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The Cryosphere An interactive open-access journal of the European Geosciences Union
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Volume 11, issue 4
The Cryosphere, 11, 1813–1834, 2017
https://doi.org/10.5194/tc-11-1813-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: The evolution of permafrost in mountain regions

The Cryosphere, 11, 1813–1834, 2017
https://doi.org/10.5194/tc-11-1813-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 04 Aug 2017

Research article | 04 Aug 2017

Modelling rock wall permafrost degradation in the Mont Blanc massif from the LIA to the end of the 21st century

Florence Magnin et al.
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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 Anna Mirena Feist-Polner on behalf of the Authors (02 Dec 2016)  Author's response
ED: Referee Nomination & Report Request started (29 Jan 2017) by Christian Hauck
RR by Anonymous Referee #2 (03 Apr 2017)
RR by Anonymous Referee #3 (17 Apr 2017)
ED: Publish subject to minor revisions (Editor review) (05 May 2017) by Christian Hauck
AR by Anna Mirena Feist-Polner on behalf of the Authors (23 May 2017)  Author's response
ED: Publish subject to technical corrections (20 Jun 2017) by Christian Hauck
AR by Florence Magnin on behalf of the Authors (21 Jun 2017)  Author's response    Manuscript
Publications Copernicus
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Short summary
Permafrost degradation in high mountain rock walls provokes destabilisation, constituting a threat for human activities. In the Mont Blanc massif, more than 700 rockfalls have been inventoried in recent years (2003, 2007–2015). Understanding permafrost evolution is thus crucial to sustain this densely populated area. This study investigates the changes in rock wall permafrost from 1850 to the recent period and possible optimistic or pessimistic evolutions during the 21st century.
Permafrost degradation in high mountain rock walls provokes destabilisation, constituting a...
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