Abstract The Arctic Ocean is a fundamental node in the global hydrological cycle and the
ocean's thermohaline circulation. We here assess the system's key functions and …

Monitoring the surface circulation of the ice-covered Arctic Ocean is generally limited in
space, time or both. We present a new 12-year record of geostrophic currents at monthly …

The meridional overturning circulation (MOC) decreases rapidly in subpolar and Nordic
regions where the warm upper layer loses its buoyancy due to intense heat loss, sinks, and …

We present measurements from two shipboard surveys conducted in summer 2012 that
sampled the rim current system around the Nordic Seas from Fram Strait to Denmark Strait …

The cumulative Greenland freshwater flux anomaly has exceeded 5,000 km3 since the
1990s. The volume of this surplus freshwater is expected to cause substantial freshening in …

Abstract The Riverine Coastal Domain (RCD) is a narrow (∼< 15 km), shallow (∼ 10 m)
contiguous feature that is primarily forced driven by an aggregate of continental runoff …

Fjord dynamics influence oceanic heat flux to the Greenland ice sheet. Submarine iceberg
melting releases large volumes of freshwater within Greenland's fjords, yet its impact on fjord …

Accelerating since the early 1990s, the Greenland Ice Sheet mass loss exerts a significant
impact on thermohaline processes in the sub‐Arctic seas. Surplus freshwater discharge from …

Abstract The Greenland ice sheet (GrIS) stores the largest amount of freshwater in the
Northern Hemisphere and has been recently losing mass at an increasing rate. An eddy …

The initial 2 years of Overturning in the Subpolar North Atlantic Program mooring data (2014–
2016) provide the first glimpse into the seasonality of freshwater in the complete East …