Seasonal variations of CO2, CH4, N2O and co in the mid-troposphere over the western north pacific observed using a C-130H cargo aircraft

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Abstract

Seasonal variations of carbon dioxide (CO2), methane (CH4), carbon monoxide (CO), and nitrous oxide (N2O), in the mid-troposphere over the western North Pacific, are investigated using air samples collected onboard a C-130H aircraft. These samples were obtained between Atsugi Base (35.45°N, 139.45°E) and Minamitorishima (MNM; 24.28°N, 153.98°E), once a month, from September 2010 to September 2012. Increasing trends of CO2 and N2O and large variability of CH4 and CO (at approximately 6 km) have been found. During summer, concentrations of CH4 and CO were found to increase with height over MNM. High concentrations of CH4 were persistently observed in the mid-troposphere throughout the observation period. The average enhancement ratios of CH4 to CO above background levels (ΔCH4/ΔCO) were 0.47 and 1.2 ppb/ppb for winter-spring and summer-fall, respectively. The results suggested that the high CH4 concentrations originated primarily from fossil fuel combustions in winter-spring, while there could be an additional contribution from increased biogenic sources during summer-fall. Because a surface station in MNM rarely observed the summer-fall high CH4 concentration values in the mid-troposphere, the aircraft measurements could provide a powerful constraint on the CH4 emission estimates for Asia, in addition to that provided by the surface measurements. This aircraft measurement program is regularly conducted for the long-term monitoring of the greenhouse gases in the mid-troposphere, and it has a significant role for filling the data gap of the existing measurement network. © 2014, Meteorological Society of Japan.

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APA

Niwa, Y., Tsuboi, K., Matsueda, H., Sawa, Y., Machida, T., Nakamura, M., … Hanamiya, Y. (2014). Seasonal variations of CO2, CH4, N2O and co in the mid-troposphere over the western north pacific observed using a C-130H cargo aircraft. Journal of the Meteorological Society of Japan, 92(1), 55–70. https://doi.org/10.2151/jmsj.2014-104

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