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<br />~ <br />c.o <br />L.'i <br />c:..> <br />,,--..., <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />CHAPTER II <br /> <br />GRAND VALLEY RIVER BUDGET <br /> <br />percent to State Line is less than four percent. On the othE!r hand, the best <br /> <br />quality components are precipitation and consumptive use. Precipitation, <br /> <br />however cannot be responsible because it is measured and small, and cannot <br /> <br />reasonably be off by 60%. Nor can the consumptive use be soley responsible <br /> <br />because some years have an unaccounted flow nearly as largess the <br /> <br />consumptive use, and a near zero value of annual consumptive use is <br /> <br />unreasonable. <br /> <br />Nevertheless, it is informative to allocate all of the unaccounted flow <br /> <br />to consumptive use to establish a maximum possible downward effect of the <br /> <br />flow adjustment on salt pickup. <br /> <br />The result of allocating all unaccounted flow to consun~tive use is the <br /> <br />same as not adjusting the flow at all (see Tables 4 and 5, and Figure 4). A <br /> <br />better method of investigating the effect of the consumptive use estimates is <br /> <br />to scale up the consumptive use such that the resulting average unaccounted <br /> <br />flow is zero (see Tables 6-9). Hence, some years will have positive <br /> <br />unaccounted flow and some negative, but the average will be zero. To this <br /> <br />end, all monthly consumptive use values were scaled up by 20.93%, and then <br /> <br />for the sake of analysis, scaled down by the same percentage. The resulting <br /> <br />consumptive use estimates are thought to be conservative upper and lower <br /> <br />bounds of the actual value. The mean annual salt pickup values using these <br /> <br />bounds on consumptive use are represented by the innermost pair of lines <br /> <br />straddling the best estimate mean in Figure 5. For all this, there is no <br /> <br />reason to believe that the original estimate of consumptive, use is incorrect, <br /> <br />II-13 <br />