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 …

Ice sheet response to forced changes—such as that from anthropogenic climate forcing—is
closely regulated by two‐way interactions with other components of the Earth system. These …

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

Monitoring Antarctic icebergs helps us understand the interaction between ocean,
atmosphere, and sea ice in the Southern Ocean. Although gigantic icebergs have been the …

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 …

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 …

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 …

Ice sheet marine margins via outlet glaciers are susceptible to climate change and are
expected to respond through retreat, steepening, and acceleration, although with significant …

Fjords are conduits for heat and mass exchange between tidewater glaciers and the coastal
ocean, and thus regulate near‐glacier water properties and submarine melting of glaciers …

The speed of Greenland's fastest glacier, Jakobshavn Isbræ, has varied substantially since
its speed-up in the late 1990s. Here we present observations of surface velocity, mélange …