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WSP08403
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Last modified
1/26/2010 2:48:02 PM
Creation date
10/12/2006 2:58:08 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8220.101.17
Description
Glen Canyon Dam/Lake Powell
State
AZ
Basin
Colorado Mainstem
Date
1/1/1999
Author
BOR
Title
GCD Modifications to Control Downstream Temperatures: Plan and Draft Environmental Assessment
Water Supply Pro - Doc Type
EIS
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<br />Chapter III Affected Environment and Environmental Consequences 25 <br /> <br />competition and predation by non-native fish, and cold-water releases and habitat <br />fragmentation from Glen Canyon Dam. <br /> <br />The biological foundation of the aquatic system in the post-dam Colorado River below Glen <br />Canyon Dam is Cladophora glomera/a, a filamentous green alga. Clear river conditions <br />created by the dam make the abundant growth of Cladophora possible. Together, <br />Cladophora, diatoms, and associated invertebrates (Gammarus and insects) provide an <br />important food source for other organisms in the food chain. <br /> <br />River Temperatures - Average monthly river temperatures predating the dam ranged from <br />just above freezing to about 260C (780F). Records show that present release temperatures <br />from the existing power intakes vary <br />little from 80C (460F). As the river <br />flows downstream through the warm <br />summer desert environment, water <br />temperatures increase about I oC for <br />every 30 miles traveled. During the <br />summer, temperatures increase from <br />80C near the dam to about l60C <br />(61 OF) at mile 240. This is below the <br />last aggregation of chub near <br />Diamond Creek and far downstream <br />of most of the known aggregations of <br />humpback chub. <br /> <br />The proposed temperature control <br />alternative would allow a <br />summertime release of l50C (590F). <br />It is expected that this would greatly <br />improve growth rates for rainbow <br />trout in the river reach between the <br />dam and Lees Ferry. Then as the <br />water flows downstream, <br />temperatures would increase into the <br />range (160C-220C) where they are suitable for most all of the nine known aggregations of <br />humpback chub. <br /> <br />234567 <br /> <br />8 <br /> <br />8 <br /> <br /> <br />25 -: <br />, <br /> <br />I <br />-20 --i <br />U <br />- <br /> <br />! 16 -+- <br />,. <br />- <br />I! .' <br />&,10 -I <br />E I <br />{!. 6~ <br /> <br />- <br /> <br />o <br />Glen <br />Canyon <br />Dam <br /> <br />HSV8SU <br />Creek <br /> <br />Diamond <br />Creek <br /> <br />Little <br />Colorado <br />River <br /> <br />Figure 6 - Water temperatures increase with <br />distance below Glen Canyon Dam (for 80C and <br />l50C release temperatures). Also shown are the <br />locations of the 9 aggregations of endangered, <br />humpback chub. <br /> <br />Lake Temperatures - A computer modeling study of Lake Powell was conducted by <br />Reclamation's Denver Technical Service Center to evaluate potential changes which might <br />impact critical resources in Lake Powell. Surface temperatures during the winter are critical <br />to the survival of the threadfin shad, an important forage fish for the Lake Powell sport <br />fishery. Threadfin shad are very near their temperature tolerance during the winter season. <br />Surface temperatures in Lake Powell vary from about 100C (500F) in winter to over 250C <br />(770F) in summer. Surface temperatures in the winter below 100C (50 OF) could cause <br />problems for threadfin shad. <br />
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