title: Formation of Winter Surface Temperature Anomalies in the North Atlantic in Decades of Negative and Positive Values of the North Atlantic Oscillation Index
abstract: Abstract An analysis of the variability of the winter surface temperature anomaly in the North Atlantic in decades of negative and positive values of the North Atlantic Oscillation Index is presented. It is found that, in a decade with negative values of the North Atlantic Oscillation Index, the slope waters of the Gulf Stream system and Labrador Current waters decrease the temperature of the Gulf Stream at the mixing zone on the Scotia Peninsula shelf and in the area of the quasi-stationary ant
journal: Doklady Earth Sciences