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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />ENGINEERING METHODS <br /> <br />Hvdrolol!ic Analvsis <br /> <br />Flood peaks for the 10-, 50.., 100, and 500-year events for Henson Creek and Lake Fork <br />were analyzed comparing three statistical methods. The selected statistical method was <br />based on regional area analysis. For the FIR, it is assumed these flood peak estimates are <br />accurate, however, it should be noted the estimates are generally higher than those <br />obtained using more recent publications using regression based methods (CWCB, 1999, <br />and Vaill, 2000). In addition, drainage areas for Lake Fork used for the flood estimates <br />were slightly higher than those estimated for the current study, however, the change in <br />the magnitude of the 100-year flood peak is insignificant when the smaller drainage areas <br />are applied to the regression curve used in the original study. These flood peaks are <br />summarized in Table 1. <br /> <br />Table 1. Flood Peak Discharge Summary <br /> <br />Location/Design Flood Peak Dischar~e (cfs) <br />Point (DP) 10-year 50-year 100-year 500-year <br />Henson Creek <br />At Lake City 1400 2000 2300 3300 <br />(H1) <br />Lake Fork Gunnison River <br />County Line (L 1 ) 6400* <br />Lake City Below 3000 4800 5800 9500 <br />Henson Creek <br />(L2) <br />Lake City Above 2000 3100 3600 5600 <br />Henson Creek <br />(L3) <br /> <br />See Catchment Area Map for Design Points <br />* 100-year discharge obtained from the area/discharge regional discharge curve used for <br />the FIS (WestWater, 1985a); drainage area at Design Point L1 equals 269 sq. mi. <br /> <br />The FIRM identifies approximate floodplains for portions of Lake Fork, Henson Creek, <br />Cebolla Creek, Mineral Creek, Spring Creek, North Clear Creek, South Clear Creek, Rito <br />Hondo Creek, Big Spring Creek, Crooked Creek, Rio Grande River, Little Squaw Creek, <br />Squaw Creek, Weminuche Creek, Los Pinos River, Middle Fork Piedra River, East Fork <br />Piedra River, Piedra River, Williams Creek, and Weminuche River, a few unnamed <br />tributaries, and numerous reservoirs and lakes. Flood peaks discharges for the 100-year <br />were estimated for some of these streams at important design points using regression <br />equations developed by CWCB (CWCB, 1999). <br /> <br />7 <br />