The Cryosphere
The Cryosphere
TC
Articles | Volume 14, issue 11
Articles | Volume 14, issue 11
https://doi.org/10.5194/tc-14-4121-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-14-4121-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 14, issue 11
Research article
 | 
18 Nov 2020
Research article |  | 18 Nov 2020

Sharp contrasts in observed and modeled crevasse patterns at Greenland's marine terminating glaciers

Ellyn M. Enderlin and Timothy C. Bartholomaus

Viewed

Total article views: 3,499 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,216 1,172 111 3,499 421 118 130
  • HTML: 2,216
  • PDF: 1,172
  • XML: 111
  • Total: 3,499
  • Supplement: 421
  • BibTeX: 118
  • EndNote: 130
Views and downloads (calculated since 12 Jun 2019)
Cumulative views and downloads (calculated since 12 Jun 2019)

Viewed (geographical distribution)

Total article views: 3,499 (including HTML, PDF, and XML) Thereof 3,044 with geography defined and 455 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 23 Apr 2025
Download
Short summary
Accurate predictions of future changes in glacier flow require the realistic simulation of glacier terminus position change in numerical models. We use crevasse observations for 19 Greenland glaciers to explore whether the two commonly used crevasse depth models match observations. The models cannot reproduce spatial patterns, and we largely attribute discrepancies between modeled and observed depths to the models' inability to account for advection.
Read more
Share