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<br /> <br />, . <br /> <br />,v'. <br /> <br />. <br /> <br />. <br /> <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />meeting the reasonable beneficial Colorado River mainstream <br />consumptive water uses in the Lower Basin as provided by the Operating <br />Criteria, <br /> <br />the delivery of firm power in accordance with energy contracts, <br /> <br />minimum and specific releases for fish and wildlife and recreational <br />purposes, <br /> <br />refilling of vacant system reservoir storage space, <br /> <br />potential for flood control releases before shortages may occur, <br /> <br />water wasted to the Gulf of California, <br /> <br />compliance with the 1944 Mexican Water Treaty and Minute No. 242 of <br />the IBWC, <br /> <br />the lack of fully developed water use in the Upper Basin, and in Arizona, <br />and Nevada of the Lower Basin, <br /> <br />the ability to store unused water apportionments, <br /> <br />guidelines for reservoir filling and draw down recommended for fish <br />spawning periods in Lake Mead, <br /> <br />complying fully with compact, decree, statutory, and water delivery <br />obligations, and <br /> <br />other short- and long-term effects of 1991 water use decisions. <br /> <br />Water Supply Assumptions <br /> <br />For 1991 operations, three reservoir inflow scenarios were developed and analyzed; <br />statistically these are approximately the upper quartile, lower quartile, and lower decile <br />inflows and have been respectively labeled the probable maximum, most probable, and <br />probable minimum (see attached graphs of reservoir parameters). Each of these <br />scenarios was adjusted for current soil moisture deficiencies throughout the basin; <br />therefore, each is lower in magnitude than the historical upper decile, mean, and lower <br />decile inflows, respectively. The National Weather Service computer model used to <br />adjust the scenarios was the Extended Stream Flow Prediction model. This model uses <br />current conditions as well as historical data to predict a range of possible future stream <br />flows. Although there is a wide confidence band associated with stream flow forecasts <br /> <br />4 <br /> <br /> <br />- <br />