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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 />5.9 TAYLOR RIVER AT ALMONT <br /> <br />5.9.1 Description of Taylor River at Almont <br /> <br />Taylor River at Almont is located just upstream of the Taylor River and East River confluence. The Taylor <br />River at this point has a total drainage area of 477 square miles at the gage. There is an extensive record <br />from the Taylor River at Almont USGS gage (ID# 09110000). <br /> <br />5.9.2 Flood Records for Taylor River at Almont <br /> <br />The Taylor River at Almont USGS gage is located in this reach. This gage provides a record of reported <br />peak flows for 1913,1916, and 1919 through 2000. However, since this gage is affected by the <br />operations of Taylor Park Reservoir, the regulated data is transformed to unregulated flows by accounting <br />for the daily change in storage (see Section 4.3). Unfortunately, daily storage information is not available <br />for the Taylor Park Reservoir (construction began in 1935) until 1958. Therefore, there is a gap in data for <br />these years, as unregulated flow data could not be simulated. <br /> <br />The travel time from Taylor Reservoir to the Taylor River at A1mont gage is estimated to be less than 12 <br />hours; therefore, no lag is applied in the conversion to an unregulated data set. <br /> <br />An estimate of the instantaneous peak flows to corresponding daily values is determined for this gage <br />using values prior to 1935. The ratio of 1.1164 peak-to-daily flows is determined by plotting a straight <br />trend line for the data. The R2 value for the line is 0.95 as shown in Figure 5.9.2.1. This ratio is applied to <br />the maximum daily value for each year of the unregulated data set to estimate peak values. The peak <br />flows for the USGS gage Taylor River at Almont are presented in Appendix A - Table A.9. <br /> <br />The REGFREQ program was used to determine the correlation of the available flow data to nearby gages <br />on the Gunnison River system. A high degree of correlation (>0.9) between the deregulated Taylor River <br />at A1mont gage and the following gages was found. <br /> <br />· Taylor River below Taylor Park Reservoir (09109000) <br />· East River at Almont (09112500) <br /> <br />The East River at A1mont gage was chosen to expand the data set for the Taylor River at A1mont daily <br />stream gage flows. The East River at Almont gage has a continuous record from 1935 through 2000, <br />while Taylor River below Taylor Reservoir has the same period of record due to the deregulation <br />procedure. The resulting family of flow records is presented in Appendix A - Table A.9. <br /> <br />40 <br />