4.7 Article

Interaction of a solitary wave with an array of macro-roughness elements in the presence of steady currents

Journal

COASTAL ENGINEERING
Volume 164, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.coastaleng.2020.103829

Keywords

Turbulence; Vorticity; LES; Wave-current interaction; Wave-structure interaction

Funding

  1. New York State Energy Research and Development Authority (NYSERDA) [105162]

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This study investigates the effects of following and opposing steady currents on the interactions of a solitary wave with an array of macro-roughness elements on a berm beach. Both laboratory experiments and high-fidelity numerical simulations are conducted, revealing that the currents significantly influence the wave breaking conditions and runup patterns on the beach. The presence of currents also alters the formation of vortices around the roughness elements.
The present study focuses on the effects of following and opposing steady currents on the interactions of a solitary wave with an array of macro-roughness elements, placed on a berm beach. A series of laboratory experiments and high-fidelity numerical simulations are conducted. The large eddy simulations are carried out using the open source computational fluid dynamics package, OpenFOAM. Wave breaking conditions on the berm are found to be controlled by the intensity of the currents. The opposing currents influence the layer of water rushing up the macro-roughness elements, leading to asymmetric runup patterns. Furthermore, the vortices forming around the elements' sharp edges, resulting from the interactions of the wave with the elements, are modified to a large extent due to the combined wave and current effect. The elliptical vortex tubes become up to (similar to)20% wider under the effect of the following current flow, whereas their size is reduced by up to (similar to)90% when the opposing currents are present. The following currents enhance the bed shear velocity, leading to intensified bed shear stress zones throughout the macro-roughness environment. On the other hand, the intensification of the bed shear velocity and corresponding stress occurs on the seaside in the presence of opposing currents. Overall, the results indicate that the currents entirely change the hydrodynamics of the interactions between the solitary wave and macro-roughness environment.

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