Lagrangian perspectives of deep water export from the subpolar North Atlantic
Lagrangian perspectives of deep water export from the subpolar North Atlantic
Direct observations at the Grand Banks have raised a quandary concerning the pathways of the lower branch of the meridional overturning circulation: In contrast to moored current meters that depict an intense, narrow Deep Western Boundary Current (DWBC), observations using different float types failed to show this continuous export path. Here, this issue is addressed by a Lagrangian analysis of synthetic particles in an eddy-resolving circulation model. Due to intense eddy activity around the Grand Banks, about 40% of the deep water in the DWBC is diverted into the interior, spreading southward along the western flank of the Mid-Atlantic Ridge or with the eddying flow field in the basin interior. Imposing constraints on the vertical displacements of particles similar to those experienced by observational floats further reduces their adherence to the DWBC, particularly near the southern tip of the Grand Banks.
L21S08
Getzlaff, K.
2b562e28-3153-422d-83f5-a9da8114aa20
Boening, C.W.
a6437f89-4fdd-4a01-a829-e33cc91abdef
Dengg, J.
8980e0c2-8c60-4986-af69-0e254cc6ce79
2006
Getzlaff, K.
2b562e28-3153-422d-83f5-a9da8114aa20
Boening, C.W.
a6437f89-4fdd-4a01-a829-e33cc91abdef
Dengg, J.
8980e0c2-8c60-4986-af69-0e254cc6ce79
Getzlaff, K., Boening, C.W. and Dengg, J.
(2006)
Lagrangian perspectives of deep water export from the subpolar North Atlantic.
Geophysical Research Letters, 33 (21), .
(doi:10.1029/2006GL026470).
Abstract
Direct observations at the Grand Banks have raised a quandary concerning the pathways of the lower branch of the meridional overturning circulation: In contrast to moored current meters that depict an intense, narrow Deep Western Boundary Current (DWBC), observations using different float types failed to show this continuous export path. Here, this issue is addressed by a Lagrangian analysis of synthetic particles in an eddy-resolving circulation model. Due to intense eddy activity around the Grand Banks, about 40% of the deep water in the DWBC is diverted into the interior, spreading southward along the western flank of the Mid-Atlantic Ridge or with the eddying flow field in the basin interior. Imposing constraints on the vertical displacements of particles similar to those experienced by observational floats further reduces their adherence to the DWBC, particularly near the southern tip of the Grand Banks.
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Published date: 2006
Organisations:
Ocean and Earth Science
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Local EPrints ID: 44276
URI: http://eprints.soton.ac.uk/id/eprint/44276
ISSN: 0094-8276
PURE UUID: 96c36430-a2de-4826-ab73-9e381f3ec724
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Date deposited: 21 Feb 2007
Last modified: 15 Mar 2024 09:02
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Author:
K. Getzlaff
Author:
C.W. Boening
Author:
J. Dengg
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