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<br />States, Atlas 2, Volume III, Colorado, published by the NOAA in 1973. <br /> <br /> <br />The 500-year value was estimated by extrapolsting the selected I-hour <br /> <br /> <br />values on semilogarithmic paper. Adjustments for depth-area were based <br /> <br /> <br />on the depth-area relationship presented in the NOAA publication. <br /> <br /> <br />Adjustments for an average length of record of 40 years were made on <br /> <br /> <br />logarithmic-probability paper using Beard's table of expected <br /> <br />probability adjustments. The I-hour rainfall distribution developed <br /> <br /> <br />from NOAA criteria is given in table 18. <br /> <br />. <br /> <br />Table 18 <br />I-Hour Rainfall Distribution <br /> <br />End of Period <br />(minutf's) <br /> <br />Incremental Rainfall <br />(percent) <br /> <br />5 <br />10 <br />15 <br />20 <br />25 <br />30 <br />35 <br />40 <br />45 <br />50 <br />55 <br />60 <br /> <br />3 <br />4 <br />4 <br />5 <br />12 <br />16 <br />29 <br />12 <br />5 <br />4 <br />4 <br />2 <br /> <br />LOSSES <br /> <br />Infiltration rates for the Sheep Draw basin were obtained from <br /> <br /> <br />Soil Resources of Colorado, Region 2 - Larimer and Weld Counties, <br /> <br />published in 1976 by the CSU Expel'iment Station, Fort Collins, and the <br /> <br /> <br />SCS. A general soil map of Weld County used in conjunction with table <br /> <br /> <br />3 of the CSU publication lists ranges of infiltration permeabilities <br /> <br /> <br />for each soil series. Table 19 contains the soil associations that <br /> <br /> <br />were taken from the general soil map, the range of infiltration <br /> <br /> <br />permeabilities at various depths for each soil series, and the <br /> <br />infiltration rate that was used in the SWMM model. <br /> <br />. <br /> <br />42 <br />