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<br />ORA F T <br /> <br />several research projects by Vardiman and Moore 14/ defined the major <br /> <br />, <br />characteristics and developed generalized criteria for winter cloud <br /> <br />. <br /> <br />seeding. These criteria provided much of the technical basis for the <br />large operational seeding programs in Colorado and Utah from 1976 <br /> <br />and added to the scientific basis for increased confidence <br /> <br />in weather modification. <br /> <br />The estimated seeding effect of 10 to 20 percent should cause an <br /> <br />average of 2 to 4 inches more winter precipitation in the Colorado <br /> <br />Basin mountains which relates to about 20 to 48 inches more snowfall <br /> <br />and generally 6 to 15 inches more snowpack. <br /> <br />There have been three well-documented studies estimating the average <br />annual water augmentation potential for seeding in the upper Colorado <br />River Basin. <br /> <br />October 1967 - Bureau of Reclamation 15/ <br /> <br />- 1,870,000 acre-feet <br /> <br />May 1972 <br />May 1973 <br /> <br />- Stanford Research Institute 16/ - 2,300,000 acre-feet <br /> <br />- North American Weather <br /> <br />- 1,315,000 acre-feet <br /> <br />Consultants 17/ <br /> <br />." <br /> <br />The Stanford Research Institute study estimated 1,200,000 acre-feet <br />would also be produced outside the Colorado Basin by seeding within <br />the Basin. The NAWC (North American Weather Consultants) study along <br /> <br />'" <br /> <br />15 <br />