Articles | Volume 14, issue 12
https://doi.org/10.5194/tc-14-4341-2020
https://doi.org/10.5194/tc-14-4341-2020
Research article
 | 
02 Dec 2020
Research article |  | 02 Dec 2020

Ground ice, organic carbon and soluble cations in tundra permafrost soils and sediments near a Laurentide ice divide in the Slave Geological Province, Northwest Territories, Canada

Rupesh Subedi, Steven V. Kokelj, and Stephan Gruber

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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
ED: Reconsider after major revisions (further review by editor and referees) (09 Jul 2020) by Christian Hauck
AR by Stephan Gruber on behalf of the Authors (11 Jul 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (22 Jul 2020) by Christian Hauck
RR by Anonymous Referee #1 (10 Aug 2020)
ED: Publish subject to minor revisions (review by editor) (23 Sep 2020) by Christian Hauck
AR by Stephan Gruber on behalf of the Authors (06 Oct 2020)  Author's response    Manuscript
ED: Publish as is (26 Oct 2020) by Christian Hauck
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Short summary
Permafrost beneath tundra near Lac de Gras (Northwest Territories, Canada) contains more ice and less organic carbon than shown in global compilations. Excess-ice content of 20–60 %, likely remnant Laurentide basal ice, is found in upland till. This study is based on 24 boreholes up to 10 m deep. Findings highlight geology and glacial legacy as determinants of a mosaic of permafrost characteristics with potential for thaw subsidence up to several metres in some locations.