The Antarctic mantle and lithosphere are known to have large lateral contrasts in seismic
velocity and tectonic history. These contrasts suggest differences in the response timescale …

The Antarctic ice sheet has the potential to make a significant contribution to future sea-level
rise. Understanding this potential and making projections of future ice sheet mass change …

We present regional-scale mass balances for 25 drainage basins of the Antarctic Ice Sheet
(AIS) from satellite observations of the Gravity and Climate Experiment (GRACE) for time …

We review the two main approaches to estimating sea level rise over the coming century:
physically plausible models of reduced complexity that exploit statistical relationships …

Relative sea-level variations during the late Pleistocene can only be reconstructed with the
knowledge of ice-sheet history. On the other hand, the knowledge of regional and global …

In this work we assess the most recent estimates of glacial isostatic adjustment (GIA) for
Antarctica, including those from both forward and inverse methods. The assessment is …

Previous GRACE-derived ice mass trends and accelerations have almost entirely been
based on an assumption that the residuals to a regression model (including also semi …

Antarctic surface mass balance (SMB) is largely determined by precipitation over the
continent and subject to regional climate variability related to the Southern Annular Mode …

The land surface beneath the Greenland and Antarctic Ice Sheets is isostatically suppressed
by the mass of the overlying ice. Accurate computation of the land elevation in the absence …

Differences in predictions of Glacial Isostatic Adjustment (GIA) for Antarctica persist due to
uncertainties in deglacial history and Earth rheology. The Earth models adopted in many …