Future projections of global mean sea level change are uncertain, partly because of our
limited understanding of the dynamics of Greenland's outlet glaciers. Here we study …

The spatiotemporal distribution and variability of surface water remained poorly known at the
pan-Greenland scale, and its dominant features (supraglacial rivers, lakes, and water-filled …

Subglacial hydrologic systems regulate ice sheet flow, causing acceleration or deceleration,
depending on hydraulic efficiency and the rate at which surface meltwater is delivered to the …

Semantic segmentation is a critical part of observation-driven research in glaciology. Using
remote sensing to quantify how features change (eg glacier termini, supraglacial lakes …

The evolution of crevasses on ice shelves plays a pivotal role in maintaining their stability.
Investigating the developmental pattern of crevasses on ice shelf surfaces necessitates long …

We present the first fully coupled 3D full-Stokes model of a tidewater glacier, incorporating
ice flow, subglacial hydrology, plume-induced frontal melting and calving. We apply the …

We investigate the physical basis of the crevasse-depth (CD) calving law by analysing
relationships between glaciological stresses and calving behaviour at Sermeq Kujalleq …

The surface melting of the Greenland ice sheet has been increasing over the last decades
due to Arctic atmospheric warming. Surface melt depends on the energy balance which …

Surface melt on the Greenland ice sheet has been increasing in intensity and extent over the
last decades due to Arctic atmospheric warming. Surface melt depends on the surface …

Herein, fast fracture initiation in glacier ice is modeled using a Material Point Method and a
simplified constitutive law describing tensile strain softening. Relying on a simple …