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28日(木) 11:00 〜 12:45 201B (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)、座長:笹川 基樹(独立行政法人国立環境研究所)

12:30 〜 12:45

[AAS21-19] つくば市郊外、落石岬、波照間島および南鳥島における大気中アルゴン濃度と大気ポテンシャル酸素の同時観測

*石戸谷 重之1村山 昌平1遠嶋 康徳2坪井 一寛3松枝 秀和3田口 彰一1Prabir Patra4近藤 裕昭1 (1.産業技術総合研究所、2.国立環境研究所、3.気象研究所、4.海洋研究開発機構)

キーワード:大気中アルゴン濃度, 大気ポテンシャル酸素, 大気海洋間熱交換

Atmospheric Ar/N2 ratio is a unique tracer of spatiotemporally-integrated air-sea heat fluxes, and expected to be a new tool to validate changes in the global ocean heat content (e.g. Keeling et al. 2004; Cassar et al., 2008). The Ar/N2 ratio is also useful to estimate thermal and biological components of Atmospheric Potential Oxygen (APO = O2 +1.1xCO2) separately, so that it will contribute to better understanding of the oceanic carbon cycle. Therefore, we have developed a high-precision measurement system of the atmospheric Ar/N2 ratio and APO (Ishidoya and Murayama, 2014), which is applicable both for continuous observations and analyses of discrete flask air samples, and started systematic observations of the Ar/N2 and APO at Tsukuba (36N, 140E) and Hateruma Island (24N, 124E), Japan since 2012 and at Cape Ochi-Ishi (43N, 146E) and Minamitorishima Island (24N, 154E), Japan since 2013. Clear seasonal cycles of the Ar/N2 ratio were observed at all the sites, and the peak-to-peak amplitudes of the seasonal cycles were in the range of 15 - 50 per meg. The observed amplitudes were found to be significantly larger than those calculated using atmospheric transport models and the seasonal air-sea N2 fluxes climatology (TransCom fluxes; Garcia and Keeling et al., 2001) with a scaling factor to convert changes in the atmospheric N2 concentration to those in the Ar/N2 ratio (Blaine, 2005). We will also present preliminary estimations of the thermal and the biological APO at our sites by using the observed seasonal Ar/N2 and APO cycles.

Acknowledgements
We would like to acknowledge N. Oda and F. Shimano, Global Environmental Forum, and many staffs of Japan Meteorological Agency for their supporting the observations.

References
Blaine, T. (2005) Continuous Measurements of Atmospheric Argon/Nitrogen as a Tracer of Air-Sea Heat Flux: Models, Methods, and Data. PhD Thesis, University of California, San Diego.
Cassar, N. et al. (2008) An improved comparison of atmospheric Ar/N2 time series and paired ocean-atmosphere model predictions. J. Geophys. Res., 113, D21122. DOI: 10.1029/2008 JD009817.
Garcia, H. & Keeling, R. (2001) On the global oxygen anomaly and air-sea flux. J. Geophys. Res, 106, 31155-31166.
Ishidoya, S. & Murayama, S. (2014) Development of high precision continuous measuring system of the atmospheric O2/N2 and Ar/N2 ratios and its application to the observation in Tsukuba, Japan. Tellus B, 66, 22574, http://dx.doi.org/ 10.3402/tellusb.v66.22574.
Keeling, R. et al. (2004) Measurement of changes in atmospheric Ar/N2 ratio using a rapid-switching, single-capillary mass spectrometer system. Tellus B, 56, 322-338.