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Model Intercomparison of Atmospheric 137 Cs From the Fukushima Daiichi Nuclear Power Plant Accident: Simulations Based on Identical Input Data
Author(s) -
Sato Yousuke,
Takigawa Masayuki,
Sekiyama Tsuyoshi Thomas,
Kajino Mizuo,
Terada Hiroaki,
Nagai Haruyasu,
Kondo Hiroaki,
Uchida Junya,
Goto Daisuke,
Quélo Denis,
Mathieu Anne,
Quérel Arnaud,
Fang Sheng,
Morino Yu,
Schoenberg Pontus,
Grahn Håkan,
Brännström Niklas,
Hirao Shigekazu,
Tsuruta Haruo,
Yamazawa Hiromi,
Nakajima Teruyuki
Publication year - 2018
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
eISSN - 2169-8996
pISSN - 2169-897X
DOI - 10.1029/2018jd029144
Subject(s) - environmental science , atmospheric dispersion modeling , deposition (geology) , atmospheric sciences , meteorology , air pollution , physics , chemistry , geology , paleontology , organic chemistry , sediment
A model intercomparison of the atmospheric dispersion of cesium‐137 ( 137 Cs) emitted after the Fukushima Daiichi Nuclear Power Plant accident in Japan was conducted to understand the behavior of atmospheric 137 Cs in greater detail. The same meteorological data with a fine spatiotemporal resolution and an emission inventory were applied to all models to exclude the differences among the models originating from differences in meteorological and emission data. The meteorological data were used for initial, boundary, and nudging data or offline meteorological field. Furthermore, a horizontal grid with the same resolution as that of the meteorological data was adopted for all models. This setup enabled us to focus on model variability originating from the processes included in each model, for example, physical processes. The multimodel ensemble captured 40% of the atmospheric 137 Cs events observed by measurements, and the figure of merit in space for the total deposition of 137 Cs exceeded 80. The lower score of the atmospheric 137 Cs than that of the deposition originated from the difference in timing between observed and simulated atmospheric 137 Cs. Our analyses indicated that meteorological data were most critical for reproducing the atmospheric 137 Cs events. The results further revealed that differences in 137 Cs concentrations among the models originated from deposition and diffusion processes when the meteorological field was simulated reasonably well. The models with small deposition fluxes produced higher scores for atmospheric 137 Cs, and those with strong diffusion succeeded in capturing the high 137 Cs concentrations observed; however, they also tended to overestimate the concentrations.