Articles | Volume 12, issue 12
Geosci. Model Dev., 12, 5291–5300, 2019
https://doi.org/10.5194/gmd-12-5291-2019
Geosci. Model Dev., 12, 5291–5300, 2019
https://doi.org/10.5194/gmd-12-5291-2019

Model description paper 19 Dec 2019

Model description paper | 19 Dec 2019

Ground subsidence effects on simulating dynamic high-latitude surface inundation under permafrost thaw using CLM5

Altug Ekici et al.

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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 Svenja Lange on behalf of the Authors (21 Aug 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (28 Aug 2019) by Min-Hui Lo
RR by Anonymous Referee #1 (29 Aug 2019)
RR by Anonymous Referee #4 (10 Sep 2019)
ED: Reconsider after major revisions (01 Oct 2019) by Min-Hui Lo
AR by Anna Wenzel on behalf of the Authors (08 Oct 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (08 Oct 2019) by Min-Hui Lo
RR by Anonymous Referee #4 (28 Oct 2019)
ED: Publish as is (14 Nov 2019) by Min-Hui Lo
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Short summary
Ice-rich permafrost thaw can create expanding thermokarst lakes as well as shrinking large wetlands. Such processes can have major biogeochemical implications and feedbacks to climate systems by altering the pathways and rates of permafrost carbon release. We developed a new model parameterization that allows a direct representation of surface water dynamics with subsidence. Our results show increased surface water fractions around western Siberian plains and northeastern territories of Canada.