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The tipping point that melts large ice sheets, findings by BAS scientists

The region beneath an ice sheet where the ground-based ice meets the sea is known as the grounding zone. A new and worrying way that large ice sheets can melt has been characterized by scientists for the first time. The research focuses on how relatively warm seawater can lap at the underside of ground-based ice, which can accelerate the movement of the ice into the ocean.

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