Abstract
The circulation in the western North Atlantic is studied within the framework of a nonlinear finite difference geostrophic inverse model using hydrographic and currentmeter data. The nonlinear inverse formalism is first reviewed. A circulation scheme compatible with the data, the mass conservation and the potential density equation is then derived. The optimal circulation scheme presents variations in the Gulf Stream transport with longitude. The variations are explained by the interaction of the Gulf Stream with recirculating gyres.
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© 1989 Kluwer Academic Publishers
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Mercier, H. (1989). The Circulation in the Western North Atlantic Determined by a Nonlinear Inverse Method. In: Anderson, D.L.T., Willebrand, J. (eds) Oceanic Circulation Models: Combining Data and Dynamics. NATO ASI Series, vol 284. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-1013-3_5
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DOI: https://doi.org/10.1007/978-94-009-1013-3_5
Publisher Name: Springer, Dordrecht
Print ISBN: 978-94-010-6946-5
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