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- W1989018100 abstract "Deep water formation in the northwestern Mediterranean Sea is investigated with a high-resolution three-dimensional primitive equation numerical model. A rectangular basin is forced by various heat and salt fluxes. A 1000-m thick patch of dense water is formed within the forcing area, which is surrounded by a cyclonic vortex. Meanders develop at the periphery of the patch and then tend to occupy the whole patch area. These features agree with observations. Sensitivity studies of the space and time variability of the forcing are presented. It is found that these variabilities are of great importance in deep water formation. Deep water formation appears to depend on a convective process parameterized by a simple non-penetrative convective adjustment and on vertical motion induced by baroclinic instability. The two processes are strongly linked. The convective process triggers the depth of the convection while the baroclinic adjustment process is responsible for the volume of dense water formed." @default.
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- W1989018100 date "1991-04-01" @default.
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- W1989018100 title "The effect of thermohaline forcing variability on deep water formation in the western Mediterranean Sea: a high-resolution three-dimensional numerical study" @default.
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- W1989018100 doi "https://doi.org/10.1016/0377-0265(91)90024-a" @default.
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