The last decade witnessed an explosion in yearly number of publications on passive glacier
seismology. The seismic signals from a wide range of glacier‐related processes fill a broad …

Recent observations of dynamic water systems beneath the Greenland and Antarctic ice
sheets have sparked renewed interest in modelling subglacial drainage. The foundations of …

Seasonal acceleration of the Greenland Ice Sheet is influenced by the dynamic response of
the subglacial hydrologic system to variability in meltwater delivery to the bed, via crevasses …

Observations indicate that groundwater-laden sedimentary aquifers are extensive beneath
large portions of the Greenland and Antarctic ice sheets. A reduction in the mechanical …

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 …

Ice sheets are currently ignored in global methane budgets,. Although ice sheets have been
proposed to contain large reserves of methane that may contribute to a rise in atmospheric …

Abstract The Greenland Ice Sheet is losing mass at an accelerating rate due to increased
surface melt and flow acceleration in outlet glaciers. Quantifying future dynamic …

Glacier-erosion rates range across orders of magnitude, and much of this variation cannot
be attributed to basal sliding rates. Subglacial till acts as lubricating 'fault gouge'or 'sawdust' …

Penetration of surface meltwater to the bed of the Greenland Ice Sheet each summer causes
an initial increase in ice speed due to elevated basal water pressure, followed by slowdown …

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 …