Articles | Volume 12, issue 9
https://doi.org/10.5194/tc-12-2831-2018
https://doi.org/10.5194/tc-12-2831-2018
Research article
 | 
05 Sep 2018
Research article |  | 05 Sep 2018

A constraint upon the basal water distribution and thermal state of the Greenland Ice Sheet from radar bed echoes

Thomas M. Jordan, Christopher N. Williams, Dustin M. Schroeder, Yasmina M. Martos, Michael A. Cooper, Martin J. Siegert, John D. Paden, Philippe Huybrechts, and Jonathan L. Bamber

Viewed

Total article views: 3,858 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,142 1,589 127 3,858 105 103
  • HTML: 2,142
  • PDF: 1,589
  • XML: 127
  • Total: 3,858
  • BibTeX: 105
  • EndNote: 103
Views and downloads (calculated since 22 Mar 2018)
Cumulative views and downloads (calculated since 22 Mar 2018)

Viewed (geographical distribution)

Total article views: 3,858 (including HTML, PDF, and XML) Thereof 3,570 with geography defined and 288 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 19 Apr 2024
Download
Short summary
Here, via analysis of radio-echo sounding data, we place a new observational constraint upon the basal water distribution beneath the Greenland Ice Sheet. In addition to the outlet glaciers, we demonstrate widespread water storage in the northern and eastern ice-sheet interior, a notable feature being a "corridor" of basal water extending from NorthGRIP to Petermann Glacier. The basal water distribution and its relationship with basal temperature provides a new constraint for numerical models.