Evaluation of the Effect of Horizontal Diffusion on the Long-Range Atmospheric Transport Simulation with Chernobyl DataSource: Journal of Applied Meteorology:;1995:;volume( 034 ):;issue: 007::page 1653Author:Ishikawa, Hirohiko
DOI: 10.1175/1520-0450-34.7.1653Publisher: 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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contributor author | Ishikawa, Hirohiko | |
date accessioned | 2017-06-09T14:09:27Z | |
date available | 2017-06-09T14:09:27Z | |
date copyright | 1995/07/01 | |
date issued | 1995 | |
identifier issn | 0894-8763 | |
identifier other | ams-13471.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4148925 | |
description 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. | |
publisher | American Meteorological Society | |
title | Evaluation of the Effect of Horizontal Diffusion on the Long-Range Atmospheric Transport Simulation with Chernobyl Data | |
type | Journal Paper | |
journal volume | 34 | |
journal issue | 7 | |
journal title | Journal of Applied Meteorology | |
identifier doi | 10.1175/1520-0450-34.7.1653 | |
journal fristpage | 1653 | |
journal lastpage | 1665 | |
tree | Journal of Applied Meteorology:;1995:;volume( 034 ):;issue: 007 | |
contenttype | Fulltext |