Articles | Volume 11, issue 4
https://doi.org/10.5194/tc-11-1691-2017
https://doi.org/10.5194/tc-11-1691-2017
Research article
 | 
21 Jul 2017
Research article |  | 21 Jul 2017

New observations indicate the possible presence of permafrost in North Africa (Djebel Toubkal, High Atlas, Morocco)

Gonçalo Vieira, Carla Mora, and Ali Faleh

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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 Gonçalo Vieira on behalf of the Authors (06 Mar 2017)
ED: Reconsider after major revisions (15 Mar 2017) by Marcia Phillips
AR by Gonçalo Vieira on behalf of the Authors (30 Apr 2017)  Manuscript 
ED: Reconsider after major revisions (03 May 2017) by Marcia Phillips
AR by Gonçalo Vieira on behalf of the Authors (03 Jun 2017)  Author's response   Manuscript 
ED: Publish subject to technical corrections (08 Jun 2017) by Marcia Phillips
AR by Gonçalo Vieira on behalf of the Authors (09 Jun 2017)  Author's response   Manuscript 
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Short summary
The Toubkal is the highest massif in North Africa (4167 m). Landforms and deposits above 3000 m show the effects of frost action in the present-day geomorphological dynamics, but data on ground temperatures were lacking. In this study ground surface temperature data measured across an altitudinal transect are presented and analysed for the first time. The highlight is the possible occurrence of permafrost at an elevation of 3800 m, which may be of high ecological and hydrological significance.