Articles | Volume 10, issue 2
https://doi.org/10.5194/tc-10-853-2016
https://doi.org/10.5194/tc-10-853-2016
Research article
 | 
18 Apr 2016
Research article |  | 18 Apr 2016

Impacts of snow and organic soils parameterization on northern Eurasian soil temperature profiles simulated by the ISBA land surface model

Bertrand Decharme, Eric Brun, Aaron Boone, Christine Delire, Patrick Le Moigne, and Samuel Morin

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AR by Bertrand Decharme on behalf of the Authors (25 Mar 2016)  Author's response   Manuscript 
ED: Publish subject to technical corrections (29 Mar 2016) by Guillaume Chambon
AR by Bertrand Decharme on behalf of the Authors (30 Mar 2016)  Manuscript 
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Short summary
We analyze how snowpack processes and soil properties impact the soil temperature profiles over northern Eurasian regions using a land surface model. A correct representation of snow compaction is critical in winter while snow albedo is dominant in spring. In summer, soil temperature is more affected by soil organic carbon content, which strongly influences the maximum thaw depth in permafrost regions. This work was done to improve the representation of boreal region processes in climate models.