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- W2314702967 abstract "Two shoal-bypassing events at the updrift end of Kiawah Island, South Carolina (USA), between 1990 and 2006 added ~4 million cubic meters (m3) of sand and created a 5-kilometer-long barrier beach/lagoon system. The volumes in the bypassing shoals were sufficient to advance the shoreline over 500 meters (m) and to form an ~100-hectare lagoon. Oceanic habitat was rapidly transformed to sheltered lagoon/marsh habitat with salt marsh dominating the lagoon within ~10 years. The accretion density of the bypassing shoals was ~1,000 m3/m relative to the prior shoreline. This volume input accounts for the large advancement of the shoreline. Habitat evolution is being monitored via ground surveys and digital terrain models using sitespecific elevation criteria for intertidal zones, washover areas, and marsh expansion. The shoal-bypassing events at Kiawah Island are believed to dwarf volumes of any previously documented event. The barrier-beach/lagoon system formed by the episodic influxes of sand demonstrates the potential rapidity of barrier-island formation. Unit accretion density is a simple parameter that can be used to project the shoreline displacement and ultimate width of the lagoon." @default.
- W2314702967 created "2016-06-24" @default.
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- W2314702967 date "2011-04-01" @default.
- W2314702967 modified "2023-09-25" @default.
- W2314702967 title "BARRIER ISLAND HABITAT CREATION AT DECADAL SCALES" @default.
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- W2314702967 doi "https://doi.org/10.1142/9789814355537_0088" @default.
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