Buoyant plumes form when glacial ice melts directly into the ocean or when subglacial
meltwater is discharged to the ocean at depth. They play a key role in regulating heat …

Thermodynamic ablation of ice in contact with the ocean is an essential element of ice sheet
and ocean interactions but is challenging to model and quantify. Building on earlier …

Rapid ice loss from the Greenland ice sheet since 1992 is due in equal parts to increased
surface melting and accelerated ice flow. The latter is conventionally attributed to ocean …

Accelerated mass loss from the Greenland ice sheet leads to glacier retreat and an
increasing input of glacial meltwater to the fjords and coastal waters around Greenland …

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

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 …

Limited measurements along Greenland's remote coastline hamper quantification of the
sediment and associated nutrients draining the Greenland ice sheet, despite the potential …

Satellite‐based estimates of ice shelf melt rates reach 200 m close to the grounding line of
Pine Island Glacier, in West Antarctica. However, ocean simulations have not yet been able …

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 …

Abstract Changes in ocean temperature and salinity are expected to be an important
determinant of the Greenland ice sheet's future sea level contribution. Yet, simulating the …