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<br />'.; <br /> <br />001H() <br /> <br />." <br /> <br />3 <br /> <br />BASIN WATER RIGHTS AND MODELING APPROACH <br /> <br />Modeling Approach <br /> <br />The Yampa River Basin Model was developed using ,a network modeling system. Inflows, diver. <br />'sions, demands. reservoirs, and river reaches were represented in the model as a network of arcs and <br />nodes. The mathematical solution of the network insures that water is allocated in strict accordance <br />with user supplied priorities, that allocations are always within user-supplied constraints reflecting <br />decree limits and physical diversion capacities and that mass balance is vigorously preserved throughout <br />the system. <br /> <br />~i <br />11 <br />1 <br /> <br />The Yampa model runs on a monthly time step over a hydrologic study period encompassing <br />water years 1930 through 1982, inclusive. TI1is study period is the same as that used in generating the <br />U.S. Fish and Wildlife Service Environmental Baseline and is the basis for the interim flow recommenda. <br />tions. The use of the same study period permits more convenient comparison of modeled hydrologic <br />regimes with the regime presented in the Environmental Baseline. <br /> <br />Existing basin water uses are represented in the model through the use of gaged flow hydrology <br />rather than virgin flow hydrology. Implicit in this method are the assumptions that historical and cur. <br />rent water use patterns continue in the future as they have in the past, unaffected by any additional <br />water development, and that existing uses are senior, in the water rights sense, to any uses represented <br />explicitly in the basin model. <br /> <br />Future demands are represented in the model as demand increments, i.e., only the differences <br />between current demands and future demands are defined in the model. <br /> <br />Water Rights <br /> <br />, <br />" <br /> <br />Water rights are represented in the basin model only to the extent necessary to properly allocate <br />water supplies among demandirtcremems. Water rights supporting historical uses were implicitly con. <br />sidered senior to all new development by the use of gaged 'flow hydrology. Water right priorities are <br />modeled through the use of ranks placed on modeled demand increments; these ranks are set according <br />to the relative priorities among water rights. The water right priorities assigned to demand increments <br />are described below. <br /> <br />_:' <br /> <br />The use of gaged flow hydrology in the model implies that historical water uses (which are em- <br />bedded in the gage record) are effectively senior to any water uses represented explicitly in the model. <br />Since the 1989.level demancls lire really a set of "adjustments" to bring historical water uses up to 1989 <br />conditions, they must also logically be considered senior to other water uses represented explicitly in <br />the model. In 'any case, the 1989.level demands can 'all safely be considered senior to the Juniper rights <br />either by virtue of their own priorities or by virtue of their being assumed to benefit from the blanket <br />65,000 af Juniper subordination. Thus the 1989.level demands are represented in the model as being <br />senior to the Juniper rights; the relative priorities among the 1989-level demands increments simply <br />reflect whether the demand in question is senior or junior to the Maybell Canal. <br /> <br />The 1989.level demands were also considered senior to the ""'sting reservoirs which were oper- <br />ated in the basin model (i.e., Stagecoach, Steamboat Lake, and Elkhead). TI1is assumption reflects the <br />fact that these reservoirs have yet to be systematically called upon to meet basin water demands and <br />have heretofore been left largely full year.around. Storage in the 'three existing reservoirs was assumed <br />to be senior to the Juniper rights by virtue of specific subordinations of the Juniper rights. TI1is means <br /> <br />