Springer, Berlin, pp 186–225įitzGerald DM (1996) Geomorphic variability and morphologic and sedimentologica controls on tidal inlets. In: Aubrey DG, Weishar L (eds) Hydrodynamics and sediment dynamics of tidal inlets. ASCE, pp 1094–1118įitzGerald DM (1988) Shoreline erosional-depositional processes associated with tidal inlets. In: Proceedings of the 18th coastal engineering conference. Unpublished Masters thesis, University of North Carolina, Chapel Hill, 120 pįitzGerald DM (1982) Sediment bypassing at mixed energy tidal inlets. Academic, New York, pp 201–216ĭavis RA Jr, Hayes MO (1984) What is a wave-dominated coast? Mar Geol 60:313–329įisher JJ (1962) Geomorphic expression of former inlets along the Outer Banks of North Carolina. In: Cronin LE (ed) Estuarine research, vol 2. Mar Geol 63:35–76īyrne RJ, Bullock P, Taylor DG (1975) Response characteristics of a tidal inlet: a case study. In: Oertel GF, Leatherman SP (eds) Barrier islands. ASCE, pp 1489–1504īoothroyd JC, Friedrich NE, McGinn SR (1985) Geology of microtidal coastal lagoons, RI. J Geol 92:531–546īarnard PL, Davis RA (1999) Anthropogenic versus natural influences on inlet evolution: West-Central Florida. Academic, New York, pp 65–80Īubrey DG, Speer PE (1984) Updrift migration of tidal inlets. In: Leatherman SP (ed) Barrier islands: from the Gulf of St. This process is experimental and the keywords may be updated as the learning algorithm improves.Īrmon JW (1979) Landward sediment transfers in a transgressive barrier island system, Canada. These keywords were added by machine and not by the authors. The variability in oceanographic, meteorologic, and. The large number of improvements that are performed at the entrance to inlets such as the construction of jetties and breakwaters, dredging of channels, and the operation of sand bypassing facilities demonstrate the importance of inlets in providing navigation routes to these harborages.ĭiversity in the morphology, hydraulic signature, and sediment transport patterns of tidal inlets attest to the dynamics and complexity of their processes. In addition, along many coastal plain settings, including much of the East and Gulf Coasts of the United States, the southern and western coasts of the North Sea, and along many deltaic coasts, the only safe harborages, including major ports, are found behind barrier islands. They serve as natural conduits for the exchange of water, nutrients, and organisms between coastal ocean and the backbarrier. Tidal inlets are an integral part of coastal barrier systems throughout the world.
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