Abstract

In the present work, an experimental investigation on the hydrodynamics of shoaling waves superposed on a steady orthogonal current is carried out. An experimental campaign in a wave tank has been performed, with waves and current interacting at a right angle over a sloping planar beach. Velocity data have been gathered during the experiments in order to investigate mean, phase and turbulent flow. A detailed preliminary analysis of the time- and space-variability of the experiments is presented. Results show that a complex interaction between waves and current occurs as the wave shoals, in terms of sheer production, momentum transfer and turbulent mixing. Superposition of waves determines a shear increase at the bottom due to an enhanced turbulence mixing, nonetheless as depth decreases and the current velocity consequently increases, shoaling waves may be less efficient in enhancing shear at the bottom. Moreover, the superposition of waves determines the current to oscillate around its mean velocity value. Nevertheless, as wave shoals and simultaneously current velocity increases with decreasing depth, waves and current oscillatory motion experience a phase lag, as a response of the larger momentum of the current to the changing of the shoaling waves acceleration distribution along the wave phase. Moreover, the turbulent bursting events of the combined flow in proximity of the bed have been investigated by means of quadrant analysis, showing an increase of the turbulent ejections and sweeps due to the superposition of the shoaling waves.

Highlights

  • Waves and currents are generally simultaneously present in coastal environments

  • In the present work an experimental investigation on shoaling waves interacting at a right angle with a current has been carried out

  • The study aimed to investigate how the hydrodynamic field of a steady current is affected by the superposition of orthogonal waves which progressively shoals over a planar beach

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Summary

Introduction

Waves and currents are generally simultaneously present in coastal environments. It is widely known that the superposition of waves significantly alters the mean current flow hydrodynamics, their combined flow drives important coastal processes such as sediment transport. Results showed that the presence of ripples acts as a macroroughness, inducing turbulence to intensify and current apparent roughness to increase. Fernando et al [13] carried out experiments on WCI at a right angle in a wave basin over a movable horizontal bed and compared results with theoretical nonlinear models of wave-current combined flow. Faraci et al [20] gathered near-bed velocity statistics of WCI at a right angle over different roughness elements: sand, gravel and ripples. The probability density function of near-bed velocities showed a Gaussian distribution for the current only case, whereas a double peak distribution was observed in the combined flow. An investigation on turbulent flow was carried out, showing an alteration of near-bed high order velocity statistics, such as skewness and kurtosis, due to the effects of the oscillatory flow on the current. The presence of nonlinear waves may induce a veering of the current from its main direction due to turbulence asymmetry

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