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Please use this identifier to cite or link to this item: https://dspace.lboro.ac.uk/2134/4260

Title: Frontogenesis in gravity-driven flows with non-uniform density gradients
Authors: Kay, Anthony
Issue Date: 1992
Publisher: © Cambridge University Press
Citation: KAY, A., 1992. Frontogenesis in gravity-driven flows with non-uniform density gradients. Journal of Fluid Mechanics Digital Archive, 235, pp. 529-556
Abstract: A horizontal density gradient may be steepened to form a front if the horizontal flow which it drives is convergent. This convergence may be caused by an initial nonlinearity in the density gradient (as described by Simpson & Linden 1989). A quadratic density profile is analysed to illustrate the mechanism, and it is shown how the flow and the density profile interact to intensify and concentrate the front near a horizontal boundary. Linear and curved density profiles in a container of finite length are also studied: the most favourable location for frontogenesis is found to be where the flow emerges into a region of significant curvature after passing through a maximum of the density gradient
Description: This article was published in the Journal of Fluid Mechanics [© Cambridge University Press] and is also available at: http://journals.cambridge.org/action/displayAbstract?fromPage=online&aid=397887
Version: Published
DOI: 10.1017/S0022112092001216
URI: https://dspace.lboro.ac.uk/2134/4260
ISSN: 0022-1120
1469-7645
Appears in Collections:Published Articles (Maths)

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