Articles | Volume 10, issue 1
https://doi.org/10.5194/tc-10-465-2016
https://doi.org/10.5194/tc-10-465-2016
Research article
 | 
01 Mar 2016
Research article |  | 01 Mar 2016

The importance of a surface organic layer in simulating permafrost thermal and carbon dynamics

Elchin Jafarov and Kevin Schaefer

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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 Elchin Jafarov on behalf of the Authors (26 Sep 2015)  Manuscript 
ED: Referee Nomination & Report Request started (05 Oct 2015) by Julia Boike
RR by Anonymous Referee #1 (23 Oct 2015)
ED: Reconsider after major revisions (27 Oct 2015) by Julia Boike
AR by Elchin Jafarov on behalf of the Authors (22 Dec 2015)
ED: Publish subject to minor revisions (Editor review) (20 Jan 2016) by Julia Boike
AR by Elchin Jafarov on behalf of the Authors (03 Feb 2016)
ED: Publish as is (10 Feb 2016) by Julia Boike
AR by Elchin Jafarov on behalf of the Authors (15 Feb 2016)
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Short summary
To improve the uncertainty in modeling of the permafrost carbon emission associated with the predicted climate warming, it is important to improve the simulation of the current permafrost carbon stock. This work shows how simulation of the frozen carbon in land system models can be improved by better addressing the coupling between plant photosynthesis, soil biogeochemistry, and soil thermodynamics.