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i <br />rights as assumed in the CPFD (i.e., South Platte flow development assumed to occur at 5% in <br />April, 40% in May, 50% in June, and 5% in July). The call records used in this analysis are from <br />the records of the Colorado State Engineer's Office. The initially assumed % water supply source <br />mix by region of the CPFD, Paragraph B, was for the period 1998 through 2002. As listed in <br />Figure 2, the weighted % of time for a July 1, 1997 water right to be in-priority is 53% for 1998- <br />2002 versus 33% for 1998-2006. <br />Figure 2 shows the analysis for adjusting the % water supply from native South Platte flow <br />development by region. Colorado proposes for the Initial Reporting Period of two years to use an <br />average for the 1998 through 2006 period for the % of time that a July l, 1997 priority water right <br />would be available for diversion. The analysis adjusts the initially assumed % of native South <br />Platte flow development by region by the ratio of % time between the 1998-2006 period (33%) to <br />the 1998-2002 period (53%) that a July 1, 1997 water right would be in-priority--that ratio being <br />33% / 53% or 62%. The results of this analysis changes the % water supply from native South <br />Platte flow development from 10°/o to 6.2% for the North region, 15% to 9.3% for the Central <br />region, and 10% to 6.2% for the South region. If the drought continues, Colorado in the future will <br />propose adjusting this percent even more to reflect the lack of native water for junior water rights <br />by using a more recent period average only such as 2003-2006 or some other rolling average to <br />determine monthly water availability by call records. <br />With these adjustments downward for the % water supply from native South Platte flow <br />development, Colorado proposes that there is a corresponding increase in % water supply from <br />water reuse. Colorado has begun a data collection effort with the major municipal water providers <br />to better define the °/o water source mixes from the six categories of water sources. Initial <br />indications from major providers is that water reuse is increasing along with in-basin agricultural <br />conversions. Note that the water reuse sources have a net depletive effect for all months while in- <br />basin agricultural conversions have a net accretive effect for all months as shown in Figure 1. <br />Figure 3 is similar to Figure 1 but the analysis has been redone using the adjusted % water supply <br />for the source of native South Platte flow development and the source of water reuse. Table 3 lists <br />a total of 26,882 acre-feet of net accretions for the winter months of October through April and <br />lists a total of net depletions in May and June of 2,713 acre-feet. At the bottom of Figure 3 is the <br />modified % water supply source mix by region. The transit loss assumptions used in this <br />modified analysis of Figure 3 are the same as those used for the original analysis in Figure 1 and as <br />approved in the CPFD in Paragraph C. <br />The transit loss assumptions in the CPFD in Paragraph C are based on the administrative losses <br />assigned by the Colorado State Engineer for routing reservoir releases downriver (i.e., protected <br />flows). Colorado is sttidying new transit loss factors that better reflect the physical situation of <br />water flowing downriver subject to rediversion and subsequent return flows (i.e., unprotected <br />flows). The Water Conservation and Water Supply Study dated December 1999 of the Platte <br />River Research Cooperative Agreement contained Appendix D written by the Water Management <br />Coinmittee, which dealt with monthly loss factors as related to water being diverted by canals. <br />Accretions and depletions from new water related activities would be diverted by downstream <br />canals as such water flows from the Front Range downriver to the Colorado-Nebraska Stateline. <br />The % diversion loss factors listed in Appendix D are gross values where lagged groundwater and <br />surface water returns are not considered as noted in Appendix D, which can result from diversions <br />2