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<br />. <br /> <br />mountains to 5-10 km east of the base by a factor varying from 1.3 to <br /> <br />2.0 depending on the depth elnd convective nature of the clouds. During <br /> <br />a cloudy period the liquid welter appears to develop first over the moun- <br /> <br />tains, and it remains there toward the end of the period after it has <br /> <br />disappeared from other direlctions. These effects on the liquid water <br /> <br />are clearly orographic. The evidence suggests the liquid water is <br /> <br />located at temperatures colder than -5 C or at altitudes greater than <br /> <br />about 3.3 km MSL. Research on delivery of seeding materials to clouds <br /> <br />over the Tushar Mtns from the ground generators used in the operational <br /> <br />project suggests delivery is frequently limited by adverse meteorologi- <br />cal conditions. <br />The 1985 field research effort and subsequent data interpretation <br />and analysis will again be conducted by the Utah Division of Water <br />Resources and associated groups. The field studies will again be in <br />the Tushar Mtns area durin~J the period 15 January to 15 March. The <br />major objectives of the rese~arch remain essentially the same and are <br />concerned with: <br />1) assessing the transport and delivery of seeding material from <br />ground-based generators to the clouds over the Tushar Mtns, and <br />2) describing the spatial and temporal distribution of super- <br />cooled liquid water in the clouds, the physical processes <br />responsible for prec:ipitation development, and the trajectories <br />of cloud and precipi1tation particles. <br />In 1983 the research toward these objectives was largely statistical in <br />nature with less emphasis on case-studies of the data. In 1985, on the <br />other hand, the reverse emphasis will prevail because the available <br /> <br />. <br /> <br />.. <br /> <br />(t <br /> <br />.. <br /> <br />,. <br /> <br />. <br /> <br />. <br /> <br />II <br /> <br />. <br /> <br />2 <br /> <br />. <br />