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The Labrador Sea is about 3,400 m (1,859 fathoms; 11,155 feet) deep and 1,000 km (621 miles; 540 nautical miles) wide where it joins the Atlantic Ocean. It becomes shallower, to less than 700 m (383 fathoms; 2,297 ft) towards Baffin Bay (see depth map ) and passes into the 300 km (190 mi; 160 nmi) wide Davis Strait . [ 2 ]
2 Europe. Toggle Europe subsection. 2.1 Iceland. 2.2 Norway. ... Map all coordinates using OpenStreetMap. ... Labrador Sea Port of Ilulissat ...
Map of the Labrador, Baffin Island and West Greenland currents. West Greenland Current originates from the movement of Atlantic water flowing around the southern point of Greenland caused by the East Greenland and Irminger currents. [42] [63] [64] It transports freshwater into the Labrador Sea, influencing the formation of Labrador Sea Water. [57]
Arctic Ocean / Atlantic Ocean / Pacific Ocean / Baffin Bay / Beaufort Sea / Bering Sea / Caribbean Sea / Chukchi Sea / Greenland Sea / Gulf of Mexico / Hudson Bay / Labrador Sea: Antarctica: Eastern / Southern / Western: Southern Ocean / Amundsen Sea / Ross Sea / Weddell Sea: Africa: Eastern / Northern / Southern / Western: Asia *Egypt
Clickable map of Europe, showing the standard convention for its continental boundary with Asia. (see boundary between Asia and Europe for more information). Legend: blue = Contiguous transcontinental states; green = Sometimes considered European but geographically outside Europe's boundaries.
The Labrador Current has an average annual velocity of 20 cm/s and is formed from very cold water that is around 1.5˚C from the Arctic through Baffin Island, Canada, and Western Greenland. These waters come together in the Labrador Sea. The Labrador Sea is affected by seasonality and will experience greater freshwater imports during the late ...
Convection in the Labrador Sea is the result of a combination of cyclonic oceanographic circulation of the sea currents and cyclonic atmospheric forcing. At the southern tip of Greenland, water enters the West Greenland Current from the East Greenland Current, continues to flow northwest around the Baffin Bay, and then southeast into the Baffin Island Current continuing in the same direction ...
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