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<br />. <br /> <br />- <br /> <br />- <br /> <br />- <br /> <br />. <br /> <br />. <br /> <br /> 5.0 <br /> 0 <br /> ct ...:t <br /> ... en <br /> er <br /> '" N <br /> ... <br /> u 4.0 <br /> '" <br /> .... <br /> er <br /> :::> <br /> '" <br /> 00 <br /> uJ:z <br /> "'0 <br /> ctu <br /> "'uJ 3.0 <br /> er", <br /> u <br /> :zer <br /> -... <br /> :lEa.. <br /> ~.... <br /> ....'" <br /> uJ <br /> Cl... <br />N ~u 2.0 <br />-oJ .....- <br />...JID <br /> :::>:::> <br /> cnU <br /> uJz <br /> er- <br /> z <br /> 0 <br /> .... <br /> ct <br /> '" 1.0 <br /> 0 <br /> a. <br /> '" <br /> > <br /> uJ <br /> <br />0,0 <br />o <br /> <br /> <br />50 100 <br />INCREASE IN SURFACE <br /> <br />150 200 250 <br />AREA OF ARKANSAS RIVER (FROM FIG. 7), IN ACRES <br /> <br />300 <br /> <br />Figure 9.--Arkansas River evaporation due to increases in surface area resulting <br />from releases from Twin Lakes Reservoir to Colorado Canal. <br />