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<br />Changnon, S. A., 1991: Cloud and precipitation development re:lated to the St. Louis precipitation anomaly. <br />SWS Contract Report 532, NOAA Cooperative Agreements NA90AAHOA175 and NA27RA017301. <br />Illinois State Water Survey, Champaign, IL, 28 pp. <br /> <br />No abstract. <br /> <br />Changnon, S. A., 1991: The dilemma of climatic and hydrologic forecasting for the Great Lakes. Proceedings, <br />Symposium of the Great Lakes Water Level Forecasting and Statistics, Windsor, Ontario, May 16-17, <br />1991. Great Lakes Commission and NOAA Great Lakl~S Environmental Research Laboratory, <br />Ann Arbor, MI, 13-25. <br /> <br />No abstract. <br /> <br />Changnon, S. A., R. R. Czys, S. E. Hollinger, F. A. Huff, K. E. Kunkel, M. S. Petersen, R. W. Scott, <br />D. W. Staggs, and N. E. Westcott, 1991: Analysis and planning for Precipitation Augmentation for <br />Crops Experiment. Annual Report, NOAA Cooperative Agreement NA90AAHOAI75. Illinois State <br />Water Survey, Champaign, IL, 122 pp. (available from National Technical Infonnation Service, <br />5285 Port Royal Rd., Springfield, V A 22161). <br /> <br />No abstract. <br /> <br />Changnon, S. A., R. R. Czys, R. W. Scott, and N. E. Westcott, 1991: Illinois precipitation research: A focus on <br />cloud and precipitation modification. Bulletin of the American Meteorological Society, 72:587-604. <br /> <br />At the heart of the 40-year atmospheric research endeavors of the Illinois State Water Survey have been <br />studies to understand precipitation processes in order to learn how precipitation is modified purposefully <br />and accidentally, and to measure the physical and socioeconomic consequences of cloud and <br />precipitation moditication. Major field and laboratory activities of past years are briefly treated as a <br />basis for describing the key fmdings of the past ten years. Recent studies of inadvertent and purposeful <br />cloud and rain modification and their effects are emphasized, including a 1989 field project conducted <br />in Illinois and key findings fro~ an ongoing exploratory experiment addressing cloud and rain <br />modification. Results are encouraging for the use of dynamic seeding on summer cumulifonn clouds of <br />the Midwest. <br /> <br />Typical in-cloud results at -lOoC reveal multiple updrafts that tend to be filled with large amounts of <br />supercooled drizzle and raindrops. Natural ice production is vigorous, and initial concentrations are <br />larger than expected from ice nuclei. However, natural ice production is not so vigorous as to preclude <br />opportunities for seeding. Radar-based studies of such c:1ouds reveal that their echo cores usually can be <br />identified prior to desired seeding times, which is significant for the evaluation of their behavior. Cell <br />characteristics show considerable variance under different types of meteorological conditions. Analysis <br />of cell mergers reveals that under conditions of weak vertical shear, mid-level intercell flow at 4 Ian <br />occurs as the reflectivity bridge between cells rapidly intensifies. The degree of intensitication of <br />single-echo cores after they merge is strongly related to the age and vigor of the cores before they join. <br />Hence, cloud growth may be enhanced if seeding can encourage echo cores to merge at critical times. <br />Forecasting research has developed a technique for objectively distinguishing between operational <br />seeding and non operational days and for objectively predicting maximum cloud-top height and seeding <br />suitability. An accuracy rate of up to 60% in predicting maximum echo-top height using four categories <br />has been achieved and suggests its use as a covariate in future experimentation. Impact studies illustrate <br />that sizable summer rain increases would be necessary to produce economically beneficial outcomes for <br />Corn Belt agriculture. Increases of ~25% in July rainfall across certain high-production crop districts of <br />the Corn Belt would produce economic effects realized nationally. <br /> <br />19 <br />