Incorporation of a two-direction freeze-thaw algorithm into a spatially-distributed hydrologic model

In the arctic environment, the active layer (the thin layer of the soil above the permafrost, which annually thaws and freezes) is the zone where most hydrologic, biologic, ecologic, and geomorphic processes occur. The active layer is a dynamic region where soil properties (both hydraulic and therma...

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Bibliographic Details
Main Authors: Bolton, W. R., Boike, Julia
Format: Conference Object
Language:unknown
Published: 2007
Subjects:
Ice
Online Access:https://epic.awi.de/id/eprint/16751/
https://hdl.handle.net/10013/epic.26594