Atmospheric CF2Cl2 and CFCl3 in Antarctica over the period between February 1982 and January 1987 (abstract)

P(論文) In order to understand the global distributions and trends of atmospheric CF_2Cl_2,CFCl_3,and N_2O, air samples have been collected at Syowa Station since February 1982 (JARE-23). Samples were analyzed by a GC-ECD method. In JARE-27,seventeen air samples were collected at Syowa Station between...

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Main Authors: Hirota, Michio, Fukabori, Masashi, Yamanouchi, Takashi, Makino, Yukio
Language:English
Published: National Institute of Polar Research 1989
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/3582/files/KJ00000035548.pdf
https://doi.org/10.15094/00003582
https://nipr.repo.nii.ac.jp/records/3582
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author Hirota, Michio
Fukabori, Masashi
Yamanouchi, Takashi
Makino, Yukio
author_facet Hirota, Michio
Fukabori, Masashi
Yamanouchi, Takashi
Makino, Yukio
author_sort Hirota, Michio
collection National Institute of Polar Research Repository, Japan
description P(論文) In order to understand the global distributions and trends of atmospheric CF_2Cl_2,CFCl_3,and N_2O, air samples have been collected at Syowa Station since February 1982 (JARE-23). Samples were analyzed by a GC-ECD method. In JARE-27,seventeen air samples were collected at Syowa Station between February 1986 and January 1987. Linear trends were calculated with the data of the period between February 1982 and January 1987. Volume mixing ratios as of Januaries 1985 and 1987 were 345 and 376 ppt for CF_2Cl_2,and 202 and 222 ppt for CFCl_3. Annual increases were 15 ppt/year for CF_2Cl_2 and 10 ppt/year for CFCl_3. According to RASMUSSEN and KHALIL (Science, 232,1623,1986), volume mixing ratios as of January 1985 were 354 ppt for CF_2Cl_2 and 205 ppt for CFCl_3,and annual increases between Januaries 1982 and 1985 at the South Pole were 17 ppt/year for CF_2Cl_2 and 9 ppt/year for CFCl_3. These are in agreement with ours. These results indicate that atmospheric CF_2Cl_2 and CFCl_3 have been still accumulating in the 1980's in Antarctica. departmental bulletin paper
genre Antarc*
Antarctica
Polar meteorology and glaciology
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
South pole
South pole
genre_facet Antarc*
Antarctica
Polar meteorology and glaciology
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
South pole
South pole
geographic Rasmussen
South Pole
Syowa Station
geographic_facet Rasmussen
South Pole
Syowa Station
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institution Open Polar
language English
long_lat ENVELOPE(-64.084,-64.084,-65.248,-65.248)
op_collection_id ftnipr
op_doi https://doi.org/10.15094/00003582
op_relation Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
2
172
AA10756213
https://nipr.repo.nii.ac.jp/record/3582/files/KJ00000035548.pdf
https://doi.org/10.15094/00003582
https://nipr.repo.nii.ac.jp/records/3582
publishDate 1989
publisher National Institute of Polar Research
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00003582 2025-04-13T14:07:53+00:00 Atmospheric CF2Cl2 and CFCl3 in Antarctica over the period between February 1982 and January 1987 (abstract) Hirota, Michio Fukabori, Masashi Yamanouchi, Takashi Makino, Yukio 1989-08 application/pdf https://nipr.repo.nii.ac.jp/record/3582/files/KJ00000035548.pdf https://doi.org/10.15094/00003582 https://nipr.repo.nii.ac.jp/records/3582 eng eng National Institute of Polar Research Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology 2 172 AA10756213 https://nipr.repo.nii.ac.jp/record/3582/files/KJ00000035548.pdf https://doi.org/10.15094/00003582 https://nipr.repo.nii.ac.jp/records/3582 1989 ftnipr https://doi.org/10.15094/00003582 2025-03-19T10:19:56Z P(論文) In order to understand the global distributions and trends of atmospheric CF_2Cl_2,CFCl_3,and N_2O, air samples have been collected at Syowa Station since February 1982 (JARE-23). Samples were analyzed by a GC-ECD method. In JARE-27,seventeen air samples were collected at Syowa Station between February 1986 and January 1987. Linear trends were calculated with the data of the period between February 1982 and January 1987. Volume mixing ratios as of Januaries 1985 and 1987 were 345 and 376 ppt for CF_2Cl_2,and 202 and 222 ppt for CFCl_3. Annual increases were 15 ppt/year for CF_2Cl_2 and 10 ppt/year for CFCl_3. According to RASMUSSEN and KHALIL (Science, 232,1623,1986), volume mixing ratios as of January 1985 were 354 ppt for CF_2Cl_2 and 205 ppt for CFCl_3,and annual increases between Januaries 1982 and 1985 at the South Pole were 17 ppt/year for CF_2Cl_2 and 9 ppt/year for CFCl_3. These are in agreement with ours. These results indicate that atmospheric CF_2Cl_2 and CFCl_3 have been still accumulating in the 1980's in Antarctica. departmental bulletin paper Other/Unknown Material Antarc* Antarctica Polar meteorology and glaciology Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology South pole South pole National Institute of Polar Research Repository, Japan Rasmussen ENVELOPE(-64.084,-64.084,-65.248,-65.248) South Pole Syowa Station
spellingShingle Hirota, Michio
Fukabori, Masashi
Yamanouchi, Takashi
Makino, Yukio
Atmospheric CF2Cl2 and CFCl3 in Antarctica over the period between February 1982 and January 1987 (abstract)
title Atmospheric CF2Cl2 and CFCl3 in Antarctica over the period between February 1982 and January 1987 (abstract)
title_full Atmospheric CF2Cl2 and CFCl3 in Antarctica over the period between February 1982 and January 1987 (abstract)
title_fullStr Atmospheric CF2Cl2 and CFCl3 in Antarctica over the period between February 1982 and January 1987 (abstract)
title_full_unstemmed Atmospheric CF2Cl2 and CFCl3 in Antarctica over the period between February 1982 and January 1987 (abstract)
title_short Atmospheric CF2Cl2 and CFCl3 in Antarctica over the period between February 1982 and January 1987 (abstract)
title_sort atmospheric cf2cl2 and cfcl3 in antarctica over the period between february 1982 and january 1987 (abstract)
url https://nipr.repo.nii.ac.jp/record/3582/files/KJ00000035548.pdf
https://doi.org/10.15094/00003582
https://nipr.repo.nii.ac.jp/records/3582