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- W4306160416 abstract "The flow speed of the Greenland Ice Sheet changes dramatically in inland regions when surface meltwater drains to the bed. But ice-sheet discharge to the ocean is dominated by fast-flowing outlet glaciers, where the effect of increasing surface melt on annual discharge is unknown. Observations of a supraglacial lake drainage at Helheim Glacier, and a consequent velocity pulse propagating down-glacier, provide a natural experiment for assessing the impact of changes in injected meltwater, and allow us to interrogate the subglacial hydrological system. We find a highly efficient subglacial drainage system, such that summertime lake drainage has little net effect on ice discharge. Our results question the validity of common remote-sensing approaches for inferring subglacial conditions, knowledge of which is needed for improved projections of sea-level rise." @default.
- W4306160416 created "2022-10-14" @default.
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- W4306160416 date "2022-10-14" @default.
- W4306160416 modified "2023-10-17" @default.
- W4306160416 title "Tidewater-glacier response to supraglacial lake drainage" @default.
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- W4306160416 doi "https://doi.org/10.1038/s41467-022-33763-2" @default.
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- W4306160416 hasPublicationYear "2022" @default.
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