“…Over the slope, the Iberian Poleward current flows towards the east and north of the Spanish and French coasts with relatively weak mean currents (~ 0.2 m.s -1 ). This current presents a marked seasonality, with stronger currents in winter that are frequently associated to positive SST anomalies over the northern Spanish slope [4,5,6,7,8,9,10]. Moreover, significant mesoscale variability has been observed along the slope, where the interaction of the current and the bathymetry gives rise to mesoscale eddies, commonly known as SWODDIES -Slope Water Eddies [5,7,11,12].…”