Resonant Scattering by Excited Gaseous Components as an Indicator of Ionization Processes in the Atmosphere

The results of lidar sensing of the atmosphere at altitudes in the range of 25–600 km from the Kamchatka Lidar Station (53° N, 158° E) obtained in 2008–2022 are presented. The results of an analysis of the data of two-frequency lidar sensing of the thermosphere are given. The increased scattering at...

Full description

Bibliographic Details
Published in:Atmosphere
Main Author: Vasily Bychkov
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2023
Subjects:
Online Access:https://doi.org/10.3390/atmos14020271
https://doaj.org/article/f7e161e50c3144488b3b930d09b33920
id ftdoajarticles:oai:doaj.org/article:f7e161e50c3144488b3b930d09b33920
record_format openpolar
spelling ftdoajarticles:oai:doaj.org/article:f7e161e50c3144488b3b930d09b33920 2023-05-15T16:59:19+02:00 Resonant Scattering by Excited Gaseous Components as an Indicator of Ionization Processes in the Atmosphere Vasily Bychkov 2023-01-01T00:00:00Z https://doi.org/10.3390/atmos14020271 https://doaj.org/article/f7e161e50c3144488b3b930d09b33920 EN eng MDPI AG https://www.mdpi.com/2073-4433/14/2/271 https://doaj.org/toc/2073-4433 doi:10.3390/atmos14020271 2073-4433 https://doaj.org/article/f7e161e50c3144488b3b930d09b33920 Atmosphere, Vol 14, Iss 271, p 271 (2023) atmosphere ionosphere lidar resonant scattering Meteorology. Climatology QC851-999 article 2023 ftdoajarticles https://doi.org/10.3390/atmos14020271 2023-02-26T01:31:23Z The results of lidar sensing of the atmosphere at altitudes in the range of 25–600 km from the Kamchatka Lidar Station (53° N, 158° E) obtained in 2008–2022 are presented. The results of an analysis of the data of two-frequency lidar sensing of the thermosphere are given. The increased scattering at wavelengths of 532 and 561 nm is due to resonant scattering by excited atomic nitrogen and oxygen ions. Manifestations of resonant scattering in the middle atmosphere are also discussed. It is demonstrated that these ions are excited during the process of the ionization of the main atmospheric species by the precipitation of energetic electrons. The findings show that, during lidar soundings of the middle atmosphere, the ionization process can form imaginary aerosol formations. The spectrum of precipitating electrons can be estimated from the shape and position of the maximum of the lidar signal profile. It is shown that the process of the excitation of ions in the ground state does not play any significant role in the formation of the backscattered lidar signal. The signal does not carry information about the content and height profile of ions at the ground state. The appearance of resonant scattering in the atmosphere indicates the presence of the ionization sources. Article in Journal/Newspaper Kamchatka Directory of Open Access Journals: DOAJ Articles Atmosphere 14 2 271
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic atmosphere
ionosphere
lidar
resonant scattering
Meteorology. Climatology
QC851-999
spellingShingle atmosphere
ionosphere
lidar
resonant scattering
Meteorology. Climatology
QC851-999
Vasily Bychkov
Resonant Scattering by Excited Gaseous Components as an Indicator of Ionization Processes in the Atmosphere
topic_facet atmosphere
ionosphere
lidar
resonant scattering
Meteorology. Climatology
QC851-999
description The results of lidar sensing of the atmosphere at altitudes in the range of 25–600 km from the Kamchatka Lidar Station (53° N, 158° E) obtained in 2008–2022 are presented. The results of an analysis of the data of two-frequency lidar sensing of the thermosphere are given. The increased scattering at wavelengths of 532 and 561 nm is due to resonant scattering by excited atomic nitrogen and oxygen ions. Manifestations of resonant scattering in the middle atmosphere are also discussed. It is demonstrated that these ions are excited during the process of the ionization of the main atmospheric species by the precipitation of energetic electrons. The findings show that, during lidar soundings of the middle atmosphere, the ionization process can form imaginary aerosol formations. The spectrum of precipitating electrons can be estimated from the shape and position of the maximum of the lidar signal profile. It is shown that the process of the excitation of ions in the ground state does not play any significant role in the formation of the backscattered lidar signal. The signal does not carry information about the content and height profile of ions at the ground state. The appearance of resonant scattering in the atmosphere indicates the presence of the ionization sources.
format Article in Journal/Newspaper
author Vasily Bychkov
author_facet Vasily Bychkov
author_sort Vasily Bychkov
title Resonant Scattering by Excited Gaseous Components as an Indicator of Ionization Processes in the Atmosphere
title_short Resonant Scattering by Excited Gaseous Components as an Indicator of Ionization Processes in the Atmosphere
title_full Resonant Scattering by Excited Gaseous Components as an Indicator of Ionization Processes in the Atmosphere
title_fullStr Resonant Scattering by Excited Gaseous Components as an Indicator of Ionization Processes in the Atmosphere
title_full_unstemmed Resonant Scattering by Excited Gaseous Components as an Indicator of Ionization Processes in the Atmosphere
title_sort resonant scattering by excited gaseous components as an indicator of ionization processes in the atmosphere
publisher MDPI AG
publishDate 2023
url https://doi.org/10.3390/atmos14020271
https://doaj.org/article/f7e161e50c3144488b3b930d09b33920
genre Kamchatka
genre_facet Kamchatka
op_source Atmosphere, Vol 14, Iss 271, p 271 (2023)
op_relation https://www.mdpi.com/2073-4433/14/2/271
https://doaj.org/toc/2073-4433
doi:10.3390/atmos14020271
2073-4433
https://doaj.org/article/f7e161e50c3144488b3b930d09b33920
op_doi https://doi.org/10.3390/atmos14020271
container_title Atmosphere
container_volume 14
container_issue 2
container_start_page 271
_version_ 1766051561237118976