Airborne observation of CO2 mixing ratio in the Arctic troposphere and lower stratosphere

Tropospheric and lower stratospheric CO2 mixing ratios were measured onboard an aircraft in the Arctic Airborne Measurement Program 1998. Steep vertical gradients in CO2 mixing ratio were observed in the lower stratosphere. Small gradients were seen in the troposphere, reflecting weak sources and si...

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Bibliographic Details
Main Authors: Toshinobu Machida, Shamil Maksyutov, Satoshi Sugawara, Shinji Morimoto
Format: Article in Journal/Newspaper
Language:English
Japanese
Published: National Institute of Polar Research 2002
Subjects:
Online Access:https://doi.org/10.15094/00009209
https://doaj.org/article/c6dddb27ca2d467f996b6000a84a2992
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Summary:Tropospheric and lower stratospheric CO2 mixing ratios were measured onboard an aircraft in the Arctic Airborne Measurement Program 1998. Steep vertical gradients in CO2 mixing ratio were observed in the lower stratosphere. Small gradients were seen in the troposphere, reflecting weak sources and sinks for CO2 in winter. A significant increase in CO2 mixing ratio was found during level flight in the lower stratosphere. Back trajectory analysis indicated that rapid upward transport brought high CO2 to the observation area. Spatial variations of CO2 mixing ratio were highly correlated with O3 mixing ratio. It is suggested that CO2 distribution was produced mainly by air transport and mixing.