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 …

Recent observations show that the rate at which the Antarctic ice sheet (AIS) is contributing
to sea level rise is increasing. Increases in ice‐ocean heat exchange have the potential to …

Antarctic ice shelves moderate the contribution of the Antarctic Ice Sheet to global sea level
rise; however, ice shelf health remains poorly constrained. Here, we present the annual …

Despite widespread efforts to implement climate services, there is almost no literature that
systematically analyzes users' needs. This paper addresses this gap by applying a decision …

Observations of ocean-driven grounding-line retreat in the Amundsen Sea Embayment in
Antarctica raise the question of an imminent collapse of the West Antarctic Ice Sheet. Here …

Mass loss from the Greenland ice sheet (GrIS) has increased over the last two decades in
response to changes in global climate, motivating the scientific community to question how …

Mass loss from the Antarctic Ice Sheet is the main source of uncertainty in projections of
future sea-level rise, with important implications for coastal regions worldwide. Central to …

Accurate representation of the viscous flow of ice is fundamental to understanding glacier
dynamics and projecting sea-level rise. Ice viscosity is often described by a simple but …

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 …

Reliable projections of ice sheets' future contributions to sea-level rise require models that
are able to accurately simulate grounding-line dynamics, starting from initial states …