ARCTIC The High Subarctic Forest-Tundra of Northwestern Canada: Position, Width, and Vegetation Gradients in Relation to Climate
ABSTRACT. A phytogeoclimatic study of the high subarctic region of Canada between Hudson Bay and the Cordillera at the northern Yukon-Mackenzie border was undertaken to provide a verifiable and quantitative synthesis of forest-tundra vegetation ecology. Three field seasons of vegetation and terrain...
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Language: | English |
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1991
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.584.9213 http://pubs.aina.ucalgary.ca/arctic/Arctic45-1-1.pdf |
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author2 | The Pennsylvania State University CiteSeerX Archives |
collection | Unknown |
description | ABSTRACT. A phytogeoclimatic study of the high subarctic region of Canada between Hudson Bay and the Cordillera at the northern Yukon-Mackenzie border was undertaken to provide a verifiable and quantitative synthesis of forest-tundra vegetation ecology. Three field seasons of vegetation and terrain studies provided ground truth for a grid of 1314 black-and-white air photos that cover Ca. 24 % of the forest-tundra and adja-cent low Subarctic and low Arctic. Air photos were analyzed for percentage cover of nine vegetation-terrain types, bedrock and parent materials, landforms, and elevations. The forest-tundra, as bounded by the 1 O: l and 1:lOOO tree:upland tundra cover isolines, spans an average 145 f 72 km (median 131 km) and increases in width from northwest to southeast. The transition from 101 to 1: lO treexpland tundra cover occupies one-fourth to one-half the area of the forest-tundra. Regional slope of the land probably accounts for much of the variation in width of the forest-tundra. Southern outliers of forest-tundra in the northwest are found mainly in areas of high elevation. Across much of the northwest, steep vegetation gradi-ents occur near the northern limit of trees. North of Great Slave Lake, steep vegetation gradients shift from the northern to the southern half of the forest-tundra and maintain this position eastward to Hudson Bay. The forest-tundra of the northwest receives roughly three-fourths the mean annual net radiation available to the southeast and central districts. Key words: air photos, boreal, climate, ecology, forest-tundra, high Subarctic, Northwest Territories, plant geography, tree line, vegetation RÉSUMÉ. On a entrepris une étude phytogéoclimatique de la zone de l’Extrême-Subarctique canadien comprise entre la baie d’Hudson et la cordil-lère, située à la frontière du Yukon-Mackenzie, en vue d’offrir une synthkse vérifiable et quantitative de l’écologie végétale de la forêt-toundra. Trois |
format | Text |
genre | Arctic Arctic Great Slave Lake Hudson Bay Northwest Territories Subarctic subarctique* toundra Tundra Yukon |
genre_facet | Arctic Arctic Great Slave Lake Hudson Bay Northwest Territories Subarctic subarctique* toundra Tundra Yukon |
geographic | Arctic Yukon Northwest Territories Hudson Bay Canada Hudson Great Slave Lake |
geographic_facet | Arctic Yukon Northwest Territories Hudson Bay Canada Hudson Great Slave Lake |
id | ftciteseerx:oai:CiteSeerX.psu:10.1.1.584.9213 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(-114.001,-114.001,61.500,61.500) |
op_collection_id | ftciteseerx |
op_relation | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.584.9213 http://pubs.aina.ucalgary.ca/arctic/Arctic45-1-1.pdf |
op_rights | Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
op_source | http://pubs.aina.ucalgary.ca/arctic/Arctic45-1-1.pdf |
publishDate | 1991 |
record_format | openpolar |
spelling | ftciteseerx:oai:CiteSeerX.psu:10.1.1.584.9213 2025-01-16T19:48:58+00:00 ARCTIC The High Subarctic Forest-Tundra of Northwestern Canada: Position, Width, and Vegetation Gradients in Relation to Climate The Pennsylvania State University CiteSeerX Archives 1991 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.584.9213 http://pubs.aina.ucalgary.ca/arctic/Arctic45-1-1.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.584.9213 http://pubs.aina.ucalgary.ca/arctic/Arctic45-1-1.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://pubs.aina.ucalgary.ca/arctic/Arctic45-1-1.pdf text 1991 ftciteseerx 2016-01-08T13:12:45Z ABSTRACT. A phytogeoclimatic study of the high subarctic region of Canada between Hudson Bay and the Cordillera at the northern Yukon-Mackenzie border was undertaken to provide a verifiable and quantitative synthesis of forest-tundra vegetation ecology. Three field seasons of vegetation and terrain studies provided ground truth for a grid of 1314 black-and-white air photos that cover Ca. 24 % of the forest-tundra and adja-cent low Subarctic and low Arctic. Air photos were analyzed for percentage cover of nine vegetation-terrain types, bedrock and parent materials, landforms, and elevations. The forest-tundra, as bounded by the 1 O: l and 1:lOOO tree:upland tundra cover isolines, spans an average 145 f 72 km (median 131 km) and increases in width from northwest to southeast. The transition from 101 to 1: lO treexpland tundra cover occupies one-fourth to one-half the area of the forest-tundra. Regional slope of the land probably accounts for much of the variation in width of the forest-tundra. Southern outliers of forest-tundra in the northwest are found mainly in areas of high elevation. Across much of the northwest, steep vegetation gradi-ents occur near the northern limit of trees. North of Great Slave Lake, steep vegetation gradients shift from the northern to the southern half of the forest-tundra and maintain this position eastward to Hudson Bay. The forest-tundra of the northwest receives roughly three-fourths the mean annual net radiation available to the southeast and central districts. Key words: air photos, boreal, climate, ecology, forest-tundra, high Subarctic, Northwest Territories, plant geography, tree line, vegetation RÉSUMÉ. On a entrepris une étude phytogéoclimatique de la zone de l’Extrême-Subarctique canadien comprise entre la baie d’Hudson et la cordil-lère, située à la frontière du Yukon-Mackenzie, en vue d’offrir une synthkse vérifiable et quantitative de l’écologie végétale de la forêt-toundra. Trois Text Arctic Arctic Great Slave Lake Hudson Bay Northwest Territories Subarctic subarctique* toundra Tundra Yukon Unknown Arctic Yukon Northwest Territories Hudson Bay Canada Hudson Great Slave Lake ENVELOPE(-114.001,-114.001,61.500,61.500) |
spellingShingle | ARCTIC The High Subarctic Forest-Tundra of Northwestern Canada: Position, Width, and Vegetation Gradients in Relation to Climate |
title | ARCTIC The High Subarctic Forest-Tundra of Northwestern Canada: Position, Width, and Vegetation Gradients in Relation to Climate |
title_full | ARCTIC The High Subarctic Forest-Tundra of Northwestern Canada: Position, Width, and Vegetation Gradients in Relation to Climate |
title_fullStr | ARCTIC The High Subarctic Forest-Tundra of Northwestern Canada: Position, Width, and Vegetation Gradients in Relation to Climate |
title_full_unstemmed | ARCTIC The High Subarctic Forest-Tundra of Northwestern Canada: Position, Width, and Vegetation Gradients in Relation to Climate |
title_short | ARCTIC The High Subarctic Forest-Tundra of Northwestern Canada: Position, Width, and Vegetation Gradients in Relation to Climate |
title_sort | arctic the high subarctic forest-tundra of northwestern canada: position, width, and vegetation gradients in relation to climate |
url | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.584.9213 http://pubs.aina.ucalgary.ca/arctic/Arctic45-1-1.pdf |