日本地球惑星科学連合2015年大会

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セッション記号 A (大気水圏科学) » A-AS 大気科学・気象学・大気環境

[A-AS21] 大気化学

2015年5月27日(水) 18:15 〜 19:30 コンベンションホール (2F)

コンビーナ:*澤 庸介(気象研究所海洋・地球化学研究部)、竹川 暢之(首都大学東京 大学院理工学研究科)、金谷 有剛(独立行政法人海洋研究開発機構地球環境変動領域)、高橋 けんし(京都大学生存圏研究所)、谷本 浩志(国立環境研究所)

18:15 〜 19:30

[AAS21-P24] CONTRAIL-CMEで観測された対流圏CO2の平均的時空間変動

*梅澤 拓1町田 敏暢1澤 庸介2松枝 秀和2丹羽 洋介2 (1.国立環境研究所、2.気象研究所地球化学研究部)

CONTRAIL is the ongoing project that measures atmospheric trace gases during intercontinental flights of Japan Airlines. Atmospheric CO2 concentration is analyzed using Continuous CO2 Measuring Equipment (CME) onboard the aircraft. From ~20 thousands of measurement flights since 2005, extensive number of CO2 data (~2 millions) along level-flight and ascent/descent tracks have been obtained, enabling us to well characterize spatiotemporal distributions of atmospheric CO2 covering large part of the globe especially the Asia-Pacific regions. In this study, we define ∆CO2 as a deviation from the long-term trend observed at a northern hemispheric baseline station Mauna Loa, Hawaii, to illustrate climatological CO2 distributions including seasonal and shorter-term variations. For instance, over airports in Japan, ∆CO2 reaches seasonal maximum at the end of April with higher values near the surface. In this season, high ∆CO2 spreads east of the Asian continent in the upper troposphere over the northern Pacific. In contrast, seasonal minimum of ∆CO2 occurs in September with more depletion in the upper troposphere. The summertime low ∆CO2 in the upper troposphere appears to be more pronounced over the Asian continent than over the Pacific. Likewise, we present seasonal variations of vertical profiles of tropospheric ∆CO2 over various airports and of spatial distributions in the upper troposphere in large-scale perspective, and discuss them from viewpoints of seasonally varying continental sources/sinks and atmospheric transport.