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<br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />3 <br /> <br />I <br />I <br /> <br />PROJECT HISTORY <br />Early in 1976, the Utah Division of Water Resources entered into a <br /> <br />contract with the Bureau of Reclamation (now The Water and Power Re- <br /> <br />sources Service). The purpose of that contract was to provide infor- <br /> <br />mation for an environmental impact statement for winter cloud seeding to <br /> <br /> <br />augment snowpack in the Upper Colorado River Basin. The contract also <br /> <br /> <br />called for formulation and testing of hypotheses related to the poten- <br /> <br /> <br />tial impact of increased snowpack on regional vegetation. The con- <br />. . I <br /> <br />tractor was also to recommend monitoring procedures for long-term cloud <br /> <br />seeding research in the Upper Colorado River Basin with particular <br /> <br />emphasis on the Uinta Mountains of Utah. On May 1, 1976, the Utah <br /> <br />Division of Water Resources formalized a subcontract with K. T. Harper <br /> <br />of Brigham Young University. <br />Earlier research programs funded by the Service concentrated on the <br /> <br /> <br />potential impact of winter snow augmentation in the Medicine Bow Moun- <br /> <br /> <br />tains of southeastern Wyoming and the San Juan Mountains of southwestern <br /> <br /> <br />Colorado. The results of those ~tudies have been reported by Knight et <br /> <br /> <br />al. (1975) and Steinhoff and Ives (1976). The work done by Brigham <br /> <br /> <br />Young University has focused on the northern slope of the Uinta Moun- <br /> <br /> <br />tains, northeastern Utah. The relationship of late lying snow to the <br /> <br /> <br />plant cover of four major ecosystem was studied during the snow melt and <br /> <br /> <br />growing seasons of the years 1976-79. Also, the distribution patterns <br /> <br /> <br />of precipitation in the Uintas and the relationship of snowpack to <br /> <br /> <br />runoff in nine major watersheds were analyzed. <br /> <br />I <br />I <br />I <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />