Articles | Volume 8, issue 6
https://doi.org/10.5194/gmd-8-1831-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/gmd-8-1831-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Verifications of the high-resolution numerical model and polarization relations of atmospheric acoustic-gravity waves
N. M. Gavrilov
CORRESPONDING AUTHOR
Atmospheric Physics Department, Saint-Petersburg State University, Saint-Petersburg, Russia
S. P. Kshevetskii
Theoretical Physics Department, Immanuel Kant Baltic Federal University, Kaliningrad, Russia
A. V. Koval
Atmospheric Physics Department, Saint-Petersburg State University, Saint-Petersburg, Russia
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Cited
14 citations as recorded by crossref.
- Role Of the Sun and the Middle atmosphere/thermosphere/ionosphere In Climate (ROSMIC): a retrospective and prospective view W. Ward et al. https://doi.org/10.1186/s40645-021-00433-8
- Spline Model: A Hydrostatic/Non-Hydrostatic Dynamic Core with Space-Time Second-Order Precision and Its Exact Tests X. Gu et al. https://doi.org/10.3390/atmos15030259
- Numerical Simulation of Vertical Current Sheets in Solar Chromospheric Plasma with the Hall Effect L. Alekseeva & S. Kshevetskii https://doi.org/10.1134/S0016793219040030
- Simulation of Propagation of Acoustic-Gravity Waves Generated by Tropospheric Front Instabilities into the Upper Atmosphere S. Kshevetskii et al. https://doi.org/10.1007/s00024-020-02569-y
- Identification of spectrum of secondary acoustic-gravity waves in the middle and upper atmosphere in a high-resolution numerical model N. Gavrilov & S. Kshevetskii https://doi.org/10.12737/stp-93202310
- Decay times of atmospheric acoustic–gravity waves after deactivation of wave forcing N. Gavrilov et al. https://doi.org/10.5194/acp-22-13713-2022
- Critical level influence on the spectra of secondary gravity waves in the middle and upper atmosphere N. Gavrilov et al. https://doi.org/10.12737/stp-121202612
- Features of the Supersonic Gravity Wave Penetration from the Earth’s Surface to the Upper Atmosphere N. Gavrilov & S. Kshevetskii https://doi.org/10.1007/s11141-018-9885-4
- Disturbances of the Thermosphere and the Ionosphere during a Meteorological Storm O. Borchevkina et al. https://doi.org/10.3390/atmos12111384
- Identification of spectrum of secondary acoustic-gravity waves in the middle and upper atmosphere in a high-resolution numerical model N. Gavrilov & S. Kshevetskii https://doi.org/10.12737/szf-93202310
- Tunneling of acoustic-gravity waves through critical levels to the upper atmosphere N. Gavrilov et al. https://doi.org/10.1016/j.asr.2024.12.005
- Numerical study of heating the upper atmosphere by acoustic-gravity waves from a local source on the Earth's surface and influence of this heating on the wave propagation conditions I. Karpov & S. Kshevetskii https://doi.org/10.1016/j.jastp.2017.07.019
- Well-Posedness of a Problem of Propagation of Nonlinear Acoustic-Gravity Waves in the Atmosphere Generated by Surface Pressure Variations Y. Kurdyaeva et al. https://doi.org/10.1134/S1995423917040048
- Critical level influence on spectra of secondary gravity waves in the middle and upper atmosphere N. Gavrilov et al. https://doi.org/10.12737/szf-121202612
14 citations as recorded by crossref.
- Role Of the Sun and the Middle atmosphere/thermosphere/ionosphere In Climate (ROSMIC): a retrospective and prospective view W. Ward et al. https://doi.org/10.1186/s40645-021-00433-8
- Spline Model: A Hydrostatic/Non-Hydrostatic Dynamic Core with Space-Time Second-Order Precision and Its Exact Tests X. Gu et al. https://doi.org/10.3390/atmos15030259
- Numerical Simulation of Vertical Current Sheets in Solar Chromospheric Plasma with the Hall Effect L. Alekseeva & S. Kshevetskii https://doi.org/10.1134/S0016793219040030
- Simulation of Propagation of Acoustic-Gravity Waves Generated by Tropospheric Front Instabilities into the Upper Atmosphere S. Kshevetskii et al. https://doi.org/10.1007/s00024-020-02569-y
- Identification of spectrum of secondary acoustic-gravity waves in the middle and upper atmosphere in a high-resolution numerical model N. Gavrilov & S. Kshevetskii https://doi.org/10.12737/stp-93202310
- Decay times of atmospheric acoustic–gravity waves after deactivation of wave forcing N. Gavrilov et al. https://doi.org/10.5194/acp-22-13713-2022
- Critical level influence on the spectra of secondary gravity waves in the middle and upper atmosphere N. Gavrilov et al. https://doi.org/10.12737/stp-121202612
- Features of the Supersonic Gravity Wave Penetration from the Earth’s Surface to the Upper Atmosphere N. Gavrilov & S. Kshevetskii https://doi.org/10.1007/s11141-018-9885-4
- Disturbances of the Thermosphere and the Ionosphere during a Meteorological Storm O. Borchevkina et al. https://doi.org/10.3390/atmos12111384
- Identification of spectrum of secondary acoustic-gravity waves in the middle and upper atmosphere in a high-resolution numerical model N. Gavrilov & S. Kshevetskii https://doi.org/10.12737/szf-93202310
- Tunneling of acoustic-gravity waves through critical levels to the upper atmosphere N. Gavrilov et al. https://doi.org/10.1016/j.asr.2024.12.005
- Numerical study of heating the upper atmosphere by acoustic-gravity waves from a local source on the Earth's surface and influence of this heating on the wave propagation conditions I. Karpov & S. Kshevetskii https://doi.org/10.1016/j.jastp.2017.07.019
- Well-Posedness of a Problem of Propagation of Nonlinear Acoustic-Gravity Waves in the Atmosphere Generated by Surface Pressure Variations Y. Kurdyaeva et al. https://doi.org/10.1134/S1995423917040048
- Critical level influence on spectra of secondary gravity waves in the middle and upper atmosphere N. Gavrilov et al. https://doi.org/10.12737/szf-121202612
Saved (final revised paper)
Latest update: 07 Jun 2026
Short summary
We performed high-resolution numerical simulations of nonlinear acoustic-gravity waves (AGWs) at altitudes 0–500km and compared them with analytical polarization relations of linear AGW theory. After some transition time, t > te, the numbers of numerically simulated and analytical pairs of AGW parameters, which are equal to confidence 95%, are larger at altitudes 30-60km and are smaller at t < te. The differences reveal circumstances where numerical simulations of waves are required.
We performed high-resolution numerical simulations of nonlinear acoustic-gravity waves (AGWs) at...