By Mick van der Wegen

ISBN-10: 0415592747

ISBN-13: 9780415592741

The most goal of this learn is to enquire the governing approaches and features that force morphodynamic evolution in alluvial estuaries by way of program of a process-based numerical version (Delft3D). it's of extreme significance to appreciate estuarine tactics in order that effect of human interference (like dredging and land reclamation) and long term alterations (like sea point upward push) could be evaluated. The examine addresses a few situations starting from an oblong basins to genuine estuaries just like the Western Scheldt within the Netherlands or San Pablo Bay in California. The extra schematized method let to review morphodynamic evolution over a number of millennia below consistent forcing and solutions extra primary questions concerning stipulations of equilibrium and comparable time scales. The extra real looking instances provide perception into the ability of the process in predicting decadal morphodynamic advancements. extra procedures are integrated to imitate practical stipulations and version effects are in comparison to bathymetric measurements over the past century. The study exhibits that the modeling strategy is nice able to describing strong morphodynamic calculations over a timescale of millennia with styles just like styles saw in fact. also, the process exhibits that it truly is attainable to foretell decadal morphodynamic advancements in genuine estuaries with major ability.

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Extra info for Modeling morphodynamic evolution in alluvial estuaries: UNESCO-IHE PhD Thesis

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The current model applies an approach that includes drying and flooding of the intertidal area developing near the head. The results show a continuous sedimentation at the head. Furthermore, shallower initial conditions will lead to more sedimentation. The sedimentation process only decreases because the deepening of the more seawardlocated profile leads to lower transport rates towards the head. The shape of the evolving profile remains similar for different initial conditions. This supports the suggestion that the profiles after 8000 years are close to equilibrium.

E. waves and/or tides) and model configuration. Its final 24 Chapter 1. Framework for morphodynamic modelling in alluvial estuaries value needs to be determined per case. The results of an extensive sensitivity analysis of different values of the MF are discussed more closely in upcoming sections. 4 Dry cell erosion The advantage of using a morphological factor is that it accelerates the morphodynamic calculations in such a way that the computational effort can be drastically decreased. The disadvantage of high values of the morphological factor is that it may lead to a wrong description of the physical processes, because erosion and deposition processes are extrapolated.

1990), Toffolon (2006), Savenije et al. (2008)]. Also, morphodynamics may be included to study width-averaged longitudinal profile development and equilibrium conditions. An example is the work by Schuttelaars and De Swart (1996, 2000) and Hibma (2003a) who developed an idealized 1D model of a rectangular tidal embayment to study the existence of profile equilibrium and its sensitivity to basin length, the presence of overtides and the relative strength of diffusive and advective transports. Other examples are the work by Lanzoni and Seminara (2002) who investigated the 1D morphodynamic equilibrium of a funnel shaped embayment.

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Modeling morphodynamic evolution in alluvial estuaries: UNESCO-IHE PhD Thesis by Mick van der Wegen


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