## Nonlinear waves in waveguides: with stratification |

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Page 16

When the horizontal

solution must include a condition of periodicity along the longitudinal axis ip and

of finiteness in the interval of possible variations of colatitude d. Then the

horizontal ...

When the horizontal

**wavelength**is of the order of the planet radius then thesolution must include a condition of periodicity along the longitudinal axis ip and

of finiteness in the interval of possible variations of colatitude d. Then the

horizontal ...

Page 17

If the

inhomogeneity H then the local dispersion equation can be used within the

framework of asymptotic methods with the small parameter \/H . If such a

condition is not valid ...

If the

**wavelength**A of a disturbance is smaller than the minimal scale ofinhomogeneity H then the local dispersion equation can be used within the

framework of asymptotic methods with the small parameter \/H . If such a

condition is not valid ...

Page 93

Now let us suppose that the dependence is such that a given range of

become a quasi-waveguide at least for a restricted

Atmosphere is an ...

Now let us suppose that the dependence is such that a given range of

**wavelengths**cannot exist in the region z > h. Thus, even an infinite medium canbecome a quasi-waveguide at least for a restricted

**wavelength**range.Atmosphere is an ...

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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