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<br />,..- <br /> <br />, <br />. <br /> <br />temperature of Lake Mead outflow has remained the same. Less energy is <br />thus available for the process of evaporation resulting in a substantial <br />water savings. <br /> <br />The temperature of inflow to Lake Mead is based on daily observations <br />at the Grand Canyon gaging station (Phantom Ranch) and corrected by a factor <br />developed during extensive evaporation studies at Lake Mead in 1952 and 1953. <br />Outflow temperatures are from daily observations below Hoover Dam. The tem- <br />perature data are weighted according to the flow of the river in deriving mean <br />annual values. Corresponding evaporation shown in Table 5 is that published <br />by the U.S. Geological Survey in its annual Water Supply Papers and consists <br />of. the mean from two methods of computing water surface evaporation; namely, <br />the Mass-Transfer Method and a Weather Bureau Pan Method, the latter being <br />modified to account for wind measurements. solar radiation. dew point, air <br />temperature, advective energy computed from inflow and outflow data, change <br />of energy stored in the reservoir and water surface temperatures, which is <br />quite a departure from the simple application of the usual Weather Bureau pan <br />coefficient. An Energy-Budget Method is used also for comparative purposes. <br /> <br />:~ <br /> <br />~, <br />;-" <br />~ ' <br /> <br />Roughly, Table 5 indicates an average reduction of over 8 inches in <br />the annual evaporation rate subsequent to 1.963. Annual water savings thus <br />approximate 75,000 acre feet at the present low surface levels of Lake Mead, <br />whereas, when Lake Mead is full, the annual savings would approximate <br />100,000 acre feet. There would also be an indeterminable, but small re- <br />duction in evaporation from the river surface. <br /> <br />-,. <br /> <br />,~ <br /> <br />(Table 5 can be found on the next page, page 12.) <br /> <br />CONCLUSION <br /> <br />!." <br /> <br />This presentation is an attempt to bring attention to positive bene- <br />fits often overlooked by critics of large dams and reservoirs in carrying out <br />their environmental concerns. The author recognizes the unusual surround- <br />ings of this particular reach containing the Grand Canyon of the Colorado <br />River and Lake Mead. Yet there are items herein of common interest to many <br />river regulatory situations which might offer encouragement to the future <br />planners and operators of large dams and reservoirs. <br /> <br />;.: <br />J...:: <br /> <br />~.: <br /> <br />11 <br />