Greenland's bed topography is a primary control on ice flow, grounding line migration,
calving dynamics, and subglacial drainage. Moreover, fjord bathymetry regulates the …

Greenland runoff, from ice mass loss and increasing rainfall, is increasing. That runoff, as
discharge, impacts the physical, chemical, and biological properties of the adjacent fjords …

Supraglacial lakes on the Greenland Ice Sheet are expanding inland, but the impact on ice
flow is equivocal because interior surface conditions may preclude the transfer of surface …

Meltwater drainage across the surface of the Greenland ice sheet (GrIS) is well constrained
by measurements and modeling, yet despite its critical role, knowledge of its transit through …

The rapid drainage of supraglacial lakes injects substantial volumes of water to the bed of
the Greenland ice sheet over short timescales. The effect of these water pulses on the …

Subglacial hydrological processes at tidewater glaciers remain poorly understood due to the
difficulty in obtaining direct measurements and lack of empirical verification for modelling …

The land-terminating margin of the Greenland Ice Sheet has slowed down in recent
decades, although the causes and implications for future ice flow are unclear. Explained …

On the Greenland Ice Sheet (GrIS), ice flow due to deformation and sliding across the bed
delivers ice to lower-elevation marginal regions where it can melt. We measured the two …

The gradient of the hydraulic potential field at the ice‐bedrock interface beneath the
Greenland Ice Sheet (GrIS) dictates the routing and energetics of subglacial water, thereby …

The subglacial hydrological system critically controls ice motion at the margins of the
Greenland Ice Sheet. However, over multi-annual timescales, the net impact of hydro …