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sized flow peak of approximately 4,000 cfs was measured on Fountain Creek. The <br /> release rate from Pueblo Dam was cut from over 5,000 cfs to less than 700 cfs to <br /> minimize the flood impacts of the Fountain Creek peak as it passed through the <br /> middle valley of the Arkansas River Basin. As a result of the increased rate of storage <br /> when Pueblo Dam outflow was cut, storage climbed into the Flood Pool early in the <br /> morning of June 13. By the morning of June 14, releases from Pueblo Dam had <br /> been brought back up to 4,850 cfs, but inflows to the project were over 6,000 cfs. <br /> Late in the evening of June 15, a very significant rain event in the Colorado Springs <br /> area resulted in a peak of over 18,000 cfs on Fountain Creek. This peak triggered <br /> another cut in releases from Pueblo Dam and reservoir storage was driven higher <br /> into the Flood Pool. By June 18, the Arkansas River above Pueblo Dam peaked at <br /> over 7,000 cfs and began a gradual decline, but the pool at Pueblo Dam continued to <br /> rise towards the historic pool of record. <br /> As a result of recent experience with large flow peaks in the middle Arkansas River <br /> valley, it was determined that the system could handle flows in excess of 6,000 cfs at <br /> Avondale. The decision was made to increase releases out of Pueblo Dam above the <br /> published channel capacity in an effort to slow, and possibly stop, the rise in the flood <br /> pool. Before making the planned increases, a monitoring plan was established for <br /> four locations on the Arkansas River which have typically been sensitive to high river <br /> stages. On June 19, USACE increased Pueblo Dam releases by 500 cfs, resulting in <br /> 6,500 cfs at the Avondale Gage. A second 500 cfs increase was made on June 20, <br /> and the pool elevation at Pueblo Dam pool began to level off. Pueblo Reservoir <br /> storage peaked at elevation 4,887.4 ft on June 22, nearly 7 ft within the Flood Pool. <br /> Over the next several days, the weather was closely tracked along with the <br /> previously identified monitoring points along the middle valley. During this same <br /> period, Pueblo Dam's pool began to drop. <br /> On June 24, after several days of high sustained flows on the Arkansas River, <br /> Pueblo Dam's release was reduced by 500 cfs to reduce river stage and ease <br /> pressures along the Arkansas River. The levee system in La Junta was showing <br /> signs of distress and localized inundation of lowlands in the Avondale area were <br /> reported. Another cut was made on the June 25, and the basin was allowed to <br /> recover for several days. <br /> By the June 29, the weather had turned hot and dry. Pueblos Dam's outflow was <br /> increased by 500 cfs to accelerate the evacuation of Pueblo Dam's Flood Pool. <br /> Shortly thereafter, notice was received that diversions along the middle valley would <br /> be reduced as off-system reservoirs in the basin reached capacity. This reduction in <br /> diversions would occur upstream of La Junta, and it would essentially put over 800 <br /> cfs back into the Arkansas River. Pueblo Dam outflow was cut by 500 cfs on July 1 to <br /> reduce the threat to the La Junta spoil bank levees. The Fort Lyon Storage Canal <br /> reduced their river diversions by 200 cfs on July 1, and then by an additional 150 cfs <br /> on July 2, returning a total of 350 cfs to the river. Arkansas River stages at La Junta <br /> continue to stay within acceptable levels, and the July 1 cut from Pueblo Dam was <br /> 2 <br />