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<br />To illustrate the effects of the Section 7 reductions on the Colorado River baseline in an avera e <br />g <br />year, the average year monthly reductions were subtracted from the monthly Historic Colorado River <br />baseline flows (discussed in Section 3.3.2) at the top of the 15-mile reach. Figure 3.6 highlights the <br />montlily effects of these reductions with the most substantial effects clearly indicated in May, June, <br />and July. <br />3.3.3.3 Adjustment for Annual Hydrologic Variation <br />To account for yearly hydrologic variations over the period studied (1975 through 1993), the <br />monthly Section 7 flow reductions for the average hydrologic year were adjusted up or down (for <br />a wet or dry year) by the ratio of the historic yearly annual Colorado River flow to the historic <br />average annual Colorado River flow for all years in the study period. The same factor was applied <br />to the reduction in each month of each year under the assumption that monthly variations were <br />already reflected in the project distributions. The USFWS concurred with this approach during <br />informal Section 7 consultation meetings. The approach resulted in specific Section 7 flow <br />reductions to apply to the historic Colorado River Flow at the top of the 15-mile reach in each month <br />of each year. The resulting subtraction became the adjusted historic Colorado River baseline flow <br />for each of the 19 years. <br />For the Windy Gap project Section 7 depletions, available historic portions in May, June, and July <br />were obtained from the Bureau of Reclamation for the years 1985 through 1993. These historic <br />depletions are already reflected in the unadjusted historic Colorado River baseline. Subtraction of <br />the entire depletion again would have resulted in a double counting of historic depletions, so it was <br />necessary to remove the historic portion from the total Section 7 monthly. flow reductions in the <br />years for which records were available. The adjustment process is documented in Attachment B for <br />detail. Table 3.9 summarizes by year the final Section 7 flow reductions (including Windy Gap <br />adjustments) which were applied to the historic Colorado River flows at the top of the 15-mile reach <br />to obtain the adjusted Colorado River baseline. <br />3.3.4 Project Flow Reductions In The 1 S-Mile Reach <br />To evaluate ro'ect related effects on Colorado River tr amflows at the to of the 15-mile reach <br />p ~ s e p , <br />withdrawals from the basin by the District which result in flow reductions were computed under both <br />the baseline and future demand scenarios. The baseline demand for the simulation was set at 6945 <br />ac-ft/yr, which is the average volume of finished water the District used during the period from <br />1984-1987 (as discussed in Section 3.2.2). Future demands of the District's customers in the year <br />2045 are estimated to be approximately 28,589 ac-ft/yr based on the Scenario C demand projections <br />(see Section 2.0). Since the goal in this task was to evaluate the reduction in flows under a wide <br />-range of hydrologic conditions (i.e., the 1975-1993 analysis period), the District's raw water system <br />model was used to simulate the operation of their system under both baseline and future demands. <br />The computation of flow reductions is provided in Attachment C. Reductions were calculated as <br />monthly withdrawals by the District over the 19-year simulation period first under baseline demands <br />(pages 1-10 of Attachment C), under future demands (pages 11-20), and finally as net withdrawals <br />(pages 21-30), which are simply the baseline results subtracted from the future results. Flow <br />CDM Camp Dresser & McKee <br />o:~soa~.iio~nocurr~e.noc 8-13 <br />