During the GALICIA-XI cruise from May 10 to May 14, 1991, the relaxation of a previous strong upwelling event took place along the Galician coast caused by a shift in the position of the Azores High. The coldest temperatures and highest nitrate levels were found near the coast corresponding to the advection of subsurface waters, particularly of Eastern North Atlantic Water (ENAW). On the basis of thermohaline properties, ENAW of polar (ENAWp) and tropical (ENAWt) origin are distinguished. The highest salinity values found correspond to a saline wedge of ENAWt located off the west coast of Galicia. The relaxation of upwelling produced a shoreward migration of surface water from oceanic stations which came into contact with upwelled Eastern North Atlantic Water from the coastal stations to form a convergence front 28 km off the coast. Meanwhile, the saline wedge displaced towards both the north and the shore which is favored by the compression of the upwelling system to a narrow coastal strip outwardly limited by the convergence zone.