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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 .
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 ...
The NADW consists of three parts of different origin and salinity, and the top one, the Labrador Sea Water (LSW), is formed in the Labrador Sea. This part occurs at a medium depth and has a relatively low salinity (34.84–34.89 parts per thousand), low temperature (3.3–3.4 °C (37.9–38.1 °F)) and high oxygen content compared to the layers ...
An intermediate cold water mass known as Labrador Sea Water is formed by convective processes in the Labrador Sea. [55] [56] It represents a key component of the Atlantic Meridional Overturning Circulation, which is a major contributor to the transport and storage of heat, freshwater and other tracers in the Atlantic Ocean. [57]
East Iceland Current – Cold water ocean current that forms as a branch of the East Greenland Current; Labrador Current – Cold current in the Atlantic ocean along the coasts of Labrador, Newfoundland and Nova Scotia; North Icelandic Jet – Deep-reaching current that flows along the continental slope of Iceland
AMOC in relation to the global thermohaline circulation . The Atlantic meridional overturning circulation (AMOC) is the main current system in the Atlantic Ocean, [1]: 2238 and is also part of the global thermohaline circulation, which connects the world's oceans with a single "conveyor belt" of continuous water exchange. [18]
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Classical Labrador Sea Water (CLSW) production is dependent on preconditioning of water in the Labrador Sea from the previous year and the strength of the North Atlantic oscillation (NAO). [6] During a positive NAO phase, conditions exist for strong winter storms to develop. These storms freshen the surface water, and their winds increase ...