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<br />~. <br /> <br />.' <br /> <br />.l .-, (", '\ <br />l.)~;; <br /> <br />37. Demand at Brady <br /> <br />38. Gothenburg Power Diversion - <br /> <br />39. Gothenburg System Losses <br /> <br />40. Irrigation Diversions <br /> <br />41. Net Sectional Gain <br /> <br />42. Platte River at Overton <br /> <br />43. <br /> <br />Demand Below Overton <br /> <br />44. Surplus Flow at Overton <br /> <br />Is equal to the Demands below Overton <br />minus Sectional Gain Brady to Overton <br />plus the Gothenburg Power Diversion; <br />if the Power Diversion is less than <br />the System Losses plus Irrigation <br />Diversions, add them on instead of <br />the Power Diversion. <br /> <br />Historic average monthly diversions; <br />if greater than Flow Below Brady, <br />set equal to Brady. <br /> <br />Average monthly losses plus the <br />shortages of the preceding month; <br />and if Losses are greater than the <br />Flow Below Brady, then Losses equal <br />Brady. <br /> <br />* <br />Input data - changed if the Flow <br />Below Brady was less than the <br />Diversions, then the Diversions <br />are equal to zero when Brady Flow <br />is less than Gothenburg Losses or <br />are equal to Flow Below Brady minus <br />Gothenburg Losses. <br /> <br />* <br />Input data. <br /> <br />Is equal to Flow Below Brady minus <br />Gothenburg Power Loss minus Irrigation <br />Diversions plus Sectional Gain plus <br />Johnson Return. <br /> <br />If the Flow minus Johnson Power <br />Return is less than zero, Flow is <br />equal to Jobnson Return. <br /> <br />* <br />Input data <br /> <br />to reflect <br />water. <br /> <br />- Historic Demands adjusted <br />the availability of storage <br /> <br />Flow in Platte River at Overton minus <br />Demand Below Overton; and if less than <br />zero, Surplus equals zero. <br /> <br />4 <br />