Special Feature the Typhoon Haiyan Response
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Climate Disasters in the Philippines: a Case Study of the Immediate Causes and Root Drivers From
Zhzh ENVIRONMENT & NATURAL RESOURCES PROGRAM Climate Disasters in the Philippines: A Case Study of Immediate Causes and Root Drivers from Cagayan de Oro, Mindanao and Tropical Storm Sendong/Washi Benjamin Franta Hilly Ann Roa-Quiaoit Dexter Lo Gemma Narisma REPORT NOVEMBER 2016 Environment & Natural Resources Program Belfer Center for Science and International Affairs Harvard Kennedy School 79 JFK Street Cambridge, MA 02138 www.belfercenter.org/ENRP The authors of this report invites use of this information for educational purposes, requiring only that the reproduced material clearly cite the full source: Franta, Benjamin, et al, “Climate disasters in the Philippines: A case study of immediate causes and root drivers from Cagayan de Oro, Mindanao and Tropical Storm Sendong/Washi.” Belfer Center for Science and International Affairs, Cambridge, Mass: Harvard University, November 2016. Statements and views expressed in this report are solely those of the authors and do not imply endorsement by Harvard University, the Harvard Kennedy School, or the Belfer Center for Science and International Affairs. Design & Layout by Andrew Facini Cover photo: A destroyed church in Samar, Philippines, in the months following Typhoon Yolanda/ Haiyan. (Benjamin Franta) Copyright 2016, President and Fellows of Harvard College Printed in the United States of America ENVIRONMENT & NATURAL RESOURCES PROGRAM Climate Disasters in the Philippines: A Case Study of Immediate Causes and Root Drivers from Cagayan de Oro, Mindanao and Tropical Storm Sendong/Washi Benjamin Franta Hilly Ann Roa-Quiaoit Dexter Lo Gemma Narisma REPORT NOVEMBER 2016 The Environment and Natural Resources Program (ENRP) The Environment and Natural Resources Program at the Belfer Center for Science and International Affairs is at the center of the Harvard Kennedy School’s research and outreach on public policy that affects global environment quality and natural resource management. -
SBC) the Jesuit Protocol for Disaster Risk Reduction and Management
Jesuit Conference Asia Pacific-Reconciliation with Creation Scholastics and Brothers Circle {SBC) The Jesuit Protocol for Disaster Risk Reduction and Management ESSC 9ENVIRONMENTAL SCIENCE FOR SOCIAL CHANGE, INC CONTENTS I. BACKGROUND AND CONTEXT I II II. THE JCAP DRR PROTOCOL I II II. ELEMENTS OF DISASTER RISK I II IV. SITE VISIT DESCRIPTIONS I II V. PROGRAM SCHEDULE I II VI. LIST OF PARTICIPANTS I II LISTOF MAPS MAP 1 Sites to Be Visited TY Yolanda Affected Areas II MAP 2 Riverine Flood Risk in Batug, Du lag, Leyte I II MAP 3 Hazards Daguitan Watershed I II MAP 4 Yolanda lnfographic I II MAP 5 Debris Flood in Anonang,Burauen, Leyte I II MAP 6 Flood Hazard, Brgy. Capiz & Dapdap. Alangalang. Leyte I II I. BACKGROUND AND CONTEXT The Scholastics and Brothers Circle (SBC) under the Jesuit Conference Asia Pacific (JCAP) gathers annually and for 2015, disaster risk reduction (ORR) and management was selected as its work theme. In recent years, many countries and communities in Asia Pacific suffered immensely from the impacts of natural hazards-turned-disasters as the usual response systems proved to be ineffective for the scale and intensity of these events. The Asian tsunami in 2004, Cyclone Nargis and the flooding in Myanmar in 2008, Typhoon Ondoy (Ketsana) that triggered floods in the Philippines in 2009, painfully reflect the increasing frequency of extreme weather events in the region. In 2011, an earthquake struck New Zealand, Australia and Bangkok were flooded, and Japan was hit by an earthquake and tsunami that left the country at the brink of a nuclear disaster. -
How HERO Did It
How HERO did it. Now it can be told. HERO is the Ham Emergency Radio Operations formally launched upon the unveiling of the logo design contest winner during the 82nd Anniversary of the Philippine Amateur Radio Association (PARA) Inc. – the Philippine national association for the amateur radio service. Preparations HERO was activated on December 4, 2015 when it became imminent that typhoon Hagupit (local name Ruby) will make landfall somewhere in the Visayas region. It was to be a live test for HERO with Super Typhoon Yolanda in mind. Upon its activation, a lot of traffic was devoted to trying to muster hams on the 40-meter band (the PARA center of frequency on 40 meter is at 7.095 MHz). Members were advised to start building up on their redundant power supplies such as generators, solar panels, batteries and other imaginable means available as power sources. Owing to the large swathe of typhoon Ruby, it was expected to be almost like Haiyan/Yolanda. There were striking similarities. Initially, Districts 4, 5 and 9 as well as Districts 6, 7 and 8 were alerted. Both Ruby and Yolanda came from the lower quadrant of the typhoon belt. Both were packing winds more than 200 kph near the center. Both had huge footprint or diameter, with Ruby estimated to be around 600 kilometers. Both were expected to generate 3 to 6 meters storm surges and were definitely considered dangerous to lives and properties. Government was not leaving anything to chance and there were plans to forcibly evacuate people along the typhoon track especially those in the coastal area. -
The Impact of Tropical Cyclone Hayan in the Philippines: Contribution of Spatial Planning to Enhance Adaptation in the City of Tacloban
UNIVERSIDADE DE LISBOA FACULDADE DE CIÊNCIAS Faculdade de Ciências Faculdade de Ciências Sociais e Humanas Faculdade de Letras Faculdade de Ciências e Tecnologia Instituto de Ciências Sociais Instituto Superior de Agronomia Instituto Superior Técnico The impact of tropical cyclone Hayan in the Philippines: Contribution of spatial planning to enhance adaptation in the city of Tacloban Doutoramento em Alterações Climáticas e Políticas de Desenvolvimento Sustentável Especialidade em Ciências do Ambiente Carlos Tito Santos Tese orientada por: Professor Doutor Filipe Duarte Santos Professor Doutor João Ferrão Documento especialmente elaborado para a obtenção do grau de Doutor 2018 UNIVERSIDADE DE LISBOA FACULDADE DE CIÊNCIAS Faculdade de Ciências Faculdade de Ciências Sociais e Humanas Faculdade de Letras Faculdade de Ciências e Tecnologia Instituto de Ciências Sociais Instituto Superior de Agronomia Instituto Superior Técnico The impact of tropical cyclone Haiyan in the Philippines: Contribution of spatial planning to enhance adaptation in the city of Tacloban Doutoramento em Alterações Climáticas e Políticas de Desenvolvimento Sustentável Especialidade em Ciências do Ambiente Carlos Tito Santos Júri: Presidente: Doutor Rui Manuel dos Santos Malhó; Professor Catedrático Faculdade de Ciências da Universidade de Lisboa Vogais: Doutor Carlos Daniel Borges Coelho; Professor Auxiliar Departamento de Engenharia Civil da Universidade de Aveiro Doutor Vítor Manuel Marques Campos; Investigador Auxiliar Laboratório Nacional de Engenharia Civil(LNEC) -
Typhoon Haiyan Action Plan November 2013
Philippines: Typhoon Haiyan Action Plan November 2013 Prepared by the Humanitarian Country Team 100% 92 million total population of the Philippines (as of 2010) 54% 50 million total population of the nine regions hit by Typhoon Haiyan 13% 11.3 million people affected in these nine regions OVERVIEW (as of 12 November) (12 November 2013 OCHA) SITUATION On the morning of 8 November, category 5 Typhoon Haiyan (locally known as Yolanda ) made a direct hit on the Philippines, a densely populated country of 92 million people, devastating areas in 36 provinces. Haiyan is possibly the most powerful storm ever recorded . The typhoon first ma de landfall at 673,000 Guiuan, Eastern Samar province, with wind speeds of 235 km/h and gusts of 275 km/h. Rain fell at rates of up to 30 mm per hour and massive storm displaced people surges up to six metres high hit Leyte and Samar islands. Many cities and (as of 12 November) towns experienced widespread destruction , with as much as 90 per cent of housing destroyed in some areas . Roads are blocked, and airports and seaports impaired; heavy ships have been thrown inland. Water supply and power are cut; much of the food stocks and other goods are d estroyed; many health facilities not functioning and medical supplies quickly being exhausted. Affected area: Regions VIII (Eastern Visayas), VI (Western Visayas) and Total funding requirements VII (Central Visayas) are hardest hit, according to current information. Regions IV-A (CALABARZON), IV-B ( MIMAROPA ), V (Bicol), X $301 million (Northern Mindanao), XI (Davao) and XIII (Caraga) were also affected. -
A Summary of Palau's Typhoon History 1945-2013
A Summary of Palau’s Typhoon History 1945-2013 Coral Reef Research Foundation, Palau Dec, 2014 © Coral Reef Research Foundation 2014 Suggested citation: Coral Reef Research Foundation, 2014. A Summary of Palau’s Typhoon History. Technical Report, 17pp. www.coralreefpalau.org Additions and suggestions welcome. Please email: [email protected] 2 Summary: Since 1945 Palau has had 68 recorded typhoons, tropical storms or tropical depressions come within 200 nmi of its islands or reefs. At their nearest point to Palau, 20 of these were typhoon strength with winds ≥64kts, or an average of 1 typhoon every 3 years. November and December had the highest number of significant storms; July had none over 40 kts and August had no recorded storms. Data Compilation: Storms within 200 nmi (nautical miles) of Palau were identified from the Digital Typhoon, National Institute of Informatics, Japan web site (http://agora.ex.nii.ac.jp/digital- typhoon/reference/besttrack.html.en). The storm tracks and intensities were then obtained from the Joint Typhoon Warning Center (JTWC) (https://metoc.ndbc.noaa.gov/en/JTWC/). Three storm categories were used following the JTWC: Tropical Depression, winds ≤ 33 kts; Tropical Storm, winds 34-63 kts; Typhoon ≥64kts. All track data was from the JTWC archives. Tracks were plotted on Google Earth and the nearest distance to land or reef, and bearing from Palau, were measured; maximum sustained wind speed in knots (nautical miles/hr) at that point was recorded. Typhoon names were taken from the Digital Typhoon site, but typhoon numbers for the same typhoon were from the JTWC archives. -
9065C70cfd3177958525777b
The FY 1989 Annual Report of the Agency for international DevelaprnentiOHiee of U.S. Foreign Disaster Assistance was researched. written, and produced by Cynthia Davis, Franca Brilliant, Mario Carnilien, Faye Henderson, Waveriy Jackson, Dennis J. King, Wesley Mossburg, Joseph OYConnor.Kimberly S.C. Vasconez. and Beverly Youmans of tabai Anderson Incorparated. Arlingtot?. Virginia, under contract ntrmber QDC-0800-C-00-8753-00, Office 0%US Agency ior Foreign Disaster Enternatiorr~ai Assistance Development Message from the Director ............................................................................................................................. 6 Summary of U.S. Foreign Disaster Assistance .............................................................................................. 8 Retrospective Look at OFDA's 25 Years of Operations ................................................................................. 10 OFDA Emergency Response ......................................................................................................................... 15 Prior-Year (FY 1987 and 1988) and Non-Declared Disasters FV 1989 DISASTERS LUROPE Ethiopia Epidemic ................................. ............. 83 Soviet Union Accident ......................................... 20 Gabon Floods .................................... ... .................84 Soviet Union Earthquake .......................................24 Ghana Floods ....................................................... 85 Guinea Bissau Fire ............................................. -
Briefing Note on Typhoon Goni
Briefing note 12 November 2020 PHILIPPINES KEY FIGURES Typhoon Goni CRISIS IMPACT OVERVIEW 1,5 million PEOPLE AFFECTED BY •On the morning of 1 November 2020, Typhoon Goni (known locally as Rolly) made landfall in Bicol Region and hit the town of Tiwi in Albay province, causing TYPHOON GONI rivers to overflow and flood much of the region. The typhoon – considered the world’s strongest typhoon so far this year – had maximum sustained winds of 225 km/h and gustiness of up to 280 km/h, moving at 25 km/h (ACT Alliance 02/11/2020). • At least 11 towns are reported to be cut off in Bato, Catanduanes province, as roads linking the province’s towns remain impassable. At least 137,000 houses were destroyed or damaged – including more than 300 houses buried under rock in Guinobatan, Albay province, because of a landslide following 128,000 heavy rains caused by the typhoon (OCHA 09/11/2020; ECHO 10/11/2020; OCHA 04/11/2020; South China Morning Post 04/11/2020). Many families will remain REMAIN DISPLACED BY in long-term displacement (UN News 06/11/2020; Map Action 08/11/2020). TYPHOON GONI • As of 7 November, approximately 375,074 families or 1,459,762 people had been affected in the regions of Cagayan Valley, Central Luzon, Calabarzon, Mimaropa, Bicol, Eastern Visayas, CAR, and NCR. Of these, 178,556 families or 686,400 people are in Bicol Region (AHA Centre 07/11/2020). • As of 07 November, there were 20 dead, 165 injured, and six missing people in the regions of Calabarzon, Mimaropa, and Bicol, while at least 11 people were 180,000 reported killed in Catanduanes and Albay provinces (AHA Centre 07/11/2020; UN News 03/11/2020). -
Typhoon Haiyan 2013 Evacuation Preparations and Awareness
International Journal of Sustainable Future for Human Security DISASTER MITIGATION J-SustaiN Vol. 3, No. 1 (2015) 37-45 http://www.j-sustain.com MITIGATIONMITIGATION Generally speaking, tropical cyclones can bring about storm Typhoon Haiyan 2013 surges that can cause great damage to unprepared developing countries, though even developed countries like the United States Evacuation Preparations and and Japan can also be greatly affected by these events [2] [3]. Awareness Typhoon Haiyan, in 2013, could be considered another defining event in raising awareness about storm surges, not only in the a* b Philippines but within the entire world. Miguel Esteban , Ven Paolo Valenzuela , Nam Category 5 Typhoon Haiyan (known as Yolanda in the Yi Yunc, Takahito Mikamic, Tomoya Philippines) made landfall in the Philippines on the 8th November Shibayamac, Ryo Matsumarud, Hiroshi Takagie, 2013 at almost the peak of its power, devastating the islands of Leyte f g and Samar and causing large damage to other areas in the Visayas[4, Nguyen Danh Thao , Mario De Leon , 5]. The maximum sustained wind speeds were around 160 knots, Takahiro Oyamac, Ryota Nakamurac. the largest in the recorded history of the Western North Pacific. The strong winds, together with the typhoon’s extremely low aGraduation Program in Sustainability Science, Global Leadership central pressure (895hPa), generated a huge storm surge which Initiative (GPSS-GLI), The University of Tokyo, Tokyo, Japan engulfed several coastal towns and caused particularly large b Centre for disaster preparedness, Manila, Philippines damage to Tacloban city. The typhoon’s strong winds caused c Department of Civil & Environmental Engineering, Waseda devastating damage to the vegetation, leaving behind bare University, Tokyo, Japan mountains and flattened fields only dotted with the rare dead tree d Department of Regional Development Studies, Toyo University eTokyo Institute of Technolgy, Tokyo, Japan trunks that were left standing. -
Responding to Typhoon Haiyan in the Philippines
Volume 6, Supplement 1 2015, Pages 1–101 Responding to Typhoon p-ISSN: 2094-7321 e-ISSN: 2094-7313 Haiyan in the Philippines EEditorialditorial UUsese ofof tthehe WWHOHO PPackageackage ooff EEssentialssential RRespondingesponding ttoo TTyphoonyphoon HHaiyanaiyan NNoncommunicableoncommunicable DDiseaseisease InterventionsInterventions iinn tthehe PPhilippineshilippines 1 aafterfter TyphoonTyphoon HHaiyanaiyan 1188 MMcPhersoncPherson MM,, CCounahanounahan MM,, HHallall JJLL MMartinezartinez RRE,E, QQuintanuintan RR,, GGoo JJJ,J, VVillonesillones MMS,S, MMarquezarquez MMAA PPerspectiveerspective SSurveillanceurveillance fforor aandnd iissuesssues rrelatingelating ttoo IIss tthehe rresponseesponse oover?ver? TThehe ttransitionransition ffromrom nnoncommunicableoncommunicable ddiseasesiseases ppost-Haiyanost-Haiyan rresponseesponse ttoo rrecoveryecovery inin tthehe hhealthealth ssectorector iinn RRegionegion 8 2211 ppost-Typhoonost-Typhoon HHaiyanaiyan 5 MMartinezartinez RRE,E, QQuintanauintana RR,, GGoo JJJ,J, MMarquezarquez MMA,A, KKimim JJK,K, GGocotanoocotano AA,, GGeroyeroy LLS,S, AAlcidolcido MMR,R, DDorotanorotan MMM,M, BBalboaalboa GG,, VVillonesillones MMS,S, SSalazaralazar MMAA HHallall JJLL BBriefrief RReportseports MManaginganaging ssurgeurge sstafftaff aandnd rresourcesesources aatt tthehe CCanan yyouou hhelpelp mmee wwriterite mmyy sstory?tory? TThehe WWHOHO RRepresentativeepresentative OfOffi ccee iinn tthehe PPhilippineshilippines iinstitutionalnstitutional aafffi lliationiation ooff aauthorsuthors ooff aafterfter TyphoonTyphoon -
Third Assessment on Impacts of Climate Change on Tropical Cyclones in the Typhoon Committee Region E Part I: Observed Changes, Detection and Attribution
Available online at www.sciencedirect.com ScienceDirect Tropical Cyclone Research and Review 9 (2020) 1e22 www.keaipublishing.com/tcrr Third assessment on impacts of climate change on tropical cyclones in the Typhoon Committee Region e Part I: Observed changes, detection and attribution Tsz-Cheung Lee a,*, Thomas R. Knutson b, Toshiyuki Nakaegawa c, Ming Ying d, Eun Jeong Cha e a Hong Kong Observatory, Hong Kong, China b Geophysical Fluid Dynamics Laboratory/NOAA, Princeton, NJ, USA c Meteorological Research Institute/Japan Meteorological Agency, Tsukuba, Japan d Shanghai Typhoon Institute, China Meteorological Administration, Shanghai, China e National Typhoon Center, Korea Meteorological Administration, Jeju, Republic of Korea Available online 20 March 2020 Abstract Published findings on climate change impacts on tropical cyclones (TCs) in the ESCAP/WMO Typhoon Committee Region are assessed. We focus on observed TC changes in the western North Pacific (WNP) basin, including frequency, intensity, precipitation, track pattern, and storm surge. Results from an updated survey of impacts of past TC activity on various Members of the Typhoon Committee are also reported. Existing TC datasets continue to show substantial interdecadal variations in basin-wide TC frequency and intensity in the WNP. There has been encouraging progress in improving the consensus between different datasets concerning intensity trends. A statistically significant northwest- ward shift in WNP TC tracks since the 1980s has been documented. There is low-to-medium confidence in a detectable poleward shift since the 1940s in the average latitude where TCs reach their peak intensity in the WNP. A worsening of storm inundation levels is believed to be occurring due to sea level rise-due in part to anthropogenic influence-assuming all other factors equal. -
Maximum Wind Radius Estimated by the 50 Kt Radius: Improvement of Storm Surge Forecasting Over the Western North Pacific
Nat. Hazards Earth Syst. Sci., 16, 705–717, 2016 www.nat-hazards-earth-syst-sci.net/16/705/2016/ doi:10.5194/nhess-16-705-2016 © Author(s) 2016. CC Attribution 3.0 License. Maximum wind radius estimated by the 50 kt radius: improvement of storm surge forecasting over the western North Pacific Hiroshi Takagi and Wenjie Wu Tokyo Institute of Technology, Graduate School of Science and Engineering, 2-12-1 Ookayama, Meguro-ku, Tokyo 152-8550, Japan Correspondence to: Hiroshi Takagi ([email protected]) Received: 8 September 2015 – Published in Nat. Hazards Earth Syst. Sci. Discuss.: 27 October 2015 Revised: 18 February 2016 – Accepted: 24 February 2016 – Published: 11 March 2016 Abstract. Even though the maximum wind radius (Rmax) countries such as Japan, China, Taiwan, the Philippines, and is an important parameter in determining the intensity and Vietnam. size of tropical cyclones, it has been overlooked in previous storm surge studies. This study reviews the existing estima- tion methods for Rmax based on central pressure or maximum wind speed. These over- or underestimate Rmax because of 1 Introduction substantial variations in the data, although an average radius can be estimated with moderate accuracy. As an alternative, The maximum wind radius (Rmax) is one of the predominant we propose an Rmax estimation method based on the radius of parameters for the estimation of storm surges and is defined the 50 kt wind (R50). Data obtained by a meteorological sta- as the distance from the storm center to the region of maxi- tion network in the Japanese archipelago during the passage mum wind speed.