Maximal two-layer exchange through a contraction with barotropic net flow

Author:

Armi L.,Farmer D. M.

Abstract

The gravitational exchange of two fluids with different densities between reservoirs connected by a channel of constant depth and slowly varying breadth is analysed as a problem of internal hydraulics. It is shown that maximal two-way exchange with a net barotropic flow requires the presence of two controls, one at the narrrowest section and a second or ‘virtual’ control lying to one side of the narrowest section. The two controls are connected by a subcritical region, but are separated from subcritical conditions in the reservoirs by supercritical flow and stationary internal bores. Solutions are found for maximal exchange without a net barotropic component, in which case the problem is similar to that first examined by Stommel & Farmer (1953). The Stommel & Farmer analysis is shown to be a rather special limiting example of submaximal exchange, not generally applicable to natural flows. The addition of a net barotropic flow yields a range of different flow types, including maximal exchange, one-layer baroclinic flow, one-layer barotropic flow, submaximal flow governed by a reservoir condition and two-layer unidirectional flow. The maximal-exchange solution is integrated for periodic barotropic flow.

Publisher

Cambridge University Press (CUP)

Subject

Mechanical Engineering,Mechanics of Materials,Condensed Matter Physics

Reference13 articles.

1. Stommel, H. & Farmer, H. G. 1953 Control of salinity in an estuary by a transition.J. Mar. Res. 12,13–20.

2. Long, R. R. 1956 Long wave in a two-fluid system.J. Met. 13,70–74.

3. Murray, S. P. , Hecht, A. & Babcock, A. 1984 On the mean flow in the Tiran Strait in winter.J. Mar. Res. 42,265–287.

4. Benjamin, T. B. 1968 Gravity currents and related phenomena.J. Fluid Mech. 31,209–248.

5. Armi, L. 1986 The hydraulics of two flowing layers with different densities.J. Fluid Mech. 163,27–58.

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