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Wave-packet formation at the zero-dispersion point in the Gardner-Ostrovsky equation
1Department of Mathematics, University College London, London WC1E 6BT, United Kingdom.
Summary
Weak rotation causes solitary waves to decay into other waves, forming nonlinear wave packets. A nonlinear spectral splitting at the zero-dispersion point explains this wave packet formation.
Area of Science:
- Fluid dynamics
- Nonlinear wave phenomena
Background:
- Internal solitary waves decay into inertia-gravity waves over time due to weak rotation.
- The formation mechanism of the resulting nonlinear wave packets remains unexplained.
Purpose of the Study:
- To investigate the formation mechanism of nonlinear wave packets from decaying solitary waves under rotation.
- To explain the role of the zero-dispersion point in this phenomenon.
Main Methods:
- Analysis of the initial value problem using the Gardner-Ostrovsky equation (rotation-modified extended Korteweg-de Vries).
- Investigation of the linear Gardner-Ostrovsky equation's properties at the zero-dispersion point.
- Numerical comparisons between the Gardner-Ostrovsky equation and a derived nonlinear Schrödinger equation.
Main Results:
- A nonlinear splitting of the wave-number spectrum at the zero-dispersion point is identified as the cause of wave packet formation.
- Energy is shifted into the modulationally unstable regime of the Gardner-Ostrovsky equation.
- Numerical results confirm the spectral splitting and its role in solitary wave decay.
Conclusions:
- Nonlinear spectral splitting at the zero-dispersion point is the key mechanism for nonlinear wave packet formation from decaying solitary waves.
- This finding provides a satisfactory explanation for a previously poorly understood phenomenon in fluid dynamics.
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