Articles | Volume 7, issue 4
https://doi.org/10.5194/esurf-7-1019-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/esurf-7-1019-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Permafrost distribution in steep rock slopes in Norway: measurements, statistical modelling and implications for geomorphological processes
Florence Magnin
CORRESPONDING AUTHOR
Department of Geosciences, University of Oslo, Oslo, 0316, Norway
Bernd Etzelmüller
Department of Geosciences, University of Oslo, Oslo, 0316, Norway
Sebastian Westermann
Department of Geosciences, University of Oslo, Oslo, 0316, Norway
Ketil Isaksen
The Norwegian Meteorological Institute, Oslo, 0313, Norway
Paula Hilger
Department of Geosciences, University of Oslo, Oslo, 0316, Norway
Geological Survey of Norway, Trondheim, 7040, Norway
Reginald L. Hermanns
Geological Survey of Norway, Trondheim, 7040, Norway
Institute for Geoscience and Petroleum, Norwegian University of
Science and Technology, Trondheim, 7040, Norway
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- Thermal photogrammetry on a permafrost rock wall for the active layer monitoring S. Ponti et al. 10.1016/j.scitotenv.2024.170391
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- Interpretation, age and significance of a relict paraglacial and periglacial boulder-dominated landform assemblage in Alnesdalen, Romsdalsalpane, southern Norway P. Wilson et al. 10.1016/j.geomorph.2020.107362
- First evidence of rock wall permafrost in the Pyrenees (Vignemale peak, 3,298 m a.s.l., 42°46′16″N/0°08′33″W) I. Rico et al. 10.1002/ppp.2130
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Latest update: 28 Mar 2024
Short summary
This study proposes the first permafrost (i.e. ground with temperature permanently < 0 °C) map covering the steep rock slopes of Norway. It was created by using rock temperature data collected at the near surface of 25 rock walls spread across the country between 2010 and 2018. The map shows that permafrost mostly exists above 1300–1400 m a.s.l. in southern Norway and close to sea level in northern Norway. The results have strong potential for the study of rock wall sliding and failure.
This study proposes the first permafrost (i.e. ground with temperature permanently 0 °C) map...