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Table of Contents - The Atmospheric Studies Group at TRC

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Section 9: CALPUFF<br />

available temper<strong>at</strong>ure gradient d<strong>at</strong>a are used to estim<strong>at</strong>e the inversion strength.<br />

Precipit<strong>at</strong>ion d<strong>at</strong>a, solar radi<strong>at</strong>ion, and rel<strong>at</strong>ive humidity are not required in CTDMPLUS. <strong>The</strong>y may be<br />

added to SURFACE.DAT in an extended d<strong>at</strong>a record. <strong>The</strong>se fields may remain blank if they are not<br />

needed for the CALPUFF options selected. Precipit<strong>at</strong>ion is needed for wet deposition modeling, and the<br />

solar radi<strong>at</strong>ion and humidity d<strong>at</strong>a are needed for chemical transform<strong>at</strong>ion calcul<strong>at</strong>ions.<br />

Other d<strong>at</strong>a associ<strong>at</strong>ed with the SURFACE.DAT and PROFILE.DAT are provided in the CALPUFF.INP<br />

control file. <strong>The</strong>se d<strong>at</strong>a include the land use type, elev<strong>at</strong>ion, and leaf area index <strong>of</strong> the modeling region,<br />

and two control variables (ISIGMAV and IMIXCTDM). <strong>The</strong> land use c<strong>at</strong>egory is used to determine if<br />

urban or rural dispersion coefficients are appropri<strong>at</strong>e when the Pasquill-Gifford/McElroy-Pooler<br />

dispersion coefficients are used during convective regimes. Also see the variables IURB1 and IURB2 in<br />

Input <strong>Group</strong> 12 <strong>of</strong> the control file. <strong>The</strong>y define the range <strong>of</strong> land use c<strong>at</strong>egories th<strong>at</strong> are to be considered<br />

urban (i.e., if the value <strong>of</strong> the land use c<strong>at</strong>egory is between IURB1 and IURB2, inclusive, the modeling<br />

domain will be consider urban). Otherwise, it will be considered rural. <strong>The</strong> leaf area index is only used<br />

by the model if dry deposition velocities are being computed. <strong>The</strong> elev<strong>at</strong>ion is used to fill the 2-D terrain<br />

elev<strong>at</strong>ion array in CALPUFF th<strong>at</strong> is normally filled from the CALMET file. This array is used to<br />

determine, through interpol<strong>at</strong>ion, the elev<strong>at</strong>ion <strong>of</strong> the gridded receptors gener<strong>at</strong>ed by the model as an<br />

option. Because a single value is available here, all <strong>of</strong> the gridded receptors will be assigned this<br />

elev<strong>at</strong>ion. Receptor-specific elev<strong>at</strong>ions are assigned to each discrete receptor by the user in the<br />

CALPUFF control file (see Input <strong>Group</strong> 17). ISIGMAV indic<strong>at</strong>es the form <strong>of</strong> the l<strong>at</strong>eral turbulence d<strong>at</strong>a,<br />

and IMIXCTDM indic<strong>at</strong>es which mixing height field (observed or calcul<strong>at</strong>ed) is to be used.<br />

Sample SURFACE.DAT files are shown in <strong>Table</strong>s 9-12(a-c). Part (a) <strong>of</strong> the table shows the standard<br />

SURFACE.DAT d<strong>at</strong>a record. <strong>The</strong> extended d<strong>at</strong>a record is shown in Part (b) <strong>of</strong> the table, and the form <strong>of</strong><br />

the extended record d<strong>at</strong>a with sub-hourly time steps is shown in Part (c). Similarly, sample<br />

PROFILE.DAT files are shown in <strong>Table</strong> 9-13. D<strong>at</strong>a records for SURFACE.DAT are described in <strong>Table</strong><br />

9-14, and d<strong>at</strong>a records for PROFILE.DAT are described in <strong>Table</strong> 9-15. Note th<strong>at</strong> the year may be<br />

specified in either a YY (e.g., 94) or YYYY (e.g., 1994) form<strong>at</strong>. <strong>The</strong> YY form<strong>at</strong> is the original CTDM<br />

PLUS form<strong>at</strong>.<br />

<strong>The</strong> PROFILE.DAT file may also be used in conjunction with the other meteorological d<strong>at</strong>a options in<br />

CALPUFF to provide measured turbulence d<strong>at</strong>a, or to provide the strength <strong>of</strong> the temper<strong>at</strong>ure inversion.<br />

When turbulence d<strong>at</strong>a are supplied, wind speeds should be provided in the file as well as the turbulence,<br />

so th<strong>at</strong> conversions between v and can be made.<br />

9-152

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