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Last modified
1/26/2010 3:16:29 PM
Creation date
10/12/2006 4:47:35 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8240.200.48.D.3
Description
Wolford Mountain
State
CO
Basin
Colorado Mainstem
Water Division
5
Date
3/12/1998
Title
Wolford Mountain Biological Opinion and attached MOU
Water Supply Pro - Doc Type
Biological Opinion
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<br />29 <br /> <br />summer. Although fast runs and riffles were used during the summer. they were <br />not used during the winter. The colder water temperatures in winter which <br />cause lower metabolic rates may account for the avoidance of high velocity <br />sites. Absolute area of pools increases as flows decrease and slow runs lose <br />velocity. Because Qsmundson et al. (1995) did not sample fish during low <br />flows in the winter (because there were no low flows), they could not <br />determine if pools would still be preferred in the winter at lower flows. <br />Therefore. they recommended winter flows at the moderate flow level which <br />maximized weighted area of preferred habitats, <br /> <br />Spring (April-July): Qsmundson and Kaeding (1989) reported that squawfish use' <br />of low velocity habitats such as backwaters and flooded gravel pits is - <br />greatest during the spri~g runoff. It is believed that squawfish use these <br />habitats during the runoff to escape the high velocity, low temperature flows <br />of the main channel. Because backwaters. flooded gravel pits. and other low <br />velocity habitats are considerably warmer than the main channel during the <br />runoff. these habitats allow squawfish to extend their growing season <br />substantially. The earlier warming of these habitats may also be important in <br />enabling squawfish to reach spawning condition by the time flow and <br />temperature in the main channel are optimum for spawning. Qsmundson et al. <br />(1995) reported that the numbers of backwaters and flooded gravel pits <br />increases with increasing spring flows (although the number of backwaters <br />eventually decreases as increasing flows convert backwaters to sidechannels. <br />the number of other low velocity habitats likely increases as increasing flows <br />inundate additional bottomlands). The decrease in the magnitude, duration. <br />and frequency of high spring flows. then. decreases the quantity and the <br />duration and frequency of availability of important low velocity. higher <br />temperature habitat in the spring. This could be affecting squawfish growth <br />and spawning success, <br /> <br />Also. the quantity and frequency of availability of inundated floodplain <br />depressions used by razorback suckers for spawning is dependent on the <br />magnitude and frequency of spring flows necessary to inundate these areas, <br />The decrease in the magnitude and frequency of spring flows necessary to <br />inundate floodplain depressions is believed to be largely responsible for poor <br />razorback sucker spawning success. <br /> <br />Biolooical Environment <br /> <br />Food supply, predation. and competition are important elements of the <br />biological environment. Food supply is a function of nutrient supply and <br />productivity, which could be limited by the presence of contaminants. The <br />modification of flow regimes, water temperatures, sediment levels. and other <br />
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