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И. В. Мингалев

Polar Geophysical Institute

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О. В. Мингалев

Polar Geophysical Institute

V. S. Mingalev

Polar Geophysical Institute

K. G. Orlov

Polar Geophysical Institute

H. V. Malova

Lomonosov Moscow State University

O. I. Akhmetov

Polar Geophysical Institute

Л. М. Зеленый

Russian Academy of Sciences

M. N. Melnik

Polar Geophysical Institute

Z. V. Suvorova

Polar Geophysical Institute

E. A. Fedotova

N. I. Lobachevsky State University of Nizhny Novgorod

V. B. Belakhovsky

Polar Geophysical Institute

Cooperative Institutions

Russian Academy of Sciences

Polar Geophysical Institute

Space Research Institute

Centre National de la Recherche Scientifique

Institute of Terrestrial Magnetism Ionosphere and Radio Wave Propagation

Austrian Academy of Sciences

Space Research Institute

Kola Science Centre

University of Graz

Moscow Institute of Physics and Technology

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"Anisotropic” plasma equilibria in the Earth’s magnetotail with magnetic shear

Л. М. Зеленый H. V. Malova V. Yu. Popov О. В. Мингалев И. В. Мингалев

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Parameterization of the Infrared Molecular Absorption in the Earth’s Lower and Middle Atmosphere

Atmospheric and Oceanic Optics (2018)

И. В. Мингалев E. A. Fedotova K. G. Orlov

Atmosphere of Earth

10.1134/s102485601901010x

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Numerical simulation of circulation of the Titan’s atmosphere: Interpretation of measurements of the Huygens probe

Cosmic Research (2009)

И. В. Мингалев V. S. Mingalev О. В. Мингалев Bobby Kazeminejad H. Lämmer

Hydrostatic equilibrium

Circulation (fluid dynamics)

10.1134/s0010952509020038

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Gas-Dynamic General Circulation Model of the Lower and Middle Atmosphere of the Earth

Mathematical Models and Computer Simulations (2018)

B. N. Chetverushkina И. В. Мингалев K. G. Orlov В. М. Чечеткин V. S. Mingalev

Atmospheric models

Atmospheric Circulation

Atmospheric models

Atmosphere of Earth

10.1134/s2070048218020047

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MHD surface waves, fluctuations of the heliospheric current sheet and related acceleration of energetic particles in the solar wind

Olga Khabarova О. В. Мингалев H. V. Malova И. В. Мингалев Roman Kislov

Current sheet

Heliospheric current sheet

Heliosphere

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Differences in the Predicted Conditions of Shortwave Radio Communication between a Medium-Latitude Transmitter and a Receiver in the Arctic Region with the Use of Different Empirical Ionospheric Models

Geomagnetism and Aeronomy (2021)

И. В. Мингалев Z. V. Suvorova В.Н. Шубин A. M. Merzly V. V. Tikhonov

Shortwave

International Reference Ionosphere

Middle latitudes

Radio Science

High frequency

10.1134/s0016793221040095

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Formation of large-scale vortices in shear flows of the lower atmosphere of the earth in the region of tropical latitudes

Cosmic Research (2009)

O. M. Belot︠s︡erkovskiĭ И. В. Мингалев V. S. Mingalev О. В. Мингалев A. M. Oparin

Rossby number

10.1134/s0010952509060033

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Two-dimensional numerical simulation of dynamics of small-scale irregularities in the near-Earth plasma

Cosmic Research (2006)

О. В. Мингалев И. В. Мингалев V. S. Mingalev

10.1134/s0010952506050030

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A MODEL STUDY OF HOW SOLAR ACTIVITY AFFECTS THE GLOBAL CIRCULATION OF THE MIDDLE ATMOSPHERE FOR JANUARY CONDITIONS

И. В. Мингалев G. I. Mingaleva V. S. Mingalev

The non-hydrostatic model of the global neutral wind system of the Earth's atmosphere, developed earlier in the Polar Geophysical Institute, is utilized to investigate how solar activity affects the formation of the large-scale global circulation of the mesosphere and lower thermosphere. Simulations are performed for the winter period in the northern hemisphere (16 January) and for two distinct values of solar activity (F10.7=101 and 230). The simulation results indicate that solar activity ought to influence considerably on the formation of global neutral wind system in the mesosphere and lower thermosphere. The influence is conditioned by the vertical transport of air from the lower thermosphere to the mesosphere and stratosphere. This transport may be rather different under distinct solar activity conditions.

Hydrostatic equilibrium

Polar night

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A MODEL STUDY OF THE TRANSFORMATION OF THE GLOBAL CIRCULATION OF THE LOWER AND MIDDLE ATMOSPHERE DURING THE PERIOD FROM JUNE TO DECEMBER

И. В. Мингалев V. S. Mingalev A. A. Kulikov

A mathematical model of the global neutral wind system of the lower and middle atmosphere, developed earlier in the Polar Geophysical Institute, is utilized to simulate global distributions of the horizontal and vertical wind for conditions corresponding to seven dates, which belong to seven different months beginning from June. Simulations enable to investigate how the horizontal non-uniformity of the atmospheric temperature affects the formation of the lower and middle atmosphere circulation, in particular, the large-scale circumpolar vortices.

Circulation (fluid dynamics)

Atmospheric Circulation

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