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<br />3.0 Scientific Basis And Underlying Principles <br /> <br />The fifth and sixth principles are based <br />on the "reset theory" of floodplain management, <br />which allows floodplains to inundate and <br />remain flooded for at least 2 years, then <br />desiccate. This "reset theory" serves the <br />fundamental ecological functions of providing <br />connectivity for fish entrainment and <br />movement, stimulated floodplain production, <br />and periodic desiccation to reduce effects on <br />nonnative fishes. This "reset theory" has not <br />been thoroughly tested, but research on various <br />components of the strategy indicate a high <br />probability of success. <br /> <br />3.3 Green River Flow Recommendations <br /> <br />3-3 <br /> <br />April 2004 <br /> <br />Ecological functions of "reset theory" <br /> <br />1. Periodic inundation allows access <br />to drifting larval razorback sucker <br />and escapement of adults, <br />2. Periodic inundation/desiccation <br />stimulates food production and <br />freshens water quality, and <br />3. Periodic desiccation strands and <br />kills nonnative fishes <br /> <br />Flow recommendations for the Green River downstream of Flaming Gorge Dam (Muth et <br />al. 2000) are designed to be implemented, evaluated, and revised according to findings of <br />scientific investigations and through NEP A and ESA compliance. Flow recommendations are <br />made for summer through winter base flows and for spring peaks for each of three longitudinal <br />river reaches, and are based on five hydrologic conditions that reflect annual river volume (Table <br />3-1). The basis for the general recommendation is that peak flows should be of the magnitude, <br />timing, and duration to provide floodplain inundation in the Ouray reach for at least 2 weeks in 4 <br />of 10 years and at least bankfull flows in 1 of 2 years. Under average hydrologic conditions <br />(30-70% peak exceedence), 18,600 cfs (527 m3/s) should occur in 1 of2 years and be maintained <br />for at least 2 weeks in 1 of 4 average years. Average peak flow ofthe Green River near Jensen <br />(RM 316), 56 years of record through 2000 (pre- and post-Flaming Gorge), is 19,706 cfs; this is <br />the instantaneous peak and does not reflect duration. <br /> <br />Area of floodplain inundation for different river flows was determined for portions of the <br />middle Green River using a HEC-2 step backwater model (F10 Engineering 1996). This model <br />determined that for existing conditions (without levees removed) in the Ouray reach (River Mile <br />[RM] 252-265), the area of floodplain inundation increases rapidly at flows exceeding about <br />18,600 cfs (Figure 3-1). With existing levees <br />removed, flooding in the Ouray reach would be <br />initiated at 13,000-16,000 cfs resulting in about 5,400 <br />acres of floodplains. Similar relationships were found <br />from aerial photography for existing conditions from <br />Pariette Wash to Split Mountain (Bell et al. 1998). <br />The majority ofthese floodplains are terraces that fill <br />and drain with river stage and may not hold water and <br />fish for long time periods and therefore, may not <br />currently be suitable nurseries for razorback sucker. <br /> <br />Relationship of flow to floodplain <br />area from Pariette Wash to SpIt <br />Mountain (240- 319; Bell et ale 1998) <br /> <br />. <br /> <br />5,904 acres at 20,000 cfs <br />9,550 acres at 22,000 cfs <br />13,927 acres at 25,000 cfs <br /> <br />. <br /> <br />. <br />