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...
Published in: | Hydrological Processes |
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Main Authors: | , , , |
Other Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Wiley
2014
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Subjects: | |
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 |