Thaw processes in ice-rich permafrost landscapes represented with laterally coupled tiles in a land surface model

<p>Earth system models (ESMs) are our primary tool for projecting future climate change, but their ability to represent small-scale land surface processes is currently limited. This is especially true for permafrost landscapes in which melting of excess ground ice and subsequent subsidence aff...

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Bibliographic Details
Main Authors: K. S. Aas, L. Martin, J. Nitzbon, M. Langer, J. Boike, H. Lee, T. K. Berntsen, S. Westermann
Format: Article
Language:English
Published: Copernicus Publications 2019-02-01
Series:The Cryosphere
Online Access:https://www.the-cryosphere.net/13/591/2019/tc-13-591-2019.pdf

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