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<br />Hydrology <br /> <br />j <br /> <br />WATER SUPPLY <br /> <br />" <br /> <br />"'. . <br /> <br />The water supply analysis covers the 33-year study period, <br />1925-1957, which was judged to be indicative of future conditions, <br />At the gaging station, Purgatoire River at Trinidad, uninterrupted <br />records of stream flow are available for the entire study period. <br />Flows at this site, consisting of runoff from the 795 square miles <br />in the basin above the gaging station, are considered representative <br />of future inflow to Trinidad Reservoir. The annual flow at this <br />station by water years ranged from 16,300 in 1951 to 197,300 acre- <br />feet in 19~2, The average annual water year flow for the study <br />period was 62,100 acre-feet, Flows of like magnitude and variability <br />are expected to occur in the future. <br /> <br />WATER RNl,UIREMENTS <br /> <br /> <br />Much of the irrigation water supply comes from spring snowmelt <br />runoff or from summer rain storms which usually occur when available <br />supplies exceed the.requirements. The water supply is very erratic, <br />with considerable variation by season and from year to year, Usually <br />only a small portion of the water needed late in the growing season <br />is available. <br /> <br />, -".-.1 <br /> <br />Table 3 shows the computed average annual water requirements <br />for the Trinidad Project, based upon the period 1925-1957. <br /> <br />...;;" <br /> <br />Table 3. --Average annual water requirement <br /> <br />Item <br /> <br />Acre-feet <br />per acre <br /> <br />Project total <br />(19,717 acres) <br /> <br />. ,....,. <br />>~, .;. ';~/ .: <br /> <br />Consumptive use requirement of crops '!:I <br />Less effective precipitation <br />Crop irrigation requirement <br />Add farm losses (30%) <br />Farm delivery requirement <br />Add canal and lateral losses C3~) <br />Diversion requirement at main canal <br />headgates <br /> <br />2.30 <br />0.78 <br />1.52 <br />0.65 <br />2.17 <br />0.93 <br /> <br />3,10 <br /> <br />61,200 <br /> <br />'!:I Computed by Lowry-Johnson method <br /> <br /> <br />13 <br />