Changing hydrologic connectivity due to permafrost thaw in the lower Liard River valley, NWT, Canada

Abstract Flows from river basins in northwestern Canada have been rising in the last two decades as a result of climate warming. In the wetland‐dominated basins that characterise the southern margin of permafrost, permafrost thaw and disappearance, and resulting land‐cover change, is occurring at an...

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Bibliographic Details
Published in:Hydrological Processes
Main Authors: Connon, Ryan F., Quinton, William L., Craig, James R., Hayashi, Masaki
Other Authors: Canadian Space Agency, Canadian Foundation for Climate and Atmospheric Sciences
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2014
Subjects:
Ice
Online Access:http://dx.doi.org/10.1002/hyp.10206
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fhyp.10206
https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.10206