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<br />4$01 <br /> <br />. <br /> <br />. <br /> <br />17. CLIMATOLOGY.- Wide variations of climate occur in the Arkansas <br />Basin above Pueblo darnsite. In the mountainous regions of the headwaters <br />precipitation varies widely over relatively short distances. It varies <br />from 10 inches annually in some locations to 40 inches annually over <br />limited areas. Much of the total precipitation at the higher elevations' <br />is in the form of snow. Runoff from snowmelt constitutes a dependable <br />water supply for municipal, irrigation, industrial, and other uses. In <br />the plains region most of the precipitation is in the form of rainfall. <br />At times, occurrences in the form of violent cloudbursts cause flash <br />floods of short durations and small volumes but of damaging intensities. <br />More than 80 percent of the average annual precipitation on the plains <br />occurs during the period April through October, <br /> <br />" <br /> <br />18. Annual precipitation normals within the watershed vary from <br />24.27 inches at Lake Moraine to 9.69 inches at Buena Vista. During <br />the six-month period, April through September, Lake ~loraine gets 76 per- <br />cent of the annual normal, and Buena Vista gets 68 percent. The maximum <br />rainfall months are Nay and July throughout most of the basin. Thunder- <br />storm activity is greatest in July with an average of 13 days at Pueblo. <br />A maximu," 24-hour, or maximum observed day precipitation of 6.10 inches <br />occurred at Rye, Co 1 0" in ~lay 1955. The June 1965 storm produced a <br />maximum 24-hour precipitation amount of 11,08 inches at Holly, Colo. <br /> <br />19. ~Iean annual sno\<fall amounts vary from 146 inches at Lake <br />Moraine to 33 inches at Canon City. Pueblo Weather Bureau Airport has <br />had a maximum month ly sno\<fall of 29.3 inches, and a maximum 24-hour <br />amount of 16.8 inches. ~fonth ly and annual precipitation normal s for <br />representative weather stations in and adjoining the Arkansas \<ater- <br />shed above John clartin Darn are tabulated in table 1. Locations of <br />weather stations are shown on plate 2. <br /> <br />20. There is a wide variation of temperatures in the Arkansas <br />Basin above the Pueblo damsite. This is due principally to the varia- <br />~ - - - - -, -tion--in-altituae-;-Leaavi11e;- aCelevatTonro-;-r77-feet, nas-a mean annual - - -- <br />maximum and minimum of 50.7 and 21.9 degrees, respectively; whereas <br />Pueblo at elevation 4,700 feet has a mean annual maximum and minimum,of <br />68.0 and 37.3 degrees, respectively. Extreme temperatures have ranged <br />from 105 degrees at Pueblo to a -54 degree" at Westcliffe, elevation <br />7,860 feet. The average last spring occurrence of 32 degrees varies <br />from 28 April at Pueblo Weather Bureau Airport to 24 June at Lake ~Ioraine. <br />TIle average first fall occurrence of frost at the same locations are <br />12 October and 23 August. <br /> <br />j <br /> <br />21. Relative humidity records are available for only one station <br />in the vicinity of the Pueblo project. The Pueblo Weather Bureau Air- <br />port record shows average relative humidities at 5:00 a.m., 11:00 a.m., <br />5:00 p,m., and 11:00 p.m. to be 65, 38, 41, and 61 percent, respectively. <br /> <br />6 <br />