Subsurface water flow pathways in the canadian High Arctic
In Arctic regions subsurface flow is often a dominant flow path of water, especially as the thaw depth progresses and the active layer water storage capacity increases. Subsurface flow through the active layer is important for water delivery to streams and can be potentially routed through subsurfac...
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Other Authors: | , |
Format: | Thesis |
Language: | English |
Published: |
2017
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Subjects: | |
Online Access: | http://hdl.handle.net/1974/22777 |