Constraining how much and how fast the West Antarctic Ice Sheet (WAIS) will change in the
coming decades has recently been identified as the highest priority in Antarctic research …

Over recent decades outlet glaciers of the Amundsen Sea Embayment (ASE), West
Antarctica, have accelerated, thinned, and retreated, and are now contributing …

We use updated drainage inventory, ice thickness, and ice velocity data to calculate the
grounding line ice discharge of 176 basins draining the Antarctic Ice Sheet from 1979 to …

Accurate prediction of global sea-level rise requires that we understand the cause of recent,
widespread and intensifying, glacier acceleration along Antarctic ice-sheet coastal margins …

Mass loss from the Amundsen Sea sector of the West Antarctic Ice Sheet has increased in
recent decades, suggestive of sustained ocean forcing or an ongoing, possibly unstable …

Pine Island Glacier has thinned and accelerated over recent decades, significantly
contributing to global sea-level rise. Increased oceanic melting of its ice shelf is thought to …

Upwelling of global deep waters to the sea surface in the Southern Ocean closes the global
overturning circulation and is fundamentally important for oceanic uptake of carbon and …

Mass loss from the Antarctic Ice Sheet is driven by changes at the marine margins. In the
Amundsen Sea, thinning of the ice shelves has allowed the outlet glaciers to accelerate and …

The southern hemisphere westerly winds have been strengthening and shifting poleward
since the 1950s. This wind trend is projected to persist under continued anthropogenic …

Satellite observations over the past two decades have revealed increasing loss of grounded
ice in West Antarctica, associated with floating ice shelves that have been thinning. Thinning …