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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 />4.7.2 Modeling Reslllt~ <br /> <br />The results of the hydrologic modeling of future conditions for each subbasin as well as <br />specific locations along the major drainageway are presented in Table 4.6 and Table 4.7. A <br />graphical representation of the discharge profile along the major drainageway is provided in <br />Figures 4.3 and 4.4 for the Godding Hollow and Tri-TownBasins, respectively. For comparison <br />with existing condition modeling results, future condition flood hydro graphs at selected locations <br />are presented in Appendix B. <br />Within the Godding Hollow Basin, the impact of future development on the stormwater <br />runoff generated during the major storm events is not significant. This is largely attributed to the <br />placement of on-site detention ponds that limit the releases during the lOa-year storm event to the <br />100-year existing condition runoff. It is likely, however, that an increase in the peak flows within <br />the major drainageway will occur even with the on-site detention facilities. Delayed peaks <br />resulting from the attenuation of the stormwater runoff may result in a minor increase in the peak <br />discharge in Godding Hollow when compared to the existing conditions. Although the peak <br />discharge may not increase significantly, the volume of the stormwater runoff will increase thereby <br />significantly increasing the duration of flooding: <br />For the Tri-Town Basin, the impact of future development on the stormwater runoff <br />generated during major storm events is significant in that a reduction in the peak discharges is <br />evident. In comparison with the results associated with the existing conditions, the peak <br />discharges within the major drainageway are reduced, thereby reducing the potential flooding. <br />The reduction in the peak discharge data and the associated flooding is attributable to the <br />placement of on-site detention ponds that limit releases to the 2-year existing condition runoff in <br />the upper portion of the basin. <br />In general, the flood problems presently experienced within the Godding Hollow Basin will <br />be slightly exacerbated with future development. As stated previously, the flood peaks will be <br />increased as a result of the placement of on-site detention ponds which may extend the duration <br />of the peak discharge. <br />For the Tri-Town Basin, the flooding problems will be reduced with future development <br />within the basin. The placement of on-site detention facilities with 2-year existing condition <br />release rates reduced the flood peaks in the major drainageway by as much as 2,000 cfs, While <br />flooding problems may still persist at several locations due to the capacity of the existing facilities, <br />the severity of the problems is reduced. Furthermore, the extent of the improvements necessary <br />to further reduce the flooding is also reduced by the placement of the on-site detention facilities <br />with 2-year existing condition release rates. <br /> <br />T:\OPEMCoweidO)\coweldOJ.tnl rpt.wpd <br /> <br />4.22 <br /> <br />September 8, J 999 <br />