Observations over the past decade show significant ice loss associated with the speed-up of
glaciers in southeast Greenland from 2003, followed by a deceleration from 2006. These …

The Greenland ice sheet is experiencing increasing rates of mass loss, the majority of which
results from changes in discharge from tidewater glaciers. Both atmospheric and ocean …

Recent changes in speed, thinning, and retreat rates of marine-terminating outlet glaciers
have raised concerns about the future stability of the Greenland Ice Sheet. Establishing a …

Past glacier fluctuations provide insight into glacier dynamics, climate change, and the
contribution of glaciers to sea-level rise. Here, the length fluctuations since the 19th century …

Marine-terminating outlet glaciers of the Greenland Ice Sheet have undergone substantial
changes over the past decade. The synchronicity of these changes suggest a regional …

A unique geographical configuration of glaciers exists in the Narsarsuaq district of South
Greenland. Two large outlet glaciers divide into seven distributaries, such that each glacier …

Widespread retreat of glaciers has been observed along the southeastern margin of
Greenland. This retreat has been associated with increased air and ocean temperatures …

To quantify recent thinning of marine-terminating outlet glaciers in northwestern Greenland,
we carried out field and satellite observations near the terminus of Bowdoin Glacier. These …

The Greenland ice sheet has been one of the largest contributors to global sea-level rise
over the past 20 years, accounting for 0.5 mm yr− 1 of a total of 3.2 mm yr− 1. A significant …

During the early 2000s the Greenland Ice Sheet experienced the largest ice-mass loss of the
instrumental record, largely as a result of the acceleration, thinning and retreat of large outlet …