Among the organisms that spread into and flourish in Arctic waters with rising temperatures
and sea ice loss are toxic algae, a group of harmful algal bloom species that produce potent …

Eddy‐resolving regional ocean model results in conjunction with synthetic float trajectories
and observations provide new insights into the recirculation of the Atlantic Water (AW) in …

Abstract The Northeast Greenland shelf (NEGS) is a recipient of Polar Water (PW) from the
Arctic Ocean, Greenland Ice Sheet melt, and Atlantic Water (AW). Here, we compile …

Understanding the climatological characteristics of marine cold air outbreaks (CAOs) is of
critical importance to constrain the processes determining the heat flux forcing of the high …

The overturning streamfunction as measured at the OSNAP (Overturning in the Subpolar
North Atlantic Program) mooring array represents the transformation of warm, salty Atlantic …

Abstract The Iceland and Greenland Seas are a crucial region for the climate system, being
the headwaters of the lower limb of the Atlantic Meridional Overturning Circulation …

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 …

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 …

Dense waters formed in the Nordic Seas spill across gaps in the Greenland-Scotland Ridge
into the abyss of the North Atlantic to feed the lower limb of the Atlantic Meridional …

Warm subtropical-origin Atlantic water flows northward across the Greenland-Scotland
Ridge into the Nordic Seas, where it relinquishes heat to the atmosphere and gradually …