Impact of climate change on radial growth of Siberian spruce and Scots pine in North-western Russia

When adapting forest management practices to a changing environment, it is very important to understand the response of an unmanaged natural forest to climate change. The method used to identify major climatic factors influencing radial growth of Siberian spruce and Scots pine along a latitudinal gr...
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Gespeichert in:

Autor*in:	Lopatin E [verfasserIn] Kolström T [verfasserIn] Spiecker H [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2008

Schlagwörter:	Climate change Growth trends Pinus sylvestris L. Picea obovata Ledeb. Dendrochronology

Übergeordnetes Werk:	In: iForest - Biogeosciences and Forestry - Italian Society of Silviculture and Forest Ecology (SISEF), 2019, 1(2008), 1, Seite 13-21
Übergeordnetes Werk:	volume:1 ; year:2008 ; number:1 ; pages:13-21

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc Journal toc

DOI / URN:	10.3832/ifor0447-0010013

Katalog-ID:	DOAJ015767884

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520			\|a When adapting forest management practices to a changing environment, it is very important to understand the response of an unmanaged natural forest to climate change. The method used to identify major climatic factors influencing radial growth of Siberian spruce and Scots pine along a latitudinal gradient in north-western Russia is dendroclimatic analysis. A clear increasing long-term trend was identified in air temperature and precipitation. During the last 20 years, all meteorological stations experienced temperature increases, and 40 years ago precipitation began to increase. This is shown by the radial increment of Siberian spruce and Scots pine. Therefore, climate change could partly explain the increased forest productivity. The total variance explained by temperature varied from 22% to 41% and precipitation from 19% to 38%. The significant climatic parameters for radial increment in Komi Republic were identified, and the relation between temperature and precipitation in explained variance changes over time for Siberian spruce.
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language	English
source	In iForest - Biogeosciences and Forestry 1(2008), 1, Seite 13-21 volume:1 year:2008 number:1 pages:13-21
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topic_facet	Climate change Growth trends Pinus sylvestris L. Picea obovata Ledeb. Dendrochronology Forestry
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container_title	iForest - Biogeosciences and Forestry
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spellingShingle	Lopatin E misc SD1-669.5 misc Climate change misc Growth trends misc Pinus sylvestris L. misc Picea obovata Ledeb. misc Dendrochronology misc Forestry Impact of climate change on radial growth of Siberian spruce and Scots pine in North-western Russia
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topic_title	SD1-669.5 Impact of climate change on radial growth of Siberian spruce and Scots pine in North-western Russia Climate change Growth trends Pinus sylvestris L. Picea obovata Ledeb Dendrochronology
topic	misc SD1-669.5 misc Climate change misc Growth trends misc Pinus sylvestris L. misc Picea obovata Ledeb. misc Dendrochronology misc Forestry
topic_unstemmed	misc SD1-669.5 misc Climate change misc Growth trends misc Pinus sylvestris L. misc Picea obovata Ledeb. misc Dendrochronology misc Forestry
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title	Impact of climate change on radial growth of Siberian spruce and Scots pine in North-western Russia
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title_sort	impact of climate change on radial growth of siberian spruce and scots pine in north-western russia
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title_auth	Impact of climate change on radial growth of Siberian spruce and Scots pine in North-western Russia
abstract	When adapting forest management practices to a changing environment, it is very important to understand the response of an unmanaged natural forest to climate change. The method used to identify major climatic factors influencing radial growth of Siberian spruce and Scots pine along a latitudinal gradient in north-western Russia is dendroclimatic analysis. A clear increasing long-term trend was identified in air temperature and precipitation. During the last 20 years, all meteorological stations experienced temperature increases, and 40 years ago precipitation began to increase. This is shown by the radial increment of Siberian spruce and Scots pine. Therefore, climate change could partly explain the increased forest productivity. The total variance explained by temperature varied from 22% to 41% and precipitation from 19% to 38%. The significant climatic parameters for radial increment in Komi Republic were identified, and the relation between temperature and precipitation in explained variance changes over time for Siberian spruce.
abstractGer	When adapting forest management practices to a changing environment, it is very important to understand the response of an unmanaged natural forest to climate change. The method used to identify major climatic factors influencing radial growth of Siberian spruce and Scots pine along a latitudinal gradient in north-western Russia is dendroclimatic analysis. A clear increasing long-term trend was identified in air temperature and precipitation. During the last 20 years, all meteorological stations experienced temperature increases, and 40 years ago precipitation began to increase. This is shown by the radial increment of Siberian spruce and Scots pine. Therefore, climate change could partly explain the increased forest productivity. The total variance explained by temperature varied from 22% to 41% and precipitation from 19% to 38%. The significant climatic parameters for radial increment in Komi Republic were identified, and the relation between temperature and precipitation in explained variance changes over time for Siberian spruce.
abstract_unstemmed	When adapting forest management practices to a changing environment, it is very important to understand the response of an unmanaged natural forest to climate change. The method used to identify major climatic factors influencing radial growth of Siberian spruce and Scots pine along a latitudinal gradient in north-western Russia is dendroclimatic analysis. A clear increasing long-term trend was identified in air temperature and precipitation. During the last 20 years, all meteorological stations experienced temperature increases, and 40 years ago precipitation began to increase. This is shown by the radial increment of Siberian spruce and Scots pine. Therefore, climate change could partly explain the increased forest productivity. The total variance explained by temperature varied from 22% to 41% and precipitation from 19% to 38%. The significant climatic parameters for radial increment in Komi Republic were identified, and the relation between temperature and precipitation in explained variance changes over time for Siberian spruce.
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title_short	Impact of climate change on radial growth of Siberian spruce and Scots pine in North-western Russia
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Impact of climate change on radial growth of Siberian spruce and Scots pine in North-western Russia

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Zugang & Verfügbarkeit

Vorhandene Bände

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