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An Independent Assessment of the Sinking of the MV DERBYSHIRE
SNAME Transactions, Vol. 106, 1998, pp. 59-103 An Independent Assessment of the Sinking of the MV DERBYSHIRE Douglas Faulkner, Fellow, Emeritus Professor of Naval Architecture, University of Glasgow, Scotland The author was appointed by the UK Department of Tranq~ort as a fellow Assessor with R.A. Williams during Lord Donaldson's Assessment (1995) of the loss of the OBO ship DERBYSHIRE and throughout the planning and conduct of the two final surveys of the wreck. This paper is drawn from the independ- ent report (b~udknel; 1998a) and may be considered complementary to those of the UK and EC Asses- sors (Williams and Torchio, 1998a and 1998b). The paper deals with the history and loss of the ship, in- cluding the concept developed in 1995 of 13 possible loss scenarios in a Jormal safety Risk Matrix" of probability and seriousness. It analyses abnormal wave effects on hatch cover collapse, on ship bending, and on flooding of bow spaces and no. 1 hold. The implosion-explosion mechanics during sinking is out- lined to explain the devastation of the wreck. The 1996 and 1997 underwater surveys are outlined as are the findings of.fact. Each of the final 14 loss scenarios is analysed in the light of the firm and circum- stantial survey evidence, plus many other factotw of service experience, analyses and experiments. The updated Risk Matrix speaks for itself and leads to the prime conclusions and major recommendations. Nomenclature ~ Register, 1987) which also depicts the oil fuel, fresh water and minimal ballast water distribution. Her estimated displacement as she approached Japan was about A = 194,000 te and hence 1. -
The Evolution of Earth Gravitational Models Used in Astrodynamics
JEROME R. VETTER THE EVOLUTION OF EARTH GRAVITATIONAL MODELS USED IN ASTRODYNAMICS Earth gravitational models derived from the earliest ground-based tracking systems used for Sputnik and the Transit Navy Navigation Satellite System have evolved to models that use data from the Joint United States-French Ocean Topography Experiment Satellite (Topex/Poseidon) and the Global Positioning System of satellites. This article summarizes the history of the tracking and instrumentation systems used, discusses the limitations and constraints of these systems, and reviews past and current techniques for estimating gravity and processing large batches of diverse data types. Current models continue to be improved; the latest model improvements and plans for future systems are discussed. Contemporary gravitational models used within the astrodynamics community are described, and their performance is compared numerically. The use of these models for solid Earth geophysics, space geophysics, oceanography, geology, and related Earth science disciplines becomes particularly attractive as the statistical confidence of the models improves and as the models are validated over certain spatial resolutions of the geodetic spectrum. INTRODUCTION Before the development of satellite technology, the Earth orbit. Of these, five were still orbiting the Earth techniques used to observe the Earth's gravitational field when the satellites of the Transit Navy Navigational Sat were restricted to terrestrial gravimetry. Measurements of ellite System (NNSS) were launched starting in 1960. The gravity were adequate only over sparse areas of the Sputniks were all launched into near-critical orbit incli world. Moreover, because gravity profiles over the nations of about 65°. (The critical inclination is defined oceans were inadequate, the gravity field could not be as that inclination, 1= 63 °26', where gravitational pertur meaningfully estimated. -
Yiddish and Relation to the German Dialects Bryan Witmore University of South Carolina
University of South Carolina Scholar Commons Theses and Dissertations 6-30-2016 Yiddish and Relation To The German Dialects Bryan Witmore University of South Carolina Follow this and additional works at: https://scholarcommons.sc.edu/etd Part of the German Language and Literature Commons Recommended Citation Witmore, B.(2016). Yiddish and Relation To The German Dialects. (Master's thesis). Retrieved from https://scholarcommons.sc.edu/ etd/3522 This Open Access Thesis is brought to you by Scholar Commons. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of Scholar Commons. For more information, please contact [email protected]. YIDDISH AND ITS RELATION TO THE GERMAN DIALECTS by Bryan Witmore Bachelor of Arts University of South Carolina, 2006 Submitted in Partial Fulfillment of the Requirements For the Degree of Master of Arts in German College of Arts and Sciences University of South Carolina 2016 Accepted by: Kurt Goblirsch, Director of Thesis Lara Ducate, Reader Lacy Ford, Senior Vice Provost and Dean of Graduate Studies © Copyright by Bryan Witmore, 2016 All Rights Reserved. ii ACKNOWLEDGEMENTS This thesis project was made possible in large part by the German program at the University of South Carolina. The technical assistance that propelled this project was contributed by the staff at the Ted Mimms Foreign Language Learning Center. My family was decisive in keeping me physically functional and emotionally buoyant through the writing process. Many thanks to you all. iii ABSTRACT In an attempt to balance the complex, multi-component nature of Yiddish with its more homogenous speech community – Ashekenazic Jews –Yiddishists have proposed definitions for the Yiddish language that cannot be considered linguistic in nature. -
Student Academic Learning Services Pounds Mass and Pounds Force
Student Academic Learning Services Page 1 of 3 Pounds Mass and Pounds Force One of the greatest sources of confusion in the Imperial (or U.S. Customary) system of measurement is that both mass and force are measured using the same unit, the pound. The differentiate between the two, we call one type of pound the pound-mass (lbm) and the other the pound-force (lbf). Distinguishing between the two, and knowing how to use them in calculations is very important in using and understanding the Imperial system. Definition of Mass The concept of mass is a little difficult to pin down, but basically you can think of the mass of an object as the amount of matter contain within it. In the S.I., mass is measured in kilograms. The kilogram is a fundamental unit of measure that does not come from any other unit of measure.1 Definition of the Pound-mass The pound mass (abbreviated as lbm or just lb) is also a fundamental unit within the Imperial system. It is equal to exactly 0.45359237 kilograms by definition. 1 lbm 0.45359237 kg Definition of Force≡ Force is an action exerted upon an object that causes it to accelerate. In the S.I., force is measured using Newtons. A Newton is defined as the force required to accelerate a 1 kg object at a rate of 1 m/s2. 1 N 1 kg m/s2 Definition of ≡the Pound∙ -force The pound-force (lbf) is defined a bit differently than the Newton. One pound-force is defined as the force required to accelerate an object with a mass of 1 pound-mass at a rate of 32.174 ft/s2. -
Vowel Change in English and German: a Comparative Analysis
Vowel change in English and German: a comparative analysis Miriam Calvo Fernández Degree in English Studies Academic Year: 2017/2018 Supervisor: Reinhard Bruno Stempel Department of English and German Philology and Translation Abstract English and German descend from the same parent language: West-Germanic, from which other languages, such as Dutch, Afrikaans, Flemish, or Frisian come as well. These would, therefore, be called “sister” languages, since they share a number of features in syntax, morphology or phonology, among others. The history of English and German as sister languages dates back to the Late antiquity, when they were dialects of a Proto-West-Germanic language. After their split, more than 1,400 years ago, they developed their own language systems, which were almost identical at their earlier stages. However, this is not the case anymore, as can be seen in their current vowel systems: the German vowel system is composed of 23 monophthongs and 8 diphthongs, while that of English has only 12 monophthongs and 8 diphthongs. The present paper analyses how the English and German vowels have gradually changed over time in an attempt to understand the differences and similarities found in their current vowel systems. In order to do so, I explain in detail the previous stages through which both English and German went, giving special attention to the vowel changes from a phonological perspective. Not only do I describe such processes, but I also contrast the paths both languages took, which is key to understand all the differences and similarities present in modern English and German. The analysis shows that one of the main reasons for the differences between modern German and English is to be found in all the languages English has come into contact with in the course of its history, which have exerted a significant influence on its vowel system, making it simpler than that of German. -
A Middle High German Primer, with Grammar, Notes, and Glossary
> 1053 MIDDLE HIGH GERMAN PRIMER WITH GRAMMAR, NOTES, AND GLOSSARY BY JOSEPH WRIGHT M.A., PH.D., D.C.L., LL.D., L1TT.D. FELLOW OF THE BRITISH ACADEMY CORPUS CHRISTI PROFESSOR OF COMPARATIVE PHILOLOGY IN THE UNIVERSITY OF OXFORD THIRD EDITION RE-WRITTEN AND ENLARGED AT THE CLARENDON PRESS 1917 OXFORD UNIVERSITY PRESS LONDON EDINBURGH GLASGOW NEW YORK TORONTO MELBOURNE BOMBAY HUMPHREY MILFORD PUBLISHER TO THE UNIVERSITY pr EXTRACTS FROM THE PREFACES TO THE FIRST AND SECOND EDITIONS THE present book has been written in the hope that it will serve as an elementary introduction to the larger German works on the subject from which I have appro- priated whatever seemed necessary for the purpose. In the grammar much aid has been derived from Paul's Mittelhochdeutsche Grammatik, second edition, Halle, 1884, and Weinhold's Mittelhochdeutsche Grammatik, second edition, Paderborn, 1883. The former work, besides con- taining by far the most complete syntax, is also the only Middle High German Grammar which is based on the present state of German Philology. ... I believe that the day is not far distant when English students will take a much more lively interest in the study of their own and the other Germanic languages (especially German and Old Norse) than has hitherto been the case. And if this little book should contribute anything towards furthering the cause, it will have amply fulfilled its purpose. LONDON : January, 1888. WHEN I wrote the preface to the first edition of this primer in 1888, I ventured to predict that the interest of English students in the subject would grow and develop as time went on, but I hardly expected that it would grow so much that a second edition of the book would be required within iv Preface to the Second Edition so short a period. -
What Is Fluid Mechanics?
What is Fluid Mechanics? A fluid is either a liquid or a gas. A fluid is a substance which deforms continuously under the application of a shear stress. A stress is defined as a force per unit area Next, what is mechanics? Mechanics is essentially the application of the laws of force and motion. Fluid statics or hydrostatics is the study of fluids at rest. The main equation required for this is Newton's second law for non-accelerating bodies, i.e. ∑ F = 0 . Fluid dynamics is the study of fluids in motion. The main equation required for this is Newton's second law for accelerating bodies, i.e. ∑ F = ma . Mass Density, ρ, is defined as the mass of substance per unit volume. ρ = mass/volume Specific Weight γ, is defined as the weight per unit volume γ = ρ g = weight/volume Relative Density or Specific Gravity (S.g or Gs) S.g (Gs) = ρsubstance / ρwater at 4oC Dynamic Viscosity, µ µ = τ / (du/dy) = (Force /Area)/ (Velocity/Distance) Kinematic Viscosity, v v = µ/ ρ Primary Dimensions In fluid mechanics there are only four primary dimensions from which all other dimensions can be derived: mass, length, time, and temperature. All other variables in fluid mechanics can be expressed in terms of {M}, {L}, {T} Quantity SI Unit Dimension Area m2 m2 L2 Volume m3 m3 L3 Velocity m/s ms-1 LT-1 Acceleration m/s2 ms-2 LT-2 -Angular velocity s-1 s-1 T-1 -Rotational speed N Force kg m/s2 kg ms-2 M LT-2 Joule J energy (or work) N m, kg m2/s2 kg m2s-2 ML2T-2 Watt W Power N m/s Nms-1 kg m2/s3 kg m2s-3 ML2T-3 Pascal P, pressure (or stress) N/m2, Nm-2 kg/m/s2 kg m-1s-2 ML-1T-2 Density kg/m3 kg m-3 ML-3 N/m3 Specific weight kg/m2/s2 kg m-2s-2 ML-2T-2 a ratio Relative density . -
Department of the Interior U.S. Geological Survey Two FORTRAN
Department of the Interior U.S. Geological Survey Two FORTRAN programs for the reduction of atmospheric data collected by aircraft along EDM survey lines by Elliot T. Endol Gene Y. Iwatsubo Lyn J. Topinka Open-File Report 85-279 This report is preliminary and has not been edited or reviewed for conformity with Geological Survey standards and nomenclature. Any use of trade names and trade marks in this publication is for descriptive purposes only and does not constitute endorsement by the U.S. Geological Survey. David A. Johnston Cascades Volcano Observatory 5400 MacArthur Blvd. Vancouver, Washington 98661 1985 Abstract The Cascades Volcano Observatory had a requirement for a computer program to reduce atmospheric data collected for electronic distance measurement surveys. Existing programs could not be easily adapted for this simple need. The program AVEINDEX.FOR described in this report fills this requirement. AVEINDEX.FOR, written in FORTRAN-77 standards, is modular in structure. The modular structure allows easy program modification. Twelve supporting subroutines and functions for AVEINDEX.FOR and one data entry program are also described. Program comments accompany each program and most subroutines. TABLE OF CONTENTS Page INTRODUCTION................................................... 1 PRIMARY ASSUMPTIONS OR APPROXIMATIONS.......................... 2 SPECIFIC EQUATIONS USED FOR CALCULATIONS....................... 4 MAIN PROGRAMS.................................................. 7 LISTING OF MAIN PROGRAMS AND SUBROUTINES...................... -
Preparation of Papers for AIAA Technical Conferences
Gravity Modeling for Variable Fidelity Environments Michael M. Madden* NASA, Hampton, VA, 23681 Aerospace simulations can model worlds, such as the Earth, with differing levels of fidel- ity. The simulation may represent the world as a plane, a sphere, an ellipsoid, or a high- order closed surface. The world may or may not rotate. The user may select lower fidelity models based on computational limits, a need for simplified analysis, or comparison to other data. However, the user will also wish to retain a close semblance of behavior to the real world. The effects of gravity on objects are an important component of modeling real-world behavior. Engineers generally equate the term gravity with the observed free-fall accelera- tion. However, free-fall acceleration is not equal to all observers. To observers on the sur- face of a rotating world, free-fall acceleration is the sum of gravitational attraction and the centrifugal acceleration due to the world’s rotation. On the other hand, free-fall accelera- tion equals gravitational attraction to an observer in inertial space. Surface-observed simu- lations (e.g. aircraft), which use non-rotating world models, may choose to model observed free fall acceleration as the “gravity” term; such a model actually combines gravitational at- traction with centrifugal acceleration due to the Earth’s rotation. However, this modeling choice invites confusion as one evolves the simulation to higher fidelity world models or adds inertial observers. Care must be taken to model gravity in concert with the world model to avoid denigrating the fidelity of modeling observed free fall. -
Mass Properties Measurement Handbook
SAWE PAPER No.2444 Index Category No. 3.0 Mass Properties Measurement Handbook By Richard Boynton and Kurt Wiener Space Electronics, Inc. 81 Fuller Way Berlin, Connecticut 06037 For presentation at the Annual Conference of the Society of Allied Weight Engineers Wichita, KS 18-20 May 1998 Permission to publish this paper, in full or in part, with full credit to author may be obtained by request to: S.A.W.E. Inc. The society is not responsible for statements or opinions in papers or discussions Table of Contents 1.0 Abstract .................................................................. 2 2.0 Stepsin Making a Mass Properties measurement .................................. 2 2.1 Definethe particularmass properties you need to measure and the required measurementaccuracy .............................................. 2 2.2 Choose the correcttype ofmeasuring instrument ............................ 2 2.3 Definethe coordinate system on the object to be used as the mass properties reference axes ............................................................ 2 2.4 Definethe position ofthe objecton themass properties measuring machine ....... 2 2.5 Determine the dimensional accuracy of theobject being measured .............. 2 2.6 Designthe fixturerequired to mount the object at a precise location relativeto the measuring instrument .............................................. 3 2.7 Verifythe position of theobject on the instrument. .......................... 3 2.8 Make the mass properties measurement ................................... 3 2.9 -
Online Companion to a Historical Phonology of English
A Historical Phonology of English Donka Minkova © Donka Minkova, 2014 Edinburgh University Press Ltd 22 George Square, Edinburgh EH8 9LF www.euppublishing.com Typeset in 10.5/12 Janson by Servis Filmsetting Ltd, Stockport, Cheshire, printed and bound in Great Britain by CPI Group (UK) Ltd, Croydon CR0 4YY A CIP record for this book is available from the British Library ISBN 978 0 7486 3467 5 (hardback) ISBN 978 0 7486 3468 2 (paperback) ISBN 978 0 7486 3469 9 (webready PDF) ISBN 978 0 7486 7755 9 (epub) The right of Donka Minkova to be identifi ed as author of this work has been asserted in accordance with the Copyright, Designs and Patents Act 1988. Contents Acknowledgements x List of abbreviations and symbols xii A note on the Companion to A Historical Phonology of English xv 1 Periods in the history of English 1 1.1 Periods in the history of English 2 1.2 Old English (450–1066) 2 1.3 Middle English (1066–1476) 9 1.4 Early Modern English (1476–1776) 15 1.5 English after 1776 17 1.6 The evidence for early pronunciation 20 2 The sounds of English 24 2.1 The consonants of PDE 24 2.1.1 Voicing 26 2.1.2 Place of articulation 27 2.1.3 Manner of articulation 29 2.1.4 Short and long consonants 31 2.2 The vowels of PDE 32 2.2.1 Short and long vowels 35 2.2.2 Complexity: monophthongs and diphthongs 37 2.3 The syllable: some basics 39 2.3.1 Syllable structure 39 2.3.2 Syllabifi cation 40 2.3.3 Syllable weight 43 2.4 Notes on vowel representation 45 2.5 Phonological change: some types and causes 46 3 Discovering the earliest links: Indo- European -
General Disclaimer One Or More of the Following Statements May Affect
General Disclaimer One or more of the Following Statements may affect this Document This document has been reproduced from the best copy furnished by the organizational source. It is being released in the interest of making available as much information as possible. This document may contain data, which exceeds the sheet parameters. It was furnished in this condition by the organizational source and is the best copy available. This document may contain tone-on-tone or color graphs, charts and/or pictures, which have been reproduced in black and white. This document is paginated as submitted by the original source. Portions of this document are not fully legible due to the historical nature of some of the material. However, it is the best reproduction available from the original submission. Produced by the NASA Center for Aerospace Information (CASI) ^I NASA Technical Paper 2147 0 The NASA Geodynamics Program: An Overview Geoud ynamics Program Office Office of Space Science and Applications I Washington, DC 20546 1983 Scientific and Technical Information Branch -11 - ---- -- r NASA Technical Paper 2147 The NASA Ge odynamics Program: An Overview %, N&SA — TY — A 14 1) Ttit bA.'-A G?.QjlMARICs L, BCGhltl: Ab GVjhV14w ( NdtiO Ual AQr0GdUtlCIj 41A U 5j;dC#j AdsiaistLatjC&j) UC AU7/Mf AUI CSCL 06G uncIds 1/46 L 44119 W Geodynamics Program Office nary 1983 - Nala-al k,fo ulcs and SP re a ^I FOREWORD The study of the solid earth and its gravity and magnetic fields has advancd significantly in the past 20 years. This advancement has been greatly assisted by the emergence of methods which use space and space- derived technology for observations of the earth unattainable bit other means.