Treeline and timberline dynamics
Polar treeline and timberline Today’s polar treeline runs along the northernmost part of Fennoscandia and further along the northern edge of the Kola Peninsula and the northern Russian mainland. In continental northern Russia the limit of tree growth (>2–3 m growth height) lies only slightly to t...
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ftunivbern:oai:boris.unibe.ch:185297 2023-10-09T21:49:08+02:00 Treeline and timberline dynamics Tinner, Willy Lang, Gerhard Schwörer, Christoph Lang, Gerhard Ammann, Brigitta Behre, Karl-Ernst Tinner, Willy 2023-06 application/pdf https://boris.unibe.ch/185297/1/2023_QuatVegeDynEurope_455.pdf https://boris.unibe.ch/185297/ eng eng Haupt Verlag https://boris.unibe.ch/185297/ info:eu-repo/semantics/restrictedAccess Tinner, Willy; Lang, Gerhard; Schwörer, Christoph (2023). Treeline and timberline dynamics. In: Lang, Gerhard; Ammann, Brigitta; Behre, Karl-Ernst; Tinner, Willy (eds.) Quaternary Vegetation Dynamics of Europe (pp. 455-466). Bern: Haupt Verlag 580 Plants (Botany) info:eu-repo/semantics/bookPart info:eu-repo/semantics/publishedVersion PeerReviewed 2023 ftunivbern 2023-09-10T23:49:36Z Polar treeline and timberline Today’s polar treeline runs along the northernmost part of Fennoscandia and further along the northern edge of the Kola Peninsula and the northern Russian mainland. In continental northern Russia the limit of tree growth (>2–3 m growth height) lies only slightly to the north of the Arctic Circle (66°32’ N) and is formed by Picea abies ssp. obovata, while in oceanic Fennoscandia it goes beyond 71° N and consists of Betula pubescens ssp. tortuosa. South of the polar treeline, dwarf shrub tundra, open birch stands and isolated birch and pine forests form vegetation mosaics. These parklands build the forest tundra and are bordered to the south by closed Pinus sylvestris forests that form the polar timberline (or forest limit) between 69° and 70° N. The polar treeline and timberline represent heat-deficiency limits, whereby, as a rough rule, the minimum for the existence of conifer trees (>2–3 m) is assumed to be 30 days per year with a temperature average above 10°C (e.g. Walter and Breckle, 1986). The global polar treeline has also been associated with growing seasons of 90– 106 days and seasonal mean temperatures between 5.1 and 6.9°C, similar to other treeline positions in the world (6.4 ± 0.7°C; Körner, 2012). Book Part Arctic Fennoscandia kola peninsula Tundra BORIS (Bern Open Repository and Information System, University of Bern) Arctic Kola Peninsula |
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Open Polar |
collection |
BORIS (Bern Open Repository and Information System, University of Bern) |
op_collection_id |
ftunivbern |
language |
English |
topic |
580 Plants (Botany) |
spellingShingle |
580 Plants (Botany) Tinner, Willy Lang, Gerhard Schwörer, Christoph Treeline and timberline dynamics |
topic_facet |
580 Plants (Botany) |
description |
Polar treeline and timberline Today’s polar treeline runs along the northernmost part of Fennoscandia and further along the northern edge of the Kola Peninsula and the northern Russian mainland. In continental northern Russia the limit of tree growth (>2–3 m growth height) lies only slightly to the north of the Arctic Circle (66°32’ N) and is formed by Picea abies ssp. obovata, while in oceanic Fennoscandia it goes beyond 71° N and consists of Betula pubescens ssp. tortuosa. South of the polar treeline, dwarf shrub tundra, open birch stands and isolated birch and pine forests form vegetation mosaics. These parklands build the forest tundra and are bordered to the south by closed Pinus sylvestris forests that form the polar timberline (or forest limit) between 69° and 70° N. The polar treeline and timberline represent heat-deficiency limits, whereby, as a rough rule, the minimum for the existence of conifer trees (>2–3 m) is assumed to be 30 days per year with a temperature average above 10°C (e.g. Walter and Breckle, 1986). The global polar treeline has also been associated with growing seasons of 90– 106 days and seasonal mean temperatures between 5.1 and 6.9°C, similar to other treeline positions in the world (6.4 ± 0.7°C; Körner, 2012). |
author2 |
Lang, Gerhard Ammann, Brigitta Behre, Karl-Ernst Tinner, Willy |
format |
Book Part |
author |
Tinner, Willy Lang, Gerhard Schwörer, Christoph |
author_facet |
Tinner, Willy Lang, Gerhard Schwörer, Christoph |
author_sort |
Tinner, Willy |
title |
Treeline and timberline dynamics |
title_short |
Treeline and timberline dynamics |
title_full |
Treeline and timberline dynamics |
title_fullStr |
Treeline and timberline dynamics |
title_full_unstemmed |
Treeline and timberline dynamics |
title_sort |
treeline and timberline dynamics |
publisher |
Haupt Verlag |
publishDate |
2023 |
url |
https://boris.unibe.ch/185297/1/2023_QuatVegeDynEurope_455.pdf https://boris.unibe.ch/185297/ |
geographic |
Arctic Kola Peninsula |
geographic_facet |
Arctic Kola Peninsula |
genre |
Arctic Fennoscandia kola peninsula Tundra |
genre_facet |
Arctic Fennoscandia kola peninsula Tundra |
op_source |
Tinner, Willy; Lang, Gerhard; Schwörer, Christoph (2023). Treeline and timberline dynamics. In: Lang, Gerhard; Ammann, Brigitta; Behre, Karl-Ernst; Tinner, Willy (eds.) Quaternary Vegetation Dynamics of Europe (pp. 455-466). Bern: Haupt Verlag |
op_relation |
https://boris.unibe.ch/185297/ |
op_rights |
info:eu-repo/semantics/restrictedAccess |
_version_ |
1779312158831542272 |