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GAO-08-1120 Disaster Recovery: Past Experiences Offer Insights For
United States Government Accountability Office Report to the Committee on Homeland GAO Security and Governmental Affairs, U.S. Senate September 2008 DISASTER RECOVERY Past Experiences Offer Insights for Recovering from Hurricanes Ike and Gustav and Other Recent Natural Disasters GAO-08-1120 September 2008 DISASTER RECOVERY Accountability Integrity Reliability Past Experiences Offer Insights for Recovering from Highlights Hurricanes Ike and Gustav and Other Recent Natural Highlights of GAO-08-1120, a report to the Disasters Committee on Homeland Security and Governmental Affairs, U.S. Senate Why GAO Did This Study What GAO Found This month, Hurricanes Ike and While the federal government provides significant financial assistance after Gustav struck the Gulf Coast major disasters, state and local governments play the lead role in disaster producing widespread damage and recovery. As affected jurisdictions recover from the recent hurricanes and leading to federal major disaster floods, experiences from past disasters can provide insights into potential declarations. Earlier this year, good practices. Drawing on experiences from six major disasters that heavy flooding resulted in similar declarations in seven Midwest occurred from 1989 to 2005, GAO identified the following selected insights: states. In response, federal agencies have provided millions of • Create a clear, implementable, and timely recovery plan. Effective dollars in assistance to help with recovery plans provide a road map for recovery. For example, within short- and long-term recovery. 6 months of the 1995 earthquake in Japan, the city of Kobe created a State and local governments bear recovery plan that identified detailed goals which facilitated coordination the primary responsibility for among recovery stakeholders. -
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. -
Texas Hurricane History
Texas Hurricane History David Roth National Weather Service Camp Springs, MD Table of Contents Preface 3 Climatology of Texas Tropical Cyclones 4 List of Texas Hurricanes 8 Tropical Cyclone Records in Texas 11 Hurricanes of the Sixteenth and Seventeenth Centuries 12 Hurricanes of the Eighteenth and Early Nineteenth Centuries 13 Hurricanes of the Late Nineteenth Century 16 The First Indianola Hurricane - 1875 21 Last Indianola Hurricane (1886)- The Storm That Doomed Texas’ Major Port 24 The Great Galveston Hurricane (1900) 29 Hurricanes of the Early Twentieth Century 31 Corpus Christi’s Devastating Hurricane (1919) 38 San Antonio’s Great Flood – 1921 39 Hurricanes of the Late Twentieth Century 48 Hurricanes of the Early Twenty-First Century 68 Acknowledgments 74 Bibliography 75 Preface Every year, about one hundred tropical disturbances roam the open Atlantic Ocean, Caribbean Sea, and Gulf of Mexico. About fifteen of these become tropical depressions, areas of low pressure with closed wind patterns. Of the fifteen, ten become tropical storms, and six become hurricanes. Every five years, one of the hurricanes will become reach category five status, normally in the western Atlantic or western Caribbean. About every fifty years, one of these extremely intense hurricanes will strike the United States, with disastrous consequences. Texas has seen its share of hurricane activity over the many years it has been inhabited. Nearly five hundred years ago, unlucky Spanish explorers learned firsthand what storms along the coast of the Lone Star State were capable of. Despite these setbacks, Spaniards set down roots across Mexico and Texas and started colonies. Galleons filled with gold and other treasures sank to the bottom of the Gulf, off such locations as Padre and Galveston Islands. -
Hurricane Ike: Do We Need to Change Our Thinking?
AIRCURRENTS HURRICANE IKE: DO WE NEED TO CHANGE OUR THINKING? EDITor’s noTE: Of the three landfalling U.S. hurricanes in 2008, Hurricane Ike was by far the costliest. Perhaps because it was the largest loss in the last three seasons, it seemed to have captured the imagination of many in the industry, with estimates of as much as $20 billion or more being bandied about in the storm’s early aftermath. In this article, AIR’s Dr. Peter Dailey 12.2008 takes a hard look at the reality of Hurricane Ike. By Dr. Peter S. Dailey, Director of Atmospheric Science INTRODUCTION neither catastrophe modelers—nor the industry—should Hurricane Ike made landfall at Galveston, Texas in the early have been taken by surprise by Ike. While the storm morning hours of September 13, 2008. It was the third displayed some interesting characteristics, and managed and final hurricane to make landfall in the U.S. this year, to cause damage well inland (long after it had been preceded by Hurricane Dolly in late July and Gustav just two downgraded to a tropical depression and was no longer weeks prior to Ike. tracked by the NHC, the AIR model in fact performed very well in capturing the effects of this storm. All three landfalling hurricanes arrived on U.S. shores as Category 2 storms on the Saffir-Simpson scale. Yet according This article traces the history of Hurricane Ike’s brief but to the latest estimates by ISO’s Property Claims Services unit, costly assault on the U.S. It also looks at how the AIR U.S. -
Lessons Learned: Evacuations Management of Hurricane Gustav
4th Symposium on Policy and Socio-Economic Research, American Meteorological Society, Phoenix, AZ, 2009. 2.5 LESSONS LEARNED: EVACUATIONS MANAGEMENT OF HURRICANE GUSTAV Gina M. Eosco1, Mark A. Shafer2, and Barry Keim3 1Department of Communications, University of Oklahoma 2Oklahoma Climatological Survey, University of Oklahoma 3 Department of Geography and Anthropology, Louisiana State University Experience is what you get when you don’t get what you want. The experience of Hurricane Katrina was not what anyone in New Orleans wanted, yet three years after New Orleans was struck by Hurricane Katrina, the city proved they were ready for the next big one. As the National Hurricane Center forecasts started indicating a possible category 3 or stronger hurricane heading towards Louisiana, the city began preparations for evacuation. Gulf coast residents responded with the largest evacuation in U.S. history. Given the contrast with Katrina, why was the response to Gustav so much better? It is true that government officials learned from Katrina, but Katrina was just one milestone along the way toward making New Orleans safer. This paper examines prior recent experience with hurricanes in Louisiana, events surrounding Hurricane Gustav, and Figure 1. Track of Hurricane Georges, September how we have learned from other disasters. Not only 20-27, 1998 (Image source: Unisys did Louisiana officials learn from prior hurricanes, http://weather.unisys.com/hurricane/). but those far-removed from the area of impact learned from their own disaster experiences to hurricane Georges was uncoordinated and chaotic. manage the influx of evacuees. The progression of Each parish had its own separate response plan. -
Federal Disaster Assistance After Hurricanes Katrina, Rita, Wilma, Gustav, and Ike
Federal Disaster Assistance After Hurricanes Katrina, Rita, Wilma, Gustav, and Ike Updated February 26, 2019 Congressional Research Service https://crsreports.congress.gov R43139 Federal Disaster Assistance After Hurricanes Katrina, Rita, Wilma, Gustav, and Ike Summary This report provides information on federal financial assistance provided to the Gulf States after major disasters were declared in Alabama, Florida, Louisiana, Mississippi, and Texas in response to the widespread destruction that resulted from Hurricanes Katrina, Rita, and Wilma in 2005 and Hurricanes Gustav and Ike in 2008. Though the storms happened over a decade ago, Congress has remained interested in the types and amounts of federal assistance that were provided to the Gulf Coast for several reasons. This includes how the money has been spent, what resources have been provided to the region, and whether the money has reached the intended people and entities. The financial information is also useful for congressional oversight of the federal programs provided in response to the storms. It gives Congress a general idea of the federal assets that are needed and can be brought to bear when catastrophic disasters take place in the United States. Finally, the financial information from the storms can help frame the congressional debate concerning federal assistance for current and future disasters. The financial information for the 2005 and 2008 Gulf Coast storms is provided in two sections of this report: 1. Table 1 of Section I summarizes disaster assistance supplemental appropriations enacted into public law primarily for the needs associated with the five hurricanes, with the information categorized by federal department and agency; and 2. -
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. -
Hurricane Ike Prepared by the U.S
Impact Report SPECIAL NEEDS POPULATIONS IMPACT ASSESSMENT SOURCE DOCUMENT Emergency Support Function #14 Long Term Community Recovery Hurricane Ike Prepared by the U.S. Department of Homeland Security Office for Civil Rights and Civil Liberties October 2008 About This Impact Assessment The following Impact Assessment examines the long term community recovery needs facing special needs populations affected by Hurricane Ike. It was prepared by the U.S. Department of Homeland Security's Office for Civil Rights and Civil Liberties, utilizing the insights of state, local, and nongovernmental organizations representing special needs populations in East Texas. The Impact Assessment was submitted to FEMA's Long Term Community Recovery Branch (Emergency Support Function 14) in October 2008. This Impact Assessment served as the source document for considerations related to special needs populations contained within "Hurricane Ike Impact Report," issued in December 2008. The document may be accessed at http://www.disabilitypreparedness.gov. For questions related to this Impact Assessment, contact Brian Parsons at [email protected]. Table of Contents I. EXECUTIVE SUMMARY ................................................................................................ 4 II. DEFINITION OF SPECIAL NEEDS POPULATIONS .................................................... 5 III. PROFILE OF SPECIAL NEEDS POPULATIONS WITHIN THE HURRICANE IKE IMPACT AREA............................................................................................................... -
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. -
Consolidated Report
Sources: ✓ Big Storms Leave Small Marks on the U.S. Economy - Studies show business slows during and after hurricanes hit, but rebuilding leads to a boost in economic activity. ✓ We Looked Into The Effects Of Hurricane Harvey And Here's What We Found - The Effects Of Hurricane Harvey. ✓ Hurricane Harvey could be the costliest natural disaster in US history: here's how we'll know the true cost. – Cost of Harvey. ✓ Hurricane Harvey Facts, Damage and Costs What Made Harvey So Devastating – Facts and damages that made Harvey devastating. ✓ What Harvey taught us: lessons from the energy industry – Harvey’s effect on energy industry. ✓ House Committee on Energy and Commerce: The 2017 Hurricane Season: A Review of Emergency Response and Energy Infrastructure Recovery Efforts. ✓ American Oil Chemist Society: Lessons Learned from Hurricane Harvey. ✓ Eye of the Storm: Rebuild Texas. ✓ Houston and Hurricane Harvey: A call to Action. ✓ Hurricane Harvey Event Recap Report. ✓ North American Electric Reliability Corporation: Hurricane Harvey Event Analysis Report. ✓ Texas Comptroller of Public Accounts: Hurricane Harvey and the Texas Economy. Title: The 2017 Hurricane Season: A Review of Emergency Response and Energy Infrastructure Recovery Efforts Author: American Fuel & Petrochemical Manufacturers Significant Report Findings (include page number): ● Harvey forced 24 refineries representing 25% of U.S. refining capacity to shut down or run at reduced rates. Just two weeks later, refiners were almost fully operational and those still down or in the process of restarting were working to resume operations. (p. 1) ● The impact on the U.S. petrochemical industry was even more pronounced- -at its height the hurricane impacted nearly 60% of U.S. -
Tropical Cyclone Report Hurricane Gustav (AL072008) 25 August – 4 September 2008
Tropical Cyclone Report Hurricane Gustav (AL072008) 25 August – 4 September 2008 John L. Beven II and Todd B. Kimberlain National Hurricane Center 22 January 2009 Revised 15 September 2009 for peak intensity and to add new data Revised 9 September 2014 for U.S. damage Gustav moved erratically through the Greater Antilles into the Gulf of Mexico, eventually making landfall on the coast of Louisiana. It briefly became a category 4 hurricane on the Saffir-Simpson Hurricane Scale and caused many deaths and considerable damage in Haiti, Cuba, and Louisiana. a. Synoptic History Gustav formed from a tropical wave that moved westward from the coast of Africa on 13 August. The wave continued westward across the tropical Atlantic, with the associated shower activity first showing signs of organization on 18 August. Westerly vertical wind shear, however, prevented significant development for the next several days. The wave moved through the Windward Islands on 23 August with a broad area of low pressure accompanied by disorganized shower activity. Organization increased late on 24 August as the system moved northwestward across the southeastern Caribbean Sea, and it is estimated that a tropical depression formed near 0000 UTC 25 August about 95 n mi northeast of Bonaire in the Netherland Antilles. The “best track” chart of the tropical cyclone’s path is given in Fig. 1, with the wind and pressure histories shown in Figs. 2 and 3, respectively. The best track positions and intensities are listed in Table 11. The depression formed a small inner wind core during genesis with a radius of maximum winds of less than 10 n mi.