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'0" . .' ,. . . ',: .-, . ";f;; .. .,. . '.... --. .. ....';..'. <br />~ . ,,. .-_,_ .......~". .~.,.~.A.'Ct....,...'* ~,... ,.-,#1'11 _.., _ . ..,.8....., . <br />~:.:...:~..~~ .:r'a.:"; 6~--.;,..~......:-:-......:_:-:..;,.....___:O:,:~,~.-.;..~..~:...:.~..:~:.:;;..,~"., <br />,"- ....'-T'......, , ".' .. <br />",_a. ,_ :.,.... ;-e,. .. ....;~~:QJ.....;..o <br /> <br />Figure 5. Thirty second "snapshots" of2D-C ice crystal irnages during times of peak ice particle concentration for 3 adjoining <br />EUs used in the case study of21 December 2003. The strip widths are 800 rnicrons, the field of the 2D-C probe. Measurements <br />along the wind are unlimited. The upper and lower panels show typical 2D images ofnaiural snowfall while the central panel <br />shows seeded ice crystals. Mean ice particle concentrations for the 3 periods from top to bottom are 67, 148 and 28 per liter. <br /> <br />While such rates are light snowfall, about half of all <br />hours with detectable natural snowfall fall at the rate <br />of 0.0 1 0 inch per hour or less in the experimental <br />area. Frequent hours with light snowfall are common <br />at higher elevations in the Intermountain West. The <br />seasonal contribution of light snowfall is important <br />because of its high frequency of occurrence. <br />Increasing the snowfall rate by 0.010 inch per hour <br />for 200 hours would result in a seasonal increase of <br />10% for a normal November through March winter, <br />based on long-term snow pillow observations in the <br />experimental area. Examination of past icing rate <br />sensor and other SL W data from the Wasatch Plateau <br />revealed that approximately 200 hours with available <br />SLW could be expected during a typical November <br />through March winter. Consequently, there is both <br />statistical and physical support for the expectation <br /> <br />that propane seeding might produce an all winter <br />SWE increase in the vicinity of 10% for the limited <br />target area examIned. <br /> <br />Consideration of Ice Particle Concentrations <br /> <br />Ice particle concentrations (IPCs) of smaller ice <br />crystals were monitored at the TAR with a 2D-C <br />particle imaging probe. Only 21 seeded and 22 <br />nonseeded EUs had available 2D-C measurements <br />and HAS wind directions suitable for targeting <br />because of electrical generator and other problems. <br />The IPCs were compared for these seeded and <br />nonseeded sample populations which may not be <br />totally representative of all 69 EUs meeting the HAS <br />wind direction criterion. The comparison ofthe <br />seeded and nonseeded samples revealed about a 1/3 <br /> <br />10 <br /> <br />