Nonlinear waves in waveguides: with stratification |
From inside the book
Results 1-3 of 8
Page 123
An internal wave propagating in the thermospheric waveguide (Sect. 5.4) is
usually a superposition of a few contributions of the form (5.49) at an altitude
lower than h ~ 500 km [6.26,27]. Above z = h the wave function is represented ...
An internal wave propagating in the thermospheric waveguide (Sect. 5.4) is
usually a superposition of a few contributions of the form (5.49) at an altitude
lower than h ~ 500 km [6.26,27]. Above z = h the wave function is represented ...
Page 125
(632) The vertical structure of an internal thermospheric wave is such that a
function / inside the interval [0, h] is closed to superposition of the functions sinJfc
„2. During the increase of z from h up to hi « /i + 27/ the function / decreases ...
(632) The vertical structure of an internal thermospheric wave is such that a
function / inside the interval [0, h] is closed to superposition of the functions sinJfc
„2. During the increase of z from h up to hi « /i + 27/ the function / decreases ...
Page 163
137 Thermosphere V, 1 Thermospheric internal wave 27,33, 123 Thermospheric
waveguide 29, 35, 41, 123 Three-dimensional instability 33 Three-level system
61 Three-wave system 9,48,81 Three-wave interaction 10,56,58,62 Three-wave ...
137 Thermosphere V, 1 Thermospheric internal wave 27,33, 123 Thermospheric
waveguide 29, 35, 41, 123 Three-dimensional instability 33 Three-level system
61 Three-wave system 9,48,81 Three-wave interaction 10,56,58,62 Three-wave ...
What people are saying - Write a review
We haven't found any reviews in the usual places.
Contents
Introduction | 1 |
The Discrimination and Interaction | 12 |
Interaction of Modes in an Electromagnetic Field Waveguide | 50 |
Copyright | |
6 other sections not shown
Other editions - View all
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