Ocean-excited plate waves in the Ross and Pine Island Glacier ice shelves [PDF]
Ice shelves play an important role in buttressing land ice from reaching the sea, thus restraining the rate of grounded ice loss. Long-period gravity-wave impacts excite vibrations in ice shelves that can expand pre-existing fractures and trigger iceberg
ZHAO CHEN +6 more
doaj +4 more sources
Change in iceberg calving behavior preceded North Sea ice shelf disintegration during the last deglaciation [PDF]
Understanding how regime shifts in iceberg calving behavior affect ice shelf stability remains a challenge for numerical models. This is an important question as we consider the fate of the ice shelves that currently buttress the Antarctic Ice Sheet and ...
James D. Kirkham +15 more
doaj +2 more sources
Widespread movement of meltwater onto and across Antarctic ice shelves [PDF]
Surface meltwater drains across ice sheets, forming melt ponds that can trigger ice-shelf collapse acceleration of grounded ice flow and increased sea-level rise.
Bell, R.E. +3 more
core +2 more sources
Calving glaciers and ice shelves [PDF]
Calving, or the release of icebergs from glaciers and floating ice shelves, is an important process transferring mass into the world’s oceans. Calving glaciers and ice sheets make a large contribution to sea-level rise, but large uncertainty remains about future ice sheet response to alternative carbon scenarios.
Douglas I. Benn, Jan A. Åström
openaire +4 more sources
Change in Antarctic ice shelf area from 2009 to 2019 [PDF]
Antarctic ice shelves provide buttressing support to the ice sheet, stabilising the flow of grounded ice and its contribution to global sea levels. Over the past 50 years, satellite observations have shown ice shelves collapse, thin, and retreat; however,
J. R. Andreasen +3 more
doaj +1 more source
A stress-based poro-damage phase field model for hydrofracturing of creeping glaciers and ice shelves [PDF]
There is a need for computational models capable of predicting meltwater-assisted crevasse growth in glacial ice. Mass loss from glaciers and ice sheets is the largest contributor to sea-level rise and iceberg calving due to hydrofracture is one of the ...
Theo Clayton +3 more
semanticscholar +1 more source
Can rifts alter ocean dynamics beneath ice shelves? [PDF]
Land ice discharge from the Antarctic continent into the ocean is restrained by ice shelves, floating extensions of grounded ice that buttress the glacier outflow.
M. Poinelli +6 more
doaj +1 more source
Ice-shelf ocean boundary layer dynamics from large-eddy simulations [PDF]
Small-scale turbulent flow below ice shelves is regionally isolated and difficult to measure and simulate. Yet these small-scale processes, which regulate heat and salt transfer between the ocean and ice shelves, can affect sea-level rise by altering ...
C. B. Begeman +2 more
doaj +1 more source
A 15-year circum-Antarctic iceberg calving dataset derived from continuous satellite observations [PDF]
Iceberg calving is the main process that facilitates the dynamic mass loss of ice sheets into the ocean, which accounts for approximately half of the mass loss of the Antarctic ice sheet.
M. Qi +14 more
doaj +1 more source
The role of föhn winds in eastern Antarctic Peninsula rapid ice shelf collapse [PDF]
Ice shelf collapse reduces buttressing and enables grounded glaciers to contribute more rapidly to sea-level rise in a warming climate. The abrupt collapses of the Larsen A (1995) and B (2002) ice shelves on the Antarctic Peninsula (AP) occurred, at ...
M. K. Laffin +4 more
doaj +1 more source

