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<br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />- <br /> <br />FIGURE 6 Trace 5 Elevation Com arison <br /> <br />13 <br /> <br /> 6040 <br />c:: <br />0 <br />; 6030 <br />lI:l <br />> <br />C1l <br />iii <br />C1l <br />(J 6020 <br />~ <br />:::l <br />tn <br />l- <br />C1l 6010 <br />-; <br />~ <br /> 6000 <br /> <br />Trace Comparison <br />Action(ALL)/Action(ALL-1 )/NoAction Trace 5 <br /> <br />6050 <br /> <br /> <br />- Action(ALL) <br />- Action(AL L-1) <br />- NoAction <br /> <br /> <br />5990 <br />Jan-02 Jan-03 Jan-04 Jan-05 Jan-06 Jan-07 Jan-08 Jan-09 Jan-10 Jan-11 Jan-12 <br /> <br />Date <br /> <br />During the early spring, the elevation of Flaming Gorge Reservoir is normally at its <br />lowest level of the year. Figures 7 and 8 show the number of occurrences when the elevations at <br />the end of April are within particular ranges. Figure 7 shows a comparison between the Action <br />(ALL-I) and the No Action model output. Figure 8 shows a comparison between the Action <br />(ALL) and the No Action model output. Comparison between Figure 7 and Figure 8 shows that <br />achieving the 18,600 cfs objective had the effect of increasing the occurrences of lower <br />elevations in the spring. The number of occurrences when elevations at the end of April were <br />below 6000 feet above sea level increased from less than 50 (2% of the time) in the <br />Action(ALL-l) model run to nearly 300 (12% of the time) in the Action(ALL) model run. There <br />were no occurrences in the No Action results where the elevations at the end of April fell below <br />6000 feet. <br />