ORCHIDEE MICT-LEAK (r5459), a global model for the production, transport, and transformation of dissolved organic carbon from Arctic permafrost regions – Part 1: Rationale, model description, and simulation protocol

Bowring, Simon P. K.; Lauerwald, Ronny; Guenet, Bertrand; Zhu, Dan; Guimberteau, Matthieu; Tootchi, Ardalan; Ducharne, Agnès; Ciais, Philippe

doi:https://doi.org/10.5194/gmd-12-3503-2019

Articles | Volume 12, issue 8

https://doi.org/10.5194/gmd-12-3503-2019

© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/gmd-12-3503-2019

© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 12, issue 8

Model evaluation paper

|

12 Aug 2019

Model evaluation paper |

| 12 Aug 2019

ORCHIDEE MICT-LEAK (r5459), a global model for the production, transport, and transformation of dissolved organic carbon from Arctic permafrost regions – Part 1: Rationale, model description, and simulation protocol

Simon P. K. Bowring, Ronny Lauerwald, Bertrand Guenet, Dan Zhu, Matthieu Guimberteau, Ardalan Tootchi, Agnès Ducharne, and Philippe Ciais

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Final revised paper (published on 12 Aug 2019)
Preprint (discussion started on 25 Mar 2019)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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- Supplement

RC1: 'Interesting model application, requires further clarifications', Anonymous Referee #1, 02 May 2019
- AC1: 'Response to Reviewer 1', Simon Bowring, 06 Jun 2019
RC2: 'Referee Comment', Anonymous Referee #2, 15 May 2019
- AC2: 'Response to Reviewer 2', Simon Bowring, 06 Jun 2019

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

AR by Simon Bowring on behalf of the Authors (06 Jun 2019) Author's response Manuscript

ED: Referee Nomination & Report Request started (11 Jun 2019) by Hisashi Sato

RR by Anonymous Referee #2 (11 Jun 2019)

RR by Hisashi Sato (28 Jun 2019)

ED: Publish subject to technical corrections (28 Jun 2019) by Hisashi Sato

AR by Simon Bowring on behalf of the Authors (03 Jul 2019) Manuscript

Short summary

Few Earth system models represent permafrost soil biogeochemistry, contributing to uncertainty in estimating its response and that of the planet to warming. Because the permafrost contains over double the carbon in the present atmosphere, its fate as it is unlocked by warming is globally significant. One way it can be mobilised is into rivers, the sea, or the atmosphere: a vector previously ignored in climate modelling. We present a model scheme for resolving this vector at a global scale.