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<br />Appendix A <br /> <br />Melt and runoff from snowpack contributes most of the reservoir storage in large portions of <br />the Western U.S., so snowpack augmentation is an attractive target in the region. Accordingly, <br />operational cloud seeding to augment snowpack in the mountains has a long history in several <br />western states. Prior studies suggest that seeding of supercooled orographic clouds has worked, <br />yielding seasonal precipitation increases on the order of 10% (AMS, 1998). More research and <br />documentation is needed to buttress these findings, however. <br />Winter orographic seeding has been dominated by the use of silver iodide (AgI), delivered <br />from ground-based generators or aircraft The last federally-assisted cloud seeding project was a <br />winter experiment in Utah during the 1990s (Super 1999). There are a number of other seeding <br />technologies that have been put forward but not tested extensively. New chemical compositions, <br />such as silver chloride-iodide complexes, may act more efficiently to produce ice particles at <br />temperatures warmer than _50C, where AgI is ineffective. Similar warm temperature results may <br />be achieved by cost-effective liquid propane generators (Medina 2000). The Utah WDMP <br />experiment operated such generators. <br />The use of tracer chemicals with the seeding materials affords a method to verify the <br />targeting of those materials. Such chemicals were employed in the Nevada WDMP experiment, <br />which even attempted to distinguish ground-based and aircraft seeding signatures. This <br />experiment also included a Lagrangian particle dispersion model and windflow from the MM5 <br />cloud model to further characterize seeding plume trajectories (Koracln et al. 1998). The <br />Colorado experiment also used a Lagrangian transport model (Uliasz 1994) coupled with the <br />RAMS cloud model (Cotton et al. 1994) to evaluate targeting of seeding material. <br /> <br />2.2 Convective Seeding <br /> <br />Research into warm-season seeding of convective clouds in the Western U.S. was <br />conducted mostly in the late 1960s through early 1980s, notably through projects such as the <br />National Hail Research Experiment (NHRE) and the High Plains Experiment (HIPLEX; Cooper <br />and Lawson 1984). These experiments had mixed results for hail suppression and rainfall <br />augmentation, respectively. Rosenfeld and Woodley (1989; 1993) reported increases in radar- <br />estimated rainfall with Agl seeding in West Texas during the 1980s. Tracer studies were <br />conducted in North Dakota in 1989 (Boe et al. 1992). <br />More recently, positive findings regarding hygroscopic seeding have been reported in <br />several experiments, e.g., in South Africa (Mather et al. 1997), Thailand (Silverman and <br />Sukarnjanaset 2000), Mexico (Bruintjes et al. 2001; Fowler et al. 2001), and India (Murty et al. <br />2000). Vin et al. (2000; 2001) have conducted modeling studies of hygroscopic seeding that offer <br />plausible arguments for why such seeding may lead to rain increases. <br /> <br />2.3 Individual Project Goals <br /> <br />The states conducting WDMP research are shown in Fig. 1. Three projects, in Nevada, <br />Utah and Colorado, are involved in cool-season, orographic seeding. The other two projects, one <br />in North Dakota and the other in Oklahoma, Texas and New Mexico, seed convective clouds <br />during the warm season. Specifically, individual project principal goals are as follows: <br />. Nevada - (1) Remotely sense supercooled cloud water to quantify cloud seeding <br />potential in a selected watershed; (2) Apply mesoscale atmospheric and dispersion <br />modeling to evaluate seeding effectiveness under a variety of storm conditions; (3) <br />Evaluate seeding effectiveness through physical and chemical analyses of snow <br />packs; (4) Use hydrologic modeling to estimate impacts of seeding-induced increases <br />in snow packs on streamflow; (5) Characterize natural and seeded cloud regions with <br />in situ aircraft microphysical measurements. <br />. Utah - (1) Conduct randomized cloud seeding on the Wasatch Plateau using propane <br />dispensers to develop embryonic ice particles; (2) Explore impacts on precipitation by <br />the cloud seeding. <br />. Colorado - (1) Configure the Colorado State University cloud model (RAMS) and conduct <br />modeling over operational cloud seeding areas; (2) Implement algorithms simulating <br />cloud seeding generators as sources of ice nuclei, (3) Simulate Lagrangian transport <br /> <br />-2- <br />