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<br />2 <br /> <br />project was the clearing of supercooled stratus by means of <br /> <br />seeding from an airplane with dry ice or siver iodide. The <br /> <br /> <br />history of early weather modification projects is described by <br /> <br />Byers (1974). <br /> <br /> <br />Over the years, a need existed for increasing precipitation in <br /> <br /> <br />the American River Basin of the Sierra Nevada in California. The <br /> <br /> <br />Sierra Cooperative Pilot Project (SCPP) was initiated in the early <br /> <br /> <br />seventies to investigate the potential for precipitation <br /> <br /> <br />augmentation by seeding agents such as dry ice and silver iodide. <br /> <br />The SCPP is a part of the winter cloud seeding research program <br /> <br /> <br />conducted by the Bureau of Reclamation (Burec), u.S. Department of <br /> <br /> <br />Interior. One objective in SCPP is to better understand <br /> <br />precipi tation development by studying the physical processes <br /> <br />involved, and thus to identify the important cohdi tions that <br /> <br /> <br />prov ide good potential to improve water resources in the Sierra <br /> <br />Nevada. <br /> <br />During the winter months of 1979 through 1986 (except the 1981 <br /> <br /> <br />season), convective and stratiform-orographic clouds have been <br /> <br />treated with dry ice or silver iodide, and the evolutlon of ice in <br /> <br /> <br />the treated clouds was documented with aircraft observations. <br /> <br /> <br />To better understand the particle growth process, calculations <br /> <br />were done for this thesis using two models: First, the "Particle <br /> <br />Growth Model" (PGM) of Heymsfield (1982) embedded in a kinematic <br /> <br /> <br />flow field representative of the Sierra barrier was used, which <br /> <br /> <br />considers crystal growth by diffusion, accretion and the <br /> <br /> <br />subsequent fall trajectories. Second, the "Aggr~ation Model" <br /> <br />. <br /> <br />. <br /> <br />e <br /> <br />. <br /> <br />. <br /> <br />e. <br /> <br />. <br /> <br />e. <br /> <br />. <br /> <br />. <br /> <br />e <br /> <br />. <br /> <br />. <br />