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<br />I <br />I <br /> <br />chamber. The model was utilized as a diagnostic tool to estimate water <br /> <br />and the transferability of results was evaluated by modeling two actual <br /> <br />I <br />I <br />I <br />I <br />I <br /> <br />supersaturation in association with experiments and it was used for <br /> <br />comparison of the predictions of new ice nucleus formulations with <br /> <br />observations from generalized seeding simulations conducted in the <br /> <br />cloud chamber. The nucleant and mode-specific formulations represent <br /> <br />vast improvements compared to available formulations for "pure" AgI. <br /> <br />The general implications of these new results were tested by using the <br /> <br />model to simulate a few common seeding situations in the atmosphere, <br /> <br />seeding experiments conducted in summertime cumuli. Within the <br /> <br />I <br /> <br />limitations of the cloud model used, agreement with the atmospheric <br /> <br />results was very good. The results of this study should be most useful <br /> <br />I <br /> <br />for designing standard and better methods for the quantitative study of <br /> <br />ice nucleation by artificially generated and natural aerosols, and for <br /> <br />I <br />I <br /> <br />evaluating cloud seeding methodologies and potential seeding effects <br /> <br />using more complex microphysical-dynamic cloud models. <br /> <br />I <br /> <br />Paul Judson DeMott <br />Atmospheric Science Department <br />Colorado State University <br />Fort Collins, CO 80523 <br />Spring 1990 <br /> <br />I <br /> <br />I <br />I <br /> <br />I <br /> <br />iv <br /> <br />I <br />I <br />I <br />