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<br /> 3600 <br /> 3500 <br /> 3400 <br /> 3300 <br /> 3200 <br /> 3100 <br /> 3000 <br /> 2900 <br /> 2800 <br /> 2700 <br /> 2600 <br /> 2500 <br />- <br />en 2400 <br />- <br />Co) 2300 <br />- <br />W 2200 <br />" 2100 <br />a: 2000 <br />~ 1900 <br />:J: <br />0 1800 <br />U) 1700 <br />- <br />C 1600 <br /> 1500 <br /> 1400 <br /> 1300 <br /> 1200 <br /> 1100 <br /> 1000 <br /> 900 <br /> 800 <br /> 700 <br /> 600 <br /> 500 <br /> 400 <br /> 300 <br /> 200 <br /> 100 <br /> 0 <br /> 0 0 N 61 D <br /> <br />" <br />.. <br /> <br /> <br />1982 <br />REREGULATED <br /> <br /> <br /> <br />< <br /> <br />< <br /> <br />122 <br />J F <br /> <br />M 183 A M 244 J <br /> <br />305 366 <br />J A S <br /> <br />DAYS OF THE WA TEA YEAR <br /> <br />Figure 11. Variability of flows on the Gunnison River (East Portal gauge) as a consequence of <br />regulation by the Aspinall Units during the 1982 water year and as reregulated to simulate the <br />predam hydro graph (from Stanford and Ward 1992b). <br /> <br />28 <br />