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<br />. <br /> <br />Table 6 <br />South Platte River Travel Times <br /> <br />From Chatfield Dam <br /> <br />Elapsed Time <br />(hours) <br /> <br />To Denver Gage <br />To Henderson Gage <br />To Kersey Gage <br />To Weldona Gage <br />To Balzac Gage <br /> <br />9 <br />15 <br />33 <br />45 <br />60 <br /> <br />The routings were done on a mean daily basis. The longest period <br /> <br /> <br />averaged was a 2-day mean. .The routed holdout values were used <br /> <br /> <br />to adjust the natural flood peaks using a mean discharge-peak <br /> <br /> <br />relationship. Holdouts were based on a reservoir system release <br /> <br /> <br />criteria which assumed that reservoir outflow would be shut down <br /> <br /> <br />to zero when the Denver gage indicates a flow of 5,000 cubic feet <br /> <br /> <br />per second. This theoretical operation of the South Platte reser- <br /> <br /> <br />voir system affected peak flows occurring in 1912, 1914, 1921, 1933, <br /> <br />1935, 1942, 1947, 1949, 1957, 1965, 1969 and 1973. The adjustments <br /> <br /> <br />are illustrated on plates 18 through 20 where the magnitude of the <br /> <br /> <br />actual event is plotted at the frequency occupied by the modified <br /> <br /> <br />flow. Although these studies indicated an apparent controlling <br /> <br /> <br />effect at the gaging stations downstream from Kersey, it was so <br /> <br /> <br />slight that it was considered negligible and no gaging station <br /> <br /> <br />flows were adjusted past that point. <br /> <br />DISCHARGE-PROBABILITY CURVES <br /> <br />Discharge-probability curves were developed from the adjusted <br /> <br /> <br />gaging records discussed above. Although the statistical techniques <br /> <br /> <br />used varied somewhat from station to station, they were all based <br /> <br /> <br />on a log Pearson Type III distribution. A top half analysis was <br /> <br />. <br /> <br />32 <br />