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Colorado River Simulation <br />Model <br />The model simulates river basin flows on a mon- <br />thly time frame starting at the top of the basin <br />and proceeding completely through the basin to <br />the bottom. Simulation is done reach by reach <br />in an order specified by the basin configuration <br />as input to the model. Within a reach, computa- <br />tions are made from upstream to downstream <br />end. <br />The general operation of the simulation model is <br />shown schematically on figure 4. <br />Riverflows aze calculated at each inflow, de- <br />mand, and reservoir sequence point. All calcula- <br />tions for riverflow aze based on the continuity <br />equation: <br />Flow at next sequence point =Flow from <br />preceding sequence point + Inflow -Demand <br />When there is not enough flow in the river at a <br />sequence point to supply a demand, a seazch is <br />made of upstream reservoirs for- the additional <br />water needed. If there are reservoirs upstream <br />with sufficient water in storage, the additional <br />increment needed is released and passed through <br />the system to the point needed. If adequate <br />water is found, the demand is met and the calcu- <br />lations proceed to the next downstream se- <br />quence point. However, if the demand cannot <br />be satisfied, the amount of shortage is com- <br />puted, the available water is diverted, and a <br />shortage message is printed and calculations <br />proceed. <br />A reservoir is generally operated to meet a target <br />end-of--month contents. A release is determined <br />7 <br />