Sea ice feedback and Cenozoic evolution of Antarctic climate and ice sheets

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Antarctic topography at the Eocene–Oligocene boundary (2012, background): “This is important because experiments to test the sensitivity of ice sheet growth at this time have thus far relied upon the present day subglacial bedrock topography, rebounded for removal of ice load, as a boundary condition (DeConto and Pollard, 2003; DeConto et al., 2007, 2008).”