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COMMENTS OF U.S. ENVIRONMENTAL PROTECTION AGENCY <br />EPA -38 Itwice the other variable). For the purposes of the calibration a <br />(cont.) i slope near one and an intercept near zero is desirable. <br />EPA -39 2. In examining the calibration curve (Figure A -6), the model <br />appears to underpredict the reservoir contents for the period <br />1980 to 1985. The final EIS should provide an appropriate <br />discussion, indicating the reason for this underprediction and <br />commenting on its significance. <br />EPA-40 3. To assess the magnitude of potential errors in the simulated <br />vs measured lake levels, the maximum difference for 1988 was <br />extracted from Figure A -6 to be approximately 100 KAF for the <br />month. This converts to over 1600 cfs. This appears to <br />overestimate water in storage, which means less water was <br />actually available for release than was anticipated. Can the <br />model calibration be refined to yield better results? The <br />analysis should include standard errors. <br />EPA-41 4. Calibration has not been presented for the various segments <br />of the system for which discharge data were available. These <br />should be provided where data are available, and especially in <br />x the reach between Overton and Grand Island where critical <br />decisions are based on model results. <br />v� <br />0' EPA-42 5. Page A -5. The relationship of historic and daily flows at <br />the Overton gage were apparently used to calculate daily flows <br />from simulated monthly flows for all alternatives. Considering <br />the potential sources of errors in the model and the fact that <br />such a relationship is likely to be different for each <br />alternative, the method may not be appropriate. <br />EPA-43 6. Evaporation is an important sink of water especially in the <br />reservoirs. The final EIS should include a section on <br />evaporation. Assuming that evaporation pan data are available, <br />the DEIS should provide the pan coefficient used to approximate <br />lake evaporation. <br />Economic Analysis <br />EPA44 1. The economic analysis (Section 2.13) and supporting <br />appendices E and G lack clarity and description. As a result, it <br />is difficult to determine what the economic and monetary values <br />presented in the RDEIS represent and whether they are accurate. <br />For example, Appendix G provides a set of computed values with no <br />description of the assumptions, components, or the method of <br />computation. In addition, there is no discussion of the data <br />inputs used to generate the Appendix G tables. Without including <br />such information, it is difficult to make an independent <br />determination regarding the accuracy or relevance of the <br />information presented. <br />22 <br />RESPONSES TO U.S. ENVIRONMENTAL PROTECTION AGENCY <br />EPA -39 Allowable reservoir levels were higher in the early 1980's. <br />Subsequent calibration in the SDEIS reflected higher allowable <br />levels in the early 1980's followed by lower values in the later <br />1980's and in the 1990's. <br />EPA -40 Standard errors were included in the SDEIS. The model remains <br />an imperfect tool, not capable of capturing all decisions made by <br />the Districts. <br />EPA41 Flows at Overton were added to the calibration analysis in the <br />SDEIS. <br />EPA -42 Additional work was performed by the staff to refine the daily <br />flow estimates. Staff recognize that these represent only estimates. <br />EPA43 Monthly evaporation losses were included in the original <br />OPSTUDY model (developed by the Bureau of Reclamation). <br />Staff made no new adjustments to the evaporation data. The <br />methods used to develop input values were documented by Central <br />(Central, 1988). Evaporation losses averaged 63.1 KAF in the <br />Baseline. <br />EPA -44 The economic analysis and cost estimates have been revised, and <br />associated tables reformatted and updated. <br />