The focal point of this study will be on the comparison of surface ozone (O3) variation over the Washington DC metropolitan area. Specifically, the real-time surface measurements from the Howard University Washington DC campus (urban site) vs. the Howard University Beltsville campus (rural site) will be employed to evaluate both AQM v6 and v7 O3 outputs.
The preliminary v6 version of the model showed that the amount of surface O3 was underestimated in the urban area (Washington, DC) while overestimated in the rural area (Beltsville, MD). The over the DC downtown was more pronounced during the nighttime. The daytime prediction appears to align well with observations, especially for O3 peak values. Version 7 of the model corrected the underestimation for our urban site. For the rural site, the overestimation remains during the day and nighttime. It appears that surface wind speed plays a significant role affecting the prediction. Wind speed in the rural area was much slower than the urban area, especially in the nighttime. The momentum flux measured in the Beltsville site decreased as well. It is suspected that the model may not address the vertical mixing in the atmospheric boundary layer properly. Currently we are quantifying the uncertainty through statistical analysis. More comprehensive results will be carried out.

