Results 31 to 40 of about 588,382 (370)
Rapid submarine ice melting in the grounding zones of ice shelves in West Antarctica. [PDF]
Enhanced submarine ice-shelf melting strongly controls ice loss in the Amundsen Sea embayment (ASE) of West Antarctica, but its magnitude is not well known in the critical grounding zones of the ASE's major glaciers.
Khazendar A +8 more
europepmc +3 more sources
Ocean-driven thinning enhances iceberg calving and retreat of Antarctic ice shelves [PDF]
John C Moore, Xiao Cheng
exaly +2 more sources
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
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
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
Widespread slowdown in thinning rates of West Antarctic ice shelves
. Antarctica's floating ice shelves modulate discharge of grounded ice into the ocean by providing a backstress. Ice shelf thinning and grounding line retreat have reduced this backstress, driving rapid drawdown of key unstable areas of the Antarctic Ice
F. Paolo +6 more
semanticscholar +1 more source
Ice shelves play an essential role in the dynamics of the Antarctic ice sheet. The surface meltwater is important, as it can irreversibly weaken ice shelves by exerting additional hydrostatic pressure.
Qi Zhu +6 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
Estimates of ice shelf mass loss are typically based on surface height measurements, assuming hydrostatic equilibrium and estimated firn thickness.
Allison M. Chartrand, I. Howat
semanticscholar +1 more source
Creep deformation and buttressing capacity of damaged ice shelves: theory and application to Larsen C ice shelf [PDF]
Around the perimeter of Antarctica, much of the ice sheet discharges to the ocean through floating ice shelves. The buttressing provided by ice shelves is critical for modulating the flux of ice into the ocean, and the presently observed thinning of
C. P. Borstad +3 more
doaj +1 more source

