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• W2558554482 abstract "In terms of grain size, surficial sediment distribu- tion patterns in back-barrier tidal basins (e.g., the East Frisian Wadden Sea, Germany) often show a landward fining trend fromtheseaboundarytothemainlandshore.Inadditiontothe cross-shore patterns, there are lateral grain-size trends toward the watersheds of the basins and toward the watersheds of tidal flats bordered by tidal channels on either side. In the present study, interrelationships between morphological evo- lution and grain-size trends in the back-barrier tidal basins of the East Frisian Wadden Sea were simulated for a period of 60years byaprocess-based forward modelingapproachusing the Delft3D system. The model outputs show that grain size displays a shoreward fining trend within the basin area, which is consistent with in situ observations; such a trend can be interpreted by the shoreward decrease in the cross-shore max- imumvelocity. Moreover, the model predictslateral grain-size trends similar to those observed in the tidal basins: coarser sediment remains in the inlets and channels, while finer sed- iment settles at the tidal watersheds and on the tidal flats between channels. The spatial patterns of tidal flat sediment grainsizewithinthetidalbasinsarethusrelatedtothedistance from the sea boundary and from the tidal channels. The modeling exercise also indicates that the development of the grain-size pattern observed in the East Frisian Wadden Sea is accomplished within a few decades, and that the time periods required to reach equilibrium are much shorter for grain size than for bed elevation. Evidently, spatial grain-size informa- tion can be used to assess sediment transport and morpholog- ical adaptation processes as, for example, attempted in sedi- ment trend analysis procedures." @default.
• W2558554482 created "2016-12-08" @default.
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• W2558554482 date "2014-01-01" @default.
• W2558554482 modified "2023-09-26" @default.
• W2558554482 title "Modeling interrelationships between morphological evolution and grain-size trends in back-barrier tidal basins of the East" @default.
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