Nonlinear Waves in Waveguides: With Stratification |
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Page 15
... temperature Ï ; H = RT / ( μg ) [ 2.4 ] . This approximation holds in atmospheric waveguides over intervals of z where the temperature gradients T2 are small . These inter- vals correspond to layers , at the boundaries of which the ...
... temperature Ï ; H = RT / ( μg ) [ 2.4 ] . This approximation holds in atmospheric waveguides over intervals of z where the temperature gradients T2 are small . These inter- vals correspond to layers , at the boundaries of which the ...
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 = 2εo2 + ( Ã " w ) ' w Using the coupling of Õ and w via ( 6.56 ) and taking Ï ' weakly depending on z outside the derivative , we get Ti = εo2 ( ww " ) ' Ï't ( 6.62 ) 2 The rate of the irreversible medium temperature ...
... temperature field Ti = 2εo2 + ( Ã " w ) ' w Using the coupling of Õ and w via ( 6.56 ) and taking Ï ' weakly depending on z outside the derivative , we get Ti = εo2 ( ww " ) ' Ï't ( 6.62 ) 2 The rate of the irreversible medium temperature ...
Contents
Introduction | 1 |
The Discrimination and Interaction | 12 |
3 | 27 |
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 dispersion branches dispersion equation dispersion relation dissipation distribution function dynamical variables effects electromagnetic electron evolution equations Fiz.Atm.Okean frequency given H₂ hydrodynamical inhomogeneity initial conditions integration internal waves ion-acoustic waves Ionosphere iteration Kaliningrad KdV equation kinetic Langmuir wave layer linear longitudinal waves magnetic field matrix mean field medium method mode interaction Moscow Nauka 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 subspaces substitution taking into account temperature thermoclyne thermoconductivity thermospheric three-wave transformed turbulence vector velocity vertical w₁ wave propagation wave vector waveguide propagation wavelength