Flood in Jakarta as Impact of Climate Change
10:3 Flood in Jakarta as Impact of Climate Change Dr. Armi Susandi, MT.
Head of Meteorology Department, ITB
Mini-Symposium: “Flood Risk and Adaptation in Jakarta” th OUTLINE
Historical Data of Flood in Jakarta
Vulnerable Areas of Flood in Jakarta
Cause of Flood in Jakarta:
- Tide Activity - Shipment Flood
Accumulation of Floods in Jakarta
Adaptation to impact of Climate Change in Jakarta
Extended Area Research on West Java
- Land Use Change and Climate Change in Citarum River - Sea Level Rise in Indramayu and Subang
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7 1621 1654 1918 1942 1976 1996 2002 2003 2004 2005 2006 2007 2008
Historical Data of Flood in Jakarta Source : Flood Report of Department of Public Work, 2007 Year
F re q u e n c y
Banjir Jakarta Saat ini
78 Points of Inundated Area
Source : Department of Public Work, 2007
FLOW Source : Department of Public Work, 2007
Causes of Flood in Jakarta
Non Permanent (Short Term) - Flood in Jakarta is affected by tide activity.
- Flood in Jakarta is caused by “Shipment Flood”.
Permanent (Long Term) - Flood is caused by Sea Level Rise.
Extremely event - Accumulation of floods from non permanent and permanent flood.
Flood in Jakarta as
Implication of Tide Activity
Penjaringan Pademangan Tanjung Priok Koja Cilincing Soekarno-Hatta Airport Monumen Nasional
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Penjaringan Pademangan Tanjung Priok Koja Cilincing Soekarno-Hatta Airport Monumen Nasional
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Penjaringan Pademangan Tanjung Priok Koja Cilincing Soekarno-Hatta Airport Monumen Nasional
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Penjaringan Pademangan Tanjung Priok Koja Cilincing Soekarno-Hatta Airport Monumen Nasional
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Penjaringan Pademangan Tanjung Priok Koja Cilincing Soekarno-Hatta Airport Monumen Nasional
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Penjaringan Pademangan Tanjung Priok Koja Cilincing Soekarno-Hatta Airport Monumen Nasional
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Penjaringan Pademangan Tanjung Priok Koja Cilincing Soekarno-Hatta Airport Monumen Nasional
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Penjaringan Pademangan Tanjung Priok Koja Cilincing Soekarno-Hatta Airport Monumen Nasional
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Penjaringan Pademangan Tanjung Priok Koja Cilincing Soekarno-Hatta Airport Monumen Nasional
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Penjaringan Pademangan Tanjung Priok Koja Cilincing Soekarno-Hatta Airport Monumen Nasional
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Penjaringan Pademangan Tanjung Priok Koja Cilincing Soekarno-Hatta Airport Monumen Nasional
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Penjaringan Pademangan Tanjung Priok Koja Cilincing Soekarno-Hatta Airport Monumen Nasional
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Penjaringan Pademangan Tanjung Priok Koja Cilincing Soekarno-Hatta Airport Monumen Nasional
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Penjaringan Pademangan Tanjung Priok Koja Cilincing Soekarno-Hatta Airport Monumen Nasional
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Penjaringan Pademangan Tanjung Priok Koja Cilincing Soekarno-Hatta Airport Monumen Nasional
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Penjaringan Pademangan Tanjung Priok Koja Cilincing Soekarno-Hatta Airport Monumen Nasional
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Penjaringan Pademangan Tanjung Priok Koja Cilincing Soekarno-Hatta Airport Monumen Nasional
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Penjaringan Pademangan Tanjung Priok Koja Cilincing Soekarno-Hatta Airport Monumen Nasional
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Penjaringan Pademangan Tanjung Priok Koja Cilincing Soekarno-Hatta Airport Monumen Nasional
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Penjaringan Pademangan Tanjung Priok Koja Cilincing Soekarno-Hatta Airport Monumen Nasional
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Penjaringan Pademangan Tanjung Priok Koja Cilincing Soekarno-Hatta Airport Monumen Nasional
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Penjaringan Pademangan Tanjung Priok Koja Cilincing Soekarno-Hatta Airport Monumen Nasional
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Causes of Tidal Wave (ROB) Flood :
Map of Land Subsidence (1982-1997) PETA PENURUNAN MUKAN TANAH TAHUN 1982-1997
N W E Penjaringan S Koja
Pademangan Cilincing
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2
4 Km Kalideres Tanjung Priok Taman Sari
Tambora Cengkareng Sawah Besar Kelapa Gading
Grogol Petamburan Kemayoran Gambir Cempaka Putih Senen
Cakung Kebon Jeruk Pulo Gadung Menteng
Kembangan Palmerah KETERANGAN :
Matraman Tanah Abang Administrasi Kecamatan Sungai
Setiabudi Penurunan Muka Tanah (Meter) : Jatinegara Kebayoran Baru Tebet
Duren Sawit 0.012 - 0.024 0.024 - 0.036 Pesanggrahan
Kebayoran BAru 0.036 - 0.048 Pancoran
Kebayoran Lama 0.048 - 0.06 Mampang Prapatan Makasar 0.06 - 0.072 0.072 - 0.084
Kramatjati 0.084 - 0.096 Pasar Minggu 0.096 - 0.108 Cilandak 0.108 - 0.12 Cipayung No Data Wilayah DKI Jakarta
Source : Dinas Pertambangan dan Energi Propinsi DKI Jakarta
Trend of Land Subsidence in Jakarta
Trend factor
- 41
- 55
- 72
- 60
- 40
- 20 1985 1990 1995 2000 2005 2010 2015 2020 2025 2030 2035 2040 2045 2050 Tahun
- Land Use Change and Climate Change in Citarum River
- Sea Level Rise in Subang and Indramayu
- For better planning in considering climate condition (climate change) in order to reach sustainable development (e.g. water resource management, agriculture)
- Long term mean climate change (exposure’s mean
- To reduce possibilty of disaster occurrence caused of climate (e.g. flood, drought, forest fire, landslide)
- Potency of extreme climate intensity and frequency (variability of
P en ur un an t an ah ( cm )
0.8 cm/year La nd S ub si de nc e (c m )
Year
Source : Priyambodo, 2005
Causes of Tidal Wave (ROB) Flood :
1. Land Subsidence
2. High Rainfall
Raifall in Jakarta will be increase caused by
a lot of water vapors . This situation is affected by warming over sea level.
Historical Data of Temperature
Change in Jakarta Region
Historical Data of Temperature Change in
Jakarta Region00:00 GMT October 2008
01:00 GMT October 2008
02:00 GMT October 2008
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04:00 GMT October 2008
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Mean Rainfall Anomalies in Jakarta Region Rainfall Anomalies in Jakarta (1996-2005)
Increase of rainfall is
occurred in rain season( January ) over Jakarta
region during period of 1996-2005. The increase is range of 20-200 mm .
The highest increase of the region is Pulogadung.
Potency of flood occurrence will be high. Rainfall Anomalies in Jakarta (1996-2005)
Period of Transition Season ( March ) will be increase of rainfall in high level over Jakarta and its surroundings.
The increase will be range of 60-540 mm.
South Jakarta to Bogor are region which have high increase of rainfall.
Most of Shipment Flood come from Bogor. Projection of Rainfall Anomalies in Jakarta (1996-2035)
The projection in rain season ( January ) from 1996 to 2035 shows increase of rainfall in North Jakarta Region .
The increase is range of 10 – 110 mm .
Potency of huge food will be occurred in North Jakarta. Projection of Rainfall Anomalies in Jakarta (1996-2035)
There is increase of rainfall about 50 – 550 mm in South Jakarta region to Bogor .
(For transition period March ) -
Potency of food in South Jakarta is “shipment food” from Bogor Region.
Flood in Jakarta as
“Shipment Flood”
Projection of
Rainfall over
Maximum Rainfall is 360 mm.
In South Region of
JakartaJakarta (January 2015 )
Maximum Rainfall is
360 mm.In South of Jakarta (Slowly spread towards North)
Projection of Rainfall over Jakarta
(January 2020 ) Maximum Rainfall is 370 mm.
In South of Jakarta
(Slowly spread towards North)
Projection of Rainfall over Jakarta (January 2025 )
Maximum Rainfall is 370 mm.
In South of Jakarta
(Slowly spread towards North)
Projection of Rainfall over Jakarta (January 2030 )
Maximum Rainfall is 380 mm.
In South of Jakarta
(Slowly spread towards North)
Projection of Rainfall over Jakarta (January 2035 )
Permanent Flood in Jakarta is Caused by Sea Level Rise Sea level rise caused by climate change is projected continues to increase.
Global Sea Level Rise 1880 – 2000 (IPCC, 2003)
in Jakarta Trend of Sea Level Rise Trend factor cm/year
0.57 140
) 123.06 m
105 (c
108.69 el
94.31 ev L
79.94
70 ea S
65.56 n
51.19 ea
1925 1950 1975 2000 2025 2050 Year
Source : Meliana, 2005
Dike as a sea water resistor
Sea level rise causes water to pass over dike.
If tidal wave occur, water will be overflow to land area.
200
5 North Source: Hadi, Susandi et al., 2007
201 Tanjung Priok Cilincin g Source: Hadi, Susandi et al., 2007
North
201
5 Pademang an Tanjung Priok Koj a Cilincin g Source: Hadi, Susandi et al., 2007
North
202 Pademang an Tanjung Priok Koj a Cilincin g Source: Hadi, Susandi et al., 2007
North
202
5 Penjaring an Pademang an Tanjung Priok Koj a Cilincin g Source: Hadi, Susandi et al., 2007
North
203 Penjaring an Pademang an Tanjung Priok Koj a Cilincin g
Soekarno-Hatta Airport
Source: Hadi, Susandi et al., 2007 North
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5 Cilincin g Koj Tanjung a Priok Pademang an Penjaring an
Soekarno-Hatta Airport
North Source: Hadi, Susandi et al., 2007
204 Penjaring an Pademang an Tanjung Priok Koj a Cilincin g
Soekarno-Hatta Airport
Source: Hadi, Susandi et al., 2007 North
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5 Penjaring an Pademang an Tanjung Priok Koj a Cilincin g
Soekarno-Hatta Airport
Source: Hadi, Susandi et al., 2007 North
205 Penjaring an Pademang an Tanjung Priok Koj a Cilincin g
Soekarno-Hatta Airport
Source: Hadi, Susandi et al., 2007 North
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Monumen Nasional? (2080?)
Cilincin g Koj Tanjung Water will inundate a Priok Jakarta region as area Pademang
2 ± 160,4 km an ( 24,3% Area of Jakarta )
Penjaring in 2050 an
Soekarno-Hatta Airport
North Source: Hadi, Susandi et al., 2007
It will occur accumulation of floods in Jakarta
by the year 2050.Projection of Inundated Area in Jakarta ) 180 )
2 160.37 156.13
2 m m K (K ( n a
135 re ga A
91.35 an
79.28
76.83 ed en at
nd
54.44
57.43 s
38.38 nu f I ua
63.64
46.81
45 o L
35.70
48.69
55.05 al
41.58 al
33.64 ot ot T T
2010 2015 2020 2025 2030 2035 2040 2045 2050 Tahun Year Mean Scenario Max. Scenario Min. Scenario
Skenario Min Skenario Rata-rata Skenario Max
Total Loss of Economic Sector in Jakarta Caused by Sea Level Rise
Min. Scenario Mean Scenario Max. Scenario Flood which is frequently occurred in Jakarta is caused by increasing of rainfall , sea level rise , and tidal wave .
SUMMARY
Adaptation to Climate Change in Jakarta Adaptation to be conducted
Planting Mangrove
Building Seawall (Water Resist Wall)
Utilizing water abundant from South Area as main water resource in Jakarta
Building Polder (Water Entrapment)
ILUSTRATION
Water Resource
Water SpaceWater Flow Pipe
PolderMangrove Seawall
Extended Area to West Java
Land Use Change and Climate Change (Citarum River)
Flow Chart of The Research Satellite Image Landsat TM
8 Band Image Satellite Landsat TM
Ground Types Map Groundwater Calculation
NDVI Projection Land Use Map Map of Land use projection
NDVI Calculation Image Digitation
Image Classification PROJECTION MAP Direct Runoff, Baseflow, Temperature
& Rainfall Climate Data
Overlay of Land Use Map – Types of Ground
Climate Projection Land Use Map Curug
PURWAKARTA Jatiluhur Cikumpay Cibeurum
Cirata CIRANJANG Rajamandala Projection of Temperature over Citarum Region
TemperatureTemperature in January 2001 Temperature
Temperature in January 2010 Temperature
Temperature in January 2020 Temperature
Temperature in July 2001 Temperature
Temperature in July 2010 Temperature
Temperature in July 2020
Projection of Rainfall over Citarum Region Rainfall
Rainfall in January 2020 Rainfall
Rainfall in July 2020 Direct Runoff PURWAKARTA
Cibeurum Curug CIRANJANG Rajamandala Direct Runoff PURWAKARTA
Cibeurum Curug CIRANJANG Rajamandala Baseflow PURWAKARTA
Cibeurum Curug CIRANJANG Rajamandala Baseflow PURWAKARTA
Cibeurum Curug CIRANJANG Rajamandala Flood Vulnerable Region PURWAKARTA
Cibeurum Curug CIRANJANG Rajamandala Sea Level Rise in Subang and Indramayu
Indramayu Subang (Source: Susandi, 2008) Sea Level Rise in
Indramayu Region
2010 Indramayu Losarang
Kandanghaur
Sindang
(Source: Susandi, 2008)2015 Indramayu Losarang
Kandanghaur
Sindang
(Source: Susandi, 2008)2020 Indramayu Losarang
Kandanghaur
Sindang
(Source: Susandi, 2008)2030 Indramayu Losarang
Kandanghaur
Sindang
(Source: Susandi, 2008)
2040 Indramayu Losarang
Kandanghaur
Sindang
(Source: Susandi, 2008)
2050 Indramayu Losarang
Kandanghaur
Sindang
(Source: Susandi, 2008)
2060 Indramayu Losarang
Kandanghaur
Sindang
(Source: Susandi, 2008)
2070 Indramayu Losarang
Kandanghaur
Sindang
(Source: Susandi, 2008)
2080 Indramayu Losarang
Kandanghaur
Sindang
(Source: Susandi, 2008)2090 Indramayu
Losarang Kandanghaur
Sindang
(Source: Susandi, 2008)
2100 Indramayu
Losarang Kandanghaur Sindang
Inundated area = 1,63 km
2 (Source: Susandi, 2008) Sea Level Rise in Subang Region
2010
Legonkulon
Pamanukan Pusakanagara (Source: Susandi, 2008)
2015
Legonkulon
Pamanukan Pusakanagara (Source: Susandi, 2008)
2020
Legonkulon
Pamanukan Pusakanagara (Source: Susandi, 2008)
2030
Legonkulon
Pamanukan Pusakanagara (Source: Susandi, 2008)
2040
Legonkulon
Pamanukan Pusakanagara (Source: Susandi, 2008)
2050
Legonkulon
Pamanukan Pusakanagara (Source: Susandi, 2008)
2060
Legonkulon
Pamanukan Pusakanagara (Source: Susandi, 2008)
2070
Legonkulon
Pamanukan Pusakanagara (Source: Susandi, 2008)
2080
Legonkulon
Pamanukan Pusakanagara (Source: Susandi, 2008)
2090
Legonkulon
Pamanukan Pusakanagara (Source: Susandi, 2008)
2100 Legonkulon
Pamanukan Pusakanagara (Source: Susandi, 2008)
Inundated area = 2,05 km
2
armi@geoph.itb.ac.id
www.armisusandi.com
Impacts Responses Adaptation Mitigation
Climate change and variability
Types of climate data needs to assess the impact:
The Objective of adaptation:
change)
exposures)