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FromLakeMurraytoaDamSlurry217
FromLakeMurraytoaDamSlurry
ClayHambrick
KatieLewis
LoriThomas
HarveyMuddCollege
Claremont,CA
Advisor:JonJacobsen
Summary
WepredicttheextentoffloodingintheSaludariverifalargeearthquake
causestheLakeMurraydamtobreak.Inparticular,wepredicthowhighthe
waterwouldbewhenitreachedColumbiaandhowfarthefloodingwould
spreaduptributariesoftheSaludalikeRawlsCreek.Webaseourmodelon
theSaint-Venantequationsforopen-channelwaterflow.Weuseadiscrete
versionofthemtopredictthewaterlevelalongthelengthoftheriver.Our
modeltakesintoaccountthewidthofthefloodplain,theslopeoftheriver,the
sizeofthebreakinthedam,andotherfactors.Weestimateparametersfor
LakeMurray,itsdam,andtheSaludaRiverandcalculatethefloodresults.
TheSouthCarolinaStateCapitolissafeundereventhemostextremecir-
cumstances,sinceitsitsonahillwellabovethehighestpossiblewaterlevel.
However,floodwaterscouldstillreach17matColumbiaandevenhigher
upstream.BuildingsinColumbiaclosetothewaterwouldbeinundated,but
thereshouldbeenoughwarningtimeforresidentstoescape.Bothourmodel
andlocalevacuationplanssuggestthatlow-lyingareasformilesaroundwould
becoveredwithwater.
Thetextofthispaperappearsonpp.229-244.
TheUMAPJournal26(3)(2005)217.@Copyright2005byCOMAP,Inc.Allrightsreserved.
Permissiontomakedigitalorhardcopiesofpartorallofthisworkforpersonalorclassroomuse
isgrantedwithoutfeeprovidedthatcopiesarenotmadeordistributedforprofitorcommercial
advantageandthatcopiesbearthisnotice.Abstractingwithcreditispermitted,butcopyrights
forcomponentsofthisworkownedbyothersthanCOMAPmustbehonored.Tocopyotherwise,
torepublish,topostonservers,ortoredistributetolistsrequirespriorpermissionfromCOMAP.
FromLakeMurraytoaDamSlurry229
FromLakeMurraytoaDamSlurry
ClayHambrick
KatieLewis
LoriThomas
HarveyMuddCollege
Claremont,CA
Advisor:JonJacobsen
Summary
WepredicttheextentoffloodingintheSaludariverifalargeearthquake
causestheLakeMurraydamtobreak.Inparticular,wepredicthowhighthe
waterwouldbewhenitreachedColumbiaandhowfarthefloodingwould