Report on UN ESCAP / WMO Typhoon Committee Members Disaster Management System
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Typhoon Neoguri Disaster Risk Reduction Situation Report1 DRR Sitrep 2014‐001 ‐ Updated July 8, 2014, 10:00 CET
Typhoon Neoguri Disaster Risk Reduction Situation Report1 DRR sitrep 2014‐001 ‐ updated July 8, 2014, 10:00 CET Summary Report Ongoing typhoon situation The storm had lost strength early Tuesday July 8, going from the equivalent of a Category 5 hurricane to a Category 3 on the Saffir‐Simpson Hurricane Wind Scale, which means devastating damage is expected to occur, with major damage to well‐built framed homes, snapped or uprooted trees and power outages. It is approaching Okinawa, Japan, and is moving northwest towards South Korea and the Philippines, bringing strong winds, flooding rainfall and inundating storm surge. Typhoon Neoguri is a once‐in‐a‐decade storm and Japanese authorities have extended their highest storm alert to Okinawa's main island. The Global Assessment Report (GAR) 2013 ranked Japan as first among countries in the world for both annual and maximum potential losses due to cyclones. It is calculated that Japan loses on average up to $45.9 Billion due to cyclonic winds every year and that it can lose a probable maximum loss of $547 Billion.2 What are the most devastating cyclones to hit Okinawa in recent memory? There have been 12 damaging cyclones to hit Okinawa since 1945. Sustaining winds of 81.6 knots (151 kph), Typhoon “Winnie” caused damages of $5.8 million in August 1997. Typhoon "Bart", which hit Okinawa in October 1999 caused damages of $5.7 million. It sustained winds of 126 knots (233 kph). The most damaging cyclone to hit Japan was Super Typhoon Nida (reaching a peak intensity of 260 kph), which struck Japan in 2004 killing 287 affecting 329,556 people injuring 1,483, and causing damages amounting to $15 Billion. -
Chapter 7. Building a Safe and Comfortable Society
Section 1 Realizing a Universal Society Building a Safe and Comfortable Chapter 7 Society Section 1 Realizing a Universal Society 1 Realizing Accessibility through a Universal Design Concept The “Act on Promotion of Smooth Transportation, etc. of Elderly Persons, Disabled Persons, etc.” embodies the universal design concept of “freedom and convenience for anywhere and anyone”, making it mandatory to comply with “Accessibility Standards” when newly establishing various facilities (passenger facilities, various vehicles, roads, off- street parking facilities, city parks, buildings, etc.), mandatory best effort for existing facilities as well as defining a development target for the end of FY2020 under the “Basic Policy on Accessibility” to promote accessibility. Also, in accordance with the local accessibility plan created by municipalities, focused and integrated promotion of accessibility is carried out in priority development district; to increase “caring for accessibility”, by deepening the national public’s understanding and seek cooperation for the promotion of accessibility, “accessibility workshops” are hosted in which you learn to assist as well as virtually experience being elderly, disabled, etc.; these efforts serve to accelerate II accessibility measures (sustained development in stages). Chapter 7 (1) Accessibility of Public Transportation In accordance with the “Act on Figure II-7-1-1 Current Accessibility of Public Transportation Promotion of Smooth Transportation, etc. (as of March 31, 2014) of Elderly Persons, Disabled -
Typhoon Hagupit (Ruby), Dec
Typhoon Hagupit (Ruby), Dec. 9, 2014 CDIR No. 6 BLUF – Implications to PACOM No DOD requirements anticipated PACOM Joint Liaison Group re-deploying from Philippines within next 72 hours (PACOM J35) Typhoon Hagupit – Stats & Facts Summary: (The following times in this report are Phil. local time unless otherwise specified) Current Status: Typhoon Hagupit has weakened into a tropical depression as it heads west into the West Philippine Sea towards Vietnam. All public storm warning signals have been lifted. Storm expected to head out of the Philippine Area of Responsibility (PAR) Thursday (11 DEC) early AM. Est. rainfall is 5 – 15 mm per hour (Moderate – heavy) within the 200 km of the storm. (NDRRMC, Bulletin No. 23) Local officials reported nearly 13,000 houses were destroyed and more than 22,300 were partially damaged in Eastern Samar province, where Hagupit first hit as a CAT 3 typhoon on 6 DEC. (Reuters) Deputy Presidential Spokesperson Key Concerns & Trends Abigail Valte said so far, Dolores appears worst hit. (GPH) Domestic air and sea travel has resumed, markets reopened • GPH and the international humanitarian community are and state workers returned to their offices. Some shopping capable of meeting virtually all disaster response requirements. Major malls were open but schools remained closed. actions and activities include: The privately run National Grid Corp said nearly two million Assessments are ongoing to determine the full extent of the homes across central Philippines and southern Luzon remain typhoon’s impact; reports so far indicate the scale and severity without power. (Reuters) Twenty provinces in six regions of the impact of Hagupit was not as great as initially feared. -
Variations in Typhoon Landfalls Over China Emily A
Florida State University Libraries Electronic Theses, Treatises and Dissertations The Graduate School 2004 Variations in Typhoon Landfalls over China Emily A. Fogarty Follow this and additional works at the FSU Digital Library. For more information, please contact [email protected] THE FLORIDA STATE UNIVERSITY COLLEGE OF SOCIAL SCIENCES VARIATIONS IN TYPHOON LANDFALLS OVER CHINA By EMILY A. FOGARTY A Thesis submitted to the Department of Geography in partial fulfillment of the requirements for the degree of Master of Science Degree Awarded: Fall Semester, 2004 The members of the Committee approve Thesis of Emily A. Fogarty defended on October 20, 2004. James B. Elsner Professor Directing Thesis Thomas Jagger Committee Member J. Anthony Stallins Committee Member The Office of Graduate Studies has verified and approved the above named committee members. ii ACKNOWLEDGEMENTS Special thanks to my advisor James Elsner, without his guidance none of this would be possible. Thank you to my other advisors Tom Jagger and Tony Stallins for their wonderful advice and help. Finally thank you to Kam-biu Liu from Louisiana State University for providing the historical data used in this study. iii TABLE OF CONTENTS List of Tables ................................................... .... v List of Figures ................................................... ... vi Abstract ................................................... ......... vii 1. INTRODUCTION ............................................... 1 2. DATA ................................................... ....... 4 2.1 Historical Typhoons over Guangdong and Fujian Province . 5 2.2 Modern Typhoon Records . 7 2.3 ENSO and the Pacific Decadal Oscillation . 8 2.4 NCEP/NCAR Reanalysis Data . 9 3. ANTICORRELATION BETWEEN GUANGDONG AND FUJIAN TYPHOON ACTIVITY .......................................... 12 4. SPATIAL CO-VARIABILITY IN CHINA LANDFALLS ............. 15 4.1 Factor Analysis Model . 16 4.2 Statistical Significance of the Factor Analysis Model . -
Recent Advances in Research on Tropical Cyclogenesis
Available online at www.sciencedirect.com ScienceDirect Tropical Cyclone Research and Review 9 (2020) 87e105 www.keaipublishing.com/tcrr Recent advances in research on tropical cyclogenesis Brian H. Tang a,*, Juan Fang b, Alicia Bentley a,y, Gerard Kilroy c, Masuo Nakano d, Myung-Sook Park e, V.P.M. Rajasree f, Zhuo Wang g, Allison A. Wing h, Liguang Wu i a University at Albany, State University of New York, Albany, USA b Nanjing University, Nanjing, China c Ludwig-Maximilians University of Munich, Munich, Germany d Japan Agency for Marine-Earth Science and Technology, Yokohama, Japan e Korea Institute of Ocean Science and Technology, Busan, South Korea f Centre for Atmospheric and Climate Physics Research, University of Hertfordshire, Hatfield, UK g University of Illinois, Urbana, USA h Florida State University, Tallahassee, USA i Fudan University, Shanghai, China Available online 7 May 2020 Abstract This review article summarizes recent (2014e2019) advances in our understanding of tropical cyclogenesis, stemming from activities at the ninth International Workshop on Tropical Cyclones. Tropical cyclogenesis involves the interaction of dynamic and thermodynamic processes at multiple spatio-temporal scales. Studies have furthered our understanding of how tropical cyclogenesis may be affected by external processes, such as intraseasonal oscillations, monsoon circulations, the intertropical convergence zone, and midlatitude troughs and cutoff lows. Addi- tionally, studies have furthered our understanding of how tropical cyclogenesis may be affected by internal processes, such as the organization of deep convection; the evolution of the “pouch” structure; the role of friction; the development of the moist, warm core; the importance of surface fluxes; and the role of the mid-level vortex. -
List of Recognized Villages Under the New Territories Small House Policy
LIST OF RECOGNIZED VILLAGES UNDER THE NEW TERRITORIES SMALL HOUSE POLICY Islands North Sai Kung Sha Tin Tuen Mun Tai Po Tsuen Wan Kwai Tsing Yuen Long Village Improvement Section Lands Department September 2009 Edition 1 RECOGNIZED VILLAGES IN ISLANDS DISTRICT Village Name District 1 KO LONG LAMMA NORTH 2 LO TIK WAN LAMMA NORTH 3 PAK KOK KAU TSUEN LAMMA NORTH 4 PAK KOK SAN TSUEN LAMMA NORTH 5 SHA PO LAMMA NORTH 6 TAI PENG LAMMA NORTH 7 TAI WAN KAU TSUEN LAMMA NORTH 8 TAI WAN SAN TSUEN LAMMA NORTH 9 TAI YUEN LAMMA NORTH 10 WANG LONG LAMMA NORTH 11 YUNG SHUE LONG LAMMA NORTH 12 YUNG SHUE WAN LAMMA NORTH 13 LO SO SHING LAMMA SOUTH 14 LUK CHAU LAMMA SOUTH 15 MO TAT LAMMA SOUTH 16 MO TAT WAN LAMMA SOUTH 17 PO TOI LAMMA SOUTH 18 SOK KWU WAN LAMMA SOUTH 19 TUNG O LAMMA SOUTH 20 YUNG SHUE HA LAMMA SOUTH 21 CHUNG HAU MUI WO 2 22 LUK TEI TONG MUI WO 23 MAN KOK TSUI MUI WO 24 MANG TONG MUI WO 25 MUI WO KAU TSUEN MUI WO 26 NGAU KWU LONG MUI WO 27 PAK MONG MUI WO 28 PAK NGAN HEUNG MUI WO 29 TAI HO MUI WO 30 TAI TEI TONG MUI WO 31 TUNG WAN TAU MUI WO 32 WONG FUNG TIN MUI WO 33 CHEUNG SHA LOWER VILLAGE SOUTH LANTAU 34 CHEUNG SHA UPPER VILLAGE SOUTH LANTAU 35 HAM TIN SOUTH LANTAU 36 LO UK SOUTH LANTAU 37 MONG TUNG WAN SOUTH LANTAU 38 PUI O KAU TSUEN (LO WAI) SOUTH LANTAU 39 PUI O SAN TSUEN (SAN WAI) SOUTH LANTAU 40 SHAN SHEK WAN SOUTH LANTAU 41 SHAP LONG SOUTH LANTAU 42 SHUI HAU SOUTH LANTAU 43 SIU A CHAU SOUTH LANTAU 44 TAI A CHAU SOUTH LANTAU 3 45 TAI LONG SOUTH LANTAU 46 TONG FUK SOUTH LANTAU 47 FAN LAU TAI O 48 KEUNG SHAN, LOWER TAI O 49 KEUNG SHAN, -
Disaster Preparedness Level, Graph Showed the Data in %, Developed on the Basis of Survey Conducted in Region Vi
2014 Figures Nature Begins Where Human Predication Ends Typhoon Frank (Fengshen) 17th to 27th June, 2008 Credit: National Institute of Geological Sciences, University of the Philippines, 2012 Tashfeen Siddique – Research Fellow AIM – Stephen Zuellig Graduate School of Development Management 8/15/2014 Nature Begins Where Human Predication Ends Contents Acronyms and Abbreviations: ...................................................................................................... iv Brief History ........................................................................................................................................ 1 Philippines Climate ........................................................................................................................... 2 Chronology of Typhoon Frank ....................................................................................................... 3 Forecasting went wrong .................................................................................................................. 7 Warning and Precautionary Measures ...................................................................................... 12 Typhoon Climatology-Science ..................................................................................................... 14 How Typhoon Formed? .............................................................................................................. 14 Typhoon Structure ..................................................................................................................... -
Appendix 8: Damages Caused by Natural Disasters
Building 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. -
Chapter 5: Getting Around Hong Kong
Chapter 5: Getting Around Hong Kong The Road Crossing Code It is safer to cross the road using footbridges, subways, “Zebra” crossings or “Green man” crossings. If you cannot find any such crossing facilities nearby, there are some basic steps for crossing roads that you need to observe: 1. Find a safe place where you can see clearly along the roads in all directions for any approaching traffic. 2. When checking traffic, stop a little way back from the kerb where you will be away from traffic. 3. Look all around for traffic and listen. However, electric/hybrid vehicles including motorcycles may operate very quietly. You need to look out for them in addition to listening. If traffic is coming, let it pass. Look all around and listen again. 4. Let the drivers know your intention to cross but do not expect a driver to slow down for you. 5. Do not cross unless you are certain there is plenty of time. Walk straight across the road when there is no traffic near. 6. Keep looking and listening for vehicles that come into sight or come near while you cross. 7. Do not carry out any other activities, such as eating, drinking, playing mobile games,using mobile phones, listening to any audio device or talking while crossing the road. Give all your attention to the traffic. Using crossing facilities Crossing aids are often provided to help you cross busy roads. Footbridges and subways: Footbridges, subways and elevated walkways are the safest places to cross busy roads as they keep pedestrians well away from the dangers of traffic. -
An Incoherent Subseasonal Pattern of Tropical Convective and Zonal Wind
An incoherent subseasonal pattern of tropical convective and zonal wind anomalies contributed to weak signals on both the Wheeler-Hendon (RMM) and CPC MJO indices during the past week. The spatial pattern of upper-level velocity potential anomalies exhibited influences from higher frequency modes, such as tropical cyclone activity over the eastern Pacific and anomalous divergence over Africa. During the past several days, however, these conflicting signals have weakened. Additionally, constructive interference of a strong equatorial Rossby Wave (ERW) and a Kelvin Wave over the eastern Indian Ocean and Maritime Continent contributed to an ongoing large area of enhanced convection. The RMM Index has responded to this evolution and is currently projecting a signal in Phase-4. Dynamical model MJO index forecasts are consistent with a rapid propagation of this signal eastward over the Maritime Continent during the upcoming week, likely due to influence from the Kelvin Wave. Beyond this period, however, the GFS weakens the MJO signal while the CFS, UKMET, and ECMWF models continue a slower eastward propagation over the western Pacific. There is uncertainty whether the enhanced convection over the Maritime Continent associated with the interactions between a more transient Kelvin Wave and the ERW will evolve into a more robust subseasonal signal on the MJO time scale. Due to the consensus among numerous dynamical models, however, impacts of MJO propagation from the Maritime Continent to the West Pacific were considered for this outlook. Tropical cyclones developed over both the eastern and western Pacific basins during the past week. Super Typhoon Neoguri, the third typhoon of 2014 and the first major cyclone, developed east of the Philippines on 3 July. -
Major Disposal and Connected Transaction (2) Proposed Special Dividend and Notice of Extraordinary General Meeting
THIS CIRCULAR IS IMPORTANT AND REQUIRES YOUR IMMEDIATE ATTENTION If you are in any doubt as to any aspect of this circular or as to the action to be taken, you should consult a Rule 14.63(2)(b) stockbroker or other registered dealer in securities, bank manager, solicitor, professional accountant or other Rule 14A.58(3)(b) professional adviser. If you have sold or transferred all your shares in Hop Hing Group Holdings Limited, you should at once hand this circular, together with the accompanying form of proxy, to the purchaser or the transferee or to the bank, stockbroker or other agent through which the sale or transfer was effected for transmission to the purchaser or the transferee. Hong Kong Exchanges and Clearing Limited and The Stock Exchange of Hong Kong Limited take no responsibility Rule 14.58(1) for the contents of this circular, make no representation as to its accuracy or completeness and expressly disclaim any Rule 13.52 Note 5 liability whatsoever for any loss howsoever arising from or in reliance upon the whole or any part of the contents of Rule 14A.59(1) this circular. This circular appears for information purpose only and does not constitute an invitation or offer to acquire, purchase or subscribe for the securities of Hop Hing Group Holdings Limited. App1B.1 HOP HING GROUP HOLDINGS LIMITED Rule 13.51A (Incorporated in the Cayman Islands with limited liability) (Stock Code: 47) (Warrant Code: 134) (1) MAJOR DISPOSAL AND CONNECTED TRANSACTION (2) PROPOSED SPECIAL DIVIDEND AND NOTICE OF EXTRAORDINARY GENERAL MEETING Financial -
North Pacific, on August 31
Marine Weather Review MARINE WEATHER REVIEW – NORTH PACIFIC AREA May to August 2002 George Bancroft Meteorologist Marine Prediction Center Introduction near 18N 139E at 1200 UTC May 18. Typhoon Chataan: Chataan appeared Maximum sustained winds increased on MPC’s oceanic chart area just Low-pressure systems often tracked from 65 kt to 120 kt in the 24-hour south of Japan at 0600 UTC July 10 from southwest to northeast during period ending at 0000 UTC May 19, with maximum sustained winds of 65 the period, while high pressure when th center reached 17.7N 140.5E. kt with gusts to 80 kt. Six hours later, prevailed off the west coast of the The system was briefly a super- the Tenaga Dua (9MSM) near 34N U.S. Occasionally the high pressure typhoon (maximum sustained winds 140E reported south winds of 65 kt. extended into the Bering Sea and Gulf of 130 kt or higher) from 0600 to By 1800 UTC July 10, Chataan of Alaska, forcing cyclonic systems 1800 UTC May 19. At 1800 UTC weakened to a tropical storm near coming off Japan or eastern Russia to May 19 Hagibis attained a maximum 35.7N 140.9E. The CSX Defender turn more north or northwest or even strength of 140-kt (sustained winds), (KGJB) at that time encountered stall. Several non-tropical lows with gusts to 170 kt near 20.7N southwest winds of 55 kt and 17- developed storm-force winds, mainly 143.2E before beginning to weaken. meter seas (56 feet). The system in May and June.