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<br />States, Atlas 2, Volume III, Colorado, published by the National Oce- <br /> <br />anic and Atmospheric Administration (NOAA) in 1973. In each case, a <br /> <br /> <br />50o-year value was estimated by extrapolating the selected Atlas values <br /> <br /> <br />on semilogarithmic paper. Adjustments for depth-area were based on the <br /> <br />depth-area relationship presented in the NOAA publication. Adjustments <br /> <br /> <br />for length of record were made on logarithmic-probability paper using <br /> <br /> <br />Beard's table of expected probability adjustments for various lengths <br /> <br /> <br />of record. The spatial variation of the rainfall potential shown in <br /> <br /> <br />the Atlas for the Cache la Poudre River basin was simulated in the <br /> <br /> <br />MITCAT model through the introduction of several hyetographs. The time <br /> <br /> <br />variation of the 6-hour rainfall for each hyetograph was based on a <br /> <br /> <br />study of hourly precipitation data recorded during major storms in the <br /> <br /> <br />South Platte River basin and refined to 30-minute values by using Civil <br /> <br /> <br />Works BuLetin 52-8, Plate No. 11 (1952) as a guide. The 6-hour <br /> <br /> <br />distribution is given in table 2 below. <br /> <br />. <br /> <br />Table 2 <br />6-Hour Rainfall Distribution <br /> <br />End of Period <br />(minutes) <br /> <br />Percent of 6-Hour <br /> <br />30 <br />60 <br />90 <br />120 <br />150 <br />180 <br />210 <br />240 <br />270 <br />300 <br />330 <br />360 <br /> <br />2 <br />4 <br />4 <br />5 <br />9 <br />10 <br />40 <br />10 <br />6 <br />4 <br />4 <br />2 <br /> <br />LOSSES <br /> <br />The Soil Conservation Service (SCS) curve number technique was used <br /> <br /> <br />to model infiltration in the MITCAT model. A general soil map of Larimer <br /> <br />. <br /> <br />12 <br />