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Generic Guidance and Optimum Model Settings for the CALPUFF ...

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Table A-4. Explanation <strong>and</strong> Recommendations <strong>for</strong> <strong>the</strong> List of Key CALUFF <strong>Model</strong> Options<br />

Option<br />

Technical Options - Input Grp 2<br />

Vertical distribution used in <strong>the</strong> near<br />

Parameter Recommended<br />

value<br />

Explanation <strong>and</strong> Justification<br />

field<br />

MGAUSS 1 Always use<br />

Terrain adjustment method MCTADJ 3 Partial plume path adjustment<br />

Usually 0, but does allow <strong>for</strong> CTDM-like treatment of sub grid scale hills (See input<br />

Sub grid-scale complex terrain MCTSG<br />

0 Group 6)<br />

Default is not to use slug model. But it is <strong>the</strong> recommended approach <strong>for</strong> area sources<br />

Near-field puffs modeled as slugs MSLUG<br />

0 with receptors in <strong>the</strong> very near field or <strong>for</strong> time-varying emissions such as accidental<br />

releases are modeled.<br />

Transitional plume rise MTRANS 1 Yes, always allow transitional rise<br />

Yes, always allow stack tip downwash. It becomes important if ratio of stack gas exit<br />

Stack tip downwash<br />

MTIP<br />

1 velocity to wind speed is < 1.5<br />

Method to compute plume rise <strong>for</strong><br />

point sources not subject to<br />

downwash<br />

Method to simulate building<br />

downwash<br />

Vertical wind shear modeled above<br />

stack top<br />

MRISE<br />

MBDW<br />

MSHEAR<br />

1<br />

2<br />

0<br />

Yes, to Briggs plume rise (1). The o<strong>the</strong>r option (2) is meant <strong>for</strong> very hot sources such<br />

as flares where <strong>the</strong> Bousinesq equation is no longer valid <strong>and</strong> plume rise needs to be<br />

treated numerically<br />

PRIME Method unless long such as aluminum smelters with aspect ratios of L/W<br />

over 5-10. For <strong>the</strong>se situations use MBDW=1 (ISC/BLP downwash method)<br />

The default is <strong>for</strong> no vertical wind shear. The model inherently includes variable flow<br />

in <strong>the</strong> vertical from <strong>the</strong> upper air data. If this option is used <strong>the</strong> model applies a<br />

power law wind speed profile above stack top.<br />

Puff Splitting allowed MSPLIT 0 No puff splitting. In long range transport, puff splitting may be necessary. In shortrange<br />

modeling, MSPLIT=0 is recommended.<br />

Chemistry to be modeled <strong>and</strong> trans<strong>for</strong>mation rates are computed internally using<br />

Chemical trans<strong>for</strong>mation<br />

MCHEM<br />

1 MESOPUFF II scheme (recommended when dealing with SO2, SO4, NOx, HNO3<br />

<strong>and</strong> NO3 concentration predictions over 10-20 km or more.<br />

Aqueous phase chemistry MACHEM 0 Aqueous phase chemistry (option is not currently active)<br />

Wet removal modeled MWET 1 Wet deposition is often important long range transport. May be used in near-field in<br />

certain circumstances. Depends on <strong>the</strong> pollutant characteristics.<br />

61

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