surface oceanic current flowing southward along the west side of the Labrador Sea. Originating at the Davis Strait, the Labrador Current is a combination of the West Greenland Current, the Baffin Island Current, and inflow from Hudson Bay. The current is cold and has a low salinity; it maintains temperatures of less than 32° F (0° C) and salinities in the range of 30 to 34 parts per 1,000. The Labrador Current is limited to the continental shelf and reaches depths only slightly greater than 2,000 feet (600 m). Its volume of water transport varies between about 125,000,000 and 190,000,000 cubic feet (3,500,000 and 5,400,000 cubic m) per second and annually carries several thousand icebergs southward.