Please use this identifier to cite or link to this item: https://hdl.handle.net/10356/95635
Title: Wave-induced longitudinal vortices in a shallow current
Authors: Huang, Zhenhua
Mei, Chiang C.
Keywords: DRNTU::Science::Geology
Issue Date: 2006
Source: Huang, Z., & Mei, C. C. (2006). Wave-induced longitudinal vortices in a shallow current. Journal of Fluid Mechanics, 551, 323-356.
Series/Report no.: Journal of fluid mechanics
Abstract: An instability theory is presented for the initiation of longitudinal vortices due to waves interacting with a turbulent current in an open channel of finite depth. With a simple model of eddy viscosity the dimensionless shearing rate of the basic current is much weaker than the dimensionless velocity almost everywhere except near the bed. We shall show that in addition to the internal vortex force, a mean shear stress exists on the mean sea level, owing to nonlinear wave–current interactions, despite the absence of wind. This stress adds vertical vorticity to the interior and augments the vortex force mechanism of instability significantly. Effects of current strength and wave conditions on the unstable growth are studied by numerical examples.
URI: https://hdl.handle.net/10356/95635
http://hdl.handle.net/10220/8725
DOI: http://dx.doi.org/10.1017/S0022112005008360
Rights: © 2006 Cambridge University Press.This paper was published in Journal of Fluid Mechanics and is made available as an electronic reprint (preprint) with permission of Cambridge University Press. The paper can be found at: [DOI: http://dx.doi.org/10.1017/S0022112005008360]. One print or electronic copy may be made for personal use only. Systematic or multiple reproduction, distribution to multiple locations via electronic or other means, duplication of any material in this paper for a fee or for commercial purposes, or modification of the content of the paper is prohibited and is subject to penalties under law.
Fulltext Permission: open
Fulltext Availability: With Fulltext
Appears in Collections:EOS Journal Articles

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