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<br />0031~9 <br /> <br />Page 48 <br /> <br />V. SUMMARY AND CONCLUSIONS <br /> <br />The primary objective of this study was to project the probable future uses <br /> <br />of additional flows in the Colorado River due to vegetation manipulation in the <br /> <br />river's headwater area. Consequently, the most obvious parameter to be varied <br /> <br />was river flow. However, additional parameters were also of interest, initially <br /> <br />because it was thought that the uses made of increased run-off might vary as <br /> <br />water demands grew over time and with differences in such factors as climate and <br /> <br />the institutions which govern water allocation. <br /> <br />A. Hydrologic Aspects <br /> <br />The anticipated runoff increase for climatic conditions equal to those in <br /> <br />I <br /> <br />~ <br /> <br />each of the years for which records were available varies from 49,000 acre-feet <br /> <br />to 106,000 acre-feet, with a mean of 82,000 acre-feet. The increase in each <br /> <br />year is distributed over the period April 15 to June 15. <br /> <br />The effects of enhancing streamflows through vegetation manipulation are <br /> <br />I <br /> <br />summarized in Table V-l. Under existing institutional arrangements, and under <br /> <br />current demand conditions, they were to increase outflow (over 80 percent of the <br /> <br />increase flowed unused into Mexico ), to increase evaporation modestly, and to <br /> <br />alleviate Lower Basin shortages and increase storage slightly. Under full <br /> <br />development conditions, the increased flows were more evenly divided between <br /> <br />outflow, evaporation, storage, and (to a lesser extent) alleviating Lower Basin <br /> <br />shortages. Removing institutional constraints did change this conclusion. <br /> <br />Enhanced flows continued to be almost entirely undiverted under current demand <br /> <br />conditions. Under full development conditions, however, increased flows were <br /> <br />distributed roughly equally between evaporation, outflow, and alleviation of <br /> <br />shortages in the Upper and Lower Basins, respectively. Under these <br />