The mid-depth ocean circulation is critically linked to actual changes in the long-term global
climate system. However, in the past few decades, predictions based on ocean circulation …

Depth‐averaged eddy buoyancy diffusivities across continental shelves and slopes are
investigated using a suite of eddy‐resolving, process‐oriented simulations of prograde …

Under-ice eddies are prevalent in the major circulation system in the western Arctic Ocean,
the Beaufort Gyre. Theoretical studies hypothesize that the eddy-driven overturning and the …

Abstract The Beaufort Gyre (BG) is hypothesized to be partially equilibrated by those
mesoscale eddies that form via baroclinic instabilities of its currents. However, our …

Thirty-four individual thermohaline sheets are identified at depths of 170–400 m in the
Canada Basin of the Arctic Ocean by using the hydrographical data measured with the Ice …

We report on a pilot study using a CO 2 optode deployed on a Seaglider in the Norwegian
Sea for 8 months (March to October 2014). The optode measurements required drift-and lag …

Freshwater content (FWC), generally characterized in the Arctic Ocean by salinities lower
than 34.8 psu, has shifted in both quantity and distribution in recent decades in the Arctic …

Against the background of wind-forcing change along with Arctic sea ice retreat, the
mesoscale processes undergoing distinct variation in the Beaufort Gyre (BG) region are …

The Beaufort Gyre mean state is theorized to be set by surface wind stress, local sea ice,
and subsurface mesoscale eddy transport. The mesoscale eddies in this context are subject …

Abstract The Arctic Ocean is unique among the world's oceans, characterized by its cold
temperatures, salinity-driven vertical structure, and shallow shelf seas. It has warmed …