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Last modified
7/28/2009 2:40:35 PM
Creation date
4/24/2008 2:52:55 PM
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Weather Modification
Title
The Feasibility of Enhancing Streamflow in the Silver Iodide in the Sevier River Basin of Utah bt Seeding Winter Mountain Clouds
Date
12/1/1991
Weather Modification - Doc Type
Report
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<br />altitude generators consistently produce AgI plumes over mountainous terrain within the SL W zone. <br />However, additional T &0 investigations are needed to enable improved delivery of adequate <br />concentrations of ice nuclei to SL W cloud regions. <br /> <br />A large percentage of winter storms are too warm for seeding with ground-released AgI which has limited <br />effectiveness at temperatures above about -8 oC. Even the expensive option of aircraft AgI seeding might <br />not be effective in many of these cases because the SL W is concentrated near the ground where the <br />temperature may be too wann for significant ice crystal formation. Options such as propane seeding <br />should be explored for wann storms so the effectiveness of seeding may be optimized. <br /> <br />Storms typically go through a series of stages in their passage over a mountain region. Studies of these <br />storm stages are reviewed with emphasis on the availability of SL W and the T &0 of ground-released Agl. <br />It is shown that seedability often varies considerably during a storm passage and also from storm to storm. <br /> <br />Long-term precipitation and temperature records are considered from a high altitude weather station in the <br />Sevier Basin, These provide estimates of typical stonn frequencies and precipitation amounts and how <br />these range from season to season. Precipitation days, which can be considered a proxy for days in which <br />seeding might be conducted, varied from 30 days during dry winters to 60 days during wet winters. <br />Although the number of precipitation days are variable, even dry winters appear to have enough for <br />frequent seeding operations. Temperature data indicated nearly 80 percent of the days with snowfall were <br />-6 oC or colder at the weather station. <br /> <br />Review of the available evidence indicates several uncertainties about the effectiveness of cloud seediitg <br />as currently practiced in Utah and the West in general. A number of options are available to deal with <br />these uncertainties as briefly discussed, The option recommended is believed to offer the most rapid <br />means of removing uncertainties associated with the Utah operational cloud seeding program, but it is a <br />relatively expensive option. The recommended approach is to conduct a demonstration program in the <br />Sevier River Drainage to validate winter orographic cloud seeding. Accordingly, design considerations <br />are reviewed and the best experimental area is selected for the basin. A two-stage program is proposed <br />that would emphasize cause-and-effect physical experiments over a limited area during the first phase. <br />The second phase would consist of a statistical/physical experiment to confinn the multi winter increases <br />that seeding could produce over a large area. <br /> <br />Preliminary benefit-cost estimates are given based on an assumed increase in seasonal. snowpack with <br />subsequent runoff calculated by a snow accumulation and ablation model. An economic analysis by the <br />Utah Division of Water Resources provided the value of the calculated additional water. Two costs of <br />operational seeding were used. The first reflects the costs of the Utah operational seeding program as <br />currently conducted, using widely spaced valley generators. The second estimate reflects the additional <br />costs of using closely spaced, high output generators well up the windward slopes to improve targeting. <br />The results indicate benefit-cost ratios from about 3:1 to more than 10:1, depending upon the assumptions <br />made. If winter cloud seeding can provide mountain snowfall increases approaching or exceeding 10 <br />percent, the technology should ltave good economic justification. <br /> <br />iv <br />
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