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

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Figure 4‐1. <strong>CALPUFF</strong>/CALMET UTM modeling domain <strong>and</strong> location <strong>of</strong> tracer release site <strong>and</strong><br />

<strong>CALPUFF</strong> receptors along am arc 100 km from <strong>the</strong> source for <strong>the</strong> SRL75 <strong>CALPUFF</strong> modeling.<br />

In <strong>the</strong> <strong>CALPUFF</strong> modeling system, each <strong>of</strong> <strong>the</strong> three programs (CALMET, <strong>CALPUFF</strong>, <strong>and</strong><br />

CALPOST) uses a control file <strong>of</strong> user‐selectable options to control <strong>the</strong> data processing. There<br />

are numerous options in each <strong>and</strong> several that can result in significant differences. The<br />

following model controls for CALMET <strong>and</strong> <strong>CALPUFF</strong> were employed for <strong>the</strong> analyses with <strong>the</strong><br />

SRL75 tracer data.<br />

4.2.1 CALMET Options<br />

The following CALMET control parameters <strong>and</strong> options were chosen for <strong>the</strong> BASE case model<br />

evaluation. The BASE case control parameters <strong>and</strong> options were chosen to be consistent with<br />

two previous CALMET/<strong>CALPUFF</strong> evaluations (Irwin 1997 <strong>and</strong> EPA 1998a). The most important<br />

CALMET options relate to <strong>the</strong> development <strong>of</strong> <strong>the</strong> wind field <strong>and</strong> were set as follows:<br />

NOOBS = 0 Use surface, overwater, <strong>and</strong> upper air station data<br />

IWFCOD = 1 Use diagnostic wind model to develop <strong>the</strong> 3‐D wind fields<br />

IFRADJ = 1 Compute Froude number adjustment effects (<strong>the</strong>rmodynamic<br />

blocking effects <strong>of</strong> terrain)<br />

IKINE = 0 Do NOT compute kinematic effects<br />

IOBR = 0 Do NOT use O’Brien procedure for adjusting vertical velocity<br />

IEXTRP = 4 Use similarity <strong>the</strong>ory to extrapolate surface winds to upper layers<br />

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