Stratopheric greenhouse gas observation using a balloon-borne cryogenic sampler at Syowa Station, Antarctica

Balloon-borne cryogenic samplers were launched from Japanese Antarctic Station, Syowa, on December 26, 2003 and January 5, 2004. Stratospheric air samples were successfully collected at 11 different altitudes from 10 to 30 km. After air samples were transported to Japan, they were analyzed for vario...

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Main Authors: Satoshi Sugawara, Sakae Toyoda, Shigeyuki Ishidoya, Shinji Morimoto, Gen Hashida, Shuji Aoki, Takakiyo Nakazawa, Takashi Yamanouchi, Hideyuki Honda
Format: Article in Journal/Newspaper
Language:English
Published: National Institute of Polar Research 2010
Subjects:
geo
Online Access:https://doi.org/10.15094/00009564
https://doaj.org/article/6f1bca6e05f845cfaac845d9ab35e085
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:6f1bca6e05f845cfaac845d9ab35e085 2023-05-15T13:51:47+02:00 Stratopheric greenhouse gas observation using a balloon-borne cryogenic sampler at Syowa Station, Antarctica Satoshi Sugawara Sakae Toyoda Shigeyuki Ishidoya Shinji Morimoto Gen Hashida Shuji Aoki Takakiyo Nakazawa Takashi Yamanouchi Hideyuki Honda 2010-12-01 https://doi.org/10.15094/00009564 https://doaj.org/article/6f1bca6e05f845cfaac845d9ab35e085 en other eng National Institute of Polar Research doi:10.15094/00009564 0085-7289 2432-079X https://doaj.org/article/6f1bca6e05f845cfaac845d9ab35e085 undefined Antarctic Record, Vol 54, Iss special issue, Pp 410-425 (2010) geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2010 fttriple https://doi.org/10.15094/00009564 2023-01-22T17:51:35Z Balloon-borne cryogenic samplers were launched from Japanese Antarctic Station, Syowa, on December 26, 2003 and January 5, 2004. Stratospheric air samples were successfully collected at 11 different altitudes from 10 to 30 km. After air samples were transported to Japan, they were analyzed for various greenhouse gases and their isotopes. The CO_2 concentration, thus obtained, shows no significant vertical gradient above 20 km. Secular increase of CO_2 concentration was clearly observable in the mid-stratosphere over Syowa station. From the average CO_2 concentrations in 1998 and 2004, the concentration difference was calculated to be 9.7 ppm, which is almost same the tropospheric trend. The average mean age was estimated to be 5.0±0.2 years above 20 km. This value was almost the same as that estimated from the CO_2 concentration data in 1998, 4.9±0.2 years. This result implies that there is no secular change of the mean age in the Antarctic stratosphere during this period. Vertical distributions of N_2O isotopomer ratios showed different characteristics among December, January, and previous observations in January 1998, showing that the short-term and long-term effects of transport processes. Article in Journal/Newspaper Antarc* Antarctic Antarctica Unknown Antarctic Syowa Station The Antarctic
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
spellingShingle geo
Satoshi Sugawara
Sakae Toyoda
Shigeyuki Ishidoya
Shinji Morimoto
Gen Hashida
Shuji Aoki
Takakiyo Nakazawa
Takashi Yamanouchi
Hideyuki Honda
Stratopheric greenhouse gas observation using a balloon-borne cryogenic sampler at Syowa Station, Antarctica
topic_facet geo
description Balloon-borne cryogenic samplers were launched from Japanese Antarctic Station, Syowa, on December 26, 2003 and January 5, 2004. Stratospheric air samples were successfully collected at 11 different altitudes from 10 to 30 km. After air samples were transported to Japan, they were analyzed for various greenhouse gases and their isotopes. The CO_2 concentration, thus obtained, shows no significant vertical gradient above 20 km. Secular increase of CO_2 concentration was clearly observable in the mid-stratosphere over Syowa station. From the average CO_2 concentrations in 1998 and 2004, the concentration difference was calculated to be 9.7 ppm, which is almost same the tropospheric trend. The average mean age was estimated to be 5.0±0.2 years above 20 km. This value was almost the same as that estimated from the CO_2 concentration data in 1998, 4.9±0.2 years. This result implies that there is no secular change of the mean age in the Antarctic stratosphere during this period. Vertical distributions of N_2O isotopomer ratios showed different characteristics among December, January, and previous observations in January 1998, showing that the short-term and long-term effects of transport processes.
format Article in Journal/Newspaper
author Satoshi Sugawara
Sakae Toyoda
Shigeyuki Ishidoya
Shinji Morimoto
Gen Hashida
Shuji Aoki
Takakiyo Nakazawa
Takashi Yamanouchi
Hideyuki Honda
author_facet Satoshi Sugawara
Sakae Toyoda
Shigeyuki Ishidoya
Shinji Morimoto
Gen Hashida
Shuji Aoki
Takakiyo Nakazawa
Takashi Yamanouchi
Hideyuki Honda
author_sort Satoshi Sugawara
title Stratopheric greenhouse gas observation using a balloon-borne cryogenic sampler at Syowa Station, Antarctica
title_short Stratopheric greenhouse gas observation using a balloon-borne cryogenic sampler at Syowa Station, Antarctica
title_full Stratopheric greenhouse gas observation using a balloon-borne cryogenic sampler at Syowa Station, Antarctica
title_fullStr Stratopheric greenhouse gas observation using a balloon-borne cryogenic sampler at Syowa Station, Antarctica
title_full_unstemmed Stratopheric greenhouse gas observation using a balloon-borne cryogenic sampler at Syowa Station, Antarctica
title_sort stratopheric greenhouse gas observation using a balloon-borne cryogenic sampler at syowa station, antarctica
publisher National Institute of Polar Research
publishDate 2010
url https://doi.org/10.15094/00009564
https://doaj.org/article/6f1bca6e05f845cfaac845d9ab35e085
geographic Antarctic
Syowa Station
The Antarctic
geographic_facet Antarctic
Syowa Station
The Antarctic
genre Antarc*
Antarctic
Antarctica
genre_facet Antarc*
Antarctic
Antarctica
op_source Antarctic Record, Vol 54, Iss special issue, Pp 410-425 (2010)
op_relation doi:10.15094/00009564
0085-7289
2432-079X
https://doaj.org/article/6f1bca6e05f845cfaac845d9ab35e085
op_rights undefined
op_doi https://doi.org/10.15094/00009564
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