The Monin-Obukhov length values (
L) corresponding to dispersion coefficients on Pasquill/Gifford chart (P/G chart), which are widely used for esimating air pollution concentration, are derived in order to use the equations of atmospheric boundary layer for the research on the atomospheric diffusion.
The classified table for atmospheric stability categories corresponding to P/G chart were proposed by Nuclear Safety Research Association originaly in 1973, revised in 1981 and used by Environmental Agency, Nuclear Safety Commission and so on in Japan. The classified table constructed by the categories of surface wind speed and insolation in daytime or net radiation in nighttime is converted to the table of
Lcorresponding to boundary of atmospheric stability categories assuming mean values of albedo (25%) and Bowen ratio (0.4 in daytime, latent heat flux is 0 in nighttime.) on the grass plane in the middle latitude. The roughness length (
z0) was assumed to be 3cm because the atmospheric diffusion experiments corresponding to P/G chart were done in the field of
z0 of about 3 cm. The values of
L derived in this research are compared with one of Golder (1972)'s chart, which were made by the observations of atmospheric stability categories on Pasquill's or Turner's methods and Ls in the several field experiments in abroad. Both values of
L coincide comparatively well.
Therefore, the atmospheric stability categories of the method of Nuclear Safety Research Association of Japan, which are corresponding to the dispersion coefficients on P/G chart, are practically corresponding to Golder's Ls in the case of z
0 of about 3 cm.
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