Articles | Volume 13, issue 7
https://doi.org/10.5194/tc-13-1889-2019
https://doi.org/10.5194/tc-13-1889-2019
Research article
 | 
11 Jul 2019
Research article |  | 11 Jul 2019

Unravelling the evolution of Zmuttgletscher and its debris cover since the end of the Little Ice Age

Nico Mölg, Tobias Bolch, Andrea Walter, and Andreas Vieli

Viewed

Total article views: 3,233 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,040 1,116 77 3,233 406 73 79
  • HTML: 2,040
  • PDF: 1,116
  • XML: 77
  • Total: 3,233
  • Supplement: 406
  • BibTeX: 73
  • EndNote: 79
Views and downloads (calculated since 18 Jan 2019)
Cumulative views and downloads (calculated since 18 Jan 2019)

Viewed (geographical distribution)

Total article views: 3,233 (including HTML, PDF, and XML) Thereof 2,697 with geography defined and 536 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 27 Mar 2024
Download
Short summary
Debris can partly protect glaciers from melting. But many debris-covered glaciers change similar to debris-free glaciers. To better understand the debris influence we investigated 150 years of evolution of Zmutt Glacier in Switzerland. We found an increase in debris extent over time and a link to glacier flow velocity changes. We also found an influence of debris on the melt locally, but only a small volume change reduction over the whole glacier, also because of the influence of ice cliffs.