Basin-wide geostrophic shear profiles have been computed for several latitudes in the eastern Atlantic between 32 and 53N. The absolute velocity on each section has been chosen so that the transport satisfies the Sverdrup relation. It is concluded that the wind-driven currents are not confined to the upper thermocline but extend to great depth....
Saunders, Peter M.. 1982. "Circulation in the eastern North Atlantic." Journal of Marine Research 40, (S). https://elischolar.library.yale.edu/journal_of_marine_research/1661