Recent studies suggest that Antarctica has the potential to contribute up to~ 15 m of sea-
level rise over the next few centuries. The evolution of the Antarctic Ice Sheet is driven by a …

Abstract The Antarctic Ice Sheet (AIS) is out of equilibrium with the current anthropogenic‐
enhanced climate forcing. Paleoenvironmental records and ice sheet models reveal that the …

During the last glacial termination, the upwelling strength of the southern polar limb of the
Atlantic Meridional Overturning Circulation varied, changing the ventilation and stratification …

Reconstructing the growth and decay of palaeo-ice sheets is critical to understanding
mechanisms of global climate change and associated sea-level fluctuations in the past …

The geological record of landforms and sediments produced beneath deglaciating ice
sheets offers insights into inaccessible glacial processes. Large subglacial valleys formed …

A robust understanding of Antarctic Ice Sheet deglacial history since the Last Glacial
Maximum is important in order to constrain ice sheet and glacial-isostatic adjustment …

Studying the history of ice-sheet behaviour in the Ross Sea, Antarctica's largest drainage
basin can improve our understanding of patterns and controls on marine-based ice-sheet …

Reconstructing the historical behaviour of the Antarctic Ice Sheet is essential for
understanding and predicting climatic interactions, ice sheet sensitivities, and sea level …

Abstract The Parallel Ice Sheet Model (PISM) is applied to the Antarctic Ice Sheet over the
last two glacial cycles (≈ 210 000 years) with a resolution of 16 km. An ensemble of 256 …

This paper compiles and reviews marine and terrestrial data constraining the dimensions
and configuration of the Antarctic Peninsula Ice Sheet (APIS) from the Last Glacial Maximum …