Laserfiche WebLink
<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />Abstract <br /> <br />This Final Report presents the first results ofthe Desert Research Institute's analysis of data <br />sets from the 1994 ~OA.A..-Ctah \\inter field program. The program is a cooperative research effort <br />bet\\"een the State of Ctah and the ~ational Oceanic and Atmospheric Administration within the <br />Atmospheric ~lodification Research Program, and is aimed at evaluating the weather modification <br />techniques currently used in the winter sno\\fall augmentation project conducted operationally by <br />the State of Utah. The problems addressed in the 1994 field program on the Wasatch Plateau of <br />central Ctah were: 1) the transport and dispersion of seeding material into clouds over the plateau~ <br />2) the evolution of supercooled liquid water in winter storms atTected the plateau~ and 3) the <br />detection of the physical effects of seeding orographic clouds using silver iodide and liquid propane. <br />The DR! work focussed mainly on the latter 1\\'0 areas of research. <br />In addition to analysis of seeding experiments, this report presents summaries of the storms <br />which affected the \Vasatch Plateau be1\\'een 15 January and 15 March 1994. The synoptic <br />characteristics of five storm periods covering 11 separate days are described. The bulk of the cloud <br />seeding experiments were conducted during a period from 18 to 22 February, when a relatively cold <br />air mass had settled into the Great Basin. Distinct weather episodes were produced by a series of <br />short waves mo\'ing through the mean trough positioned over the western U.S. The \Vasatch Plateau <br />\"'as generally to the north of the jet stream in this situation, where winds were southwesterly to <br />westerly and relatively light. The temperature at the top of the plateau, near the 700 mb level, was <br />often colder than -8" C, and supercooled liquid water was consistently present in small amounts, <br />but over lengthy time periods. The winds, temperatures and liquid water conditions were frequently <br />conducive to seeding \\lth silver iodide. <br />The results from three case studies are presented. The first on 26 January 1994 demonstrates <br />a new technique for studying ground seeding plumes using tv\o'O mobile instrument platforms~ one <br />equipped with aerosol sampling equipment and a laser imaging probe, and the second a mobile <br />radiometer. The results of tandem passes through seeding plumes are described, vvith the main result <br />in this case being that supercooled liquid water was apparently not significantly depleted at the <br />position the plumes were intercepted a few kilometers downwind of the seeding generators. <br /> <br />11 <br />