Abstract Purpose of Review Assessment of the impact of ocean resolution in Earth System
models on the mean state, variability, and future projections and discussion of prospects for …

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 …

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

Abstract Runoff from the Greenland Ice Sheet (GrIS) is thought to enhance marine
productivity by adding bioessential iron and silicic acid to coastal waters. However …

Jakobshavn Isbrae has been the single largest source of mass loss from the Greenland Ice
Sheet over the last 20 years. During that time, it has been retreating, accelerating and …

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 …

Glaciers in the Arctic have lost considerable mass during the last two decades. About a third
of the glaciers by area drains into the ocean, yet the mechanisms and drivers governing …

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 impact of these …

Subglacial hydrology is a leading control on basal friction and the dynamics of glaciers and
ice sheets. At low discharge, subglacial water flows through high-pressure, sheet-like …

Recent acceleration of Greenland's ocean‐terminating glaciers has substantially amplified
the ice sheet's contribution to global sea level. Increased oceanic melting of these tidewater …