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<br />~ <br /> <br />N <br />C7:l <br />(.oJ <br />(,Q <br /> <br />. <br /> <br />. <br /> <br />provides a some"hat different perspective on the definition of <br />"present hydrologic conditions," <br /> <br />The first approach could be labeled "flow conditons under <br />present (1975-1976) levels of development." In this instance, one <br />" depicts the flo"5 which would occur in the long run future if the <br />present level of development were to remain constant (recall, how- <br />ever, that depletions would vary some from year to year, even <br />though the level of development were unchanged). Put another <br />way, this approach depicts the future equilibrium condition to <br />which the hydrologic regime would tend over time under present <br />levels of development, <br />, <br /> <br />Estimated long-run flow condtions under present levels of <br />depletion are given in table 3.4 in the form of estimated per- <br />centile exceedence 'flows at the outflow point of each WAUl. They <br />are based upon the estimates of natural flows for the period 1906- <br />1974, as discussed above. By way of comparison with natural flows, <br />the annual means in this table can be checked against those in <br />table 3.1. In all instances, of course, the average annual natural <br />flow for a WAU exceeds the mean annual flow under present levels <br />of depletion by the average annual amount of the depletions which <br />occur above the outflow of any given WAU (see table 3.2). <br /> <br />I <br /> <br />Another comparison between natural flows and flow conditions <br />under present levels of depletion can be derived from table 3.5. <br />As can be seen, reservoir regulation would, over the long run, uni- <br />formly reduce the percentage of flows under present levels of devel- <br />opment that would occur in the months of May - July, while the <br />percentage of 001;S in the winter months would increase to some <br />extent. This effect is, of course, most pronounced at Lees Ferry <br />due .to the cumulative impact of Lake Powell's operation and that <br />of upstream reservoirs. <br /> <br />The second approach to characterizing "present hydrologic <br />conditions" estimates the flows which will occur during the present <br />year (calendar year 1979) given the level of development which now <br />exists ("now" being as of 1975-1976). In this instance, present <br />flow conditions are depicted as the flo'.s which one may, at this <br />moment in time, and under present day reservoir conditions, <br />expect to observe. EA~ressed as percentile exceedence flows at <br />the outflow of each WAU, table 3.6 represents the estimated <br />probability of certain flo1;s occurring in calendar year 1979, <br /> <br />This second approach, which could be labeled "present day flows," <br />differs from the first in that it represents an estimate of the pro- <br />bability of encountering a given flow at the present time, as opposed <br /> <br />1. A percentile exceedence flow is defined as that flow which will <br />be equalled or exceeded a specified percentage of the time. <br /> <br />3-12 <br />