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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Bibliographic Details
Main Authors: Satoshi Sugawara, Shinji Morimoto, Shuji Aoki, Takakiyo Nakazawa
Format: Article in Journal/Newspaper
Language:English
Japanese
Published: National Institute of Polar Research 2002
Subjects:
Online Access:https://doi.org/10.15094/00009211
https://doaj.org/article/a6165ad103d44a7b9ec591ecef9f82b6
Description
Summary: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%.