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<br />This is a simplified method which has many advantages over the more com. <br />man practice of drawing the flood boundaries by connecting end points of <br />the flood boundary width at each cross. section. The most important advan- <br />tage is the degree of confidence gained in the interpretation of the 100-year <br />flood boundary. The flood contours become permanent documentation of the <br />engineer's ludgmentln interpreting the flood hazards. <br /> <br /> <br />. <br /> <br />Floodplain Delineations <br />The next step of the floodplain study is the delineation of the flood limits on <br />the topographic maps. Delineation requires the depiction In plan or overnead <br />view of the information whIch is shown In vertical view in the flood water sur- <br />face elevation tables and profiles. The plan view provides a clearer picture of <br />the extent of actual flooding at specific locations along the stream. <br />Maintaining consistency IS very Important to developing a technically and <br />legally acceptable regulatory document which can be incorporated into <br />floodplain regulations and/or zoning maps, Problems may be eliminated <br />through improved reporting and interpretation procedures. <br /> <br />. <br /> <br />The procedure which the CWCS recommends for delineation of the 100- <br />year floodplain on topographiC maps IS as follows: <br />1) uSing the hydraulic analysis, the flood elevations at each cross.section <br />are tabulated: <br />2) the flood profiles are drawn; <br />3) uSing channel cenlerline slatloning from the water surface profiles. the <br />centerline stations of the whole numbered flood elevations which cor- <br />respond to the base contour Interval elevations of the topographic <br />maps are tabulated to produce the plotting table; <br />4) the location of all flood contours In the channel is marked at the appro- <br />priate station along the centerline on the base maps; <br />5) the flood contours are extended by draWing "wiggly." or reference, lines <br />perpendicular to the direction of flow until they intercept their corres. <br />ponding ground contours: thiS pOint IS the edge of the floodplain, (The <br />flood contours should parallel the cross.sections. If the cross.sections <br />were Incorrectly located, however. the flood contours may cross them,); <br />6) flooded area boundaries are drawn by connecting the ends of each <br />"Wiggly" or reference line; and <br />7) the flood delineation should be checked for reasonability and conSIS' <br />tency with the cross'sectlon data (top Width of the floodplain). <br /> <br />This method is also applicable to approximate floodplain mapping where a <br />water surface profile can be drawn uSing an assumed depth. Once the depth <br />has been assumed, It IS easy to show In plan view which areas would be <br />flooded and which would not. <br />The delineation of the floodplain Will need to be re.evaluated if development <br />activities or other factors cause a suffiCient change In the floodplain to alter <br />the threat. When reevaluation IS necessary. it IS important that previously <br />published information be reViewed and adequately correlated with the new <br />information. Maintaining this continUIty between studies will Improve (he <br />workability of a floodplain management program. <br /> <br />. <br />