Abstract The Atlantic Meridional Overturning Circulation (AMOC) is a key component of the
climate through its transport of heat in the North Atlantic Ocean. Decadal changes in the …

Arguably, the most conspicuous evidence for anthropogenic climate change lies in the Arctic
Ocean. For example, the summer-time Arctic sea ice extent has declined over the last 40 …

Abstract The Subpolar North Atlantic is prone to recurrent extreme freshening events called
Great Salinity Anomalies (GSAs). Here, we combine hydrographic ocean analyses and …

A description and assessment of the first release of the Arctic Subpolar gyre sTate Estimate
(ASTE_R1), a data‐constrained ocean‐sea ice model‐data synthesis, is presented …

The waters on the West Greenland continental shelf and slope play an important role in the
global climate system with their link to the subpolar North Atlantic Ocean circulation system …

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 …

Abstract The Labrador Sea is known for strong surface heat losses and deep ocean
ventilation in the wintertime as well as high biological productivity and carbon export …

As the only oceanic connection between the Pacific and Arctic‐Atlantic Oceans, Bering Strait
throughflow carries a climatological northward transport of about 1 Sv, contributing to the …

The decadal variability and long-term trend of upper-ocean temperature in the Southeast
Indian Ocean since the 1950s are investigated based on an eddy-resolving ocean model …

By transporting warm and salty water poleward, the Gulf Stream system maintains a mild
climate in northwestern Europe while also facilitating the dense water formation that feeds …