Airborne measurements of greenhouse gases during AAMP98
Air samples collected using aircraft during the Arctic Airborne Measurement Program 1998 (AAMP 98) were analyzed for the CO2, CH4, N20, and CO concentrations as well as for the carbon and oxygen isotopic ratios,δ^13C and δ^18O,of CO2, and δ^13C of CH4. The vertical distributions of CO2, CH4, N2O, an...
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National Institute of Polar Research
2002-06-01
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Series: | Antarctic Record |
Online Access: | http://doi.org/10.15094/00009211 |
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doaj-a6165ad103d44a7b9ec591ecef9f82b62020-11-24T23:41:41ZengNational Institute of Polar ResearchAntarctic Record0085-72892432-079X2002-06-01461A14715410.15094/00009211Airborne measurements of greenhouse gases during AAMP98Satoshi Sugawara0Shinji Morimoto1Shuji Aoki2Takakiyo Nakazawa3Institute of Earth Science, Miyagi University of EducationNational Institute of Polar ResearchCenter for Atmospheric and Oceanic Studies, Graduate School of Science, Tohoku UniversityCenter for Atmospheric and Oceanic Studies, Graduate School of Science, Tohoku UniversityAir samples collected using aircraft during the Arctic Airborne Measurement Program 1998 (AAMP 98) were analyzed for the CO2, CH4, N20, and CO concentrations as well as for the carbon and oxygen isotopic ratios,δ^13C and δ^18O,of CO2, and δ^13C of CH4. The vertical distributions of CO2, CH4, N2O, and CO concentrations showed rapid decreases from the tropopause to the lower stratosphere over Ny-Alesund and Barrow. From the measured values of the CH4 concentration and δ^13C, the apparent carbon isotopic fractionation factor was estimated to be 1.013 (士0.003) in the lower stratosphere. The contributions of the chemical CH4 reactions with OH, O(^1 D) and Cl were examined by using the isotopic fractionation factors. It is suggested from this examination that the contribution of the reaction of CH4 with Cl is 12-17%. http://doi.org/10.15094/00009211 |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Satoshi Sugawara Shinji Morimoto Shuji Aoki Takakiyo Nakazawa |
spellingShingle |
Satoshi Sugawara Shinji Morimoto Shuji Aoki Takakiyo Nakazawa Airborne measurements of greenhouse gases during AAMP98 Antarctic Record |
author_facet |
Satoshi Sugawara Shinji Morimoto Shuji Aoki Takakiyo Nakazawa |
author_sort |
Satoshi Sugawara |
title |
Airborne measurements of greenhouse gases during AAMP98 |
title_short |
Airborne measurements of greenhouse gases during AAMP98 |
title_full |
Airborne measurements of greenhouse gases during AAMP98 |
title_fullStr |
Airborne measurements of greenhouse gases during AAMP98 |
title_full_unstemmed |
Airborne measurements of greenhouse gases during AAMP98 |
title_sort |
airborne measurements of greenhouse gases during aamp98 |
publisher |
National Institute of Polar Research |
series |
Antarctic Record |
issn |
0085-7289 2432-079X |
publishDate |
2002-06-01 |
description |
Air samples collected using aircraft during the Arctic Airborne Measurement Program 1998 (AAMP 98) were analyzed for the CO2, CH4, N20, and CO concentrations as well as for the carbon and oxygen isotopic ratios,δ^13C and δ^18O,of CO2, and δ^13C of CH4. The vertical distributions of CO2, CH4, N2O, and CO concentrations showed rapid decreases from the tropopause to the lower stratosphere over Ny-Alesund and Barrow. From the measured values of the CH4 concentration and δ^13C, the apparent carbon isotopic fractionation factor was estimated to be 1.013 (士0.003) in the lower stratosphere. The contributions of the chemical CH4 reactions with OH, O(^1 D) and Cl were examined by using the isotopic fractionation factors. It is suggested from this examination that the contribution of the reaction of CH4 with Cl is 12-17%. |
url |
http://doi.org/10.15094/00009211 |
work_keys_str_mv |
AT satoshisugawara airbornemeasurementsofgreenhousegasesduringaamp98 AT shinjimorimoto airbornemeasurementsofgreenhousegasesduringaamp98 AT shujiaoki airbornemeasurementsofgreenhousegasesduringaamp98 AT takakiyonakazawa airbornemeasurementsofgreenhousegasesduringaamp98 |
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