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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 />ABSTRACT <br /> <br />QUANTIFYING ICE NUCLEATION BY SILVER IODIDE AEROSOLS <br /> <br />Laboratory studies of artificial ice nucleating aerosols used for <br /> <br />weather modification by cloud seeding have generally been inadequate <br /> <br />for describing their complex action in the varied temperature, pressure <br /> <br />humidity, and cloud conditions that can be encountered in the <br /> <br />atmosphere. This study provides a quantitative framework for predicting <br /> <br />ice formation by aerosol particles based on experiments which <br /> <br />specifically target currently accepted mechanisms by which ice can <br /> <br />form. A physical system for reproducing realistic atmospheric cloud <br /> <br />conditions, the Colorado State University dynamic (controlled <br /> <br />expansion) cloud chamber, is described. Physical simulations of <br /> <br />adiabatic cloud formation and growth are demonstrated. Methodologies <br /> <br />were also formulated to use the cloud chamber and other available <br /> <br />intrumentation to isolate the action of ice nucleating aerosols by <br /> <br />accepted primary ice nucleation modes. These methods were applied to <br /> <br /> <br />the study of two chemically different silver iodide (AgI)-type <br /> <br /> <br />aerosols, generated in the exact form in which they have been used for <br /> <br /> <br />seeding natural clouds. The results were formulated as a function of <br /> <br />bas ic thermodynamic quanti ties and particle size. An available one <br /> <br />dimensional numerical cloud model with microphysical detail was adapted <br /> <br />for the equivalent simulation of experiments performed in the cloud <br /> <br />Hi <br />