Articles | Volume 17, issue 11
https://doi.org/10.5194/tc-17-4797-2023
https://doi.org/10.5194/tc-17-4797-2023
Research article
 | 
15 Nov 2023
Research article |  | 15 Nov 2023

The evolution of isolated cavities and hydraulic connection at the glacier bed – Part 1: Steady states and friction laws

Christian Schoof

Viewed

Total article views: 3,309 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,354 797 158 3,309 184 268
  • HTML: 2,354
  • PDF: 797
  • XML: 158
  • Total: 3,309
  • BibTeX: 184
  • EndNote: 268
Views and downloads (calculated since 09 Jan 2023)
Cumulative views and downloads (calculated since 09 Jan 2023)

Viewed (geographical distribution)

Total article views: 3,309 (including HTML, PDF, and XML) Thereof 3,309 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Saved (final revised paper)

Latest update: 09 Jun 2026
Short summary
Computational models that seek to predict the future behaviour of ice sheets and glaciers typically rely on being able to compute the rate at which a glacier slides over its bed. In this paper, I show that the degree to which the glacier bed is hydraulically connected (how easily water can flow along the glacier bed) plays a central role in determining how fast ice can slide.
Share