Articles | Volume 13, issue 7
https://doi.org/10.5194/tc-13-1925-2019
https://doi.org/10.5194/tc-13-1925-2019
Research article
 | 
15 Jul 2019
Research article |  | 15 Jul 2019

Distinguishing ice-rich and ice-poor permafrost to map ground temperatures and ground ice occurrence in the Swiss Alps

Robert Kenner, Jeannette Noetzli, Martin Hoelzle, Hugo Raetzo, and Marcia Phillips

Viewed

Total article views: 3,157 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,922 1,160 75 3,157 203 72 75
  • HTML: 1,922
  • PDF: 1,160
  • XML: 75
  • Total: 3,157
  • Supplement: 203
  • BibTeX: 72
  • EndNote: 75
Views and downloads (calculated since 07 Jan 2019)
Cumulative views and downloads (calculated since 07 Jan 2019)

Viewed (geographical distribution)

Total article views: 3,157 (including HTML, PDF, and XML) Thereof 2,519 with geography defined and 638 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 25 Apr 2024
Download
Short summary
A new permafrost mapping method distinguishes between ice-poor and ice-rich permafrost. The approach was tested for the entire Swiss Alps and highlights the dominating influence of the factors elevation and solar radiation on the distribution of ice-poor permafrost. Our method enabled the indication of mean annual ground temperatures and the cartographic representation of permafrost-free belts, which are bounded above by ice-poor permafrost and below by permafrost-containing excess ice.