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 …

Over the modern satellite era, substantial climatic changes have been observed in the
Antarctic, including atmospheric and oceanic warming, ice sheet thinning and a general …

Ocean-driven melting of floating ice-shelves in the Amundsen Sea is currently the main
process controlling Antarctica's contribution to sea-level rise. Using a regional ocean model …

Antarctica's ice shelves help to control the flow of glacial ice as it drains into the ocean,
meaning that the rate of global sea-level rise is subject to the structural integrity of these …

Quantifying changes in Earth's ice sheets and identifying the climate drivers are central to
improving sea level projections. We provide unified estimates of grounded and floating ice …

Tip** elements are components of the Earth system which may respond nonlinearly to
anthropogenic climate change by transitioning toward substantially different long‐term …

The Antarctic Ice Sheet is losing mass at an accelerating pace, and ice loss will likely
continue over the coming decades and centuries. Some regions of the ice sheet may reach …

The future surface mass balance (SMB) of Antarctic ice shelves has not been constrained
with models of sufficient resolution and complexity. Here, we force the high‐resolution …

Mass loss from the West Antarctic Ice Sheet is dominated by glaciers draining into the
Amundsen Sea Embayment (ASE), yet the impact of anomalous precipitation on the mass …

There is increasing evidence that fossil-fuel burning, and consequential global heating of
1.1° C to date, has led to the increased occurrence and severity of extreme environmental …