The Cryosphere
The Cryosphere
TC
Articles | Volume 14, issue 11
Articles | Volume 14, issue 11
https://doi.org/10.5194/tc-14-3747-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-14-3747-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 14, issue 11
Research article
 | 
12 Nov 2020
Research article |  | 12 Nov 2020

Possible impacts of a 1000 km long hypothetical subglacial river valley towards Petermann Glacier in northern Greenland

Christopher Chambers, Ralf Greve, Bas Altena, and Pierre-Marie Lefeuvre

Viewed

Total article views: 7,273 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
5,866 1,275 132 7,273 165 164
  • HTML: 5,866
  • PDF: 1,275
  • XML: 132
  • Total: 7,273
  • BibTeX: 165
  • EndNote: 164
Views and downloads (calculated since 24 Jul 2019)
Cumulative views and downloads (calculated since 24 Jul 2019)

Viewed (geographical distribution)

Total article views: 7,273 (including HTML, PDF, and XML) Thereof 6,402 with geography defined and 871 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 30 Jun 2025
Download
Short summary
The topography of the rock below the Greenland ice sheet is not well known. One long valley appears as a line of dips because of incomplete data. So we use ice model simulations that unblock this valley, and these create a watercourse that may represent a form of river over 1000 km long under the ice. When we melt ice at the bottom of the ice sheet only in the deep interior, water can flow down the valley only when the valley is unblocked. It may have developed while an ice sheet was present.
Read more
Share