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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 />precipitanon development m natural and seeded orographic clouds; and <br />~) to gain a better understanding of the trajectories of natural and seeded precipitation <br />parricles m It"inter orographic clouds. <br />Since 1991 the o"~erall goal of the NOA.A.-Ctah program has been to evaluate the methodology <br />employed in the Ctah operational cloud seeding program, and to provide guidelines for improving <br />the program based on results of carefully designed and conducted field research programs. <br />In the early Utah field studies in 1983 (Long, 1984), 1985 (Long, 1986) and 1987 (Huggins, <br />1990a) the research concentrated on the structure of winter storms, primarily studying the influences <br />on, and the development of supercooled liquid water (SL W) in storms. These studies verified the <br />occurrence of supercooled liquid water in nearly all winter storms that affected the research area <br />in southwestern Ctah. A detailed case study, reported on by Sassen et al. (1990) and Long et al <br />( 1990), also revealed the importance of mesoscale weather and local topography in the development <br />and spatial distribution of SL W. Super and Huggins (1993) summarized SL Wand precipitation <br />amounts from four KOA..-\-Utah \'vinter field programs, shO\'ving that storms of all sizes contained <br />SL \V, eyen the largest precipitation producers. <br />From 1989 through the present, the NOAA-Utah program has focussed more on objectives <br />2, 3, and 4. Also, the field project area was moved from the Tushar Mountains of southwestern Utah <br />to the Wasatch Plateau of central Utah. The Wasatch Plateau offered the benefit of more uniform <br />terrain, and thus the adyantage of conducting research aircraft tlights at much lower heights above <br />the terrain. In field programs in 1991 and 1994, the main effort was spent documenting the transport <br />and dispersion of cloud seeding aerosols over the Wasatch Plateau from valley and high altitude <br />ground-based seeding experiments. In addition, the spatial characteristics of SL W were investigated <br />using a mobile microwave radiometer, and the physical effects of seeding were studied using <br />ground-based mobile and stationary instrument platforms, and an instrumented research aircraft. <br />Results from these studies can be found in Super ( 1994), Super (1995), Huggins (1995), Holroyd <br />et al. (1995), Heimbach (1996), Huggins (1996), and Super (1996). The last four papers cover results <br />from the 1994 field program, including modeling studies which describe aerosol transport from both <br />high altitude and yalley-based seeding locations and documentation of microphysical and radar <br />seeding signatures. <br /> <br />2 <br />