Summary

Ice within marine basins of East Antarctica, and their outlets, represent the ultimate limit on sea level change. The region of East Antarctica between the Ross Sea and Wilkes Land hosts a number of major basin, but has been poorly understood. Long range aerogeophysics from US, Australian and French stations, with significant British and IceBridge support, has, under the banner of the ICECAP project, greatly improved our knowledge of ice thickness, surface elevation, and crustal structure of the Wilkes and Aurora Subglacial Basins, as well as the Totten Glacier, Cook Ice Shelf, and Byrd Glacier. We will discuss the evolution of the Wilkes and Aurora Subglacial Basins, new constraints on the geometry of the major outlet glaciers, as well as our results from surface elevation change measurements over dynamic regions of the ice sheet. We will discuss the implications of our data for the presence of mid Pleistocene ice in central East Antarctica. Future directions for ICECAP will be discussed.

Authors:Blankenship D.D. Young D.A. Siegert M.J. van Ommen T.D. Roberts J.L. Wright A. Warner R.C. Holt J.W. Young N.W. le Meur E. Legresy B. Cavitte M. ICECAP team Published in: 2010 Category 3: Verbal presentation Program area: Ice, Ocean, Atmosphere and Climate
Blankenship D.D., Young D.A., Siegert M.J., van Ommen T.D., Roberts J.L., Wright A., Warner R.C., Holt J.W., Young N.W., le Meur E., Legresy B., Cavitte M., ICECAP team (2010) New constraints on the structure and dynamics of the East Antarctic Ice Sheet from the joint IPY/Ice Bridge ICECAP aerogeophysical projec, Abstract C22B-05 presented at 2010 Fall Meeting, AGU, San Francisco, Calif., 13-17 Dec. .;

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