Freshwater discharge from glaciers is increasing across the Arctic in response to
anthropogenic climate change, which raises questions about the potential downstream …

The role of icebergs in narrow fjords hosting marine-terminating glaciers in Greenland is
poorly understood, even though iceberg melt results in a substantial freshwater flux that can …

At tidewater glacier termini, ocean‐glacier interactions hinge on two sources of freshwater—
submarine melt and subglacial discharge—yet these freshwater fluxes are often …

Fjord dynamics influence oceanic heat flux to the Greenland ice sheet. Submarine iceberg
melting releases large volumes of freshwater within Greenland's fjords, yet its impact on fjord …

Greenland's glacial fjords are a key bottleneck in the earth system, regulating exchange of
heat, freshwater and nutrients between the ice sheet and ocean and hosting societally …

Subglacial freshwater discharge from beneath Antarctic glaciers likely has a strong impact
on ice shelf basal melting. However, the difficulty in directly observing subglacial flow …

Surface‐derived meltwater can access the bed of the Greenland ice sheet, causing
seasonal velocity variations. The magnitude, timing, and net impact on annual average ice …

Quantifying the impact of submarine melting on calving is central to understanding the
response of marine‐terminating glaciers to ocean forcing. Modeling and observational …

Marine-terminating glaciers lose mass through melting and iceberg calving, and we find that
meltwater drainage systems influence calving timing at Helheim Glacier, a tidewater glacier …

Meltwater from Greenland is an important freshwater source for the North Atlantic Ocean,
released into the ocean at the head of fjords in the form of runoff, submarine melt, and …