Potential for Timberline Advance in Northern Finland, as Revealed by Monitoring during 1983–99

ABSTRACT. Seedling density, tree density and basal area of Scots pine (Pinus sylvestris L.) and Norway spruce (Picea abies (L.) Karst) were monitored and compared in the timberline areas of northern Finland during the period 1983–99. Rows of 9–12 circular plots were established at 13 localities in f...

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Main Authors: V. Juntunen, S. Neuvonen, Y. Norokorpi, T. Tasanen
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2002
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.597.5342
http://pubs.aina.ucalgary.ca/arctic/Arctic55-4-348.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.597.5342 2023-05-15T14:19:35+02:00 Potential for Timberline Advance in Northern Finland, as Revealed by Monitoring during 1983–99 V. Juntunen S. Neuvonen Y. Norokorpi T. Tasanen The Pennsylvania State University CiteSeerX Archives 2002 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.597.5342 http://pubs.aina.ucalgary.ca/arctic/Arctic55-4-348.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.597.5342 http://pubs.aina.ucalgary.ca/arctic/Arctic55-4-348.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://pubs.aina.ucalgary.ca/arctic/Arctic55-4-348.pdf Key words climate change climatic variation regeneration Pinus sylvestris Picea abies seedling density tree density text 2002 ftciteseerx 2016-01-08T13:48:17Z ABSTRACT. Seedling density, tree density and basal area of Scots pine (Pinus sylvestris L.) and Norway spruce (Picea abies (L.) Karst) were monitored and compared in the timberline areas of northern Finland during the period 1983–99. Rows of 9–12 circular plots were established at 13 localities in four regions: pine-dominated northern and southern regions and spruce-dominated western and eastern regions. Temporal changes were monitored in three altitudinal zones: in the forest, at the coniferous timberline (where forest canopy closure ceases), and at the tree line (where coniferous trees higher than 2 m cease). Pine seedling densities decreased abruptly in the southern region, especially at the timberline, but increased slightly in the northern region. The zone · region · change interaction was significant. The change in spruce seedling densities was small in the forest and timberline zones, but the densities more than doubled at the tree line. Tree density and basal area increased in all the zones and regions. New regeneration and tree establishment during the study period indicate a potential for the tree line to advance. However, there was great heterogeneity in regeneration and seedling establishment among the localities. Text Arctic Northern Finland Unknown Norway
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
topic Key words
climate change
climatic variation
regeneration
Pinus sylvestris
Picea abies
seedling density
tree density
spellingShingle Key words
climate change
climatic variation
regeneration
Pinus sylvestris
Picea abies
seedling density
tree density
V. Juntunen
S. Neuvonen
Y. Norokorpi
T. Tasanen
Potential for Timberline Advance in Northern Finland, as Revealed by Monitoring during 1983–99
topic_facet Key words
climate change
climatic variation
regeneration
Pinus sylvestris
Picea abies
seedling density
tree density
description ABSTRACT. Seedling density, tree density and basal area of Scots pine (Pinus sylvestris L.) and Norway spruce (Picea abies (L.) Karst) were monitored and compared in the timberline areas of northern Finland during the period 1983–99. Rows of 9–12 circular plots were established at 13 localities in four regions: pine-dominated northern and southern regions and spruce-dominated western and eastern regions. Temporal changes were monitored in three altitudinal zones: in the forest, at the coniferous timberline (where forest canopy closure ceases), and at the tree line (where coniferous trees higher than 2 m cease). Pine seedling densities decreased abruptly in the southern region, especially at the timberline, but increased slightly in the northern region. The zone · region · change interaction was significant. The change in spruce seedling densities was small in the forest and timberline zones, but the densities more than doubled at the tree line. Tree density and basal area increased in all the zones and regions. New regeneration and tree establishment during the study period indicate a potential for the tree line to advance. However, there was great heterogeneity in regeneration and seedling establishment among the localities.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author V. Juntunen
S. Neuvonen
Y. Norokorpi
T. Tasanen
author_facet V. Juntunen
S. Neuvonen
Y. Norokorpi
T. Tasanen
author_sort V. Juntunen
title Potential for Timberline Advance in Northern Finland, as Revealed by Monitoring during 1983–99
title_short Potential for Timberline Advance in Northern Finland, as Revealed by Monitoring during 1983–99
title_full Potential for Timberline Advance in Northern Finland, as Revealed by Monitoring during 1983–99
title_fullStr Potential for Timberline Advance in Northern Finland, as Revealed by Monitoring during 1983–99
title_full_unstemmed Potential for Timberline Advance in Northern Finland, as Revealed by Monitoring during 1983–99
title_sort potential for timberline advance in northern finland, as revealed by monitoring during 1983–99
publishDate 2002
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.597.5342
http://pubs.aina.ucalgary.ca/arctic/Arctic55-4-348.pdf
geographic Norway
geographic_facet Norway
genre Arctic
Northern Finland
genre_facet Arctic
Northern Finland
op_source http://pubs.aina.ucalgary.ca/arctic/Arctic55-4-348.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.597.5342
http://pubs.aina.ucalgary.ca/arctic/Arctic55-4-348.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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