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

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UTM Y Coordinate (km) - WGS84<br />

6474.5<br />

6474<br />

6473.5<br />

6473<br />

6472.5<br />

6472<br />

6471.5<br />

6471<br />

401.5 402 402.5 403 403.5 404 404.5 405<br />

UTM X Coordinate (km) - WGS84<br />

Figure 3-10 <strong>CALPUFF</strong> peak, 1-hr average concentration map using 10-minute<br />

meteorological data <strong>and</strong> default calm threshold of 0.5 m/s. Real turbulence parameters<br />

were used with a minimum σv of 0.2 m/s, σw was left unchanged at <strong>the</strong> model’s default<br />

values.<br />

Various calm user options were evaluated <strong>for</strong> a single volume source <strong>and</strong> using ei<strong>the</strong>r <strong>the</strong> 10minute<br />

or 1-hour Caversham, WA meteorological data sets. The results are presented in Figure 3-<br />

11. Both Figures 3-9 <strong>and</strong> 3-10 are shown a second time in Figure 3-11 <strong>for</strong> brevity. There is little<br />

difference detected when lowering <strong>the</strong> minimum calm threshold < 0.5 m/s which <strong>for</strong>ces <strong>the</strong> model<br />

to step from distance to time based dispersion. In many instances 0.5 m/s is also <strong>the</strong> threshold of<br />

<strong>the</strong> instrument. There is also little difference when using 1-hour meteorology <strong>and</strong> real turbulence<br />

parameters when compared to <strong>the</strong> case using 1-hour meteorology <strong>and</strong> computed σv or, <strong>the</strong> case<br />

using 10-minute meteorology <strong>and</strong> computed σv.<br />

These results show that <strong>the</strong> single biggest difference is not <strong>the</strong> inclusion of <strong>the</strong> real time<br />

turbulence data or <strong>the</strong> sub-hourly data but using a σv threshold of 0.2 m/s. Clearly <strong>the</strong> combined<br />

effect of σv of 0.2 m/s, real turbulence parameters <strong>and</strong> sub-hourly meteorological data is <strong>the</strong><br />

preferred <strong>and</strong> most realistic option to treat calm <strong>and</strong> light wind periods, but in <strong>the</strong> event of not<br />

having sub-hourly meteorological data, or real turbulence data <strong>the</strong>re is still strong evidence to use<br />

a σv value of 0.2 m/s overl<strong>and</strong> (Barclay 2007).<br />

34

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