Articles | Volume 12, issue 10
https://doi.org/10.5194/tc-12-3123-2018
https://doi.org/10.5194/tc-12-3123-2018
Research article
 | 
02 Oct 2018
Research article |  | 02 Oct 2018

Velocity increases at Cook Glacier, East Antarctica, linked to ice shelf loss and a subglacial flood event

Bertie W. J. Miles, Chris R. Stokes, and Stewart S. R. Jamieson

Viewed

Total article views: 4,116 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,536 1,487 93 4,116 389 77 78
  • HTML: 2,536
  • PDF: 1,487
  • XML: 93
  • Total: 4,116
  • Supplement: 389
  • BibTeX: 77
  • EndNote: 78
Views and downloads (calculated since 01 Jun 2018)
Cumulative views and downloads (calculated since 01 Jun 2018)

Viewed (geographical distribution)

Total article views: 4,116 (including HTML, PDF, and XML) Thereof 3,783 with geography defined and 333 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 28 Mar 2024
Download
Short summary
Cook Glacier, as one of the largest in East Antarctica, may have made significant contributions to sea level during past warm periods. However, despite its potential importance there have been no long-term observations of its velocity. Here, through estimating velocity and ice front position from satellite imagery and aerial photography we show that there have been large previously undocumented changes in the velocity of Cook Glacier in response to ice shelf loss and a subglacial drainage event.