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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 />

H:\crca<strong>34</strong>-receptor\report\Final\sec2.doc 2-2

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