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 …

As part of the international Overturning in the Subpolar North Atlantic Program (OSNAP),
135 acoustically-tracked deep floats were deployed to track the spreading pathways of …

The coastal circulation around Southern Greenland transports fresh, buoyant water masses
from the Arctic and Greenland Ice Sheet near regions of convection, sinking, and deep-water …

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 deep circulation in the subpolar North Atlantic determines the spread and mixing of high
latitude climate signals to lower latitudes. However, our current understanding of the …

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 …

Freshwater input from Greenland ice sheet melt has been increasing in the past decades
from warming temperatures. To identify the impacts from enhanced meltwater input into the …

Recent mooring measurements from the Overturning in the Subpolar North Atlantic Program
have revealed abundant cyclonic eddies at both sides of Cape Farewell, the southern tip of …

Deep sound speed structure in the western Irminger Sea is found to be highly dynamic in
comparison to the adiabatic (uniform) sound speed gradient underpinning data assimilation …

We present the first continuous mooring records of the West Greenland Coastal Current
(WGCC), a conduit of fresh, buoyant outflow from the Arctic Ocean and the Greenland Ice …