Laserfiche WebLink
<br /> TU;!; Rilin:.all IntE'flsity I <br /> , <br /> (ll,ir..) ,~ If' ' , <br /> '..n. .r-I <br /> 2 'Jr. 5 Yr. I 10 'ir, 25 'ir, 50 "" 100 Yr. <br /> 5 .01 ,," ,," ,48 ,60 ,60 <br /> 10 ,36 ,48 ," ." ,84 .36 <br /> 15 ,48 i ,60 , " .9G 1.08 1.44 <br /> " ,;;0 ,8,1 .% 1.32 1.68 I 1.68 <br /> 25 ,84 1.56 2.16 2.28 2.40 3.00 <br /> , <br /> 3C 1.80 2,52 3.12 3.72 4.44 i 5.04 <br /> , <br /> 35 3.24 4.68 , <br /> , 5.64 6.84 7.92 9,00 <br /> 40 I <br /> 1.08 2.04 :,.28 2.Sf! 3,24 3.72 <br /> 45 ,84 1.08 1.20 1.56 2.04 2.16 <br /> 50 ,36 ,72 .84 1.08 1.44 1.56 <br /> 55 ,36 ,60 , " .84 ,96 1.20 <br /> 60 .36 .48 .60 ,72 ,72 ,04 i <br /> 65 .36 '. ! .60 .72 .72 .G\J I <br />I "".1 <br />I 70 I .'" .36 ,OR ,4R ,48 .40 <br /> I , I <br /> 75 I ' ~1 .36 .36 .36 I ,36 I ,)6 <br /> I I , <br /> 20 , .24 i I , I <br /> , to ,').4 .,f; , to ,'if; <br /> "' .'" ,24 .24 ,36 ,24 .24 <br /> 36 ." ,24 ,12 ,36 .24 .24 <br /> , <br /> 05 " .12 , .12 ,24 .24 ,2!, <br /> I 'H I <br /> 100 ,12 .12 .12 .12 2' ,," <br /> I ' , <br /> , <br /> 105 I ,12 .12 I ,12 ," ,24 ,24 <br /> UO I ,12 I ,12 I ,12 ,12 ,12 I ,2/, <br /> I <br /> <br />, U, <br />L120 <br />TOTAL <br />PRECTP. <br />(tn.) <br /> <br />." <br />.12 <br />1.10 <br /> <br />';',,8 :~l:. ::. <br />WSST V~NE D~AT~AGE nASl~ <br /> <br />IE:;IGN P]d~J:l\LL <br />~- <br /> <br />.12 <br /> <br />, " .12 ,12 <br />.12 .12 .12 <br />1.84 2,25 2.',7 <br /> <br />.12 <br /> <br />,12 <br /> <br />2.89 <br /> <br />P"'t"Cf'nt <br />of <br />Total <br /> <br />1.7 <br />U <br />U <br />4.8 <br />8,7 <br />14,5 <br />26,0 <br />10.7 <br />6.2 <br />U <br />L5 <br />2,4 <br /> <br />1,7 <br /> <br />1.2 <br />l.Q <br />1.0 <br />0,7 <br />0.7 <br />0,7 <br />0,7 <br /> <br />0,7 <br /> <br />0,7 <br />I),j <br />0,3 <br /> <br />C?.{.) <br /> <br />. 1 2 <br /> <br />1.55 <br /> <br />nh1: <br /> <br />I UBL.~ <br /> <br />DESIGN RAINFAll <br /> <br />-, ~- <br /> <br />i <br />, <br />I <br />I <br />I <br /> <br />hi1sed model. Accuracy is del-'endent on repr~scntinq th" act:u,1l <br />physic<:<l characteristics in the field. Therefore, significant <br />changes in overland flow slopes, ext~nt or type of develop- <br />ment, and overland flow lengths were represented by modelling <br />smaller subbasins. The subbasins we!'e deline"ted using the 100 <br />scale, 2 ft, contour interval mapping provided by the City, <br />Field investigations were carried out as necessary to define <br />those subbasin boundaries difficult to determine from mapping, <br />Subbasin sizes ranged from 1,8 acres to 156,8 acres with the <br />median size being 14,3 acres <:<nd the average size being 25.5 <br />..cres, <br /> <br />IV.D. Influence of Physical Features on Hydrology <br /> <br />As stated previously in this report, several existing detention <br />and retention areas exist throughout the drainage basin, sone <br />of which are natural whilf' others are caused by road embank- <br />ments, railroad embankments, or development. ~any of these <br />are<:<s exist west of Dverland Trail on property owned by C.$.U, <br />All existing detention <:<nd depression areas were modelled [or <br />the existing dev"lopment condition, The City has little <br />control over future dcvelopreent on C,S,U. property, Therefore, <br />for thi> hydr"'lo<ji" "'1"'ly"j" of f1ltur-' d,"v""l(]p"""nr, rhro\lgh <br />mutual agreement with the Technical Committee, existing dctllntion <br />and retention areas east of Overl<:<nd Trail were modell(>d <:<s <br />they ~xist, Detention areas west of Overland Trail were <br />eliminated with the exception of College Lake. College Lak", <br />was modelled <:<s a detention facility <:<ssuming the lake was full <br />to th~ crest of the e~rgency spi1lw<:<y at the beginnir.g of the <br />des~gn storm. D~sch"rge ch<:<racter~stics tor the spillwdY as <br />prcs~nted in the "College Lake Improvements Study" 11) Wrl1re used, <br /> <br />The four irrigation canals which traverse the drain"ge basin <br /><:<1'''' Capable of int.ereepting a siy-r.ificant portion of minor <br />stOITI runoff bas,~d on current. lE~'''f>l$ of (leveloprr-cnt 'Nith the <br />assumption ~hat the c~nals are not running full with irrigation <br />'~'ater. However, for purposes of this hydrologic analysis, <br />