Regional climate modeling using convection‐permitting models (CPMs; horizontal grid
spacing< 4 km) emerges as a promising framework to provide more reliable climate …

Even if anthropogenic warming were constrained to less than 2° C above pre-industrial, the
Greenland and Antarctic ice sheets will continue to lose mass this century, with rates similar …

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 …

Over the past 40 years Pine Island Glacier in West Antarctica has thinned at an accelerating
rate,,, so that at present it is the largest single contributor to sea-level rise in Antarctica. In …

This chapter considers changes in global mean sea level, regional sea level, sea level
extremes, and waves. Confidence in projections of global mean sea level rise has increased …

Antarctica's ice shelves modulate the grounded ice flow, and weakening of ice shelves due
to climate forcing will decrease their 'buttressing'effect, causing a response in the grounded …

We consider multiphysics applications from algorithmic and architectural perspectives,
where “algorithmic” includes both mathematical analysis and computational complexity, and …

The BRITICE‐CHRONO consortium of researchers undertook a dating programme to
constrain the timing of advance, maximum extent and retreat of the British–Irish Ice Sheet …

The sea level contribution of the Antarctic ice sheet constitutes a large uncertainty in future
sea level projections. Here we apply a linear response theory approach to 16 state-of-the-art …

While twentieth century sea-level rise was dominated by thermal expansion of ocean water,
mass loss from glaciers and ice sheets is now a larger annual contributor. There is …