Iceberg calving accounts for half of the mass discharge from the Greenland and Antarctic ice
sheets, which has increased dramatically over the last two decades. Through their …

Mass loss from the Greenland ice sheet quadrupled over the past two decades, contributing
a quarter of the observed global sea-level rise. Increased submarine melting is thought to …

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 …

Ice shelf basal melting is the primary mechanism driving mass loss from the Antarctic Ice
Sheet, yet it is unknown how the localized melt enhancement from subglacial discharge will …

Rapid mass loss from the Greenland Ice Sheet has sparked interest in its glacial fjords for
two main reasons: Increased submarine melting of glaciers terminating in fjords is a …

Glacier change is ubiquitous, but the fastest and largest magnitude changes occur in
glaciers that terminate in water. This includes the most rapidly retreating glaciers, and also …

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 …

Glacier ice discharge, which depends on ice velocity and terminus fluctuations, is a primary
component of Greenland Ice Sheet mass loss. Some research suggests that ice mélange …

The discharge of nutrient-rich meltwater from the Greenland Ice Sheet has emerged as a
potentially important contributor to regional marine primary production and nutrient cycling …

The injection at depth of ice sheet runoff into fjords may be an important control on the frontal
melt rate of tidewater glaciers. Here we develop a new parameterization for ice marginal …