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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National Institute of Polar Research
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ftdoajarticles:oai:doaj.org/article:6f1bca6e05f845cfaac845d9ab35e085 2023-05-15T13:51:23+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 2010-12-01T00:00:00Z https://doi.org/10.15094/00009564 https://doaj.org/article/6f1bca6e05f845cfaac845d9ab35e085 EN JA eng jpn National Institute of Polar Research http://doi.org/10.15094/00009564 https://doaj.org/toc/0085-7289 https://doaj.org/toc/2432-079X doi:10.15094/00009564 0085-7289 2432-079X https://doaj.org/article/6f1bca6e05f845cfaac845d9ab35e085 Antarctic Record, Vol 54, Iss special issue, Pp 410-425 (2010) Geography (General) G1-922 article 2010 ftdoajarticles https://doi.org/10.15094/00009564 2022-12-31T13:19:51Z 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 Directory of Open Access Journals: DOAJ Articles Antarctic Syowa Station The Antarctic |
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Open Polar |
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Directory of Open Access Journals: DOAJ Articles |
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ftdoajarticles |
language |
English Japanese |
topic |
Geography (General) G1-922 |
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Geography (General) G1-922 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 |
Geography (General) G1-922 |
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 |
http://doi.org/10.15094/00009564 https://doaj.org/toc/0085-7289 https://doaj.org/toc/2432-079X doi:10.15094/00009564 0085-7289 2432-079X https://doaj.org/article/6f1bca6e05f845cfaac845d9ab35e085 |
op_doi |
https://doi.org/10.15094/00009564 |
_version_ |
1766255228388114432 |