## Nonlinear waves in waveguides: with stratification |

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Page 74

It follows from (4.17) and (4.23) that for both types of waves there are waves

propagating in opposite directions. 4.1.2 Weakly

Plasma Let us now take into account a plasma that is

along ...

It follows from (4.17) and (4.23) that for both types of waves there are waves

propagating in opposite directions. 4.1.2 Weakly

**Inhomogeneous**BoundedPlasma Let us now take into account a plasma that is

**inhomogeneous**(stratified)along ...

Page 107

A gaseous atmosphere in a gravitational field is a good example of a medium

with

increasing height automatically leads to a decrease in the collision number and

an ...

A gaseous atmosphere in a gravitational field is a good example of a medium

with

**inhomogeneous**Knudsen number. The decrease in the gas density withincreasing height automatically leads to a decrease in the collision number and

an ...

Page 108

fundamental

of the free path length should be compared with the vector parameter of a wave:

with a wave vector, for example. Thus, the role of the Knudsen number must be ...

fundamental

**inhomogeneity**of the atmosphere that induces the vector propertiesof the free path length should be compared with the vector parameter of a wave:

with a wave vector, for example. Thus, the role of the Knudsen number must be ...

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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