Introduction and Application of a New Comprehensive Assessment Index for Damage Caused by Tropical Cyclones
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												  Enhancing Psychological SupportAppeal No. MDRCN001 CHINA: FLOODS 2006 17 October 2007 The Federation’s mission is to improve the lives of vulnerable people by mobilizing the power of humanity. It is the world’s largest humanitarian organization and its millions of volunteers are active in over 185 countries. In Brief Final Report; Period covered: 2 August 2006 - 31 July 2007; Final appeal coverage: 26%. <Click here to link directly to the attached Final Financial Report>. Appeal history: • This appeal was launched on 02 August 2006 seeking CHF 5,950,200 (USD 4,825,791 or EUR 3,782,708) for 12 months to assist 240,000 beneficiaries. • Disaster Relief Emergency Funds (DREF) allocated: CHF 213,000 Related Emergency or Annual Appeals: 2006-2007 China Appeal MAACN001 2006-2007 East Asia Appeal MAA54001 Operational Summary: Every year, China is crippled by various natural disasters. In 2006, natural disasters were responsible for the deaths of at least 3,186 people. Over 13.8 million people were evacuated and relocated, with 1.93 million houses completely destroyed. According to latest statistics provided by the ministry of civil affairs, flooding in 2006 had caused a direct economic loss of USD 24 billion (CHF 30 billion). The Red Cross Society of China first responded to meet the emergency needs in Hunan province arising from typhoon Bilis. The Disaster Relief Emergency Fund allocated CHF 213,000 to initial relief distributions. A flood affected village in Hunan province. RCSC/International Federation Through the Federation’s China Floods Emergency Appeal (MDRCN001) launched on 2 August 2006, CHF 1.57 million was raised to provide additional support to beneficiaries through the national society.
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												  P1.24 a Typhoon Loss Estimation Model for ChinaP1.24 A TYPHOON LOSS ESTIMATION MODEL FOR CHINA Peter J. Sousounis*, H. He, M. L. Healy, V. K. Jain, G. Ljung, Y. Qu, and B. Shen-Tu AIR Worldwide Corporation, Boston, MA 1. INTRODUCTION the two. Because of its wind intensity (135 mph maximum sustained winds), it has been Nowhere 1 else in the world do tropical compared to Hurricane Katrina 2005. But Saomai cyclones (TCs) develop more frequently than in was short lived, and although it made landfall as the Northwest Pacific Basin. Nearly thirty TCs are a strong Category 4 storm and generated heavy spawned each year, 20 of which reach hurricane precipitation, it weakened quickly. Still, economic or typhoon status (cf. Fig. 1). Five of these reach losses were ~12 B RMB (~1.5 B USD). In super typhoon status, with windspeeds over 130 contrast, Bilis, which made landfall a month kts. In contrast, the North Atlantic typically earlier just south of where Saomai hit, was generates only ten TCs, seven of which reach actually only tropical storm strength at landfall hurricane status. with max sustained winds of 70 mph. Bilis weakened further still upon landfall but turned Additionally, there is no other country in the southwest and traveled slowly over a period of world where TCs strike with more frequency than five days across Hunan, Guangdong, Guangxi in China. Nearly ten landfalling TCs occur in a and Yunnan Provinces. It generated copious typical year, with one to two additional by-passing amounts of precipitation, with large areas storms coming close enough to the coast to receiving more than 300 mm.
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												  Observational Analysis of Heavy Rainfall Mechanisms Associated with Severe Tropical Storm Bilis (2006) After Its LandfallJUNE 2009 G A O E T A L . 1881 Observational Analysis of Heavy Rainfall Mechanisms Associated with Severe Tropical Storm Bilis (2006) after Its Landfall SHUANZHU GAO China National Meteorological Center, Beijing, China ZHIYONG MENG Department of Atmospheric Sciences, School of Physics, Peking University, Beijing, China FUQING ZHANG Department of Meteorology, The Pennsylvania State University, University Park, Pennsylvania LANCE F. BOSART Department of Atmospheric Sciences, University at Albany, State University of New York, Albany, New York (Manuscript received 5 June 2008, in final form 8 December 2008) ABSTRACT This observational study attempts to determine factors responsible for the distribution of precipitation over large areas of southern China induced by Bilis, a western North Pacific Ocean severe tropical storm that made landfall on the southeastern coast of mainland China on 14 July 2006 with a remnant circulation that persisted over land until after 17 July 2006. The heavy rainfalls associated with Bilis during and after its landfall can be divided into three stages. The first stage of the rainfall, which occurred in Fujian and Zhejiang Provinces, could be directly induced by the inner-core storm circulation during its landfall. The third stage of rainfall, which occurred along the coastal areas of Guangdong and Fujian Provinces, likely resulted from the interaction between Bilis and the South China Sea monsoon enhanced by topographical lifting along the coast. The second stage of the rainfall, which appeared inland around the border regions between Jiangxi, Hunan, and Guangdong Provinces, caused the most catastrophic flooding and is the primary focus of the current study. It is found that during the second stage of the rainfall all three ingredients of deep moist convection (moisture, instability, and lifting) are in place.
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												  Observational Analysis of Tropical Cyclone Formation Associated with Monsoon GyresAPRIL 2013 W U E T A L . 1023 Observational Analysis of Tropical Cyclone Formation Associated with Monsoon Gyres LIGUANG WU,HUIJUN ZONG, AND JIA LIANG Key Laboratory of Meteorological Disaster of Ministry of Education, Nanjing University of Information Science and Technology, Nanjing, and State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing, China (Manuscript received 6 April 2012, in final form 31 October 2012) ABSTRACT Large-scale monsoon gyres and the involved tropical cyclone formation over the western North Pacific have been documented in previous studies. The aim of this study is to understand how monsoon gyres affect tropical cyclone formation. An observational study is conducted on monsoon gyres during the period 2000–10, with a focus on their structures and the associated tropical cyclone formation. A total of 37 monsoon gyres are identified in May–October during 2000–10, among which 31 monsoon gyres are accompanied with the formation of 42 tropical cyclones, accounting for 19.8% of the total tropical cyclone formation. Monsoon gyres are generally located on the poleward side of the composited monsoon trough with a peak occurrence in August–October. Extending about 1000 km outward from the center at lower levels, the cyclonic circulation of the composited monsoon gyre shrinks with height and is replaced with negative relative vorticity above 200 hPa. The maximum winds of the composited monsoon gyre appear 500–800 km away from 2 the gyre center with a magnitude of 6–10 m s 1 at 850 hPa. In agreement with previous studies, the com- posited monsoon gyre shows enhanced southwesterly flow and convection on the south-southeastern side.
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												  Boundary Layer Structure in Typhoon Saomai (2006): Understanding the Effects of Exchange CoefficientVol.18 No.2 JOURNAL OF TROPICAL METEOROLOGY June 2012 Article ID: 1006-8775(2012) 02-0195-12 BOUNDARY LAYER STRUCTURE IN TYPHOON SAOMAI (2006): UNDERSTANDING THE EFFECTS OF EXCHANGE COEFFICIENT 1 1 1 2 MING Jie (明 杰) , SONG Jin-jie (宋金杰) , CHEN Bao-jun (陈宝君) , WANG Ke-fa (王可发) (1. Key Laboratory of Mesoscale Severe Weather and School of Atmospheric Sciences, Nanjing University, Nanjing 210093 China; 2. Climate Center, Meteorological Bureau of Jiangsu Province, Nanjing 210008 China) Abstract: Recent studies have shown that surface fluxes and exchange coefficients are particularly important to models attempting to simulate the evolution and maintenance of hurricanes or typhoons. By using an advanced research version of the Weather Research and Forecasting (ARW) modeling system, this work aims to study the impact of modified exchange coefficient on the intensity and structures of typhoon Saomai (2006) over the western North Pacific. Numerical experiments with the modified and unmodified exchange coefficients are used to investigate the intensity and structure of the storm, especially the structures of the boundary layer within the storm. Results show that, compared to the unmodified experiment, the simulated typhoon in the modified experiment has a bigger deepening rate after 30-h and is the same as the observation in the last 12-h. The roughness is leveled off when wind speed is greater than 30 m/s. The momentum exchange coefficient (CD) and enthalpy exchange coefficient (CK) are leveled off too, and CD is decreased more than CK when wind speed is greater than 30 m/s. More sensible heat flux and less latent heat flux are produced.
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												  World Bank DocumentDocument of The World Bank FOR OFFICIAL USE ONLY Public Disclosure Authorized Report No. 82638-PH INTERNATIONAL BANK FOR RECONSTRUCTION AND DEVELOPMENT SUPPLEMENTAL FINANCING DOCUMENT Public Disclosure Authorized FOR PROPOSED SUPPLEMENTAL FINANCING IN THE AMOUNT OF US$500 MILLION TO THE REPUBLIC OF THE PHILIPPINES FOR Public Disclosure Authorized THE PHILIPPINES SECOND DEVELOPMENT POLICY LOAN TO FOSTER MORE INCLUSIVE GROWTH FOR POST TYPHOON RECOVERY December 04, 2013 Poverty Reduction and Economic Management Sector Department Philippines East Asia and Pacific Region Public Disclosure Authorized This document has a restricted distribution and may be used by recipients only in the performance of their official duties. Its contents may not otherwise be disclosed without World Bank authorization. GOVERNMENT'S FISCAL YEAR January 1 – December 31 CURRENCY EQUIVALENTS Currency unit: Philippine Pesos (PHP) as of November 12, 2013 US$ 1 = PHP43.59 Currency Unit US$1.00 ABBREVIATIONS AND ACRONYMS AIR Applied Insurance Research JBIC Japan Bank for International Cooperation BPO Business Processing and Outsourcing KALAHI- Kapitbisig Laban Sa Kahirapan- CIDSS Comprehensive and Integrated Delivery of Social Services BSP Bangko Sentral ng Pilipinas LBP Land Bank of the Philippines CAS Country Assistance Strategy LDP Letter of Development Policy CAT-DDO Catastrophe Draw Down Option LGU Local Government Unit CCT Conditional Cash Transfer NCDDP National Community Driven Development Project COA Commission on Audit NDRRMC National Disaster Risk Reduction
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												  Appendix 8: Damages Caused by Natural DisastersBuilding Disaster and Climate Resilient Cities in ASEAN Draft Finnal Report APPENDIX 8: DAMAGES CAUSED BY NATURAL DISASTERS A8.1 Flood & Typhoon Table A8.1.1 Record of Flood & Typhoon (Cambodia) Place Date Damage Cambodia Flood Aug 1999 The flash floods, triggered by torrential rains during the first week of August, caused significant damage in the provinces of Sihanoukville, Koh Kong and Kam Pot. As of 10 August, four people were killed, some 8,000 people were left homeless, and 200 meters of railroads were washed away. More than 12,000 hectares of rice paddies were flooded in Kam Pot province alone. Floods Nov 1999 Continued torrential rains during October and early November caused flash floods and affected five southern provinces: Takeo, Kandal, Kampong Speu, Phnom Penh Municipality and Pursat. The report indicates that the floods affected 21,334 families and around 9,900 ha of rice field. IFRC's situation report dated 9 November stated that 3,561 houses are damaged/destroyed. So far, there has been no report of casualties. Flood Aug 2000 The second floods has caused serious damages on provinces in the North, the East and the South, especially in Takeo Province. Three provinces along Mekong River (Stung Treng, Kratie and Kompong Cham) and Municipality of Phnom Penh have declared the state of emergency. 121,000 families have been affected, more than 170 people were killed, and some $10 million in rice crops has been destroyed. Immediate needs include food, shelter, and the repair or replacement of homes, household items, and sanitation facilities as water levels in the Delta continue to fall.
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												  China Date: 8 January 2007Refugee Review Tribunal AUSTRALIA RRT RESEARCH RESPONSE Research Response Number: CHN31098 Country: China Date: 8 January 2007 Keywords: China – Taiwan Strait – 2006 Military exercises – Typhoons This response was prepared by the Country Research Section of the Refugee Review Tribunal (RRT) after researching publicly accessible information currently available to the RRT within time constraints. This response is not, and does not purport to be, conclusive as to the merit of any particular claim to refugee status or asylum. Questions 1. Is there corroborating information about military manoeuvres and exercises in Pingtan? 2. Is there any information specifically about the military exercise there in July 2006? 3. Is there any information about “Army day” on 1 August 2006? 4. What are the aquatic farming/fishing activities carried out in that area? 5. Has there been pollution following military exercises along the Taiwan Strait? 6. The delegate makes reference to independent information that indicates that from May until August 2006 China particularly the eastern coast was hit by a succession of storms and typhoons. The last one being the hardest to hit China in 50 years. Could I have information about this please? The delegate refers to typhoon Prapiroon. What information is available about that typhoon? 7. The delegate was of the view that military exercises would not be organised in typhoon season, particularly such a bad one. Is there any information to assist? RESPONSE 1. Is there corroborating information about military manoeuvres and exercises in Pingtan? 2. Is there any information specifically about the military exercise there in July 2006? There is a minor naval base in Pingtan and military manoeuvres are regularly held in the Taiwan Strait where Pingtan in located, especially in the June to August period.
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												  Interaction Between Tropical Cyclone and Southwesterly MonsoonInteraction between tropical cyclone and southwesterly monsoon Qinghong Zhang(张庆红) Department of Atmospheric and Oceanic Science, School of Physics, Beijing 100871 Email: [email protected] Collaborator: Zhanpeng Dai Roving seminar Dec 2010 Thailand Satellite FY 2C IR observation 1953-2006 Bilis 路径南北5个经 纬度内的登陆热带 气旋共有30个 Rainfall Comparison between observation & MM5-9km simulation Rainfall Reinforcement Associated with Landfalling Tropical Cyclones in Mainland China (Dong et. al. 2010) Initial field of sensitive experiment Control weaker Comparison 850 hPa wind speed over SCS of control and weaker TC run 3-4 m/s difference Momentum budget Pressure advection gradient force Momentum budget comparison between control and weaker TC run PGD weaker TC PGD control Advection control Advection weaker TC 30 typhoons with similar track with Bilis Mesoscale convection systems accompanied with tropical cyclone landfall would enhance the pressure gradient force in low atmosphere above South China Sea Region, which would lead to intensification of the low level jet in summer monsoon. from 1950 to 2009, 80% of the tropical cyclone activities accompany with positive low level wind speed anomaly in South China Sea . TC Monsoon Rainfall Reinforcement Associated with Landfalling Tropical Cyclones in Mainland China (Dong et. al. 2010) Study on the potential impact of landfall TC in China Qinghong Zhang(张庆红) Department of Atmospheric and Oceanic Science, School of Physics, Beijing 100871 Email: [email protected] Collaborator: Qing Wei , Lianshou Chen and Zhanpeng Dai Roving seminar Dec 2010 Thailand Motivation • Landfall TCs are high-impact weather systems in China. • Prediction of TC economic loss are based on the statistics using intensity observed, forecasting track in China • How to predict the potential impact, especially economic impact before TC landfall is still not clear.
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												  Gaining from Losses: Using Disaster Loss Data As a Tool for Appraising Natural Disaster PolicyGAINING FROM LOSSES: USING DISASTER LOSS DATA AS A TOOL FOR APPRAISING NATURAL DISASTER POLICY by SHALINI MOHLEJI B.A., University of Virginia, 2000 M.S., Purdue University, 2002 A thesis submitted to the Faculty of the Graduate School of the University of Colorado in partial fulfillment of the requirement for the degree of Doctor of Philosophy Environmental Studies Program 2011 This thesis entitled: Gaining from Losses: Using Disaster Loss Data as a Tool for Appraising Natural Disaster Policy written by Shalini Mohleji has been approved for the Environmental Studies Program Roger Pielke Jr. Sam Fitch Date 5/26/11 The final copy of this thesis has been examined by the signatories, and we find that both the content and the form meet acceptable presentation standards of scholarly work in the above mentioned discipline. IRB protocol #: 11-0029 iii Mohleji, Shalini (Ph.D., Environmental Studies) Gaining from Losses: Using Disaster Loss Data as a Tool for Appraising Natural Disaster Policy Thesis directed by Dr. Roger Pielke Jr. ABSTRACT This dissertation capitalizes on an opportunity, untapped until now, to utilize data on disaster losses to appraise natural disaster policy. Through a set of three distinct studies, I use data on economic losses caused by natural disasters in order to analyze trends in disaster severity and answer important disaster policy questions. The first study reconciles the apparent disconnect between (a) claims that global disaster losses are increasing due to anthropogenic climate change and (b) studies that find regional losses are increasing due to socioeconomic factors. I assess climate change and global disaster severity through regional analyses derived by disaggregating global loss data into their regional components.
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												  Mega-Stress for Mega-Cities a Climate Vulnerability Ranking of Major Coastal Cities in AsiaMega-Stress for Mega-Cities A Climate Vulnerability Ranking of Major Coastal Cities in Asia Shanghai CHINA BANGLADESH Hong Kong Calcutta Dhaka INDIA Manila PHILIPPINES THAILAND VIETNAM Bangkok CAMBODIA Phnom Ho Chi Minh Penh Kuala Lumpur MALAYSIA SINGAPORE INDONESIA Jakarta Table of Contents Section I 3 - 6 Executive Summary Section II 7 - 8 Context Section III 9 - 10 Methodology Section IV City Scorecards 11 - 12 Dhaka, Bangladesh 13 - 14 Jakarta, Indonesia 15 - 16 Manila, Philippines 17 - 18 Calcutta, India 19 - 20 Phnom Penh, Cambodia 21 - 22 Ho Chi Minh, Vietnam 23 - 24 Shanghai, China 25 - 26 Bangkok, Thailand 27 - 28 Hong Kong, China 29 - 30 Kuala Lumpur, Malaysia 31 - 32 Singapore, Republic of Singapore Section V 33 - 34 Vulnerability Rankings Section VI 35 - 36 Policy Recommendations Section VII 37 - 39 References and Resources 2 Section I Executive Summary Asia is arguably among the regions of the world most vulnerable to climate change. Climate change and climatic variability have and will continue to impact all sectors, from national and economic security to human health, food production, infrastructure, water availability and ecosystems. The evidence of climate change in Asia is widespread: overall temperatures have risen from 1°C to 3°C over the last 100 years, precipitation patterns have changed, the number of extreme weather events is increasing, and sea levels are rising. Because many of the largest cities in Asia are located on the coast and within major river deltas, they are even more susceptible to the impacts of climate change. In response, this report highlights the vulnerability of some of those cities - with the goal of increasing regional awareness of the impacts of climate change, providing a starting point for further research and policy discussions, and triggering action to protect people and nature in and around Asia’s mega- cities from mega-stress in the future.
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												  Impact of Tropical Intraseasonal Oscillation on the Tracks of Tropical Cyclones in the Western North PacificVol.20 No.1 JOURNAL OF TROPICAL METEOROLOGY March 2014 Article ID: 1006-8775(2014) 01-0026-09 IMPACT OF TROPICAL INTRASEASONAL OSCILLATION ON THE TRACKS OF TROPICAL CYCLONES IN THE WESTERN NORTH PACIFIC 1 2 TAO Li (陶 丽) , LI Shuang-jun (李双君) (1. Key Laboratory of Meteorological Disaster of Ministry of Education, Nanjing University of Information Science and Technology, Nanjing 210044 China; 2. Wuhan Central Meteorological Observatory, Wuhan 430074 China) Abstract: In this work, an index of tropical 20-90 d oscillation (intra-seasonal oscillation; ISO) in the western North Pacific (WNP) was determined via the combined empirical orthogonal function (EOF) method using daily outgoing longwave radiation (OLR) field data from the National Oceanic and Atmospheric Administration (NOAA), daily wind field data (at 850 hPa) from the European Centre for Medium-Range Weather Forecasts (ECMWF) and referencing the Madden-Julian oscillation (MJO) index proposed by Wheeler and Hendon. An in-depth investigation was conducted to examine the impact of the ISO on changes in tropical cyclone (TC) tracks in the WNP during different ISO phases. The research results indicate that during the easterly phase of the ISO, under the impact of the northeastern airflow of anti-cyclonic ISO circulation, the easterly airflow south of the western Pacific subtropical high is relatively weak, and TCs generated in the subtropical high tend to change their tracks east of 140°E; during the westerly phase, there is a relatively high probability that TCs change their tracks west of 140°E. This work also analyzed the ISO flow field situation in cases of typhoons and determined that the track of a tropical cyclone will experience a sudden right turn when the center of the ISO cyclonic (anti-cyclonic) circulation coincides with that of the cyclone.