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<br />ORA F T <br /> <br />conditions. To recognize a seedable opportunity routinely, the <br />conditions must'be readily identifiable by standard observation <br />techniques. Past experiments have used indices (500-mb temprature <br />and cloud top temperature) that were easily identifiable but were <br />not good indicators of seeding opportunity or potential. Vardiman <br />and Moore have reanalyzed the results of seven winter seeding <br />programs in an effort to identify and generalize the key parameters <br />of these conditions into seedability criteria that are applicable to <br />a variety of meteorological and topographic conditions. They were <br />able to stratify the conditions into four physical categories. <br />These categories indicate the availability of water, nuclei, mixing, <br />and time 30/. <br /> <br />" <br /> <br />Each of these physical categories identified has a number of parameters <br />which were associated with or affected seeding results. In general, <br />cloud seeding can be expected to increase the amount of precipitation <br />produced when: (1) there is an abundance of moisture in the form of <br />supercooled liquid water, (2) there is a deficiency of natural ice <br />nuclei, (3) the air is unstable, (4) the time required for growth and <br /> <br />fi <br /> <br />42 <br />