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<br />, <br />" ' <br /> <br />(cfs). Bank-backwater numbers were maximized at 1101 cfs, <br />channel-backwater numbers were maximized at 1687 cfs and total backwater <br />numbers were maximized at 1687 cfs. Figure 7 (Appendix A) presents <br />backwater size distribution versus flow (cfs). The <20m2 size class was <br />maximized at 1687 cfs, the >20m2<200m2 size class was maximized at 1687 <br />cfs, the >200m2<5002 size class was maximized at 1101 cfs, the <br />>500m2<1000m2 was maximized at 1101 cfs, and the >1000m2 class was <br />maximized at 1381 cfs. <br /> <br />Ouray <br /> <br />Table 5 (Appendix A) presents the area of each class for each flow at <br />the Ouray site. The relationship between flow and backwater area is not <br />as well defined at the Ouray site as it is at the Island Park and Jensen <br />sites. There is a significant increase (122%) in backwater area from <br />5,260 cfs [18,789 m2 (4.6 ad] to 2,423 cfs [41,722 m2 (10.3 ac)]. <br />Backwater area increased somewhat at 1,773 cfs and again at 1,667 cfs <br />where backwater area was maximized at 52,057 m2 (12.9 ac). Large <br />decreases occurred between 1,687 cfs and 1,430 cfs (23%) and between <br />1,430 cfs and 1,381 cfs (23%). Finally, backwater area increased from <br />30,835m2 (7.6 ac) at 1,381 cfs to 41,177 m2 (10.2 ac) at 1,101 cfs. <br />Isolated pool area increased significantly at the lower flows and was <br />maximized at 1,381 cfs with 31,182 m2 (7.7 ac). <br /> <br />Table 6 (Appendix A) presents backwater number, size distribution, area, <br />and average backwater size for each flow at the Ouray site. Total <br />backwaters were maximized at 1,381 cfs (73) and were also high at 1,687 <br />cfs and 1,430 cfs with 70 and 66 backwaters, respectively. The lowest <br />numbers of backwaters occurred at 5,260 cfs (44), 1,101 cfs (57), and <br />2,423 cfs (58). With the exception of 5,260 cfs, there were more <br />bank-backwaters than channel-backwaters at each flow. As occurred at <br />the Island Park and Jensen sites, the >20m2<200m2 size class contained <br />the most backwaters, both bank and channel. However, the Ouray site had <br />a disproportionately higher number of very large backwaters (>1,000 m2), <br />at all flows except 5,260 cfs. The large nature of backwaters at the <br />Ouray site may account for the different relationship between flow and <br />backwater area than at Island Park and Jensen. <br /> <br />Closer analysis of individual backwaters indicates that a few extremely <br />large backwaters (5,000 - 10,000 m2) which occurred at 1,687 cfs did not <br />occur at lower flows, therefore, backwater area was much lower at these <br />flows. The average size of all backwaters at the Ouray site was much <br />larger than at Island Park and Jensen, ranging from 422 m2 at 1,381 cfs <br />to 831 m2 at 1,773 cfs. <br /> <br />Figure 8 (Appendix A) presents backwater area (m2) versus flow (cfs). <br />Bank-backwater size was maximized at 1687 cfs, channel-backwater size <br />was maximized at 2423 cfs and total backwater size was maximized at 1687 <br />cfs. Figure 9 (Appendix A) presents numbers of backwaters versus flow <br />(cfs). Bank-backwater numbers were maximized at 1430 cfs, <br />channel-backwater numbers were maximized at 1687 cfs and 1381 cfs, and <br />total backwater numbers were maximized at 1381 cfs. Figure 10 (Appendix <br />A) presents backwater size distribution versus flow (cfs). The <20m2 <br />size class was maximized at 1381 cfs, the >20m2<200m2 size class was <br />maximized at 2423 cfs and 1381 cfs, the >200m2<5002 size class was <br />