Mercury-Atlas 8, Spacecraft 16)

Total Page:16

File Type:pdf, Size:1020Kb

Mercury-Atlas 8, Spacecraft 16) NASA TECHNICAL NOTE NASA TNc D-4807 C,r AFWL KI RTLAMD z c 4 m 4 z FIRST U.S. MANNED SIX-PASS ORBITAL MISSION (MERCURY-ATLAS 8, SPACECRAFT 16) DESCRIPTION AND PERFORMANCE ANALYSIS Edited by John H. Boyuton i , . I 1,. I\, I ; ,.\ il'.i , _ . ..r .. , ,... I. .. /. Muizned Spucecmft Center '.. ,' I ' .' ..i .A..e; t-. , 1 . ., ,. * 1.' , , , .. .,. ,-,- Houston, Texas ,- -. .'.:)',.,:..'!. -c ;:- i., ..~ ,, ,-- ,.$ NATIONAL AERONAUTICS AND SPACE ADMINISTRATION WASHINGTON, D. C. SEPTEMBER 1968 /I I II I.IIIIIIIIIII~1111111 11111 11111111111111 I I .I TECH LIBRARY KAFB, NM Illllll Ill11 lllll Ill11 lllll1lll1 Ill11 1111 Ill /- FIRST U.S. MANNED SIX-PASS ORBITAL MISSION J (MERCURY-ATLAS 8, SPACECRAFT 16) DESCRIPTION AND PERFORMANCE ANALYSIS "--* k---. -Ed- John HI Boynton , 9- Manned Spacecraft Center Houston, Texas J NATIONAL AERONAUTICS AND SPACE ADMCmSJ-8-kFtON For sale by the Clearinghouse for Federal Scientific and Technical Information Springfield, Virginia 22151 - CFSTI price $3.00 ABSTRACT The results and analyses of the third U.S. manned orbital mission are presented. The mission was accomplished October 3, 1962, as a phase of Project Mercury. Spacecraft and launch-vehicle descriptions, mission operations, and postflight analyses are included. Particular treatment is given to the investigations of spacecraft systems performance and aeromedical analyses of the pilot. ii FOREWORD The first U. S. manned six-pass orbital mission was an extension of the two pre- vious manned three-pass orbital missions and added significantly to the knowledge gained in those two limited-duration missions. An overall analysis of the mission performance is presented, and only the minimum necessary supporting data are included. General acknowledgment is made of the extensive effort on the part of the entire Mercury team. The team consisted of many organizations external to the NASA Manned Spacecraft Center and included the Department of Defense, the spacecraft prime contractor and subcontractors, the NASA Goddard Space Flight Center for the Mercury Worldwide Network, the launch-vehicle prime contractor and subcontractors, and the many organizations and Government agencies which directly or indirectly made the success of the mission possible. This report represents the contributions of an assigned flight evaluation team which was comprised of systems specialists and operations personnel from throughout the NASA Manned Spacecraft Center, without whose analytical and documentary efforts a report of this technical completeness would not be possible. The Mercury-Atlas 8 (MA-8) report is being published at this time to complete the Mercury technical documentation series and provide a source of historical data in much greater technical detail than that previously available. Further, to preserve a public record of the state of knowledge at the time of the mission, discussions and engineering conclusions remain essentially as they were written at the end of the MA-8 postflight data evaluation, despite any results from subsequent flight programs. iii CONTENTS Section Page SUMMARY ..................................... 1 INTRODUCTION .................................. 3 SPACE-VEHICLE DESCRIPTION ......................... 7 ~ ~~ ~~ ~ ~ ~ __ SPACECRAFT DESCRIPTION ........................ 7 Electrical and Sequential ........................ 7 Environmental Control System ..................... 9 Automatic Stabilization and Control System ............... 9 Reaction Control System ......................... 10 Instrumentation System ......................... 10 Communications System ......................... 11 Mechanical and Pyrotechnic Systems .................. 11 Heat Protection System ......................... 12 Personal Equipment ........................... 12 LAUNCH-VEHICLE DESCRIPTION ..................... 12 MISSION OPERATIONS .............................. 21 PRELAUNCH OPERATIONS ......................... 21 Pilot Training .............................. 21 Spacecraft Prelaunch Preparation .................... 23 Spacecraft History ............................ 24 Launch-Vehicle Preparation ...................... 24 Flight-Safety Reviews .......................... 24 LAUNCH OPERATIONS ............................ 25 Launch Procedure ............................ 25 V . Section Page Weather Conditions ............................ 26 Photographic Coverage .......................... 27 FLIGHT-CONTROL OPERATIONS ...................... 29 Prelaunch Period ............................. 29 Launch Phase ............................... 30 Orbital Phase ............................... 30 Retrofire and Reentry Phases .......... I ........... 32 RECOVERY OPERATIONS .......................... 32 Recovery Plans .............................. 32 Recovery Procedure ........................... 33 Recovery Aids .............................. 35 MISSION PERFORMANCE 53 ~~ ___.... ~ ............................. SPACECRAFT PERFORMANCE ....................... 53 Spacecraft Control System ........................ 53 Environmental Control System ...................... 56 Communications Systems ......................... 61 Electrical and Sequential Systems .................... 62 Instrumentation System .......................... 64 Heat Protection System .......................... 67 Mechanical and Pyrotechnic Systems .................. 69 Posfflight Inspection and Meteoroid Analysis .............. 70 Scientific Experiments .......................... 72 AEROMEDICAL ANALYSIS .......................... 78 Clinical Examinations .......................... 78 Physiological Observations ........................ 78 vi Section Page Special Studies ............................. 79 Biosensor System ........................... 79 Preflight Aeromedical History ..................... 80 Preflight Physical Ekamination .................... 81 Preflight Physiological Data ...................... 81 Flight Physiological Data ........................ 82 Special Studies ............................. 83 In-flight Aeromedical History ..................... 84 Postflight Physical Examination .................... 85 PILOT FLIGHT ACTIVITIES ........................ 88 Flight -Plan Description ........................ 88 Operational Equipment ......................... 88 Control Tasks ............................. 90 Systems Management and Operational Procedures .......... 93 Conclusions ............................... 95 PILOT'S FLIGHT REPORT ......................... 96 Countdown and Powered Flight ..................... 96 Orbital Flight .............................. 98 Retrosequence ............................. 101 Reentry ................................. 102 Landing and Recovery ......................... 103 LAUNCH-VEHICLE PERFORMANCE ................... 104 Airframe ................................ 104 Pneumatics ............................... 104 Abort Sensing and Implementation System ............... 104 vii Section Page Propellant Tanking and Utilization ................... 104 Flight-Control and Guidance Systems ................. 105 TRAJECTORY AND MISSION EVENTS ................... 107 Sequence of Flight Events ....................... 107 Flight Trajectory ............................ 107 MERCURY WORLDWIDE NETWORK PERFORMANCE .......... 108 General ................................. 108 Trajectory ............................... 109 CONCLUDING REMARKS 207 ~-............................ .................................. 209 viii TABLES Table Page I SPACECRAFT 16 WEIGHT AND BALANCE DATA . 14 II PILOT PREFLIGHT PREPARATION HISTORY . 36 III PILOT TRAINING SUMMARY IN THE MERCURY PROCEDURES TRAINER NO. 2 (CAPE CANAVERAL) . 37 IV MODIFICATIONS AND TESTS MADE TO SPACECRAFT 16 . 38 V ATLANTIC MISSILE RANGE OPTICAL LAUNCH COVERAGE . 40 VI REQUIREMENTS FOR AUTOMATIC MODE SWITCHING . 114 VIT ORBIT-MODE OPERATION . 114 VITI REACTION-CONTROL-SYSTEMFUELCONSUMPTION . 115 M LOW-RESIDUE DIET . 116 X AEROMEDICAL COUNTDQWN . 117 XI PHYSICAL EXAMINATIONS CONDUCTED FOR MA-8 OPERATIONS . 118 XII SUMMARY OF HEART RATE AND RESPIRATION DATA FROM PHYSIOLOGICAL MONITORING . 119 XI11 SUMMARY OF BLOOD-PRESSURE DATA . 120 XIV IN-FLIGHT BODY-TEMPERATURE VALUES . .. 121 XV POSTFLIGHT BLOOD-PRESSURE VALUES AND HEART RATES . 122 XVI CLINICAL EVALUATION . 123 XVII PERIPHERAL BLOOD VALUES . 124 XVIII URINESUMMARY.. 125 XM YAW MANEUVERS . 126 XX SUMMARY OF MAJOR FLIGHT ACTIVITIES . 127 XXI CONTROL-MODE UTILIZATION . 133 XXII SEQUENCE OF EVENTS . 134 ix Table Page XXUI COMPARISON OF PLANNED AND ACTUAL TRAJECTORY PARAMETERS ............................ 135 XXIV ORBITAL -INSERTION CONDITIONS AVAILABLE AT THE MERCURY CONTROL CENTER .................. 136 XXV RADARTRACKING ........................... 137 XXVI LANDING-POINT DATA ........................ 139 XXVII COMMAND HANDOVER SUMMARY .................. 140 XXVIII COMMAND FUNCTION SUMMARY ................... 143 XXIX AIR-TO-GROUND SIGNAL STRENGTH ................ 144 X FIGURES Figure Page 1 Pilot Schirra prior to insertion into spacecraft ............ 4 2 Pilot Schirra on the deck of the recovery aircraft carrier after the MA-8 mission ........................ 4 3 Ground track for the MA-8 orbital mission .............. 5 4 MA -8 lift -off configuration ....................... 15 5 MA-8 spacecraft and adapter prior to lift-off ............. 16 6 MA-8 spacecraft axis diagram ..................... 17 7 Booster-engine baffled injector .................... 18 8 Booster -engine hypergolic igniter (a) Igniter locations ........................... 19 (b) Igniter configuration .......................
Recommended publications
  • US> to The* Proper Zleoralaaxd-Ty Standards, Oven ^Liougli the B
    US> to the* proper ZLeorAlaAXd-ty standards, oven ^liougli the b«)Bt possible oopy was used for preparing trie master floho • PNRI-H:<HP>89OIO , t RADIOLOGICAL IMPACT ASSESSMENT OF THE HYDROLOSICAL CHARACTERISTICS OF THE AREA AROUND PRR-1 BY L. R. DE LA PAZ and M.V. B. PALATTAO 1989 Radiological Impact A«s»»»m«nt Philippine Nucl»«r R»»»arcb In»titut« TABLE OF CONTENTS PAGE INTRODUCTION 1 MATERIALS AND METHODS 1 Probable Maximum Precipitation (PMP) Typhoon Rainfall Model Statistical Estimates of PMP DISCUSSION OF RESULTS AND IMPACT ASSESSMENT 4 Ground Water Effects of Accidental Release of Radioactivity on Streams and the Ground Water Typhoon 5 Probable Maximum Precipitation 7 Probable Maximum Typhoon 7 Effect of PMP on PNRI Compound and its Drainage System 8 Evaluation of Reactor Bay Drainage System 8 REFERENCES 9 TABLES 1-5 10 FIGURES 1 - 9 22 RADIOLOGICAL IMPACT ASSESSMENT OF THE HYDROLOB1CAL CHARACTERISTICS OF THE AREA AROUND PRR-1 by L.R.de la Paz and M.V. Palattao Radiological Impact Assessment, PNRI ABSTRACT The hydrologic characteristics of the PRR-1 site are discussed. A study of the rainfall and typhoon behaviour in the areas around the site is made and the maximum precipitation characteristic is computed, with the Probable Maximum Precipitation calculated as 1383.9mm. The possible effects of accidental release of radioactivity on streams and waterways &re discussed. An evaluation of the PNRI drainage system is made. INTRODUCTION An important factor that must be considered in siting a research reactor is the hydrologic characteristics of the area. ANSI/ANS-15.7 (1977> <1> lists the following assessments that should be made: a.
    [Show full text]
  • An Investigation on the Variations of Sea Level Due to Meteorological Disturbances on the Coast of Japanese Islands(II)* Storms Surges on the Coast of the Japan Sea
    Journal of the Oceanographical Society of Japan Vol.24, No.4, pp. 178 to 190, August 1968 An Investigation on the Variations of Sea Level due to Meteorological Disturbances on the Coast of Japanese Islands(II)* Storms Surges on the Coast of the Japan Sea Ichiro ISOZAKI** Abstract: Storm surges on the eastern coastal line of the Japan Sea are studied. In contrast with the Pacific coast, extraordinary destructive surges hardly develop there because shallow waters such as bays or a continental shelf are comparatively small. Generally speaking, the effect of atmospheric pressure is roughly hydrostatic, and northeasterly winds cause the descent of sea level and southwesterly winds the ascent of it since the shore line runs from southwest to northeast. However, the fluctuations of sea level are different remarkably according to the course of atmospheric disturbances as well as topography of the coast. Case studies are made in detail for four storms which took different courses. In some cases we can clearly recognize a typical external surge which follows the storm considerably later at a very low speed of about 3•`4m/sec along the continental shelf from the southern entrance of the sea to Noto Peninsula. Its low speed is explained by assuming a shelf wave of Robinson's type. A curious fact that the sea level sinks before the arrival of the storm is also discussed. to northeast, we can find peculiar surges on the 1. Introduction San'in coast, western half of the region in ques- In Japan, severe storm surges occur mainly in tion, which progresses very slowly as a kind of bays on Pacific coast having their mouth south- free wave and arrives at the coast considerably ward, such as Tokyo Bay, Ise Bay and Osaka late after the storm passed away.
    [Show full text]
  • Escap-1953-Jn-Fcj-1010531X-15
    UNITED NATIONS ECONOMIC COMMISSION FOR ASIA AND THE FAR EAST FLOOD CONTROL JOURNAL ST/ECAFE/SER.C/15 June 1953 C 0 N T E N T S Page I. HAVOC WROUGHT BYFLOODS DURING 1952 3 A. The typhoons 3 B. The floods 8 II. PROJECTS OF THE REGION 16 A. Aerial surveys for Ceylon projects 18 B. The Pykara and Moyar Power Development Schemes, India 19 C. Tapi Valley Development, India 27 D, Aerial survey of Pakistan's natural resources 35 E. Two-Year Priority Programme, Pakistan 37 F. Philippines Hydro Programme 37 III. PROJECTS OUTSIDE THE REGION 44 A. The Snowy Mountains Project, Australia 44 B. Plans for Egypt's Nile re-vamp life-giving river 48 C. Californian Water Conservation Project 49 D. Earthfill dam in the tropics 50 E. Flood prevention in Hungary 51 /IV BENEFIT CENSUS - 2 - Page IV. BENEFIT CENSUS OF MULTIPLE-PURPOSE PROJECTS 52 V. ARTIFICIAL RAINFALL 57 a. Increasing water resources through modification of weather 57 B. Demands for Rain-making service seen increasing 60 C. Rain-making projects aid Washington foresters 60 VI. NEWS OF INTEREST 61 A. Conciliation of high versus low dam issue 61 B. Road sprinklers for canals and dikes 62 c. Grouting stops Arizona dam leakage 64 D. Engineers to direct flood operations from helicopters 64 VII. RIVER INTAKES - A REVIEW 65 - 3 - I. HAVOC WROUGHT BY FLOODS DURING 1952 A. the TYPHOONS Floods, occurring in countries of Asia and the Far East, are caused generally by heavy precipitation brought about by cyclones (typhoons) during the south-west monsoons period.
    [Show full text]
  • Significant Data on Major Disasters Worldwide, 1900-Present
    DISASTER HISTORY Signi ficant Data on Major Disasters Worldwide, 1900 - Present Prepared for the Office of U.S. Foreign Disaster Assistance Agency for International Developnent Washington, D.C. 20523 Labat-Anderson Incorporated Arlington, Virginia 22201 Under Contract AID/PDC-0000-C-00-8153 INTRODUCTION The OFDA Disaster History provides information on major disasters uhich have occurred around the world since 1900. Informtion is mare complete on events since 1964 - the year the Office of Fore8jn Disaster Assistance was created - and includes details on all disasters to nhich the Office responded with assistance. No records are kept on disasters uhich occurred within the United States and its territories.* All OFDA 'declared' disasters are included - i.e., all those in uhich the Chief of the U.S. Diplmtic Mission in an affected country determined that a disaster exfsted uhich warranted U.S. govermnt response. OFDA is charged with responsibility for coordinating all USG foreign disaster relief. Significant anon-declared' disasters are also included in the History based on the following criteria: o Earthquake and volcano disasters are included if tbe mmber of people killed is at least six, or the total nmber uilled and injured is 25 or more, or at least 1,000 people art affect&, or damage is $1 million or more. o mather disasters except draught (flood, storm, cyclone, typhoon, landslide, heat wave, cold wave, etc.) are included if the drof people killed and injured totals at least 50, or 1,000 or mre are homeless or affected, or damage Is at least S1 mi 1l ion. o Drought disasters are included if the nunber affected is substantial.
    [Show full text]
  • Statistical Considerations of Pressure Oscillations Occurring Near the Typhoon Center
    Statistical Considerations of Pressure Oscillations Occurring near the Typhoon Center by Sadao Yoshizumi Meteorological Research Institute, Tokyo (Received November 30, 1973) Abstract The aim of this paper is to make a statistical investigation of the pressure oscillations occurring near the center of a typhoon. An analysis of the barograms recorded on the Southwest Islands, Japan, during the decade from 1956 to 1965 shows that the occurrence frequency of the oscillations with the maximum double amplitude exceeding 3 mb is approximately 10%, and the frequency of those with the maximum amplitude of 2 mb or larger is about 30%. In order to get a clue as to the relationship of pressure oscillations to an elliptical eye, the reported frequency of an elliptical eye is also examined in this paper, based on the data obtained from flight observations. The reported frequency of an elliptical eye is estimated to be about 10%, and is considered to be fairly independent of the central pressure. Considerable agreement of the occurrence frequencies of both pressure oscillations and an elliptical eye suggests that pressure oscillations are closely related with an elliptical eye. From an examination of reports on an eye shape in cases where pressure oscillations were recorded, it is inferred that some of oscillations are associated with an elliptical eye. 1. Introduction It is well known that a barogram during the passage of a tropical cyclone often shows oscillatory pressure variations with various periods, superimposed on the V-shaped trace accompanied by the storm system. Included among the pressure oscillations are pressure ripples with the period of 10 min to one hour and gusty oscillations with the period of 1 sec to 5 min (FUJITA, 1952).
    [Show full text]
  • A Probabilistic Approach to Tropical Cyclone Conditions of Readiness (TCCOR)
    Calhoun: The NPS Institutional Archive DSpace Repository Theses and Dissertations 1. Thesis and Dissertation Collection, all items 2008 A probabilistic approach to Tropical Cyclone Conditions of Readiness (TCCOR) Wallace, Kenneth A. Monterey, California. Naval Postgraduate School http://hdl.handle.net/10945/3923 Downloaded from NPS Archive: Calhoun NAVAL POSTGRADUATE SCHOOL MONTEREY, CALIFORNIA THESIS A PROBABILISTIC APPROACH TO TROPICAL CYCLONE CONDITIONS OF READINESS (TCCOR) by Kenneth A. Wallace September 2008 Thesis Advisor: Patrick A. Harr Second Reader: Jim Hansen Approved for public release; distribution is unlimited THIS PAGE INTENTIONALLY LEFT BLANK REPORT DOCUMENTATION PAGE Form Approved OMB No. 0704-0188 Public reporting burden for this collection of information is estimated to average 1 hour per response, including the time for reviewing instruction, searching existing data sources, gathering and maintaining the data needed, and completing and reviewing the collection of information. Send comments regarding this burden estimate or any other aspect of this collection of information, including suggestions for reducing this burden, to Washington headquarters Services, Directorate for Information Operations and Reports, 1215 Jefferson Davis Highway, Suite 1204, Arlington, VA 22202-4302, and to the Office of Management and Budget, Paperwork Reduction Project (0704-0188) Washington DC 20503. 1. AGENCY USE ONLY (Leave blank) 2. REPORT DATE 3. REPORT TYPE AND DATES COVERED September 2008 Master’s Thesis 4. TITLE AND SUBTITLE: A Probabilistic Approach to Tropical Cyclone 5. FUNDING NUMBERS Conditions of Readiness (TCCOR) 6. AUTHOR(S) Kenneth A. Wallace 7. PERFORMING ORGANIZATION NAME(S) AND ADDRESS(ES) 8. PERFORMING ORGANIZATION Naval Postgraduate School REPORT NUMBER Monterey, CA 93943-5000 9.
    [Show full text]
  • 1 Deadliest American Disasters and Large Loss
    DEADLIEST AMERICAN DISASTERS AND LARGE LOSS-OF-LIFE EVENTS1 Homepage: http://www.usdeadlyevents.com/ A Catalog of, and Notes on, Natural and Man-Made Events Causing Ten or More Fatalities in America/The United States and its Territories Since 1492 CHRONOLOGY B. Wayne Blanchard, PhD Blue Ridge Summit, PA May 12, 2019 Copyright August 2017 Go to Homepage to access: Event Typology (e.g. aviation, epidemics, explosions, fires heat, mining, hurricanes, violence). Breakout of Events by States, District of Columbia and Territories. Rank-ordering within Types by State. Spreadsheet. Lines highlighted in Yellow indicate there is a narrative document with more information and sources in the Spreadsheet accessed by clicking on the URL at the end of the entry. 1. 1492-1800 -- North American Native American population decline, esp. disease--~2,800,000 2. 1527 -- Nov, Hurricane, Matagorda Bay, TX -- 200 3. 1538-1539, Unknown epidemic, “Cofitachequi”2 Natives, central SC -- Hundreds 4. 1539 --~Sep 16, Napituca Massacre, Hernando de Soto executes Timucuans, No. Cen. FL-30-200 5. 1540 -- Oct 18, Spanish (de Soto) battle/massacre, with Atahachi, Mabila, AL --2,500-6,000 6. 1541 -- ~Mar 10, Hernando de Soto forces and “Chicasa” battle and “slaughter,” MS3 -- >20? 7. 1541/42 Winter, Coronado’s Expeditionaries burn-at-the-stake Tiwa Natives, NM4 --40-50 1 We use the term “Large-Loss-of-Life Event to denote ten or more deaths. There are a number in instances where, for a variety of reasons, we enter an event with fewer than 10 fatalities. We do not, though, include these in tally.
    [Show full text]
  • Okinawa Typhoons, 1954 – 1956
    P2.45 OKINAWA TYPHOONS, 1954 – 1956 Fred S. and Thresa K. Hickernell* Phoenix, Arizona Abstract: Typhoons coming close to the island of Okinawa interrupted the otherwise idyllic summer season. I was stationed as a weather forecaster for a two year period at Kadena Base Weather Station as a part of my military obligation. This was my first introduction to single station analysis and forecasting typhoons. Okinawa is affected by an average of four to six named typhoons from May to October. That a typhoon will pass near Okinawa in July is listed as an almost sure thing by the weather center in Japan. The typhoons were usually tracked by reconnaissance aircraft out of Guam, the Philippines, and Japan. If a typhoon was close to Okinawa, it could be tracked on radar. This paper is historical in nature, reporting the weather and typhoon activity on Okinawa some fifty-five years ago. This was before satellite observations became available. 1. Introduction My introduction to typhoons was the day after I arrived at the weather station, Kadena AFB on Okinawa th Fig. 1. Track of Typhoons during the 1954 season with on September 20 1954, and on the following day went special emphasis on Typhoon Marie. to the radar site at the north end of the island. Our radar officer, a captain, invited me to have a look at Typhoon 2. Normal Weather Station Duties Marie which was swinging by just west of the island. Typhoon Marie had started south of the Ryukyus island Normal weather duties at the Kadena Base Weather chain and neither the Philippines nor Japan was alerted Station included, to observe weather in the local area, to track her by aircraft.
    [Show full text]
  • Benjamin O. Davis Jr. Collection, 1928-1990
    Benjamin O. Davis Jr. Collection, 1928-1990 Paul Silbermann 2003 National Air and Space Museum Archives 14390 Air & Space Museum Parkway Chantilly, VA 20151 [email protected] https://airandspace.si.edu/archives Table of Contents Collection Overview ........................................................................................................ 1 Administrative Information .............................................................................................. 1 Biographical / Historical.................................................................................................... 1 Scope and Contents........................................................................................................ 9 Arrangement................................................................................................................... 10 Names and Subjects .................................................................................................... 10 Container Listing ........................................................................................................... 12 Series 1: Education and Civilian Life, to June 1932.............................................. 12 Series 2: Military Career, June 1932 - January 1970............................................ 14 Series 3: Civilian Life, February 1970 - 1993........................................................ 41 Series 4: Autobiography, undated........................................................................ 101 Series : Oversize materials.................................................................................
    [Show full text]
  • Bomb Hanoi Storage Area
    Nastasio Says Jury Has Pesano Transcript SEE STORY .BELOW Weather HOME Mostly sunny and cold today, high la upper 40s. Fair continued THEDAEY DJPrTQTFV cold tonight. Low tonight, in low J0«. Fair and cold tomorrow, high FINAL around 50. Outlook Wednesday, fair and continued cold. v MONMOUTH COUNTY'S HOME NEWSPAPER FOR 89 YEARS DIAL 741-0010 VOL. 90, NO. 93 RED BANK, N. J., MONDAY, NOVEMBER 6, 1967 10c PER COPY PAGE ONE Target Taken of f Restricted List Bomb Hanoi Storage Area SAIGON (AP; "^Brother tar- and is North Vietnam's main ci- road and highway from Commu- one F1P5 had a brief clash with antiaircraft sites protecting while, South Vietnamese infan- ;et in North Vietnam came of( vilian air field. nist China to, Hanoi over which one of the Red jets, but the U.S. learea. trymen battled Met Cong troops :he Pentagon's out-of-bounds list Gia Lam is also the only MIGimiiitary supplies come for North Command said neither plane The spokesman said both the near Loc Ninht One American F105 was shot down during the today as U.S. Air Force fighter- airfield U.S. warplanes have not Vietnamese troops fighting as hit. )anal des Rapides and Doumer yet attacked and one of about South Vietnam. The area is be- A U.S. spokesman said Gia ridges had been knocked out in Phuc Yen" raid, but two propel- jombers attacked a sprawling five major targets still on the tween two key bridges,' the Ca- Thuong is considered one of irevious raids and there appar- ler-driven Al Skyraiders* drove unitary storage area on the out- Pentagon's restricted list.
    [Show full text]
  • A Chronology of Notable Weather Events by Douglas V. Hoyt
    A Chronology of Notable Weather Events by Douglas V. Hoyt Edition of 8/4/2011 243 A. D. An inundation of the sea in Lincolnshire laid under water many thousands of acres (Camden). 353 Flood in Cheshire in which 3000 people died along with thousands of cattle (Hayden). 402 Euxine Sea frozen over for 20 days (Hayden) 500 The Vandals from Poland held Western Africa, the Diocese of Africa, Visigoth (Western Goth) from Scandia held Spain, Ostrogoth (Eastern Goth) from Scandia held Italy, Germanic-Franks from Scandia held Gaul, Burgundians held Rhone river, and Celts, Germanic-Anglo-Saxon held the diocese of England. The massive migration of the Mongols, the Huns, Goth, Slav-Bulgars, and Avars westward is because of adverse weather conditions driving them from their lands . The Germanic-Danes inhabited the Danish Islands, Schonen, and later Jutland. St. Brendan (521-527) in his voyage to the northwest suggests the Celts of Ireland discovered America about this time. The Polynesian reached Hawaii and established agricultural settlements. These people had traveled 2500 miles from Island to Island. It is inconceivable that these peoples didn't reach America in the past 500 years. The Polynesians colonized Hawaii, Easter Island, and Madagascar by 500 A.D. 507 Men from Tsinngan, China report being blown across the Great Sea East to a people who speak a strange language. 508 In England, the rivers were frozen for more than two months (including Thames?). Possible severe winter. Rivers frozen for two months. Years also quoted as 507 or 509. 514 St. Brendan (484-577) of Ireland explored the area discovering the Hebrides, Orkney, Faeroe Islands and Iceland, starting about this time.
    [Show full text]
  • Periodic Variations of Pressure, Wind and Rainfall Observed at Miyakojima During the Second Miyakojima Typhoon
    December 1973 Yasushi Mitsuta and Sadao Yoshizumi 475 Periodic Variations of Pressure, Wind and Rainfall Observed at Miyakojima during the Second Miyakojima Typhoon By Yasushi Mitsuta Disaster Prevention Research Institute, Kyoto University, Kyoto and Sadao Yoshizumi Meteorological Research Institute, Tokyo (Manuscript received 17 July 1973) Abstract During the passage of the Second Miyakojima Typhoon the barograph at Miyakojima recorded a pronounced pressure oscillation with the period of about 50 min on September 5, 1966. The recorded oscillation extended over half a day and had a maximum double amplitude exceeding 10mb. Simultaneously, wind and rainfall intensity showed periodic variations with the approximately same period, too. It is shown that the periodic variations of these elements were associated with the counter- clockwise rotation of an elliptical eye revealed by radar observation. which had a period of 20 to 40min and 1. Introduction maximum double amplitude of about 9mb. During the passage of a tropical cyclone a Recently the most spectacular one of pressure barograph trace usually describes a smooth V- oscillations that have ever been known was shaped variation on the time scale of about half recorded at Miyakojima on September 5, 1966 a day. Pressure variations with various shorter during the passage of the Second Miyakojima periods are frequently found out to be superim- Typhoon (Typhoon 6618, Cora) (Mitsuta and posed on such a smooth variation. One with a Yoshizumi, 1968). The barograph described large amplitude has been known as "pumping" remarkably regular oscillation with the period of of the barometer (Tannehill, 1956). Fujita (1952) about 50min, which extended over half a day classified them into two groups, i.e., oscillatory and had a maximum double amplitude exceeding and non-oscillatory perturbations.
    [Show full text]