From the wind stress computation of Bunker (1976) for the North Atlantic, the annual mean and seasonal vertical velocities which result from convergences in the Ekman Layers are computed. Charts of the geostrophic and total transport (geostrophic plus Ekman) are constructed using the Sverdrup relationship. Of particular interest are an intense current leaving the coast at the point where the Gulf Stream separates and a cyclonic gyre north of the Stream in this area....