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Last modified
1/26/2010 12:25:52 PM
Creation date
10/11/2006 9:43:19 PM
Metadata
Fields
Template:
Water Supply Protection
File Number
8220.101.10.D
Description
Colorado River-Water Projects-Glen Canyon Dam/Lake Powell-Glen Canyon Adaptive Management-
Basin
Colorado Mainstem
Water Division
5
Date
6/17/2005
Author
Korman-Hazel-Melis
Title
Effects of the Experimental Fluctuating Flows from Glen Canyon Dam in 2003 and 2004 in the Early Life History Stages of Rainbow Trout in the Colorado River
Water Supply Pro - Doc Type
Report/Study
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<br />" <br /> <br />,. 00620 <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />any young-of-year rainbow trout in Nankoweep Creek during the April 2004 survey and saw <br />only limited spawning activity. <br /> <br />Relative to Glen Canyon, we found very few YoY rainbow trout between Lees Ferry <br />and the LCR confluence during the June and August 2004 surveys. Across gear types, <br />densities ofYoY rainbow trout in Glen Canyon were 12-fold higher than in Marble Canyon in <br />June and IS-fold higher in August. Densities ofYoY in Marble Canyon were highest in the <br />IS-mile reach immediately below Lees Ferry and increased between June and August in the <br />first 30 miles downstream of Lees Ferry. Length-at-age and hatch date distributions for YoY <br />trout caught in Glen and Marble Canyons were very similar. These data suggest that the <br />limited number of Yo Y caught in Marble Canyon in 2004 likely originated from Glen <br />Canyon. The reach between river mile 4S and 60 had the lowest densities ofYoY fish of all <br />the reaches in Marble Canyon with only 14 and 4 YoYs caught in June and August, <br />respectively. Although this reach had the greatest amount of spawning habitat in the mainstem <br />and a tributary that could support a substantial amount of spawning (Nankoweep Creek), these <br />habitats clearly did not produce a significant number of viable young in 2004. <br /> <br />If our surveys in Marble Canyon are representative of reproductive conditions for <br />rainbow trout in future years, it is unlikely that flows from GCD can be used to reduce the <br />survival rate of young trout in this reach. There was virtually no spawning habitat above 8 <br />kcfs that could potentially be dewatered. The limited area of spawning habitat that was <br />observed was well below S kcfs. The very low densities ofYoY observed in 2004 indicate <br />that recruitment to the Marble Canyon population is already quite low, thus the incremental <br />effect of destabilizing shoreline habitats would be very small. Our results cannot be used to <br />definitively determine the origin of the current population of rainbow trout in Marble Canyon. <br />It is possible that these fish originated in Marble Canyon and that the limited reproduction we <br />observed in 2004 was a unique occurrence. Continued documentation of Yo 'y absence in <br />, Marble Canyon over the next few years, combined with observations of a constant or <br />increasing adult population above the mechanical removal reach, would provide strong <br />evidence that this population is supported by downstream dispersal from Glen Canyon. <br />Alternatively, if downstream dispersal is not a significant process, and if the lack oflocal <br /> <br />v <br />
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