Abstract Totten and Moscow University glaciers, in the marine‐based sector of East
Antarctica, contain enough ice to raise sea level by 5 m. Obtaining precise measurements of …

The deployment of seismic stations and the development of ambient noise tomography as
well as new analysis methods provide an opportunity for higher-resolution imaging of …

Rapid retreat of ice in the Amundsen Sea sector of West Antarctica may cause drastic sea
level rise, posing significant risks to populations in low-lying coastal regions. Calibration of …

The redistribution of past and present ice and ocean loading on Earth's surface causes solid
Earth deformation and geoid changes, known as glacial isostatic adjustment. The …

This study examines present-day changes of the Antarctic ice sheet (AIS) by means of
different data sets. We make use of monthly gravity field solutions acquired by the Gravity …

Filtering is a necessary step in the Gravity Recovery and Climate Experiment (GRACE) data
processing, but leads to signal leakage and attenuation obviously, and adversely affects the …

Many ice-sheet reconstructions assume monotonic Holocene retreat for the West Antarctic
Ice Sheet, but an increasing number of glaciological observations infer that some portions of …

The timing and impact of deglaciation and Holocene readvances on the terrestrial
continental margins of the Antarctic Peninsula (AP) have been well-studied but are still …

Abstract Glacial Isostatic Adjustment (GIA) models commonly assume a mantle with a
viscoelastic Maxwell rheology and a fixed ice history model. Here, we use a Bayesian Monte …

There has been considerable research in the literature focused on computing and
forecasting sea-level changes in terms of constant trends or rates. The Antarctic ice sheet is …