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Antarctic basal environment shaped by high-pressure flow through a subglacial river system - Nature Geoscience

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Antarctic basal environment shaped by high-pressure flow through a subglacial river system - Nature Geoscience

The stability of ice sheets and their contributions to sea level are modulated by high-pressure water that lubricates the base of the ice, facilitating rapid flow into the ocean. In Antarctica, subglacial processes are poorly characterized, limiting understanding of ice-sheet flow and its sensitivity to climate forcing.

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Antarctic basal environment shaped by high-pressure flow through a subglacial river system - Nature Geoscience

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Antarctic basal environment shaped by high-pressure flow through a subglacial river system - Nature Geoscience

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