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

  2

  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
  • 62
  • 55
  •   P en ur un an t an ah ( cm )

      0.8 cm/year La nd S ub si de nc e (c m )

    • 72
    • 78 80
    • 60
    • 40
    • 20 1985 1990 1995 2000 2005 2010 2015 2020 2025 2030 2035 2040 2045 2050 Tahun

      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 Region

      00:00 GMT October 2008

      01:00 GMT October 2008

      02:00 GMT October 2008

      03:00 GMT October 2008

      04:00 GMT October 2008

      05:00 GMT October 2008

      06:00 GMT October 2008

      07:00 GMT October 2008

      08:00 GMT October 2008

      09:00 GMT October 2008

      10:00 GMT October 2008

      11:00 GMT October 2008

      12:00 GMT October 2008

      13:00 GMT October 2008

      14:00 GMT October 2008

      15:00 GMT October 2008

      16:00 GMT October 2008

      17:00 GMT October 2008

      18:00 GMT October 2008

      19:00 GMT October 2008

      20:00 GMT October 2008

      21:00 GMT October 2008

      22:00 GMT October 2008

      23:00 GMT October 2008

      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

    Jakarta

    Jakarta (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

      203

      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

      204

      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

      205

      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 Space

    Water Flow Pipe

    Polder

      Mangrove Seawall

      

    Extended Area to West Java

    • - Land Use Change and Climate Change in Citarum River

      - Sea Level Rise in Subang and Indramayu

      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

    Temperature

      Temperature 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:

    • 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

      change)

    • 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

      exposures)