Long time interaction of envelope solitons and freak wave formations
article
This paper concerns long time interaction of envelope solitary gravity waves propagating at the surface of a two-dimensional
deep fluid in potential flow. Fully nonlinear numerical simulations show how an initially long wave group slowly splits into a
number of solitary wave groups. In the example presented, three large wave events are formed during the evolution. They occur
during a time scale that is beyond the time range of validity of simplified equations like the nonlinear Schrödinger (NLS) equation or
modifications of this equation. A Fourier analysis shows that these large wave events are caused by significant transfer to side-band
modes of the carrier waves. Temporary downshiftings of the dominant wavenumber of the spectrum coincide with the formation
large wave events. The wave slope at maximal amplifications is about three times higher than the initial wave slope. The results
show how interacting solitary wave groups that emerge from a long wave packet can produce freak wave events.
Our reference numerical simulation are performed with the fully nonlinear model of Clamond and Grue [D. Clamond, J. Grue,
A fast method for fully nonlinear water wave computations, J. Fluid Mech. 447 (2001) 337–355]. The results of this model are
compared with that of two weakly nonlinear models, the NLS equation and its higher-order extension derived by Trulsen et al.
[K. Trulsen, I. Kliakhandler, K.B. Dysthe, M.G. Velarde, On weakly nonlinear modulation of waves on deep water, Phys. Fluids
12 (10) (2000) 2432–2437]. They are also compared with the results obtained with a high-order spectral method (HOSM) based
on the formulation of West et al. [B.J. West, K.A. Brueckner, R.S. Janda, A method of studying nonlinear random field of surface
gravity waves by direct numerical simulation, J. Geophys. Res. 92 (C11) (1987) 11 803–11 824]. An important issue concerning
the representation and the treatment of the vertical velocity in the HOSM formulation is highlighted here for the study of long-time
evolutions.
deep fluid in potential flow. Fully nonlinear numerical simulations show how an initially long wave group slowly splits into a
number of solitary wave groups. In the example presented, three large wave events are formed during the evolution. They occur
during a time scale that is beyond the time range of validity of simplified equations like the nonlinear Schrödinger (NLS) equation or
modifications of this equation. A Fourier analysis shows that these large wave events are caused by significant transfer to side-band
modes of the carrier waves. Temporary downshiftings of the dominant wavenumber of the spectrum coincide with the formation
large wave events. The wave slope at maximal amplifications is about three times higher than the initial wave slope. The results
show how interacting solitary wave groups that emerge from a long wave packet can produce freak wave events.
Our reference numerical simulation are performed with the fully nonlinear model of Clamond and Grue [D. Clamond, J. Grue,
A fast method for fully nonlinear water wave computations, J. Fluid Mech. 447 (2001) 337–355]. The results of this model are
compared with that of two weakly nonlinear models, the NLS equation and its higher-order extension derived by Trulsen et al.
[K. Trulsen, I. Kliakhandler, K.B. Dysthe, M.G. Velarde, On weakly nonlinear modulation of waves on deep water, Phys. Fluids
12 (10) (2000) 2432–2437]. They are also compared with the results obtained with a high-order spectral method (HOSM) based
on the formulation of West et al. [B.J. West, K.A. Brueckner, R.S. Janda, A method of studying nonlinear random field of surface
gravity waves by direct numerical simulation, J. Geophys. Res. 92 (C11) (1987) 11 803–11 824]. An important issue concerning
the representation and the treatment of the vertical velocity in the HOSM formulation is highlighted here for the study of long-time
evolutions.
Topics
TNO Identifier
222543
Source
European Journal of Mechanics B/Fluids, 25, pp. 536-553.
Pages
536-553
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