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 …

Glacial isostatic adjustment (GIA) encompasses a suite of geophysical phenomena
accompanying the waxing and waning of continental-scale ice sheets. These involve the …

The provision of accurate models of Glacial Isostatic Adjustment (GIA) is presently a priority
need in climate studies, largely due to the potential of the Gravity Recovery and Climate …

By far the most prescient insights into the interior structure of the planet have been provided
on the basis of elastic wave seismology. Analysis of the travel times of shear or compression …

The recent release of the next‐generation global ice history model, ICE6G_C (VM5a), is
likely to be of interest to a wide range of disciplines including oceanography (sea level …

We present SELEN 4 (SealEveL EquatioN solver), an open-source program written in
Fortran 90 that simulates the glacial isostatic adjustment (GIA) process in response to the …

The most recently published model of the glacial isostatic adjustment process in the ICE‐NG
(VMX) sequence from the University of Toronto, denoted ICE‐6G_C (VM5a), was originally …

The study of glacial isostatic adjustment (GIA) is gaining an increasingly important role
within the geophysical community. Understanding the response of the Earth to loading is …

We present a glacial isostatic adjustment (GIA) model for Antarctica. This is driven by a new
deglaciation history that has been developed using a numerical ice-sheet model, and is …

Fennoscandia is the key area for glacial isostatic adjustment (GIA) research. Owing to its
long settlement and excellent infrastructure, ongoing land uplift in the north as well as …