Hurricane Katrina August 23-31, 2005
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Keepin' Your Head Above Water
Know Your Flood Protection System Keepin’ Your Head Above Water Middle School Science Curriculum Published by the Flood Protection Authority – East floodauthority.org Copyright 2018 Keepin’ Your Head Above Water: Know Your Flood Protection System PREFACE Purpose and Mission Our mission is to ensure the physical and operational integrity of the regional flood risk management system in southeastern Louisiana as a defense against floods and storm surge from hurricanes. We accomplish this mission by working with local, regional, state, and federal partners to plan, design, construct, operate and maintain projects that will reduce the probability and risk of flooding for the residents and businesses within our jurisdiction. Middle School Science Curriculum This Middle School Science Curriculum is part of the Flood Protection Authority – East’s education program to enhance understanding of its mission. The purposes of the school program are to ensure that future generations are equipped to deal with the risks and challenges associated with living with water, gain an in-depth knowledge of the flood protection system, and share their learning experiences with family and friends. The curriculum was developed and taught by Anne Rheams, Flood Protection Authority – East’s Education Consultant, Gena Asevado, St. Bernard Parish Public Schools’ Science Director, and Alisha Capstick, 8th grade Science Teacher at Trist Middle School in Meraux. La. The program was encouraged and supported by Joe Hassinger, Board President of the Flood Protection Authority – East and Doris Voitier, St. Bernard Parish Public Schools Superintendent. The curriculum was developed in accordance with the National Next Generation Science Standards and the Louisiana Department of Education’s Performance Expectations. -
After Hurricane Katrina: a Review of Community Engagement Activities and Initiatives
After Hurricane Katrina: a review of community engagement activities and initiatives August 2019 Summary This review examines how communities took control of their response to Hurricane Katrina through intracommunity engagement initiatives and how communities affected by Hurricane Katrina were engaged by organisations after the disaster occurred. This examination includes an overview of what ‘went well’ and what problems arose in those engagement efforts. The review indicates that communities were not passive in accepting decisions made by authorities that had not engaged with their wishes: where intracommunity decisions had been made, those communities fought for those choices to be upheld by authorities. Where organisations launched engagement activities, several focused on poor neighbourhoods that were badly affected by Katrina, and the children and young people living there. Fewer examples were identified of older people’s engagement by organisations or programmes. Engagement initiatives identified were, in several cases, reflective of the cultural context of the areas affected by Katrina: in particular, music played a key role in successful community engagement initiatives. Background 1 Hurricane Katrina hit the Gulf Coast of the United States in August 2005. New Orleans was flooded as a result of levees failing, and approximately 80 per cent of the city’s population was forced to evacuate.1 President George W Bush declared a state of emergency in Louisiana, Alabama, and Mississippi on 27 August 2005, which preceded mandatory evacuation orders in several affected areas of these states, including New Orleans. Many people living in poorer areas of the city were not 1 Institute of Medicine of the National Academies (2015) Health, resilient, and sustainable communities after disasters: strategies, opportunities, and planning for recovery, available at: https://dornsife.usc.edu/assets/sites/291/docs/AdaptLA_Workshops/Healthy_Resilient_Sustainable_C ommunities_After_Disasters.pdf, at page 244. -
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. -
Hurricanes Katrina and Rita – Louisiana's Response And
HURRICANES KATRINA AND RITA – LOUISIANA’S RESPONSE AND RECOVERY Ray A. Mumphrey, P.E., Louisiana Department of Transportation and Development, Baton Rouge, Louisiana, and Hossein Ghara, P.E., MBA, Louisiana Department of Transportation and Development, Baton Rouge, Louisiana KEYWORDS: Louisiana Department of Transportation and Development, National Oceanic and Atmospheric Administration, Federal Emergency Management Agency, Contra flow, Inundation, Fixed and Movable Bridges, Open Water Bridges, Coastal Protection and Restoration Authority ABSTRACT: Louisiana’s transportation and hurricane protection system took a tremendous blow from two major hurricanes that struck the coast of Louisiana in 2005, hurricanes Katrina and Rita. This presentation will introduce the audience to the transportation infrastructure damage Louisiana experienced as a result of these two storms and will describe how Louisiana is responding to the disasters and our road to recovery. Figure 1 - Hurricanes that hit the coast of Louisiana since 1900 As Louisiana residents, we become accustom to the ever present threat of hurricanes. Refer to figure 1. Much like other parts of the country, which have other natural disasters such as tornados, mud slides, avalanches or earthquakes, we just prepare for the worst, minimize loss of life and property, and thank God when it’s all over. As engineers we know we can always rebuild structures, and possibly restore livelihoods, but loss of life is not replaceable. 2005 STORMS Hurricane Katrina was a category 4 storm when it made landfall on August 29, 2005, along the Louisiana – Mississippi Gulf Coast. The storm was fast moving and provided minimum time for preparation. Refer to figure 2. “Hurricane Katrina was the most destructive hurricane to ever strike the U.S.” NOAA Just as we were getting back on our feet from the impacts of Hurricane Katrina, BAM! We were faced with another storm, Rita. -
Significant Loss Report
NATIONAL FLOOD INSURANCE PROGRAM Bureau and Statistical Agent W-01049 3019-01 MEMORANDUM TO: Write Your Own (WYO) Principal Coordinators and NFIP Servicing Agent FROM: WYO Clearinghouse DATE: July 18, 2001 SUBJECT: Significant Loss Report Enclosed is a listing of significant flooding events that occurred between February 1978 and October 2000. Only those events that had more than 1500 losses are included on the list. These data were compiled for WYO Companies and others to use to remind their customers of the impact of past flooding events. Please use this information in your marketing efforts as you feel it is appropriate. If you have any questions, please contact your WYO Program Coordinator. Enclosure cc: Vendors, IBHS, FIPNC, WYO Standards Committee, WYO Marketing Committee, ARCHIVEDGovernment Technical Representative APRIL 2018 Suggested Routing: Claims, Marketing, Underwriting 7700 HUBBLE DRIVE • LANHAM, MD 20706 • (301) 731-5300 COMPUTER SCIENCES CORPORATION, under contract to the FEDERAL EMERGENCY MANAGEMENT AGENCY, is the Bureau and Statistical Agent for the National Flood Insurance Program NATIONAL FLOOD INSURANCE PROGRAM SIGNIFICANT FLOOD EVENTS REPORT EVENT YEAR # PD LOSSES AMOUNT PD ($) AVG PD LOSS Massachusetts Flood Feb. 1978 Feb-78 2,195 $20,081,479 $9,149 Louisiana Flood May 1978 May-78 7,284 $43,288,709 $5,943 WV, IN, KY, OH Floods Dec 1978 Dec-78 1,879 $11,934,512 $6,352 PA, CT, MA, NJ, NY, RI Floods Jan-79 8,826 $31,487,015 $3,568 Texas Flood April 1979 Apr-79 1,897 $19,817,668 $10,447 Florida Flood April 1979 Apr-79 -
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. -
Tropical Cyclone Report for Hurricane Ivan
Tropical Cyclone Report Hurricane Ivan 2-24 September 2004 Stacy R. Stewart National Hurricane Center 16 December 2004 Updated 27 May 2005 to revise damage estimate Updated 11 August 2011 to revise damage estimate Ivan was a classical, long-lived Cape Verde hurricane that reached Category 5 strength three times on the Saffir-Simpson Hurricane Scale (SSHS). It was also the strongest hurricane on record that far south east of the Lesser Antilles. Ivan caused considerable damage and loss of life as it passed through the Caribbean Sea. a. Synoptic History Ivan developed from a large tropical wave that moved off the west coast of Africa on 31 August. Although the wave was accompanied by a surface pressure system and an impressive upper-level outflow pattern, associated convection was limited and not well organized. However, by early on 1 September, convective banding began to develop around the low-level center and Dvorak satellite classifications were initiated later that day. Favorable upper-level outflow and low shear environment was conducive for the formation of vigorous deep convection to develop and persist near the center, and it is estimated that a tropical depression formed around 1800 UTC 2 September. Figure 1 depicts the “best track” of the tropical cyclone’s path. The wind and pressure histories are shown in Figs. 2a and 3a, respectively. Table 1 is a listing of the best track positions and intensities. Despite a relatively low latitude (9.7o N), development continued and it is estimated that the cyclone became Tropical Storm Ivan just 12 h later at 0600 UTC 3 September. -
Ouray County Sheriff's Office Blotter August 23, 2021
Ouray County Sheriff’s Office Blotter August 23, 2021 – August 29, 2021 August 23, 2021 Deputy responded to an Animal Stray on County Road at MM 12 Deputy Assisted a Motorist on County Road 14 and Bighorn Lane Deputy responded to a suspicious report in the 2100 Block of County Road 22 Deputy did a VIN Inspection in the 4000 Block of County Road 12 Deputy did a VIN Inspection in the 500 Block of Badger Trail Deputy responded to Highway 550 for a reported Traffic Complaint Deputy arrested male party with a Warrant on County Road 14 and Gold Mountain Trail Deputy responded to a Bear call in the 36000 Block of Highway 550 Deputy responded to a 911 Open in the 7600 Block of Highway 62 Deputy responded to a Tree Fire on County Road 5 and Green Street Deputy Assisted the Colorado State Patrol on Highway 550 Deputy arrested a female party with a Warrant on County Road 14 and Sunshine Deputy responded to a report of an Overdue Party on Red Mountain Pass August 24, 2021 Deputy did a VIN Inspection at the Ouray County Sheriff’s Office Deputy Assisted the Gunnison County Sheriff’s Office with an Information report in the 5800 Block of County Road 1 Deputy responded to a report of a fall victim in the 100 Block of County Road 24C Deputy responded to a 911 Open call in the 100 Block of Fisher Canyon Drive Deputy did a VIN Inspection in the 400 Block of Snowbush Drive Deputy responded to a Lockout in the 700 Block of County Road 24A August 25, 2021 Deputy responded to a Criminal Mischief at the Blue Lakes Trail Head Deputy took a Lost Property report -
Belize), and Distribution in Yucatan
University of Neuchâtel, Switzerland Institut of Zoology Ecology of the Black Catbird, Melanoptila glabrirostris, at Shipstern Nature Reserve (Belize), and distribution in Yucatan. J.Laesser Annick Morgenthaler May 2003 Master thesis supervised by Prof. Claude Mermod and Dr. Louis-Félix Bersier CONTENTS INTRODUCTION 1. Aim and description of the study 2. Geographic setting 2.1. Yucatan peninsula 2.2. Belize 2.3. Shipstern Nature Reserve 2.3.1. History and previous studies 2.3.2. Climate 2.3.3. Geology and soils 2.3.4. Vegetation 2.3.5. Fauna 3. The Black Catbird 3.1. Taxonomy 3.2. Description 3.3. Breeding 3.4. Ecology and biology 3.5. Distribution and threats 3.6. Current protection measures FIRST PART: BIOLOGY, HABITAT AND DENSITY AT SHIPSTERN 4. Materials and methods 4.1. Census 4.1.1. Territory mapping 4.1.2. Transect point-count 4.2. Sizing and ringing 4.3. Nest survey (from hide) 5. Results 5.1. Biology 5.1.1. Morphometry 5.1.2. Nesting 5.1.3. Diet 5.1.4. Competition and predation 5.2. Habitat use and population density 5.2.1. Population density 5.2.2. Habitat use 5.2.3. Banded individuals monitoring 5.2.4. Distribution through the Reserve 6. Discussion 6.1. Biology 6.2. Habitat use and population density SECOND PART: DISTRIBUTION AND HABITATS THROUGHOUT THE RANGE 7. Materials and methods 7.1. Data collection 7.2. Visit to others sites 8. Results 8.1. Data compilation 8.2. Visited places 8.2.1. Corozalito (south of Shipstern lagoon) 8.2.2. -
A Rapid Forecasting and Mapping System of Storm Surge and Coastal Flooding
AUGUST 2020 Y A N G E T A L . 1663 A Rapid Forecasting and Mapping System of Storm Surge and Coastal Flooding KUN YANG,VLADIMIR A. PARAMYGIN, AND Y. PETER SHENG Department of Civil and Coastal Engineering, University of Florida, Gainesville, Florida (Manuscript received 16 July 2019, in final form 2 March 2020) ABSTRACT A prototype of an efficient and accurate rapid forecasting and mapping system (RFMS) of storm surge is presented. Given a storm advisory from the National Hurricane Center, the RFMS can generate a coastal inundation map on a high-resolution grid in 1 min (reference system Intel Core i7–3770K). The foundation of the RFMS is a storm surge database consisting of high-resolution simulations of 490 optimal storms generated by a robust storm surge modeling system, Curvilinear-Grid Hydrodynamics in 3D (CH3D-SSMS). The RFMS uses an efficient quick kriging interpolation scheme to interpolate the surge response from the storm surge database, which considers tens of thousands of combinations of five landfall parameters of storms: central pressure deficit, radius to maximum wind, forward speed, heading direction, and landfall location. The RFMS is applied to southwest Florida using data from Hurricane Charley in 2004 and Hurricane Irma in 2017, and to the Florida Panhandle using data from Hurricane Michael in 2018 and validated with observed high water mark data. The RFMS results agree well with observation and direct simulation of the high-resolution CH3D- SSMS. The RFMS can be used for real-time forecasting during a hurricane or ‘‘what-if’’ scenarios for miti- gation planning and preparedness training, or to produce a probabilistic flood map. -
Hurricane and Tropical Storm
State of New Jersey 2014 Hazard Mitigation Plan Section 5. Risk Assessment 5.8 Hurricane and Tropical Storm 2014 Plan Update Changes The 2014 Plan Update includes tropical storms, hurricanes and storm surge in this hazard profile. In the 2011 HMP, storm surge was included in the flood hazard. The hazard profile has been significantly enhanced to include a detailed hazard description, location, extent, previous occurrences, probability of future occurrence, severity, warning time and secondary impacts. New and updated data and figures from ONJSC are incorporated. New and updated figures from other federal and state agencies are incorporated. Potential change in climate and its impacts on the flood hazard are discussed. The vulnerability assessment now directly follows the hazard profile. An exposure analysis of the population, general building stock, State-owned and leased buildings, critical facilities and infrastructure was conducted using best available SLOSH and storm surge data. Environmental impacts is a new subsection. 5.8.1 Profile 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 (National Oceanic and Atmospheric Administration [NOAA] 2013a). 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. -
10R.3 the Tornado Outbreak Across the North Florida Panhandle in Association with Hurricane Ivan
10R.3 The Tornado Outbreak across the North Florida Panhandle in association with Hurricane Ivan Andrew I. Watson* Michael A. Jamski T.J. Turnage NOAA/National Weather Service Tallahassee, Florida Joshua R.Bowen Meteorology Department Florida State University Tallahassee, Florida Jason C. Kelley WJHG-TV Panama City, Florida 1. INTRODUCTION their mobile homes were destroyed near Blountstown, Florida. Hurricane Ivan made landfall early on the morning of 16 September 2004, just west of Overall, there were 24 tornadoes reported Gulf Shores, Alabama as a category 3 across the National Weather Service (NWS) hurricane on the Saffir-Simpson Hurricane Tallahassee forecast area. The office issued Scale. Approximately 117 tornadoes were 130 tornado warnings from the afternoon of 15 reported associated with Ivan across the September until just after daybreak on 16 southeast United States. Eight people were September. killed and 17 were injured by tornadoes (Storm Data 2004; Stewart 2004). The most The paper examines the convective cells significant tornadoes occurred as hurricane within the rain bands of hurricane Ivan, which Ivan approached the Florida Gulf coast on the produced these tornadoes across the Florida afternoon and evening of 15 September. Panhandle, Big Bend, and southwest Georgia. The structure of the tornadic and non-tornadic The intense outer rain bands of Ivan supercells is examined for clues on how to produced numerous supercells over portions better warn for these types of storms. This of the Florida Panhandle, Big Bend, southwest study will focus on the short-term predictability Georgia, and Gulf coastal waters. In turn, of these dangerous storms, and will these supercells spawned dozens of investigate the problem of how to reduce the tornadoes.