The retroflection of part of the East Greenland Current at Cape Farewell

• Published in: Geophysical Research Letters
• Main Authors: Holliday, N.P., Meyer, A., Bacon, S., Alderson, S., de Cuevas, B.
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2007
• Subjects: Arctic; Greenland; Irminger Basin; Irminger Sea; Cape Farewell; East Greenland; east greenland current; Labrador Sea; North Atlantic
• Online Access: http://nora.nerc.ac.uk/id/eprint/144770/; https://nora.nerc.ac.uk/id/eprint/144770/1/2006GL029085.pdf; http://www.agu.org/journals/gl/gl0707/2006GL029085/; https://doi.org/10.1029/2006GL029085

The East Greenland Current (EGC) and the smaller East Greenland Coastal Current (EGCC) provide the major conduit for cold fresh polar water to enter the lower latitudes of the North Atlantic. They flow equatorward through the western Irminger Basin and around Cape Farewell into the Labrador Sea. The surface circulation and transport of the Cape Farewell boundary current region in summer 2005 is described. The EGCC merges with Arctic waters of the EGC to the south of Cape Farewell, forming the West Greenland Current. The EGC transport decreases from 15.5 Sv south of Cape Farewell to 11.7 Sv in the eastern Labrador Sea (where the water becomes known as Irminger Sea Water). The decrease in EGC transport is balanced by the retroflection of a substantial proportion of the boundary current (5.1 Sv) into the central Irminger Basin; a new pathway for fresh water into the interior of the subpolar gyre.