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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. -
Dock and Crop Images
orders: [email protected] (un)subscribe: [email protected] Current Availability for September 25, 2021 Dock and Crop images Click any thumbnail below for the slideshow of what we shipped this past week: CYCS ARE RED HOT GIANT GLOSSY LEAVES BLUE MOONSCAPE SUCCULENT BLUE LEAVES SUCCULENT ORANGE LEAVES SPECKLED LEAVES CYCS ARE RED HOT RED SUNSETSCAPE Jeff's updates - 9/16 dedicated this week's favorites Chimi's favorite climbing structure 4FL = 4" pot, 15 per flat 10H = 10" hanging basket n = new to the list ys = young stock 6FL = 6" pot, 6 per flat 10DP = 10" Deco Pot, round b&b = bud and bloom few = grab 'em! QT= quart pot, 12 or 16 per flat nb = no bloom * = nice ** = very nice Quarts - 12 per flat, Four Inch - 15 per flat, no split flats, all prices NET code size name comments comments 19406 4FL Acalypha wilkesiana 'Bronze Pink' ** Copper Plant-colorful lvs 12210 QT Acorus gramineus 'Ogon' ** lvs striped creamy yellow 19069 4FL Actiniopteris australis ** Eyelash Fern, Ray Fern 17748 4FL Adiantum hispidulum ** Rosy Maidenhair 17002 4FL Adiantum raddianum 'Microphyllum' ** extremely tiny leaflets 21496 4FL Adromischus filicaulis (cristatus?) ** Crinkle Leaf 16514 4FL Aeonium 'Kiwi' ** tricolor leaves 13632 QT Ajuga 'Catlin's Giant' ** huge lvs, purple fls 13279 QT Ajuga pyramidalis 'Metallica Crispa' ** crinkled leaf 17560 4FL Aloe vera * Healing Aloe, a must-have 13232 QT Anthericum sanderii 'Variegated' *b&b grassy perennial 13227 QT Asparagus densiflorus 'Meyer's' ** Foxtail Fern 19161 4FL Asplenium 'Austral Gem' -
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. -
A Decade Lost I ABOUT the AUTHORS
A DECADE LOST i ABOUT THE AUTHORS The Center for Human Rights and Global Justice (CHRGJ) brings together and expands the rich array of teaching, research, clinical, internship, and publishing activities undertaken within New York University (NYU) School of Law on international human rights issues. Philip Alston and Ryan Goodman are the Center’s Faculty co-Chairs; Smita Narula and Margaret Satterthwaite are Faculty Directors; Jayne Huckerby is Research Director; and Veerle Opgenhaffen is Senior Program Director. The Global Justice Clinic (GJC) at NYU School of Law provides high quality, professional human rights lawyering services to individual clients and non-governmental and inter-governmental human rights organizations, partnering with groups based in the United States and abroad. Working as legal advisers, counsel, co-counsel, or advocacy partners, Clinic students work side-by-side with human rights activists from around the world. The Clinic is directed by Professor Margaret Satterthwaite and in Fall 2010 to Spring 2011 was co-taught with Adjunct Assistant Professor Jayne Huckerby; Diana Limongi is Clinic Administrator. All publications and statements of the CHRGJ can be found at its website: www.chrgj.org. This Report should be cited as: Center for Human Rights and Global Justice, A Decade Lost: Locating Gender in U.S. Counter-Terrorism (New York: NYU School of Law, 2011). © NYU School of Law Center for Human Rights and Global Justice A DECADE LOST 1 ACKNOWLEDGEMENTS The Global Justice Clinic (GJC)/Center for Human Rights and Global Justice (CHRGJ) at New York University (NYU) School of Law acknowledges the following individuals for their contributions in the preparation of this report. -
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. -
Scavenger Hunt: Learn All About the Weather!
Scavenger Hunt: Learn All About the Weather! Hello, young scientists! Your task is to go on a scavenger hunt to learn all about weather–from snowflakes to firestorms, to hurricanes and many things in between! In this activity, you will adventure between articles on the NOAA SciJinks website, learning all about Earth’s many weather phenomena and gathering the missing words or phrases needed to assemble your secret word. All About Precipitation! When you see rain or snow fall from above, you are watching precipitation in action! Follow this link to learn all about precipitation and to find the missing word: Go to: What Is Precipitation? Answer 1: When gas cools and turns to liquid water or ice, it is called _______. All About Snowflakes! Snow is not simply a frozen droplet of water falling from a cloud. What makes a snowflake different is that it forms slowly, and that it grows in the cloud. But, how exactly does a snowflake form? Learn all about it in the following article and fill in the missing word below! Go to: How Do Snowflakes Form? Answer 2: Snowflakes form when water vapor travels through the air and condenses on a _____. All About Tornadoes! A strong tornado’s winds can pick up massive objects like trucks and drop them many miles away. It is difficult to measure the winds in a tornado directly, though. Because of this, tornadoes are evaluated by the amount of damage they cause. What tool do meteorologists use to measure the intensity of a tornado? Follow the link to find out and fill in the missing word below! Go to: Tornadoes Answer 3: The ______ ______ scale is a tool meteorologists use to measure the intensity of a tornado based on damage. -
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. -
Mediterranean Firestorm, Are Extreme Wildfires a Specular Aspect of Floods?
Plinius Conference Abstracts Vol. 12, Plinius12-57 12th Plinius Conference on Mediterranean Storms Corfu Island Greece, September 2010 © Author(s) 2010 Mediterranean Firestorm, are extreme wildfires a specular aspect of floods? P. Fiorucci, L. Molini, and A. Parodi CIMA Research Foundation, Italy (paolo.fi[email protected]) Severe weather and rainfall extremes predictors are a long standing issue for risk mitigation and civil protection purposes, analogously this work is focused on finding precursors for extreme wildfires throughout Mediterranean regions. Mediterranean storm are usually related with extreme precipitation and consequent floods. In this paper we propose to consider extreme wildfires in the Mediterranean as a specular aspect of “traditional” Mediterranean storms. Floods are related with soil moisture conditions, vegetation cover and topography but the main driver is represented by extreme precipitation. Rainfall is well evident in its happening. Nevertheless, the necessity of measuring it has become fundamental since the implementation of instruments needed to prevent floods. Wildfires are usually considered as the complex results of several heterogeneous aspects. Many peculiarities make Mediterranean wildfires different from other natural risk, fire ignition, human caused in more than 90% of fire occurrences, being the most evident. Fire spread and fire damages are related with vegetation cover, topography, moisture content and wind conditions but also with the ability to cope with the fire front. In the international literature all these aspects are considered to define tools able to predict and manage wildfire risk. Strong winds and high temperature are often considered as the main drivers in extreme wildfire risk conditions. Strong winds are usually associated also to floods event during Mediterranean storm but in this case it is evident it doesn’t the main driver. -
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. -
Storm Surge: Know Your Risk in Queensland!
Storm Surge: Know your risk in Queensland! Storm surge is a rise in sea level above the normal tide usually associated with a low pressure weather system such as a tropical cyclone. Storm surge develops due to strong winds pushing water towards the coastline as well as the low atmospheric pressure drawing up the sea surface. The Queensland coastline is highly vulnerable to storm surge. This is due to the frequency of tropical cyclones, the wide continental shelf and relatively shallow ocean floor in both the Great Barrier Reef lagoon and in the Gulf of Carpentaria, as well as the low lying nature of many coastal cities and towns. While the highest storm surges are more likely to occur in North Queensland and the Gulf of Carpentaria, they can also develop in southeast Queensland affecting the Sunshine Coast, Moreton Bay and the Gold Coast. Storm surges may reach magnitudes of 1 to 10 metres above the tide depending on the intensity of the cyclone, its size and the local characteristics of the coastline. Impacts Coral Sea Storm surge can be very dangerous and poses a critical risk Gulf of Carpentaria to human life during tropical cyclones. Great Cairns Barrier Reef The length of coastline affected by a storm surge can be Innisfail tens to hundreds of kilometres wide. The rise in sea level Cardwell Townsville can be rapid and high in velocity, inundating the ground Bowen floor of buildings, even up to the roof. Mackay Queensland Storm surge has the power to easily move cars, even Gladstone houses, can damage roads and buildings and can be Hervey Bay almost impossible to manoeuvre through.