Greatbatch, Richard J. and Zhai, Xiaoming (2006) Influence of assimilated eddies on the large-scale circulation in a model of the northwest Atlantic Ocean. Geophysical Research Letters, 33 (2). ISSN 0094-8276
Full text not available from this repository. (Request a copy)Abstract
In this letter, we apply a novel technique (the “semidiagnostic method”) to assimilate the eddy field from a model with constrained large-scale circulation into a model version with an unconstrained large-scale circulation. Assimilation of the eddies (i) drives an anomalous circulation corresponding to the northern recirculation gyre of the Gulf Stream, but of insufficient strength to appear in the mean field and (ii) leads to a much enhanced circulation in the northwest corner, east of Newfoundland. We argue that the blocking of f/H contours from the east by the mid-Atlantic Ridge is a major influence on the dynamics of the northwest corner, and that the dynamics of the eddy-driven northern recirculation and the northwest corner are fundamentally similar.
Item Type: | Article |
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Faculty \ School: | Faculty of Science > School of Environmental Sciences |
UEA Research Groups: | Faculty of Science > Research Groups > Marine and Atmospheric Sciences (former - to 2017) Faculty of Science > Research Groups > Meteorology, Oceanography and Climate Dynamics (former - to 2017) Faculty of Science > Research Groups > Climate, Ocean and Atmospheric Sciences (former - to 2017) Faculty of Science > Research Groups > Centre for Ocean and Atmospheric Sciences |
Depositing User: | Pure Connector |
Date Deposited: | 23 Oct 2013 11:44 |
Last Modified: | 24 Oct 2022 04:50 |
URI: | https://ueaeprints.uea.ac.uk/id/eprint/43790 |
DOI: | 10.1029/2005GL025139 |
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