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<br />00lG87 <br /> <br />The CRSM currently uses a critical period of 12 years, from 1953 <br />throu9h 1964. This critic~l period was derived using the following <br />mass balance equation: <br /> <br />602(a) storage = (5.8 MAF depletions x n x 0.9388) <br />+ (8.23 MAF objective minimU'l1 releasl~ x n) <br />_ (natural flow at Lees Ferry over the critical period of <br />"n" years) <br /> <br />where n = the length of the critical period, and 0.9388 provides for <br />a shortage of 6.12 percent. <br /> <br />Values of 602(a) storage were computed with the above equ,ltion using <br />all possible s,~q'Jential hydrology periods of all possible lengths (n) <br />in the 1906-1983 natur'al floill record. The hydrology period that gave <br />the largest 602(a) storage was the 12-year period beginning in 1953. <br /> <br />The CRSM computes 602(a) storage at the beginning of each calendar <br />year usin9 the above mass balance equation with the following modifi- <br />cations: (1) the depletions are equal to the depletions scheduled in <br />the demand data file for the next 12 years being modeled, (2) the <br />value of "n" is equal to 12, ann (1) the natural flow at Lees Ferry <br />over the critical period is equal to 12.18 MAF. <br /> <br />Note that the method of determining 602(a) storage described here is <br />used for simulation only and is not intended to be a formal deter- <br />mination of 602(a) storage ~s required by the Criteria for Long-Range <br />Operati on of Colorado Ri ver ~,~s~rv()i rs. <br /> <br />8.3 Releases from_ !-_a_ke M~~<! <br /> <br />Initial releases from Lake Mead are determined on a monthly basis by <br />combi ni ng three factors: (1) schedul ed consumptive use requi rements <br />dOillnstream of Hoover Dam, (2) the volume of water required to meet <br />reservoi r target storage curves estdbl i sh,~d for Lake Mohave and Lake <br />Havasu, and (3) the net volume of gains ~nd loss'~s for the month for all <br />reaches of the system downstre~m of Hoover Dam. The process of deter- <br />mining initial releases from Lake Mead is simply an accounting proce- <br />dure, with all the data supplied externally to the simulation model. <br /> <br />Initial releases from Lake Mead are used unless they are increased <br />because of flood control or scheduled surpluses, or they are decreased <br />because of shortage conditions. Flood control requirements are <br />discussed in section 8.3.1. The surplus strategy is disclJssed in sec- <br />tion 8.4 and the shortage strategy is discussed in section 8.5. <br /> <br />8.3.1 Flood Control <br /> <br />Flood control operation of L~ke Mead is one of two factors that can <br />increase releases from Lake Mead above those which are needed to meet <br />downstream demands and target content level s of downstream reser- <br />voirs. The CRSM simulates the flood control operation of Lake Mead <br /> <br />37 <br />