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CALPUFF and Postprocessors

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F.7 Boundary Concentration Module File (BCON.DAT)<br />

The impact of significant regional pollution transport on concentrations <strong>and</strong> deposition fluxes computed<br />

within the modeling domain can be included in a <strong>CALPUFF</strong> analysis either by adding a spatially uniform<br />

(<strong>and</strong> either constant in time or varying by hour) field at the post-processing step with CALPOST, or by<br />

selecting the boundary concentration (BCON) module within <strong>CALPUFF</strong>. The latter choice is preferable<br />

if there are known spatial gradients in regional concentrations outside the modeling domain, or if<br />

chemical transformation <strong>and</strong> removal processes associated with the regional pollution must be explicitly<br />

modeled.<br />

Regional air-mass characteristics are defined <strong>and</strong> assigned to segments along each boundary of the<br />

computational domain when the boundary concentration module is used. A segment is equivalent to the<br />

length of one side of a grid cell. The number of air-mass types can be equal to the number of cells along<br />

the perimeter of the domain if sufficient information exists on this scale, or the number can be far fewer in<br />

typical applications where an entire side of the domain is characterized by a single air-mass. Air-mass<br />

characteristics include the concentration of each species advected into the domain <strong>and</strong> the thickness of the<br />

layer that contains these species. These concentrations are used to initialize puffs that are well-mixed in<br />

the vertical <strong>and</strong> the horizontal. The vertical depth of a puff is the thickness of the layer assigned to the<br />

air-mass, <strong>and</strong> the radius of the puff is related to the length of the segment <strong>and</strong> the component of the<br />

transport wind that is perpendicular to the segment (the mass flux into the domain <strong>and</strong> the initial<br />

concentration are conserved). The concentration of each species for each air-mass type may be scaled by<br />

factors that vary in one of the following ways: by hour of the day (24 factors); by month (12 factors); by<br />

hour <strong>and</strong> season (96 factors); by wind speed <strong>and</strong> stability class (36 factors); or by temperature (12<br />

factors). These are the same factors provided for sources specified in the <strong>CALPUFF</strong> control file. If more<br />

detailed variation is needed for one or more air-mass types, air-mass characteristics for these can be<br />

provided hourly. When this method is used, the layer thickness may change as well as the concentrations.<br />

Otherwise, the layer thickness is constant for each air-mass type.<br />

The configuration of the boundary properties is provided to <strong>CALPUFF</strong> in a "BCON.DAT" file. Two<br />

formats are available for this file. The first is a formatted file prepared specifically for use with the<br />

BCON option (MBCON = 1). It is constructed using the <strong>CALPUFF</strong> control file conventions. A sample<br />

file is shown in Table F-32, <strong>and</strong> a description of the input parameters is provided in Table F-33. The<br />

second (MBCON = 2) is a st<strong>and</strong>ard <strong>CALPUFF</strong> unformatted “CONC.DAT” output concentration file.<br />

Receptors in this file must lie along the boundary of the modeling region, providing near-surface<br />

concentrations for the air mass transported across the boundary into the modeling domain. This format<br />

may be chosen if <strong>CALPUFF</strong> results from a larger domain are available.<br />

Input Group 1 in the BCON.DAT file identifies the grid information for the computational domain, the<br />

units for the concentrations that are provided, the number of air-mass types, <strong>and</strong> the type of temporal<br />

variation used in describing air-mass properties. Four air-mass types are used in this example. Three of<br />

these use the temporal variation factors provided in Input Group 3 <strong>and</strong> one uses an explicit sequence of<br />

MAR 2006 – <strong>CALPUFF</strong><br />

F-164

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