Impact of Typhoons on the Composition of the Upper Troposphere Within The
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The Wind Features Associated with the Multiple Eyewall in Typhoon Bolaven
The Wind Features associated with the Multiple Eyewall in Typhoon Bolaven Seiji ORIGUCHI, Kazuo SAITO, Hiromu SEKO, Wataru Mashiko and Masaru KUNII Meteorological Research Institute, Tsukuba, Ibaraki, 305-0052, JAPAN E-mail: [email protected] 1. Introduction Typhoon ‘Bolaven’ passed the Okinawa Main Island at about 1200 UTC 26 August 2012, while moving northwestward. The surface observation data at Nago of Okinawa show that the rainfall intensity and surface wind speed in the typhoon’s central regions were smaller and weaker than those of the JMA’s operational forecast. Okinawa Meteorological Observatory held an unprecedented press conference before the approach of typhoon ‘Bolaven’ to take the greatest precautions for the local governments and inhabitants. However, severe damages did not actually occur. The radar images of Japan Meteorological Agency (JMA) show that the multiple eyewall structures of ‘Bolaven’ were clearly maintained for more than at least 24 hours without eyewall replacements. It is deduced that the structures of multiple eyewall affected the wind velocity and precipitation in the typhoon’s central region. In this study, the multiple eyewall structures and wind features were reproduced by the cloud-resolving ensemble simulation to investigate the relation between them. 2. Experimental settings and Multi-Eye Index A cloud resolving ensemble simulation with a horizontal resolution of 1 km, horizontal grids of 800×800, 60 vertical layers and 11 members was performed up to the forecast time (FT) of 24 hours from the initial time at 1800 UTC 25 August using the JMA nonhydrostatic model. The initial and boundary conditions for the cloud resolving ensemble simulation were taken from a mesoscale ensemble simulation with a horizontal resolution of 5 km. -
The Influence of Typhoon on the Guangdong Power Grid and Countermeasures
2018 International Conference on Energy, Power, Electrical and Environmental Engineering (EPEEE 2018) ISBN: 978-1-60595-583-4 The Influence of Typhoon on the Guangdong Power Grid and Countermeasures 1 2 1 3,* Tuan-jie GAN , Jian-feng WEN , Lian-dong HUANG and Xue-jiao HAN 1Jiangmen Power Supply Company of Guangdong Power Grid Co., Ltd Guangdong 529000, China 2Guangdong Power Grid Co., Ltd Guangdong 510000, China 3Tsinghua University, Beijing 100084, China *Corresponding author Keywords: Typhoon, Transmission line, Distribution line, Countermeasures of wind disaster. Abstract. Guangdong affected by typhoon frequently, so power sectors pay high attention to the transmission line failure caused by the typhoon. Based on typhoon data in Guangdong, this paper gets characteristics of typhoon with a scientific method of the statistical analysis. By studying the loss of Jiangmen power grid caused by typhoon, this paper summarizes the cause of power accidents and puts forward countermeasures. It shows that typhoon mainly occurred between July and September in Guangdong, accounting for 72% of all the year round; Typhoon in Guangdong showed the tendency of reduced from west to east; Form 2008 to 2010, transmission line tripped 50 times caused by typhoon, and distribution circuit tripped 710 times in Jiangmen; The main reasons of breakdown are the mechanical overload, the flashover caused by wind age yaw and the reduction of air gap discharge voltage caused by lightning. This paper proposes to strengthen the early warning of typhoon, improve the design standard of transmission/ distribution line and develop new type tower material further study. Introduction Guangdong is located in the main path for northwest Pacific Ocean tropical cyclone and South China Sea tropical cyclone to land in China [1], which is one of the provinces suffering from the worst typhoon disaster. -
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 Haiyan
Emergency appeal Philippines: Typhoon Haiyan Emergency appeal n° MDRPH014 GLIDE n° TC-2013-000139-PHL 12 November 2013 This emergency appeal is launched on a preliminary basis for CHF 72,323,259 (about USD 78,600,372 or EUR 58,649,153) seeking cash, kind or services to cover the immediate needs of the people affected and support the Philippine Red Cross in delivering humanitarian assistance to 100,000 families (500,000 people) within 18 months. This includes CHF 761,688 to support its role in shelter cluster coordination. The IFRC is also soliciting support from National Societies in the deployment of emergency response units (ERUs) at an estimated value of CHF 3.5 million. The operation will be completed by the end of June 2015 and a final report will be made available by 30 September 2015, three months after the end Red Cross staff and volunteers were deployed as soon as safety conditions allowed, of the operation. to assess conditions and ensure that those affected by Typhoon Haiyan receive much-needed aid. Photo: Philippine Red Cross CHF 475,495 was allocated from the International Federation of Red Cross and Red Crescent Societies (IFRC) Disaster Relief Emergency Fund (DREF) on 8 November 2013 to support the National Society in undertaking delivering immediate assistance to affected people and undertaking needs assessments. Un-earmarked funds to replenish DREF are encouraged. Summary Typhoon Haiyan (locally known as Yolanda) made landfall on 8 November 2013 with maximum sustained winds of 235 kph and gusts of up to 275 kph. The typhoon and subsequent storm surges have resulted in extensive damage to infrastructure, making access a challenge. -
Hkmets Bulletin, Volume 17, 2007
ISSN 1024-4468 The Hong Kong Meteorological Society Bulletin is the official organ of the Society, devoted to articles, editorials, news and views, activities and announcements of the Society. SUBSCRIPTION RATES Members are encouraged to send any articles, media items or information for publication in the Bulletin. For guidance Institutional rate: HK$ 300 per volume see the information for contributors in the inside back cover. Individual rate: HK$ 150 per volume Advertisements for products and/or services of interest to members of the Society are accepted for publication in the BULLETIN. For information on formats and rates please contact the Society secretary at the address opposite. The BULLETIN is copyright material. Views and opinions expressed in the articles or any correspondence are those Published by of the author(s) alone and do not necessarily represent the views and opinions of the Society. Permission to use figures, tables, and brief extracts from this publication in any scientific or educational work is hereby granted provided that the source is properly acknowledged. Any other use of the material requires the prior written The Hong Kong Meteorological Society permission of the Hong Kong c/o Hong Kong Observatory Meteorological Society. 134A Nathan Road Kowloon, Hong Kong The mention of specific products and/or companies does not imply there is any Homepage endorsement by the Society or its office bearers in preference to others which are http:www.meteorology.org.hk/index.htm not so mentioned. Contents Scientific Basis of Climate Change 2 LAU Ngar-cheung Temperature projections in Hong Kong based on IPCC Fourth Assessment Report 13 Y.K. -
NASA Identifies Heavy Rainfall in South China Sea's Typhoon Utor 13 August 2013, by Rob Gutro
NASA identifies heavy rainfall in South China Sea's Typhoon Utor 13 August 2013, by Rob Gutro Visible and InfraRed Scanner (VIRS) at NASA's Goddard Space Flight Center in Greenbelt, Md. TRMM PR found rain falling at a rate of over 73mm/~2.9 inches per hour in well-defined thunderstorm feeder bands extending over the South China Sea. TRMM PR also found that heavy rain in these lines of rain were returning radar reflectivity values greater than 50.5 dBZ. When Utor was exiting the Philippines yesterday, Aug. 12, the storm's maximum sustained winds had fallen to 85 knots/97.8 mph/157.4 kph. By Aug. 13 at 1500 UTC/11 a.m. EDT the warm waters of the South China Sea had helped strengthen Utor, and maximum sustained winds were near 95 knots/109.3 mph/175.9 kph. Utor's center is located near 19.5 north and 113.1 east, about 190 nautical miles south- southwestward of Hong Kong. Utor is moving to the west-northwestward at 6 knots/7 mph/11.1 kph. Utor's powerful winds are generating very high, and NASA's TRMM satellite captured rainfall rates of over 73mm/hr (~2.9 inches) happening in Typhoon Utor on rough seas. Maximum significant wave heights Aug. 12 at 2:21 a.m. EDT as it was exiting the were reported near 41 feet/12.5 meters. Philippines into the South China Sea. Credit: SSAI/NASA, Hal Pierce Although Utor's winds had increased since yesterday, animated enhanced infrared satellite imagery today showed that the convective (rising air that forms the thunderstorms that make up the As Typhoon Utor was exiting the northwestern tropical cyclone) structure of the system has started Philippines, NASA's TRMM satellite passed to weaken, according to the Joint Typhoon Warning overhead and detected some heavy rainfall in Center or JTWC. -
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. -
Basic Data Construction for a Typhoon Disaster Prevention Model : Monthly Characteristics of Typhoon Rusa, Maemi, Kompasu, and Bolaven
AAS02-P10 Japan Geoscience Union Meeting 2019 Basic Data Construction for a Typhoon Disaster Prevention Model : Monthly Characteristics of Typhoon Rusa, Maemi, Kompasu, and Bolaven *HANA NA1, Woo-Sik Jung1 1. Department of Atmospheric Environment Information Engineering, Atmospheric Environment Information Research Center, Inje University, Gimhae 50834, Korea According to a typhoon report that summarized the typhoons that had affected the Korean Peninsula for approximately 100 years since the start of weather observation in the Korean Peninsula, the number of typhoons that affected the Korean Peninsula was the highest in August, followed by July, and September. A study that analyzed the period between 1953 and 2003 revealed that the number of typhoons that affected the Korean Peninsula was 62 in August, 49 in July, and 45 in September. As shown, previous studies that analyzed the typhoons that affected the Korean Peninsula by month were primarily focused on the impact frequency. This study aims to estimate the monthly impact frequency of the typhoons that affected the Korean Peninsula as well as the maximum wind speed that accompanied the typhoons. It also aims to construct the basic data of a typhoon disaster prevention model by estimating the maximum wind speed during typhoon period using Typhoon Rusa that resulted in the highest property damage, Typhoon Maemi that recorded the maximum wind speed, Typhoon Kompasu that significantly affected the Seoul metropolitan area, and Typhoon Bolaven that recently recorded severe damages. A typhoon disaster prevention model was used to estimate the maximum wind speed of the 3-second gust that may occur, and the 700 hPa wind speed estimated through WRF(Weather Research and Forecasting) numerical simulation was used as input data. -
Typhoon Haiyan
Information Bulletin Philippines: Typhoon Haiyan Information bulletin n° 1 7 November 2013 This bulletin is being issued for information only and reflects the current situation and details available at Text box for brief photo caption. Example: In February 2007, the this time. The Philippine Red Cross has placed its disaster response teams on standby for rapid Colombian Red Cross Society distributed urgently needed deployment and preparedness stocks ready for dispatch, if required. materials after the floods and slides in Cochabamba. IFRC (Arial 8/black colour) Summary: Typhoon Haiyan is currently making its way across the Pacific and has intensified into a category 5 typhoon (super typhoon). Forecasts indicate Typhoon Haiyan will make landfall in the Philippines on Friday, 8 November 2013. Known locally as Typhoon Yolanda, Haiyan is expected to track across Samar and Leyte provinces in Eastern Visayas region, packing maximum sustained winds of 240 kph (150 mph). It is expected to bring widespread torrential rain and damaging winds, and trigger life- threatening flash floods, as well as mudslides on higher terrain. The Philippine Red Cross (PRC) has been on highest alert since the Preparedness stocks – which include standard relief items – are being transferred typhoon was sighted. The PRC is from the Philippine Red Cross central warehouse in Manila to a regional maintaining close coordination with warehouse in Cebu for immediate dispatch to areas where they will be needed. disaster authorities and has alerted Photo: Joe Cropp/IFRC all its chapters in Visayas (Central, Eastern and Western Visayas) as well as in Bicol, Mindoro, and Caraga regions for immediate response, if required. -
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. -
Research Article Application of Buoy Observations in Determining Characteristics of Several Typhoons Passing the East China Sea in August 2012
Hindawi Publishing Corporation Advances in Meteorology Volume 2013, Article ID 357497, 6 pages http://dx.doi.org/10.1155/2013/357497 Research Article Application of Buoy Observations in Determining Characteristics of Several Typhoons Passing the East China Sea in August 2012 Ningli Huang,1 Zheqing Fang,2 and Fei Liu1 1 Shanghai Marine Meteorological Center, Shanghai, China 2 Department of Atmospheric Science, Nanjing University, Nanjing, China Correspondence should be addressed to Zheqing Fang; [email protected] Received 27 February 2013; Revised 5 May 2013; Accepted 21 May 2013 Academic Editor: Lian Xie Copyright © 2013 Ningli Huang et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. The buoy observation network in the East China Sea is used to assist the determination of the characteristics of tropical cyclone structure in August 2012. When super typhoon “Haikui” made landfall in northern Zhejiang province, it passed over three buoys, the East China Sea Buoy, the Sea Reef Buoy, and the Channel Buoy, which were located within the radii of the 13.9 m/s winds, 24.5 m/s winds, and 24.5 m/s winds, respectively. These buoy observations verified the accuracy of typhoon intensity determined by China Meteorological Administration (CMA). The East China Sea Buoy had closely observed typhoons “Bolaven” and “Tembin,” which provided real-time guidance for forecasters to better understand the typhoon structure and were also used to quantify the air-sea interface heat exchange during the passage of the storm. -
Influence of Sea Salt Aerosols on the Development of Mediterranean
Atmos. Chem. Phys., 21, 13353–13368, 2021 https://doi.org/10.5194/acp-21-13353-2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Influence of sea salt aerosols on the development of Mediterranean tropical-like cyclones Enrique Pravia-Sarabia1, Juan José Gómez-Navarro1, Pedro Jiménez-Guerrero1,2, and Juan Pedro Montávez1 1Physics of the Earth, Regional Campus of International Excellence (CEIR) “Campus Mare Nostrum”, University of Murcia, 30100 Murcia, Spain 2Biomedical Research Institute of Murcia (IMIB-Arrixaca), 30120 Murcia, Spain Correspondence: Juan Pedro Montávez ([email protected]) Received: 23 December 2020 – Discussion started: 11 February 2021 Revised: 26 July 2021 – Accepted: 16 August 2021 – Published: 9 September 2021 Abstract. Medicanes are mesoscale tropical-like cyclones 1 Introduction that develop in the Mediterranean basin and represent a great hazard for the coastal population. The skill to accurately simulate them is of utmost importance to prevent econom- Mediterranean tropical-like cyclones, also known as medi- ical and personal damage. Medicanes are fueled by the la- canes (from mediterranean hurricanes), are mesoscale per- tent heat released in the condensation process associated turbations that exhibit tropical characteristics, such as an with convective activity, which is regulated by the pres- eye-like feature and warm core. These storms are character- ence and activation of cloud condensation nuclei, mainly ized by high wind speeds and vertically aligned geopoten- originating from sea salt aerosols (SSAs) for marine envi- tial height perturbations along different pressure levels. Just ronments. Henceforth, the purpose of this contribution is like regular tropical cyclones, medicanes represent a hazard twofold: assessing the effects of an interactive calculation of for the population of coastal areas.