Water Science and Engineering 2020, 13(1) 1-13 DOI:    https://doi.org/10.1016/j.wse.2020.03.004  ISSN: 1674-2370 CN: 32-1785/TV

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Keywords
Tidal inlet and estuary
Morphodynamic modelling
Aggregation
Temporal and spatial scales
Sea level rise
Equilibrium sediment transport
Authors
PubMed

Aggregated morphodynamic modelling of tidal inlets and estuaries

Zheng Bing Wang a, b, c, Ian Townend b, d, *, Marcel Stive a, b

a Faculty of Civil Engineering and Geosciences, Delft University of Technology, Delft 2600 GA, the Netherlands
b College of Harbor, Coastal and Offshore Engineering, Hohai University, Nanjing 210098, China
c Unit of Marine and Coastal Systems, Deltares, Delft 2600 MH, the Netherlands
d School of Ocean and Earth Sciences, University of Southampton, Southampton SO16 7QF, UK

Abstract

Aggregation is used to represent the real world in a model at an appropriate level of abstraction. We used the convection-diffusion equation to examine the implications of aggregation progressing from a three-dimensional (3D) spatial description to a model representing a system as a single box that exchanges sediment with the adjacent environment. We highlight how all models depend on some forms of parametric closure, which need to be chosen to suit the scale of aggregation adopted in the model. All such models are therefore aggregated and make use of some empirical relationships to deal with sub-scale processes. One such appropriately aggregated model, the model for the aggregated scale morphological interaction between tidal basin and adjacent coast (ASMITA), is examined in more detail and used to illustrate the insight that this level of aggregation can bring to a problem by considering how tidal inlets and estuaries are impacted by sea level rise.

Keywords Tidal inlet and estuary   Morphodynamic modelling   Aggregation   Temporal and spatial scales   Sea level rise   Equilibrium sediment transport  
Received 2019-09-16 Revised 2020-02-10 Online: 2020-03-30 
DOI: https://doi.org/10.1016/j.wse.2020.03.004
Fund:
Corresponding Authors: Ian Townend
Email: i.townend@soton.ac.uk
About author:

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