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

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AR by Anna Ruth Halberstadt on behalf of the Authors (26 Apr 2016)  Author's response   Manuscript 
ED: Publish as is (29 Apr 2016) by Chris R. Stokes
AR by Anna Ruth Halberstadt on behalf of the Authors (30 Apr 2016)  Author's response   Manuscript 
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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.