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One proceeds northward and then eastward around Iceland, and the other flows westward and then southwestward, merging with the East Greenland and, eventually, the West Greenland currents.
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See Greenland Current.
Along the east coast of Greenland is the southward-flowing cold East Greenland Current.
West Greenland Current, cool flow of water proceeding northward along the west coast of Greenland.
The East Greenland Current brings ice down from the north and bifurcates near the central ridge.
Other bergs pass through Fram Strait and into the East Greenland Current.
The Norwegian Gyral separates the Norway Current from a southeastward-flowing branch of the East Greenland Current.
Icebergs entering Baffin Bay first move northward in the West Greenland Current and are strongly reinforced by icebergs from the prolific West Greenland glaciers.
East Greenland Current, cold flow of water originating in the Arctic Ocean and flowing southward and southwestward along the east coast of Greenland.
The East Greenland Current flows south along Greenland's east coast, transporting large fields of ice, and then turns north into the Labrador Sea.
Greenland Current, surface oceanic current, a combination of polar sea surface drift, return flow of the North Atlantic Current, and Irminger Current waters.
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