Glacial isostatic adjustment (GIA) describes the response of the solid Earth, the gravitational
field, and the oceans to the growth and decay of the global ice sheets. A commonly studied …

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 …

To predict the future contributions of the Antarctic ice sheets to sea-level rise, numerical
models use reconstructions of past ice-sheet retreat after the Last Glacial Maximum to tune …

Future sea-level rise generates hazards for coastal populations, economies, infrastructure,
and ecosystems around the world. The projection of future sea-level rise relies on an …

Recent studies suggest that Antarctica has the potential to contribute up to~ 15 m of sea-
level rise over the next few centuries. The evolution of the Antarctic Ice Sheet is driven by a …

Sea‐level rise sits at the frontier of usable climate climate change research, because it
involves natural and human systems with long lags, irreversible losses, and deep …

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 …

Geodetic, seismic, and geological evidence indicates that West Antarctica is underlain by
low-viscosity shallow mantle. Thus, as marine-based sectors of the West Antarctic Ice Sheet …

Simulations of the glacial–interglacial history of the Antarctic Ice Sheet provide insights into
dynamic threshold behavior and estimates of the ice sheet's contributions to global sea-level …