from each of the "reservoirs" or inlet morphologic features for bypassing and beach nourishment. In
the case of Sebastian Inlet, model simulations indicate that sand bypassing from an interior sand trap
has slowed the growth of the flood shoal, and has produced minimal impact on growth of the ebb
We thank the Sebastian Inlet Tax District for providing topographic survey data. This work was
conducted under the Inlet Morphology and Channel Evolution Work Unit of the Coastal Inlets
Research Program, U.S. Army Engineer Research and Development Center, Coastal and Hydraulics
Laboratory. Permission was granted by Headquarters, U.S. Army Corps of Engineers, to publish
Coastal Technology Corporation, 1988. Sebastian Inlet District Comprehensive Management Plan.
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Volume of Ebb-Tidal Shoals, Part I: Description. Coastal Hydraulics Engineering Technical
Note IV-39, Coastal Inlets Research Program, U.S. Army Research and Development Center,
Coastal and Hydraulics Laboratory, Vicksburg, MS, 14 pp.
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Evaluation of Flood and Ebb Shoal Sediment Source Alternatives for the West of Shinnecock
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Army Research and Development Center, Coastal and Hydraulics Laboratory, Vicksburg, MS
White,W.A. 1970. The Geomorphology of the Florida Peninsula. State of Florida Department of
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Key Words: Tidal Inlets, Reservoir Model, Ebb Shoal, Flood Shoal, Shoreline Change, Sediment
Budget, Sebastian Inlet, Florida.
Zarillo et al.