USING GIS to UNDERSTAND HURRICANE WINDFIELDS in the GULF of MEXICO Jill F

Total Page:16

File Type:pdf, Size:1020Kb

USING GIS to UNDERSTAND HURRICANE WINDFIELDS in the GULF of MEXICO Jill F USING GIS TO UNDERSTAND HURRICANE WINDFIELDS IN THE GULF OF MEXICO Jill F. Hasling, President Certified Consulting Meteorologist Weather Research Center 5104 Caroline St. Houston, Texas 77004 www.wxresearch.com Using GIS to 1900-1959 determine if Hurricanes there are East of 45W more hurricanes. 1960-2006 Hurricanes East of 45W Using GIS to 1900-1959 determine if Hurricanes there are East of 45W more hurricanes. Conclusion: Since satellite use started after 1960, more 1960-2006 hurricanes Hurricanes must be the East of 45W result of satellites and not global warming. Hurricane Rita 2005 66 platforms destroyed 32 more suffering extensive damage 13 MODUs broke their moorings and were set adrift 1 jack-up sunk 7 jack-ups and 2 semi-subs had extensive damage Hurricane Katrina 2005 47 platforms destroyed 20 more suffering extensive damage 6 rigs broken from moorings and set adrift 3 platform rigs destroyed 1 jack-up capsized 2 jack-ups and 5 semi-subs had extensive damage Hurricane Ivan 2004 7 platforms destroyed 6 more suffering extensive damage 5 drilling rigs with major damage Hurricane Lili 2002 6 platforms destroyed 31 platforms seriously damaged 4 MODUs broken from their moorings and set adrift 2 jack-ups capsized GFS Adriatic VII Jack-up Before and after Hurricane Rita 2005 Shell Mars Platform Before and after Hurricane Katrina 2005 BP Eugene Island 322 Platform A Before and after Hurricane Lili 2002 MedusaMedusa Sparafter -Hurricane Mississippi Ivan Canyon 2004 582 after Hurricane Ivan 2004 GULF OF MEXICO HURRICANES – Orange are Category 3 hurricanes, Red are Category 4 hurricanes and Purple are Category 5 hurricanes GULF OF MEXICO HURRICANES CAT 5 GULF OF MEXICO HURRICANES CAT 4 & 5 GULF OF MEXICO HURRICANES CAT 3, 4 & 5 Structure of a hurricane - The strongest winds will be on the right side of the hurricane just outside the eye wall. SPIRAL BAND EYE WALL Highest sustained winds EYE WRC meteorologists have a hurricane windfield model they use to forecast and hindcast the maximum sustained winds in a hurricane. These windfields are then mapped using ESRI ArcGIS. For example, the following graph is the windfield of Hurricane Katrina 2005 when it was a Category 5 hurricane on Hurricane Alicia 1983 track into the Houston area. Highest Winds on the right of the track Katrina as a Cat 5 on Hurricane Alicia’s track WRC meteorologists then used ArcGIS to study some significant Gulf of Mexico hurricanes that influenced the oil lease areas. ArcGIS layering capabilities allow WRC meteorologists to add the well data to the oil leases. Purple - Cat 5 Red - Cat 4 Orange - Cat 3 A layer with the tracks of Hurricanes Hilda-1964, Betsy-1965, Camille-1969, Carmen-1974, Lili-2002, Ivan-2004, Katrina-2005, & Rita-2005 was added. The hurricane windfield layers were then added. Hurricanes come in all sizes. Compare Hurricane Katrina 2005 windfield with Hurricane Camille 1969. Windfield of Hurricane Camille - 1969 Windfield of Hurricane Katrina - 2005 Size of the windfield can change during the storm. Hurricane Rita 2005 when maximum winds were over the Green Canyon Lease. Zooming in on wells and maximum sustained winds Zooming in on wells and maximum sustained winds Comparison between the windfields of Hurricane Carla 1961 and Hurricane Andrew 1992. Yellow indicates winds of 64 knots or higher. Notice how much smaller the windfield for Andrew was. Windfield for Hurricane Carmen 1974 Hurricane Katrina 2005 radar layered with wells Close up of Hurricane Katrina radar and oil blocks Hurricane Katrina 2005 radar at landfall with wells Forecast of windfields for Rita on Sep 22 with actual track Using GIS to show typhoon threat versus vessel route Using GIS to demonstrate risk from cyclone in Bay of Bengal Windfield forecast of along the forecast track versus windfield for the worst track for the operation site. Cyclone with maximum sustained winds of 135 knots. 2008 Atlantic Hurricane Outlook Coast with the highest risk of landfall is Georgia to North Carolina with 90% Louisiana to Alabama has 60% chance of a landfall WRC GRAY NOAA/NWS Number of Named Storms: 11 13 Number of Storm Days: 83 60 Number intensifying into Hurricanes: 5 7 Number of Hurricane Days: 24 30 US Landfalls: 4 Cat 3 or Higher Storms in the Atlantic: 50% 3 Weather Research Center Houston, Texas www.wxresearch.com [email protected] Hurricanes from 1950 to 2003 with maximum sustained winds 100 knots or greater - 20 Hurricanes from 1950 to 2003 with maximum sustained winds 100 knots or greater - 20 Hurricanes from 1900 to 1949 with maximum sustained winds 100 knots or greater - 17 Hurricanes from 1950 to 2003 with maximum sustained winds 100 knots or greater - 20 Hurricanes from 1900 to 1949 with maximum sustained winds 100 knots or greater - 17 Hurricanes from 1851 to 1899 with maximum sustained winds 100 knots or greater - 16 Tropical Cyclones 1851-1899 1851 to 1899 16 Intense hurricanes [maximum sustained winds of 100 knots or greater] over the GOM Oil leases [North of 25W and West of 85W] 1851 to 1899 16 Intense hurricanes [maximum sustained winds of 100 knots or greater] over the GOM Oil leases [North of 25W and West of 85W] 2 year when there were 2 or more intense hurricanes - 1852 and 1856 1851 to 1899 16 Intense hurricanes [maximum sustained winds of 100 knots or greater] over the GOM Oil leases [North of 25W and West of 85W] 2 year when there were 2 or more intense hurricanes - 1852 and 1856 There were 14 years with intense hurricanes in these 50 years giving a probability of experiencing an intense hurricane over the GOM oil leases of 28% in any year. Tropical Cyclones 1900-1949 1950 to 2003 20 Intense hurricanes [maximum sustained winds of 100 knots or greater] over the GOM Oil leases [North of 25W and West of 85W] 1950 to 2003 20 Intense hurricanes [maximum sustained winds of 100 knots or greater] over the GOM Oil leases [North of 25W and West of 85W] 1 year when there were 2 or more intense hurricanes - 1985 1950 to 2003 20 Intense hurricanes [maximum sustained winds of 100 knots or greater] over the GOM Oil leases [North of 25W and West of 85W] 1 year when there were 2 or more intense hurricanes - 1985 There were 19 years with intense hurricanes in these 54 years giving a probability of experiencing an intense hurricane over the GOM oil leases of 35% in any year. Tropical Cyclones 1950-2003 1900 to 1949 17 Intense hurricanes [maximum sustained winds of 100 knots or greater] over the GOM Oil leases [North of 25W and West of 85W] 1900 to 1949 17 Intense hurricanes [maximum sustained winds of 100 knots or greater] over the GOM Oil leases [North of 25W and West of 85W] 3 year when there were 2 or more intense hurricanes - 1909, 1915 and 1916 1900 to 1949 17 Intense hurricanes [maximum sustained winds of 100 knots or greater] over the GOM Oil leases [North of 25W and West of 85W] 3 year when there were 2 or more intense hurricanes - 1909, 1915 and 1916 There were 14 years with intense hurricanes in these 50 years giving a probability of experiencing an intense hurricane over the GOM oil leases of 28% in any year. 1900 to 2003 37 Intense hurricanes [maximum sustained winds of 100 knots or greater] over the GOM Oil leases [North of 25W and West of 85W] 1900 to 2003 37 Intense hurricanes [maximum sustained winds of 100 knots or greater] over the GOM Oil leases [North of 25W and West of 85W] 5 Years when there were 2 or more intense hurricanes - 1909, 1915 , 1916, 1975 and 1985 1900 to 2003 37 Intense hurricanes [maximum sustained winds of 100 knots or greater] over the GOM Oil leases [North of 25W and West of 85W] 5 Years when there were 2 or more intense hurricanes - 1909, 1915 , 1916, 1975 and 1985 There were 32 years with intense hurricanes in these 104 years giving a probability of experiencing an intense hurricane over the GOM oil leases of 31% in any year. NOTABLE CATEGORY 5 GOM LEASE HURRICANES 165 kts Hurricane Camille 1969 155 kts Hurricane Allen 1980 150 kts Hurricane Carla 1961 140 kts Hurricane Beulah 1967 140 kts Hurricane Ethel 1960 135 kts Hurricane Betsy 1965 Comparing the last three 50 year periods: 1851 to 1899, 1900 to 1949 and 1950 to 2003 Assuming that the maximum sustained 1 minute winds in hurricanes prior to 1950 were underestimated, 15 knots was added to the 1 minute winds. The number of Category 4 and 5 cyclones over the Gulf of Mexico Oil Lease is: 1851-1899 1900-1949 1950-2003 +15 kts +10 kts +15 kts +10 kts CAT 5 3 3 5 2 5 CAT 4 13 6 12 12 8 CAT 3 17 19 10 7 7 TOTAL 33 28 27 21 20 1851 1861 1871 6 0 4 1881 1891 1901 3 3 3 1911 1921 1931 7 1 2 Number of Intense Hurricanes by Decade over the Gulf of Mexico 1941 1951 1961 5 3 6 1981 1971 1991 4 3 3 2001 6 GOM OIL LEASE INTENSE HURRICANES BY DECADE AND 30 YEAR CYCLES CYCLE 1 CYCLE 2 CYCLE 3 1851-1860 6 1861-1870 0 1871-1880 4 1881-1890 3 1891-1900 3 1901-1910 3 1911-1920 7 1921-1930 1 1931-1940 2 1941-1950 5 1951-1960 3 1961-1970 6 1971-1980 4 1981-1990 3 1991-2000 3 2001-2010 6 USING 30 YEAR AVERAGES THE FORECAST OF INTENSE GOM HURRICANES 2001-2011 5 2011-2020 2 2021-2030 3.6 ACTIVE INACTIVE ACTIVE Weather Research Center Houston, Texas www.wxresearch.com [email protected].
Recommended publications
  • Historical Changes in the Mississippi-Alabama Barrier Islands and the Roles of Extreme Storms, Sea Level, and Human Activities
    HISTORICAL CHANGES IN THE MISSISSIPPI-ALABAMA BARRIER ISLANDS AND THE ROLES OF EXTREME STORMS, SEA LEVEL, AND HUMAN ACTIVITIES Robert A. Morton 88∞46'0"W 88∞44'0"W 88∞42'0"W 88∞40'0"W 88∞38'0"W 88∞36'0"W 88∞34'0"W 88∞32'0"W 88∞30'0"W 88∞28'0"W 88∞26'0"W 88∞24'0"W 88∞22'0"W 88∞20'0"W 88∞18'0"W 30∞18'0"N 30∞18'0"N 30∞20'0"N Horn Island 30∞20'0"N Petit Bois Island 30∞16'0"N 30∞16'0"N 30∞18'0"N 30∞18'0"N 2005 2005 1996 Dauphin Island 1996 2005 1986 1986 30∞16'0"N Kilometers 30∞14'0"N 0 1 2 3 4 5 1966 30∞16'0"N 1950 30∞14'0"N 1950 Kilometers 1917 0 1 2 3 4 5 1917 1848 1849 30∞14'0"N 30∞14'0"N 30∞12'0"N 30∞12'0"N 30∞12'0"N 30∞12'0"N 30∞10'0"N 30∞10'0"N 88∞46'0"W 88∞44'0"W 88∞42'0"W 88∞40'0"W 88∞38'0"W 88∞36'0"W 88∞34'0"W 88∞32'0"W 88∞30'0"W 88∞28'0"W 88∞26'0"W 88∞24'0"W 88∞22'0"W 88∞20'0"W 88∞18'0"W 89∞10'0"W 89∞8'0"W 89∞6'0"W 89∞4'0"W 88∞58'0"W 88∞56'0"W 88∞54'0"W 88∞52'0"W 30∞16'0"N Cat Island Ship Island 30∞16'0"N 2005 30∞14'0"N 1996 30∞14'0"N 1986 Kilometers 1966 0 1 2 3 30∞14'0"N 1950 30∞14'0"N 1917 1848 Fort 2005 Massachusetts 1995 1986 Kilometers 1966 0 1 2 3 30∞12'0"N 1950 30∞12'0"N 1917 30∞12'0"N 30∞12'0"N 1848 89∞10'0"W 89∞8'0"W 89∞6'0"W 89∞4'0"W 88∞58'0"W 88∞56'0"W 88∞54'0"W 88∞52'0"W Open-File Report 2007-1161 U.S.
    [Show full text]
  • Impacts of Global Warming on Hurricane-Related Flooding in Corpus Christi,Texas
    Impacts of Global Warming on Hurricane-related Flooding in Corpus Christi, Texas Sea-level Rise and Flood Elevation A one-foot rise in flood elevation due to both sea-level rise and hurricane intensification leads to an inundation of 5000 –15,000 feet. Global Sea-level Rise Global warming causes sea level to rise through Limitations of the Analysis two major mechanisms. First, as water warms, it expands, taking up more space. Second, as ice This analysis looked only at damages due to flooding by storm on land melts (including mountain glaciers surge and sea-level rise. It is not a comprehensive analysis of the wide array of hurricane-related damages. Other simplifying around the world as well as the polar ice assumptions were made and there were limitations due to lack of sheets), this water flows to the oceans. data. For example, no data on historical flood damage to oil The thermal expansion of the oceans and the refineries was available to the researchers. melting of mountain glaciers are well understood. Increased melting and loss of ice on In addition, the study assumes that the barrier island retains its elevation and volume as sea level rises, though under high rates of parts of the polar ice sheets has recently been sea-level rise, the relative condition of the barrier island would be observed, especially on Greenland, although how expected to weaken, posing additional risk for erosion of the island much and how fast the ice sheets will increase and for flooding in the bay, both of which would increase economic sea-level rise is not well known, and this damages.
    [Show full text]
  • Hurricane Fifi and the 1974 Autumn Migration in El Salvador
    condor, 82:212-218 @I The Cooper Ornithological Society 1980 HURRICANE FIFI AND THE 1974 AUTUMN MIGRATION IN EL SALVADOR WALTER A. THURBER ABSTRACT.-In the autumn of 1974 the migration pattern in El Salvador had several unusual features, too many to have been merely coincidental: 1) delayed arrival of certain early migrants whose appearance overlapped with that of later migrants; 2) unprecedented numbers of a few species; 3) the appearance of several rarely seen or previously unreported species; 4) exten- sion of winter ranges of a few species which was maintained for several years after. These events were closely associated with Hurricane Fifi (17-20 Sep- tember) and to a lesser extent with Hurricane Carmen (l-6 September). I attribute the unusual features of the 1974 migration to Hurricane Fifi (pos- sibly augmented by Carmen) after comparison of routes and schedules of early migrants with the route, dates, wind directions, and velocities of Fifi. I suggest that other hurricanes have affected and will affect migration through Middle America but that serious disruptions are probably rare and unpre- dictable. In the course of my 10 years of netting and METHODS AND SOURCES OF DATA banding birds in El Salvador, Central Amer- From my field notes and netting records I selected data ica, the fall of 1974 was exceptional for the which show the unusual nature of the 1974 migration. early migration pattern and for the arrival of For comparison I summarized relevant information for several uncommon and previously unre- other years as given by my notes and the literature. My field notes extend from 1966, my netting records from ported species.
    [Show full text]
  • Orleans Parish Hazard Mitigation Plan
    Hazard Mitigation Plan City of New Orleans Office of Homeland Security and Emergency Preparedness January 7, 2021 1300 Perdido Street, Suite 9W03 (504) 658-8740 ready.nola.gov/hazard-mitigation DRAFT – January 7, 2020 1 Table of Contents Section 1: Introduction ................................................................................................................... 9 1.1 New Orleans Community Profile ...................................................................................................... 11 1.1.1 Location ..................................................................................................................................... 11 1.1.2 History of Orleans Parish ........................................................................................................... 12 1.1.3 Climate ....................................................................................................................................... 14 1.1.4 Transportation ............................................................................................................................ 15 1.1.5 Community Assets ..................................................................................................................... 17 1.1.6 Land Use and Zoning ................................................................................................................. 18 1.1.7 Population .................................................................................................................................. 24 1.1.8
    [Show full text]
  • Plant Communities of Selected Dunes and Sandy Areas of Florida - As Laboratories for High School Biology
    PLANT COMMUNITIES OF SELECTED DUNES AND SANDY AREAS OF FLORIDA - AS LABORATORIES FOR HIGH SCHOOL BIOLOGY By WILLIAM YANCEY BENNETT A DISSERTATION PRESENTED TO THE GRADUATE COUNCIL OF THE UNIVERSITY OF FLORIDA IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF EDUCATION UNIVERSITY OF FLORIDA June, 1961 ACKNOWLEDGMENTS The writer wishes to thank Prof. Erdman West for valuable assistance in plant identification. Sincere ap- preciation is due Dr. N. E. Bingham, chairman of the super- visory committee, for his direction and advice during the preparation of this work. Gratitude is extended to Dr. E. 3. Ford, of the supervisory committee, for his advice on special botanical problems and for his criticism of the manuscript* The author is indebted to other members of the supervisory committee, Drs. Douglas E. 3cates, Clara M. Olson and Robert D. Powell for their constructive criticism of the manuscript. Especial gratitude is expressed for the late Dr. Leon N. Henderson, whose interest and encouragement were so val- uable to the writer. ii TABLE OF CONTENTS Page ACKNOWLEDGMENTS ii LIST OF TABLES v LIST OF ILLUSTRATIONS . vi Chapter I. INTRODUCTION 1 t T Statement of the Problem Limitations and Definition of Terms Selection of Areas Plan of Dissertation II. ORIGIN OF FLORIDA SANDS . 9 Geological History Soil Types III. FINDINGS . « 25 Nature of a Plant Community Specific Plant Communities Samples of Vegetational Communities Summary IV. PLANT COMMUNITIES USED AS LABORATORIES 103 Introduction Facts to be Investigated in All Plant Communities Some Observable Factors Found in Plant Communities Equipment to be Included in Preparations for Activities Planning a Field Trip Summary iii Page Chapter 7.
    [Show full text]
  • FSU ETD Template
    Florida State University Libraries Electronic Theses, Treatises and Dissertations The Graduate School 2017 Crawl Out through the Fallout?: Civil Defense, the Cold War, and American Memory Matthew Byrne Storey Follow this and additional works at the DigiNole: FSU's Digital Repository. For more information, please contact [email protected] FLORIDA STATE UNIVERSITY COLLEGE OF ARTS AND SCIENCES “CRAWL OUT THROUGH THE FALLOUT?” CIVIL DEFENSE, THE COLD WAR, AND AMERICAN MEMORY By MATTHEW BYRNE STOREY A Thesis submitted to the Department of History in partial fulfillment of the requirements for the degree of Master of Arts 2017 Matthew Byrne Storey defended this thesis on March 24, 2017 The members of the supervisory committee were: Jennifer Koslow Professor Directing Thesis Michael Creswell Committee Member Jonathan Grant Committee Member The Graduate School has verified and approved the above-named committee members, and certifies that the thesis has been approved in accordance with university requirements. ii For my parents iii TABLE OF CONTENTS List of Figures ............................................................................................................................. v Abstract ..................................................................................................................................... vi 1. INTRODUCTION .................................................................................................................. 1 2. THE OFFICIAL NARRATIVE OF CIVIL DEFENSE ........................................................
    [Show full text]
  • Hurricane Info You Can Use- 2009
    Since 1953, Atlantic tropical storms have been named from lists originated by the National Hurricane Center. They are now maintained and updated by an international committee of the World Meteorological Organization. The original name lists featured only women's names. In 1979, men's names were introduced and they alternate with the women's names. Six lists are used in rotation. Thus, the 2005 list will be used again in 2011. For more information about the history of naming hurricanes, log onto www.nhc.noaa.gov. The only time that there is a change in the list is if a storm is so deadly or costly that the future use of its name on a different storm would be inappropriate for reasons of sensitivity. If that occurs, then at an annual meeting by the WMO committee (called primarily to discuss many other issues) the name is stricken from the list and another name is selected to replace it. 2009 Names List Ana Bill Claudette Danny Erika Fred Grace Henri Ida Joaquin Kate Larry Mindy Nicholas Odette Peter Rose Sam Teresa Victor Wanda What is the National Hurricane Center? The National Hurricane Center (NHC) maintains a continuous watch on tropical cyclones over the Atlantic, Caribbean, Gulf of Mexico, and the Eastern Pacific from May 15th through November 30th. The Center prepares and distributes hurricane watches and warnings for the general public and also prepares and distributes marine and military advisories for other users. During the “off-season," NHC provides training for U.S. emergency managers and representatives from many other countries that are affected by tropical cyclones.
    [Show full text]
  • Nola.Com's Printer-Friendly
    Nola.com's Printer-Friendly Page http://www.nola.com/printer/printer.ssf?/base/news-5/12222336728873... EDITORIAL: Not just numbers Wednesday, September 24, 2008 Louisiana's case for federal help to restore our eroding coast is often made with compelling figures: The coast is home to 1.2 million people. It helps provide roughly one-third of the country's energy supply. Its bounty includes one-fourth of the country's seafood production. Advertisement That highlights coastal erosion's economic threat to our state and the nation. But losing the coast is also a human tragedy. Few people understand that better than Chief Albert Naquin of the Biloxi- Chitimacha-Choctaw Indians. For generations, Chief Naquin's family and other descendants of these American-Indian communities have lived on Isle de Jean Charles in southern Terrebonne Parish. So many hurricanes have hit the island that residents there considered flooding a regular occurrence -- much like people in other communities in the Mississippi River Delta endured seasonal river floods until the Army Corps of Engineers bounded the river with levees. Those levees, of course, stopped the Mississippi's sediment from replenishing wetlands that protected the coast -- including Isle de Jean Charles -- from storm surge. The island was left much more exposed to flooding. Now it's also eroding into the sea. Once four miles wide, its girth reaches only a quarter mile today. The island's levee, which is 6 to 7 feet high, is hardly enough to fend off the direct strike from storm surges. So when Hurricane Gustav flooded the island this month, Chief Naquin declared it was time for its 150 to 175 remaining residents to abandon the island and relocate farther inland -- as he and his wife did after Hurricane Carmen three decades ago.
    [Show full text]
  • Southern Climate Monitor in This Issue
    Southern Climate Monitor June 2019 | Volume 9, Issue 2 In This Issue: Page 2-5: The Biggest Rain Events Ever Page 6-7: NOAA’s Hurricane Season Outlook Page 8-9: Managing the Costs of Disasters Page 10-11: Evaluating Heat Related Illnesses Page 12-13: 20 Years Later: The May 3-4, 1999 Southern Plains Tornado Outbreak Page 14-16: Are there trends in the heaviest hourly periods with rainfall? Page 17: About SCIPP Team: Barry Keim Page 18: From Our Partners The Southern Climate Monitor is available at www.srcc.lsu.edu & www.southernclimate.org Feature The Biggest Rain Events Ever John Nielson-Gammon, Texas A&M University, Texas State Climatologist While Hurricane Harvey was intensifying in available to dispose of all the water, massive the Gulf of Mexico, it was pretty obvious that flooding resulted. somebody was going to get a ton of rain. As it turns out, the highest rainfall total credibly I wondered, how does Harvey stack up against measured by a rain gauge was 60.58” in the biggest rain events ever documented in the Nederland, in the southeast corner of Texas United States? And which events were they? (Blake and Zelinsky 2018). That’s five feet of Do they normally happen in the southern rain.* United States? Or were we just lucky? As Harvey was happening, I had a hunch that To figure out the total amount of rain in a it could break some multi-day rainfall records. given area, I needed what are called rainfall So I looked the records up.
    [Show full text]
  • 45Th Anniversary of Hurricane Beulah
    NWS Corpus Christi, TX Summer 2012 Edition 45th Anniversary of Hurricane Beulah Special points of John Metz — Warning Coordination Meteorologist interest: Severe Weather Season Beulah was the 2nd storm of the 2012 most active season in 1967 hurricane season in which there 25 years! were only 6 named storms. However Beulah left its mark on Texas history as All about the wildfire on the her slow storm motion produced record Padre Island National flooding and a prolific number of torna- Seashore does. Beulah was a long track storm, developing just east of the Leeward Is the Drought Improving? Islands in the Caribbean on Sept 5, 1967, intensifying rapidly into a hurricane the Find out how to become a Hurricane Beulah – September1967 next day. Beulah passed south of volunteer at the NWS WFO Hispaniola as a Category 4 hurricane with wind speeds of 150 mph. As she churned across Corpus Christi, TX the Caribbean, she weakened to a tropical storm while skirting south of Jamaica. But by the eleventh day she made her first direct impact, on the northern tip of the Yucatan Peninsula near Cozumel, as a Category 3 storm. She reemerged in the warm waters of the Gulf of Inside this issue: Mexico, becoming a powerful Category 5 storm, with sustained winds of 160 mph. Beulah finally moved ashore in Mexico, just south of Brownsville Texas on Sept 20, 1967. Maximum wind gusts were measured at 136 mph in Brownville producing a storm surge of Hurricane Beulah 1 18-20 feet north of where the center of the storm crossed the coast.
    [Show full text]
  • MASARYK UNIVERSITY BRNO Diploma Thesis
    MASARYK UNIVERSITY BRNO FACULTY OF EDUCATION Diploma thesis Brno 2018 Supervisor: Author: doc. Mgr. Martin Adam, Ph.D. Bc. Lukáš Opavský MASARYK UNIVERSITY BRNO FACULTY OF EDUCATION DEPARTMENT OF ENGLISH LANGUAGE AND LITERATURE Presentation Sentences in Wikipedia: FSP Analysis Diploma thesis Brno 2018 Supervisor: Author: doc. Mgr. Martin Adam, Ph.D. Bc. Lukáš Opavský Declaration I declare that I have worked on this thesis independently, using only the primary and secondary sources listed in the bibliography. I agree with the placing of this thesis in the library of the Faculty of Education at the Masaryk University and with the access for academic purposes. Brno, 30th March 2018 …………………………………………. Bc. Lukáš Opavský Acknowledgements I would like to thank my supervisor, doc. Mgr. Martin Adam, Ph.D. for his kind help and constant guidance throughout my work. Bc. Lukáš Opavský OPAVSKÝ, Lukáš. Presentation Sentences in Wikipedia: FSP Analysis; Diploma Thesis. Brno: Masaryk University, Faculty of Education, English Language and Literature Department, 2018. XX p. Supervisor: doc. Mgr. Martin Adam, Ph.D. Annotation The purpose of this thesis is an analysis of a corpus comprising of opening sentences of articles collected from the online encyclopaedia Wikipedia. Four different quality categories from Wikipedia were chosen, from the total amount of eight, to ensure gathering of a representative sample, for each category there are fifty sentences, the total amount of the sentences altogether is, therefore, two hundred. The sentences will be analysed according to the Firabsian theory of functional sentence perspective in order to discriminate differences both between the quality categories and also within the categories.
    [Show full text]
  • 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.
    [Show full text]