Over the past quarter of a century the Arctic has warmed more than any other region on
Earth, causing a profound impact on the Greenland ice sheet (GrIS) and its contribution to …

The Greenland ice sheet is one of the largest contributors to global mean sea-level rise
today and is expected to continue to lose mass as the Arctic continues to warm. The two …

Antarctica's ice shelves modulate the grounded ice flow, and weakening of ice shelves due
to climate forcing will decrease their 'buttressing'effect, causing a response in the grounded …

The European Alps, the cradle of pioneering glacial studies, are one of the regions where
geological markers of past glaciations are most abundant and well-studied. Such conditions …

Abstract Purpose of Review This paper reviews the recent literature on numerical modelling
of the dynamics of the Greenland ice sheet with the goal of providing an overview of …

The Fourth IPCC Assessment Report concluded that ice sheet flow models, in their current
state, were unable to provide accurate forecast for the increase of polar ice sheet discharge …

Accurately projecting mass loss from ice sheets is of critical societal importance. However,
despite recent improvements in ice sheet models, our analysis of a recent effort to project ice …

The basal thermal state of an ice sheet (frozen or thawed) is an important control upon its
evolution, dynamics, and response to external forcings. However, this state can only be …

Ice sheet numerical modeling is an important tool to estimate the dynamic contribution of the
Antarctic ice sheet to sea level rise over the coming centuries. The influence of initial …

Several decades of ice‐penetrating radar surveys of the Greenland and Antarctic ice sheets
have observed numerous widespread internal reflections. Analysis of this radiostratigraphy …