I have to wonder if this represents a mass movement of Atl. waters north to balance what I believe is an increasing outflow at Fram. Driven by both the inevitable replacement of lost Arctic waters and the displacement that causes south of Greenland?
I'm guessing if that's the case then as the ice becomes more 'fluid' it will present less resistance to the outflow causing the anomoly in turn to migrate north, towards if not actually into Barents, whilst maintaining a similar temp to the waters south of Ireland?