Recent advances in both ocean modeling and melt parameterization in ice-sheet models
point the way toward coupled ice sheet–ocean modeling, which is needed to quantify …

Numerical modeling of the Antarctic ice sheet has gone through a paradigm shift over the
last decade. While initially models focussed on long-time diffusive response to surface mass …

Basal melting of Antarctic ice shelves is expected to increase during the twenty-first century
as the ocean warms, which will have consequences for ice sheet stability and global sea …

Warm waters flood the continental shelf of the Amundsen and Bellingshausen seas in West
Antarctica, driving rapid basal melt of ice shelves. In contrast, waters on the continental shelf …

The largest regional drivers of current surface elevation increases in the Antarctic Ice Sheet
are associated with ice flow reconfiguration in previously active ice streams, highlighting the …

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 …

A large volume of the East Antarctic Ice Sheet drains through the Totten Glacier (TG) and is
thought to be a potential source of substantial global sea-level rise over the coming …

Recent warm atmospheric conditions have damaged the ice shelves of the Antarctic
Peninsula through surface melt and hydrofracturing, and could potentially initiate future …

The Marine Ice Sheet Instability (MISI) is a dynamic feedback that can cause an ice sheet to
enter a runaway collapse. Thwaites Glacier, West Antarctica, is projected to be the largest …

Long-range airborne geophysical measurements were carried out in the ICEGRAV
campaigns, covering hitherto unexplored parts of interior East Antarctica and part of the …