The retroflection of part of the East Greenland Current at Cape Farewell
The retroflection of part of the East Greenland Current at Cape Farewell
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.
L07609
Holliday, N.P.
358b0b33-f30b-44fd-a193-88365bbf2c79
Meyer, A.
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Bacon, S.
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Alderson, S.
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de Cuevas, B.
01cc697c-2832-4de6-87bf-bf9f16c1f906
2007
Holliday, N.P.
358b0b33-f30b-44fd-a193-88365bbf2c79
Meyer, A.
70573a54-f9b5-4fd5-8940-6a7052c38f35
Bacon, S.
1e7aa6e3-4fb4-4230-8ba7-90837304a9a7
Alderson, S.
00ee9859-a11f-4040-a963-d88d4ae2740d
de Cuevas, B.
01cc697c-2832-4de6-87bf-bf9f16c1f906
Holliday, N.P., Meyer, A., Bacon, S., Alderson, S. and de Cuevas, B.
(2007)
The retroflection of part of the East Greenland Current at Cape Farewell.
Geophysical Research Letters, 34 (7), .
(doi:10.1029/2006GL029085).
Abstract
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.
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2006GL029085.pdf
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Submitted date: 13 December 2006
Published date: 2007
Organisations:
National Oceanography Centre,Southampton
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Local EPrints ID: 44770
URI: http://eprints.soton.ac.uk/id/eprint/44770
ISSN: 0094-8276
PURE UUID: bf1ae466-2679-4bcf-b307-95f3aa9b0c48
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Date deposited: 14 Mar 2007
Last modified: 15 Mar 2024 09:07
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Author:
N.P. Holliday
Author:
A. Meyer
Author:
S. Bacon
Author:
S. Alderson
Author:
B. de Cuevas
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