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Craig Stevens, Professor in Ocean Physics, University of Auckland, Waipapa Taumata Rau; Earth Sciences New Zealand

Antarctica’s ice shelves are vulnerable to melting from below – knowing how far ocean heat reaches is crucial

Craig Stevens, CC BY-SA

A rare dataset collected by instruments at the point where Antarctica’s largest ice shelf begins to float reveals ocean processes that drive melting at this critical part of the continent.

During a 2019 expedition to the Kamb Ice Stream, a river of ice which feeds the Ross Ice Shelf, we were able to deploy a string of hydrographic instruments into a thin wedge of ocean beneath the shelf where it begins to lift off at a latitude of nearly 83 degrees South.

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