Hydrodynamics and sediment dynamics in the German Bight. A focus on observations and numerical modelling in the East Frisian Wadden Sea |
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| Authors: | Joanna Staneva Emil V Stanev Jörg-Olaf Wolff Thomas H Badewien Rainer Reuter Burghard Flemming Alexander Bartholomä Karsten Bolding |
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| Institution: | 1. Institute for Chemistry and Biology of the Sea(ICBM), University of Oldenburg, Carl-von-Ossietzky-Strasse 9-11, D-26111 Oldenburg, Germany;2. School of Environmental Science, University of Ulster, Cromore Road, Coleraine, BT52 1SA, UK;3. Institute of Physics, University of Oldenburg, Carl-von-Ossietzky-Strasse 9-11, D-26111 Oldenburg, Germany;4. Senckenberg Institute, Department for Marine Science, Südstrand 40, D-26382 Wilhelmshaven, Germany;5. Bolding and Burchard Hydrodynamics, Strandgyden 25, DK-5466 Asperup, Denmark |
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| Abstract: | This work deals with analysis of hydrographic observations and results of numerical simulations. The data base includes acoustic Doppler current profilers (ADCP) observations, continuous measurements on data stations and satellite data originating from the medium resolution imaging spectrometer (MERIS) onboard the European Space Agency (ESA) satellite ENVISAT with a spatial resolution of 300 m. Numerical simulations use nested models with horizontal resolutions ranging from 1 km in the German Bight to 200 m in the East Frisian Wadden Sea coupled with a suspended matter transport model. Modern satellite observations have now a comparable horizontal resolution with high-resolution numerical model of the entire area of the East Frisian Wadden Sea allowing to describe and validate new and so far unknown patterns of sediment distribution. The two data sets are consistent and reveal an oscillatory behaviour of sediment pools to the north of the back-barrier basins and clear propagation patterns of tidally driven suspended particulate matter outflow into the North Sea. The good agreement between observations and simulations is convincing evidence that the model simulates the basic dynamics and sediment transport processes, which motivates its further use in hindcasting, as well as in the initial steps towards forecasting circulation and sediment dynamics in the coastal zone. |
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| Keywords: | Ocean circulation Sediment dynamics Tidal basins Nested models |
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