Journal
ATMOSPHERIC CHEMISTRY AND PHYSICS
Volume 13, Issue 3, Pages 1425-1438Publisher
COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/acp-13-1425-2013
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Funding
- European Research Council under the European Union [226144]
- European Research Council (ERC) [226144] Funding Source: European Research Council (ERC)
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We modeled the global atmospheric dispersion and deposition of radionuclides released from the Fukushima Dai-ichi nuclear power plant accident. The EMAC atmospheric chemistry - general circulation model was used, with circulation dynamics nudged towards ERA-Interim reanalysis data. We applied a resolution of approximately 0.5 degrees in latitude and longitude (T255). The model accounts for emissions and transport of the radioactive isotopes I-131 and Cs-137, and removal processes through precipitation, particle sedimentation and dry deposition. In addition, we simulated the release of Xe-133, a noble gas that can be regarded as a passive transport tracer of contaminated air. The source terms are based on Chino et al. (2011) and Stohl et al. (2012); especially the emission estimates of I-131 are associated with a high degree of uncertainty. The calculated concentrations have been compared to station observations by the Comprehensive Nuclear-Test-Ban Treaty Organisation (CTBTO). We calculated that about 80% of the radioactivity from Fukushima which was released to the atmosphere deposited into the Pacific Ocean. In Japan a large inhabited land area was contaminated by more than 40 kBqm(-2). We also estimated the inhalation and 50-year dose by Cs-137, Cs-134 and I-131 to which the people in Japan are exposed.
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