Top 10 Historical Hurricanes and Earthquakes in the Us
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Wind Speed-Damage Correlation in Hurricane Katrina
JP 1.36 WIND SPEED-DAMAGE CORRELATION IN HURRICANE KATRINA Timothy P. Marshall* Haag Engineering Co. Dallas, Texas 1. INTRODUCTION According to Knabb et al. (2006), Hurricane Katrina Mehta et al. (1983) and Kareem (1984) utilized the was the costliest hurricane disaster in the United States to concept of wind speed-damage correlation after date. The hurricane caused widespread devastation from Hurricanes Frederic and Alicia, respectively. In essence, Florida to Louisiana to Mississippi making a total of three each building acts like an anemometer that records the landfalls before dissipating over the Ohio River Valley. wind speed. A range of failure wind speeds can be The storm damaged or destroyed many properties, determined by analyzing building damage whereas especially near the coasts. undamaged buildings can provide upper bounds to the Since the hurricane, various agencies have conducted wind speeds. In 2006, WSEC developed a wind speed- building damage assessments to estimate the wind fields damage scale entitled the EF-scale, named after the late that occurred during the storm. The National Oceanic Dr. Ted Fujita. The author served on this committee. and Atmospheric Administration (NOAA, 2005a) Wind speed-damage correlation is useful especially conducted aerial and ground surveys and published a when few ground-based wind speed measurements are wind speed map. Likewise, the Federal Emergency available. Such was the case in Hurricane Katrina when Management Agency (FEMA, 2006) conducted a similar most of the automated stations failed before the eye study and produced another wind speed map. Both reached the coast. However, mobile towers were studies used a combination of wind speed-damage deployed by Texas Tech University (TTU) at Slidell, LA correlation, actual wind measurements, as well as and Bay St. -
NOAA Technical Memorandum NWS HYDR0-20 STORM TIDE
NOAA Technical Memorandum NWS HYDR0-20 STORM TIDE FREQUENCY ANALYSIS FOR THE GULF COAST OF FLORIDA FROM CAPE SAN BLAS TO ST. PETERSBURG BEACH Francis P. Ho and Robert J. Tracey Office of Hydrology Silver Spring, Md. April 1975 UNITED STATES /NATIONAL OCEANIC AND / National Weather DEPARTMENT OF COMMERCE ATMOSPHERIC ADMINISTRATION Service Frederick B. Dent, Secretar1 Robert M. White, Administrator George P, Cressman, Director CONTENTS 1. Introduction. • • • • • • • 1 1.1 Objective and scope •• 1 1.2 Authorization •• 1 1.3 Study method •• 2 2. Summary of historical hurricanes •• 2 2.1 Hurricane tracks 2 2.2 Historical notes 3 3. Climatology of hurricane characteristics. 8 3.1 Frequency of hurricane tracks •••. 8 3.2 Probability distribution of hurricane intensity. 8 3.3 Probability distribution of radius of maximum winds. 9 3.4 Probability distribution of speed and direction of forward motion • . • • • • • • • • 9 4. Hurricane surge • • • • 9 4.1 Surge model ••• 9 4.2 Shoaling factor •• 10 5. Tide frequency analysis by joint probability method • 10 5.1 The joint probability method • 10 5.2 Astronomical tides •••••• 11 5.2.1 Reference datum •.•••• 11 Table 1. Tropical storm parameters - Clearwater, Fla 12 Table 2. Tropical storm parameters - Bayport, Fla •• 13 Table 3. Tropical storm parameters - Cedar Key, Fla. 14 Table 4. Tropical storm parameters- Rock ·Islands, Fla .. 15 Table 5. Tropical storm parameters - Carrabelle, Fla • 16 Table 6. Tropical storm parameters - Apalachicola, Fla 17 5.2.2 Astronomical tide • • • •.• 19 5.3 Prestorm water level ••••••. 19 5.4 Tide frequencies • • • • . • ••• 19 5.5 Adjustment along coast ••••••.•••.•••. 19 5.6 Comparison of frequency curves with observed tides and high-water marks • • • • • • • • • • • . -
Florida's Water Resources1
FE757 Florida’s Water Resources1 Tatiana Borisova and Tara Wade2 Introduction: Why Water Resources Are Important “Water is the lifeblood of our bodies, our economy, our nation and our well-being” (Stephen Lee Johnson, Head of EPA under G.W. Bush Administration). This quote sums up the importance of water resources. We use water for drinking, gardening, and other household uses, in agriculture (e.g., for irrigation), and in energy production and industrial processes (e.g., for cooling in thermoelectric power generation). Clean and plentiful water resources are also important for our recreational activities (e.g., boating, swimming, or fishing). Water also Figure 1. In November, manatees migrate to warmer coastal waters, sustains wildlife (such as manatees) and is an integral part such as Crystal River on the west coast of Florida (Source: UF/IFAS/ICS) of Florida’s environment (Figure 1). The use of water is increasing along with Florida’s of Florida’s water resources is a first step toward optimizing population. Floridians rely on underground freshwater current freshwater supply use and ensuring adequate water reserves, called aquifers, to supply our diverse water needs resources in the future. (USGS 2016a). In some Florida regions, this underground freshwater reserve can no longer sustain the growing water demands of the population, while also feeding Florida’s riv- Hydrologic Cycle: Where Water ers, springs, and lakes. With periodic droughts, shortages of Originates and Where It Goes freshwater may occur. Drought and water shortages in the Toni Morrison, an American novelist, once said that “all state have caused urban planners and policy makers to pay water has a perfect memory and is forever trying to get closer attention to water use, water supply development, back to where it was.” Indeed, water is constantly moving. -
Hurricane Irma Storm Review
Hurricane Irma Storm Review November 11, 2018 At Duke Energy Florida, we power more than 4 million lives Service territory includes: . Service to 1.8 million retail customers in 35 counties . 13,000 square miles . More than 5,100 miles of transmission lines and 32,000 miles of distribution lines . Owns and operates nearly 9,500 MWs of generating capacity . 76.2% gas, 21% coal, 3% renewable, 0.2%oil, 2,400 MWs Purchased Power. 2 Storm Preparedness Activities Operational preparation is a year-round activity Coordination with County EOC Officials . Transmission & Distribution Systems Inspected and . Structured Engagement and Information Maintained Sharing Before, During and After Hurricane . Storm Organizations Drilled & Prepared . Coordination with county EOC priorities . Internal and External Resource Needs Secured . Public Communications and Outreach . Response Plan Tested and Continuously Improved Storm Restoration Organization Transmission Hurricane Distribution System Preparedness System Local Governmental Coordination 3 Hurricane Irma – Resources & Logistics Resources . 12,528 Total Resources . 1,553 pre-staged in Perry, Georgia . 91 line and vegetation vendors from 25 states . Duke Energy Carolinas and Midwest crews as well as resources from Texas, New York, Louisiana, Colorado, Illinois, Oklahoma, Minnesota, Maine and Canada . 26 independent basecamps, parking/staging sites Mutual Assistance . Largest mobilization in DEF history . Mutual Assistance Agreements, executed between DEF and other utilities, ensure that resources can be timely dispatched and fairly apportioned. Southeastern Electric Exchange coordinates Mutual Assistance 4 5. Individual homes RESTORATION 3. Critical Infrastructure 2. Substations 1. Transmission Lines 4. High-density neighborhoods 5 Hurricane Irma- Restoration Irma’s track northward up the Florida peninsula Restoration Summary resulted in a broad swath of hurricane and tropical Customers Peak Customers Outage storm force winds. -
Hurricane Sandy Rebuilding Strategy
Hurricane Sandy Rebuilding Task Force HURRICANE SANDY REBUILDING STRATEGY Stronger Communities, A Resilient Region August 2013 HURRICANE SANDY REBUILDING STRATEGY Stronger Communities, A Resilient Region Presented to the President of the United States August 2013 Front and Back Cover (Background Photo) Credits: (Front Cover) Hurricane Sandy Approach - NOAA/NASA (Back Cover) Hurricane Sandy Approach - NOAA/NASA Cover (4-Photo Banner) Credits - Left to Right: Atlantic Highlands, New Jersey - FEMA/ Rosanna Arias Liberty Island, New York - FEMA/Kenneth Wilsey Seaside Heights, New Jersey - FEMA/Sharon Karr Seaside Park, New Jersey - FEMA/Rosanna Arias Hurricane Sandy Letter from the Chair Rebuilding Strategy LETTER FROM THE CHAIR Last October, Hurricane Sandy struck the East Coast with incredible power and fury, wreaking havoc in communities across the region. Entire neighborhoods were flooded. Families lost their homes. Businesses were destroyed. Infrastructure was torn apart. After all the damage was done, it was clear that the region faced a long, hard road back. That is why President Obama pledged to work with local partners every step of the way to help affected communities rebuild and recover. In recent years, the Federal Government has made great strides in preparing for and responding to natural disasters. In the case of Sandy, we had vast resources in place before the storm struck, allowing us to quickly organize a massive, multi-agency, multi-state, coordinated response. To ensure a full recovery, the President joined with State and local leaders to fight for a $50 billion relief package. The Task Force and the entire Obama Administration has worked tirelessly to ensure that these funds are getting to those who need them most – and quickly. -
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. -
Hurricane Andrew in Florida: Dynamics of a Disaster ^
Hurricane Andrew in Florida: Dynamics of a Disaster ^ H. E. Willoughby and P. G. Black Hurricane Research Division, AOML/NOAA, Miami, Florida ABSTRACT Four meteorological factors aggravated the devastation when Hurricane Andrew struck South Florida: completed replacement of the original eyewall by an outer, concentric eyewall while Andrew was still at sea; storm translation so fast that the eye crossed the populated coastline before the influence of land could weaken it appreciably; extreme wind speed, 82 m s_1 winds measured by aircraft flying at 2.5 km; and formation of an intense, but nontornadic, convective vortex in the eyewall at the time of landfall. Although Andrew weakened for 12 h during the eyewall replacement, it contained vigorous convection and was reintensifying rapidly as it passed onshore. The Gulf Stream just offshore was warm enough to support a sea level pressure 20-30 hPa lower than the 922 hPa attained, but Andrew hit land before it could reach this potential. The difficult-to-predict mesoscale and vortex-scale phenomena determined the course of events on that windy morning, not a long-term trend toward worse hurricanes. 1. Introduction might have been a harbinger of more devastating hur- ricanes on a warmer globe (e.g., Fisher 1994). Here When Hurricane Andrew smashed into South we interpret Andrew's progress to show that the ori- Florida on 24 August 1992, it was the third most in- gins of the disaster were too complicated to be ex- tense hurricane to cross the United States coastline in plained by thermodynamics alone. the 125-year quantitative climatology. -
A Brief History of Lake Okeechobee: a Narrative of Confict Alanna L
A Brief History of Lake Okeechobee: A Narrative of Confict Alanna L. Lecher, Ph.D, Lynn University Abstract Lake Okeechobee is Florida’s largest lake, the largest lake in the Southeast United States, and the second largest lake contained entirely within the United States. The history of this inland sea is marked both by natural processes, and more recently human development and intervention. Adventurers can explore this behemoth of a waterway via the Lake Okeechobee Scenic Trail that enriches it, a part of the Florida National Scenic Trail. This paper synthesizes major natural and human-induced perturbations that shaped the lake and ultimately the trail that encircles it to create a narrative of Florida’s great lake. The story of Lake Okeechobee is a story of battles, frst between the land and sea, then between the lake itself and humankind. For the past few centuries Lake Okeechobee’s natural perturbations in water fow and fooding resisted the control of man, until recently when man triumphed, managing to control the fow of water in and out of the lake. Unfortunately, with this new found control a new bio- ecological threat in the form of harmful algal blooms has emerged, which again threatens the health and livelihood of South Floridians. Currently there are new eforts that seek to restore Lake Okeechobee towards a more natural state in an efort to thwart the blooms. Manuscript It’s a full moon weekend in February and runners lace up their shoes in preparation. They gather in the agricultural town of Clewiston southeast of Lake Okeechobee. -
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. -
Vulnerability of the Suncoast Connector Toll Road Study Area to Future Storms and Sea Level Rise
Vulnerability of the Suncoast Connector Toll Road Study Area to Future Storms and Sea Level Rise Michael I. Volk, Belinda B. Nettles, Thomas S. Hoctor University of Florida April, 2020 Suncoast Connector Coastal Vulnerability Assessment 2 Abstract The Multi-use Corridors of Regional Economic Significance Program (M-CORES) authorizes the design and construction of three new toll road corridors through portions of Florida, including the proposed Suncoast Connector. This paper assesses the potential vulnerability of the Suncoast Connector study area and specifically the U.S. 19/U.S. 27/U.S. 98 corridor to coastal hazards including storms and sea level rise. The results of this analysis indicate that the study area and existing U.S. 19/U.S. 27/U.S. 98 corridor are not only currently at risk from flooding and coastal storms, but that sea level rise and climate change will significantly exacerbate these risks in the future. Findings include that at least 30 percent of the study area is already at risk from a Category 5 storm surge, with sea level rise projected to increase that risk even further. This region also provides one of the best opportunities for coastal biodiversity to functionally respond to increasing sea level rise, but a new major highway corridor along with the additional development that it facilitates will complicate biodiversity conservation and resiliency efforts. With these concerns in mind, it is critical to ensure that investment in new infrastructure, if pursued within the study area, is strategic and located in areas least vulnerable to impacts and repeat loss and least likely to conflict with efforts for facilitating the adaptation of regional natural systems to sea level rise and other related impacts. -
P1.28 a Digital Archive of Significant Florida Weather Events to Improve the Public’S Response to Future Warnings
P1.28 A Digital Archive of Significant Florida Weather Events to Improve the Public’s Response to Future Warnings Charles H. Paxton1,2, Jennifer M. Collins2, Kortnie J. Pugh1,2,3, and Jennifer L. Colson1 1. National Weather Service, Tampa Bay Florida 2. University of South Florida, Tampa, FL 3. National Marine Fisheries Service, St. Petersburg, FL I. Introduction other artifacts. These resources are of immense The past is our guide, our manual, it helps value not only to NOAA but also the American illuminate actions for the future. Through a NOAA people their true owners. Two frail leather-bound Preserve America Initiative grant obtained in U.S. Weather Bureau means books dating back to collaboration between the NWS (Tampa Bay 1890 needed rebinding. The office also has a region) and the University of South Florida (USF) wealth of other record books, older original two students were hired by NMFS Regional office weather maps depicting major events, news to work at the Tampa Bay Area NWS to document articles, and photos of major past events. historic weather events (Fig 1) and preserve weather relics. In an effort to save items of historical content, President Bush through his Preserve America executive order (E.O. 13287) called on NOAA and other federal agencies to inventory, preserve, and showcase federally- managed historic, cultural, or "heritage" resources and foster tourism in partnership with local communities. Fig. 2. Scanned weather photos. Many old weather artifacts from the past have been photographed and existing photographs of past weather events were scanned too (Fig. 2). When in electronic form, the pages of the books make accessible viewing on the Internet. -
HURRICANE Betsy Track Aug
UPS. Weather Bureau, WW~icane Betsy, August 27-Sept . 12, 1.65... U.S. DEPARTMENT OF COMMERCE ENVIRONMENT L SCIENCE SERVICES ADMlNlSTkATlON % ,j. WEATHER BUREAU CANE BTETZ~SX Prelimi~yReport wilh Advisorks and Bulletins Issued WASHINGTON, D. C. SEPT National Oceanic and Atmospheric Administration Weather Bureau Hurricane Series ERRATA NOTICE One or more conditions of the original document may affect the quality of the image, such as: Discolored pages Faded or light ink Binding intrudes into the text This has been a co-operative project between the NOAA Central Library and the Climate Database Modernization Program, National Climate Data Center (NCDC). To view the original document contact the NOAA Central Library in Silver Spring, MD at (301) 7 13-2607 x124 or Libra~y.Keference(u~noaa.gov. HOV Services Imaging Contractor 12200 Kiln Court Beltsville, MD 20704-1 387 November 6,2007 HURRICANE Betsy Track Aug. 21 - Sept. 12,1965 Minimum Surface Pressure and Maximum Surface W~nd Mlnlrnum Surface Pressure and Max~mumSurlace W~nd Stippled area represents area traversed by radar eye. - 8 2' 8 6' 84' 4 I , 80' MIAMI-KEY WEST-TAMPA'I6 I COMBINED RADAR TRACK OF HURRICANE BETSY SEPTEMBER 6-9, 1965 Radar eye boundary Radar center track Stippled area represents area traversed by radar eye. &ELIMINARY REPORT ON I:URRICANE BETSY August 27 - September 10, 1965 On August 27, 1965 at 10:30 AM EST a Navy hurricane reconnaissance aircraft discovered a tropical depression at 13' North Latitude and 54' West Longitude or about 350 miles east southeast of Barbados in the Windward Islands, West Indies.