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- W2326205770 abstract "Extended sand banks ranging up to some hundred acres with a crest height in the MHW-level are typical structures of the outer tidal flats of the south-eastern North Sea coast (Fig. 1). Primary forms grow up in the surf zone at the sea-side tidal flat border. They are formed like bars and migrate towards the coast with a surprisingly high velocity, up to 150 m/year. The movement is caused by strong erosion on the sea-side slope - which is shaped beach-like - and deposition at the steeper land-side (lee-side) slope. It was found that surf action at the bar is linked with strong unidirectional currents across the crest, Up to 100 cm/s. The currents are most likely generated by wave set-up in front of the bank and by wind-drift water motion." @default.
- W2326205770 created "2016-06-24" @default.
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- W2326205770 date "1974-01-29" @default.
- W2326205770 modified "2023-09-25" @default.
- W2326205770 title "DYNAMICS AND MORPHOLOGY OF SAND BANKS IN THE SURF ZONE OF OUTER TIDAL FLATS" @default.
- W2326205770 doi "https://doi.org/10.9753/icce.v14.50" @default.
- W2326205770 hasPublicationYear "1974" @default.
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