Laserfiche WebLink
<br />e <br /> <br />Another interesting observation by Nehring was the need to omit the data from 1983 for <br />the Arkansas River in southeastern Colorado. Nehring (1993) states" In April 1983, while <br />brown trout sac fry were immobile in the interstitial spaces in the gravel, flows were reduced <br />66% below the October 1982 spawning flows, probably resulting in the failure ofthe 1983 age <br />class, This was justification for omitting the 1983 data pair." <br /> <br />Chadwick's assumptions in_his 1998 report on the minimal effects ofa I to 3 day low <br />flow of 4 cfs are supported by the natural conditions in Snowmass Creek. Occasionally, ice <br />dams occur that create instantaneous low flow events approaching 4 cfs that last for only a short <br />period. The effects on populations are within the realm of natural population cycles. At <br />durations of a 4 cfs flow from 3-30 days, Chadwick reports the impacts would be more severe <br />but using his 20% loss of habitat, he states effect would not eliminate brown trout from <br />Snowmass Creek. The evaluation of a 4 cfs flow for 3-30 days does not mimic natural <br />conditions as ice dams do not persist that long. There is little evidence to support the <br />assumptions that a 4 cfs flow for more then 1 to 3 days would have minimal impacts on the trout <br />populations of Snowmass Creek. <br /> <br />b) Habitat Evaluation Reports: <br /> <br />e <br /> <br />i) Don Chapman Consultants, Inc. prepared a 1996 report for the Caucus entitled <br />"Winter Ecology of Trout: Implications for Snowmass Creek." Chapman discussed the winter <br />ecology of trout, the effects of stream ice on trout winter habitat, the effects of reduced flows on <br />winter habitat, the ability of flow simulation models to predict impacts in ice-covered streams, <br />and recommendations for Snowmass Creek. Of note in this report, Chapman also challenges the <br />Chadwick high flow bottleneck theory and notes that Snowmass Creek has abundant side- <br />channel and beaver pond wetlands to provide juvenile and YOY habitat. Chapman reports on the <br />loss of habitat due to anchor ice and the increased likelihood of anchor ice with reduced stream <br />flows. This report also discussed several earlier reports on the effects of reduced winter flows on <br />trout populations including several reports on streams similar to Snowmass Creek. Chapman <br />also evaluates the various low flow recommendations of others that are primarily based on the <br />hydro graph for the stream in question. For Snowmass Creek, he recommends the Mundie Rule <br />that only allows reductions of25 to 30% of the mean monthly flows and no reductions during <br />periods of very low flows. In addition to the discussion of winter habitat requirements, this <br />report provides valuable information since it lists at least 7 published studies that document the <br />negative impacts to trout populations from winter stream depletions, <br /> <br />ii) The Permittee provided a report by C.F. Leaf entitled "Ice Formation and Winter <br />Flow Regime in Snowmass Creek." In this report, Leaf (1998) used the hydro graphs and <br />temperature measurements by Walsh and Walsh (1995) to perform a series of energy balance <br />analyses for different flow regimes. His fairly complex calculations demonstrate that the <br />relatively minor increase in ice formation would not affect average velocities and the hydraulics <br />of flow during the winter as compared to winter flows without ice formation. <br /> <br />iii) The Walsh and Walsh (1995) report provides empirical data on the effects of a <br />decreasing winter flow regime on trout redds in Snowmass Creek. A trout redd is the nest that <br />e trout use to both reproduce and incubate the young, Trout select redd locations based on depth, <br /> <br />9 <br />