An 810-year history of cold season temperature variability for northern Poland

Scots pine (Pinus sylvestris L.) is awidely used tree species in European dendroclimatology studies due to its common distribution across much of the continent. Almost all studies find radial growth strongly related to summer temperature, a result reflecting site selection at high elevation/latitude environments where trees grow at their ecophysiological limits.Dueto the amount of attention spent on these sites there is a geographical and seasonal bias in temperature reconstructions based upon tree-ring proxies in Europe. To overcome the limited availability of tree-ring data in temperate lowlands, we present a northern Poland ring-width chronology developed from living and historic Scots pine material with a strong common growth signal going back toAD1200. Investigations into climate-growth relationships found year-to-year ring-width variability to be more strongly correlated to cold season temperature (November toApril) prior to the growing season thansummertemperatures during tree-ring formation. Basedon this relationship it was possible to reconstruct cold season temperature conditions for the last 810 years. Spatial field correlations with gridded instrumental records indicated that the reconstruction provides relevant cold season temperature information across the land regions bordering the North Atlantic Ocean and Baltic Sea, lowlands and uplands ofwestern andcentral Europe, and the easternand central interiorofRussia. Despite anunsuccessful attempt to find a stationary relationship with the North Atlantic Oscillation, comparisons with several cold season temperature reconstructions confirmed the long-term connection between our reconstructed temperature series for northern Poland and the wider area.

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Main Authors: Balanzategui, D., Knorr, A., Heussner, K. U., Wazny, T., Beck, W., Słowiński, M., Helle, G., Buras, A., Wilmking, M., Van Der Maaten, E., Scharnweber, T., Dorado-Liñán, I., Heinrich, I.
Format: artículo biblioteca
Language:English
Published: John Wiley & Sons 2018
Online Access:http://hdl.handle.net/20.500.12792/744
http://hdl.handle.net/10261/289277
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spelling dig-inia-es-10261-2892772023-02-15T12:58:58Z An 810-year history of cold season temperature variability for northern Poland Balanzategui, D. Knorr, A. Heussner, K. U. Wazny, T. Beck, W. Słowiński, M. Helle, G. Buras, A. Wilmking, M. Van Der Maaten, E. Scharnweber, T. Dorado-Liñán, I. Heinrich, I. Scots pine (Pinus sylvestris L.) is awidely used tree species in European dendroclimatology studies due to its common distribution across much of the continent. Almost all studies find radial growth strongly related to summer temperature, a result reflecting site selection at high elevation/latitude environments where trees grow at their ecophysiological limits.Dueto the amount of attention spent on these sites there is a geographical and seasonal bias in temperature reconstructions based upon tree-ring proxies in Europe. To overcome the limited availability of tree-ring data in temperate lowlands, we present a northern Poland ring-width chronology developed from living and historic Scots pine material with a strong common growth signal going back toAD1200. Investigations into climate-growth relationships found year-to-year ring-width variability to be more strongly correlated to cold season temperature (November toApril) prior to the growing season thansummertemperatures during tree-ring formation. Basedon this relationship it was possible to reconstruct cold season temperature conditions for the last 810 years. Spatial field correlations with gridded instrumental records indicated that the reconstruction provides relevant cold season temperature information across the land regions bordering the North Atlantic Ocean and Baltic Sea, lowlands and uplands ofwestern andcentral Europe, and the easternand central interiorofRussia. Despite anunsuccessful attempt to find a stationary relationship with the North Atlantic Oscillation, comparisons with several cold season temperature reconstructions confirmed the long-term connection between our reconstructed temperature series for northern Poland and the wider area. 2023-02-15T08:44:26Z 2023-02-15T08:44:26Z 2018 artículo Boreas 47(2): 443-453 (2018) 0300-9483 http://hdl.handle.net/20.500.12792/744 http://hdl.handle.net/10261/289277 10.1111/bor.12274 1502-3885 en none John Wiley & Sons
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libraryname Biblioteca del INIA España
language English
description Scots pine (Pinus sylvestris L.) is awidely used tree species in European dendroclimatology studies due to its common distribution across much of the continent. Almost all studies find radial growth strongly related to summer temperature, a result reflecting site selection at high elevation/latitude environments where trees grow at their ecophysiological limits.Dueto the amount of attention spent on these sites there is a geographical and seasonal bias in temperature reconstructions based upon tree-ring proxies in Europe. To overcome the limited availability of tree-ring data in temperate lowlands, we present a northern Poland ring-width chronology developed from living and historic Scots pine material with a strong common growth signal going back toAD1200. Investigations into climate-growth relationships found year-to-year ring-width variability to be more strongly correlated to cold season temperature (November toApril) prior to the growing season thansummertemperatures during tree-ring formation. Basedon this relationship it was possible to reconstruct cold season temperature conditions for the last 810 years. Spatial field correlations with gridded instrumental records indicated that the reconstruction provides relevant cold season temperature information across the land regions bordering the North Atlantic Ocean and Baltic Sea, lowlands and uplands ofwestern andcentral Europe, and the easternand central interiorofRussia. Despite anunsuccessful attempt to find a stationary relationship with the North Atlantic Oscillation, comparisons with several cold season temperature reconstructions confirmed the long-term connection between our reconstructed temperature series for northern Poland and the wider area.
format artículo
author Balanzategui, D.
Knorr, A.
Heussner, K. U.
Wazny, T.
Beck, W.
Słowiński, M.
Helle, G.
Buras, A.
Wilmking, M.
Van Der Maaten, E.
Scharnweber, T.
Dorado-Liñán, I.
Heinrich, I.
spellingShingle Balanzategui, D.
Knorr, A.
Heussner, K. U.
Wazny, T.
Beck, W.
Słowiński, M.
Helle, G.
Buras, A.
Wilmking, M.
Van Der Maaten, E.
Scharnweber, T.
Dorado-Liñán, I.
Heinrich, I.
An 810-year history of cold season temperature variability for northern Poland
author_facet Balanzategui, D.
Knorr, A.
Heussner, K. U.
Wazny, T.
Beck, W.
Słowiński, M.
Helle, G.
Buras, A.
Wilmking, M.
Van Der Maaten, E.
Scharnweber, T.
Dorado-Liñán, I.
Heinrich, I.
author_sort Balanzategui, D.
title An 810-year history of cold season temperature variability for northern Poland
title_short An 810-year history of cold season temperature variability for northern Poland
title_full An 810-year history of cold season temperature variability for northern Poland
title_fullStr An 810-year history of cold season temperature variability for northern Poland
title_full_unstemmed An 810-year history of cold season temperature variability for northern Poland
title_sort 810-year history of cold season temperature variability for northern poland
publisher John Wiley & Sons
publishDate 2018
url http://hdl.handle.net/20.500.12792/744
http://hdl.handle.net/10261/289277
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