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Sea-level feedback lowers projections of future Antarctic Ice-Sheet mass loss
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2015
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Source: Nat Commun. 2015; 6: 8798.
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Journal Title:Nature Communications
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Description:The stability of marine sectors of the Antarctic Ice Sheet (AIS) in a warming climate has been identified as the largest source of uncertainty in projections of future sea-level rise. Sea-level fall near the grounding line of a retreating marine ice sheet has a stabilizing influence on the ice sheets, and previous studies have established the importance of this feedback on ice age AIS evolution. Here we use a coupled ice sheet–sea-level model to investigate the impact of the feedback mechanism on future AIS retreat over centennial and millennial timescales for a range of emission scenarios. We show that the combination of bedrock uplift and sea-surface drop associated with ice-sheet retreat significantly reduces AIS mass loss relative to a simulation without these effects included. Sensitivity analyses show that the stabilization tends to be greatest for lower emission scenarios and Earth models characterized by a thin elastic lithosphere and low-viscosity upper mantle, as is the case for West Antarctica.
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Source:Nat Commun. 2015; 6: 8798.
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DOI:
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Pubmed ID:26554381
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Pubmed Central ID:PMC5426515
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Rights Information:CC BY
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Compliance:PMC
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