Chapter 5 Prediction ofFloods by Weibull Ploning, lnd cunbel Analyticll Method: Th. Elfetr ol B.rng.j 51 A diskibution lor AM ooods c5lnot bc chos slcly on the basis or{ priori th@reiical arSunents Th. chsacteristics of obsercd flood dala nust d€l..nined io 6 sitabl€ fdhion Md irk.n into rcmunt vhcn b€irg cnoF. spl6 Som. distributions from rhcm do not hrrc 6 b€ .xclud.d ifit i be dislribulion h b knoM rha1 n doo cl@ctdistiq in @nmor with ob$ned n@d Until 1970 lhc suitabihy of dy pfliol& diltribution fo. nood frequency dalysis wa often jud8€d on th. bsis of physiql insp.crion of the (bla or. prcbabilily plot On scl ! plot th. wpl. vslus of lh. htdrologi.al r@rd apps.r r $ri.s of ploncd poi.c while dE cninAr.d disrdbu{on ofa prlialr fm, whos slihbility is b.ing dmined, muld app.d a a lin€ ot curye The fom ofdistribution wh$€ lin€ or tuwe show€d best aere€n€.t with Cwbel [21], in d.monslraling the us of EV disrribudonq n.de us of @nfrdcn@ i.tads a!o!t thc liic o. aRe of rhe plott.d poinrs would then b€ chos6. detuBnatu h. snitabiliry Il i or6.t \o help jndg. of th.y ditxibutiMJu 14M eri.t, ddta". thc tuIed distdbutioi otr rh. pobalility plor t is now undcr$ood how€vd, bot[ fron th@rericrl s1.ris1i6 and from lplit smple t*ts on nydroloajc.l drta, that &y @ giv.n d'st.ibuton dGplay r rMid sinele of dlla fiom a plofi.d bch.vior which is quit. difmnt fron pm eT rchtioisn p. fils a $npL frcn a $6igh line popularion @uld dhplay mrtcd d liurc on r prcba[ility plot ma.kably clos 10 a stRishr line rh. on a probabihy pbr Ther€for., rn r. is. choosing a disribution on the basis of nol the full ofih. ploi, p* se. bur disrinct polribility i.sp{tion std3 fioh ofr of@or when probability plor. This is the hjghly unenrin .itur. ofthc $ fdilid obsvld d.rr d ! prob.litiiy p.pa uing r eitrblc plordng poritid aortuh |Id tla thc dd. n tu d by . nnighl lie. Thi! mthod b mr r@nftrd.d rcw ! d.y.. Hoy cv!. iri tfituriE felturc b ihar om c{r G how rdl rhc dn. fir th. $$i|ed dirribqrion. Thc cfteB otfou plorriig -plofiig polirion fomts d €$iirurin8 rhc plobllilny wi8lr.d nloictn! ofLNO), LP (3), GEv, rnd W.t by dhnbudonr wrc inv.srisrr.d by H.l'uiir ud BozdlM [2sbl. In thjs ch.ptd w.ilull ptoning dd cu$.1 nlrlEd @ dies.d ed ts.d for Findin8 lh..tr6ts of@rurrudion ofbr.6sd or pr.diqion ofnood. Co.lidcne iitdd3 dc ctlql .d ..d e dm in srlph. Prub.biliry Pbq Pto(i.! Po{ ioru, Prob.bitt9 PrFr .nd W.ibul nolti.g A rcchniqu. B ro plor th. 5.2.1 Pob.Dili9 p.pc. .!d Prcbrbiliry not In 8.n.rd *hgl thc ondadE di!fiiburion frft{on Pr (x) is plorcd on &nhnujc p.pcr vru rh. vrluc of X r i6ishr lirc dc mr eh. 10 sd. nddr lirc oi aithndic p.pq, P. (x) wolld h.vc to bc Sive! by thc qFdion P, (x) =u + b ftus if Ihc orul.tirc di{riburion ol ! rcr of d.o plon n . nnisl tinc d dirhiEdc piFr, th. d.ta follo*s I qifom diltdbotion. Prcholiliry p!p.r crD bc dcvdopcd s th$ uy c!ruhtivc disdburion d h. plottcd B r !r6itl|. li@. Cli.r.lty . *pslrc typ. ofprob.bility plpq is r.qlircd for c$r, oflhc ditrcrcar p.obrhility dturiblrios ro plot a a llr|j8ht linc. TIE *rling of fi. prcblbility FFr m.y do h.v. ro ch.rg. s thc p.6@rd ofr pdiold dindhodon .n6gc. Codru.iing pob.bility p.pa ir r proca ofrotr{oming tlE probalil'ry r.dc so th.t rhc relling @nulltirc odc b . nniaht lie. Thc rtu3lomrion tEhniqu. u.b. illudnt d bytlsub lMFi'lt16l A prcblbility plot ir . plor of mSnirld.6s or probrlililt trcmiii.S rtr prob.bahy ro eign ! d.h poi ir @dro y cLd.d ro u d.r.mining rh. ploui.s position. lf orc it daling wirh . poplLlio4 ddmi.i.a th. plorri'rg posirioD ir @rcty . nlt r of d.|miring th. ftrdion of rlE d.r. !du6 lcs! (gora) rhd or c{ud to rhc v!lu. in quenio.. Thur ih. sdl6r (u861) topddion v.luc wqld ptol r 0.0 sd rhc l$Ben Gnlll€0 popul.tion v!lu. sould plor !r .1.0. Asignins plonins loririo.s to emplc data is not a sk.ighr foruard b@ue on, on ndo b. ture rhar a $mpl€ smllqr a..l l.tAdt v:bq of th. untnoM popuhtion Thus plotting positions of 0 ed I shNld b. rvoid.d for ernpl. d.rl! unls orc ha rddilion,l infomation on tn popubtion limit3 Frequdct dalysis i md.ly a poc.dur. for Gtiding rh. ftqu€.cy of occuf.nc. or probability of occundc. of past dd / or tulur€ d€nr. Ths probabihy @nhins the plorting wnh or {irhout any dislriburion.l ssunpliotu is a nelhod of fiequency aulyes, vilh ot wiihout The pro@durc io b. followcd in €ith.r qs. Hydrologic frequenct analysb can bc mad. disribltional assunptions. maling my is much the sme. If no distriburional Gunptions de m.d€, the inv€rigalor n€rely plots the obsfred data on any kjnd of papd ( noi o@swily prcbability p3 er ) dd ues rhis he. besl judg@dt ro s fom dd ro tbc rugritudc of pasr or tuture d€nts lbr vdious dalltic{l tehniqu. h uscd, ir is r@mmnded that tne data slill rhat onc @ gcr cn ids of now vdl rhe dat! fii rhc asdcd &alytical r€tum p€riods. b. plotl€d If ddmin an spor poEntial p.oblcms. pals do not o@r with lny lix.d p.ftd in imc or rDglDtude Timc inltuls b.t*a 0od. vrry. L.rg. nood! n tuolly h.w la.gc rdum pdiod! od vi@ vere Tne d.ffnidor of th. Gluo Fiod my not involvc ey r.f€d@ to probabih, Eo{a€r, a relario$hip belwn lh. prob.bility of o@tu@ of a {lmd tud its r.1un p.riod betftd cd in jusifi€d A givd nood 9 with . r.lum pdiod T nay br *.eded one in T yem H6ce th. probabilily of dc..dcn@ i! P (0r > 4) = l|I. Flood The cunulative probability ofnoi-exe.d€ie, F (Qr) h givfl by . F(O,\=P(O"<n\=t:f Abov. eqution is the basis for e*imating thc rognnudc of r pdiod T subsriturins F (Q.) =r - floa, Qr, givo i13 t€tum l/T in . k.oM si.tisti@l di$dbunon tuicdon, oie .n. nognitud. of Qt, Oi.n, th. drita d. plotl.d on prchability psp.r to cnek wn€rner th.y follov a paniol& di31nbldo4 ro dder ms, ed b cndk fo. an $lvc ao. 5.2,2 Plo(i|!glolirions Prolrbilitt plots rcqlir.6 inirilt .slimite ofrhe problbilily of mnqcc.dq@ F= (F (Qr). rticb ir c.ttcd t ..plolling posirim. ptouing p6itioN rc .ts u$d to .siro1e p.rmEr.d by usins rh6 9rcb.liliry wisnl.d f,o@nr, (p\W0 nEdjod Son. Connonly Uxd nortir! p6 io! Fotuur. Ploriing /V+l /v + l- ln F= T '-: 0.12 - i o.44 i-05 ,v t N + 0.25 0.175 l/+ 025 N +O.2 t-t M i HoskinS 0t5 tv nnk i. asdding ddq = N- n+r rot N. No in d€@oding o.d.r - N- i +l ,E Plolring posnion fornula is civ€n by: P(r>xq)=n (N+l) ''--------(5.1) wb@ n= ordr runber or nnk offi€ .vent, N= Tolal nunrh.. of r@s, x=Q (c{0 @sc4) (i) (ii) The data are amnged in decreasins oder ofnagnhude to IiDd m. Tn€ Fobabilily P of.ach erenl being .qun.d to or is *Fd.d calulaled by fornula (5.1) The W.ibull fomula is a @nprcn!. wnh morc sllrislial ju$iliodon. Ifrh. N vrtua dc distnbu&d ujlomly 100 p€r@nl probability, th.. th€re must be N+ I intwals, rhe data points .nd 2 int€rv0js (ii ) (Ploltins positiod) Th. Euiiene iii€rva|, a1 bdvq Nlint rysls 0 md belwn tbe cnds T (the retun peiod or 6equ.ncr, h c.lculated r= (N+l!m T=I/P s (5.2) o3) dd lanted, ed tbc w.ibull PlottiiS points (Q,T) colculrled, a shph of masritud. (Q).vs p'obabilily' t(P( pxl P( x<x ) o. T )l cu b. plotted on probabilily pap$ wilh speoial s.tle or oi Gumbel piobabilny p.r€. with rcduc€d 5.3l., i€ QVs.Yr to fit a disldbuion On€ Graphically) rhc d.r! ssies diesed i. stion Trbl6 5 I I ro 5.1.3 Ctrmb.b 5.1. show cdolariotu fo. thc gnpns by W.ibull Plot for I tul d.t! Atrrlttiql M.rhod Tnc fidely is id€ntili.d Evl dindhtiion, rl$ krcwn used di$dbutioo in n@d ft.qucncy s Cumb.l disdbutior, is tne rnalylis CDL Fx(x)- axp I-€xp [-(x-O/dl, ..(J4), wnere F(x) b rhe probdbilily of.on-dceddce for th€ valu. x, n6t t is th. l@tioi p!$*td, P(X>rr=t-e-" M6r |rr-q,+ €q, ...(5.5) €=0.57721 vdilnc: dl = 1--= = 1.645 4I C@ffi.i6t ofSlcsrEss: C.= 1.1396 C@troi.mofKonosb: G=5.4002 r,=q-oht-lnp]...............(5.6) rr =d-a tn f (By iNqtbs CDF) r'l 0-;) l-h L 1...o.?) 'I We hl@ u dt.rndiw fom: rl-k+Kror. .....(5.8),vh@ l...rs.sr ' 'L t ( -Ill r./tl r- = -91,*r'l-r.{ r NoL: Kr ir th. rtrdudiz.<l OorlbL Vri.r. (r- o, o = l). x n .l!o elLd Fr.q@icy F.dor. 5.3.2 Grntd" X, = t X, = vrluc + Eq! io! Kro-r b rh. ofx with choe'3 sc|@l cqu.lion of b/dolosicd fr.qlc'cy t .ct!m p6iod T, 7= nai ofx, Kf fr.qudct f.ctor, wiich d.tod! upon T ed rI| fr.quaq dkdbudon. .. (5.r0) . o.t t) l ]"** ,. .,,-=.l^^ T II L It, tS" -+c'577 =Dulet's Conta\t\ r1.282s,610,@ , valus of ," &d S" arc 8iv.n in labh ?.1 md T.ble sia, io Eigiffiiog Hydrologt by K. Sub.d.y [ 36 ] 53J ...(5.12),of T r"*,,0t lo Bar.drced\tiate ? 4, for ditrsern smpl. PROCEDT'R.E The alor flood nagnitude Flood e equalioN us.d und.r thc followiog prcc.dur. to mtonding 10 a givo rcluo pdiod dimr€ fte bas.d on Amnal sdiet Anege the diehdge data in d.@ndin8 ordq &d N l{€re the amudl flood value is lh. vartuc X and C.lqlate T o. for L by rhe no1€ tlrc . givd dau. WeibullPlo nsPolnioi Fomula D€rmire,- vi. & rnd S. lppropd.l. ro siv6 N.usins t!bl6 [ 36 ]. spl€ size vii. Dct mirc th. rcquircd dii. Chdk wh.ilE rh. dr@. rr. ote rd d!l. fl vrluc dirdbqrion. Nor.: Cd@Ltiotu for $c Gr.thr in Tdl.r 5l I to t.j.3. t,1 by CunU Prcblbility Pipd & slDM VEruflCATION {i) (ii) CNlculate vdu* of ?lot Xt.vs.T on Xl for Sdi somc T< N, is By qtrspolsrioi, vdw of Ning Cunbelt iomulae Log or Gumb.l Probability Plot. . slr.idt lirc scn $d point thd Gamble's dktabltio. k . ,ro!.r fn. lfthe plor tIs wd! wirh lhdrctical Gmbcl's Xl for (2 33, X ) li6 on it (wno N is 14.). r>N @ b. d.t@nEd 6ily. GT'MDEL PROBADILITY IATXR n w is r.qunc (l) o lbri$a tlr gnphic.l !?tsa|ll!on ofcumbd ilisiribulior Bde sp€idly ftr*ed for vaioG vdue. orT. Forr $!b on 6si&.. w.6[l.ud ( sdy (ii) (iii) .id for lim eihm.ti! ldle of t'r vdtr* -2 to 5) lor sl.cr.d v.b4 orT ( Ssy 2. 10, 50, . .) Iind tnc vtlu6 of yr For xr or Q vdud on ordi rq ue ather dith'rdic or log!'ithmi€ Ar Xr is a lincar tunction of yr, the poinls ( xn yr) fo' Gunbel dislribution wil plol a! . ltoight lin. on clttbcl p.ob.bilily plot. This lioe an be used for gr.phicd interpohtion snd ampol.tion. ThG Equaton of the snanelt liffi, ctlLd "nod.l Jd W.lie tl@ b! GMb.l wthod," ht en d^a *t is obt ie! ud 3hoM inTabLNo.6.l.t 10TablcNo.6.l.l in Chaplq6. Confid..c. Ljnir. Fo. Pr.dictior of noodr by Crnb.l A..tyljc.t M.rhod SiM lhe v.lue of tlE vdi.l. f.r . siEn Etum p.riod, xn d.t€min d ty Guobcls nefiod m hav. .do.s du. to linir.d 6ple d.rl wed, rherefo.€, 6nido@ limils &e deiralrl€. Th6 @nfiden@ interyal indi€tc thc limit' lboul the calqld.d v.lue b€rwed shich lh. lrue value @ b€ eid to li. with epeiiic prcb.lity on sanpling €106 or y For a confid€n@ probalilily C, thc 6nllden@ ioretu bounded by th€ !€lues X, af,d X1 givei by x,a C =Xr + f(c) sq . l of lh€ variare Xr is (5.D) wnerc f(c) is. tunction ofth. @indcn@ problbiliry Bddemined by us,ns rheLsbleoanomar 'dids(rcbdr$ C in% t0 68 0.674 1.00 {c) 80 90 95 99 1282 1.645 1.96 2.54 "** =bh Kr= ft€quocf fadorgMaby.qu|lioi(s o".' = sr.ndrd ddiaioi of thc Tabl€s 5 3.6 1 io 5.3.6 ll . (5 14) tl) mpl. sboy th. @lculatcd valu* of C I's ar 8OpZ md 95%, Gnphs 5 r I to 5. l. 13 show rh. f..quency cuN.! by W€ibull plofiing position, L S m.tbod and Confide.e inl.ryrls by Cunbel hcthod, L.S. nelhods in disNsed in Tn. E|Tectl or Co.rtruction At ol B.rn36 on Pi.dicrion ot pak Di!.rrrg. S!Lt$ B.ngG Mei dd q &<x0 &>xro yd < xr , i..,.5 flood, for .tl for tne dara b.tor. rhc for rhe dau aftd bi@s6. bs!8.t d.i! s.t3 by % ditrcr6.€, for dif.rcnt T-y.es nood{ coisttuclior ofthe ba!8.r vui6 frcn 2 43o/o 2q/ob 45Yr i . the ef€cts on Dcdidion 26./e to bdw the d.ti els, du' to thc for Gudtlu (B) for Sukku(B) of [@dt rr Suktur (B) ttuc to rnc @nrtrucrion of spprcndr.lv €qlal Gudd! (B)-and of Sukkw (B) e l:1.27: .]. Bcf@ Glddu @) And Gddu @) 1.38 lr l.lt:1.50 l: | 25:1.29 l:1.32 145 ic. 4. rhe etrects ofcrddu (B) > Thc ctrecls of Su*lu (B) and Mdinum 0ood i! (i) y@s 50 (v) 301ts dpai.d to *b0>xs>xoii r.turn.n r sins tul da13 of sukru @) ulinS d!l. bcrorc Grddu (B) Nirg d.rh .tq cflddu (B) using tu! beforc Sutlor (B) uri.g datt .nq Suthr (B) Hd@ th. nuitun tl@d it dpd€rt ro tctum .t Sukku (B) in lhc shorl'sl p'dod D€riod (i.e. 15 y€s) uling th. d;tl ,nd Guddu (B) rnd in rhe longdt i lo0 1a.2 Ar yd*) $ins th. d|t. b.forc Sukh. (B). Koti B.mg. M6 dd Qr < xr for dl &ta cn (a d Sutlotr (B)) < D, xo for ihe d.t. b.rorc .ll b.rfl.sa (M .r sul&ur (B) Dr > x,o rn.r baras6, d@pt for rhc d.L .ild Su*lur (B) 2. % ditreioe, for ditr r.nt T-y.$ ll@ds, bet*€d th. do$ scG du. lo co.$rucrion of barlg€3 vdia fron tbc 't94/,b 4e/" ior Sukku (B) 3lY"ro6e/' 41/oro22o/o i.o. the ef€cts on prcdiclion of loodr lnd de Brotet due to sukrrr (B). l: L26: I L .t Koid(B) are the l€ast due ro Gudd!(B) 16 r:1.19:1.55 1ll9:ln l:1.15:1.50 11128:1.41 I x rm> x r>x The efrects m io €&h is (i) 100'ts (ii) l0oy4 (iii) (iv) (r) (t) (ii) a3 it SuEor (B) dpat€d to rctud lnr tul dltr ofKotd @) uins dda bdore Kolri (B) usiDs 30y€s 20yaE 50y4 l00r!d 20 yds e cs, I t6 (B) >The etr c!3 ofcuddu (B) > Th. .f@ts of sukkur (B) ofKoti Mdinum llood 1.39r Bin8 dlll lnd Kot i (B) using dar! b.foc sukru (B) using drlt ift6 Sukhr (B) using dal! b.forc Goddu (B) urins d.tA rn* c!dd! @) llood to retum at Kotri (B) i. lle shon.d pcdod (i . 20y6) usins rh€ d a sct .nd Guddu (B) ed in fi. loi861 p.nod (100 ymhsing dra before Guddu(B) .d bdo€ Kotri (t r. H.ncq w€ dp€crins Minum 5.4.5 (ii)D' 2 >rr for all rh. b.d.s6. % difer€.@, for dif.rcnt T-y.es floods, vuia fton b€tw4n Suklor (B) dd cuddu(B) , 6l oel. ; 35.?70 b.t{*nKorn (B) &d S!kku(B) bdwn Koti (B) dd cuddu(B) di€ad@ k h.tw*n ih. predictons at Kori (B) md cuddu(B). xrm = I134:l4a l: l3lr 142 I I i e. lhe 6riG de l.Eali for Glddu (B) ald Th. ririos e sle itEd3in8 wi$ tift 4 Muinun For Kotri (B) l2: 146 0@d it ciP.ct dto lad for sukru(B). r.tnrid usiis tult d.1s for clddu (B) $ins tuI dat. for for sukk$ (B) usii8 tull dala for Kotri (B) (t (iD (iii) H€n@, we ee dparing m.nnun fl@d to rctun ( 20 y.ds ) and at Kotd (B) i, tnc bngrst pcnod C!dd! (B) in th. snon6i pldod i. q L Md 2 (B) The .treds on pcdiclion of floodt ar Koti (B) @ rh€ 165l duc to Ouddu rid rr€atet due io Sukklt (B). itre'a;eas on prcoiaion i:ittoo<lt at Sutkur (B) doe to th' @hsltuction or Guddu (B) md Suklur (B) ar lPProxitut.lv equal ud <x i, fd ![ th. drtr s.a D! < x o fd allth. dd! !.ls bcforc bu 86 D; > x h ro, all iJE drla *tt ns b.E$e sd sle fo' ftll dar' er3 t for 3ll datt 3.t3 itd b!.Bg* (B) 'o m" fs) .r Kotd < Th. .trock of sul(ku (B) r Kord "r..li "rctaa' 4. (t) MqinM [o.d to .aum .t Sul&i (B) .GquiB CDnd psiod ror rh' d!!i .nd cuddu (B) .d lonscsr Fiod ror the dd! b'forc sul&u (B) (i ' 3. ' x n >x$> (b) Maxinun fldd lo r.lur. at Kotri (B) r€qund shortdl P.dod ror rhc drt! !R.' Crtldu (B) ed lon8.6l Pdiod for th. da1t befor€ rori (B) (i. fot 1wo 5 Th. difcr€ncB belw.ei b.two 6 rhe prcdid.d R@ds !t Kord (B) dd at Guddu (B) > Kotri (B) and sukkur(B) > bctwcd sd&ur (B) Maximm fl@d .t Kotd (B) in the is dd Guddu (B) lo r€rum rr Guddu (B) i. tlE shond pqiod (20 lo.s6t rcriod ( l0o y4). rlt ud Corclusion Tft..f6r3 of @mtrudion of distane. | 00 - ye6 flood is largd rhe 50 - Mdinum 0ood is to rerun in the la€e bd.g6 o. a !h. dom itr€d dep6d upon th. y.r4 flood (a dpdted) .lc al cuddu (B) in thc ahonet p6iod and at Kord (B) p.dod. 33 bl.5.l.l C.lcul.lior for Gtrnb.l Prob,bility P.p.r.nd w.ibull Plor Cudd! B.rrng. 1962-1999 t.t6l l1 t.la5 Lrl t.t31 l. 33 a 1.294 C.LrLlio! Aq GlDh|. Pnb.bilrr Prpd Ald W.lbo|r llol, SlltLlt (E) TrU.No:5.1.2 '' (l9lll - t910) t.56) tr l5l5 Lltt td.ajj C.lol.ti.. ror a[. Cr4f, O. Cmb|. tu.liliv o9i,r-lt POs.!rl wdhdl tlo! 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