Atlantic Hurricane Season Outlook for June 2020
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Fishing Pier Design Guidance Part 1
Fishing Pier Design Guidance Part 1: Historical Pier Damage in Florida Ralph R. Clark Florida Department of Environmental Protection Bureau of Beaches and Coastal Systems May 2010 Table of Contents Foreword............................................................................................................................. i Table of Contents ............................................................................................................... ii Chapter 1 – Introduction................................................................................................... 1 Chapter 2 – Ocean and Gulf Pier Damages in Florida................................................... 4 Chapter 3 – Three Major Hurricanes of the Late 1970’s............................................... 6 September 23, 1975 – Hurricane Eloise ...................................................................... 6 September 3, 1979 – Hurricane David ........................................................................ 6 September 13, 1979 – Hurricane Frederic.................................................................. 7 Chapter 4 – Two Hurricanes and Four Storms of the 1980’s........................................ 8 June 18, 1982 – No Name Storm.................................................................................. 8 November 21-24, 1984 – Thanksgiving Storm............................................................ 8 August 30-September 1, 1985 – Hurricane Elena ...................................................... 9 October 31, -
Hurricane & Tropical Storm
5.8 HURRICANE & TROPICAL STORM SECTION 5.8 HURRICANE AND TROPICAL STORM 5.8.1 HAZARD DESCRIPTION A tropical cyclone is a rotating, organized system of clouds and thunderstorms that originates over tropical or sub-tropical waters and has a closed low-level circulation. Tropical depressions, tropical storms, and hurricanes are all considered tropical cyclones. These storms rotate counterclockwise in the northern hemisphere around the center and are accompanied by heavy rain and strong winds (NOAA, 2013). Almost all tropical storms and hurricanes in the Atlantic basin (which includes the Gulf of Mexico and Caribbean Sea) form between June 1 and November 30 (hurricane season). August and September are peak months for hurricane development. The average wind speeds for tropical storms and hurricanes are listed below: . A tropical depression has a maximum sustained wind speeds of 38 miles per hour (mph) or less . A tropical storm has maximum sustained wind speeds of 39 to 73 mph . A hurricane has maximum sustained wind speeds of 74 mph or higher. In the western North Pacific, hurricanes are called typhoons; similar storms in the Indian Ocean and South Pacific Ocean are called cyclones. A major hurricane has maximum sustained wind speeds of 111 mph or higher (NOAA, 2013). Over a two-year period, the United States coastline is struck by an average of three hurricanes, one of which is classified as a major hurricane. Hurricanes, tropical storms, and tropical depressions may pose a threat to life and property. These storms bring heavy rain, storm surge and flooding (NOAA, 2013). The cooler waters off the coast of New Jersey can serve to diminish the energy of storms that have traveled up the eastern seaboard. -
Florida Hurricanes and Tropical Storms
FLORIDA HURRICANES AND TROPICAL STORMS 1871-1995: An Historical Survey Fred Doehring, Iver W. Duedall, and John M. Williams '+wcCopy~~ I~BN 0-912747-08-0 Florida SeaGrant College is supported by award of the Office of Sea Grant, NationalOceanic and Atmospheric Administration, U.S. Department of Commerce,grant number NA 36RG-0070, under provisions of the NationalSea Grant College and Programs Act of 1966. This information is published by the Sea Grant Extension Program which functionsas a coinponentof the Florida Cooperative Extension Service, John T. Woeste, Dean, in conducting Cooperative Extensionwork in Agriculture, Home Economics, and Marine Sciences,State of Florida, U.S. Departmentof Agriculture, U.S. Departmentof Commerce, and Boards of County Commissioners, cooperating.Printed and distributed in furtherance af the Actsof Congressof May 8 andJune 14, 1914.The Florida Sea Grant Collegeis an Equal Opportunity-AffirmativeAction employer authorizedto provide research, educational information and other servicesonly to individuals and institutions that function without regardto race,color, sex, age,handicap or nationalorigin. Coverphoto: Hank Brandli & Rob Downey LOANCOPY ONLY Florida Hurricanes and Tropical Storms 1871-1995: An Historical survey Fred Doehring, Iver W. Duedall, and John M. Williams Division of Marine and Environmental Systems, Florida Institute of Technology Melbourne, FL 32901 Technical Paper - 71 June 1994 $5.00 Copies may be obtained from: Florida Sea Grant College Program University of Florida Building 803 P.O. Box 110409 Gainesville, FL 32611-0409 904-392-2801 II Our friend andcolleague, Fred Doehringpictured below, died on January 5, 1993, before this manuscript was completed. Until his death, Fred had spent the last 18 months painstakingly researchingdata for this book. -
Hurricane Risk Perception, Preparedness, And
The Pennsylvania State University The Graduate School College of Earth and Mineral Sciences HURRICANE RISK PERCEPTION, PREPAREDNESS, AND EVACUATION INTENTION AMONG OLDER ADULTS A Dissertation in Geography by Chongming Wang © 2016 Chongming Wang Submitted in Partial Fulfillment of the Requirements for the Degree of Doctoral of Philosophy August 2016 ! The dissertation of Chongming Wang was reviewed and approved* by the following: Brent Yarnal Professor of Geography Dissertation Advisor Chair of Committee Alexander Klippel Professor of Geography John Kelmelis Professor of of International Affairs Steven Zarit Professor of Human Development and Family Studies Cynthia Brewer Professor of Geography Head of the Department of Geography *Signatures are on file in the Graduate School. ! ABSTRACT Vulnerability of older adults in all stages of a disaster is well recognized by both scholars and practitioners. However, most relevant empirical research to date has focused on disaster recovery and reconstruction, leaving unanswered the “how” and “why” questions surrounding disaster preparedness and response among older people. The older people’s perceptions of natural hazard risks have been even less explored. To address these research gaps, this study uses a case study of older residents of Sarasota County, Florida and applies a qualitative method to understand the perception, preparedness, and evacuation intention of older people at risk from hurricane hazards. The individual in-depth interviews generate several findings. First, while older residents’ knowledge of hurricane threats varied from simple to sophisticated, their perceptions of hurricane risks were predominantly low due to a local myth and hurricane quiescence in recent memory. Second, most older residents took generic actions by preparing extra water, food, and medications, but lacked efforts in more hurricane-specific preparedness due to complacency and lack of awareness, financial capital, and social capital. -
Downloaded 09/28/21 10:59 AM UTC 1 76 MONTHLY WEATHER REVIEW Vol
March 1965 Gordon E. Dunn and Staff 175 THEHURRICANE SEASON OF 1964 GORDON E. DUNN AND STAFF* U.S. Weather Bureau Office, Miami, Fla. 1. GENERALSUMMARY spondvery well withthe composite chart for atverage Twelvetropical cyclones,six of hurricaneintensity, departures from nornml for seasons of maxinlum tropical developedover tropical Atlantic waters during 1964. cycloneincidence inthe southeastern United States as This is the largest number since 1955 and compares with developed by Ballenzweig [a]. an average of 10during the past three decades. The September was aneven more active month and cor- centers of four hurricanes penetrated the mainland of the respondence between Ballenzweig'scomposite chrt and United States, the largest number to do so since the five theobserved values was better, particularly south of in 1933. There have been only four other years with four latitude 40' W. According toGreen [3] thesubtropical or more since 1900; four in 1906, 1909, and 1926, and six High was abnornlallystrong and displacedslightly in 1916.While none of thefour renching the mainland northwardfrom normal (favorable for tropical cyclone in 1964 wits :L major hurricane at the time of landfall, formation) while the 700-mb. jet was slightlysouth of three-Cleo, Dora, and EIi1da"were severe. normal (unfavorable). The long-wave position fluctuated Florida was struck by three hurricanes in addition to back and forth from the Rockies and Great Plains east- dyinghurricane Hilda and one tropical cyclone of less ward and the tropical cyclones experienced considerable than hurricane intensity; thus ended an unequalled rela- difficulty in penetrating the westerlies. During the major tively hurricane-free period of 13 years from 1951 through hurricanemonths in 1964 the long-wavetrough failed 1963. -
Volume 1-3 North Central Florida Region Technical Data Report
Volume 1-3 North Central Florida Region Technical Data Report CHAPTER II REGIONAL HAZARDS ANALYSIS This page intentionally left blank. Statewide Regional Evacuation Studies Program Volume 1-3 North Central Florida Table of Contents CHAPTER II REGIONAL HAZARDS ANALYSIS .................................................................... 1 A. Hazards Identification and Risk Assessment ........................................................................ 1 1. Frequency of Occurrence .................................................................................................... 1 2. Vulnerability Factors ............................................................................................................ 1 3. Vulnerability Impact Areas .................................................................................................. 1 B. Coastal Storms and Hurricanes .............................................................................................. 5 1. Coastal Storm /Hurricane Hazard Profile .......................................................................... 5 2. Hurricane Hazards ................................................................................................................ 7 3. Storm Surge: The SLOSH Model ........................................................................................ 8 4. Hurricane Wind Analysis.................................................................................................... 17 5. Tornadoes .......................................................................................................................... -
Florida Hurricanes and Tropical Storms, 1871-1993: an Historical Survey, the Only Books Or Reports Exclu- Sively on Florida Hurricanes Were R.W
3. 2b -.I 3 Contents List of Tables, Figures, and Plates, ix Foreword, xi Preface, xiii Chapter 1. Introduction, 1 Chapter 2. Historical Discussion of Florida Hurricanes, 5 1871-1900, 6 1901-1930, 9 1931-1960, 16 1961-1990, 24 Chapter 3. Four Years and Billions of Dollars Later, 36 1991, 36 1992, 37 1993, 42 1994, 43 Chapter 4. Allison to Roxanne, 47 1995, 47 Chapter 5. Hurricane Season of 1996, 54 Appendix 1. Hurricane Preparedness, 56 Appendix 2. Glossary, 61 References, 63 Tables and Figures, 67 Plates, 129 Index of Named Hurricanes, 143 Subject Index, 144 About the Authors, 147 Tables, Figures, and Plates Tables, 67 1. Saffir/Simpson Scale, 67 2. Hurricane Classification Prior to 1972, 68 3. Number of Hurricanes, Tropical Storms, and Combined Total Storms by 10-Year Increments, 69 4. Florida Hurricanes, 1871-1996, 70 Figures, 84 l A-I. Great Miami Hurricane 2A-B. Great Lake Okeechobee Hurricane 3A-C.Great Labor Day Hurricane 4A-C. Hurricane Donna 5. Hurricane Cleo 6A-B. Hurricane Betsy 7A-C. Hurricane David 8. Hurricane Elena 9A-C. Hurricane Juan IOA-B. Hurricane Kate 1 l A-J. Hurricane Andrew 12A-C. Hurricane Albert0 13. Hurricane Beryl 14A-D. Hurricane Gordon 15A-C. Hurricane Allison 16A-F. Hurricane Erin 17A-B. Hurricane Jerry 18A-G. Hurricane Opal I9A. 1995 Hurricane Season 19B. Five 1995 Storms 20. Hurricane Josephine , Plates, X29 1. 1871-1880 2. 1881-1890 Foreword 3. 1891-1900 4. 1901-1910 5. 1911-1920 6. 1921-1930 7. 1931-1940 These days, nothing can escape the watchful, high-tech eyes of the National 8. -
Florida Commission on Hurricane Loss Projection Methodology
Florida Commission on Hurricane Loss Projection Methodology Professional Team Report 2019 Hurricane Standards Hurricane Matthew Hurricane Michael CoreLogic, Inc. Remote Review April 5 – 8, 2021 CL Professional Team Report April 5-8, 2021 On April 5-8, 2021, the Professional Team conducted a remote review of the CoreLogic, Inc. (CL), CoreLogic Florida Hurricane Model 2021a in platform Risk Quantification and Engineering™ Version 21. The following individuals participated in the remote review. CoreLogic Amin Ilia, Ph.D., Coastal Scientist and Engineer Branimir Betov, M.S., Director, Model Development Daniel Betten, Ph.D., Atmospheric Scientist Justin Brolley, Ph.D., Principal Research Scientist Annes Haseemkunju, Ph.D., Atmospheric Scientist Mahmoud Khater, Ph.D., P.E., Chief Science and Engineering Officer Howard Kunst, FCAS, MAAA, Actuary Ilyes Meftah, Research Scientist Sergey Pasternak, Software Architect David Smith, Senior Director, Model Development Amanuel Tecle, Ph.D., Research Scientist Professional Team Paul Fishwick, Ph.D., Computer and Information Scientist Tim Hall, Ph.D., Meteorologist Mark Johnson, Ph.D., Statistician, Team Leader Stu Mathewson, FCAS, MAAA, Actuary Masoud Zadeh, Ph.D., P.E., Structural Engineer Donna Sirmons, Staff Due to the COVID-19 pandemic and State Board of Administration travel restrictions, the Professional Team conducted the review remotely rather than on-site. The remote review followed the on-site review process as detailed in the Report of Activities and the remote review procedures adopted by -
Strategic Beach Management Plan: Northeast Atlantic Coast Region Office of Resilience and Coastal Protection Florida Department of Environmental Protection
Strategic Beach Management Plan: Northeast Atlantic Coast Region Office of Resilience and Coastal Protection Florida Department of Environmental Protection April 2020 Florida Department of Environmental Protection, Strategic Beach Management Plan – Northeast Atlantic Coast Region Table of Contents Introduction - Northeast........................................................................................................................... 1 Sea Islands ................................................................................................................................................. 2 Strategies for Inlets and Critically Eroded Beaches .......................................................................... 2 St. Marys River Entrance, Nassau County .......................................................................................... 2 Fort Clinch, Nassau County, 2,500 feet west of R1-R9 ...................................................................... 3 Fernandina Beach, Nassau County, R9-R33 ....................................................................................... 4 South Amelia Island, Nassau County, R60-R80 ................................................................................. 5 Nassau Sound, Nassau County R79 to Duval County R1 ................................................................... 6 Little Talbot Island State Park, Duval County, R21-R23 .................................................................... 7 Fort George Inlet, Duval County, R25-R26 ....................................................................................... -
A Recent Assessment of Damage from Hurricane Matthew
Page 20 January 2017 Shoreline By Gabriel Todaro Intern, EN-WC U.S. Army Corps of Engineers Jacksonville District Hurricane Dora and Hurricane Matthew struck Jacksonville Beach, Florida almost 52 years apart but they will be tied together as the strongest hurricanes to directly strike the coastal city. Hurricane Dora formed in the Atlantic Ocean on August 28, 1964. As it crossed the Atlantic, Dora continued to strengthen until peaking as a Category 4 hurricane on September 6. Hurricane Dora made landfall near St. Augustine, Florida as a Category 3 storm on September 10th. In Florida, nearly 10,000 homes received damage and 156,000 homes lost power. Floodwaters rushed up Atlantic Boulevard and onto A1A as the floodwalls Figure 1: Damage caused by the storm surge in Atlantic Beach during Hurricane Dora that protected the beach were overwhelmed. Numerous houses fell into the Ocean as steady winds of greater than 65 mph pounded the coast. Figure 1 shows the water breaking through and washing away a house in Atlantic Beach, FL. Prior to the current shore protection project, the beach looked very different than it does today. Figures 2 and 3 show the conditions between 1928 and 1963. The beach was much narrower and there were not any dunes to protect the shoreline. A rock revetment and concrete seawall protected Jacksonville Beach prior to Hurricane Dora (Figures 4 and 5). Unfortunately, these defenses were inadequate to against the storm. During Dora, Jacksonville Beach faced severe coastal flooding from the storm. Figure 2: Jacksonville Beach during the early 1960s Hurricane Dora resulted in the decision that better protection was needed along the Jacksonville shoreline. -
Noise Evidence Could Expand Hurricane Record 10 November 2009, by Chris Gorski, ISNS
Noise Evidence Could Expand Hurricane Record 10 November 2009, By Chris Gorski, ISNS seven years working for the Comprehensive Nuclear-Test-Ban Treaty Organization in Vienna, Austria. He was responsible for evaluating the ability of potential seismic monitoring stations to detect clandestine nuclear weapons tests, and in doing that work he noticed strange seismic patterns in Antarctica. "It appears that this was really well correlated with a really large storm in the South Atlantic," said Ebeling. "That's what started me thinking down this particular path." Fathogram showing swell from approaching hurricane. EXPLORER record from near Cape Hatteras. Ebeling took seismic records from stations in September 7, 1964 - Hurricane Dora. Credit: NOAA | Massachusetts and Puerto Rico and analyzed them C&GS Season's Report Moore 1964-123 for evidence of Hurricane Andrew, a Category V storm that devastated Florida in 1992. Seismic records show the motion of the ground, As sea-surface temperatures rise across the globe, regardless of the cause. While earthquakes are the some scientists believe that hurricane frequency most common source of seismic events, bomb and intensity may increase. A fresh technique blasts, building demolition and a host of other offers promise to generate new data from long- events -- including violent weather -- can be dead storms, which could improve researchers' recorded on sensitive seismographs. forecasts and make them more accurate. Typically, scientists monitoring seismographs for Carl Ebeling, a geophysicist at Northwestern earthquake activity disregard signals caused by University in Evanston, Ill., demonstrated a method human activity or by weather as "noise." But it is in to uncover the power of historic hurricanes by the noise generated by hurricanes that Ebeling is looking at how oceans churned by the storms finding his data. -
Primary Meteorological Aspects of Hurricanes Controlling Coastal & Inland Impacts Steve Lyons the Weather Channel
Primary Meteorological Aspects of Hurricanes Controlling Coastal & Inland Impacts Steve Lyons The Weather Channel Despite continued widespread use of the Saffir-Simpson scale by government forecasters, Emergency Managers and much of the media to convey potential dangers from a hurricane, maximum wind speed at one spot at one moment in time does NOT usually reflect the magnitude of dangerous impacts a hurricane or tropical storm can bring to the coast and inland. The spatial distribution of strong winds and the duration of them will be addressed and contrasted with a localized wind maximum. How the size of hurricane and tropical storm winds contribute to coastal and inland impacts will be discussed and limitations of the "total kinetic energy" index of a hurricane will be outlined. Finally tropical cyclone motion, both speed and angle of attach to the coast, will be addressed relative to the magnitude of coastal and inland impacts. Toward a U.S. Climatology of Coastal and Inland Tropical Cyclone Winds David H. Levinson 1, Michael C. Kruk 2, Ethan J. Gibney 3, Michael Squires 1 1 NOAA/NESDIS, 2 STG, Inc., 3 IMSG, Inc. National Climatic Data Center, Asheville, North Carolina Over the past several years, attempts have been made to assess the relative frequency of coastal and inland counties that experience either hurricane or tropical storm force winds from a landfalling tropical cyclone. This is traditionally done by overlaying the historical track data for the Atlantic basin and implementing a symmetrical 50 km buffer around the storm to identify those counties which are influenced by the storm.