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A new study suggests that the East Antarctica Ice Sheet in the Wilkes Basin may have completely disappeared around 400,000 years ago. Currently the Wilkes Basin is only hold back by the Cook, Mertz, and the Ninnis Glacier – the Cook Glacier shelf has already collapsed. There is also the Totten Glacier farther to the east, part of the Aurora Basin, also prone to warmer water at the grounding line, elevation has changed, though the topography is not favorable for rapid retreat in this case. Nevertheless, observations remain scarce, and the Wilkes Basin ice sheet may be the real elephant in the room.

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