Over the past two decades, ice loss from the Greenland ice sheet (GrIS) has increased
owing to enhanced surface melting and ice discharge to the ocean,,,–. Whether continuing …

Below hard‐bedded glaciers, both basal friction and distributed subglacial drainage are
thought to be controlled by a network of cavities. Previous coupled hydro‐mechanical …

Glacier slip modulates sea-level rise. Most slip models assume quasi-equilibrium process
dynamics and debris-free basal ice, but observations regularly show debris-rich basal ice …

Ice speeds in Greenland are largely set by basal motion, which is modulated by meltwater
delivery to the ice base,–. Evidence suggests that increasing melt rates enhance the …

Deformation of subglacial sediment during basal slip shapes the beds of many fast‐flowing
glaciers and ice streams. The resultant sediment flux impacts glacier dynamics and rates of …

Glacier slip is usually described using steady-state sliding laws that relate drag, slip velocity
and effective pressure, but where subglacial conditions vary rapidly transient effects may …

Surface melt forces summertime ice‐flow accelerations on glaciers and ice sheets. Here, we
show that large meltwater‐forced accelerations also occur during wintertime in Greenland …

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 …

Viscous contact problems describe the time evolution of fluid flows in contact with a surface
from which they can detach and reattach. These problems are of particular importance in …

During the RESOLVE project (“High‐resolution imaging in subsurface geophysics:
development of a multi‐instrument platform for interdisciplinary research”), continuous …