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<br />7 <br /> <br />TABLE 1 Controllinsz Criteria Analvsis of Action and o Action Model Results <br />Spring Peak Flow Recommendations Target Model Results <br />for Reach 2 0/0 <br /> Action Action No <br /> (ALL-I) (ALL) Action <br />Achieve Peak at Jensen >= 26,400 cfs 10% 11.4% 16.4% 5.0% <br />Sustained Peak at Jensen >= 22,700 cfs 10% 10,8% 12.3% 4.1% <br />for at least 2 weeks, <br />Sustained Peak at Jensen >= 18,600 cfs 10% 9.5% 18.1 % 5.0% <br />for at least 4 weeks, <br />Achieve Peak at Jensen >= 20,300 cfs 30% 44,7% 57.7% 40.4% <br />Sustain Peak at Jensen >= 18,600 cfs 40% 18.2% 43.1% 14.0% <br />for at least 2 weeks. <br />Achieve Peak at Jensen >= 18,600 cfs 50% 60.2% 66.0% 58.9% <br />Achieve Peak at Jensen >= 8,300 cfs 100% 99.7% 99.7% 98.5% <br />Sustain Peak at Jensen >= 8,300 cfs 90% 96,9% 96,9% 96.9% <br />At least I week. <br />Sustain Peak at Jensen >= 8,300 cfs 98% 97.3% 97.3% 97.3% <br />at least 2 days except in extreme dry <br />years. <br /> <br />N <br /> <br />Reservoir Water Surface Elevation Results <br /> <br />For each month of the model run, from January 2002 to December 2040, there are 65 <br />elevations that could potentially occur in any given month (one elevation for each trace), These <br />monthly data sets have been sorted from lowest to highest. The 10th, 50th, and 90th percentile <br />values have been selected from each set. Figure I shows the 90th percentile elevations that <br />occurred for all three runs of the model for the finlt lO years of the model run. The results in <br />Figure I do not represent anyone particular elevation trace. Rather, these curves can best be <br />thought of as a boundary elevation that will be exceeded 10% of the time. To illustrate how <br />individual traces fluctuate through time, trace 54, which achieved the 90% boundary elevation in <br />July, 10 years into the model run, is included in the figure, The amplitude of the curves from year <br />to year indicated how much water was being stored during the spring for release later in the year. <br />The smaller the amplitude, the less storage that took place throughout the year and the less <br />change in elevation that occurred from year to year, Both the Action(ALL) and the Action(ALL- <br />I) model runs have smaller amplitudes than the No Action Alternative indicating less active <br />storage and less elevation change during the year. <br />