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<br />the bottom, middle, and top portions of the upper riffle completed the habitat cluster. One of the three <br />cross sections on the upper riffle was located in the shallowest or widest part of the riffle. <br /> <br />Because depth, velocity, and wetted perimeter are more sensitive to flow changes in riffle habitats than <br />other habitat types, the analysis focused on riffles (per advice of the RIP selected expert panel). <br />Accordingly, during the extraordinarily high baseflows in 1997, priority was assigned to sampling riffles, <br />and in some clusters only the riffles were surveyed. Between one and three cross sections were <br />completed in the clusters where only riffles were sampled. <br /> <br />Data were collected at 25 to 30 points along each cross section. These data included habitat type and <br />substrate type (defined by Bisson et al. 1982 and Modde et al. 1991) depth and mean water velocity at <br />each point. Only one stage-discharge measurement was made at each cross section. The predictability of <br />only one stage-discharge measurement was tested by running multiple simulations and increasing the <br />Manning's n at low flow since roughness increases as flow decreases (Gordon et al. 1992). Increasing <br />Manning's n at flows of less than or equal to 40% and less of the measured flow did not change results <br />compared to using the calculated Manning's value. <br /> <br />Hydraulic Simulation <br />The conveyance channel module of the RHABSIM computer program (Payne 1995) was used to develop <br />the stage-discharge relationship for cross sections in the Yampa River. The model predicted changes in <br />channel variables at flows of 1, 10,20,40,60,80, 100, 125, 150,200,250, and 300 cfs by mesohabitat <br />type (run, riffle, and pool). Seven flow and/or channel variables were estimated by the hydraulic model <br />for each cross section by habitat type. The seven variables are defined as: <br />a) Wetted width: width of the stream at the water surface. <br />b) Percent wetted perimeter: The distance along the streambed in contact with the water divided <br />by the distance along the streambed between the grassline of each bank. <br />c) Depth: The vertical distance between the water surface and measured points on the <br />streambed. <br />d) Rise in stage: The difference in the vertical distance from the water surface elevation at a <br />flow of 1 cfs to the water surface elevation at a higher flow. <br />e) Width/depth ratio: A unit-less index of cross-sectional shape, where top width is divided by <br />average depth. <br />f) Cross Sectional Area: Wetted area in square feet determined by multiplying stream width by <br />average depth. <br /> <br />42 <br />