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Recent irreversible retreat phase of Pine Island Glacier - Nature Climate Change

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Recent irreversible retreat phase of Pine Island Glacier - Nature Climate Change

Pine Island Glacier (PIG), a part of the West Antarctic marine ice sheet, has recently undergone substantial changes including speed up, retreat and thinning. Theoretical arguments and modelling work suggest that marine ice sheets can become unstable and undergo irreversible retreat. Here, we use an ice-flow model validated by observational data to show that a rapid PIG retreat in the 1970s from a subglacial ridge to an upstream ice plain was self-enhancing and irreversible.

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Recent irreversible retreat phase of Pine Island Glacier - Nature Climate Change

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Recent irreversible retreat phase of Pine Island Glacier - Nature Climate Change

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