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<br />I <br /> <br />I <br /> <br />is a vertical cross section whose plane runs through HAS and GTR. Considerable previous plume <br />tracking had shown that plumes released from the seeding site routinely passed the TAR vicinity when <br />winds there were from the southwest quadrant. Pairs of EUs, one seeded and one not treated by random <br />decision, were declared whenever an icing rate sensor at the HAS seeding site detected the presence of <br />SL W above a threshold. It is well documented that SL W availability is the necessary "raw material" for <br />winter cloud seeding in mountains to be effective. Randomized seeding and all observations were totally <br />automated providing 24/7 operations to maximum the population of EUs. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />3000 - <br />MeIers <br /> <br /> <br />- 3000 <br /> <br />I <br /> <br />2000 - <br />Fairview (1829) <br /> <br />Wasatch Plateau <br /> <br />I <br /> <br />2000 <br /> <br />,Sanpete Valley <br /> <br />I <br /> <br />1000 <br /> <br />1000 <br /> <br />I <br /> <br />Sea . ' <br /> <br /> <br />I <br /> <br />Level <br /> <br />K1klmelers <br /> <br />I <br /> <br />2 <br /> <br />4 <br /> <br />6 <br /> <br />8 <br /> <br />10 <br /> <br />12 <br /> <br />14 <br /> <br />16 <br /> <br />Vertical:Horizontalscale = 3:1 <br /> <br />Fig. 2. Vertical cross section through HAS and GTR showing relative locations of instrumented sites, <br /> <br />I <br /> <br />Primary measurements for statistical evaluation of seeding effectiveness were from high resolution <br />precipitation gauges manufactured by ETI Instrument System, Inc. Gauges were equipped with Alter <br />windshields and were located in natural clearings in conifer (evergreen) forest to minimize wind-caused <br />undercatch of snowfall. The snow melted in an antifreeze solution within each gauge and resulting <br />weight changes were measured by a sensitive load cell. A Campbell data logger within the gauge housing <br />recorded the average weight for each minute. Each gauge was individually calibrated and its coefficients <br />were incorporated into the data logger program. The highly sensitive gauges proved to be very reliable, <br />resulting in no missing data for any EU period at any gauge. Data from gauge data loggers were <br />downloaded into a Palm Pilot device during approximately weekly visits. A running mean of five was <br />fitted to aliI min gauge samples, centered on the middle minute, before calculations ofSWE <br />accumulations. Examination of resulting smooth time history plots suggests that gauge resolution was <br />between 0.002 and 0.003 inch. While scientific papers usually report precipitation in metric units, the <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />5 <br /> <br />I <br />I <br />