The Cryosphere
The Cryosphere
TC
Articles | Volume 18, issue 7
Articles | Volume 18, issue 7
https://doi.org/10.5194/tc-18-3231-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/tc-18-3231-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 18, issue 7
Brief communication
 | 
16 Jul 2024
Brief communication |  | 16 Jul 2024

Brief communication: On the potential of seismic polarity reversal to identify a thin low-velocity layer above a high-velocity layer in ice-rich rock glaciers

Jacopo Boaga, Mirko Pavoni, Alexander Bast, and Samuel Weber

Viewed

Total article views: 1,349 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,100 189 60 1,349 29 56 63
  • HTML: 1,100
  • PDF: 189
  • XML: 60
  • Total: 1,349
  • Supplement: 29
  • BibTeX: 56
  • EndNote: 63
Views and downloads (calculated since 19 Dec 2023)
Cumulative views and downloads (calculated since 19 Dec 2023)

Viewed (geographical distribution)

Total article views: 1,349 (including HTML, PDF, and XML) Thereof 1,332 with geography defined and 17 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 21 May 2025
Download
Short summary
Reversal polarity is observed in rock glacier seismic refraction tomography. We collected several datasets observing this phenomenon in Switzerland and Italy. This phase change may be linked to interferences due to the presence of a thin low-velocity layer. Our results are confirmed by the modelling and analysis of synthetic seismograms to demonstrate that the presence of a low-velocity layer produces a polarity reversal on the seismic gather.
Read more
Share
Special issue
Emerging geophysical methods for permafrost investigations:...