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Anomalous Dynamics of Tropospheric Ozone in the Spring of 2020 in Central Russia

Anomalously low ozone concentrations in the surface atmosphere in central Russia were recorded in spring of 2020. The increase in the ozone content usual for spring due to a seasonal increase in the temperature and light was followed by a monotonic decrease. The maximum daily values of surface ozone...

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Detalles Bibliográficos
Autores principales: Kotelnikov, S. N., Stepanov, E. V.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Pleiades Publishing 2021
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8095468/
http://dx.doi.org/10.3103/S1068335621030076
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author Kotelnikov, S. N.
Stepanov, E. V.
author_facet Kotelnikov, S. N.
Stepanov, E. V.
author_sort Kotelnikov, S. N.
collection PubMed
description Anomalously low ozone concentrations in the surface atmosphere in central Russia were recorded in spring of 2020. The increase in the ozone content usual for spring due to a seasonal increase in the temperature and light was followed by a monotonic decrease. The maximum daily values of surface ozone concentrations averaged over the month in April 2020 were three times less than the values recorded at the same time in 2019. Both a decrease in regional background ozone concentrations in the near-surface atmosphere and a decrease in the intensity of its photochemical formation were observed. The most probable cause of the observed phenomenon is a decrease in combustion product emissions into the atmosphere in China, Europe, and Russia due to the introduction of special regimes in connection with the COVID-19 pandemic.
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spelling pubmed-80954682021-05-05 Anomalous Dynamics of Tropospheric Ozone in the Spring of 2020 in Central Russia Kotelnikov, S. N. Stepanov, E. V. Bull. Lebedev Phys. Inst. Article Anomalously low ozone concentrations in the surface atmosphere in central Russia were recorded in spring of 2020. The increase in the ozone content usual for spring due to a seasonal increase in the temperature and light was followed by a monotonic decrease. The maximum daily values of surface ozone concentrations averaged over the month in April 2020 were three times less than the values recorded at the same time in 2019. Both a decrease in regional background ozone concentrations in the near-surface atmosphere and a decrease in the intensity of its photochemical formation were observed. The most probable cause of the observed phenomenon is a decrease in combustion product emissions into the atmosphere in China, Europe, and Russia due to the introduction of special regimes in connection with the COVID-19 pandemic. Pleiades Publishing 2021-05-04 2021 /pmc/articles/PMC8095468/ http://dx.doi.org/10.3103/S1068335621030076 Text en © Allerton Press, Inc. 2021, ISSN 1068-3356, Bulletin of the Lebedev Physics Institute, 2021, Vol. 48, No. 3, pp. 92–96. © Allerton Press, Inc., 2021.Russian Text © The Author(s), 2021, published in Kratkie Soobshcheniya po Fizike, 2021, Vol. 48, No. 3, pp. 44–54. This article is made available via the PMC Open Access Subset for unrestricted research re-use and secondary analysis in any form or by any means with acknowledgement of the original source. These permissions are granted for the duration of the World Health Organization (WHO) declaration of COVID-19 as a global pandemic.
spellingShingle Article
Kotelnikov, S. N.
Stepanov, E. V.
Anomalous Dynamics of Tropospheric Ozone in the Spring of 2020 in Central Russia
title Anomalous Dynamics of Tropospheric Ozone in the Spring of 2020 in Central Russia
title_full Anomalous Dynamics of Tropospheric Ozone in the Spring of 2020 in Central Russia
title_fullStr Anomalous Dynamics of Tropospheric Ozone in the Spring of 2020 in Central Russia
title_full_unstemmed Anomalous Dynamics of Tropospheric Ozone in the Spring of 2020 in Central Russia
title_short Anomalous Dynamics of Tropospheric Ozone in the Spring of 2020 in Central Russia
title_sort anomalous dynamics of tropospheric ozone in the spring of 2020 in central russia
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8095468/
http://dx.doi.org/10.3103/S1068335621030076
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