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(BRAVO) Study: Final Report. - Desert Research Institute

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<strong>Final</strong> <strong>Report</strong> — September 2004<br />

20<br />

18<br />

16<br />

SO 2<br />

y = 0.405x + 2.6087<br />

R 2 = 0.1294<br />

20<br />

18<br />

16<br />

SO 4<br />

=<br />

y = 0.8404x + 0.7158<br />

R 2 = 0.3766<br />

Predicted Predicted SO2 SO2 (µg/m3) (ug/m3)<br />

14<br />

12<br />

10<br />

8<br />

6<br />

4<br />

Predicted Predicted SO4 SO4 (µg/m3) (ug/m3)<br />

14<br />

12<br />

10<br />

8<br />

6<br />

4<br />

2<br />

2<br />

Predicted TES TES (µg/m3) (ug/m3)<br />

0<br />

0 2 4 6 8 10 12 14 16 18 20<br />

20<br />

18<br />

16<br />

14<br />

12<br />

10<br />

8<br />

6<br />

4<br />

2<br />

TS<br />

Observed SO2 (ug/m3)<br />

y = 0.6372x + 1.5321<br />

R 2 = 0.2454<br />

0<br />

0 2 4 6 8 10 12 14 16 18 20<br />

Observed TES (ug/m3)<br />

0<br />

0 2 4 6 8 10 12 14 16 18 20<br />

Observed SO4 (ug/m3)<br />

Figure 9-20. Scatter plots of REMSAD 24-hr sulfur<br />

concentration predictions versus measured values at<br />

37 <strong>BRAVO</strong> network locations over the full <strong>BRAVO</strong><br />

<strong>Study</strong> period.<br />

9.10 Evaluation of CMAQ Simulations of Perfluorocarbon Tracers<br />

The dispersion simulation capability of the CMAQ three-dimensional Eulerian airquality<br />

model was tested by simulating the transport of the inert perfluorocarbon tracers from<br />

specific point sources to receptor sites. For the inert tracer simulation, the chemistry, aerosol,<br />

and dry deposition modules were disabled. Meteorological fields were generated by<br />

processing the MM5 output with MCIP version 2.1 and a four-month simulation was<br />

conducted from July 2 to October 30, 1999. The approach and results are summarized here.<br />

For details see the EPRI report (Pun et al., 2004), which is contained in the Appendix.<br />

For these tracer simulations, CMAQ was configured with the Bott advection scheme<br />

for horizontal and vertical advection, the eddy diffusion scheme for vertical diffusion, and<br />

the non-standard Smagorinsky scheme for horizontal diffusion. This is the same<br />

configuration that was used subsequently for the aerosol attribution modeling, as described in<br />

Section 8.4.4. CMAQ was initially evaluated against the tracer measurements using the<br />

horizontal diffusion scheme that is standard in the model and the alternative Smagorinsky<br />

scheme (which is the scheme used in REMSAD) that produces greater diffusion. Since the<br />

Smagorinsky scheme gave slightly better model performance when compared to the tracer<br />

measurements (Pun et al., 2003), it was selected for use in the subsequent aerosol modeling<br />

9-45

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