## Nonlinear waves in waveguides: with stratification |

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Page 9

Therefore even the form of hydrostatic approximation waves radically differs from

the dispersing waves at large times. ...

of two equal velocities, are transformed to the sine-Gordon (SG) equation just ...

Therefore even the form of hydrostatic approximation waves radically differs from

the dispersing waves at large times. ...

**Three**-**wave**systems, in the particular caseof two equal velocities, are transformed to the sine-Gordon (SG) equation just ...

Page 63

Theoretical and technical questions in these experiments still remain, but in any

case, the specific mode content can influence only the "projecting coefficients of

unit order in constants of the

Theoretical and technical questions in these experiments still remain, but in any

case, the specific mode content can influence only the "projecting coefficients of

unit order in constants of the

**three**-**wave**(n-wave) interaction". This coefficient is ...Page 163

Plasma heating 1 14 Plasma turbulence 69,87 Plasma wave V, 1, 2, 19, 76

Poincare" wave 8, 22, 24, 25, 64 Poisson ... 35, 41, 123 Three-dimensional

instability 33 Three-level system 61

interaction 10 ...

Plasma heating 1 14 Plasma turbulence 69,87 Plasma wave V, 1, 2, 19, 76

Poincare" wave 8, 22, 24, 25, 64 Poisson ... 35, 41, 123 Three-dimensional

instability 33 Three-level system 61

**Three**-**wave**system 9,48,81**Three**-**wave**interaction 10 ...

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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