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<br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />At this point in the analysis there are five regions in the Arkansas basin. Region 1 includes the <br />southern foothills. Region 2 includes the central foothills. Region 3 includes the mountains. <br />Region 4 includes the northern foothills (Colorado Springs area). Region 5 includes the eastern <br />plains. Because there were so many data points in the Colorado Springs area and because Region <br />4 is subject to a great deal of internal hydrologic variability, Region 4 was subdivided into 4 sub- <br />regions (4a, 4b, 4c, 4d). There are, therefore, 8 preliminary regression equations to address all <br />of the approximate stream reaches in the Arkansas River basin. <br /> <br />The preliminary equations and curves for the Arkansas basin were presented to the Hydrology <br />Advisory Committee for comment The approval of the methodology was given provided the <br />limitations and disclaimers are identified. The only adjustment recommended by the committee <br />was the selection of less complex equations. In those cases where it was appropriate a less <br />complex equation was selected. <br /> <br />What About Stream Gal!:e Data? <br /> <br />The Hydrology Advisory Committee included representatives of the USGS. They <br />asked why the Guidelines were based on previously designated studies which might have been <br />prepared by a variety of methodologies. Instead they suggested that regional regressions already <br />prepared by the USGS using stream gage records throughout the state could be used. In 1976 <br />just such a publication was prepared. The Board's TM-I publication, prepared in cooperation <br />with the United States Geological Survey has been useful in many hydrologic analyses. TM-I <br />presents regional regression curves which were developed from stream gage data. Over the past <br />20 years, it has been discovered that the methods presented in the manual may over-estimate the <br />IOO-year floodplain values in some regions and under-estimate the values in other regions. More <br />recent USGS publications have updated some of the TM-I analyses for specific regions of <br />Colorado. <br /> <br />There is still some disagreement among hydrologists about the suggestion that gage analyses <br />should always take precedence over other forms of hydrologic analysis. The Hydrology Advisory <br />Committee debated this issue and decided to support the Board staff position that already <br />designated data should form the basis of the guidelines. The Board staff and the committee <br />recommend, however, that the differences between gage analyses and other hydrologic analyses <br />ought to be investigated on a continuous basis, particularly in foothills regions of Colorado where <br />the gage network is not as comprehensive as it should be. The answers to the questions about <br />gage data are not cast in stone, <br /> <br />Remaininl!: Work <br /> <br />In addition to the work already performed in the Arkansas River basin, initial work <br />has begun on the South Platte River basin (including the Republican River basin). Most of the <br />data points in the South Platte basin have been entered into the spreadsheet. No subdivision of <br />the basin into regions has been performed. For the other major basins (Colorado River, San Juan <br />River, Rio Grande and Green River) no data collection has been done. Because the South Platte <br />basin includes over half of the current flood hydrology data points in the state, that analysis is <br />expected to take some time. Once the South Platte analyses have been completed, the CWCS <br />