Tropical Depression il St T il St Tropical Storm Typhoon
Transcription
Tropical Depression il St T il St Tropical Storm Typhoon
8/26/2011 DOST DOST PAGASA PAGASA EYE NESTOR B. NIMES Weather Specialist I Task Leader Department of Science and Technology Philippine Atmospheric, Geophysical and Astronomical Services Administration PAGASA, DOST Typhoon Paeng, October 24-31,2006 DOST DOST THE PHILIPPINE AREA OF RESPONSIBILITY [PAR] PAGASA PAGASA Tropical Depression ( Maximum winds less than 64 KPH ) Tropical T i l Storm St ( Maximum winds 64 to 117 KPH ) Typhoon (Maximum winds greater than 117 KPH ) (Super Typhoon- was conceived by JTWC with max winds of greater than 200 kph near the center) NAMES OF TROPICAL CYCLONES IN THE PHILIPPINES A B C D E F G H I J K L M N O P Q R S T U V W Y Z • • • • • • • • • • • • • • • • • • • • • • • • • I 2001 2005 2009 2013 AURING BISING CRISING DANTE EMONG FERIA GORIO HUANING ISANG JOLINA KIKO LABUYO MARING NANDO ONDOY PEPENG QUEDAN RAMIL SANTI TINO URDUJA VINTA WILMA YOLANDA ZORAIDA II 2002 2006 2010 2014 AGATON BASYANG CALOY DOMENG ESTER FLORITA GLENDA HENRY INDAY JUAN KATRING LUIS MILENYO NENENG OMPONG PAENG QUENNIE REMING SENIANG TOMAS USMAN VENUS WALDO YAYANG ZENY III 2003 2007 2011 2015 AMANG BEBENG CHEDENG DODONG EGAY FALCON GORING HANNA INENG JUANING KABAYAN LANDO MINA NIÑA NI ÑA ONYOK PEDRING QUIEL RAMON SENDONG TISOY URSULA VIRING WENG YOYOY ZIGZAG IV 2004 2008 2012 2016 AMBO BUTCHOY COSME DINDO ENTENG FRANK GENER HELEN IGME JULIAN KAREN LAWIN MARCE NONOY OFEL PABLO QUINTA ROLLY SIONY TONYO ULYSSES VICKY WARREN YOYONG ZOSIMO AUXILLIARY NAMES OF TROPICAL CYCLONES DOST PAGASA A B C D E F G H I J • • • • • • • • • • I 2001 2005 2009 2013 ALAMID BRUNO CONCHING DOLOR ERNIE FLORANTE GERARDO HERNAN ISKO JEROME II 2002 2006 2010 2014 AGILA BAGWIS CHITO DIEGO ELENA FELINO GUNDING HARRIET INDANG JESSA III 2003 2007 2011 2015 ABE BERTO CHARO DADO ESTOY FELION GENING HERNAN IRMA JAIME IV 2004 2008 2012 2016 ALAKDAN BALDO CLARA DENCIO ESTONG FELIPE GARDO HELING ISMAEL JULIO DOST PAGASA 1 8/26/2011 Tropical Cyclones Tracks in the WNP (1948-2006) CLIMATOLOGICAL TRACKS (Quarterly) TROPICAL CYCLONES ENTERING THE PAR DOST PAGASA KINDS OF HAZARDS ASSOCIATED WITH TROPICAL CYCLONE: Sorsogon, Sorsogon September 2006 DOST DOST PAGASA PAGASA 1)) STRONG WINDS Legaspi City September 2006 Sorsogon, Sorsogon September 2006 2. DOST DOST 4. STORM SURGE Infanta, Quezon Nov. 2004 Infanta, Quezon Nov. 2004 PAGASA (DALUYONG NG BAGYO) PAGASA 3. FLOOD/FLASHFLOOD Cagayan Pampanga Landslides Sheet Flood 2 8/26/2011 DOST DOST Storm Surge Generation Storm Surge Definition PAGASA PAGASA Tropical Cyclone Storm surge is the sudden increase in sea water level associated with the passage of a tropical storm or typhoon. This is due to the push of strong winds on the water surface (wind setup), the piling up of big waves (wave setup), pressure setup (storm central pressure) and astronomical tide moving towards the shore. Source: Wikipedia DOST DOST STORM SURGE PROFILE Storm Surge = Astronomical tide+pressure setup+wind setup+wave setup PAGASA PAGASA Example Inundation coverage Wind flow Flooded area Wave Height Actual Surge height High tide Total surge Topo-bathymetric profile Surge Height Low tide Tide height DATUM Mean lower low water mark (MLLW) Mean Sea Level (MSL) Astronomical tide during occurrences High Tide and Low Tide – Effect on surge height DOST DOST PAGASA PAGASA Storm Surge Occurrences This will happen at landfall or passage of a tropical storm or typhoon in a locality. This Thi might i ht be b ahead, h d during d i or following f ll i the th coming of a strong or high winds of the storm. 3 8/26/2011 1) ANGLE OF ATTACK - PERPENDICULAR ATTACK THE RIGHT-FRONT-QUADRANT (RFQ) 3) COASTAL CONFIGURATION-SHAPE 2) FORWARD SPEED DOST PAGASA The forward speed of the tropical cyclone/hurricane plays a critical role in the overall surge height; FAST MOVING HURRICANE: (15.1mph to 35mph: 24 to 56 KPH) The surface wind stress is increased in the right-front quadrant thus creating a higher storm surge on the outer coast versus the storm surge from a slow moving hurricane hurricane. SLOW MOVING HURRICANE: (0 mph to 15.0mph:0 to 24 KPH) However, a slow moving hurricane may produce the opposite effect inside of a bay, estuary or river system. This is because slow moving hurricanes have more time to pump water into inland water bodies than do fast moving hurricanes. AND: There are also cases where neither rule mentioned above will apply. 3) TYPE OF SLOPE AND SURGE EFFECT DOST TYPE OF SLOPE AND SURGE EFFECT PAGASA 1) Gentle Slope of a continental shelf DOST PAGASA 2) Steep Slope of a continental shelf 4 8/26/2011 Disasters due to Storm Surge DOST DOST PAGASA PAGASA Particularly those living in the coastal areas: • Destroy or carry offshore houses & bancas • Cause of death • Coastal inundation and flooding in the low lying areas • Coastal erosion -caused damage on dikes or seawalls -buildings collapsed Historical Surge Height Recorded in the Philippines DOST DOST PAGASA PAGASA This might be as one or two-storey 10m) depending on the building or more (3m (3m-10m) track, speed and sustained wind of a typhoon, coastal configuration and bathymetry (sea floor profile). The seawall was heavily damaged by surge/swell in Magsaysay, Misamis Oriental January 13, 2009 The school compound at DOST DOST PAGASA PAGASA Caroan, Gonzaga, Cagayan and the more than 2 hectare land area were carried away by storm surge during the occurrence of TY Igme (2004). The height of watermark at the wall was about 2.25 m. The seawall invaded by storm surge during TS Caloy in San Antonio, Northern Samar last May 11-12, 2006. 5 8/26/2011 DOST DOST PAGASA PAGASA The onset of surge inundation as TS Caloy battered the area in Northern Samar. A portion of the barangay in Bgy. Bangan, Botolan was heavily scoured by storm surge during T. Cosme (2008). MONITORING The inundation coverage of storm surge by TS Caloy. DOST DOST PAGASA PAGASA The totally damaged resort in Bgy. Laoag, Cabangan,Zambales by storm surge during T. Ondoy (2009). THE READY PROJECT Hazard Mapping and Assessment for Effective Community-based Disaster Risk Management Storm Surge/Flood Hazard Mapping in the Philippines 6 8/26/2011 27 PROVINCES COVERED 1. 2. 3. 4. 5. 6. 2009 1. Northern Samar 2. Eastern Samar 3. Zambales LUZON 2011 (July 2011-July 2012 Cagayan Isabela Nueva Vizcaya Quirino Agusan del Sur Zamboanga del Sur* 2010-2011 (July 2010-July 2011) 1. Rizal* 2. Catanduanes 3. Benguet* 4. Abra 5. Ilocos Sur* 6. Ilocos Norte 27 PROVINCES TARGET OF READY 2010 (June) 1. Antique 2. Iloilo 2012 (July 2012-July 2013) 1. Zamboanga Sibugay VISAYAS 2008 1. Bohol 2. Aurora 3. Cavite 4. Pampanga 5. Laguna Surigao del Sur Surigao del Norte Leyte Southern Leyte Bohol Iloilo Antique Northern Samar Eastern Samar Pampanga Aurora Zambales Ilocos Sur Ilocos Norte Benguet Abra Isabela Cagayan Cavite Laguna Rizal Nueva Vizcaya Catanduanes Agusan del Sur Agusan del Norte Zamboanga del Sur Zamboanga Sibuguey 2007 1. Southern Leyte 2. Leyte MINDANAO 2006 1. Surigao del Sur 2. Surigao del Norte 3. (Dinagat Island) READY 1 Project – 2 provinces READY 2 Project – 16 provinces covered by Storm Surge * Started the 1:10k for floods & landslide as well as Storm surge for Ilocos Sur, Tsunami EWS in ZDS started DOST DOST PAGASA PAGASA MAPPING METHODOLOGY 1. Storm Surge Model Simulation Input Data: a) Typhoon parameters from historical data: - T. Cosme (May 14-19, 2008) & T. Norming (Aug. 20-Sept. 4, 1982) - Radius of max. max wind, wind sustained wind wind, tracks, tracks and wind direction and speed b) Digitization of Bathymetric data extracted from Nautical chart (map) from BCGS/NAMRIA. DOST DOST PAGASA PAGASA SITE ((Province)) 7 8/26/2011 TYPHOON RUPING (1990) Nov. 13/10AM - landfall DOST a) Courtesy call PDOC SUBIC DOST b) Conduct interviews in the coastal areas on notable typhoon events and surge occurrences. 2) Fieldwork: PAGASA BGY. BANGAN, BOTOLAN IBA BGY. SN. MIGUEL, SN. ANTONIO PMMA, SN. NARCISO CANDELARIA c) Measure the surge height and the inundation coverage as per interview using a level instrument and a GPS. PAGASA PHIL NAVY, SN. NARCISO DOST DOST 3. Analysis, Computation and Storm Surge Hazard Map Development PAGASA PAGASA LEGEND: Inundations of 1m. Surges Inundations of >1m. to 4 m. Surges Inundations of >4 m. to 12 m. Surges 8 8/26/2011 DOST PAGASA PROVINCIAL STORM SURGE HAZARD MAP 1: 120,000 Scale 2) AURORA (LUZON-EAST) 1) ZAMBALES (LUZON-WEST) LEGEND: Inundations of 1m. Surges Inundations of >1m. to 4 m. Surges Inundations of >4 m. to 12 m. Surges 3) NORTHERN SAMAR (VISAYAS) 4) SURIGAO DEL NORTE DOST FLOOD HAZARD MAPS: PAGASA ANTIQUE BOHOL “Disasters can be prevented and mitigated if pp p p appropriate measures are adopted. These can be achieved by proper understanding and preparedness about the hazards and the threats posed by them.” Includes municipalities of San Jose, Sibalom and Hamtic Includes municipalities of Jagna, Guindolman, Anda and Candijay 9 8/26/2011 DOST DOST PAGASA PAGASA WEBSITE http://www.pagasa.dost.gov.ph DIAL-A-WEATHER 433--ULAN (433433 (433-8526) 10