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- W2018901126 abstract "The Ebro Delta coast is a microtidal, sandy shoreline affected by a low-energy mean wave climate. Consecutive topographical and bathymetrical surveys during the years 1990 and 1991 have allowed us to identify nine major longshore bar and trough systems as the main morphological feature of the Ebro coast. Bar systems show high mobility, both cross-shore and longshore. The cross-shore migration of these systems may be landward or seaward, with mean migration rates of up to 0.25 m/day. The longshore migration is produced by the longitudinal growth of the bar systems in the downdrift direction, with rates of up to 11 m/day. The major morphological changes in the nearshore zone occurred during storm periods, when the nearshore profile is modified as a consequence of shoreline erosion and the cross-shore migration and longshore growth of the bar systems produced by these events. The modifications in the nearshore profile may continue during some months after the storm, before attaining a new equilibrium profile. A descriptive model relating the shoreline displacement with the cross-shore migration and the longshore growth of the bar and trough systems is proposed." @default.
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- W2018901126 date "1993-12-01" @default.
- W2018901126 modified "2023-10-12" @default.
- W2018901126 title "Longshore bar and trough systems in a microtidal, storm-wave dominated coast: The Ebro Delta (Northwestern Mediterranean)" @default.
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- W2018901126 doi "https://doi.org/10.1016/0025-3227(93)90053-x" @default.
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