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 …

Abstract The Paris Agreement aims to limit global mean warming in the twenty-first century to
less than 2 degrees Celsius above preindustrial levels, and to promote further efforts to limit …

We discuss the emerging advances and opportunities at the intersection of machine
learning (ML) and climate physics, highlighting the use of ML techniques, including …

Cryospheric responses to climate warming include glacier retreat, altitude‐dependent
thermal instability, and abundant meltwater, which increase the frequency of catastrophic …

The disintegration of the ice shelves along the Antarctic Peninsula have spurred much
discussion on the various processes leading to their eventual dramatic collapse, but without …

It has been argued that the− 5° C annual mean 2 m air temperature isotherm defines a limit
of ice shelf viability on the Antarctic Peninsula as melt ponding increases at higher …

The variability of the Antarctic and Greenland ice sheets occurs on various timescales and is
important for projections of sea level rise; however, there are substantial uncertainties …

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 …