## Nonlinear waves in waveguides: with stratification |

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Page 11

In the local equilibrium region, the usual results with the new wavenumber

spectrum are realized. In the Kn > 1 region the deviation from ideal

hydrodynamics is radical: instead of

a wave amplitude ...

In the local equilibrium region, the usual results with the new wavenumber

spectrum are realized. In the Kn > 1 region the deviation from ideal

hydrodynamics is radical: instead of

**exponential**growth,**exponential**decrease ofa wave amplitude ...

Page 17

2.7) [2.17]. In some problems, e.g.,

earth surface, the fundamental system can be reduced by substitution to

equations with constant coefficients. Then the usual dispersion analysis may be

applied.

2.7) [2.17]. In some problems, e.g.,

**exponential**atmospheric waves over a planarearth surface, the fundamental system can be reduced by substitution to

equations with constant coefficients. Then the usual dispersion analysis may be

applied.

Page 107

Since the mean free path is I ~ 1/nao, where n is the molecular concentration and

<ro is the scattering cross- section, the

an increase in the mean free path that is also

Since the mean free path is I ~ 1/nao, where n is the molecular concentration and

<ro is the scattering cross- section, the

**exponential**decrease in the density yieldsan increase in the mean free path that is also

**exponential**. This increase is ...### 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 | |

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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