NON-EQUILIBRIUM WAVE STATISTICS IN COASTAL AREA ASSOCIATED WITH STRONG VARIATIONS OF WATER DEPTH AND AMBIENT CURRENT

Freak waves, usually defined as waves with crest-to-trough heights exceeding twice the significant wave height Hs (e.g. Dysthe et al., 2008), pose a significant risk to maritime and ocean engineering (Didenkulova et al., 2023). These anomalous waves occur under various conditions but are particularly hazardous in coastal regions with intense human activity (Li and Chabchoub, 2023). In this study, we present experimental evidence demonstrating that, as waves propagate over an uneven bottom with the presence of uniform following current, the mean flow velocity varies according to the changes of local water depth, and the inhomogeneity of current in the direction of wave propagation leads to non-equilibrium dynamics (NED). As a result, the freak wave probability is further enhanced by a following current, which was considered the opposite in the regime of MI (Toffoli et al., 2015).

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Publication Details

Journal
Coastal Engineering Proceedings
Published
2025-05-29
DOI
https://doi.org/10.9753/icce.v38.waves.20
Primary Topic
Ocean Waves and Remote Sensing
Type
article
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article

NON-EQUILIBRIUM WAVE STATISTICS IN COASTAL AREA ASSOCIATED WITH STRONG VARIATIONS OF WATER DEPTH AND AMBIENT CURRENT

Michel Benoît, Yuxiang Ma, Jie Zhang
Coastal Engineering Proceedings
Ocean Waves and Remote Sensing
article

NON-EQUILIBRIUM WAVE STATISTICS IN COASTAL AREA ASSOCIATED WITH STRONG VARIATIONS OF WATER DEPTH AND AMBIENT CURRENT

Michel Benoît, Yuxiang Ma, Jie Zhang
article en

Abstract

Freak waves, usually defined as waves with crest-to-trough heights exceeding twice the significant wave height Hs (e.g. Dysthe et al., 2008), pose a significant risk to maritime and ocean engineering (Didenkulova et al., 2023). These anomalous waves occur under various conditions but are particularly hazardous in coastal regions with intense human activity (Li and Chabchoub, 2023). In this study, we present experimental evidence demonstrating that, as waves propagate over an uneven bottom with the presence of uniform following current, the mean flow velocity varies according to the changes of local water depth, and the inhomogeneity of current in the direction of wave propagation leads to non-equilibrium dynamics (NED). As a result, the freak wave probability is further enhanced by a following current, which was considered the opposite in the regime of MI (Toffoli et al., 2015).

Coastal Engineering Proceedings(38)
Openalex Percentile: Top 52%
Ocean Waves and Remote Sensing
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