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<br />.,' <br /> <br />. <br />'!I <br /> <br />'. <br />(u) Power 1s to bE generated at Hoover to the extent that <br />water required to "eet do~nstream uses, as defined in (3) <br />above, will permi t tluch ger.9r:ltion. If such releases do not <br />permit generation 01 firm p01"~r as defined by contract, then <br />Lake Mead storage wo'Jld be drawn upon for firm power, except <br />that when Lake Mead Jtorage js thereby drawn down to 17,000,000 <br />acre-feet (active), <he accwIlLllation of additional storage in <br />Glen Canyon Reservoil' shall be restricted to the extent <br />necessary to permit '~cntinuance of firm power production at <br />Hoover without furth3r demand upon Lake Mead storage. ,later <br />already stored in Gl~n Canyon Reservoir shall not be released, <br />however, for continu3nce of firm generation at Hoover. <br /> <br /> <br />Application and furthlr'd1scussion of, and the resulting compu.- <br />tations under the foregoing basic premises are contained hereinafter. <br /> <br />Assumed Stream Flow Conditions <br /> <br />.~ .. <br />"-'I <br /> <br />1:'1 <br /> <br />~ <br />~d <br />.- <br /> <br />An assWllption as to expected stream flows is necessary in aD7 <br />reservoir filling demonstration. The assumption of average stream flow <br />conditions is a reasonable one for this study. Reservoir operation studies <br />presented herein assume average stream flow at Glen Canyon equal to that <br />obtained from the period 19lu-19u5 inclusive, modified to reflect present <br />conditions of development and progressively reduced each year through the <br />operation period consistent with a projected schedule of increasing annual <br />depletions. Of course, stream flow realized at Glen CaIlj'On will depart <br />from the average in any given year, but speculation involving variants in <br />the developing physical situation is premature and would not be useful. <br /> <br />, '.- <br /> <br />t. <br />~' <br />:JJ. <br /> <br />,; <br /> <br />~, <br /> <br />~ <br />I <br /> <br />Lake Mead storage reached a low OOint i.n1rnediately prior to the <br />1951 flood season due to a recent drought (1953-56 being the lowest four <br />years in sequence in the history of the Colorado River). The flood run- <br />orf in 1957 was considerably greater than average and Lake Mead active <br />storage content is expected to be 20.0 million acre-feet on April 1, 1958. <br />Therefore the operation studies begin April 1, 1958, with Lake Mead act1'Y. <br />storage content of 20.0 million acre-feet. <br /> <br />'I'; <br />.1 <br /> <br />Historically, the annual flow at the Glen Canyon Dam site <br />averaged 13.8 million acre-feet during the 32-year period 1914 to 1945, <br />inclusive. When modified to reflect present conditions of development <br />in the Upper Basin, the average annual flow is about 13.1 million acre- <br />feet. Further developments in the Uooer Basin, such as construction of <br />water-consuming projects and storage reservoirs, will require further <br />adjustment in the eJP ected flow. T..ble I is a tabulation of the flows <br />to be e:xpected in the near future at Glen Canyon Dam assuming average <br />stream flow COnditions. <br /> <br />2 <br />