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- W2017440857 abstract "In support of Swallow and Caston's (1973) conclusion that topography plays a significant role in determining the position of the dense water formation region in the northwest Mediterranean, a theoretical model conserving potential vorticity in flow past a conical bump abutted to the continental slope is studied. For parameters appropriate to this area it is shown that the flow falls in the weak stratification category of Hogg (1973), implying that the streamline pattern is quasi-two-dimensional. For typical values of the lateral shear and a topographic parameter, closed streamlines (i.e. a baroclinic Taylor column) are found over the bump in agreement with the observations. As the region is isolated and also possesses greater initial density and decreased stability, it is suggested that this is where dense waater is most likely to be formed." @default.
- W2017440857 created "2016-06-24" @default.
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- W2017440857 date "1973-05-01" @default.
- W2017440857 modified "2023-10-18" @default.
- W2017440857 title "The preconditioning phase of MEDOC 1969—II. Topographic effects" @default.
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- W2017440857 doi "https://doi.org/10.1016/0011-7471(73)90099-5" @default.
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