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 …

Geomorphological map** is a well-established method for examining earth surface
processes and landscape evolution in a range of environmental contexts. In glacial …

This paper presents a comprehensive review and synthesis of ice streams in the Laurentide
Ice Sheet (LIS) based on a new map** inventory that includes previously hypothesised ice …

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 …

Antarctic volume changes during the past 21 thousand years are smaller than previously
thought, and here we construct an ice sheet history that drives a forward model prediction of …

Grounding-zone wedges (GZWs) are asymmetric sedimentary depocentres which form
through the rapid accumulation of glacigenic debris along a line-source at the grounding …

Onshore and offshore studies show that an expanded, grounded ice sheet occupied the
Ross Sea Embayment during the Last Glacial Maximum (LGM). Results from studies of till …

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 …

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 …