Shallow soil moisture – ground thaw interactions and controls – Part 1: Spatiotemporal patterns and correlations over a subarctic landscape
Soil moisture and ground thaw state are both indicative of a hillslope's ability to transfer water. In cold regions, in particular, it is widely known that the depth of the active layer and wetness of surface soils are important for runoff generation, but the diversity of interactions between g...
Published in: | Hydrology and Earth System Sciences |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Copernicus Publications
2010
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Subjects: | |
Online Access: | https://doi.org/10.5194/hess-14-1375-2010 https://doaj.org/article/47f2d74530dd403fb41f03810d6ebb32 |