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 …

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 …

Ice flow models of the Antarctic ice sheet are commonly used to simulate its future evolution
in response to different climate scenarios and inform on the mass loss that would contribute …

Abstract The Southern Ocean has warmed substantially, and up to early 21st century,
Antarctic stratospheric ozone depletion and increasing atmospheric CO 2 have conspired to …

Global sea level provides an important indicator of the state of the warming climate, but
changes in regional sea level are most relevant for coastal communities around the world …

The response of the Antarctic Ice Sheet (AIS) to climate change is the largest uncertainty in
projecting future sea level. The impact of three-dimensional (3D) Earth structure on the AIS …

Abstract The Antarctic Ice Sheet (AIS) is out of equilibrium with the current anthropogenic‐
enhanced climate forcing. Paleoenvironmental records and ice sheet models reveal that the …

The rate and magnitude of the Antarctic Ice Sheet (AIS) contribution to global sea-level rise
beyond 2100 ce remains highly uncertain. Past changes of the AIS, however, offer …

Sea level rise (SLR) is a long‐lasting consequence of climate change because global
anthropogenic warming takes centuries to millennia to equilibrate for the deep ocean and …