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Documentation of the Evaluation of CALPUFF and Other Long ...

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ETEX LRT Dispersion Model Sensitivity Tests<br />

Sensitivity tests were conducted using <strong>the</strong> CAMx, <strong>CALPUFF</strong> <strong>and</strong> HYSPLIT models <strong>and</strong> <strong>the</strong> ETEX<br />

field study data.<br />

For CAMx, <strong>the</strong> effects <strong>of</strong> alternative vertical mixing coefficients (OB70, TKE, ACM2 <strong>and</strong> CMAQ),<br />

horizontal advection solvers (PPM <strong>and</strong> Bott) <strong>and</strong> use <strong>of</strong> <strong>the</strong> subgrid‐scale Plume‐in‐Grid (PiG)<br />

module were evaluated. The key findings from <strong>the</strong> CAMx ETEX sensitivity tests were as follows:<br />

• The vertical mixing parameter had <strong>the</strong> biggest effect on model performance, with <strong>the</strong><br />

CMAQ vertical diffusion coefficients producing <strong>the</strong> best performing CAMx simulations.<br />

• The horizontal advection solver had a much smaller effect on CAMx model performance<br />

with <strong>the</strong> PPM algorithm performing slightly better than Bott.<br />

• The use <strong>of</strong> no PiG module produced slightly better performance than use <strong>of</strong> <strong>the</strong> PiG<br />

module.<br />

• The default CAMx configuration used in <strong>the</strong> ETEX evaluation (CMAQ/PPM/No PiG) was <strong>the</strong><br />

best performing CAMx sensitivity test.<br />

<strong>CALPUFF</strong> sensitivity tests were performed to examine <strong>the</strong> effects <strong>of</strong> puff splitting on <strong>the</strong><br />

<strong>CALPUFF</strong> model performance for <strong>the</strong> ETEX field experiment. When EPA listed <strong>CALPUFF</strong> as <strong>the</strong><br />

EPA‐recommended LRT dispersion model in 2003, <strong>the</strong>y noted that <strong>the</strong> implementation <strong>of</strong> puff<br />

splitting likely will extend <strong>the</strong> models applicability beyond 300 km downwind (EPA, 2003). Since<br />

many <strong>of</strong> <strong>the</strong> ETEX monitoring sites are sited fur<strong>the</strong>r than 300 km downwind from <strong>the</strong> release,<br />

one potential explanation for <strong>the</strong> poor <strong>CALPUFF</strong> model performance is that it is being applied<br />

far<strong>the</strong>r downwind than <strong>the</strong> model is applicable for. Figure ES‐9 displays a time series <strong>of</strong> <strong>the</strong><br />

Figure <strong>of</strong> Merit in Space (FMS) performance statistic for <strong>the</strong> five LRT dispersion models.<br />

Although <strong>CALPUFF</strong> performs reasonably well within <strong>the</strong> first 12 hours <strong>of</strong> <strong>the</strong> tracer release, its<br />

performance quickly degrades even within 300 km <strong>of</strong> <strong>the</strong> source. Thus, <strong>CALPUFF</strong>’s poor model<br />

performance is not due to applying <strong>the</strong> model to downwind distances beyond its applicability.<br />

Eight <strong>CALPUFF</strong> puff splitting sensitivity tests were conducted ranging from no puff splitting to<br />

aggressive puff splitting for all hours <strong>of</strong> <strong>the</strong> day <strong>and</strong> relaxing some <strong>of</strong> <strong>the</strong> puff splitting initiation<br />

criteria so that even more puff splitting can occur. The <strong>CALPUFF</strong> ETEX model performance using<br />

no puff splitting <strong>and</strong> all hour puff splitting was very similar, thus we saw no evidence to support<br />

EPA’s 2003 statements that puff splitting may extend <strong>the</strong> downwind applicability <strong>of</strong> <strong>the</strong> model.<br />

In fact, when some <strong>of</strong> <strong>the</strong> puff splitting initiation criteria were relaxed to allow more puff<br />

splitting, <strong>the</strong> CALUFF performance degraded.<br />

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