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- W2334347456 abstract "Tidal bores are peculiar waves that propagate upwards in shallow estuaries, after low tide reversal. The aim of this study is to quantify suspended sediment transport in the presence of such bores in the upper Gironde estuary. Turbidity was recorded at 140 km upstream from the mouth, for two contrasted river flow regimes. Results show that during the dry season, near-bed concentration reach levels of fluid mud. The highest tidal bores generate intense resuspension and an upward suspended sediment flux, 30 times greater than that of the final ebb. However, the bore-induced fluxes are weak in comparison with later advection by flood tidal currents. The river discharge, because its effect on the turbidity maximum, controls mean turbidity in the upper estuary, and therefore the relative impact of tidal bores on fine sediment transport." @default.
- W2334347456 created "2016-06-24" @default.
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- W2334347456 date "2012-01-01" @default.
- W2334347456 modified "2023-09-24" @default.
- W2334347456 title "Dynamique des suspensions estuariennes en présence de mascarets (cas de la Garonne)" @default.
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- W2334347456 doi "https://doi.org/10.5150/jngcgc.2012.048-s" @default.
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