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Last modified
7/28/2009 2:33:58 PM
Creation date
3/5/2008 10:53:13 AM
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Template:
Weather Modification
Title
Summary of the NOAA/Utah Atmospheric Modification Program: 1990-1996
Date
9/1/1998
State
UT
Weather Modification - Doc Type
Report
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<br />. . <br /> <br />... <br /> <br />dispenser. That dispenser, and two satellite dispensers, were controlled by the presence/absence of SL W, <br />wind measurements, and (redundant) air temperature observations. - <br /> <br />The automated seeding system had some problems, but they are considered minor and easily correctable. <br />The system generally functioned very well, especially considering that no visits were made to the <br />dispensers once testing started. Some improvements should be made in the data logger program. A more <br />rigid holder for the propane stream temperature sensor would eliminate the cycling problem experienced <br />by the Bald Mountain dispenser. <br /> <br />It is recommended that future use of an automated propane dispenser system use simplified criteria. The <br />presence of SL W would continue to be measured by a Rosemount icing rate device well ~p the windward <br />slope. Seeding would commence as soon as the first Rosemount cycle occurred. Seeding would continue <br />for some time (about 2 h) after the last Rosemount cycle in an episode. Wind speed and direction could <br />be monitored but are not believed es~ential because SL W rarely occurred unless wind speed and direction <br />were appropriate for targeting the Wasatch Plateau. (It is anticipated that most north-south oriented <br />mountain ranges would experience similar conditions.) Some propane would be released during <br />essentially unseedable conditions if only SL W presence/absence was used to control seeding. However, <br />the amount of wasted propane is expected to be minor. <br /> <br />A thermoelectric generator-battery-inverter combination, as used at the HAS in early 1994, is a practical <br />means of powering a Rosemount icing rate device, a data logger/controller, a propane dispenser and radio <br />gear at an exposed remote location in all weather conditions. This system could be the master station <br />controlling a number of satellite dispensers located at similar high altitude sites crosswind of the master <br />station. All sites should be chosen where local SL W production is expected. If one wanted to be sure that <br />SL W existed at each dispenser, each site could monitor SL W with a Rosemount device. This would be a <br />superior but more costly approach. <br /> <br />Propane dispenser testing in California and Utah in recent years has demonstrated the feasibility of a <br />completely automated system that is both reliable and economical. Analysis of the early 1994 physical <br />. seeding experiments should improve understanding of the snowfall-enhancing capability. of propane <br />seeding. Prior research leaves no doubt that propane seeding can markedly enhance ice crystal <br />concentrations with liquid cloud at or below 0 oC. However, it is recommended that the ice crystal yield <br />of the currently-used (in Utah) propane nozzle and release rate be documented. The previously-cited yield <br />values of 1011 to 1012 ice crystals per gram of propane are based on investigations done over two decades <br />ago. These studies used different release rates and nozzles than recently used in California and Utah. It is <br />of obvious interest to test the current design to determine whether yield value are as high as expected. <br /> <br />, . <br /> <br />Additional key questions to be answered concern ice crystal growth and fallout times downwind of <br />propane dispenser sites. To be effective, propane dispensers need to be within SL W cloud, or at least not <br />far below SLW cloud base where saturation with respect to ice exists. This requires that dispensers be <br />located well up the windward slopes of mountain barriers. Such siting limits the time ( distance) available <br />for ice crystal growth to snowflake sizes-and fallout to the mountain surface. There is concern that this <br />time (distance) may frequently be too limited for significant snowfall to occur before the seeded ice <br />crystals are carried into the lee subsidence zone where sublimation and evaporation occur. <br /> <br />, . <br /> <br />Another concern with high altitude releases of propane (or AgI) is that crosswind dispersion may be <br />limited, requiring that the crosswind spacing of generators also be limited to avoid unseeded "gaps" <br />between seeding plumes. It may be possible to have greater spacing between AgI generators located <br />further down slope or in upwind valleys thereby requiring fewer seeding sites. Of course, use of lower <br /> <br />67 <br /> <br />L <br /> <br />
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