SC Hurricanes Executive Summary
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Tropical Cyclone Report for Hurricane Ivan
Tropical Cyclone Report Hurricane Ivan 2-24 September 2004 Stacy R. Stewart National Hurricane Center 16 December 2004 Updated 27 May 2005 to revise damage estimate Updated 11 August 2011 to revise damage estimate Ivan was a classical, long-lived Cape Verde hurricane that reached Category 5 strength three times on the Saffir-Simpson Hurricane Scale (SSHS). It was also the strongest hurricane on record that far south east of the Lesser Antilles. Ivan caused considerable damage and loss of life as it passed through the Caribbean Sea. a. Synoptic History Ivan developed from a large tropical wave that moved off the west coast of Africa on 31 August. Although the wave was accompanied by a surface pressure system and an impressive upper-level outflow pattern, associated convection was limited and not well organized. However, by early on 1 September, convective banding began to develop around the low-level center and Dvorak satellite classifications were initiated later that day. Favorable upper-level outflow and low shear environment was conducive for the formation of vigorous deep convection to develop and persist near the center, and it is estimated that a tropical depression formed around 1800 UTC 2 September. Figure 1 depicts the “best track” of the tropical cyclone’s path. The wind and pressure histories are shown in Figs. 2a and 3a, respectively. Table 1 is a listing of the best track positions and intensities. Despite a relatively low latitude (9.7o N), development continued and it is estimated that the cyclone became Tropical Storm Ivan just 12 h later at 0600 UTC 3 September. -
HISTORICAL HURRICANES in SOUTH CAROLINA September 10-22, 1989 N Average, South Carolina Experiences a Land-Falling Hurricane Hurricane Hugo Every Seven Years
HISTORICAL HURRICANES IN SOUTH CAROLINA September 10-22, 1989 n average, South Carolina experiences a land-falling hurricane Hurricane Hugo every seven years. Between 1900 and 2000, 14 hurricanes Time of Landfall: 12 a.m., 9/22/1989 Saffir/Simpson Scale Category: Category 4 Omade landfall along the coast of South Carolina including three Location of Landfall: Sullivans Island, SC Estimated U.S. Damage Costs: $7 billion major hurricanes: Hurricane Hugo (1989), Hurricane Gracie (1959), Maximum Winds at Landfall: 140 mph Estimated U.S. Deaths: 49 and Hurricane Hazel (1954). These South Carolina hurricanes made the Minimum Pressure at Landfall: 27.58” (934 mb) Estimated Storm Surge: 18-20 feet Top 40 Most Intense Hurricanes in a study by scientists at the National Hurricane Center. Rankings were based on minimum central pressures SUMMARY at the time of landfall. Hugo ranked #11 on the list, followed by Hazel Hugo originated off the coast of western Africa near the Cape Verde Islands as a tropical disturbance on September 9th and quickly gained strength to a tropical storm on the 11th and hurricane on the 13th. Hugo reached maximum intensity at Category 5 on the 15th with winds estimated at 160 mph and a minimum pressure of 918 mb east of the Leeward Islands. at #13, and Gracie at #33. Although major hurricanes are rare for the The hurricane passed directly over the islands of Guadaloupe, St. Croix, and Puerto Rico over the next few days before heading northwestward toward the South Carolina coast. By 6 a.m. coastal sections of South Carolina, averaging one every 25 years, the EDT on September 21, 1989, hurricane warnings were issued for coastal South Carolina and more than 250,000 people evacuated the coast. -
Understanding Our Coastal Environment
Preface The South Carolina Beachfront Management Act In the Beginning The Coastal Zone Management Act of 1977 was enacted to protect our coastal resources from unwise development. This legislation served the beaches well during its first decade, but as South Carolina became a more popular tourist destination, it became apparent that the portion of the Act that dealt with beaches was inadequate. As development crept seaward, seawalls and rock revetments proliferated, damaging the public’s beach. In many areas there was no beach left at high tide. In some areas, there was no beach at low tide, either. In 1988 and again in 1990, South Carolina’s legislators took action and amended and strengthened the Coastal Zone Management Act. The resulting Beachfront Management Act protects South Carolina’s sandy shores by increasing the state’s jurisdiction and encouraging development to move landward. South Carolina’s Beachfront Jurisdiction To find the boundaries of this jurisdiction, staff from the Office of Ocean and Coastal Resource Management must first locate the baseline, which is the crest of the primary oceanfront sand dune. Where there are no dunes, the agency uses scientific methods to determine where the natural dune would lie if natural or man-made occurrences had not interfered with nature’s dune building process. The setback line is the most landward boundary and is measured from the baseline. To find the depth of the setback line, the beach’s average annual erosion rate for the past forty years is calculated and multiplied by forty. For example, if the erosion rate is one foot per year, the results will be a setback line that stretches forty feet from the baseline. -
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. -
Dear Investors As You May Might Have Heard from Different Media Outlets
Dear investors As you may might have heard from different media outlets, the east coast of the U.S. is facing a potential threat of landfall of the major hurricane named Florence in the coming days. The storm is currently about 385 miles/620 KM southwest of BERMUDA and about 625 miles/1005 KM southeast of Cape Fear North CAROLINA, moving to the direction of North and South Carolina. The intensity is currently Cat 4, with maximum sustained wind speed very close to 140 mph. As the storm moves to the coast, the wind will intensify to Cat 5 and maximum sustained winds can reach 155 mph. Timing is more difficult to predict now as many meteorologists suggest Florence will slow on approach to the coast, with a possible stalling that could exacerbate the impacts for the area it nears the shore. Catastrophe risk modeller RMS said, “Florence will be the strongest hurricane to make landfall over North Carolina since Hazel in 1954 – this would be a major event for the insurance industry. As with all hurricanes of this intensity, Florence poses significant impacts due to damaging hurricane-force winds and coastal storm surge, but inland flooding is becoming an increasing threat. Forecasts include the possibility of Florence slowing down after landfall and causing as much as 20 inches of rain in the Carolinas. While very significant, this remains much lower than the amount of rainfall observed last year during Hurricane Harvey.” Wind Florence is expected to make landfall as a hurricane between Cat 3 and Cat 4. The wind speed can reach 110-130 mph and central pressure is estimated 962mb. -
Comparison of Destructive Wind Forces of Hurricane Irma with Other Hurricanes Impacting NASA Kennedy Space Center, 2004-2017
Comparison of Destructive Wind Forces of Hurricane Irma with Other Hurricanes Impacting NASA Kennedy Space Center, 2004 - 2017 Presenter: Mrs. Kathy Rice Authors KSC Weather: Dr. Lisa Huddleston Ms. Launa Maier Dr. Kristin Smith Mrs. Kathy Rice NWS Melbourne: Mr. David Sharp NOT EXPORT CONTROLLED This document has been reviewed by the KSC Export Control Office and it has been determined that it does not meet the criteria for control under the International Traffic in Arms Regulations (ITAR) or Export Administration Regulations (EAR). Reference EDR Log #: 4657, NASA KSC Export Control Office, (321) 867-9209 1 Hurricanes Impacting KSC • In September 2017, Hurricane Irma produced sustained hurricane force winds resulting in facility damage at Kennedy Space Center (KSC). • In 2004, 2005, and 2016, hurricanes Charley, Frances, Jeanne, Wilma, and Matthew also caused damage at KSC. • Destructive energies from sustained wind speed were calculated to compare these hurricanes. • Emphasis is placed on persistent horizontal wind force rather than convective pulses. • Result: Although Hurricane Matthew (2016) provided the highest observed wind speed and greatest kinetic energy, the destructive force was greater from Hurricane Irma. 2 Powell & Reinhold’s Article 2007 • Purpose: “Broaden the scientific debate on how best to describe a hurricane’s destructive potential” • Names the following as poor indicators of a hurricane’s destructive potential • Intensity (Max Sustained Surface Winds): Provides a measure to compare storms, but does not measure destructive potential since it does not account for storm size. • The Saffir-Simpson scale: Useful for communicating risk to individuals and communities, but is only a measure of max sustained winds, again, not accounting for storm size. -
Improvement of Hurricane Risk Perceptions: Re-Analysis of a Hurricane Damage Index and Development of Spatial Damage Assessments
Improvement of hurricane risk perceptions: re-analysis of a hurricane damage index and development of spatial damage assessments Sandra N. Maina Academic Affiliation, Fall 2011: Senior, Florida Institute of Technology SOARS® Summer 2011 Science Research Mentor: James Done, Cindy Bruyere Writing and Communication Mentor: Cody Phillips ABSTRACT Implementation of potential damage assessment tools in hurricane-prone areas is an essential aspect of communicating accurate hurricane risk information. Several indices currently exist (e.g., Saffir-Simpson Hurricane Wind Scale) that effectively communicate storm strength; however, they are unable to quantify potential damage. The recently developed Maina Hurricane Index (MHI) addressed this deficiency and used a hurricane‟s central minimum pressure and radius of hurricane-force winds to create damage forecasts. The MHI was developed by analyzing data from 13 historical storms – a small sample size limited by the availability of storm size data. This work revisited the MHI using a larger data set, and results showed that central pressure is the best indicator of potential damage. By creating a single damage value per storm, the MHI aids in the decision-making of government and private agencies such as emergency managers, yet it does not convey storm impacts on individuals within a community. In response, this study also developed a methodology to generate spatial damage assessments that illustrate the relative damage distribution across a storm‟s path. A swath of maximum winds was first generated using a parametric wind field model, then translated to damage using a function based on wind speed and a measure of the directional change in wind. Through the ability to forecast both net damage of land falling storms and the distribution of damage across the storm‟s path, individual perceptions of hurricane risk can be unified to make way for safer preparation and evacuation decisions. -
The Hurricane-Tornado
July 1965 John S. Smith 453 THEHURRICANE-TORNADO JOHN S. SMITH Weather Bureau Forecast Center, Chicago, 111. ABSTRACT Climatological data in recent years have become sufficient for the further study of tornadoes which occur in hurricane systems. Several characteristics of the hurricane tornado are determined from data for an 8-yr. period by plotting the center positions of each hurricane and its associated tornadoes. The data show: (1) a comparison betweenhurricane and non-hurricane tornadoes; (2) a “Significant Sector” fortornado-genesis; (3) a “Preferred Quadrant” of the hurricane for tornado-genesis; (4) the mostfavorable time of dayfor tornado occurrence; (5) tornado frequencies with,respect to various speeds and distances of the hurricane on and off shore; (6) a tenative hurricane model. 1. INTRODUCTION the “Preferred Quadrant.” Other significant patterns are established from the relationship of the tornado to the Although considerable research has been done on the hurricane. forecasting problemspresented byboth tornadoes and hurricanes, relatively little investigation has been made 2. GENERALCLIMATOLOGY intothe forecasting problems of tornadoesassociated with hurricanes. In this study of the hurricane-tornado Of 15 hurricanes that entered the United States from problem,a climatological analysishas been made by the Gulf of Mexico andthrough the Atlantic Coastal plottingthe center position of eachhurricane and its States, 11 produced tornadoes. Atotal of 98 tornadoes associated tornadoes. was produced during the period from hurricane Connie in August 1955, to hurricane Carla in September 1961. Of Recognition of hurricane tornadoes prior to 1955 was the hurricanes producing tornadoes, the average number apparently limited-unless therehas beensuddena of tornadoes per hurricane is 9, although hurricanes Audrey rash of hurricane-tornadoesin recent years, for since and Carla spawned more than 20 tornadoes each. -
174 197 2,808 263 27 146 3,354 2,875 5 137 229 43 49 228 12,285 Total Per Hr
PENNSYLVANIA BIRDS Seasonal Editors Daniel Brauning Journal of the Pennsylvania Society for Ornithology Michael Fialkovich Deuane Hoffman Volume 17 Number 4 August – November 2003 Douglas Kibbe Roberta Zwier Nick Pulcinella - Editor-in-chief Department Editors (610) 696-0687 [email protected] Book Reviews http://www.pabirds.org Gene Wilhelm, Ph.D. 513 Kelly Blvd. Slippery Rock 16057-1145 724-794-2434 [email protected] CBC Report Contents Nick Bolgiano 711 W. Foster Ave. State College, PA 16801 245 Editorial 814-234-2746 [email protected] 246 Hurricane Isabel’s Birds with notes on previous tropical storms Hawk Watch Reports and storm related birds....... Nick Pulcinella and Jim Lockyer Kyle McCarty 265 Band-rumped Storm-petrel Bald Eagle State Park, Keith Bildstein Hawk Mountain Sanctuary Centre County, Pennsylvania, 9/20/03............ Rick Wiltraut 1700 Hawk Mountain Road Kempton 19529 267 Pennsylvania’s Second Long-tailed Jaeger, Bucks County . Bill Etter (610) 756-6961 269 Autumn Raptor Migration Summary 2003 ..............Kyle McCarty [email protected] 277 BOOK REVIEW - Kaufman Focus Guides, Butterflies of North America NAMC Bill Etter ........................................... Gene Wilhelm 1030 Old Bethlehem Rd, Apt#2 278 Photo Quiz #2 Answer.............................. Rick Wiltraut Perkasie, PA 18944 (215)-258-0229 279 Summary of the Season - August - November 2003 . Deuane Hoffman [email protected] 281 Birds of Note - August- November 2003 Pennsylvania Birdlists 283 Local Notes Peter Robinson P. O. Box 482 295 Photo Highlights Hanover, PA 17331 [email protected] 314 Fall Migration tables Photo-Quiz Rick Wiltraut Photo-Quiz #3 - Inside back cover Jacobsburg EE Center 835 Jacobsburg Road Wind Gap, PA 18091 Site Guides Rudy Keller 71 Lutz Rd Boyertown, PA 19512 610-845-7310 [email protected] Data Technician Wendy Jo Shemansky 1613 Aurelius Street, Apt. -
The Flooding of Hurricane Ivan: How Far Ahead Can We Predict?
P1.7 THE FLOODING OF HURRICANE IVAN: HOW FAR AHEAD CAN WE PREDICT? Michael P. Erb*, Douglas K. Miller National Environmental Modeling and Analysis Center University of North Carolina – Asheville, Asheville, North Carolina 1. INTRODUCTION will be modeled using the Weather Research and Forecasting (WRF) Model. Naturally, since On September 17th 2004, Hurricane Ivan (by this is only a case study, the results found here then a tropical depression) began making its will not answer the question in a general sense. way along the western edge of North Carolina, But it is hoped, at the very least, that they should threatening to bring a deluge of rainfall to give interested parties a better understanding of regions surrounding the Appalachian Mountains. the problem at hand. Many of these places had been flooded by Another reason for this research is that it Hurricane Frances only two weeks before and, ties in with the goals of the Renaissance still not fully recovered, feared a repeat of those Computing Institute (RENCI), an organization events. All indicators pointed to Ivan being on based in North Carolina which is dedicated to the same scale as Frances, and forecasters solving complex, multidisciplinary problems that called for heavy rain and yet more flooding. People there, understandably, prepared for the worst. (Figures 1 and 2 show the tracks of Hurricanes Ivan and Francis.) What actually happened over the next few days turned out to be on a somewhat smaller scale. The rain did come, but not to the extent forecasters had predicted. In places where Frances had dumped 20 or more inches of rain – Mount Mitchell, NC, for instance – Ivan brought 15 or less. -
Analysis of the Deconstruction of Dyke Marsh, George Washington
Analysis of the Deconstruction of Dyke Marsh, George Washington Memorial Parkway, Virginia: Progression, Geologic and Manmade Causes, and Effective Restoration Scenarios Dyke Marsh image credit: NASA Open-File Report 2010-1269 U.S. Department of the Interior U.S. Geological Survey Cover photograph: Hurricane Isabel approaching landfall, September 17, 2003. The storm’s travel path is shaded, and trends from southeast to north-northwest. The initial cloud bands from Isabel are arriving at Dyke Marsh in this image. Base imagery taken from a LANDSAT 5 visible image; see appendix 3A. Analysis of the Deconstruction of Dyke Marsh, George Washington Memorial Parkway, Virginia: Progression, Geologic and Manmade Causes, and Effective Restoration Scenarios By Ronald J. Litwin, Joseph P. Smoot, Milan J. Pavich, Helaine W. Markewich, Erik Oberg, Ben Helwig, Brent Steury, Vincent L. Santucci, Nancy J. Durika, Nancy B. Rybicki, Katharina M. Engelhardt, Geoffrey Sanders, Stacey Verardo, Andrew J. Elmore, and Joseph Gilmer Prepared in cooperation with the National Park Service Open-File Report 2010–1269 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2011 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1-888-ASK-USGS For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. -
Tropical Cyclone Intensity
Hurricane Life Cycle and Hazards John Cangialosi and Robbie Berg National Hurricane Center National Hurricane Conference 26 March 2012 Image courtesy of NASA/Goddard Space Flight Center Scientific Visualization Studio What is a Tropical Cyclone? • A relatively large and long‐lasting low pressure system – Can be dozens to hundreds of miles wide, and last for days • No fronts attached • Forms over tropical or subtropical oceans • Produces organized thunderstorm activity • Has a closed surface wind circulation around a well‐defined center • Classified by maximum sustained surface wind speed – Tropical depression: < 39 mph – Tropical storm: 39‐73 mph – Hurricane: 74 mph or greater • Major hurricane: 111 mph or greater Is This a Tropical Cyclone? Closed surface circulation? Organized thunderstorm activity? Tropical Depression #5 (later Ernesto) Advisory #1 issued based on aircraft data The Extremes: Tropical vs. Extratropical Cyclones Hurricane Katrina (2005) Superstorm Blizzard of March 1993 Tropical Cyclones Occur Over Tropical and Subtropical Waters Across the Globe Tropical cyclones tracks between 1985 and 2005 Atlantic Basin Tropical Cyclones Since 1851 Annual Climatology of Atlantic Hurricanes Climatological Areas of Origin and Tracks June: On average about 1 storm every other year. Most June storms form in the northwest Caribbean Sea or Gulf of Mexico. July: On average about 1 storm every year . Areas of possible development spreads east and covers the western Atlantic, Caribbean, and Gulf of Mexico. Climatological Areas of Origin and Tracks August: Activity usually increases in August. On average about 2‐3 storms form in August. The Cape Verde season begins. September: The climatological peak of the season. Storms can form nearly anywhere in the basin.