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View article: Modeling active layer thickness in permafrost rock walls based on an analytical solution of the heat transport equation, Kitzsteinhorn, Hohe Tauern Range, Austria
Modeling active layer thickness in permafrost rock walls based on an analytical solution of the heat transport equation, Kitzsteinhorn, Hohe Tauern Range, Austria Open
The active layer thickness (ALT) refers to the seasonal thaw depth of a permafrost body and in high alpine environments represents an essential parameter for natural hazard analysis. The aim of this study is to model ALT based on bedrock t…
View article: From ice-filled fractures to pressurised water flow in permafrost bedrock: seasonal changes in rockwall hydrology
From ice-filled fractures to pressurised water flow in permafrost bedrock: seasonal changes in rockwall hydrology Open
Alpine permafrost is warming globally and has been extensively studied through electrical resistivity monitoring and borehole temperature measurements. However, permafrost degradation is often primarily attributed to rising air temperature…
View article: Novel concepts for the mechanical modelling of warming permafrost rock slopes
Novel concepts for the mechanical modelling of warming permafrost rock slopes Open
This paper discusses mechanical modelling strategies for instable permafrost bedrock. Modelling instable permafrost bedrock is a key requirement to anticipate magnitudes and frequency of rock slope failures in a changing climate but also t…
View article: Pressurised water flow in fractured permafrost rocks revealed by borehole temperature, electrical resistivity tomography, and piezometric pressure
Pressurised water flow in fractured permafrost rocks revealed by borehole temperature, electrical resistivity tomography, and piezometric pressure Open
Rock slope instabilities and failures from permafrost rocks are among the most significant alpine hazards in a changing climate and represent considerable threats to high-alpine infrastructure. While permafrost degradation is commonly attr…
Reply on CC1 Open
Abstract. Rock slope instabilities and failures from permafrost are among the most significant alpine hazards in a changing climate and represent considerable threats to high-alpine infrastructure. While permafrost degradation is commonly …
Reply on RC2 Open
Abstract. Rock slope instabilities and failures from permafrost are among the most significant alpine hazards in a changing climate and represent considerable threats to high-alpine infrastructure. While permafrost degradation is commonly …
Reply on RC1 Open
Abstract. Rock slope instabilities and failures from permafrost are among the most significant alpine hazards in a changing climate and represent considerable threats to high-alpine infrastructure. While permafrost degradation is commonly …
View article: Comment on egusphere-2024-893
Comment on egusphere-2024-893 Open
Abstract. Rock slope instabilities and failures from permafrost are among the most significant alpine hazards in a changing climate and represent considerable threats to high-alpine infrastructure. While permafrost degradation is commonly …
View article: Comment on egusphere-2024-893
Comment on egusphere-2024-893 Open
Abstract. Rock slope instabilities and failures from permafrost are among the most significant alpine hazards in a changing climate and represent considerable threats to high-alpine infrastructure. While permafrost degradation is commonly …
View article: Comment on egusphere-2024-893
Comment on egusphere-2024-893 Open
Abstract. Rock slope instabilities and failures from permafrost are among the most significant alpine hazards in a changing climate and represent considerable threats to high-alpine infrastructure. While permafrost degradation is commonly …
View article: Pressurised water flow in fractured permafrost rocks revealed by joint electrical resistivity monitoring and borehole temperature analysis
Pressurised water flow in fractured permafrost rocks revealed by joint electrical resistivity monitoring and borehole temperature analysis Open
Rock slope instabilities and failures from permafrost are among the most significant alpine hazards in a changing climate and represent considerable threats to high-alpine infrastructure. While permafrost degradation is commonly attributed…
Long-time permafrost evolution in alpine bedrock: quantifying climate change effects with geoelectrical monitoring Open
While climate change driven increase in air temperature has been correctly modeled in recent decades, the extent of its consequences is still uncertain. In high alpine environments, especially in steep rock walls, permafrost degradation re…
Using combined quantitative geophysical methods to delimit physical properties of low porosity permafrost bedrocks  Open
Degradation of mountain permafrost poses an increasing hazard to the stability of high-alpine infrastructures, which are predominantly located in low porosity bedrocks. Considering the dramatic climate change-induced temperature increase a…
4D quantification of alpine permafrost degradation in steep rock walls using a laboratory‐calibrated electrical resistivity tomography approach Open
Figure 1 D was incorrectly printed. The correct Figure 1D should read.
4D-Quantification of alpine permafrost degradation in a bedrock ridge using multiple inversion schemes and deformation measurements Open
Warming of permafrost in steep rock walls decreases their mechanical stability and could triggers rockfalls and rockslides. However, the direct link between climate change and permafrost degradation is seldom quantified with precise monito…
4D quantification of alpine permafrost degradation in steep rock walls using a laboratory‐calibrated electrical resistivity tomography approach Open
The warming of rock permafrost affects mechanical stability and hydro‐cryostatic pressures in rock walls. The coincident decrease in slope stability frequently affects infrastructure by creep and subsidence and promotes the generation of r…