Accurate glacial isostatic adjustment (GIA) models are required for correcting measurements
of mass change in Antarctica and for improving knowledge of the sub‐surface, especially in …

We investigate present‐day bedrock vertical motion using new Global Positioning System
(GPS) timeseries from the Totten‐Denman glacier region of East Antarctica (∼ 77°–120° E) …

In this study we combine seismological and petrological models with satellite gravity
gradient data to obtain the thermal and compositional structure of the Antarctic lithosphere …

Calculating cosmogenic-nuclide surface-exposure ages is critically dependent on a
knowledge of the altitude of the sample site. Changes in altitude have occurred through time …

The measurement of ongoing ice-mass loss and associated melt water contribution to sea-
level change from regions such as West Antarctica is dependent on a combination of remote …

GNSS networks in Antarctica are a fundamental tool to define actual crustal displacements
due to geological and geophysical processes and to constrain the glacial isostatic models …

A major uncertainty in determining the mass balance of the Antarctic ice sheet from
measurements of satellite gravimetry, and to a lesser extent satellite altimetry, is the poorly …

The long wavelength part of the Earth's gravity field can be determined, with varying
accuracy, from satellite laser ranging (SLR). In this study, we investigate the combination of …

The interaction between ice-sheet growth and retreat and sea-level change has been an
established field of research for many years. However, recent advances in numerical …

We construct long-term time series of Greenland and Antarctic ice sheet mass change from
satellite gravity measurements. A statistical reconstruction approach is developed based on …