A Look at the 2020 Hurricane Season
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PROTECT YOUR PROPERTY from STORM SURGE Owning a House Is One of the Most Important Investments Most People Make
PROTECT YOUR PROPERTY FROM STORM SURGE Owning a house is one of the most important investments most people make. Rent is a large expense for many households. We work hard to provide a home and a future for ourselves and our loved ones. If you live near the coast, where storm surge is possible, take the time to protect yourself, your family and your belongings. Storm surge is the most dangerous and destructive part of coastal flooding. It can turn a peaceful waterfront into a rushing wall of water that floods homes, erodes beaches and damages roadways. While you can’t prevent a storm surge, you can minimize damage to keep your home and those who live there safe. First, determine the Base Flood Elevation (BFE) for your home. The BFE is how high floodwater is likely to rise during a 1%-annual-chance event. BFEs are used to manage floodplains in your community. The regulations about BFEs could affect your home. To find your BFE, you can look up your address on the National Flood Hazard Layer. If you need help accessing or understanding your BFE, contact FEMA’s Flood Mapping and Insurance eXchange. You can send an email to FEMA-FMIX@ fema.dhs.gov or call 877 FEMA MAP (877-336-2627). Your local floodplain manager can help you find this information. Here’s how you can help protect your home from a storm surge. OUTSIDE YOUR HOME ELEVATE While it is an investment, elevating your SECURE Do you have a manufactured home and want flood insurance YOUR HOME home is one of the most effective ways MANUFACTURED from the National Flood Insurance Program? If so, your home to mitigate storm surge effects. -
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 -
Understanding Storm Surge
The Education Program at the New Jersey Sea Grant Consortium 22 Magruder Road, Fort Hancock, NJ 07732 (732) 872-1300 www.njseagrant.org UNDERSTANDING STORM SURGE OVERVIEW In this climate education module, students will gain an understanding of the term “storm surge” by exploring the meteorological principles that create storms and generate storm surges. Many basics of weather are discussed, including air pressure, air circulation, and the influence of the Coriolis effect on weather. TABLE OF Background……………………………………….......................1-4 CONTENTS Activity #1- Oceans of Pressure …......................................... 5-10 Activity #2- Windy Balloon ……………………….................... 11-13 Activity #3- Density Driven Currents ………………................ 14-18 Activity #4- Coriolis Effect……………………………………. 19-22 Activity #5- Pressure Driven Storms and Surge…………..... 23-25 Activity #6- Surge of the Storm ………................................. 26-34 How Meteorologists’ Measure and Predict Storm Surge…… 35-37 Why should you care about understanding storm surge? ...... 38-39 Storm Surge Watches and Warnings ………………….……. 40-42 NOAA’s Top 10 Tips for Being Ready for a Storm Surge…...... 43 References …............................................................................ 44 OBJECTIVES Following completion of this module, students will be able to: Define storm surge and the factors that influence it Learn how temperature affects air density and the formation of high and low pressure systems in the atmosphere Explore the effect of gravity on air in the atmosphere Discover the role of Earth’s rotation on global and localized wind patterns Examine the effects that air pressure has on storm surge levels Determine how storm surge affects coastal communities Explore the impact of shoreline shape and beach slope on storm surge GRADE LEVEL 5 – 12 The New Jersey Sea Grant Consortium (NJSGC) is an affiliation of colleges, universities and other groups dedicated to advancing knowledge and stewardship of New Jersey’s marine and coastal environment. -
ESSENTIALS of METEOROLOGY (7Th Ed.) GLOSSARY
ESSENTIALS OF METEOROLOGY (7th ed.) GLOSSARY Chapter 1 Aerosols Tiny suspended solid particles (dust, smoke, etc.) or liquid droplets that enter the atmosphere from either natural or human (anthropogenic) sources, such as the burning of fossil fuels. Sulfur-containing fossil fuels, such as coal, produce sulfate aerosols. Air density The ratio of the mass of a substance to the volume occupied by it. Air density is usually expressed as g/cm3 or kg/m3. Also See Density. Air pressure The pressure exerted by the mass of air above a given point, usually expressed in millibars (mb), inches of (atmospheric mercury (Hg) or in hectopascals (hPa). pressure) Atmosphere The envelope of gases that surround a planet and are held to it by the planet's gravitational attraction. The earth's atmosphere is mainly nitrogen and oxygen. Carbon dioxide (CO2) A colorless, odorless gas whose concentration is about 0.039 percent (390 ppm) in a volume of air near sea level. It is a selective absorber of infrared radiation and, consequently, it is important in the earth's atmospheric greenhouse effect. Solid CO2 is called dry ice. Climate The accumulation of daily and seasonal weather events over a long period of time. Front The transition zone between two distinct air masses. Hurricane A tropical cyclone having winds in excess of 64 knots (74 mi/hr). Ionosphere An electrified region of the upper atmosphere where fairly large concentrations of ions and free electrons exist. Lapse rate The rate at which an atmospheric variable (usually temperature) decreases with height. (See Environmental lapse rate.) Mesosphere The atmospheric layer between the stratosphere and the thermosphere. -
Winter Storm Intensity, Hazards, and Property Losses in the New York Tristate Area
Ann. N.Y. Acad. Sci. ISSN 0077-8923 ANNALS OF THE NEW YORK ACADEMY OF SCIENCES Issue: Annals Reports ORIGINAL ARTICLE Winter storm intensity, hazards, and property losses in the New York tristate area Cari E. Shimkus,1 Mingfang Ting,1 James F. Booth,2 Susana B. Adamo,3 Malgosia Madajewicz,4 Yochanan Kushnir,1 and Harald E. Rieder1,5 1Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York. 2City University of New York, City College, New York, New York. 3Center for International Earth Science Information Network, Columbia University, Palisades, New York. 4Center for Climate Systems Research, Columbia University, New York, New York. 5Wegener Center for Climate and Global Change and IGAM/Institute of Physics, University of Graz, Graz, Austria Address for correspondence: Mingfang Ting, Lamont-Doherty Earth Observatory, Columbia University, 61 Route 9W, Palisades, NY 10964. [email protected] Winter storms pose numerous hazards to the Northeast United States, including rain, snow, strong wind, and flooding. These hazards can cause millions of dollars in damages from one storm alone. This study investigates meteorological intensity and impacts of winter storms from 2001 to 2014 on coastal counties in Connecticut, New Jersey, and New York and underscores the consequences of winter storms. The study selected 70 winter storms on the basis of station observations of surface wind strength, heavy precipitation, high storm tide, and snow extremes. Storm rankings differed between measures, suggesting that intensity is not easily defined with a single metric. Several storms fell into two or more categories (multiple-category storms). Following storm selection, property damages were examined to determine which types lead to high losses. -
Hurricane Dorian
eVENT Hurricane Tracking Advisory Hurricane Dorian Information from NHC Advisory 20, 5:00 AM AST Thu Aug 29, 2019 On the forecast track, Dorian should move over the Atlantic well east of the southeastern and central Bahamas today and on Friday, and approach the northwestern Bahamas on Saturday. Maximum sustained winds are near 85 mph (140 km/h) with higher gusts. Strengthening is forecast during the next few days, and Dorian is expected to become a major hurricane on Friday. Intensity Measures Position & Heading U.S. Landfall (NHC) Max Sustained Wind 85 mph Position Relative to 150 mi NNW of San Juan, PR Speed: (Category 1) Land: Est. Time & Region: Monday on Florida Min Central Pressure: 991 mb Coordinates: 20.5 N, 66.6 W Trop. Storm Force Est. Max Sustained 90 miles Bearing/Speed: NW or 325 degrees at 13 mph 111+ mph (Category 3) Winds Extent: Wind Speed: Forecast Summary ■ The NHC forecast map (below left) and the wind-field map (below right), which is based on the NHC’s forecast track, both show Dorian passing east of the central Bahamas today and Friday, and approaching the northwestern Bahamas on Saturday. To illustrate the uncertainty in Dorian’s forecast track, Ï!D Trop Dep forecast tracks for all current models are shown on the wind-field map in pale gray. ■ Maximum sustained winds are near 85 mph with higher gusts. Strengthening is forecast during the next few days, and Dorian is expectedÏ!S Trop Storm to become a 1 major hurricane on Friday. Ï! Ca t 1 ■ Dorian is expected to produce total rain accumulations of 2 to 4 inches in the central Bahamas, 4 to 8 inches in the northwestern BahamasÏ!D Trop Dep and coastal 2 Ï! Ca t 2 sections of the southeast United States Ï!S Trop Storm ■ Swells around the U.S. -
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. -
Understanding Storm Surge
The Education Program at the New Jersey Sea Grant Consortium 22 Magruder Road, Fort Hancock, NJ 07732 (732) 872-1300 www.njseagrant.org UNDERSTANDING STORM SURGE HOW METEOROLOGISTS PREDICT AND MEASURE STORM SURGE The many factors that impact the height of storm surge make predicting storm surge very difficult; however, scientists from NOAA and the NWS (National Weather Service) have created a computer model called SLOSH (Sea, Lake, Overland Surges from Hurricanes) to predict storm surge heights and evaluate the risk of a coastal strike. The model depends on a storm’s atmospheric pressure, track, size, speed. Using complex physic equations, the model can apply this information to a specific location taking into consideration local water depth, land elevation, and other land features that could affect storm surge. All the different locations where storm surges are predicted are called basins. The New Jersey Sea Grant Consortium (NJSGC) is an affiliation of colleges, universities and other groups dedicated to advancing knowledge and stewardship of New Jersey’s marine and coastal environment. NJSGC meets its mission through its innovative research, education and outreach programs. For more information about NJSGC, visit njseagrant.org. A sample SLOSH model display from Hurricane Ike (2008). The model uses a color code to illustrate how high storm surge levels will go in feet above ground level. Since storms can be difficult to forecast, the model also takes into account historical storm surges from past storms and hypothetical storm surges, using many different factors that can change quickly during a storm such as size, intensity, track, etc. The model reports how high the storm surge inundation will be in feet above ground, so if the model predicts a 20 foot storm surge, that means the water will reach 20 feet above ground in that specific location. -
Flood ACC Article
Breadth of the Flood Exclusion: A Flood is a Flood, Including Storm Surge TRED R. EYERLY A case involving an Alaska Native Corporation and property damage caused by a hurricane is bound to be of interest. Arctic Slope Regional Corp. v. Affiliated FM Ins. Co. did not disappoint.1 The Arctic Slope Regional Corporation, based in Barrow, Alaska, and one of the thirteen Corporations formed under the Alaska Native Claims Settlement Act of 1971, owned an office and construction yard in Iberia Parish, Louisiana. The property was inundated with three feet of water after Hurricane Rita’s storm surge hit in September 2005. Arctic Slope filed a claim for property damage with Affiliated. The claim was denied and suit was filed. Before the district court, the parties disputed which policy provisions applied to the storm surge related claims. The distinction was critical because the policy covered damage caused by “Wind and/or hail,” but excluded damage caused by flood. The policy defined “Wind and/or hail” as “direct and/or indirect action of wind and all loss or damage resulting there from whether caused by wind, by hail or by any other peril . when water . is carried, blown, driven, or otherwise transported by wind onto or into said location.” “Flood,” on the other hand, was defined as “surface water; tidal or seismic sea wave; rising (including overflowing or breaking of boundaries) of any body of water . all whether driven by wind or not. .”2 1 Arctic Slope argued that, because storm surge is caused by strong onshore winds, coverage was provided under the “Wind and/or hail” definition. -
Massachusetts Tropical Cyclone Profile August 2021
Commonwealth of Massachusetts Tropical Cyclone Profile August 2021 Commonwealth of Massachusetts Tropical Cyclone Profile Description Tropical cyclones, a general term for tropical storms and hurricanes, are low pressure systems that usually form over the tropics. These storms are referred to as “cyclones” due to their rotation. Tropical cyclones are among the most powerful and destructive meteorological systems on earth. Their destructive phenomena include storm surge, high winds, heavy rain, tornadoes, and rip currents. As tropical storms move inland, they can cause severe flooding, downed trees and power lines, and structural damage. Once a tropical cyclone no longer has tropical characteristics, it is then classified as a post-tropical system. The National Hurricane Center (NHC) has classified four stages of tropical cyclones: • Tropical Depression: A tropical cyclone with maximum sustained winds of 38 mph (33 knots) or less. • Tropical Storm: A tropical cyclone with maximum sustained winds of 39 to 73 mph (34 to 63 knots). • Hurricane: A tropical cyclone with maximum sustained winds of 74 mph (64 knots) or higher. • Major Hurricane: A tropical cyclone with maximum sustained winds of 111 mph (96 knots) or higher, corresponding to a Category 3, 4 or 5 on the Saffir-Simpson Hurricane Wind Scale. Primary Hazards Storm Surge and Storm Tide Storm surge is an abnormal rise of water generated by a storm, over and above the predicted astronomical tide. Storm surge and large waves produced by hurricanes pose the greatest threat to life and property along the coast. They also pose a significant risk for drowning. Storm tide is the total water level rise during a storm due to the combination of storm surge and the astronomical tide. -
High Commissioner's Dialogue on Protection Challenges
High Commissioner’s Dialogue on Protection Challenges: Protection and Resilience during Pandemics Refugees International Written Statement for the session on Climate Action Climate-related impacts are leading to displacement and forcing people to migrate today We are in the midst of a climate crisis. The disruptive effects of climate change are being felt today. Nowhere is this more evident than in climate-related disaster displacement trends. For example, in 2019, weather-related events led to almost 24 million displaced people around the world, or more than three times the amount displaced by conflict the same year.1 While not all of these events are necessarily climate-related, they do speak to a worrying trend; namely, that sudden-onset weather events, such as hurricanes or floods, are increasing in frequency and intensity due to climate change. The climate science is clear. For instance, in 2017, Hurricane Maria was 30 percent more powerful than any other storm ever recorded in Puerto Rico – an occurrence that climate change is making five times more likely.2 The storm displaced 86,000 Puerto Ricans, with some 130,000 leaving the island for mainland United States in the aftermath.3 It also leveled much of the island Dominica and displaced 80 percent of its population.4 In 2019, Hurricane Dorian stalled over the Bahamas for more than 24 hours, supporting research that finds that hurricanes in the North Atlantic have been moving more slowly and stalling for longer periods due to climate change.5 Dorian was the strongest hurricane to ever hit the country, and it displaced 14,000 people.6 1 Internal Displacement Monitoring Centre (IDMC). -
Preleminary Report IP and ETA&IOTA Hurricanes .Indd
PRELIMINARY REPORT November 2020 ConsequencesConsequences ofof thethe HurricaneHurricane 20202020 SeasonSeason onon IndigenousIndigenous CommunitiesCommunities inin CentralCentral AmericaAmerica Destruction and Resilience PRELIMINARY REPORT ON THE CONSEQUENCES OF THE 2020 HURRICANE SEASON ON INDIGENOUS COMMUNITIES IN CEN- TRAL AMERICA DESTRUCTION AND RESILIENCE NOVEMBER 2020 GENERAL COORDINATION Myrna Cunningham Kain - President of FILAC Board of Directors Jesús Amadeo Martínez - General Coordinator of the Indigenous Forum of AbyaYala FIAY GENERAL SUPERVISION Álvaro Pop - FILAC Technical Secretary Amparo Morales - FILAC Chief of Staff TECHNICAL TEAM Ricardo Changala - Coordinator of the Regional Observatory for the Rights of Indigenous Peoples ORDPI FILAC Liber- tad Pinto - Technical Team ORDPI-FILAC Jean Paul Guevara - Technical Team ORDPI-FILAC TECHNICAL SUPPORT Ernesto Marconi - FILAC Technical Program Management Gabriel Mariaca - Coordinator of Institutional Communication FILAC Dennis Mairena - Management of Technical Programs FILAC Wendy Medina - FILAC Communication and Press Office GRAPHIC DESIGN Institutional Communication - FILAC IMAGES FILAC Imaging Archive UN Photos Shutterstock Unsplash LICENSE FOR DISTRIBUTION CC-BY-NC 4.0 This license allows reusers to distribute, remix, adapt, and build upon the material in any medium or format for noncommercial purposes only, and only so long as attribution is given to the creator. Credit must be given to the creator Only noncommercial uses of the work are permitted DOGOTAL ACCESS ON: https://indigenascovid19.red/monitoreo/ FILAC 20 de Octubre 2287 esq. Rosendo Gutiérrez [email protected] La Paz, Bolivia SUPPORT Ford Foundation, AECID and Pawanka Fund Introduction This document is a preliminary report on the human and material impacts of hurricanes Eta and Iota on the Central American isthmus. It has been an extraordinary fact that two hurricanes of this size and strength have hit the region so close in time, affecting all Central American countries.