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Last modified
1/26/2010 12:49:49 PM
Creation date
10/11/2006 11:39:58 PM
Metadata
Fields
Template:
Water Supply Protection
File Number
8210.430
Description
Colorado River Basin Organizations-Entities - Gunnison - UVWUA - AB Lateral
State
CO
Basin
Colorado Mainstem
Water Division
5
Date
7/1/2000
Author
DOI
Title
AB Lateral Hydropower Project - Supplemental Environmental Impact Report
Water Supply Pro - Doc Type
Report/Study
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<br />,~~~l(t~ <br />'tru_vvv <br /> <br />Affected Environment & Consequences <br /> <br />3-23 <br /> <br />~ , <br /> <br />3.5.2.2 Development Alternatives <br /> <br />Because hydropower diversions during the summer irrigation season will be relatively <br />small, their effect on water temperatures during that season should be minimal. During <br />the winters, when hydropower diversions are greatest, water temperatures would be <br />reduced between 1 and 2 oC, which could lead to icing in some areas. This would result <br />in somewhat greater icing than has occurred in the past (though significant icing is still <br />not expected). See the PElS for a detailed discussion. Alternatives E-2 and E-3 would <br />have somewhat less impact than the previously approved Alternative E-l. <br /> <br />3.5.3 Impacts of Alternatives - Uncompahgre River <br /> <br />3.5.3.1 Alternative A (No Action) <br /> <br />River temperatures in the Uncompahgre River would remain unchanged under the No <br />Action alternative. Temperatures would be affected by the amount of water withdrawn <br />for irrigation during summer, therefore, average summer temperatures would continue to <br />increase as one moves downstream. During winter, low flows would most likely cause <br />ice cover in slow-moving areas (toward Delta). <br /> <br />3.5.3.2 Development Alternatives <br /> <br />Higher water temperatures during the summer between the South Canal and Montrose <br />would result due to reduced flows. Because flows would still be high between the South <br />and Loutzenhizer Canals, this change would not be significant except in the reach <br />between the Loutzenhizer Diversion and the proposed tailrace where summer water <br />temperatures would likely increase. Temperature would not change between the South <br />Canal and the tailrace during the winter because flow profiles would not change. Water <br />temperatures would be expected to decrease during the summer downstream from the <br />tailrace due to relatively cooler Gunnison River water flowing through the powerplant. <br />Project refinements since 1991 would have little impact on temperature conclusions <br />reached in the PElS. Winter water temperatures would be warmer. Reduced-flow <br />alternatives E-2 and E-3 would, however, have slightly less effect than the previously <br />approved Alternative E. <br /> <br />3.6 <br /> <br />Water Quality <br /> <br />3.6.1 <br /> <br />Existing Conditions <br /> <br />3.6.1.1 <br /> <br />Gunnison River <br /> <br />Data indicates that water quality within the upper portion of the Gunnison River <br />immediately below Crystal Reservoir is a function of the limnology of and releases from <br /> <br />AS Lateral Hydropower Project <br /> <br />July 2000 <br /> <br />, . <br /> <br />.. , <br /> <br />,<- - ~ <br /> <br />-~ <br />.<< <br />t .-' <br />"'i'-'-~ <br />.;he ,;,~"Y~'k~,:il~~i <br />
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