Laserfiche WebLink
<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />Bar Height. In the relatively sediment-free environment found in the study reaches of the South <br />Platte River, it follows that high bars exist on the river bed only where the river is adequately <br />wide. The variation ofthe maximum bar height for the monitored cross sections (Fig. 2) is great. <br />In the wide river, bar heights are around six feet In the narrow reaches, rarely are they,greater <br />than two feet. <br /> <br />8 <br /> <br /> 1 " L I I ! I I I I <br />- Rural - - SUburban.i- <br /> Urban EnQiterld 1[ TT <br /> ~ <br /> Rural <br /> Suburban <br /> - <br /> I <br /> '. <br /> . <br />J I I . <br /> II <br /> . r." . i } <br /> .. . \ .. V <br /> .v II V <br /> <br /> 6 <br />... <br />- <br />.... <br />.J:: <br />Ol 4 <br />';;; <br />:c <br />~ <br />III <br />CO <br /> 2 <br /> <br />o <br />o <br /> <br />5 <br /> <br />10 <br /> <br />15 20 25 30 35 40 <br />Cross Section Number <br /> <br />45 <br /> <br />50 55 <br /> <br />Figure 2. <br /> <br />The bar height in all the monitored cross sections. The bar height is taken as the <br />difference in elevation between the top of the bar and the bed of the main <br />channel, each averaged over the period of monitoring. <br /> <br />The initial perception was that the prolonged spring runoff in 1995 had built the bars to a new <br />and higher level. An inspection of the change in maximum bars levels at the monitoring cross <br />sections (Table 2) does not support this perception. The freshness of the bar surfaces and the <br />scouring out of bar vegetation was the most obvious result, and not bar raising. <br /> <br />Six bars did not change top elevation between 1995 and 1996. Four cross sections were under <br />construction and two were not surveyed. The change between 1995 and 1996 of the remaining <br />41 bars in the surveyed cross sections follows. Twenty five bars gained 0.8 ft in height on the <br />average and 16 became lower, each by 1.0 ft, again on the average. <br /> <br />The bars at Cross Sections 1, 2, and 3 in the downstream Rural reach each changed greatly <br />during the 1995 spring runoff, most likely due to bar movement At the transect, the bars at <br />Cross Sections I and 3 lowered 2.9 and 2.8 ft respectively. At the other cross section, the top <br />of the bar was raised 2.0 ft. <br /> <br />5 <br />