Late Quaternary glacial history constrains glacio-isostatic rebound in Enderby Land, East Antarctica

Measurements of the loss or gain of ice mass from large ice sheets are presently achieved through satellite-based techniques such as GRACE (Gravity Recovery and Climate Experiment). The accuracy of these satellite-based measurements to changes in modern ice sheet mass depends on our knowledge of pre...

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Bibliographic Details
Published in:Journal of Geophysical Research: Earth Surface
Main Authors: White, Duanne A., Fink, David
Format: Article in Journal/Newspaper
Language:English
Published: 2014
Subjects:
Gravity Recovery and Climate Experiment (GRACE)
cosmogenic nuclide exposure dating
glacial erosion
mass balance
sea level
subglacial environments
East Antarctica
Rayner
Rayner Glacier
Antarc*
Antarctica
Antarctica Journal
Enderby Land
Ice Sheet
Online Access:https://researchers.mq.edu.au/en/publications/1c0501cc-e5ef-40e3-be1c-2644f920a187
https://doi.org/10.1002/2013JF002870
https://research-management.mq.edu.au/ws/files/62376942/Publisher%20version%20(open%20access).pdf
http://www.scopus.com/inward/record.url?scp=84898678867&partnerID=8YFLogxK
Description
Summary:Measurements of the loss or gain of ice mass from large ice sheets are presently achieved through satellite-based techniques such as GRACE (Gravity Recovery and Climate Experiment). The accuracy of these satellite-based measurements to changes in modern ice sheet mass depends on our knowledge of present-day glacio-isostatic crustal uplift rates caused by past ice sheet changes. To improve models of glacio-isostatic rebound in East Antarctica, we investigated ice histories along Rayner Glacier, Enderby Land, and a little explored sector of the ice sheet where GRACE data had suggested significant mass gain during the last decade. Observations from a recent glacial geomorphic reconnaissance coupled with cosmogenic nuclide dating indicate that in the lower part of the Rayner Glacier, Enderby Land, ice heights lowered by at least 300 m and the calving margin retreated by at least 10 km in the early Holocene (∼6 to 9 ka B.P.). The magnitude and timing of deglaciation are consistent with ice histories used to model the postglacial rebound corrections for present-day GRACE mass trends. These observations strengthen the body of evidence that suggests ice mass gain in Enderby Land is presently partly offsetting mass loss in other parts of Antarctica.

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