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EXHIBIT K <br />CLIMATE AND AIR QUALITY <br />K.1 INTRODUCTION <br />The project is located in a semi-arid, continental climatic region which is <br />characterized by warm summers and dry winters. Sunny days, clear nights, <br />little precipitation, extreme evaporation, and large diurnal temperature <br />changes predominate. The region's complex topography causes considerable <br />variation in site-specific temperature, precipitation, and winds. These <br />influences are less on the plateaus than down in the valleys. <br />K.2 CLIMATOLOGY AND ~4IR QUALITY OF THE PROJECT AREA <br />The climatology of the site is a function of location and elevation. The <br />growing season is approximately 100 days long with a frost-free period of <br />about 60 days. In winter, the average temperature is 20 to 24°F, and the <br />average daily minimum is 5 to 10°F. In summer, the average temperature is <br />i 63 to 69°F, and the average daily maximum is 83 to 88°F. <br />The average annual precipitation is approximately 17 inches, with about 55 <br />percent falling during the period of April through September. About 35 <br />thunderstorms occur faach year, 21 of which are in the summer. Average <br />seasonal snowfall is 40 to 80 inches. The greatest snow depth at any one <br />time during the period of record was 30 inches. On an average of 15 to 30 <br />days, at least 1 inch of snow is on the ground. The number of such days <br />varies greatly from year to year (SCS 1982). <br />The average relative humidity in mid-afternoon is less than 33 percent in <br />spring, and is about 44 percent the rest of the year. Humidity is higher at <br />night year-round, and the average at dawn is about 59 percent. The sun <br />shines 17 percent of t:he time possible in summer, and 61 percent in winter. <br />The prevailing wind is from the southwest, averaging about 7 miles per hour. <br />However, the surface wind patterns are almost entirely dependent on local <br />terrain and ground cover. Gentle air inversions are common at night, and <br />cool air tends to drain into the valleys (SCS 1982). <br />K-1 <br />