Articles | Volume 13, issue 3
https://doi.org/10.5194/gmd-13-1663-2020
https://doi.org/10.5194/gmd-13-1663-2020
Model evaluation paper
 | 
31 Mar 2020
Model evaluation paper |  | 31 Mar 2020

Lower boundary conditions in land surface models – effects on the permafrost and the carbon pools: a case study with CLM4.5

Ignacio Hermoso de Mendoza, Hugo Beltrami, Andrew H. MacDougall, and Jean-Claude Mareschal

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Ignacio Hermoso de Mendoza on behalf of the Authors (30 May 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (16 Jul 2019) by Didier Roche
RR by Anonymous Referee #1 (31 Jul 2019)
RR by Anonymous Referee #3 (07 Nov 2019)
ED: Reconsider after major revisions (24 Nov 2019) by Didier Roche
AR by Ignacio Hermoso de Mendoza on behalf of the Authors (05 Jan 2020)  Author's response    Manuscript
ED: Publish as is (25 Feb 2020) by Didier Roche
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Short summary
We study the impact that the thickness of the subsurface and the geothermal gradient have in land models for climate simulations. To do this, we modify the Community Land Model version 4.5. In a scenario of rising atmospheric temperatures, the temperature of an insufficiently deep subsurface rises faster than it would in the real land. For the model, this produces faster permafrost thawing and increased emissions of land carbon to the atmosphere.