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 Dynamicse collected by the National Oceanic and Atmospheric Administration (NOAA) and WES..The numerical modeling approach consisted of applying WIFM in a two-phase modeling study. The first phase involved a global model which included areas of the inner harbor and a substantial open ocean area with a 200-

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ingrate

Medicaid

Enhancement of Semidiurnal Tidal Currents in the Tidal Inlets to Mississippi Soundalues are caused by compound tides and overtides of the diurnal constituents, which have contaminated the harmonic constant estimates of semidiurnal currents. The K./K. ratio (K. representing the first harmonic of K. generated locally) is estimated to be 0.3 in the inlet currents, and the two waves

Delectable

DARTS (Digital Automated Radar Tracking System): Application to Tidal Inlet Hydrodynamic Studiesreturn intensities from the steep faces of approaching ocean surface waves. From this matrix of sea surface return intensities, a spatial Fast Fourier Transform (FFT) is applied to obtain an estimate of the directional wavenumber spectrum for the incident sea surface. In the current measuring mode,

NIP

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Observations of Suspended Sediment Flux over a Tidal Cycle in the Region of the Turbidity Maximum ofstream Reynolds transport arising from higher suspended sediment concentrations on the flood than on the ebb in the lower portion of the water column. Thus contaminants may be recycled through the turbidity maximum by means of this tidal pumping. A bulk vertical settling velocity of 0.3 mm/s was est

irradicable

Engaging

Processes of Sediment Exchange between Tidal Inlets, Ebb Deltas and Barrier Islandsiers (sources). . inlets that are efficient by-passers have accumulations of sediment on the downdrift ends of adjacent barriers... inlets that are poor by-passers have deep inlet gorges (sources) and large shore-normal tidal deltas (sinks). Sediment stored in deltas eventually may return to the isl

Favorable

Inlet Flood Tidal Delta Development through Sediment Transport Processesconstruction..This inlet has only a small ebb tidal shoal configuration, but the extensive flood tidal delta has grown to be the most dominant feature. Growth of this delta and changes in channel orientation through time have been documented with a detailed series of aerial photographs beginning in