Articles | Volume 37, issue 3
Ann. Geophys., 37, 447–454, 2019
https://doi.org/10.5194/angeo-37-447-2019

Special issue: Vertical coupling in the atmosphere–ionosphere system

Ann. Geophys., 37, 447–454, 2019
https://doi.org/10.5194/angeo-37-447-2019

Regular paper 25 Jun 2019

Regular paper | 25 Jun 2019

Propagation to the upper atmosphere of acoustic-gravity waves from atmospheric fronts in the Moscow region

Yuliya Kurdyaeva et al.

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Cited articles

Alexander, M., May, P., and Beres, J.: Gravity waves generated by convection in the Darwin area during the Darwin Area Wave Experiment, J. Geophys. Res., 109, 1–11, 2004. a
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Blanc, E., Farges, T., Le Pichon, A., and Heinrich, P.: Ten year observations of gravity waves from thunderstorms in western Africa, J. Geophys. Res.-Atmos., 119, 6409–6418, 2014. a, b
Fovell, R., Durran, D., and Holton, J. R.: Numerical simulation of convectively generated stratospheric gravity waves, J. Atmos. Sci., 49, 1427–1442, 1992. a, b
Fritts, D. C. and Alexander, M. J.: Gravity wave dynamics and effects in the middle atmosphere, Rev. Geophys., 41, 1003, https://doi.org/10.1029/2001RG000106, 2003. a
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Short summary
To simulate the vertical propagation of atmospheric waves, experimental data on pressure variations at the Earth's surface are used. These data are associated with the meteorological source. The simulation results have allowed for the first time estimates of the amplitudes of temperature wave disturbances in the upper atmosphere caused by waves from the atmospheric front. The simulations have been performed using the Lomonosov supercomputer.