Continuous measurement of surface O3 concentration at Syowa Station and onboard SHIRASE

Continuous measurements of lower tropospheric ozone have been made at Syowa Station, Antarctica, since February 1988. The diurnal variation of the lower tropospheric ozone was observable only for the austral spring; variation could not be seen in the other seasons. The average amplitude of the diurn...

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Main Author: Shuhji Aoki
Format: Article in Journal/Newspaper
Language:English
Japanese
Published: National Institute of Polar Research 1997
Subjects:
Online Access:https://doi.org/10.15094/00008972
https://doaj.org/article/26c6d2dbc8ce4912a23ea671563022e3
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spelling ftdoajarticles:oai:doaj.org/article:26c6d2dbc8ce4912a23ea671563022e3 2023-05-15T13:59:45+02:00 Continuous measurement of surface O3 concentration at Syowa Station and onboard SHIRASE Shuhji Aoki 1997-03-01T00:00:00Z https://doi.org/10.15094/00008972 https://doaj.org/article/26c6d2dbc8ce4912a23ea671563022e3 EN JA eng jpn National Institute of Polar Research http://doi.org/10.15094/00008972 https://doaj.org/toc/0085-7289 https://doaj.org/toc/2432-079X doi:10.15094/00008972 0085-7289 2432-079X https://doaj.org/article/26c6d2dbc8ce4912a23ea671563022e3 Antarctic Record, Vol 41, Iss 1, Pp 231-247 (1997) Geography (General) G1-922 article 1997 ftdoajarticles https://doi.org/10.15094/00008972 2022-12-31T14:04:39Z Continuous measurements of lower tropospheric ozone have been made at Syowa Station, Antarctica, since February 1988. The diurnal variation of the lower tropospheric ozone was observable only for the austral spring; variation could not be seen in the other seasons. The average amplitude of the diurnal variation reached a maximum value of about 2ppb at most in September and October. The maximum and minimum concentrations of the diurnal variations appear before sunrise and in the afternoon, respectively. The daily mean ozone concentrations showed a clear seasonal cycle with maximum concentration in winter and minimum concentration in summer, and mean amplitude of about 20ppb. Minimum concentrations of the seasonal cycle were almost the same for each year but maximum concentrations were variable from year to year; higher concentrations appeared in 1988 and 1990 and lower concentrations in 1989,1991 and 1992. These variations might be ascribed to changes of the atmospheric circulation in the Antarctic. It was found that extremely low values of lower tropospheric ozone with periods of a few days appeared sporadically between August and October every year. The ozone destruction phenomenon should be related to the photochemical processes in the Antarctic atmosphere. Article in Journal/Newspaper Antarc* Antarctic Antarctica Directory of Open Access Journals: DOAJ Articles Antarctic Austral Syowa Station The Antarctic
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
Japanese
topic Geography (General)
G1-922
spellingShingle Geography (General)
G1-922
Shuhji Aoki
Continuous measurement of surface O3 concentration at Syowa Station and onboard SHIRASE
topic_facet Geography (General)
G1-922
description Continuous measurements of lower tropospheric ozone have been made at Syowa Station, Antarctica, since February 1988. The diurnal variation of the lower tropospheric ozone was observable only for the austral spring; variation could not be seen in the other seasons. The average amplitude of the diurnal variation reached a maximum value of about 2ppb at most in September and October. The maximum and minimum concentrations of the diurnal variations appear before sunrise and in the afternoon, respectively. The daily mean ozone concentrations showed a clear seasonal cycle with maximum concentration in winter and minimum concentration in summer, and mean amplitude of about 20ppb. Minimum concentrations of the seasonal cycle were almost the same for each year but maximum concentrations were variable from year to year; higher concentrations appeared in 1988 and 1990 and lower concentrations in 1989,1991 and 1992. These variations might be ascribed to changes of the atmospheric circulation in the Antarctic. It was found that extremely low values of lower tropospheric ozone with periods of a few days appeared sporadically between August and October every year. The ozone destruction phenomenon should be related to the photochemical processes in the Antarctic atmosphere.
format Article in Journal/Newspaper
author Shuhji Aoki
author_facet Shuhji Aoki
author_sort Shuhji Aoki
title Continuous measurement of surface O3 concentration at Syowa Station and onboard SHIRASE
title_short Continuous measurement of surface O3 concentration at Syowa Station and onboard SHIRASE
title_full Continuous measurement of surface O3 concentration at Syowa Station and onboard SHIRASE
title_fullStr Continuous measurement of surface O3 concentration at Syowa Station and onboard SHIRASE
title_full_unstemmed Continuous measurement of surface O3 concentration at Syowa Station and onboard SHIRASE
title_sort continuous measurement of surface o3 concentration at syowa station and onboard shirase
publisher National Institute of Polar Research
publishDate 1997
url https://doi.org/10.15094/00008972
https://doaj.org/article/26c6d2dbc8ce4912a23ea671563022e3
geographic Antarctic
Austral
Syowa Station
The Antarctic
geographic_facet Antarctic
Austral
Syowa Station
The Antarctic
genre Antarc*
Antarctic
Antarctica
genre_facet Antarc*
Antarctic
Antarctica
op_source Antarctic Record, Vol 41, Iss 1, Pp 231-247 (1997)
op_relation http://doi.org/10.15094/00008972
https://doaj.org/toc/0085-7289
https://doaj.org/toc/2432-079X
doi:10.15094/00008972
0085-7289
2432-079X
https://doaj.org/article/26c6d2dbc8ce4912a23ea671563022e3
op_doi https://doi.org/10.15094/00008972
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