Minimum turbulence assumptions and u* and L estimation for dispersion models during low-wind stable conditions.
The U.S. Environmental Protection Agency (EPA) short-distance dispersion model, AERMOD, has been shown to overpredict by a factor of as much as 10 when compared with observed concentrations from continuous releases at the Oak Ridge, TN (OR), and Idaho Falls, ID (IF), field experiments during stable periods when wind speeds often dropped below 1 m/sec. Some of this overprediction tendency can be reduced by revising AERMOD's meteorological preprocessor's parameterizations of the friction velocity, u*, during low-wind stable conditions, thus increasing the calculated sigma(v) and sigma(w) and hence the lateral and vertical dispersion rates. Observations show that as the mean wind speed approaches zero at night, there is always significant sigma(v) and sigma(w) over time periods of 15 to 60 min, while standard Monin-Obukhov Similarity Theory (MOST) predicts that sigma(v) and sigma(w) will approach zero. This paper focuses on the u* estimation methods and the minimum turbulence (sigma(v) and sigma(w)) assumptions in AERMOD (beta option 4) and two widely used U.S. operational dispersion models, AERMOD (v12345) and SCICHEM. The U.S. EPA has provided results of its tests with the OR and IF data, with its base AERMOD version and its December 2012 modified versions, which assume adjustments to the low-wind u* and increases in the minimum sigma(v) parameterization. SCICHEM has relatively small mean bias for both data sets. The revised AERMOD shows much less mean bias, agreeing more with SCICHEM.


CONCLUSIONS
Suggestions are made for improvements to dispersion models such as AERMOD to correct overpredictions during light-wind stable conditions. Methods for estimating u*, L, and the minimum turbulence parameters (sigma(v) and sigma(w)) are reviewed and compared. SCICHEM and the current operational version and an optional beta version (December 2012) of AERMOD are evaluated with tracer data from low-wind stable field experiments in Idaho Falls and Oak Ridge. It is seen that the operational version of AERMOD overpredicts by a factor of 2 to 10, while the optional beta version of AERMOD and SCICHEM have much less bias.
Steven R
SR
Hanna
Biswanath
B
Chowdhury
D000397:Air Pollution; D008962:Models, Theoretical; D014919:Wind