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 …

Abstract In the Northern Hemisphere, an insolation driven Early to Middle Holocene Thermal
Maximum was followed by a Neoglacial cooling that culminated during the Little Ice Age …

The response of the Greenland Ice Sheet (GIS) to changes in temperature during the
twentieth century remains contentious, largely owing to difficulties in estimating the spatial …

Abstract Changes in ocean temperature and salinity are expected to be an important
determinant of the Greenland ice sheet's future sea level contribution. Yet, simulating the …

Accurate quantification of the millennial-scale mass balance of the Greenland ice sheet
(GrIS) and its contribution to global sea-level rise remain challenging because of sparse in …

Submarine melting of Greenlandic tidewater glacier termini is proposed as a possible
mechanism driving their recent thinning and retreat. We use a general circulation model …

Abstract The Greenland Ice Sheet is the largest land ice contributor to sea level rise. This will
continue in the future but at an uncertain rate and observational estimates are limited to the …

Abstract The Greenland Ice Sheet discharges ice to the ocean through hundreds of outlet
glaciers. Recent acceleration of Greenland outlet glaciers has been linked to both oceanic …

Abstract Digital Elevation Models (DEMs) play a prominent role in glaciological studies for
the mass balance of glaciers and ice sheets. By providing a time snapshot of glacier …

The effect of the North Atlantic Ocean on the Greenland Ice Sheet through submarine
melting of Greenland's tidewater glacier calving fronts is thought to be a key driver of …