## Nonlinear waves in waveguides: with stratification |

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Page 11

Large-scale disturbances that appear as a self-organized wave are called the

mean

to

in ...

Large-scale disturbances that appear as a self-organized wave are called the

mean

**field**(motion) by Grimshaw [1.83] and ... Before concluding, we would liketo

**point**out one more application of the solutions for various dispersion branchesin ...

Page 83

It is assumed that a stationary

where (£i£j)U,k is the spectral density of the electric

approximation that the

It is assumed that a stationary

**point**and spatial homogeneity leads to ... (4.48)where (£i£j)U,k is the spectral density of the electric

**field**fluctuations. ... In theapproximation that the

**field**amplitude is quadratic the spectral transform of the**field**...Page 116

contribution is related to the so-called mean

included naturally in the background ...

the vertical structure of the flow is different from the wave mode

contribution is related to the so-called mean

**field**whose dynamical functions areincluded naturally in the background ...

**point**in this assumed description is thatthe vertical structure of the flow is different from the wave mode

**field**structure.### What people are saying - Write a review

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### Contents

Introduction | 1 |

The Discrimination and Interaction | 12 |

Interaction of Modes in an Electromagnetic Field Waveguide | 50 |

Copyright | |

6 other sections not shown

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### Common terms and phrases

allows amplitude approximation atmosphere atmospheric waveguide atmospheric waves basis functions boundary conditions calculation CKdV coefficients components considered contribution coordinate decrease denote density density matrix dependence derivation described determined dielectric dimensionless dispersion branches dispersion equation dispersion relation dissipation distribution function dynamical variables effects evolution equations exponential Fiz.Atm.Okean formulas Fourier given hydrodynamical inhomogeneity initial conditions integration internal waves ion-acoustic ionospheric iteration Kaliningrad KdV equation kinetic Langmuir waves layer linear long waves magnetic field matrix mean field medium method mode interaction mode number Moscow nonlinear constants nonlinear terms Nonlinear Waves nonlocal ocean oscillations perturbation theory physical plasma waves problem projection operators quasi-waveguide quasisolitons region resonance Rossby waves S.B.Leble S.BXeble scale Sect small parameters soliton solution spectral SSSR stationary stratified subspaces substitution taking into account temperature thermoclyne thermoconductivity thermospheric three-wave transformed turbulence two-dimensional values velocity vertical wave interaction wave propagation wave vector waveguide propagation wavelength