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UPCOE-ICE-NHRC Public Presentation Typhoon Ondoy (Ketsana) and the Marikina River Flood of September 26, 2009 Venue: Beta Epsilon Multi Media Hall, Melchor Hall, UPD Time: 9:00-10:30 AM, Friday, October 2, 2009     PROGRAM   Opening Remarks (9:00-9:10 AM) Dean Rowena Cristina Guevara   Presentations* (9:10 – 10:20 AM)    Typhoon Ondoy Rainfall Intensity-Duration-Frequency Statistics   Marikina River Basin Flood, Hydraulics and Issues   Proposed Multi-Hazard Risk Assessment & Capacity Building for Metro Manila Flood Issues, Management and Climate Change   Open Forum (10:20 – 11:00 AM)   Closing     *Speakers include Dr. Leonardo Q. Liongson and Dr. Guillermo Q. Tabios III  of the UPCOE Institute of Civil Engineering
TS Ketsana-Ondoy  Rainfall Intensity-Duration-Frequency  & Flood-Frequency Statistics Leonardo Q. Liongson Professor, Institute of Civil Engineering  and Research Fellow, National Hydraulic Research Center College of Engineering, UP Diliman 2 October 2009 Beta Epsilon Multi-Media Hall Melchor Hall, UPCOE, UP Diliman
METRO-MANILA: Meycauayan (until early 1980s) Kamanava: Kalookan, Malabon, Navotas, Valenzuela Manila   Quezon City,  Marikina,  San Juan,  Mandaluyong, Pasig,  Makati,   Pateros-  Pasay, Taguig, Parañaque, Las Piñas,  Muntinlupa. Brief Background: the River Basins of Metro Manila.
Metro Manila  -   is composed of  7 small highly  urbanized river sub-basins (702 sq. km.) which drain  directly to  Manila Bay ,  and through  Pasig River ,  serves as the  only outlet of  one major tributary basin,  the  Marikina River  Basin   (535 sq. km.)  in the northeast , and  one extensive lake region, the  Laguna de Bay Basin  with 21 tributary SBs : 2300 sq. km. Lake area :  929 sq. km.  Total basin area:  3229 sq.km.  in the southeast.   Marikina   River Pasig River Laguna de Bay Manila Bay
Top: Marikina River  @Wawa Dam at Montalban  gorge as seen in the  early 1990’s. Left: The towns of  Rodriguez (Montalban),  San Mateo, Marikina & Pasig along Marikina River.
Metro-Manila Rivers: Name of River Basins  Drainage Area (sq.km.) Marikina RB  535 Mangahan Floodway-Taytay RB  63 Taguig-Napindan RB  45 Meycauayan RB  169 Obando-Malabon-Navotas Estuary  35 Novaliches Reservoir-Tullahan RB  72 San Juan RB  94 Pasig RB (north and south)  91 Parañaque-Las-Piñas RBs  73 Zapote-Bacoor-Imus  RBs  168 Source: NHRC
The detailed river network of Marikina River Basin above Sto. Niño (DA=535 sq.km.):  the basis of the NHRC SWATCH physics-based distributed hydrological (rainfall-runoff) model .
(NHRC) Marikina River Basin (535 sq.km.) and the 21  sub-basins  & lake of the  Laguna de Bay Basin (3229 sq.km.)
(NHRC) Marikina River Basin (535 sq.km.) and the 21  sub-basins  & lake of the  Laguna de Bay Basin (3229 sq.km.)
(Wikipedia) Marikina RB Pasig RB Mangahan Floodway
(Badilla 2008)
(JICA)
(NHRC)
(NHRC)
Mean daily streamflow in Marikina River at Sto Ni ñ o in year 1990.
EFCOS: Effective Flood Control Operations System (located in Metro-Manila & Rizal province) ,[object Object],[object Object],[object Object],[object Object],Effective Flood Control  Operating System (EFCOS)  of Metro Manila – was discontinued by MMDA.
The  Mangahan Floodway diverts floodwaters of Marikina River to Laguna de Bay.  The  Napindan Hydraulic Control Structure (NHCS) regulates flow between  Pasig River and the lake via the Napindan Channel The  navigation lock  of the  NHCS allows water traffic between Pasig River and Laguna de Bay through the Napindan Channel.
Track of TS Ketsana (Ondoy) –  from Joint Typhoon Warning Center (JTWC), US Navy
(PAGASA)
 
Flooding started fast at the SM North EDSA, Quezon City  (Flickr) .
Large runoff on pavements and underground floods in  the Ayala underpass, Makati  (Flickr).
Inundation of the  Provident Village in Marikina City (Googlemap; Flickr).
Coping aboard fiberglass boats in Bay, Laguna  (Flickr – IRRI).
Collapse of a wall of the Mangahan Floodway  near Rosario Bridge, Pasig City. (Googlemap; Flickr).
Property damage (Flickr).
Suffering  and death (Flickr).
And a safe passage. (www.op.gov.ph and Flickr)
8 meters high 5 meters high Marikina Riverbank 9/28/2009. Downstream view of Rosario Weir  along Marikina River.
Preliminary Computations SWATCH-computed Peak Flood Discharge = 5770 cu.m./s of Marikina River  at Sto Ni ñ o  on 26 September 2009, based on the Point Hourly Rainfall  at Science Garden, QC Synoptic Station with applied area reduction  factor = 0.6 (NHRC)
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
4. Probable Annual Max.  Discharge of Marikina River at Sto Nino station (by Log Normal Prob. Dist. and Flood Runoff Model) Return  Max. Discharge, m 3 /s  period  Existing    Future  (years)  Land Use    Land Use   Sto Nino Sto Nino Rosario 2  1350 1470 1480  5  1870 2020 2000 10  2210 2350 2320 20  2550 2740 2720 30  2740  2900  2890 (design flood) 50  2980 3120 3070 100  3310 3430 3440 Comments: The 30-year flood of 2740 m 3 /s has not yet been experienced in the 42-year period of record, 1958-2000. However, the 20-year flood of 2550 m 3 /s was exceeded in 1986. 3. Historical Annual Maximum Discharge of Marikina River  at Sto Nino, Marikina Year  Max. Discharge, m 3 /s  1986  2650 1970  2464 1959  2072 1977  2051 1966  2036 2000  1895 1998  1680 1995  1676 1999  1642 1967  1609 etc.
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Thank You.

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Ts Ketsana Ondoy 2009 Oct02

  • 1. UPCOE-ICE-NHRC Public Presentation Typhoon Ondoy (Ketsana) and the Marikina River Flood of September 26, 2009 Venue: Beta Epsilon Multi Media Hall, Melchor Hall, UPD Time: 9:00-10:30 AM, Friday, October 2, 2009     PROGRAM   Opening Remarks (9:00-9:10 AM) Dean Rowena Cristina Guevara   Presentations* (9:10 – 10:20 AM)   Typhoon Ondoy Rainfall Intensity-Duration-Frequency Statistics   Marikina River Basin Flood, Hydraulics and Issues   Proposed Multi-Hazard Risk Assessment & Capacity Building for Metro Manila Flood Issues, Management and Climate Change   Open Forum (10:20 – 11:00 AM)   Closing   *Speakers include Dr. Leonardo Q. Liongson and Dr. Guillermo Q. Tabios III of the UPCOE Institute of Civil Engineering
  • 2. TS Ketsana-Ondoy Rainfall Intensity-Duration-Frequency & Flood-Frequency Statistics Leonardo Q. Liongson Professor, Institute of Civil Engineering and Research Fellow, National Hydraulic Research Center College of Engineering, UP Diliman 2 October 2009 Beta Epsilon Multi-Media Hall Melchor Hall, UPCOE, UP Diliman
  • 3. METRO-MANILA: Meycauayan (until early 1980s) Kamanava: Kalookan, Malabon, Navotas, Valenzuela Manila Quezon City, Marikina, San Juan, Mandaluyong, Pasig, Makati, Pateros- Pasay, Taguig, Parañaque, Las Piñas, Muntinlupa. Brief Background: the River Basins of Metro Manila.
  • 4. Metro Manila - is composed of 7 small highly urbanized river sub-basins (702 sq. km.) which drain directly to Manila Bay , and through Pasig River , serves as the only outlet of one major tributary basin, the Marikina River Basin (535 sq. km.) in the northeast , and one extensive lake region, the Laguna de Bay Basin with 21 tributary SBs : 2300 sq. km. Lake area : 929 sq. km. Total basin area: 3229 sq.km. in the southeast. Marikina River Pasig River Laguna de Bay Manila Bay
  • 5. Top: Marikina River @Wawa Dam at Montalban gorge as seen in the early 1990’s. Left: The towns of Rodriguez (Montalban), San Mateo, Marikina & Pasig along Marikina River.
  • 6. Metro-Manila Rivers: Name of River Basins Drainage Area (sq.km.) Marikina RB 535 Mangahan Floodway-Taytay RB 63 Taguig-Napindan RB 45 Meycauayan RB 169 Obando-Malabon-Navotas Estuary 35 Novaliches Reservoir-Tullahan RB 72 San Juan RB 94 Pasig RB (north and south) 91 Parañaque-Las-Piñas RBs 73 Zapote-Bacoor-Imus RBs 168 Source: NHRC
  • 7. The detailed river network of Marikina River Basin above Sto. Niño (DA=535 sq.km.): the basis of the NHRC SWATCH physics-based distributed hydrological (rainfall-runoff) model .
  • 8. (NHRC) Marikina River Basin (535 sq.km.) and the 21 sub-basins & lake of the Laguna de Bay Basin (3229 sq.km.)
  • 9. (NHRC) Marikina River Basin (535 sq.km.) and the 21 sub-basins & lake of the Laguna de Bay Basin (3229 sq.km.)
  • 10. (Wikipedia) Marikina RB Pasig RB Mangahan Floodway
  • 15. Mean daily streamflow in Marikina River at Sto Ni ñ o in year 1990.
  • 16.
  • 17. The Mangahan Floodway diverts floodwaters of Marikina River to Laguna de Bay. The Napindan Hydraulic Control Structure (NHCS) regulates flow between Pasig River and the lake via the Napindan Channel The navigation lock of the NHCS allows water traffic between Pasig River and Laguna de Bay through the Napindan Channel.
  • 18. Track of TS Ketsana (Ondoy) – from Joint Typhoon Warning Center (JTWC), US Navy
  • 20.  
  • 21. Flooding started fast at the SM North EDSA, Quezon City (Flickr) .
  • 22. Large runoff on pavements and underground floods in the Ayala underpass, Makati (Flickr).
  • 23. Inundation of the Provident Village in Marikina City (Googlemap; Flickr).
  • 24. Coping aboard fiberglass boats in Bay, Laguna (Flickr – IRRI).
  • 25. Collapse of a wall of the Mangahan Floodway near Rosario Bridge, Pasig City. (Googlemap; Flickr).
  • 27. Suffering and death (Flickr).
  • 28. And a safe passage. (www.op.gov.ph and Flickr)
  • 29. 8 meters high 5 meters high Marikina Riverbank 9/28/2009. Downstream view of Rosario Weir along Marikina River.
  • 30. Preliminary Computations SWATCH-computed Peak Flood Discharge = 5770 cu.m./s of Marikina River at Sto Ni ñ o on 26 September 2009, based on the Point Hourly Rainfall at Science Garden, QC Synoptic Station with applied area reduction factor = 0.6 (NHRC)
  • 31.
  • 32.
  • 33.
  • 34.
  • 35.
  • 36. 4. Probable Annual Max. Discharge of Marikina River at Sto Nino station (by Log Normal Prob. Dist. and Flood Runoff Model) Return Max. Discharge, m 3 /s period Existing Future (years) Land Use Land Use Sto Nino Sto Nino Rosario 2 1350 1470 1480 5 1870 2020 2000 10 2210 2350 2320 20 2550 2740 2720 30 2740 2900 2890 (design flood) 50 2980 3120 3070 100 3310 3430 3440 Comments: The 30-year flood of 2740 m 3 /s has not yet been experienced in the 42-year period of record, 1958-2000. However, the 20-year flood of 2550 m 3 /s was exceeded in 1986. 3. Historical Annual Maximum Discharge of Marikina River at Sto Nino, Marikina Year Max. Discharge, m 3 /s 1986 2650 1970 2464 1959 2072 1977 2051 1966 2036 2000 1895 1998 1680 1995 1676 1999 1642 1967 1609 etc.
  • 37.