Elsevier

European Journal of Mechanics - B/Fluids

Volume 17, Issue 5, September–October 1998, Pages 739-768
European Journal of Mechanics - B/Fluids

Three-dimensional solitary waves in the presence of additional surface effects

https://doi.org/10.1016/S0997-7546(98)80023-XGet rights and content

Abstract

Bifurcations from the quiescent state of three dimensional water wave solutions of a sixth order model equation are analysed. The equation in question is a generalization of the Kadomtsev-Petviashvili equation, and is obtained due to the presence of certain surface effects. These effects are caused either by a surface tension with Bond number close to 13, or by an elastic ice-sheet floating on the water surface. The equation describing travelling waves is reduced to a system of ordinary differential equations on a center manifold. Solutions having the form of a solitary wave with damped oscillations, propagating in a channel, are obtained. In the direction transverse to the propagation they satisfy boundary conditions which are either periodic or of Dirichlet type. In the periodic case we find both asymmetric and symmetric waves. In particular, some of these solutions fill a gap in the speeds of the travelling waves where no two-dimensional solitary waves exist. We show that the critical spectra of the linear operators of the model equation and of the full water wave problem are identical.

References (25)

  • M. Haragus

    Model equations for water waves in the presence of surface tension

    Eur. J. Mech. B/Fluids

    (1996)
  • M. Haragus et al.

    Breaking the Dimension of a Steady Wave: Some Examples

  • Cited by (41)

    • Nonlinear simulation of wave group attenuation due to scattering in broken floe fields

      2023, Ocean Modelling
      Citation Excerpt :

      Despite significant progress over the past decade, the nonlinear theory is still in its infancy. Efforts have mainly focused on the analysis and simulation of flexural-gravity waves in homogeneous sea ice, using nonlinear potential-flow theory for the underlying fluid combined with linear or nonlinear thin-plate theory for the floating ice (Bonnefoy et al., 2009; Dinvay et al., 2019; Haragus-Courcelle and Ilichev, 1998; Milewski et al., 2011; Părău and Dias, 2002). A compelling thin-plate formulation in this situation is the one recently proposed by Plotnikov and Toland (2011) based on the special Cosserat theory of hyperelastic shells, which yields a nonlinear and conservative expression for the bending force.

    • Three-dimensional waves under ice computed with novel preconditioning methods

      2022, Journal of Computational Physics
      Citation Excerpt :

      Moreover, a fifth-order Korteweg–de Vries equation for two-dimensional hydroelastic waves on shallow water in channels was derived [22]. In three dimensions, a generalization of the Kadomtsev-Petviashvili equation was derived to model waves in the presence of additional surface effects [23], and to investigate solitary flexural-gravity waves [24]. Solitary waves in three dimensions have also been studied using a Benney-Roskes-Davey-Stewartson model for a fluid of arbitrary depth covered by an elastic sheet [14].

    • Hydroelastic lumps in shallow water

      2022, Physica D: Nonlinear Phenomena
    • Phase dynamics of periodic wavetrains leading to the 5th order KP equation

      2017, Physica D: Nonlinear Phenomena
      Citation Excerpt :

      The first of these is in the environment of flexural gravity waves. Such systems have already been shown to admit solitary waves that are well described by fifth order KdV and KP models [8–10], and so one expects the theory to generate a relevant fifth order KP. We consider a simple example, in which the hydroelastic sheet resting on the flow generates Euler–Bernoulli beam terms into the shallow water model.

    • Finite-depth effects on solitary waves in a floating ice sheet

      2014, Journal of Fluids and Structures
      Citation Excerpt :

      In finite depth, two asymptotic regimes are usually of interest: the long-wave regime and the modulational regime. In the former case, we derive a 5th-order KdV equation in the spirit of Haragus-Courcelle and Ilichev (1998) and Xia and Shen (2002), while in the latter case, we derive a cubic NLS equation in the spirit of Părău and Dias (2002). We emphasise again that these previous studies considered simplified models for the ice sheet.

    View all citing articles on Scopus
    b

    Permanent address: Mathematical Steklov Inst., Gubkina str. 8, 117966 Moscow GSP-1, Russia

    View full text