Underwater Acoustics: a Brief Historical Overview Through World War II
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Marine Mammals Around Marine Renewable Energy Devices Using Active Sonar
TRACKING MARINE MAMMALS AROUND MARINE RENEWABLE ENERGY DEVICES USING ACTIVE SONAR GORDON HASTIE URN: 12D/328: 31 JULY 2013 This document was produced as part of the UK Department of Energy and Climate Change's offshore energy Strategic Environmental Assessment programme © Crown Copyright, all rights reserved. 1 SMRU Limited New Technology Centre North Haugh ST ANDREWS Fife KY16 9SR www.smru.co.uk Switch: +44 (0)1334 479100 Fax: +44 (0)1334 477878 Lead Scientist: Gordon Hastie Scientific QA: Carol Sparling Date: Wednesday, 31 July 2013 Report code: SMRUL-DEC-2012-002.v2 This report is to be cited as: Hastie, G.D. (2012). Tracking marine mammals around marine renewable energy devices using active sonar. SMRU Ltd report URN:12D/328 to the Department of Energy and Climate Change. September 2012 (unpublished). Approved by: Jared Wilson Operations Manager1 1 Photo credit (front page): R Shucksmith (www.rshucksmith.co.uk) 2 TABLE OF CONTENTS Table of Contents ----------------------------------------------------------------------------------------------------------------------------------------- 3 Table of Figures ------------------------------------------------------------------------------------------------------------------------------------------- 5 1. Non technical summary --------------------------------------------------------------------------------------------------------------------- 9 2. Introduction ----------------------------------------------------------------------------------------------------------------------------------- 12 -
It Has Often Been Said That Studying the Depths of the Sea Is Like Hovering In
It has often been said that studying the depths of the sea is like hovering in a balloon high above an unknown land which is hidden by clouds, for it is a peculiarity of oceanic research that direct observations of the abyss are impracticable. Instead of the complete picture which vision gives, we have to rely upon a patiently put together mosaic representation of the discoveries made from time to time by sinking instruments and appliances into the deep. (Murray & Hjort, 1912: 22) Figure 1: Portrait of the H.M.S. Challenger. Prologue: Simple Beginnings In 1872, the H.M.S Challenger began its five- year journey that would stretch across every ocean on the planet but the Arctic. Challenger was funded for a single reason; to examine the mysterious workings of the ocean below its surface, previously unexplored. Under steam power, it travelled over 100,000 km and compiled 50 volumes of data and observations on water depth, temperature and conditions, as well as collecting samples of the seafloor, water, and organisms. The devices used to collect this data, while primitive by today’s standards and somewhat imprecise, were effective at giving humanity its first in-depth look into the inner workings of the ocean. By lowering a measured rope attached to a 200 kg weight off the edge of the ship, scientists estimated the depth of the ocean. A single reading could take up to 80 minutes for the weight to reach bottom. Taking a depth measurement also necessitated that the Challenger stop moving, and accurate mapping required a precise knowledge of where the ship was in the world, using navigational tools such as sextants. -
Lagrangian Measurement of Subsurface Poleward Flow Between 38 Degrees N and 43 Degrees N Along the West Coast of the United States During Summer, 1993
CORE Metadata, citation and similar papers at core.ac.uk Provided by Calhoun, Institutional Archive of the Naval Postgraduate School Calhoun: The NPS Institutional Archive Faculty and Researcher Publications Faculty and Researcher Publications 1996-09-01 Lagrangian Measurement of subsurface poleward Flow between 38 degrees N and 43 degrees N along the West Coast of the United States during Summer, 1993 Collins, Curtis A. Geophysical Research Letters, Vol. 23, No. 18, pp. 2461-2464, September 1, 1996 http://hdl.handle.net/10945/45730 GEOPHYSICAL RESEARCH LETTERS, VOL. 23, NO. 18, PAGES 2461-2464, SEPTEMBER 1, 1996 Lagrangian Measurement of subsurface poleward Flow between 38øN and 43øN along the West Coast of the United States during Summer, 1993 CurtisA. Collins,Newell Garfield, Robert G. Paquette,and Everett Carter 1 Departmentof Oceanography,Naval Postgraduate School, Monterey, California Abstract. SubsurfaceLagrangian measurementsat about Undercurrentalong the coastsof California and Oregon. We 140 m showedthat the pathof the CaliforniaUndercurrent lay are using quasi-isobaric(float depth controlled primarily by next to the continentalslope betweenSan Francisco(37.80N) the pressureeffect on density)RAFOS floats (Rossby et al., and St. GeorgeReef (41.8øN) duringmid-summer 1993. The 1986) to make these measurements. A RAFOS float consists meanspeed along this 500 km pathwas 8 cms-1. Theflow at of a hydrophonemounted in a glasstube that is about2 meters this depth was not disturbedby upwelling centersat Point long. These hydrophonesreceive signals from three sound Reyesor CapeMendocino. Restfits also demonstratethe abil- sources that were moored 400 km offshore between 34.3øN and ity to acousticallytrack floats located well above the sound 40.4øN.The sound sources emit 15 W, 80 s signalsa•t 260 Hz channelaxis along the California coast. -
David Moretti Phd Thesis
ESTIMATING THE EFFECT OF MID-FREQUENCY ACTIVE SONAR ON THE POPULATION HEALTH OF BLAINVILLE'S BEAKED WHALES (MESOPLODON DENSIROSTRIS) IN THE TONGUE OF THE OCEAN David Moretti A Thesis Submitted for the Degree of PhD at the University of St Andrews 2019 Full metadata for this item is available in St Andrews Research Repository at: http://research-repository.st-andrews.ac.uk/ Please use this identifier to cite or link to this item: http://hdl.handle.net/10023/19250 This item is protected by original copyright Estimating the effect of mid-frequency active sonar on the population health of Blainville's beaked whales (Mesoplodon densirostris) in the Tongue of the Ocean David Moretti This thesis is submitted in partial fulfilment for the degree of Doctor of Philosophy (PhD) at the University of St Andrews March 2019 Abstract Passive acoustic methods were used to study the effect of mid-frequency active sonar (MFAS) on a population of Blainville’s beaked whales (Mesoplodon densirostris, Md) at the U.S. Navy Atlantic Undersea Test and Evaluation Centre (AUTEC), Bahamas. AUTEC contains an array of bottom-mounted hydrophones that can detect Md echolocation clicks. Methods to estimate abundance, the risk of behavioural disruption, and the population level effect of repeated MFAS exposure are presented. A passive acoustic abundance estimation method, a parametric equation that predicts the probability of foraging dive disruption as a function of MFAS received level and an Md bioenergetics model were developed. The effect of changes in energy flow on the demographic characteristics of an Md population were explored. Passive acoustic data from AUTEC were used to estimate the behavioural disturbance resulting from sonar operations; combined with the bioenergetic model, this suggested that the effect of sonar operations could cause an increase in a female’s age at maturity, a longer inter-calf-interval, calf survival rate and probability of giving birth that could in turn result in a declining population. -
A Brief History of Nuclear Astrophysics
A BRIEF HISTORY OF NUCLEAR ASTROPHYSICS PART I THE ENERGY OF THE SUN AND STARS Nikos Prantzos Institut d’Astrophysique de Paris Stellar Origin of Energy the Elements Nuclear Astrophysics Astronomy Nuclear Physics Thermodynamics: the energy of the Sun and the age of the Earth 1847 : Robert Julius von Mayer Sun heated by fall of meteors 1854 : Hermann von Helmholtz Gravitational energy of Kant’s contracting protosolar nebula of gas and dust turns into kinetic energy Timescale ~ EGrav/LSun ~ 30 My 1850s : William Thompson (Lord Kelvin) Sun heated at formation from meteorite fall, now « an incadescent liquid mass » cooling Age 10 – 100 My 1859: Charles Darwin Origin of species : Rate of erosion of the Weald valley is 1 inch/century or 22 miles wild (X 1100 feet high) in 300 My Such large Earth ages also required by geologists, like Charles Lyell A gaseous, contracting and heating Sun 푀⊙ Mean solar density : ~1.35 g/cc Sun liquid Incompressible = 4 3 푅 3 ⊙ 1870s: J. Homer Lane ; 1880s :August Ritter : Sun gaseous Compressible As it shrinks, it releases gravitational energy AND it gets hotter Earth Mayer – Kelvin - Helmholtz Helmholtz - Ritter A gaseous, contracting and heating Sun 푀⊙ Mean solar density : ~1.35 g/cc Sun liquid Incompressible = 4 3 푅 3 ⊙ 1870s: J. Homer Lane ; 1880s :August Ritter : Sun gaseous Compressible As it shrinks, it releases gravitational energy AND it gets hotter Earth Mayer – Kelvin - Helmholtz Helmholtz - Ritter A gaseous, contracting and heating Sun 푀⊙ Mean solar density : ~1.35 g/cc Sun liquid Incompressible = 4 3 푅 3 ⊙ 1870s: J. -
University Microfilms, Inc., Ann Arbor, Michigan the SYNTHESIS of POINT DATA
This dissertation has been microfilmed exactly as received 68-16,949 JOHNSON, Rockne Hart, 1930- THE SYNTHESIS OF POINT DATA AND PATH DATA IN ESTIMATING SOFAR SPEED. University of Hawaii, Ph.D., 1968 Geophysics University Microfilms, Inc., Ann Arbor, Michigan THE SYNTHESIS OF POINT DATA AND PATH DATA IN ESTIMATING SOFAR SPEED A DISSERTATION SUBMITTED TO THE GRADUATE DIVISION OF THE UNIVERSITY OF HAWAII IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY IN GEOSCIENCES June 1968 By Rockne Hart Johnson Dissertation Committee: William M. Adams, Chairman Doak C. Cox George H. Sutton George P. Woollard Klaus Wyrtki ii P~F~E Geophysical interest in the deep ocean sound (sofar) channel centers on its use as a tool for the detection and location of remote events. Its potential application to oceanography may lie in the monitoring of variations of physical properties averaged over long paths by sofar travel-time measurements. As the accuracy of computed event locations is generally dependent on the accuracy of travel-time calculations, the spatial and temporal variation of sofar speed is a matter of fundamental interest. The author's interest in this problem has grown out of a practical need for such information for application to the problem of locating the sources of earthquake I waves and submarine volcanic sounds. Although an exten sive body of sound-speed data is available from hydrographic casts, considerably more precise measurements can be made of explosion travel times over long paths. This dissertation develops a novel procedure for analytically combining these two types of data to produce a functional description of the spatial variation of safar speed. -
OCEANS ´09 IEEE Bremen
11-14 May Bremen Germany Final Program OCEANS ´09 IEEE Bremen Balancing technology with future needs May 11th – 14th 2009 in Bremen, Germany Contents Welcome from the General Chair 2 Welcome 3 Useful Adresses & Phone Numbers 4 Conference Information 6 Social Events 9 Tourism Information 10 Plenary Session 12 Tutorials 15 Technical Program 24 Student Poster Program 54 Exhibitor Booth List 57 Exhibitor Profiles 63 Exhibit Floor Plan 94 Congress Center Bremen 96 OCEANS ´09 IEEE Bremen 1 Welcome from the General Chair WELCOME FROM THE GENERAL CHAIR In the Earth system the ocean plays an important role through its intensive interactions with the atmosphere, cryo- sphere, lithosphere, and biosphere. Energy and material are continually exchanged at the interfaces between water and air, ice, rocks, and sediments. In addition to the physical and chemical processes, biological processes play a significant role. Vast areas of the ocean remain unexplored. Investigation of the surface ocean is carried out by satellites. All other observations and measurements have to be carried out in-situ using research vessels and spe- cial instruments. Ocean observation requires the use of special technologies such as remotely operated vehicles (ROVs), autonomous underwater vehicles (AUVs), towed camera systems etc. Seismic methods provide the foundation for mapping the bottom topography and sedimentary structures. We cordially welcome you to the international OCEANS ’09 conference and exhibition, to the world’s leading conference and exhibition in ocean science, engineering, technology and management. OCEANS conferences have become one of the largest professional meetings and expositions devoted to ocean sciences, technology, policy, engineering and education. -
On Ocean Waveguide Acoustics
BOOKREVIEW ___________________________________________________ GEORGE V. FRISK ON OCEAN WAVEGUIDE ACOUSTICS acoustic waves with multilayered media is also an ac ACOUSTIC WAVEGUIDES: APPLICATIONS TO OCEANIC SCIENCE tive area of research in underwater acoustics. By C. Allen Boyles, Principal Professional Staff, In recent years, the inverse problem of determining The Johns Hopkins University Applied Physics Laboratory oceanographic properties from acoustic measurements Published by John Wiley & Son, New York, 1984. 321 pp. $46.95 has become increasingly important and has given rise to the term "acoustical oceanography," a variant of "ocean acoustics" that emphasizes the oceanograph ic implications of acoustic experiments. A major de The field of ocean acoustics is an active area of the velopment in this area is time-of-flight acoustic oretical and experimental research, with a continual tomography in which front and eddy intensity and ly expanding body of literature in research journals variability over hundreds of kilometers are measured and textbooks. Boyles' book is a welcome addition to acoustically. In ocean-bottom acoustics, direct inverse the literature and provides a useful text for both stu methods are being developed that utilize some mea dents and practitioners in the field. surement of the acoustic field, such as the plane wave Although electromagnetic waves are strongly ab reflection coefficient of the bottom, as direct input to sorbed by water, acoustic waves can, under the prop algorithms for determining the acoustic properties of er conditions, propagate over hundreds, even thou the bottom. This approach is to be contrasted with sands, of miles through the ocean. As a result, sound conventional techniques in which forward models for waves and sonar assume the major role in the ocean computing the acoustic field are run for different bot that electromagnetic waves and radar play in the at tom properties until best fits to the data are obtained. -
Overview of the Impacts of Anthropogenic Underwater Sound in the Marine Environment
Overview of the impacts of anthropogenic underwater sound in the marine environment Biodiversity Series 2009 Overview of the impacts of anthropogenic underwater sound in the marine environment OSPAR Convention Convention OSPAR The Convention for the Protection of the La Convention pour la protection du milieu Marine Environment of the North-East Atlantic marin de l'Atlantique du Nord-Est, dite (the “OSPAR Convention”) was opened for Convention OSPAR, a été ouverte à la signature at the Ministerial Meeting of the signature à la réunion ministérielle des former Oslo and Paris Commissions in Paris anciennes Commissions d'Oslo et de Paris, on 22 September 1992. The Convention à Paris le 22 septembre 1992. La Convention entered into force on 25 March 1998. It has est entrée en vigueur le 25 mars 1998. been ratified by Belgium, Denmark, Finland, La Convention a été ratifiée par l'Allemagne, France, Germany, Iceland, Ireland, la Belgique, le Danemark, la Finlande, Luxembourg, Netherlands, Norway, Portugal, la France, l’Irlande, l’Islande, le Luxembourg, Sweden, Switzerland and the United Kingdom la Norvège, les Pays-Bas, le Portugal, and approved by the European Community le Royaume-Uni de Grande Bretagne and Spain. et d’Irlande du Nord, la Suède et la Suisse et approuvée par la Communauté européenne et l’Espagne. 2 OSPAR Commission, 2009 Acknowledgements Author list (in alphabetical order) Thomas Götz Scottish Oceans Institute, East Sands University of St Andrews St Andrews, Fife KY16 8LB [email protected] Module 2, 8 Gordon Hastie SMRU Limited New Technology Centre North Haugh St Andrews, Fife KY16 9SR [email protected] Module 2, 8 Leila T. -
Cetacean Population Density Estimation from Single Fixed Sensors Using Passive Acoustics
Cetacean population density estimation from single fixed sensors using passive acoustics Elizabeth T. Ku¨sela) and David K. Mellinger Cooperative Institute for Marine Resources Studies (CIMRS), Oregon State University, Hatfield Marine Science Center, Newport, Oregon 97365 Len Thomas Centre for Research into Ecological and Environmental Modelling, University of St. Andrews, St. Andrews KY16 9LZ, Scotland Tiago A. Marques Centro de Estatı´stica e Aplicac¸o˜es da Universidade de Lisboa, Campo Grande, 1749-016 Lisboa, Portugal David Moretti and Jessica Ward Naval Undersea Warfare Center Division, Newport, Rhode Island 02841 (Received 17 December 2010; revised 18 March 2011; accepted 30 March 2011) Passive acoustic methods are increasingly being used to estimate animal population density. Most density estimation methods are based on estimates of the probability of detecting calls as functions of distance. Typically these are obtained using receivers capable of localizing calls or from studies of tagged animals. However, both approaches are expensive to implement. The approach described here uses a MonteCarlo model to estimate the probability of detecting calls from single sensors. The passive sonar equation is used to predict signal-to-noise ratios (SNRs) of received clicks, which are then combined with a detector characterization that predicts probability of detection as a func- tion of SNR. Input distributions for source level, beam pattern, and whale depth are obtained from the literature. Acoustic propagation modeling is used to estimate transmission loss. Other inputs for density estimation are call rate, obtained from the literature, and false positive rate, obtained from manual analysis of a data sample. The method is applied to estimate density of Blainville’s beaked whales over a 6-day period around a single hydrophone located in the Tongue of the Ocean, Baha- mas. -
Acoustic Cymbal Transducers-Design, Hydrostatic Pressure Compensation, and Acoustic Performance
Calhoun: The NPS Institutional Archive DSpace Repository Theses and Dissertations 1. Thesis and Dissertation Collection, all items 2004-03 Acoustic cymbal transducers-design, hydrostatic pressure compensation, and acoustic performance Jenne, Kirk E. Monterey, California. Naval Postgraduate School http://hdl.handle.net/10945/1670 Downloaded from NPS Archive: Calhoun NAVAL POSTGRADUATE SCHOOL MONTEREY, CALIFORNIA THESIS ACOUSTIC CYMBAL TRANSDUCERS – DESIGN, HYDROSTATIC PRESSURE COMPENSATION, AND ACOUSTIC PERFORMANCE by Kirk E. Jenne March 2004 Thesis Advisor: Thomas R. Howarth Thesis Co-Advisor: Dehua Huang Approved for public release; distribution 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 March 2004 Master’s Thesis 4. TITLE AND SUBTITLE: Acoustic Cymbal Transducers – Design, 5. FUNDING NUMBERS Pressure Compensation, and Acoustic Performance 6. AUTHOR(S) Kirk E. Jenne 7. PERFORMING ORGANIZATION NAME(S) AND ADDRESS(ES) 8. PERFORMING Naval Postgraduate School ORGANIZATION REPORT Monterey, CA 93943-5000 NUMBER 9. -
ARIE SKLODOWSKA CURIE Opened up the Science of Radioactivity
ARIE SKLODOWSKA CURIE opened up the science of radioactivity. She is best known as the discoverer of the radioactive elements polonium and radium and as the first person to win two Nobel prizes. For scientists and the public, her radium was a key to a basic change in our understanding of matter and energy. Her work not only influenced the development of fundamental science but also ushered in a new era in medical research and treatment. This file contains most of the text of the Web exhibit “Marie Curie and the Science of Radioactivity” at http://www.aip.org/history/curie/contents.htm. You must visit the Web exhibit to explore hyperlinks within the exhibit and to other exhibits. Material in this document is copyright © American Institute of Physics and Naomi Pasachoff and is based on the book Marie Curie and the Science of Radioactivity by Naomi Pasachoff, Oxford University Press, copyright © 1996 by Naomi Pasachoff. Site created 2000, revised May 2005 http://www.aip.org/history/curie/contents.htm Page 1 of 79 Table of Contents Polish Girlhood (1867-1891) 3 Nation and Family 3 The Floating University 6 The Governess 6 The Periodic Table of Elements 10 Dmitri Ivanovich Mendeleev (1834-1907) 10 Elements and Their Properties 10 Classifying the Elements 12 A Student in Paris (1891-1897) 13 Years of Study 13 Love and Marriage 15 Working Wife and Mother 18 Work and Family 20 Pierre Curie (1859-1906) 21 Radioactivity: The Unstable Nucleus and its Uses 23 Uses of Radioactivity 25 Radium and Radioactivity 26 On a New, Strongly Radio-active Substance