Climate Extremes and Resilient Poverty Reduction: Development Designed with Uncertainty in Mind
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7 the Analysis of Storm Surge in Manila Bay, the Philippines
INTERNATIONAL HYDROGRAPHIC REVIEW MAY 2019 THE ANALYSIS OF STORM SURGE IN MANILA BAY, THE PHILIPPINES By Commander C. S. Luma-ang Hydrography Branch, National Mapping and Resource Information Authority, (Philippines) Abstract In 2013, Typhoon Haiyan produced a storm surge over seven metres in San Pedro Bay in the Philippines that killed approximately 6,300 people. The event created significant public awareness on storm surges and exposed the lack of records and historical research in the Philippines. This study investigated the tidal height records during intense cyclone activities in 2016 and 2017 to provide accurate information about storm surge development in the largest and most populated coastal area in the country – Manila Bay. The results of this investigation indicated that there are consistencies in the characteristics of tropical cyclones that produce larger storm surges. The results also show that actual storm surge heights are generally smaller than predicted height values. Résumé En 2013, le typhon Haiyan a provoqué une onde de tempête de plus de sept mètres dans la Baie de San Pedro aux Philippines, faisant près de 6 300 victimes. Cet événement a provoqué une importante sensibilisation du public envers les ondes de tempête et a mis en évidence le manque d’archives et de recherches historiques aux Philippines. La présente étude a examiné les enregistrements des hauteurs des marées au cours d’activités cycloniques intenses en 2016 et 2017 afin de fournir des informations précises sur le développement d’ondes de tempête dans la zone côtière la plus étendue et la plus peuplée du pays, la Baie de Manille. -
Regional Tropical Cyclone Impact Functions for Globally Consistent Risk Assessments
Research Collection Journal Article Regional tropical cyclone impact functions for globally consistent risk assessments Author(s): Eberenz, Samuel; Lüthi, Samuel; Bresch, David N. Publication Date: 2021-01 Permanent Link: https://doi.org/10.3929/ethz-b-000468253 Originally published in: Natural Hazards and Earth System Sciences 21(1), http://doi.org/10.5194/nhess-21-393-2021 Rights / License: Creative Commons Attribution 4.0 International This page was generated automatically upon download from the ETH Zurich Research Collection. For more information please consult the Terms of use. ETH Library Nat. Hazards Earth Syst. Sci., 21, 393–415, 2021 https://doi.org/10.5194/nhess-21-393-2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Regional tropical cyclone impact functions for globally consistent risk assessments Samuel Eberenz1,2, Samuel Lüthi1,2, and David N. Bresch1,2 1Institute for Environmental Decisions, ETH Zurich, Zurich, 8092, Switzerland 2Federal Office of Meteorology and Climatology MeteoSwiss, Zurich-Airport, 8058, Switzerland Correspondence: Samuel Eberenz ([email protected]) Received: 9 July 2020 – Discussion started: 26 August 2020 Revised: 30 November 2020 – Accepted: 17 December 2020 – Published: 29 January 2021 Abstract. Assessing the adverse impacts caused by tropical regional impact functions are available online as a Python cyclones has become increasingly important as both climate package ready for application in practical contexts like phys- change and human coastal development increase the damage ical risk disclosure and providing more credible information potential. In order to assess tropical cyclone risk, direct eco- for climate adaptation studies. nomic damage is frequently modeled based on hazard inten- sity, asset exposure, and vulnerability, the latter represented by impact functions. -
Significant Data on Major Disasters Worldwide, 1900-Present
DISASTER HISTORY Signi ficant Data on Major Disasters Worldwide, 1900 - Present Prepared for the Office of U.S. Foreign Disaster Assistance Agency for International Developnent Washington, D.C. 20523 Labat-Anderson Incorporated Arlington, Virginia 22201 Under Contract AID/PDC-0000-C-00-8153 INTRODUCTION The OFDA Disaster History provides information on major disasters uhich have occurred around the world since 1900. Informtion is mare complete on events since 1964 - the year the Office of Fore8jn Disaster Assistance was created - and includes details on all disasters to nhich the Office responded with assistance. No records are kept on disasters uhich occurred within the United States and its territories.* All OFDA 'declared' disasters are included - i.e., all those in uhich the Chief of the U.S. Diplmtic Mission in an affected country determined that a disaster exfsted uhich warranted U.S. govermnt response. OFDA is charged with responsibility for coordinating all USG foreign disaster relief. Significant anon-declared' disasters are also included in the History based on the following criteria: o Earthquake and volcano disasters are included if tbe mmber of people killed is at least six, or the total nmber uilled and injured is 25 or more, or at least 1,000 people art affect&, or damage is $1 million or more. o mather disasters except draught (flood, storm, cyclone, typhoon, landslide, heat wave, cold wave, etc.) are included if the drof people killed and injured totals at least 50, or 1,000 or mre are homeless or affected, or damage Is at least S1 mi 1l ion. o Drought disasters are included if the nunber affected is substantial. -
Republic of the Philippines Data Collection Survey on the Incentive Mechanism for Improving Disaster Resiliency of Electric Power Distribution Network Final Report
Republic of the Philippines National Electrification Administration (NEA) Republic of the Philippines Data Collection Survey on the Incentive Mechanism for Improving Disaster Resiliency of Electric Power Distribution Network Final Report October 2015 Japan International Cooperation Agency (JICA) Shikoku Electric Power Co., Inc. (YONDEN) The Japan Economic Research Institute (JERI) 1R JR 15-053 Data Collection Survey on the Incentive Mechanism for Improving Disaster Resiliency of Electric Power Distribution Network: Final Report Contents Chapter 1 Situation of the Energy Sector ............................................................................................ 1 1.1 Economic Conditions in the Philippines .................................................................................... 1 1.2 Current Situation of the Energy Sector in the Philippines.......................................................... 3 1.3 Natural Disaster in the Philippines – Type and Impact .............................................................. 5 Chapter 2 Current Condition of the Power Network in the Philippines ............................................. 8 2.1 Response Organization at Disaster ............................................................................................. 8 2.2 EC Damage and Response Status Information Gathering ........................................................ 14 2.3 ECs’ Capital Investment Plans ................................................................................................. 21 2.4 Financing -
Regional Tropical Cyclone Impact Functions for Globally Consistent Risk Assessments Samuel Eberenz1,2, Samuel Lüthi1,2, David N
https://doi.org/10.5194/nhess-2020-229 Preprint. Discussion started: 26 August 2020 c Author(s) 2020. CC BY 4.0 License. Regional tropical cyclone impact functions for globally consistent risk assessments Samuel Eberenz1,2, Samuel Lüthi1,2, David N. Bresch1,2 5 1 Institute for Environmental Decisions, ETH Zurich, Zurich, 8092, Switzerland 2 Federal Office of Meteorology and Climatology MeteoSwiss, Zurich-Airport, 8058, Switzerland Correspondence to: Samuel Eberenz ([email protected]) Abstract Assessing the adverse impacts caused by tropical cyclones has become increasingly important, as both climate change and 10 human coastal development increase the damage potential. In order to assess tropical cyclone risk, direct economic damage is frequently modelled based on hazard intensity, asset exposure and vulnerability, the latter represented by impact functions. In this study, we show that assessing tropical cyclone risk on a global level with one single impact function calibrated for the USA – which is a typical approach in many recent studies – is problematic, biasing the simulated damages by as much as a factor of 36 in the North West Pacific. Thus, tropical cyclone risk assessments should always consider regional differences 15 in vulnerability, too. This study proposes a calibrated model to adequately assess tropical cyclone risk in different regions by fitting regional impact functions based on reported damage data. Applying regional calibrated impact functions within the risk modelling framework CLIMADA at a resolution of 10 km worldwide, we find global annual average direct damage caused by tropical cyclones to range from 51 up to 121 billion USD (current value of 2014, 1980-2017), with the largest uncertainties in the West Pacific basin, where the calibration results are the least robust. -
Hkmets Bulletin, Volume 6, Number 2, 1996
HONG KONG METEOROLOGICAL SOCIETY u--e In VOLUME 6, UMBER 2, 1996 ISSN: 1024-4468 ISSN 1024-4468 ABOUT THE COVER The cover picture shows a DMSP F12 OLS-VIS image of Typhoon Faye (9504) acquired at 0129 UTC on 22 July, 1995 when the storm was traversing north-northeast through the East China Sea to the west of Okinawa in the Ryukyu Islands. Typhoon Faye was the first of 11 tropical cyclones to reach typhoon strength during 1995 and in this image shows a well-developed circulation and a clearly defined "eye". In this issue a paper by Bill Kyle, the fourth in a series, provides a detailed summary of the 1995 western North Pacific Ocean tropical cyclone season with information and tracks for each of the 35 tropical cyclonic systems that formed in the area during the year. The HONG KONG METEOROLOGICAL SOCIETY BULLETIN is the official organ of the Society, devoted to articles, EDITOR-in-CHIEF EDITORIAL BOARD editorials, news and views, activities and announcements of the Society. BillKyle Johnny CL. Chan Members are encouraged to send any Y.K. Chan articles, media items or information for W:L. Chang publication in the BULLETIN. For Edwin S. T. Lst guidance see the "INFORMATION FOR CONTRIBUTORS" in the inside back cover. SUBSCRIPTION RATES (Two issues per volume) Advertisements for products and/or services of interest to members of the Society are accepted for publication in the BULLETIN. Institutional rate: HK$ 300 per volume For information on formats and rates HK$ 150 per volume please contact the Society secretary at the Individual rate: address opposite. -
Situation Update 1
SITUATION UPDATE 1 1. HIGHLIGHTS a. On 01 November 2020 , Super Typhoon GONI (locally known as ROLLY) made its first landfall in the vicinity of Bato, Catanduanes (Bicol Region) with maximum sustained winds of 225 km/h (equivalent to Category 4 in the Saffir-Simpson Hurricane Wind Scale) and gustiness of up to 280 km/h. It made a total of four (4) landfalls, and resulted in direct wind damage, storm surge hazard, flooding, landslide, lahar, mudflow, and r ock slides along its path. b. On 31 October 2020, the NDRRMC Response Cluster was activated to monitor and facilitate emergency response and humanitarian assistance. To date, the NDRRMC Response Cluster is still in operations. c. Impact to population in the regions of Cagayan Valley, Central Luzon, CALABARZON, MIMAROPA, Bicol, Eastern Visayas, CAR, and NCR are as follows: i. A total of 3 75,074 families or 1 ,459,762 persons were affected. ii. 46,194 families or 181,759 persons are still being served inside and outside evacuation centres. iii. 1,291 evacuation centres are still being used by internally displaced persons. iv. 178 COVID-19 patients and 417 medical/support staff in 11 mega and local quarantine/testing facilities were evacuated. v. There are 2 0 dead , 165 injured, and 6 missing persons. d. Status of C ritical Lifelines: i. 16 road sections and 6 bridges are still not passable . ii. All airports and seaports in the affected areas are now o perational . iii. A total of 128 cities/municipalities are still experiencing power interruptions/outages. iv. A total of 40 cities/municipalities are still experiencing water interruptions/outages. -
Damage Caused by Strong Wind & Wind Loads Standards for Building in Vietnam
Tokyo Polytechnic University- Graduate School of Engineering- Wind Engineering Research Center DAMAGE CAUSE BY STRONG WIND & WIND LOADS STANDARD FOR BUILDING IN VIETNAM Reported by LE TRUONG GIANG PhD Research Scholar WERC-APEC Wind Hazard Mitigation Centre Graduate School of Engineering Tokyo Polytechnic University 1583,Iiyama, Atsugi, Kanagawa, Japan 243-0297 Email [email protected] Phone & Facsimile +81-(0)46-242-9540 Date 18- June 2005 i Tokyo Polytechnic University- Graduate School of Engineering- Wind Engineering Research Center CONTENTS Page FOREWORD 1 PART I: DAMAGE CAUSE BY STRONG WIND IN VIETNAM 2 1. OUT LINES OF VIETNAM 2 1.1. Geographical 1.2. Topography 2 1.3. Climate 2 1.4. The population 3 1.5. The GDP 3 1.6. The GNI per capita 3 2. NATURAL DISASTER IN VIETNAM 3 2.1. The frequency of natural disaster 3 2.2. Damage assessment caused by disasters for the 10 recent years 4 2.3. Damage assessment caused by each kind of disasters 4 3. TYPHOON IN VIETNAM 5 3.1. The frequency of typhoon evens in Vietnam: 5 3.2. The typhoon tracks 6 3.3. Typhoon damages in Vietnam: 7 3.4. Recent biggest typhoon Linda- year 1997 in Vietnam 8 3.5. Some examples of typhoon and strong wind damages 9 CONCLUSION 11 PART II: WIND LOAD STANDARD FOR BUILDING IN VIETNAM 12 1. Summary 12 1.1. Scope of applications 12 1.2. Classification of loads 12 1.3. Concepts of (Design load) and (Basic load) 13 1.4. Combination of Loads 13 2. -
A Chronology of Notable Weather Events by Douglas V. Hoyt
A Chronology of Notable Weather Events by Douglas V. Hoyt Edition of 8/4/2011 243 A. D. An inundation of the sea in Lincolnshire laid under water many thousands of acres (Camden). 353 Flood in Cheshire in which 3000 people died along with thousands of cattle (Hayden). 402 Euxine Sea frozen over for 20 days (Hayden) 500 The Vandals from Poland held Western Africa, the Diocese of Africa, Visigoth (Western Goth) from Scandia held Spain, Ostrogoth (Eastern Goth) from Scandia held Italy, Germanic-Franks from Scandia held Gaul, Burgundians held Rhone river, and Celts, Germanic-Anglo-Saxon held the diocese of England. The massive migration of the Mongols, the Huns, Goth, Slav-Bulgars, and Avars westward is because of adverse weather conditions driving them from their lands . The Germanic-Danes inhabited the Danish Islands, Schonen, and later Jutland. St. Brendan (521-527) in his voyage to the northwest suggests the Celts of Ireland discovered America about this time. The Polynesian reached Hawaii and established agricultural settlements. These people had traveled 2500 miles from Island to Island. It is inconceivable that these peoples didn't reach America in the past 500 years. The Polynesians colonized Hawaii, Easter Island, and Madagascar by 500 A.D. 507 Men from Tsinngan, China report being blown across the Great Sea East to a people who speak a strange language. 508 In England, the rivers were frozen for more than two months (including Thames?). Possible severe winter. Rivers frozen for two months. Years also quoted as 507 or 509. 514 St. Brendan (484-577) of Ireland explored the area discovering the Hebrides, Orkney, Faeroe Islands and Iceland, starting about this time. -
FACT SHEET Municipality of Calabanga, Camarines Sur | Date Last Updated: 10 October 2014
FACT SHEET Municipality of Calabanga, Camarines Sur | Date last updated: 10 October 2014 QUICK FIGURES No. of barangays: 48 Population: 78, 845 Male: 40,556 Female: 38, 260 No. of households: 14,601 Income classification: 1st class 1. Brief historical background Founded as a small barangay by Spanish missionaries in 1578, the Spanish Military Government converted it into a full-fledged municipality on July 15, 1749, the date when it was separated from Quipayo as a political unit. At its founding, Calabanga had vast forests and swamps and an abundance of wildlife such as monkeys, wild chickens and forest lizards. Some say Calabanga derived its name from the Bicol word “Calabangan”, the plural term of “labang” or “litag”, a kind of snare for catching wild animals. Another legend says that Calabanga originated from the word “Calagbangan” meaning the wide, long and straight street spanning from the church through the poblacion, east to west, called locally as “Calabaan” or “Calacbangan”. 2. Climate and Landscape Climate: Calabanga’s climate is characterized by the absence of dry and wet season with a very pronounced rainfall from November to January. o Rainfall occurs throughout the year. However, low rainfall rates are observed during the months of April and May. o Higher rate of rainfall occurs from June to March. Northern Monsoon Winds (Amihan) prevail in the area from September to January while the strong South Monsoon (Habagat) mostly occurs in August. o Typhoons usually occur from September to January. Landscape: Calabanga is situated downstream in the Bicol River basin, where the main stream, Bicol River drains into the San Miguel bay. -
Tropical Cyclones in 1992
ROYAL OBSERVATORY HONG KONG TROPICAL CYCLONES IN 1992 CROWN COPYRIGHT RESERVED Published September 1994 Prepared by Royal Observatory 134A Nathan Road Kowloon Hong Kong Permission to reproduce any part of this publication should be obtained through the Royal Observatory This publication is prepared and disseminated in the interest of promoting the exchange of information. The Government of Hong Kong (including its servants and agents) makes no warranty, statement or representation, expressed or implied, with respect to the accuracy, completeness, or usefulness of the information contained herein, and in so far as permitted by law, shall not have any legal liability or responsibility (including liability for negligence) for any loss, damage or injury (including death) which may result whether directly or indirectly, from the supply or use of such information. This publication is available from: Government Publications Centre General Post Office Building Ground Floor Connaught Place Hong Kong 551.515.2:551.506.1 (512.317) 3 CONTENTS Page FRONTISPIECE: Tracks of tropical cyclones in the western North Pacific and the South China Sea in 1992 FIGURES 4 TABLES 5 HONG KONG'S TROPICAL CYCLONE WARNING SIGNALS 6 1. INTRODUCTION 7 2. TROPICAL CYCLONE OVERVIEW FOR 1992 11 3. REPORTS ON TROPICAL CYCLONES AFFECTING HONG KONG IN 1992 19 (a) Typhoon Chuck (9204): 24-30 June 20 (b) Typhoon Eli (9205): 9-14 July 25 (c) Tropical Storm Faye (9206): 17-18 July 29 (d) Severe Tropical Storm Gary (9207): 19-23 July 36 (e) Tropical Storm Mark (9212): 16-19 August 42 4. TROPICAL CYCLONE STATISTICS AND TABLES 47 5. -
The International Hydrographic Review, 19 Pg
INTERNATIONAL HYDROGRAPHIC REVIEW MAY 2019 THE INTERNATIONAL HYDROGRAPHIC REVIEW INTERNATIONAL HYDROGRAPHIC ORGANIZATION MONACO Publication P-1 No. 21 INTERNATIONAL HYDROGRAPHIC REVIEW MAY 2019 © Copyright International Hydrographic Organization [2019] This work is copyright. Apart from any use permitted in accordance with the Berne Convention for the Protection of Literary and Artistic Works (1886), and except in the circumstances described below, no part may be translated, reproduced by any process, adapted, communicated or commercially exploited without prior written permission from the Secretariat of the International Hydrographic Organization (IHO). Copyright in some of the material in this publication may be owned by another party and permission for the translation and/or reproduction of that material must be obtained from the owner. This document or partial material from this document may be translated, reproduced or distributed for general information, on no more than a cost recovery basis. Copies may not be sold or distributed for profit or gain without prior written agreement of the IHO Secretariat and any other copyright holders. In the event that this document or partial material from this document is reproduced, translated or distributed under the terms described above, the following statements are to be included: “Material from IHO publication [reference to extract: Title, Edition] is reproduced with the permission of the IHO Secretariat (Permission No ……./…) acting for the International Hydrographic Organization (IHO), which does not accept responsibility for the correctness of the material as reproduced: in case of doubt, the IHO’s au- thentic text shall prevail. The incorporation of material sourced from IHO shall not be construed as constituting an endorsement by IHO of this product.” “This [document/publication] is a translation of IHO [document/publication] [name].