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Last modified
7/14/2009 5:02:36 PM
Creation date
5/20/2009 3:02:49 PM
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UCREFRP
UCREFRP Catalog Number
9581
Author
U.S. Bureau of Reclamation.
Title
Final Environmental Impact Statement - Navajo Reservoir Operations Volume II Technical Appendices.
USFW Year
2006.
USFW - Doc Type
Grand Junction - Durango, CO.
Copyright Material
NO
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<br />C-6 <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />il <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />natural gains occurring within their associated river reach, this problem was avoided. Other <br />refinements included compensation for phreatophyte depletions along the mainstem and <br />adjustments to lag return flows. <br /> <br />The San Juan-Chama project was simulated following the rules of the Authorization Act. <br />Daily bypass flow requirements in the Rio Blanco, little Navajo, and Navajo rivers were <br />maintained. The maximum single year diversion (270,000 af), maximum total10-year <br />diversion (1,350,000 af), and capacity of the diversion tunnels were also respected. The <br />diverted water was stored and released from Heron Reservoir, which was also simulated in <br />the San Juan RiverWare model. The release pattern from Heron Reservoir followed the <br />mean call pattern of the current San Juan-chama contracts. <br /> <br />The ALP Project impacts were simulated in RiverWare by explicitly entering the various <br />project features and defining their operation in the system. To meet daily minimum flow <br />requirements in the Animas River, a daily operation loop was employed to determine <br />allowable pumping to Ridges Basin reservoir. All other computations were completed on a <br />monthly time step. <br /> <br />Before using the San Juan RiverWare model for project analysis, it had to be validated, <br />verified, and calibrated like any model. The configuration of the model was validated by <br />having the model simulate gaged flows from the natural flows and the historical depletions, <br />reservoir releases, and flow routing used to compute the natural flows. . This was essentially <br />a back-calculation of the gaged flows from the natural flows. The model configuration was <br />determined to be valid once the simulated flows at all gage points matched the gaged flows. <br /> <br />Once the model configuration was validated, reservoir operation rules were substituted for <br />the historic releases, and the model was rerun. The reservoir operating rules were calibrated <br />so that the end of month reservoir contents closely matched the historical observed contents. <br />Once this match was obtained, rules designed to simulate the Type I shortage were imple- <br />mented and the full irrigation demands substituted for the historical shorted demands. <br />Again the rules were adjusted until the simulated flows at all gaging stations closely <br />matched the observed gaged flows. Once this was achieved the model was assumed <br />calibrated and verified. <br /> <br />Simulation of reservoir operations, particularly operation to "mimic" natural flows, requires <br />forecasts of reservoir inflows. For forecasting inflows to Vallecito and Lemon reservoirs, the <br />fraction of the deviation of the actual inflow from the mean inflow is added to the mean <br />inflow. The deviation fraction starts small early in the year and approaches 100% when <br />close to the peak runoff month. For the Navajo Reservoir operation simulation, a forecast <br />error approach is used, whereby the mean historical forecast error for each month is pre- <br />determined and applied. Operation of Navajo Dam to maximize peak flows also requires <br />forecasting the time of peak runoff for the Animas River, allowing releases from Navajo <br />Dam to match the Animas peak. At this time, a constant peak release date has been utilized, <br />since no significant relationship could be developed for predicting timing of the Animas <br />peak. The required timing of the peak release from Navajo Dam was adjusted to optimize <br />the hydrograph statistics to mimic the 1929 to 1993 period of analysis. <br />
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