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drinking water for certain non-potable purposes, such as heating and cooling, on the <br />main campus.) <br />^ Green Lines: firture demands with the OWASA/UNC reuse project on the main <br />campus in place and operating in 2008, The "Less Reuse" and "More Reuse" <br />boundaries indicate the likely rarrge of future demands, OWASA's projections <br />reflect all information currently available about ongoing and planned development <br />on the University's main campus and Carolina North, but do not include any <br />allowance for demands that could be met by water reuse at Carolina North, The <br />basis for these projections is discussed later in this report.. <br />^ Black Stepped Horizontal Lines: the capacity of OWASA's University Lake/ <br />Cane Creek/Stone Quarry reservoir system as currently configured, with planned <br />pump improvements, and with the Quarry's eventual expansion in the early 2030s, <br />The upper stepped line is the reliable "safe yield" of the system under drought <br />conditions that would be expected to occur approximately once in 30 years, The <br />lower stepped line is the safe yield under the drought-of-record conditions that <br />occurred in 2001-2002. <br />The intersection of the diagonal demand lines in Figure 1 with the horizontal capacity <br />lines represent periods when anticipated demand will equal or exceed the estimated safe <br />yield of the reservoir/quarry system, This does not mean that we will run out of water at <br />that time; but, the system will only be able to provide the indicated amount of wcztet• if the <br />30~~eat° or 1001 drought-of-record should recur. On the basis of nearly 80 years of <br />hydrologic records, the probability that .30-year drought conditions will not occur in any <br />given year is 29 out of 30, or nearly 97 percent. In other words, there is a 97 percent <br />chance that the reservoir/quarry system will produce more than the specified safe yield in <br />any given year. The probability of exceeding the record drought yield (which is less than <br />the 30-year yield) is even greater. <br />The probability of depleting OWASA's reservoir/quarry system under various conditions <br />of supply and demand is illustrated in Figures 2, .3, and 4. These figures also provide <br />graphic guidelines for determining when to invoke different levels of OWASA's water <br />conservation standards, <br />^ Each cell of the table contains an integer and a percentage, which represent the <br />probability that reservoir levels will decline to 20 percent or less of full capacity <br />during the following 18 months, These results were derived from spreadsheet <br />model runs of almost 80 years of daily streamflow data, updated through January <br />200.3, and driven by monthly water demand and reservoir storage at the begimiing of <br />each month, Calculations were based on average amoral raw water withdrawals of <br />9.15 million gallons per day (mgd) for Figure 2; 10 mgd for Figure .3; and 11 mgd <br />for Figure 4, and adjusted with shorter term demand ratios, which are reflected in <br />monthly demands shown at the top of each column. (Actual reservoir withdrawals <br />during 2005 averaged 8.4 mgd,) <br />OWASA - Water and Sewer Capnci(y /mplicntioas of G~creased Development Densi(y <br />Pnge S of 2! <br />