Response function analysis confirmed that June, July and August temperatures were positively correlated with tree-ring widths. This climate-growth relationship was stable throughout the years 1925-2000. From summer temperature reconstruction back to AD 1820, two colder (c. 1835-1850 and 1890-1920) and two warmer (c. 1825-1835 and 1920-1940) periods were identified. The tree-ring record from the Tromsø Region, well correlated between series, sites and climate variables, is an important element of a large-scale reconstruction of pre-instrumental climate variation in the northeastern part of the Atlantic Ocean. Our dendroclimatic reconstruction corresponds well with other climate proxy data, like fluctuations of mountain glaciers in Scandinavia or sea ice extent.
format Article in Journal/Newspaper
author Opała-Owczarek, Magdalena
Migała, Krzysztof
Owczarek, Piotr
author_facet Opała-Owczarek, Magdalena
Migała, Krzysztof
Owczarek, Piotr
author_sort Opała-Owczarek, Magdalena
title Two centuries-long dendroclimatic reconstruction based on Low Arctic Betula pubescens from Tromso Region, Northern Norway
title_short Two centuries-long dendroclimatic reconstruction based on Low Arctic Betula pubescens from Tromso Region, Northern Norway
title_full Two centuries-long dendroclimatic reconstruction based on Low Arctic Betula pubescens from Tromso Region, Northern Norway
title_fullStr Two centuries-long dendroclimatic reconstruction based on Low Arctic Betula pubescens from Tromso Region, Northern Norway
title_full_unstemmed Two centuries-long dendroclimatic reconstruction based on Low Arctic Betula pubescens from Tromso Region, Northern Norway
title_sort two centuries-long dendroclimatic reconstruction based on low arctic betula pubescens from tromso region, northern norway
publishDate 2016
url https://hdl.handle.net/20.500.12128/496
https://doi.org/10.1515/popore-2016-0024
genre Kvaløya
Northern Norway
Polar Research
Sea ice
Tromso
Tromso
Tromsø
genre_facet Kvaløya
Northern Norway
Polar Research
Sea ice
Tromso
Tromso
Tromsø
op_relation Polish Polar Research
Polish Polar Research, Vol. 37, iss. 4 (2016), s. 457-476
0138-0338
http://hdl.handle.net/20.500.12128/496
doi:10.1515/popore-2016-0024
op_rights Uznanie autorstwa-Użycie niekomercyjne-Bez utworów zależnych 3.0 Polska
http://creativecommons.org/licenses/by-nc-nd/3.0/pl/
op_doi https://doi.org/20.500.12128/49610.1515/popore-2016-0024
container_title Polish Polar Research
container_volume 37
container_issue 4
container_start_page 457
op_container_end_page 476
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