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• W2149606039 abstract "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." @default.
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• W2149606039 date "2015-11-10" @default.
• W2149606039 modified "2023-10-14" @default.
• W2149606039 title "Sea-level feedback lowers projections of future Antarctic Ice-Sheet mass loss" @default.
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• W2149606039 doi "https://doi.org/10.1038/ncomms9798" @default.
• W2149606039 hasPubMedCentralId "https://www.ncbi.nlm.nih.gov/pmc/articles/5426515" @default.
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