Slushy iceberg aggregates control calving timing on Greenland's Jakobshavn Isbræ

shows that a relaxation in the thick aggregate of icebergs floating at the glacier-ocean boundary of the Jakobshavn Isbræ occurs up to an hour before calving events. This finding may help scientists better understand future sea-level rise scenarios and could also help them predict when major episodes of calving are about to occur.