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Last modified
8/11/2009 11:32:58 AM
Creation date
8/10/2009 5:11:21 PM
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UCREFRP
UCREFRP Catalog Number
9700
Author
Hayes, J.W., K.E. LaGory and G.L. Burton.
Title
Consideration of site-specific floodplain inundation thresholds in implementing peak flow magnitude and duration recommendations in the middle Green River, Utah.
USFW Year
2005.
USFW - Doc Type
Argonne National Labortory, Argonne, Illinois.
Copyright Material
NO
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<br />Green River Floodplain Inundation <br /> <br />13 <br /> <br />June 2005 <br /> <br />4 IMPLICATIONS OF FLOODPLAIN CHARACTERISTICS ON <br />PEAK-FLOW RECOMMENDATIONS AND IMPLEMENTATION <br /> <br />4.1 Timing and Duration of Connection to the Main Channel <br /> <br />Drifting razorback sucker larvae are typically detected in the main channel Green River <br />about 12 to 20 days after spawning occurs, and usually in Mayor June. In general, most drifting <br />larvae are observed in the main channel over a period of approximately two weeks (Muth et al. <br />2000). Because drifting larvae are more likely to die if they are not entrained into suitable <br />nursery habitats, these habitats must be connected to the river when larvae are drifting. <br />Therefore, connecting flows must occur concurrently with drifting larvae. The Muth et al. (2000) <br />flow recommendations identified a need for connecting flow durations of two weeks or more in <br />one of four average years, and in all moderately wet, and wet years. The basis for the <br />recommended duration of two weeks or more above 527 m3/s (18,600 cfs) was the observed two- <br />week availability of drifting razorback sucker larvae. The specific magnitude chosen (527 m3/s <br />or 18,600 cfs) was based on the relationship between flow and floodplain inundation with levees <br />in place. However, recent modification to levees allow the same amount of priority depression <br />floodplain to be inundated at flows of 396 m3/s (14,000 cfs) as would be inundated by flows of <br />527 m3/s (18,600 cfs) (Figure 4). Thus, it is possible that the same benefits for endangered fish <br />could be achieved by maintaining longer duration floodplain connections with flows of 396 m3 Is <br />(14,000 cfs) as with flows of 527 m3/s (18,600 cfs). <br /> <br />The Muth et al. (2000) recommendations also specify that peak flows should be timed to <br />coincide with peak and immediate post-peak flows of the Yampa River. This timing is consistent <br />with the appearance of drifting razorback sucker larvae, and facilitates achieving the needed <br />magnitude and duration of connecting flows. <br /> <br />There is a relationship between the duration and magnitude of flows that can be supplied <br />by Flaming Gorge Dam. For a given volume of water, a higher connecting flow will provide a <br />shorter duration of connection than will a lower connecting flow. By reducing the magnitude of <br />flows needed to maintain floodplain connections (e.g., by removing or modifying levees, as done <br />recently by the Recovery Program), the duration of connection can potentially be increased. Peak <br />flows that are much higher than those required to maintain connections between depression <br />floodplains and the main channel probably provide no increase in available nursery habitat once <br />flows recede. Increasing the period of time over which razorback sucker larvae can be entrained <br />into the floodplain may provide a substantial benefit by increasing the probability of entrainment <br />of larvae into nursery habitats. Thus for a given volume of water, it may be more beneficial to <br />native fishes to provide a lower magnitude, longer duration connecting flow rather than a higher <br />magnitude, shorter duration connecting flow. However, flows needed to adequately entrain <br />larvae into floodplain habitats or that would allow successful out-migration of reared juveniles <br />may be somewhat higher than flows that simply connect or inundate the depression floodplains. <br />
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