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<br />SECTIONTHREE <br /> <br />Whooping Crane <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />1 <br />I <br /> <br />Habitat criteria applied in the Biology Work Group model were lack of disturbance, channel <br />width, width of water in the channel, and a function that evaluates a range of water depths (both <br />shallowly submerged sandbars with deeper water). Whooping crane authorities agree that <br />whooping cranes select roosting sites on the basis of the security offered by the site(s) (Shenk <br />and Armbruster 1986; FWS 1987b). The security value of whooping crane riverine roost sites is <br />a function of the following habitat criteria: <br /> <br />I. UnobstrUcted channel width: Whooping cranes require roosting sites free of visual <br />obstructions, or an unobstructed view, presumably to allow them to see approaching <br />predators. <br /> <br />2. Presence of water: Whooping cranes roost standing in water. The availability of water is an <br />inherent requirement in sandhill and whooping crane behavior. <br /> <br />3. Depth of water: Recent sightings indicate whooping cranes use shallow submerged areas <br />bounded by deeper water. On the Platte River, water conditions provide shallowly <br />submerged sandbars bounded by deeper water in main channels (FWS 1987b, 1993; Faanes <br />et al. 1992). <br /> <br />4. Water width: In addition to simply being present and having adequate depths, the expanse of <br />water surrounding the roost must be sufficiently wide to provide a sense of isolation and <br />security (Shenk and Armbruster 1986; FWS 1987b). Water width is defined by whooping <br />crane authorities as being the sum of all wetted widths (water-filled subchannels) within the <br />unobstructed ""idth. <br /> <br />The suitability indices of the roost habitat model were updated and refined as additional data <br />became available (FWS 1993; Carlson et al. 1990; Carlson et aI. 1994). Two alternative models <br />(C4R and C5R) were eventually produced (Carlson et aI. 1994) and included as a figure in the . <br />Kingsley Dam Biological Opinion (FWS 1997). They are based on different methods of <br />estimating habitat suitability related to depth. Both show a reduction in roosting habitat below <br />2,400 cfs, with a gradual reduction as flows decrease to 2,000 cfs, and more rapid reductions in <br />habitat as flows decrease below 2,000 cfs (Figure 3-5 top). Empirical data collected from <br />whooping crane roost sites supports the model (Figure 3-5 bottom), with the proponion of <br />whooping crane stopovers being disproportionately high between 2,000 to 2,500 cfs. <br /> <br />The existing whooping crane roost habitat model was based on the roost habitat data available at <br />the time and on the expert opinions of whooping crane scientists. Model C4R is currently being <br />updated and validated by the Midcontinent Ecological Science Center of the USGS (FWS 1999). <br />This work includes incorporation of new data from numerous recent whooping crane roost sites <br />and other work to improve the model and produce curves relating habitat to flow. The draft <br />report is scheduled to be distributed for peer review in October 1999. <br /> <br />The updated whooping crane roost habitat model may be used to develop baseline indices of <br />habitat quality for each bridge segment. A sample data presentation is provided in Table 3-5. <br />However, application of the model to individual bridge segments would likely require collection <br />of additional data to represent current baseline conditions. The model incorporates three <br />suitability indices-water depth, water width, and channel width. The fourth indicator <br />(disturbance) functions as an on- or off-switch. Updated information on channel width will be <br />URS IJnIi1Iet Wb..4waI1f CIpde <br />3-8 68FC097286OO1r1.doc 612/1999(9:52 AM)/URSGWCFS12 fetIeraI SeI ~ <br />