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 …

Nearly every glacier in Greenland has thinned or retreated over the past few decades,,–,
leading to glacier acceleration, increased rates of sea-level rise and climate impacts around …

The freshwater budget of the Arctic and sub‐polar North Atlantic Oceans has been changing
due, primarily, to increased river runoff, declining sea ice and enhanced melting of Arctic …

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 …

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 …

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

Submarine melting of Greenlandic tidewater glacier termini is proposed as a possible
mechanism driving their recent thinning and retreat. We use a general circulation model …

Liquid freshwater fluxes from the Greenland ice sheet affect ocean water properties and
circulation on local, regional and basin-wide scales, with associated biosphere effects. The …

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 …