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Observations of grounding zones are the missing key to understand ice melt in Antarctica

Ice melt processes that take place at the ice–ocean boundary of Greenland and Antarctic glaciers play a pivotal role in their evolution and contribution to sea-level rise, but widespread observations in these regions are lacking. A major observational initiative will be necessary to drastically reduce uncertainties in projections and better prepare society for sea-level rise.

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Fig. 1: Observations of ice-shelf cavities required to understand ice melt.
Fig. 2: Getz Ice Shelf in West Antarctica, photographed by NASA Operation IceBridge in 2018.

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Correspondence to Eric Rignot.

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Rignot, E. Observations of grounding zones are the missing key to understand ice melt in Antarctica. Nat. Clim. Chang. 13, 1010–1013 (2023). https://doi.org/10.1038/s41558-023-01819-w

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