Typhoon Haiyan Action Plan November 2013
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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. -
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) -
WMO Statement on the Status of the Global Climate in 2011
WMO statement on the status of the global climate in 2011 WMO-No. 1085 WMO-No. 1085 © World Meteorological Organization, 2012 The right of publication in print, electronic and any other form and in any language is reserved by WMO. Short extracts from WMO publications may be reproduced without authorization, provided that the complete source is clearly indicated. Editorial correspondence and requests to publish, reproduce or translate this publication in part or in whole should be addressed to: Chair, Publications Board World Meteorological Organization (WMO) 7 bis, avenue de la Paix Tel.: +41 (0) 22 730 84 03 P.O. Box 2300 Fax: +41 (0) 22 730 80 40 CH-1211 Geneva 2, Switzerland E-mail: [email protected] ISBN 978-92-63-11085-5 WMO in collaboration with Members issues since 1993 annual statements on the status of the global climate. This publication was issued in collaboration with the Hadley Centre of the UK Meteorological Office, United Kingdom of Great Britain and Northern Ireland; the Climatic Research Unit (CRU), University of East Anglia, United Kingdom; the Climate Prediction Center (CPC), the National Climatic Data Center (NCDC), the National Environmental Satellite, Data, and Information Service (NESDIS), the National Hurricane Center (NHC) and the National Weather Service (NWS) of the National Oceanic and Atmospheric Administration (NOAA), United States of America; the Goddard Institute for Space Studies (GISS) operated by the National Aeronautics and Space Administration (NASA), United States; the National Snow and Ice Data Center (NSIDC), United States; the European Centre for Medium-Range Weather Forecasts (ECMWF), United Kingdom; the Global Precipitation Climatology Centre (GPCC), Germany; and the Dartmouth Flood Observatory, United States. -
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. -
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. -
Tropical Storm Tembin
Emergency Plan of Action (EPoA) Philippines: Tropical Storm Tembin DREF n° MDRPH026 Glide n° TC-2017-000180-PHL; TC-2017-000182-PHL Date of issue: 22 December 2017 Categorization of crisis1: Yellow Operations manager: Point of contact: Patrick Elliott Atty. Oscar Palabyab Operations Manager Secretary General IFRC Philippine Country Office Philippine Red Cross Operation start date: 22 December 2017 Operation timeframe: 1 month, 22 January 2018 Operation budget: CHF 31,764 DREF allocation: CHF 31,764 N° of people affected: To be determined after landfall N° of people to be assisted: 5,000 Red Cross Red Crescent Movement partners actively involved in the operation: PRC is working with the International Federation of Red Cross and Red Crescent Societies (IFRC) in this operation. There are 12 Partner National Societies with presence in the Philippines. PRC and IFRC are also coordinating with International Committee of the Red Cross on this operation. Other partner organizations actively involved in the operation: Government ministries and agencies including the National Disaster Risk Reduction and Management Council (NDRRMC), Department of Social Welfare and Development (DSWD), the Philippine Armed Forces, the Philippine National Police Force and Local Government Units are providing assistance to affected households. PRC have a seat on the NDRRMC. A. SITUATION ANALYSIS Description of the disaster There have been two significant weather systems to enter the Philippines Area of Responsibility (PAR) since 12 December 2017. Tropical Storm Kai-tak: On 12 December 2017, a low-pressure area (LPA) within the PAR developed into a Tropical Depression which was named Kai-tak (locally Urduja). The tropical depression moved north northwest, and by 14 December was reclassified as a Tropical Storm. -
The Year That Shook the Rich: a Review of Natural Disasters in 2011
THE YEAR THAT SHOOK THE RICH: A REVIEW OF NATURAL DISASTERS IN 2011 The Brookings Institution – London School of Economics Project on Internal Displacement March 2012 Design: [email protected] Cover photo: © Thinkstock.com Back cover photos: left / © Awcnz62 | Dreamstime.com; right / © IOM 2011 - MPK0622 (Photo: Chris Lom) THE YEAR THAT SHOOK THE RICH: A REVIEW OF NATURAL DISASTERS IN 2011 By Elizabeth Ferris and Daniel Petz March 2012 PUBLISHED BY: THE BROOKINGS INSTITUTION – LONDON SCHOOL OF ECONOMICS PROJECT ON INTERNAL DISPLACEMENT Bangkok, Thailand — Severe monsoon floods, starting in late July 2011, affected millions of people. A truck with passengers aboard drives through a heavily flooded street. Photo: UN/Mark Garten TABLE OF CONTENTS Acronyms ................................................................................................................................. vi Foreword ................................................................................................................................. ix Executive Summary ................................................................................................................. xi Introduction .............................................................................................................................. xv Chapter 1 The Year that Shook the Rich ...................................................... 1 Section 1 Disasters in the “Rich” World, Some Numbers ............................................ 5 Section 2 Japan: The Most Expensive Disaster -
Disaster Response Shelter Catalogue
Disaster Response Shelter Catalogue Disaster Response Shelter Catalogue Disaster Response Shelter Catalogue Copyright 2012 Habitat for Humanity International Front cover: Acknowledgements Sondy-Jonata Orientus’ family home was destroyed in the 2010 earthquake We are extremely grateful to all the members of the Habitat for Humanity that devastated Haiti, and they were forced to live in a makeshift tent made of network who made this publication possible. Special thanks to the global tarpaulins. Habitat for Humanity completed the family’s new home in 2011. © Habitat Disaster Response community of practice members. Habitat for Humanity International/Ezra Millstein Compilation coordinated by Mario C. Flores Back cover: Editorial support by Phil Kloer Top: Earthquake destruction in Port-au-Prince, Haiti. © Habitat for Humanity International Steffan Hacker Contributions submitted by Giovanni Taylor-Peace, Mike Meaney, Ana Cristina Middle: Reconstruction in Cagayan de Oro, Philippines, after tropical storm Washi. Pérez, Pete North, Kristin Wright, Erwin Garzona, Nicolas Biswas, Jaime Mok, © Habitat for Humanity Internationa/Leonilo Escalada Scarlett Lizana Fernández, Irvin Adonis, Jessica Houghton, V. Samuel Peter, Bottom: A tsunami-affected family in Indonesia in front of their nearly completed Justin Jebakumar, Joseph Mathai, Andreas Hapsoro, Rudi Nadapdap, Rashmi house. © Habitat for Humanity International/Kim McDonald Manandhar, Amrit Bahadur B.K., Leonilo (Tots) Escalada, David (Dabs) Liban, Mihai Grigorean, Edward Fernando, Behruz Dadovoeb, Kittipich Musica, Additional photo credits: Ezra Millstein, Steffan Hacker, Jaime Mok, Mike Meaney, Nguyen Thi Yen. Mario Flores, Kevin Kehus, Maria Chomyszak, Leonilo (Tots) Escalada, Mikel Flamm, Irvin Adonis, V. Samuel Peter, Sara E. Coppler, Tom Rogers, Joseph Mathai, Additional thanks to Heron Holloway and James Samuel for reviewing part of Justin Jebakumar, Behruz Dadovoeb, Gerardo Soto, Mihai Gregorian, Edward the materials. -
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.