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- W1963790290 abstract "An ephemeral river delta on the wave-dominated Central California coast was studied to determine how and when river sand was incorporated into the longshore transport regime. The delta, at the mouth of the San Lorenzo River, was built in January 1982 by a 30-year flood. Records of river flow, sediment load and channel volume were used to estimate the river sediment yield. Repeated topographic surveys of the delta and surrounding beaches confirmed the estimates of river yield and traced sand movement from the river mouth. Directional wave data confirmed the direction of longshore sand movement and identified sites of erosion and accretion due to divergence in the longshore transport. Most sand delivered to the delta in flood was deposited seaward of the surfzone. About a quarter of this sand was returned shoreward each summer by swell. For a time, wave refraction across the submerged delta trapped the river sand and littoral drift from upcoast on the delta, limiting the sand supply to the beaches downcoast. As storm waves broadened the delta, refraction lessened and the river sand began to disperse alongshore. Longshore dispersion was assisted by seasonal cross-shore movements: directly, through a net longshore creep; and indirectly, through the return of sand from offshore to the surfzone transport. The overall pattern of river sand dispersion was that of a low-amplitude sandwave." @default.
- W1963790290 created "2016-06-24" @default.
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- W1963790290 date "1987-08-01" @default.
- W1963790290 modified "2023-10-17" @default.
- W1963790290 title "Sand dispersion from an ephemeral river delta on the Central California coast" @default.
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- W1963790290 doi "https://doi.org/10.1016/0025-3227(87)90119-8" @default.
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