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CALPUFF and Postprocessors

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F.2.3<br />

PLMMET.DAT<br />

In addition to the capability to use three-dimensional wind fields generated by CALMET, a single-station<br />

meteorological file can also be used by <strong>CALPUFF</strong> as its source of meteorological data. One form of<br />

single station data accepted by <strong>CALPUFF</strong> is the AUSPLUME (Lorimer, 1976) type of data file. The<br />

st<strong>and</strong>ard AUSPLUME data file can be used without modification, although some <strong>CALPUFF</strong> options<br />

require additional meteorological variables that must be added as part of an extended data record.<br />

<strong>CALPUFF</strong> is normally run with a full three-dimensional wind field <strong>and</strong> temperature field, as well as twodimensional<br />

fields of mixing heights <strong>and</strong> other meteorological variables (see CALMET.DAT in Section<br />

F.2.1). However, in some near-field applications, when spatial variability of the meteorological fields<br />

may not be significant (e.g., uniform terrain <strong>and</strong> l<strong>and</strong> use), the single-station data file may be used. In<br />

single station mode, <strong>CALPUFF</strong> assigns the single value of each variable read from the PLMMET.DAT<br />

file to all grid points, resulting in a spatially uniform gridded field. However, the model does not assume<br />

the meteorological conditions are steady-state, which allows the important effects of causality to be<br />

simulated even with the single-station meteorological data. For example, the time required for plume<br />

material to reach a receptor is accounted for in the puff formulation, <strong>and</strong> curved trajectories <strong>and</strong> variable<br />

dispersion <strong>and</strong> stability conditions over multiple hours of transport will result even when using the singlestation<br />

meteorological data. However, in general, the preferred mode for most applications of <strong>CALPUFF</strong><br />

is to use the spatially variable fields generated by CALMET.<br />

The PLMMET.DAT file includes the basic hourly data required by <strong>CALPUFF</strong>, including the wind<br />

direction, wind speed, temperature, stability class, <strong>and</strong> mixing height. Note that PLMMET.DAT uses<br />

wind direction in the usual meteorological convention (i.e., winds from the west blowing toward the east<br />

has a value of 270E), while ISCMET.DAT uses flow vector (i.e., winds from the west toward the east<br />

have a vector direction of 90E). The PLMMET.DAT format also contains data for the horizontal<br />

component of turbulence (F 2 ). If both components of turbulence are available, they should be entered<br />

through the use of the PROFILE.DAT data file (see Section F.2.4). Also, <strong>CALPUFF</strong> contains several<br />

options for modeling chemical transformation that do not involve the use of a decay constant.<br />

The PLMMET.DAT format does not contain micrometeorological variables (the surface friction velocity<br />

<strong>and</strong> Monin-Obukhov length), precipitation data, solar radiation, or relative humidity. The Monin-<br />

Obukhov length is inferred from the stability class <strong>and</strong> the surface roughness length using the Golder<br />

(1972) relations. The friction velocity can then be estimated from the surface-layer similarity wind<br />

profile equation. The remaining variables must be added to the st<strong>and</strong>ard file in an exended data record.<br />

These fields may remain blank if they are not needed for the <strong>CALPUFF</strong> options selected. Precipitation is<br />

needed for wet deposition modeling, <strong>and</strong> the solar radiation <strong>and</strong> humidity data are needed for chemical<br />

transformation calculations.<br />

Sample PLMMET.DAT files are shown in Tables F-9(a) <strong>and</strong> F-9(b). Part (a) of the table shows the<br />

st<strong>and</strong>ard AUSPLUME meteorological data record. The extended data record is shown in Part (b) of the<br />

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

F-106

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