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<br />, <br /> <br />10 <br /> <br />Pre"ipitation varIes wIdely throughout the Iloaring Fork Basin above <br />Basalt. DntheCor1tinental Divide, near Independence Pass, the average <br />annualprec.1pitation Is 26.3 Inches with 17.5;nchesoccurringduring <br />the winter months (November-April). NellrBasalt, the ,,'(erag.. annual pre. <br />clpltation is approximately 16.5 Inches with 7.3 inches occurring during <br />the winter "",nths (Reference 6). Data on precipitation from the National <br />Oceanic and AtmospherIc AdministratIon indicate that in the Aspen area, <br />the 100-year 2~-hour storm would produce 2.6 Incoes of precipitation. <br /> <br />Study Reach Description <br />This floodplain study encompasses about 5.7 mile, of the Roaring Fork <br />River beginning at the Garfield County LIne and extending upstream to <br />the Pitkin County Line. In additIon, this report covers the Fryingpan <br />River from Its confluence with the Roaring Fork upstream for about 1.0 <br />ml1e. The Roaring Fork River in the study area has an average range of <br />about 90 to 120 feet wide as it flows through an alluvial valley,with <br />a grade of approximately 0.007 feet per foot. The stream channel Is <br />braided, having a bed composed mostly of gravel, cobbles, and small round <br />boulders ranging In the 6 to 15-inch diameter size. There are many riffles <br />and rapidswithmany,hallowpoolsalong its course. Several irrigation <br />ditches divert from the Roaring Fork along this reach. There are no <br />across-the-river diversion structures. In most areas, the river banks <br />arc low wi th steep slopes (often over ~5 degrees), being c","posed most Iy <br />of sand. gravel, and cobbles, with little or no vegetation below the mean <br />annual hlghwatermark. The steep slopes and ]ackofvegetationreduce <br />the resistance of the banks to scour. <br /> <br />Temperature and precipitation varies greatly from location-to-location and <br />season-to-season within the drainage basin and are Important variables ;n <br />flooding conditions. Above normal spring temperatures can cause early <br />and heavy flows on the Roaring Fork River. The Aspen weather station is <br />the only official weather statIon In the study basin. Records from the <br />Aspen weather station Indicate that the mnth of July has the highest nor. <br />mal total precipitation for the year at 2.06 Inches. The rnontll of March <br />follows closely with 1.98 Inches of total precIpitation. The fIrst month <br />with" nor",al ,pring temperature above the freezing point 15 A.prll with <br />""",an....,nthly temperature of 38.6 degrees Fahrenheit. <br /> <br />Thefryingpan in the study reachhes an average width of about 60 to 80 <br />feet, and maintains a grade of approximately 0.015 feet per foot. The <br />ri~er b"nks are steep and wel T-deftned dlong the re..ch, dnd the bed Is <br />cov",cdwithan armor ldverof largc cobbles and boulders. Todateonly <br />limited development has occurred in the floodplain areaS. Most structure, <br />have been bui It adjdcent to or in shallow flood prone aredS. <br /> <br />ThefollowingpictyresshowtheRoarlngForkandf"ryingpanstreamch..rac. <br />t~ri,t ics dt s~v~ral points. <br />