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Ocean Science An interactive open-access journal of the European Geosciences Union

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Ocean Sci., 3, 179-188, 2007
© Author(s) 2007. This work is licensed under the
Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.
26 Apr 2007
Tidal modulation of two-layer hydraulic exchange flows
L. M. Frankcombe1,* and A. McC. Hogg1 1Research School of Earth Sciences, The Australian National University, Canberra, Australia
*now at: Institute for Marine and Atmosphere Research Utrecht, Department of Physics and Astronomy, Utrecht University, The Netherlands
Abstract. Time-dependent, two layer hydraulic exchange flow is studied using an idealised shallow water model. It is found that barotropic time-dependent perturbations, representing tidal forcing, increase the baroclinic exchange flux above the steady hydraulic limit, with flux increasing monotonically with tidal amplitude (measured either by height or flux amplitude over a tidal period). Exchange flux also depends on the non-dimensional tidal period, γ, which was introduced by by Helfrich (1995). When tidal amplitude is characterised by the barotropic flux amplitude, exchange flux is a monotonic function of γ as predicted by Helfrich (1995). However, the relationship between the (imposed) free surface amplitude and flux amplitude is complicated by reflections within the channel and by the baroclinic response of the two layer system, leading to a non-monotonic relationship between the height amplitude and γ.

Citation: Frankcombe, L. M. and Hogg, A. McC.: Tidal modulation of two-layer hydraulic exchange flows, Ocean Sci., 3, 179-188, doi:10.5194/os-3-179-2007, 2007.
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