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<br />., <br />'I <br />rl <br /> <br />Interim Flow Period <br /> <br />, <br />:1 <br /> <br />Interim Flows, instituted until a Record of Decision is reached on <br />the EIS, were originally set at conservative levels on the theory <br />that high fluctuating flows were the causative agent for most if <br />not all perceived problems in the canyon. After several months of <br />studying the new Interim Flows, scientists concluded otherwise. <br /> <br />* Small up ramping rates as required under Interim Flows were <br />found to be unnecessary to prevent sandbar erosion. Scientists <br />found no evidence that raising the maximum upramp of 2,500 <br />cfs/hour under Interim Flows to 4,000 cfs/hour would be <br />detrimental to downstream natural or cultural resources. This <br />observation produced a recommendation after consultation that <br />the maximum upramp of 2,500 cfs/hour under Interim Flows could <br />be raised to 4,000 cfs/hour. We conclude that doing so would <br />not result in harm to beaches, riparian habitat, fish or other <br />downstream resources. <br /> <br />, <br />< <br /> <br />': <br />, <br /> <br />:~ <br /> <br />:~ <br /> <br />* Scientists also found no evidence that infrequent raising <br />of the maximum release from 20,000 cfs to 25,000 cfs would be <br />detrimental to downstream natural or cultural resources. This <br />observation produced a recommendation from research scientists <br />that the maximum release in the interim be raised to 25,000 <br />cfs.' We conclude that doing so would not harm beaches, <br />riparian habitat, fish or other downstream resources and would <br />likely preserve riparian areas currently desiccated as a <br />result of the more restrictive maximum release. <br /> <br />, <br />.. <br />-: <br />::1 <br />r <br /> <br />" <br /> <br />* Some biologists fear Interim Flows and eventually the <br />Preferred Alternative with their lowered river level and more <br />stable flows will accelerate the decline in Old High Water <br />Zone vegetation and species in the upper portion of the New <br />High Water Zone. In fact, decreased water levels in the lower <br />canyon has resulted in many riparian plant species and <br />individuals dying, beginning at the upper most elevations. <br /> <br />* High elevation wet and dry marshes previously maintained by <br />periodic wetting from fluctuating flows, have begun to <br />diminish in size and number. This is due to more uniform <br />flows which leaves some parts always exposed and dried and <br />some parts always flooded. <br /> <br />~;I <br /> <br />" <br />;~ <br />.'. <br /> <br />", <br />~.~ <br /> <br />... <br />" <br />~. <br /> <br />;-,.- <br />~ <br />r <br /> <br />" <br />,. <br />~ <br /> <br />< <br />...1 <br />";...: <br />~ ,. <br /> <br />* The reduction in fluctuations with Interim Flows has <br />lessened the sloughing of algae in the upper river and this <br />has caused a significant reduction in algal drift downstream. <br /> <br />* Large numbers of young Humpback chub have been found in the <br />river and the Little Colorado River but these large numbers <br />were attributed to favorable spawning and rearing conditions <br />in the LCR rather than due to Interim Flows. The EIS should <br /> <br />, <br /> <br />,;. <br /> <br />5 <br />