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: 6,308 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
3,658 2,394 256 6,308 650 233 322
  • HTML: 3,658
  • PDF: 2,394
  • XML: 256
  • Total: 6,308
  • Supplement: 650
  • BibTeX: 233
  • EndNote: 322
Views and downloads (calculated since 10 Feb 2016)
Cumulative views and downloads (calculated since 10 Feb 2016)
Latest update: 03 Mar 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