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Numerical Modeling the Circulation of the Antarctic’s Lower and Middle Atmosphere and Its Dependence on the Earth’s Relief

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Bulletin of the Russian Academy of Sciences: Physics Aims and scope

Abstract

Results are presented from numerical modeling to investigate the impact the Earth’s relief has on the circulation of the Antarctic’s lower and middle atmosphere. Modeling is done for the summer season in the Southern hemisphere (January). Results suggest the relief of the planet, and particularly the mountains of the Antarctic continent, notably influence the circulation of the Antarctic’s lower and middle atmosphere.

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CONFLICT OF INTEREST

The authors declare that they have no conflicts of interest.

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Authors and Affiliations

  1. Polar Geophysical Institute, Russian Academy of Sciences, 184209, Apatity, Murmansk oblast, Russia

    I. V. Mingalev, K. G. Orlov & V. S. Mingalev

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  1. I. V. Mingalev
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  2. K. G. Orlov
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  3. V. S. Mingalev
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Correspondence to V. S. Mingalev.

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Translated by E. Petrova

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Mingalev, I.V., Orlov, K.G. & Mingalev, V.S. Numerical Modeling the Circulation of the Antarctic’s Lower and Middle Atmosphere and Its Dependence on the Earth’s Relief. Bull. Russ. Acad. Sci. Phys. 87, 1007–1013 (2023). https://doi.org/10.3103/S1062873823702295

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  • DOI: https://doi.org/10.3103/S1062873823702295

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