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Titlebook: Hydrodynamics and Sediment Dynamics of Tidal Inlets; David G. Aubrey,Lee Weishar Conference proceedings 1988 Springer Science+Business Med

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Port of Miami Inlet Dynamics(deepening the inlet at jetty ends) further reduced the magnitude of currents. The U.S. Army Engineer District, Jacksonville (SAJ), is evaluating jetty modification plans at the entrance channel to alleviate problems with strong crosscurrents at the ocean entrance and inner harbor channels to Miami
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Seasonal Climatology of Tidal Non-Linearities in a Shallow Estuaryology of tidal distortion within this shallow, well-mixed estuary. Numerical results are consistent with these data and suggest comparable behavior in other geometrically-similar systems. The non-linear tidal response to changes in the amplitude-to-depth ratio (a/h) are investigated utilizing the sp
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Small-Scale Inlets as Tidal Filtersnlet cross-sectional area, a, and the surface area of the adjoining estuary, A, ranged from 0.36 × 10. to 111 × 10., while the length of the inlets, ranged from 42 m to ~380 m..The amplitude of the semidiurnal M. tide on the ocean side of the inlets varied from 18 cm to 98 cm with corresponding M./M
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Observations of Suspended Sediment Flux over a Tidal Cycle in the Region of the Turbidity Maximum ofe turbidity maximum to near sea water salinities at the mouth of the Saguenay Fjord. The anchor stations reveal that in the region of the turbidity maximum near surface suspended sediment concentrations are maximum during and just following the ebb phase of the tidal cycle while near the bottom sedi
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