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<br />. <br /> <br />used on the flows at the Denver, Henderson and Kersey stations <br /> <br /> <br />because it more nearly reflected the bias introduced by regulation <br /> <br /> <br />at these stations. The longer records at Kersey and Julesburg <br /> <br /> <br />were used to extend respectively the shorter records at Weldona <br /> <br /> <br />and Balzac. The correlation coefficients between Kersey and <br /> <br /> <br />Weldona and between Balzac and Julesburg were 0.95 and 0.74 <br /> <br /> <br />respectively. The record extensions were 35 years for Weldona <br /> <br /> <br />and 7 years for Balzac. A zero skew coefficient was used at all <br /> <br /> <br />stations except Balzac. Its proximity downstream from the mouth <br /> <br /> <br />of Bijou Creek, which has experienced frequent extreme flooding, <br /> <br /> <br />resulted in a computed skew slightly less than +0.5. Adjustments <br /> <br /> <br />for expected probability were based on the total years of record, <br /> <br /> <br />or, in the case where the extension of record was used, the <br /> <br /> <br />expected probability adjustment was based on the equivalent years <br /> <br /> <br />of record. Because of the positively skewed distribution used at <br /> <br /> <br />the Balzac station, no expected probability adjustment was used <br /> <br /> <br />at this location. This was in accordance with procedures prior <br /> <br /> <br />to publication of the Water Resources Council Bulletin 17. The <br /> <br /> <br />Balzac curve has not been revised, however, since the expected <br /> <br /> <br />probability adjustment was less than 8 percent at the 100-year <br /> <br /> <br />level. All curves were adjusted to partial duration by using an <br /> <br /> <br />annual series-partial duration relationship developed by Langbein. <br /> <br /> <br />The adjusted curves are shown on plates 18 through 23. A summary <br /> <br /> <br />of pertinent statistical parameters is shown in table 7. <br /> <br />. <br /> <br />33 <br />