Forecasting and Warning of Tropical Cyclones in China
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Topographic Influence on the Motion of Tropical Cyclones Landfalling on the Coast of China
OCTOBER 2016 C H E N A N D W U 1615 Topographic Influence on the Motion of Tropical Cyclones Landfalling on the Coast of China XIAOYU CHEN Key Laboratory of Meteorological Disaster, Ministry of Education/Joint International Research Laboratory of Climate and Environment Change/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters/Pacific Typhoon Research Center, Nanjing University of Information Science and Technology, Nanjing, China LIGUANG WU Key Laboratory of Meteorological Disaster, Ministry of Education/Joint International Research Laboratory of Climate and Environment Change/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters/Pacific Typhoon Research Center, Nanjing University of Information Science and Technology, Nanjing, and State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing, China (Manuscript received 17 March 2016, in final form 10 August 2016) ABSTRACT A few recent numerical studies investigated the influence of a continent, which is much larger in size than islands, on the track of a landfalling tropical cyclone. It has been found that land surface roughness and temperature tend to make a tropical cyclone move toward the continent. In this study, the effect of the elevated terrain on the western part of mainland China on landfall tracks is examined through idealized numerical experiments, in which an initially axisymmetric vortex is embedded into a monsoon trough and takes a landfall track across China’s mainland. It is found that the effect of the elevated terrain on the western part of mainland China can enhance the southerly environmental flows in the low and midtroposphere, leading to an additional landward component of tropical cyclone motion, suggesting that forecasts for tropical cyclone tracks over land should take into consideration the change in thermal condition over the continent. -
Enhancing Psychological Support
Appeal 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. -
P1.24 a Typhoon Loss Estimation Model for China
P1.24 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. -
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. -
Casualty Week Sep 10
Lloyd’s Casualty Week contains information from worldwide sources of Marine, Non-Marine and Aviation casualties together with other reports Lloyd's relevant to the shipping, transport and insurance communities CasualtyWeek September 10 2004 UASC master pays heaviest penalty for pollution HE Pakistani master of a the head of a 5 km long, 50 m wide Last year, the government United Arab Shipping slick off Cap Couronne, west of signalled its intention to get tough on T container vessel has Marseilles. marine waste dumping off its coasts received what is thought to be by transferring jurisdiction for the heaviest sentence imposed The master of the Cimil was 29- deliberate offshore pollution from by a French court since the year-old Bourak Vurnal, but, as in the Paris to courts in Marseilles, Brest case of the Khaled Ibn al-Waleed , the French authorities began and Le Havre. taking tougher action to stamp vessel’s owner, given by Equasis as out marine pollution off its Cimil Denizcilik of Istanbul, was Fine dodging coasts. ordered to pay the bulk of the fine — in this case euro 290,000. Since then, the courts have sought The Marseilles criminal court to prevent fine dodging by masters Waste dumping imposed on 54-year-old Anis Yazdani and owners by bringing offending Zuberi a 12-month suspended prison vessels into port and ordering sentence and a euro 500,000 Damages ranging from euro 3,000 payment of heavy bail as a condition ($600,000) fine, although it stipulated to euro 18,000 were also awarded to of their release. -
Observational Analysis of Heavy Rainfall Mechanisms Associated with Severe Tropical Storm Bilis (2006) After Its Landfall
JUNE 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. -
Observational Analysis of Tropical Cyclone Formation Associated with Monsoon Gyres
APRIL 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. -
Boundary Layer Structure in Typhoon Saomai (2006): Understanding the Effects of Exchange Coefficient
Vol.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. -
Chun-Chieh Wu (吳俊傑) Department of Atmospheric Sciences, National Taiwan University No. 1, Sec. 4, Roosevelt Rd., Taipei 1
Chun-Chieh Wu (吳俊傑) Department of Atmospheric Sciences, National Taiwan University No. 1, Sec. 4, Roosevelt Rd., Taipei 106, Taiwan Telephone & Facsimile: (886) 2-2363-2303 Email: [email protected], WWW: http://typhoon.as.ntu.edu.tw Date of Birth: 30 July, 1964 Education: Graduate: Massachusetts Institute of Technology, Ph.D., Department of Earth Atmospheric, and Planetary Sciences, May 1993 Thesis under the supervision of Professor Kerry A. Emanuel on "Understanding hurricane movement using potential vorticity: A numerical model and an observational study." Undergraduate: National Taiwan University, B.S., Department of Atmospheric Sciences, June 1986 Recent Positions: Professor and Chairman Department of Atmospheric Sciences, National Taiwan University August 2008 to present Director NTU Typhoon Research Center January 2009 to present Adjunct Research Scientist Lamont-Doherty Earth Observatory, Columbia University July 2004 - present Professor Department of Atmospheric Sciences, National Taiwan University August 2000 to 2008 Visiting Fellow Geophysical Fluid Dynamics Laboratory, Princeton University January – July, 2004 (on sabbatical leave from NTU) Associate Professor Department of Atmospheric Sciences, National Taiwan University August 1994 to July 2000 Visiting Research Scientist Geophysical Fluid Dynamics Laboratory, Princeton University August 1993 – November 1994; July to September 1995 1 Awards: Gold Bookmarker Prize Wu Ta-You Popular Science Book Prize in Translation Wu Ta-You Foundation, 2008 Outstanding Teaching Award, National Taiwan University, 2008 Outstanding Research Award, National Science Council, 2007 Research Achievement Award, National Taiwan Univ., 2004 University Teaching Award, National Taiwan University, 2003, 2006, 2007 Academia Sinica Research Award for Junior Researchers, 2001 Memberships: Member of the American Meteorological Society. Member of the American Geophysical Union. -
Extending Effect of a Wind Disturbance: Mortality of Abies Sachalinensis Following a Strong Typhoon in a Natural Mixed Title Forest
Extending effect of a wind disturbance: mortality of Abies sachalinensis following a strong typhoon in a natural mixed Title forest Author(s) Sato, Tsuyoshi; Yamazaki, Haruka; Yoshida, Toshiya Journal of Forest Research, 22(6), 336-342 Citation https://doi.org/10.1080/13416979.2017.1381492 Issue Date 2017-09 Doc URL http://hdl.handle.net/2115/71620 This is an Accepted Manuscript of an article published by Taylor & Francis in Journal of Forest Research on September Rights 2017, available online: http://www.tandfonline.com/10.1080/13416979.2017.1381492 . Type article (author version) File Information Journal of Forest Research_22(6)_336-342.pdf Instructions for use Hokkaido University Collection of Scholarly and Academic Papers : HUSCAP Extending effect of a wind disturbance: mortality of Abies sachalinensis following a strong typhoon in a natural mixed forest Tsuyoshi Sato Graduate School of Environmental Science, Hokkaido University; 250 Tokuda, Nayoro, 096-0071, Hokkaido, Japan Haruka Yamazaki Graduate School of Environmental Science, Hokkaido University; 250 Tokuda, Nayoro, 096-0071, Hokkaido, Japan Toshiya Yoshida * Uryu Experimental Forest, Field Science Center for Northern Biosphere, Hokkaido University; Moshiri, Horokanai, 074-0741, Hokkaido, Japan * Corresponding author: [email protected] Tel: +81-165-38-2125 Fax: +81-165-38-2410 Extending effect of a wind disturbance: mortality of Abies sachalinensis following a strong typhoon in a natural mixed forest Strong wind constitutes the major force behind disturbance of northern Japanese forests. Canopy gaps induced by disturbance are responsible for subsequent recovery of the stand (i.e., enhancement of growth and recruitment). There is also a possibility that a sudden change in stand structure, involving significant microclimatic alterations, results in further stand degradation. -
World Bank Document
Document 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 -
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.