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<br />I <br />1\ <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />j <br />I <br />I <br />I, <br />I <br /> <br />SECTION VI: IMPACTS OF CURRENT OPERATIONS <br /> <br />Current Operations Are Characterized By Flood <br />Releases And Fluctuating Releases <br /> <br />Two aspects of current operations have substantial <br />impacts on downstream resources: flood releases and <br />fluctuating releases. This chapter describes the <br />effect of these releases on the critical environmental <br />and recreational resources. <br /> <br />Flood releases are defined as releases greater than the <br />designated powerplant capacity of 31,500 cfs which are <br />discharged through the river outlet works and spill- <br />ways. The river outlet works are generally operated at <br />or near the full capacity of 15~000 cfs, or not at all. <br />Therefore, releases above powerplant capacity are <br />usually in the range of 40,000-50,000 cfs. Flood <br />releases generally occur for four to six weeks in May <br />or June in years when runoff is well above average or <br />the forecast of runoff is too low. These kinds of <br />releases were very rare prior to the filling of Lake <br />Powell in 1980. Since then, flood releases have oc- <br />curred in five of seven years. Under current op- <br />erations, flood releases are expected to occur in one <br />out of four years (Appendix D, section III). A typical <br />flood release pattern (Figure VI-la) for the 1986 water <br />year shows the high releases in May and June. <br /> <br />Fluctuating releases are made when the dam is being <br />operated to produce peaking power. A typical daily re- <br />lease pattern for peaking power operations is shown in <br />Figure VI-lb. For the purposes of the GCES, <br />fluctuations are defined as a change in dam release <br />greater than 10,000 cfs during a day. This cut-off <br />point, although somewhat arbitrary, is based on changes <br />in flow that appear significant for recreation and the <br />environment. For example, when daily fluctuations are <br />greater than 10,000 cfs, they are noticed by a <br />substantial majority of white-water boaters. Also, in <br />practice, when releases are' fluctuating, the <br />fluctuations are almost always greater than 10,000 cfs. <br /> <br />Lake Powell has the <br />necessary to provide <br />releases of 8.23 maf <br />drought (Appendix D). <br /> <br />water storage capacity <br />the required m~n~mum annual <br />even during a long period of <br />Therefore, steady flows lower <br /> <br />43 <br />