Steep, focusing waves can experience fast and local nonlinear evolution of the spectrum due to wave–wave interactions resulting in energy transfer to both higher and lower wavenumber components. The shape and kinematics of a steep wave may, thus, differ substantially from the predictions of linear theory. We have investigated the role of nonlinear interactions on group shape for a steep, narrow-banded, directionally spread wave group focusing in deep water using the fully nonlinear potential flow solver, oceanwave3d. Exact second-order correction of the initial conditions has been implemented together with a novel third-order approximate correction based on a Stokes-type formulation for surface elevation combined with a scaling argument for...
The influence of water depth on wave development increases the complexity of wave forecasting for oc...
We investigate the appearance of coherent groups in three-dimensional fully-nonlinear potential deep...
As large waves form in the open ocean their dynamics are modified from classic linear dispersion by ...
Steep, focusing waves can experience fast and local nonlinear evolution of the spectrum due to wave-...
We have investigated steep three-dimensional surface gravity wave groups formed by dispersive focusi...
This paper analyses the spatial evolution of steep directionally spread transient wave groups on dee...
ABSTRACT: Nonlinear wave-wave interaction behavior in deep and intermediate water depths and also on...
Nonlinear wave interactions and superpositions among the different wave components and wave groups i...
This paper describes an experimental investigation in which a large number of water waves were focus...
The Non-linear Schrödinger Equation and its higher order extensions are routinely used for analysis ...
A new nonlinear Schrödinger equation (NLSE) is presented for ocean surface waves. Earlier derivation...
This paper concerns the propagation of transient wave groups, focused at a point in time and space t...
The formation of 'rogue' or 'freak' waves at the ocean surface is an important consideration for eng...
The evolution of steep waves in the open ocean is nonlinear. In narrow-banded but directionally spre...
We investigate the emergence of coherent groups in three-dimensional fully-nonlinear potential deep ...
The influence of water depth on wave development increases the complexity of wave forecasting for oc...
We investigate the appearance of coherent groups in three-dimensional fully-nonlinear potential deep...
As large waves form in the open ocean their dynamics are modified from classic linear dispersion by ...
Steep, focusing waves can experience fast and local nonlinear evolution of the spectrum due to wave-...
We have investigated steep three-dimensional surface gravity wave groups formed by dispersive focusi...
This paper analyses the spatial evolution of steep directionally spread transient wave groups on dee...
ABSTRACT: Nonlinear wave-wave interaction behavior in deep and intermediate water depths and also on...
Nonlinear wave interactions and superpositions among the different wave components and wave groups i...
This paper describes an experimental investigation in which a large number of water waves were focus...
The Non-linear Schrödinger Equation and its higher order extensions are routinely used for analysis ...
A new nonlinear Schrödinger equation (NLSE) is presented for ocean surface waves. Earlier derivation...
This paper concerns the propagation of transient wave groups, focused at a point in time and space t...
The formation of 'rogue' or 'freak' waves at the ocean surface is an important consideration for eng...
The evolution of steep waves in the open ocean is nonlinear. In narrow-banded but directionally spre...
We investigate the emergence of coherent groups in three-dimensional fully-nonlinear potential deep ...
The influence of water depth on wave development increases the complexity of wave forecasting for oc...
We investigate the appearance of coherent groups in three-dimensional fully-nonlinear potential deep...
As large waves form in the open ocean their dynamics are modified from classic linear dispersion by ...