Heywood, K. J. ORCID: https://orcid.org/0000-0001-9859-0026 (1995) Seasonal and interannual changes in the North Atlantic subpolar gyre from Geosat and TOPEX/POSEIDON altimetry. Journal of Geophysical Research, 100 (C12). pp. 24931-24941. ISSN 0148-0227
Full text not available from this repository. (Request a copy)Abstract
Sea surface slopes from the altimetric satellites Geosat and TOPEX/POSEIDON are used to calculate eddy kinetic energy of the North Atlantic subpolar gyre (40-65°N, 60°-5°W). In regions of strong currents the eddies are driven by baroclinic instability of the mean flow, are not seasonally varying, and may therefore be used as a surrogate for the mean flow itself. Wind stress curl fields for the same periods show that the northward and southward shifts in the current branches across the Mid-Atlantic Ridge are related to interannual differences in the winter wind stress curl pattern when the zero in wind stress curl is well defined and wind stress is at a maximum. Outside the NAC, the eddies are driven primarily by wind stress, indicated by a significant seasonality. Time series of eddy kinetic energy and wind stress are generated for the four years, and the magnitude, phase, and significance of annual and semiannual signals are determined. -from Authors
Item Type: | Article |
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Uncontrolled Keywords: | geophysics,forestry,oceanography,aquatic science,ecology,water science and technology,soil science,geochemistry and petrology,earth-surface processes,atmospheric science,earth and planetary sciences (miscellaneous),space and planetary science,palaeontology ,/dk/atira/pure/subjectarea/asjc/1900/1908 |
Faculty \ School: | Faculty of Science > School of Environmental Sciences University of East Anglia Research Groups/Centres > Theme - ClimateUEA |
UEA Research Groups: | Faculty of Science > Research Groups > Centre for Ocean and Atmospheric Sciences |
Related URLs: | |
Depositing User: | LivePure Connector |
Date Deposited: | 20 May 2020 00:14 |
Last Modified: | 20 Mar 2023 11:33 |
URI: | https://ueaeprints.uea.ac.uk/id/eprint/75241 |
DOI: |
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