Abstract The Northeast Greenland Ice Stream (NEGIS) is the main artery for ice discharge
from the northeast sector of the Greenland Ice Sheet (GrIS) to the North Atlantic …

The dynamic mass loss of ice sheets constitutes one of the biggest uncertainties in
projections of ice-sheet evolution. One central, understudied aspect of ice flow is how the …

Only a few localised ice streams drain most of the ice from the Greenland Ice Sheet. Thus,
understanding ice stream behaviour and its temporal variability is crucially important to …

Ice-core records from the interior of the Greenland ice sheet suggest widespread thinning
during the Holocene. However, the recurring underestimation of this thinning in numerical …

Radio‐echo sounding (RES) shows large‐scale englacial stratigraphic folds are ubiquitous
in Greenland's ice sheet. However, there is no consensus yet on how these folds form. Here …

Fabrics, also known as textures or crystallographic preferred orientations, reveal information
about the deformation history of the flow of polycrystalline materials, including glacial ice …

Radio-echo sounding (RES) reveals patches of high backscatter in basal ice units, which
represent distinct englacial features in the bottom parts of glaciers and ice sheets. Their …

The Greenland Ice Sheet is a large contributor to global sea-level rise, and current mass
losses are projected to accelerate. However, model projections of future ice-sheet evolution …

Abstract The Greenland Ice Sheet covers an area of 1.7 million km 2, equivalent to∼ 79% of
the surface of Kalaallit Nunaat (Greenland) and∼ 1.2% of the Earth's land surface. The …

Greenland's glaciers have been retreating, thinning and accelerating since the mid-1990s,
with the mass loss from the Greenland Ice Sheet (GrIS) now being the largest contributor to …