P1.24 a Typhoon Loss Estimation Model for China

Total Page:16

File Type:pdf, Size:1020Kb

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. Bilis was cause damage. The high landfall frequency is a responsible for ~28 B RMB (~3.5 B USD) of result of China being at the western edge of the economic loss. Bilis had half the winds of Saomai Northwest Pacific Basin and to the fact that China but generated twice the loss. Bilis affected six has a coastline extending nearly 14,000 km in a provinces and Saomai affected three. north-south direction and spanning nearly 30 degrees of latitude - from 18 N to 45 N. While China has had a long history of significant typhoon losses, the insurance industry These tropical cyclones, or typhoons as they targeted toward these disasters is still in its are called in that part of the world, cause infancy. Worldwide, the Chinese non-life considerable damage. Over just a recent 16 year insurance market was only the 12 th largest in period, from 1989 to 2005, economic losses 2005. However, within Asia, China ranked 3 rd in totaling in the billions of US dollars have occurred Life and Non-Life Insurance Premiums for the in the coastal provinces of Jiangsu, Zhejiang, and same time (Int’l Ins. Fact Book 2006). Figure 3 Fujian (Guy Carpenter, 2006). Zhejiang has indicates Non-Life Insurance Premiums were actually been the province with the highest losses 10.7 B USD in 2003. Despite its high ranking in since 1989 (cf. Fig. 2). The heavy loss is a Asia, China accounted for only 1.4% of global combined result of high exposure and impact non-life insurance premium income in 2005. from strong typhoons. Insurance Premium Growth in China The word typhoon stems from the Chinese however is among the highest in Asia. Non Life jufeng which originated in 5th century Chinese Per Capita Premiums in China have doubled literature to mean “ a wind coming from four from 2001 to 2005. Only Thailand and Indonesia directions ” (cf. p. 19-20 in Emanuel 2005). have enjoyed higher growth rates (Benfield Typhoons in China certainly cause significant Group Ltd, 2006). damage because of their wind. But typhoons are also responsible for considerable damage from AIR-Worldwide Corporation is a catastrophe flooding that results from torrential rainfall. The modeling firm located in Boston, MA. Its mission significance of flood damage from typhoons is is to develop models and provide information for most recently highlighted by comparing two use by the insurance industry for understanding typhoons that impacted China in 2006: Bilis and risk from Natural and Man-Made Hazards. Saomai. Saomai affected Zhejiang and Fujian Provinces and is perhaps the more showcased of Founded in 1987, AIR pioneered the probabilistic catastrophe modeling technology that revolutionized the way insurers, reinsurers * Corresponding author address: Peter J. and financial institutions manage their Sousounis, AIR-Worldwide Corporation., 131 catastrophe risk. The models developed at AIR Dartmouth Street, Boston, MA 02116; email: enable companies to identify, quantify, and plan [email protected]. Fig 1. Tropical Cyclone Formation (Wind Speeds > 63 km/h) by Ocean Basin. for the financial consequences of catastrophic events. 2. GENERAL STRUCTURE OF CATASTROPHE MODELS AIR has developed risk models for hurricanes, earthquakes, winter storms, Most catastrophe models (or cat Models for tornadoes, hailstorms, wildfires, and flood, for short) share three common elements. The hazard more than 40 countries throughout North component first models the frequency, intensity America, the Caribbean, South America, Europe and duration, if applicable, of the peril that is and the Asia-Pacific region. Recently, AIR responsible for the damage. The engineering or developed a China Typhoon Model to understand damage component then determines the fraction tropical cyclone risk in that country. of the building(s) in affected areas including their contents that have been damaged. Finally, a loss The following sections provide an overview estimation component computes insured losses of the China Typhoon Model components, the by applying the policy conditions to the total regionally specific meteorological and damage estimates. Policy conditions may include hydrological aspects of the model, and results deductibles by coverage, site-specific or blanket that highlight the typhoon risk in China. deductibles, coverage limits and sub-limits, loss triggers, coinsurance, attachment points and Economic Losses 1989-2005 limits for single or multiple location policies, and risk specific reinsurance terms. 791 – 3,160 B RMB 3,161 – 13,430 B RMB For estimation of insured losses, two 13,431 – 25,280 B RMB important input data files are the event catalog 25,281 – 43,450 B RMB and the exposure file. The catalog file provides a complete list of synthesized (e.g., stochastic) Shandong events along with their attributes over a 10,000 year period representing 10,000 scenarios of Jiangsu Shanghai storm activity that could occur in any given year. Zhejiang The second file, the exposure file, contains area averaged information about building types, Fujian construction materials, construction designs, Guangxi Guangdong occupancy, and height, as well as total replacement values for the buildings and associated contents. In addition to an industry Hainan China Oceanic Disaster Bulletin (1989 – 2005) exposure file that is developed internally, exposure files are often supplied by an insurance Fig. 2. Economic Losses in China from Typhoons or re-insurance client who is interested in as reported in China Oceanic Disaster Bulletin. knowing what the potential losses would be on their particular portfolio. Non-Life Insurance Premiums (2005) of friction, terrain, and shorter-period gusts using Vietnam high resolution land use/land cover and digital- Philippines elevation data to obtain a 1-minute 10-meter wind Indonesia over land. Thailand Malaysia Windspeeds are computed at every hour of Singapore the storm’s lifetime for all exposure points and Hong Kong stored as necessary. Very weak winds are India ignored as they do not contribute to damage. Taiwan Thus, for each location in question, a temporal China profile of damaging winds is produced for use in South Korea the other two model components. Japan In the damage component of the model, the 0 20 40 60 80 100 120 temporal profile is used in conjunction with the Premiums (B USD) relevant exposure information and proprietary damage functions (DFs) developed at AIR. These Fig. 3. Non-life insurance premiums in billions of DFs account for the fact that different types of US dollars for 2005 for selected countries in Asia. buildings behave differently under strong wind conditions. Building types are based on construction material as well as occupancy class For tropical cyclone models, the stochastic and height. For example, a three-story wooden storm tracks are generated using probability residential structure will be much more models that are developed and based on susceptible to wind damage than a one-story historical information. Specifically, stochastic commercial steel structure. storms are generated by first drawing a starting point probabilistically over the Northwest Pacific At each exposure point, the fractional Ocean, for example. The initial track direction of damage of the building and its contents as well the storm, as well as forward speed, intensity and as additional time-element related damage is radius of maximum winds are assigned according computed. Time-element damage is that which to the probability distribution derived from relates to a business possibly being disrupted for historical data. Time series models are then used some time following the event. If a flood to simulate storm path and characteristics along component is included in the tropical cyclone the path – basically to move the storm forward. model, as is the case here with the AIR China This process is repeated for every 6-hourly point. Typhoon Model, then that damage is determined This way a potential typhoon is generated with in a similar way, with flood depth information hourly information. The algorithm automatically rather than windspeed information, and with flood determines whether the storm makes landfall. DFs rather than wind DFs. The flood component With this Monte Carlo method, potential typhoons will be discussed in more detail in the next are generated for hundreds and thousands of section. years. The collection of possible events is called a stochastic catalog.
Recommended publications
  • 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.
    [Show full text]
  • An Efficient Method for Simulating Typhoon Waves Based on A
    Journal of Marine Science and Engineering Article An Efficient Method for Simulating Typhoon Waves Based on a Modified Holland Vortex Model Lvqing Wang 1,2,3, Zhaozi Zhang 1,*, Bingchen Liang 1,2,*, Dongyoung Lee 4 and Shaoyang Luo 3 1 Shandong Province Key Laboratory of Ocean Engineering, Ocean University of China, 238 Songling Road, Qingdao 266100, China; [email protected] 2 College of Engineering, Ocean University of China, 238 Songling Road, Qingdao 266100, China 3 NAVAL Research Academy, Beijing 100070, China; [email protected] 4 Korea Institute of Ocean, Science and Technology, Busan 600-011, Korea; [email protected] * Correspondence: [email protected] (Z.Z.); [email protected] (B.L.) Received: 20 January 2020; Accepted: 23 February 2020; Published: 6 March 2020 Abstract: A combination of the WAVEWATCH III (WW3) model and a modified Holland vortex model is developed and studied in the present work. The Holland 2010 model is modified with two improvements: the first is a new scaling parameter, bs, that is formulated with information about the maximum wind speed (vms) and the typhoon’s forward movement velocity (vt); the second is the introduction of an asymmetric typhoon structure. In order to convert the wind speed, as reconstructed by the modified Holland model, from 1-min averaged wind inputs into 10-min averaged wind inputs to force the WW3 model, a gust factor (gf) is fitted in accordance with practical test cases. Validation against wave buoy data proves that the combination of the two models through the gust factor is robust for the estimation of typhoon waves.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Help Families Affected by Typhoon Nina (Nock-Ten) Despite Typhoon
    Help Families Affected by Typhoon Nina (Nock-ten) Despite typhoon Nina (Nock-ten) being downgraded to a severe tropical storm as it leaves the country, families in central Philippines will still need assistance following the damage to their homes and sources of income. “Clearing operations have started in the different parts of Camarines. While traveling to Naga City, we saw families leaving evacuation centres to head back home to gauge the damage caused to their property,” says Maricel Francia, World Vision‟s Programme Officer based in Camarines Norte. World Vision emergency response teams in the Bicol region have been constantly coordinating with local government units since yesterday, December 26 to determine the immediate need of the affected population and the extent of damages to infrastructure and property. World Vision‟s rapid assessment team of staff skilled in emergency response management, child protection, health and nutrition and documentation is now heading to Bicol region from Manila, to reinforce WV staff on the ground. According to the national disaster risk reduction and management council (NDRRMC), about 25,000 families, with around 81% coming from the Bicol region, were affected by typhoon Nina (international name: Nock-ten). Officials have declared a „state of calamity‟ in the provinces of Catanduanes, Camarines Sur and Albay. Six casualties have been reported. As of December 27, 13 road sections and three bridges in regions II, MIMAROPA, V and VII are still not passable while 114 areas are experiencing power cuts since December 25. “Our main focus is on assessing the immediate needs of families and communities, especially the children displaced by the typhoon.
    [Show full text]
  • Review of Surge Practices
    TYPHOON NOCK TEN - THE PHILIPPINES REVIEW OF SURGE PRACTICES TRANSFORMING SURGE CAPACITY PROJECT START NETWORK SURGE RESEARCH TEAM: LOIS AUSTIN, SARAH GROSSO AND GLENN O’NEIL DECEMBER 2017 TRANSFORMING SURGE CAPACITY 2 PROJECT Acknowledgements The research team would like to express its appreciation to the international, regional and national platforms of the Surge Capacity Project and the Core Humanitarian Standard on Quality and Accountability (CHS) Alliance for their support. Particular thanks to the Philippines platform and the Nock Ten learning report authors, Ana Marie Dizon and Mary Joy Gonzales. The team found the feedback and information provided by all project member agencies and their local partners very useful. Thanks also to the UK Department for International Development for funding the project that covers this research. About the authors This research is the work of Lois Austin, Sarah Grosso and Glenn O’Neil, who have extensive experience in the humanitarian and development sectors. The team has significant experience in research, managing surge responses and serving as part of surge teams. Lois Austin: Lois has worked for 20 years in the humanitarian field, serving in a broad range of field-based and headquarters positions. Lois has managed and provided technical inputs into wide-ranging assistance, protection and recovery programmes for vulnerable populations in a number of complex and often fluctuating environments in: the Balkans; the North and South Caucasus; the Middle East; Afghanistan; Asia and throughout Africa. Lois’ field and headquarters experience has formed the basis for a solid understanding of humanitarian issues, including approaches to surge response, from both policy and operational perspectives.
    [Show full text]
  • China Date: 8 January 2007
    Refugee 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.
    [Show full text]
  • Preparing for a Changing Climate
    CHAPTER ONE— INTRODUCTION History of the Assessment the box below). Such research includes long-term monitor- ing of greenhouse gases at sites like Mauna Loa in Hawai‘i; studies of the regional and global influence of Pacific “The impacts of the 1997–1998 El Niño are ocean-atmosphere processes such as ENSO; and studies of fresh in our minds, and the latest reports from the ocean’s role in the carbon cycle, as well as the region’s the work of the Intergovernmental Panel on significance in terms of biodiversity and endangered Climate Change (IPCC) confirm what all of you species. already know— changes in climate matter to individuals, communities, businesses and Finally, the Pacific Assessment was an effort to build on the governments who call islands home. Your valuable natural resources, traditional ways of leadership of the Pacific Region in establishing and sustaining a critical dialogue on climate variability and life, critical economic sectors, community support change among scientists, businesses, governments and infrastructure, and, to a great extent, your future, depend on developing an effective community leaders. Elements of this dialogue include the role of Pacific Island governments and regional organiza- response to the challenges presented by climate tions in raising international awareness of the potential variability and change.” (Morrison, 2000) consequences of climate change, as well as the success of innovative programs like the Pacific ENSO Applications With these words, Dr. Charles Morrison, President of the Center (PEAC), which is designed to facilitate use of East-West Center, welcomed participants to the “Workshop emerging climate forecasting capabilities to support on Climate and Island Coastal Communities” convened in decision-making.
    [Show full text]
  • Incident Command System (Ics) Performance Evaluation Philippines
    INCIDENT COMMAND SYSTEM (ICS) PERFORMANCE EVALUATION PHILIPPINES COUNTRY REPORT This publication was produced at the request of the United States Agency for International Development. It was prepared independently by DevTech Systems, Inc. INCIDENT COMMAND SYSTEM (ICS) PERFORMANCE EVALUATION PHILIPPINES COUNTRY REPORT A Performance Evaluation of the ICS System in Philippines Covering the Assistance Provided by USAID/OFDA from 2011 August 14, 2017 USAID Contract No AID-OAA-I-15-0008 DISCLAIMER The author’s views expressed in this publication do not necessarily reflect the views of the United States Agency for International Development or the United States Government. Cover photo: Microtel Incident Command Post managing ASEAN50 Meeting near Mall of Asia, Manila, Philippines i Contents Acronyms ....................................................................................................................................................................... ii I. Evaluation Purpose ............................................................................................................................................... 1 II. Evaluation Questions ............................................................................................................................................ 1 III. Project Background ............................................................................................................................................... 2 IV. Evaluation Methods & Limitations.......................................................................................................................
    [Show full text]
  • Chlorophyll Variations Over Coastal Area of China Due to Typhoon Rananim
    Indian Journal of Geo Marine Sciences Vol. 47 (04), April, 2018, pp. 804-811 Chlorophyll variations over coastal area of China due to typhoon Rananim Gui Feng & M. V. Subrahmanyam* Department of Marine Science and Technology, Zhejiang Ocean University, Zhoushan, Zhejiang, China 316022 *[E.Mail [email protected]] Received 12 August 2016; revised 12 September 2016 Typhoon winds cause a disturbance over sea surface water in the right side of typhoon where divergence occurred, which leads to upwelling and chlorophyll maximum found after typhoon landfall. Ekman transport at the surface was computed during the typhoon period. Upwelling can be observed through lower SST and Ekman transport at the surface over the coast, and chlorophyll maximum found after typhoon landfall. This study also compared MODIS and SeaWiFS satellite data and also the chlorophyll maximum area. The chlorophyll area decreased 3% and 5.9% while typhoon passing and after landfall area increased 13% and 76% in SeaWiFS and MODIS data respectively. [Key words: chlorophyll, SST, upwelling, Ekman transport, MODIS, SeaWiFS] Introduction runoff, entrainment of riverine-mixing, Integrated Due to its unique and complex geographical Primary Production are also affected by typhoons environment, China becomes a country which has a when passing and landfall25,26,27,28&29. It is well known high frequency of natural disasters and severe that, ocean phytoplankton production (primate influence over coastal area. Since typhoon causes production) plays a considerable role in the severe damage, meteorologists and oceanographers ecosystem. Primary production can be indexed by have studied on the cause and influence of typhoon chlorophyll concentration. The spatial and temporal for a long time.
    [Show full text]
  • Tropical Cyclogenesis Associated with Rossby Wave Energy Dispersion of a Preexisting Typhoon
    VOLUME 63 JOURNAL OF THE ATMOSPHERIC SCIENCES MAY 2006 Tropical Cyclogenesis Associated with Rossby Wave Energy Dispersion of a Preexisting Typhoon. Part I: Satellite Data Analyses* TIM LI AND BING FU Department of Meteorology, and International Pacific Research Center, University of Hawaii at Manoa, Honolulu, Hawaii (Manuscript submitted 20 September 2004, in final form 7 June 2005) ABSTRACT The structure and evolution characteristics of Rossby wave trains induced by tropical cyclone (TC) energy dispersion are revealed based on the Quick Scatterometer (QuikSCAT) and Tropical Rainfall Measuring Mission (TRMM) Microwave Imager (TMI) data. Among 34 cyclogenesis cases analyzed in the western North Pacific during 2000–01 typhoon seasons, six cases are associated with the Rossby wave energy dispersion of a preexisting TC. The wave trains are oriented in a northwest–southeast direction, with alternating cyclonic and anticyclonic vorticity circulation. A typical wavelength of the wave train is about 2500 km. The TC genesis is observed in the cyclonic circulation region of the wave train, possibly through a scale contraction process. The satellite data analyses reveal that not all TCs have a Rossby wave train in their wakes. The occur- rence of the Rossby wave train depends to a certain extent on the TC intensity and the background flow. Whether or not a Rossby wave train can finally lead to cyclogenesis depends on large-scale dynamic and thermodynamic conditions related to both the change of the seasonal mean state and the phase of the tropical intraseasonal oscillation. Stronger low-level convergence and cyclonic vorticity, weaker vertical shear, and greater midtropospheric moisture are among the favorable large-scale conditions.
    [Show full text]