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Palmer, M.J., Burn, C.R., Kokelj, S.V. (2012) Factors influencing permafrost temperatures across tree line in the uplands east of the Mackenzie Delta, 2004–20101This article is one of a series of papers published in this CJES Special Issue on the theme of Fundamental and applied research on permafrost in Canada.2Polar Continental Shelf Contribution 03611. Canadian Journal of Earth Sciences, 49 (8) 877-894 doi:10.1139/e2012-002

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Reference TypeJournal (article/letter/editorial)
TitleFactors influencing permafrost temperatures across tree line in the uplands east of the Mackenzie Delta, 2004–20101This article is one of a series of papers published in this CJES Special Issue on the theme of Fundamental and applied research on permafrost in Canada.2Polar Continental Shelf Contribution 03611.
JournalCanadian Journal of Earth Sciences
AuthorsPalmer, M.J.Author
Burn, C.R.Author
Kokelj, S.V.Author
Year2012 (August)Volume49
Issue8
PublisherCanadian Science Publishing
DOIdoi:10.1139/e2012-002Search in ResearchGate
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Mindat Ref. ID484846Long-form Identifiermindat:1:5:484846:6
GUID0
Full ReferencePalmer, M.J., Burn, C.R., Kokelj, S.V. (2012) Factors influencing permafrost temperatures across tree line in the uplands east of the Mackenzie Delta, 2004–20101This article is one of a series of papers published in this CJES Special Issue on the theme of Fundamental and applied research on permafrost in Canada.2Polar Continental Shelf Contribution 03611. Canadian Journal of Earth Sciences, 49 (8) 877-894 doi:10.1139/e2012-002
Plain TextPalmer, M.J., Burn, C.R., Kokelj, S.V. (2012) Factors influencing permafrost temperatures across tree line in the uplands east of the Mackenzie Delta, 2004–20101This article is one of a series of papers published in this CJES Special Issue on the theme of Fundamental and applied research on permafrost in Canada.2Polar Continental Shelf Contribution 03611. Canadian Journal of Earth Sciences, 49 (8) 877-894 doi:10.1139/e2012-002
In(2012, August) Canadian Journal of Earth Sciences Vol. 49 (8) Canadian Science Publishing
Abstract/Notes Air and near-surface ground temperatures, late-winter snow conditions, and characteristics of the vegetation cover and soil were measured across the forest–tundra transition in the uplands east of the Mackenzie Delta, Northwest Territories, in 2004–2010. Mean late-winter snow depth decreased northward from 73 cm in the subarctic boreal forest near Inuvik to 22 cm in low-shrub tundra. Annual near-surface ground temperatures decreased northward by 0.1–0.3 °C/km near the northern limit of trees, in association with an abrupt change in snow depth. The rate decreased to 0.01–0.06 °C/km in the tundra. The freezing season is twice as long as the thawing season in the region, so measured differences in the regional ground thermal regime were dominated by the contrast in winter surface conditions between forest and tundra.


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