Abstract The East Antarctic Ice Sheet contains the vast majority of Earth's glacier ice (about
52 metres sea-level equivalent), but is often viewed as less vulnerable to global warming …

The variability of the Antarctic and Greenland ice sheets occurs on various timescales and is
important for projections of sea level rise; however, there are substantial uncertainties …

The land ice contribution to global mean sea level rise has not yet been predicted using ice
sheet and glacier models for the latest set of socio-economic scenarios, nor using …

Ocean-driven basal melting of Antarctica's floating ice shelves accounts for about half of
their mass loss in steady state, where gains in ice-shelf mass are balanced by losses. Ice …

Ice flow models of the Antarctic ice sheet are commonly used to simulate its future evolution
in response to different climate scenarios and inform on the mass loss that would contribute …

Antarctic ice shelves moderate the contribution of the Antarctic Ice Sheet to global sea level
rise; however, ice shelf health remains poorly constrained. Here, we present the annual …

Antarctica's ice shelves modulate the grounded ice flow, and weakening of ice shelves due
to climate forcing will decrease their 'buttressing'effect, causing a response in the grounded …

Projection of the contribution of ice sheets to sea-level change as part of the Coupled Model
Intercomparison Project–phase 6 (CMIP6) takes the form of simulations from coupled ice …

Observations of ocean-driven grounding-line retreat in the Amundsen Sea Embayment in
Antarctica raise the question of an imminent collapse of the West Antarctic Ice Sheet. Here …

Climate-forced, offline ice-sheet model simulations have been used extensively in assessing
how much ice-sheets can contribute to future global sea-level rise. Typically, these model …