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1 <br /> <br /> <br /> <br /> <br /> <br /> <br />t <br />u <br /> <br />i <br /> <br /> <br /> <br /> <br />value has been used to provide estimates of water availability. For rights already adjudicated and <br />currently used for domestic purposes, a S percent CU rate is used. <br />It is important to note that the SO percent CU rate assumed does not imply that the District will divert <br />SO percent of the decreed rate of a right, but rather only SO percent of what that right has historically <br />diverted for agricultural use. For example, the District owns 1.625 cfs in diversion rights in the <br />Welch Ditch on Coon Creek. If the rights diverted year-round at this rate, they would divert 1176 <br />ac-ft. However, historical irrigation diversions have only occurred in April through October, <br />averaging about 274 ac-ft/yr. At the SO percent rate, the District will divert an average of 137 ac- <br />ft/yr after the transfer, or less than 12 percent of the total volumetric decreed capacity of the ditch. <br />Any remaining water which the rights would have diverted historically must be left in the stream to <br />satisfy junior and conditional water rights which are entitled to protection of stream flows that reflect <br />historical conditions. <br />CU diversions are shown in Tables 3.1 and 3.2 as CU diversions to Ute Water (or WTP) and CU <br />diversions by agriculture. Under baseline conditions, only the Mason and Eddy Ditch right is being <br />utilized by Ute Water for municipal purposes, providing S09 ac-ft/yr. However, the District's other <br />agricultural rights have diverted a CU rate of 623 ac-ft/yr for irrigation and domestic use. Under the <br />future scenario, all District rights will be transferred with 1132 ac-ft/yr available for diversion to the <br />municipal system. However, modeling results indicated that the 623 ac-ft/yr of CU water diverted <br />to agriculture under baseline conditions will not always be fully utilized for municipal use under <br />future conditions. Though in many years the full amount will be utilized, an average of 129 ac-ft/yr <br />will not be diverted when excess supplies prevent full utilization of all supplies. Note that the CU <br />diversions result in no net future depletions to the basin, since diversions will be limited to historical <br />CU. Under Scenario C, net depletions will actually be 129 ac-ft/yr less due to under-utilization of <br />the transferred water. While it is true that diversions by these rights result in depletions to the <br />streams, such depletions have historically occurred from their former use and are not a result of the <br />District's operations. <br />3.2. S Jerry Creek Reservoir Evaporation <br />Net evaporation from the Jerry Creek Reservoirs adds to the overall depletion to the Colorado River <br />system. Net evaporation is estimated as the additional evaporation that results from the operation <br />of the reservoirs, which is in excess of the normal evapotranspiration that would occur without the <br />existence of the reservoirs. Precipitation over the surface of the reservoirs is also considered in <br />calculating net evaporation. <br />The Jerry Creek Reservoirs are generally utilized only under drought conditions and remain nearly <br />full at all other times. Evaporation averages 670 ac-ft/yr under baseline conditions. Under future <br />conditions, the reservoirs would be utilized more frequently due to larger demands. This results in <br />less full reservoirs,~less exposed surface area, and reduced evaporation. This is indicated by the <br />slightly lower average evaporation of 661 ac-ft/yr in the future scenario resulting in a minimal <br />decrease in net depletions. <br />CDM Camp Dresser & McKee <br />0:18047-I 101DOC1APPEND-B.DOC B-S <br />