Abstract
The objective of this study is to investigate heat and water transfer processes over the permafrost region. For this analysis, we develop a 1-D energy and water transfer model which can consider permafrost hydrogical processes, and apply it to the permafrost region on the Tibetan Plateau. The result of analysis indicates that the model which is developed in this study can represent heat and water transfer and the active layer depth accurately. By using this model, the impacts of climate change on the permafrost hydrological processes are demonstrated.
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