Abstract Analyzing a high‐resolution (1/60°) numerical model over 2008–2018, the inter‐
annual variability of the West Greenland Coastal Current (WGCC) on the shelf and West …

Increased freshwater input to the Subpolar North Atlantic from Greenland ice melt and the
Arctic could strengthen stratification in deep convection regions and impact the overturning …

Abstract The Icelandic Coastal Current (ICC) is a buoyant flow fueled by multiple rivers.
Satellite observations during the October–November 2019 study period indicate the ICC …

Increasing freshwater fluxes from the Greenland ice sheet and the Arctic to the Subpolar
North Atlantic could cause a freshening of deep convection regions and affect the …

We use a global 5‐km resolution model to analyze the air‐sea interactions during a
katabatic storm in the Irminger Sea originating from the Ammassalik valleys. Katabatic …

Arctic‐origin and Greenland meltwaters circulate cyclonically in the boundary current system
encircling the Labrador Sea. The ability of this freshwater to penetrate the interior basin has …

The pathways and fate of freshwater in the East Greenland Coastal Current (EGCC) are
crucial to the climate system. The EGCC transports large amounts of freshwater in close …

Abstract The shelf based West Greenland Current System carries both Arctic Water and
Greenland meltwater around Cape Farewell, the southern tip of Greenland, where it may …

Abstract The Irminger Sea is one of the few regions in the ocean where deep (> 1,000 m)
convection occurs. Convection is followed by restratification during summer, when the …

Abstract The Greenland Ice Sheet is losing mass at an accelerating pace, increasing its
contribution to the freshwater input into the Nordic Seas and the subpolar North Atlantic. It …