Nonlinear Waves in Waveguides: With StratificationS.B. Leble's book deals with nonlinear waves and their propagation in metallic and dielectric waveguides and media with stratification. The underlying nonlinear evolution equations (NEEs) are derived giving also their solutions for specific situations. The reader will find new elements to the traditional approach. Various dispersion and relaxation laws for different guides are considered as well as the explicit form of projection operators, NEEs, quasi-solitons and of Darboux transforms. Special points relate to: 1. the development of a universal asymptotic method of deriving NEEs for guide propagation; 2. applications to the cases of stratified liquids, gases, solids and plasmas with various nonlinearities and dispersion laws; 3. connections between the basic problem and soliton- like solutions of the corresponding NEEs; 4. discussion of details of simple solutions in higher- order nonsingular perturbation theory. |
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Page 104
... temperature T ( z ) on the height oscillates . At low altitudes the temperature falls , then after reaching a minimum at about 15 km ( tropopause ) it begins to increase and reaches a maximum at≈ 40 km ( stratopause ) . It then ...
... temperature T ( z ) on the height oscillates . At low altitudes the temperature falls , then after reaching a minimum at about 15 km ( tropopause ) it begins to increase and reaches a maximum at≈ 40 km ( stratopause ) . It then ...
Page 105
... temperature which is proportional to H in the upper layer is higher than in the lower layer . Examples of such a situation are the splitting of the troposphere - mesosphere by the tropopause , or the thermosphere - mesosphere system ...
... temperature which is proportional to H in the upper layer is higher than in the lower layer . Examples of such a situation are the splitting of the troposphere - mesosphere by the tropopause , or the thermosphere - mesosphere system ...
Page 131
... temperature field Ti = 2ɛo2t ( Õ " w ) ' ω Using the coupling of Ỗ and w via ( 6.56 ) and taking Ï ' weakly depending on z outside the derivative , we get Ti = εo2 ( ww " ) ' T't 2 ( 6.62 ) The rate of the irreversible medium temperature ...
... temperature field Ti = 2ɛo2t ( Õ " w ) ' ω Using the coupling of Ỗ and w via ( 6.56 ) and taking Ï ' weakly depending on z outside the derivative , we get Ti = εo2 ( ww " ) ' T't 2 ( 6.62 ) The rate of the irreversible medium temperature ...
Contents
Introduction | 1 |
The Discrimination and Interaction | 12 |
3 | 33 |
Copyright | |
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amplitude approximation atmosphere B₁ boundary conditions calculation CKdV coefficients components contribution coordinate denote density density matrix dependence derivation described determined dielectric dimensionless dispersion branches dispersion equation dispersion relation dissipation distribution function dynamical variables effects electromagnetic electron evolution equations frequency given group velocities H₂ hydrodynamical inhomogeneity initial conditions integration internal waves ion-acoustic waves ionospheric iteration KdV equation kinetic Langmuir wave layer linear longitudinal longitudinal waves magnetic field matrix mean field medium method mode interaction nonlinear constants nonlinear terms Nonlinear Waves nonlocal oscillations particles perturbation theory physical plasma waves problem projection operators quasisolitons region resonance Rossby waves S.B.Leble scale Sect small parameters soliton solution spectral SSSR stationary subspaces substitution taking into account temperature thermoclyne thermoconductivity thermospheric three-wave transformed turbulence velocity vertical w₁ wave propagation wave vector waveguide propagation wavelength