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• W2316716639 abstract "Rates of relative sea level rise in excess of 1 cm/yr are forcing rapid landward migration of barrier/tidal inlet systems along coastal Louisiana. Additionally, the conversion of interior wetlands to open water increases tidal prism, resulting in barrier degradation by means of increased inlet cross-sectional area and sediment sequestration in ebb tidal deltas. Historical bathymetric maps (dating to the 1880's) and up-to-date bathymetric data for Little Pass Timbalier provide a time series that shows the morphological evolution of this tidal inlet. The historical evolution includes: landward and lateral migration of its main channel (44 m/yr and 28 m/yr, respectively); changes in inlet throat geometry; and formation of a new stable ebb channel. The inlet throat cross-sectional area increased from 3,117 m2 in 1880 to 17,510 m2 in 2005. The ebb tidal delta is prograding seaward leaving a quasi-progradational sand body on the inner shelf as the barrier islands migrate landward." @default.
• W2316716639 created "2016-06-24" @default.
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• W2316716639 date "2007-05-11" @default.
• W2316716639 modified "2023-09-25" @default.
• W2316716639 title "1880 to 2005 Morphologic Evolution of a Transgressive Tidal Inlet, Little Pass Timbalier, Louisiana" @default.
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• W2316716639 doi "https://doi.org/10.1061/40926(239)90" @default.
• W2316716639 hasPublicationYear "2007" @default.
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