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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 />I. I~TRODlTTIO~ <br /> <br />\Vater shonages in the western United States have prompted state and private agencies to <br />seek alternatives to increasing water supplies for agriculture, power generation and municipal use. <br />The states of~evada and Utah have conducted operational cloud seeding programs for the purpose <br />of increasing \\inter sno\\-packs for many years. The goal in these programs is primarily to increase <br />stream flow in the spring and summer for municipal and agricultural use. Recreation and wildlife <br />also potentially benefit from the additional water. The benefits of these projects depend a great deal <br />on the cost of the operations, which must be compared to the amount of additional snowtall that can <br />be produced by cloud seeding operations, and the dollar value of that additional water. <br />Although some statistical studies of the effects of cloud seeding in the 1960's and 1970's <br />indicated promising positive results from seeding winter storms, the physical basis for the apparent <br />effects was not completely documented. Carefully controlled experiments in several mountainous <br />regions of the \Vest in the 1980' s began to piece together the physical" chain of events" that occurred <br />after seeding orographically enhanced cloud systems. Among these studies were results reported by <br />Super and Heimbach (1988), Super and Boe l1988) and Deshler et al. (1988), for mountainous <br />regions of Montana, Colorado and California, respectively. All found evidence of microphysical <br />changes, ~-pically ice panicle concentration increases, from seeding orographic clouds with silver <br />iodide. In some instances the link to increases in precipitation at the ground was made, but these <br />cases were fe\\' in number. <br />In 1983 the state of Utah, along with the state of Nevada, began conducting research on <br />winter storm modification as part of a cooperative program vvith the National Oceanic and <br />Atmospheric Administration (NOAA). ~ear the beginning of the Utah program, the scientific <br />objectives were defined to be: <br />I} TO describe the spatial and temporal distributions of supercooled liquid water (SLW) in <br />l'dnter clouds over Utah's mountains, and the factors controlling the SLW; <br />2) to understand haw silver wdlde cloud seeding material may be deltvered from ground <br />generaTOrs to the "rimer cloud regwns containing SLW; <br />3) TO gain a better understanding of the physical processes responsible for winter <br /> <br />1 <br />