Hurricane/Blizzard/Storm Damage, 1933 - : Guide
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Guidelines for Storm Preparedness
Eleven Days after Hurricane Carol slammed the Island in August 1964, Hurricane Edna struck on September 11, flooding Edgartown (Vineyard Gazette Archive) Guidelines for Storm Preparedness West Tisbury Climate Action Committee May 2020 May 3-9, 2020: Hurricane Preparedness Week National Weather Service 1 of 11 Storm Preparedness It should come as no surprise that Martha’s Vineyard is vulnerable Nor’easter storms formed over the cold Atlantic between September and April; and hurricanes formed over warm tropical waters from June to November. The absence of hurricanes in recent years have lulled some into thinking they are no longer a serious threat to the Vineyard. The truth is that storms and hurricanes will lash the Vineyard, flooding low-lying portions of our villages, uprooting trees, bringing down power lines, snatching boats from their moorings, and disruption ferry service to the mainland. It is not a question of if; it is a matter of when and with what degree of severity. What is equally sure is that with a modicum of preparedness, your chances of riding out a storm and coping with the inevitable disruptions in the aftermath — the loss of power, telephone and internet connections, and delayed resupplying from the mainland — increase substantially. This manual breaks down emergency preparedness into stages; What you can do immediately without a storm in sight. What you can do when you know a storm is on its way. And, what you can do to make your surroundings as safe as possible when the storm hits. Storm risk varies by the size and path of the storm and by the population of the Vineyard. -
ABSTRACT Title of Document: the EFFECT of HURRICANE SANDY
ABSTRACT Title of Document: THE EFFECT OF HURRICANE SANDY ON NEW JERSEY ATLANTIC COASTAL MARSHES EVALUATED WITH SATELLITE IMAGERY Diana Marie Roman, Master of Science, August 2015 Directed By: Professor, Michael S. Kearney, Environmental Science and Technology Hurricane Sandy, one of several large extratropical hurricanes to impact New Jersey since 1900, produced some of the most extensive coastal destruction within the last fifty years. Though the damage to barrier islands from Sandy was well-documented, the effect of Sandy on the New Jersey coastal marshes has not. The objective of this analysis, based on twenty-three Landsat Thematic Mapper (TM) data sets collected between 1984 and 2011 and Landsat 8 Operational Land Imager (OLI) images collected between 2013 and 2014 was to determine the effect of Hurricane Sandy on the New Jersey Atlantic coastal marshes. Image processing was performed using ENVI image analysis software with the NDX model (Rogers and Kearney, 2004). Results support the conclusion that the marshes were stable between 1984 and 2006, but had decreased in vegetation density coverage since 2007. Hurricane Sandy caused the greatest damage to low-lying marshes located close to where landfall occurred. THE EFFECT OF HURRICANE SANDY ON NEW JERSEY ATLANTIC COASTAL MARSHES EVALUATED WITH SATELLITE IMAGERY by Diana Marie Roman Thesis submitted to the Faculty of the Graduate School of the University of Maryland, College Park in partial fulfillment of the requirements for the degree of Masters of Science 2015 Advisory Committee: Professor Michael Kearney, Chair Professor Andrew Baldwin Associate Professor Andrew Elmore © Copyright by Diana Marie Roman 2015 Forward Hurricane storm impacts on coastal salt marshes have increased over time. -
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. -
2014 New York Hazard Mitigation Plan Hurricane Section 3.12: HURRICANE (Tropical/ Coastal Storms/ Nor’Easter)
2014 New York Hazard Mitigation Plan Hurricane Section 3.12: HURRICANE (Tropical/ Coastal Storms/ Nor’easter) 2014 SHMP Update Reformatted 2011 Mitigation Plan into 2014 Update outline Added Tropical Storms, Coastal Storms, & Nor’easter hazards to Hurricane Profile Added new key terms to 2011 Mitigation Plan’s list of terms Updated past hurricane occurrences section Inserted Events and Losses table Inserted new Hurricane Events and Property Losses maps Added information on New York Bight Added active State development projects 3.12.1 Hurricane (Tropical/ Coastal Storms/ Nor’easters) Profile Coastal storms, including Nor’easters, tropical storms, and hurricanes can, either directly or indirectly, impact all of New York State. More densely populated and developed coastal areas, such as New York City, are the most vulnerable to hurricane-related damages. Before a storm is classified a hurricane, it must pass through four distinct stages: tropical disturbance, tropical depression, tropical storm and lastly a hurricane. Figure 3.12a: Four Stages of a Hurricane Tropical Disturbance (Stage 1) Tropical Hurricane Depression (Stage 4) (Stage 2) Tropical Storm (Stage 3) 3.12-1 Final Release Date January 4, 2014 2014 New York Hazard Mitigation Plan Hurricane Characteristics Below are some key terms to review relating to hurricanes, tropical storms, coastal storms and nor’easters: Hazard Key Terms and Definition Nor’easter- An intense storm that can cause heavy rain and snow, strong winds, and coastal flooding. Nor’easters have cold, low barometric -
Town of Kent Hazard Mitigation Plan
TOWN OF KENT HAZARD MITIGATION PLAN DECEMBER 2014 MMI #3843-04 Prepared for the: TOWN OF KENT, CONNECTICUT Kent Town Hall 41 Kent Green Boulevard Kent, Connecticut (860) 927-3433 www.townofkentct.com Prepared by: MILONE & MACBROOM, INC. 99 Realty Drive Cheshire, Connecticut 06410 (203) 271-1773 www.miloneandmacbroom.com The preparation of this report has been financed in part through funds provided by the Connecticut Department of Emergency Services and Public Protection (DESPP) Division of Emergency Management and Homeland Security (DEMHS) under a grant from the Federal Emergency Management Agency. The contents of this report reflect the views of the Town of Kent and do not necessarily reflect the official views of DEMHS. The report does not constitute a specification or regulation. Copyright 2014 Milone & MacBroom, Inc. ACKNOWLEDGEMENTS & CONTACT INFORMATION This plan was prepared under the direction of the Town of Kent. The following individual should be contacted with questions or comments regarding the plan: Mr. Bruce Adams First Selectman Town of Kent 41 Kent Green Boulevard Kent, CT 06757 (860) 927-4627 This Natural Hazard Mitigation Plan could not have been completed without the time and dedication of the following individuals at the local level: Mr. Rick Osborne, Highway Department Mr. Bruce Adams, First Selectman The consulting firm of Milone & MacBroom, Inc. (MMI) prepared the subject plan. The following individuals at MMI may be contacted prior to plan adoption with questions or comments using the contact information on the title page or the electronic mail addresses below: Mr. David Murphy, P.E., CFM Associate, Water Resources [email protected] Copyright 2014 Milone & MacBroom, Inc. -
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 Gloria's Potential Storm Surge
NOAA TECHNICAL MEMORANDUM NWS ER-70 HURRICANE GLORIA'S POTENTIAL STORM SURGE Anthony F. Gigi, WSO N~w York, NY (LGA) David A. Wert, WSO Newark, NJ Scientific Services Division Eastern Region Headquarters July 1986 u.s. DEPARTMENT OF I National Oceantc and National Weather COMMERCE Almosphenc Admonostrabon I Servtce ,, NOAA TECHNICAL MEMORANDUM NWS ER-70 HURRICANE GLORIA'S POTENTIAL STORM SURGE Anthony F. Gi gi, WSO New York, NY (LGA) David A. Wert, WSO Newark, NJ Scientific Services Division Eastern Region Headquarters July 1986 .) ' __ / IJ INDEX Introduction. 1 Storm Surges. l Hypothetical High Tide Flooding Damages 2 Maximum Damage Possibilities. 7 Conclusion •... 8 Figures 1 through 4 - Actual Storm Surges Which Accompanied Hurricane Gloria During Low-Tide Figure 1 - Bergen Point Figure 2 - Sandy Hook Figure 3 - The Battery Figure 4 - Willets Point Figures 5 through 8 - Hypothetical Storm Surges Which Would Have Accompanied Hurricane Gloria During High-Tide Figure 5 - The Battery Figure 6 - Willets Point Figure 7 - Bergen Point Figure 8 - Sandy Hook Reference Maps Map 1 - Battery Tide, Bergen Point, and Willets Point gauges; JFK, LaGuardia, Newark, and Teterboro Airports Map 2 - Sandy Hook gauge and u.s. Military Reservation Map 3 - Long Island \J J -------------------------- - --- --- ------ Introduction Hurricane Gloria threatened residents of the New York City metropolitan area on Friday, September 27, 1985. Gloria was one of the strongest north atlantic hurricanes of the century, yet the area never received the full fury of the storm due to the following reasons: 1) The upper right hand quadrant (in this case the northeast quadrant) of a hurricane usually contains the strongest winds and most damaging storm surges. -
Verification of a Storm Surge Modeling System for the New York City – Long Island Region
Verification of a Storm Surge Modeling System for the New York City – Long Island Region A Thesis Presented By Thomas Di Liberto to The Graduate School in Partial Fulfillment of the Requirements for the Degree of Master of Science in Marine and Atmospheric Science Stony Brook University August 2009 Stony Brook University The Graduate School Thomas Di Liberto We, the thesis committee for the above candidate for the Master of Science degree, hereby recommend acceptance of this thesis. Dr. Brian A. Colle, Thesis Advisor Associate Professor School of Marine and Atmospheric Sciences Dr. Malcolm J. Bowman, Thesis Reader Professor School of Marine and Atmospheric Sciences Dr. Edmund K.M. Chang, Thesis Reader Associate Professor School of Marine and Atmospheric Sciences This thesis is accepted by the Graduate School Lawrence Martin Dean of the Graduate School ii Abstract of the Thesis Verification of a Storm Surge Modeling System for the New York City – Long Island Region by Thomas Di Liberto Master of Science in Marine and Atmospheric Science Stony Brook University 2009 Storm surge from tropical cyclones events nor‟ easters can cause significant flooding problems for the New York City (NYC) – Long Island region. However, there have been few studies evaluating the simulated water levels and storm surge during a landfalling hurricane event over NYC-Long Island as well as verifying real-time storm surge forecasting systems for NYC-Long Island over a cool season. Hurricane Gloria was simulated using the Weather Research and Forecasting (WRF) V2.1 model, in which different planetary boundary layer (PBL) and microphysics schemes were used to create an ensemble of hurricane landfalls over Long Island. -
Case 12-E-0283
STATE OF NEW YORK DEPARTMENT OF PUBLIC SERVICE Case 12-E-0283 In the Matter of the Review of Long Island Power Authority’s Preparedness and Response to Hurricane Irene June 2012 TABLE OF CONTENTS Page 1. EXECUTIVE SUMMARY ............................................................................................................. 1 Tropical Storm Irene ............................................................................................................... 3 Overall Conclusions ............................................................................................................... 4 Recommendation Summary .................................................................................................. 6 II. ELECTRIC OPERATION STORM PREPARATION ................................................................ 8 A. Overview of Storm Preparation Activities ................................................................ 8 B. Emergency Response Plans ......................................................................................... 8 C. Emergency Operations Center Preparation ............................................................ 13 D. Crew Resources ........................................................................................................... 14 E. Alert Levels and Damage Prediction ....................................................................... 16 III. STORM RESPONSE .................................................................................................................... 20 A. Overview -
Historical Perspective
kZ _!% L , Ti Historical Perspective 2.1 Introduction CROSS REFERENCE Through the years, FEMA, other Federal agencies, State and For resources that augment local agencies, and other private groups have documented and the guidance and other evaluated the effects of coastal flood and wind events and the information in this Manual, performance of buildings located in coastal areas during those see the Residential Coastal Construction Web site events. These evaluations provide a historical perspective on the siting, design, and construction of buildings along the Atlantic, Pacific, Gulf of Mexico, and Great Lakes coasts. These studies provide a baseline against which the effects of later coastal flood events can be measured. Within this context, certain hurricanes, coastal storms, and other coastal flood events stand out as being especially important, either Hurricane categories reported because of the nature and extent of the damage they caused or in this Manual should be because of particular flaws they exposed in hazard identification, interpreted cautiously. Storm siting, design, construction, or maintenance practices. Many of categorization based on wind speed may differ from that these events—particularly those occurring since 1979—have been based on barometric pressure documented by FEMA in Flood Damage Assessment Reports, or storm surge. Also, storm Building Performance Assessment Team (BPAT) reports, and effects vary geographically— Mitigation Assessment Team (MAT) reports. These reports only the area near the point of summarize investigations that FEMA conducts shortly after landfall will experience effects associated with the reported major disasters. Drawing on the combined resources of a Federal, storm category. State, local, and private sector partnership, a team of investigators COASTAL CONSTRUCTION MANUAL 2-1 2 HISTORICAL PERSPECTIVE is tasked with evaluating the performance of buildings and related infrastructure in response to the effects of natural and man-made hazards. -
MASARYK UNIVERSITY BRNO Diploma Thesis
MASARYK UNIVERSITY BRNO FACULTY OF EDUCATION Diploma thesis Brno 2018 Supervisor: Author: doc. Mgr. Martin Adam, Ph.D. Bc. Lukáš Opavský MASARYK UNIVERSITY BRNO FACULTY OF EDUCATION DEPARTMENT OF ENGLISH LANGUAGE AND LITERATURE Presentation Sentences in Wikipedia: FSP Analysis Diploma thesis Brno 2018 Supervisor: Author: doc. Mgr. Martin Adam, Ph.D. Bc. Lukáš Opavský Declaration I declare that I have worked on this thesis independently, using only the primary and secondary sources listed in the bibliography. I agree with the placing of this thesis in the library of the Faculty of Education at the Masaryk University and with the access for academic purposes. Brno, 30th March 2018 …………………………………………. Bc. Lukáš Opavský Acknowledgements I would like to thank my supervisor, doc. Mgr. Martin Adam, Ph.D. for his kind help and constant guidance throughout my work. Bc. Lukáš Opavský OPAVSKÝ, Lukáš. Presentation Sentences in Wikipedia: FSP Analysis; Diploma Thesis. Brno: Masaryk University, Faculty of Education, English Language and Literature Department, 2018. XX p. Supervisor: doc. Mgr. Martin Adam, Ph.D. Annotation The purpose of this thesis is an analysis of a corpus comprising of opening sentences of articles collected from the online encyclopaedia Wikipedia. Four different quality categories from Wikipedia were chosen, from the total amount of eight, to ensure gathering of a representative sample, for each category there are fifty sentences, the total amount of the sentences altogether is, therefore, two hundred. The sentences will be analysed according to the Firabsian theory of functional sentence perspective in order to discriminate differences both between the quality categories and also within the categories. -
Coastal Storms Are a Reality for New York City, Arriving As Hurricanes, Tropical Cyclones ,And Nor’Easters When Certain Meteorological Conditions Converge
CToaS AL STORMS CHAPTER 4.1 Coastal storms are a reality for New York City, arriving as hurricanes, tropical cyclones ,and nor’easters when certain meteorological conditions converge. Not only dangerous, these storms can be deadly, sustaining destructive winds, heavy rainfall, storm surge, coastal flooding, and erosion. Climate change and rising sea levels are likely to worsen their impacts. W HAT IS THE HAZARD? TROPICAL cycLONES Tropical cyclones are organized areas of precipitation and thunderstorms that form over warm tropical ocean waters and rotate counterclockwise around a low pressure center. Such storms are classified as follows: • A tropical depression is an organized system of clouds and thunderstorms with a defined low pressure center and maximum sustained winds of 38 miles per hour (mph) or less. • A tropical storm is an organized system of strong thunderstorms with a defined low pressure center and maximum sustained winds of 39 to 73 mph. • A hurricane is an intense tropical weather system of strong thunderstorms, a well-defined low pressure center (“eye”), and maximum sustained winds of 74 mph or more. In the North Atlantic Basin—where New York City is located—tropical cyclones often form in the Atlantic Ocean between Africa and the Lesser Antilles, in the Caribbean Sea, or in the Gulf of Mexico. Typically, they first track in a westerly or northwesterly direction. They are then pushed northward and eventually eastward by the force of the Earth’s rotation. They may track up the East Coast of the United States and reach New York City if water temperatures are warm enough and the prevailing winds steer them in this direction.