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(Article of periodic en Anglais - 2009)

Document title

The thermal regime of permafrost and its susceptibility to degradation in upland terrain near Inuvik, N.W.T.

published at : Permafrost in the Mackenzie Delta, Canada. Special issue

Authors(s) and Affiliation(s)

BURN C.R. (1) ; MACKAY J.R. (2) ; KOKELJ S.V. (3) ;
(1) Dep. of Geography and Environmental Studies, Carleton Univ., Ottawa, CANADA
(2) Dep. of Geography, Univ. of British Columbia, Vancouver, CANADA
(3) Renewable Resources and Environment, Indian and Northern Affairs, Northwest Territories, Yellowknife, CANADA

Abstract

In this paper, the AA. report permafrost temperatures from south of treeline in the upland, open-canopy, boreal forest near Inuvik. The aims are to : 1) define the thickness and annual thermal regime of permafrost in the Inuvik area; 2) examine the response of ground temperatures to changes in surface conditions, especially snow cover; and 3) discuss the ground temperature at Inuvik in the context of permafrost temperatures in the boreal forest of the Mackenzie River valley and Yukon Territory

Source

Thematical fascicle

published at : Permafrost and periglacial processes / ISSN 1045-6740 / CODEN PEPPED

Editor : Wiley, Chichester - ROYAUME-UNI (1990)

Millesime : 2009, vol. 20, no 2 [pp. 221-227]

Bibliographic references : 18 ref.

Collation : fig., tabl.

Language

Anglais

Digital Object Identifier

Go to electronic document thanks to its DOI : doi:10.1002/ppp.649

Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 2009
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