We present a new reconstruction of the Antarctic Ice Sheets between 20 ka BP and the
present day. Our reconstruction is derived using a numerical model to generate a physically …

We review and synthesize the geologic record that constrains the sources of sea level rise
and freshwater discharge to the global oceans associated with retreat of ice sheets during …

We combined an ensemble of satellite altimetry, interferometry, and gravimetry data sets
using common geographical regions, time intervals, and models of surface mass balance …

Antarctic volume changes during the past 21 thousand years are smaller than previously
thought, and here we construct an ice sheet history that drives a forward model prediction of …

A robust understanding of Antarctic Ice Sheet deglacial history since the Last Glacial
Maximum is important in order to constrain ice sheet and glacial-isostatic adjustment …

Reconstructing the historical behaviour of the Antarctic Ice Sheet is essential for
understanding and predicting climatic interactions, ice sheet sensitivities, and sea level …

Retreat of the Last Glacial Maximum (LGM) Antarctic ice sheet is thought to have been
initiated by changes in ocean heat and eustatic sea level propagated from the Northern …

Bedrock uplift in Antarctica is dominated by a combination of glacial isostatic adjustment
(GIA) and elastic response to contemporary mass change. Here, we present spatially …

Dynamical changes in contemporary ice sheets account for significant proportions of their
current rates of mass loss, but assessing whether or not these processes are a natural part …

Abstract The Weddell Sea sector is one of the main formation sites for Antarctic Bottom
Water and an outlet for about one fifth of Antarctica's continental ice volume. Over the last …