Current measurement by use of synchronous wave probes: Method and example of laboratory experiments for progressive or partially standing waves

In the context of studies of interactions between waves and currents, a method of calculation of the current through synchronous free surface deformation measurements at various locations is proposed and discussed in the case of either progressive or partially standing waves, and for either homogeneous or vertically sheared current. For partially standing waves, the method takes advantage of separation of incident and reflected wave method through minimization algorithms, which are still applicable in the limit case of a progressive wave. Discussions on the accuracy of the method are based on comparisons to laboratory experiments including regular and irregular waves in following or opposite current conditions. The vertically averaged current is recovered since current has a significant influence on the wave celerity. Vertically shear has less influence on the wave celerity in comparison to the averaged current in the experimental conditions considered, and is hardly directly recovered because of the noise inherent to the measurements. However the shear can be estimated through the calculated vertically averaged current which depends on frequency in the presence of shear. The present study concerns the unidirectional case, including regular or irregular waves.

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Publication Details

Journal
Applied Ocean Research
Published
2024-12-25
DOI
https://doi.org/10.1016/j.apor.2024.104386
Primary Topic
Ocean Waves and Remote Sensing
Type
article
Field-Weighted Citation Impact
0.00

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article

Current measurement by use of synchronous wave probes: Method and example of laboratory experiments for progressive or partially standing waves

Fabrice Ardhuin, Julien Touboul, Vincent Rey, Alfredo Cuevas
Applied Ocean Research
Ocean Waves and Remote Sensing
article

Current measurement by use of synchronous wave probes: Method and example of laboratory experiments for progressive or partially standing waves

Fabrice Ardhuin, Julien Touboul, Vincent Rey, Alfredo Cuevas
article en

Abstract

In the context of studies of interactions between waves and currents, a method of calculation of the current through synchronous free surface deformation measurements at various locations is proposed and discussed in the case of either progressive or partially standing waves, and for either homogeneous or vertically sheared current. For partially standing waves, the method takes advantage of separation of incident and reflected wave method through minimization algorithms, which are still applicable in the limit case of a progressive wave. Discussions on the accuracy of the method are based on comparisons to laboratory experiments including regular and irregular waves in following or opposite current conditions. The vertically averaged current is recovered since current has a significant influence on the wave celerity. Vertically shear has less influence on the wave celerity in comparison to the averaged current in the experimental conditions considered, and is hardly directly recovered because of the noise inherent to the measurements. However the shear can be estimated through the calculated vertically averaged current which depends on frequency in the presence of shear. The present study concerns the unidirectional case, including regular or irregular waves.

Applied Ocean ResearchVol. 154
Centre National de la Recherche Scientifique (FR), Ifremer (FR), Université de Bretagne Occidentale (FR), Laboratory for Ocean Physics and Satellite Remote Sensing (FR), Centrale Méditerranée (FR), Institut Méditerranéen d’Océanologie (FR), Institut de Recherche pour le Développement (FR)
Agence Nationale de la Recherche, Agence de l'innovation de Défense, Division of Grants and Agreements
Affordable and clean energy
Openalex Percentile: Top 75%
Ocean Waves and Remote Sensing
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