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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 />Figure 4.2.1 <br /> <br />Comparison of Regulated vs. Unregulated Instantaneous Peaks at Taylor River <br />below Reservoir <br /> <br />3000 <br /> <br /> IIIlI U n re 9 u I at ed <br /> .. <br /> [J Re 9 u I at ed <br /> n <br /> -, <br /> u <br /> .. .' <br /> , <br /> n > <br /> > - 1 <br /> , > <br />B .. <br /> > > <br />, . .' , - <br /> " ,. > > <br /> , , <br /> , , > <br /> > > > ; > <br /> , " , , <br /> , .. ., > , , > <br />., .' > <br /> , > ,- > > > > > <br /> .' .' " , > " > , <br /> , , , > .' <br />. <br /> <br />2500 <br /> <br />o 2000 <br />U <br />af <br />~ 1500 <br />.t: <br />u <br />o <br />is <br />1000 <br /> <br />500 <br /> <br />o <br />~~~~~~~~~~~~~~~~~~~~~ <br />~~~~~~~~~~~~~~~~~~~~~ <br />Year <br /> <br />In addition to the Taylor River reach immediately below the reservoir, the Taylor River at A1mont and the <br />Gunnison River at Gunnison gages are affected by the reservoir, though the level of influence decreases <br />as additional unregulated drainage area contributes flow. <br /> <br />The regulated flow data sets at both of these stream gages are adjusted to simulate unregulated <br />conditions. The adjustments are made by first adding or subtracting the change in Taylor Reservoir <br />storage values (converted to daily flow) to the regulated flow data sets. The second step is to identify the <br />annual maximum daily flow. Lastly, the peak to daily ratio is applied to estimate the instantaneous peak <br />flow. For the Taylor River at A1mont, the peak to daily maximum ratio was determined for water years <br />1913, 1916, and 1920-1935 to be 1.1164. This ratio is applied directly to both the regulated and change in <br />storage portions of the flow to create the unregulated peak flow record for that location. <br /> <br />At the Gunnison River near Gunnison, the data are treated differently. First, the daily regulated flow is <br />added to the daily change in storage for all values from 1959 through 2000. Next, the annual maximum <br />daily value is identified based on the sum of the values. The instantaneous peak is estimated by applying <br />two different factors: one for the change in storage flow and one for the regulated portion of flow. The <br />change in storage is multiplied by the ratio (1.2481) determined for the Taylor River at Taylor Park gage. <br />The regulated flows are multiplied by the peak to daily ratio of 1.0687 derived for this gage from water <br />years prior to the reservoir construction. <br /> <br />13 <br />