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<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 />CHAPTER II - WATER SUPPLY - INVENTORY AND ANALYSIS <br /> <br />General <br /> <br />The White River rises in the Flattops area of northwestern Colorado and <br />flows westward into Utah where it joins the Green River. The drainage basin <br />in Colorado totals about 3700 square miles, ranging in altitude from <br />approximately 4950 feet at the state line to over 11,500 feet in the <br />headwaters. Water supply for the Yellow Jacket Project will come entirely <br />from the North Fork of the White River. The North Fork drainage area covers <br />254 square miles, approximately 94 percent of which lies within the Routt <br />and White River National Forests. <br /> <br />The annual flow of the White River at the state line is <br />503,000 acre-feet. Water use within the basin has not changed <br />during the past 40 years. The primary use is the irrigation of <br />acres of land. <br /> <br />approximately <br />significantly <br />about 32,000 <br /> <br />The White River is typical of major rivers in Colorado in that the majority <br />of the annual runoff volume results from snowmelt during the spring and <br />early summer months. Historic water use in the basin was for the production <br />of hay, small grains, and pasture. Large land areas can be irrigated <br />through direct river diversion without the need for regulating storage since <br />snowmelt runoff occurs during the time of greatest agricultural demand. <br />However, irrigation demands have grown and have created shortages during the <br />summer months of drier years. It is apparent that any, new water project <br />requiring a significant amount of water must include a storage reservoir. <br /> <br />Water Availability <br /> <br />Table 11-1 presents the average annual runoff of the White River at various <br />locations in the basin. As illustrated in this table, there is a <br />significant decrease in the water yield per unit area in the lower basin due <br />to major topographic and climatologic differences. These effects produce an <br /> <br />11-1 <br />