Fourth-order Stokes theory for capillary–gravity waves in arbitrary water depth on linear shear currents

In this paper the two-dimensional steady surface capillary–gravity waves, incorporating the effects of linear shear currents, is studied in water of constant depth. Herein, linear shear currents are considered to be a linear combination of depth-uniform current and uniform vorticity. Employing an excellent Stokes expansion method, where the expansion parameter represents the wave steepness itself, a fourth-order perturbation series solution for plane progressive waves is developed. The key results of this work are (a) to find the influence of both co-flowing and counter-flowing currents on the wave profiles using the fourth-order approximation (b) the strong dependence of the wave velocity on both the magnitudes of the shear and depth-uniform current, (c) the Wilton singularities in the Stokes expansion in powers of wave amplitude due to a inverse Bond number of 1 / 2 , 1 / 3 and 1 / 4 , which are the results of the non-uniformity in the ordering of the Fourier coefficients are observed to be influenced by vorticity and depth-uniform current, (d) distinct surface profiles of capillary–gravity waves are obtained and the effects of depth-uniform currents on these profiles are described. This analysis also shows that for any given value of the water depth, there exist a threshold value of the vorticity above which no resonances occur. For the steepest waves considered in this analysis, it is observed that when the wavenumber is not in the vicinity of certain critical values, determined by the depth and the vorticity, the present fourth-order analysis shows significant deviations on the surface profiles from the third-order analysis and provides better results consistent with the exact numerical results. • In this note we find the effect of vorticity on the critical wavenumbers. • The strong dependence of the wave velocity on the magnitude of the shear is obtained. • For given water depth, there exists a threshold value of the vorticity above which no resonances occur. • The influence of depth uniform current on the wave profiles is investigated.

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Publication Details

Journal
Wave Motion
Published
2025-04-01
DOI
https://doi.org/10.1016/j.wavemoti.2025.103546
Citations
1
Primary Topic
Ocean Waves and Remote Sensing
Type
article
Field-Weighted Citation Impact
1.79
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article

Fourth-order Stokes theory for capillary–gravity waves in arbitrary water depth on linear shear currents

A. K. Dhar, Sourav Halder, Suman Mukherjee
1 citations
Wave Motion
Ocean Waves and Remote Sensing
1.79
article

Fourth-order Stokes theory for capillary–gravity waves in arbitrary water depth on linear shear currents

A. K. Dhar, Sourav Halder, Suman Mukherjee
article en
1 citations

Abstract

In this paper the two-dimensional steady surface capillary–gravity waves, incorporating the effects of linear shear currents, is studied in water of constant depth. Herein, linear shear currents are considered to be a linear combination of depth-uniform current and uniform vorticity. Employing an excellent Stokes expansion method, where the expansion parameter represents the wave steepness itself, a fourth-order perturbation series solution for plane progressive waves is developed. The key results of this work are (a) to find the influence of both co-flowing and counter-flowing currents on the wave profiles using the fourth-order approximation (b) the strong dependence of the wave velocity on both the magnitudes of the shear and depth-uniform current, (c) the Wilton singularities in the Stokes expansion in powers of wave amplitude due to a inverse Bond number of 1 / 2 , 1 / 3 and 1 / 4 , which are the results of the non-uniformity in the ordering of the Fourier coefficients are observed to be influenced by vorticity and depth-uniform current, (d) distinct surface profiles of capillary–gravity waves are obtained and the effects of depth-uniform currents on these profiles are described. This analysis also shows that for any given value of the water depth, there exist a threshold value of the vorticity above which no resonances occur. For the steepest waves considered in this analysis, it is observed that when the wavenumber is not in the vicinity of certain critical values, determined by the depth and the vorticity, the present fourth-order analysis shows significant deviations on the surface profiles from the third-order analysis and provides better results consistent with the exact numerical results. • In this note we find the effect of vorticity on the critical wavenumbers. • The strong dependence of the wave velocity on the magnitude of the shear is obtained. • For given water depth, there exists a threshold value of the vorticity above which no resonances occur. • The influence of depth uniform current on the wave profiles is investigated.

Wave MotionVol. 137
Indian Institute of Engineering Science and Technology, Shibpur (IN)
Clean water and sanitation
Openalex Percentile: Top 19%
Ocean Waves and Remote Sensing
1.79
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