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 …

Ice loss from the Greenland ice sheet is one of the largest sources of contemporary sea-level
rise (SLR). While process-based models place timescales on Greenland's deglaciation, their …

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 …

Atmospheric warming is increasing surface melting across the Antarctic Peninsula, with
unknown impacts upon glacier dynamics at the ice-bed interface. Using high-resolution …

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 …

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 …

Intense rainfall events significantly affect Alpine and Alaskan glaciers through enhanced
melting, ice-flow acceleration and subglacial sediment erosion, yet their impact on the …

Reliable projections of ice sheets' future contributions to sea-level rise require models that
are able to accurately simulate grounding-line dynamics, starting from initial states …

Abstract Purpose of the Review This review discusses the role that meltwater plays within
the Greenland ice sheet system. The ice sheet's hydrology is important because it affects …