Articles | Volume 11, issue 3
The Cryosphere, 11, 1351–1370, 2017
https://doi.org/10.5194/tc-11-1351-2017

Special issue: The evolution of permafrost in mountain regions

The Cryosphere, 11, 1351–1370, 2017
https://doi.org/10.5194/tc-11-1351-2017

Research article 09 Jun 2017

Research article | 09 Jun 2017

Wind-driven snow conditions control the occurrence of contemporary marginal mountain permafrost in the Chic-Choc Mountains, south-eastern Canada: a case study from Mont Jacques-Cartier

Gautier Davesne et al.

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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Gautier Davesne on behalf of the Authors (09 Jan 2017)  Author's response    Manuscript
ED: Publish subject to minor revisions (Editor review) (15 Feb 2017) by Ketil Isaksen
AR by Gautier Davesne on behalf of the Authors (09 Mar 2017)  Author's response    Manuscript
ED: Publish as is (09 Mar 2017) by Ketil Isaksen
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Short summary
This study presents data from Mont Jacques-Cartier, the highest summit in the Appalachians of south-eastern Canada, to demonstrate that the occurrence of contemporary permafrost body is associated with a very thin and wind-packed winter snow cover which brings local azonal topo-climatic conditions on the dome-shaped summit. This study is an important preliminary step in modelling the regional spatial distribution of permafrost on the highest summits in eastern North America.