Changes in thaw lake drainage in the Western Canadian Arctic from 1950 to 2000

Abstract The permafrost of the Western Canadian Arctic has a very high ground ice content. As a result, the vast number of thaw lakes in this area are very sensitive to a changing climate. With thaw lakes prone to either increases in area due to thermokarst processes, or complete drainage in less th...

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Bibliographic Details
Published in:Hydrological Processes
Main Authors: Marsh, Philip, Russell, Mark, Pohl, Stefan, Haywood, Heather, Onclin, Cuyler
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2008
Subjects:
Ice
Online Access:http://dx.doi.org/10.1002/hyp.7179
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fhyp.7179
https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.7179