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<br /> <br />;, <br /> <br />EV ALVA TION OF OPERATIONAL CLOUD SEEDING IN W&~"TERN <br />KANSAS <br /> <br />1. INTRODUCTION, SUMMARY, AND CONCLUSIONS <br /> <br />In 1975, agricultural interests in southwestern Kansas organized a weather modification program <br />to sec~ summer clouds for the purposes of increasing rainfall and suppress~g crop-hail damage. <br />1be project has continued each year since then, although the project area has: varied as individual <br />counties elected to participate or not to participate on a yearly basis (figure 1.1). For its first few <br />yean>, the project was called the "Muddy Road" Project. More recently it, has been Cluled the <br />Western Kansas Weather ModifICation Project. Administrative suppon for the project is provided <br />by the Western Kansas Groundwater Management District No.1, headquaftered in Scott City, <br />Kansas. <br /> <br />The project has been conducted each year during the growing season, which extends from late <br />April to September. The actual starting and stopping dates vary from year: to year. Se:eding is <br />carried out each year by several aircraft equipped with one or more types of s~ing devi<:e5. The <br />silver iodide generators used have included both liquid-fueled generators burning solutions of <br />silver iodide in acetone and solid (pyrotechnic) generators. Most of tne seeding has been <br />conducted in updrafts below the bases of convective clouds. During some years, high <br />performance aircraft capable of cloud-top seeding have been available. The high perlormance <br />aircraft are equipped with racks for droppable pyrotechnics, dry ice dispensers, lOr both. <br />Additional information on seeding operations is provided in section 2. <br /> <br />The project has operated on the assumption that additional ice particles pr~ced in the clouds hy <br />the seeding agents would grow into snowflakes, graupel panicles (sometimes 'called snow pellets), <br />or small hail, and then melt to raindrops during their fall to the ground. It was reasoned that this <br />process would tend to increase SUI1}ll1er rainfall and would also, by increaSing the numbers of <br />frozen precipitation particles, tend to reduce their sizes and thereby decrease the probabililty of any <br />of tbm1 reaching the ground as hailstones before completely melting to raindxops (the competing <br />emblYo concept of hail suppression). <br /> <br />Since lenS, the operators of the project have recognized the impolUJllce of ev8tuating the effects of <br />their operations. Some generally inconclusive analyses of the rainfall data have been published hy <br />scientists of the illinois State Water Survey (Hsu and Chen [1] and Huff et aJ.. [2]). In 1985, the <br />Kansas Water Office asked the Bureau of Reclamation's Southwest Regional Office in Amarillo, <br />Texas, for assistance in evaluating the project. The Southwest Region in turn requested the <br />Bureau's Engineering and Research Center in Denver, Colorado, to conduct ~ evaluation. Work <br />got underway in the DARR (Division of Atmospheric Resources Research) in the fall of 1985 <br />under a plan calling for the evaluation to extend through September 1987. 111lis report sununarizes <br />the evaluation and sets forth the conclusions reached. <br /> <br />The basic approach followed was to acquire rainfall and hail data for the t8l.'get area and a large <br />surrounding study area and then examine these data for changes that could be attribute:d to the <br />projc.'Ct activities. In addition, copies of logs of seeding activities were obtairied from the Western <br />Kansas Groundwater Management District No. 1 so that information about the: location and amount <br />of seeding could be compared with the rain and hail data. Details are provided in later sections of <br />dUsJ~pon. ' <br /> <br />Daily rainfall data were obtained from the National Climatic Center in Asheville, Nonh Carolina. <br />Crop-hail loss data were obtained from the Crop-Hail1nsurance Actuarial AssOCiation of Chicago, <br />