Article ID Journal Published Year Pages File Type
4463720 Global and Planetary Change 2012 12 Pages PDF
Abstract

Abundant indirect evidence suggests that the West Antarctic Ice Sheet (WAIS) reduced in size during the Last Interglacial (LIG) compared to the Holocene. This study explores this possibility by comparing, for the first time, ice core stable isotope records for the LIG with output from a glacio-isostatic adjustment (GIA) model. The results show that ice core records from East Antarctica are remarkably insensitive to vertical movement of the solid land motion driven by a simulated hypothetical collapse of the WAIS. However, new and so far unexplored sites are identified which are sensitive to the isostatic signal associated with WAIS collapse and so ice core proxy data from these sites would be effective in testing this hypothesis further.

► The paper examines the impact of changes in surface elevation at Antarctica ice core data. ► Results are shown for ice models simulating a hypothetical West Antarctica collapse. ► Ice core data are insensitive to detecting changes in the West Antarctica Ice sheet. ► Treasure maps identify sites sensitive to detecting this simulated collapse.

Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Earth-Surface Processes
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