Articles | Volume 20, issue 10
https://doi.org/10.5194/tc-20-5675-2026
https://doi.org/10.5194/tc-20-5675-2026
Research article
 | 
06 Oct 2026
Research article |  | 06 Oct 2026

Simulating jökulhlaups from an ice-marginal lake within a 2D model of subglacial drainage and basal sliding

Adam J. Hepburn, Sammie Buzzard, Andrew J. Sole, Stephen J. Livingstone, Felix Ng, Mathieu Morlighem, Elizabeth A. Bagshaw, Caroline Clason, Lisa Craw, Christine F. Dow, Samuel Doyle, Jonathan Hawkins, Matthew Peacey, and Robert Storrar

Viewed

Total article views: 468 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
321 117 30 468 29 23
  • HTML: 321
  • PDF: 117
  • XML: 30
  • Total: 468
  • BibTeX: 29
  • EndNote: 23
Views and downloads (calculated since 16 Jun 2026)
Cumulative views and downloads (calculated since 16 Jun 2026)

Viewed (geographical distribution)

Total article views: 468 (including HTML, PDF, and XML) Thereof 439 with geography defined and 29 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 07 Oct 2026
Download
Short summary
Lakes at glacier margins can drain beneath the ice in devastating, floods called jökulhlaups. We present the first 2D model of jökulhlaup propagation, first applying it to a synthetic glacier, before then assessing its ability to reproduce an observed record of lake fill-drain cycles in Greenland. Our results match a 17-year record of flood timing but underpredicts peak discharge likely because we are missing certain physical processes. Our results hold promise for simulating jökulhlaups.
Share