Articles | Volume 10, issue 3
https://doi.org/10.5194/tc-10-1003-2016
https://doi.org/10.5194/tc-10-1003-2016
Research article
 | 
13 May 2016
Research article |  | 13 May 2016

Past ice-sheet behaviour: retreat scenarios and changing controls in the Ross Sea, Antarctica

Anna Ruth W. Halberstadt, Lauren M. Simkins, Sarah L. Greenwood, and John B. Anderson

Viewed

Total article views: 7,078 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
4,014 2,727 337 7,078 759 296 367
  • HTML: 4,014
  • PDF: 2,727
  • XML: 337
  • Total: 7,078
  • Supplement: 759
  • BibTeX: 296
  • EndNote: 367
Views and downloads (calculated since 10 Feb 2016)
Cumulative views and downloads (calculated since 10 Feb 2016)

Cited

Saved (final revised paper)

Latest update: 25 Oct 2026
Download
Short summary
Geomorphic features on the Ross Sea sea floor provide a record of ice-sheet behaviour during the Last Glacial Maximum and subsequent retreat. Based on extensive mapping of these glacial landforms, a large embayment formed in the eastern Ross Sea. This was followed by complex, late-stage retreat in the western Ross Sea where banks stabilised the ice sheet. Physiography and sea floor geology act as regional controls on ice-sheet dynamics across the Ross Sea.
Share