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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />5 <br /> <br />mechanism or ice nucleation were assumed with corresponding rates and <br />yields of ice crystal production. Nucleation was then followed <br />spatially and temporally through the model predicted cloud. The model <br />is also capable of predicting the location or precipitation reaChing the <br />ground as controlled by the predicted location of ice nucleation in <br />cloud. <br />Application or chemical kinetic methodology to ice nucleation and <br />the procedures for inoorporating it into the theoretical orographic <br />cloud model are presented in chapter three. Laboratory facilities, <br />analysis and results are presented in chapters four and five. Results <br />of the application of kinetics to the theoretical model are presented in <br />chapter six. In the remainder of this paper, silver iodide is written <br />in its ch8llical abreviation as AgI, and sodium iodide as NaI. AgI-NaI <br />will refer to any mixture or AgI and NaI regardless or the proportions <br />of the substances. Formulations, such as 2AgI"NaI or AgI"NaI"4H20 will <br />refer to specific complex compounds. <br /> <br />