Articles | Volume 8, issue 1
https://doi.org/10.5194/essd-8-151-2016
https://doi.org/10.5194/essd-8-151-2016
06 Apr 2016
 | 06 Apr 2016

Subglacial landforms beneath Rutford Ice Stream, Antarctica: detailed bed topography from ice-penetrating radar

Edward C. King, Hamish D. Pritchard, and Andrew M. Smith

Viewed

Total article views: 4,273 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,213 1,848 212 4,273 169 163
  • HTML: 2,213
  • PDF: 1,848
  • XML: 212
  • Total: 4,273
  • BibTeX: 169
  • EndNote: 163
Views and downloads (calculated since 12 Nov 2015)
Cumulative views and downloads (calculated since 12 Nov 2015)

Cited

Saved (preprint)

Discussed (final revised paper)

Latest update: 23 Nov 2024
Download
Short summary
Large, fast-moving glaciers create long, linear mounds of sediments covering large areas. Understanding how these features form has been hampered by a lack of data from the bed of modern-day ice sheets. We give a detailed view of the landscape beneath an Antarctic glacier called Rutford Ice Stream. We towed a radar system back and forth across the glacier to measure the ice thickness every few metres. This is the first place such a highly detailed view of the sub-ice landscape has been created.
Altmetrics
Final-revised paper
Preprint