Tidally Induced Residual Currents in Estuaries of Variable Breadth and Depth

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Abstract
Analytic solutions are derived for the longitudinal and cross-channel Eulerian and Lagrangian residual currents induced in narrow tidal channels of variable breadth and depth, but rectangular cross section, by the nonlinear interactions of the first-order tides. The solutions are shown to be valid as long as the system is weakly nonlinear such that gη0σ−2Δx−2 ≪ 1, and as long as breadth variations are sufficiently gradual that fb0σ−1Δx−1 ≪ η0 is a typical tidal amplitude. g is the acceleration of gravity, σ the tidal frequency, Δx the length scale over which the breadth changes, f the Coriolis parameter and b0 the channel width. Results are given for channels with exponentially decreasing breadth and depth profiles and for a channel with a constriction in the breadth profile. These results indicate that significant differences from the residual currents in constant breadth and depth channels occur for all three types, but especially for the constricted channel. For this channel a strong two-layer... Abstract Analytic solutions are derived for the longitudinal and cross-channel Eulerian and Lagrangian residual currents induced in narrow tidal channels of variable breadth and depth, but rectangular cross section, by the nonlinear interactions of the first-order tides. The solutions are shown to be valid as long as the system is weakly nonlinear such that gη0σ−2Δx−2 ≪ 1, and as long as breadth variations are sufficiently gradual that fb0σ−1Δx−1 ≪ η0 is a typical tidal amplitude. g is the acceleration of gravity, σ the tidal frequency, Δx the length scale over which the breadth changes, f the Coriolis parameter and b0 the channel width. Results are given for channels with exponentially decreasing breadth and depth profiles and for a channel with a constriction in the breadth profile. These results indicate that significant differences from the residual currents in constant breadth and depth channels occur for all three types, but especially for the constricted channel. For this channel a strong two-layer...

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