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III. SCOPE OF WORK <br />A. Background Information <br />Climatic Information: <br />It is common in Colorado for flooding to occur in the spring and summer from <br />rainfall events. The highest rates of storm water runoff are caused by intense <br />rainfall on a watershed. The intensity of rainfall can vary considerably during each <br />storm event. Summer rainstorms that cause flooding of the communities of <br />Dacono, Frederick, Evanston, and Firestone are generally associated with frontal <br />systems involving cold air from the north�vest and warm moist air from the Gulf <br />of Mexico. From approximately May 15th - May 30th and July 15th - August <br />15th, monsoon moisture typically enters Colorado from the Gulf of Mexico. The <br />rainstorms vary in duration from a few hours to several days depending on the <br />extent of the storm and its speed. One or more storm cells of high rainfall <br />intensities generally exist within a given rainstorm event and the path of these <br />storm cells often determine the location of flooding. Highest recorded rainfall <br />events in Colorado typically occur during the last week of July and the first week <br />of August. <br />Storm Drainage Situation: <br />A copy of portions of the report titled I-25 Corridor Master Drainage Plan <br />Godding Hollow and Tri-Totivn Basins South Wel�l County, Colorado by Anderson <br />Consulting Engineers, Inc. draft dated June 24, 1999, were available for public <br />distribution and are included in Appendix 1. <br />The communities of Dacono, Frederick, Evanston, and Firestone have a long <br />history of flooding problems. In these communities, there is currently no <br />significant existing detention storage for storm water runoff. These communities <br />outfall storm water runoff into the Tri-Town Drainageway (shown on Figure 2) <br />which originates near Dacono. The drainageway conveys storm water runoff <br />northerly toward Frederick, �vest along the south side of Frederick, and north along <br />the west side of Frederick, Evanston, and Firestone. The drainageway is currently <br />a small earthen channel with a capacity to convey somewhere between a 2-year and <br />a 10-year existing condition storm event runoff. Storm events greater than the <br />existing channel capacity flotiv overland through the communities causing flooding <br />of residential homes, businesses, and roadways. <br />The District is very proactive and sees the need for storm drainage improvements. <br />They have adopted very strict criteria for localized detention ponds for new <br />developments within the communities of Frederick, Evanston, and Firestone by <br />5 <br />