Articles | Volume 12, issue 5
https://doi.org/10.5194/tc-12-1563-2018
https://doi.org/10.5194/tc-12-1563-2018
Research article
 | 
03 May 2018
Research article |  | 03 May 2018

Simulating the roles of crevasse routing of surface water and basal friction on the surge evolution of Basin 3, Austfonna ice cap

Yongmei Gong, Thomas Zwinger, Jan Åström, Bas Altena, Thomas Schellenberger, Rupert Gladstone, and John C. Moore

Viewed

Total article views: 3,557 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,207 1,240 110 3,557 156 100 99
  • HTML: 2,207
  • PDF: 1,240
  • XML: 110
  • Total: 3,557
  • Supplement: 156
  • BibTeX: 100
  • EndNote: 99
Views and downloads (calculated since 03 Nov 2017)
Cumulative views and downloads (calculated since 03 Nov 2017)

Viewed (geographical distribution)

Total article views: 3,557 (including HTML, PDF, and XML) Thereof 3,289 with geography defined and 268 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 20 Nov 2024
Download
Short summary
In this study we apply a discrete element model capable of simulating ice fracturing. A microscopic-scale discrete process is applied in addition to a continuum ice dynamics model to investigate the mechanisms facilitated by basal meltwater production, surface meltwater and ice crack opening, for the surge in Basin 3, Austfonna ice cap. The discrete element model is used to locate the ice cracks that can penetrate though the full thickness of the glacier and deliver surface water to the bed.