In this paper, we study Bragg resonance, i.e., the triad interaction between surface and/or interfacial waves with a bottom ripple, in the presence of background velocity. We show that when one of the constituent waves of the triad has negative energy, the amplitudes of all the waves grow exponentially. This is very different from classic Bragg resonance in which one wave decays to cause the growth of the other. The instabilities we observe are "explosive" and are different from normal mode shear instabilities since our velocity profiles are linearly stable. Our work may explain the existence of large-Amplitude internal waves over periodic bottom ripples in the presence of tidal flow observed in oceans and estuaries.</p
Interfacial phenomena, viz. roll waves and elastic tremor, are considered in the first part, wherea...
Interfacial phenomena, viz. roll waves and elastic tremor, are considered in the first part, wherea...
The effects of Fourier components of cross-stream topographic slope are included in the classical li...
In this paper, we study Bragg resonance, i.e., the triad interaction between surface and/or interfac...
In this paper, we study Bragg resonance, i.e., the triad interaction between surface and/or interfac...
We investigate, via perturbation analyses, the mechanisms of nonlinear resonant interaction of surfa...
In this paper, we show that Stokes drift may be significantly affected when an incident intermediate...
In this paper, we show that Stokes drift may be significantly affected when an incident intermediate...
In this paper, we show that Stokes drift may be significantly affected when an incident intermediate...
The development of shear instabilities of a wave-driven alongshore current is investigated. In part...
Weakly nonlinear internal wave-wave interaction is a key mechanism that cascades energy from large t...
Large amplitude edge waves are shown to be modified by nonlinear effects in a way very similar to su...
[1] The development of shear instabilities of a wave-driven alongshore current is investigated. In p...
Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Mechanical Engineering, 2008.Includ...
We present observations that reveal the existence of horizontally propagating, tidally-driven, high-...
Interfacial phenomena, viz. roll waves and elastic tremor, are considered in the first part, wherea...
Interfacial phenomena, viz. roll waves and elastic tremor, are considered in the first part, wherea...
The effects of Fourier components of cross-stream topographic slope are included in the classical li...
In this paper, we study Bragg resonance, i.e., the triad interaction between surface and/or interfac...
In this paper, we study Bragg resonance, i.e., the triad interaction between surface and/or interfac...
We investigate, via perturbation analyses, the mechanisms of nonlinear resonant interaction of surfa...
In this paper, we show that Stokes drift may be significantly affected when an incident intermediate...
In this paper, we show that Stokes drift may be significantly affected when an incident intermediate...
In this paper, we show that Stokes drift may be significantly affected when an incident intermediate...
The development of shear instabilities of a wave-driven alongshore current is investigated. In part...
Weakly nonlinear internal wave-wave interaction is a key mechanism that cascades energy from large t...
Large amplitude edge waves are shown to be modified by nonlinear effects in a way very similar to su...
[1] The development of shear instabilities of a wave-driven alongshore current is investigated. In p...
Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Mechanical Engineering, 2008.Includ...
We present observations that reveal the existence of horizontally propagating, tidally-driven, high-...
Interfacial phenomena, viz. roll waves and elastic tremor, are considered in the first part, wherea...
Interfacial phenomena, viz. roll waves and elastic tremor, are considered in the first part, wherea...
The effects of Fourier components of cross-stream topographic slope are included in the classical li...