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

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

Research output: Contribution to journalArticlepeer-review


The transition between riverine and estuarine environments is characterised by a transition 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.
Original languageEnglish
Pages (from-to)176-188
JournalEstuarine, Coastal and Shelf Science
Publication statusPublished - 27 Jun 2018

Bibliographical note

© 2018 The Authors. Published by Elsevier Ltd. This is an open access article under the CC BY license (http://creativecommons.org/licenses/BY/4.0/).


  • Sediment transport
  • Tidal constituent
  • Residual flow
  • Tidal-fluvial interactions
  • Columbia river estuary
  • Model parameterisation


Dive into the research topics of 'Hydrodynamic modelling of tidal-fluvial flows in a large river estuary'. Together they form a unique fingerprint.

Cite this