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FLOOD02442
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Last modified
1/25/2010 6:24:28 PM
Creation date
10/4/2006 10:53:44 PM
Metadata
Fields
Template:
Floodplain Documents
County
Rio Grande
Community
South Fork
Stream Name
South Fork Rio Grande River
Basin
Rio Grande
Title
Flood Hazard Study
Date
10/1/1980
Prepared For
South Fork
Prepared By
USDA Soil Conservation Service
Floodplain - Doc Type
Floodplain Report/Masterplan
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<br />I <br /> <br />I <br /> <br />I <br /> <br />APP<:NDIX <br /> <br />The Rio Crande Re"er~oir Dorn was raioed in 1979 w,~\\ modificulons to <br />the emergency spillway. The current emergency sp;I1.."y capacity is 10,000 <br />cIs. The eHimated IOO-year p"ak infl"" i. 5600 do, 'hich i"'pli... ~hat the <br />IOO-year frequcncy flood will not o""rtop the clam. For this reosons <br />b<eaohin~ analysis O/S8 not made. <br /> <br />I <br /> <br />I <br /> <br />INVESTIGATIO~S, ANALYSES, AND TECHNICAL DATA <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Hydrology and Hydraulics <br />llydrology <br />Peak disehaq~,,-!requency data used In this study were developed from <br />(requeney analyses of peak discharges for selected streamgages. U.S. Waeer <br />ltesourees Council Guidelines for Dete>:1llining Flood Flow Frequency, "Bulletin <br />17-A",wereusedasamajorrefet'ence. <br /> <br />Peakdi8eharlles fortl1e 10-, SO-,IOO-andSOO-y"ar flood. ore <br />tabulated for each croSS .ection in'!:able 1 "Flood Frequency-Elevation and <br /> <br />I <br />I <br /> <br />I <br />I <br /> <br /> <br />Discharge values for the South Fork segment of study were based on th e <br />,~uth Fork Streamgage No. 2195 "'1th 53 years of data. Adoptions for other <br />~~catlona along the stream ",ere based On procedures in Colorado Water <br />:onservatiouBoardTechnlcalManuaINo.l. <br /> <br />Oi.char'teData." <br />Ilydraulics <br />The hydraulic analy.is used in this study con.isted of computin" water <br />surface profiles using the Soil Conservation Service WSP-2 computer progra~. <br />11 description of thi.progra",is avsilahle in soilConaervstioo Ser vice <br />TechoicalReleaseNo. 6l "WSP-2Co",puterProllr81o." Basically the prograro. <br />uses a standard .tepOlethod for runnioghsckwliter profiles, and includes a <br />bridge los. analysis described in "Hydraulics of llridge Water..ay." by thO' <br />ll"re"u of Public Rond.. <br />Cros.sectiondatli,andrench leoo;th infor..ationwereobtainedfroOl <br />photo"ralll!l\etricOlap. prepared especially for thi. study. Ilydraulic <br />roughness coefficienta ("n"vlilues) were dete"oined fro.. field inspection, <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />The Del Nocte (62 years) and Wason (40 yeacs) streamgages were selected <br />;~: de,elo~ing discharge-frequency val~es for the Rio Crandc ~~in atem scg- <br />"""': of at~dy. A drainage area vs peak discharge retaHonsbip was estab- <br />:is"c~ for tbe main atcOl1Jsi"<l these two gages. D.1t" fcoc slI".,.."l other <br />.::eaag"ses in the region werll used foc checking and cocrelation purposes. <br /> <br />I <br /> <br />I <br /> <br />- <br />-- <br /> <br />Colorado Water Conservation Board Technicai Manual No. i. <br />U.S. Geological Survey regional CurVe~ in Water. Supply PapH 1682. <br />Hood Plain Inforlll3tion Report for the Rio Crlinde - M(>nte Vista, <br />Colorado, by tbeCorl's of Er>zlncers, U.s. Ar",y. <br /> <br />and docu",entedwith pl1otograph.. <br />follow in" are a ubuhtion of hydraulic rou.."neu coefficient. for <br />various locIltionaalongthestudyarea. <br /> <br />I <br /> <br />:t~er cefetences used for checking purposes inciude: <br /> <br />I <br /> <br />,- <br /> <br />I <br /> <br />] <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />~~~nr r~~~q',,!r ~O'l.~",.,etl"n ~nn~ "bop n" th~ Rf" r:r""~,, ~"dn~ th" <br /> <br />I <br /> <br />Jc:LoJ 1910-1?lS. This had an affett on flo..." to the river, therefore only <br />:~ period 0' record follOWinG 1915 waS used in the study. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />;';>-2 <br /> <br />I <br /> <br />Ae-' <br /> <br />I <br />
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