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<br /> <br /><::> <br /><,:7) <br />o <br />,... <br />oo,J <br />Q <br /> <br />In the UB series, <br />38) to sununarize <br />and type of use. <br /> <br />pie charts <br />Upper Basin <br /> <br />have been included <br />consump~ive uses <br /> <br />(UB-36 through <br />and losses, by <br /> <br />UB- <br />year <br /> <br />In the L.S series, the years 1971 through 1975 are often empty; <br />however, for those years, it cannot be assumed that the actual <br />consumptive use for the identified type of use is zero. The first <br />uses and Losses Report did not incorporate as much summary data 1n <br />the Lower Basin as did the later two reports. Similarly, the first <br />five years in this series may not be comparable because not all <br />consumpti ve use categories were included. <br /> <br />Coo:ments <br /> <br />The overall data <br />are substantial. <br />in agricul tural <br />Colorado, the <br />are decreased <br />been made' in <br />Colorado. <br /> <br />differences in the draft Uses and Losses Reports <br />In the Upper Basin, much of differences occurred <br />uses, mainly in Colorado, New Mexico and Utah. In <br />differences are mainly in agricul tUl"al uses, which <br />up to 150,000 acre-feet per year. These changes have <br />conjunction wi th data provided by the State of <br /> <br />The most striking differences are evident in New Mexico. <br />Irrigation uses have been decreased 1n the San Juan Basin in excess <br />of 60,000 acre-feet per year. Other changes, such as municipal and <br />industrial uses 1n New ~1exi co, were increased. <br /> <br />The changes in the Lower Basin are minimal, except for changes <br />New Mexico, which are significant. In my August 25, 1989, memo, <br />pointed out that the main stem channel losses were not reported <br />1981 through 1985. Fortunately, this has been included in <br />latest draft. However, I take strong exception to the data <br />years 1982 and 1984. As seen on <br />the chart to the right, the data <br />in these years are ,negative. <br />This is because the channel <br />losses are computed rather than <br />measured. All known - diversions <br />and evaporations are backed out <br />of the water balance in the <br />lower basin. Any water that is <br />unaccounted for is deemed to be <br />channel loss. While I do not <br />argue with this accounting <br />methodology, the logical lower <br />limit to this procedure should <br />be zero, rather than a negative <br />number. A naga ti ve number <br />suggests that there 1S water <br />added to the system in the lower <br />basin channel. In the context of <br />only happen when water is imported <br /> <br />RESERVOIR EVAPORATION <br />CHANNEL LOSSES <br /> <br /> <br />400 <br /> <br />200 <br /> <br />o <br /> <br />-200 <br /> <br />-""" <br /> <br />-.... <br /> <br />11 72 73 74- 715 71S n 76 n 60 111 82 83 54 56 <br />Water Year <br /> <br />this <br />over <br /> <br />report, <br />the basin <br /> <br />such an even t can <br />boundary, such as <br /> <br />2 <br /> <br />in <br />I <br />for <br />the <br />in <br />