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...
Published in: | Hydrological Processes |
---|---|
Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Wiley
2008
|
Subjects: | |
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 |