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<br />1.50 <br /> <br /> <br />-Average 10/49 - 9/06 <br /> <br />r-1 <br /> <br />. <br /> <br />5.00 <br /> <br />4.50 <br /> <br />4.00 <br /> <br />'~~ ,-~" <br /> <br />3.50 <br />i <br />_ 3.00 <br />GJ <br />e>> 2.50 <br />ftI <br />.c <br />~ 2.00 <br />Q <br /> <br />1.00 <br /> <br />0.50 <br /> <br />0.00 <br /> <br />~~ <br />0.,:'S <br /> <br />':)'b~ <br />0.,: <br />";) <br /> <br />~ <br />o.,:~ <br /> <br />_'to..~ <br />0.,:......- <br />";) <br /> <br />~ <br />~l' <br />~ <br /> <br />.~ <br />s::f~~ <br />~ <br /> <br />,::,~ <br />Pf'S <br />.,; <br /> <br />':)~ <br />Pf <br />.,; <br /> <br />,::,C?J <br />~l' <br />'\) <br /> <br />t!i~ <br />~' <br />'V <br /> <br />(} <br />~p <br />'V <br /> <br />04- <br />fO~ <br />~ <br /> <br />(if' <br />ro<J <br />~ <br /> <br />Date <br /> <br />Fig. 2. Comparison of discharge in Bear Creek to recommended flows. The average daily flows through <br />Bear Creek above the Bear Creek Pipeline for the period of record are plotted. The original R2CROSS <br />analyses indicated that flows should be 1.8 cfs t'hroughout the summer. However, to ensure that the 50% <br />exceedences were met, the flows between 8/16 jmd 10/31 were reduced to 1.3 cfs. <br /> <br />. <br /> <br />Precipitation Data <br />TU has identified local precipitation data from Colorado Springs. These data are included <br />in Appendix C. I <br /> <br />Existing Water Right Information <br />There appear to be three sets of records lassociated with the Bear Creek Ditch Diversion. <br />All three diversions are believed to be withdrawn from the same place and simply <br />represent the evolution of the structure's management. Between 1958 and 1973, it was <br />I <br />managed as structure 534, between 1973 and 1993 it appears to have been managed as <br />535, and since that time it has been mariaged as 7043. Although these diversions do not <br />I <br />affect the proposed reach, the relevant Structure Summary Reports and Annual Water <br />Diversion Reports are attached (Appen4ix D) as further evidence of the magnitude of <br />flows through the upstream reach. <br /> <br />. <br />