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<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 />do not contribute directly to the drainage facility. This <br />water may be held in small depressions in the ground or on <br />roof tops or may be absorbed or collected by plants. The <br />guidelines used for establisning depression and detention <br />losses were those given on Table 2-2 of the "Runoff" section <br />in the Urban storm Drainage Criteria Manual. <br /> <br />Infiltration. Infiltration is the amount of water that flows <br />through the soil surface and does not contribute directly to <br />surface runoff. Infiltration values established in the Urban <br />Storm Drainage Criteria Manual were used as the basis for <br />determining infiltration in the study area. <br /> <br />Unit Hydrograph <br /> <br />Under the CUHP, local hydrographs for specific areas are <br />developed by applying the effective rainfall data to a unit <br />hydrograph. A unit hydrograph was developed for each of the <br />study's subareas. It is a graph of direct runoff from 1 inch <br />of rainfall uniformly distributed over the drainage area for a <br />specific unit of storm duration. The hydrograph simulates the <br />basin's characteristics including tributary area, basin shape, <br />street patterns, channel capacities and slopes. <br /> <br />Formulas 4-1 and 4-2 in the "Runoff" section of the Urban <br />Storm Drainage Criteria Manual were used to determine the peak <br />of each subarea hydrograph. Two additional points were plotted <br />representing the width of the hydrograph at 75 percent and 50 <br />percent of the peak discharge. These widths were derived from <br />Figure 4-5 in the Urban Storm Draina e Criteria Manual. A <br />trial plot of the un1t y rograph was s etc ed an t e area <br />under the curve was calculated. The shape of the unit hydrograph <br />was adjusted until the area under the curve matched, within 5 <br />percent, the volume of a 1-inch runoff from the entire basin. <br /> <br />Local Flood Hydrograph <br /> <br />A local flood hydrograph is a graph of runoff versus time for <br />a storm event from a local drainage area. These hydrographs <br />were determined by distributing the effective rainfall times <br />the unit hydro graph ordinants during the unit storm time <br />periods. Pertinent local hydrograph data for each subarea of <br />Basin 6100 and the North Tributary to Basin 6200 are presented <br />on Tables 4-3 and 4-4. <br /> <br />Routed Hydrograph <br /> <br />At restricted waterway crossings where a ponding area is <br />formed, the local flood hydrograph has to be combined with the <br /> <br />4-5 <br />