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The 'Labrador Current' is a cold current in the north Atlantic Ocean which flows from the Arctic Ocean south along the coast of Labrador and passes around Newfoundland, continuing south along the east coast of Nova Scotia. It is a continuation of the West Greenland Current and the Baffin Island Current.
It meets the warm Gulf Stream at the Grand Banks southeast of Newfoundland and again north of the Outer Banks of North Carolina. The combination of these two currents produces heavy fogs and also created one of the richest fishing grounds in the world.
In spring and early summer, this current transports icebergs from the glaciers of Greenland southwards into the trans-Atlantic shipping lanes.
The waters of the Labrador Current have a cooling effect on the Canadian Atlantic provinces and coastal New England, but rarely have a significant effect on waters south of Cape Cod. This can most clearly be seen in the fact that the northern limit of tree growth can be as much as ''fifteen degrees'' farther south than in Siberia, Europe or western Canada.
The transport of the Labrador Current is believed to contain a large barotropic component. Early estimates indicated that the current may be 30% stronger than geostrophic calculations indicated as a result of a significant barotropic flow component (Hayes and Robe, 1978). Greenberg and Petrie (1988) calculated a total transport of 7.6 Sv while the geostrophic transport was calculated to be just 4.1 Sv (based on IIP sections). With a 30% increase (due to barotropic flow) the transport is only 5.3 Sv so, the high transport values are thought to largely from the inclusion of deep currents indicated by a deep water mooring. Speeds for the Labrador Current are about 0.3-0.5 ms-1 along the shelf edge (Greenbergand Petrie, Reynaud et al, 1985. Current speeds of 0.3-0.5 ms-1 were found by Reynaud et al. (1995) for the Labrador Current. Including the barotropic component, they estimate a value of 3Sv for the continental shelf branch of the Labrador Current and 16 Sv transport for the slope branch of the Labrador Current. The inshore branch of the Labrador Current is approximately 100 km wide and 150 km deep and it passes through Avalon Channel and the splitting of the Labrador Current around Flemish Cap can be seen in the tracks of satellite tracked drifters (Petrie and Anderson, 1985). Within Flemish Pass, Petrie and Anderson (1985) report that the width of the Labrador Current is reduced to 50 km with a speeds of 25 ms-1 which they believe is actually 30 ms-1.

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See also

External link

See also

★ Ocean current

★ Labrador Current

★ Baffin Island Current

★ West Greenland Current

★ East Greenland Current

External link

★ Surface Currents in the Atlantic Ocean