Eddies generated off the west Greenland coast modulate the deep convection in the
Labrador Sea, while there are still open questions related to their formation mechanisms …

Deep convection and associated deep water formation are key processes for climate
variability, since they impact the oceanic uptake of heat and trace gases and alter the …

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 …

By ventilating the deep ocean, deep convection in the Labrador Sea plays a crucial role in
the climate system. Unfortunately, the mechanisms leading to the cessation of convection …

The cyclonic boundary current that circumnavigates the Labrador Sea plays an important
role in modulating the strength of wintertime convection in the interior basin, as well as …

The hydrography and stratification of the subpolar North Atlantic is highly variable, with
convection activating and deactivating across parts of the Labrador and Irminger seas …

A 1/60° numerical simulation is carried out within the Labrador Sea to investigate eddies
produced along the western coast of Greenland. These eddies, known as Irminger Rings …

The impact of horizontal resolution on meridional Ocean Heat Transport (OHT) and sea ice
in the Arctic is investigated using the GFDL CM2‐O climate model suite (1°, 1/4°, and 1/10°) …

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 water mass produced during wintertime convection in the Labrador Sea (ie the
Labrador Sea Water or LSW) is characterized by distinct thermohaline properties. It has …