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<br />I <br />I <br />I <br />I <br />I <br />I <br /> <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 />D. <br /> <br />nn0994 <br /> <br />C. <br /> <br />: ~;:....~, <br />Climate <br /> <br /> <br />Mos~of the Uncompabgre Valley is semiarid, but rainfall and <br /> <br /> <br />temperature vary widely with elevation. Tbe prevailing wind <br /> <br /> <br />is from tbe west, but a wide range of surface wind condi- <br /> <br /> <br />tions exists as influenced by specific topographic features. <br /> <br /> <br />Average annual precipitation ranges from 8 inches at Delta <br /> <br /> <br />and 13 inches in tbe upper valley south of Montrose to as <br /> <br /> <br />much as 110 inches in tbe mountains. The frost-free period <br /> <br /> <br />averages about 127 days annually and varies from 112 days in <br /> <br /> <br />the upper valley to 1118 days in the lower valley area.1 <br /> <br />Water Quality ~ Salinitv <br />As a part of the Colorado River Water Quality Improvement <br /> <br />Program (CRWQIP) 1, the U.S. Department of tbe Interior <br /> <br /> <br />Bureau of Reclamation prepared a feasibility report and <br /> <br /> <br />draft environmental impact statement to determine a feasible <br /> <br /> <br />plan for improving the water quality in the Lower Gunnison <br /> <br /> <br />Basin Unit which includes the Uncompahgre River Valley. The <br /> <br /> <br />intent of the Lower Gunnison Basin Unit investigations, com- <br /> <br /> <br />pleted in December 1982, was to determine a feasible plan <br /> <br /> <br />for improving tbe quality of water in tbe Uncompabgre River, <br /> <br /> <br />a tributary of tbe Gunnison River which in turn flows into <br /> <br /> <br />the Colorado River. Tbe large amount of salt pickup is <br /> <br /> <br />attributable to conveyance system seepage and deep percola- <br /> <br /> <br />tion as the water passes through the weathered and fractured <br /> <br /> <br />E-8 <br />