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Our in-situ measurements confirm meltwater-driven acceleration of grounded ice in Antarctica.
https://doi.org/10.1038/s41467-026-72724-x
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Meltwater-driven acceleration through elevated basal water pressure is known from mountain glaciers and Greenland, but direct observations beneath grounded Antarctic ice are sparse. This sentence claims that link for Langhovde Glacier, based on borehole pressure and GNSS speed and uplift. The evidence comes from one site in one summer, and pressure was recorded for only one of the two speed-up events. With more melt expected along the Antarctic coast, how general this is matters.
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Anne Fouilloux
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2026-10-09T08:22:44.913Z
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Paper annotation: Our in-situ measurements confirm meltwater-driven acceleration of grounded ice in Antarctica.
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