Shoaling Waves Interacting with an Orthogonal Current

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 da...

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Main Authors: Massimiliano Marino, Carla Faraci, Rosaria Ester Musumeci
Format: Article
Language:English
Published: MDPI AG 2020-04-01
Series:Journal of Marine Science and Engineering
Subjects:
Online Access:https://www.mdpi.com/2077-1312/8/4/281
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spelling doaj-2d11d687c1c54934b38a45152815d3292021-04-02T13:28:49ZengMDPI AGJournal of Marine Science and Engineering2077-13122020-04-01828128110.3390/jmse8040281Shoaling Waves Interacting with an Orthogonal CurrentMassimiliano Marino0Carla Faraci1Rosaria Ester Musumeci2Department of Civil Engineering and Architecture, University of Catania, 95123 Catania, ItalyDepartment of Engineering, University of Messina, 98166 Messina, ItalyDepartment of Civil Engineering and Architecture, University of Catania, 95123 Catania, ItalyIn 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.https://www.mdpi.com/2077-1312/8/4/281nearshore hydrodynamicswave-current interactionnonlinear wavessediment transportquadrant analysis
collection DOAJ
language English
format Article
sources DOAJ
author Massimiliano Marino
Carla Faraci
Rosaria Ester Musumeci
spellingShingle Massimiliano Marino
Carla Faraci
Rosaria Ester Musumeci
Shoaling Waves Interacting with an Orthogonal Current
Journal of Marine Science and Engineering
nearshore hydrodynamics
wave-current interaction
nonlinear waves
sediment transport
quadrant analysis
author_facet Massimiliano Marino
Carla Faraci
Rosaria Ester Musumeci
author_sort Massimiliano Marino
title Shoaling Waves Interacting with an Orthogonal Current
title_short Shoaling Waves Interacting with an Orthogonal Current
title_full Shoaling Waves Interacting with an Orthogonal Current
title_fullStr Shoaling Waves Interacting with an Orthogonal Current
title_full_unstemmed Shoaling Waves Interacting with an Orthogonal Current
title_sort shoaling waves interacting with an orthogonal current
publisher MDPI AG
series Journal of Marine Science and Engineering
issn 2077-1312
publishDate 2020-04-01
description 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.
topic nearshore hydrodynamics
wave-current interaction
nonlinear waves
sediment transport
quadrant analysis
url https://www.mdpi.com/2077-1312/8/4/281
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