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Last modified
7/28/2009 2:36:15 PM
Creation date
4/16/2008 10:09:04 AM
Metadata
Fields
Template:
Weather Modification
Contract/Permit #
NOAA/NA-81-RAC-00023
Title
Evaluation of the Utah Operational Weather Modification Program - Final Report
Date
4/1/1982
Weather Modification - Doc Type
Report
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<br />~ . .r' ~.~.! <br /> <br />ABSTRACT <br /> <br />This study is an evaluation of a winter orographic cloud seeding <br />project in Utah. The evaluation is based upon both intensive field <br />me asurement sand h is toric~l records. For the fie ld measurements, <br />ground and airborne data were collected during February and March, 1981 <br />in the vicinity of the Tushar Mountains. <br /> <br /> <br />In evaluating the physical data three aspects are emphasized: the <br />dispersal of artificial ice nuclei, the distribution of supercooled <br />liquid water, and the growth and trajectories of precipitation. <br /> <br />Ground based measurements were made by K and X band radars, a dual <br />frequency microwave radiometer, a network of precipitation gages, an ice <br />nucleus counter, radiosonde/cloudsonde instruments and other standard <br /> <br />measurements. <br /> <br />Airborne data were obtained from the University of Washington's <br />cloud physics aircraft. Instrumentation consisted of five ice particle <br />probes (PMS), a Johnson-Williams and a Rosemount liquid water meter, an <br />ice nucleus counter, and other devices for reference such as altitude, <br />airspeed and position. <br /> <br />Results derived from these data indicate that ice nuclei released <br />from ground based generators did not generally. reach cloud alt itudes in <br />sufficient quantity for effective nucleation and that the area covered by <br />the weak upper edges of the plumes was limited to the order of about 10% <br />of the barrier. <br /> <br /> <br />Supercooled liquid water was found to reach a maximum typically <br />just upwind of thp harr; pr crest. Amounts found during - the research <br />period were generally below that associated with. seeding opportunities, <br />but meteorological conditions at the time were unfavorable for the <br />development of greater liquid water concentrations. Relationships of <br />liquid water to other meteorological conditions are also investigated. <br /> <br />i <br />
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