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<br />~ <br /> <br />00163S <br /> <br />c <br />, <br /> <br />MODEL OPERATION CRITERIA <br /> <br />Disclaimer <br /> <br />Nothing in these Colorado River Simulation System (CRSS) model studies nor <br />any of the related summary information is intended to interpret the <br />provLsLons of the Colorado River Compact (45 Stat. 1057), the <br />Upper Colorado River Basin Compact (63 Stat. 31). the Water Treaty of 1944 <br />~ith the United Mexican States (Treaty Series 944. 59 Stat. 1219). the <br />decree entered by the Supreme Court of the United States in Arizona v. <br />California, et al. (376 U.S. 340), the Boulder Canyon Project Act, <br />(45 Stat. 1057), the Boulder Canyon Project Adjustment Act (70 Stat. lOS, <br />43 U.S.C. 618a), the Colorado River Storage Project Act (70 Stat. 105, <br />43 U.S.C. 620), or the Colorado River Basin Project Act (83 Stat. "885, <br />43 U.S.C. 1501). <br /> <br />The CRSS Studies <br /> <br />Three studies ~ere performed using, the CRSS computer model. One study ~ill <br />be used to update the "Central Arizona Project Water Supply Study" which <br />~as last published in December 1984. This CRSS study used a natural flo~ <br />hydrology data base representing the period from 1906 through 1985. <br />Natural flo~ is both undepleted and unregulated, Additionelly~,this run <br />used the 12-year most critical period from 1953 through 1964 for "602(a)" <br />storage determination. <br /> <br />T~o additional studies were performed at the request of the Colorado River <br />Commission (CRC) of Nevada to analyze the impactS of a more adverse ~ater <br />supply upon ~ater availability for the Robert B. ~riffith Water Project <br />(SNWP) in southern Nevada. Both of these CRC studies use the more adverse <br />hydrologic period from 1922 through 1985. The t~o CRC studies differ from <br />one another in that one uses the 12-year most critical period from 1953 <br />through 1964 for "602(a)" storage determination ~hile the other uses a <br />12-year 90 percent probability of exceedance or 10 percent probability of <br />nonexceedance of flo~ represented by the period from 1955 through 1966. <br /> <br />The hydrology for years 1920 and 1921 ~ere substi~uted for 1984 and 1985 <br />hydrology to create a data base through 1985 for all three studies. The <br />natural flo~ volumes for 1984 and 1985 are estimated to have been 24.1 and <br />20.4 million acre-feet (maf). respec,tively. The natural flo~ volumes for <br />1920 and 1921 are 21.9 and 22.7 maf, respectively. The Sum of 1984 and <br />1985 estimated flo~s is 44.5 maf, while-the sum of 1920 and 1921 flows ~as <br />44.6 maf. The rationale for using the 1920 and 1921 hydrology is that the <br />data available for 1984 and 1985 are limited. provisional, and subject to <br />change. <br /> <br />Each of the three model runs was performed on a calendar year basis. The <br />projected study period ~as 1986 through 2050 in all cases. Initial <br />conditions of beginning reservoir contents for all studies corresponded to <br />the Ja~uary 1, 1986 conditions, as described in the January 1986 24-month <br />study entitled "Operation Plan for Colorado River System Reservoirs." <br />