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Letter Regarding Cumulative Effect Report for Colorado's Plan for Future Depletions
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Letter Regarding Cumulative Effect Report for Colorado's Plan for Future Depletions
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Letter to PRRIP Governance Committee Regarding Cumulative Effect Report for Colorado's Plan for Future Depletions
State
CO
NE
WY
Basin
South Platte
Water Division
1
Date
4/30/2009
Author
Ted Kowalski Alan Berryman Jon Altenhofen
Title
Letter to PRRIP Governance Committee Regarding Cumulative Effect Report for Colorado's Plan for Future Depletions
Water Supply Pro - Doc Type
Correspondence
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wells. In the future SPWRAP plans to work with other augmentation plans /recharge groups upstream of Sterling to <br />the Morgan - Washington County line. <br />All of these plans have been decreed in Colorado Water Court and accounting procedures are reviewed by the <br />Division Engineer's office. Inflows to all recharge areas are recorded with flumes and meters approved by the <br />Water Commissioner and pond evaporation is subtracted per decreed procedures. Net pond evaporation in the <br />winter months is typically around 2;% of inflows. All recharge areas have decreed groundwater flow parameters <br />(i.e., river and boundary distances, harmonic transmissivity, specific yields or SDF values). The decreed AWAS <br />(Alluvial Water Accounting System; I)ttp ids. colostate .edu /index.11tail ? / projects solatt software utilizing <br />Glover methodology developed by the Integrated Decision Support Group -IDS at CSU is used to compute the <br />lagged groundwater return flows /accretions for the net groundwater recharge at the ponds (i.e., net recharge is <br />measured inflows minus net pond evaporation). <br />Table 4 is a summary of the mitigation accounting for the initial reporting period of 2007 and 2008. Block 1 of <br />Table 4 lists on an irrigation year (Nov -Oct) basis the accretions from the CPFD analysis and the depletions in <br />May /June (depletions are those from Figure I and 1B). CPFD accretions are utilized at the Tamarack SWA <br />recharge project (Block 2) with any remaining CPFD accretion (Block 3) utilized prorata in the other recharge <br />projects. Block 4 of Table 4 lists the total net recharge in the other recharge projects while Block 5 lists the amount <br />of the remaining CPFD accretions after Tamarack -SWA diversions that are diverted by the other projects. Block 6 <br />shows that not all diversion by the other projects are counted or "colored" as coming from CPFD accretions. Block <br />7 computes the quantity of CPFD accretions utilized and shows that most all are diverted. Block 8 is the output from <br />the AWAS groundwater model and lists the lagged groundwater return flows from the recharge of the CPFD <br />accretions with totals for May /June. These lagged return flows from recharging CPFD accretions are from recharge <br />activities starting in 1998 and following these same accounting procedures of "coloring" actual net recharge <br />diversions as CPFD accretion water. For 2007, 2008 the average May /June replacement was 2,502 acre -feet, which <br />on an average annual basis adequately replaces the May /June average CPFD deficit of 1,642 acre -feet listed in <br />Block 1. Replacements are higher in 2007 because it was a wetter May /June and the other augmentation /recharge <br />plans had more excess because their augmentation needs were less. Lagged groundwater return flows from the <br />recharge of CPFD accretion return to the river in all months. As noted in Block 1 and 8 of Table 4, some of these <br />return flows in March 2007 and March 2008 are rediverted by the projects further downstream if they have <br />remaining capacity in an effort to "recycle" more of the CPFD accretion water and have it return in the May /June <br />months for CPFD depletion mitigation. <br />Note that the reason the CPFD has depletive effects in May and June is because the main diversion of native South <br />Platte flows under junior water rights occurs in these two months of snowmelt runoff. The CPFD analysis as <br />described earlier is based on an average 2005 -2009 call scenario for the determination of an average water source <br />percent from new native South Platte flows but it is the wetter years like 2007 where more diversions under a junior <br />water right will occur so having more replacement in 2007 as shown in Table 4 Block 8 is a good mitigation buffer. <br />The CPFD analysis will be updated if a running average on calls indicate a consistently wetter or drier period <br />average than assumed for 2005 -2009. <br />7 <br />
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