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LiveScience
LiveScience
Ben Turner

Warm ocean water is rushing beneath Antarctica's 'Doomsday Glacier,' making its collapse more likely

A 3D image showing the tidal flow beneath Thwaites Glacier.

Antarctica's "Doomsday Glacier" is melting significantly faster than scientists previously thought, thanks to warm ocean water that is infiltrating miles beneath its surface, a new study has found. 

The Thwaites Glacier, which is nicknamed the Doomsday Glacier because of its potential to massively increase sea levels, is located in West Antarctica and is roughly the size of Florida. 

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