The Cryosphere
The Cryosphere
TC
Articles | Volume 20, issue 7
Articles | Volume 20, issue 7
https://doi.org/10.5194/tc-20-3977-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-20-3977-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 20, issue 7
Research article
 | 
20 Jul 2026
Research article |  | 20 Jul 2026

Late Holocene stabilization of Conway Ice Ridge

Andrew O. Hoffman, Paul T. Summers, Jenny Suckale, Knut Christianson, Ginny Catania, and Howard Conway

Viewed

Total article views: 6,822 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
5,753 848 221 6,822 294 431
  • HTML: 5,753
  • PDF: 848
  • XML: 221
  • Total: 6,822
  • BibTeX: 294
  • EndNote: 431
Views and downloads (calculated since 27 Mar 2025)
Cumulative views and downloads (calculated since 27 Mar 2025)

Viewed (geographical distribution)

Total article views: 6,822 (including HTML, PDF, and XML) Thereof 6,822 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 09 Aug 2026
Download
Short summary
In Antarctica, fast-flowing ice streams drive most ice loss. Radar data from Conway Ice Ridge reveal that the van der Veen and Mercer Ice Streams were wider ~3000 years ago and narrowed progressively. Numerical modeling demonstrates that small thickness changes can rapidly alter shear-margin locations. These findings offer crucial insights into Late Holocene Ice Sheet readvance.
Read more
Share