Labrador Current
Encyclopedia
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 iceberg
s from the glacier
s 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 . (One Sverdrup (Sv) is equal to 106 cubic meters per second.) The geostrophic transport was calculated to be just (based on IIP sections). With a 30% increase (due to barotropic flow) the transport is only 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 along the shelf edge (Greenbergand Petrie, Reynaud et al., 1985. Current speeds of were found by Reynaud et al. (1995) for the Labrador Current. Including the barotropic component, they estimate a value of 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 wide and deep and it passes through Avalon Channel and the splitting of the Labrador Current around Flemish Cap
can be seen in the satellite
tracked drifters (Petrie and Isenor). Within the Flemish Pass, Petrie and Isenor (1985) report that the width of the Labrador Current is reduced to with a speed of which they believe is actually .
The Labrador Current has a tendency to sometimes go farther south and/or east than normal. This can produce hazardous shipping conditions as it can carry icebergs into an area of the Atlantic where they are not usually found. The current has been known to transport icebergs as far south as Bermuda
and as far east as the Azores
. The International Ice Patrol
was set up to track icebergs, including those found in areas of the ocean where they are rarely located.
Arctic Ocean
The Arctic Ocean, located in the Northern Hemisphere and mostly in the Arctic north polar region, is the smallest and shallowest of the world's five major oceanic divisions...
south along the coast of Labrador
Labrador
Labrador is the distinct, northerly region of the Canadian province of Newfoundland and Labrador. It comprises the mainland portion of the province, separated from the island of Newfoundland by the Strait of Belle Isle...
and passes around Newfoundland, continuing south along the east coast of Nova Scotia
Nova Scotia
Nova Scotia is one of Canada's three Maritime provinces and is the most populous province in Atlantic Canada. The name of the province is Latin for "New Scotland," but "Nova Scotia" is the recognized, English-language name of the province. The provincial capital is Halifax. Nova Scotia is the...
. It is a continuation of the West Greenland Current
West Greenland Current
The West Greenland Current is a weak cold water current that flows to the north along the west coast of Greenland. The current results from the movement of water flowing around the southernmost point of Greenland caused by the East Greenland Current....
and the Baffin Island Current
Baffin Island Current
Baffin Island Current is an ocean current running south down the western side of Baffin Bay in the Arctic Ocean, along Baffin Island. Its sources are the West Greenland Current and outflow from the Arctic Ocean. Its speed is approximately per day.- See also :* Labrador Current* East Greenland...
.
It meets the warm Gulf Stream
Gulf Stream
The Gulf Stream, together with its northern extension towards Europe, the North Atlantic Drift, is a powerful, warm, and swift Atlantic ocean current that originates at the tip of Florida, and follows the eastern coastlines of the United States and Newfoundland before crossing the Atlantic Ocean...
at the Grand Banks
Grand Banks
The Grand Banks of Newfoundland are a group of underwater plateaus southeast of Newfoundland on the North American continental shelf. These areas are relatively shallow, ranging from in depth. The cold Labrador Current mixes with the warm waters of the Gulf Stream here.The mixing of these waters...
southeast of Newfoundland and again north of the Outer Banks
Outer Banks
The Outer Banks is a 200-mile long string of narrow barrier islands off the coast of North Carolina, beginning in the southeastern corner of Virginia Beach on the east coast of the United States....
of North Carolina
North Carolina
North Carolina is a state located in the southeastern United States. The state borders South Carolina and Georgia to the south, Tennessee to the west and Virginia to the north. North Carolina contains 100 counties. Its capital is Raleigh, and its largest city is Charlotte...
. 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 iceberg
Iceberg
An iceberg is a large piece of ice from freshwater that has broken off from a snow-formed glacier or ice shelf and is floating in open water. It may subsequently become frozen into pack ice...
s from the glacier
Glacier
A glacier is a large persistent body of ice that forms where the accumulation of snow exceeds its ablation over many years, often centuries. At least 0.1 km² in area and 50 m thick, but often much larger, a glacier slowly deforms and flows due to stresses induced by its weight...
s of Greenland
Greenland
Greenland is an autonomous country within the Kingdom of Denmark, located between the Arctic and Atlantic Oceans, east of the Canadian Arctic Archipelago. Though physiographically a part of the continent of North America, Greenland has been politically and culturally associated with Europe for...
southwards into the trans-Atlantic shipping lanes.
The waters of the Labrador Current have a cooling effect on the Canadian
Canada
Canada is a North American country consisting of ten provinces and three territories. Located in the northern part of the continent, it extends from the Atlantic Ocean in the east to the Pacific Ocean in the west, and northward into the Arctic Ocean...
Atlantic provinces and coastal New England
New England
New England is a region in the northeastern corner of the United States consisting of the six states of Maine, New Hampshire, Vermont, Massachusetts, Rhode Island, and Connecticut...
, but rarely have a significant effect on waters south of Cape Cod
Cape Cod
Cape Cod, often referred to locally as simply the Cape, is a cape in the easternmost portion of the state of Massachusetts, in the Northeastern United States...
. 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
Siberia
Siberia is an extensive region constituting almost all of Northern Asia. Comprising the central and eastern portion of the Russian Federation, it was part of the Soviet Union from its beginning, as its predecessor states, the Tsardom of Russia and the Russian Empire, conquered it during the 16th...
, Europe
Europe
Europe is, by convention, one of the world's seven continents. Comprising the westernmost peninsula of Eurasia, Europe is generally 'divided' from Asia to its east by the watershed divides of the Ural and Caucasus Mountains, the Ural River, the Caspian and Black Seas, and the waterways connecting...
or western Canada.
The transport of the Labrador Current is believed to contain a large barotropic
Barotropic
In meteorology, a barotropic atmosphere is one in which the pressure depends only on the density and vice versa, so that isobaric surfaces are also isopycnic surfaces . The isobaric surfaces will also be isothermal surfaces, hence the geostrophic wind is independent of height...
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 . (One Sverdrup (Sv) is equal to 106 cubic meters per second.) The geostrophic transport was calculated to be just (based on IIP sections). With a 30% increase (due to barotropic flow) the transport is only 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 along the shelf edge (Greenbergand Petrie, Reynaud et al., 1985. Current speeds of were found by Reynaud et al. (1995) for the Labrador Current. Including the barotropic component, they estimate a value of 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 wide and deep and it passes through Avalon Channel and the splitting of the Labrador Current around Flemish Cap
Flemish Cap
The Flemish Cap is an area of shallow waters in the north Atlantic Ocean centered roughly at 47° north, 45° west or about 350 miles east of St. John's, Newfoundland and Labrador....
can be seen in the satellite
Satellite
In the context of spaceflight, a satellite is an object which has been placed into orbit by human endeavour. Such objects are sometimes called artificial satellites to distinguish them from natural satellites such as the Moon....
tracked drifters (Petrie and Isenor). Within the Flemish Pass, Petrie and Isenor (1985) report that the width of the Labrador Current is reduced to with a speed of which they believe is actually .
The Labrador Current has a tendency to sometimes go farther south and/or east than normal. This can produce hazardous shipping conditions as it can carry icebergs into an area of the Atlantic where they are not usually found. The current has been known to transport icebergs as far south as Bermuda
Bermuda
Bermuda is a British overseas territory in the North Atlantic Ocean. Located off the east coast of the United States, its nearest landmass is Cape Hatteras, North Carolina, about to the west-northwest. It is about south of Halifax, Nova Scotia, Canada, and northeast of Miami, Florida...
and as far east as the Azores
Azores
The Archipelago of the Azores is composed of nine volcanic islands situated in the middle of the North Atlantic Ocean, and is located about west from Lisbon and about east from the east coast of North America. The islands, and their economic exclusion zone, form the Autonomous Region of the...
. The International Ice Patrol
International Ice Patrol
The International Ice Patrol is an organization with the purpose of monitoring the presence of icebergs in the Atlantic and Arctic Oceans and reporting their movements for safety purposes. It is operated by United States Coast Guard but is funded by the 13 nations interested in trans-Atlantic...
was set up to track icebergs, including those found in areas of the ocean where they are rarely located.