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 …

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 …

Sea-level rise may accelerate significantly if marine ice sheets become unstable. If such
instability occurs, there would be considerable uncertainty in future sea-level rise projections …

Abstract Wilkes Land and Totten Glacier (TG) in East Antarctica (EA) have been losing ice
mass significantly since 1989. There is a lack of knowledge of long-term mass balance in the …

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 …

Oceanic melting beneath ice shelves is the main driver of the current mass loss of the
Antarctic ice sheet and is mostly parameterised in stand-alone ice-sheet modelling …

The Totten ice shelf (TIS) in East Antarctica has received increasing attention in recent years
due to high basal melt rates, which have been linked to a presence of warm modified …

Subglacial freshwater discharge from beneath Antarctic glaciers likely has a strong impact
on ice shelf basal melting. However, the difficulty in directly observing subglacial flow …

Recent studies have revealed the presence of a complex freshwater system underlying the
Aurora Subglacial Basin (ASB), a region of East Antarctica that contains∼ 7 m of global sea …

Totten Glacier (TG), the primary ice discharger of East Antarctica, contains 3.85 m sea level
rise equivalent (SLRe) ice mass and has displayed ocean‐driven dynamic change since at …