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Dispersion ofFukushimaradionuclidesintheglobalatmosphere
Applied Radiation and Isotopes 81 (2013) 383–392Contents lists available at ScienceDirectApplied Radiation and Isotopes0969-80 http://d n Corr E-mjournal homepage: /locate/apradisoDispersion of Fukushima radionuclides in the global atmosphere and the ocean P.P. Povinec a,n, M. Gera b, K. Holy a, K. Hirose c,g, G. Lujaniené d, M. Nakano e, W. Plastino f, I. Sykora a, J. Bartok h, M. Ga?ák h a Department of Nuclear Physics and Biophysics, Faculty of Mathematics, Physics and Informatics, Comenius University, 84248 Bratislava, Slovakia b Department of Astronomy, Physics of the Earth and Meteorology, Faculty of Mathematics, Physics and Informatics, Comenius University, 84248 Bratislava, Slovakia c Department of Materials and Life Sciences, Sophia University, Tokyo, Japan d Environmental Research Department, SRI Center for Physical Sciences and Technology, Vilnius, Lithuania e Japan Atomic Energy Agency, 4-33 Muramatsu, Tokai-mura, Naka-gun, Ibaraki 319-1194, Japan f Department of Mathematics and Physics, University of Roma Tre, and INFN, Section of Roma Tre, Via della Vasca Navale 84, I-00146 Roma, Italy g Geosphere Research Institute, Saitama University, Saitama, Japan h MicroStep-MIS, 84104 Bratislava, SlovakiaG R A P H I C A L A B S T R A C TH I G H L I G H T S Modeling of Fukushima radionuclides in the atmosphere. Modeling of Fukushima radionuclides in the Pacific. Comparison of the Fukushima radionuclide impact with global fallout. Comparison of Fukushima and Chernobyl radionuclide releases.a r t i c l e i n f o a b s t r a c tAvailable online 9 April 2013 Keywords: Fukushima accident Radionuclide source terms Atmospheric radioactivity Marine radioactivity Lagrangian atmospheric modeling Ocean global circulation model43/$ - see front matter 2013 Elsevier Ltd. A /10.1016/j.apradiso.2013.03.058 esponding author. Tel.: +421 260295544; fax: ail address: povinec@fmph.uniba.sk (P.P. PovinLarge quantities of radionuclides were released in March–April 2011 during th
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