Articles | Volume 20, issue 2
https://doi.org/10.5194/tc-20-1163-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-20-1163-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
13 Feb 2026
Research article |
| 13 Feb 2026
| 13 Feb 2026
Multichannel Analysis of Surface Waves (MASW) for the internal characterisation of the Flüela rock glacier: overcoming the limitations of seismic refraction tomography
Ilaria Barone
CORRESPONDING AUTHOR
Department of Geosciences, University of Padova, Padua, Italy
Alexander Bast
WSL Institute for Snow and Avalanche Research SLF, Permafrost Research Group, Davos Dorf, Switzerland
Climate Change, Extremes and Natural Hazards in Alpine Regions Research Center CERC, Davos Dorf, Switzerland
Department of Geosciences, University of Padova, Padua, Italy
Steven Javier Gaona Torres
Department of Geosciences, University of Padova, Padua, Italy
Luca Peruzzo
Department of Geosciences, University of Padova, Padua, Italy
Jacopo Boaga
Department of Geosciences, University of Padova, Padua, Italy
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Short summary
Different geophysical methods such as electrical resistivity tomography (ERT), seismic refraction tomography (SRT) and multichannel analysis of surface waves (MASW) were jointly used to characterize the internal structure of the Flüela rock glacier, Switzerland. We show that the MASW method can efficiently resolve an ice-rich layer even in presence of a supra-permafrost water flow and noisy data, a situation when SRT may fail. Our results are corroborated by seismic synthetic modelling.
Different geophysical methods such as electrical resistivity tomography (ERT), seismic...
