Rapid mass loss from the Greenland Ice Sheet has sparked interest in its glacial fjords for
two main reasons: Increased submarine melting of glaciers terminating in fjords is a …

Glacier change is ubiquitous, but the fastest and largest magnitude changes occur in
glaciers that terminate in water. This includes the most rapidly retreating glaciers, and also …

This study presents the application of a cost-effective, unmanned aerial vehicle (UAV) to
investigate calving dynamics at a major marine-terminating outlet glacier draining the …

X‐ray fluorescence (XRF) core scanning and X‐ray computed tomography data were
measured every 1 mm to study the structure of Heinrich Event 1 during the last deglaciation …

We present a 1986 through March 2020 estimate of Greenland Ice Sheet ice discharge. Our
data include all discharging ice that flows faster than 100 m yr-1 and are generated through …

We discuss Greenland Ice Sheet (GrIS) surface mass balance (SMB) differences between
the updated polar version of the RACMO climate model (RACMO2. 3) and the previous …

This study presents a data set of daily, 1 km resolution Greenland ice sheet (GrIS) surface
mass balance (SMB) covering the period 1958–2015. Applying corrections for elevation …

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 …

Grounding-zone wedges (GZWs) are asymmetric sedimentary depocentres which form
through the rapid accumulation of glacigenic debris along a line-source at the grounding …

Mass loss from the Greenland ice sheet (GrIS) has increased over the last two decades in
response to changes in global climate, motivating the scientific community to question how …