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<br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br /> <br />mile contributing drainage area using the hypothetical storm record in the HEC-I program. The <br />duration depths required for the HEC-I analysis were computed using the methodology published <br />in NOAA Atlas n, Volume m. The 24-hour rainfall was applied uniformly to each subarea in the <br />watershed using a triangular (critical) distribution pattern which places the peak intensity at the <br />center of the storm and the remaining increments so that they ascend in magnitude to the peak and <br />descend in magnitude to the end of the storm. <br /> <br />InfIltration Rate Calibration <br /> <br />. To determine appropriate infiltration rates, the Albuquerque District generated a HEC-l <br />watershed model for Bear Creek, a tributary to the Los Pmos River, and calibrated the HEC-I model <br />to peak discharges calculated from regional equations presented in U.S. Geological Survey Water- <br />Resources Investigations Report 96-4112, Analysis of the Magnitude and Frequency of Peak <br />Discharge and Maximum Observed Peak Discharge in New Mexico (1996). The following regional <br />equations presented in Report 96-4112 were developed for the northwest plateau region of New <br />Mexico including the San Juan River watershed in southwestern Colorado: <br /> <br />Q(50.0%)= 8.47 X 101 x A 0.47 <br />Q(20.0%)= 1.97 X 102x A 0.46 <br />Q(lo.O%)= 3.06 X 102x A 0.46 <br />Q(4,0'/") = 4.86 x I 02X A 0.45 <br /> <br />Q - 6 54 02 0.45 <br />(2.0%) -. x I x A <br />Q = 8 53 X 102x A 0.45 <br />(1.0%) . <br />Q(0.2%) = 1.45 x 101X A 0.45 <br /> <br />To simulate a critical storm, the rainfall in the HEC-I was reduced for the 19-square-mile <br />drainage area of Bear Creek. Based on this analysis, the Albuquerque District adopted infiltration <br />amounts and applied the infiltration rates to the HEC-I model for the Los Pinos River watershed <br />above Bayfield. The infiltration amounts for each frequency are listed in Table 2. <br /> <br /> TABLE 2 <br /> INFILTRATION RATES <br /> Initial Loss Rate Above Bayfield Uniform Loss Rate for Entire <br />FREQUENCY Watershed <br /> (in/hr) (in/hr) <br />1O.0o/...Chance (10-year) 1.035 0.30 <br />4.0%-Chance (25-year) 1.217 0.30 <br />2.0o/...Chance (50-year) 1.340 0.30 <br />1.0o/...Chance (IOO-year) \.379 0.30 <br />0.2o/...Chance (500-year) 1.435 0.30 <br /> <br />4 <br />