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<br />-\ <br /> <br />. <br /> <br />. <br /> <br />~ <br /> <br />.' <br /> <br />n~~''''7~~') <br />~~, :,) '_' J 1 "" <br /> <br />0" <br /> <br />SUMMARY DESCIUPTION <br />OF <br />EXISTING GUNNISON BASIN MODEL <br /> <br />0,.- <br />( <br /> <br />lNTRODjlCOON <br /> <br />This document is a summary description of the existing basin model based on the executive <br />summary and excerplS from Task Memorandum No.5 of me Colorado Water Resources and power De- <br />velopment Authority's ~hase 1 Study. A diagram of the model network and tables listing important data <br />and information supporting the summary are attached at the back of this document. <br /> <br />MODELING APPROACH <br /> <br />The basin model was developed using a network modeling system and runs on HJM-compatible <br />microcomputers. In the model, the basin is characterized as a network of links representing inflows, <br />stream reaches, diversions, reservoirs, and demands. The priorities placed on various links in the <br />network arc derived [n)ffi water rights considerations. These priorities control the allocation of water to <br />various uses represented in the model. Opera.ting rules {or various facilities are implemented through l <br />special computer code which adjusts the priorities assigned to specific links, such as those which l\ <br />represent reservoir storage or releases. <br /> <br />The model operates on a monthly time step over a 1952.83 study period. In each month, the <br />model solves for an optimal allocation of available water supplies according to the priorities placed on <br />various Imks by the user. Reservoir carryover slOrage and lagged return flows are the connections be. <br />tween one month's solution and the nt:Xl. A diagram of the model network is attached to the back of <br />this document. <br /> <br />Ci, ('/._ r <br />/o./p' - <br /> <br />Files of model inflows at 59 sites were derived by U.S. Bureau of Reclamation (lJSIJR) staIT in <br />. / <br />Grand Junction. These inflows are of three types: 1) virgin Oows, 2) gaged/flows, and 3) imputed reach <br />ga.ins. Vi-tWO flows at gaged shes were derived from historical Clow records' corrected for upstream reser. <br />voir operations, basin impons and exports, and irrigation depletiOnsl Historical irrigation depletions <br />were cstimalcd from consumplive use rates derived from the CRSS database, acreages oblaincd from the <br />USBN., the SCS, and the Gunnison County assessor, an.d ftom detailed operating studies of seleclt~d <br />ditches. Virgin (lows at ungaged sires were developed from virgin flows at "reference gages" corrected <br />for area and elevation differences; Table llisLS these reference gages. <br /> <br />;> <br /> <br />S11JDY PJiRlOD IIYDROLOGY <br /> <br />Gaged flows were used to represem inflows from the North and Smith Forks of the Gunnison <br />and the inflows to Ridgway Reservoir. Reach gains imputed from gaged flows were used to represent ac- <br />cretions along the Uncompahgre River abov~ the South Canal and along the Gunnison below Delta. <br /> <br />Return flows from ceflain water uses are also represented in the model as inflows; these 20 in- <br />nows arc compuled. internally by the modcJ based on user-supplied lag, factors. The specific rClUrn flow <br />factors V'....ry depending on type of water use and amount diverted and were adjusted during calibration. <br /> <br />o <br /> <br /> <br />~ <br /> <br />(9. <br />FEB 1 3 1992 <br /> <br />BY O\VI~N 4 <br />