Model depiction of the atmospheric flows of radioactive cesium emitted from the Fukushima Daiichi Nuclear Power Station accident

被引:57
|
作者
Nakajima, Teruyuki [1 ,2 ]
Misawa, Shota [1 ]
Morino, Yu [3 ]
Tsuruta, Haruo [1 ,4 ]
Goto, Daisuke [3 ]
Uchida, Junya [1 ]
Takemura, Toshihiko [5 ]
Ohara, Toshimasa [3 ]
Oura, Yasuji [6 ]
Ebihara, Mitsuru [6 ]
Satoh, Masaki [1 ]
机构
[1] Univ Tokyo, Atmosphere & Ocean Res Inst AORI, 5-1-5 Kashiwanoha, Kashiwa, Chiba 2778568, Japan
[2] Japan Aerosp Explorat Agcy JAXA, Earth Observat Res Ctr EORC, 2-1-1 Sengen, Tsukuba, Ibaraki 3058505, Japan
[3] Natl Inst Environm Studies NIES, 16-2 Onogawa, Tsukuba, Ibaraki 3058506, Japan
[4] Remote Sensing Technol Ctr Japan, Minato Ku, 3-17-1 Toranomon, Tokyo 1050001, Japan
[5] Kyushu Univ, Res Inst Appl Mech, Kasuga Pk 6-1, Fukuoka 8168580, Japan
[6] Tokyo Metropolitan Univ, Grad Sch Sci & Engn, 1-1 Minami Osawa, Hachioji, Tokyo 1920397, Japan
关键词
Fukushima Nuclear Power Station accident; Aerosols; Radioactive materials; Cs-137; Chemical transport modeling; Ensemble models; SOURCE-TERM; AEROSOL; RADIONUCLIDES; DEPOSITION; DISPERSION; SIMULATIONS; TRANSPORT; PARTICLES; SULFATE;
D O I
10.1186/s40645-017-0117-x
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
In this study, a new method is proposed for the depiction of the atmospheric transportation of the Cs-137 emitted from the Fukushima Daiichi Nuclear Power Station accident. This method employs a combination of the results of two aerosol model ensembles and the hourly observed atmospheric Cs-137 concentration at surface level during 14-23 March 2011 at 90 sites in the suspended particulate matter monitoring network. The new method elucidates accurate transport routes and the distribution of the surface-level atmospheric Cs-137 relevant to eight plume events that were previously identified. The model ensemble simulates the main features of the observed distribution of surface-level atmospheric Cs-137. However, significant differences were found in some cases, and this suggests the need to improve the modeling of the emission scenario, plume height, wet deposition process, and plume propagation in the Abukuma Mountain region. The contributions of these error sources differ in the early and dissipating phases of each event, depending on the meteorological conditions.
引用
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页数:18
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