## Nonlinear waves in waveguides: with stratification |

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Page 19

Determination of wave type according to its

complete identification because the

. Every measurement system used for identification can be correlated (as in

quantum ...

Determination of wave type according to its

**frequency**is not sufficient forcomplete identification because the

**frequency**(wavelength) intervals can overlap. Every measurement system used for identification can be correlated (as in

quantum ...

Page 72

Therefore -ifc = 4ne2kn[l + fc2(p2)/mV]/imw2 and the dispersion relation follows.

For the Maxwell distribution f° it has the form w2 = <4. + 3KBTek2/m (4.17) where

wj,e = leyjvnjrn is the Langmuir

Therefore -ifc = 4ne2kn[l + fc2(p2)/mV]/imw2 and the dispersion relation follows.

For the Maxwell distribution f° it has the form w2 = <4. + 3KBTek2/m (4.17) where

wj,e = leyjvnjrn is the Langmuir

**frequency**of the electrons and Te is the electron ...Page 105

Let us write the dispersion relation given by (2.56) in dimensional form at a — ▻

oo, Q = 0 but taking into account the vertical acceleration w2(w2 - u\) - cWk2 +

cWg k2± = 0, (5 .38) where wa = 7<7/2c, ug = y/j — lg/c are the limiting

Let us write the dispersion relation given by (2.56) in dimensional form at a — ▻

oo, Q = 0 but taking into account the vertical acceleration w2(w2 - u\) - cWk2 +

cWg k2± = 0, (5 .38) where wa = 7<7/2c, ug = y/j — lg/c are the limiting

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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