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Hydrodynamic modelling of tidal-fluvial flows in a large river estuary

Sandbach, S.D.; Nicholas, A.P.; Ashworth, P.J.; Best, J.L.; Keevil, C.E.; Parsons, D.R.; Prokocki, E.W.; Simpson, C.J.

Authors

S.D. Sandbach

A.P. Nicholas

P.J. Ashworth

J.L. Best

C.E. Keevil

E.W. Prokocki

C.J. Simpson

Abstract

© 2018 The Authors The transition between riverine and estuarine environments is characterised by a change from unidirectional to bidirectional flows, in a region referred to herein as the Tidally-Influenced Fluvial Zone (TIFZ). In order to improve our understanding of the hydrodynamics and morphodynamics of this zone, we present a combined field and numerical modelling study of the Columbia River Estuary (CRE), USA, tidally-influenced fluvial zone. The CRE is large measuring 40 km in length and between 5 and 10 km wide. A shallow water model (Delft3D) was applied in both 2D and 3D configurations and model sensitivity to the key process parameterizations was investigated. Our results indicate that a 2D model constrained within the estuary can sufficiently reproduce depth-averaged flow within the TIFZ of a stratified estuary. Model results highlight the interactions between tidal-, fluvial- and topographic-forcing that result in depth dependent tidal rectification, and thus zones of residual sediment transport that: i) may be flood-directed along shallow channel margins and in the lee of bars, and simultaneously ii) is ebb-directed within deeper channel thalwegs. This condition is enhanced at lower discharges, but increased fluvial discharge reduces the number and size of regions with net flood-directed sediment transport and flow. These sediment transport patterns provide a mechanism to extend the bar/island topography downstream, and generate flood-directed, ebb-directed, and symmetrical bedforms, all within the same channel. Analysis of the model data reveals flood-directed sediment transport is due to both tidal variability and mean flow. These results highlight the need to include the mean flow component (M0) when considering the long-term morphodynamic evolution in a TIFZ.

Journal Article Type Article
Publication Date Nov 15, 2018
Journal Estuarine, Coastal and Shelf Science
Print ISSN 0272-7714
Publisher Elsevier
Peer Reviewed Peer Reviewed
Volume 212
Pages 176-188
Institution Citation Sandbach, S., Nicholas, A., Ashworth, P., Best, J., Keevil, C., Parsons, D., …Simpson, C. (2018). Hydrodynamic modelling of tidal-fluvial flows in a large river estuary. Estuarine, coastal and shelf science, 212, 176-188. https://doi.org/10.1016/j.ecss.2018.06.023
DOI https://doi.org/10.1016/j.ecss.2018.06.023
Keywords Sediment transport; Tidal constituent; Residual flow; Tidal-fluvial interactions; Columbia river estuary; Model parameterisation
Publisher URL https://www.sciencedirect.com/science/article/pii/S0272771417310843?via%3Dihub

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Copyright Statement
This work is licensed under a Creative Commons Attribution 4.0 International License.



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