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<br />I <br />I <br />I <br />I <br />II <br />i I <br />, <br /> <br /> <br />. <br />. <br />I <br />I <br />I <br />I \, <br />I <br />I <br />I <br />I',.. <br />,_I'" <br /> <br /> <br />I <br />,. <br />I <br /> <br />Mr, Wayne Bethurum <br />Page 3 <br /> <br />The baseline HEC-2 model using flows of 2,800 cfs and 3800 cfs indicated the flood flows would <br />spread out in general agreement with the extent of flooding shown in aerial photography supplied <br />by the CWCB. The model actually indicated somewhat wider flooding than the aerial <br />photographs showed, but the photographs were taken some four (4) hours prior to the estimated <br />peak. It is our understanding that the aerial photography was taken at about 6:00 p.m. and that the <br />peak runoff from the storm did not occur until about 10:00 p.m.. We were informed by the <br />CWCB that at the peak of the overflows, storm water was about 2 feet deep at your construction <br />trailer. Based on the site topography and spot elevations completed by Liebert McAtee, your <br />construction trailer is set on ground with an elevation of 3947.30. Our baseline model completed <br />for 2800 cfs computed a water surface elevation of 3949.41 at cross-section 3 which crosses your <br />property near the location of your construction trailer. Based on this information the model was <br />accepted as a baseline condition <br /> <br />ICON created a proposed conditions model to evaluated the impact of the improvements to your <br />property that have been constructed, or are planned to be built as part of the most recent filing. <br />This was done by adding elevation data from the overlot grading plans for the South Point <br />Subdivision of Lot I to the surveyed cross section data Planned single family houses were coded <br />into the modeled cross-sections using the top of foundation elevations presented on the <br />construction drawings which are enclosed with this letter. A roughness Coefficient of 0.035 was . <br />used to represent the streets and bluegrass areas within the subdivision. The results of the baseline U <br />model and proposed conditions model are presented in the following tables: ,~ j \. c: . L'-" \ <br />.6-\./\ C \ ' <br />J-' . I <br />~~J(LI <br />Water Surface Elevations - Discharge = 2,800 cfs )J l <br /> <br />--<,c" , i;; ,/, <br />I ,). .. r <br />~Vl'C) -,1- <br />? '-) L, <br />-- ,. -! / <br /> <br /> / <br /> Baseline Water Surface WSEL with 1./ Difference <br />Cross Section Elevation Improvements (ft) <br />1 3946.60 3946.60 0,00 <br />2 394838 3948.28 / -0,10 <br />3 3949.41 3949.59 . 0,18 <br />4 3949.96 3949,97 0,01 <br />5 3950,71 3950.80 0.09 <br />6 3951.32 3951.03 -0.29 <br />7 3953,29 3952,99 -0.30 <br />B 3957.64 3957.74 0.10 <br /> <br />Water Surface Elevations - Discharge = 3,800 cfs <br /> <br />,I <br /> <br /> Baseline Water Surface WSEL with Difference <br /> Cross Section Elevation Improvements (ft) <br /> 1 3947.00 3947.00 0,00 <br /> 2 3948.74 3948.67 -0.07 <br />. - 3 3949.74 3949.93 0.19 <br /> 4 3950.29 3950,32 0.03 <br /> 5 3950.96 3951.09 0.13 <br /> 6 3951.52 3951.27 -0.25 <br /> 7 3953,61 3953.10 -0.51 <br /> 8 395B.31 3958.47 0,16 <br /> <br />,; , <br />I vii' I <br /> <br />,j' ~ I-t f. ~) <br />