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<br />4 <br /> <br />I <br />1 <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 />Data collection for SCPP began during the winter of 1976-77. The SCPP <br /> <br />field office was set up at Auburn, California in September 1977. SCPP <br /> <br />has been in the field each winter since then with the exception of 1980-81, <br /> <br />which was a stand-down year for analysis of the data collected during <br /> <br />the 3 preceding years. Cloud seeding experiments have been conducted <br /> <br />on SCPP since the winter of 1977-78, but on a limited scale and with <br /> <br />close attention to suspension criteria, which were designed to prevent <br /> <br />seeding during hazardous weather situations. <br /> <br />The next section of this report details the procedures used in conducting <br /> <br />the SCPP field operations, both past and present. Following this section <br /> <br />the major findings of these field studies will be reviewed and their <br /> <br />impact on planning for the next 3 winters of field operations will be <br /> <br />discussed. <br /> <br />2. SCPP Field Operations <br /> <br /> <br />2.1 Operational Programs <br /> <br /> <br />Operational cloud seeding projects to increase precipitation and runoff <br /> <br />from the Sierra Nevada have existed since 1948. Nearly all of these <br /> <br />projects have been based on the hypothesis that the precipitation rate <br /> <br /> <br />in a mountain storm can be increased by increasing the concentrations <br /> <br />of ice crystals in the clouds at temperatures warmer than about -200C. <br /> <br /> <br />This hypothesis is based on the observation that some clouds contain <br /> <br /> <br />liquid (supercooled) droplets at temperatures below OoC, and the fact <br /> <br />that ice crystals in the presence of supercooled cloud droplets grow <br /> <br />in a few minutes into small snowflakes. The additional ice crystals <br />