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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 />produce significantly different results, as compared to NOAA Atlas. The results of this study show <br /> <br /> <br />that the 1997 values has a pronounced impact on the results. <br /> <br />When using either the GEV regional analysis or the Log Pearson III "at-site" analysis, the effects of <br /> <br /> <br />the longer period of record and the July 1997 storm have a considerable effect on the results, as <br /> <br /> <br />compared to currently used design values. It was the recommendation of technical advisory committee <br /> <br /> <br />that all of the available data be used with an GEV distribution based on the "at-site" data set rather <br /> <br /> <br />than the regional analysis. The results obtained by CSU using the GEV distribution and L <br /> <br /> <br />Moments compared very closely to the results obtained using Log Pearson III for the "at-site" <br /> <br /> <br />analysis. <br /> <br />D. <br /> <br />CONCLUSIONS: <br />As was explained in the results, it was felt by many members of the committee that the City of Fort <br />Collins appears to be dissimilar from the other gage sites in the region and most likely experiences <br />"preferred storm tracks", producing more frequent extreme rainfall events in comparison to nearby <br />areas. In the regional analyses, 7 of the biggest regional events occur above the 20-year return period. <br />In all cases, either 3 or 4 out of the 7 events are from the Fort Collins gage (CSU, 1998). This <br />observation supports the use of an "at-site" analysis using the data set available through 1997 for the <br />City of Fort Collins. <br /> <br />The number of extreme events will have a significant impact on the results obtained from the analyses <br />since the majority of the data points are lower values. This posses somewhat of a problem with plotting <br />position. The current data set for Fort Collins has relatively few recorded large values that influence <br />the fit to the data for the upper region of the frequency curve. Therefore, the 1997 storm will have <br />more of an impact on the analysis since it is the most extreme value recorded and there are few data <br />points in that range of magnitude. As more data is collected, the plotting positions for the 1997 event <br />will likely be shifted to the right. As a result, the predicted values for the less frequent return periods, <br />based on this analysis. may be slightly conservative and may decrease as more data is added to the <br />analyses. It was the consensus of technical advisory committee that the inclusion of the 1997 value was <br />appropriate, even if it may be a high outlier, because of the importance of such a large magnitude event <br />to the record. <br /> <br />-9- <br />