Articles | Volume 15, issue 4
https://doi.org/10.5194/tc-15-1863-2021
https://doi.org/10.5194/tc-15-1863-2021
Research article
 | 
19 Apr 2021
Research article |  | 19 Apr 2021

Grounding zone subglacial properties from calibrated active-source seismic methods

Huw J. Horgan, Laurine van Haastrecht, Richard B. Alley, Sridhar Anandakrishnan, Lucas H. Beem, Knut Christianson, Atsuhiro Muto, and Matthew R. Siegfried

Viewed

Total article views: 2,026 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,310 618 98 2,026 77 73
  • HTML: 1,310
  • PDF: 618
  • XML: 98
  • Total: 2,026
  • BibTeX: 77
  • EndNote: 73
Views and downloads (calculated since 16 Jul 2020)
Cumulative views and downloads (calculated since 16 Jul 2020)

Viewed (geographical distribution)

Total article views: 2,026 (including HTML, PDF, and XML) Thereof 1,946 with geography defined and 80 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 13 Dec 2024
Download
Short summary
The grounding zone marks the transition from a grounded ice sheet to a floating ice shelf. Like Earth's coastlines, the grounding zone is home to interactions between the ocean, fresh water, and geology but also has added complexity and importance due to the overriding ice. Here we use seismic surveying – sending sound waves down through the ice – to image the grounding zone of Whillans Ice Stream in West Antarctica and learn more about the nature of this important transition zone.