Magnetospheric Electron Precipitation Recorded in the Atmosphere at Middle and Polar Latitudes in 2022–2023

The study of precipitation of high-energy electrons from the magnetosphere into the Earth’s atmosphere is important for studying the physical mechanisms of electron acceleration during interplanetary disturbances in near-Earth space, the processes of formation of trapped electron fluxes in the magnetosphere and their subsequent precipitation into the atmosphere. In addition, the precipitating electrons affect the spacecraft operation and often lead to significant destruction of mesospheric ozone, etc. Since 1957, the Dolgoprudny Scientific Station of the Lebedev Physical Institute has been conducting continuous measurements of cosmic ray fluxes at altitudes of 0–30 km in the atmosphere of polar latitudes (Murmansk oblast, Antarctica) and at middle latitude (Moscow oblast). During this time, almost 600 cases of electron precipitation were recorded, mainly from the Earth’s outer radiation belt near its polar boundary due to measurement in Murmansk oblast. At the same time, several cases of electron precipitation were recorded at mid-latitude (Moscow oblast) and at the Mirny station in Antarctica, in particular, in 2022–2023. The paper discusses interplanetary and geomagnetic conditions during these events. Analysis of measurement data in the stratosphere made it possible to establish the absorption spectra of secondary bremsstrahlung photons and, on their basis, using the method we developed, to determine the primary energy spectra of precipitating magnetospheric electrons.

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Publication Details

Journal
Cosmic Research
Published
2024-12-01
DOI
https://doi.org/10.1134/s0010952524600446
Primary Topic
Ionosphere and magnetosphere dynamics
Type
article
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article

Magnetospheric Electron Precipitation Recorded in the Atmosphere at Middle and Polar Latitudes in 2022–2023

N. S. Svirzhevsky, А. Н. Квашнин, Y. I. Stozhkov, В. С. Махмутов et al.
Cosmic Research
Ionosphere and magnetosphere dynamics
article

Magnetospheric Electron Precipitation Recorded in the Atmosphere at Middle and Polar Latitudes in 2022–2023

N. S. Svirzhevsky, А. Н. Квашнин, Y. I. Stozhkov, В. С. Махмутов, G. A. Bazilevskaya, М. Б. Крайнев, A. K. Svirzhevskaya
article en

Abstract

The study of precipitation of high-energy electrons from the magnetosphere into the Earth’s atmosphere is important for studying the physical mechanisms of electron acceleration during interplanetary disturbances in near-Earth space, the processes of formation of trapped electron fluxes in the magnetosphere and their subsequent precipitation into the atmosphere. In addition, the precipitating electrons affect the spacecraft operation and often lead to significant destruction of mesospheric ozone, etc. Since 1957, the Dolgoprudny Scientific Station of the Lebedev Physical Institute has been conducting continuous measurements of cosmic ray fluxes at altitudes of 0–30 km in the atmosphere of polar latitudes (Murmansk oblast, Antarctica) and at middle latitude (Moscow oblast). During this time, almost 600 cases of electron precipitation were recorded, mainly from the Earth’s outer radiation belt near its polar boundary due to measurement in Murmansk oblast. At the same time, several cases of electron precipitation were recorded at mid-latitude (Moscow oblast) and at the Mirny station in Antarctica, in particular, in 2022–2023. The paper discusses interplanetary and geomagnetic conditions during these events. Analysis of measurement data in the stratosphere made it possible to establish the absorption spectra of secondary bremsstrahlung photons and, on their basis, using the method we developed, to determine the primary energy spectra of precipitating magnetospheric electrons.

Cosmic ResearchVol. 62(6)
P.N. Lebedev Physical Institute of the Russian Academy of Sciences (RU), Moscow Institute of Physics and Technology (RU), Moscow Power Engineering Institute (RU), Lomonosov Moscow State University (RU), Moscow Aviation Institute (RU)
Climate action
Openalex Percentile: Top 84%
Ionosphere and magnetosphere dynamics
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