Golubenko, K., I. Usoskin, E. Rozanov, E. Bard, New SOCOL:14C-Ex model reveals that the Late-Glacial radiocarbon spike in 12350 BC was caused by the record-strong extreme solar storm,Earth and Planetary Science Letters, Volume 661,2025,119383,
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Doronin, G.; Mironova, I.; Rozanov, E. Comparison of the Chemical Composition of the Middle Atmosphere During Energetic Particle Precipitation in January 2005 and 2012. Atmosphere 2025, 16, 506. https://doi.org/10.3390/atmos16050506
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Kuchar, A., T. Sukhodolov, G. Chiodo, A. Jorimann, J. Kult-Herdin, A. Stenke, E. Rozanov, and H. Rieder, Modulation of the northern polar vortex by the Hunga Tonga–Hunga Ha’apai eruption and the associated surface response, Atmos. Chem. Phys., 25, 3623–3634, 2025, https://doi.org/10.5194/acp-25-3623-2025, Q1
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Imanova, A.; Rozanov, E.; Smyshlyaev, S.; Zubov, V.; Egorova, T. Investigation of the Influence of Atmospheric Scattering on Photolysis Rates Using the Cloud-J Module, Atmosphere, 2025, 16, 58. https://doi.org/10.3390/atmos16010058
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Timofeev, Y., and G. Nerobelov, Satellite Investigations of the Atmospheric Gas Composition, Izvestiya, Atmospheric and Oceanic Physics, 2024, Vol. 60, No. 6, pp. 660–688
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Polyakov, A., E. Kriukovskikh, Ya. Virolainen, G. Nerobelov, D. Kozlov, and Yu. Timofeyev, Determining the Total Ozone Column from Spectral Measurements of IKFS-2 in 2015–2022, Izvestiya, Atmospheric and Oceanic Physics, 2024, Vol. 60, No. 6, pp. 689–698, Q4
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Nerobelov, G.; Timofeyev, Y.; Polyakov, A.; Virolainen, Y.; Rozanov, E.; Zubov, V. An Investigation of the SOCOLv4 Model’s Suitability for Predicting the Future Evolution of the Total Column Ozone. Atmosphere, 2024, 15, 1491. https://doi.org/10.3390/atmos15121491
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Koval, A.V., Gavrilov, N.M., Zubov, V.A., Rozanov, E.V., Golovko, A.G. Modified Parameterization Scheme of Orographic Gravity Waves in the SOCOL Chemistry-Climate Model. Pure Appl. Geophys. (2024). https://doi.org/10.1007/s00024-024-03619-5
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Gavrilov, N., S. Kshevetskii, A. Koval, and Yu. Kurdyaeva, Tunneling of acoustic-gravity waves through critical levels to the upper atmosphere, Advances in Space Research, 2024, doi: 10.1016/j.asr.2024.12.005