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Af % <br />Considerations Related to Equal Monthly Volumes <br />• The AMWG developed twelve resource goals in order to maintain the "balance" between <br />impacts to electrical power and improvement in downstream environmental resources. <br />Experimentation should be focused on environmental improvement while minimizing the <br />impact to the electrical power resource (EIS ROD). <br />• The proposal for equalized monthly volumes goes against the this approach by focusing <br />exclusively on sediment conservation without consideration of other downstream resources and <br />without attempting to accomplish environmental improvement at minimum power loss. <br />• The necessity for a transition to equalized monthly volume operation is not supported by the <br />scientific evidence: <br />• The sediment modeling results presented by GCMRC to the TWG at its January annual <br />reporting meeting compared sediment transport under MLFF (with fall steady flows), <br />MLFF without daily fluctuations, equalized monthly volumes (EMV), and steady year - <br />round flows. Given a starting input of 1.5 million metric tons of Paria sand, the results <br />indicate that all, or nearly all, of the sand would be vacated by the end of one year <br />under all four scenarios.' <br />• When comparing sediment transport between MLFF and EMV, less sediment appears to <br />be vacated under MLFF than EMV for the initial four months. For the remaining 8 <br />months of the modeling period, the two trajectories are nearly identical. The EMV line <br />actually crosses the zero- line (pre -input sediment condition) before the MLFF line. Only <br />in the last two months of the year does the MLFF line dip below the EMV line. <br />o The model is sensitive to the timing and amount of sediment input from the Paria River <br />and could affect the results and the comparison among scenarios. <br />o Sediment input from the Little Colorado River (LCR), or other side drainages, could affect <br />comparisons among scenarios that only consider input from the Paria River. <br />o Because most of the sediment is found below 8,000 cfs (up to 90%), it is unclear how <br />total sediment relates to habitat availability under MLFF or EMV. <br />o Sediment grain size greatly affects transport rates, and is not considered under the <br />analysis by GCMRC. <br />o It is likely that HFEs can increase sediment retention over the short-term and that flows <br />post -HFE will transport sediment out of the system. It is unclear what the relationship <br />between sand inputs, frequency of HFEs, and flow operations should be based on <br />current modeling results. Because sediment inputs are uncertain, this creates even <br />greater uncertainty in speculating whether one flow regime is likely to meet resources <br />goals. <br />' The graphical representation of the modeled comparison among four operational scenarios: Example — <br />Evaluation of dam operations, is attached. <br />