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<br />Where relIable storm data Joes nUl exlS1, (he rrequen"y (;ulVe be(;umes the only data-basea LOol <br />to compare results. Basins where this is an issue are calibrated to minimize the sum of the <br />residual and the sum of the squared residual between the simul<iteP peak discharge and that of the <br />frequency curve for the 5- and 10- year flood. This ensure~e simulation ~, if unable to <br />exactly match the calibration points, will pass between them ~d be as close as possible. The <br />systematic records for most of these sites are eleven years. Short records increase the amount.of <br />sampling error when the frequency curve is e"trapolated much beyond twice the length of the <br />record. Given this, the 5- and I a-year floods should exhibit less variability than other points on <br />the frequency curve. <br /> <br />The multiple scenario simulation used to develop the limits of the frequency curve provide the <br />upper and lower limits of the 1 00 equally likely frequency curves. It is desirable to simulate <br />peak flows as close to the mean frequency curve as possible. The model simulation is deemed <br />good if the simulated peak falls within the bounds of the frequency ensemble for a given quantile <br />and questionable if the simulated peak is outside the ensemble but within the 95 percent <br />confidence limits. The model is deemed invalid for simulating a given quantile if the point falls <br />outside the 95 percent confidence limits. <br /> <br />4. Discussion of results <br /> <br />4.1 Paleoflood analysis <br /> <br />Table 2 summarizes the maximum floods believed to have occurred in the past 50 to 100 years <br />based on the PSI evidence collected at each site. <br /> <br />Table 2 - Estimated maximum discharges in the past 50 to 100 years. <br /> <br />Basin name Discharge (cfs) <br />[go Creek tributary nr Keota 245 - 390 <br />Geary Creek tributary nr Rockport 375 - 670 <br />Owl Creek tributary fir Rockport 3,400 · <br /> <br />'Occurred within the systematic record. <br /> <br />Figure 7 illustrates the two cross-sections taken at Igo Creek tributary. <br /> <br />16.0 <br /> <br />A~trw>ge <br /><A inundation <br /> <br />".0 <br /> <br />EleYHIoncomtlspondlngto <br />UlSllmilofinundalion <br /> <br />... <br /> <br /> <br />_ tOO <br />" <br />I 80. <br />i <br />. " <br /> <br />..... <br />Small woody debris <br /> <br />..... <br />Sman woody debris <br /> <br />18.0 ~ SrNllwoody <br /> <br />. E :::. "~d~~~~~=:/-//. <br /> <br />t 10,0 <br />~ U: <br /> <br />12.0 <br /> <br />6.0' <br /> <br />4.0. <br /> <br />0.0 .-.__~______ <br />0,0 \0.020.030.0400 SO,Q <br /> <br />600 TOO SOD <br /> <br />900100,0110.0120,0 <br /> <br />40: <br />2.0; <br />0.0:.-____ <br />0.0 to.O <br /> <br />".0 <br /> <br />30,0 40,0 SO.O <br /> <br />".. <br /> <br />70,0 <br /> <br />"'. <br /> <br />2.0' <br /> <br />9lMionino;!lftl <br /> <br />Stationi"9lfQ <br /> <br />w 00 <br />Figure 7 - Cross-section plots of the (a) upstream and (b) downstream stations at [go Creek tributary. <br /> <br />/ <br /> <br />II <br />