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    Evaluation of the Effect of Horizontal Diffusion on the Long-Range Atmospheric Transport Simulation with Chernobyl Data

    Source: Journal of Applied Meteorology:;1995:;volume( 034 ):;issue: 007::page 1653
    Author:
    Ishikawa, Hirohiko
    DOI: 10.1175/1520-0450-34.7.1653
    Publisher: American Meteorological Society
    Abstract: The effect of horizontal diffusion on the long-range transport simulation is examined with a Lagrangian particle transport model. The transport of radioactivity released from Chernobyl is simulated by the model with different values of horizontal diffusivity. The computed concentrations are statistically compared with measured concentration. The best simulation is found when the magnitude of the horizontal diffusivity is between 3.3 ? 104 and 1.0 ? 105 m2 s?1. The performance of empirical formulas of horizontal diffusion, in which mean-square displacement σy is specified as a function of time, is also examined. A part of measured concentrations, which are relatively low concentrations, cannot be explained by transport and diffusion only. It is shown that these measured concentrations can be explained by resuspension of deposited radioactivity.
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      Evaluation of the Effect of Horizontal Diffusion on the Long-Range Atmospheric Transport Simulation with Chernobyl Data

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4148925
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    contributor authorIshikawa, Hirohiko
    date accessioned2017-06-09T14:09:27Z
    date available2017-06-09T14:09:27Z
    date copyright1995/07/01
    date issued1995
    identifier issn0894-8763
    identifier otherams-13471.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4148925
    description abstractThe effect of horizontal diffusion on the long-range transport simulation is examined with a Lagrangian particle transport model. The transport of radioactivity released from Chernobyl is simulated by the model with different values of horizontal diffusivity. The computed concentrations are statistically compared with measured concentration. The best simulation is found when the magnitude of the horizontal diffusivity is between 3.3 ? 104 and 1.0 ? 105 m2 s?1. The performance of empirical formulas of horizontal diffusion, in which mean-square displacement σy is specified as a function of time, is also examined. A part of measured concentrations, which are relatively low concentrations, cannot be explained by transport and diffusion only. It is shown that these measured concentrations can be explained by resuspension of deposited radioactivity.
    publisherAmerican Meteorological Society
    titleEvaluation of the Effect of Horizontal Diffusion on the Long-Range Atmospheric Transport Simulation with Chernobyl Data
    typeJournal Paper
    journal volume34
    journal issue7
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450-34.7.1653
    journal fristpage1653
    journal lastpage1665
    treeJournal of Applied Meteorology:;1995:;volume( 034 ):;issue: 007
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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