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

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

For the 10-day simulations, apportionment estimates for all but the northeast Texas<br />

source region are within the standard error of the REMSAD results. Simulations with shorter<br />

trajectories reproduced the REMSAD apportionments in fewer source regions.<br />

In the lower part of Table 9-10, it is interesting to note that the attribution to all of<br />

Texas is overestimated by about the same amount that the attribution to the western U.S. is<br />

underestimated, while the attributions for the eastern U.S. and Mexico source regions<br />

properly reproduce the REMSAD result (i.e., they’re within one standard error). The cause<br />

for the Texas estimating error was explored, and it was found that the FMBR technique has a<br />

tendency to increase the attributions to closer source regions at the expense of more distant<br />

source regions. Also, when included, boundary condition contributions tend to be incorrectly<br />

attributed to the closer source regions. When these potential biases are taken into account,<br />

the FMBR method can be a useful method for regional source apportionment.<br />

9.8 Evaluation of REMSAD Simulations of Perfluorocarbon Tracers<br />

We now turn to assessing the performance of the regional air quality models used for<br />

source attribution in the <strong>BRAVO</strong> <strong>Study</strong>. These models were evaluated against the<br />

perfluorocarbon concentrations measured during the tracer study and against ambient sulfur<br />

measurements at Big Bend and throughout Texas. The tracer evaluations assessed the<br />

performance of the regional modeling system (i.e., the air quality model and the<br />

meteorological field) when simulating transport and diffusion. Since the perfluorocarbon<br />

tracers are inert gases, the tracer evaluations did not assess the ability of the modeling system<br />

to simulate chemical transformation or deposition.<br />

This section describes the evaluation of the REMSAD system against the<br />

perfluorocarbon measurements. A similar evaluation for the CMAQ system is described in<br />

Section 9.10. Evaluations of the REMSAD and CMAQ-MADRID modeling systems against<br />

ambient sulfur measurements, which also test the chemical transformation capabilities of the<br />

models, will be presented in Sections 9.9 and 9.11, respectively.<br />

In order to evaluate its performance at simulating the transport and diffusion of inert<br />

emissions, the REMSAD regional air quality model was used to simulate the four<br />

perfluorocarbon tracers that were released during the <strong>BRAVO</strong> study (as described in Section<br />

3.2. The configuration of REMSAD for the tracer simulation was similar to that used for the<br />

base emissions simulation described in Section 11.1, except that 1) the chemistry mechanism<br />

was not invoked, since the tracer did not undergo chemical transformation, 2) loss via<br />

depositional settling was not considered, since it was assumed that the tracers have very low<br />

deposition velocities, and 3) background concentrations were set to zero. The grid scale of<br />

the model was 36 km. Horizontal winds, temperature, and other meteorological fields were<br />

simulated by MM5. Details of the evaluation are provided in the CIRA/NPS report<br />

(Schichtel et al., 2004), which is included in the Appendix.<br />

Each of the four tracer releases was treated as a point source emission. Two of the<br />

tracers were released in the stacks of power plants, the northeast Texas tracer (PPCH) at the<br />

Big Brown power plant and the Houston tracer (PTCH) at the Parish power plant, and thus<br />

were lofted higher into the boundary layer due to buoyant and momentum plume rise.<br />

9-34

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