Reversed North Atlantic gyre dynamics in present and glacial climate

Eddy salt transport from the upper boundary current into the upper central basin effectively counteracts surface freshwater flux at the beginning of the experiment until

Weaker subpolar gyre cyclonic circulation during winter is likely contributing to the heat accumulation in the northern North Atlantic region observed for the R2 simulation

Using four different climate models, we investi- gate sea level pressure variability in the extratropical North Atlantic in the preindustrial climate (1750 AD) and at the Last

The weakened AMOC in the freshwater integration is caused by reduced deep-water formation rates in the North Atlantic subpolar gyre and in the Nordic Seas, and by a reduced

[ 35 ] In addition to a warm eastern North Atlantic and Nordic Seas, the weaker subpolar gyre results in a north- ward shift of the North Atlantic Current, creating a warm anomaly

Abstract The response of the North Atlantic subpolar gyre (SPG) to a persistent positive (or negative) phase of the North Atlantic oscillation (NAO) is investigated using an

Abstract The dynamics of the North Atlantic subpolar gyre (SPG) are assessed under present and glacial boundary conditions by investigating the SPG sensitivity to surface

In the Nordic Seas, changes in surface forcing are directly transported to intermediate depth south of the GSR through deep water formation and alter the density distribution