2017
DOI: 10.1098/rsta.2017.0102
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Prediction of the free-surface elevation for rotational water waves using the recovery of pressure at the bed

Abstract: This paper considers the pressure-streamfunction relationship for a train of regular water waves propagating on a steady current, which may possess an arbitrary distribution of vorticity, in two dimensions. The application of such work is to both near shore and offshore environments, and in particular, for linear waves we provide a description of the role which the pressure function on the seabed plays in determining the free-surface profile elevation. Our approach is shown to provide a good approximation for … Show more

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Cited by 22 publications
(17 citation statements)
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References 36 publications
(65 reference statements)
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“…As shown in [39], the equations (88) admit a local conservation of energy, the energy density being here the sum of the energy density associated to the irrotational SGN equations and of a rotation (or turbulent) energy e rot ; a similar correction must also be made for the energy flux, so that (27) becomes (89) ∂ t e NSW + e rot + ∇ · F NSW + F rot = 0, where e rot = 1 2 TrE and F rot = 1 2 TrEV + EV .…”
Section: 32mentioning
confidence: 99%
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“…As shown in [39], the equations (88) admit a local conservation of energy, the energy density being here the sum of the energy density associated to the irrotational SGN equations and of a rotation (or turbulent) energy e rot ; a similar correction must also be made for the energy flux, so that (27) becomes (89) ∂ t e NSW + e rot + ∇ · F NSW + F rot = 0, where e rot = 1 2 TrE and F rot = 1 2 TrEV + EV .…”
Section: 32mentioning
confidence: 99%
“…quite obviously, enstrophy (or, equivalently, turbulent energy), is created in the vicinity of wave breaking, where the gradient of the velocity becomes important; the mechanical energy of the wave is consequently decreased. This mechanism restores the local conservation of the total energy (89). However, in a second step, the small scale dissipation of the total energy must be taken into account; there should therefore be a dissipation mechanism D such that ∂ t e NSW + e rot + ∇ · F NSW + F rot = −D.…”
Section: 4mentioning
confidence: 99%
“…There are an infinite number of real positive roots ν j of (3.3) such that ν j ∼ 3j − 1/2 − √ 3/2πj as j → ∞. There are also two complex roots, approximately −1/2 ± i × 1.0714, that do not appear in the extreme wave (as they would yield an unbounded free surface); they do play a role in near extreme waves, however (Longuet-Higgins & Fox 1977). In order to derive expression (3.2), we use -cf.…”
Section: Stokes Extreme Wavementioning
confidence: 99%
“…Until recent years, most studies were based on a linear transfer function (Escher & Schlurmann 2008), primarily due to the intractability of the nonlinear governing equations, and even then for irrotational waves (cf. Henry & Thomas (2018) for linear, and weakly nonlinear, recovery formulae for waves with vorticity). However, the inadequacy of linear formulae for waves of even moderate amplitude is well known (Bishop & Donelan 1987;Tsai et al 2005), hence the importance of taking into account nonlinear effects.…”
Section: Introductionmentioning
confidence: 99%
“…Consequently, the investigation of the pressure field beneath a surface water wave is currently of great interest. This topic is covered by three papers in this issue: theoretical aspects are addressed in [36,37], while [38] presents experimental studies.…”
mentioning
confidence: 99%