According to a report published in Nature Communications,

roughly 55 gigatonnes of ice were lost via frontal ablation

from around 1,500 glaciers in the Northern Hemisphere between 2010 and 2022.

The findings imply that this mechanism has a larger effect on glacial mass loss than melt in some places,

which has consequences for monitoring sea-level rise

and identifying hotspot areas where this process occurs.

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