20 citations as recorded by crossref.

1. Dynamical processes in the midlatitude mesosphere S. Panasenko et al.
2. A Simulation Study of the Effect of Geomagnetic Activity on the Global Circulation in the Earth’s Middle Atmosphere I. Mingalev et al.
3. A study into the effects of gravity wave activity on the diurnal tide and airglow emissions in the equatorial mesosphere and lower thermosphere using the Coupled Middle Atmosphere and Thermosphere (CMAT) general circulation model S. England et al.
4. Numerical Simulation of the Global Neutral Wind System of the Earth’s Middle Atmosphere for Different Seasons I. Mingalev et al.
5. Solar variability, coupling between atmospheric layers and climate change J. Thompson & N. Arnold
6. Modelled effect of changes in the CO2 concentration on the middle and upper atmosphere: Sensitivity to gravity wave parameterization I. Cnossen et al.
7. The global ionosphere–thermosphere model A. Ridley et al.
8. GCITEM-IGGCAS: A new global coupled ionosphere–thermosphere-electrodynamics model Z. Ren et al.
9. Numerical Modeling of the Influence of Solar Activity on the Global Circulation in the Earth’s Mesosphere and Lower Thermosphere I. Mingalev & V. Mingalev
10. A Review of the Effects of Non-migrating Atmospheric Tides on the Earth’s Low-Latitude Ionosphere S. England
11. Orbit-centered atmospheric density prediction using artificial neural networks D. Pérez et al.
12. An Overview of Ionosphere—Thermosphere Models Available for Space Weather Purposes A. Belehaki et al.
13. A Computational Study of the Transformation of Global Gas Flows in the Earth’s Atmosphere over the Course of a Year I. Mingalev et al.
14. Disturbances of the circulation of the lower and middle atmosphere, which can be caused by an isolated mountain array I. Mingalev et al.
15. Neutral Atmospheres I. Mueller-Wodarg et al.
16. Global EAGLE Model as a Tool for Studying the Influence of the Atmosphere on the Electric Field in the Equatorial Ionosphere V. Klimenko et al.
17. Disturbances in the Circulation of the Lower and Middle Atmosphere That Can be Caused by an Isolated Mountain Range I. Mingalev et al.
18. Comparing high-latitude thermospheric winds from Fabry–Perot interferometer (FPI) and challenging mini-satellite payload (CHAMP) accelerometer measurements A. Aruliah et al.
19. Numerical Modeling the Circulation of the Antarctic’s Lower and Middle Atmosphere and Its Dependence on the Earth’s Relief I. Mingalev et al.
20. Numerical Modeling of the Influence of the Relief of a Planet on the Global Circulation of the Earth’s Stratosphere and Mesosphere I. Mingalev et al.