Hurricane Preparedness Guide for Parishes & Schools
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Waste Management Strategy for the British Virgin Islands Ministry of Health & Social Development
FINAL REPORT ON WASTE MANAGEMENT WASTE CHARACTERISATION STRATEGY FOR THE BRITISH J U L Y 2 0 1 9 VIRGIN ISLANDS Ref. 32-BV-2018Waste Management Strategy for the British Virgin Islands Ministry of Health & Social Development TABLE OF CONTENTS LIST OF ACRONYMS..............................................................................2 1 INTRODUCTION.........................................................3 1.1 BACKGROUND OF THE STUDY..........................................................3 1.2 SUBJECT OF THE PRESENT REPORT..................................................3 1.3 OBJECTIVE OF THE WASTE CHARACTERISATION................................3 2 METHODOLOGY.........................................................4 2.1 ORGANISATION AND IMPLEMENTATION OF THE WASTE CHARACTERISATION....................................................................4 2.2 LIMITATIONS AND DIFFICULTIES......................................................6 3 RESULTS...................................................................7 3.1 GRANULOMETRY.............................................................................7 3.2 GRANULOMETRY.............................................................................8 3.2.1 Overall waste composition..................................................................8 3.2.2 Development of waste composition over the years..........................11 3.2.3 Waste composition per fraction........................................................12 3.3 STATISTICAL ANALYSIS.................................................................17 -
BUYOUTS and BEYOND: Politics, Planning, and the Future of Staten Island's East Shore After Superstorm Sandy
BUYOUTS AND BEYOND: Politics, Planning, and the Future of Staten Island’s East Shore After Superstorm Sandy By Alexander F. Brady B.A. Comparative Literature Princeton University, 2010 SUBMITTED TO THE DEPARTMENT OF URBAN STUDIES AND PLANNING IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER IN CITY PLANNING AT THE MASSACHUSETTS INSTITUTE OF TECHNOLOGY JUNE 2015 ©2015 Alexander F. Brady. All Rights Reserved. The author hereby grants to MIT permission to reproduce and to distribute publicly paper and electronic copies of this thesis document in whole or in part in any medium now known or hereafter created. Signature of Author ____________________________________________________________________________________ Department of Urban Studies and Planning May 18, 2015 Certified by ____________________________________________________________________________________________ Professor Lawrence J. Vale Department of Urban Studies and Planning Thesis Supervisor Accepted by ___________________________________________________________________________________________ Professor Dennis Frenchman Chair, MCP Committee Department of Urban Studies and Planning BUYOUTS AND BEYOND: Politics, Planning, and the Future of Staten Island’s East Shore After Superstorm Sandy By Alexander F. Brady B.A. Comparative Literature Princeton University, 2010 Submitted to the Department of Urban Studies and Planning on May 18th, 2015 in Partial Fulfillment of the Requirements for the Degree of Master in City Planning ABSTRACT In the aftermath of Superstorm Sandy, two separate, federally funded programs began purchasing storm-damaged homes from voluntary sellers in the low-lying, working- class communities of Staten Island’s East Shore. New York State’s, offered in three specific, geographically bounded neighborhoods, requires that the land procured be preserved as open space. The City’s acquires any substantially damaged properties, with the goal of redeveloping them as more resilient housing. -
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 -
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. -
UB Powerpoint Template
converge.colorado.edu CONVERGE ethical, coordinated, and scientifically rigorous social science, engineering, and interdisciplinary extreme events research Lori Peek Principal Investigator, CONVERGE, SSEER, and ISEEER Director, Natural Hazards Center Professor, Department of Sociology University of Colorado Boulder Session 2: Collecting, Managing, and Archiving Social and Behavioral Science Data Describe opportunities for identifying and coordinating social science researchers so that we can best share information and publish our data as well as data collection protocols using DOIs, repositories, etc. Discuss some of the overarching challenges and concerns with sharing social science data, such as privacy, data management plans and related IRB policies, duplication vs. replication, etc. converge.colorado.edu 4 Things converge.colorado.edu 1. NSF has funded the CONVERGE initiative converge.colorado.edu Why CONVERGE? Why CONVERGE? • identify and coordinate researchers and research teams; • advance hazards and disaster research; • encourage the publication of data and data collection instruments and protocols (DesignSafe Cyberinfrastructure + CONVERGE). • support and accelerate training and mentoring; • fund virtual reconnaissance, field research, and the development of novel research instruments and data collection protocols; • accelerate the development of mobile applications for social science data collection (NHERI RAPID); Why CONVERGE? 2. NSF Supports Extreme Events Research (EER) Networks converge.colorado.edu Why the EER’s? Disciplinary -
Richmond, VA Hurricanes
Hurricanes Influencing the Richmond Area Why should residents of the Middle Atlantic states be concerned about hurricanes during the coming hurricane season, which officially begins on June 1 and ends November 30? After all, the big ones don't seem to affect the region anymore. Consider the following: The last Category 2 hurricane to make landfall along the U.S. East Coast, north of Florida, was Isabel in 2003. The last Category 3 was Fran in 1996, and the last Category 4 was Hugo in 1989. Meanwhile, ten Category 2 or stronger storms have made landfall along the Gulf Coast between 2004 and 2008. Hurricane history suggests that the Mid-Atlantic's seeming immunity will change as soon as 2009. Hurricane Alley shifts. Past active hurricane cycles, typically lasting 25 to 30 years, have brought many destructive storms to the region, particularly to shore areas. Never before have so many people and so much property been at risk. Extensive coastal development and a rising sea make for increased vulnerability. A storm like the Great Atlantic Hurricane of 1944, a powerful Category 3, would savage shorelines from North Carolina to New England. History suggests that such an event is due. Hurricane Hazel in 1954 came ashore in North Carolina as a Category 4 to directly slam the Mid-Atlantic region. It swirled hurricane-force winds along an interior track of 700 miles, through the Northeast and into Canada. More than 100 people died. Hazel-type wind events occur about every 50 years. Areas north of Florida are particularly susceptible to wind damage. -
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 Dorian Hits Eastern NC by Chris Collins, Meteorologist
National Weather Service, Newport/Morehead City, NC http://weather.gov/Newport —> Bookmark it!! Fall 2019 Edition Hurricane Dorian hits Eastern NC By Chris Collins, Meteorologist Hurricane Dorian was the fourth named storm, second hurricane, and first major hurri- cane of the 2019 Atlantic hurricane season. Dorian formed on August 24, 2019 from a tropical wave in the Central Atlantic and gradually strengthened as it moved toward the Lesser Antilles, becoming a hurricane on August 28. Rapid intensification occurred, and on August 31, Dorian became a Category 4 hurricane. On September 1, Dorian reached Category 5 intensity, with maximum sustained winds of 185 mph, and a minimum central pressure of 910 mb, while making landfall in Elbow Cay, Bahamas. The ridge of high pressure steering Dorian westward collapsed on September 2, causing Dorian to stall just north of Grand Bahama for about a day. It is the strongest known tropical system to impact the Bahamas. On the morning of September 3, Dorian began to move slowly to- wards the north-northwest. Dorian moved over warmer waters, regaining Category 3 in- tensity by midnight on September 5. In the early hours of September 6, Dorian weakened to Category 1 intensity as it picked up speed and turned northeast. Dorian would pick up speed and move northeast along the North Carolina coast September 6, moving just south of the Crystal Coast, clipping Cape Lookout and eventually making landfall at Cape Hat- teras. CONTENTS Hurricane Dorian 1-2 Skywarn Recognition Day 3 Summer Volunteer 2019 4 Saharan Dust 5 July Heat 6 Path of Hurricane Dorian, August 24-September 6, 2019. -
Hurricanes of 1955 Gordon E
DECEMBEB1955 MONTHLY WEATHER REVIEW 315 HURRICANES OF 1955 GORDON E. DUNN, WALTER R. DAVIS, AND PAUL L. MOORE Weather Bureau Offrce, Miami, Fla. 1. GENERAL SUMMARY grouping i,n theirpaths. Thethree hurricanes entering the United States all crossed the North Carolina coast There were 13 tropical storms in 1955, (fig. 9), of which within a 6-week period and three more crossed the Mexican 10 attained hurricane force, a number known to have been coast within 150 miles of Tampico within a period of 25 exceeded only once before when 11 hurricanes were re- days. corded in 1950. This compares with a normal of about The hurricane season of 1955 was the most disastrous 9.2 tropical storms and 5 of hurricane intensity. In con- in history and for the second consecutive year broke all trast to 1954, no hurricanes crossed the coastline north of previous records for damage. Hurricane Diane was Cape Hatteras andno hurricane winds were reported north undoubtedly the greatest natural catastrophe in the his- of that point. No tropical storm of hurricane intensity tory of the United Statesand earned the unenviable affected any portion of the United States coastline along distinction of “the first billion dollar hurricane”. While the Gulf of Mexico or in Florida for the second consecutive the WeatherBureau has conservatively estimated the year. Only one hurricane has affected Florida since 1950 direct damage from Diane at between $700,000,000 and and it was of little consequence. However, similar hurri- $800,000,000, indirect losses of wages, business earnings, cane-free periods have occurred before. -
Service Assessment Hurricane Irene, August
Service Assessment Hurricane Irene, August 21–30, 2011 U.S. DEPARTMENT OF COMMERCE National Oceanic and Atmospheric Administration National Weather Service Silver Spring, Maryland Cover Photographs: Top Left - NOAA GOES 13 visible image of Hurricane Irene taken at 12:32 UTC (8:32 a.m. EDT) on August 27, 2011, as it was moving northward along the east coast. Map of total storm rainfall for Hurricane Irene (NCEP/HPC) overlaid with photos of Hurricane Irene’s impacts. Clockwise from top right: • Damage to bridge over the Pemigewasset River/East Branch in Lincoln, NH (NH DOT) • Trees across road and utility lines in Guilford, CT (CT DEP) • Damage to homes from storm surge at Cosey Beach, East Haven, CT (CT DEP) • Flooding of Delaware River closes Rt. 29 in Trenton, NJ (State of New Jersey, Office of the Governor) • Damage from storm surge on North Carolina’s Outer Banks (USGS) • Damage to home from an EF1 tornado in Lewes, DE (Sussex County, DE EOC) • River flooding on Schoharie Creek near Lexington, NY (USGS) • Flood damage to historic covered bridge and road in Quechee, VT (FEMA) ii Service Assessment Hurricane Irene, August 21–30, 2011 September 2012 National Oceanic and Atmospheric Administration Dr. Jane Lubchenco, Administrator National Weather Service Laura Furgione, Acting Assistant Administrator for Weather Services iii Preface On August 21-29, 2011, Hurricane Irene left a devastating imprint on the Caribbean and U.S. East Coast. The storm took the lives of more than 40 people, caused an estimated $6.5 billion in damages, unleashed major flooding, downed trees and power lines, and forced road closures, evacuations, and major rescue efforts. -
Sustaining Category Five Hurricane Intensity by Greg Machos
Sustaining Category Five Hurricane Intensity By Greg Machos Thermodynamics of the Atmosphere Dr. Alan Robock November 20, 2003 Sustaining Category Five Hurricane Intensity 2 Abstract Category Five Hurricanes are a rare phenomenon in nature. Of all the hurricanes ever recorded in the Atlantic, these extremely intense storms only account for less than five percent. Nevertheless, they represent a hurricane in its most perfect form with winds exceeding 69 ms-1, a very clear and narrow eye, excellent outflow, or exhaust, and an organized mass of clouds encompassing the eye called the central dense overcast. Fortunately for those living along the coastal regions of the United States, Category Five Hurricanes are unable to maintain this intensity for very long due to internal changes from within the system such as eyewall replacement, and changes external to the system from its surrounding environment such as cooler sea surface temperatures, dry air intrusion, and moderate to high upper level wind shear. These internal and external changes disturb the highly efficient, yet delicate heat engine of such an extremely powerful storm just enough so that it becomes unstable and cause things like concentric eyewalls or lower temperature gradients between the ocean surface below the hurricane and the high cloud tops at the height of the hurricane to occur. Consequently, the duration of Category Five Hurricane intensity is usually brief. Sustaining Category Five Hurricane Intensity 3 Introduction A hurricane is one of the most fascinating phenomena in nature. Viewed from space, a mature hurricane can be absolutely breathtaking with its well-defined eye, distinct outflow, and highly organized central dense overcast. -
August 12, 1955 Hurricane Connie Was Also a Flood Maker in The
August 12, 1955 Connie weakened while slowing and turning to the north, and struck North Carolina on August 12 as a Category 2 hurricane. Connie produced strong winds, high tides, and heavy rainfall as it moved ashore, causing heavy crop damage and 27 deaths in the state of North Carolina. Connie made a second landfall in Virginia, and it progressed inland until dissipating on August 15 near Sault Ste. Marie, Michigan. Four people were killed in Washington, D.C. due to a traffic accident. In the Chesapeake Bay, Connie capsized a boat, killing 14 people and prompting a change in Coast Guard regulation. There were six deaths each in Pennsylvania and New Jersey, and eleven deaths in New York, where record rainfall flooded homes and subways. At least 225,000 people lost power during the storm. Damage in the United States totaled around $86 million, although the rains from Connie was a prelude to flooding by Hurricane Diane. Hurricane Connie was also a flood maker in the Richmond area dumping 8.71 inches of rain on the 12th. Connie deposited 5-10 inches of rain within 100 miles of its track but gave Richmond little in the way of wind. Hurricane Diane A tropical wave spawned a tropical depression between the Lesser Antilles and Cape Verde on August 7. It slowly strengthened and became Tropical Storm Diane on August 9. After a Fujiwhara interaction defined as when two nearby cyclonic vortices orbit each other and close the distance between the circulations of their corresponding low-pressure areas. Hurricane Connie, Diane had such an interaction curved northward or north-northeastward and quickly deepened.