The thermal regime of permafrost and its susceptibility to degradation in upland terrain near Inuvik, N.W.T
Mean near-surface ground temperatures in upland terrain near Inuvik range between -4°C and -1.2°C and the thickness of permafrost is about 90m. The warm permafrost is due to the relatively deep snow cover that accumulates in the open-canopy forest. Changes in surface conditions may lead to permafros...
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Language: | English |
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Online Access: | https://ir.library.carleton.ca/pub/4509 https://doi.org/10.1002/ppp.649 |
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ftcarletonunivir:oai:carleton.ca:4509 2023-05-15T16:55:42+02:00 The thermal regime of permafrost and its susceptibility to degradation in upland terrain near Inuvik, N.W.T Burn, C. (Christopher R.) Mackay, J.R. Kokelj, S.V. 2009-04-01 https://ir.library.carleton.ca/pub/4509 https://doi.org/10.1002/ppp.649 en eng https://ir.library.carleton.ca/pub/4509 doi:10.1002/ppp.649 Permafrost and Periglacial Processes vol. 20 no. 2, pp. 221-227 Mean annual ground temperature Permafrost Snow cover info:eu-repo/semantics/article 2009 ftcarletonunivir https://doi.org/10.1002/ppp.649 2022-02-06T21:51:53Z Mean near-surface ground temperatures in upland terrain near Inuvik range between -4°C and -1.2°C and the thickness of permafrost is about 90m. The warm permafrost is due to the relatively deep snow cover that accumulates in the open-canopy forest. Changes in surface conditions may lead to permafrost degradation in this environment, as is evident from elevated ground temperatures beneath disturbed surfaces in a gravel pit, in terrain burned by forest fire and where the snow depth has been increased by fencing. The values for mean annual ground temperature near Inuvik are lower end-members of the distribution of ground temperatures in the boreal forests of northwest Canada. The range in the mean temperature of near-surface permafrost throughout this 1200-km wide belt (from 0°C to about -4°C) is comparable to the range over 100km northwards from Inuvik across the treeline (from about -4°C to -8°C). Article in Journal/Newspaper Inuvik permafrost Permafrost and Periglacial Processes Carleton University's Institutional Repository Canada Inuvik ENVELOPE(-133.610,-133.610,68.341,68.341) Permafrost and Periglacial Processes 20 2 221 227 |
institution |
Open Polar |
collection |
Carleton University's Institutional Repository |
op_collection_id |
ftcarletonunivir |
language |
English |
topic |
Mean annual ground temperature Permafrost Snow cover |
spellingShingle |
Mean annual ground temperature Permafrost Snow cover Burn, C. (Christopher R.) Mackay, J.R. Kokelj, S.V. The thermal regime of permafrost and its susceptibility to degradation in upland terrain near Inuvik, N.W.T |
topic_facet |
Mean annual ground temperature Permafrost Snow cover |
description |
Mean near-surface ground temperatures in upland terrain near Inuvik range between -4°C and -1.2°C and the thickness of permafrost is about 90m. The warm permafrost is due to the relatively deep snow cover that accumulates in the open-canopy forest. Changes in surface conditions may lead to permafrost degradation in this environment, as is evident from elevated ground temperatures beneath disturbed surfaces in a gravel pit, in terrain burned by forest fire and where the snow depth has been increased by fencing. The values for mean annual ground temperature near Inuvik are lower end-members of the distribution of ground temperatures in the boreal forests of northwest Canada. The range in the mean temperature of near-surface permafrost throughout this 1200-km wide belt (from 0°C to about -4°C) is comparable to the range over 100km northwards from Inuvik across the treeline (from about -4°C to -8°C). |
format |
Article in Journal/Newspaper |
author |
Burn, C. (Christopher R.) Mackay, J.R. Kokelj, S.V. |
author_facet |
Burn, C. (Christopher R.) Mackay, J.R. Kokelj, S.V. |
author_sort |
Burn, C. (Christopher R.) |
title |
The thermal regime of permafrost and its susceptibility to degradation in upland terrain near Inuvik, N.W.T |
title_short |
The thermal regime of permafrost and its susceptibility to degradation in upland terrain near Inuvik, N.W.T |
title_full |
The thermal regime of permafrost and its susceptibility to degradation in upland terrain near Inuvik, N.W.T |
title_fullStr |
The thermal regime of permafrost and its susceptibility to degradation in upland terrain near Inuvik, N.W.T |
title_full_unstemmed |
The thermal regime of permafrost and its susceptibility to degradation in upland terrain near Inuvik, N.W.T |
title_sort |
thermal regime of permafrost and its susceptibility to degradation in upland terrain near inuvik, n.w.t |
publishDate |
2009 |
url |
https://ir.library.carleton.ca/pub/4509 https://doi.org/10.1002/ppp.649 |
long_lat |
ENVELOPE(-133.610,-133.610,68.341,68.341) |
geographic |
Canada Inuvik |
geographic_facet |
Canada Inuvik |
genre |
Inuvik permafrost Permafrost and Periglacial Processes |
genre_facet |
Inuvik permafrost Permafrost and Periglacial Processes |
op_source |
Permafrost and Periglacial Processes vol. 20 no. 2, pp. 221-227 |
op_relation |
https://ir.library.carleton.ca/pub/4509 doi:10.1002/ppp.649 |
op_doi |
https://doi.org/10.1002/ppp.649 |
container_title |
Permafrost and Periglacial Processes |
container_volume |
20 |
container_issue |
2 |
container_start_page |
221 |
op_container_end_page |
227 |
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1766046756363042816 |