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Table 4. Mean and Standard Deviation of Inflection Points all riffles above Cross <br />Mountain (Strata 6 and 8 combined). <br />Variable vs. Flow <br />Units <br />N <br />NI* <br />MEAN <br />STD <br />C.V. <br />Wetted Perimeter <br />(cfs) <br />53 <br />1 <br />185 <br />87.52 <br />0.47 <br />( %) <br />53 <br />1 <br />59% <br />0.13 <br />0.23 <br />Wetted Width <br />(cfs) <br />53 <br />1 <br />207 <br />80.93 <br />0.39 <br />(ft rT <br />53 <br />1 <br />207 <br />58.00 <br />0.28 <br />Average Depth <br />(cfs) <br />48 <br />6 <br />146 <br />64.60 <br />0.44 <br />(ft) <br />48 <br />6 <br />0.67 <br />0.26 <br />0.39 <br />Change in Stage <br />(cfs) <br />53 <br />1 <br />157 <br />70.10 <br />0.44 <br />(ft) <br />53 <br />1 <br />1.21 <br />0.44 <br />0.36 <br />Width /Depth Ratio <br />(cfs) <br />54 <br />0 <br />182 <br />63.86 <br />0.35 <br />54 <br />0 <br />325 <br />181.28 <br />0.56 <br />Average Velocity <br />(cfs) <br />54 <br />0 1 <br />174 1 <br />67.33 <br />1 0.39 <br />(ft/s) <br />54 <br />0 1 <br />1.58 1 <br />0.59 1 <br />0.37 <br />Tables 3 in Appendix V.A and VI. A show the stream width for each of the riffle <br />cross sections for Strata 6 and Strata 8 respectively. The average stream widths for each <br />flow were plotted (Figures 5 of Appendix 5A and 6A) and the inflection point for that <br />curve was identified using the same approach as individual cross sections (Table 5). The <br />inflection points for Strata 6 and Strata 8 were 80 cfs (43% wetted perimeter) and 200 cfs <br />(57% wetted perimeter), respectively (Table 5). The inflection point determined by this <br />method (Method B) produced a lower value than the mean of individual inflection points <br />(Table 4). <br />The t -test was used to determine if there was a significant difference between <br />wetted stream widths for Strata 6 and Strata 8 (Appendix VII, Table 1). The null <br />hypothesis was that mean stream widths were similar between strata and it was not <br />rejected at an alpha of 0.05. <br />19 <br />