A Statistical Model to Forecast Short-Term Atlantic Hurricane Intensity

Total Page:16

File Type:pdf, Size:1020Kb

A Statistical Model to Forecast Short-Term Atlantic Hurricane Intensity A STATISTICAL MODEL TO FORECAST SHORT-TERM ATLANTIC HURRICANE INTENSITY DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University By Kevin T. Law, M.S. ***** The Ohio State University 2006 Dissertation Committee: Approved by Professor Jay S. Hobgood, Adviser Professor Jeffrey C. Rogers ___________________________________ Professor Lawrence Krissek Adviser Graduate Program in Atmospheric Science ABSTRACT The accuracy of hurricane intensity forecasts has lagged the accuracy of hurricane track forecasts thereby creating a need for improvement. Many models struggle capturing the rapid intensification period and identifying when it will occur which causes a large amount of error in the intensity forecasts. The method described in this paper uses a discriminant function analysis (DFA) to help identify how intense the tropical cyclone will become and also how close it is to the rapid intensification period. Identifying the proximity to the rapid intensification period is a key factor in improving the intensity forecasts. Based upon the intensity and its proximity to its rapid intensification period, as selected by the DFA, an appropriate regression model is applied to forecast the 24-hour and 6-hour pressure reduction and wind speed increase. Other statistical intensity models apply the same regression model throughout the entire lifecycle of the tropical cyclone. This model relies on the premise that factors which cause intensification affect the tropical cyclone differently throughout its life cycle. Therefore, by using the DFA, different stages in its life cycle are identified, which allows the regression model to use the most significant variables at the particular stage. They are shown to improve the intensity forecasts at the stages leading up to and during the rapid intensification, which ii happen to be the most difficult stages to predict. The forecasts were validated with 13 independent case studies and compared with the official National Hurricane Center (NHC) forecasts. iii ACKNOWLEDGMENTS I wish to thank my adviser, Jay Hobgood, for always having the time to answer questions and correct errors. In addition, I would like to thank Gustavo Goni for personally making the AOML Hurricane Heat Potential data readily available. Both of whom without their support, this dissertation would not have been possible. iv VITA July 9, 1976………………… ……... Born – Parkersburg, West Virginia 1998………………………………... B.A. Geography, West Virginia University 1999-present……………………… Graduate Teaching Associate, The Ohio State University 2001………………………………... M.S. Atmospheric Science, The Ohio State University FIELDS OF STUDY Major Field: Atmospheric Science v TABLE OF CONTENTS Page Abstract.............................................................................................................................. iii Acknowledgments................................................................................................................v Vita..................................................................................................................................... vi List of Tables .......................................................................................................................x List of Figures.................................................................................................................. xiii Chapters: 1. Introduction .............................................................................................................1 2. Literature Review ....................................................................................................6 2.1 Environmental Influences on Tropical Cyclone Intensity Change ...................6 2.2 Potential Rapid Intensification Predictors ........................................................7 2.3 Other Factors Affecting Rapid Intensification ..................................................8 2.4 Wind Shear Processes .....................................................................................10 2.5 Vertical Wind Shear Numerical Simulation Studies ......................................13 2.6 Vertical Wind Shear Observational Studies ...................................................15 2.7 Vertical Wind Shear Individual Case Studies .................................................16 2.8 Thermodynamic Processes ..............................................................................20 2.9 Statistical Modeling of Tropical Cyclone Intensification ...............................25 3. Scientific Objective and Methodology .................................................................28 3.1 Introduction .....................................................................................................28 3.2 Tropical Cyclone Selection and (HURDAT) Data .........................................29 3.3 NCEP/NCAR Reanalysis Data .......................................................................32 3.4 AOML Tropical Cyclone Heat Potential ........................................................34 3.5 Variables and Data Used in the Study ............................................................37 3.5.1 NHC HURDAT data ........................................................................37 3.5.2 Vertical Wind Shear and Relative Humidity ....................................39 3.5.3 Holland MPI......................................................................................41 3.5.4 Attained MPI.....................................................................................43 3.5.5. Tropical Cyclone Heat Potential......................................................44 3.6 Discriminant Function Analysis ......................................................................45 3.7 Multiple Regression.........................................................................................49 vi 3.8 Testing the Models with an Independent Dataset............................................51 4. Results and Discussion..........................................................................................55 4.1 Discriminant Function Analysis Classification ...............................................55 4.2 Multiple Regression Equations........................................................................59 4.3 Evaluation of the Models with an Independent Dataset ..................................67 4.3.1 Hurricane Alex..................................................................................68 4.3.2 Hurricane Charley.............................................................................76 4.3.3 Hurricane Danielle............................................................................84 4.3.4 Hurricane Frances .............................................................................92 4.3.5 Hurricane Gaston ............................................................................100 4.3.6 Hurricane Ivan ................................................................................109 4.3.7 Hurricane Jeanne.............................................................................118 4.3.8 Hurricane Karl ................................................................................126 4.3.9 Hurricane Lisa.................................................................................134 4.3.10 Hurricane Dennis ..........................................................................142 4.3.11 Hurricane Emily............................................................................150 4.3.12 Hurricane Irene .............................................................................158 4.3.13 Hurricane Katrina..........................................................................166 5. Conclusion ..........................................................................................................176 Bibliography ....................................................................................................................187 Appendix A: Tropical Cyclone Tracks............................................................................193 vii LIST OF TABLES Table Page 1.1 Saffir-Simpson Scale...............................................................................................3 3.1 Tropical cyclone selection list from 1988-2003. Storms that are in boldface are considered “major”............................................................................31 3.2 List of variables used in the study..........................................................................40 3.3 Number of cases in each category for the multiple regression analysis ................52 3.4 List of Hurricanes in the Independent Dataset.......................................................53 4.1 Classification results for step one of the discriminant analysis .............................56 4.2 Step 2 of the DFA for major hurricanes.................................................................58 4.3 Step 2 of the DFA for minor hurricanes ................................................................58 4.4 Future 24-hour pressure drop regression equations...............................................63 4.5 Future 24-hour wind speed increase regression equations ....................................64 4.6 Future 6-hour pressure drop regression equations.................................................65 4.7 Future 6-hour wind speed increase regression equations ......................................66
Recommended publications
  • Wind Speed-Damage Correlation in Hurricane Katrina
    JP 1.36 WIND SPEED-DAMAGE CORRELATION IN HURRICANE KATRINA Timothy P. Marshall* Haag Engineering Co. Dallas, Texas 1. INTRODUCTION According to Knabb et al. (2006), Hurricane Katrina Mehta et al. (1983) and Kareem (1984) utilized the was the costliest hurricane disaster in the United States to concept of wind speed-damage correlation after date. The hurricane caused widespread devastation from Hurricanes Frederic and Alicia, respectively. In essence, Florida to Louisiana to Mississippi making a total of three each building acts like an anemometer that records the landfalls before dissipating over the Ohio River Valley. wind speed. A range of failure wind speeds can be The storm damaged or destroyed many properties, determined by analyzing building damage whereas especially near the coasts. undamaged buildings can provide upper bounds to the Since the hurricane, various agencies have conducted wind speeds. In 2006, WSEC developed a wind speed- building damage assessments to estimate the wind fields damage scale entitled the EF-scale, named after the late that occurred during the storm. The National Oceanic Dr. Ted Fujita. The author served on this committee. and Atmospheric Administration (NOAA, 2005a) Wind speed-damage correlation is useful especially conducted aerial and ground surveys and published a when few ground-based wind speed measurements are wind speed map. Likewise, the Federal Emergency available. Such was the case in Hurricane Katrina when Management Agency (FEMA, 2006) conducted a similar most of the automated stations failed before the eye study and produced another wind speed map. Both reached the coast. However, mobile towers were studies used a combination of wind speed-damage deployed by Texas Tech University (TTU) at Slidell, LA correlation, actual wind measurements, as well as and Bay St.
    [Show full text]
  • REPORT of the 46Th MEETING
    REPORT OF THE 46th MEETING ARCADIA, CALIFORNIA NOVEMBER 27-29, 2012 2012 NAFC-FMWG Minutes Minutes of the 46th Annual Meeting of the North American Forest Commission – Fire Management Working Group Arcadia, California, USA Angeles National Forest Conference Room November 27-29, 2012 Tuesday November 27th, 2012 Hosted by the US Forest Service 1. Welcome Meeting called to order by Dale Dague of the US Forest Service, who welcomed everyone on behalf of the North American Forest Commission, thanked them for their attendance, and introduced Angeles National Forest Fire Management Officer James Hall. James Hall, Fire Management Officer, US Forest Service Angeles National Forest expressed his pleasure at having this group on the Angeles National Forest as the inaugural meeting in the newly remodeled training facility located at the Angeles National Forest Headquarters. 2. Introductions Roundtable introductions completed (see Appendix 1 for list of delegates in attendance) and Dale Dague conducted a review of the agenda and meeting logistics. 3. Meeting Overview Tuesday, November 27/13 Country Reports – Mexico, Canada, USA Review of 2011 FMWG meeting minutes CONANP Membership Proposal FMWG Charter Review Reducing Emissions from Deforestation and Forest Degradation NAFC website proposal Review FMWG Work Plan and Action Items Hurricane Sandy Report International Liaison Committee (ILC) Update 6th International Wildland Fire Conference Update Wednesday, November 28/13 Field Trip to the Station Fire, Angeles National Forest Banquet for meeting delegates Thursday, November 29/13 Texas Wildfires of 2011 Forest Fire Managers Group (FFMG Update NAFC Update Travel to San Dimas Technology and Development Center (SDTDC) Tour of SDTDC Bilateral Wildfire Agreements update ICS Glossary Update (French Translation) Page 1 of 62 2012 NAFC-FMWG Minutes 4.
    [Show full text]
  • Conference Poster Production
    65th Interdepartmental Hurricane Conference Miami, Florida February 28 - March 3, 2011 Hurricane Earl:September 2, 2010 Ocean and Atmospheric Influences on Tropical Cyclone Predictions: Challenges and Recent Progress S E S S Session 2 I The 2010 Tropical Cyclone Season in Review O N 2 The 2010 Atlantic Hurricane Season: Extremely Active but no U.S. Hurricane Landfalls Eric Blake and John L. Beven II ([email protected]) NOAA/NWS/National Hurricane Center The 2010 Atlantic hurricane season was quite active, with 19 named storms, 12 of which became hurricanes and 5 of which reached major hurricane intensity. These totals are well above the long-term normals of about 11 named storms, 6 hurricanes, and 2 major hurricanes. Although the 2010 season was considerably busier than normal, no hurricanes struck the United States. This was the most active season on record in the Atlantic that did not have a U.S. landfalling hurricane, and was also the second year in a row without a hurricane striking the U.S. coastline. A persistent trough along the east coast of the United States steered many of the hurricanes out to sea, while ridging over the central United States kept any hurricanes over the western part of the Caribbean Sea and Gulf of Mexico farther south over Central America and Mexico. The most significant U.S. impacts occurred with Tropical Storm Hermine, which brought hurricane-force wind gusts to south Texas along with extremely heavy rain, six fatalities, and about $240 million dollars of damage. Hurricane Earl was responsible for four deaths along the east coast of the United States due to very large swells, although the center of the hurricane stayed offshore.
    [Show full text]
  • AL012016 Alex.Pdf
    NATIONAL HURRICANE CENTER TROPICAL CYCLONE REPORT HURRICANE ALEX (AL012016) 12 – 15 January 2016 Eric S. Blake National Hurricane Center 13 September 2016 NASA-MODIS VISIBLE IMAGE OF ALEX AT 1530 UTC 14 JANUARY 2016. Alex was a very unusual January hurricane in the northeastern Atlantic Ocean, making landfall on the island of Terceira in the Azores as a 55-kt tropical storm. Hurricane Alex 2 Hurricane Alex 12 – 15 JANUARY 2016 SYNOPTIC HISTORY The precursor disturbance to Alex was first noted over northwestern Cuba on 6 January as a weak low along a stationary front. A strong mid-latitude shortwave trough caused the disturbance to intensify into a well-defined frontal wave near the northwestern Bahamas by 0000 UTC 7 January. The extratropical low then moved northeastward, passing about 75 n mi north of Bermuda late on 8 January. Steered under an anomalous blocking pattern over the east-central Atlantic Ocean, the system turned east-southeastward by 10 January, and strengthened to a hurricane-force extratropical low. The change in track caused the system to move over warmer (and anomalously warm) waters, and moderate convection near the center on that day helped initiate the system’s transition to a tropical cyclone. The low began to weaken as it lost its associated fronts, diving to the south-southeast late on 11 January around a mid-latitude trough over the eastern Atlantic. Significant changes were noted the next day, with the large area of gale-force winds shrinking and becoming more symmetric about the cyclone’s center. Convection also increased near the low, and by 1800 UTC 12 January, frontal boundaries appeared to no longer be associated with the cyclone.
    [Show full text]
  • Portugal – an Atlantic Extreme Weather Lab
    Portugal – an Atlantic extreme weather lab Nuno Moreira ([email protected]) 6th HIGH-LEVEL INDUSTRY-SCIENCE-GOVERNMENT DIALOGUE ON ATLANTIC INTERACTIONS ALL-ATLANTIC SUMMIT ON INNOVATION FOR SUSTAINABLE MARINE DEVELOPMENT AND THE BLUE ECONOMY: FOSTERING ECONOMIC RECOVERY IN A POST-PANDEMIC WORLD 7th October 2020 Portugal in the track of extreme extra-tropical storms Spatial distribution of positions where rapid cyclogenesis reach their minimum central pressure ECMWF ERA 40 (1958-2000) Events per DJFM season: Source: Trigo, I., 2006: Climatology and interannual variability of storm-tracks in the Euro-Atlantic sector: a comparison between ERA-40 and NCEP/NCAR reanalyses. Climate Dynamics volume 26, pages127–143. Portugal in the track of extreme extra-tropical storms Spatial distribution of positions where rapid cyclogenesis reach their minimum central pressure Azores and mainland Portugal On average: 1 rapid cyclogenesis every 1 or 2 wet seasons ECMWF ERA 40 (1958-2000) Events per DJFM season: Source: Trigo, I., 2006: Climatology and interannual variability of storm-tracks in the Euro-Atlantic sector: a comparison between ERA-40 and NCEP/NCAR reanalyses. Climate Dynamics volume 26, pages127–143. … affected by sting jets of extra-tropical storms… Example of a rapid cyclogenesis with a sting jet over mainland 00:00 UTC, 23 Dec 2009 Source: Pinto, P. and Belo-Pereira, M., 2020: Damaging Convective and Non-Convective Winds in Southwestern Iberia during Windstorm Xola. Atmosphere, 11(7), 692. … affected by sting jets of extra-tropical storms… Example of a rapid cyclogenesis with a sting jet over mainland Maximum wind gusts: Official station 140 km/h Private station 00:00 UTC, 23 Dec 2009 203 km/h (in the most affected area) Source: Pinto, P.
    [Show full text]
  • 2014 North Atlantic Hurricane Season Review
    2014 North Atlantic Hurricane Season Review WHITEPAPER Executive Summary The 2014 Atlantic hurricane season was a quiet season, closing with eight 2014 marks the named storms, six hurricanes, and two major hurricanes (Category 3 or longest period on stronger). record – nine Forecast groups predicted that the formation of El Niño and below consecutive years average sea surface temperatures (SSTs) in the Atlantic Main – that no major Development Region (MDR)1 through the season would inhibit hurricanes made development in 2014, leading to a below average season. While 2014 landfall over the was indeed quiet, these predictions didn’t materialize. U.S. The scientific community has attributed the low activity in 2014 to a number of oceanic and atmospheric conditions, predominantly anomalously low Atlantic mid-level moisture, anomalously high tropical Atlantic subsidence (sinking air) in the Main Development Region (MDR), and strong wind shear across the Caribbean. Tropical cyclone activity in the North Atlantic basin was also influenced by below average activity in the 2014 West African monsoon season, which suppressed the development of African easterly winds. The year 2014 marks the longest period on record – nine consecutive years since Hurricane Wilma in 2005 – that no major hurricanes made landfall over the U.S., and also the ninth consecutive year that no hurricane made landfall over the coastline of Florida. The U.S. experienced only one landfalling hurricane in 2014, Hurricane Arthur. Arthur made landfall over the Outer Banks of North Carolina as a Category 2 hurricane on July 4, causing minor damage. While Mexico and Central America were impacted by two landfalling storms and the Caribbean by three, Bermuda suffered the most substantial damage due to landfalling storms in 2014.Hurricane Fay and Major Hurricane Gonzalo made landfall on the island within a week of each other, on October 12 and October 18, respectively.
    [Show full text]
  • Adam J Zebzda
    INFLUENCES OF THE URBAN HEAT ISLAND EFFECT AND BROWN OCEAN EFFECT AND THEIR IMPACTS ON LANDFALLING TROPICAL CYCLONES AN PROVINCIAL ATMOSPHERIC CONDITIONS Adam Jozef Zebzda*1 Mount Tabor High School INTRODUCTION (TS) individually. The criteria for selecting a TS for the study was fairly simple. The necessary aspects of each Through the decades, tropical cyclones have shaped system were that it over went intensification overland our coastal infrastructure and continue to do so. During (characterized by an increase in wind speed and a the 2017 Hurricane Season alone, Hurricanes Harvey, decrease of central pressure), that the location of the TS Irma, and Maria have shown us our flaws in urban was within 75 miles (121 kilometers) of a major development and planning, costing billions of dollars in metropolitan area (characterized by containing a damages and loss of life. Tropical Meteorology has population more than 500 thousand residents), and was shown that these cyclones intensify over warm, tropical, substantially far enough from an ocean so as not to be oceanic waters with low vertical wind shear and a moist directly influenced in intensification. With the use of atmosphere; however, could a large metropolitan area satellite, it was possible to determine the area and do the same? Records exist of overland cyclone magnitude of an urban heat island remotely and intensification, such as Tropical Storm Erin (2007). This accurately. particular system intensified over the state of Oklahoma, only 65 miles (105 kilometers) northwest of Oklahoma Once TS case studies were developed, the exact City, reaching winds of 80 miles per hour (mph).
    [Show full text]
  • 2021 Rio Grande Valley/Deep S. Texas Hurricane Guide
    The Official Rio Grande Valley/Deep South Texas HURRICANE GUIDE 2021 IT ONLY TAKES ONE STORM! weather.gov/rgv A Letter to Residents After more than a decade of near-misses, 2020 reminded the Rio Grande Valley and Deep South Texas that hurricanes are still a force to be reckoned with. Hurricane Hanna cut a swath from Padre Island National Seashore in Kenedy County through much of the Rio Grande Valley in late July, leaving nearly $1 billion in agricultural and property damage it its wake. While many may now think that we’ve paid our dues, that sentiment couldn’t be further from the truth! The combination of atmospheric and oceanic patterns favorable for a landfalling hurricane in the Rio Grande Valley/Deep South Texas region can occur in any season, including this one. Residents can use the experience of Hurricane Hanna in 2020 as a great reminder to be prepared in 2021. Hurricanes bring a multitude of hazards including flooding rain, damaging winds, deadly storm surge, and tornadoes. These destructive forces can displace you from your home for months or years, and there are many recent cases in the United States and territories where this has occurred. Hurricane Harvey (2017), Michael (2018, Florida Panhandle), and Laura (2020, southwest Louisiana) are just three such devastating events. This guide can help you and your family get prepared. Learn what to do before, during and after a storm. Your plan should include preparations for your home or business, gathering supplies, ensuring your insurance is up to date, and planning with your family for an evacuation.
    [Show full text]
  • 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.
    [Show full text]
  • Hurricane Irma Storm Review
    Hurricane Irma Storm Review November 11, 2018 At Duke Energy Florida, we power more than 4 million lives Service territory includes: . Service to 1.8 million retail customers in 35 counties . 13,000 square miles . More than 5,100 miles of transmission lines and 32,000 miles of distribution lines . Owns and operates nearly 9,500 MWs of generating capacity . 76.2% gas, 21% coal, 3% renewable, 0.2%oil, 2,400 MWs Purchased Power. 2 Storm Preparedness Activities Operational preparation is a year-round activity Coordination with County EOC Officials . Transmission & Distribution Systems Inspected and . Structured Engagement and Information Maintained Sharing Before, During and After Hurricane . Storm Organizations Drilled & Prepared . Coordination with county EOC priorities . Internal and External Resource Needs Secured . Public Communications and Outreach . Response Plan Tested and Continuously Improved Storm Restoration Organization Transmission Hurricane Distribution System Preparedness System Local Governmental Coordination 3 Hurricane Irma – Resources & Logistics Resources . 12,528 Total Resources . 1,553 pre-staged in Perry, Georgia . 91 line and vegetation vendors from 25 states . Duke Energy Carolinas and Midwest crews as well as resources from Texas, New York, Louisiana, Colorado, Illinois, Oklahoma, Minnesota, Maine and Canada . 26 independent basecamps, parking/staging sites Mutual Assistance . Largest mobilization in DEF history . Mutual Assistance Agreements, executed between DEF and other utilities, ensure that resources can be timely dispatched and fairly apportioned. Southeastern Electric Exchange coordinates Mutual Assistance 4 5. Individual homes RESTORATION 3. Critical Infrastructure 2. Substations 1. Transmission Lines 4. High-density neighborhoods 5 Hurricane Irma- Restoration Irma’s track northward up the Florida peninsula Restoration Summary resulted in a broad swath of hurricane and tropical Customers Peak Customers Outage storm force winds.
    [Show full text]
  • Development of a Nationwide Real-Time 3-D Wind and Reflectivity Radar Composite in France Olivier Bousquet, Pierre Tabary
    Development of a Nationwide Real-Time 3-D Wind and Reflectivity Radar Composite in France Olivier Bousquet, Pierre Tabary To cite this version: Olivier Bousquet, Pierre Tabary. Development of a Nationwide Real-Time 3-D Wind and Reflectivity Radar Composite in France. Quarterly Journal of the Royal Meteorological Society, Wiley, 2014, 140 (611-625), pp.qj.2163. hal-00955745 HAL Id: hal-00955745 https://hal.archives-ouvertes.fr/hal-00955745 Submitted on 5 Mar 2014 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Development of a Nationwide Real-Time 3-D Wind and Reflectivity Radar Composite in France Olivier Bousquet1 and Pierre Tabary Météo France and CNRM-GAME, Toulouse, France Submitted to Quarterly Journal of the Royal Meteorological Society August 2012 Revised December 2012 & February 2013 Abstract The ability to perform multiple-Doppler wind synthesis from operational weather radar systems on an operational basis has been investigated by the French Weather Service since 2006 using a (sub) network of 6 Doppler radars covering the greater Paris area. This analysis has been recently extended to the entire French radar network so as to implement a nationwide, three-dimensional reflectivity and wind field mosaic to be eventually delivered to forecasters and modelers, as well as automatic nowcasting systems for air traffic management purposes.
    [Show full text]
  • 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.
    [Show full text]