Muon intensity variations and atmospheric temperature

Muons in the atmosphere are formed during the decay of pions resulting from nuclear interactions of cosmic rays with nuclei of air atoms. The resulting muons are also unstable particles with a short lifetime. Therefore, not all of them reach the level of observation in the atmosphere. When the atmos...

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Main Author: Yanchukovskiy V.L.
Format: Article
Language:English
Published: INFRA-M 2020-03-01
Series:Solar-Terrestrial Physics
Subjects:
Online Access:https://naukaru.ru/en/nauka/issue/2163/view
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spelling doaj-aa4ceb297bb64800818dd48096c3cf572020-11-25T02:02:14ZengINFRA-M Solar-Terrestrial Physics2500-05352020-03-016110811510.12737/stp-61202013Muon intensity variations and atmospheric temperature Yanchukovskiy V.L. 0A. Trofimuk Institute of Oil and Gas Geology and Geophysics SB RAS, Novosibirsk, RussiaMuons in the atmosphere are formed during the decay of pions resulting from nuclear interactions of cosmic rays with nuclei of air atoms. The resulting muons are also unstable particles with a short lifetime. Therefore, not all of them reach the level of observation in the atmosphere. When the atmospheric temperature changes, the distance to the observation level changes too, thus leading to variations in the intensity of muons of temperature origin. These variations, caused by atmospheric temperature variations, are superimposed on continuous observations of muon telescopes. Their exclusion is, therefore, extremely necessary, especially in the data from modern muon telescopes whose statistical accuracy is very high. The contribution of various atmospheric layers to the total temperature effect is not the same for muons. This contribution is characterized by the distribution of the density of temperature coefficients for muons in the atmosphere. Using this distribution and the continuous intensity observations from the muon telescope in Novosibirsk, the inverse problem has been solved, from the solution of which the atmospheric temperature variations over a long period from 2004 to 2011 have been found. The results obtained are compared with aerological sounding data.https://naukaru.ru/en/nauka/issue/2163/viewcosmic raysmuonstemperatureatmosphere
collection DOAJ
language English
format Article
sources DOAJ
author Yanchukovskiy V.L.
spellingShingle Yanchukovskiy V.L.
Muon intensity variations and atmospheric temperature
Solar-Terrestrial Physics
cosmic rays
muons
temperature
atmosphere
author_facet Yanchukovskiy V.L.
author_sort Yanchukovskiy V.L.
title Muon intensity variations and atmospheric temperature
title_short Muon intensity variations and atmospheric temperature
title_full Muon intensity variations and atmospheric temperature
title_fullStr Muon intensity variations and atmospheric temperature
title_full_unstemmed Muon intensity variations and atmospheric temperature
title_sort muon intensity variations and atmospheric temperature
publisher INFRA-M
series Solar-Terrestrial Physics
issn 2500-0535
publishDate 2020-03-01
description Muons in the atmosphere are formed during the decay of pions resulting from nuclear interactions of cosmic rays with nuclei of air atoms. The resulting muons are also unstable particles with a short lifetime. Therefore, not all of them reach the level of observation in the atmosphere. When the atmospheric temperature changes, the distance to the observation level changes too, thus leading to variations in the intensity of muons of temperature origin. These variations, caused by atmospheric temperature variations, are superimposed on continuous observations of muon telescopes. Their exclusion is, therefore, extremely necessary, especially in the data from modern muon telescopes whose statistical accuracy is very high. The contribution of various atmospheric layers to the total temperature effect is not the same for muons. This contribution is characterized by the distribution of the density of temperature coefficients for muons in the atmosphere. Using this distribution and the continuous intensity observations from the muon telescope in Novosibirsk, the inverse problem has been solved, from the solution of which the atmospheric temperature variations over a long period from 2004 to 2011 have been found. The results obtained are compared with aerological sounding data.
topic cosmic rays
muons
temperature
atmosphere
url https://naukaru.ru/en/nauka/issue/2163/view
work_keys_str_mv AT yanchukovskiyvl muonintensityvariationsandatmospherictemperature
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