Articles | Volume 14, issue 9
https://doi.org/10.5194/tc-14-3175-2020
https://doi.org/10.5194/tc-14-3175-2020
Research article
 | 
18 Sep 2020
Research article |  | 18 Sep 2020

An analysis of instabilities and limit cycles in glacier-dammed reservoirs

Christian Schoof

Viewed

Total article views: 2,231 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,499 633 99 2,231 169 109 99
  • HTML: 1,499
  • PDF: 633
  • XML: 99
  • Total: 2,231
  • Supplement: 169
  • BibTeX: 109
  • EndNote: 99
Views and downloads (calculated since 15 Jul 2019)
Cumulative views and downloads (calculated since 15 Jul 2019)

Viewed (geographical distribution)

Total article views: 2,231 (including HTML, PDF, and XML) Thereof 1,958 with geography defined and 273 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 27 Mar 2025
Download
Short summary
Glacier lake outburst floods are major glacial hazards in which ice-dammed reservoirs rapidly drain, often in a recurring fashion. The main flood phase typically involves a growing channel being eroded into ice by water flow. What is poorly understood is how that channel first comes into being. In this paper, I investigate how an under-ice drainage system composed of small, naturally occurring voids can turn into a channel and how this can explain the cyclical behaviour of outburst floods.
Share