Simulating the thermal regime and thaw processes of ice-rich permafrost ground with the land-surface model CryoGrid 3

Thawing of permafrost in a warming climate is governed by a complex interplay of different processes of which only conductive heat transfer is taken into account in most model studies. However, observations in many permafrost landscapes demonstrate that lateral and vertical movement of water can hav...

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Bibliographic Details
Published in:Geoscientific Model Development
Main Authors: Westermann, S., Langer, M., Boike, J., Heikenfeld, M., Peter, M., Etzelmüller, B., Krinner, G.
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2016
Subjects:
Ice
Online Access:https://doi.org/10.5194/gmd-9-523-2016
https://noa.gwlb.de/receive/cop_mods_00014097
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00014053/gmd-9-523-2016.pdf
https://gmd.copernicus.org/articles/9/523/2016/gmd-9-523-2016.pdf