TY - JOUR
T1 - Inverse modeling of the 137Cs source term of the Fukushima Dai-ichi Nuclear Power Plant accident constrained by a deposition map monitored by aircraft
AU - Yumimoto, Keiya
AU - Morino, Yu
AU - Ohara, Toshimasa
AU - Oura, Yasuji
AU - Ebihara, Mitsuru
AU - Tsuruta, Haruo
AU - Nakajima, Teruyuki
N1 - Funding Information:
We gratefully acknowledge K. Katsumata and M. Ishimoto of The University of Tokyo for supporting the measurements of atmospheric 137 Cs concentration retrieved from atmospheric aerosols collected on a filter tape of suspended particulate matter (SPM) monitoring system. We thank T. Maki and M. Kajino for useful discussions about this study. This work was partly supported by the Japan Society for the Promotion of Science (JSPS KAKENHI Grant Number 25220101 , 26701004 and 15K05296 ), the Ministry of Education, Science, Sport, and Culture (MEXT KAKENHI Grant Number 24110002 ), and the Global Environment Research Fund (No. S-12) of the Ministry of Environment, Japan .
Publisher Copyright:
© 2016 Elsevier Ltd
PY - 2016/11/1
Y1 - 2016/11/1
N2 - The amount of 137Cs released by the Fukushima Dai-ichi Nuclear Power Plant accident of 11 March 2011 was inversely estimated by integrating an atmospheric dispersion model, an a priori source term, and map of deposition recorded by aircraft. An a posteriori source term refined finer (hourly) variations comparing with the a priori term, and estimated 137Cs released 11 March to 2 April to be 8.12 PBq. Although time series of the a posteriori source term was generally similar to those of the a priori source term, notable modifications were found in the periods when the a posteriori source term was well-constrained by the observations. Spatial pattern of 137Cs deposition with the a posteriori source term showed better agreement with the 137Cs deposition monitored by aircraft. The a posteriori source term increased 137Cs deposition in the Naka-dori region (the central part of Fukushima Prefecture) by 32.9%, and considerably improved the underestimated a priori 137Cs deposition. Observed values of deposition measured at 16 stations and surface atmospheric concentrations collected on a filter tape of suspended particulate matter were used for validation of the a posteriori results. A great improvement was found in surface atmospheric concentration on 15 March; the a posteriori source term reduced root mean square error, normalized mean error, and normalized mean bias by 13.4, 22.3, and 92.0% for the hourly values, respectively. However, limited improvements were observed in some periods and areas due to the difficulty in simulating accurate wind fields and the lack of the observational constraints.
AB - The amount of 137Cs released by the Fukushima Dai-ichi Nuclear Power Plant accident of 11 March 2011 was inversely estimated by integrating an atmospheric dispersion model, an a priori source term, and map of deposition recorded by aircraft. An a posteriori source term refined finer (hourly) variations comparing with the a priori term, and estimated 137Cs released 11 March to 2 April to be 8.12 PBq. Although time series of the a posteriori source term was generally similar to those of the a priori source term, notable modifications were found in the periods when the a posteriori source term was well-constrained by the observations. Spatial pattern of 137Cs deposition with the a posteriori source term showed better agreement with the 137Cs deposition monitored by aircraft. The a posteriori source term increased 137Cs deposition in the Naka-dori region (the central part of Fukushima Prefecture) by 32.9%, and considerably improved the underestimated a priori 137Cs deposition. Observed values of deposition measured at 16 stations and surface atmospheric concentrations collected on a filter tape of suspended particulate matter were used for validation of the a posteriori results. A great improvement was found in surface atmospheric concentration on 15 March; the a posteriori source term reduced root mean square error, normalized mean error, and normalized mean bias by 13.4, 22.3, and 92.0% for the hourly values, respectively. However, limited improvements were observed in some periods and areas due to the difficulty in simulating accurate wind fields and the lack of the observational constraints.
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U2 - 10.1016/j.jenvrad.2016.06.018
DO - 10.1016/j.jenvrad.2016.06.018
M3 - Article
C2 - 27372443
AN - SCOPUS:84976892495
SN - 0265-931X
VL - 164
SP - 1
EP - 12
JO - Journal of Environmental Radioactivity
JF - Journal of Environmental Radioactivity
ER -