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Climate <br />Summers are warm or hot in most of the valleys in <br />the survey area but are much cooler in the mountains. <br />Winters are cold in the mountains. Valleys are colder <br />than the lower slopes of the ad}acent mountains <br />because of cold air drainage. Precipitation occurs in the <br />mountains throughout the year, and enough snowpack <br />accumulates during winter to supply sufficient water for <br />agriculture in most areas and to supply dowristream <br />users. In the valleys, summer precipitation falls as <br />showers, and some thunderstorms occur. In winter the- <br />snow cover in unshaded areas of valleys and on south- <br />tacing mountain slopes often melts within a few days of <br />snowfall. <br />Table 1 gives data on temperature and precipitation <br />for the survey area as recorded at Canon City and <br />Salida, Colorado, for the period between 1951 and <br />198D. Table 2 shows probable dates of the first freeze <br />in fall and the last freeze in spring. Table 3 provides <br />data on length of the growing season. <br />In winter, the average temperature is 38 degrees at <br />Canon City and 30 degrees at Salida. The average <br />daily minimum temperature is 24 degrees at Canon City <br />and 14 degrees at Salida. The lowest temperature on <br />record, which occurred at Salida on February 1, 1951, <br />is -33 degrees. In summer, the average temperature is <br />73 degrees at Canon City and 64 degrees at Salida. <br />The average daily maximum temperature is about 84 <br />degrees. The highest recorded temperature, which <br />occurred at Canon City on July 11, 1954, is 107 <br />degrees. <br />Growing degree days are shown in table i. They are <br />equivalent to "heat units." During the month, growing <br />degree days accumulate by the amount that the <br />average temperature each day exceeds a base <br />temperature (40 degrees F). The normal monthly <br />accumulation is used to schedule single or successive <br />plantings of a crop between the last freeze in spring <br />and the first freeze in fall. <br />The total annual precipitation is about 13 inches at <br />Canon City and 11 inches at Salida. Of this, 65 percent <br />usually falls in April through September. The growing <br />season for most crops falls within this period. The <br />heaviest 1-day rainfall during the period of record was <br />2.74 inches at Canon City on May 18, 1955. About <br />1.75 inches fell at Salida on October 29, 1961. <br />Thunderstorms occur on about 60 days each year. <br />Average seasonal snowfall is about 37 inches at <br />Canon City and 52 inches at Salida. The greatest snow <br />depth at any one time during the period of record was <br />25 inches at Canon City and 42 inches at Salida. On <br />the average, at least 1 inch of snow is on the ground for <br />2 days at Canon City and for 6 days at Salida each <br />year. The number of such days varies greatly from year <br />to year. <br />Average relative humidity in midafternoon is about 40 <br />percent. Humidity is higher at night, and the average at <br />dawn is about 60 percent. The sun shines about 80 <br />percent of the time possible in summer and 75 percent <br />in winter. The prevailing wind is from the north- <br />northeast. Average windspeed is highest, about 12 <br />miles per hour, in spring. <br />