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• W2037998918 abstract "Our poor understanding of tidewater glacier dynamics remains the primary source of uncertainty in sea level rise projections. On the ice sheets, mass lost from tidewater calving exceeds the amount lost from surface melting. In Alaska, the magnitude of calving mass loss remains unconstrained, yet immense calving losses have been observed. With 20% of the global new-water sea level rise coming from Alaska, partitioning of mass loss sources in Alaska is needed to improve sea level rise projections. Here we present the first regionally comprehensive map of glacier flow velocities in Central Alaska. These data reveal that the majority of the regional downstream flux is constrained to only a few coastal glaciers. We find regional calving losses are 17.1 Gt a−1, which is equivalent to 36% of the total annual mass change throughout Central Alaska. Alaskan mountain glaciers are losing ice and contribute to sea level rise, but contributions from specific ice-loss mechanisms are not known. Here, calving losses in Central Alaska are found to equal 36% of the net regional mass change each year and regional flux is dictated largely by snow accumulation rates." @default.
• W2037998918 created "2016-06-24" @default.
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• W2037998918 date "2013-07-16" @default.
• W2037998918 modified "2023-10-14" @default.
• W2037998918 title "Flow velocities of Alaskan glaciers" @default.
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• W2037998918 doi "https://doi.org/10.1038/ncomms3146" @default.
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• W2037998918 hasPublicationYear "2013" @default.
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