The New Navy 1954–1959
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U.S. NAVAL RADIOLOGICAL History of DEFENSE LABORATORY
NAV1.940715.005 .. U.S. NAVAL RADIOLOGICAL History Of DEFENSE LABORATORY for the year 1961 SAN FRANCISCO CALIFORNIA TABLE OF CONTENTS -Chapter -Page I 1961 -- EXPANDED HORIZONS NRDL's Parent Organization. BuShips, Comes ofAge . 1 New Associate Scientuic Director , . , . , . 4 Strope Selected as DOD,OCDRandD Director. 4 Other Major Personnel Changes. , . 6 Organizationchart , . 7 Organizational Changes . + . 8 Mission, Tasks, Functions . e . 9 Tri-Service Induction Takes Place. I . , . 9 I1 TECHNICAL ACCOMPLISHMENTS (including Facilities and Equipment Acquired) Weapons Effects and Related Information . 11 Bio-Medical Research and Hazards Evaluation . 17 Shielding Studies . , 21 War Gaming Information, Simulator and Fallout Models . 9 22 Radiac Systems and Dosimetry . - . * . 24 Shelter Year , . , . 25 Disaster Control, Civil Defense and RadiologicalRecovery. v I . - . * - 26 Technical Bases for Operational Doctrine e I . 27 Operational Capability for Radiological Contamination Control. 29 Applications and Techniques. 31 I11 PUBLICATIONS . , . , . I . , . 34 IV AWARDS -- COMMENDATIONS -- HONORS * * * + * * - 36 V SEMINARS -- SYMPOSIA -- CONFERENCES Meetings at NRDL -- Meetings Eisewhere , . 43 VI TRAINING. *. , . 4; VI1 VISITORS. -., . 49 VI11 PUBLICITY. 53 IX MISCELLANEOUS, . , . 54 - 1- 355 PHOTOGRAPHS Subject Page L_ Welcome Aboard. Chief .. RADM R . K . James ............ 2 Another Milestone .. Exhibit for BuShips 21st Birthday ........ 3 Dr. E . R . Tompkins . Associate Scientific Director .......... 5 Tri-Service Induction ....................... -
OFFICE of the JUDGE ADVOCATE GENERAL § 5131. Bureaus
TITLE 10—ARMED FORCES § 5131 SEC. 2. Abolition of Certain Bureaus and Transfer of struck out items 5150 ‘‘Office of Naval Research: Chief, Functions.—The following bureaus, named in chapter appointment, term, emoluments; Assistant Chief; suc- 513 of title 10, United States Code, and the offices of the cession to duties’’, 5151 ‘‘Office of Naval Research: du- chiefs, deputy chiefs, and other officials of such bu- ties’’, 5152 ‘‘Office of Naval Research: appropriations; reaus are hereby abolished and all their functions are time limit’’, and 5153 ‘‘Naval Research Advisory Com- transferred to the Secretary of the Navy: mittee’’, and redesignated item 5155 as item 5150. (a) Bureau of Naval Weapons; 1980—Pub. L. 96–513, title V, §§ 503(8), 513(6), Dec. 12, (b) Bureau of Ships; 1980, 94 Stat. 2911, 2931, struck out items 5134 ‘‘Deputy (c) Bureau of Supplies and Accounts; and Bureau Chiefs: pay’’, 5139 ‘‘Bureau of Medicine and Sur- (d) Bureau of Yards and Docks. gery: Medical Service Corps, Chief’’, 5140 ‘‘Bureau of SEC. 3. Performance of Transferred Functions.—Subject Medicine and Surgery: Nurse Corps, Director’’, and 5143 to the provisions of sections 5012 and 5013, title 10, ‘‘Bureau of Naval Personnel: Assistant Chief of United States Code, the Secretary of the Navy may Women’’, and added item 5155. from time to time make such provisions as he shall Pub. L. 96–343, § 11(b), Sept. 8, 1980, 94 Stat. 1130, sub- deem appropriate authorizing the performance by any stituted ‘‘Chaplain Corps and’’ for ‘‘Bureau of Naval other officer, or by any office, agency, or employee, of Personnel:’’ in item 5142 and added item 5142a. -
On the Structure of Hurricane Daisy 1958
NATIONAL HURRICANE RESEARCH PROJECT REPORT NO. 48 On the Structure of Hurricane Daisy 1958 ^ 4 & U. S. DEPARTMENT OF COMMERCE Luther H. Hodges, Secretary WEATHER BUREAU F. W. Rolcheldorfoi, Chief NATIONAL HURRICANE RESEARCH PROJECT REPORT NO. 48 On the Structure of Hurricane Daisy (1958) by J6se A. Coltfn and Staff National Hurricane Research Project, Miami, Fla. Washington, D. C. October 1961 NATIONAL HURRICANE RESEARCH PROJECT REPORTS Reports by Weather Bureau units, contractors, and ccoperators working on the hurricane problem are preprinted in this series to facilitate immediate distribution of the information among the workers and other interested units. Aa this limited reproduction and distribution in this form do not constitute formal scientific publication, reference to a paper in the series should identify it as a preprinted report. Objectives and basic design of the NHRP. March 1956. No. 1. numerical weather prediction of hurricane motion. July 1956- No. 2. Supplement: Error analysis of prognostic 500-mb. maps made for numerical weather prediction of hurricane motion. March 1957. Rainfall associated with hurricanes. July 1956. No. 3. Some problems involved in the study of storm surges. December 1956. No. h. Survey of meteorological factors pertinent to reduction of loss of life and property in hurricane situations. No. 5. March 1937* A mean atmosphere for the West Indies area. May 1957. No. 6. An index of tide gages and tide gage records for the Atlantic and Gulf coasts of the United States, toy 1957. No. 7. No. 8. PartlT HurrlcaneVand the sea surface temperature field. Part II. The exchange of energy between the sea and the atmosphere in relation to hurricane behavior. -
P6.3 Using ERA40 in Cyclone Phase Space to Refine the Classification
P6.3 Using ERA40 in Cyclone Phase Space to Refine the Classification of Historical Tropical Storms Danielle Manning* and Robert Hart The Florida State University *Corresponding author email: [email protected] I. INTRODUCTION The goal of this study is to, when feasible Understanding of cyclone structural evolution within the ERA40 data, extend and refine the structural both during and beyond the tropical stage has increased characteristics of existing best-track cyclones. These tremendously over the past fifty years through various refinements may include the tropical or extratropical satellite-based, model-based, and analysis-based transition points in the lifecycle or the genesis point of classifications. This new knowledge has brought tropical cyclones that formed from cold-core origins. forward the reanalysis of historical storms in the context Finally, through a detailed examination of the full 45 of present understanding (Landsea et al. 2004) in order years, several cyclones were found of warm-core or to extend and revise the National Hurricane Center’s hybrid structure that may qualify for subtropical or (NHC) North Atlantic hurricane database (HURDAT; tropical status, but were not documented within the Neumann et al. 1993). This reanalysis is vital for the existing best-track archive. Case examples of all these filling of gaps within, and further improvement overall events are presented below, along with an evaluation of of the track and structural evolution of tropical cyclones. CPS intensity bias evolution over the ERA40 period. II. DATA AND METHODOLOGY Using ECMWF Reanalysis dataset (ERA40; Uppala et al. 2005), three parameters that classify a cyclone within a continuum of structure (warm to cold core, shallow to deep, and frontal to nonfrontal) can be calculated (Hart 2003). -
From the Sea to the Stars: a Chronicle of the U.S
From the Sea to the Stars i From the Sea to the Stars: A Chronicle of the U.S. Navy’s Space and Space-related Activities, 1944-2009 Sponsored by Deputy Assistant Secretary of the Navy (C3I and Space) Dr Gary A. Federici Edited by The Applied Research Laboratory The Pennsylvania State University Revised and updated edition, 2010 iii CONTENTS Illustrations ...................................................................................................................................................... xi Preface ............................................................................................................................................................ xiii Acknowledgments .......................................................................................................................................... xiv Introduction ...................................................................................................................................................... 1 CHAPTER 1 – THE NAVY GETS INVOLVED IN SPACE (1944-1961) ................................................................... 7 Early Navy Space Programs (1944-1958) ..................................................................................................... 9 The Space Probes ...................................................................................................................................... 9 Naval Research Laboratory's Space Probes ......................................................................................... 9 -
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. -
The Great Storm of 1893 and the Schooner Riverside
The Great Storm of 1893 and the Schooner Riverside David Michael VanZandt Kevin Scott Magee Director and Chief Archaeologist Co-Director Cleveland Underwater Explorers Inc. Cleveland Underwater Explorers Inc. 1226 Lakeland Avenue 4363 West 182nd Street Lakewood, OH 44107 Cleveland, Ohio 44135 The year 1893 was the third most energetic Atlantic hurricane season ever recorded in the United States. There were ten hurricanes and two tropical storms which devastated many coastal communities; however, the damage was not limited to the coastlines. The Great Lakes region was also affected by Hurricane No. 9, or the “North and South Carolina Hurricane.” This storm made landfall near Charleston, South Carolina, on 13 October 1893 and continued far inland, wreaking havoc along its path. Shipping on the Great Lakes was severely impacted and resulted in the sinking or strand- ing of at least 39 ships. One of the vessels sunk in the storm, the three-masted schooner Riverside, was recently discovered by the Cleveland Underwater Explorers (CLUE) on 6 October 2007. Its tragic loss with its entire crew of seven was typical of the storm’s effect on the people who made their living carrying cargo and passengers on the Great Lakes. Introduction hurricanes in 1893 are Hurricane No. 6, the “Sea Islands Hurricane,” and Hurricane No. 10, the “Chenière The year 1893 was a year of hurricanes. This Caminada Hurricane” (National Oceanic and Atlantic hurricane season was unusual not only in the Atmospheric Administration 2009e). These hurricanes number of storms but in their size and power. It was are named not only from their modern National Oceanic the third most energetic Atlantic hurricane season and Atmospheric Administration (NOAA) nomen- ever recorded (National Oceanic and Atmospheric clature but also from their historic names. -
On Quantitative Precipitation Forecasting
<\ ^ fc <?' <3> V U. S. DEPARTMENT OF COMMERCE Frederick H. Mueller, Secretary WEATHER BUREAU F. W. Reichelderfer, Chief NATIONAL HURRICANE RESEARCH PROJECT REPORT NO. 38 On Quantitative Precipitation Forecasting by C. S. Gilman, K. R. Peterson, C. W. Cochrane, and S. Molansky Hydrologic Services Division, U. S. Weather Bureau Washington, D. C. August 1960 NATIONAL HURRICANE RESEARCH PROJECT REPORTS Reports by Weather Bureau units, contractors, and cooperators working on the hurricane problem are pre-printed in this series to facilitate immediate distribution of the information among the workers and other interested units. As this limited reproduction and distribution in this.form do not constitute formal scientific publication, reference to a paper in the series should iden tify it as a pre-printed report. No. 1. Objectives and basic design of the NflRP. March 1956. No. 2. Numerical weather prediction of hurricane motion. July 1956. Supplement: Error analysis of prognostic 500-mb. maps made for numer ical weather prediction of hurricane motion. March 1957* No. 5. Rainfall associated with hurricanes. July 1956. No. k. Some problems involved in the study of.storm surges. December 1956. No. 5. Survey of meteorological factors pertinent to reduction of loss of life and property in hurricane situations. March 1957. No. 6. A mean atmosphere for the West Indies area. May 1957* No. 7* An index of tide gages and tide gage records for the Atlantic and Gulf coasts-of the United States. May 1957. No. 8. Part I. Hurricanes and the sea surface temperature field. Part II. The exchange of energy between the sea and the atmosphere in relation to hurricane behavior. -
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. -
Hurricanes and Hurricane Tides
CHAPTER 2 HURRICANES AND HURRICANE TIDES Gordon E* Dunn U. S. Weather Bureau Miami, Florida Most of the maximum tides of record between Cape Hatteras, N*C., and Brownsville, Tex., have been produced by tropioal cyclones, or, as they are generally known in the United States, hurricanes. Some of the highest tides of record northward along the coast from Cape Hatteras to Cape Cod have been produced by hurricanes* From tine to tine our "northeasters*, which are extra-tropical storms, may also cause millions of dollars of damage along the Atlantic coast between Miami, Fla., and Eaetport, He* The Atlantic hurricane is identical with the Pacific typhoon and the tropical cyclone of the Indian and South Pacific Oceans. The term "hurricane" is defined as a storm of tropical origin with a cyclonic wind circulation (counter-clockwise in the northern hemisphere) with winds of 75 nph or more. However, in popular terminology, any winds of 75 mph or more are often described as hurricane winds. FORMATION Tropical cyclones develop in essentially homogeneous warm moist tropical air with no fronts or temperature and moisture discontinuities. The exact nature of the physical processes involved in the formation of hurricanes is not definitely known* However, there appears to be a number of meteorological conditions essential for tropical storm forma- tion: fl) comparatively warm water 80-8l*F or higher; (2) a pre- existing wind or pressure perturbation; (3) some outside influence which will Intensify this disturbance, and (It) a type of wind flow in the high troposphere which will permit ready removal of the excess air and heat to other regions outside the hurricane area. -
Aviation Commands
Chapter 21 Aviation Commands In order of their establishment: Office in Charge of Aviation Director of Naval Aeronautics Director of Naval Aviation Capt. Washington I. Chambers 26 Sep 1910–17 Dec 1913 Capt. Mark L. Bristol 17 Dec 1913–4 Mar 1916 Capt. Noble E. Irwin 17 May 1917–May 1919 Capt. Thomas T. Craven May 1919–7 Mar 1921 Capt. William A. Moffett 7 Mar 1921–26 Jul 1921 The person in charge of aviation affairs for the Navy was initially designated as the officer to whom all correspondence on aviation should be referred. This position was a special duty assignment as Officer in Charge of Aviation. The position was identified by the title Director of Naval Aeronautics on 23 November 1914. It was discontinued on 4 March 1916 and reinstituted as Director of Naval Aviation on 7 March 1918. The title Director of Naval Aviation was replaced in July 1921 by the establishment of the Bureau of Aeronautics. Officer–in–Charge, Aviation, Headquarters Marine Corps Director of Marine Corps Aviation Deputy Chief of Staff (Air), Marine Corps Deputy Chief of Staff for Aviation, Marine Corps Deputy Commandant for Aviation, Marine Corps Maj. Alfred A. Cunningham 17 Nov 1919–12 Dec 1920 Lt. Col. Thomas C. Turner 13 Dec 1920–2 Mar 1925 Maj. Edward H. Brainard 3 Mar 1925–9 May 1929 Col. Thomas C. Turner 10 May 1929–28 Oct 1931 Maj. Roy S. Geiger 6 Nov 1931–29 May 1935 Col. Ross E. Rowell 30 May 1935–10 Mar 1939 Brig. Gen. Ralph J. Mitchell 11 Mar 1939–29 Mar 1943 Maj. -
THE WEATHER and CIRCULATION of SEPTEMBER 1957' Including a Discussion of Tropical Storm Activity EMANUEL M
SEPTEMBEB1967 MONTHLY WEATHER REVIEW 315 THE WEATHER AND CIRCULATION OF SEPTEMBER 1957' Including a Discussion of Tropical Storm Activity EMANUEL M. BALLENZWEIG Extended Forecast Section U. S. Weather Bureau Washington 25, D. C. 1. COMPARISONWITH THE SUMMER MONTHS and precipitation. Only 56 of 100 stations in the United States changed temperature by one class or less compared The weather and circulation of the past summer was with a normal of 72; similarly, fewer than normal stat8ions marked byextreme heterogeneity. The month of June (20 instead of 35) remained in the sameprecipitation class was characterized by a mean trough through the central (last line of table 1). Part of the associated reversal in part of the United States with ridges along each coast [ti]. weather regime(figs. 2B and 2C) can be interpreted in A marked reversal in circulat,ion characteristics took place terms of the changes in 700-mb. height anomalies from between June and July [5] as a pattern more typical of August to September (fig. 2A). summer emerged with a trough off each coast and a ridge over theGreat Plains. The sharp circulationreversal 2. MONTHLY MEAN CIRCULATION AND WEATHER from June to Julywas followed by strongpersistence from July to August at middle Mitudes of the Western Rem- Thefairly well-defined temperatureand precipitation isphere [4]. patterns for t,he month of September (Charts I-B, 11, and The circulation experienced yet another oscillation in its 111-B) can be related quite well to the monthly 700-mb. transitionfrom August to September. Theplanetary height and height anomaly patterns (fig. l), despite the wave train became relnarkably akin to that of June 1957 changes in these patterns whichtook place duringthe [6], with a trough again in themiddle of the United States month (section 3).Temperatures as much as 5' F.