prlialr fm, whos slihbility is b.ing dmined, muld app.d a a lin€ ot

advertisement
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
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1962-1999
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