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Table of Contents - The Atmospheric Studies Group at TRC

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Section 9: CALPUFF<br />

<strong>The</strong> following procedure is recommended to determine the terrain inputs for the CALPUFF CTSG<br />

algorithm from a topographic map.<br />

a. Identify the sub-grid terrain fe<strong>at</strong>ures to be modeled.<br />

Such fe<strong>at</strong>ures will generally be small enough th<strong>at</strong> they could be contained within one grid-square.<br />

This does not mean th<strong>at</strong> they cannot straddle two or more squares. <strong>The</strong> fe<strong>at</strong>ures should be<br />

prominent, and possibly lie near source regions so th<strong>at</strong> the additional comput<strong>at</strong>ions required by<br />

CTSG are warranted in resolving important pollutant impact areas.<br />

b. Decide on the orient<strong>at</strong>ion <strong>of</strong> the fe<strong>at</strong>ure.<br />

<strong>The</strong> orient<strong>at</strong>ion <strong>of</strong> the fe<strong>at</strong>ure is generally evident if the fe<strong>at</strong>ure is longer in one direction than<br />

another. If there is no dominant direction to the fe<strong>at</strong>ure, model it as a symmetric fe<strong>at</strong>ure, and<br />

choose an orient<strong>at</strong>ion <strong>of</strong> north.<br />

c. Obtain height-pr<strong>of</strong>iles along each axis <strong>of</strong> the fe<strong>at</strong>ure.<br />

Choose an approxim<strong>at</strong>e center for the fe<strong>at</strong>ure and draw axes through it (one axis should lie along<br />

the direction <strong>of</strong> orient<strong>at</strong>ion). Along each axis, measure the distance between approxim<strong>at</strong>e<br />

intersections <strong>of</strong> the axis with marked contours. <strong>The</strong> distances so measured should extend from<br />

the contour furthest to the south to the same contour furthest to the north (for a north-south axis).<br />

Divide each <strong>of</strong> these distances by two, and tabul<strong>at</strong>e the results.<br />

d. Identify the maximum elev<strong>at</strong>ion <strong>of</strong> the fe<strong>at</strong>ure.<br />

Take the peak elev<strong>at</strong>ion directly from the map.<br />

e. Identify the elev<strong>at</strong>ion <strong>at</strong> the base <strong>of</strong> the fe<strong>at</strong>ure.<br />

Generally, the base <strong>of</strong> the fe<strong>at</strong>ure will be th<strong>at</strong> point <strong>at</strong> which the fe<strong>at</strong>ure becomes<br />

indistinguishable from terrain vari<strong>at</strong>ions around it.<br />

f. Convert all elev<strong>at</strong>ions th<strong>at</strong> were tabul<strong>at</strong>ed to heights above the base <strong>of</strong> the fe<strong>at</strong>ure.<br />

g. Use optimizer program (OPTHILL) to obtain shape parameters.<br />

<strong>The</strong> "relief" parameter is just the peak elev<strong>at</strong>ion less the base elev<strong>at</strong>ion. <strong>The</strong> "axmax" value for<br />

each axis should be represent<strong>at</strong>ive <strong>of</strong> the maximum extent <strong>of</strong> the fe<strong>at</strong>ure along each axis <strong>at</strong> the<br />

elev<strong>at</strong>ion <strong>of</strong> the base <strong>of</strong> the fe<strong>at</strong>ure. With these two variables fixed for each axis, the heightpr<strong>of</strong>ile<br />

d<strong>at</strong>a from step c. can be put through OPTHILL to obtain "expo" and "scale" for each axis.<br />

9-324

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