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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 />9 <br /> <br />stages of cloud seeding than is currently available, and they <br /> <br />will provide some comparisons between laboratory results and <br /> <br />computer model simulations of cloud and ice nucleation for well <br /> <br />defined experimental conditions. <br /> <br />2. The results will serve the needs of conceptual models and <br /> <br />computer models for accurate descriptions of ice nucleating <br /> <br />behavior along different paths into and through clouds. <br /> <br />3. The results will provide information to be applied as guidance <br />in operational weather modification programs, for choosing <br /> <br />seeding agents and seeding methods. This is useful for planning <br /> <br />experimental tests and for evaluating program effectiveness. <br /> <br />4. The results provide a data base for comparing to existing <br /> <br />theories, or for formulating new ones, for ice nucleation by <br /> <br />aerosols. <br /> <br />5. Establish simple general procedures for characterizing any ice <br /> <br />nucleant, natural or artificial. <br />