Articles | Volume 6, issue 2
https://doi.org/10.5194/tc-6-517-2012
© Author(s) 2012. This work is distributed under the Creative Commons Attribution 3.0 License.
Research article
| 
19 Apr 2012
Research article |
| 19 Apr 2012
Influence of surface and subsurface heterogeneity on observed borehole temperatures at a mountain permafrost site in the Upper Engadine, Swiss Alps
Related subject area
Mountain Processes
Mountain permafrost in the Central Pyrenees: insights from the Devaux ice cave
Glacier–permafrost relations in a high-mountain environment: 5 decades of kinematic monitoring at the Gruben site, Swiss Alps
How much snow falls in the world's mountains? A first look at mountain snowfall estimates in A-train observations and reanalyses
The Cryosphere, 17, 477–497, 2023
The Cryosphere, 16, 2083–2101, 2022
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Cited articles
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Barsch, D.: Ein Permafrostprofil aus Graubünden, Schweizer Alpen, Zeitschrift fuer Geomorphologie, 21, 79–86, 1977.
Delaloye, R.: Contribution à l'étude du pergélisol de montagne en zone marginale, Ph.D. thesis, Fac. Sciences, Université de Fribourg, GeoFocus 10, 2004.
Delaloye, R. and Lambiel, C.: Evidence of winter ascending air circulation throughout talus slopes and rock glaciers situated in the lower belt of alpine discontinous permafrost (Swiss Alps), Norwegian Journal of Geography, 59, 194–203, 2005.
Delaloye, R., Reynard, E., Lambiel, C., Marescot, L., and Monnet, R.: Thermal anomaly in a cold scree slope, Creux du Van, Switzerland, in: 8th International Conference on Permafrost, pp. 175–180, Zürich, 2003.
