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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. -
A Numerical Study on Rapid Intensification of Typhoon Vicente
MARCH 2017 C H E N E T A L . 877 A Numerical Study on Rapid Intensification of Typhoon Vicente (2012) in the South China Sea. Part I: Verification of Simulation, Storm-Scale Evolution, and Environmental Contribution XIAOMIN CHEN Key Laboratory for Mesoscale Severe Weather/MOE and School of Atmospheric Sciences, Nanjing University, Nanjing, China, and International Pacific Research Center, and Department of Atmospheric Sciences, School of Ocean and Earth Science and Technology, University of Hawai‘i at Manoa, Honolulu, Hawaii YUQING WANG International Pacific Research Center, and Department of Atmospheric Sciences, School of Ocean and Earth Science and Technology, University of Hawai‘i at Manoa, Honolulu, Hawaii KUN ZHAO Key Laboratory for Mesoscale Severe Weather/MOE and School of Atmospheric Sciences, Nanjing University, Nanjing, China DAN WU Shanghai Typhoon Institute, China Meteorological Administration, Shanghai, China (Manuscript received 14 April 2016, in final form 3 December 2016) ABSTRACT Typhoon Vicente (2012) underwent an extreme rapid intensification (RI) over the northern South China Sea just before its landfall in south China. The extreme RI, the sudden track deflection, and the inner- and outer-core structures of Vicente were reasonably reproduced in an Advanced Research version of the Weather Research and Forecasting (WRF-ARW) Model simulation. The evolutions of the axisymmetric inner-core radar reflectivity and the primary circulation of the simulated Vicente before its landfall were verified against the Doppler radar observations. Two intensification stages were identified: 1) the asymmetric intensification stage (i.e., RI onset), repre- sented by a relatively slow intensification rate accompanied by a distinct eyewall contraction; and 2) the axisymmetric RI stage with very slow eyewall contraction. -
Formation of Winter Supertyphoons Haiyan (2013) and Hagupit (2014)
3800 IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, VOL. 55, NO. 7, JULY 2017 Formation of Winter Supertyphoons Haiyan (2013) and Hagupit (2014) Through Interactions With Cold Fronts as Observed by Multifunctional Transport Satellite Yung-Sheng Lee, Member, IEEE, Yuei-An Liou, Senior Member, IEEE, Ji-Chyun Liu, Ching-Tsan Chiang, and Kuan-Dih Yeh Abstract— This paper incorporates remote sensing imagery prevention [1], [2]. The satellite data that provide cloud images and image processing techniques to analyze typhoons’ evolution may be used to analyze the cloud structure and dynamics of into supertyphoons through interactions with cold fronts in the typhoons [3]–[8]. When two tropical cyclones (TCs) are close Western Pacific Ocean. The purpose is to enhance understanding and predictability of the tracks and profiles of supertyphoons. to some extent, they affect and interact with each other. Such Evolutions of typhoons Haiyan (2013) and Hagupit (2014) into cyclone–cyclone interaction is known as “Fujiwhara effect” supertyphoons were studied. The 3-D profiles of weather systems in honor of pioneer Fujiwhara [9]. Several types of cyclone– were reconstructed using multifunctional transport satellite IR cyclone interactions were studied [10]–[12]. The distance cloud images. When interactions between typhoon and cold front between two typhoons, and intensity and translation speeds of happened, enhancements of typhoons were observed causing typhoons Haiyan and Hagupit to strengthen power and evolve the binary typhoons were investigated recently. The impacts into supertyphoons. The origins of typhoons Haiyan and Hagupit of binary typhoons on the upper ocean environments that were are closely located at 152°50E/05°12N and 151°30E/04°19N, explored included physical and biological environments [12]. -
Big Data in Geoinformatics
GIS Karimi Techniques and Technologies Big Data in Geoinformatics Big data has always been a major challenge in geoinformatics as geospatial data come in various types and formats, new geospatial data are acquired very fast, and geospatial Big Data databases are inherently very large. And while there have been advances in hardware and software for handling big data, they often fall short of handling geospatial big data efficiently and effectively. Big Data: Techniques and Technologies in Techniques and Technologies Geoinformatics tackles these challenges head on, integrating coverage of techniques and technologies for storing, managing, and computing geospatial big data. in Geoinformatics Providing a perspective based on analysis of time, applications, and resources, this book familiarizes readers with geospatial applications that fall under the category of big data. It explores new trends in geospatial data collection, such as geo- BIG DATA crowdsourcing and advanced data collection technologies such as LiDAR point clouds. The book features a range of topics on big data techniques and technologies in geoinformatics including distributed computing, geospatial data analytics, social media, and volunteered geographic information. Features Edited by • Explains the challenges and issues of big data in geoinformatics applications • Discusses and analyzes the techniques, technologies, and tools for storing, Hassan A. Karimi managing, and computing geospatial big data • Familiarizes the readers with the advanced techniques and technologies used for geospatial big data research • Provides insight into new opportunities offered by geospatial big data With chapters contributed by experts in geoinformatics and in domains such as computing and engineering, the book provides an understanding of the challenges and issues of big data in geoinformatics applications. -
1St WMO International Conference on Indian Ocean Tropical Cyclones and Climate Change, Muscat, Sultanate of Oman, 8-11 March 2009
WWRP 2010 - 2 1st WMO International Conference on Indian Ocean Tropical Cyclones and Climate Change, Muscat, Sultanate of Oman, 8-11 March 2009 For more information, please contact: World Meteorological Organization Research Department Atmospheric Research and Environment Branch 7 bis, avenue de la Paix – P.O. Box 2300 – CH 1211 Geneva 2 – Switzerland Tel.: +41 (0) 22 730 83 14 – Fax: +41 (0) 22 730 80 27 E-mail: [email protected] – Website: http://www.wmo.int/pages/prog/arep/index_en.html WMO/TD - No. 1541 © World Meteorological Organization, 2010 The right of publication in print, electronic and any other form and in any language is reserved by WMO. Short extracts from WMO publications may be reproduced without authorization, provided that the complete source is clearly indicated. Editorial correspondence and requests to publish, reproduce or translate these publication in part or in whole should be addressed to: Chairperson, Publications Board World Meteorological Organization (WMO) 7 bis, avenue de la Paix Tel.: +41 (0) 22 730 84 03 P.O. Box 2300 Fax: +41 (0) 22 730 80 40 CH-1211 Geneva 2, Switzerland E-mail: [email protected] NOTE The designations employed in WMO publications and the presentation of material in this publication do not imply the expression of any opinion whatsoever on the part of the Secretariat of WMO concerning the legal status of any country, territory, city or area, or of its authorities, or concerning the delimitation of its frontiers or boundaries. Opinions expressed in WMO publications are those of the authors and do not necessarily reflect those of WMO. -
Significant Data on Major Disasters Worldwide, 1900-Present
DISASTER HISTORY Signi ficant Data on Major Disasters Worldwide, 1900 - Present Prepared for the Office of U.S. Foreign Disaster Assistance Agency for International Developnent Washington, D.C. 20523 Labat-Anderson Incorporated Arlington, Virginia 22201 Under Contract AID/PDC-0000-C-00-8153 INTRODUCTION The OFDA Disaster History provides information on major disasters uhich have occurred around the world since 1900. Informtion is mare complete on events since 1964 - the year the Office of Fore8jn Disaster Assistance was created - and includes details on all disasters to nhich the Office responded with assistance. No records are kept on disasters uhich occurred within the United States and its territories.* All OFDA 'declared' disasters are included - i.e., all those in uhich the Chief of the U.S. Diplmtic Mission in an affected country determined that a disaster exfsted uhich warranted U.S. govermnt response. OFDA is charged with responsibility for coordinating all USG foreign disaster relief. Significant anon-declared' disasters are also included in the History based on the following criteria: o Earthquake and volcano disasters are included if tbe mmber of people killed is at least six, or the total nmber uilled and injured is 25 or more, or at least 1,000 people art affect&, or damage is $1 million or more. o mather disasters except draught (flood, storm, cyclone, typhoon, landslide, heat wave, cold wave, etc.) are included if the drof people killed and injured totals at least 50, or 1,000 or mre are homeless or affected, or damage Is at least S1 mi 1l ion. o Drought disasters are included if the nunber affected is substantial. -
Communication: Mass Media and the Science of Disasters
MONTEMAYOR AND CUSTODIO COMMUNICATING RISKS 39 Kasarinlan: Philippine Journal of Third World Studies 2014 29 (2): 39–74 Communicating Risks, Risking (Mis)communication: Mass Media and the Science of Disasters GARRY JAY S. MONTEMAYOR AND PAMELA A. CUSTODIO ABSTRACT. The experience brought about by super typhoon Yolanda (internationally known as Haiyan) in November 2013 highlights the need to look into how we can improve ways of communicating risks and the science about natural hazards in national and local settings. This paper attempts to highlight the value of risk and science communication in national and local disaster mitigation and management. After analyzing the preparations done before super typhoon Yolanda’s landfall using extant documents from the national government and different government agencies, weather forecast news published in newspapers and broadcasted on TV, and other several post- Haiyan scholarly literatures, we examine emergent communication-related issues to come up with recommendations toward mainstreaming risk and science communication in the country. This study found out that the government as well as the experts engaged in concerted efforts to prepare the citizens for the typhoon; and that the media did attempt to communicate risks and science before the typhoon’s landfall. However, problems involving (1) psychological and social factors; (2) information dissemination through mass media; and (3) institutional mechanisms in disaster risk reduction provided by the government emerged, which have serious implications on how we shall mitigate disasters in the future. KEYWORDS. science communication · risk communication · science and the media · Haiyan · public understanding of science INTRODUCTION One of the most daunting tasks of a communicator involved in disaster preparedness and management is to communicate hazards and its potential risks—including the science behind these—to vulnerable communities. -
National Park Service Assateague Island National Seashore 2019 Hurricane and Coastal Storm Plan
National Park Service Assateague Island National Seashore 2019 Hurricane and Coastal Storm Plan Updated & Reviewed by: ______________________________ Date: ___6/4/19_____ E. Walter West Incident Commander Updated & Reviewed by: Date: ___6/10/19___ Deborah A. Darden Superintendent TABLE OF CONTENTS SECTION: TITLE PAGE Hurricane and tropical storm forecasts 1 I Introduction and Mission 1 II. Hurricane Plan Distribution and Definitions 2-3 III. Description of conditions 4 IV. Legal Authorities 6 V. Situation discussions 7 VI. Chain of Command 7-8 VII. ICS Operational Objectives 9-23 Appendix A NPS Incident Command Organization 24 Appendix B USFWS Incident Command Organization-Major Response 25 Appendix C USFWS Incident Command Organization-Minor Response 26 Appendix D NPS Delegation of Authority 27-28 Appendix E Useful Links & Contact Numbers 29-37 Appendix F Hurricane Shelter Information 38 Appendix G Division Checklists, Sensitive items 39-40 Appendix H Town of Chincoteague, Causeway closure SOP 41-43 Appendix I Glossary: National Hurricane Center glossary of terms 44-49 Appendix J Operational Charts to 5 days out from storm 50-64 EXTENDED RANGE FORECAST OF ATLANTIC SEASONAL HURRICANE ACTIVITY AND LANDFALL STRIKE PROBABILITY FOR 2019 (CSU Tropical Meteorology Project) We have increased our forecast slightly and now believe that 2019 will have approximately average activity. There remains considerable uncertainty as to whether El Niño conditions will persist through the Atlantic hurricane season. The tropical Atlantic has warmed slightly faster than normal over the past few weeks and now has near average sea surface temperatures. We anticipate a near-average probability for major hurricanes making landfall along the United States coastline and in the Caribbean. -
A Numerical Study on Rapid Intensification of Typhoon Vicente
MARCH 2017 C H E N E T A L . 877 A Numerical Study on Rapid Intensification of Typhoon Vicente (2012) in the South China Sea. Part I: Verification of Simulation, Storm-Scale Evolution, and Environmental Contribution XIAOMIN CHEN Key Laboratory for Mesoscale Severe Weather/MOE and School of Atmospheric Sciences, Nanjing University, Nanjing, China, and International Pacific Research Center, and Department of Atmospheric Sciences, School of Ocean and Earth Science and Technology, University of Hawai‘i at Manoa, Honolulu, Hawaii YUQING WANG International Pacific Research Center, and Department of Atmospheric Sciences, School of Ocean and Earth Science and Technology, University of Hawai‘i at Manoa, Honolulu, Hawaii KUN ZHAO Key Laboratory for Mesoscale Severe Weather/MOE and School of Atmospheric Sciences, Nanjing University, Nanjing, China DAN WU Shanghai Typhoon Institute, China Meteorological Administration, Shanghai, China (Manuscript received 14 April 2016, in final form 3 December 2016) ABSTRACT Typhoon Vicente (2012) underwent an extreme rapid intensification (RI) over the northern South China Sea just before its landfall in south China. The extreme RI, the sudden track deflection, and the inner- and outer-core structures of Vicente were reasonably reproduced in an Advanced Research version of the Weather Research and Forecasting (WRF-ARW) Model simulation. The evolutions of the axisymmetric inner-core radar reflectivity and the primary circulation of the simulated Vicente before its landfall were verified against the Doppler radar observations. Two intensification stages were identified: 1) the asymmetric intensification stage (i.e., RI onset), repre- sented by a relatively slow intensification rate accompanied by a distinct eyewall contraction; and 2) the axisymmetric RI stage with very slow eyewall contraction. -
The Origin of "Fujiwhara Effect": the Typhoons Postponed the End of World War II
17th History Symposium, 99th American Meteorological Society Annual Meeting, Phoenix, AZ , 7 January 2019 204 The origin of "Fujiwhara effect": The Typhoons Postponed the End of World War II Akira Yamamoto Meteorological Research Institute Japan Meteorological Agency Meteorological Research Institute / Japan Meteorological Agency 気象研究所 17th History Symposium, 99th American Meteorological Society Annual Meeting, Phoenix, AZ , 7 January 2019 2 Summary • The origin of "Fujiwhara effect“ was investigated by bibliographic survey. The following hypothesis suggested. • "Fujiwhara effect“ is NOT the effect suggested by Japanese meteorologist Sakuhei Fujiwhara (1884-1950). – It was theoretically derived initially by Japanese meteorologist Diro Kitao (1853-1907) in his paper Kitao (1889). – Bernhard Haurzitz (1905-1986) analyzed detailed motion of two typhoons in late August 1945 with input from Herbert Riehl (1915-1997) , and confirmed his theory of two cyclone rotation based on Kitao (1889). 2014/5/22 日本気象学会春季大会 Meteorological Research Institute / Japan Meteorological Agency 山本「世界各国における地上気象観測環境基準の現状」 気象研究所 17th History Symposium, 99th American Meteorological Society Annual Meeting, Phoenix, AZ , 7 January 2019 3 Summary(cont.) • The word of "Fujiwhara effect“ was generated very finely timed in the closing days of World War II. – Damage to U.S. forces during WW II by typhoons was a motive that they established a accurate typhoon tracking in North West Pacific. – Kitao’s theory of two cyclone rotation was initially demonstrated by motion of two typhoons (Susan and Ruth in U.S. name) in late August 1945, that progressed slowly in the western Pacific between Okinawa and the main Japanese islands interacting each other. 2014/5/22 日本気象学会春季大会 Meteorological Research Institute / Japan Meteorological Agency 山本「世界各国における地上気象観測環境基準の現状」 気象研究所 17th History Symposium, 99th American Meteorological Society Annual Meeting, Phoenix, AZ , 7 January 2019 4 Summary(cont.) – It was believed that these typhoons postponed McArthur's occupation plan of Japan for 48 hours. -
Report for Typhoon
Country Report ( 2007 ) For the 40th Session of the Typhoon Committee ESCAP/WMO Macao, China 21–26 November 2007 People’s Republic of China 1 I. Overview of Meteorological and Hydrological Conditions 1. Meteorological Assessment From Oct. 1st 2006 to Sep. 30th 2007, altogether 23 tropical cyclones (including tropical storms, severe tropical storms, typhoons, severe typhoons and super typhoons) formed over the Western North Pacific and the South China Sea (Fig. 1.1). Among them, 8 TCs formed from Oct. 1st to Dec. 31st in 2006 and 4 of them affected China’s coastal waters but didn’t land on China’s coastal areas. They were super typhoon Cimaron (0619), super typhoon Chebi 0620), super typhoon Durian (0621) and severe typhoon Utor (0622). In 2007, 15 tropical cyclones formed over the Western North Pacific and the South China Sea. The number was obviously less than the average (19.7) during the corresponding period from 1949 to 2006. And 9 of them developed into typhoons or beyond, which accounted for 60.0% of the total. The percentage was higher than the average (58.6%). During the same period, 4 TCs formed over the South China Sea. The number was slightly less than the average (4.7). Moreover, 6 TCs made landfalls over China coastal areas, all of them exceed tropical storm category. They were tropical storm Toraji (0703), severe tropical storm Pabuk 0706), tropical storm Wupit 0707), super typhoon Sepat (0708), super typhoon Wipha 0712) and tropical storm Francisco (0713). The total landed TC number was slightly less than the average (about 6.79), but the percentage of landed TCs (40.0%) was obviously above the average (30.8%). -
Tropical Cyclone Motion Due to Environmental Interactions Represented by Empirical Orthogonal Functions of the Vorticity Fields
Calhoun: The NPS Institutional Archive Theses and Dissertations Thesis Collection 1991-06 Tropical cyclone motion due to environmental interactions represented by empirical orthogonal functions of the vorticity fields. Gunzelman, Mark J. Monterey, California. Naval Postgraduate School http://hdl.handle.net/10945/26819 NAVAL POSTGRADUATE SCHOOL Monterey , California THESIS TROPICAL CYCLONE MOTION DUE TO ENVIRONMENTAL INTERACTIONS REPRESENTED BY EMPIRICAL ORTHOGONAL FUNCTIONS OF THE VORTICITY FIELDS by Mark J. Gunzelman June 1991 Thesis Advisor: Russell L. Elsberry Approved for public release; distribution unlimited T256203 Unclassified SECURITY CLASSIFICATION OF THIS PAGE Form Appiovi '/ REPORT DOCUMENTATION PAGE OMB No 0704 01 fid la HH'OKT SECURITY CI ASSIFK ATION lb RESTRK IIVE MARKIMCiS Unclassified 2a SECURITY CLASSIFICATION AUTHORITY 3 DISTRIBUTION /AVAH ARIliTY OF REPORT Approved for public release; distribution 2b DECLASSIFICATION /DOWNGRADING SCHEDULE is unlimited. 4 PERFORMING ORGANIZATION REPORT NUMBER(S) 5 MONITORING ORGANIZATION REPORT NUMBER(S) 6a NAME OF PERFORMING ORGANIZATION 6b OFFICE SYMBOL 7a NAME OF MONITORING ORGANIZATION Naval Postgraduate School (If applicable) Naval Postgraduate School 35 6c ADDRESS {City, State, and ZIP Code) 7b ADDRESS (C/fy, State, and IIP Code) Monterey, CA 93943-5000 Monterey, CA 93943-5000 ia NAME OF FUNDING /SPONSORING 8b OFFICE SYMBOL 9 PROCUREMENT INSTRUMENT IDENTIFICATION NUMBER ORGANIZATION (If applicable) 8c ADDRESS (City, State, and ZIP Code) 10 SOURCE OF FUNDING NUMBERS PROGRAM PROJECT