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Biological Data <br />Most of the upper segment is a moderate gradient stream within a confined canyon that allows <br />for some channel movement during high flow events. The substrate consists mostly of cobbles <br />that are regularly moved during high flow events. The narrowleaf cottonwood - sandbar willow - <br />skunkbrush sumac riparian community is vigorous, and shows evidence of new riparian <br />recruitment on sand bars that are formed during high flow events. The upper reach supports a <br />beaver community, and beaver ponds on side channels are common. Fishery surveys indicate <br />that this part of reach provides habitat for a self - sustaining rainbow trout and speckled dace <br />populations. <br />Field Survey Data <br />BLM and CDOW staff used the R2Cross methodology to quantify the amount of water required <br />to preserve the natural environment to a reasonable degree. The R2Cross method requires that <br />stream discharge and channel profile data be collected in a riffle stream habitat type. Riffles are <br />most easily visualized, as the stream habitat types that would dry up first should streamflow <br />cease. This type of hydraulic data collection consists of setting up a transect, surveying the <br />stream channel geometry, and measuring the stream discharge. <br />Biological Flow Recommendation <br />The CWCB staff relied upon the biological expertise of the cooperating agencies to interpret <br />output from the R2Cross data collected to develop the initial, biologic instream flow <br />recommendation. This initial recommendation is designed to address the unique biologic <br />requirements of each stream without regard to water availability. Three instream flow hydraulic <br />parameters, average depth, percent wetted perimeter, and average velocity are used to develop <br />biologic instream flow recommendations. The CDOW has determined that maintaining these <br />three hydraulic parameters at adequate levels across riffle habitat types, aquatic habitat in pools <br />and runs will also be maintained for most life stages of fish and aquatic invertebrates (Nehring <br />1979; Espegren 1996). <br />For this stream, four data sets were collected with the results shown in Table 1 below. Table 1 <br />shows who collected the data (Party), the date the data was collected (Date), the measured <br />discharge at the time of the survey (Q), the accuracy range of the predicted flows based on <br />Manning's Equation (240% and 40% of Q), the summer flow recommendation based on meeting <br />3 of 3 hydraulic criteria and the winter flow recommendation based upon 2 of 3 hydraulic <br />criteria. It is believed that recommendations that fall outside of the accuracy range of the model, <br />over 250% of the measured discharge or under 40% of the measured discharge may not give an <br />accurate estimate of the necessary instream flow required. <br />Table 1: Data <br />Party <br />Date <br />Q <br />250 % -40% <br />Summer 3/3) <br />Winter (2/3) <br />BLM/DOW <br />6/19/2003 <br />2.51 <br />6.3-1.0 <br />out of range <br />2.86 <br />BLM/DOW <br />6/19/2003 <br />2.13 <br />5.3-0.9 <br />out of range <br />1.80 <br />BLM/DOW <br />6/2/2006 <br />8.1 <br />3.2-20.2 <br />3.89 <br />out of range <br />BLM/DOW <br />6/2/2006 <br />8.09 <br />3.2-20.2 <br />5.62 <br />out of range <br />-3- <br />