Influence of the Background Nitrogen Oxides on the Tropospheric Ozone Depletion Events in the Arctic during Springtime

Ozone depletion events (ODEs) in the springtime of the Arctic have been frequently observed since the early 1980s, and the correlation between the ozone mixing ratio during the ODEs and the nitrogen oxides (NO x ) concentration is still unclear. In the present study, the role of the background level...

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Published in:Atmosphere
Main Authors: Jiashu Zhou, Le Cao, Simeng Li
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2020
Subjects:
Online Access:https://doi.org/10.3390/atmos11040344
https://doaj.org/article/7856a82c9c634228a0ca2104b8065128
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spelling ftdoajarticles:oai:doaj.org/article:7856a82c9c634228a0ca2104b8065128 2023-05-15T14:59:11+02:00 Influence of the Background Nitrogen Oxides on the Tropospheric Ozone Depletion Events in the Arctic during Springtime Jiashu Zhou Le Cao Simeng Li 2020-03-01T00:00:00Z https://doi.org/10.3390/atmos11040344 https://doaj.org/article/7856a82c9c634228a0ca2104b8065128 EN eng MDPI AG https://www.mdpi.com/2073-4433/11/4/344 https://doaj.org/toc/2073-4433 doi:10.3390/atmos11040344 2073-4433 https://doaj.org/article/7856a82c9c634228a0ca2104b8065128 Atmosphere, Vol 11, Iss 344, p 344 (2020) concentration sensitivity analysis ozone depletion events nitrogen oxides Meteorology. Climatology QC851-999 article 2020 ftdoajarticles https://doi.org/10.3390/atmos11040344 2022-12-31T00:59:56Z Ozone depletion events (ODEs) in the springtime of the Arctic have been frequently observed since the early 1980s, and the correlation between the ozone mixing ratio during the ODEs and the nitrogen oxides (NO x ) concentration is still unclear. In the present study, the role of the background level of NO x in ODEs was investigated by using a box model implementing a chemical reaction mechanism containing 49 chemical species and 141 related reactions. A concentration sensitivity analysis was also applied to discover the dependence of the ozone mixing ratio during the ODEs on each constituent of the initial air composition. The simulation results showed that a critical value of the NO x background level exists, with which the ozone depletion rate is independent of the initial concentration of NO x , and the critical value was found to be approximately 55 ppt (ppt = part per trillion, 10 −12 mol/mol) in the present study. The concentration sensitivity analysis also showed that the existence of NO x has a two-sided impact on the depletion of ozone, depending on the initial amount of NO x . With a low background level of NO x (less than 55 ppt), the increase of the initial NO x can advance the ozone depletion. On the contrary, with a high initial NO x level (more than 55 ppt), NO x would delay the consumption of ozone during the ODEs. Article in Journal/Newspaper Arctic Directory of Open Access Journals: DOAJ Articles Arctic Atmosphere 11 4 344
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic concentration sensitivity analysis
ozone depletion events
nitrogen oxides
Meteorology. Climatology
QC851-999
spellingShingle concentration sensitivity analysis
ozone depletion events
nitrogen oxides
Meteorology. Climatology
QC851-999
Jiashu Zhou
Le Cao
Simeng Li
Influence of the Background Nitrogen Oxides on the Tropospheric Ozone Depletion Events in the Arctic during Springtime
topic_facet concentration sensitivity analysis
ozone depletion events
nitrogen oxides
Meteorology. Climatology
QC851-999
description Ozone depletion events (ODEs) in the springtime of the Arctic have been frequently observed since the early 1980s, and the correlation between the ozone mixing ratio during the ODEs and the nitrogen oxides (NO x ) concentration is still unclear. In the present study, the role of the background level of NO x in ODEs was investigated by using a box model implementing a chemical reaction mechanism containing 49 chemical species and 141 related reactions. A concentration sensitivity analysis was also applied to discover the dependence of the ozone mixing ratio during the ODEs on each constituent of the initial air composition. The simulation results showed that a critical value of the NO x background level exists, with which the ozone depletion rate is independent of the initial concentration of NO x , and the critical value was found to be approximately 55 ppt (ppt = part per trillion, 10 −12 mol/mol) in the present study. The concentration sensitivity analysis also showed that the existence of NO x has a two-sided impact on the depletion of ozone, depending on the initial amount of NO x . With a low background level of NO x (less than 55 ppt), the increase of the initial NO x can advance the ozone depletion. On the contrary, with a high initial NO x level (more than 55 ppt), NO x would delay the consumption of ozone during the ODEs.
format Article in Journal/Newspaper
author Jiashu Zhou
Le Cao
Simeng Li
author_facet Jiashu Zhou
Le Cao
Simeng Li
author_sort Jiashu Zhou
title Influence of the Background Nitrogen Oxides on the Tropospheric Ozone Depletion Events in the Arctic during Springtime
title_short Influence of the Background Nitrogen Oxides on the Tropospheric Ozone Depletion Events in the Arctic during Springtime
title_full Influence of the Background Nitrogen Oxides on the Tropospheric Ozone Depletion Events in the Arctic during Springtime
title_fullStr Influence of the Background Nitrogen Oxides on the Tropospheric Ozone Depletion Events in the Arctic during Springtime
title_full_unstemmed Influence of the Background Nitrogen Oxides on the Tropospheric Ozone Depletion Events in the Arctic during Springtime
title_sort influence of the background nitrogen oxides on the tropospheric ozone depletion events in the arctic during springtime
publisher MDPI AG
publishDate 2020
url https://doi.org/10.3390/atmos11040344
https://doaj.org/article/7856a82c9c634228a0ca2104b8065128
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source Atmosphere, Vol 11, Iss 344, p 344 (2020)
op_relation https://www.mdpi.com/2073-4433/11/4/344
https://doaj.org/toc/2073-4433
doi:10.3390/atmos11040344
2073-4433
https://doaj.org/article/7856a82c9c634228a0ca2104b8065128
op_doi https://doi.org/10.3390/atmos11040344
container_title Atmosphere
container_volume 11
container_issue 4
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