Math 2.0

Fluid mechanics Water waves and free surfaces Example

Stokes wave

Builds on Airy wave theoryDispersion relation of water waves

Example

A Stokes wave is a periodic travelling wave of permanent form that solves the full nonlinear water wave problem. Stokes constructed it as a power series in the wave steepness kaka, where aa is the amplitude and kk the wavenumber. In deep water, with θ=kx−ωt\theta = kx - \omega t, the surface elevation to second order is η=acos⁡θ+12ka2cos⁡(2θ)+O(k2a3),\eta = a\cos\theta + \tfrac{1}{2}ka^2\cos(2\theta) + O(k^2a^3), and the angular frequency to third order is ω=gk(1+12k2a2)+O(k3a3).\omega = \sqrt{gk}\left(1 + \tfrac{1}{2}k^2a^2\right) + O(k^3a^3). The first term of η\eta is the linear wave of Airy wave theory. The second harmonic makes the crests sharper and the troughs flatter. The frequency now depends on the amplitude, so steeper waves travel faster than the linear dispersion relation predicts.

Remarks

The existence of small-amplitude Stokes waves as exact solutions was proved in the 1920s, by Nekrasov and by Levi-Civita for deep water and by Struik for finite depth. As the height grows, the family ends at a wave of greatest height whose crest is a corner of interior angle 120∘120^\circ, as Stokes predicted. Amick, Fraenkel and Toland proved this Stokes conjecture in 1982. Stokes waves on deep water are unstable to slow modulations of their amplitude, the Benjamin–Feir instability.

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  1. Airy wave theory concept
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Further reading

  1. Web https://en.wikipedia.org/wiki/Stokes_wave
About this page
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Kindexample
WritingW0 stub
MSC76B15
Instance ofWater waves
UsesAiry wave theory, Dispersion relation of water waves
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Changed3 November 2026

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