CRC Report No. A-34 - Coordinating Research Council
CRC Report No. A-34 - Coordinating Research Council
CRC Report No. A-34 - Coordinating Research Council
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April 2005<br />
Meteorological input data for CAMx were developed using the Penn State/NCAR Mesoscale<br />
Model, version 5 (MM5). The MM5 is a non-hydrostatic, prognostic meteorological model that<br />
simulates atmospheric properties based on fundamental equations, but also permits assimilation<br />
of observed data to nudge the simulated meteorological fields toward the data (Dudhia, 1993).<br />
MM5 was run with assimilation of SCOS measurement data assembled by the CARB (i.e., radar<br />
wind profiler upper-air data and surface site data) and Eta Data Analysis System data from the<br />
National Centers for Environmental Prediction (NOAA-ARL, 2002). The CAMx modeling grid<br />
was closely matched to the MM5 grid and, in particular, CAMx layer interfaces exactly matched<br />
MM5 layer interfaces to facilitate direct mapping of meteorological parameters from MM5 to<br />
CAMx.<br />
UTM <strong>No</strong>rthing (km)<br />
3850<br />
3800<br />
3750<br />
3700<br />
Pacific<br />
Ocean<br />
Kern County<br />
Los Angeles County<br />
Ventura<br />
Crestline<br />
County<br />
Van Nuys<br />
Diamond Bar<br />
LAX<br />
Hawthorn<br />
Lake Perris<br />
Long Beach<br />
Anaheim<br />
Orange<br />
County<br />
300 350 400 450 500 550 600<br />
UTM Easting (km)<br />
San Bernardino County<br />
Riverside County<br />
San Diego County<br />
2600 m<br />
2400 m<br />
2200 m<br />
2000 m<br />
1800 m<br />
1600 m<br />
1400 m<br />
1200 m<br />
1000 m<br />
800 m<br />
600 m<br />
400 m<br />
200 m<br />
0 m<br />
-200 m<br />
Figure 2-1. CAMx photochemical modeling domain showing terrain height (m) and receptor<br />
locations for the CMB analysis.<br />
Selection of a Photochemical Mechanism for the Host Model<br />
The photochemical mechanism for the host model is important because it provides the oxidant<br />
fields to chemically decay the PAMS species reactive tracers. CAMx supports both the CB4<br />
(Gery et al., 1989) and SAPRC99 (Carter, 2000) chemical mechanisms. Emission inventories<br />
for the August 1997 SCOS episode are available for both the CB4 and SAPRC99 chemistry.<br />
The CB4 chemical mechanism was selected because, together with the other model inputs, it<br />
better replicates the observed ozone levels for the August SCOS episode than the SAPRC99<br />
mechanism (Yarwood et al., 2003b).<br />
Reactive Tracers (RTRAC) for PAMS Species and Source Categories<br />
Atmospheric concentrations of specific PAMS species from specific source categories were<br />
modeled using a reactive tracer methodology (RTRAC) included in CAMx (ENVIRON, 2004).<br />
This methodology was developed and tested for modeling air toxics species in Los Angeles for<br />
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