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ENVIRONMENTAL CONSEQUENCES in rocky mountain coniferous ...

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I<br />

Where: Cs is the concentration at the surface;<br />

C, is the concentration <strong>in</strong> the atmosphere and<br />

r' is the resistance to flow<br />

Table 1 lists measurable <strong>in</strong>direct factors for each of the operational factors.<br />

Table 1 .-- Some operational factors, or those capable of be<strong>in</strong>g exchanqed, and<br />

measurable parameters for each.<br />

Operational factors<br />

Heat<br />

Moisture<br />

Measurable parameters<br />

Soil temperature<br />

Air temperature<br />

Radiation<br />

Water potential<br />

Soil moisture<br />

Precipitation<br />

Evapotranspiration<br />

Snow accumulation<br />

Snow me1 t<br />

Nutrients Soil nutrients<br />

Gases<br />

Light<br />

Mechanical energy<br />

Oxygen<br />

Carbon dioxide<br />

Qua1 ity<br />

Radiation<br />

W<strong>in</strong>d<br />

Soil creep<br />

Frost heav<strong>in</strong>g<br />

It is important that we base our studies on the operational factors so that<br />

models and predictive relationships will be more widely appl icable (Berg1 und<br />

1974). Further, this permits us to measure only what is needed to answer our specific<br />

questions which Federer (1974) calls the rifle approach. This is opposed to the<br />

shotgun approach which measures as many th<strong>in</strong>gs as possible hop<strong>in</strong>g someth<strong>in</strong>g will be<br />

useful . Model s constructed based on these concepts wi 11 have more uni versa1 appl i -<br />

cabil ity.

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