Gas-chromatographic measurements of atmospheric CF2Cl2, CFCl3 and N2O from Tokyo to Syowa Station late in 1993, and at Syowa Station between February 1982 and January 1984

P(論文) Atmospheric CF_2Cl_2,CFCl_3 and N_2O were measured by a gaschromatographic method in order to assess the influence of these gases on the stratospheric ozone. Air samples were successively obtained by the 24th and 25th Japanese Antarctic Research Expeditions. From Tokyo to Syowa Station, volume...

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Main Authors: Hirota, Michio, Makino, Yukio, Shiobara, Masataka, Chubachi, Shigeru, Muramatsu, Hisafumi
Language:English
Published: 1985
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/1830/files/KJ00000012462.pdf
https://nipr.repo.nii.ac.jp/records/1830
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author Hirota, Michio
Makino, Yukio
Shiobara, Masataka
Chubachi, Shigeru
Muramatsu, Hisafumi
author_facet Hirota, Michio
Makino, Yukio
Shiobara, Masataka
Chubachi, Shigeru
Muramatsu, Hisafumi
author_sort Hirota, Michio
collection National Institute of Polar Research Repository, Japan
description P(論文) Atmospheric CF_2Cl_2,CFCl_3 and N_2O were measured by a gaschromatographic method in order to assess the influence of these gases on the stratospheric ozone. Air samples were successively obtained by the 24th and 25th Japanese Antarctic Research Expeditions. From Tokyo to Syowa Station, volume mixing ratios of CF_2Cl_2 and CFCl_3 decreased toward the equator and were almost constant in the southern hemisphere. This is because most of CF_2Cl_2 and CFCl_3 have been released in the northern hemisphere. Volume mixing ratios of CF_2Cl_2 and CFCl_3 at Syowa Station as of January 1983 were lower by 6% than mean volume mixing ratios of them over Japan from October 1982 to February 1983. As for N_2O, no gradient in mixing ratio from Tokyo to Syowa Station was found. The mean value of total 19 samples was 302 ppb (=(10)^<-9>v/v). Over the period between February 1982 to January 1984,CF_2Cl_2 and CFCl_3 showed a steady increase at Syowa Station, and their annual increases were 19.2 ppt (=(10)^<-12>v/v)/year for CF_2Cl_2 and 10.2 ppt/year for CFCl_3. In the same period, N_2O was almost constant. departmental bulletin paper
genre Antarc*
Antarctic
Memoirs of National Institute of Polar Research
Polar Research
genre_facet Antarc*
Antarctic
Memoirs of National Institute of Polar Research
Polar Research
geographic Antarctic
Syowa Station
geographic_facet Antarctic
Syowa Station
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institution Open Polar
language English
op_collection_id ftnipr
op_relation Memoirs of National Institute of Polar Research. Special issue
39
57
62
AA00733561
https://nipr.repo.nii.ac.jp/record/1830/files/KJ00000012462.pdf
https://nipr.repo.nii.ac.jp/records/1830
publishDate 1985
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00001830 2025-04-13T14:08:24+00:00 Gas-chromatographic measurements of atmospheric CF2Cl2, CFCl3 and N2O from Tokyo to Syowa Station late in 1993, and at Syowa Station between February 1982 and January 1984 Hirota, Michio Makino, Yukio Shiobara, Masataka Chubachi, Shigeru Muramatsu, Hisafumi 1985-12 application/pdf https://nipr.repo.nii.ac.jp/record/1830/files/KJ00000012462.pdf https://nipr.repo.nii.ac.jp/records/1830 eng eng Memoirs of National Institute of Polar Research. Special issue 39 57 62 AA00733561 https://nipr.repo.nii.ac.jp/record/1830/files/KJ00000012462.pdf https://nipr.repo.nii.ac.jp/records/1830 1985 ftnipr 2025-03-19T10:19:56Z P(論文) Atmospheric CF_2Cl_2,CFCl_3 and N_2O were measured by a gaschromatographic method in order to assess the influence of these gases on the stratospheric ozone. Air samples were successively obtained by the 24th and 25th Japanese Antarctic Research Expeditions. From Tokyo to Syowa Station, volume mixing ratios of CF_2Cl_2 and CFCl_3 decreased toward the equator and were almost constant in the southern hemisphere. This is because most of CF_2Cl_2 and CFCl_3 have been released in the northern hemisphere. Volume mixing ratios of CF_2Cl_2 and CFCl_3 at Syowa Station as of January 1983 were lower by 6% than mean volume mixing ratios of them over Japan from October 1982 to February 1983. As for N_2O, no gradient in mixing ratio from Tokyo to Syowa Station was found. The mean value of total 19 samples was 302 ppb (=(10)^<-9>v/v). Over the period between February 1982 to January 1984,CF_2Cl_2 and CFCl_3 showed a steady increase at Syowa Station, and their annual increases were 19.2 ppt (=(10)^<-12>v/v)/year for CF_2Cl_2 and 10.2 ppt/year for CFCl_3. In the same period, N_2O was almost constant. departmental bulletin paper Other/Unknown Material Antarc* Antarctic Memoirs of National Institute of Polar Research Polar Research National Institute of Polar Research Repository, Japan Antarctic Syowa Station
spellingShingle Hirota, Michio
Makino, Yukio
Shiobara, Masataka
Chubachi, Shigeru
Muramatsu, Hisafumi
Gas-chromatographic measurements of atmospheric CF2Cl2, CFCl3 and N2O from Tokyo to Syowa Station late in 1993, and at Syowa Station between February 1982 and January 1984
title Gas-chromatographic measurements of atmospheric CF2Cl2, CFCl3 and N2O from Tokyo to Syowa Station late in 1993, and at Syowa Station between February 1982 and January 1984
title_full Gas-chromatographic measurements of atmospheric CF2Cl2, CFCl3 and N2O from Tokyo to Syowa Station late in 1993, and at Syowa Station between February 1982 and January 1984
title_fullStr Gas-chromatographic measurements of atmospheric CF2Cl2, CFCl3 and N2O from Tokyo to Syowa Station late in 1993, and at Syowa Station between February 1982 and January 1984
title_full_unstemmed Gas-chromatographic measurements of atmospheric CF2Cl2, CFCl3 and N2O from Tokyo to Syowa Station late in 1993, and at Syowa Station between February 1982 and January 1984
title_short Gas-chromatographic measurements of atmospheric CF2Cl2, CFCl3 and N2O from Tokyo to Syowa Station late in 1993, and at Syowa Station between February 1982 and January 1984
title_sort gas-chromatographic measurements of atmospheric cf2cl2, cfcl3 and n2o from tokyo to syowa station late in 1993, and at syowa station between february 1982 and january 1984
url https://nipr.repo.nii.ac.jp/record/1830/files/KJ00000012462.pdf
https://nipr.repo.nii.ac.jp/records/1830