Hurricane Camille: August 1969
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TIROS V VIEWS FINAL STAGES in the LIFE of TYPHOON SARAH AUGUST 1962 CAPT.ROBERT W
MONTHLY M7EBTHER REVIEW 367 TIROS V VIEWS FINAL STAGES IN THE LIFE OF TYPHOON SARAH AUGUST 1962 CAPT.ROBERT w. FETT, AWS MEMBER National Weather Satellite Center, Washington D C [Manuscript Received April 18 1963, Revised May 28, 19631 ABSTRACT Four TIROS V mosaics showing typhoon Sarah on consecutive days during the period of its dccliiie are deecribcd. The initial development of what later became typhoon Vera is also shown. It is found that marked changes in storm intensity are rcflected in corresponding changes of appearance in the cloud patterns view-ed from the satellite. 1. INTRODUCTION read-out station shortly after the pictures were taken is also shown. Through cross reference from the niosaic to . The 3-week period froni the middle of August through the nephanalysis, locations of cloud I’eatures can con- the first week of September 1962, was one oE unusual veniently be determined. Photographic distortions of the activity for the western Pacific. No fewer than 6 ty- pictures and niosaic presentation are also rectified on the phoons developed, ran their devastating courses, and nephanalysis. The pictures begin in the Southern Hem- finally dissipated in mid-latitudes during this short spa11 isphere and extend northeastward past the Philippines, of time. over Formosa, Korea, and Japan, to the southern tip ol The TIROS V meteorological satellite was in position the Kamchatka Peninsula. The predominant cloud to view niany of these developments during various stages reatures in the southern portion of the mosaic consist of growth from formation to final decay. This provided mainly of clusters of cumulonimbus with anvil tops an unparalleled opportunity to obtain a visual record sheared toward the west-soutliwest by strong upper-level for extensive research into inany of the still unresolved east-northeasterly winds. -
Azimuthally-Averaged Structure of Hurricane Edouard (2014) Just After Peak Intensity
Quarterly Journal of the Royal Meteorological Society Q. J. R. Meteorol. Soc. 144: 1–5 (2018) Azimuthally-averaged structure of Hurricane Edouard (2014) just after peak intensity Roger K. Smitha∗, Michael T. Montgomeryb and Scott Braunc a Meteorological Institute, Ludwig Maximilians University of Munich, Munich, Germany b Dept. of Meteorology, Naval Postgraduate School, Monterey, CA, USA c Laboratory for Mesoscale Atmospheric Processes, NASA Goddard Space Flight Center, Greenbelt, Maryland, MD, USA ∗Correspondence to: Prof. Roger K. Smith, Meteorological Institute, Ludwig-Maximilians University of Munich, Theresienstr. 37, 80333 Munich, Germany. E-mail: [email protected] Analyses of dropsonde data collected in Hurricane Edouard (2014) just after its mature stage are presented. These data, have unprecedentedly high spatial resolution, based on 87 dropsondes released by the unmanned NASA Global Hawk from an altitude of 18 km during the Hurricane and Severe Storm Sentinel (HS3) field campaign. Attempts are made to relate the analyses of the data to theories of tropical cyclone structure and behaviour. The tangential wind and thermal fields show the classical structure of a warm core vortex, in this case with a secondary eyewall feature. The equivalent potential temperature (θe) field shows also the expected structure with a mid-tropospheric minimum at outer radii and contours of θe flaring upwards and outwards at inner radii and, with some imagination, roughly congruent to the surfaces of absolute angular momentum. However, details of the analysed radial velocity field are somewhat sensitive to the way in which the sonde data are partitioned to produce an azimuthal average. This sensitivity is compounded by an apparent limitation of the assumed steadiness of the storm over the period of data collection. -
Florida Hurricanes and Tropical Storms
FLORIDA HURRICANES AND TROPICAL STORMS 1871-1995: An Historical Survey Fred Doehring, Iver W. Duedall, and John M. Williams '+wcCopy~~ I~BN 0-912747-08-0 Florida SeaGrant College is supported by award of the Office of Sea Grant, NationalOceanic and Atmospheric Administration, U.S. Department of Commerce,grant number NA 36RG-0070, under provisions of the NationalSea Grant College and Programs Act of 1966. This information is published by the Sea Grant Extension Program which functionsas a coinponentof the Florida Cooperative Extension Service, John T. Woeste, Dean, in conducting Cooperative Extensionwork in Agriculture, Home Economics, and Marine Sciences,State of Florida, U.S. Departmentof Agriculture, U.S. Departmentof Commerce, and Boards of County Commissioners, cooperating.Printed and distributed in furtherance af the Actsof Congressof May 8 andJune 14, 1914.The Florida Sea Grant Collegeis an Equal Opportunity-AffirmativeAction employer authorizedto provide research, educational information and other servicesonly to individuals and institutions that function without regardto race,color, sex, age,handicap or nationalorigin. Coverphoto: Hank Brandli & Rob Downey LOANCOPY ONLY Florida Hurricanes and Tropical Storms 1871-1995: An Historical survey Fred Doehring, Iver W. Duedall, and John M. Williams Division of Marine and Environmental Systems, Florida Institute of Technology Melbourne, FL 32901 Technical Paper - 71 June 1994 $5.00 Copies may be obtained from: Florida Sea Grant College Program University of Florida Building 803 P.O. Box 110409 Gainesville, FL 32611-0409 904-392-2801 II Our friend andcolleague, Fred Doehringpictured below, died on January 5, 1993, before this manuscript was completed. Until his death, Fred had spent the last 18 months painstakingly researchingdata for this book. -
An Analysis of Hurricane Cleo (1958) Based on Data from Research Reconnaissance Aircraft
694 MONTHLY WEATHER REVIEW OCTOBER-DECEMBER1963 AN ANALYSIS OF HURRICANE CLEO (1958) BASED ON DATA FROM RESEARCH RECONNAISSANCE AIRCRAFT N. E. LA SEUR Florida State University, Tallahassee, Fla. and H. F. HAWKINS U.S.Weather Bureau, Miami, Fla. [Manuscript received July 5, 1963 revised September 6, 19631 ABSTRACT The structure of hurricane Cleo (1958) is presented, based 011 observations of wind, temperature, pressure, humidity, clouds, and precipitation obtained from three research reconnaissance aircraft of the Kational Hurricane Research Project. Insofar as possible, the data are analyzed in terms of departures from the mean tropical atmos- phere; and the physical processes which produce these departures are discussed. The central eye region of the hurri- cane emerges as the seat of the most important contributions to the structure of the entire storm, a result anticipated by Wexler from what may be termed the first research reconnaissance of a hurricane in 1944. 1. INTRODUCTION Simpson, who participated as a supplementary observer aboard operational military reconnaissance planes, pro- On September 14, 1944, a little more than one year after duced many valuable results [2]. However, the limited the first aircraft Aight into a hurricane, Dr. Harry Wexler obserrational capabilities, especially of wind, plus the (then a Major in the Army Air Corps) participated in what necessity of manual recording of data were severe handi- may be called the first research reconnaissance flight into a caps in such flights. The first aircraft equipped -
National Hurricane Research Project
NATIONAL HURRICANE RESEARCH PROJECT •'•'•'• / •ST" jj&ifs v •'•'T' 0 W- L7 REPORT NO. 67 On the Thermal Structure of Developing Tropical Cyclones F=* ^ \ S>1 lv'r*;>k . SPritiJ LABORATORY i U. S. DEPARTMENT OF COMMERCE Luther H. Hodges, Secretary WEATHER BUREAU Robert M. White, Chief NATIONAL HURRICANE RESEARCH PROJECT REPORT NO. 67 On the Thermal Structure of Developing Tropical Cyclones DATE DUE V, Jr. -Project, Miami, Fla. QEMCO 38-297 Washington, D. C. January 1964 UlfiMDl DbDlH4fi I NATIONAL HURRICANE RESEARCH PROJECT REPORTS this seSeTto'f^ the hurricane problem are preprinted in paperthis limitedin the seriesreproductionshouldandideS^Tdistributionasa^XSTrSJo!!?in this fom %?ZTC°nStltUte+T2S V*f0rnalWOrkers•*««««•»* otherpublication,interestedreferenceunits. toAs a Bo. 1. Objectives and basic design of the NHRP. March 1956. So. 2. Numerical weather prediction of hurricane motion. July 1956 Supplement: J™ «£jj ^prognostic 500-mb. maps made for numerical weather prediction of hurricane Ho. 3. Rainfall associated with hurricanes. July 1956 Jo. k. Some problems involved in the study of storm surges. December 1956. «o. 5. ^^-teorological factors pertinent to reduction of loss or life and property in hurricane situations. Mo. 6. Amean atmosphere for the West Indies area. May 1957 foil:, jtriTtsiwa^:^^^^^tr'i^zr1^"^^^^^0-and the atmosphere in relationVi^lSS^Sl^'j^^. "* QXtbB^ °f eBer6y between **«***•8ea «o. 9. Seasonal^variations in the fluency of Horth Atlantic tropical cyclones related to the general circulation. Ho. 10. Estimating central pressure of tropical cyclones from aircraft data. August 1957. Ho. 11. Instrumentation of National Hurricane Research Project al^Sft™Amaurt^s? Ho. 12. Studies of hurricane spiral bands as observed on radar. -
Florida Hurricanes and Tropical Storms, 1871-1993: an Historical Survey, the Only Books Or Reports Exclu- Sively on Florida Hurricanes Were R.W
3. 2b -.I 3 Contents List of Tables, Figures, and Plates, ix Foreword, xi Preface, xiii Chapter 1. Introduction, 1 Chapter 2. Historical Discussion of Florida Hurricanes, 5 1871-1900, 6 1901-1930, 9 1931-1960, 16 1961-1990, 24 Chapter 3. Four Years and Billions of Dollars Later, 36 1991, 36 1992, 37 1993, 42 1994, 43 Chapter 4. Allison to Roxanne, 47 1995, 47 Chapter 5. Hurricane Season of 1996, 54 Appendix 1. Hurricane Preparedness, 56 Appendix 2. Glossary, 61 References, 63 Tables and Figures, 67 Plates, 129 Index of Named Hurricanes, 143 Subject Index, 144 About the Authors, 147 Tables, Figures, and Plates Tables, 67 1. Saffir/Simpson Scale, 67 2. Hurricane Classification Prior to 1972, 68 3. Number of Hurricanes, Tropical Storms, and Combined Total Storms by 10-Year Increments, 69 4. Florida Hurricanes, 1871-1996, 70 Figures, 84 l A-I. Great Miami Hurricane 2A-B. Great Lake Okeechobee Hurricane 3A-C.Great Labor Day Hurricane 4A-C. Hurricane Donna 5. Hurricane Cleo 6A-B. Hurricane Betsy 7A-C. Hurricane David 8. Hurricane Elena 9A-C. Hurricane Juan IOA-B. Hurricane Kate 1 l A-J. Hurricane Andrew 12A-C. Hurricane Albert0 13. Hurricane Beryl 14A-D. Hurricane Gordon 15A-C. Hurricane Allison 16A-F. Hurricane Erin 17A-B. Hurricane Jerry 18A-G. Hurricane Opal I9A. 1995 Hurricane Season 19B. Five 1995 Storms 20. Hurricane Josephine , Plates, X29 1. 1871-1880 2. 1881-1890 Foreword 3. 1891-1900 4. 1901-1910 5. 1911-1920 6. 1921-1930 7. 1931-1940 These days, nothing can escape the watchful, high-tech eyes of the National 8. -
The Hurricane Season of 1966 Arnold L
March 1967 Arnold L. Sugg 131 THE HURRICANE SEASON OF 1966 ARNOLD L. SUGG* National Hurricane Center, US. Weather Bureau Office, Miami, Florida I 1. GENERAL SUMMARY ward in the United States in September (Green [4]), but The 1966 hurricane season began early and ended late. While the number of storms was only slightly above normal, hurricane days totalled 50, well above the yearly average of 33 and the second highest of record tabulated since 1954 (table 1). Hurricane days for June and November exceeded the previous 12-y ear totals. Except for a late May-early June hurricane in 1825, Alma, the first tropical cyclone of the 1966 season, made landfall in the United States earlier in the season than any other hurricane of record. Faith and Inez were tracked over very long distances (fig. 1). The 65 advisories on Inez were the most ever issued for a hurricane and the total of 151 bulletins and advisories also exceeded previous advices on a hurricane. The unusual path of Inez made her the first single storm of record to affect the West Indies, the Bahamas, Florida, and Mexico. She was also the first of record, so late in the season, to cross the entire Gulf of Mexico without recurvature. The season continued active through July. Since 1871, there have been only thee other years when the fifth tropica.1 cyclone developed as early as July. These were 1933 (fifth tropical cyclone on July 25, total of 21 cyclones), 1936 (July 27, 16 cyclones), and 1959 (July 22, 11 cyclones). According to Wagner [14], the June 700-mb. -
Estimation of Probable Maximum Precipitation in Korea Using a Regional Climate Model
water Article Estimation of Probable Maximum Precipitation in Korea using a Regional Climate Model Jeonghoon Lee 1, Jeonghyeon Choi 1, Okjeong Lee 1, Jaeyoung Yoon 2 and Sangdan Kim 3,* 1 Environmental System Science (Major of Environmental Engineering), Pukyong National University, Busan 48513, Korea; [email protected] (J.L.); [email protected] (J.C.); [email protected] (O.L.) 2 Department of Environmental Engineering, Korea University, Sejong 30019, Korea; [email protected] 3 Department of Environmental Engineering, Pukyong National University, Busan 48513, Korea * Correspondence: [email protected]; Tel.: +82-051-629-6529 Academic Editor: Athanasios Loukas Received: 19 January 2017; Accepted: 24 March 2017; Published: 30 March 2017 Abstract: Extreme precipitation events have been extensively applied to the design of social infra structures. Thus, a method to more scientifically estimate the extreme event is required. This paper suggests a method to estimate the extreme precipitation in Korea using a regional climate model. First, several historical extreme events are identified and the most extreme event of Typhoon Rusa (2002) is selected. Second, the selected event is reconstructed through the Weather Research and Forecasting (WRF) model, one of the Regional Climate Models (RCMs). Third, the reconstructed event is maximized by adjusting initial and boundary conditions. Finally, the Probable Maximum Precipitation (PMP) is obtained. The WRF could successfully simulate the observed precipitation in terms of spatial and temporal distribution (R2 = 0.81). The combination of the WRF Single-Moment (WSM 6-class graupel scheme (of microphysics), the Betts-Miller-Janjic scheme (of cumulus parameterization) and the Mellor-Yamada-Janjic Turbulent Kinetic Energy (TKE) scheme (of planetary boundary layer) was determined to be the best combination to reconstruct Typhoon Rusa. -
Florida Newspaper History Chronology, 1783-2001
University of South Florida Digital Commons @ University of South Florida USF St. Petersburg campus Faculty Publications USF Faculty Publications 2019 Florida Newspaper History Chronology, 1783-2001 David Shedden [email protected] Follow this and additional works at: https://digitalcommons.usf.edu/fac_publications Part of the Journalism Studies Commons, Mass Communication Commons, and the United States History Commons Recommended Citation Shedden, D. (2019). Florida Newspaper History Chronology, 1783-2001. Digital Commons @ University of South Florida. This Other is brought to you for free and open access by the USF Faculty Publications at Digital Commons @ University of South Florida. It has been accepted for inclusion in USF St. Petersburg campus Faculty Publications by an authorized administrator of Digital Commons @ University of South Florida. For more information, please contact [email protected]. __________________________________________ Florida Newspaper History Chronology 1783-2001 The East-Florida Gazette, Courtesy Florida Memory Program By David Shedden Updated September 17, 2019 __________________________________________ CONTENTS • INTRODUCTION • CHRONOLOGY (1783-2001) • APPENDIXES Daily Newspapers -- General Distribution Weekly Newspapers and other Non-Dailies -- General Distribution African-American Newspapers College Newspapers Pulitzer Prize Winners -- Florida Newspapers Related Resources • BIBLIOGRAPHY 2 INTRODUCTION Our chronology looks at the history of Florida newspapers. It begins in 1783 during the last days of British rule and ends with the first generation of news websites. Old yellowed newspapers, rolls of microfilm, and archived web pages not only preserve stories about the history of Florida and the world, but they also give us insight into the people who have worked for the state’s newspapers. This chronology only scratches the surface of a very long and complex story, but hopefully it will serve as a useful reference tool for researchers and journalism historians. -
Herter Outlines Plan to Ease World Strife
« i"'' WEDNESDAY, SEPTEMBER 1*, 19BI tAGM TWENTY-ETGHT Hanrh^istpr lEnenittg 1|i?ralb Aveng* Daily N«t Pr«M Ron The Waalhar rw r Mm W s M i OWtod Peraeaat af 0. R. Waatbai •.ami lUy ttrfi. IMW msklflg 6 turn Into th# westbound ] I Mia* Busan King, daughter of MiH Judith Taitl, daughUr of Rockville Driver portion of the street. As her] Oeo) wtdeapread tro ti trndgM. Mr. and Mrs. James V. Tapi. Con the left lane, it^ L T. WOOD 00. Utr. and Mr*. Haiwey King, 218 ear moved Jnto 12,925 O m la 86a. P a ir cswitlaiM d aaal About Town HeniA- St . naa enrolled as a fresh- cord Rd , has returned to ,Mary-1 CUUIUITUcollided witlfrr.^.w -.a car.................. driven east ' ICE P U N T ' mount College, Tartytown, N Y . , i Injured in Crash •Uttber «f Mm AndH tamermw. Wgh aear aa. man ' at New Elngland College. thaTlane by Morgan F. Steele. 22, St BItMBLL OT. BorsMi pf OraolaMM Robert 2. HoUenbech, formerly Henniker, N. H Her sister. Miss to begin her. sophomore year. of 205 Porter St. Mancheater-r-A City of VUlago Chorm nf i3 Oreen Hill Rd., ha* Joined .Nancy King, has returned to Lea> ^ Rockville driver, John Martin. Damage was light, according t o , Cu beB-C.riukeiUBlockB the facuJtv of Ixw-ell TechnoloRi- ley College. Cambridge, Mass , as The first fall meeting of Cfiar-I 62, of Ellingtoir Av*„ was taken to police, and no one was hurl. Mr*.; cal Inatltiite. Lmvell. Maas., as an ter Oak lodges, B'nal B’rlth. -
An Evaluation of 700 Mb Aircraft Reconnaissance Data for Selected Northwest Pacific Tropical Cyclones
Calhoun: The NPS Institutional Archive Theses and Dissertations Thesis Collection 1983-09 An evaluation of 700 mb aircraft reconnaissance data for selected northwest Pacific tropical cyclones Dunnavan, George Milton Monterey, California. Naval Postgraduate School http://hdl.handle.net/10945/19786 ^'^ lA 93943 : NAVAL POSTGRADUATE SCHOOL Monterey, California THESIS AN EVALUATION OF 700 M3 AIR CRAFT RECONNAISSANCE DATA FOR SELECTED NORTHWEST PACIFIC TROPK:al CYCLONES by George Mi It on Dunnavan The sis Advisor R. L. Elsberr^y Approved for public release; distribution unlimited T21^53 SECURITY CLASSIFICATION Of THIS PACE (Whmn Dmta Entmrad) READ INSTRUCTIONS REPORT DOCUMENTATION PAGE BEFORE COMPLETING FORM 1. REPORT NUMBEM 2. GOVT ACCESSION NO 3. RECIPIENT'S CATALOG NUMBER 4. TITLE (and Subtilla) 5. TYPE OF REPORT & PERIOD COVERED An Evaluation of 700 mb Aircraft Master's Thesis; Reconnaissance Data for Selected SeDtember 1983 Northwest Pacific Tropical Cyclones 6. PERFORMING ORG. REPORT NUMBER 7. AUTHOMr«> 8. CONTRACT OR GRANT NUMBERr»J Georse Milton Dunnavan I. ^eHFORWINO OROANIZATION NAME ANO AOORESS 10. PROGRAM ELEMENT. PROJECT. TASK AREA i WORK UNIT NUMBERS Naval Postgraduate School Monterey, California 939U3 II. CONTROLLINO OFFICE NAME ANO AOORESS 12. REPORT DATE Naval Postgraduate School September 1983 Monterey, California 939^-3 13. NUMBER OF PAGES 92 14. MONITORING AGENCY NAME A ADOHESSfll dUturant tnm Controttlna Otilcm) 15. SECURITY CLASS, (ol this report) UNCLASSIFIED 15«. DECLASSIFICATION/ DOWNGRADING SCHEDULE l«. OISTRISUTION STATEMENT (et ihia Kap»ri) Approved for public release; distribution unlimited 17. OISTRIBUTION STATEMENT (ot tha abatraet antarad In Block 30, It dlHaranl Irom Raport) IS. SUPPLEMENTARY NOTES It. KEY WOROS (Canllnua on rararaa alda II naeaaaaiy i*d Idanllty by black rtumbar) Tropical cyclones Tropical cyclone intensity Typhoons Equivalant potential temperature Hurricanes Moist static energy Aircraft reconnaissance 20. -
WAKE ISLAND HALS UM-1 (Wake Island National Historic Landmark) HALS UM-1 (Peale Island) (Wilkes Island) (Wake Atoll) Wake Island US Minor Islands
WAKE ISLAND HALS UM-1 (Wake Island National Historic Landmark) HALS UM-1 (Peale Island) (Wilkes Island) (Wake Atoll) Wake Island US Minor Islands PHOTOGRAPHS WRITTEN HISTORICAL AND DESCRIPTIVE DATA FIELD RECORDS HISTORIC AMERICAN LANDSCAPES SURVEY National Park Service U.S. Department of the Interior 1849 C Street NW Washington, DC 20240-0001 HISTORIC AMERICAN LANDSCAPES SURVEY WAKE ISLAND (Wake Island National Historic Landmark) HALS No. UM-1 Location: Wake Atoll is a small tropical coral atoll in the Pacific Ocean consisting of three islands (Peale, Wake, and Wilkes) enclosing the shallow, central lagoon and surrounded by a narrow fringing reef. From reef to reef, the atoll is approximately 5 miles long and 2.5 miles wide. At 19 degrees 17 minutes north latitude and 166 degrees 3 8 minutes east longitude, the atoll lies just west of the International Date Line. Wake Atoll is 2,458 miles west ofHawai'i, 1,591 miles east of Guam, and 691 miles north ofKwajalein in the Marshall Islands (Aaron 2008:1-1). (Refer to Figure 1). Present Owner: Wake Island is an unorganized, unincorporated territory (possession) of the United States, part of the United States Minor Outlying Islands, administered by the Office of Insular Affairs, U.S. Department of the Interior (Aaron 2008b and Aaron 2008: 1-1 ). Effective October 1, 2010, 611 th Air Force in Alaska assumed management responsibility for the atoll. Previously, this responsibility was under 15th Air Wing (AW) of the U.S. Air Force (USAF) at Hickam AFB in Honolulu. Present Occupant and Use: Access to the island is managed by the U.S.