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Table of Contents - The Atmospheric Studies Group at TRC

Table of Contents - The Atmospheric Studies Group at TRC

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Section 9: CALPUFF<br />

table. A description <strong>of</strong> the contents <strong>of</strong> the header record is provided in <strong>Table</strong> 9-10, and the d<strong>at</strong>a records<br />

are described in <strong>Table</strong> 9-11. <strong>The</strong> header record contains an 80-character title <strong>of</strong> the d<strong>at</strong>a set.<br />

Note th<strong>at</strong> other d<strong>at</strong>a associ<strong>at</strong>ed with the PLMMET.DAT are provided in the CALPUFF.INP control file.<br />

<strong>The</strong>se d<strong>at</strong>a include the anemometer height, surface roughness length, land use type, elev<strong>at</strong>ion, and leaf<br />

area index <strong>of</strong> the modeling region. <strong>The</strong> anemometer height is required in the vertical power law<br />

extrapol<strong>at</strong>ion <strong>of</strong> the wind speed. <strong>The</strong> roughness length is used to estim<strong>at</strong>e the micrometeorological<br />

variables, the turbulence-based dispersion coefficients (when selected), and in the calcul<strong>at</strong>ion <strong>of</strong> dry<br />

deposition velocities. <strong>The</strong> land use c<strong>at</strong>egory is used to determine if urban or rural dispersion coefficients<br />

are appropri<strong>at</strong>e when the Pasquill-Gifford/McElroy-Pooler dispersion coefficients are used. Also see the<br />

variables IURB1 and IURB2 in Input <strong>Group</strong> 12 <strong>of</strong> the control file. <strong>The</strong>y define the range <strong>of</strong> land use<br />

c<strong>at</strong>egories th<strong>at</strong> are to be considered urban (i.e., if the value <strong>of</strong> the land use c<strong>at</strong>egory in the PLMMET.DAT<br />

file is between IURB1 and IURB2, inclusive, the modeling domain will be consider urban). Otherwise, it<br />

will be considered rural. <strong>The</strong> leaf area index is only used by the model if dry deposition velocities are<br />

being computed. <strong>The</strong> elev<strong>at</strong>ion is used to fill the 2-D terrain elev<strong>at</strong>ion array in CALPUFF th<strong>at</strong> is<br />

normally filled from the CALMET file. This array is used to determine, through interpol<strong>at</strong>ion, the<br />

elev<strong>at</strong>ion <strong>of</strong> the gridded receptors gener<strong>at</strong>ed by the model as an option. Because a single value is<br />

available here, all <strong>of</strong> the gridded receptors will be assigned this elev<strong>at</strong>ion. Receptor-specific elev<strong>at</strong>ions<br />

are assigned to each discrete receptor by the user in the CALPUFF control file (see Input <strong>Group</strong> 17).<br />

9-147

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