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Last modified
1/25/2010 7:10:23 PM
Creation date
10/5/2006 2:36:34 AM
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Template:
Floodplain Documents
County
Statewide
Community
Nationwide
Basin
Statewide
Title
Storm Drainage and Urban Region Flood Control Planning
Date
10/1/1974
Prepared By
US Army Corps of Engineers
Floodplain - Doc Type
Educational/Technical/Reference Information
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<br />, <br />, <br /> <br />RATIO OF PEAK FLOW UNDER STATED CONDITIONS <br />TO THAT UNDER EXISTING CONDITIONS <br /> <br />Moderate Intense <br />Watershed Existing land Use Urbanization Urbanization <br />1.7 mi.2 1.0 1.75 2.20 <br />15 mi.2 1.0 1.2 1.5 <br />(without channel <br />improvement) <br />15 mi. 2 1.3 1.6 1.95 <br />(with channel <br />improvement) <br />These two examples indicate that the amount of peak flow increase for <br />urbanization is a function of the intensity of urbanization and of the. <br />exceedence interval of the event of interest. The intensity of urbanization <br />relates to the amount of the watershed that is covered by impervious areas <br />and the amount of the ~Iatershed that is storm se~le,red. The relative effect <br /> <br />of urbani zati 011 for the 1 ess frequent events tends to dampen out for the <br /> <br />following reasons: (a) for the increasingly rare events the watershed <br /> <br />under natural conditions would be more saturated; (b) the channels would <br /> <br />be more filled or overflowing; and (c) the flow velocities would be greater, <br /> <br />~ <br /> <br />and therefore conversion to more efficient man-made systems has incrementally <br />less impact. In other words,' under natural conditions when the watershed is <br />saturated, it is in effect quite impervious. <br /> <br />Analytical Techniques <br />The general state-of-the-art in developing information for the sizing <br />of the initial drainage systems (sewer systems) is the simple concept <br />termed "the rational formula." The rational formula is based on the assump- <br />tion that the amount of flOl'1 contributing to the peak runoff is directly <br />proportional to the intensity of rainfall for a duration that is equal <br /> <br />12 <br />
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