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A logarithmic bottom boundary layer model for the unsteady and non-uniform swash flow

Zhu, Fangfang; Dodd, Nicholas; Briganti, Riccardo; Larson, Magnus

A logarithmic bottom boundary layer model for the unsteady and non-uniform swash flow Thumbnail


Authors

Fangfang Zhu

NICHOLAS DODD NICHOLAS.DODD@NOTTINGHAM.AC.UK
Professor of Coastal Dynamics

Magnus Larson



Abstract

This paper presents a bottom boundary layer model for the unsteady and non-uniform flow in the swash zone, by extending the momentum integral method so as to include spatial gradients. The developed model is further incorporated into a hydrodynamic model based on the Nonlinear Shallow Water Equations. Two swash zone cases are examined to investigate the effect of the inclusion of spatial gradients. In the first of the two, boundary layer development under non-breaking periodic waves formulated by Carrier and Greenspan (1958) is investigated (wave-driven swash). Results show that the spatial gradients have the most pronounced effect in the lower swash, and in the region just seaward. In both these regions the spatial gradients enhance (diminish) onshore (offshore) bed shear stress, thus potentially contributing to onshore sediment transport under non-breaking waves. The second case investigated is the Kikkert et al. (2012) dam-break swash event (bore-driven swash). The model results are qualitatively and quantitatively accurate when compared against the laboratory measurements, and the velocities in the later backwash agree more closely with the measurements than those of Briganti et al. (2011). Results show that the inclusion of spatial gradients also favours onshore sediment transport in the lower swash. In addition, the bottom boundary layer is more fully developed in the uprush tip, resulting in smaller bed shear stress in the upper swash. The extended momentum integral method thus appears to capture more comprehensively the swash boundary layer, and the approach, therefore, offers a way forward in more accurate reproduction of swash dynamics in computational modelling.

Citation

Zhu, F., Dodd, N., Briganti, R., & Larson, M. (2022). A logarithmic bottom boundary layer model for the unsteady and non-uniform swash flow. Coastal Engineering, 172, Article 104048. https://doi.org/10.1016/j.coastaleng.2021.104048

Journal Article Type Article
Acceptance Date Nov 7, 2021
Online Publication Date Nov 20, 2021
Publication Date 2022-03
Deposit Date Nov 12, 2021
Publicly Available Date Nov 21, 2022
Journal Coastal Engineering
Print ISSN 0378-3839
Electronic ISSN 0378-3839
Publisher Elsevier
Peer Reviewed Peer Reviewed
Volume 172
Article Number 104048
DOI https://doi.org/10.1016/j.coastaleng.2021.104048
Keywords Ocean Engineering; Environmental Engineering
Public URL https://nottingham-repository.worktribe.com/output/6681275
Publisher URL https://www.sciencedirect.com/science/article/abs/pii/S0378383921001885

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