Articles | Volume 12, issue 8
https://doi.org/10.5194/tc-12-2609-2018
https://doi.org/10.5194/tc-12-2609-2018
Research article
 | Highlight paper
 | 
14 Aug 2018
Research article | Highlight paper |  | 14 Aug 2018

Channelized, distributed, and disconnected: subglacial drainage under a valley glacier in the Yukon

Camilo Rada and Christian Schoof

Viewed

Total article views: 7,454 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
5,483 1,819 152 7,454 623 124 106
  • HTML: 5,483
  • PDF: 1,819
  • XML: 152
  • Total: 7,454
  • Supplement: 623
  • BibTeX: 124
  • EndNote: 106
Views and downloads (calculated since 19 Jan 2018)
Cumulative views and downloads (calculated since 19 Jan 2018)

Viewed (geographical distribution)

Total article views: 7,454 (including HTML, PDF, and XML) Thereof 6,569 with geography defined and 885 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Latest update: 29 Jun 2024
Short summary
We analyse a large glacier borehole pressure dataset and provide a holistic view of the observations, suggesting a consistent picture of the evolution of the subglacial drainage system. Some aspects are consistent with the established understanding and others ones are not. We propose that most of the inconsistencies arise from the capacity of some areas of the bed to become hydraulically isolated. We present an adaptation of an existing drainage model that incorporates this phenomena.