preliminary report on field survey of -...
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http://hydro.iis.u-tokyo.ac.jp/
Preliminary Report on field survey ofPreliminary Report on field survey of 2011 Chao Phraya River Flood
1st December 20111st December, 2011
Daisuke KOMORI
IMPAC‐T
The University of Tokyo1
http://hydro.iis.u-tokyo.ac.jp/Inundation situation at Chao Phraya river flood
Natural levee
A deposit of sand or mud built up along, and sloping away from, either side of the flood plain of a river or
2
http://203.150.230.27/FloodMap/ (As of Nov. 28)Photos provided by Kimio TAKEYA, JICA senior expert (Okura, Haruyama, Ooya,1989)
side of the flood plain of a river or stream.
http://hydro.iis.u-tokyo.ac.jp/Inundation situation at Bangkok (As of Nov. 16)
3http://203.150.230.27/FloodMap/ (As of Nov. 16)
http://hydro.iis.u-tokyo.ac.jp/
Questions before the survey
Why was it occurred such massive flood? Is the capital, Bangkok, protected from flooding?protected from flooding?
The flood situation of Rojana Industrial Park, Ayutthaya
(provided by Kimio TAKEYA, JICA senior expert )
The flood situation of Bangkok
(provided by the University of Tokyo)
4
(p y , p ) (p y y f y )
http://hydro.iis.u-tokyo.ac.jp/
Outline of field survey■Date:
b bMain Survey: November, 4, 2011 –November 10, 2011
■Purpose of Survey:■Purpose of Survey:To clarify the factor of flood and grip the situation of disaster site and flood fighting activityg g y
■Survey Site:Th iddl d b i f Ch Ph RiThe middle – downstream basin of Chao Phraya River
5
http://hydro.iis.u-tokyo.ac.jp/
Outline of Chao Phraya RiverOutline of Chao Phraya River and latest floodf
‐Why was it occurred such the massive flood ? ‐Why was it occurred such the massive flood ?
6
http://hydro.iis.u-tokyo.ac.jp/
• Basin area: about 162 800 km2 100
■ Basin Area: 162,800k㎡Outline of Chao Phraya River• Basin area: about 162, 800 km2
➔ 44% of Japan, 32 % of Thailand 0(km)
• Ping River, Wang River, Yom River Nan River confluent at
(km)
River, Nan River confluent at Nakhon Sawan
Nakhon Sawan
Ayutthaya
Bangkok
7Basin Map of Chao Phraya River
http://hydro.iis.u-tokyo.ac.jp/Past flood and Damage situation(Source: JICA Report)
2011
8Return period of flood occurrence in Bangkok is 3 year
http://hydro.iis.u-tokyo.ac.jp/Situation of 2011 precipitation
The basin average precipitation in 1982‐2002 over
May‐Oct (5 months).
2011 was recorded maximum precipitation in
Jul. and Sep.
h l f i i iThe total amount of precipitation over May‐
Oct., 2011 is 143 % of 21 yrs average
precipitationprecipitation. ※The basin rainfall was caluculated by Voronoi diagram using TMD Observation Data.‐ Daily precipitation data of May.‐ Oct., 2011 (From GTS)‐ 1982‐2002 of daily precipitation data (From GAME‐T Data Center)
250
300
350
400Ave.1982‐2002_2011
Ave.1982‐2002 2011
100
150
200
250
0
50
100
May Jun. Jul. Aug. Sep. Oct.
161% 134% 178% 132% 144% 111%
http://hydro.iis.u-tokyo.ac.jp/Rainfall‐inundation
The total from May to October‐ Rainfall 1 192 mm 100 70 3070 %‐ Rainfall 1,192 mm‐ Pan evaporation 842 mm
100 – 70 = 30↓
70 %
120140
143 – 70 = 73
Runoff increase 243 %
Rainfall increase 143 %
6080100120
Runoff
Runoff increase 243 %
204060 Runoff
Evapotranspiration (& Infiltration)
0Normal year
This year
(& Infiltration)
1030 yrs average at Sukhothai observatory(1971‐2000)
http://hydro.iis.u-tokyo.ac.jp/The Impact of Typhoon in Thailand (2011)Provided by Assoc.Prof. Kanae, Tokyo Institute of Technology
4: HAIMA 8: NOCK‐TEN 17: NESAT 18: HAITANG 19: NALGAE
There are 5 typhoons which affected in Thailand.
6/21 ‐ 6/25 7/26 ‐ 7/31 9/24 ‐ 9/30 9/25 ‐ 9/27 9/27 ‐ 10/05
985 hPa 984 hPa 950 hPa 996 hPa 935 hPa
40 knots 50 knots 80 knots 35 knots 95 knots
The number of landfall in Thailand
‐ yearly average is 1.5
‐ only 3 years (1964, 1971, 1972)→ more than 5 landfalls
1951 1961 1971 1981 1991 2001 2010
‐ 1964, 1971 is La Nina year
11
http://hydro.iis.u-tokyo.ac.jp/
Si ikitダム Bhumibol DamSi ikit D
Inflow and discharge from major DamsSirikitダム
ダム貯水量(2011)
ダム貯水量(2011)
Bhumibol DamSirikit Dam
3 )
Total Storage Capacity 9.51×109㎥ Dam Storage (2011)
Total Storage Capacity 13.462×109㎥
Dam Storage (2011)
106 m
3 )
rage (×
106 m
3
am Storage (×
Sediment Storage 3 80×109 m3
Dam Storage (2006)Designed Storage
2,000 3,000 4,000
量、放流量
m3 /s)
流入量 (2011)放流量 (2011)
Nakhon Sawan
Dam
Sto
Sediment Storage 2.85×109 m3
Dam Storage (2006)Designed Storage Capacity
Da 3.80×109 m3 Designed Storage
Capacity
ge
Inflow (2011)
Discharge (2011)
0
100
(k ) ※流入量=(当日の貯水量-前日の貯水量)ー揚水発
0 1,000
流入量 (m
2,000
3,000
、放流量
m3 /s)
流入量 (2011)
放流量 (2011)流入量(2011)流出量(2011)
Ayutthaya
Bangkok
Discharge
m3 /s)
Inflow (2011)Discharge (2011)
Inflo
w ,
Discharg
(m3 /s)
※Inflow=Storage(day)‐Storage (a day before) pumping up for power generation(km)
データ出典:http://ichpp.egat.co.th/statusdam_report_internet.php
※流入量=(当日の貯水量-前日の貯水量)ー揚水発電のための汲み上げ量+放流量
0
1,000
流入量 (m
Inflo
w , (m – pumping up for power generation
+ discharge
Reference: http://ichpp.egat.co.th/statusdam_report_internet.php
・Inflow increased from the beginning of Jul. to the end of Oct.
・After the reservoir was fulfilled in the beginning of Oct., the inflow became to equal to the discharge.
・By the beginning of Oct., two reservoirs contained 10 billion m3. 12
http://hydro.iis.u-tokyo.ac.jp/Inundation area by satellite observationProvided by Assoc. Prof. Takeuchi, IIS, the University of Tokyo
‐ Yom river flood was struck at the confluence of Nan and Yom river, where is in downstream of Sirikit Dam.
Ratio of Inundation area in 16 X 16 km grid
http://hydro.iis.u-tokyo.ac.jp/
Flood SituationFlood Situation in Upstream Ayutthaya p y y
‐Why was the industrial park flooded ? ‐Why was the industrial park flooded ?
14
http://hydro.iis.u-tokyo.ac.jp/
abbr Co Compan
Flood in Ayutthaya and Industrial park
Nakhon Sawan
?Saha Rattananakorn Industrial ParkFlooded Co.: 42 (Japanese Co.: 35)
Oct. 4
j d i l k
abbr. :Co.= Company
Ayutthaya
Nakhon Sawan ? Oct. 9Rojana Industrial ParkFlooded Co.: 218 (Japanese Co.: 147)
Hi‐Tech Industrial Park
Ayutthaya100
Bangkok
Ayutthaya
0
100
(km)
Oct. 13Hi Tech Industrial ParkFlooded Co.: 143 (Japanese Co.: 100)
Bangpa‐In Industrial Park100
(km)
Flooded Ind. Park
Non‐flooded Ind. Park
Oct. 14gp
Flooded Co.: (Japanese Co.: 30)
Oct 15Factory Land Industrial Park
Bangkok0
Oct. 17Navanakorn Industrial ParkFl d d C (J C 104)
Oct. 15 Flooded Co.: 93 (Japanese Co.: 7)
Oct. 17Flooded Co.: (Japanese Co.:104)
Oct. 20Bangkadi Industrial ParkFlooded Co : (Japanese Co : 28)
‐ Flood struck Industrial parks in order, from upstream.
15
Flooded Co.: (Japanese Co.: 28)
Source from: http://www.jetro.go.jp/world/asia/th/flood/complex.html
‐ Flooded industrial park all located on the left bank
http://hydro.iis.u-tokyo.ac.jp/
Nakhon Sawan
Discharge Capacity of Chao Phraya River
Nakhon Sawan Nakhon Sawan3590
Ayutthaya
Nakhon Sawan
h h
Unit: (m3/s)Chao Phraya Dam
Sing Puri
Ayutthaya100
Bangkok
y y
0
100
(km)2840
Chao Phraya Dam(Large Intake Weir)Ang Thong
Sing Puri
100
(km)2340Sing Puri
Bangkok0 2690Ang Thong
Ayuttaya1155‐ Flood occurred over discharge capacity.
‐ Discharge capacity decrease in
16Discharge capacity of Chao Phraya River (Source: RID)
To Bangkokdownstream.
http://hydro.iis.u-tokyo.ac.jp/Day of overflow from Chaophraya river
Nakhon SawanSep. 153,590㎥/s
単位㎥
Nakhon Sawan3590
Sep. 112,840㎥/s
:㎥/s
h h
Unit: (m3/s)
Sep. 52 340㎥/
2840Chao Phraya Dam(Large Intake Weir)
d
2,340㎥/s
2340Sing Puri
No inundation2,690㎥/s
2690Ang Thong
Sep. 111,155㎥/s
Ayuttaya1155
Overflow was started in the beginning of Sept., from NakhonSawan to Ayuttaya
River discharge of each station17
To Bangkok
Discharge capacity of Chao Phraya River (Source: RID)
Sawan to Ayuttaya.
http://hydro.iis.u-tokyo.ac.jp/Inundation area by satellite observationProvided by Assoc. Prof. Takeuchi, IIS, the University of Tokyo
Ratio of Inundation area in 16 X 16 km grid
http://hydro.iis.u-tokyo.ac.jp/Breaking of Levee between Nakhon Sawan and Ayutthaya
8 le ee cre asses on the left bank ( ) L h f L C
1
① Sep. 22‐Oct. 28 (25m)
② Sep 24 about 2 weeks (1 300m)
‐ 8 levee crevasses on the left bank
from the middle to the end of Sept.
( ):Length of Levee Crevasse
1
2
② Sep.24‐about 2 weeks (1,300m)
③ Sep.18‐unknown (1,000m)
④ Sep 22‐unknown (20m)
Sept.
➔①,⑥ took 1 month to fix the levee 2
34 5
④ Sep. 22 unknown (20m)
⑤ Sep 22‐unknown (40m)
‐Most of levee crevasses locate
on a curve (water colliding front) ⑤ Sep. 22 unknown (40m)
【Video】 Inundation situation
⑥ Sep.13‐Oct.12(40m)
Nakhon Sawan
6⑦ S 14 b t
78
⑦ Sep.14‐about 2 weeks (20m)
⑧ Sep 17‐about
Ayutthaya
Provided fromRID
⑧ Sep.17‐about 2 weeks (40m)
Point of levee crevasse between Chao Phraya Dam and Ayutthaya (Source: RID)19
Bangkok
http://hydro.iis.u-tokyo.ac.jp/Traveling time from Levee Crevasse Point to Ayutthaya‐ Levee was broken from the middle
: Levee crevasseChao Phraya Dam
‐ Levee was broken from the middle to the end of Sept. ‐ On Oct. 4, flood was struck SahaR tt k I d t i l P k
Overflow Pa SakRiver and flow to downstream area
Rattananakorn Industrial Park.➔It takes about 2 weeks from levee crevasse point to industrial parks
(From the hearing at RID)
about 120kmSupposing 1) Slope: 1/50,000 and 2) Inundated water level: 2 m, flow
Nakhon Sawan
velocity is 0.14 m/s*.
In this case, it takes 10 days from
Pa Sak River
, ylevee crevasse point to industrial parks.
SahaRattananakornInd. Park
Ayutthaya
➔ It is reasonable values considering the influence of slow up effect by embankment and road.
20
Ayutthaya* Is calculated from Manning formula. Roughness coefficient is 0.08 considering the effect of paddy straw.
Ind. Park
BangkokThe point of levee crevasse and flood area
in Upstream Ayutthaya (Source: RID)
http://hydro.iis.u-tokyo.ac.jp/Inundation area by satellite observationProvided by Assoc. Prof. Takeuchi, IIS, the University of Tokyo
Ratio of Inundation area in 16 X 16 km grid
http://hydro.iis.u-tokyo.ac.jp/
m3/s
Estimation of flood volume from Nakhon Sawan to Ayutthaya
4000
4500
5000 NakhonSawan(C2)Chainat(C13)SingBuri(C3)
:Levee Crevasse
Chao Phraya Dam*Flood Volume
3000
3500
4000 SingBuri(C3)AngThong(C7A)
Flood Volume
Indicating nearly identical waveform until the
Bre Sing Puri
2000
2500 beginning of Sept.
eaking
1000
1500
of Leve
Ang Thong
0
500
6/1
6/11
6/21 7/1
7/11
7/21
7/31
8/10
8/20
8/30 9/9
9/19
9/29
10/9
0/19
0/29
Ayutthaya
ee➔About more than 5 billion m3 water inflow to floodplain on the
l f b k hi / f h l fl d l6 6 7 7 7 8 8 8 9 9 1 10 10
River discharge of each RID stations
Flood volume from Nakhon Sawan to Chao Phraya Dam is *1.8 billion m3.
left bank. This means 1/4 of the total flood volume.
22* Flood volume is calculated by removing the discharge capacities of Ta‐chin river and Noi river (650 m3/s).
Flood volume from Chao Phraya Dam to Ang Thong is 3.9 billion m3.
http://hydro.iis.u-tokyo.ac.jp/
R j I d t i l P k
Land Classification of Flood Disaster in Ayutthaya downstream
High‐Tech Industrial Park
:Industrial ParkRojana Industrial Park
Bangpa‐In Industrial Park
Lagoon Ⅱ
Navanakorn Industrial Park Back Marsh ⅢBack Marsh Ⅱ
Natural Levee Ⅱ
Asian institute of tech.
M f th ff t d i d t i l k i A tth l t d i th fl d l i(大倉・春山・大矢,1989)
‐Many of the affected industrial parks in Ayutthaya are located in the floodplain upstream of the narrow pass. ‐ Referring to the geomorphological map of flood damage, many of the industrial parks are located in back marshes or lagoons surrounded by natural levees. → It would take time to drain the flood water off since this area is a depression surrounded by a natural levee.
23
http://hydro.iis.u-tokyo.ac.jp/
Flood situation andFlood situation and flood fighting activity in Bangkok f f g g y g
‐ Is the capital, Bangkok, protected from flood? ‐Is the capital, Bangkok, protected from flood?
24
http://hydro.iis.u-tokyo.ac.jp/Synthesized design of flood control ‐ Plan and current situation ‐
Kings Dike
Flood① Set “Kings Dike”, Surrounding Levee, to protect Bangkok from flooding of north part
Gree
➔ height about 50 cm, and using it as road as well
➔ partially uncompleted enbelt
➔ partially uncompleted
②Set the regulation of land use around Kings Dike, and designated as Greenbeltdesignated as Greenbelt
➔Greenbelt plan exists on plan, but actually it became residential area and industrial
SuvarnabhumiInternational Airport
residential area and industrial park.
③In the future, diversion channelwill be constructed in
http://www.bangkokplan.org/documents/English_mapIn.pdf
Scheme of Bangkok Flood Control Plan
will be constructed in Greenbelt.
➔Suvarnabhumi International Ai t t t d i
25➔In fact, it didn’t implement as planned. Airport was constructed in downstream of greenbelt
http://hydro.iis.u-tokyo.ac.jp/Flood Fighting in East BangkokBasic idea is that water from
Navanakorn industrial complex(Start inundated around18th OCT.)
Basic idea is that water from upstream should be diverted along East‐West direction canal.➔building a temporary dike for
P【Present situation】Two routes exist for drainage.
( )➔building a temporary dike for draining water to Banpakorn river.
PP
P
PTwo routes exist for drainage.① One route is to divert the water to Banpakorn river by closing the water gate of canal HokWa and building a
Temporary dike
PPg g
temporary dike along canal.②Another route is to drain the water to the sea and downstream of Central Bangkok
Banpakor
PPSuvarnabhumi
Banpakorn river by opening the part of the water gate from canal HokWaand utilizing the downstream canal
Central Bangkok rnRiver
PInternational Airportnetwork.
➔From the viewpoint of prompt drainage, it is wiser to conduct ②.
26Royal Thai Survey Department: http://www.rtsd.mi.th/index.php
PP
PPPPPPPPPBut considering the land use and drainage capacity in downstream area,① is the major measurement.
http://hydro.iis.u-tokyo.ac.jp/Flood fighting in West Bangkok
Flood water flowed over Kings
Flood
Flood water flowed over Kings Dike and inundated the downstream areas.
Kings Dike It is necessary to protect
1Central Bangkok
the national road toward South-West Thailand.
• Drain the water using North-South 2
BangkokPP
canal and divert into two directions at Pasri Chari canalタ
ーチン川
Pasri Chari canal.①Chao Phraya River②Th Chi Ri
タ
②Tha Chin River
http://hydro.iis.u-tokyo.ac.jp/Conclusion
1) One of the main cause of the 2011 flood is the high precipitation.
2) Y i fl d t k t th fl f N d Y2) Yom river flood was struck at the confluence of Nan and Yom river, where is in downstream of Sirikit Dam.
3) Both Bhumibol and Sirikit Dam were contained about 10 billion m3 of water until full capacity in the beginning of Oct.
4) In the Ayutthaya upstream, the flood was struck the industrial k d A tth b b ki f lparks around Ayutthaya by breaking of levee.
5) The flood volume from the levee crevasse point is more than 55) The flood volume from the levee crevasse point is more than 5 billion m3.
28
6) The flood fighting activity in Bangkok is to drainage using the east‐west channel for the upstream flooding.
http://hydro.iis.u-tokyo.ac.jp/Supplement
• Flood field survey team– The University of Tokyo
Daisuke KOMORI, Shinichiro NAKAMURA, Kazuo OKI, Masashi KIGUCHI, AsakoNISHIJIMA, Dai YAMAZAKI, Jeanne FERNANDEZ, Jiro KAKEHASHI, Cherry MATEO, Misato OKANEYA, Takahiro TSUNEKAWA, Taikan OKI
– Thai researcherPhonchai Klinkhachorn, Thada Sukapunnapan, Vanisa Surapipith, AdisornChampathong, Nontawat Junjaroen
• Cooperation toward field survey and Provision of information– The University of Tokyo
A P f W T k hi A P f Aki ki KAWASAKI Hi ki YUTANIAssoc.Prof. Wataru Takeuchi , Assoc.Prof. Akiyuki KAWASAKI, Hiroaki YUTANIMichio MURAKAMI, Yukio TANAKA “Wisdom of Water (SUNTORY)”
– Tokyo Institute of Technology Assoc.Prof. Shinjiro KANAE
– JICAKimio TAKEYA (JICA Visiting Semior Advisor), Akihisa TANAKA, Kai KIKUIRI, KatsuyaMIYOSHI, Mikiko NAGAI, Kobchai Songsrisanga, Mesinee Sarikaputi
– JAXAShinichi SOBUE, Makoto KAWAI
29
http://hydro.iis.u-tokyo.ac.jp/
Thank you for joining us during the massive flood 2011 Chao Phraya Rivermassive flood 2011, Chao Phraya River