IMPACTS OF INLET MIGRATION ON BARRIER ISLAND PLANFORM AND OCEANFRONT CHANGES: NEW TOPSAIL INLET, NC
The migration of the inlet has promoted the development of an expanding erosion hot spot along southern portion of Topsail Beach. During the 1950-1970 development phase, structures were constructed along the primary dune ridge paralleling the recurved portion of the southwesterly extending spit. During the 1960's, the southern 2.0 km of the barrier assumed a pronounced bulbous shape that was a by-product of spit accretion and updrift bar welding associated with the cyclical reorientation of the ebb channel. Chronic erosion that has characterized the southern 3.0 km of oceanfront stemmed in part from the realignment of the trailing shoreline's planform as the inlet migrated. Oceanfront erosion rates between 1974 and 1986 ranged from 1.6 - 5.2 m/yr reflecting increased migration rates. The chronic erosion has been a major management problem and due to the prohibition of shoreline hardening structures the only viable option available for erosion mitigation is beach nourishment. However, the success of the recently proposed major re-nourishment project is likely to be short considering the inlet's history and the poor performance of previous projects.