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<br />01n183 <br /> <br />26 <br /> <br />A total of 26 demands have been represented in the Yampa Basin model to represent the 1989. <br />maximum demand scenario. These demands, which are listed in Table 4-5 as demand numbers 1 <br />through 261 represent municipal, industrial, agricultural, recreational "and trans-basin exPOrt wJ.ter uses. <br /> <br />It is important to remember that these demands are in fact increments to move from the <br />historical demand condition, which is embedded in the gage hydrology used ill (he model, 10 the 1989 <br />maximum demand condition. Total depletions representing 1989 maximum conditions are 121,174 af. <br /> <br />Three additional demands represented in the model and operational for the 1989 demand <br />.condition are demands 34, 37 and 38. Demand 37 is the portion of currelll Steamboat Springs <br />municipal demand that could not have been met historically through ihe City's Fish Creek delivery <br />system. This water would historically have had to have been pumped directly from the Yampa River. <br /> <br />Demand 34 represents increased irrigation watcr use in thc upper Yampa basin above <br />Stagecoach Reservoir occurring as a resuil of the Yamcolo . Stagecoach exchange. This demand totals <br />4000 af per year and is modeled as approximately 25 percent eonsumptive. <br /> <br />Demand 38 is the historical Maybell Canal diversions. Diversion records were obtained from <br />the Division 6 office of the State Engineer. This demand is represented as a withdrawal rather than as a <br />depletion because it was considered important to represent its effect as the sedor downstream water <br />right in the basin. <br /> <br />It should be noted that in several instances demands that occur on tributaries to the Yampa <br />River have been placed directly on the mainstem. This was done in order to avoid synthesizing <br />stream flows on the many small triputaries. Rather than individualized gains from each tributary, "reach" <br />gains were defined that include several sources. <br /> <br />By placing tributary demands On. the mainstem, there will be no net effect to other mainstem <br />demands so long as these tributary demands were not historically shorted. If shortages wo'uld have <br />occurred, the demand as represented in the model will be satisfied by water from the mainstem, a <br />physical impossibility, However, because these shortages are intrcquent and of relatively small amounts <br />and because the net effect on the Yampa Hiver mainslem is the same, this error is considered, negligible, <br /> <br />Demands 25 - 33 in Table 4.5 represent demand increments to mow to future conditions. <br />These demand are represented in the model as a single sel of demands whose magnitude changes <br />depending on the demand level under evaluation. For demand level 1. (1989 maximum conditions) <br />these demands are set equal to zero. The second arid ihird demand levels represent the growth from <br />current to future near.term (year 2015) and long-term (year 2040i conditions. Demands 25 - 33 are <br />assumed constant from year to year throughout the stud~ period and are given a priority lower than <br />Juniper.Cross rights in the model. <br /> <br />In the Yampa model, demand arcs representing future demand increments have priorities lower <br />than the priority assigned to the T&E instream Oow arc (i.e., the priority of the Juniper Project water <br />right) while demand arcs representing existing (1989) maximum demands have priorities higher than <br />that of the instream Oow arc. In several scenarios, the effect of subordinating the Juniper right to the <br />future demand increment is examined by changing the rank on the Juniper right to be junior to the <br />future demands. <br /> <br />," <br />