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<br />I <br /> <br />I <br />I <br /> <br />I <br />I <br /> <br />I <br />I <br /> <br />I <br />I <br /> <br />I <br />I <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />4.3 EFFECTS OF TAYLOR PARK RESERVOIR REGULATION <br /> <br />Taylor Park Reservoir is located on the Taylor River approximately 16 miles upstream of the confluence <br />with the Gunnison River. Construction of the reservoir began in 1935 with the first releases made in 1937. <br />The Bureau of Reclamation owns and operates the dam in conjunction with the Blue Mesa Reservoir <br />(downstream on the Gunnison River) primarily to augment irrigation supply in the later portions of the <br />growing season. All releases are made directly downstream; there are no diverted releases from this <br />reservoir. <br /> <br />The reservoir does not serve as a flood control facility; however, a primary operations objective is to avoid <br />discharge flowing over Taylor Park Dam's uncontrolled spillway. In addition, attempts have reportedly <br />been made to reduce peak flows if a request is made for reduction in outflows (Stanton, 2002). Current <br />operation practices tend to reduce peak flows as some of the peak runoff is retained for release <br />throughout the irrigation season extending into October. However, if the reservoir is full, higher releases <br />are possible. <br /> <br />The Taylor Park Reservoir downstream regulated flow data (discharge records for Taylor River below <br />Reservoir) are used in conjunction with changes in reservoir storage to generate the downstream <br />unregulated or natural flow data. The unregulated flow data is then compared to regulated data to <br />determine the effects of the reservoir. A detailed explanation of the procedure used to develop the <br />unregulated flow data follows. <br /> <br />The daily change in storage in the reservoir, reported in acre-feet-per-day, is converted to cubic-feet-per- <br />second. Positive change in daily storage represents water that would have been in the channel just <br />downstream of the reservoir; it is therefore added to the regulated flow data. A negative change in daily <br />storage indicates that the discharge, as reported at the Taylor River below Reservoir gage, should be <br />decreased to accurately represent what would have been flowing in the channel. Storage records for <br />Taylor Park Reservoir are available from the Bureau of Reclamation beginning on October 1, 1958. Inflow <br />records are also available; however, inflow data is calculated by Reclamation using outflow records <br />(Taylor River below Reservoir) and daily storage information. Therefore, this data does not provide any <br />additional information for this analysis. The reported storage values are somewhat sporadic due in part to <br />the measuring techniques and to weather conditions such as wind and rain. The daily values of storage <br />are therefore averaged over a three-day period to help account for the inherent variability in the reported <br />values.2 <br /> <br />An unregulated flow daily data set is created for the Taylor Park below Reservoir gage beginning on <br />October 1, 1958 and extending to September 30, 2000. This flow data series provides 42 years of daily <br />flows and annual maximum daily flow values. The annual maximum daily flow value must be adjusted to <br />estimate the instantaneous peak value used to perform flow frequency analyses. This is done by <br />estimating a ratio of instantaneous peak flow values to the daily flow value reported on the same day for a <br />similar gage with both data sets available. The Taylor River at Taylor Park Gage is located upstream of <br />the reservoir. Because this gage is not affected by the reservoir, the instantaneous peaks and <br />corresponding daily value sets from this gage are used to determine the ratio. The resulting ratio of <br />1.2481 is applied to the unregulated annual maximum daily flows at the Taylor River below Reservoir <br />gage, located just downstream of the reservoir outlet. <br /> <br />The regulated instantaneous peaks, as reported at the Taylor River below Reservoir stream gage, are <br />compared to the simulated unregulated instantaneous peaks for the same location. The results, depicted <br />in Figure 4.2.1, indicate, as expected, that the peaks regulated by the Taylor Reservoir are less than what <br />would have occurred in an unregulated scenario. <br /> <br />2 This method of using a three-day average is recommended by Coil Stanton of the Bureau of Reclamation, Grand <br />Junction office. (Coli Stanton, Hydraulic Engineer, Water Resources Group, personal communication, 2003) <br /> <br />12 <br />