Not exact matches
The
glacier is currently experiencing
significant acceleration, thinning and retreat that is thought to be caused by «ocean - driven» melting; an increase in warm ocean water finding its way under the ice shelf.
A similar behaviour might be occurring on the Amundsen Sea sector of the west Antarctic Ice Sheet (WAIS), where Pine Island and Thwaites
glaciers have lost
significant portions of their fringing ice shelves, and show signs of recent
acceleration.
This suggests that glacial ice
acceleration due to changes in seasonal meltwater flux tend to not make a
significant overall change in outlet
glacier ice velocities.
Pine Island and Thwaites
glaciers have experienced
significant flow
acceleration since the 1970s.