The Cryosphere
The Cryosphere
TC
Articles | Volume 18, issue 3
Articles | Volume 18, issue 3
https://doi.org/10.5194/tc-18-1125-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/tc-18-1125-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 18, issue 3
Research article
 | 
08 Mar 2024
Research article |  | 08 Mar 2024

The staggered retreat of grounded ice in the Ross Sea, Antarctica, since the Last Glacial Maximum (LGM)

Matthew A. Danielson and Philip J. Bart

Viewed

Total article views: 926 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
644 227 55 926 51 34 40
  • HTML: 644
  • PDF: 227
  • XML: 55
  • Total: 926
  • Supplement: 51
  • BibTeX: 34
  • EndNote: 40
Views and downloads (calculated since 28 Jul 2023)
Cumulative views and downloads (calculated since 28 Jul 2023)

Viewed (geographical distribution)

Total article views: 926 (including HTML, PDF, and XML) Thereof 913 with geography defined and 13 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 08 May 2024
Download
Short summary
The post-Last Glacial Maximum (LGM) retreat of the West Antarctic Ice Sheet in the Ross Sea was more significant than for any other Antarctic sector. Here we combined the available dates of retreat with new mapping of sediment deposited by the ice sheet during overall retreat. Our work shows that the post-LGM retreat through the Ross Sea was not uniform. This uneven retreat can cause instability in the present-day Antarctic ice sheet configuration and lead to future runaway retreat.
Read more
Special issue
Icy landscapes of the past (CP/ESSD/ESurf/TC inter-journal...