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...

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Bibliographic Details
Published in:Hydrology and Earth System Sciences
Main Authors: X. J. Guan, C. J. Westbrook, C. Spence
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2010
Subjects:
T
G
Online Access:https://doi.org/10.5194/hess-14-1375-2010
https://doaj.org/article/47f2d74530dd403fb41f03810d6ebb32