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<br />2.2 PRECIPITATION DATA <br /> <br />Using TP-40 (USDOC, 1961), the USACE estimated 1-, 2-, 10-, 25-, 50-, 100-, and 500-year <br />(500-yr) point precipitation depths for durations of 15 minutes to 24 hours. Values for the 25- <br />and 100-yr return periods with some corrections are shown in Table 2. The 100-yr values <br />estimated from NOAA Atlas-2 (NOAA, 1973) are within 1 to 5 % of these values. Therefore, <br />the values shown in Table 2 are judged'to be reasonable and are used in this study, The 5-minute <br />precipitation depth is taken to be 0.37 times the 30-minute precipitation depth (USDOC, 1961). <br />The 48-hour precipitation depths shown in Table 2 are estimated from TP-49 charts (USDOC, <br />1964), <br /> <br />Table 2 <br />Point Precipitation Depths in Frenchman Creek Watershed <br /> <br />Duration Precipitation Depth (inches) <br /> 25-yr 100-yr <br />5 min. O,67a 0.87a <br />15 min. 1.31 b 1.69b <br />30 min. 1.82b 2.35b <br />1 hr, 2.30 3.02 <br />2 hrs. 2.61 3,27 <br />3 hrs 2,70 3,58 <br />6 hrs, 3.10 3,99 <br />12 hrs 3,50 4.40 <br />24 hrs, 3.84 4.93 <br />48 hrs 4,10 5.50 <br /> <br />a Taken to be 0.37 times the 30-minute precipitation depth (USDOC, 1961) <br />b Re-computed based on TP-40 charts and tables (USDOC, 1961) <br /> <br />2.3 HYDROLOGIC CHARACTERISTICS OF SUB-WATERSHEDS <br /> <br />To estimate Soil Conservation Service (SCS) curve numbers (CNs), the USACE used soils <br />information available in soils survey reports of the area (USDA, 1976) and divided the 19 sub- <br />watersheds into three categories with CN values of 72, 81, and 85, respectively. A value of 72 <br />was used for two sub-watersheds, 81 for seven sub-watersheds, and 85 for ten sub-watersheds <br />(See footnote b, Table 4), However, site inspections by USACE persollilel indicated that the <br />basin should have significantly higher infiltration than indicated by the Soil Survey Reports <br />(USDA, 1976) and that parts of the upper basin and large areas in surrounding basins dead end <br />behind stabilized dunes. This suggests that the CN values should be significantly lower. <br /> <br />The average annual surface runoff for the region is reported to be about 1,0 inch (Geraghty, et aI, <br />1973), The same average annual surface runoff is reported for northwestern Kansas and <br />southwestern Nebraska. The average annual precipitation in these three regions are 17.63 inches <br />at Holoyoke, Colorado; 16,88 inches at St. Francis (northwestern Kansas); and 18.29 inches at <br /> <br />Draft Letter Report <br />Independent Review of Hydrologic Analysis for Frenchman Creek <br />Contract No, DACW41-00-D-0026-0001 <br /> <br />Flood Plain Management Services Special Study <br />Holyoke, Colorado <br />June 18,2001 <br /> <br />Page 3 <br />