It is suggested that the stratosphere may-act as a wave-guide for certain types of acoustic-gravity waves. An isothermal layer model is proposed which introduces gravity terms into the equations governing wave propagation. An expression for the phase change on reflection at a boundary of the layer is derived. Numerical solutions to the equation for wave-guide, modes of propagation are obtained by the use of a digital computer. Results are given in the form of dispersion curves. Cutoff is found to occur at a frequency well above the Brunt resonant frequency for the stratosphere. The model stratosphere proposed in this study does not behave as a lossless wave-guide for gravity coupled acoustic waves. This is shown to be consistent with the r...
The upward propagation of linear acoustic waves in a gravitationally stratified atmosphere is studie...
The nonlinear propagation of low-frequency acoustic waves through the turbulent fluctuations induced...
Vertical propagation of acoustic waves of finite amplitude in an isothermal, gravitationally stratif...
Homogeneous wave guide theory is used to derive dispersion curves, vertical pressure distributions, ...
In this paper, we study, in theoretical terms, the structure of the spectrum of acoustic-gravity wav...
The propagation of pressure waves in a stratified, non-isothermal atmosphere is studied in the lin...
International audienceWaves propagate in a free-surface ocean due to compressibility and gravity (an...
A two-dimensional nonlinear numerical model has been developed to study atmospheric coupling due to ...
We study the atmospheric structure in response to the propagation of gravity waves under nonisotherm...
An atmosphere is modelled by averaging measurements taken at eight locations for 1968 September 9. T...
The upward propagation of linear acoustic waves in a gravitationally stratified atmosphere is studie...
An exact expression is obtained for the acoustic-gravity layer matrix for an atmospheric layer havin...
Part I: A matrix formulation is used to derive the pressure variation for acoustic gravity waves ...
The excitation of acoustic-gravity waves in an isothermal atmosphere is considered in this paper. It...
It is shown that low-frequency acoustic gravity waves propagating parallel to the earth's surface sa...
The upward propagation of linear acoustic waves in a gravitationally stratified atmosphere is studie...
The nonlinear propagation of low-frequency acoustic waves through the turbulent fluctuations induced...
Vertical propagation of acoustic waves of finite amplitude in an isothermal, gravitationally stratif...
Homogeneous wave guide theory is used to derive dispersion curves, vertical pressure distributions, ...
In this paper, we study, in theoretical terms, the structure of the spectrum of acoustic-gravity wav...
The propagation of pressure waves in a stratified, non-isothermal atmosphere is studied in the lin...
International audienceWaves propagate in a free-surface ocean due to compressibility and gravity (an...
A two-dimensional nonlinear numerical model has been developed to study atmospheric coupling due to ...
We study the atmospheric structure in response to the propagation of gravity waves under nonisotherm...
An atmosphere is modelled by averaging measurements taken at eight locations for 1968 September 9. T...
The upward propagation of linear acoustic waves in a gravitationally stratified atmosphere is studie...
An exact expression is obtained for the acoustic-gravity layer matrix for an atmospheric layer havin...
Part I: A matrix formulation is used to derive the pressure variation for acoustic gravity waves ...
The excitation of acoustic-gravity waves in an isothermal atmosphere is considered in this paper. It...
It is shown that low-frequency acoustic gravity waves propagating parallel to the earth's surface sa...
The upward propagation of linear acoustic waves in a gravitationally stratified atmosphere is studie...
The nonlinear propagation of low-frequency acoustic waves through the turbulent fluctuations induced...
Vertical propagation of acoustic waves of finite amplitude in an isothermal, gravitationally stratif...