Appendix 8 Hazard Analysis
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Observation and a Numerical Study of Gravity Waves During Tropical Cyclone Ivan (2008)
Open Access Atmos. Chem. Phys., 14, 641–658, 2014 Atmospheric www.atmos-chem-phys.net/14/641/2014/ doi:10.5194/acp-14-641-2014 Chemistry © Author(s) 2014. CC Attribution 3.0 License. and Physics Observation and a numerical study of gravity waves during tropical cyclone Ivan (2008) F. Chane Ming1, C. Ibrahim1, C. Barthe1, S. Jolivet2, P. Keckhut3, Y.-A. Liou4, and Y. Kuleshov5,6 1Université de la Réunion, Laboratoire de l’Atmosphère et des Cyclones, UMR8105, CNRS-Météo France-Université, La Réunion, France 2Singapore Delft Water Alliance, National University of Singapore, Singapore, Singapore 3Laboratoire Atmosphères, Milieux, Observations Spatiales, UMR8190, Institut Pierre-Simon Laplace, Université Versailles-Saint Quentin, Guyancourt, France 4Center for Space and Remote Sensing Research, National Central University, Chung-Li 3200, Taiwan 5National Climate Centre, Bureau of Meteorology, Melbourne, Australia 6School of Mathematical and Geospatial Sciences, Royal Melbourne Institute of Technology (RMIT) University, Melbourne, Australia Correspondence to: F. Chane Ming ([email protected]) Received: 3 December 2012 – Published in Atmos. Chem. Phys. Discuss.: 24 April 2013 Revised: 21 November 2013 – Accepted: 2 December 2013 – Published: 22 January 2014 Abstract. Gravity waves (GWs) with horizontal wavelengths ber 1 vortex Rossby wave is suggested as a source of domi- of 32–2000 km are investigated during tropical cyclone (TC) nant inertia GW with horizontal wavelengths of 400–800 km, Ivan (2008) in the southwest Indian Ocean in the upper tropo- while shorter scale modes (100–200 km) located at northeast sphere (UT) and the lower stratosphere (LS) using observa- and southeast of the TC could be attributed to strong local- tional data sets, radiosonde and GPS radio occultation data, ized convection in spiral bands resulting from wave number 2 ECMWF analyses and simulations of the French numerical vortex Rossby waves. -
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 Harvey Oral History Project Shelby Gonzalez HIST 5370
Hurricane Harvey Oral History Project Shelby Gonzalez HIST 5370 December 9, 2017 Hurricane Harvey Oral History Collection PROJECT TITLE: “Hurricane Harvey Oral History Project” NARRATOR: Dr. Kelly Quintanilla DATE OF INTERVIEW: November 6, 2017 INTERVIEWER NAME: Shelby Gonzalez DATE and LOCATION OF ITNERVIEW: Dr. Quintanilla’s office, Corpus Christi Hall at Texas A&M University-Corpus Christi, Texas. President of Texas A&M University-Corpus Christi (TAMU-CC), Dr. Kelly Quintanilla is one of many persons being interviewed for the “Hurricane Harvey Oral History Project” being conducted by Graduate Students in good standing in the History Master’s Program at TAMU-CC. Dr. Quintanilla explains to us the policies and procedures she followed to prepare the university and students for the possibility of Hurricane Harvey making landfall in Corpus Christi, Texas. This project was turned into the Hurricane Harvey Oral History Collection, which explores, uncovers, and highlights the lives of residents from South Texas who experienced Hurricane Harvey. The collection was created in an effort to ensure that the memories of those affected by the hurricane not be lose, and to augment the Mary and Jeff Bell Library’s Special Collections and Archives Department records. The collections contains interviews from residents of Port Aransas, the President of TAMU-CC,… (will be continued) 1 Dr. Kelly Quintanilla Narrator Shelby L. Gonzalez History Graduate Program Interviewer November 6, 2017 At Dr. Quintanilla’s office Texas A&M University-Corpus Christi Corpus Christi, Texas SG: Today is November 6, 2017. I am here with the Texas A&M University-Corpus Christi President, Dr. -
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. -
Ch 5. the Atmospheric Environment Observed at Big Bend National
Final Report — September 2004 5. THE ATMOSPHERIC ENVIRONMENT OBSERVED AT BIG BEND NATIONAL PARK DURING THE BRAVO STUDY The BRAVO Study intensively researched the properties of the particulate matter, atmospheric optics, meteorology, and air pollutant emissions of the study area during July through October 1999. The study also explored transport and diffusion by injecting perfluorocarbon tracers into the atmosphere at specific locations. Findings produced by these multiple experiments concerning the environment around Big Bend National Park and throughout the study area are summarized in this chapter. Some of these findings were carried into the source attribution analyses that are described in Chapters 10 and 11, while others advanced scientific understanding for future application. More detail on many of these studies and their results is provided in published papers and reports that are cited in the text; some of the reports are in the Appendix. 5.1 Particulate Matter Characterization by the Routine Measurement Network As described in Section 3.3, the BRAVO Study included an extensive network of particulate matter samplers that routinely collected 24-hour and 6-hour samples over the four-month study period. This section summarizes findings derived from the routine measurements concerning the temporal and spatial characteristics of the study area particulate matter and its composition. 5.1.1 Particulate Matter Temporal and Spatial Characteristics Evaluation of BRAVO Study particulate matter sample composition and temporal variation found similar behavior at groups of adjacent sampling sites in the study domain. The map in Figure 5-1 shows the grouping of sampling sites that this evaluation suggested. To provide a manageable description of the study period aerosol, concentration measurements at sites within each group were averaged together. -
June Is a Month Full of History and Celebrations
This Month: Celebrating June Father of Flag Day Food Bank RGV Valley Birding JDA Academic Honors Gerald Sneed, Wildlife Hurricane Season Begins TSA Captains Leaving RGV June 2017 The Little Paper You’ll Want To Keep & Share Vol. 4 No. 1 The Valley Spotlight Is Celebrating Its Fourth Birthday! This issue marks the beginning of our fourth year of pub- We also say a BIG THANK YOU to all of you who have lishing The Valley Spotlight! With much gratitude, we thank enjoyed reading The Valley Spotlight for the past three years. all of the individuals and businesses in the Rio Grande Valley Without YOU, there would be no reason to continue. - So with great enthusiasm and joy, we begin Volume 4 and tributions in writing stories and articles. look forward to many more to come. June is a Month Full of History and Celebrations On June 6, 1944, more than 160,000 Al- On June 8, 1874, Apache leader Cochise On June 16, 1963, Valentina Tereshkova, lied troops landed along a 50-mile stretch of died on the Chiricahua Reservation in south- eastern Arizona. After a peace treaty had been in space as her Soviet space- Nazi Germany on the beaches of Normandy, broken by the U.S. Army in 1861, he waged war against the Tyuratam launch site. the operation a crusade in which, “we will settlers and soldiers, forc- She manually controlled the accept nothing less than full victory.” ing them to withdraw from spacecraft completing 48 or- southern Arizona. In 1862, bits in 71 hours before land- he became principal chief ing safely. -
A Classification Scheme for Landfalling Tropical Cyclones
A CLASSIFICATION SCHEME FOR LANDFALLING TROPICAL CYCLONES BASED ON PRECIPITATION VARIABLES DERIVED FROM GIS AND GROUND RADAR ANALYSIS by IAN J. COMSTOCK JASON C. SENKBEIL, COMMITTEE CHAIR DAVID M. BROMMER JOE WEBER P. GRADY DIXON A THESIS Submitted in partial fulfillment of the requirements for the degree Master of Science in the Department of Geography in the graduate school of The University of Alabama TUSCALOOSA, ALABAMA 2011 Copyright Ian J. Comstock 2011 ALL RIGHTS RESERVED ABSTRACT Landfalling tropical cyclones present a multitude of hazards that threaten life and property to coastal and inland communities. These hazards are most commonly categorized by the Saffir-Simpson Hurricane Potential Disaster Scale. Currently, there is not a system or scale that categorizes tropical cyclones by precipitation and flooding, which is the primary cause of fatalities and property damage from landfalling tropical cyclones. This research compiles ground based radar data (Nexrad Level-III) in the U.S. and analyzes tropical cyclone precipitation data in a GIS platform. Twenty-six landfalling tropical cyclones from 1995 to 2008 are included in this research where they were classified using Cluster Analysis. Precipitation and storm variables used in classification include: rain shield area, convective precipitation area, rain shield decay, and storm forward speed. Results indicate six distinct groups of tropical cyclones based on these variables. ii ACKNOWLEDGEMENTS I would like to thank the faculty members I have been working with over the last year and a half on this project. I was able to present different aspects of this thesis at various conferences and for this I would like to thank Jason Senkbeil for keeping me ambitious and for his patience through the many hours spent deliberating over the enormous amounts of data generated from this research. -
FLORIDA HAZARDOUS WEATHER by DAY (To 1994) OCTOBER 1 1969
FLORIDA HAZARDOUS WEATHER BY DAY (to 1994) OCTOBER 1 1969 - 1730 - Clay Co., Orange Park - Lightning killed a construction worker who was working on a bridge. A subtropical storm spawned one weak tornado and several waterspouts in Franklin Co. in the morning. 2 195l - south Florida - The center of a Tropical Storm crossed Florida from near Fort Myers to Vero Beach. Rainfall totals ranged from eight to 13 inches along the track, but no strong winds occurred near the center. The strong winds of 50 to 60 mph were all in squalls along the lower east coast and Keys, causing minor property damage. Greatest damage was from rains that flooded farms and pasture lands over a broad belt extending from Naples, Fort Myers, and Punta Gorda on the west coast to Stuart, Fort Pierce, and Vero Beach on the east. Early fall crops flooded out in rich Okeechobee farming area. Many cattle had to be moved out of flooded area, and quite a few were lost by drowning or starvation. Roadways damaged and several bridges washed out. 2-4 1994 - northwest Florida - Flood/Coastal Flood - The remnants of Tropical Depression 10 moved from the northeast Gulf of Mexico, across the Florida Panhandle, and into Georgia on the 2nd. High winds produced rough seas along west central and northwest Florida coasts causing minor tidal flooding and beach erosion. Eighteen people had to be rescued from sinking boats in the northeast Gulf of Mexico. Heavy rains in the Florida Big Bend and Panhandle accompanied the system causing extensive flooding to roadways, creeks and low lying areas and minor flooding of rivers. -
Preparedness and Mitigation in the Americas
PREPAREDNESS AND MITIGATION IN THE AMERICAS Issue No. 79 News and Information for the International Disaster Community January 2000 Inappropriate Relief Donations: What is the Problem? f recent disasters worldwide are any indication, Unsolicited clothing, canned foods and, to a lesser the donation of inappropriate supplies remains extent, pharmaceuticals and medical supplies, I a serious problem for the affected countries. continue to clog the overburdened distribution networks during the immediate aftermath of highly-publicized tragedies. This issue per- sists in spite of health guidelines issued by the World Health Organization, a regional policy adopted by the Ministries of Health of Latin America and the Caribbean, and the educational lobbying efforts of a consortium of primarily European NGOs w w w. wemos.nl). I N S I D E Now the Harvard School of Public Health has partially addressed the issue in a com- prehensive study of U.S. pharmaceutical News from d o n a t i o n s (w w w. h s p h . h a r v a r d . e d u / f a c u l t y / PAHO/WHO r e i c h / d o n a t i o n s / i n d e x . h t m). Although the 2 study correctly concluded that the "problem A sports complex in Valencia, Venezuela, which served as the main temporary shel- Other ter for the population displaced by the disaster, illustrates what happens when an may be more serious in disaster relief situa- Organizations enormous amount of humanitarian aid arrives suddenly in a country. -
ON the PERFORMANCE of BUILDINGS in HURRICANES a STUDY for the SAFFIR-SIMSPON SCALE COMMITTEE by Tim Marshall, P.E
ON THE PERFORMANCE OF BUILDINGS IN HURRICANES A STUDY FOR THE SAFFIR-SIMSPON SCALE COMMITTEE by Tim Marshall, P.E. Meteorologist HAAG ENGINEERING CO. October 18, 2009 DRAFT COPY INTRODUCTION Over the past 30 years, the author has surveyed building damage in 30 hurricanes beginning with Hurricane Allen (1980). Many of these hurricanes, the author has experienced firsthand by riding out the storms in hotels, vehicles, or parking garages. Within weeks after each hurricane, ground and sometimes aerial surveys were performed to document the performance of buildings and measure the heights of the storm surge using levels, rods, and benchmarks. Then, the author spent several months in the disaster areas conducting individual inspections to hundreds of structures. To date, the author has amassed tens of thousands of images of hurricane damage to buildings and has written and assembled numerous references with regard to building performance in hurricanes. One thing that is clear is that not all buildings perform the same in a hurricane and that certain types of buildings, or their components, fail at relatively low wind speeds. This is especially true if there are poor attachments at critical connections. Certainly there have been a number of building improvements due to code upgrades in Florida and a few other states, after Hurricane Andrew, which has resulted in better building performance in subsequent hurricanes. In the author’s study of storm surge, it has become obvious there is not a direct relationship between the magnitude of the wind and the height of the storm surge. There are many reasons for this including the size of the hurricane, angle of its attack to the shoreline, coastal topography, bathymetry, etc. -
Florida Commission on Hurricane Loss Projection Methodology
Submitted: November 5, 2018 Revised: January 21, 2019 Revised: February 13, 2019 Revised: March 22, 2019 Revised: April 9, 2019 Revised: July 12, 2019 HurLoss Version 9.0 Florida Commission on Hurricane Loss Projection Methodology 2017 Hurricane Standards Prepared for: Florida Commission on Hurricane Loss Projection Methodology State Board of Administration 1801 Hermitage Boulevard Tallahassee, Florida 32308 Prepared by: Applied Research Associates, Inc. IntraRisk Division 8537 Six Forks Road, Suite 600 Raleigh, North Carolina 27615 Copyright © 2019 Applied Research Associates, Inc. For Evaluation by the Florida Commission on Hurricane Loss Projection Methodology 1 Applied Research Associates, Inc. April 9, 2019 4 4/9/2019 5:30 PM Florida Commission on Hurricane Loss Projection Methodology Model Identification Name of Hurricane Model: HurLoss Florida Model Hurricane Model Version Identification: 9.0 Interim Hurricane Model Update Version Identification: N/A Hurricane Model Platform Name and Identifications: HurLoss Software Platform Interim Data Update Designation: N/A Name of Modeling Organization: Applied Research Associates, Inc. Street Address: 8537 Six Forks Road, Suite 600 City, State, Zip Code: Raleigh, NC, 27615 Mailing Address, if different from above: N/A Contact Person: Frank Lavelle Phone Number: (919) 582-3350 Fax Number: (919) 582-3401 E-mail Address: [email protected] Date: April 9, 2019 Applied Research Associates, Inc. April 9, 2019 3 4/9/2019 5:30 PM Applied Research Associates, Inc. April 9, 2019 4 4/9/2019 5:30 PM November 5, 2018 Floyd Yager, FCAS Chair, Florida Commission on Hurricane Loss Projection Methodology 1801 Hermitage Boulevard, Suite 100 Tallahassee, FL 32308 Re: ARA Model Submission under the November 1, 2017 Standards Dear Mr. -
The Rapid Intensification and Eyewall Replacement Cycles of Hurricane
MARCH 2020 F I S C H E R E T A L . 981 The Rapid Intensification and Eyewall Replacement Cycles of Hurricane Irma (2017) MICHAEL S. FISCHER,ROBERT F. ROGERS, AND PAUL D. REASOR NOAA/Atlantic Oceanographic and Meteorological Laboratory/Hurricane Research Division, Miami, Florida (Manuscript received 7 June 2019, in final form 17 December 2019) ABSTRACT The initiation of a rapid intensification (RI) event for a tropical cyclone (TC) at major hurricane intensity is a rare event in the North Atlantic basin. This study examined the environmental and vortex-scale processes related to such an RI event observed in Hurricane Irma (2017) using a combination of flight-level and air- borne radar aircraft reconnaissance observations, microwave satellite observations, and model environmental analyses. The onset of RI was linked to an increase in sea surface temperatures and ocean heat content toward levels more commonly associated with North Atlantic RI episodes. Remarkably, Irma’s RI event comprised two rapidly evolving eyewall replacement cycle (ERC) episodes that each completed in less than 12 h. The two ERC events displayed different secondary eyewall formation (SEF) mechanisms and vortex evo- lutions. During the first SEF event, a secondary maximum in ascent and tangential wind was observed at the leading edge of a mesoscale descending inflow jet. During the ensuing ERC event, the primary eyewall weakened and ultimately collapsed, resulting in a brief period of weakening. The second SEF event displayed characteristics consistent with unbalanced boundary layer dynamics. Additionally, it is plausible that both SEF events were affected by the stagnation and axisymmeterization of outward-propagating vortex Rossby waves.