Observations of resonant scattering in the thermosphere and upper mesosphere in the winter season of 2021
An analysis of the Kamchatka lidar station data obtained in January-February 2021 is presented. Pronounced light scattering layers at altitudes of 300 km have been detected. Layers at these heights appear during precipitation of electrons with energies of about 300 eV. Analysis of the lidar data sho...
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EDP Sciences
2021
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oai:doaj.org-article:55195b6a0d7346c581297bd2f417dbd72021-11-12T11:44:52ZObservations of resonant scattering in the thermosphere and upper mesosphere in the winter season of 20212100-014X10.1051/epjconf/202125401005https://doaj.org/article/55195b6a0d7346c581297bd2f417dbd72021-01-01T00:00:00Zhttps://www.epj-conferences.org/articles/epjconf/pdf/2021/08/epjconf_strpep2021_01005.pdfhttps://doaj.org/toc/2100-014XAn analysis of the Kamchatka lidar station data obtained in January-February 2021 is presented. Pronounced light scattering layers at altitudes of 300 km have been detected. Layers at these heights appear during precipitation of electrons with energies of about 300 eV. Analysis of the lidar data showed that increased light scattering was observed at the heights of the mesosphere, accompanied by an increase in the ionospheric parameter fmin. It was concluded that the observed aerosol formations in the mesopause region could be caused by precipitation of charged particles with energies of ∼ 500 keV. Aerosol formations in the area of 60-75 km should be recognized as imaginary. This is a manifestation of resonant scattering by excited ions of atomic nitrogenBychkov VasilySeredkin IliaDmitriev AlexeiEDP SciencesarticlePhysicsQC1-999ENEPJ Web of Conferences, Vol 254, p 01005 (2021) |
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Physics QC1-999 |
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Physics QC1-999 Bychkov Vasily Seredkin Ilia Dmitriev Alexei Observations of resonant scattering in the thermosphere and upper mesosphere in the winter season of 2021 |
description |
An analysis of the Kamchatka lidar station data obtained in January-February 2021 is presented. Pronounced light scattering layers at altitudes of 300 km have been detected. Layers at these heights appear during precipitation of electrons with energies of about 300 eV. Analysis of the lidar data showed that increased light scattering was observed at the heights of the mesosphere, accompanied by an increase in the ionospheric parameter fmin. It was concluded that the observed aerosol formations in the mesopause region could be caused by precipitation of charged particles with energies of ∼ 500 keV. Aerosol formations in the area of 60-75 km should be recognized as imaginary. This is a manifestation of resonant scattering by excited ions of atomic nitrogen |
format |
article |
author |
Bychkov Vasily Seredkin Ilia Dmitriev Alexei |
author_facet |
Bychkov Vasily Seredkin Ilia Dmitriev Alexei |
author_sort |
Bychkov Vasily |
title |
Observations of resonant scattering in the thermosphere and upper mesosphere in the winter season of 2021 |
title_short |
Observations of resonant scattering in the thermosphere and upper mesosphere in the winter season of 2021 |
title_full |
Observations of resonant scattering in the thermosphere and upper mesosphere in the winter season of 2021 |
title_fullStr |
Observations of resonant scattering in the thermosphere and upper mesosphere in the winter season of 2021 |
title_full_unstemmed |
Observations of resonant scattering in the thermosphere and upper mesosphere in the winter season of 2021 |
title_sort |
observations of resonant scattering in the thermosphere and upper mesosphere in the winter season of 2021 |
publisher |
EDP Sciences |
publishDate |
2021 |
url |
https://doaj.org/article/55195b6a0d7346c581297bd2f417dbd7 |
work_keys_str_mv |
AT bychkovvasily observationsofresonantscatteringinthethermosphereanduppermesosphereinthewinterseasonof2021 AT seredkinilia observationsofresonantscatteringinthethermosphereanduppermesosphereinthewinterseasonof2021 AT dmitrievalexei observationsofresonantscatteringinthethermosphereanduppermesosphereinthewinterseasonof2021 |
_version_ |
1718430553098682368 |