Modelling The Greenland Ice Sheet following The Mid-Eemian: A study of the impact of including lateral variations in the sub-Greenland Earth rheology on the GrIS' evolution since the mid-Eemian in a coupled 3D ice sheet and 3D GIA model

Uncertainty in ice sheet modelling affects centennial and longer time-scale projections of the Greenland Ice Sheet's (GrIS) sea level contribution. One source of this uncertainty is the interaction between the ice sheet’s evolution and the Earth’s deformation in response to changes in the applied surface loading as the ice sheet waxes and wanes....

A 3D Glacial Isostatic Adjustment model for Northwestern Europe

The Earth is subjected to 100,000 year cycles of glaciation and deglaciation. The deformations induced by glacial and oceanic loading and the continuous attempt at recovery of the isostatic equilibrium within the solid Earth, are referred to as Glacial Isostatic Adjustment (GIA). This process is ongoing still and yields a large contribution to...