“Coastal Hazards Caused by Storm Surge and Flood”

Total Page:16

File Type:pdf, Size:1020Kb

“Coastal Hazards Caused by Storm Surge and Flood” ON REGIONAL OCEAN GOVERNANCE FRAMEWORK, IMPLEMENTATION OF THE UNITED NATIONS CONVENTION ON THE LAW OF THE SEA (UNCLOS) AND ITS RELATED INSTRUMENTS IN THE SOUTHEAST ASIAN SEAS AND THE INDIAN OCEAN “Coastal hazards caused by storm surge and flood” Dr.Wattana Kanbua Director, Marine Meteorological Center Thai Meteorological Department On March 16, 2016 , held in Phuket, THAILAND ON REGIONAL OCEAN GOVERNANCE FRAMEWORK, IMPLEMENTATION OF THE UNITED NATIONS CONVENTION ON THE LAW OF THE SEA (UNCLOS) AND ITS RELATED INSTRUMENTS IN THE SOUTHEAST ASIAN SEAS AND THE INDIAN OCEAN Outline • Tropical Cyclones • Storm surges impacts • Storm surges physics • Earth Observation applications • Storm surges and our coastal lives • Summary On March 16, 2016 , held in Phuket, THAILAND ON REGIONAL OCEAN GOVERNANCE FRAMEWORK, IMPLEMENTATION OF THE UNITED NATIONS CONVENTION ON THE LAW OF THE SEA (UNCLOS) AND ITS RELATED INSTRUMENTS IN THE SOUTHEAST ASIAN SEAS AND THE INDIAN OCEAN What is Tropical Cyclone (TC)? A “tropical cyclone" is an intense vortex or a whirl in the atmosphere with very strong winds circulating around it in anti-clockwise direction in the northern Hemisphere and in clockwise direction in the southern Hemisphere. On March 16, 2016 , held in Phuket, THAILAND ON REGIONAL OCEAN GOVERNANCE FRAMEWORK, IMPLEMENTATION OF THE UNITED NATIONS CONVENTION ON THE LAW OF THE SEA (UNCLOS) AND ITS RELATED INSTRUMENTS IN THE SOUTHEAST ASIAN SEAS AND THE INDIAN OCEAN Definition - A tropical cyclone is a meteorological term for a storm system characterized by a low pressure center - which develops over tropical or subtropical waters, - thunderstorms that produces strong wind and flooding rain. - A tropical cyclone feeds on the heat released when moist air rises and the water vapor it contains condenses. - They are fueled by a different heat mechanism than other cyclonic windstorms. On March 16, 2016 , held in Phuket, THAILAND ON REGIONAL OCEAN GOVERNANCE FRAMEWORK, IMPLEMENTATION OF THE UNITED NATIONS CONVENTION ON THE LAW OF THE SEA (UNCLOS) AND ITS RELATED INSTRUMENTS IN THE SOUTHEAST ASIAN SEAS AND THE INDIAN OCEAN Creation • Lows pressure form over 26 C (82F) ocean • Condensation, release of latent heat causes surfaces temperature, often in ITCZ. increased buoyancy, thus increased ascent, • If conditions are right, the rising warm air and increased convergence over low-latitude, solar-warmed waters sets • Area of convergence enlarges, more water off a positive-feedback: vapor to draw on • Ascent causes convergence On March 16, 2016 , held in Phuket, THAILAND ON REGIONAL OCEAN GOVERNANCE FRAMEWORK, IMPLEMENTATION OF THE UNITED NATIONS CONVENTION ON THE LAW OF THE SEA (UNCLOS) AND ITS RELATED INSTRUMENTS IN THE SOUTHEAST ASIAN SEAS AND THE INDIAN OCEAN Classification • Tropical depression A weak tropical cyclone in which the maximum surface wind is 38 mph (62 km/h or 33 kt) or less • Tropical storm A tropical cyclone in which the maximum surface wind ranges from 39 to 73 mph (63 to 118 km/h or 34 to 64 kt) • Typhoon A tropical cyclone with highest sustained winds 74 mph (119 km/h or 65 kt) or more On March 16, 2016 , held in Phuket, THAILAND ON REGIONAL OCEAN GOVERNANCE FRAMEWORK, IMPLEMENTATION OF THE UNITED NATIONS CONVENTION ON THE LAW OF THE SEA (UNCLOS) AND ITS RELATED INSTRUMENTS IN THE SOUTHEAST ASIAN SEAS AND THE INDIAN OCEAN Saffir-simpson Scale On March 16, 2016 , held in Phuket, THAILAND ON REGIONAL OCEAN GOVERNANCE FRAMEWORK, IMPLEMENTATION OF THE UNITED NATIONS CONVENTION ON THE LAW OF THE SEA (UNCLOS) AND ITS RELATED INSTRUMENTS IN THE SOUTHEAST ASIAN SEAS AND THE INDIAN OCEAN Characteristics • Size - 300 to 1500 km in diameter • Horizontal structure – Eye - 20 km – Eyewall - 30 to 50 km – Spiral bands On March 16, 2016 , held in Phuket, THAILAND ON REGIONAL OCEAN GOVERNANCE FRAMEWORK, IMPLEMENTATION OF THE UNITED NATIONS CONVENTION ON THE LAW OF THE SEA (UNCLOS) AND ITS RELATED INSTRUMENTS IN THE SOUTHEAST ASIAN SEAS AND THE INDIAN OCEAN Tropical Cyclones Worldwide Typhoon Hurricane Cyclone Data Source: NOAA / NHC and JTWC On March 16, 2016 , held in Phuket, THAILAND ON REGIONAL OCEAN GOVERNANCE FRAMEWORK, IMPLEMENTATION OF THE UNITED NATIONS CONVENTION ON THE LAW OF THE SEA (UNCLOS) AND ITS RELATED INSTRUMENTS IN THE SOUTHEAST ASIAN SEAS AND THE INDIAN OCEAN WMO’s Global Tropical Cyclone Early Warning System • 6 Regional Centres designated by WMO to provide advisories for countries in region • 6 regional tropical cyclone committees On March 16, 2016 , held in Phuket, THAILAND ON REGIONAL OCEAN GOVERNANCE FRAMEWORK, IMPLEMENTATION OF THE UNITED NATIONS CONVENTION ON THE LAW OF THE SEA (UNCLOS) AND ITS RELATED INSTRUMENTS IN THE SOUTHEAST ASIAN SEAS AND THE INDIAN OCEAN Storm surge and flood impacts • Throughout history, flooding has impacted more people and caused greater economic and insured losses than any other natural peril. For example, – Half of the more than USD 40 billion in insured losses that stemmed from Hurricane Katrina in 2005 was related to storm surge. – The tsunami that devastated the northern coast of Honshu in March 2011 is estimated to have caused insured losses of USD 3.5 billion. – Economic losses following the riverine flooding in Thailand 2011 later that year were estimated by the World Bank to be USD 45.7 billion (THB 1.4 trillion). On March 16, 2016 , held in Phuket, THAILAND ON REGIONAL OCEAN GOVERNANCE FRAMEWORK, IMPLEMENTATION OF THE UNITED NATIONS CONVENTION ON THE LAW OF THE SEA (UNCLOS) AND ITS RELATED INSTRUMENTS IN THE SOUTHEAST ASIAN SEAS AND THE INDIAN OCEAN Storm surge impacts - Significant destruction of property, structures, vegetation, and coastal landscapes are just a few of the many impacts that result from storm surge. The following animation shows the effects of storm surge on coastal areas. On March 16, 2016 , held in Phuket, THAILAND ON REGIONAL OCEAN GOVERNANCE FRAMEWORK, IMPLEMENTATION OF THE UNITED NATIONS CONVENTION ON THE LAW OF THE SEA (UNCLOS) AND ITS RELATED INSTRUMENTS IN THE SOUTHEAST ASIAN SEAS AND THE INDIAN OCEAN Storm surge impact - humanitarian • Currently, around 0.6% of the world’s population live and work in risk areas • One of the most disturbing impacts of storm surges are the mass fatalities that can occur • Examples: – Cyclone Sidr (10,000) – Hurricane Katrina (USA - 1500 approx) – Cyclone Nargis (Myanmar - 140,000 approx) – Windstorm Xynthia (France - 50 approx) – Supertyphoon Haiiyan (Phillipines – 4500 approx) • The occurrences of storm surge often necessitates a significant global humanitarian response On March 16, 2016 , held in Phuket, THAILAND ON REGIONAL OCEAN GOVERNANCE FRAMEWORK, IMPLEMENTATION OF THE UNITED NATIONS CONVENTION ON THE LAW OF THE SEA (UNCLOS) AND ITS RELATED INSTRUMENTS IN THE SOUTHEAST ASIAN SEAS AND THE INDIAN OCEAN Storm surge impact - economic • Damage to key infrastructure (roads, rail, port facilities) can impede short term recovery and economic activity • Short term food supply disruption (and associated price volatility) with the destruction of local fishing infrastructure and agriculture • Medium-term loss of agriculture (due to saline intrusion into coastal agricultural areas) • Loss of skilled & experienced element of the workforce • Loss in tourism revenue • Cost of rebuilding & loss of economic assets can be significant On March 16, 2016 , held in Phuket, THAILAND ON REGIONAL OCEAN GOVERNANCE FRAMEWORK, IMPLEMENTATION OF THE UNITED NATIONS CONVENTION ON THE LAW OF THE SEA (UNCLOS) AND ITS RELATED INSTRUMENTS IN THE SOUTHEAST ASIAN SEAS AND THE INDIAN OCEAN Storm surge impact - social • Breakdown in local governance (e.g. Philippines re Typhoon Haiyan 2013) • Social shock as communities and families must come to terms with personal losses, survival experiences • High potential for breakdown in law and order in the immediate aftermath • Severe disruption to social support networks (families and communities) • The widespread impact of social disruption – Loss is not restricted to the coastal area, but extends over a wide area with the weather damage • Potential for medium-term psychological trauma to persist in the community On March 16, 2016 , held in Phuket, THAILAND ON REGIONAL OCEAN GOVERNANCE FRAMEWORK, IMPLEMENTATION OF THE UNITED NATIONS CONVENTION ON THE LAW OF THE SEA (UNCLOS) AND ITS RELATED INSTRUMENTS IN THE SOUTHEAST ASIAN SEAS AND THE INDIAN OCEAN Storm surge impact - environmental • Habitat and protected area destruction: – Key coastal habitats (e.g. mangrove swamps, salt marshes) are overwhelmed by the surge and can be structurally damaged – Loss of remaining protected species refugees • Pollution: – Key debris from damage/destroyed human settlements spread into the environment – Damage to infrastructure containing toxic pollutants releases them into the local environment • Resource re-allocations: – Environmental concerns are often deemed secondary to humanitarian needs On March 16, 2016 , held in Phuket, THAILAND ON REGIONAL OCEAN GOVERNANCE FRAMEWORK, IMPLEMENTATION OF THE UNITED NATIONS CONVENTION ON THE LAW OF THE SEA (UNCLOS) AND ITS RELATED INSTRUMENTS IN THE SOUTHEAST ASIAN SEAS AND THE INDIAN OCEAN Storm surge impact - vulnerability • Increase in population’s short-term vulnerability to – Further weather events – Disease – Governance disorder and breakdown • Loss of key breakwater habitats and coastal defence infrastructure can inhibit coastal resilience to future events in the medium term • With the aid effort response, the population risks becoming aid dependent • Allocating resources to an area while
Recommended publications
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Defining Storm Surge, Storm Tide, and Inundation
    Defining Storm Surge, Storm Tide, and Inundation Understanding the risk associated with storm surge-driven coastal flooding requires using common references and language. When common references or language is not used, flooding risk can be misunderstood, having significant implications on the ability to communicate life-saving information and decisions during an event. To help ensure clear communication and understanding of storm surge-induced flooding, the terms used to describe storm surge, storm tide, and inundation are described below. Storm surge is defined as the abnormal rise of water generated by a storm, over and above the normal astronomical tide, and is expressed in terms of height above predicted or expected tide levels. Since storm surge represents the deviation from normal tide levels, it is not referenced to a vertical or tidal datum. By contrast, storm tide is defined as the water level due to the combination of storm surge and the astronomical tide, and is expressed in terms of height above a vertical or tidal datum. A vertical datum is simply a base elevation used as a reference from which to measure heights (or depths). Similarly, a tidal datum is a base elevation defined by a certain phase of the tide. The definitions of various tidal datums can be found here: http://tidesandcurrents.noaa.gov/datum_options.html. Inundation is the total water level that occurs on normally dry ground as a result of the storm tide, and is expressed in terms of height of water, in feet, above ground level. Inundation provides the most clearly and commonly understood method for communicating storm surge-driven coastal flooding.
    [Show full text]
  • Hurricanes and Tropical Storms Location and Extent of All • Severe Thunderstorms Natural Hazards That Can Affect the Jurisdiction
    HAZARD I DENTIFICATION The United States and its communities are vulnerable to a wide array of natural hazards that threaten life and property. These hazards include, in no particular order: • Drought 44 CFR Requirement • Extreme Temperatures Part 201.6(c)(2)(i): The risk • Flood assessment shall include a description of the type, • Hurricanes and Tropical Storms location and extent of all • Severe Thunderstorms natural hazards that can affect the jurisdiction. The plan • Tornadoes shall include information on • Wildfire previous occurrences of hazard events and on the • Winter Storms probability of future hazard • Erosion events. • Earthquakes • Sinkholes • Landslides • Dam/Levee Failure Some of these hazards are interrelated (i.e., hurricanes can cause flooding and tornadoes), and some consist of hazardous elements that are not listed separately (i.e., severe thunderstorms can cause lightning; hurricanes can cause coastal erosion). It should also be noted that some hazards, such as severe winter storms, may impact a large area yet cause little damage, while other hazards, such as a tornado, may impact a small area yet cause extensive damage. This section of the Plan provides a general description for each of the hazards listed above along with their hazardous elements, written from a national perspective. Section 4: Page 2 H AZARD I DENTIFICATION N ORTHERN V IRGINIA R EGIONAL H AZARD M ITIGATION P LAN Drought Drought is a natural climatic condition caused by an extended period of limited rainfall beyond that which occurs naturally in a broad geographic area. High temperatures, high winds, and low humidity can worsen drought conditions, and can make areas more susceptible to wildfire.
    [Show full text]
  • What Is Storm Surge?
    INTRODUCTION TO STORM SURGE Introduction to Storm Surge National Hurricane Center Storm Surge Unit BOLIVAR PENINSULA IN TEXAS AFTER HURRICANE IKE (2008) What is Storm Surge? Inland Extent Storm surge can penetrate well inland from the coastline. During Hurricane Ike, the surge moved inland nearly 30 miles in some locations in southeastern Texas and southwestern Louisiana. Storm surge is an abnormal Storm tide is the water level rise of water generated by a rise during a storm due to storm, over and above the the combination of storm predicted astronomical tide. surge and the astronomical tide. • It’s the change in the water level that is due to the presence of the • Since storm tide is the storm combination of surge and tide, it • Since storm surge is a difference does require a reference level Vulnerability between water levels, it does not All locations along the U.S. East and Gulf coasts • A 15 ft. storm surge on top of a are vulnerable to storm surge. This figure shows have a reference level high tide that is 2 ft. above mean the areas that could be inundated by water in any sea level produces a 17 ft. storm given category 4 hurricane. tide. INTRODUCTION TO STORM SURGE 2 What causes Storm Surge? Storm surge is caused primarily by the strong winds in a hurricane or tropical storm. The low pressure of the storm has minimal contribution! The wind circulation around the eye of a Once the hurricane reaches shallower hurricane (left above) blows on the waters near the coast, the vertical ocean surface and produces a vertical circulation in the ocean becomes In general, storm surge occurs where winds are blowing onshore.
    [Show full text]
  • Coalescence De L'écologie Du Paysage Littoral Et De La Technologie
    Université du Québec INRS (Eau, Terre et Environnement) Coalescence de l’écologie du paysage littoral et de la technologie aéroportée du LiDAR ubiquiste THÈSE DE DOCTORAT Présentée pour l‘obtention du grade de Philosophiae Doctor (Ph.D.) en Sciences de la Terre Par Antoine Collin 19 mai 2009 Jury d‘évaluation Présidente du jury et Monique Bernier examinatrice interne Institut National de la Recherche Scientifique - Eau Terre et Environnement, Québec, Canada Examinateur interne Pierre Francus Institut National de la Recherche Scientifique - Eau Terre et Environnement, Québec, Canada Examinatrice externe Marie-Josée Fortin Université de Toronto, Ontario, Canada Examinateur externe Georges Stora Université de la Méditerranée, Marseille, France Directeur de recherche Bernard Long Institut National de la Recherche Scientifique – Eau, Terre et Environnement, Québec, Canada Co-directeur de recherche Philippe Archambault Institut des Sciences de la Mer, Université du Québec à Rimouski, Rimouski, Canada © Droits réservés de Antoine Collin, 2009 v Imprimée sur papier 100% recyclé « Nous croyons regarder la nature et c'est la nature qui nous regarde et nous imprègne. » Christian Charrière, Extrait de Le maître d'âme. vi vii Résumé La frange littorale englobe un éventail d‘écosystèmes dont les services écologiques atteignent 17.447 billions de dollars U.S., ce qui constitue la moitié de la somme totale des capitaux naturels des écosystèmes de la Terre. L‘accroissement démographique couplé aux bouleversements provoqués par le réchauffement climatique, génèrent inexorablement de fortes pressions sur les processus écologiques côtiers. L‘écologie du paysage, née de la rencontre de l‘écologie et de l‘aménagement du territoire, est susceptible d‘apporter les fondements scientifiques nécessaires à la gestion durable de ces écosystèmes littoraux.
    [Show full text]